SCIENTIFIC ABSTRACT SHCHEPOTYEVA, Y.S. - SHCHERBA, M.M.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001548820007-6
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: March 14, 2001
• Sequence Number: 7
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

SHCHEPOT'YEVA9 Ye.-S.; ARDMHNIKOV, S.N.
Utilizatioh of natural radioactive isotopes at health resorts
and in other conditions for therapeutic purposes. 'Med.rad. 5
no.6:3-11 160. (MIIRA 13:12)
(RADIOTHERAPY)

TRETIYAKOV, A. F.; SH~HE~P_WYEMA--S-; FRENKUKH, Kh. G.
Tre--",MenI- of chronic eezemp, with radioactive bandages containing
.7). -lest.
active substa-ces of thoron decay products (alpha. the:---p
derm. i ven. 34 no.1:35-41 Ja l6o. (MIRA IJ.:12)
1. Iz radiologicheskoy laboratorii (zav. - prof. Ye. S. Shchepotlyeva)
GosudarstvennoRo nauchno-issledovatellskogo instituta kurortologii i
fizioterapii (Lr. - kandidat meditsinskikh nauk G. N. Pospelova) i
Klinicheskoy kozhno-venerologicheskov bollnitsy imenj Korolenko
(glavnyy vrach A. I. Pustovaya),
(ALPHA RAYS-THERAPEUTIC USE) (ECZRIA)
(THORIUM-THERAPEUTIC USE)

SHCUEPOTlYLVA, Yo.s.; ARDASIMIKOV, S.N.; LURIYE, G.Ye.; RAKINUNOVA, T.B.
Specificity of the manifestation of oxygen effect under the action
of alpha rap. Izv. AN SSSR. Ser. biol. no.l,:642-652 Jl-AF, 161.
(MIRA 11,: 9)
1. TSentralInyy institut kurortologii i f.izioterapii.
(ALPHA RAYS-PHYSIOLOGICAL EFFECT)
(PHYSIOLOGICAL CHEMISTFY)

F. 17
Trt-- a tm-erit of s c! y: ra" Oa-t!
bandages., ontaining zi anive coatirg C: ~'.Ugnt'er U.'ro-JU2113 cf
I
Lhoriuir (alphatheray
1. Radiologicheskaya laboratoriya (zav. - prof. 'le.l.
I -illnogo institu a kurcr L
"'3entri t' tologi, I fJ.z!olerar,4i (jir. Kand.
.m-ea. nauk. G.N. fospelova ).

SHCH&PTEV, N.F.; YUZE21AYA, Ya.A., redaktor; MELINIKOVA, N.V., takhrodaktor.
.
[SquIpment of peat enterprises and its care] Oborudovanie torfianykh
predpriiatii i ukhod z& nim. Moskva, Gos. izd-vo mestnoi promvshl.
RSFSR, 1954. 216 p. (MLEA 8:5)
(Peat machiner7)

BEZZUBOV, Nikolay Dmitriyevich; SOKOLOV, Aleksandr Alekseyevich; SHCHFMV,
N.Y., rodaktor; VORONIN, K.P., tekhnicheskiy redaktor.
[Winning chunk peat with a MPDK machine] Dobycha kuskovogo torfa
mashinoi RPDK. Moskva, Gos. energ. izd-vo, 1955. 95 P. MRA 9:4)
(Peat machinery)

GALYBIN, N.A., inzh.; inzh.; KOLOTUSHKIN, V.I., red.; LANGE,
V.I., red. izd-va; MELINIKOVA, N.V., tekhn. red.
[Organization of fuel depots] Organizatsiia toplivnykh skladov.
Moskva, Gos. izd-vo mestnoi pronqshl. RSFSR, 1955. 210 p.
(Fael-Storage) (MIRA 11:7)

SLiGHEPT1,1. N F
N/5
735.
jaz 4
TCTFOFIL.-'DFF.IYATITY I TCRFOEPIKETNY-KH ZAIOKO'V
(FA'.'Dl-CC'K FCF, THL NLCHA!i!IC; D PLAT AND PEAT I-RIQUETTE FA(;TCRIiiS) 2. IZD.
ISFE. i DOP. MOSK-1A, ROSGIZ-~,E,-TPI--(X-1, 1955.
4?1 P. ILLUS. , DIAG~,-'. , TABLES.

BEZZUBOV, Nikolay Dmitriyevich; SOKOLOV, AlekBandr Alekseyevich; SHCHRPTEV,
N.F.. redaktor; LARIONOY, G.Ye., tekhnicheskly redaktor
[The KDN-2 block peat machine] Dobycha kuskovogo torfa mashinoi
KDN-2. Moak-va, Goa. energ. izd-vo, 1956. 68 p. (MIRA 10:1)
(11'eat machinery)

SHCHEPTEV, N.F.
Trends in the development &ad mechanization of the peat industry
tinder the Ministr7 of the Fuel Industr7 Of the R.S.F.S.R. Torf.
prom-33 no.2:28-31 156. (Mlak 9:6)
l.Glavnyy inzhener Glavnogo upravlaniya torfyanoy i. briketuo7
promyshlonnosti Ministerstva toplivnoy promrshlonnosti RSIPSR.
(Peat machinery)

SHCHEPTEV, N.F.. lnzhanar.
.. -I..
Use of the PK-3 loading crane In nonalectrified peat diggings. Torf.
prom.34 no.1:37-38 '57. (MT-RA 10:2)
1. Miniateretvo toplivnoy promyshlennosti RMMR.
(Cranes, derricks, ate.)

nc re as 1. ng t
the fuel f.- R. Y, S.
RSFSR.
Peat

SHCHIMAV, N.F,inzh.; VOLOTSEOV, S.I., red.; LAHOROV, G.Te., tekhn. red.
-----
[Mechanization of heavy operations at small and middle-sized
peat enterprisesJ Nekhanizatsiia trudoemkikh rabot na torfo-
predpriiatiigkh maloi i srednei moshchnosti. Moskv3, Gos. energ.
izd-vo, 1958. 70 p. (MIRA 11:12)
(Peat machinery)

SHCHEFTEV, IT.F., inzh.
Modernization of small peat-winning excavators. Torf. prom. no-1:29-32
158. (MIRA 12:12)
l.Gosplan RSFSR.
(Peat machinery)

SHCREPEEV, N.Y.
. -1.
Developments of the manufacture of peat briquets. Torf. prom. 35
no.3:23-26 158. (KM 'A.-5)
I.Gosudarstvenny7 nauchno-,tekhnicheakiy komitet Soveta Ministrov RSFSR.
(Peat) (Briquets (Fuel))

6i,CfU~FTEV, -,-.F., inzh.
t;-156 uni7ersal excavator. Torf. prom. 36, ro-5-31-12 '59,
(MIRA 13:1)
l.Gosu~4.arstvennri'nauchno-tekhnichoskiy komitet IZSFS'~.
(Peat machinei-7)

SHCHEPTEV, N.F., inzh.
New -machinery for the preparation of milled peat fields. Tor-.".
prom. 37 no.3:7-10 160. (M-IRA 13:9)
1. Gosudarstvennyy nauchno-tekhnicheakiy komitet RSFSR.
(Peat machinery)

SHCFEPTEV, N.F.1 inzh.
Techniqu-e of the peat briquet production. Torf. Prom. 37
no. 3:16-18 160. (KIRA 14:1)
1. Gosudarstvennyy nauchno-tekhnicheskiy lomitet RSFSR.
(Peat) (Briquets (Fuel))

SHCHEPTEV, N. F.
New equipment designed by the technical design bureaus of peat
winning and transportation enterprises. 13iuI.tekh.---kon.iaform.
no.7:21-22 161. (.MIRA 14:8)
(Peat machinery)

I
SPCIF,_ PIFI-N I - -
Over-all 7--C-112ni7ation ol winning cut peat operations. Biul.tekh.-
_,~ -z-:27-15 '~1.
-kon . tn`~-,rm ... . 1 4: 9 )
(Peat machinery--Technolopical in--ovations)

t~,l V ,-" . I* ~
I -
Iric.rovi-ji, ~he equiL,.rnF:rA ir, peat-briquettJng enterpr-ses. 'Hui . tEk h -
~,kon.inforrq. no~11:1~'-13 ' 6.1. (MIRA 14:12)
(Peat machinery)

Si7CHEPTZvI N.F.
Present state of scientific research and experimental works on the
utilization of peat in metallurgy. Torf. prom. 38 no. 3:35-37 161.
(MIRA 14-4)
(Peat) (Metallurgy)

jJIGIIEFTOY N.F.
In the State Scientific and Technical Committee of the
Council of Ministers of the R. S. F. S. R. Torf. prom.
38 no-4:35-36 161. (MIRA 14:9)
(Peat induatry)

SIIIC~E PTEV, N.F.
Seminar on better equipment for Russian peat briquet factories.
Torf. prom. 38 no.5:36-37 161. (MIRA 14:1-C)
(Peat machinery)

SHCFEFTLV, N~F,
Over-a-U mechanization of peaT, transportation and handling~
0
Biul,tekh.-ekon.inform. no,1:16-19 162. (MILR-k 15-2')
(Peat machinery)

SHC ~:,!.:I 1,11, -11, , I" i".
!-jrWl D i 20A t,ri of* ;i Br- I Lnt.i f* I c cc) unc 11 f*or rver-a I I lit I I i za Uo I ~
,)f peat !irid T),-ut, deposlts~ fiitil,tekh.-okon.inf*orm.Gos,riaucI , -
- I ,
4S.q',2-nst,naur,h,i tekh.Inform. no
J.70-71 162. (AURA 15,.',,)
(Peat industry)

SHCREPTEIV, N.F.
The BPD-l (2) peat-briquet double-die press without a bed. Biul.tekh.-
el,-on.in,-rorm.Gos.nauch.-issl.inst.nauch. i tekh.inform. no.7:10'-18
162. (MEU 1r,;7)
(Briquets (Fuel)) (Power presses)

SifuEPTE'v, 11.
Prospects of peat utilization in metallurgical plants.
Torf.prom. 39, no.,4:37-38 162. O-EFJ~ 15:7)
(Peat industry)
j
(Coke)

SHCHEPTEV, N. F.
Production of peat-moss litters and peat-mineral-,wmoniae ferti-
lizers for agriculture. Biul.tekh.-ekon.inform.Gos.nauch.-issl.
inst.nauch. i tekh.inform. no.10:55-59 162.
(MIRA 15:10)
(Fertilizers and manures) (Peat)

SIMEPIPEV, V,F. (lloskva)
Private on conatant watch. Zdorovlo 7 no. 5:32 My 161.
(IIE'DICAL CARE)
WIRA 14:4)
t

'j 40
0 0 0 0 0 & a * 0 * 0 0 0 0 0 4 0 0 0 0 a W 0 0 0 * 6 4
,a
ea ~ I I . .6 . '. ; .1 .
. . . 1111.11.1.11 1- " P. J, 12 a M M . !, IS 1. V ft
V I t 6 11 j 4 L a h F 'J I .,VJ V-1 I I I AA ft LE LV It, k 4
IC t(c- ID rEY VN 00
00 -00
00 SA B 64 .00
00 q
67. . CALC"I.Arl~ 14 vF rtfi: )"A :NF.rC SYSIEM OF AN KLK--'TRIC -4141
C 'TT % -, rCOL -ELECTS C S PAR~ U rFX
;.1 .V.N. Shcheptov. Flektrichostvo ~66
0 0 No. F) 26-3,-, June 1960) In R,tssfan. -00
*0 The atithor deals mainly with thq6olen.lid drive which Provid0 the vlssft~ -00
00 Pie movement t ontrnl '00
-rkirir mov.-ont or the spark olectriAen. I
according to the varying elactrxi* :pacing durli!g the cn~i so of oper
0* to atior
00 and shoAd be kept -orstant an far as possible. A furth-wdifficulty is
00 j teriation of the oporating current, which again depends upon the electrode J~ 1,06
60 3ri-t-r. The solon id curren6 can be derived orly from the pporat _ . z :0 0
00 current (this being the only po3-ible meann of automatic regulsticn). ~jo 0
60 -urt~.*r difficulty rosides in the aquare-law rolnior between the attractive! 990
00 forin f the solonoic and cirrent. and the !a rand,%nce ,)f t~n force on the :0 0
the core. 1he theory has anaLled the existini- x6thed of electrt' .0 0
0 #
0 -rarnotid control), (o-je t- Livshitg nnd P.N. .4ooentb?-I) to be improvied.1
C !.F. Kraus
tio 0
Do
SITALLVPGK4L LITINS?LRt CL.SSIFIC.T.C. z
U
i*0 ':' 1:1 " " 1" -0 0 0 0 0 0 0
0 a o 0 0 0

vil'Mcaul OV) V.; SHCHERB, A.; YURIN, B.A., red.; KOROBOVA, E.D.,
tek.hn. red.
[The trade unions of Cuba; collected articles, addresses
and materials] Profsoiuzy Kubj; sbornik sta-Lei, vystuiDlenii
i materialov. Moskva, Profizdat, 1963. 166 p.
(MIRA 17: 2)

SHCHERB,K, A.
Lida oncounters. Rab.i sial. 36 no.1:12-13 Ja 160.
(MIRA 13:5)
(Lida--Industrios) (Woman-Employment)

ACC NRt
ARG0350G1 SOURCE CODE: UR/0058/66/000/008/HO02/HO02
AUTHOR: Shcherba, A. M.
TITLE: Frequency conversion in p-n junctions
SOURCE: Ref. zh. Fizika, Abs, 8Zhli i
REF SOURCE: Tr. uchebn. in-tov svyazi. Mi-vo svyazi SSSR, vyp. 27, 1965, 55-60'
TOPIC TAGS: frequency conversion, pn junction, spectral distribution, amplitude
t
distribution, nonlinear capacitance. nonlinear resistance, active componen
i reactive component
ABSTRACT: Spectral amplitude distribution of voltage combination components in
a p-n junction is analyzed for the case when its equivalent circuit under frequency
conversion conditions may be represented by the coupling of nonlinear capacitance
and nonlinear active resistance. Expressions for cophasal and antiphase modula-
Lion of the active ajid I-CiLCUVC COLDPOnent of juiictiun total conductivity are derived.
[Translation of absLi-acL] [DWI
SUB CODE: 12, 09/
Card 1 / 1

ordena Lellina

KOV I I VIKIH~l f!'"I"i, P..; .; .,"if" iii. i-(, i-1. ; .;
V.T.
Hiarnosis of -Iumz canc-.r ana 111-vcess. Vop.onk. 11
no.1-L.-3-7 161. (MIRA 19,1)
1. iz krifeci-Y pospital'noy klhirurgii- (zav. - 1~turpal, f--m,-r,.src,)y
pr-mii, AMN SSSH, z~ts-lu--.,~if--Y)nyy deva~pll riauki,
IHSMP Kallesnikov) ordena 'L.-r-'ra
nk.,idemli lmv!ni S.M.Kir'(~Vfl,

SHCITMA, F.I., POGOREIKO, I.P.
Use of an electro-ohoretic method with streptomy-cin and An athetics
.an treating tuberculous and trophic lesions of the bladder. Sov.
med. 18 no.9:3?-33 S 954. (MLRA 7:11)
1. Iz fizioterapevticheskogo otdeleniya (zav. - prof. V.A.Ivanov)
i urologicheskoy kliniki (dir. - prof. A.P.Frumkin) TSentrallnogo
Instituta usovershenstvovaniya vrachey na baze Klinicheskoy ordena
Lenina bolunitsy Imeni S.P.Botkina (glavnyy vrach - prof. A.H.
Shabanov)
(BLAD M , diseases
trophic lesions, electrophoresis of streptoMrcin ther.
& anesthetics)
(STREPTOMYCIN, therapeutic use
tuberc., venal & trophic lesions of bladder, electro-
phoreiii)
(ANESTHSTrCS, therapeutic use
same)
(TUBERCULOSIS, RENAL, therapy
anesthetics & streptomycin eleotrophoresis)

SHCHMA. F.I.; KOGAN, S.A.
A method of inductothermy in the treatment of diabetic polyneuritis.
Sov.med. 21 no.5:109-112 My 157. (MLRA 10:7)
1. 1z fizioterapevticheskogo otdelaniya (nauchnyy rukovoditell -
prof. V.A.Ivanov) i andokrinologicheskogo otdaleniya (zav. - N.I.
TSyganova) Moskovskoy gorodskoy klinicheskoy ordena Ienina bollnitsy
imeni S.P.Bbtkina (glavnyy vrach - prof. 1-N.Shabanov)
(DIAB.NTES MELLITUS. compl.
polyneuritis, ther., inductothermy)
(FEVER TWUPY. in various dis.
inductothermy in diabetes mellitus)
(POLYNEURITIS, btiol. and pathogen.
diabetes mellitus, inductother.)

e z
lioszva, 1949

1. SHCTERBA, G. 11.
2. US3R (6oo)
4. Rocks, Igneous - 'Altai :.fountains
7. Concerning the article "Magama of small intrusions of the Altai." A. P. Nikollskiy.
Reviewed hy G. N. Shcherlba. Izv. SN SSSR. Ser. geol. No. 2, 1953.
t~
9. Monthly List of Russian Accessions. Library of Congress, Aoril 1-953, Uncl.

S -` 1: - 1 :- A i 3 . I I- .
"Experience aai-ie,.-L in-die Stut- of the Iriter-mll Contacts of the CiranJ-ite
Hassifs", Iz-.;. An Kazakh SSR, Ser. Geol, 110 17, 93-104, 1953 (Kazalchstani-
resume) .
Usi--ig certain S-ran massifs of Central Kazakhstan and Alta., as m
emunple, the aut'Lor -eneralizes the facts which arc the proof for the di-
v,--i--,e a.~-es of the rocks of t,-.e rxu~sj-f: presoric(~, of sharp cont;jcts, chanZe
of structure Of you-C-er rocks inoontacti-ith older rocks, nonconformity
of-die elements of prototectonics, gradual contact, intersection of lines
E,
of contact. (RZ~Pjeol, 110 5, 195,41). SO: S=. 110. 443, 5 Apr. 55

SHCHERBA, G. N.
I'Vulcanic Cupola of the Region of Leninogorsk," I7v. AN KazakhSSR, ser.
geol., No 18, 42-49, 195h
On the baEis of a
canic fornationS in the
prcposes the technical
the unique structures occurring
and partly disjunctive deformations
study of the structure of dislocated Devonian vul-
region of Leninogorsk in Rudn-,vy Altay, the author
term "vulkanokupolall (vulcanic cupola) to designate
as a result of the imposition of plicative
on primw7 cones of stratorulcanoes.
KhGeol, No 1, 1955

SfICIMRBA. G.N_
Fine-grained granites of certain massifs of Central Kazakhstan.
Izv.AN Kazakh.SSR.Ser.geol. no.19:146-151 '55. (MLRA. 9.8)
(Xazakhstan--Granite)

15-1957-7-9176
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 7,
p 54 (USSR)
AUTHOR: Shcherba, G. N.
TITLE: Deep Mobile Zones of Central Kazakhstan (Glubinnyye
podvizhnyye zony Tsentrallnogo Kazkhstana)
PERIODICAL: Izv. AN KazSSR, ser. geol., 1955, vol 20, pp 52-59
ABSTRACT: Five geological structural units are differentiated
in central Kazakhstan, characterized by distinctive
structural features during the period of their develop-
ment from Precambrian to Mesozoic time. The author
considers the central anticlinorium extremely impor-
tant; it can be traced through Precambrian outcrops in
Yeremantau, Atasu, Mointy, and Bulattau, and it sepa-
rates two regions of different tectonic form and ore
mineralization. The structural development of central
Kazakhstan was controlled by deep mobile zones and by
Card 1/2 the mosaic pattern of the basement associated with

Deep mobile Zones of Central Kazakhstan (Cont.)
15-1957-7-9176
these zones. Mobile zones do not always appear at the sur-
face; for the most part they are distinguishable because of
elongated belts of contemporaneous intrusions, which may be
traced for hundreds of kilometers. The deep mobile zones are
divided into four age groups: early Caledonian, late Cale-
donian, early and middle Variscan, and late Viriscan. The
occurrence of widespread mobile zones may be used in predic-
ting endogenic mineralization. A map shows the distribution
of several deep mobile zones of central Kazakhstan.
Card 2/2 A. L. Knipper

SHCdFabA, G. M.
Geological conditions of the formation of some stockworks and the
zonality of mineralization. Izv.AN Kazakh.SSR.Ser.geol. no.21:
3-13 '55. (MLRA 9:8)
(ore deposits)

15-57-4-4836
Metallogeny of Central Kazakhstan (Cont.)
Variscan, late Variscan, and Meso-Cenozoic. The most important
stage for the develorment of rare metals is the late Variscan.
Endogene deposits of vein quartz-greisen, skarn, and secondary
quartzite formations were formed during this stage. Deposits of
the vein quartz-greisen are of greatest importance. They are listed
as follows: trie Shalgiinskoye, the Karaoba Ithe Akchatauskoye, the
Baynazarskoye, the Verkhne-Kayraktinskoye, the Zhanetskoye, and the
Kounradskoye. The ore-bearing rocks of the late Variscan stage
represent intrusions of leucocratic granites which formed small
masses of complex structure. Most of the rare metals deposits (62
percent) were contained in granites. The following genetic classi-
facation of rare metals deposits is proposed for Central Kazakhstan:
1) endogene deposits: a-epimagmatic dispersions of mineralization in
volcanic rock, b-pegmatite formation, c-skarn formation with a super-
imposed type of mineralization, d-vein quartz-greisen formation, e-
formation of secondary quartzites; 2) exogene deposits: a-original
sedimentary formation, b-deluvial, deluvial-proluvial, alluvial, and
Card 2/5

15-57-4-4836
ivietallogeny of Central Kazakhstan (Cont.)
0
places of superimposition of later zones on the earlier ones and at
the junction of zones. The principal rare-metal ore concentrations
are associated with the junctions of mobile zones. Ores are local-
ized either at the contact planes or in the various fissured zones;
the latter may be of parallel, stockwork, ring, or interformational
type. Many deposits are loc.,ited on the end of sandstone-shale
strata which are unconformed with the effusive-pyroclastic Devonian
and Carboniferous overlying complexes. Zoning is observed in the
complex deposits--tin and molybdenum ores are found closer to the
sources of mineralization, while the tungsten deposits are located
farther from the sources. A territory of 800 000 sq km was mapped
for mineral potential on the basis of these investigations. Areas
of mineral potential were distinguished on the basis of: 1) geologi-
cal criteria; 2) actual distribution of deposits and of hydro-
thermally altered rock carrying ore concentrates and metal-bearing
aureolas. Four categories of areas were distinguished during the
investigation. Basic directions of further exploration for rare
Card 4/5

Metallogeny of Central Kazakhstan (Cont.)
15-57-4-4836
metals in Central Kazakhstan should be: 1) continuation of explo-
ration for the major deposits of rare metals; 2) organizing e~plo-
ration for deposits of favorable genetic types located at the inter-
sections of deep mobile zones; 3) geological surveys and exploration
of other areas with mineral potential.
Card 5/5 Ye. P. M.

SHCHERBA, -,. N,
~ -, -4 ~,-a
Paleozoic zonm of deep tectonic movements In eastern
Kazakhstan. Izv.A-N Kazakh.SSR. Sar.geol. no.24:3-7
156. (MLRA 10:2)
(Kazakhstan--Geolog)r)

15 -1957-10-13923
Translation from: Referativnvy zhurnal, Geologiya, 1957, Nr 10,
P 80 (USSR)
AUTHOR: Shcherba G. N.
TITLE: An Example of the Relation Between Aplites and Quartz
Veins (Odin iz primerov sootnosheniya aplitov i kvar-
tsevykh zhil)
PERIODICAL: Izv, AN KazSSR, ser. geol. 1956, Nr 25, pp 20-26 (Summary
in Kazelch)
ABSTRACT: The Kuu intrusive mass is located at the western end of
a belt of intrusions associated with the Kau-Kzyl-tau-
Mamantasske,va deep mobile zone of central Kazakhstan,
along which acid magmas were intruded in the middle Her-
cynian and late Hercynian stages. Tile intrusive mass
has a form approaching a flattened ellipsoid and its em-
placement took place in three stages: 1) intrusion of
porphyritic coarse-grained granites, forming the great-
est areal extent of the mass; 2) intrusion of granitic
magma in the central zone with the formation of medium-
Card 1/3 grained granites; and 3) intrusion of fine-grained gran-

15-1957-10-1392,3
An Example of the Relation Between Aplites and Quartz Veins
ites. After the fine-grained granites were emplaced, aplite
dikes, pegmatites, and granite porphyry bodies were formed.
There are interrelations among the dikes of aplite, pegmatite,
and greisen, and the quartz veins. Aplites I are confined'to
three systems of steeply inclined fractures and are cut by the
later aplites II, pegmatites, and quartz veins, and also by
bands of mica-quartz greisen. Aplites II, confined to the
same systems of fractures as aplites I, are distinguished from
the first group by the rather high content of quartz and plagio-
clase. They intersect and displace dikes of applites I, pegma-
tites, and hig h- temperature quartz veins. After the intrusion
of the magma into the dikes of aplites II, there followed two
generations of quartz veins. Postmineralization intrusive
activity appears most extensive in the rare-metal deposits of
Kuu and Shalgiy. At the Shalgiy deposit nine generations of
hydrothermal veins have been identified. The origin of the
subsequent series of granitic dikes--with their systematic as-.
sociation of aplites and pegmatites, and later of ore as well--
is considered by the author to be the result of active magmatic
Card 2/3

SHCHERBA, G.N.; SERGIYEV, N.G.. otvetstvewlyy redaktor; RZHONKOVSKAYA, L.S.
ALFEROVA, P.P.. takhnichei3kiy red3ktor
[Geology of the Narym Range granitoidB in Southern Altai] Geologiia
Narymskogo massiva granitoidov na IUznom Altae. Alma-Ata, Izd-vo
Aky3d.nauk Xazakhekoi SSR, 1957. 213 P. (MLRA 10:7)
1. Chlea-korrespondent Akademii nauk KazSSR (for Sargiyev)
(Narym Range-Granitoids)

SHCHERBA, G.N. ; YTEMIOLAYTV , K.Ye. -, KAYUPOV, A.K. ; KIR, V.A. , NIKITINA, L.G.
FLEROV, Ye.A.; SATRAYEV, K.I., akndemik, red`v*-, BOK, I.I., red.;
SEM-_?NOVA, M.V., red.; POPOV, N.D., tekhn.red.
[Geology of the Leninogorsk nnd Zyrynnovsk mine regions in the
Altai Mountains] Geologiin Leninogorskogo i Zyrianovskogo
rudnykh polei na Altae. Pod red.K.I.Sat-Daeva. Mosk7a, Gos.
nauchno-tekhn.izd-vo lit-ry po geoll okhrane nedr, 1957. 370 P.
(MIRA 11: 1)
1. Akademiya nauk Kazakhskoi SSR, Alma-Ata.
(Kazakhstan--Geology, Structural)

i~ ti . L,
~,c*.'ects in the scientifl,! aiscussion on the ;~Itni
~z-.-- Ali Kazeta. z:,,' 5-.7. 10:7)
~, A! t a I a ins deoos,.ts 'i

7Wtl if- LA 1 t 2 ir. go~,' -.we s torr, Alta4 rzv. -Ail Kazakh
Se r i- e ril-.2 (YL2A 1~':a)

SHCHERBA, G.N.
Concerning "New data" on the magmatic nature of the Cherdoiak region.
Izv. AN Kazakh.SSR. Ser.geol.no-3:129-111 '57. (MIRA 10:1o)
(Narym Range--Rocks, Igneous)

SATPAYEV, K.I.; BORUKAYEV, R.A.; AKHMEDSUIN, U.M.; BOK, I.I.; KUSHEV, G.L.;
S)IRGIYBV, N.G.; SHLYGIN, Ye.D.; �11CHIOLBA, G.H.; MONICH, V.K.;
LOMONOVIGH. I.I.; LAVROV, T.T.; MEDOYICV, G.TS.; NOYOMTSKIT. 1.P.;
BARBOT-DE-MARNI, A.V.: GALITSKIY, T.V., KOWTILIN, N.Y.; ZHILINSKIY.
G.B.; KAYUPOV, A.Z.; KLZANLI, D.N .; SATPAY&VA, T.A.; ABDULK&BIROVA.
M.A.: GAZIZOVA. K.S.; VIIYTS. B.I.; KHAYRUTDINOV. D.ra.; MUKRAMOZHANOT,
S.14.; CHOLPANKULOT, T-Ch.; PARSHIN, A.V.; TAZHIBAYNVA, P.T.; YANUIA)VA,
M.X.; BYKOVA, M.S.; VOLKOV, A.N.; BOLGOT. G~N.; MITRYA)!EVA. N.M.;
0116KARiLYEV, S.Ye.; KUMAYEV, D.S.; YARANSKLYk, M.A.; REBROVA, T.I.
Tireless explorer of the depths of the earth's crust; on the 65th
birthday and 40th anniversary of the scientific engineering ac-
tivities of Academician M.P. Rusakov. Test. AN Kazakh. SSR 13
no.1,0:96-97 D 157. (MIELA 11:1)
(Rusakov, Mikhail Petrovich, 1892-)

0 m
01
1
I
o, do -o
o. *0 0.
2 1:
0 0
~.2-
in
o0g, ad 0
a I :Owl. a*!
a o 8. uo a
o"'. c c
No So t. *a ii 08
1 1600 .4
:10 b~ S 06
0-d 0
'00 0 ir "a I z'-.; .0 -o* ;U03 4H 0
1-5 A 00 0. u .0
3 1
Kw. t
ni
14, TO
as ; -5
Hot
T
0. 0 .90 A3 weal
9 v Im 111 Eli

SMMULt, G.11.
Rare metals and ijenetic types of deposits in eastern Kazak-listan.
Izv.All Kazakh.SbR.Ser.geol. no.4:20-37 '58. (91R& 12:4)
(Kazakhstan--Ore deposits)

S0V/7-r6-6-13/'l6
AUTHORS Shcherl-la va-nov. A. I,
TITLE; Diz,-ussion (D"-skussiva On the Age of Some Granite
in Central Kazakhstan Bearing Rare Metals
-iozrasta nekotorykii -ie'al'rykh granitnykh
,,~o ~ovcdu redkor.
Yazakh3tana\
uzi.; Tsontr-:il ~'()=o
0
PERIODICAL. Geokhimiya. 1~5B; Nr 6: PP 607 - 609 (USSR)
ABSTRACT: L, V Komlev, S. I, Danile,;ich, K, S. Ivanova and collabora-
tGrs believe the intrusions of Akchatau, Maytas and Zhanet
to h---i.;-? !~,~st:-.alz-dori-an but not Fosthercynian age (Refs 1
and 2), The atithors investigated these regions and carried
cut additional a6e determinations for Akchatau and Zhanet-
Tile assumintions of L. V. Komlev and others are in contra-
d-ct~.--n to the ceological conditions, In their investiga-
tion5 Kofplev ind his collaborators used age determinations
a-.c,.,rd-Jng ~c the heliuri, lead and argon method which resulted
In an averac-e cf 700 -- 31' million years, A. I, Ivanov
and N, 1, Zamyatlr on the other hand found in the
Labo~at,:,riya IG-N AN Yaz..SSR according to the argon method
2AO - 2,1t8 million years. homiev's determination for Zhanet
Card 1/2 was '12C mill-icn years, the authors, hoivever, find 207-243

Dis,~ij as -irr. - Cr: th-~ Az,-,~ I- F S ~:nm~ Gr:~n i t-~ lntrusi:~D 3SCV/7-5e-6 -13/16
In Cent-Tal Ya-z-arkiista., B-a,`n- Pare 1-.etals
m1llit,n -recirs (Table 2)- The sequence in the region of
Zv--a.,iet vias i-vesti.-ated in detail by R, N. Mallkova,
V F. Mura-vlyeva, V, L, I,,':eI',iikova. There are 2 tables
Z~.ri(" , whic', are Se)viet,
SUB~'IT'TED :a
Card 2/2

SATPATEV, K.I.; POIDSUKHIli, A.P.; BAISIMV, S.B.; CH)KIN, Sh.Ch.; BORUKAYNV, R.A.;
AKITODSAFIN, U.M.; KUSHEV, VA.; RMYST,
G.TS.; LAVROV, V.V.; BARBOT-13-K.MI, A.V.; GALITSKIT, V.V.;ZH1',INSKIT,
G.B.; KATUPOV, A.K.; KAZANLI, D.H.; KOWTILIN, N.Y.; MUKHAMMHAWV, S.N.;
SATPAYVEVA, T.A.;VEYTS, B.I.; GAZIZOVA, K.S.;CBDLPA1FLUIDV, T.Ch.;
PARS!TIN, A.V.; BTROVA, M.S.; MITHT-AYEVA, N.M.; VOLKOV, A.H.; CHAKABAnff,
S.Ye.; TARXNSXATA, M.A.; KF1AYRUTDIN0V, D.Kh.
On the 60tb anniversary of the birth of I.I. Bolt. Academician of the
Academy of the Kazakh S.S.R. Vest.Alf Kazakh.SSR 14 no.10:95-96
0 1-513. (MIRA 11:1-2)
(Bok, Ivan Ivanovich, 1898- )

3~-NWJ-FTOV, S.M.;BESPALOV, Y.F.; BOGATYREV, A.S.; BOK. I.I.; GALITSKIY,
V.V.; ZHILINSKIY, G.B.. IVSHIN, N.K.; KAZANLI, D.M.; KAVYUPOV.
A.Z.; KONEV, A.K.; KUSHEV, G.L.; LTAPICHEV, G.F.; LIANDOYET, G.TS.;
MDNICH, V.K.; MTAGKOV. V.M.; NIKITIN, I.F.: 14C)VOKHATSKIY, I.P.;
SATPAYEV, K.I.; SHLYGIN, Ye.D.; SHCHERBA, G.N.
Eminent geologist of Kazakhstan. Veat~kff Kazakh.SSR 15 n0-1:
94-95 ja 159. (MIRA 12:1)
(Borukanv, Rariazan Aslanbekovich, 1899- )

I', I 1 .1 N D-7 -, I F I
P.ya.; Z',. A.; AUVOV, M.O.; S;i_-P 3ATISFlCH-_,V-
WATJOVA, T.T.1%; 3AISUIV, S.B.; 3AY'rl.'Olj'nOV, A.D.;
30(',ATYF_:,,'-V, A.S.; ROK, I..-.; 3ORTAL-7-~W, 31 3-H
ZYK
BTKOV,~_, !:.S.; ZHIT.I:-S.-'IY, OV, D..-..;
KUAIFLI, D, laYUPOV, A.'!,,7 KERMAYN , S.K.; KOLOTILIIT, F.
i,-MTAYF,V, 1). r,.L.; O.Zh.; v00"."
G.TS., 1.11,i6a:11'OV, G.; Ilb-K_IIA!DDZHA,'CV, S.I.I.;
4 P,')* Tr:ly, S.'T.; POWzRTlrHll_-
PAR,SKIIT, F'ROT T, A.F.; RU6:'~KOV, V.P.;
SM(IMN, 3MYYUIJJ", S.Sh.; TAZH13AT~,V, P.T.; 72',SETKOV, r.".G.;
SHLYGITI, Yc,.D.; SHCL:',T~A, (,HOT.Il,, Sh.Ch.; CHOLPii_'~TKULOV, T.Ch.
Sixtir-t!) of' Acn~~!--- --ician Yanysh I-.antaevinn Satnaev. Vest.
JIN Ka:3a'ri. SSR 15
0 p (MIRA 12:7)
(SatDaev, -, r-
a-sh I,r~nntafivirh, IriQO-)

Grit;orly Ilikiforovich; AYTALIYEV, Xh.A., otv.red.;
IIZIOIIDKOVSUYA, L.S., red.; ALFEROVA, P.F., tolchn.rod.
Pc-rujtion of rare metal deposits in central Kazakb-stan]
Fortairovanle rodkometal'afth mostorozlidenii TSentrallnogo
K~z~akhstana. -Alma-Ata, Izd-vo Aked.nauk Kazakhskoi SM,
1~6r_.. 373 P. (miRA 14:1)
1. Chlen-korrespondent AN KazSSR (for Aytaliyev).
(Kazakhatan-41a tale, Rare and minor)

SHCHERBA, G.N.; KUDRYASHOV, A.V.
-
One of the criteria of genet!c association in ore formation. Izv.
AN Kazakh.SSR.Ser.geol. no-3:116-119 160. (MIRA 13:11)
(Feldspar-Optical properties)

AN Fa~Lb~IFkoy
i,.axA and

SHCn,'RBr`j G.N.
Conference on tl-e metallogeny of the iacific ore be2t. Izv, AN
Fazak.h. SSR. Ser. geol. no.I:SM5 161. (MIRA 14: C'- ')
(Soviet Far East-Ore deposits) --

('A, , YU,A.; KUMINUA, VI,V,; IMIROSHNICHEIN,~O, L,A,
S . .. .1
Subolirface mcbile z~mes in central Kazakhstan. Izv, All Kazakh.
no, 118-22 'o2. ( MIRA 15 : "' )
Qn,zakhstnn-Geology, Structural)

,-Uc F7 ~i BA,
cf ear-,C 1 ru s r. 1'
e E Aa 0
n- (KRA 15:~
(KazakhsTan,-Earth--S,_,rf

SHCIERBA~ G.N.
Some problems in prospect-in'- fol- hidd,~-n, ~.I. Mb, Bi deposits as
revealed by prospeectLrig in central Haz4khszan. Izv. Ali Kazakh.SSR
Ser.-ejI. nq.-0:5--12 t62. (HISiA 16-5)
0
(Kazakhstan--Ore deposits) (Kazakhstan-Prospecting)

~LITRYAYEVAJ, H.M.; hOZMOV, A.A.;- SHCHEiLBA, G.N.
Genesis of complex ratal ores cf the Atasu regirn (central
Kazakhstan). Izv. AN KazaLh.S.SR. Ser.geol. no.0':53-64
162. (14IRA 16:5)
(Ataju regi~n-Qre deposits)

SHICHERBA, G.N.; YFRSHOV, B,V.; IVANOV, A.I.; KUDRYASHOV, A.V.;
Z"CRIW7, H. P.
Possible Mesozoic age of the Khorgos intrusive complex in the
Dzungarian Ala-Tau. Trudy Inst.geol.nauk AN Kazakh.SSR #:226-236
162. (MIRA 16:6)
(Dzungarian Ala-Tau-Geological time)

6hk',i;E;-I-Ay G-i".
All-Union GDnfe-c~:.,-.ce -D,-. -Lhe Gre pctenlial -cf. *v----L-------'c
tary Formations. !---- '~' no.4.-III-1-12
t,3.
C, (MIRA .16:9)
1. Institut ceolocicil-skii~h nau'r: &N ,~azakhskoy SSR, Alma-Ata.

l.". " . - ~ ri-P, i cjr!. Ili!! I i?
slicll~PW, G.N. , i;- , , ~ - i.
I
Fre-~uen~ -,f bet.-.,E,--- rnIJ*ner-al-:zm,',.:'-i and fmgmatic P'c,-
cellisee. -v'es~. .-*-*,i 2~~ 11.).9:1 7-7r; S "-~4, (fERA 17'.10)

VT~
an-; res,.~'-z cf thE c---r-.b-'npa ~'n~VeS-4E!a--Crj of the
s p P, r sr'. m'O'Dile zc~nS n CE-IT--al Fazakhs-,an- , 7ZV. AN Kazakh.
S""R. Ser. geol. ---~l no.3:3-10 My-Je
(M--,Pj, 17:11)
lnvltut geologricheskikll nauk im. K.T. Satpayeva "N KazSSR,
th.

ra-ak,
,T,T.C'IIA, Vera Dm-ituiyevna
zasluzi-iennyy leya,,c- -,L*nauki - - - I
C~
K RYASHOV, Ark ac:-:, j
Panteleyevi!-hj :F.3'77,q('.IIA !.I., ren.
1. - _L
P,reisens,veiri qiinrtlz,and, p,jta,!-.i(, felisprir in mc'y'bdenu
%ungqten deposits rX Greizeny, zhil'nyi kvarts i
kalishpaty molit~derio-vol'i.'rijrcvykh in~~stcr,.)zhdenii Kaza~hstana.
Alma-Ata, lq64. 306 p. rAkanir~m4ia -ai~k Kazakhskoi )")R. Institut
;_eOic"gich,~skikh rauk. Tr,iciy, vt~1.8) (MIRA i-7.6)

, I;*!, KO, L.A. ,
'RBA , C. 1, geo joFrO_j:,, !ne valc k, 1 c -le 0; ikh nauk; I.
I I jokfur I .~ 1 1.
SjICHL
kar,j. lrl-i_r.,.;-,,:l Inera log. nauk
- a-, N
Etiuoggenic ore f ormations c-f Siberia ancli ~,e 7 1 I-East, Vest- A'
Kazakh. SSF 20 P; .7-.85-86 i1 *614~ (M--qA 17:11)

SffCfl'---fTA, (I.N.
Some of Atasu--type deposits. Iz',. AN
Kazakh. SSR. Sec. geol. 21 no.~615-33 &-0 1644- (MIRA 18t r)
1. institut nauk im. Satpayeva AN K13zSI;R, AIM8-AtS.

Y,~ R B'
m,,r, ob va 94 no 4~.47 -
(MIP-4 lszg)
'skiv I proyeMnyy institut "Gipronikell",
(for Shishkin). 2. Leningradskoye otleleniye
MatematichaSk,-)o instituLa AN S5~2.q J.meni Steklova (for Demina).

S/169/63/000/003/006/042
D263/D307
AIrl HORS Alelcaeyev, V.P., Beayadovakiy, Ye.A., Biryul-ova, L.A. ,
Golyaliev, G.I,, Ivanovokiy A I
Kokin, G.A., lWrilova, Yu.~.' '~ivllhita' 1I.S., Petrov,
Rozhdeatvenskiy, B.G., Solov'yev, N.V., :Speran-
akiy, K.Ye., Khvostilcov, I.A., Gh4idkovskiy, Ye.G.
and Shcherba, I.A.
TITLE: Study of the upper layers of the atmosphere vith the
aid of meteorological rockets
PERIODICAL: Referativnyy zhurnal, Geofizika, no. 3, i963, 23,
abstract 3,1166 (Tr. Vses. riauchn-Leteorol. sovesh-
chaniya. T.I.L., Gidrometeoizdat, 1962, 91-103)
T=-T: In the present review-type article the authors give
the results of studies carried out at TsentraInaya aerologichaskaya
obaervatoriya (Central Aerolbgical Observatory) on atmospheric sound-
ing with.mateorological rockets. Measuring methods are described and
the main points are given for obtaining such atmospheric character-
Card 1/2

S/169/63/000/003/006/042
Study of the upper layers ... D263/D307
are giv-
istic:s as pressure, temperature, and wind. Certain results
en: data of seasonal temperature variations at heights up to 50 km
in the middle latitudes of the USSR and in polar regions, cases of
sudden warming up, characterization of temperature distribution
curves, a table characterizing the temperature inversion belour tba
stratopause under the conditions of polar night, and data regarding
he circulation in the upper atmospheric layers.- Information is
t
given an the constructed meridional sections of temperature fields
and on the zonal component of the gradient wind. (25 references).
f-Abotracter'a note: Complete translationy
C
ard

LUPYAN-N, A.V.; SHCPERBA, I.G.
Overthrust in the reFion of Kenebek-Zhondytau Mountains in central
Kazakhstan. izv. AN 535R. Ser.geol. 26 no.8:10~rlC9 kg '61.
(MliLA, 14:9)
1. Geolopicheskiy in5titut AN 5SSR, Moskva.
(Kazakhstan--Faults (Geology))

V.v - SHCIfEIIL4,
Some charac~leristics of the magmat-ic penc--,r~:---on zones
in the Northern Bal~hash SynclinoriijM. Tnidy GIN no.PO:,
"' 5 -
,- 1 -.311 '63. (MIU 17:6)

PET:T11 'K A., MIFANT'Y".11, E.Ye. KHORKHOYOU, L.V., I ~G.
I i - . SHCHERTBIAI
Phosphlt6s and phosunInites of trioln and the-;.r Zriur.ob.
khim~ 34 no.1,70-77 Ja 164. (MA 17:3)

S HC I LERBA.1 1 as p f ran.
Des ~,-:,-irg a sevn-rq-- mr~,:-.nanism -w- nucus
mot -;On of the 'Lo' !owe. r '-itrl ng a ve:, neg--~-e of Lhe an: fir ~Cavi aion
during Its function L)e-rjctj. vy-s. -ucheb. zav.;
10. -- 1 65.

a s r --: r ~. t
lirka:-e: c;7c,,i---r
mot;n,. cf- thr- follower an6i a mo-t fav-rfible
u
Lraj-smisf~ion ar:,-"e. Izv. v-,,,,l. ucheb. zav.; mashLnostr.
r.,. 1n:5-19 ' '05
1. Siilrr-~+,t,ecl February 29, lc?O/+.

3URT, , I k , ; DTJ6H -'--~`i , T . K, ; S-I-EDUVA 5 1'.V. Y- S H G I L"RBA Y I Ya
Detem,ination of boron with crystal violet. Zav.lab. 271
zio.6:61,/P-650 161. O."MA 14:6)
1. Ka,,,~.d-hskiy institut odnerallnogo syrIya, Tsentrallnaya
laboratorlya Chelyabinsizogo geologicheskogo tresta i TSentrallnaya
lnburat.ori.ya pologichoskogo upravleniya.
(13orui-Analysis) (Crystal violet)

Distri 4UI/411-0
.;PrePATaIon of a. windows pr Wig.'.
T. N Pribory i Tekh. MO.'
rpVr
Ine a o. 3, 1 pie nietfiod for the prelm.
of AgCI windows for obtaining infrared absorption spectra is
offered. AgCl was Optd. from Ag.\O~ and then filled into
20 cc. Pyrex glass aminits, which were placed into muffles,
slowly heated to480% and held them for 40-50 min. Theni
in the course of 10-12 hrs. the temp.:was very slowly low
cred to 19-0-50'. Under such. conditions relatively largi;
AgCl crystAls are formed, The cooled inan ~ is removed
from the glass mechanically and. wished with HN03 and
1110. 1 The transparent man is then pressed- in, Cr-plated
molds. During. IiS-tM min. the preswe- is grddually In-
creased to 92(W atm. After release of pvessure the ma" is
beat-IrLated a,, 100* for 2-3 firs. The pressure is then-sWwly
;increased to 350 atm., held for IG-12 br!,-, and gradually
released. Transparency of the product b 70-80%. Av.
crystal size is 0.5 min., -------- 9~~w~itch
A

7 IE J 11, 1 c a t _J or. s t ~-_e ! n r ar ed S e c 1. 1 "'m o o ri 1 a t e
i-a- i , n z - t--- Gaseous to t-e L4-,u;d State (7=enenJye
io r o...
v inffa,-r:,sno- -,-.?'-'re hode 4~ -a-o-
-.a L:rl uerek
0 'L r ~ z "'. 0o V i e ,; o s 't o y a n i y e
E 1~ 1 7 C L I z v e 2 t a A':,-;. d e -i I n a i i SS S R - S e r J_ ,r 'a f c ~'. e s 1: 9 58,
ol 2 2, 1 r 112 2 12 ~! (UE
S T 7 '-. 4 0 i ~
of t,-,e i, fr--red snectr,.,.m, of
li-:uid ammonia and of ammonia solution in car con tetra-
chloricie. T'~e snectra viere taken with the spectro:::e-6--'r
~KC-11, uSin~; LiF and NaC1 prisms. The .:pectrum of
lic:uid ammonia aas recorded in t,-,e rL-nje 2 04 15,,.- at
-500. T;.e soectrum. of the ammonia solution was only
obtai-ed in t~-,e of t'-e 11-H valence oscillations.
SyrithtA`c ammoni-, ~sas used in t-~
I . he ex,,~eri-.enuc,
was dri4~--d '-v condenzation above metal],ic sodium. On
t'-e 7~as-ls of cot--ceived hyd-_-o~--en binding in arn-ionia,
.:fre-_-4er modifications had to be exoeczed in t~,e sT)ectr-_m-.
of the licuid, is to saj t.,-,e occurrence of a new
band cornected ,,iitIn the distur~~-ed 11-H occillation

fi c -_ t z; 1' -; t ',.e ! nfr_:-ed S ,,ec ~ rum of i a SYI? -22-)-2o /4 o
at -..-ie `runc:ition Fro::. t-,.e :;aseous to t*-. T.i--.-*d State
..e
and a decrease of t',-.e delener~~tlon of t;,e ineq-,lality
of t-e th~ *ee 1.'~: b-*Izl(-,~-,-,,,:-,. Actual'y no essential modi-
f--cations were observed in tbe infrared spectrum, with
t.)e excez~tion of a stron& increase of the rel~__tive
inter--ity of the N) band und a com~jaratively Creat
-,-. tof `n~ band IT,-.ble). This result can be
(I L I a c e:,i, U
the U-SUT.-M-ion of ~,n interaction betv-,een
all t",~rec, 7:-~' bin,~_in,-s oll a molecule with the free -.)air
of t,-.e ot'-..,?r mol~-ci~le. In a case t'ne 11H bin-.,,-'n,,-s
are For tilis co-,-;ception, howe%er,
t"ie ~or:-.Ltiqcn of non-linear hydro-en bo~,d is a pre-
(, .11 L, - C~
requisite. T;Iere ure 5 figures, 1 tallh le, and lo r,_--_--"-_re_r..ces,
2 Of 1.7%ic, are Soviet.
AS S I j'.- 3-os.institut uri~71:~dnoy khimii(Statue instit-ute of AEolied
Carl 2/2

25 (Q' 130V/64--59- 1-16 1/124
,T M -. -
Uftz)
Vany,:shina 7. S., VJ 1 e s ova , M1. SShcherb-a, L. D.
TITLE: Control of the Hydrogenation of Adiponitrile and z,f the
Purifieation of 11examethylenediamine by the Methc-d of
Infrared Spectroscopy (Kontroll Jidrirovaniya adiponitrila
i ochistki geksametilei~diamina metodom infra-krasnc-., sl~ektrc-
qkopii)
PERIODICAL: 1[himie-heskaya promyshlennoW. V)'Y), Nr 1.- p!) 4'--43 (TTSSP)
AMRACT: At the Gosudarstvennyy institut prikladnoy khimii (State
Institute cf AppliedChemis-cry) an analytic method was de.-
veloped which served the examination of the reaction mixture
in the continuous hydrogenation of adiponitrile (,-) (Ref 1)
luring 'lie synthesis of hexamet-hylenediamine (II). This
L3
analysis takes, however# 2.5 - 5 hours. For a faster determ-ina-
tion of the conversion of (I) in the hydrogenation the
spectrometry by the -C-~N group is suggested for the present
case. The purity of (II) is particularly important for the
production of nylon. It is stated that a judgment of the

pur- L 11
*-ty of (II) by the freezing temperature is inadequa--r:,
and that a perfect judgemert Jis only possible ---n the basis
rd '12 of an infrared spectrum analysis in which no abs,,rpt-on band

SOV/64--5) -! -', 1/24
Control of the Hydrogenation of Adiponitrile and of the Purification of
ilexamethylenediam-ine by -che Method of Infrared Spectroscopy
of the --C~_N gro--ip may 'be observed and in whl,,h thzi jrcups ITH
and ITH2 appear. It is recommended to carry out the re;,,tifica-
tion -3f raw (II on a rectification column (under vacuum and
in. nitrogen, atmosphere). Prom the fraction T, = 40.0c a control
by the irfraved spectrum by means rf any spetrometer (e.S.
IKS-11) should be oarried out whereby the required rectifi~-_-a-
tion conditions can be established. 3 examples are ~3_Jven 4-:i
which a column with an efficiency of about theoretical
bottoms in nitro-en atmosphere was applied. Results of
examinati~jns cf the freezing tempexat-ure of the individual
sam.-les are indicated (Table). There are 1 table and 9 ref-
erences, 4 of which is Soviet.
Card 2/2

'S; 66850
A_4_)_ SOV/76-33-11-3/47
AUTHORSz Shcherba, L. D.. Sukhotin, A. M.
TITLE: Study of the Hydration of Ions by Means of Infrared Absorption
Spectra IA
PERIODICAL: Zhurnal fizicheskoy khimii, 1959, Vol 339 Nr 11, pp 2401-2404
(USSR)
ABSTRACT. Investigations (Refs 1,2,5,7) of an absorption band shift at
4.7p, by dissolution of salts in water show that the shift in-
creases with rising salt concentration. Ions with a small
radius have an effect on the absorption band similar to a
temperature drop and ions with a largerradius act on it like a
temperature rise, which is in agreement with Bernal~s and
Fauler~s findings (Ref 10). Waldron (Ref 8) studied the effect
of dissolved salts on the infrared spectrum of EDO. In the
present case the influence exercised by LiClO 4~ LiJ, NaJ9
mg(clo 4)2" 14gi 2~ (iso-C5H4)4NJ, and butyl quinoline iodide in
a small quantity of water dissolved in acetonitrile (H 20 and
Card 1/2 D20.) on the infrared spectrum was investigated. The authors LK

6b8410
SOV/76-33-11-3/47
Study of the Hydration of Ions by Means of Infrared Absorption Spectra
studied solutions of water and of the salts in the concentration
range 0.01-0.1 mol, as the salts are practically completely
dissociated at these concentrations and the water is associated
with acetonitrile in the form of a monomer. The spectra were
taken on the spectrometer IKS-11 (with an LiF prism) in the
ranges 3300-3600 cm-1 (for H20) and 2400-2800 cm- 1 (for D20).
It was found that in the spectra of salt solutions one may ob-
serve, besides the valency absorption bands of dissolved free
water, new bands shifted toward lower frequencies, which are as-
signed to H20 molecules penetrated into the solvate envelope of
the cations. This sh-ift is explained by the polarization of the
H20 molecules. Consequently it depends on the polarizability of
the ionsg it decreases in the order Mg 2+ 7 Li+, Na+9 05 R11)4N+
I
and is 120. 83, 103 and 108 cm- .Salts of the quaternary am-
monium bases the cations of which have a lesser tendency to
hydration do not cause the abo-vementioned effect. There are
Card 2/2 4 figures and 10 references, 2 of which are Soviet.

SHCHTR A, M. L. A V-, 1964
UVA,uto
KIDNEYS - DISEASES c-11963

VOL71;SKr-,', Z;roviy !.-oiseyevich; GOGIN, Yevgeniy Yevgenlyevich;
~;HCHEHBA, red.
[Diseases of the pericardium] Zabolevaniia perikarda.
Leningrad, Meditsina, 1964. 303 P. WDRA 18:1)

RYABOV. S.I.; SHCHERBA, M.M.; ROS~'C~Irl'!~, G.M.
Pathogeriesis of ~ri arf".-It-L's. Terap. arkh. 35
no-5:82-86 My'63 (MIRA 16:12)
1. Iz kafedry faku-11-tetskoy terapii Nav. - zasluzhennyy deyatell
nauki pro% T.S.1.stamanova) i kafedi-
y propedevtiki vnutrennikh
bolezney (zav. - prof. M.L.Slicherba) I Leningradskogo meditsindo-
go instituta imeni akademika I.P.Pavlova.