SCIENTIFIC ABSTRACT UMANSKIY, YA.S. - ULPE, YA.YA.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001857920008-1
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: March 14, 2001
• Sequence Number: 8
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

26623-66. UNTW/EWP(t) Ij~(c) JD
UR
ACC NR: AP502537i SOURCE CODE: /0181/65/007/01.0/29.5812961
AUTH0R:. kLyr_Ya I Prildpskiyj V, 1.
ORG: Moscow Institute of Steel and Alloys (Hoskovskiy institul: stali i splavov)
temperature
TITLE: Elastic oscillation spectra and characteristic* a of itertian um
and silicon
SOURCE: Fizika tverdogo tela, V. 7, no. 10, 1965, 2958-2961
TOPIC TACS. germanium, silicon, elastic oscillation
X-ray characteristic temperatures (0m) of germanium.and silicon from
elastic oscillation spectrum were-computed. Values of x-ray characteristic.temr-
peraturec obtained from the spectra coincide well with the experimental values.
of the authors. Calculations as to actual spectra indicate that mean ranges
of the spectrum contribute the most to the summatiofi during temperatures approach.
ing absolute zero. This is also confirmed by the disagreement of 0 with the
value of 0 determined by the elastic.modulus method, The elastic Jduli method
provideo:values of 9 which depend only on- the initial long wave portion of thp-
spectrum, This also explains the good agreement of'clastic ind beat capaci
ty
L C A -I Z
g

_car -

ACC
f jkP6032052 SOURCE CODE: UR/0148 66/ooo/oog/0115/0119
J
AUTHOR: Varli, K. V.; Skakov, Yu. A.; Uzaanskiy, Ya. S.; Shpitsberg, A. L.
ORG: Moscow Steel and Alloys Institute (Moskovskiy insttut stali i oplavoy)
TITLE: Effect of molybdenum on the 'phase composition and microstructure of chromium-
nickel steels
SOURCE: IVUZ. Chernaya metallurgiya, no. 9, 1966, 115-119
TOPIC TAGS: chromium nickel alloy, molybdenum containing alloy, titanium containing
alloy, alloy structure, aIloy property, alloy heat treatment A/M.5 C_
c!j'r.,~V.L m I ('WO G*'7rRV0.7WR,* OrEF Aj, E~k
I- 0.1<
ABSTRACT: The effect of molyb&num (from 0 to 9%) 'on structural changes in chromium-
nickel steels (17% Cr, 7.5% Ni) has been investigated. The hardness of steels con-
taining'4.3% or more molybdenum significantly increased after water quenching-firom.
1200C and aging in the range 500-900C; the structure of this steel consisted of a-
and y-phases. The x phase was formed after quenching from 1000C, and the amount of
a-phase decreased sharply. In steels containing up to 2.3% molybdenum, quenched from
900C, the content of a-phase increased, that of y-pbase decreased, and the steels
became magnetic. In steels with 4.3-5.9% molybdenum, quenching from 900C reduced
the content of cc-phase but caused the formation of x-pheze, the ainount of which
increased with increasing molybdenum content. However, with moly7.3denum content
increased to the content'of x-phase decreased and the structure consisted mainly of
Card 1.12 imav 669.i5-l94:669.26124.o46.51:669.28.62o.i83:54i.4:L2

NRj Av 4n .7 -,)n r'q
2
y-phase. An increase of molybdenum from 2.3 to 5.9% increased the* amount of 6-ferrite',
from 30 to 70%. Maximum hardness (400 HV) was obtained in steels contairAing
ff
molybdenum after aging at 850C. No hardness.increase was observed in steels with 4A
molybdenum or less aged at the same temperatures. An increase of molybdenum content
and hardness brings about embrittlement in the range 600-1100C. Orig. art.
has: 4 filpres. [AZI
SUB CODE: 11, 13/
Card

~-ACC NRt _A70002 8376 60URCS CODE,
AMHOR: Rostovtsev, N. N.; Surkov, V. S.; Umantsev, D. F,
ORG: none
the west Siberian lowland
TITLE: Geological and geophysical investigations ia
SOURCE: International Geological Congress. 22d, New Delhi, 1964. Geologicheskiye
rezullta.ty prikladnoy geofiziki (Geological results of applied geophysics); doklady
sovetakikh geologov, problema 2. Moscow, Izd-vo Nedra, 19651 111-11T
TOPIC TAGS: geologies* Y -8&JZ3b5M1EM, 0'.1A
gravity .1 "q'~
ABSTRACT: An analysis of recent geological studies of the west Siberian lowland is
presented. Geotectonically, the west Siberian lowland forms the -base of the Ural-
Siberian Epihercynian platform. The geological structure of its deep-seated horizons
is hidden under the overburden of Tertiary and Quaternary sediments and hence cannot
be studied by geological surveying. The geological structure of such areas is now
being studied by geophysical methods and deep drilling. The area of the lowland
has been covered by aeromagaetic and gravity surveys, and a great amount of seismic
and electrical prospecting has been conducted. Stratigraphic and. exploratory holes
were drilled at a number of points. This work made it possible to establish the
principal features of the geological structure of the lowlands an, a Whole, and to
Card

ACC ~ NRs
investigate some of the areas in' detail. The west' Siberian platform consists of
two structural stages: the folded basement and the sedimentary overburden. The
aeromagaetic and gravity surveys have detected folded units of the, platform basement
which are reflected in. Yesozoic and Cenozoic platform overburden &x gentle rampart-
like uplifts. The same investigations have established the the heterogeneity of the
basement and the presence of intermontane Paleozoic depressions in the basement. A
sand and clay series of the Mesozoic and Cenozoic platform overburden proved to be
favorable for seismological surveys, which, in combination with deep bore holes and
the data of aeromagpetic and gravity surveys, made it possible to outline the geneal
features of the geological structure of the overburden and to -study some areas in
detail. The seismic survey. located and prepared for drilling numerous loci i
Tnanv nf whinh have nroved to contain co rical renerveo-of oil-and vase. Or-
Card 212

-Hisamutdenovich; USTIMENKO, I.L., red.; BAKHTIYAROV, I.,
re
(Industrial development of Soviet Uzbekistan; an account of its
history and economy] Promyshlennoo razvitie Sovetskogo Uzbekintana;
istoriko-skonomicheekii ochark. Tashkent, Gos.istd-vo Uzbekskoi SSR,
1958. 243 -P. (MIRA 12:3)
Mbekistan--Industries)

ULIMASOV, A.U., kand. ekon. nauk; ULIMASBAYEV Sh N doktor ekon.
9 u= -IL
nauk; DZHAMAIDV, O.B., doMr -ekon. nauk; BLIVIO, I.B.., kand.
ekon. nauk; KHDDZHAYF.V, S.M.,, kand.ekon. nauk; RASULEV, M.,
kand. ekon. nauk; SABIRDV, Kh.R., kand.ekon. nauk; SAFAYEV, A.S.,
kand. ekon. nauk; ABDULLAYEV, M.A.p kand. ist. imuk; ABDURAIMOV,
M.A., kand. ist. nauk, red.; AMINOV, A.M., doktor ekon. nauk,, red.;
MILIMAN, Z.A., red.; GORIKOVAYA, Z.P., takhn. red.
[History of the national economy of Uzbekistan]Istoriia, narodno-
go khoziaiatva Uzbekistana. Tashkent., Izd-vo k1cad. nauk Uzbek-
okbi SSR. Vol.le 1962. 389 p. (MIRA 16:1)
1. Akademiya nauk Uzbekskoy SSR, Tasbkend. Institut ekonomiki.
(Uzbekistan-Economic conditions)

A-!XMT+--Akhmad-Ul!manu-i-chl-DZHAKALOY, O.B. 0 prof., dcktor ekon.nauk,
otv.rod,; KNOPOT, B.L. rod.; BARTSMA, V.P.. takhn.red.
(Nationalization of industry in Soviet Turkestan] Hatnionali-
zataiia promyshlennosti v Sovetskom Turloistane. Tashkent. Izd-vo
Akadenauk Uzbekskol SM, 153 p.
(KIRA 14.-~)
(Turkeotan-Government ownerahip)
(Turkaotan-Industrial organization)

UL'MASOV A U . kand. ekon. nauk; ULIMASBAYEV, Sh,N., doktor ekon.
naUK; 1)1/,HAMAWV, 0. B. v doktor skon. nauk; BLIBER, I. B. 0 kand.
ekon. nauk; KHDDZHA7EV, S.M., kand.ekon. nauk; RASULEV, mv
kand. ekon. naukl SABIROV, MR., kand.okons nauk; SAFAYEV, A.S.,
kand. skon. nauk; ABDULLAYEV, M.A., kand. ist. nauk; ABDURAIM3V,
M.A.,'iand. into nauk, red.; AMINOV, A.M., doktor skon. nauk, red.;
MILIMAN, Z.A., red.; GORIKOVAYA, Z.P., tekhn. red.
[History of the national economy of Uzbekistan]lstoriia narodno-
go khozWstva Uzbekistana. Tashkent, Izd-vo Akad. nauk Uzbek-
.okkbi SSR. Vol.l. 1962. 389 p. (MIRA. 16:1)
1. Akademiya nauk Uzbekskoy SSR, Tashkend. Institut ekonomiki.
(Uzbekistar.-Economic conditions)

DZHAMALOV2 O.B., doktor ekon. nauk; VOLOTKO, N.A.; YUN, D.N.j
kand, ekon. nauk; FOFONOV, B.M., kand, ekon. nwak;
KALYAKIN, P.V., kand.ekon. nauk; DMATCHIKOV, B.A.,
kand. ekon. nauk; KHUDKOVSKIY, A.B., kand. ekun. nauk;
ARTYKOV, A.,, kand. ekon. nauk; FOKIN, A.I.i_ UL"I-4ASOV-,`--A.)
kand. ekon. nauk; YAKOVENKO, Ye., red.; BAKHTI'YAROV, A.p
tekhn. red.
[Principles of the economics of Uzbekistan industry] Osno-
vy ekonomiki prorayshlennosti Uzbekistana; uchebnoe posobie
Tashkent, Gosizdat UzSSR, 1963. 282 p. (MIRA 17:1)

orlov 01- To il--
1. A. a 0 0 P40 A. I. Koricina.
This c-d1lectlon of papers is Intended for those. engaged
An. reseircit- on and design--of nomogrtiphm,

collected Papers- on Nomography SOV16352
TABLE OF CONTEWTS:'.
-Editor's Preifabe. 3
:j Khov~tnsklyj. Go S.,# Moscovid Nolwgraph -and Its
Possibilities 5
Plaoe.:Pf * nomography, In oompOtatlonal mathematics
--of -use -of- nomograme and bl4ipentary
-'-nature of their
theoretical foundation 6
341 Relationships which can be reprenented by namo-.
Brame,
4. .-Toohniquei,~of~,Using..nomograme-
.-~Difflcultieu-ifi the-construction of nomogramrs. ~q
:uSe,
of nomograms Ana yeis~and investigation
or 1
10
70 Use of ftdmograms-in~a.typical-deoign:
' 11
~The ourrent state-of nomosmphy-
8.
9. .-On. methods:- foi 'the furtherAevelopmeht of n.01no-
'
by

gmp
13

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10

a apm-~ on: N(im ft0h VA

IX-0 - Fe1rdrMn,--.Y4
Soluti of lowe Prob-
'
1ems of.Sohlicht
Confortal Mapping
6o'
Aij., Nwaow.~ Graphio DoOtOlration oJI No-
on n 16,
m ta,With the'Ald of a Novi 5 d'a,
t

C'Ous
16 Theorem on the:exiatena o
an orthappal f
in 7, the'
determinition of a Stiel
tjes. Integral, ..71
,
h
the n mownt of the
GraphIL9 d6teirmination of -
2,
_
.
a-rem. oIf,a- gure
fi 74
moving for the- graphic- detariAnation,of the

seas 6f - the. centers' of .'gravity of thq~ aireas
abaci
bounded by the -,curves 77
40 Grapfit~ - determi%tion,'. with the aid :of moving
r
An moment. of the area. of a figure
scalo, of the. W 82
ne~:~
Oirerjko~,_ -Vblgograd,--..-
New
-~Xethod of Atalig
_
.
_
_N mi -;,H%v1ngan, Orl4nttd,, Moving. Scale -
omos~m 1102
cad-'5~10

-Collected Papers on Nomography' SOV/6,352
$0.
XX. IBAkh'Alb'~,- F.'s V

gWomo rams
va v s nstpuatih 9.
_
for Solutions of Diffe-mntial'Equations 180
-of thw
Ye Projeative Equivalanoo'
_Obtdined'by Kdl1bgg'd'Meth6d for an
Wom Iograitis
Eque a Order.
ation of the.ThIrd Nomographi .188

XXII ]Kldz 'I'mi Y R Siilutibn rob
n' e' '76f theI, 3 4~i of

io -'for an
Ariamorphod . ftm#on of the-Third Nomo-
.192
~ - BVkhvaIov'- A,-7M* Rdpiiesent0ions by'Xomograms
XXITX
I
of Equations-of Aligned Point- of Zero 'Genus 205

- * A I " f the gmpirio-*
A M' epresentat on o
hvalbV,, R
-Th
oil RolationshIps'Betwedh ree Variables, Given
inVabular Form W Romo9mms of Aligmid Points
:of.Zero Genus. 212,

rd, OA -0,

ULIMASOV~ N. (Moskva)
ft-~
Nomogram constructed from allgned points for solving a three-
parameter transcendental equation. Nom. sbor. no.1:39,44 162.
(MM 16:5)
(Nomography (Mathematica))

UWMA,SOV, N.; KHOVANSKIY, G.S., doktor tekhn. nauk, otv. red.;
-ORLOVA, I.A... red.
(Nomograms for the bydraulic design of sowerage networks)
Nomogrammy dlia gidravlicheskogo rasch6ta kanalizatsion-
nykh setei. Moskva, VTs AN SSSR, 1964. 30 p.
(MIRA 17:8)

ULIMASOV, N. (Moskva) I/
Nomographingtbe hydraulic calculation of circular pipez, using
Fedorovis iormula. Nom. abor. no.206-47 164.
Nomograms for analysing certain equations in bydraidice.
Ibid.:48-52 (MIRA 180)

UL I MAS Ov I N.
. . . .. ........ 7,~~ ". -
Nomograms for the calculation of sewer systems. Vod.i san.
tekh. no.4tl5-17 Ap 165. (MIRA 191l)

KHAMRABAYEV., I.Kh.; URUNBAYEV, K.; RA]31N(IVICH, A.V.j NEUMMOHEV, N.Ye.,-
,-gVA,,,M.
~~'W
Distribution of rare alkalies and thallium in the rocks
and minerals of granitoid massifs in western Uzbekistan
and the central part of the Cbatkal-K=.-ama Rangeti. Uzb-
geol. zhur. 7 no.3:26-34 163- (MM 16-11)
1. Institut geologii imeni Xh.M. Abdullayeva All UZSSR,

-6-"V-1-13112 Inter -1 d. Dec 4c)
0 ma rrP
7041. CIRCULATORY CHA14GES IN MARATHON RACE RUN14ERS - Observations
concernant lea modifications circulatoires chez les coureurs de Marathon -
Ulmeanu F C_ Cioranu V., Clejan L. and Moldoveanu G.
_P . e - ysiol., Inst. de Culture Phys.. Bucarest - AIED.SPORTIVA
1958, 12/1 (20-33)
During 4 consecutive years the authors examined Marathon race runners in the
International Athletic Competitions at Bucharest. Examinatiom; were made of
the athletes some days before the competition and also before and after the race.
Heart rate and arterial pressure were measured. An ECG and both teleroentgeno-
grams and kymograrns were made. Additional studies included blood counts,
haematocrit, blood sugar variations, serum protein changes, Ca and K levels,
and cholinesterase activity. The hindrance phenomenon of Domiggio was studied in
the urine, as well as microscopic examination and routine chemical tests. After
the end of the race the increased heart rate persisted for some time. Systolic
blood pressure was elevated only in the fastest runners. Some of those who arrived
latest were in a state of circulatory collapse with systolic prevaure around 70 mm.
Hg. These had intense thirst, somnolence and cold extremitiec. Minor neurological
findings such as changes In the retinal vessels and pyramidal tract Irritation -
hyper-reflexia and positive Babinski tests - were also noted. X -ray kymography re-
vealed diminution in the cardiac shadow. Haematological findings included a mark-
ed leucocytosis and variable changes in the red blood count. Depressed blood sugar
and Ca levels- were noted. 7be cholinesterase values were increased. Changes in
arterial pressure observed at the end of the race should be carefully studied and
their pathogenesis determined. Training for the rigors of Marathon racing should
be carried out under careful medical control. Lewis - Berkeley. Calif. (XIX, 6)

ULMANU, F. C." prof.; MESTES, E.; RUGENDORFF.. S.W.
Experimental radiomicroangiographic investigations during effort.
ian M Rev. no.1$273-274 Ja-Mr 161.
1. Chair of Physiology of the Institute of Physical Culture. Head of
the Chairs Professor F.C. Ulmeanu.
(EXERTION physiology) (BLOOD CIRCULATION)
(ANGIOGRAPHY experimentAl) .1

ULIaR, JL.N.
%WU __
Stratigrapby and history of the formation of lover Carboniferoua
deposits of the Moscow Basin (an lysis of the structrure of deposits
of formation cycles and its practical application). Trudy Inst.
geol.nauk. no-90:70-73 '47. (MLRL 9:11)
(Moscow Basin--coal geolocr)

UttM, A. 1.
n1mer, A. I. - "Caesarean operations in the Maternity Hospital Im. prof. Snegireva
for a ten year period (1936-1945).." Collection dedicated to the Maternity Hospitel
In. Snegirevag laningrad, 1949,, p. 124,36
SO: U-4355, 14 August 53, (Letopin 'M=rnal Inykh Statey, No. 15, 1949)

uUmm, T-.
Fundenental principles employed in the processinE- of viscose rayon, especially of
knitting yarns, ano the developuent of - new lubrl4cant.
p. 81 (Veda a Vyzkum v F-mimyslu TertJllnim. No. 1, 1956, Praha, zechoslovokia)
Eonthly Index of East European Accessions (ELEJiT) LC. Vol. 7, no. 2,
February 1958

UIMI K.
Contribution to fundamental questions concerning the finish treatment. p, 65,
TEXTIL. (Ministeretvo lehkeho prurWolu) Praha,, Czechoslovakia. Vol. 14, no. 2,
Feb. 1959.
Mond0y list of East European Accessions (EEAI), IC, Vol. 8, no. 10, Oct. 1959. Uncl.

U124.&R, X.; BRUB, &.,- TRIETSCH, FJO; K9*TTI, W.j HE$S, W.
Adhesion of metals* Technika 7 no.6-.2 Je 163.

KAKHNOVSKIY, I.M.; WIER, V.S.
Methodology of electro-oscillograph . Yardio!V-)Zlia 5 ri.2:84-
Y
85 Mr-Ap 165. (ff-I.RA 18:7)
1. Kafedra fakulltetskoy terapii (zav. - prof. V.N.Vinogradov)
I Moskovskogo ordena Lenina Meditsinskogo insti-tuta Lmeni I.M.
Sechenova.

r'"- ffl
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r" v(CA twice a
00 ~"Y with 4 2-hr- 1111mal just before cluddlOth And tile -00
o0 a :1 AllulloW fluid and the urine of tile newly txwm were le,,Ied -00
forthfildrus. The firdt puttion, of the uline we" neg.' ot
00 -2111Y PWtive; the next wtre strongly paq.; and tiam 100
J *e drug could bc found eved 48 hrs. After birth. The lee
00 a
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AT Iftis were Illso Made After an oral " -W ce.
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(r- fron, the dent. The urine of the newly born con -
go .3 Lailled tracm only in a few cases, the remaining cow,
00 a It IS LVIWIUd-d t hAt t he Mill itio(je 111clul jf&lle j,
i1wrioruble to while streptucide. but not Ill rt~l. .I.he fill. lee
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BRONNIKOVA, M.A.; GARKAVIp A.S.; MASIS, T.M.; ULIMERO V.E.
-- --- ------
Group differentiation of himn fetuses (isoserolqgical systems ABO,
HNSs., P, and-Rh). Sud.-med. ekspert. 5 no.1:31-37 Ja-Mr 162.
(MM 15 4)
1. Nauchno-iseledovatellskiy inatitut sudebnoy meditsiny (dir.
prof. V.I.Prozoravskiy) lUnisterstva zdravookhransaill"-SSR.
(BLOOD GROUPS) (FETUS)

BRONNIKOVA, M.A.; GARKAVI, A.S.; MASIS, T.M.; ULIMER, V.E.
Characteristics of the methods and technique for studying blood
group differentiation in human fetuses. Sud.-med.ekspert. 5 no-3:
30-34 JI-S 162. (MIU lrl-.9)
1. Nauchno-issledovateliskiy institut sudebnoy meditsiny (dir. -
prof. V.I.Prozorovskiy) Ministerstva zdravookhranenJ.ya SSSR.
(BLOOD GROUPS)' (FETUS)

ERMMVA, M.A.; GAMVI, A.S.; MASIS, T.H.;_RMT4~2J.E.
Identification of agglutinogens of the ABD isoserological system
and P agglutinogen in the body tissues of human fetuses. Sud.-med.
ekspert. 6 no.1:37-39 A-Hr '63. (MIRA 16s2)
1. Nauchno-iseledovatellskiy inatitut sudetnoy meditsiny (dir. -
prof. V.I. F~!ozorovskiy) Ministerstva zdravDokhraneniya SSSR.
(AGGLUTINOGENS) (FETUSS)

BRONNIKOVA, M.A.; GOKAVI, A.S.; MASIS, T.M.; ULIMER, V.E.
Characteristics of the development of the ABO isoserological
system in human fetuses. Sud.-med. eksperto 8 no.1:21-25 Ja-
Mr 165. (MIRA 18;5)
1. Nauchno-iseledovateliskiy institut sudebnoy meditsiny (dir.
prof. V.I.Prozorovsk-4y, Ministerstva zdravookhraneniya SSSR,
Moskva.

r I.T.1 LAVIKOVA, V.Yet.-, MIJ;INDEMI, S.V.) ITRUSOV, A.V., ULIMISIEEK, G.F.;
KHENVINO T.I.
Upper-371ermUji and Trlas3lc sedimantz of the -westarn wnd n::rthern
parts of the north-C,Ltsplan iAl- and gas-bearing baain. (Tmdy-l
UlLneftegaza no.10".236-256 163. (MIRA :L87.,3)
1. Naiiehnc-isolpdrvatellakaya..l%b,,-,ratorl&7.u geologrichoskikh
luriteriyev ctaenk-l parspaktIv n&ftegnzonf)sncstij NizJmav-r,*Izhuki7
nauchno-Assledovatallskiy institut aeologii i geofizAl 1.
Vo3gogradski-y nauchao-l-ssladcvat~E:I'jkiy Institut neftyanoy :1
gazovoy, promyshlennosti.

GRACHEVSKIYI M.M.; MARINBERGp S.V.; MOZRAYEV, N.S.; ULI~agjjEK G~F.
Lower Kazan uncompen-gated trough in Oren~firg Provin-ceo rieftegaz,
geol.i geofiz. no.9:20-24 163. (MIRA 17:3)
1. Nauchno-issledovatel'skaya laboratoriya geologicheskikh kriteri-
yev otsenki perspektiv neftegazonosnosti Gosudarstvennogo geologi-
cheskogo komiteta. SSSR.

ULIML':T-EK.-, KHEINV,/~-Nll I'ATISKOVA, V.Ye.; URUSOV, A.V.
nwe--Perm~,an 2ed',Ments of the western and northera partL
Of the nor4-.h-Casplan and gaB-baaring basin. (Trady]
no.-SO.21-2-J-235 163. (MIRA 180)
1. Nau~hrc - s I ed ova'. el 'skayq laboratoriya geologicheskikh
krl-:,c-,riy~--~,, persp-iiktiv nel-tegazonosr,03ti-, Nizhnevolzhakly
I.nst,ltat geolog i i geo'll z'k!- i
ly inslUtut rieftyanoy i
a,~c c;myah') c-nc.~3%~

WMISHEK, L. G -
"The Production of Electric Incandescent Lamps" (Proizvodstvo elek'tricheskil-h
nakalivaniya), Gosenergoizdat, 1949, 444 pp.

----
NILUMAR, R-A, prof.; 70MIN, V.N., inzh.; UL'MISHM, L.G.. h.
The electric lamp Industry in the U.3.S.R. during the past 40 years.
Svetotekhnflm 3 zio.llrlO-14 N 157. (NM 10:12)
1. Moskovskly elektrolenpovyy zavod.
(Blectric lamps)

:ULIMIM=oI-tw-Grlgorly9Tioh; '24LA INMY9 B&L,,, rad,'l 7IMNIN, A.M., tek~hn.
r~4
[Pk6dmCtlOl2 of Ine'Wesiceint lamP63 Proisvodatv6 e:Loictriobaskikh
1DAT niamilTMAI&O isdA. sauovo parer*' Hoskra, (N)so- auerg,
izd-yo, 19380 535 Po* Wootric Ismse, -Incaudescomt) (KMA 12tIO)

- 21~,-,~-., ~K --I~i I
, WHISM, L.G., inzh.
Concerning a review of the government standard on ordinary filament
lamps. Svototeldinika 5 no.4:1-7 Ap '59. (MIRA 13:1)
l.kookovskiy elektrolampoyyy zavod.
- (Blectric ifLne)

- PLOMM V,L
Remats of using seismologic data in stadying thet d esper stractwe
of the w&Ws crust in Central Asia.,' Izv. AN SSSR. Ser.geofiv.
no.10t1307-1319 0 162. (HM 16t2)
1, Mentral*naya seyamicheskaya stantaiya "Tashkent* Institata
matematiki AN Usbekskoy SSR.
(goviet Central Asia-Seismology) (Zarth-~face)

3(7),3(10)

AUTHOR: OV166-59-2-911.1.
Ulomov,V.I. S
TITLE: Regional Cut of the Earth's Crust in Central Asia arl the
Cardinality of Sediments in V Re6lon P Tashkont (Regionalinyy
razrez zemnoy kory v-Sredne.Y Xzii i moshchaost' nanosov v
pritashkentskom rayone)
PERIODICAL: Izvestiya Akademii nauk Uzbekskoy SSR, Seriya fizlk~-

F'959,~*,Nr 2,.Pp 70-82
matexatloh*alfikh (USSR)
ABSTRACT: The paper contains the results of the evaluation of a heavy
explosion carried out by the Academy of Sciences of the USSR on
December 19, 1957 ca. 100 km to *the north of Tashkent.
Oscillograms of the explosion oscillations taken by 29 seismo-
logical stations were evaluated. The abundant material of
observation permitted to construct a proftle of the earth's
crust of 1000 km length taking its course in south-eastern
~h
direction. The profile is extended from the 68th to the 78
degree of longitude and lies between %P - 380 and%F = 449. The
author givesthe course of the layers of granite and basalt as
well as the surface of Mokhorovict,ioh (Compare f-Ref 4_.,7).
Oard 1/2

Regional GLut of the Earth's Crust in Central Asia c;OV/166-59-2-9/11
and the Cardinality of Sediments in the Domain of TasEkent
Simultaneously the width of the alluvial 'Layer in the domain of
Tashkent was measured, where the data of observation of the
explosions on August 3, 1952 and April 12, 1953 were also used.
The author mentions D.P.Kirnos, Ye.M.Butovskaya, and N.P.
Vasillkovskiy.
There are 3 tables, 7 figures, and 15 Soviet references.
.ASSOCIATION:Inatitut matematiki i mekhaniki imeni V.1.Romanovskogo AN Uz-SS~R
(Institute of Mathematics and Mechanics imeni V.I.Romanovskiy
of.the AS Uz.SSR)
SUBMITTED: October 28, 1958
Card 2/2

Zen
u 0 -d
4
~74
IJ.
. ffl A .
a X~ to to
ISO,
zp
1A
a
i ;
a

V04,9/60/000/ol./015/027
9201/E191
AUTHOR: __Ulomov, V.I.
TITLE: Some Properties of the Earth's Crust 11tructure in
Central Asia Determined from the Recordings of a Strong
Explosion
PERIODICAL: Izvestiya Akademii nauk SUR, Beriya geofizicheskayaq
1960, No 1~ pp 131-134
T=t The paper reports some of the results of an analysis of
seismograms obtained after a powerful explosion on 19th December
1957 about 100 km north of Tashkent. The vibrations produced by
the explosion were recorded by 29 permanent and temporary seismic
stations, and from these recordings the author obtained a cross-
section of the crust along a line 1000 km long, shown as I-I in
Fig 1. This line was in the north-easterly direction and extended
from the Tadzhik depression to the northern slopos of the Tien Shan
mountains. The cross-section (Fig 2a) shows that the Mohorovicie
discontinuity lies mostly at a depth of 50 km, rising in the
Northern Tien Shan region by 10-15 km. Configuration of the
Mohorovicic surface in the northermost end of the section was
Card 1/3

s/o4q/6p/Ooo/oi/ol5/o27
B201/E191
Some Properties of the Earth's Crust Structure in Central Asia
Determined from the Recordings of a atrong Explosion
rather doubtful because the results were unreliable. The depth of
the basalt layer varied by more than the Kohorovicic discontinuity.
The greatest thickness of basalt (about 40 km) was found in the
region where the Southern Tien Shan joins the Fergana, depression;
the lowest depth (about 10 km) occurred in the Tadzhik depression.
Comparison of the results discussed above with those obtained by
deep seismic sounding along three profiles (Fig 2Q making various
angles with the I-I line and with gravimetric dat& (upper parts of
Figs 2a and 26) showed satisfactory agreement. Calculation showed
that increase of the negative gravitational anomaly in the northern
part of the profile is related to a. lowering of the basalt and
Mohorovicic. boundaries.. The minimum of the negative anomaly in the
region where the Fergana depression joins Southern TIKn Shan is. due
to the basalt layer being thicker there. A negativegravitational
.anomaly maximum at the junction of Southera Tien Shan OEM
Tadzhik depression is due to reduction of the thickness of the
basalt layer. Acknowledgements are made to Ye.M. Butovskaya for
Card 2/3

s/o1fq/6o/ooo/oi,/oi5/O27
E201/H191
Some Properties of the Earth' s Crus,t Structure in Central Asia
Determined from the Recordings of a Strong Explosion
supply of the seismograms and for her advice.
There are 2 figures and 12 Soviet references.
ASSOCIATION% Akademiya nauk SSSR, Institut fiziki zemli
(Institute of Physics of the Earth, Acad. Sci,
Usain-
SUBMITTED: May 12, 1959
Card 3/3

88747
3"9300 S1166J601000100610071008
C111/C222
AUTHORt =RSnL-L1--
TITLEt Statistic Investigation of Near Earthquakes and the Structure of
the Earth's Crust in Central Asia
FERIODICALs Izvestiya Akademii nauk Uzbekskoy SSR, Seriya fiziko-
matematicheskikh naukt 1960, No. 6, PP- 78 - 91
TEXTs The author proposes a new method for the investigation of the
structure of the earth's crust. The method is based on the evaluation of
those times in which the elastic waves of near earthquakes reaoh-the
seiomologic stations. Por a diminution of numerous random errors the author
chooses earthquakes with a common origin or earthquakes the origins of
which are not far from eachother. 96 earthquakes were treated statisticallyp
where the earthquake on April 15, 19551 in Ul gohat in Sin'tozyan
(coordinates of the epicenter LP - 39.9 9 p ~ - 74.6 N) served as a base.
The author calculated the time in which the longitudinal waves P* and P
of these earthquakes, interpreted as principal waves corresponding to the
basalt boundary and the Mokhorovich boundary, respeotivelyt reached the
seismologic stations (22 stations in distances from 205 to 650 km), Prom
Card 1/ 7

88747
S/166
,/60/000/006/007/008-
C111/C222
Statistic Investigation of Near Earthquakes and the Structure of the
Earth's Crust in Central Asia
these data there resulted the charts of the isochronous curves for the
waves PW and P.
Card 2/7

3(
0

887417
3/166/60/000/006/007/008
C111[C222
Statistic Investigation of Near Earthquakes and the Structure of the
Earth's Crust in Central Asia
Figure I i Chart of the isochronoua curves for Pt t
1. Points of observation ; 2. Lines of the observed field of isochronous
curves ; 3. Lines of the normal field 4. Izolines of the difference of
the observed and the normal field 5- Epicenter to which -the orlculations
are related.
Then the charts of isochronous curves were used for obtaining from them
the charts of the isodepths. For the construction of the surface of the
basalt layer the author assumed that the layer over it has a mean velocity
of 5.7 km/see 1 for the basalt layer he assumed a mean velocity of 6.4 km/
sec. The Mokhorovich - surface was calculated with and without a
consideration of the refraction at the basalt - granite boundary. The
results of the calculations are summarized in two charts for the isodepthe
and in 3 cuttings through the region. E.g. the figure 10 schematically
shows the propagation of the seismic waves P# and P from the origin to
the station Andiz:han.
Card 5/7

88747
S/I 661601f)00100 610071008
C111/C222
Statistic Investigation of Near Earthquakes and the Structure of the
Earth's Crust in Central Asia
A"vU -4~, a.
A
I*- re 0 a yn e V. toof 13 'r a C-W 1
I' y a CW.,
C4 ? W. %A it 0
IC
P-
WV% P
k
Fact
Fig. 10. Scheme of the propagation of the waves P* and P (the horizontal
and the vertical scale are equal).
Card 6/T

68747
S/166J60/000/006/007/008
C111/C222
Statistic Investigation of Near Earthquakes and the Structure of the
Earth's Crust in Central Asia
The author mentions N.N. Leonov. There are 10 figures, I table and
14 SoViet references.
ASSOCIATIM Institut matematiki imeni V.I. Romanovskogo AN Uz SSR
(Mathematical Institute V.I. Romanovskiy o2 the Academy of
Sciences Uzbekskays SSR)
SUBMITTEDs xiy 99 196o
X
Card 7/7

BUTOVSKAYAp Ye.M.; KONIKCV; A.T.,- 19RSESOVO I.L*;, PAKp V*A*;
TROSTYANSKIZ, G.D.,- ULOMOV, V.I.; SOKOLUVA., A.A... red.;
J, Z, 'ja - ~-
GCR OKMAYA I., te
(Seismism of Uzbekistan) Seismichno8t' Uzbekistana. Tashkent,,
Izd-vo Akad.nauk Uzbekskoi &M. Vol.l. [The Pergara Valley]
Ferganskaia dolina. 1961. 97 p. (KMA 15:5)
1. Akademiya nauk U!~bekskoy M. Institut matematjjci.
(Fergana,--Sei=o1ogy)

AUTHOR: Ulomovi V. I,
V-431
S/049/61/000/002/009/012
D242/D301
TITLE: Modeling of the.foci of tectonic.earthcluakes by means
of ultrasonic-emitters
PERIODICAL: Akademiya~nauk SSSR.. Seriya geofizichoskaya.
Izvestiya, no. 2,1961, 255-258
TEXT: Despite theoretical.research.by V. I. Keylis-Borok (Ref. 3:
0 dinamicheakoy kharakteristike ochaga-po seyamichiaskim.nablyudeni-
yam (Dynamic Characteristics of-the Focus.from Seiismic Observations)
Dokl. AN.SSSR, 70, No. 6, 1950) (Ref, 4: K voprosu o opredelenii
dinamicheskikh.parametrov ochaga (Problem.of..Deteruining the
Dynamic Parameters of..the.Focus) Tr. Geofiz..in-ta AN SSSR N
o 9
1950) (Ref . 5: K voprosu ob . issledovanii. istochnikov, ekivalentaykh
ochagam.zemletryaseniy (Problem of Studying.Sources Similat, to
Earthquake..Foci)'Tr..Geofiz..in-ta.AN SSSR, No. 9, 1950) A. V.
Vvedenskaya-(Ref. 9:-Ob qpredelenii napryazheniy.deystvuyushchikh
vocbag'akh zemletryaseniy,, po-.nablyudeniyam:seysmicheskikh-.stantsiy
Wetermination-of Stresses Acting..at-Earthquake..Foci-from Obser-
Card V 7

22431
S/049/61/000/002/009/012
Modeling of.th; foci... D242/D301
vatious.at Seismic.Stations)t AN Nauk SSSR, Ser. Geofiz., No. 4,-
1960) on the displacement fields.of.different-types of.fractures,
the problem of the dynamic,-parometers.of.earthquake- foci has not
lost.its.urgency. Such a study may clarify.the features of move-
ments at the. foci. of.- earthquakes -and. may also. verify... the accuracy
of existing-theoretical methods.for,determining.tIx.- dynamic para-
meters of these foci. Available.data-suggest-that fracturing
accompanied,by sliding is..the most-probable form of..dislocation
at earthquake..foci,.so it is.necessary.to.create..artific:Lal foci
simulating-fracturing accomRanied-by sliding.and.-other-.taovements.
The,widely-used ultrasonic.method.developed.by.Yu. V. Riznichenko
(Ref..10:,Modelirovaniye,seysmicheskikh-.yavleniy (Simulation of
Seismic.Phenomena) Vest. AN SSSR, No. 5,, 1952) Yu. V. Riznichenko,
B. Nz Ivakin and B. R. Bugrov (Ref. 11: Modeliroveniye seysmich-
eskikh voln (Simulation-of.Seismic Waves) Izv. Akad. Nauk
SSSR, Ser. Geofiz., No. 5, 1951) appears to be the most effective
method, but.the equipment.for.modeling seismic waves largely con-
Card 2/7

:,S/049/61/000/002/009/012
D.242/D301
Modeling.of the foci.
sists of point emitters. pnd. cannot simulate,,an. earthquake focus.
The',author.therefore made-an.emitter'with the..same distribution
of forces.as is.the cas'e.at an actual focus .with the.help of a
special piezoelectric.transmitter.. Tectonic-fracturing-takes place
as a result cEiniUal. 6lastic'Btresses.which.. exceed. the. durability
of the material-constituting the medium,,and,parts of.the medium
situated on differen't sides of the,fracture.'are displaced in
opposite directions. Similar movements may.be.obtained by in-
stalling-two freely-sliding plates whose.outer,-surfaces..are firmly
glued to.the material of the medium.and displacing them-in opposites
directions. . Thel esseiitial.difference. between- the.-natural- and arti-;',
ficial.movementq.is..tfiat-the former.are.due to.tangential elastic
stresses-which &crease A-the moment of fracture.from.a.limiting
-TALil-p the latter create at the. "fracture 11 faces,
value T., to 01
tangential.strespes whidh'Increase from 0 to T. Elastic waves
s
that are propag*ed in the elastic.medium.arise.3-n both cases.
The apparatus usAed by. the- author consists of two blocks _. a sinusoid
al vibratory ge rator forming.right-angled,.electric impulses and
Card 3/7

444-_31
S/049/61/600/602/005/012--
D242/D301
Modeling.of the'foci...
a cathodic oscillograph.. The required.impulses are converted into
mechanical vibrations of. an ultrasonic frequency which.are emitted
by a piezoelectric transmi.tter.in an elastic medivm. Mter pene-
trating the-medium the elastic waves are taken.up by a piezo-
electric receiver with a punctate membrane.and are retonverted
into electric signals.which are scanned, ph~otographed on the screen
of the.oscillograph and produced as..seismogrmns. Fig. 2 illustrates
the design'. and working of the -wave emitter simulating fracture-
type movements; Nos. 1 - 5 denote the piezoelectric transmitter,
plates, rubber urashers,,membrane.and castor
oil respectively. The transmitter consists
of two.rectanplar parallelopipeds cut from
a crystal.of Seignette,salt and is'actuated
by the plates. As electric stress is fed
into the foil facings both parts work'by
compression. -The parallelQpipeds are orien-
ted so that their reverse.piezoelectric Fig. 2.
Oxr. 2. Vci7oftTno:z an"a.
Card 4/7 OP-OMRARB: ';Op... no~ TOZR (a) IL
ema ero Wo.
1130TOP01308 Jdacno 7U

2-2431
S1049V61itOO0100210091012
D242/ T1301.
Modeling of the foci...
effect is in counterphase,.and these movements arc! transmitted to
plates.attached to their working edges. Thug, at the moment of the
input of an impulseAnto- the --emitter,.. the. plates- cause movements, in
the medium-analogous.to fracturing-and-sliding. The emitter simul-
ating,a fracture~.type movement accompanied.by.the turning of one
edge in.relation..to-.the..other is.-more.complex-The piezoelectric
transmitter-consists-of~four.similar-.parallelepipe~ds-mounted on a
cube, and.its working.surface-undergoes-.complex.-de-formation. The
plates.are.attached.to.the working.-surface-of..the.transmitter so
that two parallelQpipeds act-on each plate, thus.turning-one plate
in relation-.to.the other.,.Quasi-periodic...seismic.waves.induced
by impulse.forces.or stresses originate..from fooal,,processes and
are generally. considered -as representing actual.vibrat ions of the
focus. In the model.-the.focal.*vibrations.are caused-by actual
vibrations.of the-piezocrystal. Their-frequency depends on the
crystal size.and may be.calculated.theoretically.or.derived.experi-
inentally, the.attenuation--of.these.vibrations-of-i.-he'-piezotrans-
mitter being-controlled.withih certain limits....Thus, processes
C ard 5P

Modeling-of the foci...
2203.
S/049/61/000/002/009/012
D242/D301
giving-rise..to.earthquakes.at the focus are.replaced in the model
by those taking.~place in.the def romed. crystal which.emits under
impulsq.action.quasi.iperiodie.elastic vibrations. -The amplitude
of the displacements-transmitted-.by.the,plates.to-the medium lies
within the limits of.elastic deformation.of-the.latter so that no
fracturing takes place at.the plate-medium.contacl:, permitting the
repeated reproduction.of..the.process.i,7ithout..undue--distortion and
th7e procurement-of a.fixed image-on the-oscillograph screen. During
simulation -of -a - s liding...f racture.- the -plane of -the platesAs perpen-
dicular to.the observation,surface.. The-diameter of.the area of
contact.of.the..receiver-.with the-medium-As a little-less than a
quarter.the.length of.the receivedwaves. When moving-along the
observational.surface..the-receiver.is turned towards.the emitter
so that any directional.effect..on-.the.recording of..its.sensitivity
is excluded.. The emitter.is.placed in the center of a circle with
a radius of about.twice.the length of the longitudinal waves in the
paraffin, and the receiver.is moved in steps of 22.50 around the
circumference. There are 5 figures and 13 references:.12 Soviet-
Card 6/7

Modeling-of the foci...
M31
S/049/61/000/002/009/012
D242/D301
bloc and-l non-Soviet-bloc. The reference to.the.English-language
publication.reads.as.follows:.F..Press, Elastic.wave radiation from
faults-in ultrasonic models. Publ. Domin. Observ., Ottawa, 20, No.2,
1957.
ASSOCIATION: Akademiya.nauk Uzbekskoy SSR. Institut matematiki im.
V. I. Romanovskogo (Academy of Sciences Uzbek SSR.
Institute of Mathematics im. V. I. Romanovskiy)
SUBMITTED: August 13, 1960
Card 7/7

S11661621000100210021008
B112/B104
AUTHORSt Butovskaya, Ye. M. Dzhunisov) Sh. A.,
Atabayev, Kh. A.p Flenov, Yu. P., Yakovlev, V. H.
TITLE: Specific hodographs of powerful blasts recorded in parts
of Uzbekistan
PERJODICALt Akademiya nauk Uzbekskoy SSR. Izvestiya. -Seriya
fizikoTmatematicheskikh nauk, no. 2, 1962, 34-41
TEXT: Data on powerful blasts recorded in the central Asiatic districts
of Pritashkent and Fergansk are,evafuated. Durations Df the seismic waves
are related in the usual way to uniform standard conditions and their
phases identified by the following procedures (1) Deiermining the
angle of departure of seismic radiation. (2) Correlating the respective
seismograph records. (3) Plotting the amplitude curves. The phase
identification is followdd by composing a universal hodogrdph for all
types of longitudinal and tranoverse.wavou and this ie decomposed into
its basic branches. In addition, the specific hodographe presented here
are derived for the districts under consideration. There are 5 figures
Card.1/2

9036-66 EWT(l)/EWA(h) GW
ACCESSION TIR: AR5013958 ua/616c1/!'15/00O/Wi/G0V:;
/G005
SOMICE 1tcr-,zh..Geofizika, Abs. J1019
Ulomov
_TITIR: Distortion of abyssal relief due to errora in determining the coordinates
of earthcjualw, epicenters
CITED SOURCE: Tr. In-ta matem. AN U7ZSR
vYP- 27, 1963, 156-167
TOPIC TAGS., earthquake, ~Leismic wave eisnic souading., SCISMO&PAPHY
TWISIATION: Evaluation is given of_the~accuracy-of a method developed by the
-author for interpreting surface hodographs of the longitudinal waves due to earth-
quakes. A fbrmula is,derived linking the error in the determination o.L
the loca-
tion of.the refractive layer in the vertical (8h) and horizontal (81) planes, de-
pendin on the~-epicentral distance (R) and the length of the-observed are prorile
(S), with the errors made in determining the epicenter coordinates (�K). A chart
givenfor calculating errors for the range of values S a 100-1500 kin, R - 300-
500 hm, K - �5-20 Ia. The errors viU diminish in proportion to a diminished 3,
'as compared vith R. In order to reduce errors in.determining the underground re-
Card

L 6-66
9031 -
ACCESSION IM: AR5013958
4-
lief it is advisable to select are profiles ohd epicenters. such t~hat the m1nor
axis of.the ellipse of conceptration of the probable location or the epicenter is-
directed aldn the course--or-the pTofile. The method proj*sed is an improvement
of the Interpretation eyetem previo=3~y developed by the cuthor, in 41hich-only the
relative relief of the division boundaries of the earthOscrust haa been determined.
An example is-given of the'a-pplication of the calculationti to the processing of
repeated shocks which had occurred in the Ulugchatskoye earthquakp on April 15,
1955. When K a t5 km, the-errors in determining the bounilary locations in the
north east part of the region for surface M were: &h = +1-2 km, Se = 2:1-3 km; for
:intermediate boundary they were: Sh = +1-4 kn, +37-8 In; in the western part of
'or boundary M they were:
the area f Sh 4 ku, Sk 4. 5 1m; imd for the intermediate
boundary they were: Sh = + 6 ~m, SP- U-2. The indica:.ed accuracy may be at-
to the schemes for the~abyssal structure of the f!arth's crust which had
been developed by the author in his- earlier work. ("Izv. AS UzSSR, Ser. Fizrmat. nadc,
~196O.-no.,6), The schemes are in good agreement with data provided by deep seismic
sounding.
A_ SUB OWE: ES EWL: 00
jW
6(d 2

VLOMSKIT, S.N.
-----------
Role of crustacea in the relative densit7 Of lakia plankton (method of
determining the density of zooplankton of species). Trudy probl.i.teme
sov.no.1:121-2.30 151. (KM 937)
(Fresh-water biology)

1. UL014SKIY, S. N.
2. USSR (6oo)
4. Iset', Lake - Plankton
7. Influence of a swompy watershed and a hydroelectric power station on the develo~-
meat of lake plankton. Trudy Gidrobiol. ob-va No. 4 1951.
9. Monthl List of Russian Accessions, Library of Congress, April _ 1953, Uncl.

1. ULCHSKIY., S. N.
2. ussR 600
4. Plankton - Iset', Lake
7. Influence of a swampy watershed and a hydroelectric po"rer station on the develnp-
ment of lake plankton., Trudy Gidrobiol. ob-va, 4., 1952.
9. Monthly List of Russian Accessions, Library of Crngress2 April 1953., Uncl.

1. ULOMSKIY, S.N.
2. ussR (6co)
4. Copepoda
7. New aspects in the ecology of certain species of Copepoda; Mesocyclops leuckarti
(Claus), 1857, Dokl. AN SSSM 90 no. 2, 1953.
9. Month List of Russian Accessions, Library of Congress,
APRIL
1953, uncl.

a
Conditions for the development of plankton In bodias of water polluted
by waste waters. Trudy Gidroblol.ob-va 7:67-76 '56. (NTJU 10:2)
1. Ural'skoye otdolenlys Yeesoyuznogo n&uchno-issladovatellskogo in-
stituta osernogo I rechnogo khozyuystva.
(Volchikhinskoye Reservoir--Plankton) (Water--Pollution)
1%

VLOKSKIT, S.N.
Aphanizomenon oviaisporum Yorti in the Ural lakies. Bot.mat.
Otd.opor.r&ot. 11:0*33 Ja .156. (MLRL 9:11)
(Shablish, Lo&e--Algas)

UT,OMSKIY. S.H.
Wet weight of crustaceans of Tajikistan rice fields. Trudy AN
Tadzh.SSR 89.#133-140 138. (MBA 13:5)
1. Urallskoye otdoleniye Vvesoyupnogo nauchno-ionledovatel'skogo
instituta ozernogo i redbnogo rybnogo khozyaystva.
(TaJikistan-Crustacea)

KOMM, N.V.; UWMSKIT, S.N.
---- ------ I.,.-.---
Brief characteristics of the hydrological regimen and the
Population of microscopic.organisms of lake Galich. Trudr leb.
sapr. otl. no.7:68-88 159. (MIRA 12:12)
(Galich, lake-Limnology)

UIOHSKIY' S.N.
Plankton formation In Xama (Perm) Reservoir [vith ni-mary in
English]. Zool.xhur. 38 no-1:3-14 Ja '59. OIRL 13:4)
1. Ural Branch of the All-Union Research Institute of lake and
River Fishery Managements, 6verdlovsk.
(Perm ReserToir--Plankton)

ULONSKIT, S.N.
19-wer--crimtaceans, of rice fields in the vicinity of Stalinanbad
and their scologro Trudjv-AVTadzh.BSR1,L2:27-65 159,
(XM 13: 11)
1.. Urallskoye otdolaniye Gosudarstvannogo nim, huc-issledovatell-
skogo instituta ozernogo i rechnogo rybnogo khozy-aystva.
(Stalinabad Distriat--Crustacea)

~L~!LSXKIL_~Rffl___:
Seasonal variations in the population density and biomass
of aquatic organisms in vaters of the Urals. Trudv Gidrobiol.
ob-va M136-157 160. (HIRA 13:9)
(Sverdlovsk Region-Froe h- water biologr)
V_

< 9 W__M - -B. N - -
Variation of taxonomic characters in Zidlaptomus graciloides (IdIl.)
Prustaces, Copepoda) in relation to the environmental conditions.
Zool. zhur. 39 no.9:1312-1323 S 160. (MIRA 13:9)
1. Ural Department of the All-Union Research Institute of Lake and
River Fishory Management, Sverdlovsk.
(Naryk, leke,-Copepoda)

UWMSKIY 0 -A-11 -.
ECO1097 Of MeQOCYCIOPS CMBSUS (B-PiObb-), 1853 (Crustacea,
Copepoda). Dokl.Aj1 SSSR 134 no.2:453-JP56 5 16. (MIRA 13;9)
1. Urallskoye otdeleniye Gosudarstvennogo nauchno-iseledovatell-
skogo instituta ozernogo I rechnogo rybnogo khoz3raystva.
(Ural Mountain region--Copopoda)

ULONSKIYV S.N.
A rare case of bermaphroditiam in Eud#lptomus gra-ciloides (Lill-)
(Crustaceaj, Copepoda) from Kama (Perm) Reservoir. Dokl.. AN SSSR 137
no-3:732-734 Nr 161. (HIPA 14:2)
1. urallskoys otdolenip Gosudarstvennogo.nauchno-isaledovateliskogo
limtituta ozernogo i rechnogo rybnogo kbooaystva.. Predstavleno
akade~iiom Ye.N.Favlovskim.
(Hermaphroditmom) (Kama Reservoir-Copepoda)
i

LESHCHINSKAYA, A.S.;--!MMSKqx S.N., otv,reds; HAKAROVA, N.U., red.izd-va;
TAMWVA, N.F., tekhn.red.
[Zo4lankton and benthos of the ObI Bay as food for fishes)
Zooplankton i bentos Obskoi guby kak komoviaia baza dlia ryb.
Sverdlovsk,, 1962. 75 P. (Akademiia, nauk SSSR. Urallskii filial,
Sverdlovsk. Salekhardskii statsionar. Trudy, no.2).
(KRA 16 :2)
(Obt Bay-FisheeFood)

ULCMSKIY, S.N.
Taxonomic position of cyclops of the subgenus Thermocyclops
Kiefer (Crustacea, Copepoda) in Kayrakum Reservoir. Trudy
Inst. zool. i paraz. AN Tadzh. SSR noo26295-123 1163
(MM 17:3)

ULOMKIY., S.N.
Development of phytoplankton in lakes and reservoirs of the
Urals-and the Ural region. Trudy Gidrobiol. ob-va 13:126-
145 163. (MIRA 16:11)
1. Urallskoye otdeleniye Gosudarstvennogo nauchno-issledovatell-
skogo instituta ozernogo i rechnogo khozyaystva, Sverdlovsk.

S.N., deceasecl]
Characteristics of plankton in some lakes of the trans-Ural peneplain.
Zool. zhur. 4.3 no.9:1388-1"91 164.
(141RA 17: 11)
1. Urallskoye otdeleniye Cosudarstvennogo naucbnc-issledovateliskogo
instituta ozerhogo i rechnogo rybnogo khozyaystva~ Sverdluvsk.

lJL%EKlY9 S.N. (daceased]
F,-ology of apecieB cf the gc-nu.-; 'Me-uricy-l-c-pef
living In the bodies of water of the UraI3 and Ural Mcjuntuln reglori.
7ool.. zhur. 44 no.l.-127-330 "5. M, 1 fa, .9
Urallskoye otdo2enlp, Gosudarstvenflogo
instLtuta ozernogo _i rc~3hnc;go i-ybncg,)

kz~~ Tr
GORIZONTOV, P.D.; KOGAN, A.KR.;ULOVICK, A.I.
Depressor effect.of fish fat in experimental renal hypertension.
Ter. arkh., Moskva 24 no. 3:68-73 Mar-June 1952. (CM 22t4)
1. Of the Department of Pathological Physiology, First Moscow Order
of Lenin 4edical Institute.

/Inffuence ~f naycotics an Surviv al of mi,-
*in 03 Ygen e
Uncy. Yu, .1. Viklilyaz~,v ~!-sd A. 1. Ulovidt ( 3t Med.
1115t., Parmakol. i MoWkat
A& 1
0 tieficiptiev in noice bt uut~vatcd by 11tv-
Owl, Cl,CC1IO.fTIO, chloral,ew, atimNarbital Rfa, und
est. imellsifving effect, M1 thic Small'-st. In
severia 0 defitiency thes---Amp p"ilong t ,, 1110 )f Inim.
The, cfTects are evidently related to tlie witral nervatm
acmating and c-nirolling comp, mq~,tnry
systom functiva in
action in the body, btst t1i mediankm is still obsekirc.

ULOVICH A.I.
Study of the transanimase activity (asparticoaminopherase)
of blood serum by the colorimetric method* Lab.delo 5
no.2:3-6 Mr-Ap '59. (MIU 12:5
1, Iz TSentral'noy nauchno-issledovatellskoy laboratorii
imeni S.I.Chechulina (zav. A.S.Cheohulin) I Hookovskogo
ordem henina meditsinskogo iinstituta imeni I.M.Sechenova.
(TRLNUNIMASE) (COLORIMETRT)

cULOVICK, A. 1.
)bthod for the extir
pation. of the hypophysis in rate. Probl.
endok.1 gorm. 5 no.5:32-39 S-0 159. (NM 13:5)
1. Is Wantrallnoy nauchno-inaledovateliskoy laboratoril Imeni
Prof. 8.1. Chachimlina (sav. - kaud.med.usuk A.S. Chachulin) I
gookovskogo ordena lenina moditsinskogo instituta Imeni I.M.
Sechezi-ma.

ULUVIGH., A.I.
Negative effect of narcotic substances in oxygen starvation. Farm.
toks. 24 no.3s284,288 My-Je 161. (MIRA 25---1)
1. TSentrallnaya nauchno-issledovatel,lakaya laboratoriya imeni
prof. S.I.Chechulina (zav. - kand.med.nauk A.S.Chechulin) I
Moskovskogo ordena Lenina maditsinskogo inatituta imeni I.M.Sechenova.
(AI,IOXUUA) (NAItCOTICS--PhMIOLOGICAL EFFECT)

MOVICH
A.I. (Moskva)
Increased semsitivity and decreased resistance of the body to
narcotics, sedatives and analgesics in oxygen* Arkh.pat. no-3:
60-68 162. (MIRA 15:3)
1. Iz TSentrallnoy nauchno-issledovatellskoy laboratorii imeni
prof. SJ. Chechulina (zav. - kand.med.nauk A.S. Chechiain)
I Mookoviskogo ordena, Lenina meditsinskogo institute. imeni I.M.
Sechenova.
(AIIO=A) (NARCOTICS) (SEDAINES) (AITALGESICS)

ULOYAIII S.M.
Permissible concentrations of buty-ric aldshyde in the air of
industrial premises. Zhur. eksp. i klib. med. 5 no.2:89-95 164'~
.L
(,,,!Ipjt 19:1)

ROOKSy G.Kh.; ULIP, K.A.
--------
Critical comments on internati6nal anatomical nomenclature. Arkh.
anat.gist.i embr. 38 no-3:90-95 Mr 160, , (MIRA 34:5)
1. Kafedry anatomii (zav.-dots. G.Kh.Roolcs) meditsinskogo fakullteta
Tartuskogo josudarstvennogo universiteta.
(ANATOMY-NOMENCLATURE)

IW2j, Ya. Ya.
ULPFG, Ya. Ya. "Hysteresis Losses in Wood for an Asymetric Cycle." Latvian State
U, 19-54 (Dissertation for the Degree of Candidate of Technical Science)
SO: Izves&iya Latviyakoy, SSR. No. 9, Sept., 1955