SCIENTIFIC ABSTRACT BOGORODSKIY, N.V. - BOGOROV, V.G.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000205930007-5
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 99
• Document Creation Date: November 2, 2016
• Document Release Date: June 9, 2000
• Sequence Number: 7
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

0 06-- O'C C-)~,,D Sr / y W, //~
BOGORODSKIT, N.Y., podpoliovnik meditsinskor slushby
T, "'.
r--
Use of "Calcax" in treating certain skin diseases@ Toone-madezhurm
no.7:83 A '57. (MIRA 11:1)
(SKIN-DISIASUS) (aALCIUH CHLORIDR)
(MMMMISMATRIAMINE)

BOGORODSKIY, 0. [Bohorodf--Ikyi.. 0.) kandfiz.-matem.nauk
I'lauka i zhyttia 11 nolc4
Address; the moonl , 6-47 Ja W.
- OUR& 15.2)
(Space research)

BOGORODSKIY, O.F. [Bohorb"'kjri, O.F.1, doteent
Why we strive io reach space. Znan, ta. pratsia, no. 3:16-18 Mr 161.
(MIRA 1415)
1. Direkior Astronomicheekoy o'beervatorii Kiyevskogo gosudarstvennogo
universiteta " Shevchenko,
(Astrophysics)
1

ACC NR, ARW;W761 SOURCE-00riF,:--WO269/66/000/r,03/CO38/0038
AUTHORs BogprodsLkj&U0. Fj, Turchaninova,
TITLE: jnvestigation of the spectral enorc)1distribution at the centers of planetary
nebulaeW'
SOURCE: Rafe zhe katronomiyaj, Abse 3.51.328
RFF SOURCE: Visnyk Xyyivatke un-tue Sere aatronep no* 6. 1964.9 3-8
TOPIC TAGS& spectral energy distribution; nebula
ABSTRAM Various methods are-considored which are usod to determine temperatures
at the centers of planetary nebulae. spectral energy distribution at the centers is
presented as a sequence of sections of Flanckle curves corresl*nding to various tem
aturess 'The spectral energy distribution is-calculated for the center of nebula
NGC6572, V, G, CTranslation of abstrtot
7
SUB COM& 03

V'
TJSSR/Solid =e PhysIs' - Structure of Deformable Materials.
Abs Jour : Referat Zhur - Fizika, No 5, 1957, 1i863
Author : Bogorodskiy, O.V., Umanskiy, U.S.
Inst : Moscow Institute of Steel, USSR.
Title : Change in Fine Crystalline Structure of Austenitic
Manganese Steal During Plastic Deformation.
Orig Pub : Izv. AN SSSR, ser. fiz., 1956, 20, No 6, 614-620
E-9
Abstract : The great strengthening observed in cold deformation of
austenitic high-carbon steel (Radfield steel) are explai-
ned. Hardened specimens were subjected to compression in
a Gagarin press at a rate of 3 mm per minute. X-ray dif-
fraction investigation has shown that as the degree of
compression increases, one observes a rapid reduction in
dimensions of the mosaic blocks and a growth in the micro-
deformations of the grains. The hardness increases sharply,
Card 1/2

USSR/Solid State Physics - Structure of Deformation Materials. E-9
Abs Jour Ref Zhur - Fizika, No 5, 1957, 1.1863
and the lattice period of the austenite diminishes.
A decisive cause of the strengthening of manganese aus-
tenitic steel is the crumbling of the mosaic-structure
blocks, due to the separation of the carbides. Also
investigated was the change of the ferromagnetic proper-
ties.
Card 1/2

-M
UNNOV, Sarkis Androyevich; DOGORMSKII6.9ALA Iaede'; BIMUN, TeA, red.
isd.-im; VAYNSETIMF, F84,
[Me'rs6metrio"=ta*ll4mphvY Sterisometriolhookmis. metallograftia,
lzd;2o-. perer~ I day, Moskya, MD~*', muAno-tskhn, isd-vo lit-z7
'1958. 446 P, (mm. ntio)
po chernol I tevetnol metallurgis &
(yatallography)

24(2)$ 16(2) SOV/48-23-5-20/31
AUTHOR: Bogorodskiy, 0, Ve
-----------------------
TITLE: On the Determination of the Grain Size and the Microdeformation
by the Method of ' Harmonic Analysis (K opredeleniyu velichi-
ny blokov i mikrodeformatsiy melodom garmonicheakogo analiza)
PERIODICAL: Izvestiya Akademii nauk SSSR. Seriya fizicheskaya, 1959,
Vol 23, Nr 5, pp 635-636 (USSR)
ABSTRACT: The introduction to the present paper deals with the possibili-
ty of determining the distribution of the grain sizes, micro-
deformation, the distribution of t1hn textural grains in the
structure and their size. This possibility is offered by the
application of the harmonic analysin on the intensity of
the diffraction lines. The theo;:et1nal fundaments of the
harmonic analysis are then discussed and a diagram (.Fig
shows the intensity profile of a atandard and an amplified
diffraction line. These are split up into Pourier series;
the coefficients are determined by the aid of a diagram.. In-
other diagram (Fig 2) shown the results obtained in this way
Card 1/2 conoerning the distribution of tho textural grain size.

SOV/48-23-5-20/31
On the Deti-rmination of the Grain Size and the Microdeformation by the
Method of Harmonic Analysis
There are 2 figures and 4 references, 2 of which are Soviet.
Card 2/2

9/032 601026100810031011
B015 3064
iNTRORS.. Foxin, V, Go, Bogoradck&p, 46Jq
I -
TITLEs DeternInAtion of tko Degree of Nicresegregation in
_pCruanium-Asilioe Alloys,
]PERIODICAL: Zavodakaya laberatoilys. 9 1,60t Tel. 26, 109,89 PP- 91T-9T9
TIM. -Tko dqdr*ls of dondrit*:. sspo#atioa~ was dot*rqinod in papers of
-Vista, (.1aiq 1 J'and, (10fi- :k-4) fres the line Abroadex-
i;;:i-a- the I-raj *icturs; -In. this counsation ii wasp however, t9kittod to
C61isId4ikr:*'%4 mqftoc 4SOUTs tka41-M&Y also Ibriag about a broidening.of the
.14 the, pr .6
X-ray, "Ot *&lot th's d4grea- of sicrosegragation
was coupai Otlair~-, in-ctq-,cQrrqMpOnding,-,
~ TMM",
to the. glanc -ing angles. The examinations were made on Ge-Si semiconductor
~Ilojys a PKY (RKV) X-r&7 -cansia. A gasple Pulverized to 0. 1 p -1
vai,U46djhe ,X-rV:liJkOS COrrappeading to the .1arger.glansing angles. were
piotonitricilly-oValwatedg and'-t-keir VOk and 'areadening-diaterninede the
pr6pottionality between the 'broadening of -,tke X-ray 'line and the tkagent
of po, j1aiidjW angle showed tkat the line ',~r.oadexing was only due -to
Card 1/2

DOeraind tion of the ~qgree-of.1ficrosogtisgatien 8/032/60/026/008/003/011
in*60ph""ism. - Rilicel AL11sys B015/BO64
sicros*grogation (jVg- 2)IISince the line:bro *adening depends lia*arly on
.the - i t i A.
oompos !of the Ge-Si alloy, it was possible to determine from the
-~ixe 'broadening a d~viaiiou t-f the ahenicil composition of the sample from
the average valuee The minissum silicon content varied from 0 to 8 at% in
the ,'individuaj jar,ts of the Ban
p~*. There are. 2~flgpren and 4 ref"onals:
3 IS.
-ASSOCI.ATIOX: Go*%d&rstv*mxyy mauohn"issladovatel-Iskiy i proyaktayy
(Ataii Scientific Research and;Planning Institute of the
Rare Metals-,Iadustryj-
Caj.4 2/2

86235
4 .110 ID 51 S/032/60/026/008/035/046/xx
B020/B052
AUTHORS: Bogorodskiy, 0. V. and Shillshteyn, S. Sh.
TITLE: Goniometer Head for X-Ray Structural Analysis by a
Double-crystal Spectrometer
PERIODICAL: Zavodskaya laboratoriya, 1960, Vol. 26, No. 60
pp. 1012 - 1013
TEXT: The double-crystal X-ray spectrometer detects errors in the strue-
ture of single- and polyorystal samples, exactly determines the stress
distribution in wide single-crystal regions, and the lattice periods of
single- and polyarystal materials. The device type 9PG-5011 (URS--50I)
used at present does not permit sufficiently rapid and exact studies.
The goniometer head designed by the author (Fig.1) simplifies the fixa-
tion of the objects to be studied in a position which corresponds to the
reflection of X-rays from every crystallographic plane. Thus, an ae-
curacy of up to 0-5" is attained. The double-crystal spectrometer is at-
tached to the device URS-50I. The first crystal is put into the clamp
Card 1/2

86235
Goniometer Head for X-Ray Structural 9/032/60/026/ma/m/046/n
Analysis by a Double-crystal Spectrometer B020/BO52
of the monochromator, the second one into t-he goniometer head. The
widths of the rotation curves of a natural calcite crystal (211) and a
germanium single crystal (111) were determined by the above goniometer
head attached to the device URS-501 (Fig.2). The theoretical width of
reflection of an ideal calcite crystal is 5.811. In the given case, a
width of 11" was obtained due to the insufficient quality of the crys-
tal. The experiments showed that the band width of a germanium crystal
with a dislocation density of 10- 2 om-2 is 20", and of a crystal with a-
dislocation density of 104 0m-2 it is 40". The rotation curves thus
have two maxima which is due to the presence of blocks in the germanium
single crystal, vith disorientation angles of approximately 20". The
theoretical width of the rotation curve of the ideal germanium crystal
is 15.8". There are 2 figures and 1 non-Soviet reference: 1 German.
Card 2

8356o
8/020160/134/001/012/021
q3,VO B004/Bo6o
AUTHORS: 2ogorodski;~q 0. V., UmanskiZ, Ya. S. Qhil'shteZn# S. 8h.
to
TITLE; On the Nature of the Mosaic Striint"r of Single Crystals
of Germanium and Silicon
v]
]?ERIODICAL: Doklady Akademii nauk SSSR, 1960, Vol. 1349 No- 1,
Pp- 114 - 116 V~/
TEXT: The authors wanted to check the dislocation character of the
mosaio structure (Fig. 1),,and studied single crystals of germanium and
silicon that were drawn from the malt along the (111)-axie. The samples
used were 2-3 mm thick foils out perpendicular to the (ill)-axis. it
was established by,etching that almost all of the dislocations exhibited
the Burgers vector a/2 (1T0). In.some cases, the authors observed lines
which corresponded to small-angle boundaries. The density of surface
dislocations was 102 _ 100 ed'4 for germanium, 102 - 103 cm-2 for
silicon, The principle of the X-ray analysis is described.(Fig. 2). The
monochromatic X-ray beam is reflected from the crystal 19 and hits on
crystal II which is rotated around small angles. The authors used the
Card 113

8356o
On the Nature of the Mosaic Structure of S/020/60/134/001/012/021
Single Crystals of Germanium and Silicon B004/BO60
JPC-50H (URS-50I) apparatus with Geiger counter. The curve of the in-
tensity of double reflection of I as a function of the angle of rotationo
is defined as rotation curve. The authors constructed a special gonio-
meter head which allowed rotations around small angles with.an accuracy
of Oc5l'. The rotation curves obtained experimentally are shown in Fig-39
the data are given in Table 1. The distances between'the in&xima equal
thedisorientation angle of the crystal blocks. Experimental data show
that.the Ge single crystals have a mosaic structure with all disloca-
tion deneitiesp while'the disorientation angles of the blocks change
-little,,*although the dislocation densities differ by four orders of
magnitude. This cannot be explained by the Burgers model. In silicoing
the blocks are considerably smalierp which likewise contradicti'the
Burgers model, since the la-*U*tioe constants of Ge and Si are little
different. The germanium crystals with small-angle boundary showed
fragment structure. The authors arrived at the conclusion that the block
boundaries in Ge and Bi may be connected with dislocations, but not ac-
cording to the mechanism of the sm4ll-angle boundary. Also structural
defects might play a role here. The interfaces between the fragmentsp
on the other hand, consist of dislocations in agreement with the
Card 2/3

8356o
On the NatuTe of the Mosaic Structure of S/020/60/134/001/012/021
Single Crystals of Germanium and Silicon BO04/B06O
Burgers model. Thusy the nature of the block- and-fragment boundaries
is different. There are 3 figures~ 1 table, and 5 references: 2 Soviet,
1 US,~and 1 German.
ASSOCIATION: Moskovskiy institut stali im. 1. V.
Steel Institute imeni 1. V. Stalin)
PRESENTED,- April 26~ ig6o, by P. A. Rebinder,
SUBMITTED: March 2p 1960
Stalina (Moscow
Academician
Card 3/3

20026
14,1100 S/070/61/006/001/oo4/011
B032/E5i4
AUTHORSt Bogorodskiy, 0. V., Nashellskiy, A.Ya.. and Ostrovskaya,
V.Z.
TITLE-a X-ray Study of the Solid Solutions InAs-InP
PERIODICALt Kristallografiya, 1961, Vol.6, No.1, pp.119-121
TEXTt The basic materials employed were 99.999% pure indium
(brand 14H-0 (In-0)), 99.99% pure crystalline arsenic and 99.99% pure
red phosphorus flused for semiconductors of class A211. The alloys
were prepared with the aid of a special furnace shown in Fig.2.
The furnace consisted of two parts. The left-hand part was
maintained at a high temperature and contained indium in a quartz
boat, while the right-hand part was kept at a lower temperature and
contained phosphorus and arsenic. This procqdure has been
described by the second of the present authors in Ref-5- The alloys-
thus obtained were subjected to zone recristallization as described
by 0. Q. Folberth and H. Weiss (Ref.6). Chemical analysis of the
specimens was not carried out. The composition was checked by
comparing the weights of the elements loaded into the ampoule and
the solid solution obtained in the end. The specimens were ground
in an agate mortar until the average particle size was about 0.01 mm.
Card 1/4

20026
S/07o/6i/oo6/ooi/oo4/on
X-ray Study of the Solid 99.oso 9032/Z314
The X-ray photographs were obtained-by the Debye method,.using
copper radiation in the PKY (RKU) camera (86 mm in diameter). The
X-ray photographs w ere measured up on the 03A-A (IZA-2) comparator.
The lattice paramet ers were calculated from the 642 and 731 reflec-
tions. The table showsthe lattice parameters obtained.
Table
Lattice parameters of solid solutions of the
InAs-InP system
Composition, mol*% Lattice period, A
InAs InP __. Folberth Koster hnd Present-data
(Ref.1) Ulrich (Ref.4)
100 0 6.0 6.o6 6.042;0.001
95 5 - 6.034
90 10 6.026
8G 20 - 6.oi6
75 25 5-99 6.02
6o 40 - 5.96o
50 50 5.93 5-96 5.935
40 6o - - 5.910
30 70 5.892

21YO?6
!3/070/61/006/001/004/011
X-ray Study of the Solid B032/E514
Table cont.
Composition, mol.% Lattice period,
InAs InP Folberth Koster and
4) P~esent data
(Ref.1) Ulrich (Ref.
25 75 5.89 5.92
20 80 - 5.876
10 90 - - 5.857
0 100 5.86 5.88 5.86o
Fig.4 shows the dependence of the width of the diffraction lines and
the physical broadening (micro-liquidation effect) on the compositIon
after zone equalization. The physical broadening was calculated
.froin the formula
2
=JB - b
Vaere B is the width of the broadened line and b is the width
'of a standard line for InAs. There are 4 figures, 1 table and
8 references: 3 Soviet and 5 non-Soviet.
Card 3/4

20026
S/070/61/006/001/004/011
X-ray Study of the Solid E032/E514
ASSOCIATIONt. Gosudarstvennyy nauchno-isaledovatellskiy i
proyektnyy institut redkometallicheskoy promyshlennosd
(State Scientific Research and Project Institute of
the Rare Metal Industry)
suBmirrED: JulY 15, 1960
Fig.2 Fig. If
yvamah z
1B
eo 70
5
JR4
Pile. 2
InAs 0 AV
Card PKC. 41
A/',

FOMINt V.G.; OVODOVAI AN.; BOOORODSKIY* O.V.; SHILISHTEYN, S.Sh.
Some features of the crystallization of germanium-silicon alloys
in zone melting. Kristallograftia 6 no.2:256-260 Mr-Ap '61.
(MIRA 14-9)
1. Gosudarstvannyy nauchno-issleaovatel'skiy I proektnyy institut
redkometalliche3koy proMrshlennosti,
(Germanium-silicon alloys) (Dislocations In crystals)
(Melting)

FOMIN, V.G.; BOGORODSKIY, O.V.
Invostigation of microliquation in the crystallization of
gemanium-silicon alloys. KristallcgMMA 6 no.3:455-459
My-Je 1610 (MIRA 11,.. 8)
1. Gosudarstvannyy naucho-issledovatellskiy i proyektnyy in-
stitut redkometallicheskoy promyshle=osti.
(Cormanivn--Silicon alloys) (Crystallizati'on)

1. BOOORODSM, Pe A.
2. USSR (6oo)
4. Stock and Stockbreeding--Yaroslavll Province
7. Highly productive animals in Yaroslavl' Province, Sots. zhiv.,
15, No. ls 1953-
9. Month List of Russian Accessions, Library of Congress, April, -1953, Uncl.

'BOGORODSKIr. S.M.1 KRAVCErUK, V.N.; CHOWAKHOVSKIY, A.G.
Lower-Middle Miocene elavium in the Ust-Urt. Kora vyvetr.
no.3072-373 163, (KMA 16.- 7)
1, Vsaooyuznyy aerologichaskly trest.
(Ust-Urt-Weathering)

BOGORODSKIY, V.
Centrifugal machine with hydraulic push rod. Mor.i toch.flot 14 no.3:
22-24 Mr 154. (HRA 7:5)
1. Glavnvy inzhener Gorodetskogo mokhanichookogo zavoda.
(metal cladding)

BOGORODSKIYI__V.p kand.tekhnsnauk; DOBROTINp D.p nauchnyy sotradnik
Ultrasonic pulse gauge for thickness measurement in produ4 control.
Mor.flot 21 no.5s29-31 VV 161. ~MIRA 14:5)
lo Naohallnik Gidroakuptioheakoy laboratorii Arkticheskogo i
Antarkticheskogo nauchfiQ-~iseledovatellskogo.instituta (for 13ogorodskiy).
2. Gidroakusticheakaya liboratoriya Arkticheskogo i Antarkticheskogo
nauchno-iseledovatellsiogo instituta, (for Dobrotin).
(ShifL-Maintenanoe and repair)
trasonic testing)

S/194/61/000/012/078/097
D273/D301
AUTHORS: Bogorodskiy, V. and Dobrotin, D.
TITLE: Ultrasonic pulse thickness gauge for component control
PERIODICAL: Referativnyy zhurnal, Avtomatika i radioelektronika,
no. 12, 1961 22, abstract 12E119. ("Morsk. flot" 1961,
no, 5, 29-31~
TEXT: A detailed description is given of a portable instrument
7.37'W-,3 (UZTI-3) designed for determining the thickness of components
lqith rough or corroded surfaces in the range of thicknesses from
5 to 60 mm. Schematic and principle diagrams of the instrument are
presented and also a stress diagram at various points of the dev
sign. The instrument uses an MT (ELT) /-Abstractor's note: Elec-
tron-beam, tube 7. Pulses of 1.5 microseFond duration are used. At
a distance bet7veen two consecutive reflected pulses, the thickness
of,the component is determined. The instrument is provided with a
piezo-probe with a magnetic holder. The instrument worked success-
Card 1/2

S/1 94/61/000/012/078/097
Ultrasonic pulse thickness ... D273/D301
fully during experimental trials, and also in determining layers
and fractures in pipes. Z-Abetractor's note: Complete translation.7.,)~,
T3~
Card 2/2

BOGORODSKIXI-Y Y-t--,
Modern physical methods for measuring the thickness of sea ice.
Okeanologiia 3 no,4t720-730 163- (MIRA 16:11)
1. Arkticheskiy i Antarkticheekly nauchno-issledovatellskiy
institut, g. Leningrad.

24(l) SOV/112-59-2-4042
Translation frorn:. Ref erativnyy zhurnal -. Elek-trotekhaika; 1959, Nr 2, p 263 (USSR)
AUTHOR. Bogorodskiy, V. V.
TITLE; Ultrasonic Method for Determining Thickness of Ice
(Ulltrazvukovoy metcd opredeleniya tolehchiny I'dov)
PERIODICAL7 V sb.: Prob! Arktiki, Nr 4, L. "Morsk. trz-nsport, " 1958. pp 65-77
ABSTRACT: First experiments have been con-lucted in "he ultrasonic investigation
of physical properties of ice cover and ice thickness in f resh-water reservoirs
and seas. The ultrasonic method proved tobe bcttex- than other kn')Own mc:thQds
(acoustical, vertical electric soundiag, seismic-.A,~ou3t tical, capacitive). A
theoretical investigation is confronted with diffli,nilties due to textural and
structural peculiarities of the ice cover, as well as to dependence of the ice
properties on the composition of the water which created the ice, In
determining the damping factor of ultrasonic propagation in ice, the ice
thickness should be divided into two regions. (1) isotropic where the ultrasonic
Card 1/3

SOV/112-59-2-4042
Ultrasonic Method for Determining Thickness of Ice
wavelength is longer than the average dimension of the crystals; (2) anisotropic
where the reverse relation holds true. In each of the above regions, the
mechanism of dissipation and absorption of ultrasonic waves has its own
peculiarities. No attempt to evaluate the damping factor quantitatively has
been made as there is no data on the elasticity moduli of the ice crystal and
their temperature dependence; also the heat conductance and the heat capacity
of ocean ice are only approximately known. The author, in cooperation with
Z. I. Shvayshteyn, has used the supersonic method in determining ice thickness
on the Neva River and Ladoga Lake. Earlier, the velocity of ultrasonic
propagation in ice at -50C up to -200C for ocean ice and at -OOC up to -?50C
for fresh-water ice was measured. It has been found that the maximum relative
error in measuring ice thickness up to I meter by the ultrasonic method is
about 51/6. The method permits measuring (with the vibrator frequency 500 kc)
the ice thickness up to 2 meters (with an error of 5-776). The method was used
Card 2/3

SOV/11Z-59-Z-4042
Ultrasonic Method for Determining Thickness of Ice
at the drifting station "Severnyy polyus -4. " With the 500 -kc f r equency and an
acoustic pulse power of 150-200 w, the ma)dmum ice thickness that can be
determined is 0. 8-1.0 m. This limit can be raised if the frequency is lowered
and the ultrasonic power increased.
B.V.A.
Card 3/3

SOV/124-58-11-12230
Translation from: Referativnyy zhurnal, Mekhanika, 1958, Nr I I ~, p 38 (USSR)
AUTHORS: Bogorodskiy, V. V. , Gusev, A. V.
TITLE: - Use of Ultrasonic Vibrations in Hydrological Investigations
(Primeneniye ul'trazvukovykh kolebaniy dlya gidrologicheskikh
issledovaniy)
PERIODICAL: V sb. : Probl. Arktiki. Nr 3. Leningrad. "Morsk. transport", 1958,
pp 69-78
ABSTRACR: Desribed briefly are several methods for determining the speed of
sound in liquids: the interferometer method, the pulse method, and
the phase method. To eliminate the factor of ambiguity from results
obtained when the phase method is used to determine the speed of
sound in the sea, the authors propose a combination pulse-phase
method. A short account is given also of a phase--type gage for
measuring the speed of currents. The authors recommend that
ultrason-c-wave methods be used, for example, to study the utider-
side of ice covers upd for other types of hydrological investigation.
L. K. Zarembo
Card 1/1

46-4-1-3/23
LUTHOR: Bogorodskiyj
TITIS: Elastic Properties of Ice. (Uprugiye kharakteristiki
11da.)
P~RIODICAL: Akusticheskiy Zhurnal, 1958, Vol.IV, Nr.l.
pp.19-23. (US8R)
ABSTBACT: An ultrasonic pulse method was used to determine
elastic constants of polycrystalline ice. The circuit
used is shown schematically in Fig.l. A primary
generator 1 is connected to a display generator 2
and a pulse generator 3. The pulse generator excites
a piezoelectric transducer 4, which emits an acoustic
pulse into the sample studied. After passing through
a known distance in ice the pulse excites a piezo-
electric receiver 5. A sigaal from the receiver is
passed through an amplifier 6, a detectuor 7, and then
it is displayed on a cathode ray oscilloscope 8. To
measure the time interval between the emission and
reception of an acoustic pulse, the oscilloscope display
is calibrated by means of an electronic device 9.
-The apparatus is calibrated by means of a standard
acoustic line shown in Fig.2. Excitation of
Card 1/3 longitudinal waves inice was produced using barium

Elastic Properties of Ice.
46-4-1--jJP3
titanate plates and shear waves were excited by means
of quartz vibrators with a Y-cut. All piezoelectric
transducers had a resonance frequency of 500 kc/s.
Both the longitudinal and shear wave velocities could
be aeasured simultaneously, and D~om these velocities
the values of all elastic constants of an ice layer up
to 2 x thick could be found. The first series of
measurements was carried out in the author's laboratory
using ice blocks 6Dx6OxIOO cm in size. Other
measurements were made on the ice cover of the Iadoga
lake. Fig-3 shows the dependence of the velocities
of the longitudinal and shear waves on the temperature
(zero to -2500) and density of fresh-water ice. A
practically linear dependence of the elastic wave
velocities on temperature was obtained. Fig.4 ~'ves 2
the dependence of the Young's modulus (6-10 x 10 ks/cm,
and shear modulus (2-4 x 10 4 kg/cm 2) on the temperature
and density of fresh-water ice. The values of the
Poisson's ratio (of the order of Oo34) are given in
Table 1. Similar measurements were made for sea-water
Card 2/3 ice. These measurements were carried out in 1955 by

Elastic Properties of Ice.
4~
46- 4 -1-.~S/23.
a drifting Polar station SP-4, The results for sea-
water ice are given in Table 2. There are 4 figures, 2
tables and 4 references, of which 1 is Soviet, 1 German,
1 American and 1 a translation of a Westem work into
Russian.
ASSOCILITION: Arctib Scientific Research InstAtuteo-Ieningrad
(Arkticheskiy nailchno-issledovEtellskiy institut,
leningrad.)
SUBMITTED: February 3, 1957.
1. Ice-Elastic pre"rties
Card 313

j
g.gooo,24-2130,211-7800 77 3 _3
SOV/57-30-1-1','/18
AUTHORS: Rudalcov, V. N., Bogorodskly, V. V.
TITLE: Measurements of Glacier Thickness by Electromagnetic
Mothods
PERIODICAL: Zhurnal telchnicheskoy fizilcl, 1960, Val 30, Nr 1,
pp 8'2-89 (USSR)
ABSTRACT: The problem arose during measurements of ice layers in
the Antactic as a part of the International Geophysical
Year program. Gravimetric and magnetometric methods are
only relative while the seismic methods are Impractical
due ",'o a thick damping layer of snow. The authors dis-
cuss, therefore,the possibi lity of using retarded, re-
flected electromagnetic signals. (1) Electromagnetic
properties and the structure of ice: The authors review
the data about the dielectric permittivity E and the
tan 8 of the angle of electrical losses In t-he
dielectric obtained by Eder (Ann. d. PhYs., 1, 7-8,
3Bi-398, 1947). They compare them to those computed
Card 1/8 using the Debye equation

Measurements of Glacier Thickness by 77333
Electromagnetic Methods SOV/57-30-1-12/18
E1=etg3= to-too X, (2)
X"
where
V (3)
(I
Here 0 is value of P- at f Is value of
at optical frequencies (tip to the start of electronic
dispersion); f0 is frequency at which F- I reaches its.
maximum value. Taking the values of the constants from
the work by Eder, the authors computed Table A. Assuming
a linear temperature change In the deeper layers of ',-,he
ice,
t:=t;--b(h-z), (5)
where z Is the coordInate perpendicular to the glacier;
t0 is It-'emperature of the earth beneath; b Is temperature
Card 2/8 h

Measurements of Glacier Thickness by 77333
Electromagnetic Methods SOV/57-30-1-12/18
Table A
Dielectric permittivity and the tangent of the angle
of electric losses of insipid ice at t = -100 C
(a) Frequency-f, c cles; (b) computed using the
Debye equation; (c~ experimental data by Eder;
(d) experiments data by Pasynicov, RQdakov, and
Kholuyanov.
e. d,
a,
Ira is a
0 SD.0 0.000
10 80.0 O.OD4
102 WO 0.041 80.0 0.167 -
103 6&0 0.410 64.3 0.695 -
101 6.2 2.8DO 11.0 2.19S - -
103 2.0 0.850 2.0 0.721 3.2 0.600
105 2.0 0.086 2.0 0.222 zo 0.140
107 2.0 0.009 - - 2.0 0.014
108 2.0 9-10--4 - - 2.0 -
109 2.0 9-10-5 - - -
Card 3/8 1010 2.0 9 - H~-O - - 2.0

Measurements of Glacier Thickness by 77333
Electromagnetic Methods SOV/57-30-1-12/18
g:-adient. Taking b = 0.02 deg/m and t = -30 C, they
Calculated the relationship between the dielectric
permittivity and the distance from the surface of the
glacier (see Fig. 3).
Fig. 3. Dielectric permittivity of
the glacier vs distance from the
surfacn of the glacier: (a) a9
f = 10 cycles; (b) at f = 10
cycles; h is the glacier thick-
ness.
Card 11/8

Mr~asuromontn of Glacier Thickness by 77333
Electromacnet-le Methods SOV/57-30-1-12/18
The afitho~s also note that the ice at 8 to 10 m
under the surface of the glacier is made mostly out
of crystals of 1-2 cm size. No data are available
for greater depths. Electromagnetic investigations of
ice crystals were made only iii the region of light waves.
(2) Propagation of electromagnetic waves In ice: Since
tan 0, pormitutivity of Ice han to be complex:
(7)
Using Maxwell's-e-qUations, the authors oVtain an
equation for the electric vector E (E = b~f.)
AE -#- L'~ 1E -+- grad (E grad 0. (9)
CS
Assuming a slow variation of' and t%king the wave
propagation to be along the axlo, the solution can be
obtained In the simplified Porm
P(0>11 -j *(,Y)dr-r13
A (16)
Card 5/8 E(z)= P' e e

Measurements of Glacier, Thickness by
.Electromagnetic Methods
Car~d 6/8
where
77333
SOV/ 57-30-1-1-2/18
(17)
tg?=i
and where W in Eq. (9) was first substituted by
k (x, y, z) V~(x, -y, z)
C
and then k was written in a complex form
k (z) CL (Z) - jk9 (13)
For the time of return of the signalat high frequencies and
sufficiently low temperatLi.res, the authors derive an
approximate equation 2nh (19)
. C
where n is index of' refraction. For h = 2 Km; nz:vrF--=
= v r2-, -r comes out to be 18. 9 a sec. There exists one
kind of damping due to absorptVon by Ice. An approxi-
mate equation at high frequencies Is
lVdb, 8.65 -L' V;- h ix 6.
.IC (22)

Measuramonts of Glaclei, Thickne3's by 77333
Electromagnetic Methods SOV/57-30-1-i2/18
where Ndb denotes the number of docibels. Foy,
6 1
f > 10 cycles, tanS I/Lj , and n = const-, so
11
that for h = 2 Kin, Ndb., 1-1- 40.8 db. The scattering
contributes another damping given by
Vdb. 20' - Ig 1 (23)
qV
where
ex I a P OVI (24)
is "-he effective cross section of scattering, and V
is the volume of single crystals. As is known,
3 a - 1
4x a -*- 2
Card 7/8
(25)

Measuremen4~s of Glacier Thickness by 77333
11
Electromagnetic Methods SOV/57-30-1-12/16
3 cycles,
Assuming V I cm), Ndb,,'-', 0.01 db at f = 108
but Increases rapidly to Ndb2'_,~100 for f = 109 cycles'
The authors discuss other contributions to the damping
(partial reflection on the air-ice or air-snoW surface,
non-mirror reflection from the ice-ground surface, waves
not being plane) and conclude that for,\= 1 m wavelength,
the damping does not exceed 100 db. With a 10-1cw
gonerator one need3 a recolve of 14 vol I. ur.-nnitivIty and
a 0. 1
- /1 nec Impulue sequence with pauses larger than
110 ~, occ, which Is all technically fcasible. Th~
auttiors note that the offects diSCUSOCd In the present
paper are probably the cause of' 100 to 120 in altimeter
readings In airplanes landing on glaciers of that
approximate thickness. The authors conclude that there
probably exists a possibility of using highly directional
millimeter waves, but that one first needs experimental
investigations of scattering of such waves in ice. There
are 4 figures; I table; and 6 references,-4 Soviet, 1 German.
SUBMITTED: July 4, 2-958
Ca-Pd 8/8

43203
31046
/62/008/004/003/017
BIOS/B186
AUTHORS: Bogorodskiy, V. V., Romanov, V. N.
TITLE: Relief-capaoitance technique of measuring the intensity of
ultrasound
PERIODICAL: Akusticheskiy zhurnall v. 8, not 4, 1962, 415-419
TEXT: A possibility of measuring the intensity of ultrasound is discussed.
The pressure of ultrasound and some minor factors mill produce a relief on
the free surface of a liquid or on the interface between two immiscible
liquids. The heigh 't of this relief depends monotonically on the intensity
of the ultrhsound. The free surface or interface can therefore be used as
one electrode of a measurement cell serving.as 'a capacitor, the capacitance
changing with the height of the relief. It was verified in experiments that
the height of the relief is directly proportional to the intensity of the
ultrasound. The error does not exceed 15
-20%. Measurpments with the
ielief-capacitance technique, in which a plane electrode was placed above
the free aurface of the liqui-d, showed that at high intensities the relief
height increases more slowly than expected in proportion to the intensity.
V
Card 1/2

Relief-capacitance technique of...
S/04 62/008/004/003/017
B108YB186
This is due to a higher absorption resulting from the distortion of the
shape of the wave. Capacitor cells with two liquids are more suitable
for intensity.measurements, since the reflected ultrasound does not interfere
as much as in free-surfaoe-liquid cells. There are 8 figures.
ASSOCIATION:
SUBMITTED:
Arkticheskiy i antarkticheskiy n.-i. institut, Leningrad
(Arctic and Antarctic Scientific Research Institute, Leningrad)
July 26, 1960
Card 2/2

-#RW=U4- ~-V-- RUDAKOV, V.N.
Electromagnetic methods for determining the thickness
floating ice, Zhur,tekh,fiz. 32 no*7s874-882 JI
(Electromagnetic waves)
(Ice)
of
162.
(KM l5s8)

S10461631009100110211026
B104/2186
AUTHORS% Bq&aEa~~ ~., Dobrotin, D. D.
TITLE: Some results of an investigation into the physical and
mechanical properties of the snow cover
PERIODICALs Akusticheskiy zhurnal, v. 9, no. lt 1963, 115 - 116
TEXT: The physical and mechanical properties of arctic snow were deter-
mined at the drifting polar station Q-10 (SP-10) during April - 14-ay 1962.
Using an ultrasound pulse method, the velocities of longitudinal and trans-
verse waves were determined from the snow cover and from sam:)l,s of dlffer-
ent densities. Measurements were carried out in horizontal and vertical
directions both in the snow cover and in samples. Results: Young's
modulus and the velocities of the waves determined from the samples in-
crease monotonically with density and show no great difference whether the
snow is investigated in horizontal or in vertical direction. The velocities
determined in the snow cover in vertical direction are greater by a factor
of 2 than those determined in horizontal direction. These results can be
explained by the effects of recrXetallization. There are 1 figure and
1 table.
Card 1/2

S/04 63/009/001/021/026
Come results of an investigation... B104YB186
ASSOCIATIM Arkticheskiy and aniarktiaheskiy n.-i. institut, Leningrad
(Arctic and Antarctic Scientific Research Institute, Leningrad)
SUBMITTED t July 25, 1962
Card 2/2

,PqqpRQDSrIY,,,.V,V..; DOBROTIN,, D.D.; KHOMWV, G.P.
Ultrasonic thickness gauge for controlling corroded'surface(se
Zav. la.b. 2.%~no-10$1254,125~ :163, '(MM 16:12)
1. Arktich6skiy i antarktlc~i~skiy nauchno-isaledovatellskiy
institut Hinisterstva morskogo flota.

B(GORODSKIY, V.V.
-.-I - ~ - 1 -, - ~
Elastic moduli of lee cryBtalv,, Akust, zhur, 10 no.23~152-255
164. (MIR-1 1706)
1. Arkticheskiy i antarkticheakiy nnuchnc--ossledovatellskly
institut, Ieningrad.

-A' /f,
AC ESSION NR, AF-5015642 UV 0 0 5 76 -E- C'3CC66 IL I S3
V.N.v Tyull,A-, V.A.
TAUMOR: Bagorodaldy, V.V.,* Radakov r
TITLE:
ElectromFignetic probing of the antarctlc
U70 %~, .72' .* L'ahumal tekimicheskoy fiz-1ki, v#35, no.6, 1965, 1150-LI53
TOPIC TAGS; radar, ice, thielmess gagge
-TRf
AB-S iCT: The authors briefly discuss the deficiencies of thin sei!g-
F
mic -jethod for measurimF, the thick-ness 1)f the antprctl--
e -9 1 r at I I i to f d eve-1 o pine- a ra P - :D,,- t
n r, u 01-13 Surveys to 't);:- Mnrje ~r )Lr .il
'S te3t p-r~o'-med early iii 1964 on the
nVy cb3ervatcry and the Pionerskaye stR',Ion L". '1'
star-iard qyLjyA-,~A'i~1radar set operating -,t a v R -0
a pui3e power of R W and a 4410 antenni~ patterni.
mounted on a tractor sledge, the anterina was laid directly on tne
snov, and the position -,ms determined witnin 500 m. A 23trong i-3flec-
tion was received corresponding to an 1*,!o cap thllcknf)s:'~ E611" N;
CorrA/,3

L 54773-6a
ACCESSION NR: AP5015642
this is to be compared'vith '.',he thielmass of 900 n determined seis.
mically for the ice tap in this region. The measured attenuation
was approximately 150 db! this is considered "Co be in good e-greement
vit;h the attenuation of 117 to 120 db calcula"I"ad on 1.1,118 ba-sis of the
theorry of V,V.Bogorodskiy and V.N.Rudakov (Zj-,TF '31-0,82,1960). During
'Inovam'~rrlt of the apparatus to awther locatior an acc-; 6ent occurred
,-ehicb torminated the tests. It is concluded tftal~
.,o-r-ads1--,',v P-tnd FCidakov has be-en. eonfiived. TIP.)
H -Wai te, who succeeded in meking meaq)- remkzit sa h,-
t a i -nua dqimilar results. nIn conclusion, the aurnors coDsiaert
their pleasant dljt to express their gratitude to the thcracred ~cien-
t a W'Pelsor
tist L-nd -gi-T) 0-1 -,-P.Boaor~.(-Iskly Aft T, ti ~z) s-, Lr
en
~oTmLnp tb~i York.' Orig.art.hasl' 2 fc-u'u'Las 1-71-"
Card V3

SUBIAITTM: 1ZAuge-4 EICL: 00
MR RE7 BOV: 003 OTHER., 000
Card3/3
SUB GODS: t5l,0'

BOGDRPP~Kll _Y~V. . red,
[Utstj of radioplqsical methods In oceanographic and ice
research] Primenenis radiofizicheakikh metodov v okeano-
graficheakikb I. ledovykh isaledovaniiakh, Leningrad,
1965- 106 D. (MIRA 18:12)
1. Leningrad. Arkticheskiy I antarkticheskiy nauchno-
isoledovatellskiy institut.

ACC-NRt A1160.10993 (N) SOURCE. CODE.:--- -ult/0213/66/006/00310551/0'052
AUVOR: Tsurikov, V. L.; Bogorodskiy, V. V.
1 ORG: none
TITLE: conference on physical investigalion methods of world's ocean waters and sea
and continental ice
SOURCEt Okeanologiya, v. 6, no. 3, 1966, 551-552
TOPIC TAGS: oceanographic conference, geophysic conference,
- - - - - ~ -= 's Eq / 42 R- Z--4 6-4c rR / c- Ae 0 Pe 12 r (f
ABSTRACT: The Second Inierdepartmental Conference on the Use of Radiophysical
Methods in Oceanographic and Ice Investigations took place on 14-18 December 1965
in Leningrad. The conference was organized by the Arctic and Antarctic Scientific
Research Institute, according to a resolution of the Main Administration of the
Hydrometeorologic Service. More than 350 persons from 56 organizations participated.
Problems on the use of radiophysical investigation methods and problems concerning
the electrical properties of sea ice were discuised in two sections and presented
in 58 papers.
SUB CODE: 08/ SUBM DATE: none
Card 1/1

ACC NRs
A1Y7OOOV,3 (A) soURCE CODE: UR/0046/66/OLI/~-,D/.,/O/.11/LV.15.
AUTHORS: Bororodskiy,0 V. V.; Galkin, Yo. 1.
ORG: Arctic and Antarctic Research Institute, Leningrad (Arkticheskiy i
antarktichoskiy n.-i. institut),
1MLE.- Investigation of the internzal friction of fee plates with a layer of snow
during bending vibrations
SOURGEt Akusticheskiy zhurnal, v. 12, no. 4, 1966) lal-4-15
TOPIC TAGS: ice, snow, vibration analysis, friction
ABSTRACT: The internal friction of homogeneous ice plates with a surface snow layer
was investigated during bending vibrations in the temperature region from 0 to -20G.
The values for the logarithmic decrement A . coefficient of loss F- , and the energy
absorption coefficient q) were determined. The determination is based on the i
known expression for the eigenfrequencies of bending vibrations Of PlateS
n2 (2n 1) 2YE h:
6) #1 =
/w
and the experimental data of V. V. Bogorodskiy (Uprugiye kharakteristiki I'da. Akust.
1/2 UDC:' 534.291-539.67:551.322

ACC NRt AIY7000243
Fig. 1. Lomarithmic decrement A as a function
of the temperature and amplitude of
vibration
vo
AP 44P 747 IIA7
zh., 1938, 41 19-23). Numerical values for and were detem, ined with
an experimentalinstallation consisting of a vibrator, sound receiver., and oscin-
graph. The experimental results are sur=rized in graphs and tables (see Fig. 1).
It. was found that the loss of mechanical energy in nonhomogeneous ice plates depends
olathe amplitude of vAlbration and the temperature. The inner friction of ice is
increased considerably by a surface snow layer, especially if i1o thielmoss of the
N
atier exceeds one half the thickness of the ice plate. The authors thank V.
for his valuable advice. Orig. art. has*. I table, 6 graphs, and 10
~."'e-'-'oquations.
SUB CODE: 20, 04/ SUBM DATE; 20.Tul64/ ORIG REF: 001
c.,j 2/2

130GORODSKIY, Ye.S.-, SUSHKIN, V.S.
Mechanization of assembling operations at the "Tizpribor" Plant.
Priborostroenie no.~:22-23 F 162. (MIRA 15-2)
(Instrument manufacture)

2109h
1,1110 21091 if 1'5
3/135/6 1/"/00-5/006/011
Aoo6/A 10 1
AUTHORS: Bykhovskiy, D. G., Bogorodskiy,-Yu. A., Engineers
TM,Et Gas electric cutting of metal plates
PERIODICALs Svarochnoye proizvodstvo, no. 5, 1961, 16 - 18
TM: The mechanized gas-electric cutting of over 100 mm thick non-fer-
rous metals and stainless steel was for the first time in the world practice
achieved with the aid of equipment developed by VNIIBSO, including an arc cutting
torch, a power supply source for the electric arc and a control system. Pouring
channels of 100 x 100 mm section can now be out off cast-iron, silumin, copper
and copper alloy castings with satIsfactory quality of the edges. The advantages
of the new equipment are; greater thickness of the material to be cut, higher
cutting speed, lower gas and, electric power consumption. Cutting is performed
with an are burning in the gas flow between a tungsten electrode and the work
piecot. The cutting process has the following technological pectiliarities: inde-
pendence of the arc current on the thickness of the out metal; correlation of the
thickness of cut metal and are voltage; the cutting process has to be condu,-~ed
at initial and operational speed. A formula is given showing the dependence be-
Card 1/4

21094
S/135/61/OW/005/006/011
gas electric cutting of metal plates Aoo6/Aloi
tween the thickness of the material and the are voltage-. Ua = -rr + B - 19 S,
where Uarc is the are voltage in v; S is the thickness of Me plAe in mm, A and
B are the coefficients depending on the composition and rate of the gas feed and
on the nozzle diameter of the are torch. The narrow range of regulating the opera-
tional current and the relatively wide ramge of changes In the are voltage are
specific peculiarities of gas-electric cutting, requIrIng new ways of considering
the problem concerning the electric are power supply source. Investigations car-
ried out in this direction proved that the most efficient power supply source is
a rectifier on t;emi-conductor valves and an improved control stray transformer.
This power source is efficient, light, small-sized, simple and reliable. VNIIESO
developed moreover a power source on the basis of multiampere selenium rectifiers
assembled by a three-phase push-pull circuit with 270 v idle-run voltage and stable
burning of the are up to 450 amp current; and a power source with ignitron recti-
fiern. Metallic ignitrons 0 -70/0.08 (1-70/0.C)8) and m-14o/o.8 (1-140/0.8)
assembled by various systems were investigated, including a three-phase push-pull
and a six-phase single-cycle circuit (Fig-are 3). The main deficiency of Ignitron
rectifiers is the need of a ballast rheostat. Therefore, they will remain in use
only until series production of sufficiently cheap silicon rectifiers will be or-
ganized. The new type aro-cutting torches present a series of advantages, such
as Satisfactory centering of the electrode in respect to the nozzle; reliable
Card 2/ 4

21094
S/135/61/000/005/006A 11
Gas eleciric cutting of metal plates AG06/A101
electric insulation of.the electrode and the nozzle; hermetic nozzle cooling,
system, intensified cooling and simple nozzle design. The T-2 arc torch (Figure
4) consists of two silumin castings containing the adapter with the electrode and
the nozzle. The insulation of1the nozzle and the electrode is achieved by the
use of epoxy resin. Furthermore the possibility.was studied of using high-temper-
attire fluoroplastic and super-poreelain insulators for are torches. The develop-
ment of the described equipment makes it possible to consider the centralized
cutting of sheet material so that savings of scarcemetal and a reduction of pre-'.'
paratory operation costs will be achieved, and a great number of metal cutting
mills will be liberated which pvesently are needed for mechanical cutting of metd2s
unsuitable for oxygen cutting process. There are 1 table, 5 figures, 7.rdfarences
4 Soviet and non-Soviet.
ASSOCIATION: VNIIE-30
Card .3/4

Gas electric cutting of metal plates
Figure 3:
Six-phase single-cycle circuit of ignitron
rectifier: I - ruse; 2 - magnetic start-
er; ~ - push-button set; 4 - transformer
5 - ignitrons; 6 - selenium rectifier; 7
- hydrorelay contacts; 8 intermediate
relay.
21094
S/135/61/000/ID05/006/lDil
Aoo6/Alol

BYIQIOVSKIY, D.G., kand. tekhn. nauk; E~ ~GORODSKIY, Yu*A,,, Jnzh.;
ROGOV, V,D,p Inzh.
Hand operated gas electric cutting torch. Sudostroenie 30
no.11:49-52 N 164. (WRA 18:3)

ACC NRiAR6029333 S.OURC.
AUTHOR: Bogorodskiy, Yu. L.
Am,; P'21-signal limiting
SOURCE: Ref. zh. Radlotakhnika ielektrosvyazt, Abs. 5B287
REF SOURCE: Tr. Vses*. n.-i. in-ta magnitn. zapisi i takhnol. radioveshch. :1 televid.,
vyp. 303), 1965, 41-55
TOPIC TAGS: FM signal, iM--4-4- FX receiver
Ls
ABSTRACT- The limiter in question comprises several stages loaded by resonant
circuits shunted by diodes. A circuit is suggested and investigated which ensures
a stable passband in a wide dynamio range of input signals. The effectiveness of
using rejector circuits in each Btage of the limiter is demonstrated.
A. K. [Translation of abstract]
SUB CODE: 09
Card UDC: 621-374-34

BOGOROV, G.V.
Boring the earth's crust on the ocean bottom. Okeanologiia 2 no.!:
190-191 '62. (YdRA 15:2)
(Mohole project)

ILIINI A.V.; EOGOROV.-.-G,V, ,
Recent photographs of the bottou-of the Atlantic Ocean.
Okeanologiia 3 no.2s346-348 163. (MIRA lds4)
(Atlantic Wean--Ocean bottom) (Photography, Submarine)

ILIIN, A.V.; BOGOROV, G.V.
New data on the bottom geomorphology of the abyssal Nares plain.
Dokl. AN SSSR 148 no.6sl392-1393 F 163. (KIRA 16:3)
1. Akusticheakiy inBtitut AN SSSR. Predstavleno akademikom D. I.
Shcharbakovym.
(Atlantic Ocean-Ocean bottom)

&s.
00
W-0-M-WWO 10-0-0-0-0-WANAM-M
Its& p I 6101fatilau"
A iL
WWWWWWWWW - - - -
IF p--v -a m x io irs W-tv 41 -it U--iii
-it u.
-00
nee
zoo
nee,
zoo
goo
goo
tie 0
1104141
wommis.
c-d C., IDd-). FeCtshm I Akes'Awas
INS. 9. 35-7.-Wetfiry revaimmmE. a wqpnnl
I,,-- d"ns-cal ulft -pbasis an an adeqmte suppi
of vifazWm A, D. and C.
G. m. Kasokpoff
nee
IS So AV 00 Ali*, load 0 4 a Iar 0 9 A aI VZ
0 000 060006 ***is* Ole 01414041 a a so 0090000000

NIXOLAYIV, A.H.; B I., professor, zaveduYushohiy; SMOTA, H.T., Dro-
fessor, direkI*CorF&JW4~---I
Role of consultation stations for women in the prevention of stillbirth.
Vopopediat. 21 no,3:43-50,M (MMA 6--7)
'y-Je 153.
1. Akashersko-ginekologichookaya klinika Leningradskogo goeudaretvennogo
pediatrichookogo meditainskogo instituta (for Nikolayev and Bogorov).
2..Leningradskiy gosudaretvannyy pediatricheakiy maditainakly institut
(for Shutova). (Stillbirth) (Obstetrics)

7'
v
FIGURNOV, X.M., professor, radaktor; KAMMLISHTAK, A.A., professor,
I.I. professor,
zaeluzhenW dayatell nauk. redaktor; j
redaktor; PWTROV4USMKOT. N.A.. professor, r~ namo-rll MAUROV,
R.R., doteent, radaktorl TMNOVA, Ys.So, doteent, redaktor;
RUDAKOT, A.Y., redaktor; KURASH. G.A.. tekhaichaskiy redaktor
[Problems In the neurohumoral rwlation of physiological and
pathological processes of the sexual functions in vomen] Toprosy
neiro-tgworallnot regullataii fisiologicheakikh I patologichookikh
proteassov shenskot-polovot sfary- LIoaningrad) Goo. izd-vo mod.
lit-ry. Iganingradekoe otd-nis. 1936, 146 pe (HLRA 10:3)
1. Chlen-korrespondent ANN SSSR (for ligumov)
(MVOUS SrSTM) (MITOnInRYMUNS-DISBASIS)
(HaRmuss, six)

BOGOPIOV, Isay Isaakovich
[Wor"en's lVglene] Gigiena zhenshchiny. lzd.3., ispr. i dop.
Leningrad, Ob-vo po raspr. jolit. A nauchn. zraiiii 1960 Clfl ..
. 1~ '
(VIRA !I,: I
'I",; frif-IMT)

I
BOGOROV, Isay Isaakovich
[Pediatric gynecology] Ginekologiia detskogo votreata.
Leningrad, Medgiz, 1960. 266 p. (MIRik 14:1)
(GnW.OLWY)

.0
BOGOROV, Is Isaak of.; VOROBIYEV, G.S.., red. izd-va;
- ZHIMA, A.M., tekhn. red.
(Female hygiono]Gigiona zhenshchiny. Izd*4-t ispr. i dop.
Leningrad, Ob-vo po raspr. polit. i naucbn. znanii IRSFSPy
1962. 66 p. (WOMEW-HEALTH AND HYGIM) (MIRA 15:9)

BELYAYEV, Ye.I., prof. [deceased]; BADYUK, Ye *Ye 13QW-Qy.,
j --jj_ts
prof.; BUBLICHENKO, L.I... prof.(deceaffe~j,--ILIIN, 1.V.,
dots.; KEYLIN, S.L., prof.; MAZHBITS, A.M., prof.;
MALININ, A.I., zasl. deyatell Kaz.SSR, pfof.; MOSHKOV, B.N.,
prof.; NIKOLAYEV, A.P., prof.1 PERSIANINOV, L.S., prof.;
POKROVSKIY, V.A., prof.; RPLYAKOVA, G.P., kand. med. nauk;
RAFALIXES, S.B., dots.; KHASXIN, S.G., prof.; SHTERN, I.A.,
prof,
[Multivolume maralal on obstetrics and gynecology) Mnogo-
tomnoe rukovodetvo p0 akusherstvu i ginekologii. Moskva,
Meditsina. Vol.3. Book 2. (Pathology of the labor and post-
natal period. Pbysiology and pathology of the newborn infant)
Patologiia rodov i poslerodovogo periods. Fiziologiia i pa-
tologiia novorozhdennogo. Pt.l.[Patbology of labor] Patolo-
giia rcgoff.- "".- *5 P.-v; (MIRA 17:7)
Je~A- f ~ I
1. Chlen-korrespondent ANN SSSR (for Permianimml ~Uystlt-
tellnyy chlen AMN SSSR (for Nikolayev).

I BO-GOROV, L.V.
Methods of concentrating phytoplankton samples. Gidrobiolo
zhur. I no.401-72 165. (MIRA 18t10)
1. Moskovskiy gosudaretvennyy universitet.

ZENWICH9 L.A.;. BOGOROVp V.Gol SSTODMj I.B.
Swmn Vladimirovioh Brueviohl on the fiftieth anniversary of
his 80iontifio activity. Okeanologiia 3 110-51931-932 165, -
I
(WRA 18i11) .

130GOROVj, Vo Go
"The Biological Seasons In the PlanIcton of the Seas on Various Latitudes, a
Ddkl. AN SSSRj, 19., No.8p 1938

BDGOROV, V. G.
"Diurnal Vertical Migration of Zooplankton in Arctic Seas," Dokl. AN SSSR,
40, No-4, 1943
I.ab. Oceamlogy

BOGOROV, V. G.
"Distribution of Brackwater Planktonic Fauna in Siberian Po;ar Seas," Dokl.
AN SSSR, 44 No.5, 1944

BC-G ',LI*L-, V. G. D "S
OkcanoErafichcstde issleclOVIMIla Ia-dadu.,,,dl-. Kaul.
(In !dmdU=iI-a N'aw: SSSR. Vsesoiuznyi ko.,;-.itat oa p~-OvciL-.11-
iiU 22-U-Ietiaa Alcaderaii Nau:~. GeO-Lor-o-,t,-orraficiiez;:de
L - ) Q u u
nauia. ':0skv-, 85 92
D7C:
C, Soviet Part 1., 1. 5j, U.11cl.

BOGOP6V, VA I'A
Marine Biology
"Diurnal Vertioal Migration of Zooplankton in Polar~
Sias," V. 0. Bogorov, 8 pp
*Trudy, Instituta. Oksazol" Vol r
PIAnktoh'zak6 ahily-ioirtloal x1grationsp sinking t
ds~thsd,~klng defatA asoending- to surfsoe at nights
Polar conAltions '*ovided ideal laboratory for sup_~.
vor of-theory that lIght'le,factor determining +,his:
*d -]Db--- e'durIng"I -hour'dayligh um.-
t a
gratIon. .. earva oh -4
as r'- -damns ra ~thit *1^ i~6'does not occur vhen
t grat
Allot I x Jhh ponstant., Migration resumes during
polar autvm.
5M9

BOGOIOV ~ V.
. t'Vertical Distiibution of Zooplankton and the Vertical Distributlon of Ocean Wateral's
Tr. In-ta okeanotogii ZTransadfions of the Institute of Oceanography
./, No 2j, p 43) 1948.

USOR/Biology Tau.na, Sea May/Jtm 49
"Periew, of Professor L. A. Zenkevichle Book,
'Fwma of the Seas and Their Biological Produc-
i1vity, I" V. Bogorov, 2J Vp
vZool Zhur" No 3
Reviews favorably 'subject book, which is Vol.1i of
series, "Seas of the USSR." Work is a combination
of Bogorav Is own study and that of many impor-'..
taut Soviet scientists. Covers general chwacter-
istics of the sea,,history of the study, pbysico-
geographical, hydrological, bydrochemical,.and'
fipologJ-ca:L characteristics, floira*,'fax-not, '-prob
15=
UMR/B~ology F-a-, Sea (Coutd) may/J=~49
of,genesis, apd, zoogeographical cb acteristicO
of many seas of the USSR. Vol 11-1 will c aver
faima of far northern seas.
Jal 15#6

9~i. tryP Hydrology - Fisherieo,
Jul 51
Chemicals
"Water," Prof V. G. Bogorov, Laureate of Stalin
~Prize
"Nauka I Zhiznl" Vol XVII1,No 7, PP 14-16
In addn to the-existing huge Shcherbakov Sea
Lifybinsk reservoir7, other artificial int seas--
the Kuybyshev (500 aq km), Stalingrid (600 eq km)
and Tsymlyansk reservoirs--will be created in'
the near future. On the basis of product value,
the USEM f ishing industry is the lot in the
world: 250 species of fish are caught In the
199"
USSR/Chenistry, Hydrology Fisheries, Jul. 51
Chemicals (Contd)
US,SR as; ccmpared with 121 in the US and 36 in,
England. Large chem ecimbines, have been built
:in areas where salt water which has been coned
by evapa in available. At Xara-Bogaz-Gol
(Caspian Sea), x1rabilite (Glauber-salt) is
duced on au' extensive scale.- It serves 'for tbal,
sanuf of soda and other products.'
CL. 19W9
C
9=_

DMOROVp VENYAMTN ORTGORIYEVMH
Science
Animal life of seas aM ocesm and its economic sipifioance; Moskva, Goo. izdvo
geop. lit-ry., 1952.
9. Monthly List of Russian Accessions, Library of Congress, October -195$~ Unclassified.

1. BCGOROV, V. 0.
2. USSR (600)
4. Marine Fauna
7. Deeps of the ocean. Geog. v shkole no 6, 1952.
9. Mon~Ul List of Run-slan Accessl2na, Library, of GongraBs, MArch 1953, Unolaasifled.

BOOOROV$ V . 0.
"Life In the Seas.." Zool. zhur., 31, No.l. 1952. Reviewed by Ye, N, PavlovskLy

1. BOGOTROV, V. G. , Prof.
2. USSR (6oo)
4. Karelin, D. B.
7-- Seas of our country. D. Karelin. Reviewed by Prof. V. G. Bogorov. Vokrug
sveta No. 3, 1953.
9. Monthl List of Russian Accessions, Library of Congress, June -1953, Uncl.
m

UM/deography - Scientist, Obituary May/Jun 53
"Academician Petr Petrovich Shirshov (deceased),"
~Q)V- G. Bogorov (reporter)
Iz Ak Nauk SSSR, Ser Geog,, No 31 pp 69-70
Reports obituary of Acad P. P. Shirshov (25 Dec 1905-
17 Feb 1953), who was well known for his polar inves-
tig6tions, hydrobiology, oceanography, and state ac-
tivities.
25ft65

SUSLOV, B.N.; BOGOROV, V.G., professor, redaktor; KAMM. Ta.M., redaktor;
KCKnRrrs]MYXO,illr.!?".':"tekhnicheakiy redaktor.
[Water and its use] Toda i so primenenis. Pod red. Y.G.Bogorova.
Moskva, Voennoe izd-vo Ministerstya oborony SSSR, 1954. 104 p.
Niar of nal (VTRA ?-.11)
(Water)

BOGOROV. Veniamin Grier r1yevich; MAMITNTA, 0., rodaktor; HIKHATLOVSKAYA,
rrdaktor
(Life of the G*oal MAsn' morta. [Mookval Izd-vo TsK VIKSM "Molo-
dala gvardiia," 1954. 299 p. (HLRA 8W
(Marine biology)

BOGOROV,V.G.
V ~ . WAWWWOWMI~
Fatr Petrovich Shirshov as a scholar and administrator in science.
Trud7 lust okean. no.9:3-4 154. WAA 8;6)
iShirshov. Petr Petrovich, 1905-1953)

BOGOR07 V.PL~-, laureat StaUnskoy premii, professor; D013ROVOLISKIY, A.D.,
dortor geograficheskikh nauk, professer, radaktor; KAZA OTA, V-V-,
tekhnicheekly radaktore
[The man] Okean. Mockva, Voennoe izd-vo Ministeratva oborony
Soiuz- SRR. 1955. 139 pe (MIRA 8:4)
(ocean)

ASLLNCVA,N.Ye.; BOGOR(N.V.G.; ZUSSER,S.G.;
N
--NOMMOMOWW"
Scientific and technical research of
Gidrobiol.ob-va no.6;17-22 155.
(Mesiatsev, Ivan Illarionovieh,
KINNOVA,M.V.; STAROSTIN,A.D.
I.I.Mesiatsev. Trudy
(HLRA 8:9)
1885-1940)

BOGCROV,V.G., professor
"Vitiax'" in the Pacific Ocean. Vokrug oveta no.8;7-11 Ag'55,
(MMA 8: 12)
(Pacific Ooean--Deep-sea deposits) (Pacific Ocean--Marine
Biology)

BODMOV, T.Gt; EXEMIEW, K'T.
Pr6thictive capacity of phytoplankton in the northwestern region*
of the Pacific Ocean. Dokl.An SUR 104 no.1:141-143 S 155.
(MM 9:2)
i4A6tI%u% okeanologit Akadmil nauk SSSR. Prodstarleno akademiken
A.A.Grigorlyevyn.
. (Pacific Ocean-Plankton)
I