SCIENTIFIC ABSTRACT VOLVOVSKIY, I.S. - VOLYNCHIKOVA, M.

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• Collection: Scientific Abstracts
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• Document Creation Date: November 2, 2016
• Document Release Date: August 9, 2001
• Sequence Number: 2
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

VOLIVOVSKIY_ 1. RYABOY V.Z.; SHRAYIKAN, V.I.
Use of the methods of frequency analysis and synthesis in inter-
preting the gravity field in the Bukhara-Rhiva area. Prik2e geofiz.
w.33:161-168 162. (HIM 15:10)
(Uzbekistan-Gravity)

Wl,'MSKLY, I.S.; GAFIFT;Kly, R.G.; SHLE1,INGER, A.Ye.; SHRAYBRAN, V.I.
Surface structure of the basement of the Turan Plateau. Biule
IADIP, Otd. geol. 39 no.6tl9-29 N-D 164. WRA '18:31
A'f-MK)
rg, "I ~ "U `X '~ sm
1-6 M
A .1-04, :' ~n mvvess~'m -A 0-:20-M-PUNROM NORM RMIN

GODIII, YuoN*p akademik (deceased]; VOLIVDVSKIYj I.S.j RYADOY, V.Z.
Some results of the use of seismic echo waves in a study of the
earth's crust. DokI, AN SSSR 146 no.2:340-343 S 162#
(MIRA 15:9)
19 Mel razvedochnoy geofiziki i seysmologii AN Turkmenskoy SSR
i Vsesoyuznyy nauchno-issledovatellskiy institut geofizicheskikh
metodov razvedki. 2. M Turkmenskoy SSR (for Godin).
(Seismic prospecting)

GODINj YUAI akademik [deceased]; VDLIVOVSKlYp B.S.; yq;~.Iyc S.
RYABOY,, V.Z.; SMU734AN,. V.1.
Characteristics of the*otructure of the earth's crust in
the veetern part of Central Asia. Doklo All SSSR 146
no.4:W-&5 0 162. (MIRA 15:11)
1. Institut geologii. AN Turkmenskoy SSR, Vsesoyuznyy
nauchno-iosledoviteltakiy inatitut goofizichookikh
metodov razvedki i Moskovskiy institut neftokhimichookoy
i gazovoy,promyshlennosti. 2. AN TurkmenskoySSR (for Godin).
(Asi#,-Central--Seismic prospecting)

ALEKSEYEV, A.S.; VOLIVOVSKIY, I.S.; YERMIIDVA, N.I.; KRAUKLIS, P.V.;
RYABOY.9 V.Z. '''
Physical nature of certain waves recorded in hodographic seismic
sounding Part 2. Izv. AN SSSR. Ser. geofiz. no.1:3-19 Ja'64.
(MIRA 170)
1. Kontora Spetageofizika Gosudarstvennogo geodezicheskogo
komiteta SSSR i Leningradskoye otde-leniye Matematicheskogo
instituta imeni V.A. Steklova AN SSSR.

ALEKSE-YEV, A.S.;_YQ~Iy PT,I.S.; YERMILCIVA, N.I.; KRAUKLIS, P.V.;
RYABOY, V.Z.
Physical nature of certain waves recorded in hodographic seismic
sounding. Part 1. Izy. AN SSSR. Ser. geofiz. no.lltl620-1630 N
163. (wRA 16:12)
1. Kontora "Spetsgeofiaika", Leningradskoye otdoleniya
Matematicheskogo institute. imeni Steklova AN SSSR.

A,
1k,.`-1~*.,--ACCESS1O1( NRt AP4014023 ---~---.----S/004'75//'ue4/000/091/0003/0019
-i;",i UUMORSt Alekseyeyl A. So; jqk~xoysklyo Sol Termiloval No Isl Kr&uklis, Pf Ve;
FW&boV9 V. Z_
TITLEs The pbyrjioal nature of some waves recorded during deep seismic mounding@
Theoretical analysis of models of the earth's orust for regions of Central Asia
BOURM AN SSSR. Izv. Beriya geofiziobeeksys, no. is 1964y 3-i9
TOPIC TAGS: deep seismic sounding, earth's orust, Central Asiap head waves
A- reflected wave, refracted wave, kinematic characteristics dynamic characteristic,
Turkmeniag shot point, apparent wave velocity
AWMACTs The authors present results on theoretical comparisons of the kinematic
and dynamic, characteristics of the earth's orust in southeastern Turkmenia. They
have con
sidered possible laws governing changes in apparent wave velocity with
distance from shot point in layered inhomogensous media with plane-parallel inter
f
&aM Three different models of the earth's crust were used# based on different
velocity Yalu*sp densities, rates of change with depths and combinations of these$
Results show Vat in layeredg inhomogeneoue media the following relat one
i d~ways
1hold for the different k4nA-of waress for head waves dV*/dx 0 and d 01
Card

ACCESSION M AP4014023
for refloated waves dv*/dx < 0 and d2V*/dz';,,O; and for refroLgt*d wavell
2V#/di if 2
11 > 0 or d V*/dx 40.
dv*/dx Ot but if dV*/dx >Oj then either d
Theme relations my be used for control in the correlation of waves. From these
results it follows, in particular, that there are no waves in inhomogeneoug layered
av*/dx 4o and d2V*/dx24 0 may be fulfilled simultane-
media for which the relations
Thus, in such inhomogeneous lVered mediap changes in apparent velocity of
A oWly-
headt reflected# or refracted waves with increase in distance from shot point may
take place according to but one of the laws illustrated in Figo I on the Eholosure.~
Orige arts has' 13 figures and 10 formulas.
ASMIATIOffs lontors, Spetapofisiks GGK SSSR (Office of Spetegoofisika GGK SSSR);*
Akademiya nauk SSSR (AaMaW of Sciences SSSR) I LM ins Steklove, (IM)
SUMITTEDs
261"3 DATE ACQI 14Fsb64 ENCLo 01
M CODBI AS 000
NO RM Wo 005
CWd"

RYABOY.. V.Z.; SHRAYBHAN, V.I.
Nature of regional gravity anomalies in the Mhara-Khiva region
and adjacent areas. Izv. AN SSSR. Ser.geofiz. no.5s644-651
Yq 162. (MA 15:8)
1. Vaesoyu2nyy nauchno-isaledovatellskiy institut geofizicheskikh
metodov razvedki i Moskovskiy institut neftekhimichaskoy i
gazovoy promyshlennosti im. akad.Gubkina.
(Uzbekistan-Gravity prospecting)

8/169/61/000/011/018/065
D228/D304
AUTHORSi Vollvovskiyp B.S., Vol'-vovskiy. and Ryaboy, V.Z.
TITLE: Laboratory use of the method of controllable d1rected
reception for interpreting the data of deep seismic
sounding
PERIODICAL: Referativnyy zhurnalt Geofizikaq no. 11, 19610 219
abstract 11A197 (V sb. Razved. i promysl. geofiz.,-no.
36, m., 196o, 8 - 13)
TEXT: The laboratory modification of the method of controllable di-.,/
rected reception was used for distinguishing waves reflected from
deep discontinuity surfaces. The substantial difference in the fre--
quency characteristics of the apparatus of deep seismic sounding
and controllable directed reception was overcome by means of the
approximately fourfold enlargement of the time scale and summation
base. Extended hodographs (to 35 km) of reflected waves correspond,-
ing to the surface of the suberustal and granitic layer were con-
structed as a result of the processing of seismograms. Reflected
Card 1/2

Sll69V611000101110181065
Laboratory use of the method of D228/ '304
waves were also distinguished at the point of origin. Anomalous
apparent velocities and sharp changes in the form of the wave re-
cordings were observed in the region of the points of origin. tAb--
stractor's note: Complete translation).
Card 212

VOLIVOVSKIY.. I.S.; AYABOY, V.Z.
Frequene y caqposition of seismic waves corresponding to the
main divisiona.3 boundaries of the earth's crust. Izv. All Turk.
SSR. Sler. fiz.-tekh.j khJm. i geol. nauk no-4:50-55 161.
(14M 14:12)
1. Otdol razvodochnoy geofiziki i seysmologii pri Prezidiune
Ali TurkmenBkoy SSR,
(seismic waves)

GODIN, Yu.N.; VOL'VOVWqIY, B.S.; VOL1VOVS1:1Y1 I.S.; FOI-ENKO, K-Ye.
Studyinp the structure of the earth's crust in the course of
repional seismic explorations on the Russian Platform and in
Central Asia; materials presented at the 12th General Assembly of
the International Union of Geodesy and Geophysics. Izv. All ~15SR.
Ser. peofiz. no.10:140;-1471 0 161, (MIRA 14:9)
1. Ali Turkmenskoy SSR i Vsesoyuznyy nauchno-issledovitel'skiy
institut reofizicheskikh,metodov razvedki.
(Spisomometry) (Earth--Surface)

8/16
D2289/62/000/006/002/093
/D304,
AUTHORS: Vol1vovsh_jY_,_J_,_SO, Ryaboy, V. Z. and Shraybman, V.I.
TITLE: Abyssal geologic structure of the Ferganskaya Depres-
sion according to geophysical data
PERIODICAL: Referativnyy zhurnal, Geoftzika, no. 6, 1962, 5,.ab-
stract 6A21 (Sov. geologiya, no. 1, 19062, 156-160)
TEXT: A brief description is giv 'en of the results of regional
seismic investigations (deep seismic sounding) on the Ferganskaya
Depression's territory in 1958-1959, as a result of which the
crust's structure was ascertained to a depth of*50 - 60 km. Know-
ing the character of deep crus~tal interfaces (the surfaces of the
folded basement and of the granite, the basalt, and-the suberus4l"al
layers) and the stratal velocities, has allowed a better grounded
approach to be made to the solution of the question of the large
gravity low over the Perganskaya Depression. A correlative relation
between the propagational velocity of elastic seismic vibrations
and the density was derived in the form a'= (0.24 VStr km/sec +
C&rd 1/2

Abyss< 9e Oz 0
t"Ll L
oil 'e
tj2e 2aye 0~'d
bo~' clens, t-ra Upo, e- to
S/
a toz. 'y 2
tab7 - Y 'rO8e, O-f t'h e cl 8 0p t 769 6,0
t.he -4shed kl,-Ch C-rust .9-ra aln 28 00
as a:2d 42 V, t y r1 th 04 0/00
.r2 re2 I e Of a 6100~109
veq rocjc. eza. I I
Z).2~e8a . e oil th t' Ult 04101"1 8 Ive'-
.104. Qe X4.1
0 f02 O-f th "104a e obt,'.cldajt.e Of
thla d L
Irl t bj, e C, 012 t 0
'd b ' q tla4 t - -ZIICII,
ze2cl 229 -its dallo Y f S e4~ ta t a 0
tLI-re. OC127 ' WS Z el d 0 e22 t SLI I ve ect a Ves thla a deep
th 40t , epth ofgralIt f 2, Oe th 4 1 t' -' C1.4 t
Oe , 'the fu 0 C-alcul Oda Of a
C2-Q,'ltcj7 e ezj. Que occur..y aur -In t e h,,, atlo - Xt la,
rZa t t tene o2 zL,4 - Irey OZIM a
Oorapi . - e .4s. Is,
te e2- to ce. dat 04 t~27 00226.1c, - 7') t es-
loz-422S2 May, 212 Pee ' 2) a & e Pe,~ -e-rab2e
421 th #'o be
'the a2-ea Plo
4 tj 012 t eo ganakajr 112
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as.SLZM Sj the d
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caz-d *~c tezs 1 112 a 0-
a 220te: ub,

CC Nk, AR4009029 ~OOR6EiTVRI UP,/0169/65/000/010/GO03AO03
AUT11OR% Vollvovskiy, B.S.; Vollvoyakin 1. S.; Tall-Virskiyj 9,~Bj �Pra b!!an
y
ORG.- None
TITLE; The structure of earth crust and the top mantle of the basic geostructural
zones of "ntralAsia
SOURCHI Ref. zh. Geofizika, Abs. IOG13
REP SOURCEs Sb. Geol. resul'taty prikl. geofiz. Geofiz. isaled. stroyeniya zemn. koryp
M., Nedra, 1965, 26-32
TOPIC TAC93: ea7toh "cru'st crust structure, seismology /Contr'81 Asia or----
tum" Turanf&*%aru2t=xtrux;OMb-, Tyan'.5han, cxv**=a WAZM M"
ABSTRACT: in the present geological structure of CentralAsia, there are regions rela-
ted to the three basic geotectonic categories of continents, the Turanian epi-florcyni
platform, the alpine folds region of Kopet-Dag, and the orogenic region of Tyan'-Shan,
The relation between surface relief of thefolded foundation, the thickness of the eart,
Crust, and the relative density changes of the stir(ace mantle of these regions is dis-
cussed. Seismological.data indicate a correlation between the geetectonic state, the
earth structure, and the character of the density changes of the subcrustal Passes.
To the Tyan9-Shant orogenic region (relative to the Turanian platform) corresponds an
increase, in the crust thickness and a relatively 6maller density of suberustal masseo6
CWd UDC 350,311%551,141

ACC NRs AR6009029
Besides, increased gradients of the earth crust thilknes3 and a high contrast relief of
the Mohoravicia . surface characterize the Tyan'-Aant. The Turanian platform and the
Tyan'-Shan' are also substantially different in their gravitational characteristicss
The gravitational anomaly decreases at the transition from the Turanian platfom to.tht
Tyan'-Shanl. [Translation] .
SUB OWEs 08/ -------
Card 2,12
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NEW,% 41MRS iNMR, 3

VOLIVOVSKIY, B.S.,; VOLIVOVSKIY# I.S.; TALI-VIRSKIY, B.B.
Using seismic methods in prospecting for oil and &u deposits in the
Yergana Valla7. Geol. nefti i gaza 4 no.1:18-25 A 160.
(MIRA 13:10)
1. Uzbekneftegoofizika.
(Fergana-Seismio prospecting)

VOLITOVSKIT, B.S.; VOLITOVSKff, I.S.; TALI-V'R"'To B.B.
Oonditions for seismic prospecting In the Fergana Valley.
Razved. I prom. geofiz. no. 35:73-77 160. (MIRA 13:12)
(Yergana-Setemic prospecting)

VOLIVOVSKIT, B,S.; VOLIVOVSXTTI.I#S,; RYABOY,.V.Z.
laboratory use of the controlled directional sensitivity method
in interpreting the materials of deep seismic somndings. Razved.
I, prom. goofiz. no.36:8-13 160* (KIRA 13112)
(Selsmio prospecting)

GODIN, ru,N., akademik; VOLIVOVSKIY, B.S.;
Seismic investigation of the earth's crust in the region
of the Yargana Intermontane trough. Dokl.AN SSM 133
no.6:1398-i4ol Ag l6o, (XLRL 13:8)
1. Uzbekskiy geofizicheekiy treat i Yeasoyusnyy usuchno-
ioriledovatellakly inatitut geofisichookikh metodov razvedki.
2. Akademiya nauk Turkmenskoy SSR (for Godin).
(Fergana-Seismometry)

GODIN, Yu.N., akedemik; VOLIVOVSKIT, B.S.; VOLIVOVSKIT, I.S.
Seismic investigations of the earth's crust in the Bukhara region
of the Uzbek SSR. Dokl. All SSSR 134 n0-5:1069-1072 0 l6o.
(MIRA 13: 10)
1. Vaesoyuznyy nauchno-ionledovateltakiy geofizicheekikh metodov
razvedki. 2. AN Turkmenskoy SSR (for Godin).
(Bukhara-Seismic waves)

VOLIVOVSKIY, B.S.; V2~~~~
Seismic.investigatiow along the regional base profile Amu Darya
(Karabekaul) - Nura-Tau (Koytaah). Izv.AN Turk.SSR.Ser.fiz.-tekh.,
khim*i geol.nauk no*3t28-32 161. (KMA 14:7)
lo Otdel razvedochnoy geofiziki i seyamologii pri Prezidiume AN
TurkmenBkoy SSR.
(Uzbekistan-Seismic prospecting)
0

5/552/61/000/031/001/003
D218/D304
AUTHORS- Vollvoskiy, B.S., Vollvovski'y and Ryaboy, V.Z.
TITLE Some data on seismic waves corresponding to the subcrustal
layer (based on the results or seismic studies of the
earth's crust in Uzbekistan)
SOURCE. Moscow. Vaesoyuznyy nauchno-isoledovatellskiy institut
geofizicheakikh metodov razvedki. Pri)dadnaya geofizika.
No. 31, 1961# 3-10
TEXTs The authors report on some methodological results obtained during
the 1958-1959 regional seismic studies of the earth's crust along the
Leninabad-Karaungur, Abadan-Vuadill and Karabokaul-Koytash profiles.
This research was carried out by the Uzbekskiy geofizicheskiy treat
(Uzbek Geophysical Trust) and the Vaesoyuznyy nauchno-issledovatellskiy
institut geofizicheskikh metodov razvedki (All-Union Scientific Research
Institute for Geophysical Methods of Prospecting). It was the continua-
tion of deep seismic soundings carried out in 1949-1955 in various regions
of Soviet C*ntral Asia by the Geofizicheskiy institut AN SSSR (Geophysical
Card 1/4

S/552/61/000/031/001/003
Some data on seismic waves ooo D218/0304
Institute of the AS USSR) previously known an Institut fiziki Zemli
(Institute of Physics of the Earth) on the initiative$ and initially un-,
der the direction of Academician G.A. Gamburtsevo Multiple seismographs
were employed (4 instruments per group), the distance between the groups
being 100 mo 1-2 ton charges of TNT were exploded at distances between
15 and 70 km and the maximum distance of the points of observation from
the charges was between 200 and 300 km. It was found that the recorded
waves can be divided into 3 types, neMely 1) longitudinal refracted waves
recorded both in first and subsequent arrivalog 2) reflected waves from
lgw-lyj*Lng separation boundaries in the crust recorded both at near,
(60, ~80 km) and distant (300 km) points, and 3) waves which could be as-
aribed to multiple reflected-refracted and domposite waves due to low-
-lying separation boundaries. Some typical hodographs and velocity and
amplitude spectra are reproduced and discussedg The experimental re-
sults have been evaluated on the basis of a dynamic theory of propagation
of seismic waves developed at the Leningradskoye otdeleniye matematiches-
kogo instituta AN SSSR (Leningrad Branch of the Mathematical Institute AS
USSR) by G.I. Petrasheng, A.S. Alekseyev and others. These calculations
Card 2/4

S/552/61/000/031/001/003
Some data on seismic waves ooo D218/D304
have shown that the predominating waves in uniformly layered media are
not head waves (as it was assumed so far), but waves reflected beyond the
critical angle (i.e. so-called postcritical reflections). In gradient
media the dominating waves are reflected and refracted waves (the calcu-
lations were carried out for a perfectly elastic model of the crusi).
In the present studies waves reflected from the surfaca, of the subcrustal
Layer (Mohorovicic discontinuity) were observable beginning at 30-40 km
from the point of explosion and were recorded in subsequent arrivals in
the entire range of distances. The apparent velocities of these waves
were found to decrease from 9-10 km/sec at 80-00 km to 6.5-7-0 km/sec
at 250-300 km. Their hodographs have a hyperbolic form. The predomi-
nating frequencies vary between 9-11 and 14-15 cps and tend to decrease
slightly with distance. The refracted waves are weaker in intensity
and have apparent velocities between 8 and 9.5 km/sec. They tend to
increase slowly with distanceg The predominating frequencies in the spec-
tra of these waves lie in the range 10-16 cps and are as a rule greater
by 2-4 cps than in the case of the reflected waves. The frequencies tend
to decrease with distance. It is pointed out that the dynamic theory
mentioned-above prediots that the reflected waves should have higher
Card 3/4

S/552/61/000/0031/001/003
Some date on seismic waves D218/D304
frequencies than the corresponding refracted waves which is an apparent
contradiction with observations. The general conclusion is that seismic
studies of the earth's crust in Soviet Central Asia show that waves re-
fleeted from the Mohorovicic discontinuity before and after the critical
angle can be determined from seismographso There is also a complex reflec-
ted group consisting of head waves produced on the surface of the sub-
crustal layer and weakly refracted in the latter4 For the purposes of
deep seismic *ounding thes6 waves may be -interpreted as head waves cor-
responding to the surface of the subcrustal layer. There are 8 figures
and 10 Soviet-bloc references.
Card 4/4
M U-
'n M4 M,
NO` " I
's, M, Ve M_ M-9 W IM
N RRIM ir _iT PE W E

BELOUSOV V.G.; VOLVMKI) B.S. [Vollvovskiy., B.S.jj VOLVOVSKI, I.S.
tVoltvcy7okiy,, I.S.1; REABOI, V.Z.
Experimental researoh on the registering of the waves reflected
by depth. Analele geol geogr 17 no.3-.51-64 Jl-S 163.

VOLIVOVSKIYI B.S.; VOLIVOVSKIYp I.S.; iswm, V.V.
Results of the regional seismic studies in the central Ks--a-Kus.
Trud7 VNIGNI no.351l62-166 161. (KRI 160)
(Kara Kum-Seiamic prospeoting)

ISIFJTIN, V.V.; SEMF
S. MOVICH, V.V.;
VOLIVOVSKIY, B.S.; ~ VOLI-IMMLU, I
TALI-VIRSKIY, CHAMOj 9.Se
Regional geophysical studies in central Asia and their further trends.
Sov.geol. 6 no.l2sll2-117 D 163. (MIRA 16:12)
1. Natichno-issledovatellskayn sredneaziatakaya geofizicheskaya
ekspoditsiya kontory "Spetsgeofizika" i Uzbekskiy geofizicheakiy
treat.

ACC NRiAT6028367 W SOURCE CODE: UR/0000/65/000/000/0026/0032
AUTHOR: Vol!vovakiy, B. S.; Vollvovskiy, I. S.; Tal'-Virakiy, B. B.; Shraybman, V,*I
ORG; none
TITLE: Structure of the Earth's crust and upper mantle or the main geoutructural
zones of western Soviet Central Asia
SOURCE: International Geological Congress. 22d, New Delhi, 196h. GeologichcGkiye
rezulltaty prikladnoy geofiziki (Geological results of applied geophysics); doklady
sovetskikh geologov, problems. 2. Moscow, Izd-vo Nedra, 1965, 26-32
TOPIC TAGS: seismology, Earth crust, -+Vgw~F-: gravity anomaly, basement,
meganticline megasyncline, upper mantle.% MO-V0,90VICIC DtJCoAxr.WVt71Y / W-r5-7F,4x1
,5c, ve V. 7- CEA.-7-4194 t915h9
ABSTRACT: Three different zones distinguished in western Soviet Central. AzAa Fire
ar. follows: an area of recent contrasting movements of Tien Shan, the Epilierzynian
platform and the Kopet-Dag foredeep. These zones include major striictural f~~-qturcs
of the first order, such as arches and depressions in the platform and
and magasynclines in Tien Shan., The data obtained from deep sreismic solvncling tind
seismological observations made it possible to estimate the crustal thic?nes:3 OIL'
western Soviet Central Asia and to discover certain regularities in variation of the
crustal thickness. In general, the data suggest that, in the orogenic area of
Tien Shan, the crust is much thicker than vithin-the platform. In addition, Tien Sh

XbC Nk-. -A-, T-6-6-2-83-6 7
is characterized by higher gradients of crustal thickness variations and g,~neral
geomorphic contrasts of the Roho discontinuity. Both in Tien Shan ruid vithin the
platform, uplifted zones (positive structural featues) are characterized by sm-0.1er
crustal thicknesses, and zones of depressions, by large thicknesses. The tk)ho
discontinuity and the basement surface practically conform. The thickness of the
crust changes mainly on account of the thickness of the overburden covering platform,
formations. At present the main source of information about the mantle structure
is gravity data. However, Its inleq)rclatlon Is complIcated by 1he fact tl,,,L gravily
..anomalies reflect the total effect or many factors, the most inTortanL of which are
relief and petrographic nonuniformity of the basement, variations of the thickness
of the crust and its layers and, finally, inhomogeneity of subcrustal material.
Within Tien Shan and the Turaniam platforni, local variations of the residual anomaliee
correspond to major structural feetues of the first order, auggenting the presence
of local inhomogeneous types of suberustal masses in each, of these area. Orig. art.
has: 3 figures.
SUB CODE- 08/ SUBM DATE: 06Jan65/ ORIG REF: 010
Card 2/?

Volya, 0. S.
"The:Searetory, Absorptive, and Motor Punctions of the Small Intestino
of Sheep When Yed with Various Rations." Min Higher Education USSR.
Odessa Agricultural Inst. Odessa, 1955,
(Dissertation for the degreo of Candidate in Biological Sciences)
SO: Knizhnaya letopiel ITo. 27, 2 July 1955

PROSVIIOV, Te.S.; SKORNTAKOV, V,I,; BATALITAMS, K.Ta. Prinimali
uchasti7e: VOLYAL_G.-S * INTYUKHOV, V.I.; SHMONINA. N.V.
,,- P
PASHCHINSKAYA, G., red.izd-va; NIXOLATjWA, T., tekhu.red.
[Commercial and some noncommercial fishes of the western
coast of Africa (from the Levrier Bay to the Gulf of Guinea);
textbook for fishery workers] Promyslovys i nekotorys nepro-
myslovye ryby zapadnogo poberezhlia Afriki (ot bukhty Levris
do GvInaiskogo zaliva); posobie dlia promyslovikov. Kalinin-
grad, 1961. 175 P. (MIRA 15.-2)
1,, Konigsberg. Baltiyakiy nauchno-issledovatel'skiy institut
morskogo rybnogo khozyaystva i okeanografil. 2. Baltiyski7
nauchno-isaledovatellskiy institut morekog'o rybuogo khozyaystva
i okeanografil (for Prosvirov, Skornyakov, Batallyants).
(Atlantic Ocea*a--Fiohes)

VOLYA, Oleg nadimirOviahj GAYDUK, K.V., red.j BODANOVA, A.P.,
tekhn. reT.-
(Present-day wooden bridges] Sovremennye dereviannye mosty.
Moskva, AvtotranBizdat, 1963. 54 P. (MIRA 16:6)
(Bridges, Wooden)

TJSSR / Human and Animal Physiology (Normal and Pathological).
Digestion6
Abe Jour Ref Zhui- - Biologlya, No 15, 1958, No. 6o476
Author Faytollberg, R. 0. Vo L, Z. M.; Alcknoyova, Z. 1.
Inst Odooon Univoraity
Titlo :Glucoso, Poptono and Chlorido Absorption in the Small
Intestine of Shoop
Orig Pub :Pratei Odealk. un-tu. Sor. biol. n., Tr- Odosek. un-ta&
Sor. biol. n-, 1957, 147, No 8, 27-33
Abstract :The glucose, peptone and chloride absorption in a loop
of tho small intestine isolated, according to Tiri in-
croaacd with tho increase in concontration of the admin-
istored solutions.
T

VOLYA, Z. M.
Volys, Z. M. - "Sex cycles in guinea pigs so Trudy Odes. gos. un-ta im. Bechnikova,
Vol IV9 1949, p. 135-63- Dibliog: 25 Items
SO: U-3ZW# 17, Deco 53v (Letopia 'Zhurnal 'nykh Statay. No. 23, 2949).

USSR/Human and Animal Physioloa ., Digestion - I The Intestines T-7
AbsIjouri Ref ZhurDiol., NO 12, 1958P 55768.
Author : Faitel'berg, A. 0., volya, Z..M., Alekseyeva) Z.I.
Inst : University of OdOGGa.
Title : Simultaneous Absorption of Carbohydrates, Peptones,
and Chlorides by the Small.Intestine ln*Sheep.
Orig Pub: Nauch. yezhegodnik. Odeask..un-ta, 1956, Odessa,
1951; 232-233.
Abstract: In sheep with a severed small intestinal loop accord-
-ing to the method of Tiry, the following substances
were absorbed during a 30 minute period: 8-20
percent of C1 from a 9 percent or a 2 percent solu-
tion of NaCl; 6-30 percent of glucose (I) from a
5 percent solution of 1; 18-29 percent of I from
Card 1/2

BLUTEKIYI V.A., .Inzh.1 PAVLOVA, Ye.F.p inzh.; KUCHERENKO, L.A.,, Jnzh.;
RYBCHINSFIY, 0.1., inzh.; VO,LYAK, G.E., inzh.
Effect of the surface area on the linear dimensions of leather and
application of the dependence in -the establishment of technical
norms, Nauch.-isslatrudy Ukr NIIKP no.l3x2l6-221 162. (MIRA 18:2)

1131:); cl, z4vadlidys W, Is. V j)XtOTj fallhi"I
4 a vatkal cipMwy Is lmuwrmf In water. TIw invalwu%
litimpWiWallOwnwolm-us
~Wlmyb idowly witMawu (two
=71%:bm
101hermn

VOLYAK, L. D.
"Measuring the Surface Tension of Liquids at Ifigh Temperatures and Pressures," Theals for
degree of Candidate Technical Sol. Sub 22 May 50, Moscow Order of Lenin A71ation InEt
imeni Sergo Ordzhonikidze
Summary 71, 4 SOP 52, D192Artationn Pr Rented for Devrels In Sojeace Ald Zarl-neeriap.-In
Moocow in 1950. From Vecheravaya TlopMa. Jan-Doe 1950-

mostmem"I W Watts 40"61" of poemloso east
44MIM144*64 oil Of WIS OF two 414141 11. 11.
-11l,favals. id",ebar.u.mby
shwInrreakd. fam The thoeftme of tho .1. 1.
2 nWPkrke (cf, &.#,. 0,113 land OAM mm. ) t".
vJcw4 is a thki-ir tube. The Kv ton 10
of the nowfle 11411111M yt twid diplomyl t"If
49.X..02 380 Mrb-14.7. A" WWI "Aart lwj~
114'a, W'X"ikl'is NI'l. plil'. vinst Ahl .
at the 1,4timaim ig Ifill sold, valmo. A MA";
1041 (dj' OAMT) OWN, W. 9--g., 23.4 said IVA at If$.?
&list 1321, frop.j thit CA, fettip. of this Oak. am 201,
111her"m

it is so a #11 a of So p Al It 9 a
L I 4-.U 11111111MISWIS61
to 0
'"0 !Ewtel, -ads
00 =612-41
Mi. 149gotho" of tm m 0
100 %(W9 I , twoolmogwow. LD..VlWYAK. AAJ,
00 Alk-1. Nda*. US& 74 (No. 2) 307-10 (1930) 14
Ittsults off shvts of rwasumn"Us 0( ft gwr&v -00
fmakm a( lilt) witma the twwmlum moo ar-
354r. tmk* Ule nuchad of 2 capilmy tuba. SfiA
app-mus *as und at Wshw taropemium it *as
rolow that The rawls Oh4ped for llw Wnpuslum =4111111
3 fall" ZW-JIS*c (aiw with van Ja We&,
funnute #-4TIPNI whole PVV too
of 211 AtM r, - 647-1, VW 0-60. The odaw
A 0
06 rOmulA c&n be used rut the inteml 3SP-37Vc. It
riAlm-s Out wata b prllvi"ly noti-Assixisted abuvo
00 .4 23Wc. by Wolf P&W stowl" a(,tA1/D)j
00 z - t 2v, - r the desm or amx", ", or 9*0
zoo
water (2) was cyaluawd fur Uw frAcnall 0-32Wc.
The empWW Immuls o( bochn"ii v - I D - 4)4 SO 0
00 1
(,D - dc"IY Of The liquid. J - vapour dervitify) Sim
r 70 for the rano W_ 3Wc-.
I.At'"MAN
UICIA14011 CLASWKAfIC*
, I": . - . 7..;: ~ I -_ __ . 0
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U a AV 10 AS ltemedifeuK a ; a,
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jjj i

VCLYAY, L.D.
Surface Tensicn volume. aur. fiz. k1jim. 26 no. 3
Surface tension of liquids a2 a function of reduced
t52
10,52 Uncl.
of Congress,
ssian Accessions, Library
ist o f E~u

..VW/Chemistr-y Physical chemistry
Cdxd
Authors Vollyakl, L. Do
Title i About, a more accurate. expression for the dependence of surface ton3ion
of liquids upon their reduced voluwe
Periodical Zhur. fiz. khim. 283 Ed, 63 1095'- 1097, June 1954
Abstract. A formula, giving a more accurate expres .sion of the relation between
r-face-tension and densit in liquid and gaseous phases, is presented.
s
u WY
Aformula, based on the van der Waals capillary theory, expressing
the surface tension of liquids as a function of density, is described.
IR references. Table.
Three USS
Institution Aviation Institut,e, Moscow
Submitted November 9, 1953

, --.' - , "; , ~ i- I..,
--.- - -:.
~- -- -~n=

USSR/Statistical Physics - Thermodynamics. D-3
Abs Jour : Referat.Zhur - Fizika, No 5, 1957, 11439
Author : Volyak, L.D.
Inst Moscow Aviation Institute
Title Heat of.Evaporation as a E'unction of the Specific Volume
of the Phases.
Orig Pub : Zki. fiz. khimii, 1956, 30, No 10, 2244-2247
Abstract : An equation is pro-posed with which to express the depen-
dence of the heat of evaporation on the specific volume of
the phases of a substance, namely r = D Lexp (-cjv1) -exp
vi _v) 7] . 'She values of the constants of
fcl _c2 (v1 I
the equation, calculated for 18 substances are given.
Comparison of the calculated and experimental values of
the heat of evaporation shows that the equation is applica-
ble
Card 1/2

USSR/Statistical Physics - Thermodynamics. D-3
Abs Jour Bef Zhur - Fizika, No 5.1 1957., 11439
over a very wide range of temperatures, including also
the critical point; to some substances this equation
is applicable in a narrover range: the boiling point
at normal pressure -- critical point. In a temperature
range that falls short by approximately 200 of the cri-
tical point, the simpler equation r =11, exp (-civ,)
is adequate.
Card 2/2

AUTHORt Volyak, L.D., Cand.Tech.Sci. SOV/96-58-7-9/22
TITLE: Equations for calculating the surface tension of liquids (Uravneniya
dlya raseheta poverkhnostnogo natyazheniya zhidkostey.)
PERIODICALs Toploonergetika, 1958, V#R- T , 71o.7) pp. 33-37 (USS11)
ABSTRAM Surface tension d4ta in often required for heat-exchauge calculationts,
but experimental data in available only for a limited number of
substances and not at high temperatures. Therefore, various formulae
are used to calculate surface tension but their reliabilityis
doubtful near the critical temperatures. One such formula is that of
Oetvos (1886), given as equation (1); it is very accurate for benzole,
.less accurate for heptane, but, as will be seen from Fig.l., it is.
inapplicable to water. The linear relationship is observed for only
a few substan-.es. Var, der Weals showed that surface tension is a
function of the ratiu of the temperature to the critical temperature;
he did not determine the nature of the function but it has since been
established. Van der Weals formula, in the form generally used,
applies to a considerable number of substances, but not to others such
as water and alcohols, as will be seen from Fig.2. A characteristic
of the graphs is the increase in steepness near the critical point.
Bachinakiy, in 1921, proposed an empirical formula for the
relationship between the surface tension of a liquid, and the densities
of the liquid and its saturated vapour. It is seen from Fig.3- that
Card 1/4 for some substances such as ethyl alcohol and benzole the formula is

Equations for calculating the surfs" tension of liquids. SOV/96-58-7-9/22
valid over a wide temperature range, but for all of them it is
inapplicable near the critical temperature. Some investigators who
have made use of Bachinskiy's work have forgotton this point. A new
equation is then proposed in which surface tension is expressed as a
function of the specific volume of the substance. A version of this
equation published in 1950 was very approximate, but a now and more
accurate form is given in terms of the specific volum of the liquid
and gas phases and two tonstants characteristic of the substance
considered. Unlike other formulae, this equation can be applied to
all substances. The second term of the formula is much smaller than
the first. An will be seen from Table.2., only the latter need be
taken into account beyond a few degrees below the critical point,
and a simpler expression can be used for most practical purposes.
According to this expression, the logarithm of the surface tension
minus the logarithm of the specific volume of the liquid phase should
be a linear function of the specifia volume. Experimental data for
associated alcohols and benzole are given in the graph in Fig.4.,
from which it will be seen that this relationship is fulfilled with
high accuraty. The equation is applicable to all other substances;
Card 2/4

Equations for calculating the surface tension of liquids SOV/9,3-58-7-9/22
the constants required in the equation are given in Table.2. for
about 30 substances, The table also shows the lower limits of
temperature for which the difference between experimental and
calculated values of surface tension does not exceed 1 - 2%. It WU3
of interest to check the formula in application to water. It will
be seen from Table.3. that over the temperature range of 100 - 3200C
the calculated and experimental values are in very good agreementj
at 3300C the error is only 2.7%, which is lose than experimental
error. At temperatures below 1000C the error is systematic and
increasing, apparently because of the anomalous behaviour of water
at low temperatures. The difference is somewhat greater also above
3300G, and reaches 5% at 3400C4 this is probably due to errors in
the eiperimental determinations rather than to error of the
formula. The equation can be refined, but it in already
serviceable for extrapolation to temperature ranges in which no
Card 3/4

Equations for calculating the surface tension of liquids. SOV/95-58-7-9/22
surface tension data are available; the surface tension of water
has been colculated for the temperature range 340 - 3740C, with
the resultt- shown in Table.3. There are 4 figures, 3 tables and
10 literature references (I German, 1 English and 8 Soviet
(of which 2 translated from English or German)).
ASSOCIATIONs Mookovskiy Aviatsionnyy Institute (Moscow Aviation Institute)
1. Liquids - Surface tension 2. Liquids - Temperature factors
3. %thematies - Applications
Card 4/4
Eta I I
~-R

17860
S/535/61/000/132/Oo6/ol2
P.0/00 E03o/&484
AUTHOR Volyak, L.D., Candidate of Technical Sciences
TITLE: -1-nv;`st-,9ation of the surface tension of kerosene T--l,
gasoline 0-70 (B-70) and liquid fuel T-5
SOURCEt Moscow. Aviatsionnyy inatitut. Trudy. no.132.1961.63-78.
Teplofizicheskiye avoystva nekotorykh aviatsionnykh
topliv v zh1dkom i gazoobraznom sontoyanii,
TEXTs Surface tensions have been measured over the temperature
range -50 to 300'2C, by using the capillary attraction method.
Meniscus corrections were reduz;ed by using two capillaries of
different diameters and measuring H the difference in liquicr
heights. The surfa-ze tension o is then given by the formula:
a -- la 2 (D - d)
where D and d are liquid-and vapour dansities, and a is
given by 2 R
a
Card 1/ 3

Investigation of the surfa-ae
1660
S/535/61/000/132/oo6/ol2
9030/9484
and b1 and b2 are the radii of turvaturen of the menuscis in
the capillaries. Two different sets of apparatus, developed at
the Kafedra fiziki (Physics Department)of MI. were used,
depending on the -value of surfatzu tension to be measured;
they hadradii. rl =7 0.1348 mm and- r2 = 0.326 mm (Apparatus 1)
and rl a 0.1507 mm and- -2 -70,418 mm (Apparatus 2). Below
ambient temperatures, a Dawar --ressel with dry ice and alcohol was
used'.as thermostat, and above ambient temp6ratures an air bath was
used. All the -rapour densities were ~:alculated from the formula
d w pM/RT, where the equilibrium vapour pressures were taken from
the data of S.N.Sokole-r and'Yu.V.Tarlakov (P.123 of this volume)
and the molecular weights f=om E.A.Balamutova (p.144 of this
volume). For kerosene and T-5, the data are accurate to 3% at
the highest and 1.3% at the lowest temperatures. For gasoline.
the accuracy is similar at the lowest temperatures but greater at
the-highest temperaturss due to un,_-ertainties in the necessary
extrapolation of the density data. All the da+a have been fitted
to various formulae, and for that of Ba,:.-hinaky, i.e.
0 -,- 56 (D - d )Ii
with a in erg/.=2 and densities in g/-.m3, the data (smoothed
Card 2/3

Investigation of the surfac-a
values) are:
17W
S/535/61/000/132/0o6/oI2
Table 6-
t '*C Gasoline Kerosene Fuel t OC Gasoline Kerosene Fuel
B-70 T-1 T-5 B-70 T-1 T-5
20 2.6 0.8 1 200 9.5 5 2.
100 2.7 1 1.4 300 85 17 6
At intermediate temperatures for kerosene and T-5, interpolation is
valid using any reputable formula, such as Bachinsky's, Eotvosl,-
van der Waals' etc. but for gasoline, because of the wider range
of its composition, no formula can be regarded as satisfactory for
interpolation. There are 4 figures, 6 tables and 6 Soviet
references.
Card 3/3

. VOLYAK, L.D.j ANDREYEVA, L.P. (Moskva)
Study of the surface tension of n-heptane and n-ootane. Zhuro
fiz. kbim. 35 no.7:1416-1A17 Jl 161. (MIRA 14:7)
(Heptane) (Octane) (Surface tension)

3042-
S/170
/62/005/003/004/012
B1521B102
AUTHOR: Volyak, L. D.
TITLE: Dimerization of alkali vapors and calculation of their
thermodynamic properties up to 150001C
PERIODICAL; Inzhenerno-fizicheskiy zhurnal, v- 5, no, 3. 1962; 51-57
TEXT; Apart from an experimental study of dimerization effects the entropy;
enthalpy, specific heat, and den 11 ity of sodium vapors are calculated, with
allowance for dimerization, up to 15000C and a pressure of 35 atmospheres.
The luminescent intensity of a mixture of the vapors of sodium and bromine
was found to be proportional to the number of diatomio molecules NR2 in
the reaction: Na2 + Br - NaBr + Na + 68 kcal/9-mole. The dimerization
energy was calculated from the ratio of radiation intensities at different
temperatures. The author completed the data given by Sittig (Ref- 7, see
below) by the specific heat ap, the vapor density d, and the specific
entropies s', a lit, a2 It, and all corresponding to the condensed phaaej the
monatomic and the diatomic form in saturated vapors, and the equilibrium
Card (13)

S/170/62/005/003/004/012
Dimerization of alkali vapors B152/BI02
mixture of both forms in saturated vapor, respectively,
al cPC /T dT + const, where al 4000C '0, Bill - s' -~ r,/T,
82" a' + r2 /T, s" - a' + r/T. For the i(s) Plot up to 15000C the values
at* a 111.4 82 ", it, r,, r2, r, 'd) 'I"9 Yt ill were extrapolated along the
"aturation curve. Using r I and r2 and numerically integrating
Clausius-Clapeyron's equation the author determined the partial pressures
p, and P2 and the total pressure p as well as the volume concentrations
X1 W pj/p and X2 a P2 /p along the saturation curve and the equilibrium
constant K = p2 . The specific enthalpy and entropy are additive
P 1/P2
functions: i - (X IiI + 2X212)/(1 + X2); a - (Xial + 2X 282)/(1 + X2). The
volume2concentrations were calculated along an isotherm with
KP 0 XIPA' Xj) and X 2 - 1 - X1. a 1 and a2 also are calculated along an
isotherm a a," - R/A ln(pX,/p,X,,), analogously 82 . The subscript a
Card 2/3 A

S/170/62/005/003/004/012
Dimerization of alkali vapors ... B152/B102
indicates values on th6 saturation curve at equal temperatures, The
specific heat follows2from: o p . Cpf - 21 d(8X2/aT)p/(l + X2)2. Using
d 1n Kp/dT - 46 1d/RT 9 Kp . x1p/(1 - Xj), the author obtains
cp - 0pf + 92 XI x2 ('d/T )2/R(1 + X2 )3. epf is the specific heat of the
solid alkali; it increases only slightly (0.212 to 0.216 kcal/kg deg) but
the effective specific heat attains 0.918 kcal/kg deg. The results show
that dimerization causes a considerable increase in specific heat. There
are 3 figures, 1 table, and 7 references: I Soviet and 6 non-Soviet.
The three references to English-language publications read as follows:
Fraser, R. Molecular Rays, 1931; Loomis, F. W. and Nusbaum~ R. E. Phys.
Rev. 40, 380, 1932; Sittig, M. Sodium, its manufacture properties and uses,
N--J-t 1956.
ASSOCIATION:, Aviatsionnyy institut im. Sergo Ordzhonikidze, g. Moskva
(Institute of Aviation imeni Sergo Ordzhonikidze, Most.,ow)
SUBMITTED: May 12, 1961
Card 3/3

L 3h116-& w(m)AWMATI IJP(c) JDtWd1Jq
ACC NR: AP6008828 SOURCE CODE: UR/0294/66/004/001/0050/0054
AUTHOR: Vinogradov, Yu. K. (Moscow); Volyak,, L. ~ (Moscow)
ORG: none
TITLE: Experimental determination of the saturated vapor pressure of sodium and
potassium
IA
4SOURCE: Teplofizika vysokikh tomperatur, v. 4, no. 1, 1966, 60-64
TOPIC TAGS: vapor pressure, sodium, potassium
A13STIIACT: Using the equilibrium method, the authors measured the saturated vapor
pressures of sodium and potassium in order to be able to use these values for ctilc-uTa-ting
the dissociation energy of the Na2 and K. molecules. It Is shown that the equations describ-
ing the experimental data obtained for the vapor pressure are of the form
V 0
lp-A 71-
the coefficients of these equations being (in physical atmospheres)
Card 1/2 UDC: 646.32+546.33,536.421.3.001.5

L 341i6_66
ACC NR: AP6008828
A 0 ID-106 X-10, Floge 0
Element
-Sodipgi, to ~898i 5720.4 2 0076 6.00362 0 92568 0.48510 2458
10 10888 1 91400 4.9M 1 070.~ 0.56762 '2641
Potilwalu.1 4768.1
Table 1. Coefficients of equations In the measurement of saturated vapor pressures In
physical atmospheres.
iFrom these equations, the vapor pressures of sodium and potassium were obtained for 700
750, 800, 850, 900, and 950C. The experimental values of P and equations log p = f(T)
Obtained will be used further to calculate the dissociation energies of Na2 and K., molecules.
The work was carried out under the guidance of N. B. Vargaft1k, to whom the authors
express their sincere appreciation. Orig. art. 2 figures, 3 tables, and 8 formulas.
SUB CODE: 07 SUBM DATE., 06Jul66 ORIG REF; 003 OTH REP: 007
Card 2 2

VOLYAK L. D.
Calculating the thermophysical properties of sodium, Inzh.-fiz. zhura
5 no.7-.83-85 JI 162. (HIPA 15:7)
1. Avi-atoionnyy inotitut Imeni Sergo Ordzhonikidze, Moskva.
(Sodium-Thermal properties)

Phenomenon of dimerization in vapors of alkall metalz and calculation
of their theomphysical properties up to a temperature of 15WOCe
Inz~.-'fii.zh~r. 5 no.3151-57 Mr 162. (MIRA 150)
1'.Aviatsionnyy institut imeni Sergo OrdzhonWdze,, Moskva.
(Polymers)(Alkaili metals-Tharmal properties)

VOLYN"M 0 N-V. huz.-5~tam oizv.
process of forging die blocks. pr
TechnoloEical iml.R~ 14.n)
3 no.11:22-23 N 161. (Forgine)

386o6
S/170/62/005/007/008/010
B104/B112
AUTHOR. -Vol ak L.
TITLE: A calculation of thermophysical properties-. of oodium
PERIODICAL: Inzhenerno-fizicheskij zhurnal, v. 5, no.,7-i 1962, 83-85
TRIXT: The calculation of the heat of evaporation L and* dL/dt of sodium
is discussed. The results obtaine4 by Inakansi at al. ~(J. of Chemical
and Engin. date, 5, no. 4, 1960) for the properties of sodiun on the
assumption that the enerey of dimerization DO at the absolute zero of
0
temperature is equal to 16,840 kcal/nole are shown to-be incorrect. The
0
correct value of Do is given as 18,200 kcal/mole (cf, It. Sittig, Natriy,
yego proizvodstvo i primeneniye - Sodium, its production and'uae.
Gosatomizdat, 1961; L..D. Volyak, IPZh, no- 3, 1962).
Card

3/170 62/005/007/008/010
A calculation of thermophysical B104/B112
,ASSOCIATION: Aviatsionnyy institut imeni, Sergo Ordzhonikidze,'g. 1;oskva
(Aviation Institute imeni. Sergo Ordzhonikidze, Eoncov)
SUB';."ITTED: April 28, 1962
Card 2/2,

A.
Spiders Cilltasa
Froblfm of r-azz prolagatiop r:f th- spid~~r -TAtlircoJeettta
vicinity of Wessa. Ved. I:araz. i Tway.
Montbly Lis'. of Acc,,~sgj=, Librar-, of Cor~;rcss
Jme 1953. TOG!-

,-VOIZA5S*k4,,.j.3. [Toliinslka. I.B.], student biol. fakulltata;
SAVCHUK",'M-P-, naucbzW rukovoditall. prof.
Effect of royal jolly an the growth and productivity of the
silkworm. Pratst Od.un. ZbIr.9tud.rob, 149 no.5:148-149
159. (MIRA 13110
1. Chlen-korrespondebt AN USSR (for Savchuk). 2. Odeaskiy
gosudarstvenW universite~t.
(Royal jolly) (Silkworms)

VOLYAMUTA,, YO.A.
Hasa m1tiplimtions of Utrodectus lugabris in the Odessa region.
Had. parazit., Nobkva no.1:98 Jan-Yeb 1953. (CIML 24:4)
1. Of Odessa Oblast Anti -'Walarlal Station (Head Physician - Benovich).
-------------

TOLTAMKATA, Ye.A.
Nffect of WT and hexachloriscyc'lohexans on Istrodectur treftzimguttatuil.
Had. paraz. i paraz. bol. 2? no.4:488-489 JI-Ag 158. (MIRA 12:2)
1, Iz otdela parazitologii Odesskoy oblnstnoy sanitarno-epidesiologicheakoy
stantsii (glavuyy vrach A.M. Syrgin, zav. otdolom M.A. Belovich).
(SPIUM, effect of drugs on,
Istrodectus treducumguttatus, Benzene hexachloride & DVf
(Ras
(BANZM HEUCHIORID3, effects,
on latrodectun treducumpttatus (Run))
(WT, effects,
same)

VOLYANSXAYA, Te.A.
DIZ"o= 4-e-9-6-f- Culex esills and Uranotaenia unguiculata in Odessa
and NikolWev Provinces. Kedeparaze i paraz.bol. 27 no.6:737
N-D 158. (MIRA 12:2)
1. Is Odesskoy oblautney sanitarno-opidetiologicheakoy stantsil
WIRAINS-MOSqUITOICS)

K A YA" rs. A,
VOLTANSUYA To A
Preparing permanent specimens from discarded skins of mosquito
larvae and pupae. Ked.parax. i paraz.bol.supplement to no.1:6 '57-
(MIRA 11:1)
1. Iz Odeaskoy oblastno saniterno-epidemidlogicheskoy stantati.
(MOSqUITOiCS) . IIIUCTS--COLIEGTION AUD PRISIRVATION)

VOLUN SXAYA'* Y-8 : A:
f
Odessa - 13piders
Problem of mass propagation of the spider Lathrodectus tredicimguttatus Rossi in the
vicinity of Odessa. Mad. paraz. i parax. bol. No. 1, 1953.
503 Mont List of Russian Accessions$ Library of Congresaj, June 1953, Uncl.

"V
STRUTIJISKIY. Aleksey Bonifstlyevichi insh.; TRSTIYAKOV, ley 'IMMI~evich.
kand.tekhn.nauk; TSBYTLIJI, Aleknandr Alekeendrovich, 7TTIRtakhn.
nauk; VOLYAUSKIYP. A., red.; WVCHITSKATA, 0., red.; (971,41KIS, A.,
tokhnXcf.'"',-IqMfb'f'A.* tekbnored,
(Builderle handbook] Spravochaik waters-etroitelia. 4 M-- Gos.
izd-vo lit-ry po atroit. i arkhit., 1957. 340 p. Owlk 11:3)
(Building)

VOL I Y, -41
.9- r rc. Don' V3 S
-t%Q b.- a mr& u
rc',Ii tnrWro ti fic rch
(Acnd of
rUcloo),
of

tS
7',
jq:~q
t
U-4~- 31

VOLYANISKIT$ N, [Wolanski, NO (Varshava)
Problem of human morpholo&7 in modern Polish anthropolog7o
Arkh.anat. gist i e'mbre 35 uo.W115-128 R-Ag '56 (XIRA Iwo)
AMMOPOLOGY, aspects (BUO)
in Poland, morphole
(MadmOLDGY.
in Polandv anthropol. aspects (Run))

10imov, M.N., doteent, icand. takhn.nauk; 'ALYAMMU70k. P.14., spatered.;
AKIMOTA, L.D., red,; KISLUt Tool., tskhn.red.
(Using pneumatic-tnbe transportation in the food industry]
Opyt primenanila puevmticheakogo transports v pishchavol
promiyahlennosti. Moskva, Piahchepromisdat, 1957. 37 P.
(MIRA 12:5)
(Food Indus t ry-lquipwnt and a lies)
transportati:
(Pneximtic-tube

VOLYANSKAYk,YE. A. and FUTRAN, G. S.
"The Making of Charts of the Parasitic Fauna of Odessa Oblast'."
Tenth Conference on Parsitological Problems and Diseases with Natural
Reservoirs, 22-29 October 1959, Vol, II, Publishing House of Academy of
Sciences# USSR, Moscow-Ieningradv 1959.
Odessa Oblast' Sanitary-Ppidemiological Station

I.L.; AVTZDV, 1.~, GUTNIKOVA, R.I.; VOLYANSKAYA) Ye.
cf pTp7pnting the c-opre4~41tatim ct cotelt (11) 84d
(111). zh-ur. VYKC) 16 nc?.2:0238-239 165.
(KERA'28t6)
1,151.1tit klr2mlli AN Vzl!plolr,~y SM.

MATEVOSYAN P.A.; DANILOV, V.I.; LAPSHOVA, M.P.; KISELEV, A.A.; LISOV, LV.-
0
VOLYANSK1YO,,-V'.H.--.
Improving the quality of blooming mill ingots. Stall 23 no.12:1086-
1087 D 163, (MIRA 17:2)
1. Volgogradskiy metallurgicheskiy zavod "Krasnyy Oktyabrl".

VOLOYEROV, G.B.
Practical training in the me-thods of tbaching chemistry. Khim. v shkole
18 no.608-89 N-D '63# (KRA 17%:L)
1, Pedagogicheskiy institut, g. Chelyabinsk,

VOLIMOV, G.B. (Chelyabinsk)
OFrom the experience of practical application and teaching chemistry
in secondary schools" by IU. I. Xolos6v. Ihim. v shkole 13 no-1:74-76
Ja-I 158. WIM 10:L!)
(Chemistriy-Study and teaching)
(Iolosov, IU. 1.)

VOL,rYUOV.,,G~A.,,. uchitell
Setups for collecting gases by displacement of water. Kh1m.v
shkole 14 no-5:57-59 S-0 159- (MIILI 12:12)
1. Sradnyaya ohkola No-53, Chelyabinsk.
(Chomistry-Manipulatten)

VOLITEROV,-G.B.t uchitell
lxposition of tacbnical creativitYe Khim.y ahkole 14 m -5:95
(MlIth 12:12)
S-O
1. SrsdrWaya(shkolu, flo-53 g.CholyabinakfL.
r --fthibitions)
"helyabinsk-Technoing7

VDLIYERO'V, G.B. (Chelyabinsk)
Apparatus for experiments on establishing the correlation between
the rate of chemical reactions and various factors. Dim. v
shkole 17 no.3:62-65 MY-Je 162. (MIRA 15:6)
(Chemical apparatus)
(Chemical roaction, Rate of)

VOL'YEROV, G.B. (Cholyabinsk)
Studying rosin in a chemical club. Khiz. v shkole 16 no.5:
80-86 S-0 161, (MIM 14:9)
(Gling and resins) (Chemistry--Experiments)

VOL'YEROV, G.B., uzhitell; SOSKIN, G.A. (KaragandiskWa oblast, go
*Classroom experiments in inorganic chemlstryO by T.S.Polosin.
Reviewed by G.B. Vollerov, G.A. Soanin, XhIm. ve ahkole 13
no.4:86-89 il-Ag 160. (MIRA 13:9)
1. Srednma sb3cola No 53, g Chelyabinsk (for Vollyerov).
(chemistry-lxperiments)
(Chemistry, Inorcanic-Laboratory munals)
(Polosin. Vos.)

VOLIYEROY,-A,I.,-,DIYAKOV, I., ucbenik 11 klassa.
New method for the laboratory production of nitric oxide.
Dim. v shkole 16 no.2:78-79 Mr-Ap 161. (MIRA 3.4:6)
1. Chelyabinskiy D7orets pionerov. Mola NO-84 (for Dlyskov).
(Nitrogen oxide)

Va /~,
BANMOV, A., gvardii general-mayor; BOLDYREV, Ns,'Polkoynik; PORTTAM, D.,
polkovnik; XMILITSIV, I., polkovnik; IMRITSOV, A., polkovnik;
VOLINIIIj, A., polkovnik; SHVIDCHIM, IG, polkovnik; PISMV, G.,
NBYNWV, 21., polkovaik; VZRTZIA, 11.9 gvardii polkovnik;
KURATOVAq A,q polkovnik; NIMrAYN, A.$ polkovnik
We discuss projects of now Army regulations. Voen. vest. 38 no.7:2-9
J3. 158- (Russia--Army--Regulations) (MIR& 11:6)

VOLYKHINp Alsksey Mi~~ovlch, polkovnik; DUKACHKV 0 M.P., polkovnik.,
a---KUZ"fflN, red.
r
e
(Regulations on service of the armed forces of the U.S.S.R. in the
zone of the interior are the lav of life for serviaemen and for
mutual relations among them) Ustav vnutrennei sluzbby Vooruzhennykh
Sil Soiuza SM - zakon zhizni voonnooluzhaebobikh; obahchie obiazan-
nosti voomooluzbashohikh i vzaimootnoshaniia mezbdu nimi. Moskva,
Voen. izd-vo M-va oborony SSSR, 1961. 53 p. (MIRA 14210)
(Russia-Armed forcoo--Regulations)

VOLTIICHrl -,Z-,-_
Ungrooved tape. Stan.i Instr. 31 no.,4:38-39 AP '60-
(Tape and dies)
-0
FEW'
'M- SM RROMIMA , Alfflr- PMEB-45IMM, ulge,

S11 84/62/OW/005/00.3/CO3
D040ID113
AUTIIOA: Volynch k A Z, cer
TITLL: Threading in 3taii-dess and heat-resistant; steel elements
P U ODICAL: Nhimicheskoye washillostroyeniye, no. 5, 1962, 32-33
TLXT: New fluteless taps (Fig. 1) now being introduced in the SovieL i;1achine
industry eliminate the usual jamining and breakage of taps when threading in
tough stainless and heat-resistant steels, and are more durable than all existing
fluted taps. Reco-wendations are given concerning the gcoi-wtry of flutcless
taps, selection of proper bore diameters, and cuttingIluid,. These recoliullen-
dations are based on the results of laboratory and-shop tests on a vertical
drilling machine. Test threadin- was conducted in 12 rim thick steel discs, usin,
a cutting fluid comprising 40% sulfof-rezol, 25% kerosene and 35% oleic acid.
Tests proved that the proper selection of the bore diameter results in increased
durability of the tap and improved strength of thread connections. There are
3 figure4 and 2 tables.
Card 1/2

S/184/62/000/005/003/003
Threadin. iii stabiless and hcat-resistant ...... D040/DI13
A
A
N
41
fie,
\A
fz 4.1 \A F ig. 1. The design of th-_- :'Lurcless
A-A tap for threadin., in sta-0.1,.~~.,
heat-resistant steel elements.
Le-gend: (1) dint.11m_x. (2) davera.,e
d
3 ext.
45
csvl
Card 2/2
m

ACC NR:,
AUTHOR:
EWP(l) IJP(c) DAIMAIM111MIM
Volynchik, A. Z.
--%^
9)0
5~3
ORG: None
%A
TITLEt Continuous operation line for assembling and welding of oylindrical.abolls
SOURCE; Byulleten' tekhniko-ekonomicheakoy informataii, no. 2, 1966, 29-31
e T 4 UA. A" ~," , f7.41J-'J1JL ,
TOPIC TAGS: '"ms`t*A*""QuftVr1,- ' forming, buttwelding, conveying equip-
,,,, metal
ment, welding equipment / ;;)~_UFO welding converter, VSK-300 welding generator, TS-17
welding tractor, K374V,pross 19 to IZ
10
ABSTRACT: A description of an assembly line used by the Xurgan Chemical Machinery Plan
is presented. The line is used for assembling and woldine of shells having a diameter
from 1500 to 3000 mm. The operation of the line is explained by means of a floor-plan
ayout. The production line is divided in 13 sections. The operating procedures of
each section are examined and the use of roller convoyora, telphers and other equip 9t
Y-2 tr
for hoisting and conveying of materials are mentioned. Marking, cuttin welding of
rolled she*Sootion I to 5) and the use of PSI-1-1000 welding oonvorte5 Soction 6) and
X374V press, action 7) are mentioned. After rolling operation Section 8), a longi-
tudinal joint is formed by temporary welds made by means of a WK-300 welding generator
(Section 9). Then, the joint is welded from inside by using a TS-17 welding tractor and
1/2 UDC: 658.5Z7:621.757+658.5Z7:621.791

L 45516-66
kCC NRs AP6022176
~SXI-1000 weldine converter (Section 10). The same 4..,me of converter is used for final
)utside, joint welding (Section 11). After calibrati;~ (Section 12), joint tri=ming and
I-ray control inspection (Section 13) the formed and welded shell is removed from the
Losembly line. orig. EAAhas: 1 photo and 1 diagram.
)M CODE: 13/ SM DATE: None

VOLYNCIIIKOVL_Ll Y obl.)
_(g.Lebedyan', Lipetsko.
Along difficult paths of creativeness. Sov. profsoluzy 13
no.2tll-12 Ja 162. (MIRA 15:4)
(1,ebedyan'--Machinery industry--Technological innovations)

VOLYNCHIKOV, N., inzh. (g.Lebedyan'); ZAMKOVSKIY, I.; OBER, Kh.;
MXMWO, M., inzh.,- VLASEKKO, B. (g.Krasnodar)
The reader continuOs the discussion. Sov. profsoiuzy 18 no.gs
16-18 162. WRA 15:4)
1. Prodsedatell meatkoma sluzhby vodo5nabzheniya at. Simferopol'
(for Zamkovskiy). 2. Predsedatell postroykoma stroyupravloniya
No.3 tresta "Promstroy", g. Dushanbe (for Okner). 3. Chlen
mestnogo komiteta proyektnogo inatituta "Mosbasagiproshakht",
g. Tula (for Nikolenko).
(Socialist competition)

vr. XkqHIXQV,,Nik la Vasillyevich; NIKITINA, S.; CHERRENSKIY, P.
y
(Lebodyan) Labedlant. Lipetsk, Lipetakoe knizhnoe izd-
vo, 1962. 35 P. (MIRA 16:11)
(Lebadyan-Description)

USSR / Pharmacology and Toxicology--14edicinal Plants V-5
Abs Jour: Ref Zhur-Biol, 110 232 1958, 107351
Author Koroleva, K. Is, Krasnoperova, E.t Volynchikovaq
M., Korchuganova, G.
Inst Gorno-Altayskiy State Pedagogical Institute
Title The Effect of Black Mountain Ash and Sea Buckthorn
on the Rate of Regeneration of Injured Tissue
Orig Pub: Uch. zap. Gorno-Altayskiy gos. ped. in-t, 1957,
vyp. 2, 278-28o
Abstract: Experimental wounds in rabbits were ..*3-tted with
juices of the black mountain ash and sea buckthorn.
Observations showed that the wounds wetted with the
juices, especially with the simultaneous introduc-
tion of the juices per os, in a dose of 3 ml,
Card 1/2
23