SCIENTIFIC ABSTRACT FR:OGNEVA, T.A. TO:OGNEV, K.G.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001237800010-6
• Release Decision: RIF
• Original Classification: U
• Document Creation Date: November 2, 2016
• Sequence Number: 10
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTR

At the Final Meeting of thr! Scientific Cou~:rcil ~If ttae rain S~:'~f~o~~;~-�-~y%~;~
Geophysical ~Jbeerva#:ory irn~lni A. I. ~Ioyeykav
Shifrin re,art~~ed on ~.nver,t~."�itions of radiation char~rct�~ristic:~
i.n plsyi.~d~ r~t1d ;fag} a.r~d eta tkic~ svczrk~n~ �ut ~f, ~n o},tis;~I u~t~~t~liocl
of investi~;e,ti:rig the fine tttx~ucture of clouds and Pogo I~~ ~o
Krasilf shcl~ike~v reparted an the dev~elopme.nt of a flyring apparatus
fox investie,ting the spectral. chax~acteristics of tr~f: atz.es,~
Card 2%3 I.F. 5kachkavs and Yu. D. Yanishevskiy spoke on the improvement
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AII~iIC7I?: O~n~:va~ T. A.
TI`SLY:: At tI"iP Y~ir~al Ydeeting of tha Sei.en~~ifie Council of trio l~fain.
Geoph,Ysics.l C"bservator;~ ~.r~eni A. :L. Voy�ykov (~~(a itogo~b~oy sessii
Uahenogo r;ove~ta Glavnoy geofizichi,skay obse~'vai;orii im. A. I.
Vayrykova)
pL1~ICIDTCAL: ~teteorologiya i gidrolUgiya, 19~~, Pfr 5, pp fo - 61 (Uii~I,)
111;alI~bCT: A meeting of tl~e Scientific Cou21ci1 t4O1+: place at tiie {flavnFa.ya
) on
tor
Ub
y
ser~a
geofizic};cskaya observatori.ya (Fain Geaphysica;L
DecertbE~r ?3�~7: 19jt3. It waa dedicated i;o the .Pinar. rep>ults in
the fulfilment of the plo.n for ac~.entif~:e reee,~rch work: in 1~~5~,~
:ore tha.. 2C reports ~raerR delivered. M. ~. Yud,in x�E:ported on
problems cor.:~~ected ~vith _�e im~}rovement of cal~~ula~:ian. methods
for baric f~.elds temperature e,nd ,vind fnreeast.s. 0. ~. Droz~?ov
spa?~e about can~iderin~, the rules of moisture exc~wn~;e in pxe-
czpitation f'arecasts. T. V. Y'okrovsl;aya report ~~d on tb.~: resu:lts
of general.ix,e.tian of the data on air-tQrn~~o-raturc araornr.lies in
the ~urolac3ar- part of the U~Sf~ ar~~. in lf~est Sib~;ria for pracl:i~:al
use in l~ang.,termwcl fnrecs,ets. YI. ~. Shishkin spoke on th~~ va.,rieties
Card 1~3 of convecti~-~Q cloudiness e,t tl~e fall of precil~if:ai;ion~~. ~d as
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Research in the ~Procesees (ICont. } S4V~~1.73~
Chestnaya, I.I. A:i:r Current~a Over Lake Sevart 3
5elezneva, Ye.S. 9~he Origin oP Northern Seer Wia~ds in the Lake 5evau
Basin '
Matve;~ev, L.T. Ai:K~borne Stuuiiea of the Strutcturel c-f Turbutlent Air Curren~ta
in the Heigime o:C' Lalte Sevt~an
Matveyev, J:.'C. Stx~;-Ctt~ral 1~'unctian at the Veartical Velocity' o~ the Air
Cuxrent aaad a N~s~~r Method off' Computing the t:oefPi eient et Tu~'bu~,ence
in the ~'r~se Atm~�~phere
Vorontsov, P.A. ~e~�tical Movements o4 Air Over Labe Sevaa
0,~ T A. Trial Camput~t~:on oP Sutrf'ace Water Evapoiration aMd ~~he
Heat-Air Fxehaz~e~ Over Lake Halkhash
Card 3~`'~
~t
6g
77
8~
98
108
124
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Reaea~rch in the Processes (Cont. )
SOV~~1734
the meteorological and a~e:rological investigation conducted at Loge Se1-~Etti ~mder
field coa~ditiona during �tik~e summer of 1956. TWO artic].ea are devgted to meteoro�~
logical conditions prevailing over Lake Balkhs~-, No personalities are mentioneii.
The articles are acccarpa-~;Led by tables, diagramit, and bibliographic rexerencer~.
TABLE OF CONTENTS:
Timofeyev, M.P., and T.A. Ogneva Relationship Betgreen Evaporation and a
DePicienc~ in Air~t;y ~
Drosdov, O.A. Mo~at~utre Cycle in a Mounte~.nous Aeprus~ion IQ
Ogne~r~,, T.A. Compu~i;ing Evaporation Fran the Surface of LE~lce Sevau 16
� tCi.ri]~tova,T.V. Rad~,lation Ba;iance of Lake Sevan ~ 25
I~i.ril~.ova, T.V., an~i R.F. Bylaring . Results off' 3ubat~ueoua Radiation
Measuramente 3t~
Vorontsov, P.A. C~.aracteriatics of the Wind and T~-exmsl. Regimen t?vet�
Lake Seven ~I
Card 2~~ J
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3(7) ~) ~ 'r ~ PffASE x BCtQK ~FTAIT~~IC~ SW/].7~}
Leningrad. Gla~n~ra geoPizi:cheakaya obaervetoriy8
Is,sledovaniy~e, protaesaov te~,~lo- i vlagoob~uena nad ~-odoyemami (Research in tYae
Px~oceseee, oP Heat and Mod suture Exchange Cher Hager ReaervQire) Leningrad,
Gidraneteldizdat, 1958. 130 p. {Series: xta: Ty~+, vyp� 78) 1,75
copies printed.
Sponsoring A.gericy: USSR. Glavnaye upravleniye gidreffieteoa~ologicheakoy
sluzhby
Ed. (title page) : M.F. TiBaofeyev, Candidate oY Fktyal~cal and Mathematical
Sciemces; Ed. {inside book): Yu.Vo Vlaaova; ~Pec~. Ed.: N.V. Yolkov.
PURPOSE: T'hia publication is intended Por acient~.fic and technical ~~ra~oranel
working 1.n meteorology, }aydrology, hydrotechnolc~gq and related, Fields.
COVERA4E; This collection ~~f ax~tic],es, b~- several authors, reports tl~e results of
~!xperimex~tal work carriers on in 1856 ia1 in~reati~~sting the aneteorol+~gie,a~}. con-
ditions c-ver water reaer~~oira. xt cantaiaaa t}~e re$ults `sand an exeaainatir~n of
Card 1/~
r;
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~_ ~ -6~-~-7/16
AIOR: 4gr:eva, ~. A.
.... _,.,r .._.._,~, _~.~_~,~,_.,~,.~.,
TITLE:
~arbnlence C~effie;Lent Valt~s Over Lis ,mod Resex~3rs (J ve~.ic.bins~kti
koeffitsiyea~~s t~axla~.lentsfi rr~d v~~3.~; yemu~ai. )
PRRIfIDICAL: Trt~y ~aasm~x ~~f'L~ichesk:~y o~ase~ra~-:.~rii , 1957,
Nr 69a 51-56 ~~~3R)
AA3TAACT: Ttirb'u1~n4 mi~4.t3g, c~m~arisi~2q evap~ra~ci~:~, �transf~rms,;;ics~~ of air n-aases,
and ~B in win~t ve].acity, .he~~ �~h~.a~ fir been seldom studisd G-~r
su~1.1 'k~ss-~.:te$ a~ xa~;er s~zch as IAkes ar.~. ~-servai:~s. They a~x'~hnr z~ev'S.e:xe~
this prsyblem an3 �:f"ferg a few mather~tica:l. ft~rmu:lae fc:r ccrosiderstion.
The costa qunted re:f�er mainly to Lake Balkl~sh. '.@he t~ea~~ ttxrbu]~,d,c:e eo-
efficient i~ c~,e~'ia~.~d as the ratio of turbatlence coeffief.ent to xind v+e2-
aeity. Tail mean ~t~arbu~:~ce c~ff~.cient carer re:3erYU~,r9~ and lakes eras
fc~wnd +,a be~�~teen 0, 41 and 4.02. Th~x~ are! 3 tab:tns azad 7 3~x~riet refer-
enc:es.
AVAII.APf:CF: Li'~ra.~; of Ccr.:.~:~sr~~
Card 1~1
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if~h'~Y~{, T.A.
.. 3wwr.?~nn,s'Yh +~Y K+ry ~,d `~~((Fe~y.~.S aXa."."s-
Di.~tribntfon ~~ mat~~~orological elements oee~r b4d.i~e of ~at~r. ~`~
G40 no.59xb1-b3 "5~~~. .(its Io:;3
(Ml cr ome t e or~~~ I ogy ~
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~ {{~
IITiI~A~L~ 'P.~ OG6~YA 't' . � '~'I~:4FB'YRY~ H.F'.
rati~n~ ipo~ e~~rf~a~ of i~].end bodi~a a-f xat~rr. ~~ ~ nc~~,~ ~s~'-
~r~Po ~ i~A la s~ 3~
44 "5~.
(~~p~ra~t~.nn)
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Oat~lA, T. A. ~ Bt7~U~~0, ',[. ~. j A,Y~~HT~Ty ~.A.
~plnfluet~ae of I;irrigatlcfn Upon the Distribution. of ~teorolog:ical. L~1.ea~nts
~- the Layer Near the f,rQUndn
'Tr. Gl. Ceofix. pbr~exvs~torii~ No 39, 61~9t3, 1953
The author ~~.v~1e the aci~gaarative characterist~,cs~o~ters~and~inothsei~ail
arolo~l.cal elements in the later of air up '~ 5
F to given aerological ~tnd ground observations in a
doXn tc- 50 cry acoordin!?, It ie found that the weed
semide~-ert aYUI in an i~;~rigated cotton field.
of ~rincl is r+sduced ~0-~~~G percent under the in~'~Luence off' irrigation a~~~d fore8t
belta~. ~~,Z,ZhGeol~ Ida ~!, 195t~~
SOs W~~31187, 8 l~tr 55
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~.~QtVA, T.~..; T~ro~~r, ~.~.; T~~Tr~, o. ~~. ~ ,~Y'~~~'r~6;~`, ~�~..; tA, T.~.;
,I~YKH'Tb�fAN, D. L
~Messux~ment of the Keat Na,lanc� of the Activl~ ~trf~e for tie Cage of
xrrigafi.icm"'
Tr. (33. tieofi~. ~bezvai~orii, No 39, 374, 39'73
The authors present data onatdesrt andsinf ~a~n irrigated fj.~ldatiThe~t~ace
of the aati~e surface ,tn a
xn~ obi~ained ~ an czxp~~diticm of the 1V~,in t~-aphyeiaa7� pbser~ratorar in ~Iuly
3952 is~ the savk`no~ nF~khta~re~.,~+ a ca~lleati:ve fiaxm ~n Ceni~r~-1. ~.~~.� it
area fo~md that heat exchange in sail practica~.ly does not ct-ange under the
influence of irrigation. (KZhGeol, No 3, 1q~.t)
s0: ~'-3'1187, 8 Mar 55
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_ ~'
Kt)I;15r~II~ ~ A. ~ pro~',- ~ doktcl:r tekhn.nauk, OGd+1~YA~-� , Icand.tekbn..n~uk; FA'.~ERSHTF~~DT,
D,
gp~~g up tha r~~;~ening of vegetab3a a. Srn-. tang. 35 nc (br~R~' ~ s7 )
t~~
~ Ve;~;etable trade )
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T~ze C:Ii~.I1~e of the Properties of Lac.2zer i?eair~s Viz:;?er ~j',- ~,~~~ _,.~_~~~:sr.
the A~~tion of Oxid9.zero "'' `""
part of tl-e-~a gas s.~ectroscoped iz- itlf'r~.rEd li~;:~~t. H2O irapro~ve~l
t:.e I;-raperti~.s of lacquer resins ('.Fable 1 } ; t?~ie free ~~~~;e~;ol,
t~~e rlioxydipl~-er-yl :~etii:~nes se
ti24 ~~;r~pzlc~.ty of he:it~~; di;~t~olved, ar of beizl~~ x.ls.:z~denE.d in tl;e ca,;~e
of a lank--l~~:~tinc; trea,tr~er-t ~7ith forr~s.ldei-ryrie. Triese x~euins
px~ac'I:ic4il.ly tla ziut contFa.in any lc~d~-znolecul~~r ~;~ater-solu.bl.e
cornpt:>unds, have an increased ~aeltin~ point and hid�i~er acid
nu:ab~srs, bi-t tP-e; cs.r~ t,e dyed Pe~~r.�::ently-blwck. Furt!:er, it
~r~~s,pxovec~ t~-s,t t-e refiins treatE-d as above readily c;y~bine
durirz~ pxcssi,l7~ both n~ith o:�~~'aziic; aild *~iF-eral fil].iz-f ~ateri~.lss
~n c~antr~ad~.ct~ior- to ordin,~ry ~.acc;uer resins n~~t anl;~ he;{a.-
mQth;~lone tetrar.~iries, bt-t al ,o fc~r,~>~alc~ehyde holy-aer.s (,of t~~e t,~,~e
of p~-polyoxytzletl~u lens; } may be used as solidifiexz: fax ox dir .: p
}~ i d 1l 1 4~ ~ 1 ~ M^ c J,
o f 115~1`C.dv~.iC..~l. ~"~~ Lo'' i..:~~~.('.'.~ �'y. '~ f .a Yi:7 ~ t.'.l~ :~... ~.� ^ ''~
., ;~ ~:.~~~be~r
p'�La~y'~hlanrzd~ ~~ ~ ,
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~~V/b8,m~8~I2~:~2/2',i
An In~pro~~ement ~.~ the T~echno:logy of F~�ocess~.ng Coal Tar T~her~ols
durat~.ou of heat~.ng than on the temperature (~rithin ,~
range of 170~~,3o�G, Table ~;-0 4) A considerable amount
o~ ~;~~.uab:l.e h~..gh bo.i.~.~,ng ph4~ndls ~ pr~..ma~�i1y ;naphtho~.s,
,~rere found .~,n 1~~ae res~.duesa Thus ~.~' the phe;r.~ol~.o p~,tc~~
iwa~l be separated before the distillation. of ;phenols .and
'the d,u~atio.n cif their Y~eat~.rig decreased? the o. the yj.el~,
~~f tt~~e ~ esldu~~s c~auld be a1.~~ decreased and ~.n addi#:~.on
the res idu�s would contain ~t h~.ghe~� prc~partion of
ns.pht~hclls and their homo3.og~kc:sa Foxy th� abo~'e reasc>.ns
Flash. e~~-~aporat:i.on of aqueou:~ raw phenols with a sho~.~t
heat~r~~ time ~~as tested (Talales ~9~)~ It was found that
'~y heat.,ing to 190-200c' (100-,~.~Omn H~) a complete separation
+a~' phex,i~~ls rare be obtained ;end due to a short heati~Zg time
I~10.~~?{~ ffi~.n) t~~e degree of t~^ansformation of phenols is lo't~v
Ga~�d. ~I3
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AZ+-;~CHURS: ~h,a_r, ~.a~npo~~~. ~Nh, G4 ~~ i and, tJ~~~l6~~58,~12...1202 j
TI71'LEa An Irriprovem,c-nt in the Tec~znol.o ~ .~~.~~~:-_ ,..
Phenclls ~~sovershsnstvovax~iye tekhnolooiessing CoE~.1 Tar
kamer~nougnl ~nYkh ~�nolov, g i .~ererabotki
p~I~IU~IICALs Kok:s i Khimi a ,
ABaTRACT~ The composition oflre$r Nr 1~' PP 4:1m~.5 ~U~~SR)
of ~?henals f:t~om ~a.sterndookine.e o~f1'er the distillation
The r'~~sidues ware redistilledg ~nder~vaas 1zavestig~~tedA
a to:m;~era tur~~ of lBQo cuo (~ 5~1pmm,~ up to
nvr~-a:L pressure) o The ~ ~~zniasi tnt to 305~3~1t)o
C under
furthE~r inve.~tigated bar re~ytif.ioat~oroif {T~bt~illate was
oQmpa~sition ~If raw phenols and those obtai~,~d tr3)� The
residUi.es w,a~s hemparad (Tab7.� ~.~ , om tho
.z~ coal ta:~ p nolsp partic:uiar:~ hithwas found th~~ts
considerable than es ~ g er phenols u:~~dergo
phenolic g dux�in~~ hea~~ing' name~.~ the ~'i~el~.d of
nh~nnl pitch increases while ~~he ~ont6nt cad' lowe�
.~~-_,_.. _ ~ degreases and the ix com~sos~,t j.om chaxx es
coffipos.i.t~.or:- o:~ phen�1s and ~ri~nE~ril~r the rt�~ a ~_) ;~},~.
phenol;~tc; pitc~~~, i e compone;qts ~-oilir a p ence o.~;
GarcC l!3 ~ dec�i~~ing inj.luence on the decomposition ve,, 3a5�G;, has
3) I`he degr~,e of decomposit:on d,e ends �'~ pheno~.,3,
p more ox~ the
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r j
ti~~~~~Y~~ ~.Ss j ~~'~?A~u'~~, ~..~� ~ ~~LYA~~~~~~Y~ p.~. ~ ~.i~~t.~+i-SI-I~`k~AI~T~, '~. ~.;
1yU~iCtOVS~ Y"f ,~ tz, ~. , ,
T~ARIfi431~t~.Y, L.Ya.; KF~3ASKOY, ~.P.; SH~YNMAbi, Yu,I~,; la~ifiRE'YS, I9,A.;
Y'~'SHIN, A.L.; Y~tSTAK, (~.V'. radal:~tor i~datel'stva; Ci1JROVA, O.A.
t;ekhnicheskiy xed,aktor
[fiectonic map of the U.S.S.R. $nd adjacent countries on a scale of
]~:5,000,04~; eapa.ana.tory notes fi~gktonicheekaia karts SSSx i
sopred�1'nykh strap v ~masshtabe 1; 5,OOQ,ObO; ob"iasni'tel'nsia
lapisks.. Moskvs:, aos. nAUChno-teklan. izd-vo lit-rv po geol. i
okhr�~ne nedr, 1957. 77 P. (~:C~ 10:5;1
'l. A1t~demiya nau~r SSSR.
(Rusela~..Geology__~,p$ ~
k
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r' cif the Paleozoic t~oc~,s of the ~outhwe:~tern trc~nt. }
mhe S tra ti. EsraP hY
UI as ~v_tr
U'I'bt~ '~eri�~ ~~v~
Bulgy;htarrr~~ Series C~t~
~'~rkG~an'sk~~~5e ~~rsj [,t,,e
~~
.4.. �a :i~ ~'~:
� .~

s;arcl, 5/~fi
Du~htArma diver
of ZubP~tk~a
I
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' k

1b-bri~bw~7b~
., ~ F ~ Soai.c~~re.i tern ~ -giant. )
The S Grab grsph~r of tk;~: lPaleoza is :rtoc~s o~ k~;A
autsi~:ie tt~Eis region. To the northeast along the strikE~, the section
ctaanges E~ssanti~:lly+ crv~arywt~~R~ra, along an extent of s~~varal
I~ilom~s tors, alrt~ost alb. tC~.n sadimon tart' farpnati onksoe ndt,ttuffaceousd
middle Tou.rnaisian give '~~ to volcanic flow roc and
.r:ateria~.. The authar.~ were able to trace 'she beds in detail,
they discovered, alan~ the bukhtarma rover ~ from the v.lllage af'
2ubavka tc~ the village cf Kandrat' yevka, e.cposur~es of laalcanic rocs
tha`c3 ~fr~~ ~~~~~r~l.~t.~.vea of lower and ~tddle 'i'ourna~aian ;pediment&ra
beds, referred kit' ~. ~. ~ul~:ll.ct~eE~k~a t:c~ thug l~evon3.an. Uuut~t i~- also
raised concerning the "Devonian" age of bed9ian wi thrt'zencl$ss~,cing
regions. A comparison of thQ described set
section of the I)evanian and Carboniferous in the valley of th� U1'bEi
River~~ is stxown in the figure.
Gard 4f6
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15-57-~5-5753
The St.ratigraphy of the Ptileozoic Rocks of 'she Sauthwes!tern (Crone. }
are also present: Rote orina altaica t�b'0 ~~3khor. find N.~kiforovelle
altern~ata Nekhar. , were `d~~verof the upper ha7~~ o~~ie~
xe_~;~na beds of the Ta.rkhanskaya series. Sandstones inter~~.xed
with t~.~ffaceous breccias (5UU m ~h.~ck) occur higher yet. A11 these
deposits, begtnning with the bed of tufface~~us brec:cia, are refarred
by the author to the Tarkl:xanskaya series, o:f lower end middle Tour-
naisian age. The Bukhtarma series (upper Tournais:Len} ~;onaists of
t~~ limestane formations s$parat9d by a san~~.stone ~�ormation, which
gives way southward slang the sartkoftthe lowerllimestonepemiddle
organic chore), In the lower p
Tournaisian S ~iri.fer cf.. sibiricus Lab., S. lit no us,, and ether
forms are st~p~resent. `A~iove~he zone of t1~sg` 4ipacies occur the
upper Tou.rnaisian Camarotoechia aff. Pcetzf Tolm. ]'roductus (Dic:tYo-
dQ c;t us Rom. anc~many bryozoans ; Fetle is eT~a ru~~~
clostu.s) cf. ~r ~ ~ a'n~ot~iers.
~"~'r, ; ~~. serra u~.a a hor . , F. bukhtarmens is Nak~.. ,
tipper Tourna s ati~fossila area so ours n~the up~7er limestone
f'ormat:,iori (the authors give a long list}, clay sh~iles, grading into
siltst.,one~f~ and s�~ndatones higher in t; he section, rest v~~.th apparent
~,onfox~mit;y on the Lukhtarma limestones. Tr,e age o.~ thaw shales and
coarsf:.r elastics has 'oeer~ determined to be lower V:Lsear,~ from data
Card _':~/6
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15-57-5-;a75~
The ~tratigraphwr of the Paleozoic Rocks of the iouthwe:~tarn (vn~;, }
Parphyri tee and rata ted to e1's with is cgrs of barnon s ~lliceous
shalels, occur in the corn o.C a :Large ar-tic,line. The tl~iickness ~idered
the beds reache:3 2000 m and the age has bel~n provisionE~lly con,
to bE~ Upper Devonian, I'he boundary betwee':~ the Devoni~~n and the
Carbc-niferous its drawn at the change from these basic volcanics to
a4id~.c types. ,4 seq~~encc~ ("~:~~ m thick} of tuffnceous lareccia ~Nith
unite of sandstones and rare layers of quartz keratoph,~res has b ec~n
assigned to the later period, No fossils have been fa:~rd. Calcare-
ous ~-iltstones (700 m to 900 m thick) occur above this sequence and
cont~~in poorly preserved. fossils, In the lower part, .S irifer. cf.
ostEjrus Hall, Productus niter Goss., P� cf� resets` riculuLs 1Val.
and ~ er forms have~eln found, indi cat~ng a lower troeungt age.
The middle part eo ntai rise the bryozoans Fenestella quadru___ll.~ N~khor. ,
F. c~�. tarkhancQ Nekhcr., and Rete orir;a a a ca (a, ., c, d} Nekhor.,
char~icter s c of the lower ha o e Re epor na_layers of the
Tark9~anskoye series. Occasj.onal brachiopods we a collected higher ir,
the s3ection. The siltsl;ones give way to limestones, which are inter-
bedded with sandstones and v~rhich contain numerous brachiopods;
5 ir:Lfe~;, lp atynot~us. Wel]~., a. sibiricus Leb. and others. Bryozoans
C~~
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'~ ,?, 1,
` ~ 15-57-~5-5753
` Translation from: Ref.'ertitivnyy zhurnal, C,eologiya, 19:7, PFr 5,
pp 6-'7 (~JaSR)
ATJTHOE~5 : F!e1' kova , L. N. , Ogne~: N.
~� Ths StratiF;:raphy of tt7a Paleozoic Rocks of the Sou.th-
TI TLE. .
western Altc~y (K stratigrafii paleozoyskik;h tolsrich
Yu~;o -Zapadn+~ go Alt aya )
PERIODICAL: F~.t;erial;r Uses. n.-i. gea].. in..ta, 1955, rlr 9, pp 65�-b9.
AF':STRAC`I': V. F. Nekhorostiev has worked aut th� s tratigraphi.r, sub--
division;~ for the southwesterr.~ Altay (MatE;ria,ly Vices.
n.-�i, ge,o.l. in-tai 1Lf~~, sb. E3). Ir, this plan a :large
place in the L�wer Carl~~ublichenkoehasocr~.tiacizedttheto
volcanic rocks. N. L� 1951 Nr 5)
clf~ssifi cations tlzv. AN SSSR ~ ser. geol. � ,
be:Lievin~3 that the volcanic activity in the southwestern
Al{~ay ceased at the end of thc~ Devonian. The. au~tilors of
thEr present paper describe a ,jection in the region of
th~~ vi Ll a~;e of Va si 1' yevka , in the lower ;reac;hes of the
Card 1/6 ~rui~htarrt~a~:ivor, that sheds 1:Lght on this problel~.
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~':x.,.,..,~;, ... ~ .._~ parr ;~~.~~_ .~1~~.~1~~,, I`~
1'1 , . ,
! ~~ i ~ { ~ j
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ACC NRc A P 6 0 l _-~ ~~-~~~ ..--
21b8 SOURCE {:ODE: 1JR/01~.13J~6%000/'OQ17 p :~
TNVEN~'t7g; Bryndiny V. G, -Denis / A� 5/0095
Old .......,,,...,.~.,....... ~...__....T ~~..,,., S �_,.._ ~v e~..�~,~ `,,_~,~' ' .~ ~~~.~.~~-~ ` -
G� Wane
'CITLE;
>OU12C,C
J.966, +'~~
~~
Sealing or coatin ~ ~~
R poraug materinll faith a carbon
~~
~ ~~
~.~o ret~:niya~ pr~~myshlennyyls obrezi~ay, tlav,~rny;re zn~akl
~ na. 7,
TOPIC ;TAGS: sealing, coating, carbon film
ABSTRACT: An Author Certificate has ef,
sealing; or co_ ~~~I~porous materials ~~ n issued de,~cribin
Cory materials, with a carbo~ 2 ~'m~k~~gaug~aoban- g a~ method of
g~,~e~~or refrac-
position of carbon containing ga$es. To speed of the thermal decom-
$ dense smooth surface, the work is carried out intaeflui~ess and obtain
graphite particles produced b ized bs'd of
bath th~a article being workedyonasndnthencarlyon$ agsases while heating
SUB CODpa; 11/ SUBM DATE: 2SJun64 8 e8, CLD)
Cardl/1
UDC: fix1,793,1k `
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i
t '�
' ACCESSION NR: ~~.P~009?8;~ - - - - - -~ , _ __.. _ _ _ _ _..
' less free carbr~~n and alysolutely~ no of-,Y'- com onents. Th -
Hated samples ~a~e:~e then .itized. F e impreg
nat3n mixtures not onJ:yy~aP~ It :I:s concluded that ir~preg-
elec~`~rode samp~.e~~ but ~tlsaiint~ract witracl'h~ks in the sintered
a greater e1ec~;r~.c resistivity and siren ;his.:nateria:~. resulting in
samples. In its impre~~atin~ properties tD:� B~th18`Vib~~tu~ ated-
proaches oil pitcch (pit~:h ,~. 5 to 1~~ anthracen� oily Daresently usad
for impregnation of elegy�trode materials. trig. art. Dias; 1
figure, 2 tables.
~, ~ ASStK;IATION: UD~.rtsvetmel; .Ukrainian nron-fel
rr�us DKetals~ j
SUD31~hTTED s QO DATE ACQ : lOFe b6
~ 4 ENCL: q~?
SUD3 CODE : CH ~1Dt REF ~OV ~ OQ ~
C~,'HBR s tDi~y,
,~ .~
hard ~~~ .. _... . ~.. - _ _..... _ .,. , .,,.
_..
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} ~.-~,
...s� .
NCCE~SSIt~N MR: A.P~Oa~71~;5
n
s/oo~5/~,~/o~QV/c~,~~~~?/~a~~
AUTH~~R3: V1.asenkc>, I. ~!~,. ; Qgn�v,~,tik,~. YK..
,,,.;.~
TITL~~: fJse of petroleum: bitumens for impr~s,gnating carbon graphit~z
materials
SQURt;;E: Khi~t~,ya i, tekhn+~logiy~>. topliv i m;~sel, ano. 1, lyb~., ~.7-5(~
TOPI{~; TAGS: carbon anode, car;~vr, electrodE~, petroleum bitumen, ct>al
tar ~~>itch substitute, ~;~raphite electrode xaanufacture
ABSTFI;ACT: Because the ],jLterax~,~ data is sc~-nt on the u:~e of petro-~
leum bitumens in.~,tead oj," coal tar pitch tc~ bind carbon when rnanu-~
factu.ring graphite elec~t;rodes, tests, were run with HN-~TII, B1J-IV
,and oxidized pe~wx oleum ~>itu~aena for impr�~~atiozr of c~-lcined carbon
~ sa~npl.,es of elec~cY~bde+ynat;erials.
The open tion consisted in heating
these' samples t~~ 300_5Q in an ~utoclave furnace um in the air
out f''or 30 min {P' bs=0 � ci kG/c:n ) , filling the autocla~'s with bitumezi
~ BNaIZYehing ft ~u~~er pressure of P ~~ kG/cmx f or ~ hours. :Bitumen
~ as a soi'tening point of 20~~~jC and differs from coal tar ,,
pitch in that i~; has more volatile ~ractiozxs bailing cut at ~+6QG,
~ ~a~d , ;1/2 _.
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s/oE ~ ~~/000/021/a~~/09~
8138 8101
AUTHOR:,{. Ognev, R. K. , Cherenionav, B. I.
TITLES Use of Irkutsk coals far coking
PERIOD2CaL~ Referativnyy zhurnai.. I{hi.miys , no~ 21 , 196 ~ , 39'7, abstract
z"~37 (Sb ~ "Pod gctavka 3. kc~ksovaniye u~,ley ~ Sverd:~ovsk,
f ~etallurgixdat, r,e~ 2,, 1964y 7789)
TEXTr The authors observe that the present prcoes~ employed :~'or i;he
coking of local Irkutsk coals without adding ether coals does not permit
'the crs~ani.zation of metallurgical coke productiono They preslant t;he
results of a systematic j.nvestigatior. cif the coals of three o:E the'
deposits in the coalfield. Cheremkhovo coals can only be use~~s irl
quantities of the rrder of 30 ~- 35 f of the charge, if the cha:cge i.s
rammed With the addition of fat coalsa Cheremkhovo coals ca~~ be used
for the production of nar,~matallurgical cake in quantities of about 80~.
If Novometelkina coals are used for the productian of metallurgical coke,
the amount of local coals in the charge can be brought up to 1~0~. For
Card 1~2
~~
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JOT ~Z-4,r-;- ~/ ~
At3..fI0R', OF;a~ev, R. ~.. T._..__._
..K._.--......------~..._~,.-. ~.
~. The Yolaro~;rr~~Y~a.a Dcterr-iA:~tita,on af' t:~e~Ad~ored~].erz~;~e{~F~,d~~a:ct~t.~:,io~--
TITLE.
Coal ~,nd Se1;~1,..Cr)l..e (F'ol;~~.ro~;z'ai'~.ci~eol.ofe Y
nod g~puQl)nJ5'tl u~ley i pQlul.ol::~ov)

i'1�;1tIC)DICAL: Zr+vod rl`~~yr:z L