SCIENTIFIC ABSTRACT VOLVOVSKIY, B.S. - VOLVOVSKIY, I.S.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001860730001-5
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 9, 2001
• Sequence Number: 1
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

GODIN,, Yu.N., akademik (deceased]; VOL'-YOVSKIYL B.St; VOLIVOVSKIY, I.S.;
RIABOY, V.Z.; SHRAYBKAR, V.I.
Characteristics of the structure of the earth's crust in
the vestern part of Central Asia. Dokle' AN SSSR 146
no.4:813-815 0 162. (MIRA 1511l)
1. Inatitut ge4ogii AN Turkmenskoy SSR, VsesoyumW
nauchno-iooledovatellskiy institut, geofizicheskikh
metodov razvedki i Moskovskiy inBtitut, neftekhimichookoy
i gazovoypromyohlennosti., 2. AN nirkmanskoySSR (for Godin).
(Asi4p-Central--Seismic prospe'cting)

I"ACCESSION 11R: AR4036339 0/0169/64/000/003/0004/G004
'SOURCE: lieferativny*y zburnal. Geofizikaj Abe, 3G19
AUTHOR: Vollvovskiyp I..S.j Vol.1vovskiy, B. S.
TITLE: Characteristics of the st;:~eT --'6f'the-4&rtb1e crust in the western
part of Soviet Central Asia (on the basis of data from integrated geophysical
investigations) I - I
CITED SOURCE: Sb. Tezisy* dokl'* Soyesbchaniya po probl. tektoniki. M., AN SSSRA
1962, 147-149
TOPIC TAGS: geology, geophysics, geophysical exploration, earth's crust,
Moborovicie discontinuity, seismology, crustal structure, deep seismic sounding
gravimetry
TRANSLATION: On the basis of the structure of the earth's crust in Central
Asia it is possible to define two zones: a western.zone with relatively simple
structure and an eastern zone which has a considerably more complex structure.
In the eastern zone there is a deep downwarping of the Moborovicie discontinuity
;Card

ACCESSION NR: AR4036339
in the Fergana depression,, a decrease in crustal thickness in the bordering
ranges and a plunging of the surface of the suberustal layer toward the Pamir-
Alay system. Individual uplifts are noted in the western zone against a back-
ground of smooth plunging of the Mohorovicic discontinuity in a southward di-
rection. On the whole, within the Kopet-Dag and Pamir-Alay system there is an
inverse relationship between the surface relief and the surface of the suberustal
layer, whereas in the mountain structures of the zone of renewed folding (Kura-
tinskiy, Ferganskiy, Turkestanskiy and Ku~aminskiy Ranges) there is a direct re-
lationship between the two forms of relief. Within the limits of a platform
uplifted sectors of the crust correspond to an arching uplift of the surface of
the folded basement, tbat"'is, the thickness of the crystalline crust remains
approximately-constant. In geologically uniform regions the earth's crust in
the process of tectonic development apparently does not experience special ad-
justments; the cause of movements is physicochemical processes in the suberustal
matter. A comparison of deep seismic sounding and gravimetric data makes it
possible to detect those relationships between density differentiation of the
Card 2/3

AccEssioN m: AR4036339
1; subcrustal matter and tectonic movements in the crust wbich vill serve as
confirmation of the hypothesis of phase transitiohe of suberustal matter.
I. Galkin
DAIE ACQ: i7Apr64 SUB COLE: AS SNCL: 00
Card 3/3

B/169/61/000/011/018/'065
D228/D304
AUTHORSs Vollvovskiyq B.S.9 Vollvovskiyq I.S.9 and Ryaboy~ V~Z.
TITLE; Laboratory use of the method of controllable dl -rected
reception for interpreting the data of deep seismic
sounding
PERIODICAL: Referativnyy zhurnalp Geofizikat no. 11, 1961, 21,
abstract 11A197 (V sb. Razved. i promysl. geofiz., no.
369 M., 19609 8 - 13)
TEXT: The laboratory modification of the method of controllable di-
reoted 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 112

31169161100010111'0!8106-
laboratory use of the method of D228/D304
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 OTigin, [Ab
stractor's note: Complete translationi.

GODIN, Yu.N.; VOL'VOVSKIY, B.S:j VOL'VOVSYIY' I.S.; FOMNEO, K.Ye.
StudyinF, the structure of the Parth's crust in the courEe Of
reFlonal- 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. AN VISSR.
Spr. ppofiz. no.10:11A_1471 0 '61. (14IRA 110 9)
1. All Turkmenskoy SSR I Vsesoyuznyy nauchno-issipdovatel'skly
institut peofizicheskikh metodov razvedki.
(Seisomometry) (Earth--Surface)

5/049/62/000/0 W 002/003
1046/1246
AU'L'IiO?.'-,: ;3elousov, 7.G., Vol'vov3kiy, B.S., Vollvovakiyp I.S. and Ryaboyo V,Z,
TITL3: Experimental inventication of the reg~ntration of deep-reflecteO
waves
frR I DDIt i)l- j'U:adr--.-.Aya naW, S~;SR. Izvestiyao "e37iya gOOfizicheskaya, n6. 8, 1962,
1034-1044
TI-=L: A report on the deep seismic s-ziundine with reflected (subcritical) waves
carried out in 196N10,61 in the South-!~astcrn 'Aurkmenia over a 120 km profile. The
noise waves were eliminated by uoin,- directional reception: seismorecolver3 and sources
of scumic vibrations were f-rojped together (9 rec~ivera spaced evenly over a linear
distance of 4.00 m, anch group rq~.;oved by 100 m from its neighbors). Comparison of the
resulto with the data obtained in 11,~50 in deep neismic sounding with reflected (hyper-
critical) and leadinj; waves L:Ood at;rccment in j;eneral features on the eeismo-
grams, though subcritical reflection is better in detecting fine details. It is
Card 1/2

Experimental inventilation of the regi3tration....
recomm.ended to use ~an far 110 po3nible a combination of the two methods. There are
8 fif;ure3.
SIMNITTED: ','Cbruax-j 26. 1962
_Y aauchno-issledovatellskiy institut f;eofizicheakikh
CSOCIATION: Voesoyuzny
metodov razvcd",i (The All-Union Scientific Research Institute of
Geophysical -;at~ods of Prospecting)

VOLIVOVSKIY, B.S.; VOLIVOVSKIY, I.S.-, RYABOY, V.Z.
Some d-a-VI-on seismic waves corresponding to the layer beneath the
crust. Prikl. geofiz. no-31:3-10 161. (KIRA 15:3)
(Uzbekistan--Seismic prospecting) (Earth--Internal structure)

BELOUSOV V.G.; VOLVOVSKI, B.S. ULok'vovs)dyj. B.So); VOLVOVSKI, I.S.
Nollvovokiyp I.S.1; RUBOI) 'V.Z9 -' '
Experimental research on the registering of the waves reflected
by depth. Analele geol geogr 17 no.3:51-6/+ JI-S 163.

~S/552/61/000/031/001/00,5
D218/D304
AUTHORS: Vollvoskiy, B.S., Vollvovskiy, I.S. and Ryaboy, V.Z.
TITLE- Some data on seismic waves corresponding to the subcrustal.
layer (based on the results of scisruic studies of the
earth's crust in Uzbekistan)
SOURCE: Moscow. Vaesoyuznyy nauchno-iseledovatellskiy institut
geofizicheakikh metodov razvedki. Prildadnaya geofizika.
No. 31, 1961, 3-10
TEXT3 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 Karabekaul-Koytash profiles.
This research was carried out by the Uzbekskiy geofizicheskiy treat
(Uzbek Geophysical Trust) and the Voesoyuznyy nauchno-issledovatellskiy
institut geofizicheakikh 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 Central Asia by the Geofizicheakiy institut AN SSSR (Geophysical
Card 1/4

S/552/61/000/031/001/003
Some data on seismic waves D218/D304
Institute of the AS USSR) previously known an Institut fiziki Zemli
(Institute of Physics of the Earth) on the initiativej and Initially un-
der the direction of Academician G.A. Gamburtsev. Multiple seismographs
were employed 0 instruments per group), the distance between the groups
being 100 m. 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, napely 1) longitudinal refracted waves
recorded both in first and subsequent arrivals, 2) reflected waves from
low-lying separation boundaries in the crust recorded both at near
(W~O km) and distant (300 km) points, and 3) waves which could be as-
4ribed to multiple reflected-refracted and 6omposite 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 Leningradakoyo otdeleniye matematiches-
kogo instituta AN SSSR (Leningrad Branch of the Mathematical Institute AS
USSR) by G.I. Petrashen', A.S. Alekseyev and others# These calculation&
Card 2/4

-9/552/61/000/031/001/003
Some data on seismic waves see 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 crust).
In the present studies waves reflected from the surfaca of the subcrustal
llayer (Mohorovicit discontinuity) were observable beginning at 30-40 km
from the point of explosion and were recorded in subsequent arrivals in
the entire range of distanceso The apparent velocities of these waves
were found to decrease from 9-10 km/see at 80-90 km to 6.5-7-0 km/set
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 2A 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 prodiots that the reflected waves should have higher
Card 3/4

S/552/61/000/0031/001/003
Some dot.* on seismic waves o*o 0218/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-
flected from the Mohorovicic discontinuity before and after the critical
angle can be determined from seismographs. 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 latter. For the purposes of
deep seismic *ounding these, waves may be interpreted as head waves cor-
respondiog to the surface of the subcrustal layer. There are 8 figures
and 10 Soviet-bloc references.
Card 4/4

GOLUBOV, LEIGEYDA., N.F.; ZAiTTAROV, A.Ye.,, FAPFYEV, A.Yu.,, FANIKIN, 'I.I.;
SAFRYGINP KII.M.; NOSOV) V.S.; VOLITER "ir- V SHUL"JA, 'Yr,.A.;
MMOSIRUCHNFOY 5.1.
Effect of,Lhe rate of plate cooling an the quality-of the metal
after rolling. Met. i gornorud. prom. no.1:33-36 Js--F 165.
(MIRA 18:3)

tumd idd mletra here, takits Lzto scc-mxt JaMs=ce shear wd
Nt c--Zrr-iz*m i I F.Jvcr. ~erwrzll Eteat ~q;tu4
.:54 mqC-&.zA

--)- - . ---- - - ~ -~ --- -- I . 1 .1 --. -
I')
,, !~, "I

V,Z,/ rxllgl?.I,i
VOWTKAN, X. [Voltmanis, Ir.]
Imigrant falsehood and Soviet reality. Bov. profsoiuzy 6 no.1:48-53
Ja 158. (RIM ll: 1)
I.Predsedatell Istviyakogo respublikanskogo soveta profsoyuzov.
Petvians)
0419 MM"M ME A rd I I 10 10 U e
074=~W-M --~-TMIM-,

Trade-Unions - Latvia
Daily attention to building up a trade-unton core, V pom. profaktivu, 13, No. 7, 1952
Montha List 2.f Russian Acc2ssLoas, Library of Congress, PAY 1952, Unclassified.

VOLITHAN, X., predsedatall.
Latvian trade-unions' work with the masses in industry. Prof. soiusy 8
no. 6:35-39 Je '53. (MLEA 6:5)
1. 1&tv1yskiyr~Bpub1ikansk1y eovet profsoyuzovs (Efficiency, Industrial)

SHMALI, G. (Kiyev); KRIVOSHEM (Kirovogradakaya obl.); RAPCHINSKIY, A.
(Dnepropetrovskaya obl*I,-'imROT, Z.j VOLITMkN,_.V. (g.WYazin;
"lininskoy obl.); KOIWOV, I.,, yurist,
Replies to our readers. Sov.profooiuzy 17 no.3.1:41 je. 161.
(MIRA 14:5)
1. KonBulstant 7twidicheakogo sektora Ukrainskogo reptailrain kogo
sovets, profsoyuzov (for Sizorot). -
(Wage psyment'systems) (Vacation4., Employee)

V, L
5(1,3) PWE .1 BOOK EXPLO=-TAMON SGV/3170
Fabrikant, Tamara. Llvovna, and.Vollf Leonovich Volltman
Asbovinil I yego px4meneniye v khwchesko3r promysl-ftennosti (Asbovinyl and Its
Ptilization in the Chemical Industry) Moscow, GOBIrbimizdat'.1958-
78 p. Errata slip inserted. (Series: Korroziya v k3himicheakikh
proizvodatvakh I sposoby zaahchity, vyp. 1-1) 3,000 copies printed
Ed.: I.Ya. Klinov; EditorialCOMMIssiOn: N.A. Baklanov, V.Ye. Volodin,
V..-S. Kiselev (Chairman); I.Ya.! Klinov, V.I. Kruchinin (Secretary),
'G.V. Sagalayev (Deputy Chairman), and F.G. Udyma.
FURME: , This booklet in intended for workers Bpep ializing In corrosim preventim
and for design engineers of chemical and related industries
COVERAGE: This bpoklet deals vith the prevention of corrosion ant anticox''g '1ve
materials. It reviews rehVicochemical and meebanical properties of asbavinyl
which is an anticorrosive mixture, the uaoic components of which are ethynol
(divinyl acetylene),lacquer and asbestos. Methoda for preparation of the
Card 1/5

Asbovinyl and Its' Utilization (Cont.) SOV/3170
asbovinyl mixture and the utilization of this mixture as a protective material
against corrosion are briefly outlined and safaty te-~hniques during pro-
duction are reviewed. Chemical resistance of &Iffer*nt types of asbovinyl to
corrosive agents is discussed. The expmriercn of the induntry in using asbovinyl
mixture for the lining of varioun containers., ff1ters, gFw conduits, pipes, ate.,
is outlined. The procedure for using this mixture as a corrosion resistant
material is explained as well as methods of storing, tranBporting, packing, etc.
Studies of A.L. Klenbansldy, I.M. Dolgapollokiy and I.P. Shabodalov proved that
asbovinyl mixture can be used succesafully for protecting equipment of the chem-
ical industry against corrosion. It in now vid,&V, used in Soviet industry. There
are 16 mferences: 14 Soviet and 2 English.
TABLE OF CONTENTS:
From the Editor 3
Foreword 5
I. General Information 7
11.. Basic Materials 9
Caid 2/5

Asbovinyl and Its Utilization (Cont.) SOV/3170
Rthynol lacquer 9
As'bestos 13
III. Production Process for the rreparation of Asbqviayl Mixture 19
Preparation and dosing of rav material 19
Mixing 19
Packing 20
,storing 20
Production contro2. 20
Consumption of materials used im preparing th(* Initial anbovinyl
mixture 20
Technical specifications for the asbovinyl mixture 21
IV, Properties of Asbovinyl 29
Physical and mechanical properties 22
Chemical resistance 26
V. Use of Asbovinyl as an Anticorrosion,Mat~eriai 34
Card 3/ 5

Asbovinyl and Ito Utilization (Cont.) BOV/13170
Use of asbovinyl as fettling 34
Use of asbovinyl as dyeing lacquer '38
Use of aabovinyl as a base coating 38
VI. Experience of the Industry- In Using Anboy-Inly a6 a Protective
C.oating 42
Lining of bubbling towers used in the produett~--n of sulfuric acid 42
Lining of acid tanks 43
Lining of fermentation druns 44
Lining of alkali neutrallizers 44
Lining of filters made of reinforced concrete 45
Lining of vane wheels of exhaunt, fans and small tarbines 46
Lining of gas conduits 47
Lining of pipes 47
Lining of wooden towers and their metallic ban6 49
Lining of electrofilters (selenium precipitation chambers 50
A base coating 51
Asbovinyl cement 54
VII. "DovInyl Section of the Corrosion Pme-ention Department 55
Card 4/5

Asbovinyl, and Its Utilization (Cant.) SOV/3170
with
VIII. Safety Techniques During Work/Eth"ol LacWr and Asbavinyl
Mixture, 61
Appendix 1. Instructions for Using Asbovinyl MIxtures an FettlAng 62
Appendix 2. Excerpts From MIKhM Regulatima Concerning the
.Procedure of Combined Coating or Metal Surface With
Polyisobutylene and Asbovinyl, Mixture 67
Appendix 3. Excerpts Frm VTU M1Q,-P 3109-53 Specifications for the
Asbovinyl, Lining Mixture 74
Bibliography 77
AVAILABLE: Library of Congress
Card 3/5 2-i7-6o

Vo 12 fl N,
LEVIT, LA.-,
Linirg, digester bollers with corner tiles. 3ur.pro=. 12 po.6:22-22-
Je
1.Friozerakiy tusellyuloz-,V-1 zavod (for Levit, 1!akaimov)
2,Mos'r--)vF4-iy iP3t1tUt IdAmicheakogo mashinoutroyeniya (fnr Vol'tman)
Gloodpulp in1uatry--BqiAp-.*nt and atippliou)

FABICKANT, Tamara Llvovna; VOLITMU,jollf Leonovich; KLINOV, I.Ta., red.;
ATZENSMAT, I.I., red.; -1AZULffAT1,__V&_Y_,__q ---- to- Fchn & re d
("Aabovinyll and its use in the chemical industry] Asbovinil i ego
primenenie v khimicheakoi promyshlennosti. Pod red. I.IA.Klinova.
Moskva, Goe.nauchno-takhn.izd-vo khim.lit-ry, 1958. 78 p. (Kor-
roziia v khimichookikh proizvodstvakh i sposoby zashchity, no.11)
(MIRA 12:3)
(Protective coatings) (corrosion-resisting materials)

USSR / Cultivated P.Iante. Cereal Cropa M-3
Abs Jour Ref Zhur - Biologlyal No 13) 1958, No- 58559
Author Kravchuk, L I.; Voij�LQxal-ka, 0. B.; Guft', G. A.;
Dubinina, 1: A6; C5-e)mv4-Iov-a-,-T-.-N.
Inst Chorkaek. Pedagogicai 34istitute
Title Preliminary Data on High Yielding listervaxieties of
Hybrids of Corn, Produced at the Agrobiological Station
of the Pedagogical Indtitute
Or1g Pub I Nauk, Zap. Cherkao'ke derzh. pod. in-tp 1957, 1-1, 301-311
Abstract No abstract given
Card 1/1

VOLITOV!iKITl Boris lovlevich (Volltovalkyi, B.1; MMTARMMO, 0., red.;
LTANKIN -V., teklui.~reid.
Eftifil: in good time the seven-year plan for aninal husbandry;
based on the practices of the party organization in Cherkassy
Province] Somyrichku v haluzi tvarynnytetva - dostrokovo;
s doevidu robory Cherknelkoi oblasnoi pnrtilnoi orgnnizatati.
llyiv. Dersh.vyd-vo polit.lit-ry URSR, 1960. 78 p.
(MIRA 13:5)
Is Sokretarl Chorkneekogo oblastnogo komitata Kommunistichookoy
partii Ukrainy (for Volltovskly).
(Stock and stockbreeding)
~~-5-2
E Rhiff-r0q, .59",

Czechoslovakia / Analytical Chemistry. E-2
Analysis of Inorganic Substances.
Abs Jour: Ref. Zhur - Khimiya, No. 2, 1958s 4331
Author : Voltr.. Toushek, Toushkova
Title : On the Chemistry of Ferrates. I, Note On the
Analysis of Ferrates
Orig Pub: Chem. zvesti, 1957, 11, No. lo 30-34
Abstract: The arsenite and gasometric methods for the
ferrates determination are described. Approxi-
mately 0,1 g of the material to be analysed
Is dissolved in 10 ml of an 0.2 N alkaline
solution of the arsenite. The resulting solu-
tion is acidified with a mixture of 30 ml
water and 15 ml. concentrated HCL, and made up
with water to 250 ml. To that, 10 ml. of the
Card 112

VOLTR. J,
Calculating capacity, efficiency and time in jigger dyeing. P. 310. (Textil,
Praha, Vol. 9, no. 10, Oct. 1954;
SO: Monthly list of East European Accessions (EEAL), Lo Vol 4, No. 6, June 1955, Uncl
mw

VOLTRI, L.; IAAMIAE, V.
Preliminary results of a embined test feeding of bacon hogs. p. 312.
GAZ, WODA I TECHNIKA SANITARNA. (StowarvyBzenie Naukowo-Techniczne
Inzynierow i Tochnikow Sanitarnych, Ogrzewnictvia i Gazownictwa)
Warszaura, Poland, Vol. 32, no. 6, June 1958.
Monthly list of East European Accession (EEAI) W, Vol. 9, no. 2, Feb 1960
Uncl.

VOLTRII L
If, and how much, should pasture be used for bacon hogs? P. 408
GAZ, WODA I TECIINM SA14ITARNA (Stowarzyszenie Nauk~lwo-Technicmie Inzynierow I
Technikow Sanitamych Orgrzewnictwa i Garownictwa) Warszawa., Poland
Vol.13, no.9, Sept. 1958
Monthly list of East Euronean Accessim (F1UI) LC, Vol.9, no.2, Feb.,1960
Uncl.

VOLTRT, L.; LAAMIUB, V.
%----------
Replacinp, skimmed milk by hay flour in the feed rations of bacon hogs. p. 21
SOTSILIKTLIK POLLMIJAIMUS. 1001JAIIIJAIMUS IMP-IISTEAMM.
Tallin, Hungary. No. 1, 1958
I
1",onthly List of East European Accessions (EEAI) W, Vol. 8, no. 11
November 1959.
Uncl.

,!OLTRI, L.; LAMff.',AF,, V.
Dry feed mixtures for use in automatic feeders. p. 65
SOTSILKTLTK POLLIMANDUS. POLLIR-IJANDUS MINISTEIII(IUM.
Tallin., Hungary. No. 1., 1958.
Monthly List of East European Accessions (ERAI) W, Vol. 8, no. 11
Ro7ember 1959.
Uncl.

VOLTRI., L.
Make the work of swine caretakers easier.
p. h72 (Sotsialistlik Pollumajardus. Vol* 12, no. 10, Oct. 1957. Tallinn, Estonia)
Monthly Index of East European Accessions (EEA1) LG. Vol. 7. n,--. 2,
February 1958

LAAN", Vambols Eduardovich [Loanm5o, V.X.], kand.sel'skokhoz.nauk:
.IVCLITRI, Leonikhard Yurlyevich [Voltrit L.J.1. nauchny7 sotrudaik;
KATSUM~-soN, r-ej.--,--AtA-O-:3ACaWO, L.Te., tekhn.red.
(Yottening meat-type swine; practices of Astonion collective
and state forms] Bekonnyi otkorm ovinei; iz opyia kolkhozov i
eovkhozov Istonskoi SSR. Moskva, Izd-vo "Zoanie," 1961. 30 P.
(Vuenoiuznoo obahchostvo po rasprostroneniiu politicheoklkh i
nauchnykh znanii. Sor.5, Sollskoe khosiaistvo, no.3).
(MIDU 14; 2)
(Xotonin-Swine-Fooding and foods)

VOL'TRI, L. Yu., Cand Agr Sci -- "Practical and hygienic
I
0
methods 0 feeding and maintalning young ~~-Under condi-
A,
tions of ESSR,11 Tartu, 1961. (Min of Agr ESSR. Estonian
Agr Acad) (KL, 8-61, 253)
354

k
. VOL, TS. M.
S~rnthetic powder Instead of lead-tin solders. Obm.tekh.
op.rt.na avt.transp. no.3:3-13 160- (MIRA 13--7)
(Solder and ooldering)

00
00
00
009

1 .
00
43
00
A. 1.

I qj~j

"
0
00 SK;V. F
A4 L
iw

M
7

,
j
Of per Ix OIL
hr
Son b 0 3
00140
00 J_
-Ar~
see. 11.41&V.
It I S.,O" .. 1 #4#" 441 amw oat SPAIN1011 i~.
I I F I f 1A I 1 8 fw 0 0 1 x is t a a I
u 5 AT 00 It" to co 64 1 a ; 9 c
-0 00 be goo 0
0::**:Oooooouoooooot***
AAASASAG 0 60606060safte
.00
'00
.00
go
'log
-00
coo
1. goo
00
goo
1200
see
see
00
logo

A ' "Pt"
"'Aft Lt
.
.A
F as
$Ili,. mwmcuimim minemom or (DOILM)WATOt 10 R24OVS
oskkovat IN (J. App'.
OXIGIS. trasilwAlkovo Al amd Volt
!;I -
oboe. ruse 1944 17# 242-2511 btiC.-a-51r. Ns 19451
oss
Is offtoted by cotthadic rsdwtion
3M dool7gonation
betwoon Ye altalrOdes. Using a nov rato of 3-2 L w hr.,
0#6 mis, par w& and 2.5 v., the consimption Is, 0.3kw hr.
Par a. and 130 g of ft per a.3*

GOO

slow w0P

ww

Ago 0
see

ZOO
ties
ttli*At#At CLAISWICATMIN

4.3
Slom #"SAW We*
-
u IL At 40 &C it it i Ot
Is ita a 'l 4A i i is AA L I W K

'
a 0 0 o 0 o 0 a o 0 o 0 0 a a 0 0 41
41 0 Is 0, 0 41 41 0 000 : 40
1
0- 000 0 0 0 0 0 0 9 0 0 0 0 0 9 0 0 0 41.41 0 0 0 0 0 A 0 41
0

VOLITSINGER, N.Ye.; SIKM, L.M.
ftmerical integration of shallow water equations for purposes
of forecasting Leningrad floods. Trudy GOIN no.7033-" 163.
(MMA 16M
(Differential equations)
(Imningrad-nood forecasting)

VOL'ISINGER) N.Ye.; L.&I)ZOVSKIY, N.A.; MA5KOVSKLY, H.V.
Numerical calculation of rises of sea level at Lenlngr&d. Tnudy
GOIN no.81314,-36 164. -u 0. 1,7

VOLITSKAYA, I.I. (Laningrad, prospokt M. GorIkogo, 65-2, kv.7-a)
Calculi of the bile duct. Vest. khir. 92 no.3t73-79 Mr 164.
(MIRA 17:12)
1. 1z fakul'tetskoy khirurgicheskoy kliniki (zav. - prof. P.N.
Napalkov) Leningradskogo sanitarno-gigiyonichoskogo meditsinskogo
instituta.

VOLTYANSKIY) V. 0.
"0 Vlokheniyakh Poliedrov v Evnlidovl Prostranstva"
Report submitted for Symposium on General Topology and its relations to
modern Analysis and Algebra, PrAgue, 1-8 Sep 61

7011'-'PrRrr!3KIY, D.; -H7M7Z
Fle!ctric Rallro2ds
Confer~mce Qnd v.-minar on no!w mSincering methods on o!lx,-c,.ric r4ilrold5.
cqektrich,!-.mtvo no. 9, 1952.
9. M"tMILY LIST 0-- RMSIPI ACCE~MOIIS, Library of Congrea3, DecTimber 1952. Uncl.

294b8
S/137/61/000/',10,8/026/037
A060/A101
AUTHORS: Volubuy ev, 1. V., Ryaguzova, S. A.
TITLE: Influence of hardening temperature upon the mechanical properties
of manganese steel containIng niobium
PERIODICAL: Referativnyy zhurnal, Metallurgiya, no. 8, 1961, 7, abstract 8!50,
("Tr. Khar1kovsk. politekhn. In-ta.", ig6o, 15, 111-114)
TEXT: An investigation was carried out on specimens of steel with tho
following composition (in 45r2 (4502) - C 0.5. Mn 1.93, Si 0.25, P 0-035,
S 0.035; 45r2E15 (45G2B15) C 0. 51, Mn 2.05, Si 0. 33, Nb 0. 15, P 0 .054, S u.0 14;
45MB30 (45G2B30) - C 0.46, Mn 2.o4, si o.47, Nb 0.30, P 0.049, j 0.009. Mn-steo_
complementarily alloyed with Nb has higher db and ds than steel without Nb.,
m -steel with Nb may be recommended as I ,000
Ihe hardening temperatures for Mn C,
since hardening from this temperature with subsequent high tempering yields '.he
best combination of strength and ductility. There are 5 referencen,
R. Humyartseva
[Abstracter's note: Cemplete translation]
Card 1/1

VOLUBUYXV, Po,,,,-
Yontnrtis )f tire derz:w of -i~)w3pol;r capitalism In Rissia. To", . ebm.
no.2:60-?o 7 158. (MIRA 11:3)
(Runsia-D-onomic conditione-History)
Mp

Lit. ~V;
2WMITW S&I-10CHURSY, I.M.; BONDARINKO, P.O.; IZMYLOV, V.G., inshaner;
DUTRUZU-0-M., redaktor; YUM4 X.. tekhnichniv redaktor.
CContinuous-sequence method in plastering work) Potokovo-rozchleno-
vanyi metod shtukaturnykh robit. Kylv, Dersh.vyd-vo takhn. lit-ry
UFSR, 1954. 61 p. (KLRA 8:2)
(Plastering)

VOLUBUIEVI, V. R.
"Soile-and Climate," a paper presented at the 6th International Soil Science
Congress,, Paris.. 28 Aug to 8 Sep 56
Library Branch

j; W;;;;;;
00; 1 1 1 a s I I a 0 0 is Q u I III n All P do :all uu Idlau
#'A A-L-A-4- A..ALIA.LL I ~ M. 14 CC to U 4 0, 1, 6 il P, I a4 l w 0 vA.. s
vAmbwk &Wawaoom so "M in Dim" "aftie",
00, 4611 "d
WMNWAWW,.
M."ita= a, "Pow. 6m. 41, d I 1 ;-66
tItfstw (he pt. of W), -
lead k fletod" With
N&AA wo umd with pood rcomills In thir deem. of NO# in
the ribmak. SO. w" srpd. by ImAon of the amPho
wibxxoHQr'N*#c()~--
:0 j
Soo
J1
woo
'60
doe
kit
on2s, id r loscol, "it ON 0list 7 0,;
u so &1 4 if 4-3
IV a V a IV a a[ it it it a if ill w A
0 0 0 0
00 0 00,10000 so 0 0 0 0 0 a 0

m )V'm it u u 1. a b .1 0 11 .1 .1 -rw

uspij dOtteirmw.1i'm 4.1 alu"Jin"m in OrIAT
1huI,4'vAkA%ps and M. 1. V.4,11pCIA,
d:dj'-J#k.))q 1AN

Me$- I!Ok 11.414 1, CIA
it It;! x ~.,f X., of 1,
C%I. lilt 1,101 V11116 IMA14.1 kild litl Ott 11" 1111f,str .1114

All

00 1: -.go
00.1c
o
e"' '00
doe
0,1 '00
no*
'
K66

Obt. %-"' It

A fsJ 1 1 W tri An 6 ad 0

6
4X1
a 0 o 0 0 0 o 0 0

W~o 09* *0 *9 0
03 1 1 1 a 1 4 0 6 1 a 11 11 1$ N n It 1, -4 W a 1, a a is a so V a 30 Is V U U 34
A I r L -a.-A-A.-J~ a, -A - f 4 1 1 t - It - t1la A& W. - I A- k - A -- 9- - . t--t,-JL-L--V
Of A "Of4l At. 4#2f$1
Rim. 24g2l) Apfd 30, lal CAGA
emov are heid topther Ily means of aa of a condem ~~uct of um and aide
In sk. The ak it removed before prraWns by drying ki a trolp. of about 102'. -00
c1 1'. A. M. "W)
00 .00
0
IN #00
00 J,
00
000
sov lij Ilse
40
fee
00
too
ties
we*
5 U a AW 4 a 0 6 1 IN be 9 a a .2 a v
U a Aw IV 1,
5
so 0 0 0 0 0 IV 0 0 0 0 Is 0 0 6 0 0 0 0 0 0 a 0 0 0 4
0 *is 0 * 0 0 0 0 0 0 4 6 0 0 0 0 0 0 0 0 0 a 4 0 0 0 0 a 0 a 0 0 0

11 ti is of i
s a
I
1 I,
"
1 N a it At a is 5
to 4 a of a x v

I t
L a I v
P
L1
-4 0 4,
O
I A I A. AA u (A a A I I a A p
1
0 a I ,
~,* *
. -Its)
.*.Rok 4 A.& 0
001-efittl

.60

00 a ;-09

00 a aft held tarilber by a candmatim prodoct of phaak mby*Me mW *"jW which
is in paw4tir lom on the heated gbn mfem, -0
-00
.00

zoo
CIS 0
-oo

Z-00
so 01 go*
FLO 400
lip" I

too
9
0 Af..JLA *C?AtLL#'CKAL CITCRATL&C CLAISOOCA14" too

l
b U 11 AV 10 it 6 411111,34-

3t
t
a
50 tvivillpal flows p
turflf:
0 0 0 0 0 0 0 9 0 0 C 0 6 0 ,
o
W4
* 0 0:0 0

;6`0909600666069 0 0 * 0 0,
9 0 0
* a 0
1% ux 1041 41428) al *

At 0 PO I I T I cy A; 11 nuld 2
~SICKSran

*
8 71 f ~, -1.
I
ST
Gto.p$
lot t. C.0
.
,
0
Z.

* "64111 lve 9 1 S v "oil
ic
.

0 Ot

sew
:
or

OOF
66
Sty 10 go
00
so,

1~" IM;00 a4l r- IILUWA-A a4l XUP"P PNWJI&

00- If 'q4-,4 qJ141 J-10414idtaf I"- aqj tq Ina pAWso Wwls Ipuy jqj jpqm 1104Apm
3
JD 3f#4
W
A
wn uv iq Ino p4uw " ucowmip- ju Aftp jug mU J)
00
00- !
q
4
M
I
lAlulp"atr Al .1c
-
-
s '
W
- A
1CM ulf P4"*s
10'Al ""?I "'Im"'W"N
PAMN
F
S
00
00
'
I
t
T
1-01
o
I" it
,
,
g N of tT n
1( fl
0 0 0 0 g 00
0
0

A,
A At
I - I . 4
0 41
go
00 ft Of f"Wdod. N. 1. V111111inkin.
OrMU'llm)(It
Chise. (U. S. S. R.) 9. M&"
1110411 The im7=v I in the wasad proordive for the pro-
use of a INIMPI funting
00 int"I 11) me: the
11,914 In OW WAIIIXMtiOn Of CJ14. I'Milting in 101% xv-
40 CJt.19(hll)t (0). The simplification of the eonvws&M
00 of U into the Nit salt, the redurtiost of N*011 amt. in
the alk. fusion of ff. the aulsitituOin of Hiso-CJ14 for
0 Ft#O In the 4,zta* of 1, owl the Crysta. of vatimin-distd.
016 W f tI frons PbMe with little H40. givittic while I OPM& I
00 by the U. S. 5. R. phanniscoptia. C.114 is sullonalrd
1 with 2040% fuming 11.5% at M-2mil, depending on
tion
the etretwh c4 the fuming 11,50t tord. The resic
inatia is fired from HtKh with Ca(OH), in H.0; the
filtrate. after fteutralisifig with N*,Cth or XS011, is
Pd. to dryum iv v"m. and the U Is drird at 1010' and
a"
powdered. Yqually S,wd Iritids am obtained by fusing
sols. of N&OH inotead of id mots. With the -
11 with 7 a
use C4 a suit" sti"ri this ratio affair be fvdore4 to 5
t a ~ 1, a T-i-~
Insist. NAKM W% fire") 10 1 "1 NO"11 is
broad tlarldmily In (A Ve Pat at 311f Df*, The 141
thhd pw of U is Initudurra alf-ly and the laWbrV
rtipj*, Toward the end of the rtar6m t1w
raisidt*319-20". a
I cf. at the indt to a defialte Conva.. followed Ily I he w1do.
of 11) Lv. of 0.5% 1-dia:o-2-naphihni-fl-suffam: wW and .
The matipariss-in a( the offln, with the premlinur (to and
a statulard 4oln. similarly prvpd. The melt if, dimOrd
in 11#0 with the odilts. a( JICI to aft swid reartkon vo-l I,
extd. with a mixt. of Miff) and C4114 (b. fift-Mi, I is
freed from PhOll by vermini disin. In a Pperial app. All
tomoectmg pipes. Wslvr4 WW the 2 rnvivm we AN.-
irk-any heated at 111) 2r. The Crysta. of I is &~ted
with As definite Pe wtion of PhYde wrived with 1f,0.
Chas. 81,Dc
7
-so
of
.00
Zoo
to 0
I
L40
000
,is**
zoo
0111ALLUNGICAL LITIOST649 CLASWOCAIC*
9 Z-
a saw 41v,#1jva7-,77:
sanoss, .1 #DIV.
S&144" Wit ONV Gilt
U 0 -4 f 4 1 1 -ii ii i ;1,
; a A I An I -U a 0 a 3 If
so
&;treat Itasca Ice
an Uji i
0 0 0 0 0 0

Vaulc~rjiu.
Retrospecti-te view on the revision of stiinditrds for annlyzing methods of
solid fuel. P. 132.
(Standardizarea, Vol. 9, No. 3, Yar. 1957, ]Xcuresti, Rumitnia)
SO: Monthly List of Fast Nuropean Accessions (121.1,) Le. Vol. 6, No. 8, Aug 1957. Uncl.

VOLMITIARU, A; ORN31.7111i N.
The standardization o'. tenoi-o-active oroducts.
P. 560 fk3TA;'!J--)A*,':)D7A7Tt'A) -111,rania) Vol. no. 11, :o,,,.
50: ',-~Onthl- inrlex o.," Fn3t '7uropean ;~ccessiom ("-7A!) L,- Vol. 7. 7,0.

r1u.
.... ............
- - - - - - - - - - - - - - - - -

RVIANI!, / Chomical Tochnology. Fats, oils, viaxos, soaps., H-25
dotorgonts, substanoos, flotoroagont
Abs Jour iRof, Zhur-Khimiya, No 12, 1958, 41175
Author iVoluntaru, Ornshtoyn.
Inst ?Not givon.
Titlo tStandardization of surfaoo aotivo agonts
Orig Pub iStandardizaroa, 1967, 9, No 11, 560-562.
Abstract iIn roviowing tho oxiating standards and norms of surfaco
aotivo agonts with tho purposo to oliminato tho imporfootions
of tho systom, it hau boon rooommondod that tho aurfaoo aotivo
agonts bo dividod into groups and sub-groupe aooording to
thoir ohomioal composition. Appropriato nomonalaturo should
bo omployod.
Card 1/1

U SSR /Medicine Toxicoinfection FD-3313
Card 1/1 Pub 148-9/24
Author Voluolko, DO F,
Title : A study of food toxicoses and toxicoinfections and their pre vention
(Author's Abstract)
Periodical : Zhur. mikro. epid. i immun. io, 46, Oct 1955
Abstract : Two instances of food toxicoses from contaminated beef and one from
preserved fish are discussed. Proper handling of foodstuffs is rec-
ommended as a means of preventing food toxicoses. No references are
cited.
Institution : Mogilevskaya Oblast Sanitary-Epidemiological Station (Read Physician-
A. NO Bakalov)
Submitted : March 29, 1955
VOLUSIKO, DOF".
Portable alsotrical thermostat and Its us* under rural conditions,
Zhuromikroblol.epid. I Immun, 29 n0-71122-126 J1158 (MIRA lls8)
11 ZZ Mogileyokor oblastnoy sanitarno-epidemiologicheakoy stantaii.
(MIGROBIOLDGY, war. A inat, en a.
portnble electric thermoatnt for microbiol. inventigntion
in rural condo (Bus))

VOLUISKAlAs E. N. ,
"Spectrophotometry of biuret complexes as a method for investigations of proteins and
peptidea. Part 16. ComrArative actitity of copper, nickel,, and cobalt during the
formation of the biuret complex of tripeptide (glygyl),tt Plekhan, M. I.,
Voluiskaia. E. N. (p. 343)
SO: joloal of General (;hemistrT (Zhurnal Obshchei Mimii) 1953., Volume No. 23, No.2.

CAUGORY : Chemical TechnninsFy. C~-emical Products and Their
Annlications. Pes-ticides.
ADS. JOUR. : =mum.; 110 1,')p lq~-)q,, 110. 6F3937
AUT,qCF l,anc--,n., Voliivniv-,c. M.

OUG. WB. : cerel,arll ActR. UPRI, Vil. CI
9, --vo 1-4 , T7 1-1 -1 G,
ABSTRACT : l7fzitont of the -0--yolv isnof-r 'Inyslox" in 11,
i.ecliviev" tyrade !rn,ltirl, iF. determinvO !,v, odn-

lyerolvri!7 c,..^ - ' -(- , 5*r-r
ri c -C kj j oj E. -1. ,- r t 17 p r

1 5(3) A. Granov
Card:

RUMANIA/Analytic Chemistry - Analysis if Inorganic E-2
Substances.
Abs Jour Ref Zhur - Khimiya,, No 14, 1958, 46413
dithizone (chloroform solution) - color from green
into stable light gray, which corresponds to the start
of the formation of the chelate of Bi.with dithizone
after the quantitative precipitation of BiPO
The titration method of PO 3- with Bi(NO3), ~s-.similar
in general with the titraln method of
PO4-1- by (CH 3C00)2 Pb solution descktbed in the report
I (RZhKhim, 1958, 43051-)
Card 2/2
fi1-5--"~N'~~-"17'T tP MR't Hm-
'~n
--5

VOLUSIMC., It.; V.-APICEA, M.
Contributions to the study of Systox. p. 171.
Academia Pepublicii. Poulare Rcminc. F-1.1in-la Cluj.
1.ontb.ly Tot of East ",,rorem '-cc.,3:Acns (MXi Vol
Uncl.
"I CE."
no. 7, Jaly 1959.
twl

VANCEA, Marin; VOLUSNIUC, Maria
Rapid gravimetric determination of bismuth an bismuth =,alate. Studii
cerc chimie Cluj 10 no.2.*283-286 159. (EUI 9.9)
1. Academia R.P.R. - Filiala Cluj, Instiutul do chimie.
(Rismuth oxalate) (Bismuth) (Oxalic acid)
(Nitric acid)
--n-, I!n f !r-'r

VOLUSNIUC, V.;VANCEA, V1.
A rapid gravimetric method of determining lead as lead phosphate. p. 155.
Academia RerAiblicii Populare Romine. Filiala Cluj. Sr(IDII St CERCETARI DE
CHIMIE. Cluj, Rumania. Vol. 9, no. IA, Jan./boo, 1958.
Monthly List of East European Accessions (EEAI) Vol. 8, no. 7, July 1959.
Uncl.

IMANIII/Analytical Chemistry. Analysis of Inorganic
Substances., E-2
Abs Jour; ]Ref Zhur-Khim., No 13, 1958, 43051-
Author Vancea Marin, Volusniuc Maria.
Inst Rumanian AcaderI__________
Title Direct Titrimetric Determination of Phosphates. I.
Orig Pub: Studii si cercetari chim. Acad. RPR Fil. Cluj, 1957,
8, No 1-2, 85-88.
Abstract: PH is titrated with a solutioi, of Fb(CHjCOO)k at
PH 2-3 in the presence of,dithizone as an indica-
tor for Pb)+. 0.05 - 0,1 C; of the phosphate being
analyzed are dissolved in 10 ml of water, there are
added 2-3 ml of buffer solution (6 ml glacial m3com
+ 13.6 g CHjCOCNa in 1 liter of solution), 1 mi Zif
freshly prepared chloroform solution of dithizone
Card 1/2
10
E-2
Substances.
Abs Jour: Ref Zhur-Mim.) No 13, 1958, 43051-
(0-03 g in 100 Ml), and titration io carried out
with 0-05 u solution of (CHJCoo) Fb to the first
change in color of the solution ~roa green to
violet. Determination error does not exceed 0-5~-
The rethod is suitable for series analyses of phos-
phate fertilizers.

C 0 UN T'R RlAm an i a L-2
C AT,!, G G' R, -1 An-IlYtic7,1 Chamietry.
AE"). JOUR. RZY%.him., WO. 7, 1959. ll'o 230;~O
-ic)? ncea p R. ; vollus.-Illic M.
Rlmmnlan Acl.,7-.(--,L-y
T I (ILL T, AmilysIs of Superphosphates. III. "'trimtrIc
Dete rm inaCl ion of ilhosphorus Availatle to
Flar.'.s A~.:cording to the Reaction cf
1 G ?Ucl. Stud~l si cercetarl chiff,. Acad. Fil.
clu~~ 81 ~10 3-41 al-264: 2(5-268
I f
TIJ d-temination )f F *n 5,dperphos#-Ab~
ABSTRACT
use -4-c made of the mell'"'nod previou:3iy nevelcped cy the
aut'llors) which is ba5e~`. on titra". on of POUS+ w.',.-,.h a sol:'Itia-i
of Pb(CI13C(-'2)2 irl a-Ce'- 4C Et C i'~ U'le 7'
--iium usL-Iz. d4l-hzone as a
L rl
indicator (RZhKhim, 1430551). The Jons which
n~erfere with th h
l
U -1 -e titratiori are first prcl-1pitated, wit- a
Solution of Ba(1103)2, Excess Ba'e'+, JL ar. acetic acid mediurm,l
is not precipltat.ed by PO,,3- ions arx" conseqaently does tict
interfere with determination of P. 10-20 m! mixed aqueous
and acetic acid extract of sil-erphosphate (prece rL a Ib-
Y Cl'
ntact are added 5 ml acetate 6uf fer so'ut-I ron (0.1 ~ CH Cc-
solution Bak
N
01' + 0 -1 Cf3COONa, 1:1), 3 ml saturated
CA.U: IA
F *of Lead Phosphate in the Presence of Dithizone as I
T IT LIE
~U
orm S .on of di-
lv~' cy'lorof ut
'Ution of
NCT 4nd I ml O.C- s o- J.
--ed with 0-0
AB'QTFL
thl,,.zcne
Pb (Clilc 02
CARD: 2/1+
iate presence of
Formation of .9isTru, phospi in thr
Dithizone as -TridicatGro 17-.2 ef -- --~j

-7
COUNTRY : Rum an i a F-2
CA I Zrr 0 RY : Jknftlytif- Cha;f .1
j, try,
A13.3. JOUR. : A L,"n"Az.., -0. 7,
AUTHOR
i 111:,, 1) T I
T IT LS.
0 R Ir.'T .PUB. :
AB3TRAC'T : solut-ion changes to a light gray. TiLer of the
Bt(N03).3 solation t.5 detcradlnL-d with chumically pure
iU12PG1, urdcr analogous conditions. Coirziunication 11 see
RZhIv.him, 4(4.13. B. Ya,%ole.
11-A
RUMANIA/Analytical Chemistry. Analysis of Inorgnnic
' Substances. E-2
jibs Jour: Ref Zhur-Mim-, No 13, 1956, 43052.
Author : Vancea Marin, sniuc Maria.
Inst : Rumanian Academy.
Title : Gmvir-etric Method of reterrdnation of Phosphate-
Ion as Leas Phosphate.
Orig Pub: Studii si cercetari chin. Acad. RPR Fil. Cluj,
1957, 8, No 1-2, 93-96.
Abstract: Dencripticn of a nethcd based an precipitation of
P043- in the forn of Pb3(P00A at pH 2.3. In
determininG P0,f3_, 0.05-0.1 g of the taonophosyhate
being analyzed are dissolved in 20 n1 water, 1-2 al
of a buffer solution (6 a concentrated C11JCC011 +
13.6 g CHjC00Na per liter) are added, the mixture
Card 1/2

RMAIIIA/Analytical Chenistry. jIndlysis of InorGanic
Substances. E-2
fibs Jaur: Ref Zhur-Khim., No 13, 1958, 43052.
is heated to boiling, and hot 0.05 11 Pb(CHICOO)z
is added, dropwise with continuous stirririf,, until
copplete precipitation has occured, after which
the precipitate is allowed to settle to the bottom
of the beaker on a water bath. The precipitate
is filtered off, washed with 0.3cp' solution of
C4SCOCH, dried, calcined at 600-7000 and weighed
as Fb'4 (Fo~),Z.' The described method yields re-
sults'that are copparable with those of the pyro-
phosphate or of the phoophoro-nolybden= Liethod3
and is suitable for deterTaination of available
PA~~ in natural phosphates and in superphosphates.
Card 2/2

RU1-W1lA/Analy+,ical Chemistry Analysis of Inorganic E-2
Substances.
Abs Jour Ref Zhur - Khimiya, No 8, 1958, 24829
Author Vancea., M., Liteanu) C,y Voluenius) M.
.Inst Rumanian Academy.
Title New Rapid Method of Gravimetric Determination of Fhosphate
Ion,
Orig Pub Studii si corcetari chim. Acad. RPR Fil. Cluj, 1956.- 7.,
No 1-4, 101-110
Abstract POj3-is determined by pre cipitation in the form of BiPO,,L
in nitric acid solution at p1l M-o-7-- Ca~-+, Fe -S 4and
A134 do not interfere with the determination. 0.1-0.2 g
KH.i.PO,tare dissolved in 50 ml water, heated to boiling,
0,5 ml of 03% M10; are added) and then, dropwise and
with stirring, a solution of Bi(NO?)j containing
Card 1/2
/7

VOLIVOVSUY, I.S.-O ISHUTIN, V.V.
Results of the regional seismic studies In the central Kara-Xtm.
Trudy VNIGNI no-35tl62-166 161. (MRA 160)
(Kara Kum-Seismic prospecting)

VOLIVGVSKIY, B.S..j VOLIVOVSKIY, I.S.
Seismic investigations along the regional base profile Amu Darya
(Karabekaul) - Nura-Tau (Noytash). Izv.AN Turk,SSR.Ser.fiz,-tekh.,
khimei geol.nauk no.3:28-32 161. (RDU 14:7)
1. Otdel razvedochnoy geofiziki i seysmologii pri Prezidiums AN
TurkmenBkoy SSR.
(Uzbekistan-Seismic prospecting)

VOLIVOVSKIY, B.S.; VOLIVOVSKIY, I.S.; TALI-VIRSKIY, B.B.
UnIng seismic methods in prospecting for oil and Ms deposits In the
Fergana Valley. Gool. nefti I gaza 4 no.1:18-25 A 160.
(MIRA 13:10)
1. Uzbekneftegeofinika.
(Yergana-Seismic prospecting)

GODIN, Yu.N., akademik; VOLIVOVSKIY B.S.; VOLIVOVSKIY, I.S.
Seismic investigations of the earthls crust In the -lak-hiLra region
of the Uzbek SSR. Dokl. AN SSSR 134 no-5:1069-1072 0 l6o.
(MIRA 13:10)
1. VsosoyuzW nauchno-iseledovatellskiy geofizichookikh metodov
razvedki, 2. AN Turkmenskov SSR (for Godin)s
(Bukhara--Seismic waves)
m f*

GODIN, ru.N., akademik; VOLITOVSKIT, B.S.; VOLIVOVSKIT, I.S.
Seismic investigation of the earth's crast in the region
of the Fergana lntermontane trough., Doid.AK WAR 133
no.6:1398-1401 Ag l6o. OCLRA 13:8)
1. Usbekskiy geofizicheakiy treat i Vaef,ayusnyy naucbno-
iseledovateltakiy iastitut geofisicheskikh matodov resvedkie
2. Akademiya nauk Tarbmenslcoy SSR (for Godin).
(Fergana-Seismometry)

VOLIVOVsKry, B.S., vm1yovsKry, r.s.; TILI-VIRSKrY, B.B.
Conditions for seismic prospecting in the Fergana Valley.
Razved. i. prom. geofit. no. 35:73-77 l6o. (NEU 13:12)
(Fergana--Seismic prospecting)

VOLIVOVSKIT, B.S.; VOLIVOVSKTY..I.S.; RYABOY,.V.Z.
laboratory use of the controlled directional sensitiTity netbod
in Interpreting the materials of deep seismic soundings. Razved.
I prom, geofis. no-36:8-13 160. WU 13:12)
(Seismic prospecting)

VOLIVOVSXIY,~.S,: VOLIVOVSKIY, I.S.; ISHUTINO V.V.; SEMENOVICH, V.V.;
~TALII-4ff~kIY, CHAM), S.S.
Regional geophysical studies in central Asia and their further trends.
Sov.geol. 6 no.12:112-117 D 163. (MIRA 16-U)
1, Nauchno-issledovatellskayn sredneaziatskaya geofizicheskaya,
ekspeditsiya kontory "Spetageofizika" i Uzbekskiy goofizichenkiy
trest.
A "b",
e 0 -1

ACC NRI jj~6j6367
AUTHOR: Vol 1vovsk Vollyovskiy, 1. S.; Tall-Virokiy, B. B.; Ghraybman,
Az~
ORG: none
TITLE: Structure of the Earth's crust and upper mantle of the main geostructural
zones of western Soviet Central Asia
SOURCE: International 6ological Congress. 22d, New Delhi, 196h. GeologichecMye
rezulttaty prikladnoy geofiziki (Geological reaultu of applied geophynica); doklady
sovetskikh geologov, problema 2. Moscow,, Izd-vo Nedra, 1965, 26-32
TOPIC TAGS: seismology, Earth crust, gravity anomaly, bftsernent,
meganticline megasyncline, upper mantley MOoYooeoviCIC DIwYCowriAlW7~V / 4x)e57FeA)
Sov,e.-r (_'eA.-reqj_ &sio
ABSTRACT: Three different zones diitinguis~ed in western Soviet Central Asia are
as follows: an area of recent contrasting movements of Tien Shan, th-~ Epiliercynian
platform and the Kopet-Dag foredeep. These zones include major structural f-mtures
of the first order, such as arches and depressions in the platform mid
and magasynclines in Tien Shan.. The data obtained from deep sciamic and
seismological observations made it possible to estimate the crustal thic?newj of
western Soviet Cxntral Asia and to diacover certain regularitlen In varf(AlOn Cf the
crustal thicknesa. In general, the data nuggest that, in the orogenic nren of
Tien Shan, the crust' is much thicker than within -the platform. In addition, Tien Shar
souRcE coDE:-tjR/oooo/65/000/000/0026/0032
Cord

AC~'i~R_,AT66ib~!
is characterized try higher gradients of crustal thickness variations -aid ~,!,-neral
geomorphic contrasts of the Koho discontinuity. Both In Tien f3han and wit,hin the
platform, uplifted zones (positive structural featues) are characterized b- s er
y M11
crustal thicknesses, and zones of depressions, by large thicknesses, The I'Soho
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 interpretation is complicated by the fact that gravity
anomalies reflect the total effect of many factors, the most iLTortant of which are
relief and petrographic nonuniformity of the basement, variations of the thickness
of the crust and its layers and, finally, inhomogeneity of subcruntal material.
Within Tien Shan and the Turaniam platforni, local variations of the residual anomalie
correspond to major structural featues of the first order, suggesting the presence
of local inhomogeneouB types of suberustal masses in each- of these area. Orig. art.
has; 3 figures.
_8tM_'_CODE':- 08/ SMM DATE: 06jan65/. mia REF: olo
Cc-rd 2/?

:C NRI AR6009029 SOURCE CWE: UR/0169/65/000/010/GO03/GO03
AUVIOR: Vollvovskiy, B.S.1 Vol*vovskiyp 1. S,; Tall-Virskiy, B,B I ~ra bqM,,--Y,-jv
ORG: None
.TITLE: The structure of earth crusiland the top mantle of the basic geostructural
zones of CentralAsia
SOURCE: Ref. zh. Geofizika, Abs. 10G13
REP SOURCEi Sb. Geol. resu 11taty priki. geofiz. Geofiz. issled. stroyeniya zemn. kory,
M., Nedra, 1965, 26-32
TOPIC TAGS: ea th crust, earth crust structure. seismology /central Asia Iolloob ab _P
Uu= Turan I CUB&, Tyan'-Shan'
ADSTRACTt In the present geological structure of CentralAsia, there are regions rela-
ted to the three basic geotectonic categories of continents, the Turanian epi-Horcyni
platform, the alpine folds region of Kopet-Da-, and the orogenic region of Tyan'-Shan',
The relation between surface relief of thefolded foundation, the thickness of the earts
crust, and the relative density changes of the surfnce manfle of these regions Is dis-
cussed. Seismological data Indicate a correlation between the geotectonic state, the
earth structure, and the character of the density 7!tanges of the subcrustal 1"asses,
To the Tyang-Shan' orogenic region (relative to the Turanian platform) corresponds an
increase:in the crust thickness and a relatively smaller density of subcrustal masses.
Ccwd 1/2 UDC 550.311051*14

ACC M4 AR6009029
C
Besides, Increased gradients of the earth crust thj'cness and a high contrast relief of
the Kohorovicic . surface characterize the Tyan'-Slian', The Turanian platform and the
Tyan'-Shan' are also substantially different in their gravitational characteristics,
The gravitational anomaly decreases at the transition from the Turanian platforis to. th t
Tyan* -Shan'. [Translation] .
SM OWES 08/
Ccwd 2/2

ACC NR. AL17010085 SOURCE CODE: UR/0215/66/000/012/0118/0123
AUTHOR: Rikhtor, V. G.; Vollvov~kly, 1. S.
ONZC: VNII Goof Izilta
TITLE: Neotectonics as an index of anomalous crustal thicknesses
SOURCE: Sovetskaya goologiya, no. 12, 1966, 118-123
TOPIC TAGS: tectonics, upper mantle, lower mantle
S U3 CODE: 08
ABSTRACT: R. It. -Domenitskaya has. demonstrated that the elevations of the
earth's surface are in close functional dependence on the thicitness of the
earth's crust. I-Satinematically this relatiorx-hip is expressed by the formula
1.1 - 33th(O.3811-0.18)+38,
whoro M Is the crustal thickness at a particular pointv It Is the elevation
of the carthts surface above sea level, in km. However, It 6as been shown
that many spacial curves Intersect the generalized R. M. Damenitukaya curve
or run parallel to It. In this roflnomnt of that author's work, the
authors consider points not falling on this generalized curve (c1mrActeriting
Isostatic equilibrium of the crust) to be anomalousp and seek to interpret
Card 1/2 UDC: 551.241
4-7e2A /J -5

ACC NR: AP7010685
thoir pattern. Howovor, Instead of using heights of relief, as In earlier
studios, the authors now use the wiplitudar, of tho most recent toc,:onic rxwo-
nonts. The analysis of thicknesses of the crust and the amplitudes ef those
recent vertical tectonic movements, Illustrated in this paper, roveaiad a
close dependence between the latter and anomalous deviations In crustal
thicknoso. It in concluded that deviations from the R. M. Demenitskaya curve
In any diroction charactoriza ragions of rocant uplifto or downwarp)-ignp
regardless of their gonetic nature. OrIg. art, hass 3 figures and 3 for-
mulas. rj"PRS: 40v299
Card- 212

AMURSHY, (%T.; V9i1[,1YE'V, V.G.; L.S.; GARFTSKJY, R.G.;
6Ai,1R1E'LYA1!TSv G.A.
Basic tectonic elements in the western part of Central Asia.
rieftegaz. geol. I geofiz. no.4:7-10 165. (MIRA 18;7)
1. Upravlenlye geologii i okhrany nedr pri Sovete Hinistrov
Turkmenskoy SSR; Vaesoyuznyy nauchno-insledovatollskly Inntitut
pr1rodnogo gaza; IOU AN SSSR i Nauchno-lasledovatellskaya
Sredne-Aziatskaya geofizichaskaya ekapeditsiya, kontora
Spetsgeofizika.

VOLIVOVSKIY, I.S.; RYABOY, T.Z.; SHRAYBMAN, V.I.
Subsurface geology of the Fergana Valley accordi to
geophysical data. Sov-9001. 5 no.l:1.5&-160 Ja JMIR& 15:2)
1. Vaesoyuznyy nauchno-issledovateltakiy institut, geofizicheskikh
metodcv razvedki.
(Pergaha-Goology)

ACCESSION m: ARW36339 S/0169/64/000/003/=4/GW4
'SOURCE:
Aeferativny*y zhurnal, Geofizika.. Abe, 3019
AUTHOR: Vollvovskiy) I..S.; Vollvovskiy) Be Be
TITLE: Characteristics of the structure of the 'earth's crust in the western
part of Soviet Central Asia (on the basis of data from integrated geophysical
investigations)
CITED SOURCE: Sb. Tezisy,.* dokl'. Bovesbcbaniya po probl. tektoniki. M.j. AN SSSR4
1962, 147-149
TOPIC TAGS: geology, geophysics, geophysical exploration, earth's crust,
Mohorovicic discontinuity, seismology, crustal structure; deep seismic sounding
gravimetry
TRANSLATION: On the basis of the structure of the earth's crust in Central
Asia it is possible to define two zones: a western.zone with relatively eiml
)le
structure and an eastern zone which has a considerably more complex structure,
In the eastern zone there is a deep dawnwarying of the Mohorovicia discontinuity
',Card

ACCESSION NR: ARW36339
I in the Fergana depression, a decrease,in crustal thickness in the bordering
ranges and a plunging of the surface of the suberustal layer toward the Pamir-
Alay system. Individual uplifts are noted in the western zone against a back-
I ground of smooth plunging of the Moborovicic discontinuity in a southward di-
rection. On the whole, within the Kopet-Dog and Pamir-Alay system there is an
inverse relationship between the surface relief and the surface of the subcrustal
layer, whereas in the mountain structures.of the zone of renewed folding (Kura-
tinskly, Ferganskiy, Turkestanskiy and Kuraminskiy Ranges) there to a direct re
lationsbip between the two forms of relief. Within the limito of a platform
uplifted sectors of the crust correspond to on arching uplift of the surface of
the folded basement, that is, the thickness of the crystalline crust remains
approximately constant. In geologically uniform regions the earth's crust in
the process of tectonic development apparently does not experience special ad-
justments; the cause of movements is pbysicochemical processes in the suberustal
matter. A comparison of deep seismic sounding and gravimetric data makes it
possible to detect those relationships between density differentiation of the
jj;q,d 2/3

ACCESSION NR: AR4036339
suberustal matter and tectonic movements in the crust vhich vill serve as
confirmation of the hypothesis of phase transitioi2a of subcrustal mattere
I. G~lkin
SUB COIX: AS ENCL: 00
DATE ACQ: 17Apr64
I.Card.

ACCESSION Nit: AP402,3372 S/0049/6h/000/002/0184/0195
AUTHORS t Alekseyevs A. So; V J-._4., Yermilovap N. I.; Kraukliss P. V.&
Ryaboy,, Ve Ze
TITLEt The physical nature of some waves recorded during deep seismic sounding&
Comparison of theoretical amputations with experimental data- 3
SOURCE-.' AN SSSR. Izv. PSeriy% geofizicheskaya, no. 2, 1964, 184-195
!TOPIC TAGS: seismic wavex deep seismic sounding, head waves refracted wavej
fretlectod wave., suporcriticalwave,. "granite" layer, "basaltic" layerj wave groups
'Mohorovicic discontinuity
JABSTRACT: The authors have used theoretical computations and experimental data
from Vio earlier papers (K voprosu o prirode voln, registrirayemy*kh pri GSZ.. II.
Teoreticheskiy analiz nekotory*kh modeley zemnoy kory*j Izv. AN SSSR, ser. geofiz.,,
!No. 1, 1964; K voprosu a prirode volnj registriruyemy*kh pri GBZ L KharaktarisUka
leksperimentaliny*kh danny*kh. Tiv. AN SSSRp'ser. geofiz.9 No. 11, 1963). They-
0
th~ 'first waves of the F group-are head or weakly refractedwaves
conclude that
h
3
Card

:ACCESSION NR: AP4023372
1corresponding to the upper P*) is A!
part of the "granitic" layer. The wave group T(
lex wive formation. The first wave of the group consists of a head (weakly
icomp
refracted) P* wave (up to a distance of 120-130 km from the shot point) and a super-
h
critical reflected wave from the.surface of the "granite" layer (PO or
refl
!"basaltic" layer (P* )i depending on the relative thickness and velocity of the
refl
!,~,.licrustal layers. The P nd P waves are the Bupercritical reflected and head
1, 1 rerl , h
~!(weakly refracted) waveso respectivelyj corresponding to the suberustal boundary
!(Mohorovicio discontinuity).,/The nature of the P, wave group is not uniquely
detomined.' It may represent a complex group of waves consisting of supercritical
-reflected and head waves formed at a discontinuity below the Hohorovicic disconn- i
,:nuity or refracted in the subcrustal layer (if it is assumed that velocity-
increases with depth in this layer)* The P group, which is apparently recorded in'
iother regio ', may become the source of very valuable information on the structure
ns
of the upper'part of the mantle, The principles of wave-group correlation in deep
seismic sounding may lead to a combination of waves of different physical nature'
into a single group. To:test~correlation it is necessary to make preliminary
,,C rd2

ACCESSION NR: AP4023372
detailed analysis of theoretical views concerning ampl tude and attenuation of
waves of different physical types, Orig, art. hast.; 8 figuroee
S R (Office of "Spetageofizikall MG
SOCIATIONt Kontora "Spetageofiaika" 140 1 ON SSS
A
land ON SSSR); Akademiya Nauk SSSR (Academy of Sciences SSSR); Leningradskoye
!Otdelc~hiya matematicheskogo ihstituta im. Steklova (Leningrad Department of the
Mathematical Institute)
ZUBMITTED: 26Mar63 DATE ACQ: 274r64 ENCL: 00,~
000
UB OODEs AS NO REF SOVS 013 OTHER
T,:
card 313

3/049/62/000/00e/002/003
1046/1246
AWHO113: 3010usov, V.G., Vol'vovskiy, B.S., Vollvovskiy, I.S. and Ryaboy, V.Z.
TITLE., Experimental investis-:ation 'of the regkotration of deep-Teflected
waves
(CRIDDI(OL, JU.Ud--.MiytL nauk SLZR. izvestiya. Seriya geofizicheskaya, n6. 8, 1962,
1034-1044
T---,IrL: A report on the deep seiunic eDunding with reflected (oubcritical) waves
carried out in 1960-10,61 in thn South-Nastern 'AueKmenia over a 120 km profile. The
noise waves were elirninated by uoint, directional reception: seiamorecoivers and sources
of st~;tic vibrationn were Crouped together (9 recAvers spaced evenly over a linear
distance of 400 m, anch group by 100 m from ito neighbors). Comparison of the
results with the d2ta obtained in 1f,50 in deep aeiamio sounding with reflected (hyper- 1z
critical) and leadinG waves sliown I:ood agreement in general features on the seismo-
ertmas, though subcritical r,-flection is better in detecting fine details. It is
Card 1/2

Experimental inventii;ation of the reeistration....
recom,rended to use al far as possible a combination of the two methods. There are
8 figures.
.jIJBI-,ITTt;D: ?ebruarf 26. 1962
AGIJOCIATION: Vsosoyuznyy aauchno-issledovatellskiy institut veofizichoskikh kl
metodov ra--vc&d (The All-Union Scientific Research Inatitute of
Geophysicul Nethoda of ProEpectine)
Card 2,12

VOLIVOVSKIYI B,S.; VOLIVOVSKIY, I.S.; RYABOY, V.Z.
Some data on seismic waves corresponding to the layer beneath the
crust. Prikl. geofiz. no-31:3-10 161. (MIRA 15:3)
(UzbekiSt2n-_Seismic prospecting) (Earth--Internal structure)