SCIENTIFIC ABSTRACT A.P. CHEMBARTSEV - V.M. CHEMERIS

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000308320013-1
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 12, 2000
• Sequence Number: 13
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

-CHEMB.ARTSAV A.P., gorVy Vazh.; PADMYV, A.B., gornyy inzhe
Response to V.S. Khokhriakova and A.S. Tkachovals article w7ruelc
transportation In open-pit mines should be under the control of
the mine". Gor.' zhur. no. 1:80 Ja '61. (KIRA 14:1)
1. Somilukekiy ogneupornyy zavod (for Choubartsev). 2. Severnoys
rudoupravleniye Trosta, Soyuzasbest (for Pedoyev).
(Kig hauja
.Se I (Iqdpstgial
(Khokhria ova, . 0 %Tzac ova P.Owr.T!5ucks)

ROSTOVTSMV, N.F., akademik. glavnyy red.toma; SOKOLOV, N.S., prof., red.
toma; LIMOV, P.A., kand.gool.-mineral.nauk, red.toma; KUMICHEY,
A.T., kand.biolog.nauk, red.toma; UffLOV, P.A., kand.biolog.nauk,
red.toms; RUT-IMATA. Te.A., kand.biolog.nauk. red.toma; C-M-00-M-11
R-Ts-- kand.biolog.nauk, red.toma; BARDIN, I.P., akademik, glavnyy
red. (deeeased]; LAVRFM ITIff, K.A., akademik, red.; VOLIFKOVICH,
S.I., akademik, red.; DIKUSHIN, V.I., al,-.ademikg red.; MEHCHINOT,
V.S., akademik, red.; VZYTS, V.I., red.; LIVITSKIT, O.D., red&;
NJURASOV, U.N.. red.; PUSTOTAIDV, L.V.. red.; KRACHATURCY. T.S.,
redo.1 POPOV, A.N., red,; GRAFOY, Me., red,; GASHEY, A.D., red.;
VASYMIN, V.P.. prof.. red.; PROBST, A.Ye.. prof., red.; KROTOV,
VoA*j prof.. red.; VASMOYET, P.V., doktor skonom.nauk, red*;
LYUDOGOVSKIY, G.I., kand.takhn,.nauk. red.; MMOLINIKOV, K.G.,
lmndeekonom.nauk, red,; KLYUSMIN, P.A., red.lzd-va; DOROKHINA.
ION99 takhn.red, (Continued on next card)

ROS20VTSW. N.Y.---(continued) Card 2.
[Development of the resources of lastern Siberia: agriculture]
Razvitie proizvoditellnykh oil Tostochnoi Sibiri: Sellskoe kho-
sisistvo. Moskva, Isd-vo Akod.nauk sssR-. 196o. 426 p.
(KIRA 13:6)
1. Konferentsiya po razvitiyu proizvoditellufth ail TostochnoY
Sibiri. 1958, Irkutsk. 2, Tsesoyuznaye akademiya sellskokho-
syaystvennykh nauk im. T.I.Lenina (for Rostovtsev). 3. Chlen~-
korrespondent Vsesoymznoy akademli seliskokhozynystvennykh nauk
im. T.I.Lenina (for Sokolov). 4. Chleny-korrespondenty AN SM
(for Veyts, Lovitskiy, Nekrasov. Pustovalov, Khachaturov). 5. Days
stvitelinyy chlen Akadexii stroitel'stva i arkhitektury SBSR (for
Popov). 6. Zomeatitell predoedatelya Gosplana RSFSR (for Grafov).
7. Chlen Gooplans RWSR (for Gashev)
(Siberia, Zastern-Agri;ulture)

I., kandidat ekonomicheskikh nauk; INYAZHEVSKIY.
Material requisition and Inventor7 cards. and the reduction of
repair and maintenance costs of automobiles. Avt.tranap.32
no. 10: 13-16 0 154. (Xft 7 -12)
1. Dotsent Koskovskogo tnthenerno-okonomichookogo institute, in.
Sergo Ordzhonikidze (for Chamber) 2. Glavnyy bukbgalter
Kinisterstva. avtomobill rta. I shossayi7kh dorog
nogo transpo
Latviyakoy SSR (f or Kwazhevskiy)
(Automobiles-Repairing)

CMPMZR. N.
Recent norm for tire wear. Avt. transp. 35 no.4:6-7 Ap 157.
(KM 10:5)
(Automobiles--Tires)

SAFRAY, Gets. Yefimovna; CMNBER, Nina Yevgenlyevna; KHROMOV, I-A-o
red.; D014SKAYI, --
[Financial planning, accounting and the analysis or the
financial condition of an automotive transportm&Alm unit]
P3.anirovanie finansov, bukbgalterskii ucbat i ;;A-iz fi-
nansovogo sostoianiia avtokhoziaistva,. Moskwai- Avtotransizdats,
1962. 61 P* (MIFLA 15:5)
(Transportation., Automotive-Finance)

Category :USSR/Nuclear Mysics Elementary Poaticles
Abs Jour :Ref Zhur - Fizika, No 1, 1957, No 443
Author :Chemberlen, 0., Segre, B., Vigand, X., and Ipallantis, T.
Title :-&s-e-rv-&t-i-o-n-o-? Antiprotons
Orig PQb Uspekbi fiz. nauk, 1956, 58, No 4, 685-692
Abstract No abstract
C-3
ill
C" 1/1

CITEEHILOV, F.
Volga River - De~.cri,)Uon
The Volga Fegion; From Gorlkiy to Astrakhan. V. V. Pokshishevskiy. Reviewed
by F. Chembulov. Geog. v shkole No. 1, 1953,
Honthly LLL of Russian Accessions, Library of Congress, June 1953- Uncl.

C191MULOV, F. Z.
"Film Course in Russian Geography," Gcog. v Shkole, No.5, 1952

m)/EWA(d)/ETGW-6/EWA(l) WW
ACC NR, AP ODEt U-R~~ho/66/03-070-01/0154/0163 I
6007 SOURCE C
AUTHORS: (Moscow); ChekimKqy,,.,~(Leningrad)
ORG-t none'
TITLEt Steady-~SW 1 ,of an anisotropically conducting medium in a half-space'
SOURCE: Prikladnaya mtematika i mokhanikap v. 30., no* 1, 1966, 154-163
TOPIC TAGS; MHD, compressible flow, steady flow, conductive fluid, plasma
ABSTRACT*. The steady flow of a conducting fluid over an infinite plane under the
action of a uniform magnetic field Bdis investigated. An assumption is made that
the temperature dependence of the physical properties of the fluid is known. As a
first approximation, these properties are assumed constants and a finite solution
is obtained in the form
V* V~.o + cle-riw + cseyw.
81.2 + i(ol's 1/0 A.'w /a f(R T R.51 4 (RJ?"~-M
where it is shown that the solutions Vo(y), B*(y)p J*(y) in general have a nonmono-
tonic characteristics, Next, the wavelength 'A 2T-/W is juxtaposed on the
Card 1 2

L 23442-66
ACC NR, Ap6w7584
velocity profile for To evaluate the effect of variable properties and.
compressibility on the flow field, an approximate solution is attempted by means of
small perturbations on the various flow parameters. To study the effect of
nonmonotonic velocity distribution, thecase of a rotating flat plate in an
incompressible fluid is analyzed with the magnetic field aligned parallel to the
axis ofrotationo Orige art. hast 50 equations and I tablee
SUB CODEV 20/ S-UBM DATEs 09Aug 65/ ORIG REFs 007/ OTH REF i' OD~

MMIN, G.S.;,CMMM, X.T.
pactory eolqmtltlon of the Scientific and Technical Society of
the Nachimery Industry. Plad.prom. 14 no.4t64 Ap 160. (MU 13:6)
1. Modiko-lostrumatallaWy savod OWasnogwardoyetsm.. -
(MICAL U&M 8 AND AMRAWS)

BULGARIA
Col MC IM. ANTONOV and Lt Col MC R. C11" "MCOV
"Treatment of Ascending Paralysis Type Landru.11
Sofia, Voenno Meditsinsko Delo., Vol 18, No 3, Jun 63; F-T, 45-46.
Abstract : Polyncuritis (Guillain Barre) in 7 ratienz:s, including one
following vaccination with triple cholcra-dysentery-typhoid vaccine; 2
of the patients died. Stresses seriousness o~ condition and need for
energetic treatment, also comments on a case allc---edly due to Sabin
oral poliomyelitis vaccine. Five Soviet, 4 Bulgarian references.
[1/1 -j

UM/Geophysics'm- Alluvial Deposition 'Nov 51
"Andient Alluvial Depositions," Yu. F. Chemekov
"Priroda" No 11v YP 55, 56
Presents the scheme of constructionof the vari-
ous types of subject accumulations and their'dii-
tribution along a river bed. Such phenomenon is
videspread in the taiga and montane-taiga regions
of the LISSR, on the shores of taiga rivers in
Siberia and*in the Far East. There these ancient
alluvial deposits of trees and soil jutting into
rivers go under the name of ."Zftloil" fbroken"'
207T48
IIEL~R/Geophysics - Alluvial Deposition Nov' 51
(Contd)
suggesting the broken trees that created the
initial accumulations of river debris and allu-
vium, caught in the branches of the fallen tree*7.

USSR/Geology
Card
Authors ~Crasnyy, L. I. Chemakov, Yu. P., andBultvankor, E., Z.
Title I First Pambrian era discoveries in the Dzhagdy ridge (Khabar-
ovsk region)
Periodical t Dokl. AN SSSR, 96, Ed. 4, page 801,Jitne 1954
A%Arict:.~, ThezCambrian. bra,'Aepoislts. of -the Dzhagdy ridge. belong, to..thp~A
geosyne na 0 c, a ge,- 0
Mongol-Okhbtsk~ it 1:region, the,palaoz I -:- ta
Aevelopment, which-is only recently being explained. Th*e
Cambrian era deposits.of the Dzhagdy ridge were c~~;,ectedlby
a general basin with Eastern Zabalkal and,.South,Siberia at
-the west, and the Ussri basin at the east, where Archasocya-
thus sp of the Cambrian era are known to exist. Cambrian i
find.9 w;re also rade recently at the Maloy KhIngan. All''
these finds point-toward a broad development of Cambrian
transgression in Eastern USSR.
'Institu.tion A1.1-ITnion Sc lentif ic-Re search Giological Institute, Leningradl
-Presented by:~ Academl-p tan D.,V. Nalivkin,. March 20, 1954

C I t- I e. /;, V C- ec, 1, / /I f
-r-
KWNYT, L. 1. DZALNVSKAYA, Ta.A.
Devonian deposits of the Dshugdzhur and Pribrezhnyy Ranges.
Inform.9bor. VSM9I no.1:82-M '55. (MI&k 9-12)
(Dsbugdzhur Rauge-Geoloff, Stratigraphic)
(Pribreshrjy Rauge-Geology, Stratigraphic)

CHEMOV,YU.F.
.......
Driftwood deposits. their formation and development. Izv.Vsea.
geog.ob-va 87 no.2:134-146 Kr-Ap 155. (KL!RA 8:9)
(Rivers--Regulation)

CHRMOV, Tu.F.
of tbaloya-Baroya-Asur Deprension. Mat.TSBGSI no.lt42-
49 156. (MM 10: 1)
(Asir Talley-Geology)

14-57-7-14434
Translation from: Referativn zhurnal, Geografiya, 1957, Nr 7,
p 26 (USSRTY
AUTHOR: Chemekov, Yu. F.
TITLE: Contributions to the Stratigraphy of the Quaternary
Deposits of Central Sikhote-Alinf (Materialy k strati-
grafii chetvertichnykh otlozheniy Srednego Sikhote-
Alinya)
PERIODICAL: V sb: Materialy po chetvertich. ge6l. i geomorfol.
SSSR, Moscow, Gosgeoltekhizdat, 1956, PP 76-103
ABSTRACT: The author states that the Far Eastern territory
preserves traces of two glaciations of the mountain-
valley type, and he considers it possible (if general
climatic factors are considered the cause of glacial
formations) to discover parallel glaciation periods
in both the European and Far Eastern parts of the USSR.
Card 1/2 He assigns the pre-glacial period and the lower

Contributions to the Stratigraphy (Cont.)
14-57-7-14434
glaciation to the Lower Quaternary epoch in his tentative outline
of the stratigraphy of the Quaternary deposits. He assigns the
middle interglacial period and the middle glacial period to the
Middle Quaternary, even though acceptable evidence has not yet been
uncovered in the southern half of the Far East; however, the nature
of the deposits testifies to some climatic cooling. He assigns the
upper interglacial period and the last glacial period to the Upper
Quaternary. He distinguishes a moment of post-glacial climatic
optimum and a modern stage in the present period. The article
includes tables of data on spore, pollen, and diatomaceous analyses,
and a bibliography of 22 titles.
Card 2/2 D. A. Timofeyev

"I.. / -4-
CHWXOT, YU.F. -
Gemorphological division Into dletrIcts of the eastern part of the
Soviet Per last. Natj~l Chet.gool.1 C*oaorf. ao.1:104-128 056.
(MIRA 10:1o)
(Soviet Par last-Physical geography)

14-57-7-14549
Translation from: Referativnyy zhurnal, Geografiya, 1957, Nr 5,
p 45 (USSR)
AUTHOR: Ghemekov,-XU.!,-F.-.
TITLE: Geomorphological Subdivision of the Southern Part of
the Soviet Far East (Opyt geomorfologicheskogo rayo--
nirovaniya yuzhnoy chasti sovetskogo Dallnego Vostoka)
PERIODICAL: V sb: Materialy po chetvertich. geol. i geomorfol.
SSSR, Moscow, Gosgeoltekhizdat, 1956, pp 104-128
ABSTRACT: After analyzing existing systems of geomorphological
subdivisions in the southern part of the Soviet Far
East, the author proposes a new system and give a
brief description of its component parts. The article
contains also a geomorphological and an orographical
chart and a chart showing the traces of Quaternary
glaciation. A province, a zone (district) and a region
Card 1/4 serve as division units. By a geomorphological

14-57-7-14549
Geomorphological Subdivision of the Southern Part (Cont.)
province the author means a broad territory lying within a large
geotectonic area where a particularly well-expressed type-of r6lief
predominates. Geomorphological zones (districts) have similar
historical development, occupy similar positions in a geotectonic
region and have certain similar features in their reliefs. Such
zones lie in geosynclinal areas and are clearly divided due to the
zonal distribution of geotectonic elements. A geomorphological zone
lies within dissimilar platforms and shields. A geomorphological
region represents a territory containing one or several genetic
relief types interrelated by a common historical development, geo-
logical structure, nature of unconsolidated deposits, signs of recent
tectonic movements and geomorphological forms. The author discusses
the following geomorphological provinces and zones (districts) to-
ether with a number of regions contained in them: A. The Eastern
M
atic geomorphological province of mountains and depressions
belonging to the Alpine and Quaternary geotectonic epochs. 1. the
Sakhalin zone of horst and graben structures of mountains and
Card 2/4

14-57-7-14549
Geomorphological Subdivision of the Southern Part (Cont.)
depressions. B. The Amur geomorphological province composed of
folded and eroded block tectonic mountains and depressions, with
folds of the Mesozoic geotectogenetic epoch, augmented by recent
tectonic movements. 1. The Sikhote-Alin fold and dome forming an
uplift zone. 2. The discontinuous zone of Khanka and Lower Amur
Mesozoic-Cenozoic and Cenozoic depressions with numerous complex
lacustrine alluvial plains. 3. 11he Wndan"nSu zon6" of eroded tec-
tonic mountains restored by recent tectonic movements. 4. The
Khingan-Burein zone of faulted and folded and eroded block tectonic
Gault mountains with traces of an ancient glaciation. 5. The Zeyd-
Selemdzhinsk horst and folded and eroded block tectonic intermountain
zone with Gault relief and traces of an ancient glaciation. 6. The
Zeya-Udsk zone of Mesozoic-Cenozoic and Cenozoic depressions with
numerous plains of lacustrine and fluvial origin. 7. The Dzhugdzhur
zone of folded and eroded block tectonic Gault mountains with traces
of early glaciation. C. The Aldan geomorphological province of
plains of erosion, plateaus and highlands, forming the southeastern
Card 3/4

14-57-7-14549
Geomorphological Subdivision of the Southern Part (Cont.).
section of the Siberian Platform. The district of dissected
plains of erosion and plateaus at the head of the Aldan River.
D. The Zeya-Burein-Amur geomorphological province of plains and
eroded tectonic relief. 1. The District of Zeya-Burein-Amur
depression. 2. The Turan eroded horst mountain district. A
bibliography of 16 titles is included.
Card 474 D. A. Timofeyev

CHAMIOVI Tu.F.-
-Z-:- ..
%iaternary history of the Sea of Okhotsk. Izv.Vsejj0geog.ob-v& 8~
no.3:203-220 Ny-Je '57.. (MIRA 10:11)
(Okhotsk, Sam of--Geology, Stratigraphic)

VIRISHORAGIN, ~.N., otv.rad,; KRASNYr, L,I., otv.rad.4 VLASOV, G.M., r ~ad,;
ZOLOTOV, N.G., red.;'9KMOYDA9 I.I., red.'; ITPAR SOYA, L.D., red.;
MMAMSKAYA, red.;.-OPIKKINOTS141, T.T,, red.; SATRASOT, N,P,;
qm!m~~S"OJTSOT. 1F.P.', red.; AVMIY]ffA. ?.A.. takhn.red,
[Resolutions of the Interdepartmental Conference on the Iriaboration of
-6tindard ttiatikrapk4o Systoin for.the tar last] Reshamila no"shchanlia
Koshmdometyannago sa0eshobmblia pa rospOotka unifitalrovanzykh stra-
11grafiche-ki1rh ekhms dlia.Balinego Tostoka. Kooky&, Gosammohno-tekbii.
Izd-Y.o.1it-ry,po geole I okhrans nedr. '1958, 51 p. (MIRA 12:.3)
1. .11ashwedomalvennoye moveshchanlys po rasrabotke xmffitsIrov&"zI3*b
stratigrafiche.~kM ekbou'dlyatallnegoJostokst Miabarovsk, 1956.
2. Predsedatell Orgkomitsta Mashisdowtvenziogo sq*isbabasilya'~P0 ras-
rabotke wifitalrav strat rafichookikh ikhavi dlya Mallnego
U
Tostdka,(:fbr Kra
.(Soviet ftr Nest-41sology, StratIgriphic)

V
ANIKMV. N.P.,.,glavnYY red.; BISKE, S.F., red.; BOBYLEVSKIT, V.I., red.-
VASIXOVSKIT, A.F., red.; VMS11GRAGIN, Y.N., red.; DWKIN, I.Te.,
red.; TZVANGULOV, B.B., red.; UFIMOVA, A.1%, red.; ZI14XIN, A.T.,
red.; T-ARTN, H.I., red.; LIKHAREV, B.K.. red.; MElam, V.V., red.;
KIKHAYLOV. A.F., red.; NIKOLAYEV, A.A., red.; POPOV, G.G., red.;
POPOVv Tu*N., red,; SAKS, V.N.. red.; SHMENIN, A.I., red.;
SINAKOV, A.B., red.; TITOV, V..A., red.; SHIW. N.A., red.; RL'YANOT.
N.D., red.; TAKUSHEV, I.R., red.; V redaktirovanii.prinimali uchas-
tiye: AHM TEVA, O.H., red.; BATKOVSKAYA, T.N., red.; BOLKHOVITINA.
N.A., red.; BORMX, M.O., red.; VASIL'YXV, I.V., red.; VASIUVSKATA.
N.D.. red.; VOUVODOVA, Ye.K., red.; YEVSHYEV. K.P.. red.; KIPARI-
BOVA, L.D., red.; ZRASNry, L.I., red.; KRISHTOFOVICK. L.V., red.;
MUM, N.V.. red.; LIBROVICH, L.S.. red.; KARKOV. F.G., red.;
KODZALAVSKATA, Te.A.. red.1 NIKIFOROVA, 0.1., red.; OBUT, A.M.,
red.; PCHILINTMffA, G.T., red.; RZHONSNITSKATA. M.A., red.; S11DOTA,
N.A.. red.; SWAROV. D.L., red.; TIMOF&TXV, B.V., red.; XMTDOLBY,
X*K., red.; C OV, Tu.F., red.; CBZRNTSHETA, N.Te., red.i
DIMZHAVINA, GUROVA, O.A., tekhn.red.
(Continued on next card)

ANIKOBV, N.P.-(continued) Card 2.
(Decisions of the Interdepartmental Conference on the Unified
Stratigraphic Columns of the Northeastern Part of the U.S.S.R.]
Resheniia Nexhvedometvennogo soveahchaniia po razrabotke unifitsi-
rovannykh stratigraficheskikh akhem dlia Severo-Vostoka SSBR,
Moskva, Goa.nauchno-tskhn.izd-vo lit-ry po geol. i okhrane nedr,
1959. 65 p. (MIRA 13:2)
1. Nezhvedomstvennoye soveshrhaniye po razrabotke unifitairovannylzh
stratigrafichaskikh skhem d1ya Severo-Vostoke SSSR, Magadan, 1957.
(Soviet Far East--Geology. Stratigraphic)

CHEMEKOV, Yu.F.
Quaternary system of Khabarovsk Territory and Amur Province. Mat.
VSEGEI. Chet. geol. i.geomorf. no.2:88-95 159.. MRA :L4*- 5) ~
(Khabarovsk Territorp-Geology, Stratigraphic)
(A*r Provin6e-Geology., Stratigraphic)
I

BOYTSOVA, Ye.P.; VITTEMBURG. F.V.; GANESHIN, G.S.,; GROMOV, V.I.,; ZUBAKOT,
V.A.; IVANOVA, I.K.; KRASNOV, I.I.; LUNGMSGAUZ3W. G.F.'- - . I
NIKIFOROVA, X.V.; FOKROVSKAYA, I.Mv; CHEMOV. YU.T.: EPSHTIM,
S.V.; TAXOMMA, S.V. - ..--
Sergei Aleksandrovich lAkovlev; obituaiy. Biul.X-om.chetv.per.
no.23:97-101 159. (MM 13:5)
(Iftoylev, Sergei Aleksandrovich, 1 ",-1957)
(Geology)

30)
AUTHOR: Chemekov, Yu. SOV/20-127-1-50/65
TITLEt Ancient Surfaces of Denudation Levelling in the Priamurlye 0mr
hegion) and Adjacent Territories (Drevniye poverkhnosti denudatsionnogo
vyravnivaniya Friamurlya i sopredellrWkh territoriy)
PERIODICAL: Doklady Akademii nauIc SSSRg 1959, Vol 127, Nr 1, PP 100-183
(USSII)
ABSTRACT: The author's investigations (Ref 7) shored that the =rfaces
mentioned in the title ar6 widely developed in the Soviet Par
Fast. Them out the dislocated rocks to a different extent
without adapting themselves to the geological structures. The
widely distributed weathering crusts are characteristic of it.
They form morphologically slightly hilly surfaces vith broad
river valleys without distinctly marked terzaces through which
small rivers vith not distinctly marked beds flov. The valleys
are separated by not too high slightly concave water divides
consisting of parent rock. On top of it there are in places
residual mouhtains of a height of 100-300 m with convex or
convex-concave slopes which form a volcanello landscape
Card 1/3 (melkosopochnik). Residual mountains and melkosopochnik consist

Ancient Surfaces of Denudation Levelling in the SOV/20-127-1-50/65
Priamurlye (Amur Region) and Adjacent Territories
of rocks most resistant to weathering. The levelling surfaces
014 are marshy in the Par-East, and their loose covering is
often subjected to insular ground frost lasting many years.
The DLS developed almost everywhere in this region. Individual
regions of the DLS distribution are enumerated. Their
description shows that DLS developed in various geological-
structural zones: on the plateau (south-eastern part of the
Aldan mountain country), in the region of a central massif
~~r-Zeyiskays depression), in the zone of Proterozoic folds
0
(Stanovoy- and Dzhugdzhur chains), in the tiongolo-Okhotskaya and
Sikhote-AlinskaA 'folded regions during the period of relative
tectonic staticity. 111heir age is very different: Cretaceous,
Upper Cretaceousq Pro-Upper-Oligoceneg Upper Tertiary, Mocene,
Pliocene, Pliocene-Lower Quaternary. The different age of their
individual sections is characteristic of great DLS. The narrow
spatial connection of these formations speaks in favor of the
genetic connection between the melkosopochnik, the denudation
hills, insular mountains, and the DLS. In the transition from
the mountains to the DLS, there exists a rule governing the
alternation of landscapes which proves a genetic sequence of
Card 2/3 denudation types of the relief. This process was interrupted

Ancient Surfaces of Denudation Levelling in the SOV/20-127-1-50/65
Priamurlye (Amur Region) and Adjacent Territories
ASSOCIATION:
PRESENTED:
SUBMITTED:
by the tectonic activity without having reached the peneplain-
stage. The typical peneplains lack therefore in the Far Fast.
It must not be spoken of pediplainel since a humid climate
existed here. This is confirmed by the spore-pollen-spectra
and leaf flora from Jurassic-, Cretaceous-, and Tertiary
sediments, furthermore by the kaolin type of -neatherince Yany
useful minerals are connected nith the DLS (gold, cassiteritet
clay for refractory material and bricks, as well as mineral
colors)* The almost flat relief is suitable for agricultui-e.
There are 8 Soviet references.
Vsesoyuznyy nauchno-imsledovatellskiy geologicheskiy institut
(All-Union Scientific Geological Research Institute)
February 27, 1959, by I. P. Gerasimov, Academician
February 25, 1959
Card 3/3

30, 5)
AUTHORs. O.hemekov, Yu. Fe SOV/20-127-2-53/70
TITLEs quaternary Glaciations in the Monsoon Region of the Far East
of the USSR
PERIODICAL: Doklady Akademii nauk SSSRv 1959, Vol 127, Nr 2, PP 423-426
(USSR)
ABSTRACT: In mostrec~,nt years repeated Quaternary glaciations could be
detected in the Far East of the USSR. They w9re synchronous
to those of other regions of Fast Asia and Europe. Their tracea
were.proved in all important mountain ranges and mountain
regions of the Far East. This holds also in the case of Mongolia,
China, and Japan. Recent glaciers exist only in Kamchatka and
in the Himalaya. The mentioned traces are represented either
by sculpture- or accumulative relief forms. The following
types of goomorphological old glacier landscapes occur in the
Par East: (1) Cirque-thro'ugh-glaoiation of deeply and
intensively structured mountain ranges, distributed mostly in
iip to 2500 m highchains. Cirque-, hanging-, simple and complex
valley glaoiers.existed here. (2) Highland glaciation with a
Card 113 semi-cover glaciation (polupokrovnoye oledeneniye)

quaternary Glaciations in the Monsoon Region of SOV/20-127-2-53/70
the Far East of the USSR
(Aldan mountainous countryg or at its periphery, at the foot of
the Stanovoy range -.probably a glacier of the Malaspina type).
(3) Glaciation of table mountains (Kamchatka, Kurillskiye
Islandi). Glacier of the Scandinavian type which flew down the
river valleys like a snout and formed simple or complex valley
glaciers. (4) The glaciation of mountains of volcanic origin
(Kamchatka, Kuril Islands) was characterized by a composed
glacier complex with a basin which has already existed before
(Kallder glacier), by valley-, radial-, migrating-, cirque-
and hanging glaciers, glaciers with broadened end, and glaciers
at the foot of the mountain (ledniki podnozhiy) just like the
recent-glaciation. During the Quaternary glaciation the snow-
line showed:a considerable depression (Table 1) which increased
from the north to the south from 500-700 m to 1400 m- Its
position beoame higher from the north to the south and from the
east,to the west. This holds also in -the case of the direction
from the periphery of the mountain ranges towards their axial
parts and iiithe case of the increasing sea level in the same
direction, finally in the case of the distance from the sea
coast (from the south-east) to the inner part of the continent
Card 2/3 (to the north-east). The reauction of the snow-line

Quaternary Glaciations in the Monsoon Region of SOV/20-127-2-53/70
the FaL! East of, the U~P -
(i.e. of the lower boundarj of the -'h-lonosphere) was assumed to
be-related to the reduction of the annual temperature average.
it is rather certain that the climate of the Par East of that
time was a monsoon climate with mainly summer precipitations.
The mentioned temperature drop could prolong the cold season of
the year and cause the precipitations to fall during the whole
year as snow. Table 2 shows the areas computed by the author
by means of a planimeter within which remains of Quaternary
glaciation are found for the estimation of the int "ensity of the
latter, These areas amount to approximately 609000 km2 for the
oontinentai part of the Soviet Far East and to approximately
260tOOO km for Kamchatka. There are 2 tables and 14 Soviet
references. I
ASSOCIATION: Vsesoyuznyy nauchno-issledovatellskiy geologicheski institut
(All-Union Scientific Research Institute of Geology~
PRESENTEDs February 27, 1959, by I. P. Gerasimov, Academician
SUBVITTEDs February 25, 1959
Card 3/3

KRASIMI Lev Isaakovich; C L , red.; FILATOV, V.G., red.izd-va;.
PERIKOVA, S.A., iqkhn.red.
[Geology and miner4Xs in the area west of the Sea of Okhotsk]
Geologiia i pcIemye iskopaemye Zapadnogo Priokho*ttia. Moskv4s
Gos. nauchn-t6kbn.izd-vo lit-ry po geologii i okhrane nedrp 1960.
161 p. (Leningrad. Vsesoiuznyi geologicheskii institut. Trudy,
vol. 34) (KIRA 14:7)
(Okhotsk region--Geology)
(Okhotsk region-Mines and mineral resources)

Cil;`~IKOV YU.141.
Brackish imter and marino diatoms in Chiaternary soiiments of the
lower Amur Valloy and Silchoto-wjUinl !,,anoe. Gool. J goofiz. 10:
83-91 '60. (ITEM 14; 2)
1. Vsesoyu-.zKrf mucl-no-isslcdova'e'L'Aziy .-cologlel.oshy institut,
Leningrad.
(Soviet Far East-Diater-O

(' CHNIIEDV, Yu.F.; SIT, I.I.; SIDOVA, M.A.; BURILINA, L.V.
Stratigraphy of incoherent sediments in the Amur-Zeya DWesslon.
Sov. geol. 3 no.2:17-38 7 160. (KL'BA 13:11)
1. Vaesoyuznyy nauchno-issledovatellskiy geologicheskly institut.
(Amur Valley--Geolog7, Stratigraphic)

CHEMKOV, Yu. F,, Doc Geog Scl -- "Stratographic quaternary
deposits and the geomorphology of the RlverLAmJu7rjegion
F
and adjacent territories." Len, 1961. (LeninjOrder of
Lenin State U im A. A. Zhdanov) M. 8-61, 232)
- 90 -

GANESHIN, G.S.; KORNUTOVA, YO.I.; KRASNOV, I.I.; CH M.JJL~-
EPSHTEYN, S.V.; YAKCVLEVA, S.V.
Map of Quaternary sedimnts of the U.S.S.R. Izv. AN S55R. Ser.
geog. no. 4:14-24 JI-Ag 161. I(KIPIA 14:7)
1. Vsesoyuznyy nauchno-i3sledovatel"3kiy geologiche3kiy institut.
(Geology, Stratigraphic-Maps)

KATS, N.Ya.; KATS, S.T.; CHEMEJiCV, Yu.F.
Tetyukhe peat bogs and their importance for Quaternary stratigraphy
in the southern Soviet Par East. Geol. i geofiz. no-4:96-105 161,
- (MIPA 1415),
1. VBesoyuznyy nauchno-ineledovatel'skiy ge.ologipheskiy institut,
Isningrad. (Soviet Far7&mt,-Geology, Stratigraphic)
(Tetyukhe region-Peat bogs)

CIMMOV, Yu.F. ---
The snow line of the,last.upper Quaternary in the south of the
Soviet Far Fast. Izv. AN SSSR. Ser. geog. no.6:7347 NZ 664
(MM 14:12)
1. Vaesoyuzr4y nauchno-issledovateliskiy goologichookiy imatitut
MMI).
(Soviet Far East-Glacial epoch)
(Soviet Far East-Snow)

GANESHIN
j, G,S'; CHEMEKOV,, Yu*F*
First enlarged plenary session of the Intordepqrt4ental Geozorphological
Committee of the Department of Geological and Geographical Sciences
of the Academy of Sciences of the jj.S.S.R. Soy. geol. 4 no.3:120-126
Mr 161. (MIRA 14:5)
Vaesoyuznyy nauchno-isaledovateltakiy g*ojo icheakiy *titut.
(Geology.. Structural-Congressipf

GANF.SHIN_, G.S.; ZUBAKOV,, V.A.; POKROVSKAYA, I.M,,; SELIVERSTOV, Yu.P.;
CHEMKOV, Yu.F.; EPSMT.YN, S.V.; YAKOYMA, S.V.
Sca:Le,, content,, and terminology of stratigraphic subdivisions of
the Quaternary system, Sov. geol. 4 no.8:3-15 Ag 161.
(KRA 16:7)
1. Ysesoyuznyy nauchno,-iosledovatel'skiy geologicheskiy institut.
(Geologj, Stratographic)

G.S.; C RjQY,-Jm.F,
anniv.6roary of S.V. Obruchevls birthday.
93 no.4:341-344 n - Ag 161.
(Obruchevp Sergdi Vladimirovichi
Izv. Vses.
(MIRA 14:7 )
1891 -)

CHENSKOV, Yu.F.
Quaternary tectonics of the Amur region and adJacent areas (Scvwiet
Far last). Dokl. AN SSSR 137 no.3:67/v.677 * 161. (MIRA 14:2)
1. Vaesoyasnyy nauchno-lsaledovatellakly geologicheskiy institat,
Predstayleno akadamikm I.P.Gerasimovyu.
(Saviot Par East-Ceologyt Structural)

CUMKOV, Yu.F.
Quaternary sediments and basic phaseB of thrj &va2opmew. cf vege-
tation in the Far Fast of the U.S.S.R. Xqt,, VS*,GEl Chet, geol, i
geomorf. no-4:183--196 161. (MIRA -17: 5)

CHEMKOV, Yu.F.- ~ - - ,
Quaternary glaciation in the Far East and the northeastern part
of the U.S.S.R. Trudy VSEGEI 64a119-134 161. (MM 15:6)
(Soviet Far East-Glacial epoch)

WREYSM, N.G.; GAISMIN, G.S.j KRAMIOV., I. I. - CHEEKOV 1u F
Fourth Congress of the*Inteimational Association an Quaternary
Research (INQM). Sovegeol. 5 no-5:260-165 Mjr 162. (MIRA 15:7)
10 VaesoyuzLV nauchnow-issl6davate-319kiy geologichoskiy institut i
Vsesoyuznyy nauchno-issledowatellsIdy institut gidrogeologii i
inzhenernoy geologii.
(Geology, Stratigraphic-Congresses)

GANESHRI, G.S..;- C mov U -F.--
IN.
At the Sbrth Internaticml~Congreas on the StWY of the Quaternary*
Izv. Vaes. geog. ob-va 94 no.3:281-284 11-Je"62. (mMh 15--7)
(Geology, Stratigraphic-Congressea)

CHEMEKOV, Yid,, F.
Boundary between the Quaternary and.Neoggne. Trudy Kom. chetv.
per. 20:146-149 162. 1 (MIRA 16:1)
k,
(Geology,, Stratiamphic)

CHEMKO ru,F, I
Significance of the posorphological wthod in proqmting for
kaolin in the Far gast. Inform.sbor. VSB2I no.52:121-131 162.
I (MIRL l5s 11)
(Azar Valley-Kaolin)

CITI " " , ya.,P
~ 0
I
Morphology, genesis, ags anii the wmiit4,,c)nA rrnv~;.rning Lhe
0
form&tion of the anclent surfaces t denudation 'qnation in
th-3 south-ern part of the Far East, of tha Tr-ady VSEGET
163. (Mi,`-RA a'? - 5)

QAMSHIN, G.S*-; CHRMOV, Tu.F.
Results or Up Sedond-ft2"ged Plenum of the Geawrphological
Commission attachad.to'tbe Department of Geological and
Geographical Sciences of~tbe Academy of Sciences of the U.S.S.R.
Sove pol. 6 no,5tl52-156_.My 163. (MIRA 16s6)
(Geworphology)

CHEMEKOV,.Xu.F.
History of the development of the river network in the Amur Basin.
Izv. AN SSS.R. Ser, geog. no.1:81-93 Ja-F '64. (MIRA 17:3)
1. Vsesqyuznyy nauchno-ionledovatellskly goologicheakiy institut.

GENMOVP YU.P.
Geomorphological cycles. Izv. AN SSSR Sar. geog. no-4:136-141
t64 (MM 17-.8)
1. Vsesoyuznyy naucbno-issledovatellskly geologicheski-y institut.

GANESHIN, G.S.; CHEWXOV, Yu.F.
Third Plenary Session of the Goomorphological Commission.
Sov. geol. 7 no.3tl39-1" Mr 164. (VJRA 17:10)

LOKSHIN. Te.L.; ZOTOV, A.G.; CH31M. V.P.; SHIPILOV, N.G.
Ways to Improve the Industrial and economic Indices In the
preparation of underground gas producers by boring. Podzem.
gas.ugle no.3:67-n 159. , (MIR& 12:12)
1. Angrenskeya stantelya "Podsongas."
Moal. sification, Underground)
fBaoring)

KSTLIN, GaS.; CHWORA, K.V.
IN ~-ka~
Struggle for technieal progress. Ned.prom. 13 no.4:114-45
AP '59. (MIRA 12:6)
1. Nediko-instrweental'Wy zavod "Krasnogvardeyets"s
(SCIMIFIC AWAUTUS AND IliSTRL4UNTS)

KUCHMENT,.-L.S.; CHSWRENKO, Ye.P.
Hydrologic calculations on electronic computers abroad. Trudy
TSIP no.117s98-116 163. (MM 16t7)
(Hydrology) (Blectronic computers)

- CHEMERENKO, Ye.P. -
Calculation of the bydrologic regime
using electronic computers. Meteor. i
ja 164.
of Kuybyshev Reservoir
gidrol. no.1;35-40
(MM 17:3)
1, TSentralInyy institut prognozov.

CHEIERENKO, Ye.P.
Cal-culntion of the transfommijf)n of a flood in a reservoir.
Trudy TSIF no.13301-43 164. (MIRA 170,0)

AGGENION NRs Ap4ou749 S/0161/64/006/001/0128/0133
!'WJ0RSj Serap To raoi Chenit4sy*# Go a,
.iTITLEs The photoelectric properties of single cryntsla of cadmium, selenide treated,
iby gas discharge
ISOURCEs Fizika tverdogo telap v. 69 no. 1. 1964s 128-133
TOPIC TAGS-. photoelectric-effects cadmium selenides cadmium selenide single
crystal, gas discharges photocurrents spectral distribution, thermal conduotivityp
I
f
u~damental absorption,, photosensitivity$ dark current,, extinction bands capture
..'cross section, hole, electron
!ABSTRACTs Measurements were made on single crystals of GdSe grown by recrystal-
,lization from the vapor phase@ Ga or Ga-In alloy was used to obtain ohmic conta0t16
The spectral measurements were made with a DM-4 double monochromator with quarts
ioptics, Before treatments the dark resistances the spectral distribution of the
,photocurrent, the dependence of intrinsic time on wave length of incident lighk#
the spectral dependence of phatoourrent yields, and the extinction of photocuisut
wets measured@ The specimens were then subjected to a single treatment of gas
Card

ACCESSION NRs AP4011749
idischarge. After treatments the same parameters were measured again, It has been
'shown that this treatment leads to a considerable increase in intrinsic time and in;
photocurrent yield in deep bands of'fundamental absorption because of the marked
increase in photosensitivity of GdSe in this band, A large capture cross section
;for holes results, and a small capture cross section for electrons., Recombination
;of carriers at the surface is greatly diminished. The yield of electrons at room
ant
~temperature by neutral vacancies in Sep forming by the gas-discharge treatm J,
:leads to an increase in thermal conductivity. It was observed that the dark cur-
rent increased. A new extinction band of photocurrent was observed in the vicinity(~
:oi 7300 1, forming as a result of treatment on the surface of the crystal* "In
:conclusion, the authors express their thanks to V. N. Dulldiyer for making some of I
I i
ithe measurements." Orig. art* hass figurese
ASSOCIATIDN t Odear~r V0audarstvenzV*y universitet L 1. Mechnikova. (Odessa
IState University)
ISUBMITUDt l7Jul63 DATz AcQs 24Feb64 EWLt 00
;'SO CODEs PH
Card
NO MW SM 006
OTHERt
010

T. 7 1.- 7T 7j*- 1 C,, jD
T
7
SOUP~,Cji', CODIL':
I UTI-70' Chenicresy
013.G: 0,1,-,ssaS'LateUiiivcrsi'L*yimen:Ll. 1.
universitet)
iViceiiiii)~ovk'Odcsskiygosudars'6vennyy
TITLE: Generation of electric oscillations in single crystals of cadmium
SOURCE: Fizika tverdogo tcla, v. 8, no. 10, 1966, 23841-288G
TOPIC TAGS: crystal, cadmium selenide, single crystal, differential resistance,
0
ct.irrent, r,lras discharge, volt ampere saWration, low frCq.',IL!.-,eY Oscil-Aiatilon,
oscillation
ABSTRACT: When sinale cadmium selenide crystals are sub ected to a gaseous
a i
d-ischarge, the crystals attain volt-ampere szituration and manifest a negative
differential resistance. They exhibit low-frequency oscillations in a current
whose period depends on the voltage applied, the wavelength, and the intensity of
the incident light. Fluctuations in current occur for both direct and alternating
voltage applied to the crystals. The author is greatly indebted to S. G. Kalashni-
Card -1 / 2

L 09896-67_____
,~-ACC
AP6033547
kov and M. K. Sheynkman for discussing the results and valuable comments.
[Author's abstract]
SUE CODE: 20/ SUBM DATE: 07FebGGI ORIG REF: 004/ OTH REF: 005/

CHEKEREVSKIY, R., arkhitektor-
I "
Designing apartment houses for rural areas in the Far North.
Zhil. stroi. no.lOsU-18 165. (MM4 18tll)

GORBOTSKATA, T.G.-. WEROW,
KAIRFSKATA, R.K.
To.G.; SOBOIJVSKATA. O.P*; CHIBMINSKILYA,X.S,
In honor of professor Jr.Aelaryshemle 70th birthday, 'Feet. van, I
dorm*' 20-3:63 IV-Jo 154. (Km 7:8)
(KWSWA, XSMIU 1883-

WTSHBTA, K.A., professor; CHIMERINMTA& K.S.
OynthosWein there" of postganorrheal and nongonorrheal diseases of
the genItourInar7 tract In young girls. Vast. von. I dern. no.5:
47-48 S-0 154. (NLRA 7:11)
1. U otdel& gonorrel (z&v. Prof. K-A.Kaz7sheva) Klyovskogo
pauchno-Issledomtellskogo dermato-venerologichookago Institute
%dIre MeJorlskin)
(UROMMITAL SYS=, diseases,
there, abloramphen1col In female child.)
(CHUMAKPMICOL. therapeutic use,
urogenltal Use In female child.),

OCnOTSUTA. T. G.; CHDMINSUTA K. S.; UXOGMGMX, P. A.
W V W ~ ~-, MMP-4 - W ~11 C -
Preliminazy data on the combined antibiotic therapy of chronic gonorrhea In
girls with combination of antibiotics. Test. van. I derm. no.5:43-46
5-0 155 (KLRA 9:1)
1. Is Kiyevskago aw-ohno-Issledovatellskogo koshno-venerologichaskogo
instututa, (dir. 0. To Koryakin, nsuoharyrukovoditelf-prof. K. A. Karysheva)
I 11yevskago gorodskogo koshno-venerologichookogo dispensers. (say. A.S.
Ivanov)
(GCNQMMU. In Infaut and child
ther, antibiotics combination in girls)
(AMIDIOPICS. ther. us's
gonorrhea in girls. combination ther)

WIMINSIATA, K-S.; SOBOUTMU9 O.P.; PLOTCHER, S.M., laud.blolognauk
JWWold dismses of the skis and genitourluary organs In girls
and women. Trach.delo no-4t423-424 AP 060. OCMA 13 t 6)
1. Itlyevskly gorodskoy Imshno-venerologicheekly dispenser.
(OMMATITZ ORGARS, FMALB--DISUSIS)
(ANUBIONCS)

KARYSHEVA, K.O., prof.; SOBOLEVSKAYA, O.P. [Sobolovalka, O.P.);
CHEIERINSKAYA, K.S.,[Ghemerynslka, K.S.]
Treatment of young women with chronic gonorrhea with terramYcin.
Ped., akush. i gin. 22 no.6:62-63 160. (MIRA 3-4:10)
1. Kiivslkiy misl4y sh!drno-venerologicbniy dispanser (golovniy
likar - A.S.Ivanov), viddil gonorologii (naukoviy kerivnik - prof.
K.O.Karisheva).
(TERPAMIN) (GONORPJEA)

~V i 'iO8 '91166 EtIT(m)/hWA(d)/~W(t)/EIVP(k)Awp(z)Awp(b)/EWA(C.)
X_~C NR, AP6=60T SOURCE CODE: LIR/0129/65/000/012/002T/0030
AUMOR: Yuferov, V. M:,; Chemerinskaya, R. I.; Lezinskaya, Ye. Ys.; Vovsina, A. D.;
Karpenko, V. P. .1, 44's yr, 5- r i
ORG: UkrNITI
C4 U S 1~
TITLE: Deform2ion-induced martensitic trans .format-ionin lKhl5N9S3B steel
YY' f'~
SOURCE: Metallovedeniye i termicheskeya obrabotka metallov, no. 12, 1965, 27-30
TOPIC TAGS: steel, austenitic steel, stainless steel, steel tube, tube.rolling, cold
rolling, warm rolling, steel austenite, austenite transformation, martensitic trans-
fromation/lKWN983B.steel
ABSTRACT: Cold rolling of lKhLl5N9S3BIsteel tubes presents serious difficulties owing
to the formation of large --70-70%) of martensite.
amounts This martensite appears
~to be the only cause of difficulties since it has been proved experimentally th at
the steel in fully austenitic condition is not. age-hardenable. Tensile tests at 20
to 500C showed that deformation at temperatures below-150C promotes martensitic
transformation. . The maximum,anount of martensite (40-57%) forms with deformation
at 20C. Additional annealing at". 850C (after annealing at 1100C) intensifies the
martensite formation. Annealing of cold-rolled.-tubg"llat 450-700C brings about a
reversed alpha-to-gamma transformation, but in following cold working, the austenite
transforms back into martensite.' Examination of a tube section taken from a stopped
tme. 620.l8.-66q.'l4.oi8.8--

L 10891-66
AM NR: Ap6ooo6O7
-cold-rolling mill showed that, as.-the redu ction increases from 0 to'38%, the amount of
martensite increases from..O..3,to,38% and the hardness, from 235 to 388 HBI At this
point,; apbarentlk~, the temperature of the metal becoiiies higher than 150C, and no more
martensitd- is formed with a furthp~- increase in reduction to 45%. On the basis of the
11 above experiments, Ilware' rollingPis recomrm-nded for LXhl5N9S3B steel tubes; either
the. tubes should be preheated to 300-350C- before entering the cold-ro 9
or - the. mill rolls should be preheated. The rolling should be-done without a coolant.
w0rig.,art. has: 4 figures,- JDVI
:SUB.00DE: 11, 13/ SUBM DATE-'-~ ,-none/ ATD PrMS: 4#72-
Cind 272

inzhoner; CHMNIRIIVMWA. R.1., inchoner
Iffect of the I*Mft of Skm1p bmatlM tim on the quality of pipe.
stall 15 no.6:537-540 Jo 155. (KM 8:8)
1. Pervauralloldy Novetrubnyy saved. (Rallm (Notolmork))
(Pipe, Stool)

133-12-17/26
AUTHORS: Vashchenko, Yu.I.,and Uhemerinskaya, R.I Engineers.
TITIE: On the Problem of Limitation of Control Tests of Rolled
Products for Hair Cracks on Metallurgical Works (K voprosy
o sokrashchenii kontrollnykh ispytaniy na volosoviny na
metallurgicheskikh zavodakh)
PERIODICAL: Stall, 1957, No.12, p. 1119 (USSR)
ABSTRACT: The authors support the proposal of S.N. Filipov
(Standarizatsiya, 1955, No.6) and Z.B. Kalinina (S~tall, 1957,
ho.2) on limiting the number of control tests of rolled
products for hair cracks, as the test consumes a considerable
amount of metal without giving a real evaluation of its quality.
There are 2 Slavic references.
ASSOCIATION: Pervourallsk Rovotrubnyy Works (Pervourallskiy
Bovotrubnyy zavod)
AVAILABLE: Library of Congress
Card 1/1

STASEVICHY P.K;; FREYBLRG, M.A,; OSLON, N.L.; CHEMERINSKAYA, R.I.;
KOMIANY L.T.; MOSKALENKO, V.I.
Drawing unamealed.carbon steel tubes without mandrels.
Stall 21 no.8:725-727 A# 161. (MUU 14:9)
1. Pervourallskiy novotrubnyy zavod.
(Deep driving (Metalwork)) (Pipet Steel)

OSTRENKOP V.Ya.; YIJFEROV, V.M.; GEYKO, I.K.; TYR, V.R.; OSLON, N.A.;
CHEICRIVSKAYA, R.I.; VILIYAMS, O.S.; IAGUTINA, R.V.
''
Pipe production from new heat-resistant ferritic-martensitic
steels. Stall 23 no. 3:258-263 Mr 164. (MIRA 17:5)
1. Ukrainskiy nauchno-issledovatellskiy trubnyy institut,
Pervourallskiy novotrubnyy zavod i Nikopollskiy yuzhnotrubnyy
zavod.

, 13 Ul'? C, 1114 (11! 1', ,V . ,. . ,tt,; t ,' I k T k r
OSLON, N.L.; KOKIMAINI, L,V.;J~~IjRFR
- -L I j , M-ji,
V.A, ....
Investigating the effect of ingut metal density on the quality of
internal pipe surfaces made of 'Mh15 steel. stall 24 no.6-,529-530
Je 164. 411P'A 17-tPI
1. Permskiy politekhnicheskiy institut i Pervanrallskiy Ncvctriibnv-v,
zav0d.

L 30055-65 Efl(mlllFd?!W)lFjiA(d)ITI&iP(t)IE.P(k)li7dP(b) Pf-4 MN/JD/hW
4 000/-'00'*1'/0* 0-491005-27
ACCESSION NR: APS00297 9/0133/65/
iAUMOR: rlyatskovskiy, 0. A.(Doct6r of technical 6~iences); Yuferov, V. K.(Candi-
date of technical scienc 'Pavloysay, B. G (Engineer); Voron . V. M. (Enginver)l
Y&.(EngIneerT-. -Vovaina A. D.(Engineer)t Cheseri
Lezinskan, Ye~
itEngineer); Karpenko; V. 8.4~g _;.Zh. V. N. Owe
jT1TLE* Mastering the produ 9S35 steel
IMURUM: btall, no. 1, 1965, 49-52
)TOPIC TAGS: steel pipe, pipe rolling, austonite steel, martensite steelg at&inles&#.
.'steel stainless steel pipe, steel phase transformation / steel lXhl5N993D I
'ABSTIUCT: Phase transformations of austenite Into martensite in lWhl5
N9S3B stain-
less steil during cold deformation has been taken into consideration in developing
:the technology of hot-and cold-rolled pipes. The sartensite point F4,for the de-
iforastion of this steel lie* around ISOC and.,the range Of reversal from
,rrtens to
,to oustenite to between 500 and 700C. Was* production of thinwalled 15N9S33
tool pipe to quite-possible If the car material is free of ponmetallic Impurities
i7nitrides and carbanitrides). The above stool type (-1P302)u,4iffero from
.jby having a 3% lower Cc contest substituted by 3 1: it Kas Interesting proper-:
ILCWd In
- ----------

WS14BVNR- AP5002974
A
ties:
thus, its ductility changes during hot deforestion and the breakdown of un-
stable austeiiite into martensite taken place during cold deformetion. Tests on the
Aot rolling of forged 90 = diameter billets are described In great detail. Great i"; 4
W.
accum~lationa of nitrides were observed. Cut-out samples were subjected to tensile
strength tests at various temperatures and the content of the ferro-magnetic alpha.
phase was determined. On the basis of these tests, the following procedure was re-:, f
comended: first pass@* of cold rolling are to be done at 130C. Ready pipes are
onsiderably
heat treated at 1050-1100C. This steel has a tendency to be hardened c
by cold working but b"t.treatmant later remove* this hardness nearly completely.
Despite martensits formation, cold rolling was astisf tory up to 60% deformstim
Cold drawing was also satisfactory szeept for crackticre there was considerable,
accumulation of nitride impurities. "G. X. Syusin and S. X. W=nstsaw participated
to the work." Orig. art.'bas: 6 It
p s an tables.
VXMI ftweizaboyy ssvod'("Novotruhnyy"'plait)
ASSOCUnox ~7. 'j,
SUIMMM: 00 VXLS 00 M comi M
W REF SM: OW OM I ON.

YUYL;ICV, V.M.; qlBNffiI%KAYA,
LEZINSKAYA, Ye.Ya.; VOVSINA, A.D.;
Martrinaite transformation during the deforma-tIon of IKhl5N9C3B
stee Metalloved. i term. obr. met. no. 12:27-30 D 1659
(MIRA 18:12)
1. Ukrainskiy nauchno-issladovatellskiy trubnyy institut.

ACC NR: lIP7003873 S 61~c'-_66DE: UR/0133/67/000/001/0070/0072
0
A'U-,L'HOR: Kaufman, M. Sh.; Aleshin, V. A.; Chemerinskaya, R. I.;,Dovbenko, R. P.;
~n__d_
r
Moiseyev, G. P.; Kuznetsov, B. N.; Aleks ovskw kova, M. A.
ORG: Pervoural'sk New-Tube Plant (Pervoural'skiy novotrubnyy zavod)
TITLE: Manufacture of tubes from EI-711 steel
SOURCE: Stall, no. .1, 1967, 70-72
TOPIC TAGS: me-rivL. tube. chromium manganese nickel steel, titanium containjr
steel, tensile strength, yield stress, elongation 01-711 steel
ABST RACT, BI-711 steel (Khl4Gl4N3T) has been substituted for Khl8N1OT steel (AlSl-32:
in tube production at the Pervoural'sk New-Tube plant. Tube blanks, 50 mm in diamete
and 250 mn, long, are heated up to 1100, 1150 or 1180C and pierced into shell cases
50 mm in diameter and 500-550 mm long, with a 6.5 mm wall thickness. Shell cases
heated up to 1180C before piercing have the best interior surface. The shell cases
are hot rolled to 83 x 6.5 mm, warm-rolled (at 100-150C) to 32 x 2.7 mm, cold-rolled
to 18 x 0.9 mm, and finally cold-drawn into 10 x 1.0 mm tubes. The mechanical
properties of finished tubes in the heat-treated condition were: tensile strength
75-78 kg/mm-2, yield strength 37-43 kg/=2, and elongation 44-56%. Orig. art. has:
2 figures and 2 tables.
SUB CODE: 11, 13/ SUBK:IkATE: none/ ORIG REP: 002/ OTH-REF: 001/
Card 1/1 UDC: 621.774.35

CHEMERIS., G. I. Cand fed Sci -- (dies) YMN "Tuberculosis and
V& Antitubercular Measures in Galicia Within the
IIWJ,AAVV)C~.)
Ow Present FourNO-blasts or the UkrainianIg SSR Prior To Their
f#nIon With the Soviet Ukraine (1870-1939)-" LIvov, 1957. 18 pp 22
(LIvov State Medical Inst), 200 copies (KL, 28-57, 112)
- 41 -

--
From the history of tuberculosis control in Galicia. Trach.delo
40.8:885 Ag 157. (Kw 10:8)
1. LIvovskly amuchno-Imeledovatel'skly institut tubarkuless
(muchW rukovoditell - prof. I.T.Stukelo)
(MUCU--TMMUU)SIS)

CHEMMS, I.I.; SERR SKIY, A*I.
The UZDV-2 ultrasonic disperser for the preparation of objects
for -electron microscopes. A".i prib. no.407-W O-D '62.
16s1)
ji Swaskoy savod elektronnykh aikroakopov i elektroavt
(Blectron microscope-Technique)

BELAVTSEVA, Ye.M.; GUMARGALIYEVA, K.Z.; CHEMERIS, I.I.; DONOVSKIY-YAnCHUK, A.G.
---------
Use of the UZDN-l ultrasonic disperser in electron microscopy. Zav.lab.
30 no.12tl478-1480 164. WRA 18-1)
1. Institut elementoorganicheskikh soyedineniy AN SSSR.

BERBINOVSKIY, A~I.; ~E-Rrsf 1J,
Ultrasonic disperser for preparing electron microscope objects. Zav.1ab.
30 no.12sl5l6-1517 164* (MIRA 18:1)
1. Sumakoy zavod elektronnykh mikroskopov i elekiroavtomatiki.

L 49?5!!4q- - W/ZWT(m)jEFF'C
ACC NR3 "5026681 SOURCE CODE: UR/0073/6,r,/031/010/1071/1073
14P kA NSP
'AUTHOR! TLq~l Solomko, V.P.; Chemeris, 4P.
ORG: Kiev State University im. T. G. ShevchenkX'Yevskiy gosudarstvennyy-u'dversiteqC3 J
TITLE: Dispersive acceleration of radical pobMEizationllv~tl%~~
SOURCE- Ukrainskiy khimicheskiy zhurnal, v. 31, no. 10, 1965, 1071-1073
:TOPIC TAGS: radical polymerization, vibration effect, polymetbyl methacrylate, hydrogen
bonding
ABSTRACT: The dispersive acceleration of radical polyg-*erization of vinyl monomers was
studied during the vibration milling of _montrnortUonitels Cause of the acceleration is a facili-
tation of the radical decomposition of the adsorbed Wtiator under the influence of the impact'
loads. A rise in temperature decreases the effectiveness of the phenomenon as a result of a
decreased adsorption of the initiator (benzoyl peroxide) and an acceleration of its decomposi-
tion in the homogeneous phase. When montmorWonite is dispersed in a medium of vinyl
mon s n chemical grafting of the polymer to the solid surface takes place. olymethyl
P
m "
mel-MO; Niate, not extractable with boiling benzene forms as a result of the bindir A its
hacy 19
macromoleL3O-1 is to the hydroxyl-containing surface of montmorillonite by hydrogen-bond,7 i
forces. A lowering of temperature promotes the formation of bound polymethyl methacrylate,
since under, these conditions a larger amount of polymer is formed in the immediate
vicinity of the solid surface.. Orig. art. has: .3 figures and I table,
SUB CODE: GC SUBM DATE: 29MaY65 ORIG REP: 004 / OTH REP. 003
CaM
UDC 541.64

LIKHVA?,,, Daniil Fedorovich[IOkhvar, D.F.]; CJI4M-US,-Fatr-UimQyjc4
[Chemerys, F.K.]s aspirant; GURENK6- V.A.(Hurenko, V.A.].
y
red.; VLASYUK, P.A., akademik, otv. red.: NAMICHUK.. O.A.,
tekhn. red.
[Companion croppIng of corn with pulse for silage] Sumisne vy-
roshchuvannia kukuxadzy z zernobobovymy na sylos. Kyiv,, 1961.
45 P. (Tovarystvo dlia posbyrennia po:LitycbMkh i naukovykh
znan' Ukrainslkoi RSR. Ser.5, no.24) (14M 15:42)
1. Chlen-korrespondent Ukrainskoy akadevii sel'skokhozyaystven-
nykh nauk (for Iikhvar). 2. Vsesoyuznaya akademiya 981'sko-
khozyaystvennykh nauk im. V.I.Lenina, Akademiya naUk USSR i
Ulxainskaya akademiya sel, slcokhozyaystvenrWkh nauk (for Vlasvuk),,,
(Companion crops) (Ensilage)

CHEMERIS, S., general-mayor teklinicheskikh voysk
War work of military drivers. I~rl. i snab. Sov. V:)or. Sil 21
no.6:46-48 Je 161. (MIRA 14:8)
(World War, 1939-1945--Transportation)

GAT MiO,, N.F.; PROSIMINp A.A.; Q~~~T.A.; , KOVALENKOv 19.A.;
GOLUBCHENKOl-I.T.
Production of mrboa.dimafide. Gaz. prce. 5 no. 3.2:46-49 D 160*
(mm 14:1)
(Carbon dimdfide) (Gam l Natural)

SOURCE CODE.
AtrfHOR: Qladyshev, G. I.; Chemeris, V M.
ORG: none.
TITLE: Automatic-vide-band wavemeter forthe microwave region
10
SOURCE: Izmeritellnaya tekhnika, no._9,.i965, 47-4g..
TOPIC TAGS- frequency meter'll-centimeter wave, microwave detector, videband detection
ABSTRACT;, A description is given of- a wavemeter developed both for continuous visual
observation of the frequency spectfum of a generator of up t6.200 Me at I = 2.9 cm
.and up to 900 Me atX=3.8 cm andfor the measurement of preliminary power distribution
with respect t o the spectrum of generated frequencies. It can also be used as a sen-
sitive detector for the adjustment and testing of shf instruments. The operation of
the device is based on the method of successive analysis by a passive filter in the
form of a torroidal resonator. The electrical portion of the instrument is a two-
stage amplifier using one 6N9S tube and ,a trigger using one 6N8S tube for shaping
negative quenching pulses * Separate shifters-are provideaTor controlling the scan-
ning voltage and thequen1hing pulses. The sensitivity of the instrument is no lover
than 100 uv, and its resolution, vhich is determined by the Q of the resonator, is no
higher thah 40 Me. Orig. art. has: 3 figures. [JR11
6
SUB CODE: EC/ SUBM DATE: none/ ATD PRESS:
UDC: 621-31T.763.02Q-4h

CHOMIS. V.S.
Behavior of a derivative on the boundary of reflectod dowdus.
Dope AN URSR no.5: 425-428 455. (NLVA 9-3)
1. lilvalkly derzhavniy universitet. Predstaviv diysniy chlen
AN UM O.Yu. lahlinolkiy.
(punctiono)