SCIENTIFIC ABSTRACT KRESTINSKAYA, V. N. - KRESTNIKOV, YU. S.

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• Collection: Scientific Abstracts
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• Document Creation Date: January 3, 2017
• Document Release Date: July 31, 2000
• Sequence Number: 3
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

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KM.STIIJSY.'iYAJ, V. N.
0
"Tho Mechanism of the Adoorption of Silver SulphAte on Soln of "ilicia and Acid Of
Aluminium I~rdroxide." KrestinskMa, V. N., and Hakimov, Z. V. (p. 129)
SO: J.aurnal of General Chemistry (Zhurnal Obshchei Mimli) 1944., Volume 14, no- 3-

KRESTINSKAYA, V. N. i SHATFMIROV, K. SP.
,W429. Peptiziruyushcheye delstvlye k1slot Bhchelochey I soley na
kolloidy karbonatinikh pochv kirpizii. Trudi Khim in-Ta. (K:LrFlz
Filial Akad. flauk SSSR.) Vyp. 2v 194? (izd: 1948) S. 3-16-PibIlopr: 19 Nazv.

n- - - z 171 NS F A Y it I IV . 17" 1
h2CF0, KFEMNSKAYA, V.N., PELOVA, 0.1.-Adsorbtsiya ionov vert.9a i tsJn~i na zolyakh
gidratopektina i pektinovoy kisloty. Trudy khim. in-'s (Kirgiz, f'jlial Akcad.
nauk SSSP), vyp. 2, 190 Uzds 19hf.), a. 29-35'.-I'Ablioir: 10 nazv.
So: Setopist Zhurnallnykh STatey, Vol. h7, 19h8

KRIISTINSKAYA, V.N.; BBWVA, 0.1.
. .:: . -: 7,-
Hydrophobization of pectin substances of sugar beat. izvest. Kirgiz. Filial.
Akad. Vauk S.S.S.R. '47, No.7, 139-46. Off-H A 5: 10)
I (CA 47 no.22:12472 '53)

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drelove I KlIghis map 11 IRM" It I In Wor; %&lloo of -N"(I% Which AM 24 slabdl&t.
OWN, Lit
har 0 No. 1. 43 IT a' thif a Got' into
t I , I is'. -6211941 .-The oil Is. "t letter is 10" dLWMd, thlin
"WPO",
i "UiM6 was to elucidate glive di bet &Y- the dMit. sold its Mob. lMpUt h Age to .*is
the Pilot
trandennex
a drophilic and hydrophobic coll" sort Ion it* MiCilles. Furttm addns. of 1171 .4!L I dissom
III (mir Into the othrt W. C A m 7W). Tlw ad studic"I 01 Hs&()* still Inorv and tht'vLy enhanm this hydiroqihil~ *00
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The pptd. S was peptisad with distd. WO. tlw miloid and %ttains its mail. stawlity. IICI addrd Imyund .46
*14 neutralised to litmus with NAHM SHOW. 9M this Point acts as c,moulant. TV pit values at d1tratc, -
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t 111"m III Me 4 IlCJ were del.l. In 4mder to test whether 110 040
the I(A) was chsnpd flvqucnlly until Im of polyt - qua
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in. `4111110
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11 11
i"I'SKAY A,V.iv.
h2081. KPESTIN,tzKXYA, V.N., KONDFAF, P.A.-Isaledovaniye kbJ.loidnykh rastvorov vollfrarro-
voy kisloty v stntemt vollframat natriyarodanid ammotiiya-sernaya kislota. Trudy
khim. in-ta (kLrgiz. filial Akad, nauk. --S,)R), vyp. 2) 190 (izd: 19bl), s- 65-93-
FA bliopr: 8 nazv.
Soi Setopis' Zhurnallnykh Statey, Vol. 47, 19h8

r1#
Admervel" *I aban metal amol alkame garth WOW Ifte
by a tolino" OMMOM of Aulfar dwiNg Its telgilititm.
V. N. bralmdeare and N- (1, Abdullina (KIFIfix Hmneh,
Aml. U.S.S.R.). KPII#W. Zhur. 13. 20-97(1961).-
lisfin vWs lam coagulated by aLks. and tbo amt. It of the
tx lating cution wharted by the ppt. wrA dctd. The
a 7= * * Was W-W% of the amt. *quiv. to the .14
-lablusing the vol. for Call It wall M%, Me*,
Co I KT%. Rh 1'17~6. K * 0%, Na 1 41%. itall 1.1 1 WHW
M "AUIA11111 COIWII. W&A AbOUt 0.01 E. eQUIT./lAW44.
IlaC4 and C&M. 0.2) for ArCh. 0.073 for CoCi arul Rb-
N09. 0 10 for KCI, O-XI (or -N&CI, amt 6A for LICI. As
ilm wil"s of the ions Im a awl for ~ivdation do not agy"
dild so d to &I'mawl mwk Irse than II0%, 11W exch"Re all.
olwislilml Won" fit barol OmwNiltry il"tKorlAnev In 41W et"Ou.
durille Completion. it.

,iLk
Itemoval
i. I; I i~lildl
coctxm
.I jK
S7.,' d. f;L.
"nz =fact at
1" P"A frot"
C~.A
2-r, h, Such I Ilanthy
Own temp. or than llg0-
tow silk tnom

The role of amino Wds in tho solution which ripmoves
cefesine from raw SQ- V. N KrestinAArA mid Nf H
m,do 7r; _T7XV
lmukha va. Zhur. 746 j~F-fj -- Applied
'hem. I I S. S. R. ) 24. 1 ZA IN1.14 MIA 1: cf. thid W1 I -The
Wy.ed -iin _,IX. --ine h'.1 ... 1-i. 1-1.
cf% 14 active In the rcturival tit err"ne from ulk Ilem,
true soln. or irty highly (Inlivi,te mAte of itit, mii%v ni.,~
erial Is respon-jible for the vffrct. Amino acidi Are not thr
active material since the most active solni. ILive the low-,
~
AroinO " content. Concri. of soln. increaws activity
and the content of polylieptides. but the amino acid content
droo to nearly zero. On ~t.tnding the activity drops and
polypepticle concn. drops while th.it of amino mids rimt,,;
the same occurs on boilins. C, M. K"'kooff

At
Clietnicst wn nr ,*I'
In,
by
."rl
.,,b
clivity Abluty
to rema",
f,,
firm. In A Rr"t tllr~l bl~ the
re fkh in amirin =,j
Oatc.
t%"'I'uy ..- !- -A .%,.
shl

heMICal COMPO;ition of the ilibl(I ~Zer of serldn.
timk
Chemical Abst. 1. 46, 96,38j,
Vol. 48 No. 9
May 10f 1954
Biological Chemistry

1 4:2.

-'2 21

MM/ Scientists - Commemoiation
Card -1/1 Piib. 3.24 - 34/39
Authors t Krestinskiyj Yu, A.
Title years since the death of A. N. Tolatoi
Periodical 1 Vest. AN SSSR 25/5, 98 - 99, May 1955
Abstract I An account is given of a special session held by the A. H. Gor1V Institute
of World Literature of the Academy of Science on February 18th. The ses-
sion-oo=emorated the 10th anniversary since the death of A. N. Tolstoiq
Soviet writer and'aaademician. Papers were read recalling his life his-
tory.
Institution
Submitted t *seam

XRI~SMYIII Me. (w3kyl)
Two fatal complications in a woman treated with cortico-
steroids. Klin. zed. 40 no.12:111-113 D 162.
(MIRA 17:2)
1. Iz GorodaRoy infaktsionnoy klinichaskoy bollnitay No.7
(glavnyy vrach N.G. Zaleskver).

KRE5TNIKGV, A.M., inzh.
Pneumatic transportation of
Je 161.
(Kuybyohov--Aggregates
kerammit. Stroi.mat. 7 no.6:28
OURA 14;7)
(Building materials)-Transportation)

KHUKHROV, I.; KIESTNIKOV, I.
From practices in the utilization of power presses for lard
crackling pressing. Mias.indeSSSR 33 no.2:41-42 162. (MIPA 15:5)
1. lAningradskiy nVasokombinat.
(Lard)

MITROFANOV, Yuriy Mikhaylovich. Prinimali uchastiye: SHISHKOV,
V.N., inzh.; KRESTNIKOVj I.L., inzh.; IVAIJOVSKAYA, K.M.,
red.; DODANOVA, A.P., tekhn. red.
(Reinforced concrete sectional spans] ZhelezobetonrVe chlerten-
nye proletnye stroeniia. Moskva, Avtotransizdat, 1963. 55 P.
(MIRA 17:4)

ABRI"OV9 B.D., insh.; KRESTNIKOV I L inzh.; HIMN, NjI.,, inzh;.-,
KUREBAVA
Constructing pile foundations using 0.6m precast reinforced
concrete ahells. Transp. stroi. 3.1 no.l'U-13 J& 161.
I .. (KLPA 14t1)
(Ural River-Bridges-4pundations and piers)

MITRCFLNGV., Yu.M.; POLYEVKO., V.P*-; IMESTNIKOV, I.L.
Laying span structures by pushing without temporary supports.
Avt.dor. 25 no*7:8-10 JI 162. (IMIU 15:8)
(Bridge construction)

.7 ..r .i'. " , -, - -':
. -0. . -
US~,R/,.:cd-ic--'ne - -77piile.,-iology
!',edicizie - Epizaotic Diseases
jL~l '14-
"'Ll-le Use of 'Czechoslowkian Holes' for the DisNsal o1' Infcxtious Anii,,lal L"orpses,"
Prof ". A. Pcj~ia~ov, Dr Vet. Sci, 1% V. Krestnikov, Engr, 2p-
I'Velucrinariyall No 7
Fk 31/49TH

31
USSR/Medicine Vaterinary Medicine Aug 48
Medicine Hospitals) Administration
and OrgAnization
*Building of Veterinary-Medical Institutions,"
N. V. Krestnikov, Engr, 4-1 pp
4
*7eterlnarlya" No 8
Describes project for typical rayon veterinary
hospital. Includes ward for ambulatory patients,
noninfectious ward, Isolation ward, washing and
dryLng rooms, gas chamber, and smithy. Article
contains five plane.
Im... .. _. 31/49T96

KILLiTNIKOV) S. V. PA2,7T37
Fab
Voltage Regulators
Transformers
"variations In Transformer Efficiency during Vol-
tage Regulation of Theater-Type Autotransformer., of
S. V. &eetnikov.* Nagrp GosteaSvet Worlm, 3 pp
*Vast Zlektro-Prae No 2
Describes changes in transformer efficiency of
regulated theatrical autotransformer during the ad-
justment of voltage by sliding contact system.
Transformer operating at -4raw efficiency vhan the
contact placed at tap 4/5 of the total turns of the
coil, at vhIob time transformer diselpation Is equal
t0'9.8% of nall"I capacity of Imps U the clz=it.

UM/Elactricity - Tftnsforwars A-ag 51
Voltage Regulation
"Gostesevet" Plant
"Autatransformers.With Continuous Voltage ReguIA-
tions," A. B. Podollner, S. V' Krestnl3wy,
Ingineers, G.-K. Aladzhalov, V: P. Krylov, S. G.
Pelldmftn, "Gosteasvet" Plant, Moscow
"Elektrichestvo" No 8, pp 26-30
Describes series of autotransformers which pro-
vide continuous voltage regulation under load,
and gives principles underlying'their design.
196M
USSR/Electricity - Tr-aformers (Contd) Aug 51
These transformers were designed and put Into
series production by the "Gosteasvet" plant.
Submitted 9 Dec 50-
196T25

KRP MIKOVP V. N.
SEE ALSO: "HIM'ScTolpiliKov) V. N.

MESTNIKO': N.
PA ~2TD
UM/00010gr Oct 1947
Geological Prospecting
"Arkosic Sandstone in the Hoadvaters of the Alzan'
and Storl Rivers'," V. ff. &estnikov, 2j pp
*Dok And Wauk MM" Vol LVIII, No 1
Discussion of formatIon of sandstone In this area.
Two auto show: 1) mudcovite A, blotite 1%, quartz
27%, microoline-43%, plagloclase 20%, calcite 6%;
2) muscovite 5%, quartz 51%, miorooline 43%, Plagio-
clase 8%. Sibmitted by Academician D. S. Belyankin,
22 Mar 1947.,
41M
52T33

KRF-57NIKOV) V. N.
117he Stratigraphy of the Devonian Deposits on the 1.'estern Slope of the
Urals," Byul. Mork. Obshch. Iapytat, Pr1rody, Otdol. Gool., 53) 110.6) 1948.

Y,%E.S5TN'JY,0'1) V. N.
"The IIistor7 of the Geological Development of the Eastern Caucasun in the
ReCion of the Tushet Intersection, 11 Iz. Ak. INauk SSSR. Ser. geol.., 2, 1949

y ~' I-T A.T.- 'I.
Ca!,c,ijus
Comrarison of the seisilcity and structure of 'F,~st Centrpl Caucasus. Dc'-l. All SSSR 85
I~o. 5, 1952.
9. Monthl List of Russian Accessions, Library of Congress, Doc,~Inibr-r 1953,~Ay
, Uncl.

-1/. jrV
USWGeology
Card 1/1 11als- 46 6/ig
Authors i Krestnikov, V N.
Title S History of the development of the structure anA the saismism of
northern Tan'-Shan
POriOdiCal I Izv- ANISSSR. Ser. geolo 3,-92 - 108. May - lun 1954
Abstract i Geological data are presented regarding the 14eso-Cenosite history of the
development of northern Tan*-.Shan, problems of its structures newest
migrations and the saismiam of this section. Twenty-two'Ruestan and
USSR references (1886 - 1952). Maps.
Institutions ....a
Submitted: September 29. 1953

KUSTNIKOV V.11.
- - -
19ffoct of the Falaoz*ic structural plan on the devele7ment of
uplifte in northern Tien Shan during the Neogeno and 04mrtor-
nary periods. BIxt1.HDIP.Otd.gsol,30 n9.6;55-68 H-D 155.
(Tien Shan-Geology) (MIRA 9:4)

VIARTNIKOV, Y.N., POPINNON, V.11.
On the Paleozoic in northern Kakhatia. Dokl. AN SSSR 105 no.5:
1076-1079 D '55. (KIRA 9:3)
1. Geofizicheakiy institut kkadeaii nauk SSSr. Predstavlano
akademikon D.I. Shcharbakavym.
(Kakhatia-Geology, Stratigraphic)

KRESTITIKOV, V.N.
Relationships between geological and seismic phenomena in Tien Shan.
Biul. Sov. po seism. no.3:81-94 157. (MIRA-11:5)
(Tien Shan--Seismology-)

KRESTITIKOV, V.N., kand. gool.-mineral. nauk.
....
Selomicity~-~a~-!n-aiii-i'aologicaI structure. Priroda 46 no.8:25-34 Ag 157.
(MLRL 10:9)
1. Inotitut fiziki Zemli Akadamil nauk SSM Moskva.
(Tien Shan--Geology, Structural)
(Seismic waves)

'S f~ v
AUTHORS: Gzovskiy, 14. V. , fle SeSov
Reysner, G.I. -
TMB: Tectonic and Seismic Condition~; o.' Garmskiy gay6n in
Tajik SSR (Sopostavleniye tektonik.i- ::,
Garmskogo rayona -Tadzhikskoy SSR.I) Part I.
PERIODICAL: Izv,,~stiya Akad mii Nauk GSSR, Spriya Goofi,,~Iola)skayn,
ABSTRACT: A junction of U.- vast Asian mountain chairis, fliralaya-
Pamir Eeosyndine and tlic Vien-Shan RanL~e v;ith the Tajik
depression represen'6 tecrit,)r.y o.L very active seismic
activities. Particularly, the Garms3r-iy rayon is known for
its biGhest concentration of the epicentres (Figures 1
and 5).
The history of its alpine, tectonic i,,ovements and the
formation of its geological structure can be represented
in thp form of diagrams. The structural chan,n-ps which were
undergone during tbe periods- of the Liesozoic an~i the
Kainozoic in the eastern rArt of the reCion alonC the
line VW-SE are shown in Figure 2, while FiCure 3
represents the same cross-section running tlirrDu~;I, Garm-
C'-1:d115 skiy rayon.

SOV/ 40-58-8-3/1?
Tectonic and Seismic Conditions afG&rnkiy Rayon in Tajik SSR
Some of the data given in the diagrams were interpolated
from the places situat!d f&rther away (Figure 4) but it
was assumed that the p3ssibility of error could not affect
the general character of the graphs.
A clear difference in the tectonic movements between the
geosyncline and the plateau areas can be clearly distin-
guished in Figures 5 and 6.
The preoent structure (Figure 7) of the Garmskly rayon and
,NE part of the Taj:Lk depression is characterised by several
divisions of which the most important is the alpine district
of Pamir and Darvaz.
A main feature of the structure of tli,- Garmskiy rayon Is a
vertical displacement of the isolated blocks separated by
the tectonic faults which break through the Earth's core.
The traces of these faults can be found even in the
Palacozoic base. Achange o(curred in their direction in
comparJ,son, with that in the Neogen and Quaternay periods
at the time when an inversion took place of the pre-Pamir
depression and when the region of the Kabudltxin rose above
the surrounding areas.
Card2/5 At the same period in the vorth-west of tl-,e Kabudkrim

6OV/40-58-8-3/17
Tectonic and Seismic Conditions of Gamsl&j Ra~ron in Tajik SSR
anticline, a series of faults developed, the depth of
which is characterised by the lon and narrow grabens
filled with small rocks (Figure 1~. These grabens could
not be independent structures as those in other areas
(Figure 7). It can be assumed that they are the remnants
of the changed direction of the movements of neighbouring
regions. Originally, a rise of one of the regions caused
the formation of a fault. The faults, in turn, caused a
break in the general movement of the area. Thus7 at the
boundary of two neighbouring tectonic regions, the faults
can be found, usually at the narrow ridges (Figures 1 and 3).
The formation of new faults in relation to the dislocations
are explained by the faults being not vertical. They are
mostly inclined towards its lifted side.
A noticeable feature is a very well-maintained range of the
young faults and folds of Beogen-Quaternary origin.
Their large number signifies a horizontally directed course
of the tectonic regions. Also, it can be assumed from
their general orientation that the shear effect as directed
along the Meridian.
Uard3/5 The Palaeozoic foundation of the Garm8kiy rayon was effected

Tectonic &.ad Seismic Conditions of Gumskly Rayon in Tajik SSR
by both the strong, vertical forces and the weaker,
horizontal shearinG stresses, thus being subjected to
a deformation which was of plastic character. This can
be seen on the surfaces where the Palaezoic is found
close to the Mesozoic rocks. Where this type of deform-
ation occurred with great speed, the faults were formed.
It could be said that all the blocks of Palaeozoic origin
behaved not as rigid bodies but as 0~_ plastic medium
with some parts of the Earth core beinG somewhatlof
greater viscosity in relation to the Me~;ozoic and. the
Tertiary sedimentations.
The general character of the mechanism of formation of
the alpine structure of th- Garmskly rayon could be also
applied to the regions of TajiK depit~ssion (riCui-e o).
It can be assumed that the developments in the Garmskiy
rayon took place during the second half of the quaternary
Veriod and lasted about 120-230 thousand years which can
be corpared with 600 thousand years of the total time of
the Quaternary period.
Card

Tectonic and Seismic Conditions of GarmsIcLy Rayon in Tajik SSR
There are 8 figures and 28 references, 25 of vihich are
Soviet and 3 German.
ASSOCIATION: Akademiya nauk SSSR Institut fiziki Zemli
(Ac.Sc.USSR,Institute of Terrestrial Physics)
SUBMITTED: August 28, 195?
1. Geology--USSR
Ca rd 5/5

,i,)V/ 49 -55-12-1/17
AUTHORS: Gzovskiy, M. V. -.Krestnikov,,--Y..-Ii.,.,-A~ersesov, I, L.,
Reysner, G. I.
TITLE; Comparison between the Tectonics and Seismicity of GexMSkiy
Re-yon of Tadzhik SSR. II (Sopostavleniye tektoniki s seys-
michnostlyu Garmskogo rayons. Tadzhikskoy SSR. II)
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya geofizicheskaya,
1958, Nr 12, pp 1425-14-42 and 2 inserts (USSR)
ABSTRACT: It was observed th U more than 9000 epicentres of the
energy from 104 - 1019,-j showed act'vity during 1955 and 1956
in Garmakiy ra7on of about 13 500 ~~ (Figs.2, 3 and 8). The
earthquakes were registered in sufficient detail to give a
complete picture of the seismicity of this region (Fig.1).
This region, therefore, was chosen for the investigation on
the relationship between seismicity and tectonic structure,
A quantitative method of investigation was chosen so that the
analysis of tectonics could be utilised in the determination
of seismicity. The mean gradient of the velocity of vertical
tectonic movements of the earth crust was calculated from
Eqs.(l) and (2). Some results are shown in Figs.4, 5 and ?
and Tables 1 and 2. The cross-sections I-I and II-II
employed in the calculations can be seen in Fig.G. The com-
Card 1/3 parison showed that in Garmskiy rayon the ai~eas of higher

SOVI 49-58-12-1/17
Coniparison between the Tectonics and Seismicity Of Garmskiy Rarn of
Tadzhik SSR. II.
seismic activity coincide with the banded structure 9 for which
a mean gradient of tectonic movements in the Quaternary period
was high (Figs-5 and 6). Therefore, it can be stated that the
velocity of seismic activities increases with an increase of
mean tectonic gradient. In order to verify this relation, a
method was devised which could be applied to any region having
seismic activity of short duration (2 to 3 years), provided
weak earthquakes and the measurable gradients of tectonic
movements are of recent origin. This method is based on the
detailed analysis which showed -that the correlation between
the frequency of earthquakes (Fig:l) and the tectonic grad-
ient Fig.6, is maintained in various areas of the Garm region
(Tabie 3, A,7 - frequency). As the above relation was found
for one region only, it is possible that some modifications
Card 213

SOVI 49 -58-12-1/17
Comparison between the Tectonics and Seismicity of Gamskiy Rayon of
Tadzhik SSR. II.
are necessary for the different tectonic structures or for
various depths of the earth crust. Therefore, the investi-
gations in this matter are not yet concluded and the addit-
ional information will be presented at some future date.
There are-3 tables, 8 figures and 28 references, of which 23
are Soviet, 3 are German (2 translated from Hungarian), and
2 are English.
ASSOCIATION: Akademiya nauk SSSR, Institut fiziki Zemli (Academy of
Sciences, USSR, Institute of Physics of the Earth)
SUBMITTED: August 4, 1958.
Card 3/3

MSTIIIKOV, V.N.
Developmont of the Palsozoic goooynelinal area In the Pamlrfl
ard adjacent parts of Asia. Izv.v7s.ucheb.zav.; geol.i razv.
2 no.4:3-28 AP 159. (MMA 12:12)
1. Institut fisiki zemli AN SSSR.
(Asia, Central-Geoloff , Structural)

KRICSTNIKOV, V.N.
Development of the Paleozoic goosynclinal area In the Pamirs and ad-
jacent parts of Asia. 1xv. vys. ucheb. zav.; geol. I razv. 2 no-7:
3-26 J1 159 WMA 13:3)
1. Inatitut fisiki zemli Akademii nauk SSSR.
(Asia--Geology, Structural)

PHASE 1 BOOK F"WITATION SOV/5096
Bune, V, 14, V, K, K. Zapol-'skiy V, I. Keylia-Borok,
-V, N,, Krestnikov, L, 11, Malinovskayav 1, Dersesov, G. 1. Pavlova,.
L G. Pautian,. G, 7.. Reysner, Yu. V. Riznichenko, and V. 1. Khalturin
Metody detal'nogo izuchenlya seysmichnosti (Methods of Detailed Seismic Research)
Moscow, Izd-vo AN SSSR, 1960, 327 p. No. of copies printed not given,
fSeries~ kk-ademlya nauk SSSR. Institut fiziki zemli. Trudy, vyp. 9 [176])
Resp,, Ed-, Yu. V. R1znichAnko,, Corresponding Member AS USSR; Ed. of Publishing
House~ S. 1, Mosarskly) Tech, Ed,- O~ G. Ullyanova
PURPOSE,, This b,)ok is intended for geophysicietsj, particularly seismologists.
COVERAGE.- The book summarizes the principal results of the work of the TKSE
Instituta fizikl z!5m!i AN SSSR (Tadzhik Complex Seismological Expedition
of the institute of Physics of the Earth of the AS USSR) and the Institut
seyamologii AN Tadzbikskoy SSR (Institute of Seismology of the AS Tadzhik
SSR) during the period 1955-1957. Among the topics discussed are.- seismic
apparatus used, new methods for determining the coordinates of earthquake
Card-1/1-&-

Mqthods if retailed Seismic Research
SOVIr,096
foci, detailed methods for determining the structure of the earths crust,
gome zesults of these determinations, methods of determining seismic energy
on the basis of a series of' criteria, analysis of dominant frequencies,, the
use of frequency-selective apparatus, a general description and analysis
of seismic conditions in the Garm and Stalinabad areasi the geological
stiixtu-re of the Garm region and the history of its development, and a
~-zmparison of the spatial di3tribution of seismicity and the geological
and te,;Aonic structuro of tb4i area. The Foreword mentions Academician
G. A, Gamburtsev [deoenoedl wh:) laid the foundations for this work wben
he was director of the !KSE,, The individual chapters of the book were
written bye Introduction and Chapter I -- 1. L,,Ner3esov and Yu. V,. Rizni-
chenkoj Chapter 2 1, L,. Chapter 3 L, flerseuov and T. G.
Rautian; Chapter T, G,, Rputlan,, Chapter K. K_ Zapollskiy and
V, I, Khaltux-irij Chapter 6 -- V~ 1. Keylis-Borok;,, L. N, Malinovskaya,
G~ I. Pavlova, ', and V_ 1. Khalturin; Chapter 7 -- V. 1, Buns, I. L. trersesov
and Yu, V. RlznlchenkD; Chapter 8 -- M. V. Gzovskiy, V. N,. Krestnikov.
avid G, 1, Reysner; Chapter I -- V~ 1. Bune, H. V. Gzovskry-aRT-f.-L. Herse-
sov, Thsr6 are 272 r6fez6n~,os! 185 Soviet, 73 English~ and 14 German.
Gard--77~6-

Methods of Detailed Seismic Re h SOV/5096
d eismic Re
'le S
of 'a Stalin
5. Seismic regime of a Stalinabad region 239
a
Study of eart a frequency curves 239
r
a frequenc
e
re ;ag e in time of t
Study of c a in time of the seismic regime 242
c
On the me for further investigation of the seismic regime
a for further inv
t5alinabad reirion
in the S alinabad region 244
Ch. 8. History of the Geological Development and the Present
Structure of the Garm Region 247
1. History of Alpine tectonic movements and the formation of
the geological structure of the Garm region 2-47
Triassic and Jurassic 2,49
Cretaceous 252
Palsocene and Eocene 253
Oligocene and Neocene 253
Quaternary, peri6d '. 256
2. Present structure of the Garm region 262
Internal structure of Paleozoic formations 263
Form of the upper surface of Palebzoic formations 263
Car"4/1-6-

Methods of Detailed Seismic Research SOV/5096
Internal structure of Mesozoic and Tertiary deposits 265
Form of the upper surface of Mesozoic and Tertiary deposits 269
General arrangement of the present structure of the region 270
3. Mechanism of the formation of the Alpine structure 274
Structural results of change in direction of the movement
of tectonic zones 274
Indications of additional weak horiz=tal compression 276
Mechanism of fold formation 276
Formation of transverse faults 278
Form of tectonic zones 278
Ch. 9.--4ismicity of the Region and Its Comparison With the
St tural, Geology 279
al Geolo gy
~tur
enters
1. Map o icenters 279
Method f of epicenters 280
0
rawing a map
drawing a map
r _s C
te istic
General cha teristics of the composite map of epicenters 282
.3
Comparison of epicenter maps for 1955 and 1956 283
G
m
arm region 286
-.w'.StpLlinabad region 288
Card~

El/049/60/000/03/001/019
1131/2691
AUTHORS I Ozovskil, Move, Nersesov, I.L and Reysuer, G.I.
TITLSt Now Principles of Beimio Zoning Derived for Central Trml-Shan. I]
PERIODIC&Ls Isvestils Akadadi nauk SSSR, Seriya goofizichookays, 1960, Nr 3,
pp 363-370 (VOSR)
ABSTUM This is a continuation of work published in this journal, Nr 2. 1960.
The invnetigation In based on the seismic zoning chart of the USSR
(Ref 13). Only earthquakes of magnitude 9, corresponding to the
energy I - 1015j, wore considered. The purpose of the investigations
vas to establish those areas considered to be the safest from the
point of view of engineering construction. The method vas based on
the rate of tectonic movements as described by Gzovskly st al. (Ref 5).
The map shown in Fig I was ccmpiled on the basis of the results thus
obtained. The method of seismic prognosis consisted of three separate
stagest
1) The territory was divided according to the gradients of tectonic
movements.
2) The zones thus determined were cl4asified according to the
Card 1/.3 magnitude of the above rate.

S/OAQ/60/000/03/001/019
313i73691
Now Principles of Seismic Zoning Derived for Central 2yan' -6han. U
3) 2he seismic safety -*me decided on the basis of the above in
conjunction with geological date.
As an WMMP1G' the three safety zones, 1, 2, 3, are shown in Fig 2.
The seismic activity A of a zone is defined an a period of the
earthquake frequency, 2 M 1/1, the isolinse of vhich were plotted as
shown In Figs 3-5. The first chart was based on the observations
during 19W.5e. the second during the period 1960-66 and the third
ins based on the strong earthquakes during the period starting 1885.
The unit zones an the charts are of 100062, the time unit is one year
and the energy I - 1010J (K - 10). The seismic charts obtained,
therefore, differ frcm the usual zoning charts by inclusion of the
frequency of earthquakes. The final choice of a zone for hydro-
engineering oonstruction could be based on the magnitude of earthquakes
Ca rd 2/3 defined by the standards SI-2-57 (Raf 14) or GOST 3999-48 (Ref 8) -

3/0,6X60/000/03/001/019
1131 691
Now Principles of Seismic Zoning Derived for Central Tyan, -Shan. 11
As an example, the probability p< 0.001 of occurrence of earthq!_'Akes
(once or lose in 1000 years) in suitable for the erection of lesa
durable structures and p< 0.0001 (once or lose in 10000 years) for
long-lasting structures. Determination of such a probability can
be based on the above soning charts and the umogram given in Fig 6.
Charts showing the regions of various probabilities of the occurrence
of earthquakes, calculated for Central Tyan-Shan, are given in
Pigs 7 and 8. There are 8 figures and 19 references , 17 of vhich are
Soviet and 2 English.
AMOCIATIONtAimdaiya aguic SUR, institut fisiki, sonli (Academy -of Sciences USSRL-
institute of Physics of-the Earth)
SUMITT-RDs July 9, 1969
Ca rd 3/3

GZOVSKIY, H.V.; KRXSTNIKOV, Y.N.; LADMOV, N.N.; RXWOV, I.A.; RITSME, G.I.
Hap of recent tectonic mmeme-its in Central Asia. Izv. AN SSSR. Ber.
geofiz. no.8:n68-1172 Ag 160. (MIRA 13:8)
1. Akademiya nauk SSSR, Institut fiziki Zemli.
(Soviet Central Asia--Geolog7, Structural-Maps)

S/169/61/000/010/009/053
D228/D304
AUTHORS: Buns, V. 1*9 Gzovskiy, Me V., Zapollskiy, Ko Keg
Keylis-Borok, V. I., Krestnikov, V. N., Malinovskaya,
Le N*, Nersesov, I. Rautian, T. G.,
Reysner, G. I., Riznichonko, Yu. V., and Khalturin, V. I.
TITLE: Methods of the detailed study of seismicity
PERIODICAL: Roferativnyy zhurnal, Geofizika, no. 10, 1961, 12-13,
abstract 10A144 (Tr. In-ta fiz. Zemli AN SSSR, no. 9,
1960, 327 P-)
TEXT: The Tadzhik complex seismolo.,,ic expedition was organized with
the aim of studying the nature of earthquakes and the conditions of their
genesis. The most seismically-active zones of the USSR (Garmo, and Stalina-
bad) were chosen as the work areas. The specific conditions of working
and processing the data demanded the development of special systems of ob-
servation and methods of interpretation. The large amount of recorded
Card 1/6

S/169/61/000/ 010/009/053
Methods of the detailed... D228/D304
seismic phenomena permitted the use of statistical methods for studying
their distribution in space and time; these methods, in their turn, pro-
vided the basis for introducing the quantitative indices of the seismicity
characteristics of the seiamically-active areas. The actual seismic ob-
servations were closely coordinated with geologic inventir,~-Aionsj and this
provided the possibility of exposing the tectonic basis of the seismic
phenomena. A general review of the work area is Given in Chapter 1, and
concise data on major earthquakes are cited toj,ether with the general. posi.
tion of the expedition stations. A description of the standard main and
auxiliary apparatuo used at the stations, and also tile layout and descrip-,
tion of newly developed equipment--including an automatic seismic station
with a magnetic momory--ia cited in Chapter 2. The methods developed and
utilized in the expedition for studying the cnist's structure in the [iron
under investigation from the records of nearby earthquakes are described
in Chapter 3- Horizontal and vertical hodo,-raphs were constructed. The
resultina material enabled tile crust to be represented as a one-layer riass
Card 2/6

V1,5 1/0-"j/010/009/053
Methods of the detailed... D228/D304
with a lonCitudinal-irave. velocity of 6,oo v. 691 km/3ec. At the M10horovicic
boundary, the velocity suddenly changes~ ?o 8.0 kni/sec. and then somewhat
decreases, but at a depth of 300 kni it subsequently increases to 9*2
kin/see. These data underlay the construction of isochrone charts used to
localize the epicenters and to determine the focal depths. The isochrone
charts were constructed with an account:jf the hotero(.;eneity of the work
area's geologic structure and the peculiarity of the seismic stations'
location. This enabled the precision of hypocenter localization to be
substantially increased, reducing it to I - 2 km at the center of the
work area's topographic map., In Chapter 4. the definition of the concept
of seismic energy at the focus is giveng,and the basic formulas are de-
rived for its calculation. On the basislof experimentally obtained laws
for the dyine out of energy with distance, nomographs were constructed
to determine practically the energy at the focus from the records of nearby
earthquakes. Appraisal of the precision of calculation of the energy in
relation to different factors shows that it may be determined accurately
to the order of its magnitude. In this connection, the value K - 1g E j.
Card 3/0'

S/169/61/000/010/009/053
Methoda of the detailed.., D220/D304
is introduced for characterizing the enerey class of earthquakes. The
value of K is compared with the earthquake magnitude M. The study of
the iso-energy lines shows that the differont do.groes of the dying out of
seism*lc energy along and across the strike of Geologic structures exert
a decisive influence on the form of the isoseisms. In Chapter 5, the
frequencies of seismic vibrations are studied--in relation to the earth-
quake ener67, the distance from the source, the Geologic conditions at
the point of observation and at the hypocenter, etc.--from recordings at
both the customary stations and a special qViCC (ChISS) seismic-station
intended for frequency analysis of soismic waves directly at their place
of re.-istration, A detailed description is E;iven for the frequency-
selective seismic-station TAU-,- 1984 (C41-S-1954) and for the results of
the investigation of its recordinga. Certain eDicentral zones with an
anomalous frequency are thereby revealed. The procedure for theoretically
calculating the focal characteristics, and also for appraising these
latter from empirical data, is iven in Chapter 6. Scjveral formulas are
Card 416

S116 611000101010091053
Methods of the detailed..* D228YD304
cited for determining the size of a focus in-relation to its energy on the
basis of different physical propositions. The dynamic parameters of the
foci are determined; there appear to be definite predominant directions
for both the strike and dip of the fracture planes. The characteristics
of the seismic conditions of the Garmo and Stalinabad seismically-active
regions--both as a whole and in individual areas--are quoted together with
the variations in the parameters of the conditions in time. The quantita-
tive expression of the seismicity during constant seismic conditions is
determined by the seismic activity. The possibility is shown of construct-
ing graphs of the recurrence-of earthquakes from short observations of
weak shocks, and methods are given for determining the period required to
obtain the parameters of the seismic conditions with a pre-set precision
in relation to the energy of the recorded earthquakes. The statistical
constancy of the seismic conditions is determined by the so-called measure
of dispersion of the frequency of earthquakes. A brief description of the
area's stratigraphy and the history of its geologic development is given
in Chapter B. The structural schemes and deocriptions of the most important
Card 5/6

9/169/61/000/010/009/053
Methods of the detailed.*. D228/D304
deep faults are cited* The contemporary structure of the Garmo area is
depicted as two main regions,. the alpine goosynclinal zone in the south
and the activatod api-Hercynlan platform in the north. In sectiong it is
d-rawn as several steps of Paleozoic basement adjoinin,-, each other along
deep faults. A comparison of the seiamicity with the tectonics of the
study areas is made in Chapter go The construction of maps of isolines
of seismic activity and gradients of the rate of tectonic movements is
reconuaended for appraising the connection between the seismicity and the
tectonics. Methods are cited for constructing such maps. The congruence
between these magnitudes is established for the regions under investiga-
tion, and areas with the maximum Gradient values correspond to those with
the highest values of seismic activity. 272 references. f-Abstracter-s
note% Complete translation.2
Card 6/6

1"-;oTi-1MjV, V.N.; -- G.I.
AlIdi,4; .--utonicu of the central Tion Shan. --ov. geol. 3
ric. D 161. (ED, -!.,'.:2)
1. .i~ t,,--cut fl".iki Zemli AN
(Tien Shan--Goolo~y, Otmetural)

_KRESTNIKOV, V.N.
History of the geological development of the Panirs and adjacent
parts of Asia in the Meso-Cen020iO (Triassic and the lower Cre-
taceous). Sov. geol. 4 no.4:60-85 Ap 161. (MIRA 14:5)
1. Institut fiJJki Zepli AN SSSR.
(PamIrs--ZeolbgyI Stratigraphic)

ll~- V.i:.
Geological deveio.-ment of' t-.e 7janily-L and adjacent r,,.'
Asia in the Vesozoic and Ccnozoir; up-.c-r Gretacec7--o -i2-0
Sov.geol. 4 no.7;6e-94 JI 161. Jj,--LD"
1. InstLtut Ter-li imeni 33M.
I
(Panlr,------Gcolof7:

PETRUSMSKIY, B. A., gablog; BELOUSOV, V. V., geolog; GZOVSKIY, M. V., geolg;
GORYACHEV, A. V., goolog; KIRILLOVA, I. V., geologi KRESTRIKOV, V. N.,
geolog; RASTVOROVA, V. A., geolog; REZANOV, 1. A., geol6-g-,-SCMXIf;-
A. A., goolog.
Geolo'gic principles of seiamis division into districtso Studii
astron saismol. 6 no.2:181-186"61.
1. Institut, fiziki Zemli AN SSSR.

KRESTIUKOY, Vladimir Ilikolayevich, BFJOU60V, V.V., otv. red.;
,e IIIKOJ V.1.1 red, izd-va; POIYAKOVA, T.V.p tekhn. red.
(History of the development of epeirogenic movements of the
earth's crust in the Pamirs and adjacent areas of Asia] Istoriia
razvitiia kolebatellukh dvizhenii zemnoi kory Pamira i sopredell-
nykh chastei Azii. Moskva, Izd-vo Akad. nauk SSSR, 19(2 177
(MIL 15:J*
1. Chlen-korrespondent Akademii nauk SSSR (for Belcusov).
(Central Asia-Earth movements)

IRESTPrIKOV, V.N.; NERMOV, I.L.
C
Tectonic pattern of the Pamirs and Tian Shan and its relation
to the surface relief of Mohorovicic. Sov.geol- 5 no.11:36-69
N 62. (MIRA 15:12) .
1. Institut fiziki Zemli AN SSSR imeni O.Yu, Shmidta. I
(Tian Shan-Geology--Structural) (Pamirs-Geology, Strucf*ral)

Characllerl3tiCl Of' the IMe.9t tectonlr~ of
1 *1 1 1,- ,, P
lqyzin Houritairo and tNIDU'll TWILL. 1(,ij n,3.4.-8r4'-900
F 165. (NJF,-A IF:2)
1 . -in v Li tut, f - Zik i --n:' i I!n. Y: i.
il 3LI-1. SU b;n L 0 d

~IrJJTFOV V.N.; REISNER, G.I.
Sc ratigraphy of the Tc--r-Liary (-unL'rental of Tu.!u In
Central Asia. Dokl. AN ](:4
(MIRA 18:10)
1. Institut fiziki 'llemli im. O.Yu.Shmidta "ill CS)SSR. Submitt-d
Arril 19, 1965.

ACC NR:- AP60321982 S.OUR CE -- C.ODE:- U-R-/-0-Oll/ 6-6 /000/0i-0/0076/0090
AUTHOR: Krestnikov, V. N.; Reysiter, G. 1.
ORG: Institute of Physics of the Earth, Academy of Sciences SSSR, V(Institut fiziki
Zemli, A'Kademiya nauk SSSR)
TITLE: Naryn-Chichkan transverse region of the subcrustal fault of Vestern
Tyan-Shan'
SOURCE: tLN SSSR. Izvestiya. Seriya geologicheskaya, no. 10, 1966, 78-90
TOPIC TAGS: geologic exploration, geologic surveying, geomorphology, physical
geology, subcrustal fault orogeny, earth crust -kc4cm~C..I.,
ABSTRACT: The present article describes the Naryn-Chichkan transverse region of
the subcrustal fault of Western Tyan--Shan'. It is shown that the Nar-In-Chichkan
subcrustal fault and the associated depression strike transverse to the main
tectonic blocks of the lower Naryn Ptiver basin. It is assumed that the fault extends
liurther 3outh into the West-Karastr/ and Fergana valleys near the city of "I'amangan,
where it Aoins one of the subcruSLal faults along the northern boundary of the
--arzana. valley. The fact that the Naryn-Chichkan subcrustal fault dates back to
before the Lower Quaternary indicates recent tectonic changes in the ancient:
structural plan of this part of Tyan-Shan. The Ndryn-Chichkan subcrustal fault
region was formed unevenly with respect to time and space. it underwLnt down-
Ca,-d 1/2
-Wki

_;V60 32!M2
warping during most of the Quarternary period in..the area of confluence of the
Chichkan, Naryn, and Uzunakhmat Rivers. The most intense downwarping in the
Oi-Ichkan area took place during the Uppe r-Qua ternary period. Chronological
analyses are presented of the major geological processes. -of the Tyan-Shan' , and
tectonic r-aps showing the Alpine and quaternary orogenies are included. Oris. art.
has: 7 figures.
SUB CODE: 08/ SUBIX DATE; 26May64/ ORIG REF: 010/
Card______212

SLAV-fAXffIYO V.T., KnSTNIKOVo To. N., PROSMTAKOV. K-V-
Now method for anglysing genes In flAle, Stek. I ker. 17
no.6t29-33 Je 160# (MIRA 13t6)
(Glass)

SO V /1 _17- 58-12-242V#
Translation from: Referativnyv zhurnal. Metallurgiva: 19;i8; Nr 1-1, p 53 (USSR)
AUTHOR: Krestnikov, Ye. P.
TITLE- Production of Calcium I-Ivdride n Confinuous Equpnient 1,P,-o1zvods1vo
gidrida kal'tsiya v appdralo nt!pre,,-yvnc)go dvvs!viya~
PERIODICAL- Tr. Ural skogo n. -i kl~-,mi in-ta, 1(4~7 - 10;8~, Nt r,, pp 118-135
ABSTRACT: An investigation is made of fbe process of Ca I-vdrogendtion. with
selection of optimum conditions fo, ,ndustr,al performance of this
process. The influence of the level of puritv of the Ca and lbe struc-
ture of the material upon the livdrogenation process is noted. It is
found that addition of up to 11/4 Na to ti-e ground Ca 0'by fusing with
metallic Na or with its chloride) results in a stable reaction at 2400C
and is efficient with Ca of various levels of puritv. O%ving to the
highly exothermic nature of the reacnon and fie similirily of the
melting points of Ca and its hydride, t is possible to overheit and
fuse the material Inhibition of I)-.e reaction is performed by the
charging of return hydride or inert gas A cont,,xiuous equipment has
been developed. It is a gastight shelf-tvpe electric furnAce with ~
Card 1/2 groups of beaters and automatic temperature cont ro' . The equipment

SOV/1 37-58- 12-24299
Production of Calcium Hydride in Continuous Equipment (cont !
works at a 50-100rnin lig excess 1-12 preti8urv. The Ca shavings enter the fir8t zone
of the furnace at a temperature of 2500, and Ar is introduced to prevent overheat-
ing. The upward progress of the H2 in the furnace provides assurance that Ar will
be present only in the upper portion of the furnace. The ternperaturo of the next
zone is 300-3500. The material is in the furnace for i hour altogether. The
charging of the shavings, the motion thereof through the furnace zones, the grind-
ing of the hydride in a cone crusher (down to l- 1. 5 mm grain size), and the unload-
ing are mechanized. Several hundred kg of hvdride were produced on a test mod-
el. Bibliography: 23 references.
L. P.
Card 2/2

PILASE I BOOK EXPLOITATION SOV/6417
Suslov, Nikolay Ivanovich, Aleksey Dmitriyevich Grigorlyev, Igor'
.geniy,Pavlovich Krestnikov,, Valentina
Veniaminovich Pimenovp jq~v
I7anovna Susorova, Valentina Ivanovna Morotskayap Tamara
Vasillyevna Basarginaand Pavel Alekseyevich Zaytsev
Nametallicheskiye materialy; spravochnik (Nonmetallic Materials;
A Handbook). Moscowp Mashgiz, 1962. 360 p. Errata slip
Inserted. 32pOOO copies printed.
Ed. (Title page): N.I.Suslov, Engineer; Reviewers: A.V.Podollskiy,
Engiseer, A.I.Lesik, Engineer, T.V. Basarginap Engineer,and Yu.I.
Bagln, Engineer; Tech. Ed.: N.A. Dugina; Executive Ed. of
Ural-Siberian Department (Mashgizi: N.D.Chilikinap Engineer.
FMPOSE: This handbook is Intended for engineers and technicians
j
4~m the machine building industry.
COVERAGE: The book contains syste.-iatized information on non-
metallic materials used in machine building in the Soviet Union.
C&rd 1/3

",,all ic Materials (Cont.)
sov/6417
Trade names, GOST designations, properties, and applications
are given in tabular form for plastics, adhesives, varnishess
dyesp oilsp and chemicals. The book deals primarily with
plastics, which are divided into seven classes. Chapter I
was compiled by Engineer N.I.Suslov; Chapter II,,b7 Candidate
of Technical Sciences A.D.Grigorlyev and Engineer I.V.Pimenov;
Chapter III, by Engineer V.I.Susorova; Chapter IV, by Engineers
E,P,Krestnikov, V.I.Morotlskaya, and T.V.Basa.-Lgina; and Chapter V,
b.-7 Engineer P.A. Zay-bsev. The.-e are 84 references: 83 Soviet
and 1 English.
TABLE OF CONTENTS;
Freface 5
Ch. I. Plastics 7
Ch. II. Adhesives 151
Card 2/3

USM/ Physics
Card 1/1 Pub. 22 12/63
Authors t Blinov, G.A.; Krestnikov, Yu. S.; and Pershin, I.I.
Title ~I Observation of tracks of ionizing particles
Periodical 1 Dok. AN SSSR 99/60 929-930, Dec PA, 1954
Abstract I Experiments with molybderium glass ampoule filled with propane (C3 Ha)
are described. The experiments were conducted to determine the posa-
ibilities of using the "bubble" cameras for photographing very-high
energy ionizing particles which would provide a valuable means for the
solution of various problems of nuclear physics. Six references (1952-
1954). PhoLogrmms.
Institution; 606699
;Irezented by: Academician A.I. Alikhanov, November 4. 1954

BLIVOY, G.A.; MUSTMIKOV, Yu.S.; FUSHIN, I.I.
Liq;id babble chambers for investigating ionizing particles.
IIIv.AN SSSR.Ser.fis. 19 ne.6:758-760 N-D 155. (MLRA 9:4)
l.Akademiya nank SSSR.
(Cosmic rays) (Nuclear physics)

(X tile i!`.*-AZj,` --r,
U'r e c I ,a.-: c I -
Ge,nova, 11-23 Twic
'In. Frwxh

i of A a
lGrA P,--2 9f-7 -The t nrk d. of Dat S In a

A X 'C' -"3 1 /q _L A & V X ci I
SUBJECT USSR / P71'131CS (;,'.PD 1 if 2 PA - 1770
i'UTHOR BLI1TOVyG.A., KRESTNIKOVIYU-S., LOMAITOV,M.F.
TITLE Measuring the _o_n-1_z`aon Power of Particles in a Bubb'e Chamber.
PERIODICAL ~,urn.ekap.i teor.fis,j1,fa(5c-5,76?-770 (1956)
Issued: 1 / 1957
Cahtrary to other authors the authors of the present work employed the method
of pressure drop up to a certain level, which warranted a very stable operation
of the chamber. The experimental part of the work was carried out by means of
the synchrocyclotron of the Institute for Nuclear Problems of the Academy of
Science in the USSR.
Structure of the chamber and selection of mode of operation: The work space
of the chamber consists of a cylindrical vessel of stainless steel (inner dia-
meter 92 mm, height 70 mm)- Simply distilled technical propane with a vapor
density of 30 atm at 640 C was used as an operating liquid. The construction of
the chamber is discussed on the basis of a drawing. A particular feature of the
device described is the drop of pressure in the chamber down to a constant
regulatable level. By a pressure stabilizer and through an electromagnetic in-
let valve carbonic acid gas is introduced under pressure of 38 atm. This
pressure is transferred by means of water to two membranes. After complete con-
densation of the gaseous phase the chamber is ready for expansion. During work
with an accelerator the chamber was fitted in a collimated bundle of neutrons
with average energy, in a bundle of f-quanta originating from the decay of
neutral pions, or in a bundle of particles emitted from the target and from the

~urn.eksp.i toor.fio,31,fasc-5,762-770 (1956) CARD 2 / 2 PA - 1770
walls of the collimator in the direction of the protons. A control system made
the remotely controlled measuring of temperature, pressure, and other quanti-
ties POS3ible in the chamber.
Methods for the measuring of the density of the traces: At present the grain
densities in nuclear photo emulsions are being determined by the method of the
average length of distances and from the number of distances. The authors em-
ployed similar methods, viz. 1.) The method of simply counting the number of
bubbles* 2.) Tr method of the average length of distances, which is the most
objective. 3. Determination of the number of distances exceeding a certain
minimum distance. This method is the most accurate for dense traces. The densi-
ties of the traces of 5 cm length can be determined within a 20-fold variation
range with errors of from 6 to IV,. without modifying the accuracy of the
chamber.
In conclusion the identification of the particles and the dependence of the
density of the trace on the velocity of the particle is discussed. The
distinguishing features of electrons, protons, deuterons, and pions are
pointed out.
IRSTITUTION:

Pi tri

MEMYREMENT OF THE tOWNG POWER OFj&q!t_
Ct,
Krestfl
__KtLnIk', and - to lletph - ~JETP

The jwm%lbillty of, the m"WrtmeAt o(Oa WoWr4 K,%tr
of Particles in a prquele bubble etwimbiir is damoostrated.
Th.-ghamber was operatleg in with an aceelers-
tor. %rhe Lse of the mtthod ot the rcdopt Ion of pressure to
s tontrollable constant level eesured the stability of cham-
ber opem(On necemmkry for tontrition memsturemenX47kThe
period Of serkitivity wts 40 matc. easurement% of tke
lonixing PO W ut Orlitits were carried out In the range
up to eight titneo minimum ionlistion. It was found ftt the
track dunsIty changeii* with th& vilocity of " particie as
_1101forilcO.0, For valueltivs cluse to that of Ilght. rc)A-
tiviRtle ircr.AJ6~ in OV trAck (Amitty, is Otmtrved. V4 used
Methods (m the track evalwulum are &srrilird. (Ruth,

AUTHOR BLINOV 56-&4 0/56
G.A. YU.S -KREST11IKJV LCILIANOV !:.Z.,SHALAMOVj Ya.Ya.
TITLE On the Use of-a--RlYfu~reof Ti,o Liquids for a Bubble Chamber.
(Primeneniye smesi dvukh zhid;:ostej dlyg pugyrIkovoy kamery-Russian).
PERIODICAL Zhurnal Ekaperiq.i Teoret.Fi-_,iki,1957,Vol 32, Nr 6, PP 1572-1573
U.S.S.R.
ABSTRACT If the dimensions of bubble chambers are enlarged,the technical
difficulties connected with their operation are increased, for it
is necessary to provide for such temperatures and pressures in the
chamber as correspond to the liquid used.These difficulties might be
removed to a considerable extent if it were possible to work at a
temperature that is near room temperature.Perhaps a good working
temperature might be attained by the suitable miAira of two liquids
(as e.g. propane andphreon). For this purpose the authore carried
out experiments with a bubble chamber which was filled with a mix-
ture of phreon-12 (CC12F2) and phreon-13 (CCIF3).The construction
of the chamber used for this purpose has already been described in
a previous paper.By fitting a Cobo-j,'- source beside the chamber,
it was possible to watch the traces of the electrons and to photo-
graph them.In this way it was possible to find out at what tempera-
tures,pressures, and concentrations,the traces can be observed.The
authors selected mixtures of two different compoaitions.The data of
the two mixtures are given.The experiments were carried out in the
Card 1/2 case of the first mixture at temperatures of from 19 to 300C and in

On the Uae of a Mixture of Two Liquids for a Bubble '
Chamber. 56.6_4o/'~&
the case of the second at temperatures of from 43 to 520C. ~he results
of these experiments are given in form of a diaSram. The chamber
was expanded every lo minutes.In the case of all experiments car-
ried out preusure in the chamber between eXDansions amounted to
35 atri. The duration of sensitivity was determined photographical-
ly.The chamber works satisfactorily with a mixture which,at room
temperature,has a pressure of the saturating (saturated) vapors of
about 21 atm. The mixture used here is suited for riany nuclear
inve3tigations because of its high density (-1.0 3/CM3). Using
ouch a mixture of liquids might render selection of the filling me-
dium forthe chamber more easy.Also mixtures containing hydrogen
as e.f. rjethane and propane,are interesting.
(1 illustration).
ASSOCIATION Not Given.
PRESENTa BY
SUBMITTED 8.2-1957
AVAILABLE Library of ConEresa.
Card 2/2

(7)
AUTHORS: Kreptaikov, yu. S., Meahkovokiy, A. G., SOV/56-37-3-52/62
5h-aTWW;--Y**-X&wy,o.9kebanov, V. A. , Kobzaxev, I. Yu.
TITLEs on the DecaysA4e +rand^4 e+v + 3+-r
PERIODICAL: Zhurnal eksperimentallnoy i tooreticheekoy fitiki, 19591
Vol 37, Nr 3 (9), pp 873-875 (USSR)
ABSTRACT: From the hypothesis of the existence of an intermediate boson
of great mass (univerval A-V interaction) it follows that the
decay u -o e +-r is possible, which is forbidden according to
A-V point interaction. Feynberg calculated the probability of
this interaction and showed that the ratio
?i = R(,u -> e + r)/R(,& i e + v + 7) depends on the ctit-off
parameter A. If A is equal to the boson mvLas 9 ~~ 10-4,
if -,~ < M, it may become arbitrwily small. The auUora of the
present "Letter to the Editor" searched for the /.4-> e + rdecays
by means of a 17 liter freon bubble chamber . The chamber waB
located in the.external 'M + beam of the synchrocyclotron of the
OIYaI (Joint Institute of Nuclear Research). The 200 Mev
1r +-mesonn were s10-ved down by means of a graphite filter and
Card 1/3 were stopped in the chamber space. About 20000 8tereophotographo

On the Decays ~, + a + or and p 4 a + v + ~ + r SOV/56-37-3-52/62
were obtained, which were twice evaluated. The evaluation lines
are given. Of the three pocBible decays m -# * + Y + V + r ,
Ir ,, A + V + 'r, and /A. 4 e + r not a single one of the third
kind was found among 91000 7r-~L-e decays. P, was determined as
amounting to gt 4-301o-5 . In the evaluation of the plates
reactions of the first kind were found with 1800; such
a photo is shown by figure 1. Such a decay has hitherto not
been observed. A table shows all cases in which Er-> 15 - 20 Mev
and in which the angle (a, r) -> 50 -60". The 'table contains
data concerning the (e,-r)-angle, Be and E7, as well as the
energy of the decay productsA. For processes of the first
kind it was found that q - 105.2 Mev, for those of the second
kind - 33.9 Mov. Figure 2 shows investigation results in form
of a diagram, where the number of recorded pairs is plotted
versus the angle of rotation in the mon stopping oint. The
ratio of the reactions 92 - R(IL -* e + io + _i + r)/Rf/u -# e + v +
was determined as amounting to .0.80 + 0 24 10-3.
- o:36).
Card 2/3 Theoretically, 1.02-10-3 < ~2< 1.80*10-3 wAs obtained

On the Deoayo,,u+e+ randA-*a+V +~ +r SOY/56-37-3-52/62
(for the A-V interaotion). The authors finally thank
Academician A. I. Alikhanov for his discussion and interest,
It. F. Lomanov, Yu, I, Makarov, and V. I. Smetanina for their
assistance, Is-Se Bruk for mhking it possible to carry out
computations on the electronic computer of the type U-2 of the
Institut elektronnykh i upravlyayushchikh mashin AN SSSR
(Institute'for Electronic and Control Machines of the AS USSR),
and R. A. loffe for carrying out these computations. There
are 2 figures, 1 table, and 8 references, 1 of which is Soviet.
SUIaTTED: June 99 1959
Card 3/3

b6893
b ioo B029/BO77
AUTHORSi Barmin, V * V. , Kreugig".&Mftw, Pershin, 1. 1. ,
Rumyantsevl, V. F., 5halamov, Ya. Ta., Shebanov, V. A
TITLE. The Asymmetry in the Decay of A! Hyperons Produced by
Negative Pions With a Momentum of 2.6 Bev/c and Observed
in a Freon Bubble Chamber
PERIODICAL: Zhurnal eksperimentallnoy i teoreticheskoy fiziki~ 1960,
Vol.. 39, No. 501), pp. 1229-1231
TEXT: Tho distribution of decay products of & particles with respect to
their production level is described by W(f) dj, (1 +o~_Pf)df ; the asym-
metry coefficient c4 denotes the degree of non-conservation of parity
during the decay of /Y particlest P donotes the average polarization of
the hyperon over all directions of I?, and the following relation is
4
p p and p are the
valid too: PTrprim 4T[decayl 4ITprim' Tdocay
unit vectors of the momenta of the Rparticle, the primary and the "decay
pions", In general,o(~ is calculated from the formula oiF.2(N,,- 114,)/ ( Np , 11,,V
C it rd 1 A
S/056/60/039/005/009/05--

86893
The Asymmetry in the Decay of.A~ Hyperons S/056/60/039/005/009/051,
Produced by Negative Pions With a Momentum of B0291BO77
2.8 Bev/c and Observed in a Freon Bubble Chamber
N,t and N, denote the number of pions leaving ~he production level in an
upward or downward direction. The values of 9(P at energies above 1 Bev
permit conclusions about the polarization of lYhyperons produced at these
energies, Therefore, the authors investigated the asymmetry in the decay
of _Z~ hyperons which were produced on light nuclei by negative pions with
~ momentum of (2.8 t 0.3) Bev/c in a 17--liter Freon bubble chamber without
~ magnetic field. The measurements were made with a beam of negative mesons
of the proton synchrotron of OIYaI (Joint Institute of Nuclear Research)
For negative pions with a momentum of 2.8 Bev/c, /~! particles were produced
mainly according to the reaction ir - + N--)A!~ K + nil, and a preliminary
estimate yielded 7i -- 1.5. The first examination of about 6o,ooo stereo-
photos showed about 1200 "forks" at the end of pion tracks, 1631~ decays
were selected, of which-165 refer to the production of,1T particles by
Freon (that is, by nuclei of C,F,Cl). 18 cases refer to production by a
propane-xenon mixture, that is, by nuclei of H, C, Xe. The average
momentum of the X particles used for the measurement was 650 Mev/c in
the laboratory system. Resulta ofv(P measurement.
Card 2/4

86893
The Asymmetry in the Decay of J~Hyperons S/056/60/039/005/009/051
Produced by Negative Pions With a Momentum of B029/BO77
2.8 Bev/c and Observed in a Freon Bubble Chamber
Filling material Total number Number o-f negative pions
of the chamber of 1~ ducays produced by the decay of
a R hyperon
omitted
upward downward on the produ-
cing level VII
Freon 165 67 95 3 -0~3410.16
Xenon-propane 18 9 a 1 +0,,12+-0 47
Total number 183 76 103 4 -0..30'-0 15
of cases
The systematic errors tire below 20%. The value of aip is most likely negative
during the decay of hyperons, which gives rise to 3-Bev negative pions This
could be caused by the change of sign of the polarization during the
transition from 1 Bev to higher energies of the negative pions produced
But the statistical accuracy of this investigation is not adequate for a
definite statements The authors thank A I- Alikhanov, A. G.. 14eshkovskiy,
Card 3/4

86893
The Asymmetry in the Decay of Z2 Hyperons S1056,1601039100510091051
Produced by Negative Pions With a Momentum of B0291BO77
2.8 Bev/c and Observed in a Freon Bubble Chamber
and I, Yu. Kobzarev for a discussion of the rebults obtainod, V,T.. Veksler
for making possible the experiments with the proton synchrocyclotron in
Dubna, the operators of the synchrocyclotron, and several laboratory
assistants of OlYaI. There are I table and 8 referencoo: 2 Soviet and
6 us,
SUBMITTED: July 2, 1960
Card 4/4

yu. Yi7i;,~:,::,~V, 7, "1.;
jv,-
41TIN y . P.1 "'T
"-7r'-I'roiurtIon Jn the Ccullmb Fb-Id o,,' N,trloin"
n2p,r~ pn,armt-l nt th,~ 11th liltl. conrer"I;r~- On W.,111 1~1;-Iyj
4-11 JOY 1562
Inotitute of 'Meoretical find ExperInontril 0!ynI,,,i,

BVM11, V.V,, Yu. G-, 07MIRM, Ye. V., A. G., nnd
GRELANOV,
%search for fiLsonances in the P--action, of 6~Vmir Prodtiction"
report prenent4od at the Intl. Conference on High Enerpy, Phyalca, Genevn,
4 -u - July ig(;2
bwt. of 'lleorentical and Experimental rboica, Moscaw, =R

8/056/62/04 3/004/616/061
B1 021 If 1 (10
AUTiltd(J: ba r. - in, V. %, gre:;tn I kov, Yu. J. , r.uzn a t a o'v,. Ye. V. . Mesh-
WKI
)vz;'F.iY' it. . I IT tiy~' Y11. P. , Shebanov, V. A.
ii.enon production in the nuclear - Cott lomb field
PE'l 101) 1 ~;A Zhurnal eksperimentil"noy 1 teoret16hesitoy fiziki, N. 43,
no. 400), 1962, 1223 -1230
1;,;XT: 'To otody tho mechaniom of coherent interaction, in which nomentum,
t~r;tnsfer i- very lox rind nucle-,.ir excit-ition absent, T + NA - _:* + -ILO + TIA
z z
relictionn. ,-.,err. exurained. They can only occur.via int6raction with the
nucleir CoiiLomb field, diffrartive pion I'dissociations" being strongly for-
bid-len. Lnly one pion dissociation experiment is hitherto known (BaYdawar-
re et f'1. :Tuovo c1m. 21, 45), iq6i). Using a 2-liter xenon bubble chamber
.and 2.8 iiev/c z_- ti,caons from the proton-3ynchrotron of the OIYaI about
10,000 :,tereophotographs were obtained, and a similar numnber with a freon
ch,imber-. 48 -ind 31 events ofi-t- scattering through 3-30 0 accompanied by
two electron-positron pairs were found respectively. After kinematic ana-I
bard 112

0 '
'rL Menon production ...
z;/cr)6./'&-2/04 3/'(;U4/)16/061
B102/ ill 80
I - s '~X-t_- re,mtined 25 ;tml 13 evrnt-j could b.-? ;!ttributed to the
+ + j(-0 ~ Ae rn,ict~on. T1118 is (".7�1-3)-10-5 of the total n'uai-
bui- ot the cro,;.-- i5pcti~',n of vllhicl; -;-nn 120~) mb,
fl,D:"I the. pic)", di.-:ocia~Jon croso ,3ection found to 'ur 0-.1' 4+1.6
7--h cfficii~ncy taken into account. There .%as a F,.,rp* p e -i k
rit P