SCIENTIFIC ABSTRACT FEDOTOV, P.D. - FEDOTOV, S.G.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000412730004-0
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: January 3, 2017
• Document Release Date: July 27, 2000
• Sequence Number: 4
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

KUZfZTSOV9 I.S.p kaM.maditsinskikh nauki PETROVP V-I-p kAnd-M8ditV'rjk'kh
naukj FEDQTQY4-PDw-
Roentgen diapooiO of act1poWcosis of the thoracic And
Abdominal cavity* Vest. rent* i rade 35 no., 507-0 84
160. (MM 13:12)
10 Iz rentgono-radiologichookofo otdola (save - kandidat
maditainskikh nauk Me Petrov) Moskovskogo oblastnogo nauchno-
iooledovatelinkogo klinicbeakogo Iwtituta imerLi M.Fj
Vladimirskogo (dir. kand.med. nauk-P.M. Lsononko),
(ACTINOMICOSIS)

DUBIROV, Ya.G., prof.j BUACHIDZE. O.Sh., kqnd. med. rLauk,,_,MOTOV, P.D.
Bone chondroma. Vest. khir. 91 no.11:41-46 It 163.
(MIRA 17t.12)
1. *Iz ortopedo-travmatologicheskogo otdeleni2la (rukovoditell - Prof.
Ta.G.Dubrov) i:rentgano-radiologicheskogo otdela (rukovoditell - Prof.
V.I.Petrov) Moskovskogo oblnstnogo no.uchno-i:3sledovatellskogo k]Jniche-
skogo instituta. Adres avtorovi Moskva, ul. Shcbepld-na., d. 61/2,
ortopedc-trav'matologicheekoye otdelerilye.

DUBROV, Ya.G., prof.; BUACHIDZE, O.Sh., kand.med.naul:; FEDOTOV, F.D.
Solitary bone cysts., Ortop., travm. I protez. 25 no,3:19-23 Mr
164. (MIRA 18:3)
1. Iz ortopedo-travmatologichaskogo otdeleniya (rukovoditell
'prof. Ya.G.Dubrov) i rent-ino-radiologicheskogo, otdela (rukovoditell
prof. V.I.Petrov) MoskoNakogo oblastnogo k'---Lcheskogo instituta
.(dlr. - kand.med.nauk P.Mjaonenko), Adres vatorov: Moskva I-110,
u1. Shchepkinao d.6i/2,, Moskovskiy oblastnoy "-clinicheskiy institut.

FEWTOV~ F.D.
Calculating the qualitative indices for work in X-ray clinics. Vest.
rent. i rad. 36 no.6t82-83 " 161. (MBA 15:2)
1. Iz rentgeno-radiologioheBkogo otdola (rukovoditell - doktor
meditsinskikh nauk V.I.Petrov) Mookovskogo oblastnogo nauchno-
issledovateliskogo klinicheskogo instituta imeni M.F.Vladimi skogo
(dir. zasluzhennyy vrach RSFSR P.MLoonenko).
(HADIOGMPHY)

"Iriability of Dyoontery-Bacilli of the flaxnir droup in Yood Products$
-Svr. Mravookhranenlye Kirgizii, No 2, 1953, pp 4.&-47
The viability of dysentery bacilli was investigated in miD:, curds, sour
crew, sausage, and (fresh) meat cuts. For instance, pieetis of meat were
placed. in a sterlie jar and coverei with two milliliters of an emulsion
of' 1 billioh microbe bodies. This infect"terial was etued at 18 to 25
-degreen and at 4 to 6 degrees (centigrade).1 The flexner be.cilli surviyed
in sterile milk 30 to 40 days and in cooked~meAt and a terile: cheese 35 to
45 days. Some ct the r1axner.bacilluB cultures'Vere tested for their
biochemical properties in comparison to paracAon (baclllu.-)* They ag-
glatinized at one fourth to one eighth the Ifloxner serum titer. Dysentery
culture which were typiol for their biochemical proyetties agglutinized
at one half the PlexcLer serum titer, Their virulence was unstable.
(RUMiol, No 4, 1954)
SO: Sum. No. 42: 2, 12 May 55

OBrl3NWV,l T.A., dots; SLATIN, A.M. xootakhnik; TIDMV!-~
Paniall1lum n7collum as swine food. Zhivotnovodetvo 21. w.6172-74
Je 159. (XIRA 1218)
*skovajcsya,,yqtqrlVRrnsrR -aAadimlra (for Ob-,y*&,qnnov).' 2. Jlav-
zW vetvrach sovkbos "Bolava daeba.9 Ukhtomokogo rayona. Kotkovakoy
oblasti (for Fedot-ov)
(Swine-looding and feeding stuffs)

nWTOT , _ P. I. . _ gorn. inxh.
Automtising the food of boring machines tows4rd the work
face, Goroshur, no.8.77-78 Ag 16o. (MULL 13: 8)
1. lasakhokiy gorno-metallurgicbesidy inatittt, Alma-Ata.
(Borlug machinery) (Automatic contz-ol)

FBDOTOV, P,I.; PZTROV, V.a.; ROZHAM, Sh. V.
Notopic chorioapithelloma of themediastimm, Boyet. mad* 23 no,2s
135-137 1 159. (KM 12:3)
.((;HORIOUR033OHL, case reports
medlastinum (Rus
(MIASTINN, neoplasms
chorlocarainoma (Ras))

FEDOTOV, PO I* Oand, Teoh Soi "Automation Pf the -f ead and produetivity
roTor,~:*a- "boring machinca. Alma-Atp, 1960 :(Min oj' Higher
Education, Kazakh Polytechnio Inst). (KL, 1-61, 198)
-256-
RiMM
:71 o z~';

FSDOTOV
An LSD for each large stockbreeding farm. Vaterinarila 36 no.6:
71-72 Je 159. (MIRA 12:10)
1. Glaynyy vaterinarMy vracb, sovkhosa "Belaya Dachau, Ukhtom-
skogo rayona, Moskovskoy oblasti.
(Disinfection and disinfectants-Mquipment and oupplies)

FEDOTOV, P.I.
Modernizing-rock drills for the purpose of increasing boring
speed. Trudy, Alt. GMNII AN Kazakh* SSR l5tlO4~108 '63-
Method of studying the operation of a rock dri.11 feeder,
Ibid.: 109-111 (KM 1713)

"Aspects of the course of croupous Pneumonia in recent years" p. 20
Voyenno Yleditsinskiy Murnal, No- 3) 1962

FEWTOV., P. L (Khabarovsk)
Marked pbysical, and roentgenological changes ir- the lungs in
croupous pneumonia., treated with sulfanilamide preparations and
antibiotics# Klin. mad. no.6tlO6-110 161. (MMA 14S12)
(PNEUMONIA) (SULFONAMIDES) (ANTIBIOTICS)

POLIKARPOV, B.V.; FEDOTOV, P.I.; RUDNEV, A.A.
Prophylaxis of hog oholera. Vaterinarlia 39 rio.8s34-37
Ag 162. (MIRA 17j12)
1. clavnyy vaterinamyy vrach Lyuberetskogo rayona, Moskovskoy
oblasti (for Polikarpov). 2. Glaynyy veterinemyy vrach
sovkhoza "Belaya dachaff, Lyuberetskiy rayon, ~bskovskoy oblasti
(for Fedotov). 3. Glavnyy veterinarnyy vrach sovMoza imeni
Monsoveta, Lymberetskiy rayon, Moskovskoy oblasti (for Rudnev).

KANUTUM CURVED FOR AIR-LXAD AND TIM ANGU-
OP
slid P. 1.
awmi tfvtst ALM, Suk
S,'ft, Mr, Ftt, IC 661

tm/physias cosmic partidles
Card
:P0. 22
Autban I Zh4an0v#4*_,P*0 and rodo*ove7Po Is,
A

Tit,le I MM
V
The- trawsiemt~ offe4i -aA&-the--aneular-distritution-of-

1,
k4-, AN -1
At Wv,
7~
rostent WOW le~
awid_~eiav- Or are described and
--stars Y p _'oualyzed. -The froo path
and- the- -aboorDtibri--oe,6ii!4iition-'ci.f- th1#-aoqpone4in_-load_-ves_
ted and anplar-distriVuti I)a of aingular aosmic particles was
studied. The results are presented in gr4pho and a table* Light
raferencep:~ 2 Zrerioa--2- (_ __-
Italian 1940 -1952)-,,
1- graphs-
Ivstitution~ i Aoade of Sos.s UM, T A.-00-M31(vin Radia,tlon-Institute-~;,
Ito
Presented by i Aeademiaian P.-I. Lukirskiy, October 9m 1934

MMIOV, A. P., KARTUYANSKIY, A. L., KUZ'MIN, V. N., RYM,.OVA, I. V., FEDOMV, P. I.,
and SHUR, L. 1. Moscow, USSR.
"Preparation'Des Ehmsllons Nucleaires et Mecanisme re Leur Sensibili satin
ar La Triethanolamine."
paper presented at Program ofthe Second International Colloquitim on Corpuscualar
Photography. Montreal, 21 Aug - 7 Sep 1958.
Encl: B-3,114647-

SOV-.120-58-1-8/43
AUTHORS:Zhdanov, A.P., Kolpakov, M.I., Kuzlmin, V.N., Raguzin, R.M.,.
Fedotov.
TITLE: An Instrum6-.t for Measuring the Gap Lengths in the Tracks
for Particles in Photo-Emulsions (Pribor dlya izmereniya.
Pr08vetov v trekakh chastita v fotoemul'siyakh)
PERIODICAL: Pribory i Tekhrika Ekeperimenta, 1~)58, Nr 1, pp 46-47
(USSR)
wh!"
ABSTRACT:. The instrument is in form of an eye-piece in ose
fi6ld o'f:_view_one,sees asiia.16, a pair..of parallel- lines
and the usual- crosswire. The cross wire is set parallel to --------
the track and the gap defined by the two parallel wires is
moved along the trac.-,. This motion is achieved by means of
the two micrometers shown in Fig.2. The motion of the-two
micrometers is independent of each other. There are 2
diagrams, no tables and 3 references, one of which is English
Card 1/2

SOV-120-58-1-8/43
An Instrument for Measuring the Gap Lengths in the Tracks for
Particles~ in Photo-Emulsions.
and 2 Soviet.,
ASSOCIATION: Radiyevyy institut AN SSSR (Raditui Institute of the.
Academy of Sciences USSR)
SUBMITTED: June 22, 19570
1. Partiolea-Photographic analysis 2. Particles--Penetration
Measirament 4. Optical,instruments--Applications
Card 2/2

05461
SOV/120-59-3-32/46
AUTHORS: Zhdanov, A. P. and PeMMQy,_~~
TITM; The Use of a Diamond Dust Suspension in the Study of
Nuclear Disintegrations on Carbon (Frimeneniye
suspenzii iz almaznoy pyli dlya lzucheniya yadernykh
rasshchepleniy na uglerode)
PERIODICAL: Pribory i tekhnika eksperimenta, 1959, Nr 3,
P 133 (USSR)
ABSTRACT: Zhdanov et al. (Ref 1) have suggested that the inter-
action of various particles with the nuclei of different
elements may be studied by introducing these elements
In the form of suspensions into nuclear emulsions, The
size of such particles is usually 5-12 4. However, this
method involves a number of difficulties due to the
fact that the dust particles are opaque so that some of
the disintegrations which take place on the nuclei of
the emulsion itself may be taken as disintegrations on
the nuclei of the suspension, This effect can be
reduced by using spherical parIU-icles and by soaking the
emulsion in the vicinity of the surface of the particles
(Ref 2). However, disintegrations which take place in
Card 1/2 the immediate vicinity of the suspension particles are

05461
SOV/120-59-3-32/46
The Use of a Diamond Dust Suspension in the Sti;dy of Nuclear
Disintegrations on Carbon
still Lmpossible to separate from disintegrations on
nuclei of the element under investigation, since the
centre of a particular event cannot be seen againatthe
background of the opaque suspended particles, The
present authors have used a suspension of diamond dusb
-in their investigations of proton-carbon interactions,,
Diainond particles 5-10 11 in diameter are quite
transparent so that the above effect is removed. Any
doubtful events which take place under one of these
diamond particles can be looked at from the glass side
of the piate laing a long focus objective (31 x 0.6).
Several hundred disintegrations have been found which
are definitely due to disintegrations in the diamond
particles. There are 2 Soviet references.
(Note: This is.a complete translation)
ASSOCIATIONi Radiyev" institut AYSSSR (Radium Institute of the
Ac.8c.9 USSR)
SUBMITTED: February 24.) 1958
Card 2/2

21M SOT/56-37-2-10/56
AUTHORS: Zhdanov# A, P.g Fedotov P I.
Disintegretion of
TITLEs Result# of an Inv 'sotigat-I.on of the/6'arbon Nucleti Caused by
Protons With Energies of 660 XeV
FERIODICALi Zhurnal skoperimentallnoy i terorstioheskoy fizikit 19591
Vol 37p Hr 2(6), pp 392-390 (USSR)
ABSTRAM In the introduction the authors discuss the method of investi-
gating the interaction of high-energy particles with light
nuclei (0, N, O).by means of nuclear emulsions and the dif-
fioulties occurring hereby. The results obtained by several
earlior papers are mentioned. Like in a previous paper (Ref 6)
the authors used a diamond duct suspension for the purpose of
investigating the (p,C) intoraction. They used three-layer
emulsions (layer thickness 15-20 M, site of particles 5-7 (A) -
Two types of emulsion were used - the type D for recording pro-
tons with 16-20 Xev, and type 5 (relativistic emulsion). Ir-
radiation with 660 Mey-protons vas carried out on the Ihauotron
of the Ob" 'yedinennyy institut yadernykh issledovaniy (Joint
Institute of Nuclear Research). Invostigation results are shown
Card 1/4 by 2 tables and 4 diagrams. 540 disintegrations of carbon nuclei

DisintegratAon of sov/56-37-2-10/56
Results of an Investigation of the/-carbon Nuclei caused by Protons With
Energies of 660 MeV
were foundt 190 in S-smulsions and 350 in D-emulsions. The
average number of secondary tracks in C 12_ stars was det ermined
as 3 in consideration of the absorption of short tracks (mainly
a-particles). The correction was made by using the formula
NIN true ' 01/43) (112 _ 1 12), where N denotes the number of
72
reoorded trooks with a length 1, Ntrue the true number of
tracks with the range 1 (0-6 1 &&2fl, the mean radius of
the diamond particles MA). Tho distribution of disintegrations
according to the number of prmp and the nature of the reaction
is shown by 2 tables. Table 1 shows the number of tracks (1-8)t
the percentage of the total nuwber of disintegrations in each
case# and the corresponding crove section. Five-track dis-
tntegrations (34%) are the most frequent, next range the 4-, 6,
1, 2, 3, 7, 8 track ones. The m&ximum crous section is 78tO mb.
'Table 2 shows the distribution of stare according to the nature
of the reaction and tha respective cross sections. The absorp-
Card 2/4 tion cross sectiongIven as &mounting to 6 a - 227t12 mb for

Disintlegration of BOY/56-37-2-10/56
Results of an Investigation of the/C-arbon Nuclet,*1 Caused by Protons With
Knergieu of 660 MeV
650 MOV protons was obtained from a paper by Moskalev and
Gavrilovskiy (Ref 9). The following kinds of disintegration are
contained in table 2s G 12 (p pn )C 11,10 , C12 2p)tl 1110, 2p2a,
6 P2~ 6 6 (P'2pn 5
4a, 3a, paLi, 2pBe, 6p, 2p;a%,'3pLi, 5pale'j the highest per-
centage is attained by the type 2p2a with 32.6%. The data con-
tained in the table are discussed more in detail with respect
toparticles with Z :;0- Energy- and angular distribution of
secondary particles are shown by 2 diagrams respectively
(pigs 1029). The forward-backward ratio for a-particles is given
as amounting to 1-77�0.2 and for protons to 1.55t0.2. The
velocity of the recoil nucleus was calculated as amounting to
Y - (2-710*6),10 CM/000. The authors finally thank M. G.
Meshcheryakov and V. P. Dzhelepov, who made it poosible for the
experiments to be carried out, 0. M. Subbotina for hot help in
evaluating the experimental material, and I. M. Kuka for dis-
cussions. There are 2 figures, 2 tables, and 15 references,
6 of which are Soviet.
Card 3/4

Disintegration of SOV/56-37-2-10/56
Results of an Investigation of the/-Carbon NuclejA Caused by Protons With
Energiee of 660 JdeV
ASSOCIAT10Nj Radiyevyy institut Akadesii nauk SSSR (Radium Institute of *the
Academy of Sciences, USSR)
SURMlTTEDt March 219 1959
Card 4/4

ODOTOVI-i~-x-,
Application of the potential barrier criterion to the studY of
disintegrations In nuclear emulsions. Zhur.ekep.l teor.fize
37 no.4%944-949 0 159. (KLU 13:5)
1, Radiysyyy inatitut Akadevii mulc SSSR*
(Particle track photography) (Nuclear reactions)

11
__ -j-
OjAzlel
PEDOTOV, P. 1,9 Oand Phys-Math So~ -- 113tudy of theinter-
WPAJA%
actiodiftP high-energy protons =ddle nuclei of carbon*"
Len$ '1961. (Acad Sol U88R, Phye-Tech Inst Im A, F. loffe)
(KL, 8-61, 229)
- 52 -

HDAR-TV11 ASP*; FEDOTIOV, P.I#
Inelastic interaction of 660 Mov. protons and carbon nuclei. Zhur.
ekep. i teor. fit. 41 no.(:1870-1878 U '61. (11IRA 15:1)
Is Radiyevry Institut Ali SSSR.
I (Protons.-Scattering) (Carbon)

FEDOMV, P.I.1 KOSKULIKO, P.M., dotsent
Feed of a bit on the bottom of a borehole for standardizing the
drilling process. Sbor. nauch. trud. Kaz GKI no.19:103-lo8 16o.
(KIRA 15:3)
:(Boring machinery)

FEDOT'OVP.,P,,#Ie; KURMANKULOV, Ye.M.1 BRICHKIN, A.V.t prof.
Vibrating automatic feed. Sbor. nauch. trud. Kaz GMI no.19:167-170
,6o. WRA 15:3)
(Boring machiner7)

FEDOTIOV, P.I.; FAVORSKIY, V.V.0 dotsent
Hydraulic vibrating automatic feeder. Sbor. nauch. trud. Kaz GMI
n0.191202-207 160. (MIRA 15:3)
(Boring machinery-Hydraulic drive)

6 00
AUTHORS: Zhdanov, A. Pop Fedotov, P. I.
31785
8/05 61/041/006/033/054
BI 25YBI 02
TITLE: Inelastic interactien of 660-Mev protons with carbon nuclei
PERIODICAL: Zhurnal sksperimentallnoy i tsoreticheskoy fiziki, v. 41,
no. 6(12), iq6it 1870-1878
TEXT: This article deals with the applicability of the nuclear model of
R. Serber (Phys. Rev., 72, 1114, 1947) and M. Goldberger (Phys.. Rev., 2,
.L
1469, 1948) to the calculation of an intranuclear cascade in light nuclei.
The most important differences between inelastic interactions of high-
energy particles with light and heavy nuclei are as follows: In cascade
processes in a light nualeusp both nucleons and complex particles
(presumably alpha particles) participate. This assumption will be
discussed in detail in a later paper. -The resonance effect can be
neglected when calculating the intranuclear cascade, since the excitation
cross section of levelp with U >10 Mev is not greater than 1% of the total
inelastic scattering cross section. The "losses in range" of a nucleon in
the nucleus are studied for different collision parameters. The nuclear
Card 1/4

3118i
S/056 61/041/006/033/054
Inelastic interaction of ... B125X10
cascade was calculated using the distribution found by the Meshcheryakov
group (L. S. Azhgirey, I* K. Vioroy, at alo I ZhETF, L6, 63, 1959) and
allowing for the production, absorption, and scattering of pione from
nuclear nucleons. About 500 interaction events of 660-9ev protons were
evaluated by the Montejtrlo method for constant and variable densities of
nuclear matter in th a 6 nucleus. The absorption cross section for a
nucleus of constant density was 220 millibarns, atd that for a nucleus of
variable density was 235 millibarns. These theoretical Talues correspond
beat to the experimental cross sections of V. 1. Moskalay and B. V.
Gavrilovskiy (DO SSSR, 110, 972, 1956) for the interaction of 650-MOT
protons with various nuclei. The quasi-elastic pp and np scattering cross
sections, calculated by the model of radially variable nuclear density,
agree with experimental cross sections. According to M. G. Meshcheryakov
at al. (L. S. Azhgirey at al., ZhETF' 36, 63. 1959), the proton energy
spectra obtained when bombarding various nuclei, such as carbon, exhibited
a distinct maximum at high energies. which corresponds to single quasi-
elastic collisions of protons with nuclear nucleons. The angular
distribution calculated for _C12 is not essentially changed by allowing for
6
Card 2/4

8/056/61/041/006/033/054
Inelastic interaction of ... B125/B102
radially variable nuclear density. When comparing theoretical and
experimental energy and angular distributions$ it should be considered
that (1) intsraotione in calculated opectraq in which the excitation
energy U of the residual nucleus after the emission of one or two
cascade protons does not suffice for the emission of at least one proton
or alpha partiole, are to be negleotedl (2) 'charged pione must be taken
into account in calculated spectra. Under these circumstances, the total
number of cascade protons and the general shape of the experimental
spectrum for Q / const'are in satisfactory agreement with the theoretical
spootrum.L This is confirmed by a comparison of experimental and
theoretical yields of residual nuclei with the distributions among the
excitation energies followinS from an analysis of spallations on carbon
nuclei. V. V. Chavchanidze is thanked for comments, G. M. Subbotina for
assistance# L. I. Shur and I. V. Ryahkova for photoemulsions, as well as
Vs N. Kuzimin and I. M. Kuke for discussions. There are 5 figures,
2 tableso and 22 references: 8 Seviet and 14 non-Soviet. The four most
recent 'references to English-language publications read as follows:
M. Rotenbergt Le Wilets*,Phys. Rev., 110, 1126t 19581 H. F. Ehrenbergj
R. Hofetadtorl U. Heysr-Borkhout, S. F. Sobbotka. Phys. Rev.9 Mt 666#
Card 3/4

SA /041/006/033/054
Inelabtic interaction of ... B125PB102
19591 J. D-IDowell, W. R. Frisking G. Martelli, B. Musgrave. Proo. Roy.
800of Up 24t 19601 N. Metropolis et al. Phys. Rev. 110, 204, 1958-
'ASSOCIATIONi Radiyevyy institut Akademii nauk SSSR (Radium Institute of
the Academy of Sciences USSR)
SUBMITTED: June 24# 1961

Ceqexxe
Table I
Na epHutuT 46�tO. 54�12
Pmer (P const) 17�3 19�3
Patqrr (p const) 33�5 33�6
Card 4/4

B/05 62/043/003/016/063
B102YB104
AUTHORO: Zhdanov, A. F,j Fedotov, P. I.
TITLE: Cascado alpha particles from carbon nuclei disintegrated by
660-Mev ]protons
PERIODICAL: Zhurnal eksperimentallnoy I teoreticheskoy fiziki, v. 43t
.no. 3(~), 1962, 835-838
TEXT: The energy and angular distributions of a-particles produced in V
12
C disintelration induced by 660-Mov protons are compared with the spectra
a~ calculated for Antranuelear a-cascades. The number of cascade
a-particles per disintegration was experimentally deteimined to be
0.15 1.0.02,.theoretically 0.09 was obtained. This divergence Is
attributed to the difference in the number of a-particles emmitted between
0 and 300. In this angular interval more than 50 % of all cascade
a-particles are emitted,(calculation: almost Isotropic distribution
between~O Lnd 900). An.analysis of the spectra shows that about 70 % of
the cascude a-particles of the experimental spectrum are due to direct
Card 1/

X
S/056/62/043/003/016/o63
Cascade alpha particles from... B102./BI04
interaction between the* cascade nucleons and the intranuclear a-substructure.
There are A fieures.
ASSOCIATION: Radiyevyy institut Akademii nauk SSSR (Raditim Institute of vi
the Academy of Sciences USSR)
SUBMITT~ D: April 14, 1962
Card 2/2

L 19649-63 .:AFFTC/ASD
ACCESSION NRs 'AP3007061. S/0056/63/04~/003/0455/0459 i
AUTHORS:
:Zhdaftov, A. P.1 Fedotov, P. 1.
tXTM: ke esidual n, Cie ilproduced.in the interaction of 660
pf r
.pa
MeV protons with carbon nuclei
4
...SOURCEi Zh- Ocaper. i teoret. fiziki, v, 45,.no, 3, 1963, 455- 59
TOPIC TAGSt carbon nuclei, disintegration induced by protons,,re-
sidual mucleus decay, cascade process
ABSTRACT: The,experimental and calculated excitation yields and
iidual nuclei pr6duced after terminaikon of the cas-
energies of red
cade process in the C12
nucleus have been obtained from an analysis
of disintegrat~ons produced on'diamond particles irit,roduced in emul-1--
sions. The analysis is based on the assumption that the-possible
final states have a frequency of occurrence that is-proportional to
their statist.-Leal weights. The calculations agree well with experi--.'
Card

L 19649-63
ACCESSION NR: AP3007061
ment. "The authors are grateful to OR MR. !j~q for g at helps*
Y,4jnqhile re
in peiforming the measurements and calculations# to L* 1. Shur for
preparing the emulsionse and to VA-"U-1110 and 1. X. Kuka for
diSC=Sions." Orig.-art. has 1 figure, 3 formulas,--ain 2 t4les,
ASSOCIATION: None
SUPA14ZTTED: 22 Mar 63 DATE ACQs Q80ct63 ENcvt,
SUB CODE: PH NO REP SM 005 OMER: 003
Card 2/04

0
FNDOTIDV , P. 1.
.1 11w..Awm .... "....WWWO
Aboorption of stopped ff-mesons by cazbm nuolai. lAda fiz*
2 no.3s466-470 S 165. (MRA..180)
.Afl-
f-

ACX NRi "6001153 SOURCE CODE: UR/03117/66/002/003/0466/0470
AUTHOR: Fedotov, P., L
OIRG: None
TITLE: MU absorption of arrestedf-raesons by carbon nuclei
SOURCE: Yadernaya flzika, v. 2t no. 31 1965l 466-470
TOPIC TAGS- pi meson, photoemulsion, particle interaction, fast particle, charged
particle/ rw4&v-
ABSTJRAC!~. Th
thor investigates the-absorptiort c-fTr-7-mescms by-carbon nuclei -- -----
__Plamond pi ticle about 7ain diam.),were introduced into the nuclear phatoemulsions for
interaction wl-th the carbon. An emulsion chamber (10 x 10 cmQ) was designed, consisting
of 70 layers each 400z--thlck of type K nuclear photoemulsion. The dimensions of this
chamber made it possible to observe the fastest charlMd particles generated during the
capture of the-Ir-mesons until they were completely at rest. The spallations due to the ar-
rest of the _W --racson in a diamond particle were taken for analysis. The emulsion
chamber was irradiated by a beam of 80-MeV11--meoons plane parallel to the emulsion
layer on the OIYAI synchro-cyclotron. The mesons passing thrixigh the emulsion were
slowed down to a position of rest The ma)dmum number of mesons at rest was located about
6 cm from the spot th(- mesons entered the emulsion layer. The transparancy of the diamond
particles made it possible tck completely do away with the effect of the "Indeterminate zaaes"--

7 ZIMM
ACC NR., AP60011531
-which leadsto vonsiderable-mixtures-of spallations -from -other elements contained in-the..---
emulsion. On the basis of an analysis of 520 captures of W-me sons by carbon nuclei, -it
is shown that the share of the "one-nucleon" absorption does not exceed 16% lUe ex-
imental data agree with the asemption of the two-nucleon mochanism of the capture of.
-mesons. The probability of capture of .171-- -mesocts by np- and pp-pairs-Is estimated.
Author expresses his gratitude to-A. P. - Zhdanov for Interest in the work, V. P. Dzhel
and Yu, - D. . Prokoshkin for c at-'_t?g-tn setting uex e L. L Shur andN._V._--
]VOke- _p_r1tqent;t_ -_ '1~
ub-sequent-fin the emu on ohat ~berr
-Skirde for-assista e-in-the-'manufacture- and- s _ __ Ishtnj~o(
andO. Przhesmit! ula, G..N. Zhikhareva, andA. A.;'Ij.
Blyu in- or assistance in examining Se emulsion layers and tho measurements. OrIg.
art. has: 2figUres.
SUB CODE: 120/ SUBM- DATi8i 'O'Mug64/ ORIG REF: 007/ OTH TLEF.. -007
7,7
N
Z.
N.
'74
vo
a
SL
a TZ

FEDOTOVp P.M.
improving the working conditions. Put' I put. Moz. 7 no.11:29 163.
(MIPA 16:1-2)
1. Nachallinik Ivano-Frankovskoy distantaii.

CRIZHOV,D.G.; EDOTIV.G.I.; LAVRMMIKO.K.D.; SJIMIN, S.A.; MMLASOF,A.K.; rVANOV,
H.I.; UPAYOV,H.Ya.; GRISHIN, I.I.; KOEMIN,M.F.; Pa?GV.V.A.; ZAGCIROIXIM,
P.I.; YMCToT._P.N.; WIRIN, A.V.; F(iKrcmw, G.i.; YmHov.p.r.;
tmsHdmyA-1-(o-v7n. OV,S.G.; LWIN, I.S.; LBTUCM,L.I.; KOKUM.
S.V.
Ilikolai Alekissevich Andreav. Enargetik 4 no.9:40 S 156. (KLRA 9:10)
(Andreav, Mikolai Alekasevich, 1896-1956)

V, P. V. MANKIMI, I. P.; BAYANOVA, M. G.
Types of Diphtheria Cultures in Material From the Town of Frunze and Their
Connection to the Clinical Cource of the Disease," Zruly Instituta Epideviologii i
Mikrobiologii Ministerstva Zdravookhraneniya Kirgizskoy SSR, Frunze, Vol 1~ 1951,
pp, 26, 29. ,

FEDOTOV, P., V.# "Bacteria dissemination by toys and methods of do-
contaidnating them," Kirgiz State Medical Inst, Fruze., 1956.
(Dissertation for the Dogma of Candidate in Biological Sciences)*
SO: KnithnM letopis', No 23p 1956

FKDOTOV, P. V. Cand Biol Sai -- (dies) "On certain f actorsi oontrib n to I/
- 0
the spreadft of infection in children's collectivesi%nd measwes Of
Molotov, 1957. 16 pp 20 om. (Molotov Mod Inst). 175 copies (KL, 24-57, 117)
-27-

q-"DOTOV, P.V.j BAGYSHBZKOVp A.B.
Experimental.effect of Acidophil-milk on certain. protective functions
of the.organim. Repor.t No.l. Sov. zdrav. Kir. no.1:30-33 -TaY 162.
(KM 1514)
14-Is Kirgisakogo instituta epidemiologiip mikrobiologii i gigiyeny
(direktor -,kand.med.nauk V.H.Perelygin).
(KEUO ACIDOPHILUS-PHYSIOLOGICAL EFIFECT)

PEDOT072 P.V,; G0HYACHIKHj I.A#
Aoidophilus milk-it the prevention of intestinal infections and
diewmeo of the respiratory tract of emall children. Sovzdrave
Kir. no,.2124-28 Mr-Ap 263. (HIRA 1615)
1, Ts.Kirgisokogo instituta epidemidlogiiq mikrobiologii i gigiyany
W~. - kand.med.nauk VeH. Perelygin) i kafedry detakikh bolesney
(zav. - prof. B.Fa. Shagan) Kirgizalcogo gosudarstrennogo meditsin-
skogo institute, (rektor - chlen-korrespondent AN Kirgizekoy SSR
V.A. Isabayeve.).
(HIUj ACIDOPHILUS) (INTESTINES-DISEASES)
(RESPIRATORY ORMNS.-DISEASES)

FEDOTOV,-~ P.V.; KOZFOZGWIDV, T.A.; MAMYTOV, B.M.
Chemical c4m of maksym,
position and antibacterial properties
the Kirghii national beverage* Sove zdrav* Kiro n0-4/5&85-89
J1-0263 ("Alm 17:1)
1.IzfKirqizskogo, instituta spidemiologii, mikrotiologii i
gigiv.eny ( dlr. - kand. mad. nauk V.M. Perelygi:a) I,kafeiry
giglyeny sanitarnogo fakultteta ( zav. - dotaent B.M.Mamytov)
Kirgizakogo, gosudaretvennogo meditsinakogo instituta.

-a I)r p ~I
zh# Biologiya. Sv. t.# Abs. 22B125
Via K-6,ou ~W&j 'Jo%
r1ri ain't a al a tipirvi t t I tin ayiA brittbmatoplal nrontirtian of tho
-a L- -- o nall ar nK maksym"
Q pq
ATM 2, Cj(%V. gdjavoold2r ~, Kirgislij nt--,
ol thc-~ YInahiz nQtional drink makcs7m'o were investt-ated, All the
TI
ma
-.nd ii ta phylococa I The antiblotIc tffect isq 1101 .21":j "i r.
SUB CODE: Ls ENOL 00

49'
STARTSBV$ Do,- KOLESM, So, saslusbannyy doyatell nauki; BOMUp To;
KHORMHOM, Do; SKURDMINp I.;KHOXEMOT, To.; BUTAXOTp I.,
.dvaxbdy Oeroy Botsialisticheek-ogo Tim&; TRUINOT, As; SMANT9 IF.-,
'FAMOTO So
The roeA toward now achievements, Sots, trud, nolokI4-36 Ap 158,
(KM UW
Is' 1tarehly ekonoulet 12outrallnogo, planovo-okomomichestogo upmv-
lenlya Ministerstva sellskogo khozyayvtva SSSR (for Startserl.
2. Chlon-korrespondent Teesoyusuoy aladoxii sellskokhozyaydvenarkh
uaukim~ V.I. loulta (for Kolesnev)o 3. ZavedurtAhohly sektorou okono-
micheekDgo atimlirovaulys eel lelcokhosyaystvamcgo proisvodstra
Vueecy=noy- akadoxii eel Iskokhozyaydronufth mwk im. V.1. Ionica,
(for BOML 4o Zavedaushohly eel Iskokhosysyst-rounya otdolou
Noskovetogo komiteta Kommistioheskoy partil 3cmetskogo Soyusa
(for Xhorokhoriu)e 3,' Zureduyubehly kafedrov ekonomiki i organizatsil
eel 1e1cDkhozyaptvbuuogo proisvodetva Ivanovskogo soliskokhozyayntven-
nogo Institimta, (for 31mrikh1u)o 6. Vadhalluilc SiMsiallnogo konstruk-
torekDgo byuro sayoda sellkhosmashin im Ukhtome).ogo (for Miokhlov),
7. Predesdatell kolkhosa "Term V ITanovakogo rayon&$
Iva novskoy. oblasti (for Trofimov a 8. GlarW sigronom Ramenskoy
medtdimo-traktoruoy stanteft (for Atepanov), 9. Sekretar,Partly-
noy organizatsit Rmenskoy mshinxi4-traktornoy irtantsit (for
Fedotov). 10. Predeedatell kolkhoza im. Vladimira Illiaba (for
(Mohine-tractor stations) (Collective fame)

FUMVVI S.
- - .. -_.- _11.viopla ', a.nd deeds. Mast. ugl. no.10:24-25,24a,-:14b 0 159 (KM 13:3)
(Chelyabinsk Basin--Goal mines and mining)
0

FEDOTOV S
Combined section. Sov.shakht. 10 no.3:34-15 Mr 161*
(MIRA 14:7)
I. SW:hta No-5# VOlYnOkaya oblaot'.
(Coal mines and mining)

FEDOTOVI S*A*, Inzhe po mekhanizatali
Contribution of ihe innovators. Pat' i put. khoz. 7 no.n:30 163o
(KIRA l6tl2)
-4?

GOSTEV.. M.A.j FEDOTOV, S.A.
Spectral characteristics of the foreshocks and aftershocks
of the catastrophic earthquake of November 6, 1958. Izv.
AN SSSR. Ser. geofize no-5:675-U7 My 164. (MIRA 17:6)
1. Institut fiziki.Zemli AN SSSR.

USSR/Gecypbysics Conference FD_ 762
Card 1/1. Pub 44-10/1.1
Author Kirillov, F.
Title Chronicles.- Conference of young scientists of the Geophysics InAitute,
Academy of Scientists ofthe USSR
Periodical Izv. AN SSSR, Ser. geofiz.) 495-496, Sep-Oct 1.954
Abstract May 17-20, 1954, the Geophysics Institute held a conference at which
junior scientific workers participated with 18 reports; e.g. Ye. A.
Lyubimova (heating of.the Earth), S. L. Solovyev (intensity of
earthquakes in Turkmenia 1912-1951),,S. A. Fedotov (wave hodographs),
Yu. I. Vasillyev (use of amplitude d~t-a-li"iw~s"erii*m"f'c'*prospecting), 0. G.
Shamina (elastic impulses during collapse of rocks in earthquakes),
Q. I. S12ayeva (velocity of propagatlon of elazitic waves in granite,
marble) etc.), V. I. Tatarskiy (propagation of waves in medium with
random weak inhomogeneity of refraction coefficient), L. P. Zaytoev
(reflection of waves from boundary), A. S.Chaplygina (measuring the
~thermobaric field in the atmosphere by statist",cal treatment of empiric
data).
Institution
Submitted

Approximate method for calculating dynamic hodographt, of waves
refracted on curvilinear boundaries, Trudy GeofIz.Inet,.no.35t51-
07 156. (MMA 10: 1)
(seismic waves)

ESDOXV, S.A.
AUTHOR: Kirillov, F. A.
49-3-13/16
T'ITLE: Conference of junior research workers, engineers and
aspirants of the Institute of the Physics of the Earth,
Ac. So., U'*'S.S.R. (Konferentsiya mladshikh nauchnykh
sotrudnikov, inzhenerov i aspirantov Instituta Fiziki
Lemli AN SSSR).
PERIODICAL-~ "Izvestiya-Akademii Nauk. SejjZa Geofizicheskayan
(Bulletin of the Ac. So., Geophysics Series), 195?,
No. 3, pp. 411-415 (u.s.m)
ABSTRACT: The conference was held on December 24-26, 1956, 21
papers were read relating to work completed in 1955 and
1956. In this report the contents of the individual
papers are briefly summarised. Fedotov, 'S.A. read a
paper on the kinematic and dynam:1d-r�NUu-ret;-oT waves
refracted at curvilinear boundaries.

49-~3/18
AU~LTOR: Fedotbv, S. A.
arrival time of
TITIS: Dynamic features of reflected wavest the c-sobennostyakh
which is not a minimum. (0 dinamicheekikh
voln, vremya 'orikhoda kotorykh ne yavlyayetsya
otrazhennykh
minima,linym vozmozhnyx vremenem).
PERIODICAL: "Izvestil a Akademij Nauk Seri ra Geof J.zicheska an
B u 11 9 _e -71 ~g M.L,~ ZC.. "M I - 5, 0 9 .59
,~~ UT '.R'
pp-575-!?CMU~-9- ;.
ABSTRACT: The dependence of the type of ;Scillations on the type of
the extremum of the wave's arrival time is discussed on the
basis of results obtained by the author, summarizing also the
work of H. Jeffreys (3) and of Anderson, Northwood and Barnes
(6,7). Anderson et al. compared records of reflected wa7es
with maximum and with minimum time paths. In this paper
minimum path reflections and maximum-minimum (or saddle point)
path reflections are compared. The work is based on the
observation that both maximum and mi-nim= ath reflections
change to maximum-minimum (or saddle points path reflections,
after having traversed a foeussing zone or caustic. A dis-
advantage of Andersonis method is the use of a coincident
transmitter and receiver; when these are noved, the distance
from the transmitter to the reflecting surface is varied and
Cmcdl/5 so is the relation of the curvatures of the incident wave
front and of the reflectJng surface; the directional pattern
Dynamic features Of reflected waves$ the arri,
which is not a minimum. (Cont.) 49-5-3/3.8
Of the transducers is ogive al time Of
experiments apparatus was shaped.
Geoph. For the seismic
model
ysics Institute Of th used which was developed by the
AN ~83R) and described by e USSR Ac.Sc.(Geofizicheskii Inst.
Riznichenko
this is Similar to Andersonts
ultrasOni YU*V- et al.(8-10);
differing experiments were made. The
ments was c aPparatus.
on Passing to check whether the shape first series ofSixteen
through a
focussing zone. For llations chanZes
ments were made along one ray Of the of 08.31 experi-
focussing zone, where the ray was that al t12'8 Purpose meas
path and ted wave before the
after the focussi refle1% ur
ng zone, where 0119 a minimum
tj,e time
s0"urimum_min-'mum Path. In these experiments
ceq the shape Of the reflec Same ray was a
ating.
Point were always the Same; the wave alwaE; the position of
receiver under the same angle -urf.,,C, the
arrived at the
directional Pattern of the pi? and the reflection
considerably in vari ezwhch is imilortant since the
ocrystal receivers differs
Of the Oscillations -0u8 directions.and,
angle at which re therefore$ the pattern
card 2/5 gistered depends considerably on the
ing surface was the wave arrives at
in which the Observations were made the receiver. The reflect-
a cy"nd-rically bent brass sheet. The Plane
was perpendicular to
the

49-5-3/18
Dynamic features of reflected waves, the arrival time of
which is not a minimum. (Cont.)
generatrix and passed through its middle, so that the
problem was essentially a two-dimensioaal one. The relative
position of the transmitter and receiver were experimentally
determined so as to avoid interference bet%een the reflection
(after it had passed the focussing zone) and other arrivals
and to make the reflection sufficiently strong. The path
of the rays and the position of the caustic were determined
graphically. The seismograms show the reflected ray before
the focussing, travelling along the minimum time path with
developed "code", the same ray-passing through the caustic
where, due to interference, the amplitude decreases and
finally behind the caustic, travelling along the maximum-
minimum path where the "code" becomes weaker and shorter.
In accordance with the triple-valued travel-time curve,
the reflection from the bottom of the reflecting surface
is preceded by two reflections from the slopes of this
surface, travelling along minimum time paths and arriving
almost simultaneously; with increasing distance, the
resolution of these reflections from themaximum-minimum
Card 3/ 5reflection improves. In seismic prospecting, when waves
are reflected or refracted by curved surfaces, they are
focussed and dispersed. The evaluation of seismic prospecting

49-5-3/18
Dynamic features of reflected waves, the arrival time of
which is not a minimum. (Cont.)
results is based on the assumption that seitamic energy
propagates along rays However, the type of waves passing
through a focussing z;ne is changed and thezefore in the
second series of the experiments the aim wa13 to check
whether, in spite of this, the amplitude of waves can be
calculated approximately on the assumption of their propa-
gation in the form of rays. The second series of experi-
ments was made with similar equipment to that used in the
first. A triple-valued travel-time curve was plotted on the
surface of water above the curved reflecting surface, where
the arrivals were sufficiently resolved. The amplitude of
the third arrivals was experimentally determined and
compared with a theoretical curve, calculated on the
assumption of ray propagation of seismic ener&7. The cal-
culation method is given; it is based on the determination
of the directional pattern of the transduce:~s. It was found
hat both curves are very similar, which confirms that
C&vd4/5 seismic energy prc-oagates along rays both in and beyond the
focussing zone. Tt,3 paper contains 9 figures and 13 references,
9 of which are Slaric.

49-5-3/18
Dynamic features of reflected waves, the arrival time of
which is not a minimum. (Cont.)
SUBMITTED: December 22, 1956.
ASSOCIATION: U.S.S.R. Ac. So. Institute of Physics of the Earth.
(Akademiya Nauk SSSR Institut Fiziki Zemli).
AVAILABLE: Library of Oongmss
Card 5/ 5

FEDOTOV9 S.A. Cand Phys Math Sci (dies) N Concerning
kinemqtic and dynamic of seismic waves
refracted on.curvolinear boundaries." Moa 1958v lDpp
(Acad Sci USSR* Inst of Physics of Earth) 100 copies
Mt 21-58,, 87,88)

OV
?p2j-.~~J,A
Kinamtio and dynamic features of seismic waves refracted at
curvilinear boundaries. Izv. AN SSSR. Ser. geofiz. no-1:174-175
Ja 159. (MIRL 12:1)
1*Uohenyy Sovet Instituts, fisiki Zemli AN SSSR.
(Seismic waves)

"Seismicity of the South of the Kurile Islands."
report sifomitted for the Second World Conference on Earthquake Encineering, Tokyo and 40t0,
Japan, 1l-18 July 196o.

FEDO%V, S.A.i AVERIYANOVA, Y,N.; BAMASAROVA, A.H.; XUZIN, I.P.;
TARAXANCV, R.Z.
Sems results of a detailed'att* on the seiaml-city of southern
Kurile Islands. IzvoAN SSSR.Ser.goofit. ro.5:633-642 My #61.
(KLRA 14:4)
1. Adademiya nauk SSSRp Inatitut fitiki Zemli,
Mrile Islands--Seismometz7)
mmpmmmgm~j awn

ARKHANGF,LIS,KAZA, V*M#j YejDOROVp S*A,
scow results of studier. on the attenuation of Rayleigh surface waves.
Izv. AN SSSR. Ser. geofit. no.8:1122-3-131 Aj 161. (MM 14:7)
1. Akademiyz nauk SSBR, Inatitut fiziki Zemli.
(Seismio waves)
IN'R

AVF.RIYANOVA, V.N.1 FEDOTOV, S.A.j FERCM p M.D.
Preliminary data on the earthquake and tiumuzdo of November 6p 2958.
Biul. Sov, po asioms no~949-" 161. (MIRA 14:4)
Kurile tolands-Earthquake, 1958)
~Xurile Islands-Tidal veve, 1958)

-8/169/62/000/009/029/120
D228/D307
AUTHORs Fedotov, B. A.
TITLE: Some kinematic and dynamic peculiarities of seismic
waves refracted at curvilinear boundaries
PERIODICAL: Referativnyy zhurnfLl, Geofizika., no. 9, 1962, 28t
straot 9A188 (Tr. Sakhalinsk. kompleken. n.-i, in
no. 10, 1961j 131-146)
TEXT: Head wave peouliaritisel related to the boundary curvatureq
are considered. The case of one curved refractIng bounda;ry was inve-
stigated, the observation surface being flat aqd-the seismic wave
propagational velocities constant. The boandaryle-risee and hollows
were considerably greater than the wavelength. The refracting*wave
was assumed to slide along the*boundary. It is shown that seismic
waves# refracted at curved boundariesq have essential kinematic and
dynamic peculiaritiest hodograph loops, wave-duplicates and multiple
waves, sharp amplitudinal changes in consequence of the effects of
-the focussing and the dissipation of energy. The greater the depth
Card 1/3

3/169/62/COO/009/029/120
Some kinematic and ... D228/D307
of the boundary, its slope angles and the value of the critical
angle# the larger the hodograph loops. The probability of thei:~ for-*
mation increaues as the medium's velocity differentiation increases.
Wave-duplicates arise as a result of a wave falling at tile critical
angle on several points of the boundary. Their probability of ap-
pearance, their number, and the time intervals between them increase
as the boundary's depth, the hollowel-curvatare, and the critical
angle increase. In deep concavities, when the alope angles consti-
tute approximately 9100-1c9 approximately horizontally-directed
seismic waves can fall on the boundary at the critical angleg giv-
ing rise to multiple refracted waves. The larger the bounda3~yls
slope angles and the lower the medium's velociiy differentiationt
the higher the probability of appearance of such waves. In the
three-dimensional case there may be two more effects: 1) The "break-
ing away" of the hodographle loop from the firat arrivals' hodo-
graph in consequence of the fact that the geometric site of.the
boundary's pointet whose rays reach the given profilet may consist
of several lines having no common points, 2) Distortions (increase
Carl 2/3. 0

8/16 62//000/009/029/120
Some kinematic and D228YD307
in the arrival times) of nonlongitudinal hodogrEphs in consequence
of the boundary's curvature between the detonation point and. the
nonlongitudinal profile. As a result of the effect of 'the seismic
energy's focussing hnd dissipation the amplitude graphs of refrac-
ted waves can have a sawlike-form even over gentle weakly undulat-
iug boundaries. These effects depend on the-curvature of the boun-
dary's sections and on its depth. The third arrivals, which repre
sent a wave from the bottom of a holloq that has passed the focus:
.sing zonel possess the maximum intensity within the hodograph's
loop. The author notes that all seismic boundaries are variously
curved, and that all the peculiarities considered can be observed
over them of the boundary's depth is greater than the radius of
curvature of its concave elements. Waves, reflected from curved
boundaries, also have analogous kinematic and dynamic peculiaii-
ties, 23 references. /-Abstrac*ter's note: Complete tranBlation._7
Card 3/3

DV S As
~t~ojl
Dstftuinizg th'S MSA Of the mi9b of tm=ti ftring the IMOMtka
Earthquake of November 4,, 1952 and the Itamp PArt*MAO of jjoyember
60 1958. IsveAX SM, Ber.geofis. no.10033-11439 0 162.
(KMI I# t2)
lo Tzatitut fiviki 2wU AN SWR,
(Imabatlm-ftw vxvo,, 1952) (Itump Talud-lidal vws,. 1958)

FEDOTM S, A,
Dot&LW oelowlogical research in the ooutka= kwile ISISM
Biulo HDI.Po Otdo goole 37 no.,4&133-134 ii-Ag 162. (HIBA 3.60)
(tnr:Uo IalwAs-4siomology)

L lo186_63 EWT(I)/BDS--AFFTC/ZSD-3--TF
49/i53/000/005/067n InKPA -
___$/0C
AUMM: Fjdd
74 TLE t_ Ve10_0LV__Sftfile -of MantleL in--the - area- at -the- southern- Wile
Islands
SCURM: AN Sin. Izve Seriya geofizichesksiya, no. S, 19i3, 670-W
TCPIC -TAM. selsmia-weve-yelmities, -u tle, MobodtacontinuitV
mW
AISIRAM, A xspld me _YU#
!-t-bQli-:to3~--matrue-tin"elt3city-profill.tS-U$iD& _V,
Blzatcheneo Is theoretical hodographs_ was investigated usiqg data frm the near.
suberustal ACLAW&AMW of the. southern Kurile Islands. TO avoid errors due to
irregularities -in -the. ~ - lctrusto --arriyal _timees -.were neasiwed- from-nes --the base-
of the crust 20 km below the stations. Corrections were introduced to compensate
for the intervening thlcLiwae of the crust. The accuracy of this method, with
correctlons for a depth of 40-50 km, mw + or _ 0. 2 se c; the. systematic error in
detenexing focal depth v .9A about 2 km* 'om theIbase of the crust down to 80 kmp
V sub go= 7 7 km/eec and V sub a in 4.4 km,75,ec, Velocity Laereases vith depth
below km: Outface waves indicate the existence of two -.ypes of structure of
card .1/2

. r -
,;, ~; ~ 1:1.~,~-,~, c li'll - 4.il ~4:6016ii
--I". ro
- ,----,",-,t- 1'2~42,n ", rl "
".-
. - - . ~ I ~ - tI :~i -l

L AQUI-63
AX,= - M, AP3009W5 S/OD49j'63/000/006/0629/0849
Mum MgWs A
53:
c lasalflcatlon ~of nesA7 gigagMakU of interme&ate f oca:, depth
ZMM AN SM. Izv. gar, geofizichasksyto no. 60 196,1, 829-849
70PIC TAGS: selsole vavosj, suberustal earthquakes,, upper mantle., energy
classification of earthquakes,, seismology of KwIle IslanIs
nothod-for-dtitei-miulng-fla-lomic -%we -absorption - In -the- upper- mantle
evaluated on the basis of earthquake data recorded in .1,956-1959 in the
v;uthtrn Ku--lle lalwAB. Th3 erergy absorptJon of tranavorse eeismic mes ~w
ft~,Lzr.id to be normal at depths of 2N-40 km,, to increase w; depths of 6o--no kn6
r-:%,l to reach a maxix= at depths of 80-90 km. These lata sug
,gest that magma
rchrvZers Wet In those formtions in vhIch Ixansverse wwre absorption is
;n,=milously large. With the velocity cross -vection and cbtta on transverse vnve
Ebsorption In the earth's crust and in the upper mantle, nomograms were
Cormtructed for the energy classification of earthqw3kes with normal and
Cr2rd 1/2

GCRYACM, A.V.; YERSHOV, 1,A,; NIRILLOV9 F.A.1 KUZIN, J.P.;
LTAMZINA, O.A.1 MOMVj B.T.; POPOVv V-V.; FEDO,TOV,, S.A.;
SHTErNBMG, Va..
Seimdo microsoning at. the Petropavlovsk-Kanchatshy area.
Trudy InBt, fiz# Us* 28.Vopo inob,. oeism. no.8:3-W 163.
(KMA 16: 11)
:4.

FEDOTOVj S.A.1 BAGDASAROVA, 1,N,; 1WZINp I.F.; TARAKANGV, R.Z.
Seismicity and the subsurface structure of the southern part
of the aro of the Xurile Islands, Dokl, Vi SSSR 153 no.31
'P.
668-671 N 163. (MIRA 17i1)
le rhatitut fisiki Zemli in. O.Yu, Sbaidta AN SSSR, Pred-
stayleno akademiken V.S. Sobolevym.

FMOTOV, S.A.j 14ATUMA., N.H.; TARAMOV, R.Z.,- YANOVSMA, T.B.
WON
Longitudinal vave velocities in the earth's upler mantle
In the region of the Japanese and Kurile Island.a. Ixr.
AN SSSR. Ser. geofizo no.W185-1191 Ag 1&4 (MIRA 17:8)
19 Inatitut fiziki Umli AN SSSR,

1.7007-65 WMAga(h) Peb LFWAM/AlM Gw
if 01% 100'. 1
hCCES91011, sit
'~UTROR* Fedetov~ 9. 1. : Kuiin- T, P- 1Rqbk ov k F_
Xq,
TITLE: Detailed atis oloxieftl investigations at Kamchatka
n 1961 and 1962
cMURCE: -AN GGGR. rzv*suy&. Scriya geofiricheakays, no. Q, 1964,
:60-13T5
TOPIC TAGS: seismic activity, aelsmological stationj P&cffic seismid
telt. deiamography, Kamchatka
A.BSTRACT: The.results or observations made at a netvork of seiamic
atmtionv cits:b1inhed 1~y & special Pacific seismic expedition to
~amchatka during'the period 1961-1962 are revtevcd. The instrumentsi
aethods, and techAiques of observatiou and data reduction vere eseen-
tially the east as those u-sed in an earlier ecpeditton to the Kurile
irtlands from 1958 to 1962. It hts beezi experimentally c-rt~blisbed
--c-ar-earthqu"es, with 10 are ele&rly recarded ELt distances
ef 200-300 ka. On the basis of the seismic tateriala gathered durilig'
first year at Kamchatka, it vas possible to compile a map or epl-
Ctrid 3

L 70-,W-45
ACCIVTS-iOli MIR: AP4045TBT
a M&P 0r wei-64XLC -at-ti-VLt-y (Vanle-44- Ol- e&r-t?I-,Ijmke- vith foci
0 f 10 ct a than 60 km), ft compound v~srtitai tont-inn, PnA a rr-_
.' J.' a ~ r a m A distinct earthquake btlt vau Ide itified runnina
r e . t a !, h F,- d e e p - v at e r I e p r e s s I on t h r o u g h t h ! tIps Dr tne Krono-
y nn d Ghtpunsk iy peninsulas southwes t to the 52 ~ latitude line.
xTAt. compouad vertictl sect-tart ithovw thitt this belt Is an outcrop or
the Pacific focal-zone which crosses the deep-vater depression and
the elevated Kauchatk&4' The -belt reflects the. L,,%teasive contemuorary-
nrocensea tmk ing pla-ce iG the earth ' nt Lns!it le %rhi !h led lo, th'r, devel-
~v-ert of the ioland arc and the deep -v&_'.f-r dc- p -e P: ;ion. -h- map of
indleatea that the deap-water deprt3u.on, tne sLrxicrure
ttle, E;I)Ipljnskiy peninsula and its unde-vater ette -,vion, and the
r~ Z 1 or, nr th'a K4meh4tka River ard bn--ior ! ng
1 n "~-easlyeLy te'iay. i_orrectioni~ v-, I T h
'_-C bade the
map of seismic zouLng of Kamchatka. On ;he east4ern shore of Kamchatka
the nine-point intensLty.z~ne should be (txpanded to include the town
of Orfg; arti hztit 8 rig,trea in-d 2, -,"ableab
M
ASSOCIATION: Akadeikiya nfLuk GRSRj Inatttut ftcCti, teall (Xc-4!t!ny of'
"i^ !Nrth
96 a P j_rjej jtqt o 2~f Ph s t~ V I !. ~Ibiy-akove otde-

L 7007-65
ACCESSroli IR: AP40MT
lemiy.e. Irstitut vulkano-logil (Silb-erlap )Wm_&rtmenl t I t-lita nt
SUBMI'MED; 26ju163 ATU PREGGi 3103 EXCL: 00
CODE1 Es RIr 90V: 025- OTHER: 00k

_)'Q4-Z4-66 C
E;Yr(Q /MfA(h_ a
IX NR: AT6ooTI94 WIRCE, CODE: UII/26iq/65/ooo/o36/0003/0033
KITHOR: Yershov. 1. Medvedev S. V. (Professor);~ ~edcrtov, S. A Sht
V V.
ORG:
TITLE: SeismicVIM croregionalization of Petrepavlovsk (Kamchatka)
SOURCE: ~~M_ SSSR. Institut,fiEjbLjjLejQ;i.; Trudyg no. .36 (203), 1965. BeYsmicheitkoye
mAroray6filrovanlye; vcr;rosy inzhenernoy seyamologii--(I;'eis--nic-mi--rodistrictlng;-'!-.-.-,-, -
-problems-of -ergineering--iiei-smoldgk)-,--,-n--o--.---I-O, 3-33
TCPIC TAGS: seismicity, seismic mapping, seismic survf-j, inicroregiormlization
APMUCT; The city of Petropavlovsk (KWhatka) lies in seismic -zone -IX-laccording- -
--to the nev-map- of seismic zonei-6k.the_ USSR), a few tens o" kilometers from tbe
Pacific Ocean seismic belt. The slope of the basin off southern Kwnchatka is one of
the most active segments of the circum-Pacific belt. The (!ity lies in the north-
eastern part of the Kurile-Kamchatka folded zone. The georiorphology and geology
of the district are described briefly. Investigations over a period of three years
(1961-64) by the Pacific Ocean Seismic Expedition of the 3nstitute of Geophysics,
AN SISSR, on Kamchatka have led to refinement of intensity data for Petropavlovsk
00imchatka) and -have permitted compilation of maps showing divisions of the city-. into
seismic uubdistricts. This work represents the first cinibined operation of instru-
ment work for such-detailed subdivisions of seismic districts. Data include
CarcL ~lZv-_ UDC: - 550-34

L__2P4247-66
ACC NRt AT60(Y7194
recordings of nearby earthquakes by.automatic equipment,measurements of-longitudinal
---ar!d transverse vave-velocitieti,---"d-ileasurements of mieroseisms. The work has-
furnished better data for compil Ing maps of seismic dintri:ts and for comparing
MeL
di.fferent %,hods of determining intensity increments by iastrumental. recording.
Different instrumental methods have shown rather good atgre,!ment. It is noted that
tle most valuable information concerning possible seisrdc activity may be -obtained-----
by- analyzing ground - movements from nearby earthquakes by nv-ans of automatic equip-
ment. An esocntlally new aspect of the maps is the delineation of zones with dif-
ferent spectra of earthquake effects on buildings and cther structuren. This is an
Important contribution to engineering practice in constructing earthquake-proof
buildings.--At many points in zones of scale IX along the Kamchatka coast and on the
Kuriles, geologic conditions of bedrock and soils are simi].ar to those in Petropav-,-
lovsk (K%mchatka). -The - saw technique of dividing Into districts has been followed,
but where instrumental data have not been available, characteristics of bedrock and.
soils as observed at Petropavlovsk have been used as the basis for delineating -
di;stricts. Orig. art. has:-* 13 formulaoq 14 figures, and h tables. [041.
SUB CODE, 08/ SM DATE: none/ OHIO RED: 034/ OTH RU ATD PRESST -2,z I
Card!

-L 2 -AA
AC
SOURCE CODE: Uf 1264/61/000/036/0061/0065
A
AUTH011%. Fedotov -13 A-
TITU% Bei=0109ical investiptions of tbe Pacific -Ocean 13elemic'fteditions- -4574
itute of the Physics -of the- C14 of Sciences in 195T-1963
WLIRCZ%,*AN SOOR In titut fisiki'Zowais Trudy, no. 36 (1?03)9 1965. Seys:micms"
bLikrorayonirovaniye; =rosy inshenernoy seysmologii (Selside -~ziorodistrictlng;
problems-of enigneerinF seismology)*_ n-0.10, 61-65
TOPIC TAM selasia oarth"am
ABSM(-,r: All projectalconducted by-tbe Pacific Ocean Seismic Wor;
De' eats Of Zng14eer Ing - Seiamology~ and: Eartbquake Pbysiee Institute of- he--
c - -Ear Ilk -are described briefly "Ckmillra I
the Ah , ), - Although e(,% of the e
'tie~:f*iet Union originate in the Khrile-Kamchatka, region, cnly three low magai-
h
fic.p~tion seismic stations were in operation here prior to the IGY. In 195T" using
deep Belsmic-sounding methods,tthe Pacific Ocean Complex Geilogical-Geopbysical Xx_!
'Ation of -the In began its vark, vhich vas mostly perforwd at sea. A seignologi
ped
c 4 team vas organized to conduct detailed seismological investigations in the South
er~ Kurile Islands. In 19599 the team was reorganized into tho Pacific Ocean Sei a
ftedition, which is still active, In X957-4958s the mein objective of investiss-
tion vaR to make a Astailed study of the seismicity and selitmot2ctonice of the
cat'd 1/1

--ACC-- Nits--- M~OOT19T
crust snd mantle, The'.Beismol.ogr Laboratory of,the VAkhal.-In Coglex 8 ientific-
-Res arihilnetitute. Siberian- Brancli-.- Ail 0689-A 16111) vx;r-k-el with th
lp-
est lish a nei;;&~_k-of_'_Av_e -sensitive seismic stations in the vouthern Xuriles
(September 195T). Continuous earthquake recording began on I January 1958. Up
to Veptember 1958, all stations were located on Iturup, Iolend, where stations were
establAshed on Shikotan and Kimashiro Islands* in 1959-1962, the principal assip-
men it of the TSE were tc study deep structures, properties of t te upper mantle, and
se,~ -the Wile Archlpeleigo. Detailed
,mic-conditionvin the4outhern-part of
mespurements were made of the severe earthquake ( M - 8.2) of (; November 2958 in. the
ocean off Iturup Island, with intensities of 8-9 which caused tsunami. Studies of
the seismicity and properties of the uppe-r-mantle shoved that-1he southern- Kurile
foclal -zone is -far more -compact - than: ko~rly believed and a ently is not a channel
-Ppaz
for them escape of magma from deep depths. A somewhat slower seismic wave velocity
Was found to exist in the upper mantle under the southern Kuriles and adjacent shelf.
The absorption of transverse seismic waves was found- -to increase at depths of
60-110 km, and the temperature in the upper mantle to be.bigher :in this region than
under the continents _. (by 100C at- depths. of -50-70 km). Mthodo - were developed for
engineering seismological observations with devices which were switched on-automati-,
cally when earthquakes- occurred and -for high-speed recordinii on photographic'Papers
Detailed seismological Investigations In, 'the-southern Khriles were essentially com-
pleted by the TSE in the summew of 1962.. Only"atudies of the v~?ectra of southern
-Kuriles earthquakes are still'being studied by the TBS. Obcervittione are being
continued by the S&kbXXII w1th fewer statl6niss In 19609 a tev aesitoment was to -
compile a new seimdc regionalization map of Kewhatka and the Kowndorskiye Islands
-Card -2L1
*MEOW"_

J. 215
-ACC +09
-AT
#A
tLnd the4icroregionalization' of Petropsylovsk (Kawhatka). Detailed seismological
-investigations of both areas vere.started In tbe . 61-, - with -the coopera-
-sumer of'19
tion otthe-Laboratory~of Gebphy ilc_ a -18tationd.1ofthe Insti anology (IV
tuto of Volc
Siberian Branch -AN SSSR. --The objective was to obtain
_Y6iiti- ii of Ksmciwt man Is#
0 foci, seismotectonice properties of the upper _t
and the relationships betveen-volcanism and seismic-conditions.- The-nituork-of-
sensitive-regionalL:aelesic- I tjtions__oU_Ke=hxtVA_be__
k'of--th
Tit m
7:7
-a pa--batve4n- wec' Fsmidtt~-and-, on a an a new mp- was c(upiled of the eeigMic
regiona~Lization of Kamchatka'. the NuAle Islandso and the Komanilorskiy Islands. A 1.
stud'y of the dietribution patterns of earthquakes in the Kurile.-Kamchatka region led
pilation -maps Ar long-range for~ecaetin
to the development-of a procedure and com -of 9
-')f -~Laxiltum- magnitudes of earthquakes in that region. The TIS mid IV Vill investigatej
sei4mic conditions, search for ways to forecast earthquakes,. study ground motions
dur*g grtrong earthquakes, improve the seismic' regionalization of some- sections of
Kamchatka, and investigate propertles*of the upper Vmtle In thc vicinity of KnI.-
chatka, 9 the Kurile Islands, ad In KbmandorskV_ Islands.
SUB CME: 08/ a= DATE t 'none/ -o-Rio, iws'-L!~- m8/ on Ras OC2/ ATD PUSS I
Card

7-
1.248EZ.66 EWT(1~#~A(Q.
ACC NR: A-A6007198 SOURCE COM, UR/2619/E 5/000/036/0066/0093
,AUTHOR: Fedotov. S. A,
,ORG: Institute of-Physics of the EgIfth. AcadeM of Sqien1ME4�ES3 (T44stitut fi ziki-I
:Zemli Mademli nauk SSSR)
arities in the distribution of strong qi=bs ion of th
'MME: Regul Quoko in the reg e
Kamchatka I Peninsula, the Kuril Islands. and Northeastern Japan
A,
~~SOURCM AN SSGR. Institut fiziki Zemli. Trudyj no. 36 (203), 1965. Seysmicheskoye
jrakrorayonirovanlye; vo sy inz
_pro henernoy as smologii- (Seisinic nicrodistricting'.-
__Y
:i3robloms of emg i neirIT-Ig- -seismology) no. - 10, 66-93
ITOPIC TAGS: earthquake, aeismol.09Y
'ABSTIMT: It has been shownbyv, IN!._~ski~ that strong eartiquakes over the':en.
'tire 1,rlobe a-re distribute_&acco~_dlng to Poisson law and are ap,~arently -random -inda- A-,
inct -fro-
Tenderit events.- -As -die-t-i - m, this general rules strong ea~-thquakes in the-
region are interconnected events. These earthquakes are geographi-.
'cally distributed accordi,ng.to a regular law within the linits of the seismogenic-
!.Card 113 .......

lZU11t: CX1U 'LCIIU W AM 1:41dC, Vne
earthicuakes within the limits of other regions are also interainnected events. - This',
)shoul~'i be taken into account when using. statistical pmbabi.litir to evaluate the rv- 1
ter7- -earthquakes. -The- focal regions of strong Kurilo--
.1curi-ence in ral-of-strong
'Kamchatka earthquakes in the 20th, Century have -ten.ded--not- to, o1rerlao -one another,
'Whlch-idapparefitly due-to--jilih stress' relief in the focal reg!.on. Since the Mcur-
;rence interval for. strong_ Kurilo-Kamchatka and Japanese -eazthquakes at one point is-
greater than 100 years, this. tendency should continue for the next few decades.
;These coasiderations are used as 4 basis for pointing out rotential locations of fu-
Iture- strong shallow earthquakes W >,r/,) in the region of the, Kamchatka Peninsulas
The ity -of these prediction - is
.1the Kuril: Islands'and Northeasterm Japan. pr6babil 3
.-,--'evaluated at 0. 8-0. 9. Perio&,- o-f-increased--seismic activity--aie- considered- Ele--- W
evaluations give a probability of less than- 0. 05-for nndom tim-- distribu-
tion o strong Kurilo-Kamchatka earthquakes.in the 20th CentM-. This Is natural
since -a catastrophic earthquake-changes.stresses throughout a vide region and in-
Ocreases the strdsses at the ends ok'a-fault causing other strorg earthquaMs in the
,area which may be widely.'separated ft-om the first earthquake. The Kurilo-Kamehatka
-this. These earthquakes occurred in
-,earthquakesof 1962-1963 are a good.example of
pairs! an earthquake at Ho',ckaLdo-,on:,VHartch 1952 was folloved eight months later by -
~ij
Tard

L 24838-66
HR. AT60071.9.0.
-an earthquake on the Kamchatka-Peninsula ors4November 1952,1000 km to the north-
:east; another earthquake on 6-June 1958 was followed six months later' by a Kamchatm
;earthquake 1000~km to the northeast* Active periods and series of idarthquakes are i
;known in Japan, Chile, Middle Asia,,Turkey etc.,.The tendency for stress faulting in'
,.short periods throughout an entire area may be a common property of region',--With
high seismicity. The focal regions plotted for strong underwater earthquaken in the
Xurilo-Kamchatll(a area may be considered in comparing -tsunami maps as probable loca-
tions of tsiinamis in the past- The-probable sites of fut-are strong Kurilo-Kamchatka
aarthquak2s -- the small Kurii'group, the middle Kuril Islands and the Kamchatka-
Gulf-Kronotskiy Peninsula region -- are also probable sit-as of future large tsunamis.
T,he authors consider the peculiarities for distribution of the strongest earthquakes
:Ln the Kurilo-Kamc*hatka Archipelago. -It is still n:)t clear -to what extent
7these peculiarities are true ;for strong earthquakes in ot'her structures, for in-
stance in Middle Asia where -the magnitudes of the strongest earthquakes are usually..
Ismal-ler and the recurrence intervals are larger. Several isolated examples am
;citel which confirm the peculiarities noted in the 'Paper, . altho'Ugh systematic stud-
iies are necessary for.definite conclusions. Orig. art. has; 7 figures, 4 tables.
'SUB, CODE: 08/ SUBM DATE1__00/' ORIG REr: 024/ 6Tit mr: 029
4
Ica
rd 3 3 - ------

BELYAKOV, F.Ye.; BABIN, B.N.; BALI, V.; BOROVIOV, P.N.; VOYRVODIN, I.N.;
GUUVICH, G.M.; GORBUNOVA, P.I.; KOHNOV, I.S.; KALANTAROVA, M.V.;
KASHIRSKIY, A.Ya.; KAZANCHEYU, Ye.K.; LEKSVIKIN, A.F.; LRTI-
CHWSKIY, M.A.; LOPATIN, S.Z.; MIRSKIT, V.N.-, PODSHVALOV, Y.N.;
SUBBOTINA, V.P.; TANASIYCHUX, N.P.; FWO FISENKO, K.N.;
.ELIKIND, I.G.; BOTIN, S.S.; VASIL' T.; DRI3KOV, V.D.; DALZ-
CHIN, N.I.; DADAGOV, I.A.; YMMOSHINA, V.I.; ZHU11OV. I.V.; ZIMIN,
D.A.: IVANNIKOV, A.Ya.; KOVALNV, M.X.; LUGAKOVSKIT, N.L.; NALWSKIY,
A.F.; SEREZHNIKOV, V.K.; SEMIGLASOV, M.D.; SIXODW, A.Vq; SUPANOV,
V.I.; SAKHARIN, G.S.; SAVERO, P.A.; SOLODOV, V.P.; UMEROV, ShAh.;
CHIKINDAS, G.S.; SHCHXRBUKHINA, S.N.; DYNKIN, G.Z.; LYSOV, V.S.;
OSHEROVICH, A.H.; ROKITSINSKIT, Z.V.; BRASLAVSKIT, H.S.; FXIMO,
I.A.; ZHUKOBORSKIY, H.S.; 2HDANOV, I.Ye.; SIPSLIN, V.A.; BRUS, A.Ye.;
VOLYNSKIT, S.A.; KLYUYEV, V.A.; ISTRATOV, A.G., TIKHOMIROY, I.F.;
BUTYRIN, U.N.; VOLYNSKIT, S.A,; MINNYEV, M.P.; 1U11TSKV, V.I.;
VIDETSKIY, A.F., kand.takhn.nauk, glavnyy red.; DEMIDOV, A.H.. red.;
KRAVETS, A.L., red.; KLIMOVA, Z.I., tekhn.red.
[Industrial Astrakhan] Promyshlennain Astrakhan'. Astrakhan'.
Izd-vo gazety "Volga," 1959a 318 p. (MIRA 12:11)
1. Astrakhan (Province) Bkonomicheskiy admitiistrativnyy rayon.
(Astrakhan Province-Economie conditions) -

voll-KOV9 V.Y5., FEDOTCV, SODO
4an-areatic fistulae In acute pai,,reatitis and their trPaLment.
"lov. mod. 28 no.M83-86 0 16r (M;RA 18-.11)
1. Kafedra khirurgiti,neotlozhnoy kbirurgii I:zuv.- prof.
U.7. Kravchenko) Kazonskogo Instituta usoveribenstvovanlya
vrachey, imeni iAjnlna&

F" Zj a Q
k'
0 tit idd
AR
~Zl 0

f

nd F
studied the bins
4
.
1,
o
of
r
W
f iw ih 6 a$.-% of W. Ido, Nit, Ti, and as sing
s
lid
b
f
l
h
U
l
N
d ,
a
e so
so
u
s
ectro
i an
the mercially
ytic
ng e
p
pas umdals, 100-g. Ingots wen pnrm*pMived from melted
i
d
ibl
I
H
F
A
C
.-
n oonm
om cruc
es
n a
.
miste.
oarse Znx
WM U ow durb c tn. a by
V`C
d
&nnie& a an
11
. Turn.
id
hl
i
k
t
c
ness of indiv
(nearto th
ud graim) were pro
pared
from the undefo allo ani ralmoradlographs obtained
"0
:
ith F
di
ti
f 24 T A
li
96 h
f
of the Institute of Metals
J
ourn w
e r&
a
on o
n.
or
. at 9W C.
,,g
.
21 Part 7
Vol + 50 hr. at 1100'C. did not hoinogenzis the dandritic grains
.. In cast NI-W alloy, The dandrits saw appmrod lighter In
Mar. 1954 the radlogra
phs, being enriched In W. The grain bOUnClAries
Pro rties of Alloys

Pe appear as.broken lines, X-myt belrq weakly absorbed by
-500/0 of the whole grain surfacts. This weak sbarorption can
be attributed to the presence of essly melting Impuritle-s,
shrinkage Itor ity, or solid soln. low In W. In NI-31o alloy
1
h
annealed for 96
r. at 950
C., Oakes end needlei enriched i
No were observed. Microscopic Inytatigation 3howed th n
at
the needles represent on inditpontitnt phase, possibly a

compound
of Mo and N or one of Mo and Ni. However, the
flakeo were not observed under the rilcro4ropa. The pnrts
of the grains nest the boundarim wwo itiso enriched In Mo.
As-out NI-Nb alloy had a cored chindritic structure, but

7 became homogenized after 50 It. at 1100"0., although the
edges of the grains were stJlI enriched in Nb and the grain,
boundaries absorbed X-rays WCLkly. The Ni-Ti &Hoy used
:
contained'on) -8 at
Ti
d
d f
N
.-%
i-
, an
wus prepare
rom
y
4 vd.. TL maxter alloy; annotaling for 60 hr. at 11000 Qi
'
areas of a weakly ateorbirg phase. but
not the
codn~~ inside the gr&OAW solid soln. The heterogeneity of
i
To allo
Nal tol
d
l

,4 uee
on annea
ing.
y
Imp
do Investigatli 5irlous alloys indicited hat&b.-

Metalwork
Makin,- barff vd-Uhaut the help of framework.
Rom. energ. 9 110-73 1.952.
Month] List of Russian Accessions, Library oT Congrdvs, October, 1952, IMICLASSMED
-Y

IDSIPOV, K.A6,- YEDUTOY, S.G*
Softening 0 limited solid solutions of metals. Doklady Akad. Nauk S.S.S.R*
85, 1081-4-152. (MLRA 5t9)
(CA 47 no.22:11897 153)
g-

UM/Netallurgy - Wtsilso Solid I JkLr 53
solutions
"On the 'New, Plasticity Mechanism of Polid Metal
Solutions.." K. A. Osipov.,(,,S. G. Fedot6vvy:~M. G.
Lozinsklyj,"Inst of Wcb1ne Studies, Aced Bt*.i IIBSR
MN OB, Vol 89, No 1, Pp 57-60
Authors su-- ize conclusions of several British
investigatoroj whose works on "new" mechazLem of
plasticity in Al and Zu when they ar6 deformed with
low rates at elevated,temps were published in
Journal of the Inst, Of MetAls" for 1949 - 1952.
259T15
They discuss exptl date which corroborate possi-
bility of similar mechanism of plasticity in solid
soln of Cu-Sn system, considering 2 possible inter-
pretations of the nature of this mechanism and die-
puting assumption that this mechanism is "Tow'N
not actually representing phenomenon of recrystal-
lization. Four'mi6rojOmVhx article.
~PIVNOUW by Ac" W Ti Ondtsay -12 Doe, 52. - -

tallo
, : I
In
of,
~.rairi 1~0uir.iario."
1.15 jc"
Qu
"ol 91,
S,~ n t "3 j-'j,ltz; Of *
I I n i.
durizi:- i 1 ' L " ~tj L,-on6 into
Sot,
- 'iovria
a'
bounri in
riu,s or, tvjo
Of bo-un 1)isf.'ussus b'
rul
dal-y ra-I
AD
6 61'