SCIENTIFIC ABSTRACT RUDICS, I. - RUDIK, A.P.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001445920013-2
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 20, 2000
• Sequence Number: 13
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

IUJDIC
Resection of npiphrmnal diverticulum of esophagus. Hael. eebeszet
9 nn.4:263-266 Aug 56.
1. A Budapeatl Oryostudomariyl Egyetam Sebesztovabbkepzo Klinikajanak
(Igazgato: Littman, Iweegyeteml tanar) kozlomenye.
(ESOPRAGUS, divarticula
apiphrenic, surg., resection (Hun))

T r

RUDIC-TILANIC, J.
Subotica and its metayers. D. 94.
Periodical: ZBOFI-IIK ZA PRIRODNE NAUKE-. IvIatica srpska. 14,.)Vi Sad.
SCIENCE
No. 9, 1955.
S'): Mbnthly List of East European Accessions (EFAI) W
Vol. 8, No. 4
April 1959, Uncl.

Its
"Nh.= Fc;rmaticn-,; cf ti-ie Central .',~artls ,-' tl-e Sarytncev a:~
Content of Ore."
d-.-ser-.atlon defended for the degree of Candidate of Geolcgical Scie-~Ces, at the
inst. lcr '-he Geology cIf Ore DepcDsits, Pe'u-rc!-raT)I-lv, Mineralogy and GeochemisUry.
(Jan-'ul 1957)
Defense kif Dissertations
Sect. t~X ScL.
Vest. All S'~'S)R, 19757, v. 27, 11 12 pp. 113-115-

RUDICH Kjj.j AV. red.; MARMINA., T.Yu., red.izd-va; DOROKEBA,
tekhn. red.
[Geological and geopbysical studies in volcanic regional
Geologicheakie i geofizicheskie issledo-vaniia v vulkaniche-
skikh oblastiakh. Moskva, Izd-vo AN SSSR, 1963. 165 P.
(MIRA 16:12)
1. Akademiya nauk SSSR. Sibirskoye otdeleniye.' Institut vulka-
noicgii.
(Volcanoes)

-,RUDICH, K.N.
"PbstgranitO dikes in the Berelekh Basin (sources of the Kolyza
River)., Sov. geol. 3 no.6:131-134 A 160.- (MIRA 13:11)
L Vaesoy=nyy natichno-issledovatel'skiy institut plyezoopticheskogo
syrlya.
(Berelekh Valle7--Dikes (Geology))

SOV/124- 57--8- 953 1
Translation from: Referativnyl, Atirnal. Pvlekhonika, 1957, Nr 8, p 137 (USSR)
AuTHOR-, Rudich. M.A
Tvri-E~ Allowing for tile Combined Effect of Bents Interconnected by Rigid
Coverings (Uchet sovrnes1noy raboty rarn pri nalichii zhestkikh
perekrytiy)
PLf.'',OD!CAI-- Nauchn, zap. U~.ovsk. politeklin- in-t. 1956 Nr If pp ~- 15
A P, P C j By the usual methods of structural mechanics an anaivsls is rnade
of -i systern of bews inlerconnected fly covering.s vvhich are absolutely
ri- id within 'heir own planes, The author neulect.s the flexure of the
framc meoibers in the horizontal plane due to t.wisrino of the system
\vilh rk-spect fo a ~,ertical axis; neglected also is the torsional reac-
lion ot the struis, It is considered that the load is applied to the bents
w0hin their own planes only,
I- K- Snitko
Card I/t

I,- ~17- ',, ,

RUDICHY Serge7 Ivanovich., kand*tekhne SITSILIANO., Denis Denisovichy
ka~d.tekbn.nauk; NAGORNYY, A.G. [Nabo i., A.H.]. red.1
CHEREVATSK371 S.A. [4herevatslkyip S.A. . tekhn.red.
[Mechanization of the procurement and placement of local
fertilizers] Mekhanizateiia zahotivli ta. vnesemia mistsevykh
dobryv. Kyiv,:Derzh.vyd-vo sillslkohospodarslkoi lit-ry URSR
1961. 150 P- (MIRA 15-51
(Ukraine-Fertilizers and manures)

RUDICH V.
Helping brigades of comtrUnist labor. NTO 2 no.12:39-40 D 160.
OAIRA 14:3)
1. Predsedatelt pervichnoy organizataii khopchatobumazhnoy
fabriki imeni M.V. Frunze, g. Moskva.
(Moscow-Zotton manufacture)

Rb'-Z.C",f, V. F. -- It'Llie Process of "ci-matim of Concepts on I istor
among
Npils ir the lirst Four Classps.11 Mosco-,r Stat~ Pedagogical inst
imeni V. I. lenin. l-!oscow, 1955. (Dis!7crtation for the Degree cf
CandL;ate in Pedagogical Sciences).
3o.: Kni.zhnaya LcAopisl, No. 2, 1956.

RUDICH, Ye. M., SKI-EA. S-I-
Principal stages of relief development and recent
tectonic in southern Sakhalin. Vent. Moak. un. Ser. biol.,
pochv., geol., geog. 141 no-3:209-220 '59. (MIRA 13:6)
1. Kafedra geomorfologii Moskovskogo universiteta.
(Sakhalin--Geolop,v. Structural)

RUD_jGjj,_-Xg_VggAiy y.=kQdj IRUSIIEVSKIY, B.A.,, otv. red.; MIRAKOVA,
q_4; Pr
L.V,, red..izd-va; POMIOVA,, T.P., tekhn. red.
[Basic cha racteristics of the tectonic development of.
Sakhalin, Japan, and the Maritime Territory as the transition
zone fror. the continent to the ocean]Osnovriye zakonomernosti
tektonocheskogo razvitiia Ftimorlia, Sakhalina i IAponii kak
zory perekhoda ot kontinenta k okeanu. Moskvaj Izd-vo Akad.
nauk SSSR, 10/62. 271 p. (MIRA 15:11)
(Soviet Far East-Geology, Structural)
(Japan-Geology., Structural)

------- ----
S/519/60/000/008/026/031
11051/11113
AUTHOR; Rudich, Yet Lit
TITLE: On the geological basis of the seismicity of Sakhalin Island
SOURCE; Akademiya nauk SSSR* Sovet po seysmologii. BytLlletenJ? no. 8p
Moscow, 1960. Voprosy seysmicheskogo rayonirovaniya7 196-199
TEXT: A new scheme of seismic zoning for Sakhalin Island is proposed.
it is based on a comparative study of seismostatistical and geologic-tectonic
data and supersedes the old system of,zonation carried out by Go Po Gorshkov.
It also differs from the schemes of V, Ye. Dibrov (Refe 3: Seysmo-tektoni-
cheskoye rayonirovaniye Sakhalina [seismic-tectonic zoning of Sakhalin] .
DAN SSSRI 113# No- 4, 1957) and M. Do Ferchev (Ref- 4: K voprosu a seys-,
michnosti ostrova Sakhalina [Contribution to the seismicity of Sakhalin
Island7t. Nastoyashchiy sbornik), whose evaluation of geological factors is
partly rejected. According to the author, during the Tertiary period the ,
southern and central section preserved the character of geosynclinal develop-
ment,.whereas from the end of the Cretaceous period,the northern part remain-
ed relatively stable. These two zones are still observed on the.island.
Card 1/2

S15191601000100810261031
On the geological baois of 99#& D051/D113
In addition,during the whole of the Mesozoic and Cenozoic periods southern
and central Sakhalin were divided into two subzones: a western intrageo-
synclinal and an eastern intrageanticlinal zone. All these features suggest
a decrease in seismicity from south to north and from west to east; this is
fully substantiated by seismostatistical data. The author divided the islandl,!~~
into five zones of various seismic activity. In many cases the distribution7
of seismic intensities up to 7 differs from that of M* D. Ferchev's scheme.
In the south-west section of the island)an area of intensity 8 is assumed on
the basis of Japanese data on earthquakes of intensity 8 in the southern part
of the Tatarskiy Strait. The present microseismicity of Sakhalin is explain-
ed. There are 1 figure (map of seismic zoning) and 5 references: 4 Soviet
and 1 non-Soviet-bloc. The English-language reference is: T. Tametaro. Bull.
Earthquake Res. Inst. Tokyo Univ. 10,pt., 1, 1932.
iISSOCIATIONt Institut fiziki Zemli AN SSSR (Institute of the Physics of the
Earth of the AS USSR)
'Card 2/2

SOV/5-58-6-5/13,
AUTHOR: Rudich, Ye.M.
TIT TJE: To the History of the Formation of the filesozoic-
Cenozoic "itructure of Sakhalin (K istorii for-
"'i"ova"iya mezozoysko-kaynozoyskoy struktury
PERIODICAL: Byulleten' 111'osl_-ovskoL~o obshchestva ispy-
tatele,f prirody, Otdel geoli-icheskiy, 1958,
1,1-r 6, D 1-9-88 (USSR)
.1
The author gives an e.-c-turemely detailed de-
scriDtion of the Cretaceous and Tertiary de-
Posits of Sakhalin and of the history of 'the
f o rm a 11-1 i o n o fl~ i t s s tructu-_-e, in thle -','esozoic-
Card 1/4
Cenozoic era. ~ccord-_-ns to his findings,the
formation of the est Sakhalin 11ountains oc-
C)l
curred in the late Uo-oer "Miocene evo h., and
before that time, the region 7,as a d=-oression
L
(maps Nr 4 9). He disa-rees with some of the
0
geologists who. thinh that beginning vdth the

SOVI/5-58-6-5/13
To the History of the Fcrmation of the 11.'esozole-1-aenozoic
Structure of Sakhalin
Paleogene time, the West Sakhalin elevation
existed. As for the Eeological development
of the island the author fixes the following
fundamental stages: 1) the Upper-Cretaceous
stage, which embraced the period from.,the I
end of the Albian to the Sennonian st ages;
it was characterized by intensive downward
movements; 2" the stage of a continental
develoDment, vinich continued up to the Eocene
epoch;_ 3) the Eocene-Milocene stage, character-
ized by a considerable sinking of almost the
entire island; and 4) the Pliocene-Quaternary
stage' when the elevation process started again.
In the Upper Cretaceous.epoch the Sakhalin de-
pression formed.a part of the Nippon geosyn-
cline. This connection became more loose in
the Tertiary period, and was not felt at all
Card 2/4 in the north of the island. The following

SOV/5-58-6-5/13
To the History of th-- Formation of the Liesozoic-Cenozoic
Structure of Sakhalin
geologists %fao ~.-~orked on the island are men-,
tioned by the author: S.N. Alekseychik, A.
0 Arkhipenko, III.F. Budnil%ov, IT.A. Voloshinova,
A.A. Kapitsa, V.N. Kirkinskaya, L.V. Krishto_
fovichl I.N. Kuzina, B.S. Nikonov, I.I. Ratnov-
skiy, S.S. Razmyslova, L.M. Sayapina, Ye. M.
Smehhov L.N. Solomat-inal V.V. Tumakov, T.V.
Ulkhina, N.D. Tsitenko. N.Ye,. Yerofeyev, V.N.
Vereshcha-in. B.M. ShEempel?, K.F. Yevseyev,
Card 3/4 F.G. Lautenshleger, O.G. Red'11-ina,'LI.I. Borsuk,

SOV/5-58-6-5/13
To the History of the Formation of the L:esozoic-Cenozoic
Structure of Sakhalin
N.N. Tikhonovich, I.B. Pleshakov, L.I.
Krasnyy, K.F. Rak-hmanov, Ya. Ye..Pashchenko,
P.D. Shklyayev, R.Z. Genkina, L.M. Zhidkova
and A-1. S6-Lovlyev. There are 7 maps, 2
schemes and 1 table, and 17 Soviet references.

5/030/62/000/011/oo4/oo3
D216/D306
AUTHORSs Levin, B.Yu., Doctor of Physical and
Mathematical Sciences, and Rudich Ye 14.
TITLE: The fourth conference on astrogeology
PERIODICALt Akademiya nauk SS311. Vestnik. no. 11, 1962,
131 - 154
TEX": The conference took place on May 7 - 12 in
Leningrad. The present authors report that some of the papers
read at the conference, and indeed "astrogeology" itself as
defined by the participants in this conference, must be treated
with some reservation, since there is some doubt as to their
scientific validity. Among the papers read at the conference
were the following: P.S. Voronov "Main contemporary problems
in astrogeoloEy" G.Zt. Katterfelld, "Astrogeoloey, its content,
problems and place in the sciences" B.L. Lichkov, "Interaction
between the earth's shells and the conditions of its rotation
as the cause of all the,geological phenomena on the planet"
Card 113

S/030/62/000/011/oo4/005
The fourth conference D218/D308
B.L. Lichkov and I.I. Shafranovskiy, "The universal importance of
some angular quantities characteristic for the earth" G.N. Katter-
felld, "Pregeological era in the history of the earth and its effect
on the evolution of the geoid" P.S. Voronov, "On the rotational
causes of tangential stresses in the lithosphere and 3ome of their
geostructural consequences." M.V. Stovas, "The effect of external
factora on the seismicity of the earth." A.V. Shnitnikov, "Tidal
force as a factor in landscape dynamics." Papers were also read
by F.P. Krendelev, I.G. Flushin, A.A. Khlobustov, R.I. Burtman,
V.S. Vasillyev, A.V. Volin, V.S. Voropinov, A.V. Dolitskiy, 0 1.
Islamov and G.G. Tamrazyan, but the present authors find t~em-
selves unable to take them seriously. The remaining papers were:
G.G. Khizanishvili and M.V. Klenova, "The origin of submarine
terraces in the light of the rotational dynamics of the earth."
V.A. Bunin, "Recent problems in gravitation in the light of classi-
cal physics." B.V. Timofeyev, "On the discovery of organic resi-
dues in stony meteorites". G.U. Lindberg, "On geocratic oscil-
lations in the ocean level." V.A. Zubakov, I'Absolute dating of
glaciation in the last 70,000 years." V.V. Kochegur, "Faleomagnetic
Card 2/3

S/030/62/000/011/004/cO5
The fourth conference ... D218/D308
a tudips of bani.1 ts in the Soviet Par East. 11 V.S. Lebedev, "Fo r7
mation of chemical elements in meteorites under the action of
cosmic rays." V.F. Derpgollts, "The 'hydroclilorospherel as a
planetary source of all natural water in the outer shells of the
earth." V.I. Vallfson, "Free oxygen in the earth's cruet." The
resolution of the conference noted that the conclusions rea ched
in many of the papers were not sufficiently well argumented, but
nevertheless, it was recommended that the proceedings of the con-
ference should be published. The present authors are highly scepti-
cal about the entire venture.
Card 5/5

ILIVIN, B.Yu., doktor fiz.-matem.nauk; RUDICH, Ye.M.
Fourth conference on astrogeology. Vest. Ali SSSR 32
no.U :131-134. N 162. (MIRA 15:11)
(Earth)

P"re -baitted for the IOU Peoria Sdiande 4:OnCra*-, HcnDlulc. Hawaii 21
SPO 1961.
A-MMAI-G, Y, MOLMLA-L.-I.,
I jv~
VAJ LAW
All f2vos the Institute of 0-lovo Ac.~Alv or "-itzc,s L1,33
'MO lWttom r-110f0f the t~irlc 0.ean end Ito c.:-tr-phjc
re OWL (8.1tio, It
Acade
at t :7 of
or
phid fishe. oCthe Antar~tlc azA the probltc- .; their
birol r ustritution in the Patiric oeeae (Section :mc)
,# - - r., end $4ZAMVA_j,_p~, 1.2t... Of
"The vinagame. of the P-IrIc Oc cn, (3-tt.. VII.C.1)
AM --- irEV, 0. V. (tt-e blurrcd, bt may be AFk
Ust tute of GeoloV of Or* D-posits# PetraZrullir. ?Ltermlugy,
and Geochealstrr - (Title of ;.per In blurr-.; L~
appro,xi. a title) - dise.n..Inu-1 1-1cj layer
.-rogrph Icdatet( -ttoq V11.0
e or r-rth Thy,le. 11-11 0. 1. 1cluallt -
r or atre.. a .4 -.;-ures 1. the r-L of the
Irle ..16mle ..nde. (Section VII.C.,I)
IM-It.t. of ZOOIa 'On the of
the AnsrhLQ6411ae famity, (section, 'JI.C)
Ta)Ct5% State thj~#,.Uy - "0. the heat
MM~of the Tor 51st (section '111.n)
BEM=C-~-Y- laatltu~.,c 0"-.Ol.v - "an the
of be Plemlftoa Of -be PwIfIz drift ani in t4e %;Qft--ew- -tt-s-
(Section 111.0
3==CT,-t-r- and I 1..titat. of Barth Phynits 1-,a
0. Tu. Schmidt - of the 0y.n.1 dt7ros.i.n of
the "a or ip.61 (s.~ti.n ri.C.2)
In tltut~ of Da~oIDV of q,ld
-1 t
:eth e. the oce- floor" jj:.C)
-,~= rnstituto of Oce~loa "s-ent xed.reatation
and the geologLcel hLvtory or the Okho-;~L ea4 (Settlon V:I.C.1)
V. GrA SMR-rfAMIA,
or 0-emaolcm, - 'airee.
la. VII.C.1)
-&-, and Z-lt.-tvtc or Octonol.p
"Bome "QUIc f, et-ev in the Emiari;hlc.~, d43tribut ton of st7sull
pelagle animals (Amphip.60" (section 1114)
X.st it.t. of C-ca.nol7a, - -N- 'h--. or to. jd~i 11'e.
and the character of tidal fhenoneun In the Ocertft" (Se~tlcn
T=.B) q
7, " 711,*~,~7~~Zj, 1. 1! :-t1tut.
or Oct.".1na - 'Th, dl.%rLL~~L-.n or -ie ~,Pl tw~o In the
purl"Ic or.=" (section Z11.C)
-0. Its-itute of C-1ca LpI2t*-ttc-, -1 C~,t-tLblc
VAterials - "Me ditCenetlc chor4to in bottom -1!~nts rma
the cratre,,- par- of the vnx.l)
a- I=tL-.-e of Gcolo,- - !.d the
tie. in the dls-rtbutiloa or =Lneril resa,rcai -a t.-~ geov.-linal
or 'he Ter-Lary In the oxca cr ~A
s.kh.1 I. Iland* V-,1 -C)
and -C
fe.-ure. cc 11-Ullia
the I tter L. the ForLfk f tha
(Sec-L.. Ynx,l)
BUT=-Y~A, Tutitte of "A of c,11.t.rW
Mxre.t . in the P1.1-fit"
and t-tLt~tc I
,The "--tio. of' air -,a 'c ift toe -i,er, ~f the
Ocesm- (Settion VJI.A)
lnutlt~te Otvt~~!,-v - ~Tje rr;4,an.. oV
and tr~--tlon wuro~o of In "c wrth- pe- .., thr,
(S-.I--.
pec.t.-Ic Ocew

P-r. Z.1tted for the loth racris 3et- conc-s, non-into, H-kit 21 Ag-
6 a., 61.
S., institute of Geci.Gy - "Mto-.t.tc dopma.iong and trou&A
OT Wi.t isfitte type =4 their position 1, the Gy..t_6%lc. of tee-OtIe
forms" (section VZZ.C)
A, Moscow 3tate Unlvvmttyj Physuai racuity - The rAr_-a-rmT
spoctrtc trta maxer onto c! a.-Ificial r%dLoact.-vitl in up-,er lnyvrp
of the O%an- (sect=Le. vrz.3.6)
Vt-P.j Chair or rorestr7, The Arrimatural AamdM-7 !Lent X. A -
"Forest fire resea:rch ml =eth-le of fLrt =troll (5acticu V.11)
Institute Of 0-anoloa - 'BLvre.9lSphlcz W-d
morphological amnly.lo of ";rc4uction and dr-L-1,cot or fltrl.h
in the seas of the ucrth~_st Pacific' (rieett on ttl.~)
~.' Institute of Co._OlCL' - 'In.'ett ~r the IwItmto.1
turbulent exchange in the Pacific Ocean" (Sect on
EA~;i-p. V., rnntltute of 0ce3nOlcj:- n the
distribut Ion or flying floh~3 -n t-he P~clfit Civ=" (~-tl~= M.C)
YPGA=:7. -H. A., In:-ltute cfC'!.l.C7 - "3.r.-L.7-nt. h~rit'- .1.1 tt'e
hotju~' .. vnx)
I of Xr.
erttaceou, a t c_ (Scctl
do,
Institute of Oceanology - "The prot"s.re of recent ftodi-
ventation In the "stem ;art cf the equatcria.1 -no to the McIfW
.ct,
(e
D. A., Institute or E=th rl%~ico !~nl 0 N. 50=114t -
*The netanic roological :vnd-.t; to.,* In the nc~hw_stcm vj-lylnp
or the Pacific basin" (:~c-tcn *41:X-1)
Institute of Ct.-I.a 1. the
northern ;w- of the Pacific- (Soctl~n inx)
Institute off :oola - '-,he [-bll- or ti,e J~d
brjdM frec, the zooloc~.C&l i,oitt -r 'I e e' r~ttlcn UNI.A.3
Lt~q*-~403M.-Xuk'N., Institute of G-loa - ":-a zpe_Clfl: fc.t.rei
In the -ettomics of the acr-.h rart of be (5ettlen Vit-C)
2nu=,jA, Moscov 3tate ~hvt'al F~cult~ -)'A ir-e1%
device for rewrdt.r -..t3 (-MV ) 3--ti.n
PADlTJ'tCr,,Y.. A., Institute or seol.a - -Cn the Stelllty -a
dimimk~~cW of 2-mctl=&l eements In the fr- of the racifLe Oce=
p Osten. (Section frz.c)
md GClT*'*:tl';A_3.jT.' Indtit.... Of
lo re
0c.-loor reca!~it ci .4 _ircd,ctt~n and
4.1op .. t of)mgs fish" to the morthe.-O po~- or the
Root I- firx I
ZCLA.'=_lzr= a.A. InIlIt.-O of Dcowcl.C.T - "Crcvllc lub,tore. la
bott- a.dl-.te in the llotern rurt or the P.-Iric'
Te cf T~-.b my-.I~A tnent C. TA. t
-on d-;, -th-. ~.k". In ho or
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Th~'mrrol.-Lv -thd fL.r t,41~1or 7U.C.2)
of otca,-'c%7
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the reoh.~J.G of -be
f ~tvl the
th-ry of 'he "Cnnt In o-3 ~d -nc~*
(U~tlcn VII'A)
!MTMN G. 1. th~
'"WEVAL MA-Ta" 1-tit-2 of 3c,,IQL7
71I.C
A, Y. inottt~ote of "Ttleu. my.'al. in
el.tl. of the pl.M.2* (31~ttcn ltr.~)
to, -t -
ln.tl-.ltt~ of i1q, &
(T) cr.Cln ~ 30 -a '-r -C -2)
-he Cent,sa C.,-,-l-tlcn f 'm3
p-b.
11.1-o3 E;-C,-~yhy old th,ir 311c,~lrllc=- I.. ;r~;tqla,,t1c
SIM3111KIT. P, A. rn.tt."! ~f F'.m'r,.t of
Antarctica*
lnottt.tt cf C-,-ca, - 'Pith t--v,t, p
curro.t. 1. the cot- -d %~r, "-Ite ---f t~,'., ~;rl
Pacific OcIm" (3ectLcn

LA11;4 SKIY. V.I.; STUPARI, K.I.; RUDICHEV, K.P.; OLMENKO, V.V.;
AI-ISKIYY A.K.
Pouring rimmed steel into bottle shaped ingot molds. Izv. vys.
ucheb. zav.; chern. met. 6 no.11:65-69 163. (MIRA 17:3)
1. Unepropetrovskiy metallurgicheskiy institut.

LAPITSKIY, V.I., doktor tekhn. nauk, prof.; MARINOV, A.I., inzh.; OYKS; G.K.,
doktor tekhn. nauk, prof.; OIMMMO. V.V*' inzh.; 04wv. V.I.,
kand. tekhn. nauk; RUDIGHEY, ro-P., inzh.; STUPAR',X.I., kand.
tekhn. na&, dots.
Reducing the inhomogeneity of large rimming steel ingots (up to
18 t.). Izv. vys. ucheb. zav.; chern. met. no.2::19-33 IF 158.
(MIRA 11:5Y
l.' Dnepropetrovskiy metallurgicheskiy institut, Moskovskiy institilt
stali i zavod "Zaporozhotait.0
(Steel ingots)

BRAG13, V.F.; PUPIMEVI K.P.
Intc-naification is a muns of increasing the production
ane reducing the cost of open-hearth steel. Met. I
garnorud. prom. no.6:11-13 N-D 165. (MIM lSzl2)

TIP*" ;7-,,'X "Y". Go M, kend# gecggraf.
fare,~i,311 fcr the U.S.'J.P. 3r
g.' 'rr)L. no.12:69-72 D W-,. f -Lp
is J." en'tral r-
,yy inst!"ut prnFnc,7oj.

LITTMA.N11. Imre. dr..; HARKANYI, Istvan, dr..; PADANYI, Alajos, dr.,;
TOTH, Jozsof, dr.,; RUDICS. Imre, dr.,; TAKATSY, Indre. okl. gm.
Induction and abolishment of ventricular fibrillation by
electradhock. Magy. sebeezet 9 no.3-166-169 June 56.
1. A Budapesti Orvostudomanyi Xgyetem Sebeaztovabbkepzo Klinikajanak
kozlemenye Igazgato: Littmann Imre dr.. egyeteml tanar.
(VNUTRICUIAR FIMILLATION, exper.
induction & abolishment bv electric fibrillator-
defibrillator appar. in dogs (Hun))

FVUDIC- VRANIC, J.
SCIENCE
RUDIC-VRANIC, J. Matica srpska. Novi Sad.
No. .9, 1955. Subotica and its metavers. P. 94.
Monthly Index of East European Accessions (EEAI) LC Vol. 8, Nol 4, April, 1959

.4 t ~t t T rarbide-titanhun
~4 system mrbide-chromium

Nu. 5 0, RUdivig- Metall 7. 967-43(1953).-In the ter-
-
-
nary sysfe
m
WC-4fG-erjC, the soly. relations on, the Cr-.
'
10, 1954 poor side were detd. by rantgenographic and metallographic

raphy
means.
It is shown that WC dissolves neither TiC nor
CrsC2 in noteworthy quantities but that in the entire investi~
gated rt:gion TiC takes up CrsCt and WC. The range of~
Lattice consts. and tnicrahardness were detd. In the region
of 56% TiC. 23% WC, and 21% CrsC*, a aum. of ruicro-:
Mrdness occurs. Its value is 4300 knoop per sq. mm.
H. Stoertz

(CEREBRAL CORTEX). (HEART)

RUDIGER, W.
Interfering subcortical stlimilations and cortical spreading depression.
Fhysiol. Bohemoslov. 11 no.5:392-398 162.
1. Institute of Physiology, Czechoslovak Academy of Sciences, Prague
and Physiological Institute of Humboldt Uni~ersity Berlin.
(CEREBRAL CORTEX) (CONDITION15D LEABJMTG~
(MESENCEPHALON) -(MOTIW.AMUS)

RUDIGER, W.; BURFS, J.
Cortical .spreading depression and tegmental and hypothalamic threshold.
stimulation producing locomotor flight. Physiol. Bohemoslov. 11 no.5:
399-403 162.
1. Institute of Physiology., Czechoslcrvak Academy of Sciences, Prague,
and Institute of Physiology, H=boldt University., Berlin.
(CEREBRAL CORTEX) , (MESENCEP11AWN)
(WOTHALAMUS) (AVOIDANCE LEARNING)

MaSOVA, 0.; RUDIGER, W.; BUMS, J.; FIFKOVA, E.
.dvthalamle drinking centre in unconditioned and conditioned
The rcEe & the Ir
control of water intake., Physiol. Bohemoslov. 11 no.6:492-496 .162.
1. Institute of Physiology, Czechoslovak Academy of Sciences, Prague.
(HYPOTHALAMUS) (REFLEX COJIDITIONED) (REFLEX)

RUDIGER, W.; GRASTYAN, Z.: MADARASZ, I.
Connection of effects of electric stimulation of the cortical
accoust1c area to conditioned reflex activity in dogs. Acts,
physiol. hung. 9 no.1-3:163-172 1956.
1. PhysiOlOgiBches Institut der Medizinischen Univeraitat, Pecs.
(RIWIEX, CONDITIONIM
salivary, inhib. eff. of electric stimulation of cerebral
accaustic area in dogs (Ger))
(C)OMRAL VX14TRICLES, physiol.
electric stimulation of accoustic area inhibiting conditioned
salivary reflexes in dogs (Ger))
MOM;.-

RUDICiEROVA, Marie, Inz.
Minimizat-ion of Boolean functior,3, Apl.'kace ma-, 10 no,1-49-
58 ICE5.
1. State Re3earch Institute of' Heavy Current Engineering,
Pragutt 1-11rildcany, Loretanske namesti 3. Submitted December

'
a a it 9 AS Ad A As Al -11--W-~
11 11 ul 11116 0111 "Alin
a a Is AV a _
A L r__A 1 1. 1 . , .1 ~G u- 0 cr . I . & I A 0 .
c
lit ..0 1.0 Coates sea ..a .1. cozies
i R 'Soctills ..0 pec"81113 -Vs.
-ffv L>1 K A
.
PO

0 0 A

ly
*0 vx
4141111 8543
06 FOP-MATION OF l, QUANTA AND OF HEVTRAL MESONS
DURING CAPTURE OF r MESONS BY DEUTERONS. B.
loffe. A. Rudik, and 1. libmushisevich. R#j&
t Ak" Nook-
_
(Init ... i.)
An examination Is nLh& cd Me 3 variants I)) it s n

so n. (2) it # a- - is + a + y, NO (3) d . s' - is - n - A, Asoum.

-
so
LV,LW Me spin of ir
to zero. the scalar and the pseuda-
*
scalar mesons are alone considered. While for the scalar =
o
meow process (1) Is strictly forbidden (the capture being coo

,3 assumed to proceed from (he 3 level), oi the case of the
poeudoscalAr mewA (1) will compete with (2). However. a zoo
00 computation of (1) would present considerAble difficulties

00 ,
since it would require the knowledge of the wave function Aso*
so
411 of the deuteron within the range a( action of nuclear forces.
~ j ", A calculation is made of the probabilities of Of and JJI, coo
using the perturbation tre"ont of the several variants of see
themeson theory at zero-spin particles.
zoo
No$

1:109

xEtALLURfKAL LITERATURE C1.011FKATION
A a 'SL A no*
IF 7,
ON,
411111 net ov, M

A is AV 10 11,; . , . " ; ' .1 .1 ' .1 ' -
It An I I 1 14 0 0 10
0 0 0 0 0 0 * & 0 0 0 0 6 0 0 0 0 00 0 0 giI.
: : : : ------------

RUDIK, A. P.
,USSR/Nuclear Physics Mesons, Neutral Jan 52
"Formation of Gamma-Quanta and Neutral Mesons Dur-
ing Capture of "neg pi.mesons" rc--Mesons by Deu-
terons._I," B. L. Ioffe, A. P. Rudik, I. M. Sh-
mushkevich, Acad Sci USSR
"Zhur~ gksperi Teox:et Fiz" Vol XXII, No 1,pp 11-20
A brief exposition of results of present vork vas
published 'in "Dok Akz Nituk.', SSSR" Vol IMIT, 1951,
403. Calculates the probability of gamma-quanta
formation during capture of 1('~-mesons by deuterons
for various variations of the meson theory of par-
ticles vith zero spin. Considers the capture of
pseudoscalar mesons and the capture of scalar
mesons. Submitted 22 Mar 51.
204T79

RUDIK A. P.
USSR/Nuclear Physics Mesons, Neutral Jan 52
"Formation of Gamma-Quanta and Neutral Mesons Dur-
ing Capture of "neg pi-mesons"rt--Mesons by Deu-
terons. II," B. L. Ioffe, A. P. Rudik and I. M.
Shmushkevich, Acad Sci USSR
"Zhur Eksper i.Teoret Fiz" Vol XXII,No 1, pp 21-28
Calculate the probability~of capture of TI--mesons
by deuterons with the emission of neutral mesons.
Computations are carried out for particles of dif-
ferent evenness with zero spin. Agreement with
exptl data is obtained only in that case where n
and Tt 0 -mesons are pseudoscalar particles. Sub-
mitted 22 Mar 51.
2o4T6o

-and
L. 10fre
4nteraction Of y-me
P
0
.

27-8(1952);,
'A. P. Zhur.. EAjpU. i Teard. Fis. 22, 1
Rudik
'
'
-
d
it
d
f
l
0

R
u
e
or
ers o
magn
.
Zc
tdrce Absir. SOA, 30(1
53)..~-Expt
0
-ged v-, Cap
of cmas sections for the photoproductlon of Chas
byll,andsca"crtngo(85-m.e.v.ir-b H(Also,
ture of r
Could not be
Ahee magnitude of.thc!.rO lifetime -10-11 sce
fitted in lowest order perturbation theory by using pscudo~- W,
Ismlar mesons with -inly one kind of couplin but an gest
udoscalar con ling jIlAc 1 and pseudovedorP/
p
r
C
K. L~
_.
h

Pisinte 2wnieson. %X I.& and Rudik.
KUtio"Jo( ke -7.= -IT- --aS94M(TM"=_
DO Allad. aU S_ . . 82, o. 7,
Chemical Abot, cfTVA. 46,301d~ft has been observed In some cam
of the decompn. of the r-meson that the paths of the #&- -
Vol. 48 No. 3 mesons which am obtained am significantly smaller thin
Feb. 10, 1954 those of the usual 0-mesons. In order to explam,tbe dif-
ferent energies of the Wmesons, it must be assumed that
Nuclear Phenomena the r-meson decomp. to foz. at least 3 particles. TW
simplest assumption is that the r-mesoa decomp. to give a
p-mesen, a neutrino, and a quantum. . The probability of
Ahe occurrence of this process is calcd. on the assurnptions-
that the spin of the r-meson is equal to zero and that the,
spins of the neutrino and of thep-meson are equal to 0.5.
Rovtar Leach
,A
Oman=

h if te

01
~Akad'. Mal
2_-
NvU C~min. NSF-tr-2 9i 4 pp,'(1 254)).
ftwed -as U.S. A L B _2 .4

The priAmbilidis of capture are cateit on the assaimp, too a 5
L

6551bis types of intetacdo"i vector I V) - brusor
71 Ivectbr(A),-dp=T_ud= PS)~ The~itloof
Xl
a
Q
J
~
b
l
jtlC2 of Capture Of 17~meson
Y Ai deuteron %nd
~proba E
a IcOrid essentially b 'th
pr6ton -W
fis sh6w
td i a e
e L
t3
V
off",
abont 0.75 for th
t dA ATiw4
I,Interact n' and to bi
I
T
.
V types. ft
lypes; and about 0.3 toe the Sand - -T eencl
fo
in
da
i
ict
t f th
e
t
on
g the t
e n
u
rm
r
n
e
on is
r
ruin 0
g
e to the type of interact on. Ili'
+ vis
'
E
-V) type the spectrum bas the form of a curve with 2
i
ii~:- the lsl 6 iriarrovier and ties id,the region A neutron.
cnerj~-##r. A- I in 6 IV - in the 2ndj the wIderonc In the
i region of
Be$
~
d.
a4ls f
d t
b
i
ld
t
thi 2 --- ---
oun
con
n
tn
o
e
i
cJU
of ~interatt
on i
'
~
-
he'
;
d-
~
thc
6ne V; nes from
%jenkencd~
an
, lit
elleirgy' :e'
t
0/9
-
"

0 le: I
t
tI
ellerily tr*n results iepott.
,
i

-A

-'s ow t at the captiure or a ~'!-ineson by-am
of
h h -theqx tl.js!uqY
f4m~'~
!d
i th
k
t
r
o
lbj
t
E
bit
h
i
h
~
h
j
f
h
-
s
Lni
vrot
d
e
v;
e
o
a
l
o
l e t
etxet
t,p
w
c
t
are-
cally. adialssible typcg+of lateraction
*
l
,_j_-)
IV I, dn&~'O C43
43 6owil to be-0, It forAT, and PS
a

E
F

A,
SUBJECT USSR / PHYSICS CARD 1 / 2 PA 1895
.AUTHOR IOFFE,B.L., POMERANCUK,I *JA" RUDIK,A.P.
TITLE The Dispersion Relations for th-e-5-okMe-ring of Pions by Deuterons.
PERIODICAL Lrn.eksp.i teor.fis,31,fase.4,712-713 (1956)
Issued: 1 / 1957
The present work investigates the elastic scattering of pions by deuterons with
the scattering angle 0. The dispersion relations which correspond to this pro-
cess differ as follows from the dispersion relations for the scattering of
pions by free nucleons: Firstly, the dispersion relations depend on the polar-
ization of deuterons and secondly, only one single dispersion relation for the
sum of the scattering amplitudes of positive and negative pions is,obtained if
COULOMB'S interaction is neglected.
Let the real- and imaginary parts of the amplitude of the scattering of pions
with the energy co by deuterons whose spin projection onto the direction of the
motion of the pions is equal to m, be denoted by D m(CO) and A m(W) respectively.
By using the connection between the real part of the amplitude of scattering in-
to the angle 0 and the total cross section A M(W) = (k/4n)dm (W ), (where
k2_0J2_e1 2applies and dtk denotes the mass of the meson), the following equation
is obtained by the ordinary method for the determination of dispersion relations:
6"&,,1A (WI)dwl CD WICF (00)dail
2 m 2 2 ~_m
Dm(W) Dm (~a (2k 2 2 + (k /2n 2 2
0 k' (WI t02 (60 1 CA) k

Zurn.ekBp.i teor.fis,~1,fasc-4,712-713 (1956) CARD 2 / 2 PA - 1895
For the determination of the contribution originating from the domain
0 the following expression is used:
_6126
Am(co n T~m M (a) , 'f j, 0 - (k 2AM) _ f2/M]. Here Mm(W I f)
f
denotes that matrix element which corresponds to the capture of a pion by a
deuteron in the state m. with the production of two homogeneous nucleons and;.mo-
mentum. f of the relative motion. This matrix element is explicitly written
downlit differs essentially from zero only in the domain f - k/2. Also the
HAMILTONIAN of the interaction between two nucleons, which is required here,
is written down in a general form without taking tensor forces into account.
The dispersion relations determined by means of this HAMILTONIAN for deute-
rons which are polarized parallel, antiparallel, and vertical to the inciding
bundle are written down. They contain, apart from the constant g, certain
effective values of the potential energy of the interaction between two
nucleons in different states. It is from these effective values that the
amount of the pole term for deuterons which are polarized vertical to the in-
ciding bundle depends essentially.
INSTITUTION:

V.B.) ;M A.P.,,
A.
~%c at. iSc i . USSR
jc) ccir.-servaticin of Pas~-*-%, in. t,.-,e
,
r c
--~r sub, at thke A-U Crinf. on w-
a- di Low
Nl;sr-w, -2! "ov

luviolt
TITU
Pli-RIODICAL
AB-jTRACT
card L/2
RUDIK, Jk.,P.~ 87-5 :)0
The Nonconservation of Parity in the case of Weak Interactions.
(NesoKhranonlya chatnosti v slabykh vz&imoaeystv-iyakhL_ Hussiaii)
Atomnaia Energiia, iY57, Vol 2, Nr 5, pp 463-466,
Hectl_Lwwa 6/-w57 Reviewed 7/1957
I) Theoretical investigations. The author among others makes the fol-
lowing reports - Tne r,4 -4neson can OecayAA accocrdance with the two
schemata At -+ ff+ 0 +
+ Tr . q -+ n+~+ ff+ + n-. in znis conntiction there are
the following two possibilities, tither the X + meson and zric K+
1 2
are two different particlela with the same mass tne same spin, and the
same life, wnien differ as to their interior parities, or these two par-
ticles are the same, and in the case of one of the two reactions men-
t1oned parity is not conserved. The autrior next discusses the possioi-
lities offering tnemselves as &esult of the non-conservation of parity.
A physically well-founaea metrioa or solving the problem of finding out
what laws of conservation apply in the case of weak interactions was
supplied oy LANDAU, L.D., Nuciuar rhysics, Vol 3, p 127 W57). Landau's
ldeas,,also those concerning two-component neutrinos, are discussed.
11) Experimental Results. Quitea short time ago short provisional ac-
counts were given of some experimental work by which the non-conservation
of parity in the case of waek interactions witn participation of a neutrino
was estanlisned. These experiments dealt, among otners, with tne following-
tne angular aistriDution of electrons on the occasion or the P-decay or
polarized nuclei, anZular asymmetry on tne occasion of ff_,ii-e- decay pro-

Tbe Nonconservation of rarlty in wie Case of Weak Interactlon;~.
cesses, the energy dependence u! angular asymmetry in tnv cane or v-
uecay acts, tne po.Larizar,.Lun of electrons on the occasion of P-decay.
All experimental wcjrxo uiscussed here clearly establish the non-conser-
vation of spatial- and charge parity in the case of weaK interactions in
which a neutrino participates. These worKs lead to suppose that, tne
r-uuzrxno Is longitudinal.
(witn 3 jilustrations)
AabvulATION
kRk;bk;NTt;ij B.E
zi UBMITT w 0. 4. -L~;57
AVkILABiz iaorary ef Congress.
Garu 2/2

)L

WMPMMN BELATION9 F(M MONS SCATTERED BY
'12~mtg ~ jl-L~ 1, U, P. M,..Wk,
---- dAUk--�Eqet MIS rrP 4, 688-9(195'1) hUy.
The dispersion relations obtained for the ocattering of
pions bry dauterans ountAln. in addition to the censtant.
.,ertain effective values 4 the potential intprwtlou energy
4 two mucLsons in dlffar-d states, and These values affect
inbstantially the value at the singularity term for deuter-
a", polarized perpendiculs-rly to the I

%
~6
z

Djnt.r!
43"
PO=BLE CMPELATIOM IN 7-9-t DECAY L. Okun'
and A. Ppk.,._ ~*Vltl PhLa. JVrP !, 520- MS57) Ocrt~
vtolated in v, -t decay, there must be carre-
imclamb between the ortentatl(MB of the moment.1 of the,&
masms and the stectrons The resufts of calculaticas of
such aorrelallom are pmeated when parity to vIaLued in
both the - deday and ths jo - a + 2 decay- (L. T.W.)

AUTHOR IOFFE B.L. OKUNI L.B.., RUDIK.A, PA 27o7
TITLE on the Problem of Non-Conservation of Parity in the Case of Intera4tions
(K Yoprosu o nesochramenii chetnosti v slabykh vzairodaystv-iyakh,Russian)
FERIODICAL Zhurnal Eksperis. i Tooret.Fiziki,1957, Vol 32, fir 2, PP 396-397,
Received 5/1957 Reviewed 6/1957
ABSTRACT The authors here show that, proceeding from the conservation of charge
parity, the conclusions are arrived at differ essentially from those
drawn by LEE and YANG. The invariance of the HAMILTONIAN with respeetto
the charge conjugation in the case of different types of interaation leads
to certain phase relations between the cooffiaients. The authors at first
studied the decay Ao - p + ff. If the conservation of parity is not re-
quired, the HAMILTONT-kN of the interaction for this process (if only the
existence of a coupling without derivatioRsis assumed) has the following
forml H - g( ~) p q)A) T tr + iG py5 ~jA TP) 7 4 +iG *( ~,-y5 1*) +
IT rl"T
Here, by the way, the denotations used by FEYNMAN are used. In order that
the HAMILTONIAN be invariant., G and g must be real:
If parity is not conserved, the square of the matrix element of transi-
tion may, besides scalar terms, contain also posudosealar terms. In or-
der to determine whether such paeudoscalar terms exist on the occasion of
Ao -decay, the authors exazine the decay of a polarizedi'2-particle at
rest. The square of the corresponding matrix element is written down ex-
Card 1/2 plicitly. Apparently, the pseudoscalar terms can result only from an in-

On the Problem of Non-Conservation of Parity in the PA 2707
Case of Interactions.

terfereace term. The pseudoscalar terms proportional to Op become
,equal to zero also in the case in which a scalar and a vectorial coup-
ling exists. Also in the case of successive processes Tr- + p -t
M+K0
-
,
1~~p + rr- the paeudosealar terms will be lacking in the differential
probability. It is therefore not possible to determine by measuring the
angular distributiox of the 'protons 'whether parity is hereby conserved
or not. Also on the occasion of P-decay, phenomena may occur which are
connected with the non-conservation of parity. The authors here examine
the P-decaT of a polarized nucleus. Also in the most simple cases of P-
decay, the difference between the possibility of the conservation and
nox-conservation of spatial parity is lacking if the demand for charge
conjugatiox is taken into account.
ASSOCIATION
PRESENTED BY
SUBMITTED 21/11. 1956
AVAILABLE
Card 2/2

!ME=
OMI, L.-,,.RUDIK,
Possible correlations in decav. Zhur. sksp. i teor. fiz.
32 no-31627-628 Mr '57. (KLRA 10:11)
(Illeetrons) (Mesons)
-.A7.-Yt? V,

A. I Rudik
:-E-c:-nted nt 2n-: Ator -for-Feace Conference, ect

M
RUDLK A.F. and TF.N-1-1VL~T1R0SYA1-, K.A.
B. L.
(Ac-ad. Sci. U00JR)
-Decray and NOn-Conservation of Parity," Nuclear PhYS-ics, V 1- 5, 110- 3)
Feb 195" (110. flclLn_zid' 1~ubl. Co.,
Al)otl: ~~uc! 1.0n--,-,.,nservaUt,,jn of vm-it,: ou-il no
-,-v. i.'e'a I'In Cj , ": - -
angular dis'ribuli
4, on of /-elecktruns from, an oriented
1111CLeus (includiiirr the case when the direction of Ule recoil nucleus mc)r;v_,ntum is
are oxamin2d in ti,c -~:.rescnt -paper for tbe cases ol allowed if,' -transitions and
4-rasit ions. It is shown that owing to 'he iffluence of the
Ct~uj.Qmb, field tile of these effects for forbidden transitiors in heavy
anu, Intermedliate neulei is the smae as for allowed transitions, -erceT,tible de-
viations are obst--rved in light nuclei C_ 20). In the -particular case o-f a
(~-O transition Comlzrison with exj~eriment nay T-eld,ii-mortant data on the contribution
',')f PSeUdOSCalal' COUlAil1g. Unique transitions (.4 2,yes) for which the el&ctron.
angul.a.- disti-ibut-ion o' orierted nuclei es3!mtiall" differs that for sllove5
7m

AUTHO-i,:! B., RUj 4
TITLE: The Polarization of the Internal Conversion Electrons
Following a P-Decay (PoLyarizat2iya elektroriov vnutvenney
korivernii, fil ed iiyu.,;hc hey ;,,tt 13- raoqpatl olli)
PERIODICAL: Zhurnal ekspurimentallnoy i teoreticheskoy fiziki, 1958,
Vol 35, Nr 1, PP 159 - -164 (USSR)
,kBSTRA.CT: The authors in the present paper investigate the
connection bet-..,een the uolarization of the conversion
electrons and the direction of tile electrons emitted
during a P-decay. The Coulomb-(Kulon) field of the
nucleus is ne.-lected in thic connection. For the (axi--11)
vector of the polarization of the conversion electrons
the following ansatz is made (for the case of permitted
P-transitions) : ' = a(-v"'n')A + b('v
\0 /
(a and b are constants which depend on the momenta of the
nuclear state and the transition energy, ev is the velocity
of P-electrons, and n the unit vector in the direction
of the conversion transitions). For the case of a magnetic
Card 1/3 multipole the following is obtained:

The Polarization of the Internall Convernion Electrons SOV/c"-35-1-22/59
/ tj
0110'...'ing a -ay
F Dec
(r 51j 2)1(~7~)' In this case the polarization is
longitudinal and does not depend on the energy of the
conversion electron. The folio-aing holds for the case
of an electric multi-pole:
2
L + 1 5 (K_ + ~q2 VO M
r 1 +21c (2L+1)/'L J2 n n4)-,V)4-L. (nv
(F_ -?n) As
r EL(L,-l)+j 202 +1) - J101 +1 0 /2L(L+ 1 1) .In this.case
a lon,--itudinal as %,.,ell as a transversal polarization exist,
both Fein& dependent on energy. At low velocities,
v. of the conversion electrons longitudinal polarization
i_- orooortional (v,_/c)4, and transversal polarization
V(v,/c). In conclusion the authors thank A.I.Alikhanov,
Academician, and V.I.L,,,rubimov for the interest they
disDlayed and for their discussions, T"--~ere are 3 refer--
ences, 2 of -ahich are Soviet.
Card 2/3

21(l.8); 24(5) PIWE I BOOK MLIDIT&TICN SCV/3369
Vsssoyu=ay =*zhvuzov3kfty't konferantaiya po kvantovOy tooril poley
-
elementarnywh chlatits. Uzhgorods 1958
1 tooril
Problemy savr t crit clementarnykh chaxtits. No. 2: Trudy
ITen'"'04=
or Elementary
or
Th
i

e
y
. t
1em,
konforents I he Modern
PLrti4l*g. i;: 2, Transactions of =e All-UnLon Inter-Vuz
Conference on the -2%zarltum Field Theory an4 the Theory of
kxrp&t3koyc oblastnoye lzd.vo,
z
14
2
~
ngar,
,
Zleclenta Particle$) Uz
1
. 5... copies printed.
1959. 21
Ed.: Yu. Lomsadzes Docent'. Tech. 94.1 X. BelcuG.
PMOSIS nag book is intended ror physicists. particularly those
concerned with problem3 In trio field of elelzentary particles and
the quantum theory.
C0V1WAGX& This book contains articles on elementary P-rtloles
origimally read at the All-UnIon Tnter-vuz conrerence held at
UxhjOrOd 3tato UnIveratty on October 20, 1956. Among the topics
_
ld theory, the :us.4cn theory,
discussed are: the spinar fl
14rentz contractions, parity tudl~*, nucleon-nucleon scattering.
:

h article. Hererenoes
;II 'h abstracts accompany eac
ate. %
h Article,
i
follow
,
ew Formulation or Fusion Theory 26

a
lama dze Yu.X,, and 5-1 -KX41L'~- A111114tion of
Ibwingerl a VArlat16-n-Mithod to the Pair Theory 30
Sokollk, G.A. Generalization of the "-tntz Group 37
"I:nltg~4Y~.' 0..!- 0encrall-.ed Equivalent potentle, and
9 a equence Of InfinitoplOji Lorentz Controctl~nA Unde
r
Rotary notion 44
S0kOl1k, G.A. Representation or the Complete Lorentz Gnoup 52
30k l1k. G.A. Connection Between the -Ano..&I-
0 Representation
or
the 3PAce-Ttale Inversion Group AYXI the PILUIL Tranarormatlons 5&
-020"kenbty", A-V-A A and A.?. RudLk
Von-ConservWfion or PaLrIty In R39
58
RLl9n'kI7-!-M- and R.N. kndln. Determination or PArity
d"tr"go Firticies-
63
loomsaeizo Yu-N, The Possible Versions or tile jr
;
1,90"y Th
'OrY 1 69
1quAtIons or the St-cna Order for Spinor
-VILYO Functions
so
0
C naervatton of the Combined Pgrity, as a
r the Symmetry In Nature 83
G#Shkenboyn, B.V. P-14rizatlon or z1octrong or the Inner
C-Onvorsion Subsequent to JS -- Deasy. Taking Into Account
the Kl"Otric Field of the Nucleus
89
.1 LtOnk0a A.G. Polarization or the Nucleons Under the
_
35i1_PW5a-XdMIon in the High Mn-rgy Region 99
n~glaSs~Kh- see RqUatlons for Liomentary particles
log
Barambankov; V.3., and B'X
t_LLrj,AahOV. r 30M. Remarks on the
_
Inner 3tructure of the Nucleon 117
On the SUPerrItLid 3t&t* Of an Atom Nucl
eus

21(8),24(5)
MHORS: Geshkenbeyn, 3. V,, SOV/56-36-2-26/63
Nemirovskaya, S. A.,_Rudik,.,.A._Yj
TITLE; The Polarization of the /3-Electrons From RaE (Polyarizatsiya
/3-elektronov RaE)
PERIODICAL: Zhurnal eksperiment0noy i teoreticheskoy fiziki, 1959,
Vol 36, Ur 2, PP 517-525 (USSR)
A13STRACT: After the nonconservation of spatial parity hed become known,
the /3-decay of RaE was investigrted by several reseprch
scientists. Lewis (Lyuis)(Ref 1), FujitR (Fuzhita) et al.,
(Ref 2) also pointed out the possible nonconservation of time
parity, and Alikhanov showed by experiment (Ref 3) that the
longitudinal polarization of/3 -electrons from RPE deviates
from v/c and !hat the degree of devintion charecterizes the
measure of the nonconservation of parity with respect to time.
Also in the present paper the authors derive a formula for the
longitu4innl polarization of the /3-electrons, viz. for S- and
T- interaction as well as for V-A - interaction,.basing upon
the results of references 7 and B. NumericrL1 results are given
Cerd 1A by a number of tables. Thus; table I shows (6) /(v/c) for

The Polarization of the /3-Electrons Frorm RaE SoVe/56-36-2-26/63
3- nnfl T- interpction and tnble 2 shows the same for Y-A at
r = 1-17-10- 13. Tables 5 and 6 show W /(v/c) at
F . 6.10 "'(V-A), figure 7 shows /(v/c) for 3- and T- inter-.
action types for various F values. The experimentsl data
relating to the magnitude of the polsirizntion of the RaE
/3-electrons considerably restrict the region of a possible
violation of time parity. VA-interaction type: In the case of
nonconservation of time parity the measured extremal polariza-
ticn excludes F < 0 at F2 = 6.io-3 and p2 = 3.10 3. For F > 0
experimental and theoretical results Pgroe for
x -- 0.2(F2=6.10-3) or 0.7(F2 =3.10-3).
ST-interpetion type: At F2 = 6.10-3 and F2 = 3.1o-3 F < o is
excluded and at F > 0 agreement is found for any such F2 values
within the rpnge of x, - 1.7.
The authors finAlly thAnk Academician.k. I. Alikhnnov for
Card 2/3

Thelblarization of the /3 -Flectrons From RaE SOV/56-36-2-26/63
suggesting this work and for his discussions, nnd they Plso
thank B. L. Ioffe and V. A. Lyubimov for discussions, There
are 9 tables and 12 references, 01 of which are Soviet,
SUBMITTED: July 24, 1958 (initially) and October 28, 1958 (after revision)
Card 3/3

85697
S/056/60/038/006/040/049/Xx
B006/BO70
AUTHORS: Geshkenbeyn, B. V., Rudik, A. P.,
TITI.E-, The Relationship Between the Polarization of (3-Blectrons.and
the Form of the P-Spectrum
PERIODICAL: Zhurnal eksperimentallnoy i teoreticheskoy fiziki, 1960,
Vol. 38; No, 6, pp~ 1894 - 1895
TEXT: The coefficient of the form of the P-spectrum is given by
C(W) =7-M.(Z'W)fi(W,X); and the longitudinal polarization of P-electrons is
given by Mi(Z,W)f i(W,X)ai(Z,W)/L Mi(Z,W)f i(WX) ~ (Z - atomic
c i i .
number of the nucleus; W and v - energy and velocity, respectively, of
P-electrons; X - nuclear matrix elements; Mi and ai - complex functions
describing the motion of the electrons in the Coulomb field of the daughter
nucleus, the function f. depends on the electron energy and the matrix
elements), Both these formulas are briefly discussed in the present papers
Card 1/2

0
The Relationship Between the Polarization of S/05'/60/038/006/040/040AX
P-Eleotrons and the Form of the P-Spectrum B006/BO70
It is pointed out that for Fermi form of the spectrum, the polarization of
A-electrons is practically coincident with v/c~. As, however, first forbid;.
den P-decays are also known where the longitudiral polarization of
_
e' ectrons
L is essentially different from v/c, the spectrum ~s not of Fermi
type. In this connection the classical example of RaE (17--->.O )IS-decay is
discussed.. The P-decay of Au'98 (27--.>-2.+) is also discussed, for which the
longitudinal polarization of Velectrons is widely divergent from V/C for
small energies (according to data of A. 1. klikhanov et al.,). For high
energieB it is equal to v/c, These deviations are expla I'ned by a eviation
32 k
of the spectrum from the Fermi form., The cases for P nd-ln,-'''are
analogous (see L; A., Mikaelyan and P. Yp,, Spivak). Academician
A, 1. Alikha and V.. A. are thanked for their interest in the
ub imoy
.~Kh n
work., There are 10 referencess 6 Soviet. 3 US, and 1 Canadian~
SUBMITTED- February 15, !960
Card 2/2

KOLKM;OV, V.A.; OKWII, L.B., RUDIX, A.P.; SUDAKOV, V.V.
Position of the nearest singularities of the 7~11--scattering
amplitude. Zhur. eksp. i teor. fiz. 39 no.2:340-344 Ag 160.
(MIRA 13:9)
(Field theory) (Scattering (Ph7sics))

OKMII, L.B.; RUDIK, A.P._
X+2Y-deca7 and magnetic moment of the ZO-h7peron.
Zhur. eksp. i teor. fiz. 39 no.2:378-383 Ag 160. MU 13:9)
(Mesons-Deca7)

KOIZUNOV, Y.A.; OKUHI, L.B.; RUDIK, A.P.
Singularities of some Feynmn di&Vams. Zhur.ekop.i teor.
fil. 38 no-3:877-881 Mr 160. (MM 13:7)
(Collisions(Muclear physics))

GESEMBEnT, B.V~.; RUDIX, A.P.
Connection between the polarization of,,g-electrons and the form of
the,,S spectrum. Zhur.eksp.i teor.fiz- 38 no.6:1894-1895 Je
16o. (MIRA 13:7)
(Slectrons)
(Beta rays)
(Decay, Radioactive)

84963
S/056j6O/O79/003/049/056/71
B006/Bo-!o
4-
6
AUTHORS; Olk-in L~ B,,,, Rudik, A.. P.
TITLE: Th-~ D= -,aye K' --~ n' 4 e i e ard K' I + i p
PERIODICAL: Zy~'-'Mal P-k2P9rim9Etal'nc7 leor~ttichesk:~y f,4 zlki~ 1960,
"
o". 39,
j No. 3(g), pp. 600 604
TEXT: A "her-r-,i-al at,,ady of the decayrea-~-+_,llons'(2).- KI n" ~- e + e
and (3): K' -~ Ti 4 1.,; made tn thls paper. The~Ee rea.-lions have
nr~t y-zt been observed, they are- not absolutely forbidden !n the
r,~alm rf '.hs, pres-irt-day 4.h-?or.;,--s csnn._%~ te due 11-o weak intera-.fiora
alc,ne. The authcra s'l-)w that bc~lh thea,~ zeactions may be due to th~_ Com---
bined weak leptcn -Interactior. and electrc~magnetic interaction and nan be
I llust.ratad by -,he Feynman graph of. Fig. 1 . The dotted llne represer ts a
virtual photo-r-2 and the full c~irvle of the graph
shrews a K-de,iay irto.picn gamma quar!,~um. Sunh a
graph -Is sh,~wn. in Fig. 2.
G")
Fig,

84963
The Decays K +
S e ani
S/056/60/039/003/1049/or8/XX
Boc)6/Br,7n
K
K The decays (2' and are aaa!ogou.a ti th~' known 0 - 0
soaversicn tra"ritions -4n nuziil. Th= mat,:r'-x
the graph (Fig. 1) -.,:7, formula-lsd s5
P K n
M - ?fGk 2 'u
U ~ V4-n-IaGPu'
l
whore
p
2 p
p
T
K
p k
2
a - e o
1; vi are spin--ra t~f the Iap',Ort
It e or ar- a-re the wavs, funct!cns ct
1 1P
Y K .
(Fig. 2) K ~- and n fields, G is the weak- lnt~-ra,--tlon Inonstan~
2 4 4a the 7erlex
(G-10" w p , rr'. P "protor~ mass)" p
Palltl (f-;l! :3'Lvels) cf th e graph (Ftg. 1); f i.3 a~ i4menzionleass fun.-,ticm,
2 2
f k k 2 2
ID
t, Ir - ?E w and As ~o
naidered tr lc~ ocrztant. The tonal
Y
r-robatilit .ies four T-he fir-,;ay-q (2) ard (3) are fojnd 4-.o be W
- 0.56 W
.
r

InA W 0

w G T, 5
w 6 2

. To 1 w f
re W t6 ,he

Carl ?/4

84963
The Decays X+ -4 n+ +*e+ e' and S10561601039100310491058X
K+ + + + + Boo6pO70
probabi ity of -v decay. From the number of the observed T decays in
which n single decay of the type (3) was found, it is concluded that
2
-4. The relative probability, however, does not depend on f2
f 5- 0
e 0.2. In the following, the authors discuss the calculation of
W ~'V
electron, and muon spectra for.the decays (2) and 3). The
resuitsia-re given by formulas (9) and (10), and (12),and (13~, respec-
tively'land are illustrated in Figs. 3 and'4, respectively. The authors
thank Lj D. Landau and I. Yu. Kobzarev for discussions, S. A. Nemirov-
skiy fot numerical calculations, and Ye. D. Zh:Lzhin for pointing o7it an
error. here are 6 figures and 2 references: 1 Soviet and I US.
SUBMITTED: March 1960

7111
910) PRASS 1 5009 ZXPL0ITATrCN SOV/2583

International Conference on the PaaetrUl Used or Atomic Engtrgy.
,.2nd, Gonave, 1958.
bokladY sovetskikh uchsnykh; 7%dornyye reaktory I yadernnya aner.
gettka. (Repo rts or Soviet scientists*. Nuclear Reactors and
Nuclear Power) MOSCOW* Atomi.-dat, 1959. 707 p. (Serleat Ttat
-TrQdY, vol. 2) Xrrata slip Inserted. 8,000 copies printed. %_j
Ooneral Ida.i N.A. Dollethale Corresponding Member, USSR Academy or
3clancess A.X. Kroatno Doctor or Pnysicat and Mathematical Sciences,
A.1
Le unakly, Member* Ukrainian SSR Academy or Science&, I.I.
p __ T
i
Nov knvf
Corresponding Member# U33H Academy of Sciences, and V.3.
ftroov, Doctor or PhyalO&I and Mathematical Sclonood; H4. t A.?.
AlYablyevi Tech. Sd.t To. I. Mazall.

PM MSK: This book Is Intended for scientists and engineers engaged
in reactor designing, an well an for proreasors and stUdento Of
higher technical schools where reactor design to taught.
_C_0VZRAUXz This IsO* seemed values of . wi-volume oall-tion , as the _P- N'
-
use or
aronac energy. The six volumes contain the reports pp..
sent*d by Soviet scientists at the Second International Conf.rem-4
an Peaceful Uses Of Atomic RnerW, hold from September I to 13
,
1958 In 0oneva. volume 2 consists or three Parts. The first to
devoted to atomic Power Plants under construction In the Soviet
Unlon;-tnt second to exPerIzental and research reactors, the ox-
POPiments carried out on the., and the work to Improve them, and
the third, which I* p"dominantly thcoratIO&I, to problems Or
nuclear reactor physics and construction a"Ineoring. Yu. 1.
ROrYakin Is the science, editor or this volume. see soV/2081
for title@ or all Volumes or the set. References appear at the
OA4. of, the articles.
Nostovoy, v.1., V.S. Dikarev, M.B. Yogtzarov. and Tu. S. Saltykov.
Neutron spectra In Uranium Water Litttc*s (Report
In
Aau
r
,,, 5"
::
2
j
Xraalns A.K.. B.O. Dubovskly, R.N. Lanteov, TU.Tu. Glazkova

.K, Goncharov, A.V. Kamayevs L.A. Goraneva, V.V. VayllOv,
'
t
.. 1. Inrutln, and A.P. Senchonkov. Studying the Physical
I
Characteristics or it Beryl I ium~oderator Reactor (Report No.
21k6) 555
Golanln, A.D., S.A. Naaarovskaya, _A.P. RuAlk, Yu. 0. Abov, V.P.
Balkin# and P.A. KrupchItakly. CritTc-&17Yx
e ~Tment on an Zxporl-
"ntal Heavy-water Reactor (Report No. 203b 570
y
KLrchuR, 0.1., V. To. Pupko, To. 1. ?OgUdALLna, V.V. Smaloy,
I.P. Tyutorev, S.T. Platonova, and 0.1. DruzhIntnA. Certain Pro-
bless in Nuclear Reactor Physics and Methods or Calculating
Then (Report No. 2L 51) 588
3l.nyutin~ O.V, and V.N. 3amenov. Determination or Control Rod
1froctIveneon In it Cylindrical Reactor (Report No. 2469) 613
Gollrand, I.M.s S.M. Paynberg, A.S. Prolov. and X.N. Chentsov.
Using the Monte Carlo Method or Random Sampling for Solving the
JUnttla Squation (Report No. 2141) 628
.L&Ietins W.I. Neutron Distribution in a notorog*neous Medium
(Report No. 2189) 634
Kazarnovokly, N.V. A.V. anov, and P.L. Shapiro. N utron
Step
t
Therimalixation and
Dirruslon In Heavy X.d1A (Report No. 21-46) 651
Voynlk, A.I- V.S. Tormakovo and A.V. Lykav. Doing the Onsager
Theory ror Studying Woutran Dirrunton In the Absorbing Media or
clear Reactors (Report No. 2224) "8
Broder, D.L., S.A. Kurkln, A.A. lastu2ov, V.V. Levin, and
V.V. orlov. Studying the spatial and Knor
y Distribution or
g
Neutrons in Difrorent Media (Report No. 21 7) 674
Dwitrlyev A 0 Boron lonixatton Chambers for Work In Nuclear
*actors JR~;P;t No. 2084) 69o
Re
ionr
rillin. V.A., and S.A. Ulybin. Kxporlsaontal. Dater.Inat or
Specific Volumes or Heavy Water in a Wide Temperature and Pro-
L
j
sure Hang* (RapertINo. 24TI) 696

T I T K
"On the Possible Strong InterAction of the Intermediate Boson"
paper presented at the Intl Conference on High Energy Physics, Rochester, N.Y.
and/or Berkly California, 25 Aug - 16 Sep 1960.
Joint Inst. fc-- Nuclear Resersh, Dubna, USSR

RTjD1K, Aleksay P.
,"-Investigation of Chev~_Mandelstam Equations"
"Singular Points in Scattering Amplitude"
"Scattering of Particles of Super-High Energies"
"Asymptotic Behaviour of Kffective Gross Sections at High Lnergies"
paper presented at the Intl Conference on High Energr Physics, Rochester,, N.Y.
and/or Berkly California, 25 Agg-16 Sep 1960.
Joint Inst. for Nuclear Reserch, Dubna, USM

89222
B/05 61/040/001/028/03T
0 B102YB212
AUTHORSt Patashinskiy, A.Z., _Rudik, A. P., Sudakov, V. V.
TITLEI Singuliritibs3 of scattering amplitudes in the perturbation
theory.
PERIODICALi Zhurnal eksperimentallnoy i teoreticheskoy fizikit V. 40,
no. 1, 1961, 298-311
TEXTs A study has been.made of the position of singularities of the
scattering amplitude and its asymptotic behavior in the perturbation
theory. Due to conservation of the four-momentum of seattered particles,
the four-momenta of the scattering and virtual particles are located in a'
three-dimensional space for any perturbation-theoretical graph. The three
linearly independent four-vectors are chosen for basis vectorst W
P1+P2
2 2
p +p P p +P For M (1.1,-.4)
39 1 4* Pi i
2QW MI, M2, M,3 + M,3, 2WP=M2-M2+
2 M2 - M"I
1 3,
Is. (1.2) holds.
2QP =.M2
I + M2 - MI2 - M121: Q2 + W2 + P, M'2 + M., + M, + A,
3
Card 1/5

89222
8/056/61/040/001/028/037
B102/B212
Singulirities of scattering...
The scattering amplitude is characterized by six arametersj for con-
p
2 2 2
venience they are chosen to bes M and the invariants W and 0. Only the
singularities with real invariants are considered. There is a certain
2 2
relation between W and the masses of the virtual particles at the
singularity; this relation is ch racterized for graphs of the type shown
in Fig.1 by the ratios between and the squares of masses of virtual
V3
'
articles. Fi&;2 shows some singular curves of this
4_
graph.
'The authors thenwanted to find out under what conditions
anomalous singularities do occur for more complicated (than
Fig.1) graphs of perturbation theory. An analysis is made ~7
for an asymptotic case, *here one invarint approaches

Z
-infinity. The condition that
2 Q2)1 < IW (co )I holds as a
F 1W
Fig.1 criterion for the anomalous type of singular curves. First
of all the singularities of the "open envelope" type graph (Fig-3) are
studied and:the asymptotic behavior of the position of its singularities
is studied for one of the invariants approaching infinity. It can be shown
Card 2/5

Singularities of scattering...
89222
S/056/61/040/001/028/037
3102/B212
1F, that the singular curve of the "open envelope" has several
.3 ~)
branches, two in the general case. The two possibilities
x