SCIENTIFIC ABSTRACT GUTMAN, L.N. - GUTMAN, N.R.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000617710005-4
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Sequence Number: 5
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

, I..
GROSSMAN, N.Ya.; KOVAL' V.A.; GUTMAN L.M.; SLI-faIENK0, D.P.
Automatic lorry car in operation. Koks i khim. no.2 29-32 163.
.1k (KRA 16:2)
1. Spetsialluoye konstruktorskoye byuro izmeritellnykh mashin
(for Gross-an, Koval')* 2. Donetskiy koksokhimcheskiy zavod (for
Gutman., Semenenko).
(Donetsk-Goke industry-Equipalent and supplies)
All

GAYLIVOY, T.V,; HZIN, A.I.; ASN13, Me.; L.M,
We-11ding up cracks in locomotive wheels by the electric slag
method. Avtom. svar. 16 no.12273-78 D 163.
(MIRA 17~1)
2. Poltavakiy parovozoremontnyy zavid (for Gayevoy, Kuzin).
2. Institut elektrosvarlcf~ imeni Patona AIN UkrSSR (for Asnis,
Gutman).

ASI:"L'-'., Arkadiy Yefjm(.)victi, dokLor tekhn. nauk; CUIT-,T', Li-'-
Mironovna; OSYTNIK, N.K., red.
[Reconditioning track links of crawler tractors] Vossta-
novlenie zvenlev gusenichnykh mashin. Kiev, Naukovu dumka,
1964. 65 P. (MIRA 18:1)

L 63462-65- 'E-.-'iT(1)/FCC GN
ACCESSIOM N_R: AP5019149. 'UR/0362/65/.001/0'0710677i 068.7:1
AUTHOR: Konyakhina, A. A.,,, ShaRoshnikova, M. I.- Gutman L. N
-TITLE: Nonlinearity effects in the slope.wind problem (4umerL~al experiment
SOURCE: AN SSSR. Izvestiya. Fizika atmosfery i okeana, v, I ;n .;7; 1961
677-687
-TOPIC T&GS slope- _~dn& mechanism, _J__ iii__ u1
nonlifile cy-effect" ope4liid.c4 c
4
slope wind
j:1
.. ABSTRAM The paper investigate,4 the~~iol6:.df.,iibnliii6ar:toL-ma !ih!!the~~01
aha
stationary-slope wind problem on.'the b-sis' va.' f
a of a numerical,: e ItM.tion o the
fundamental.nonlinear system of equations, These equatiohe an first: ftahilv-
f ormed into a system of finite difference equations %iii
eh: are ~Oubsequently:
solved on an M-20 electronic computer by means of rmatrix ~_Ild Omj~'le factqrJzatfc1n,-----_
coupled with the interaction approach. Flow, patterns, charactdrlzinj~ various
reliefs, are established on the basis of these calculatiqPa. Vliysical dedlictlAnis I
concerning the role of nonlinear terms ic-:-.7ape wind mech pinisuid. are also.gfven
Orig. art, has- 30 formulas and 4 figure

K 0 .Nf A ~:; -1 1; ~~ ., -~ . , --~ I i;,i-Cl-~i!fllKV.!A, f.l. " " 1" N,
~, '! e, 11
i
. ~ -t of nonlinearlty in 1-he slope. problem (el ntmerical
experiment) . Izv. AN SSSI?. Fiz. atm. i okpjtn. I no.'7:677-
() F, 7 il 165. (MIRA 18,S',
1
1. Vy,:.h--lslltel'ny-v ts,,,r,.tr- Silbirskoge. ot,delpnlyq A14 SSSR..

iZ7.V. 1, - T . V . ; !VOUTl, A. S.
Monsoons
Vertical structure of monsoons. Met. i gidrol. no. 6, 1947.
Monthly List of j!.Ussian Accessions, Library of Congress, December 1952. Unclassified.

Al'-.1 I'll I . . . I
. . 1 11 . I I .! " i2 :1, , , ...,
y . . .-- i i j- .,
i
-ki -. 1-3. . 1 - I - ~- !- ~ 1,
. - , , , I I

0 4 0 0

-
'-

tM LAMIIIA? T%Zmal
rma Convection on a Mationar Source of
Convection on

00 A W-f-CIL July- 44f. - T-
Avg 149 (1

so The author Investigate* the motion of air which originst91--,
In a stationary heat source located at any givvn "I ol &R-
are&, or even on a similar horizontal surface. Such kind of
motion. AW&r*ntly. taken place tit clouds during the procipi-
tAtIon of beat as a coftseqNance of coadessation at water vapors
during thermal convection over the beate4 earth's surface,
when oscillating streams al warm air can ba observed. Uml r**
nar thermal convoction can also lIPA good applicaUcat in Itch-
ntques since the pbsnomens of thermal convoction also take
place in combustion processes. The article ccmtAins formulas
which are based an equations of motion of viscous coin press FbIe
flulds and are simplified In conformity with ttm theary of
thermal coft"MUM.
13-2-230
00 600
so
00
00 4
too 0
00
90 '306
00
06
Y'l
41 1 4 N 1
I j it j
0 W* * 0 41 0 0 0 0 0 0
000000*0000000000000*0 .
0000000000006000006040 00~0000*00000
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AVec 4,c -ft;
r
ON jtWPWbA=v-,Aksd. Nauk WA411; flf~ rwo, 2,
IMALf 190).
rm"Wering a OPP641 type of Mountain In "" the Ob" Is
41104,014114 4619 an arbitrary dirm4,1to, the author uww a sorsolvat of
curvillnew Otooreinsta", othe" the X-Axia is always
&We" sk" the slooloc. In OLW% a system all A nots to then do-
"I printwily upim the x-coordinsta. To elivainate the. offed at
Arrinal furtmilence, he ansumps furtlwr that the lemprraturv on 0*0 In Z, the Mefficie"Is In which we OWN sivoost by a "Viom of
CAN "Iffser,4 tow "wountod" is twrywhere the sum. anot that the aluxuana. Tuarevallonseembe
&-,ope in sufficient for spoplying the thenry v4 hnuvwf#Lrv layer. &A"I successively ¬ the authow lives the Wolum" (of 00 Am
rwirf these, ammumpti,wis thoo author obtains tow the eomporoentjo d "PoIlleirnlo. rojorravrolint; the Rest approsionsUm low t1w vvcUW
"I,~ty wA the tionistion of the potential temperature Imm its "fievity aml the cievistinn of potevilial tomperaMm. The VWU.
mhooturfied vothion (without any maik)n) a system, ot "ationg. 1113 distribotwi, of them quaritities in plotted. No ollaw asechb.
"Vrd from Ow Njuallon for a Mmiortmouible viWoup &dd. apply. 1i"" About the cheracterinties at Mounlain-T&A7 wi" it Oven.
Ing the owvwy of beamolary layer and the throoror M ceprivertion, L Fleoluors. USA
tMilf-ifill the fr-4W -t A-I&DdMLADd-F,- IAWU Off"'11"4ko"
*Wb4OA cmd, 1944). Thlooyoolem 6 flien ~4W by ovaltliagg
onall Worm and infrocluvinig other restrictive assumptions (co-
tollruout, of vim 1y am the"Mal Meod"Vily tonn"I. QNW1-
fly WOO" Of M~- ehWOOloreWit qft%-
fillroo the Pysivion to fransforoved to a notondivasaivional two with
sely aussrorkoal evorMck - tx~ wl" Uw author triss, to ashrot by the
sulked d separation o( varishirs, expandim the wilut6on In

\,gGlutman, L. N. On (Iter'nial dlsturk~inccs;, .5orizo
I(A air
'
-rikf
Mat, NN h. 14, 1:
(Russian)
A line source ofheat located ift a hcr~rcwt ,Sir 6iv- givit's
rise to a pattern of vertical fre-e con.vectii,~jil,~iiii4Lriiiilit]-_4Q(I j
on the forccd Convective w,ake4ront th~. hdai!
pattern is invie'-flgated first for latnii,tar fl84 With tj~e~jrqd
convective distertion entering as a convection, Thesibrity
and temperature distributim 4 obtained as.~t jlowitfi sArids
in a parameter proportionni to (tic thermal e.',pansion- coefil-
Cient of tile gas. Several tv.-Inq in this 'wkii are alltmlwd
CXplicitly. The &IMC prob-lem is 'Consideml for turibukrit
flow assuming a Prandtf-Taylor mixing lenj,701
proportianal
to the horizontal conipolient of distance Nom tb(h heat
source. It
So
.
Ealhematlxal Revi.ew 70'

u S S 1.
~Sl c e
L~ fr.,n

GIITI,'-*~%N, I . 'T. ::3
USSR/Geopirfoics - ',-JLcroc.ILw.1te
"CAlculating the Temperature of the Air layer Near the Ground," L. N. Gutman
Iz AI: Naul: 533R, Ser Geofiz, 'No 5, PP 451-459
Approx solves the problem of the temp variation in soil air lt)yer nesir the gromd
under the influence-~ of solar radiation. Presents tin exwnple of concrete calcns of the
behavior of air temp accordinL, to data of actinometric oboorvatlonis.
267T78

Gulman.-L 1 ulatioll of the ficat rvgi~ne -if
IL Oil file Com
6 Utes. "lwleu. Sb. 15, 99-136 (1953). (Russian)
The purpose of 'W5 paper is to put the solution of the
ont'-dimmiatial 11ouricr Itcal enuafion into a form suita-
tile (or in,lusttial appiscation." such as metallurgy, Pro-
duction of cel-amics, etc. The author considers a munbu of
practical situations, amorij, them: 1) th-~ case when
Surface tCnll)Cr.ItlIrC is QbSVrVCd %t CCTtain CqW-Ili-j Spaced
time intervals; 2) the cas- whero. surface tempent t tire
satisfivs -AiO/PI=zexj7'(t)-Oj; 3) the case where the body
has an outside rovei with a different heat constant;
4) the case where the surface ternpo-rature is t.) L,,? dc-
termined to produc- a (l(-irv(I internal state of tumper-
ature.
For ttio,;t of Owso vrobicrus fit( classical Solution in
exponential. in([ ti-igonotnetric functions is unsuitable.
The author uses the solution
3
0=,E NnW" ( 2 %I(ki)
in which the /~ av~! constants and the function,> L,(.i;) are
solutions of
L."(x)+',: -211L,(x)~O
t,vhich satis(v L,(O)=. 1, T_(_>o)=O. Fmit-place of
these functimis arp supplic(i for it =0, 1, - - -, t,, -.it iiit(,r-
vats of 0.01 in I lit, at'gument x. 11'. E. Hiltie.

USSR/Geophysics - Soil temperature
Card 1/1
Author Gutman, L. N.
F70 3141'51
Title A contribution to the problem on tile calculation of tile temperature of the
Soil
Periodical Izv. AN SSSR, Ser. geofiz. 2, 114-122, Kqr/APr 1951,
Abstract Considers the problem concerning the thermal interaction between the air and
soil not covered by anything. Obtains formulas for the calculation mean-
daily temperature of the soil according to data on the temperature of the
air at the level of a meteorological stall. Presents an example of a con-
crete calculation. Eighteen references, all Soviet.
Institution
Submitted may 8, 1953

USSR/Electronics - Condensers FD-533
Card 1/1 Pub. go-9/18
Author Semenov, N. A., and Gutman, L. N., Active Meml)ers, VNORiE
Title Calculating the plate shape for a continuously rotating condenser
Periodical Radiotekhnika 9, 72-73, MaY/Jun 1954
Abstract Gives formula for determining plate shape (based on number of condenser
plates, space between plates, and internal radius of the stator plates)
of a continuously rotating condenser for use in application such as
sweep circuits.
Institution : All-Union Scientific and Technical Society of Radio Engineering and
Electric Communications imeni A. S. Popov (VNORLE)
Submitted : November 27, 1953
hi!~ :j;'p

11/1 Pub- '.~()-5j9
Jutman, L. N., 'ctlve M mbers, VNORiE
ithor Leytes, R. D. , an L e
Title A method of investi7ga~ion o ransient ~,.rocesses in linear system
Periodical Radiotekhnika, 10, 36-51, Jun 55
Abstract Approximation method of calculation of transient processes, based
on application of the theory of finite differences to an integral
equation (Duhamal's), is liscussed in the art.,.-le. The introduc-
tion of special coefficients perinits t.hL! deriv_ation of simple ex-
pre-ssion for the relationship. between input and output voltages.
This relationship helps to solve a number of problems related to
tran3ient processes in amplifier circuits. As an ecarEple, a stage
with plate corrective compensation is investilr,-tei. Approximation
methods for calculating ti,:,,nsient characteri!-L'~. ~ directly from a
differential equation are -..15o e-.amined. Re-port JeLivered to All-
Union Session of VNORiE in Z-1ay 19,53. Graphs. Nirm.: references:
7 USSSR.
InsLitution LIl-Unicn Scientific and Technical Society of !5 "Ulio Engineering and
Zlectric Communications i-meni A. Popov VTIOFil~'
3ubiaitted '.1-arch 22CL, 1954

I OWTMAN, L. , - WRWANY.VSKAYA, M.A.
Calculating the temperature of soil covered by snow. Izv.Ar, SSbA.
Ser.geofiz. no.10-1188-1199 0 156. (MIRA 10-1)
1. Akademiya nauk SSSR Institut fiziki atmosfory.
(Soil temperature)

GUTMAh, L.N. (Moskva); MUCEITIKOV, V.M. (Moskva)
An equilibrium equation of elastic bodies taking after effect
into consideration. Inzh.sbor. 24:165-173 '56. (KLRA 10:5)
(Elastic solids)

6b-37 -1/7
AUTHOR: Gainan, L. N.
TITLE: AITheory of Computing the Temperature of Soil (K teorii
r1ascheta temperatury pochvy)
PERIODICAL -./Trudy Geofizicheskogo i nstituta Akademii nauk SSSR,
1956, Nr 37(164), pp. i -49 (USSR)-
ABSTRACT: The author offers a theory of computing the temperature
of soil at various depths on the basis of measurements
of the temperature of the air. Solution of a system of
equations, based on the distribution of heat in the soil,
in snow (when there is a snow covering), and in the
near-surface layer of air, provides a basis for computa-
tion. The author takes into account changes which occur
with the passage of time, in the depth of the snow, in
the coefficients of heat and temperature conductivities
of snow and soil, and In the turbulence of the near-sur-
face layer of air. The solution of algebraic linear
infinite systems with an upper triangular matrix and the
solution of Volterra's integral eauations with an infi-
nite lower limit of the integral (using the method of
finite differences) are stated in general terms in the
Card 1/2

!j
r I
LJ
IT!
tuttrinn, Theoreffed model afe larilp.,dG. ltt%
l
i"T
MkMMMMTK7~-SR zer 6c.QfLiz. 1957, 79-~T-/.Rumitll
41s 01 A tij~jhtwrfi) Cif
lxr:ii ;r(;--~Vnctn-wL:~ uL~ '~.o jdea~ij-,~j
pri S~rn( t, :2-. rl:,
A I Jrl;!
IRl �R
3. OT T Mill

AUTHORS: Gutman, L. N. and Koronatova, T. D. 49-10-4/10
TITLE: On the theory of slope winds. (K teorii vetra sklonov).
PERIODICiL: Izvestiya Akademii Nauk SSSR, Seriya Geofizicheskaya,
1 1957, No.10, pp.1238-1248 (USSR)
ABSTRACT: The author defines as slope winds, winds in mountains
which occur owing to thermal conditions above an inclined
ground surface which is uniformly heated or cooled. The
theoretical model of a steady state slope wind was first
expounded by Prandtl (Ret.1) on the assumption that the
mountain slope represents an infinite thermally uniform
surface and that the coefficients of turbulent exchange
are constant values. In earlier work one of the authors
(Ref.4) generalised the problem to adapt it to a more
real relief shape, copsidering the slope winds in a
shallow valley or above a shallow mountain ridge; such a
formulation leads to non-linear equations and a method was
proposed to simplify these equations, indicating the
possibility of finding an accurate solution for the case
of a relief which is symmetrical relative to the centre of
the bottom of the valley (or the top of the mountain ridge)
without obtaining concrete results. In this paper
Card 112 the solution of this prQblem is expounded in greater detail,

On the theory of slope winds.
a/10
disregarding the humidity field; certain physical
cunclusionu aro drawn froni Lhe rosults ana coiicretu-
calculation examples are included,stating that the
conclusions are in agreement with experimental data
published by VulYson, N. I. (Ref.8).
There are 2 figures, 1 table and 8 references, 7 of which
are Slavic.
SUBMITTED: February 27, 1957.
ASSOCIATION: Ac.Sc., U.S.S.R. Institute of Physics of the Atmosphere.
(Akademiya Nauk SSSR Institut Fiziki Atmosfery).
AVAILABLE: 11brary of Congress
Card 2/2

.AUTHDR: GUT3_M L N PA - 2887
TITIZ: 'iWe--o_r_eTT_c__6l Model of the Cumulus. (Teoretichegkaya model'
I kuchevogd oblaka, Russian)
FMODICAL- Doklady Akademii Nauk SM, 1957, Vol 112, Nr 6. PP 1033-io36
(U.S.S.R.)
Received: 4 / 1957 Reviewed: 7 / 1957
ABSTRACT: In the coordinate system (XPZ) ( x - horizontal coordinate,
z - vertical coordinate) the author investigates the plane steady
prablan of the ordered thermal convection which is due to the verti-
cal instability of the atmosphere. Neglecting the total motion of
the air the complete system of the equations of the themodyniLmics
of the atmosphere is simplified while takinf account of the small-
ness of the disturbances & (X,Z) " P(X.z of temperature and
pressure re3pectively compared to the assumea functions 0 (z) and
P(z) (which satisfy the static equation). The equation system ob-
tained while neglecting the horizontal modification of the relative
humidity, the turbulence, and the ooriolis force is written down.
The boundary conditions result frcm the symmetry of the motion am
from the local character of the disturbances. The (nonlinear) system
of equations just mentioned has a trivial solution in the case of
homogeneous boundary conditions which apparently corresponds to the
equilibrium of the atmosphere. It is then shown that, besides the
Card 1/2 trivial solution, also a definite non-trivial solution ought to

Theoretical Model of the Cumulus. PA - 2887
exist, qven if only in a very thin layer of the atmosphere. This non-
trivial solution apparently corresponds to an expansion of instabil-
ity,ana on oertain conditions such a process way lead to the forming
of a cumulus. These ideas are then carriod out mathematically. By
means of the solution obtained also V(x,z), the forming velocity of
the liquid phase, may be determined. Also for the wnter oontent an
equation is given. The hydrodynamic image corresponding to the solu-
tion found here reminds strongly of a massive powerful cumulus. For
the purpose of illustrating this conclusion a concrete example is
computed. (2 Illustrations).
ASSOCIATION: Institute for Atmospheric Physics of the Academy of Science of the
U.S.S.R.
PRESEiM BY: A.A.DORODNYTSYU, member of the Academy, on 5.10.1956
SUEU 4.10-1956
AVAIIABLE: Library of Congress
Card 2,/2

AUTHORs Gutman, L.N.
20-3-21/59
TITLEt The Applicatlon of the Method of Long Waves to the Problum of
the Flow Passing Around Mountains (Primeneniye metoda, dlinnykh
voln v zadache obtekaniya gor)
PERIODICALi Doklady Akademii Nauk SSSH, 1957, Vol- 115, Nr 3, PP, 497-500
(USSR)
ABSTRACTs In the system of the coordinates x, z (x - horizontal coordi-
nate, z - vertical coordinate oriented upwards) the author
here examines the plane, stationaryt nonlinear problem of the
air flow above a mountain. The horizontal dimensions of this
mountain shall be so much greater than the vertical ones, that
the problem can be solved by the method of the long waves.
The velocity of the approaching flow may change linearly with
the height. Starting from the genwal system of equations of
the thermodynamics of the atmosphere, the author simplifios
the theorems of the convection and neglects the turbulence and
the Coriolis force. The thus found equation is explicitly writ-
ten down. The mathematical solution of this problem is follow-
Card 1/2 ed step by step. On the occasion of this solution three diffe-

sc-i :~e;rree of'
of
dissertp.tion: "Thermiril convecti.on, as
i s, -t ~-~b i L I t- o.~' t at m, o a r t t, d i I f t 1 F7 1- i t 5
I)P, S S F,, H -
L,-,w A
liec
t
-Prot -,,o 7, 29 512.
2-

AUTHORS: Tsvang, L.R. aad Gutman, L.N. -cOV/4Q,-58-7-7/16
TITLE: The Measurement of tie ~'~M-Uspheric Ion S ectruz,
~~13
(Izmereniye spektra le6kikh atmosfornykh ionov
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya Geofizicheskaya,
1958, pp 891 - 902 (USSR)
ABSTRACT: A --aew impulse method of measurinS the spectrum of light
ions in the atmosphere has been t,.-orked OL!t at the
Akademiya nauk SSSR Institut prikladnoy 17-eofiziki (Institute
of Applied Geophysics) (Refs 1, 2). A cylindrical ion
chamber takes a Eamole of air and then has a const&nt
intensity applied to an external electrode. Thisproduc~~-s
an ionic current which dies avilay with time as the ions
reach the electrode. Measuremt.nts at diff erent times
Give the ionic spectrum from the current. As is sho,.-.,n in
Ref 2, t-Le current flovinC through the centr!-,l electrode
is given by Eqs.(l) and (2), where I (t) and I (t) are
CD +
the currents at the central electrode for positive and
negative intcnsities on the external cylinder; n +(W)
and n-(w) are the density distributions of the positive
Cardl/6 and negative ious; A, B, al, a2, b17 b2 are constants

SOV/49-58-?-~/16
The Measurement Of the LiCht Atr is-oheric Ion "pectrur,
determining the parameters of the chamber and the pot-ential
on the external cylinder; t is the time, calculated from
the moment that the field appears. a 1, a21 b1' b21 B, w and
t are connected by the relations:
B 1 1 2 2 Wt = B
a1 + a.2
Eos.(l) and (2) are two interdependent integral equations
and the authors nol.; wish to go over to two independent,
integral equations. Eqs.(l) and (2) are added and
dimensionless variables (4) are substituted (3) . The
resultant equation cannot be solved exactly but since
M(TO is a monotonic bounded function it can be represented
approximaiely by the sum of tx,.,o exponentials (?). f(-e)
is then obtained explicitly (8) differentiated twice and
combined to give finally (10). With a chamber
having internal and external electrodes of radii 2 cm and
uard2/6 10 cm and length ?0 cia (Ref 2), Eq.(11) is obtained

SOVII~C,_,-U
The Neasurement of the LiCht Atmospheric Ion SDectrum
~ f " (-t-) is of much less siGnificance in these en uations
than f (C) of P(t) ). Eo.(121) L.Jves the final equations
in terms of n(t) and Eqs.(14) and (15) in terms of
n+(t) and n_(t) . The factors I , I' and I" in
these equations are obtained from the oscillo~-r_nrh 11;races.
Owing to fluctuations, all th~ree band especially thre
latter two) may be inaccurate, so it is necessary to smootl-,
out the curves. lvi~~ure 1 s1,oi,.,s the original and the
smoothed curves.
In order to simplify thle calcuiations, (14) and (1';) are
replaced by (13) and (19), which divide the ionic current
u
up into positive and neGative parts. The current derivatives
are obtained from E(ls.(20) and (21). On making the
necessary substitutions, Eq.(26) is obtained for calculatiaL.,
the density distribution of the positive ions and (2?) for
the negative ions. The coefficients in (26) and (2?) are
tabulated and the crilculations are inade by a method indi-
cated in Figure 2 - a paper strip has the value for the
current I k at a time t. printed on it; this is 711aced
Card3/6 over the table and the corresponding coefficients read off.

SOV/49-58-7-2/16
The Measurement of the Light Atmospheric Ion Spectrum,
The major error in the results occurs in working out the
oscillogram traces: the aPparatus errors for v, ~ and a
(ion concentration, average mobility, dispersion of spectrum)
are about 2016 and in the graphical solution about 7,~, and
5-55~&, respectively. The impulse method is restricted to
light ions as the current for heavier ions becomes too small
to be measureable.
This apparatus was used in 19'?5 in an aeroplane (type IIr-12).
An indication of the layout Is given in Figure 5. Great
efforts were made to cut down the effects of vibration since
this has considerable influence on the oscillograph tr.-ices.
(The oscillograph chosen was of type POB-12.) Samples of
air were taken in through the openinC 4 and alonr~ the iipes
to the chamber 1. The chamber took 1-2 secs to fill '~.'ith
air and. a similar le-n-th of time -,,,.-as required for measure-
ment of the ion current.
On -the Elbruz expedition, measurements were made at tLe
Terskol observatory and station (stations round Terskol
which gather meteoroloCical data are shown in Firure ED).
The aim was to find the dependence of cloud development
uard4/6 on the li-,ht ion specLrumi. Dui.-inU 19~)2-53, 500 measurements

sov/49- 5 8-7- 7/ 16
The Measurement of -the Light Atmospheric Ion Spectru:r!
were made at Terskol observatory and 35 on Mount Terskol.
The results of September 9, 1953 are particularly _interestJ'Lr_'-,,-.
All the meteorolo--ical conditions (temperature, hu-nAdity,
pressure, speed and direction of 1xind, precipitation) ,.-.-ere
approximately constant. Ficures ?a and b show the variation
with time of the ion spectrum - as cloud~started to cooler
mountain the concentr~-,tion of positive and ne[~,ative ions
started to fall and continued to do so ,~ihile the clouds
thickened; the cloud-&'then began to clear away and the -ion
concentration correspondinCly rose. It is characteristic
that -the decrease in ion concentration was accor,,,panied by
an increase in averaLe mobility. Norin6er and Siksna 1-1-ave
suggested an exl)lanation for this (Ref 4).
These data were confirmed by measurements made when the
observatory lay under cloudSin trhich the station itself was
situated (F%ures 8a and 8b and the table). The Graphs
indicate that cloudsover the station -,-)roduced a decrease
in both positive and nefSative ions and. an increase in the
average mobility. It is characteristic that for w_,) 1.6
CM2/v.sec and w 2 both
Uard5/6 _> 1.9 cm /v.see the spectrum for

The L'easurement of the Lifht Atmospheric Ion Spectrw'i
cases practically coincides.
The concentration of negative ions chianges less than the
positive ion concentration after precipitation, whilst the
opposite is true when the station is situated in the clouds.
On days on wbicia the cloud cover is small, the concentrDtion
of both kinds of ions increases ' The average, absolute
humidity on such days is 8.5 g/cm3 (as compared with.
10.1 g/cm3 on cloudy days): this cbange may explain the
increase in N+ .
There are 6 flEures and 4 references, 3 of ohich are
Soviet and 1 Enc-lish.
U.
ASSOCIATION: A11--ademiya nauk SSSR,Institut 'Liziki atmosfer,
(Ac.Sc.USSR Institute of Atmospheric Ph,7sics)
SUBLITTED: July 2, 195/
uard6/6 1. Ionic current--Measurement 2. Ionic current--Spectra
3. Ionization chwnbers--Applications 4. Mathematics---
Applications

Gu 1.111-Vul ? L. 14 . and 1WNn, F . I . (Ila l I :,I I -I"%-)
"A Zydro-ThermodyTiamical model of the Bora."
report rxesented at the First A.11-Union Con6Tess on Theoretical and Applied
Mechanics, Moscow 27 Jan - 3 Feb 1960.

510031601=;,'0091CC?1C', '
K19"BO54
A UTH~R I
T IT LE.

PER V)D ICAL. T-:;1k .1tklly, 960. ri. pp. !7-40
TEXT .L

%
of Phy;l..
lro.rt-n rep4r-.x -ret by
hL;"r inatitt-, of 1-nr.; -1 m- !t- therI
hr'. hi6l,r inatt -t., ofI-n.nfr, 7 ~11
Fr, 11
.he

to F:
r'r 4, 11 nh
-
n
-
ol -n
t:.,
w
r, i tn n,
Ar-1 r'

C.rd 1/4
:~--k by 3. T. of 2.r.t:-1y
in -.h. of -.n. cl~,, :y,l, F', I
(5.r.t. U"-; ~7
s1P.1,t. Line. I

*
of xt-i-klj -11rKIn I ... .1, t~ "7 .1. App',!vt.,-n:f
"
the St;&tCh-li~e 1--1,1 to -
&in ni.
- -- f-'- P. n t,
Theory .1 4-t .,tt -.ne -n ... n~T

- - .- 1-1 -.h
Pr.ttt
r,;,rt
ty
roble=2 of t~- .1 r,
n
;.
t,rfP'T.-I -.1 nn
i n iiryt I. I. I. t , t ~ t i k IyC..fzikl Ll 33~~!
f the llltlt~t~ if

:k.. z~ --anly
-ST- Prc~.'-, f

t! t'
R2

Within theo
y
't'.
at. of t", E

9-
1-t6 St.1-ti of

'L .pl.. of tt, Rlt.tl. G., v .....ITIt. 1or St
fCc
:
C-i 214'
!;t..Jj E.0141 Fl.. of Gee *, 1 4 photonb1
t be 'k
Zmt
I.-
.0, t-.
'
dI-IthProIf1h, Plen-p-1-1 -,I.- of P-~
.
7.
;
l-
-"-
Pcogic;-ki; t
4&
"

-
he
P -T., o-,
"
ort an --~L-Inverv, T
r:
Pr,bl ... of Ilhl-
t
It%h . Fr.. to,

b.r"r,o
in th- -;-%. by X. T--, f the F
.v:
ro
.r. -h C. 11 ily, !)*,
r.
!t IZ
t"
ktIt
it
deg he
,;
~
T -
.1 t. hnich ij, i-tit... (Od.". i.,Y%.C~,ni,
W
of
. y
~
it -.hqory of aleMati-. S;*,--.al Attention wk* ;m-.d to a
h '
-
4 .1
r:;,.rt by Prn,11-n, h.
-ttmd of t: L report by i.
n
- I.-,- . ho int.-ting 1.ti- to one of th.
----
-
f-"'1 and to . r-;Ort by -~
t on .to; r
Ark.bly., h. ofho tent
C.rd 3/4
1=0CIATION; K%b%rdino-?,11,r,11y 6... unIv-11.1
v. r-. I "ty

GUP4#N,_k.N.
Theory of cumulus clouds. 1Z7, AN =R, Ser, geofiz, no,7,.1040-
1057 T1 '61, (MIRA l4t6)
1. Akademiya nauk SSSRJ, Vyookogorn" geofizicheakiy institut.
(Cloud physics)

GI)TiW,,' L 11 - TEBIJYEV, D. 1.
Theory of the foehn. Izv. All, 56SR. Ser. geofiz. nc.8:11~2-11C)S
Ag 161. (MIRA 14--7)
1. All SSSR, Vy,,okogorny-y goofizicheskiy inatitut.
(Foelm)
N

3/ 0 14/.017
C'
A UT-'ORS Gutman, L. i. and Yal'?,D, L. N.
TITLE: Theory of frentf,
P'~"R 7 0 D7 A Do'l-lady Akade2ji4 ~~,q , no. 1961 537 - 590
T E'XIT : T h e hydrodynamic equationo for ~hl, atlnosnlhore i~,re simplified on
C. 0
c ii -r s b,:, t,.v e . n 10 and
the followi-~~ assumption~7': I ) :.;'o - i ,,
10 0 0 Thus, it is c ilb t o coordinate system
x a nd Y indicate t*-- horizontal -~nd' static eauatiorI3, 2) Fluctu-
s -0( - - e t:.. ~,t3 i jn 4 Can$ .
a t ion , 0~ tem -'ratul , - - 3) Acceleration
in the direction of motion -ice A) All clements of motion are
indep~-ndent of y, and t'h~-. '--ront iL,, , er:,fore', a cylindrical surface
ha v i nez a n -, I ement d -ro c f1i a I L, 11~;-' t'-~ 5) The frort isshifted in
the pcsitive x-direction at ,~. con!~~an~', v--~Joc4ty c~--Ci ylittiout changing its
lorm. -B-nsed on this al-;sumption, the pzo-esses occurring in the coordInate
nyste.m. :Tievin8 aio'!L"' cQnsidered to be steady. Ac-
cord ors "o t"he atmos-~,here read-
Card

3/020/611/138/003/014/017
Thecry of -F--onts I-) ~ ~, 3 2 C:z
0:
p
X
0;
:0 (3)
RO
_-, ) =xo, 0/ (4)
uk, vl,, and w,, are the ccrnonents of velocity relative to the ear th; -8k
and n,l are the deviations o-f temnerat'are and Dressure, res7oectlively, from
Uneir mean values 9 and P; u and vG are the given and the cons-~ant com-
ponents, respectivel.-.7, of the geoFtrophi~.- wind; the subscripts 1 and 2
refer to cold and war:a --ir nass--~s; 6 iz,~, '.he Gravitational constant;
1 - 2.:.)sir?, .,.,here ~-% indicates the angular velocity of the earth's rotatior;
and i is the -eol~raphic latitude. It _-,s furt)-er assumed that the temper-
ature ~*luctuatilons -are an a r e :,.L V,-! 0, where'
s ' n b z 6r, I
stands fc- tn
,e difference -n tpmDerfit.ir between cold and warm air
10
Card 2/.U

Theory of f rontus
I.,-;/ C`3/G-,4/C1 7
3 1 C 2 C, 5)
masses on the earth's ourface, and d~,note-~3 t-,e difference between the
vertical on"~; of t.`.ese _-9 and ~-are con-
sidered to oe constar~. rit-, th]'.s problem. read
III) I,. Z 0: (5)
11P 11
V1 h (x); (6)
W1 CZ-2 (R1 C) I" Y', f7, P2 "IP11 Z=h(x); (7)
U2 0 np;1 z (8)
Taking account of and (5).
P, I
U., Z) Z' P, 0, (9)
T
is obtained by integration of ~,q. (40, Thus, Ea-. (1) acquires the form
,~2u,
U,) - -v Wi' (x) + rzhh'(.c) (10)
In t egr a t ion of 3 ove z- fro::-. 0 c h IeE.ds to
0,
e- dz
Card 316~ pg

5/ /020/61,/13a/.603/014/017
Theory of fronts 3104/B201-
This is t'he mass of air e-Znre--sut! 4n -ah,4clh passes from the warm to
6he cold a-*r mash-. 4n one second per un-It length of the front. Next, the
following expreo-,Jo. are obtainod f2-on-, (2) and (10):
U, (11) Sin B (11) Cos
I
. - B 01 - n~), F, (12)
VL Vt va v e-E [B (ij) sina + A (n) Cos
where' (0-11 e 0s I )u di, d, B('~I) sh
-sin~:u d-/d'.'...; xlu 1 2.-; u u -4~- cos'~: v e- ~'sinF -v u a
9 9 9 9
+ v (1-e- co-----). is determined b~,,,
9 :- I . .
I + V-2(1 -C) -q- i" [(V + i)=Tj + (V-1) sin
d~t 31.1- 2c-' (cosq + sin il) - 1/ze-" (cor 271 + siti 2,q) (13)
Here, V = v /U ; C = c/U The numerica'. integration of (13) is discisell
9 9 9 t
in all detail. The results obtained tire graphicaAy represented in Pigs.
3 and 4. Fig. 3 shov.'s a section througln 'the fronts (Q = -1100; C - 0.25;
V - -0-5) in 'he coordinate system mo-,-inj,, along -,vith them. Fig. 4 shous
a cold front -10 C; C - 1.5; V Arrows indicate the wind
Card 4/1
5

Theory of fronts
2 401~' 2
S/020/61/136/003/014/017
B100205
direction.. A. P. Dyubyuk (Meteorologiya i gidrologiya, no. 4 - 5 (1937);
Tr. Tsentr. inst. Dogody, no. 26 (53) (1951); Isv. AN SSSP, ser. geofiz.,
no. 9 (1956)) is mentioned. There are.4 figures and 3 references:
1 Soviet-bloc and 2 non-Soviet-bloc. The reference to English-language
publications reads as follows: F. K. Bal.1, quart. J. Roy. Meteorolog.
Soc., 86p no. 367 (1960).
ASSOCIATION: Kabardino-Balkarskoye otdeleniye Instituta prikladnoy
goofiziki Akademii nt~luk SSSH (Kabardino-Balkarian Departmont
of the Institute of Applied Geophysics of the Academy of
Sciences USSR)
PRESENTEDt January 11, 1961, by A. A. Dorodnitsyn, Academician
SUBMITTED: January 10, 196 1
Card 5/c
17)

Stuation,xy c,.' t*-o :!olu-jo- o1 ; cc!,-,,
Do]-!. ]41 no.1:77-79
CTU 14:11)
1. V-00-o"Cri"- 3.-ntit~'t A"', "~!M% Predstavleno
L - -
A.A.Doro-_'ritsy:r,--..
(Boi,malary vall~c --rc*Pl--,-:i)

KHATUKAYEVA, Zh.M.; GUTMAN,-.-L.II.. -
Problem of the crossing of a cold air mass over a mountain range,
taking into account a decrease in the density of the air as the
altitude becomes higher. Izv. AN SSSR. Ser. geofiz. no.9:1251-
1260 S 162. (KRA 15:8)
1. Kabardino-Balkarskiy gosudarstvanRyy, universitet.
(Winds) (Mountains)

GUTMAN, L.N.
Motion of air in valleys. Meteor. i gidrol. no-3:3--B fir '62.
(Winds) (Valleys) (141RA 15:3)

GUTMA,N,, L. N.,
"Stationary spatial model of cumulus'.
Report to be submitted for the 13th General Assembly, Intl. Union of Geodesir
and Geophysics (IUGG), Rerkeley Calif., 19-31 Aug 6-3

KHALKkCHEV, V.A., GUTMAN, L.N.
Spatial stationary nonlinear problem of the cold air-mass flow over
a complex relief. Izv. AN SSSR. Ser.geofiz. no.2:349-361 F 163.
(MIRA 16:3)
1. Kabardino-Balkarskiy goaudarstvennyy universitet.
(Air flow)
A
I

KHALKFCHEV, V.A.; GUTMAN, L.N.
Movement of coldeeir masses along mountain ranges. Izv. AN SSSR.
Ser. geofiz. n~.9-139)-1409 S 163. (MIRA 16:10)
1. Kabardlno-Balkarskly gosudarstvennyy universitet.

GUTMAN, L.N.
Stationary axisymmetric model of a cumulus. Dokl. All SSSR 150
no.1:81-84 My 163. (MIRA 16:6)
1. Vysokogornyy geofizicheskiy institut kN SSSR. Predstavleno
akademikom Ye.K.Fedorovym.
(Glouds)

ACCESSION NHt AP4010573
S/0050/64/000/001/0023/00,29
(39t 'L
AUTHORSi Vullfson., No Io; ymt- *;No; Paylova, Io 5,
TITLE: Effects of gravitational waves on the formation of hail clouds in
mountainous regions
SOUNCEs Meteorologiya i gidrologlya, no. 1,, 1964# 23-29
TOPIC TAGSt gravitational wave,, hail cloud,, cumulus cloudp wind velocity., taqw-
ature gradient, precipitationg hail
ABSTRACT: The authorsi purpose is to examine the conditions under which the ef~-
fects of gravitational waves may lead to the formation of vertical movements
sufficiently intense to have a noticeable influence on the development of hail
clouds. They consider the model of an infinitely long mountain range of arbitrary
cross section and with transverse wind of constant velocity. They derive equations
for air movement, and compute values for different heights and breadths of the
mountains. These computations show that wave forms developed by a mountainous
zone may lead to the fornation of strong, stationarys ascending moirenents of aire
To test thiss they investigated the relationship between development of hail in
the Alazani va.3-ley and fields of temperature and wind favorable for producing
atmospheric waves, For completeness and comparison they also examined temperature
Card JX,,~2-

AGG&SSION NR: AP4010573
and wind fields associated with cumulus rain clouds not producing hail as well as
fields associated with cumulus clouds yielding no precipitation at an. The rela-
tionship of precipitation to wind and to temperature gradient is illustrated by
lFig, 1 on the Enclosure. For winds blowing parallel to the range) regardless of
:temperature gradient, the weather was fair (for the four years represented by the
;data of Fig, 1). All kinds of clouds were observed for winds blowing at right
.angles to the trend of the range,, but hail was more likely the nearer the wind
direction was to this right-angle direction,, and the higher the temperature gradi-
ent was. This means that hail is most probable under conditions most favorable foi
the development of gravitational waves. Orig* art, hass 3 figures and 15 form"IA96
MMCIATION3 Inatitut prikladnoy geofiaiki (Institute of Applied Geophysics)j
i Vy*sokogornM geofizicheskly institut (High4bxtain Geophysical Institute)
low
SOMITTEDs 00 DATE AcQo Web64 ENCL 1 02
'SUB CODEs AS NO REF SM 002 OTHERs 002

.kCCSSSION' NR: APLOILO31 S/0049/64/cco/001/0--136/0149
AUThORS: Kalazhokov, Kh. Kh.; Gutman., L. N.
TITLE: The dynamic structure of fronts
SOUI-LOE: AN SSSR. Izv. Seriya geofizicheskaya, no. 1, 1964, 136-149
TOPIC TAGS: front, air front, cold front, air circulation, ascending air current,
descending air current, convection
~OSTRAGT: This work combines and develops the ideas of A. F. GYuby-A and F.
Dall (discussed in a number of articles) ard atte,-,-;,)ts to find the form, of 'the
frpntal surface separating two thermally different air masses. A-lie present authors
also investigate the movement of the air that may- tWko place near and irinodiately
next to the surface. For t1iis purpose they have sivinlified the system of equations
for hydrodynamlics of the atmosphere on the basis of the following assumptions:
1) a horizontal scale on the order of 102-10 km,- 2) a disturbance of temperature
and pressure small in comparison with the average for the given height, 3) accel-
eration of equalizing movements may be neglected, 4) the frontal surface is
cylindrical, elongated along the y direction,, 5) the frontal surface is displaced
Card 1/2

AcassioN ~a: ApWiW31
along x, at%a constant velocity,, without change in form. Equations are derived
to define the different types of fronts: 1) with a closed line of flaw in the cold
air mass, 2) with a rising movement of warm air directly at the front and a weak
., 3) with a weak descending current beneath the frontal
circulation of cold air 0
surface, 4) with the current of (3) and circulation of air in the fox-,iard part of
the cold air mass, 5) with weak circulation of warim air at the front, and 6) with
ascondinr, warm air before the front, Vertical sections are plotted for each of
these. The authors point out that their theoi-f requires serious experimental
.verification. Such work is now being carried out, and preliminary rasults are
rather encouraging. A section of a front moving throueh. Rostov on 24 Aumst 1961, 1
plotted from radio-pilot data, corresponds rather well with the section obtained
by theoro'wic&'- considerations. Orig. art. has: 10 f i4tures - and 24 f ormilas.
ASSOCIATION: Kabardtio-Bnlk skiy gosudarstvenny*y universitet (Kabardino-
Balkarian State University)
LD : 104pr63 DATE, ACQ: 14Feb64 LNCL: 00
SIM COD:;: !S WO REEW SUV: 007 OTHER: 001
Card 2/2

L 15742-65 wMACC
1 ArCEI'STW MR i AP4045781 5/9050/64/000/0091/0017/002V
AUTHORI -Gutman# L*-N-. (Doctorlof physica-mathematLeal-~~ticiences.;
v S V."
P r o f a 8 a
TITLE17. New method for the construction of vertical profiles of
fronts
SOURCEI He teo ro lo g ty a, i gidjcologiya, mio, 9, .1964
7-3 1; .
lISRsphe ic frdn frontal vartL.cal.: prof ij'a,'Vartic~sl
I TOPIC TAGS$ r
profile construction
ABSTRACTt An eleven-step me.thodo supplementing the m6i:hod used y,
the GLdrometeosluzhba SSSR (Hydrometeorolo,gical Sal I!vL 66~:.o fthe UiSSR~
is proposed for the construction.of the. Verti.cal P ro f A I e:s ;of a tho S
pheric fronts* The principal difference between' the tuo; Procedures;
is th-at the new method emphauLzaa dynamic rather than:: tk*a cum! .0'a'etoirs.
The basic procedure involves the construction, itvia. 9lEd .Lnp..oyat~ev% of
coordinates$ of a vertical profile of the flow field nOrmat' to and
moving with the, fronts as fall;owst ~1) the directio'zi an4 averaga ~speiidj
lof a selected portion of the front in determined fdr a4ariod of 12
Card l 3
- - ----------

L 15742-65
~ACCESSION HRI AP4045781
.or 24 hours.from successive weather charts; 2) a line-, Is constr'uctiid
normal to the front; 3) radiosonde data,points ate pl6tted on the lindl
14) the horizontal scale to be used in plotting the profile is c*hOsOn; !I.
5) the same is done for the vertical Scale , and the riid.iosonde, ldat~.i
are plotted; 6) actual wind data are computed for all: 61avation4 Old,
Iverticals normal to the front for which the horiv'ontal'compoftent 0 f I
iwind velocity((u) is known, using the formula u-m :cos 4 vhere a* :is the
,angle between the direction of frontal movement and the wind direction
'M the differences u - c (c is the actual speed:o'f thelront) a:re
computed for all verticals and altitudes. and- plot'ted 4m horizontal
jarrows drawn from the appropriate points; 8) th6 ~'flow' function'
Computed for all. verticals and altitudes according to the formula
-0*08Z
(u C) dze
0
!where x is the vertical coordinate (in kin) of the' orip';in of co6r~dittates
ion the front; 9) the (0) values are then noted at, the -:appropriate pro-~-
ifile points and connected by interpolation; 10) in the same manneri
d 2/3
Car

L 157-12-65
ACCESSION NR: AP4045781
the projection of the frontal surface is plotte& in th'e 'plane of t h'e
profile; 11) comparisons of the densities and devIntio.na in the :line
of flow then give a qualitative derivation of the,,. dis tribution in : I
space of the vertical component of wind velotity,., Thes~i procedures~
were tested by constructing 10 vertical profiles of fTonts (7 eold,
2 warm, and I stationary), using radiosonde data 'collected over Rika,
Velikiye Luki, Smolensk, Volgograd, and Moscow. Results of these t:ests
were in agreement with theoretical computations, and t.he time requIred.
to perform the work was so short that the method was judged suitable
for use in meteorological operations. Orig. art.. h as t 3 figures,
table, and 4 formulas.
ntain
ASSOCIATION: Vysokot-lo.tny~y.!,,geofiziche (IlLgh-Mou
Geophysical Ini-Wiu-te)
SUBMITTED: 25Jun6"3 iENCL.: 00 SUB ~..ODE -ES
NO REF SOV: 005 OTHERt 000
Card 3 3
F~' T i'T"

S/0049/64/0001009/1414/1428
ACCESSION Nil: AP4045791
AUTHOR: Gutman, L. N.
TTTLE: A stationary, axially symmetrical Model Of a CUMUDIS Cloud With
evaporation of water drops talken into arcourit
SOURCE: AN SSSR. Izventlya. Seriya geofizicheskaya, no. 9, 1964, 1414-1428
TOPIC TAGS* meteorology, cloud phy!;ics, cuintilus cloud, cloud, atmospheric
turbulence, Cloud model
ABSTMCT: The author obtains the solution of the nonlinear, stationary, axially
syTm-,ictrical problem of a cumulus cloud, considered as the process of resolution
of a moist-unstable atmosphere, in closed form. An allowance is made for the
influence of evaporatton of water drops and the influence of turbulence IS 11130
taken into account. On the basis of this solution the author describes the
spatial pattern of distribution of meteorological elements in .1 cloud model.
The following is the author's interpretation of the physical processes occurring
in a well-developed cumulus cloud. Moisture-saturated air enters a cloud
through tile lower and side boundaries and Immediately begins to rise. At thiS
time the water vapor which it contains is condensed, releasing latent heat of
r1pKation and thus, heating the central part of the lower part of tbri clou'~'

ACCESSION NR: AP4045791
and saturating it with liquid moisture. The heated air, under the influence of
the Archimedean force, rises into tile central part of tile cloud, entratning
the water drops forming in it. Almost all the water vapor call apparently
be condensed in the lower part of the cloud. The rising of the lir in tile
central part generally follows tile dry adfabatic law, and .10 a result the devia-
tion in temperature, while remaining positive, begUis to decrease, becoming
equal to zero oil tile axis of the cloud at a point approximately one-third of
the distance from the top of the cloud to its base. A further ascent of air
together with water drops occurs due to inertia and the temperature deviatfon
cotittnues to decreise wLth heLght, now becoming negative. The Arclift,.iedoin force
developing at this time, directed downward, slows down the air flow, forcing
the air to spread Out in a horizontal direction. T'he further tile- ascending
1);irticies move away from the axis of the cloud the less they can be heated
during, the condensation of water vapor and the more rapid is their cooling
with icight. Thercfore, in the central par,, of the cloud, a nucleus call be
heated at a time when the periphery will be cooled in comparison with tile air
outside the cloud, situated at the same height. With respect to the neighborhood
of tile cloud top, where the vertical velocity becomes equal to zero, it will
ru,-j 214

ACCESSION NR: AP404579i
obviously be colder than tile surrounding medium and extremely saturated with
moisture . The air and tile water drops, spreading out in a radial direction,
from tile central and Upper parts of the cloud, which are betng cooled in corn-
parison with tile surrounding air, sho-,ild begin immediate descent under the
influence of the Archimedean force; the liquid mof-sture which Lt contains,
will evaporate, leading to still rre,i! er cooling,. The latter fact, Ln turn,
LnLenrifies the descending flow, which Lherefore call attain considerable values.
As a resul-1, all the. liquid moisture can evaporate and dry air will emanate.
,4iLh respect to tile a-fr outside, but in contact with tile cloud, as a result of
turbule"L friction and turbulent heat transfer it will be drawn into tile des-
cen(!Lng niovum-~-.ut and will be coote-d somewhat in tile direct vicinity of the
cloud boundary. This cooling attenuates rapidly in a horizontal direction vith
inereastnt, distance from the cloud and then experiences transition into a slight
warming Caused by the adiabatic character of the process. "it is noted in con-
clusion that this theory has been In tile stage of development for some time
under the direction of G. K. SULakveltdze...". Orfg. art. has: 75 formulas
,-.ind 6 figures.
ASSOCIA'rION: Vpcsokogorny*y geofizichesi(ty InatitUt (111till-Momitain Geophystcal
Institute)
SMIMIMM: lAOct6-1 ENCL: 00 SUB CODE: ES
'Card-

ACCESSION NR: A114065791
NO REF SOV: 010 OTHER: 000
1~ %Cord
.414

I I
GUTMAN, doktor fiz.-ma%em. nauk, Drot'.;
A new method of constnicLing vertical sectionB of fronts.
Meteor. i gidrol. no.9:17-21 S 164.
1. Vysokogornyy geofizichpskiv institut.

I - - ."'C", -
GUTM;*, ~ 7, L. i. ; MLA L, "rdl i, r 1-.
Theory of the gravity ..,Inds of' Antarct-l-a. Meteor. fs,;~. rlc-~:
150-155 165. (m:!U 19: 1,

GUTMAN, M.; DIALBONS G.; URSESCUP D.
Recont improvements in unipolar machinese po 155*
STUDII SI CERGETARI STINTIFICE, FIZICA SI STINTE TEFINICE,
Iasi, Rumania. Vol. 6. no. 29 1957
Monthly list of European Accessions (EEAI) LC, Vol. S. no. 8, Aug. 1959
Uncl.

RLRAUTI~,,/Fhysical Cherlistry - Electracherxistry.
Abs Jour Ref 21itir Kiiaiya, No 19, 1959, 67380
Author D'Albon, Gerard; Ursescu, Dau; Gutmail, Marcel
Inst Folytechnical Institute Iasi
Title A New Phenomenon Ubserved at a Mercury Chromit%i Contact
(for a Thin Liyer). Frelii-Anary Repovt.
Orig Pub Bul. Inst. politehii. Iasi, 1958, 41 No 1-2, 297-3o4
Abstract When current was passed through a system- thin Cr layer
on steel f-H3_7 Cr layer oil steel, periodic variations
of the resistance of the system were observed at coie-
tant voltage. The Cr layer was "' 30~k thick. The ef-
fect of the Cr layer oil Vie phenomenon described aad the
effect on the layer of variotis cheraical compau;7,ds, H3
purity, sublayer material, current maL;uitude, tenigerature,
and other factors were studied. -- Yu. Pleskov
Card 1/1
- 32 -
GAIGINSCHI, S. ; DUMITRASGU, T. GUTMAN, M.-;- -ZUGRAVEL, H.; BIRJOIANU, A-
Aspect of the Akulov-Bitter figtLreg in case of olastic defoxoat ions.
Studii fiz tehn Iasi jo no.1-.85-91 '59 (Aul 9:3)
1. Filiala. Iasi a Academiej Reuublicii Populare Romiue- Ida)
(FlasticitY) (Deformations(Meci-'anics)) 00110
(Spectrum analysis) (Magnetic fields)

L 28382-66 EWP'C)~E-WP(k)/E1YT(d)/EwT(M) EWPL
R '~006p'/Oor'6
AP5023387 (A) SOURCE, CODE: UR/0317/65/ooo/005
I[JP(c) DJ/JD
AUTHOR* Vovk, F* (Major general of engineering-toohnical service);
Gayenko, A& Engineer Gute
Lieutenant Colonel);_. _~gn. M. (Engineer, Lieu-
tenant C516-nel); GLershteyn, S (Engineer, LidiMilliht~'061onel)
ORG: None
TITLE: Prolongation of machine life B
SOURCE: Tekhnika i vooruzheniye, no. 5, 1965, 62-66
'OPIC TAGS: ordnance engineering, military tank, internal combustion
ngine
BSTRACT: The present paperconsisting of three separate articles,deals
,ith the operation, maintenance and repair of armored tanks, engines and
uxiliary equipment. The authors of the first article, F. Vovk and
. Gayehko, do not recommend overhauling new engines of the B-2 type
ntil a general overhauling of the entire tank is required. However,
eticulous checking of engine parts between general overhauls is strong-
y recommended. -In connection with this subject, an example of the
,onthly discussions at the Ull anov Guard Armored To
n1S_aotqpJ was men-
ioned. Reduoing-gear begLX ngbgF-o? Heavy UaUis are to be checked after a
un of 200 to 300 km. The level of liquid in the engine cooling system
ust be checked every 2 or 3 hours. A regular replacement of track
Card

L 28382-66
ACC NR: AP5b23387
chain pins can increase the run distance by 600 to 800 km. The cater-
pillars service life can be twice as long if they are kept well adjusted
and maintained. A set of gages for caterpillars -was proposed by Officer
Lopatin. This set was shown in a figure, as well as a device for chang-
ing pins.- In conclusion, further development of special commissions fox
inspection of tanks was strongly recommended. The second article, by
M. Gutman, deals with the repair of engines and their parts at an auto-
mobile-repair plant. hTeohanioal cleaning of oil pipes and channels, use
of diamond drills for honing, careful cleaning of parts (including.ult-
rasonic method) and other improvements were recommended. Filters, oil
radiators and fuel equipment were cleaned by using the UZG-10AI device.
Mass production methods were introduced for cleaning and polishing oper-
ations. A special automatic device was invented for honing operations
of YaAZ engines. The advantages of diamond honing were stressed. The
machining of crankshafts was organized in cooperation with the Khas
Automobile-Road Ijastit"te. Following the experience of the KharlkoWa_nd
Yaroslavl' engine plants, the tightening of bolts mere checkwd-Vy-d-yna-
mometric wrenches. -A-t_aMe was presented showing the wrench types and
tightening-forces to be applied to different engine parts. The third
article, by So Gershteyn contains some critical observations on various
suggest iond__4u_dY-as : i6te"Plng the heating system connected in summer or
muffling the engine if the temperature of cooling liquid is 80 Go Lrj_

-Jzl~
L 2b382-66
ACC NRt AP5023387
cessile inspection and duplication in control checking-was also criti-
oized. ThO 3UCCeSSfUl maintenance and repair practice of7Omsk Armored
Tank Technital School was mentioned. Orig. art. has: 2 fieures and
1 table.
SUB CODE: 19 SUBM DATE: None ORIG REF: 000 OT11 FW: 000
Card 3/3

POFEAO Florica; GUIVAN, Madeleine
Detemination of cadmiwn traces in p .olymethylic nulfide.9 ard in
soils, in the presence of other cations. Studii care chim 0, no.4:
673-6-80 161.
1. Laboratorid de geachimie al Intreprinderii de prospectimi si
laboratoare, Buturesti.

I-, ,-.- / iT / 1 .4 'o ~:r-,
RUBIN, G.K., inzhoner, GMAN, H.B., inzhener.
Now series of chamber-type electric furnaces for wide application.
Vest. elektroprom. 27 n0-10:55-59 0 156. (KIRL 10:9)
1. Treat "Elektropecht."
(Ilectric furnaces)

RUBIN, G.K.; GUTKAN, M.B.; GLEBOV, S.V.
- - IY
Use of very lightweight refractories ia electric resistance
furnaces. Ogneupory 22 no.1:6-9 157, (KaA 10:))
1. Ppytno-konstruktorsko3re byuro tresta "Blectripech'" i LeningradskAy
institut ognsuporoy.
(16fractory materials) (Blectric furnaces)

. 1, 11
. . 1y IL -f ..I - v I) M,B, 4
15911

J
f PU Ili:
AUTHORS: Rub lia, G.K. and Gutman, Y.B'. (Engineers) 110.-7-4/30
TITLE: Method of modernising chamber-type electric furnaces.
(MetQdy modernizatsii kamernykh elektropechey).
PERIODICAL: "Vestnik Elektropromyshlennosti" (Journal of the
Elect_rl"=4LIndustry), Vol.2b, '70-7-1957, PP .11-13 (USSR) -
ABSTRACT: There must be in service at least 10 000 cUmber-type
electric furnaces with a total installed power of not less
than 200 MW. Most of these furnaces are of poor technicall
characteristics. A great many of the existiz& furnaces
should be modernised, which will ensure considerable power
economies. This article makes specific recommendations for
the improvement of such furnaces. One of the main causes
of low efficiency.in furnaces is inward leakage of cold air
through the doors. Methods of correctimig this are described
in detail and illustrated by sketches. Recommendations are
then madt about relining furnaces to cut down heat losses.
In doing this difficulties are sometimes encountered in fix-
ing the 4eaters because tile lining materials are mechanic-
ally weak, and a method of installing the heaters in tubes
Card is described and illustrated. Methods of increasing the
size of the charge in furnaces are also described. The ad-
1/2 vanta,,ges that often result from increasing the power of

FEL'DMAN, Iosi-f Alelwandrovich; GUTHANy Mark Borlsovich; RUBIN, Georgiy
Kusiyelevich; SMIGIW4skV 9--A-.D-s-9--"r'-e-d-.-;---S'APAROVA, A.L, red.;
VORONIN, K.P., tekhn. ved.
(Calculation of heating elements for eleciric resistance
furnaces].Raschet nagrevatelei elektropechei soprotivleniia.
Moskva, Gos. energ. izd-vo, 1961. 26 p. (Biblioteka elektro-
termista, no.5) (MIRA 14:8)
(Electiric furnaces)

GUMM) M.B., inzh.; DUKHAYLGV, L.A., inzh.; RMIDESWEN-SKIY, 0.1., inzh.
Heating in a fluidized bed. Vest. elektroprom. 34 no-8:53-~7
Ag 163-~ (MIRA 16:9)
(Furnaces, Heating) (Fluidization)

.77

JD;
T/wP(0/1V-P(bY . ....... ... ....

ACCESSION NR:
-AR5009006 S/0137/651000/02/nis

SOURM: Ref. zh. ffetallu~rgiya, Abs. 21856
'
AUTHOR: Gutman, M. B.; MikhLylov, b. K.; Kaufman, V.
G
TITLE: Research on deep salt vats
CITED SOURCE: Elektrotermiya. Nauchno-tekhn. sb., vypo 38, 196!~, 9-i1
TOPIC TAGS: metallurgy, elcctM-tic heat treatment
TRANSLATION: Resoarch has been done at the M-Union Sci(iuntific: Research institute
for EquIpment for designing salt vats with allepth~o:-F 1700 mm and
l
palt Vat WIt
* surface areia of 0.25 ml and more. At t"lle ~IoF=w Instrument Pliint
* depth of 16150 mmi3 - power of 75 ),-,q land a ri-,olixn salt temperatii ra of 12$tr Wa,,i:;
tested. At -,he Sverdlovsk instrument Plant a salt bath with i.'l d eptil;o:F IT50
posier of 100 1cfi and molten salt., temr~i~~rature o~ 12500 was te-sted. TIN! ~.--!Iectric 11
processes for var1louz3 desig. s of deep salt vats were simulated,.-mi a ~,,tqhputer. It
was found that a'vather ni-i-iform tempevature Nithin limitq of IV) prolridqd, id
Is
t 6ootaminat
the deep salt vats at a depth of IL1000-1200 mm (when 4;0. iot
insignificant). Uniformity of temperatuni distribution througtjout tbe:worki,ng.s'paC
Card 1/2

GUTMAN, M.B.; MIKRAYLOV, L.A.; KAUFMAN, V.G.
lemperature distribution in the working space of deep gait
baths. Metalloved. i term. obr. met. no.9:14-17 S 164.
(MIRA 17%11)
1. Vsesoyuznyy nauchno-issledovatellskiy inatitut elektrotermi-
cheskogo oborudovaniya.

L 4oS?.1-66 EWTW/E'NP(t)/ETI IJP(c) JD
ACC NR, AR6014925 soullcE cODF,-- uft/012-4A5/000/oll/Boix/Bol()7~
ALITHORS: Gutman,.M. B.; Mikhaylov, L. A.; Rozhdostvonskiy,.O._I,_
TITLE: Investigation of heat exchange in a fluidized bed
SOURCE: Ref. zh. Makhanika, Abs. 11B725
REF SOLRCE: Elektroternaya. klauchno-tekhn. sb., vyp. 41, 1964, 10-11
TOPIC TAGS: heat transfer fluid, conductive heat transfer, heat transfer coofficientt
heat treating furnace
10STRACT: The coefficient of heat transfer fron a fluidized bed with a fixed tenner-
ature to a copper or steel specimen located in the fluidized bed (which consists of
sand particlGs with a fractional composition from 0.6 to 0.85 =n) was investigated.
During the experiments the reduced velocity of the liquefying air varied from 0.55
L'o m/soc. For the copper specimen, values of the heat transfer coefficients wore
obtained from 160 to 350 kcal/u?-hr-deg (with 2bed tenperatures from 310 to 815C and
for the steel specinen from 200 to 400 kcal/m! _hr--dog (with the oven temperature
Irom 835 to 960C). The experimental results are presented graphically in the form
of the dependence of the heat transfer coefficient on the fluidl:~od bed tomperaturo
and on the reduced velocity of the liquefying air. Tho temperature fields in the
fluidized bed in tho temperature Interval from 300 to 800C wore also investigated.
r--4 1/2
Card 2/2 11b

GUTK&H, M.G., podpolkovnik meditainakoy nluzhby
Course of acute pneumonia in the North. Toen.-med. zhur. no-3:86
Itr 15 6. (nu 9 . 9)
(RUSSU. NORTH=--PHIUMONIA)

ALEKSETEV, N.I., inzhoner; GUTMAN, M.M., inzhaner.
Efficiency experts of on@ plant. Sudostroanie 22 no.11:
38-41 N '56. ()Uk 10:2)
(Shipbuilding-p3quipment and supplies)

atulov!3e~.iy,
and 7.
of snorzc~--;.c us in Kitri,
I , f , * , " . 11 1
':at-ri~dv nauchm!-1-h Kiev,
+.(',l I :~l 4 n s -4 t11 I :.r d,.,

- G-UTRAN,-14.N,-,. inzh.
New design of revolving joints and mouthpieces for inter-
communication systems. Suaostroenie 27 no.6:24-26 Je 161.
(MIRA 14:6)
(Intercommunication systems)

F 1 7 -1 1
Translation from: Referativnyy zhurnal, Metallurgiya, 1958, Nr 3, p209 (USSR)
AUTHORS: Voronova, N. A. , Gutman, M. R. Troskunov, Ya. L. , Armen,
B. D. , Leppeta, ~._G.
TITLE: Low Carbon Cast Iron Rolls (Prokatnyye valki iz
nizkouglerodistogo chuguna)
PERIODICAL: Tr. In-ta chernoy metallurgii. AN UkrSSR, 1957, Vol 11,
pp 196-214
ABSTRACT: An account of the results of an investigation performed on
rolls made of low-carbon cast iron (LCI). The LCI was obtained
by blowing oxygen through Cr-Ni cast iron in a converter with a
Z.5 t capacity. Rolls 515 mm, 480 mm, and 400 mm in
diameter were cast into a lubricated metallic mold at tem-
peratures between 13600-14000C. Two versions for the modi-
fication of LCI in the converter were investigated: Fe-Si of
the SI-45 type and Si-Ca. After the Fe-Si processing of LCI
containing 0.6-0.8 percent Si and 0.8-0.9 percent Cr, no carbon
remained in free state, whereas after Si-Ca treatment most of
the C was in the form of graphite. Compared with the LCI with
Card 1/2 Fe-Si, the LCI with Si-Ca exhibits better fluiditv, In order to
4i .V 14111; 1 -1

1 37 3-5920
Low Carbon Cast Iron RolLs
attain an HB of 380-400, it is recommended that the rolls be cast at tern-
peratures of 13600-14000 with cast iron of the following chemical composition:
in the case of Fe-Si treatment: 2.4-2.6 percent Ct,t.; 0.9-1.0 percent Si;
0.5-0.6 percent Mn; 0.8-0.9 percent Cr; and 1.2-1.3 percent Ni; in the case of
Si-Ca treatment: 2.4-2.6 percent Ctot. ; 0.6-0.7 percent Si; 0.5-0.6 percent
Mn; 0.9-1.0 percent Cr; and 1.2-1.3 percent Ni. Rolls made of cast irons
exhibit uniform hardness and uniform cross-sectional microsLructurc. The
durability of LCI rolls is 2-2. 5 times that of rolls made of cast irons of
standard C content; their employment has resulted in a 3.5 percent increase
in productivity of rolling mills.
E. Sh.
Card 2/2
J V

VORONOVA, IT.A., kand.tekhn.nauk;.O~~ N. M.P., Insh.; TROSXUNOV, Ta.U., inzh.
ARMN, V.D., insh.; LIPEM, B.G., Inzh.
Rollers made of low-carbon cast iron. Biul.TSNIICHM n0.17:27-36 157.
(min 11: 4)
l.InBtitut chernoy metallurgii AN USSR i Stalinskiy metallurgichookiy
zavod.
(Rolling mills)

"Effects o" the 1~nviroriment on the llio~:i,-Icatior n4 Prrm~!rtlos o' Tmflurmza Virus,"
I"Lv o" V7!-,z~-es, ~:tat.E~
V. V. 301OVI-vtw, S. t.'art-_Inj.kov".i' N. 5'. 6I.J.mnrf T,It
im.eni L. A. Tarasevich
"Zhur ~'.Tikrobiol, Eri:k!micl q i Liimunobiol" 'No 1, pp 12-16
Adaptation of the -fresh huiran influenza strain 11,mi to white L,creises patho,_~enicity
0" mice, raises hema~-Jutlnln UL_~rs townr,4- ch;c` n and -',Uinea
the strain to ,:hite
pi,; eryth-rocytes, and increa~ies tho toxic.1ty. he antl.~,-Inic rs are
also mo-!-ified. A dantation o'-"' this sfrain 41-1o all-witoic tissue chir!-,~~n ei:'bryos
incrr-,ases to sr--me 2xtent toxIcity is meaE~.ire,; 1,v Iritrc~;ixIn - the virus -Intc the -nnterior
chamber o ~' r abbi tsIeyes. The antigenic charactcristIcs r-,~rrain uric hn, and the
lack of pathog(.Inicity towards white mice L- r-it-Ined.
.Pk 21,lTg

US.',R/~-'edicine- Infect-!Duis Deseases
7
5~3
11 The Characterisl~ics oil Substances Which Pro,-~uce Shwartzman's V,nenon,~~non,ll Ye.
Melikova-, S. L. Stepanova, 1.. R. Gutman, State Control 7,111L 1::,,eni L. A- Tarasevich
"Zhux "fik-robiol, EpLiamiol , i laimunobiol" 'so 1, pp 72-73
Shwartzman's phenowenon (I) is produceci a!,onts which hav,,? no,- anly a preparatAve,
out also a releasin.;7 capacity on similarly to t'il-trat~~s ofF I~okiUlon cultures, of'
col 1 . Un-!-'~r uge o' the metlic-, describe Jiphthiz~rla, L;-~tnuws, ano
-o: . I i- mo
brucellesis bacill.i do not pi Juce s ;t prt~nuutwo:; kact-?ria o~* the
intest-inal group. S-forws o~ B. coll pro~ijce a more ru.6 c.lrtalln T thnn
H-f orms . 'When 1 is Pro4.iAced i~i ~Irictorllrev-Shit,-a d--,,:,-%?nI2ry bncill- prepar-at'-ons
freed ol-~xotoxln, the pt-Ircenta-e or wiLmLd-s which lie afb-x a vorU;,re
is 2.-3.-3 times Uiari with the ii.,le ol' ~Iexn~~r d'V-,eTIf.t!rv or t.%phoH microb--
pr!ipns.
VA ;?~atlo

USSR/Medicine - Influenza Vaccines Oct 53
"Modifiability of A Influenza Virus in the Process
,of Adaptation to Chicken Embryos," V. D. 3olev'yev,
11. R. Gutman''Div of Viruses, State Control Inst
-2 Sera and Vaccines im Tarasevich
Zhur Mikro Epid i Immun, No 10, pp 65-68
Prolonged passing (100 passages) of A inflAenza
virus strain Em, through the allantoii of growing
chicken embryos increased the -infectiousness and
pathogenicity of the virus to chicken embryos.
Adaptation to chicken embryos increased somewhat
26&:22
the toxicity of the virus to rabbits urd raised
the level of its hemoagglutinating activltly to-
wards chicken and guinea 'Dig erythrocytes. The
virus adapted to chicken embryos (EM3) has the
capacity of deveioping on the mucous membranes
of the upper htunr%n res-11' -ratory tract (--), the
property of creating leukopenia in the per5ons
immunized (II), rind that of producing antibodies
(III). While indices of I and II are lower in
EM3 than in Em Em3 is taore activ(! '-han the
variant ad 1-t inl~ (Em2)'
266T22

GUTKAN, N.R.; MMOVICH, 1.
Significance of virus Al in the epidemic process in influenza.
Zhur. mikrobiol. spid. I Immun. no.9:38-43 S '54. (MIRA 7:12)
1. Is
imeni
(sav.
tuta
otdela virusov Goaudarstvannogo kontrallnogo inatituta
Tarasevicha (dir. S.I.Didanko) I kafedry epidemiologii
prof. V.D.SolovOyev) 11 Moskovskogo meditsinskogo insti-
imeni I.V.Staling.
(INFLUINU, epidemiology,
role of influenza virus A, in
morbidity)
(INFIMMU VIR'USIS,
Al , significance in increased
Influenza)
increased hiberaal
hibernal morbidity of

SOLOV'YEV, V.D, GUTRAII, N.R.
Modification on the antigenic structure of influenza virus in
experimental conditions. Zhur. mikrobiol. epid. i immun. no.10:
44-48 0 954. (MIRA 8:1)
1. Is otdela virusov Gosudarstvennogo kontrollnogo instituta
vaktain i eyvorotok iment L.A.Tarasevicha (dir. S.I.Didenko)
(IlULUINZA VIRUSES, immunology,
antigenic changes)

MELIKOVA, Ye.N.; GUTMAN, N.R.; STEPANOVA, S.L.
--.- 1 41-1 -..,
Schwartzmann phenomenon in rabbits vaccinated with typhoid and
Flaxner's bacillus preparations. Zhur. mikrobiol. epid. i immun.
no.10:98 0 154. (MILRA 8:1)
1. Is Gosudaretveanogo kontrollnogo Instituta im. Tarasevicha.
(VACINATION)

IIELIKOVA,Ye.N.; STPTANOVA, S.L.; GUTHAN, X.R.
Comparative experimental study of the antigenic and irnmnogenic
properties typhoid fever and dysentery (Flemner's) antigens.
Zhur.nikcrobiol.apid. i immun. no.8:104 Ag '55 (MLRA 8:11)
(AMIGENS AND ANTIBODIES) (IMERTHELLA TTPHDSA)
(SHIGELLA PARADYSSMICRD3)

C II ~, 1 1.11 N, ~f- n-
11 ,.
GUTMAN, N. R.: "Hereditary properties of the influenza virus and its
varigbility under experimental conditions." I-Iin Health USSR.
Central Inst for the Advanced Training of Physicians. Moscow, 1956.
(Dissertation for the Degree of Candidate in '-'edicnl Science.)
Knizhnaya. Ietopis'
No 32, 1956. Voscow.

- XAIjY.AYI;V, A. V.
f
Strains of influema virus A-L isolated in 1956 [wIth au.-mary, in
Anglish]. Vop.virus. 2 no.3:146-151 My-Ja '57. 10-10)
1. Otdel viruBov -Minskovskogo neuchno-insledovatel',./,-...~,,o instituts
vrAktsin i eyvorotok imeni I.I.Mechnikova, Koskvt..
(IWLUEN',',A VIRUSEb.
Al strain (Rue))

USSIR/HuEan and Ani:ial Viruses. Grippe Virus E
Abs Jour : Rof Zhur - Blol., No 4, 1959, No 14608
Author : Gutman N.R.
f-h
Inst o 'Moscow Institute of Vaccines and Sera.
Titlo The Changes of the Antigonic 3tructuro of the
Virus of the Grippe In Exporlr.~onts on Mice.
Ori,-
Pub : Tr. Mosk. n.-i. in-ta vaktsin I syvorotok, 1957,
9, 13-21
Abstract : Following 9-10 passa3os of the PR-8 strain (type
A) in mice il=.unized with the strain PR-8 and
Shkl, a variant PR-8-I-mlco was obtained. (Typo
A'). The changed characteristics woru preserved
following passages In normal mice. The pas3ages
of the rR-8 strain in -.iice li:imunlzed with the
honolo3ous virus did not load to char43es in Its
antigenic structure. PR-8-I-alco proved to be
Clard 1/2
7
USOSR/Human and Ani.---ial Viruses. Grippe Virus E
Abs Jour : Ref Zhur - Biol., No 4, 1959, No 14608
Identical In antigenic structure to the variant
PR-8 In chicken oubryos, In the presence of an-
t1bodios to the strains PR-8 and Shkl, oven
though the variants differed in their patho-
Genicity to mice. -- T.Ya., Luzyanina.
Card 2/2
Human jr Influenza , Virus. -P-3
ussR / Virology. .1d Animal Virus,~s.
Abs Jour : Rof Zhur - Biol., No 18, 1958, No 81231
Author -.-Pulmap -Nq, Rk
Inst : moscow,Scientific Research Institute of vcccin-s and Sera.
Title : Characteristics of influenza B Virus Strains.
Orig pub : Tr. ~bsk- n.-i. in-ta %ra1ftsin i syvorotok, 19571 9, 22-28.'
Abstract : The increase of disease in January-February 1955 was caused by
influenza virus type B. The antigenic structure Of tha strains
is closest sorologica.1ly to strain Kri mid differs marko(Ily froll
sbrain Li.
Card 1/1

USSR / Virology. Human and Animal Viruses. Influenza
Virus.
Abs Tour: Ref Zhur-Biol., No 2, 1959, 5339.
Author : Gutra-an N. R Palyayev, j~6. V.
Inst : -Mat'(51 lific Research Institute of Vaccines
and 3era.
Title : New Strains of Influenza Al Virus.
0'rig Pub: Tr. 'osk. n.-i. in-ta vaktsin i syvorotok, 1957,
9, 29-31.
Abstract: No abstract.
Card 1/1
E
17
ly
I NST.
M%,'
URIG. YUB.
~ABSEUCT
lie. 19% 3X?%-
Gutman, N. R.
-s and Sera
Yk 4! -1i ~. kkrch In'!Aitute ~)j vncrinj_ US
,~Yatnral Sni-rdlpoy, Vir -
stutly of tii4t.* P~7op,~rtles, of -Lbe.
orulak, 1957. 9,
1, n-ta vllktsill
Ma.;Jrovsk. n. -i. i
ed
2 strains of the jiyus ,)f natural '.N'tre isolat
th-40th
he 30
oj patients with !11y1jil~pox on t'
front t1le,
day of the disease in thn- 3rd Und 5tli.paasages throu&'),
/--day
chick ehibryos. The cho I. joalla-ato Lc ally infected I'
chick embryos were. incubmted for 7 -96 hours at 330.
I virus strain studied in 75 pp-sgages through chick our.
embryos was pathogenic for chick embryost infec'i
for rabbits after Intradermal injection. and toxic for
glatination of
ynice. The virus produced er,.,`.,eocytc
9 'j L1'Q o f the chickens out of 300 examined. In the

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