SCIENTIFIC ABSTRACT ZHILYAKOVA, O. - ZHIMERIN, D.G.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R002064820001-8
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: July 20, 2001
• Sequence Number: 1
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

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~~o vladimirlhkawovicb.. zaal.--agronom-USSRI_Z
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VAZEIOV, Tesilly Ivanovich, kand.geograf,nauk; BWMW, Dmitrly Antonovich;
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Fa -Ajj~mals# Small Hotned Stock.
USSR
Abs' Jours Rbf.~ ZhUr-Biol No 12j' .1958, 54960.
Author 7 S
Inst' Not given,
Title. Certain.Biological Peculiarities of the Karakul
Sheep, of "Sur" Hue
Orig Pub: KarakulavodstvoA zverovodstvo, 1957p No 30
.25-28,
Abstract., In order to study the internal peculiarities
of theblaok and sur-colored Karakul.lambst
:129 ram lambs (69 black and 60 sur) were s.ac-
~rifioed-at birth* The black ram lambs had.an-
average:liv,e:wMght of 5 3 kg., oareass.weight
2.3 kg., steamed skin.78; go, heart 39-19 go
and lungs..64-91 go The sur ram lambs had 5,
2.2, '885, 24-39, and 52-94, respeetivgly.. The
highest number of twins (9.23%) was found in:

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zunZAXU,-bL,, redi j.XONDRASWp4*M&# redo; USRWVI, FON.t
MAW~, S.I.,,,re4sizd-Ta; SEMAR,S.Ya.9 tekbnored,
s r the iusULUtiou and safe operation of elevators]
Pravila ustro'istva ibezopasnoi ekspluatataii lilltovt Izd~3&
Koskwav Ugletekbisdatt' 19599 71 p,
10, Ruaiia (192~-~, ts*sA*) lomitet, po'nadzora wbe2opam
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vedetavdm r-jahnt w,rA-Amvm*hla"ivnnA4 4 rm"Armt ncA-Pt%vm
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140ROZOV M,P.., red.; GUTOROV.,,V.G,O, red.-,GRINBODI, S,M*j red.-
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ZHILYAUVj AJA~. bred. 1* KONDRAWIOV, A*M., red.; LITVINOV,
~D.Ao- red.* TATARMKOp V*'A.p red,; VOLKOVt V.A., red.
izd-va; MINSKER,.Lol&F~tekbn-._-rSd..
f th6 mnuf
(Regu4tichs--or. acture and safe operation of high-
pressure vessels; mndat,ory-for al"Inistries and departments)
Pravila ustroiatya bezo snoi ekspluatatsil. sosudov,, rabo-
pa
~tai~ushchlkh pod davlaniem; obiazatellny dlia, vsekh ministerstv
:i vedomstv, Izd-4o~ MoskvF,, Gosgortekhizdato 1961, 79 Do

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heavy g az
Kdza~hstan -, whe re as auring..typle E4tmosp4eric circulation.~ theie is

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1 12 figure and'. 2~ tab ies

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AUTHORS s Baydal I M Kho t Zhilyayevt F. G.

TITLE i . ........ .. -- ---------
Experience Oollected-in the Hydrometeorological Service of
Tishing in Fall:in,the Northeast Caspian Sea
PERIODICALI. Meteorologiya~,.i'gidrolo'giyaI 1959, Nr 10, PP 32- 33.(USSRY
%ABSTRACT i In the Northeast..Casplan Sea, the greater part -of fish is
'Caught in fall and especially in..the period before the lake
-vice
freezes -up. In this'connection, the hydrometeorological.sex
master.,-responzible tasks, that is.to say, the fishing
organizationa.must be. given reliable advice and special weather
forecasts. Fishing is mostly done in the shallow coastal zone,
which is silted up by off-shore storms. Further, the actions
of the trawlers are-complicated, and the tackles are torn off
-and.carried,away. Dangerou.s.temperature drops are accompanied
by water temperature of almost zero. In 1956 and 1957 experts
-,Of- the. Kazakhskiy nauahno.~-issledovatelfsk�y gidrometeorologiches-
institutl(kazakh.Scientific Hydrometeorological Research
-byuro pogody (Alma-Ata Wea~,her~
Instit ute) and klma-ktinskoye
Bureau)'assisted:ft ~Gur'lyevakoye gidrometoobyuro (Gurlyev Hydro--
Card-1/2 meteorological Bureau) by establishing a joint service for the

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Z/023/61/000/004/002/003
Seismic energy meter D006/DI02
d:.] The authors dosignQd a
osoillations~ COstracter's notei t not explain6
robording noiamio onargy motor which p it th rooording of tho oquuro of
arm ~ o
v and.makes possible the determination of.; Pt. The energy meter consists
of a velocity meter and a function converter. The purpose of the function.
conIverter.is to.convert rz into V2 or into some other convenient.function,
e.g. log V. A schematic diagram of the instrument is shown in Fig. 1. A
lamp base witha projection lamp (1), a condenser (2), a mask (3) and a pro-
jection lens (4) are assembled in the tube of thelight source. The light
from the source is reflected.by the mirror of the galvanometer (5) and reach-
es the slit (6) of the.receiving unit. A film (7) is just behind the slit.
...,For squaring 4~ the mask has :the form of two similar parabolas.with a common
apex, When the-galvanometer-is not'inaction, the parabolas' reflection is
disposed symmetrically to the slit: and. the . latter is in full light. When the
galvanometer ose.illates,,a part of the slit is obscured. The ordinates,Z of
the-obscured Dart of the slit are PrODortional to the square of the y-axis.
The film is moved by tape-moving mechanism. -When the galvanometer oscillat-
es, the obscured part of the'mask reflectionmore or less covers the middle
part of the slit. As a result of this a-strip of light of variable width
Card.2 4
U "Flip 111 "111

-28597 Z/023/61/000/00,4/002/003
Seismic.energy meter D006/D102-
appears on- the f ilm af tor. it, hash been. ~developed. When the gask has the form
of a-parabola, the width of Ithis~.strip is proportional -ta i _. INhen ithas
the form of a lo ' r
ga ithm- the vidth.of:.the strip is proportional,to log :i.
Th'o'area oftho -light, strip Iis'd~tarminad by beans of a, planituator. A Method
af~rrocessing -the obtained.data ~is.: given,for the surface viaves yielding the
equation's
2,
dtl= dt, ~dt.+
+ V 2dt
Z
where Ni - E, Z are-- indices, of the displaceme nt oomponetits on the free sur face,
Thereare 3 figures,;1 table -and 5'r-eferene6s: 4 Soviet-bloc and 1 n.on-Sov-
iet-bloc.'- The reference to the Englisih-language publication reads no fol-
lowat H. .Jeffreys, Tho Pamirearthquake of 1911 February 18, in relation to
the depths of earthquake foci. IIIW.S, Geoph.,SuppI.',''v. 1, no 2, 1923~
(Technical Editor: V. Tobyas).
ASSOCIATIONe Physics Department, Moscow State University, Moscow
SUBIJITTED: December-7, 1960
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ACC-NRt AT6021022 SOURCE CODE: UR/0000/65/000/000/0172/0176
Ak~Holz-. ZhilyAyava V.. 'A.
'ORG: nor
TITLE: Magnatic vis cos ity JnL rocks
'A
'SOURCE If SSSR- Institut fiziki Zemli.' Hastoyashcheye i *proshloye magnitnogo polya
Nauka, 1965,.
Zemli (The present and past,of the earth's magnetie,field). Moscow, I zd-vo L
cl
'TOPIC TAGS: spontaneous magneti, zation igneous rock magnetic viscosity ferromagneti
material 'L.
ABSTRACT: The author s study of igneous rocks revealed that one ferromagnetic fraction
co Lnsis.ts of fairly coarse,parti.cles (15 to LBOL Microns) of maIgnetite and hem atite and
0 L t ' L foM -
ithat* -the second fraction:is pulveruln. and occurs in the of hematite dust. Only,
An one case was a pulverulent fraction found to consist of hydrogeothite dispersed
ithrough a clay. , Several experimefital models, duplicating such compositions, weremade
It became evident
1up, for purposes of.analysis of their behavior in magnetic fields.
I at the strength of magnetic field iscontroll le theLin-
Ith .ed by.the coars.a fraction whil
Itensity.of magnetization is inversely proporti erulent.
6 onal to the ~aantity of the pulv
fraction. For pzxnzicles of 20 to 100 microns, the intensity of magnetization is inde-'
CC,~Cj 1/2
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-ACC NRo Xt6636364 SOURCE CODE: 0 0 0 0
~AUTHOH:- Zhilyayeia V
n
A.; Koles 1kair, L. V.
A
OHG:~ :~Moscow State University' ft
sics,Department (Moskovskiy,gosudarstyenropy univer
'sitet 'Fizicheskly.fakulltet),
TITLE:.-Dependenceof.the coefficient of magnetic viscosity Ov on the peculiarities.of
theferromagnetic grai
-SOURCE: AN:SSSR.--Izviiatiya"::Fizika~Zemli., no. Us 1966) 122-12T
-magnetic viscosity in structure
TOPIC TAGS:, . . I , ~ Jgra ferromagnetic structures mineral..
~mag4etoimeter, phase transition
ABSTRACT: This-is a.continuition..of earlier work (Izv. AN SSSR., Fizika Zemili, noo 2P
1965), dealing with,variatidns, observed in the natural residual magnetization of
volcanic and sedimentation minerals., where large variations in the*magnetic.viscosity-
were observed. The present investigation was undertaken to determine the dependence
.6f,the.magnetic.viscosity bn the features of the.ferromagnetic grain of the mineral.,
-since earlier attempts to explain the variation ofthe magnetic viscosity did not
take the grain into account.4, The tests were made on single-crystal magnetite and
ma gnqs1oferrite with different percentage content of MgOj and also large-grain polyp
cryaltalline.-magnesioferrites having the same percentage of MgO, Changes in the graii
were!"produced1n. the laboratory,Lby various beat treatments* In additions the de-
~jp!qiclence..of Sjr on'the phase. ttansformetlon of the natural seA*les of various Oren
2 -3
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36364.1.
were.measured. Themeasurements were made witha Dolginov magnetometer, and.-coveredj~
besides:-the magnetic viscositi.,-*also the saturation coercive-force and the dependence
of-the.coefficient of.magnetic-visebsity and the degree of martitization. The in-
crease,in the coefficient of the magnetic viscosity is a consequence of the decrease
ifi,the volume.of:the domains.of the ferromagnetic grains. It can be due either to
Ancie4e,of elastic stresses produced when the,grains of the magnetite and magnesio-
magnetite are broken up bya grid.of ma.rtite., or to a decrease in the ferromagnetic
grain as such.'.. However., ~ the size of theIgrain.observed under the microscope cannot be
regarded as a parameter Aich determines the magnetic properties of the ferrcmagnetic
materialf.iince the grain structure plays a larger role than the grain size., for
graina.ofall dimensions., and plays the most important role for grains vitb diameter
lawserAhm 20 ji.;- The'effect can be explained from the point of view of fluctuational
4iscositY., The authors: sincerer tbank Doctor of ftaical-Mathematical Sciences G. N',
Pittova. for valuable advice. jOrig. aft obest., 6 figures* 4 forwilaso and 4 tablese'.
OMM MAne, OM M', post
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8/049/61/
t..0001008100L.1002,
Paleomagnetic research in~ "he USSR
t D260/D304
Paleomagnetic research for studying~the Earth's magnetic
i -in the
f eld past and' correlation of geological strata.
Study~ of~,the different geological-gpophysica.1 conditions wh t
:cause the formation of ferro-magnetic:roak- 3) P h y s i oa 1basis
of paleomagnetism. 4).~Study of reversed.magnetisation of var-
~ious.,kinds of rock. .5) 'Quality of equipment. Papers surveying
the,p;ogress.of.paleomagnetie'research in the USSR and o 'I-; ~ae-r
countries were by R. M. Yanovskiy and G. N. Petrova., I'Flsi~!he--~
skiye osnovy paleomagn.etisma" (Physical Basis of PaIeomavnvrism)*,
A.5. Khramov,_ Paleomagnitnyye issledov-aniya v stratigrafil Vol'
geokhronologii, ~(Paleomagnetic. Research in Stratigraphy and
A-. G. Kalashnikov~- "Istoriya geomagnitnogo
polya na osnovanii paleomagnitnykh issledovariiy" (History of
the Geomagnetic Field on the Basis of Paleomagnetic Research);
P
N Kropotkin _~"Obzor sovremennykh geotektonicheskikh teoriy..
0
v osobennosti-teorii gorizontallnogo ya zemnoy
peremeshc4erri
kory" (Review of Modern Geotedtonic Theories, especially -the
Card 7

s/o4q/61./ooo/oo8/002/002
Paleomagneticirelsearch in -the'MUR: D260/D3QL9_
--'Theory izontal~Displacem6nt of th Earth's Crust). Other
of Hot e
-papers dealing-with groups-1 to~-4 were.% 1 A. 11. Khramov and
hii colleagubs,reported.,on the.first positive experimentato
draft sections of:rock idth,the aid of the paleomagnetic method
for the correlating strata in vast territories. T.. 1. Lintkova
gave a paleomagnetic analysi6~.of the sedimentary layers of.the
upper Devonian system, and explained that reversal of the Bar-ti-Lis
magnetic field had,taken,,place in the Devonian period, -3
directly and reversedly magnetized rock proved to have the z1m:
f erromagnetic component. . G. I.'Kruglyakoira and A. N. Tret- - yEik_
reported on the results o -f testing.,the,residual magnetizatio'a
of rock belonging to the Cambrian, Ordovician, Silurian. De-
vonian and Carboniferous systems. Coordinating data fo~ the
magnetic'poles and respective periods were established by -Pa-
-culation. Ts. G. Akopyan spoke on,,stratigraphic correlatioij
and"differentiation'of.Cenozoic volcanic Tormations. V. V.
Kochegur and B. Rusinov reported on the results of studying
Card 3/7
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Paleomagnetic research iii theTSSR
-.continents.-hAd occurred~ hypothesis, he~says, is erroneous,
..~and:ls'probably:due to the fact of overmagnetization',of rock
in successive.-erase 2), A. G.Xomarov.investigated the changes*
which occur'in effusive-J?oqk.after its formation. A. N 'Shmelva
studied%the magne'tizatioh.of:sedimentary rock in its naiural'
state And after re sedimentation. A. Ya. Vlasov and colleague's
studied the influence'on.the-residual magnetization of artifi-o-
cially~.Produced:sediments, caused by,the.force of compression,
The authors found that compactness of the sediment obtained by
vertical pressurereduc9d the incline by almost 100. Pressure
sideways, on the other hand, cau8ed increase. T. A. Martynoval
~reported on-her studie's of changesin KKA quartzites in connec-
tion with.the.parameter of,.their.magnetic -characteristics. N.
P. Mikhailova gave'a,:report on the magnetization of alkaline
rock. During.the.discussiohs which took place in this second
group various opi 'nions were expressed concerning further studies
of artificiall sedizented rock and the conditions of re-sedi-
y
Card 517

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ZHIMMIN, Dmitriy Goorgiyevich; KIPNIS, S.Te., rodaktor; EMITRIBTVA. R.V.
i 1. J..
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NOTIKOVO-IoTet-
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Ch; -CHEIWTOVA -V -,,--red- - -NEZNANOV
N tekbn red
:[Histor7, of the eleotrification.of the'U.S.S.R.]istoriia elek-
+.Vo4 N Un + 04 4O'CUM -Mo%olfgrgs --Q^+g2alr"4m- 10AJ- Arl

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L1 115418.66 EWT(d)/9WP(k` IEVI-P,(1)
A
N& AP6005028 SOURCE CODE
CC URT0105T65 000TOm/0091/0091
AUTHOR i Ayvaz-f M3, IV. Q.; Aleksandroyj Be K.; Andrianov,,Va N.; Beschinskiy, A. A.
Rudzko, f~ Ap _MekinJJ6A*; Krasnov V. So; Kruzhilin,, Go ff.; Kulebaking Ve So;
Markvardtp K. kovichp 1. Me I Popkove Y. lei Styrikovich
List?1r, P. N., He At:
ORGt 'none
4) 4-
TITLE: Professor Andrey GeorgiZ!vich Ukharin
Elaktrichestvop'noo 1,:1965 91
TOPIC TAGSs electric power engineering$ electric engineering personnel
ABSTRAM, A Bhort.biography of subject on the occasion of his 60th birthday in
November 64, A close disciple of Krzhizhanovskiy.#'he now.heads sector.of general
methodological problima and forecasting at ENIN Institute of Power Engineering
)i and power engineering section within its scientific councils
imeni Krzhizhanovskiy,,
In 1927-1932,, worked in designing and construction of power stations and industrial
power installatione in the Trans-Caucasus* In 1932* having graduated as electrical
engineer from Tbilisi F61,yItechnical Institute, he switched to scientific work at
All-Union Institute of Fam Electrification.. and. at ENIN since 1944. Became
candidate of technical sciences in 1937; doctor,.in 1948* :Subject is credited
the moth
with working out Oda for designing efficient and economical regional and
local power syotems# utilizing local power resources and coordinating them idth th"
power grids* He participated in-studies on elsotrification through 1980, and on
Card
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AINFOR- Aladlyev. 1. T.t Aleksandrov, B. K 1 Baum. V. A. Go S.
Golldenberp. So As.,-Zhim".4-24
-b t 7.mW-2.4.' At 0#1 Iyqvle~' Ve x Knorro, Vt Go;
K6'a&V-,Go- lot 14ont-yeva, Zi Io; Haricovich ' I* Hal )~Mmrovich. E, As; t khnovich, Go *I
1!2pKov' -1, IrOPOV. Vv A,v- yoditaTo-y. I: S.; PyotnUgUy. ji. Net Styrikovich.
III Aq. o oy, Ygo-Gal Touldig-21j.-at.A.1 t1mkhancy. Zs Fol B~OyndUnq Ao Is* /
ORGt none
71=t Lev Jakolayevic-11 Xhitrin
z 3351.6 lizvootlyat SnarglUka ItransPax~te not Zo 1963t
TOPIC TAGS% acadovdo porsonnal, physics personnel# combustion, carbon.high.
temperature rosoarch, plasm ba&IN" fuel
ABSTOZA, ProtossorIL. R. bitrin' Corroaponding'Mmber, Academy of Scionbox
uurq, state Pries LAarsato. and Doctoror IM&Incerine Sciences, died after a
short but sa4cra Mn a at the age of 58. He was woU known hors and abroad
as an.outa'tanding ad:nqtist and specialist in'tho field of combusuon theory
and the development of method* for opeading up burning offucl. He began his
scientific vorU at the AU- Union Heat ftinooring institute after grad"tint
-fron the physicz dopartnont of Moooov University 1A 1930. His early wo was
~cn the propagation of flames In gases, and an heterogonous embustion. Xn
'1914 he dofondod his Doctorle Dissertation on tho theory of,combustl*n.of. car-
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bon., His monograph OColtbustion of Carbon" vaia~ardad !he State Pri".,ain 19~041
-In 1951 he became the yomanant director of the lalsora
tory for tho intonllWiCa
tion of -combustion processes of. the 0, Ho Xrahi;hanoyak~Z Power Institute.'/ He
was elected a corresponding mmbor 'or the A adW of Scion= U55d In 1953. He
'headed the All Union Advisory Doard on combustion, represented Sovict science
$at Intern ational Symposia, and was a mcmbor of the International Initituto of
cGnbustion. For a number of years, he directed the HoscoV Soncral 3oninar on
coi4buation, and took an active part in the work of the Scientific Council of
the Acadeny of Sciences USSR#~ on hinh temperature heat physics, and of the
scientifte council on the comprehen3ivo utilization of fuel. Ile devoted a
larp amount of attention to,, toaching work. He directed tlie_q2!Lbustion Mi.
. . . . .............
.V - crav
dion of the Physics Nortmod, f-.jjdGcovt St-ite Univorat Ilia miino
"Physics d"Combustion and Dqatsioni'11957) lo a basic text for students in
.this field. Three otorls Dissory-ld no And fifteen Candidate DiMrUtiona
woro defended under his direction. In the last years of his life he directed
work on methods for comprehansive utilization of fuel at power stations so as
to obtain valuable products free the sinaral part of the fuel, as well as work
on the.physicAl chemical prooesses in a plama stream, and thd laochanism of
interaction between- carbon and'gaass. He wall the author of more than 60
is6ientific workep got which he was awarded the Order of the, Red Bs=er of,
Labor and~modalse-, origo art* heel lfigur96 fjM-V..,'-.
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