SCIENTIFIC ABSTRACT VESHEV, A.V. - VOSIN, S.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001859620011-8
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 1, 2001
• Sequence Number: 11
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

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VNSHRV, A.V.; TOKIN, A.F. I OCHEM, N.A.
.0000"""Obw
Use of ccabined electric profiling techniques in large-scale geological
mapping$. Vop.rud.geofiz. no.1*38-47 '57. (MIRA 10:10)
(Prospecting--Geophysical methods) (Geology--maps)

; /. IF
VESHEV, A.Y.; H31YER, V.A.; LARIOROV, L.V., BARKHATOV, D.R.
Magnetic susceptibility logging In slightly asgueti.c rocks.
Vop.rud.geofix. no.1:69-78 '57. (MMA 10:10)
Caorings) (Prospecting--Geophysical methods)

1. V30SHEV, A.Y.
.
Iffact of the relief on the results of combined electric profiling.
Uoh. zap. W no 278:83-108 159. (KM 13:2)
5lactric prospecting)

SAMOSYUK.* G.P.j VESHEVj A.V,,
The fie:Ld of a point source of current in the presence of a sphere.
Uch. zap. LGU no.286:3-12- 160. (IMA 3-4:3)
(Electric prospecting)
-
r
4

VESHEV., A.V.
Effect of the relief on work results in dipole axial profilim
Uch. zap. LOU no.286:13-34 160, (MIRA 1476
(Electric prospecting)

VWHEVp AoV*
Presentation of the results of observations in the ?om of aPparent
. specific electric resistance in electrio proqpeoting methods employ6--
ing'alternating current. Uch,zap,WU no.303sl67-166 162*
(MA l51-U)
(Electric prospecting)

BUMAKOVO Xxt.Ij V~SHZV, A.V.
Use: of low-frequana7 altermting ourrout, in olectric prot.134ng and
oowding, UchozapsIOU no*303s187-192 162. (,KM 15sil)
Mactrio prospecting)

VE4 V.; LYUBTSE;VA, YO.F.; SAMSYUX, G.P.
Deteraination of the offectiv,,
,otrame4ersor a Wdtu7in.-tlv~ field of a
finite grounded cable. Uch, zap. -j,~I n,,-~J~U:J-63 '63.
(MIRA 16:9)
(Electric prospecting) (Aeronautics in geology)

cc-N-6 AM-602369o
Monograph
Veshev, Aleksandr Vasillyevi
Electric profil;n~g rw4i~th,,d,,~,iAre-a,tand alternating current (El6ktroprofilirovaniye na
postoyannom i peremennom toke) Leningrad, Izd-vo "Nedra", 65. 047.7 P. illus-,
biblio., tables. 2,300 copies printed.
TOPIC TAGS: mining engineering, electromagnetic fieldt,olootric field
PURPOSE AND COVERAGE: The.theoretical and experimental fundamentals of the methods of!
electric profiling with direct and alternating current and the problems of the
technique, proceduret and application of these methods for the solution of structural
mapping and prospecting problems are considered. The theoretical and methodological
problems are discussed prima ily as applied to the problems and the working conditional
of mining. According to the content and purpose of the work the monograph generalizeal
the results of etu&ies in the field of electric profiling and at the same time can be 1,
considered as a han1book for geophysical engineers and as a textbook for students and i
graduate students of geophysical institutions.
TABLE OF CONTUTS jibridgel7i
Preface 3
Introduction - 7
LCard 1/2

L 02000-67
Ch. I Normal fields 11
Ch. II Anomalous fitalds - - 133
Ch. III Apparatus and observational techniques 232
Ch. IV Application of electric profiling methods - 289
Conclusion - - 361
Bibliography - - 368
Appendix Tables of eleotric and magnetic quantities of low frequency electromagnetic
. fields above a un:Lform conducting half-apace - 383--475
SUB COM, 08/ SM DATE: 07Deo65/ ORIG MW: 248/ OM RWz 045
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io orcjrl'~' Xr," /0=9
CC)I,,: U.
A. G.; Veshev, A V
uogl cal pin g o ore, c1(
c r
~~.!oloc-icaj Congre.;s. 22d, Now Delhi, 1964, Ge o lo &i ch4: skiye
I
Noolodcg~l -e-volta of f-pplUed doklady
1-.-) 2. 1':.AI,;J, 1)65,
i;eolcf-'ic 'Tap, ore deposit
IZ07)TC
C-
T 4 a-pp.1-1-cation of*
o' 1 v. - r C'.~ (-ji' L. -w-frtqjont- f-'eld'for a
Y
'I in -A, '.Q iC-D-;-c ~'c.r mapp'n;' puzrpc~zc~~. Vhp- calculations have -been used
n ro c, n j, wid lncrxial 11.Ilir l-'r'l-I'requency
can be C~~' t,rpe- i'or rnaipetic
t
!;Urtcy 46 mad'~ Inidor cond- =3 wh'~-n
-n May uc. uzed th-. coull rn,:aniL "Dr Th e
wo rt'.. tcce 1'cj,- cov,;d:jn' 7,-r~ or var'
p J. 'J
by
o b- 1 e, -c, -,dIn inntrtimen tat ion, ~,e- v~rjdoloedj
-D h'r o I c 13 t:~ o i.;-g wtan~- --z, connect,
-:Cord ~.12

-,hc- theory
f f-,elcs. 0 rg. ar~
022/
C

YAYOVIYV, A-11-
3n~,e of the medium from Mea3we-
Vi- 1-13-3,
ments 01, low-frequf"nc~y fiplds. Uch* z9po LCU no.324:250-
294 1&i& (MIRA 184)

VESIM, A.V.; 14YUHTSEVA, ve.F.; G.P.
..... ..
DetArmining the offective parameters of the medi= in the field
of a firilta grotmded cable. Part 2. Ucb. zap. L'Al no.3241174-21,.9
164. (MIRA 18:4)

UMB/Physics of the Eal'th Geophysical Prospecting, 0-5
Abet Journal: Referat Zhur - Fizika.. No 12, 1956, 36468
Authors Veohey, A. V.,, Fokin, A. F., Ivanov) Vo K., Semenov,, A. S.
Inatitutions None
Title: Experimental Work on Dipole Profile Tracing
Original
Periodical: GeofizIcheskiye metody razvedki, Moscow, Gosgeoltekhizdat, 1955,
Abstract: Experimental work was performed in a water tank measuring 2 x 2 x
1.5 m. The obpawwations were made on the following models; (1)
conducting sphere taluminum sphere with a radius of 3 r-M); (2)
conducting plate (duraluminum plate measuring 20 x 20 x 0.4 cm);
(3) 2 conducting plates of the same material and size; (4) 2 non-
conducting plates (glass plates of the same size)j (5) 2.plates,
one coziducting the other not; (6) step-like contact of 2 medium
(dibedral right angle made of plywood)j (7) conducting plate in
the presence of a step-like contact (vein of ore near a fault).
Card 1/3

USSR/Pbyaics of the Earth - Goophysical Prospecting, 0-5
Abst Journall Referat Zhur - Fizika, No 12, 1956, 3&68
Abstractt The plates and the contact were always placed vertically. The
depths to the upper edges of the plates vary from 2 to 4 cm.
The distances between the plates (in the cases when 2 plates
were used) or between the plate and the contact, varied from
zero (P:Lates stuck together) to 24 cm. The measurements were
performed with a potentiometer using a pulsator and a semiauto-
matic recorder. An axial dipole installation was used. The
exciting and measuring dipoles were equal to each other (one
or 2 am). The distance between the centers of the dipoles varied
in different experiments from 5 to 30 cm. As a result of the
experiments performed, the following conclusions were drawn:
in dipole profile tracing it Is possible to obtain results that
are fully analogous to the results of combined profile -tracing
of similar objects. What makes the curves obtained by dipole
profile tracing substantially different Is the presence of ad-
ditional extrema, and the high extent to which the limes are cut
up in the anomalous zones (over conducting and nonconducting
bodies of the above form). The degree of the anomalies is
greate:r in dipole curves than in curves obtained by combined
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USSR/Pbysics of the Ew-th Geppbysical Prospectlng, 0-5
Abst Journals Referat Zhur - Fizika, No 12, 1956, 36468
Abstracts profile tracing of'the same object. The results obtained ma it
possible to recommend extensive testing of the dipole prol'ile
tracing under field conditions. One must bear in inind in this
case that in addition to ore objects, there will be disclosed
also sharp anomalies and irregularities of the containing rocks,
which can also be used for detailed mapping. What makes ;he
method of dipole profile tracing difficult to employ is the need
for good grounding devices, particularly in the supply circuit,
for otherwise the difference of potentials that is to be measured
will be. too small. Dipole 'profile tracing offers promisIng pros-
pectB tecause of the possibility of employing al4ernating current
in this case.
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57-
-H-a 1~- - - --- - - ~--- -- -- --- --
T~~
N
SOMOT, A.S.; NOVOZHILOYA, R.Ye.; VESHEY, A.V.
*Varying natural electric field' In the earth.
n0-1:83-113 157. (Terrestrial electricity)
Tap.rud.geofiz.
(MIRA 10:10)

SOV/169-59-7-6722
Translation from; Referativnyy zhurmal, Geofizlka, 1959, Nr 7, P 30 (USSR)
AUTHORS: Semenov, A.S., Fokin, A.F., Veshev,__A.V-., Novozhilova, M.Ye.
TITLE; The Field of a Point Source of Cur-rent on t Plane Day Surface
in the Case of an Anisotropic ffe-=um
PMUODICAL: Tr. Wes. n.-i. in-ta metodiki I tekhn. razvedki. 1958. Nr 1,
pp 210 - 135
ABSTRAM The results of computing the field of a point source of current
placed in a homogeneous anisotropic medium are reported, taking
into aocount the anisotropy coefficient equal to 2. The medium
is conisidered to be homogeneous for simplifying the computations.-
The formulae for computing the potential and the potenti&L gra-
dient and also for detemining the coordinates of the extremal
values of the curves of potential and Its gradient are olLed.
The computations are performed for the following cases: an Iso-
tropic medium, a medium having horizontal cleavage, that with
vertical cleavage, and a medium having cleavage with dip angles
Card 1/2 of the layers of 30 and 600. The first part conceims: the

analysis of the varying form of the curves of potential and its gradient,
depending o5n the dip angle, the anisotropy coefficient, and on the depth of
submergenci of the current source for profiles oriented in the direction of
the strike and dip of the layers. The second part concerns the case of an
arbitrary orientation of the investigated profiles relatively to thb strike
of th6 cleavage, Fcr the latter case the formulae for computing the depen-
dence of the potential and its gradient on the medium parameters and on the
angle between the direction of the investigated profile and the strike of the
layers are quoted. The author assuL-:es that the study of the field of the point-
shaped current source in anisotropic media permits the singling out of the
field distortions ctiused by the anisotropy of the rocks from the distortions
caused by other factors, and that this fact guarantees a more rellable Inter-
pretation of electroprospecting carried out by the method of the charged body.
V.P. Dobrobollskiy
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PUM I BOOK IWIXTATION UW/4059----
Veshev, A. V.,, L. Ia.. Wzyt*., G. A. Petrov., A. F. Fokint and A. M. Chirlyev
llektronnsm elektro:mzvedochnaya apparaturs, ZSX-1 0 XMI-1 i KM-1
XSR-1s, and WN-1 Electronic Equipment for Electrical Prospecting)Moscov,,
Googeoltekbizdat., 1959- 103 P- Mnv~tx slip inserted. 4#000 copies printed.
Sponsoring Agencies: Vsesoyu=yy nauchno-issledovatel'skly institut netodiki
i tekhnJk4 razvedki; USSR Mini6terstvo geologii i okhrany nedr.
Ed. of Publishing Hcuse: V. I. Korchagia; Tech Ed.: V* V* BALCM0
PUHPOSE: This textlx)ok is intended for geopbysicists., field Epologists, and
persons engs d in geological exploration.
COVERAGEt 7he book describes nev electronic equiTment manufactured for electrical
prospecting by tJoe use of direct current. Tue book also describes principles
,of operation, caastruction, &ad efficiency tests performed udder both field
and laboratory conditions. The book also gives directions for using the
iastrm3ents, and lists possible cwses of trouble,, along with methods of
Card 1/5

elimirating them. The basic diagrams and first models of the equipment were
devel*ped by the Tzistitute of Science of Machines and Automation., Ac mV of
Sciences,, Mcr 63R) In cooperatica with the electrical prospecting lAboratory
of the VIRG (VITR). Field tests of the equipment were carried out jointly by
the above-mentioned labomtory and the DIA AN Ukr SM. Production models of
the apparatus were do-veloped in the OKB of the JUnistry of Geology and Conserva-
tioa of Mineral Resources, US= The following rersons participated in the
devcjIDTment of the electrical prospecting equipment: A.V. Vesbev, V.G. Zubov,,
K.B. rQu-andsyev, L.U. YAzyuk, G.A. Petrov, F.P. Sogolovskiy. A.A. Flaksman..
A.F. Fbkint G.A., Shtamborger., A.N. Chirlyev, and L.H. Jaffe. In writing this
textbook.. the following persons participated on behalf of the OKB MiON:
A.N. Chirlyev and G.A. Petrov; on behalf of the D% AN Ukr MR: L.Ya.
Ydzyuk,, V.G. Zzgxyv-, an bebalf of V37R; A.V. Veshey, L.V. Larionov,, and A.F.
Flokin. General editing was done by A.V. Veshev. 7here are 15 references:
12 Soviet, 1 Swedish., 1 English.. and 1 Fivnah.
TAZZ OF CCNTKM:
Ploreword
3
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ESK-1,p and XM-1 Fazetranic: Equipmut, (cont.) S-0-VI/4059
Ch. 1. Buie DIBV,*&Ms of Electronic Automt1c ftepenzators ESK-1, KM-1
.
.
and KW-1 8
1. Mock diagnum of the ESK-1 and IM-1 instruments 8
2. Operating principle of the automatic compensation eircult. 10
3. Operating principle of computing aurtantic compensators MM-1
and XMH-l 14
4. vibropack :matures and construction 21
5. D-C electroide #Aplifier 27
6. Polarization. camVensatdr 36
Ch. 11. Electronie. Pointer Cagpensator ESK-1 37
1. ' Tecbnic&l fbatures of the Instrument 37
2e Basic d1wxm of the Instrument 38
3. ConstrwA1,012 Of the instrument 43
4. Adjtwtment and testing of the instrument under laboratory and
field conditions 48
Ch. nX. Computing Compewmtors MM-1 and ISRU-1 52
1. Machnical, features of the instrument 52
2. Basic diAgran of the MM-1 instrument 55
Card 3/5

Mill on
ESK-19 and xm-1
3- OWstructioa Of the MR-1 Wt--=Ont 61
4. Buie diagram of the EM-1 in8trment 65
5- owwtr6-ctIoa of the EWI-1 Instrawnt 70
6. Adjustment and testing of the instruamts under labarat=7 and
field conditions 74
7. Sources of trouble of the IISK-1., MR-I &ad XM-1 instr=ents 81
Ch. M 11scoownfttions on Using Equipment In Accoz%lftace With the Basic
I 116thods of- Ilectrioal Prospecting 82
1. Measurement technique 82
2. Characterlifte features of electronic eqjuipment oremi-ions
using basia methods of D-C electrical pivapect-ing 88
Conclusion 92
Ribllogmphy 93
Card 4/ 5

ESK-Ij, and Electronic Equipmnt (Coat. SOV/4059
Aoendimes:
1. Wiring tab le of the ESK-1 instrument 94
2. Wiring table of the KBR-1 instrument 9T
3. Wiring diapam of the ISKA instrument [insert]
4. Wiring dUg= of the XBR-1 Instrument
control panel linsiert]
5- %sic di"rea of the ESM-1 instrument [insert]
AVAnAXZ.* Mroxy. of Congress
IN/m/fal
Card 5/5 8-lo-6o

MWAXOV, Tu.I.; LARIOMV, L.V.
Bridge type instrumats used In wouring mgnetic ffunceirtl bill tir
of -rocks and ores. Uoh. sap, IOU no,278:136-142 159.
(MRA 13:2)
(magnetic Instr=ents) (Rocke-Maguetle propertiae)

SOV/169-59-4-4555
Translation fromi Referativnyy zhurnal, Geofizika, 1959, Nr 5, p 41 (USSR)
AUTHORS: Veshev, A,,V., Pokin, A.F., Petrov, G.A.
~50
"7611M I-V
TITLE: A Nfyw Device for Electric Prospecting by Direct Current
PERIODICAM Tr. N~aen. n,-i. in-ta metodiki i tekhn. razvedki 1958, J1r 1,
pp 145 - 160
ABSTRACT: An eleotronic-needle compensator ESK-1 and a computing c-ompensator
KSF. for electric prospecting by direct crrent are described,
11;t which are developed by the Institute for Science of Machines and
Automation of the AS USSR and produced by the plant "Geclogoraz-
ve(tka". The devices function on the principle of auto-compensation
realized by means of an amplifier of direct current with trans-
fo:mation. The principal circuits of ESK-1 and KSR are presented
and the main characteristics, the description of the device, and
the methods of handling the latter are given. A note on the
development of a third device is added, which Is an electronic
automatic compensator designed for the separate registration on
Card 1/2 a film of the quantities & U and I. Field tests of the ESK-1,

SOV/169-59-5-4555
'A New Device for Mectrlc~Prospecting by Direct Current
KSR' and EAK y1elded positive results. The accuracy of measurements with
electronic devicei3 to somewhat higher than that of a potentiometer, and the
performance increases even In relatively simple oonditions by 1.4 - 1.7
time.-i.In regions with industrial disturbances, the electronic devices have
no advantages in ..,omparison to the potentiometer. The introduction of the
devicee into the practice is recommended.
A.A. Smirnov
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---------- ------------------
lam I -------- --
,-V It. 5 -
USSR/Physice of the larth - Geopbvoical Prospecting, 0-5
Abst Journal: Refera' Zhur - Fizika
4. , No 12., 1956, 36456
Authors Vashav., A. V.
Institutions None
Title: Scheme for Magnetic Iogging of Strongly4iagnetic Rocks and Ores
Original
Periodical: Collection: Geofizzicheakiye metody razvedki,, Moscow,
te*zdat, 1955, 57-59
Abstract: A scbeme in a description is given for an instrument for ishe
logging of magnetic susceptibility X. The sensitive elemimt of
the Instrument is a self-induction coil vith an iron core., vhich
Is dropped into the bore hole with the aid of a vinch. The coil
is ccnnected into a bridge circuit, containing a standard induz-
tance and 2 active resistances. The bridge circuit is fed from a
vacimm tube oscillator with a frequency of 56 cycles. Thl~ oensi-
tive element is located on the surface and the bridge nearly
balanced. When the susceptibility of the surrounding meUum
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USSR/Pbysics of the Urth - Geophysical Prospecting, 0-5
W'6
Abst Journalt Refer 10 Zhur - Flzika, No 12, 1956, 36456
Abstract: changes, the bridge becomes unbalanced, and the change in its
inductive reactance depends on the change in the self-induction
of the sensitive element, which in turn, de nds on dZ. The
sensitivity threshold of the circuit is loTema
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3/169/62/000/000/035/093
D228/D304
AUTHOR: Veshev, A. V.
I---
TITa Influence of rock irregularities in electric profiling
PERIODICAL: Referativnyy zhurnal, Geofizika, no. 6, 19629 31, ab-
stTact 6A233 (V sb. Vopr. rudn. geofiz., no. 2, M.9
GoSgeoltekhizdat, 1961, 36-55)
TEXT: The results of modelling irregularities of a 8tratal nature
in combination, symmetrical, and dipole electric-profiling are gi-
ven. The following were modelled: A thin bed of.high resistance,
two beds and a -ack of 5 --8 beds of high resistance, a conductor
P
in the presence of a high-resistance bed and a pack of beds of
high resistance, two conductors, and a variable thickness of loose
deposits. The curves Of Pk for different angles of 8trathl dip,
with the interstratal distance being somewhat less than "'he detup's
dimensions, are cited and analyzed. The dependence'of the nature
-of the Pk curves on th e correlation between the set-up's dimensions
Card 1/2

S/169/62/000/006/035/093
Influence of rock ... D228/D304
and the thickneos of t~e pack of beds, and also on the pack's
depth, was investigated. The distance between the conductor and the
high-resistance bed, with the conductor being placed inside the
pack of beds, and the set-up Is dimensions were varied. The follow-
ing conclusions which are recommendably taken into account in sear-
ches for conductors, are drawn: 1) Poorly conducting irregularities
cause The direct intersections of the Pk graphs to shift to the
side of the cond.uctor; 2) when influenced by a variable thickness
of deposits, conductors are marked only by the approach
Of j; 3) irregularities in rooks of high resistance a1_
10 k. Curveg
so cause the direct intersections of the Pk graphs, In connection
with the obtained data it is recommended that the distinguishing'
and The determination of the location of poorly conducting objects
should be made on the basis of the analysis of the nature-of all
the p, curve peculiarities along the whole observational profile.
I Y.
/%.bstracterls note: Comolete tranelation.7
Card 2/2

-1 VESHEV) A V.- YLIYSHEVf B.P., nauchnyy red.; CIMSMIK, V.11.9 otv,
==~IMMT, L.A.,, ved. red.; FIMOROV, S.S., tekhn. red.
[Low-frequency electric prospecting apparatus) Elektroraz-
vedocbnala apparatura, nizkoi chastoty. Lenin ad., Gostop-
tekhizda:t, 1962. 49 p. FMIRA 15:8)
(Electric prospecting-Equipment and supplies)

VESHEV,-Dinko, inzh., sutrudnik; ZAKHARIEV, Georgi, inzh., sutrudnik
To raise the standard of asphalt-concrete mixtures to the current
scientifio and technological level. Ratsionalizatsiia 14 no. 3:
29-30 16i~.
1. NIIPe

VESIMV, V. V., FOKINI. A. F.) PETROVy G. A.
"New Appliances in Direct Current Electro-surveyingil
(New Developmentu in the Metbods and Tecbniques of Geological Exploration)
Leningrad, Gostol)tekbizdati, 1958- 423 P- (Seriest. Its: Sboralk trudov 1)

1WHI F
"The way we work to increase the production of cow's milk.
P. 14 (Per Bujqesine Socialiste) Vol. 12, no. 1, Jan. 1958
Tirane., Albania
SO: Monthly Index of East European Accessions (EEAI) LC. Vol. 7, no. 4,
April 1958
T
P T, 14

VESHII L.: KALESHII V.
"Nitrification in Albania and measures for soil sterilization"
Buletin. Seria Shkencat Natyrore. Tirana, Albania. Vol. 12, no. 4, 2958
Monthly list of East European Accessions (EEAI), LC, Vol. 8, No. 6, june 59, Unalas

vi, ~. N I M -
"Draining the Vurg and Mursi plains."
p. 8 (Teknika) Vol. 4, no. 5, Sept./Oct. 1957
Tirane, Albania
SO: Monthly Index of East European AccesEions(EEAI) LC. Vol. 7, no. 4,
April 1958

Tx-~~-YAy-LVXWL, Slavo~], prof., doktor mad.; BYSTRCUT07, D.A.
[translator]; OSTRDYSrATA, L.S.. red.; GABERLAO, M~Iep
tekim.red.
(Radiographic diagnosis of hemoblastomeal Rentganodiagaostika
gemoblastom. Moskva, Gos.izd-vo mad,lit-ry Kedgiz, 1960 85
Translated from the Czech. (xi;; 14:13*
(13LOOD--DISIUSES) (RADICLOGY, MOICAL)

GOFMAN-ZAKHAROVI
E-ples of hydraulic calculations in the design of gas pipelines
for liquefied gases. Gaz. prom. 7 no.11:35-36 N '62.
(MIRA 17:9)

ACCESSION A241008917 BOOK EXPLOITATION
Gofmah-Zakharov, Petr Maksimovichp Veshitskiy,, Villyam Anat-ollyevich
S/
Tran*rtation and storage of liquefied hydrocarbon gases (Transport i 1,ehraneniye
szhizhenny*kh uglevodorodny*kh gazcv), Kiev., Gostakhizdat USSR, 1963,. 278 po
illus.j biblio, 600 copies printed.
I I
TOPIC TAGS: transportation, storage, liquefied hydrocarbon gas, hydra-ulics,,
oil pipeline, pumping station., underground storage
PURPOSE AND COVERAGE: The book deals with the problems of transportation of com-
pressed hydrocarbon gases and examines the progreasive methods of storing them,
in particular, in isothermic Imi-temperature reservoirs, underground cavities in
salt formations and other impermeable strata. The thermodynamic fundamentals of
isothermic low-temperature storage of liquefied gases and specific hydraulics prob-*
lems of pipeline transportation are discu u. d
ssed. The methods of equipping undergro n
containers of liquefied gases, the sldj=dn operations, problems.of selecting opti-i
9
mal parameters and the basic equipment when designing equipment for transp
orting
and storing liquefied gases twe also discussed. A lat-ge part of t1ut book is de-
voted to foreign experience in pipeline transportation of liquefied gases and their:
underground storage. The book is intended-for engineers, technicimis, and research-

ACCESSION HR AV4008917
ers of the petroleum.,chemical., and related industrios who are connected with. the
design,, construction., and use of transportation facilities and storage facilities
.for liquefied gases and other,yolatile liquids. i
TABLE OF CONTENTS [abridged)i
Foreword 3
Transportation of liquefied hydrocarbon gases
Ch. I. Current state of transportation of liquefied hydrocarbon gases 6
Ch. II. Specific features of pipeline transportation of liquefied hydrocarbon
gases 45
Ch. III. Hydraulic calculations of liquefied hydrocarbon gas pipelines 66
Ch. IV. 111echanic,-A strength of pipelines for liquefied gases 106
Ch. V. Pumping st-ations of liquefied hydrocarbon gas pipelines 13.5
Storage of liquefied hydrocarbon gases
Ch, U. Storage of liquefied hydrocarbon gases in steel pressure containers 160
Ch.-VII. Isothermic containers of liquefied hydrocarbon gases 178
Ch* V111, StoraSe of liquafiod hy&oaarbon gasee in nonmotallia shalla and
mine shafts 214
C=4-2A.

MIKLOS, Anatol-ily Georglycvlch; VESHKELISKIY S A j'jnzho, retsenzent;
lAb-Z-0, M.D., kand. t retsenzent; ALE"ANDROV,
A.D.v naucrAn. red.i Tu,l., red.
[Automatic control and control and measuring apparatus of
marine power plants) Avzomatika i kontrollno-izmeritellnye
pril:v)ry sudovykh sih)N7kh ustanovok. Leningrady Sudostroanie,
1965. 139 p. (MIRA 16:6)

KUDINOV, Nikolay Nikolayevich; ALIKIMOVICHj A.V., inzh.p
retsenzent; VESIUMLISKIY S A retsenzent; BADIV,
Yu . P * p nauc W.- M. "; t)", - ~.* -1 ~''- , - . red .
(marine atomic power plantel Sudovye atomnye energotiche-
skie ustanovki. Leningrad) Sudostroanie,, 1964. 330 P.
(MIRA 18:2)

VESHKO, E. I.
Cand Agr Sci - (diss) "Significance of liming of light- pod-zolic
soils of forested areas for the evolution of organic substance
in the body of the soil and processes of its cultivBticn." Kh-3r'kov,
1961. 21 pp; (Ministry of Agriculture Ukrainian SSR, Khar'kov
Order of L9bor Red Banner Agricultural Inst imeni V. V. D,-,'.%-uchayev);
150 copies; free; (KL, 6-61 sup, 2~11)

VIMMINVSKIT, Stanislav 111kolayevich; SAPAROVA, A. L. radaktor; VORONIN,
T~Pi,Aekhnlcheskir redaktor.
[Calculation of characteristic curves and resistance for alLaCtric
motors] Rashchat kharaketristik i soprotivlenii dlia elektr)dvi-
gatelei. Izd. 3-e perer. Hoskva, Gos. energ. izd-vo, 1955, 336 p.
. (Blectric motors) (MLRA 8:8)

1. VESHEV. AN. - SD-IZ-.WVp A.S. - NDVOZHIIDVft:, M. Ye
2. USSR (600)
4. Geophysics
7. Now aspect of earth's natural electrical field. Dokl. AN MR 87 no.6, 1952
9. Monthly list of Fassian Accessions, Library of Congress, March 1953, Unclassified

VWHN, A.T., rodaktor; GAMBUFUSIVA, Te.Ts., redaktor; OMTA, O.A.,
N"Yw"Icheskly rodaktor.
[Geophysical methods of prospecting; a collection of articles]
Geofisicheskis metody raxvedki; sbernik statei. Moskva, Gee.
nauchno-tekhn.isd-vo lit-ry po geologit i okhrane nedr, 1955-
68 Pe (MLRA, 9;1)
1. Howcow.Vassoyuznyy naucbto-iseledovatelinkiy institut
rasyedochnoy g'sofiziki,
(Prospecting-Goopbysical methods)

VESHEY.- A.I.-- 1,
Bridge circuit of a magnetic logging device, Razwed,1 okh.
nedr 21 no.2'.32-37 Mr-Ap 155. (WRA 9tl2)
(Magnetic measurements) (Prospecting-Geopbysical metbods)

FA Z4Ur83
U'SSR/Geophysics - Electric Field of 21 Dec
Earth
"New TyDe of Electric Fiel-I in the Earth," A. V.
Vesbev, A. S. Semenov and M. Ye. Novozhilova, All-
UAi0h OCI-Reb Inat or Vurvey Goophycilert
"DA,N SSSR" Vol 87, No 6, PP 939-941
Certain anomalies in terrestrial elec field were
found in 1939 by V. P. Bogdanov and in 1945 by
V. A. Vedernikov. Author confirmed these facts
in 1951 and established their connection with an
unknown natural elec field. Presented by Acad
0. Yu. Shmidt 30 Oct 52.
240T83

USSR/Geophysics - Ble ctropruipectiri,; Mar/Aix 53
t?Review of I Ins truct ion,3 f or '--'Iec ID.-opraspec ti-ri:7,AG. Dranolr) (mviesier~
Iz Ak Hauk SSS111 Ser Geofizp No 2, PP 193-195
Favorable rwriew of book "Instructions f or Zlectroprospecting" (Instruktsiya po
Elektrorazvedke), published by the Main Geophysics Admin, Xin of Geoloa USSIZ,
Moscow, 1952; 130 PP) 8)000, copies, price 4.30 rubles. Co-authors are j',,. S.
Semenov, A. V. Veshev, A. S. Polyakov, and 11. 1. Shakhov. FAitor is A. M.
Za,garmistr.
Pik 254T82

VESHEV, Dinko, inzh.
What makes changes in the road bitumen standards necesaary.
Ratsionalizatsiia 13 no.703-34 163.

'.Service awards. Grazhd.av. IS no.7:10-2.1 J1 161. (MIRA 14:8)
(Aeronalatics, Commercial)

41

.--YMHITSK,IY, V.A.
Seleciing t~e doisign'for.laother~dc storage of liquefied
gases. Gaz.delo no.11:19-24 165. --
(HERA 19ij)
1. Gosudarstvenvy komitet po koordinataii nauchno-issledo-
vatel'skikh rabDt pri Sovete Ministrov UkrSSR,

VESHITSKIY, V.A., red.; KACHUR, O.Yu., ved. red.; ROZOVA, S.T.,
,- ". "... ~ 1. . - -
(Isothenua storage of liquefied gases] Izotemicheskoe
khranenis szhishenrqkh gazov. Moskva, 1962. 65 P.
(MIRA 16:10)
1. Institut tekhn#eheskoy informataii i ekonomicheattkA
iosledovaniy po-neftyanoy i gazovoy promyshlennosti.
(Liquefied petroleum gas--Storage)'

., V.A.; TAFISTO'~N.V.; POVOLOTSKIY,, I.A.
VESHITSKIY P
I--
Map of pipelines of Western Europe. Neft. i gaz. prom. no.2:77-79
Ap-Je 162 (MIRL 15t6)
iftrope,, Wastern-ripeunaa-:-~po) ,

Effepot of 11xing the light turfs am podficle of Polesie
provineji~" the changes oftheir organit dUbAtanc48- ZeOz
probl pG-'Ot roln no-50at221-230 164.
1. A.N. sokolovskii Ukrainian Research Institute of Soil Science.

0
MIRZAYANTS, G.G.; VESHNEVA, I-V-; ZEFIROVA, G.S.; KIIAYYJNA, M.B.
Fainefelter's syndrome. Vest. APT SSSR 20 no-3:17-20 IE5.
(,laRA 18: 7)
1. Inatitut morfologii cheloveka At-IN SSSR i TSentrallnyy
institut usovershenstvovaniya vrachey, Moskva.

PROKOVIYEVA-BELIGOVSKAYA, A.A.; 1!~T!N~VAV,I.Vj,
Spontaneous chromo.,3ome injuries in embr-fonic human fibroblasts in
vivo and in vitro. Dokl. AN SSSR 153 no.2-.457-459 N 163.
(MIRA 16:12)
1. Institut biologichaskoy fiziki AN SSSR. Predstavleno akademikom
N.A.Engellgardtom.

SHVARTS,.Aa,, kand.tekhn.nauk;,~~HIIIKIIVI A. inzh.
For inventors of rotary engines. Izobr, i rate. no.7051-40"and 3 of
cover J1 161. (14IM 14.: 6)
(Gas and oil engines)

1A mif it oil yu Ion lou OP041
It It I
y , 1,08 Cal I d-t.1 ail to .11
fit A-* 1'vi~lqs f-!
M I..a
00
0
00 a 0
66 j
00
049 w
008
00
U AV
7ev p 4,410
0
000 V:
0
A.Ns&UW%Ul and A. A. ivavmvv. Rum.
314,714, urpt. ;W, 1%04, "all to OWS104 "n-W or"Iming
CU"Itoaoitlgfwuppl"wctkmolavacuutnturlww which
it OMf*14?d In omb m"n" im to p,,t"jI file oq%Z~a ow
voltifillant 'I* 'a the Rad"k MCII(Ift Oftl its CWtiltsuatiou in
the. "Tit P%" tht (11IFUMICV.
onset*
Wes
be
.00
=40
ig 0
600
r90
00
:0 0
ligol ad owtv .04 goo
J-4 -4- -i a -W - - - - - -
m
to to to it at of a a wK PCUel Ila
0 * 11111 0 0 11111 0 0 0 00 0 6 0 0 e 0 0 0 0
0
0 0 0 0 0411110 0 0 0 00 00000041 00000 411111

MARTS, A., kandidat aa, tokhnicheakite nauki; VESHNIKOV, A., inzt,; KCMV.. S.
On the rotor motors with Internal combustion. Hatsionalizataiia 12
no.9:13-17 161.
1. Direktor na Voeuiuznila naucbno-tekhnicheaki institut pri Durzbaynata
patentua ekspertiza(for Komov)
(G" and oil engines)

L 1174-66 WT (I /T/FCZ, (k
ACCEMION MRs AP5017655 UR/0109/65/0101007MI0111189
621.396,6TT-Ti-
AUTHOR.- Veshnikova, I., Ye. 1 Yevstropov, G._1.
TMEs Theory of matched slot rad-lLatore
.SOURC3t Radiotekhnika i eleltronika, v. 10# no* 7, 1965t 1131-1189
TOPIC TAGSt slot radiator, slot antenna
ABSTRACT's Formulas for the conductance of a resonance slot having an arbitrary
position in the.wider wall of a rectangular.waveguide are developed by moans of
a power-balance equation and a Lorentz 1==t. The resonance-slot equivalent
circuit can be represented-L~r a length of 2-4dre line with.a parallel conductancee
An equation is set up that -lescribes the sl(it position required for matching by an
Inhomogeneity placed in tho slot center. Alito formlas are derived fo:! tho
radiated power and the matching reactance. Experimental verification of tho
formulas on a waveguide with a cross-section of 1.46A30-435X is 01SAMd-
Orig. art., hast 6 figures ard 34 formulas,
Card 1/2

L 1174-66
ACCESSION MRS
ASSOGIATION: none
SUBKr=: I UW64 ENCL,i 00 SUB CODES Ec
NO REF SOVt 002 OTHERS 006
1~ccrd 2/2

lot
J* *v4"m rwonomm fm""Go an is omm rnwm~-* Am pow"W"s %-"a
*A-$ v I
(6-wh u of 31
O-ft *4
SLUO" UINSURV UVA32 I
AM@ how ft lusboh limmol-im-mv
d--u 'm I
ME-on m

Oct 1947
-~T Sol
1%~*Istratlcn of Rztensive Deformation of the Ms-
*k+,k of the SwUls Crust during larthquakosjp" X. Vv'
'MoOnyakovp Selamol rust, Ace& Sol MW~ 4 pp
Akad Sauk SSSR, Nova Ser' Vol Lvni, xo~ 3
-Aither discusses various points to bear out his oan-
Iao~ticn that tke action or deformation shouia be
1= VItb the action of agitation in- 661=0-
laiia obse"atians. Claims that main reason for not
-IWtlztg defarmaticn is that it is more difficult to
O"aris and also noticed rar less tiAm the aetlan or
, .0
,4411tation. Macummes use of selamlo extensometer,ibe
49M3
WO/6sology (cont&) Oct 1947
4~~93.ops& for registering extensive deforwation of
:91~wmie In the earth's crust. Submitted by Adedsal-
*Im 0. Tu. Maidt, 10 Wq 1947.

PA iAoml
Jui/AUS 48
Seismograph
"Modern Selemometric Apparatus," D. P. Kirnos and
S. V. Veabnyakovo Acad Sol USSR, GeophX Inst, 0 pp
*Iz Ak Nauk SSSR, Ser Geog I Geofit" Vol nI, No 4
Describes apparatus recently released by Seis-
mological Inst, Acad Sol USSR: nev type of seis-
mograph wltb galvanometer type register for
registerIng displacement of C t-during-earth-
uakes--and 4. e romagnetic type extensometer for
determining dynamic deformation of soil. Submitted
3 Wr 1948
I A9263

USSR/Geophysics - Seismology FD-1781
Card 1/1 Pub 45-3/18
Author Veshnyakov, N. V.
Title Quantitative evaluation of the strength of an earthquake
Periodical : Izv. AN SSSR, Ser. geofiz. 207-214, may-jun 1955
Abstract : The author discusises existing methods for evaluating the strength of an
earthquake at the point of observation. He Introduces and logically es-
tablishes an assumption for determining the strength or intensity of an earth
quake in accordance with the maximum energy density of the seismic waves In
mineral rocks sittLated on the eartJ21s surface, and for expressing it in joule
per cubic meter. Sixteen references; e.g. S. V. Medvedev, "New seismic scale
Trudy Geofiz. in-ta, No 21 (148), 1953-
Institution: Moscow State University im. M. V. 1,omonosov
Submitted : January 28, 1954

AUTHOR: Veshnyakov, 11,V. SOV/49-58-8- 01/ 2 7
TITLE: On Certain Errors in the Determination cf
Azimuths Usin,F, the Three-stations Method (0 nekoto.E-y--fh
osl-dbkakh opredeleniya azimuta mikroseysm po retoda
troynykh Stantsiy)
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya geofiziche:~',,-aya,
19581 Nr 8, pp 1020 - 1025 (USSR)
ABSTRACT: The three-station method is normally used fo~~- deterrininS
the cc-ordinates of microseismic sources au,--;h as cyclones.
The layout is as follows. A vertical seismograph is
placed at each'vartex of a trianele OBC (FiCure 1) which
has sides of length 1-3 km.. These are counected tc, a
central observation noint. where the oscillati-jus are
registered simultaneously. The trace thus obtained er,)tles
the time for t.-te wave front to pass the triar-gle to be
measured. Hence, the azimuth of the surface normal can be
calculated - assumin.6 the wave to be plane with constant
velocity of propagation. The co-ordinates of the uicro-
seism. source are obtained by an intersection r.th,~~d i.,Sinj-
two observation points. The main value of the ~-station
method is that, so lonG as all the wAves are propag-ated
uard 1/'/

Un Oertain Errors in th4-.- Determination of SOV/49-~8-8-9/1?
the Threo-51Ulationfi j-jTj-~,tjj()jj em Azimutiio
in the same direction, interf (-f f-,nce between waves does
not interfore witi, tlie men3uremeats.
The direction of the microseismic source defined by this
method does not usually coincide with the centEe of rl!~,e
cy clone (Ref 1). ~This difference can reach 90 or
The author considerF4 I!ha'j systematic errors niLjit hel,-p
to produce this result.
1) Errors in measuring the elements of the trianSle and its
orientation - these are easily determined and the author
does not consider them further.
2) Errors arising from incorrect determinations c~f the
time of passage of the wave front between the vertices
of the triangle.
~3) Errors due to peculiarities of the gological. Ftr~i-tare
cfr the Earth crust between tbe cyclone- and the observation
poin-1-
Onljv~rrors of type 2) arr- cDusldered in this artlcie~
Seismographs are placed at tt-P 1)oints 0, B, C (Fissure 1).
OC makes an anGle y wilth t-be meridian and the angle,
C,grd2/? at 0 is e . The azimuth of the beam is denoted.by A.

SOV/49-58-8-9/17
On Certain Errors in the Determinatton of Microseizni Azir,,utLe U'-111,r,
the Throo-statione Methoij
tb is the time of passaSe of a wave along side b and
t. along side c Then 114he azimuth of the wave is giver.
by Eq.(l) (Ref 2). It is sometimes preferable to determine,
instead of AZ , the angle (x between the wave surf,-~,ce
and one of the sides of the triangle. This is given by
Rq~(2) (Ref 3), where AZ and a are connected by
A.Z = 'IY/2 + y - m Introducinif the notation k3) and
assuming that dt d-to ~ dt the differential forn
b
of (2) becomes 3q.(4). If 'v is the velocity of Proipa-
Sation of the wave, MI-0) Lives tb and t. ';1hi:!h
gives Eq.(6) as an alternative form of Eq.(4). Ec.(6)
represents the required relation between the eri,Qr ;,n
azimuth da and thecloror in the time of passa~~,'e olf. the
wave, dt . 0)
It is assumed that the triangle is equilateral (e = 60
that b = a =lkm. and v = 2.?5 km/sec. Eq.(6) th(.,r
Gard3/7

SOV/49-58-8-9/17
On Certain Errors in the Determination 3-[ Vicroseism, Aziml~ithc
the Three-stations fdetho6
transforms into (7). The averaSe distance of the source is
assumed equal to 3 000 km, which is to be deternined to
+ 100 km. Table 1 gives the corresponding permitted eriorz;
in tinie, dt , as a function of a .
The error in the Bleasurement of the time of passage must
thus not exceed 0.006 se-- 7 so that the Deismographs rust-
jaeasure to 0.001 sec.
The author now cDnsiders what conditions must be fulfilled
by the iastruLieff1j-s used. As is known, the seismoEr_aplis
reproduce the wave phase with a certain time change - this
m-ust be the sarae for all three seismographs.
Ti is the period of free oscillation of the pendulum;
T is the period of free oscillation of tl:e a 1 v an omt e r;
2
D1 is the dartiping constant of the renduljm; D2 is the
2
damping constant o'L the ~F_Ivanoneter; 0 1 the r e; 1 a It, i v e
coefficient of the pendulum. Ptid galvano:irter. The phase
hange -r_ can bc- calculated from Eq.(8) (Ref 4). 'TLis cdn
Gard.4/7 ~e written as Eq.(10), if 9- is the peiiod of th essei3zic

sov,/49-58-8-9/1'/
On Certain Errors in the DeterL,~inatio-rl Of 14icrossisr Azi,,utl-~s
the Three-stations YetllodF
2 t
wave and w 'V/e. This, can, be simplified to Eq-(13)
uoing the notation (12).
The error iu 'Vi cai,, be obta.-'Laed from Eq.(14) for de
where the coeffj.cients on the riCht-hand side s-re replaceeb-le
by coefficients - -),( -,,( and -k, iaa'l
Itl 1 %21 3, 4 ', L
have a sintilar E;tracture of the type (15). Table 2 Lt-i-ieE;
expressions forthe coefficler,"Us Ai, Bi- Ci and B4 i-n
terms of P1 Q,, M and S and their differentials *
The author now uses these cquat4ons for a particulor case
with T, = 7.0 see, T2 = 4.0 s;c, Di = 1-.5, D2 = 2.0)
(52 = - calculated
0.25 Table 3 tives the corresponding X,
from Eq.(15). It is next assumed that the Dora-m(-.ters are
determined with the folloviiiq errors: dTl = dT2 O.C.1 sec;
2
dD, = dD2 = 0.05 see: d(Y = 0.05 sec- UsinC this dal--a in
Eo. (14) , the errors in Id can be calculated (Table 4) -
where the time is expressed in milliseconds.
Card.'/?

-OV/4-9-58-8-9/17
On Certain Errcrs in the Determinatirn of Microseism Azinlith8
he, Three-stations Method
Vost microseisms heve a period 4-8 kees. Table 4 i't'di'a-te-3
that in this c.,~~se the phaze cha%e of each saismoeruph cail
be in error bj 0.02 - O.OE sec - or two seisino rilphs coi.,
differ by 0.04 - 0.1-2 sec. The correspondin,-- ervors in
azimuth, (alculated from Ea.(?), are 6iven in the last
(It if~ assured that the instxu-ment parameters are known
accurately - if, for example, the damping constant is knov.:n
to a~ accuracy of 0.1, the error iii azimuth c3n rise to
j~ 70 ) ~
The accuracy of the method can be improved in the following
ways. The .5implest way -is by increasing the lenCths of the
sides of the trianfle to 06-7 km. (half the shortest wave-
length). Eq.(6) shovis them this can lower the error bv
6-7 times, down to 1.5 - 5 . Difficulties will arise, of
course, due to the long electric cables used. The other
method available is to improve methods of dete;-rriining the
instrumental parameters and of maintaining the latter
c,onstant for long -periods of time.
There are 1 figured 7 tables 2nd 4 references, 3 of which
Card6/? are Soviet and 1 E.nglish.

SOV/49-58-,9,-9/lr/
On Certain Errors in the Determimtion of Microseism Azimuths Using
the Three-stations Method
AS SOCIATION: Moskovskiy gosudarstvennyy univeraitet
im. 11.V. Lomanosova (Moscow State University
imen-i M.V. T-e-)monosov)
SUBMITTED: February 12, 195,8
I. Microseiams--Mathematical analysis
Card ?/?

SOV/49-59--4-13/20
AUTHORS: Belotelov, V. :r., Zhilyayeir 1, 1.
if. V.
TITLE: A Seismic Energometer (Seysmicheakiy energometr)
PERIODICAL: Izvestiya Ucademii nauk SSSR, Seriya geofizicheskaya, 1959
Nr 41 pp 611-616 (USSR)
ABSTRACT: A seismic enorgome-cer was designed by A. V. Rykov for
the Institute of Physics of the Academy of Sciences USSR.
The apparatus is able to rgeord the following kinematic values:
1) the squared velocity v- of vibration of the Earth's sur-
face at the point; of observation,
2) its time integrall, i.e. ~,,2 dt
0
The differential equation of motion for this type of apparatus
can be defined as Eq (1). If the damping effect is great and
2e~ >> n2 ., then this equation can be substititted by
Y
Eq (2). In order to obtain the velocity of vibration? the
parameters of the qDparatus should satisfy the following
Card 1/6

SOV/49-59-4-13/20
A Seismic Energometer
conditions. 1) The period of the pendulum To should be
equal to the mean period of the seismic waves, i.e.
T
0 V'P m- n TP max
2) The constaunt of damping D should satisfy the formula
T
P
D P max M
F min
(VI P
where 6 error in fraction of unit. Therefore, the main
part of the energometer wao designed for the following para-
meters:
Card 2/6

SOV/1+9-59-4-13/20
A Seismic Energometer
T1 10.0 sec. D, - 3.68,
T2 6.9 see., D2 - 8.611
K1 229,x 0 g cm c12- - 0.0521
~2 m-16.3 x 10-2 g Om it - 100 em
A - 70 cm
where 1 - pendulum, 2 - galvanometer, K - moment of inertia,
Cr 2 _coupling coefficient9 1,0 - length, A - optical sect-
ion. In this case the deflection of the indicator is
y -- ;7(t) , where -q - 140. The interval of the velocity v
is 3-26 see (Fig 1) with an error of 6% (dotted line in Fig 1
The value of v is transformed into ~2 by means of a mask
with a parabolic opening (Fig 3). It is denoted by 3 in
Card 3/6

SOV/49-59-4-13/20
A Seismic Energometer
the general layout of the apparatus shown in Big 2. Its
other components are: lighting and optical systems - 1-4
and 11, galvan,ometer with a mirror - 5, a photographic
camera - 6-9, with an automatic control - 10. The image
of the vibration (transferred from a seismograph attached
to the galvanometer - 5) as photographed on the film is
shown in Fig 4. If the abscissa of the masking parabola
2
is y and the ordinate is z then z - ky In this
-t 2
case k -1.25 and z kj x Since z is reduced N
times on the film,..(Pl)
YZ
ki12 P-
The value of Y of the apparatus is equal to 8 x 10-5
(in CGS system). The electric circuits of the apparatus
are shown in Fig 5 and the separate unit which integrates
the expression:
Card 4/6

SOV/49-59-4-13/20
A Seismic Energometer t
S (~2 * *2 * ;2 cm2
PC v )dt erg/-
0
is shown in Fig 6. The integration is done by determiring
.the dark area on the film (4 in Fig 6) by meaiis of the
lamp - 1, condenser - 2, and the alit - 3. The film is set
in motion by.-Reans of the motor - 5. The light, through the
objective -6 . falls on the photocell g nerating the
t 2
current which is proportional to the value S v dt As
0
an example, the results of an earthquake in the Philippines
on September 24, 1957, are given, as measured by means of
this apparatus: v2 = 12.2 x 10-6 Cm2/see2
v dt - 2.2 x 10 -4 cm2 /see
These values, as obtained from the seismogram SVK, are as
Card 5/6

SOV/49-59-4-13/20
A Seismic Energometer
follows: t
v2 . 29.4 x 10-6 c12/sec2, v2dt - 53 x 10 -4 cm2/sec
The difference was due to the smoothing effect of the curve
on the seismol3ram. There are 6 figures and 9 references, of
which 7 are Soviet and 2 are English.
ASSOCIATION: Moskovskiy gosudarstvenn;~y universitet im. M. V. Lomono-
sova(Moscow State University imeni M. V. lomonosov)
SUBMITTED: January 28, 1958.
Card 6/6

GOLITSYN, Boris Borisovich, skademik; BORCHKOVSKIY, V.1%, prof., otv.red.Il
tome; PREDVODITALET, A.S., otv.red.1 tome; GORSEMOT, G.P.v prof.v
red.; KIRNOS, D.P., prof,, red,; SAVARENSKIT, Te*Fej profes red.;
WYN M. TA, A.T., kand.nauk, red.; _VHSHUAK
QV,_I.V._, kand.nauk.
red.; LEVITSKAU, A.Y., kand.nauk, red.; LIMEN, N.A., kand.nauk.
red.; FILIPPOV, L.P., kand.nauk, red.; MAR , D.A., kand.nauk, red.;
SZM, D.M., red.isd-va; KASHIMA, P.S.. tekhn.red.
(Selected workal Izbrannye trudy. Koskva. Izd-vo Akad.nauk SSSR.
Vol.2. [Seismology] Saiamologiia. 1960. 489 p.
(MTRA 13:12)
1. Chlen-korrespondent AN SSSR (for Pradvoditelov).
(SAGM01067)

.73. ~360 (/6 Ild
AUTHORS: Belotelov, V.L.,
Feofilaktov, V.D.
28597 Z/023J61/000/004/002/003
D006/D102
Zhilyaov, I.I., Veohnyakov, 1F.V., and
TITLE: Seismic ener6y meter
PERIODICAL: Studia geophysica et geodaetica, no- 4, 1961, 361-363
TEM The paper presents some results of the authors' studies on the mea-
surement of the seismic-wave energy. Ass;!ming that both the kinetic and
potential energies are equal, they found that the density of this energj,
as well as the seismic en,~.rgy passing through the observation point, can be
determined by the following formulas:
V2, and accordingly ecl V2 dt
where e Is the density of the medium, v the velocity of oscillations of an
incide~.t wave, c the velocity of energy propagation, and 'C the durt..tion of
Card l/-4

28597
t/02 61/000/004/002/003
Seismic energy motor D006XD102
oscillations [Abstracterts note: t not exDlained:.] The authors designed a
recording seismic energy meter which permit2 the recordin7 of the square of
v and makes possible the determination of '~ Idt. The energy meter consists
of a velocity meter and a function converter. The purpose of the function
converter is to convert V into V2 or into some other convenient function,
e.g. log V. A schematic diagram of the instrument is shown in Pig. 1. A
lamp base with a projection lamp (1), a condenser (2), a mask (3) and a pro-
jection lens (4) are assembled in the tube of the light source. The light
from the source is reflected by the mirror of the galvanometer (5) and reach-
es the slit (6) of the receiving unit. A film (7) is just behind the slit.
For squaring 7 the mask has the form of two similar parabolas with a common
apex. When the galvanometer is not in action, the parabolas' reflection is
disposed symmetrically to the slit and the latter is in full light. When the
galvanometer oscillates, a part of the slit is obscured. The ordinates Z of
the obscured part of the alit are proportional to the square of the y-axis.
The film is moved by tape-moving mechanism. When the galvanometer oscillat-
es, the obscured part of the mask reflection more or less covers the middle
part of the slit. As a result of this a strip of light of variable width
Card 2/4

.25597 Z10231611000100410n,21003
Soismic enerey meter D006/11102
appears on the film after it has been developed. When the ask has the form
0i a parabola, the width of this strip in proportional to . When it has
the form of a logarithm, the ridth of the atrip is proportional to log ~;.
Tho area of tho light strip in determined by ~eane of a; planimoter. A method
of -rocessing the obtained data is given for the surface waves yieldizic the
equatior
V2 dt dt + 17 2dt + ;r 2dt
vN2 E z
where 11, E, Z are indices of the displacement oomponehts on the free surfac
There are 3 figuresq 1 table and 5 references: 4 Soviet-bloc ani 1 non-Sov
iot-bloo. The reference to the Engl inh- language publication reaJs as fol-
lows: H. Jeffreys, The Pamir earthquake of 1911 February 18, in relation t
the depths of earthquake foci. EINRA3, Geoph. Suppl., v. 1, no 2, 1923.
(Technical Editor; V. Tobyas)
ASSOCIATION: Physics Department, Moscow State University, Moscow
SUBUITT.E.Dt December 79 1960

IZ-SHO,, Aleko
The treatment of 7 cases of thromboc:rtopenia with corticosteroids.
Bul. univ. shtet. Tirane(Mjek] 2:35-42 f62.
(FURPURA, THROMBQPENIC) (PMNISONE)
I (CORTICOTROPIN)

MHOS K.
Urging more P=tensive use of national wealth for construction p. 6S
~ i
TEKNIKA, (Ministria Industri-Miniera dhe Ndertim-Komunikacion
Tirane, Vol,, 3., No. 2, Mar./Apr. 1956
SOURCE; East European Accessions List, (EEAL) Library of Congress,
Vol. 5-, No. 12, December 1956.

VESIIOVp D., inzh..-
Test in making rond, top dressing vith cold sand asphalt ccocrete.
Stroitelstvo 8 no.6-.13-17 161.

VESHOVY . inzh,l RkIEV:, Kr,., inzh.
On lie scientific application of bitumen in highway construction.
Stroitelstvo 9 no,4:27-20 JI-Ag 162.

VESHOV, Dinko. inzh.,, frutradnik; KALCHEV, Stefenp lnzh.v sutrudnik
-, .
Standard for mineral powders cn a high scientific and
technological level. Ratsionalizatsiia 13 noollt24-26 163
1. Nauchno-iuledovatelski institut po putishtata*

VESIIOV I Dinko . inzh.
Cold~laid sand-asplitilt cencrete, Avt.dor, 24 no.9:28-29 S 'U.
(1.'.MA 14:10)
(Ptivements, Concrete)

VWICv A.
Adhesion stresses of rainforced-conorete beans in the
stage of sporadic cracks. p. 1201.
Vol. 9. No. 8. 1954. TEMINA. Beograd, Yugoslavia,
SOURCE: East European Accessions List, (REAL) Library
of Congress, '701. 5, Wo. 8, August, 1956.

vM100 A.
Plastic hinges at the ends of slander brifto pillam., p 1229
Sshnikaj, Beograds Vol 109 No* 9., 3.955
SO: EMs Vol 51 No- 7. Ju4 1956

VESICS A.
Contribution to the statics of continuous bridge framess p. 1562
. TmwM,, Beogard, Vol 10., No - U., 1955
SOI EUL, VOL 5.. No., 7.. Julv., 2:956

VESINs, L.
VESIN, L. Istoricheskii obzor uchebnikov obshchei i rus!:koi geografii, izdaanykh so vremeni
Petra VeMogo po 1876 god. (1710-1876 g.). S.-Peterburg, 1876. 111, 674, iv p.
DIL: Z6001. M5
SO: IC, Soviet Geography, Part 1, 1951, Uncl.

IT.P.3 IN , L
Istoriche-Adi ob;wr ucliabnikov obilic-,ioi i ru:;.-.kA c,ijo-frafti, i'/, 111-W!"ll
so vre;-,d,,ni retra Ve:iko:~o po 18io -O'i. (1:10- ~ t"'7
111, 674) IV p. L,:
30; LC) ';oviot -.wo,'raj.ljy, 1-art 1, 1951, vllc'

1. Ustradni rentgonove oddelani nemo=ice OURZ v Hoots, prednosta
RUDr. Le Slavik.
(URETKUL CALCULI) (UROGPAPHY)

MIN, Slavojg prof. KUDr
Phenomenon of water spray from the punp " a now radiologic sign In
eardial cancer* Cesk.rente. 9 no-3tl14-116 Aug 55.
1. 1 ustrecIniho rtg oddelani nemocnice n Pmso-Kotole
(STCMCH, neoplasms,
diag.. sign of water spray from the pump-like snophago-
cardial passage in cardial cancer)

1 1- -p.! I,",; "I ;-,--- -, -1.

CZECHOSLOVAKIA/Hur-on and Animal Physiology. Digostion. T
Abs Jouri Rof Zhur-Blol,, No 81 1958, )6595.
Author Vosin, S.
Inst
.Ti tlo Duodonal Charactor of tho Motor Function of tho Scrill
Bowol.
Orig Pub: Casop. Lokarn coskych., 1957, 96, ITo 42, 1A.49-1354.
Abstract: Roontgonological oxamination of 35 pationts with duo-
donal ulcors damonostratod incroasod motility of tho
stomach and small bowol in tho majority of tho pntiontB.
Tho tonus of tho small intostino was normal in 2/3 Of
tho pationts; in tho othors it wac mostly lovorod.
Card 1/1