iL. ~., ; L.
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ZJIhTOY PETROV, A.A.; AGINWA, V.A.; UKHANOVI, Y.A.; BOVVA, D.L., red.;
~
~TYUTYAYHY, B.A., red.
1110vgorod Province during forty yearalof the Soviet regimei 1917-1957;
a statistical manual] Novgorodakais oblast' za 40 let 5ovetakoi
vlauti (1917-1957): statisticheskii abornik. [Movgorod] Knizhnain
red. ge2ety "Novgorodsksis pravda,* 1957. 501 P.
(HIRA 11:3)
10 11ov.gorcAskays oblast'. Statisticheakoye upravleniye, 2. Haehall-
nik Novgorodekogo oblastnogo Btatichesticheekogo upravlenlya.(for
Bovva). 3. Novgorodskoye oblastnoye stattatichaskoye upravlantya
.(for Zhatovo Petrov,, Ageyeva, Ukhanova)
i
~ i
.fil I 11,11111fil N 1111
i
.
-, * -- , :L=
,f~ I; -~c r- F lle~
-V ~
Igulikov, 0. A- P-t--i? Pn--14 I - its
fif-"th 'jir-hdll- I- 1 .1
't .
(Differential equations)
SOV/124-57-7-8101
Translation from:, Referativnyy zhurnal. Mekhanika, 1957, Nr 7, p 99 (USSR)
AUTHOR: Zhautykov, 0. A.
I----------------------
TITLE: On a Certain Seepage Problem (Ob odnoy zadache fil'tratsii)
PERIODICAL: Izv. AN KazSSRj- ser. matem. i mckhan., 1956, Nr 4, pp 70-79
ABSTRACT: The author investigateis the plane-radial unsteady-state seepage of a
uniform elastic f luid in.an infinitely extended elastic layer. The flow
toward a well with, radius RC inside. a zone of radius Rk is examined;
the porosity of the layer is designated as m , its permeability is k,
t A the total volumetric. yield of
and- its piezoconductivity coefficien
the.w.ell is assumed as constant. Thc pressure p(r, t) at any point of
the layer is determined. The solution is reduced to the finding of the
solution of the differential equation
~2
'a 1 a 1
0 P OP
Z ar az a t
49 r
sa db 'dary conditions; on
which tisfieg:several initial un
an 0 e o these
Card 1/2 conditions- is the following
- - - --- --- ----
sov/124-58-11-12901
Tr .anslation from: Referativnyy I zh urnal, Mekhanika, 1958, Nr 11, p 148 (USSR)
AUTHOR: Zh'autYk-DM-1_0_A.
TITLE: On the Solution of a Particular Problem of the Theory of Seepage.
(P.
o ovodu resheniya odnoy zadachi teorii fill tratsii)
P
'~PE:RibDICAL-: Iz"v. AN KazSSR, Ser. matem. i mekhan. 1957, N r 6 (10),
pp 46-50
ABSTRACT: -An examination of the problem (Zhautykov, 0. A. , Izv. AN
KazSSR,,Ser. Matem. i mekhan., 1956, Nr 4, pp 70-79; RZhMekh!
1957, Nr.7, abstract 8101) on the pressure distribution in an
elastic stratum following the sudden stoppage of the operation of a
deep-well pump, ass'uming that the continuing flow of the liquid
toward the well results in a dynamic rise of the free surface, 'i. e. ,
the pressureon the.well bottom is increased. The solution of the
heat.-canducti.vity equation
0-p + '_l ap '3P R0
Br r= 12t) r=R
where, -y is a constant and R. is'the radius of the well, is sought in the form of
p(r,, t).=, u(r, t) 'Wherein the, Laplace transform is used, The expression
for. the function U(r, Q is found; however, in the transition to u(r, t),the author does
not.investigate the existence of the roots of the polynomial of the Bessel functions,
that enters as a factor into the denominator of the expression of the Fourier-
M.ell'in inversion formula under the, integral, i.e. , the possible presence of addi-
~tional poles is not investigated. Therefore, the problem as set up does not appear
complete, and the final result thereof appears unsubstantiated.
V. N. Nikolayevskiy
Card Z/z
AUTHORt ZIILUTYKOV, O.A. (Alma-Ata) 39-1-3/8
TITLE: The Generalization of.the Poisson Brackets for Functions of
Enumerably Many Variables (ObobshchenJ~e skobok Puassona dlya
funktsiy schetnogo,mnozhestva peremennykh).
RIODICALi
;957 VOI 43, Nr 1. PP- 29-36 (ussR)
MatMUCUSkly SbM ;Uj 0
ABSTRACTt Let the functions (x,,x2,' ;,z 11'21 and -Y(x lPx2P"
z PZ20 ... be continuous in the domain H: Ix < Rj Jzrj< R
k!
with respeot to the metric
(k,r _,14' 22")'
1
_z and
X1
_'V ....
x .;z OZ jz
`1 "
P ~1'
,
'
1
j
1
1 2 1 2
uniformly bounded, They are assumed to possess continuous,
uniformly bounded partial derivatives of first order and satis-
fy the.conditione
J(x zjz ZI ZI
VX21#0*1 ~m-llxmll x1+19-1..; 1 2"**Izm-l' ml m +
f(xlrx .*.Ix IjX11 z1f0z1f ...
11`1 zlyz2f ... lzm-If m MW
V M-11x~
m+
E a Z; etc. f or %p, where &z sup xf X11
M
I t ze - z1f
I m m
M
m
For m -.>oo it is assumed that 6 m tends to 0 uniformly in
CELrd 1/2
RV TY Ir'o N6, r)
16(1)) lVIO) PHASE I BOOK EaWITATION SOV/1281
'.~Akedemiya.nauk Kazakhakoy PSR. :Sektor matematiki i mekhaniki.
Trudy, t. 1 (Transactions of the Mathematics and Mechanics Section,, Kazakh S.S.R.
Academy of Sciences, V. 1) :Alma-Ata, Izd-vo AN Kazakhakoy SSR, 1958. 207 P.
-2,500-copies printed.
Eds.: Vaslavskiy, N.A& and Shevchuk, T.I.; Tech. Ed.: Rorokina, Z.P.; Editorial
Board: Akushskiy, I.Ya., Archashnikov,
P (He p. Ed.),
Zhilenko, L.G. (Reap. Secretary), Molyukoy,, I.D,, Strelltsov, V.V.
PURPOSE: This book is intendecl.for scientists, and students taking senior physics
:and mathematics courses at vuzes.
-COVERJQE: The book contains contributions by scientists in.Kazakhatan in thefle3da
differential equations, theory of elasticity, algebra, nomography, calculation
by,machine, theory of plasticity, mechanics of a medium of variable mass, . etc.
it is dedicated to the 10th amiversary of the organization of the Sektor mate-
matiki i mekhaniki Akademii nauk Kazakhskoy SSR (Mathematics and Mechanics See-
tion, Academy of Sciences, Kazakh M.)
Card l/ 4
Transactions of the Mathematics (Cont.) SOV/1261
Strelltsov, V,V. Evaluating the Length of a Curve on a Surface of
'GiVen Diameter 71
Akusbakly, I.Ya* OnSoly0bility by a Nonhomogeneous Operation Cycle 1.11
Akushakiy, I.Ya. On the Solvability of a Computing Problem for a
Triangular Matrix
Archashnikov, V.P. Calculating Stresses in.Intereameral Pillars in
the.Caae When Floor and Roof Remain 133
-th
ArchashnIkovt V.P., On e Problem of Determining the Pressure on the
Supports [Sets] in Horizontal Mining 140
Gulyayev, M.P. and M. 0shibayev. On the Stability of the Rotation of
a Heavy Solid Body With One Fixed Point in the Case of D.N. Goryachev wd
S.A, Chaplygin 144
Kharasakhal, V. On the.Characteristic N=bers of Linear Systems of Dif-
ferential Equations, With Variable Coefficients 147
Card 3/4
(Differential equationB, ftrtial)
400
16 3 08
057
-
T
12HORt
' 0 A Alia4ta)
rOYO
S
OV/39-49-3-4/7
1ITLN: ~...'On, Denumertble: Syo tem of Differential Equationo With
Variable' Parameters
'PERIODICALs , !-MatIematicheskiyabornik# 1959#Vol 49,Nr 3PPP 317-330(VSSR)
ABSTRAM Lattthe,.denumerable'systen
dX
(14 f (t~x rX2 1A,) 1 #2j
dt
* Lot t -be a real variableg.x
be given real or Pomplex
,
variables, f x9al -or complex ftinctiols t /u.parameter. Let
5t x
f be. coa.t
#mdua__in..Hs0, T
R 1j2v**)
.
in H lot
(2) If,(t x **.#qx -1 x 1:, xm+I I
M-1 M
f (t X X X
v 20
~au,
M_ a M+ M
Card 1/3 (s',w
ZTI'FmT*-n; 'AT~~A
0. A.
TrTLEi lie of tha raetbcx.
inootinterftJ In vlbratlw t! twr, -y
g-,xljnts solution, vibre.Wlcm thow-f, --hvvrkj_m%e~ tl, 29 Al
LBMACT: Th_U UVil-110 axmfd*t-a t-tw 7arih m- rrs ts w4i istj
Una" psurtA&I lifferarrtiA"L
~O -raiaa the ;W-WIAM of a vfbmttag rte .'")d .Og-o ';b4vj*' t'bil 'I'll 5;w"
.he go"ri&l ta takau kat4 4'qrv If- I
;Olyz%mi&A or halmorphi6 '*4 -'m' 14 bi Mti :I tP 4 t .)I L.-i
and looti)sItir-1
--va t e 1
t rincAt--,A ~,,;
loll llill~lllli
A -'Yj:Z ~,k ,jp r f -.k.
A.
PENTKOVSKIY j M-V.,, otv- red. V 0 red.; MOLYUKOVI I.D.I.
red.; PERSIDSKIYp K.P~# red.; TAYEV,M.,Fed.;BEDELIBAYEV,,A.K.pred.,-
OSADCHIY, F.Ya., red.j,'.SHEVCHUK, T.I.#'red.; ALFEROVA) P.F#j
red.
9 -U6 Second Republic Conferencie on Mathematics,
(Transaction of
and,14echanics]Trudy Vtoroy respublikanskoy konferontsii po ma-
tematike i m3khanike. AlmaAta, lzd-vo Akad.nauk Kazakhskoy
SsEy 1962* 183 p, (14IRA 15:7)
Respublikanskeya konferentsiya po matematike i mekbanike.,
'2d, Alma-Ata, 1999
(MatheLtics-Congresses) (14echanics-Cor#e sue a)
Axanding the Hamilt=-.Tacobi th#orems to an iufinite mmical
system of.equations. Hateabor. 53 no.3013-328 Mr 161., (KM 2-4:3)
-
L
- - .- - I
t,
. i
L~715)Al, -
-'-L-42733 -66
mw
ACC M.75011714 SOURCE CODE: UR/0203/60/008/002/0411/04-1-2-,---
21
~'AUTHOR: Kpustln, L N - Zhavkov~ V. A.
OAG: Polar GeophysRal Institute, Kola Branch of AN SM (Polyarnyy gooftichesklY,
InstitutKollskly filial AN SSSR)
TrrLE;: Use of the BI-50 counters'id the pro-Geiger plateau
URCE: Gedma etizm.i aerollo T.1. so. 2, 1966p 411-412
TOPIC TAGg:" Geiger counter, oarticle counter, cosmic ray particle' coamto ray measure-
ment
ABSTRACT: The comparatively long dead tinie of counters *hen operating in the Geigor-~"
rbgion and the Hffiit~d service life appreciably lower the qualitative Indices of apparatus
recording cosmic rays and Its reliability. Consequently, the authors measured the dead.
time and recorded the counting characteristics In the pro-Geiger plateau in order to find
out if counters could operate at low voltages. The counting characteristic curves are given:
for the SI-5G counter obtained upon changing the voltage from 1000 to 1300 V at a sensitivity:
of the recording electronic circuit from 1-10-8 to 64- 10-8 A. The section of the character-:-
Istic curve above 1200 V characterizee the work of the counter in the Geiger plateau.
L~C~Fd 1/2 UDC 623.166
)`/Wr
3
/035 00100,1042,10rd2
AUTHOR3: Zhavoronkin, 1o A., Pavlovskiy, V. I.
TITLE:: On adjustment of variometric and gravimetric surveys
PMIIODICAL. Referativnyy zhurnai, Astronomiya i Goodeziya, no. 2, 1962, 27,
abstract 2G164 (V sb. "Razved. i promysl. geofiz.", no. 41, moscow,
1961, 84 - 93)
TEU: On the basis of observational,data.in the Kursk Magnetic Anomaly,
region, the authors investigated the problem on the joint utilization and adjust-
ment of measurements performed with Yariometers and gravimeters urAer different
conditions of topography relief and the character of occurrence of anomalous ,
They.provide recommendations for the favorable arrangement of observa-
masses.
tional. stations for variometers and, gravimeters. The methods are indicated how to
take into account the effect,of.vertical gravity gradients. There are 7 ref-
erences.
P. Shokin
(Abstracter s note: Complete translation]
Card. 1/1
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A 4 P
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we
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01
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L'S
-all
KAN
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0
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9:0
Ag I.;
os
1] -.
: 9 ; 3 b a In no
I ; . I - Z
H MOB 0 e
1,
al
-0 31
.0:o
list
V X v 15
. t:.a I
M3 0
'J.9 46
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4401 1 a 1 :91. 1 .
h A
KIM.
I:*,* I
001 ;i i HOW: o
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MI .4
lilt HI,
I T..
4-9-58-3-4/19
AUTHORS: Zhavoronkinai_~~ and Dmitriyev, A. A.
TITILE: Distribution,of~the chlorine,concentration in atmospheric
precipitation above mainlands. (Raspredeleniye
kontsentra'tsii-khlora v atmosfernykh osadIcakh nad
Materikom)
IERIODICAL: I
zvestiya Akademii Nauk SSSR, Seriya Geofizicheskaya,
1958, Nr- 3,Ipp. 330-336 (USSR).
ABSTRACT: The distribution of chlorine in the atmospheric
precipitation above mainlands is considered and an
attempt is,made to derive theoretically the distribution
of chlorine-by means of analysis of a model of a mainland
of rectangular:contour of a width H and a length L in
the case of a wind in the longitudinal direction7 assuming
a.constant salinity c of the rain masses at the edges.
The, loss in salinity.is proportional to the original
salinity multiplied by therelative speed of precipitation.
Thebasic relation ie Eq.(1)1 P.330. The law expressing
the distribution of the concentration for the mainland
model under consideration is Eq.(19)? P-332. For obtaining
statistically justified data on the salinity of the
precipitation, a mass collection was made of samples which
were analysed spectrally by.a network of meteorological
oCard. 1/3 stations distributed -along two straight lines, one from
49-;58-3-4/19
Distribution of the chlorine concentrationin atmospheric
-,precipitation above,mainlands..
west: h
-to east along t e.middle zonal direction of the
-he
viind:,in the atmosphere; the other along a meridian in
central part of,the European part. of the Soviet Union.
enabling obs.ervation.of the distxfl)ution of the salinity
from the Barents.
Seato the Black Sea., In addition to
salinity, the chlorine cor.;entra,tion was investigated.
The"valv6s-of:chlorine.con~ontration measured in twelve
stations during winter 6nd s e enter,ed in c,
summer ar
tab-leg P.333~an,d the.values of the average dispersion
of the individualobservations for the respective months
and periods are also, given. The experimentally determined
results are plotted:on chartsl Pies.2 and 3, and compare
favourably with the.theoretically derived results. The
assumptio.h was confirmed of the smaller role played by
the smaller Black Sea than by ~he larger northern seas;
however,,the differences are within the limits of random
divergences andl' therefore, cannot be considered as
sufficlently-conclusive. 'AcknowledL;pents are made to
V..V. Shuleykin for formulating the subject of investiGations..
There are 4 figures and 1 table,
-Card 2/3