SCIENTIFIC ABSTRACT KOMAROV, N.M. - KOMAROV, N.V.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000824030002-2
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 14, 2000
• Sequence Number: 2
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT


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-'g;9aswW M~- -ff VL
KOMAROV, N.M., prof#; SEMENYUTA, A.T., kand. veter. nauk
Mastitia In the group inethod of machine milking. Vntorinarl!-a
'-P
41 no.7:74-76 J1 t64.. (M-A 18sll)
1. Vsesoyuznyy institut eksperimentallnoy veterinarii.

XCRMOVO X.M.j BORSHOM, M.S,
Hygiene as a basis for the prophylaxis of anivAl diseases
and for increasing their productivity. Veterinariia 42, not71
96 J1 165, (MIRA 18:9)

L ~4-!95466 tiimy-
-All-C 14R; A?0017294 SOURCE CODE.
"~'R,1032.L!r~6.!1)27/r,1031'036010366
i ~j
~`R: Komarov, N. M. Semenyuta, A. T.
'~ 1 imental Veterinary Science Moscow sesoyuznyy
-:-'nion Institute of Exper 0
InSL!LuL an.SperiraeaLal'noy VeLerinarii
-.-L: ~-Ynamics of thermal responses of the organism to the effects
of low
environmental LeWeratures
~SOURCE: Zhurnal obshchey b4ologii, v. 27, no. 3, 1966, 360-366
TOPIC TAGS: animal physiology, thermoregulation, hypothermia,
cardiovascular systemi
!adaptation, climate chamber, pig, mammal
A-3STRACT: Changes in the temperature reaction of mammals during the
early postnatal.
(first 10 days) period were studied in piglets exposed to cyclic low
temperatures
(to -5C and -12C). Piglets were exposed in a climate chamber for 6
hr daily to tem--
peratures of -44C to -5C or -8C to -12C (relative himidity, 85% to
901). Controls
w-ere separated from the mother but kept at room temperature (12C to
18C). A pattern
was observed in the behavior of the newborn piglets as the
temperature dropped: the
animals at first lay quietly (at temperatures above 5C), then became
restless and
active for 2 to 3 hr (5C to OC), then lay quietly once more (even as
the temperature
droppei to -5C). The controls, kept at room temperature, lay quietly
throughout. As
the piglets grew older (2 to 3 days) this pattern persisted; but the
restless phase

L 1919346
_ASQJ4R,_,
AP6017294
began at a lower 'temperature -and. waIsbriefer (10 to 15 min)
16 ~4__ -to
JI-day-old piglets, restlessness did not appear at -2C to -3C;
at -4C to -5-C the-~ _mlere4
Y
J*attempted to crawl beneath one another. After the fifth day
the restlessness dis--
appeared entirely at temperatures to -5C. The animals cooled to
-12C were extremely_
restless throughout the experiment, and did not lie quietly at
any time. A patter -a
was likewise observed in the behavior of skin and body
temperatures, which rose
sharply, leveled off, then dropped. As the animils became
conditioned to the cold
stimulus, the adaptive drop in skin and body temperatures became
greater and occurred
I more readily. It is concluded that in the early postnatal
period, vascular thermo-
regulatory responses-to cold stimulus are reflexive in nature.
With repeated exposure
to this stimulus the vascular reaction takes on specific
features, i.e., becomes
conditioned. This means that training of the body's
thermoreceptors and the physiolo-
gic.i. merhanisms for analysis and synthesis of *the thermal
environment by systematic
exposure to a wide range of cold stimuli is essential to the
development of a better
7~~:Iex res7an~~e to ther-mal stress and ar. adequate adaptive
capacity. The organic
CE6~jnse to cold of animals not so trained is inferior in many
ways (overreaction of
rez,_i~atorv systems, poor blood distribution during stress,
impaired fluid balance in
major organsl, which may,.go, far Lo-'explain the connection
between cold stress and in-
creased susceptibility to fispirato-ry_---_an& other
digeasea.,in mammals. ELS1
06/ SUBM DATE, i5jul64/ ORIG REF : Ollf ATD PRESS: 40,;
Cara

KC-MAFOV, N. N.-
Moscow State U imeni If. T. lomonosov
KOMARDVI N. N.- "The problem of the method of studying the
ionization state of the.-
ground layer of air." Moscow State U imeni M. V. Lomonosov. Physics
Faculty.
Moscow, 1956.
(Dissertation forAhe Degree of Candidate of Physicomathematical
Science)
SO: Knizhnaya Letopial No. 13, 1956.*

109-3-2-2/26
AUTHORS: Braude, S.Ya., Komarov, N.N. and Ostrovskiy, I.Ye.
TITLE: On the Statistic Hature of the Scattering of Centimetre
0
Radio Waves by a Rough Sea Surface (0 statisticheskom
kharaktere rasseyaniya santimetrovykh radiovoln vzvolno-
vannoy poverkhnostlyu morya)
PERIODICAL: Radiotekhnika i Elektronika, 1958, Vol.III, No.2
pp. 1?2 - 1?9 (USSR3.
~her
ABSTRACT: The problem can be - analysee~/by So lvins the Maxnell
equations for a statistically non-uniform medium (Refs. 3, 4
and 5) or by assuming that the received signal is statistical
(Refs. 6 and 7). The second approach is easier and it is
adopted in this work. For the purpose of analysis, it is
assumed that the propagation path is comparatively short so
that the main cause of the amplitude fluctuation of the
received signal is the scattering of the waves from the rough
surface. The field intensity at the receiver is due
to the super-position of a "direct" wave v,,hichpropagates
directly from the transmitter to the receiver, a reflected
wave and a number of waves scattered by the seai The field,
is 'expressed by:.
Cardl/5 E(t) = Eocos Wot + EoT-_p cos(wot + (p) + ZESCOS(Wst + ~Ps)
(1)

109-3-2-2/26
On the Statistic Nature of the Scattering of Centimetre Radio
Waves
by a Rough.Sea Surface
where B cosw t is the direct wave, E cos(W t + T) is the
0 0 oTp 0
reflected wave and ZES cos(Ws t + (Ps) is the sum of the
scattered waves; these waves have random wkplitudes B s and
phases w st + ~0S which are distributed ovcr an iaterval
0 to 2--j. It is assumed that the amplitude distribution for
F-( I0 can be expressed by Bq.(3), where Io W is the
modified BBssel function of the zero,order. The average square
deviation and the average deviation of the amplitude-are
expressed by Bqs, (6) , where - 0 is given by DO-- (5)-'and -
IJW
is the modified Bassel function of the first order. The ratio
of the average square value of the ar-plitude and its mean
value is expressed by Eq.(6a). The rouShness of the sea surface
is defined by: -g2
(X Z2s
Card2/5 Bo

109-3-2-2/26
On the Statistic Nature of the Scattering of Centiretre Radio
Tilaves
by a Rough Sea Surface
so that it can be expressed by:
M2 . 1 2 (8)
T 1 +
0
The maSnitude of the reflected wave can be determined by
finding an expression for f (see Eq.(4)). The phase distri-
bution of EM is in the form of Eq.(12); it is impossible,
however, to find the square deviation of the phase directly
from this expres-sion and therefore the dependence
of the phase deviation on 0 is expressea indirectly bI-j
Eq.(15). The scattered waves undergoa frequency shift Qs
which is due to the Doppler effect and is caused by the regular
and random motion of the sea surface. Ascuming that the
regular motion has a velocity v= and the random motion has
velocities vs 9. is ex.-)ressed by:
4-m- (v= vs)
Card3/5 Qs "Os (16)

109-3-2-2/26
On the Statistic iiature of the Scattering of Centimetre Radio
Waves
by a Rough,Sea Surface
where
4AIv= 4rvs
X and 90S = - X- (l?).
It is shown that the two velocities can be determined from
the Eqs.(19) and (2?). On the other hand the low-frequency
spectrum of the fluctuation envel2pe F(~3 is expressed by
Eq,~38), wher, to and 2a are given by Bqs.(36) and
(3 is, Dirac function. A curve of F(J)
, while 64)
calculated from Eq.(l) for 0 = 3, X = 3 cm v0 = 10 cm/sec.
and v= 0 is given in Fig.l. The theory was checked by
some measurements which were carried out at a wavelength of
3.2 cm; the height of the transmitter was 6 m, while the
heights of the receivers were 1, ?.5 and 16 m; the propagation
path was 750 m. The amplitude fluctuationsas a function of
timed were recorded and these are shown in Fig.2; the values
of the amplitude of the received signal, as a function of the
height of the receiver, are shown in Fig-3. Fig. 4 shows the
Caicd4/5 overall probability of the amplitude distribution 1(y)
;

109-3-2-2/26
On the Statistic Aure of the Scattering of Centimetre Radio
Waves
bY a Rough Sea Surface
the circles denote the values obtained from the measurements,
while the curve illustrates the calculated results. Fig.5
shows the sea roughness coefficient c4 as a function of
h0eA where h 0 is the average height of the surface non-
uniformities, 0 is the sliding angle and X is the wave-
length. From the above I it is concluded that the method of
investigation adopted in this paper is suitable for deter-
ining a number of important physical parameters (0, a$ (Ps
vo) V= and F(j) ) which characterise the scattering
processes. The method can also be used to study the propa-
gation of radio waves in the troposphere and, in particular,
the nature of the non-uniformities causing the tropospheric
scattering. There are 5 figures and 9 references, 6 of which
are Russian and 3 English.
ASSOCIATION: Institute of Radj6pbyajqs. and Electronica-AS of
the
Ukrainian SSR, Khar1kov (Institut radiofiziki i
elektroniki AN USSR, g. Khar1kov)
SUBMITTED: January 18, 195?
AVAILABLE: Library of Congress
Card 5/5 1. Radio waves-Scattering 2. Oceans-Turbulence-Effects
3. Mathematical analysis

AUTHORS: javang, L. R. an Id Komarov, N..N. SOV/49-59-8-9/27
TITLE: Investigation of the Spect;Z '~Simple Ions in the
Free Atmosphere
PERIODICAL: Izvestiya Akademii nauk SSSR, Seriya geofizicheskaya,
1959, Nr 8, pp 1167-1176 (USSR)
ABSTRACT: The results are given of a method of measurement of
the spectrum of simple ions in the free atmosphere. The
measurements were carried out from an aircraft flying,at
heights of 100 to 5000 m. Simultaneously the electric
field, the air temperature and the atmospheric pressure
were determined. The apparatus employed is shown in
Fig 1, where 1 and 3 - high voltage electrodes,
2 and 4 - collectors, 5 - shell; the amplifiers and an
oscillograph are shown on the right-hand side, The
position of the apparatus on the aircraft is shown in
Fig 2. The concentration of ions, N4 the.mean mobility
; and the polar air conductivity X-1 were calculated
from the formulaeon pp 1170-1171- The results are
plotted in the graphs 3 to 8 which represent the following:
Fig_,-3a-An&b_a-nd Fig 4 -.mean spectra of simple ions on
Card 1/2 br:L_gtii_-- days, *all days and at heights of 500 to 4500
M,
respectively;

SOV/49-59-8-9/27
Investigation of the Spectrum of Simple Ions in the Free Atmosphere
Fig 5 variation of ion spectrum characteristics in
relation to height;
Fig 6 - mean mobility w in relation to height
(thin lines - experimental data, thick lines - theoretical
data);
Fig 7 - relationship between ~ and N during climb (a),
descent (b);
Fig 8 - spectrum characteristics on cloudy (dashed lines)
and cloudless (continuous lines) days.
There are 8 figures and 12 references, 7 of which are
Soviet, 1 German and 4 English.
ASSOCIATION: Akademiya nauk SSSR Institut prikladnoy geofiziki
(Institute of Applied Geophysics, Ac.Sc., USSR)
SUBMITTED: October 28, 1958
Card 2/2

90)
AUTHORS
TITLE:
PERIODICAL:
ABSTRACT:
Card 1/4
BOV/142-2-1-13/22
Braude, S.Ya., and Komarovp N.N.
Gener'alized.Cu'rves_~f ~the -Fres~nel R~eflection.Coef-
ficients for Horizontal and Vertical Polarizations
(Obobshchenyye krivyye koeffitaiwntov otrazheniya
Frenelya dlya gorizontallnoy i vertikallnoy poly-
arizatsiy),,
Izvestiya vysshikh uchebnykh zavedenly radiotekh-
nika, 1959, Vol 29 Nr 1, pp 100-106 (USSR)
For calculating some wave propagation problems it
will be necessary to determine,the Fresnel reflec-
tion coefficient f for the horizontal and f for
the vertical-polar)Llzation. This is done by Vknown
f orjraulae ZR-ef I V.. However, dptermining the modu-
and the phaseo-f the Fresnel coefficients from
these formulae is verytime-consuming, especially
when the permittivity.--is a complex number.. For
this reason various graphs have been produced which
are used for engineering calculations, but they are
not applicable in all cases. G.P. Ohman, IRE ZRef.5

SOV1142-2-1-13122,
Generalized Curve 8 0f the Fresnel Reflection Coefficients for
HorizoAtal and Vertical Polarizations
Ph 1 2 q inI FV I - 2
1+ 1+, sin
whereb .y is the angle of slide. Assuming that
0, + ic~ they deterinine C and C and pre-
2 - 1 2
sent the following formulae for 6alculating the
modulus F -1P; and the phase'":
4(C -1) 2 2
C 3 C = 1 + 20 otg'4 I-C
4 .2' 3 3 4 4
There are 6 graphs and 3 references, 1 of which in
American and 2 SovIet.
Card 3/4

s/o4g/60/000/02/014/022

E131/E459
AUTHOR:
Koma N.
TITLE:
Problems in
Calculating the Unstable Currents in

Measuring Condensers otihon
Counters and I_on

Spectrometers
PERIODICAL:
Izvestiya Akademii nauk
SSSR, Seriya geofizicheskaya,

196o, Nr 2, Pp 309-317 (USSR)
ABSTRACT:
The calculation of unstable currents in suction

condensers is
described. Formulae are given for

calculation of the ohmic and
saturation currents. The

parameters are introduced which determine
the various

types of inertia condensers. The measuring condenser

of
the ion counter, through which the air containing

ions is sucked, is
calculated where the air input W is

taken into account. Fig I
illustrates such a condenser,

where the regions 1, II-and III are
described by the

coordinates 0