SCIENTIFIC ABSTRACT LOPATIN. G.S. - LOPATIN, I.V.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000930510016-6
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: January 3, 2017
• Document Release Date: July 31, 2000
• Sequence Number: 16
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

Lv- UBIMV ,N.N., doktor ekon. nauk, prof.; FOKIN, D.F., kand.
ekon. nauk; SHMESMSKIY, M.G., doktor ekon.nauk, prof.;
FISKOPPEL, F.G., doktor ekon. nauk, prof.; DY]TYU101, I.I.,
kand. ekon. nauk;,LOPATIN, G.S.,, doktor ekon. nauk, prof.;
MOGILEVCIIIK, A.Ye., red.
(Foretgn trade of the U.S.S.R., 1946-19631 Vneshniaia tor-
govIia SSSR (1946-1963 gg.). Pod red. D.F.Fokina. Moskva,
IMO, 1964. 189 p. WIRA 17:6)
1. Moscow. Institut mezhdunarodnykh otnosheni-y. 2. Kafedra
mezhdunarodnykh ekonomicheskikh otnosheniy Moskovskogo go-
sudarstvennogo instituta mezhdunarodnykh otnosheniy(for all
except Mogilevehik).

LOPATIN, G.6.1- PLAKSIN, I.N.
Extraction of goldp platinum and palladium b7 isoam7l a1cchol.
Izv. vys. ucheb. zav.; tavet. met. 4 no.4:87-90 '61.(MIRA 14:8)
1. Krasnoyarskiy institut tsvetn;Vkh metallov, kafedra
metallurgii blagorodnykb metallov.
(Precious metals-Metallurgy)
(Isopentyl alcohol)

K01,PAKOV , L.G. ; SA !-'I WINOV , V-Ya- ; Ib i'J"kTIN , (I . K. ; F!'iJO I t0v , T."'. ; T. iTj N" N, V. I.
Possibility of using C-lardless purmps for pipelines. T.-l.!d.,r --
I
neft' ro.3:lG7-:7-3 1,4.

- LOATIN, 04 V.
Analytical Study of Methods of Sampling Suspended Sediment, Report No 3 from the
series, "Investigation of Methods of Leter-r-Ining the Run-off of 'Sediments", 1941.
SO: U-3039, 11 Mar 1953

LOPATIN I '. V.
Verbatim: - " 'Buluunnyakhs' in the Lona River d-.,Ita," Problemy ,Irktiki, 1948
(Published in 19491, No. 3, p. 110,28, - Sibliog: 21 items
SO: U-4355, 14 August 53, (Letopis 'Zhurnal InIkh StR-ley, No. 15, 1949.)

Ln

7C,

VS
T C IQ C

"~PATT~-' Ir. 't, .
Lj, ~ P
LOPATIH. G.V.
Role of river depositions In Aral Sea sedImentation. Trudy Ieb.
oxeroved. 1:12-27 050. (KW A 7:7)
(Aral Sea--Sedimentation and deposition) (Sedimentation and
deposition--Aral Sea)

1 , ~ ...' 11 7.1 - . .
-i-ler,
Turbid zrm-7~s oC r~vcrs of li-- - -) - 7(" "'-~l
9. Monthly List of Russian LAccession , Library of Congress, 195X'), Uncl.
L_essions -

LOPA-,IN. G.V.
[Alluviu of the rivers of the U.S.S.R.; formation and movement] Manosy rek
SSSR; obrazovanie i verenos. Mockva, Gos.izd-vo geogr.lit-r7. 1952. 366 D.
(MMA 6:7)
(Alluvium)

1 . LOATT'l, G. V.
2. USSR (600)
4. Geography & Geology
7. Alluvial deposits In rivers of the U.S.S.R. Moskva, Geografgiz, 1953.
9. M nthly List of Russian Accessions, Library of Congress, April 1953. Unclassified.
-E.0- -

LOPATIN., Goergi Vladimirovich
Laboratory of Lake Science Acad Sci USSR, Acadmic degree of
Doctor of Geographical Sciences, based on his defensey 29
Novem')er 195h, in the Council of the Leningrad Order of Lenin
State U imeni Zhdanov, of his dissertation entitled: I'Alluviun
of Rivers of USSR".
Acaderdc degree and/or title: Doctor of Sciences
SO: Decisions of VAK, List no. 91 16 April 55, Ryulleten' MVJ SSSP., No. lb.,
Jul 56, Moscow, pp 4-22., Uncl. JPi-BAIY-h29

LOPATIN, G.V,, kandidat takhnichookikh nauk.
........
Formula for calculating the discharge of alluvium carried by
lowland streams. Gidr.stroi.23 no.1:43-44 '54. (MIRA 7:2)
(Stream measurements) (Silt)

LOPATIII, G.V.
. I
Long-term fluctuation of the Baikal Lake level. Dokl.AF SSSR
94 no.6:1o4i-1o43 F 154. (MLRA ?:2)
(Baikal, Lake)

LOPATIN, G.T.
Zones of turbiditr of rivers In Siberia and the Far Uat. lzv.Vasso
geog;ob-va 87 no-1:23-30 Ja-Y 155. (KMA 8:4)
(Siberia,-Runoff) (Soviat Far last-Runoff)

Lo P h V.
3(4,5) PHASE I BOOK EXPLOITATION SOV/1655
Akademiya nauk SSSR. Kcmitet yo geodezil I geofizike.
Tezisy dokladav na XT Generallnoy assambleye Mezhdunarodnogo geodezicheskogo i
geofizicheskogo soyuza. Mezbdunarodnaya assotsiatsiya nauchnoy gidrologii
(Abstracts of Reports Submitted to the llth General Assembly of the
Tnternational Union of Geodesy and Geophysics. Theluternational Asso-
ciation of Scientific Hydrology) Moscow, 1957- 101 P- /Parallel texts
in Russian and English or French/ 1,500 copies printed.
No additional contributors mentioned
PURPOSE: This booklet is intended for hydrologists and civil engineers.
COVERAGPe This collection of abstracts covers reports presented at the llth
General Assembly of the International Union of Geodesy and Geophysics on
hydrologicali erosional, and glaciological processes. Studies related to
problems of underground waters, snow, and rivers are also discussed.
the abstmots arr, in Russlanj, with English or French translations. Those appear-
ing in English are designated by a single uteriski those in Frencb by two.
There are no references given.
Card 1/4

Abstracts of Ileports (Cont.)
TABLE OF CONTMM:
SOV/1655
Aloks".ev, G.A. Principles for Computing M4&m Runoff in the Absence of
Actual Observations 5
K&3JnJn, 0.0. Computing and Forecasting Runoff by the Inflow of Water
into a River Basin * 12
Llvovich, II.I. Factors Affecting River Runoff 17
Lopatin, G.V. Deposits in USSR Rivers * 22
Piotrovich, V.V. Computing Dates of Freeze-Up and Ice Clearance in
Water Reservoirs -~
27
Popov, I.V. Variations in the Shape of Water Reservoir Rims and the
Forecast of Such Changes * 31
llakhmanovl, V.V. Influence of Forests on the Accumulation and Thawing
of Snov in Relation to Meteorological Conditions 36
Card 2/4

Abstracts of Reports (Cont.)
sov/1655
Shullts J, V.L. Basic Characteristics of the Regimen of Rivers of Central
Asia in Connection With Problem of Their Utilization * 40
Bogomolov, G.V.jand Ni.A& Plotnikov. Classification of Underground
Waters and Their Representation on Maps ** 45
Maka-enko, F.A. ,Characteristics of the Formation of Underground Runoff
Into Open Reservoirg and Rivers and Methods of Determining Them 48
Kunin,, V.N. Conditions of Undergrouna Water Accumulation in Deserts 52
7 V.V. The Study of the Process of Atmospheric Water Vapor
Tugarinov,,
Condensation and Its Role in the Formation of Underground Waters 57
Kudelin, V.I. Principles of Regional Evaluation of Natural *Reserves
of Underground Waters and the Problems of Water Balance 60
Ovchinnikovs A.~4. Hydrogeological Maps of Folded Mountain Regions
and Their Significance In the Evaluation of Underground Water
Reserves 64
Card 3/4

Abstracts of Reports (Cont.) SOV/1655
Sllin-Bekchurin, AOI. Types of Hydrochemical Maps in Hydrogeology* 68
Churlnov I M-V- Hydrological Maps and Their Importance in Evaluating
the Water-Bearing Capacity and Reserves of Underground Water 71
Avs3rik., G.A. Glaciological Studies in the USSR 74
Smlakvel-idze, G.K. Physical Properties of a Snow Cover 81
Shvetsov, P.F. Subject and Basic Problems in Geogleciology in the UWR 85
Shumakiy, P.A. Bftsic~ Problems in Modern Glaciology in the Light of
Present-dBy Studies by Soviet Scientists * 88
Armand, D.L. PtoblemB in the Study of Erosion Processes on the
Territory of the USSR 95
AVAILABLE: Library of Congress (GB653.A37)
Card 4/4 N4/gnp
5-21-59

LOPATIN, G.V,
------- - -
The atrwtarr- of t,.e ;r-u Dryn wo the history of its form,-tion.
Trudy Lab.ozeroved. 4:)-34 '57. (xLRA 10:91)
,'Pp.u L!!iryp Delti,-- igeogrpDhy)

1. ,f /Y/4. (f) , ~
.2 ,
IDPATIN 0 V
Conforenca on silted small rexar,7oirB of plain areaO in the U.S.S.R.
Izv. AN SSSR. Ser. geog. no.14,137-138 JI-Ac 157. (MIRA 11:1)
(Silt) (Reservoirs)

LII).IATIN, G.7.
ilydroiGgicn! data ou tYe I-mu 7jarfn ;'clta. Tri100 Mev differs from by 1 %. In th;is case,
I e !~' a
the sensitivity of the instrument is C -1W , Mbere X is the
6 7- 0
Z 0
plate diameter of a multiplate ionization chamber, and i is the mean
spacing of the plates. At energies of - 100 Xeyt C resaini constant. -7or
very low energies, C* and Q increases by 2-5 % as
W~ 6Z X0 ST
E drops from -100 to'15 Mev. For these energies it is necessary to
max
compare 'the data with a dalorimeter. The experimental arrangement is
shown in Fig. 1. The curves obtained for the sensitivity of the quantometer
are normalized using experimental data, and the sensitivity can thus be-
represented as a function of E in the range 15-300 May. The error is
max
less than 10 There are 4 figures.
Card 2/3
7.7

S/02 62/145/002/008/018
Sensitivity determination of a... B178YB104
ASSOCIATION: Fiziko-tekhnicheskiy institut im. A. F. Ioffe Akademii nauk
SESR (Physicotechnical Institute imeni A. F. Ioffe of the
Academy of Sciences USSR)
SU13YLITTED: April 14, 1962
%1.
4C
M S
C
Card 3/3 Fig. 1

3/05 62/032/011/012/014
BI 04YBI 02
AUTHORS: Kruglov, S. P., and Lopatin, I. V.
TITLE: A study of the energy leakage of a bremsstrahlung ray from
the absorber of a calorimeter. II-
PERIODICAL: Zhurnal tekhnicheskoy'fiziki,v. 32, no. 11, 1962, 1.399-1403
TEXT: In Part I of this paper (S. P. Kruglov, I. V. Lopatin, ZhTF, 30,
424, 1960) the angular distribution of the energy leakage from absorbers
of length 1 - 120 mm and diameters D - 55, 75, 95, and 120 mm was studied
for an energy of Eymax 85 Mev. The diametex:of the ray an the surface
of the absorber was d 35 mmv in some measurements it was 20, 45, 60 or
80 mm. Now the same experimental arrangement is used to determine th-e
dependence of the energy leakage from a cylindrical lead absorber as a
-function of-ita diameter and of its length for different values of E
?max
(Figs. 2 and 4). Using these results, the energy leakage from absorberg
of different lengths is represented in Fig- 5 as a function of the energy
leakage from an absorber of length 120 mm. The curves enable the energy
Card 1/5

S/057/62/032/011/012/014
A study of the energy leakage.... B104/BIO2
leakage of different absorbers to be estimated if that of an absorber
120 mm long is known. Absorbers shorter than 60 mm are found to be
unsuitable. The fraction of the ray energy carried away by the
transmitted component is estimated on the basis of the papers of L. 1.
Schiff (Phys. Rev., 83, 252, 1951) and G. White-Grodstein (NBS Circular,
No- 583, 1957) (Fig. 6). An experimenter developing a calorimeter has to
determine those absorber dimensions that will guarantee a given energy
leakage. For this purpose a large number of diagrams based on the
results obtained are given, supplying the desired dimensions for a lead
absorber with different E...x (50, 85 and 300 Mev). There are 7 figures.
ASSOCIATION: Fiziko-tekhnicheskiy institut AN SSSR im. A. F. Ioffe,
Leningrad (Physicotechnical Institute AS USSR imeni A. F.
Ioffe, Leningrad)
SUBMITTED: June 15, 1961 (initially)
October 30, 1961 (after revision)
Pig. 2. Energy leakage as a function of the absorber diameter. Legend:
The curves 1 to 5 refer to the ray diameter of 20, 35, 45, and 80 mm.
Card 2/5

KOWs A.P., akademik; KRWLCV,,
Determining the oensitivity of a quantimeter for the energy range
of 15 to 300 ~bv. Dokl.AN SSSR 245 no.2s3og-31i. n 162.
WMA 15s7)
1. Fiziko-takhnicbeskiy institut imeni A.F.1offe AN SWR.
Akademiya nauk Ukrainskoy SSR (for Komar).
(Radiation-Measureseat)