SCIENTIFIC ABSTRACT FR:OFITSEROV, A.S. TO:OFENGENDEN, R.G.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001237800028-6
• Release Decision: RIP
• Original Classification: U
• Document Page Count: 1
• Document Creation Date: November 2, 2016
• Sequence Number: 28
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTR

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S//1~-3 1 ~r0O1/?~03/CQ3
A Continuous 9tee1 Teeming Equi};>ment ('~;--{~~(tINRS)) A00;~ A00
trol desk located at an altitudr:: of 6.~ m. exerts the contr~~~l of the gas cutting
process and the subs6quent proc~ldures and is equipped with �to].evisio~~ devices.
At present, the steel casting i~r introduced for slabs with +cross sec~,ion of v20 x
x 150 mm, 784 x 150 mm, and 1,Oi:"O x 174 mm with a productivity of up to }+5 t/hr,
..
Figure:
~w~
Diaj;ram of the outfit for
continuous te~eminF; of
steel (~!-~~J( (UNR;i))

Card 5/5
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s j1~3/61/ao~/oo 1~''~ 1 joo8
A Continuous Stee]'. Teeming Equipment (y ~f i~~ (UNRB)) AC~d~7/A(701
water is thrown a~'f from the .ingot by a spacial devise. ~`hi~ ingot ~~snt+~rsd to ~wh~
machine axis gets into they rolls of the pulling stand which is eont:rolledl hydr~nu�~
lically at 35-45 F~tm pressure dependent an the ingot arose ~ssetion .~.nd tY:is stc~ex
grade. The secant;ric ingot grab 11, arranged behind the p~u111ng stl~.nd arld irt~r_
locked hydraui.ical.ly with the pulling device, is intended for $upp~a~rting the in~.
gstt in Dees of hyd'saulia pressure drop in the pulling systerns. The a~rac~~etylene
auttsr 5 is fixr~bl.e to the ingot and outs the latter to slabs of mu;ltip].e~ lengthg ~
then it returns ix;~to its initial position; is controlled autornatic~~lly ~~y a phota.�
relay or by hand Frith the aid of a televisor. The cutting. gaga pressures are 15s
12 atm of oxygen ~~nd 0.6 -~ 0.9 at India . of acetylene . The iri~ot gists dt~~ring +~he
cutting into the r-eaeivin~; basket, is let down to the stop at the well b~c~ttana ara3
is then lifted by the inclined freak to the dragging devise m~~unted on this }~larx~,
bottom. The trane,port motions are automated. They internal s~eetion of the ou~..fit
performing the ink;ot crystalliz~~tian and the cutting is sep~ar~ated f~^om th,e ether
section of the well by thel bric:`_- ~*alls. In this part of thewell, a3pecial preven~
five measures are taken euoh gs shielding and intense oonditionirt,g. There are t~wr~
desks of machine oantrc~l end a ;panel with indicators of the liquid ~~ts~e7 temperaw
tore in t~~e teaming and intarn~ediate ladles, the ingot travt~l rata, and ~,he wa~~er
diseharpe i� the crystalli~ers ~~ th~a secondary cooling s.ystem~ Ttie ~~:canii con-.
Card 4/5
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A Continuous ~5tec~~. Teeming Equipment (~N~'C ~~)~ A1~15~~~0!)0/OO~,~p~)i,~'00$
When producing transformer steel, butane propane gas as prc-tecting mediuir~ is sup_
plied automatically at 1.2 _ 1,5 atm pressure thro
Th� gas prevents the oxidation of the metal surface and i:ncreas~ ei~hheavin13o~ore~,
face quality. E~'feative ,het protecting methods az~e not knc~~rn tads ~` la sur~
liter travel, up end down vertically far avoiding the hanging of thc~ ~inTo~lt c~rysta~..v
grades; downward it travels w:~th the ingot, upward it moves three times faster
and the crystallizer walls are greased automatically with heated li. uid ,~ara
whose prese~ure and quantity are chosen from praetiaal exp~eriences~ gThe c;,onsump~
tion of copper in th� pouring prooess is negligible. The initial ~thickne~lss of
the eoppor sheet crystallizer walls is 25 mm; because of the scrat,chess this wails
~'e regr:[nded two ~. three time~~ to thickness of down tc 1:! .. z2 mm;
thickness is ina~nissible because of the distortion of thss -~alls an,d .~~ni~.~~artio~ ~
of the needed ci`y~~tallizer geometry. Each crystallizer w~ltttstands usuall ~
casting of 3y000 .- 3,500 t steel. Chromium bronze is mar~r ~tear_resistani buts
cannot be applied beaauee ~t im~ai.rs the ingot surface quF~2ity, Frain the crystal..-
liter, the ingot E3ets into the :;econda eooli
distributed over i;he e'htire len; th of ~ ~ zone witY- the water spry;~-ers 2
charge amounts to 60 ~. 65 m3 !S 7 m of the liquid phase, The water ciis..
got aver the entire cooling z~capformavoidin itre roll aalapters 10 guide the in.~
$ s buCkliYl~;, and at ita~ enc;l, the
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A Continuous 5teei Teeming Equipment ~ y ~~I PC (t1~tS)) ROt};/A041
and the eccentric ir,IgEt grab 11. -The outfit 15 ~:la pd in the Plant ir. ~>.z~h a
manner that the process begins i~1 the tee~r;ing seeticn and the ready slabs r,;yx,+, in-
to uniform lengths ar$ delivered in the thermal see~.l.t~n. The total hi~ight of the
unit is 25 m, above the Plant gr+~und level 9 m, the rest i.n a special, we:li ,~ fihe
90 t-isteel teeming ladle $ is mo~uited at the crane above the intermediate :;ladle 7
having 10 t holding capaci+.yg its fettling is heated b~ gas up trs 11,00�C the
ladle is centered over the aryst!~llizers. An intermediate l:sdle is a~-piiefi which
distributes steel among two crys�tallizers far obtaining a constant rel,at.v~~:.lr I a~~r
ferrostatical pressure, a quiet ~1on-spraying steel ~et~ and a deerease~ ire ~~~he~
quantity of non -metallic inclusions. After filling up the in~:ermediate 1+f~cly.e
and removal of the s~toppera ~ the metal gets into the 1.~ m l+~ng cryst~,ll.iz Mgr made
of copper whose wall's are intensely cooled by water. The water discharge ~,Eor
cooli~�~g the crystallizer is cont;rc~lled in such a manner that the temperatui.e drop
be+.ween outgoing and incoming water sh .uld amount to 7 - $oC and the d.ischi3r~;e per
eryste,llizer to 2;YJ rr~~hr. The ,steel, gett.i~ng ante the erysta,llizer fills .~~p a
hallow in the primer head and the r~ntire crystallizer height fsrm~.r_g thrcl~~~h 'he
primer a sirt~le ingot 9 which is drawn downward by the pulling stand ~~ a~: ~~. rbaWe
in the limits of 0.6 - 1 m/min, Then the ingot is cut off by the gas cu ~~~~@Y' 5
from the primer head in such a manner that the latter can be used repE:ated:l.y.
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Yf
AUTHOR;
0~~'itserov, A,S~
~3/1!~3/61/Or~0%z1~~0 x~
~-00!~/A001
~_-'^ 9
PERIODICALt
A Continuous StE+~e~. Teeming Equipment { y ~ fir ~ ~) )
B3''ul.isten' tekhniko_skonomiaheskoy inf~ar`~tts.~sii, 196],y N~:s, .,1~ pt;s.
9 - 12 ..
TEXTr Th~~ continuous steel teeming equipment of 'the ?Jovoli et
A skf3r mEta,~
Iurgichesniy zava;i (Novolipetsk:ty Metallurgical Plant) waft d+~signed b
yekt" for the protiuetion of killed, rimmed, and transformelr :steel y f ~ St,al `pros
consists of two pE-rallel v~erticre,l machines at ~900Q ttuc~ distance and isedo~'tf;tt
ed by increased produativit istinguish~r/
pouring of Slabs of large crossl~lseetions $and$ per hour per one machine), the ,~--
Acoording tQ the dia ram each c, a high degree cif procelss aut~~mation,
g , f the machines consists cf the follflwing c~;;mponent.s�
the crystallizer 2,,, the rec:iproeating travel mechanism of i:he e s#~alli
secondary cooling ::system 2 over the � r'3' zer. ,, thQ
the device ~ blowir,ig away the water fromltheningotf the ~.ul~uid phase of h~,~ ingot,.
cutter 5, the recej,ving basket 6;, the basket telting meehanissm~ then' ne ~ �~,~ gas
the ingot delivering mechanism ~~~he intermediate ladle linE:~ tracks
g 9
Gard 1/5 7s the rerll ati,pter 10
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SUV/'1~4-58-5-5373
Translation from Referat;.vny;r zhurnal, Mekhanaka; I~5�s .
I~3r 5, P ~`~ I USSR,
AUTHpK: Ofitserc~v, A,S.
TTT'Z.E, ~'
The Us�~ of b;.started Analogs in Wave-�behavzor lnvesti atron
(Islcazhennyye~ models r rin~; caftentirr~c~s Llnavaidable o~~,~ ~ c
posszbxlxty of x�~7f~~~su~r3n~; c~xtrcrrxcil 5ma11 u,~, Irr to ii~l:~ rxx~
watt-r . l:tEa ~ `� Vf'~ ;lil VE'.r�/ ~}t,~tliq'r.
/ ~i.I~tC~ d2'f' ~l1,l~rl at! t~Va 51'3 y.
} tk ~r'Im('i1t8 tV
drrectian 1 ~ -p herein wateradc~p rsrand wav~e~ this
heights were ir~.:creased, and 2) eXp~'rrment~l wherein thy:, mode -
Gard 1/Z basin walls we.;-e alternately slopirrl~ and vertlr� r~ ~
al. 1 hr. rr,sults
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SOV/12.4-58-'1-'1675
The Dependence of the Sur.f.-ce t~Yaviness in a Harbor Basin ~cont.j
waves the use of impe�rviou~~a walls with a slope of 1:2 or i:3 is recon:l.m~ended,
and for gently sloping wave.~> a slope of 1:3, .A wall slope in ex,~ess o9' 1:3
cuts substantially rota the area of the harbor basin, vvith only a smal;i, iri-
crc~as~~ in t:hc w~sve,-cl~~t.7~p~n~; c~f.iyc.,ti.vc~r~css. It: -s lio~nl;c~cl out th~~t thc~ ~~nast
favorable type of surft:~ce w~~viness obtains when harbor walls ~~ontain la.rge-
~cale pores. The effect of :doping walls of either impervious gar coax:�sely
porous construction is lessened with the decrease of the relative widl;h of the
entrance mouth and also wi;;h the decrease in whe size oi: the harbor basin. A
recommende~,l arrangement of the ship moorings in a harbor with vertical
walls is giver. The conc:lu:~ions drawn o~7 the basis of t]~e exp~erimeni:s per-
formed on a particular model of a harbor basin are con~~idere~d qualit.ati,vely
representati~~e for any hartlar., but quantitatively so only for t'hase harbors to
whir.h the laws of similarit~,~ may be applied.
T3. Kh. G~lukhov-kiy
1. Harbors--l~lave charc.etera.stics ~. Harbors--1}esig~z
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SOV/1.24-58-7-7675
Ta-anslation from: Referati~,~nyy zhurnal, Melchanika, 1858, Nay 7, p 49 (USSR)
` AUTHOR: Ofits~erov, A.~~.
TITL~I/: The I)epe:nden~:c of the Surface 'Waviness in a Harbor Basin
upon the Type of Wall Structure Constituting its :[nner F'eri-
mete:r (7avisirnost' volneniya v portu at roda stenki, obrazu-
yushchey vnut:~enniy perimetr yego akva~torii)
FERIODICAI.,: Tr. C_,idravl. labor. Vses. n.-i. ia7-t vodc~snabzli., kan~~liz,,
giclrotekhn, sooruzh. i inzh. ~;idro~;eo:l., 1957, Nr ~, lip
5?.-73
.4E~STRACT: The results of laboratory investigations concerning tl~-e in-
fluence of` the ;~Ihape of the wall ~-tructure, on the wave re;;ime
in a harbor ba::,in are described. It is noted that the heit;;ht of
the waves in a harbor may be on the avea�age twicf-, as hil,h as
the originating wave and may attain maximum vali:ies of ns for Harbor 3asins
thE~ waves impinging oii the harbor structures, and 3J~ diffraction of tl7c
waves rcflectc~d by thc' breal:~waters. This energy either subsides on i:he per-
imeter of the harbor basin c:~r is e.~.i~ended on the form.at~on of surface rough-
ness in the harbor. The author points out that the magnitude o!' the w~~ve
energy entering a harbor m~.~y be reduced if the projection of th.e width of the
harbor entrance on the dire,~tion of the highest and most frequent waves is
decreased, anal if sloping, c:~oarsely porous wills are provided on the outside
of thr- pier, at: least near the pier hcad5. L~i~~l>ratory ire 19~~. The author
n�tes that ~~ to tY~e prese;.yt the isaline ehaz-~ of the rea.ative wave ?,nights in a
harbor basin way the only ~;:riterion for e'~1.uating the surfacer waviar,~ss in a har-
bor sud offers a method whel.ch fn his c~inian isc more re.Iiable name that of
the enr~rgy ChaxaCteristic 4'If the .stu'fetce ~avineres. A`Ca!~rding~ to ~1~3 rauthor' 8 eXM
~riments they, eve er.+~rgyr ~.;-enetrates ~.nto a hs~z~bor by r~r~~s of ~,~ th~i~ direct en~
try of waves, ~~ d~f~'rectic~~m of
Gard ~./~
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lz4-~ ~-z- 1940
Translation from R~~fe:~ativn~y zhurria, ~:~o};ha,nika, ~5i, :~r ~, p tssr~ (f SSRj
AUTHOR: Ufitserov, A.S
TITLE. Vtrave Inves,tigaticins in I-Iarbor Basins (Volnc~vyye issledoti~aniya
akvatar:iy i~ortov)
~I~:RItJI")I~~1I., 'I'r t;;iclravl. l.abc~r VsE 5 ix.-i iu-ta vodosnal~. lcanaliz.
git:lrotc~}~:}il'i s00'r.xzh. i inr.h f;idrogeo} 195r~, I\Tr ~z, pp ~ua1 A1rdnAtit~a��~d !R#. ~, Mil �
~'~ 1. I;) s,1~.; (/t+tMiiE (K'~ervaw), II>A!, 19, dttno, 7!'NI�rt%1i1. ~ ��
� ~ � ~ In o t~ r 1�frr~ m~Nfi+r~ mrirwr< iu�+.~tittutltulrt ut~ ol. t ~ �
� ~ t { f,~tn~r, ploy( ~hi~~Fr aMI n� th.~ir r~hj.Mt util(a:ing it l~- (-nahrrr
nl't(I!UtHrfl (M If It( Irillc~.i5>tii. :. P1. e
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Q ~ ,,~�~.� ; C1tUHAK~Y, N ,,.W. ; S.EidTSKIY, N.S. , akadem'.lk� glavx~q~- red. ;
TTTGOD:~SOY, D..S, , r~::d. tome; ~tS~i~ YEV, .A.9. , r+~d� to~ia; ~.UN, N.R. ,
red. i zd-vas ; ~STROY � ~1. Y. , red . i zd-va ; ~t7SEY.~, l�P. , te~:hn. red.
[TectonicP~ cf the 1I.S~S.E.] Tektonika SSSR. i~1~~v.red.tf.S.
Shatakii. Moskva. Yo1.4. [Tectonics and val+~ania pipe~a in the
central part of th+:~ Siberian Platform] Tektonika i vulk:anirheskie
trt~b?ci tae+ntra~.'no~i c'r~sti Sibirakoi plat~orm;~. [5trati~;rr~ph~ and
tectonics of the sl~uth~estern part of the Yil;~~;~ ~.o~slan+d] Strati-
r;rafiio i tektonik~~~ ittgo-zapadnoi chasti Yili7iiakoi vpa~diny.
1959 � 46~. P � (HIFf~ 12 :11)
1.Aicademi3ra nauk S~5SR. Geologicheskiy instit~st~,
(Ru>;}sian Platform--Geology, Structural)
(Russizin P'latfo:cm--Volcanoes) (Yilyuy I~ow:la:nd--(3eo].o~)
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C1n Volcanic Tubes of the Southern. Fert of the Siberiarl Plateau and ter `l'.g
Origin of Ir on Ores Associated 'Nj.th These Tubes
The plutonic, texture of the Krasnoyarovsk:aya volcanic tube is
shown with l3c~'iemati.;ed dett~ils in Figure ~.. The Krasnoyar~,fv~
skaya tube, as tl:e rrra~ority of other tubers, travc;rsee num�7^ous
crevices, which, are in all instances fil7,esd with basalt. ':the
Krasnoyarovl~kaya tulae represents typical forme of texture ~~f
this type. It has ~~reen proved that other known iron ore dle-
posits of tae AngarF~~-Ilim district are a;3sociated with vol~-
cani.c tubes. IVo se�; tectonic system can be established as to
the arrangement: of ~;ubes within a certain group or individual
tub~~e of each ~-roup w
There are 4 figures and 10 references, oi' which q are Slavic
!Russian).
ASSOCIATION: Geological Institut~:~ of the Academy of Sciences USSR, Moscow
. (Geologicheskiy lzre'~itut AN SSSR, &[oskva~
SU$MITTED: g Ma,y 1957
AVAILABLE: Library of Congress
Card 5/5
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u-10-~/~~
On Volcanic Tubes of the Soui;hern Part of the Siberian Plateau and on the
Origin of Iron Ores Associated ~Ni�th These Tubes
were also conducted 1~y a number ~f ether i.nstitutiong, among
which is the Cealogi+; Institute of the Acs~demy of Sciences USSR.
Based or. new da1;a, t'~ze former hypothesis cif the sedimentary
origin of the Arigara~~Ilim deposits, and treat they are associat-
ed with erosional depressions, graben or elimpl@I ruptures could
not be upheld. The author's contention treat the Angara-Tliro
deposits are associated with volcanic veins of the same type as
the Krivlyakovslcoye 3eposits is being gradually accepted. Be-
ginning in 1951-1953, the studies of the Siberian volcanic
tubes have been intensified. Tha rocks filling; the volcanic
tubes are mainly agglomerate or pyrite-like turfs of fragmental
texture (Figures 1-3). "1 he volcanic tubes of the Krasnoyarov-
skaya deposits contain blocks of agglomerates, similar to
"krivlyakitas", which contain, beaides angular and rounded
fractions of basalt enclosed in laves cement, :Large quantities
of foreign rocks, such as sandstones, tuffs, ti^aprocks, ma~;-
netit~es~and others. "Krivlyakites" are found only in the central
section of the Krasnoyarovskaya deposit, where they form ov~al-
Card 4~5 shaped blocks with an axis length varying between 50 and I1,0 m.
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lI-1Q-2,23
Volcanic Tubes of the Southerr7 Part of the S~.beri;~n Plateau and on tie
Or_
Origin of Iron Ores Associated 'N'th These Tubes
rocks of the Silurian period.. pdost widely
� the grabens among to whit;h the deposits
accepted were i;he d~aductione according '~rasnoyarov-
of the Angara-'[lim ~~istriot - Korshunikhskoye,
skoye, Kezhemslcoye, Rudnagorskoye and ether dt~gosits - ceriod
in contact with rocs of the Upper and Loner l.aleozoic p
on the surfaces of the ruptures,rWthehinfluencesofudepth e~n-
skarned to a certain decree unanriehed with ore. According to
crustation and simultaneously
Bogdanov~ich are of fun-
present knowledge, th� studies of K.I.
damental importance, insofar es thearea.tahBogdanovichldis~�c
origin of rocks of the Angara-Ilim Kezhemskoye and
covered that thiroyrroreodepasitsparentu,ffsy�and specifically
Krasnoyarskoye
effusive protrusiazie of basaltic magma. The author ciAes~ok-
several other geol�gists, such .nedNthe geologic structure of
torovich-Grebnitskly, who exami
The Irkutsk Geologic Administrat-
iron ore depos3it~ ~~f Siberia.
ion conducted systematic andth~tAastdye~arSpeCTheseostudies
Gard 3/5 Angara-Ilim deposits during P
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~ l-l0-2/2~
On Volcanic Tubes of
f iron Ores
the Southern part of
Associated '~Ui`,h These
the Siberian plateau arld on tYle
Tubes.
Origin o
� a result of ~,h�se studies, common structura'1 features were
As
cted to exist between the Angara-ilimA~~sed onet~!~e~ssfi~id-
dete
and the Krivlyakovskaya volcanic tubes.
the author and A. ~~
inga, the opinion was first eagitesof the ,fin ara-Ilim district
g It
Novikov that the iron ore d8p
are s,sgociated with volcanic forms iA trocksnNere noFetrap-
was established that, the metal-bear 8
or au ite-por~~hyrites, but fragmentaleT3lc~siS.A:cks.
rocks g other explcr ,
These views were nog, shared by
who is of the opj.nion that the Uc~lo-
Doktorovich-Grebnit.3kiy, Krasnoyarovskoye and Kezhemskoye de-
novakoye, Yermakovssoye, but are transformed SiJ.ur-
posits are not of volcanic origin, According tG these ti-iews
ian sandstones, clays and trap'rocks.
eologists support the opinionassociated~withorul~tur-
numeraus g
posits of the Angara-Ilim district are ,rocesaE~s of mine;cal-
es, in the cavities of avhich subsequent ~'
ion took place. Other opinions of this subject are t'7at
1. Zat
cks containing the aforementioned oresuskatxange~~hich fill
ro
Card 2~5 district are tuff-:tandstaries of the ung
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4� ' Y ~ t '^ r + , / i ~ l ~ tlf l^+, 1 1 ~ 7 lam.
AUTHOR; Offmann, P. Xe. 11-20-x/23
TI~'LE: On Volcanic Tubes o:.' the Southern Part of the Siberian P1a.teau
and on the Orin,-in o} Iron Orea Ar~sociated W~.th These Tubes
. (0 vulkanicheskikh ~!;rubkakh yuxhnoy chasti :~ibirskoy plgtformy
i o proiskhozhdenii zheleznykh rud, priurocriennykh k etim
trubkam)
PFRIOAICAL: Izvesti.ya Akademii tdauk SSSR, Seriya Ceologj.cheskaya, 1957,
/~ 10, ~~ 15-2~ (USSR i
ABSTRACT: In 195c!, volcanic tt;bes were discovered at i;ha Podkamennaya
Tunguska near the Ks~~ivlyaki survey mark, Thule tubes were
filled with tuff, and in several instances i:h~l tuffs were trans-
formed into skarns. It was found that thes~~ craters were as-
sociated with the ec.ge of a newly formed sirieclise (Russian:
"sinek].iza"), at thE~ forming of which thick layers of tuffs
were involved. On the basis of these data .it became apparent
that the pyroclastic material, of which the tuffs are composed,
were effused through. volcanic tubes, and that numerous such
tubes ~sre likely to be found at the periph�ry of the deep 3e-
pressions(sineclise). The author draw attention to the data
obtained at the studies of the boundaries of the Tur.iguska 'ba-
Card 1~5 sin, at the formation of ~-hieh volcanic rocks were i.nvolve~~.
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