1980 - National Institute of Oceanography
1980 - National Institute of Oceanography
1980 - National Institute of Oceanography
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NATIONAL INSTITUTE OF OCEANOGRAPHY<br />
DONA PAULA GOA<br />
INDIA
The <strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong> (NIO) came into<br />
existence in 1966. The <strong>Institute</strong> besides having its Headquarters<br />
in Dona Paula, Goa, has three Regional Centres in Cochin,<br />
Bombay and Waltair.<br />
The <strong>Institute</strong> has identified 8 major priority areas for Research<br />
& Development with the object <strong>of</strong> utilizing the Sea and its<br />
resources for the benefit <strong>of</strong> our people and to develop technology<br />
to be utilized by the users <strong>of</strong> the Sea. The major R & D areas are:<br />
1. Food from the Sea<br />
2. Minerals from the Sea<br />
3. Energy from the Sea<br />
4. Drugs from the Sea<br />
5. Coastal Zone Management<br />
6. Protection <strong>of</strong> Marine Environment from Pollution<br />
7. Marine Instrumentation<br />
8. Ocean Engineering<br />
The <strong>Institute</strong> is also aiming at developing self sufficiency in<br />
ocean technology and be the focal point <strong>of</strong> oceanographic Data and<br />
Information pertaining to the Indian Ocean region.<br />
Main building <strong>of</strong> the <strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong> at Dona Paula, Goa
ANNUAL REPORT<br />
<strong>1980</strong><br />
16<br />
NATIONAL INSTITUTE OF OCEANOGRAPHY<br />
(Council <strong>of</strong> Scientific & Industrial Research)<br />
DONA PAULA-403 004<br />
GOA, INDIA
CONTENTS<br />
Page No.<br />
1. Director's Report 1<br />
2. Major Scientific Highlights 5<br />
3. Research Activities<br />
3.0 Oceanographic Cruises 9<br />
3.1 Physical <strong>Oceanography</strong> 19<br />
3.2 Chemical <strong>Oceanography</strong> 27<br />
3.3 Geological <strong>Oceanography</strong> 37<br />
3.4 Biological <strong>Oceanography</strong> 45<br />
3.5 Ocean Engineering 57<br />
3.6 Marine Instrumentation 61<br />
3.7 Planning, Publication, Information & Data 65<br />
3.8 Regional Centres 71<br />
3.9 Sponsored Projects 83<br />
3.10 International Projects 89<br />
4. Infrastructure Services 91<br />
5. Administrative Set-up<br />
5.1 Cruise Planning and Programme Priorities<br />
Committee for R.V. Gaveshani 95<br />
5.2 Research Advisory Council 96<br />
5.3 Executive Committee 97<br />
54 Finance and Building Committee 98<br />
5.5 R.V. Gaveshani Committee 99<br />
5.6 Policy Planning Committee 99<br />
5.7 Stores and Equipment Committee 99<br />
5.8 Grievance Committee 100<br />
5.9 Staff Quarters/Hostel Allotment Committee 100<br />
5.10 Budget 100<br />
5.11 Scientific and Technical Staff 101<br />
6. Visitors 105<br />
7. Colloquia 108<br />
8. Awards, honours and membership <strong>of</strong> various committees 110<br />
9. Deputations 113<br />
10. Meetings, exhibitions, seminars, symposia and special lectures 115<br />
11. Radio Talks 122<br />
12. Publications<br />
12.1 Scientific Papers 123<br />
12 2 Popular Articles and Book Reviews 129<br />
12.3 Technical Reports 131<br />
12.4 Sponsored Project Reports 131
1<br />
Director's Report<br />
The year marks the completion <strong>of</strong> 15 years <strong>of</strong> R & D activities by the <strong>Institute</strong>,<br />
during which period it has developed competence in practically all fields <strong>of</strong> oceanography<br />
and is now in a position to provide its services to the nation in the fields <strong>of</strong><br />
exploration and exploitation <strong>of</strong> the vast, yet inadequately tapped resources <strong>of</strong> the<br />
seas around India.<br />
During the year, R.V. Gaveshani had spent 239 days at sea on 19 cruises in<br />
the Arabian Sea and Bay <strong>of</strong> Bengal and worked at 645 stations. The ship, for the first<br />
time, paid a goodwill visit to a foreign port at Penang. Malaysia in January, <strong>1980</strong>.<br />
A large volume <strong>of</strong> information was collected during these cruises on the physical,<br />
chemical, geological and geophysical aspects and on the living and non-living resources<br />
as well as on environmental conditions <strong>of</strong> the seas around India. The knowledge thus<br />
gained is being utilised in different ways as a major input to the research and development<br />
programme <strong>of</strong> the <strong>Institute</strong> which is comprised <strong>of</strong> 25 projects. Work on<br />
these projects has been carried out from the headquarters by the physical, chemical,<br />
geological-geophysical and biological oceanography, marine instrumentation and ocean<br />
engineering divisions. These were assisted by the planning and data division and<br />
three regional centres <strong>of</strong> NIO at Cochin. Bombay and Waltair.<br />
A. R and D Projects<br />
Much impetus was given to physical oceanography by the launching <strong>of</strong> an<br />
oceanographic and meteorological data buoy. This buoy was moored from R.V.<br />
Gaveshani <strong>of</strong>f Goa in the Arabian Sea at a water depth <strong>of</strong> about 100 m. All the<br />
probes installed on the buoy worked satisfactorily.<br />
Studies on chemical data collected from the seas around India revealed some<br />
nteresting features on the relative fertility <strong>of</strong> the Andaman Sea. Biochemical investigations<br />
on marine organisms showed that certain species possess antifertility and<br />
antibiotic properties. Pollution studies along the oil tanker routes in the Arabian Sea<br />
and Bay <strong>of</strong> Bengal revealed the presence <strong>of</strong> about 3700 and 1100 tonnes <strong>of</strong> floating tar<br />
balls respectively, while the petroleum hydrocarbons in the upper 20 m <strong>of</strong> the two<br />
seas was estimated to be several million tonnes. A new multidisciplinary project<br />
on studies <strong>of</strong> the estuarine regions <strong>of</strong> major rivers <strong>of</strong> India was initiated.<br />
•
Under the geological and geophysical programme, the survey <strong>of</strong> the entire<br />
western continental shelf has been completed. This has not only provided some<br />
basic information on geomorphology, sediment distribution and surficial geology <strong>of</strong><br />
the area but has also led to the demarcation <strong>of</strong> areas <strong>of</strong> economic interest potentially<br />
important from the point <strong>of</strong> view <strong>of</strong> future exploitation.<br />
As a part <strong>of</strong> the programme on <strong>of</strong>fshore mineral exploration, the <strong>Institute</strong> has developed<br />
the methodology and techniques for the exploration <strong>of</strong> shore deposits <strong>of</strong> heavy<br />
minerals.<br />
The biology programme <strong>of</strong> the <strong>Institute</strong> include an intensive survey <strong>of</strong> seaweed<br />
resources along the west coast and the location <strong>of</strong> areas <strong>of</strong> high concentration <strong>of</strong> economically<br />
important seaweeds, demarcation <strong>of</strong> productive areas in the Arabian Sea and Bay <strong>of</strong><br />
Bengal and the investigations on benthos and their relationship with demersal fisheries.<br />
In the aquaculture project, modified techniques were employed for the culture <strong>of</strong><br />
shell fish, shrimp and Artemia. The Artemia is in great demand as food in the<br />
aquaculture experiments and the <strong>Institute</strong> has located new resources <strong>of</strong> Artemia and<br />
has also cultured Anemia on a mass scale in the salt pans <strong>of</strong> Gujarat.<br />
A new project on the "energy from the sea" was started and status reports<br />
on the energy from ocean thermal energy conversion (OTEC), waves, tides, salinity<br />
and from marine biomass conversion are being prepared. The design <strong>of</strong> a laboratory<br />
model <strong>of</strong> OTEC plant with 200 watt capacity is ready for fabrication. Reports on<br />
methods developed for wave hindcasting and storm surges were also prepared.<br />
Efforts to develop some <strong>of</strong> the oceanographic instruments in the <strong>Institute</strong> were<br />
intensified and design and fabrication <strong>of</strong> 'sea probes' such as CTD system, buoy<br />
telemetry system and a shallow water echosounder were completed and successfully<br />
tested. A pr<strong>of</strong>ile current meter was also designed and fabricated.<br />
The Cochin Regional Centre <strong>of</strong> NIO has gathered considerable information<br />
on the living resources <strong>of</strong> certain regions <strong>of</strong> the Indian Ocean while the Bombay<br />
Centre continued to work on the protection <strong>of</strong> marine environment and monitoring<br />
<strong>of</strong> pollutants along the Maharashtra and Gujarat coasts. Baseline water quality<br />
analysis <strong>of</strong> the river Narmada in Gujarat and a comparative study on the behaviour<br />
<strong>of</strong> some metals in polluted and unpolluted waters were completed during the year.<br />
The Waltair Centre made a steady progress in oceanographic work <strong>of</strong>f Waltair and<br />
nearby areas and studied the crustal structure and basement tectonics <strong>of</strong> the Bay <strong>of</strong><br />
Bengal.<br />
B. Sponsored Projects<br />
During the year, the <strong>Institute</strong> has fully utilized the expertise and available<br />
indigenous technology and has provided services and support to various public and<br />
private sector undertakings through as many as 26 sponsored projects on areas such
as development <strong>of</strong> <strong>of</strong>fshore oilfields, pollution control, coastal development, and<br />
resources survey at a total cost <strong>of</strong> Rs 36 lakhs (Rs 3 6 million) These projects<br />
were <strong>of</strong> direct interest to the user community<br />
C. Services<br />
Planning, Publication and Information Sections <strong>of</strong> the <strong>Institute</strong> have done<br />
commendable work by releasing regular publications in time. An Indian <strong>National</strong><br />
Directory <strong>of</strong> Marine Research Projects was compiled and released. The Indian<br />
<strong>National</strong> Oceanographic Data Centre acquired and stored data on standard formats<br />
pertaining to more than one thousand stations. The statewise atlases covering hydrographic,<br />
current and biological date for three Indian states (Maharashtra, Karnataka<br />
and Tamil Nadu) were also completed.<br />
Under the 'computer s<strong>of</strong>tware services' several programmes were developed<br />
for processing various oceanographic data and information. The computer facility was<br />
also made available to various public/private organizations and educational institutions.<br />
More than 850 books, 720 technical reports and 10 new journals were added to the<br />
library. The NIO library also received a valuable personal collection from Pr<strong>of</strong><br />
E C Lafond as a gift to the <strong>Institute</strong>.<br />
Photography drawing, printing, binding and xeroxing groups have rendered<br />
valuable services to various Divisions. Similarly, workshop electroplating and prototype<br />
groups have continued to give their full support. The maintenance and servicing group<br />
did the needful for the maintenance <strong>of</strong> both laboratory and shipboard equipment<br />
Several new instruments (systems) were acquired and installed to enhance the<br />
working capability <strong>of</strong> the <strong>Institute</strong>. Among these the boomerang grab, programmable<br />
automatic scintillation counter coulter counter double beam atomic absorption spectropholometer,<br />
ATP meter, are worth mentioning.<br />
D. Miscellaneous<br />
During the year 130 research papers and popular articles were published in<br />
standard national and international journals besides many technical reports. A<br />
number <strong>of</strong> colloquia were organised and more than 3,000 persons with a scientific interest<br />
visited the <strong>Institute</strong>. The visit <strong>of</strong> Pr<strong>of</strong> Nurul Hasan, Vice President <strong>of</strong> CSIR<br />
was most stimulating and generated a lot <strong>of</strong> interest among the scientific staff<br />
The <strong>Institute</strong> hosted an international seminar on 'India and the East African,<br />
Littoral, Hinterland and Island States' - Areas <strong>of</strong> Co-operation in January <strong>1980</strong>. This<br />
seminar was co-sponsored by the Indian Council for Cultural Relations the Centre <strong>of</strong><br />
East African Studies <strong>of</strong> Bombay University and the <strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong>.<br />
About 50 scientist and educationists from India and African countries participated<br />
in the Seminar.
An all India seminar on 'Protection and Control <strong>of</strong> Coastal Erosion in India',<br />
was organised in May <strong>1980</strong> in which more than 60 papers were presented. A manual<br />
on Protection and Control <strong>of</strong> Coastal Erosion in India was released on this occasion.<br />
A national workshop on 'Energy from the Sea' was held in December, <strong>1980</strong>.<br />
About 75 delegates (engineers, technologists and scientists) from different organizations<br />
in the country participated in this workshop.<br />
The year was marked by the participation <strong>of</strong> many scientists <strong>of</strong> the <strong>Institute</strong><br />
to several national and international seminars, workshops and symposia.<br />
Director.<br />
<strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong>
2<br />
Major Scientific Highlights<br />
• R. V. Gaveshani carried out 35,000 line kilometres <strong>of</strong> oceanographic survey<br />
in the seas around India and collected a large amount <strong>of</strong> oceanographic information-<br />
The ship paid a goodwill visit <strong>of</strong> 4 days to Penang (Malaysia). While at Penang, the<br />
ship was visited by a large number <strong>of</strong> local dignitaries and scientific personnel who were<br />
very appreciative <strong>of</strong> the progress made by India in the field <strong>of</strong> marine science.<br />
• Results from MONEX-79 programme indicate that in spite <strong>of</strong> the increase<br />
in sea surface temperature by about 1°C and decrease in the thickness <strong>of</strong> the mixed layer<br />
by about 10 metres, the cyclone neat potential shows an increase from May to June<br />
(1979). Transformation <strong>of</strong> the thermodynamic energy suggests that the energy due<br />
to contraction <strong>of</strong> mixing is important in understanding the watermass structure.<br />
• Oceanographic data collected from the Andaman Sea revealed that an annual<br />
evaporation rate <strong>of</strong> about 137 cm over the region and the vertical heat transport were<br />
confined to 20 m <strong>of</strong> water where a strong halocline prevented the heat transfer to<br />
greater depth. These findings have an important bearing on the moisture transfer<br />
and atmospheric circulation in the area. In the Andaman Sea, Persian Gulf water<br />
was identified in the depth range <strong>of</strong> 200-500m with a characteristic high salinity,<br />
temperature and deltat. Below this and in the depth range <strong>of</strong> 500-900 m the water<br />
<strong>of</strong> Red Sea origin seems to be present. In the northern part <strong>of</strong> the Andaman Sea,<br />
mixed layer with a thickness <strong>of</strong> about 75 metre was identified.<br />
• Hydrochemical data <strong>of</strong>f the west coast indicated the presence <strong>of</strong> two oxygen<br />
minima associated with two phosphate maxima at a depth <strong>of</strong> about 300 and 1000 m.<br />
• Pollution surveys along the oil tanker routes in the Arabian Sea and in the<br />
southern Bay <strong>of</strong> Bengal from south <strong>of</strong> Sri Lanka to the head <strong>of</strong> the Malacca<br />
Strait showed an abundance <strong>of</strong> oil slicks amounting to nearly 3700 tonnes and 1100<br />
tonnes <strong>of</strong> floating tar balls in the Arabian Sea and Bay <strong>of</strong> Bengal respectively.<br />
• The effect <strong>of</strong> three heavy metals (copper, cadmium and zinc) on two copepod<br />
species showed that copper is a more toxic metal than the others.<br />
• A total magnetic intensity map <strong>of</strong> the northern part <strong>of</strong> Konkan coast was<br />
prepared on a 100 gamma interval which showed a N-S trend with a number <strong>of</strong><br />
closures. The conspicuous feature <strong>of</strong> the map is the two major NNW-SSE lineations.<br />
• The exploration for ilmenite placers in Ratnagiri, Mirya and Kalbadevi bays<br />
showed the ilmenite reserves to be <strong>of</strong> the order <strong>of</strong> 2 million tonnes. Shallow seismic<br />
5
ecords in 13 other bays showed the thickness <strong>of</strong> the sand to be about 21 metres.<br />
Thus, the total reserves <strong>of</strong> ilmenite in these bays appear to be many times greater<br />
than that <strong>of</strong> the Ratnagiri Bay.<br />
• A study <strong>of</strong> the sediments <strong>of</strong> the region surrounding Cape Comorin showed<br />
that its western side is dominated by terrigenous sediments while its eastern side<br />
is dominated by carbonate sediments.<br />
• X-ray diffraction studies on limestone dredge from the shelf (90 m. depth)<br />
showed that its mineralogy does not indicate its exposure to fresh water resulting<br />
either from rainfall or from percolation <strong>of</strong> ground water. These results support<br />
earlier findings that the Peninsular India had a semi-arid climate in the past.<br />
• Studies on the crustal structure and basement tectonics <strong>of</strong> the Bay <strong>of</strong> Bengal<br />
have delineated several new surface and subsurface structural features such as an<br />
escarpment as a surface and a subsurface high over the continental slope extending<br />
along the east coast, a deep and wide marginal basin over the southern continental<br />
margin and graben extending in southeast and northeast directions.<br />
• Experiments on raft-grown mussels showed that the cultured mussels develop<br />
special behavioural, physiological and bio-chemical adaptations to overcome the<br />
range <strong>of</strong> variation in the environmental factors at the culture site. Growth studies<br />
on the shrimps Penaeus indicus and Metapenaeus dobsoni under different frequency<br />
<strong>of</strong> feeding revealed that growth patterns in both tne species follow a linear trend.<br />
• A system was designed in the laboratory to simulate the field conditions for<br />
the study <strong>of</strong> the role <strong>of</strong> microorganisms in specialized ecosystem like mangroves.<br />
• Memodyne digital cassette recorder interfacing circuits have been developed<br />
for temporary storage <strong>of</strong> oceanographic data.<br />
• A single board computer-based microprocessor was designed and developed.<br />
A serial monitor programme was also developed to communicate with the microprocessor<br />
through a teletype or an RS-232-D terminal.<br />
• The design and fabrication <strong>of</strong> an indigenous CTD system, shallow water echosounder<br />
and a pr<strong>of</strong>ile current meter were completed.<br />
• The design <strong>of</strong> a laboratory model <strong>of</strong> OTEC plant <strong>of</strong> capacity 200 watts was<br />
completed.<br />
6
Research Activities
3.0<br />
Oceanographic Cruises<br />
Research vessel Gaveshani<br />
Of the 19 cruises carried out during the year by R.V. Gaveshani. 11 were in<br />
the Arabian Sea and 8 in the Bay <strong>of</strong> Bengal. Oceanographic data from 645 stations<br />
were collected during these cruises. Besides this, surveys <strong>of</strong> the pipeline routes from<br />
Bassein to Bombay High and Direction Bank and in the estuarine regions <strong>of</strong> the<br />
rivers Hooghly and Mahanadi for fixing the position <strong>of</strong> the drilling rig "Chancellors<br />
Ville" <strong>of</strong> Oil India Ltd., were also carried out.<br />
Shipboard facilities on Gaveshani were also availed by a large number <strong>of</strong><br />
scientists from other organizations such as the Bhabha Atomic Research Centre<br />
(BARC,.<strong>Institute</strong> <strong>of</strong> Petroleum Exploration (IPE), Geological Survey <strong>of</strong> India (GSI),<br />
Oil and Natural Gas Commission (ONGC), Oil India Limited (OIL), <strong>National</strong> Geophysical<br />
Research <strong>Institute</strong> (NGRI), Tata <strong>Institute</strong> <strong>of</strong> Fundamental Research (TIFR).<br />
<strong>National</strong> Physical Oceanographic Laboratory (NPOL), Space Applications Centre<br />
(SAC) and India Meteorological Department (IMD).<br />
9
Summaries <strong>of</strong> the cruises 66 to 84 are as follows:<br />
Cruise 66 ( Chief Scientist—T.S.S. Rao)<br />
This 17-days cruise from 27 December, 1979 to 14 January, <strong>1980</strong> formed a<br />
part <strong>of</strong> the continuing programme <strong>of</strong> NIO to monitor the pollution in the seas<br />
around India. The objective <strong>of</strong> the cruise was to survey the oil tanker routes,<br />
from south <strong>of</strong> Sri Lanka to the head <strong>of</strong> Malacca Strait and to pay the courtesy<br />
call at Penang (Malaysia) and to visit the marine science institutes and discuss<br />
problems <strong>of</strong> mutual interest with the Malaysian scientists.<br />
Physical, chemical and biological data were collected from 22 stations and an<br />
area near the Rondo Island, where in early 1979 an American Navy oil tanker<br />
'Sealift Mediterranean' spilled about 5000 tonnes <strong>of</strong> crude oil, was also surveyed.<br />
No tar balls nor any other floating pollutants were found. Probably strong wind<br />
and heavy swell acted as a deterrant to their accumulation.<br />
After completing all the observations, the ship reached Penang on 9th January.<br />
This was the first time that R.V. Gavashani visited a foreign port. An "open house"<br />
was organised to enable the scientists ar,d other interested persons to visit the ship<br />
and see the research facilities on board. More than 200 persons visited the ship.<br />
They appreciated the work carried out by NIO and stressed the need for collaboration<br />
between Indian and Malaysian scientists to work on some <strong>of</strong> the common<br />
problems in the field <strong>of</strong> marine research. All scientists on board visited the Fisheries<br />
Research Laboratory and Tunku Abdul Rahman Aquarium at Glugor. Penang and<br />
Schools <strong>of</strong> Physical, Chemical and Biological Sciences <strong>of</strong> the University Saing<br />
Malaysia at Minden. Penang and had a fruitful discussion on various subjects.<br />
Visit <strong>of</strong> R.V. Gaveshani to Penang-<br />
Participants <strong>of</strong> the cruises 66-68.<br />
11
Cruise 67 (Chief Scientist—T.S.S. Rao)<br />
The main objective <strong>of</strong> the 13-days cruise from 14 to 26 January was to make<br />
further and in-depth study <strong>of</strong> the Andaman Seas including the interaction <strong>of</strong> water<br />
masses coming through the Malacca Strait into the Bay <strong>of</strong> Bengal via Andaman Seas.<br />
Twentysix stations were worked during this cruise and 1900 analyses <strong>of</strong> 245<br />
water samples were carried out on board. About 200 samples were preserved for<br />
the analysis <strong>of</strong> heavy metals. Zooplankton samples were collected using IOSN and<br />
HT nets and sediment samples by a snapper. The oxygen minimum layer, which was<br />
observed at about 200-300m depth along the 10° ridge during the cruise 52, was<br />
not noticed during this cruise. However, low oxygen concentration was observed<br />
at about 150 -200 m depth at all the stations on the western side <strong>of</strong> the Andaman<br />
islands.<br />
Cruise 68 (Chief Scientist—T.S.S. Rao)<br />
The 12-days cruise from 27 January to 7 February, was conducted to make<br />
a further study <strong>of</strong> the changes in the quality <strong>of</strong> water along the oil tanker routes<br />
in the Bay <strong>of</strong> Bengal and around Nicobar islands.<br />
Twentyfive oceanographic stations were worked during the cruise and 1048<br />
analyses on 134 water samples were carried out on board. Some samples were<br />
preserved for the analysis <strong>of</strong> heavy metals. The patchy distribution <strong>of</strong> floating tar<br />
balls along the shipping line (80°E longitude) and a large quantity <strong>of</strong> tar balls<br />
along the western part <strong>of</strong> the shipping lane were observed. The freshness <strong>of</strong> tar<br />
balls indicated that they were formed from some fresh oil spill somewhere north<br />
<strong>of</strong> 5°30'N latitude which is a shipping lane.<br />
At the request <strong>of</strong> Chief Secretary, Andaman and Nicobar Administration,<br />
the ship, on its return cruise from Port Blair worked at five stations in the<br />
Campbell Bay in the Great Nicobar island area. From this region several samples<br />
<strong>of</strong> plankton, benthos and chlorophyll were collected.<br />
Cruise 69 (Chief Scientist—D. Panakala Rao)<br />
This 12-days cruise was from 14 to 25 February between latitudes 11° and<br />
15°N and longitudes 68° and 71°30' E to work out the oceanographic and meteorological<br />
conditions during late winter. This area was earlier studied under MONEX-79<br />
programme.<br />
In all, 58 stations were worked during the cruise. Lower sea surface temperature<br />
was observed during this season as compared to the earlier cruise. Salinity maxima<br />
and minima characteristic <strong>of</strong> the Arabian Sea were once again recorded in the<br />
column pr<strong>of</strong>ile. Two oxygen minima at 200 and 600 m separated by a layer <strong>of</strong><br />
relatively high oxygen at about 400 m were recorded during the cruise.<br />
On the day <strong>of</strong> total solar eclipse (16 February), biological and meteorological<br />
observations were made in the zone <strong>of</strong> total solar eclipse (13°25'N and 71°30'E).<br />
12
Using IOSN, zooplankton samples were collected before, during and after the<br />
total solar eclipse from 100 to 0 m to work out the pattern <strong>of</strong> vertical migration<br />
<strong>of</strong> animals during the various phases <strong>of</strong> the eclipse. Hourly surface meteorological<br />
observations were also taken from 1200 to 1700 hours which did not show any<br />
decrease in the air or sea surface temperatures during the total eclipse.<br />
Cruise 70 (Chief Scientist—H.N. Siddiquie)<br />
This short cruise <strong>of</strong> 3-days from 5 to 7 March was primarily organised <strong>of</strong>f<br />
Goa for testing the equipment received under NORAD assistance programme on<br />
'Geological and geophysical surveys <strong>of</strong> the west coast'. The trials during the cruise<br />
indicated some fault in the records obtained from the ORE-mud penetrator. The<br />
fault was arising from the hull-mounted transducers. Some mal-functioning in the<br />
triggering <strong>of</strong> EG and G sparker and boomer was also noticed. Remedial measures<br />
for these problems were undertaken before the next cruise.<br />
The CTD system designed and fabricated at NIO was successfully tested and<br />
the results were compared with the Guideline CTD system.<br />
Cruise 71 (Chief Scientist—H.N. Siddiquie)<br />
This cruise <strong>of</strong> 17-days duration was from 11 to 27 March. The main objective<br />
<strong>of</strong> this cruise was to fill in the gaps in the geological and geophysical surveys<br />
<strong>of</strong> the western continental margin carried out earlier so that the coverage may be<br />
extended upto the shelf south <strong>of</strong> Cochin.<br />
During the cruise, 2061 line km <strong>of</strong> echosounding, 972 line km <strong>of</strong> side scan<br />
sonar, 1595 line km <strong>of</strong> shallow seismic pr<strong>of</strong>iling, 390 line km <strong>of</strong> deep seismic<br />
pr<strong>of</strong>iling and 1469 line km <strong>of</strong> magnetics were carried out. Underwater camera was<br />
operated at 4 stations. Water samples and grab samples were collected from 25<br />
and 73 stations respectively.<br />
The surveys indicate that the continental shelf upto a depth <strong>of</strong> about 40 m<br />
and in some cases upto 25 m (<strong>of</strong>f Cochin), is marked by an even topography due<br />
to clay cover. Beyond this depth, the topography is uneven and along the shelf<br />
break, <strong>of</strong>f Mangalore and Cochin, a number <strong>of</strong> pinnacles are clearly seen. The<br />
samples collected show that the outer shelf is largely covered by olive grey to<br />
greyish olive silty to clayey sands and the slope has silt and clayey silt.<br />
Samples <strong>of</strong> Trichodesmium were also collected <strong>of</strong>f Kerala coast where bloom<br />
was seen in pr<strong>of</strong>usion.<br />
Cruise 72 (Chief Scientist—H. N. Siddiquie)<br />
This 12-days cruise from 2 to 13 April formed a part <strong>of</strong> the NIO-IPE-ONGC<br />
collaboration programme (NCST Priority Project No. 6), entitled, "Sedimentological,<br />
geochemical and microbiological studies in the continental shelf between Bombay High<br />
and <strong>of</strong>fshore <strong>of</strong> Kutch including the Gulf <strong>of</strong> Cambay and Kutch".<br />
Four tracks on the shelf covering 975 line km <strong>of</strong> echosounding, 870 line km <strong>of</strong><br />
ORE pr<strong>of</strong>iling, 200 line km <strong>of</strong> EG & G sparker and 993 line km <strong>of</strong> magnetics were<br />
13
covered during the cruise. In addition, 29 water samples, 46 grab samples, 4 dredge<br />
samples, 4 core samples and 12 bottom photographs were taken.<br />
The surveys indicated that the continental shelf from the shore to a depth <strong>of</strong><br />
60-75 m is marked by even topography because <strong>of</strong> the clay cover.<br />
Cruise 73 (Chief Scientist—H.N. Siddiquie)<br />
This cruise <strong>of</strong> 19-days duration was from 13 April to 1 May. It was sponsored<br />
by the ONGC for the development <strong>of</strong> <strong>of</strong>fshore oilfields. The work included: survey<br />
<strong>of</strong> the pipeline routes from South Bassein to Direction Bank, from Direction Bank up<br />
to the shore and shallow seismic surveys at South Bassein and Direction Bank.<br />
During this cruise, more than 290 line km <strong>of</strong> echosounding, 660 line km <strong>of</strong><br />
ORE mud penetrator pr<strong>of</strong>iling, 1060 line km <strong>of</strong> sparker and 120 line km <strong>of</strong> magnetic<br />
surveys were carried out.<br />
Along the proposed pipeline route (from Bassein to Direction Bank), the depth<br />
varied from 51 m at Bassein to 65 m on the southern side and 41 m at the Bank.<br />
From Direction Bank along the route the depth ranged from 45 m at the Bank to<br />
55 m towards east and 15 m near the shore.<br />
Cruise 74 (Chief Scientist—H.N. Siddiquie)<br />
This 12-days cruise from 4 to 15 May was carried out in continuation <strong>of</strong> the<br />
earlier cruise. During the cruise shallow seismic pr<strong>of</strong>iling on the Bassein structure and<br />
the post-lay survey <strong>of</strong> the pipelines from Bassein to Bombay High were carried out.<br />
In all, 20 lines were surveyed in the south Bassein and the pipeline pr<strong>of</strong>iling<br />
was done along 50 lines. Over 673 line km <strong>of</strong> echosounding. 200 line km <strong>of</strong> side<br />
scan sonar and 671 line km <strong>of</strong> shallow seismic pr<strong>of</strong>iling were carried out.<br />
The depth on south Bassein ranged from 38 to 69 m and increased, in the<br />
northern and eastern sides and also in the southern and western sides- The pipeline<br />
was crossed, in 64 tracks and the pipes were seen in 43 tracks. Along 52 tracks, the<br />
pipelines were very well covered by 2.2.5 m thick sediments and in the remaining 2<br />
tracks, the pipelines apparently were on the seabed or were covered by a thin sediment<br />
only.<br />
Cruise 75 (Chief Scientist—M.G.A.P. Setty)<br />
This 14-days cruise from 21 May to 3 June was devoted to the study <strong>of</strong> oceanographic<br />
conditions in the MONEX square ( between 11-15°N and 68-71° 31' E) during<br />
the onset <strong>of</strong> southwest monsoon. Another aspect <strong>of</strong> the cruise was to study primaryproductivity,<br />
nannoplankton and extra cellular liberation <strong>of</strong> photosynthates at<br />
various depths <strong>of</strong> the euphotic zone.<br />
The cruise covered a distance <strong>of</strong> 3892 line km. in which 50 stations were<br />
worked. Data on phosphate, nitrate, nitrite, ammonia and silicate were collected at<br />
all the stations.<br />
At the request <strong>of</strong> BARC, sediment samples from deeper parts <strong>of</strong> the sea were<br />
collected for their use- Radon activity was also studied during the cruise.<br />
14
Cruise 76 (Chief Scientist—M.G.A.P. Setty)<br />
This cruise <strong>of</strong> 7-days duration was from 7 to 13 June. It started from Madras<br />
and terminated at Visakhapatnam as a joint project between the NIO and GSI.<br />
Sediment samples during the cruise were collected from 61 stations in the<br />
depth range <strong>of</strong> 18-250 m for sedimentological, geochemical, micropaleontological and<br />
benthic studies. In addition, samples were also collected from 12 m below the water<br />
surface, and close to the bottom sediment. Water sediment interface samples (nearshore<br />
<strong>of</strong>fshore) from 35 stations were also collected to study the paniculate matter and<br />
suspended load present at these stations. Sample were also obtained for the study<br />
<strong>of</strong> macro and meiobenthos at all the stations.<br />
Cruise 77 (Chief Scientist—M.G.A.P. Setty)<br />
This cruise <strong>of</strong> 12-days duration was from 15 to 26 June to study the continental<br />
shelf from about 20 m depth near the shore up to the shelf edge between Visakhapatnam<br />
and the mouth <strong>of</strong> the river Ganga at 'Swatch <strong>of</strong> no ground'. Samples were<br />
collected for bathymatric, sedimentological, micropaleontological and geochemical<br />
studies and for benthos distribution in the shelf area.<br />
In all, 115 samples were collected during this cruise. Alphid lobsters (Synalpheus<br />
sp.) with young oysters were collected from a substrate <strong>of</strong>f Puri (Orissa). The<br />
sediment here was coarse and sandy.<br />
Cruise 78 (Chief Scientist—R. Sen Gupta)<br />
The 18-days cruise from 3 to 20 September was undertaken to survey the delta<br />
region <strong>of</strong> the river Hooghly and the mouth <strong>of</strong> the river Mahanadi and to carry out<br />
the position fixing <strong>of</strong> the drilling rig "Chancellors Ville" <strong>of</strong> the Oil India Ltd. in the<br />
Bay <strong>of</strong> Bengal.<br />
During the cruise, the ship covered a distance <strong>of</strong> about 1900 line km and.<br />
worked at 15 stations. Apart from this, 3 anchored stations were worked inside<br />
the river Hooghly where currents and waves were recordede very 2 hours and hydrographic<br />
casts and plankton hauls were taken at 3 hourly interval. 385 water samples<br />
were processed, filtered and/or preserved on board for the examination <strong>of</strong> different<br />
biological constituents, heavy metals, petroleum hydrocarbons, suspended minerals, etc.<br />
The ship was at anchor for 6 days <strong>of</strong>f the Oil India drilling rig "Chancellors<br />
Ville" during which time 29 satellite navigation fixes were obtained. In addition,<br />
currents, waves, tides and heave <strong>of</strong> the ship were also measured every hour.<br />
Cruise 79 (Chief Scientist—L.V.G. Rao)<br />
The 14-days cruise was undertaken at the request <strong>of</strong> ONGC from 23 September<br />
to 6 October to carry out current measurements near the oil bearing structure <strong>of</strong>f<br />
the Godavari basin, south <strong>of</strong> Visakhapatnam. Current observations were made at<br />
different depths and at different time intervals using a current meter mooring system<br />
developed by the <strong>Institute</strong>.<br />
Apart from this a survey was conducted to identify some ship wrecks <strong>of</strong>f<br />
15
Visakhapatnam Port at the request <strong>of</strong> the port authorities. There was another request<br />
from the drill ship "Fredericksberg, for the bathymetry survey <strong>of</strong> their new location<br />
for the deployment <strong>of</strong> the drill ship. These surveys were also completed.<br />
Cruise 80 (Chief Scientist—C.K. Gopinathan)<br />
This cruise was organised for 11 days from 8 to 18 October to study the physical,<br />
chemical and biological features <strong>of</strong> the waters <strong>of</strong>f Coromandal coast (southwest<br />
Bay <strong>of</strong> Bengal) at the site <strong>of</strong> the proposed OTEC plant in Tamil Nadu.<br />
A distance <strong>of</strong> about 350 line km was covered<br />
during the cruise and 24 stations were worked.<br />
Surface meteorological observations such as<br />
recording <strong>of</strong> wind speed and direction, sea surface<br />
temperature, atmospheric pressure at sea<br />
level, wet and dry bulb readings were carried<br />
out at all the stations.<br />
Oceanographic and Meteorological<br />
Data Buoy deployed <strong>of</strong>f Goa in<br />
the Arabian Sea.<br />
Cruise 81 (Chief Scientist—V.V.R. Varadachari)<br />
This short cruise <strong>of</strong> 3 days, from 23 to 25<br />
October, was organised <strong>of</strong>f Goa for launching a<br />
meteorological and oceanographic data buoy procured<br />
by the <strong>Institute</strong> from the Marine Exploration<br />
Ltd. U.K. (MAREX). The buoy was<br />
deployed with the help <strong>of</strong> the ship's derrick on<br />
24th morning at location lat. 15°2l'N, long.<br />
73°05' E, where water depth was 100 m.<br />
The buoy was retrieved and brought back<br />
into the ship on the same day in the evening-<br />
Apart from the NIO. scientists from BARC,<br />
TIFR, IMD, NPOL, SAC and MAREX (UK)<br />
participated in the cruise. BARC scientists conducted<br />
B.T. observations and ship's speed during<br />
the return journey <strong>of</strong> the ship. Scientists from<br />
the TIFR made Radon measurements and scientists from SAC collected data on<br />
chlorophyll from the sea and made irradiance measurements.<br />
Cruise 82 (Chief Scientist—V.V.R. Varadachari)<br />
This cruise was for 15 days duration in the MONEX square (occupied earlier<br />
during MONEX-79 programme and in three other cruises) to study the oceanographic<br />
conditions in the area during the peried from 1 to 15 November.<br />
Data were collected from 48 stations. Results indicated that air temperature<br />
and sea surface temperature were low. At all the stations, plankton samples were<br />
also collected.<br />
Besides the NIO scientists, one scientist from TIFR and two from GSI also<br />
16
participated in the cruise. They collected data on Radon and water samples for<br />
determination <strong>of</strong> mercury respectively.<br />
Cruise 83 (Chief Scientist—Ch. M. Rao)<br />
This 15-days cruise was undertaken from November 21 to December 5 to collect<br />
geological and geophysical data to decipher the regional geology, structure and tectonics<br />
<strong>of</strong> the continental shelf between Dabhol and Khanderi along the west coast <strong>of</strong> India.<br />
During the cruise 1820 line km <strong>of</strong> echosounding. ORE sub-bottom pr<strong>of</strong>iling<br />
sparker and magnetic surveys were carried out. Seabed and water samples were<br />
collected from 33 and 12 stations respectively while the underwater camera was<br />
operated at 7 stations. At 16 stations sediment samples collected were sieved for<br />
benthic faunal studies. The surveys revealed that the shelf is marked by even topography<br />
to a depth <strong>of</strong> about 85 m. Beyond this (70 to 85 m) depth the topography<br />
on the outer shelf is uneven and somewhat rugged. Acoustic masking <strong>of</strong> reflectors<br />
due to gases was noticed in the inner shelf. Several low amplitude (100 gammas)<br />
magnetic anomalies in all the pr<strong>of</strong>iles were also observed-<br />
Besides the NIO participants, three scientists from NPOL, Cochin also participated<br />
in this cruise and carried out sound reverberation studies at 4 stations.<br />
Cruise 84 (Chief Scientist—Ch.M. Rao)<br />
This cruise <strong>of</strong> 13 days was organised from 11 to 23 December for geological and<br />
geophysical surveys <strong>of</strong> the continental shelf between Mangrol and Dwarka along the<br />
west coast <strong>of</strong> India.<br />
During the cruise about 1270 line km <strong>of</strong> echosounding, ORE sub-bottom<br />
pr<strong>of</strong>iling, sparker and magnetic serveys were carried out on ten lines. In addition<br />
magnetic surveys for about 170 line km were carried out on a N.S line while returning<br />
to Goa. Bottom sediment samples were collected at 37 stations and the underwater<br />
camera was operated at 7 stations.<br />
The results <strong>of</strong> the surveys indicated that the seabed to a depth <strong>of</strong> 130 m is<br />
largely marked by even topography- The shelf break occurs between 100-140m and<br />
the slope is characterised by rugged topography and steep gradients. The seabed<br />
is carpeted by transparent clay to a depth <strong>of</strong> about 80 m. The magnetic surveys<br />
indicated three types <strong>of</strong> magnetic anomalies viz. (i) region to about 20 km from<br />
the shore is characterised by very high amplitude high frequency anomalies, (ii) the<br />
middle shelf is characterised by several prominent high amplitude anomalies, and<br />
(iii) the magnetic signature is smooth on the outer shelf to slope. The sediment<br />
samples show that the outer shelf is largely covered by gray to grayish white clayey<br />
sands with shells and the slope by olive green clayey-sandy-silts.<br />
17
3.1<br />
Physical <strong>Oceanography</strong><br />
3.1.1 Studies on ocean-atmosphere interaction<br />
3.1.2 Studies on physical processes in the seas around India<br />
3.1.3 Studies on land-sea interaction and nearshore circulation along the<br />
Indian coastline with application to coastal zone management<br />
Ocean currents, their driving forces and land sea-air interaction are some <strong>of</strong><br />
the major topics <strong>of</strong> interest in physical oceanography. A large amount <strong>of</strong> data on<br />
the variations in temperature, salinity, pressure, wind speed and direction, movement<br />
<strong>of</strong> the watermasses was collected employing various methods/equipment from the<br />
ship, moored or drifting current meter systems.<br />
During the year, an oeeanographic and meteorological data buoy was moored<br />
from R.V. Gaveshani <strong>of</strong>f Goa in the Arabian Sea. Various instruments for measuring<br />
Pr<strong>of</strong>iling current meter developed at NIO.<br />
19
the meteorological parameters have also been installed on the terrace <strong>of</strong> the main<br />
building. To measure the vertical pr<strong>of</strong>ile <strong>of</strong> the horizontal current, a pr<strong>of</strong>iling current<br />
meter has been designed and fabricated. The system was tested in the Bay <strong>of</strong> Bengal<br />
and the preliminary results were found to be encouraging.<br />
3.1.1 Studies on ocean-atmosphere interaction<br />
(a) Distribution <strong>of</strong> stability <strong>of</strong> the waters<br />
A comparative study <strong>of</strong> the vertical stratification in the upper 300 m in<br />
the Arabian Sea and Bay <strong>of</strong> Bengal was made. The study revealed that (i) the zone<br />
<strong>of</strong> maximum stability coincides with the discontinuity layer; (ii) the water column was<br />
strongly stratified in the Bay <strong>of</strong> Bengal as compared to that <strong>of</strong> the Arabian Sea.<br />
This feature appears to be one <strong>of</strong> the factors governing the low level <strong>of</strong> nutrients<br />
occurring in the surface layers <strong>of</strong> the Bay <strong>of</strong> Bengal.<br />
(b) Circulation and its relation to the distribution <strong>of</strong> oceanographic parameters<br />
Based on the IIOE data collected during February-March, charts on dynamic<br />
topography, mass distribution, temperature, salinity, dissolved oxygen and inorganic<br />
phosphates in the upper layers <strong>of</strong> the Bay <strong>of</strong> Bengal, were prepared. This analysis<br />
revealed that:<br />
1. the field <strong>of</strong> motion in the near-surface layers <strong>of</strong> the Bay <strong>of</strong> Bengal during<br />
late winter is the result <strong>of</strong> various factors such as (i) the winter cooling near the head <strong>of</strong><br />
the Bay, (ii) the influence <strong>of</strong> northeast monsoon winds, (iii) the influence <strong>of</strong> north<br />
equatorial currents in the southern regions and (iv) the influence <strong>of</strong> fresh water discharge,<br />
especially in the northern Bay, Andaman Sea and along the east coast <strong>of</strong> India.<br />
Typical vertical distribution <strong>of</strong> temperature ( 0 3<br />
C), salinity (per mil), oxygen (ml/1) and PO4 -P (μg-at/l).<br />
20
2. the integral mean concentration <strong>of</strong> the nutrients in the surface mixed layer<br />
is in agreement with the near-surface circulation. The high value <strong>of</strong> nutrients associated<br />
with low dissolved oxygen are confined to thicker surface layers indicating<br />
clearly the effect <strong>of</strong> divergence or cyclonic gyre (convergence or anticyclone gyre)<br />
present in the near-surface circulation.<br />
3. the salinity structure shows that the Bay <strong>of</strong> Bengal has estuarine type <strong>of</strong><br />
circulation due to heavy discharge <strong>of</strong> fresh water all along its land peripheries.<br />
(c) ΜΟΝΕΧ-79 studies<br />
The hydrographic and MBT data collected during MONEX-79 programme<br />
were processed. For the analysis <strong>of</strong> these data, the following computer programmes<br />
were developed: (i) Bionomial filter programme for smoothening the digitized data,<br />
(ii) A programme for computing the potential energy <strong>of</strong> the water column and the<br />
energy changes due to mixing and (iii) A programme for analysing the wave<br />
records.<br />
The study revealed significant variations in the upper 500 m during the period<br />
May to June 1979. The sea surface temperature increases by about 1°C whereas<br />
the thickness <strong>of</strong> the mixed surface layer decreases by about 10 m. Inspite <strong>of</strong> the<br />
above features, the cyclone heat potential showed an increase from May to June<br />
1979 in the MONEX square (the region from where the data were collected). The<br />
heat potential was estimated to be about 30 kcal/cm 2 which can maintain a moderate<br />
cyclone for a period <strong>of</strong> 6 days. The rise in thermocline is attributed to the entrainment<br />
<strong>of</strong> cool subsurface water into the surface layer. Further studies to prove<br />
this are being carried out using the continuity equation. The influence <strong>of</strong> equatorial<br />
watermass in the MONEX area is clearly seen during May-June 1979.<br />
Preliminary studies on the thermodynamic potential <strong>of</strong> seawater indicated that the<br />
changes in energy associated with contraction or mixing are important for understanding<br />
the watermass structure in the MONEX square.<br />
(d) Heat budget <strong>of</strong> the Andaman Sea<br />
The seasonal heat storage including the fluxes <strong>of</strong> net radiation, latent and sensible<br />
heat have been worked out for the Andaman Sea. These studies indicated an<br />
annual evaporation rate <strong>of</strong> about 137 cm over the region <strong>of</strong> the Andaman Sea and the<br />
vertical heat transport is confined to the upper 20 m where a strong halocline exists<br />
which probably inhibits the heat transfer to deeper waters.<br />
3.1.2 Studies on physical processes in the seas around India<br />
Field data were collected during 7 cruises from the Bay <strong>of</strong> Bengal including<br />
the Andaman Sea and the eastern Arabian Sea. During two <strong>of</strong> these cruises (viz-<br />
69th and 75th) observations were carried out in the MONEX square for studying<br />
the post-monsoon conditions. CSTD System was operated and continuous pr<strong>of</strong>iles<br />
21
Distribution <strong>of</strong> temperature (A), salinity (B) and density (C)<br />
along fifth transect in the Andaman Sea.<br />
22<br />
Oceanic cyclone heat potential (kcal cm -2 ) for cruise<br />
54 (A), 55 (B) and 56 (C).
<strong>of</strong> temperature and salinity/conductivity mostly upto 2000 m depth were obtained at 41<br />
stations. These data are being processed and some <strong>of</strong> the results are mentioned below:<br />
(a) Surface boundary layer studies<br />
Based on the surface meteorological and wave data collected from two<br />
locations in the western Bay <strong>of</strong> Bengal in July 1979 during the 58th cruise, surface<br />
layer conditions <strong>of</strong> the atmosphere <strong>of</strong> different surface circulations, associated sea<br />
surface roughness and the height <strong>of</strong> surface roughness were studied. The thermal<br />
stratification <strong>of</strong> the surface layer as inferred from the Bulk Richardson number<br />
values revealed neutral and near-neutral conditions. The convective activity affected<br />
the sea-air temperature difference and seemed to cause variations in the characteristic<br />
height <strong>of</strong> the surface layer. Larger variations in the surface layer were encountered<br />
during the rough condition <strong>of</strong> the sea. The wind hodographs <strong>of</strong> diurnal variations<br />
showed anticyclonic and a precursor and cyclonic circulations.<br />
(b) Sound velocity structure<br />
Using the hydrographic data collected by R.V. Vityaz during the IIOE<br />
(January-March 1961), sound velocity structure <strong>of</strong> the Bay <strong>of</strong> Bengal including the<br />
Andaman Sea has been studied. In the upper 200 m, sound velocity varied significantly<br />
with longitude (8-11 m/sec). It was relatively greater in the low latitude.<br />
The depth <strong>of</strong> SOFAR channel (axis <strong>of</strong> primary sound channel) varied between 800 m<br />
and 1750 m. Geographical variations <strong>of</strong> SOFAR axial velocities were found to be<br />
related to the characteristics <strong>of</strong> general circulation in the area.<br />
(c) Hydrographic features<br />
Physical characteristics in the Andaman Sea during the winter were studied<br />
using the data collected by R. V. Gaveshani during the period January-February in<br />
1979 and <strong>1980</strong>. Distributions <strong>of</strong> temperature, salinity and density along six transects<br />
were studied and characteristics <strong>of</strong> watermasses were investigated. The Persian<br />
Gulf water was identified in the depth range <strong>of</strong> 200-500 m with a characteristic<br />
high salinity <strong>of</strong> about 35.l%o, temperature range 10 to 12°C and σ- t range 26.7 to 27.0.<br />
Below this, in the depth range 500-900 m the water <strong>of</strong> the Red Sea seems to<br />
be present. In the northern part <strong>of</strong> the study area, a mixed layer with thickness<br />
upto 75 m was encountered. The presence <strong>of</strong> a warm deeper water in the Andaman<br />
Sea area has also been confirmed.<br />
(d) Wave characteristics<br />
Using the wave data collected with a shipborn wave recorder during the 51st<br />
and 52nd cruises (February 1979) and 67th cruise (January <strong>1980</strong>) <strong>of</strong> R.V. Gaveshani<br />
the wave characteristics <strong>of</strong> the seas around the Andaman and Nicobar islands were<br />
studied. The distribution <strong>of</strong> zero crossing period, significant wave height and spectral<br />
width parameter were also studied. The predominant zero crossing period and<br />
significant wave heigh were found to be 6-12 secs and 0.6-1.4 metres respectively.<br />
23
3.1.3. Studies on land-sea interaction and nearshore circulation along the Indian coastline<br />
with application to coastal zone management<br />
Studies under this project have been carried out partly from headquarters and<br />
partly from Regional Centres <strong>of</strong> Cochin and Bombay.<br />
(a) Studies at Mangalore<br />
The physical characteristics <strong>of</strong> the water <strong>of</strong> Gurpur river and New Mangalore<br />
Harbour were investigated to assess their suitability for the proposed disposal <strong>of</strong><br />
effluents from the Kudremukh Iron Ore Co., Ltd., Mangalore. The data on currents<br />
(speed and direction), temperature and electrical conductivity were collected at intervals<br />
<strong>of</strong> fifteen minutes for 25 hours continuously using Aanderaa recording current<br />
meter at a few selected locations. Dispersion studies using Rhodamine-B dye were<br />
also carried out. These studies showed accumulation <strong>of</strong> pollutants in these water<br />
bodies especially during the non-monsoon months.<br />
(b) Beach studies in Goa area<br />
Studies started during the previous year on the Miramar beach were extended<br />
towards the south covering the region upto Caranzalem. Two locations were continuously<br />
monitored on the northern side to assess the stability and the spatial variations in the<br />
morphology <strong>of</strong> the various sections with special reference to the impact <strong>of</strong> probable<br />
movement/shift in the location <strong>of</strong> the Aguada Bar/shoal present in this environment-<br />
Further studies are in progress.<br />
(c) Development <strong>of</strong> computer programmes<br />
Computer programmes were developed for spectral analysis <strong>of</strong> time series data<br />
on waves, currents, temperature, salinity etc. These are (a) autospectrum - using both<br />
FFT algorithm and autocorrelation methods and (b) cross spectrum through FFT<br />
algorithm. The salient features <strong>of</strong> these programmes are :<br />
(i) Any number <strong>of</strong> sets <strong>of</strong> data can be handled,<br />
(ii) Five built-in windows (rectangular, Cosine Taper, Tukey, Blackman and<br />
Hamming) are available in time domain,<br />
(iii) Built-in functions to do ensemble and frequency averaging,<br />
(iv) Removal <strong>of</strong> noise and correction for the attenuation (wave data) and<br />
(v) Availability <strong>of</strong> Inverse Fourier Transforms.<br />
En addition, a programme was developed for computer plotting <strong>of</strong> two dimensional<br />
data.<br />
(d) Estuarine studies<br />
Studies on the dynamics and physical characteristies <strong>of</strong> the Mandovi and the<br />
Zuari estuaries and the Cumbarjua Canal were undertaken. Taking the average<br />
run<strong>of</strong>f for the Zuari and the Mandovi estuaries as 9 km 3 /year and 16 km 3 /year respectively<br />
and their water sheds as 550 km 2 and 1150 km 2 respectively, the run<strong>of</strong>f ratio and<br />
the water shed ratio for the Mandovi-Zuari was found to be approximately 2. Peak<br />
24
discharges occur during August in both, the estuaries (500 m 3 /sec for the Mandovi and<br />
250 m 3 /sec for the Zuari) with slightly lower values in July and much lower in September<br />
(160 m 3 /sec for the Mandovi and 80 m 3 /sec for the Zuari approximately).<br />
Studies on the turbulent mixing at the interface <strong>of</strong> the saline wedges occurring<br />
in these estuaries during the monsoon months and the response <strong>of</strong> the interface to tidal<br />
forcing factors, have also been taken up.<br />
(e) Beach changes along the Kerala coast<br />
Detailed work in respect <strong>of</strong> this investigation has been reported separately in<br />
Section 3.8.1.<br />
(f) Erosion studies at Versova<br />
The work carried out under this investigation has been reported separately<br />
in Section 3.8.2.<br />
(g) Beach studies at Thal-Alibag coastline.<br />
The progress made under this investigation has been reported separately in<br />
Section 3.8.2.<br />
25
INSTRUMENTS INSTALLED IN THE INSTITUTE
3.2<br />
Chemical <strong>Oceanography</strong><br />
3.2.1 Chemical studies in the coastal and <strong>of</strong>fshore waters <strong>of</strong> the Arabian<br />
Sea and Bay <strong>of</strong> Bengal<br />
3.2.2 Drugs from the sea<br />
3.2.3 Protection <strong>of</strong> marine environment and monitoring <strong>of</strong> pollutants along<br />
the Indian coast<br />
3.2.4 Characteristics <strong>of</strong> the estuarine regions <strong>of</strong> major rivers <strong>of</strong> India<br />
The major concern <strong>of</strong> chemical oceanographers is to determine the chemistry<br />
<strong>of</strong> the marine environment and the changes therein induced by natural and man<br />
made activities. Studies on the marine environment also include the determination<br />
<strong>of</strong> the amount <strong>of</strong> organic carbon present in the surface waters, the distribution,<br />
nature and biochemistry <strong>of</strong> marine compounds in marine fauna and flora thereby<br />
identifying new drug resources, and pollution and related aspects like the protection<br />
and control <strong>of</strong> oil pollution, sewage and industrial discharge. These studies were<br />
carried out under four projects and the summary <strong>of</strong> each is given below.<br />
3.2.1 Chemical studies in the coastal and <strong>of</strong>fshore waters <strong>of</strong> the Arabian Sea and Bay<br />
<strong>of</strong> Bengal<br />
The work under this project was carried out at headquarters as well as at<br />
Regional Centre, Cochin.<br />
1. Chemical characteristics <strong>of</strong> the Andaman Sea and Bay <strong>of</strong> Bengal<br />
During the cruises in the southern Bay <strong>of</strong> Bengal from 78°E to 98°30'E, hydrographic<br />
stations were worked at 1 degree intervals. In the Andaman Sea almost all the<br />
stations worked during the cruises 51 and 52 in 1979 were repeated in <strong>1980</strong> and in addition<br />
70 new stations were occupied to study the changes that might have taken place during<br />
the course <strong>of</strong> the year. A total number <strong>of</strong> 4152 analyses were carried out on board and<br />
317 samples were collected for the analysis <strong>of</strong> major ions in the shore laboratory.<br />
In the upper 50-75 m, <strong>of</strong> the entire Andaman Seas the concentrations <strong>of</strong> nitrates,<br />
phosphates and silicates were low. These were associated with high oxygen and pH-<br />
Nitrite was detected only between 50 and 75 m depth. A thick oxygen minimum layer<br />
extended from 100 m to 1000 m. In <strong>1980</strong>, the concentrations <strong>of</strong> nutrients increased with<br />
simultaneous decrease in the oxygen and pH. At a station in the Malacca Strait, north <strong>of</strong><br />
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Sumatra low oxygen concentration was observed at the surface associated with high<br />
concentrations <strong>of</strong> nitrate, phosphate and silicate and low pH, probably indicating the<br />
presence <strong>of</strong> upwelled water.<br />
Very low oxygen concentration (0.05-0.06 ml/l) was observed at 150-200 m depths<br />
at stations near the eastern end <strong>of</strong> the 10° channel along a north-south transect east <strong>of</strong><br />
the Andaman and Nicobar islands during 1979. Repeating the same section in <strong>1980</strong> it was<br />
observed that oxygen concentration at about the same depth levels has increased to<br />
about 0.3 ml/l. An attempt was made to study this phenomenon by plotting the potential<br />
density and using dissolved silicon as an indicator to examine if any new water has entered<br />
into the basin. Indeed, the presence <strong>of</strong> deep water renewal could be identified using<br />
these indicators. As before, such low concentrations <strong>of</strong> oxygen were absent along the<br />
western side <strong>of</strong> the islands which has more or less the same water characteristics as the<br />
open Bay <strong>of</strong> Bengal.<br />
In the north western Bay <strong>of</strong> Bengal, a few anchor stations <strong>of</strong>f the mouths <strong>of</strong> the<br />
rivers Hooghly and Mahanadi were worked over one tide cycle <strong>of</strong> 12 hours to study the<br />
effect <strong>of</strong> run<strong>of</strong>f from the rivers. Also samples from the mid-depth at each station over<br />
the tidal cycle were mixed and analysed for all the parameters including suspended solids.<br />
2. Hydrochemical characteristics <strong>of</strong>f the west coast <strong>of</strong> India<br />
Data obtained during the 46th and 59th cruises <strong>of</strong> R.V. Gaveshani indicate the presence<br />
<strong>of</strong> two oxygen minima associated with two phosphate maxima at about 300 m and<br />
l000 m depths respectively. These extend to about 15°N <strong>of</strong>f the central west coast <strong>of</strong> India.<br />
The second oxygen minimum gets diffused away from the shore due to mixing processes in<br />
the watermasses. About 34% <strong>of</strong> the available nitrate-nitrogen in the depth range 75-1200 m<br />
appears to be depleted by denitrification. The 'standing crop' <strong>of</strong> denitrified nitrogen has<br />
been calculated to be 70 g/m 2 . Combining the rates <strong>of</strong> denitrification at an intermediate<br />
depth with the photo synthetic productivity within the euphotic zone, the mean residence<br />
time <strong>of</strong> the watermass in the depth interval <strong>of</strong> denitrification in the Arabian Sea has been<br />
found to be in the range <strong>of</strong> 13 to 54 years.<br />
The data collected during the MONEX-79 cruises <strong>of</strong> R.V.Gaveshani were used<br />
to evaluate the two modes <strong>of</strong> calculation <strong>of</strong> original nitrate concentrations adopted earlier<br />
to study the denitrification in the Arabian Sea. Nitrite at the intermediate depths was<br />
not found to be restricted to the Persian Gulf water but it was maximum at much shalower<br />
depths than the depths at which this watermass was encountered. It was thus<br />
concluded that the use <strong>of</strong> nitrate-salinity relationship for the calculation <strong>of</strong> the original<br />
nitrate concentration, as followed in a recent study would, therefore, underestimate the<br />
nitrate deficits. A region-specific but slightly modified method, which involves the use <strong>of</strong><br />
oxidative ratios, has been tried to re-examine the values in the eastern central Arabian<br />
Sea. The nitrate deficits obtained lie in between the values reported earlier. A steady<br />
southward decrease in the intensity <strong>of</strong> denitrification was observed upto 11—12°N<br />
latitude. Taking a value <strong>of</strong> 30 years as the average residence time <strong>of</strong> water for the layer<br />
in which denitrification occurs, the denitrification rate in the Arabian Sea has been<br />
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calculated to be about 3.2 x 10 12 g/yr · This represents about 5% <strong>of</strong> the annual global<br />
denitrification.<br />
3. Major nutrients <strong>of</strong> the Mandovi and Zuari river systems<br />
Seasonal studies in the Mandovi and Zuari rivers show that the stations at the<br />
marine-end have two peaks <strong>of</strong> nitrate and phoshate corresponding to monsoon and post<br />
monsoon seasons, while the stations at the river-end showed only one peak during the<br />
monsoon. Silicate showed a well-defined pattern <strong>of</strong> distribution with only one peak<br />
during the monsoon.<br />
Applying a 'simple mixture' relation using salinity as an indicator it was observed<br />
that in the pre-monsoon season, nitrate, phosphate and silicate are removed from the<br />
water column <strong>of</strong> the two estuaries. During the monsoon season, however, only phosphate<br />
was removed while nitrate and silicate show a near-conservative behaviour. In the<br />
post-monsoon season there is an addition <strong>of</strong> nitrate and phosphate to the estuaries while<br />
silicate shows a reduction <strong>of</strong> about 50%.<br />
4. Studies on the carbon dioxide system in sea water<br />
Distribution <strong>of</strong> different components <strong>of</strong> carbon dioxide system in the northern<br />
Indian Ocean, is being studied from the data collected during cruises 66 to 68 <strong>of</strong> R.V.<br />
Gaveshani. A seasonal study has also been completed in the Mandovi-Zuari estuarine<br />
system to understand the carbon dioxide equilibria in the estuarine process.<br />
5. Silicon cycle in the sea<br />
Studies on the dissolved and particulate organic forms <strong>of</strong> silicon showed that the<br />
organic fraction <strong>of</strong> silicon was not detectable in appreciable quantities at any depth <strong>of</strong> the<br />
Arabian Sea. The particulate silicon, however, in the surface samples varied from 10.7<br />
to 27.9μg-at/l, and it decreased from the surface to a depth <strong>of</strong> 200 m. Below this depth, no<br />
systematic variation was observed upto a depth <strong>of</strong> 2050 m where the values ranged from<br />
15.1 to 75.2 μg-at/l. The particulate silicon formed a small proportion <strong>of</strong> the total<br />
silicon as the concentrations <strong>of</strong> dissolved silicon increased with depth.<br />
6. Calcium phosphate saturation in sea water<br />
Water samples collected during the cruises <strong>of</strong> R.V. Gaveshani from the Andaman<br />
Sea were analysed and the preliminary examination <strong>of</strong> the data indicated that the trend<br />
<strong>of</strong> variation in the degree <strong>of</strong> saturation <strong>of</strong> sea water with respect to calcium phosphate is<br />
similar to that encountered elsewhere, i.e., about 50% saturation occurs in the surface<br />
layer and an undersaturation (about 10-15%) is found in deeper layers.<br />
Variations in calcium and magnesium along 5°N and between 86° and 99°E were<br />
also studied. The average values <strong>of</strong> Ca, Ca/Cl, Mg and Mg/Cl were found to be 409,<br />
21.36x10 -3<br />
, 1268 and 66.16xl0 -3<br />
mg/kg respectively. Higher Mg/Cl ratio was<br />
observed in this region as compared to the other areas <strong>of</strong> the northern Indian Ocean,<br />
presumably because <strong>of</strong> lower salinity. The calcium values, on the other hand, were<br />
comparatively low.<br />
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7. Studies on some major constituents in the estuarine regions<br />
Distribution <strong>of</strong> calcium, magnesium and sulphate was examined in the Mandovi-<br />
Zuari estuarine system. While the behaviour <strong>of</strong> calcium and magnesium was found to be<br />
semi-conservative probably due to the precipitation <strong>of</strong> these elements in biogeochemical<br />
cycles, sulphate was found to behave in a purely conservative manner, remaining in a<br />
steady state in the rivers. A 'simple mixture' relationship was applied to calculate the dilution<br />
and mixing processes in the rivers using calcium, magnesium and sulphate as indicators;<br />
it has been observed that the percentages <strong>of</strong> sea water in the estuarine regions <strong>of</strong><br />
Mandovi varied from 88-92 during the pre-monsoon, 12-23 during the monsoon and 78-<br />
79 during the post-monsoon seasons. The corresponding figures for Zuari are 94-99,<br />
27-43 and 79-91 respectively.<br />
8. Chemical special ion <strong>of</strong> important metals in the Mandovi estuary<br />
An attempt was made to determine the labile and organic fractions <strong>of</strong> cadmium,<br />
lead and copper in the Mandovi estuary using an anodic stripping voltameter (ASV). The<br />
results with each metal were as follows :<br />
Labile cadmium varied from 0.05 to 0.9 μg/l whereas the organically associated<br />
form was detected in the concentrations ranging from 0 to 0.83 μg/l. In general, the<br />
bottom waters contained a higher percentage <strong>of</strong> organically associated cadmium than<br />
the surface water. Both the forms decreased towards the fresh water zone <strong>of</strong> the Mandovi<br />
river.<br />
Labile lead was found to vary from 0.5 to 5 μg/l, while the organically associated<br />
form ranged from 0 to 2.5 μg/l. The concentration <strong>of</strong> both the forms remained more or<br />
less uniform in the upper reaches <strong>of</strong> the Mandovi river.<br />
The variations in labile copper and the organically associated form were found to<br />
range between 0-12.5 μg/l and 0.5-6 μg/l respectively. The values decreased towards<br />
the fresh water zone <strong>of</strong> the river.<br />
9. Phosphorus retention capacity <strong>of</strong> estuarine sediments<br />
Laboratory experiments were carried out to determine the phosphorus retention<br />
capacity <strong>of</strong> the estuarine sediments at pH 4, 7 and 10 at different added phosphorus concentrations-Samples<br />
<strong>of</strong> sediments collected were silty sand, silty clay and sandy silt with<br />
organic matter ranging from 5.21 to 13.58%. The amount <strong>of</strong> phosphorus retained in<br />
the sediment varied with pH rather than with the concentration <strong>of</strong> added phosphorus.<br />
Maximum retention could be observed at pH 4 and minimum at pH 10.<br />
10. Studies on organic constituents <strong>of</strong> sea water<br />
Investigations on dissolved amino acids in sea water were started during the<br />
current year. The amino acids are being estimated by densylation and characterisation<br />
by TLC. The method has been standardised and the R f values obtained agree with<br />
those reported from other parts <strong>of</strong> the oceans-<br />
The estimation <strong>of</strong> vitamin B 12 in the surface waters at the mouths <strong>of</strong> Mandovi<br />
and Zuari estuary, at the mouth <strong>of</strong> Sanquelim river and at upstream station near<br />
30
Sanvordem was carried out. The results obtained are tabulated below:<br />
Concentration <strong>of</strong> vitamin B 12 (μg/l)<br />
Station Minimum Maximum<br />
Mouth <strong>of</strong> Mandovi estuary 0.4 7.0<br />
Mouth <strong>of</strong> Zuari estuary 0.2 1..1<br />
Mouth <strong>of</strong> Sanquelim river 0 2.5<br />
Near Sanvordem 0.4 6.5<br />
11. Studies on halides (other than chlorides) in sea water<br />
During the year, studies on the chemistry <strong>of</strong> halogen compounds (other than chlorides)<br />
in the estuarine and nearshore regions <strong>of</strong> Goa were started. Analytical methods for<br />
fluoride and bromide have been standardised and suitable techniques for the determination<br />
<strong>of</strong> iodide and iodates have been developed. Samples from the two stations along the<br />
MONEX track in the Arabian Sea have been analysed for bromide and the results are<br />
being processed.<br />
12.. Solar dryer for marine and farm products<br />
Keeping the basic configuration similar to that <strong>of</strong> a multi-surface solar still developed<br />
earlier at this <strong>Institute</strong>, a cabinet type solar dryer to be used for farm products<br />
has been developed. The working model <strong>of</strong> this dryer has 0.5 m 2 <strong>of</strong> floor area and is<br />
capable <strong>of</strong> drying 50 large sizedcoconuts in about 48 hours, whereas the open Sun drying<br />
<strong>of</strong> the same number <strong>of</strong> coconuts takes about 9 days. However, for drying <strong>of</strong> grapes<br />
and red chillies the dehydration period was found to be about 72 hours. One <strong>of</strong> the<br />
important features <strong>of</strong> this design is its detachable metallic hanger which accelerates the<br />
process. The feasibility for drying marine products (fish, shrimps, etc.) is also being<br />
undertaken in this solar dryer.<br />
The solar dryer and the solar still developed at the <strong>Institute</strong> have received excellent<br />
public response. Several government and private agencies have shown interest in these<br />
devices and a number <strong>of</strong> units have already been supplied to several organizations.<br />
13. Studies in Cochin backwaters<br />
Work under this investigation was carried out at Regional Centre, Cochin.<br />
3.2.2 Drugs from the sea<br />
1. Screening <strong>of</strong> marine organisms<br />
Some marine organisms from the Andaman Sea were screened and the extracts<br />
have been prepared for a preliminary testing. Antiviral activity observed in Codium<br />
elongatum has been located in the water soluble fraction. The activity appears to be<br />
localized in the polysaccharide fraction. Further work on the identification <strong>of</strong> the<br />
polysaccharide is in progress.<br />
Acantophora specifera, Sargassum tenerrimum, Acanthus illicifolius and Porites<br />
lutea have been fractionated for the confirmation <strong>of</strong> drug activity observed in them.<br />
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2. Chemical investigation on marine organisms<br />
Two more new diterpenes, acetate and ketone coriesponding to the diterpencalcohol,<br />
stoechospermol have been isolated from Stoechospermum marginatum. The<br />
identity has been confirmed by the superimposibility <strong>of</strong> IR spectra and R f values with<br />
the authentic samples. Reactions are also being carried out for the confirmation <strong>of</strong> the<br />
structure assigned to stoechospermol.<br />
Petroleum ether extract <strong>of</strong> the coral Porites lutea led to the isolation <strong>of</strong> four<br />
major and some minor compounds. Two <strong>of</strong> the major compounds were identified as<br />
steroid and brassicasterol based on GC-MS spectral data and the lipid n-batylalcohol<br />
based on NMR data.<br />
Petroleum ether extract <strong>of</strong> Acantophora specifera led to the isolation <strong>of</strong> a number<br />
<strong>of</strong> crystalline compounds, the spectral data <strong>of</strong> which arc being collected.<br />
Methylene chloride extract <strong>of</strong> the sponge Ircinia ramosa on chromatography<br />
gave a resinous sticky material which was acetylated to give acetate. Further work<br />
on the isolation <strong>of</strong> this acetate is in progress.<br />
Chemical studies on Chondria armata which was found to contain bromine in<br />
high concentration and was toxic to mice, have resulted in the isolation <strong>of</strong> several<br />
new bromo-compounds which are expected to have unusual structures. The structures<br />
<strong>of</strong> these compounds are being finalised from the spectroscopic data and chemical<br />
evidences.<br />
3. Studies on algal polysaccharides and histamine<br />
Sulphated polysaccharides were isolated from Hypnea cervicornis, Chondrococcus<br />
and Acantophora specifera and the carbohydrate end sulphate content <strong>of</strong><br />
these polysaccharides were studied. Further, polysaccharides from these algae have<br />
been sent to Central Drug Research <strong>Institute</strong>, Lucknow for inflammatory, cardiovascular<br />
and isolated ileum tests. A chromatographic method has been standardized for the<br />
detection <strong>of</strong> histamine, a biogenic amine which causes contraction <strong>of</strong> smooth muscles,<br />
dilation <strong>of</strong> capillaries and secretion <strong>of</strong> hydrochloric acid by the gastric glands using<br />
cellulose layers <strong>of</strong> 500 μm thickness and ninhydrin as the detecting agent. This<br />
32
particular substance has been detected in Caulerpa racemosa (hypotensive), Padina<br />
tetrastomatica (spasmogenic), Corallina (spasmogenic) and Chondria armata (spasmogenic).<br />
It is to be confirmed whether the activity reported is due to the presence<br />
<strong>of</strong> histamine. The extracts <strong>of</strong> Sargassum tenerrimum, Galaxaura elongata, Galaxaura<br />
rugosa, Ulva reticulata, Chondrococcus sp. and Codium elongatum were found to be<br />
devoid <strong>of</strong> histamine.<br />
4. Halogens in algae<br />
Iodine and bromine contents were measured in 16 species <strong>of</strong> red, brown and<br />
green algae. In all the species examined the concentration <strong>of</strong> iodine was found to be<br />
lower than that <strong>of</strong> the bromine. Phaeophyta and Rhodophyta were found to be<br />
relatively richer in both these elements. The iodine concentration varied from 0.003<br />
to 0.119% and bromine from 0.008 to 0.128%.<br />
3.2.3 Protection <strong>of</strong> marine environment and monitoring <strong>of</strong> pollutants along the Indian coast<br />
The studies under this project were carried out partly from headquarters and<br />
partly from Regional Centres, Cochin and Bombay.<br />
1. Monitoring <strong>of</strong> petroleum hydrocarbons in the marine environment<br />
Two cruises were carried out along the oil tanker routes across the southern<br />
Bay <strong>of</strong> Bengal from south <strong>of</strong> Sri Lanka to the head <strong>of</strong> the Malacca Strait. The area<br />
traversed was between 5°30' to 6°30'N latitude and 78°00' to 98°30'E longitude.<br />
A part <strong>of</strong> the Andaman Sea was also surveyed. The components observed were: oil<br />
slicks, floating pollutants, particulate petroleum residues (tar balls) and dissolved/<br />
dispersed hydrocarbons.<br />
Depthwise mean concentration in μg/kg <strong>of</strong> dissolved/dispersed petroleum hydrocarbons<br />
along the oil tanker route in the Arabian Sea and Bay <strong>of</strong>.Bengal are as<br />
follows:<br />
Arabian Sea (μg/kg) Bay <strong>of</strong> Bengal (μg/kg)<br />
Depth Mean Range Mean Range<br />
0 m 35.3 0-395 29.1 4-229<br />
10 m 30.6 3-217 25.1 2-147<br />
20 m 29.4 2-112 17.6 1-75<br />
Mean 32.5 Mean 24.1<br />
Computation on the total volume <strong>of</strong> petroleum hydrocarbons in the upper<br />
20 m <strong>of</strong> the Arabian Sea and the southern Bay <strong>of</strong> Bengal gave figures <strong>of</strong> 4 x 10 6<br />
and 0.4 x 10 6<br />
tonnes respectively.<br />
2. Laboratory studies on biodegradation<br />
Investigations have been initiated to isolate tar-degrading organisms by sequential<br />
degradation method. Laboratory studies gave encouraging results but field<br />
trials on the tar deposition on beaches presented some difficulties due to wind and<br />
surf activities. Modifications are being tried to overcome these problems.<br />
33
Twentyfour hydrocarbon-utilizing strains <strong>of</strong> bacteria were screened for their<br />
ability to utilize different types <strong>of</strong> hydrocarbons. Arthrobacter and Candida spp.<br />
gave a broad spectrum <strong>of</strong> hydrocarbon utilizing pr<strong>of</strong>ile. An examination <strong>of</strong> their<br />
capacities to degrade Saudi Arabian and Bombay High crudes, showed that they could<br />
degrade 16-20% <strong>of</strong> the former and 50-70% <strong>of</strong> the latter crude. Column and gas<br />
chromatographic studies revealed that these two bacterial strains preferentially degrade<br />
n-alkane fractions from C 11 to C 35 in both the crudes as compared with their aromatic<br />
and polar fractions.<br />
Five chemical dispersants <strong>of</strong> Indian make and two <strong>of</strong> foreign make were tested<br />
individually and in combination with the crude oil for their biodegradability <strong>of</strong> natural<br />
microbial population. Only one dispersant was found to be toxic to the microbes.<br />
All <strong>of</strong> the dispersants, either alone or in combination with the oil, supported<br />
a good growth <strong>of</strong> bacteria. The oil by itself was toxic to the bacteria, and all the<br />
oil-dispersant mixtures reduced the rate <strong>of</strong> biodegradation. Biodegradability <strong>of</strong> oildispersant<br />
mixtures, using natural population <strong>of</strong> marine bacteria, ranged from 19.6<br />
to 46.4%. Testing and evaluation <strong>of</strong> 5 indigenously manufactured chemical dispersants<br />
for their efficiency in the removal <strong>of</strong> spilled oil under Indian conditions were also<br />
conducted. The tests carried out were: solubility, BOD, COD, dispersing capacity,<br />
emulsion stability, biodegradability and toxicity. All the dispersants were found to<br />
be quite efficient in oil removal. The addition <strong>of</strong> dispersants in excess <strong>of</strong> about onetenth<br />
<strong>of</strong> the volume <strong>of</strong> oil did not increase the efficiency. Static bioassay tests, using<br />
the green mussel, Mytilus viridis, for both oil and oil-dispersant mixtures indicated<br />
that, excepting one all the other dispersants were fairly non-toxic. LC 50 values<br />
for 24 and 48 hrs were greater than 7500 ppm for four dispersants. However, 96hour<br />
LC 50 values decreased by about 30% from those <strong>of</strong> the 48-hour values. The<br />
oil-dispersant mixture was found to be less toxic than the dispersant alone. It was<br />
thus concluded that these four indigenously manufactured d ispersants should be fairly<br />
safe in our marine environment and that in the event <strong>of</strong> an accidental oil-spill they<br />
should be used.<br />
3. Toxic and non-toxic heavy metals in sea water and marine organisms<br />
Analysis for copper, iron, manganese, zinc, nickel, cobalt, mercury, lead and<br />
cadmium was carried on samples <strong>of</strong> water and paniculate matter collected from<br />
depths upto 1500 metres and zooplankton and fish samples collected from the southern<br />
Bay <strong>of</strong> Bengal and the Andaman Sea.<br />
Depthwise variations <strong>of</strong> all metals in dissolved and particulate forms were<br />
observed to vary according to the redox condition <strong>of</strong> water and the characteristics<br />
<strong>of</strong> different watermasses. The ranges <strong>of</strong> concentrations <strong>of</strong> dissolved fractions<br />
were: Cu 1-5: Fe 2-21.7; Mn 1.5-24.7; Zn 1.2-12.8; Ni 0-1; Co 0-1; Pb 0.25-7.5 and<br />
Cd 0.15-1.9 μg/l. The particulate fractions were: Cu ND (non-detectable)-104; Fe<br />
49-3100; Mn 0-64; Zn 17-1060; Ni ND; Co ND; Pb 0-250 and Cd ND-25 μg/g<br />
wet weight.<br />
Concentration <strong>of</strong> all the metals in water were within the acceptable range and<br />
the concentrations in zooplankton and fishes also did not exceed the accepted limit.<br />
34
4. Monitoring activities in and around Goa<br />
Monthly monitoring activities <strong>of</strong> several environmental parameters have been<br />
initiated in the rivers Mandovi and Zuari. Four stations extending from the salt water<br />
to the fresh water zones in both the rivers were sampled at mid-depth. The parameters<br />
monitored were: pH, O2, temperature, salinity/chlorinity, Ca 2+ , Mg 2+ , SO4 2- , F - ,<br />
PO4 3- -P, NO3 - -N, Hg, Mn and Fe. The last three parameters were monitored in all<br />
the three phases (dissolved, particulate and sediments)<br />
Monitoring activities were continued in the Velsao Bay also for the different<br />
forms <strong>of</strong> nitrogen compounds.<br />
5. Pollution monitoring along the Kerala coast<br />
Studies carried out under this investigation are reported separately under<br />
Section 3.8.1.<br />
6. Marine environmental monitoring along the Bombay coast.<br />
The details <strong>of</strong> this investigation are given under Section 3.8.2.<br />
3.2.4 Characteristics <strong>of</strong> the estuarine regions <strong>of</strong> major rivers <strong>of</strong> India<br />
A new multi-disciplinary project to survey the environmental features in the<br />
estuarine region <strong>of</strong> 7 major Indian rivers was initiated during the year. One set <strong>of</strong><br />
observations has been completed in September, <strong>1980</strong> in the estuarine region <strong>of</strong> the<br />
river Hooghly, from Diamond Harbour to Sandheads (a distance <strong>of</strong> approximately<br />
60 nautical miles) and also at a station <strong>of</strong>f the mouth <strong>of</strong> the river Mahanadi.<br />
Each station was worked over a tidal cycle <strong>of</strong> 12 hours to measure temperature,<br />
salinity, current speed, current direction, dissolved oxygen, phosphate-phosphorus,<br />
nitrate-nitrogen, ammonia.-nitrogen and suspended solids. The nutrients, dissolved<br />
oxygen and suspended solids were measured at individual collection every 3 hours<br />
at 3 depths. A composite sample at mid-depth over the tidal period was also collected.<br />
Current direction at the Diamond Harbour was SE-NNW (134°-344°) turning<br />
210° over the tidal cycle. The values at Haldia were SE-ENE (222°-071°) turning<br />
151° and at Sagar SW-SSE to N-NNE (192°-011°) turning 179° over the tidal cycle.<br />
This shows that the currents turned almost 180° at all the stations. At the Diamond<br />
Harbour and Haldia, salinity values were 0.09 and 0.8l%o respectively, while at Sagar<br />
during the ebb tide, a layer <strong>of</strong> low salinity water <strong>of</strong> about 8%o was observed in<br />
the upper 7 metres. Similarly a layer <strong>of</strong> a higher salinity water <strong>of</strong> about 14%o upto<br />
15 metres depths was observed.<br />
Comparing the nutrient values with tidal fluctuation, it was observed that in<br />
general, at all the 3 stations, the values were higher during the ebb tide and lower<br />
during the flood tide indicating a net transport <strong>of</strong> the nutrients seawards. However,<br />
a proportionate increase <strong>of</strong> these values was not observed at the Sandheads station. This<br />
probably indicates that a major portion <strong>of</strong> the nutrients along with the enormous<br />
35
amount <strong>of</strong> silt gets carried away by the rivers. It settles at the junction <strong>of</strong> the river<br />
and sea water.<br />
Samples were also collected for the analysis <strong>of</strong> calcium, magnesium, sulphate,<br />
dissolved and particulate fraction <strong>of</strong> several toxic and non-toxic heavy metals and<br />
these are being processed. . .<br />
A preliminary examination <strong>of</strong> the zooplankton samples collected every 3 hours<br />
at all the stations showed an abundance <strong>of</strong> prawn larvae together with a number <strong>of</strong><br />
fish larvae, which are yet to be identified. Some <strong>of</strong> them appear to belong to the<br />
family Clupeidae.<br />
36
3.3<br />
Geological <strong>Oceanography</strong><br />
3.3.1 Geological and geophysical surveys to assess the petroleum and<br />
mineral prospects <strong>of</strong> the continental margins <strong>of</strong> India<br />
3.3.2 Regional geology and manganese nodule deposits in the Arabian Sea<br />
and Central basin <strong>of</strong> the Indian Ocean<br />
3.3.3 Geochemistry <strong>of</strong> the sediments <strong>of</strong> the continental margins <strong>of</strong> India<br />
3.3.4 Sediments <strong>of</strong> the western continental margin <strong>of</strong> India<br />
3.3.5 Foraminifera as indicators <strong>of</strong> pollution in the marine environment<br />
Detailed studies are being made on the continental margins, marginal base,<br />
morphology <strong>of</strong> the sea floor (Arabian Sea, Bay <strong>of</strong> Bengal and Central basin <strong>of</strong> the<br />
Indian Ocean) and its underlying structures as well as on the physical and chemical<br />
properties <strong>of</strong> the sediments, to determine mineral and petroleum prospects. Foraminifera<br />
in relation to pollution formed the part <strong>of</strong> the studies. Work was carried<br />
out on five projects as follows:<br />
3 3.1 Geological and geophysical surveys to assess the petroleum and mineral prospects<br />
<strong>of</strong> the continental margins <strong>of</strong> India<br />
Geological and geophysical studies were carried out on the continental margins<br />
<strong>of</strong>f Mormugao, Mangalore, Cochin and Bombay and these covered 3036 line km <strong>of</strong><br />
echosounding, 972 line km <strong>of</strong> side scan sonar, 1873 line km <strong>of</strong> shallow seismic pr<strong>of</strong>iling<br />
and 2462 line km <strong>of</strong> magnetic surveys. Underwater camera was also operated<br />
at 16 stations. The work dene on the various topics is described below:<br />
(1) Geomorphology<br />
(a) Mormugao to Cochin: The continental shelf upto a depth <strong>of</strong> about 40m<br />
but in some areas upto 25 m only (Off Cochin) is marked by an even topography<br />
due to clay cover. Beyond this depth, the topography is uneven and on the shelf <strong>of</strong>f<br />
Cochin, at a depth <strong>of</strong> about 50 m, a series <strong>of</strong> pinnacles and ridges are prominent<br />
and another set <strong>of</strong> ridges is seen before the shelf-break. A rock outcrop <strong>of</strong>f Netrani<br />
Island identified on the echogram and also from seismic and magnetic records followed<br />
by dredging was found to be amphibolite, indicating that the ancient rocks <strong>of</strong><br />
Dharwar extend upto the middle <strong>of</strong> the shelf with a thin sediment cover. A pro-<br />
37
minent 30-35 km wide flat terrace at a depth range 350-400m <strong>of</strong>f Quilon and a ridge<br />
<strong>of</strong> about 700 m <strong>of</strong>f Cochin were recorded.<br />
(b) Off Bombay: The shelf-break in the area occurs at a depth <strong>of</strong> about 97 m<br />
and 210-270 km from the shore. The shelf upto a depth range <strong>of</strong> 60 to 75 m and<br />
from 115 to 130 km away from the coast is marked by an even topography. Beyond<br />
these depths, the topography is uneven and is marked by numerous pinnacles. Isolated<br />
basins <strong>of</strong> even topography are also seen at some places·<br />
(c) Lakshadweep: Geomorphological maps <strong>of</strong> Chetlat, Kiltan, Bitra, Kadmat<br />
and Amini atolls were prepared. The maps indicate that the reef is wider on the<br />
windward, i.e., W, NW and SW side than on the leeward eastern side. The reef on<br />
the windward side is marked by a number <strong>of</strong> prominent terraces which probably<br />
indicate the changes in the sea level or the stages in the growth <strong>of</strong> the reef. The<br />
sand ridges and gravel trains indicate that in most <strong>of</strong> the lagoons and on the windward<br />
side, the direction <strong>of</strong> the sediments is SW to NE. In some lagoons, due to<br />
wave refraction, the direction <strong>of</strong> sediment movement is from NW to SE also. The<br />
radio carbon dates <strong>of</strong> the storm beaches range from modern to 2975 ± 1000.<br />
BP and indicate clustering between 3000 to 2000 BP and from present to 500 BP.<br />
The younger storm beaches towards the shore suggest that parts <strong>of</strong> the islands have<br />
grown by about 30 m in the last 2780 years (Chetlat), 120 m in 1620 years (Kiltan)<br />
and about 100m in 470 years (Minicoy). The absence <strong>of</strong> the storm beaches on some<br />
<strong>of</strong> the islands, younger beaches towards the shore and clustering <strong>of</strong> ages and the<br />
lack <strong>of</strong> lateral and chronological continuity can be explained by periodic stormy<br />
conditions rather than by the changes in the sea level. The number <strong>of</strong> storms in the<br />
Arabian Sea has varied from a minimum <strong>of</strong> 1 in 1949 to 10 in 1893, 1926 and 1930.<br />
It is very likely that such changes would have occurred in the past also.<br />
2. Surficial Geology<br />
(a) Off Mormugao-Mangalore: More than 10 m thick clay was observed near<br />
the coast which thins out beyond 40 m depth and the underlying sands are exposed<br />
on the outershelf. Seismic records show that about 3 m acoustically transparent<br />
clay overlays a reflector. Another undulating reflector at about 10 m is also seen.<br />
(b) Off Cochin-Quilon: The shelf between the depths <strong>of</strong> about 25 to 40 m is<br />
covered with clays and beyond this depth, sand is exposed. On the outer shelf,<br />
prominent reflectors are seen at 35-40m and 50-60 m depth ranges which apparently<br />
dip seawards. At the shelf edge, a number <strong>of</strong> transparent layers are present.<br />
Their formations have a low dip at the shelf edge which steepens along the slope<br />
and some <strong>of</strong> the formations are underlain by transparent horizons. The slope appears<br />
to be disturbed and faulted with many anticlinical features some <strong>of</strong> which lie<br />
at a depth <strong>of</strong> about 300 m. On the upper slope, a prominent synclinal depression<br />
with about 150 m thick sediments is seen. This is followed seaward by an uplift and an<br />
anticline. The outer slope is marked by a well-defined faulted trough followed by a<br />
ridge rising to about 400 m. Beyond this depth another depression occurs.<br />
38
Seismic pr<strong>of</strong>ile (4.5 kjl sparker) on the continental slope <strong>of</strong>f Cochin.<br />
(c) Off Bombay: In this region the clay is about 15 m thick near the shore<br />
and at about 20 m depth. It thins out to less than one metre at about 70 m depth<br />
at a distance <strong>of</strong> about 140 km from the coast. The transparent layer in this region<br />
reaches a maximum thickness <strong>of</strong> 50 to 60 m. Based on seismic records, four strata <strong>of</strong><br />
different ages are recognisable. A depression is seen at about 90 m depth and a series<br />
<strong>of</strong> faults are also noticed on the edge <strong>of</strong> the continental shelf.<br />
3. Acoustic masking due to gases<br />
The shallow seismic and echosounding records <strong>of</strong> the clays on the inner and<br />
middle shelf <strong>of</strong>f Bombay, Konkan, Karnataka and Kerala are marked by turbidity.<br />
In some cases, the turbidity which is due to acoustic masking by gases extends over<br />
50 to 60 km and covers more than 2500 km 2 . The cores collected in the area show<br />
bubbles and fissures in the turbid zone. The gas from these bubbles and fissures<br />
was predominantly methane with traces <strong>of</strong> higher hydrocarbons. The gases were formed<br />
by the degradation <strong>of</strong> large quantities <strong>of</strong> organic matter produced by increased<br />
productivity or because <strong>of</strong> a greater influx <strong>of</strong> organic matter on the recent past.<br />
4. Magnetics<br />
(a) Off Cochin: The nearshore area between Cochin and Quilon is marked<br />
by a few high amplitude anomalies (about 200-300 gammas). Besides these anomalies,<br />
the rest <strong>of</strong> the shelf and slope appears to be magnetically smooth. Over the<br />
39
terrace (350-400m depth range), a broad wave length <strong>of</strong> low amplitude (100 gammas)<br />
anomaly was observed.<br />
(b) Off Mangalore: The total magnetic intensity map <strong>of</strong> the area shows that<br />
the inner shelf upto a depth <strong>of</strong> 50 m is marked by a series <strong>of</strong> magnetic lows and<br />
highs while the outer shelf is magnetically smooth. The acidic rocks reported from<br />
the islands are perhaps intruded in the Dharwar and probably the magnetic susceptibility<br />
contrasts between the rock types coupled with an uneven topography resulting<br />
in magnetic lows and highs. The nearshore (30 m depth) anomalies (highs) may be<br />
due to some intrusive bodies at a depth <strong>of</strong> about 1.5 to 2 km.<br />
(c) Off Vengurla: The total magaetic and residual anomaly maps show a<br />
NNW-SSE to N-S trend. These depict the trends <strong>of</strong> Dharwars in the adjacent coastal<br />
areas and tectonic movements which occurred later on along the NS weak zones in the<br />
basement. Short wave length, high frequency anomalies in the near coastal area upto<br />
a distance <strong>of</strong> 10 km and a depth <strong>of</strong> about 35-40m indicate the <strong>of</strong>fshore extension <strong>of</strong><br />
the basement at a shallow depth. Beyond 35-40 m depth, the basement is probably<br />
deeper.<br />
(d) Direction Bank: The total magnetic anomaly map shows a NNW-SSE<br />
trending high (about 250 gammas) on the bank bordered by a prominent low to<br />
the east. North <strong>of</strong> the Bank, a magnetic flat area with E-W trending features is<br />
seen and further to the north a series <strong>of</strong> N-S highs and lows are seen. The Direction<br />
Bank appears to be a NNW-SSE trending structure with a faulted eastern flank.<br />
The depth at the magnetic source on the Bank is around 1.5 km. The short period,<br />
high frequency anomalies near the coast extend from a depth <strong>of</strong> about 20 m to<br />
about 50 m. for a distance <strong>of</strong> approximately 15 km and these may be due to a cluster<br />
<strong>of</strong> dykes.<br />
(e) Off Bombay: The magnetic pr<strong>of</strong>iles indicate more or less similar trends<br />
as those found along the Direction Bank. At some places, anomalies <strong>of</strong> the order <strong>of</strong><br />
200 gammas are noted which may be due to a basement uplift. In all the pr<strong>of</strong>iles, a<br />
broad anomaly is seen which may be due to some intrusion.<br />
5. Exploration <strong>of</strong> ilmenite placers <strong>of</strong>f the Konkan Coast<br />
The exploration <strong>of</strong> ilmenite placers was extended during the year to Vetye.<br />
Ambolgarh, Rajapur and Vijaydurg bays and more than 200 samples were collected from<br />
an area <strong>of</strong> 13 km 2 , 1870 line km <strong>of</strong> echosounding, 571 line km <strong>of</strong> seismic pr<strong>of</strong>iling<br />
and 672 line km <strong>of</strong> magnetic survey were carried out from Jaigad to Vijaydurg. A total<br />
magnetic intensity map <strong>of</strong> the northern part <strong>of</strong> the area was prepared on a<br />
100 gamma-interval. The map shows N-S trends with a number <strong>of</strong> closures. The<br />
conspicuous feature <strong>of</strong> the map is the two major NNW-SSE lineation. These appear<br />
to be the two major faults/fractures extending from land to <strong>of</strong>fshore. Seismic<br />
records show that the sand cover is about 4 m thick in most <strong>of</strong> the bays and extends<br />
below the clay upto a depth <strong>of</strong> 15 to 17 m beyond which a change in the reflector is<br />
observed. This was confirmed by obtaining more than 50 piston gravity cores.<br />
40
In the Ratnagiri, Mirya and Kalbadevi bays, the reserves <strong>of</strong> ilmenite upto<br />
a depth <strong>of</strong> 1 m were inferred to be 2 million tonnes. With the thickness <strong>of</strong> sand<br />
indicated by seismic records to be 21 m and with their probable extension upto the depths<br />
<strong>of</strong> 15 to 17 m, the total reserves in the other 13 bays may be many times greater. The<br />
extensive data collected during these surveys are being analysed and processed.<br />
The other organisations which collaborated in this project were the Oil &<br />
Natural Gas Commission, Geological Survey <strong>of</strong> India, <strong>National</strong> Geophysical Research<br />
<strong>Institute</strong>, Regional Research Laboratory (Bhubaneshwar), Physical Research Laboratory<br />
and the Birbal Sahni <strong>Institute</strong> <strong>of</strong> Paleobotany.<br />
3.3.2 Regional geology and manganese nodule deposits in the Arabian Sea and Central<br />
Basin <strong>of</strong> the Indian Ocean<br />
Necessary equipment such as Free Fall Grab, Boomerang grab, Radio marker,<br />
Underwater camera and Direction finder etc. for sampling and photographing the<br />
manganese nodules have been procured. The deep sea grabs and dredges have been<br />
designed and fabricated. A double beam atomic absorption spectrophotometer is<br />
being installed for the analyses <strong>of</strong> the samples. Based on the analyses <strong>of</strong> the data<br />
collected earlier, a cruise plan has been finalised.<br />
3 33 Geochemistry <strong>of</strong> the sediments <strong>of</strong> the continental margins <strong>of</strong> India<br />
Geochemical studies were continued on the sediment samples collected from<br />
the western continental margin between Ratnagiri and Mangalore, Mangalore and<br />
Cochin and from the eastern shelf between Ganges and Calimere Point. The findings<br />
<strong>of</strong> these studies are briefly given below.<br />
1. Western continental margin<br />
(a) Ratnagiri-Mangalore: In the bulk samples Si, Al, K, Na. Mg, Fe, Mn,<br />
Li, Cu, Co, Ni and Zn decrease while Ca and Sr increase as we move away<br />
from the coast but phosphorus does not show any distinct trend. The distribution<br />
<strong>of</strong> the elements in the HCl soluble leaches clearly indicates that the major portion<br />
<strong>of</strong> these elements is held in the clays. This is also confirmed by the strong correlation<br />
between Al and Fe, K, Na, and Mg. Negligible amounts <strong>of</strong> elements in the<br />
acetic acid leaches indicate that the adsorption by clay minerals and the Carbonate<br />
phase are not the significant factors for the fixation <strong>of</strong> the elements in these sediments.<br />
SiO2 content in these sediments is significantly less than the other nearshore<br />
sediments. This is mainly contributed by detrital quartz as indicated by the lack <strong>of</strong><br />
correlation between Al and Si.<br />
The outer shelf sediments are carbonate rich (75%) and biogenous while in<br />
contrast to the outer shelf, carbonate sediments in the northern part <strong>of</strong> the study<br />
area is oolitic in nature. Similarly, phosphorus in this area is associated with<br />
organic matter as indicated by the strong correlation between P2O5 and organic<br />
matter while in the northwestern region it is associated with carbonates.<br />
(b) Mangalore-Cochin: The concentration <strong>of</strong> Al, Mn, Cu and Zn in the bulk.<br />
41
sample is high in the inner shelf terrigenous sediments and low in the outer shelf and<br />
continental slope sediments. In contrast to the shelf between Ratnagiri-Mangalore,<br />
in this region the concentration <strong>of</strong> Si and Ni is higher in the outershelf than the<br />
nearshore and slope sediments. The partition patterns <strong>of</strong> Al show that Al is mainly<br />
held in the HCl soluble fraction and to a small extent in the HCl insoluble residue<br />
indicating that the clay minerals are the major contributors for Al.<br />
2. Eastern continental margin between Ganges-Calimere point<br />
Fractionation studies <strong>of</strong> Fe show that the major portion <strong>of</strong> Fe is held in the<br />
clay minerals. However, higher concentrations <strong>of</strong> Fe are associated with the terrigenous<br />
sediments <strong>of</strong> the Visakhapatnam-Calimere Point than the sediments <strong>of</strong> the<br />
Ganges shelf. The acetic acid leaches <strong>of</strong> the sediments from the Ganges shelf contain<br />
higher Fe than that <strong>of</strong> the sediments <strong>of</strong> the other region suggesting that adsorption<br />
by clays is an important factor in the fixation <strong>of</strong> Fe in these sediments. Reducible<br />
iron oxides are higher in the sediments <strong>of</strong> the shelf between Visakhapatnam-Calimere<br />
Point in the sediments <strong>of</strong> the Ganges shelf which indicate favourable conditions for<br />
the formation <strong>of</strong> iron oxides.<br />
3.3.4 Sediments <strong>of</strong> the western continental margin <strong>of</strong> India<br />
The surface sediment distribution map <strong>of</strong> the western continental shelf <strong>of</strong><br />
India was prepared. Relatively small parts <strong>of</strong> the continental shelf have remained to<br />
be studied but they are unlikely to alter significantly the general conclusions regarding<br />
the texture, mineral composition, origin, age and sediment dynamics that have already<br />
been reported.<br />
1. Sediment dynamics and transport<br />
A comparative study <strong>of</strong> the topography and sediment dynamics <strong>of</strong> the region<br />
surrounding Cape Comorin was completed. The western side <strong>of</strong> the Cape is dominated<br />
by terrigenous sediments while the eastern side (the shelf fringing the Gulf<br />
<strong>of</strong> Mannar) is dominated by carbonate sediments. Despite being a relatively sheltered<br />
environment, as compared to the open ocean environment on the west, the eastern<br />
part shows active sediment transport as evidenced by the presence <strong>of</strong> sand waves and<br />
ripples on the sea bed. The shelf from Quilon to Cape Comorin is potentially important<br />
for quartz sands and heavy minerals.<br />
Studies <strong>of</strong> the relative variation <strong>of</strong> kaclinite, montmorillonite and chlorite over<br />
a distance <strong>of</strong> about 1000 km on the continental shelf are in progress to understand the<br />
regional transport <strong>of</strong> fine-grained sediments and the influence <strong>of</strong> the monsoon currents<br />
flowing towards south on this transport.<br />
2. X-ray diffraction studies <strong>of</strong> limestone and carbonate sediments<br />
Limestone dredged from the shelf from a depth <strong>of</strong> 90 m were analysed by<br />
X-ray diffraction and it was found that its mineralogy does not indicate its exposures<br />
to fresh water cither from rainfall or due to percolating ground-water. These<br />
42
esults support the earlier findings that peninsular India had a semiarid climate in<br />
the past. Further studies on this subject are in progress.<br />
The X-ray analysis <strong>of</strong> the carbonate sediments shows that its organic constituents<br />
determine its overall mineralogy. Thus, where the benthic foraminifera are<br />
abundant, high-magnesium calcite is the prominent mineral and where molluscs or<br />
corals are found in larger proportions than others, aragonite is the prominent mineral.<br />
These studies are relevant to the problem <strong>of</strong> diagenetic changes taking place in<br />
the hydrocarbon-bearing limestones. Such diagenetic changes determine the porosity<br />
and permeability <strong>of</strong> carbonate reservoir rocks and in turn indicate the recovery <strong>of</strong><br />
hydrocarbons.<br />
3. Calcareous nannoplankton<br />
Sediment samples collected from the north western continental shelf <strong>of</strong> India<br />
during the Oceanovex programme (INS Darshak) 1973-74 were analysed. Of the<br />
total 16 species encountered, Gephyrocapsa oceanica was the most predominant<br />
whereas Emiliania huxley which is supposed to be the most abundant species in the<br />
modern seas was poorly distributed. This implies that the nannoplankton at present<br />
are subjected to predation by some other group <strong>of</strong> animals, possibly zooplantkton.<br />
The presence <strong>of</strong> G. oceanica in abundance is attributed to the relict sediment as<br />
pleistocene was its acme zone. Studies are also in progress on the variation and<br />
correlation <strong>of</strong> nannoplankton from five cores collected from the outer continental<br />
shelf <strong>of</strong>f Kerala.<br />
3.3.5 Foraminifera as indicators <strong>of</strong> pollution in the marine environment<br />
1. Foraminiferal distribution<br />
Studies <strong>of</strong> the distribution and ecology <strong>of</strong> foraminifera from Ratnagiri to<br />
Mangalore are in an advanced stage and 78 species have already been identified.<br />
The cluster analysis <strong>of</strong> foraminiferal population from Ratnagiri have led to the demarcation<br />
<strong>of</strong> two biotops.<br />
Samples from Direction Bank are being processed for the identification and<br />
estimation <strong>of</strong> organic carbon in the sediment.<br />
Virgulinella sp. which was common in Miocene and Pliocene sediments <strong>of</strong> the<br />
world was living in the present day sediments also 133 samples from the western<br />
shelf and slope and from a part <strong>of</strong> the eastern shelf were studied for the distribution and<br />
ecology <strong>of</strong> this species and its comparison with others. This species is dominant<br />
in 10-60 m depth and its maximum occurrence is in the area between Vengurla to<br />
Mangalore. Organic carbon and substrate appears to be the chief controlling factor<br />
in its distribution.<br />
Planktonic (14) and benthonic (42) foraminiferal species encountered from<br />
Deep Lake Terraces, Vestfold Hills <strong>of</strong> Antarctica revealed disparity in the abundance<br />
and dissolution effects was quite marked in certain genera.<br />
43
2. Effluent discharge sites studies<br />
Foraminifera from four effluent discharge sites, viz., Thana Creek, Cola Bay,<br />
Karwar and Trivandrum were studied. The magnitude <strong>of</strong> corrosive effect, diminishing<br />
ornamentation, deepening <strong>of</strong> grooves and sutural thickenings, enlargement <strong>of</strong><br />
pores, widening <strong>of</strong> apertures in foraminifera were taken as indices <strong>of</strong> pollution effect.<br />
The results reveal the effects <strong>of</strong> pollutants on both living and dead foraminifera.<br />
Living/dead ratio was negatively oriented at all sites.<br />
3. Organic carbon and foraminifera<br />
Quantitative analysis <strong>of</strong> organic carbon in the sediment and relation to foraminiferal<br />
assemblage in three regions, <strong>of</strong>f Karwar, Vengurla-Dabhol sector and<br />
Bombay-Daman indicate that Ammobaculites and Ammonia have positive correlation<br />
while miliolids (Quinqueloqulina, Spioloculina and Triloculina), Florilus-Nonion and<br />
Nonionella show negative correlation. The relationship between total foraminifera and<br />
organic carbon at Cola Bay is inversely proportional. In Gulf <strong>of</strong> Kutch, it is inconsistent<br />
due to very low values.<br />
44
3.4<br />
Biological <strong>Oceanography</strong><br />
3.4.1 Survey <strong>of</strong> biological resources in the seas around India<br />
3.4.2 Coastal aquaculture<br />
3.4.3 Biogeographical, ecological and experimental studies on phytoplankton<br />
and zooplankton from the Indian Ocean<br />
3.4.4 Biology <strong>of</strong> ecosystem under different environmental stresses<br />
3.4.5 Marine fouling and wood-boring organisms<br />
Areas <strong>of</strong> work in biological oceanography are productivity, planktonology,<br />
benthic biology, microbiology, aquaculture and distribution <strong>of</strong> marine organisms, their<br />
interaction with each other and with the evnvironment. Other major activities include<br />
mangrove and seaweed ecology and physiological adaptations in marine organisms. The<br />
progress made under each project during the year is as follows:<br />
3 4-1 Survey <strong>of</strong> biological resources in the seas around India<br />
1. Primary production<br />
Studies on primary production, Chl. a and paniculate organic production<br />
were made along the latitude 5°30' N and longitude 82° to 98° E (16 stations) in<br />
the Andaman Sea (21 stations) and from 6 anchored stations in ;he Hooghly estuary<br />
and at the Mahanadi river mouth. The results obtained are tabulated below:<br />
45
2. Extracellular production<br />
Studies on the extracellular production by the phytoplankton at 26 stations in<br />
the Andaman Sea and Bay <strong>of</strong> Bengal revealed that production varied from 0 to 1.4 mgC/<br />
m 3 /hour. In terms <strong>of</strong> percentage, it varied from 0-90% <strong>of</strong> the total organic production.<br />
The trend in extracellular production in the Andaman Sea was found markedly different<br />
from that <strong>of</strong> the Laccadive Sea.<br />
3. Secondary production<br />
Estimates <strong>of</strong> secondary production were made from the zooplankton samples,<br />
collected from the different regions <strong>of</strong> the Arabian Sea and Bay <strong>of</strong> Bengal. The zooplankton<br />
standing stock <strong>of</strong>f Karwar was 524 ml/100 m 3 . This was due to the congregations<br />
<strong>of</strong> bioluminescent ostracods. Copepod swarm (25974 to 138420 individuals/m 3 )<br />
caused by 4 species <strong>of</strong> family Pontellidae, viz., Pontella spinipes, P. princeps, P. securifer<br />
and Pontellopsis regalis was observed in the Campbell Bay (Andaman Sea). Aggregations<br />
<strong>of</strong> euphausiids were also seen in the zooplankton samples collected during the 80th<br />
cruise <strong>of</strong> R.V. Gaveshani from the subsurface scattering layer between Madras and<br />
Pondicherry.<br />
A comparative study <strong>of</strong> the zooplankton abundance and distribution <strong>of</strong> various,<br />
taxa and dominant species from the Malacca Strait and the Andaman Sea (cruise<br />
67 and 68) indicate that zooplankton production was higher than that obtained<br />
from the same areas in early 1979.<br />
4. Biochemical investigations<br />
Biochemical composition <strong>of</strong> mixed zooplankton, major planktonic groups and<br />
some common species collected from the Andaman Sea showed that protein was<br />
the dominant constituent followed by lipid. Carbohydrate content was usually very<br />
low especially in such forms which had a high water content or with calcareous<br />
shell. The low lipid and carbohydrate concentrations probably indicate that protein<br />
serves as metabolic reserve in the tropical zooplankton.<br />
46
5. Detritus production<br />
Detrital carbon in the Andaman Sea constituted about 92% <strong>of</strong> the total perticulate<br />
carbon while phytoplankton and zooplankton made up small fractions <strong>of</strong> the<br />
total suspended matter. Latitudinal relationship between phytoplankton and zoopankton<br />
was found to be inverse. The Andaman Sea is oligotrophic in nature with<br />
low primary and secondary productivity rates and hence the production <strong>of</strong> large<br />
quantities <strong>of</strong> detritus appear to supplement the nutritional inadequacy <strong>of</strong> these waters.<br />
6. Benthic production<br />
As a part <strong>of</strong> continuing project on survey <strong>of</strong> living resources <strong>of</strong> the seas<br />
around India, benthic studies were carried out and some <strong>of</strong> the findings are as follows:<br />
(a) Arabian Sea<br />
(i) Ecology <strong>of</strong> fish trawling ground <strong>of</strong> Goa coast: A detailed investigation on<br />
the role <strong>of</strong> benthos in demersal fisheries <strong>of</strong> the coastal zone <strong>of</strong> Goa indicated that<br />
inspite <strong>of</strong> significant spatial and temporal variations in the environmental variables,<br />
the benthic population and biomass were very high and varied from 25 to<br />
7823 m -2 (Av. 1256m -2 ) and 0.2 to 2251.25 gm -2 (Av. 67.07 gm -2 ) respectively.<br />
It is deduced that the benthic standing crop could possibly sustain a higher exploitation<br />
<strong>of</strong> demersal fish by at least 15% more than that being harvested at present.<br />
(ii) Benthic population <strong>of</strong> polluted environments: A comparative study <strong>of</strong> the<br />
annual cycle <strong>of</strong> settlement, growth and propagation <strong>of</strong> bottom living communities<br />
in the environs <strong>of</strong> sewage, domestic and industrial effluent outfall in the Mandovi<br />
estuary, Goa, has been initiated. Collection <strong>of</strong> environmental and biotic data from<br />
4 polluted and 4 control stations is in progress.<br />
(iii) Solar eclipse and its possible effect on the behavioural activities <strong>of</strong> intertidal<br />
animals and zooplankton: To study the effect <strong>of</strong> total solar eclipse (16<br />
February, <strong>1980</strong>) on locomotory and metabolic activity <strong>of</strong> intertidal animals (sand<br />
dwelling nematodes, worms, oyster (Crassostrea cucullata) from rock pool and periwinkle<br />
(Littorina intermedia) from the exposed rocky shore, field observations covering<br />
pre-eclipse (14 and 15/2/80), eclipse (16/2/80) and post-eclipse (17 and 18/2/<br />
80) period were carried out in the environs <strong>of</strong> Dias Beach (Lat.15°25' N; Long-<br />
73°45 E), Goa. Results indicate that stratification <strong>of</strong> nematodes which was maximum<br />
in the top 1 cm layer at all the tide marks in pre and post-eclipse period, drastically<br />
declined by more than 50% on the day <strong>of</strong> the solar eclipse. Similarly, the metabolite<br />
contents (water, glycogen and total carbohydrates) in C. cucullata and L. intermedia<br />
suddenly fell by 10 and 16% respectively almost coinciding with the planetary<br />
events <strong>of</strong> 16 February, <strong>1980</strong>.<br />
During the period <strong>of</strong> the total solar eclipse, zooplankton samples collected<br />
from the mouth <strong>of</strong> Zuari estuary showed significant vertical migration. Chromosomal<br />
aberrations were observed in Paracalanus aculeatus, a copepod collected from the<br />
surface waters at that time.<br />
47
(ix) Marine fauna at Malvan: Intertidal and subtidal fauna <strong>of</strong> the rocky, sandy<br />
and muddy shores <strong>of</strong> Malvan (Lat. 16°0'N. Long. 73°30'Έ) consisted <strong>of</strong> 208 species<br />
belonging to 172 genera, 97 families. 16 classes and 9 phyla. The most significant<br />
faunal components were 9 species <strong>of</strong> living corals including a variety <strong>of</strong> red coral,<br />
and the pearl oysters <strong>of</strong> the species, Pinctada chemnitzi.<br />
Zonation and distribution <strong>of</strong> intertidal fauna at Malvan in relation to tidal height<br />
and percent exposure.<br />
Eight zones indicating the range <strong>of</strong> vertical distribution and three critical levels<br />
limiting the expanse <strong>of</strong> distribution <strong>of</strong> fauna could be demarcated. Rock pool habitat<br />
was observed to harbour maximum number <strong>of</strong> species which displayed a high order<br />
<strong>of</strong> faunal diversity.<br />
(b) Bay <strong>of</strong> Bengal<br />
An extensive survey <strong>of</strong> the benthic fauna from the coastal zone between<br />
Madras and Sandheads and at the mouth <strong>of</strong> Diamond Harbour in the Hooghly<br />
estuary was conducted during the 76th to 78th cruises <strong>of</strong> R.V. Gaveshani. In all,<br />
175 stations were worked and the data are being processed.<br />
(c) Andaman Sea<br />
A comparative study <strong>of</strong> the benthic fauna collected during the period January-<br />
February 1979 (cruise nos. 51 and 52) with those collected in January-February<br />
<strong>1980</strong> (cruise nos. 67 and 68) from the same area was made. An extensive<br />
area (ca 90.000 km -2<br />
lying between latitudes 6-15° N and longitudes 91-97°E) in the<br />
depth range <strong>of</strong> 11 to 2150 m was surveyed and the distribution, abundance, composition,<br />
prevalence and standing crop measurements in relation to environmental and<br />
biotic conditions were carried out.<br />
48
The macrobenthic fauna comprising <strong>of</strong> 22 taxa was dominated by polychaetes<br />
(76.80%). Their distribution was substrate specific with a maximum <strong>of</strong> 410m -2<br />
organisms in clayey deposits and minimum 266 m -2 in the sandy areas. The standing<br />
crop was relatively low 6 g m -2 and varied from 0.3 to 74.4 g m -2 . Biomass <strong>of</strong><br />
the infauna was considerably lower than those <strong>of</strong> the epifauna and production was<br />
found to decrease rapidly with the increase in depth.<br />
Total meiobenthos number varied between 68 and 48/10 cm -2 (Av. 247.8)<br />
and the biomass ranged between 3.57 and 32.8 mg/10 cm -2 (Av. 14.46). Faunal density<br />
was maximum in sandy sediments and minimum in the coarse coralline sand<br />
and clayey deposits. Impoverishment <strong>of</strong> fauna at the intermediate depths <strong>of</strong> 200-<br />
500 m was observed. The fauna was mostly present in the upper 2 cm <strong>of</strong> the sediments<br />
and only nematodes and foraminiferans were found below 4 cm depth.<br />
(d) Malacca Strait<br />
Bottom fauna (macro and meio) <strong>of</strong> the Malacca Strait in the depth range <strong>of</strong><br />
80 to 1350 m is dominated by meiobenthos and it exceeds macrobenthos by 12-5 times<br />
in weight and by more than 780 times in the population density. Standing crop was<br />
high (Av. 11.79 g m -2 ) and the fauna was dominated by the Indo-Pacific species.<br />
7. Mangroves and seaweeds<br />
(a) Mangrove ecology : Ecology <strong>of</strong> mangroves in the model region <strong>of</strong> Mandovi<br />
estuary was studied during the year. Seasonal growth <strong>of</strong> the two mangrove species,<br />
49
Kandelia rheedii and Rhizophora mucronata was studied with the help <strong>of</strong> tags. Peak<br />
growth in the Rhizophora mucronata was observed from November to December.<br />
Study <strong>of</strong> the seasonal variation in the accumulation <strong>of</strong> heavy metals like Fe,<br />
Mn, Cu, Co, Pb and Ni in the foliage <strong>of</strong> seven mangrove species was determined-<br />
High concentration <strong>of</strong> Fe and Ni do not appear to have any toxic effect on the<br />
plants.<br />
( b ) Seaweeds and alga<br />
(i) Goa coast: Survey was undertaken at 12 different localities to study the<br />
distribution, zonation and algal yield. In all, 81 algal species were collected, <strong>of</strong> which<br />
23 were chlorophyta, 21 phaeophyta, 32 rhodophyta and 4 cyanophyta.<br />
Light and dark bottle method was used to study the rate <strong>of</strong> photosynthesis<br />
and respiration in four marine algal species. Sargassum, Stoechospermum marginatus<br />
(phaeophyta) and Caulerpa sertularoides (chlorophyta) showed a production <strong>of</strong><br />
2.677, 2.634 and 0.988 gC m -2 day -1 respectively.<br />
The effect <strong>of</strong> seaweed extracts on the growth <strong>of</strong> land plants such as turnip,<br />
chillies, pineapple and paddy was tested. It was found that 1% extract induced a<br />
better growth, high germination rate, increase in the leaf size and enhanced yield<br />
in all the plants. The extract <strong>of</strong> Stoechospermum marginatum induced maximum growth<br />
The effect <strong>of</strong> different seaweeds extract on the growth <strong>of</strong> Turnip plants.<br />
50
(treated 491-92 gm, control 277.628 gm) in the turnip plant. Green chillies showed<br />
6.3 kg yield in a plot <strong>of</strong> 3 m 2 within 40 days after the first spray while in the<br />
control the total yield was less than 1 kg. Similarly, the pineapple plants when<br />
sprayed with 1% compound extract showed a maximum <strong>of</strong> 31 kg per fruit while<br />
in the control it was 2.57 kg per fruit.<br />
Eight algal species were cultured in different concentrations <strong>of</strong> secondary treated<br />
sewage under laboratory conditions. It was observed that the species <strong>of</strong> Pudina,<br />
Stoechospermum, Gracilaria, Ulva and Chetomorpha showed a good growth in 5% concentration,<br />
while the other concentration produced no effect.<br />
(ii) Karnataka Coast: In view <strong>of</strong> the limited information <strong>of</strong> algal resources<br />
available along the Karnataka coast, a survey was undertaken. This revealed the<br />
presence <strong>of</strong> 31 algal species dominated by rhodophyta and followed by phaeophyta.<br />
The small number <strong>of</strong> seaweeds may be due to the nature <strong>of</strong> the coast which is<br />
predominantly sandy with small rocky regions.<br />
(iii) Maharashtra Coast: Fortythree algal species from the Maharashtra<br />
coast were analysed for their biochemical composition. Chlorophyta and rhodophyta<br />
were found to be richer in protein and carbohydrates as compared to phaeophyta.<br />
Organic carbon was maximum (33%) in chlorophyta. C:N ratio varied from 5.2 to<br />
29.8 and showed an inverse relationship with protein.<br />
51<br />
Marine algal samples<br />
collected from the Maharashtra<br />
coast were analysed<br />
for trace metal concentration.<br />
A few t race metals were<br />
found to be in higher concentrations<br />
than their normal<br />
levels.<br />
8. Bloom studies<br />
Studies on algal blooms<br />
were continued. Trichodesmiurn<br />
phenomenon showed<br />
a direct relationship with<br />
zooplankton abundance. The<br />
main components <strong>of</strong> zooplankton<br />
during Trichodesmium<br />
blooms were cladocerans,<br />
copepods, decapod larvae,<br />
chaetognaths, fish eggs and<br />
larvae and appendicularians.<br />
There was a periodicity in the appearance <strong>of</strong> various groups <strong>of</strong> organisms and<br />
this seems to be repeated with return <strong>of</strong> Trichodesmium phenomenon every year.
9. Microbiological studies<br />
Water samples collected with J. Z. samplers at 25, 50, 100 and 200 m depths<br />
from 15 stations during the 75th cruise <strong>of</strong> R.V. Gaveshani, were analysed for<br />
various physiological groups <strong>of</strong> bacteria. Heterotrophic denitrifying rate (determinated<br />
using an organic medium) ranged from 0-5 to 92 μg-at NO 2 -N/ml/24<br />
hrs. Some <strong>of</strong> the highest rates <strong>of</strong> reduction were found in samples from 200 m<br />
depth. Samples from 25 and 50 m dtpths showed a high reducing capacity. The<br />
stations with highest activity did not, however, show the highest number <strong>of</strong> nitrate<br />
reducers. The estimation <strong>of</strong> the anaerobic sulphate reducers showed that they occur<br />
at all the stations irrespective <strong>of</strong> depths. Their occurrence at the various stations<br />
showing high Eh, as indicated by thedissolved oxygen concentrations, suggestedthat there<br />
could be microniches which provide the necessary conditions for their existence/proliferation.<br />
Their number varied from 10 to 200/ml. Their activity as determined by the<br />
sulphate reducing capacity showed as much as 6-8 μg-at/ml/day in media provided<br />
with 0.75% organic substrate.<br />
A model system was designed in the laboratory to simulate the field conditions<br />
to study the role <strong>of</strong> micro-organisms in specialised ecosystems like mangroves.<br />
Species <strong>of</strong> Planococci, Pseudomonas, Mucor and Fusarium were found to play major<br />
role in the effective conversion <strong>of</strong> mangrove foliage into protein rich detritus within<br />
a period <strong>of</strong> one month. This protein-rich detritus can be used as the readymade<br />
energy source for the economically important detritovorous fishes, crustaceans and<br />
edible bivalves.<br />
The sediments from the Andaman Sea were rich in physiologically active<br />
heterotrophic bacterial flora. There appeared to be a direct relationship between<br />
the density <strong>of</strong> mci<strong>of</strong>auna and bacterial population in the sediment indicating the<br />
importance <strong>of</strong> this flora in the food chain.<br />
3.4.2 Coastal Aquaculture<br />
1. Aquaculture in waters <strong>of</strong> Goa<br />
(a) Shellfish culture: Studies on the techniques and prospects <strong>of</strong> culture <strong>of</strong> 7<br />
species <strong>of</strong> edible bivalves including mussels, oysters and clams were continued.<br />
Improvements in the technique <strong>of</strong> raft culture <strong>of</strong> green mussel. Perna viridis were<br />
undertaken and the field trials were also carried out. Some aspects <strong>of</strong> environmental<br />
physiology <strong>of</strong> mussels transplanted from the intertidal area and grown on rope were<br />
studied. Development <strong>of</strong> a physiological mechanism for compensating the water<br />
balance in relation to wide fluctuations in salinity was observed. Similarly, a<br />
synchronizing mechanism where the annual reproduction cycle gets balanced with the<br />
magnitude <strong>of</strong> interaction <strong>of</strong> exogenous and endogenous variables was also noticed.<br />
Results indicated that the raft grown mussels developed special behavioural, physiological<br />
and biochemical adaptations to overcome the large range <strong>of</strong> variations in the<br />
environmental factors at the culture site.<br />
Field trials for testing the efficiency <strong>of</strong> indigenously developed spat-collectors<br />
for mussels, edible oysters and pearl oysters were undertaken. Out <strong>of</strong> the various<br />
52
materials tested so far. the best settlement <strong>of</strong> 83/cm 2 with an efficiency <strong>of</strong> 70% was<br />
achieved by using the loose coir threads in nylon netting.<br />
Seasonal changes in the meat condition and in major biochemical constituents<br />
<strong>of</strong> the black clam. Villorita cyprinoides in the Colvale river (Goa) were observed to<br />
be closely associated with the reproduction, storage and utilization <strong>of</strong> reserves. The<br />
main period <strong>of</strong> increase in the biochemical constituents coincided with the gametogencsis<br />
and maturation <strong>of</strong> gonads. Spawning was found to be biannual and produced<br />
a marked fall in the quality <strong>of</strong> meat. Accordingly, the most suitable period for<br />
harvesting the clam will be from October to January and not the traditionally followed<br />
fishing season from May to August.<br />
Raft culture <strong>of</strong> pearl oysters including their spat collection and growth in<br />
sandwich nets has been initiated at Malvan where a natural bed <strong>of</strong> P. chemnitzi<br />
has recently been discovered.<br />
(b) Shrimp culture: Further studies were carried out on cheap and acceptable<br />
feeds for the shrimp. Various ingredients were tried in different composition and<br />
tested on penaeid prawns for their specificity and efficiency <strong>of</strong> diets. The juveniles<br />
<strong>of</strong> penaeid prawns, viz. Metapenaeus monoceros, M. affinis and P. indicus, when fed<br />
on the prepared diets, showed good growth. The effciency <strong>of</strong> growth was found to<br />
be species specific. The mangrove swamps were found to be a rich source <strong>of</strong> prawn<br />
fry and considerable number <strong>of</strong> juveniles <strong>of</strong> Metapenaeus dobsoni, M. monoceros and<br />
Penaeus affinis were collected from December to June for stocking in culture ponds.<br />
(C) Unialgal culture: Unialgal cultures οf Metapenaeus dobsoni and Coscinodiscus<br />
sp. have been maintained for experimental studies.<br />
53
(d) Artemia culture: A one acre salt pan having a salinity <strong>of</strong> 110%o was<br />
selected for the culture trials <strong>of</strong> Artemia at premises <strong>of</strong> Bharat Salt and Chemical<br />
Industries Ltd. Mundra, Gujarat. Since the water temperature in the salt pan was<br />
as low as 13°C during November and December, a low-temperature-tolcrant San-<br />
Francisco Bay strain <strong>of</strong> Artemia was inoculated. The water level at the salt pans was<br />
maintained by drawing fresh sea water from an adjacent reservoir. The larvae which<br />
were introduced grew to adult size in about 12 days and started reproducing. At<br />
the salinity 110%o Artemia reproduces by directly releasing the nauplii from the pouch—<br />
a condition known as viviparity.<br />
During the month <strong>of</strong> March, the salinity was allowed to reach 180%o by<br />
natural evaporation and also by drawing high salinity water from 8 neighbouring condenser<br />
ponds. This sudden change in the salinity made Artemia to release the cysts<br />
directly—a condition known as oviparity. By the end <strong>of</strong> March <strong>1980</strong>, 15 kg/<br />
acre Artemia cysts were harvested. The harvested cysts were cleaned, packed and<br />
marketed to various universities and research institutes at the rate <strong>of</strong> Rs. 500 per kg.<br />
A large area <strong>of</strong> about 50 acres in Mundra is being utilised for Artemia culture to<br />
increase the commercial production <strong>of</strong> eggs.<br />
2. Aquaculture in waters <strong>of</strong> Cochin<br />
The progress made under this investigation is reported separately under Regional<br />
Centre, Cochin (Section 3.8.1).<br />
3. Laboratory and field studies on bioenergetics <strong>of</strong> some marine and estuarine animals<br />
Studies on the culture aspects <strong>of</strong> the estuarine fish, pearl spot (Etroplus suratensis)<br />
were undertaken during June 1979 to June <strong>1980</strong>. About 2300 pearl spots (Av. 8.83 gm,<br />
in weight and 69 mm in length) were stocked in June 1979 in an 0.16 ha. pond in a<br />
fish farm (Goa). Studies on environmental characteristics, primary production, population<br />
dynamics, growth and yield, nutritional characteristics <strong>of</strong> the ingested food and energetics<br />
were carried out. Some <strong>of</strong> the highlights <strong>of</strong> these studies were: Primary production<br />
ranged from 104 to 8823 mg C/m 3 /day in the culture pond. The annual contribution <strong>of</strong><br />
nannoplankton to the total primary production was as high as 83%. The estimated annual<br />
production amounted to 416 gC/m 3 /yr. Chlorophyll a and nitrate content showed a<br />
significant correlation with the primary production. In the cultured population <strong>of</strong> E. suratensis<br />
females were dominant. From length frequency studies, growth was found to be 1.1<br />
cm/month. Fecundity was generally low. Daily increments in length and weight during the<br />
culture period were found to be 0.075 mm and 0.066 gm respectively. Growth in general<br />
was low and was attributed to over stocking and low level <strong>of</strong> protein present in the diet<br />
(35%). The total production <strong>of</strong> fish in the pond was 437.5 kg/ha/yr and the rate <strong>of</strong> return on<br />
investment was 33%. The estimated amount <strong>of</strong> organic carbon available at the level<br />
<strong>of</strong> primary producers was 99840 gC/yr which should give a potential yield <strong>of</strong> 9984<br />
gC/yr <strong>of</strong> fish. The exploited yield as a net increase in the fish carbon was 3342 g/yr<br />
and therefore there appears to be scope for increasing the production <strong>of</strong> the fish by<br />
at least 3 times.<br />
54
Stomach analyses <strong>of</strong> E. suratensis revealed that the fish is principally a phytoplankton-detritus<br />
feeder. Detritus formed a major part <strong>of</strong> the consumed food (44%)<br />
and the diatoms were the next important items (38%). Of the total food consumed,<br />
56% was contributed by the organic constituents and 44% by the ash content. Protein,<br />
lipid and carbohydrates, on an average, amounted to 35, 12 and 9% respectively.<br />
Energy content <strong>of</strong> the consumed food was 2706 cal/gm dry wt. Organic carbon<br />
constituted 16% and C:N ratio was found to be 3.29:1. This study revealed that<br />
feeding at a low level <strong>of</strong> dietary protein was probably responsible for the reduced<br />
growth rate observed in the harvested population.<br />
An annual energy budget was constructed for the captured population <strong>of</strong> E. suratensis.<br />
The production <strong>of</strong> body tissue, gonads, respiration and faecal production were<br />
determined and the total consumption was derived as a summation <strong>of</strong> these factors.<br />
The total annual consumption, production, energy loss through respiration and faeces<br />
were estimated to be 117054, 365, 15037 and 1652 kcal respectively. E. suratensis had<br />
high assimilation efficiency (90.31%) but low conversion efficiency (K1 = 2.14% and<br />
K2 =2.37%). A very large proportion <strong>of</strong> energy was lost during respiration.<br />
3.4.3 Biogeographical, ecological and experimental studies on phytoplankton and<br />
zooplankton from the Indian Ocean<br />
The progress made under this project is reported under the Regional Centre,<br />
Cochin (Section 3.8.1).<br />
3.4.4 Biology <strong>of</strong> ecosystem under different environmental stresses<br />
(i) Effect <strong>of</strong> some heavy metals on Tilapia mossambica: Experimental studies on<br />
the long-term effect <strong>of</strong> sublethal concentrations <strong>of</strong> some heavy metals—mercury, copper,<br />
cadmium and arsenic on the blood serum, haemoglobin and eye lens proteins <strong>of</strong> the fish<br />
T. mossambica were undertaken. Significant changes were seen in the electrophoretic<br />
patterns <strong>of</strong> serum proteins on exposure to mercury. The eye lens proteins and haemoglobin<br />
<strong>of</strong> fish were not much affected.<br />
(ii) Ecosystem: The relative abundance <strong>of</strong> biochemica compounds in the<br />
estuarine waters <strong>of</strong> Goa is being studied in relation to plant and animal production<br />
in the ecosystem. The results would give a better understanding <strong>of</strong> the different ecological<br />
processes influencing the uptake and incorporation <strong>of</strong> these biochemicals in the<br />
aquatic organisms.<br />
The status <strong>of</strong> estuarine fauna in relation to different ecophysiological stresses<br />
originating from the metal inputs, organic enrichment due to detrital load and sewage<br />
run-<strong>of</strong>f are being studied. To evaluate the trophic relationship in the food chain and<br />
also in the bivalve culture, the physiological responses to different environmental<br />
stresses are also being investigated.<br />
Zooplankton samples from 200 m depth to the surface were collected from 26<br />
stations in Central Arabian Sea during the 82nd cruise <strong>of</strong> R.V. Gaveshani. 25% <strong>of</strong><br />
the samples were used to estimate the biomass and faunal composition and the remaining<br />
were subjected to biochemical and heavy metal analyses. The aim <strong>of</strong> the work was<br />
55
to determine the heavy metal concentration in this region at the secondary trophic<br />
level.The samples were processed. The effect <strong>of</strong> heavy metals (copper, cadmium<br />
and zinc) on 2 copepod species revealed that copper was the most toxic metal. The<br />
estuarine species Acartia spinicauda was more sensitive to heavy metal accumulation<br />
than the neritic form Tortanus forcipanis.<br />
3.4.3 Marine fouling and wood-boring organisms<br />
A new project to study the biodeterioration <strong>of</strong> materials in the coastal ecosystem<br />
was started during the year.<br />
During April-May <strong>1980</strong> collections were made <strong>of</strong>f the New Mangalore Port area<br />
as a part <strong>of</strong> the Kudremukh sponsored project (Phase II) during its prepollution<br />
survey. The fouling organisms consisted <strong>of</strong> barnacles (Balanus tintinabulum, B. amphitrite)<br />
mussels (Perna viridis), bryozoans (Alderina sp., Eletra sp.) and polychaetes<br />
(Pomatococeros sp. and Hydroides norwegion). The organisms settled at the various<br />
depths have teen collected for further<br />
studies regarding their rate <strong>of</strong> growth,<br />
systematics and other biological studies-<br />
Collections were also made from a<br />
channel-marked buoy anchored in the Mormugao<br />
harbour. The collection comprised<br />
<strong>of</strong> barnacles such as Balanus tintinabulum,<br />
B. amphitrite, mussels (Perna viridis) and<br />
bryozoans. When compared with the collection<br />
made at Mangalore, the rate <strong>of</strong> growth<br />
especially that <strong>of</strong> the mussel Perna viridis<br />
seems to be much greater a! Mormugao<br />
than at Mangalore.<br />
Fouling organisms from Mangalore and<br />
Marmugoa Port areas.<br />
56<br />
Observations on the settlement <strong>of</strong><br />
fouling organisms on moving barges in<br />
the estuarine environment <strong>of</strong> Goa region<br />
were also made during the year.
3.5<br />
Ocean Engineering<br />
3.5.1 Ocean engineering studies related to coastal and <strong>of</strong>fshore development<br />
3.5.2 Marine geotechnical studies<br />
3.5.3 Energy from the sea<br />
3.5.1 Ocean engineering studies related to coastal and <strong>of</strong>fshore development<br />
A field programme for the collection <strong>of</strong> data on waves, currents, tides and<br />
changes in the bathymetry was initiated during the monsoon starting in May/June<br />
<strong>1980</strong> to develop an understanding regarding the factors which causes the formation<br />
<strong>of</strong> Aguada sand bar and the associated navigation problems.<br />
Mooring system used for the wave rider buoy consisted <strong>of</strong> a 12.6 mm diameter,<br />
5 m long galvanized M.S. chain connected immediately below the wave rider<br />
which in turn was connected to a 19 mm diameter, 5 m long chain <strong>of</strong> similar quality.<br />
To the end <strong>of</strong> this chain a cast iron anchor <strong>of</strong> about 100 kg in weight was connected.<br />
The current meter mooring consisted οf a concrete block <strong>of</strong> 0.6 mx 0.6 mx<br />
15 m in which a 38 mm diameter stainless steel pipe was embeded. The data on<br />
waves and currents and for the monsoon tides <strong>of</strong> <strong>1980</strong> were processed and analysed.<br />
A status report on the wave hindcasting has been completed. Studies on the<br />
various wave hindcasting models, presently available, are being carried out. A model,<br />
based on the energy equation with the wind, waves and swells as independent factors<br />
is being developed. Wave heights were calculated at 3 hourly intervals at all the<br />
points in the numerical grid network <strong>of</strong> the selected area using 6 hourly weather data-<br />
Another status report on the storm surge research in India with a discussion<br />
on the available numerical models has been prepared. Work has been initiated for<br />
the development <strong>of</strong> a model for the storm surges and storm-generated currents to<br />
suit the Indian conditions. The numerical models used by the India Meteorological<br />
Department are also being studied and applied to certain storms. It will be possible<br />
to study the past 20 to 25 years data for generating the necessary information on<br />
design water levels.<br />
Plans have been finalized to intensify the collection <strong>of</strong> field data on waves,<br />
using wave rider buoys. The collected data will also be used to calibrate the<br />
wave hindcast models. Steps have been taken to procure a sophisticated computer<br />
programme called "NEPTUNA" from Norway under the ongoing Indo-Norwegian<br />
57
Technical Assistance Programme. This computer package is being implemented at<br />
the DEC10 computer <strong>of</strong> the TIFR, Bombay.<br />
Numerical studies on dispersion/diffusion <strong>of</strong> pollutants in the sea, computation<br />
<strong>of</strong> tidal currents, current circulation in bay and estuaries, have been made.<br />
3.5.2 Marine geotechnical studies<br />
The piston gravity corer developed by NIO earlier has been further modified.<br />
In order to minimize the soil disturbance certain modification have been introduced<br />
in the core cutter, core catcher, piston, casting weight, tail fin, trigger mechanism<br />
etc. The design has been completed and its fabrication is in progress.<br />
A piezometer is being designed and developed for measuring the hydrostatic<br />
pressure and hydrodynamic pressure in the seabed soils. The instrument contains<br />
two pressure transducers to measure hydrostatic and hydrodynamic pressures<br />
simultaneously.<br />
Studies on the stability <strong>of</strong> submarine pipelines have been completed. A relationship<br />
between friction factor <strong>of</strong> submarine pipeline resting on the seabed and the<br />
horizontal and vertical components <strong>of</strong> forces acting on the pipeline has been developed.<br />
Simultaneous effects <strong>of</strong> wave and current forces on the submarine pipeline,<br />
resting on the seabed, have also been studied.<br />
3.5.3 Energy from the sea<br />
The growing interest in some problems related to the energy from the sea has<br />
prompted to accelerate some <strong>of</strong> the investigations. Under this project, several groups<br />
have been formed to undertake a study on (i) Ocean thermal energy conversion,<br />
(ii) Tidal power, (iii) Wave energy, (iv) Salinity power (v) Energy from biomass,<br />
(vi) Coastal erosion and (vii) Aquaculture.<br />
The major task <strong>of</strong> these groups at the initial stages was to prepare status<br />
reports bringing out clearly the feasibility <strong>of</strong> these sources <strong>of</strong> energy. A resume <strong>of</strong><br />
the work done is given below:<br />
A laboratory model <strong>of</strong> an OTEC plant <strong>of</strong> 200 watts capacity has been designed.<br />
It will demonstrate certain working principles and will bring out some <strong>of</strong> the<br />
related problems. Studies are being undertaken to design, fabricate and install a<br />
small wave power extracting device <strong>of</strong> the type similar to that <strong>of</strong> the 'Cockerrel<br />
Raft', <strong>of</strong>f Goa. Studies on the wave climate, selection <strong>of</strong> material, design and<br />
construction aspects <strong>of</strong> the floating raft, hinges, moorings and bottom anchors are<br />
being carried out.<br />
Under this project a two-day workshop was organised to analyse the state<br />
<strong>of</strong> art on the subject on 15 and 16 December, <strong>1980</strong>. A large number <strong>of</strong> participants<br />
from different organizations participated and presented about 40 papers. Some <strong>of</strong> the<br />
final recommendations are as follows:<br />
(a) India has a high potential for Ocean Thermal Energy Conversion plant (OTEC).<br />
(b) Lakshadweep is geographically well suited for the installation <strong>of</strong> a mini OTEC plant.<br />
58
(c) A mission oriented research programme with a well coordinated multi-disciplinary<br />
approach should be developed in the country. A consortium consisting <strong>of</strong><br />
experts from ΝIO, IITs, BHEL, Hindustan Shipyards, BHPV etc., should be<br />
constituted to go into the various aspects in connection with the development<br />
<strong>of</strong> an experimental OTEC plant <strong>of</strong> one megawatt.<br />
(d) The wave activated generator developed by Madras Port Trust should be widely<br />
utilized for charging batteries <strong>of</strong> the navigational light buoys <strong>of</strong> all the ports and<br />
harbours in the country.<br />
(e) Intensified programme on the collection <strong>of</strong> wave data for determining the feasibility<br />
<strong>of</strong> extracting energy from the waves should be undertaken.<br />
(f) Premising sites for the development <strong>of</strong> tidal power plants in India are the Gulf<br />
<strong>of</strong> Kutch, Gulf <strong>of</strong> Cambay and Sunderbans and these should be studied intensively.<br />
(g) A well coordinated system approach should be made by experts from various<br />
organizations so that time-bound programmes are taken up for Ocean Thermal<br />
Energy Conversion (OTEC) and tidal power development in India.<br />
(h) Detailed R & D work should be initiated to study the feasibility <strong>of</strong> extracting<br />
energy from salinity gradients and marine biomass conversion-<br />
MANUAL ON<br />
PROTECTION AND CONTROL OF COASTAL EROSION IN INDIA<br />
___ P. BRUUN & B. U. NAYAK<br />
This manual presents a summary <strong>of</strong> some<br />
<strong>of</strong> the applicable remedial measures including<br />
guidelines for practical designs to<br />
control coastal erosion with special reference<br />
to Indian conditions.<br />
While some <strong>of</strong> the basic information<br />
has been presented in the text under<br />
4 sections, more detailed information<br />
has been included separately under 6<br />
appendices in the manual.<br />
146 pp., 82 figures, 6 plates and 20 tables<br />
Price: Rs. 70 U.S. $ 16<br />
(in India ) ( Abroad )<br />
PUBLISHED BY<br />
NATIONAL INSTITUTE OF OCEANOGRAPHY<br />
Dona Paula-403 004, Goa, India<br />
59
3.6<br />
Marine Instrumentation<br />
3..6.1 Development <strong>of</strong> marine instrumentation system<br />
3.6.2 Development <strong>of</strong> multi-parameter buoy telemetry system<br />
3.6.3 Development <strong>of</strong> microprocessor based systems<br />
3.6.4 Development <strong>of</strong> underwater acoustic instrumentation system<br />
The main objectives <strong>of</strong> this division are to achieve as far as possible selfsufficiency<br />
in marine instrumentation and we should be able to operate, repair and<br />
maintain all the sophisticated oceanographic instruments imported from abroad both<br />
in the laboratory and on board the research vessel.<br />
The R and D work related to oceanographic instrumentation was continued<br />
under 4 different projects and the progress made under each has been summarised<br />
below:<br />
3.6.1 Development <strong>of</strong> marine instrumentation system<br />
(i) Conductivity-Temperature-Depth (CTD) Recorder: The development <strong>of</strong> CTD<br />
recorder, partly sponsored by Electronics Commission <strong>of</strong> India, has been completed.<br />
The instrument has been tested successfully from R. V. Gaveshani during various<br />
cruises and now it is being released through ETDDC for commercialisation.<br />
Sea probes <strong>of</strong> CTD System developed by NIO.<br />
61
Tide gauge developed by NIO<br />
(ii) Tide gauge: This instrument is capable <strong>of</strong> recording continuously tidal data<br />
on a strip chart recorder at any interval from 1 to 255 minutes and stored on RAMS.<br />
This unit is solar powered and the insrtument uses a strain gauge pressure transducers<br />
to measure water depth.<br />
(iii! Rotor flow meter: This equipment which was developed earlier, has been<br />
modified and updated. The modified version has a redesigned rotor, changed accounting<br />
system and improved method <strong>of</strong> supporting the cable.<br />
(iv) Seven line slip-ring winch: This small portable winch with 500 metre cable<br />
<strong>of</strong> seven cores was developed for the porfiling instruments.<br />
3.6.2 Development <strong>of</strong> multi-parameter buoy telemetry system<br />
This project deals with the development <strong>of</strong> a "Mechanical buoy" with capabilities<br />
to transmit wind speed, wind direction, humidity, air temperature, surface<br />
temperature, water current and its direction and wave height.<br />
The sensors have been received and logic/control circuits have been designed<br />
and fabricated using SDM 857. Memodyne digital cassette recorder and interfacing<br />
circuits have been developed for the temporary storage <strong>of</strong> ocean data. Circuits<br />
for flash-light and battery charger have also been designed and tested for their<br />
satisfactory performance.<br />
62
The buoy is expected to be launched by June 1981.<br />
3.6.3 Development <strong>of</strong> microprocessor based systems<br />
This project was undertaken to develop microprocessor based systems accessible<br />
in remote controlled, low powered and low cost operation for the simple control<br />
measurements and for the 'on line' acquisition <strong>of</strong> data.<br />
The 8086 microprocessor based kit was assembled and interfaced to Aanderaa<br />
Tape reader to read the current meter data recorded on the 1/14" mag. tape and<br />
to dump it on a teletype in the proper format. The necessary s<strong>of</strong>tware has also<br />
been developed to transfer this data on 1/2" mag. tape (M/s. Kennedy Model 1600<br />
make) in the computer compatible format for further processing.<br />
The single board computer based oh 8085 microprocessor is designed and<br />
implemented. The serial monitor programme is developed to communicate with<br />
the microcomputer through a teletype or RS-232-C terminals. Microcomputer board<br />
has the total capacity <strong>of</strong> 4K-byte PROM storage and 2K byte <strong>of</strong> RAM and 48programmable<br />
I/O lines. The keyboard display monitor is under development.<br />
The single board computer will be used for the development <strong>of</strong> s<strong>of</strong>tware and<br />
hardware for the 8085 microprocessor based instruments.<br />
The SDK-86 microprocessor kit is made to turn and verify the programmes in<br />
the 2716 erasable programmable memories-<br />
3.6.4 Development <strong>of</strong> underwater acoustic instrumentation system<br />
The project aims at developing self-reliance in the development <strong>of</strong> marine<br />
instruments using ultrasonic techniques for the collection <strong>of</strong> oceanographic data. The<br />
following work was done:<br />
(i) Ultrasonic wave gauge: The design, fabrication and testing <strong>of</strong> an ultrasonic<br />
wave gauge were completed this year. The performance <strong>of</strong> this instrument<br />
compared very favourably with the standard equipment. The prototype model <strong>of</strong><br />
the wave gauge features readout <strong>of</strong> the wave-height in metres, an output for recording<br />
the wave data on chart and a printer that provides a hard-copy <strong>of</strong> the digitised<br />
data that can be conveniently used for power spectral analysis. Necessary computer<br />
programmes for computing the power spectra from the wave data have been developed<br />
for the instruments.<br />
(ii) Echosounder: Developmental work on the low-cost echosounder is now<br />
completed and a unit containing improved circuits has been designed and fabricated<br />
and is being tested in the field. The new model has a facility for averaging ten echotime<br />
signals and displays the average result on seven segment L.E.D.S.<br />
63
3.7<br />
Planning & Data<br />
3.7.1 Planning, Monitoring and Evaluation<br />
3.7.2 Publication and Information<br />
3.7.3 Indian <strong>National</strong> Oceanographic Data Centre<br />
The activities <strong>of</strong> Planning and Data Division include planning and budgeting<br />
<strong>of</strong> projects, publication and information work under "Technical Information and<br />
Publication Services" (TIPS) and management <strong>of</strong> oceanographic data. Details <strong>of</strong> the<br />
activities in each <strong>of</strong> the sections are as below:<br />
3.7.1 Planning, monitoring and evaluation<br />
The Planning Section has the prime responsibility <strong>of</strong> collecting and disseminating<br />
information on diverse problems related to project planning. Research projects have<br />
been formulated for the new five year plan proposal. The Annual Plan document for<br />
the year 1981-82 comprising <strong>of</strong> revised estimates for <strong>1980</strong>-81 and budget estimates<br />
for 1981-82 and the Five Year Plan for the period <strong>1980</strong>-85 have been prepared for<br />
the ongoing and new research projects, infra-structure and services. The costing for<br />
All India Coordinated Projects and Rural Development Projects was done and<br />
costing for other major projects is being initiated.<br />
This section is also responsible for the preparation <strong>of</strong> documents for Research<br />
Advisory Council <strong>of</strong> NIO and also the Coordination Council <strong>of</strong> the Physical and<br />
Earth Sciences Group <strong>of</strong> CSIR Laboratories.<br />
Two documents, entitled, 'Marine Science Component in the Science and<br />
Technology Plan <strong>of</strong> the CSIR for Sixth Five Year Plan' and 'Current Research Projects<br />
<strong>1980</strong>-81' were also prepared by this section.<br />
3.7.2 Publication and Information<br />
The Publication and Information Section during the year continued its activities<br />
under the "Technical Information and Publication Services in <strong>Oceanography</strong>"·<br />
(a) Publications<br />
The following regular publications were released during the year:<br />
1. Annual Report 1979: An annual publication dealing with progress <strong>of</strong> the R & D<br />
projects and other activities <strong>of</strong> the <strong>Institute</strong>.<br />
65
2. Cruise Reports (cruise Nos. 66 to 84) <strong>of</strong> R.V. Gaveshani: A report pertaining to<br />
each oceanographic cruise prepared and issued soon after the completion <strong>of</strong> each<br />
cruise <strong>of</strong> R.V. Gaveshani.<br />
3. Annual Oceanographic Cruise Report <strong>of</strong> R. V. Gaveshani 1979: This report consolidates<br />
the information gathered during all cruises undertaken during the year.<br />
4. NIO Newsletter Vol. 2, Nos. 1-4 (<strong>1980</strong>): A quarterly newsletter highlighting the<br />
various R & D and other activities <strong>of</strong> the <strong>Institute</strong> for the respective quarter <strong>of</strong><br />
year.<br />
5· Collected Reprints Vol. 9 (1977) and VoI. 10(1978): A bound and yearly collection<br />
<strong>of</strong> the research papers published by the staff <strong>of</strong> the <strong>Institute</strong>. It is distributed on<br />
exchange basis to marine institutions <strong>of</strong> the world.<br />
6. Mahasagar, Vol. 13 (<strong>1980</strong>) Nos.1-4: A quarterly bulletin <strong>of</strong> the <strong>Institute</strong> incorporating<br />
original research papers on marine sciences.<br />
(b) Information<br />
The information service in the <strong>Institute</strong> was further strengthened this year and<br />
its activities were greatly enhanced and continued during the year.<br />
(i) Directory services: Indian <strong>National</strong> Directory <strong>of</strong> Marine Scientists (INDMS)<br />
was updated, compiled and processed. This directory includes the names <strong>of</strong> Marine<br />
Scientists and their field <strong>of</strong> specialisation, working in various organisations, institutions<br />
throughout the country. The directory is in the stage <strong>of</strong> computerization.<br />
Indian <strong>National</strong> Directory <strong>of</strong> Marine Research Projects (INDMRP) was updated,<br />
compiled, processed and released in the form <strong>of</strong> a computer print out. This Directory<br />
gives a list <strong>of</strong> current marine research projects in different institutions <strong>of</strong> India and<br />
includes information such as duration <strong>of</strong> the projects, name <strong>of</strong> the project leader and<br />
participants, estimated cost <strong>of</strong> the project, area <strong>of</strong> operation and objectives in brief.<br />
(ii) Computer aided bibliographic information services (CABIS): Under this programme<br />
the selected bibliographies on Aquaculture and Mangroves were processed and<br />
released. In addition to the references, these provide subject, author and keyword<br />
indices.<br />
(iii) News to CSIR and Press: News items based on the scientific and other<br />
activities <strong>of</strong> the <strong>Institute</strong> were sent to CSIR for publication from time to time and<br />
also released through press.<br />
(iv) Monthly progress report: Progress <strong>of</strong> work is highlighted every month and<br />
brief summaries depicting the achievements <strong>of</strong> NIO were sent to all the members <strong>of</strong><br />
CSIR Society and Governing Body, members <strong>of</strong> Research Advisory Council and<br />
Executive Committee <strong>of</strong> NIO for information.<br />
(v) Brochures: Two new brochures on "What is NIO" and "Sponsored Projects—<br />
1979" were prepared and released. These brochures provide information about NIO<br />
and the sponsored projects undertaken by NIO during 1979.<br />
66
(vi) Additional services: Public relation work was attended more vigorously and<br />
the VIPs were shown around the laboratory explaining to them the R & D activities<br />
<strong>of</strong> the <strong>Institute</strong>. During the year <strong>1980</strong>, nearly 3000 visitors including students and<br />
research scholars visited the <strong>Institute</strong>.<br />
The section also participated in various exhibitions where major achievements<br />
<strong>of</strong> the <strong>Institute</strong> were highlighted through charts, maps and working models <strong>of</strong> various<br />
equipment.<br />
(vii) Reprography services: Reprography and xeroxing services <strong>of</strong> the Planning<br />
& Data Division were extensively used by different divisions and sections <strong>of</strong> the<br />
institute at various levels.<br />
(viii) News clippings: Under this service, all the available newspapers were<br />
screened and news items <strong>of</strong> scientific interest related to different fields <strong>of</strong> oceanography<br />
and marine sciences were clipped, filed and catalogued for their quick retrieval when<br />
required. News items regarding NIO and its activities were dealt with separately.<br />
(ix) IOC depository centre: The centre continued to receive publications from<br />
various organizations such as UNESCO, UNEP, WHO and WMO which were catalogued<br />
and made available to the users.<br />
A list <strong>of</strong> the holdings <strong>of</strong> the important technical reports was circulated to<br />
various oceanographic and marine science institutes, colleges and universities and<br />
request for any <strong>of</strong> these reports were promptly complied with.<br />
3.7.4 Indian <strong>National</strong> Oceanographic Data Centre (INODC)<br />
The centre acquires, processes and disseminates oceanographic data collected<br />
during the various cruises in the Indian Ocean and the seas around India and keeps in<br />
touch with the activities <strong>of</strong> IOC Working Committee for International Oceanographic<br />
Data Exchange (IODE). It also works as an Input Centre to the Marine Environmental<br />
Data Information Referral System (MEDI).<br />
(a) Acquisition: During the year, following data sets were acquired, coded in<br />
INODC format and stored on magnetic tapes.<br />
(i) R. V. Gaveshani Data: Meteorological, physical, chemical and biological data<br />
<strong>of</strong> the cruises <strong>of</strong> the year 1977 (total number <strong>of</strong> stations: 426).<br />
(ii) INS Darshak data: Hydrographic data <strong>of</strong> INS Darshak cruises undertaken<br />
in 1973-74 (total number <strong>of</strong> stations: 239).<br />
(iii) Oil pollution data: Data on oil pollution and dissolved petroleum hydrocarbons<br />
was acquired from Japan Oceanographic Data Centre, Japan (number <strong>of</strong> observations:<br />
6,689).<br />
(b) Processing: A large amount <strong>of</strong> meteorological and oceanographic data have<br />
been processed and analysed for various purposes as per the request and requirements<br />
<strong>of</strong> the scientists from NIO and other organisations. Some <strong>of</strong> the details <strong>of</strong> data<br />
processed and disseminated are as follows:<br />
67
(i) 'Monex' data <strong>of</strong> CSTD, MBT, XBT, hydrocast and environmental parameters.<br />
(ii) Hydrographic and current data <strong>of</strong>f Visakhapatnam (iii) Current data <strong>of</strong>f Godavari<br />
(iv) Current, wave, tide and wind data <strong>of</strong>f Paradeep Port (v) Data collected during<br />
the oceanographic survey for marking the position <strong>of</strong> oil rigs, pipelines etc. were processed<br />
for the Coordinate Converison (UTM, Shoran, Geographical) on DCM-1101 and<br />
analysed on computer for quality control and plotting <strong>of</strong> the same. (iv) Preparation<br />
<strong>of</strong> state-wise atlases <strong>of</strong> hydrographic, biological and surface current data from Exclusive<br />
Economic Zone was continued. During the year plotting <strong>of</strong> data <strong>of</strong>f Maharashtra,<br />
Karnataka and Tamil Nadu were completed.<br />
(c) Computer s<strong>of</strong>tware services: Under this service, the following systems/programmes<br />
were developed for processing the oceanographic data and information.<br />
(i) CABIS (Computer aided bibliographic information system): This system<br />
consists <strong>of</strong> a number <strong>of</strong> programmes in COBOL Language for retrieval <strong>of</strong> the bibliographic<br />
information.<br />
(ii) SPHD: The system for processing <strong>of</strong> hydrographic data has been developed<br />
in FORTRAN IV. This performs the following functions: (a) Plotting temperature<br />
and salinity versus depth, (b) Interpolation <strong>of</strong> temperature, salinity and oxygen<br />
values at standard depths, (c) Computation <strong>of</strong> density (sigma-t), (d) Computation <strong>of</strong><br />
dynamic depth anomaly at standard depths, (e) Determination <strong>of</strong> pressure at each<br />
depth, (f) Computation <strong>of</strong> potential temperature and density and (g) Computation<br />
<strong>of</strong> sound velocity.<br />
(iii) WAVEX: For analysis <strong>of</strong> the data obtained from the ship borne wave<br />
recorder and incorporates the correction factor for the wave heights.<br />
(iv) POTENG: Determines the potential energy <strong>of</strong> water masses at regular<br />
depth intervals.<br />
(v) BIWTS: Smoothening X-Y curves using binomial filters.<br />
(vi) RXENL: Preparation <strong>of</strong> environmental data reports for data collected<br />
during Monex-79 ctuises.<br />
(vii) TIDEX: Existing TIDE Programme has been extended to provide the tidal<br />
plot along with the tabular value at any given regular interval.<br />
(viii) IOSLP: For plotting any parameter and demarcating the coast lines. It<br />
also prints the range and values and the total number <strong>of</strong> observations-<br />
(ix) WAVES: This programme computes coordinates <strong>of</strong> the wave rays and the<br />
refraction coefficient for waves approaching the shore.<br />
(X) PAYR: Payroll programme for NIO employees. It also takes care <strong>of</strong> pay<br />
and without pay leaves, etc. It has following subroutines: (a) Subroutine for DA calculation,<br />
(b) Subroutine for additional DA calculation, and (c) Subroutine for HRA<br />
calculation.<br />
(d) Data dissemination<br />
(i) INODC Newsletter: INODC Newsletter for the year 1979 has been compiled<br />
and released. It contains information on the data collected by R.V.Gaveshani during<br />
68
A view <strong>of</strong> the TDC -316 Computer installed at INODC in NIO<br />
the cruises in the year 1979. Compilation work for the INODC Newsletter <strong>1980</strong> is<br />
nearly completed and the document will be released soon.<br />
(ii) Inventory forms: The inventory forms <strong>of</strong> ROSCOP (Report <strong>of</strong> observations/<br />
samples collected by occanographic programmes), ROMBI (Results <strong>of</strong> marine biological<br />
investigations) were completed for the R.V. Gaveshani cruises undertaken during<br />
1979.<br />
(iii) The IODE/IOC has developed a General Format-3 (GF3) for oceanographic<br />
data exchange. The centre has initiated its implementation and the data are<br />
being transferred in this format.<br />
(iv) Data holdings: INODC data holding for physical, chemical and meteorological<br />
parameters were updated by the addition <strong>of</strong> data from five cruises <strong>of</strong> INS<br />
Darshak and ten cruises <strong>of</strong> R.V. Gaveshani. The preparation <strong>of</strong> data catalogues was<br />
also initiated.<br />
(e) Additional services<br />
Computer facility <strong>of</strong> the INODC was made available for the processing <strong>of</strong> the<br />
data and information to various public/private organizations and educational institutes.<br />
69
Location <strong>of</strong> Headquarters & Regional Centres<br />
Θ Headquarters<br />
• Regional Centres<br />
70
3.8<br />
Regional Centres<br />
3.8.1 Regional Centre, Cochin<br />
3.8.2 Regional Centre, Bombay<br />
3.8.3 Regional Centre, Waltair<br />
3.8.1 Regional Centre, Cochin<br />
This Centre continued to work on the various projects in collaboration with<br />
the Headquarters.<br />
A. R and D Projects<br />
A.1 Biogeographical, ecological and experimental studies on phytoplankton and<br />
zooplankton from the Indian Ocean<br />
(a) Distribution studies <strong>of</strong> IIOE collections<br />
Systematics and distribution pattern <strong>of</strong> 27 species <strong>of</strong> planktonic copepods <strong>of</strong> the<br />
family Scolecithricidae were completed. High population densities <strong>of</strong> most <strong>of</strong> the<br />
species are found in the upwelling regions close to the land masses. They occupy a<br />
greater geographical range in the northern regions <strong>of</strong> the Indian Ocean and in the<br />
Arabian Sea as compared to the southern region <strong>of</strong> the Indian Ocean and Bay <strong>of</strong><br />
Bengal. The largest area <strong>of</strong> high population density was in the north-western border<br />
<strong>of</strong> the Arabian Sea close to the upwelling areas.<br />
The hyperiid amphipods <strong>of</strong> the family Oxycephalidae were studied with reference<br />
to their morphology, ecology, development and distribution. It was observed that the<br />
newly hatched larvae <strong>of</strong> Rhabdosoma whitei differ considerably from the adults unlike<br />
in other related forms.<br />
Information on the general abundance, distribution, seasonal and diurnal variation<br />
<strong>of</strong> fish larvae collected during the Π0Ε has been brought together. Detailed<br />
studies on the flat fish larvae were made from both IIOE and Naga Expedition samples.<br />
The later material had a better representation <strong>of</strong> the flat fish larvae. Their distribution<br />
was studied and the life histories <strong>of</strong> 10 species <strong>of</strong> flat fishes could be fully established<br />
from the material. The larvae seem to prefer low salinity and neritic region.<br />
(b) Other Studies<br />
(i) Distribution <strong>of</strong> calanoid copepods in the Bay <strong>of</strong> Bengal: During the<br />
7th cruise <strong>of</strong> R.V. Gaveshani, zooplankton samples were collected along two<br />
71
sections, 18°N across the Bay <strong>of</strong> Bengal between the east coast <strong>of</strong> India and Burma.<br />
In the shelf area, Eucalanus monachus was the most abundant species while Undinula<br />
vulgaris and Euchaeta consimilia were abundant. Paracalanus sp. and Acrocalanus<br />
sp. were abundant in the nearshore waters <strong>of</strong> India and Burma. In the surface<br />
samples from 18° N latitude Rhincalanus cornulus, Undinula darwini, Euchaeta marina<br />
and Temora stylifera were the dominant species. Immature forms <strong>of</strong> Pleuromamma<br />
indica were also present in large numbers.<br />
In the deeper waters, the bulk <strong>of</strong> the copepod population was formed <strong>of</strong> Pleuromamma<br />
indica which can tolerate a wide range <strong>of</strong> temperature (6°-23°C) and low<br />
oxygen content (1 ml/1). Another feature noticed was that the herbivorous forms such<br />
as Undinula vulgaris, Eucalanus monachus, E. pileatus, Paracalanus parvus were abundant<br />
above the thermocline while omnivorous and carnivorous species such as P.<br />
indica, Lucicutia clausi, Heterostylitis longicornis, etc., were abundant below the thermocline.<br />
(ii) Sex ratio <strong>of</strong> copepods: Plankton samples collected <strong>of</strong>f Cape Comorin and<br />
Tuticorin were used to study the sex ratio in the five common calanoid copepods.<br />
The number <strong>of</strong> males and females in the 83 samples were as follows:<br />
Species Males Females<br />
Undinula vulgaris 5861 10667<br />
Centropages furcatus 908 2767<br />
Temora trubinata 8665 53600<br />
Temora discaudata 2682 5564<br />
Caudacia bradyi 1281 2227<br />
These figures show that the females were more abundant than the males.<br />
(c) Plankton studies in the estuarine system <strong>of</strong> Kerala<br />
Plankton studies in Kerala estuaries were continued. The various groups <strong>of</strong><br />
animals found were hydromedusae, ctenophores. chaetognaths, copepods, amphipods,<br />
caridea, ostracods, cumaceans, isopods. copelatas and fish eggs and larvae. Seventy<br />
species were identified, <strong>of</strong> which 45 were copepods.<br />
Studies on the phytoplankton <strong>of</strong> the estuarine systems <strong>of</strong> Kerala revealed the<br />
occurrence <strong>of</strong> 24 species <strong>of</strong> diatoms. Phytoplankton were present during pre and<br />
postmonsoon months but relatively absent during the monsoon season. Different<br />
population <strong>of</strong> diatoms was observed in pre and postmonsoon seasons. All the stations<br />
showed a very high concentration <strong>of</strong> pigment throughout the year.<br />
A.2 Coastal aquaculture<br />
(a) Laboratory Studies<br />
(i) Dynamics <strong>of</strong> the growth <strong>of</strong> prawn: Growth data <strong>of</strong> Penaeus indicus and Metapenaeus<br />
dobsoni from laboratory experiment under different frequency <strong>of</strong> feeding with<br />
72
pieces <strong>of</strong> fresh earthworm revealed that growth pattern in both the species adopted<br />
a linear trend under all feeding levels and was not described by the von Bertalanffy<br />
equation. The growlh rate in length was found to increase proportionately with the<br />
level <strong>of</strong> feeding and this trend was maintained throughout the study.<br />
(ii) Experimental culture <strong>of</strong> forage organisms (Tanaidacean-Aspeudes chilkensis)<br />
With earlier experience on short term mass culture, an attempt was made to<br />
continuously culture the species throughout the year in a periodically enriched semicontrolled<br />
system in which salinity and pH were maintained at 9·5-10%o and 7.5-8.0<br />
respectively. The experiment clearly proved that it is possible to raise and maintain<br />
the brood stock <strong>of</strong> these organisms in the laboratory throughout the year.<br />
Similarly, the year-round cultures in semi-controlled systems have been maintained<br />
in the case <strong>of</strong> amphipod Corophium triaenonyx and copepod Nitocra spinipes also.<br />
Brood stock <strong>of</strong> the latter could be maintained in this laboratory for the past six years.<br />
Experimental studies on hatching and growth <strong>of</strong> N. spinipes at different temperatures<br />
have been successfully completed.<br />
Protein rich diets such as egg yolk, Bengal gram, etc. accelerate the growth but<br />
stable population is not maintained with these diets. Low protein food such as<br />
Salvinia detritus does not promote fast growth but maintains steady populations.<br />
Small shrimps belonging to the genus Caridina (20-25 mm) and inhabiting the low<br />
saline upper reaches <strong>of</strong> the estuary were bred and reared in the laboratory. It has<br />
been suggested that these shrimps could easily be mass cultured and utilised as live feed<br />
during the aquaculture <strong>of</strong> bigger shrimps as they are too small to be marketed directly.<br />
(b) Ecological studies<br />
(i) Primary production and benthic studies in relation to prawn culture: Studies on<br />
primary production and benthic organisms in culture ponds at Ramanthruth Island<br />
near the Cochin harbour entrance revealed certain interesting features <strong>of</strong> the environment<br />
in which prawns are grown during the estuarine phase <strong>of</strong> their life history. All<br />
the ponds were highly productive almost throughout the year- The gross primary<br />
production varied from 24 to 1500 mgC/m 3 /day.<br />
(ii) Studies on the improvement <strong>of</strong> traditional shrimp culture in paddy fields:<br />
Hydrographic features monitored during the season revealed no drastic change from,<br />
that <strong>of</strong> preceeding season except that a thin film <strong>of</strong> crude oil was present on the<br />
surface <strong>of</strong> the waters which entered the paddy fields in early December. However,<br />
Penaeus indicus suffered heavy mortality, but such a mortality was not seen in Metapenaeus<br />
dobsoni.<br />
The experimental fields yielded nearly 700 kg <strong>of</strong> shrimps per hectare at Narakkal<br />
and 850 kg at Kumbalangi while the yield in the adjacent ponds employing<br />
traditional methods <strong>of</strong> culture was low-<br />
73
A.3 Protection <strong>of</strong> marine environment and monitoring <strong>of</strong> pollutants along the Indian<br />
coast<br />
Pollution monitoring along the Kerala coast including the major estuaries,<br />
beaches and inshore waters have been undertaken. Seven estuaries and 14 beaches<br />
have been covered in these studies.<br />
(a) Oil pollution monitoring along Kerala coast: For the past three years<br />
Kerala coast from Vizhinjam in the south to Ezhumala in the north remained under<br />
observation for oil pollution and were worked in accordance with the procedure<br />
adopted by the IGOSS. It was noticed that in most <strong>of</strong> the Kerala beaches the magnitude<br />
<strong>of</strong> tar deposition is low as compared to the other beaches in the northern<br />
parts <strong>of</strong> the west coast. Deposition <strong>of</strong> tar balls was high in the open sea beaches<br />
and low at the high tide levels. The quantity ranged between 45 to 550 gm/m 2 .<br />
Underway observations on mangroves and retting grounds from Cochin to<br />
Ezhumala were also made during the year.<br />
(b) Bacteriological studies <strong>of</strong> pollution: Kerala beaches were examined with<br />
reference to indicator bacteria, viz, E.coli, S. faecalis and coliforms in general and<br />
pathogens like Salmonella sp. and Vibrio parahaemoliticus in particular.<br />
A pathogen, viz., Salmonella sp. from some <strong>of</strong> the beaches was isolated and<br />
studied. Its percentage occurrence was 22.71. However, water samples failed to give<br />
positive Salmonella isolation. Beaches like Vizhinjam, Neendakara and Mopla bay<br />
registered E. coli, S. teccalis and coliforms higher than the accepted limits.<br />
The bactericidal property <strong>of</strong> a secretion from Fusarium isolated from Fort<br />
Cochin beach was studied in detail.<br />
(c) Baseline studies on the major estuaries <strong>of</strong> Kerala coast: Studies on seven estuaries,<br />
three in the south and four in the north <strong>of</strong> Cochin were continued. Based on<br />
suspended solids, chemical oxygen demand, permanganate consumed and biochemical<br />
oxygen demand, the water quality <strong>of</strong> estuaries was assessed. Kallai, which has a large<br />
timber industry on its shores, and the Beypore estuary which receives effluents from<br />
a rayon factory in its upper reaches (at Chaliyar), showed a high organic load during<br />
the premonsoon and early monsoon seasons. The dissolved oxygen values, however,<br />
did not show any significant depletion except at Kallai which on some occasions<br />
showed 005 ml/1 in the dry months. No estuary could be described as being grossly<br />
polluted though some <strong>of</strong> them showed much impact <strong>of</strong> human influence.<br />
Organic carbon in the sediments <strong>of</strong> the above estuaries had the following<br />
annual averages: Veli - 2.1%, Neendakara - 1.4%, Thottapally - 2.9%, Kallai - 2.9%,<br />
Beypore- 2.5%, Korapuzha- 3.1% and Mahe- 2.2%. These values were lower as compared<br />
to the annual average <strong>of</strong> 3.5% for Cochin backwaters.<br />
(d) Assessment <strong>of</strong> the status <strong>of</strong> pollution <strong>of</strong> beaches <strong>of</strong> the Kerala coast: Twelve<br />
beaches along the Kerala coast, six in the north and six in the southern side <strong>of</strong><br />
Cochin were monitored for their water quality. The beaches <strong>of</strong> Alleppey, Neendrakara,<br />
West Hill, Kappad, Calicut, Payyambalam and Moplah Bay had much lower salinities.<br />
74
The oxygen saturation values in the clean beaches seldom went down below 90%<br />
while Calicut. West Hill and Mopla Bay showed oxygen deficits due to sewage<br />
discharge. BOD values at the three beaches were generally high. The COD values<br />
ranged from 500-3500 mg/l and permanganate consumed was 60-70 ml/1.<br />
Sand and water samples for environmental characters, bacteriological estimation<br />
and water quality were studied at Ezhumala beach in north Kerala. Based on the<br />
seasonal observations, Ezhumala should be regarded as a 'clean' beach. It is also a<br />
'safe' beach from the public health point <strong>of</strong> view and its water quality. Ezhumala,<br />
Ettikulam and Kappad beaches are under intensive study for their use by the Tourist<br />
Department.<br />
(e) Pollution studies in Cochin backwaters: The three sources <strong>of</strong> pollution, viz.,<br />
sewage, industrial effluents and retting <strong>of</strong> coconuts were extensively studied in the<br />
Cochin backwaters. The daily BOD5 load <strong>of</strong> the sewage systems was worked out as<br />
6.5-7.25 tonnes. Sewage discharge was also found to cause localised depletion <strong>of</strong> oxygen.<br />
A 2000 m 2 retting yard showed a BOD5 load <strong>of</strong> 908 metric tons annually.<br />
The sediment <strong>of</strong> the retting yard was characterised by high organic content 95.3 mg/g.<br />
high C/N 15.0 and high energy content 1994 J/g. The biological effects <strong>of</strong> organic<br />
pollution were clearly evident at all the affected sites. The polychaete Parahetaromastus<br />
tenuis which was found to attain very high population in the retting yard<br />
may be treated as an indicator species <strong>of</strong> pollution.<br />
A view <strong>of</strong> a clean beach Ezhumala<br />
75
The industrial effluents discharged into the northern part <strong>of</strong> the Cochin backwaters<br />
were found to exert varying and intermittent stress on the receiving waters.<br />
The discharge site had varying pH and chloride content. The area had high nutrient<br />
levels especially ammonia. An incidence <strong>of</strong> fish mortality due to high ammonia<br />
(23 ppm) was noticed in Chitrapuzha in the southern part <strong>of</strong> the backwaters.<br />
A.4 Chemical studies in the coastal and <strong>of</strong>fshore waters in the Arabian Sea and Bay <strong>of</strong><br />
Bengal<br />
(a) Particulate trace metals in Cochin backwaters: Particulate matter was analysed<br />
for various trace metals, viz., iron, manganese, copper, zinc, cobalt and nickel<br />
from the Cochin backwaters at various stations covering an area <strong>of</strong> about 15sq km<br />
during the different months <strong>of</strong> the year. Particulate iron content showed a variation<br />
between 80 and 8000 ppm. Manganese concentration was between 4 and 80 ppm. Zinc<br />
content showed a variation from 5 to 500 ppm. Copper was not present in large<br />
quantities and it varied between 2 and 18 ppm. Cobalt and nickel concentrations<br />
varied from 1 to 3 ppm and 1 to 5 ppm respectively. Some <strong>of</strong> the metals like iron,<br />
manganese, etc., were higher at the barmouth entrance channel to the Cochin harbour.<br />
(b) Metal concentration in the sediments <strong>of</strong> the Cochin backwaters: The concentration<br />
<strong>of</strong> non-lithogenous fraction <strong>of</strong> some <strong>of</strong> the metals like iron, manganese<br />
copper, zinc, cobalt, nickel and lead in the sediments <strong>of</strong> the Cochin backwaters were<br />
studied. The general distribution <strong>of</strong> these fractions revealed that there is no marked<br />
seasonal change in the sediments <strong>of</strong> the Cochin backwaters. The concentrations were<br />
slightly higher than the values reported for the shelf and slope sediments <strong>of</strong>f Cochin<br />
This indicates that there is some other source like industrial waste which brings in<br />
these metals into the environment.<br />
A.5 <strong>Oceanography</strong> <strong>of</strong> the waters around Lakshadweep<br />
Studies on the fisheries resources <strong>of</strong> Lakshadweep revealed that Kavaratti atoll<br />
has very poor fisheries. However, at Suheli and Agatti, the catch is quite large.<br />
Studies were also carried out on the distribution <strong>of</strong> tuna based on the available data.<br />
A.6 Studies on land-sea interaction and nearshore circulation along the Indian coastline<br />
and their application to coastal zone management<br />
Beach changes along the Kerala coast: Studies were continued from Munambam<br />
(near Azhikode towards north <strong>of</strong> Cochin) to Cochin. Selected beaches at Azhikode<br />
Edavankhad, Saudi, Chellanam, Thumboli, Punnappra, Karoor were visited to monitor<br />
the beach changes and to study the effects <strong>of</strong> the seawalls constructed.<br />
Studies on the slumping <strong>of</strong> the seawall under the impact <strong>of</strong> scoring effect <strong>of</strong><br />
the breakers at certain location along the beaches revealed that the size <strong>of</strong> armour<br />
should be increased to 20-40 m 3 and the seaward slope <strong>of</strong> the seawall should be<br />
decreased to 1:10. Near Azhikode the sand bar formation continued and extended<br />
southwards beyond the southern bank <strong>of</strong> the barmouth. The beaches at Pannappra,<br />
76
Saudi, Thumboli and Karoor, eventhough· responded to the <strong>of</strong>fshore wave climate<br />
from season to season, they did not show any significant "loss <strong>of</strong> material. These<br />
beaches remained more or less stable.<br />
B. Sponsored Project .<br />
The work carried out under the project, 'Sorting <strong>of</strong> Zooplankton' sponsored<br />
by CSIRO is reported under the Section 3.9.<br />
3.8.2 Regional Centre, Bombay<br />
A greater emphasis was laid during the year on environmental problems and<br />
pollution control studies both under the institutional and sponsored projects. A summary<br />
<strong>of</strong> the work done under the various projects is given below:<br />
A. R and D Projects<br />
1. Protection <strong>of</strong> marine environment and monitoring <strong>of</strong> pollutants along the Indian coast<br />
(a) Base-line water quality <strong>of</strong> the river Narmada (Gujarat)<br />
Suspended solids, pH, chlorides, DO, BOD, PO4 3- -P, NO3 - -N, NO2 - -N and<br />
NH4 + -N were measured at 12 stations along a 70 km stretch <strong>of</strong> the river Narmada<br />
during March-August. Tidal range <strong>of</strong> 1 m was observed upto a point 52 km upstream.<br />
The absence <strong>of</strong> sea water beyond this point became evident by the low<br />
77
chlorinity values (0·02%o). Significant intrusion and mixing <strong>of</strong> saline water which was<br />
upto 44 km upstream in early June was confined only upto 20 km during March.<br />
The water was vertically well mixed and there was no stratification. By August all<br />
traces <strong>of</strong> sea water seem to flush out completely from the river during each tidal<br />
cycle. The pH varied considerably over the tidal cycle. The estuarine zone is characterized<br />
by a high suspended load which decreases appreciably in the fresh water<br />
region. High DO and low BOD indicate the absence <strong>of</strong> gross organic pollution in the<br />
estuarine and riverine zones. NO3 - -N decreased in the direction downstream while<br />
PO4 3- -P showed an increase. NH4 + -N concentration showed normal values throughout.<br />
(b) Comparative study <strong>of</strong> behaviour <strong>of</strong> boron, calcium and magnesium in polluted and<br />
unpolluted estuaries<br />
Behaviour <strong>of</strong> boron, calcium and magnesium in the polluted Ambika and<br />
unpolluted Mindola estuaries (South Gujarat) was studied. A textile mill, a distillary<br />
and a paper and pulp mill release on an average 4.8, 4.3 and 3.8 million litres per<br />
day <strong>of</strong> industrial waste through natural drains into the Ambika estuary. Analysis <strong>of</strong><br />
industrial effluents at the points <strong>of</strong> discharge gave the average boron levels <strong>of</strong> 9.16,<br />
0.78 and 0.23 mg/1 respectively for the different industries.<br />
Although concentrations <strong>of</strong> calcium and magnesium in the Ambika estuary<br />
decreased with decreasing chlorinity, a definite increase in boron concentration was<br />
observed at the ebb slack. Their respective ratios with chlorinity increased systematically<br />
to attain a maxima at the ebb slack water with a abrupt decrease just at<br />
the beginning <strong>of</strong> the flood. The water from the fresh water zone gave a mean concentration<br />
<strong>of</strong> 0.072 mg/kg, 0.0292 g/kg and 0.0188 g/kg for boron, calcium and magnesium<br />
respectively. Mixed behaviour <strong>of</strong> boron during its removal at the early stage<br />
<strong>of</strong> the ebb tide and its maximum addition to the extent <strong>of</strong> 263% at the ebb slack<br />
was observed at the head <strong>of</strong> the estuary indicating large inputs <strong>of</strong> boron coming<br />
from extraneous sources. This phenomenon <strong>of</strong> boron addition was not observed in<br />
the Mindola river estuary and contrary to the expectation its overall removal was 9%<br />
Calcium and magnesium revealed non-linear relationship with chlorinity in both the<br />
estuaries.<br />
In the Mindola estuary, an inverse variation between percent addition/removal<br />
<strong>of</strong> calcium and magnesium suggested an ion-exchange between the two elements. Inverse<br />
relationship between the addition/removal <strong>of</strong> boron and total suspended solids<br />
in the Ambika estuary indicate that boron most probably gets mixed with the<br />
suspended clay minerals in the mixed zone <strong>of</strong> the estuary-<br />
(c) Studies on zooplankton and benthos <strong>of</strong> the Auranga, Ambika, Purna and Mindola<br />
estuaries <strong>of</strong> South Gujarat and waters around Bombay<br />
(i) Zooplankton: Zooplankton variability in the four estuaries in the different<br />
tidal conditions were compared. Mean biomass <strong>of</strong> zooplankton in Auranga, Ambika,<br />
Purna and Mindola were 4.31, 3.46, 3.58 and 3.17 ml/100 m 3 respectively. Relatively<br />
a greater biomass was recorded during the ebb period in Auranga, Purna and at the<br />
78
mouth <strong>of</strong> the Ambika river. In Mindola and in the. upper reaches <strong>of</strong> the Ambika<br />
estuary, the flood period was associated with a greater biomass: Copepods, molluscan<br />
veligers, decapod larvae, mysids and chaetognaths were, the major constituents<br />
in the collection. However, some reduction in the biomass. and population density <strong>of</strong><br />
certain groups was observed in the Ambika and Mindola rivers.<br />
In Bombay waters the chaetognath fauna showed. a maximum density at all<br />
the 4 stations during the postmonsoon period. Among the chaetognaths, Sagitta<br />
bombayensis, S. enflata, S. oceania, S. pulchra, S. bedoti and S. robusta observed, S. bedoti<br />
was the most common species throughout the period <strong>of</strong> investigation. Species diversity<br />
was greater in the unpolluted waters. However, the fluctuation in the population <strong>of</strong><br />
chaetognaths was larger in the polluted region than in the unpolluted area. Disappearance<br />
<strong>of</strong> sensitive species followed by a decrease in the diversity may be the first<br />
indication <strong>of</strong> impending deterioration <strong>of</strong> the environment.<br />
In the case <strong>of</strong> copepods, maximum population density (av.5360/m 3 ) was observed<br />
at Mahim which was about twice as high as that recorded at the other stations.<br />
Mean density <strong>of</strong> copepods at the other three stations varied between 2280 and 2800/m 3 .<br />
Monthly variation <strong>of</strong> total population density <strong>of</strong> zooplankton<br />
79
Major peaks were noticed in the month <strong>of</strong> October/November and March/April. Of<br />
the 21 genera <strong>of</strong> copepod recorded, Paracalanus, Acrocalanus, Acartia and Oithona were<br />
the most common genera. The polluted region was characterised by the dominance<br />
<strong>of</strong> Paracalanus, Acartia and Oithona. But the generic diversity <strong>of</strong> copepods was greater<br />
in unpolluted areas.<br />
(ii) Benthos: Significant abundance <strong>of</strong> macro and meio fauna was noticed in<br />
the four estuaries. Mean densities <strong>of</strong> total benthos per metre square in Auranga,<br />
Purna and Mindola were 318690, 54727, 122350 and 88368 respectively and the<br />
average biomass was 7085, 411, 1814 and 1922 mg respectively. Foraminifera<br />
was the dominant group in all the four estuaries. The diversity <strong>of</strong> benthos was<br />
low in the Ambika as compared to the other three estuaries. Considerable reduction in<br />
the population density <strong>of</strong> benthos was recorded between premonsoon and postmonsoon<br />
in all the four estuaries excepting Auranga. The Auranga and the Purna sustain a<br />
higher benthic productivity than the other two estuaries. High dissolved oxygen,<br />
low biological oxygen demand and average nutrient values were observed in all<br />
the four estuaries.<br />
Around Bombay, qualitative and quantitative benthic studies were undertaken<br />
at eleven stations in polluted and relatively unpolluted waters at Versova,<br />
Mahim and Thana creek. Polychaetes formed the most dominant component <strong>of</strong><br />
the macro benthos while nematodes were the major group <strong>of</strong> meiobenthos. Offshore<br />
stations located in Versova and Mahim had a relatively clean zone with a larger<br />
number <strong>of</strong> faunal group than the other stations. Variations in the group diversity<br />
were quite common among the stations <strong>of</strong>f Versova and Mahim. But a consistancy in<br />
the group diversity which was low was noticed among the different stations <strong>of</strong>f Thana<br />
which probably indicate highly polluted environment.<br />
A.2 Studies on land-sea interaction and nearshore circulation along the coastline<br />
and their application to coastal zone management<br />
(i) Erosion studies at Versova<br />
Field observations on littoral parameters were made at the three stations located<br />
along the Versova beach. Bathymetry and wave regime <strong>of</strong> the area are being analysed<br />
to determine the causative fector and subsequently to determine remedial measures<br />
(ii) Beach studies at Thal-Alibag coastline<br />
Changes in beach-pr<strong>of</strong>ile were monitored at 5 stations along the Thal-Alibag<br />
coastline and the wave climate was studied to estimate the seasonal variability <strong>of</strong> the<br />
accreting/eroding processes near some fishing villages. Dredging is going on in the<br />
Thal creek for navigational purposes. The impact <strong>of</strong> this dredging on the beach<br />
configuration is being investigated.<br />
B. Sponsored Projects<br />
Four sponsored projects were undertaken during the year. These are:<br />
1. Selection <strong>of</strong> waste water disposal site and unloading facility for the fertilizer<br />
plant at Thal.<br />
80
2. Investigations for the undercreek pipeline at Kasheli, Bombay.<br />
3. Seawater sampling and analysis for Bombay High water injection project.<br />
4. Hydrographic studies at Dharamtar Creek along the submarine pipeline route<br />
<strong>of</strong> ONGC.<br />
The progress made under each project has been given separately under the<br />
section 3·9<br />
3.8.3 Regional Centre, Waltair<br />
The various aspects on physical, chemical and geological and geophysical studies<br />
were carried out under the R and D project "Coastal studies <strong>of</strong>f Waltair and adjacent<br />
areas". The centre also undertook two sponsored projects. The details <strong>of</strong> the work<br />
done are as follows:<br />
A.l Physical oceanography studies<br />
A. R and D Project<br />
Beach pr<strong>of</strong>ile studies started in 1979 were intensified for a further period <strong>of</strong> 14<br />
months and observations were taken at monthly intervals. The analysis and interpretation<br />
<strong>of</strong> the data pertaining to erosion and accretion along the beach are being<br />
finalized. Rip currents, which are dangerous to swimmers were identified. Similarly<br />
the other beach characteristics suitable for recreation have also been enumerated at<br />
some points <strong>of</strong> the beach. Observations on a time series on the vertical distribution<br />
<strong>of</strong> temperature and currents at a single station <strong>of</strong>f Waltair have been initiated. These<br />
measurements were made at hourly interval once in a month over a tidal cycle to<br />
study the seasonal distribution <strong>of</strong> these parameters. Temperature and salinity distribution<br />
were also studied along three transects <strong>of</strong>f Visakhapatnam—each extending upto<br />
100m water depth to identify the upwelling and sinking <strong>of</strong> the water masses in these<br />
areas. The effect <strong>of</strong> cyclone <strong>of</strong> May 1979 on the beaches has been studied.<br />
A.2 Chemical oceanography studies<br />
Chemical studies along the three transects upto 100 m water depth in the continental<br />
shelf <strong>of</strong> Visakhapatnam, covering an area between Bhimunipatnam and Appikonda,<br />
were made. The samples are being analysed to study the concentration <strong>of</strong> the<br />
nutrients such as phosphorus, nitrogen, oxygen and trace metals.<br />
Studies have been undertaken in the Visakhapatnam inner and outer harbour<br />
areas to estimate the concentrations <strong>of</strong> the pollutants and to study their seasonal<br />
distribution. Collection <strong>of</strong> the data for a period <strong>of</strong> one year has been completed and the<br />
analysis <strong>of</strong> the data is in progress. A modified spectrophotometric method for the<br />
determination <strong>of</strong> copper has been developed and laboratory studies have been undertaken<br />
for the estimation <strong>of</strong> copper.<br />
A.3 Geological and geophysical studies<br />
In conjunction with the other studies, geological work consisting <strong>of</strong> mineralogy<br />
81
and geochemistry <strong>of</strong> the continental shetf between Bhimunipatnam and Appikonda<br />
were conducted. Nearly 150 sediment samples at 10 m water depth interval between<br />
10 and 100 m depths were collected to study the grain size distribition. the mineralogy<br />
and the geochemistry <strong>of</strong> the sediments. Grain size analysis has been completed for<br />
more than 100 samples. Heavy mineral separation is in progress.<br />
The sediment samples collected from R.V. Gaveshani from the continental margin<br />
between Visakhapatnam and Madras have been analysed for the grain size distribution<br />
and their geochemical properties. Beach rock samples obtained from the Visakhapatnam<br />
port authorities have also been analysed.<br />
In the field <strong>of</strong> marine geophysics computer programme for the analysis <strong>of</strong><br />
magnetic data by solving the linear equations has been developed. Theoretical studies<br />
for the analysis <strong>of</strong> the magnetic data using the models such as horizontal plate and<br />
thin sheet have been completed. Marine magnetic, gravity and bottom topographic<br />
data <strong>of</strong> the Bay <strong>of</strong> Bengal were analysed and interpreted to study the crustal structure<br />
and basement tectonics <strong>of</strong> the Bay <strong>of</strong> Bengal. The studies have delineated<br />
several new surface and subsurface structural features such as an escarpment as a<br />
surface and subsurface high over the continental slope extending along the east coast <strong>of</strong><br />
India, a deep and wide marginal basin over the southern continental margins <strong>of</strong> the<br />
east coast <strong>of</strong> India and a graben extending in southeast and northwest direction.<br />
Extension <strong>of</strong> volcanic activity into the <strong>of</strong>fshore regions <strong>of</strong>f central east coast <strong>of</strong> India<br />
has been identified from the topographic highs associated with the prominent magnetic<br />
anomalies.<br />
B. Sponsored Projects<br />
The centre undertook the following two sponsored projects during the year:<br />
1. Oceanographic studies for determining the point and mode <strong>of</strong> discharge <strong>of</strong><br />
treated effluents from the steel plant into the sea for Visakhapatnam Steel Plant, sponsored<br />
by Steel Authority <strong>of</strong> India Limited, Visakhapatnam.<br />
2. Shallow seismic and side scan sonar surveys for Visakhapatnam Port Trust,<br />
sponsored by the Visakhapatnam Port Trust, Visakhapatnam.<br />
Details <strong>of</strong> the work done under these two sponsored projects are separately<br />
given under the Section 3.9.<br />
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3.9<br />
Sponsored Projects<br />
3.9.1 Development <strong>of</strong> <strong>of</strong>fshore oilfields<br />
3.9.2 Pollution control and monitoring<br />
3.9.3 Coastal development<br />
3.9.4 Resources survey<br />
3.9.5 Miscellaneous projects<br />
3.9.6 Consultancy services<br />
A total number <strong>of</strong> 26 sponsored projects for a total value <strong>of</strong> Rs. 36 lakhs were<br />
undertaken at the request <strong>of</strong> various organizations. These projects being <strong>of</strong> direct<br />
benefit to the user community, were given a high priority.<br />
3.9.1 Development <strong>of</strong> <strong>of</strong>fshore oilfields (sponsored by ONGC)<br />
(i) Survey <strong>of</strong> the submarine pipeline routes from Bassein to Gujarat (Phase III)<br />
In continuation <strong>of</strong> the earlier surveys, the routes from Bassein to Dahanu and<br />
Bassein to Navapur were surveyed. Along the route from Bassein to <strong>of</strong>f Dahanu (108<br />
km), the depth range was from 25 to 53 m and the gradients were from horizontal to<br />
1 : 1000. The seabed was found to be covered by 10 to 20 m clay in which acoustic<br />
masking due to gases occurred upto a distance <strong>of</strong> about 60 km. Along the route from<br />
Bassein to Navapur (88 km), the depth varied from 15 m near the shore to 53 m near<br />
Bassein. The seabed was covered with more than 50 m clay and acoustic masking dueto<br />
gases occurred for about 38 km.<br />
(ii) Seabed surveys on the D & I structures, Kori Great Bank and on the Tapti Dome<br />
Structure<br />
The seabed surveys for the proposed drilling sites on the Kori Great Bank (D & I<br />
structures) comprised <strong>of</strong> 240 line km <strong>of</strong> echosounding. 220 line km <strong>of</strong> side scan sonar<br />
and 145 line km <strong>of</strong> shallow seismic pr<strong>of</strong>iling while at the Tapti Dome Structure, it<br />
consisted <strong>of</strong> 25 line km <strong>of</strong> echosounding. side scan sonar and shallow seismic pr<strong>of</strong>iling<br />
followed by seabed sampling.<br />
(iii) Postlay survey <strong>of</strong> the Bombay High to Bombay pipelines<br />
The surveys included 640 line km <strong>of</strong> echosounding. 185 line km <strong>of</strong> side scan,<br />
sonar and 640 line km <strong>of</strong> ORE subbottom pr<strong>of</strong>iling. The analyses <strong>of</strong> the records<br />
83
showed that: (a) out <strong>of</strong> 50 tracks in which pipelines were recorded, the pipelines are<br />
exposed in 5 tracks and buried in 0.8 to 2.7 m clays in 45 tracks, (b) the interpipeline<br />
distance varied from 65 m to 100 mm and (c) out <strong>of</strong> the 78 line km <strong>of</strong> pipelines,<br />
about 76 line km were covered and about 2 line km were exposed. The survey<br />
report has been submitted to ONGC.<br />
(iv) Surveys <strong>of</strong> the pipeline routes from Direction Bank to Bassein and Murud<br />
Along the proposed pipeline route from Bassein to Direction Bank, the depth<br />
varied from 41 to 65 m and the seabed was covered by clay upto 22 m thick. Along<br />
the route from Direction Bank to the shore, the depth ranged from 15 to 55m and the<br />
seabed was covered by clays upto 30 m thick. Along both the routes, thick clays<br />
covered the uneven topography <strong>of</strong> the underlying sands at many places.<br />
(v) Bathymetric and shallow seismic surveys <strong>of</strong>f South Bassein<br />
The surveys comprised <strong>of</strong> about 630 line km <strong>of</strong> shallow seismic pr<strong>of</strong>iling. The<br />
echograms and seismic pr<strong>of</strong>iles indicate that the seabed in the northern and eastern<br />
area <strong>of</strong>f Bassein is marked by even topography due to clay cover (maximum about<br />
25 m) and in the south-western area by an uneven topography where the underlying<br />
hard strata are exposed.<br />
(vi) Bathymetric and shallow seismic surveys on the Direction Bank<br />
The depths on the Direction Bank ranged from 36 m in the south to 65 m in the<br />
north and west. The bank slopes gently to the north. Its western flanks are steeperthan<br />
the eastern flanks.The crest <strong>of</strong> the bank is marked by an undulatory or dissected<br />
topography. Seismic pr<strong>of</strong>iles show that it is a lensoid body <strong>of</strong> clay with a maximum<br />
thickness <strong>of</strong> 34 m on the crest which gradually thins out towards the flanks. The<br />
clay overlies the relict sands with an uneven topography.<br />
(vii) Seawater sampling and analysis for Bombay High water injection project<br />
The work was carried out to evaluate the best depth for the intake <strong>of</strong> water to<br />
be used for flooding or for pressure maintenance in the <strong>of</strong>fshore oilfields at Bombay<br />
High for the secondary recovery <strong>of</strong> oil. Sampling programme was undertaken at three<br />
locations and included the various physical and chemical parameters. On the basis <strong>of</strong><br />
these findings, 30m depth has been considered as the best depth for water intake-<br />
Monthly variations <strong>of</strong> the different parameters at this depth will be studied to facilitate<br />
the design <strong>of</strong> the treating systems.<br />
(viii) Hydrographic studies <strong>of</strong>f Murud-Janjira<br />
Collection <strong>of</strong> field data on currents, temperature, etc. in support <strong>of</strong> the drilling<br />
activities <strong>of</strong> ONGC <strong>of</strong>f Murud-Janjira was undertaken during May to October <strong>1980</strong>.<br />
This work was carried out <strong>of</strong>f Ratnagiri (Maharashtra).<br />
(ix) Hydrographic studies at Dharamtar creek along the submarine pipeline route<br />
<strong>of</strong> ONGC<br />
Short-term observations on the currents, temperature, etc. were made at certain<br />
locations in Dharamtar creek in June <strong>1980</strong>. Echosounding was also carried out.<br />
84
3.9.2 Pollution control and monitoring<br />
(i) Hydrobiological survey <strong>of</strong> the Gurpur river, New Mangalore Harbour amd the sea<br />
<strong>of</strong>f Mangalore (Phase II)<br />
This project was undertaken at the request <strong>of</strong> Kudremukh Iron Ore Co. Ltd.,<br />
Bangalore. Periodic sampling <strong>of</strong> the bottom population in the area has been carried<br />
out for the collection <strong>of</strong> baseline information covering the pollution period. The<br />
analysis <strong>of</strong> the samples is in progress.<br />
(ii) Oceanographic studies for determining the point <strong>of</strong> discharge <strong>of</strong> treated effluents<br />
from the Visakhapatnam Steel Plant into the sea<br />
This project was sponsored by Steel Authority <strong>of</strong> India Ltd., Visakhapatnam.<br />
The work during the year included the analysis <strong>of</strong> data collected during the previous<br />
year and the preparation <strong>of</strong> the report.<br />
(iii) Selection <strong>of</strong> waste water disposal site and unloading facility for the fertilizer<br />
plant at Thal.<br />
At the request <strong>of</strong> Rashtriya Chemicals and Fertilizers Ltd. (RCF Ltd.) who<br />
proposes to put up a giant fertilizer complex at Thal-Vaishet near Alibag. a survey<br />
was undertaken to locate a. suitable discharge site for the wastes from the plant and<br />
to evaluate the environmental impact <strong>of</strong> the waste on the water quality and biological<br />
productivity <strong>of</strong> the region. The observations included recording <strong>of</strong> the tides,<br />
currents, waves, wind, temperature, salinity, bathymetry, etc. The water quality <strong>of</strong> the<br />
region was studied and baseline data were collected. Seasonal changes in various<br />
chemical parameters and the probable influence <strong>of</strong> the toxicants, if any, present in the<br />
effluents on the water quality were investigated. Studies on primary, secondary and<br />
benthic productivity <strong>of</strong> the area were also investigated along the northern, middle<br />
and southern transects. Further analysis <strong>of</strong> the data is in progress.<br />
3.9.3 Coastal development<br />
(i) Shallow seismic and side scan sonar surveys in Mormugao harbour<br />
This project was sponsored by the Mormugao Port Trust. More than 125<br />
line km <strong>of</strong> echosounding, side scan sonar and shallow seismic pr<strong>of</strong>iling (ORE Mud<br />
Penetrator) were carried out along the lines at 100 m apart. The depths in the area<br />
surveyed ranged from 2 to 16 m and the seabed was marked by even and uneven<br />
topography and the thickness <strong>of</strong> the top, unconsolidated sediments varied from 1 to<br />
26 m. Based on the results, some positive recommendations have been made. The<br />
report has been submitted to the Port Trust Authorities.<br />
(ii) Shallow seismic and side scan sonar survey in Visakhapatnam outer, inner and<br />
fishing harbours<br />
At the request <strong>of</strong> the Visakhapatnam Port Trust, some surveys were carried out<br />
in 1979 in the outer harbour area. During the year, the work was extended to inner<br />
85
and fishing harbour areas. The surveys comprised <strong>of</strong> about 140 line km <strong>of</strong> echosounding,<br />
46 line km <strong>of</strong> side scan sonar and 115 line km <strong>of</strong> shallow seismic pr<strong>of</strong>iling.<br />
The side scan sonar and seismic records confirmed the occurrence <strong>of</strong> the rock outcrops<br />
near the shore, the breakwater and isolated outcrops at some places. Side scan<br />
sonar records also indicated two anomalous objects in the oil mooring area and a<br />
ship wreck in the outer channel at a depth <strong>of</strong> 35 m. The report incorporating the<br />
recommendations <strong>of</strong> the surveys has been submitted to the sponsors.<br />
3.9.4 Resources survey<br />
(i) Seaweed cultivation at Malvan<br />
This project has been undertaken at the request <strong>of</strong> the Government <strong>of</strong> Maharashtra.<br />
The work includes development <strong>of</strong> techniques for the cultivation <strong>of</strong> seaweeds<br />
in coastal waters. The seaweeds <strong>of</strong> economic importance are being cultivated on the<br />
coir rope frames <strong>of</strong> suitable size.<br />
(ii) Photorespiration in marine environment<br />
This project has been undertaken at the request <strong>of</strong> Department <strong>of</strong> Science and<br />
Technology, New Delhi. The experimental work is <strong>of</strong> a basic nature and would lead<br />
to a better understanding <strong>of</strong> the living matter in the sea. The laboratory facilities<br />
are being built up.<br />
3.9.5 Miscellaneous projects<br />
(i) Investigation for the undercreek pipeline at Kasheli, Bombay<br />
At the request <strong>of</strong> the Bombay Municipal Corporation, studies were undertaken<br />
to gather the baseline data on the parameters pertaining to the mechanics <strong>of</strong> sediment<br />
transport in relation to dredging and maintenance <strong>of</strong> an undercreek channel for<br />
laying a freshwater conduit from Bhatsai reservoir across the Bassein Creek/Ulhas<br />
River near the existing Kasheli Bridge, north <strong>of</strong> Thana.<br />
Investigations on the tidal regime, tidal currents, suspended sediment load,<br />
sediment characteristics <strong>of</strong> the bed and the pr<strong>of</strong>iles <strong>of</strong> the channel were conducted<br />
at a portion <strong>of</strong> Thana/Bassein creek to understand the pattern <strong>of</strong> sediment transport.<br />
The results <strong>of</strong> the investigations in the form <strong>of</strong> a report have been submitted to the<br />
sponsors.<br />
(ii) Survey to measure the distance between the piers <strong>of</strong> the Zuari Bridge, Cortalim, Goa<br />
M/s Gammon India Ltd., the construction engineers <strong>of</strong> the bridge at Cortalim,<br />
Goa, requested NIO to measure the distance between P2 and P6 piers <strong>of</strong> the bridge.<br />
The work was completed with the help <strong>of</strong> Theodolite and Mini Ranger MRS III and<br />
the report submitted to the sponsors.<br />
(iii) Development <strong>of</strong> a marine park at Malvan (Maharashtra)<br />
This project was sponsored by the Government <strong>of</strong> Maharashtra and included<br />
86
ecological studies at Malvan in order to set up a marine park. The report has been<br />
submitted to the sponsors.<br />
(iv) Design and fabrication <strong>of</strong> conductivity-temperature-depth recorder (CTD)<br />
This project was undertaken at the request <strong>of</strong> Electronic Commission <strong>of</strong> India.<br />
The instrument has been developed and tested on board the research ship Gaveshani.<br />
The know-how is being released for commercialisation.<br />
3.9.6 Consultancy services<br />
(i) Ocean Thermal Energy Conversion Plant site studies<br />
At the request <strong>of</strong> Tamil Nadu Electricity Board, physical, chemical and<br />
biological features <strong>of</strong> the waters <strong>of</strong>f Coromandal Coast site for OTEC plant were<br />
studied. These studies included recording <strong>of</strong> wind speed, wind direction, sea surface<br />
temperature, atmospheric pressure and the collection <strong>of</strong> samples for various biological<br />
and chemical parameters. A preliminary report has already been submitted to the<br />
sponsors.<br />
(i) Nautical and physical oceanographic observations <strong>of</strong>f the drilling rig "Chancellors<br />
Ville" in the Mahanadi Basin<br />
As requested by Oil India Ltd., Bhubaneshwar, observations on some nautical<br />
and physical parameters were carried out <strong>of</strong>f the drilling rig "Chancellors Ville" in the<br />
Mahanadi basin. These included satellite navigation fixes, currents, waves and tidal<br />
measurement. The Decca Navigator and radar were also operated. A report incorporating<br />
the findings <strong>of</strong> the work has been submitted to OIL, Bhubaneshwar.<br />
(iii) Sorting <strong>of</strong> zooplanklon samples<br />
The Regional Centre. Cochin continued the sorting <strong>of</strong> zooplankton samples for<br />
the Commonwealth Scientific and Industrial Research Organisation (CSIRO), Sydney,<br />
Australia. About 15,000 ml <strong>of</strong> samples received from CSIRO were sorted during the<br />
year.<br />
(iv) Location <strong>of</strong> underwater object for NSTL, Visakhapatnam<br />
At the request <strong>of</strong> NSTL, Visakhapatnam, the Regional Centre <strong>of</strong> NIO at<br />
Waltair carried out a side scan sonar survey to locate some underwater object in<br />
the waters <strong>of</strong>f Visakhapatnam.<br />
(v) Miscellaneous services<br />
A number <strong>of</strong> services comprising <strong>of</strong> chemical analysis, geotechnical analysis etc.,<br />
were rendered to various private and public sector organizations and universities.<br />
87
Some clients <strong>of</strong> NIO<br />
1 Alkali and Chemical Corporation <strong>of</strong> India<br />
2 Atomic Power Authority ( BARC ), Bombay<br />
3 Ballarpur Industries Ltd·, Karwar<br />
4 Bharat Salt and Chemical Industries, Bombay<br />
5 Bombay Municipal Corporation, Bombay<br />
6 Bombay Port Trust, Bombay<br />
7 Central Board for Prevention and Control <strong>of</strong> Water Pollution, New Delhi<br />
8 Cochin Port Trust, Cochin<br />
9 Commonwealth Scientific & Industrial Organization, Sydney, Australia<br />
10 Department <strong>of</strong> Science and Technology, New Delhi<br />
11 Eco-Zst Co. Pvt. Ltd., Tehran, Iran<br />
12 Electronics Commission <strong>of</strong> India, New Delhi<br />
13 Engineers India Ltd., New Delhi<br />
14 Environmental Engineering Consultants, Bombay<br />
15 Fiskeridirektoratets Havforsknings <strong>Institute</strong>, Bergen, Norway<br />
16 Gomantak Land Development. Panaji<br />
17 Government <strong>of</strong> Andhra Pradesh<br />
18 Government <strong>of</strong> Goa, Daman and Diu<br />
19 Government <strong>of</strong> Gujarat<br />
20 Government <strong>of</strong> Kerala<br />
21 Government <strong>of</strong> Maharashtra<br />
22 Government <strong>of</strong> Tamil Nadu<br />
23 Gujarat Narmada Valley Fertilizers Ltd., Baruch<br />
24 Gujarat Water Pollution Board, Ahmedabad<br />
25 Hoescht Pharmaceuticals Ltd., Bombay<br />
26 India Resort Hotels Ltd., Bombay<br />
27 Indian <strong>National</strong> Science Academy, New Delhi<br />
28 Indian Navy<br />
29 Indo-Norwegian Project, Cochin<br />
30 International Foundation <strong>of</strong> Science, Stockholm, Sweden<br />
31 Kudremukh Iron Ore Co. Ltd., Bangalore<br />
32 Mangalore Chemicals and Fertilizers Ltd., Mangalore<br />
33 Mangalore Port Trust, Mangalore<br />
34 Mormugao Port Trust, Mormugao<br />
35 Oil & Natural Gas Commission, Bombay<br />
36 Oil India Ltd., Bhubaneshwar<br />
37 Tamil Nadu Electricity Board, Madras<br />
38 Rashtriya Chemicals & Fertilizers Ltd., Bombay<br />
39 Steel Authority <strong>of</strong> India Ltd., Visakhapatnam<br />
40 Travancore Titanium Products Ltd., Trivandrum<br />
41 United Nations Environment Programme, Nairobi<br />
42 United Shippers and Dredgers Ltd.,<br />
43 Vikram Sarabhai Space Centre, Govt. <strong>of</strong> India, Trivandrum<br />
44 Visakhapatnam Port Trust, Visakhapatnam<br />
45 World Wild Life Fund, Bombay<br />
46 Zuari Agro-Chemicals & Fertilizers Ltd., Zuari Nagar, Goa<br />
88
3.10<br />
International Projects<br />
3.0.1 Marine pollution monitoring under Integrated Global Ocean Station<br />
System (IGOSS)<br />
3.10.2 Culture <strong>of</strong> mussels, oysters and prawns using treated domestic<br />
sewage under International Foundation <strong>of</strong> Science, Stockholm, Sweden.<br />
3.10.1 Marine pollution monitoring under Integrated Global Ocean Station System<br />
(IGOSS)<br />
Under the project "Marine Pollution (Petroleum) Monitoring Pilot Project<br />
(MAPMOPP)" oil slicks and other floating pollutants, particulate petroleum residue<br />
(tar balls) and dissolved/dispersed hydrocarbons were monitored along the oil tanker<br />
routes in the southern Bay <strong>of</strong> Bengal, from south <strong>of</strong> Sri Lanka to the head <strong>of</strong> the<br />
Malacca Strait, and in a part <strong>of</strong> the Andaman Sea deploying R.V. Gaveshani. Oil<br />
slicks could not be observed during the two crossings along the tanker routes. However,<br />
freshly formed tar balls, very <strong>of</strong>ten in high concentrations were encountered<br />
during the second crossing (January-February, <strong>1980</strong>) at 5°30'N Latitude and 79°00<br />
to 88°00'E Longitudes. The density <strong>of</strong> occurrence <strong>of</strong> the tar balls ranged from<br />
005 to 69.75 mg/m 2. For the hydrocarbon analysis, water samples were collected<br />
from three depths and analysed in the shore laboratory employing UV Spectrophotometry<br />
method developed by NIO. The analysis indicates that their concentration<br />
ranged from 5.3-42.0 μg/kg at the surface, 2.2-3.4 μg/kg at 10 m; 1.08 μg/kg at 20 m;<br />
11 and 13.0 μg/kg at 30 m (2 samples) and 7.1 μg/kg at 600 m.<br />
The project was completed and all the data collected from the Indian Ocean<br />
region from 1975-<strong>1980</strong> were compiled and a report was submitted to IOC as a regional<br />
coordination activity <strong>of</strong> NIO. Some <strong>of</strong> the features <strong>of</strong> the report are:<br />
Oil slicks were sighted on 5582 occasions which is 83.5% <strong>of</strong> the total observations<br />
numbering 6689. This indicates that the Northern Indian Ocean appears to<br />
be a fairly notorious area for oil slicks. Concentration <strong>of</strong> tar balls ranged from<br />
0-6.0 mg/m 2<br />
with a mean value <strong>of</strong> 0.59 mg/m 2<br />
in the eastern oil tanker routes along<br />
the Arabian Sea. The same ranged from 0 to 69.25 mg/m 2<br />
with a mean value <strong>of</strong><br />
1.52 mg/m 2<br />
. At a first approximation the Arabian Sea oil tanker route will have<br />
about 3700 tonnes <strong>of</strong> floating tar balls and the Bay <strong>of</strong> Bengal oil tanker route<br />
will have 1100 tonnes <strong>of</strong> floating tar balls at any one time along the route.<br />
89
3.10.2 Culture <strong>of</strong> mussels, oysters and prawns using treated domestic sewage under the<br />
International Foundation <strong>of</strong> Science, Stockholm, Sweden<br />
(a) Phytoplankton culture: Differeat phytoplankton cultures were tested as a food<br />
material for green mussels and the rate <strong>of</strong> intake, selectivity and relevant aspects were<br />
investigated.<br />
(b) Artemia culture: A survey was conducted on the occurrence <strong>of</strong> brine<br />
shrimp, Artemia along the coasts <strong>of</strong> Tamil Nadu, Maharashtra and Gujarat to identify<br />
Artemia resources. This led to the finding <strong>of</strong> new Artemia populations in the salt<br />
pans along the Saurashtra and Kutch coasts <strong>of</strong> Gujarat. Ailarge deposit <strong>of</strong> Anemia<br />
cysts was also located in the Rann <strong>of</strong> Kutch.<br />
90
4<br />
Infrastructure Services<br />
41 Computer<br />
4.2 Geotechnical laboratory<br />
4.3 Library<br />
4.4 Electroplating<br />
4.5 Workshop<br />
4.6 Reprography<br />
4.7 Prototype<br />
4.8 Analytical facilities<br />
Under the infrastructure services, various facilities were made available to the<br />
<strong>Institute</strong>'s R & D staff. Besides the staff <strong>of</strong> NIO some private and public sector<br />
organizations were also benefitted by these service.<br />
4.1 Computer<br />
The computer facility available at the Data Centre was made use <strong>of</strong> by NIO<br />
scientists, and also by many outside agencies for their commercial and technical<br />
data processing. Notable outside agencies were Zuari Agro Chemicals Ltd., Cancer<br />
Research Society Hospital, Goa Engineering College and Mormugao Port Trust.<br />
For details <strong>of</strong> the programme and s<strong>of</strong>tware please see page 67.<br />
4.2 Geotechnical Laboratory<br />
This laboratory is equipped with the following facilities besides usual apparatus<br />
for testing <strong>of</strong> the soil:<br />
(i) Triarial test equipment, (ii) Swelling test apparatus, (iii) Consolidometers,<br />
(iv) Pesoneability and settlement test apparatus and (v) Tore vane shear.<br />
A large number <strong>of</strong> soil samples were analysed and services were Tendered to<br />
many public and private organizations.<br />
91
machine.<br />
4.3 Library<br />
With the acquisition <strong>of</strong> 853 books, 721 technical reports and 10 additional<br />
journals during the year, the total number <strong>of</strong> books, technical reports and journals<br />
have reached 9210, 3021 and 290 respectively. Out <strong>of</strong> 290 journals received, 80 were<br />
received on an exchange basis with NIO publications.<br />
Besides these additions, the library received a very valuable personal library<br />
<strong>of</strong> Pr<strong>of</strong>. E.C. La Fond, as a gift to the <strong>Institute</strong>. Pr<strong>of</strong>. La Fond is a physical<br />
oceanographer <strong>of</strong> great eminence and repute from the United States. He is at present<br />
the General Secretary, IAPSO, California, U.S.A. The collection includes 100 books,<br />
800 technical reports and back volumes <strong>of</strong> important journals, atlases and thousands<br />
<strong>of</strong> reprints. The NIO greatly appreciates his kind gesture. Dr. La Fond has been<br />
associated with India since a long time and he is a great well-wisher <strong>of</strong> NIO and<br />
its staff.<br />
Under the Documentation Services, the New Arrivals (monthly), Aquatitles<br />
(fortnightly) were continued like the previous year. A new Bibliographic Service was<br />
initiated this year and the first bibliography on Primary Production in the Oceans<br />
was compiled and distributed to all concerned.<br />
Library facilities at the regional centres at Cochin, Bombay and Waltair were<br />
further strengthened in respect <strong>of</strong> both books and journals.<br />
4.4 Electroplating<br />
Electroplating <strong>of</strong> various components and gadgets <strong>of</strong> CTD, CTD winch, echosounder<br />
unit, tide gauge unit, side scan sonar, current meter, microscope pressorsensor,<br />
petroleum hydrocarbon sampling device, Marex data buoy and various other<br />
significant jobs were carried out by this group-<br />
4.5 Workshop<br />
The workshop is equipped with a variety <strong>of</strong> machines to render repair and maintenance<br />
services. Following are some <strong>of</strong> the machines available:<br />
(i) Shaping Machine (BSH-63), Batliboi & Co. Ltd.<br />
(ii) Lathe Machines: (a) HMT Lathe Machine (H-22), (b) HYT Precision Mini<br />
Lathe, (c) GEDEE WELLER Precision Lathe (Voltas) and (d) Kirloskar<br />
Lathe MGD-2.<br />
(iii) MT Milling Machine FN-2.<br />
(iv) SME VS Universal 3-dimensional Pantograph engraving and pr<strong>of</strong>ile milling<br />
(v) Various drilling, folding and cutting machines.<br />
During the year the workshop completed more than 400 jobs ranging in<br />
quality from electronics to automechanical types.<br />
92
4.6 Reprography<br />
(i) Photography: Photographic services were rendered to all the R and D<br />
projects <strong>of</strong> the <strong>Institute</strong> both in the laboratory and in the field including on board<br />
the research vessel Gaveshani. In all about 300 major institutional jobs were attended<br />
to including photographic assistance in the preparation <strong>of</strong> several scientific papers<br />
and technical and sponsored project reports.<br />
(ii) Drawing: A very large number <strong>of</strong> jobs such as line drawings, charts,<br />
scientific and technical diagrams, maps, civil, mechanical, electrical engineering<br />
drawings were attended to in addition to ammonia copying and photocopying services.<br />
(iii) Printing and binding: The printing and binding facility was utilized to the<br />
fullest extent by the various divisions and administrative wing. Most <strong>of</strong> the<br />
<strong>Institute</strong>'s printing work except the Annual Report and Mahasagar was undertaken at<br />
the NIO press.<br />
(iv) Xeroxing: A very large number <strong>of</strong> jobs were attended to including the jobs<br />
from library and individuals. Efforts were made to provide this service at all levels<br />
<strong>of</strong> the <strong>Institute</strong> and more machines are being procured.<br />
4.7 Prototype laboratory<br />
The group rendered its services in carrying out the following works:<br />
(i) Fabrication <strong>of</strong> different types <strong>of</strong> sensors and fibre glass box casings for the<br />
instruments,<br />
(ii) Fabrication <strong>of</strong> fibre glass cable drum for the assembly <strong>of</strong> winches and<br />
(iii) Fabrication <strong>of</strong> printed circuits on double sided boards.<br />
4.8 Analytical facility<br />
Under this service a large number <strong>of</strong> samples were analysed for Government<br />
institutions, universities and research centres. This facility is available in the<br />
Chemical <strong>Oceanography</strong> Division and provides help to different types <strong>of</strong> users.<br />
93
Λ view <strong>of</strong> Library<br />
A view <strong>of</strong> workshop
5<br />
Administrative Set-up<br />
5.1 Cruise Planning and Programme Priorities Committee for R. V. Gaveshani<br />
1. Director-General. SIR<br />
CSIR. Rafi Marg,<br />
New Delhi.<br />
2. Capt. M. Sethi<br />
Shipping Corporation <strong>of</strong> India<br />
Bombay.<br />
3. Shri S. N. Batra<br />
Technical Manager, Shipping Corporation <strong>of</strong> India<br />
Bombay-<br />
4. Shri A. Ananthakrishnan<br />
Director (Development)<br />
Ministry <strong>of</strong> Shipping & Transport<br />
New Delhi-<br />
5. Shri V. R. Venkoba Rao<br />
Geological Survey <strong>of</strong> India<br />
Calcutta.<br />
6. Capl. V. Ravindranath<br />
Director (OPS), Coast Guard H.Q.<br />
New Delhi.<br />
7. Shri R. K. Kutkar<br />
Assistant Wireless Adviser<br />
Ministry <strong>of</strong> Communication<br />
New Delhi.<br />
8. Shri P. Satyanarayana<br />
Naval Hydrographic Office<br />
Dehra Dun.<br />
9. Shri K. R. G. K. Murty<br />
Naval Physical & Oceanographic Laboratory<br />
Naval Base, Cochin-<br />
10. Dr. V. L. N. Sastry<br />
Chief Geophysicist, ONGC, Bombay Offshore Project<br />
Bombay.<br />
11. Dr. K. L. Kaila<br />
Project Coordinator, Deep Seismic Survey Project<br />
<strong>National</strong> Geophysical Research <strong>Institute</strong><br />
Hyderabad-<br />
12. Dr. D. K. Rakshit<br />
Department <strong>of</strong> Science & Technology<br />
New Delhi.<br />
95
18. Dr. E. G. Silas "<br />
Cochin.<br />
4. Dr. P. K. Das "<br />
13. Dr. V. V. Bhartiya „<br />
Principal Scientific Officer<br />
Department <strong>of</strong> Science & Technology<br />
New Delhi.<br />
14. Shri K. N. Johry „<br />
Head. International Scientific Collaboration<br />
CSlR, Rafi Marg<br />
New Delhi.<br />
15. Dr. D. Shankar Narayan ,,<br />
Additional Secretary<br />
University Grants Commission<br />
New Delhi.<br />
16. Pr<strong>of</strong>. D. Lal, FRS „<br />
Director, Physical Research Laboratory<br />
Ahmedabad.<br />
17. Dr. S. P. Jagota<br />
Joint Secretary and Legal Adviser<br />
Ministry <strong>of</strong> External Affairs<br />
New Delhi.<br />
Director, Central Marine Fisheries Research <strong>Institute</strong><br />
19. Dr. A. K. Ganguly<br />
<strong>National</strong> Fellow in Environmental Sciences<br />
Bhabha Atomic Research Centre<br />
Trombay-Bombay.<br />
20. Commodore I. K. Puri ,,<br />
Adviser, NIO (Ship matters)<br />
CSIR, Rafi Marg<br />
New Delhi-<br />
21. Dr. S. Z. Qasim Convenor<br />
Director, <strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Dona Paula, Goa.<br />
5.2 Research Advisory Council<br />
1. Pr<strong>of</strong>. D. Lal, FRS Chairman<br />
Director, Physical Research Laboratory<br />
Ahmedabad.<br />
2. Dr.R. Raghu Prasad Member<br />
Assistant Director-General, ICAR<br />
New Delhi-<br />
3. Dr. V. V. Sastri "<br />
Director, R & D<br />
<strong>Institute</strong> <strong>of</strong> Petroleum Exploration<br />
Kaulagarh Road, Dehra Dun.<br />
Director-General <strong>of</strong> Meteorology<br />
India Meteorology Department<br />
Lodhi Road, New Delhi-<br />
96
5. Vice-Admiral O.S. Dawson, AVSM, PVSM<br />
Flag Officer Commanding-in-Chief<br />
Southern Command, Naval Base, Cochin.<br />
6. Dr. A.K. Ganguly<br />
<strong>National</strong> Fellow in Environmental Sciences<br />
Bhabha Atomic Research Centre<br />
Trom bay, Bo mbay.<br />
7. Dr. D. Srinivasan<br />
Director. Naval Physical & Oceanographic Laboratory<br />
Naval Base, Cochin.<br />
8. Pr<strong>of</strong>. N. B. Nair<br />
Head <strong>of</strong> the Department <strong>of</strong> Aquatic Biology & Fisheries<br />
University <strong>of</strong> Kerala, Trivandrum·<br />
9. Dr. V. K. Iya<br />
Director. Isotope Group, Bhabha Atomic Research Centre<br />
Trombay-Bombay<br />
10. Dr. S. Z. Qasim<br />
Director, <strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Dona Paula, Goa<br />
11. Dr. V. V. R. Varadachari Member-Secretary<br />
Deputy Director, <strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Dona Paula, Goa<br />
12. Ex-Officio Members<br />
(i) Director-General, SIR or his nominee &<br />
(ii) Chairman. Coordination Council <strong>of</strong> Physical & Earth Sciences<br />
Group <strong>of</strong> Laboratories, CSIR.<br />
5.3 Executive Committee<br />
1. Dr. S. Z. Qasim<br />
Director, <strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Dona Paula, Goa.<br />
2. Dr. D. Srinivasan<br />
Director, Naval Physical & Oceanographic Laboratory<br />
Naval Base, Cochin.<br />
3. Pr<strong>of</strong>. N. B. Nair<br />
Head <strong>of</strong> the Department <strong>of</strong> Aquatic Biology & Fisheries<br />
University <strong>of</strong> Kerala, Trivandrum.<br />
4. Dr. A. K. Ganguly<br />
<strong>National</strong> Fellow in Environmental Sciences<br />
Bhabha Atomic Research Centre<br />
Trombay, Bombay.<br />
5. Dr. V. V. R. Varadachari<br />
Deputy Director &<br />
Head, Physical <strong>Oceanography</strong> Division<br />
<strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Dona Paula, Goa.<br />
6. Shri C. V. G. Reddy<br />
Head, Chemical <strong>Oceanography</strong> Division<br />
<strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Dona Paula, Goa-<br />
97
7. Dr. B. N. Desai "<br />
Scientist-in-Charge, Regional Centre <strong>of</strong><br />
NIO Bombay.<br />
8. Finance & Accounts Officer "<br />
<strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Dona Paula, Goa<br />
9. Administrative Officer Member-Secretary<br />
<strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Dona Paula, Goa<br />
10. Ex-Officio Members<br />
(i) Director-General, SIR cr his nominee &<br />
(ii) Chairman, Coordination Council <strong>of</strong> Physical & Earth Sciences<br />
Group <strong>of</strong> Laboratories, CSIR<br />
5.4 Finance & Building Committee<br />
1. Dr. V. V. R. Varadachari Chairman<br />
Deputy Director, <strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Dona Paula, Goa<br />
2. Dr. S. P. Deshpande Member<br />
Director, Environmental Planning & Design Consultancy Services<br />
Government <strong>of</strong> Goa, Daman & Diu<br />
Panaji, Goa.<br />
3. Shri H. N. Siddiquie<br />
Head, Geological <strong>Oceanography</strong> Division<br />
<strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Dona Paula, Goa.<br />
4. Shri R. S. Panesar<br />
Head, Engineering Division, CSIR<br />
New Delhi-<br />
5. Dr. B. N. Desai<br />
Scientist-in-Charge<br />
Regional Centre <strong>of</strong> <strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Bombay.<br />
6. Shri Lakhbir Singh<br />
Administrative Officer<br />
<strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Dona Paula, Goa-<br />
7. Shri A. Rajachandran „<br />
Finance & Accounts Officer<br />
<strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Dona Paula, Goa·<br />
8. Shri George Philip Convenor<br />
Civil Engineer,<br />
<strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Dona Paula, Goa<br />
98
5.5 R. V. Gaveshani Committee<br />
1. Dr. T. S. S. Rao<br />
2. Shri H. N. Siddiquie<br />
3. Dr. R. Sen Gupta<br />
4. Dr. A. B. Wagh<br />
5. Shri A. Rajachandran<br />
6. Shri S. P. Mittal<br />
7. Shri R. K. Nair<br />
5.6 Policy Planning Committee<br />
1. Director, NIO<br />
2. Head. Physical <strong>Oceanography</strong> Division<br />
3. Head, Chemical <strong>Oceanography</strong> Division<br />
4. Head, Geological <strong>Oceanography</strong> Division<br />
5. Head, Biological <strong>Oceanography</strong> Division<br />
6. Head, Ocean Engineering Division<br />
7. Head, Instrumentation Division<br />
8. Head, Planning & Data Division<br />
9. Scientist-in-Charge, Regional Centre, Cochin<br />
10. Scientist-in-Charge, Regional Centre, Bombay<br />
11. Scientist-in-Charge, Regional Centre, Waltair<br />
12. Administrative Officer<br />
13. Finance & Accounts Officer<br />
14. Section Officer<br />
15. Purchase Officer<br />
16. Stores Officer<br />
17. Civil Engineer<br />
18. Resident Medical Officer<br />
19. Library Incharge<br />
20. Executive Officer, R. V. Gaveshani<br />
21. Dr. R. Sen Gupta<br />
22. Dr. T. S. S. Rao<br />
5.7 Stores & Equipment Committee<br />
1. Shri H.N. Siddiquie<br />
2. Shri J. S. Sastry<br />
3. Dr. E. D'Sa.<br />
4. Dr. B. U. Nayak<br />
5. Shri C. V· G. Reddy<br />
6. Shri R. M. S. Bhargava<br />
7. Shri P. M. A. Bhattathiri<br />
8. Shri R. R. Nair<br />
9. Shri R. K. Nair<br />
10. Shri S. P. Mittal<br />
99<br />
Chairman<br />
Member<br />
Chairman<br />
Member<br />
Convenor<br />
Chairman<br />
Member<br />
Convenor
5.8 Grievance Committee<br />
1. Dr.V. V. R. Varadachari Chairman<br />
2. Dr. B. U. Nayak Member<br />
3. Shri Lakhbir Singh<br />
4. Shri V. Kesava Das<br />
5. Shri R. M. S. Bhargava Member-Secretary<br />
5.9 Staff Quarters/Hostel Allotment Committee<br />
1. Dr. V. V. R. Varadachari Chairman<br />
2. Dr. T. S. S. Rao Member<br />
3. Shri. H. N. Siddiquie<br />
4. Shri. Lakhbir Singh "<br />
5. Shri A. Rajachandran "<br />
6. Shri George Philip ,,<br />
5.10 Budget<br />
The budget <strong>of</strong> the <strong>Institute</strong> for the year <strong>1980</strong>-81 is as follows:<br />
(Rs- in lakhs)<br />
100
5.11 Scientific and Technical Staff<br />
The staff (upto a level <strong>of</strong> JSA/JTA)as on December 31, <strong>1980</strong>.<br />
Director Deputy Director<br />
Dr. S. Z. Qasim Dr. V. V. R. Varadachari<br />
A. Divisions at the Headquarters<br />
1. Physical <strong>Oceanography</strong> Division<br />
Head <strong>of</strong> the Division<br />
Scientists<br />
Dr.V. V. R. Varadachari<br />
Dr. J. S. Sastry<br />
Shri L.V.G. Rao<br />
Dr. C. S. Murty<br />
Dr. D. Panakala Rao<br />
Shri M. J. Varkey<br />
Shri P. K. Das<br />
Shri C. K. Gopinathan<br />
Shri V. Ramesh Babu<br />
Shri K. K. Varma (on deputation)<br />
Senior Scientific Assistants<br />
Shri V.esava Das<br />
Shri A. F. Anto<br />
Shri A. D. Gouveia<br />
Shri P. V. Sathe<br />
Shri Y. K. Somayajulu<br />
Shri D. V. Rama Raju<br />
Shri Johnson Samuel<br />
Shri R. J. Krishnamacharyulu<br />
Junior Scientific Assistants<br />
Shri V. S. N. Murty<br />
Shri M. S. Sarma<br />
Shri G. Venkata Reddy<br />
Shri A. A. Fernandes<br />
Junior Technical Assistant<br />
Shri G. Nampoothiri<br />
Junior Research Fellow<br />
Shri P. Vethamony<br />
2. Chemical <strong>Oceanography</strong> Division<br />
Head <strong>of</strong> the Division<br />
Scientists<br />
Shri C V. G. Reddy<br />
Dr. R. Sen Gupta<br />
Shri S. P. Anand<br />
Shri S. Y. S. Singbal<br />
Dr. S. Y. Kamat<br />
Dr. A. Rajendran<br />
Dr. C. G. Naik<br />
Shri S. N. De'Souza<br />
Mrs. Solimabi Wahidullah<br />
Senior Scientific Assistants<br />
Shri S. P. Fondekar<br />
Shri M. D. George<br />
Shri S.W.A. Naqvi<br />
Shri N. B. Bhosle<br />
Shri M. D. Rajagopal<br />
Shri R. S. Topgi<br />
Miss S. S. Naik<br />
Junior Scientific Assistants<br />
Mrs. C.D'Silva<br />
Shri K. Sawkar<br />
Shri P. K. Mittal<br />
Shri T. W. Kureishy<br />
Miss S. M. Sanzgiri<br />
Mrs. L. D'Souza<br />
Miss A. Braganca<br />
Junior Technical Assistants<br />
101<br />
Mrs. C. F. Dias<br />
Mrs. B. Das<br />
Mrs. T. Joseph
Junior Research Fellows<br />
Shri M. Dilip Kumar<br />
Miss F. D'Souza<br />
3. Geological <strong>Oceanography</strong> Division<br />
Head <strong>of</strong> the Division<br />
Shri H. N. Siddiquie<br />
Scientists<br />
Dr. M.G. Anantha Padmanabha Setty<br />
Shri P. S. N. Murty<br />
Shri R. R. Nair<br />
Shri Ch. Madhusudan Rao<br />
Shri D. Gopala Rao (on deputation<br />
to West Germany)<br />
Dr. M. Veerayya<br />
Shri G V. Rajamanickam<br />
Shri M. Manoharan (on leave)<br />
Shri R. M. Kidvvai<br />
Shri B. G. Wagle<br />
Shri M. V. S. N. Guptha<br />
Shri N. H. Hashimi<br />
Senior Scientific Assistants<br />
Shri F. Almeida (on deputation to<br />
Japan)<br />
Shri G. C. Bhattacharya<br />
Shri A. L. Paropkari<br />
Shri L. V. Subba Raju<br />
Shri K. H. Vora<br />
Shri A. R. Gujar<br />
Shri R. Nigam<br />
Dr. S. M. Karisiddaiah<br />
Shri A. Mascarenhas<br />
Shri M. V. Ramana<br />
Shri V. Subrahmanyam<br />
Dr. A. B. Valsangkar<br />
Junior Scientific Assistant<br />
Shri V. Purnachandra Rao<br />
Senior Technical Assistants<br />
Shri K. L. Kotnala<br />
Shri M. C Pathak<br />
Shri E.Dias<br />
Shri P. Marat he<br />
Junior Technical Assistants<br />
Shri S.K. Nanyasi<br />
Shri H. R. Raghavendra<br />
Junior Mechanical Assistant<br />
Shri A. V. Sonavane<br />
4. Biological <strong>Oceanography</strong> Division<br />
Head <strong>of</strong> the Division<br />
Dr. T. S. S. Rao<br />
Scientists<br />
Dr. A. H. Parulekar<br />
Shri V. P. Devassy<br />
Dr. A. G. Untawale<br />
Shri S. C. Goswami<br />
Dr. (Miss) Aditi Pant<br />
Dr. (Mrs.) Sumitra Royan<br />
Dr. D. Chandramohan<br />
Shri P. M. A. Bhattathiri<br />
Dr. (Miss) Loka Bharathi<br />
Shri R. A. Salvakumar<br />
Senior Scientific Assistants<br />
Shri C.T. Achuthankutty<br />
Shri S. N. Harkantra<br />
Dr. M. Madhupratap<br />
Shri Z. A. Ansari<br />
Shri S. R. Sreekumaran Nair<br />
Junior Scientific Assistants<br />
Mrs. L. Krishna Kumari<br />
Mrs. S. Achuthankutty<br />
Shri X.N. Verlencar<br />
Shri T. G. Jagtap<br />
Senior Technical Assistant<br />
Shri V. Subramanian<br />
Junior Technical Assistants<br />
Shri V.K.Dhargalkar<br />
Miss Maria R. Menezes<br />
Research Associates<br />
102<br />
Dr. (Mrs) Usha Goswami<br />
Dr. Joseph Royan<br />
Dr. A. K. Chatterjee
Senior Research Fellow<br />
Shri V. V. Agadi<br />
Junior Research Fellows<br />
Shri C.L. Rodrigues<br />
Shri S. Gouthaman<br />
5. Ocean Engineering Division<br />
Head <strong>of</strong> the Division<br />
Scientists<br />
Dr. B. U. Nayak<br />
Shri N. M. Anand<br />
Dr. A. K. Jain<br />
Shri S. G. Diwan<br />
Shri T. Balasubramanian<br />
Senior Scientific Assistant<br />
Shri B. A. Ramesh<br />
Junior Research Fellow<br />
Shri D. Sen Gupta<br />
6. Instrumentation Division<br />
Scientist-in- Charge<br />
Dr. E. Desa<br />
Scientists<br />
Shri M. R. Nayak<br />
Dr. E. S. Desa<br />
Shri R. G. Prabhu Desai<br />
Senior Scientific Assistants<br />
Mrs. V. B. Peshwe<br />
Shri H. Srikantan<br />
Senior Technical Assistants<br />
Shri A. Paneerselvam<br />
Shri Md. Wahidullah<br />
Shri V. M. Date<br />
Senior Mechanical Assistant<br />
Shri S.B. Tengali<br />
Junior Technical Assistants<br />
Shri S. Chellam<br />
Shri O. D'Souza<br />
Shri A. Joseph<br />
7. Planning & Data Division<br />
Scientist-in-Charge<br />
Shri R. M. S. Bhargava<br />
Statistical Officer<br />
Shri S. G. Dalal<br />
Scientists<br />
Dr. R. Mahadevan<br />
Shri J. S. Sarupria<br />
Shri Avinash Chandra<br />
Senior Scientific Assistants<br />
Dr. R. K. Sharma<br />
Shri P. V. S. S. R. Sarma<br />
Junior Scientific Assistants<br />
Shri S. R. Bhat (on study leave)<br />
Shri P. G. Patil<br />
Shri Arvind Ghosh<br />
Pro<strong>of</strong> Reader<br />
Shri S. P. Sharma<br />
Junior Technical Assistants<br />
Mrs. R. Thomas<br />
Shri Andrew Menezes<br />
8. Library<br />
Jr. Documentation Officer<br />
Shri M. P. Tapaswi<br />
Senior Librarian<br />
Mrs. S. H. Oka<br />
9. R.V. Gaveshani<br />
Advisor<br />
Commodore I. K. Puri<br />
(Chief Hydrographer, Indian Navy-<br />
Retd.)<br />
Executive Officer<br />
Dr. A. B. Wagh<br />
B. Regional Centres<br />
1. Regional Centre, Cochin<br />
Scientist-in-Charge<br />
Dr. M. Krishnankutty<br />
103
Scientists<br />
Shri V· S. Rama Raju<br />
Dr. R. V. Unnithan<br />
Dr. V. N. Sankaranarayanan<br />
Dr. P. Sivadas<br />
Shri P. Udaya Varma<br />
Shri U. K. Gopalan<br />
Shri P. Gopala Menon<br />
Shri K. J. Peter<br />
Shri B. M. Panikkar<br />
Dr. (Mrs.) M. Saraswathy<br />
Shri P. N. Aravindakshan<br />
Dr. George Peter<br />
Shri V. T. Paulinose<br />
Shri T. Balachandran<br />
Mrs. C. B. Lalilhambika Devi<br />
Shri K. Kameswara Rao<br />
Shri P. S. Gore<br />
Shri T. C. Gopalakrishnan<br />
Dr. (Mrs) V. Santhakumari<br />
Shri K. K. C. Nair<br />
Senior Scientific Assistants<br />
Mrs. P. P. Meenakshi Kunjamma<br />
Mrs. Rosamma Stephen<br />
Shri P. Haridas<br />
Mrs. U. P. Saramma<br />
Junior Scientific Assistant<br />
Shri T. Balasubramanian<br />
Senior Technical Assistant<br />
Shri P. Venugopal<br />
Junior Technical Assistants<br />
Shri Abraham Pylee<br />
Shri B. Narayanan<br />
Mrs. K. Sarala Devi<br />
Shri O. Raveendran<br />
2. Regional Centre, Bombay<br />
Scientist-in-Charge<br />
Dr. B. N. Desai<br />
Scientists<br />
Dr. M. D. Zingde<br />
Shri S. A. H. Abidi<br />
Shri G. Narayana Swamy<br />
Dr. (Mrs) Vijayalakshmi R. Nair<br />
Dr. K. Govindan<br />
Senior Scientific Assistants<br />
Shri M. M. Sabnis<br />
Shri R. V. N. Sarma<br />
Shri S. N. Gajbhiye<br />
Junior Scientific Assistants<br />
Shri A. Suryanarayana<br />
Shri C. V. Vijayakumar<br />
Shri A.Lalitananda Prasad<br />
Junior Technical Assistants<br />
Shri P. V. Narvekar<br />
Shri S. A. Marathe<br />
Shri S. K. Bhakta<br />
Junior Research Fellow<br />
Shri P. K. Varshney<br />
3. Regional Centre, Waltair<br />
Scientist-in-Charge<br />
Scientist<br />
Shri T. C. S. Rao<br />
Shri K. S. R. Murthy<br />
Senior Scientific Assistants<br />
Shri P. Chandra Mohan<br />
Shri K. Subrahmanyam<br />
Shri M.M. Malleswara Rao<br />
Dr. V. V. Sarma<br />
Junior Scientific Assistants<br />
Shri T. V. Narasimha Rao<br />
Shri B. Prabhakara Rao<br />
Shri P. Vijayakumar Rathod<br />
Shri K. Mohan Rao<br />
Junior Technical Assistants<br />
Shri S. Kannan<br />
Shri M.K.Prema Kumar<br />
Senior Research Fellow<br />
Dr. T. Bose Babu<br />
Junior Research Fellow<br />
Shri G. R. K. Raju<br />
104
6<br />
Visitors<br />
Visit <strong>of</strong> the Vice-President <strong>of</strong> CSIR<br />
The Vice-President <strong>of</strong> CSIR. Pr<strong>of</strong>. S. Nurul Hasan visited the <strong>Institute</strong> from<br />
May 14-16. <strong>1980</strong>. This was Pr<strong>of</strong>. Hasan's first visit to ΝIO after taking over as<br />
the Vice-President <strong>of</strong> CSIR. He was taken to different laboratories by the Director<br />
and was shown and explained the research activities <strong>of</strong> the various divisions. He<br />
showed a keen interest in the research work in all fields <strong>of</strong> <strong>Oceanography</strong> and held<br />
meetings with the scientists for discussing their problems. He also visited the research<br />
vessel Gaveshani where he saw the diffrent laboratories, the research equipment and<br />
the living and working facilities on board.<br />
During his brief stay at the <strong>Institute</strong>, he inaugurated, the seminar on "Protection<br />
and control <strong>of</strong> coastal erosion in India" organised by the <strong>Institute</strong> from 16 to l7 May<br />
<strong>1980</strong>. In his inaugural address he emphasized the importance <strong>of</strong> protecting the vast<br />
coastline <strong>of</strong> India as many industrial complexes and population centres are located<br />
along the coast. He commended the work done and steps taken by NIO in this respect.<br />
Pr<strong>of</strong>. Nurul Hasan in the Computer Centre.<br />
105
Visit <strong>of</strong> Chief Minister <strong>of</strong> Goa, Daman & Diu<br />
Honourable Chief Minister <strong>of</strong> Goa, Daman & Diu, Shri Pratapsingh Rane visted<br />
the <strong>Institute</strong> thrice during the year. He visited the <strong>Institute</strong> for the first time<br />
after taking over as the Chief Minister on 3rd March, <strong>1980</strong> alongwith the Speaker <strong>of</strong><br />
Goa Assembly Shri F. Machado and the Agriculture Minister Shri J. Aguiar. Director,<br />
NIO took them around the <strong>Institute</strong> explaining the various research and development<br />
activities. The Chief Minister and his colleagues appreciated the work done by NIO<br />
for the Union Territory <strong>of</strong> Goa in various fields <strong>of</strong> resources survey, pollution control,<br />
pipeline surveys, coastal development and sea farming. They also visited the research<br />
vessel Gaveshani <strong>of</strong> the <strong>Institute</strong>.<br />
For the second time the Chief Minister visited the <strong>Institute</strong> on 16th May, <strong>1980</strong><br />
when he was invited to be the Chief Guest at the inauguration <strong>of</strong> the seminar on<br />
"Protection and control <strong>of</strong> coastal erosion in India."<br />
The Honourable Chief Minister once again visited to inaugurate the <strong>National</strong><br />
workshop on "Energy from the Sea"' on 15th December, <strong>1980</strong>.<br />
A number <strong>of</strong> other VIPs, dignitaries, scientists and pr<strong>of</strong>essors visited the <strong>Institute</strong><br />
and its Regional Centres during the year under report. Some <strong>of</strong> them are:<br />
Pr<strong>of</strong>. D. J. Crisp, Marine Science Laboratory, Anglesey, U.K.<br />
Dr. Sethu Raman, Atmospheric Science Division, Department <strong>of</strong> Energy &<br />
Environment, Brookhaven <strong>National</strong> Laboratory, New York, USA-<br />
Dr. Noel Pierre Yues, University <strong>of</strong> Paris, France.<br />
Shri S. P. Srivastava, Bedford <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong>, Dartmouth, Canada<br />
Pr<strong>of</strong>. O. Siddiqi, Tata <strong>Institute</strong> <strong>of</strong> Fundamental Research, Bombay.<br />
Dr. J. Szilard, Loughborough University <strong>of</strong> Technology, U. K.<br />
Dr. K.G.Vohra, Bhabha Atomic Research Centre, Bombay.<br />
Pr<strong>of</strong>. P. Bruun, Norwegian <strong>Institute</strong> <strong>of</strong> Technology, Trondheim, Norway.<br />
Pr<strong>of</strong>. O. G. Houmb, Norwegian <strong>Institute</strong> <strong>of</strong> Technology, Trondheim, Norway<br />
Dr. Morterza Amini, Head, Engineering Geology Division, G.M.S.I., Tehran, Iran-<br />
Pr<strong>of</strong>. M. L. Sahare, Chairman, Union Public Service Commission, New Delhi-<br />
Pr<strong>of</strong>. E. C. Lafond, Secretary Genera] <strong>of</strong> the International Association for Physical<br />
Sciences <strong>of</strong> the Ocean, USA.<br />
Dr. S. M. Haq, Assistant Secretary, Intergovernmental Oceanographic Commsi-<br />
sion, UNESCO, Paris.<br />
Pr<strong>of</strong>. A. Ovchinnikov, Vice President, USSR Academy <strong>of</strong> Sciences, leading a<br />
Russian delegation consisting <strong>of</strong> Pr<strong>of</strong>. S. E. Severin, Dr. E. V. Grislin and Dr. T. V.<br />
Marchanko.<br />
Dr. W.D. Forrester, Canadian Hydrographic Service, Canada.<br />
Dr. P. K. Bhattacharya, Indian <strong>Institute</strong> <strong>of</strong> Science, Bangalore.<br />
Dr. Maurice Cross, Fort Bovisand Underwater Centre. U. Κ.<br />
106
Dr. R.S. Mehta. Chairman, Gujarat Water Pollution Control Board, Ahmedabad.<br />
Dr. Enrico Cantore, Director, World <strong>Institute</strong> for Scientific Humanism. New<br />
York, USA.<br />
Dr. B. V. Srikantan, Director. Tata <strong>Institute</strong> <strong>of</strong> Fundamental Research Bombay.<br />
Dr. A. K. Mukharjee, Deputy Director-General. Meteorology (Forecasting) India<br />
Meteorological Department. Poona.<br />
Mr. P.G. Dikson, Director MAREX, England, UK.<br />
Mr. Martin Springett, Senior Project Engineer, Marine Exploration Ltd.,<br />
England, UK.<br />
Dr. Bryan Johns, Department <strong>of</strong> Meteorology, University <strong>of</strong> Reading, Reading, UK.<br />
Mr. Mohd. Yusuf Abdul Rahim, Chief, Anti-pollution Department, Government<br />
<strong>of</strong> Kuwait, Kuwait<br />
Mr. Makan Berggren. Counsillor. Swedish Embassy, New Delhi.<br />
Regional Centre, Cochin<br />
Dr. A. M. Jayasekara, Asst. Director, Inland Fishery Division, Ministry <strong>of</strong><br />
Fisheries, Colombo, Sri Lanka.<br />
Dr. P. K. Rohatgi, Director, Regional Research Laboratory, Trivandrum.<br />
Dr. Klaus Deninger, Naval Architect, Horshalm. Denmark<br />
Dr. Vagn Hansen, DFH, Denmark<br />
Regional Centre, Bombay<br />
Dr. S.M.Haq, Asst. Secretary, IOC, UNESCO, Paris.<br />
Admiral J. Cursetji, PVSM, Retired Chief <strong>of</strong> Naval Staff, Indian Navy.<br />
Mr. D. Edwards, Consulting Engineer, Belfours Consulting Engineers, Ltd., UK.<br />
Dr. Roger Perry, Public Health Engineer, Imperial College. London.<br />
Pr<strong>of</strong>. D. J. Crisp, Marine Science Laboratory, Anglesey, UK.<br />
Regional Centre, Waltair<br />
Pr<strong>of</strong>. S. Nurul Hasan, Vice-President, CSIR.<br />
Shri M. R. Appa Rao, Vice-Chancellor, Andhra University, Waltair.<br />
Shri S. Alwardas, MLA, Member <strong>of</strong> State for Municipal Administrator and<br />
Urban Development, Andhra Pradesh.<br />
Dr. S. Balakrishna, Acting Director, <strong>National</strong> Geophysical Research <strong>Institute</strong>,<br />
Hyderabad.<br />
107
7<br />
Colloquia<br />
Speaker Subject Date<br />
1 Dr. S. Sethu Raman<br />
Brookhaven <strong>National</strong> Laboratory<br />
New York<br />
2 Pr<strong>of</strong>. D. J. Crisp, F.R.S.<br />
University <strong>of</strong> Wales, U.K.<br />
3 Dr. Noel Pierre Yues<br />
Paris University, Paris<br />
4 Shri S. P. Srivastava<br />
Bedford <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Dartmouth, Canada<br />
5 Pr<strong>of</strong>. O. Siddiqi<br />
Tata <strong>Institute</strong> <strong>of</strong> Fundamental<br />
Research. Bombay<br />
6 Dr. J. Szilard<br />
Loughborough University<br />
<strong>of</strong> Technology, U. K.<br />
7 Dr. K. G. Vohra<br />
Bhabha Atomic Research Centre<br />
Bombay<br />
8 Dr. Sharad Vaidya<br />
Goa Cancer Society<br />
Goa<br />
9 Dr. Allan W. H. Be<br />
Columbia University<br />
New York, USA<br />
10 Pr<strong>of</strong>. V. K. Gaur,<br />
University <strong>of</strong> Roorkee<br />
Roorkee<br />
108<br />
Coastal studies at 21-2-80<br />
Brookhaven <strong>National</strong><br />
Laboratory<br />
Extending conservation 21-2-80<br />
seawards<br />
Biology <strong>of</strong> prawns 22-2-80<br />
Continental margin <strong>of</strong> 7-3-80<br />
eastern Canada-structure<br />
and development<br />
Genetics <strong>of</strong> chemo-sensory 10-3-80<br />
mechanism<br />
Ultrasonic lenses 15-3-80<br />
Primeval hydrosphere 25-3-80<br />
and evaluation <strong>of</strong> life,<br />
atmosphere and ozone layer<br />
Human resource development<br />
for fight against cancer 2-4-80<br />
Planktonic foraminifera 8-9-80<br />
—its biology, ecology<br />
and paleoclimatology<br />
Multi-dimensional inter- 19-9-80<br />
pretation <strong>of</strong> geodata
11 Dr. Eugene C. Lafond<br />
International Association<br />
for the Physical Sciences<br />
<strong>of</strong> the Ocean, USA<br />
12 Dr. W. D. Forrester<br />
Canadian Hydrographic Service<br />
Canada<br />
13 Dr. P. K. Bhattacharya<br />
Indian <strong>Institute</strong> <strong>of</strong> Science<br />
Bangalore<br />
14 Dr. Maurice Cross<br />
Fort Bovis and Underwater<br />
Centre, U. K.<br />
15 Dr. R. S. Mehta<br />
Gujarat Water Pollution Board<br />
Gujarat<br />
16 Dr. Enrico Cantore<br />
World <strong>Institute</strong> for<br />
Scientific Humanism.<br />
New York. USA<br />
109<br />
Studies from an oceano- 27-10-80<br />
graphic tower<br />
Validity <strong>of</strong> the geostrophic 18-11-80<br />
approximation in coastal<br />
waters<br />
Directions <strong>of</strong> research in 18-11-80<br />
the eighties in marine<br />
microbiology and microbial<br />
chemistry<br />
Underwater photography<br />
and diving 24-11-80<br />
Industrial development with<br />
special reference to Gujarat 10-12-80<br />
environmental impact on<br />
industrialization<br />
(i) Science. Technology and 23-12-80<br />
Society - Religious and<br />
Ethical Problems<br />
(ii) Science and Man 27-12-80
8<br />
Awards, honours and membership <strong>of</strong><br />
various committees<br />
Dr. S. Z. Qasim acted as<br />
— Chairman, Working Committee for the Training, Education and Mutual<br />
Assistance (TEMA) in the Marine Sciences <strong>of</strong> International Oceanographic<br />
Commission, UNESCO.<br />
— <strong>National</strong> Coordinator for the project 'Development <strong>of</strong> Inland Fisheries under<br />
the Rural Technology Programme' <strong>of</strong> the Commonwealth Science Council,<br />
Commonwealth Secretariat, London.<br />
— Member, Indian <strong>National</strong> Commission for Cooperation with UNESCO.<br />
— Member, <strong>National</strong> Commission on Environmental Planning and Coordination<br />
<strong>of</strong> Department <strong>of</strong> Environment.<br />
— Adviser, Marine Ecology Progress Series <strong>of</strong> the Biologische Anstalt Helgoland-Hamburg.<br />
— Member, Council <strong>of</strong> Scientific and Industrial Research (CSIR) Society.<br />
— Member, Governing Body <strong>of</strong> CSIR.<br />
— Chairman, Coordination Council <strong>of</strong> Physical and Earth Sciences Group consisting<br />
<strong>of</strong> 5 laboratories <strong>of</strong> CSIR.<br />
Dr. V. V. R. Varadachari was elected as Fellow <strong>of</strong> the Indian <strong>National</strong> Science<br />
Academy (F.N.A) and continued to serve as<br />
— Member-Secretary <strong>of</strong> the Indian <strong>National</strong> Committee for SCOR (Scientific<br />
Committee on Ocean Research)<br />
— Member, Board for Ocean Engineering Centre. I.I.T. Madras.<br />
— Member, Board <strong>of</strong> Studies in Physical <strong>Oceanography</strong>, University <strong>of</strong> Cochin,<br />
Cochin.<br />
— Member, Marine Sciences Advisory Committee for Centre for Earth Science<br />
Studies. Trivandrum.<br />
Shri H. N. Siddiquie continued to serve as<br />
— Member <strong>of</strong> Board <strong>of</strong> Studies in Marine Sciences, University <strong>of</strong> Cochin, Cochin.<br />
— Member, Council <strong>of</strong> Association <strong>of</strong> Exploration Geophysicists <strong>of</strong> India.<br />
— <strong>National</strong> Correspondent for the Commission on Marine Geology. International<br />
Union <strong>of</strong> Geological Sciences-<br />
Dr. J. S. Sastry<br />
— has been nominated as the member <strong>of</strong> the Joint IOC/WMO Working Committee<br />
for IGOSS.<br />
— acted as Member <strong>of</strong> the Indian Ocean Panel, SCOR Working Group 47.<br />
— acted as Member <strong>of</strong> the ISI - Thermometers Sub-Committee, CDC-33.2.<br />
Dr. B. U. Nayak was enrolled as a member <strong>of</strong> the Indian Geotechnical Society <strong>of</strong><br />
India.<br />
110
Dr. B. A..Desai was recognised as a guide for M.Sc. and Ph.D. degrees in Applied<br />
Biology by the University <strong>of</strong> Bombay and continued to serve as<br />
— Member, Science and Technology Advisory Committee. Government <strong>of</strong><br />
Maharashtra.<br />
— Member, Advisory Committee. Maharashtra Prevention ot" Water Pollution<br />
Board .<br />
— Member, Committee on Marine Disposals. Indian Standards Institution.<br />
— Member, Board <strong>of</strong> Studies in Environmental Biology, University <strong>of</strong> Jodhpur,<br />
Jodhpur.<br />
— Member, Board <strong>of</strong> Studies in Environmental Sciences, University <strong>of</strong> Bombay,<br />
Bombay.<br />
— Member, Study Group for Fisheries in the Bombay Metropolitan Region.<br />
Dr. R. Sen Gupta has been<br />
— recognised as a guide for Ph.D. in Chemistry by Poona University.<br />
— nominated as a Member <strong>of</strong> the Advisory Committee on Dispersion <strong>of</strong> Substances<br />
in the Oceans <strong>of</strong> International Association for the Physical Sciences <strong>of</strong><br />
the Oceans.<br />
Dr. M. Krishnankutty acted as Member, Board <strong>of</strong> Examiners, University <strong>of</strong> Cochin, Cochin.<br />
Shri T. C. S. Rao served as<br />
— Member, Association Exploration Geophysicists.<br />
— Member, Acoustical Society <strong>of</strong> India<br />
Shri R. M. S. Bhargava<br />
— acted as Indian <strong>National</strong> Coordinator for International Oceanographic Data<br />
Exchange (IODE) <strong>of</strong> IOC.<br />
— was selected as Member <strong>of</strong> Group <strong>of</strong> Experts on Format Development <strong>of</strong><br />
International Oceanographic Data Exchange <strong>of</strong> IOC.<br />
Shri L. V. G. Rao acted as Alternate Member <strong>of</strong> the ISI-Thermometers Sub-Committee,<br />
CDC-33.2.<br />
Dr. R. V. Unnithan acted as<br />
— Member. Senate <strong>of</strong> the University <strong>of</strong> Cochin.<br />
— Member. Sasthra Sahitya Patishad, Ernakulam.<br />
Dr. A. H. Parulekar acted as<br />
— Member, Konkan Krishi Vidyapeeth & ICAR Committee on Education, Research<br />
and Development in Fisheries.<br />
— Member, Board <strong>of</strong> Examiners (Fisheries Biology),. Central <strong>Institute</strong> <strong>of</strong> Fisheries<br />
Education (ICAR), Bombay.<br />
— Member, Board <strong>of</strong> Examiners (Marine Biology), Karnataka University,<br />
Dharvar.<br />
— Member, Regional Advisory Committee on Exploratory Fishery Project (Goa<br />
base), Ministry <strong>of</strong> Agriculture, Government <strong>of</strong> India.<br />
— Expert Member, Marine Fisheries Committee (Legislative) for drafting the Goa<br />
Fisheries Bill, Government <strong>of</strong> Goa, Daman & Diu.<br />
Dr. A.G. Untawale acted as<br />
— Member, Board <strong>of</strong> Studies in Botany, Nagpur University, Nagpur.<br />
111
— Member, Biosphere, Forest and Wild-life Theme Committee, Government <strong>of</strong><br />
Gujarat.<br />
— Member, <strong>National</strong> Mangrove Committee <strong>of</strong> DST, Government <strong>of</strong> India, New<br />
Delhi.<br />
Shri S. A. H. Abidi was awarded Certificate <strong>of</strong> Merit (Tampatra) by Nav Par Nal<br />
(A Hindi Academy). Port Blair and acted as<br />
— Member, Committee <strong>of</strong> MPEDA for International Fair to be held in 1981 at<br />
Madras.<br />
— Member, Regional Committee No. ΠΙ—Humid Eastern Zone Himalayan region<br />
and Bay <strong>of</strong> Bengal Islands <strong>of</strong> the ICAR <strong>1980</strong>.<br />
— Member, State Level Environment Committee <strong>of</strong> Andaman & Nicobar Island.<br />
Shri V. K. Gopalan continued to act as<br />
— Member, Board <strong>of</strong> Studies in Environmental Studies. University <strong>of</strong> Cochin<br />
and Member, Consultative Committee for the establishment <strong>of</strong> a School <strong>of</strong><br />
Biological Sciences <strong>of</strong> the same University.<br />
— Member, Executive Council, Marine Biological Association <strong>of</strong> India.<br />
— Member, Kerala Sasthra Sahitya Parishad.<br />
— Member, Cochin Chapter <strong>of</strong> the Friends <strong>of</strong> Trees.<br />
— Secretary, Cochin Science Association.<br />
Dr. (Mrs) Vijayalakshmi R. Nair has been recognised as a guide for Ph.D. in Applied<br />
Biology by the University <strong>of</strong> Bombay, Bombay.<br />
Dr. K. Govindan has been recognised as a guide for Ph.D. in Applied Biology by the<br />
University <strong>of</strong> Bombay, Bombay<br />
Shri M. V. S. N. Guptha has served as a Member. International Nannoplankton<br />
Association, the Netherlands for the year <strong>1980</strong>.<br />
Shri G. C. Bhattacharya has been elected as Member, Association <strong>of</strong> Exploration<br />
Geophysicists <strong>of</strong> India.<br />
Shri S. M. Karisiddaiah<br />
— was awarded Ph.D. degree by the Karnataka University, Dharwar for his<br />
thesis "Geology <strong>of</strong> the area around Bellary, Karnataka, India"<br />
— has been elected as a Fellow <strong>of</strong> Geological Society <strong>of</strong> India<br />
Shri X. N. Verlencar was awarded a cash prize for his popular article in the "Water<br />
Chemicals Forum" by Glaxo Laboratories (India) Ltd., Bombay.<br />
Shri P. V. Narvekar was awarded M.Sc. degree in Inorganic Chemistry by the<br />
University <strong>of</strong> Bombay for his thesis entitled "Study <strong>of</strong> boron in marine<br />
environment with special reference to boron-chlorinity ratio".<br />
Miss K. Radha Krishna was awarded M. A. degree in Philosophy by Andhra<br />
University.<br />
Shri Jiyalal Ram was awarded B.Sc. degree in Botany by University <strong>of</strong> Bombay,<br />
Bombay.<br />
112
9<br />
Deputations<br />
Dr. S. Z. Qasim was deputed to<br />
— Argentina to chair the Third Session <strong>of</strong> the Working Committee for the Training,<br />
Education and Mutual Assistance in the Marine Sciences <strong>of</strong> IOC/UNE-<br />
SCO at Buenos Aires.<br />
— Sri Lanka to participate in the Planning Meeting <strong>of</strong> the project "Development<br />
<strong>of</strong> Inland Fisheries" under the Rural Technology Programme <strong>of</strong> the<br />
Commonwealth Science, London at Colombo.<br />
Dr. V. V. R. Varadachari on being nominated by INSA as India's delegate, was<br />
deputed to attend an International Conference on "<strong>Oceanography</strong> from<br />
Space" organised by SCOR/COSPAR/IUCRAM at Venice, Italy from 26-30<br />
May, <strong>1980</strong>.<br />
Dr. T. S. S. Rao was deputed to West Germany from September 20 to October 8,<br />
to participate in the 15th European Marine Biology Symposium at Kiel.<br />
Sliri C. V. G. Reddy was deputed to USA under the 'CSIR-NSF Exchange <strong>of</strong><br />
Scientists' programme from 13th October to 22nd November to study the<br />
latest developments in the field <strong>of</strong> chemistry <strong>of</strong> marine natural products.<br />
Shri R. M. S. Bhargava was deputed to<br />
— USA to participate in (i) the First Meeting <strong>of</strong> Group Experts on Format<br />
Development and (ii) Intersessional Consultations on International Oceanographic<br />
Data Exchange (IODE) held at Washington DC from September 8 to 17<br />
<strong>1980</strong>.<br />
— attend a workshop in INFOTERRA organised by the Department <strong>of</strong> Science<br />
& Technology and UNEP at New Delhi from July 14-24, <strong>1980</strong>.<br />
Dr. A. G. Untawale was deputed to Malaysia to attend the International Symposium<br />
on 'Mangroves Environmental Research' organized by UNESCO at University<br />
<strong>of</strong> Malaysia Kaula-Lampur from 24 to 30 August, <strong>1980</strong> and presented a<br />
paper "Present status <strong>of</strong> the Mangroves along the west coast <strong>of</strong> India".<br />
Dr. J. S. Sasitry was deputed to UK to participate in the Indian Ocean Panel<br />
meeting <strong>of</strong> SCOR Workshop Group 47 at the <strong>Institute</strong> <strong>of</strong> Oceanographic<br />
Sciences, UK during 25 to 26 June, <strong>1980</strong>.<br />
Dr. C. S. Murty was deputed to Triesty, Italy for three months (September to<br />
November, <strong>1980</strong>) to participate in a course on "Physics <strong>of</strong> flow in the oceans,<br />
atmosphere and deserts" at Centre <strong>of</strong> Theoretical Physics, Triesty.<br />
Shri A.Rajachandran and Shri S.G. Dalal were deputed to attend the workshop on<br />
'Financial Management" organized by CSIR at New Delhi from July 3 to 6, <strong>1980</strong>.<br />
Dr. A.K. Jain, Shri S.G. Diwan. Shri P. Chandramohan, Shri T. Balasubramanian,<br />
Shri M. J. Varkey and Shri G. Narayanaswamy were deputed to Norway for a<br />
113
period <strong>of</strong> six months (January to June <strong>1980</strong>) under NORAD Assistance<br />
Programme to attend a specially designed six months course in Applied<br />
<strong>Oceanography</strong> and Ocean Engineering at Norwegian <strong>Institute</strong> <strong>of</strong> Technology,<br />
Trondheim, Norway.<br />
Shri S. P. Fondekar was deputed to UK for six months (January to June <strong>1980</strong>) to<br />
attend Diploma course in Marine Pollution Chemistry at the Department <strong>of</strong><br />
<strong>Oceanography</strong>, University <strong>of</strong> Liverpool.<br />
Dr. R. K. Sharma was deputed to Japan<br />
— to attend "International Training Course in Data Dissemination" organised<br />
by UNESCO/CODATA/Japan CODATA at University <strong>of</strong> Library & Information<br />
Science, Tsukuba, Japan from 1 to 4 October, <strong>1980</strong>.<br />
— to participate in the 7th International CODATA Conference at KYOTO<br />
organized by ICSU/CODATA/Japan CODATA/UNESCO from 7 to 11 October,<br />
<strong>1980</strong>.<br />
Shri K. H. Vora and Shri E.Dias were deputed to Norway for training under the<br />
NORAD Assistance Programme for training in marine geology and geological/<br />
geophysical instruments respectively.<br />
Shri Y. K. Somayajulu and Shri B. Prabhakar Rao were deputed to attend an "Intensive<br />
Course on Sound Transmission in Coastal Seas" conducted at the Indian<br />
<strong>Institute</strong> <strong>of</strong> Science, Bangalore in June <strong>1980</strong>.<br />
114
10<br />
Meetings, exhibitions, seminars, symposia and<br />
special lectures<br />
Dr. S. Z. Qusim<br />
— delivered a key-note address to the participants <strong>of</strong> the Small Harbour Engineering<br />
Course on January 12, <strong>1980</strong> at IIT, Bombay.<br />
— participated in the planning meeting <strong>of</strong> the project "Development <strong>of</strong> Inland<br />
Fisheries under the Rural Technology Programme" <strong>of</strong> the Commonwealth<br />
Science Council held in Colombo (Sri Lanka) from 3 to 5 June, <strong>1980</strong> and presented<br />
the country report from India which dealt with the state <strong>of</strong> art <strong>of</strong><br />
Inland Fisheries and the prospects for the development <strong>of</strong> inland fishery resources<br />
<strong>of</strong> the country.<br />
— participated and chaired a session in the International Symposium on Management<br />
<strong>of</strong> Environment at BARC, Bombay.<br />
Shri H. N. Siddiquie delivered lectures on "Status <strong>of</strong> Marine Mineral Exploration in<br />
India" and "Exploration for Offshore Mineral Deposits" at Ocean Engineering<br />
Centre <strong>of</strong> ΙIT, Madras in June, <strong>1980</strong>.<br />
Shri H. N. Siddiquie, Shri G. C. Bhattacharya, Dr. S. M. Karisiddaiah, Shri M. V<br />
Ramana and Shri V. Subrahmanyam participated and presented papers in<br />
the Sixth Annual Convention <strong>of</strong> the Association <strong>of</strong> Exploration Geophysicists<br />
<strong>of</strong> India held at Bangalore from 23 to 25 October, <strong>1980</strong>.<br />
Dr. B. U. Nayak delivered<br />
— five lectures during the ISTE Winter School on "Design and Construction<br />
<strong>of</strong> Offshore Structures" at Engineering College, Farmagudi, Goa.<br />
— three lectures for the Small Harbour Engineering Course conducted at IIT,<br />
Bombay from January 2 to 12, <strong>1980</strong>.<br />
Dr.B. N. Desai participated, in the<br />
— International Symposium on Management <strong>of</strong> Environment at BARC,<br />
Bombay.<br />
— Workshop on Reservoir Fisheries for Rural Development at Central <strong>Institute</strong><br />
<strong>of</strong> Fisherise Education, ICAR, Bombay.<br />
— Symposium on Coastal Intakes and Outfalls organized at Engineers India Ltd.,<br />
New Delhi.<br />
— delivered lectures at the University <strong>of</strong> Jodhpur for postgraduate students in<br />
Environmental Biology.<br />
Dr. B. N. Desai, Dr. M. D. Zingde, Shri S. A. H. Abidi, Shri G. Narayana Swamy<br />
Dr. (Mrs) Vijayalakshmi R. Nair, Shri S. N. Gajbhiye and Shri P. K. Varshney<br />
participated in a Television Programme on the "Pollution <strong>of</strong> Coastal Waters<br />
<strong>of</strong> Bombay"·<br />
115
Dr. R. Sen Gupta participated and delivered talks<br />
— at the 3rd Workshop on Marine Pollution Monitoring, New Delhi from 11 to<br />
15 February, <strong>1980</strong> organised by IGOSS <strong>of</strong> IOC as a member <strong>of</strong> Indian<br />
delegation.<br />
— at the <strong>National</strong> Seminar on Environmental Education, Bangalore from 13 to<br />
17 June, <strong>1980</strong> organised by Indian Environmental Society.<br />
— at the Seminar on Environmental Pollution in Madras Metropolitan Area,<br />
Madras from 24 to 25 November, <strong>1980</strong> organised by Max Muller Bhawan,<br />
Madras, as an invited speaker.<br />
— at the <strong>National</strong> Convention <strong>of</strong> Chemists, Bombay from 9 to 14 December. <strong>1980</strong><br />
organised by Association <strong>of</strong> Chemists, India as an invited speaker.<br />
Dr. M. G. Anantha Padmanabha Setty<br />
— delivered lecture at Rotary Club, Panaji on the topic "Ocean Wealth" in<br />
October, <strong>1980</strong>.<br />
— delivered lectures on Marine Micropaleontology at the Department <strong>of</strong> Marine<br />
Geology, Cochin University from 27July to 6 August, <strong>1980</strong>.<br />
— attended and presented a paper in Symposium on "Three Decades <strong>of</strong> Developments<br />
in Paleontology and Stratigraphy in India' at Hyderabad from 10 to<br />
12 December, <strong>1980</strong>.<br />
— attended Third Indian Geological Congress held at Poona from 24 to 31<br />
December, <strong>1980</strong>.<br />
Shri T. C. S. Rao presented a paper entitled "Gravity Low in Bay <strong>of</strong> Bengal" at<br />
Sixth Annual Convention <strong>of</strong> the Association <strong>of</strong> Exploration Geophysicists<br />
and Seminar on Exploration Geophysics organized by Centre <strong>of</strong> Exploration<br />
Geophysics at Osmania University, Hyderabad.<br />
Shri R. R. Nair delivered a series <strong>of</strong> lectures in September, <strong>1980</strong> at the Centre <strong>of</strong><br />
Earth Science Studies, Trivandrum.<br />
Shri S. P. Anand participated in the "All India Symposium and Exhibition on Solar<br />
Energy" held at Osmania University, Hyderabad from 22 to 23 March, <strong>1980</strong>.<br />
shri L. V. Gangadhara Rao attended the Seminar on Bhaskara held on 27 June, <strong>1980</strong><br />
at ISRO Satellite Centre, Bangalore.<br />
Shri U. K. Gopalan delivered a series <strong>of</strong> lectures on diverse aspects <strong>of</strong> Marine Environment<br />
at various colleges in Kerala.<br />
Dr. R. V. Unnithan<br />
— delivered lecture on ''Cochin University—Today End Tomorrow"at Cochin.<br />
— participated in the seminar on "Training for Rural Development in Kerala" held<br />
at the University <strong>of</strong> Cochin, Cochin.<br />
Dr. A. H. Parulekar presented two background/experience papers in "Workshop on<br />
Mussel Farming" held at Madras from 25 to 27 September, <strong>1980</strong> under the<br />
UNEP/ICAR Centre <strong>of</strong> Advanced Studies in Mariculture.<br />
Dr. (Mrs.) Sumitra Royan and Mrs. L. Krishna Kumari presented a paper on "Food<br />
conversion efficiency in the shrimp, M. monoceros fed on decomposed mangrove<br />
leaves" at International Symposium on Coastal Aquaculture held at<br />
Cochin from 12-18 January, <strong>1980</strong>.<br />
116
Dr. A. G. Untawale and Mrs. Sayeeda Wafar attended the International Wetlands<br />
Conference at New Delhi from 10 to 17 September, <strong>1980</strong> and Dr. Untawale<br />
presented a paper on 'Application <strong>of</strong> remote sensing technique in the studies<br />
<strong>of</strong> distribution <strong>of</strong> mangroves in Goa'.<br />
Dr. J. P. Royan presented a paper on "Importance <strong>of</strong> Artemia salina as food in shrimp<br />
culture' at the Symposium on Coastal Aquaculture held at Cochin during<br />
12 and 18 January, <strong>1980</strong>.<br />
— delivered a special lecture on 'Culture <strong>of</strong> Artemia salina in India' on 29 July<br />
<strong>1980</strong> at the Summer <strong>Institute</strong> on Brackish water capture and culture fisheries,<br />
held at the Central Inland Fisheries Research <strong>Institute</strong> (ICAR), Barrackpore,<br />
West Bengal.<br />
Dr. (Mrs.) Usha Goswami and Shri S. C. Goswami presented a paper "Formulation <strong>of</strong><br />
cheap prawn diets and their biological evaluation on some penaeid prawns'<br />
at the Symposium on Coastal Aquaculture held at Cochin from 12 to 18<br />
January. <strong>1980</strong>.<br />
Dr. M. D. Zingde attended Third IOC/WMO Workshop on Marine Pollution Monitoring<br />
at New Delhi from 13-15 February, <strong>1980</strong>.<br />
Shri N. M. Anand delivered a lecture during the ISTE Winter School on 'Design and<br />
construction <strong>of</strong> <strong>of</strong>fshore structures' held at Engineering College, Farmagudi, Goa.<br />
Dr. (Mrs.) Vijayalakshmi R. Nair delivered a series <strong>of</strong> invited lectures on "Plankton<br />
and Productivity" at Central <strong>Institute</strong> <strong>of</strong> Fisheries Education, ICAR, Bombay.<br />
Shri B. G. Wagle attended a seminar organised by the Ministry <strong>of</strong> Home Affairs,<br />
Government <strong>of</strong> India on Security measures for restricted maps and aerial<br />
photographs from 6 to 7 October, <strong>1980</strong> held at New Delhi.<br />
Shri S. N. Harkantra participated and presented two papers in 'International Symposium<br />
on "Coastal Aquaculture' held at Cochin from 12 to 18 January, <strong>1980</strong>.<br />
Shri Rajiv Nigam participated and presented a paper at the Eighth Indian Colloquia on<br />
Micropaleontology and Stratigraphy held at Baroda from 14 to 16 February, <strong>1980</strong>.<br />
Mrs. V. B. Peshwe participated in the Fluke Calibration Seminar organised by M/s,<br />
Hinditron Services Pvt. Ltd., Bangalore at the Indian <strong>Institute</strong> <strong>of</strong> Science-<br />
Bangalore from October 29 to 30, <strong>1980</strong>.<br />
Shri C. L. Rodrigues participated and presented a paper in the "First All India Symposium<br />
on Invertebrate Reproduction' held from 28 to 30 July, <strong>1980</strong> at Madras.<br />
Shri V. K. Dhargalkar and Shri V. V. Agadi attended <strong>National</strong> Workshop on Algal<br />
Systems at Madras on 3rd and 4th October, <strong>1980</strong>. Shri V. K. Dhargalkar<br />
presented a paper entitled "Some observations on the effect <strong>of</strong> seaweed liquid<br />
fertilizer on the higher plants'.<br />
Dr. T. Bose Babu, Shri G. R. K. Raju and Dr. V. V. Sarma presented a paper entitled<br />
"Studies on the distribution <strong>of</strong> pollutants in the coastal waters <strong>of</strong>f Visakhapatnam"'<br />
in the seminar organised by Bhabha Atomic Research Centre, Bombay.<br />
117
International Seminar on India and East African, Littoral, Hinterland and Island States:<br />
Areas <strong>of</strong> Cooperation<br />
This Seminar co-sponsored by the Indian Council for Cultural Relations, the<br />
Centre <strong>of</strong> East African Studies <strong>of</strong> Bombay University and the <strong>National</strong> <strong>Institute</strong> <strong>of</strong><br />
<strong>Oceanography</strong> was held at NIO. Dona Paula. Goa from January 16-18, <strong>1980</strong>.<br />
Pr<strong>of</strong>. Ram Joshi. President. Seminar Committee and Vice-Chancellor. Bombay<br />
University, welcomed the participants and guests. Mr. M. A. Vellodi. IFS. Adviser to<br />
the Department <strong>of</strong> Atomic Energy, inaugurated the Seminar and Dr. S. Z. Qasim-<br />
Director. ΝIΟ. Vice-Chairman. Organizing Committee proposed a vote <strong>of</strong> thanks.<br />
Shrimati Shanti Sadiq Ali. Member. Governing Body, I.C.A.R. New Delhi and<br />
Chairman. Organizing Committee highlighted the theme <strong>of</strong> the Seminar.<br />
About 50 scientists and educationists from India and African countries participated<br />
in this Seminar.<br />
More than 20 papers pertaining to the theme <strong>of</strong> the Seminar were presented<br />
which were followed by very lively and indepth discussions. Finally the committee<br />
made the following recommendations:<br />
1. To reinforce cooperative efforts to make the Indian Ocean a <strong>of</strong> peace and<br />
more in the direction <strong>of</strong> the principle <strong>of</strong> collective self-reliance.<br />
2. To explore the possibility to form an Indian Ocean Economic Community<br />
supplemented by a multi-lateral organisation to look after the economic and technical<br />
efforts in the region.<br />
118
3. To organize proper training courses and to provide mutually negotiable<br />
educational, cultural and technological assistance including the meteorological aspects<br />
to the countries in the region-<br />
All India Seminar on Protection and Control <strong>of</strong> Coastal Erosion in India<br />
This Seminar was organised by NIO at the <strong>Institute</strong> premises at Dona Paula<br />
on May 16 and 17. <strong>1980</strong>. The Seminar was inaugurated by Pro. S. Nurul Hasan,<br />
Vice-President <strong>of</strong> CSIR. More than 60 senior scientists and engineers from organizations<br />
like Central Water and Power Research Station, Pune; Engineering Research<br />
<strong>Institute</strong>s <strong>of</strong> Kerala, Karnataka, Maharashtra and Gujarat; Port Trusts and Public<br />
Works Departments <strong>of</strong> various States, India Tourism Department Corporation, New<br />
Delhi, academic institutions like IIT and Karnataka Regional Engineering College,<br />
Suratkal participated in this seminar. Two distinguished scientists Pr<strong>of</strong>. P. Bruun and<br />
Pr<strong>of</strong>. O. G. Houmb <strong>of</strong> the Norwegian <strong>Institute</strong> <strong>of</strong> Technology also participated in the<br />
Seminar. The Chief Minister <strong>of</strong> Goa. Daman and Diu. Shri Pratap Singh Rane was<br />
the Chief Guest, who released the manual on "Protection and control <strong>of</strong> coastal<br />
erosion in India' prepared by Pr<strong>of</strong>. P. Bruun and Dr. B. U. Nayak.<br />
In the seminar, deliberations were held under four technical sessions, viz. (i)<br />
causes <strong>of</strong> coastal erosion, (ii) procedures for field and laboratory studies, (iii) remedial<br />
measures and (iv) coastal protection and management. In the concluding session,<br />
the seminar emphasized the need for further research and recommended concentrated<br />
efforts for developing the following:<br />
1. Conservative methods for the protection <strong>of</strong> beaches and dunes and their<br />
restoration by placement <strong>of</strong> sand from inland <strong>of</strong>fshore sources and growing dune<br />
vegetation-<br />
2. Various remedial measures for eliminating erosion caused due to man-made<br />
coastal developments such as harbours, coastal protection structures, fishery jetties, etc.<br />
119
3. Various low-cost equipment for handling artificial beach nourishment and<br />
sand by-passing projects.<br />
4. A national policy for coastal zone management taking into consideration the<br />
multiple use <strong>of</strong> the shoreline.<br />
5. Comprehensive rules and guidelines in regard to direct removal <strong>of</strong> sand<br />
from beaches and dunes for commercial purposes.<br />
6. A multi-disciplinary approach for solving country's shoreline erosion pro-<br />
blems and a leading role <strong>of</strong> NIO in this context.<br />
<strong>National</strong> Workshop on Energy from the Sea<br />
A national workshop on "Energy from the Sea", the first <strong>of</strong> its kind organised<br />
in India was held at the <strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong>, Dona Paula,<br />
Goa on 15 and 16 December, <strong>1980</strong>. The main objective <strong>of</strong> the workshop was to<br />
review the state <strong>of</strong> art on the subject and to identify R & D areas on 'Energy from<br />
the Sea' to be carried out by a team in India.<br />
The two day workshop sponsored jointly by NIO and Spencer's India Ltd.,<br />
Bangalore was inaugurated by the Honourable Chief Minister <strong>of</strong> Goa, Daman &<br />
Diu - Shri Pratap Singh Rane on 15th December, <strong>1980</strong>.<br />
About 75 delegates consisting <strong>of</strong> engineers, scientists and planners from various<br />
leading research and academic institutions <strong>of</strong> the country and the State Electricity<br />
Boards participated in the workshop in which 37 papers were presented and discussed.<br />
The deliberations <strong>of</strong> the workshop were grouped in five technical sessions dealing<br />
with Ocean Thermal Energy Conversion (OTEC). Wave Energy, Tidal Energy. Energy<br />
from Salinity Gradient (ESG) and Marine Biomass Conversion (MBC).<br />
Some <strong>of</strong> the recommendations <strong>of</strong> the workshop were:<br />
1. India has a high potential for 'OTEC' plants.<br />
2. Lakshadweep is geographically well suited for a mini-OTEC plant.<br />
3. A coordinated multi-disciplinary research programme should be developed<br />
for an experimental OTEC plant <strong>of</strong> one megawatt.<br />
4. The wave activated generator developed by the Madras Port Trust should<br />
be widely used for lighting navigation buoys.<br />
5. Studies in the Gulf <strong>of</strong> Kutch, Gulf <strong>of</strong> Cambay and Sunderbans for the<br />
development <strong>of</strong> Tidal Power Plants should be intensified.<br />
6. Collection <strong>of</strong> wave data for extracting energy from waves should be carried<br />
out intensively.<br />
7· Development <strong>of</strong> a national time-bound programme for OTEC and tidal<br />
power development is necessary.<br />
8. The R and D work for extracting energy from salinity gradients and marine<br />
biomass conversion should also be undertaken.<br />
120
Honurable Shri Pratapsingh<br />
Rane, Chief Minister. Goa,<br />
Daman & Diu inagurating<br />
the <strong>National</strong> Workshop on<br />
Energy from the Sea.<br />
Pr<strong>of</strong>. Nurul Hasan on board Gaveshani
Dr. A. B. Wagh<br />
11<br />
Radio Talks<br />
1<br />
2<br />
3<br />
4<br />
5<br />
6<br />
7<br />
8<br />
9<br />
10<br />
11<br />
12<br />
13<br />
14<br />
Speaker<br />
Dr.S. Z. Qasim<br />
Dr. J. S. Sastry<br />
Dr. B. U. Nayak<br />
Shri T. C. S. Rao<br />
"<br />
Dr. E. Desa<br />
Dr. A. H. Parulekar<br />
Shri S. A. H. Abidi<br />
Shri S. N. De Souza<br />
Shri S. G. Dalal<br />
"<br />
Dr. M. Madhupratap<br />
Shri K. Sawkar<br />
122<br />
Subject<br />
• • Science and International<br />
Cooperation<br />
• • Monsoon Experiment 1979<br />
• • Coastal protection and control<br />
• • Blue Revolution<br />
• • Aquaculture (in Marathi)<br />
• • Fishing—Mechanical or<br />
treditional (in Marathi)<br />
• • Energy from the sun<br />
• • Importance <strong>of</strong> prawns in the<br />
development <strong>of</strong> Fisheries in Goa<br />
• • Sagar Manthini Gaveshani<br />
• • Pollution <strong>of</strong> the sea (in Konkani)<br />
• • Computer and Society<br />
• • What is Computer? (in Marathi)<br />
• • Energy from the sea<br />
• • Synthetic fibres
12<br />
Publications<br />
12.1 Scientific Papers<br />
Abidi, S.H. and S.B. Singh, <strong>1980</strong>. Fishery <strong>of</strong> the Nyumba Ya Mungu Dam—A man<br />
made lake in Tanzania. Jour. Indian Fish. Ass., 6:72.80.<br />
Achuthankutty, C. T. and S.R. Sreekumaran Nair, <strong>1980</strong>. Mangrove swamps as fry<br />
source for shrimp culture-—A case study. Mahasagar Bull· natn. lust. Oceanogr.,<br />
13: 269-276.<br />
Achuthankutly, C T., M- Madhupratap, V.R. Nair, S.R.S. Nair and T.S.S. Rao,<br />
<strong>1980</strong>. Zooplankton biomass and composition in the western Bay <strong>of</strong> Bengal<br />
during late SW monsoon. Indian J. mar. Sci, 9: 201-206.<br />
Almeida, F. and G.C. Bhattacharya, <strong>1980</strong>. Ripples on the seabed in the Bombay<br />
harbour area. Indian J. mar. Sci.,9: 212-214.<br />
Anand, S.P. <strong>1980</strong>. A solar dryer for marine-cum-farm products. Mahasagar—Bull·<br />
natn. Inst. Oceanogr., 13: 383-384.<br />
Ansari, Z.A., A.H. Parulekar and T.G. Jagtap. <strong>1980</strong>. Distribution <strong>of</strong> sublittoral<br />
meiobenthos <strong>of</strong>f Goa coast, India. Hydrobiologia, 74: 209-214.<br />
Anto, A.F. and L. Hasse, <strong>1980</strong>. Methods for the determination <strong>of</strong> the fluxes <strong>of</strong><br />
momentum and heat in the surface layer over the Sea. Mausam, 31: 1-8.<br />
Anto, A.F.L. Hasse and C.S. Murty, <strong>1980</strong>. Stability parameters and their interrelationships<br />
at the Naviface.Mahasagar—Bull.natn.Inst. Oceanogr., 13:295-302.<br />
Bhattathiri, P.M.A., V.P. Devassy and K. Radhakrishna, <strong>1980</strong>. Primary production<br />
in the Bay <strong>of</strong> Bengal during south-west monsoon <strong>of</strong> 1978. Mahasagar—Bullnatn.<br />
Inst. Oceanogr., 13: 315-323.<br />
Braganca, A.and S. Sanzgiry, <strong>1980</strong>. Concentration <strong>of</strong> few trace metals in some coastal<br />
and <strong>of</strong>fshore regions <strong>of</strong> Bay <strong>of</strong> Bengal. Indian J. mar. Sci., 9: 283-286.<br />
Dalal, S.G., <strong>1980</strong>. Relationship between benthic foraminifera and sediment in the<br />
estuarine complex <strong>of</strong> Goa. Mahasagar—Bull. natn. Inst. Oceanogr., 13: 77-79.<br />
De Sa, S.E. and E. De Sa, <strong>1980</strong>. A closed-loop electromagnetic flowmeter. J. Phys.<br />
E. Sci. Instrumn., 13: 233-235.<br />
De Sa, S.E. and E. De Sa, <strong>1980</strong>. Sensor design for an electromagnetic flowmeter.<br />
Indian J. Pure and Applied Physics, 18: 351—353.<br />
Dhargalkar, V.K. and A.G. Untawale, <strong>1980</strong>. Some observations on the effect <strong>of</strong><br />
seaweed liquid fertilizers on the higher plants. Proceedings <strong>of</strong> <strong>National</strong> Workshop<br />
on Algal System, <strong>1980</strong>, p. 63-72.<br />
Dhargalkar, V.K., T.G. Jagtap and A.G. Untawale, <strong>1980</strong>. Biochemical constituents<br />
<strong>of</strong> the seaweeds along the Maharashtra coast. Indian J. mar. Sci., 9: 297-299.<br />
123
Fondekar, S.P., R.S. Topgi and R.J. Noronha, <strong>1980</strong>. Distribution <strong>of</strong> petroleum<br />
hydrocarbons in Goa coastal waters. Indian J. mar. Sci., 9: 286-288.<br />
George, J. and Vijayalakshmi R. Nair, <strong>1980</strong>. Planktonic ostracods <strong>of</strong> the northern<br />
Indian Ocean. Mahasagar—Bull. natn. Inst. Oceanogr., 13 :<br />
29-44·<br />
Gcpalan. U.K., P. P Meenakshikunjamma and K. S. Purushan, <strong>1980</strong>. Fungal infection<br />
in the tiger prawn (Penaeus monodon) and in other crustaceans from the Cochin<br />
backwater. Mahasagar—Bull. natn. Inst. Oceanogr., 13: 359-365.<br />
Gopalan, U. K , K. S. Purushan and T. S. S. Rao, <strong>1980</strong>. Case studies on the economics<br />
<strong>of</strong> an improved method <strong>of</strong> paddy field shrimp culture in Vypeen Island,<br />
Kerala. Proc. First Nat. Symp. on Shrimp Fanning, Bombay, 175-186.<br />
Gopinathan, C. K. and P. S. Joseph, <strong>1980</strong>. Physical features <strong>of</strong> nearshore waters <strong>of</strong>f<br />
Karwar. Indian J. mar. Sci., 9: 166—171.<br />
Gore, P. S. T. S. G. Iyer, O. Raveendran and R. V. Unnithan, <strong>1980</strong>. Isolation and<br />
significance οf Salmonella sp. from some beaches <strong>of</strong> Kerala. Mahasagar—Bull. natn.<br />
Inst. Oceanogr., 13: 147—152.<br />
Govindan, K., R. Kashinathan and B. N. Desai, <strong>1980</strong>. Quantitative studies on macrobenthic<br />
fauna in the polluted Thana Creek and Bombay harbour. J. Indian<br />
Fish. Ass., 6: 129-138.<br />
Haridas, P. P. Gopala Menon and M. Madhupratap, <strong>1980</strong>. Annual variations in<br />
zooplankton from a polluted coastal environment. Mahasagar—Bull. natn. Inst.<br />
Oceanogr., 13: 239-248.<br />
Harkantra, S. N., Ayyappan Nair, Z. A. Ansari and A. H. Parulekar, <strong>1980</strong>. Benthos<br />
<strong>of</strong> the shelf region along the west coast <strong>of</strong> India. Indian J. mar. Sci., 9: 106-110.<br />
Jacob, P. G. and M. D. Rajagopal. <strong>1980</strong>. Variations in stomach contents and biochemical<br />
composition <strong>of</strong> tissues in some marine fishes. Indian J. war. Sci.,<br />
9: 207-211.<br />
Jagtap, T. G. and A. G. Untawale, <strong>1980</strong>. Effect <strong>of</strong> petroleum products on mangrove<br />
seedlings. Mahasagar—Bull. natn. Inst. Oceanogr., 13:165-172.<br />
Jagtap, T. G. and A. G. Untawale, <strong>1980</strong>. Some ecological observations on Cataglossa<br />
lepoieuii (Harvey) from Zuari estuary, Goa. Seaweed Research and Utilisation,<br />
4: 17-24.<br />
Kesava Das, V. A. D. Gouveia and K. K. Varma, <strong>1980</strong>. Circulation and water<br />
characteristics on isanosteric surfaces in the northern Arabian Sea during<br />
February-April. Indian J. mar. Sci., 9: 156-165.<br />
Lalithambika Devi, C. B., T. Balasubramanian, H. Krishna Iyer and M. Krishnan kutty,<br />
<strong>1980</strong>. Feeding efficiency <strong>of</strong> Penaeus indicus and Metapenaeus dobsoni in different<br />
substratum. Mahasagar—Bull. natn. Inst. Oceanogr., 13: 353-357.<br />
Lingaraja, T. R. A. Selvakumar and V.K. Venugopalan, <strong>1980</strong>. A simple continuously<br />
monitoring apparatus for respiration study in aquatic organisms. Indian J.<br />
Exp. Biol, 18: 413-415.<br />
Madhupratap, M., <strong>1980</strong>. Ecology <strong>of</strong> coexisting copepod species from Cochin backwaters-<br />
Mahasagar—Bull. natn. Inst. Oceanogr., 13: 45-52·<br />
124
Madhupratap, M., V. P. Devassy, S. R. S. Nair and T. S. S. Rao, <strong>1980</strong>. Swarming<br />
<strong>of</strong> pelagic tunicates associated with phytoplankton bloom in the Bay <strong>of</strong> Bengal.<br />
Indian J. mar. Sci., 9: 69- 71.<br />
Mascarenhas A. H. N. Siddiquie and R. S. Topgi, <strong>1980</strong>. Distribution <strong>of</strong> strontium<br />
in sediments <strong>of</strong> the Minicoy Atoll, Lakshadweep. Indian J. mar. Sci., 9:281-283.<br />
Matondkar, S. G. P., S. Mahtani and S. Mavinkurve, <strong>1980</strong>. Seasonal variations in<br />
the micr<strong>of</strong>lora from mangrove swamps <strong>of</strong> Goa. Indian J. mar. Sci., 9: 119-120.<br />
Matondkar, S. G. P., S. Mahtani and S. Mavinkurve, <strong>1980</strong>. The fungal flora <strong>of</strong> the<br />
mangrove swamps <strong>of</strong> Goa. Mahasagar—Bull. natn· Inst. Oceanogr., 13: 281-283.<br />
Menezes, M. R., <strong>1980</strong>. Soluble lens protein polymorphism in oil sardine, Sardinella<br />
longiceps Val. Mahasagar—Bull. natn. Inst. Oceanogr., 13: 183-185.<br />
Menezes, M. R., <strong>1980</strong>. Some observations on the morphometry and biology <strong>of</strong> Psettodes<br />
erumei (Bloch) and Pseudorhombus arsiwn (Ham-Buch) from the Goa region-<br />
Mahasagar—Bull. natn.Inst. Oceanogr., 13: 377-381.<br />
Menezes, M. R., <strong>1980</strong>. Immunological analysis <strong>of</strong> the soluble lens proteins in some<br />
marine fishes. Indian J. mar. Sci., 9: 63-65.<br />
Mishra, D. C., K. S. R Murthy and T. C. S. Rao, <strong>1980</strong>. General expression for the<br />
spectrum <strong>of</strong> magnetic anomaly dus to a long tabular body and its characteristics-<br />
Indian J. mar. Sci., 9: 250-252.<br />
Murty, C.S. and V.V.R. Varadachari, <strong>1980</strong>. Topographic changes <strong>of</strong> the beaches at<br />
Valiathura, Kerala. Indian J. mar. Sci., 9: 31-34.<br />
Murty, C.S., M. Veerayya, J.S. Sastry and V. V. R. Varadachari, <strong>1980</strong>. Beach morphological<br />
variations over micro-time scales. Indian J. mar Sci., 9: 35-44.<br />
Murty, C.S., J.S, Sastry and V. V. R, Varadachari, <strong>1980</strong>. Shoreline deformation<br />
in relation to shore protection structures along Kerala coast. Indian J. mar-<br />
Sci-, 9: 77-81.<br />
Murty, P. S.N., Ch.M. Rao, A.L. Paropkari and R.S. Topgi, <strong>1980</strong>. Distribution <strong>of</strong><br />
Al, Mn, Ni, Co and Cu in the nonlithogenous fractions <strong>of</strong> the sediments <strong>of</strong><br />
the northern half <strong>of</strong> the western continental shelf <strong>of</strong> India. Indian J. mar.Sci.,<br />
9: 56-61.<br />
Naik, S. and C.V.G. Reddy, <strong>1980</strong>. Calcium phosphate saturation in the western Bay<br />
<strong>of</strong> Bengal. Indian J. mar, Sci., 9. 179-183.<br />
Nair, K.K.C. and K. Anger, <strong>1980</strong>. A closed sea water flow through siphon system<br />
for the cultivation and rearing <strong>of</strong> marine animals. Mahasagar—Bull. natn. Inst.<br />
Oceanogr., 13: 133-145.<br />
Nair, K.K.C. and K. Anger, <strong>1980</strong>. Seasonal variation in population structure and biochemical<br />
composition <strong>of</strong> Jassa falcata (Crustacea, Amphipoda) <strong>of</strong>f the island <strong>of</strong><br />
Helgoland. East Coast Marine Sciences, USA, Part II, 505-513.<br />
Nair, R. R. and N. H. Hashimi. <strong>1980</strong>. Holocene climatic inferences from the sediments<br />
<strong>of</strong> the western Indian continental shelf. Proc. Indian Acad. Sci., 89: 299-315.<br />
Nair, S.R.S. C. T. Achuthankutty, Vijayalakshmi R. Nair and V. P. Devassy, <strong>1980</strong>.<br />
Plankton composition in the coastal waters between Jaigarh and Rajapur along<br />
west coast <strong>of</strong> India. Mahasagar—Bull. natn. Inst. Oceanogr., 13 : 343-352.<br />
125
Nair, Vijayalakshmi R., <strong>1980</strong>. Production and association <strong>of</strong> zooplankton in the estuaries<br />
and nearshore waters <strong>of</strong> Goa. Indian J. mar. Sci., 9: 116-119.<br />
Nair, Vijayalakshmi R., <strong>1980</strong>. Organic carbon content <strong>of</strong> tropical zooplankton. Indian<br />
J. mar. Sci., 9: 114-116.<br />
Nair, Vijayalakshmi R. and G. Peter, <strong>1980</strong>. Zooplankton from the shelf waters <strong>of</strong>f the<br />
west coast <strong>of</strong> India. Mahasagar—Bull. natn. lnst. Oceanogr., 13: 61-65.<br />
Nair, Vijayalakshmi R., V. P. Devassy and S.Z. Qasim, <strong>1980</strong>. Zooplankton and Trichodesmium<br />
phenomenon. Indian J. mar. Sci., 9: 1-6.<br />
Nair, Vijayalakshmi R. and V.T. Paulinose, <strong>1980</strong>. Decapod larvae from the nearshore<br />
waters <strong>of</strong> Karwar. Mahasagar—Bull. natn. lnst. Oceanogr., 13: 277-280.<br />
Namboodiri, P.N. and P.Sivadas, <strong>1980</strong>. On the occurrence <strong>of</strong> Bullia tranquebarioa<br />
(Roding) Nassaridae (Gastropoda) in Kavaratti atoll (Lakshadweep). Curr.<br />
Sci.; 549:683-684.<br />
Nigam, R. and M.G.A.P. Setty, <strong>1980</strong>. Paleogene reworked foraminifera in the recent,<br />
sediments <strong>of</strong>f Daman, western India. Proc. 3rd Indian Geological Congress,<br />
Poona, 273-280.<br />
Pant, A·, V.K. Dhargalkar, N.B. Bhosle and A. G. Untawale, <strong>1980</strong>. Contribution <strong>of</strong><br />
phytoplankton photosynthesis to a mangrove ecosystem. Mahasagar—Bull.<br />
natn. Inst. Oceanogr., 13: 225-234.<br />
Paropkari, A.L, R.S., Topgi, Ch. M. Rao and P. S. N. Murty, <strong>1980</strong>. Distribution<br />
<strong>of</strong> Fe, Mn, Ni, Co and Zn in the nonlithogenous fractions <strong>of</strong> sediments <strong>of</strong><br />
Gulf <strong>of</strong> Kutch. Indian J. mar. Sci., 9: 54-56.<br />
Parulekar, A.H., V.K. Dhargalkar and S.Y.S. Singbal, <strong>1980</strong>. Benthic studies in Goa<br />
estuaries: Part III. Annual cycle <strong>of</strong> macr<strong>of</strong>aunal distribution, production and<br />
trophic relations. Indian J. mar. Sci., 9: 189-200.<br />
Paulinose, V.T., <strong>1980</strong>. Decapod Crustacea from the International Indian Ocean Expedition<br />
(Larval and postlarval stages <strong>of</strong> Parapenaeus Smith (Penaeinae). Jour.<br />
Nat.. Hist., London, 13: 599-618.<br />
Peshwe, V.B., S.G. Diwan, A. Joseph and E. Desa, <strong>1980</strong>. Wave and tide gauge.<br />
Indian J. mar. Sci., 9:73-76.<br />
Qasim, S. Z. and R. Sen Gupta. <strong>1980</strong>. Present status <strong>of</strong> marine pollution in India. Management<br />
<strong>of</strong> the Environment, edited by B. Patel, Wiley Eastern Ltd. pp. 310-329.<br />
Qasim, S.Z., <strong>1980</strong>. Adaptations in phytoplankton to changing conditions in tropical<br />
estuaries. Mahasagar—Bull. natn. Inst. Oceanogr., 13:117-124.<br />
Rajendran, A., M. D. Rajagopal and C.V.G. Reddy, <strong>1980</strong>. Distribution <strong>of</strong> dissloved<br />
silicate in the Arabian Sea and Bay <strong>of</strong> Bengal. Indian J. mar. Sci., 9: 172-178.<br />
Rajendran. A., T. Joseph and C.V.G. Reddy, <strong>1980</strong>. Experimental studies on urea<br />
degradation in sea water. Mahasagar—Bull. natn. Inst. Oceanogr., 13: 303-313.<br />
Ramesh Babu, V. M.J. Varkey, V. Kesava Das and A.D. Gouveia, <strong>1980</strong>. Water<br />
masses and general hydrography along the west coast <strong>of</strong> India during early<br />
March. Indian J. mar. Sci., 9: 82-89.<br />
Rao, T.C.S., X. Terry Machado and K.S.R. Murthy, <strong>1980</strong>. Topographic features<br />
over the continental shelf <strong>of</strong> Visakhapatnam. Mahasagar—Bull. natn. Inst.<br />
Oceanogr., 13: 23-28.<br />
126
Rao, T.C.S. and K.S.R. Murthy, <strong>1980</strong>. Magnetic surveys over the continental shelf<br />
<strong>of</strong> Visakhapatnam. Mahasagar—Bull. natn. Inst. Oceanogr., 13: 83-89.<br />
Rao, T.S.S., <strong>1980</strong>. Zoogeography <strong>of</strong> the Indian Ocean. In: Zoogeography and Diversity<br />
in Plankton, edited by Drs. Van der Spoel and Pierrot Bults, pp. 254-292.<br />
Remani, K.N., P. Venugopal, K. Sarala Devi, S. Lalitha and R. V. Unnithan, <strong>1980</strong>.<br />
Sediments <strong>of</strong> the Cochin backwater in relation to pollution. Indian J. mar.<br />
Sci., 9: 111-114.<br />
Royan, J. P., <strong>1980</strong>. Decapsulated brine shrimp cysts—an ideal feed for shrimps in<br />
aquaculture. Indian J. mar. Sci., 9: 125-126.<br />
Royan, J.P., <strong>1980</strong>. Laboratory and field studies on an Indian strain <strong>of</strong> the brine<br />
shrimp, Artemia. In: The Brine Shrimp Artemia, Vol. 3: Ecology, culturing and use<br />
in aquaculture. edited by G. Persoone, P. Sorgeloss, O. Reels and E. Jaspers,<br />
Universa Press, Wetteren, Belgium.<br />
Rosamma Stephen and T.S.S.Rao, <strong>1980</strong>. Distribution <strong>of</strong> bathypelagic family Arielethidae<br />
(Copepoda, Calanoida) in the upper 200 m in the Indian Ocean. Jour.<br />
Plankton Res., 2: 239-247.<br />
Santhakumari, V. and U. K. Gopalan, <strong>1980</strong>. The protozoan associates <strong>of</strong> some<br />
crustaceans. Mahasagar—Bull. natn. Inst. Oceanogr., 13: 125-131.<br />
Saraswathy, M. and J.M. Bradford, <strong>1980</strong>. Integumental structures <strong>of</strong> the antennule <strong>of</strong><br />
the copepod Gaussia. New Zealand Journal <strong>of</strong> Marine and Freshwater, 14:79-82.<br />
Saraladevi, K. and T. S. S. Rao, <strong>1980</strong>. Genus Haloptilus (Copepoda: Calanoida)<br />
from the equatorial region <strong>of</strong> the Indian Ocean. Mahasagar—Bull. natn. Inst.<br />
Oceanogr., 13: 67-70.<br />
Selvakumar, R.A. V. R. Nair and M. Madhupratap, <strong>1980</strong>. Seasonal variations in the<br />
secondary production <strong>of</strong> the Mandovi-Zuari estuarine system <strong>of</strong> Goa. Indian<br />
J. mar. Sci., 9: 7-9.<br />
Sen Gupta, R., S. Z. Qasim, S.P. Fondekar and R. S. Topgi, <strong>1980</strong>. Dissolved petroleum<br />
hydrocarbons in some regions <strong>of</strong> the northern Indian Ocean. Mar. Poll.<br />
Bull., 11: 65-68.<br />
Sen Gupta, R., S.P. Fondekar, T.W. Kureishy, S.Y.S. Singbal and S.Sanzgiry, <strong>1980</strong>.<br />
Pollution studies in the Arabian Sea. Proc. International Symp. on Environmental<br />
Pollution and Toxicology, edited by D. S. Gupta and S. P. Roy Choudhury,<br />
Today and Tomorrow's Printers & Publishers, New Delhi, pp. 67-82.<br />
Sen Gupta, R., A. Braganca, R.J. Noronha and S.Y.S. Singbal, <strong>1980</strong>. Chemical oceanography<br />
<strong>of</strong> the Arabian Sea—Part V:Hydrochemical characteristics <strong>of</strong> the<br />
central west coast <strong>of</strong> India. Indian J. mar. Sci., 9: 240-245.<br />
Setty, M.G.A.P., <strong>1980</strong>. Foraminiferal constituents in marine sediments—a parameter<br />
in some coastal engineering problems. Mahasagar—Bull. natn. Inst. Oceanogr.,<br />
13: 111-315-<br />
Setty, M.G.A.P. and R. Nigam, <strong>1980</strong>. Microenvironmental and anomalous benthic<br />
foraminiferal distribution within the neritic regime <strong>of</strong> the Dabhol-Vengurla sector<br />
(Arabian Sea). Revista Italiana di Paleontologia e Stratigrafia, 36: 1037-1048.<br />
Setty, M. G. A. P. and R. Nigam, <strong>1980</strong>. Excentricity and twining in Virguinella pertusa<br />
(Reuss). Rivista Espanol de Micropaleontologia, 12: 202-204.<br />
127
Setty, M.G.A.P., R. Williams and K.R. Kerry, <strong>1980</strong>. Foraminifera from the Deep<br />
Lake Terraces. Vestfold Hills, Antarctica. Jour.Foraminiferal Res., 10: 303-312.<br />
Shanta Nair and Loka Bharathi, <strong>1980</strong>. Heterotrophic bacterial population in tropical<br />
sandy beaches. Mahasagar—Bull. natn. Inst. Oceanogr., 13: 261-267.<br />
Siddiquie. H. N., <strong>1980</strong>. The ages <strong>of</strong> the storm beaches <strong>of</strong> the Lakshadweep (Laccadives).<br />
Marine Geology, 38: 11-20.<br />
Siddiquie, H.N., D.Gopala Rao, M. Veerayya and B.G.Wagle, <strong>1980</strong>. Acoustic masking<br />
due to gases in shallow seismic pr<strong>of</strong>iling on the shelf <strong>of</strong>f Bombay. Indian<br />
J. mar. Sci., 9:51-54.<br />
Solimabi, L. Fernandes, S.Y. Kamat and S. K. Paknikar. <strong>1980</strong>. New diterpenoids <strong>of</strong> the<br />
seaweed Stoechospermum marginatum—structure <strong>of</strong> Stoechospermol. Tetrahedron<br />
letters, 21: 2249.<br />
Solimabi, B. Das, S. Y. Kamat, L. Fernandes and C. V. G. Reddy, <strong>1980</strong>. Seasonal<br />
changes in carrageenan and other biochemical constituents <strong>of</strong> Hypnea musciformis-<br />
Indian J. mar. Sci., 9: 134-136.<br />
Solimabi, S.Y.Kamat, C.V.G. Reddy, V.R.Naik, N.V. Agshikar and G.J.S. Abraham,<br />
<strong>1980</strong>. Comparison <strong>of</strong> carrageenan from Hypnea imisciformis wulfen with other<br />
carrageenans. Indian J. Exp. Biol., 18: 649-650.<br />
Somayajulu, Y.K, L.V.G. Rao and V.V.R. Varadachari, <strong>1980</strong>. Small scale features<br />
<strong>of</strong> sound velocity structure in the northern Arabian Sea during February-May,<br />
1974. Indian J. mar. Sci., 9: 141-147.<br />
Sumitra Vijayaraghavan. V. Ramadhas. L. Krishna Kumari and J. P. Royan. <strong>1980</strong>.<br />
Biochemical changes and energy content <strong>of</strong> the mangrove, Rhizophora mucronata<br />
leaves during decomposition. Indian J. mar. Sci., 9: 120-123.<br />
Sumitra Vijayaraghavan and V. Ramadhas. <strong>1980</strong>. Conversion efficiency in the shrimp<br />
Metapenaeus monoceros (Fabricius) fed on decomposed mangrove leaves. Indian<br />
J. mar. Sci., 9: 123-125.<br />
Sumitra Vijayaraghavan, M. D. Rajagopal and M. V. M. Wafar, <strong>1980</strong>. Seasonal variation<br />
in biochemical composition <strong>of</strong> seaweeds from Goa coast. Indian J. mar. Sci.,<br />
9: 61-63.<br />
Swamy, G.N., V.M. Kolhatkar and A.A. Fernandes, <strong>1980</strong>. Currents and siltation at<br />
Dharamtar Creek, Bombay. Mahasagar—Bull. natn. Inst. Oceanogr., 13: 191-203.<br />
Untawale, A.G., V.V.Agadi and V.K. Dhargalkar. <strong>1980</strong>. Occurrence <strong>of</strong> Monostroma<br />
(Ulvales, Chlorophyta) from Ratnagiri (Maharashtra). Mahasagar—Bull. natn.<br />
Inst. Oceanogr., 13: 179-181.<br />
Untawale, A.G., T. G. Jagtap and V.K. Dhargalkar. <strong>1980</strong>. Dichotomosiphon salina sp.<br />
Nov.—A new marine algal form, Goa estuary, India. Mahasagar—Bull. natn.<br />
Inst. Oceanogr., 13: 73-76.<br />
Untawale, A.G., Sayeeda Wafar and N. B. Bhosle, <strong>1980</strong>. Seasonal variation in the<br />
heavy metal concentration <strong>of</strong> mangrove foliage. Mahasagar—Bull. natn. Inst.<br />
Oceanogr., 13:215-223.<br />
Varkey, M. J., <strong>1980</strong>. Power spectra <strong>of</strong> currents <strong>of</strong>f Bombay. Indian J. mar. Sci., 9:<br />
278-280.<br />
128
Varma, K.K., V. Kesava Das and A. D. Gouveia, <strong>1980</strong>. Thermohaline structure and<br />
water masses in the northern Arabian Sea during February-April. Indian J. mar.<br />
Sci. 9: 148-155.<br />
Verlencar, X. N., <strong>1980</strong>. Distribution <strong>of</strong> area in the waters <strong>of</strong> the west coast <strong>of</strong> India-<br />
Indian J. mar. Sci., 9: 230-233.<br />
Vora, K.H., A. R. Gujar and S. M. Karisiddaiah, <strong>1980</strong>. Sandwaves <strong>of</strong> the Gulf <strong>of</strong><br />
Khambhat. Indian J. mar. Sci., 9: 90-93.<br />
Wafar, M. V. M., M. D. Rajagopal, M. R. Menezes and A. Stirling, <strong>1980</strong>. Physicochemical<br />
features and energy input in three sandy beaches <strong>of</strong> west coast <strong>of</strong><br />
India. Indian J. mar. Sci., 9: 25-30.<br />
Wagle, B.G. and G. Victor Rajamanickam. <strong>1980</strong>. A petrographic study <strong>of</strong> Precambrian<br />
quartzites from Goa coast. Mahasagar—Bull. natn. Inst. Oceanogr., 13: 9-21.<br />
Zingde. M.D., M.M. Sabnis, A.V. Mandalia and B.N.Desai. <strong>1980</strong>. Effects <strong>of</strong> Industrial<br />
waste disposal on the water quality <strong>of</strong> the river Kolak. Mahasagar—Bull.<br />
natn. Inst. Oceanogr.,13: 99-110.<br />
Zingde. M.D., P. V.Narvekar. R.V. Sarma and B.N. Desai. <strong>1980</strong>. Water quality <strong>of</strong> the<br />
river Damanganga (Gujarat). Indian J. mar. Sci., 9: 94-99.<br />
Zingde, M. D. and B.N. Desai, <strong>1980</strong>. Waste water discharge and its effects on the<br />
quality <strong>of</strong> water <strong>of</strong> Mahim Creek and Bay. Mahasagar—Bull. natn. Inst.<br />
Oceanogr., 13: 205-213-<br />
12.2 Popular Articles and Book Reviews<br />
Abidi, S.A.H. <strong>1980</strong>. Utilisation <strong>of</strong> creek areas for coastal aquaculture. The Daily<br />
Telegram, January 28, <strong>1980</strong>.<br />
Abidi. S.A.H., <strong>1980</strong>. Grameen Vikas Aur Machhli Udhyog. Kheti ICAR Monthly<br />
Bulletin (Hindi), April, <strong>1980</strong>.<br />
Abidi, S.A.H. <strong>1980</strong>. Rashtra Ka Samudra Par Adhikar Evam Uski Seemayyain. Dweep<br />
Prabha Publications (Hindi), January/March, <strong>1980</strong>.<br />
Abidi, S.A.H., <strong>1980</strong>. Samudra Garbha Men Khanij Sampatti. Navneet Bombay (Hindi),<br />
May, <strong>1980</strong>.<br />
Bhargava, R.M.S. <strong>1980</strong>. Coasts and estuaries· James Ferguson Lees and Bruce<br />
Compbell Eds., Holder and Stoughton Ltd., London, 1979 (Book Review).<br />
Mahasagar-Bull natn. Inst. Oceanogr., 13(1). 81-82.<br />
Das. P.K. and S.Z.Qasim, <strong>1980</strong>. Advances in <strong>Oceanography</strong>. H. Carnak and G. Deacon<br />
(Eds), Plenum Press, N.Y.1978 (Book Review)· Jour. Scientific and lndu. Res.,<br />
39(4).<br />
Gopinathan, C. K., <strong>1980</strong>. Energy—New ocean resources. Science Reporter, 17.<br />
Kesava Das, V., <strong>1980</strong>. Satellites for remote sensing <strong>of</strong> the oceans. Science Reporter, 17 (7).<br />
Kasava Das. V., <strong>1980</strong>. Harnessing the ocean heat. Science Reporter, 17(11).<br />
Kesava Das, V., <strong>1980</strong>. Power from the oceans. The Sunday Navhind Times Daily<br />
November 23, <strong>1980</strong>·<br />
Kesava Das, V., <strong>1980</strong>. Energy from the ocean. Physics News, December, <strong>1980</strong>.<br />
129
Madhupratap, M., <strong>1980</strong>. Progresss in oceanography. Martin V. Angel and James O<br />
Brien (Eds). Pergamon Press. Oxford, 1979 (Book Review). Mahasagar-Bull.<br />
natn. lnst. Oceanogr. 13(3): 293.<br />
Murty, C. S., <strong>1980</strong>. Descriptive Physical <strong>Oceanography</strong>. G. L. Pichard Ed., Pergamon<br />
Press, 1970 (Book Review). Mahasagar—Bull. natn. Inst. Oceanogr., 13(3).<br />
Nair, S.R.S. <strong>1980</strong>. Are oceans our last frontier? The West Coast Times Daily, Goa.<br />
October 23, <strong>1980</strong>·<br />
Nayak, M. R. <strong>1980</strong>. Micro-computers selection factors. Electronic Engineer, 32-48-<br />
Pant, A., <strong>1980</strong>. A pr<strong>of</strong>ile study. Hindustan Times, Sunday Edition, August, <strong>1980</strong>.<br />
Qasim, S. Z. <strong>1980</strong>. Endless energy form the sea. Science Today, 14(9): 17-23-<br />
Qasim, S. Z., <strong>1980</strong>. Ocean, the saviour <strong>of</strong> civilization. In: Souvenir <strong>of</strong> Institution <strong>of</strong> Engineers<br />
{India). Diamond Jubilee Number, 104-108.<br />
Qasim, S. Z. and R. M. S. Bhargava, <strong>1980</strong>. Developments in deep-sea biology. N. B.<br />
Marshall, Blandford Press. Dorset (Book Review). Mahasagar-Bull. natn. Inst.<br />
Oceanogr. 13(4): 385-386.<br />
Santhakumari, V., <strong>1980</strong>. Whales. Kuttikalude Deepika, 23 (3): 16-18.<br />
Santhakumari. V., <strong>1980</strong>. Coral reefs—the wonderful garden in the sea. Balarama,<br />
Magazine for Youth, 9(9): 61-63.<br />
Santhakumari, V., <strong>1980</strong>. Coconut crab or robber crab. Kuttikalude Deepita.<br />
Santhakumari, V., <strong>1980</strong>. Rocky shore. Sastragathy (Science Magazine). 14(8): 333-334.<br />
Siddiquie H. N., <strong>1980</strong>. Growth conditions <strong>of</strong> manganese nodules-comparative studies<br />
<strong>of</strong> growth rale magnetization, chemical composition and internal structure by<br />
Dictrich Hoye. In: Progress in <strong>Oceanography</strong>, edited by Mary Swallow (Review).<br />
J. Geol. Soc. India, 21: 421.<br />
Unnithan. R. V. <strong>1980</strong>. If there is no pollution. Deshabhimani (Weekend Daily) Cochin,<br />
13(3): 3-4.<br />
Unnithan, R. V. <strong>1980</strong>. Cochin University. Aim and Implementation. Deshabhimani,<br />
(Weekend Daily), 13(34): 4.<br />
Unnithan. R.V.. <strong>1980</strong>. Cochin University should have a dynamic leadership. Deshabhimani<br />
(Weekend Daily), Cochin. 13(35) : 4.<br />
Unnithan, R.V., <strong>1980</strong>. Law <strong>of</strong> the sea. Deshabhimani Onam Special, 203-211 ·<br />
Venugopal, P., K. N. Remani, K. Sarala Devi and R.V. Unnithan, <strong>1980</strong>. Fish kill<br />
in Chitrapuzha. Seafood Export Journal, 12:17-20.<br />
Verlencar, X.N., <strong>1980</strong>. Importance <strong>of</strong> quality chemical in testing water for bioassay<br />
studies in marine environments. Water Chemists Forum (Glaxo Laboratories<br />
India Ltd).<br />
Parulekar, A. H. <strong>1980</strong>. Culture <strong>of</strong> bivalve molluscs: 50 years experience at Conwy.<br />
P. R. Walne (Ed.), Fishing News Book Ltd. Furnham, Surrey, England (Book<br />
Review). Mahasagar-Bull. natn. lnst. Oceanogr., 13(4): 387.<br />
130
12.3 Technical Reports<br />
Current trends in store procedure and evaluation.<br />
The Andaman Sea.<br />
Evaluation <strong>of</strong> chemical dispersants for their suitability to Indian conditions.<br />
Status report <strong>of</strong> MAPMOPP <strong>of</strong> IGOSS for the Indian Ocean region.<br />
Nautical and physical oceanographic observations <strong>of</strong>f the drilling rig Chancellors<br />
Ville in the Mahanadi basin.<br />
Wave energy oscillator-Α concept in shore protection and coastal engineering.<br />
Ocean wave statistics.<br />
MBT data report <strong>of</strong> Monex-79 Cruises I-VI <strong>of</strong> R. V. Gaveshani·<br />
Hydrographic data report (from Nansen Casts) <strong>of</strong> Monex-79 Cruises <strong>of</strong> R. V. Gaveshani.<br />
Environmental data report <strong>of</strong> Monex-79 Cruises <strong>of</strong> R.V. Gaveshani.<br />
Lateral soil resistance against submarine pipeline stability.<br />
Control <strong>of</strong> rider data.<br />
Deep water mooring for oceanographic instruments.<br />
Internal report on CTD system (Electronics Commission).<br />
Internal report on wave and tide gauge (Electronics Commission).<br />
Report on Aanderaa Instruments RCM 4 current meters deck unit.<br />
12.4 Sponsored Projects Reports<br />
Current measurements at Dome Structure <strong>of</strong>f Tapti.<br />
A brief summary <strong>of</strong> the oceanographic and meteorological observations <strong>of</strong>f Cochin<br />
during February and March.<br />
Wave data acquisition at Bombay High using wave Rider Buoy and Analysis.<br />
Reconnaisance survey <strong>of</strong> Beach erosion at Fisherman's Cove, Covelong, Madras.<br />
Pollution and hydrographic survey <strong>of</strong> Auranga, Ambika, Purna and Mindola rivers.<br />
Survey <strong>of</strong> the proposed submarine pipeline routes from Bassein to Gujarat, Phase II·<br />
Seabed surveys on the D & I Structure, Kori Great Bank and on the Tapti Dome Structure.<br />
Postlay survey <strong>of</strong> the Bombay High to Bombay pipelines.<br />
Survey <strong>of</strong> the pipeline routes from Direction Bank to Bassein and Murud.<br />
Bathymetric and shallow seismic surveys on south Bassein, Bombay.<br />
Bathymetric and shallow seismic surveys on the Direction Bank, Bombay.<br />
Survey to measure the distances between the Piers <strong>of</strong> the Zuari Bridge, Cortalim, Goa·<br />
Shallow seismic and side scan sonar surveys in Marmugao Harbour, Goa.<br />
Shallow seismic and side scan sonar surveys in Visakhapatnam outer, inner and fishing<br />
harbours.<br />
131
NATIONAL INSTITUTE OF OCEANOGRAPHY<br />
DONA PAULA-403 004, GOA, INDIA<br />
Grams: OCEANOLOGY, PANJIM ' Telephones: 2155. 2156, 2157<br />
Telex : 0914-216 NIO IN · · 2158,2159<br />
2612 (Director's Off.)<br />
29C9 (Director's Res.)<br />
<strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Regional Centre<br />
Pullepady Cross Road<br />
Post Box No. 1913<br />
Cochin - 682 018<br />
<strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Regional Centre<br />
1st Floor, Sea Shell Buildings<br />
Seven Bungalows<br />
Versova, Bom bay-400 061<br />
<strong>National</strong> <strong>Institute</strong> <strong>of</strong> <strong>Oceanography</strong><br />
Regional Centre<br />
Andhra University Campus<br />
Waltair<br />
Visakhapatnam -530 003<br />
REGIONAL CENTRES<br />
Telephones: 33306, 31814; 33384<br />
Grams : OCEANOLOGY<br />
COCHIN<br />
Telephones: 573773, 574807,532620<br />
Grams : OCEANOLOGY<br />
BOMBAY<br />
Telephones: 4634, 3992<br />
Grams : OSTECHLAB ·