SCIENTIFIC ABSTRACT KONDOREKAYA, K.B. - KONDORSKIY, YE.I.

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• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

XONMRMYA, X.B.
BoactIvity of peripberal blood vessels to vasoconstriators In ox-
perimental ohols4rla atherosclerosis. Tr. Vessolus. obah. filial.
no. 1: 132 1952. (CLUL 24:1)
Is Delivered 26 fty 1"01, Noscow.

K01-MORSKAYA, G.K.; KAGAN, Z.S.; KRETOVICII, V.L.
Effect of light on the dynamics of armnonium assimilation by
wheat sprouts. Izv. AN SSSR Ser. biol. 30 no.1:141-144 Ja-F
165. (1,[IRA 18:2)
1. Institut biokhimii im. A.N. Bakh% AN SSSR i Tekhnologicheskiy
institut pishchevoy promyshlennosti, Mloskva.

SEMENOVSIUYAO Te. WO
Distorted reactions of the visual analysor to stimulation of the
eyes with red light; effect of Instillation of adrenalin an electric
sensitivity and lability of the visual analysor In red and green
lights..Probl. fisiol. apt. no.10:63-66 152. (Nm ?..1l)
1. Otdelenlye f1siologichaskoy optiki Goa. nauchno-isal. In-ta
gla W kh bolesney Ia. Gellogolltea. Z&Y. otdolentyes chl.-korr.
AN I AKIF SSSR prof. S.T.Irarkov [deceased)
(count VISION,
eff. of epinephrine on electric sensitivity & lability
In red & green lights)
(2PINIPHRINS, effects,
on color vision. electric sensitivity & lability In red
& green lights)

KO)WORSKAYAS I.V.;POSTOLUKO. G.A.
INNNNNWMN
Seismic activity of the Kurile Islands--Kamchatka region for the
years 195"1956. Ity. All SSSR Ser. goofts. no. 9:1114-1120 158.
(Unu 13'slo)
1. AN 555R, Institut fisiki Zemli.
(Seismology--Soviet For Ust)

9.2
Kondor~hNLa,___1.. V., Tikhonov, V. I. SOV/20-130-1-42/69
TITLE': Oil the Problem Regarding thel~~eismic Activity and Structurq Pf
Kamchatlkq and the Northern Fart of the Kuril Island Chain
Doklady kkadler.1i nauk SSSR, 196~,, Vol 130, Nr 1, PP 146-4-49 (USSR)

,DSTRACT: In the prezent paper, the authors give new data on the
struct~lr.Ll diviaion of the Kuril a-ad Kamchatka seismic zone
on the banis of an investigation jeries carried out for many
Years b:y the expanded network of seismic stations of the USSR.
The mentioned zone is part of +lie Pacific seismic belt and
ceismically it is the mc.t active one of the USSR. It belongs
to a youn~~, ,-eoaynclinal region. Former researchers: A. N.
Zavaritskiy, 0. S. Vyalov, B. F. D'yakov, Y. V. Dvali and
G. ML. Vlasov (Refs 1, 8) imagined the tectonic structure of
Kamchatka ana the Kuril Isles to be a uniform, lineally
extended system of anticlines and synclines. During earthquake
investigat ions, a number of earthquake foo-as groups with the
Sreateat density of eploenters per areal wiit was found
besidea the linear extent along the chain. These groups are
jepzLrated by boundaries running transversally to the main chain

Card 1 P, t,hw
direct-.%oii (".efs 2, 3). No explanation was founaby

On ' ;0he ri:ublem Regarding the Seismic Activity and SO'7/20-1 30-1- A-,"'
Structure of Kamchatka and the Northern Part of the Kuril le'tre Chain
tectonic schemes hitherto existing. The most recent geological
data ha7e been applied in the tectonic scheme by V. I. Tikhonov
(Rof 7)- A number of lineally extended antiolines occur in the
nouthern half of Kamchatka. Th.;y are separated from one
another by synclinal depressions which apparently were
developed in the Paleozoic era. Their structural outlW wan
probably maintained by the structural complexes of Cretaosoun
and Tertiary Systems6 These fold structures form a packet. On
the south-east continuation of the central part of this packet
a reggion of greatest eartbqivnke density stretches from the
Kamchatka coast to th., ruril-Kamchatka, depression (Fig 1).
The region south of the u4suu-cural zone mentioned (on the
continued West Kumchatka depression) hcmiever, is slightly
seismic. Also north of the Shipunskiy peninsula, in the
continuation of the great depression, earthquakes are less
frequent. On the strength of data obtained the authors arrived
at the following conclusions- the seismic zone of Kuril Isles
and Kamchatka is divided into a number of transverse groups of
increased and reduced seismic activity. Belts of heavy earth-
Card 2/3 quakes occur in the above zone. These belts are of meridional

On the Problem Rogarding the Soilimio Activity and :3011/20-130-1-42/69
Structure of Xamchatka and the Northeni Part of tho Kuri-' Islarld Wt-lin
ASSOOIATION:
PRESENTM
SUBIUTTED
Card 3/3
and south-eastern extent. The t.-ansverse (1ireotione muntionod
m cky be closely connected to the extent of fold and fault
structures of the-lower structural steps. Hence an analogous
interrelation may be assumed between the kinds of seismic
activity and the tectonic structures of the northern KamohatJ
and the Kuril Islands* The MOTphological contours of the
great and.the small Kuril chains belonging to this seismio
zone, are probably due to young tectonic movements and are part
of the superimposed.structures. There are 1 figure and
8 references, 7 of which are Soviet.
Goologicheskiy institut Akademii nauk SSSR (Institute of
_.Gq,q~cmv_ qLt_4~ Lcp4jemy of q_qi94qes, . PSSR)
July 61 1959, by 11. S. Shatskiy, Academician
July 2, 1959
_01-MIM ~
USSR/Soil Science Genesis and Geogaphy of Soils.
Abe Jour Ilef Zhur Diol,, N:) 22, 1958, 99979
clitnte, was fDrr.,ea last year -iunder the cover of forest
veC;etation; the other, to the vast (a continental type
of Zonality), vas formed in the donditions )f a dry cli-
mate undcr the cover of c-,rcen veCetatim- The total
scheme of the sails' horizontal zoimlity,is disturbed by
the presence in the east and northeast of expansive Qn-
cient del!, , plains vith a hydromorphic type of soil form-
tio-;,. and of muntain systens, the 9,)1! cover of which is
stibjected tD the lw4 of vertical zoi,_Uity-
DiblioEyap;hy of 33 titles. -- T,D. Morozova
Card 2/2

2
Country : USSR
CatoGory: Boll Scionce. Cultivatim Djproveziant
Brosion
Abs jour; F=Lol No 14i 1958s No 63135
Author : Rozanev, ]KQn42F!ka*4 N I
Inst : Soil Science Institute of the A.B. of the USSA
Title : Soil Irk)rovemnt Conditions of the' icirovabad-
X,izakhslziy Mount~ln Rmee
Orit, Pab: Tr. Fochv~- in-ta ~X SSSR, 11.957, L2, 5-112
Abstract: In the hichor parts,of,th6 Little Caucasus foot-
hills thora-are distribute& dark L:ray-brown so.ile,
which ~~ ara - di6tinLp__iAcd- by the ercat (raore than
120 c:3) thicl= -is of'the hunus-profilo; "-hc'voU-
exp.raised carbdfirito~611tivMl horizon and the- cl*ip,
C4xd 1/5

Country : USSR
,L rovorsont -
Dry: S0,jS Cultiv_"tion. un
catog( do
F'rosion
,%bs Jour -p=iol., 141 1958, 110 63135
The div ,r0Vabrd_Mz0jh6jtiy Uountain
is:Lcnl Of the Y
r=ce into rcL;ion$ of soil inprovem"It 18 11"e-
seated S..,-. Nikitin
Card 5/5
DissertatioA"
- -- "N-teStion on the Construction of a
of the M~fi-" 03nd FhYs-Math Sci) Geophysics Inst, A116dograph for tile Territory
(Vechernyaya Moskva, Moscow, 7 Jun 54) cad Sci USSR, 16 Jun 54.
SO: S-am 318p 23 Dec. 1954

D r\
AUTHOR: Kondorskays. N. V. 60-36-4/10
TITLE: beparation and Use of sP Waves in Shallow Earthquakes
for Determining the Depth of a Focus (Vydelenlye volny
sP pri neglubokikh zemletryasenlyakh i ye e Ispoll -
zovaniye dlya opredeleniya glubiny ochagal
PERIODICAL: Trudm Geofizicheakogo instituta,- AN SSSRt 1956, Nr 36,
Pp. 37-47 (USSR)
ABSTRACT: The author discusses the possibility of separating sP
and sS waves reflected close to the epleenter (sP and
SO in recordin
,gs of earthquakes with foci located in
the earth's crust.at epicentral distances of 2* - 80'.
An analysis of the dynamic characteristics of the sP
wave., which is related to the focus mechanism, demon-
strates the existence of a sufficiently intense sP wave
In comparatively shallow earthquakes. The depth of the
focus in the earth's crust is determined on the basis
of differences in arrival times of sP and P, sPP and PP,
sPPP and PPP, and sS and S waves. There are 10 figures,
6 tables, and 7 references, of which 5 are Russian and
2 English.
AVAILABLE: Library of Congress
Card 1/1

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IDUM.UrA, N.V.
-
KO*tixg of the Cousell on Uis"Isgy. ISv.. AX 5S.SR. Ser.goofiz.
no*ls295-12? JIa '5N, .(xm 10:3)
(1411selogy)

49 - 2- 11/13
AUTHOR: Kondorskaya, N.V. and Postolenko, G.A.
TITLE: Seismicity 1n.the Soviet Union during 1955. (SeyBmichnoat'
SSSR za 1955 9.)
PERIODICAL: Izvestlya Akademli Nauk, Seriya Geofizicheakaya, 1957,
No..2,~pp.255-257 (U.S.S.R.)
t
ABSTRACT: A seismic activity map for 1955 showing plotted earth-
quakes with intensities of M >/- 4 is given. It Ir
based on.information supplied by the bulletins of the
various Seismic Stations in the USSR. The map is
limited to seismic zones,, the boundaries of which are
given in Table 1, P.256.
The text includes four tables and one map,. depicting
the epioerters of earthquakes of seismically active zones
of the Soviet Union for 1955. There are 5 references,
Card 1/2 3 of which are Slavic.

/V V
AUTHOR: Kondorskaya, N,,V, 49-7-4/14
TMLE: On the regional features of the time of transmission of
seismic waves. (Po povodu reeionallnylch osobennostey
vremen prpbega seysmicheskikh voln).
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya Geofizicheskaya,
1957, No-7, pp. 895-913 (USSR)
ABSTRACT: On the basis of the study of the results of observations
of intensive earthquakes in the Far East (Kamchatka and the
South East of the Hokkaido Island), Central Asia and Turkey,
it was found that the observed transmission time of seismic
waves to the stations in the Far East, Central Asia and the
Caucasus are larger then those determined by means of
hodographs worked out in 1939 by Jefferies and Bullen
(Seismological Tables 191W). By statistical averaging
corrections were found to these hodographs which enable
more accurate determination of the location of epicentres.
Acknowledgments are made to Ye. F. Savarenskiy for his
Guidance and to S. S. Mebel' and G. A. Postolenko for
Card 1/2 doing some of the computing work.
There are 20 fiGures, It tables and 11 references, 8 of which
are Slavic.
49-7-4/14
On the regional features of the time of transmission of
seismic waves. (Cont,)
SJBMITTED: October 16, 1956.
ASSOCIATION: Institute of Physics of 'the Earth, Ac.Sc., U.S.S.R.
(Akademiya Nauk SSM Institut Fiziki Zemli).
AVAIL"LE: TAbrary of Congmen
CLrd 2/2

SOV/49-58-9-7/14
AUTHORS: Kondo r,-M.77--~Md Postolenko,, G.A.
TITLE: Seismic Activity of Kuril-Kamchatka Region (Seysmi-
cheskaya. aktivnos4v-l Kurilo-Kamchatskoy oblasti za
1954-1956-gg)
PERIODICAL: Izvestiya Akademii 14auk SSSR Seriya Geofizicheskaya,
1958, vr 9, pp 1114 - 1120 (USSR)
ABSTRACT: The seismic activi-l-ies of Kuril-Kamchatka region in
v
1954-1956 were investigated and found to be especially
intensive in S.E. Kamchatl-a and along the Kuril Islands.
The exact positions of epicentres were determined by a
method of intersection of S-P and P waves and by
the application of Wadati (for near stations) and
Jeffreys-Bullen (distant stations) odographs. The
accuracy of distance determination was 25-50 km. The
focus depth of the earthquakes was found from the tables
of relationship between the time interval of sP-P and
sS-8 waves and the depth.
The determination of the intensity of earthquakes was
based on the amplitude and period of te surface waves as
measured by various stations. The number of earthquakes
observed during the wb-le period was 219 (Tables 1-3)-
.Vardl/3

SOV/ 4 8-y~~r/14
Seismic Activity of Kuril-Kamchatka Region ?934-
A chart (Figure 1) was prepared to show all the epicentres
plotted according to their classification, intensity and
depth. This chart shows the following peculiarities: all
the earthquak9s were direc,,,*.ed along the Kuril-Kamchatka
line and grouped in the parallel chains. The deep earth-
quakes (below 300 km) were found in the Okhotsk Sea. Those
of the depth between 100 and 300 km were situated near
the Kuril Islands, while the oneshaving a depth of less
than 100 km were found off the east coasts of Kamchatka.
Generally, the earthquakes could be divided into several
groups, such as: S-ra. Kamchatka, B. Kuril, E. Simushur,
E. Upur and A. Iturup.
In order to determine the frequency of the earthquakes, a
density chart was plotted (Figure 2). This chart was 2
based on a number of earthquakes per unit area (1 degree
of longitude and latitude). The highest frequencies were
found in the regions: S.M. of South Kamchatka, East of
Paramushir and the Onekotan Islands.
The chart, however, could not show the most enagetic
centres of the earthquakes. Therefore, another chart
uax!d2/3 showing the density of energy distribution was prepared

SOV/49-58-9-7/14
Seismic Activity of Kuri.L-Kamchatka R,,gion 1954-1956
(Figure 3). It was based on an amount of energy (S) per
unit of the same area as taken for the frequency chart.
This chart shows six regions of various energies from which
the East of Urup Island is the most energetic one.
It was observed that a large number of transverse tectonic
breakswere accumulated in the regions of the most ac';ive
seismic activity. The region east of the Urup Islai,, being
one of the most active areas, is sitiiated at the juncture
of te longitudinal and transverse breaks (8 in Figure 3).
Here, in 1918 took place one of the most devastating
earthquakes. There are 3 figures, 3 tables and 14 references,
10 of which are Soviet, 1 French and 3 English.
ASSOCILTION: Akademiya nauk SSSR Institut fiziki Zemli
(Ac.Sc.USSR,InstitutZ of Physic-el c;f%hd Eaj:-th)
SUBMITTED: August 28, 1957
vard 3/3

SOV/49 -58-12-2/17
..AUTHORS: Kirnos 9 D. P. ap&_Aqndorsk!~~a, N. V._
TITLE Amplitude of Ground Movement at the Onset of a Seismic Wave
(0
vychislenii istinnogo znacheniya pervoy ampiitucty dvizheniya
pochvy pri vatuplenii seysmicheskoy volny)
PERIODICAL: Izvestiya akademii nauk SSSR, Seriya geofizicheskaya,
19589 Nr 129 pp 1443-1450 (USSR)
ABSTRACT: As a preliminary condition of the calculation, a determin-
ation of the magnification (7) in the registration by a
seismogram should be made. Next, a mathematical formula is
found, where the displacement of soil, X is related to
time t .. Thus a dif rential equation (15 is'formed. From
Rt' a y(t)/'V the distortion of the seismgra*
the graph X (t) and
can be shown in the form X where J e V-t~*s
k/'~c - "k 9 ~k _Aj~ .
re&xced amplAude and Xk is the sW31tude of p-ound/ This
formula contains the form Eq.(2) for the first amplitude. Then
the true value of the amplitude of displacement is equal, to
Card 1/4

SOV/ 49 -58-12-2/1'?
Amplitude of Gi*ound Movement at the Onset of a Selmtlfd,,W~ve
Eq. (3). If the apparatus gives no distortion, then
Uk = Ul = 1 and X, = yj1V (3a). The sinusoidal character
of the seismic wave having the characteristics (4) is consid-
ered. Then the Eq.(5) can be applied for the apparatus of
linear registration (Y - coordinate, 9 coefficient of
pendulum damping, n, - pendulum frequency, V 0 - normal
magnification). The coordinate y can be found from Eq.(6)
(Ref.8), whez. Ul - frequency characteristic, yj -
pendulum phase, FW - time function. This equation becomes
Eq.(7) for the apparatus with a galvanometric registration.
The indicator magnif ication V can be f ound f rom Eq,, (8) where
A2 is the distance from the mirror of the galvanometer to
the photocell. When a 2 -200 do not enable any con-
elusion to be drawn regarding the possibility of the greater ener-
Card 4/7

26982 3/049/60/000/01-2/006/011
On the question of calculating o,, D214/11305
gy of transverse waves as compared with lgngitudinal waves. The va-
riation of the individual values for log 9 p and log N. may be rela-
ted to certain patterns in the deviations of these values from the
average magnitud3 determined for each area as a whole. In the au-
thor's opinion such deviations should be considered as corrections
which have to be applied when determining '� from measurements at se-
parate stations. They are probably due to peculiarities in the geo-
logic structure near each seismic station. With regard to the depen-
dence of log '4 on the icentral distance the following regularities
were observed.- 1) log Fie at a maximum for epicentral distances of
440 -- a fact established by N.V. Kondorskaya (Ref. 13: Stud. geo-
physi.et geodaetap 39 1959) during the earthquake of 3-161957 -- 570
and 0; 2) The general tendency for log 3 to increase'with the
epicentral, distancep especially in the case of P-waves; and 3) The
values of log 5 are lower at epicentral distances of ---250. The au-
thors believe these trends to be due respectively to the focusing
of seismic rays within layers which condition discontinuity surfa-
ces of the second typeg to the decrease of the absorption coeffi-
Clard 5/7~

26982 3/049/60/000/012/006/011
On the question of calculating ... D214/D305
cient of.:the earth's shell with depthp and to the fact that the
Petropavlovsk station -- which, according to S.Ya.-Kogan (Ref. 15:
Izv. Akad. Nw--dc SSSR. sero geofiz.# no* 9, 1959), usually gives re-
duced values -- was used in the case of small epicentral distances.
The foregoing method is considered to be suitable for measuring the
elastic-wave energy of earthquakes by means of observations at re-
mote stationso The authorep howeverp recommend the use of an even
greater number of stations to obtain more precise values of log &.
The reliability of the method would also be improved by additional
information on the vibration groups of P- and 3-waveop the correc-
tion's required in the energy calculationsp a simpler means of deter-
mining the form of f(ep a) and on the spectral composition at the
boundary of the focal sphere. There are 5 figuresp 4 tables and 15
references: 10 Soviet-bloc and 5 non-Soviet-bloc. The references to
the English-language publications read as follows: B. Gutenberg,
Bull. Seism. Soc. Ame'.4. 34, no. 2. 1944; B. Gutenberg, Ibid 35, no.
2p-1945; H. Hodgeong Ibid 439 no. 1, 1953; M. Bath, Trans. Amer.
Geophys. Union 36, 1955.
Oard 6/7

26982 S/049/60/000/012/006/011
On the question of calculating D214/11305
ASSOCIATION: Akademiya nauk SSSR9 Institute fiziki zemli, Moskovs-
kiy gosudarstvennyy universitet im. N.V. Lozonosova
(Institute of Physics of the Earth, Moscow State Uni-
versity im. N.V. Lomonosovs Academy of Sciencest USSR)
SUBMITTEDt May 5, 1960
Card 7/7

23458
S/049/61/000/001/003/008
-3, c1,30 0 D226/D306
AUTHORS: Belotelovo V.L.t Kond-orskaya, N.V.
TITLE,% On the relation between earthquake energy and the
maximum displacement velocity in body waves
PERIODICAL: Akademiya nauk SSSR. Seriya geofizicheskaya. Izvestiyap
no. 1, 1961# 38 - 45
TEXT: This article appears to be the third of a series of papers
devoted to this topic, based on an extension of the method of B.B.
Galitsin (Ref. 1:.Ye.P. Savarenskiy, N.V. Kondorskaya, V.L. Belo-
telov, Ob opredelenii energii uprugikh voln, porozhdayemykh zemle-
tryaseniyem.- Izv- All SSSR, ser. geofiz., No. 5t 1960)._The end-pro-
duct of the paper is a set of relations between -3P or BSt the mean
energy of all the P-wave, S-wave reBpectivelyp radiation from an
earthquakep e - the epicentral distance and (A/T)pZ, (A/T)pjlv
(A/T)SZ, (A/T) the quantities read frL-i the seismograms where
SH
Card 1/4

On the relaticn between ...
23168
S/049/61/000/001/003/008
D226/D306
A is the amplitude (of the actual earth's surface displacement).
T is the period and P, S, 24H have their usual significance. (A/T)
is supposed to be read at its maximum value. These relations are:
Deep Earthquakes Sup~erficial Earthquakes
P, f Ifop =23,05+0,0
W -22,75+0,0180*+ Ig A '25 0* + 1A
(A)
1 A PE Ig57p -23,35+0,025 Q, + Ig A
JCI, .23,0+0.0118 00+ g (T)PIr 071')PH
le-), -M,3+0.02 0'+Ig A)SZ Igs + Ig A
(AT (47)82
IgUs - ZI,0+0.020*+ 19 1 A lg~jS =23,45+01,02 0* + 19(AT)SH
~ _P).9H -
The analysis is based on 132 records of eleven earthquakes. Some
causes of the lower average result for dee*o earthquakes are dis-
cussed. 1) The traces from deep earthquakes often consist of one
large energetic pulsel whereas those from superficial earthquakes
are spread over many osoMations. 2) A factor in the equations de-
Card 2/4

23458
8/04 61/000/001/003/008
On the relaiion between oso D226%)306
pending on the angle of incidence is more critical for a shallow
focus. 3) Integration from a superficial focus is only over a hemi-
sphere, not a spherej so one would expect 1g 3 to be 0.3 less for
surface earthquakes. 4) At small 8, The difference in the reflexi-
on coefficients at the surface becomes importaxitp and many more ob-
servations are needed at each station to aetermine them in the
range 0.1' to 0.5 Hz. There are 3 figures, 2 tables and 8 referen-
ces: 3 Soviet-bloc and 5 non-Soviet.-bloc. The references to the
English-language publications read as follows: B. Gutenberg, C.F.
Richter, Magnitude and energy of earthquakes. Ann. Geophya. Roma
9, No. 1, 1956; B. Gutenberg, Amplitude s of P, PP and S and magni-
tude of shallow earthquakes. Bull,~ Seism. Soc. Ameri., 35, No. 2,
1945; B. Gutenbergv Magnitude determination for deep focus earth-
quakes, Bull, Seism. Soc. Amer. 35, no. 3, 1945; B. Gutenberg, The
energy of earthquakes. J. Geol. Soc. London, No. 8, 1956.
Card 3/4

On the reiation between
2 ffl8
S/04 9 E11/000/001/003/008
D226/D306
ASSOCIATION: Akademiya nauk SSR, institut fiziki zemli Moskovskiy
gosudarstvennyy universitet im M.V. Lomonosova (Aca-
demy of Sciences. USSR,. Institute of Physics of the
Earth, Moscow State University im M.V. Lomonosov)
SUBMITTED: July 6t 1960
Card 4/4

lVV, 14
S/049/62/000/002/001/005
D218/1)301
AUTHOP"S Vanevir, J. A., K Milre." V. t -1':Ondorrk 14,Y_
11'Lizniche*,*.o, Yu.V., Savare-askiy, Ye.-Y., Solov yev?
O.L. and Shebalin, N.V.
TITLZ: Standardization of the macrnitude scale
PE."'luDIC.U.: _Alhademiya nauk. 333111. Izvestiya. "Jeriya geofiziches-
haya, no. 2, 1962, 153-158
T ~T it is pointed out that various ma-_nitudc scales .-.-.re
used at thc. ',jresent time and that their tmain (lisadvantarrc is thkit
they provide different magnitudes for a given earthquake. This is
because in many cases the methods used to calculate the magnitude
are not clearly defined and are inadequately described. A sipecial
conference of Soviet and Czechoslovak seismologists was convened in
,Lrague on December 7-14, 1960, to deal with this problem. The aim
of the present paper is to give an account of the main results of
the 2rague meeting and to suggest a standard method for deter-m3-ning
Card 1/4
;S/049/62/000/002/001/005
Standardization of the magnitude scale D213/D301
the earthquake magnitude. It is suggested that the scale should be
based on the following standard formula:
max
where A is the maximum displacement amplitude, T is the correspond-
ing period in seconds and x (A) is a calibrating function which
describes -the variation of VTI with epicentric distance a7ad is diff-
erent for different types of waves. This formula has been discussed
by B. Guterber- a-Lid G.F. Richter, and by the first three of tile pre-
sent authors in an earlier work. The calibration function is -LakL-n
as an avera--e of- the Q function of Guterbercr and Richter and the
;3 function of J. Van6lk &nd j. Stelzncr. 2)L t_ble is reproduced civ-
ing the smoothed average calibratin2; functions f or *_dF1, 2V, 1?1?1,, aud
SH waves. In the case of surface waves, the calibrating fu-action
is taken to be of the form or (6) . a log A + b. it was -found that
the coefficients a and b for LH waves are on average equal to 1.66
and 3.3 respactively. This result holds for surface waves at epi-
Card 2/4

3/04 62/000/002/001/005
Standardization of the magnitude scale D218YD301
cenrric distances between. 2 and 1600. 3elow 50, 3J,',e oxd L waves
fl'Illy (listinq ishLd. It is pointLd out that the Droblem
must be care. ou
o:F. defini-n-t a single value for 1.1 is not yet solved because different
U
average values are obtained for M with different tyfc-- of waves
1-11?1j, 1-i-ji, and so on). Fievertheless, it was decided not to
combi-ne these values as on t1v unified Gutenberg-Itichter scale, but
to use the -iiethod described above to accumulate a larcre amount of
data and return to the problen, of defining an average magnitude
later. Je-cinning with 1962, all stations of Czechoslovakia and the
UL3SR wi-M use the method described in the prese-at paper. Thcre are
2 tables and 20 references: 11 Goviet-bloc and 9 non-ooviet-bloc.
The 4 most recent references to the Znglish-lanL~uage publications
read as follows: 3. (jutenberg and C.F. Ilichter. kin. Geophys., 9,
(1956); Report of the committee on magnitudes 12th General Assembly
Of the 1UGG, Helsinki (1960); j. Van9k and J. Stelzner, Ann. Geophys,.,
13 (1960); T. Nagamu-ne and A Seki, Geophys. Macr., 28 (1953).
Card 3/4
S/049/62/ooo/002/001/005
Standardization of the magnitude scale D218/D301
ASSOCIATION: Geofizicheskiy institUt Ahadomij naul,. -h SR (Geo-
Physics institute of: the - . U 0
Academy of sciences,
Czechoslovak SSP,), Geofizicheskiy
Universiteta, Praga (Geophysic' institut 1%-arlova
University, s institute? Charles
Prague) and Alcademiya nauk Q-S.D1, institut
fizil-,i zemli (Academy Of Sciences USSR, I-Listitute of
PhYsics of the Earth)
SUBMITTED: October 31, 1961
rard 4/11,

Z/023/62/000/001/002/004
D006/D102
AUT!f*: arnfk, V., Kondorskaya, N. V., Riznic-henko, Yu.V., Savarensky, E.F.,
Solovyev, Vank, J., and diopek, A.
TITLE: Standardization of the earthquake magnitude scale
YERIODICAL: Studia geophysica et geodaetica,.Ano.1, 1962, 41-47
TEXT., The paper,presents a proposal for standard methods of magnitude determination
of both shallow and deep earthquakes, and describes the practical application of
the suggested magnitude,scale as agreed upon ky Soviet and Czechoslovak seismolo-
gists at meetihgs held in Prague on December 7-14, 1960 and in early 1961. The
proposal is based on the following postulates: (1) General acceptance of a Unified
formula for the definition of the earthquake magnitude M
M =clog (A/T) max + e( A) (1)
where A is the maximum ground amplitude of the wave considered (in microA6), T is
the corresponding period in secoids) and is the calibrat' f nction
expressing the'relation between A/T and the'epicentral distance which is
Card 1/3

Z/02
6y62/000/001/002/004
Standardization of the .... DOO D102
1
6, (1958), 222. (Technical editor: L. Ruprechtova)
ASSOCIATION: Geophy3ical Institute, Czechoslovak Academy of Sciences, Prague
(V. arnfk, J. Van%k); Institute of t.he Physics of the Earth, Academy
of Sciences of the USSR, Moscow (N.V. Kondorskaya, Yu. V. Riznichenko,
E. F. Savarensky, S. L. Solovyev, N. V. Slebalin); Institute of Geo-
physics, Charles University, Prague (A. Ntopek)
SUBMITTED: November 11, 1961
Card 3/3

VVEDENSKAYA, N. A.; MHANUZAKOV, K. D.; IODKO, V. K.; XONDORSKAYA -- N.-V.;
LANDYREVA, N. S.; MISHARINA,, L. A.; SULTANOVA, Z. Z.;
TSKHAKAYA, A. D.; YURKEVICH, 0. 1.
Bulletin of strong earthquakes in the U.S.S.R. in 1959. Trudy
Inst. fis. Zem. no.22, Vop. insh. seism. no.7:3-24 162.
(MIRA 15:10)
(Earthquakes)

DORSKAYA,, N.V.; L4NDMMVAt N.S.
Fentures of the selmicity of Znihatka Province according to
observation data from a netAmk of permanent seismic stationme
Tzv. AN SSML Ser.geofiz. no.lOxl320-1332 0 162o (MMA 16:2)
1, lustitut fizlki MuLli AN "M
(ramcbmtka, Province-Seismology)

KONDCMAYA~ N.V.
4 -~-
Conference of the comittee on the International Seismological
Su=Ary. Geof~a.biul. -no.12S10-13 162. (MIRA 160)
(Saimology-Congresses')

...KCMDORSLAYA, N.Vt LANDMWA., B.S. .
Features of the seiamicity of Kamchatka Province according to
observation date from a network of permanent i3eismic atationes
Izv, AN SM* Ser,geofiv. no.lOsl320-1332 0 162. (MMA 16:2)
I* Inatitut fizlki Zmli AN SM
(Kamchatka Pfovince-Seismology)
02

VVEDENSWA, N. A.; IMKO, V.K.; SKLYA._XLf LANDYREVA, N.S.;
MISRWNAP, L.A.; SDIENO-7, P.G.; TABULEVICH, V.N.
BuUetin of strong earthquakes in the U.S.S.R. in 1960.
T
Trudy Inst. fiz. Zem. 28 Vop. inzh. seism. no.8:61-76 163.
(MIRA 16:11)

ACCESSION NR: AT405972 S/2619/64/000/033/0124/0143
.~-AUTHOR: Vvedenskaya, N. A:; Dzhanuzakov' K. D.; lodko, V. K.; Kondorskaya, N4 Vk i~,
~an1y*rf,yg,,N.,,1l;; V!sh?rln.1, L. A.; f~natsakanyan,' D. M.; Rag I
G.; ev
TITLE: Byulletenl sll1ny,*kh:zemletryasenl'Y SSSR (Bulletin of the Strong Earth-
quakes of the SSSR) for 1961
,:SOURCE: AN SSSR. Institut fI2*Iki Zemll. Trudy*, no..33(200), 1964. Voprosy*
Inzhenernoy seysmologil (problems of earthquake engineering), no. 9, 124-143
,JOPIC TAGS: geophysics 'seisf!~,Iogy, earthquake, earthquake focus, earthquake
epicenter, earthquake Intensity, seismicity'
J. ABSTRACT: The "Bulletin of the Strong Earthquakes of the'SSSR11 Is a periodic
annual summary which simultaneously summarizes all Instrumental and noninstrumen-
tal data on the strong earthqua kes (1i >4) occurring In the Soviet Union.The Bulletin
contains a catalogue of earthquakes (reroduced in the paper for 1961 in the form
of a lengthy table), a map of the epicenters and a brief description of the strong-
est earthquakes. The catalogue includes instrumental data on the coordinates of
the epicenter, focal depth,. magnitude M and the time of occurrence of earthquakes,
taken from the Byulleten' setl seysmlchesklkh~ stantsly SSSR (Bulletin of the Net-.
wo
rsk Seismic Stations of the SSSR) pri'd'nonini,-trumental. data Information on
C
or
ACCESSION NR: AT4045972
the sensed intensity of earthquakes, received from reports submitted by local in-
habitants or from Investigations devoted io descr;ptions of the strongest earth-
quakes. With the exception of the Kuril&Kamchatka zone, in-the catalogue there
are data for all earthquakes with M >'4, and all earthquakes for which M was not
determined but which were recorded 6y- seismic stations of the general type,as'.
having epicentral distances greater-than 1,000 km. Data for the Kurile-Kamchat',--.-6
zone include all earthquakes with M > 5~ A map is presented in the pape'r which
- f the earthquakes listed In the catalogue;
shows the location of the epicenters 0
numbers on the map correspond to the numerical listing In the catalogue. In 1961
there were 272 earthquakes in the SSSR with m > 4. Their distribution by regions
and intens*t* Is tabulated in the original t7ext. Fig. I of the Enclosure shows
1 17)2 SSR for 1961,
the value Y, E for individual seismically active zones of the S
co6puted using the formula~lg E =*.11.8 + 1.5 M. Fig. 2 of the Enqlosure shows the'.
change with time of the deviation from the mean o.nnual-value S E112 for four sels-,',;
micalli activemnes. Along the'~y-axls of the graph there is plotted the valu
2 E / - (,7 E 2)'mean and along the x '-axis -- time .(1946-1961). The value (E
mean for each zone is indicated at the right of the graph.- The authors go on to.
describe briefly, but Individually, thd most important seismic phenomena occurring
in various regions of the SSSR In 1961. The annual publicatl6n of the Bulletin'
was begun in 1956 and until 1961 It was printed In the Trudy* Instituta FlzlkI
Zeglifiy SSSA In the collection of articles Vopro3y Inzhenernoy seysmologil
Car Z/b

ACCESSION NRt AT4045972
-Flg. 2~
Card 5/6
ENCLOSUM t 02
Inc
At fro-
51 5.
AOW
ftph ?40

BELOTELOV, V. L.; KONDORSKAYA, N. V.
Spectra of body waves in Kamchatka earthquakes. Izv. AN SSSR.
Ser*geofiz. no. 4:475-482 Ap 164. (MIRA 17:5)
1. Institut fiziki Zemli AN SSSR i Moskovskiy gosudarstvennyy
universitet.

VVEDENSKAYA.% N.A., otv. red.; KOWDORSKAYA, N.V., otv. red.
(Earthquakes in the U.S,S,R, in 19621 Zemletriarenila v
SSSR v 1962 godu. Moskvaj Nauka, 1964. 153 p.
(MIRA 18: 6)

VVF-DENSKJ,.YA , !!,A~ ; EZRATRIZAKC71, K.D. ; IODKO , V.Y,. ; KONDORMAD, 11 V
';DYJ 'VA , N. S. SHA R 1 NA . L. A . ; 1-11 LA T l-'IKA 1-11 1 ill ). 4'. ,
11. 1WE D -Fji G-1,10
'V, Sh.S.;
SEI-TENOV , P.G.; TABULEV1Q.11, V.N.
Bulletin of powerful earthquakes in Ithe U.S.S.R. during 1961.
Trudy Inst. C-iz. 27.em. no.33. Vop. inzh. seism. no.9:124-143
t64'.

AT6033686 SOURCE, CODE: UP./3231/66/000/001/0031/0053
AUTHOR: Xondorskaya,, N. V.; Zhelankina, T. S.; Mebell, S. S.; Vartanova, L. Y-
ORG. none
TITLE: Certain results of using an electronic computer to collate seismic observations
SOURCE: &INT SSSR. Institut Mild Zenili. VychislitclInaya soysi-nologiya, no. 1, 1966.
-~naliz seysmicheskikh nablyudeniy naelektronnyhl,,mashinakh (Use of electronic computers in
the analysis of seismic observations), 31-53
TOPIC TAGS: electronic computer, data analysis, earthquake, seismologic station,
pro-rain
0
ABSTRACT: The article analyzes the experience gained in the more precise determination
of the coordinates of earthquake epicenters with the aid of an electronic computer by the me
described by L L Pyatetskiy~Shapiro et al. (DAIN SSSR, 1963, 151, no. 2, 323) (the 11EPI-111
pro.-ram). The epicenter coordinates were determined by the USSR Meteorological Service
'I
IV, en drafting composite seismic bulletins for the period from the 4th quarter of 1960 until
0
1963. The use of the EPI-1 program proved beneficial in that it increased the number of the
determined epicenters by a factor of 1. 5, enhanced the accuracy of their determination, and
Card 1/2
ACC NR: AT6033686
led to the solution of additional problems: a) an averaged law of the distribution of closing
errors fl., (deviations from the standavd Jeffroys-Bullen hodograph) was found for seismic
stations in the USSR; b) the s.ccuracy of determination of the epicenters of earthquakes occur-
ring in various parts of the terrestrial globe (Central Asia, Kuril as -Kamchatka Are, Japan,
Alaska, California, etc.)is estimated,with the regions being divided into 4 groups according to
the accuracy of determination; c)the possibility of the coincidence'of findings with respect to thE
accuracy of determination of epicenter coordinates is proved as regards observational findina-s
from -90 foreign stations and 14 Soviet stations with enhanced accuracy of observations. The"
dependence of the accuracy of determination of epicenter coordinates on the depth of the
earthquake focus is demonstrated. "In conclusion, the authors are indebted to V. I.Keylis-
Borok for his comments on this project. It Orig. art. has: 7 figures, 8 formulas, 6 tables.
SUB CODEPL-,~- / SUBM DATE: none/ OJUG REr.: 003/ OTH REF: 004
Card 212

ZHEREBKOV, S.K., MAYOROVA, A.S.; GROZHAN, Ye.M.; KONDORSKAYA, V.A.
Using rubber and ebojite for the protection of equipment from
the action of chemical media. Standartizatsiia 26 no.2:37-38
F 162. (KMA 15-- 2 )
(Rabber coatings)

KOCM*MVA, I.P.; KONDORSKAYA V.R.
,=n~
Using Cerapa&s an rootstock for the oweet cberry (Ceramm avits
L. Hoench.); anataw of tb6 atock-scion union* Nauche dokl. vyze
shkoly; biol. mailki no. 1:118-122 l6le (MIRA 1/,:2)
1, Rokmenda=m kafedroy vysshkikb rasteniy Hookovskogo goeu-
darstvennogo universiteta " X.V. Lamonosova.
(aMY) (GRAFTING)

AUTHDRs IRZKMMJF.B., KaBCOMA.Z. JPA - 294
TIT L14 ToWerature Depandenog of the OVEMMER Effect in Metallic
LI'Udm. (Taperaturneya, savisimst' effekta, OV*rh&MQrg T
wtallichaskm litil, Russism)
PgRiWICAL: Zhurnal. Mcaperim. i Teoret.Pisild, 1957, V01 32, Nr 3, pp 01-612
(U.S.S.R.)
Reasivedt 6 / 1957 Reviewedi 7 / 1957
ABSTRAM A.W.OVMUM (PlUs.Rev. 99 P 689, 1953 and Phys.Rev.92o 411 , 1953)
showed that In the me* or an astals the saturation of the re,-
sonanoe caused by the conduction electrons mint lead to a strong
=ua*ar polarization. This efroot me repeatedly dbserved experi-
Mentally and is investigated here on metallic lithim at, tnpera-
tures of from 77,20 to 3730 K (the experimental order in descvO:b*d
in detail). Results axe compared with the for-11- by
Pmovr= - G~ cm (Nuovo cim. 11, 618, 1954). Vie ratio or the
signal proportional to the order of nuclear polarization at 00 and
570 0 amunts to 105 4coording to the experiment, and to 1921
m Wing to the formula. lqerlmntal results show that the width
of'the resonanoe line increases with decreasing temperature.
(i illustration and 8 Gitations from Works Published).
Card 1/2

RYBALKIN, G.I., inzh.; SHARAPOV, V.A., inzh.; VELIKIY, I.G,, inzh.j
MALIOVANOV, D.I., doktor tekh. nauk; PRUZHNIER, V.L., insh.; J%'
KONDQR~&7T,X, R.L., inzh.; TUMANOV, V.Ya., inzh.; POGORELOV,
W-.C, kand# OU. nauk
The BUKS-Isquipment is an important step ir the accomplishment
of overall mechanization of shaft sinking. Shakht. stroi. 9 no.2t
1-3 F 165. (MIRA 18W
1. Kombinat Luganakshakhtastroy (for Rybalkin, Sharapov, Velikiy).
2. TSentrallnyy nauchno-issledovatel'skiy i proyektno-kc -,truktorskif
institut podzemnogo i shakhtnogo stroitel.'stva (for Ma3iovanov,
Pruhnier, Nondorskiy, nimanov, Pogorelov).

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inensaini. f2) Tbp fiwmulw "lite cm live funv. ntagmfip milmnesim.
and btalpirmia Inura with &M Intemill , whkA wrm tlAisintril in I I I fiw frml-
'J sit: itpirlioi with Inlitilleky Itaill. jumd:f. cylindfinill Mrxina. an, In gimid mijinv.
~11 with 11do eatteriawokal r"mills Ow "Wirawn air-. N. IL V.
I L A RITALLURGICAL 1,1112,11110111 CLAMOCAIMS
Ill i I I did afte is I
0 0 0 to

A-0 49
'0 0 0 0 41 to 0 a
I~ssjr I 1 4 1 6 1 0 1 4 0 u 4A ft 1 '10 a 11 It It is Is of is if o- 0 Al
AMA d-f-l 1 4 j 1 0. 1 a
Oo .10) #f. J:lptol
T, ~114
up"gMe a# pdpoponjaw fawpoNuft W Wak Ilm"
IfAl, 10, 51)3-
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I tn extermian of
-41a Knithsh
A 1h *71)
4, .
.
-[
pmvkme wwk tiW. 19M 9L 738: Md. Abs,, J941, IL "0), an a [mate
d palycryaWlisom A"mmwwtic mbstmomms lop
tbwgy of I rllopr4,
inte"etim betow"n the wparate parts.
acculust being taken of amr migmew
@k work agM willk thow of Rkylvigh.
btalmod for h
ti
Y
om o
quai
3
Ibm" Ills d a fl_b~
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a' v
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coo
no w
FPO

F- J. P*yj.. U.55.R.. 6. JA PP, 93-1106 194.Z.-
a Amox. Ommy Of the wAratinu;m of -Ge
polycrystaDine firromsewic bodies with mprd to
t1ft nosmic lawactim baw. ther FW% refro-
'We's
-Woks Consisting of MOM" with I xds of may
MAPAWMim aft Oanvim". A S"*rA c4wookm is
gilen Am an* kmaugmics aftich cormaLms ffmn
ffaMiMion with fald stmogtk md a commion
is goobli" bKw. da S ku" mvJ hystam
A d -, ical fonvW& Is dwivod for the do*
h)" Wov in the "aim at Smak ma &ad for
dow4nux of *Mamab lomm om Wd stmVIL
MW momiop 0( the a(matim *bm dur pats ba%t
IbRikr rimp" ma form MW Mom the amm of ftsy
INWmiation a#* dhedhood at famimn is Com-
41 4diffed. Thmmw CAV%" aft' cotmand with OW
%ur," of actud "We4ritth,
400

IrLL~00~~At LITIRAYWHI CL#NvKATAO

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-

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a mche 6m w qkbm *Ap. An
b"W

al, - - $IV" Rw a herawAsmic
. . w" PMIM cyfhkk-al
esal -MmW&** Ibb d~y is chKKW by t2
waft CW*dMM Wb+8 Ed N "&W dw
mftmw49vwmkw~ Tftmrv~imssraww-
rw.dmy is dm son" w indob immmion
00 WhiIM AF*VWMW"WMU)Or PWROMPWM-.
Tw oim sow" offt wapohmts am dan
m"m GowcWN M,
pshipw ma wom. *A. fm awve of bm*418ow
IL W. WAAM
10 - I L A INIMLIFINSICA& klyll"All"t Ck""'C"lle"
sold" dot
u 0 AV Is
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An I I a ad a 0 4 1 9 60 9 a 4 3 6 9
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09 A J-11 "03!!P1
04

O~O
00,9
40 a
00 a lboony of 1W CSPVI- Werve of Giesh. ~In Russian.)
X. Kondorskii, Duktody Akodewii Na,,4 SSSR (Rc-
War a 4 porti-o"MrAcademy of Sciences of the USSR).
.
*0 8 now our.. V. 63, J)tc, 11, 1948, P. 5074110.

00Z The Influence of Incluslons an the rtitical field anif
coercive force was laveiltigated theoretically U41111C
00 3 a different approach from that commonly uxt4l.

00 a it
i

ew formulas art- f,,r ths.
001.3 1 the critical fichl. Obtaincil data flee in agrevrovia
00,0 with those r"ulting fn,n, VXpertinental investi.

ILA METALLURGICAL L111141009 CL&SWICAYMN
9
0Mb It UAT PO is it
00 0i 0 :10 0 0 0 0 0
.:0]e 0*0 0 9 0 * 0 0 0 0 V:
-00
000
Va
-60
100
too
10; moo
1! No 4j
coo
of
Isom WOMW
filial tie GOT its
AM A I I No 0 a I or a 9 a 4 3 0 0
0 0 0 * 0 0 0,:.,: 0 0 * 0 0 0:6
0 0 0 0 0 *~ -1 , ~gb

(1049).-In cmnftlkm witb the %tructurv~ otwiml and
4UIsins. Bwmtb, and I;btckky (Phy
W. i*
I M In cubic ny,tunt%ith "mulaoll;1I c
inclu"ut. the condititloslorthe slonuin t"ini.
itties t1unit tlw Inchit 4,112 Orr v %;I III, L.Ilmly I i.-Aly. 1111he
caw of Nxial (frulzatilletle with InInnillollf-lic
Aukvs, tin latter "Invic- the hift of ImKintlatic,,
(Cakim pAyr. No~ 25, ull
Thist Is olmutlotoot with N
(1%4)) cronclu". thut th" 6xitulativ* rim 1%m thrivush
my instill incloomimo. the clit. firld Illcfeoing with file
tautuidly goeq,endiculit au- of c,.Al-
mmmagnefle Inclusiono. the r"utt% a" "orntimily identi.
clj vVith the conclusims of Kroten "Groffi4itm fine?
Tbrw* dff forowlarlim" 11yoom, wtW drip Kwiihr-
brafl, 190 (C.A. 311. reacliftl withmit cm.
.sirlerntion of the domain ofuctowe moround the inchmi(mis.
N. Th-

F, '_1 Ij i I I-
V~
'V jLLVWaittj And tho Part Played Cy 16'DisplaLe-
mt of Domain Boundaries In L49 Process of RemUneU=fIGn
of W4b4WUdTU7 ABOT& -N.Malgakov-and orsky
(DoWdy An& Nook SAN.R. 1949, 40, (3),_ 325-2U)~~
[In Russian]. The nnnello yiscmity in the BUOYS (1) Ni
24, Al 72, On 1-5%. remainder Fe, after various thamal
treatmont4 causing dMumut decompa. of the MOM Doi".
and (2) Ni 13, Al 81 03 3, CA) 24%, remainder Fo, cooled In a
magnoLio fie!d and else given various thermal truatmenta,
was studied. Experiments were carried out At vaiinna
temp. The time interval, T, fivra the moment of appa. or
change of the magnetic field to the moment of rn uroment
of the change ofmagnotization oftho n3ton variod between
the limits 2 x 10-3 to 81 see. For r 15 x 10-3 me. a
Helmholtz pendulum breaker with a ballistic galvanometer
wasusedfarthemeasurements; fbrT=O-Isec,.,'&irAnu3Uy
oparaW fl,symoter. The measurements were taken on 'the
do-zward branch of the hy-itcresia loop and also at the
beginning of the magnat"tion, curve. In the latter caed
the opectmens were carefully demagnothad before the
experHnent. The influence of oddy currents and auto-
induction was sh(rprn theoretically to be unimportant.
The results indicate that the high viscosity which occurs in
relatively magnetically soft materials also occio in high-
coercivity alloys. It in concluded that the movement of.
domain boundaries playa an important part in the rernag-
netization of such alloys, which is contrary to the views
currently Accepted. B. and K_ also show theoretically that
the growth of thermsUy nucleated domains of favourablo
orientation is possible at fields greater than the mitical value.
A purely rotational process can take place only In very fin'JL

KONDORSUY, Ye. I.
"Theory of the Magnetic Properties of Conglomerates end Powders,"
Iz. ASUSSHp Ser. Geograf. i Geofiz., 14, No. 4, 1950.
Geophysics Institute, Department Physico-Meth. Sci., AS USSR

C-.o,7
One-detods samclume Is" ibi. 'd 9
41-m-as m6mm". ff.
banonosur
-Appm,
V S..V-V.R. 70
ST.-Foa -
substances was1wil"I 01 "Irmat pwlkko, M*rtl:
Unwftafi- .'. 'tt'
I for wiskik the rmaticift an abs.
4"w4lummlo. i.e.. ref"Aill U"llimmly t"amium in any
SM. only the V'tw 111wit the AM (a dirwed alotis
the latiji Ak6 of the t'Yhlkllk'Al Of tlf4VA*W PAftk'1V
C" Cd. AU.1 thC Alk Of VNI MASOCIUAl Wn is Sm"Mi
with It. The alt. wducs of the W04nWh for
me: 4 (OR a CIWCF;
COMMMUS 00660etifttift. A is t11w exchmv integral (dold.
kout the temp. depaWm" of wam. I* the raup of low
temps.). e - I/,. 1. 2. remp.. for slample. budy-wateitti. wal
teml-nolmle 611kv4. a is She inimt. distance Woug;
I-
.he "far id the vulm, X# to thr ilcoutan"Iskm factor twnwil-
dicutor to the loug &%is. Kn~a espel. vAlum we uwd to
CO&C. 14 fLW WAWnPIC% it$ Whitll V1 - 2. anif Ow C%Kwn. of the
le"onwopteck- timilmsticist 6 sittall: & (cw %phcum. 14 tcw cJfil~
wAds. am) J. for cylln4m aft fut V* 1114 A., WAA.. and 106 A..'
$.a .11 :1491 A.. 24-1 A.. .1 Z170 A.. 11.
30% hirom"Mik- sub"Amm. to is ovpftm. a time- the
values in the tAble. The cowlitim &w 0". cm c vt Ituce
11, is The mnw " that for OWA00aidow. MW V - 0.3
matt Nj so 2wilo. toss. Us - 6W oerstatim oW 4 Rp SJU A.
----ie tin,
a function of their funn wW dinwmims, The d, of the
lCWjjp tMity is WM*Wd CUMM. at a& pgWIA W tbW IwAr-
ticks, The mdi" for one4mmifibm IN WbKW Par-
ficles it r i; ps it is abv the tow-jurt
for ubtaluins m--. cort, ve form, ff... N Is dw dt--
anagntUAtion factor. wbkh depencis om the Coac . so Par.
ticics; A - sjJ, in which J is the elchow liat"FrAl Ow S.
Is the M. of valence electrons: c - 1. 2. mp.. Ow wam and
s1mm- of a partick.
port.. :mlerW cable lattka; r is the md'
llipp"I pa"Icks. lithe taliol/pispaj)(119tho IS
of the kwiter hall awls). the condition for On. IS
uru* "d tu". It. Is r r~ P. ~ (I //#) %/'flitA 7ix' - is. For
Witt values of I/r, im>ictlc rcvm4 takas ptace as In the
CAW Of CytirklIkOl PAFtMCS fiftit 1). TU EMW*tk MVtt.
ml for latetinctliate values u( 1jr is shown in a gnLpb.
Ellen It. MAW

-17
I11th(dww&w*dh**Jr) unaillfwas loop. Tbeardwathim
moveirs lor as Now. depam6mv of , aw a bw - that
sum mua*. J al the
Jim that jwPbvt*.b*1qIh*4mrAdbwA v k4kid-by if
-mm
nds 4d I fma thm imp Sw
jIf*
QVJ , The W. so wm9w
0 - than JIM sm. of Pbsoo-balm)
k 694-
molkadvely. The kbWk armliew
d - , I WIP
Ow "a times, al Jim W. a of at JIM ELI
rwwkv*, lawth
Ar. md dle ow m of 16" In dw grwmd mielme al-VION
+ ad v - " v:
wbm " mad " an the W0001111"Mim Cd!i~#w the -
oW-- U'lavololectnow. war.. "It thea-eml-somme books.
"oom air thk v*"awl Siva as IP161 - 7012":
Ots - -")112700 - 9-vomm) - *41 a1w. kof 9
go. ad Phato Carriers PLT NA WhMuttlamacead, awfam arft
*.d-. and bmKv for the mtmetkwwY Nt.
Mary Vt. q0t
r-ut..u
bm law 41 an c4md, 00
7bou (111m, mdr eRmt obw ) -a FVmd to
>
It. mwmm. u >
n. th" N4 - (ef.M7.)
f-T ). whilaived - I/t. wMA m& trA nP41.
T, h 0 - pedt1b, &FA.
rIC"Amor"Iows ='"0k
aummi to be c &,wtwv of a t"Op. t
A. Ow m, fez apeowle t m - t1# -a aw f4m. a
(211s/csf); I sives. For the hmp. favAg" I Md IL ftm..
bg Q~rq#.
"Whis"11- ONOWia" I" CvbO bw bmnw on by Ibr
of pbo - In the nor of q abmpdm im
C&40- Tbe c . c am bt wMtt" t - pie'. whime 01
ratiocithavo.e1qvionfacmd. bythelight ftewthig Arbwek ~
MANI the ow of qamsta a' I I in the intwwtko so VSM
with tbw lvc~ me. It Imimn that a - Irls and,. ff 0,
IMN'Tatumot - Iltbamov.0- V1. Forlbri'd..
0
W-vw" of Age the th"wy civ". In the imp
Na. - tfal2vose -- et"r,'mod lie III, No, pt=
m Ap"Ment Willi expd. a Tbw

o 0 00 a 0 00-0* 0,411,1016 to a* o dlwt '.1-
0 0 0 4 '" 1
Id 11 yj 13 14 it V Is 30 a 41 a a at a 0
00
IT Ak "'m A J-1---

IL

(11 Russian.) E. KondorAil. DrAladj, AA4.
I u uk SSSR (H
clx)rb of the Academy of Sjenm
4 tilt! USSR), rK'w sc-r., v. 74, ScIA. 11, 19W. p. 213-
216.
004 MarKik' Pn4w"k-s of fmutualpiak-
sublunm
-11powd of spheift-Al -PAI elliplit-A j)Artjc-jL,. Alki
'000 the rektionship of thnfr cocircive (orce to shape and
04
-rr -in] -rent
land init wi for difft values of
991.0 iN
4io;1

'T
AIL!

&%..%LA I.ETALLURCKAL LITERAT&MIE CLATIVICATIOW
V)v 0011 ;14 Ila' ;Ik of a CIE It It
0 0 a 0 a 0 * 4
19 :1
0 0 0 0 0 0.0000 0 0
An I. t v w o I N
UO n I in
0 0 010 0 0 0 0 0 0 0 0 0 0 0 0 0
9 -0-66 11111111 0
;1-*-o o L : : L : :
-00
Ah Ah
-91
v04
:tol
Mal

Ut~~/Physics Ferrom'agnetic Powders 11 .Sep',33.,
"Theory of Coercive Strength and Magnetic 3 .uscepti-
bility of z'erromagnetic Powders (Dependence Upon
Packing Density)," Ye. Kondorskiy, Inst of Phys,,.
14oscow.Stat.e U imeni Lomonosov
"Doh Ak UP-4,k SSSR" Vol =, No 2, PP 197-200
Concludes that if the particles are one-domain for
very small concn,. then they remain one-domain dur~
ing incre ase in tLe density of packing; thus the
coercive strength of powders with spherical parti-
cles does not deper-A on concn, and the coercive
strength of powders vith elongated particlez can
increase for small concns with increase in the
221.
packibg density. If not one -domain for very , amall
c.onchs, the pa~zicles.can become one-dommin vith
increase in the packing density at a certain concn, vo.
Submitted by-Ar-ad M. A. Leontcrvich 13 Jul 51.

Hoeks SqpA
eeg" les N69OWUSUP
"Theory. or Napetic Frow-ties of Rocks and Powder*,"
To. Kondorikiy, Geoph" InSt,~ Acad Sci UM
"Is Ak Nauk SOR, Ser Piz" No 5., PP 47-54
continuation of a previous work (c:t Ye. Kondorskiy,'.
Ak Nauk SSSR Ser Geograf I Geof :LZ * No 4, 1950).
Describes method of detn of magnetIc susceptibility
ar aixts contg elongated or flat grains, variously
located, and derives formlas of magnetic suscepti-
bi2ity of these mixte. On basis of these formilas
226T57
he evaluates the effect of elongated and flat gra In&
of rock on its magnetic susceptibility., Derives
formw2as for obtaining the max magnetization of -the
mLxt. in the terrestrial magnetic field. Received
NaY 52.
226T57

KOPI)ORSKY, YEE.
*00/0*ies coerelvity
..113ature of High-Coercive Force of Finely Dispersed
Ferromagnetics and Theory of Single-Domain Structure,"
Te, Kondorskiy) Sci-Res Inst of Phys, Nos State U
"Is Ak Nauk, Ser Fiz" Vol 16, No 4, Pp 398-411
Studies cases of high coercive force and the condi-
tions of existence of single-domaim atructure., Con-
diiiiii that it 'p irtic' les "w'-e o.f. s.in.gl.e-d'o-ma-ifi- wtruc-
titre af, low concns,.they vill remain so at higher
concus.
241T85
PA 241T85

KOIMORSKIY, E
~USSR/physjcg- Mpetic BILturation Jul/Aug 59
-"Depende=6 on Teuperature of )kgnetic Saturation
of:Binary"Perronickel Alloys at Low Temperatures,"
.-To. Kondorskiy and L.'N. Fedorov, Cent Sci-Res
~Inst of Ferr Ketallurgy
"1z Ak Nauk, Ser Piz" Vol 16, No 4, pp 432-448
~Ztudy of effect of thermal treatment on magnitude
of magnetic satn of binary ferronickel alloys.
Finds that the "law of tvo thirds" satisfactorily
4escribes the thermal dependence,of alloys of
,pervalloy tM at varioua concus.
241TOO
PA 241T88

Moaq-o"nedomala-putichm. BrKondorskif (M. W
"3~'V ffO3')Y, 'cf. VM. ;4, 213jig"
so).
C_4.4S,9WSg The short half-axis Re for which ellipsoidal
Chemical Abst. particles of a f;22guetic powder remain absolutely one-
Vol. 48 No. 6 domalu. Is calcd. Functions of a different type from those
used previously are used to represent the cwnponent3 of the
Mar, 25P 1954 I'magnetization I wh:ch correspond to a min. free energy IV.
General and Physical Chemistry The Iterative method Is used to solve the variation problem.
The largest R for which I remains uniform -is R :!~ Re -
(0-0511,) VIO _cA/a*1Vx, where aa is the distantft betneen
atoras of the cubic lattice; Nx Is the demagnetizing factor
along the short axis of the particle. This 13 tht: same result
as obtained before. empt for the factor 0.05. The coer-1
cive force is now 11, - (2 K11,)[1 - p (I -
where P h a coeff.' depen,fing an I., K, and M, and N de-
Mids on die -oncn. of particles In the powder. E. 11, 5.

KONDORSKI, YE. It
ireieso wigineer
June 1954
Materials and Sulsidiary Techniques
-1 Nickel-=na X-OMM.--.
a C
Mlol'k.-. (C. R. Acad. Scs.
U.R.S.S., 11th
Nov. 1053, o. 9 o. 2. pp. 237-240.
In Ruwimn.) The relaxation times and g-factors of three,
ferritts were calculated from resitIts of an experimental
determination of tile real ;tnq Imaginary component3 of,
the magnetic pernicability ind Vic dielectric constant at!
Wavelengths of 3-2 and 8-6 cm WiAl tile &qmpl. pl;=ed in ~
a steady magnetic firld. Tfic ellm-rimental methodis.
described. Results aft- tabulattkl and. for one ferrite,
whown graphically.

Y, Lle ,
XMMMKrT-j*.; PAIRMV, A.
On the theory of the rolfV `-on Vetween spontaneous most i2at ion and low
temPeratum- DAIO'M 0 ?3 n0-3:431-434 N 153. 6;1.1.)
1. Inetitat Mild FAskovskoge-goandarstvannogo univereltsts, in. K.T.Iame-
nosova. Prodstavlono Wmdealkou K.A.Leoutoviches. Me IruouLaOlem)

The Comittee on Stalin PrIzes (of the Cotmcll of Ministers USSR) In the fields or
8CIe=* Wd InVentim& OUPOUums tbat the follavUzg ocientific warko, popular sclon-
tific boakn, szA textbooks have bew-subatitted for compatition for SWIn PrIteo for
the years 1952 and 1953. (Sovat#M, natura,, Moscow, No. 22-40,, 20 ftb - 3 Apr 1954)
Title of Work
Kondorshiyj Ye. 1.
Vbrks on the V~eory of
fel.r.- mr-'rnutism
Nominated by
IbSCOW ~Itate University
imeni 11. V. 101=030V
SO: W-30604, 7 Jay 1954

-2~
UnHhhysics
Card
Authors Konderskiy,.E. and-fakhom'ov, A.
Title I Theory.o.0 the relation between spontaneous magnetization of metals and
alloys and temperature in the low temperature-range
Periodical Dokl. AN 533ftj 96, Ed. 61 1139 - 1142, June 1954
Abstract A formula was derived for-the relation between temperature and spontane-
-4
OUS-magnetization,of a weakly conductive ferromagnetic latt.,ce each atom
of whi6h has two electrons on the,unfilled shell. The number of energy
levels becomes double In comparison with tha case in which each atom has
only one electron on the.unfilled shell. Four references.
Institution The M. V. Lomonosoy Statc University, Moscow
Presented by Academician M. A..Leontovich, March 17, 1954

EDNDORSKIY, Ye.; OZHIGOT. 1.
loililillilli$~l
Blectr1c resistance of Iron-nickol, alloys and its variation in a
,goetic field In the low (14--90 1) temperature range.
strong ma
Dokl,AN 3SSR 105 ime.6:1200-1203 D 155. (KUU 9: 4)
l.Institut fisiki Reskovskogo goadarstwennege universitsta Imeni
M.T.1emonesova. Zrodstavlans, akademikom G.V.Kardy=ovym.
(Iron-nickel alloys-Blectric properties) (Metals at low temperatures)

KOm)OaSKIY,,I:.5 GALKINA, O.S, and L.A. CILMUKOVA
i
"The Ualvanomagnetic liffects in Nickel and Nickel Alloys at
the Low Temperature It (2-20degreesK) -,IIoscOW
Conference on Physics of k1agnetic Phenomena,
JUY 1956, Sverdlovsk, USSR
f

KONDOR~JKIY and OZHIGOV, I.E.
I';.- L~-
"Electrical Resistance and its Change iril.the Strong I*netic Field
in Fe-Ni AnWa at the Lov Temperature" (14-77 degrees K) Hoscov
Conference on Physics of Magnetic Phen=enal
fty 1956, Sverdlovsk,, USS2
0

KONDORSKIY, E.
"Low Temperature Properties of Ferrimagnetx.," a paper presen$ed at the Institution
of Electrical Engineers Convention on Ferritea,, Londons 29 Oct - 2 Nr Mmber 1956

LIVSHITS# - Boris Grigor' yevich. prof Saw, doktor takhnicheakikk nank;
rofessor, doktor f1siko-matexaticheekM sank#
retse"OnSI-MMURADT A.G.,, doteento kandidat takhnicheek14
1 0
nank, radektor; $MV, D.I., tekhatcheekly redaktor
Utweleal properties of metals and alloys] rivicheekle evoletva
astallow i splavov. Noskyas 1kove usuchno-tskbn. Isd-vo ushiso-
stroito lit-ry. 1956. 352 p. (NLPA 10:2)
(Alloys) (&%81B)
USSR Magnetism. General Problems F-1
AbsJour Ref Zhur - Fizika,, No 4j 19*57.. No 9471
Author Kondorskiy, E.I.
Inst Wo-T-gi-i-ren--
Title DeveloFment of Research in the Field of Physics of Magnetic
Phenomenon. (Conference in Moscow)
Orig Pub t Vestn, AN SM, 1956, No 9, 95-98
Abstract Report on a conference on the physics of magnetic phenomena,
held in May 19569 in Moscow, together with a survey of the
papers,
Card 1A

137-58-2-3853
An Investigation of the Magnetic (cont.
relationship, of MS to temperature at low temperatures is better described
by the "T3j 7.,' than by the "T21' law which is usually employed at the higher
temperatures. An increase in MS is observed when the alloys are annealed;
this may be explained by the effect of the ordering process. The change in
mean atomic magnetic moment on ordering is 3-3. 5%. The IRT3/?-" law for
MS makes it possible to calculate the 191 parameter characterizing the ex-
change reaction in the alloy. Annealing causes 81to increase by about 15%
relative to the value for the hardened state. An analogy with the similar
Fe-Pd system leads to the conclusion that this change in exchange energy
is due to the ordering processes. The Curie point 0 of the corresponding
alloys undergo little change as this occurs. The 0;49 ratio dimishes with
with diminution in the Ni content of the alloy, inasmuch as Oland 6F are
dependent to different degrees upon the value of the mean atomic magnetic
moment and consequently change differently with variation in the composi-
tion of the alloy. P.S.
1. Lrew-nickel ILuoys--mapetis prope.Uos-Thernal factors 2 9 Im-tdakel
aLueys-mispetic pnportiea-4baswessat
Card 2/2

137- 58- 2 -_385-T------
Translation from: Ref6rativnyy zhurnal, Metallurgiya, 1958, Nr 2, p 226 (USSR)
A UTHORS; Gurvich, Ye.I., Kondorskiy,_.Ye,1., Popova, V.P.
TITLE: The Permeability and Losses of Magnetically Nonretentive
Alloys of Various Thickness in Alternating Fields (Pronit-
sayemost' i poteri magnitomyagkikh splavov raznykh tolsh-
chin v peremennykh polyakh)
PERIODICAL: Sb. tr. Tsentr. n. -i. in-t chernoy metallurgii, 1956, Nr
15, pp 131 - 151
ABSTRACT: Measurement of the magnetic permeability and lossi(L)
was performed by a bridge 'circuit in accordance with a'
method previously suggested (RzhMet, 1957, Nr 12, abstract
25220K), and at induction values attaining 80% of the satu-
ration level in the frequency interval of 400-300 kc. 0. 2-0. 02
mrn gage strips of the following commercial alloys were in-,
vestigated; 50N,.N79MA, 8ONKhS, 5ONKhS, and 79NM. The
L of high-nickel alloys drops invariably with a diminution in
the thickness of the strip, since in the case of these alloys
the L are fundamentally determined by eddy currents. In the
Card 1/2 case of low-nickel alloys a significant portion of the L are

137-58-2-3857
The Permeability and Losses of (cont.)
hysteresis losses, increasing as the thickness of the strip diminishes.
Therefore, in the case of these alloys, each frequency value corresponds
to an optimum thickness of the strip at which L is minimal. Recommend-
ations are rnade U?r the employment of various alloys in different fre-
quency intervals, band the optimum strip thickness. for.the various fre-
quencies is indicated.
P.S.
II, Nickel allays-Magnetic properties-Masweant
Card 2/2

IAU()Rszlr, YO.I.
v""Immum- --. .
Pr6grass In sbudiss on tbo PbYllC~ gg vp~pqtjc phenomena (con-
ference in Koscow). Test. AN SM 26 no.9:95-98 3 '56-
(valpetlim) OU-M ggil)

K0 N D 0 R 5 K %Y1 le-
'SUBJECT USSR / PHYSICS CARD061 / 2 PA 1471
J%UTHOR KONDORSKIJ,E.1.9 PACIMOV0A.S., SIKL 9T.
.,,.TITLE On the Theory of the Spontaneous Magnetization of Ferromagnatio
Semiconductors within the Domain of Low Temperatures.
PERIODICAL Dokl.Akad.Nauk, 101, fasc.5, 931-934 (1956)
Issued: 10 / 1956- reviewed: 11 / 1956
Here the temperature dependence of spontaneous magnetization is computed by the
method of second quantization in the form worked out by N.N.BOGOLJUBOV and
S.V.TJABLIKOV. On the occasion of an indirect exchange, as e.g. in ferrites? the
RAI-d'ILTONIAN can be represented by the introduction of the so-called integrals of
indirect exchange in the same manner as in the case of direct exchange inter-
action. This HAMILTONIAN is explicitly given. The crystal lattice of the ferrite
examined on this occasion can be represented as the totality of two inversely
magnetized not equivalent sub-lattices A and B. For the energy of the ground
level (the lowest level) an expression is given. The energy spectrum of the
-L
system, which is necessary for the determination of the temperature dependence
of the spontaneous magnetization, is determined in the state near the ground
level E 0 of energy, i.e. for weakly excited states. The IWAILTONIAN is transformed
by transition from spin operators to FERMI operators.
The eigenvalues E k of the HAMILTONIAN are determined from the conditions for the
solution of several equations mentioned here and from normalization conditions.
The solution results in 2 systems of equations for the determination of the
coefficients. The two solution ansatzes for EM and E(2) are written down for
k k
DOkI.Akad.Nauk, 109, fasc-5, 931-934 (1956) CARD 2 / 2 PA - 14711
the here investigated case of two nonequivalent sub-lattices. These solutions
for ferromagnetic lattices differ essentially from the corresponding expressions
for the antiferromagnetic lattice mentioned by 1T.N-B0G0LJUB0V and S.V.TJABLIKOV,
Zurn.eksp.i teor.fis,]J, 251,256 (1949)-
By transition to approximation of the next neighbors the formulae:
E(')- ~ + E a 21k 12, E(2) . Z a2 Jk12 are obtained by the development in series
k 0 1 k 2
of the coefficients according to low values of the wave number k restricted to
terms of second order (with respect to k). Here a denotes the distance between
the next neighbors; ~ 1 9, and E2 are expressed by the integrals of the direct
exchange among the nex? neighboring ions. Now the effect produqed by an exterior
magnetic field on the system of electrons of the ferrite is taken into account,
an&, after carrying out the usual statistical thermodynamical computations, the
expression is obtained for the temperature dependence of the spontaneous maEneti_
zation of the ferrite within the range Of low temperatures.
In the same manner it in possible to deal with forrite, the crystal lattice of
which consists of a totality of three nonequivalent sublattices.
INSTITUTION: Moscow State University "1l. V. LOMWOSOV,1.

r
48-8-12/25
A
L
AUTHORS: -
.
Chernikova,
Kondorskiyj Yee Is, Galkinal 0. S-Y
-
OWTITLE: ---------
The Electric Resistance and Its Modifications in the
Magnetic Field and in Nickel Alloys at Low Temperatures
(Elektricheakoyo soprotivleniye i yego izmeneniye v
eraturakh)
kikh tem
i
s
p
magnituds pole u epleov njWya pri n
PERIODICILt IzvestUa Aked. -Nauk SSSR, Ser. Piz., 1957, Vol. 21, Nr 8, pp.
1123-1130 (USSR)
ABSTRACTt The task to~bia accomplished by this paper was to investigate
the specific slectrie'resistance and its deviations in the
magnetic field in the case of nickel and its alloys with copperp
-
ah4-14~V204
chromium, &n& manganese at temperature of VW6_46,2
1. The present work intends to re-oxamine the theories cou-
cerning anomalies of electric conductivity of ferromagnetic
alloys* and the furtheLr development of knowlodge of this
field* Such Scientific papers an deal with thissubject-are
u"Istisfactory. Existing scientific tre-
here described.as
.
atises concerning this field by the scientistas Meisnet and
Voygt, Smitp ~ondorskiy and Ozhigov, Mazumoto and Shirakava
Are mentionedq bUt J%L if said in this connection that the
problems raised by the present paper have hitherto not been
Card 1/ 3 dealt with. In the chapter dealing with Measuring Methods it is
WZGn CO
Pp4~F-a_n,_d7_a7-
pro-
_2K- -resistance is onl
depende
t
y t
n
.
on temp
I
w
o very 0 degree
erature at 4.242o
4OX
l

Card 2/ a
t
loys
w
, but that in t
he case of
ith 15 and 2o% copper cont
t
;

3 en
2*3ooO t
and at a t
he decrease Of th
mPerature of
e resist-,,-e was determined according to
'he Electric Resistance and fts Modifications in the Magnetic 48-6-12/25
Field and in Nickel Xlloys at Low Temperatures.
the increase of temperature. In the chapter dealing with Modi-
fications of the electric resistance in Ni-Mn alloys becominL_
"ordered" it is said that the value RT7RT of th e doma orien-
tation in the longitudinal magnetic field diminishes in the ca-
se of the aforementioned NJ_Mn alloys- At the temperature of li-
quid helium this value increases to six times the value it has
at a temperature of 2830K in the case of a hardened alloy. In the
case of NJ 3Mn samples this value at first rises after cooling of
longer duration with the rising of the field, but it then decrea-
sea againg and in the case of strong magnetic fields and tempera-
tures of between 195 ard 2030K it even beoomes negative. The co-
efficient characterizing the inclination of the curves of this
value from the.field is reduced according to the extent of the de-
crease of the temperature, and therefore this value changes its
sign at low temperatures and Particularly strong fields. There
ar.e 11 figures, 1 table, and 11 keferences, 5 Of which are Slavic.
ASSOCIATION:
Dept' Of FdYsics. Of XoscowoState University imeni M.V.Lomonosov
(Fiziche8kiy fakulltit Mosk V-gkogo 908-Universtet& imeni U.V.Lo-
AVAILABLE: Librarv of monosova)

AUTHORSt Kondorskiy, Ye. I.0 Ozhigov, I. Ye. 48-8-13/25
TITLE: The Electric Resistance and Its Modification in a Strong Magnetic
Field in Iron-Nickel,Alloys Wi%'hin the Range of Low Temperatures
(14-770K) I
_(Elektr1cheskoye soprotivlen,.Jye i yego izmeneniye v
sillnom magnitnom pole u'zhelezonikelevykh splavov v oblasti niz-
kikh (14-770K) temper'stur).
PERIODICAL: Izvestiya kN SSS.R,Ser.Fiz., 1957, Vol. 21, Nr 8, pp. 1131-1132
(USSR)
ABSTRACT: It is'the purpose of this paper to re-examine the quantum theory
of the electric oonduotivity of ferromagnetio metle as well am
to develop this theory further. The data given by Shirakava are
cited here which refer tb the temperatures up to -1950. The next
stage of the-work is the investigation of the specifio resistance
and galvanometric effectA *R /R of the longitudinal magnetic field
of iron- nickel alloys with a" nickel concentreltion of 4o-loo% with-
in range of the low temperatures 14 # goo K and determination of
the temperature oonnection Q with the 8 R /R value, as also the
explanation of the respective effect prodftced by thermal treat-
ment of the samples is given. The samlies are taken from the melt
in the high-frequency furnace. In order to attain an"Ordered
position" of the samples they are annealed in stages during a
period of 14 days (and nights) at temperatures of 5oot 41o0' af-
'
Card 1/2 ter which they are slowly cooled. The "unordered state" was
again

lye " z
AUTHOR PAIMOKOV A.S. PA - 2679
TITLE -MC09=1111"U~11yell'No the theory of forromagnetism of metals and
allsys'at-14W 16APer4tutes, (K toorii ferromagnstisma
motallov I - splaw6v -pri'algilkh temperatukakh. - Russian).
PERIODICAL Zhuinal Mesperim. L Teeret, Piziki 7-957t Vol 32, Nr 2.
pp 323 .. 332 (MMR).
Rociived : -5/1957 Reviewed% 6/1957
ABSTRACT The pr*#*nt-*ork.bAs the folloving six:
ormination of the theoretical dependence of spontaneous
asoetisatlsn'isA ~4sikporaturs in close proximity to absolute
zero if the-'naiibror of electrons with ot oomponastod nagnotic
moments Is 1a-rf'o'r than the number of atoms,,
-2.).Doki a of, temperature dependence of
T*t1of for*u~a*.:ror the
the Apontan6fts'Aagnot1sation (at low temperatures) on binary
forromw4noite ordered alloys of a different crystal.. structure.
&M.'with 41ffetent - composition.
,it titit the goa#X&I-eass of & arystal-is investigated which
consists'ef 1-ateas of-types..t4t are,aiffor*nt froa h.
'Those^ atoms A'": assumd to, be located in th'-- nedes'ef the
latt0*- and- each atexi Is assumed to have f *Xrox.4anIOtto
tle 8 'sh
ciien (which differ fre's each other by theiii'stat0lo
The RMLWSW the ry#toa is written dwn for the case
that only an electrostatic interaction is taken into account.
CARD 1/2
CARD 2/2
USSR/Magnetism, Magnetic Resonance F-.5
Aba JOur : Ref 221ur - Irizika) No 1) 1958) 1198
Author : Bweshko, I.Ae, Kondorskiy, Te.l.
Moscow state MiTersity
Title TemPerat'ure Dependence of the overhouser Effect in Metallic
Lithium.
Orig Pub M. eksperim. i teor. fiziki, 1957, 32, No 3, 61l-612
Abstract 7he Overhouser effect was invegtisLted in d_jspx-8ed me-
tLIlic lithim in the teaperature range from, 77.2 to 3730
X in & constant nagnetic field of intensity 30-10 oex~sted.
The results obtained show that the width of the resonAnce
line increases with dim4nishing temperature.
Card 1/1

KPIM I. and SEDO-) V. L. (University of Moscow)
r.
"Variation of Saturatim Magnetization and Electrical Pasistivity of FeNi
Alloys, under Isotropic Compression at Lcv Temperatures."
report presented at Colloquix on-Magnetism, Grenoble, France, 2-5 Jul 58.
Eval: B - 3,111,755 3 SOP 58-

VOLKOVP D. I., XPINCHIK, G. S., MIRYASOV, N. Z., PARSANOV,
A. P.), RMEO V. E.J. CIMCMMNIKOV, V. I.# and GOFMAN, U. (Moscow
I uwy 9
"Results of Studies of Certain Magnetic and Magneto-Optical Properties of
Ferro-Maguetical."
"Saturatior Magutization of CuNi Alloys at Low Temperatures."
"Magnetic Tropertlen of MbB System."
"Thmperature Dependence of Paramagn tic Susceptibility of Ferrites."
'Nagmto-optical Resonance In Ferromagnetiss."M (Krinchik)
Report presented at Colloquim on Magoettem, Grenoble, France, 2-5 Jul 58.
Dwal: B - 3,111,755. 3 SeP 58.

240)
AUTHORS: Kondorskiy,Ye.l.,and Bakoshko,N.A.. SOV/155-58-2-43/47
TITLE: Overhauser-Effect in Metallic Lithium (Effekt Overkhauzera v
metallicheskom litii)
PERIODICAL: Nauchnyye doklady vysehey ahkoly. Fiziko-matematicheskiye nauki,
1958, Nr 2, pp 204-207 (USSR)
ABSTRACTs The arrangement of the exp eriment and the method described by
the authors in [Ref 5,61 are used for the experimental in-
vestigation of metallic lithium.-The authors investigated the
dependence of the nuclear polarization on the achievement of a
high-frequency magnetic field (by meap'A-rinq the amplitude of the
magnetic nuclear resonance) and the dependence of the nuclear
polarization on the frequency of the electronic resonance-The
results are represented in five figures and in essential they
agree with the theory. The strong #ispersion considered under
othetwise equal conditions for the difforent-inivestigated pieces
of lithium seems to be very interesting.'
There are 5 figures and T referencesp 2 of which are Soviet,
3 American, and 2 Italian.
Card 1/2

A.Iborl Voice, C.P., CoAdidate of Pk:.tc4l- -07/55- 5,1-2-34/35
11"heastical sciences
111"Al 3%r..y of blots Mead by cf zaaZz.
VaLvermitjr attheJ111-ftion CorCresscathwPhysks j.'
Obsor doklado~ U.h.nyka -0 ...... IC.
so'.Gh4haall po risik.
FMODICAL8 TGItAtk Wookovskogo Univeralleta-"orkys satemstW, smismak"s,
astrommit, fLsLbA, khM%, 1958. Sr 2.;; 2.7-250 (:::1) Mb
AWnCT. Irca December 6 - 11$1957 there took place the four-r. -&tan
Cow* as an phy.tas at magnetic swit.rt.l. IA L.nAnar". (-he
first two meetings took place 1946 and 1951 to
third 2.0tine 1956 in Rome..). The co~4r*.* .48 a .,.tied
Aced. my a,scienvom of the nstt. Npart-.1tt of Flyk I.
.to C..~'I 0. ru.d.miestal
1111themat isati,
fatut. or S.itcorA.Ctord of SLO
Probtaw cc f
Academy of 3cionces, USSR had Co=itt*o for V-Cottmes. it.re
@*to mom than '00 F:rticlpatorm. 59 I.atur.. -or. C%..A.
4111ang Shea the rot 1. tug I .tores of ch. of
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FafX#'1*rI&. of the F.rroz. *tic*-. ,
2. Frotom .or I.T. Taltenift. T-.T. X-Lrt~_-ttns. L-01-tmas
Ms "In*110 "I'm rerritea-.
SUthkoe. I.pIrmt
Olffact at Madmatic VIscoatty ou the Froquicy ClaieracterIsLics,
of rerrttoe-.
4. N'l.-". ty6r. Lecturer "7.rL&Iios of 3t.--Wro Q&4 Lati.
forromagisti* Proportis;, of Xi 3Pa..
I.A Go-bo,skis, L.oturs,,. S.Y.. 33~adpkays. _'unior Zri.ntific
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.;,ra,ry AllojFsI.
T. Irafeador Asai.tozt
-Bloc Sria
4. I.ZjLry now. Senior Scientific Asots:azt. A.?. 7arsotav.
sopirs.t !"CCOtic Prol.r.-I.0 and stru..." ar F.CC140.0 -
%*ran - Alloys..
9. X.&. SS91-ko.. Senior 3cl..ttfic
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