SCIENTIFIC ABSTRACT YUSHKIN, N. P. - YUSHKO, V. I.
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SCIENTIFIC ABSTRACT
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hT
TISIHIUN
Ulay pebbles and teisir forrdition. Izv Voss geog ob.-va 96
--rio. 1:60-64 Ja-F 164. (MIRA 17-5)
of -eolt,-~y ar--l Mrs genesis of the Cct,:,,r--r nat,=adl
sulfur depoEit, Zap. Tadzh. ctla. 'loes. :aln. cbl-va nc.2,1123-131 164.
1, Gic-.moye upravlemilye goologil Ji. Okhrany riedIr pri Savete Ministrov,
SSRy Tashk-e-at.
YUSHKIN. N.P,
Mineral composition,of sulfur ores of the Shorsu deposit.
Uzb. geol. zhur. 8 no.600-38 164. kMIRA 18:11)
1. Institut, geologii Komi filials. AN SSSR.
SRE13RODOLf,liKI-Y-B-1--;--YUShl(I-il-j
0
Determination of the hardness of the native sulfur crystals of the
Shorsu and Rozdol deposits. Min. sbor. 18 n0-4:437-439 164. (MIRA 18:7)
1. Gosudarstvennyy universitet imeni Franko, LIvov i Institut
geologii Komi filiala AN SSSR, Syktyvkar.
YUSHKINj N.P.--
Reviews and bibliograpby, Biul. HDIP. Otd. geol. 40 noo31llO--Ul
MY-Jo 165# 1818)
YUSHKM, P.
WWWWWWOOKOW-W
New wnge system for sta6l workers, 10jats,truA no.8:1~5-88 M 156.
(Ja;RA 9:20)
1e Rachallnik otdala organizateii truda cavoda I'KrasW Oktyabrlol
Oteal I~dustry---Produatlou Standats)
YUSHKIH. P.
Choosing a working schedule in CO=8ctloa with. the seven-hour work-
ing day, Sote,trud .4 no.6:12i-i23 So '59. (WA 12:8)
1. RacbiLlInik otdole. arganizatall truia Stalingradskago imetallur-
gicbeakogo zavoda "Kraetqy Ok abrl.fS
(Rest perloZs
--- - - - -- -- -- ---- - -- - --- ---
~-YU K~3~ V.H., inzh.
.q~_
Training personnel to be able to perform duties of other crew
members. Rech transp. 18 no.10:54 0 1590 (MIRA 13:2)
1 1. Unland vater transportation)
I
YUSHKIII. V.T., insh.; SHOR, L.D. Inzh. -
Using suspension-bridge methods in ccnatructing river crossings.
Stroi. truboproy. 5 no.4:16-18 Aio 160. WMA 11:9)
(Gas, Ratural-Pipe 1 Ines )
0
VXILKOVSKIY2 A.S.; YUSHKIN., V.V.; hItUDYAKOVs 0 F.; SAVVINtAs Ya-D-
--------------
Conciso data on so me gas-condensate fields of the Soveit Union*
Trudy VNIIG" noal7:58-65 1629 (HIRA 15:12)
(Condensate oil Uells)
A.K.: VELIKOVSKIY, A.S.- YUSHKIN V.V.
- ----------
Selection of an effective method for extracting and separating
condensates based on reservoir and well head c6nditions, the comm-
position of gas., and transportation systems. Trudy VNIIGAZ no.17:
142-153162. (MIRA 15.:12)
- (Condensate oil wells)
Fit=
TOSMKIN, V. V.
ItThe use of the method of electrical modeling to inventigate the
temperatire field at the base oP a blast iurnace with a broken
and with an unbroken floor." Min Higher Education USSR.
11 Moscow,- 1956.
Moscow Institute of Sti~el ineni I. V. Stalin.
(Dis!;ertatlon for the Degree of Candidato in Tochnical Sciences),
SO: Knizhnaya letopis', No. 16, 1956
----------
mimary.-AAS YUMIN TV
0 256. QPA 9:10)
Gza comdozoats rosorisirs. Gaspirovi-AS-20:1-6
.- (0". Natural) -
I .
TUS
Studying gas condensate characteristics of the depo Isit of the
Stapnovskii, field. Gizoproma no*5;6-10 Ky '57. (KLRA 10:5)
(Ga's, Ilatural)
X
Al
X
AUTHOTI: Yushkint V. V. (Stalinsk). 24-4-27/34
of a,method of electrical modelling of the
temperature f leld -of the *hearth bottom and the foundation
of a blast furnace. (Issledovanlye metodom elektricheskago
modelirovanlya temperaturnogo polya 4shchadi i fundamenta.
domennoy..pechi).
PERIOPICAL: "Izv. Ak.. NAuk9 Otd. Tekb:.. Nauk.1 I (Bulletin: of the Ac~, Se
'
0156-161 (USSILi.
VacEnIcal Sciences Section), 1~157, Mo.49-PP
ABST*
PTt
With certain simplifying assumptions the heat propagation
I in the hearth bottom and the foundation of a blast furnace
can be described by the:Laplace equation in cylindrical
Ooordinatest eq.-(I)P- P-156. The Type I boundary condi-
tions are thereby the respective temperatures at the in-
"(1400 C) and at the surface o-' the
ternal hearth surfaods J.
d water V C)i the Type III boundary conditions are
gro
giv y t - rfa -ch
b he convective heat exchange at*the sa ces whi
j:
are water-cooled by plate*coolers or by thetoutside air.
The analogue of the-network of thermal resistance is formed
by" a network -of electrical resistances of the integrator.
.Detailed information,on the elootrical,modelling of thermal
13roblems -is contained it them. book of L.* 1. Gutemakher
T"Meatrical ModellLagll, Ac So., 1949). It is pointed
card 1/3 out that the change of the ihermal conductivity of the
materials caused b y the rise in the temperature of the
hearth bottom and the foundatiout which is usually
Investigation,of-a'method of electrical modelling of the
temperature-field'df the"'hearth bottom and the foundation
of-a-blast furnace. (cont-.)- 24-4-27/34
Card 2/3
disregarded, -may reach-25to-404. -In,addition#- the sbArp
inorease in the heat conductivity-in the spaceAbove the
isothermal surface-of liquid- iron: id usually alsonot taken
i jato' cons id6ration. A-method Is -desoribed-in wh1oh-Z-a
attempt is made to''oongider the charge In the beat conduct-
Ivity--of the -mat6rial caused- by the"iffeat of -high tempera-
turos.- First-a model,was'iriv6stigated-which consisted of
electrical resistances simulating -the -;.-t.hermal conductivity
of the'materials at:20.'C', --The obtained general picture of
the -temperatu3~e-'f ield was- thei! 'atilised- for calculating
afresh the resistances-in accordance-with the new values
of the hoat-conductivity and this'process was repeated
until the position of the isotherms did.not change any more.
Thust-the temperature-conditions-were investigated in the
centire of the foundation- and- also. along -the, radius; further-
more, the depth of penetfttioA'of'th6 liquid iron was
'rho here described~"m6thod-is-aoouxstep simplep
clear# flexibU andenables rapid solution of the prdbleme
andf'~ therefore,,"th6re- is: every 'Justift cation for it to ',
become the basic method of investigation during the design
of blast furnaces. The here described investigations were
Investigation of a method of.electrical modelling of the
-temperature field'of the hearth bottomand the foundation
of a blast furnace. (Cont.) 24-4-27/34
effected in the Electro-Modelling Laboratory of the
Institute,for'Precision-Mechanics and Computer Techniques
10.f the Ae'Sc-, USSR. G. K. Kuzminka gave valuable infor-
mationreiating to the execution of the tests.
There Are 8 figures, 2 Russian, one American -reference,
SUBMITTED: April 3, 1956'.
AVAILABLE:
~~Card 3/3
r
-Is Gat urcm no,3:4-6
Uondensate 10-9000 in gae-condensate poo
(nmfi. In-
-.9)
voridensate oil valley
. --- )/V S "-/ k- /'t~ V, t/,
133-9-3/23
AUTEOR: Yushkin, V.V., Candidate of Technical Sciences-
TITIZ: Me Use of Electric Integrator for the,Investigation of the
Temperature Distribution in the Hearth and Foundations of a
Blast Furnace. (Primeneniye elektri,cheakogo integratora
dlya issledovaniya temperaturnogo, polya leshchadi i .-4k
fundamenta domennoy pechi)
PMODICAL: Stall, 1957, Ro-9, pp. ??9 - 787 (USSR)
,-,-----.---ABSTRACT-:--- The paper describes an investigation of the thermo-technical
quality of various- designs- of -blast -f urnaae --hearths-using an
electric integrator of the -3K-12 type. The investigati-on-w-a-s---l-
carried out under the direction of L.I. Gutenmakher, Po(tor of
Technical Sciences in the electro-modelling laboratory of the
Academy of Sciences of the USSR. no.1 blast furnace of the
,_Kuqaetsk Metallurgical Combine (M) was chosen as the object of
investigation. The scheme of designs investigated is shown in
Irig.l. Principles of application of an electric integrator are
outlined (Figs.2-5). The methods of investigating temperature
distributions for various designs of hearth, refractory materials
(chamotte and carbon),various degrees of the wear of lining and
cooling conditions are described in sope detail. The distri-
bution of isotherms in hearths of various designs before and
(;ardl/4 after the formation of a bear hole 3 500 mm deep is shown in
133-9-3/23
The Use of Blectric Integrator for the Investigation of the
Temperature Distribution in the Hearth and Foundations of a Blast
1furnace.
Irig. 7; calculating scheme for the Inve8tigation of temperature
changed with the growth of bear hole in the hearth (Fig.8).
Temperature changed alonS the axis of the hearth are shown in
Fig.9 and temperature changes along the hearth radius in FiS.10.
The depth Of Denetration of liquid iron for various hearth
designs is given in Fig.11. On the basis of the results obtained
the following conclusions are drawn: 1) the height of the
hearth should be not lower than 0.40 - 0.415 of the height of
the foundations; 2) hearths with carbon layer below a chamotte
layer, or below a chamotte layer and on the periphery are the
most efficient in decreasing the temperature of the upper part
of foundations and secure a minimum penetration of liquid iron;
3) hearths with a carbon layer only on.the periphery have a
somewhat better temperature distribution than chamotte ones but
advantages are-rather-small; 4) hearths with a carbon layer
p1t4o'�d on top A* well aa wholly carbon-lined have the highest
6 - , tho 14PJ4P pormi.paible for
temperbttLrt~d at tho ba 61 C;X-060ding
concrete. The distribution of temperatures in the d6&bon heoxth
even with a ring oi a complete underhearth cooling is less
Card2/4 advantageous than that in a chamotte/carbon hearth with a lower
133-9-3/23
The Use of Electric Integrator for the investigation of the
Temperature Distribution in the Hearth and Foundations of a Blast
Furnace.
or- -lower and peripheral carbon layeri, 5) wholly carbon hearths
unlike all others are unstable (the-rate-of their wear in -creases
with increasing depth of bear hole) and therefore require careful
control of their erosion; 6) it is necessary to attain a relia-
ble fixing of carbon blocks and meticulous filling of seams
between them,.as the depth of penetration of liquid iron is
larger than the thickness of the blocks manufactured at present;
?) the bottom peripheral cooling is of great importance for
lowe7i-ng the temperature of the bottom of the hearth. Under-
estimation of the influence of this cooling can lead to large
errors in determining the depth of bear hole; 8) the investi-
gation confirmed the correctness of the view on the primary
importance of axial removal of heat for &creasing hearth tempera-
ture; 9) lower carbon layer intensifies the axial removal of
heat; the influence of this layer is approximately equivalent to
the action of ring-like underhearth cooling; 10) in order to
improve thermal properties of wholly-carbon and combined
carbon/chamotte linings, the production of carbon refractories
should be such that a maximum heat conductivity is obtained in
Card3/4 the -longitudinal and a minimum in transverse directions.
133-9-3/23
The Use of Electric Integiator for the Investigation of the
Temperature Distribution in the Hearth and Foundations of a Blast
Furnace.
In conclusiont the author remarks on the incorrectness of the
statements made by F.I. Loshkin and G.P. Moshkin (Stall, 1956,
No 2) that the best temperature distribution is obtained in the
Mrth fully-lined with carbon blocks and cooled on the periphery
and the bottom. The present author's results indicate that the
depth of penetration of liquid iron in the hearth with a combin-
,ation lining with carbon blocks at the bottom, or at the bottom
and on 'che periphery decreases with increasing depth of the bear
holewhich should lead to stabilisation of the depth of the hole.
In the carbon hearth the depth of the hole increases continuously.
There are 11 figures and 4 references, 3 of which are Slavic.
_ASSOCIATION: Siberian Metallurgical Institute (Sibirskly Metallurgi-
cheskiy Institut),,-.
AVAILABIS: Library of Congress.
Card 4/4
Idlt--
YUSHKIN, V. V., Cand Tech Sci (diss) Ogethods of G- gas
V,06, 1958. 15 Pp
and gE~s-petrole= deposits Qjij-' gae conaenBability-" 110NI
ietrole=-Gas Sci Res In8t), 110 copies (KL,
V31LIKOVSKIT, A.S.; A:RUTMOT, A.I.; Yu=;~v V*V.
Irperience in low teoperature separation of condensate and water
ont of gas from a gas condensate field. Gaz. pro=. to*5:19-14 YT
'584, (MIRA 110)
(Gas, Fatural),
TUSHKIN, J,
ing Samnies from gas-condensate wells. GOz. PrQ=. so. 7:4-6
J1 '58. (Coudensate oil W6113) (KIRA 11-7)
V. V -
UZI
3
till,
i
..53 Ag
a 4
s w.. R1
aa
a iills
1111all a
va
uush
gig
1g o.5 ;1 "-
fj
i
&A
2v ~A
a
.71 1 ji
vzLiKovarr, A.q., samm, Ya, D., YusEam, Y.Y., UOYAKOTs OPP.
studying the potential of the Leningrad gas-condensate field,
Gaz.prom 5' noo2WI-8 7 160. (min 13.-6)
uban-Condeneate oil wells)
I
,jKjjj, Va.
JV,UIQV, A.K.; VFLIKO'ISYIY, ~-S,; Y'JS
ior, of condensates from gas at gas-corden-
Processes for the extr-3ct 7 no.1:15-20 162.
sate fields. Gaz.prom.
(Condensate oil wells)
v.OYTS-ITSKNr V.P.; YUSHUN, Me
Otion of condensate
Siv,dy, of cortdkroblaml in th* produ 1 162.
_tllo __~hebajjbka gtia floldo a,,z. prom.7 no.310
4v
YUSHKIN, VGV.; IUWDYAKOV) O.Fes, SUVADCHAK, N.S.
Investigation of the gas potential of the ga3 condenvatit p-ools
of the Bitkov field. Gaz. dalo no.12,11-13 163. (MIRA 17xIO)
1. V.-.esoyuzayy naualmoo-issledovatol Iskiy institut prirodnogo gaza
i Ivano-Frankovskaya tsentralInaya nauchno-issledovatollukaya labora-
toriya.
YUSHKIN VV KHUDYAKOV -0 F.
.Phase trangfomrations of the reservoir fluids of-thie gas-
-Y *or North field when it
condensate bode of the Ruask,' -Xhu'.
is developed by pressure reduction. Gaz. prom, 9 no.113
6-9 164. (ICP_k 'L7-.-L2)
VELIKOVSKIY, A.S.; SAVCHENKOP V.P.; SAVVINA, Ya.D.;,TY~HKIN, VOV.;
ZYKINP M.Ya.-
in a gaa COndensate layer
Prediction of the petroleum fringe
n of formation gas* Gaz. prom. 10
based on the compositio
noo91l-6 165. (MIRA 18111)
u -s1 ~ T-1-1 I -V.V.; SAVMIA, Ya*D*
rlebovo gas-conden0ate flOld, Voft. i gaz. Prom, no.4141-43
(MIRA 18*21)
O-D 264
YUSHK]Ilf V.V.;- SAIMPA, ya.D. I
Nature of the producing horizons of the Russkiy Uu+.or Central
gas field. Gaz. delo n0-9:3-9 164. (11,aRA 17:-L--')
1 1. Voesoyuznyy nauchno-iosiodovateliskiy institut prircdnogo gaza.
YUSHMp-V.V.; SAVVINA, Ya.D.
Estimating the reserves of stable-condensate and ita recovery
factor. Gaz. prom. 9 no.70-n 164. (KIRA 1788)
I
I SAVVINA, Ya.D.; YUSHKIN V'VG ---
5 the,Glinskoye-ROzbiahevka field for gas condensate.
Investigatinj prom, no.2j41,47 Ap-Je 164. (MIRA 17:9)
Naft. 1 94%*
~V~5 '000/0 310099 '0'9-)
A
4
-"'~t ejector
nr- 2 - movable
n-lece, 3 control
it
7,3~-.-!anism rod; 3teiunary
!,.-zle-n- -;e 5
oaded
pac n g.
Card 2/~
YUSIIKRIP-yu--I--
)Pment of health prolu,e~~tion in Ibrdliais, dLiring the ---Lastv-
sl.,,kn Y.U, "The de7eb sk 194'
1
1;11 19 k nauch. trudov vrachey Mordov. ASSR, Saran 01
30 ea Sborni
7 r5
pp. 3-33.
SO: U-326i, 10 April 53 (Letopis tZhurnal ln~~ Statey No. 11, 1949)
YUSHKIN, Tu. I.
YMO(KIN, Tit. 1. #On tho diagnoois And troatment of functioma ham0raloplal. Sbornik nauzh.
-trudov vrachey Mordov. AM, garanalt, 19140, p.50-61, Dibliogi 11 Its-mr.
SO- U-3261, 10 April 53 (Letopis - Zht=nal Invkh Statey No. 11, i9o)
133 1. SCIENTIFIC AND ORGANIZATIONAL BASIS OF THE CAMPAIGN AGAINST
TRACHOMA, AND ITS LIQUIDATION IN THE USSR (Russian text) -
Yushkin Yu. I. -SARAN
'SK 1956 (152 pager.)
A short rev1-e_W__orTH_e_Frstory of the fight against trachoma in pre -revolutionary
Russia and in the USSR Is presented. At the end of the fourth 5-year plan period
fresh forms of trachoma were almost universally extinguished. General morbidity
of trachoma Is now greatly reduced. At the beginning of 1950 the trachoma morbidi-
ty in the Mordovian ASSR (Autonomous Socialist Soviet Republic) had decreased by
87%, in the Marii ASSR by 03%, in the Chuvash ASSR by 92.1114, in the Udmurt
ASSR by 81%, 'in the Bashkirlan ASSR by 83%, and In Tatar ASSR by 7274. The
organization of the campaign against trachoma, in the Mordovian ASSR is schematic-
ally outlined. The details of the work of trachomatous rural nursing units, and the
organization of the work of rural medical sectors and regions are thoroughly dis-
cussed. The organization of the fight against trachoma in the former Ismael region
is outlined. A special chapter is devoted to the discussion of Soviet ophthalmolo-
gists, achievements during the last 20 years, The author proposes a new method of
reporting the trachomatous patients according toathree-stage system. Theauthor's
opinion on the 'inechanism of repeated follicular.expressions in trachoma to laid
out. (S),
~MMMMO IE-77ER*F
SILPILIBNRG, G.I., keni.med.nauk; TUSHKIII T
u kand.med.nauk, vasluzhemVy
vrach RSFSR; ROMA, V.G-ziwe-S--9-a4T,"
Timely problems in the development of local health resorts. Trach.
delo no.12:1329-1331 j) '57. (HIRA 11:2)
1. Ot4aleniye organizataii kurortov (zav. - G.I.Shpillbarg)
Ukrainakogo institute kurortologii.
(UCRAIVE --HFAIO!H RMORTa, WAMING PLAUS. FITG.)
YUMMIN, Th.I.; KOMIA, V.G.
Organization and work of the receiving department of a sanatorium.
'7op.kmr.,flzloter.j lech.fis.kallt. .25 no.1:67-69 160.
(KM 13:5)
1. 1% Ukraiuskogo instituta kurortologli (dir. A.T.,Sokolov).
(SAIWORIMG)
Lagnosis Of female goll"rheasit'
V. toThe probUm Of &" 19481 p. 2-63-72-
assk, un-tap Vol. Is
Trudy, mede fak* KOM t
In loithuanian., Russian abstrac
No. la 1949
SO: U-2888# Letopis Zhurnalinykh StateYs
MMAR
JUSM A.V. assiateut
0
in trichinosis* Zdrav.Bolor. 3 :6)
]glee t rocardlographic Chlll3gl3l3 (KM 13
no,lot42-44 0 157-
1. Iz tafedry P3ropadsvtlkl v=trenuiktk bolezueY (zav- - Prof-
I.D Klehouln) miuskogo gleditstookogo instituta.
jTRI09M AS TRICHIMS'S) (MMIMARDIOOUPHT)
cO -y
YUS'HKO, A.V., Cand !.~ed -ci (diss) 11r, Lchinosis
Fr
-Mbmj*t~o Pinsk, (16.nsk Statl!l Led
Inst) 200 copies (FL, L2-58i 119)
- 73
TUSHKO. A.T.-I
Case of repeated Infestation with trichinosis. Zdrar. Belor, 5 no,10:
1 72 0 '590' (MA 13:2)
1. lz-kafedry gospitalluoy terapil (zavedWushchly - prof. G.Kh.
Dovgyallo). (TRICHINA AND TRICHIROSIS)
YUSHKOP A.V.; VOLKOV., N.F.
~~~ viii-i
Characteristics of the course of trichinosia. Zdrav. Bel
8 no.6:63 Je'62- (1URA 16:.8)
1. Iz goopitallnoy terapovticheskoy kliniki (zav. - prof.
G. Kh. Dovgyallo) 14inskogo meditsbiskogo instituta.
(TRICHINA AND TRICHINOSIS)
YUSELKOI A -7-.
rarly -ohloroalar.- Zdrav-. %le 8 no.11:84-85 t62*
(MMA 105)
1* Iv kafedry gospitallnoy terapii (zav. prof. G.Kh. DDVORnO)
Hinskogo meditainskogo inatitutaw
(CHtORCSIS':)
C -APIOG?6181 ~~W(rii36/66/11:M~/002/0064/0061-ii
8WRCE COPE:
j;AC
UTHOR: 'Kormer, B.; Yushko,,'K B.; Kirshkovich, G. V.
AU
P; none
04
4?TITIE: Depvndenc~ of the rerractive index on the density of the solid and liquid
)Ppreade dionic dryetalse He
Tphase 6. of - shock-ci laiatidn time of phase transformation
under shock'compressibn
S.OURCE: Zhurnal.. sperimntallnoy i teoraticheakoy fizikio Pialma v redaktsiyu,
-64
Y. 3, no. 21. 1966p -49
TOPIC TAGSi bionic crystal, rofractive indox, alkali halida# comproadon ahock wave#
shock wave,fiont
ABSTRAMi The, ref active indices of shock-compressed alk~ili-halide compounds were
investigated. F UF,-which remains transparent in the investigated range Of
uO to P 700-kbar, the refractive index was determined directly from the
pressures
paths of~the rays n the compressed matter. 'For flaclp CaBr, K01,, and KBr crystals#
which becom, opa" behind the shock-wave front,, the refractive indices were
determined by...Fre Is. formulas from the experiment ally-maoured coefficients of
reflection,~6f. nat light incident on the front of the shock wave. The dependence
of the refractive'- Wex on the - degree of dompre asion et (where q - p1p is the running
the'denaity at T 390,0K ano PcwO) Air the arystale I, Wit and
I cam 5 IJDC: none
7
-ACC NR. AP7007678i 7-
statecharges the refractive index by about 1.5 timep more than in the'solid state*
Investigating she reflectivity of the shock-wave front in the aoUd phaaft of KG1
KBr it was nd,e.d that at P -z., 140 k~ar the rorleotion coefficient to 2 tidne
'N olithlor thmi that corrouponding to A rolAtIon of tAo type (1) for n(w), with Valwon
"df dn/& that fol Low from whereas at P ge, 200 kbar f or K01 and 260 kbar for KOr the
ne -close to
~obtai d resilts those expected. We recall (see Sees 1 and the tabl:e)
AWA for other c tals the results of the measurezaants were-in satisfactory agreement
with earlier data "is n ur o re e e Im c e rence e
~~RT:~K6rphic trans 'ormation of KC1 and KBr into the CsG1 structure, which occurs at
P =20 kb kbar t6 phase transformation of KC1 and kBr
ar assum.ng that uY to P < 140
occurs after a tij ib.,r > 10- 1 see, ~Iw. light will be r eflected from a layer of matter.
situ'atedo'n the font MP
-of the shock wave in a ~tastable state (point 1, Fig. 2),
aoritsponding to. he dynamic adiabat of the first phase 6). Since the 3-atter is I
steeper-than the, - a of second phase# a smaller density jump on the shock-wave
4ion~ corresponds also to a smaUer refractive index. The non-equilibrium states of.
AY16 --flebt "phase ~ o KC1 and Or (Point A F. g. 2),, deteradned- from the shock-wave
th dependence (1) with d"n/'d-a as given in the tables and from the
64"uAd r6flecti6n coefficient,, are:shown in Fig. 2.9 For K01 the point obtained
'i16's- 1-6666what tolthe left of the first-phase adiabat calculated from the equation
'of state 4'~ 'With increasire pressure#-the temperature increases (for El. T = 1300.OK
,at P = -136""kbar afid T - 2100'K at P - 200 kbar), the relaxation time decreases, apd
fhe_ phase -tr&nsfoi-mation -takes placed in a- layer, thinner thanX-/21C (;L-wavelengt1i ~~_ -I
of the indident Ught)* In this. case the refractive index will correspord to the,
Card 3/
ACC NR, AP700767~
total jump in volume behind the front of the shock wave (point 21, Fig. 2).
Considering that the values of dn/do obtained for pfiase II turned out to bd
close to the valt es for phase I. the measured reflection coefficients were close'
,to those expectec. Thus, upon shock compression with P - 200 = 260 kb the
Ilymorphic trant ition in K01 and KBr takes, place within a time T . Mri, sece
e polytorphic rans ion, nterestings has no effect on the n(cr) dependence of.
these ionic c als.) The same time is characteristic also of melting in the
J shock-wave front, since the refractive index (reflection coefficient) experiencaq
a jump at presswes corresponding to the transition,of the solid phase into
i~ liquid (Bee Fig* 1). Orig. arte has: four formulas*
SUB: CODE: 20. SUMU DATE s 01HO65. ORIG Ws 005.
0TH *REF:, 008
Ck~d 5/5'"
.:14, 3
AUTHORS;
TITLEs
PERIODICAL:
25335
S/020/61/138/006/011/019
ao" B104'/B2_14
Zelldovich, Ya. B., Academician, Kormer, S. B., Sinitsyn,
M. V.j and YQshko, K. B.
An investigation of the optical properties of transparent
nubote.nceo at ouperhigh pressures
Akademiya nauk SSSR. Doklady, v. 13,8,-no. 6, 1961
1333 - 1336
TEXT: The propagation of strong shock waves in transparent media permito
to study the properties of substances at pressures of some thousands or
millions of atmospheres (Zelldovich et al., DAN 1229 no, 1, 48(1958)~
At pressures not too high if the compressed substance remains transparent
throughout its thickness the refractive index may be determined geometri-
cally. The authors first studied water, plexiglass, and glass. A diagram
of-the-experimental-set-up-~!ith which the reflection of light by the
T
.-shock wave can be determined-) is diidwn :fn~ The- ref-looted -rays
it --V were raawrdod 11 y a fast photochronograph * Water was found to re-
maln 411(10- prvo~ltir~3n of 09 -'144 tholoand atmoophorea. Glues
becomes opaoue at a pressure of 200,000 Tho Oknut vqlto~"
Card 1/5 - -
25335
S/020/61/138/006/011/019
An inveatigation of the optical... B104/B214
for water are collected in Table 1. in the discuarAon of the reaulto
the authors used the data of V. Raman and K. S. Venktaraman (Proo. Roy.
Soo-, E-1, 137 (1939),)and gave the following relation for the temperature
and density depondonco of the rnfraotive index% n - 1,334 + 0-334(~-')
- 1.90.10-5T3 (1), T being in OC. Fig. 3 shown graphIcally ti comparloon
of the values of n calculated by (1) with those determined by geometrical
methods~ The dotted line in this diagram corresponds to the Lorentz -
Lorenz formitla. The deviations of the results obtained photometrically
can-be-partly-e"I~ained by the increase in viscosity of water at high
pressure. L. V. Allishuler--(Ref~ -6)-had--detected a decrease of the
o" the reflected light at pressures above 15-000-atm--and----______
O"A--.it-l-to.-"-b-e~--r,elated tlo.t4e~ phase transformation at this pressure. This
effe-ot-cou-ld not- be -de t ad ted:-by them-- pro's eat athom--They are of the
opiniorL that water remains transparertt: up-to -360M0- atm-4-Ao-G. Oley-niki
V. 11. Mineyev, and R. M. Zaydellare mentioned. The authors thank V. P.
Arzhanov, G. V. Krishkevich for carrying out the experiments and A. G4
Ivanov, R. M. Zaydell, A. G. Oleynik,and V. N. Mineyev for valuable
discussions. There are 3 figures, I table, and 10 references$ 5 Soviet-
Card 2/5
25335
S10201611138100610111019
An investigation of the optical... B104/B~14
bloc, and 5 non-Soviet-bloc.
SUBMITTED4. March 30, 1961
Fig. 1: Experimental set-up.
Legend: I)jncident ray. II) -and III)
light reflected from the stationary
boundary between plexiglass and water.
IV) light reflected from the front
of the shook wavo,V) lipht roflooted
from tho moving bounAary between
compressed water and compressed plexi-
~A rA LT
glass. 1) plexiglass prism. 2) cater
in front of the shock wave front. 3)
water compressed in the shock wave.
Card 3/5
A P L
J.-
105 3
i o v i a A c a i c a q Kormer S
5 it il. e V L C rl Yushko, Y
T TLL u J v 0 n C 'I e 5 M 0 0 t 'I e F a 4CLOnatLor, front tn a I t u i d
9 6 4 , 10 5 1 - 10
3 a v64 da tonat ion , ,,a ~onatlc"
j 77 1" t., 1 . 11 r a n t r. r o D a g a t i r-~ L V, a S C t
ri ~i L t e r I -- a r - 1 c n r o e h
ane mixture was S t ti d i C j
1 1 17 9 n -I j e e J f r OM the detonation ano qci~Do7k
-I! a - v. e t r --j o e x -i I o -; i. v e mixt,ire was
e', C u V 12 L r. e s a t I c r a c t with an organic gi a a s
r c f r i: c e d E, x, e i c ri n a i d e r a b I v from that of
2
C e. d e L
o, n a
:i ed v t h a
50/50 trotvl-h-~!x-
g t fn tf. f) r1 B P :I -P. 71 i Am a t e 1. A de tonatfou ve~
a r C!
A P -
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s v (-, t (.
, r., 1; 0 't C, 2 c Comparison of the re-
e L 0 n a t I tj g h o w 44 t
q m, I r r t-, r - Lt k c- a 11 d w a i r# h a r p -
Y d e n e a on c u 0 d R t o i c 10 m e t r i c 11)
'10 - -d i c 11 1 D-
o 4-1 d n v e 1 9 0 b t a i n e d w i t ei a p I a n e
0 c L- z- i? 9 ~e e ac o
-and th8t inhomo?eneitte,3
W. OU u JL it i a re au a in e4nrraet tn ~revleuv fIndfrigg by DrQ -
m t -in r r; n v .4 :n 1 1 1', o i-n -3 0 1 ft i t i e. s 1 11 t h e
A S
SUB CODE A
"i 0
),)0 ATD PRESS 31
W.F.; ROSTOVTSEVA*
%ta or, tho 9trntIgr;!Ph.*p IW40100o AM A01"d Of T011"Int AIA
lower Visa sediments in the Tatar A.S.Se-A. Trudy V914A no.14:
224-244 159. (KM 12:10)
(Tatar A.S.S.R.-Goology, Stratigraphic)
~M IS tR M
-iUSHK0 L.A
New data on, the distribution of peridians-in the central regions
of the Eurcpean Part Of the U.S.S.R. Mat.po geolA pol.iskop.
tsentr.raic,n.evroP.chasti SSSR noe5:98-101 162. (miRA-16-.6)
(Foridinjidael -Fogoil)-
YUSHKO, H.0 zaslushannyy uohitell alkol HSISR 06zhitaa); OL .ISHEVSKAYA, T.
-MAShitca)
Use of self-~madp models in solving steraccetric problems. Hat. v
--sbko--l-e-- no-.-6als~-16 N--D (KLRA 7: 11
'54.
(Kensuration)
MOROZy F4G.; YU.SHXO# M-14*
Foamed conaete roof slabe for industri&1 buildings. TranaP.
atroi. 12 r10#,;',: 52 MY 162. (MIRA 15;6)
1. GlaViomr tekhnolog + Dneprotranastroy (for Morov.).
westa
2. Ilachallnik tsentrallnoy laboratOrii trOst-DIlOProtranastroy
(for YuahIVD) .
(Lightweight concrete) (Roofingy Concrete)
MA MsL__ firle-matraempatt e -
OMPAt
jvia*seq~" by, K.~ candjdi~,e of:*dlcal
~U.Cqrtainlz~w-D_ _ - ~ - -, A~Jma $ ~Z, - . .
c e- _- --V.--_, - e - __~ Fhe Tr6f, N'0, T* 0 C_
i nces, (11mir of Sy. Dlseae7s a4, iiaO'6~akajii) i
S
rubjw Mcdjj!al jnatitute,~ Vestnik Oftalmologi IN 31 May/ju~a
pp 37-39
Twenty-aix~tran4PU$iona were administered to 10 patients. ranging from-
A-- i:oviov of-th# uatc-lrioo ~or tho WX p4t,teato. ItIdIcatgo that
ifitt-UrAdrWil b1loA trarofuslotij t6ntributed to improved local sympto=s in
-the eyes. As it result this therapy had a beneficial effect on nine patier-tz
Vhose eye sight beca~ue zwre acute, regardless of the severity of the diseaae
during which the transfusions were administered.
Yu. A. Dykhno points to the signif icant, stimulating effect of
intrasternal blood transfusion and its greater effect-as compared with
iiatravenous blood tranzfusion, regardless of the smaller amount of blood
transfused.
The admiuistration of heterogenous blood into the extremely sensitive
receptor zone of the-sternum had a more pronounced effect than the usual
ti~nsrusiont
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4-42(i
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1935
434)
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The Karpushinskii cOpper and zinc dePOsits in the Central Urals, 1936. 110
(49-432054)
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The methodn Of studyinf, ores under Microscope and by reflected light .2.
dop. i perer. izd. Moskvap Gos. izd-vo gaol. lit-ry, 1949. .2;oa p. (-,C-P5379)
QE-3611. IA
1. -Microscoi)e and "Ticroscopy. 2. ores
13 3 92
.1 , ~I, ~)NT 41
F-11ASE I TREASURE ISLAND BIBLIOGRAPHICAL REPORT AID 645 -- I
BOOK Call No.: QE389.5-I8
Author: YUSHKO,-S. A.
Full Title: NEW 14ETHODS FOR MINERALOGICAL SqJDY OF OXIDIZED ORES
Transliterated Title: Novyye metody mineralogicheskogo issledovaniya
okislennykh rud
.PUBLISHING DATA
Originating Agency: None
Publishing House: State Publishing House of Geological Literature__
bat,~: --1953- Not pp*:- - 48 116 of,- copies.. 5,060
Editorial Staff:. None
PURPU3E: This booklet is recommended by P. Postnov, Chief of the
Technical Administration of-the Minintry of Geoloeyj au a manual
for workers In mineralogical-petrographical laboratories and for
surveying parties and expeditions.
TEXT DATA
Coverage: This is a short booklet which gives to the mineralogical
prospector the information necessary to identify by chemical means
the presence of some metals in the oxidized (hypergene) ores. It
should be used as an auxiliary manual for a portable field labora-
tory chemical kit. It explains the-spot method of ore sample
analysis, chemical reactions forming color films on mineral surfaces,
1/2-
Novy've metody mineralog'icheskogo isaledovaniya AID 645
okl, lennykh rud
the imprint method of using some reagents on a polished mineral
surface and then printing its impression on photographic paper,
~and-finally,, the microscopic method of,.1dentification of minerals.
Tables, charts, photos and color pictures supplement the text.
No. of References: Russian 27 (1937-1951)
Facilities: Moscow Oeological Prospecting Institute im.
S-A Ordzhonikidze.
2/2
YUSM, 3,A,; PXR MI S.S., ra&&klor; POPOV, N.D., takhalcheekly rodaktor.
r
clkv methods In the Mineralogical study of oildical ores] NoVe
astody ulmoraleglahsokage loolodavamila *klsl4ivyft rud. lsd.2-so.
- 1. - ~ I Kookvs,, Gesonauchao-takhm. ltd-ve lit-ry po pol. I oklueze itedr,
1955. 52 P. -*--,- -- - . - - - - ---. - - - . - - - (KIRA 9:6) - - - -
(Mixoraloff, Datermizative) I
-- --- -YUSMCO'--S.OA#;.-- BORISHANSUTAS S.S**, SPMIYA, R.I., redaktor; GUROVA, O.A.,
Ituffifficheskly - - --- ---- - --- - --
[Tables for the Identification of minerals in PlIuvial sands] Tablitea
diagnosticheakik'a priznakov mineralov v shlikhakh. Moskva, Goo* nau-
chno-teMm. izd-vo lit-ry po gsologil I oWnrans nedre 1.955. 59 P.
(Mineralogy, Determinative) (HIBA 8:5)
-- - . -- 0 &
. 11. :, I. . , - " ,
T'- ~l " : Cri + 1 't --" fil q,711 Q 41 r%?) ~F-ArPAIM MnCWR On ErurUULUrCZ5 RM bt;AxUl---Zl VA vl~i?
All IJOAZ-. 5--l ; imeays~- 1. van ll;~ -z - z- - -- - - --. ... .
ISAYSM, K.P.; TUSHKO, S.A.
NAtlas of. ore stractUres 8-ad t~XtUr"s*.* 5.1. Taldykim,
11.1. Goncharik, G.N. Ralkeava, B.B. Rains. R"iswed by
M.P. Isaenkoj S.A. iUKko. Izv.Aff'SSSR. Ser.geol. 21 no.9:
li~-116 S 156. (MLRA 9:11)
1. Yoskovskiy geologo-razvedochnY7 Institut im8ni Sargo Ordzhonikidze.
(ores)
AUTHORi Yushko, S. A. 5-6-25/42
TITLEt Mineralogy of the Lead-Zinc Mineralization of the Karatau
Range (Mineralogiya avintsevo-tainkovogo orudeneniya
khrebta Karatau)
PERIODICAL: Byulleten' Moskovskogo Obehchestva Ispytateley Prirody,
Otdel Geologicheskiy, 1957, # 6, P 139 (USSR)
ABSTRACTs The mineralization is represented by the three main types
of orost ingrained, otreak-ingrained and aggregatives By
the shape of ore bodloa# the mineralization ia divided into
blanket deposits (ingrained and streak-ingrained ores)t
crossing zones (streak-ingrained ores) and lens-shaped vein
bodies (aggregative ores). More than 50 ore-forming minerals
have been discovered in the ores. The primary minerals are
as followst galenite,, sphalerite, wurtzite, pyrite,,mareasite
chalcopyrite, chalcosine, tennantite, sulvanitet freibergite,
argentite, native silver, cinnabar, ankerite, dolomite,
calcite, quartz and barite. Cinnabar was detected only in
the Terekty deposit in the form of relies in the oxidized
zinc ores.
AVAILABLE: Library of Congress
Card 1/1
Geochemical characteristics oflead-zinc ores in the ram-Tau.
Izve vyoo ucheb* save; gool, I razv. 2 no.2-.076-90 7 159.
(MIRA 12: 10)
lAbskovskiy goologorazvodoohnyy inatitut Im. S. Ordzhonikidze.
Kafedra poleznykh Jokopeqemykh.
(Kara-Tau--Lead ores) (Kara-Tau-Zine ores)
Qualitative mineralogical characteristics of principal tMe
of ores In Kara-Tan lead-zinc deposit. Izv.v7s.ucheb.zav.:
gool.i razv. 2 no.5:87-97 MY 159. (KIRA 12-.12)
1. Moskovskiy geologorazvedoch institut im. S.Ordzhonikidze.
-(Kara-Tau--Mineralo97r
Basic mineral associations and their structural features in
the-Kara-Tau lead-zinc deposits, -Izvvysucheb.zav.;geol.
i razv. 3 no,2 -.77-91 F 16o. (IMU 15: 5)
1. 14oskovskiy goologorazvedochnyy institut Ordzhonikidze.
(Kara-Tau-Mineralogy)
YUSIOM, S.A.; IFAHTOPULO~ T.N.
Cinnabar in oxidized lead and zinc ores of southern Kazakhstan.
Trudy Mine muzo no*U%23.1-214 161, (la-RA 16:7)
(Kazakhstan-Cinnabar)
YUSHKOI S.A.
sulvanite-in zinc-lead OreM Of the Nara-Tau. Trudy Min. muzo
.no.32-.215-219 161o (MLRA 16:7)
(Kara-Tau-SulVsmite)
complex- m-e-tal-d it Ar -e-
epos 5 L ,-'M yal a--
-Tau. Trudy MGRI 371:102-lo7 161. (MIRA 15:1)
(Kara-Tau--Wulfenite)
YUSIIKO; S.A.
Lead and silver minerals in lead and zinc ores of the Kara-
Tau. Izv. vys. uchebe zav.; geol. i razv. 4 no.1:25-40 Ja 161o
(14IRA 34: 7)
11 Moskovskiy geologorazvedochnyy institut imeni S. Ordzhonikidze.
(Kara-Tau-Ore deposits)
YUSHED, S.A.
new genetic classification or textures and stracttwes in ores.
Sov.geol. 5 no.2:100-121 F 162& (MM 15:2)
L.Moskovskiy geo3.ogorazvedochnyy institut imani S.Ordzhonikidze,
(Orea-Classification)
tiALKIN,_I.bf.,-kand.te.khn.nauk; ALBOROV, Z.B. gornYY Sep?
inzhener-mekhanik
If4proving, boring, with ainkar dirlla At the lAntnogorak Combine.
Gor.zhur. no.3:36-38 Mr 060, (MM 1415)
1. Laninogorskiy polimetallicheakiy kombinat.
(taL4it Keiia~dwtwi-lavvince-Rock driLls)
riw inzhener;.,P 0 -P-P
Zj B, , go
Recent dervelopMentis bY ths SPecial-design section of the Lenlno-
gorsk Combine, Gor. zhur. no* 5:7-* -72 bly 161. (MM 14:6)
1. L-eainogorskiy kombinate
(R oak drU3A)
ALBORDV, Z.B.; YUSHKO, S-P-
Drilling opqrations in the mines of the Leninogorsk Combine. Vzryv.
delo no.46/3:139-149 161, (MIRA 15:1)
-I (Leninogorsk region (East Kazakhstan Province)-Boring)
ALBOROV,-Z.S..; YUSHKO, S.P.
New machines for drilling deep slim holes in hard rock. Vzryv.
delo no.46/3:150-160 '61. (MIRA 15:1)
(Rock drills)
LEBEDEV, I.I.; YUSHKO, S.P.
-an Vachine
--Min-.4ng- and, ore -dressing-.eqiApwn4' of the Z-astg-azakhst
Manufacturing Plant., Gor.zhur. no.209-61 F 64. (MRA 17:4)
L Glavnyy inzhener Vostochno-Kazakhstanskogo mashinostroitellnogo
zavoda (for Lebede-.)*, 2. Glavnyy konstruktor Vosto--hno-Kazakh-
stanskogo mashinostroitallnogo zavoda (for Yushko).
TUSHKO, T.L.
Re inforced coz=ete slabs for crossings. Put, i put.khoz. 4 no.8:
25 Ag 160. (MIRA 13:7)
1. Nachallnik distantaii Puti, stantsya Apostolovo, Donetsko7 dorogi-
(Railroads--Crossings)
(Reinforced concrete construction)
YUSERO, T.1. I
- F
4~llast looseners for tie tampers. Puts i put.khoz. , 4. no.10:16
0 160. ' .(MIRA 13:9)
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