SCIENTIFIC ABSTRACT LYUBIMOVA, YE.A. - LYUBIMTSEV, A.A.

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• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

BALAKWA, L M.
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AUTHOR: Lyubimova, Ye. A.
TITLE: On the role of radiation
regime of the Earth. (0
teplovom rezhime zemli).
49-5-@ 7'18
heat exchancre in the thermal
0
roli luchistogo teploobmena v
PERIODICAL: "Izvestiya Akademii Nauk, Seriya Geofiziciieskaya'f
(Bulletin of the Ac.Sc., Geophysics Series), 1957, No-5,
pp. '073-676 (U.S.S.R.)
ABSTP,!.'%'T: In investigatinG t1lie temperarure dependence of the thermal
conductivity of the ceramic materials of the %@pe MgO,
Al203, BeO, it was established that for T < 1500 to 1800 C
thermal conductivity decreases, in agreement with the theory.
According to the equation A/Tn wnere a ^-,l and for
T above 1500 to 18OU C, the heat condu9tivity starts to
increase rapidly proportionally with V which cannot be
explained by any of the existing heat conductivity theories.
An explanation can be sought on the assumption that the
heat transfer in solid insulators at very high temperatures
is effected not only by molecular thermal conductivity but
also by radiation heat exchange between the neighbouring
volumes of the substance and this is con-firmed by experiment.
Card 1/3 Since the shell of the Earth consists of substances which
are similar to glass and ceramics, it is very likely that

49-5-1 -@@ /18
On the role of radiation heat exctian-Ee in the
regime of the Earth. (Cont.)
radiation heat exchange plays an important role in the
depths of the Earth. In this paper it is shown triat for
calculations pertainin6 to the depths of the Eartt it is
inadmissible to disregard tlie drop, of the molecular heat
conductivity with the temperature which takes place in the
upper layers of the Earth and prevents considerable
removal of heat from the depth's 'of the Earta and, trierefore,
the Earth cannot solidify quicicly. At@.present the thermal
conductivity at a depth of 100 km is about a third of that
pertaining to surface rocks and the effective thermal
conductivity at a depth of 2000 km increascs three to four
times. Decrease of the thermal conductivity of t1ae upper
layers prevents any appreciable flow of heat from the depths
and as a result of that the depths of the Earth continue to
heat up even now and the thermal history of the Earth has,
Card 2/ 3 generally speaking, the same character as was established in
earlier work of the author (19,20) in considering a constant
coefficient of thermal conductivity. Acknowledgments are
made to B. I. Davidov for his valuable advice and criticism:
There a-re two graphs and 20 references, 7 of which are Slavic.

SUBMITTED: January 29, 1957.
49-5-13/18
ASSOCIATION: Ac.Sc. U.S.S.R. Institute of Physics of the Earth.
(Akademiya Nauk SSSR Institut Fiziki Zemli).
AVAILABLE- Library of Congiess
Card 3/3

WMIMOVA. Y ".. KEYLIS BOROK, V. I., REZNICHENKO, Yu. V., BELOUSOV, V. V., and
MAIGNITSKIY,V. A.,
"Seismological Problems and Questions Concerning the Physiral Struct-ure of
the Ea�th's Deposits."
paper presented at the XIth General Assembly of the Int'l. Union of Geodesy and
Geophysics, Toronto, Canada, 3-14 Sept, 1957 (Izv, Ak Nauk SSSR - Ser. Geog. 1918,
No. 2, PP 3-8 [USSRD.

-4 JIN -7@';
AUTHOR: Lyubim 3.' V5 -4 - 53
TFTLE; The Thermic History and Temperatures of tne -7ar,:-
skays istoriya i temperature @emli;'
PFRIODICAL: Byulleten' Mloskovskogo obshchestva ispyteteley prirody,
Otdel geologicheskiy, 1958, Nr 4, pp 30-49 @@',TSSF@'
ABSTRACT: The author gives a short review of the Intest research results
in the field of the thermic history of the -F'arth, mentioning
in this connection the work of the following scientists:
H. P. Costei ' H. Hughes, T.Rikitake, V.A. 1M.Rovnitskiy, V.N.
Zharkov, 1. @omeranchuk, S.P. Clark,F. Preston, E. van der
Held, V. Gol'dshmidt, V.Q. Fesenkov, N,,', @Ielov, F. Igerch,
K. Bullen, B.T. Davydov, 1. Verkhugen, J.A. Jacobs Allan,
O.Yu. Shmidt, B.Yu. Levin, V,S. Safroncv, ',,. Kuipsr, ':,en-
field-, Ye.A. Lyubimova,H.C. Urey, I.Ye. 'jtarik, M.,.,i- Shats,
W*Rubey J. Wilson, H. Jeffreys and G.S. @,orshkov. '@n the
basis o? these research studies, the author comes to the con-
ClU3ion that as a wnole the Earth cannot ,Ielt as a result of
radioactive heat, but that the phenomenon of Tolten zones
is perfectly possible and that it Is always indevenden@ of
variations of the initial data. Thus, t-e con@itions for
Card 0 that differentiation of the matter necessary for the dynamic

The Thermic ffistory and Temperatures of the Earth SOVI/5-58-4-5//43
force in the formation of the Earth's crust are given. He
states that the secular heat of the Earth's core should lead
to a cortain expansion of the internal zones of the Earth,
but that the external Earth strata show a tendency to cool-
ing off, and that thu -s their volume should be reduced a little.
Consequently, the upper strata lying at the expanding in-
ternal sphere should be subject to an expanding tension.
Considering this effect on the basis of equations of the
theory of elasticity, the conclusion can be drawn that the
radius of the Earth should continuously but irregularly
become larger. This expansion is at the same time an ex-
planation for the occasional ruptures in the crust. All
data given do not contradict the main point of the secular
heat of the Earth's core.Whatever the original temperatures
of the Earth might have been, the fact of a wide dispersion
of radio elements, especially Calium, cannot be denied and
Card 2/3

The Thermic History and TeMDeratures of the Earth SOV/5-r-A-4-5'4@
this again leads to quite different consequences than 'he
theory of a secular cooling off of the Earth and its con-
traction.
There are 6 graphs and 41 references,21 of which are @_oviet
and 20 English.
1. F-arth-Thermodynamic properties 2. Geophysics
Card 3/3

L@tA@ , tA a j A Y@- Pf.
24(8) PHASE I BOOK EXPLOITATION SOV/2768
Vsesoyuznoye soveshchaaiye po geotermichesk-im issiedovaniyam. ist, 1956.
Problemy geotermii i prektichaskogo ispolIzovaaiya tepla zemli; trUAy, t.l.
(Geothermal Problems and the Prac-tical UtilizatIon of Terrestrial Heat;
Transactions of the lst All-Union Conference on Geothermal Investif.91tions,
vol. 1) moseow, rzd-vo AN SSSR, 1959. 254 p. Errata slip in@.arted.
1,300 copies printed.
Sponsoring Agency: AkedemiYa nauk SSSR. Otdeleniye geologo-geogmlpicheskll@h
nauk.
Ed. of Publishing House: L. V. Gessen; Tech. Ed.: I. N. Guseva; Editorial
Board: V. 1. Vlodamts (Chairmn), 1. D. Dargunov (Deceased), V. V.
I-vanov, F. A. Vakareako, and N. I. Khitarov.
PURPOSE: This book is intended for geologists, hydrogeologists, and geophysicists
in geaexal and petroleum and coal geologists in particular.
Card 1/5

Geothermal Problems and the Practical (Cont.) sov/2768
CGIIERAGE: This volume,, one of two published on the subject, is a collection
of 22 articles based on reports presented at the First All-Union Conference
on Geothermal Studies held in March, 1956. The Conference was sponsored
and organized by the laboratory of Vuleanology, the laboratory of Hydro-
geological Problems im. F. P. Savariaskiy, the Tnatitute of Geochemisti-i
and Analytical Chemistry, the Geophysical Tnstitate,
and was attended by rep-
resentatiNes of more than 60 research org%niza-Gions. The material preseuted
in this Irolune may be divided into three general categories: (1) general
geothermal problems of the Earth (2) current status and methods of
geothermal research(3) leginnal geotherml problems. References accompany
bach Article -
TABLE, OF CONTENTS:
Foreword
PART 1. GENERAL GEOTHRRMAL PROBLEMS OF THE EARTH
3
Dergunov, I. D. (Deceased). Contemporary Concepts of the Thermal Regime
of the Earth's Crust
Card 2/5

Geothermal Problems and the Practical (Cont.) sov/2768
L
M0-jg2v.aYe..A- Thermal History of the Earth and Its Geophysical
Consequences 17
Dost.,.)valov, B. N. Tbermodynamic Study of the Far.',h 2`7
I4-u.stikh, Ye. N. The Role of Volcanoes and Thermal Springs in
Carrying Heat Out.-Frem the Earth's Tj:kterior 31
Vl,@davets, V. 1. Basic Types of Steam Hydrothex-m! Fbrmations in
Ita4 and New Zealaud 37
Ogillvi, N. A. Problems in the Theory of Temperature Fields as
Applied to Geothe 1 Methods of Exploration for Sub-
s-i--f-ace Waters 103
Zbiz-manskiy, A. M. Problems of.Geotherml Power lip
PAWF 11. COHTKMFAHY STATE AND MMODS OF
GEOTFEM%L SYUD32S
Card 3/5

Geot-hermal Problems and the Practical (cont. ) SOV/2768
Kraskovkiy, S. A. Some Standing Problems of Geothermal E13search in
the USSR ii.6
Dlyakonov, D. I. Historical Development and Contemporery State of
Geothermal Research in t1he USSR 126
Derganov, D. I. (Deceased) Geotherml Explo-ratiju Yethods I'An
Ovehl nni-Ir v, A. M. Geothermal Study of Mineral Watoear Deposits 142
Bedcher, A. Z. Characteristics of the Geothermal Gradient of Oil
Deposits ija the Kuban' and the application of Tbeer-I Studies to Solve
Oil P-roduction 'Problems 150
PART r1l. REGIONAL OOTHEWAL PHOBLEMS
Dubinskiy, A. Ya. The Geothermal Regime of the Ciscaucasus and
Adjacent Areas 171
Babinets,- A. Ye. Geothermal Conditions in the Ukrainian aad
'Moldavian SS918 190
Card 4/5

Geothermal Problems and the Practical (Cont.) SOV/2768
Kashpur, Ya. N. The State of and the Problems in the
Study of the Geothermal Conditions of 1@-,ep Coal Relds In the Donbass 208
Orda, V. Ya. Geothermal Pagime of the Central Part of the Donbass P-26
Vamkovskiy, V. A. (Daceased) The Geothermics of the Donbass 236
Sogomo3n-V, G. V. Data on the Geothermal Conditions in the Belorus-
skaya SSR and Adjacent Areas 240
Allbov, S. V. Nev Data an the Geothermics of the Crimea 244
Cherewnskiy, G. A. R--sults of Geothermal Studies in Siberia 246
AVXUABLE: Library of Congress
MR/ fal
Card 5/5 12-21-59

9000 3/049/59/000/1-'/017/027
AUTHOR: Lyubimova, :Ye_.,A. E131/E391
TITLE: On the Temperature Gradient in the Upper Layers of the
Earth and an Att- istence of the
empt to Explain the
Low-velocity Layer
PERIODICAL: Izvestiya Akademii nault SSSR, Seriya geofizicheakaya,
1959, Nr 12, pp 1861 -, 1863 (USSR)
ABSTRACT
Cardl/3
In addition to the lovi-velocity layer at 100 km depth,
A.N. Tikhonov (Ref 4) found that heat flow also can be
distinguished at that depth 9 The calculationo shcwed
that during the last 2 X 10 years the temperature
variations in the top layers of the Earth took place very
slowly. Therefore, heat flow can be expressed -as Eq (1)
for the uppermost layer and as Eqs (2) to (5) for n
consecutive layers below that. Taking the top layer
(10 km deep) as the granite, the second (basalt) 30 km
deep and the third - peridotite.. the amount of heat
generated in these three layers, Hi. HO and H_
respectively, can be found as;

C-9236
S/049/59/000/1.2/0171/027
E131/E391
On the Temperature Gradient in the Upper Layers of the Earth and
an Attempt to Explain the Existence of the Low--velocity Layer
H1 = 53-10 -14 Cal/cm3see; H2 =15-10 -14 cal/cm3see;
H., = o.4 . lo- j4 cal/cm3S (_.c
The curve of thermal conductivity of the mantla shows a
minimum at the depth of 100 km (Figure 1). This minimum
causes an increase of the temperature gradient as foJlows.
X, km 4o 5o 6o Bo loo 150 200
dT
-, deg/km 6 13 16 18 19 9 4
dx
The temperature distribution in the continental cru-st
is given in Figure 2, which shows that the difference of'
temperatures under continents and oc@eans can reach 300 to
400,C. The horizontal gradient of the, temperature is
Card2/3

b -"J 2 36
S/049/59/000/12/017/02-,
E131/E391
On the Temperature Gradient in the UpI)er Layers of the Earth and an
Attempt to Explain the Existence of the Low-velocity Layer
considered as the cause of the convective transfer of
heat.
There are 2 figures and 12 references, 5- of which are
Soviet, 06 English and 1 Italian.
ASSOCIATION: Akademiya nauk SSSR Institut f'izik-1 Zemli
(Institute of Pbysics of the Earth, Ac.Sc.USSR)
SUBMITTED: January 20, 1959
Card 3/3

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@tn=63t-. This Lowar of the mr asotions of tbw Enstl- of Mystet of the tarlh
1-1 To. glawidt -talzo %,rtIcLPw on thoomt1cmi probl- in -tlmloxy @l on
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ft,,blPs of Intaryretation Of Mncip&l jyy,,gOl%ritl-
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or. boa.1 - g-il .1tit=t&S obtained by L. T-I to 11,1B 1-f.
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Of 5011A TAIA= to tb- PlAts,11L@ Ph---
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rthque.l.. 121
A -thod f@r MAO@In4 th. of
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t_j If' ys@ of ob..".-LI.- C- C-
vorthwot of tbo Dollshay Sa.11hu sountsin range (T@@uvmly-). -@I-
-lxAw that tbA wthod dscribol to cu@nrsoor, tit that 1- 1,
b7 the ftw*ltir4 slapUfleation, of nods-I lirs pLotting for Ihi
b". M ftrWL3. Miss. Th. ro-Its of this tly. b-4 on
ths, Tookl[Ill"IM1. tneplakonS7. So"vologicbealtals nl@podltwiy% T
cmuln" Expedition) vot-rk of stations, ard or,
tke. Ut.-tam,' indi&&U thAt 'Ithout proli.1-7 or
obso,r-ttoo, them to on mseon for o-ral.1 study It a re, mgiI, r
isooh-d.. osr *%rtbq.W-, ow It. v&o. p-.Ing of -7 Y.- rf ib.--
tioeso ftr any parpoxe whnt@r. T.14s, pri=lplo t t1w b- ,f -S@
orthod ftr etndrlolc tkw pre-slo.t atrikee and dips, Abirts Of dAx_Ib!lllltt-,
4tc.,CM be wppurd In ttw solution Of a @bor of otber PrvbZoa. 4@ mr.
wootutt- - wevottned.

LYU13IMOVA, TFt.A-.,-
- --- 11
On conditions of magmatism origin and role of volcanic actvity, in the
thermal regime of earth's crust.
Paper presented at the 12th General Assmbly of the IUGG
Helsinki, Finland July 1960

LYUBIKOVA. Te.A.; LYUSOTA, L.B.; FIRWY. F.V.;STARIKOVA. G-ji.; SHIJSHPANOV, A-P-
Determination of surface heat flow in Staraya Ustsesta. Izv. AN
SSSR. Ser. geofiz. no.12:1806-1811 D 160. (HIBA 13:12)
1. Institut fiziki Zemli AN SSSR.,
(Earth temperature)

LYUBIMOVA, Ye.A.
Sources of the internal heat of the earth. Vop.kosm, 3497-108
162. 04I@' 15.-7)
(Earth temperature)

LYUBIMVA, Ye.A.
Tharmoelastic stresses inside the earth. Trudy Inst. fiz.
Zem. no.20:51-56 162. (KRA 15:3)
(Earth temperature) (Seismology)

LYUBIKOVA, Ye.A.
---------------
Distribution of thermoeldAtic stresses inside the earth and the
.speed of their accumulati6n. Izv. Ali SSSR. Ser. geofiz.
no.3085-:396 Mr '63. (MIRA 16:3)
1. Institut fiziki Zemli AN SSSR.
(Earth temperature)

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'. T, I E 1 IM ';V A , "@- , , . , , (; @l 7 , S;.' IY I V, A
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:1- :tpa ."m T 1 c -1 -- - -, - -10 , () " . t 1.11-1 Fl, A 1 -11 - @' )l

,-LYULIMOU, Ye.".., kand. fiz.-7aterr.. nauk, otv. red.
ar _ . .. r,
- @ p
(Geothermal studies ,, Geotermichesxie L;slerjov 4 4 1 1
1 . . (,/
slrva, Izd-vo Nauka, 1964. 173 P. (Vj.@, 17:"'
1. Akadei.,iya nauk SZSil- In::titut fiziki Ze,71i.

1MCVA Y-- -A. , karid. f iz.-mater- * .' : ';'::l`V, G.B. , karid. geol . -minera I .
nauk
The goo the rinaj' expect i tion "Anp. '@ @r- I . '14,-t. AN' 'j I, no . 1:
59-64 ja 65. ( MI P A 18 - 2 ;

LYUBD4GVA, Ye.A.; TJDIVrSEV, G.B.
Expedition on the American scientific research ship "Argo".
Geofiz. biul. no.15:79-83 165. (MITRA 18:11)

J 46202-66 Otrr(l) GW
ArC NRI AP6028797 SOURCE CODE: UR/0033/66/043/004/0837/0845
AUTHOR: Lyubimova, Ye. A.
ORG: Institute of Phvsics of the Earth . Academy of Sciences, SSSR (In-t
fiziki Zemli--hkademii nauk SSSR) q,I
TITLE: Distribution of heat-flow,and thermal processes In the earth's
mantle
SOURCE: Astronomicheskiy zhurnal, v. 43, no. 4. 1966, 837-845
TOPIC TAGS: earth mantle, terrestrial heat flow,_===1= seismicity,
ABSTRACT: Data on the distribution of heat flow in different regions
of the earth's crust are analyzed, and regional histograms for the USSR
given. The world map depicting heat flow compiled by Lee and Uyeda
[Review of Ifeat Flow Data. Geoph. Monograph no B. Terrestrial Heat
Flow, Am. Geophys. Union. Publ., no. 1288, k 5651 is revised to
include pertinent data for the SoVet Union. Heat flow is classified
as anomalously low (0.6-0.9).Io- 12. ec in the region of ancient
0-gal/cn
crystalline shields, normal 1.4*1 cal/cin see in the r@gion of
platforms and troughs, and anomalously high (1-8-3.0)'10-0 cal/cm2
see in active regions of the earth's crust. Fig. 1 shows the
distribution of heat-flow stations In the USSR and heat-flow values
recorded throughout the country. In magnitude and quahtity, annual
Card --1/3 --- UDC: 525.215

Pig. 1. Map of the
distribution of thq
values of heat flow
in the USSR contodr
lines encircle area
of near-Q values'--
- Heat flow stationi
91 - amoun of heat
:
flow In 10-@ cal cm2
sec.
ACC NR1 AP6028797

ACC NR- AP6028797
earthquake records rate the Baykal region as one of the most seismically
active regions in the world. The Baykal# Stavropol Trans-Carpath-j
ian, and Przhevallsk regions have records of high heat flow;
Kazakhstan, the Russian platform, and the Crimean platform have avexage:
readings; the Black Sea region shows relatively low values. Anomalies
of heat flow are also analyzed. Orig. art. has: 15 figures. EDMI
SUB CODE: 08/ SUBM DATE: llDec65/ ORIG REP: 015/ OTH REF: 012
Card

ACC NRI A-165035091
AUZIOR: Lyubiznova, Ye. A.; Shelyagin, V. A.; Shushpanav, A. P.
:CiG: none
TITLE: Instrumentation for determination of the plutonic heat flux
.SOURCE: AN SSSR. Institut fiziki Zem.1i. Problemy glubinnogo teplovogo potoka
(Problems of heat flow in theearths's interior). Moscow, Izd-vo Nauka, 1966, 107-132
TOPIC TAaS: heat measurement, heat transfer, conduction heat transfer, convection
,heat transfer, geology, earth crust
A3STRACT: The article reviews Soviet and foreign literature dealing with equipment
!and methods for measuring the heat flux from the deep layers of the earth toward its
:surface. J[he difficulties connected with these measurements are very considera 'le
.because L th 2P
of ' a minute values of the heat flux; it is of the order of 1,u, cal/c "see
(the flux from the sun is about thousand times greater). aecent impr6vements in
methods include the substitution of thermometers (thermocouples) by thermistors
I(se-niconductors), which have the advantage of smaller size, and the elimination of
;heavy cables for heat transmission (not practicable for depths of several kilometers)
and si@naling temperature by transmitting ultrasonic waves. Associated problems-heat
,conductivity and heat capacity of rocks-are approached with a variety of methods used
SOURCE CODE: LTR/0000/66/000/000/0107/013?.
Card

AM035091
both in the laboratory and in nature. and by the sationary and the pulse method. The I
requirements for accuracy of temperature measurements are high (� 0.0050C). Finally, 1
in the measurement of the heat exchange at the bottom of the ocean, heat flux by water@
convection must also be considered. Orig. art. has: 9 figures and A equations.
SUB CODE: 08/ 5MM DATEs 07Apr66/ oRiG REF: oog/ oui REF: oo4
Card 2 12-

ACC NR1 AP7002934 SOURCE CODE: UR/0020/66/IT1/006/1321/1@@]
AUTHOR: 1,yubUaavap Ye. A.; Shelyagin, V. A.
ORG: Institute of Physics of the Earth, AcadeW of Sciences, SSSR (Institut fizw
Zemli Akademii nauk SSSR)
TITLE: Heat flow through the bottom of Lake Baykal
SOURCE: AN SSSR. Doklady, V. 171, no. 6, l966, 1321-1324
TOPIC TAGS: qarth themo(brnamics, earthquake, heat measurement, 5o /? M,
4 C @r@ r t-, ^@ Y _F Zl_
ABSTRACT: /In/@iAew- odftt)o'he interest attaching to the region of Lake Baykal, where a
large number of earthquakes still occur, the authors have used an oceanographic pro-
cedure for determining the heat flow by introducing a thermal-gradient gauge into the
bottom of the lake. The work was organized in 1965 by the Institute of Earth Physics
AN SSSR in conjunction with the Limnological Institute and the Institute for the
Earth's Crust of the Siberian Department of AN SSSR, using the research vessel "G.
Yu. Vereshchagin." The construction of the thermal-gradient gauge was described
elsewhere (Apparatura dlya opredelenlya teplavogo, potoka (Apparatus for Heat-flux
Determination], Nauka, 1965). The heat flux was measured at depths greater than
700 meters. The test procedure is briefly described. A table listing the heat flux
in different locations is presented, and the arithmetic mean of the flux is found
to be 2.6 X 10-' Cal/CO2 sec. Before the true heat flux can be calculated it is
necessary to determine the influence of topographic irregularities, the role of the
r_4 1/2 UDC: 550-361

A%-'- NKz AYPD29.@4
cold water mass, and the role of the river deposits an the bottom of the lake. It
is tentatively estimated that all these factors will increase the average heat flux
by 23%, raising it to 3.2 x 10-8 cal/c=2 see. nis report was presented by
Academician A. P. Vinogradov 3 February 1966. OrIg. art. has: 3 figures, 2 formulas
and 2 tables.
SUB CODE: 08/ SUBM DATE& 1TJarb6/ MG W.- 009/ om 1w: 004
2/2

LINIKOVA, N.P.-,_@@fUBIMQVA A.
, -le-
Index of literature on psycholog7 publiahed in 1959. Vop.
psikhol. 6 to.4:149-186 Jl-k- 16o. (MIRA 13:9)
(Bi bl i ography-Puychol ogy)

LYUBINDVA, Ye.D.
Books on psychology published in 1960. Vop.psikhol. 7 no.2:163-
168 Mr-Ap, 161. (MM 14:6)
(Bibliography-Psychology)

EERSZINA, G.A.;_jMBIMDVA, Ye.D.
Index of literature. on psychoma published,$b 1961. Pp. psi-khol.
8 no.5:124-162 3-0 !6;0 1. (MM 16:5)
(BibliographAP
sychology)
-A-

BEREZINA, G.A.; LYUBDIOVA, Ye.D.
B11 iography of the literature an psychology published in
190. VoP. paikhol. no.5@153-186 S-0 164 (mlm 1-8@1)

LYUBIMOVA, YE- I.
LYUBD!OVA, Y--I, I.: "Diseases of the sunflower plant under conditions of
iroldavia and measures to combat them." Min Higher Education USSR.
KharIkov Order of Labor Red Banner Agricultiiral Inst inc-ni V. V.
Dokuchayev. KharIkov, 1956
(Dissertation for the degree of Candidate of Biological Sciences)
SO: Knizhnaya Letopis, No 36-P 1956, Moscow.
P

LYUBIMOVA, Ye.I., kand.biolog.nauk; TSIJFT@OVA, T.T., lab-yf-49-it-tekhnIk
microhora of the retting liquor in case of the modified twc-phase
retting of kenaf and jute bast. Mauch.-issl.trudy TSNIILV 17:
36-" 162. (MIRA 16:10)

LYUBMVA, Ye.I.0 starshiy naucmriv./ sotrudnik; RAU, N.V., ml4dshiy nauchnyj
5otrudriik
Biological testing of textile fabrics for resistance to the action
of fungi and bacteria. Nauch.-isal.trudy TSNIILV l7tl48-153 162.
(MIRA 16:10)

LYUBINOVA,Ye.L.
Botanical and geographical investigation of the southern area of
the subarctic Urals. Trudy Inst.geog. no.64:201-241 155.
(Ural Mountains--Phytogeography) (MY-RA 8:11)

LYUBIMOVA, Ye.L.
Studies on the vegetation of natural zones of'7#osoow Prcmince. Trudy
I
Inst. geog. no.71:-42-82 '57. - (HIBA 10:9)
(Moscow Province--Botany)

LYUBIMDVA, Ye.L., kand.geogr.nank
Snow piles in the Moscow area. Priroda 49 no-5:128 My 16o.
(MM 13:5)
1. Institut geografii AN SSSH, Roakwa.
(Moscow Province-Snow)

LTUBIMOVA, Te.L.. lmnd.geograficheakikh nauk
Flowering of vegetation in the forest. Pr1roda 49 no.8:326-127
Ag l6o. (KIRA 13:8)
1. Inatttut geografii AN SSSR, Moskva.
(Forest ecology)

Y4UBIKOVA,- Yelena Llvovq@t RIKHM, G.D., otv.red.; NIKCLI&KAYA, V.V.,
otv.red..- Mfdiff. T*H*q red*; XONOTALYU19 19K., m1adahly red*;
KALICMEKLY. G.N.. red.kart; KOSRZMA, S.K., telchn.red.
i
(Kamchatka: phyeicomographical study] Kamchatka; fisiko-geogra-
fichaskil ochark, Moskva, Gos.izd-vo geogr.lit-rT 1961.
(Kamchatka--Physical geography) . -0 1 @V 51r.

LYUBIMOVAq Ye.L.9 kand.geograf.nauk
Snow and subalpine vegetation. Priroda 50 no. 2:125-126
F 61. (MIRA 14:2)
1. Institut geografii AN SSSR, Moskva.
(Alpine flora) 0 @j -..- Pe
. 4.&-Vw

LYUBIMDVA, Ye.L.,, kand.geograficheskikh nauk
In tha Siberian steppe. Priroda 50 no.6:125 Je 161. (MIRA 14:5)
I* Insiltut geogra-fii AN SSSR, Moskva.
(Siberia-Spring)

LYUBIMOVAp Ye.L.
Vertical divisions of the vegetation in the forest zom of the
East European Plain. Biul.MIP.Otd.geol. 37 no.2.*168 Mr-Ap
162. (MIU 15:7)
(East European Plain-Pbytogeography)

Lyubimova, Yelena Llvovna
Geography Of Kamchatka. Washington, U.S.JPRS. 1963.
191 P. Illus., Maps (JM: 17.336)
Translation Of The Original Russian; Kamchatka
Fiziko-Geograficheskiy Ocherk, Moscow. 1961.
Bibliography: P. 173-191

LYUBIMVA, Ye.L.; XAZAREVSKIY, O.R.
Conference on the problems of onaftastics and toponymy. Izv.AN
SSSR.Ser.geog. no.22153-156 Mr-Ap 163. (KIRA 16:4)
(Names, Geographical-Congresses)

LYUBIMDVAI- IGILI.-
Conference on the principles of toponymy. Izv.Vses,geog.d@.va
95 no.lslO2-104 Ja-F 063. KIRA 16:4)
(Names, Geographical-Congresses)

LYUBIWVA, Ye. L.; MURZAYEV, E. M., Moscow
"Place-name evidence of former geographic conditions on the Russian Plain."
report submitted for presentation at the 20th Intl Geographical Cong, 6 Jul-
ii Aug 64, London.

&nt
'cn:
Fr)ci mo -, k ov I a
( , - @ 1 -, ;, 1 7 : I Z )

LYUBIMOVA, Ye.L.; KHOTINSHY, N.A.
Frospecis for studying plants as indicators cf gcollcg@cal cond-*@tirms
in the insular forest steppe of central Siberia. Tr-.;,,y MEL? 8:137-141
164. (M:RA 1-7: 12)'

Im inzhener.
t
Kobile unit for repairing statiOWW7 batteries. Blek.sta.27
no.2:36-38 IF 156. (MLRA 9:6)
(Storage batteries--Repairing)

LYUBIMOVA, Ye.M.
------
Vertical distribution of organic phosphorus in waters of the
Black Sea. Trudy 14GI 16:127-160 159. (141Rk 13:5)
(Black Sea--Phoophorus organic compounds)

LTUBIMDVA, Ye.14.
Axsenic in waters of the Black Saa. Trudy 14GI 16:167-173
159. (MM, 13:5 ) -
(Black Sea--Arsenic)

TAIf.131MOVAj YE. N.
"Experiments in the Activation of Processes of Raterification of Cellulose." Cand Tech
Sci, Forestry Engineering Academy, Leningrad , 1953. Dissertation (Referativnyy Z@,urnal--
Khimiya Moscow, No 2, Jan 54)
so: sum 186, 19 Aug 1954

AID P - 2779
Subject USSR/Chemietry
Card 1/1 Pub. 152 - 7/19
Authors Lyubimova, Ye. N. and N. 1. Nikitin
Title Use of activated cellulose in the synthesis of methyl
and ethyl ethers of low degree of substitution
Periodical Zhur. prikl. khim. 28, 4, 402-406, 1955
Abstract Methylation and ethylation of pretreated cellulose Is
described. Methyl and ethyl iodides, ethyl chloride
and dimethyl sulfate were used in the etherification.
The solubility of ethyl cellulose containing 2%
OC2H5(in 6% NaOH at 200C) was 94%. Five tables, 9
references (2 Russian: 1941-1951).
Institution : Laboratory of Chemistry of Wood and Cellulose of the
Wood Technical Academy im. S. M. Kirov.
Submitted : my 3, 1954

LYUBD(OVA. U.N.
Synthesis of cellulose benzyl ethers in the prezence of xylene.
Zhur.prikl.khim. 28 no.11:1220-1224 H '55. (MMA 9-3)
(cellulose) (Xylene)

) J, @ " -4- , t - ; - t I ,
1 LYUBIKO MM'KINA, Z.D.; IZYUKSD.TA, K.P.; KOKAROV, F.P.
DeterrAning the degree of cellulose polymerization for production
control. Aim. prom. 32 no.10:7-10 0 '57. (MMA 11:1)
1. TSentrallnyy naitchno-issladovateltakiv inatitnt tsellyuloznoy i
bumzhnoy promyshlennosti.
(Woodpulp) (Polymerization)

YURIYEV, Yu.K.; SADOVAYA, N.K.; 4lui-l-W-Al-Te. 90
Chemistr7 of selenaphene. Part 30: chloromethylation of ketones
of the selenophene series. Zhur.ob.khim- 30 no.8:2'732-2737
Ag '60. (MIRA 13:8)
1. Moskvoskiy gosudarstvennyy universitet.
(Selenophene) (Chloromethylation)

LYUBIMOVA Ye N
Synthesis of myrtenyl eater of cellulose. Report No.l.
Trudy LTA no.91:135-141 160. (MM 15:12)
1. TSentrallnyy nauchno-issled,ovatellskiy inatitut,
tsellyuloznoy i bumazhnoy promyshlennosti.
(Cellulose eaters) (Myrtenyl chloride)

ACC NRI AP6032904 SOURCE CODE1 UR/0062/66/000/009/1607/16.3
AUTHOR; Mamayovq V. P.; Lyubimova, Ye. N.
ORGI Novosibirsk Institute of Organic Chomistr- 40
y, Siberian Branch, A idopq of Sci-
onces, SSSR (Novosibirskiy institut organicheakoy khimii Sibirskogo otdeleniya
Xadomii nauk SSSR)
TITIL-1 Synthesis of 5,6-dihydrothiono(302-blpyrrol-5-one
SOURCE: AN SSSR. Ivwestiya. Seriya khimichaskaya, no. 9, 1966, 1607-1613
TOPIC TAGSi organic sulfur compound, organic nitrogen compound, acetic acid
ABSTRACT& 5,6-Dihydrothiono[3,2-b]pyrrol-5-one (1), a sulfur-containing isostere of
oxindole, was synthesized from 2-chloro-3-nitrothiophene (II)l
Card
UDCI 4 .91+547.74/75t*1,219

ACC NR. AP6032901;
NO,
@S COG113
CI
-1
NO, 1, NO, NO,
COOGIIII
Sx - (I V)
k
Cl NOz -kd'@ ClItCOOH S)"blicooclis
C00c,11 (V) (VII)
ks x C@'
I
COOC211'
N Nil,.IICI NII:-HCI
C -k
0 -kS)\CH,COOH S)\'CIICOOCH.
(VA) (Vill)
The boiling range of (I) is 142-1490. The 3-aminothienyl-2-acetic acid obtained
cyclyzes with much more difficulty than o-aminapharqlacetic acid. Condensation of
2-chloro-3-nitrothiophone with sodium malonate and sodium acetoacetate foIlowed by

ACC NR, AP6032904
hydrolysis of the condensation products yielded 3-nitrothionyl-2 acetic &aid.
Orig. art. hast 2 figures and I table.
SUB CODES 07/ SUBM DATE$ 18Apr64/ ORIG REFI 003/ OTH WS 008
C.,d 3/3

PRCSKMUKGV. R.I.; LYUBIMOVA, YeAb
Interaction of disulfides and thiols with the protein complex of
wbpat flour. Izv. vys. ucheb. sav.; pishch. tekh. no.2:36-39 163.
(MIRA 16:5)
1. Moskovskiy gosudarstvenny universitet imeni Lomonosova,
kafedra biokhimii rasteniy.
(Wheat--Analysis and chemistry
(Sulfides) (Proteins)

LY-UBI'fOVA, Ye. Ye.
"The Experience of Reclaimina Degenerated Meadows into FUghly
Productive Fodder Land in the Conditions of Tambovskaya Oblast";
dissertation for the degree of Candidate of Agricultural Sciences
0
(awarded by the Timiryazev Agricultural AcadeV,, 1962)
(Isvestiya TIWtr7aZeVskoY Seliskokhozyaystvetmoy Akademij, Moscow, No. 2,
1963, pp 232-.1.16)

KAZAKOV., Ye. I.; LARIN, A. Ya.; VORONRIA, T. B.; @[e-mail] --V.,*
GOROSHKO, G. K.
Surface-active substances from peat tar hydrocarbons. Trudy
IGI 17:157-168 162. (MIRA 15:10)
(Surface-active agents) (Peat)

KAZAKOV, Ye. I.; LARIN, A. Ya.; VORONIIIIA, T. B.; LYU13II-_',OVA, Z. V.,*
GORGSHKO, G. K.
Light oil of a mean temperature brown coal tar as a raw material
for the production of surface-active substances. Trudy IGI 17:
169-173 162. (MIRA jr1:10)
(Coal-tar products) (Surface-active agents)

!'--,-Ilj:!I:IJB-IIMOVA-GERASIMOVA, R.M.
Changes in cerebral circulation during the total-body iaaizing
irradiation of animals. Med. rad. 5 no-4:24-29 Ap 160e
(MIRA 13:12)
(BRAIII--BLOOD VESSEW) (RADIATION-PHISICLOGICAL EFFECT)

f " h
ilni7.-Irig Y.
'Th

BIBIKGVA, A.F.; BUSYGIN, V.Ye.; GRIGORIYEV, Yu.G.; KALYAYEVA, T.V.;
L'TVBI:MqVA-GERAS1M0VA. R.M.; TSYPIN, A.B.
Reaction of the organism to massive IV-irradiation. Pat.
fiziol. i eksp. terap. 6 no-4:57-62 Jl-Ag 162. 041 RA 17: 8)

;L 0
39564
S:@205.-'62/0021'003 0 10 015
10 154215
AUTHOR: Lyubimova-GerasIT9-va- R M
TITLE: Changes in the cerebral vascular reaction to adrenalin, acetylcholin and hexonium following
whole body irradiation
PERIODICAL. Radiobiologiva, v. 2, no. 3, 1962, 455-460
TEXT: The functional changes in the CNS following ionising irradiation have been insufficiently studied until
now In the present study the cerebral blood flow rate was investigated with flat thermoelectrodes invented
by Marshak The results were recorded photokyrnographically during the entire course of the radiation
sickness 18 male rabbits weighing 2-3 kg. were subjected to a single whole-body x-irradiation of l(X)Or in
176 experiments. The animals developed acute radiation sickness and died within 1- 12 days, except for 3
animals which survived. Adrenalin (4-8y/kg b.w.) were injected into the marginal vein of the ear during
10- 15 sec The reaction was recorded during 15 min. and the time interval between the injections was 20- 25 min
The reactivity of the cerebral vessels to adrenalin, acetylcholin and hexonium was changed in acute radiation
sickness. These changes were dependent on both the severity and stage of radiation sickness Alteration in
the neuroliumoral rgulation of the vascular tonus in radiation sickness was established i-licre are I figures
SUBMITTED September 29, 1961
Card 1/1

LYUBIMVA-GERASIMVA, R.M.
Some pathogenic mechanisms of acute cerebral circulatory disorder.
Biul.eksp.biol.i med. 53 23-28 Je 162. (MIRA 15-10)
1. Nauchnyy rukovoditell - deystvitellnyy chlen AMN SSSR AN.
Lebedinskiy. Predstavlena, deystvitellnym chlenom AMN SSSR A.V.
Lebedinskim.
(CEREBROVASCULAR DISEASE)

ACCESSION NR: AT4037698 S/2865/64/003/000/0278/0288
AUTHOR: Lebedinskiy, A.V.; Grigorlyev, Yu. G.; Lyubimova-Gerasimov, R. M-9
Polyakov, B. I.
TITLE: Vegetative reactions during stimulation of the vestibular analyzer and
their possible role in complicating space flight conditions
SOURCE: AN SSSR. Otdoleniye biologicheakikh nauk. Problemy* kosmichaskoy
biologiiq ve 3, 1964, 278-288
TOPIC TAGS: acceleration, vestibular analyzer, space flight, Coriolis acceleration,
rabbit, vegetative reflex
ABSTRACT: The role of angula@ accelerations and Coriolis accelerations on the
vestibular function was studied by means of a BY-2 type accelerator, on which it
was possible to produce angular accelerations ranging from 0.05 up to 12000 sec 2
and any magnitude of angular velocity up to 1800/sec. Vegetative reactions are,of
special interest since by stimulating the vestibular apparatus, it is possible to
observe practically all known vegetative reactions. It has been established that
the magnitude of the reaction depends on the duration of the stimulus (accelara-
tion). Data obtained indicate that after whole-body irradiation of the aninal,
L--- 1/3
'@ord
IU

ACCESSION NR: AT4037698
more time is required for acceleration to produce an equal reaction. There is
reason to believe, in this case, that radiation affects the central nervous
system and not the receptor. So far there have been practically no attempts made
to evaluate the biological significance of vegetative reflexes which arise during
stimulation of the vestibular analyzer. When rabbits were gubjected to rocking in
the horizontal (duration of acceleration, O.J5 sec), at 66'sec 2, a diminution of
re6piration amplitude wasooted; at 4000/cec the diminished amplitude increased
in frequency; at 6000/sec the amplitude dropped off sharply with no marked
frequency increase; and at 120OP/soc there was a distinct break in respiration.
Reactions of the cardiovascular system to acceleration are complex. Thus, when
0 2
rabbits are subjected to an acceleration of 0.05 /sec for 30 sec, skin temper-
2
ature rise a. But, if accelerations are increased to 1 .5 or to 3.20/sec for the
me duration of time, skin temperature drops. The depressive reaction appears,
apparently, only in response to large acceler@tiona because when rabbits were
accelerated in the range from 60 to 8000/sec (duration, 0.15 aec), no depressive
rsacti2n was observed. When rabbits were exposed to short-term acoaleration of
5 /sec , a diminution of blood circulation in the brain was observed. This effect
was distinct if the acceleration lasted 12 or 24 seconds, but Indistinct if the
duration waa only 6 sezondao The authors have stressed the importance of
1"- 2/3
Card d

ACCESSION NR: AT4037698
duration of effect of acceleration on appearance of vestibular reactions. Very
possibly this indicates the significant role of inclusion of the endocrine mechan-
ir,m, particularly of the adrenal Erj6tem, into the complex of vegetative reactions,
and the consequent stimulation of the reticular formation. If the appearance
of vegetative reflexes observed during stimulation of the vestibular mechanism
is tied to the stimulation of the reticular formation, then, in the final analysis,'
their involvement must be controlled by the cortex of the cerebral hemispheres.
It was also noted that stimulation of the vestibular apparatus liMits the aCtivity,
of the cortical component of.vagetative reactions.
ASSOCIATION: none
SUBMITTED: .00
NO REF SOV: 010
ENCL; 00 SUB CODE: pg, LS
or=: 004
3/3

LUS, Ya.Ya.; tEDVEDEV, N.N.; PROKOFIYEVA-BELGCVSKAYA, A.A.;
LYUBIMOVA-LEPRM, V.F.
In memory of Tenis Karlovich Lepin, 1895-1964. Biul. lCIP.
Otd. biol. 70 nc.2:153-'.55 Mr-Ap 165.
( "'ll 11A 18: 5 )

LYUBIRSKIY, 2- Z. , f@ITZNIII, S. S. and SHTARIC4AN, V. S.
O,jtimum information Coding in AutomaLi.,,r and Multistt!p Aut,imat-L!ji.
Production Processes."
repoTt pweemted ut tt@ Co:@@Icrcrv-e m Aut(=,.itlw, &-A CczirjtAtlC= LO-Z-gtr.!@-'T
M=-cu. 5-8 10"'57. 0--Snalu-nd by AU &--i. Fog@ aW Tec@lh. z34-wipt;i 5or
Arpsun TAo Do I I-d I

VZ-,,j'BI,',f3KFf E. Z. : Mustli%'r lln.,o-Mat sc, 0s) -- "cn
ir,L-a='ln_u and the technim.,e of nrc,@:Uums% C: rij
(Acad Sci USSR, Dept of '[,IojjP@ ?,9:1 rf t@-, Tns@.
(KL, T40

S11 12/59/00C/3 1 1/@,68
A052/A002
Translation from: Referativnyy zhurnal, Elektrotekhnika, 1959, No. 15, p. 153,
# 32053
AUTHORS: Kamynin, S.S., Lyubimskiy, E.Z., Shura-Bura, M.P.
TITLE: Automation of Programming @y a Programming Routine
\10
PERIODICAL: V sb.: Probl. kibernetiki, No. 1, Moscow, Gos. izd-vo fiz.-mat.
'it., 1958, pp. 135-171
TEXT: Basic information is given on the programming of problem solutions
on digital computers. A method of programming by means of generalized commands-
operators is described. These command-operators include certain algorithms the
representation of which in a form of a sequence of elementary operations can be
delegated to the machine itself by a program given once and for ever. The
generalized commands-operators are divided into the main and auxiliary ones. To
the former belong arithmetic, logical and re-addressing commands-operators; tn-
put and preservation commands-operators and a nonstandard conmand-operator belong
to the latter. The task of the programmer consists in giving the arrangement of
commands-operatorz and the information to each of them in form of a line of
Card 1/2

S/112/59/tOO/0,15/03I/068
Automation of Programming by a Programming Routine A052/AO02
numbered symbols corresoonding to the type of machine on which the problem will
be solved. One of six letters designating in abbreviated form each command-
operator can serve as a symbol. A line of symbols and the information to them
is the program scheme. The compositlon of the program proper according to a
program scheme can be performed by the machine itself by means of the programming
routine. At the same time the algorithm will become more precise: the positions
of commands-orders in the storage unit, the addresses of working cells etc will!
be determined. A description of the " TT17-2" (PP-2) programming routine is given.
The conception of conditional numbers is introduced on which, as well as on the
conception of an operator scheme, this method of programming automation is based.
An instruction for composing programs by means of the PP-2 programming routine
is given in an appendix.
A.V.Sh.
Translator's note- This is the full translation of the original Russian
abstract.
Card 2/2

LYUBIMSKIY, E.Z. (Moskva)
Arithmetical unit in the programming program flo.2. Probl.k1b.
no.1:178-181 '58. (MIRA 12:4)
(Programming (Mathematics))

AUTHORg Lyubimakiy, E, Z.
S/030/60/000/008/004/013
B021./B054
TITLE? Problems of Automatized Programmin
PERIODICAL,., Vestnik Akademii nauk SSSR, 1960, No, 8., pp, 47-55
TEXT4 With the introduction of high-speed computers; the fraction of
time assigned to programming has relatively increased. Therefore, the
problem of automatized programming, i.e. the use of high-speed computers
for programming, gains importance. In the present article, the author
describes the posing of the problem For an automation it is necessary
to determine the exact form in which the initial information is fed into
the computer and the result is presented; to work out the algorithms
for the transition from the computing scheme to the programming scheme,
and from the programming scheme to the program, respectively; these
algorithms for the transition must be programmed in the code of the
computer which is to be used for automatic programming. Further, the
author describes the automation of the first stage of programming, and
explains it with the aid of mathematical formulas As to the automation
Card 1/2

Problems of Automatized Programmin.- S/030 60/000/008,'004/013
B021/V.054 V/
of the second programming stage, the following available methods are
indicatedi the method of symbolic addresses; the method of library
subroutine; the method of the programming plan. Finally, the author
mentions the so-called interpretation systems which may be used both
for the automation of the s6cond stage and for the programming as a
whole. He briefly outlines the advantages and disadvantages of these
systems.
Card 2/2

1 @12
5/044 /62/000/005/067/072
C 1 11 /C444
THG R -Lyubiws,.iy, Z.
TI T ---E : Cr the ;!,obable n !,hf, I, ntTu
P EIR I _u 10L @i t i v,,,,., zhu r:;,i 1 n D 7
5VLi65- ("Zh. vj,: .n i.,@; :jii, t - --;1. 1 "r, r,I
1, i-.o. 2, 561-564)
TEXT: Title ia&er LL iumb,.r ,f the
in tnu
ol '-hL --onditic-)ni'l ojjeratur@' of the t-1-pe, if
lo6ic term then --:f operator - , - operator . In thils
ciise tne amnbi6-uit, of the decouini@ of the operators of the c@-clcs which
cont,in conuitionul operators, is eliminated. In the'way of the first
correction one proposes because of greater uniformi-ty to vary the con-
struction of the conditional tcrins by admitting after then an arbitrary
term instead of just ;. simple term.
F
1.t@bstracterfs note: Complete translation.]
,Card 1/1

ACCESSION NR: APW12006 S/0208/64/004/001/0096/0212
AMORS t Shura-Bara, H. R, (Hoscow); Lyuk4opkiy, F. Z. (Hoscow)
TITLE: Translator for Algol-60
SOURCE: Zhurnal vy*chial. matem. i matem. fiz., v. 4. no* 1. 1964s 96-112
TOPIC TAGS: tranalatorp input 17hinguage, computer, function identifier, teletype
symbol, Latin letter, meta linguistic formula, magnetic tape, translator TA 2,
Algol 60
ABSTRACT: The basic features and the input language used by the translator TA-2,
built to exploit computers for translating purposes, are presented. 'Three
constraints are put on Algol-60. These are: 1) labels or signs can be used only a
.identifiers; 2) the array "own" must have constant cutoff pairs; 3) standaYd
function identifiers may not be actual parameters. 114- is shown that this input
language can be universal (makixg possible the formal exchange operation concepts)
and that it is a refine nt of Algol-60 procedure-code. The input alphabet is
based an teletyps symbols containing 26 lower case Latin letters# a set of special
signss and a 8stressO sigm. In additions it contains lower case Greek letters and
Cam 2/3

IAMESSION MRs Aftol=6
-.elementary function notations. The program assignment for TA-2 consists of a meta-1
linguistic formula < program,>, : t - 4!@ operator),.; I< preliminary commentary for
,execution >;