SCIENTIFIC ABSTRACT ZHILINSKAYA, M.A. - ZHILINSKIY, G.B.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R002064810014-5
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: July 20, 2001
• Sequence Number: 14
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

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77323
% AUTHORSi SOV/57,30-1-2/18
Gol.ant V. Ye. Zhilin
_skjy P.
Propa gation of Elect .roma
gnetic Waves in Waveguides
FilleO. With Plasma_
FMODICALt". ...Zhurnal 'tlk'hni c~heskoly riziki,
US 19600 vol 30j,xr 1j,
_~'pp.16 24~ sh)
AMTRAM'~ Propagation~of.eleotro
MagnstiO Waves through wave.
guides filled withz9aseous diaoharge plasma is
ulilized-in'oonstruotions of ultrahigh frequenoy
oommutati6n devices'and in plasma investiiations,
One would.likej therefore, to establish a relationship
between.the propagation constAnt.ot these eleatro-
magnetia.waves and the complex conductivity Qf
plasma.',This problem in thi oases of real plasma
must,take into account the varying conductivity,of.
piaom~ain the waveguide due tb VarYing.concentrations
of electrons in the plasma.. In the present paper,
the authors inVestig&ta wave propagation-through a
uniform wav
eglkide filled with plasma homogeneous
~.along the.axis of the waveguide. Waveguide boundaries
Card IA6 and plasma oon&ictivity are then independent of-the
TI

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Propagation of Electromagnetic Waves, in 77323
a
~Waveguides Filled With Plasm, SOV/57-30--l-2/18
'and in the second:
AP(2)P.02 C2 ' d15
I, ~UF)! G,EVF
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2.

,E,E dF) E,EkdA
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0,EOE,dF
(31)
110
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POO ff a,EO*dF

y,E.E,dF) ( -,E,,E,dF)

it' [
(j 0AE,(IF
OjEOEjdr)jj (32)
.
pt 2
:Card .6/16
1 41"'! fi~, -11 dii,

-~M
Propagation of Electromagnetic Waves in 77323
Waveguides Filled With. Plasma SOV/57-30-1-2/18
where k now denotes TE waves and the-TH waves. -
The:authors,'di
scuss the case when the frequency.of
electron collisions with neutron pa'rticles is much
ions. Tney also discuaB
higher tban.c.ollisions with
the possibility that the plasma is conducted through
the waveguide by means of 4ielectrid tubes. One could
try to develop relations for unperturbed fields in
the -Waveguide-with.the tubing but without the plasma.
However., this,problem often does not allow exact
solutions., and in.the case of small tube thickness one
can againanalyze its.contribution to the phase-shift
and damping by,means of the perturbation theory.
Finallyl,..the authors calculated the cylindrically
symmetrical case. The geometry of,the problem is
given in Fig. I.
Card
7/16
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P p S ~)606~11/61/031 /001/009/0
r o agation.of centime trile wave a 17
B1 04/B204
electrons Is t1hrw Iellian, and.,,that'the concentration distribution of
eleot:~6fts' over the croas ssction and electron temperature do not change.
The homogeneous longitudinal. 'Aield,, however, is changed by the presence
6VA"hi-h'frequency field and the following concentration distribution
9
of electrons takes place,in the positive column:
nF, - I r !!L ' 1
d F I/d El n '-a here the
In, con I Ill. 2 a 2
In
Con
electron concentration, I the discharge current, E the field strength
Coll
of the constant field, E the~amplilll-ude of the h.~gh-frequency field,
hf
In. the plasma conductivity in the constant field per electron, (f 1r the
active component of hi -f requenoy conductivity perolectroll. A similar,
gh
expression _is-'tiven~ for the increase of the discharge ourrent produced by,
applying the high~-freq',~ency:field. From these,formulas it may be seen
tfidt-the application, of a homogeneous high-frequency field to a positive
column discharge in steady-state conditions does not modify electron
-Card' 21'Y

26664
~Propagation-of.centimetrie waves S/05 61/031/001/009/017
B104YB204
tempetaturd't 'but-leads:to a,decreaee-of the longitudinal constant iield.
band to an increase ofth6 oonc6ntration of.charged particles. The authors
'W' i3tiito'that'i,n*first.pdrturbation-theoretical. approximation, the wave,
:propagation',boiiitiLht',dhiLhges-pr6portional to the electron concentration,
wheni'di.plasmia is introduced into a waveguide. The changes ifi the phase
conqtant ,Ap*:and the,'damp'ing constant Aa* in the.presence of a high-
frequency field are determined in first'perturbation-theoretical approxima-
tion by them relation.
a /A ~,-~-Ao YAO (7)v
k
-where ba*:~,and Ap*.werg determined at a, given high-freqqency:field
stimhithi :ind A a, and AP at an, infinitely -low high-frequency field
sfrength. ~The experimental determination~of the dependence 'of the:
phase constant upon field-,6trength was carried out by means of the
f acili ties.* described in the previois paper (Ref. 1). The resul to obtained
are graphic ally. represented ~in Figs. 2-5* As may be,seen, deviations
and experimental -values,for helium are below 15%,
anafor argon below 30%. The causes for these. deviations are said to be
Card 3/

20664
Propagation of centimetric waves
B104/B204
change s In, th e'.f lux of force, Inholmokeneities of the field, inexact
f field longitudinal components,and of conductivities
determination.0
Finikllk' lhd, use of nonlinear effects-for the stabilization of the
power of siitei-.;.high'frequ6ilcies',,occurring in a waveguide filled with a
plasda.is.discussed.. 'Fig. 9 shows the~scheme of such a stabilizer. This
scheme' rep--r-esents'-a'po'wer.divide,r made from three-decibel alit-bridges.
The superhigh-frequency signal is,divtded between the input channels,
and"tht ratio'of the-power-flows in the various output channels-is de-
termined from the phase difference between the waves passing through
the upper and lower waveguidese If a waveguide contains a gas discharge-.
ahd~phase shifter, 6 possibility:offers itself in that power range in which
nonlinear interaction effects of:the~plasma with the superhigh-frequency
field occur, of stabilizing the.power flow at the output of the power
divider. There are 9 figures and 8 references- 6 Soviet-bloc.-
ASSOCIATION: Leningradskiy p'olit,ekhnicheskiy institut im. M.~I. kalinina
(Leningrad Polytechnic Institute immi Me I. Kalinin)
D
SUBMITTE. :JulY.13, 19601
Card
4/

S/05/~76;~80/001/017/018
B111 B102
AuTHORS t Golant, V. Ye. and Zhilinskiy, A. P.
TITLE t Experimental study of the diffusion decomposition of A plasma:
in a magnetic fields' II
PERIODICALs Zhurnal 'tekhnicheskoy fiziki, v-~32, no. 1, 1962, 127 -.129
TEXT: The~authors measured the'de endence of the diffusion rate in a,
p
helium plasma~on pressure (0.02''- 0.8 mm Hg) and on the longitudinal
magnetic fielcl (uP to WO oe)- The measutements were made in pulsed'.
operation (20:cps, pulse'duration 1-2 liseo)i in the intervals between'the
pulses the plasma electron concentration was measured by the wavdgUide ~nethod.
''The 3.
diffusion coefficients measured are in good agreement with a formula
calculated in Ref.1 (V..Ye. Golant and A. P. Zhilinskiy, ZhTF, 30P-745,
ig6o). , it is found that the', transverse escape rate of charged particles inVK
thq magnetic,field.is.considerably.higher than the diffusion rate calcul-
at6d from-collisions between electrons and atoms. The plasma decomposition
constant was'found to depend practically linearly both onthe magnetic
field and~on. -pressur e. The orbital velocity of charged particles along the
Card 1/2
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A
CC NR: AP4009M
The ddcay.was.followed.bv,.,obs.orving the shift of the resonant frequency ofa micro-,,
wave resonant, cavity surround'Ing part of the discharge tube. In some. cases the
cha'nge' in the Q of-the ca ity was.also f llowed in order to obtain information about
v 0
~electronlcollision rates. Vlavelengths,in the neighborhoods of 3 and 30 cm, were em-
.-ployed. :Transverse diffusion coefficients were calculated :from the obrServed , do-
cay,curves with the aid of suitableassumptions concerning the longitudinal-diffus-
The transverse diffusion coefficients obtained-for pldsmas in discharge tubes
with.diametersl-of-4.cm 6r.greater agreed well with theoretical values., Those.for
plasmas in smaller discharge tubes did not, the observed transverse diffusio.i. coel-
ficients being greater than the theoretical by a 'quantity that is roughly indepen-
dent of the magnetic field. The following possible causes for this anoj~alous be-
havior are briefly discussed and rejected:::impurities in the gas; enhanced electron
temperatures; disturbance--of-the ambipolar diffusion mechanism by magnetic field in-
-homogeneities. ~The'authors consider it-most likely that an instability develops
and-gives rise to anomalous:transverse diffusion. The-excitation of oblique drift
waves,or ionial-acoustic waves, and1he development of small scale flute instability
are montioned.as possibilities,-During the experiments it was noted that even a vezy
small misalignment of the disoharge tube with:rospeat to the magnetic field would
plasma decay rate. The diffusive decay of a plasma in,a Pao-
Cod,2/3

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77. F-
,41 'rjt I -.1. 11
ng rai 8 y
TIM: Electromagnetic radiation from an electron boom traversing a plasaa in a mag-
netic fi
BOUkM-. 2hurnal tekhnicheakoy #xlkis.-v. U, no. 11, 1065. 2034-2041
-helivA ma,
TOPICw.TAGi; Elasm:beWt nt6raction :plasma, plasma oscllldti
on,;
asma-vave,-cyclotron resonance,:_electron beam
RACr-t The. autbx~rs' : ~
--AWT -hsveLjaV46mt'jg" -cit-wavelengtil~ Ajj~ .7
and... -a f aapi~uce~d6j 20 to 900 b
-radi tioun 9 ram,plam ems of 0.8 to 2 k*V elections
hoij.un At -r6a u g 5 16-4 to I x 10-1 mm Hg in t 1) me e
raversing p 8 rem ram he re no of a
2kOe or weaker uniform longitudinal magnetic field. The plasmas were produced in a
5 em diameter 40 cm long glass tube containing at one end an electron (p&n producing a
0.5 em diameter beam. The electron gun was operated with 2 Msec pulsea at a repeti-
tion rate of 50/sec. The radial distribution of the longitudinal aicvKKrave electric
field was determined with the aid of a uhf probe consisting of a section of twinlead
with 4 mm spacing, and the radiated microwaves were received with an open ended wave-
Card
MC., 533.9

ACC NRi Ap502&318
guide section located close to the discharge tube. The uhf signals were recorded
with a superheterodyne receiver with a 2 Re passband and a sensitivity of 5 X 10-12W.
One conductor of the uhf probe was employed also as a Langsuir probe to determine the
plasma density. The discharge tube contained in the end opposite the electron gun an,
anode and a directly heated cathode, with the aid of which a gas discharge plasma
could be produced. This plasma was employed to calibrate the LaaMuir probe in the
presence of the magnetic field and In some other auxiliary experiments. The plasma
produced by the electron beam was found to extend far beyond the limite of the beam.
The microwave field strength and radiation Intensity were investigated as functions
of the magnetic field strength, gas pressure, beam current, and electron energy, and
the results are presented graphically and discussed. The intensity of the uhf radia-
tion varied greatly with the conditions of operation, but such radiation was observed
at magnetic field strengths an order of magnitude lower than that C07reSponding to
the electron cyclotron resonance, and In soots cases In the absence of a magnetic
field. Further work will be required to elucidate the nature of the coupling between
the longitudinal ple-sma oscillations and the transverse electromagnetic waves which
makes the radiation possible. Orig. art. hast 9 figures. (151
SU13 CODES ME, EW SUMI DATES ISFeb65/ ORIG REP: 011/ OMI FMFi 006 ATD PRE SS:
V'V
Cqr~ 2/2

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WSR/Agriculture - Minerals
1/1 Pub 123
Card
A-ui'h- ora t thilinsklyt G'. B.) Cand. of Geological-Mineralogical Scienceo
Title t Mineral raw materials resources for needs of agrictilture

6
IAZEIGeology - Minerals

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W081/62/000/005/029/090
B15O/D101
AUTHOR. Zhilinskiy, G., B.
TITLE: Some rules governing the distribution of germanium in iron
ore deposits
PERIODICAL: Referativ.nyy zhurnal Khimiya, no. 3, .1962, 127, abstract
3G93 (Izv.~AH~KazSSR. Ser. geol., no. 2 (43), 1961, 70 - 77)
TEXT: By meIans-of spectrum analysis. a a tudy is made of the distribution
of Ge in deposits-of sediment.ary-metamorphic Fe-?&i formation (tabular
data are not aiiorn). , For cheo'king purposes about 100 chemical and
microchomical determinationsof Go were made in different minerals, rooks,
and ores.. Complex Fe-Mi ores are referred to a powerful stratum of Upper
'Devonian and Lower Carbonifer oue sedimentary rocks. Mn ores in general
play.a secondary part.- Brief.details are given of the mineralogical,
composition and, 1he -genesis of the deposit's studied., Curves are plotted
reflecting the .distribution of Ge in the ores assayed vith a different
c6ntent of Fe. Besides having the greatest concentration of Ce, the
ore assays containing 40~ and more of Fe also differ by a moreuniform
Card 1/3

3/081/62/000/003/029/090.
'Some rules governing the ... B150/B101
...,distribution of this element. Based on.an analysis,of the pure minerals
hematite, magneti,te,,.,aiderite,.braunite, usilomelane, galena, sphalerite,
pyrite and arsenopyrite:- itiq.,establish~d that the only minerals carrying
Ge in the Iores-atudiedlare magnetite (more) and hematite (less).-In the
assays of concentrated carbonaceous rocks no Go was found. Correlative
Curves are submitted showing the interdependence of the distribution of
Ge with the. principal chon., i1cal* componento of the iron ores studied (Fe,
Mn, S, P). A direct Correlative dependence is observed between Fe and
Ge, rhich is leas.clearly expressed in the hematite ores, but more so in
the magnetite ores. The same dependence between the content of Cc and Fe
is also established in the ferrous rocks. In the case of Un and P there
is.inverse dependence. 'Nith a very small content of Go and S in iron ores
a clear direct deDendence is observed bet,,,een theze elements. '-7ith an
ease of concentration Go and S inverse d nendenceja
incr (> 0-3CA of
revealed. The author comes to the conclusion thdt Go in the iron orcls
studied in geochamically comibincd only with Fe and, possibly, ia prosent
in the form of germanatesp rohich-are near, to the mineral stottitfe. 011 the
baois'that the hematites with the largest imprognation of Go art- of the
earliest generation and the least impregnated hematites are of the latest,'
Card 2/3

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3(5) PHASE I BOOK EXPLOITATION SOV/2243
''Zhilinskly, German Borlsovich
Olovonoanost' T8entrallnogo Kazakh8tana; olovono8nyye rormat8ii I
mesto v qbshchey metallogehii regiona (Tin-bearing Possi-
bilities of Central Kazakhstan; Tin-bearing Formations and Their
Position in the General Regional Metallogeny) Alma-Ata, Izd-vo
AN Kazakhskoy SSR, 1959. 209 p. Errata slip Inserted, 1,006
copies printed.
Sponsoring Agency: Akademiya nauk Kazakhskoy SSR. In.stitut geolo-
gicheskikh nauk.
Reap. Ed.: N.G. Sergiyev,.Corre8ponding Member of the Kazakh SSR
Academy of Sciences, Professor; Ed.: L.S. Rzhondkovskaya; Tech.
Ed.: Z.P. Ror6kina,
PURPOSE: The book is inte6ded:for geologists and engineers engaged
in tin exploration and.mining.
~Car,d 1/8
14
V

Tin-bearing Possibilities (Cont.) SOV/224
3
COVERAGE: The book deals with the geology of tin-bearing formations
in Central Kazakhstan. All deposits are described,'and evaluated
as to the content of tin Mineralogical peculiarities and petro-
chemical features of.tin:bearing intrusions and a genetic classi-
fication of lode and alluvial tin d6posits,are provided. Admixt-
ures of other elements in tin ores are-treated to a considerable
length. Both lode and placer formations 'even if not of direct
economic.significance, are treated in detail. Themetallogeny of
such formations is discussed, including rock alteration, migration
and mineralization processes. Genesis of all individual occur-
rences is analyzed and explained. A short history of-discoveries
is given in the introduction. The leading geologists are mentioned
chronologically. The.chronology is divided into two periods.
Period I extending from 1935 to 1942: A.V. Birin, P.A. Ostrovskiy,
Ye. A Fierov, M N. AlItgauzen, Yu S Vyazovoy, I.A. Grechukhin,
S.P. iershov, F.i. Kostyuk, D.M. i~vl;nko, N.M. Salov, and L. Ye
Khazanovich. Period II, extending from 1948 to 1953: G.V..Tsapiin,
M.Ts. Medoyev, V,G. Volobuyev, M.A. Zhukov, M.N. Grinvalld, A.K.
S.M. Zharin, P.O. Nikitin, M.*G. Popov, A.A. Rostorguyev,
A.V. Stepanov, S.,Sermagulov, M.A. Yurchenkov, V.M. Shullga, and
Card 2/ 8

Tin-bearing Possibilities (Cont.) SOV/2243
Ye.A. Flerov. Most of the prospecting was carried out by the
Sredazolovo Combine. The author thanks-M.P. Rusakov and I.I.. Bok,
both of the Kazakh Academy of Sciences; N.G. Sergiyev and Ye.D.
Shlygin, corresponding,members of the KaeAkh Academy of Sciences;.
G.N. Shcherba,,.,V..V. Lavrov, and V.K. Monich, Doctors of Geolog-
ical and Mineralogical Sciences; I.G. Magaklyan of the Armenian
Academy of Sciences; Kh M. Abdullayev of the Uzbek Academy of.
Sciences; Professor V.A: Sokolov; and Ye.A. Radkevich, V.S. Koptev-.
Dvornikov,.Iv.F. Grigorlyev, A.D.:Kalenov, and I.I. Chupilin,
Doctors of Geological and Mineralogical Sciences. There are 193
~so
references: 180' vie7t;-il2.'Ewilfo)CAtid,t-l;-French.
TABLE OF CONTENTS:
Foreword 3
PART I GENERAL GEOLOGY 6
'Ch. I. Brief Information.on the'Main Stages in the Geological
'Development of Central Kazakhstan 6
Card 3/8

Tin-bearing Possibilities (Cont.) SOV/2243
Ch. 11. Tinbearing Districts of Central Kazakhstan (Description of
Deposits)
15
Tin-bearing district west of Lake Balkhash
a. Maykull deposits 21
b. Sholpan'deposits 27
c. Shakshagayly deposits 31
d., Karaungur.deposits 33

e. .
Southern Balaktan deposits ,
35 ,
f. Additional data.on.the manifestations of tin minerali-
zation in the district 38
2. Tin-bearing district of Atasu 39
a. West Atasu deposits 42
b
. Placers of.Yakovle'vskiy Valley (Log) 43
l SouthAtasu deposits 44
The, `g'roup' of, North Atasu placers, 48
e. The lode tin ~ineralization in the district of North
Atasu.placers, 52
J. Placers of.Buzauullgenskly Valley 52
g. -Tin-tungsten deposits of Karaob 53
~Card ~4/8

Tirl-bearing Pis sibilities (Cont.) SOV/2243
h. Other-tin-bearing manifestations in the district (of
Atasul 56
3. Ulutau tin-bearing district, 58
a. The Ulutau,group of placers 60
b. Tin-bearing manifestations in the Ulutau Mount
ains 63
c. Placer-type tin-bearing indications in the right
tributaries of the'Karaturgay River
4:. Kokchetav tin-bearing district
64
a. Dhebanay De posits 6V
b. Placers-of the Valley Nr- 3 68';.
Placers of the 'Valley Xr. 15
d. Knyazevka,'placers,;. 70
e., Placers of.Orlinaya~Mountain 71
f. Other indications of tin In the Kokchetav district 73
5. The district of Karkaraly and Lake Balkhash 74
6. Brief notea on tin-bearlng possibilities in the.remaining
regions of Central Kazakhstan; presence of tin in the ores
of other metals 76
..Card 5/8
7

Tin-bearing Possibilities,,(Cont.) SOV/2243
PART Ii SPECIAL TOPICS
Ch. III. Metallogenetic Characteristics andthe Classification
-0
f:Tin--bearing Deposits of Central Kaz
akhstan 87
1. Brief notes on the geochemistry of tin 87
.2. Genetic types of.tin-bearing deposits in Central.Kazakhstan 91
A. ~ Formation of tin-bearing (cassiterite granites 92,
B. Formation of tin-bearing tcassiteritfl granitic pegma-
tites. 94
C. Cassiterite-quartzose formation 96
a. The greisen type of deposits 96
The quartz-vein type of deposits 102
D. Formation of cassiterite-sulphide ores (skarn-type
deposits),
E. Placer formations 109
a. Ancient placers, 118
b. Recent placers 120
Ch. IV. Tin-bearing:Intrusions of Central.Kazakh8tan - 120
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I f"J
T I 111111

'Tin-bearing Possibilities (Cont.) SOV/2243
1. Back round of the problem 120
9
Age,of tin-bearing; manifestations and. the relationship;
between the-tin mineralization.and various stages of.intrusive
action
124
.3. Position,of tin-bearing massifs within the regional geological
structures;- particularities in the composition and structure
of such massifs-
a. Geological types of massifs and their relationship with
the structures 129
b. Mineralogi,cal composition.of tin-bearing intrusion's 133-.
a. Chemical composition of tin-bearing Intrusions
Ch. V. Geochemical Characteristics of the Tin-bearing Deposits
of-Central Kazakhstan; Metasomatism Processes; Tin
Transfer,.by Postmagmatic Solutions; Specific Associations
and Other Geochemical Factors of OreFormation 159
I. Geochemical characteristics of deposits. 159
2. Metasomatic processeL and the significance of the ex-
ternal mineral sources in the processes of endogenous ore
formation 163.
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Tin bearing Possibilities (Cont.) SOV/2243
3. Examples of mineral and geochemical associations 16~
4. The mode of transportation of tin in natural solutions
5. Nature of or e.filling cavities 170
Ch.,VI. Structural Geological Cbaracteristics of Central
Kazakhstan; and Significance of Tectonic Features in
Controlling the Distribution of Various Types of Tin~
Mineralization 172
Ch. VII. Basic Metallogenetic and the'Endogenous Tin Formations
of Central Kazakhstan 182
Ch. VIII. ExogeneouB Tin-bearing Formations of Central Kazakhstan
and Certain Problems of Placer Formation 190
Conclusion 200
BiblIography 204
A31AILABLE: Library of Congress
MM/ec
Card U8 9-22-59

AYRO7, P.Ya.; AYTIALIVEY, Zh. Ai; ALMOV, M.0,; AKHIMSAFIII, IT.R.; BATISHCK97-
TKRASOV, S.D.; ~ WARM,: N.TJO; BAISM, M. t, 13AYKC)MMOV, A.3,;
AWTUROV,:A.B.; BOGATYRFIV, A.S.; BOX, I.I.; BORTMUM, R.A.; M-rMCW"lW((O,,
BrICOW, 14.8. ZYWV' D.A.; IVAINKIII, P.-F.;
KAZAITLI, D.Na'; KNI~. A.~X#,; ~.AYV , S.X.; KOTATILINT , "'I .' V .
KMLkYZV, D.A,.; )CUSM,~O.L.; L~Ar,*,!, MSHANOT, O.Zh.,.JCb'DO'r,;'T,
MS.; IfORCH, V.K*;JMJTOV, S.: MJSR:-,'MV, G.; MUKEIAMMMOV, S.A.;
rARSHIII, AoV,; POFROVSKIY, SOL; POLOSUKH111, AoF.; RUUKOV, R.P.;
SMRGITAV, N.r..; sirmuill, S.Sh.; TAZHIBAT.MVO P.T.; FASMOKOV, 7.1%;
SRLTGIU, Ye.D.; 5HICIMBA, G.N.; CHOKIN, Sh.Ch.; CHOLPARCULOT, T*Ch.
4jxtleth birthday of AcademieiAn Kanyah Irmdaevich Satpaev. Vest,
AN Kaza%h. SSR 15' no.4:58-61 Ap t59. (MIRL12:7)
(Srntpaev, Kanyah Imantaevich, 1899o-)