SCIENTIFIC ABSTRACT BOGOROV, B. - BOGOSLAVETS, A.I.

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• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

BOGOROV, B.., Inst. Oceanology, AS USSR
"Perspectives in research of life cycles and the generation quantity
of plankton in nny geographical latitude)" a paper submitted at the International
Union of Biological Sciences SyMosium on.Perspective5 in Marine Biolo6j, La
Jolla, California, 24-31, Mor '56.
so; E-982

BOGOROV. V.G.
Research on the expeditionary ship OTitlaz" in the Pacific Ocean.
IZT.Al SSM.Sor.geog. no.2:3-5 Mr,-,LP 136. (NLRL 9:8)
1. Institut oksanologli AN SM.
(Pacific Oceam-Oceanographic research)

DOGOROT, V.,professor.
The White Sea. Blok.agit.vod,tmamp. no.5:1&23 Mr '56.(HM 9:8)
(White Sea)

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BOGOROVP V.G.; DOBROVOLISKIY,
A.D.
Oceanographic ressarah in the Chinese People's Republic. Izv.
AN SSSR Sbr. geog. no.2':,137-14Z Mr-Ap 157. (MM 10:12)
(China-0aaanography)

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BOG&6vo V.G.; UMVICH, L.A.: RASS, T.S.
The worldla oceans and thoir resources. 12V. AN SSSR. Ser. geog.
no.5:39-49 5-0 157. (K= 11:2)
(oceanography)

25-10-13/41

AUTHOR: Bogorov, V. G., Doctor of Biological Sciences, Professor
TITLE: The Expanse of World Oceans (V prostorakh mirovogo okeana)
PERIODICAL: Nauka i Zhizn', 1957, # 10, PP 33-35 (USSR)
ABSTRACT: During the international Geophysical Year the Soviet Union
will carry out its research in the northern part of the Paci-
fic Ocean (from 50 degrees northern latitude to the equator),
the northern part of the Atlantic Ocean, in the Antarctic and
in the Arctic Seas. Already in 1953/54 the Soviet Expedition
organized by the Institute for Oceanography of the Academy of
Sciences of USSR on the "Vityau'll studied the western areas
of the Pacific Ocean and established that the representation
of the Tuakarora depression on the map in the form of a round
spot is not correct but that it is a narrow chink stretching
for about 2,000 km along the Kuril Islands and South Kamchat-
ka, and that its maximum depth amounts to 10 km (not 8,513 m
as formerly given by an American scientist). Moreover, the
existence of simple organisms was discovered in these depths,
which disproves former scientific assertions that life is
not possible beyond a depth of 6 km. It was also disclosed
Card 1/2 that the Marian depression with 10,863 m is the deepest in

The Expanse of World oceans
25-10-13/41
the Pacific and not the F=Fplne ftression.
In April 1957 a test expedition was organized by the Insti-
tute for Oceanography of the USSR Academy of Sciences headed
by N. N. Sysoyev. The first Soviet expedit�on of the Interna-
tional Geophysical Year was started on I July 1957 on board
of the ship "Vityas"' under the leadership of Professor A. D.
Dobrovoltakiy. The region to be studied stretches from
Eastern Japan to the 180th degree of longitude and from the
Kuril Islands to New Guinea. During the first three monthet
unknown submarine mountains have already been discovered, the
circulation of the various currents and streams has been
studied, the waters and sea bottom have been investigated
chemically. Special attention was paid to the research of
living organisms. A seismio-acoustio method was applied to
determine the layer of sea bottom sediments.
There are three sketches.
AVAILABLE; Library of Congress
Card 2/2

USSR/Gencral Biology - General Hydrobiolocy, Be
Abs Jour Hof 7-aiur - Biols, No 21, 1958, 9472B
Author Bogorovp V#G*
................................................. --" -
inst Institute of Occanography AS USM
Title Standardization of Marinc Plankton Investigationa,
Orig Pub : Tr4 Tii-ta okemiol, AN SSM) 1957.. No 24, 2oo-23.4
Abstract : A discourse is given on the most extensive methods and
instrumonte for collection of plankton groups of
rcut dimensions mid tho met offuctive nothods of tr,:!at-
ing the collected nateriale The quantitative methods
described arc recomendcd as standards for the stuCly of
plankton, Tables are appended -with standard weig1its of
mas species of plankton anivale in the Barentsp Bcring
and Okhotsk Seas. -- N.Oe Kashkino
Cara 1/1

BOGCFtOV, 1q. 0. MA MMPSJ E. M.
'Disebwging Radioactive Waste Into Deep-Water Ocean Depreasions."
paper tobe presented at 2nd UN Intl. Conf. on the peaceful uses of Atomic
Energy, Geneva, I - 13 Sept 1958.

BOGOOR'"M V. G. and VIVIOGRADOV, 1-1. Ye.
Distribution of Zooplankton in the Northwestern Part of the Pacific Ocean.
The article examines the problem of plankton distribittion in connection with concentrations
of fish and :Lx discusses the possibility of pronostication. 'P.
Oceanographic Research of the Northwestern Part of the Paci]~ic Oilean Moscow, Izd.-Vo
AN SSSR, 1958, 146 p. I~s: Trudy, t-3.
This collection of articles reports the results of observationsf made in the Pacific
by the institute of Oceanology fo the Academy of Sciences, USSR. In 1949, the Institute
launched a systematic five-year program of scientific exploration of certain hydrographic
peculiarities of the Soviet Pacific Area. The operations were carried out as a "CCmplex
Oceanographic Expedition," using the Motorboat Vityaz' as its base. The Expedition worked
in collaboration with the hydrographic Institute of the Soviet Navy (WIS), the Pacific
Institute of Piscatology and Oceanography, and some 40 other institutes of the Academy of
Sciences. Between 1949 and 1954, 18 trips were made, covering about 130,000 miles. Among
the subjects of direct concern were: Meteorology, hydrology, oceanog-rapby, hydrochemistry,
sedimentation, geography of the littoral, geology and contrours of the sea bottom, fauna,
plankton, microbiology, and gravimetry. Wenty-eight, authors contributed to the collection
vbich consists of 27 articles. There are: 6 gables, 23 diagrams, 3 illustrations (photo-
graphs of the littoral), 4 maps. There are no references.
Research of the Northwestern Part of the Pacific Ocean, Moscow, Izd-vo AN USSIR, 1958-

BOGOROV, V. G.
"The Qualitative and Quantitative Distribution of Ground- and Planktor
Organisms."
report presented at the*A11-Union conference on Biological Foundations of 0-~ean
Fishing, 11-16 April 1958, by Ichthyological Committee of AS USSR, VNIRO, and
Inst. Oceanography, AS USSR.
(Vest. AN SSSR, 1958, No- 7, PP. 131-133)

BDqM
Recommendations for the-standardization of plankton sampling during
the International Geophysical Year. Biul. Okean. kom. no.lt49-51 158.
(MDU 3-1: 9)
1.1natitut okesnologit AN SSSR.
(Plankton) (International Geophysical Year, 1957-1958)

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AUTHOR: Bogorov, V.G., Professor 26-58-2-37/45
TITLE: The First Ocennological Ship of the XNR (Pervoye okeanologi-
cheskoye sudno KNR)
PERIODICAL: Priroda, 1958, Nr 2, P 115 (USSR)
ABSTRACT: The Morskoy biologicheakiy institut Akademii nauk KNR (YLarine
Biological Institute of the Academy of ScienceR of the Chinese
People's Republic) has received a 1,000-ton sea tuir with a
speed of 12 mph and re-equipped as an expedition ship. It has
been named "Venera" and has 5 lqborstories snd cnbins for '~C
scientific workers. In 1957, the ship carried out reseArch
.in the China Sea and the Bokhay Sea.
ASSOCIATION: Institut okeanoloe,,ii Aksdemii nauk SSSR, !Jcskvs (Tnstitute of
Oceanology of the USSR Academy of Scierices, 1I.YoFcow)
Card 1/1 1. Oceanography--China sea 2. Ships--Applications

BOGOrO7;' -T . - 0.
In the Department of Geological-Geographical Sciences 30-58-5-13/36
Vent Ak Nauk SM, NO; 51 1958, p~ 56-59
f oceanology.
Thm1he detailed report of Professor V. G. Bogorov on the
results of the 26-th voyage of the e_x~peditionary vessel
"Vityaz" was heard which had according to the plan of
the International Geophysical Tear been entrusted with
the investigation of the central part of the Pacific
ocean. During the visit of the ship in the harbors of
Suva (Fiji. Islands )j, Wellington Anew Zealand)
and Humes, ( Nev Caledonia the Soviet scientists made
themselves acquainted with the scientific work of their
Englishp New Zealand and French colleagues. Scientific
conferences were held with the ooeanologists of New
Zealand, as well as with the Prenah at Humea. N. S.
Shatskiy, Member, Academy of Sciences, USSR and S. V.
Obruchev, Corresponding Member, Academy of Sciences,
USSR appreciated the researches of the "Vityaz" as an
important achievement of Soviet science.
I& Scientifid-research-USSR 2. Geology--USSR 3. Geography--USSR
chrd
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SOV/169-59-6-5724
Translation from: Referativnyy zhurnal.' Geofiz:Lka, 1959, Nr 6, p 44 (ussR)
AUTHOR- E2-gorov- V.G.
TIME: on the ~yjt
The Second Expedition _yaz" in Connec-en With the
IGY Program
PERIODICAL: Mezhdunar. geofiz. god. Inform. byul., 1958, Nr 5, PP 78 - 82.
ABSIRACTg Comprehensive explorations of the central part of ths Pacific
Ocean have been carried out during the period frcm November 5,
1957, to February 27, 1958. The zonal distribution of the
oceanological, characteristics and the depth water circulation
have been studied. The following observations were owied
out.- 1) physical observations fV studying the solar %adiation,
the distribution of temperature'and moisture of the air, the
characteristic motions of air masses, the structure ard dynamics
of water masses, the water circulation, the heat. contant c-f
water, the optical properties of water, and geophysio-al oharac-
teristics of the Earth's crust under the bottom of the caean;
Card 1/2 2) chemical observations for studying the chemic~-- p:r-:,p4r-Uea

SOV/169-59-6-5724
The Second Expedition on the "Vityaz'" in Connection With the IGY Program
of water and ooze, the radioactivity of water, sediments, animals, and the
balance of carbon dioxide content; 3) geological observations for studying
the relief of the bottom, sediments, suspensions in water and air, and geo-
chemical characteristics; photographs of the bottom of the ocean wer-- made;
4) oomprehenj~ive biological investigations. The main renearch work was carried
out in the region along 1720W.long. from 330n.lat. to New Zealand and along
1720 e.long.- from New Zealand to 300 n.lat. Comprehensive studies of the
Tonga, Kermadek and New Hebrides depressions were performed. A new depression
was discovered, extending in western direction from the area north of the F1dji
Islands. Investigations were performed into variations of boundaries of trade-
wind and inter-tradewind our-rents in the sout1iem and northern hemispheres.
When landing in Wellington, a conference was held for acquainting with the
work of the 'Vityazl".
V.M. Lifshits
Card 2/2

SOY-26-56-8-12/51
AUTHORt Bogorov, V.G., Associate Member of the USSR Academy of Scienoes
TITLE; On Board the "Vityaz"'in the Central PsT-t of the Pacific (Na
"Vityaze" v tsentrallnoy ohasti Tikhogo okeana)
PERIODICAL: Prirodav 1958P Nr 8, pp 66-73 (USSR)
ABSTRACT. From November 1957 to February 1958P the Soviet expedition
ship "Vityazill conducted reseaz-.h work in the Central Pacific.
The expedition lasted 115 days and covered 17,425 miles. The
scientific and auxiliary team consisted of 70 people. The
"Vityaz"' is a 5,500-ton research ship with 12 laboiatories.
She is equipped with 12 winches, among them a trawler winch
permitting the trawling in the greatest depths and an anchor
win0h for anchoring at depths exceeding 11 km. Investigations
were made in the passate and interpassate zones. The Tonga
and Kermadek depressions were investigated at the end of
December and the beginning of January. The Soviet oceano-
logists now have material available on 14 depressions of the
18 in the Pacific. In Wellington, Few Zealand, a scientific
conference was convened by the scientists of the "Vityaz"'
Card 1/2 together with scientists from New Zealand in which 12 papers

SOV-26-58-8-12/51
On Board the "Vityaz"' in the Central Part of the Pacific
were presented. During the expedition, 25 hydrological series
from the bottom and 96 from the 2,000 m level were investi-
gated. The geologists took 41 mud samples, made 16 photo-
graphs of the bottomv and 29 explosions for determining the
structure of the ocean bottom by seismo-acustic methods.
Plankton from the bottom was taken in 16 oases and from 500 M
in 97 cases.
There are 12 photos and I map.
ASSOCIATION: Institut okeanologii Akademii nauk SSSR (Institute of Oceano-
logy of the USSR Academy of Sciences)
1. Pacific Ocee-n--Oceamography 2. Oceean bottom--Samplizrig
3. Mari-ne biology--Pacific Ocear. 4. Seismic waves-.-Applications
Card 2/2

SOV-26-58-9-7/42
AUTHORS: BR&p
__ Z~.n , .,G.,,Kreps, Ye.M., Member Correspondents of the
AS USSP
TITLE: Is it Possible to Bury Radioactive Wastes in the Deep-Water
Trenches of the Ocean? (Vozmozhno li zakhoroneniye radioak-
tivnykh otkhodov v glubokovodnykh vpadinakh okeana)
PERIODICAL. Priroda, 1958, Nr 9, pp 45-50 (USSR)
ABSTRACT: According to the authors' opinion, the problem of the dispo-
sal of radio-active wastes has not yet been studied sufficiently.
The suggestion to bury radioactive wastes in one or several
of the 19 deep-water ocean trenches is considered. The Tonga
trench investigated in 1952/53 by the American research ve8-
sel "Capricorn" and in 1957/58 by the Soviet "Vityazl" is
taken for an example. It is described with respect to its
bottom relief, distribution of temperature, salinity and wa-
ter density, conditions characterizing the processes on the
trench bottom (tables 1 - 3), based partly on work by A.N.
Bogoyavlenskiyknd L.A. Zenkevich of the Institut okeanologii
(Institute of Oceanology). The ensuing discussion of water
Card 1/2 circulation in a given part of the ocean and the mixture of

SOV-26-56-9-7/42
Is it Possible to Bury Radioactive Wastes in the Deep-Water Trenches of the
Ocean?
diverse waterB is partly based on N.N. Zubov's investigations.
The authors conclude that the radiation wastes will get into
the general circulation of the upper water layers comparative-
ly quickly and enter the organisms of plants, animals, fish
and mammals there and consequently affect man dangerously.
There are 2 diagrams, 3 tables and 8 references, 3 of which
are Soviet, 3 American and 2 English.
1. Radioactive waste--Disposal
Card 2/2

AUTHOR: Bogorov, V. G. 2C-118-5-19/59
TITLE: The Production of Plankton and the Characteristic of the
Biographic Regions of the Ocean (Produktsiya planktona i
kharakteristika biograficheskikh oblaotey okeana)
PERIODICAL: Doklady Akademii Nauk SSSR, 1950, Vol. 110, Nr 5, pp. 917-
-gig (1133R)
ABSTRACT: According to data of several authors the primary production is
very different in different regions of the ocean. The determinat-
ion by sections of the primary production is of utmost importance.
The expedition of the Institute for Oceanology of the AS USSR in
1954 (on board the ship "Vityaz") determined the production of
the carbon produced during the photosynthetic activity of the
phytoplankton by means of the oxygen method. This expedition
worked in the northwestern part of the Pacific. The border bet-
ween the boreal and the tropical area goes through this district
at about 400 of north latitude. The perceptible composition of
the plankton is modified in this region to a great extent. North
of 400 of north latitude there are typically boreal species liv-
Card 1/3 ing in the plankton of the surficial layers, the names of some

The Production of Plankton and the Characteristic of the '20-118-5-19/59
Biographic Regions of the Ocean
of them are given here. South of 400 and especially of 35' of
north latitude the plankton contains mainly tropical species.
The amount of the living plankton is highly different from dis-
trict to district, the author here gives numerical data for the
different districts. Towards south the production of carbon de-
creases and in the warm waters of Kurosio the production of
carbon is ten times smaller than in the zone of intensive growth
of plankton. The production of carbon and the amount of the liv-
ing zooplankton on an average in boreal waters is ten times as
high as in tropical waters. The differences are mainly con-
ditioned by the decreased possibility of primary production
(especially by the intermixture of the waters, by the dynamics
of nutrients for the phytoplankton etc.). The decrease of the
amount of living plankton also lowers tho possibilities of
nourishing fishes and thales . The primary production determin-
es the possibilities of nourishment not only for surface layers
but also for the whole depth of the ocean. The borders of pro-
pagation of the different plankton masses are somewhat different
from season to season and from year to year. The primary pro-
duction, the distribution of the amount of the living plankton
Card 2/3 and of the fishes are closely correlated. The results here ob-

The Production of Plankton and the Characteristic of the 20-118-5-19/59
Biographic Regions of the Ocean
tained can additionally be used as follows: The districts of the
ocean with raised concentration of organic matter in the sludge
give evidence of a rich life in the upper layers of the water.
Consequently the possible borders of the distribution of plankto-
phagies among the fishes and whales prevailing in the trade can
be plotted into the soil map. Moreover the things reported here
ought to be of interest for geologists of mineral oil. There are
4 figures and 5 references, 5 of which are Soviet.
ASSOCIATION: Institut okeanologii Akademii nauk SSSR (Institute of oceanog-
raphy- AS USSR)
PRESENTED: October 8, 1957, by S- I. Mironov, Member, Academy of Sciences,
USSR
SUBMITTEDt October 4, 1957
Card 3/3

BOGMOVj, V. G., TARMV, B. A. and FEDMOV., K. H.
The Depths of the Ocean and the Problem of Waste Disposal Therein."
report presented at the Scientific Conference on the Disposal of Radioactive
Wastes, Monaco, 16-21 November 1959.

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BDGOROV. V.G.; MRUYS710H, S.V.; F=SOV, M.V.; UDIRrSE7. G.B.
..
Methods of oceanographic research In the U.S.S.Re Nek. probl.
I rez. okesm. Issl. no.ltl2-16 159. (MIRA 13:2)
(oceanographic research)'

SOV/26-59-1-18/34
AUTHOR: Bogorov, V. G. , CorrexpqpdP4 Memberf AB LWR
TITLE: The Achievements of 8 oviet oceawgrapby (Dostizheniya
sovetakoy okeanologii)
PERIODICAL: Friroda, 1959, Nr 1, pp 43 - 45 (USSR)
ABSTRACT: The author gives a brief survey of recent Soviet
oce Cal research. He enumerates some of the
fields co ed by various marine expeditions in the
Arctic, Pacific and Antarctic Oceans, including deep-
sea water circulation(almost 10 times faster than
that of the surface waters at depths of a few hundred
meters) geographical zonation, deep-sea precipices,
the continental shelf in the Antarctic region, ani-
mal and plant life, and the factors important to
weather forecasts. The research vessels "Vityazl"
and ltObIll played an important part in marine re-
search in the Pacific Ocean. The Vhaling fleet "Sla-
Val' is intensely engaged in plankton research. Its
annual reports will be decisive for the assignment
Card 1/2 of two new Soviet whaling flotillas in the Antarctic

The Achievements of Soviet Oce SOV/26-59-1-18/34
ocean. The study of coastal lines, under the effect
of tbsbuilding and destroying forces of the sea,
yielded important data uecessary for the establish-
ment of ports and harbors. The results will be of
interest not only to the USSR but also to Poland
and Red China. Research stations on drift-ice floes
in the Arctic Ocean gave valuable information on wa-
ter circulation and other conditions. The combined
effort of Soviet oceanogr6W6sl! research has demon-
strated that any layer of the world's oceans can be
of great economic importance. In 1959, the entire
northern part of the Pa6ific Ocean up to American
waters *ill be studied. Complex research will be
conducted in the Indian Ocean. Large research teams
will work on the "Ob" and "Lomonosov" research ves-
sels during their meridional crossing of*the Atlantic
Ocean. There is 1 photo.
ASSOCIATIOW: Institut okeanologii AN SSSR /Moskva (The Institute
of 06euvgivaW of tbe" AS ~ UBM~ Noscov)
Card 24~-

BOGOROV. V.G.
The indivisible nature of-the oceans yest.Hook.un.Ser.biol., pochy.,
geolt, geoge 14 no.4-201-207 '59. (MIRA 4.3:6)
1. Kafedra geografii polyarnykh strau.
(Oceanography)

SOV/10-59-5-15/25
AUTHCR: Bogoroy, V.G. and Dobrovol"skiyq A.D.,
TITLE: Oceanographic Research in North Korea
PERIODICAL: Izvestiya Akademii nauk SGSR, Seriya geograficheskay-a,
1959, Nr 5, PP 101-103 (USSR)
ABSTRACT: The third plenary session of the International Com-
mission on the Fishing Industry, Oceanological and
Limnological Research in the western part of the
Pacific Ocean took place in August 1958 in Pyongyang.
The authors give neither the composition nor the aims
of the Commission, A short description of the organi-
zation of scientific research is given. The study of
the seas is carried out by two scientific research in-
stitutes, the Institute of the Western (Yellow) Sea
in Chosan and the Institute of the Eastern (Japanese)
Sea in Wonsan. The study of the sea is also carried
out by the Central Meteorological Observatory in Pyong-
Card 1/2 yang. All these institutions were orgoaiized with the

Oceanographic Research in North Korea
SOV/10-59-5-15/25
help of the Soviet Union, especially by the Tikhook-
eanskiy Institut rybnogo khozyaystva i ake-Emografii
(The Pacific Ocean Institute of the Fishing Industry
and Oceanography) (TINRO). Soviet text books are also
used in the institutes, namely those by N.N. Zubov,
V.V. Shuleykin, V,A, Saezhinskiy, and G.R. Zhukovskiy
(his book "Oceanography" has already been translated
into Korean).
ASSOCIATION: Institut okeanologii AN SSSR (Institute of Oceano-
logy of the AS USSR)
Card 2/2

BOGOROV, V.G.
I
Depths of the ocean and their life. Geog.v shkole 22 no,5:
41-46 s-o '59- (MIRA 13:2)
(Oceanography)

3 (9)
AUTHOR:
TITLE:
Bogorov, V, G Corresponding Member
The Biological Structure of the Ocean
SOT/20-128-4-51/65
PERIODICALs Doklady Akaaemii nauk SSSR, 1959, Vol 128, Nr 4, pp, 819-822
(USSR)
ABSTRACT: -In a paper with the same title as above L. A, Zenkavich
developed in 1948 the concepts of the symmetry of the
distribution of life along the meridian and the parallels. The
most recent cuoceesful research of the ocean yielded now data
in this field and an enlargement of the concept of the
peculiarities of the biological phenomena in different geographi-
cal zones. This confirmed the theoretical topic of the
quantitative plankton distribution according to the
geographical latitudes (Ref 6). The author used as material
the yield of the ship "Vityaz"' which crossed the central part
of the Pacific in meridional direction from November 1957 till
February 1958 (1740 western longitude and 1720 eastern latitude).
A space of 400 of northern latitude up to 400 southern latitude
was investigated (Ref 4). The following zones are well marked
Card 1/4 for the surface water in the central part of the Pacific:

The Biological Structure of the Ocean SOV/20-128-4-51/65
northern semitropioalp northern trade-wind zonep inter-trade-
wind zone, southern trade-wind zonep and southern semitropical
one. The number of geographical zones is different for the
upper and lower water layers. There are less zones at a greater
depth, and only one tropical zone exists on the bottom.
Conditions favoring life to a different degree are established
in consequence of the special types of interrelations between
the physioalq chemioaly biologicalp and geological processes
characteristic of individual zones. Figure I shows the
interrelations for the pelagic surface layer. This shows that
the largest plankton quantities occur in the northern part of
the northern semitropical zone, in the inter-trade-wind zone,
as well as in the southern part of the southern semitropical
zone. The phosphate quantity is here the highest, too. The
biomass of the pelagic fishes reproduces naturally the variation
character of the plankton biomass. The chain of processes
governed by a certain rule, which take place in the photo-
synthesizing layer influences the distribution of life in the
entire depth of the ocean (Fig 2). The impoverishment of the
plankton at the surface leads to the same phenomenon in the
Card 2/4 depth. Since the deep layers in the semitropical zones are not

The Biological Structure of the Ocean SOV/20-128-4-51/65
only enriched by the sinking of surface waterep but also by
an active importation of plankton, detritus, and other
nutritive substances from the moderate regions of the northern
and southern hemisphere (Refs 1, 5) the curves of the
plankton biomass have a characteristic curved shape. Little
plankton is produced in the tropical zone. The benthos in the
tropics is insignificant since plankton and its remains are
the only direct or indirect source of nourishment of the
animals at the bottom far away from the shore. This was
completely confirmed by the determination of itsbiomass by
Z. A. Filatova, G. M. Belyayev, and 11. G. Vinogradova, (Fig 2).
The development of the chain of interrelations takes a quite
different course in the trade-wind zones. The current caused
by the winds leads to a rise of the waters off the American
coast. This causes many nutritive salts to be transported to
the surfaces Therefore a considerable quantity of plankton is
produced here (Ref 7) andt consequently, the waters are
abounding in fish. Plankton, fish, and birds decrease in the
western direction. Finally the seasonal dif ferenoes in the
plankton quantity are discussed with respect to growing
Card 3A distance from the equator. Figure 3 shows the bluck scheme of

a
The Biological StMtZO of the Ocean SOV/20-128-4-51/65
the biological struature of the Paoifio. There are 3 figures
and 7 references. 6 of which are Soviet.
ASSOCIATION: Institut okeanologii Akademii navk SSSR (Institute of
Ocepmogmphy of the Aoademy of Soienaes,, USSR)
SUBMTED. July 2, 1959
Card 4/4

BDOOROV) V. G.
"Geographic Zonality of the Biologicals Physicals and Chemical Phenomena
and processes in the Ocean"
report to be submitted for the Intl,, Geographical Unions 10th Oepqral Assembly
and 19th Intl. Geographical Congressp Stockholm., Swdden,, 6-13 August 1960.

S/010'/(O/OO0/OO4/0O2/006/a
A053/AO26
AUTHORS., Bogorov, V-G.; Tareyev, B.A.
TITLE: Oceanic Depths and the Problem of Dumping Radioactive Waste
PERIODICAL: Izvestiya Akademii nauk SSSR, seriyakpCgraacheskaya, 1960, No. 4,
PP. 3 - 10
TEXT: The authors refer to the recommendation given by V.G. Bogorov and
Ye.M. Kreps at the II International Conference on the Peaceful Utilization of
Atomic Energy in Geneva in September 1958, to the effect t-hat the dumping of ra-
dioactive waste in depths of the ocean should not be permitted. In this article
the authors furnish new proof in favor of their viewpoint based on the latest
observations made by Soviet and foreign oceanollogists, in particular on the oc-
casion of the Danish expedition on the SS Galatea in 1952 and the Soviet expedi-
tion on the SS Vityazlin 1958. The article compares the 23 deepest depressions
In the Pacific, the Atlantic and the Indian Ocean, in indicating maximum depths
and their location. It also gives information on the prevailing temperatures at
various depths ranging from 0 to 10,000 m In different areas and at differerrit
seasons. These temperatures even at maximum depths are subject to varlatlon3
Card 1/4

,,/oio/00/cx)t),/oo4/oo2/oc)O,/.xx
A053/AO26
Oceanic Depths and the Problem of Dumping Radioactive Waste
which permits to conclude that nowhere the water is Btagnant but constantly on
the move, however slow this movf-ment may be in certain places. The vertical
movement of the water in the depths of the hilippine and T-he Bougainville de-
pressions have been calculated as being 10-~=2/sec or about 30 - 50 m per annu.%
The speed of horizontal movement of ocean water as a rule exceeds by far that cf
vertical movement, particularly In the upper layers. The article refers to in-
vestigations carried out in recent years pertaining to depth circulations, men-
tioning the findings of Doctor Swallow and of Doctor Laughton, The article cites
a number of other phenomena, which all tend to prove the movement of water, re-
sulting in a continuous agitation and mixing process, which creates favorable
conditions to the development of life, even down to the greatest oceanic depths.
During deep-sea trawling of the Vityazyin 1958 in the Pacific, going down to a
depth of 10,700 m, the existence of fauna was revealed even in these ulrraabys-
sal depths, consisting of sponges, worms, mollusca, etc, though in small quanti-
ties, because at a distance of 10 km from the photosynthetizirg layers on",y veiry
little food is brought down. Life in the mass of water is in a state of con&ant
migration. Even plankton covers considerable distances. The migration of ani-
Card 2/4

S/010/60/000/004/002/006/Xx
AO53/A026
Oceanic Depths and the Problem of Dumping Radioactive Waste
mals and biocirculation are a powerful means of transportation of all kinds of
substance including absorbed radioactivity. Harley found that in a district
west of the Bikini Atoll radioactivity of plankton was 470 times greater than
elsewhere in the ocean. Japanese authors state that as a result of radioactive
fallout infected fishes were found near the Marshall Islands, later on near the
Caroline Islands and further north near Taiwan and the Bonin Isles. Fishes
caught within a radius of 3,000 km of the district of Bikini had to be destrKyed
on account of their radioactivity. This district being the spawning place of
tuna and swordfish, it is likely that its contamination by radioactive fall-out
will be of far-reaching consequences in the way of infected tunafish, in which
connection the authors refer to the findings of the Japanese scientists Y. Miya-
ke and Y. Suguira. Interesting in this respect is also the theory developed by
R.H. Ketchum aild T.V. Bowen concerning the physical and biological transfer of
different substances, concluding that biological transfer often exceeds therole
of the physical mixing process. In respect to biocirculation a great deal of
re5earch work remains yet to be done, especially in deep-water circulation, al-
though it is known that big plankton migrates in deep layers (down to 6 km).
Thus radioactive wasle buried in the depth of the ocean, when dissolved willr1se
Card 3/4

S/010/60/000/004/OOP,/006/XX
AO53/AO26
Oceanic Depths and the Problems of Dumping Radioactive Waste
by means of physical as well as biological circulation and eventually endanger
the life of human beings. The theory that the radioactive substances after a
while will be dispersed and in a dissolved state mix with the entire mass of wa-
ter is ill founded. Water currents are localized and the same refers to biocir-
culation'following a certain cycle. The authors agree with H.T. Dunster that
the disposal of radioactive wastes In coastal waters is highly dangerous, and so
is the dumping of such wastes in the depths of the ocean. Further investigation
and research work should clarify in particulari "The behaviour of radioactive
substances in the ocean." - "The accumulation of radioactive substances in marim
organisms and their tissues." - "The age of different layers of water and the
duration of a certain mass of water remaining in a given layer, types and speeds
of mixing processes." - "Speeds of vertical 9-rid horizontal circulations of dif-
ferent layers." - "Biocirculation, daily, seasonal, multiannual'.' - "Geo-chemical
factors influencing distribution of radioactive substances". There are 16 ref-
erences: 9 Soviet, 6 English and I Japanese.
ASSOCIATION: Institut okeanologii AN SSSR (Institute of Oceanology, Academy of
Sciences, USSR)
Card 4/4

BOGORDV, V.G.
- - - - - - --------------------
Oceanographic reoearch in Now Zealand. Biul. Okean. koti. no-5:
42-47 16o. (KTRA 13:10)
(Now Zealand--Oceanographic research )

BOGOROV, V.G.
--
Feeding grounds of fishes and whales in the northwestern part of the
Pacific Ocean. Trudy sov. Ikht. kom. no.10:197 160. (HIM 13:10)
1. Institut okeanologii Akadsmii nauk SSSr.
(Pacific Ocean--Plankton)

BOGO~OV -To.
~_Y!G_q VINWRAWV, M.
Distribution of the biomass of zooplankton in the central
Pacific. Trudy Gi(Irobiol. ob-va 10:208-223 160.
(MIRA 13:9)
(Pacific Ocean--Zooplankton)

Characteristics of geographical mnes in the central nart of the
Pacific Ocean. Trudy Okean kom. 10 no,4:3---7 t60, (I-IM 140)
19 Institut okeanologii a SSSR,
(Pacific Ocean-MELrine biology)

BOGOROV, V.G.; VINOGRADDY, X.Yee
Distribution of zooplanktou in the Kurile-Kamchatka area of the
Facifla Ocean, Trudy Inst, okean, 3W60-84 1600' (MIRL 13110)
(Pacific Ocean--Zooplankton)

,BOGOROV, V.G..- DOBROVOLISKIY A.D.i PETELIN, V.P.; SERGEYEV, I.V.
First expeditions of the "Vitiaz"I under the program of the
Intemational Geophysical Year (cruises 25, 26, and 27). Trudy
Inst.okean. 1+0:3-22 160. (MM 11+:8)
(]Pacific Ocean-Oceanographic research)

'-~QV, V.G.
Geogrg-phical zones In the pelagic region of the central Pacific;
materials of the 26th ermise of "Vitiax". Trudy Inst. okean.
41t8_16 16o. (min 13:9)
(Pacific Ocean)

DOOOROT, T.G.
DivIsion of the ocean into biogeographical regions* Vope
geoge no 48t7l-89 16Q. OMA 13:7)
iftcifio Ocean-Zooplankton)

BOGORDV, Y.G.
Geographical variation of fatness in ocean *Ukton. DOk1. AN SSSR
134 no.6tl441-1442 0 1600 (MIRA 13:10)
11 Institut okeanologii Akademii nauk SSSR. 2. Chlen-korrespondent
AN SSSR,
(Atlantic Ocean-Zooplankton)
(ftoifio Ocean-Zooplankton)

RIO&
52
. j
14V
Na
f:n g t-, 9
at -
jr
r, Rn
f

BOGOROV Veniamin Gr I lah; SHIMOVA, V.P.., red.; NAZAROVA, A.S..,
to . red.
[Distant voyagen of the ffVitiaz'"I Dal,nie plavaniia. na ffVitiaze."
Moskvaj Izd-vo "Zn=ie," 19619 47 p. (Vaeooiuznoo obahchestvo po
rasprootranenilu politicheskikh i nauohrqkh znanii. Ser.12, Geolo-
gii i geografiia,, no*17) (MIRA 14:10)
le Chlen-korrespondent AN SM (for Bogorov).
(Indian Ocean-Moooription and travels
(Pacific Ocean-Desoription and travel

BOGOROV. V.G.
Fridtjof Nansen's life a3~d work. Izv. AN SSSR. Ser. geog.
nd.6:101-.UO N-D 161. (RMA 14:12)
1. Institut okeanologii AN SSSR.
(Namen, Fridtlof , 1861-1930)

BOGOROV, V.G.
Marine research organizations in the Indian Ocean. Okeanologiia
I no.5:937-939 161. MRA 15:3)
(Indian Ocean--Oceanographic research)

DOGOROV, V.G.; BEZRUROV, F.L., prof.
IlVitiaz"' In the Indian Ocean. Priroda 50 no.1c,:8e_irc 'V Ifl.
(YJRA 14: 9)
1. Institut, okeanolouli Ail SSSR (Moskva). 2. Chlen-korrespondent
AN SSSR (for Bagorov),
(Indian Ocean--Oceanographic researeb)

BOGGROV, V. G.
Review Of the *TrudY* of the White Sea Biological Station of
Moscow University, Vol, li "Biology of the White Seam. Zool.
zhur. 42 no.6z967 163. (MMA 16:7)
(White Sea-Marine biology)
4e

BOGOROV, V. 0.
'tiological resources in the tropical oceans"
report, to be submitted for the ftited Natims Cogsterence OA the
AppUcation of goiftee and Tochnoloa for the Benefit of the Lest;
Developed Areas - Oenevap Mtzerland, 4-20 IFeb 63.

BOGOROV, V,G,,, prcx.
Petr Ivanovich Usachev, 1892-1962. Trudy Inst. okean. 71:3-4 163.
(MIRA 16:11)

V,c.
N''KcIal N-vk-ilrev-'7h 1909-a.96/4. Okeanoiogiia 4 164.
(MIRA 1-7:10)

BOGOROV, V.G.
1 -::,.
Productive, 'tegions or the crcan, Trady VNIRO 57.329--332 165.
. I (MBA 18.- 6)

i F.
71
AGGESSIGH NRa Lo5oV628 tJ.'1/0026/65/000/007/OC)53/0056
AUTHOR B V 11, (CorreVonding nember AN SM),
TITLE: Famous investigator of the depths of the seass L, A. Zankevich and his
book "Biology of the Saw vr the SSSR-4
rrAsj, 'n
--3Wffl1i Pri: 0 7~' 196~,1_53-56~
TOPIC TAGS i ~q2po h biological product$ biology research
a This is a ruvierw of the book "Biology of t awarded
ABSTMCT, fie Seas of the SWR"
a Lenin pri.%9) written by the tamous investigator of the ocearns, L. A. ZenIkevich.-5
The author sliccesded in including all the biology of the seas in one volume.
The book., resulting -from almost 40 years of research work, includes the character-
istics of the Baltic, North Atlantic, Caspian, Black, Azov, and North Pacific
I Oceans# It describes the physicogeographical peculiarities, geological history,.
I water and soil chemi3try, the history of the study of the cor.'spos-ition of the flora
and fauna., and th-air origins (especially the quaternary history and role o ~hoe,s
lee
-lora and the biogoography, of " a
-Age). The propagation of the fauna and I fth
am discasard in detailt_ 7he material concerning -the quantitative propagation of F_~
life) for which mmerical data "are given in this article, is of exceptional J

signifitancee The !=Itiplivation of f1sh., invertebratesp olgao,, and sea manmls.*
-van ao the atolimtizution permitting, the greater utilization of the riches Of
as
~the.saas wa discunsed. in dotalL The book contains much general theoretical and
conereve material, and the scientific activities of Zenkovich are acImowledgedt
~His 'apecial achievement lies in the introauction of tho quantitative method Zor
--ti:ld- the regola:-itiOD in th.6 aistribution of organism. ,M tho prG-ductivity
of seas and the dewlopaent of ",be theory md syatc-m of the biological structure
of seas and oceaw. Th!? mrards won by him are listed. Orig. art. has- I phato-
-7aph.
A&SICCIATIC)Ili noni
SUEUMTED: 00
M) R~ SOVI 000
Card
ENGLi 00
OTIER 000
L-

BOGOROV, V.G.
4 --, -1-1 -:""-
Quantitative evaluation of the animal and vegetable population of an
ocean. Dokl. AN SSSR 162 no.5slI81-1183 Je 165. (MIRA 18:7)
I.Institut okeanologii AN SSSR; ahlen-korrespondent AN SSSR.

L 13076.&
ACC NR: APS028916 SOURCE CODE: UR/0020/65/165/003/0686/0689
IAUTHOR: E29 rov, V. G. (Corresponding member AN SSSR); Makstmov, V. N.;
Fedorov, V.D.
ORG: Moscow State University im. M. V. LomIonosov (Moskovskly gosudarstvennyy
universitet)
TITLE:- Selection of an optimum composition of ihe medium for the photosynthesis of
fgreen serous bacteria Chlorobium. thlosulphatophilum using methods of mathematical
planning of experiments
SOURCE: AN MR. Doklady, v. 165, no. 3, 1965, 696-689
ITOPIC TAGS: bacteria, bacteriology, pbotosynthesis,r-491"'eAl'
ABSTRACT: The attainment of a large yield of a given Bacterial culture can be achieved
by the proper selection of Me optimum medium for the type of organisms under study.
Generally, three problems should be solved: 1) select from the totality of n factors only
those the concentration of which significantly affects the yield of the culture; 2) establish
the optimum qualitative relationships among the selected significant and possibly
1/3 UDC: 676,851.222

ACC NR: AP5028916
interacUbg factors; and 3) eliminate surpluses In the concentration of nonessential factors,,,
with opUmum combination of essential components. The optimum composition of the
medium for the Chloroblum thiosulphatophilum bacterin was selected by the method of
random balanve (T. S. Budne, Tdchnometrics, 1, No. 2, 139, 1959). A modified Larsen
medium (H. 1.1irsen, J, iicteriol,- 64, 187, 1952) was used to the base. The optimum
combination of the selected factors was performed following the method of steepest
ascent. After reducing the excess concentrations, the authors obtained an optimum
medium, shmm in Table 1, yielding 3 times as miW bacteria as the Larsen medium.
Table 2. Comparative composition of nutrient media (in mg/1)
Optimum medium, 3D
500. t0DD mw' '~:Ww 2R--,
Larsen medlum
1000, or 3000. M ~:75'
or.

L 13076-6,6
ACC NR: AI~5028916
Orig. art. ban: 2 figures and 4 tables.
SUB CODE: 06 /'SUBM DATE: 24JuIG5 ORIG REF: 004 OTH REP: 003

Boamovo_y~.Oq.
1.4- -.., 4 .. ''. - ~ I
Reviews, Bot. 2h=. 50 no.5025 M3r 165o (Km is tio)
1. Hookovskiy goeudarotvan.W uniTeraitato

BOGOROV, V.G.
Life of the seas of our country. Zen. i vael. I no-4:
2-4 Jl-Ag 165, (MW 18:12)
1. Chlen-korreapondent AN SSSR.

BOGCROV,,~.T.G.; MAKS124OV, r-.N.; PEDCROV, V.D.
Selection of the optimal composition of the medium for photo-
synthetizing groan sulfur bacteria (Chlorobium thiosulphatophilum)
with the help of mathematical planning of the experiment. Dokl.
AN SSSR 165 no.3:686-689 N 165. (MIRA 18.11)
1. Mookovskiy goeudarstyennyy universitet, 2, Chlon-korrespondent
AN SSSR (for Bogorov).

NI'm Ap6ol4285 (N) SOURCE CODE: UR/0213/66/oo6/002/0314/0325
AUTHOR: B gorov, V. G.; B Vinogj:adov. M. Y6.
~ logo,-
ORG: Institute of Geology and Development of Mineral Fuels (Inatitut-geologii i
razrabotYl gopyuchikh iskopayenWkh); Institute of Oceanology, AN SSSR (Institut
okeanologii AN SSSR)
TITLE: Biochemistry of ocean plankton. Distribution of certain chemical componenti
of plankton in the Indian Ocean
SOURCE: Okeanologiya, v. 6, no. 2, 1966, 314-325
TOPIC TAGS: calcium carbonate, carbon,-,A-. 13 FA
Lvoli-rFR',
ABSTRACT: The material for this study was collected by the research vessel "Vityaz
during the 31st cruise in the Indian Ocean in October 1959 and April 196o. An
0-100 m layer of the ocean floor was sampled. The samples were dried without fixing
Calcium carbonate, organic carbon, andlipide contents were determined. The organic
carbon content of the plankton investigated averages 29.9% (ranging from 24.2 to
35.6%) of the dry weight. The lowest plankton carbon content was observed in areas
of intensive upwelling where an essential part of the total biomass is composed of
phytoplankton (diatoms). Because of the constant relative amount of organic carbon
in plankton, its absolute distribution in the upper 100-m layer generally follows
rather closely the distribution pattern of the total plankton biomass. *The lipide
fraction content ranges from 6.4 to 13.6%, averaging 9.4% of the dry weight. Plankto
Card 1/2 UDC: 55o.42:517/475(267)

ACC NRz
(5 ,
is especially rich in lipide where it has maximum concentration. A high correlation
between the amount of lipide in plankton and the depth of the upper boundary of the
depth of the upper boundary of the thermocline was found. A simil*_rly high correla-
tion exists between the lipide~ content of the plankton and the temperature at the
depth of 100 m. The data obtained lead to the conclusion that an increase or decrease
in the lipide content of 'plankton is closely connected with environmental conditions.
The distribution pattern of absolute'amounts of lipide follows the general biomass
distribution pattern of plankton. The calcium carbo~dte content averages 11.7%
(ranging from 4.8 to 21%) of the dry weight. Comparison of the carbonate content
of plankton with the distribution of pteropods and globogerins shows that, apparently
the calcium carbonate content of tropical plankton is determined, firat of all , by
the amount of globigernia. Orig. art. has: 4 figures and 1 table. (Based on :
authors' abstract.] [NT]
SUB CODE: 08, U/ SUBM DATE: 24Dec65/ ORIG REF: 022/ OTH REF: 008

L
ACC NR, AP 018143 SOURC, CODE: UR/0020/65A62/005/1181/1183
AUTHOR.
(Corresponding rember AN 5,95R)
ORG: Institute of Oceanology, AN SSSR (Inatitut okeanologii AN &SSR)
TITLE: Quantitative evaluation of the animl and plant population of the ocean
SOURCE: AN SSSR. Doklady, v. 162P no. 5, 1965, 1181-1183
TOPIC TAGS: biology, oceanography, primitive plant, protozoology, microbiology
ABSTRACT: !The pelagic zone of the oceans of the world may be di-
vided Into three groups of regions: highly productive - with a
[plankton biomass In the 0-100 meter layer higher than 100 milli-
!grams per eublo, meter; 'medium-productive - with a plankton blo-
.mass In the 0-100 meter layer higher than 50 milligrams per cubic
,meter; iow-productive - with a biomass less than 50 milliGrams
.per cubic meter. Considering new data, the author estimates the
Itotal mass of phytoplankton In the world's oceans at 1-7 billion
.tons and the total mass of zooplankton (without the microplankton)
tat 21.5 billion tons. A tentative estimate of the mass of animal
mieroplankton brings this value up to about 23 billion tons.
lPhytoplankton production Is e'stimated at 550 billion tons per y-ear:,
!production of.meso- and macroplankton Is estimated at 53 billion
-tons per year for the world's oceans. Since the bulk of the plant
Xass of the ocean consists of single-celled algaeg which multiply
Card 1/2

ACC NRs AP601814)
rapidly, their annual production Is more than 300 times as great
~as their biomass. This enormous productivity of the phytoplankton,
makes possible the development of enormous amounts of zooplanktonj
and ultimately fish, squid, whales, and other commercially impor-
tant animals, The total plant production is ten times as great
as the total animal production. The Interrelationships among the
,various layers of water and the organisms that Inhabit them and
the role of procesues of vertical migration-arQ discussed. Orig. art. has:
1 table. (JPRS]
SUB OODE., . 060 08 / SUBM DATE: 26Mar65 ORiG REF.- 918 / ON REF-. 002

ACC NR, A1,7008880 SOURCE CODE: UR/CO30/66/000/009/0101~/0107
AUTHOR: Bogorov, V. G. (Corresponding member AN SSSR)
OIRG' : none
TITLE: Primary production of the ocean and its use
SOURCE: IN SSSR. Vestnik, no. 9, 1966, 104-107
TOPIC TAGS: oceanography, biology
.SUB CODE: 08, 06
ADSTRACT: 7he article cited below is a brief but fact-filled generaliza-
tion of available data on the primary,production of the occon. For
examples the following information is given: In the ocean, in contrast
-to the lands the biomass of anim alL-- is almost 20 t1rpns. groator than the
vegetable masse This is possible because the ratio'of the annual pro-
duction. to the biolaads of one-celled plankton algae is renewed every day*
Regions.with a high productivity of zooplankton (above 100 mg/m,3 of bio-
mass in the surfaco'100-m layer) occupy 17% of the area of the world
oceans regions of intermediate productivity (from 50 to 100 mg/0) -
-1 20%, low produotivity (from 25 to 50 ma/m,3) --29%# impoverished (less
1-than 25 mg/0) - 34%. The mass of organisms is distributod nonuniformly-
Card
472.(26
4

'.ACC NRi ANObBOBO
vertically, Phytoplankton$ due to rapid absorption of light by the water,,
lives primarily in the upper 100-m-layere About 65% of the zooplankton
is in-tho layer from the surface-to a depth of 500 m. On the continental
shelfp-at depths from 0 to 200 =j the biomass of bonthos on the average
is 200 &/m2p from 200 to 3.,000 m - 20 g/m2s and at depths greater than
3,,000 m less than 0o2 g/m2o Depths of 0-200 m constitute only 7.6,cQ'
of the area of the world ocean, but 82s6% of all the b;iomass of bentho3.'
found there. Depths of 200-3,000 m occupy 15.4% of the area and
,account'for 16.6% of the total biomass of bentho3. Vast areas of the
ocean with depths greater than 3tOOO m (77%) havo only, 0.8% of the total
biomass of benthos of the world ocean. Orig. art. has;.-' 2 tables. IJMS: 38,6771
Card 1,21?

ACC NR. AP7013694 SOURCE CODE: UR/0213/66/006/006/1055/!058
AUTHOR: Log
_,,orov, V..G.&I.Rass, To So
ORG: Institute of Oceanology, Ar SSSR (Institut okennologil AN SSSR)
TITLE: Dependence of the distribution of fish on the distribution of
productive redons, of plankton In the Indian Ocean
SOURCE: Okqanologlya, v. 6, no. 6, 19669 1055-1058
TOPIC TAGS: plankton, oceanographic research facility, animal physiology,
research ship, biologic ecology
SUB CODE: 06
ABSTRACT: Three voyages of the research vessel "Vity4z"1 were made in the
Indian Ocean by the Institute-of Oceanology In 1960-1963. Plankton and
Ichtyological studies over vast areas of this ocean were made during the winter
monsoon (31st and 33d voyages) and during the sumor monsoon (35th voyago).'
The data show that the Indian Ocean north of 200S can be divided into several
areas differing In plankton productivity (biomass of the s3rface layer plankton
in m
g/m3)! 1) highly productive areas (moro than 250 mg/m off the Gulf
of Aden, at tho Seychelles, sou5h of Java, at Christmas Island; 2) rich
productive areas (100 -250 mg/m, middle and northern Arabian Sea, Comores,
Card_ 1/2 ~13 -? - ~2 z Y X~

- - --------
ACC NRt M03304
off northeastern Africa, between the Seychelles and Maled'1ve Islands, a
latitudinal belt south of the equatorl off the southern coast of Java; 3)
S/m3) bordering the rich productive
moderately productive areas (50-99 n
re-Ions, which are far more extensive o the west of 8009 than to the.east;
4)0areas of low production (25-49 mg/ms), characteristic mostly of the
eastern Rarts of the Indian Ocean from 800E to 1000E; 5) a nonproductive
(25 mzlm-3) re,-Ion extending through a vast area of the central Indian Ocean
to the south of 18-200S, excluding only the area of the Vest Australian
Current. A striking characteristic of the Indian Ocean Is the far greater
productivity of its western.part than Its eastern part. In the eastern part
there is high productivity only between Java and.northwestern Australia.
Quantities of large pelagic predator fish such as tuna, dolphins, spearfish
and swordfish apparently are considerable. ibis is'confirmed by direct visual
observations of schools of fish, the abundance of larval fish of the mentioned
groups.and the development of pelagic fisheries over the last decade. The
distribution of larval fish naturally Is closely related to the distribution
-of productive plankton areas*. Sthools of adult fish also are encountered
mostly.in these areasp cept for the Mgration periods, when they cross areas
of low productivity. JPRS: 3999t.;7
cord 2/2

ACC NRs AP7013695 SOURCC CODEt UR/0213/66/0061006r-*10931'109
AUTHOM 11onin, A. S.; Bogorov, V. G.
ORGs none
TITLE: Ttientleth anniversary of the Institute of Oceanology of the academy
of sciences U3SR
SOURCEt Okeanologlya, v. 6, not 6, 1966, 1093-1099
IMPIC TAM oceanography, oceanographic research facility$ oceanographic
personnel
SUB CODE: 08
ABSTRACT:
Me article cited below is an extensive summarizat~ion of'the
;work of the Institute of Oceanology during the last twenty ye=-s, the
most important personalities vjho havo participated in its activities,-
.a progressive year-by-year acevant of the broadening of its field of
!operations, its cooperation with other a,,,?,,encies0 its participation in
!international programss its expeditions and research vessels and the
outstanding advances it has contributed in the'Xield of oceanoloMr.
.of particular interest is 'a listing of all the institute's expeditions.,
their, es, ~he!-Yessels.useds -~he i-egions involved and the n=-e of
Card OM16:551#46-

ACC I"- AP7013695
!th*e chlef'ok tile e'xpeditione The specialists of the institute have
produced more than 2.,400 articles and 60 books.' Th6 transact-10.qs of
;the institute now constitute 80 volumes. Its associates have defended
10 doctoral dissertations and 76 candidatets dissertations. 7he present
director is Andrey Sergeyevich Monin. There are two branches -- *.a
Pacific Ocean Divisiong in Vladivostoks and the Kalin.,:.-grad Division,
in the city of the same name, both founded in ig6l. Me inetitute has,
a new Laboratory in Moscow, has racentli obtained the 6,800-ton reseweli.
'vessel "Akademik KurchatovIlp and is scheduled to receive 'a number of
iraaller, research vessels in the.comi= year's*., OrIgs art. hastI table.
CJPR--:
7..
2/2-

ACC NRt AR7004035 SOURCE CODE: UR/0081/66/000/022/GO20/GO20
AUTHOR.; Bogova, L. V.
TITLE: Phase and chemioal analysis of zirconium diboride
SOURCE: Ref. zh. Xhimiya, Part I, Abe, 22GI38
REF SOURCE: Tr. Wes. in-ta nauchno-Iseled. I proyektn. rabot ogneuporn.
prom-sti, vyp. 37, 1965, 164-178
TOPIC TAGS: zirconium, phase analysis, zirconium analysis, zirconium
diboride
ABSTRACT: The results are described of the determination Of Zr02, B4C,
ZrSi04, metallic Zr, S102, B203, B, Al, Ca, Mg, Fe, TiB2. C, and ZrB2,
during the phase analysis of zircontum diboride. The analyzed components are
separated by treating the samples with various acids and acid mixtures (HN03,
H2S04, H2S04+HF) and fusion with K2S2O7 at this point, ZrSt04 is separated
from B4C. Various fortpe of Zr and Ca, Mg, and Al can also be determined by
titration with a complexone III solution. Fre,-) B and Its compounds B2013, B4C,
following separation from other components and conversion into H3BO3,, are
g~tgrmined by titration with NaOH solution in the presence of mannite. Fe and

NRI
AR7004035
Ti are determined photometrically MOST 2642-60), while free C is determined
by the Wedeking method (Wedekind. Chem. Zeitung, 1907, 31, 654). A. Zozulva.
(Translation of abstract), [AM]
SUB OODE: 07/

k_k22L"6 EWP(k)/9q(m)/&P(w)/EWP(v) IjP(c) EON
ACC NR& AR6006201 SOURCE COD93 UR/0124/65/000/010/BO52/BO52
AUTHOR, Bogoryad, 1. B.
B
TITLE: Variation methods to the problem of the motion of a thin-walled hollow beam
partly filled with fluid in a lisitlasSfluid
SOURCE: Ref. th. Makhanika, Abn. 10B368
REF SOURM Dokl. 3-1 Sibirsk. konferentaii po matem.i makhan., 1964. Tomsk, Tomaki
un-to 1964, 289-291
TOPIC TAGS: thin walled beam', Ruler equation, functional oquation.'sItaA ~~v-A
ABSTRACT: The summary of a paper. A linVF problem of lateral oscillations of a
#, In a limitless ideal fluid is studied.
thin-walled beam partly filled with_�Lui
problem Is formulated and the functional, for which the Euler's formulas coincide wi
the equations of this problem are given, The problem of self oscillations is
discussed, The problem is solved using the Ritz method. It also is stated that
results of the calculations are given in this paper, As At Petrov,
SUB CODEs ?.q,12/ SUBM DATE-s none
Card

43324
B/040/62/026/006/012/015
D234/D308
AUTHOR; Bogoryady I&B, (Tomsk)
TITLE: Solution of the problem of oscillation of a liquid par-
tially filling a cavity, by the variational method
PERIODICAL: Prikladnaya matemat,ika i mekhanika, v. 26, no. 6, 1962j
1122 - 1127
TEXT: The method makes it possible to obtain any degree of appro-
ximation for a cavity of any form* The displacement potential of
the boundary problem is represented as
CD
U(x' Y, zi t) pn(t)4S1d(X# Y# 00 (1-5)
n=1
The problem reduces to
%At. dQ - ~~ T6 ~~ do - ~j t6
0V do 1= 0 (1-9)
where Q is the volume occupied by the liquid, S is the wet surface
Card 1/2

8/040/62/026/006/012/015
Solution of the problem of ... D234/D308
and E the free surfacep Ritz' method'is applied and the system of
equations for the k-th approximation of the n-th eigenfunction is
k
YJ (oil - Obij) C, - 0 k)
(1.12).
where (1-13)
The method is applied to a spherical cavity, numerical results are
given, with the conclusions: 1) Equivalent pendulum is a good appro-
ximation to the oscillatine liquid for dimensionless depthsl =
Z= h/R0-z 0.1. 2) For sufficiently accu rate (up to I %) determina-
tion of the first natural frequency one should take 3-4 terms in
the expansion in the case of small relative depths and 5-6 terms in
the case of large relative depths. The results agree with experi-
mental data. The author thanks Z.M. Polyakova and B.I, Rabinovich.
There are 7 figures'.
SUBMITTED; March 26, 1962
Card 2/2

Rumania
ivo' it-IM. t RZKhiM,j, 14-0, 5 1960s NO#
A11111M I
_1~9'L
IN.- T. I Not
TITLE l The Application of Hydraulic Cyclones in the
Treatment of Coal-Washing Effluentfi
G?,jG. PUB, I Ifidrotehnica, 4, No 2, 61-62 (1959)
The tests were made in a low-pressure hydraulic
cyclone with the followingr characteristics: diam-
eter 500 mm, height of cylindrical Dart 220 irm,
height of conic section 580 ram, dia-meter of feed
pi-Pe 50 mm, diameter of discharge pipe 65 1,1M. It
is shown that optimum operating results are ob-
tained at a water consumption rate of 45 14 0/hr
anda pressure of 0.5 atm. Under these conditions
2.5 0 of sludge are discharged per hr; the sludge
contains ?90 gms qf solids per liter. Particlea
MRDI 112 225

c Rumania
CAMMY I
ABS. JOUR. t RMiinvt No* 5 1960,9 Woo 18315
t
I
T*.~:'IU
CRIc". PUB4
ABSTRACT I of 0.4 raa diaraeter are retained izi the water.
Ya. MaT.Iis
212

ro~csp GTH
Extension of mieumatic transportation to the match industry. P.425
IIPJMTF,IA ISITMIMUI (Asociatia Stiintifica a Iginerilor si Tehnicienilor
din Rominia si Vdnisterul Industriei Iemnului, Bucuresti, Rumania
Vol-81 no-11, lbv 1959
~bnthly Ust of East European Accessions (ESAI) LCI Vol. 9, no 2, Feb. 1960
uncl.

BCGOS~ GH.
-:-L:7-~'
Extension of pneumatic transportation to the match industry. p. 421.
INDUi'IHIA LIWLUI. (Oasociatia Stiinifica a Inginerilor se Tahnicienilor
din Rominia so Yintsterul Industriei MrAnlui) Bucuresti, Rumania.
Vol. 8, No. 11, Nov. 1959.
Monthly List of East lwopean Accessions (EKAI) LC, Vol. 9, No. 2, Feb. 1960.
Uncl.

BOOCS * K.F. (Rumynsksvi Narodnaya Respublika, g. Iksi)
I
"Handbook for the pipe fitter* by [kftnd.te)chn muk] M 14. Sapozhnikov.
Rbviewed by K.F.Bogos. Vod. i san.tekh. no.M59 N 191- (NIM 15:6)
(pipe fitting) (Sapozhnikov., ~.14.)

GICOW, Anna; BOGOSAVLTIVIC, Hal-ina; MAGLIMICZ, Maria
Several problems on the clinical course & treatment of purulent
meningitis. Polski tygod. lek. 14 n0.12:534-539 23 Mar 59.
1. Z Hiejskiego Sspitala ZeJmznego nr 3 w Warazawis; ordynator
oddzialu, ueuroinfakajit dr mod. Damts, IWmszewiez DeLmeowa, dy-
rek-tor.e'%pitala: doe. dr mad. Anisla Marks-7;akrzewska. Adrest
Warnsawa, ul, Sienna 60 Hiejaki Swpital Za)mzrq nr 3.
(M)WITS, in inf. & child
diag. & ther. of purulent meningitis (Pol))

LUWZNICZ-DANCOWA, Danuta; WROBLEWSKA, Monika;_K - 7- -
05
DOBROWOLSKk, Halixa; TAYSCH, Zofia; WROBLEWSKA,-Zofia
Role of extoroviruses in aseptic cerebrospinal meningitis in.
children. Polski, tygod. lek, 16 10-4081524-1529 2 0 161.
1. Z.Mi*jakiego Sapitala Zakazaego Nr 3 w Warazawio; dy-r.: do*.
Marks-Zakrzow8ka, ordynator oddzialu neuroinfekoji; dr DLuuta
Lukazzwies-Dansowa i z Paustwowego Zakladu Higiony v Warasawie;
dyr.s prof. dr med. F. Przesnyeki.
(ENCEPHALITIS virol) (VIRUS DISFASES in inf & child)

BOGOSAVWEVIC, M.
Continual proces-es in the chemical industry. p. 565,
TEHNIKA (Savez inzenjera i techicara Jagoslavije) Beograd.
Vol. 11, no. 4, 1956
SOURCE: East Europe Accession List (EEAL),
Library of Congress, Vol. 5, no. 11, Nov. 1956

0 6 5 /Y' VL 7-r- V
YUGOSIAVIA/Chemical TechnoloGy, Chemical Products and Moir Appli- H-15
cation. Industrial Otgahic Synthesis
Abs Jour Ref Zhur - Khin., No 24, 1958, No 82562
Author -
Inst 110, ~aavi~16vic
Title Review of Methods for Manufacturing Dinitro-o-Cresole by
Sulfonation and a Possibility of its Obtninnont by the
Direct Nitration of 3-Crosole with the Use of Sulf.-nation
Mixtures I.
Orig Pub : Tehnika, 1957, 12, No 11; Hem. ind. ii, no 11, 165-169
Abstrict : The presently used nothod. for obtaining dinitro-o-cresole W
of 86-860 melting point, consists in the action of H2S04
on o-crosolo (II) and of dilute HN03 on the obtained sul-
focresole (III) thant sulfo-groups in the orto- and para-
positions. Of the moat i,portant factors iffecting sulfo-nation
(S), are: temperature, duration of the reaction, and the
weight ratio of H2S04: II which usually aDiistitutes 1.2:
1.6. In order to prevent oxidation of II during S,
Card 1/3

YUC-03UNIA/Cheuical Technolo~57. Chemical Products and Their Appli- IT-15
cation. Industrial OrLpnic Synthesis
.,',bs Jour Ref Zhur Min.) Ho 24., 1958., No 82562
normally 70% H2SO4 (Usually 93%) is being eriployed. The
optimum temperature of S is 90-1001. :m excess Of U2904
causes formation of disulfocresole,, that docroasas the
yield of I durin.3 the nitration phase (which is normally
conducted in tvro stops). Methods of coiz,.ercial production
of I in different countries are also presented. L11 of these
methods have the following characteristic features: 1) con-
centrated H SD4 is opployod in S; 2) after S, the reacting
medium is Muted so that the nitration in conducted with
uiniuuLi heating; when 55-6o% HNo is eriployed, it is di-
luted with water Is uLiployed,, no water is
,, when 25% HNO
added; 3) in the production o IY U-804 and HN03 are used
separately, and not as a mixt 8; 41 spent acid (S,',) con-
tains H2S041 which cannot be used in S, and considerable
quantity of HNO * 5) tomporature of Ch is 80-900 and the
nixture is hi;,3h~; oxidizino. Analyses of the existing
Card 2/3
54

YUGOSLMA/Chemical Thchnology. Chemical Products and Their Appli- H-15
cation. Industrial Organic Synthesis
Abs Jour Rof Zhur - Xhim., No 24., 19581 tio 82562
methods indicate that it is theoretically possible to ob-
tain I by the direct two-stago nitration of II, utilizini,,
a nitratin-3 mixture (W). On the baiis of calculations
the author offers t1he following composition of a nono-ly,
(exprssed in nols per mol of II): 1-H2SO41 1-11HO-.7-,* 36-H20;
composition of EM: 1-H2S04., 37 - H20- For the d-101:
I - H2 S04, 1.8-HN03, 37-H20; composition of S:,,: s - H2904,
o.4 - 'U'03o 37 - H20. -- Z. Rachinskiy
Card 3/3

COUNTRY Yugoslavia H-15
`0 A TW 0P_','
ADS. JOUR. iZl[him. !~o. 21 195), 1~00 75661

B 0 L? 0.- a a'. C
P
M
~
_n
37~ v
A Survey of Methadr. for the Production of Dinitrc
-o-CreFol by Sulfonation. [sic) and the Possibil-,
ity of It8 Production by the Direct Nitration oi
OiIG. U 13. Tehnika, 12, No 12, 95?; Hem Ind, 11, iio 12, 194-
187 (1957)
A critical aralysis of methods used -in the pro-
ducti *on of dinitro-o-cresol (I) shows the fess-
ibility- of the direct nitration, carried out
in two waysi (a) the single step nitration of
o-cresol (II) to I and (b) the multistage nitra-
tion via mononitro-II to 1. 100 gms of a mix-
ture of 1~ $04 , HN(~ , and water (14 ; 2 : 84)
is poured into the reactor and heated to 75* witt
the continuous addition for 1 hr of 50 gms H
and 7?5 me of a mixture containing 15.12% H2GOk
0.4RD: 1/3. o-Cresol with a Mixture of Sulfuric and Nitric
Acids. II.

Yugoslavia
CAT,~-GOPY
JOUR. RZKh3aa., No. 21 1959, INT o 75664
ABS
.
AUTAOR
RIST.
T ITL
011~ Ut U 10 .
A 5S) T R A 0 T 11-04% RNC~, and ?3.84% water. The reaction pro-
ceeds at ?50i at the completion of the reaction
the product mixture is heated to 850 for 30 min.
The I obtained has an mp of 82.85*, yield 74%.
This product is charged into two reactors con-
nected in series and 50 gma 11 and 1,094 gms of
a mixture of 13% H2SO4, 8% IINO), and 79% water
are added at ?5* to the first reactor each hr;
from the second reactor, which is maintained at
85', 1 is withdrawn, MP 73*, yield 75%. The
CA:ID: 2/3
208

BOGOSAVLIEV'rC,, Riodrag, dApl. inz.; MISMANOVIC, dipi. Inz.
Dynamic cnaracterl6tics -" the reactor for onitrati(M.
Autoinatike 5 no.4082-2E7 164.
1. Faculty of Technology, Novi Sad (for Bogosav.1jevic).
2. faculty of Technology, Holgrado (for Krt;manovisli.

SHIFULIN, A.P., inzh. (Kharikov); BQG , inzh. (Kharlkov)
Standardized station relay blocking system. Zhel. dor. transp. 46
no.8:7,r-76 Ag 164. (KM 17:11)
i 1,
1. Stantsiya Kharlkov-Balashovskiy (for Bogcslavets).
I ,