SCIENTIFIC ABSTRACT KURBASOV, A. S. - KURBATOV, A. I.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000927620013-1
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 23, 2000
• Sequence Number: 13
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

YIREiASOV, A.S., kand.takhn.nauk
Improving the commutation of electric traction motoru operating
on a pulsating =-rent. Vest.TSNII 15'S 20 no-4t8-11 961.
(MIRA 14:7)
(Electric railway motors)

URBASOV) A.S., kand.tekhn.nauk
What causes the wear oS the collectors of electric tract.ion motors.
Vest.TSNIIM 21 no.748-11 162. -(MIRA 15:12)
(Electric railway motors)

-KWU"QT,-Aj.., kand.tekbu,bauk (Moskva)
Fundamentals of the-pover theory of the com=tation of doce
machines. Klektricheefto no.7:V*-28 J1 162, (KERA 15:7)
(Blectric'muhinerr-Direot current)
(Camtation (Electricity))

WMIS"OV, It.S., kandatokhri.nauk (MwAva)
....... 6,:- -- - -
Calculation of the com-,utation of d.c. machines. -Elektrichestvo
no.8:0'9-72 Ag 162. ('11111U, 15:7)
(Electric machinury-Diroct current)

KOBASOVO Aleksandr Sevantlyanovich, kand.tekhn.nauk, starsbiy nauchnyy
-----*o-fr-uN-Ik
Power Consideration in the theory of co=utation. Izv.vya.ucheb.
zav.; olektromekh. 5 no.9tlO?6-l(Y79 !62. (KCRA 16i1)
1. Vsesoy-uznyy nauchno-issledovatellski7 institut zheleznodo-
rozhnogo transporta
(~omautatlon (Eleo4ficity))
(Electric machinery-Direct current)

KUfWASIJV, A.S., kwid. takhn. nAuk
Devico for checking the coimaitation of olectric traction motoro,
Vest. elektroprom 34 no.6:53-56 Ja 1639 (MIRA 16:7)
(Blectric railway motors-Testing)
(Slectric measurements)

ALEKSEYFV, A.Ye.; KffVOSTOVp V.S.; KURBA.)'OV9 A.S., kfind. tekhn. nauk
Concerning A.S. Kurbasov's articles 'Trinciples of the energy
theory of the commutation of d.c. machines" and "Calculation
of the commutation of d.c. machines." Elektrichestvo no.12:
75-81 D 163. (MIRA 17:1)
1. Chlen-korrespondent AN SSSR (for Alekseyev).

KURBASOVIP A.S., kand.tokluij~aWc
Critoria of the coviihationa-1 atrringth o&A..c. machines.
Elektrotekbhika 34 no.9.-9-12 S 163. (MIRA 16:3.1)
i
I
I
I

KURBASOV, A.S., kand. tekhn. nauk
Experimental determining of induction In the commutation zone
of traction motira for electric locomotives. Vost. TSNII MPS
23 no.7:27-30 164. (MIRA 1813)

.1 gotrudn'k
KURBASOV, Aleksandr Sevaslyanovich, starshiy naucliny,
Current distribution between brush holders of the same polarity
in electric traction motors. Izv. vys. ucheb. zav.; elaktromekh.
8 no.4:477-479 165. (MIRA 18:5)

lc~IJRBA-~707) I
I A.S., kan(I. oklin.rau'r-4 WINCT
Fxperimental r,4.udy of the potential conditirun3 of the traction motor
collecton3 of electric locomotivao. Trudy TS11TH MPS no.286.160-165
165. (MIRA 18:8)

ACC NRI SOUIZC~ CO 01663
Aul"10R.- F=basov,-Alo~Aandic Sovantlyanovi,!h. (Candidato of technical sciences; Chic,
5cionco associa (Chief engineer)
ORG: ffurbasaj All-Union Scientific Research Institute of Railway Trianijort
(V-,o-oyu=yy nauchno-ia31od-ov-a-E6lTi-3TE[Y-:fn-Fillu-f-z-ho-lo-zn76ffo-r-o-gi-n-or-,o--tr-a-n-a-p-or-fA);
follc& Eovochorkausk Electric Locomotive Works (11ovochorknooldy eloktrovozo-
stroitollnyy zavod)
TIM: Construction of load inserts in tho frame of a pulsed current drive motor
SOURCZ: IWZ. Elolctromokhanika, no. ), 1966, 28)-287
TOPIC TACTS: electric z
,vtor, alternating current
1~ - A
OSTIUCT: An NB-412H rive Mato has no special frame devices for passing
the variable component of the commutating current, and therefore it exhibits
up to twice as much brush arcing when it is operated with a pulsed current
as compared with d-c. Previously proposed load inserts for the cast frarne
of this motor were defective in that they were designed solely for the
jalternating commutating current but shorted the constant current of the main
:poles; furthermore they became saturated, %bich sharply increased their
gnetic resietance to the alternating current. A design is proposed that
avoids these defects.
Card 112 iw! 621.111

--L 31701-66
ACC NRs A1'tQZ1J.3b 0
,The new inserts ai-~ laminated packets) the element a of ,hich are stamped out
ofan electrotechnical steel. Owing to a system of gaps) magnetic resistance
to de of the main poles is increased) whereas it is practically unchanived.
f6r--i~'O' *d-c component and is *significantly decreased for the alternating
,component of the interpoles.
Tests of the modified design were made at the Central Scientific Research
,Institute of the I~TS, and the results indicate greatly reduced arcing. Other
results are tabulated and compared with tabulated test data for an unmodified
motor; the :~m ro nt in operation is marked.' has: 3 fi* .. .
p eme Orige art* Gures and
2 tables, 17 . .
,rjpRs
SUB CODEt 09 / SUM DATEt 12NOV65
Card

L P1298-67 ~ _ EWT(l ) / 1-1 - . . - - _1
r-A-
AC_CNR_,,AP60l5'M SOURCE CODE: UR/0144 66/006/004/6410/0415
AUTHOR: Kurbasov, A. S.
ORG: none
TITLE: Magnitude and phase of the commutating flux in various types of traction-
motor stators
~
1URCE: IVUZ. Elektromekhanika, no. 4, 1966, 410-415
TOPIC TAGS: electric motor, dc motor, commutation, electric traction
ABSTRACT: The results are reported of an experimental investigation of these d-c
traction motors: (1) DPE-400, 400 kw, 1500 v , 4 poles, cast-steel frame,
laminated main-pole cores; (Z) NB-41Z, 650 kw, 1450 v, 6 poles, design same as
above; (3) NB-412 M, 690 kw, 1450 v, laminated (0. 5-mm) commutating poles, cast-
steel frame, 4 (0. 5-mm) laminations ("insert") under main poles; (4) NB-415 A,
720 kw, 1450 v, 4 poles, a larninated core including commutating poles placed inside
the cast-steel frame. Motor performance was tested under both pulsating -current
conditions (with various ripple factors) and d-c plus 100-cps current conditions; the
Card 112 UDG: 6Z1.3.013.4+621.3.091

A'eCNR. AP6015029
Jac was fed either to the commutating poles or to the armature winding. Conclusions:
1(1) Types I and Z stator designs are permissible if the a-c component of the reactive
lemf is lower than the noncompensated emf; (2) The stator magnetic-circuit
characteristics are better (the degree of noncompensation of the reactive eml equals
0. 65) in type 3; (3) The type 4 stator improves the magnetic -circuit characteristics
1
.only to a certain degree; (4) As the magnetic - circuit saturation is approached, the
ia-c commutating flux either changes little (type 1), or essentially decreases (types 2
iand 4), or increases (type 3), (5) The laminated insert (type 3) reaches saturation
!very quickly; at ZOO amp, the insert passes only 201o of the a-c commutating flux; the
laminated core (type 4) reaches saturation with s malle r -than- rated current. Orig.
lart. has; I figure and 2 tables.
UB CODE: 09 / SUBM DATE: lOJu163 / ORIG REF: 002
i7. Card 2 / 2 Ir

ACCESSION NR: AP4037178 S/0069/64/026/003/0330/0334
AUTHOR: U~r asoy,_V
TITLE: Relationship between dichroism and the degree of polarization
in the electrooptics of colloids
SOURCE: Kolloidny*y zhumalt v. 26, no. 3r 1964, 330-334
TOPIC TAGS: colloid, electrooptics, dichroism, polarizations
dichroism polarization correlation, intrinsic dichroism, Kerr
effect, orientation theory, spectrophotometry, polarization spec-
;,,tral function, dichroism spectral functions optical density,
hydrosol
I'ABSTRACT: This article proposes and experiment'ally verifies a
formula correlating dichroism and polarization. The study ini-
tially consider3d two basic quantities usually used as a measure
of electric dichroism: intrinsic dichroism, as determined by the
formula:
D (k + A.L~
(where and k.L are tho'coefficients of extinction for incident
Card
V~W

,ACCESSION NR: AP4037178
light components parallel and perpendicular to the direction of
orientation)- and the polarization of light passing through a
dichroic medium: P (I.L
1(where IH and'11 are the light intensities of the vibration planes
-parallel and perpendicular to the electric field). Further con-
:sideration developed the following expression based on the formula
of the orientation theory of the Kerr effect, for the absorption
of colloidal solutions in an electric field:
k - (k I + 2h.L)/3.
The following relationship between dichroism and polarization was
also determined: 3 In fit + PKI - P)j
D
6kd +1n ((i +,P)I(t - P)l
.It was concluded that dichroism can be determined if polarization
:is known and if the optical density of the solution without a
...... field is calculated from spectrophotometric measurements: kd -ig(L/I).
;It was'.determined graphically that the degree of polar-
lization approaches unity*with high optical density values and
Card W4

ACCESSION NR,. AP4037178
significant dichroism,that the polarization does not change with
change ih dichroism or optical donsity,,and that the spectral
function of the degree of polarization approximates that of dich-
roism. An examination of the absorption spectradegree of polar-
ization,and dichroism of dyes (methylene blue acid and neutral
Congo red, Brown Kkh): adsorbed on cellophane shows there is
agreement between the absorption spectra and the polarization and
dichroism functions. The stationary method for determining eloc-
trodichroism (measuring the optical density of plane polarized
light passing through a colloidal solution placed in an electric
field) was used in a study comparing the dichroism and optical
density of the hydrosol of Brown Kkh and of the acid hydrosol of
Congo rod. It was found that the developed formulas I and II hold
true for molecular-disperse systems; and the experimental data and
values obtained by the equations I and II differ by less than 5-6%.
1,Orig. art. has: 1 table, 3 figures,and 14 equations.
ASSOCIATION': Kry*mskiy pedagogicheskiy institut im. M. V. Frunze
Kafedra fiziki (Krymsk Pedagogical Institute, Phyaijcs
Department)
Irl'~7 3/ 4
N

ACCESSION NR: AP4037178
;iSUBMITTEDi 2lJan63 ATD PRESSt~ 3071 ENCL: Oo
SUB CODE: Go. EK NR REF SOV: 005 OTHER: 003
4/4
Card

KURBASOV, V.V.
Particular foaturev of the electrical dichroism of Congo red
hydrosols. Koll.z~ur. 27 tio.3:396-401 ltr-Je 165. (1,121 18:12)
1. Ya-ymskiy pedaeogicheskiy institut imni Frunzet kafedra
fi7iki. Sulinitted Jan. 10, 1964.
. ..... . ......

ACCESSION NR; AP4019968 5/0020164/154/006/1303/1305''
AUTHORS: Grasyuk, A.Z*; Zuyevj V*Se; Kokurin, Yu.L.; Kryukov, P.G.4
Kurbasov, V.V.; Lobanovj V.F.; Mozhzherin, V.M.; Sukhanovi'mr,
he- y*kh, N.S.; Chuvayev, K.K.
rn
TITLE: Optical moon ranging
SOURCE: AN SSSR. Doklady*, V. 154, no. 6, 1964, 1303-1305
TOPIC TAGS: laser, ruby laser, moon ranfing, moon
light reflectiong celestial rangingtopt cal ranging
.ABSTRACT: The paper de'scribes the preliminary results*.of moon
ranging with a niby laser. For the transmission and reception of
the light lses, a telescope was used with a mirror diameter of 2.6
M. (see Fig.fulf die: Endomxe)'* 2m lasw %med vas developed by V . S. Zuyev Ind
i'P.M. Kryukov and had the following parametera: wavelength 6943 t
I pulse energy 50 to 70 Joules, pulse dur*tion 2'psec,, diameter
*11.of the beam 2-1 mm., and divergence 3t. By taking into consideration i
:!-the light"scattering in the atmosphere, the diameter of the spot on
1:the moon is estimated to be 14 km. For the detection of the signalp

ACCESSION NR: AP4019968
a photomultiplier cooled with dry ice was used. The signal to noise
ratio was 0.16. Therefore, statistical treatment was necessary.*
The authors believe that the results prove the reality of the re-
flected signal. "The authors are grateful to corresp. members A* G#
Basov and A. B.'tSeverny*yp and to B. I. Belov, F. Kh. Nigmatullin
of the Lebedev Phys. Institute, and to V. B. Nikonov, V.-K. Prokof~qv~
P. P. Dobronravin, N. V. Stesheuko, and B. P. Abrazhevskiy of the i
Crimean Astrophysics Observatory." Orig. art. has: 1 figure..
ASSOCIATION: Fizicheskiy institut im. P.N. Lebedeva AkMemLi nauk
ISSSR (Institute of Physics, AN SSSR), Kry*makaya astrofizicheskaya,
.iobservatoriya akademil nauk SSSR (Crimean-Astrophyaics Observatory,
AN SSSR)
ISUBMITTED: 05Nov63 ATD PRH~Ss '3047~" ENCL: 01
SUB CODE: W, AA NO REF SM."00; OTHERt 001
2/3

ENCLOSUREI 01
~6-rd-,
3/3
Fig. 1. Diagram of unit for optical moon
rangLag
T - Telescope; OKG - optical quantized gen-
erator; L, matching Ions; Z - throwover
mirrorl D diaphragm; IF - interference fil -
ter; FZY electron,photomultiplier$ OK dr
y
er
Lee contain6r,
ACCESSION NRi AP4019968

L 22702-66 on 1
JJP(c) JXT(Wd)/(.N
ACC N I AP6010439 SOURCE CODE: UR/0386/66/003/005/0219/0223
AUTHOR: Kokurin, Yus L ; Kurb&sayj..V*,Vs1: Lobanovo Ve ro; MozhzherLa
Vo He; Sukhanovskiy, A, N
ORG: Physics Institute Lm. P. N. Lebadev Academy of Sciences SSSR
_SSS-RT
kv/
TITLE: Heasuring the distance to the _Rq_91 by an optical method
9M
SOURCE: Zhurnal eksperimentallnoy i teoretLeheskoy fiziki
v redaktsiyu. Prilozheniye, v. 3, no. 50 1966# 219-225
Pialms
tO
TOPIC TAGS: moon, moon earth distance, distance measurement, Moon,
location, optical location, laser application
ABSTRACT: A description is given of the experimental measurement of
the distance to the moon by means of an optical locator. A schematic
of the locator is shown in Fig. 1. Ruby laser I and photomultiplier 2
are fixed rigidly in the Kude focus of telescope 3. A tunable inter-
ference filter 4 is placed in front of the photomultiplier and behind
diaphragm 5. Hirror 6 can be automatically switched from receiving
to transmitting operations, Photonultiplier output amplifier and pulse
shaper 7 follow 2, and the measurement of the time intervals between
the emission and reflection (from the moon) of laser pulses is made by
Card

227~J2-66
[`~C- C NRt AP6010439
Fig. 1, Schematic of the locator
counter 8, which is activated by that portion of the laser pulse
directed to the photomultiplier. The laser o terated at 6943 1, with a
pulse energy and duration of 5-7 j and 5,10- sac, respectively. The
diameter of the main telescope mirror was 2*6 m and its focal length
104 m; the beam diameter was 13 mm, and the divcrgence of the beam
reflected from the telescope mirror was 3o3 see of arc. The filter pass-
band was 10 X, and the instrumental error in the measurement of time
�10-7 sec. The observation of the lunar surface was confined to an area
Ilocated at the bottom of the Flammarion crater with the selanosraphic

-f Aj
ACC NRI AP6010439
Npulaes
f0
.8
8
.6
4
2
Fig. 2. Results of measurements
0 /0 20 JO 40 50 60- V W
tE'-tT, Usec
coordinates of A-3*.57 and 0-2*.98. The results of observations are
shown in Fig. 2, as a frequency distribution of the quantity tE-tT in
10-poee class intervals (tE and tT are the expertmental.,and calculated
times, respectivelyp required by a signal to c6mplete the round trip)#
The signal-to-noise ratio was 1-5 and the mean of the useful signal was
found to be distributed within the 15-20 usee class boundary, with
a standard devidtion of 1.2 x 10-6 - _sec.,~7 The total A-.erroi
_:Cn-po s itfion-ing -t h adistribution center was 1,1.3 x 10-b see, which corre-
4

ACC NRi A P 6 0-1 0439
sponds to-31200 m error Ln the measurement of dLotance, OrLg. art, has:
2 figures. (YKJ
SUB CODE: 20/ SUBH DATEt 22Jan66/ ORIG REFt 002/ OTH REF 001
ATD PRESS94(2 17
a
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ACC NR, ANO19595 UR/0293/66/004/003/0414/0426
SOURCE CODE
AUTHOR: Nokurinp Yu. L.; KurbasoV, Ve V.; Lobance, V. F.; I/Whzhoring V. 14,;
Sukhanovskiy, A. N.; Chernykh,. N. S.
ORG: none
TITLE': On the foasibility of measuring lunar disk and orbital paramotors
by optical radar
SOURC6: lbsmichesklye lssladovnntya, v. 4, no. 3, 19660 414-426
TOPIC Z%GS: lunar albedop moon, lasor application
ABSTR,kCT:
Yu. L. - Kokurin and coworkers (11 have reviewed the thcoretical
problems in laser ranging of the moon, with the object of determining more
accurate values for several Earth-Moon parameters. The authors discuss
methods for 1) obtaining a more detectible reflection signal and 2) using the'
measured range to compute such parameters as mean lunar orbital radius,
lunar disk radius-parallax constant. and Earth equatorial radius.
The basic range equation for a reflected electromagnetic signal is taken
:as astarting point. The factors are the same as in the radar range equation,
except that the return signal varies inversely as the square, rather than as
the fourth power, of range, since it is assumed that all the generated laser
flux is incident on the Moon. Using an average figure for atmospheric ab-
sorption, a lunar albedo of 0. 1, and an effective t e I e s c o p e a r e a o f
5.3 m2 (actual area of aAalescope currently in use), the authors calculate
Card-1/5 UDCs 523.31.082.5 + 521.61.082.5

ACCKRt jPG0i9595_____
that the re1zitiontihip between rc.-flected and tran5mitted energy it;
Wrefl.,", 2, x 10-19 Wtr-
It follows that with the highest sensitivity photodetectors now available,
Wt,, must be at least 150 joules in order to obtain from the Moon a con-
sistently detectible reflection, i.e. , one that does not require statistical
.analysis to be detected. The pulse must be as short as possible, to maxi-
-mize range resolution; however, present laser pulses of the energy level
demanded would have durations of the order of milliseconds, which means
a range uncertainty of several hundred kilometers. If Q-switching is used
to shorten pulse time, there is an intolerable lose in power amplitude. The
conclusion is that only when more powerful short-pulse lasers are developed
can there be a significant refinement in lunar ranging measurements.
Factors which degrade the laser technique are also discussed. One of
these is the unavoidable divergence of the beam in the atmosphere, estimated
at 2" to 3", which would give 'a lunar spot of some 3.5-5 km across. Con-
'Lour irregularities within the illuminated area can add to the range un-
certainty in the return signal, in the form of range "smear. " Owin'r to the
Moon'6 curvature, a similar effect occurs which increases as a funt;Lion of
0-r C!---

ACC NR, A1,6019595
the distance of the target area from the center of the lunar disk. An obvious
way to improve'the technique would be to place some form of mirror on
the Moon; the authors propose an optical corner reflector for this purpose
(see Fig. 1) and have analyzed ways of optimizing Its ~csign. With the density.
of the reflec tor material assumed to be the limiting factor, it is shown that
one large reflector is more effective than several small ones. For a glass
corner reflector the gain 0 in return signal over that from the lunar sur
face alone (assuming a ruby lasei) is calculated to be 0 = 2.15 x 10-1 a'
0
where a is the length of.a.joint edge in cm (see Fig. 1). Assuming a glass
density of 2.7 g/cc,. the authors find values of gain ranging from 8 = 25
for a cm up to 0 - 1330 for a 28.2 cm. Some loss in reflectivity
'7i9. 1. Corner reflector'(Hexagon indicates effective reflective are4
musi be anticipated, such as by dust contamination, so the foregoing fig-
ure.s are based on a reflection coefficient of only 0.5...
Ca,d 3/5
p
F
17,

ACC NR. AP6019595
A
4
Orientation of the reflector would be critical. If the plane of the aper
ture is not nearly normal to the laser beam, a severe loss in return signal
-results; for example, a 151 offset would mean a signal loss of approximately
307o (Initial acquisition of the reflector is not discussed). Constraint3 on
reflector geometry are also quite severe, if diffraction losses are to be
minimized. For a reflector with a = 14 cm, it is estimated that the angular
tolerance between adjoining planes should be held within 0.1"; with such
tight tolerances,. t9mperature extremes and mechanical stresscH could be
d 4/5

ACC NP. 1-3019595
r-LL
c
"ical factors in-refle6tor performance. Under reasonably good condi-
tions, however, it is calculated that a reflector with B = -40 would return
an adequate detectible -signal to Earth from a Q-switched ruby laser of
4 to 5 joules output.
The possibility of confusing a genuine signal with noise or surface
rather than reflector return can be minimized by using Inultiple Lletcction
and correlating the results. In fact, if three photomultipliers, are used
simultaneously, the experiment could be performed in daylight, with a low
probability of error.
The authors conclude by giving tile procedures foi, ca1culatinif mean
lunar orbital radius (mean distance between Earth and Moon mass centers),
radi,js of thc lunar disk, Earth equatorial radius, and Parth-Nloon parallax
constant. All of these are obtainable froin luiowledge of an arbitrary line-
of si( lit distance from the rarth to the Vioon, nicasured as described above.
! The caiculations sho%Y that, with tht, improv,.-d ranlring method, parameters
such as the Moon's orbital radius and disk radius could be determined to
accuracics of 6everal hundreds of rncters, a great improvement over tile
present as--curacy of several k1loineters. Unfortunately, these 'accuracy figures
d t Ppem to b ed. to any tolerance on the range measurement.
~kMB~ V. Z,-no.'Y~ Orl ff IL
art, hns: 33 form iapoLfl tos nnd ) tablo.
~-Card 5/5 SUB CODES 03,260/ 9~TJM DATE: 26M;iy~ R G REFS 009 OTH REFS 003

AUTHOR: Kurbatkin) G.P. 49 - 2 - 9/13
TITLE: Hydrodynamic determination of the annual characteristics
of the temperature of the air at sea level. (Opredeleniye
metodami gidrodinamiki godovogo khoda temperatury voz-
dukha, na urovne morya).
PERIODICAL: Izvestiya Akademii Nauk, Seriya Geofizicheskaya, 1957,
No.2, pp. 228-243. (U.S.S.R.)
ABSTRACT: The solution of the problem of determining the annual
temperature variation at sea level is given.on a world
wide scale. The dependence of the thermal properties
of the underlying surface of the geographical coordinates
is taken into consideration more accurately than has been
done in earlier published work. The calculated examples
are compared with observation data and with resialts
Card 1/4 obtained theoretically by other authors.
49 - 2 - 9113
TITLE: Hydrodynamic determination of the annual characteristics
of the temperature of air at sea level. (Opredeleniye
metodami gidrodinamiki godOvogo khoda temperatury voz-
dukha na urovne morya).
The a1mcf the author is to present a more detailed
theory which would particularly permit taking into con-
sideration the effect Of densification and sharp bending
of isotherms near the shores. The method presented here
permits taking into consideration fully the heat flow
from the soil and providing a Solution which is lese
dependent on the slow convergence of spherical function
series. The obtained Solution Is independent of earlier
given longitude and latitude ranges. The starting
equat1on for determining the annual variation of the air
temperature at sea level is the relation expressing the
heat inflow in the form of eq.(J), p.228. The finally
derived relations are expressed by eqs.(45) and (46),
p.238. Thereby the problem was reduced to solving a
system of linear non uniform integral equations of the
Card 2/4 second Fredholm type.

49 - 2 - 9/13
TITLE: Hydrodynamic determination of the annual characteristics
of the temperature of air at sea level. (Opredeleniye
metodami gidrodinamiki godovogo khoda temperatury voz-
dukha na urovne morya).
For practical calculations a number of simplifying
assumptions are made and It is shown that even the first
approximation yields a non stationary and non zonal
temperature field which is close to the real one. In
Figs.1-8, pp.240-242, claculated values are given for
January, and in Figs-3-5, these values are compared with
real values (curves), actually measured at sea level
during January. The method, for instance, can also be
applied In long term forecasting of temperature at sea
level, taking into consideration the transofrmation of
air masses under the Influence of the underlying surface,
the investigation of the influence of the orography on
Card 3/4 meteorological fields, etc..

49 - 2 - 9/13
TITLE; Hydrodynamic determination of the annual characteristics
of the temperature of air at sea level. (Opredeleniye
metodami gidrodinamiki godovogo khoda temperatury voz-
dukha na urovne morya).
The text includes 1 table, 2 world temperature distri-
bution maps, 7 graphs, and equations throughout the text.
There are 3 references of which 2 are Slavic.
ASSOCIATION; Academy of Sciences of the USSHp Institute of Terrestrial
Physics.
PRESENTED BY:
SUBMITTED: 12/3/56
AVAILABLE: Library of Congress
Card 4/4
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1Z~c
Y~o
"Ci 112SR. Inct4pisk-4 of An-Ait'-d
104) -
0

I-T
LA
0
J.", 21
a:'OLun'l -1121.1
n~ u I.
,'lows over thoia. ljupendinL 01I thc- hc~_!Jit
0 n' of the mountain bar:Ue:cs tIi,_,_j.- influ,,_~jm~
L,_-~~e-ccclc atiro.,~pheric procosa~,.: in
c7isc.s the Ltir flo~i ovor th~, b~,.rrlcr is inost
cLnt in Uhc de'u-erT;Iination. of V.-C-2thOr
,yylos), and in othel, c2.!-,eC i-lu- ic
1111,.~ obstacle (the iliroajayas~ I-Jjr
-it- ic
u 11
In rccc~niu- yearo have apps_-Ir~~d rjany
dc;voted to "he problei.i o--:" 'u-Ile b-',
UILC flow anC or-,)L~,rzaj.,iiic obstaclz.,S; bq-'U- in
u
1/12 1 S I
bheco (00"o)

:En-lu,-,~ncc- of Or:)j~raphic Obstacies 0.-
Air Flov.
influence of mountains ic 0::-pro.,,sod by
UU
3%
where U is the zonal flow, and is tII---
of the mountain pro-Cile alonf, .,_-i contour lino.
thi--, tom takes into account on!y the afruct of
mass flfy;i over the mountuLn; it -1-ocs -not acrount
flov.r round mountain obstacli- in --~v
theoretical attorkpt ;Pado -tj-o ob-'U-,,).in -'Gho
a mountain 'by solvin,,~ an ovoi-idealizod i)roblc-,Ii in
which the nass fl(jvi over the riot-u-it-rtin v.,-2.s
for a baro-.'--,.-;) )-ic iiiodal v,,i-t';Ii r,.on :.4-
bant Incj.J-,,nt flovi
1)2:-obl(,,Li of influ~lnco o! C1110 Oil 'U110
cast flov 0 -olved by G,-,I"Ibo
paper pro.)oses another solution o~ f 'U-hi~~ -,voblcT-~, LM~
--Iiich the zonal "jov., is Lj
j~ Iroil fulic-61-011 of 1,-!,0
'~~',"12 latitude. Thl, atlGhor conrI(Ae-vI,), a

49-58-2-10/18
f1he Influencu of large-Scale Orographic Obstacles on the dest-
East Air Flow.
barotropic model. fjoiurbulent friction forces are
ic-nored, and it is a,--,umed ti--,at the air density deDends
weakly on the altitude. The boundai-j conditions are
given on the earth's surface and are, firstly, that the
normal component of the viind velocity vector to the
mountain surface is zero and, secondly, that at infinity
(pw)z__ 0. Equations of motion are written
3'..
(in spherical coordinates) vihich~,describe the motion of
a two-dimensional compressible layer on a rotating
sphere in the presence of an uneven relief on the
surface of the earth. The motion of the atmoL-phere
consisting of a pure zonal circulatior, upon which is
imposed a p rtur7bation caused b-v oror,raDhic obstacles,
is considered, i.e.
vo~vo's vxn; X+V)I" W=W, + I , 7x=a, a sin
Here a, is the earth' s radius, is tho complement
of the Geographical latitude, X is the geoGi-aphical
Card 3/12 lonGitude, v, , v. and w arc the 'velocity components

The Influenec, of Jarge-Scale
East Air Flow.
OroGraphic Obstacles on the --'iootu-
along the axes 4 1 X I-tnd ,, (z = r - a; r is the
distance from the contra of the etrth), fy is the
vertical component of the curl of the v(.!locity and
a is the index of tiiu circulation. Barvea qu--ntities
refer to zonal values, ~-,id. y*oimes to th-air po:Lturbat ions.
Let the su-.,.-'~-ace of the be (Winnd by the equation
z 7 ) and let H denote the hciZ~bt of the
homo no 611.01 S' 'p-t-mosphe re Then we de f ine
111( e , X) = I( i , ?L) .
H -
The linearized equations of motion and of continuity,
and the liniarized boundary condition at the earth's
surface may be written
ve, vX w
-*- (t + 2w cos + + 2(1) cos =0
a Be a sin ei + ( It 1
Card 4/12 (Eq.7)

~9-~-~ Ej -2-10/18
The In-^11.1(, -e on -'-Ic "'Iest-
.1. of jar[, -Ecale Orographic Obstaclc-
-,,)Vt sin E) j + 0,
vi -'471 1
+ vxI) C~'
71 7 -3-9 + a sin
-whe re (j) is the angular velocity of the eaith, can(I
is not to be considorod a rimall ant ity
4~1 fit
~conLrary to 'Pof*2)o Tho f1motion V + i iL~
introduced, the Imovm zonal part which satisfies Eq.8
and is related to the velocities V, and VXI by the
relatiuns:
VI VI + 'ICL Sin
9 a
Card 5/12 1-ij a sin y a '.- - ! (i!,q.10)

The Influenec: of JarGe-Scale Orot;raphic Obstacles on the
East Air Flow.
Substitutin(S in Eq.7 from Eqs-10, ,.oid oliminatinL: w
from Eos. 7 and 9 with the assumptions that
(-Vpt = V6 (vj)~ = V!, and c,~ = qcL (0 Z- qt6:. 1)
-.v~! obtain for
BASF a~? 2 Wq
a- + 2(j) 2w cot 2c-,,a aICos
whe re
which is accurate to the first ord;)r of ma6pitude.
V1e note that to define the lmovn zonal deviation of the
stream functionIrl introduced for an incompressible
layer, vie obtain an equation exactly similar to Eq.11.
Cla'ard 6/12 In this case the equation of continuity has the form:

or
(v Ein + v
v V.,
sin a
Thu-s v;~. h-ave to .9olvo Eq,11 in the compres~dble ca~-,r!
usinL; and in the inm:;pressiblo case u s, i i v-,'c .1 c]: a
The solution for can be vritten in the -fona:
-in
I ( h , TW 0.1 dl~l - I . . 11
Tr 7r I _.~)L
/1. 2

lr-.I--.u(-,nee of lar~-C ,_~'calc OroUraj).Idc Obstacl~.,:-, f)n thc
jast Aj.;~ .10VI.
re
n
_N)pla(co,. q)_,h(co
~09,3' a sin E,
Cos 11 n n
n=1 h=1
'7.
W, I), =1 (Eq.22)
(Ph(coo 9,) are normalized associat-ea ie,~cn,~, re poly-
noRials). Solution of Cq.2~ wm be applied' to
ilw(~Z`AGate the influenco o-f the hir.'alaylas anC, 'Vibet on
~h_,, ~anei:-al circulat-ion of 'Glic '10he region
oZ influcnee of the lu-lhe Tib~_,-Van ixplands
i,,; talken ~_,.s -from 400-1500 lont.-l'umde, f -,.-()ia
1
150-70o N. latitude. ~,.quation 213 can bo solved by the
m-tiiod of successive appro-riLL--tions, by t,:~Idn,-~ ;Iiesh
a lon.-itude intorval of IOC) 1aI.-J.tu6.e interval
Of 50 vrith';' tems in the selles (22) -ap to n=20 and
11=8. Thi-c mesh appro:,imatcs -to the, _'ibotan plateau by
"IL 15 -?oints. The in.'c:r of circulation varies lurinG the

49-~50-2-10/18
f2j,(_ Influence of Iarge Scale OroCraphic Obstaclo'3 on the
East Air Flow.
course of a years and influences the behaviour of the
function K. flence it was decided to obtain a DicturO
of the flow over Asia for the Nvinter and su=er seasons.
CL
For the winter season is taken as OoO34, and for
the summer snason as 0*020. It was assumed that for
winter a ~:c 1/2 a, and for summer a a. Isobaric
charts for summer ar4d winter are introduced for compari-
son Ath the lines 'Y + V I = const, which are obtainea
from the solution of Eq.23. FiGs.5 and-8 show that if
only the term - V W 6T) in Eqo9 is ta.ken into account,
a sin 0 aX
the picture obtained is very far from the tzue one; 'L-)ut
if the remaining terms are included the flow round Tibet
Card 9/12 and the bifurcation of the zonal flow are obtained, In

The Influence of Iarge Scale Or-)graphic Obstacle3 on t.,e .'Os't-
East Air Flow.
Figs. 6 and 7 are clearly seehL the southern jet stream
and the broad winter cyclonic region over Tibet and to
the south of it. Thus it "is possible to suppose that
the high cyclonic region of wcather on winter maps
arises through the interaction of the central Asian
mass with the winter zonal flow. On Figs.9 andlO is
seen a depression towards the south and a weak anti-
cyclone over Tibet. Many meteorologists explain the
transition from the vinter picture to the summer one
in Tibet only by a displacement of the maximum wes-Uern
flow towards the south. The au-'U-,hor has obtained the
typical synoptic situation for summer only as a result
of the general iveakeninG of the zonal flow, its maximum
not being displaced. A reduction in the intensity
of the west-east flow and the displacement of the
maximum speed towards the south occur apparently approx-
imately simultaneously as a result of a chanGe in the
thermal conditions in the atmosphere. It seems that in
describing the beginning and the establishment of the
Card 10/12summor circulation in the reGion of Tibet, and alloviinG

Uri: - r; 1
a f tho 1.1"L ul
c i
,mirullf it i.,., to t in 0 A 01
in(! i G 0 i'L ;1,bove, ari~-dm, f'vo;71 ~-7ic -'1T c ct
CollditiOll.': ~XC VO:CY
i)icturc O-f t,c -wamor fl(,Vi. taldn'.. acccw-ilt 0-
-'Jou'Up iwt is passiblu to und:~~L-~-,Vcri,]. tho unu su,~k n. c 1
in iritcm,sity o-C 'Wic so-,!,huin j-t r-,-ofL -Umcl- "o I nt,,~-:v,
Jo i i i,) a i - i n um,,l 4 %-Ath and .10, L I I
of !311)c rr-~ f-
I'lie ivun ol)!-,Q i-v,-- -L !on c It not(,,,. on!:(
j-nf luenec of lar, -C-scale- nouri~ .U .Ln mac:--,as or-
flow has been djr,CU---~,-,. 'Lf'-or construlc-`-hi~~ thc
L, - L, u
lilies ir + T I cou."t; it i,-~, nn- di-'-Ticult t.)
a qu"Llitia,1jive c'-,P,-1u,-,,thc)n -61-Lo Tole pl:-,.y--1-'. by tl,c.
J
vc;r~ical coiaprcs~;ibliity. -;q.11 it i~.; th--i',
of the layer on'l.: a pe:trs: o,%,r.;:, i.-)
..1CAL1l'u-'dn; it "Gund-c to smooUl. oi:,'U- t 1 i,~ .'.i ont inu it iu, s
-in volocitj. 1u:; f 1, 0 11 0 1. f,:)2.- a coi ,p lb 1,D
loi T, -1- -L 0'. CJQI~1' 0 V JX " ".. 'I I
L 1, '1- ,:i,)urt-,Aa ---T be

Or.) `d.(~
U -I(,
dr
inc --rjsed. Thr~,-re are- 1.0 -riLu ;I,--nco,7, of
, 11i. - -C'ussi-,,.n --~ml
wt cli 6 ar~
A-;~C~jj,k~jol --
of '-'ciencr~s of the In:7-titutc, of
I'Llp-plicc! G,7--ophysics. GLhad~;:7dya n--.ui-- Institut
prildadnoy ,,eofiziki.)
junu 1-9, Y.: 57
L--brcvy of Congress.

AUTHOR._K4.7batkin,. -G-, PW
TITLE: The Known Geostrophic Effect
(Uchet negeostrofichnosti v
aniya gor)
~;OV/4)-59-4-9/20
in the Airflow Over Mountains
prostranstvennoy zadache obtek-
PERIODICAL: Izvestiya Akademii nauk- SSSR, Seriya geofizicheskaya,
1959, Nr 4, PP 581-592 (USSR)
AB6THAUT: The effect of airflow over high mountains is described
in the system of right-angled coordinates with no Earth~s
spherical shape considered. The motion is assumed to be
stable and adiabatic, and the atmosphere is considered as
baroclinical. The suggested linear equations are based on
the longitudinal waves. The partial derivatives of U V1
W and P are determinad aa Eqs (1-4) which are calcuiated
from the basic equations of wind, velocity, pressure, density,
and temperature (u v p , and T ) on p 582, The first
two equations (Eqs (0 aL (~ ~ can be substituted by Eq (5),
thus the value of VV(x, y, z) can be derived as Eq (6), for
which 'the limiting conditions are Eqs (7) and (8). The
Card 1/4

SOV/49-59-4-9/20
The Known Geostrophic Effect In the Airflow Over Mountains
solution of the expression (6) can be shown as
W ._(1 - Z)wo(x, y) + S(x, y, z) (Ref 2) where
the value of 3 can be calculated from Eq (9) -for
f(xy) -AWO . The latter can be determined from the Fourier
transformation (P 584) and the parameter 62 taken as
f?- 100 (Ref 10). Finally, the expression (10) is derived
which gives the solution for W When an assumption is
made that the motion is quasi-geostrophic. then the express-
ion (5) should be substituted for AP = eA . The value of
W in this case will take the form Eq (11) and its solution
will be shown as Eq (12). Then the value of W is determined
and the pressure can be found from Eq (4) and its solution
Eq (13) or Eq (14) in the case of the -quasi-geostrophic con-
ditions. The values of U and V are calculated at this
stage from Eqs (1) and (2). In order to determine the effect
of the separate harmonic on W , the coefficient k in
Eqs (10) and (12) can be analyzed by using Ok and y
Card 2/4 calculated f rom the f ormulae at the f oot of p 586 and the top

SOV/49-5~-)--4-9/20
The Known Geostrophic Effect In the Airflow Ovpr Mol_mtains
of p 588 and the results tabulated on P 587. In order to
-verify the above calculations, a profile of the mountain
was taken:
-b 2[(, .2-x )2+(, .4-y )2
ap
where a unit on the axes x and y 1000 km and on
z - 10 km. The height of the mountain was 2 Im. The co-
efficients were a = 0.2 - b = 3.6 7 the horizontal dia-
meter - 800 to 1000 km. T~e vertical velocities were cal-
culated from the formulae (10) and (12) with the first and
second approximations. The results are shown in Pigs 1 to
20. The quasi-geostrophic and non-,geostrophic cases are
shown in Figs 1-5 and Figs 6-10 respectively, where the
vertical dimensions were obtaineq for.,~ 1.8 , 1.6 ~ 1~4
1.2 and 1.0 (w' multiplied 101-' tim F' 11 and 12
show the field of vertical velocity wl X 10Y1rS,/,,, at the
.Plane z - 0.4 and z = 0.6 in the non-geostrop :hic case,,
In the quasi-geostrophic case there is a deflection of the
Card 3/4

SOV/49-59-4-9/20
The Known Geostrophic Effect in the Airflow Over Mountains
flow to the right in front of the mountain. The line of
flow behind it is bent upwards and to the left, which is
also diown La Fig 13. Figs 13 to 20 were calculated for
z - 0.2 - 0.6 . It can be noted that thewaves are dist-
inguished on the,windward side of the mountain i-n Figs 6-10
and 11-12. There are 20 figures, 4 tables and 10 references,
of which 5 are Soviet and 5 English.
ASSOCIATION: kkademiya nauk SSSR, Institut prikladnoy geofiziki
(Academy of Sciences USSR, Institute of Applied Geophysics)
SUBIMITTED: May l?, 1958.
Card 4/4

BYKOV, V.V.; XURIUTxIN,_q_j!,__-
Analysis of meteorological and aerological data with the a id of an
electronic computer. 'Dokl. AN SSSR 134 no.5:1065-1068 0 160.
(MDA 13 110)
1. Inotitut prikladnoy geofiziki Akademii nauk SSSR. Predstavleno
akademikom A.A.Dorodnitaynym.
(Zlectronic data processing) (Meteorology)

,.Y,,DV, V.V.,-
- ------
Obj ac LiVe 0 2 wirollri; '; dUta. I zv. 'I; '*S":i. Sor,
It ;l 0
" ofiz. no. 2:307-318 F 161. (1:1161 1l,:2)
.0
I* Inutitut prildadnoy t-,--o-"JiziU Al' SSO"..
,.'OrccL:jtbig)

KIRMTKINY G.P.
Two-level. pressure field forecasting for the Northern Hemisphere.
Izv. All SSSIR. Ser. goofiz. no.2:229-232 F 16?.
it I All 888R1- Gidrometaluzhba 33%II*OIARj&ennyy meteorclogichropkiy
Atmoopheric pressure)
Weather forecasting)
~

KURBATKIN, ft*.P~
Forecasting of the barometric field, temperature, and verticol
velocities of hemisphere for a period not exceeding 5 daya.
Izv.AN SSSR. Ser.geofiz. nolil2:1825-1836 162. (MIRA 16:2)
1. Vychislitellnyy matecrologichaskiy tsentr.
(Numerical weather forecasting)

ACCESSION NRI AT4034612 S/OOOO/64/OOO/OOO/OoI9/O04I
AUTHORt Kurbatkin, G, N_.
TITLE: Two-leval scheme of short-range forecasting of geopotential and vertical
movements
SOURCE: AN SSSR. Ob"yedInenny*y meteorologichaskly vy*chislitellny*y tsentr,
.Gidrodinamicheskly dolgosrochny*y prognoz pogody* (Hydrodynamic long-range weather;
forecasting). Moscow, lzd-vo "Nauka," 1964, 19-41
TOPIC TAGS! meteorologyr atmospheric pressure, weather forecasting, atmospheric
geopotential, atmospheric vertical movement
ABSTRACT: Atmospheric pressure Is forecast using the baroclin;c two-level non-
linear model proposed by Ye. N. BlInova (Doki. AN SSSR, III, No. 6, 1956), using
Blinova's vorticity and heat flux equations in a spherical system of coordinates
as the Initial equations. Forecasts for up to five days were made using an elec-
tronic computer. it was found that with an Increase In the forecasted perrod the
Indicated model causes a continuous Intensification of westerly winds In the mid-
dle latitudes; In the middle latitudes there Is a systemtlc Increase In the value
of moment of wowntum. As a result of this middle-latitude exaggeration the fore-
.ca~sts,tQr 3-days In advance already were bad and computations for 5-days In ad-
7
F

ACCESSION NR: AT4034672
vance led to unreal values of the heights of Itobaric surfaces. Two exampres are
cited as an Illustration. A smoothing method Is proposed for eliminating this
difficulty, making it possible to make generally valid 5-day forecasts (although
in certain cases processes associated with a sharp change of zonal velocity are
not described sufficiently well In particular regions). The improved method then
was used to make five sample forec st of AT3900 AT700 and OT) 8 charts and charts
of vertical velocities; evaluation:'os these torecasts are gi en. OrIg. art. has:.
14 formulas, 7 figures and 10 tables.
ASSOCIATION: OIY'yedinenny*y meteorologicheskiy vy*chislitellny*y tsentr (Joint
Meteorological Computation Center)
SUBMITTED: 22Nov63 DATE ACQ: 16Apr.64 ENCL: 00
SUB CODE; ES NO REF SOV! 004 OTHER; OW

at ni-11 Y.I I r(-)U).R anG Lne flUlw III IF U
Ts=,
gin! -q~
ei

~IIIIRA'

fin

NJ ~v4,

Walmm
LP113

i~ J
~UF

- - - -- - , - :. a,~- ~Ili-'.,4,Pz~zq,~Z-4,~,-:--.i

WKIATKIN" G.P.
Changos in the kinetic ener" of atmospher1c motlonu. Izv.
AN' SSSR. Fiz. atm. i okeana 1 no.12:12-60-1,269 D 16-5.
(MIT-J, 1.9:
1. Vychislitelinyy tsentr,sibirz~oyo otdclenlye All. S~;Slt.
Submltted I-lay 26, 1965-

L
JD70-66 EWT(I)/FCC GS/GW
;ACCESSION MR: ATSOOO059 S/0000/64/000/000/0204/0213
AUTHOR: Bykov, V. V.; Kurbatkin 0. P.1 Go 5
~L_ ~ 1 J.4 1-1 t
TITLE: Numerical. V'r,
levels analysis of the.-geopotential and of wind.at five atmospheric
SOURCE: Simpozium po, chislannym metodam pr~ognoza Rogody. Moscow, 1963. -Trudy.
Leningrad, Gidrometeoizdat, 1964, 204-213
ITOPIC TAGS: meteorology,,geopotential, wind, objective analysis
ABSTRACT: A multilevel method for objective analysis of aerological data is de-
,scribed. This method is based on representation of the field
l 'of the analyzed
:meteorological element by means of a polynomial. In the proposed scheme of object-,
ive analysis of geopotential and wind at five atmospheric levels some methods
-adopted from the usual synoptic analysis of charts of baric topography ~(ere used.
In the matched analysis at several levels erroneous Infom. atlon was cor, ct"d anti
.gaps in the data idere filled in. The results of the computations a" eiven. A new!
rethod of numerical analysis of the absolute ger4titintial Is prrcposeA tfhlcb 1A.
basc4 cn the principles of plottirg of bar.1c' topp_ffriphy rhartn. Orit. 0t, hJF31
Card '1/2

193701-66,,-..
ACCESSION MR: AT5008059
2 figures, 3 tables, 6 equationso
JASSOCIATIONt none
SUBMITTEDi 060ct64 ENCL: 00 SUB CODEt ES
NO REF SOY$ 005- OTHER:' 001

KURBATOV, A,
Comprehonsive mochanization of potato warohousea. Sov.torg. 34
no.7:5/4,-.56 JI 161. (MM 140)
(Mao cow-Po tatoes--3 torage)-

EURBANV, A.
Storing pickles in containers filled with water. Sov.torg. 35
no.l:Yi-55 Ja 162. (MmA 15:1)
(Canning and preserving)

_KURBATOV, A.
Mechanizing the sorting and packaging of potatoes. Sov. torg.
35 no.5:61-63 Mv 162. (KRA 15:5)
(Potatoes-Grading)

I/ I I i_, I ,
!\~ -,,,A % ~-
I
MANSKIY, N., Inzh.; KLWATOV -, A., Inzh.; KOSTRIKII, Ta-, lnzh.
Collective farm work-shops for current repairs. Nauka i pored* ON
v neilkhoz. 8 no.51ll-12 W 158. (HERA 11;5)
(Agricultural maohiner7--Maintenance and repair)

XURBATOV, A.
Recording instrument for multiple-bucket dreGger operations. itech.
transp. 21 no.2:_1;14 F t62, I (MIfiA 1..:))
1. Novasibirskiy tekhnicheskiy uchastok puti.
(Dredging machiner7) (Recording instruments)

KURBATOV, A.D.
Heredity modifications, and increase
by transplantation of fecundated ovum
rabbit. Effect of the mother-carrior
appearance and vitality. Uup. novrom.
120 Julr-Aug 1951.
of vitality of progeny
of another breed of
on development,
biol. 32 no.1:113-
(CUIL 20:11)
1. Loningrad.

KTRBA~~107) A. D.
"Changes of Heredity an-d Increase in Vitality of Lho Of"spr-Ing b.-t '-!Pan:3 of inter-breer,"Ing
m
transplantation of Fecundated Ovicel-1s in ~Fevzle Rabbits. --.0port !I.' (p. 11`1)
, 1,
b
y .,urbatov, !t. D.
I (Uslpokhi 'ovromonnoy U.1ologii) Vol. "M110
SO: Achievempts of iMorn Biolopm 1j
Mo3c
ow-Leningrad, July-Auguzt, 1951.

KUMATOVp A. D.j TMOXrWVAj K. H.
Metabolism
Basal metabolism in anivials rind sex of progeny. Agrobiologiia, No. 4, 1952.
Monthl List of Russian Accessions, Library of Congrass. November 1952. Unclassified.

1. KURPATOVo A. D.
2. USSR 6w
4. Rabbits
7- Change in the ingeritance of coat color In rabbits wider the influence of
the development of their parents in the organism of mothers of other breeds,
Vest Len unp 7, No. 4j, 1952o
9- Monthly List of Russian Accessions# Library of Congress, April 1953p Uncl.

KURBATOV, A. D.
- - - , , '' I - I ".
Abrupt h"redItar7
Usp. Qavreim- biol.
1. Loningrad.
ebangee in v-Abhits following cross breading.
33 no. 31466-471 MaY-Jun" 1952. (CLHL 22-4)

YUEBAT011, A. r.
EMBATOV, A.D.; TIKHOMIROVA. M.N.
Iffect of the intensity of banal metabolism in animals on the
ratio of sexes in their progeny. Uch.sap.Len.un. no.165 153.
(MMA 7:7)
1. Laboratolya genetiki zhivotnykh kafedry genatik-i i selektali
(zaveduywhchiy kafedroy professor N.V.Turbin)
(Metabolism) (Sex(Biology))

MAMTOV, A.D.; HINYATID, D.D.
MWW~-
Iffect of the &V of mated pigs on the ratio of sexes in offspring.
Vest.Len.un. 9 n0-1:57-64 J& 154. Mn 9:7)
(Swine breeding)

USSR / General Biology. Genetics. B-5
Abs Jour: Ref Zhur-Biol., No 100 1958, 42869.
Author Kurba~q
ven.
Inst 9
Title Change of Heredity In Rabbits In Intravarlety
Zygote TrAnsplantation.
Orig Pub-. B.sb..- Probl. sovrem. embriologil. L., Un-t, 1956,
ZZI-226,
Abstract: An attempt is made to prove the effect of the
mother-bearer on hereditary fetal processes. in
the experiments females of the varieties white
angora and white giant, and males of the chinchilla
variety, were used. The females and a portion of
the males were pure-bred; another portion of the
males of chinchilla variety were developed in the
organism of mothers of a different breed, i.e.,
Card 1/4
21
USSR / General Blojogy~ Genetics, 8_5
Abs Jour: Ref Zhur-Slol., No 10, 1958, 421369.
Abstract: these males were the tesult of transplanting
Intravarietal'zygotes, Through mating of females
of the Indicated varieties with pure-bred chin-
chilla males, 398 young were born, wh!ch had a
gray fur color characteristic of the chinchi!la
variety, The fur color of young begotten by males
which developed in the organism of white angora
females was not always grey. Thus$ of 9Z young
born from mating these males with white angora
females, 4Z young were grey, but 48 had a fur
characteristic of Russian ermine young, From a
chinchilla male which developed In the organism of
a white giant female and was mated with ,,bite giant
Card Z/4

USSR / General Biology. Gienetics. B-5
Abs Jour: Ref Zhur-Biol ., No lop 1958p 42869.
Abstract-. females, 41 Young were born, of which 15 had a
color characteristic of chlnchil',a; the remainder
had the color of Russian ermine young. In othe,.-
experiments the effect of the mother-bearer organ-
Ism was shown in the length of the fur cover,
Usually when animals of variety white giant, which
possess a fur cover of normal length, were mated
with short-furred animals of rex variety, the nor-
mal fur length is dominant over the short fur. In
an eXperiment by the author with a male of white
giant variety which developed in the organism of
a female of rex variety, mated with a female of
rex variety, all four offspring obtained from mat-
Ing the animals were short-furred. From his experi-
ments the author concludes that the assimilation by
fetuses of maternal plastic substances from a
Card 3/4
2Z

USSR / General Biology. Genetics. B-5
Abs Jour: Ref Zhur-Biol., No 109 19589 42869.
Abstract: different variety exerts a considerable effect on
heredity.
Editorls note: The Irregularity of results obtained
and the appearance In the offspring under experiment
of animals with ermine coloration show evidence of
heterozygoticity of the animals In the experiment,
which makes the general conclusijns of the author
hardly reliable.
Card 4/4

KURBATOVO A.D.,, kand, biol. nauky KORB4N,,II.V.
Treatment of bens and eggs wlVj hc)r.-!cn,3.1 on(!
sex of ohicke, Agrobiologiia nc.40471--'548 Jl--,'j '6".
Is Pushkinakiye 3Aboratorii razvedentya
zhivotnykb g. Pushkin, lAriingradsknya oblo:at'.

KUKUTOV, A.I. (Leningrad, P-22, Bollshoy pr., d.106, kv.38)
Tomographic study in oatoo-articular tuberculositi. Voct. rent. i
rad. 36 no.6t29-34 N-D 161. WIRA 15:2)
1. Iz kafedry rentgenologii i radiologii Voyenno-meclitsinskoy
ordena Ioenina akademii imeni S.M.Kirova.
(BOMS-TUBERCULOSIS) (JOJII'fS--TUl3EiWULOS IS)

KURBATOV. A.I.. kand. med, nauk
I
Significance of tomography In omtoomyelitis. Vest.. rent.. 1 rad. 3', no.4t
25-28 Jl-Ag 164. (MIRA 18:7)
1. Kaff3dra rentgenologil i rAdiologli (nachRlInik - prof. V.S.Vakhtell)
I kafedra voyenno-polevoy khiriwgii (nnchallnik - prof. A.N.Perkutov)
Voyenno-meditsins~oy ordena Lanina akademli im,3ni Kirova, Lenlngrnd.

KURRATOY.A.L. master
_- ~ a*", - --Kjf.~j
Automatic steam pressure control mechanism. Inergetik
no.7:13 JI '55. (MI2A 8:9)
(Manometer) (Boilers--Safety appliances)

XURBATOV, A. I.
With the railroad workera. Sov.profnoluzy 16 W-5:18
Mr 16o. (MIRA 13:3)
(Lenin, Vladimir Illich 1870-1924)
(Railroads--Mmploveqs~

.KI.J.RB.ATOV A * I priyems hchik
The 64/01.18 voltage stabilizers. Elek.i tepl.tiaga 5 n0.4.,34-37
Ap 161. (MM 14:6)
1, Depo Leningrad-Baitiyskiy Oktyabrlokoy dorogi.
(Diesel locomotives) (Voltage regulators)

STREKOPYTOV, Viktor Vasil'yevIcb;.YURBATOYp Anton Ivanovich;
YELSUKOV) V.A.) inzh., retienz4nt;*-NOVIXOV, A.V., inzh.,
red.; aROMOV, Yu.V., tekhn. red.
[Eelbttrie drive of the VMEI diesel locomotive) Blektriche-
skaia peredacha teplavoza V14BI. Moskvap Tranezheldorlzdaty
1962. 54 P. (MMA 15:6)
(Diesel locomotives-Electric driving)

BOLISHAKOV, Anatoliy Stepanovich; SARIN) Valeriy Ivanovich;
SHVAYIISHMN, Boris Simonovich; P0N0KA;XV, V.S., inzh.,
retsenzent; ZAWV3XIY, D.G.p inzh., retcenzont; VAKAROV,
M.S., inzh., retsenzent; POPOV, ON., inzh., retsenzent;
KURBATOV, A.I., retsenzent; KITAYEVA, Z.A., inzh.,
retsenzent; SDOBIIIKOV, Te.F., retsenzent; I:OVAIZV, A.K.,
inzh.9 retsenzent; KESAREV, A.P., inzh., retsenzent;
KISELEVA, II.P., inzh., red.; GRVXOV, S.A., kand. tekhn.
nauk$ red.; SHCHERBACHEVICH, G.S., inzh., red.; USENKO, L.A.,
taklm. red.
(Shunting diesel locomotives)Manevrovye teplovozy. Moskva,
1962. 383 P. WMA 15:6)
(Diesel locomotives)