SCIENTIFIC ABSTRACT BYUSHGENS, S. S. - BYVSHEV, S.V.

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• Collection: Scientific Abstracts
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• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 12, 2000
• Sequence Number: 5
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

BYV3H:;3!S, S. S.
0b izgibanii poverilnostey na glavnom osnovanii. N'. 1-79.
Six cc!-taines ftmilles invariables de tiourbes. Yataza. SB, 32 (1?25"', ~,V-352-
Sur !as surf'-Icus de "Uanphi. C.R. Acad. Soi., 2013 'l,,6 7,;2-76!4.
'-tcjrno=o pc'.v-ft. DIT,
Geomet 1-ya vek
Goometriya vektornop polyu II DAN 43 (1 )45), Wo.3- 404.
7 -95.
Geo:-,etrilya vektornogo polya, Ser. YvItem. 10 13
llathow~;~'Loics in thn U35R, 1~17-1947
edited by Kurosh, ',.G.,
I!
Alarklishevich, A.I.,
Rashevskiy, -.K.
Ylos co-47 Leningrad, 1948

ri~~--tf dii _- I -
on ons

BYUSM3NS, Sergey Sergeyevich, 1882-
[Aluilytic geometry] Anaiiticheeksia geosetriia. Isd. 4., perer.
Mos)-va, Gos. Isd-vo tekhn.-teoret. lit-ry, 1947. (KLRA 7:8)
(Geometry, Analytical)

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(1947);
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M,sIIVj8) S. 8.
Fle nsAS.. g. I(Cn a siAral currnri.,"' Mauch. (VnnR. rirlrnrnf~lirat.
in. Villyarsa), Vol. XIIII, 194q,, p. 71-90
SO: U-3264 10 April 51, (Letopis tZhimnal Inykh Statey, No. 4, 1949).

BMHGENSI S. 15.
NNomoiraphic Manual,," Moskva Itd.

BYUSHGENS, S. S.
*Gemetry of Adiabatic Flow,,,* Uch. sap. Moak. un., No.148, 1951

Geometriia acLiavaticheskugo potoka. (Moscow. Universitet. Uchenye zavi~,ki, 19.51.
no. lh8., Matematika, v. h, p. 30-52, bibliography)
Title tr: Geotietry of adiabatic flow.
Reviewed by D. J. Straik in Mathematical Reviews, 1953, v. lb, no. 3, p. 328-329.
Q&0.M8z)8 1951, no. 148
SO: Aeronautical Sciences and Aviation in the Soviet Union, Library of Congress,
1955.

USSR/Mathematics - Tensor 11 Jun 52
"Flow Lines. Il," S. S. Byushgens, Sci Reis Inst of
Math, Moscow State U imeni Lomonosov
"Dok Ak Nauk SSSR" Vol LXXXIV, No 5, pp 861-863
In the previous article C'Dok Ak Nauk SSSR" Vol
LXXVIII, No 5, 1951) the author attempted to es-
tablish the characteristic geometric properties
of congruence of flow lines of the stationary flow
of an ideal incompressible fluid. However, only
one of the conditions obtained by him contained
geometric elements of congruence, which was not
able to permit him to exclude kinematic elements,
223T68
He shows here that by way of a small variation in
applied method one can obtain both conditions in-
purely geometrical form. Submitted by Acad A. N.
Kolmogorov 10 Apr 52.
U;
M
P4

7~ 66 (at
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.
A.
h - see
e con
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Uh eterm
i6d suffic
n
till M-al-of

e curvim inte~s6~~tikilv,-
:~ftthd~'inatWrf -,N
re tlla~a. e, Ines 0 cum ure:
_set
04
-~f thc*rnptotic fincj: Of
ci:~bii~Arf~eii
'di tliat case the'
a norn an n
aid Cobgruent
normaL7_ j eso'. lines o curva uii,irc,
yinb-IficW. Ner
congruence is
4 d
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4-of'stra '.1it lines..",

1.1. thee
red to be formulated h

Call Nr: AF 1108825
Trafisaet:Lons.of t1je Third All-union Mathematical Congress~t-(Cont.)moEjrcFw,
Jun-Jul '56, Trudy '56, V. 1, Sect. Rpts., Izdatel'stvo AN SSsR, m cow, 1956, 237 pp.
Berezman, A''.. H. (Kemerovo). Laplace Transformation inl-
Applied to TransforrAtion Fibered Congruence Pairs. 140-141
Mention is made of Finikov, S. P.
Blank, YiL. F. (Jetarlkov). On Congruences 141
Borisov, YU, F. (Leningrad). Parallel Shaft of Vector
and the Curves on Irregular Smooth Surfaces. 141-3.42
Mention is made of Aleksandrov, A. D.
Borisov,/Yu. F. (L-eningr0d). Geometry of Semineighborhood
in Two-dimensional Manifolds of Bounded Curvatures. 142-143
sh ene- S
~ f=(Moscow). Congruence Lines on the
A
v 0~
- f SM
y of Surfaces. 143-144
Card 46/Bo
41-

AUTHOR: Byushgens, S.S.
80205
S/038/60/024/02/03/007
TITLEt. The Geometry of the Instationary Flow of a Perfect-Incompressible
Fluid V
PERIODICAL: Izvestiya Akademii nauk SSSR, Seriya matematicheskaya, 1960,
Vol. 24, No. 2, pp, 171-202
TEXTz 'After having reduced the geometric structure of a stationary flow in
(Ref. 2) by consideration in a movable tripod and application of the differ-
ential geometric methods of Cartan to a purely geometric investigation, the
auth6r now extends this method to instationary flows. The hydrodynamic
equations of motion are referred to a tripod depending on time. The author
introd-ucea the notion of the eddy-current plane of a point of the flow
region (_i"C. contains the directi(.,-~ of velocity as well as the direction of
the eddy in the-considered poin-.1. The author gives examples of instationary
flows for which in every moment the eddy-current planes of every point
envelop certain surfaces% the eddy-current surfaces.
N.I~ Ale_~.s~_.yev and B.K. Uladziyevskiy are mentioned in the paper. There are
7 referen-3es S 4 Soviet, 2 American and 1 Roumanian.
PRESENTEDz by P.S. Aleksandrov, Academician
SUBMITTED: January 19, 1959
Card 1/1

ARIYELI, N.Z.; BYUTNER, R.K.; KONSTANTINOVp A.Re
Methods and results of the spectral characteristics of
turbulent pulsations in the lowest layer of the atmosphere.
Trudy GGO no.244:59-67 163. (MIRA 17:6)

; y D. , . ; -BYIUTN,~ti , r!,,K.
Turbuleu,.~a In J-t streaTb in i-ne j-'rezence of ~ -,.: - ; ,d
!- - - . W-!-
f "i
sh2 f L. Trud-v ri(.-,.15:-)- 63-63 C". 1 1 . 1 ,7,
. I . .- I I .

IN.' .; BVITWX, K.K.; 13. p.
7
D
etermining thp. v-comcnnnts of wind velocity from ILruct.ural.
measurements. Trudy GGO no.150.69-z"'? ' 6-4. 1?.7)

BY'l j I N-Vlii I E . K .
..aponds.~~,2jr~ 3f t.hF ex---nt, nC the d~.5tw~rsion -,f* -us c;m-itte-i
by a constant. scurce or. tr~A time interval of -.hA-
Trudy G~Xj C ciz,. .

L 5022=~6 EV1T(11/rCQ G#
ACC NR U'5024882 SOURCE CODE: UR/2 531/65/000/171/003 2/003 7:
AUTHORSI Laykhtmanj B-vutner
-ORG Min g2op aya
_RqK_ enjnjp--ad (Glavnaya geofizichesk
fiysi~al Ob yA~or
observatoriya) 14-4
iTITLE: Basic criteria defining the intensity of turbulence in a mountain region
SOURCE. Leningrad. Glavnaya geofizicheskaya observatoriya. Trudy, no.
-171., 1965.
Rezul'taby incledov6niya atmosfernoy:burbulentnosti na vertoletnykh trassakh
:)!(Results of the investigation of atmospheric turbulence on helicopter routes).,
32-37
TOPIC TA,"jS. wind, atmosphere, atmospheric turbulence, mountain atmospherics,,
meteorology
ABSTRACT-t An effort is made to coppite the characteristics of air currents in
mountainous regions. The study avaida the use of an oversimplified terrain model
such as one in which a mountain ridge is treated as a single obstacle of one form
or another. The authors take the approach:that the complex structure of an air
1'Card- 1/.4.,-- J

L 5022-66
J~_ -
ACC NR: -AT502h882
stream in a mountainous area may be represented as a certain smoothed motion U
upon which are superimposed macroscalar pulsations U1. These pulsations are the
result of the current break op upon incidence with the mountain ridge. Hened, the
i.mountaina'are visualized as a lattice:wherein the-basic generation of turbulence
energy ocau,rs in a layer ranging from,a certain mean height to the mountain
summits, Above this layer the inflow of enorgy of turbulence is caused by diffu-,*,.
The
sion. from below. This pulsavon-diffusion concept is depicted in Fig. 16
Fig. 1. 1- the layer
in which the basic
pulsation energy
-originates, Il- the
layer in which
turbulence energy
diffuses from below;
- ~10 III- free atmosphere.
_qard 2A.-..-

L 5022-66
AGG NRt AT5024882
process is be6t,q*uantified by a judicito of properly selected-parameters.1
iIt is desired to establish the physical"dependency of the mean square wind gust
U12 up
on physical quantities ~hicft may be rt,~adily evaluated. A discussion of the
necessary parameters is-given and U12 is written as a function of six dimensionod.
param-c-bvra..
L,; U; z;, w,;
Te
P
where L(z) is the vertical* c6atiiiiolon parameter given by
y). 2
a sea level and h is thet mean.
where h(x y) is the height of a,relief point abov
height of the mountain region above sea level. The variable z is the height
measured from 3, ())z is the-Coriolis parameter, and R/(ocp is the radiation
balance and thermal nonuniformity parameter. The functional ation is transm-
equ
Iformed t1irough considerations of nondistinct stratification and thermal convection,t
Wind gust data from the I-lay) 1962p a
xpedition of GGO) NIIGVFI NGUI and Ts.&O in
Crimea aracompared in a correlation analysis* The authors claita only that the
I-results.of the correlation do not contradict the validity of the model. ~Orig. arto",
Ihas. fi
2 gures, 5 equations,, and I table,

i '-'
~1
2
i -
OTH RM. 001 1
i

ACC NR: A!,-, ~ - ,5 SOURCE CODE: UR/0362/66/002/009iO993/0996
AUTIMR: Ariell, N. Z.; 3yutner Z. 1'
ORG: Main Geophysical Observatory (Glavnnya goof izichaskaya observatoriya)
TI'I'LE: Roliti~onshlp bon;oen Lagrangian correlation and maxima of
ouler space-time correlation functions for surface layer of the atmosphere
SOURCE: AN SSSR. Izvestiya. Fizika atmosfory I okeana, v. 2, no. 9, 1966,
993-996
TOPIC TAGS: Lagrange equation, surface boundary layer, correlation function,
atmospheric diffusion
SUB CODE: 04,12
A33STRACT: This paper presents an evaluation of the decrease of the maxima
of space-time correlation functions with an increase of time on the assumption
of an absence of individual changes in moving volumes. It was found that
the decrease of the maxima observed in the experiments in the surface layer of
the annosphore (tho decrease of the height of the maximum occurs for Lwo
reasons -- due to the presence of individual changes in volumes during
the tire of-their movement between two points; fluctuations of rho value
and direction of the vector U of current velocity) is substantially greater
t1an computed with the above-mentioned assumption. Accordi 1 tile
Card 1/2 UDC. r'7
01~9_5 0-

ACC NR: AP7010705 - - - ----
principal role in this effect is played by individual changes.
has: 2 figures and 6 formulas. [jPRS. 40,29g
Orig. art.
C-rd 2/2 . . . - - - .. --- - . --- - - 1- - -- - -- .

-13ITTINER, E. K.
USSR/Nuclear Physics - Optics,
oct 51
110ptically Active k1olecules in External Field," 12. V. Volkenshteyn, E. K. 33'Utner,
Leningrad State U
"Zhur Eksper i Teoret Fiz" Vol M, Ib 10, PP 1-132-1-138
Discusses behavior of optically acti,,,e gas or soln in external field taking into
account elec dipole and quadripole and magnetic dipole of polarizin,'7, InecuJum (cf.
M. V. Volkenshteyn, ibed. 20, 342, 1950, and "Folecular Optics" 1951). Authors
acknowledge A. T. Umorev's advice. Submitted 22 Nov 50.
PA 197196

UM/Pbyiieu- Cryat~p&*y I. Yeb- 51.,
"Optically'Active Crystals," M. V. Volkenshteyn,
E. K. Byutner,.Leniugrad State U ineni A. A.
Zhdanov-
!Dok Ak Nauk SSSR- Vol--IXM, No 4, pp 515~-517
Only accumte theory of rotating crystals in
that of Born. Exptl data 6n. relation between
crystallic:spectria and rotating capacity vere
found by Saiaoylov, studying uranyl acetate at
temp of liquid helium. Sub.mitted 20 Nov 50 by
Acad S. I. Vavilov.
178T107

PA 2`36T85
VSM/ftnies Dichroism nov 52
"Circular Dichroism in Crystals," M. V. Vol'kenshteyn
and E...K. Byutner, Leningrad State Univ
"Zhur Eksper i Teoret Fiz" Vol 23, No 5, PP 584-587
It is shown by means of a classicial model of a system
of coupled oscillators with helical symetry that
erystals in the plane of polarization may possess a
.strong circular dichroism. Received 13 May 52.
236T85

Physics
Card 1/3, Pub. 22 14/63
Authors i Gotlib, Yu. Ya.,- Vollkensht-eyn, M.B.; and Byutner, E.K.
Title Anisotropy of the Polarizability of chain molecules
Periodical I Dok..,AN SSSR .99/6, 935-938.. Dee 21, 1954
Abstract i An analytical derivation of the polarizability of a chain molecule
containing a number of equal links characterized by a symmetrical
voltage of the inner rot is presented. The matrix
ation (V(-!? )=V(-!r
and tensor method.was used for the computations. Five references;
3-USSR (1942-1953). Table.
Institutions: The Leningrad State Pedagogical Institue im. A.I. Gertsen; The Institute
of the Figh Molecular Comoounds of the Acad. of Scs. of the USSR
Presented by; Academician A.F. loffe, September 18, 1954

30) SOV/33-35-4-6/25
AUTHOR: Byutnerp E.K.
TITLEz The Dissipation of Gas From Planetary Atmospheres I~ The
Dissipation of an Isothermal Ideal Gas in the.,Central Field
of Gravitation (Dissipatsiya gaza iz atmosfer planet.I. K
voprosu o dissipatsii izotermicheskogo ideallnogo gaza v
tsentrallnom pole tyagoteniya)
PERIODICAM Astronomicheakiy zhurna,191958v Vol 359 Nr 4, PP 572-582(USSR)
ABSTRACTs The present investigation is based on the Lennard-Jones
method CRef 37 for the calcualtion of the rate of di"ipat~ion
from planetary atmospheres. The author gives an expression
for the rate of dissipation of particles from each layer of
an ideal gas in a central field. Re considers the deviation
of the velocity distribution from the equilibrium Maxwell
distribution. The number of particles which acquire by colli-
sions, velocities larger than the critical velocity of escape
vor is determined. The rate of dissipation is less than the
rate of dissipation of the gas is in the state of equilibrium;
the factor is 0-27 if v or has the double value of the mean
Card 1/2 velocity of thermal motion. The difference of the two rates

The Dissipation of Gas From Planetary Atmospheres I. SOV/33-35-4-6/25
The Dissipation of an Isothermal Ideal Gas in the Central Field of
Gravitati'on
of dissipation decreases rapidly, if the ratio of vcr to the
thermal velocity increases. The author particularly refers to
the papers of V.A.Krat ZRef 57 and S.B.PikellnerZleflV
He thanks Professor V.A.Krat for suggestions.
There are 4 figures, 2 tables, and 7 references, 2 of which
are Soviet, 3 English, 1 American, and 1 German.
ASSOCIATION:Leningradakiy gosudarstvennyy pedagogicheakiy institut
(Leningrad State Pedagogical Institute)
SUBMITTEDs April 17, 1957
Card 2/2

BYUTIM, E. K., Candidate Phys-Wth Sci (cliss) -- "The dissipation of gases from
the atmospheres of planete. Leningrad, 1959. 10 pp (Min Higher Educ uSEp,,
Leningrad Pedagogical Inst im A. I. Gertsen, Chair of Tbooretical Phys), 150
copies (KLv No 24, 1959, 124)

9
30)
AUTHOR: SOV/33-36-1-11/31
T,ITLE: The Dissipation of Gas From Planetary Atmospheres. II. The Total
Velocity of Dissipation of Gas From a Planetary Atmosphere. The
Problem of Terr4strial Helium
PERIODICAL: Astronomicheskiy zhurnal, 1959,Vol 36,Nr 1,pp 89-99 (USSR)
ABSTRkCTt The author gives a general expression for the velocity of gas
dissipation from a planetary atmosphere. For two cases he ,
calculated the-velocity of gas dissipation and the thickness and
position of the layer from which the di esipating process is most
effective: a) a single component atmosphere, b) an atmosphere
composed of a heavy gas with a small admixture of a light gas.
Under equal conditions in the case b) the thickness of the layer
is less than in the case a). The thickness of the layer always
increases with an increasing kinetic energy of the gas. Further-
more the distribution of the intensity of dissipation along the
effective layer and the position of the layer of maximum
intensity are determined. Finally the possibility of dissipation
Card 1/2

The Dissipation of Gas From Planetary Atmospheres. 11. 30-7/33-36-1-11/31
The Total Velocity of Dissipation of Gas Prom a Planetary
Atmosphere. The Problem of Terrestrial Helium
of helium from the earth's atmosphere is discussed.
The author tharflis'Professor V.A.Krat for adviock
There are 4 figures, 1 table, and 23 references, 6 of whi'ch are
Soviet, 9 American, 3 English, 4 French, and 1 German.
ASSOCIATION:Leningradskiy gosudarstyennyy pedagogicheskiy institut imeai
A.I.Gertsena (Leningrad State Pedagogical Institute imeni A.I.
Gertsen)
SUBMITTED: November 29, 1957
Card 2/2

30)
AUTHOR: Byutn SOV120-124-1-14169
TITLE: On the Dissipation of Hydrogen From the Atmospheres of Planets
(0 dissipatsii vodoroda iz atmosfer planet)
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 124, Nr 1, PP 53-56 (USSR)
ABSTRACT: A. B. Meinel (Ref 1) discovered hydroxyl bands in the luminescence
spectram.offthe nocturnal sky, and this indicates a dissociation of
the water vapors in the uppar strata of the earth's atmosphere. The
present paper investigates the problem concerning the quantity of
water lost by a planet. The altitude of the stratum in which photo-
dissociation of water takes place and,the average number of H 20 mol,
cules decopposing in '.the time unit can eaai-. be estimated from the
da-ta at present available. The total probability of the photo decay
of a 11~ 0 molecule'on.the boundary of the earth's atmosphere amounts
-6 -1
to 2.5-10 3ec.....The.photo decay of water occurs mainly in the
layer of between 70 and 80 km altitude under the action of a radiati
of 1860 to 1760 1. However, photodissociation does not disturb the
uniform distribution of H20 particles with respect to altitude.
Card 1/2 A formula is then derived for the dissipation F of atomic hydrogen.

SOV/20-124-1-14/69
On the Dissipation of Hydrogen From the Atmospheres of Planets
From the layer in which dissociation of water occurs, a diffusion
flux of atomic hydrogen is directed upwards. It essentially in-
fluences the distribution of atomic hydrogen with respect to
altitude. A formula is written down for the amount of this diffusion
flux. For the mate of dissipation of the hydrogen of the earth
F~109 CM -2 sec -1 -is found. If'such a steady flux has been lasting
already for 4.10 9 years, hydrogen of 6.5-10 25 molecules of water
has already evaporated into space, which corresponds to about 1 %
of the quaptity of water existing on the earth. The author thanks
Professor V. A. Krat for his valuable advice.-There are 23 refer-
ences, 8 of which are Soviet.
ASSOCIATION: Leningradskiy gosudarstvennyy pedagagicheskiy institat im. A. I.
Gertsena (Leningrad State Pedagogical Institute imeni A. I. Gertsen)
PRESENTED: August 8, 1958, by V. G. Fesenkov, Academician
SUBMITTED: May 30, 1958
Card 2/2

S/020/6'./138/009/007/025
B~.WB205
AUTHOR: Byutner, E. K~
TlTLE-. Time of attainment of a steady amount of oxygen in planetary
atmospheres containing water vapor
PERIODICAL: Akademiya nauk SSSR, Doklady, v, 138, no, 5, 496", 10-50-11053
TEXT: In a pre7icus paper, the author calculated the amount of hydrogen
vapor decomposing in the -,er-restrial atmosphere at an altitude of 7(;-80 km
under the action of solar Tadiation. (DAN-. 124, 55 (!959))- At present, the
content of 0, in the tervestrial atmospher; is so high that 'the amount of
0,
', produced by photodisintegration of water and the amount loat due to oxi
dation on the ea7~h;s surface are in eqiLUibrium. It is, however, clear
that the 1.berat-ion and absorption of oxygen in the biosphere exceed the
two above-meritic-ned processes appreciably. In this connection, the ques-
tion of whether the accumulation of a noliceable amount of oxygen in
the terrest.-La: atmos1heze as a result of photodi sint ee,-rati -'n of H20 was
card /,P)q

S/020/6 J'8/005/007 /025
11-ime of' ;i-zta~~nmen- of a 3104/B20'.1
poes4~ble pn~:r tc the evolutic-n of organic I-fe, The pr-serit paper is de-
voted to this probleir, The author estimates the -~erlod of time required
for the of -,). gIvr.r. q-,lantity of oxygc-n in -.-he Earthis atmos-
phere as a result of phr.-,,~Is.~nt,?gration of H 0. taki-PE oxida'~ion on the
2
Earth'-- s--irfa-e intc -ccount The aithor makes use of 7e,,ent data concern-
ing the spe~?-tra_, composition cf solar radiation., and assumes that at an
altiTi~de -,f "~-80 km. th,~ atmo,sphere i~ completely intermixed. and the con-
tent of wuter vapor a~.,co-untsq for 2%10--% of the total amount of Eas per
unit volume, The alticuie of "i km is taken as z = 0, The number of H 20
photodi-s--ntegraziono occurr-Ing in a planetary atmosphere free from oxygen
but cr-,ntaining water vapor. in whi,,-h the prote3tive effeol, of free oxygen
is absent, is given by I(z)n kz)o., dz jn,(z)cle 0
0 0
where 1 0 is the intensity of radization incident in the range of 18060-1430 A,
expressed in photons Der cm 2 and per se-,, At a distance of '50-10 6 km
Card 2/,Ff ~A

S/020/61/138/005/007/025
Time of attainment of a B104/B205
12 -2 -1
from the Sun, one has 1 0 10 am see . The quantity of 02 produced
11 -2 -1
in the atmosphere under these conditions amounts to 5-10 am see . On
account of the accumulation of 0 2 in the atmosphere of the Earth, the pro-
duction of 02 is slowed down, while the alt'itud,e of the layer where photo-
disintegration is strongest is increased. The intensity of radiation pene-
trating down to an altitude z is given by I(Z) - 1 0 exp(-c1n1 (Z)+d2n 2(z,-r)H),
where n1(z) indicates the concentration of water particles, and n 2 that of
free oxygen; i is calculated from the instant at which n 2 was zero. It is
shown that the spectral range of 1760-1430 A loses the role played by it in
the photodissociation of H 20 within a comparatively short time during which
the concentration of 0 2reaches that of H 20. The rate of oxidation on the
Earth's surface is given as V = Ae 211 20(.')' where A is a constant determined
by the condition of the Earth's surface. The results of calculation are
compiled in Table 1 for two different values of A, The value olC
Card 3/2 q

Time of attainment of a
S/020/61/1 38/005/007/025
B104/B205
A =- 3.3-10-10 was calculated by G, E,. Hutchinson (The Solar System, 2,
Chicago, 1954, P, 396). The conclusion is drawn that the amount of 0 2 now
present in the atmosphere has accumulated within a period of about 60
million years, as a result of interaction of atmospheiic water vapor with
solar radiation, provided no appreciable absorption of 0 2 has taken place.
This is a very short period compared to the age of a planet. The evolution
of life is thus believed to have begun in an atmosj~here containing oxygen.
In the concluding part, it is shown that the number of photodisintegrations
in the atmosphere is much smaller than that of H 20 photodisintegrations.
There are 1 table and 6 references: 2 Soviet-bloc and 4 non-Soviet-bloo.
ASSOCIATION: Glavnaya geofizicheskaya observatoriya im. A. I. Voyeykova
(Main Geophysical Observatory imeni A. I. Voyeykov)
PRESENTED: February 17, 1961, by V. G. Fesenkov, Academician
SUBMITTED: November 19, 1960
Card 41)5 ~

S/531/62/000/127/006/0(77
1053/1253
Alr.MIOTIS: Layiditmanp D.Lop 1
T ITTLE The problom of tia,bulanoo In the free atmosphere
S MR17Z Leningrad. Gle.viialya geofizicheskaya observatori-a. Trudy.
no. 127. 601. Fi,,Silca prizemnogo sloya vozduler-ba,, 122-126
TEXT : A totn]. s3xpreusloyj is obtained for the %vind speed In a jot
n tr eam In terms of an arbitrnry law cono6rning the change of the
'hot-izontal pressure gradient with Filtitlide - z. The vertical pro-
f 11(m of the v.-Ind and Ittj dolrroo of &-istinoss when f (z) = b(z) and
tha 3po(,,Ial enno of the presonce of a strong leap In horizontnl grad-
Innl,- of orossure over a narrow Interval of altitudes when u W
b(.-.), Rre calculated. According to the-formulne obtained 9the
vnlues of the coefficient of turbulence k and of wind -9 stiness,ci,
typicnl of the jot stream, waro found to be k = 500 W m /see and
~' im/sec.
Mnx
VN
ar

All
a 'Drill Flam v
wit 021
p r I p ti j v lan 2
1; 1 3".1 J~~[ -i IWe IF;j
~ ~ig
2R 04 r
HN -
F P
if
o v
pi"
19 1
5W:1 F.
.8,0
i
5 p p 91 o-a
A 7 7
61

CHERNOV, L.A.
"Acoustics of Moving Medium."
report presented at the 3rd International Congress on Acoustics, Stuttgart, September 1-8,'59.
Austiches Institut, Adademie der Wissenschaften, Moskau, UdSSR.

I
AUTHORS Blyakhman, E.A. and
TITLE Dependence of the Frequency of Field Pulsations at the FoctAs of a LGn,4
on Diaphragm Dimensions (Zavisimost, chastoty pul'sataiy polya V
fok-use linzy ot razmarov diafrapiy)
MRIODICAL: Akustichesiciy Zhurnal, 1959, Vol 5, Nr 1, pp 21-24 (USSR)
ABSTRACT: The authors calculated the root-mean-squ-stre value of the frequency
of uulsations of a wave which passed through a medium with random
inhomogeneities. The case of random motion of these inhomogensities
is dealt -with in the present paper. Dependence of the root-mean-square
frequency of pulsations at the focus of a lens on the lens-diaphragm
aperture vas found (figure on p 24) to be the same for random and
for ordered motions of the inhanogeneities causing the pulsations;
the case of ordered motion of the inhomogeneities vas discussed earlier
by Blyakhman (Ref 1). This dependence agrees well with the experimental
data (dots and crosses in the figure on p 24) obtained by
Card 1/2

SOV/46-15-1-3/24
Dependence of the Frequency of Field Pulsations at the Focus of a Leas on
Diaphragn Dimensions
Nettelblad (Ref 3) in observation of the scintillation of stars. There
is 1 figure and 3 references, 2 of which are Soviet and 1 Swedish.
,kSSOCIATION: Yaroslavskiy gosudarstvennyy podagogichaskiy institut im.
K.D. Ushinskogo (Yaroslavl' State Pedagogical Institute imeni
K.D. Ushinskiy)
SUBEETTED: June 20, 1253
Card 2/2

Mmov.
filicolal likoluevich Andreev; on his 80th birthday. Usp.
fis.nauk 71 no-3:325-528 Jl 160. (HIM 13:7)
(A,ndreev, Ilikolal likolaevich, 1880-- )

CHERINOV, L. A. LE)'PbMKTY7 A. I., KlIZENTSC-V V A A T-1179CV, Y.,
.1 - I . . I Liz
11CGII-TIER) A. 1.1 PRCK-qOf%OV, Y. A., STEKLUMSKIY, V. ".
IlEperimental stuaies nf some of the physical feaWres of
Ber~vllium-noderated in terpiedate reactors."
Report submitted for the IAEA Seminar on the Physics of East and Interi-ediate
Reactors, Vienna, 3-11 Aug !961
Acad. Sci. USSR Yoscow

CHERNOV, L. A., BLVMMN, Ye. A., and KROM, M. N.
"The focal system influence aver statistical characteristics of vaved
propagagated through the medium vith random inhomogeneties"
report submitted for the 4th Intl. Congress of Acoustics,
Copenhagen, Dermark, 21-28 Aug 1962.
Acoustical Inst. of the Academy of Science U.S.S.R., Moscow.
3

ARIYELI, Na. ; BYUIWIR Z-11
L~-
Methodology of determining the turbulence characteristics in
jet stream. Meteorei. gidrol. no.11:33-36 IN 162* (MIRA 15t12)
1. Glavnaya geofizichwkaya obeervatoriya.
(Atmospheric turbulence)

ACCESSION NR: AT4028743 S/2531/63/000/1"/0068/0075
AUTHOR: Byutner, E. K.
TITLE: On the calculation of structural and correlated functions on the final period
of observations
:'SOU~C-E: Leningrad. G1. geofiz. observ. i Ukr. n.-i. gidrometeorol. inst. Trudy*,
~no. 144/40, 1963: Fizika pogranichnogo sloya atmoofery* (physics of the atmospheric
boundary---Jayery~'Dneprovskaya expeditsiya GGO i UkrNIGH19 68-75
10
TOPIC TAGS: turbulence, atmosphere, correlated function, structural function
ABSTRACT: The author obtains an expression for the dispersion of structural and
correlated functions calculated according to a single recording copy with a length
of T. Numerical evaluations of the extent of*this dispersion in the case of a sys--
tem with a correlated function of theiypa e
qjTj are conducted. The relatiye die
persion of the structural function DT(T)'and the relative dispersion of the mean
quadratic value of the function dependent an the averaging range of T are presented
.in graphs. By comparing the behavior of the errors, it follows that the calculation
~of the structural function according to a separate recording can be carried out for
:values of the arguments -r4lbich do not exceed 0.1 T. In addition, the saturating
-value D(T) which1equals 2v'- is obtained from -the calculation of the mean values of
Card-

ACCESSION RR: AT4028743
'V throughout a entirs'abservation piriod T
2 th The values of D(T) in the case of
c
'intermediate values of the argunient c be ained only through extrapolation. It
is apparent that a'aufficiently large at of recordings, madeunder relatively
:identical external conditions, is requ red in.order to reproduce more precisely the
structural function, particularly In order to show its dependence on weather con-
'ditions. Orig #rt. has: 3 figures ifid 23 o
f las.
ASSOCIATION: Leningradakaya-glavna ge~ftzlcbakaya observatoriya (Priwipl*
iGeophysicpl Observ Of I 4--rad)
atory
SUBMTTED 00 DAIE ADQ: 16Apr".,. MM 00
I
SUB CODE: M,AS NO REF SM: 00 1 003
Card

BUTNER, E.K,; GISINA, F.A.
Effective coefficient of the capture of aerosol particles
by rain and cloud drops. Trudy Ien. gidromet. inst, no.15:
103-117 163. (MIRA 17-1)

BYUTNER, E.K.; KHTMAN, D.L.
I- -I - ~ I ~ I L4'l
Scattering of passive particles from a point source in a
heterogeneous medium. Trudy Lan. gidromet. inst. no.15:130-
136 163. (bURA 17: 1)

1,CCESSION NR: AT4028741 S/2531/63/0001144/0048/0058
AUTHOR: Ariye-l', N. Z.- Byutner, E. K.; Panin, B. D.; Radikevich, V. M.
=E: Results of measuring the temperature and wind direction pulsations in the
surface. layer of the atmosphere
SV
JRCE: Leningrad. Cl. geofiz. observ. i Mr. n.-i. gidrometeorol. inst. Trudy*,
:'no. 144/40, 1963. Fi~ika pogranichTiogo sloya atmosfery* (physics'of the atmospher"
boundary layer);,Dneprpvskaya expeditsiya GGO i UkrNIGNI, 48-58
TOPIC TAGS: temperature pulsation, wind direction, surface layer, temperature
ABSTRACT: ~& daily plot'of the average hourly values of horizontal wind direction
julsations a~ at an altitude of 16 m is produced. The dependence of the value of
a on strati ication, th~ recurrence of various deviations from the average direc-
tv,on dependent on_t4e sqatIfication and the -knd velocity, and the temperature
pqlsation values AT' with altitudes of I and 7 m are also obtained in the article.
Th, and A
r s ding spectral characteristics of the values cra are plotted in
gr phs. It is shown that the spectral function of the pulsation of wind direction
is subject to the 5/3 law in the frequency range from 0.02 to 0.1 cycles at a wind
,velocity of approximately 4 a/sees A diagrm of the wind vane circuit in given,
Card'. 1/2

ACMSION N&:'* Ai402874l-"__'-
the recorded ezamples of:vind direction values and graph plots. Froal
,ithe graph it follows that the basic col;Ltribution to the oscillation energy respon-
~sible for the temperature pulsation at-an altitude of 7 a is carried by the fre-
quency w of from 0.06 to 0.2 sec-I and from 0.1 to 0.6 sec-I at an altitude of 1 a
.(wind velocity in both cases vas equalito 2.4 m/sea). Orig. art. ~aszz 12 figures
anda table.
ASSOCUMN: Leiiingradskaya Slowns, geofizicheakays, observatoriya (Principle
Geophysical* Obiikiatory of Amaingrad)

ACCESSION LR: AT4028742 S/2531/63/000/144/0059/0067
-AUTHOR: Ariyel',: X. Z.; Byutner, E. K.; Konstantinov, A. R.
TITLE: Method and results of investigating spectral chara-. teris tics of turbulent
'pulsations in the surface layer of the atmosphere
SOURCE: Leningrad. G1. geofiz. observ. i Ukr. n.-i. gidrometeorol. inst. Trudy*,
no. 144/40, 1963. Fizika pogranichnogo, sloya atmosfery* (physics of the atmospherta
boundary layer); Dneprovskaya expeditsiya GGO i UkrNIGMI, 59-67
TOPIC TAGS: surface layer, spectral characteristic, turbulent pulsation, Dnieper
,expedition, Constantan alloy
ABSTRACT: In this paper, the authors'present a method of spectral expansion of
pulsation energ3f bf weather elements -in recording instantaneous values of the mea-
iiagnitude. Results of spectral analysis and module and pulsation wincLvelocity
u are derived, together with the vertical component, the velocity w, the direction
of the wind a, and the temperature-T; these are presented in a series of separate
records obtained in the Dnieper expedition (GGO) jointly with the UkrNIGMI. Two
characteristics from which it is possible to obtain the spectral function W(w) were
..calculated according to the experimental records of the pulsation values of the

ACCESSION NR: AT~4028742
measured magnitudes: 1) the structural function D(T) and 2) the-magnitude of the
mean quadratic dispersion of the measured value CF2(t) dependent on the averaging
time t. The experimental method is based on the use of the cooling intensity of a
heated wire located in an air flow on the velocity and running angle of the flow in
the wire. The cqoling intensity depenaence on-the velocity is used for determining
the value of the flow velocity; the cooling intensity dependence on the running
angle is used for determining its vertical components. A Constantan wire with a
diameter of 100 p is used. The results of the:experiment are presented in graphs.
Orig. art. has: 8 figures and 6 formulas.
ASSOCIATION: Leningradskaya glavna, geofizicheskaya observatoriya (Principle
Geophysical Observatory of Leningrad)
'SUIMITTED: 00
SUB CODE: AS
Card 2/2
DATE ACQ: 16Apr64 ENCL: 00
NO REF.SOV: 004 07M: 003

LAYKHTMAN, D.L.; BYUTNER, E.K.
Determination time of the stationary distribution of concen-
trations from a point source. Trudy Len. gidromet. inst. no.15:
97-102 163. (MIRA 17:1)

ARIYELIP N.Z.,
-~Y~TNER, E.K.; PANIN, B.D.; RADIKEVICH, V.M.
Results of the temperature pulsation measurements and the
wind direction in the lowest layer of the atmosphere.
Trudy GGO no-144:48-58 163. (MIM 17:6)

BYUTNERP E.K.
Calculation of structural and correlation functions for
a finite observation interval. Trudy GGO no.144t6g-75 163.
(MIRA 17:6)

BYUTNER, E.K.; KRVER, N.I.
Calculation of the horizontal scattering of particles from
an imobile source according to data of meteorological
measureirents. Trudy GGO no.167:178-183 165.
(YLILP-A 19: 1)

ACC HR, AT6021516 SOURCE CODEt UR/2531/66/000710 M0116
AUTHORt Byutners go K.
ORGs None,
TITLEt Formulas for the determination of the turbulence coefficient
from flow-structure data
SOURCEs Lisningrad. Glavnaya keofizicheakaya observatoriya. -Trudy$
no. 187# 1966. Fizika pagranichnogo sloya atmoofery '(Physics ofthe,
atmospheric boundary-layer), 207-216
TOPIC TAGSs atmospheric turbulence, turbulence coefficient, turbulent
transfer, atuosphorle boundary layer, air pollution
.AOTRAM
,i review is *made of the approximate formulas used to determine the'turbu-
jence coefficient kfrom data on fluctuations in turbulent flow ku and k
,obtained from structural measurements. The physical model is based on L
assumption that a volume of the atmosphere is horizontally homogeneous and
that the turbulent flux of momentum and changes in concentration vary ver-.
tically only; the enEire volume is divided into cells (moles) whose sizes
.are small compared with the distance! in which fluctuations in.uia~~_r

ACC 14Rt AT6021.510
.(velocity componenEs'and .pollut ant .. concentration) o.ccur, but large- in com-
parison with the molecular scale; the velocity field for ui is characterized:-
by a distribution function. The formulas reviewed for determining it
include those of Resselberg (1929), Lyapina (1948),'Dubov (1959), and
Ertel (1930). Their advantages and disadvantages are discussed. The error.,
in determining k is computed as a-function of the time interval involved
in an experiment. A proposal is made that the results obtained by com-
puting'k with approximate formulas be compared with exact values for the
surface boundary layer of the atpotiphere.in .9rder properly to-evaluate the
various approximate.formulas.-i' Orig . art ha a's
M No. 10
SUB CODEs..:AV ?SUDM DATEs -nonst ORIG.REFs 012/ OTH REF: 009

BYUTITER, K.G.
Use of D-163B steam ganc-rators on tank far-no. Transp. JIL khran.
neft-, i nefteprod. no,,6t29-30 165. (MI-Rk 18:8)
1. LerLingradakoye -upravlenlye r',lavnogo upravleniya po
transportiz I snabzhariiyu neftlyu I nefteprodurktami
pri Scivate Tiinistrov RSFSR.

GRINENKO, V~V.; BYUTNER, Ye.G.
1-ological incompatib-41-it-
Phys y of grafting componen-,s in fn-141
trees. Bot.zhur. 50 no.10:3409-1108 0 165.
(MIRA 18:12)
1. Severcr-Kavkazskiy zonallnyy nauchno-issledom tell skiy
institut sadovodstva :L vinograda-rstva, Krasnodar.

BYUYRIN,,
Glancification of slightly pitching ore deposits according to their
thiokness. Izv. AN TA%akh. SSR. 36r. gor. dela, not., stroi. J.
stroimat. no,'2:22-Z7 157(. (MI;RA 10:9)
(Ore deposits)

BYUYRIN, A.I.
B111YRIN, A.Ls Cand Tech Sci - (diss) "Study of basic production
processes in the working of low-grade deposits of Dzhezkazgan. Alma-Ata,
1956 16 pp with graphs. (Min of Higher Education USSR. Kazakh Mining-
Yetallurgic Inst). 320 copies (KL, 20-58-96)

BYUYRIN, A.I.
Ways of breaking ore in mining thin deposits in Dzhezkazgan.
12',V, AN Kazakh, SSR9 Sero gor. dials, no.1:3-16 158.
(MIRX 16:5)
(Dzhezkazgan District-41ining engineering)

BYUYRIN, A.I.
Investigating the process of scraper haulage when mining thin
Dzhezkazgan deposits. Izv. AN Kazakh. SSR. Ser. gor dela no.2:
72-80 '58. ()URA 12:10)
(Dzhaskazgan--Mine haulage)

MUZGIN, S.S.; BYUYRIN, A.I.
Ore loading for trackless haulage in thin sections of the
Dzhezlmzgan deposit. Izv. AN Kazakh. SSR. Ser. gor. dela no.l:
r?o-96 '59. (MIRA 12:9)
(Dzhezkazgan-Ore handling)

BYUYR IV. A. 1.
Determining certain -parameters of blasting operations in
mining thin Dzhezkazgan de-oosits. Trudy Inst. gor. dela
AN Uzakh.SSR 4:80-87 160. (MIRA 13:9)
(Dxhezkazgan--Mining engineering)

~_BTMIN, A. I.; WWFWW, I.N.
Use of anchor bolting in horizontal workings at the Dghezkazgan
mines. Trudy Inst. gor! dela AN Kazakh. SSR 6:62-67 160.
(Dzhezlmzgan re~Iion--Mine roof bolting) WMA 13:12)

BYUMN% A.I.; TSOY, S.
Some Droblens in the transfer of the Dzhezkazgan mines to a
new mining procedure. Trudy Inst. gor. dela AN Kazakh. SSR
7:67-75 160. (KM 14:6)
(Dzhezkazgan region--Mining engineering)

BYUYRIN., A. I.; NEGIN, IS.S.
Effect of oversized pieces of ore on the productivit7 of an
excavator in underground mining. Trudy Inst.gor.dela All.Kazakh.
SM 8:87-91 -'61. (MIRA 15:4)
(Excavating machinery)

BYUYRIN, A.I..; BAKAYEV, N.T.; URUMOV, T.H.; SALYKOV, K.; YESHPANOV, D.Ys.
ExIxidiency of widening the panels in the DzhezkazgaLn Ydne.
Tmly Inst.gor.dola AN Kazakh.SSR 9:13-20 162. (MIRA l5t8)
(Dahezkaagan District-Mining engineering)

I BYUYRIN ...A.-1 t.--- --,-
Way3 of incroaalng labor productivity in operating Dzhezkazgan
miDgs. Trudy Inst.gor.dela AN Kazakh.SSR 906-39 162.
(KRA 15:8)
(Dzhezkasgan District-Y"Ing engineering-Labor produotivity)

LTSEMKOV ZIIUKOVICV, BYUY-t;,!N, A.-T.
ld-,~ya of improving the chamber-and-pillar system of rdnirg.
T,,.-udy Inst. gar. dela AN Kazakh. SSR 190-8 165. (MIRA l8il2)

.8(5)
AUTHORS: Basharin, A. V., Profe,.s.,)r, Doctor of SOV/105-58-11-12/28
Teclinical Sciences, Vino,'-raOov, I. N., Candidate of
Tech:iical Sciences, Bychkov, A. I. CLIndidate of Technical
Sciences, B-,rvallkevich, I. B., Enji,-i--!er
TITLE: Motor-Genert-tor Drive With Amplidyne and Magnetic
AiaDlifier (Elel-.troprivod po siote:,-ie Lor-dviigatell s
elektromashinnym i magnitnym usilitelyami)
PERIODICAL: Elehtrichestvo, 1956, TIr 11, PP 51 - 55 (USSR)
A~3STRtCT: This is a description of an electric drive system
developed at the kafedra elektrifikat.-ii promyshlennykh
predpriyatiy LeningradskoCo elel-t rot ekhni cheslko:-o
instit-.?,ta imeni V.I.Ullyanova (Lenina)(C!Mir of
Electrification of Ind-astrial' Enter
prices at the
LeninL-rad Inotitiite of Electrical ligineering imeni
t:3
V.T.Ullyariov (Lenin)) by order of the Uralriasilzavod.
The system is based upon a utilizp.-Lion of ma-etic
a-"'Dlifiars and of symmetrical non-lil.c-ar ce-1- --.ic
semicondi,otor resistances, which vere developed under
Card 1/3 the suoervision of N.P.Bogoroditskiy (Ref 4). The

MoIUor-Gr--.(,,--:-tor Drive With Am-plidyne and 1"L~;-netic SC)V/105-58-11-12/28
AmDlifier
mnin -)rcb"-,e-i was tl!e of an ant-::.Utic7,-'-,y
_U -1 -
control-led electric drive sz:stem, tile qualitative
service factors of nhich P-re not below those of t-'-e
po,.-.er s, stem (Ref 1 whi c h, howeve r, i s cac. abl e of
controlling startinj&, revercin.- and braling operation
witilout contact This ja--~cr an
illustri-tion of the circ~iit di 6rram of tile eloctric
drive. This system is ca-pable of --,,,to-.Ia-Lic and manual
control. The system was tested with a sufficiently
powerfiil model. The different modes of ooeration,
startinj,~, braking and reversin,~, are descrilood. in
order to compute the tranrientun ir this system a Gr,-phic
mothod de-~,el-c;,,~,ud in the LETI (Ref 5) was used. The
calculated and the experimental characteriotic cl,,rves
for t"o transient Drocesses fror. motor startin-
to ----a::imum c~cced sho,;,,ed a satisfactory acreement.
The system is distin,~uished from others by Good
qualitative service factors and good static and
d.=-amic characteristics. The circuit diaL~rar, is zimple, it
Card 2/ 13 incorporates only a mininum of contacts L-;nd it

Motor-Generator Drive With Anplidyne and SCV/105-53--11-12/28
Am il i f'14 or
guarantees a reliable braking without "cref-oin,- speedr1l.
There are 8 fiCures and 5 Soviet references.
ASSOCTATIOl.: Lcnin6iadskiy elel, 'rot aklinic:ieskiy J,-,rt-tA imeni V.I.
.-u - - - - I -
Ullyanc-va (Lenina) (Lenin-rcLd Inctitute of Electrical
&q;ineeri-11- imeni V.I.Mlyt-uiov (Lenir)
SUBIdITTED: May 29, 1950
Card 3/3

MALINEVICH, Igor' Borisovi,,h3 BYCHKOV, Aleksandr Ivanovich;
POLI, Aleksey Yullyevicb;
BASHARIN, A.7., duktor tekhn. nauk, prof., red.; YEVEMEV,
V.I., red.
(Theory of electric drives; manual for independent design
work] Toorilit elektroprivoda-, uchohnoe posobie k samo-
stoiatelInym raschetain. Leningrad, Leningr. elektrotekhn.
in-.'
V., 1964. 80 1). (141RA 18:8)

ALIYEVI, Eduard Arkad'yevich; DYUKAREV, Yuriy Ak--ertlyevich;
LATENKO, Boris Vasilt-yevich; iEALYO) I.G.) doktor
biol, nauk) red.; ONISHGMKO, L.I.,
[Soilless growing of vegetables in greenhouses] Vyrashchi-
vanie ovoshchei v teplitsakh bez pochvy. Kiev, Gosoell-
khozizdat USSR, 1964. 141 P. (MIRA 17: 6)

BYVALITSEV, L.
Laying out the markings for dredging purposes on the terrain with
the-help of a.sextan.t. Rech. transp. 22 no-10159 0 163.
(NIRA 16:12)
1. Nachallnik ruslovoy izyskatel'skoy partii No.4 Kamskogo
basseynovogo upravleniya puti.

F-2
5
3-vlzi*-,i -1.11,6
t1--. ~Iath
0'r 4L -]3uj
u
r,~ c;
u
ro-.)r,)(luctJ-un, ~'.nd i,;
C; c -u- i~,d b.;,- 1~) it
in P51
in ol itr.
it do-.-)c)s i-- i-'
C 0:-, dm,~j
i.3 '-I~Jc CLir"T Go
cco--., )llr.' th i 1

I P--2
Z b .-II-ol. c 15,
C', IAL-ct .-:L.i -U*.I,:~
:-"l-- c oi, -,C-L lon
t-- lo
Z--u-c;r 2*,.i,:; -'Aul-1 he i I
C 7
]-,~viu3culii-, :)rov."t
.,C. ).L' 1,uo -2.
r-- 2/2

DOBROVOLISKIY, D.S., kandAekhn.nauk; BYVSHEV, A.V., inzh.; LEVIN, B.D., inzh.
Pulp grinding with the help of acoustic media. Bum. prom. 36 no-9:
26-27 S 161. (MIRA 15:1)
(Papermaking machinery)

DOBROVOLISKIY, D.S.; BWSHEV, A.V.
Pulp grinding by means of a generator of sonic vibrations. Bum.prcm.
(38] no.7:3-5 Jl `63. (MIRA 16:8)
1, Sibirskiy tAikhnologicheskly institut.
(Woodpalp industry-Equipmont and supplies)
(Sound waves-Industrial applications)

BYVSHEV, B.V., inzh.
New model of the flash ncandlemeter." Svetotekhnika 4 no.6:14-16
Je 158. (miRA 11:6)
(JPhotometr3r)

L Lq w
*

A Wrong dows of 'zinc oxide (in rubber). l.N.IIyv-Jsrv,
0* tt: No. 7. 41 3,
.!;. s. R.) 1939. N
CUNI(flilary to add 5% (if Z110 lip nalilral 110'N.1
will% NA-butedicur vtIlliefic 1111)lwl -00
0410 It lhat in "tic milait. ZU0 i~ not an activalm Wait
I in other inifits. a 5% atidn. (if ZnO iA t4k, hich and even
00 I&;jrjlj(jjl I" lut,twt. Zinc oxide in rubber production.

00 A. V ,INUI.md. /bid, 46- The If Z110 ... I I tic I...
It's,I,. 'Ittil lut-Itt-1114'. III filtitt., ,if th'.
00 -mlm. of ?.he .1-111114 fit- fuld-4-1 111W., I'll It", I )Cfal.,t, du+
.
.
- ~400

*0 Ife "KI41.11vi It.'at'llyl
1,14111
tiler lavit" %.
I
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sov/96-59-5-16/19
A Conference on the Use of Steam-Gas Installations with High-
Head Steam Generators
stations using the steam-gas cycle.-, Operating experience
with ItVelox" boilers operating on gas, The significance
of steam-gas installations in increasing the effective
application of gas.-fuel pover tachnology, The use of
steam-gas installations with free-piston engine gas-
generators in municipal pcwer engineering; The energy
characteristics and comparative efficiency of condensing
steam-gait power stations. There were also
communications on the state and prospective development
and applisation of gas-turbines in power engineerlng2 on
their design and manufacture at the Leningrad Metal Works
and on the development of the steam-gas cycle using
steam-gas generators with direct introduction of water
into the combustion chamber. Doctor of Technical Sciences
A.N.Lozhk:Ln and Candidate of Technical Sciences
M.I.Korneyev reported on the steam-gas installation with
combustion at constant pressure and a high-head steam
generator, developed by the Central Boller Turbine
Card 2/8 Institute, the schematl1c circuit diagram of which is given

Sov/96-59-5-16/19
A Conference on thia Use of St-eam-Gas Installations with High-
Head Steam Generators
in Fig 1. A considerable number of advantages o-;rer
ordinary steam turbine power, installations are claimed:
the efficiency is higher and the fuel consumption is
about 112% less than in a condensing station with medium
steam conditions. When a heat and electric power station
operates: on the steam-gas cycle, the output of electric
power is: increased by 100 to 200 kW hour/Mkcal as
compared. with steam turbine he&t iand electric. power
stations. Relevant