SCIENTIFIC ABSTRACT SILIN, YU.I. - SILINA, G.F.

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• Collection: Scientific Abstracts
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• Document Creation Date: November 2, 2016
• Document Release Date: August 23, 2000
• Sequence Number: 13
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

3 (5)
AUTHORS: Starik, 1. Ye., Corresponding Member SOV/20-126-1-39/62
AS USSR, Ravich, Y1. G., Krylov, A. Ya-f
Silin, Yu. I,.
TITLE: On the Absolute Ago of the Rocks of the East-Antarctic Platfo=
(0b absoly-utnom vozraste porod Vostochno-Artarkticheskoy plat-
formy)
PERIODICAL: Dol-lady Akademii nauk SSSR, 1959, V~pl 126, ?Tr 1, PP 144 - 146
(USSR)
ABSTRACT: In the prosent paper tac first determination results of the
rocks mentioned in the title, mainly of Precambrian age, are
discussed. For this purpose the collection of the Sovatska a
antarkticheskaya ekspeditsiya (Soviet Antarctic Expeditlon~
1956-58 was used. It was collected daring the prospecting cf a
coastal strip of almost 5000 km length (Refs 1,2). The invest-
igated region has the structure of a 3-stage plateau which is
in many a respect analoCous to the othe - Godvanskiye platformp
All three stages are characterized in short. No Mesozoic sedi-
ments have hitherto been found in the region of the mentioned
plat.eau..Conozoic sediments are only represented by covers of
Card 1/4 basic effusives among which leucite basalts predominate. The

On the Absolute Age of the Rocks of the East-Antarctic SOV/2G-126-1-39/62
Platform
first 40 determinations of the absolute age by means of the
argon method made more precise ideas possible concerning the
structure of the aforesaid plateau. Several results were suxr-
prising and their geological interpretation meets with sariolis
difficulties (Table 1). The highest age,- i. e. 1020-1270 ril-
lion years were obtained at first for the oases Langeneset,
Grirson, Banger, and Obruchev, i. e. for leucocratic granites
and peL-;matites. The a-e of the weakly migmatitic (Barger oasis
andother regions of the crystalline basement) rocks fluctuates
between 940 and 1050 million years. So-called poly-migmatites
which are 700-730 million years old occur at the same time at
several places, especially in the Banger oasis. Thus two =igma-
titization staCes can be separated: a) an earlier one which
occurred more than 1000 million years ago, and b) a late one
- core than 700 million years ago. Thus the nigmatitization of
the oldest masses of the eastern Antarctic belongs to the Pro-
terozoic. A paccrket of Lrnelsses in the region of the Einsvort
bay and the Villac-i elevation is for the time being the only
exception. Weakly migmatitized biotite-gneisses are here 425-
Card 2/4 485 million years old. This agrees almost with the age of the

Cn the Absolute Age of the Rocks of the East-Antarctic SCV/20-126-1-39/62
Platform
here occurring porphyroblastic Granites. The age of the S-zeen
schiat3 and mica phyllites (piddle stage of the plateau) flue-
tuatea between 400 and 500 million years. This corresponds to
Sinisian and Lower Cambriar. The Rapakivi granites in the ex-
trome east of the irvestigated region has approximately the
same age. The cost recent granitoide are the subalkaline bio-
tite-hornblande varieties. They are Caledonian, with an age of
305-315 million yea::,3. The age of the gabbro-dolerite from a
stratiform intrusion within the Bikon (Beakon) aeries (170
million years old) agrees rather well with the geological po-
sition (Lower Triassic). The same holds in the case of Terti-
ary loucite-granite (nountain Gauss) which is approximately
20 million years old. The age determinations of the mentioned
rocks confirm on the whole the authors' assumption concerning
the 3-stage structure of the plateau. The old Gerling constant
Ak - 6.02*10- 11 year-1 which is much used in the USSR was used
for the determination. The data are only temporary and pr,-.babl;r
Card 3/4

On the Absolute Age of the Rocks of the Sas4- Antarctic SOV/20-1 26-1 -ItO/62
Platform
somewhat too low. There are 1 table and 3 Soviet references.
ASSOCIATION: Radiyevyy institut !m. V. G. Khlopina Akademii na-1-k SSSR
(Radium Institute Imeni. V. G. Khlopin of the Academy ef
Sciences, USSR). Hauchno-issledovateliskiy institut on-ologii
Arktiki (Scientific Research Institute of the Geology of the
Antarctic)
SUBMITTED: January #q, 195),
Card 4/4

ATRLAWOK, L. Ya.; AVD7.EYKO, G.V.-, KRYLOV, A. Ya.; SILIN, Yu. I.
Absolute age of the Mcnastyri type granites of Kalbot. Gookhimiia
no.3:278-279 160. (KIRA 14:5)
1. Radiyevyy institut Imeni V. 0. Khlopina AN SSSR, laningrad.
(Ka.1ba Range-Granite)
(Geological time)

KRYLOV, A.Ya.. SILIN. Yu.1-
......-
Using the argon method for determining the age of clastic
aedimentar~v rocks. Izv.AN SSSR.Ser.geol. 25 no.1:56-66 Ja
,6o. 041RA 13:8)
1. itallyevyy institut Iment Y.G.4lopina AN SSEM. loningrad.
(A-gon) (Rocks, Sedimentary)

STARIK. J.ye.; HAVIcH, M.G.; KRYWT. A.Ya.:--SILIN. Yuj.; ATRASHNJOK, L.Ya.;
LOVTSYUS, A.Y.
Recent data on the absolute age of rocks in eastern Antarctica. Dokl.
AN SSSR 134 no.6:1421-1423 0 160. (MMA 13:10)
1. Radiyevyy institut im. V.G.Mopina Akademii nauh SSSR. 2. Chlen-
korrespondent All SSSR (for Starik).
(Antarctic regions-Rocks) (Geological time)

e,i-,YLC-'V ~A.Ya.-. UjM;Yll, A.P.; 'ILIN, Yu.I. L6ili
0 ns,, J. I. I
Sig-nificance of the argon - potagsium ratio In oceard-c si-1t. Izv.
All ~'66R.Ser.geol. no-3:87--100 Mr 161. (KIRA 15:2)
1 . luidiyevyy inutitut AN !;~R, Lealngrad I Institut c keanologii
All S~jjh, 14oskva.
(Ocean bottom.-Deap-sea deposits)
(Geological time)

STARIK, I.Yo.; KRYLOV, A.Ya.; SILIN, Yu.I.
Ab3olute age of base rocks in the eaotern part of the Ruejian
Platform. Blul.Kom.po opr.abs.vozr.geol.form. no.4:6,-65 161.
(MMA 15:1)
(Russian Platform-Rocks, Crystalline and metamorpiic)
(Geological time)

'rZ',YLCV. A T!)~; VOIHIVJ-'~U, P-O)~; J~Rj'. Yu I
1 .0
Absolutc age of tha .-rystallinc- basement of eastern Antarctica.
Dok]. AIN SSSR 143 no.l.-184-lE7 I-Ir 162. (NIRA 15:2)
1. Radiyevyy Institut in. V.G.alopina AN SSSR. Pr-3datavleno
akadeaikom D.I.Shc~erbakovymo
(Antarctic regions--Geology, Stratigmphic)

RAVICHP M. G.; KRYLOV, A. Ya.; SOLOV'TEV, D. S.; SILIN, Yu. I.
Absoluts age of rocks of the central part of the mountains In
Queen Maud Land (eastern Antartica). DAL AN SSSR 147 no.62
W3-1436 D 162. (MIRA 16:1)
1. Nauchno-looledovatellskiy institut, goologii Arktiki, L
Radiyevy3r institut in. V. G. Xhlopina AN SSSR. Predstavleno
akademikom D. I. Shcherbakovym.
(Queen Maud Land-Petrolory)

AVRASHOV, A.S.; KRYLOV, A.Ya.; SILIN, )(u.I.
1-
- " A, New data an the age of granitoid Intrusives in the central
1 1,-
!I- I Pamirs. Dokl. AN SSSR 153 no.5tll36-1139 D 163.
1-i -p (MIRA 17:1)
1. Predstavleno akademikom D.I. Shcherbakovym.

GRICH. A.; SOBILIMAN, I.M. Ctranslatorl;_AILIX, Tu*S.,,redaktor;
IZVONMXAYA, L.G., tekhaichookly radaktor
Clkplanatory index to a short guide to Leningrad) Leningrad;
ukazatell k kratkomu putayoditeliu po gorodu Laningradu.
[Leningrad] Lenisdat, 1956. 34 p. [Parallel text@ in Russian and
Raglishl [Phototatat) (NLRA 9:9)
(Leningrad--Directories)

JAXCESSIO-111 1111: AP11020334. S/0089/64/016/003/0252/0253
AU11"HORS: Karamyan, A.S. (Deceased); Kuzeyev, B.I.; Kress, R.P.;
Yu,,-S.; Stukov, G.M.; Shchebolev, V.T.;
a., I.A.
TITLE: Absolute determination of a number of neutrons emitted by
source, using the associated particle method
SOL-RCE: Atomnaya enerZiya, v. 16, no. 3, 1964, 252-253
TOPIC TAGS: absolute determination, absolute neutron determination,
azzoelated particle method, alpha particle, emitted neutron, gra-
p'lit.e, neutron determination
,'-`!STRACT: The method of associated particles is based on a com-
par'llson of neutron flux from the source being studied with neutron
f1u:-c from the reaction T(d n) He4. Since onea-particle corres-
pondo -%o each out~;oing neutron in this reaction, it is possible to
deter.mine the number of emitted neutrons by the absolute counting
ofoc-particles. In a medium for which the moderation length in
Cord 1/3

ACCESSION N-R; AP4020334
1,~ss th;~-n the diffusion length, it is possible to find such spacing
of thermal neutrons from source to detector where the density of
the---aal neutrons does not depend on the energy of neutrons emitted
by the source and is determined only by its intensity. Graphite In
the form of a sphere with a 4 m. diameter was used as such a medium.
T-nree curves for 3 different sources are given in the figure in the
Laclo-sure. The point of intersection of curves determines the
radius of the efficiency constant for a given device. This dis-
tance is 82 cm. To find the number of neutrons being emitted by
va,:~ious zouz-ces, it is not necessary to measure the full curves of
%*Ih~~r,zal neutoron distribution in the graphite globe. It Is suffi-
cient to determine the number of detector readings in the spacing
of the constant. Mean square error of method in about
� 1.4,1.". art. has: 2 figures.
A'SOCIATION: None
SUE:U~:TZD: 18Apr63 DATE ACQ: 3lMar64 ENCL: 0 1
11 COD-7; PH NO REP SOV: 001 OTHM: 002
ZUB
C.,d 2 / 3

ACCESSM,11 11R: AP4020334 JO
7-
Zk
+

ZI N 1

1 X

ENCLOSVREt 01
9 20 40 60 60 W 129 99 142 W AV UN
Fig. I
Space distribution curves for thermal neutrons in graphite sphere:
1--for neutrons of Ila-Be source;
2 - for neutrons of Po-Be source; 4
3 - for neutrons obtained from T d, n)He reaction
Card 3/3

;, ~. -". ~ I ~. , -Iii, ~V-11-1
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:. .; 1.A.
I
-~.' sv.~rceO. Atom. energ.
' --j A:-,.2. I Pil - A g I ~ I, . (PIRA 18:9)

Dr. Geolo,,:ical & 11-diieralogical Sci. I-Ibr., Lab. Hydrogeolog-ical Problems im. F. 3.
3avarenskiy, Dept. GeoloZico-Creoo,. Sci., Acad. 3ci., -19L~5-48-.
Q
IlConcerning the Problem of the Formation of Salt Water in BachkLria,g Dok. AN, 52,
14o. 1, 1946;
"The Effect of Kinematic Density, Reduced Pressure and Pormeability of Rocks on the
Speed of Filtration of Brine in the Oil Bearinc Strata of the Ural-Volga Oblast,"
ibid.s 58, iio. 6, 1947;
1IFornation of Subsurface Waters in Eastern Oil Regions" (bk) 1948.

1. --,- 1.
2. vs,;q (6oo)
4. Idater, 11nderground - 113econd Baku"
Ii7. Hydrogeological conditions and the flood potential of the principal oil
fields or the "Second Baku." kAbstract.) Izv.Glav.upr.geol.fon no. 3, lA7
9. Monthly List of Russian Accessions, Library of Congress, March 1953, Unclassified.

F. P.
MIC109").--ch"T Scol. shoming hem
fr"h (river) watersve changed in comian (metanvartolity"41b
Irv the "Hoe highlY Mineaftfifff! Water% Of InIM reach IWWA
Own the level of rich rorks Is tWwd. Iliad 4 the paper
(14MAIS With the (OrMAtiflel and -IfItniCtilarl Of PWACUM 4W
gwnift under well-trc"Miml peni. crooditi.,n4. Thu-.
tw1rokurn 4bwsbrd bar rock% is gradually disptAml lev
wAter. t"C" .1w" the few& f.W" are as UnAll A* thow ..(
dAyi Thera, Is a rebliom between the Orgree ,I nirtA-
nearphiint of the 4nhteffAnrAn water And the rAtV 44 AC-
u4iloorsofthrpraralollsetrolman. V. 11. Gotischislia
=

3igned by:
ldr),
'2 lor or'K0

STI T11-BEYCITRPI, A. T.
Water, Underground
Method of approximate piezometer computation of velocities of filtration and underground
flow or brines. Trucly. Lab. gidrogeol. probl. No. 2, 1949
!!onthly List of Russian Accessions, Library of Congress, December 1952 UNCLASSIFIED

v " I - - --- - - - . -,-7r7F-- - --
'~' 3 A- ~ 1 , 1. .. . p - ..' - -- ~:' ~- I . .. : . , " 1 1 ~' ~ , - . I .
,4*atur,
lroblem.s in the fcrmatLon cC ~-rcunj waterB ba::,es on rzterials frcn. the trarlsacticns of the
Laboratory of liyd-.cj,,eclc -ical Frcblems, Vol. 1. Trudy Lab. gidrcgeol.prob2.. '.,'o. 2, 1949.
"onthl List of Russian Accessions, Librarv of Icngress, December lgt2. Unclas-sified.
Y
- 1~ I

I . STLIN-BEICHRIN, A.T.
?. USSR (600)
It. Geolopy and Georraphy
7. Special Ilydrogeology. A.T. Sili-Fekchurin. (Moscow, State Geolrpical Press, 1951).
1~
iu--viewed by M. Ye. Al'tovskiy. Sov. KniEa, lo. 6, 1952.
9. 40 Report U-30P1, 16 im . 1953, Unclassified.

C,,rfC)R

SILIN-BIKCHURIK, A.I.
--.- I . - 1 1.
Hydrochemical sonality of the underground water of the syncliniss near the
Caspian. Isvest. Akad. *auk S.S.S.R., Ser. Geol. '52, 27-40.
(CA 47 no.22sl2706 '53)

BOGONOWV, Gerasim Vasil 'yevIch;,_�ILIN-BKCHURI-N'Aleksay Iyanovich;
GOKANIKO. K.1.. redaktor; redaktor-, GbiCIVA, O.A.,
taktiatchmakly redaktor.
[Special hydrogeology) Spetsiallnela gidrogeologiia. Moskva,
Goo. nauchno-tekhn. lzd-v,o lit-ry po geologil i okhrane nedr,
1955. 246 p. (KIRA 9:5)
(Geology) (Water, Underground) Iw

SKMOV, S. I.CtrFinslator); SILIX-RUINMIN Ao I.,. redaktor; SYN. Ta.M., . - -
redAktor; SHAPOVAL 0 0 .. -e-WrI1116111eimly redaktor.
(Arid zone hydrology; a collection of articles. Translated from tho
Inglishl Gidrogeologiia i gidrologiis ariduci zony sommago shars;
sbornik statei. Pereved s anglilskogo S.I.Sairnowa. Pod red. i a
predial. A.I.Silina-Bokchurina. Moskva, lzd-v* inostrannoi lit-ry,
1955. 372 p. (KM 9:4)
(Arid regions) (Water supply)

SILIN-BUGHLIIUN, JL.I.
- ---- -
Formation of the chemical composition of ground waters In arid
regions. Biul.MOIP.Otd-Cool. 30 no-1:91-93 JA-F 155.(KLRk 8:5)
(Vater, Underground)

15-b7-10-14631
Translation from: Referativnyy zhurnal, Geoiogiyu, 19b?, Nr 10,
p 211 (USSR)
AUTHOR: Silin-Pekchurin, A. I.
TITLE: Chemical Composition of Ground Waters in Arid Regions
(K vonrosu formirovaniya khimicaeskogo sostava grun-
tovykh vod v arldnykh oblastyakh)
PERIODICAL: Uch. zap. ',',Tosk. un-t, 1956, Nr 176, pp 175-193
ABSTRACT: Experiments were conducted to study chemical composition
of ground waters in arid regions: 1) on successive
leacUng of salt-impregnated loams; 2) on the misci-
bility of some types of ground waters. For the first
series of experiments loams from different depths of
the Caspian plain viere tested. The author describes
four experiments on successive leaching of salt-
impregnated loams. On the basis of these experiments
he has established a transition from sodium sulfate to
Card 1/2 magnesium chloride and then to cblclum chloride

Chemical Composition of Ground Waters (Cont.)
15-b'1-10-14631
solutions. On repeated leaching. of the same samples, he
established that the exchange occurred in reverse order. In
the first instance, suits accumulate in the solutions after
the latter have filtered through the lo-ms; in tLe second
instance, each new solution washes the salts out of these same
samples and gradually lowers their salt content. The second
series of experiments is concerned with how certain types of
ground waters blend, and pEarticulurly how sodium bicarbonate
waters, such as are usually found in deposits of salts, blend
with calcium chloride solutions. The experiments show that a
change takes place In the chemical composition of solutions
formed by infiltration of rain or fluvial waters through salt-
impregnated ground, when these waters blend with waters of low
mineral content. Thus, magnesium chloride solutions may
result from a blending of calcium chloride solutions with
alkaline waters, while alkaline solutions with an admixture of
chlorides and sulfates originate from sodium sulfate solutions.
Tables of data derived from the experimerts, are included.
Card 2/2 N. G. Borvinok

f
Lvws of the Fol'matiC!-4- Of UljerL;17cuT:d Water i-I Arid Zones of
Lccturez in Y~56, Vest. U., Pjj,rSiCO :.Jat~j ond Talu-"aj
-DP C--'cllog:,- -vocUltY
I'I'onslctioll U-%,054,3(l,

SILIN-RIINC : BOGORODITSKIY, K.F.
-
Influence of water on the underground gaelficAtion of coals. Dokl*
AN SSSR. 109 no,41832-833 Ag 1956* (MA 9:10)
1. Lotborntortya gidrogeoloeicheik ikh problem Imeni F,P. Savareaskago
Aksidemii nnuk SSSR. Predstjtvleno akstdomikom II.N. Strakho"me
(Coal ga"iftention.,Underground)

Popov
Palms I DOM OWLOITAMCE
remi"t pe sembesil 1 penstall.
feeley 4-his4ow es, a Gemerva'sur @*"*I"* mimmamewfilew pea."malobw a
fvan-b"p *arsse. a."Awwrommaws "Oe"I"Min oweeklar SIAMISNU
(Abetroate at Repo owindt"d to t" ut& comeorat alemooly t ime,
Was of 0004"r Old Goo"lles. as istwmtlaml Aooq~
"tatice, of 2.1seting rit"Inow) momew. 1937. M V. /Parsual ummin
IA met"Go -4 MWU-b - "soeb/ 1'"O, evoice psoud.
go -wUQ Mostriwtov, mooum"
FUNIMS 2US ba-blet I@ w4newa for wareloopte" led 41.11 mgme-M.
COWWAM TMe tallottlem at Astrefte sumn weverld, Pften" 84 as UI&
00"ral Moomaly of as laterwUMM UM~B or QN&M maj ggoovelft M
k7amlogical, emnional, -4 62-1014oft, Pensions. fteum "WAG be
P~*Iwmn at unfierarvand waterm. Mor, ona rl"M an &I"
Us GMU-40 - in Poostem. witil migumb lop rpm* livemploumme. fteem qWmap.
114 Le 204ugh an ante"" IV a "Raw ap%orid,, uaga is r"mms to
Tbere am w allow sives.
of loareerigoom was is Nagesm."We
Cbwl%o-, N.V. cm Ibety, impopmom Is slalom"
16* WWt4Wwt" CoSediF ad sopgr"S or M&WWommel M&W TI
A"re, GA. 41molougleal Somsee in as gss
O%IM&WDUON. 0-19. Roal"L prepwum at 0 map, a~ k
malm"elf Pr- 616.09% ad own twablame in SmasloodmLow is so sw
ftooldy. PA. lamli pool. 1. deandle WAG& so an won at
?Memmoww oftomme IV Mmew fulalual, 0
Alme". I.L. Pft%l~ to the NOW at Opeftem PMMM me Ift
Torriteor of me qssm
MWILINIA, UW-W
owe 4A

-j - j ": i.C I I
"I . 0 C% "%so
~11' - iw_ IIJMJIV- rpolop-ninernlOgicheakit,'i nAmle. r f r.
lirainage Of YORcow 3nsin lismite devosits beine P*siftod. :Jodxom.
JrAZ.ul:l. ne,.;>.65-67 '57. NLRA in:,7)
I
. Laborfttorlyn glirogeologichaskikh problem ~kndemij mmk SjS'.q.
(Poncow Basin--Lignit~) (Mine drainVa)

SILI14jKCW,=.,Alsk"y Ivanovich; SHILOVA. K.A.. red.; TXRK&KOVA, H.S.,
tel&n. redo
[Dymmics of under 9'round'vaterl Dinsmilm podzenzykh Yod. C*skval
lzd-vo Nomk, univ., 1958. 257 p, (KIPA 11:9)
(Water, Undergrowid)

TtTL9, The 3..t1.. eekletya)
PUZODICALt Syullot.n- lookovokoga abotichestwe Isplistaloy prirody.
Otaol 8-16810.skly. 1958, Ir 5. go 151 - 153 (USSR)
ANSTIACTo ?%~ fiydroq..I.xt..I r the 3-1.ty. O.K.
L-6#:: SO-r-tory - 11.7. Lobeftovs) board the following re-
po 'I On 10 April 1959. by L.S. WMIz_-r. -1..* Q.0stion
of Risroshostost of 'Upp-a-T-7#7616a Deposits $a the
S."th arst Ismigh" and *T%s Rare%* later* of the Trans-
tq4& 9~06ftolo %I Th* pstoo.#
to k sort In the 49.04001... s &.A. At.ttia, A.f. T.ko.ka*%.
97 N.'ritably. S.W. vlktorov, I.?. Lobsnave. K.&. glass.
fontove end O.N. Lan" . On I? April 1951. br
Trasive Surfaces of moustatme. the 31"a.ure of fountalfte
..d Ryd'.6-101Y., and by I.$. Resorts 'The 0 ... orph.lea
..4 the Ryd,og..I.ct. way'. Thi foll..I,g per@.*$ Seek
part 1. these dissensions, M. Skalo~. 0.1. musitroshko.
N.A. Tovicrovskays. A.A. losaplyantsev, A.S. Dulall'yer,
I.T. n later. A.4. Droiskly. V.I. moyeas. On may 15. IY
Cord 1/5 1,V. FA at.. 'Th. Best* 1.10. of %be RY61 "hooleal C.Drost-
bterranoen Voters of Os Alter, and eome Coast-
1 1. " 1 0 Proble. of Their Conselso. and by L.M.
c.d..%k a 15ndfaverlig and Coolarival Cheresteriettes
.M.A. a the Lim-its gotten-. The following persona,
tooli part In the discussions, to.s. T.Tt.o.s. V.I. Popov.
A, .4. 7.19dom..., N.Y. L*tm*,&. To. V. 1kkhI.. U.S. Sak.1-
we& O.C. L--g-. 00 "Y 22 , b a T To a. 'The Goanthe.
mistry of Par* so.. .10
of the Caspian sea.. and by ckj&_jroI-.
of For Solutleam of Carboniferous Deposits of the Reason
01.1d0$!.. ?ho following per"No took part to the 410610.
*least I.#. Popme. A.4. Gowryukht". G.L. 31admikov. W.f.
Dollsbarso Ch. To. Krolp, A.C. 209140sove md 0.1, l4LB".
00 Nor It 1950. the reports more, 0~40 1.1 Aj,.jjjAN,-jIkLvm.
r"Moss, at Irdrogwelow to m_64-
Carl 1/5 6a4 by A-1,3"UNWO *11tv, larval" goUst of
I%* 18"Ov Obloss'"). of follselme peresso took part Is
AM disessale"I To.M. 8*%tM. A.0. Z6916406911. N.&. V"i-
ors,ok"s, a.m. lobtl1yer. 0.K. Laods, md &.I. Sills-vok-
*barim,

A UT 110R: Silin-Bekahurin, A.I. SOW/5- 59-5-19/20
y in 'orth Africa and Hindustan
'TTLE: Some Problems of Hydrogeolog
(Nekotoryye voprosy pidrogeologii Severnoy Afriki i Indo-
stana)
PERIODICAL! Byulleten, Itloskovskogo obshchestva ispytateley prirody,
Otdel geologicheskiy, 1958, Nr 5, P 159 (USSR)
ABSTRACT: The author sums up the report he read on 29 May, 1958 in
the Hydrogeological Section of the Society. The author,
as a scholarship student of UNESC) visited North Africa
and Hindustan and studied the problem of hydrogeology in
arid countries.
Card 1/1

- :7 _'r11 fr I
1 1-1L i~'

AUTHORt A. cov/',7-58-6-14/16
TITLE: .1 ronf~x-an.;a on Goo.-hfamical and
F. ad i* ~-f saa;~"h ?~~-)&Ps_-tlng for
le.r.: a_-.a N tv;,L'_i al Ga!? D spoi-I L 3(Khrorika - Vaesoyuznoye

r-iiftyanyk-', J, gazo-?-jvkh meatorozhdanii) I
PERIODICAL% 1953, Nz ~, pp 6~O - 61.1. (USSR)
ABSTRACT% Th-es. :.orf:?ren-.9 tr,,,)k plaois im Moscow from April 21 to April
-Y.-. G-**ek~rj.ka '-f) the As USSR.
a w7ow:ip-:~. of 41
g a. z 2.,. ve,)~a rapvecented by about 240 msabers of
tha AS VSSR~ i-,,s branches, the Academies cf the Republics
of tht Uni..,n, of a r_,zm1:3r of high sphools, of single instit-
.;.2.-es, pxd icxzlicx-tion. of the Ministeratyo
geolzgi 'J' rkh-ret.7,y :radr (Min-_'.9t::y of Gsolvcgy and Protection
Cf #at--xx.-P5 11 f; 1i G'j:.: -;as) ', vf Gcqpler. SSSR and RSFSR, of
":.Ytuihu*tskhn_'jhe&kiy komitet Soveta
Vj.nj.i1;rc-q- SSSE (S-.ata 9c~.nn~rific an~~ Tenhnical Committee
of ae .~.f W__'-L-.~Steza of fhq ussp.)~ 0~' Councils of
Hst:~.onall Z_-~)n=Zr "-,I otho-i- ~xgsnizations. other active
Card 1/4 parLj.;.4.pan~,s Y~ire frcm the German Democratic

Chronic-' a - A! I G Er-~! SOV 17-1;t3-.6-14/16
Radiometric Method. St~,-.,7ch 5,r-2
F i n e r al 0 1' 1 a n d Fi D " e.
Pl.;-xFknia and Yugoslavia.
D. T. A.-taiemy -,f Sc-lences USSR,
geclogo-
r.,irk (D,-~-pax%menf: rf Gq~:graphi-zal Sciences)
-,he. 2ro main wexe given. 65
r7.ad 7 r,:zs!g:i or-ien".ists contributed with
tf r-a t i 0 miy `~q divided into 3
U reports);
i'!uj.;mrrTt for the search and
--.nii gas deposits (7
c -.r of the methods and
s ~~n -i3az-l ani prosy.93ting of
ge.7 doapogitS (7 reports).
As A_ of chemical elements,
V. A. ~h.- 9,Jr-ntlfi~ baaeu of geoohemical
S. 1. deals in hie report
Vi "11 j34 -:a4 ti-ig m,
_L a~ prTdr.%-; n thod s -F. A. Alekseyev
dls,~as,4ed. 'Ah-i se-.-*%em'~-' fir; 1.-mjis of -;hg zadi'cmetric prospect-
Card 2/4 iag zet,-'6d (rsAu~~a'! gamma field.). A. I. Silin-

Chronicle - Ill Uni-on Oor.~qran~;e on Geochemical ind SOV./7-58-6- 14116
Radiometric Methods of Searob and Prospecting fo--
and Natural Gav Deposito.
Bekeburi.n Rpoke about the movemen-, of deep subterran-
waf-irs. L. B. Ronov reported on investigation
results dealing with the distribu%ion of organic carbon
in the sedimentary rooks of the Russian Plal.form. Methods
and.techzUque were the subject of the following reportes
G. A. Mogjl*V8kjY - The present ~zage .-3f the problem of
anomaly of gas bacteria and a suitable method for its
aolut~or-; Tq. A. Bara hYdr,)rheni,.,aI investigations
in proopel-ting f) -11 , ..
ind natural ga.91 V. A. Kovda
and P. S. Slavin - so.1 geochemical features for the yield
of nd natural gas to be expected;
V, V. Fi~>rowskaya - a lum-iniv--enze-.bituminol-ogical matbod
for the inreotigatton and prospscling of natural gas and
Isposits; V. A. Sokojov - gasanalytical
wAthod and equipment and ways to v.omplate them; and others,
The u49 if g9ochemical.methods in various regions of the
USSR was alao treated: Timano-PaLh9rakaya gazoneftenoanaya
provintsiya (A. N., Krams, G. G. Grigor~yev, A. S. Madvedev),
Card 3/4 Sarat,,--aKuye Forolzh'ye (Ye. M., Geller), Stavropol"ye

Chronicle - All Union on Gt.trihomi-cal &wl SOV/7-58-6-14/16
Radiometric Methodu of S.?Ar~b tir.4 PTO$p6rting ffiz
-nd Natuxal Gaa I
(V., N. Tf.,).rtA4!lvhtfyn), Ula Fon~.nmula (.I# A, Peterall's)
arvi )thi:~-a
Card 4/4

T 7
AUTHOR: Sol-olov, V. A., Profeosor 30-58-7-36/49
TITLE: Go o c he -.1 i,,;al zmd Radiometric-al Methods of Search and Prospecting
.ror De,;ooits (Gookhimicheskiye i r..-diovetricheskiye metody
I A .1
;)oislkov i r~tzvedki ieztorozhdcniy) Transactions of the Confevence
in Vu Denart~.ient of GeoloGical and GeoOraphical Sciences
(Soveshchaniye v otdelenii. jeologo-jeogr:~ficheskikh nauk)
LI
PERIONCAL: Vc-.-~tnik Akademii nauk SSSR, 1958, lir 7, PP- 125 - 126 (USSR)
A-STRACT: Thio confererce took :)lace ;,,ril 21st to April 26th
A& . Apart
from. the :-c.-.ibers of tite and -cientific branch research
inL;titi;tc-3 re'J."et: ell t,-. t ives of the i3e,-loCical renearch institutes,
of the econo-dc councils of the Gosplan, of the State Committee
of New TechnoloJy (Gonud%rstvennyy k,-;ritet po novoy tekhnike)t
of the '.11inio-try of Geoloey and Protection of Mineral Resources
(Llinicteratvo ..-eologii i ol-hrany nedr) participated as well as
ociuntizts from th, countries of the people's democracies. The
Me7-.'er, Ac,,.!c:--.y of Sciences, USSR, D.I.Shcherti-kov opened the
CQ:-kfcre.;ce. Ful"ther reports viere ,!rlivcred by: 1) A.A.Saukov,
of the AS USSR inve[-;ti~;--ited -eoche.-.iical
C%rd 1/4 2cth,~).Ia. 2)V.A.Sokolov an-ilysed the sciontific

7-tr.l I. of Search ard 30-58-7-36149
.'r-.::s~-,ctions of the Conference in the De7-Z.rt--ent
of GeoloL-,-ictl and Sciences
fou,-cl-,tions of -coc-.emical ;~ros,~ectir:(,:- methods and of the
,r--n:octin- for ac.3 and mineral ails.
7' S-I,Kuz-ietsov opoke about nicrobiclo--ical prospecting nethods
of Ie;ojits of minpral oil and
4) F..A`%,A1e':seyev re,~orted on the rardiometrical prosPecting methods
a If dekov~ts of min,-,ral oil and --as.
5) A.I.Silin-DekchUrin --,po:~e --,bout the movements of deep ground
vi a
6) "I.B,11onov -Am--t Or~~nic cclrbon in sedimentary rocks of the
Ruosi~.-n Plain"(Russkaya platfor..-.a)
7) G.A-'Io,~ilevsI-iy oo444,aetPThe presqnt state of the problem
concernirZC, the bacteriolo--ical anowilies of gas.
8) YL,. A-.Baru r4~+~ted on"kerult3'o"f"'hydroche.-iical research work
obtained in the course of ijrospectir,~; for mineral oil.
9) V.A.Kovda and P.S.Slavin reported--sn"~eochenical soil data
concerninL; tl-~c miner-~Toil and ~as content."
11)V.N.Florovokaya ~~ ~.,~Vlhe luminescence method for the
pur,~Z)3e of' invectill'%tion and ;)rospectin6 for deposits of mineral
oil d
Card 2/4 11)~'.S.Giircvich a report, on the importance of the geochemical

Geochemical and RLdionetrical met'node of Search ani 30-50-7-36/49
Pron~ectin- for De,~ocits. Tra-,isactions of the Conference in the Depart=ent
U
of Geolo I;i cal and Geo-raphic-al Sciences
0
zones of -round water for mineral oil pros;ecting.
12)V.A.Sokolov, N.M.Turkelltaub and A.A.Zhukhovitskiy spoke
abont"&1sanalytical methods and apoaratus for geocl.,,emical research.
13)B.P.Yaoenev and Yu.YI.Yurovskiy reported ori' Uas surveyinj; work
in the nort,iern Cai-casus_(-Severnyy Kavkaz).
G.G.GriCorlyev and A.S.Medvelev spoke about the
ex,,eri.-:(_,ntal application of ~;eoche-7_i,."l Methods of ;ros;;ccting
on the terri t ory of the province of Timiano-Pecbwsk which is rich in
mi,ieral oil and n,-.turvl ,-,as."
15)I.,A.Petersillye re,)orted on work dealin- with -as-containine
i~ 0
intrusiiZ,7 manoiveo of the Kola peninsula (Kollskiy poluostrov).
inveuti--,ated some problems of the Geochemical
fiiidir:g of a3 and nineral -oil -c Ont., ining deposits in the rock.
17)V.N',Kortsenshteyr. spoke about the mechanism of gas deposit
for.-.ation in the ro,-jon of Stavropol'.
ld)A.,L.G-eodekyan and G.A.AMogilevskiy jave a survey on research
Card 3/14 work in t'-e field oil .,-eoche:,!ical metl.,ods carried out abroad.

Gebf;,Ie:~Iical ".1A Me"hoda of scarch %nd 30-50-7-36/49
Proojecting fDr Doi.orito., Tv;..n.3i:,.tinns of the C3nfnrence in the Departnent
of Geolof-ical Scienxes
Furt.liorn,.)re, re;orts by foreii~n from tile German
De..-,oer!tti(- I'lepublic, lloum.-,riia (Ilumyniya), Poland (Pol'sha),
Czechnsloval:ia (Chvkhoulova~iya) ~inid Hunl;ary (Ven,,_;riya) were
!ie---rd, Tl%e conference found t.-1 t the theoretical work is carried
out on an 11"GLIffiCiently wide scol~c L.,,d th,-tt a number of problems
is :Aill little investi,-.-Aed. Vne -.ethods of investi,;ation are
i,r;',.(--ticnl:y still insufficiciAly uoe,.i. The decisions of the
:30.-~wrs cont:-ir a4vice for t,'.e future.
Card 4/4

STLJN-31TCI.IrRri, A.I.
Zonal and azonnl procecaes in the formation of underKround waters.
Trudy La").Cidrogeol.probl. 16:181-186 15S. (MIRA 12:2)
1. Laborntoriya gidrogeologicheakil-1, problem imeni F.P. Savarenskogo
All SSSR.
(Water, UnderGround)

SILIN-BY,KCHURIN, A.I.
Hydrod7namic and hydrochemical characteristics of the Baltic
Sea region. Trudy Lab.gidrogeol.probl. 20:3-28 '58.
(KIRA 120)
(Baltic Sea region--Water, Underground)

SILI 1;-DlTGl9JRl N, A.I., referent
Hydrogeology of North Africa and Hinduetan. Biul.MDIP. Otd-9901- 33 no-5:
159 S-0 158. (MIR& 12:1)
(Africa. North--Water. Underground) (India--Water. Underground)
(Palcintan--Watnr, Underground)

~rj ~~.I
Aleksr-f lvaroi&,; pC-jj-r-L;j-,y, Eonstantin ~edorovich;
YONONOV, V11dimir Ivanovich; LOUOVOLOV, G.V., doktor i-ol. -mineral.
nauk, otv.red.: FILIPPOVA, Mop redAzd-va; HYLINA, Yu.V., tekhn.
red.
[Role of underpround water and other natural factors in undor-
Fround coal pasification; from observations in the Moscow and
Lisichansk "Podzempas" stations~,Uol'podzemnykI-. vod i drugikh
prirodnyl-h faktorov v protsesse"nodzemnoi razifikatsti uFrlei; na
Imere Podmoskovnoi j Lisichanskoi stantsii "Podzempaza."
skva, Izd-vo Akad.nauk SSER, 190. 125 P. (Akademiia nauk
g
SSSH. Laboratorlia vidropeolopicheskikh problem. Trudy vol 23).
?MIRA'13'-12)
(Coal vasification, Undervround) (Water, bnderground)

KIJDELIN, Boris Ivanovich; BO"OLOT, G.T., prof., reteenzent; KAKARMO,
P.A., prof., rateen2ent: SILI-V=RKCHQRIN,-A,".-prof., rateenzent;
TQLSTIKHIN, N.I., prof.,'retsenzant; FAROMA, 1.1.9 red.;
IJQIKA OT, U.S., tekhn.red.
[Principles underl ng regional eatimation of natural resources of
underground waters~ PrIntsipy regionallnoi oteenki estestvennykh
reaursov podzemnykh vod. Koskva, Iz~-vo Konk.univ., 1960. 343 P.
(mm 14:4)
(Water, Underground)

jILIN-DENITIA1,11 A.I., prof.; DOGOMOUN, G.V., prof., akaderuk, otv.
~ I - - - - -.-iR -0 -P- - EMIN, - M;L. . rod. 4. zd-va; POIYAKOVA, TN.., tekhn. red.
[Underground waters of Forth AfrictilPodvemnye vody Severnoi
Afriki. Moskvr, lzd-vo Akad. nauk SSSR, 1962. 201 p.
(MIRA 15;10)
1. Akaderriya nnuk Belorusskoy SSSR (for Bogomolov).
(Africa., North-Water~ Underground)

BOGONDLOV, G.V.; VALEDINSKIr, V.I.; KOCHNEV, S.S.; MANIS, M.N.; FANTELEYEVA,
U.N.; POPOV, I.V.j SYROVATKIN, V.G.j* FOMICHEV, M.M.1
BOGORODITSKIr, K.F.; DURRANINA, V.I.; KRASIXTSEVA, V.V.;
MAKARENKO, P.A.; POKROVSKIrt V.A.; Aj.;
FOMIN, VX; SHAGOYANTS, S.A.
Illia Illich Kobosev; obituary. Trudy Lab.gidrogeol.probl.
42:101-102 162. (MIRA 150)
(Kobosev, Illia Illich, 1908-1961)

KUDELIN, B.I.; SILIN-BEKOURIN, A.I.
Concerning the book "Cord it.lons In Uzbjktstan from the point of
view of hydrology and engineering geoloi-,.r.lt Uzb.geol,zhur, 7 no*
5:89-89 163. (MIRA 17:3)

S T
TATARINOVA, Y-3.1., red.; BABU3HKIN, V.D.,
doktor geo-J.-miner.
'ekhi-naak, n4uchnaed.: KUDELB, B.I.,
nauk, prof., nauchn. red.; PLOTNIKOV, N.I., doktor geol.-miner.
naitkp prof@# nanchne reds
!Dynamics of underground waters; with the fundamentals of
hydraulics] DIiiamika podzemnykh vod; s osnovaml gidravliki.
Moskva, lzd,-.-,-o Mosk. univ., 1965. 379 p. (MIRA 181",

L !,tb81-66 EWT(m)/*E PF (n)-2/EWA (h) DM
AGU ?a: AF6=57 SOME CODEs ER/0089/65/M9/002/0181/0183
Y IT
AUTHOR: Andreyevp 0. L.; Si~llni. ; Stukovi-Go Y4; Fcnjpykhp Vo I*;
---7--= /1-2-
Shchebolev, laritsynag
CRGt none
TITIE: International comparison of neutron sources
SOURCE: Atomnaya energlyat v. 19,, no. 2p 19659 181-183
TOPIC TAGS: neutron distribution# radioactive source# neutronp radium# berylliump
radiation counter
ABSTRACT: The relative measurements of the Canadian Ra-*-% neutron source were
carried out considering the neutron distribution in open geometry and using a long
counter which could turn the source at any required angle. With the source axis
of rotation coinciding with the cylinder exist the asymmetry was 1% and with the
source axis turned to the side of the surface it was 105%o The relative measure-
ments for the source Indicated 3.25 neutrons/see. Orig. art. has,'2 figures and
I table. BL7
SUB CODE i 20p 18 SUBM DATE: 13Oct64 / CRIG W: 003 / UM M71 005
Card 1A MCs 539.16*081 539.1250

L 2983-66 EWA( k)jFP1E4T(l)1EWT(!n
- )ZqF(c) (k)-2/T/ t)/
ACCESSION NR: AP502-4-05-1--E--W,A-(inT-~2/1~WA(-hj SCTB/ UR/0057/65/035/009/1678/i684,
WG/JD LIP(c) 537-523.7
76
AUTHOR: Krindach, N. I.; Bilin-Bekchurin, I. A.; Tunitskiy, L.,N., CherkaBov, Yee- M*-,~
TITLE: Study of a high-frequency discharge in a neon-helium laser
SOURCE: Zhurnal tL-khnicheskoy fiziki, v. 35, no. 9, 1965, 1671-1684
TOPIC TAGS: gas laser,,neon helium laser, hf discharge, plasma discharge
ABSTRACT: A new method is proposed for determining the current and voltage diB-
tribution along a high-frequency discharge and a study, is made of the effect on
laser operation of inhomogeneities along such a discharge. The method is based
on the assumption that the voltage and current at any cross section of a discharge
tubc can be determined by the distance of that cross section from.the end of the
glowing portion of discharge. This assumption holds for any stationary discharge
at any cross section of which electron rise due to ionization if a unity. The
experiments were carried out by means of a,gas laser Ox - 6328 X) (see Fig. 1 of
the Enclosure) which incorporated a fused-quartz discharge tube 1.7 ca long and
8 mm in diameter (internal) filled with a neon - helium mixture at a 10:1 ratio
at a pressure of 0. 8 mm Hg. Two plane-parallel quartz. plates 0, and 02 were

L 2983-M
ACCESSION NR: AP5024051
placed at the tube ends at Brewster's angle. The equivalent circuit of the
discharge tube Is shown in Fig. 2. The b;be was placed between the two confbeal dielectric 'i
mirrors M with a 2-m radius of curvature and an - 1% transmission around 6328
The mirrors were adjusted by means of an AKT-400 collimator. The discharge tune
was fed by a 30-Mc frequency from an h-f oscillator, whose voltage was supplied
to 8-cm electrodes E and E 22 while electrodes E E49 and E5 (2-5 cm each) were
grounded. The oscillator was L-coupled to the 11charge tube and the currents I
and 12 and voltages Vrand V2 were measured by T-22 hot-wire ammeters and S-95
electrostatic voltmeters.(4-pf input capacitance) respectively. The output energy
was measured by means of a calibrated thermopile. The capacity of the discharge
tube, varied by a movable ground rod R placed above the tube, was deter-mined by
its distqnce from R. In the experiments a discharge with a maximum length of 35 CA
was studi *ed. The experimental method and results are discuseed in detail and
indicate good agreement with computed data. Orig. art. ha-: 1 table and 7 figure
[YKIT.
ASSOCIATION: Fizicheakiy institut imeni P. N. Lebedeva AN SSSR, 1406cbv.- .(Physics
Institute,AN SSSR),
SUBMITTED: l8Jan65 ENCL: 02 SIM CIOEE:
NO REF SOVI 004 o=R: oo6 ATD PFM

L 2983-M
ACCESSION'NR:
6VK
i.

7.4-222
Ivanov, L A. - Stilina A A. - Zhmur. D. G. and Ts"imr. Ob "rodakell trims-.
piratsionnogo ;;Ib~~ lexa. [On the determination of transeiration by a
forest stand.] Bo0axidwsks'11 Zkurxd, Moscow, 36(1):5--20. 1951. 11 tables. zv(s. DLC-
Method of quick weighing of tree leaves tested and applied tor a region near Moscow. Tram-0
soration intensity of 17 tree species was determined in more than 6000 cases. StAtiadcal
tabulation of observational materials shows that during the growing waarm good relation
exists between the air temperature and the transpiration intensity. Correlation coefficients
were 0.6".95. Transpiration rates at sufficient. moisuire supply am resented for each
species, arranged by temperatures from 4' to 29C. S&.bjtd Headixg. T=.tj; of
forests.-N. T. ZANY.

S"AS
ivanov L A, s;Nffa A. A. aw rserniker, JU. 0 tram"hAtfiff polexashch"kh
' " 'bl " - "
poradvusl.,il.kh ar~-~t~. [Trampira tion of wind shellul Plants under cundit ions
of the Dcrkul' steppe.] BoUkirhelkil ZA ur mat, hloseow, 37(2)-.113-121. 1952. fig., 8tables,Gf
refs. DI.C-Traitstitrailoh rib:* of different kinds of trees are giien for a region of ample
mokture sU k '(near Aloscow) and the Derkul' steppe, Tempe. ature, solar radiation and
batur-ailoit Ocit are higher in the steppe, but the transpiration nevertheless lowtr. Cor-
rtlak%A with temperature i!i high at suffit ait mo6ture ~Mj.!y. (up to 0.98) and low or even
,wgutsvu in the stelipt% No rulatiun to wind sp". subj"I Ilejiggs: 1. Transpiration of
frees 2. Moscow Region 3. Derkull' Steppe, Kazakbalan.-A. A

IVANOV, A.A.; SILIHA. A.A.; TSILINUM, Tu.L.
On the transpiration of shelterbelts on the Derkul Steppe. Bot.zhur. )8
no.2:166-184 Mr-An '53. (MLRA 6:6)
1. Derkullskaya opytnayu stantslya Instituts lea& a SSSJL
(Derkul Steppe--Trees) (Plants--Transpiration)

1 1, . I i "
. ~. I
IVANOV,L.A.; SILINA,A.A.
Actinometric determination of forest trnnsoiration in connection
with energy relations in different forestel areas. Fisiol.rnst.
2 no.4:313-319 JI-Ag'55. (MLRA 8:12)
1. Institut less, Akademii neuk SSSR, Moscow
(Plants--Transpiration)

SILINA.A.A.
Transpiration in tree species In the Tellermanovskii Fortat.
Fisiol.rust.2 no.4:364-372 Jl-Ag'55- ()WA 8:12)
1. Institut less, Akademii nauk SSSR, Moscow
(Borisoglebak Forest--Plants--Trnnspiration)

SILIXA, A.A.
Affect of tranapiration in some tree species on transpiration
in other species growing in mixed forest-eteppe stands. Trudy
Instassa 41:96-103 158. (MIRA 12:1)
(Foreet ecology) (Plants--Transpiration)

SILINA, A.A.
Transpiration in earlp- and late-opening oak races in the forest-
steppe. Trudy Inat.lesa 41:io4_lio '58. (MIRA 12:1)
(Oak) (Plants--Transpiration)

SILINA, A. D.
28988
Sluchay makhrovesti V tsvyetkakh l1vinego eyiva. Prtroda, 1949, No. 9, C. 71-72.
SO: Letoplal No. 34

MNUSOVA, A.N.; MLLINIKOVA, N.A.; BM"OVSKAYA, Z..j., ZAKIROVA, M.I.;
SILBA, A.G.
Nutrition of children in prefthool boarding establialuents in Kazan
and.isuggeBtions for its improvemont. Kaz. mod. zhur. no.4:84-88 JI-Ag
161. (14IRA 15:2)
1. K&Mm gigiyony pitaniya Isav. - dotsent A.K.Yunusova) Kazanskogo
mediUinskogo Instituta i gorbdakoy sanepidstantaii. (glavnyy vrach -
A.N.Kreppheva). (KAUN,CHILURF14--NUTRITILN)

L 02435-67 EWT(d)/EWP(l) TJP(c)
ACC NRt A106027322 O"d~-edi6t-:-di/b~04--3-~C6-iO-0-0-/-0-02/-010-7/0114
AUTHOR: Silina, A. S..
ORG: none
TITLE: An evaluation of the effect of a discrete control signal on side movement of
an aircraft on landing
i SOURCE: Leningrad. Univer3titet. Vestnik. Seriya mafematiki, m*khaniki L astronemii,
no. 2,
TOPIC TAGS: optimal control, numerical solution, aircraft control
Z,04 A/ 0 1,V 0 7'eO-L
ABSTRACT: The effect of control by discrete signals an the lateral movement of an
airplane are studied under the assumption that the radio control signal is continuous
within discrete intervdls of up to two seconds. Calculations we given to support
the reasonableness of this assumption. Lateral movement of tho aircraft is studied
because of the interest of the problem of discreteness of controlsignals on list and
yaw, lateral movement due to wind, etc.REquations arn derived for let* 'ral movement ol
a semi-automatically controlled airplanelon the glide path Uand;j)~ 'A numerical si-
lution is given for the resulting- system of equations and these results are presentid
in tabular and graphical form. Orig. art. has: 9 formulas, 3 figuresi'3 tables.
SUB CODE: 01/ SUBM DATE: 25Dec64/ ORIG X'W: 002 %
UDC: 533.601.3
Card L, 'Lf
W

L Oh93h-67 NT(d) IJP(c)
i'_ACZ _NRAP6__02_8__3_6_1 SOURCE CODE: lik/-06-4-3/6-67o-o-o76-6-~/6-68-~7do-i~6
AUTHOR: Silina, A. S.
................. ...
ORG: none
TITLE: An estimate of the influence of discrete control signals on the lateral motion of air-
craft during corrected landing
SOURCE: Leningrad. Universitet. Vestnik. Seriya matematiki, mekhaniki I astronomil,
no. 3, 1966, 83-90
TOPIC TAGS: aircraft control equipment, aircraft landing system, discrete automation
I
AVSTRACT: Using the simplest correction scheme based on aircraft-re corded velocity data,
th4 author investigates the discrete signal correction method. An analysis of comprehensive
Q~oretlcal calculation of the side-slip equation solution shows that durpg landing approach
s4eeds of the order of 100 cm/sec it Is possible to use a discrete signal control with up to 10
sqc intervals. In the case of speeds approaching 200 m/sec, the discrete signal must be
smoothed out (this can be achieved with even the simplest schemes). The buiing of the cor-
rtction system requires the solution of the simplest system of equations of motion of the
1/2 UDQ 533.601.3

ACC NRi AP6028361
aircraft. The author thanks Irof. 1. P. Ginzburg for valuable advice.
formulas, 5 tables, and 2 ftgures.
SUB CODE: 01, ZVI SUBM DATii 25Dec64/ ORIG REF: 003
kh
Orig. art. has: 26

BEWSTOTSKIY, Isaak Abramovich; MURAWA, Faina Savellyevna; SILINA,
Alevtina Vasillyevna; MAKAROV, V.I.,, red.
[Multiple-unit TS-1 trolleybus] Sochlenryi trolleibus TS-1.
Moakvaj Stroiizdat,, 1965. 173. p. (mjRA 18:8)

.Ie

SILINA, E.H.
1
ImportAnce of certain reactivity indicators in chronic nutritional
disorders in children (with summary in English]. PedintriiA 16
no.5:29-34 My 158 (KIRA 11:6)
1. Iz domn rebenka No.2 Sverdlovskfk (glavnyy vrach T.S. luklina.
nAnchnyy rukovoditell - zavkafedroy nervnvkh bolezney Sverdlovskogo
meditainskogo institute prof. D.G. Shefer).
(CH ILDRM--D ISMAISES)

SILINA,-E.M.; KHkRITONOVA,,A,V&
Dyramico and structure of blood system diseases and hemorrhagic diatheses
in children. Vop. okh. mat. i dot. 5 no.6130-32 N-D 160*
(HIM 13:12)
1. Iz Sverdlovskogo nauch**.isBledovatellskogo instituta okhrany
materinstva I, m1adencheBtva (direktor - kand.zed.nauk RA-Halyshevap
nauchnyy rukovoditall - dotsent R.Ye.Leyenson) i kafedry detskikh
bolexpey (zav. - dotsent k.F~Bobylevii) Sverdlovokogo gosudaretvennogo
4ditiinskoio institute. (direk-tor - prof. L.F.Zserev).
BLOOD-DISFASES) . (DIATIM IS)

ALMOV, Zh.I.; SILIM, E.Y.
Iffect of the surlacm state on the breakdown voltage of silicon
alloy diodes. Fiz.tyer.tela 1 no.12-.1878-1879 D 159.
(MIU 13:5)
1, Yiziko-tekhnicheskiy- institut AN SSSR, Leningrad.
(Diodes)

L 52235-65 EPF(o)/EPA(s)-2/FW(m)/ EWG(m)/kWP(b)/EWP(i.) Pr-h/R-7 IJP(c)
RDVJ a
ACCESSION NR: AT5012663 UR/2539,1'63/000/044/0020/0023 _32
iAUTHOR: SlUna, E. Yu.; Khachaturyan, T.A.
----------
TITLE: Temperature dependence of the saturated vapor prearure of mercury selenide
SOURCE: Moscow. Khimiko-tekbnologichealdy institut. Trudy, no. 44, 1963. Iseledovanlya:
v oblasti fizicheskoy khimii, analiticheskoy khimil 1 elWdiokb Imii (Research in the field
of physical chemistry, analytical chemistry and electrochemiatry), 20-23
TOPIC TAGS: mercury selenide, mercury selenide vapor prossure, mercury selenide
sublimation, vapor pressure determination
f
ABSTRACT; Tile purpose of this work was to determine the Eaturated vapor pressureP
mercury selenide (11gSe) in the range 240-500C. Between 500 and 340C, the vapor pres-
sure was determined by the now method from the weight loss and betwets 325 and 240C,.
-by Knudsen's effusion method. The results of measurements made by both methods are
described by the equation log P 9.032 - 597 6 1 obtained by the least-squares method.
T
From the slope of this curve, AH was found to be 27.3 kcal/mole. Li their treatment Of
subl
the results. the authors adopted the molecular weight correiqjonding to the formula HgSe,
Ca,d 1/2

L 52235-65
iACCESMON NR: AM12663
However, since there are indications In the literature that Hg;3e dissociates in the vapor,
the data obtained represent some arbitrary pressure which riEflects the VnPorization
rate of HgSe and Is proportional to the vapor pressure of HgStj. Orig. art. has*. 2 tables,
1 figure, and 4 formulas.
A
ASSOCIATION: Moskovskly khImiko.tekbnologlebeekty inst] tuts (Moscow Chemical
Engineering Institute)
SUBMITTED: 00 ENCL: 00 SUB CODE: GC
I NO REF BOV: 011 OTHER: 003
2/2
Card

SILINA, E.Yu.; KHACHATURYAN, T.A.
Accounting for the effect of thermal diffusion In the determination
of saturated vapor pressure by the gas stream method. Trudy MTI
no."il3-19 164. (KRA 18 11)
Temperature dependence of the pressure nf mercury selenide
saturated vapor. lbid.M-2)

L 24786-65 EPP (0/ EPA (a 5 It) Pr-4/.Pt-10
ACCES NR: AP4049619 JW/JD/JG StOW'6164/0381011127331213b-
AUTHOR: Mina, E. Yu.; Karape(lyanta.-M. Kh.
"C
-,-, i " i. -
TITLE, Temperature dependence Of the PTVBBurt of saturated-MSES-MEry- telluride
vapors
SOURC-14": Zhurnal lizicheakoy khImII, v. 38, no. 11, 1964, 2733- 2735
TOPIC TAGS: saturated vapor pressure, mercury telluride vapor, vapor pres-
sure temperature dependence
ABSTRACT: The pressure of saturated mercury telluride vapors as a funct
ton of
temperature has been measured by the Knudsen method in the range from 215 to.
309 C and by thenuxmethod from 292 to 388 C. The results are described by
the equation
log P -(56401T) + 9.13 (mm Hg)
It Is deduced from this equation that A H
subl 23. 6 kcal/ mole. Orig. art. has:
2 figures and I table
Card 2/2

L 24786-65
ACCESSION NR: AP4049619
'ASSOCIATION: Moskovskiy khimiko- tekhnologicheikiy inatitut im.
D. L Mendeleeva (Moscow Institute of Chemical Technology
SUBMITTED: 24Dec6.q ENCL: 00
SUB CODE: GC, t4E
NO REF SOV.- 009
OTHER: 003

SILINA, E.Yu.1 KARMZT1YANTS, M.Kh.
Temperature dependence of the saturated vapor pressure of
marcury telluride. Zhur.fiz.khim. 38 no.11:2733-2735 N 164.
(MIRA 18:2)
1. Moskovskiy khimiko-tekhnologicheokiy institut imeni
Mandeleyeva.

E . yu V.*~-,AAI-*--.T 'U., I
I
i.etermination of saturated vapor pr-ss-,.;re by the flow method
under conditions of signif~.cant effects. Zhjr.
f iz. khIM. 38 112:2907-2912 P
(MIRLA 18:2)
',',oskuv3kiy Fhimi.ko-tekhnol6gi~:tpo'f-liy institut imeni D.I.
v%ndt.fleynva.

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Alexh N.* :Idst4f!

1'. , 11 288
AUTHOR: Zarembo, YU.I. and Kal~,Ianq G.E.
TITIAS Mod!--rn m~Aliodc in bei-jllium technolo~W (Sovremennyc metody
Lo1dinoloi--ii b(~rilliya. )
Pi~itiODIGAL: "Tzv(,ltn,,Ie i..etally111 (11,on-ferrou,_7
19579 110. 1, i)ij. GrG - 71, (U.S.S.R.)
AE,S_ciUGT: This is a review of recent developments in the metallurgy
of bvrylliua, os,.,Qcially in connection with atomic energy.
The work, discusced is almost entirely non-Russian; Russian
~-,-ork considered is that reported at t1he-Geneva Conference on
tile peaceful uses of atomic energy, 1955. It is suggested
that in the U.S.S.R. future wor-'c on beryllium production should
be directed to improving the yield, automation of process
operation, development of new and cheaper methods of obtaining
berylliui.i comiounds and the :.i.-it-al anl the utilisation of
low--6a-ade (less ~IiLm 101,-, &,0) concentrates.
Thei-e are 14 refe1ence.S, of w1li3h 1 is Russian.

W87
S/136/60/000/012/005/010
1/0 Mtao VC18 9193/E183
AUTHORS: Silina, G.F., and Grinberg, L.L.
TITLE: Kle~ctroifyt C~efining of Beryllium
PERIODICAL: Tsvetnyye metally, 1960, No. 12, pp. 1+7-53
TEXT: The object of the present investigation was to develop
an electrolytic process of refining beryllium that would produce
material sufficiently pure to be suitable for nuclear engineering
applications. The laboratory experiments were carried out in
quartz vessels. Nickel strip cathodes and commercial grade
beryllium anodes, made by the powder metallurgy technique (hot or
cold p:-essing), were used. To avoid contamination of the metal
by chlorine (in the form of beryllium oxichloride)t an electrolyte,
consisting of KF-NaF-2BeF2 and melting at approximately 600 OGI
was first tried. The current efficienoy attained was low; the
metal was deposited in a finely-crystalline form and difficulties
were experienced in washing off the solidified electrolyte. Since
the KC1-NaCl-2BeF? mixture proved unsatisfactory for the same
reasons, the elec rolyte normally used In electrolytic extraction
of beryllium, and consisting of approximately equal proportions
Card 115

86687
S/136/6o/ooo/ol2/oo5/010
B193/9183
Electrolytic Refining of Beryllium
of beryllium and sodium chlorides (melting point equal 220 OC),
was employed in subsequent experiments. The results of tests in
which the cathode current density was varied between )+ and 16
amp/dm2, showed that up to 12 amp/dm2 the current efficiency
remains practically constant and a compact beryllium deposit)
consisting of bright crystals, is roduced. When the current
density was increased to 16 amp/dJ, a small quantity of spongy
deposit was formed. The berylll-qm anodes contained
4 to 5 x 10-2% Fe, 1 to 5 x 10-?-% All 2 x lo-2% Cu, 1 x lo-3% mn,
and 5 x 10-2% Ni. Variation of the anode current density
between 6 and 50 amp/dm2 hardly affected the Impurity content of
the cathode deposit, which contained 1 to 3 x lo-3$ re,
3 x io-3% Al and Nit 1.5 x lo-3% Cut and lo-3% Mn. Determination
of the current efficiency was the object of the next series of
experiments, carried out under the optimum conditions, i.et
current 3 to 1+ amp; cathode current density 8.8 to 12 amp/dm2-
temperature 31+0 OC; voltage 0.3 to 0.5 V. It was found that'
Card 2/5

86687
B/136/60/000/012/005/010
E193/E183
Electrolytic Refining of Beryllium
the time required for the current efficiency to attain a steady
value was the same (about 24 h), irrespective of the purity of
BeC12 in the electrolyte, but the maximum current efficiency
attained was lower when impure BOC12 was used. The current
efficiency and recovery attained in a 180-hour test were 85 and
83% respectively. Under these conditions, 50% of beryllium was
deposited in the form of large, plate-like crystals and 50% in
the form of smaller grains, strongly adhering to the cathode.
The laboratory experiments were repeated on a somewhat larger
scale, after which long-term tests were conducted in a pilot plant.
In view of promising results obtained, a series of tests on an
industrial scale was carried out. A standard bath for electrolytic
extraction of beryllium was used for this purpose. The anode
consisted of seven beryllium powder compact rings (each weighing
I kg), suspended on a graphite rod. Before starting the refining
operation, the bath was operated for a short period with a
graphite anode, in order to remove from the electrolyte those
metallic impurities which are more electro-positive than beryllium.
Card 3/5

86687
S/136/60/000/012/005/010
R193/E183
Electrolytic Refining of Beryllium
The voltage and current emplo ed were 5.5 V and 800 amp. The
electrolyte (50:50 BeC12:NaCl~ was replenished from an adjacent
bath with an Insoluble anode, The energy consumed in one test
amounted to 34 000 amp-h, the maximum output being 3.5 kg of
refined beryllium, which corresponded to an average current
efficiency of 80%. Recovery of beryllium attained was also 80%.
The cathode deposit constituted 94% of the dissolved anode
material. A homogeneous deposit, in the form of bright plate-
like crystals, measuring 15 x 20 mm, was produced. For the
preparation of anodes, beryllium obtained either electrolytically
or by thermal reduction of fluoride, was used. In the former
case, it contained 0.02-0.05% Fe, 0.1% Ni, and 0.005-0.008% Cu;
in the latter case the impurity content was 0.12% Fe, approxi-
mately 0.01% Ni, and 0.01% Cu and Mn. In most cases the refined
metal contained 0.005-0.006% Fe, 0 01% Ni and 0.003% Cu; the
manganese content did not exceed ~ x 10-4%, that of zinc and
silicon being less than n x lo-3%; the deposit contained less
than 0.3 g/t boron and less than 0.01+ g/t rare earths.
Card 4/5

86687
S/136/60/000/012/005/010
H193/R183
Electrolytic Refining of Beryllium
The metal in the anodic slime collector contained (after washing)
0.05-0.02% Fe, 0.05-0-03% Ni, and 0.02-0-03% Cu; no
agglomeration of impurities in the electrolyte was observed.
It was concluded that beryllium obtained by the process
described in the present paper satisfies most stringent
requirements and approaches in quality metal refined by
distillation.
There are 4 figures, 6 tables and 2 Soviet references.
Card 5/5

SOV/136-58-12-9/22
AUTHORS: Ostroushko, Yu.I., Meyerson, G.A., Silina, G.F. and
Shtrapenina, R.B.
TITLE: Electrolytic Method of Producing Tantalum (Blektroliti-
cheskiy spowob polucheniya tantala)
PERIODICAL: Tsvetnyye Metally, 1958, Nr 12, pp 38 - 44 (USSR)
ABSTRACT: Electrolysis of melts for tantalum production was first
developed in 1929 (Ref 1). The method, which was adopted
outside the USSR, depended on the decomposition of Ta2O 51
whose presence in the K2TaF -KF(-KCI-NaF) melt eliminated
the anode effect. Electrolysis becomes progressively more
advantageous than the sodium-thermic method as the scale of
operations is increased, a further advantage being the
increasing availability of the pentoxide. The work des-
cribed had as its object the study of electrolysis conditions
for a type of electrolyte (based on NaCl + KC1 eutectic)
not used in practice. Electrolysis wasiffected in a nickel
crucible (cathode) (Figure 1) 100 mm in diameter, the bath
depth being 180 mm. The cylindrical graphite anode, with a
working surface of 546 am , wa's fixed centrally. The
electrolyte was made by fusing the eqUi-molecular chlorides
Cardl/3 (calcined, chemically pure) mixture and the K2TaF ? (pure.,

SOV/136-58-12-9/22
Electrolytic Method of Producing Tantalum
dry) at 650 - ?00 0C and then adding pure dry Ta2O
(10-lW* of the weight of the K TaF could dissolve) after
the anode had been inserted a~g thZ direct current switched
on. The influence on recovery and current efficiency of
the K2TaF7 content (10-100%)0of the electrolyte (Figure 2)
and of temperature (610-?20 C) (Figure 3) were studied, as
was the effect on electrolysis of anodic current density
(5-140 A/dm 2). The influence of these factors on the size
composition of the tantalum powder was studied as was the
behaviour of impurities (Figure 4 shows the impurity
contents of the bath as a function of tim&4 Table 2 giving
the corresponding information for the powder). It was
found that a pure powder, suitable for producing malleable
tantalum could be advantageously made by electrolysis
(followed by the-usual purification) from electrolytes
containing 67-70% (NaC1 + KCl)j 25-30% K2TaF7 and
3-3.5% Ta205 which melts at 600 0C, is highly fluid and
Card 2/3 relatively non-volatile at the electrolysis temperature

Electrolytic Method of Producing Tantalum SOV/136-58-12-9/22
(about 700 OC) and has litle effect on the nickel. A
system for maintaining electrolyte quality over long working
periods has been devised. The cell used provides for
continuous operation with periodical removal of the 70 %
Ta cathodic deposit. There are 5 figures, 2 tables and
12 references, 9 of which are English and 3 Soviet.
Card 3/3

FILASE I 13C*K MPU)ITATION SOV/5022
Silina, G.F., Yu. I. Zarembo, and L.E. Bertina
BeriDAy4 kbialcheskays tekhnologiya i meta1lurgiya (Beryllium; Chemical Technology
P
and Metallurgy) Moscow, Atomizdat, 1960. 119 P. 4,000 copies printed.
Ed. (Title page): Viktor I. Spitsyn; Ed.: A.F. Alyabyev; Tech. Ed.: N.A. Vlasova.
PURPOSE: This book is intended for metallurgists, physicists, chemists and other
persons who may be interested in the production, properties, and use of berylli-
um and its compounds.
COVERAGE: The book gives a critical review of literature published in the last
fifteen years on the physicochemicalpnpclear, mechanical, corrosion, and chemi-
cal properties of beryllium. It describes the industrial processes of produc-
ing beryllium and its compounds on the basis of non-Soviet and Soviet literature
published up to 1959- Chapters I and II were written by Yu,.I. Zarembo; Chapter
III, by Viktor I. Spitsyn (Editor), G.F. Silina, and L.B. Bertina; Chapter IV,'
by G.F. Silina; and Chapter V, jointly by Zarembo and Silina. No personalities
are mentioned. The book is based mainly on Western sources. There we 261 ref-
erences,of which 67 are Soviet.
Cax&__1"

SILINA Gj~,; ZAREMBO, Yu.I.; bEhTINA, L.E.; SPITSYN, V.I.., akad.,, red.j
-- -I---
ALYA131YLV, A.F., rcd.; VLASOVA, N.A... tekhn. red. I
[Beryllium; chemical technology and metallurgy] Berillii; khimiche-
Asia tekhnologiia i metallurgiia. Pod red. V.I.Spitsyna. Moskva,
Izd-vo Gos.komiteta Soveta Ministrov SSSR po ispollzovaniiu atomnoi
energii, 1960. 119 p beryllium) (MIRA 14:12)