SCIENTIFIC ABSTRACT GLADKOVSKIY, A.K. - GLADKOVSKIY, V.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000515220015-0
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 26, 2002
• Sequence Number: 15
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

3(5) 15(6) PHASE I BOOK EXPLOITATION SOV11254
Akademiya nauk SSSR. Otdeleniye geologo-geograficheskikh nauk
Boksity, ikh mineralogiya i genezis (Mineralogy and Origin of Bmixites)
-61.1 Moscow, Izd-vo AN OSSRR 1958. 488 p. 2,200 copies printed.
Compiler: Dolgopolov, N.N.; Chief Ed.: Strakhov, N.M., Academician;
Reap. Ed.: Bushinskiy, G.I.; Ed. of Publishing House: Nosov, G.I.;
Tech. Ed.: Polenova, T.P.
PURPOSE: The book is intended for scientists working in geology and associated
fields, and managers of industrial and engineering concerns.
COVERAGE: This collection of articles by various authors on the mineralogy and
geochemistry of bauxites appeared as a result of a 1955 conference on the
origin of bauxite (Chairman, Academician N.M. Stakhov). The c:)nference dis-
cussed the genetic theories propounded by various Bcientistsp underlining the
weakness of L.S. Berg's biochemical theory and the hydrothernal theories
developed by some French scientists. The majority of Soviet geologists
appear to-be in accord with the sedimentary origin theory. The book discusses
problem on the origin of bauxite and describes some deposits found in the
USSR. Each article is accompanied by Soviet and other references, photographs,
diagrams, tables and maps.
Card 1/14

Mineralogy and Origin of Bauxites SOV/1254
TAKE OF CONTENTS:
Foreword
PART I. MffNERAIDGY Or BAUXITES
Mineralogy of Sedimentary Bauxites (S.I. Beneslavskiy) 7
1. History of mineralogical investigations of bauxites 7
2. Alumina-containing minerals 8
3. Silica in bauxites 21
4. Iron-containing minerals 23
5. Calcium in bauxites 26
6. magnesium in bauxites 28
7. Titanium minerals 30
8. Sulphur minerals 33
9. Phosphate minerals 35
10. Sodium and potasslum in bauxites 36
11. Trace elements in bauxites 37
12. "Lode f acies" in baxixites 42
13. Some problems of mineral formation in bauxites 44
14. Genetic classification of sedimentary bauxite minerals 48
Card 2/14

Mineralogy and Orij~tri of ?,wixites SOV/1254
Bibliography 49
The Origin of Alumina-bearing Minerals in Bauxite (K.F. Terentlyeva) 52
Bibliography
69
Mineral Composit ton, Origin and Metemorphism of IAnmr Cretaceous
Bauxites of the Ea~qtern Slope of the Urals and the Turgay Plainfl
(A.K. Sharova and A.K. Gladkovskiy) 70
Bibliography
PA!?T if. GIWRAL PROBIaB ON THE ORIGIN OF BAUXITM
71
A.D. Arkhangeil.,3,iiy'-~' 7.beOT-Y on the Origin of BawxiteB in the Light of'
Modern Science (6-1. Bushinskly) 83
Bibliography
91
Regularities in the I)istribution of Bauxite Deposits and Conditions
Under Which Th,:~y Werf: Forned (Y,--,K.Goretskiy) 93
Card 3/14

Mineralogy avrl O~ ieio of Bauxites SOV/1254
I. Regularities in the distribution of bauxite deposits 93
1. World baxi-xi. te- bearing areas and their zoning 91~
2. Gen-:~ral pxttt(~rns in th(, distribution of bauxite deposits
in the principal structural elements of the earth's cnist 99
II. Formation cc-niUt.ions of bauxite deposits 1108
Bibliography
118
The Geochemisti--
y of Altiminiun, Titanium, Iron, and Silica Under the
Effect Sulfate Weathering (in Connection with Bauxite Origin)
(M.N. Yakovleva) 120
Introduc'.Ion
I. Status of
.1 of' iniT-stigation
II. Methodolog-
1 P-1
124
III. The geochemistry of aluminum, titanilam, iron and silica
under sulfat~7-, weathering of base rocks in areas of pyritic
depostts 125
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Mineralogy and Origin of Bauxites SOTI/1254
1. Weathered crust 135
2. Ground waters in the sulfate weathering zone of base rocks 138
3. Surface waters 138
IV. Geochemistry of aluminum, titanium, iron, and silica in sulfate-
boggy weathering conditions 142
1. Alum-peat bog (weathered cnist) 142
2. Ground and surface waters 150
V. Review of observations 154
Conclusion 157
Bibliography 160
Conditions of Ba7xxite Formation (F.G. Pasova) 162
Bibliography 162
Genetic Types of Bauxites (G.I. Bushinskiy) 176
I. Genetic classification of bauxites 176
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Mineralogy and Origin of Bauxites SOV/1254
II. Solution, transfer and p1'ecipitation of bauxite componerlts
on the earth's surface 177
III. Laterites and laterite-bauxites 185
1. Laterites and laterite-bauxites of India 185
2. Laterites Pnd laterite-bauxites outside of India lq~.
3. Conclusions concerning laterites and laterite-bawKites 202
4. General characteristics of laterites and laterite-bFuirites 206
rV. Sedimentary bauxites
1. Arkansas bauxites
2. Jemaica and Haiti bauxites
3. Ural DevorLian bauxites
209
2CK)
213
220
Limestones, underlying bauxites, and the configuration of their roofs 222
Karst breccia and conglomergte 223
Red and gray bauxites
Some diagenetic and later alterations in bau:xites 236
Brief history of the development of concepts concerning the origin
of Devonian bauxites of the Urals 240
Patte.rn of the origin of the Devonian bauxites of the Urals 253
Card 6/ 14

Mineralogy and Origin of Bauxites SOV/12511
V. Indications in exploring bauxites 25'1
Bibliography 259
PART III. ORIGIN OF BAUXITE DFM03ITS
Geology and Origin of Bokson Bauxites in Eastern Sayan (H.3. Illina) 267
1. Geological cross section 267
2. Age of bauxite beds 270
3. Position of the deposits in the structure of Eastern Sayan 271
4. Tectonics of the'deposits 272
5. Appearance and composition of bauxites zT4
6. Morphology of bauxite beds LYT5
7. Manifestations of bauxite in the vicinity of the deposits 278
8. Origin of bauxites 279
Lithology, formation conditions, and patterns in the distributioll of
Bokson bauxites (P.V. Orlova) -,82
1. Lithological features of Upper Proterozoic and Cembrien deposits 282
2. Type of ores, their structure, and chemical and mineral compositions 287
3. Indications in the distribution of high grade ore 291
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Mineralogy and Origin of Bauxites S017/1254
4. Conditions of bauxite formation
Bibliography 505
Origin of Devonian B-au;xitc-o of the Salair Ridge (M.P. Nagorrkiy) 3(),--,
1. Underlying limestones 301;,
2. Origin of the pre-ore relief In limestones Yk
3. Morphology Fuid composition of the ore horizon 309
4. Trace elements in bauxites 311
5. Facies changes in the ore horizon 311
6. Signs of terrigenous weathering of the Devonian 313
7. Overlying limestones 313
8. Origin of Devonian bauxites 315
Bibliography
3.18
AnciezTt Weathered Laterite Crust of the North-Onega BmLKite Deposits
(K.N.'Trubina) 319
1. Ancient relief 319
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Mineralogy and Origin of Bauxites SOV/1254
2. Geological structure 321
3. Weathered crust of Proterozoic rocks 324
4. Weathered laterite crust of Upper Devonian beds 328
5. Weathering stages in basic extrusive rocks 330
Bauxite Deposits of the Podmoskovnyy Basin (K.N. Trubina) 335
Bibliography
346
Carpathian Bauxites and Their Origin (A.A. Denisevich) 3),17
South Ukrainian Bauxites and Their Origin (Yu. B. Bass) 351
Lover Cretaceous Bauxites of the Eastern Slope af tim Urals and
Their Origin (N.A. Karzhavin) 355
Bibliography
360
Regarding the Origin of Lower Cretaceous Bpmxite Deposits in the Urals
(B.P. Krotov) 361
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Mineralogy and Origin of Bauxites SOV/1254
1. Variegated clwjs 363
2. Bauxite clays 363
3. Clayey bauxites 363
4. "Be an- shaped." or "pisolithic" bauxite
5. Origin of the Sokolov bauxite deposits 373
Bibliography
Geology of the Sout4western Section of the Turgay Downwarp and Its
Possibilities in Bauxite Mining (Ye.P. Boytsova., B.M. Mikhaylova,
377
N.K, Ovechkin) 378
I. Stratigraphic outline 378
1. Upper Proterozoic and Carboniferous 378
2. Mesozoic weathered crust 379
5. Cretaceous deposits 381
4. Tertiar~r deposits 387
5. Quaternax7,, deposits 388
II. Formation conditions and general features of bauxites
Card 10/14

Mineralogy and Origin of Bauxites SOV/1254
III. Recommendations for future exploratory work 390
Conclusions 392
Bibliography 392
Kazakhstan Bauxites and Their Origin (A.N. Volkov) 393
I. Stratigraphic position and chaxacteristics of bauxite facies 393
1. Mugodzharj deposits 395
2. Upper-Tobol deposits 396
3. Kushmurun deposits 397
4. Amangelldy deposits 398
5. Akmol-insk deposits group Wo
11. Origin of Kazakhstan bauxites 402
1. Source of alumina 402
2. Character of adumina solutions and conditions of their
migration 404
3. Composition of solutions 405
4. Precipitation conditions 407
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Mineralogy and Origin of Bauxites SOV/1254
5. Diagenetic processes 410
Epigenetic Drocesses 412
7. Possibilities of anotherv non-chemical origin of
Kazakhstan bauxites 413
Bibliography
Gibbsite Deposits in the Amangelldy Biwxite Mining District of
414
Centrnl Kazakhstan (B.A. Tyurin) 4i6
1. Basic lineaments in the geological structure of the
Amangelldy bauyite mining district 417
2. Brief description of bauxite end refractory cla,-,- deposits 422
3. Origin of bauxites -4_~,8
Concl-asions
4
Bedling Cond-itions of Cenozoic Terrigenous Bairdtes of the Western
Slope of the Kazakhstan Uplands (N.A. Lisitsyna) 431
1. Existing concepts of bedding conditions in baLccite-bentring- rocks 431
Card. 12/14

Mineralogy and Origin of Bauxites
SOV/1254
2. Position of bauxite-bearing rock in the structure of the-,
Paleozoic basement 432
3. Bedding conditions of bauxite-bearing rock and the morphology
bauxite accumulating basins 439
Bibliography
439
Stratigraphic Position and Age of Bauxites in the Head Wftters of the
Ashi-Tasty-Turgay River in Kazakhstan (V.11. Rasumova) 44o
Bibliography
450
Variegated Sediments of the Salair Ridge (M.P. Nagorskiy) 451
Bibliography
453
Regarding the Stratigraphic Position and Origizi of the Yenisey
Ridge Bauxites (K.V. Bogolepov) 454
card 13/14

Kineralogy and Origin of Bauxites
Bibliography
SOVAP54
454
Data on the Bauxite -Be aring Possibilities of Yenisey Reg;ion
(Yu,A., Lavrushin slid Yk,.N. Shchukina) 4-6 2
Bibliography
4052
Mesozoic Bauxites of Central Asia (L.P. Konnov) 478
Resolution of the Conference on the Origin of Dmixites 483
AVAILABLE: Library of Congress
Cara 14/14 w/mas
3-15-59

GLADKOVSKIT, A.K.; MTYARRY, D.D.; SHRTGINA, X.Y.
Origin of Devonian bauxites in the Urals. Nauch. dokl. YyB. shkoly;
geol.-geog. nauki no.3:134-138 158. kHIRA 12:1)
l.Sverdlovskiy goruyy institut.
(Ural Mountains-Geology, S tratigraphic)
(Bauxites) (Petrology)

Y. A.K.
It2estones P n-1 11 ir. ni-oapnnting for
--,!dtna. Kit.--- .- !-!.I no.6:

GTADKDVSXIY, A.K.
Distribution of lower Cretaceous bau~dte deposito on the eastern slope
of the Urals and methods of prospecting for them. Trudy Gor.-geol.
inst. LTrAll SSSR no.40:165-173 159. (MIRA 13:11)
(Ural Mountains--Bauxite)

GIADKOVSKIY, A.K.; SH&ROVA, A.I.
Minerals fromed durini, the weathering of bauxites in the Southern
Ural Basin and their role in the geophemistry of bauxites. Izv.
vys. ucheb. 2aV.; g601. i razv. 3 n').7:130-134 J1 '60.
(MIRA 13:9)
1. Sverdlovskiy gorny7 institut.
(Southarn Ural Banin-Bauxites)

( GILMVSKIY, A.K.; GUTZIN, TO.S.
Formtion of the Ural Devoulan bauxites. Geol. rud. wastorozh.
no-5:107-112 S-0 160. (MMU 13: 10)
1. Gorno-geologicheskir institut Urallokogo fillala A21 SSSR,
Sverdlovsk.
(Ural Mountains--Bauxite)

...
GL&DKOVSKIY, A.K.; USIIATINSKIY, IS..
Composition, origin, and alteration of bauxites in Tikhvin
District. Trudy Gor.-geol.inst. UFMI SSSR no.56:109-135
161. (MET' 15:7)
(Tikhvin District-Bauxite)

W"OVSKIY, A.K.; SHAROVA, A.K.
Regularities in the composition and formation of bauxite deposits
in the Urals and the Turgay Plain. tt%Wy 43r.-geol.inst, UFAN SM
no.58:169-205 162. (KM 15:12)
(Ural Mountains-Bauxite) (Turgay Tableland-Muxite)

GI"OVSKIY A.K.
t~-
Metliodology of comT&Iing maps of the prospects Ond metallogeny of
Cretaceous bauxites in the trans-Ural region and the Turgay Plain.
Trudy ODr.-geol.inat. UFAW SSSR no.58:207-219 162. (MIRA 15tl2)
(Ural Mountain region-lkuxite-44apa)
(Turgay Tableland-Plauxite-Maps)

GLADKOVSKIY, A.K.; SHAROVA, A.K.
"Triassic" bauxites on the eastern slope of the Urals. Dokl.
AN SSSR 151 no.6:142C~-11,23 Ag, 163. (MIRA 16:10)
1. Institut geologit Uraltsko~:o filiala AN SSSR. Predstavleno
akademikom D.I.Shcherbakov=.

GLADKOVSKIY, A. K.; SHAROVA, A. K.
Bauxite potential of the Lower Mesozoic Bediment5 of the ea5tern
slope of the Northern Ural Mountains. Izv AN !%mr ~:er)- 29 no. 5:
67-75 My 164. (1-1 :..,. 1,/:-))
1. Institut geologii Ural'skogo filiala AN _SSSR, ~,.,!rdlovsk.

G[,ADKOV3KlY, A.;;.; RUDNOVA, N. fp,.
Jeat.:arinj, of Do-,ror.,.an bauxites in the Sou--riern !I-aas. Lit. i pol.
i5kop. nG.31131-139 !-.~-Je '6/- (IMIRA 17:11)
1. tmit~tut g7uolool~ ', '.'~ I iit~ij AN rjS3i'll.

GLADKOVSKIY, A.K.; USI;ATINSKIY, I.N.
Mineral corapooltion of the maln bauxite of' tix world; origin
and alteration of alumina m1nerals and bLuxitev. Trudy lnu~.geol. UFAN
SSSR no.6/,,:5-40 164. (XIRA 17112)
1' '3-
Pj-,ip-qrks on the book "Rauxltes, their nLiner-alo,7,y a,-I(I gerjet3iS.I Tbid. 2-
252

GLOKOVSKIY, A.N.; RUD."ICVA, M.Ta.
5tl-u,;'.urc, ar.(i :ompoo, I t ion of L'rjo wnicherl1re.. Z~)(,c ()," ~Uf*: ,,r t tfl
in the Southem Ural Rasin. Trutiy fnst.gnol. UFAN 5-"SR
'64. (,!~-PA 17:12)

GLADKOVSKIY, A.K.; SHAROVA, A.K.
Significance of the facies primary and secordary characteristics of
bauxites in forecasting. T~rudy Inst.geol. TJFAI%' SSSR no.6/-:167-176 '64.
(M-TRA 17:12)

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r, , ~!'r: r f tviii brU X ; te ~j ' ' ',, ', . ,V- f; ', '~ : - 1, -'.* 1". ~, ~ Cr..
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GLADKOVSKIY, A.K.~ SHAROVA, A.K.; KHRAMTSOV, V.N.
f
'barar
U -teristics of the Cor-position, orif'I.-I. and of
and Cenozoic teuxite deposits in the Asiatic part cf U.S.S-R.
Trudy rnst.r,,eol. UFAN SSSR n(,.64,1-,7-166 164. (v[ r"'I

GLADKOVSKIY, A. F.
Clinical characteristics of ornithosis. Trudy Len. iLs--.
epid. i mikrobiol. 25:192-200 '63. (KLRA 17.,l)
1. Iz Leningradskay infektsionnoy bollnitsy imeni Botlana,

TOKAREVICH, K.N.; VISHIIYAKOVA, L.A.;, YAXOVU,7, N.N.
Outbreak of ornithosis of an occupational naturO. Trud Lan.
'IT
inst. epid. I mikrobiol. 2151:185-191 163. (MIRA 17-1
1. Iz otdela onobo opasnykh infektaiy Leningradakogo insti-
tuta epidemiologii i mikrobiologii imeni Pastera i Lenin-
gradskoy infektsionnoy bollnitsy imeni S.P. BoLkina.

VISHNYAKOVA, L.A.; GLADKOVSKIYVA.P.
Duration of the preservation of complement-fixing aritt-
bodies following the recovery from ornithosiB. Trudy Len.
inst. epid. i mikrobiol. 25:219-221, '63.
(MIRA 17. 1)
1. Iz otdela osobo opasn7kh infektsir Laningradskogo inFti-
tuta epidemiologii i mikrobiologii imeni Pastera i Lenin-
gradskoy infektsionnoy bollnitsy imeni Botkina.

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VANSHGYDT, A.A.; I-ELINIKOVA, Yo.P.; a NPV,'~KJY, G-A.
Y'D
Preparation and properties of polyphenylene-t e
polymers. Part 2: Preparation of polyarylenemethyls
by polycondensation of aromatic hydrocarbons with their
bis-acetoxy and bis-chloropiethyl derivatives. Vyaokom.soed,
4 no.9:1303-1309 S '62. (IIERA 15:11)
1. Institut vysokomolekulyarnykh soyedineniy All SSSR.
(Hydrocarbons) (Polymers)

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S/C` a -50/01 2/009/01, 1
B01'~'~B056
AUTHORS: Af rosimov, V. 11. , SLLadkovskig, V G-Drdeyev. Yu. S.,
Kalinkevich, 1. F. , and-Fe-dore n H-t!
TITLE: Investigation of Atomic Flux Emitted by r-lasma
PERIODICAL: Zhurnal tekhnicheskoy fiziki, 1960, Vul. 30, 11:,. 12,
PP. 1456 - 1468
TEXT: The authors developed a method of measuring the flux -f uncharged
atoms having an energy of 300 ev to some thousand kev. The method is
based upon the recording of individual atoms after their ionization and
acceleration to 10-20 kev~ Fig.1 shows a scheme of this instrument, in
which the ionized particles are directed onto an Al-Mg target, where they
produced secondary ions which were measured by a scintillation counter.
For the calibration of the installation, a spef~ial device for mono-
chromatic ions and atoms was used. The calibration curves arc shown and
discussed in detail. Further, installations are descrited in detail,
which permit the time dependence of the atom flux, the energy dis%ribu..
tion, and the mass analysis of the atoms to be determined by an
Card 1/4

~~7;462
Investigation of Atomic Flux Emitted by S/Oc 60/0!0/0r~/OC)q/0-'1
Plasma BO!9XBO56
oscilloscope. The energy distribution -~f tht, ;J:~-ms o6 i~; vil;h Ihn
relation dJ/dE - J -+ (E,)/&0( E) pE, -t' 5econdarv
T'n- a,.~ nt v , -
ions, and ~O(E) the mean re~,ording ~f the at,
flux was determined from the relation
E
dJ/d9 - (1 ~S J (E)~tE, wbere'~' --,t3 Mice mean ~6. angle,
eff E _(E)dE/a0
and S eff the effective plasma surface, For :calculating the :::,.nc~ntra
tion of atoms per unit volume the formula
~2
n0 . 2~1iM ~ (dJ/dE)dEfi-E was used. By charging the -light irtens-Lty 1~,
E1
and the thickness of the gas target, it is p,:,ss1'D1e to 3~mpi--E- ,hz
sensitivity considerably. The leaat measuied denaitv )f' thwi f*]~.~x :~f
hydrogen atoms having an energy of 300 E-v in th- a,, i-~rcpi--
Card 21,1

Investigation of Atomic Flux Emitted by S A 5 7 /6 0//' 1 5 0/0 1 -/C C)q /0 11
Plasma B0191DOr6
10 2
velocity distribution was 1-10 a t /C"11.sec. There ar,~ 10 fiEures and
5 references: 4 Soviet and 1 US.
ASSOCIATION: Fiziko-tekhnicheskiy institut AN SSSR Lenin6-rad
(Institute of Physics and Technology AS USSR, Leningrad)
SUBMITTED: July 15, 1960
Card 3/4

M target. U M source of acceleration
photomultiplier. Hi 9 H and H
receiver. 3
voltage.
S/05 60/0)0/012/009/011
BOI,QYB056 -
Legend to F~g.'
nlasma 3-JU^'e. ell-
trance Slit of the in-
strument. K 1 capacitor
for the deflection of
charged particles. C ioni-
zation chamber.- 2 and 1 3
entrance and exit slits
of the ionization chamber.
and B tubes for the
lead-in of a gas and pres-
sure mea3ure-nent. K 2 ana-
lyzer. detector-en-
trance Slit. _', detector.
','-,.scintillator.
diffusion pumps.
Faraday auxiliary
rig.
vxLK Cxema npH(5oPa AAJI RCCACAOSHNIIA rIOTOXa 8TOMOD.

S10571601,._~ 16/~" -
BO 1 9/BO5 lt-
AUTHORS: Afro3imov, V.. V. Y u S.
-~trov, M_ P~ And
Kalinkevich, I. F.. Pt Fedor~,nrr , N. V.
TITLE: Investigation of a Flux ef Neutral At,~~ii. :. irlart,,.' 1:~s
Emitted by the Plasma of "Al I fall R,~sqar: h Tvi tii I lation
PERIODICAL: Zhurnal tektinicheskoy fizi.ki, !960~ V~-.I~
pp. 1469 -- 1484
TEXT: The authors used the devi,,e descr:b-~d iii t-llo issue
P. 1456 ff to investigate the atomio flux with prierg:.t..Ei cc 5co ev !~o
10 kev, emitted by the plasma of "Al,fal' The Deasur~niier.~-3 showed that
practically all atoms recorded are hydrogen at-om3 '11i-i qt,,antity of the
fast atoms grows with an increase of the capacitor volt,~.gr-, w-,th a de-
crease of the external magnetic field H Z' or with a of th~
hydrogen pressure in the chamber. In the ,.ourse of dischar~ge, the quan-
tity of fast atoms reaches a maximum, While the d15-hit7t;:l~ currerl ',n.-
creases to its first maximum. However, ther-~ is no
Card 1/4

Investigation of a Flux (if Neutral Atomic Part,,!- Ileg S/057/60/C,50/07. 010'
Emitted by the Plasma of "Al'fa'' Research BO';9/BO56
Installation
difference in the energy distributi.,n of atams -lurin-, '__acharge' A '~at!
gives data on the atomic flux. Analysis -.)f the dci~--L ~jln;wzf(! that Q.,-
fraction of atoms in the atomi-- flux generated bj i-,,fl ?,: ti Ai ~-f
from the wall, is small compared to the fraction _:,iminF Airect. 1'rofr,
plasma. It was further shown that, the en-~igy disti;bUt.icr, -,f atDmb _~nd
ions in the plasma .9pace are .,ery similar, and that, %tic err-rgy dis'~rlbu
tion cannot be approximated by Maxwell distribution The m-in energy of
hyd-rogen atoms reflected from a metal surface 1.s est-mated .n an appe-1-
dix. The authors thank B. P. Konatantinov for h~.Es advi7e and
discussion, D. M. Kaminker for his alntero?st, 0. 11 a-nd
Vz 1. Perell for taking part in disoussions, aa -1~ as Ye: G
A. Y. '31--olov, and V. A. Glukhikh for their assistan,. f-'ri rr.~-a~' urt-m,nts.
There are 11 figures, 1 table. and 8 ref~,rencr-s: , 5 :4nd __- TIS
~'urd 21il

Investigation of a Flux of Neutral Atomic S/057/50/030/012/010/011,
Particles Emitted by the Plasma of "Allfa" B019 B)56
Research Installation
ASSOCIATION: Fiziko-tekhnicheskiy institut A1, S551i (-rnstitllte of
Physics and Technology of the AS USSH). Nauchno-
issledovatellskiy institut, elektrofiziche:3koy apparatury
(Scientific Research institute of Keclr~.-jhys-'cal
Apparatus)
SUBMITTED; July 15, 196o
Card 3/4

?
5 xB, 360 OPCT. 1.9 10-13
10 xB, 3W 8PCT. 8.6 10-13
10 xn, 720 OPCT. 5.3 IG-13
15 P, it, MO &PCT. 5.0 10-13
15 pt 9, 360 qpcr. 3.5 10-13
15 xn, 720 BPCT. 4.4 10-13
S/057/60/030/012/010/011
B019/Bo56
C
K_
t
1.2 10"
5A 1011
3.3 1011
3.1 1011
2.2 1014
21.8 10:4
1.0 10-2
4.5 10-
2.S 10-
3.1 10-
2.3 10--
2.4 10-2
LI

4S0 3.0
530 13.5
*0 -'.5
67r) 9.4
030 7.0
530 7.2
Legend to Table 1 : 1 ) Experimental conditions, voltage at the di3charge
capacitors in kv, magnetic field in oe. 2a) Atoms per unit of sclid
angle. 2b) Density of atomic flux in isotropic velocity iistri,)'~:tion.
2c) Energy of atoms in joule3/cm2.
Card 4/4

ACCESSION NR: AT4025308 S/0000/63/000/000/0182/0192
AUTHORS: Afrosimov, V. V.1 Gladkovskiy, I. P.; Petrov, M.' P.
TITLE: Plasma diagnostics by means of fast neutral particles in
apparatus using a discharge in a strong magnetic field
SOURCE: Diagnostika plazmy* (Plasma diagnostics); sb. statey. MOB
cow,-Gosatomizdat, 1963, 182-192
TOPIC TAGS: plasma turbulence, plasma research, magnetic mirror,
ion mass analysis, nuclear stripping reaction, mass analysis, ioni_
zation, ionized plasma
ABSTRACT: In view of the large amount of information that can be
obtained from a study of the flux of fast neutral atomB emitted by
a plasma in toroidal-discharge installations in a strong magnetic
field, an atomic analyzer was employed for the analysis Of the flux
of fast atoms emitted by the plasma in the "Tokamak-2 (T-2)". appara-
Cam

FACC"ESSION NR: AT4025308
tus. The analyzer was described in detail earlier M. tekhn. fiz.
v. 30, No. 12, 1456, 1960). A fraction of the fast atoms entering
the instrument was converted into ions by stripping on nitrogen
molecules. These ions were analyzed by energy in an electric field
Iand then by mass in a magnetic field, after which they proceeded to
the detector. The instrument was calibrated with auxiliary appara-
tus described in detail in the same reference as the main apparatus.
The various precautions needed to ensure precision are discussed.
It was established that the plasma from the T-2 apparatus emits an
atom flux with energy of hundreds and thousands of electron volts.
A mass analysis of the secondary ions produced by stripping the ni-
trogen atoms has shown that about 99% of the ions are protons. The
only noticeable impurity was carbon-12. The main mechanism produc-
ing this flux of fast atoms is neutralization of the plasma ions via
charge exchange with the atoms entering the plasma. The conditions
for the occurrence of this flux are estimated. Preliminary measure-
ments of the spatial distribution of the atom flux over tbeivolume
Card

I
i ACCESSION NR: AT4025306
of the chamber was also carried out and it was established that the
fast-atom flux comes from all parts of the chamber. The energy dis-
tribution of the fast atoms indicates that the plasma ions have no
Maxwellian energy distribution, a feature characteristic of turbu-
lent plasma. Orig. art. hast 3 figures and 6 formulas.
ASSOCIATION: None
SUBMITTEM 190ct63
SUB CODE: ME
DATE ACQt 16Apr64
NR REF SOV: 003
ENCL: 02
OTHERt 002
Card 3/5

ACCESSION NR:AT4025308
a,
ev,
ENCLOSURE: 01
millioee.
51 ComparLson of t, Ime de-
.r pendence of' the hydrogen
alam Clux, discharge
current, and energy
supplied.
a hydrolren atom flux
(E 300 e'V), b - energy'
delivered to plasma
(1 - per Perticle within,
the plasma pinch, 2 -
per particle within the
chamber volume), c
discharge current
Card 4/5

ACCESSION NR: AT4025308
eV. -,o-
Card 5/5
keV
ENCLOSURE:- 02
Energy diatribution of the
hydrogen atoms it) the stream

8/057/63/033/002/011/023
B108/B!86
AUTHORSt Afrosimov, V. V., G'Aadkovskiy, 1. P., Kinlyakov, A. I., and
Petrov, M. P.
TITLE i A mass analysis of the current of neutral aton1c particles
ejected from the plasma in the "Alpha" machine
PERIODICALs Zhurnal tekhnioheakoy fiziki, Y. 33, no. 2, 1963, 205 - 211
TEXT: Fast neutral particles with energies of 500 - 5000 ev were mass-
analyzed by measuring the flight time of the particles as described in
ZhTF, , 30, 12, 1456v 1960. A magnetic mass analyzer wau used to avoid
difficulties in handling high-;energy particles. The hydrogen plasma in
the Alpha machine was found to be a source of a Inr,;e numbEr impurity
atoms. Since the impurity concentration varies with tlae and depends on
the working conditions of the machine in the same way as the hydrogen con-
centration it can be assumed that the impurity and hy..irogen atoms form in
similar processes (recharging, desorption of gases from chamber wall,
evaporation of wall material, etc.). The current of the impurity atoms in-
creases at the end of the discharge. This may lead to an increase in
impurity ion concentration of the plasma, and also to an increase of the
Card 1/2

S/057/63/033/002/011/023
A mass analysis of the current ... B108/Bi86
current of particles on which the impurity ions are recharged. There are
4 figures.
ASSOCIATIONs Fiziko-tekhnicheakiy institut im. A. F. laffe LN SSSR, Lenin-
grad (Physicotechnical Institute imeni A. F. ioffe As ussa,
Leningrad)
SUBMITTEXt February 2, 1962
Card 2/2

GLADKOVSKIY. P.S.
,
Tho PW-200-trpe steam turbina with a 200,000 Kv Plul.
telrh.-ekoyi. Inform. no.7:~6-19 ' 5" 9 - (VIIA 11:9)
(Stoam rurl)inpq)

GLADKOVSKIY, P.S., inzh.
The K-300-240 steam turbine manufactured by the Leningrad Nbtalworks.
Energamashinostroenie 8 no-3:1-3 lAr 162. (,'ff.RA 15:2)
(Leningrad-Steaxa turbines)

G~-Ua`,RLIDJ, G.: QLA.DKOVSKEY, T.,
~-Ilag---tm-ce conc--.-ete in rare!:-, of outer walls. r~-- 9-.roi. Ros.
3 no..',-:22-23 I'y 167. (Mix, 1r:9)
1. Ruk,voditell laboratorii stroitelInykh rqaterir-JOV Tiral'skogo
filiala AkAdemii syroitellstva i arkhitektury SSSF: (for
Gemmerling). 2. Nachaltnik tsentrallnoy sLrcitellnoy laboratorii
trcqta Mielyabmietallurgstroy (for Gladkovskiy)
(Concrete walls)

'J-:~_,ti/Engineering - Construction, 15 Jul 52
Materials, Testing
"Instrument for Determination of Calcium Chloride
in Cob Brick," T. K. Gladkovskiy, V. Ya. Savellyev,
Frwftneers Trust Tagilstroy