SCIENTIFIC ABSTRACT KOSHKINA, T.V. - KOSHMAN, M.M.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000825110018-5
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 14, 2000
• Sequence Number: 18
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

KOSHKINAY T.V.; XHALANSKIYj A.S.
Age-related variations In the skull and an analysis of the age
composition of populations of the Novmgian lemning (fei=Lw lemmus).
Biul. MOIP. Otd. biol.-66 n0,20-14 Mr-Ap '(A. (MM 14W
(KOLA PENINSULA-LEMMINGS) kBKULL)

KOSHKINA, T.V.
Recent data on the fooi of the IfOrVegian le=ung (Lemmus lemms).
Biul. MOIP. Otd. biol. 66 no.6%15-32 N-D 161. (ITIRL 14:12)
(KOLVITSA VALLEY-IMMINGS)
(ANIMALS, FOOD MBITS'OF)

KOSHKINAJ. T.V.; KHALANSKIY, A.S.
Reproduction of the lemming Lew.,ja lemmus L. on the Kola Peninsula.
Zool. zhur. 41 no.41604--615 AP 162. - (FdRA 15:4)
1. Natural Reserve of Kandalaksha.
(Kola Peninsula-Lemmings)

KOSHKINA, T.V.
Migration of the Norwegian leming (Lemmus lemmus). Zool. zhur.
41 no.121l859-1871+ D 162. (KRA 16:3)
1. State Game Presdrve of Kandalaksha.
(Murmansk Province--Lemmings) (Animal migration)

rl~ll~ To"l-0
r, - .~ ~ -,r-, 6firiol Ly ar-A it7 ti I yrA r, ~, an(; 7! '-,r. scnirollLng Vne ab-~xA ar) ---
m,lf I~c-i red-bac-icudl betle- -Bit-.1 *M0.Tlr-.0t.d.b!cl. 70 rC*195--:i9 i a-.
I * ~:
G.'s (MIRA 13:6),

BUKHAROV, P.S.; FERTMAN, V.G.
Using the polarography method for determining heavy metals in
wines. Metod.issl.v vin. no.ls2-15 162. (MIM 1616)
(Wine and wine making--Analysis) (Polarography)
(Metal"nalysis)

7 trii er "r-lons r,:-, r j, cl-1.
for t'he 'DE-rcc 0i,
Jn:-Lrlr.--Drc :Ile-:

KOSHKINA, Te.F.
Procurement, 'pi"e'servation and use of water-plants for academic
purposes. Biol. v shkolo no.3:87-88 My-Je 163. (MIRA 16slO)
1. Michurinskiy pedagogicheskiy institut.

VODTAKOV, L.T.; XQ-5 40._YP..3'
Water softening with catioultes prepared from Pliocen and
Hauterivian clays. Trudy XMI no.16:77-84 '51 [Publ. '521.
(MIRA 12'.12)
(Water--Softening), (Base-exchanging compbunds)

KAMAY, Gilim;.KOSHKIRA, Ye.S.
Nitro- and chloro-derivatives of triphanyl phosphite atd triphonyl
phosphate. Trudy KKHTI no.17:11-20 152 [publ. 153]. (MIRA 12:11)
(Phenyl phosphate) (Phenyl phosphite)

KOSHK-BA Ye. S.
USSR/Chemistry - '?.Water Treatment FD 179
Card 1/1
Author : Vodyakov, L. T.j.andloshkina, Ye. S.
Title : Softening of water with cationites based on Pliocene and Hauterivian
clays'.
Periodical : Khifa.-prom. 3, 53-54 (181-182), April-May 1951,
Abstract Deomonstrated that it is possible to prepare artificial cationites from,
Pliocene and Hauterivian claysi and that these cat4onites can be regener-
ated with sodium chloride' after treatment of water. Data are listed in
I ar-'a pended.
3 t0les. 2 USSR references,. e ,p

KOSHKO, 1~1- iFILATOV, fi,S.v, SURYGIA; A..P.
- ........ --,- -- .
Air drtl 'I ~~ng f or !~eislrjlc, p;-C.".9pec", '-n? ~ Ra zv-~d, . I. oVr- , %; ~il .
?C, no.11:54~59 N 164. 11.1 RA 18! 4 )
1. Ploskcvskiy ordena Trudoirogc Krqsr,,,-jo Zna;nnuni in-.0 -~ttl,,
noftekIrr-inichoskoV i gazovo,.., pvcviyEhlc-ni.:)s,,d im.,uni. nikafion.---ka
J.M.Gubkina.

MALIOVANIY, I. [Mallovanvi, I.] (selo Gnilitsy, Chernigovskoy oblasti);
STMINIKOV, Volodya (g.Aleksandriya, Kirovograako'y oblati);
KOS=HLAtX- G. oshlak, &I (celo MalaNekhvoroshcha, Poltavskoy
--
obluti)
The page Of OUr Teaders. ZnELn.ta pratsia no-7:23 Jl '6o.
(MIRA 13:8)
(Cabinetwork)

KOSNLOKo~ &.R.
BUTOV,A.S., kandidat tokhnichemkikh imuk; ROSHCHUPKIN,D.V., kandidat
takhnichookikh nauk; KOB[IIAKOV,G.A., inzhener.
Increasing the efficiency of hodraulic machinery. Makh. stroi.
12 no-5:15-20 Kv '55. (MLRA 8:6)
(Itrdraulto maclinery)

Hosl-Llakov, G. A. "The of f ect of systems of operation a
dredge on the productivity of floating earth-drediging
scowc used in transportation constructim." Min Trans-
port- Ea chino Building USSR. All-Union Sci Res Inst of
Transport-44achine BujIding. Eosccra, 1956. (Disserta-
tion for the Degree of Candidate in Technical Science)
SO: Knizhndya letopis', 140. 27, 19.56. lioscow. Pages 0,4-109; '111.

5
BUTOV, A.S., kandidat tekhnicheekikh nauk; ROSHCHUPKIN, D.V., kandidat tekhni-
cheskikh nauk; KO.SHT-AKOV, G.A., kandidat tekhnichookikh nauk.
Increasing the productivityof hydraulic n1pelinedredges in building
railroad roadbeds. Trudy TSNII5 no.22t1907215 '56. (mLRA 1o:6)
(Railroads--garthvork) (Dredging-I
1%

KOSHIAKOvj, L.S., inzh.
Experience in using automatic magnetic gas analyzers. Elek.sta.
34 no.2284 F 163. (MIRA 1634)
(Gases-Analysis)

KOSHLAXOV, M.V.; LIPOVSKIY: 1.S.
New pressure gas-tunk equippel truck ZIS-156A. Avt.trukt.prom. no.8:22a-b
Ag '5 3. 04T-'RA 6:13 )
(Motor trucks)

SOURCE COM UR/O /65/001/004/0471/0473,
n6015
AUTHOR: Koshlakoa Romanova L. V.; Fallk, Ye. Yu. Chernomorg~~JS.~A.
-Union Scientific Research Institute of Fats (Vsesoyuz-W nauchno-
ORG. All
.1isoledovatellskiy institut zhirov)
TITIE: Effect of gamma irrarl I ation on the storage of sunflower seeds
-473
SOURCE: Prikladnaya biokhimiya i.mikrobi,o ogiya, v. 1, no. -4, 1965, 471
TOPIC TAGS: fungus, radiation plant effect, bacteria, gamma irradiation
MTRACT: The results-of the-experiments repozted showed that 300.,000 r was
!the minimum lethal dose for molds-. Howevers despite the sharp decrease in
!quantity of molds and bacterid-on the seeds after exposure, the number of
imicroorganisms increased markedly an moist seeds stored under nonsterile
:conditions, although it was less than in the control samples. Seed respira-
~tion immediately after exposure was more intense than in the control. With
;an increase in the duration of storage and a moisture content of 15-20%j the
intensity of respiration and acid number of oil in the seeds increased along
!with the number of microorganisms on the seeds. In these respects the ir-
Iradiated aeods we're not'appreciably superior to nonirradiated seeds.
The content :ompounds. also rose after irradiation. Exposure,
of peroxide
of sunflower seeds*moistened about 13% to 300AD0 and l..OOO.,OOO r increased.
:the peroxide number 5-7 fold. After 3 days of storage respiration of the
Arradiated seeds was-much'lese intense than that of the control. However
i~~ Coed 1/2 UDC: 633.854.78+665-347.8

KOBELAKOVA, L. V., and AUMATOV, A. ~.
"The Investigation of Elastic Properties of Too-Dimensional Molecular
Crystals of Fat Acide F d on Netal Surface.
report presented at the Conf. on Mechanical Properties of Non-Metallic SolidB.
Leningrad, UBM, 19-26 may 1958.
Inst. of Machine-tools and Instruments. Moscow.

Koshlnkova,__&. V., and Akhmatov, A. S.
"On the 1-1--asurement of the Llvstic Constants of Boundz~ry-Lubri-
cation Layers,, cc - ! -- Lf
Sukhoye i -ranichnove treniye. Friktsionny c m--tcrialy (Dry End
BoundE~'~ry ~rlction. Friction !-Iaterials~ 1joscovI., Iz-J-vo A-it'
SSSH, 19b0. 302 p. Errata slip inserted. 3,500 copies printed.
(Series: Its: Trudy? V. ~)
Sponsoring Ag~%ncy: Al'ademiya nai;-k ~360'-H. Institut me,-Ininovedeniyn.
r
nesp. EL.: I. V. Kra'-ellskiy, Doctor of Technicz;1 Z)ciences,
FrofeL.-sor; Ed. of Publishing house: K. 1. Grigora3h; tech.
Ed.: S. G. Tikhomirova.
The collection published by the Institut nas'1-1innvC("C-11iya,
p
Al-tl S63R (Institute of ~)cience of Machines Academy of' ociences
USSR) contains paners presented ~,.t the lIi Vsesoyuzw~ya konferent-
himl-h (Third "ll-Union Conference
siya Do treniyu i i,-.nosu v mas. 1~
on Friction and Wear in i--lachines, Apri` `)-15, 1958.

NIKOIAYEV, Konstantin Ivanovich; GENIIIj, B.S.j, red.; SAGAVOVA, V.V.y
red. izd-va; KOSIILIYEVO G,, tekhn. red.
(Some principles of construction in earthquake districts] Ne-
kotorye polozheniia stroiteltstva v soismichaskikh ralonalch.
Ashkhabad, Izd-vo Akad. ns&uk Turkmenskoi SSR, 1959. 49 P.
(MIRA 15:5)
(Earthquakes axid building)

LUNDINA M.G., kand.tekhn.nauk; 11'12SH~, ; kand.tekhn.nauk; KATSMAN,
I LAK, L.L.
L.M.P inzh.
Use of single-layar ceramic panels in experimentdl building
Trudy NIIStroikeramiki no.21139-54 163. (14M 17:2)

_KOSHLYAK. L.L.
C_ -
Efficient nerformance of fine-grinding rollers. Stek. i ker. 17
no. 11:23-26 N 160. (MIRA 13:12)
(killing machinery)

KOSHLYAK, L.L., in~,h.; LTMIRA, M.G., kend.tekhn.nauk
.
The role of preparatory moistening in the molding preparation
of a ceramic mixture. Stroi. mat. 7 no.3:30-.32 Mr 161.
- (Ceramics) 041RA 14:4)

KOSHLYAK, L. L,, Cand. Tech. Sol. (dies) "Investi._~atlon of Pro-
cess of Destruction of Natural Structure of Clay in Plastic Con-
dition,11 Moscow, 1961, 16 pp. (Acad, of Construe. and Archie.
USSR. All-Union So. Res. Inst. of New Construction 'Ilaterials)
160 copies (KL Supp 12-61, 269).

LUNDINA, M.G., kand.tekhn.nauk; KOS3LYAK, L.L., kand.tekhn.nauk
Choosing the optimum design of efficient ceramic blocks for
one-layer wall slabs of exterior walls. Stroi. mat. 8 no.8-
22-14 Ag 162. (InRA 15:9)
(Ceramics) (Walls)

YiATVEYKVA, F.A., kand. tekhn. nauk, otv. red.; MELEKHOVA, T.F.,
nauchn. sotr., zam. otv. red.; hl'YATKOVSKAYA, K.K.,
kand. tekhn. nauk, red.; KOSBIYAK,, L.L..._kand. tekhn.
nauk, red.; PLEKHANOVA , Yt'. -~-otr. , red.
SNITSAHENKO, A.A.., red.
[Prospects of the development of the ceramic industries
of Siberia and of the Far East; materials] Perspektivy
razvitiia kerawicheskoi promyshlennosti Sibiri i Dallnego
Vostoka; materialy. Novosibirsk, Red.-izd. otdel Sibirsko-
go otd-niia AN O"SSR, 1964. 183 F. (1,111U 17:11)
1. Soveshchaniye po khimii i tekhnologii keramiki i per-
spektivam razvitiya keramicheE;koy promyshlennosti Sibiri
i Dallnego Vostoka. Novosibirsk; 1962. 2. Khimiko-~
metallurgicheskiy institut Sibirskogo otdeleniya All SSSR
(for Matveyeva). 3. Gosudarstirennyy nauchno-issledovatell-
skiy institut stroitellnoy keramiki (for Kvyatkovskaya,
Koshlyak).

KOSHI.Yhx, M. -~.
Inspection is a powerful factor* Put' i put. khoz. 9 no.9:
8-10 165s (MRA 18 19)
I. Glavnyy revizor po bezopasmistl dijaheniya Ministeretva putey
soobshcheniyao

'I- KOSHLYAK, M.I.
The base of a flawless operation of transportation is the
safety of train traffic. Zhol.dor.tranap. 43 no.12:47-51
D 161, (MIRA 15: 1)
1. Glavnyy revizor po bezopasnosti dvizheniya Ministerstva
putey soobshcheniya.
(Railroad;3--Safety measures)

A:
GURIN. N. (Kiyev)-, KOSHLYAK, N., inzhener (Klyev).
Machine accounting of production expenses of a machine-tractor
station. Bukhg.uchet 16 no.2:35-42 P 157. (KM 10:2)
1. Glavnyy bukhgalter Rinisterstva sellskogo khozMstva Ukrainskoy
SM. (for Garin). 2. Soyuzmashuchet (for loshlyak).
(Machine- tractor stations-Accounting)
(Machine accounting)

KOSIUXAK, Pikolay Danilovich; TERESHCIUMKO, N.I., red.; SOKOIDVA, V.N.p
EWET-r-eT.
[Mechanizing accounting on colloctive and state farms] Mekhani-
zatsiia ucheta v kolkhozakh i sovkhozakh. Moskva, Sellkhozizdato
1962. 113 p. (MIRA 15:7)
(Agriculture-Accounting) (Machine accounting)

KALTNAN, P.A.; KDSIILY&K, T.V.
Oxidation of adrenaline in the organs and tissues of white
rats. Biokhimiia 26 no,4:729-735 J-1-Ag 161. (MIRA 15:6)
1. Chair of Biochemistrys, Hodical Institute, Kharkov.
(ADREMLIM, )

KC)SHITAK, V.A.; ODIWLAZOV, V*V*
gieribution of bitumens In the Mesozoic cross section of the
Yushno-Kolpashavo upland. Geol. nefti 2 no.9o.67-71 S '58.
(MIRA 11:10)
I.Kolpashevskaya FGZ* (Kolpashavo District--Bitumen)

KOSRT,YA , V.A.
Thermal studies of Mesozoic and Cenozoic sediments in the
eastern part of the West Siberian Plain. Sov-9001- 3
no,5:97-106 My 160. (MIRA 13:7)
1. Kolpashevelmva ekspeditsiya.
(West Siberian Plain Rocks-Thermal properties)

KOSHLYAKV A,
Z-
Relationship between the thernal field of the West Siberian
Plain and the relief of the Pro-Cambrian basement rock. Gaol.
nefti i gaza 5 no. 1:39-44,Ja 161. (KM 1-4:1)
1. Trost Bashneftegoofizika.
(West Siberian Plain-Earth temperature)
All

KOSHLYAK, V. A,; YAKUPOV, 1. A.
Formation of oil and gas pools in the reef zone of the cis-
Ural trough. Geol. nefti i gaza 7 no.4-7-12 Ap 163.
(MIRA 16:4)
1. Treat Baahneftegeofizika i treat Baohzapadnefterazvedlm.
Ural Mountain region--Petroleum geology)
al Mountain region--Gas, Natural-Geology)
M

KOSHLYAKP V.A.; YAhIJPOV, I.A.
Formation of water-oil interface in an oil pool.'., Neftegraz.
geol. i geofiz. no. 5:52-57 163. (141RA 17:5)
1. Trest "Bashneftegeofizi-ka".

KOSHLYAK9 V.A.; 5~MF70, Ya.A.
Two stages and the time of' tha formAtion of oJI and gas pools in the
reef zone of the cis-Ural trough. Sov. geol. 8 no.42136-140 Ap 165.
(MIRA 18:7)
1. Trest "Bashneftegeofizikall I. Ilsesoyuznyy nauchnC-issledovatellskiy
institut prirodnogo gaza.

AU!~HOR, Kcshlyakov.
TITLE: Some Problems of the General Circulation of Oceanic Viaters
(_N1eko-'.-oryye voprosy obahchey tsirkulyatsii vod okeanov)
PERIODICAL-~ izvestiya Aklademii nauk SSSR - Seriya geograf-icheskaya,
1958, Nr 4, pp 11-23 (USSR)
ABSTRACT: The views contained in this article on the general c-ircula-
tion of oceanic waters are hypotheses, The general circula-
tion of oceanic waters is understood to be a fixed system
of currents corresponding to the average annual scheme of
circulation. The author states that the whole mass of oce-
anic waters is subject to some common circulation originat-
ing from convective winds, lie explains his statement by
quoting foreign and Soviet scientists, such as P.S. Lineykin,
A.S. Sarkisyan, K.P. Fedorov and V.B. Shtokman. The ideas de-
veloped by the author on the spatial-dynamic unity of oceanic
circulation refute the possibility of the existence of
several uniform intermediate surfaces without movement ex-
tend-4ng over the whole water area and dividing geostrophic
streams., which are connected with the shifting of water
massea of different origins, He comes to the conclusion
Card 1/2 that among the general balance of forces directing the move-

S07-11 0-5e- 4-2
Some Problems of the General. Circulation of Oceanic Viaters
ment of the water of the Atlantic, frictional forces must
play an important part, and that the surface and sub-suz-
face Atlantic waters in the central part of the Arctic
basin are subject to a uniform system of horizont,al cir-
culation, The laminated structure of the waters of the
basin is explained by The action of specific climatic
factors transforming and freezing the upper layers of the
-ic
water masseB. An to the northward movement of Antarct
waters, this might be eXDlained by the complex bottom re-
lief of the ocean causing a specific change-over of the
thickneas of the ground waterG under the influence of frie-
tional. forces. There are 5 diagrams, 3 charts and 18 re-
ferenoes, 4 of which are Soviet, 3 German and 11 American.
ASSOCIATION: _nstitut okeanologii AN SSR (institute of Oneancior'Y,AS
USSR)
1. 0-:e_-Liography 2. Ocean cuxrents--Measurement
Card 2/2

3 (9)
AUTHORS: Burkovp V. A., Koehlyakov, M. N. SOV/2-0-127-1-18/65
TITLE: On the Dynamic Balance :Ln the Field of Deep Currents of the
Pacific Ocean (0 dinamicheskom balanse v pole glubinnykh
techeniy Tikhogo okeana')
PERIODICAL: Doklady Akademii nauk 3,133R, 1959y Vol 127, Nr 1, PP 70 - 73
(USSR)
ABSTRACT: The dynamic balance in ,;he field of the integral wind current
in a baroclinic ocean iti described in the steady case by the
equation of total currents by V. B. Shtokman (Ref 1) and W. H.
Munk (Ref 2):
W* T - 2 T ZLI df 37 S
- --m- = 0. Here
A
+ T-
,
y x
y
4
5
,
ax4 2 1 9
x D
,
F
~
.
y

vdz holds, and T denotes the function of total currents,
and v - the meridional components of the total current and
S
y
of velocity, H - the depth of the ocean, f - the Coriolis para-
Card 1/5 meter, T - the tangential stress of wind on the surface of the

On the Dynamic Balance In the Field of Deep Currents SOV/20-127-1-18/65
of the Pacific Ocean
oceang A the coefficient of horizontal turbulent exchange,
? -the average density of the sea water. The above equation
holds for the northern hemisphere. However, the solution of the
above equation is rendored difficult, apart from the known
mathematical difficult-ies, by the fact that the amount of the
coefficient A, ~s at pr;),sent still unknown. According to the
opinion of some resear(,h workers, the first term of the above
equation (describing the r^0le played by horizontal turbulent
friction) is negligibly small compared to the two other equa-
tions. Herefrom then follows the wide-spread equation for the
balance in the field of deep currents
1 -* df H
=-curlzT. vdz. The significance of this expression is
? TY ~
based on the fact that in a quasisteady oceanic circulation in
the open parts of the ocean, the divergence of the purely drift-
-like current is compensated by the divergence of the gradient
current with the reversed sign due to the planetary formation
Card 2/5 of eddies. If the gradient current is assumed to be geostrophic;

On the Dynamic Balance in the Field of Deep Currents SOV/20-127--l-18/65
of the Pacific Ocean
H z
___3P go tg T
curlz7 = + 0 dz) dz is finally found. Here g de-
notes gravitational acoeleration, T - geographical latitude,
R - the terrestrial radius, - the variable density of the sea
water, D - the depth ill whict there is no geostrophic current.
The minus sign in the above expression refers to the southern
hemisphere. If the firat term of the equation written down in
the first part of this paper is neglected, it is comparatively
easy to solve some problems of the dynamics of the baroclinic
ocean. It is really MOElt necessary to check the equation
__r1 7 = df vdz empirically. The authors attempted to do
z dy 0
so for the central part of the Pacific. These calculations were
based on the hydrological data of 9 pairs of deep-sea stationa
(which were recorded by the expedition vessel "Vityazg" of the
Institut Okeanologii AN SSSR (Institute of Oceanology of the
AS, USSR) in the)centre,l part of the Pacific from November '1957
Card 3/5 to February 1958 - Besides, the values of the turbulence of the

On the Dynamic Balance in the Field of Deep Currents SOV/20-127-1-18/0'5
of the Pacific Ocean
tangential stress of wind, which were obtained from the unpub-
"ished paper by N. S. Lytochkina, were taken into accourt. The
results obtaiaed by calculations are given in a table. In all
cases without exoeptio~,.x the absolute value of the divergence of
the purely drift-like nurrent is many times greater (on the av-
erage 10 times) than the divergence of the geostrophic current
in the field of the Coriolis force. This holds independent of
the position of the zero-horizon. These calculations permit the
preliminary conclusion that the equation
-4 H z
curl zIr M Izskl�_~ (;a~~ ? d) dz does not*,hold in the central
part of the Pacific. The dynamical:balance in the system of
quasi-steady depth-circulation is attained by the active parti-,
cipation of the forces of horizontal turbulent friction. There
are 2 figures, 1 table, and 9 references, 3 of which are Soviet.
Card 4/5

A
On the Dynamic Balance in the Field of Deep Currents SOV/20-127-1-18/65
of the Pacific Ocean
ASSOCIATION; Institut okeanologii Akademii nauk SSSR (institute Of oceano'-r--;--
phy of the Academy of Sciences, USSR)
PRESENTED: March 14, 1959, by V. V. Shuleykin, Academician
SUBMITTED: February 11, 1959
Card 5/5

:701-ILYAf:W.F, te. ',!* C~,-nd GpoL; Sci -- "C9ri-nin Tlec',iliprii-ino of H-ie
. 0 1- - - - ------------- j~Ll-~IWJL -
and V-1,et--ire o" 4a6yp#gm*tw occ~,pp o
-or,
1 0
-79-

KOSHLYAK4W, M.N. --
I.
Investigation of wind and corivective owl currents as applied to
the tropical equatorial part of the Pacific Ocean. Trudy Inst.okean,
40:W-151 160. (IOU 14:8)
(Pacific Ocean--Ocean currents)

papers s.b.ItL.J far the loth Pearls SCI.W. Congress, Honolulu, P...11 n A.4-
6 Sp 1961.
G., PZVQYAro'?.. A. A., wd XVVIVA, Z.. S., Moscov State
U.1-r.Lty, Ph'141-1 Faculty, Chair of Marina Physics and Terrain
Water& th,* calculation of rate of raAhout.1vtty spreaAl-Z
depth." (Section VII.B.6)
Institute of Zoalea - "I'- -thd of z;tcul. acaly.ta
ao4 posaLbUitle. of Its use in palcogeoeraphical. studios of the
Pacific 0..-" (S.Cuc. rII.r)
ja9V=j4A1__Iq,._V., Institute of U4ologr - "Distribution or al'o7as =1
ll= of terrestrial plants in botton sed-lents of the Pneific"
S.
cuot.
r
he heat
G Dir-tor, 1-,.tlt.ta of O-~I.a - "T.
'
bet-
- the At-tI. unter. -4 the dj...t oc,-Lc
CS_. Ion VMZ.D.L)
X=Mxkwl HL-t', Institute of Oce=olca -pIc of ti-A
tAtt.. of the 4cep cur~._t. In -.1. -rtv."tcm (3.ctl~a
m
Institute o: ccecno'~a
'Tt Lte".1ation bet-c. turbidity, pnyto; =ktcn ~d ;rL-_-; ;rc-
duction" (Section 11r.c.4)
Institute of O~anoloa - -On the relatlcn te--
~t.r transpaxency and the character of I. .~=c arc.a or the
P"LfIc Ocaaz" (Sectiot, 'nT.B)

I., and GAI.1T'-7-Zj1, 9, J., Institute ur Zarth Physics
~~n:~F;A. U.
-
1cwa. 0. Y4. S.I.Idt - *it~ture or -be earth crust In the transition
zons frovi the wrth~3t4rn part of the Pacific to the Asiatic contLnent~
(Section VII.C.2)
~d SNEV-S...M., Institute of
Carth Physics 1==i 0. Tu. Octr_idt - "3;,vcL:ic features of the se4iccz-~y
layer in the Okhotsk Sea =4 in the a4j=ent parts or the Paz-ifLc-
(Section VII.C.2),
NX!r'CVI C' 811 IMMOMOV'
~-
O, tt.
arid or occanaloic, -
mla I= bntwea ae,11mantaticn and b t- to
06-phy in the vorth-stern
t o ~
Part of the Pacific Oceno. (Section %=.C.1
3
Institute of C~lcEY - -The tc-.Unic mp of the PULfic
li
cesa and tbw circun Pacific while belt (scale 1:10,000,000)" (Sectica
Vf1.C)
I---- . . . 'LlErx
_,nd U!AM=. -ye P -,he SLb~riac De;artacat of
the Acadecy, of ScLancas I=SR - "On the results of LcvcstLgmtIcav of
In the L-W (S.Cti.n V.B.1)
L;M
_Y_V1, Urttttrte or Occanolocy - "HydrolacicLI data invcl"d
U
.1th In the Pacific and -. ymbl-ma onaaat.d .1th
1-..pect r. arch' VIr.3)
.c-) Institute of Ethnolorr - "Once wre on the Alm problec"
B)
Institute of 0-1ori .-Tha cm;oattion of orrnic xua-
peoded catcrIna In the Pacific in connectioni with the problecs of sedi -
surat-tterr (sneticn, YEt C . 3.)
U0r=_A._ r., Tmv*lt-t- or Oc.-.l.Cy - "Btt= ..di.-t. in the
Antarctic' (section vrr.D.i)
Institute of oceanology - "C"cicallc activity ~d
ClicAtOlogIC Crcats In the northern part of the Pacific Ocoac-
(se.ti- M A)
1 All-UnLo. Scientific P...-h Institute of M~Ict
T.
G.
__
_
.
, am 0. anoemphy - --e reaults of 1cthyolcC:Icm1 IavostiCoticn3
t=
"
I. the Callf of Alaska
(Sectl-n III.C)
Moscow State University, PhyaieLl Faculty, Cr-Ur ef
Bard Crust - -Ocojh;Ysical data =4 the poblc~_ of the crigin of the
Pacific Ocean" (Section VIt.C.2)
P., Institute of Om-L.Cr - "Th~ feet-.. f
bench forcation in tidal ease" (Sectirn Vlr.C.1)
P~=Y_91._B- Institute or Oceanoloa - "4unJitatve-qu=tIt.tiv.~
d1striltten or the 11tharal f.,- and f!.= In V~o north-t,rn. parl.
or the Pacific" (Section rIT.C)
rarzttutc of o-jicey . "',be procceo of -::.i
sedimentation in the areac or th,: Kurl I ialc arc" (S~tion

KOSHLYAKOV, M.N.
Studying the dynamic and kineinatic stmiture, of deep meridional
currents as exemplified in the northeastern part of the Pacific
Ocean. Trudy Inst. okean. 52t133-154 161. (MIRA 14:6)
(Pacific Ocean-Ocean currents)

KOSHLYAKOV, M.N.
Vertical circulation of waters in the JCuroshio area. Okeanologiia
I no.5:805-814 161. (MIRA 15:3)
1. Institut okeanologii AN SSSR.
(Kuroshio)

YOSIILYAYOV, M.N.
Calculation of deep circulations in the ocean. Okeanologiia I
no,6:~-r,7-1002 '61. (MIRA 15:1)
1. Institut okeanologii AN ISSSR.
(ocean currents)

KOSHLYAKOV, M.N.
Smoothing of results of oceanographic obseinv&tions.
'u..Q
4 no.3:4188-.1,96 164 11 .;~
1. Insti-tut- okeanologi.1 JUl' 13SSR.

KOSHLYAKOV, M.N.
Indirect methods of calculating deep currenta in the ocsano
Okesnologlia 4 no.52910 164 0,11i~ ls,~,A

KOSHLYAKOVF M.N.; NEYMAN, V.G.
. Some results of measuremento amd calculations of zonal currents
in the equatorial region of the Pacific Ocean. Okeanologiia 5
no.2t235-249 165. (MIRA 18:6)
1. Institut t5keanologii AN SSSR.

KosliTIMOV, V. E.
Ili k-
2920-5. Ballistiches-3-- deviptsi-i i_ r.-bot.-
- it
korlnnqo~ Un.- (kurs). Xapi s?i no F,ich-wrrnf-U~ 1c)499 'No. 1, Sl,
. - pt
K0SliLY.!A0V, V. N., M.~IiKAN, 1). R. I Da-6`i!SKIY. YU. a.
SO: Letopis' Zhiirn--l'rky)c!) StateY, Vol. 39, 1.:oskvi, 1949

13,
37 778
S/040/60/024/005/001/026
C111/C222
AUTHOR; Kosh-lyakov, V.N. (moscow)
TITLE: On the Asymptotic Solution of the Motion Equationn of a Gyro-
compass
PERIODICAL: Prikladnaya matematika i mekhanika, 1060,Vol.24, No-5,
pp-790-795
TEXT: If the unknown functions are denoted with 0(, then the
motion equations of the two-rotoric gyrocompass considered by the
author in (Ref-3) read:
2
fLtg 0, X_.+ -P- u sin ~PS +-a 0
u cosp V2
+ u cos %f OL - 0, v +-Qctg ~Py_ 0,
7ain
where the other notations are the same in R ef.3). The system (1.1)
" 7
can be replaced by the two equations
d'+ ( v2_ X~ ) C< = 2 ntg f &'+ Q:tg P
(1.2) + %) 2_ 2)E _ '~'c ta
F-s" ( Ea -,2 F-&)-ctg 2
Card 1/4

87778
S/040/60/024/005/001/028
C111/C222
On the Asymptotic Solution of the Motion Equations of a Gyrocompass
According to (Ref.3) it can be assumed that
(1-3) p --V-P1-s = const,
2B sin,r
where Pl is the pendulum moment of the gyroscope sphere, 2B is the
double kinetic gyroscopic couple of the gyroscopic rotor, f is the
degree of latitude, and s is the inclination of the characteristic
curve of the restitution moment depending on the rigidity of the
spring connection between the gyroscopes.
Under the assumption that s is sufficiently large, and consequently
that E