SCIENTIFIC ABSTRACT RZEWUSKI, J. - RZHANITSYN, A.R.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001446530014-3
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 26, 2002
• Sequence Number: 14
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

io4q; MR 10, 34S

-d- " ,
'. : !~: : -,$eOm
--, . ., - - -"."dynai
- -.- ';,: -.- -~ i-1-

Uic

K"
Ig
Ahii intdactialf-'or rar es ev
n
-IM !S -, =CO
1 54)
. ! I
s is an expository account of the actfbiwat-i-
I amics-.due to.
di t ice formulation of nuantum electioOn
R. P. Feynman [P -,2) 76 (.t949)-,. 769z-789.1 ~MR
hys. Rev.,
I
11, 76511. The Iii-brrespondiiig, fohriali sri is.; a--bo d.eriv-;(I for
the thecry;-6f.'nuclcons7 ifitamOig'.. 69atged
ve-dor me~o~ Peld 'F-..- ----D)4
UN
Kf

m is 'll JAX Mir X*441
1,76; M&
t!b A.
537M
.00
9 4N- 24) 121-8 -00
Pohm
Go S!, Aj*&--~Mw dAWFAIld OM-ft~
00 81,7 Is oWimd a nWWm coUision ivlwm two
by dis w4w 9q"tioo. With orjy
Stmic hourecdU&I, Now "W4 1 wq law
of the scomp-Illokbo forimulm is otolaimcl. **cW st a**
00 law warmim AWN!"o Ownwo am
A#vw wilw-
too 0: kcp.-Iror do PW zoo
-&twimn .k-dm6Alm& -For owl
virkwid" it vmdobm6 bw hr:fmmp voindtin It b of
ft mm ordw em"do brcmwdgmg m-mcdon.
Thm romWm for kwp 1 10, - an Wid for the
reverse Pft%,VSI of pwr protbA-tion In the field of an
0. J. K.
see
x9o
X**
0,00
ties
IRA!. -a
rise
I L mlT4LLU4GK4L LPIF*klbgf CLASSIFKATION
tie 0
I I
woo
T,
A ~v 49( oil i ii OK O.;V is
~19
9 to
Kx,
MLO ad a '" 0 It. 0 ~ 0. 1
IS % AV In K te it it 01 , n 1 S4
004 04 0000 0 0 0 0 0 0 OL0 * 0 & 00 0 0.0, 0
0 9 * 0 0* 0 0 *~e 0 0 0 OS Or'0`0 9 0 9

~-,;:j-RZYWUSKI-- JAN
Mathematical. Reviews Rzewuski Jan.. StatistIca,linterpretation of.the
Vol. 14 No 7 Klein-Gordon equation. Acta Phys, Polonica 10,
July-Aug. 1953 296-299 (1951).
Mathematical Physics. A space-tinie.6pproach [cf.; Feynman, Physical Rev.
(2) 76, 749-759 (1949)1is applied to particles
satisfying the K.Lein-Gordon equation.
K. M. Case

WKOVIGH, Ye.N.; R711AKHOVA, O.Ye.
Serological diagnosis of tick-borne apring-sumer and Japanese
encephalitis. Report no.2: Preparation of inactivated and del7drated
antigens from brain tissue fo chick embryes infected with tick-borne
encephalitis virus. Vop.viruso 1 no-3:26-29 My-Je 156. (KLRA 10:1)
1. Institut virusologil imeni D.I.Ivanovskogo ANN SSSR, Moskva
(ENCEPHALITIS. JAPANISN'B. die.
serol., prop. of Inactiv&ted 4 del7drated antigens from
brain tissue of chick infectee. chick embryo (Rua))
(INCEPEALITIS. EPIDEMIC. diarnosis,
same)
(ANTIG;1S.
eneephalitis antigens, -rap. from brain tissue of chick
embry,oo infected with tick-borne viras for serodiag. of.
Japanese vernal encephalitis (Rue))

LZVKOVICH. Ye.1I.;'GOLIDFICL'D, A.Ya.; RZHAKHOTA, O.Ye.
Sffect of short-wave ultraviolet rays on the viability and antigenic
properties of viruses of Russian tick-borne and Japanese encephalitis
[with summary in English]. BiulAsp.biol. i.med. 77-81 Jl 1570
(MIRA 10:12)
1. Iz laboratorii enteefalitw(zav. - Prof. Ye.N.levkovich) Institute
virusologii,imeni D.I.IvanovBkogo (dir. - Prof. P.H.Kosyakov) AMN SSSR,I
Moskva. Predstavlena daystvitellixym chlenom.AMN SSSR prof. N.I.
Zhukovym-Yerezhnikcvymo,
(ENCICPHALITIS, JAPANNSI 3V virus,
eff. of short wave & ultraviolet rays on viability &
antigenic, properties (Rus))
(37NOSPHALITIS, 3PPD3MIG, virus,
Rusetan tick-borae, eff. of shoit :-eve & ultraviolet
rope--
re a vaibility &, an'tigenic p _8 (RUB))
ITIQtVIOUIT Xi-'YS. sXfoctt3,
-)n -iapaacisiG &~Rrsrilk% t.I.A.-bome anaepha'IJUS biruB-
viability 4' Liatig nic pr(,perties (Ras))
a

RZHAKHOVA, O.Ye.
diagnosis of tick-borne encephalitis; comparison of
different methods for DrepRring antigens, VoD,virus, 3 n0.3:178-183
Y (MIRA -.7)
-Je 158
M
1. Institut virusologii imenIi D. I. Ivanovskogo AMN SSSR, Moskva
(ENGEPHALITIS. diaznosis

15-57-10-14398:
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr lu,
P 169 (USSR)
AUTHCR: Rz hani kova, L. N
TITLE: The Petrography of the Coals and the Spore-Pollen.,
Content of the Tertiary Continental Beds of the Zhilanchik-
J04Y. Basin (Southeastern Part of the Turgay'Basin)
Zpetrografiya ugley i sporovo-pylftsevoy sostav tre tic h-
noy-kontinentallnoy tolshchi Zftilanchikskogo basseyna
(Yu.-V. chast' Turgayskoy vpadiny!7
.PERIODICAL: Tr. In-ta geol. nauk. AN KazSSR, 1956, Nr 1, pp 5-141
ABSTRACT: The Zhi-19Lnehikskiy- codl basin is a platform in
traconti-
nental basin. The coal deposits are not persistent,
as a rale,.and are variable in thickness. Their s ize
and thickness were determined primarily by the con-
ditions of peat formation in theancient swampy and
steam-bordering basins, but also by syngenetic and*
epigenetic erosion. The coal, beds contain many mineral,
Card 1/4 admixtures) the chief of which are amber, finely dis-

15-57-10-143918
The Petrography of the Coals and the Spore-Pollen (Cont.)
persed clay material, pyrite, jarosite,.sulfur,-melanterite,
and gypsum.. The deposits generally show a simple structure'.
Petrographically they are divided into complex and.homogeneous
types. The coal is of the brown varie.ty,. in them first stages
of coalification, and is-humic. On the basis of, outward
appearance, the coal is,divided into three groups: lignite,
brown dense, and brown porous. In each group megascor'c and
microscopic types and varieties are, distinguished. The coal
deposits of Bolattam, Altynzhar, Kushuk, and, apparently, of
Dyusembay are composed of low-quality types of brown coal,
argillaceous clarain,and lignite. The coal deposits of
Zharkuy and, ai3parently, of Kayddul~ are high-ouality brown
coals, durain-ciarain, -mixed and spore-polien-durain-, pollen
liptobiolith, and lignite. The original material of the coals
was the remains of higher plants: swamp cypress, swamp poplar,
-er lilies, pond weed, reed, alder
royal fern, polybody fern, wat
hornbeam, hazel, walnut, oak, chestnut, elm, and others. The.,
coal formed under conditions of high moisture by.autochthonous
and allochthonous means. A relationship between spore-pollen:
Card 2/4

15-57-10-14398
The Petrography of the Goals and the Spore-Pollen (Cont.)
groups and the petrographic type of coal is recoanized. Each,
'Aral, and Pavlo-
stratigraphic unit (the Indricottleritim, ~Turgay,.
dar series) of the Tertiary continental beds of the:Zhilanchik
basin is characterized by a definite spore-pollen group. The
following groups are described for the different series. The-,
coals of Bolattam, Altynzhar, Kushuk, Zharkuy , Kaydaul, Sarly-,
tam, Dyusembay, and the coal oc3urrence at Chink-Naush are
characterized by the same composition and the same spore-pollen
types. They are all of the same age and are confinea to the.
Indricotherium beds of the middle Oligocene Indricotherium
series. The brown-coal deposits and 'the oolitic iron ores of,
the Aral region, Turgay, and Northern Kazakhstancontain similar.,
spore-poller groups and are of the same age. It is thus demon_
strated that 'Tertiary brown coals and oolitic~iron ores formed
on the Kazakhstan plain synchronously during a single period of
time and are associated with the accumulation of carbonaceous-
le-otochloritic formations. Data from spore-pollen studies
have furnished details on the problem of the climate.-if the
basin in Indricotherium time, on the landscape, and on the
.Card 3/4

m

m

RZHANITSYN, A.?.. professor, doktor taklinichosk1kh ,.auk; AFANASIYXV, A.M..
TaOdMit tekhnicheskikh riauk, rjauchnry redaktor; TUMARKIII, D.M.,
redaktor izdatel'stva; BORODINA, I.S., redaktor izdatel'stva;
HF.DVEDEV, L.Ya., tekhnicheskiy redaktor
CStudias on problems of construction mechanics and the theory of
plaeticity; a collection of articles] Iseledovanlia po voprosam
stroitellnoi mekhaniki i teorii plasttchaosti; sbornik statei.
Pod red. A.R.Rzhanitsyna. Moskva, Gos. izd-vo lit-ry po stroit. i
arkhitekture, 1956. 326 P. (MLRA 9:9)
1. Moscow. TSentrallnyy nauchno-issledovatel'skiy institut
promyshleanykh sooruzheniy.
(Plasticity) Otlasticity)

-
-
-
W
60 off 91-
6
4
Itifftif 00 0
jifi
yl
T
01 ix4vo
x
d h I a
-
j . L . ilou is
A

A ._
..
pg*l
I IT ANO IMP 0 .2!R_AMO
10 1`410CISRS Ave FOOP11111111 was.
7

-
;L
condidon , 9.
chi4~ ;iii
k P_Rsbouiits7n~ Fork. Phys. (U.S.&R.) 17,491-6
0-
A M.-The creep brhavior
(1047): CA*'"' Zp4r- 144Y. 11. 1
of olatedailk Is iun~.Ijntrtl front the theoretical standlitAlit
under the "mcuVAon that their structure mimixts o(a I'artl

ir
it vis,,~ous sul"tunce
skeleton with lac-M-orts Mcd with
- Vv: u
tion of alls
ual assum
b
ii
th
oje~4
s
.
s
.
at can
e t
p
& clutiticity of this szeet-ain Wa to a linvur relation lietwern
g
mr.-it vid dr',,,ra,*tko_ %~.j friplalno only rrver,tible mw-
-.e" to conlro.t to'W"Is upti
the prol...
A 4"nuipiloo o0

z
-
,
ek-A ij. An ballistic su~-i4xivl am 4-t-tilictl 14) thr hani oo
0 cnnstituent of the mattl-al. Inch a it, -lei of a ulatriiall %4
the hard eDilgitilurnt le Which d0-$ nOtL '-jrmtoilooke% =00
law, coffri4it"14% wl-z u Wilf, if --;: 's to Ch "!tual lwhAvi,w
of stnicturitil mottL9~u.. TM --t;,.t of tita%, anti dy"notiv
-
l %0
1 ffrep. the title of whie
l
Olfriiov4 Is exprivI041 In the funn fee
i-unot pruportitaial to the magliquile of the adlug furve,
l

re
h t delwatia also upon the time cif action. rlie inateria
,ia,lft does not return to Its orifficial condition after mnovul of 1:0 q
the at". but retains a definite residual &U.-i-mation.
Analyqio of the lirtifilkwil model off-rrs a elmrrr exislanatimi
l ago
lliferp"tatiotl
A MW twhavilw than It lxvwlllr fly the um~m
11 tT"lp ritrvr,. M- G,
b
0o
MOO

- 2100

Ao
111 I
L ANTALLUJIMICAL LITINATUNt CLAUNFICATION
-

I
P too". 00,4111V
Sanoso .0
1 21111t S.10.0 It O.W 081
Vvill
" U .
a go K IMF 9 If off
7
0 0 009 0 0 0 0 0 o a fill 0 0 0 :00000 a 00 Ges ell
0 a 0-0 0 0 0 0 so 4111 0
_0 000 0 0- 0-6 0 9000 0 *000*0 0 0 0 0 0 0 4D a

16
-

A a
-we cfscpm;b.4r la the woos, -A "Some
whia 10:56c 4alt

Ve'. ;WAllki9kTqw2m

1-4~i f~m ful 5--P-W2 M, %ff

~li A-IEMM-tl

BOV/24-53-12 1/27.;
THOR
itsynq~'!_AOR. (Alos~6iv);
Rzhan
-TITLE: imitiug Eq3iilibrium. of Ferroconcrete Plates.
IL
- ----- zhelezobdtonnykh, 1 ihok)
p ast

i~?,kIODICAL: Izve st' a Akademii:5duk -d' Tekhnicheskikh~.
eni e
Ot, e 1

_N,
-12 ~(~SSR
auks 1958
~.ABSTRACT: The: 'Condition ~~Of_ flow:,in: ferroconcrete 'plait' s~ differs
e
Huber-Henchy-Mises ~eriterion and for a 'late
from~the
p
uniformly. reinforced on~ both,,., id ' two
si es in- er d cular
pen i

directions may,. e. writte~~

-
th
b
ii mm, (1 w here Im 'is

max
:
b
,
e
aw
Mu moment: an he ing
ending
:

iit~ If the piatd is 4-~_piid
Mome or e on-one side.only the
flow cohdit ions are mmg~x:,= mT 0
mmin
'
Consideration of the internal.ene, gy of, the plate
,and of

the 'work done by, ad
-the,exteimal f orde s 1e s to. the
condit io
qw mrl.92~AF m
the 'xt'erna fored w is-the deflection of
-,whj6're cl -is :e
2 AY is. ele

2 + '2~ lay. and an ment.
v N
/ax
'
"
..
plate. surface. :,For a pOlygonal
plate wlth:hinged
::th6 te als y

Oig gr
4 -- 1 2 -_ in ma be

rwl--Z~Ap wv.O-T~l tM

IV . .,--
* I %
-