SCIENTIFIC ABSTRACT KONSTANTINOV, A.I. - KONSTANTINOV, A.R.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000824410005-7
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: December 30, 2016
• Document Release Date: June 19, 2000
• Sequence Number: 5
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

2088h
2.
S/033/61/038/002/008/011
9032/E414
AUTHOR: Konstantinov, A.I.
TITLE: An Investigation of the Molecular Frequency Generator
of the KharOkov State Institute for Measures and
Measuring Instruments (KhGIMIP) and its Use in the Time-
and Frequency Service
PERIODICALs Antronomicheakiy zhurnal, 1961, Vol.38, No.2,
pp-361-372
TEXT: The maser developed by A.Ya.Leykin (Ref.1) has been in
continuous operation at the above Institute since March 1958.
The maser employs an ammonia beam and its frequency stability in of
the order of + 3 x 10-10 (relative root mean square error). This
figure was estimated by A.Ya.Leykin in Ref.l. Since April 1959,
the Khar1kov molecular generator has been continuously compared
with four quartz generators KXI (KKhl), KX2 (KKh2), KX3 (KKh3)
and KX4 (KKh4) which in turn are compared with each other by the
method of beats using a quartz resonator at 60 kc/s. These
comparisons have lead to four series of corrections to KKh3
relative to the maser. The first series was obtained by direct
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20"4
3/033/61/038/oWoO/oli
An Investigation of ... B032/9414
comparisons of KKh3 with the maser while the three other series
were obtained from comparison of KKh3 with KKhl, KKh2 and KKh4
which in turn were compared with the maser. Assuming that the
difference in the corrections in largely due to a nonlinear
variation in the frequency of the generators and the latter can be
characterized by a root mean square variation in the diurnal tate
of 'the clocks, it was found that the relation between the error in
the correction relative to the maser and the root mean square
variation in the clock rate is
A f - + a /t '-t 0
The root mean square variations in the diurnal rate for the
clocks KKhl, KKh2, KKh3 and KKh4 during the period under
investigation (March 1958 - March 1959) were found to be
A: f + 2 V"T --To
Thin result is in agreement with the results reported by J.P.Blaser
in Ref.2. In order to investigate the frequency stability of the
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10884
S/033/61/038/002/008/011
An Investigation of ... Z032/E414
above maser,.a determination was made of its frequency between
.-.I March 1958 and March 1960 relative to the.standard time corrected
for seasonal changes in the-rotation of the earth (TU2). The
maser frequency was also determined"rglative to the cesium
frequency standard-s at'Washington and London. The frequency of
the molecular generator was calculated from the formulae
Fm =,FO
g) 86 4W (2)
(UW1+1& U1),
and.was chicked with the formulae
(4)
FO + AF.
F
F
0,
/0 T9 _4W'
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S/033/61/038/002/008/011
An Investigation of-. E032/E414
'.where PD1 is the frequency -of the maser averaged over 15 days,
Fo is the approximate value-ofthe maser frequene used to
;.Calculate'the frequency of the quartz generator f in Eq.W,
9M,'i~ the'diurnal rate of the quartz clock relative to the maser i
as c
alculated from Eq.,U) to (3) and averaged over 15 days,'
is the diurnal rat of the quartz clock relative to TU2 and
I averaged over 13 dayst fm~ais the frequenc)~ of the quartz-gonern
!,-.relative to the molecular generator whose average frequency over
1A days is taken to be FO. Fi-g.2 xhows a plot of FM and
g - g As a function of time. Table 2 gives the values of the
--frequency of the abovo.ma,--er and the accuracy with which it was
determined,' It is conciudod that the possible change in the
frequency of-the molecular Stne'rator'Vetween 1958 and 1959 was
0.021=/M.or,one part and 107. The use of the molecular t'
'generator at the above Institute will'. *nsur the determination
n 01 and the reproducti:
-frequency to an accuracy of one part d I n
of the time scale can be.achieved with the same accuracy. There
are .3 figures, 3 tables and 2 references: I Soviet and I non-Soviet.
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y

.0/-189/62/000/058/001/002
AOO1/AIOI
AUTHOR: Kons tAnav,,_ A I
TITLE- The astronomical system of time reckoning
SOURCE: USSR. Komitet standartov, mer i izmeriiellnykh priborov. Trudy
institutov Komiteta, no..58 (118). 1962,.Issledovaniya v oblasti
izmereniy vremeni, 4 - 38
TEXV: The author describes the development of ideas of time, in particu-
lar Newtonian absolute uniform time, and emphasizes that there is no time flow-
ing by itself: real is not time in general, but time inseparably related to mo-
tions and changes. The astronomical system of time 'reckoning is based on Earthts
rotation assumed to be proceeding at a constaAt angular speed. Definitions of
true solar and sidereal day, as units of astronomical time reckoning, are given,
as well as expressions for corresponding hour angles which determine local true
solar and local true sidereal time. Since both of them are not linear functiona
of t, Newtonian time, a necessIty arises of introducing fictitious points whose
motions relative to absolute time are uniform; therefoxe concepts are introduced
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S/589/62/000/058/001/002
The astronomical system of time reckoning A001/A101
and explained of the mean point of vernal equinox, first mean Sun and second
mean Sun. Expressions for mean hour angles and their relations to true hour
angles are given, and the notion of equation of time, E, as a correction term
in the conversion from one system to the other, is described. It Is pointed out:,
that the expression of E contains a quadratic term which leads to continuously i
increasing discrepancy between the values of mean time as determined from ob-
servationssof the Sun and from sidereal time; by the 8present this discrepancy
attained 0.005 and by year 2,000 it will amount to 0.02. The next problem dealt
with is non-uniformity of the Earth's rotation, its discovery and a brief his-
torical account of observations of the Moon, Sun and planets, supporting this
concept. Lunar theories are mentioned including the latest theory of the Moon
by Brown who introduced tile Great Empirical Term describing periodical fluctua-
tions in the Moon longitude. The fluctuations are *ascribed entirely to non-uni-
formity of the Earth's rotation. Their values, starting from 1681, determined
by various authors are presented in three tables. Next, the concept of ephemeris
time is explained and defined in terms of universal time and an empirical cor-
rection term taking into account the non-uniformity of Earthts rotation. Recom-
mendations of the International Conference in Paris 1950, approved by the 8th
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KONSTANTINOV, A.I.
Using the XhGIKP molecular-generator for determing actual
frequencies of the quartz o9c13:1ator In the time and frequency
service. Trudy inst.tom.stand., ner I izm.prib. no.59:94-98
162. - (KMA 16 il)
(Frequency measurement)

L 19339-63 EPA(b)/EWT(1)/FCC(W)/FS(V)-2/BDS/ES(V)' AFFTC/ESD-3/
.~PGC Pd-4/Pe-4/Pg-4/Po._4/Pq-4 Gw_...
ACCEESSION XR- AR3002036 S/0269/63/000/00310012/0012.
SOURCE: RZh. Astronomiya. Otdel1W vypu~_
Kwittan ov, A. 1.
AOR in
TIM:.' An astronomical sys for computing time\:
CITZ D SOURCE -Trudy institutov Komitota standartov.
i pri Sovet Xinist~ov SSSR,' _~8(1181-19_6Z,_4-
-38
TOPIC TAGS: astronomical time, polar motion, ephemeris time
TRAUNSIATIO."T.- 7he *author discusses the principles ,:_iderlying an astronomical
system for corTuting time, the motion of tlie Doles, irregularity in the earth a
f
:rotation, and ephemeris time. He gives a brief survey of studies of the R(jtJ&r;N/
of the moon, sun and planets.
DAM ACQ: 301-taY63 SUB COM-;- Al ENCL: 00
Card

ACCESSION NR: AT4026434
AUTHOR: Konstantinov, A. 1.
S/2589/62/000/069/0094/0098
Trr!X; Use of the molecular generator of the Xbarlkovskly gosudarstvenny*y Institut
mer I izineritelIny*kh priborov (Khartkov State Institute of Measures and Measuring
Listrumonts) ~QGIMIP) for determining the actual value of the frequency of a Metal
generator In the time and frequency service
SOURCE: USSR. Komitet standartov, mer I izmeritelfny*kh priborov. Trudy*
institutov Komiteta, no. 59(119), 1962. Issledovanlya v oblasti izmereniya chastoty*
(Investigations in the field of frequency measurement), 94-98
TOPIC TAGS: time, standard time, frequency measurement, molecular generator,
crystal generator, quartz generator, astronomical time
ABSTRACT: At the present time, the requirement for constancy in the value of a re-
produced standard frequency for the solution of manF extremely Important problems is
given by a relative error between 1- 10-9 and 1- 10-J 0. However, the possible accuracy
of astronomical time determinations, an used by the modern tima service, is limited In
principle Ito a relative error of 1. 10-8, since the very nature of astronomical time (TU2)
includes inequalities of this order of nuWltude. Astronomiod techniques therefore
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ACCESSION NR; AT4026434
cannot be used to maintain a standard frequency over the course of a year with an error
of not more than 1- 10-9. This article describes the molecular generator constructed by
A. Ya. Deykin of the Kharlkov State Institute of Measures and MoRsuring Instruments
OQGBIEP) and in permanent operation since March 1, 1958. Ite generator has been used
as a time standard in the time broadcasting service since 1959. Every 24-hour period,
the frequency of the Klr,,h3 crYstal clock generator to determined with respeetto the mole-
cular generator. The KXh3 clocks are the working clocks of the KhGIMIP time service.
This made it possible to determine the behavior of the KKh3 clock both within the astro-
nomical time (TU2) system, as well as within the new type of signal transmission system
of Washington and London. In this connection, it was assumed that the second signals of
the KEh3 crystal clocks are in phase with the K1Kh3 resonator frequency, while the second
radio signals of the WWV transmissions (Washington) and MSF transmissions (LOndon)
are in phase with the carrier frequency of these radio stations. as controlled by the
cesium frequency standards at Washington and London. 7he calculations used to deter-
mine the value of the frequency F? of the molecular generator are explained in the
article. On tho average, the roW" mean square error in the determination of the
molecular generator frequency, connected with errors in the recording of radio signia's
in a 1-month Interval, was +2. 10 -9 for 1958 md +1- 10-9 for 1959. Aomeding to formulas-
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ACCESSION NR: AT4026434
given In the text with the mem-monthly values of the frequency of the crystal generator i
i fM and the behavior of thejrystal clocks g, the author derived the values of the frequency
of the XhGD.41P molecular generator for the middle of the month. These are tabulated In
the article and represented graphically in Figure 1 of the Enclosure. On the basis of re-
ducod deviations of the partial values of the molecular generator frequency from the mean
for a two-year period, a computation was made of the mean-square errors of the partial
Values. These errors are given In Table 1 of the Enclosure separately for 1958 and for
1959-1960 in both an absolute measure (in kc) and a relative measure (in 1- 10- ). Since
the method for the determination of the molecular generator frequency includes, as an in-
termediate link, the determination of frequency and of tho behavior of the crystal clocks I
at the standard time and frequency- services of both VNEFTRI In Moscow and the Kbar1kov
State Institute of Me'asures and Measuring Instruments, the conclusion Is valid that it Is
1 possible to determine the frequency value of crystal generators In Moscow and Xbarlkov
with an error of less than 1- 10-9. The article concludes with the following recommenda-
tions: 1) that each year, the frequency of the molecular generator be determined with
respect to TU2 time. The value of the frequency of the molecular generator with respect
to ephemeral time is assumed to be known on the basis of previously made determinations;;
2) that the value of the molecular geperator frequency, determined according to TU2 for
the year elapsed (N-1), serve as a frequency reproduction standard in the current year
(N); 3) that, as the determination of ephemeral time progresses, the constancy 0 0
3/6
1 Card

ACCESSION NR: AT402M4
molecular generator frequency be checked against this time and that, simultaneously, a
correction factor be worked up for the reproduced
_frequency in order to reduce it to a
system of ephemeral time. Orig. art. has.- 5 formul", 2 tables and 1 figure.
ASSOCIATION: Komitet standartov, mer i izmeritellny*kh priborov (Commitiee for
Standards, Measures and Measuring Instruments)
suBmITTED: 0OFeb6O DATE ACQ: 24Apr64 ENCIa 02
SUB CODE: AS NOREFSOV: 000 OTHER: 000

VINNIKOV, YevLeniy I-Ilkhaylovich; 1"ON."If.TTINOV, A.I., nauchn. red.
0
(Measurement are -eproduction of short time intervals]
Izmerenie i wsproizvedenile korotkikh intervalov vrenteni.
Moskva, Standartgiz, 1963. 113. p. (MILLA 17:7)

.'-I; 15029~.65
ACCESSION NR: AP4044434
an elaborate canditione d, res pons e After stabitttation of the.
temporary connection to the location of the feeding spot, the,motar
'
habit rapidl
becomes auto
y matic- - Following a change in the fe.eding
point, a change in the motor stereotype was observed in all the
animals, i.e., gradual extinction of the initial rectLlinear
trajectory of movement and-elaboration of a nev optimal path, The
process of the reshaping of-spatial analysis with the etaborat
ton
of an optimally directed.flight was accelerated as the eoxperiments - -i,
were repeated, Orig, arto., has: 3,figures.

Lentngradskogo gosudaratyannogo, untvarsLteta (Dapartment of PhyaL-v~:
-k
ology of IRS or ervous Aetivtty, Leningrad State Un-versity)

SUBMITTEDi 040at63 ENCL: 00
SUB CODEe. LS AO REF SOVt 009 GTHERs. 008
Card Z/Z.

K61,1.'~TA ll'I'l f, (jV ) A. i .
:.',
Ilifillence Of U10 Oxclusion of v1sual reception on the controlled
behavior of bats. Vest. LGU 19 no.15:72-75 '614.
(MIRA 17:11)

7
ACCESSION 14R AP5010844 VR/0020/65116110041096910991-~
AUTHOR: Kong.t an tinov, A. j*
TITLE-. The effect of partial and full exclusion of the cerebral
cortex on echolocatton abiltty of 4ats
SOURCE. AN SSSR. Doklady, v. 161, no. 4, 1965, 989-991
TOPIC TAGS: echolocatLon,'carabral cortex, auditory analyzer,
depressive agent, trephination, bat
ABSTRACT: The functional value of the cerebral cortex of bats during
echolocation of small obstacles has been studied. Because of morpho-
lo_~ical features of the auditory analyzer, it is suggested that
analysis of high-frequency signals is less connected with the function
of the cortex but depends moce on the size and complexicy of the sub-
corcical auditory centers, ExperLmenti were conducted with common
bats lllecocus auritus- and brown bats Myotts,mystacinus in a chamber
with 'L;kio 'pir~ll'al 'ro,.~s of vertical wires'. `D~PEg' frie5-flight periods,
che number of CLmes the bats flaw through the barriar without touching
t.ne wires was recorded. Trephination was then performed above tho
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L43217-65- -
ACCES910H NR: AP5010944-
temple regions of the cortex# and a control experirt-ent vas conducted
using the same flight periods. Functional exclusion of the cortex
was accomplished by application of potassium chloride (KC1)~ a general
corttcal depressant) to the exposed skull areas of six animals. 1%
I K), was applied~to the Lemple
jLocaL deoressant, y-aminobutyric acid (GAM
areas of six other bats. It was found that GAMK did not noticeably
affect the behavior of the bats nor impair their acoubtical orienLation
in the detection and avoidance of obstacles. Application of KC!, how-
ever, caused complete cessation of motor activity in the first few
minutes. Normally, the test animaLs passed through the wires with a
frequency of 75.6 t 2.6%; after trephination the frequency reached
83 � 1.3%. Statistically reliable differences in this frequency were
observed only in the first five minutes after the application of
KCI (63.4 t 5%). These aifferences were explained in terms of the
coordinate wind movements during flights 1jetwasa.
animals' inability to 1.
two wires, and not by any reductior. in echolocation capability. It
was concluded that temporary exclusion of the cortical section of the
auditory analyzer causes no essential changes in the echolocation
ability of bats for small obstacles. During b7lef total depression
of the cortex, spatial motor orientation is disturbed-
C-rd 2 /3

I . - II. I
, 1. . i I I - I ,i
; I , - - i
I

"The Problem of the Effect of the Protein Level in Fodder Rat-i~.n7 0.1 the
Increase in '.16ijit of Calves Daring the lvleariin~- Sta~,e." Cand Agr Sci, Lcnint;rad
Yeterinary InsL, Lenin,-,rad, 1)53. (RZIiBiol, No 6, 1-11ar
So: Sum. Ho 670, 29 SePt 55 - Survey of Scientific and TecNi.,.cal Dissertatims
Defended at USSH Higher &,ucational Institutions (15)

KONSTOTINOV, A.K.
Phosphorit-ea of the Mezhozernoye section
reg-lon. KLn. syrla nd.10*.33-40 164.
i
in the Selety-Stapnyak
- (MIRA 18:3)

-S TA N -CI
AUTHORS:
TITLE:
2 5 ; 1,_;6
S/198/61/007/003/001/013'
D264/D303
Kil'ohevs kyy, M 0 Konstantynov, A.Kh-p and
Protsenko: O-P . ~~iv
On the theory of longitudirial vibrations of a system of
material Doints connected by springs
238
1961, 233
-
PERIODICAL: Prykladna mekhanika, v- 7, no. 3,
TEXT: The article considers a material system under the action of
non-periodic forces, donsisting of m8:sdes m' (i = ly 2p ... 7~) joi-
i
ned by springs whose constants are c (i 1? 21 ... n 1).
- M
P, (t) M, M, 77ozi... Mn
AKAAAA401A L]WA,...V0VVVVVV*
M
C12
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S/198/61/007/003/001/(:P-3
On the theory of ... D264/D303
From an investigation of the longitudinal vibrations of such ~ eye-
'tem in order to find the frequency whigh-order determinant is ob-
tained. The article proposes a method of solving the resulting equa-
tions. The authors consider the action of.a non-periodic force P
M applied to the mass m The system is considered in two parts:
l'
The system of masses whose indices are < k, k+1, and those whose in-
dices are _>-k+l, k+2. The action of the spring b'etween Mk anI mk+1
is replaced by elastic forces which must be determined. The gene'r~-
lized co-ordinates are the displacements of the masses of the syd.-
tem. Considering the'motion for each system separately, the equa-
tions ~f motion for the system m 2, ... k) are given bLnd
solved. From the known coordinates of the center of inertia of
the system, and by substitution the equation of motion may be wr~~-
ten
Mx, MIXI C3 COS Wit mIA, ((02
+
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p
'S/198/61/007/003/001/013
On the theory of ... D264/0303
E E (0) + (A + Bt) in,
+ D,sina),t
where m It is supposed that at a given instant-of time the
first and last mass of the system experience unit impulses. Then
the initial expressiono ta-e
xW-0
j0
(12)
X(
12)
0 Mk
When the system experiences forces P 1M and Fk(t)p the displace -
17
ment of the points of the system amy be written
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On the theory o-L ... S/i98/61/007/003/001/013*
D264-/1)303
H)
X~I - A, (f02 Pt Qj) sin w, (i - fl) dt, +
(01 m.A2 (0)2)
a-I
39)
I Ft (11) sin o), (I
+ A,% ((02) to dt, + P, (I - 1.) dt, +
0
+ F. (to (t - t~) dt~.-
MA
The general solution is of the form x X(l) (2)
+ x 2v
k). The equationof frequency of the-original system has one
L
zero solution. Using the proposed method, as many zero
solutions
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'S/19 61/007/003/001/013
On the theory of ... D264YD303
are obtained as 'U-',(., num~)er of parts, into which the system is -di--
videdt [Abstractor's note: In the above case two]. There iQ no in-
consistency here, since there is still. one non-zero solution which
has not been evaluated and which enters the analytical expression
of the elastic force P insofar as Pk(t) is a continuous func-
k(t)'
tion possessing P-11 derivatives, it may be written as a Taylor se-
ries for each interval. By this method t)ae unknown function is ob-
tained in the folipwing form:
P-i
F, t) 4Dkk+1 (P
P _P
P-1- I
A2
k+1
+ Ck.k+l n Fk cosp-
Y, - E I (P P (21)
0)2 M.A2 (W,
i-0 0-k+1
Cos (a.1 4- F, t sin
P (P
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S/198/61/007/003/001/013
On the theory of ... D264/D303
I sin P-j-i- I (0,t +P-1-If- Itcosp- 1-i- I W,t
wa p p p
P-i-i tcos P-1-i W't +
p p
2,
P-j-1
+ k Fk p t Cos --- w,,t -
(_2) p (21)
(02
, E M.62
a-I
Cos P j + F~ t sin wat-
p p )(G)a p
P-j--i- I p--j--!- I P-j-i-
sin -- wLt + ---- t cos - wet -
(00 p p
P-i-I P-i-I
I Cos Wat) + +
p p nik+ I
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25106
'61/007/003/001/013'
S/198/
On the theory of ... D264/D303
(2i-2p+ 1)t2
t
Fa +
Mh 2P2
(P
(21)
3 p (2i +1) - 2 (30 + 3i + 1)_ OF;
+ 6p3
P
where F The author states that this method is
k(0) = ~D-ktk+1(0)' k. ,
sufficiently effective for investigat
ing transient processes which
last for a short time interval. In this case the appearance of se-
cular terms In the solution does not,cause any diffic lty. These
u
terms may be avoided if the formulae of, mechanical quadratures are
used to solve the integral equation. If the system consists of a
large quantity o~ basses,. it can be broAn down into several pye-
tems so that the problem becomes *one of solving a system of inte-
gral equations. There are 1 figure and 2 Soviet-bloc references.
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F-1- ---

33712
S/198/62/008/001/005/005
D299/D302
AUTHOR: 49nstantinov, A. Kh. (Kyyiv)
TITLE; Approximate estimate of the influence of radial dis-
placements on the frequency of free oscillations of
a cylindrical shell
PERIODICAL: Prykladna mekhanikag v. 8, no. 1, 1962, 95-98
TEXT: It is shown that neglect of radial displacements in the in-
vestigation of longitudinal oscillations of cylindrical shells may
lead to considerable error in calculating the frequencies. Ray-
leigh's method is used for an approximate estimate of the influence
of radial displacements on the first frequency of the free oscilla-
tions. Only axisymmetrical oscillations are considered. The longi-,
tudinal displacements are denoted by u(x,t) and the radial ones
by w(x,t). The lowest frequency satisfies the relation
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W2 = Pmax
Tmak
(3)

A,pproximate estimate of ...
33712
S/198/62/008/001/005/005
D299/D302
where P is the potential energy and T the kinetic energy, The dis-
placements u and w are approximately expressed by the formulas
u(X't) = u0 (x) coscot; W(x't) = w0(x)cos&t
(4)
where the functions u 0 and w. are determined from a statical cal-
culation of a shell which is subjected to the constant longitudinal
compressive stresses F. After computations, one obtains the ex-
pressions
Pmax A(! + O.1v2 (141,
T B 1 + 3v2)
max 2 (15)
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Approximate estimate of ...
33712
S/19 62/008/001/005/005
D299YD302
where & =7rRF21/Eh and B = mF 212/6E2h2 (R being the radius of the
middle surface, h the thickness and I the length of the shell).
With v = 0.3, one obtains from (3), (14) and (15) the formula
2 1,,01A
0 *
B(I + /1 2-71
(16)
If the radial displacement is not taken into account, one obtains
ZY 2 = 0,21A
0,82B
(17)
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Approximate estimate of
33712
3/198/62/008/001/005/005
D299/D302
Transforming formulas (16) and (17) to dimensionless quantities,
one obt-ains
"k 1,74
1&7+-o 27 (18.)
1 82
.U=
where
E711
6) TE
a a a p
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Approximate estimate of ...
33712
S/198/62/006/001/005/005
D299/D302
- 1* (
being the density). The graphs of the functionso)'(p) and6o ,U)
a e plotted on a figure,, (p = l/R). With small values of/d (i.e.
s1lort shells), the grapes differ considerably; -thus, for/u - 1,
formula (19) yields an 18% higher value for the frequency than for-
mula (18) which makes allowance for the radial displacements. In
the case of long shells (M >2)0 the radial displacements account
for a 5% decrease in the value of the frequency. There are 2 fi-
gures and 4 references: 3 Soviet-bloc and 1 non-Soviet-bloc (a
translation of Rayleigh's "Theory of Sound").
ASSOCIATION: Instytut mekhaniky AN USSR (Institute of Mechanics
AS UkrRSR)
SUBMITTED: June 22, 1961
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~',M_ZV3KY 'N A. ;.KC:.N5rAI%'T I INCV, A. Q. ;MEM I ZCVA N. I. (Kiev)
"Solutions of dynamic boundary value problems of the theory
of shells ensuing from the integrodifferential enuations of motion"
report presented at the 2nd All-Union Congress on Theoretical
and Applied Mechanics, Moscow, 29 Jan - 5 Feb 64.

KILICHEVSKIY, N.A. [Killeheysikyi, M.O.]; KONSTANTINOV, I n. [KOn3t&.n--
tynov, A.Kh.]
Forced vibrations of a thick conic panel in the nonclassical for-
mulation . Dop. AN URSR no.2-.194-197 164. (MIRA 170)
1. Institut mekhaniki AN UkrSSR. 2. Chlon-korrespondent AN UkrSSR
(for Killehevskiy),

KONSTANTIN01p !~.Kt. (Yj.yev)
porel. FrLk).. m6k-h. 3. no.94!1-1-57 16,~. Nrn
2, lutitut nekbaniki AN b1crWHo
.rsion of the systems of equations of classical shell theory. Attention is concen
,ad mainly on solutions of concrete boundary va ue problems. An example is given 0
dynamics of a thick plaft, rectangular in Plan, supported at the corners an smooth

ACC NRs AR6019264
olutely rigid supports, under the effect of a concentrated force variable in time
lied at an arbitrary point and directed along the normal to the mean surface of the
te. Also considered is the analogous problem for a thick conic panel. X=erical
hods are discussed for the solution of systems of integro-differential equations,
particular, methods based an the introduction of focused nuclei and on the method
collocation, allowing the application of high-speed calculating machines. 34 ref-
sees.
CODEz 12
MOM
I Iv.'; k i 1.1, N. A. A. (K j (-v)
ORC: Insticlice 0~
AN UjcrSsjj (Tnstftut meldianflci AN Ijkl:,43sTz)
eji-jF;r,'c irplct of an anisotropLc plate by a pliere
SO"',RCE: Prikladnnya mteldlanika, v. 2, no. 1.1, 1966, 1-11
- "IC, "'Ac
'S. nolia body -Impact, p.1.1te j.j,,jp;jCt, 11111,1t,
t (1111*, t 10 d
Al -)Sj-PAG"': J110 d0flection of an anisotropic thin Til-Ite
of rCcLangtilar planform, I
L C(Igc'~j
SUTTOrtCd 110111~ ill. r-11150d by
i. ~-' (I C' - ~Ijj inotropLc el,l-~,LjC Spilere
tOrl-R."'LlOt.j, .1-,; 1,1CIJ 'I,
I " tile forces due to in tc~~7~-c-L Cory between plate and sphere-'--aii-d
Liw duration a-- tile impact. Tile Partial differential equation taken from S. A.
Ambartsumvin's "Theory of Anisotropic PI,
ltes" ,,rilicl, describes tile tronsverse vibra-
Lioils 01 iin impacLed PlatL is used-as initial one, taking an uaknown concentrate~d'-T,5-;id-
as a result Of tile spli,ir-c-pl.,tte interact-Lon, Tile cqtlation is solved by an operational
iltoLhoej using tile UIPLIce-Carson transform and tile form Of U10 solution proposed y
Nilvier. A "c"017,11 cxi)rc!;sion for the deflection of tIlL plate as a function of
ill"Pact-POint coordinates and time is derived, and a formula
Lear the deflection at
tile cc-nter of the Plate caused by a centril, ct -;S deelucee- The procedure o
aPproximate deZerminaLlon of the interaction ;:orce is indicate(l, and a formula
(containing the velocity, mass, elasticity and time Parameters) for calculating its
Card 1/2

KONSTANTINOV, A.N.
Classification of technical documents. Vent. mash. 38 no.9:
69-70 S ~58. (IGRA 11:10)
(Classification-Ingineering) *

KONWAITINOV.-, Aloksandr,,Nikolayevich; SAMSONOV, Nikolay Aleksandrovich;
Tmqw, Moi soy 'Abrami;;~icfi'; -- IVIMS, Konstantin Yakovlovich;
TRIMOVA, T.D., vedushchiy red.; FAMOTA, I.G., takhn.red.
[Machinery and equipisent of petroleum refinories; design and
construction, Reference bookj Apparsty i oborudovania nefte-
pererabatyvalushchikh savodov; raschat i konstruirovents.
Spravochnais kniga. Moskva. Gos.nsuchno-tekhu,izd-vo neft, I
gorno-toplivnoi lit-ry, 1960, 573 p, (HIRA 13:5)
(Petroleum refineries-2quipment and supplies)

NO OWIl Ln'cltloh; ?"NO, A.P., redaktor; XHITWT, P*Aot
Als)
oft
T r,
h o as y redaktor.
[Kmml on safety measures for conductors of passenger cars]
Pamlatka po tokhnlko besepasnostl proyodniku paseashirskikh va'-
gonov. Isd.2-*e. Kookwa, Gosotranspoxhal-der.isd-vo, 19,56. 50 p.
(Railroads--Safetjr measures) (MLRk 9:6)

KONSTANTINOV, A N SUIHOTSIIY, K.L., SUXAGEMV, T.V., XAMYSHANOV, G.L.
red*; IHVROV, P*Ao, tekhnored,
[Advenced work methods for passenger service personnel] PeredoTye
metody truda paseashirskikh rRbotnikov. Koskra, Gos.trenspe zhel-dor.
lid-vo. 1958. 91 p. (KIM 11:7)
(Rallronds-Burployees)
(Railroads-Nesenger traffic)

YZVDPKIMOV, I.I.; A13XSNYBV, V-D.;. ASHIKEDUN, A.X.; BAYEV, N.V.; BEZARIYAN.
P.A.-,'Bf=OV. Ye.T.; VYZHMMOVSKAYA, N.Y.; GURZTSKIT,
S.A.; EWDOV, I.M.; TISIPOV, Te.P.; ZHUKOV. V.D.; ZILINSKIT, N.G.;
ZCLINIKOV, r.T.: ZOLOTOVA, L.I.; KIVIN, I.N.; KOKAIWITSKIY. Yu.A.;
-&QWt KULICHITZWAYA. A.K.; KAKSIKIRIKO, I.I.; KUMOUT.
A.A.; MOROZOV, I.G.; XMINOV, K.I.; GZMLOVSKIT. Ch.S.; OSTRYAKOV.
X.I.; PANINA. A.A.; PAVLOVSKIT. V.V.; PHRMINOV. A.S.; PERSHIN. B.7.;
PRONIN, S.F.: PSONOT. A.I.: POKROVSKIY. K.I.; RASPOKOKAREV. Te.A.;
SIKIN, I.N.; SELTAROV. Tu.N.; TIBABSUV. A.I.: FARBICROV, Ta.D.;
FIDOROV, G.P.; SELIGIN, Ya.S.; YAKIKOV, I.A.; VERIHA~ G,P,, tekhn,red,
(Labor feats of railway workers; stories about the innovators)
Trudovye podvigi zhelesnodorozhnikov; rasakazy o novatorakh. Moskva,
Gos.transp.zhal-dor.l.zd-vo, 1959. 267 p. IAKIRA 12:9)
(Railroads) (socialist competition)

MNSTANTINOV, A. 11.
Now posters for railroad employees. Pat' i put.khoz. 4 no.9:46 S 160.
(MIRA 13:9)
1. Nachallnik plakatnoy redaktaii Tranesheldorizdata.
(Rod1roads-1hployees)

GEMAM, VasMy Tamillyevich; KUZIIFTSOV, Konstantin Alakneyevich;
LIVSHITS. Ley Zakharovich; FLTAWNOV, Tlndimir Ivanovich;
'XONSTANTINOT, A.P., kand.int.nauk. obehoMy red.; IAZAROV,
~ ?AMIN. P.S., takhn.red.
[Workerm of the Baltic Factor7 in three revolution@] Rabochis-
Beltilt97 v trekh revollutaiiakh. Pod obehebei red. A.P.Konstan-
tinova. Leningrad, Goo.solusnoe izd-vo sudoetroit.pronyuhl..
1959. 146 p. (KMA 12:5)
(Leningrad-bldpbuilding workers)

---
A-- W - --- --
Konstattinov, A. P. (ussR). (Electrical Seismograph). Russian Patent 1058h6,
issued July 31, 1933.
Relates to electrical seismograph consisting of a generator and a resonance body.
Capacity of latter is so arranged that it can be changed by effects of shocks.
I Claim allowed - 1.

KGNSTANTIIII(~V. A. 11.
"Measurement of Light Wind Velocities Under Normal Conditions," No 2, pp 21--30.
(Meteorologiya i Gidrologiya., No 6 Nov/Dec 1947)
Sot U-321% 3 Apr 1953

UM/Geophysics - Forest-Protective Belts 21 Oct, )0
MiC=ocl1=te'
"Influence,of Forest Belts on Wind Structure and
Speed," A. R. Konstantinov, State Hydrol Inst
"Dok Ak Nwjk SSSR" Vol LXXIV, No 6, pp io65-io6q
Action of f orest -protective belts upon wind has shown
y.-otective effectiveness of belts of different vilth,
but equal deg of spacings fl_e., not solid belt, but
belt having openings at intervalJ is practically
equal. Thus, width of belts from standpoint of wind-
protection can be reduced to min; available data isk-
dicatles -this min Is 10 m for most steppe and
172T33
USSR/C.ecphyaics - Fore s t -Prot-ec, tive Belts 91 Oct 50
(Coutd)
forest-st-eppe regions. Independent of width, wind-,
protective belts are effective for deg of openness.
of about 30%. Submitted 10 Aug 50 by Acad A. A.
Grigor'-yev.
.172T33

USSRAbteorology - Precipitation Aug 52
"Problem of Influencing Atmosyberic Precipita-
tions by a System of Wasures of Control-ling
Nature," A. R. Konstantinov, Cand Phys-Math
Scip Leningrad State Hydrol Inst
"bbteorol i Gidrol" No 8, PP 7-19
Zffect of wooded belts on humidity and yptnsi
previously discussed by G. P. Kalinin (Cf.
"Wteorol i Gidrol" No 1, 1950) and others, is,.',
confirmed by the author. During the sumer,
i.e., the most important aRricultural season,
229TIM
'4W-.,1addn1.70$ of-pptrA rAq.-g6.-jjLt*d, thus produc.-
'Inj high and stabilized crops, he'statis.
0
M
El'
229T102

KONSTANTINOVt.A. R-
A 245T85
UM/atemloa - TtwbuUnt NIzing Nov 52
"Structural Wthods for Calculating Coefficient
of Turbulent Mixing," A. R. Konstantinov and
A. F. Marenkova,, Candidates of Physicomath Sci,
Leningrad State Inst of Hydrology
"Meteorol i Gidrol" No 11., PP 30-33
Discuss the turbulent structure of wind and the
accuracy of various methods in calculating the
coefficient of turbulent exchange.
245T85

1. XONSTANTINOt, A-.
2. MSR (600)
4. Noteorologyp Agricultural
7, Change of climate in relation to tho plan for the transformation of natun in
the and regions of the U.S.S.R. Kh, P. Pogoayan. Reviewed by A. R. Konstantinov,
ed. Izv. Vues. geog. obehah. 84p go. 5p 1952.
9. Monthly List of Russian Accessions, Library of Congress, 2T&ntLqsz 1953. Unclassified.

XONSTANTINOW.A.R.. kandidat fisiko-matematiche2kikh muir
". .. I
Adjustment for vertical gradient of the temperature In comput-
ing the turbulent heat exchange of the underlying surface of the
atmosphere. MeteorA g1drol. no.1:32-35 Ja '53. (KUU 8:9)
1. Goendaretvannyy g1drologicheskly Institut, Iftningrad
(Atmospheric temperature)

KON3TANTINOV, A. R.; STRUZER, L. R.
Windbreaks, Shelterbelts, Etc.
Effect of the size and shape of fields bounded by shelterbelts on yield of
agricultural crops, Les. i step' 5, No. 2, 1953.
9. Monthly List 2f Russian Accessions, Library of Congress, June -1953, Uncl.

.-T T
71 ro-neou,3 scht-no oC Tur",ul ~It "1-:4 "'c"o-Orol. i ~Irid--010
p
criticj~-!;-l of H. I. Budyka's proposeci sche"aa for Co.:lplztin!~ thc cricf-f]-ciont of tur-
bulent in the atmosr)l,.ere. It is shomi thLt LIW' ccntracts
elcrio-itary :)Ilysical corcapts. Tile pvescn,Le~ cam-tricon of tho vr,;lu,,;L; of Lii~, Coefficient
of turbulent coillnuted ,.cc-ordiinc to the L'adyk-0 scliaic an,' -Lo ez:rcrint~,n-
tal f0 of cva:--~ratlon fro.a resorvoirs. stci,,:*- -r,.-
-it. Tho z:,rriv,3 o
crabl,-; ",iv("v;-c1c(.- cl-,-Jnnitation and cxv:lwim~;i
that t'10 0' comrutAinn. of thu coofficienL ,f L111-hul,en".
out 1) Ludyka 1.3 rrA Imt ahx) in -r ~:rcc-
!o 6,
Mct-IL d~.ta of c-.z-ic;rjjnc-ntki1 obrorvatlanz:. H
9 1bv 55

KONSTANTINOY',A.R.
Vertical profile of meteorological elements in the earth's
atmospheric layer. Meteor. L gidrol. no.9 :32-34 S-0 '53.
(Atmosphere) (MLHA
surface
8:9)

KONSTAIRIN OV.,A.R.; STRUZn,L.R.
Measurement of the total evaporAtion and transpiration of agrIL
cultural crops by means of evaporimeters. Trudy GO no.45:66-94
'54. (MWA 8: 11)
(Plants-Transpiration) (Evaporntion)

KONSTANTINOV,A.R.
-
Comparison of different methods for determining evaporation. Trudy
GGI no.45:95-120 054. (MLRA 8:11)
(lvaporntion)

14-57-6-12065
Translation from: Referativn zhurnal, Geografiya, 1957, Nr 6,
P 57 (USSRT y
AUTHORS: Fedorova, T. G. Konstantinov A R
TITLE: An Experiment on the Use of a Floating Evaporator
(Opyt ekspluatatsii plavuchey isparitellnoy ustanovki)
PERIODICAL: Tr. Gos. gidrol. in-ta, 1954, Nr 45, pp 182-195
ABSTRACT: This paper describes the experiments on a floating
evaporator (FE) built by S. S. Ginko, and the results
of observations made on it in 1952 and 1953. FE was
placed in use in May, 1952, on Lake Valday, which is
21 km2 in area, and 25 m deep in the place where FE
was installed. FE was mounted on a raft which turned
in such a way that the apparatus held a constant po-
sition in respect to the wind. The raft was provided
with spray guards which were effective in waves up to
Card 113 1 m. high; even with a greater wave height, only the
14-57-6-12065
An Experiment On the Use of a Floating Evaporator (Cont.)
ar the edge could be sprinkled by the sprayo No
evaporators ne~ to splash out of them. FE contained apparatus for
water was seen wind speed variations, air temperatureq
measuring evaporation (E) iake surface and at various depths$ and -
ure at the ere in the form of
water temperat All the evaporators w ;Jon was measuzed
atmospheric humidity. . 4th flat bottoms- Precipitat elements
ylindrical containers W variations Of other meteorological ient
(0.05 m2); means of a grad
by rain gauges 2 M. were determined by
eights Of 0.21 1 and re were measured by large suction
at h iperatures and moist" anemometers water temper-
by manual
pole; air ten wind velocities) and at depths
psychrometers;, Of 0.01 m by floating thermometers, Evaporation
thermometers. d
ature to depth 15, 20, and 25 m, by depth lements were Atudie
of 1' 3' 5, 10, and 7 pm. All other e Diselts of the.
was observed at 7 am L60192-1 pm_and.7 Ves- ake's
four tl**B 4 as V 4.ift P 'T IOlute humidity above the 1
stablished that abs average wind velocity at
observations e higher, and that
surface was four percent s high as the values obtained at
the elevation of 2 m was twice a
Card 2/3

K0fiSTANTJWA.R.;PUSHKAM.V.F.
. - -mm-wvi.~-4tq
Characteristics of conditions of evaporation and transpiration
from agricultural fields in a zone of excess humidification.
Trady GGI no,46:146-192 054. (KLRA 8:11)
(1vaporation) (Plants--Transpiration)

KONSTANTINOT, A.R.; PUSHKARST, T.F.; SAMOKHINA, K.P.
Characteristics of evaporation regime in agricultural fields in reclaimed
Virgin and'vasto lands. Trudy GGI no.48:5-21 '55. (KM 9:7)
Olvaporation)

KONSTANTINOY A,R,
.: ~-Z -;-
:~A . ~
~4_- ~
rr1nc1ples of methods of computing evaporation In natural conditions.
Trudy GGI no.48t22-37 '559 (MMA 9:7)
(Draperation)

1, Geografiya) 1957, Nr 1,
Translation from: ReferativnnY Zhurna
pp. 56-57 (USSR)
AUTHOR#. Konstantinol t A. R. CalculAting Evaporation According
TITLE:
Basis f Or 9, 14ethod Of
labl. to Metebrological stations
to theData Avai, dannym
(OboBnOvanlye mstodiki rascheta, ispareniya Po
meteorologicheskikh st&ntsiy)
5-74
(io8),
PERIODICAL:
ABSTRACT:
Card 1/4
pp.
1956, Nr 54
Tr. 005. g1drol. in-tat
,g metereological station network does
Since the exi8til ions, the problem ar:L8e8 Of
not make gradient obeervat teo-elements at two
adapting a,p3Ay% Or nai.culation of me network.
to the observations conducted by this liary data
heights apt&tIon would take into account auxi ce and the
This ad ghness of the underlying surfa I-
such as tile rou leal connection between the metereolog
objective., emPir network stations. The calcu-
cal data submitted by the Ing to gradient
lation of turbulent currents accord
14-1-513
Bdsis for a Method of Calculating Evaporation According to the Data
Available to Meteorological Stations
measurements (Tr. Goa. gidrolog. in-ta, 1955, Nr- 45)
is the basis of the method worked out by the author.
Correlations were established in measuring the tempera-
ture of similar surfaces which made It possible to de-
teruine the value of temperature and.humidity at the
level of the layer of roughness (the height at which the
wind velocity Is reduced to 0 Is taken as the lower
level of the measurements : To'-'T200 - mT (Tn - T200);
e0 - e200 m me (elk where Tog eo and T2000 0200
stand respectively for the temperature and absolute
humidity at the level of the layer of i!oughness'ahd at
the 2 motor level and ZIT and Me are the empirical co-
efficients, determined by given gradient measufroments,
depending on the parameter of roughness ( z 0 ) an d Jh*
type of stratification. Introducing the zo value-(AI)
(Ki - Richardson's number) make's it possible to exclude
the dependence on stratification Of mT and me. The
values zog ZAT and me were determined on the basis of
gradient measurements, for water, snow and soil surfaces.
The wind, temperature and humidity cdntours above these
Card 2/4 surfaces were drawn according to their values. The rise

ZMD.LD LVI- C16 PAWWAV~A VA.
Available to Meteorological Stations
compiled to determine the actual difference betWeen the
temperature of the soil (Tn) and the temperature at a
height of 2 meters., A gradient for absolute humidity
has also been established. These measures will el-
iminate the difficulties noted. Observations made at
1, 7, 1~ anA 19 hours should be used in order to
culate evaporation according to the proposed met,"--_,~d.
They determine the average intensity of evaporall.ion,for
each period and then for the 24-hour period. Mie amoitat
of evaporation for a period under calculation is obtained
by multiplying thes6,quantities by the time. This
method of calculation was chocked by observations made
by the Valday.SQLentific Research Hydrologleal Labora-
tory. The chlick,indicated a satisfactory agreement
of calculated and measured quantities. The author be-
lieves that the method described above could be adapted
to widespread practical use. Bibliography: 43--
references. A. Be
ASSOCIATION: State Hydrological Institute (Goo. gidrol. in-t.)
Card 4/4

KONSTANTINOT, A.B.; MU*CHMO, I.I.
Determination of ovapomtivitr In the Sal Stapp* region, ftw GGI
no.57:73-85 156. (K= 10s6)
(Sal Steppe--lyaporation)

KONSUMMOV, A.R.
:--
ory of eup anemometers and its applicatlon to wind "d
measuz-oments and tothecholes .of beat design for the inotru-
Mont. [Trudyl LO W20 hiborprom. Sekt. gidromet. i geofis
prib, no.1:5-67 '57. (Asenowtor) (GA 11:6)

XONSTANTINOV, A.P.; MOLCHMV. A.L.
-,
latimating changes produced by
and water balance of sells in
Suropean part of the U*S.S.R.
(Forest influences) (Soil moisture)
afforestation in the evaporation
steppe and forest-steppe zones of the
Trudy KazNIGMI no.8:64-93 157.
(MIRA 11:12)

KONSM'TINOVP A. R. 61A KUPRIYANOVO V. V. (Rditom)
lxperlmnftl lnventliption of the ZieumlU of the Water SalawA JA VaIdAy.
2n& GosudafttvvnwS2 gldF?lo4?hssjRV lwtltuta (TrarAaCtIOM of the State
HydrOlWJL"l Imt.) No. 59, 1957, 224pp., 6 artlclss.

~AUTHOR., Konstantinov, A. R. SOVI 50-58-7-15/2o
TITLE: Directions for the Carrying out of Observations of the
Evaporation of the Fields (Rukovodstvo po proizvodstvu nablyu-
deniy nad ispareniyem 9 sellskokhozyaystvennykh poley)
H. Observations of the Evaporation by Means of the Gradient
k6thod (Chast' II. Nablyudeniya nad ispareniyem gradlyentnym
metodom) Gidrometeoizdat. L. 1957
PERIODICAL:.- Meteorologiya i gidrologiya, 1958, Nr 7, PP- 56-59 (USSR)
ABSTRACT: The 2nd part of the "Directions for therarrying out of Ob-
servations of the Evaporation of Fields" published in 1957
deals with the observations of the *vaporation by means of
the gradient method, This is a further development of this
method which had been originally explained in the "Meteoro-
logioal Directions for Hydrometeorological Stations"v 1954,
Nr 5* The calculation scheme by D. L. Laykhtman (Refa 4 and
5) was taken as basic for these directions, as it is far
better founded than that elaborated by the Geophysical Main
Observatory. This scheme lately has been simplified to a
great extent and thus is suited for general use. -'.. It
Card 1/3 is, however, farli-om being perfect. The main error oi the

SOV/ 50-58-7-15/2o
Directions for the Carrying out of Observations of the Evaporation of the
Fields. Il. Observationsr jf the Evaporation by Means of the Gradient Method.
Gidrometeoisdat. L. 1957
calculation method by Laykhtman as well as of other schemes
of the GGO is to be found in the use of the hardly eiact
classical calculation' schemes of the influen&e of the lem-
peraturo stratification'of the atmosphere on the amount of
evaporation. It must be pointed out that the table of the
stability of the parameter E in the "Directions" contains
wrong data. This contradicts the calculation scheme by Laykht-
man as well as the experimental data by D. L. Laykhtman (Ref 5)
T. A. Ogneva (3ef 7) and S. A. Saposhnikova (Ref 8). The nomo-
gram proposed by the "Directions" for the calculation of the
evaporation cannot be regarded as good as it is impossible
to calculate by its use the condensation quantities. They
play, howeverp a decisive role in the humidity exchange between
the surface of the earth and the atmosphere, especially in
arid areas. The only calculation formula is written down in
a wrong way and is only insufficiently corrected in the en-
closed list of misprints. The interrelation between the dis-
placement stratum and the height of the growth of grass sug-
Card 2/3 gested in the "Directional', which is equal to 2/3, is not

800.5
sov/169-59-4-3735
Translation from: Referativnyy zhurnal, Geofizika, 1959, Nr 4, p 8o (USSR)
AUTHOR: Konstantinov A R
_60wiw6ft
TITLE: Three-Bladeetlemograph - a Device for Recording the Horizontal
and the Vertical Componen s of the Wind Velocity In the Layer
of the Atmosphere Near the Earth's Surface
%7V--
PERIODICAL: Tr. Gos. gidrolog. in-ta, 1958, Nr 70, pp 84 - 96
ABSTRACT: A three-bladed anemograph developed by the author for recording
simultaneously the instantaneous values of the horizontal and
the vertical components of the wind velocity is described. A
description of the method of operating the device under field
conditions and the method of processing the results are given.
The device consists of a barrel fastened rigidly to the vertical
pedestal of a usual weather vane, which is directing the hori-
zontal axis of the barrel into a place perpEndicular to the in-
flowing stream. Along the axis of the barrel, two shafts, in-
sulated from each other, are led out; to one of the shafts
Card 1/2 a plate is fastened in a horizontal plane, to the other - a plate

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H sit g
ZO)ISTAIVIIOVO A.R.9 JJUTOVA9 T.V-
Iteppe and forest
Ivaporation from f&rm, fields In the athe R. TrAY
sts"e zones of the Jbiropeftn V"t Of (UM13:6)
GGI no.72:70-10,1 159. (W,,,,t--Water requirements)
(wap.ration)

I[ONSTANTINOT. A.R.: PUMARN, V.P.
Observations on evaporation from the surface of water and moll in
the U.S.S.Re Nek.probLueteore no-1:72-95 160. (KML 13:8)
(31raporation)

XONSTANTIMV. AoR.; PADMTAO T.G.; GOWEIV, V.S.
~- f
I
Effect of different factors on the readings of water avepori-
meters placed In the ground. Trudy GGI no.76:67-111 160.
(MI" 13:6)
(*avoration)

KONSTANTIBDV. A.R.-. JZDDROTA, T.G.
Thermal regime of Lake TaIday and distribution of meterological
elements over its surface. Trudy GGI no-76:112-151 160.
(XR& 13.- 6)
(Valfty region-Mitteoroloff

KONSTANTIMOV, A.R.: GGWMV, V.S.
Possibility of measuring gradients of atmospheri-- temperature
and humidity by the use of station psychrometers Installed in
instrument shelters. T=dY GGI no-76:152-167 160.
(MM 13:6)
(Bygrometry) -

IMSTANTBOV# A.Re; GOLUBVP V*S9; ~OKMV, V.V.
Studying the characteristicis of air currents determining ebangea
in the evaporation from tbel surface of a body of water. Trudy GGI
no.glx65-90 160. (MIRA 3.411)
(Valdai, Lake-4vapoiration)

-r7e
IMSTANTIMOV. A.R.; MXRCVt S.I.
Using gradient =WU to determine evaporation and heat exchange in
forests. Trudy GGI no*81:91-D4 160o (MM 4:-11-
(Valdni Hill&-41etcorology-4bservations)
(Aorest influences)

KONSTANTINOV,-,A.R,------_
Method of deter-iningjaporation from soils, watert .and snow by
air temperature and h dity measuTements made at meteorological
stations. Trudy GGI nOl-81:115-153 160. (MIU 14: 1)
Waporation)
W

XONSTANTINOV, A.R.
Estimating errors of aspiration and station psychrometers in a
thermally inhomogeneous atmosphere. Meteor. I gidrol. no.10:40-45
0 161. (MIRA 14:9)
(Hygrometry)

KOINSTANTINOV., A.R.; VORONTSOV, P.A.
Effect of forest belts on winds and turbulent exchange in
the atmosphere. Trudy UkrNICA-II no.26:99-110 161.
DURA .15.2)
Forest influences)
nds)
t

KONSTANTINOV, A.R.
Critical evaluation of methods and apparatus for experimental
stiidy of the wind structure. Trudy UkrNIMI no.26.-Iii-136
j01, (MIRA 15:2)
(Winds)
(Meteorological instruments)

KONSTA.NTIVOV,, A.R.
Errors of inertial apparatus measuring the temperature
and humidity of the air in a thermally hoterogeneous.atmosphere.
Trudy UkrNIG14I no.26:1o-157 61., ' (KrRA 15:~2)
(Meteorological inBtrumenits)

SbWtAMINOV, A.R.; POPOV, O.V.; PUSHKAREV, V,F.
Evaluating methods of determining evaporation and other components
of the water balance of farm fields. Trudy UkrI4I%II no.30:19o-30
161. (MIRA 15:1)
(Evaporation)
(Metewologyp Agricultural)

KONSTAI]TINOV., A.R.
Notes on the technique of measuring evaporation from WM
fields. T2-udy UkrNIGHI.no.30:31-1+0.161. (Mikk 15:1)
(Evaporation)
(Meteorology, Agricultural)

KONSTANTINOV, A.R.; JUIARCIIENKO, K.I.; B.-IROATOVA, H.R.; BUROV, V.S.
Investigation of evaporation from firm fields. Trudy GGI
no.91:76-109 161. (MIRA 14:8)
(Evaporation)
(Crops and climate) . ,

3
99/62/()00/031/001/006
/5
A066/A126
AUTHOR: Ilon-stantlnov, A-11.
TITLE: The principles of the oemi-empirical theory by Prandtl and K&rmAn
from the standpoint of the str~ioture of turbulent pulsations in a
ground layer of the atmosphere
SOURCE: Kiyev. Ukrainskly nauchno-issledovateltakiy gidrometeorologicho-
skiy institut. Trudy, no. 31, 1962. Voprosy fiziki atmosfery, 3
16
TEXT. A detailed analysis of the most important characteristics of the
turbulence of air-streams, established by the author between 1947 and 1959 by
means of anemographsi, shows that some propositions of Prandtl s and Mrmfints se-
mi-empirical theory are inadequate from the physical point 6f view. It is point-
ed out that the commonly accepted opinion that upward vertical pulsations are
stronger than downward pulsations is wrong. In the case of an isothermal state
and a small vertical equilibrium gradient, downward pulsations are stronger than
upward pulsations$ but at medium and high vertical equilibrium gradients they
Card 1/2
----------

3/599/6P/000/031/OOV006
060126
AMMOR: Konstantinov, A.B.
------------------
TITLE. The influence of temperature stratification on intensity of evaporl-
tion, turbulent heat transfer, and flow of momenW-n
S JPICE. 'Kiyev. Ukrainskiy nauchno-issledovatellskiy gidrometeorologiche-
skiy institut. Trudy, no. 31, 1962. Noprosy fIziki atmo,afery, 17
-35
TEXT: Shortcomings of Prandtl s and KhrmAn's semi-empirical theory are
eliminated by allowing for the influence exerted by the temperature stratifica-
tion of the atmosphere and by the forces.following from the Archimedean princi-
pie on the intensity of vertical turbulent flows of heat, moisture, and momentur'.
A thorough investigation of turbulent heat transfer is greater than the intensity
of heat transfer.caused by the gradient of the mean temperatures. The intensi-
-by the shape of
ties are influenced tho eartfirs curfaac. Bojentu relation is ob-
tained as
P OGT T -T P
0.62 - P (25),
;~e ep e 1033
card 1/2

KONSTANTINOV, Aleksey Rodionovich; STRUZER L.R.,
I otv. red.;
VLASOVA, Yu. V. , ria-.T -A'JONS, Ft. A. ,tekhn. red.; BRAYNINA,
M.I.,, tekhn. red.
[Evoporation in nature] Isparenie v prirode. Leningrad,
Gidrometeorizdat, 1963. 589 p. (MIRA 16:11)
(Evoporation (Meteorology))

KONSTANTINCIV, A.R.
-,
Climatological and hydrological research in the People's Republic
of Poland. Meteor. i gidrol. no.1l.-53-54 N 163. (MIRA 16:11)
1. Ukrainskiy nauchno-isaledovatellskiy gidrometeorologichoskiy
institut.

VITKOVSKIY, B.1,; GOYSA, N.I*; K0ffS=1WV,-A.R.; XUDINA, A.V.;
OLEYNIK, R,N.; SAKALI, L.I.
Meteorol6gical conditions and heat balance of the underlying
surface during the work of the expeditions of the Ukrainian
Scientific Research Hydrometeorological. Institute and the
Main Geophysical Observatory in the su=er of 1960 and 1961.
Trudy UkrNIGRI no.350-17 163. (MIRA 17:1)

KONSTANTINGV, A.R.; SAKALIJ, L.I.
Methods for calculating the turbulent heat exchange of the
soil surface and the atmosphere baoed on air temperature and
humidity measured at meteorological stations. Trudy UkrNIGMI
no-35:18-30 '163. (MIRA 17:1)

KOrSTANTINOV, A.R.; GOYSA, N.I.
Methods for calculating the balance of radiation and effec-
tive radiation based on the temperature and moisture of the
air being measured at meteorological sba'Uons. Trudy
UkrfG'GMI no-35t62-72 163. (MIRA 17- 1)

KODISTANTINOVp I.R.
Methods for calculating the evaporation based on gradient
meaourement data. Trudy UkrNIGMI no,,35:84-108 163.
(MIRA 17:1)

KOI-ISTANTTNOVS A.14; Ar P.11.
Evar-yration from the waste land of the Ukrainian steppes
in ~le summer. Trudy UkrNICR41 no.35:109-115 163,
(MDU 17: 1)

KONSTANTRffj_A*R.; KOINA, A.V.; GLEYNIK, R.N.
Method for taking into account the effect of the sea on
the temperature and moisture of the air above land. Tru
UkrNIGMI no.35t140-152 163. (MIRA 17:1~

ACCESSION NR: AT4018982 S/2599/63/000/036/0003/0013
AUTHOR. Konitentinov, A. R.
TITLE: Vertical prof Iles of meteorological elements In the lowest layer of the
atmosphere and the concept of the displacenent layer
SOURCE: Kiev. Ukr. n.-I. gidrometeor. institut. Trudy*, no. 36, '1963. Vaprosy*
fiziki atmosfery* (Problems in atmospheric physics), 3-13
TOPIC TAGS: meteorology, displacement layer, air temperature, wind velocity.
atmospheric surface layer, atmospheric stratification, meteorological profile,
agricultural meteorology
ABSTRACT: On the basis of an experimental investigation of vertical profiles of
meteorological elements in the surface layer it is demonstrated that the generaliz-
ed logarithmic law is not satisfied under natural conditions. A method is describ-
ed for determination of the height of the displacement layer and experimental data'
are cited on the height of this 'layer over a meadow, grain crops and forest. Be-
cause of the defects in the generalized logarithmic law and the generalized power
law, and since theoretical solution of the problem Is difficult, the author has
developed his own system based on the stabiiity of temperature stratification of-
eth gmosphere. It is noted that particular attention must be given to a study
of

ACCESSION NR: AT4018982
of the difference between the true derivatives of meteorological elements for a
particular temperature stratification and the derivatives c(4nputed by the simple
logarithmic law; a cor7ection factorY Is supplied. Fig. j of the Enclosure shows
various values of this correction factor as a function of stability of stratifica-
tion and height above the earth's surface. Injhe rangeof ordinarily observed
Richardson numbers from 0.2 to -0.3 the value I height of I motor varies
from I I to 0.86, so that it can be assumed that ~ a. I for computations not re-
quiring great accuracy. over a call and.dense grain field an air current rises,
pushed upward by the grain, as-shown In Fig. 2 of the Enclosure. The height of
the layer to whose upper boundary the air current Is raised has been called the
"displacement layer" by certain Soviet meteorologists and is denoted zdi . The
methods for determination atificat?
Of ZdIs at the time of equilibrium str an are
described; the importance of the concept in agricultural meteorology is discussed.1
Formulas are derived for computationcF the gradients of wind velocity, temperatures
and humidity over a tall field of grain in a temperature-nonhomogeneous atmosphere*'
Methods and instruments for field observation of these parameters are described.
Results of a:comparlson of experimental wind velocity data and the values of the
displacement and roughness laye'rs computed from thorn Indicate a considerable de-
pendence of these p;rameters on wind volocity,av shown In Fig. 3 of t.he-Enclosure.
Orig. art. has: 9 ormuiest 5 figures and I Is.
Cgrd 2/6
3/6

ACCESSION NR: AT4018983
S/2599/63/ooo/036/0014/0022
AUTHOR:, Konstantinov, A. R..
TITLE: Investigation of the relationship between the Profiles Of metecrobOCal G1=MW
and characteristics of the underlying surface
SOURCE: Kiev. Ukr. n. -1. g1drometeor. institut. Trudy*, no. 36, 1963. V0PrOsY*
fiziki atmosfery* (Problems in atmospheric physics), 14-22
TOPIC TAGS: meteorology, meteorological profile, air temperature, air humidity, wind
velocity, atmospheric stratification, atmospheric roughness layer
XBSTRACT: Experimental data are presented which characterize the dependence of the
height of the roughness layer over different types of underlying surface on wind velocity
and the stability of atmospheric stratification. The author empirically establishes a uni-
versal relationship between the temperature and humidity of the air directly in contact
with the surface and determines the values of these elements at the upper boundary of the
roughness layer and at a level of 2 meters above the earthts surface. The formula is
given for determination of the height of the roughness layer,, characterized by the rough-
ness Parameter zo. It in demonstrated that by knowing tho value to it is possible to
-determine the values of humiditf 00 when a by extrapolation of
To am I&
Ckwd
ACCESSION NR: AT4018983
the temperature and humidity values from the above
_lying
levels to the upper boundary of
tmheoarsouurgehdnaet"thleayheeri-ghtlaltztr,apolaUo'1 of the values Of temperature and air hum!dity,
09 2 and Z2 2. 0 m to.the leVel a =
cOmPlished using the forujubs: X 9 for sKample,'Is so_
7'0 - T2.0
+ (To.2 - 72.0) Zo
ZO
e0-e2,o+(0o.,-e,,.)jg 200
'AG values To and .0 can be
determined from the known temperature Of the surface and
the temper"uO T2. 0 and air hmldity 62. 0 (at the height 2m) UBiDg the relatiou:
To - T2.o -1nT (7~
t
eq C2.0 - nt. (e. - e...) (2)
Cwd
203

ACCESSION NR: AT4018M
where mTand me are empirical coefficients whose numerical values can be determined,
from gradient measurement data using the formulas:
200 7a. 7r,7. 0
MT Zo r.~3_7 -
2W e0-7 - c2-0 (3)
M.-Ig=
11. 0
In the case of an unstable stratification of the atmosphere there is a decrease of the Pam-
meter z0 (Fitg. I of the Enclosure), leading to an increase in the values To and % and an
increase in the differences To - T2 0 and e0 - eZ 0. I'he values of the roughness para-
meter over soil and snow, comput;a using the IoWMrithmic law, decrease with an increase
in velocity (Fig. 2 of the Enclosure). Profiles of meteorological elements are described
well by the generalized power law only beginning at a height of 60-90 cm; below this leveli
the curvature of the actual profiles of meteorological elements changes sign (Fig. 3 of the
Enclosure). Orig. art. has: 4 formulas, S figures and 2 tables.
ASSOCIATION: Ucrainsidy nauchno-issledovatelliddy gidrometeoralogidwddy Inolitut
(UkraWan Hydrometeorclogical 3dentiflo Research InnUtuts)
Curd 3#

KONSTANTINOV., A.R.
EvaPOmt:LGU MOW from the surface of ponds and reservoirs.
T2vo UkrNIGMI n0.39%7" 263. (MMA 16 3 7)
(ITaperation)