SCIENTIFIC ABSTRACT SHABUNIO, I. F. - SHACHUNKINA, V. M.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001548510014-2
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 9, 2001
• Sequence Number: 14
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

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A UTHOR: Shabunya, V.A. SOV/3-.58~12-14./43
TITLE; Basic Introductory Lectures (Ustanovachnyye lektsii)
PERIODICALi Vestnik-vysshey shkoly, 1958, fir 12, PP:47-:49 (U3SR)
ABSTRACT: In the author's opinion- the purpose of-basic lectures is to-
give the correspondence students who have'begun to study the-
USS-history, a fundamental orientation,:to help them to un--
derstand the most important theoretical,.tenelts.and to d,ecide
in what sequence ench theme should be Ftudled . In these
lectures, the students are also advised how to organize in-
dependent work more successfully and to:use the time at 'their
disposal most efficiently.-_The author does not share the-,-
opiniQn of some instructors who believesit best to present-
the basic lectures in a correspondence v-uz, in the same man-
ner as ordinary lectures in resident vuzes. ~Fle deals in de-
tail with the method in which various themes i: n 1.1irxism-Le-
ninism are to be handled in the basic lectures.'
ASSOCIATION: Vysshaya shkole YND SSSR (Higher School~ of the M1VD MSR)
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L 30777-66 EWT(M)*/ETC(f) RM/DS
ACC NR- AP6022137 SOURCE CODE: UR/0080/65/038/012/2666/26701
AUTHOR: Sha
burov, M. A.
TIG:
. none
0
TIM!,': Stability of -the All-17 anion exchange r -esin-in the Cl-form upon heating in
water and certain alcohols
SOURGO: Zhurnal prikladnoy khimii, v- 38, no. 12, 1965, 2666-2670
TOPIC TAGS: anionlexchange rosin, chemical stability/AV-17:anion exchange resin L
ABSTRAM. The report attempts to show how_much the bulk ca0acity- of the
AV-17 anion exchange rosin in the Cl-form changes when heated in,'water and-,
certain alcohols and what reactions occur In the process. In all the experi-'a
,ments, the AV-17 anion exchange rosin containing 6% diving1butyl in the Cl-: I
*form was used. The anion exchange resin was.dried at 110 for 4 hours and
ex glassampule,
used in studying thermal resistance. It was placed in a pyr
and covered with 1 ml of liquid in which the resistance of the resin was
m6asured. Thenthe ampule was sealed and thermostatted. k1characteristic
feature of the anion exchange resin AV-17 in th- Cl-form is its relatively
high rosistance to heating. For example, at 1000 and 30 days of Continuous
heating in H 20, the volume of tho resin remained wholly unchanged.: The
,same resin iii the OH-form at 100, in H 0 after 30 dare of hop * Aost 26%
ting
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L 34372-66 LoL(m) DS/PM
ACC NR, AP6010744 SOURCE CODJE~ UR/0076/66/040/003/0561/0567
AUTHOR: Shaburov, M. A.;Saldadze, K. M.
ORG: Novokuybyshevskiy Branch, -Scientific -Research Institute ~of Synthetic Alcohols and-
Organic Products (Nauchno-isoledovatellskly institut sinteticheskikh spfrtov I organichefficlith
produktov, Novokuybyshevskly filial)
TITLE: Investigation of the behavior of the hydroxyl form of the,strongly basic anion
exch and some alcohols'
~an ys AV-17 and AV-27 upon heating In water
SOURCE: Z I v. 40, no. 3, 1966, 561-567
hurnal fizi heskoy khImi
Xe
TOPIC TAGS: anion exchange resin, thermal degradation, e hange reaction/ AV~47 anion
exchange resin, AV-27 anion exchange resin
ABSTRACT: The authors investigate the stability to heating of the.widespread strongly.basic
anion exchangers AV-12 and AV-27 In the Off-form. The preliminary preWation'of the
exchangers was described elsewhere (N. G. Polyanskly, M. A; Shabdrov, Zh. analit.Ahim.11,
18, 304, 1963; Zh. analit. khimil, 117, 1965). The only difference was in the methodology
of investigation of the liquid phase in -which the AV-27 was heated. Heating of AV-27 resins_...
at 160C was found to cause a slight loss of total exchange capacity (18%.in 10 days).-,:: At 75C,
the loss is 8% in the same period. In alcohol media, a slight increasein the loss of'Wx-change
1/2 UDC: 543.544
-Card

ACC NRt AP6010744
capacity was observed for ethanol and methanol. An increase in length of the hydrocarbon
radical of the alcohol used causes a reduction In the loss, It being apprOdmately equal in
water and n-amyl alcohol. For AV-17, which differs only In the replacement of a methyl
radical by an ethanol radical, a similar change in capacity in wi ter Is.noted, In alcohols,
however, the loss of capacity is considerably greater (6 1% Ys 2~% for: "-27 in methanol).
After three days of heating in methanol at 100C, AV-27 loses almost all strongly basic groups
AV-17 loses 62%. The dearnination and degradation typical for AV-17 are therefore also
characteristic of AV-27. Deamination Is the dominant reaction for AV-17, degradation for
AV-27. Laboratory technicians L. G. Myasnikova and Z. Ye.:Antonovit took part: in the
experimental part of the work. Orig. art. has: 3 tables, 3 figures, and 2 formulas.
SUB CODE: 07/ SUBM DATE: 24Dec64/ ORIG REF: 010/ OTH RE F: 003
Card 2/2

USSR/Wdicine Brucellosis Sep,~ 50
Vaccines
..... ......
~'Xxtraction of aLiving Microbic Culture of Brucella
-'From Killed Semiliqidd Pormol Ant ibinicellos ii"Nac-
cine," 1. Xe. Skorin, Cand Biol Sci, M. S.-Shaburov,
M., I.: PopovIyants, Candidates Vet Sci, Div of Bio-
chem, All-union Inst of Exptl Vet Med
.8
'4Veterinariya"... :.no 9, _-pp 2 -30
'Conducts series of tests on properties of a living
mitrobic--c'ul tur-c.-isolated by_G.._:M._,_BoshIyanI~sI.M_.I
thod from killed semiliquid f6rmol
vaccine, series no 31, and f ind' them identical to
I f]M/Medicine -Brucellosii (Contd). Sep.. 50,,
-Brucella melitensis. .'Concludes formalin in con-
centrations used to~prepare subject vaccine,does"'
not kil '1 causal agents.of the disease.but merely
inactivates them, changing their form and proper- I
ties, and under specific. conditions' this changed
but living culture from vhich killed vaccine is
prepared can acquire form and Properties inher-
ent in original strain. Head, Div of Biochem.,
Dr G. M. Boshlyan.
AW& 166T50

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80) PHASE I BOOK EXPLOITATION SOV/2828
Shaburov, Salomon Ivanovich
Spetsiallnyye voprosy proyektirovaniya gornykh liniy elektroperedschi
(Special Problems in Designing Electric Transmission Linesin
Mountainous Areas) Moscow, Gosenergoizdat, 1959. '111 P0 3,450
copies printed. -
Ed.: M.A. Getsov; Tech. Ed.: G. I. Matv,-.yevo
PURPOSE: The book is intended for electrical engineers working
in the design of power transmission lines.
COVERAGE: On the basis of long e-xperience in the'Tbilisi branch
of "Gidroenergoproyelct" (All-Union Trust for the Design.and
Planning of Hydroelectric Power Plants and Hydroelectric Develop--
ments) in the design of power transmission lines, in mountainous
regions, the author analyz.,js the following problems: the right
route of transmission lines in mountainous.terrain, the location,
of towers and their special design dictated by unusual :conditions,
the length of spans under conditions of steep rise and descent,
the meteorological conditions affecting the performance of-.
Card 1/4

Special Problems (Cont.) SOV/2828
transmission lines, etc. No personalities are mentioned.
There are 5 references, all Soviet.
TABLE OF CONTENTS:
~Foreword
3
Ch* 1. Spacing of Towers According to the Mountainous Profile
of the-Transmission Line
1. General information 5
2. Dependence of wire tension upon the length of span 7
3. Spacing of towers on a standard profile,according to. the
17
formula y= kx2 (k- const)
4. Spacing of towers with consideration for the differences
in height of the wire suspension points~ 25
5. Conclusions 31
-Ch.-2. Maximum Spans for Wires of Various Types
1. General information 33
2. Maximum spans according to the permissible overtension
of the wire at its suspension points 34-
Card 2/4

Special Problems (Cont.) SOV/2828,
3. Maximum spans according to the operational allowance for
wire tensils strength 43
4. Conclusions 68
Ch. 3. Permissible Difference inLength of Adjacent Sparis
1. Lines on suspension insulators 69-
2. Lines on pin-type insulators 80
3- Conclusions 82
Ch. Equilibrium oT.Insulator Strings on Lines Running
Through Mountainous and Areas of Sever6 Icing
1. Operating experience 82
2. Conclusions 89
Ch. 5. Selection of Rated Span for Assembly CU'rves and Tables
in Lines on Pin-type Insulators
1. General-information 90
2. Lines on pi-n-type insulators with rigid;intermediats
towers 92
3. Lines on pin-type insulators with flexible intermediate
towers-
Card 3/4

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L 54784-65
ACCIRSSION NR: 'AP5013993;
ir vs, ~i ~ abul a
tions. :The energies and, inten'sities': of: 158: -g
g a- t -a d; i. r a'
U64 Pre
of' which 149 are ascribed to, the 'In~ibiti dot ioli
work raises the number of-known gamin6;, trwidit loliian
Sur
Zia energies. of 39,of.the lines are,,.compardd eas bibnts or
ft,241_1060~ The .Va; ;s'pj 6, a are
0
Bu.schhorn M.Naturforsch*l
~ex
shown to agree within . the limits of,,the. perimeaitbl ~a,~but;.
re iati6l:~hhd,s.. 1
Buschhorn's data are regarded as the.1 Acau
0 sent:meas en S.ind iara-
matic differences are ascribed~t ~ the' P'rq Pirlaq .
accordingly,-removed. Estimated errokslof. a energynj ~sqrement
:15 M
range from 10 to 900 6V (for .- ten ~'of tha'~, line s'~ no '6. ~mit6&!~error
_jt abso
dt 0
measured relativb.An 6hViarte
given). The ten~itiies:,~wer6
iznt-ensities by, comparisoii with 556~.kev Fd~C&'_.Ii~he' al
"th
el and transition scheme for M wds! deti-in,d.-IirdOd 6: astred.,
-descil
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gies by a "general suti-difference m 'do:similai-i
etho
841'
by- B.Hamemesh at al,:(Ann.PIIy6ik$I3i2 1961 latibis~-'
)4~
jo
are discussed,in.some detalle The resiAtNe s,ch6t6i!'oAd~JI6:14j').7
on 'CI!'k:fIn
rans i b~
beilow 738*09 keV. end aeecwnt~ -for' 38:'ot the t
'bM _~'that
IldS 1
foian
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grouping of the lines vas~observed 016 1; 0
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ACCESSION NR; AP5013993~

198
ir by'Hamemesh at -al.
A

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'
~ai*..'gititefu.L'~';'
cussed at some length* lime '.authorEi

ending a prepublication :A
'List', o
r tfib 96MM iineso~_
;
lished by U.Gruber (Zeitschrift fueli Pfik4jk ~ 178147
Gr2g4_qv, A.M.Demidov.and I&VtEstulih f6r discussib~
the wov&, and to V.G.Zaik
- i Xor asslRan6e~ in4eifi
a-D-1-9-f 6nmilas 101 f
ts. Orig. rtbh
men iguires. abd
A's S OC 1A T I Mnone

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ACCESSION NR: Ap4o34598 S/0182/64/000/004/0005/OW7
AUTHORS: Kazarinov, B. N.; Shaburovi V- Yee
TITLE: Investigation of the process of closing axial defects by,.upsetting
SOU RG E Kuznechno-ditaMovochnoye proizvodstvos no*~hp 19649 5-7
TOPIC TAGS: forgingt defect structure,, defect fw~sutions leads steels steel Will/
UIY60 testing machines U7 steel
ABSTRACTt The authors proposed and elaborated the method or,upsetting for use in
'closing axial defects in steel and lead. The.influence of~nonhomogeneity of
deformation on both the closing of defects and on the strain condition of the
sample and the dependence of defect closing upon sample size and:form werealso
investigated. The samples ~iade from U7 steel and white lead) were cylindrical,
with a circular orifice cut into the axis of each sample.-Testing was carried.out-
with testing machine UIXI-50; samples were placed in a special container (ass Fig.
1 on the Enclosure) for use in conjunction with the1esting~ machine. A photograph-.
ic record shows the sequential steps in theclosing of defects s~4 gives rsoordings.
of the change in H/D ratio. The authors present a achemat Iia diagram shovUg the
mechaniam of defect closing. It J-j concluded thats 1) tfie mkgrttuds of the H/D
Card 1/3

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Nauch.-Iaottdovalel. (W01. [list., lkwi%L&V, t'kr.
lapoik; 11iijoyms. Misinal, Obikhfitra (.Nt#tn. ow. ruisk-
minkral ) 77, 2lU-14(JVV').-Thi* rare Pe-NIn MI)IIAluslie
#*Vnro in cryst. Whisto of Timplo"A' vakul;;I. stsswL
ith quartailex '4rld Onriwa. at m4d
notiteand basic Ca-Mark-hists. Theluragenesipwitliblo'.
titc. feltisp4r. sillimaulte, altitandite. rutik-, chlirrile, M(kt-
titc, graphite, magartitc, and hematite is typical.- Vui-
title W% short-prisinatic ctystab tuaktv oil d1krilt 1%,01
quart zitr. Mvrk-ip~wt. nearly hUck. harthir-A (;.Aa
d. 3.21. (hitically ". with sts (,NA): -r - 1.727, a
1.679. Pleuchroismstrotig,litifett-w-yellow; ddtcp&T'LsS_
rrreti, a yellow-appic gn-en; absorption .1 > -, >a_ I
Alxsorption cur%-es we" detti. for -r and a by inicrophnta~
inctric methods. The chem. anAlysis shows the high Mo.
v,mtent (7.W~' ) of the titincral, but the absorption char-;-
iteter is chiefly dctd, by the Fes0i content (9.60%).~
Thisupp,trent contradiction is explained by the assumption
that the Mn is pretwitt, not as AfnA replacing A110t, (lot
in tht l,iv;ttcnt fnrut. The formula is therefore in doubt;
The x-my diagram of this viridine is identical with that of
Californian an,Llu,ite. W. Fitcl

Two chlorites from S. Valcutis. 1.. 1. Shi Ithy"in, (Kat-
WA M1,C7", Horislov).
3lipirtal. Objluhij~~j (.%fkln. soc. Msw
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grad, K foch Oumjl-l I fit- Wilmliedcroollill.
pr~.Ilwt. 4 xralolt.~ to "Willijilill -A'hilt., 4nd 11tOUltht
AARIt ill iufvts~ oillu'upo of 1111cilla,W magnij, which
-m L.1tr cluill(rd I'l Vrjxrlllilli1-. talv~jrtpocmlc altil
lcllkt~, %ticas (wridir allif margurite)
mu I --hl,,ri tv.4tv i Ile t vi.ic,j I IA yet, -,I, jjj~j jj,,o,raIsftWnled
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ill '11e 1111-1-4111"WhiltW I*wo vari,tivs ill hh,it,
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nicif'r. lur ill-lat'. pfc.ithmi'm 1, )Ft-lluwi,h tit
..... ... .W Thc - w1n. i, rcut.fkable for
the high 1,111, " b.W Fell i 1.151.
Ine'lLite Itti.tVIt J.r ajj~l infer.
croll'.
t1l"t"' efIrcts"" thl' -1111CIC1111.11 t-e-1 570-4)7o' AmI
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Ristile (,age, ite) ollcrarowth, Jr~ fritlively: .."riv.
Ill! air ~Vutclnlly CAU
-A thi, clitur, Wit
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by local Ti. Cr. and The (trigniA 11PAItt Of 1114L
InAry sulolrAturn i~ al., in.ficatet! by the prvcitce Of chou-
littinite, foi-mcd from 4)IiViIW of tile UIjt-.4jNt-jVN AbOUL 4imul-
fAlwMAl4y with villwite (1). or oullit-61tely bdime it 1111,
A chitwite 4 wax -Yvlltlw ctlltw il 'he
ti%ltll 11111 tile yrif,,-
fly MptcWtItilt. n, I L.W;
1,57.11; bitc(ringriwe 0-thil, nearly imi.mal. The ch,tu.
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high G.,7 :3 i.but mucithigbri
At,(), lfttu all I = L'I"). CTO, is M~p nold,
higher thAtt in 1. Pri.m.ttic Wife .11141 VVYPIM1161C AtV
typical ititergrowths in the yellow 11, ttlivia in rather i~ijx-
J;t1liVV CX101n. structure,. The ititergrow-th of It with
kyanile is another charavit-riliv inslicaii;ytt (or the IyAra-
xxnei, with the urixiiial cmumbloa tuiumils,
- - %%% Fill-I

777

es in
wDetsitimbsistim of bars slimes.

-
L
Sh
l
l
Z
hi di i C

_* , ! minerals art eml
Lion I t JeL ra
Lion I lio it(
f
6
l
ib
i

a
ivn
n,
, VSC30YUS. bsbehal
in
0
OPU
szairbelyil
e
luilborite
and k
-LudwiVEe
446110"EV91111JEU
t ear
4
r c
1e
cic
k
scopic precision methods are indisf
stinction of clitiolminite and kotbki; ~ tile latter! mineful,
di
.
.
,
,
tolte occur in magnetite, phlogopite, or calciph skarn , -Ay~s?taibefyitc, may be confuskil with talc.
changed to fine-si
suited. also with clinoliumite, In the contacts of grauito
In reflected light ilynite and ludwigtiL ~lxre alsb: e4sily con-.
,
,intruslonswIth.doloutite, in distinct connection with on:

i
f
h
b
i
l
d
C
Z
A fused b"Ause-or'llicir anisaq
use Of Intir high
tifica. -
Oi
Id
1
li f
4
rate an
tions o
u. T
n
epos
n, BI, anti
e
Fe,
u,
crab am always restricted to the metasomatic zones of the or
l
4a
I
:
tion. TZiurinallite, axinite,. or; (tito I e may. Olitetilues.
altered dolomites. The typical aswens. are with forsterite xur in-om skarns alid'iudiviti~ tilt, possiblMy of tile
(usxatly serpentinized) or ditioliumite, serpentine, spincl,
presence oU udwigite.
mtiWyite;' etc; The
phlocalpite, sometimes also with We, brucite, and periclaw. .
indication. It wever, wiJI always be'~the stud~W the
Staibelyite usually occurs ia pseudomorphs after ludwigite,;: conditions olothe: cootacwnetasomid!fin on! thil',boundary
oer fildependently, also in scaly aggregates pseudornorphous es; 1'r
bet cen multes and.doleindtlis.'
after fluoborite. The latter borate. occurs assocd.: with. -
l
i d

l ca
cite. a,
OgGlitte ad magnetite in coarse-gramilar rocks
F
which it is easAy confused with clinoliumite or hypers-~
thene. ?Vith forliterite the fluotiorite reacts to form clino-, L
C.A.
humite juld kotcUr (cf. Watambe, C.A. 32, 62032;
46, 69f),'ju c-ilciphyres assoed. with Pb-Za ores; fluoborite
also reads.wnh magnetite to form ludwigite. The typical
lated extensively.
rgene I -h kam borates am tabu
clt
uded am the parageneses with We, prebuite, i1valte,
Acalacrinite, icroo'.Ite, and p*xene (pigeonite).- The
he i~jdtntifi-

T
j

N;

--------- --- --
j
oy
WS 'I
q -analy-is was p:in-Ole. Sv:m1dibite clu Y:KIieciirs,1
diopside Awns with tiiii
t
fonns palml-L hg~lqatej up toI-c1n.
e1 Cpl-
Characterist: rt2e
-ia calck,-
filhd d
6umalint Mid ddoriie whl~h aLp 'I- di 4
p,repacescren bife--
~1 , . . , ,iPC4
irunaal With II
a intimate iutugravjt~ai Sp lie 013 a r
i1i'din a ma&-~ EL sp pn.: 111vi -au alrxlysis 4f ~ th e SaIiiidlb 0! h
The Min d ;,V I*
;ufii)Or JIch 9 Sir
very juani. till fl
',1`1x~I1hIIdpt1v RO PiCILN-1 It .1,k.
flipsoldq do not. 6in6citz, i:v . V it Qns dre It dus'd
(pMatalre tvdulitnpl;~ tfi~w% 1 o
age plarre T 1) ,it' ir
tile Chief ellill-luld FW:s ill ill A tAga,
700 inp show MrWtig. dOIL,
mucrit
14 for the Spet'val 111!,~ F 1.7 for thti Q 11
The absuptim tkh-M0
:J 'abmt 660 my, In -,ts L
t
dibitj~ is itspeciaily varlablic !it Its' it B, 'at !,UL I" l
curve is givets. ivhi~h: -166w tha;`
H T~-
barmu a'
'of thi Fe-,01'~Ontl
c:L-r wny,~
tile Optjw ct-Arn be, ci)f.h~r CKII j.. -Vi,, -Z
'1V

I Iii - : ~ --7, i
: i I"!
1 - - 11' 1~ -, ff ,
: i I
i I; g 1 .1 li
LLii i H I IL 11"i". I 11! 1111 L11,111,111-11 ." I
i I " ~i . , : 1 ;:114

V36
AUTHOR SHABININ, L.I., cand. of irti tier alogic al-geo lo:-, ic al
T IT LE Utilization )f Boron-Gontainin& Ores
(0, kompleKstioin ispoizovanii barrio -z nelez ni kh. a6sian)
PERIMIOAL Vestnik Akademii ?!auk SSSR, 1957, V61 27,' N-r 7,'pp 29_- 32: (U.S.S.R.
ABSTRACT boron is won from deposits of volcanogeneous an~ exoreneous type-#
The special property of boron raw rnaterial'occui~rlrt_~ in the U.S.5,R.
consists of its complex character. The bornn reserves hitherto de -
termined in boron-containing iron ores are co;1siderable. -If the va-
rieties of cbemical composition and the physic.:.tl properties of borates
are taken into consideration, a very thorough.in.vestigation of mine--
ral type samples and subsequently of avera&.; :.7re samples -vas from
the beginning a prerequisite of a rational .0r.46etion of borf)n. The
percentage of the obtained boron doubtless dep4bds-on-the correct
,working of the ores and has to be technalogicaliy.founded to a'suf-
ficiient degree. The author is convinced-that t6e pertinent-planning
stations have to work out a comprehensive~.prog~an of research and
utili-,.ation- for the purpose. of fast and rationil winning of boron.
iV13SOCIATION Not given
PRESENTED Bf
SUBMITTED
AVAILABLE Library of Congress
Card 1/1

(0 "nezise
De posl
on ore
to 0
ShabynIn a f y kh M s r
1K.u e z
~,U T HO R Of South Y t5 By 1958,
The Gen'515 %helezorucin Che ~ayE
log
iya Geo,
yuzhnO-ya Y Ser
TITLE' 55SR9
of
'Iraaemij gau
A - - 11~ -teristics~
Izvestiya,-61 (USS" Oharac & ore
# pp 4 rinciPal~~ f rocy-5 a'n
PS1110-DICkb: - th the P itiba 0 inclusive.
1e aeaJ5 W1 & the compos &ePOsits I the various
an . )n ore f, vip,85
The artletructures kirc thor re , b the'
'al s th jalc-uts aU -shere I
A.BSTRkCT: eologio .the SOu The deposits 2. the,
9 ts of ores- hese futecl, an
aeposl iron of t re in the JjSSR
complex boron rormatlo n is being es
the tio sof the - genesis no snalOgi, iron
r n orphic re are comple,
.Oncep The talline enes-Is 0
cryp
se(jimentarY roven- kutsk tions of, 9 eo-
character P South Ya The ci'Lle' several 9
skarn pre-Cambrian shiel&- Is. tely by re expresseci*
to tile pldarl calnine -at sw e
of the been e) r. . e (D'S'
~ 3 vjew,P01
deposits- -ts have ~tasomatic tyP formeli
I f 01:10wing -ts are , .
these dLePOs` the contact-me -1 aeposi - th high
,hereby of the I&ineTa nts 'W1 . rredL
logists, posits are 2 1 f edime - occu
ae h-jsni 0 atiOU5
The Shabynln SO.me Joe Iro
jinskiY meta.mOrp n
. only , chenkO
yorzl tions Serdv,
aresult of re93
as con6entra n (D-P-
and borOrl.rorl and b0 0
iron of I
- f ting
a Shl
ral
Car Car( __1._-_1_9R__temper-
-~-Z'Ur-regard t
2 types 6fL I ~ 0 Ores,
--------- --l-H dolomit pard~enesis:
es. 2. p~iragenesis
Occurring
ZHARIKOV. vil,.n Andreyevich; WOR HUSKIT, D-S-,Rkademik, glavMy red.;
_5H&M11f._L--L.otv.red.; 270DOT'YBV. X.M.,red.1zd-va; NOVICHROVA.
tekhn.red.
[Geology and metasomatic phenomena in deposIti;af skarns and
complex metals In the western Xara-Kazar Mounta'insl Geologila
I metasomaticheskie lavlenits skar ojo_p0,jimetA licheakikh
n
mestorozhdenii zapadnogo 1aramaxara..Mosk-wa._Iid,vo Und.nauk
SSSR- 1959. 370 p.'(Akademiia nauk SSSR. Ingtitut ge,016gli
rudnYkh mostorozhdenit, petrografti, mineralogii I gookhtmil.
Trudy. n0.14) (MIRA 12:5)
(Ura-Kazar Mountains--Ore deposits)
(]Lara-Kazar-Hountain's--Skarne)

AUTHOR- Shabynin, L.I.
TITLE; The Laws Governing the Distuributd.on -and Formation' of
Conditions of Boron Concentrations in. Endogenetic
Borates of Skarn Deposits (0 7,ak-onomernostyakh
razmeshchen-iya i usloviyakh obrazovaniya kontsen-,
-me' to-
tratsi y bora v endogeznn~kh boratakth skarnovykh s
rozhdeniy)
PERIODICAL- Izvestiya Akademii Nauk SSSR, Seriya.GeologiGheskaya,
-90 (USSR)
1959, Nr 3. pp 81
ABSTRACT- At present. there exist 3 types,of.boron deposits:
exorrenous (halo-en-sed'm-entary VolCano.-S
ed-iment.ary
and endogenous. The third type of bo-ron.deDosits is
twofold-, datolite: in lime-skarn deposits ~and_magnesia
as well as ferrous-magnesia borates in magnesia-skarn
deposits. From the large group4of magnesia borates
of endogenous concentration are ofL' interest to in-
Card 1/4 dustr,-y::ascharite 1 2 rJ1gO-BPO 30H0.) -1 ud T, i g J_ t

i, ~ I 1 1:1;" 1:,
...... . ........
The Laws Governin- the D_43L-,ribution and Format-ion all' Cond_-itions
of Boron Concentrations in Endogenetic Borates of-Skarn Deposits
latter
TA G Fe)n- Fe BO and cotoii~e Mg: (BO -he
4: 03 3-12;, u-
is rflostu rarely f ound A detaila,d description of the
critcria for determ-Lnincr the laws Governing the dis-
tribution and the. Ecrma1.-.Lon of boronAeposits is Dre-
sented for conSideration.. The dependency of the mi-
neral composiltion of' bovai;es upon -the- composition of
-~neralizaticn is still: inadequately -clari-
metallic mi,
fied. It can'be stated onily that ludwigib is the
leadin- -primary borate i-.n i.ron.ore de
Y posits, It'is
imDossibie ruo-find cotoite concc--nt-rations (cotoite,
plus m_-7,gnetite ludsigit.)- -vrithiin mar-- etite mine-ali-
n
zat-ion --ories in i.ron ore deposits. Out-of 67,knovrn
endogenous borate deposits there are only 7 bearing
boron in form of tourmaline and.ax-inite in feldspar
rock. The boron-bearing province covering the terri-
tory to -`U-ne East of Lake Baikal,:-.as selected by the
Academician S.-E. Smirnov, joins ;the iuidest orb strip
Card 2/4 along the Pacific Ocean and is characterized by an

SOV/11-59-3-6/1'/
The Laws Governing the Distribution a-rid Fo_-mation of._Conditions~
of Boron Concentrations in Endogenetic BoratesowofL Skarn Deposits
abundant boron-bearing zone. Borate raw material o-C
volcano-sedimentary.deposits is still unkiaoun in the
USSR. Therefore-, the author emphasize.s,that it isl
necessary to undertake comprehensive geologica.l.re-
C3
search aimed at discoverinE; such deposits in the
USSR. The study of the facies composition of carbo-
Ueposi-ts in the territory under discussion. is
required for-successful~skarn prospecting of boron,
deposits in form of datolites and~laiso.of borates.i
In this respect, Soviet llmoviledge-~is extremely limitueCL.
The chemical composition of carbonate rock. even in
ore districts, is studied very 14 ttle. As a rule,:
,even those carbonate rocks. known by the mineral para-
geneses developing during.their skarn process. area
called limestones., Such a situation- the author' con-
eludes, ', cannot be regarded as normal and therefore
-Card 3/4 more attention-is to be-devoted to-zhe,study of.the

SOV/11--59-3-6/17
The Laws Governinr '-he Distribution and Formation,of Conditions
LD
of Boron Concentrations in Endogenetic Borate.,,~, of Skarn-Deposits
facies composition of carbonate depos-its in -folded
areas. Thereare 3 tableS anci 8 -references, 6 of which
are Soviet and 2 En-li-sh.
ASSOCIATION: Institut-geologii rudnykh mestoro'zhdeniy, petrog~raf ii,
mineralogii i~geokhimii AN SSSR,1.Toskva (Institute
of Geology for Ore-Deposits, Petrography, Mineralogy
and re o U
a -Ch-emis'ry of the USSR Acade~-,iy~of Sciences,
Moscow)
SUBMITTED: -December 16, 1957,
Card 4/4
P

I I I ; I" I ~ 11 : i: I .; 1111 11 , z 1 1 1 ~ 11 ,
U. .. - -I -, - -
i
! 4 i
; : ! ; .': . : .3 : -
I : . .
~ i i i :11 i 1~ 111:i til 7111 1~ -,., 1-1117 11-i-l"IrP TO FIFF.-T-T-11il.,

SOKOLOV-, G.A., doktor geol.-min. nauk, otv. red. Prinimali uehastiye; VLASO-
VAY D.K.; GLAGOLEV, A.A.j ZHARIKOV, V.A.; LOGDOV, V.P.; LUKIII, L.I.1
I.IYAJELYA., R.O.; 01,fELIYAITE21K0j B.I.; OSTROVSKIY, I.A.; PERTSEV, N.N.1
PODDLESSKIY, K.V.3 0512TOV, L V.; SOFIARO, T.A.3 TB40,F1ffEVA,- L.Lx-
'LH SHADLUP, IAP121, V.V., red. izd-4ya; MUNI., -Ye.V.j.
S NII T.N-
ABI
T.Ahn. red.
(Physicochemical problems in connection with the-Tormaiion of rocks.,
and ores] Fiziko-khimicheskie problemy formirovaniia gornykh porod i
rud. Moskva, Vol.l. 1961. 658 p. (KIRA 14: 10)
1. Akademiya nauk SSSR. Institut geologii rudrjykh mestorozhdaniii pet-
rografii, mineralogil i geokhimii, 2. Institut geologii rudnykh mesto-
rozhdeniy, petrografti, mineralogii i geokhimii'~AN SSSR, Moskva (for-
Vlaeova, Glagole-v, Zharikov, Omellyanenkoo Ostrovski3~,..Pertsovy I Sha-
bynin). 3. Moskovskiy goologo-razvedochnyy institut im.S.0rdzhonikidze
(for Shabynin, Pertsev.)
(Petrology)

I . : . ! Hi ! :I. ..: 1: X: I
. I . : , I I ; . ; : .: !, i ;
. a
.:. ; .; . , 1 1: ": ~i g I j,:-.
. i I , ill*. il'i 1: ilill Tflill-IIIII!, lill
. :, I

I i . z i : I
I . I H I '1111i llll~ :1111111:1 '1 11;11~
I T!

; I[. I Wil! .4 ; 171 P III, - I A 1z 1111 !11 .1 :~r. 1;

i i 1: ; I ii. 1 11 T - - , , 1.
j I . . . . .- . ~ i
! :. : :4 i ; - I
I 111 11 1~!.F. !!' 1, 1;; 11T :! ITI il

a ; . ; ! ~ i 'i i I I ., i!I ,
I* Ifl I :j; 7
I Jill.

i .I ; I "! It IIT I'll VIM .; liffil 1~

K mka!;Krl - 30" H.1 M,
2, Hill I
lllla*AiB 1JUVRIJ 4 1191m;

: :~ j, , ,
. , , .- 1 -11 i T i_- -i1 Ii !I , 1! "` ! iI -I !I : ~I:-, t I :z-
i ! . . . . .: . . '. : I

AUTHOR: Shachin A.V. , Engineer. ~122-2-9/33
TITIE: The Running-in and Testing of Two Worm Reduction Gears by
the Closed Contour Method (Obkatka i ispytaniye dvukh Pherl-
vyachnvkh reduktorov zamknutym metodom)
PERIODICAL.-- Vestnik-Mashinostroyeniya, 1958, No. 21 PP031-34 (USSR),.
ABSTRACT: Two layouts of close circuit test rigs,are shown, both
distinguished by the minimum number-of gears in the Iclosi ng
link between the worm-wheels, the direct-driving of the worms
-and the disposition of the loading device between the worm
wheels. This arrangement permits the testing of both rever-
sible and irreversible worm gears. Owing to the low efficiency,
a considerable difference in loading can exist between the-two
gears. In practice, it follows from formulae derived in.the
paper that the gear,.whose leading element is the worm wheel,
is loaded to the -extent of only 0-5-0.85 of-theload of the
other-gear. The recommended sequence- of riinning-in includes
preliminary running-in of the less loaded gear and a-finishing
run after changing the other gear and reversing the wnse~of
rotation. The power of-the driving motor is computed for
reversible and irreversible gears. A rapid method is.given
for an experimental determination of the-worm~~Sear efficiency.
The closed contour method for running-in two.worm gears
Gardl/2

It*' HI Him: m, Iq I, I 'I: Ji J~j j!
- ---------
Country U, 6 SIR
CatcSory Farm AtiLaals.

Abs. Jour
Re-P Z' -Biol,, No 21, 3.0"0 9,A~41
Author
All
inatitut. -#-Institute- niual :,-.,orPho1o,-v JUS USSR*

Titlo t h of G t1e,
Data St -,dying t j i oGr ow A
Ori.,j Pub. 77r. Lyll-t a nior'FO--. ZhiVotnY1'-%9 Xi WSRs 3.9571
_ -jyp. 22 145-156
Abstract
The -cona-ection betrweer, t?2;:! correlation o f the-
LInimalst -,-jeight and size on the One h,-.nd
wid
1;ht forn-ation of and lmd1i -or- them ~-er
a
c- -rlt -a-s Conducted
was cia-ified, The,
-lith !-'0 one -ear old calves of the black-spot-
*
orowr
ted b--~,eedj dividO. into 2 E:~Oupse The Ist
received rations for a d .-.;alight gaLi of
c'
0
800-900 ~g the Zad group for a gaia of 650-700
g. The irl group received more digestible pro-
teln, and when on pasture aso I kg of' oil cam
Card: 1/3

I
WHMVGR112127~. IN m 26

r- Iffl, m
J11MI11 till w
rr wrl

.. ... .....
Country USSR
Category Far-m Animals,
C att I e.

Abs. Jour 41
Ref Zhur-Biol., 'Xio 219 19,89 968
Author
Inatitut.
Title
Orig Pub,

Abstract Cal
kes,per car. Theaverage IiVe wei-ht ot
ves In the ist group in6reased dLr I..'Lle , ~t am
lf-
giloup by
period by 48 percent in the icolntx
1
~

tAe s 'he~
Percent - during unmer u r
3-5
changed to 31 and 37 percentj in-the ist group
the size of the ajaimals increased. during the
stall period by 42 percent and during the pa-
e.coat~ol
sture period by 49 percent. Ma. th
'
group the corresponding. indicators were 32' Wrld
-ie winter u
4-8 percent. During 'he weigh:u o?
the animals increased faster' P-L=in the sum-
Card: 2/3-
61,15 SIR
I all,

Ir 74 11 F", I I r-11: FIN
RIM[ U IR-1 III!

11 1;-. ! - ;i I I , I I - ;- . - - : , . ,

1 11 IF IT11 V
42102
5/179/62/ooo/005/005/012~
E191/L-135
AUT!"OR: S h a!;~b ne_v_9__V,_Ak. (Moscow)
TME: ()n the axially symmetrical problems. of thermo-
elasticity
PERIODICAL: Akademiya nauk SSSR. Izvestiya. Otdeleniye
tekhnicheskikh nauk.. Mekhanika i mashinostroyeniyel
no.5, 1962, 75-79
TEXT: An analysis is givenfor axially symmetrical problems
of the static theory of-thermo-elasticity for the case of-a.;
Circular cylinder of.finite length. In the conventional method,
using a stress function, the problem is reduced~to a differential
equation with mixed derivatives. In solving such equations by
the Fourier methodg separation of varia~bles in s~omecasescan 'only
be achieved by establishing for one-of thevariables a differential
equation of a special kind. The solution of this special equation
c'annot always satisfy all the necessary boundary conditions. For
this reason, the axially symnetrical problem is~ solved by the
Fourier method only for an infinitely long cylinder,~or a. cylinder
of finite length with special boundary conditions.
Card 1/ 3

1 21,111 Tk~
S/179/62/000/005/005/012
on '_ae axially symi-iietrical problems ... E191/8 135
A.I. Lurlye introduced "homogeneous" solutions in order to satisfy
approximately the arbitrary boundary conditions.'at the end face.of
a semi-infinite cylinder. The solution of-the problem for the
finite cylinder by the method of-separation of variables has led
to an infinite system of algebraic equations. The present author
Xntroduces a stress function in-a special manner and, to begin
with a particular problem with mixed boundary~ onditions is
Solved. This permit.-5 reducing the solution of, the partial
differential equation in the case of an arbitrary axially
symmetrical loading to the solution of an integro-differential
eqLiation of a single variable. To simplify the.discussion, the
problem of a solid cylinder with simpler boundary conditions.is
solved. The stress function is introduced as a. Igeneral solution-
of the second differential equation of elastic equilibrium. A
special set of boundary conditions is chosen to~~elimiriate the
known solution for the case in which temperature is not taken-into
acCoulit. -A differential equation is derived for the stress
function For introdlicing thermal stresses only the knowledge of
the heat flow over the cylindrical surface is r Ieq~iired. ~Before
Card 2/3,

s/,137/62/000/002/00, 2/008
A006/A101
Dolgopojova.,r A. M.
J.,~ S_ev,
THORS: Fedorov, P. hachn
A
U
am of the lead-bismuth-magnesium system
TTTLE: Phase diagr-
ebnykh zavedenlyp Tsvetnaya Imetallurgiyap nIo,
pF vysshikh uch
,RjODjcAL-. izvestiya -
2, 1962, 58-64
The authors studied the phase diagram of Pb-Bi-Mg,system by the
TIM: On the whole, 8 sections were investigated in~the
method of thermal an, ~he results obtained are illustrated by~a number of graPhs
given ternary system. are,,b IinarY ones and:that,
which show that sections Pb-Mg2-BW'4g3 and Pb-B12M63 Ie -tems,.namely;
the given ternary system is divided Into three separate,t-rnarY sYs
and in seCti6nLPb?4g,,-Bi the
Pb-Bi-Bi Pb-PbMg2-BI2r"g3 PbMgq-Mg-Bi2~193- C by 2M93
2rilg phase was observed, which decomposed at 5200
formation of a ternary
liqsolut.-+(-~. There are 11 figures and 3 references:
peritectic reactionS
1S I t-bloc and 2 non-Soviet-.bloc.
ov e
ASSOCIATION8: r-loskovskiy institut tonkoy khimicheskaj t .eldmologii (Moscow
te of Fine Chemical Technology); Kafedry~khimiii:
Institu
Card 1/2
3/003/Oll
"/000/00
1,,49/6
pomp
01 06A10'
PIC
8nd
V antimony
shacbrle V ------ dL Tn3L
bismuth an
01
-,,juubbji1
pint So ,jjf a j.
Studyinrl tlie Mol-ten lead :Tsvet-WEL metallLur.
7,av eclenly I I ~ ~
cliebi"JI'Ja cLearly
be more
,7,vestiYa vy~ 99 je,adL can and
M
62, 94 muti.,izins. 0 14 Lut I s N4as
1~11WIODIG no. 3, 19 debis f, Is
durilng t S01ubillty c -eeSystem were
ths
currinG -1 01 Le-Is
0C the 303.n iubil mater~,
al
Int SO
C Ini
L; 0 lata .0%,
f The 30'
99 92%)
Tf- ty, the 'd The f 0110VIIISI.Xim Mutl-k -~96-
~ST- lea - 0c .
Ited 4.-en at 400 - 1) masno ate b1s, jr, preparing
anuldb
rep -50,1 '. ixim -n r em
Magne A pro _
t".non'j- , ~ lc~ J51s ade 3153 the
an sotlie, - , '-YS IV ~The Ma assuring,
L sA not
. -1 3- 65~) - '' 'tioni,
Stud1ed by t'-e - (99. 0
-to V net*O,,. specinoo
,,,are e coMp
used -C).9 r e _recl ~erjdr
U contiil'~' oss
de lead (99 .9 -1 e lrecL~jj ous jbi-e.
I Of at a Imp
gra on 1 1
3~ pb) ec V -es Vlas
as . a e 0 amp
Bj fe-so -prase
Nq
a110 s U
ta 0
-0
e amount
tyl EL rk
ptiMum
0
or hen
Card 1/3
M 1 N Mir H"

:3/149/62/000/003/003/011
Studying the joint... A006/A101
produced showed a distinct boundary between segregated crystals~of the solid
phaor '-ipper 'Layer) ana the settled liquid phase (lower layer). The results o,r
cinal..-,.. ng the upper ana lower portions were plotted on a concentration triangle
and composition of the solid phase was determined according to Shreynemaker's
method. The results obtained are Illustrated. It was found that in the Pb-Bi-M&
system,. there are i solid phases in equilibrium with the melt at the given tem-
perature, These phases represent ternary solid solutions~on the base of the fol-
2 the ints of double sa ura--
lowin_- compounds: PbM92, B'2~g -2PbKg and Bi2Mg- p0 t
tion (E and P) contain: 0. Mg and 96-70 0.30% Bi
.L 94.9WPb, 35% Bi, 4.67% % Pb,
3-00% t4g, respectively. In the Pb-Sb-Mg system ternary solid solutions on IPbM92,
Sb2K,~, and antimony base-are in equilibrium with the liquid,phase. The composi-
tionsjof double saturations ooints are: 96-55% Pb, 0. 20%1Sb,-3..25,'e Mg (point El'i
and 88.2w% Pb, 11-30% Sb, 0.30% Mg (Point D). The possibility is shown of eli-
minatin when over
.g bismuth from lead in the form of ternary phase B12M9 .2PbMg2
3 percent magnesium is added. Maximum refining of lead from gismuth (11p to 0 .1%)
at the experimental -temperature ts obtained when about 2%:jKg is:added. The .re arn
6 figures and 2 tables.
Card
3

s/149A2/ooo/co3/Oo3/oil
Studying the joint ... ~006/AlOl
ASSOCIATION: Moskovskiy institut. khimicheskoy tekhnologii (Moscow Instituteof
Chemical, Techniques) Kafedra khimii i tekhnol6gii redkikh i rasse-.
yannykh elementov (Department of Chemistry and Techniques of Rare and
Dispersed Elements)
SUBMITTED: June 23, 1961
F16-ure 1. 0\0
Isotherm and conodes in
-the Pb-Bi-F~g system at
'too,(;
P6 /a 20 39 49 69 90
o0c. %
Alng',
Fi.-,ure 4.
Isotherm and conodes in 20
the Pb-Sb-rlg system at
4oo0c
NA,
20
9J7 SA
it, sec. %
Card 3/3

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: . , 1 1 , ; ; ; -
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im.m.-Mo.... . .............

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I I T!, 11,14"
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I : ; . , i. : . ! II ! i a . - I a

SIX316 1/001/00 5/0 25/0 28
A006/A 10 1
A UIWORS Shachunkina, VIM, Turbin, R.I.
T HE - Preliminary results of observing the lonosphe.ric effect of the: sc-
lar eclipse on-February 15, 1961
PERIOTCAL2 Gecmagnetizm i.aeronomiya, v. 1y no 5~ ig6i, 835~
TEXT* An expedition to Troilisi was organized for the purpcse of studying
the ionosDherie-effect of the solar eclipse of February 15, 1961. The phase of
eclipse -wa= 0,955 for 240 km altitude. Ionospheric observiations.over Thills!
were carried out for the first +.ime;. -an CA (S-4) type-ionosound was employed.
An analysis of f-graphs plotted shows considerable variability of f F2 durin-
the day. The E layerlis characterized by the frequent appearaxice o the E2 layer
at 200 km altitude. A marked decrease of cri-tical frequencies:of the E, E2 and
F1 layers was -onserved immediately after the, beginning of,' the eclipse, The -nini-
mum of electronic density in the E and F1 layers coincides with the maximulm phase
of the eclipse. Regular changes in TOE and foFl during the eclipse made-it pos.-
sible to determ ne ~he recombination factor for these layers. For e E-layer.
=.1.5 10- cm/sec, qo 4oo ei/CM3 see. For F 2~10- cm~/=ec. In
E F
Card 1/2