SCIENTIFIC ABSTRACT BULANZHE, Y. D. - BULAT, A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000307420012-2
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 9, 2000
• Sequence Number: 12
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

S/030/62/000/002/008/008
B105/B110
AUTHOR: Bulanzhe, Yu. D., Doctor of Physics and Mathematics
TITLE: Present movements of the terrestrial crust
PERIODICALi Akademiya nauk SSSR. Vestnik, no, 2, 1962, 113 - 114
TEXT: The third interdepartmental conference on the present
movements of
the terrestrial crust dealt with the importance of the present
movements
of the terrestrial crust in geology and for the forecasting of
earth quakes,
The conference had been convened by the komissiya po
sovremennym tektoni.-
cheskim dvizheniyam sektsii geodezii Mezhduvedomstvennogo
geofizicheskogo
komiteta pri Prezidiume Akademii nauk SSSR (Commission for
Present Tectonic
Movements of the Section of Geodesy of the Interdepartmental
Geophysical
Committee at the Presidium of the Academy of Sciences USSR)
from November
14 - 18, 1961 in Moscow. It was attended by experts of the
Academy of
Sciences USSR), of the Academies of the Union ReDublics, the
Gosudarstvawy
komitet Soveta Ministrov SSSR po koordinatsii
nauchno-issledovatellskikh
rabot (State Committee of the Council of Ministers USSR -for
the Coordina-
tion of 5cientific Research Work); the ministerstvo vysshego i
srednego
Card 1/3

S/030/62/000/002/008/008
Present movements of the-... B105/B110
spetsiallnogo obrazovaniya SSSR (Ministry of Higher and
Secondary Special-
ized Education USSR) and the corresponding ministries of the
Union Repub-
lics, of the Ministerstvo geologii i okhrany nedr SSSR
(Ministry of Geolo-
gy and Preservation of Mineral Resources USSR) and other
authorities,, The
Y,ork was conducted in plenary meetings and in the following
sections: (1)
geologic and geomorphologic section; (2) section of geodesy and
oceanogra-
pby; (3) geophysical section. The compilation of a map of the
present ver.
tical movements of the terrestrial crust in the western part of
the Euro-
pean territory of the USSR is regarded as a success, The
principles of the
geophysical interpretation of elastic flows in the terrestrial
crust that
were developed at the Institut fiziki Zemli im. 0. Yu. Shmidta
(Institute
of Physics of the Earth im. 0. Yu. Shmidt) are mentioned. V. P.
Shcheglov,
Corresponding Member AS Uzbekskaya SSR, dealt with the
movements of the
continents in the light of present astronomical research, It is
suggested
that international centers should be established for the
compilation of
world maps of the present movements and that the data should be
available
to the members of the International Association for Geodesy and
Geophysics.
Among others, the following tasks are suggested: (1)
compLlation of a map
of the present movements in the entire territory of the
Europenn part of
Card 2/3

S/030/62/000/002/008/008
Present movements of the - B105/B!10
the USSR; (2) development'of stationary polygons for
comprehensive resedrcl:;
(3) development of new methods for the investigation of the
motions; (,,~i)
establishment of special laboratories for the development of
methods of
astronomical determinations of the changes in the lengths and
widths for
solving the problems of the presont movements 6f the
continents-,
Card 3/3

S/030/62/000/005/006/006
B100108
U'l "0 1~' Bulanzhe, Yu. D., Doctor of Physical and
Mathematical
51 Ile 11 ~s
"7r!7 -:1: naval quartz gravimeter
1962, 138-89
~',kademiya nauk SSSR- Vestnik, no, 5,-
in the Institut fiziki Zemli im. 0. Yu. Shmidta Akademii nauk
(Inc-~itute of ?hysics of the Earth imeni 0. Yu. Shmidt of the
of Sciences USSR) the naval quartz gravimeter ['If- -r,
(GAL-P) was
6eveloood and tested. It is designed for submarines, for use
on drift ice and in the calm arctic and antarctic seas. The
sensitivity
6 o-f the -ravimeter consists of elastic quartz threads and is
i-i-lersed. in aviscous organosilicon liquid. An electric
thermostat
controls the temperature. The gravimeter indications are
recorded on a
,,hoto,-ri-~Phic film. The instrument is mounted in a Cardan's
suspension
with s.~ecial shock absorbera. Gravimetric measurements made
on the sea
-,-iith 3 - 4 instruments showed a maximum random error of
+1-5 mgl. The
sys-e:~;aiic error in the measurement range of 2-5 - 3.0 91 is
less than
Card 1/2

S/030 62 000/005/006/o06
naval quartz gravimeter B10610~
m~;l. This accuracy of the instrument is maintained for
several.months.
Data: graduation in recording 10 to 20 mgl/mm; at 25 0C the
zero shift
wit'ain 24 hours is 0.6 - 0.9 mgl? the temperature
coefficient is
2 m6-1/deE;; power consumption 50 w; the weight is 25 kg- A
small series
0~ There is
sucl! instruments is being produced at the above institute.
I figure.
Card 2/2

BUIANZHE, Yu.D. _
International classification of literature on earth
tides. Geofiz.
biul. no.22:70-74 162. OMM 15-8)
(Classification-Books-Tides)

th"ZHE Yu D - HESHCHERYAKOV, Yu.A.
Study of recent crustal movements. GeofLz.biul.
no.12:3-6 162.
1 (MIRA 16:5)
(Earth-Surface) (Geology, Structural)

BULANZHE, Yu.Db
Fifth Conference of the Representatives of European and
Asiatic
Countries. Geofiz.biul. no.1209-42 162. (MM 160)
.(Geophysies-International cooperation)

BULANZHE.
Secular variations of gravity. Geofiz.biul. no.12:74-80
162.
(MIRA 16:5)
(Gravity-Secular variations)

IWTOV, A.A.- BULANZHE Yu.D.; MAGNITSKIY, V.A.;
MESHCHERYAKOV, Yu.A.;
BLAG6VRTW-,' KS. -
Establishment of the Crimean geophysical polygon for the
study
of crustal subsurface geology and recent tectonic
movements.
rjeofiz.biul. no.12:82-84 t62. (NiRA 16:5)
(Crimea-Geophysical research)

DOLMN, Sh. Sh. and MIA=,. yu, j)s
Present state of magnetic Measurement techniques.
Title: Conference on problems of marine magnetic
surveys (held in Moscow in
April 1962.
Source: Okeanologiya, v. 3, no. 4. 1963, p. 752

GERASIVIOV, I.P., akader.ik, otv. red.;
ff~ANZH-T,._)~4,D,_, doktor
fiziko-mater.. nauk, otv. md.; M-ESHOMYAKOV,
Yu.A.,
kand. geogr. nauk, otv. red.; VERSTAK, G.11.,
red.;
GUSEVA, A.L.p tokhn. red.
[Recent crustal rovements] Sovremennye dvizheniia
zermoi
kory; sbornik stated. Fo--kva, lzd-%,o AINI No.l.
3'Q63.
382 p. (MIRA 17: 1)
(Earth-Surface)

ACCESSION XR: AT4024453 5/3010/63/000/013/0041/0042
AUTHORS: Avayuk, yu. X.; Bujanzhe, Yu. D.
:TITLEs Base gravimetrio stations in Antarctica
SOURCF,: AN SSSR. XezhduvedomstYon;V*y goofizicheakiy 1comitat.
Ceofizicheskiy
byulletenlp no. 131 196~9 41-42
:TOPIC TAGS: gravimetry, gravimoter, base station, base
gravimetric station, La
Casta gravimeter
A4PTRACT: The Mirny station has been established as the primary
base station for
all Soviet work in Antarctica. The bench markt a ooncrere alab
in the cosmic-ray
building, is at 660 33.21 S. lat., 930 00.91 E. long., and at an
elevation of
20-7 m. The value of g at this station, determined by D.
Sparkman with a La Costs,
gravimeter and tied to the value at Washington, is 982 407-4 t
2.0 mgal (on tvhe
Potsdam base). The authors have verified this value through
several Soviet
stations, checking the gravity difference between these stations
and the Ui=y*y
station on the one hand and between these stations and the
Amundsen-Scott station
of the U.S.A. on the other, and they agree with the Sparkman
determination within
3.0 msal, which they consider to be within the limits of
measurement error. They
Card. 0

ACCESSION NR; LT4024453
:tharefore aooept Sparlman's value as a preliminary base value,
subjeot to the
refinements of more detailed work. Orig. art. has: 1 table.
ASSOCUTION's- Uezhduvedomstve=y*y geofizicheskiy komitat IN SSSR
(Interdepart-
!mental Geopbysioal Committee AN SSS'D~
R.,
SMUTTED: 00 DATE ACQ.. 16Apr64 ENCLz 001
SUB CODE: AS NO REP SM 000 OTIMs 000
Card 2/?_

L 32563-66 EWT?i
~
SOURCE CODE:
AUMOR: Bulanzhe., Yg.D.; PopgX,_je.I.; Tulin, V.A
ORG: none
b
TITIE: Automatic processing of gravimetric o servations
SOUIRCE: Ref. zh. Geodeziya. Otdellnyy vypusk, jibs. 6-52.194
V60-~l
MF SOURCE: Sb. Vychisl. tehhn. v upravlenii. M., 11auka, 1964,
212-215
TOPIC T,%GS: gravimetry, gravimeter, gravimetric analysis, aerial
survey, data
processing
VMEISIATION: The Aerogravimetric Laboratory of the Institute of
the F-hysicG of the
Earth of the SSSR Acade~ay- of Sciences has developed a s~,ron3ly
d~K;ipcd g
ravimetery-',
s -Eiristed quartz glassftlireaq.'- T
based on the elastic propertie ct he meqsurerent 0f2
i9ravity acceleration is made by-thle-v-d-ri-a-tion of 'the
t7hread angle of
the force of J.
tvist. It is determined by the deflection angle of the pendulum.
The i-,Istx'xlent is
used in naval gravimetry survey on submarines and surface ships,
as well as for ex-
perimental worl-, on aircraft. The time spcnt for ~rocessina of
recordin~;s, durin--
which the effect of turbulent accelerations is excluded,
significantly exceeded the
time of observation. The special features and the conditions for
autoinatic processi
L_.Sard

L 32563-66
ACC NRi V-150111703
of Gravimetric data were studied. By observation from low-speed
submarine or surface
vessels the automatic computor has only to perforia the
operation of averagin3 the
record for a given period of time. In observation from an
airplane the functions of
the computor are more complex. Computing slipping average values
of gravimeter in-
dications or the current values of inte,-ral from the A-unction,
which represents the
motion of elastic system pendulum in time, can be considered as
a preliminary problem i
in this case. The device transforming the movement of the
gravimeter penduluz;i inLo
an analogy or code system must have an accuracy of 21-5- The
most comprehensive vray
of talldng readings is the method in which the measurement unit
of the pendulum siqing
is t'.,,e chanGe of the distance between two bloc1m, reflected
from the elastic system
speculum. Other known methods (for example the volume one) will
hardly secure the
necessary accuracy. B.U.
SIM CODE: 09
2

L-256,17-65 EVT(l) GW
ACCESSION HRt AP51DD4552
AbMaq: b~jimif~e_j Yu. D. (Doctor of pbysico-mathematical
S/0030/65/O00/O01/01o4/oio6
sciences)
(Fourth
TITL.Et Investigation of contemporary motions of the earth's crust
!interdisciplinary conference)
!SOURCE: AN SSSR. Vestnikj no. 1, 1965, 104-106
~TOPIG TAGS: geoactivityt geophysical research, (~ ~th c~rust,
earthquake
ABSTR ACT: The problem of observing the motion of the earth's crust
was diecuaged in
conference at Tallinn, October 12-16, 1964. It was
the jq
called by the Mezhduvedoms veiuW geofiziches iy -omitet pri Prezidium
Akademii nauk
SSM (Interdisci-olinar7_q_qppt~yptqpI_Co=aittee at the Praesidium of
the Acade-my of
6ie Geomorfologicheskaya komiseiya pri Welenii-'nauk o Zemle
Adademii nauk SSSR (GeomqKpholqg~cal Commission of the Division of
Earth Sciences,_
Acadew of Sciences Sisk) Geologii Adademii mak
of Sciences,__
Estonian SSR), 'j;~d Pribaltiyokaya nootektonichonkaya komisoiya
(Near-Baltic
Teoteotonic Only qualitp6tive axplanations could be ifv for a
crwt movements. An underatmuling of physicol-chemical. processes
within the earth

!A~o~aWW~ j4A Lj.VC.L %LV~%4jDf U"61&U L)A4VU QWAMV Faro- WAL -AV
I-V-- P-,F-
ties of the earth. A systematic investigation is nor under way in
various Soviet
territories, such as the Crimean polygon, Ashkhabady Kamchatka, and
other places,
with geologicalgeomorphological and geophysical tools. Observations
are made from
variations in terrestrial surface slopes and 2- to 4-meter horizontal
shifts in the
,vicinity of Ashkhabad. Plans were made in the conference to draw
compound maps of
vertical and horizontal crust movements in eastern Europe and to
prepare polygons
:for intensive geological, studies in various Soviet countrieu duxing
the forthcoming
ithree years.
~ASSOCIATIOIT: none
SUBInTTEDi 00
NO R'9F 50V 1000
ENCLs 00
OTMMs ODD
SUB CODE - ES
1h

BULANZHE, Yu.D.,, prof., otv. red.
(Apparatus and experimental methods for
gravinietric
research] Apraratura i metody
eksperimentallnykb isaledo.-
vanii po gravimetrii. Moskva, Nauka, 1965. 108
p.
(MIRA 18-3)
1. Akademiya nauk SSSR. Institut fiziki Zemli.

BULANME, Yu.D., doktor liz.-matem. nauk
Study of the recent movements of the earth's crust;
4th inter-
departmental conference. Vest. AN SSSR 34
no.1:104-206 Ja 165.
(14IRA 18:2)

BUIAN2M , Yu.D., doktor fiz.-matam. nauk
Symposium on the study of the figure of the earth held
in Prague.
Vest. AN SSSR 35 no.2:86 F 165. (MIRA 18:3)

BULANZHE, Yu.D.JS prof.
I--
Does gravity change with time? Zem.i vsel. I no.2:7-13
Mr-Ap 165.
(~ff RA :LS: 8)

BULANZHE, Yu.D., otv. red.
(Apparatus and methods for marine gravJr,.etric
observt-
tions] Apparatura I metody morskikh
gravimetricheskikh
nabliudenii. Moskva, Nauka, 1965. 132 y,. (MIRA
19:1)
1. Akademiya nauk SMR. Institut fiziki

GG GA
ACC 1-4r(-. AT6011158 SOURCE CODE: UR/31S)7/65/000/002/0338/03h3
AUTHOR: Bulanzhe, Yu. D. 5
ORG: I;nstitute of the_Physics of the Earth,__AN SSSR (Institut
fiziki
zemli AN SSSR)
TITLE: Study of the contemporary movements o--F' the earth's crust
at
permanent polygons [test areas)
SOURCEi AN EstSSi. Institut fiziki i antronomii. Sovremennyye
dvizheniya zemnoy kory. Recent crustal movements, no. 2, 1965,
338-343
.TOPIC TAGS. earth crust, geophysic research facility, gravimetry,
seismology,
epeirogeny I tectonics
ABSTRACT: Study of the contemporary movements of the earth's crust
requires multidiscipline investigations including geology,
geochemistr
geophysics, geomorpbology, geodesy, astronomy, and other
geosciences.
Of particular importance is the study of the vs.riations of
geophysical
fields vhich are the result of processes occurring in the Earth's
interior. Since large-scale multidiscipline research is very
complical
and expensive% the author proposes that studies of this type be
carried,
out at special permanent polygons (test areas) located in regions
vith
Card 1/2 - U-Ml- 550-34-2----- - - ____ - ____ -----------

ACC NRt - Aj?6017986 SOURCE CODE: UR/0413/66/ooo/010/0086/0086
MENTOR: Bashilov, I. P.; Jju.1.jn
D.; Dubovik, A. S.; Yerofeyev, V. I.;
Kevlishvili, P. V.; Kobrin, L. V.; Kogan, B, Ya.; KazImin, A.
I.; Popov, Ye. I.;
Milthaylov, N. N.; Churbakov, A. I.; Shileyko, A. V.
ORG; None
TITLE: An automatic device for determining acceleration due to
gravity on a movable
base. Class 42, No. 181833 [announced by the Institute of
Physics of the Earth
imeni 0. Yu. Sbmidt, AN SSSR (Institut fiziki Zemli AN 8SBR)j
SOURCE: Izobreteniya, promyshlennyye obraztsy, tovarnyye znaki,
no. 10, 1966, 86
TOPIC TAM gravity, electron optics, electronic equipment,
gravimQter
ABSTRACT: This Authorts Certificate introduces an automatic
device for determining
acceleration due to gravity on a movable base, using a strongly
damped,elastic gravi-
meter system. The installation contains a meter for
acceleration due to gravity,
a system of mirrors, lens, light source, two condensers and a
slotted prism. Ac-
curacy of measurement is improved, and processing of the
resultant information ia
sutomated by using an electron-optical converter wiLich changes
angles of turn of a
pendulum to digital code. This converter is made in the form of
a code mask with
lenses attached. A prism is mounted behind the lenses with
metallic mirrors and
photocells.
UDC: 531-768-08:528,026

ACC NRi AFbUl'19(Jb
1--accelerometerS 2-system of mirrors; 3--objective lens; 4-light
source; 5 and 6-
condensers; I-slotted prismj 1-el~oi~bn-optical converter; 9--code
mask; 10-
lenses; 11-photocells; 12-prism ia,* metailic mirrors
SUB CODE: 09,'081 SUBM LiTE: / Am'ay64

ACC NR% - AR6024298 SOURCE CODE: UR/0270/66/000/004/0035/0035
AUTHOR: Bulanzhc, Yu. D.
..T.ITLE: Investigation of present motions of the Earth's crust on
stationary platforms
,80URCE: Ref. zh. Geodeziya, Abs. 4.52.289
AtF SOURCE: Sb. Sovren. dvizheniya zemn. kory. No. 2. Tarty, 1965,
338-342
`f0PIC TAGS: earth crust, earth gravity, earth magnetic field
".ABSTRACT: The nature of present motions of the Earth's crust can
be comprehended onl)
by studying the mechanisms which govern the physicochernical
processes occurring in
the Earth's interior. These studies are to be made in combination
with other sci
ences, such as geology, geochemistry, geophysics, geomorphology,
geodesy, and astron-
omy. Of special importance are the studies of variations in the
geophysical fields
which, together with deformations of the crust, are caused by the
physicochemical
processes occurring in the Earth's interior. In view of the
complexity and high
costs of such large-scale operations it is suggest-ad that the
studies be made on
special stationary platforms located in geologically different
regions. As the first
step the following operations are proposed: gravimetric and
magnetometric surveys,
seismic surveys and depth sounding, determination of the velocity of
thermal currents
and magnetotelluric sounding. Next the following .3ystematic stuaies
are recommended:
1/2 UDC; 551.241
C.,-d

ACC NR: AR6024298
observation of vertical and horizontal crust motions, investigation
of defo-mations
and seismic and thermal regimes of the crust, and observation of
slow variations in,
the gravity and the magnetic field. The following platforms have
been or are being
established in the Soviet Union: Crimea, Ashkhabad,, Baskunchak,
Garm, Alma Ata, and
Petropavlovsk-on-Kamchatka. It is noted that the creation of
similar platforms in
the (hucasus, on Kola peninsula, and in the region of Baikal is of
special scientific
interest. [Translation of abstract) A. Pevuev
SUB CODE: 08

BUIASH, Mikhail Alekseyevich, kand. ekonom. nauk-
DaICHENKO V.P., kand.
~ko-n. -nai~J~, ~otv~ f~~d-.,--TUBOLEVA,
M.V.[TubO'Iieva,M.V.j, red,'
(Decisivelfactor in the development of mankind;
development and
consolidation of the international socialist economic
system]
VyrisbalInyi faktor rozvytku liudstva; rozvytok ta
zmitsnegmia
svitovoi sotsialistychnoi sisteqr bospodarstva. Kyiv,
1961. 47 p.
(Tovarystvo dlia poshyrennia politychrqkh i naukovykh
znan' Ukrainsl-
koi. RSR, Ser*4, no.4, (MIRA 14:9)
(Communist countries-Economic conditions)

BUIA SH M
In the branch of the academic institute staffed with
volunteers.
Vop. ekon. no-9:156-157 S 163. (MIRA 16;9)
1. Uchenyy sekretarl Ukrainskogo otdoleniya Instituta
ekonomiki
mirovoy sotsialisticheskoy sistemy AN SSSR, Kiyev.
(Ukraine--Economic research)
(Matual economic assistance council)

BULASHIEVA). L.K~
boundod Cuachy problem. Izv. AN Kazakh. S5-R. Ser.
fiz.-m-apt. t--ik
no.2:65-71 Ja-AP 165. (YJR.1 18-.5)

BULASHEVA, Ye.D*
Analysis of the effectiveness of therapeutic and
preventive care
based on materials of the medical-sanitary squad.
Sov.zdrav. 15 no.5
supPlameat:8-9 0 156. (KIZRA 10:1)
1. Zaveduyushchaya Stalingradakim gorsdravotdelom.
(INDUSTRIAL HYGIM
morbidity among factory workers, lowered rate In
Russia)
(VITAL STATISTICS
same)

KUZNBTSOV, Petr Vasillyevich; BUIASHVICH, D.N.,
redaktor; IARIONOV, G.Ye.,
tekhnicheskiy redaktor
[Installation of high tension distributors3 montazh
raspredelitelf-
nykh uBtroistv vyBokogo napriazheniia. Izd. Z-oe,
parer. Moskva,
Goo. energ. izd-vo, 1956. 223 p. (HLRA 9;9)
(Blectric switchgear)

KUZWSOV, Petr Vaaillyevich; SMMNOV, A.D., inzhener, redaktor;
SOWVIYFV,
P.F., Anzhener, -redaktor; BULASHEVICH, DN,,, redaktor;
VORORIN, K.P.,
tekhnicheakiy redaktor.
(InstallRtion of distributing equiPment UP to 35 kwl Hontash
raspredelitelln.vkh ustroistv naprte,zheniem do 35 kv. Moskva,
Goa.
energ.izd-To, 1957. 272 p. (Spravochnik elektromontera, No.1)
(MIRA 10:11)
(Ilectric power distribution)

BULASHEVICH, Dmitriy Ni-kolayevich; YURMOV, Viktor
Dmitriyevich;
- kOZMWYAKiN--, V.G., inzh., retsenzent;
BRAbDENBURGSKAYA. 3-Ya..
red.; LARIONOV, G.Ye., tekhn.red.
[Capacitive take-off of power from an electric
transmission line]
Rmkoatnyi otbor moshchnosti ot linii
elektroperedachi. KoskVs,
Gos.energ.izd-vo, 1959. 135 P. (MIRA 13:5)
(Electric lines)

KUZNETSOV, Petr Vasillyevich; SHIRNOV, A.D., inzh.,
red.; SOLOVIYEV, P.F.,
inzh... red.; BULASHEVICH, D.N., red.; VORONIF, K.P.,
tekhn. red.
[Electrician's handbook) Spravochnik elektramontera.
Pod red.
A.D.Smirnova i P.F.Solovleva. Moskva.,
Gos.energ.izd-vo.
No.3.[Installation of distribution devices with
voltages up to
35 kv.] Montazh raspredelitellnykh ustroistv
napriazbeniem do
35 kv. 1957. 272 p. (MIRA 15:1)
(Electric engineering)

F~LASTI,EVTCII, D.N., inzh.
Determination of parameters ax.,d operating
c'n&-,acterjs-U4-cs of
III
capacitor power takeoff systems. Trudy W E no.
20:5-43 f65
("!Tlu~ 1~):I)
Capacitor voltage transformers. Ibid.-.59-91

BULASPEVICH, G.A.,,gornyy inzbener; GORDEYEV, V.P.,
gornyy inzhener;
I_ - -----PERMYAYOV_t V.M., gornyy inzhener
Improving boring and blasting operations in strip mines
of the
Noril'sk Combine. Vzmw. delo no.47/4.-63-73 '61. (MIRA
15:2)
1. Gornometallurgicheskiy opytno-issledovatel'skiy tsekh
Norillskogo
kombinata.
(Noril'sk region--Blasting) (Boring)

M6017571 SOURCE CODE: UR/0196/66/000/001/IO45/1045
AUTHOR: Bulashevich, D.,
REr SOURCE: Tr. Vses. n.-i. in-ta elektroenerg., vyp, 20, 1965,
59-91
TITLE: Capacitor voltage transformers
SOURCE: Ref. zh. Elektrotekhnika i energetika, Abs. 11297
TOPIC TAGS: electric transformer, electronic transformer,
electric capacitor
TRANSLATION: The advantages of capacitor voltage transformers
over inductor voltage
transformers are considered, An analysis of capacitive power
selection (yield) for
measurement purposes is given. The conversion scheme is
analyzed, expressions for er-
rors are derived, and the effect of various factors on summary
error in the transforme
is described. The operating characteristics of capacitor
voltage transformers are ex-
amined and areas of application are suggested. 12 figures, 13
references.
SUB CODE: 09/
UDC: 621.314.222.8
Card

- BULLSHEVIGHP R.Ye. (Moskva).
Use of synthetic and vegetable estrogens In livestock
farming. Usp.
sovr. biel. 43 ne.2:208-223 Kr-Ap '57. (KIRA 10:6)
(STIlalIMIOL) , (STOCK AND STOCKBREbIbG)

86434
S/181/60/002/011/020/042
B006/bO56
AUTHORS: Korovin, L. I. and BZ!j~,,UgA
, "~YI;W
TITLE: Oscillation,s of the Absorption Coefficient of Tellurium
in a Magnetic Field Running Along the Optical Crystal Axis
PERIODICAL: Fizika tverdogo tela, 1960, Vol. 2, No. 11, pp.
2795-2804
TEXT: An analysis of the absorption spectrum of tellurium
single crystals
in polarized light within the region of absorption by free
carriers makes
a construction of the holeband of tellurium possible. As
already shown, the
hole band is not degenerate and has either one extromum in the
center of
the Brillouin zone or two centers symmetrically arranged on
the optical
axis (C ). Measurements of the absorption coefficient carried
out by
V. M. Orsunskiy and M. P. Lisitsa indicate that the second
probability
is more probable. The authors of the present paper study
oscillations of
the absorption coefficient in a magnetic field, which are due
to direct
transitions of electrons from the filled valence band to the
hole band.
Contrary to Refs. 5, 6, the dispersion law in the lower band
is assumed
to be not only quadratic but also linear with respect to the
irreducible
Card 1/3

4 4
Oscillations of the Absorption Coefficient S 1
-1/60/002/011/020/042
of Tellurium in a Magnetic Field Running Along BOO /B056
the Optical. Crystal Axis
quantum number of the terms. Besides, the mutual position of
the bands dif-
fers from their position in transitions into the conduction
band. This
entails an extraordinary dependence of the oscillations on
light frequency.
The absorption spectrum of infrared radiation in tellurium
single crystals
is calculated for a magnetic field that is parallel to the
symmetry axis
of the crystal. The calculations are carried out in
single-electron apprmi-
mation by the method of the effective mass. The prezent paper
consists of
two parts. Chapter 1 derives expressions for oscillations
'Without taking
account of collisions between electrons and phonons or
impurity ions. This
simplification causes the absorption coefficient to tend to
infinity at
certain frequencies. In Chapter 2, these collisions are taken
into account
by the phenomenological introduction of a half-width of the
electron levels
in the hole band. Thus, not only the position of the
oscillation peaks on
the frequency curve may be determined, but also the shape of
the absorption
peaks may be described. The results are finally discussed.
Professor
A. I.- Ansellm is thanked fordiscussions. There are 1 figure
and 7 referen-
ces: 4 Soviet and 3 US.
Card 2/3

86434
Oscillations of the Absorption Coefficient
S/181/60/002/011/020/042
of Tellurium in a Magnetic Field Running Along B006/B056
the Optical Crystal Axis
ASSOCIATION: Institut poluprovodnikov AN SSSR Leningrad
(Institute of Semiconductors of the AS USSR, Leningrad)
SUBMITTED: June 28, 1960
j
Card 3/3

AID P - 2784
Subject USSR/Chemistry
Card 1/1 Pub. 152 - 12/19
Author Bulashevich, Ye. A.
Title A new laboratory method for preparation of phosphorus
pentachloride by chlorinating red phosphorus in carbon
tetrachloride
Periodical Zhur. prikl. kh1m. 28, 4, 4-31-433, 1955
Abstract A detailed description of the method Is given. The
phosphorus pentachloride obtained contained a very
slikht amount of phosphorus trichloride and 25-40%
carbon tetrachloride. One diagram, 12 references
(2 Russian: 1930-1947).
Institution None
Submitted Jl 12, 1952

BULASEVICH, Ye. A.; TOLKAGRIN, 3, S.
Preparation of alminum oxide dihydrate. Ilast, NA
1.9 no.10.-
123-124 '64. (I-MU 17:7)

I
F C", "k, . L.
BULASHRVICR, Yu.L.
% I ~
Mapping graphitized rocks. R&zved.1 okh.nedr 23 no.2:59-60
F 157. (MINA 10:5)
l.Gorno-goologicheakiy institut Ural'skogo filials, AN
SSSR.
(Prospecting-Geophysical methods)

BIILASHEV L CH, Yu. P -
X y W t
T 7NO ORDERS AND .7ii'vPT(r%
PROrf%L*% A-D
Influence of it nutgnetic fictEl on the formfion 0( Mrs-
cmducling nuclei. Vn. 11. Bularlirvieh. J. -7N-FF
I Amra. I U. IN. 113. It. is, imi-7111 il ).-rheo- -31
it, tlt~ BrIpVtMoilUttlill;
Pli,es withill tile 14-AIY RK ft trilem haviog h sudam
xvith respect to (Ire winsupertomfudivig plinw., and then
c.Ak--. the Tnte of gtowilt of tire nuclei. For fig nt 4"K.,
tile t(Iiiii. rndius is 1.5 X 10-6 cm. and the surfnve Irnsion
0A'-' X IU- I crg./,rq. Col. Hathionun-

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Geophycial Section of Ylining-geological Inst.t.,
Ural Branch of the
Acadeqr of Sciences.

The thetity of the
interptetation of
titdicimictive stionis
ties.
YUJI"Bulahe'.-jell. 1:1,
q. Ak'Id. Aq,d S, 1 .1 R
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10, 46i) Che- Zent,
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USM/Geological 'Prnspecting Mar/Apr 1948
Petroleum - Prospecting
Coal
"Use of the Theory of Neutron Core Sampling
by Elec-
trical Means in Prospecting for Oil and Coal
Deposits,"
Yu, P. Bulashevich, Mining-Geol Inst,
Sverdlovsk,14 pp
"Izv Akad Nauk SSSR, Ser Geograf i Geofiz"
Vol XTI,
NO 2
Discusses method for calculating the
retarding effect
of fast neutratis. Delivered characteristic
of the
rook during neutron core sampling depends on
the size
of the neutron zone, and can change until it
assumes a
reverse characteristic. Presents a more
effective
43.1,43
'USSR/Geologica,1 Prospecting (Cmtd) Mor/Apr
1948
method of using neutron core sampling In
surveying
fcr petroleum and coal deposits. Submitted
by Aoade-
mician L. S. laybenzon, 28 May 1947.
43243

YIII PO
USSR/Geopbysics - Carottage, Neutrons MaY/Jun 51
"Theory of the Neutron Carottage," Yu. P. Bula-
shevich, Mining-Geol Inst, Ural Affiliate, Acad
Sci USSR
"Iz Ak Nauk SSSR, Ser Geofiz" No 3, pp 30-37
Derives soln for eq of diffusion of thermal neu-
trons taking into consideration stoppage of fast
neutrons of source. Constructs curves showing
distribution of neutron density around source for
pumber of minerals and rocks that characterize
presence of petroleum deposits. Discusses prob-
lem on conversion of neutron diagram in connec-
tion with variation in size of the sonde. Sub-
mitted 5 Feb 51 by Acad 0. Yu. ShmJdt. 186T41

Ya
wo/Geophysics - Anomalies
Card 1/1 Pub 45-11/18
Author : Bulashevich, Yu. P.
Title : Anomalies in the case of stratum-shaped disturbing bodies
Periodical : Izv- AN SSSR. Ser. geofiz. 270-274, May-Jim 1955
Abstract : In the interpretation of anomalies of various force
fields in geophysical
prospecting widespread use has been made of the method of
matching, based
upon geological data and observed structure of the field without
any as-
sumptions as to the form of the body (stratum, ellipsoid,
cylinder, etc.).
In the present work the author analyzes the same mathematical
expressions
for areas where the form of the bodies are assumed beforehand to
be stratum-
shaped, without the nature of the anomaly being made definite;
i.e. with
definite limitations being placed on the type of anomaly, but not
an the
nature of the field. Eleven references; e.g. Yu. P. Bulashevich,
"The
relation between electrical and gravitational anomalies," Trudy
Gorno-geol.
in-ta UFAN SSSR (works of Mining Geological Institute, Ural
Affiliate,
Academy of Sciences USSR), Symposium'NO 1, 1950.
Institution: Ural Affiliate of Academy of Sciences U3SR,
Mining-Geological Institlllt(!
Submitted : may 16, 1954 ~

BUIASHEVICH, TV.P.
WMWAWA-MWM""d"ftWMMW
Calculating Induced potential fields for spherical
ore deposits.
Isv.AN SSM.Ser.goofis. no-5:504-512 My '56. (MLRA 9:8)
1. Uralskly filial Akademil nauk SSM,
Gorno-goologicheakiy
institut.
(Ore deposits-Zlectric
propertion)(Prospecting--GeophysicaI
nethod.9)

BULASHIVIG# Tu P.; ZARHARCHUKO, V.F.
Z!,I-a
]Potential of a nAturally polarized ellipsoidal body.
Izv.Aff SSSR
Ser.geofiz. no.10:1174-1181 0 1566' (MLRA 10:1)
1. Uraltakiy filial Akademii nauk SSSR
Gorno-geologichaskiy institut.
(Torrea.trjaj electricity) (Ore deposits)

6u~jj S~l C-V,C,14 YU P
SUBJECT USSR / P~YSICS CARD 1 / 2 pA - 1676
AUTHOR BULAEVI C, J`U. P.
TITLE On the Self-Absorption of a Radiating Sphere.
PERIODICAL Lrn.teohn.fis 11.6, fasc.11, 2599-2600 (1956)
Issued: 12 / 1956
The derivation of the correction for the self-absorption of a
radiating sphere,
which was given by M.A.BAK et al. Zurn.techn.fis,26,379 (1956)
can be consider-
ably simplified. The density of the radiation cl~r_rent impinging
at the point A
and originating from a volume element dv - 2nR 2 sin 0 d 9 dR has
the shape
dI = (Ke-~1(R-Rj)/R2) cos 0 dv. If this formula is integrated
over R from R 1 to
R2 and within the corresponding limits over 9, one obtains
arc sin a
I (2nK/4^) f 'r sin 9 Cos 9 1 1 -e_~~ (R2-RI) I dQ. One obtains
r-09-~ 2,
R2 Ri = 2r a and here it applies that a fl - (a/r)2, where a
denotes the radius of the sphere. With the substitution x = oos 9
there follows
1 2 2
_'7
PjirVx a
I - (2uk/~ e 6- - )x dx. The computation of this interval is
carried out elementarily and results in:

V
Zurn.techn.fis,26,fasc.11, 2599-26oo (1956) CARD 2 2 PA - 1676
(3/4 a) 1 - 1 2 a]~
0 36"A 2 f 2Qa)2 + 2,u a) 9" 6 Here 10
- (4/3)na (K/r ) denotes the density of the radiation current
in the case of
lacking self-absorption.
The computation of the radiation intensity j which
corresponds to measuring
with a punotiform indicator is reduced to the above mentioned
integral formula
for I, but without the factor x in the function below the
integral sign. This
integral is taken in finite form in the special case of the
spherical surface
j/jo 2 1a -2,," al.
2nKa d notes
Here Jo e t e intensity in the case of lacking
self-absorption.
The latter formula at a --) oD goes over into the known
expression j - 2nK
for the radiation intensity on the surface of a radiating
half-space.
INSTITUTION:

3(6,10); 9(6) PHASE I BOOK EXPLOITATION SOV/1924
Akademiya nalPSIS"S)"RI. Ural'skiy filial. Gorno-geologicheskiy
institut.
Geofizicheskiy sbornik, no. 2. (Collected Papers on Geophysics,
Nr. 2.)
Sverdlovsk, 1957. 207 P. Issued also as Its Trudy, VYP. 30
Errata slip inserted. 2,400 copies printed.
Resp. Ed.: Yu.P. Bulashevich, Doctor of Physical and Mathematical
Sciences; Tech. Ed.: L.A. Izmodenova.
PURPOSE: This collection of articles is intended for field geo-
physicists and exploration party leaders.
COVERAGE: These articles discuss many new techniques and some
theore-
tical considerations involved in gravitational, magnetic seismic,
electrical and gamma radiation exploration methods. In 4 articles
V.N. Ponomarev discusses various aspects of magnetometry;
N.I. Khalevin - the study of elastic wave propagation; and
G.M. Voskoboynikov - gamma radiation. Extensive bibliographies
accompany each articles.
Card 1/5

Collected Papers (Cont.)
TABLE OF CONTENTS:
SOV/1924
Rodionov, P.F., V.D. Kokourov. Application of a High
Frequency

Electromagnetic Field in Exploration for Sulphide
Deposits in

the Urals
3
Rodionov, P.F., Application of the
Non-grounded Loop Method

in Search for Pyritic Deposits in
the Urals
24
Kokourov, V.D., and A.A. Bashmakov. Field
Vacuum-tube Volt-

meter
32
Bashmakov, A.A, and V.D. Kokourov.
Alternating Current

Generators
36
Kokourov, V.D.
Low-frequericy Field Comparator
42
Bulashevich, Yu.P.
Similarity Principle in Modeling the

Potartzattuff-of Ore
Bodies Caused by Current
53
Gelfand, I.S. Alternating Field
of a Vertic al Electric

Dipole in a Bedded Medium
60
Card 2/5

Collected Papers (Cont.)
SOV/1924
Gelfand, I.S. Alternating Field of a Horizontal Frame in a
Bedded Medium 72
Ponomarev, V.N. Magnetization Curve of a Sample of Magnetite
of Contact-metasomatic [Replacement] Origin 84
Ponomarev, V.N. Portable satuzation magnetometer 87
Ponomarev', V.N. Application of Magnetometry in Exploration
for
Pyritic Deposits in the Southern Part of Zaurallye 93
Ponomarev' V.N. Temperature Effect Problems in Magnetic
Compensation Devices 97
Bulashevich, Yu.P. Magnetic Fieldata Horizontal Layer With
NonIfffIrDrm-DI-s-tribution of Magnetic Minerals 100
Orlov, G.G. Nomogram to Determine the Depth Position of
Bodies by the Points of Intersection of Potential Deriva-
tives Curves Taken at* Various Elevations 105
Card 3/5

e
te.,Medlat
tyle Ila ,.qes latlori 116
'astle 0 07
't 'Ossl~ss, .-re
0 ted ,qe ol~S
~ 'Opass-
'?ap its of Of '? 1,acted oa-LDe
Go, Ikeel y..ef ~Or 10"L
_1ected -g .1 - 'LOCI lt-5,es O~ tyke 10r, Is Ila
-LeVl" -4all -qe tlo'(1 -Lorat e '3-ra tloa
,,,a,a I-ater Ilea Ila S'-'-P of
N99 Tcjj a slope- -CopaSa
sea teTTL j .q e 1-33
.4 la tyle S 'atle
I I'a tyie 'Fla 13. StA
J.,hoc 01, O~ Y, , ,.,
V~e %P os-Its 0 C S tije -Fla "40,
-DeP Ve 0 ti"S
-g.1 - OTIVIat , 140-5-aTIIIS
i_e-0-f" ,tar j Oble'm 0 S, It tj'as the
,,Ipe jk.1 - ?r ii III jva - 00ast-clic
-ql~v O~ ?,001CS d O~ Ket)~Iod lo aa
jketllo as tv
'bajeloc olame
e ltj Syiovt Sectlo ,ate
I tae a
jl* Of oj~'~ -~a tjo
1101 les NpPT pad,'
'13~sa" TOL ar lolis '8016
130'a -jxi -? - t O~
Ta-,
,ste 0 .ate S the 14edLVO
YOV COVBP_ dlo
0,00vl ~
S'Y- rajas 1: or -aeO'as
L~-Yo-r!, ~Lomo
-q0 Se

collected Papers (Cont.) SOV/1924
Karasik, M.A., and V.A. Bugaylo. The Genetic Relationship of
Magnitogorskiy Granitoid Massif With the Eruptive Rocks of
Basic Nature 173
Timofeyev, A.N. Computations of the Interpretative Grids for
Geophysical Surveys 178
Timofeyev, A.N. Graphic Interpretation of Geophysical
Anomalies by the Method of Tangents 189
AVAILABIE: Library of Congress
Card 5/5 MM/ad
6-15-59

BULAS7.M,Tftv.Ttx.P.; VOSIOBOINIKOV, G.M.
in Ural coal mines and the possibility of
coreless boring of a pprtion of exploratory
bersholes. I2,r. A
SSSR. Ser.geofiz. no.1:109-11Z Ja 106' (MIRA 10:3)
1. Ural'skiy filial AN SSSR. Gorno-geologichookiy
institut.
(Arespecting-Geophysical methods) (Coal geology)

SOV/169-59-3-2292
Translation from: Referativnyy zhurnal, Geofizika, 1959, Nr
3, pp 33 - 34
(USSR)
AUTHOR: Bulashevich, Yu.P.
TITLE: The Analogy Principle for Simulating the
Polarization of Ore
Bodies by Current
PERIODICAL: Tr. Gorno-geol. in-ta, Urallskiy fil. AS USSR,
1957, Nr 3c),
pp 53 - 5
ABSTRACT: The author shows that it is impossible to perform
an unambiguous
distinction between ore-bearing and rock anomalies when
using
the conventional%l'e'lectrical 2rospecting methods, since
the
anomalies of artificial constant and quasiconstant fields
are
connected only with the difference of the specific
resistances
and do not depend on the current passage mechanism. It is of
great importance that a deposit behaves In a current f1e2d
as
an ideal conductor, beginning with some higher conductivity
of
the deposit compared to the conductivity of the enclosing
rocks.
Card l/ 3 In this case, the intensity of the anomaly is
determined only

SOV/169-59-3-2292
The Analogy Principle for Simulating the Polarization of Ore
Bodies by Clirrent
by geometric factors - dimensions of the ore body, its shape
and depth of
occurrence, but not by the degree of difference in electric
conductivi-~y.
Boundary values of the anomaly correspond to comparatively
small differences
in conductivity. Thus, high values of electroconductivity of
pyrite occurrences
are not the basis for a reliable distinction of ore
anomalies. The author dis-
cusses the influence of the polarization in the zones near
the electrodes on
the observation results obtained by the method of induced
polarization. A
criterion is developed for the analogy between results of
t1he simulation and
field investigations. This criterion will be l/ P a - a -
)o/Jres - Const
for spherical deposits, where a - resistance of the
surrounding medium;
a - radius of the deposit; Jo current density in the normal
field; J,es
density of the residual discharge current. The Introduction
of linear
4- +
dimensions of the object into the criterion is connected
with the fact tha.
the anomaly from a sphere is proportional to the volume,
1.e, a3, in the
residual field in the zones Around the electrodes, while the
field of Induced
polarization is proportional to the surface area. The
assumption of an intense
polarization of the zones around the electrodes and their
discharge after
Card 2/3

SOV/169-59-3-2292
The Analogy Principle for Simulating the Polarization of Ore
Bodies by Current,
switching off the feed current is of essential importance
for the mallogry
criterion. Special experiments under laboratory and field
condittions- are
recommended for checking the criterion developed and also
for explainLng, the
influence and extent of polarization zones arourd the
electrodes.
A.A. Smirnov
Caz~d 3/3

BUUSHZVICII, Yu.P.
.134ajAl -~- -.:- - , , , ~
:.-,A~:'
Magnetic field in hOriZODtal strata with
';-Iete-.-;-)Irranou-s distribution
of' magnetic minerals. Trudy Gor.-greol. in~?t. ,
~-.30tlOG-I,G4 157.
(I,fIRA 11:7)
(~Iagnetic fields)

SOV/169-59-2-1253
Translation from% Referativnyy zhurnalj Geofizika, 1959, Nr 2, p
35 (USSR)
AUTHOR- Bulashevieh, Yu.P.
T 17-M - The Equivalenc~e of the Vol'Ime and Surface Radiation
PERIODICAL: Tr. Gorno-geol, in-ta..' Uraltzkiy fli, AS USSR,
1957, Nr- 30, P-, ~146 - 153,
ABSTRACT-, The anthor PrODOSeS the. method of zzubstitution of
the equivalsnt surface
density (ESD) ior the volume density of 7- -emitters to simplify
the
coqputl-ation of Intensity of the I -emissionlrom volume
sources, A
formula connecting the magnitude of volume density with the ESD
is derived
for an emitting stratum covered by an Inactive lkyer. The
formalae, ar-,
cited for the case of an emitting stratum of unlimitled.
thickness, out-
cropping on the surface, and of an. emitting thin layer,
Examples are given.
for computing the intr~.,nsfty of T -emission from -ar, =11mited
barld, fro-M a
semiplane, and from an element of a circul~Lr- ring. The author
points cut
that the results are best in the ease of lirn'.tsd bodies, when
the volume.
density Is substituted by the ESD. It is assumed for deriving
the formul'a'e
and for c-31cul.ationS 4 at-. the original. and resox-ded
emissio~is are monc-
,,h
Card 1/1 chromatic. A pedcn~v

.1 rl C 1.
'11c". L'.4 I,c L cli C.
uy Y.
Report pre-~-ented at 2T)d ij', AtCr-.S--f*r~1-l-c-.-,--'-~

SOV/.49-58-1l-'11/18
AUTHOR: Bulashevich Yu P..
TITLE: Method of Determination of EmanELting Coefficient of
Rocks in Natural Strata (Metod opredeleniya koeffitsi~enta
emanirovaniya gornykh porod v yestestvennom zaleganii)
PERIODICAli: Izvestiya Akademii Nauk SSSRI, Seriya
Geofizicheskaya,
1958, Nr 11, PP 1383-1388 (USSR)
ABSTRACT: The concentration of emanation in the pore air
depends
not only on the radio-active elements but also on the
coefficient of emanating and porosity, or more exactly
on their relationship. Therefore, the emanating fields
should be classified according to their Radon (or Thoron)
content and the emanating coefficient. The emanating
coefficient should be determined in the conditions of
natural stratification of rocks, This can be done by
means of combining the emanatioh and gamma intensity
measurements pei~formed for the same points,, The method
is simple, The pore concentration of emanation depends
on the relative emanating coefficient and the percentage
of initial radio-active element, while the intensity of
gamma radiation depends only on content, From two
equations describing this relationship, it is possible
Card 117

SOV/ 49-58-11-11/18
Method of Determination of Emanating Coefficient of Rocks
in
Natural Strata
to exclude the content in order to find the emanating
coefficient, To find the amount of concentration of
emanation the equations (2.1) for Radon, R., can be used
(Ref 2) where cLR, concentration coeff-icient of Radop-7
I - porosity, volume weight, q - content of
radium, If the uran P content is substituted, the
equation (2.2) is obt~yned. If the emanometer*is
scaled in emans, the initial electric curren't iRn
gives the value of concentration, i,e,.
iRn = CRn,
When the amounts of Thoron and Radon become eaual, this
current for each element can be expressed as
iTn eX Th -A L (k Tn + kThA);
Th
Rn eXU -AN kRn
U
Card 217 therefore, the transition coefficient can be
calcill-A

OOVI 4 9-58-11-11/18
blethod of Determination of Emanating Coefficient of Rocks in
Natural Strata iTn ,
as k = .:-- = 0.8.
'Rn
The assumption is made in this case that all the ions
from the decomposition of Thoron remain in the camera of
the emanometer, To find the relation of the initial
current i Tn to the content (in percentage) of Thoron
in the formula (2.2). the
concentration of Thoron is
of ionisation (Ref 5) from
defined:
C kRn
Tn ~ kTn + kThA
i,q,(2,3) is used, The actual
found by eliminating the factrr
iTn 'd the new equation
0,42i
Tn 9-In
In order to determine the emanating coefficient, the
percentage of thorium. and uranium in formulae (~.2) and
(2.3) should be substituted by the intensity of gamma
radiation. Thus, the equation (3.1) is obtained where
A~ B and C - conversion coefficients (Table 1),
II - residual ions. The determination of the*emanating
Card 3/7 0

SOVI 49-58-11-11/18
Method of Determinati.on of Emanating Coefficient of Rocks in
Natural Strata
coefficient in practice depends on the various conditions.
The most common case is when only one radiating element
is -present. If I = APU (4.1), then from (2.21 arid (4,1)
the relation (4.2) is obtained for uranium. Similarly.,
the relation (4.3) is obtained from (2.3) for gajwna
radiation of Thoron, By using the formulae (4.2) and
(4,3) it is possible to find the 6ifferent emanation
characteristics, For instance, three types of Radon
anomalies can be distinguished by taking account of the
emanating coefficient
O'Rn greater than I (slow emanation),
TI
greater than 5 (Radon aureole) and less than 1 (increased
initial radiation). The first case of Radon anomaly is
found in the layers of granite-gneiss and graphitic rocks.
The measurements were made by the author (Ref 11) of
ionisation currents and of the intensity of gamma
radiation and some of the results are a-iven in Table 2.
According to this data the relationship of thorium and
Card 4/7

~3OV/ .49---58-.11-11/18
Method of Determination of Emanatin- Coefficient of Rocks in
Natural Strata
uranium in granite-gneiss rocks could be expressed as,
O'Rn ip
- O~8 'Rh ja
'Rn PU ITn
Card 5/7
i~e. (xRn ly a-T.-
The graphitic-carbonaceous-silicon slates are character-
ized by the high emanation of gamiria radiation, the
ratio of aR]a/A being equal to 3~4, The emanation of
Thoron in this case is small, sim~~lar to granite-gneiss
rocks, In order to determine the emanatinG coefficient
of exo-contact rocks in the granz--te intrusive layers,,with
the variable concentration of Radon showing some
correlation to the gamma intensity, the measurements were
carried out by means of the two lines method (L-1 and L-2),
The results of one line (L-1) are shown in Fig,1
(1 - ionisation current of Radon, 2 - Thoron.. 3- gamma
intensity), In order to determin'e the distribution of

60VI 49-5S-11-11/18
Method of Determination of Emanating Coefficient of Rocks in
Natural Strata
emanation with depth for the maximum points of C Rn'
two holes, 4 and 4.5 m deep, were dr-Jiled
(Sh-l. Sh'2). The mean values of the ionisation current
and gamma intensity are shov%,n in Table 3, It is possible
to determine the relative emanating coefficient of Radon
at the maximum point by the application of the whole
value of gamma intensity, Thus. for the point 2 of
L-1 (Fig,l) with volume weiGht -2 g/cm3 the ratio
aRn/11 = 1,,7 is obtained, It is possible to calculate
this coefficient for Sh-l b.Y takinG the mean concentration
of Radon and the gamma intensity re3ative to L----1 (Table 3),
The surplus of Radon will be 16f--/Cl emans and of gamma
intensity 171 mkr/hr,, Substituting these values into
the formula (4.2) the relative emanating coefficient of
Radon for Sh-1 was found to be 2.1, Similarly, the
emanating coefficient can be calculated for Sh-2 and L-2.,
Gezerally, it can be stated that the measurements show
that the relative emanating coefficient represents a
constant value dependent on the kind of rock, When the
calculation is based on Radon, the 3oeffici.ent is equal
Card 6/7

8OV/ 49-58--1i-11/18
blethod of Determination of Emanatini~ Coefficient of
Rocks in
hatural Strata
to 0.24 for bituminous granite- Ene is s, 3.4- for granite-
carbonaceous-silicoa slates and l..8-2,1 for granite-
--neiss in exo-contact granite intrusion layer,
There are 3 tables, 1 fi6ure and 1l references,
all of which are Soviet..
ASSOCIATION: Urallskiy filial AN SSSR,Instit-ut -eofizik-i
0
(Ural Branch of the AC.Sc. USSR, Institute of
Geophysics)
SUE~1ITTBD,,, November 22, 1957
Card 7/7

VP
ON
14 '1
Ali,
Ali
a All
I I'maii -lit
D.21 -111W

21(8)

AUTHORS:
Bulashevich, yu. P., Kartashov, N. F.
SOV/89-6-5-23/33

TITLE:
On the Shifting of the Equilibrium Between
Radon and Its

Decay Products in an Air Current (0 advige
ravnovesiya

mezhdu radonom i produktami yego raspada v vozdushnom
potoke)

PERIODICAL:
Atomnaya energiyal 1959, Vol 6, Nr fl, PP
584-585 (USSR)

ABSTRACT:
In a mine in which emanating rock is
found, the exhaust air

contains radon and its decay products. The
shifting of equi-

librium is calculated. Radon concentration may
be calculated

o--
from Y 0 + lo - " - Q (1), where q denotes the
4

xx
S

quantity of radon yielded per unit E.,rea in the mine, v - the

convection velocity of the exhaust a.irl c - radon concentra-

tiong A - radon decay constant, 1 - perimeter of the excavation,

S
- the area of the excavation. The exhaust air is assumed to

move
in the x-direction. If c - 0 ar.d x = Ot

c a
11 - exp(-~ x)] is
calculated from (1). As t

A
v v

(time during which the air volume
element passes over the

Card 1/3
excavation), the following is
obtained for the

On the Shifting of the Equilibrium Between Radon and Its
SOV/89-6-5-23/33
Decay Products in an Air Current
RaA-concentration (in analogy to the solution of equation
(1)):
do A 0 [1 - exp (-At)] . The RaA-concentration,
dt A A
which is in equilibrium with Rn, is obtained from
1 exp(-At) AE1 -exp(- A At)l
A = Q 9~ 'A - + - -A A( ~ 1) 1 - Thus, as shifting
coefficient 'qA for RaA equilibrium the following is obtained:
-exp(_~ t)
A Li A -rresponding coefficients
A _~ - A-A 11- 71 .The co
77:7 + exp(-At
for RaB and RaC are derived in the same manner, and all three
are recorded in form of curves in degendence on t (0 to 60
min).
The sum coefficient 'IA+13+C is formed graphically. If the
YI-values and Rn-concentration are known, it is possible from
ci ='qic VpC/1 to calculate the concentration of any decay
Card 2/3 product. In the case of nonuniform emanation,
calculation of

On the Shifting of the Equilibrium Between Radon
SOV/89-6-5-23/33
and Its Decay Products in an Air Current
'Q is more complicated. At the air exhaust outlet a higher
concentration may be expected than in the case of a homo-
geneous emanation. There are 1 figure and 5 references, 3 of
which are Soviet.
SUBMITTED: January 6,1959
Card 3/3

S/049/59/000/12/007/027
E032/E591
AUTHORS. Bulashevich. Yu. P,, and Khayritdinov,. R.K~
TITLE- On the Theory of Diffusion of Einanation3 in Porous
Media&
PERIODICAL: Izvestiya Akademii nauk SSSR, Seriva geofizicheska-%ra..
1959, Nr 12, pp 1787-1792 (USSR)
ABSTRACT: The present paper examines the basic equati.=s of 'Iha
theory of diffusion of radioactivf! emwations In
porous media, and gives a general deri-vation of the
diffusion equation, taking conve.:,I.ion into account
The diffusion and convection curronts are defined
Eqs (2.1) and (2.2), where c is the concentration of
the emanation in the pores, D is the diffusion
coefficient, I is the porosity, Q ).s the -zate of
liberation of the emanation into the pores per un:Li-
volume of the medium, % is the decay C-:)nstant of the
emanation and v is the velocity of coiwec t -i ve
transport,, The rate of charige D1' Lhe amount, of the
emanation in the pores in a volumc. I c---n then be
-written in the form given by Eq By transform-iiig
j
Cardl/4 the surface integrals into voltime iiitegr-als and equat

S/049/59/000/12/007/027
E032/1;591
On the Theory of Diffusion of Emanations in PDrous bledia
the integrands, one obtains Eq (2.~), In the case of a
uniform porous medium, and with v = const, Eq (2~5)
is obtained. Eqs (2.4) and (2-5) also describe the
case where the pores are filled by a liquid rather than
by gas. If surface phenomena are excluded, then on the
boundary between two porous media, the total diffusion
and convection current density must be continuous and
this is expressed by Eq (2.7). The normal velocity
components on the separation boundary are subject to
special boundary conditions. In particular, in the
case of filtration of an incompressible liquid, Eq (2.8)
must be obeyed. Bearing this equation in mind, the
boundary condition (2-7) may be rewritten in the form
given by Eq (2.9). If the diffusion of the emanation
can be neglected in comparison witli the convective
transport, then D 1 = D 2 = 0, and the degree of
equation (2-5) is reduced. Accordingly, Eq (2,9) gives
a single sufficient condition on t'he separation boundary,
namely, the condition given by Eq (2.10). In the
Card2/4 absence of convection, Eq (2.9) leads to Eq (2.11)~ 0

S/04()/59/000/12/007/027
E032/1591
On the Theory of Diffusion of Emanations in Porous Media
In this case, Eq (2.10) becomes an extra requirement,
It is shown that this extra condition is satisfied in
the case of a stationary distribution of the emanation.
In the case of stationary diffusion, Eq (2.5) leads
to Eq (2.12). The above equations, namely, Eq (2.12)
and the boundary conditions, may be rewritten in the
K
form given by Eqs (2.12) to (2.15), where c ~c and
D D/1- In the major�ty of papers on the theory of
the emanation method, use is made of Eq (2.13) and the
boundary condition (2.15) However. the condition (2.14)
is usually replaced by c 1 = C 2 and no indication is
given as to which concentration is being considered,
i.e. volume concentration or pore concentration. To
check this point, an experiment has been carried out
and it was found that if the dimensions of the micropores
are greater than the mean free path of the diffusing
atoms of the emanation, then the concentration in the
pores is continuous across the separation boundary of
Card3/4 two media with different porosity. It is pointed oU0,

sl'049/59/000/12/007i"027
E032/E591
On the Theory of Diffusion of Emanations in Porcus Media
that the numer: ical results obtained by Budde (Ref 8)
are incorrect because his calculations were carried
out on the basis of equations of the type given by
Eq (4.1) with boundary conditions (4.2) and (4,3).,
It is shown, however, that under these boiindary
conditions the correct diffusion equation is
C - ~a C = 0.
D
The experimental work reported in the present paper
was done on builders' sand with a density of 1.110 g/cm-),
porosity of 39% and humidity of 4%. The diffusion
length was found to be 80 cm and the diffusion
coefficient 0.54 x 10-2 cm2/sec.
There are I figure and 10 references, 9 of which are
Soviet and 1 German.
ASSOCIATION: Urallskiy filial AN SSSR Institut geofiziki
(Ural Branch of the Ac.Sc., USSR, Institute of Geop~hjsi
SUBMITT D: April 4, 1959
Card4/T

s/o4g/60/000/02/006/022
E131/E459
AUTHORS,. Qlashevich, Yu.P. -, and Shulyatlyevv S.A.
7'-'--"-'- "
TITLE. The Optimal Conditions of Activated Continuous Prospecting
PERIODICAL~Izvestiya Akademii nauk SSSR~ Seriva geofizicheskayal,
196o, Nr 2, PP 253-262 (USSR)
ABSTRACT3 The authors describe their research on the distribution
of activated atoms along the axes of wells. The
activation was effected by the generator of neut.rons
being in motion, stationary or pulsating, The
relationship between this distribution and the speed.of
prospecting and the parameters of the medium were also
considered. The amount of atoms of a radioactive isotope
produced by the activation during the time to was
calculated from Eq (1.1)., where X - constant of decaying,
No - maximum possible number of activated atoms. The
rate of activation per unit of a cylindrical layer is
given as Eq (2.1), where z - coordinate of the
observation point, vt - coordinate of the source of
neutrons, L - parameter of the distribution, A - rate
of activation. The expression (2.1) corresponds to the
Card 1/4 experimental distribution of the thermal neutrons. The

S/049/60/000/02/008/022
E131/E459
The Optimal Conditions of Activated Continuous Prospecting
experiments showed that in the case of a Po-Be
in water and r >20 cm, r2 = ke-r/L is the density
of thermal neutrons), the migration distance is equal
to 10 cm. The linear density of the activated atoms n
can be determined from Eq (2.2), where I is obtained
from Eq (2.1). The initial conditions are defined by
the relationships (2.3) to (2.10). Fig 1 shows the
distribution of the activated aluminium in bauxite
calculated from Eq (2.9) and (2.10) for different speeds
.of prospecting. It can be considered that the intensity
of y-radiation is proportional to the concentration of
the radioactive isotope as shown by Eq (2.11). The
optimal sounding is obtained when its length is equal to
the distance between the generator of neutrons and the
point of maximum concentration of activated atomsi this
can be found from Eq (3-1) (see Fig 1). Fig 2 shows
the relationship (2.10) calculated for the concentration
of activated atoms Al in bauxite and the speed of
prospecting for a constant soundi ng d ~ 150 cm, The
Card 2/4 optimal speed can be calculated from Eq (3.2) for the

s/049/60/000/02/008/022
E131/E459
The Optimal Conditions of ActivAted ColitillUOUS Prospecting
condition (dn/dv) = 0 and d =-constant, The rate of
activation produced by the pulsating generator of
neutrons can be determined from Eq (4.1). In this case
the conditions in front of the generator are described
by Eq (4.2) and those behind it from Eq (4.3). The
density of activated atoms at a distance d behind
the generator can be calculated from the latter equation
,when z = vt -- d. The expression (4.3) can be
simplified when d = 0 and can be shown as Eq (4.7) and
(4.8). If the activation is performed in respect to one
out of many elements in a rock, the proportion of
neutrons Qo used for activation of that particular
element can be calculated from Eq (5-1), (5.2) and (.5.3)-
where 'To is the mean lifetime of a thermal neutron in
a rock, KO is the mean rate of capture of the thermal
neutron, v is its mean velocity, 1i is the density
of i-atoms, ai is the corresponding rate of capture,
No is the total number of thermal neutrons in a rock.
The total number of activated atoms of aluminium in the
Card 3/4 bauxite zone of the hydrargillite sti-ticture can be

s/09/6o/ooo/02/008/022
E131/E459
The Optimal Conditions of Activated Continuous Prospecting
calculated from Eq (5-8)-
between the proportion of
of Al and the content of
figure that the magnitude
than the concentration of
and 15 Soviet references.,
Fig 4 shows
neutrons used
k'203 It can
I iEq 5.10)
A1203, There
the relationship
for activation
be seen from this
increases faster
are 4 figures
V
ASSOCIATION; Urallskiy filial AN SSSR Institut geofiziki
(Ural Branch of the Academy of Sciences USSR,
Institute of Geophysics)
SUBMITTED2 June 27, 1959
Card 4/4

BULASHVICH, YU.P.
"Nuclear geophysics"; collection of articles on the use
of radioisotope
emissions in petroleum geology. Izv. AN SSSR. Bar.
geofiz. no-8:1223-
1226 Ag 16o. (MIRA 13:;)
(Prospecting-Geophysical methods) (Petroleum geology)
(Radioactivity)

L F V; c. 11, U I:)
PHASE I BOOK EXPLOITATION SOV/5592
Vsesoyuznoye soveshchaniye po vnedreniyu radioaktivnykh izotopov
I
yadernykh izluchenly v narodnom khozyaystve SSSR. Riga, 1960.
Radioaktivnyye i-zotopy i yadernyye izlucheniya v narodnom
khozyaystve SSSR; trudy Vaesoyuznogo soveshchaniya 12 - 16
aprelya 1960 g. g. Riga, v 4 tomakh. t. 4:' Poiski, razvedka
i razrabotka poleznykh iskopayemykh (Radioactive Isotopes and
Nuclear Radiation in the National Economy of the USSR; Tran-
sactions on the Symposium Held in Riga, April 12 - 16, 196o.in
4 volumea. v. 4: Prospecting,Surveying, and Mining of Mln-'
eral Deposits) Moscow, G6stoptekhizdat, 19061. 284 P. 3,640
copies printed.
Sponsoring Agency: Gosudarstvennyy
nauchno-tel&Lnicheskil-y:komi-tet
Soveta Ministrov SSSR. GosudarstverTnyy komitet Soveta'Ministrov
SSSR po ispoilzovaniyu atomnoy energii
Eds. (TItle page): N. A. Petrov, L. 1. Petrenko, and P. S.
Savitskly;
ed. of this volume: M. A. Speranskiy; Scientific ed.z M. A.
Speranskiy; Executive Eds.: N. N. Kuz'mina and A. G. Ionell~
Y
Card 1/11

Radioactive Isotopes and Nuclear (Cont.) SOV/5.592
Tech. Ed.: A. S. Poloaina.
PURPOSE : The book is intended for engineers and techn1clans
dealing with the problems involved in the applicaticn of
radioactive iEotopes and nuclear radiation.
COVERAGE: This collection of 39 articles is Vol. 4 of the
Trans-*--c-
ticna of the All-Union Conference of the Introduction of
Radi.o-
active Isotopes and Nuclear Reactions in the National
Economy
of the USSR. The Conference was called bv th-
Gosudarstvennyy
nauchno-tekhnicheskiy komitet Sovet MinistrovSSSR (State
Scientific-Technical Committee of the Council of Ministers
---f
the USSR), Academy of Saiences USSR, Gosplan SSSR ~State
Planning
Committee of the Council of Ministers of the USSR
Goc;udar_=tv!Fr-
nyy kom-itet Scveta Ministrov SSSR po avtomatizatsii i
mash'-no--
stroyeniku (State Committee of the Council of Ministers of
the
USSR for Automation and Machine Building),and the
Counle-.11-o-P
Ministers of the Latvian SSR. The reports summarized In
publication'deal with the advantages, prospects, and
Card 2/11

Radioactive Isotopes and Nuclear (Cont.) SOV/5592
development of radioactive methods used in prospecting, sur-
veying, and mining of ores. Individual reports present the
results of the latest scientific research on the development
and improvement of the theory, methodology, and technology of
radiometric investigations. Application of radioactive
methods
in the field of engineering geology, hydrology, and the con-
trol of ore enrichment processes is analyzed. No
personalities
are mentiorkL There are no references.
TABLE OF CONTENTS:
Alekseyev, F. A. Present State and Future Prospects of
Applying
the Methods of Nuclear Geophysics in Prospecting, Surveying,
and
Mining of Minerals 5
Bulashevich, Yu. P , G. M. Voskoboynikov, and L. V.
Muzyukin. -19
Neutron and Gamma-Ray Logging at Ore and Coal Deposits
Gordeyev, Yu. I., A. A. Mu-kher,and D. M. Srebrcdollskly. The
Card 3/11

- BULASHEVICH, Yu.P.; SENIKO~BUIATTO'Y, I.N.
Experimental testing of optim= conditions for
continous ac-
tivation logging. Izv. All SSSR. Ser. geofiz.
no,4:541-543
Ap 161. (MIRA 14-3)
1. Institut geofiziki Urallskogo filiala AN SSSR.
(Radioactive prospecting)

DYARDIN, 1. G., NTIA~~----,,~4'!C)l A'a P r" I
Vi ': 0, ?,.
f- i~- *
proumu in tL:-,i ur --:: ,
roport to bo aul"Itt~d for c~~i Nualoca-
Erakow, rokad, 24-30 C,-Vt 1,("'22.

.-BULASHEVICH,-Xu.P ; SENIKO-BULATNYY, I.N.; DEYEV, L.L.
Gama-spectrometric activation logging,. lzv. AN SSSR.
Ser. geofiz.
no.9:1153-1157 S 162. (~aRA 15:8)
1. Urallskiy filial AN SSSR, Inatitut (;eofiziki.
(Radioactivo prospecting)

2.
L 1235-66 PIT(;)
ACCESSION NR: AT5022651 UR/2874/65/000/003/0003/00151
_:'AUILHOR: Bulashevich, Yu. P.; Khalevin N. I.. Timofeyev, A. N.;
Kuznetsov, A. :5,V
.4.5 Vq
TITLE: Selection of a site in-tbe Urals for sinking a spRerdeep
boreho3,e
SOURCE: AN SSSR. UraL'skiy filial. Institut geofiziki. Trudy, no.
3, 1965.
sbornik, no. 4: Metodicheskiye voprosy rudnoy geofiziki Urals,
(Geo_~:
physical papers, no. 4: Methodological problems of mining
geophysics of the Urals),
3-15
TOPIC TAGS: superdeep drilling, 14oho discontinuity, Conrad
discontinuity, gravity
survey, seismic survey, seismic profile, aeromagnetic survey,
magnetic survey, earth
crust
ABSTRACT: Since 1961, several Soviet scientific organizations have
carried out inve.s-
tigations in the'Ural Mountains to determine the optimum location
for drilling
a
.superdeep borehole. The arqa covered extended along the range from
511201 to 580hol:
N. Lat. The announced purposes of these studies, both of scientific
and industria-L-i
import, were as follovs, 1) thickness, composition, and
stratigraphic'sequence of
geological formations; 2) nature of the geosynclinal
sediment-"granitic" transition
zone; 3) thickness and tomposition of the~*,"granitid" layer 4)
nature of the
gran.~

14
[A~CESSXON NH: AT5022651
itic" layer-"basaltic" layer transition zone; 5) physicochemical
changes in the
rockes with depth; 6) types of igneous intrusions and ore bodies;
7) physical propeil-
ties of the rocks and the nature of discontinuities (Conrad and
Moho), and 8) chanpa
in temperatures with depth and the thermodynamic conditions at
great depths. Result,s
of preliminary studies indicate that the most favorable site for
the borehole will
probably be in the Tagil-Magnitogorsk synclinorium in the
Verkhotur'ye-Krasnoural'ok
region where a number of industrial boreholes have already been
drilled to a depth
of 1.,2 km. Final selection of the site, however, will require
additional gravity
and magnetic (terrestrial and aerial) surveys as well as deep
seismic sounding and
reflected-vave profiles. Orig. art. has: 6 figures. [ER)
ASSOCIATION: Akademiya nauk SSSR.' Urallskiy filial. Institut
geofiziki (Ural
Branch, Academy of SciencesSSSE; Institiite of Geophyqij~s)
SUBMITTED: 00 ENCL: 00 SUB CODE: ES
NO REF.,SOV: 012 OMER: 000 ATD PRESS

BITIAT, A.
J. KACZMAREK; A. BULAT
"Tables of suggested conditions for machim manufacti3ring.11 P.
95
(Mechani , Vol 25 No 2 Feb 53 Warszawa)
SO: Monthly List of East European Accessions, Vol 2 No 9 Library
of Congress Sept 53 Uncl