SCIENTIFIC ABSTRACT SHISHKIN, N.I. - SHISHKIN, N.S.

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• Collection: Scientific Abstracts
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• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

SHISHKINY N.I.
Providing a steady personnel for the northern regions of the
country. Probl. Sev. no.6-.18-24 P62. (MIRA 16-66)
1. Nauchno-issledovatellskiy institut truds, Gosudarstvennogo
komiteta Soveta Ministrov SSSR po voprosam truda i zarabotnoy
platy.
(Russia, Northern-Labor supply)

IAZUTKB,I, Ye.S.; ltUSANOV, Ye.S.; EYDELT~i, R.A.; T:iUBIIIKOV, S.V.; KAHAN,
T~TAFJNOVA,
!.I.; ZAGG-HODFIKKCV, M.I.; GOL2TSOV, A.N.;
N.I.; SONIN,
I doktor geogr.nauk; ANTCEZ14K V, Ye.G.;
V.Ya. ; ~0
ZH.I,YKHOVA, I.I.; K09YAKOV, P.O.; RATROZOVA, I.!,; ZELENSUlY, G.N.;
SU",EIIKOV, Ya.S.; ZALKIND, A.I., red.; iUJSAIX)V, Ye.S., red.; SIYT~Y"R)
A.V... red.; MIIMAL'CHENYO,N.Z.,red.; GERASIMOVA, Ye.S., tekhn. red.
[Manpower of the U.S.S.R.; problems in distribution and utilization]
Trudo-.-ye resursy SSSR; problemy raspredeleniia i ispolIzovaniia. Pod
red. N.I.Shishkina. Moskva,lzd-vo ekon.lit-,ry, 1961. 2/+3 p. (141IRA 14:12)
Moscow. Nauchno-issledovatellskiy institut.
(Manpower)

SHISHIKID!, Ilikolay I., red.
I--------
[Labor resources of the U.S.S.R.;
and exploitation]Trudovye resursy
leniia i ispollzovaniia. Moskva,
problems of distribution
SSSR; problenv rasprede-
Ekonomizdat, 1961. 24" P.
(IaRA 15: 10)
(Iabor supply)

SHISHKIN, N. I.
"Methods of effective utilization of manpower resources"

6
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On 5785. PRINCIPLES GuVERNINti THE fRODUCTIONOF LUMICAMTS WITH Sr-AM

001 - VISCOSITY TWINNATURE COEMIENT!i. Kobeko, P? and Shisk4i.9,-
- --

0 4
KI (ayp~. visc. liquids and colloids acad. eci. u.$. i.' 9"R
l
-00
2, 161-166; J. inst.petrol. 1945, 31, 410A) It is pointed out -06
me that the mixing of simil-r li,imids has little effect in .00
improving the viscosity temperature codfficient of the mixture,
00 as compared with that of the components. If, however$ the A =00
000 solut has a M.W. which is very great compared with that of the COO
0 0 J: solvent, then the change in viscosity with temperature is 000
00-, similar to thtit of the latter, which in the case of non viscous goo
00 solvents in very small. Results are givan on mossuremtna
00
i of the viscosities c)f solutions of polystryons (AW.39 4W,ODO)
M
and eyhthetic rubber in toluen* and turuentins, respectively
Am f. over the temperature range -W to 1 100*0. Whilst an ordinary 800
4 0 1' lubricating oil changos in viscosity by.-1010 times within :500
00 this temperature Intar',,al, the "a iq the case of the
1
solutions examined is only about 10 -10
times. Results we
also jv n for a mixture of rubber, turpontins and transformer oil.
&$a ILA NITALU-F~-VAL LITINATUNI CLASSWICATFC%
*00
gjil7f ii 5- Ali Smat
v
t? tr 11 CW&( Knit% RICCI It 11 W 0 1 1 a a 2 1

0 0 0 0 0! 0 0 0 9 0 0 0 0 0 0 0 41 0 0 0 a 0 0 Ole 0 0 0 0 0 0 0 0 0 0 0 0 0 ~
0 0 0 0

SHISFIKIN, N. 1.
2
er
salts, :-',~ls, ;3ir. 1. T ourvers 'nave n,
F)r I
r! 7rV~, I-
V Cc~ 0 X jo-4 i s e s
d~ rection
e 1

4 *-*-tV*tVO a 0 06 Goat; 0 * a a a0
at '
l
4 IT a
IN " a M 11 oil No NU
O41 ItO 61 O
)
e
A"
L
L a T
A
f
X
1 I
Ci AAA 0
L
A L
0
.
.,
_
of Ar _
__
., -
.
,
I.P W1

'4,0

so
so _40

00

*49 -A The anwrPbom state. X3L Principles 9(developuteat
Of heavy Oil$ with MMU temperaWra de
mudence of their
490
00 l
viscosity. P. P. Kobcko, and N. 1. Shishkin. J. T~A.
-
e
IA
U
SS
R
.
.
yl. (
.) 14, 10-17(1944Y.-
ra
mmire satis.
6
4
f
l
bd
i
i .00
Actury
u
uAt
on
n a temp. rantre from -50
to I(x)
it is necessary to develop lut"-ants with a justall tenip. -00
timit. of viomity and a viscasky of soate 8 12 lxaws. The
t
b
d
i
f hi
h -00
a
ors exam
. sa
o
ns. o
-tual. substances in low-mal.
g
wAvcnts and found that the virmsity increased consider-
.00
ably. the tetup. coeff. rentaining smidl. Test rcmdu of
so In q as a function at temp. (ra go- SO-)
"
1"
p"
scin
d i
5
h
i
an
"s
T
=
e
n
s cover
grap
ng: (
.
10
li
o
Of
W
7 =180
styrene In pyridine; (2) toluene, 1% suln. at styrene
bnol
t
100
000
i
z0 0
. w
.
,
n toluene. 107, mAt. of styrene
)
(m
l
wt
IOOAK)O) i
l
10
u
.
.
n to
uene.
% solu. of styrene (mol.
A t. 4000) in toluene; (3) turpentine and 10% YAn. of Na
butaItirac rubl
i
t
i
4
f
ier
n
urpent
) traim-
ortucr oil and
ne; ~
uAn. of Na butadkuc rubber in tr"ortner ad; (5) me
17~,, turpentine and &1c;,, traustomer oil &nd a d.5" soln.
k"
of Na butadime rubber in this mixt. S. P& %%%rx coo
ARE
0 - S L A ACTALLURGICAL LITERATURE CLASSIFICATION
_T
------- _F I
A' a IF ;6,( Miff(W K[t?t It 49
o 0 0!0 0 0 0 * 0 0 0 0 0 0 0 0 0 0 a
:T41, 0 q ol~ go**** 0 0 0 0 00 0-k-9
too
ba.Lnv
'It,"141AL %VFW 0 0 V 'I IT 84 5 a 0 9 T
o :16 0 0 * 0 0 0 ID 0 0 0 0 6 0 0 0 a 0 0
0

& #I &1
F -'Q', !A - U" -M T I -- Z . L r I 0
004 .-W-A~hj- i"**IP*
MW9WdhIfiWU*U~tM' I. Cecil$ -60
00" -
sun" of w0harietric dkonnal "Pitedon an the viecado -00
go Go sohdas. 8, V. Ke"Mus" (Phys.-Ictli. lust,
And. W bwinvad), A r^A. Phyt. (UBA.R ) 14 "00
0001 741-MORO.-Wben cancludons on the kogtW oWJ 41
*0 9 rlgxlity of polymer mols. am derived truca the temp. .00
cod. d the Intrinsic vbwdty, thie coeff. sbould be eakd.
for a ca"tt. val. ctel". (mob. W 1. at the list temp.). '60
Ttw coeff. c". fur a const. wt. couca. e (tnols, Pcr Its.)
l .*0
- moft the rem.
dure" incrtiubtly from the Correct one, i
t~vv viscosity * varies t1th conen. A iNciverilent eq"-
be
i
h
d
i
U
T
l
i .0
on
.
t
er c an
s
0g V, - Q'r +
.
erapen
virs
%
d
f
i
V
*k*il
d
l
H
K
d

" ence o
w
.
uv
an
nce
.
9pu
ly.
N. -1.
-aj---
m-M
-irbe retail
juar
VO vLwwt
tj
.
.
y
P
j
: :
at a coast. e and dificreat tamps. is exprund
by log T, - log a + W lot ", go belux the Viscosity of the
000 solvent at the test temp., and a and is emsts. From the
f Coo
go 13 expt's. o
K. and S. x is O~O for polybobutylent in spktdk
no, 0.041 for butn6kalt rubbw fix machine oil (both within
the rance 0-100% 0
12 for butadiene rubber in kerosene

00 .
frown -PA* to IA'), 0.13 for 1% polystyrene in Wucne
a
*
from -83
to M
l OA4 for 10% polystyrene in pyridlue
Ean - 64, to 49-) Jand 0 U for pot N
i methacr
late
s
y
y
in acetone (frown to Th= 4 a 6 ittialler, o*

11 the temp. cat#. ofisof thesolvent. Tbetemp.
=a"intrinsic viscosity calcd. for a const. vul. cown.
-0
-O
OaM -0
0010
Is Par these systems O
OWG
0002
.
.
.
.
.
.
.
J
0000
d
3o 0
-
, an
-0.0012, temp. accept tar pobjobcyj,, I
the Pol
faer Ien
th d
y
eavases wben temp. rim.
s 0
J. J. Bilerman
tf* 41
A$$-$La atIALLUOMKAL LSTtlk7VAI CIAWFICATION a t% go

t. a.. cat aj&IjI C.C CO-V Alt
U Is AV 10 1%;
P 00 P 0 it to it x it K it it tt It K IF
A I TA 3 1
IS
000 0 0 0 * 0 0 000 0 0o 0 of go 0 a q 0 a 0 0 a 0 0 o1

SYIS-~EIN _N. I., Kobeko, P. P., Marey, F.I. (Deceased), and N. S. Ivanova
"Plastic Deformation and Viscosity of lee," nurnal Tekhnicheskoy Fiziki,
Vol. XVI., No. 3, 1946
Physico-Technical Inst., Acad. Sci. USSR, Leningrad.
Full Trans - w 583, 15 jun 1948

004
1
00 a
0* A
00 a
oe 'e
00 At
00
09
00
66
. ths, amorphous stele. dependence -J the ol#4trkal
cooducuTfly of undeftwed liqwdjl on prw"*, TIWIMP,
turg I Ito And N. 1. r A.
101, J. 1`tsh. "POW,
It.
Ruskian) .-In a cylladrical
botub 13 cm. in diAin.. ill c,o. long. wall thicknesis 5.4
c"t., permitting prrmurr, p tip to OLXIO atm., equipped
with a cylindrical inner clevitrode and proteefive ring to
pri-init rrsistivily lnca%tlmtlwnts up to 10' Ohm- cm-P
dello'. ;rrrc madr oil a fus,,sl 1: 1 (by wt.) mixt. of phenol-
phthadebt and salol. t'llilcr 3350 atm.. the dielec. coast.
Ooca,uml in I.e.) tvinaim coust. in the temp. range
I N) to UbLK1t frool wbegr it begins to inicreative
rtAn 1.
vrith further rising trulp.; the transition "I ds I
that frool tile Vor"na, to the liquid 6, and 'C".1 ,
ate &ct
ilictra-d f. k a '1011 of IhAt pollit (4) lit her te . b
M'. The I--- .., I"S 0 (.1'. etec. resist ty
inctraing p at co,11t. tetop. is line". the slope k. -
1,,) I(Vi, p/l)p 1W ilia iffeAter tile loymir the truip.: k - 1.4 X
,.,Cx it) latoi.tandI10%re.p. Glycerolshows;
iii;IrAr &I~lldeo- .4 1,4 0 on p. and about Ile
tuml of k between -M.4. nd _1MA.. The k
Values of ill, highly vi-to, liquid, are several Hill" as
high all those grnerully inificated by Bridgman for more
lit ternii of the vol.V. log P increases with
.&CTramilit r at at"ut tile 11111C rate as vnith increasing P.
A aivrn vArial ion of r, if br,might about hT, changing the
lotivil 'mm,, .1"ingly than I W same varia.
OW11 t-Ut!Wll by it VILMI(P J eg,. is b, ,
by InvAqurv. III voll.t. irfull., only all x 10 fold
hicovit- lit "I** Slli-t .1 .1 * Ill, IAJ
Ing Ito (hr .4 ite'NAtle lit ? A. hirvrll by .4 11"VA, lowrillid
of trulp, Coult.-P curvTO of kv P against 1/1' an shtficki
ticarly paralial to each other to hislirr I/ r with lucrriazing
p: flow I to 404 and from I to 1340 atm., the shifts in
Itpir are 0.12 And OM; at all three P. the slopes 0 log
/a(1/7) increase continuously with falling temp.
Const.-v curv-e- of 108 P against i / r air of the same n4-
ture as the const-p hut have a lesser slope And intersect
tile latter when plotted on the same I/ r scale. Between
two not too distant trrnp%. r, atilt Ek. (fir coeff. k (at
"lost.
71 will 0 0 1-6 0/00 / n (at ""W P) A"
I I - ( M-
hted by k/11 '.) I/P A
T') or. .1(1 i 71 he is I Ir 1.4,4 111"*o P, k., It -
Most.. i LO. k and B vury lit I fir 'kill'. A AV. 1,111. 1., 1. A... I
the contrast lit tile r9octs on 0 CA P Arid of (ellip., are Cyl-
drove of the deep differriter between the structural
changes brought about by comprr~om aod by thermal
contraction anif a challenst, to currem theories finkitill
Properties of Uquids essentially with change. of den%ity.
Tbon
MITALLUMKAL LITIRATI011111 CLASWKATON
sko" *"Inv
~_Oo
- 00
-90
lee
-00
lee
lee
lee
-00
11144111
=00
4490
goo
see
goo
are 0
1:0 0
see
goo
Not
0
goo
WOO
lb U N AV k0 AS i0ro 40 4-911me -0 o- It ne 0 a 9 1 W M 9 a a j 0
f
4 ooooo*eoo*OOOOO,. 0000e000000000
loooooooo*oooe.oo.oo-000000000000*000000

S I
U S S R
s. Denendeace of infra-
in lIquI
ectra of he 11 bond cii tempernturW"9E_ia,-__
,!kl. litod 1. 1. Novak. 7hur. Tekh.
r i7
weeestudied
bit the 1.3-1.7-p region o~ pore PrOff, hP.4yl d1c., heptyl
and Iloityl ule. alld 4.1 jilwlioljor their sOmq. 'in CCII, und uj
Cir at. preiinrcsup to I-k4 ik-7si~ A
CIIII Ck-o'l ralaps. 184W. The of 1~,so.-o, com be ~j
det'l. it oo% I lie inwi'lit y of ballel
groop~.- ai~bcd, hya I I h(aid, :wd b,iti;l 1.41 1, coem;panding
to "free" CH groups. A 1111ger it-juble spectrophotonvAcr :a
-isith a PbS cell was tised for the expls. The ~mnpfL w
plno?d undvi- hydranlic pm:,~,orv in CCIj; lim"i-cr, swc'!
CCIA ery~suwffizcs [it rolia, temp. at 1000 ktr./~i+ ctu.,
f 50% CS-_ and 50" CCIA wqs used at lt;glitr pressures.:
The change of Lite optQ density is 4D A t47* atid A D
DflAP, when er is the thermal expan%ion uW fi the comprts-!
sibility coLff.. D - koct, where k4 is the absorption per bond
c the vol. concn. of bonds, and I the thickness ot t he sample.
-For the temps..20-70' and pressures 1-02000 kg./sr, cm.'
;k� Is coast. The values -of La X 10- are 2.75 2,85- 2.8
'W.
and 3.9 sq. =,/mol.. resp.,- for PrOH: hexyl nit., hEptyl.
rhe conett.-dependent,const. k,. variu.
;a1c., and phenol.
i with tetrip. and pressure, this indicates a cliatG in the no.
-.1of Il.bridges. Increased pressure has the same effect.as.,
IdecreaseA-temp. decreasing the no. of h-ee OIT.grnitps.:
'-A change in temp. of V corresponds to CO-130,kg,/sq. I
en
f
:dmngc.- The slope of (ApIAT)k. is the same az~_tb~at o
z (ApIAT.), where T. !s the cryswi temjy.;:Jbj-_.9TAtes thht~
-jai conditions: of
err TI.-Occu. c ioA -
A rs at eq ta~,
M.-M ~Fr~_M_~74M_I

SI!I:17'rIKIIT, 1'. 1.
"Kinetic Prot-erties of Liquiis and Gases." Dr Phys-7,11ath Sci, Leningrad
m
Fhy31 CO t~~Cfltli Cal InsL, Aca-3 Sci US"SR, Leningrad, 1954. No 1, Jan 55)
Survey of Scientific and Technical LIssertations Defended at U:713R Higher
Elducal-,onai Institutions (12)
SO: Sum. No. 556, 24 Jun 55

Lm.~ .1 vi) nov Lc, h
CHISH-:1', Nikolail Ivanovich - Academic Oe,ree t)4,' D)i~tor of 1'h~7 f~i -,,)-?,lath empiti cp 1
C,
Ociences 'hased on his defense, 21 FelbrJary 1955, in the Courivil t r the Lerdri-rad
Physical and Technicel Inst Acad o'ci ',7E~_',R., of his dissertation entitled: "Kinetic
prxl,erties o'L fluir4is and glass." for the Academic Degree of Doctor of__'_-c-Lence5
S,': Byullet-cml Minist,7--rstva Vysshego _.:,ebruarl~,_ 1956
Decisims of the H,igher Ce tification Gomm_is,-dori Conc
ar~ Titles.
---,~_, S/'i'Y I 5~ I ~

USSR/Physics Vitrification FD-3034
C_~~rck -X/2 Pub. 153 - 3/23
Author Shishkin) N. I.
Vitrification of liquids under pressure. I: Dependence of volume
upon temperature and pressure
Periodical Zhur. eksp. i teor. fiz., 25, February 1955, 188-195
Nbstract The author presents experimental data on the dependence of the %101-
izae of supercooled liquids upon temperature and pressure. From
the character of the curves v=f(p) correspondinS to various temper-
atLu-es he determines the external pressures for which the liquid
vitrifiQs. He shows that vitrification of a liquid sets in for
hiZher temperatures than for higher pressures. The volume of the
liquid under the conditions of vitrification becom- mmller the
higher p and T. The author concludes that density increases during
vitrification that are pi-oportional to pressure are observable at.
even lower pressures, and compression of -he atoms or molecules in
this case does not possesz essential significance, the main cause
for the density increase beinG the decrease in the free s-3-ace be-
tween the molecules, i.e. decrease in free volume, the result of
the measurements consesuently indicate that the freE volume of the

Carl~ 2/2 FD-3034
substance situated under conditions for vitrification is less ~Ihe
higher the temperature and pressure and therefore is not an essen-
tial factor determining the condition for vitrification. Four
references: e.g. BridGman etc.
! -i tution : --
Su'b,mitt--:d : April 15, 1954

USSR/Physics Vitrification FD-3035
Card 1 2-D Pub. 153 - 4/2--
Aur,hor Shishkin, 11. 1.
Vitrification of liquids under pressure. II: Dependence of di-
electric permeability and relaxation time upon temperature and
pressure
Periodic-al Zhur. tekh. fiz., 25, February 1955, 196-203
AbstracL In part I the author presented data on the dependence of the vol-
ume of supercooled liquids upon temperature and pressure and con-
claded that the temperature of vitrification of liquids is en-
hanced with increase of external hydrostatic pressure, the free
volume during vitrification becoming less the higher the tempera-
ture and pressure. In the present part the author presents data
on the dependence of dipole polarization upon temperature and pres-
sure and thus obtains more accurate determination of 'the transition
of a liquid to the vitrified state, this data moreover allowing him
to determine the time of dielectric relaxation of the liquid. Ac-
cording to the author's opinion, there is no data in the literature
on the dependence of the relaxation tillie of liquids upc-n 71iressure,
such daLa being, neceosary for aa understand-inr__1 oF the -P A

Card 2/2 FD-3035
liquid which is being vitrified at high external pressures. The
author thanks M. V. El'konina and L. I. Rozgacheva, who partici-
pated in the measurements. He cites his earlier works: ibid.,
10, 1940 (co-authors: P. P. Kobeko and Ye. V. Kuvshinskiy) and
8, 1938 (co-author: same).
Institution : __
Submitted : June 4, 1954

USSR/Physics Vitrification FD-3036
Card 1/1 Pub. 153 - 5/23
Author Shishkin, N. I.
Title Vitrification of liquids under pressure. III: Dependence of elec-
trical conductivity upon temperature and pressure
Periodical Zhur. tekh. fiz., 25, February 1955, 204-216
Abstract In parts I and II the author presented data on the dependence of'
volume and relaxation time of supercooled liquids upon tempera-
ture and pressure, and showed that the temperature Tc of vitrifi-
cation of liquids is enhanced for increase of external hydrostatic
pressure and that the free volume for vitrification becomess less
the higher the temperature and pressure, the relaxation time of
the liquid during vitrification becoming constant. In the present
work, part III, the author determines the state of vitrification
of a liquid under pressure from the character of the dependence of
specific resistance rho upon temperature and pressure, and discusses
both the character of the dependence of rho on T and rho on p for
liquids and glasses and also the phenomenon of vitrification. He
thanks Professor Ye. V. Kuvshinslcly and Yu. N. abraztsov for dis-
cussion of the manuscript and M. V. El'konina. 11 ref.
Sub.-nitted June 5, 1953

SUBjECT USSR / PHYSICS
~IUITHOR 3CHISCHKIN , N . 1
TITLE The Dependence of
Glisses cr, Temperature,
PERIODICAL L-rn. techn- fis,
Publ. 7 / 19156
CARD I / 2 PA - 1207
'the Kinetic Characteristics of Liquids and
Pressure, and Volume.
267 1461-1482 (1956)
reviewed 8 / 1956
!,~,de-rn theories know no strict distinction between the mechanism of motion
of molecules in liquids and such a mechanism in solids. The dependence -:~f
kinetic chara-~:t,~ristics on temperature is in both cases expressed by the
aame f,~r-mulae. The amcunts of activation energies are not ascertained by
th~-sc- theories, b-at the latter offer the pcssibi1ity of a modification of
a--t-var.icn energries oil the occasion of, a modification of exterior conditions.
In the -oresent work hypotheses concerning the character and the extent of
the modific-atil-n of actLvation energy is investigated in dependence on
tpmperatiare., but also in dependence on exterior conditions. It is shown
the ac.-.i-ation energies computed according to the formula are lower
lor glass t1han f~,r liquids. This d---screpancy -was caused by neglecting inte-
rior The "Latter consist in the modification of Intermolecular
i.nterac-tion whish develops in a different manner in glass and in liquids.
n the case of glass these modifications are only sl4ght ani not
accompanied by a. reshuffle of molecules, they are considerable in the case
of 4uid,-,, and are accompanied by a reshuffle, The lower the temperature
of t'ae ijqt~id, the higher -s the degree of intermolecular interactionj the

L-J r11. -~Oflf!
?6, 1461-1482 (1956' CARD 2 2 PA - 1207
the time constant of relaxation~ the greater the activation energy,
It 14S sbown thar tne activation energy of kinetic pr,)::~esses and the equi -
co.,Istarts or rea-.tion are modified in accordance with temperature,
shows 'h%t a r-duction of the temperature of the liquid the
enerc;etic thresholds are increased as a result of the formation of new
relations Next, Eirin6ts theory is investigated with re-
spect, ta 11-,Ehly viscous and only slightly viscous li.quids; ~It Vlas found
t'--t contradictions ~:,ccur, which is indicative of the formal charac~ter of
t f o rmulae f or the entropy LL S * and the volume L v The theor,,,, of
Fr-kel. i_~ sub-;,z-cted to a close scrutiny with the result that the a~~tiva-
+ion ener- for d-Lffu5ion at a constant temperature of the liquid was found
.y
to Jncreage a linear tb 'he increase of 'he molecular vol-
law, i. e. Y;1 t, 4
'L,, m e , f t h ? d. Ji f lf un E mi o 1 e c u 1 e .Such a governing law is equivalent- to the
14, -z~a~- depend~_-nce of 'he activation energy upon volume. In conelus--ion, the
J,3pender),:e of kitie~ic properties on exterior conditions in liquids and Class
waT- Stated to be only a special case.
INSTITUTIONt': Ph.-.7sical-Technical Institute of the Academy of Science in the
U Lening-rad.

snsluml, [I-. I., Professor
'12lectric CoadUCtilrity of Solidified Glasses"
*At 3 COaf'~Mnce 0:1 Sl-'-40 ')4
v~ Nc- 7, f,13

SHISHKIN, N. I., TSEKHAXSKIY, M. I., Kh-UDOYAROV, K. V., and SUSLOPAROV, G. D.
"Use of Ca 45. "
report presented at The Use of Radioactive Isotopes in Analytical
Chemistry, Conference in Moscow, 2-4 Dee 1957
Vestnik Ak Nauk SSSR, 1958, No. 2, (author Rodin, S. S. )

SHISHKM, N.I.; VERSHINIffA, M.P.
Temperature dependence of the electric conductivity of polymers.
Fiz.tver.tela 1 no-5*7,98-802 my 159. (MIRA 12:4)
1. Fiziko-tekhnicheakiy institut AN SSSR, Leningrad.
(Polymers--Electric properties)

SHISIIKIIII 11. 1.
Vitrification of 14-uids nnfi DOI.ymers under pressure. Part 5.
Production of condensed glass. Fiz. tver. tela 2 no.2:350-357
F 160. (MIRA 14:8)
1. Fiziko-tekhnicheskiy iwtitut AN SSSR, Leningrad.
(Glass mantifacture--Chemistry)

- SHISIIKIZL,-N-J-;--,KO~IALICIEV, O.F. ,
Vitrification of liquids and polymers under pressure. Part 6:
Temperature dependence of the volume of condensed glass. .
Fiz. tver. tela 2 no.2:358-360 F 160. (MIRA 14:8)
1. Fiziko-tekhnicheskiy institut All SSSR, Leningrad.
(Glass manufacture-Chemistry)

S11 a 1 /62/004/010/006/063
B10�/B186
AUTHORS: Shishkin, N. I., and Milagin, M. F.
TITLE: Birefringence and the stretching of polymethyl methacrylate
aj
AS,
SU13A
Ca-rd
PERIODICAL: Fizika tyerdogo tela, v. 4, no. 10, 1962t 26al-2688
TEXT: To study the orientation processes in polymethyl methacrylate
(PMMA) the authors made stretching tests for establishing a relationship
between the elongation L and the birefringence [In. The latter can then
bp regarded a positive measure of orientation since it increases as the
an"isotropy of the polarizability of the molecules increases. Samples were
0
heated to 100 - 2001 C in a thermostat, and-were then stretched and cooled
to room temperature under a load. After removal of the load the
birefringence was measured at 20 0C in dependence on the degree of
stretching. The theoretical formula An - B(L 2 ii 1/L) (L. R. G. Treloar.
Trans. Far. Soc., 43, 277, 1947) is satisfied only for elongations ~ up to
25%, where 71 - (L - I)-100; B is a constant accounting for the anisotropy
of the polarizability and for the length of the.molecular chains. L is
Card 1/2

S/181J62/004/012/032/052
B125/B102
AUTHORS: Milagin, M. F., and Shishkin,._N..,-I.
TITLE: Breaking strength and birefringence of caprone and poly-
propylene fibers
PERIODICAL: Fizika tverdogo tela, v- 4, no. 12, 1962, 3578-3580
TEXT: Data on the correlation between breaking strength and birefringence
of caprone and polypropylene fibers are reported. The caprone fiber
samples were produced at room temperature by "cold" drawing of the non-
oriented fiber (diameter 0-04-0-07 mm)- Not all of the fibers had a
circular cross section. Various values for the double refraction (A n)
were obtained by stretching the fibers to various extents (from 0 to 350'/-)-
A polarizing microscope of the type MWH-a (MIN-8) with a Babinet-Soleil
compensator was used for measuring An at 200C in the center of the
samples. one end of the sample was clamped, whereas the other was loaded
at +200 and -195 0C, the load being increased until 'the sample fractured.
The breaking strength (result averaged from 10 to 30 measurements) of
caprone and polypropylene increases with increasing birefringence, at
Card 1/3

S/161/62/004/012/032/052
Breaking strength and ... B120102
first weakly and then more and more 0strongly. At -1950C the breaking
strength is much higher than at +20 C. The dependence of the breaking
strength a on the birefringence, as here detected, satisfies the empirical
a 6 n
relation a - 6 0e . LI0, the strength of the isotropic nonoriented fiber
and a are empirical constants involved.
0
k ZMM2
caprone -195 0, 20 44
polypropylene +200C 14 50
-1950C 27 50
According to the theory (see e.g. C. C. Hsiao. J. Appl. Phys.9 30Y 10,1492t
1959), the higher strength of the oriented fiber (in caprone at least
ten-fold) is attributed to the effect of the lateral chains of the
molecule, to partf.al crystallization in the fiber substance and to other
facts determined theoretically. There are 2 figures and 1 table.
Card 2/3

S/181/62/004/012/032/052
Breaking strength and ... B125/B102
ASSOCIATION: Fiziko-tekhnichbskiy institut im. A. F. Ioffe AN SSSR,
Leningrad (Physicotechnical Institute imeni A. F. 10'ffe
AN SSSR, Leningrad)
SUBMITTED: July 11, 1962
Card 3/3

S/181/62/004/010/007/063
B108/B166
AUTHORS: Milagin, M. F., and WiAhk~qj___N. I.
TITLE: Breaking strength and birefringence of stretched '(oriented)
polymethyl methacrylate
PERIODICAL: Fizika tverdogo tela, v. 4, no. 10, 1962, 2689-2691
TEXT: It was found earlier (FTT, v. 4. no.' 10, 1962, 2681-2688) that the
degree of orientation of polymethyl methacrylate (PMMA:) is no ezplicit
function of the degree of stretching. Since birefringence can be used as
art unambiguous measure of the orientation.of the molecules in PMMA it is
.used to establish a rela-;ionship between the orientation 0and the breaking
strength of PMMA. Stretched samples were'examined at 20 C, samples without
any stretching at -195 0C. A definite relationship between the breaking
strength a and the orientation or the birefringence 4n of oriented samples
was found: d = a 0(1 + aAn), where cT0 is the strength of the unoriented
sample, a is a constant coefficient equal to -1.3-10 in the authors,
experiments. There is nc relationship between the-strength and the degree
Card 1/2

S/181/62/004/010/007/063
Breaking strength and birefringence B108/B186
of stretching. There are 4 figures.
ASSOCIATION: Fiziko-tekhnicheskiy institut im. A. F. loffe AN SSSR,
Leningrad (Physicotechnical Institute imeni A. F. loffe
AS USSR, Leningrad)
SUBMITTED: April 21, 1962
Card 2/2

zcEsnc;i~ %a: APL-oo4650
S/0181/63/005/012/3453/3462
&-dshlcin W. I.; ~Iilagin, M. F.; Gabarayeva, A. D.
Mlolecular network and orientation processes in amorphous polystyrene
SOURCE: Fizika tverdogo tela, v. 5, no. 12, 1963, 3453-3462
T02IC TAGS: polystyrene, amorphous polystyrene, polyner, linear polymer, molecular,
r elasticity, birefringence
n
etWork,
ABSTR-ACT: The authors' purpose has been to study the processes of orientation and
stretching in linear polymers. The study was made on atactic unfractionated
polystyrene. Data were obtained on double refraction and elasticity for average
molecular weights of 9*lo4, 2-lo5, and 7,105. It was shown that in the temper-aturo
interval 110-160C, with specimens belng stretched for periods ranging from 2 to
1OU00 seconds in the region of linear strain dependence., highly elastic deformation
of the polymer took place, with no indications of irreversible deformation. It
was shown that Brewster's laii held under these conditions. The experimental dati
were considered in light of the kinetic theory of photoelastic. properties of
rubber. It was concluded that the number of stress nodes in the molecular network
Card 1/2

ACCESSION NR: Ap4oo485o
per uni olume of amorphous oriented polymer diminished markedly with rise in
tem.perature and passage of time (during interval of stretching) and with decreaze
in average molecular weight of the polymer. It was further concluded that, by
varying the conditions of stretching, unfractionated polymer samples and fibers
may be obtained that are oriented at the expens *e of all the molecules or of only
the large molecules in the polymer. Orig. art. has: 9 figures, 2 tables,, and 7
ormulas.
ASSOCIATION: Fiziko-tekhnicheskiy inst1tut im. A. F. Ioffe AN SSSR, Leningrad
(Physical and Technical Institute AN SSSR)
SUBMITTED: 25Jun63 DATE ACQ: O3Jan64 ENGL: 00
SUB CODE: PH NO REF SOV: 006 OTHER: 006
Card 2/2

ACCLSSION NR: A
P4034921
S/0181/64/006/005/1413/Ua7.
AUMORS: Uilagin, M. F.; Shishkin, No Ioj Gabaray-eva, A. Do
The change in double refraction during annealing of oriented polystyrene
tverdogo tala, v. 6,
no- 5, i~641 1413-1417
TOM TAGS: -'ouble refraction, polystyrene, annealing, hyperelastic deformation
1, U
ABSTRACT, The temperature and time dependence of double- refraction and hyperelasti6
d--formation during annealing of oriented samples of polystyrene were studied. It
wa~i found "hat the double refraction of oriented samples depends both on the anneal-
i,np_ ~empezn?~tum- and on the duration of Vie annealing process. 11hen samples witli
ends are annealed (for any fixed period of arwealing) the dependence of
1,eiativz degree of orientation on temperature is the same for all samples %,
oriont-ed undar -1--fferont conditions. As a result, complete disorientation of
,;arapie8 reaches completion at approximately the sama temperature. When annealitig
saraplas with definite lengths., the dependence of crientation on temperature for any:-LL
definite annealing period is different for 9=ples oriented under different
Ljondit~onse The same is true for dependence of orientation on duration of anneaUng
6,d

ACCESSION MR: Ap4o34921
'at some constant temperature. The temperature and duration of annealing for
complete disorientation are greater the higher the molecular weight of the chain
and the molecular weight of the polymer* In annealing,, as well as in pullingp
samples of a linear amorphous polymer may have simultaneously greater hyperelastic
deformation and practically no double refraction. Orig. art. hast 5 figures and-2'---
tables.
ASSOCIATION.- Fiziko-tekhnicheskiy, institut im. A. F. loffe AN SSSL, ioningrad
:(Physicotechnical Institute AN SWR)
;SUH41TTEDt 20Kov63 EKICLt 00,
!SUB CODEt MT, OP NO REF SOVt 002 OTHER2 0011'"':
2/2
Card
.... ........

Ut, 1:~:12fll lOffe
fling rac.

L 18246-65 EWT(m)/EPF(c)/DT(J)/T P.C-h/llr-4 RM
3
ACCESSION N
R: AP5000661 _S/0181/64/006/012/3636 639
AUTHORS: Milagin, M.P.; Gabarayeva, A.D.; Shishkins N.I.
TITLE: Rupture.strength and double refractionof pol
ystyrene
SOURCE: Fizika tverd,ogo tela,- V-161.no. 128 19641 3- 6- 3-6-- 3-6- 3 9
TOPIC TAGS: polystyrene, polyme'r.chain, polymer Lheolbqy rupture
strength
ABSTRACT: This is a continuation of earlier-,~rork (FTt v. 4
2681, 1962 and v. 5, 3453, 1963) on solid oriented
-polymers
whose properties depend on such parameters as the-nurd)er of chains
or knots of the molecular grid andalso themolecular weight.of
the chain. It was shown earlier (FTT v. 6, 1413, 1964 and v. 6
1413, 1964) that the rate of relaxation~of theoriented polymer
during the course of its annealing and drawing.is connected with
these parameters. In the present article the effect of these
Card 1/4

L 18246-65
ACCESSION NR: AP5000663
parameters on the rupture strength of a solid oriented polymer
is investigated. oriented samples of-polystyrene were produced, by
drawing samples of amorphous polystyrene at-a fixed.temperature and
for a fixed time, and rapidly cooling to room temperature under load...,...-,
The double refraction was measured-at 20C. The drawing conditions-
were varied in such a way that t e molecula5 weight of the chains
in the sample ranged from 6 x 10 to 2-x-10 The rupture:strength.-.',,-.....
of the samples was measured at 20 and -195C at an approximate rate,
of 100%/min. The results have shown that:the drawing conditions
are determined by a function whose parameters are the temperature
of the polymer and the time during which the-drawing takes place.
If the drawing conditions of the polystyrene sample are identical,
the molecular weight of the chain remains the same. :The variation
of the rupture strength with the double refraction is'shown in
Fig. 1 of 11-the enclosure. An analysis of-theresults shows that
the knots of the grid are defects which reducei the strength of
Card 2/4

L 18246-65
ACCF-9SICN NR: AP5000663
N
il 4
1 0
1 -V
. 10
Card 4/4
- I z 3
- -4n. 1172

7_~ ~7_41?6023391. /0601003/0323/03'29
'SOURCE CODE: UR 10374166
AUTHOR: Ph1sh1in, N. I.; Milagin, M. F.
IGRG: Mysicotechxiteal InatitiAe imi. A. F. lo"e, Aradd my- of Sciences Sssp,~
Leningrad iko-i
ekhoi _�k(Y justitut, AN
TITLE: Relax-ation processes i-n pob .rized amorphous polymers
'S'OUR CE: Mekhanika polimerov, no. 3, 1966, 323-329
I
TOPIC TAGS: polystyrene, stress analysis, stress relaxation, elasticity, tem-
perature test
ABSTRACT: The rates of relaxation processes in amorphous polystyrene are
examined. Three conditions are considered, i. e. , 1) with the sample under constdnt
stress, the elastic deformation increases with time, 2) if a prestressed sample's j
length is fixed, the stress drops with time, and finally, 3) if such a sample is re-
leased from the clamps maintaining it's length, the elongation produced is minimited
to zero with time. The concept of lattice structure in linear polymers is used in the
Card 1/2 UDC: 678-539. 32
ACC NR: AFbUZ3jv1 ic theory of rubber elasticity is
f experimental results. The kinet tress and deformation, and to
interpretation 0 lationship between the S and time
.-pplied to formulate the re elasticity and firefringence on the temperature
a endence of relaxation process in
express the dep ar mechanism and the rates of presented. The author
he molecul. jaental
clusions on t xpt-rir
Con jymers under application of stress and heat are luation of e
he eva
amorphous PO al participation in t7 [KPI
thanks A. 1. Gubanov for his person! 9 formulas.
results~~rig- ~arC has: I figure and OTHREF: 003
J.SIUB CODE' SUBM DATE: 1014ov651 o1RIG REF: 003
VIT
d

ALAMPIYEV., P.M.; ZHIIHMSKIY, M.M.; XUPT, V.S.; KONSTAFTIWOV, O.A.;
MMMOVSKIYY A.G.; S12EOKIY, B.N.; FEYGIN, Ya,G.; SHISHKIN,
_ N-1-4 YARITSKIY, F.F. -----------
letter to the editors of the journal "Izvestiia AN SSSR, Seriia
Geograficheskaia.ff Izv.AN SSSR. Ser.geog. no.6-.146-147 N.-D 162.
(MIM 15:12)
(Geography,, Economic)

FM'GIN., Ya.G., dolctor ekon. nauk, YANITSKIY, N.F., doictor geogr.
naW-; ZHDU-'.UII'SKIY, MJI.V doktor geogr. nauk; ALAIIPIYEV,
M.P., doktor ekon. nau~-~ KOSTFINIKOV, V~M., kand.ekkon.
nauk; BUYANOVSKIY, 11%S.1 kand. geogr. nauk; SHISHKI21 R-J,,
doktor geogr. nauk; MOSK-VIN, D.D., kand.e~on.-n
Ye.L- Icand.ekon.nauk; VOTROV, A.S., kand.geogr. nauk;
LlSETSKAYA, A.P.., red-.; POEOMAREVA, A.A., tekhn. red.
[Methodological problems of economic geography] Metodo-
logicheskie voprosy ekonomicheskoi geografii. Moskva, Eko-
nomizdat, 1962, 278 p. (MIRA 15:7)
1
1. Chlen-korrespondent Almderii nauk USSR i Institut ekono-
i.~L-d Akademii nauk SSSR (for Fenin). 2. Institut geografii
Akademil nauk SSSR (for Yandtskiy, Zhirmunski-Y, B'I~Vanavskiy).
3. Institut ekonomiki mirovoy sotsialisticheskoy sistemy
Akadenul. nauk SSSR (for Alampiyev). 4. Gosudarstvenn3rj na-
uchno-ekonomicheskiy sovet Soveta Vinistrov SSSR (for
Kostennikov ). 5. Nauchno-issledovatellskiy insti-tut truda
Gosudarst.vennogo komiteta Soveta Yinistrov SSSR (for Shishkin).
6. Institut ekonomiki Akaderiiii nauk SSSIR (for Moskvin). 7. Oren-
burgskiy pedagogicheskiy instivat (for Vetrov).
(Geography, Economic-11"ethodology)

SpISIIIm;, N.I. ___
Redirectinu the Vychepda and Pechora River runoff's into the Volga
B;7,sin. Izv. AN SISR. Ser. geog. no.5:86-94 S-0 '61. (MIRA 14:9)
1. Nauchno-issledovatel'skiy institut truda. Goskoiiteta Soveta.
Ministrov SSSR po Aioprosam truda i zarabotnoy platy.
(VycheFda River--RpFulation) (Pechora River--Regulation)
(Volga River)

ISHISHKIN NJO~A~ c
, ~~* 4; MARGOLIN, Ya.A., red.; KOITOVALYUK, I.K.,
, 'Y'_
__ shly red.; Gbi.ITSYN, A.V., red.kart; KOSHMVA, S.K., tekhn.red.
(The Komi A.S.S.R.; economic-geographical features] Komi ASSR;
ekonomiko-geografichoskaia kharakveriatika. Moskva, Gos.izd-vo
geogr.lit-ry, 1959. 222 p. (MIU 12:12)
(Komi A.S.S.R.--Bconomic conditions)

SHISIMIN. N.N., red.
[Instructions 246-54 for checking standnrd *hroncmeteraj In-
struktsiia 246-54.po p'overke obraztaovykh khrononetrov. Izd.
ofitsial'noe. Moskva, 195?. 36 p. (11IRA 14:5)
1. Russia(1923- U.S.S.R.) Komitet standortov, mer i izwri-
tel'nykh priborov.
(Chronometer-Testing)

f r I
BIRMOVSKIY, V.Ye.; VASILENKO, M.I.-, VELU;R, R.L.; VERBLOVSKIY, A.M.;
VERNER, B.F.; VOYDALOVSKAYA, Ye.N.; VOL'SKIY, A.N.; GLAZKDVSKIY, A.A.;
GRANOVSKIT, B.L.; GREYVER, N.S.; GUDIMA, N.V.; DOWOPOLOVA, V.I.-,
KARCHEVSKIY, V.A.; KOVACHRVA, Ye.B.; kqMYAVTSEV., P.S.; IMBEDEV, A.K.;
LISOVSKIY, D.I.; LIKHNITSKAYA, Z.P.; MATVEYEV, N.I.; MELINITSKIY, A.N.;
MIRONOV, A.A.; MIEIDMVA, A.A.; MURACH, N.N.; OKUN, A.B.; OL'KHOV,N.P.;
OSIPOVA, T.B.; PAVLOV, V.P.; ROTINYAN, A.L.; SAZHIF, N.P.; =YUKOV,N.N.;
SIDOROV, P.M.; SOBOL', S.I.; KHEYFETS, V.L.; TSEYN-ER, V.M.;
SHAEHNAZAROV, A.K.; SHEYN, Ya.P.; SHE-TU2M'YL'V, S.D.; SHERMAN, B.P.;
SHISHKIN, N.N.; SHLOPOV, A.P.
Georgii Ivanovich Blinov. TSvet.met. 28 no.6:62 N-D 155.
(MIRA 10-11)
(Blinov, Georgii Ivanovich, 1911-1955)

SHI SHKIN, - 9. N. _ ~
I -
mAtlas of ore structure and textures." S.L.Taldykin, N.F.Goncharik,
G.N.Enikeeva, B..B.Rozina. Reviewed by N.N.Shishkia. Zap.Vaes.min.
ob-va 85 no.1:122-124 056. (HLRA 9:7)
1.Ruano-gaolagicheakaya laboratoriya inatituta Giproutkell.
(Ores--Classification)(Taldykin, S.I.)(Goncharik, N.F.)(Inikeeva, G.N.)
(Rozina, B.B.)

AUTHOR: Shishkin, N. "N.
TITLE: Some Data on a Hi&ily Nicke2iferous Variety of Cobaltite
(0 nikelistoy raznovidnosti koballtina)
PERI'JDICAL: Doklady Akademii Nauk SSSR, 1957, Vol. 114, 11r 23 PP-414-415
(USSR)
A3STRACT: As it is known, cobaltite contains 20 - 34 ~o cobalt, 2-3 7-")
nickel, and 1.6 - 10 ~b less frequently up to 16 % iron. In
this latter case, one speaks of the strongly ferrifemus spe-
cies of cobaltite, namely ferro-cobaltite, but this distine-
tion is sometimes questioned, because analytical investiga-
tions have failed to confirm the high percentage of iron.
During his research work on cobaltite from the Altai Mountains,
the author of the paper under review has found a highly
nickeliferous variety of cobaltite, with reduced contents
of cobalt and with differing optical properties. Some time ago,
a similar discovery was made in the Ural Mountains. Vladimirovskoy*e
the d6posi-tw-whae the highly nickeliferous variety of cobaltite
Card 1/2 was found in the Altai Mountains, is situated in the "skarns"

Some Data on a Highly Nickeliferous Variety of Cobaltite 20-2-50/60
of the 11exocontact of the diorite intrusion" and an effusive-
-sedimentary mass of the mid-Devonian. The form of the cry-
stals is octahedral, pentagonal dodecahedral, and combination
of cube and octahedron. The highly nickeliferous variEty of
cobaltite has a somewhat brighter pink color than normal co-
baltite, with a violet shade in reflected light. The present
paper lists additional properties of the mineral variety under
consideration. On bais of the above, together with other data
published so far, it can be stated that tbwe exists a nickeli-
ferous variety of cobaltite. Because the existence of such
a variety confirms the wide boundaries of isomorphism bet-
ween cobalt, nickel, and iron, this discovery is of great
scientific interest, and it also may be of interest from the
point of view of its use in practical work. There are 1 table,
and 5 references, 4 of which are 80vi6t.-
PRESENTED: November 15, 1956, by A. G. Betekhtin, Member of the Academy
SUBMITTED: November 15, 1956
AVAILABLE: Library of Congress
Card 2/2

Shishkin, N.N. SOV-11-58-9-1111'14

TTTLE: "Cn Conditions
Few Comments on the Article by D.C. Ontoyev,
of Localizstion of Nickel-Cobalt-Arsenide Ores in the Carbonate
Veins Between the Sksrns" (Neskollko znmechaniy po povodu stat'i
P.O. Ontoyeva "0b usloviyakh lokalizatsii nikell-koballtovykh
arsenidnykh rud v karbonatnykh zhilakh sredi skarnoV~
P--RIODICAL: Izvestiya Akademii nauk SSSR, Seriya geologicheskaya, 1958,
%r-9, p 100 (USSR)
ABSTRICT: The above-mentLoned -.rticle by D.O. Ontoyev was published in
~,~r 9 (1957) of this periodical. These ores were discovered
'IT
by V.A. Unksov, G _ Ivanova, A.A. Bogomol and V.A. Bobrov in
Khovakhsy of the Tuva Autonomous Oblast'. Since then these
deposits wdre studied by V.I. Pondarenko, S.N. Kondakov, Ye.G.,
Starostina, R.S. Tarasova, N.A. Tikhomirova, Ye.I. Nefedov
IVSEGEI), !,'arkinav A.Ya. Vclzhenkova, A.P. Polushkina
(V!,','3) , N.-1. Shishkin, A.Ye. Aleshunins, V.A. 14ikhaylova
(Ijipronikell), 1-.A. Frutov, L.K. Yakhontova, A.A. 3odovikov
(Y~`,U) and L.I. Gavrilova (Uralmekhanobr). The results oll their
research were pullished in a series of articles (Ref. 6).
Card 1/~

SOV-11-58-9-11/14
A Few Comments on the Article by D.O. Ontoyev, "On Conditions of Localization
of Nickel-Cobalt-Arsenide Ores in the Carbonate Veins Between the Skarns"
D.O. Ontoyev did not take into consideration .heir findings and
treated many facts incorrectly or even wrongly.
There are 6 Soviet references.
1. Nickel cobalt arsenide ores--USSR
Card 212

AUTHOR: Shishkin, 11. 11.
SOV,1'2o-121-4-41/54
TITLE: Julukulite - a New Cobalt 111ineral (Dzhulukulit - novyy
kobal'tovyy mineral)
PERIODICAL: Doklady Akademii nauk SSSR, 1958, Vol. 121, Nr 4,
PP. 724 - 726 (USSR)
ABSTRACT: A.I.Igoshin handed over a collection of minerals from the
Dzhulukullskoye ore deDosit to the author; in this collection
the mentioned new mineral was contained. This deposit lies
in the southwestern Dart of the Tuvinskaya Autonomous Area
10 km north-east of lake Dzhulu-Kull. The rocks containing
the deposits are metamorphosed porphyrites from the Cambric-
Ordovician (? ). The mineralization is restricted to zones of
hydrothermally changed rocks along short strata in a north-
east and a north-west direction. Julukulite forms small
disseminations and veinlets up to 2 mm and nests of 2-2,5
cm in size in short quartz ancherite veins. It occurs together
with tennantite, glaucodote, pyrite and bornite. Is fine
crystalline ag~re-ates are grey and shine like metal.
U 0
Harc'ness = 6, the crystals are octahedric, size = 0,008 to
Card 1/3 0,3 mm in most cases 0,00'. Also grains and aggro-ates of
0_ -

Julukulite a New Cobalt Mineral SOV/2o-121-4-41//54
irregular shape occuln. On polished sections the mineral
is greyish white in incident light. In single crystals and
druses sometimes a very weal-, anisotropy is observed: The
color changes from liEht yellow to grey. Zones are visible
in the crystals: In the case of etching with HITO3 the
fSreyish white zones are i.,iore t-apidLy etched and become black.
The Spectrum analysis showed minute admixtures of antimone,
silver, bismuth, aluminium, Ma,rnesia, calcium, traces of lead,
zinc and manganese. Table 2 reveals the results of the X-ray
structural analysis. The size of the new elementary cell
is close to that of cobaltine and Jerstorffite. The nickel
content of julukulite is higher than of nickel cobaltine. The
new mineral may be re,,,:arded as a transitory product between
~7
cobaltine and g;rerstorffite. There are 2 tables and 7 refer-
ences, 6 of which are Soviet.
ASSOCIATION: Proyektnyy i nauchno-issledovatellskiy institut "Giproniklell
Leningrad (Leningrad, Planning and Scientific Research Institute
Card 2/3 "Gipronikell 11)

SHISHKINJI IJ-.11.
Gersdorffite from the Butrakhtinskoye deposit (Khakass
Autonomous Province). Zap.Vses.min.ob-va 90 no.5:588-591
,61. (IiIRA 14: 10)
1. Institut "Gipronikell", Leningrad.
(Khakass Alitonomous Province--Gersdorffite)

SHISHKI-A, INI.M. -
hiF!hly cobaltous variety of glaucodot. Zap. Vses. min. ob-va 91
no.1:102-103 '62. MRA 15:3)
1. Institut "Gipronikel'", Lenin rad.
Gaucodot)

IIIAI~
Cc-pp,~r-n-',-'r-eL sulfide mineralization of baoic and ultrabasic
rocks ip the Yokc-,Dolyrenskiy Massif. Geol. rud. mestorozn.
6 no. 1: ~713 -98 7-F 1`4- ( M.:-m-k _7 7 -. I L)
Ja 0
1.. tia,,~~~-~ino-issi-edovate.1'skiy i proyektnyy institut "Gipronikell",
Lernirgrad.

ShISHKINY N.N.
Gene~,~c t, -S Or bait and cobal~--bea-r-'n-v, ore deposits
I c0 I - c
and s Lme Ic a ue ~U_
0 IT-ar c' ristics of their mineralogical compos"on.
Sov.geol. 8 no.11:34-45 N 165.
('MIRA 19:1)

~5 H 1 11: ji K ! 1; , 11 , ' , ; j')-PjfT JjA , Yi~Ye.; SHCHFRBA, GA.
i
i I e v -;, P, ws and bibliography. Zap. Vses. min. ob-va 94 no.4:477-
),~i5 16 C~ (MIRA 18z9)
1.
1, Naijchno-issledovatellskiy i proyektnyy institut "Gipronikell",
Leningrad (for Shisnkin). 2. Leningradskoye otdeleniye
Mateniaticheskogo instituta AN SSSR imeni Steklova (for Demina).

KORCHAGIII, A.I., master; MUSHINSKIT, A.R,, master; BHISHKIN,
master
Useful book ("TE3 diesel locomotive" by X.A.Shiahkin and
others. Reviewed by A.I.Korchagin, A.R.Mushinskiy, N.P.,
Shishkin). Zhel.dor.transp. 41 no.11:92-93 N 159.
(MIRA 13:2)
1. Depo g.Orsk.
(Diesel locomotives) (Shishkin, K.A.)

(Uhe role of Ln t.,ie cri.-in of li.~Jitnin.,-- cLLsch.-a,,,.e:;. 1) llol'kca---ulLab,-ii
voCli-aiw1kh kaneltv vozni~z-no-venii --rozovv.,zil razriadov. !.
3 3-R. 3 !A CG., ~A-,7- a, Sli'~,J "'L-7Z I "SLU 10( h
(Translation does not include biblior-raphy.)
t,

I,.S~_TSHi-jj-', ". S.
2. ussR (6oo)
"Forr.ation of Gells on Snow Surface."
Izvestiya vseseyusnogo geograficheskogo obshchestya, Tssue 1, 1948 (90-91)
9. -ete-Drologiya i Gidrologiya, 1,10. 3, 10,49. IM Report U-2551. 30 Oct 52

UM/Geology Mar/Apr 1948
Soil Science
Arctic Studies
"The Role of Convective Circulation In the Formation
of the Cellular Forms of Mic~orelief," N. S. Shish-
kin, Central Geophys Observatory, 5 pp
Izv Akad Nauk SSSR, Bar Geograf i Geofiz" Vol XII,
No 2
Argues against Loy's and Gripple theory of oonvec-
tion, based on acme cellular forms of microrelief
discovered in the arctic and the subarctic. Sug-
gests that with the aid of the theory of convective
circulation it is possible to explain the regular
4.IT42
-(Ccntd) Me6r/Apr 1948
construction of all cellular forms of microrelief,
,which appears in very moist soils. Among these
forms are polygons, squares and hexagons. Submitted
by -Academician A. A. Grigorlyev, 29 Mar 1947.
Ab
41T42

0 7_~ I
USSR/Motecrological Research YI&y1Jun 1948
Clouds
"The Problem of the Development of Droplets in Clouds
and Fogs," N. S. Shishkin, Main Geophys Obs, Lenin-
grad, 5 pp
"Iz Ak Nauk SSSR, Ser Geograf i Geofiz" Vol XII) No 3-
Discusses question of the coagulation of droplets In
clouds and fogs due to variation in the speed Of fan
Theoretical method to calculate the grovth of drops
during their continuous distribution. Data obtained
theoretically conforms favorably to data obtained frcm
microphotographic analysis of drops. Submitted by
Academician L. S. Leybenzon 29 Jkr 1947.
Jim 66795

S. PA 53/49T94
USSR/Physics Sep/OCt 46
Atmosphere
Convection
"The Interconnection Betveen I-olegul Turbulent,
and Convective Heat Conductivity, N76. Shishki-n.
Main Geophys Obs, Leningrad, 9 pp
"Iz Ak Nauk SSSR, Ser Geog i Geofiz" Vol XII, No 5
Considers men'banism of thermal convection in liquid
or gaseous media and compares it with molecular and
turbulent heat conductivity. Detailed study of the
problem of vertical convection currents in the at-
mosphere. Substantiates gradual character of con-
vection in the troposphere and suggests a theory
9f the origin sf mmali. Lb-Jitted by Acad L. 5.
Leybenzon, 3 an 45.7
Aw 53/49T94

SHISHKIN, N.S.
Calculating the inte-nnity of preciPitntion from rain clouds.Trudv
GGO n0-13:78-88 148. (MIRA 10:1)
(Clouds) (Precipitation (Meteoroloj7))

SHISHKINY N. S.
iA 5)ii2~
USSR/Ge;jr -hy --jan#eb 19W
-ip
"Formation qf Honeycomb on the Surface of Snow," N. S.
Shishkin, 11 pp
"Izv Vaescyuz Geograf Obeh" Vol =, No 1
Briefly discusses cause of the Interesting phenomenon
of formation of honeycomb pattern on the surface of
anow in mountain areas during su=mer.- Such fcraaticn~
caused by unstable condition due to the difference In
twDerature under the surface of the anov an& the air
over the surface of the snow.
J
51T22

HrQ HYL.,i) PA 37/49T87
USSR/Geophysics Feb 49
Rain
Meteorology
"Precipitations and Thunderstorms," N. S. Shishkin,
4 pp
"Priroda" No 2
Treats under: (1) clouds and their development,
(2) precipitations, and (3) mechanism of rain forma-
tion, thunder electricity. Includes two graphs.
37/49T8-7

VO
Metecliolegical Abst.
V01-4 No- 5
May 1953
Miscellaneous
Appliep tions
55 1.594.25:551.574.1:551.515.41
Sh=-fikN. S., 0 zarlade kapel' v grozovykh olslakakh. [oil the charge or drops in
thundettlauds.] U.S.S.R. Glawtop Uprat,lenie GidrottittenrolagicheikA Sluzkby, Informa.
Isionnyl Shormik, 1:47-54, 1951. 5 figs.. 8 refs., 17 eqs. DLC-Calculation of the coagulation
cliarze or drorm in i DoIYtJiqPrrqe Onm "'i h an a cc Or! t cam. The primary stage In drop
I L . 'I
growth is attributed to water vapor r.,,d ", ; is. n.' elopment Is very quick at the
outset and slowq down with increasing drop size. After reaching a size near 201A the further
growth k much affected by coagulation. The calculations made by the all thor show the most
rapid growth of the drop charge in the layer 600-1200 m above the base of the cloud, when the
:.speed of the asccnding qtream is I iu/sec. Charges of the order of 10-1 CGSE arc! obtained at
the height of 2.5-3.5 kin over the clowl base (3.4-4.5 km above the ground surface). While
failing from this height to I kilt abnve the cloud base, the charge of the sizable drops and the
speed of growth increase rapidly and therefore the author considers this layer as the most
probablearea of the origin of thunderstorm electrical phenomena. The freezing of drops does
not essentially change the restilts. A brid summary of measurements made from airplane by
ROSS GuNN. (Physi(at Rrvi(-,v, 71:181, 19-17) concludes the paper. Subject Headilips:
1. Drqktharge -2. Thunderclouds 3. Drop growth 4. Thunderstorm electricity. 1. Gunn,

U M7 .1NE HY ~-R.J
3 - 5 5'.'4. It ',I. '17o. 11
JU21~kljiv U 30'1i~inli oblachnyk:i kapell. (Coaleucence
:"r rl-t.d rm-latm.) Laninorart, (jltvn.%i.,% Georizichenkaia Ubservatori i a,
lrudy, 'k llb~:27-38,1951- 3 fivm., 7 tabl,.-3, 8 refs., 28 n?',:Itlons.
.',"ter a brief, theoreticAl disduesion,*of thevgrowth- of 'raindrops
t,y conjens-Itirn, the aut.t,or pr-sents a theoretical anal5-513 of tle
mechnni3m. or con!"scende. The discusnict, covers rollisicr. of
-1ro IWn In t!e field or 9mvity, and the coalesxence of Iro,s -during
nulJuri ir. O~v vfylocit.~ cf air flow rind durir-.,- peri-dic chvige3
in the velocit. %~r rl,,w. .;ublect Ileadingsz 1. L~rv- accretion 2.
. I I -Scence.
. riv -, ~' . 5's 30 1 -"L

~.5-237 5SLI,
Lsadki iz konvektivriykh oblakov. (Precipitatim
f'rc--. !_nvocteve- c1 uls.. Uninggr-td, 'ilim-d-i Geofiziehe-:kaia Libservatorila,
7r--d,., No. 1951. 3 r1rs., 2 tabl,!s, 9 refs., ll~ equations.
:)U,'- -k thccrctlc7~1 -Inve5tiration of the growth of !ro:?s and -, calcL;lation
of -'r-_c!,-it tion f rorn clouds in WI!10% , he
of s,-a- irapor pressure and radius of the dr-,7r, v%r~- wit*- height,
approx1p loris. 1he author do-no.-.!3Lr tee
.~jte4~- -is w~ler natural ccndit'
-.r-cedure for tlx- t-,rawth of dro;,!3
-,i;rt:;; cliuds am! the nLober of raindro-)s an! the intensity
of -ind dis,-i.!sses the uouth of Particles 1:,, clouds
.-a+er 14: the n(,11,1 -hriia. -Jub,',ect It eadLngss 1. Prcclpit,'ILI(~n meC~;,viism,
roT ic,!reLion 3. ~onvective clouds 4. loud physics.- I.L.D.

N
USSR/Meteorology - Precipitations Nov 51
"Investigations of Processes of Formation of
Summer Precipitations," N. S. Shishkin
"Uspekh Fiz Nauk" Vol )MV, No 3, PP 313-356
Investigations of microstructure of clouds started
in ussR in 1935. in 1946 aircraft investigations
were performed by Ye. S. Selezneva, V. A. Zattsev,
I. I. Chestnaya, A. M. Borovikov and others. Drop
distribution in clouds shaved increasing size-with
altitude. Describes radar search of storms in US.
Shishkin performs some computations of the forma-
tion of drops andp;ecipitations.
194T83

SHISHKI14, N. S.
PA 237T51
USSR/Geophysics - Rail Nov/Dec 52
"Investigating the Growth of Spherical Hail," N.S.
Shishkin, Main Geophys Observatory imF-.ni Voyeykov
"Iz Ak Nauk SSSR, Ser Geofiz" No 6, PP 73-78
Considers process of hail formation As a result of
freezing of cloud drops in ascending cloud move-
ments and concomitant decrease in temp. Describes
dependence of characteristic elements of the phe-
nomenon (velocity of hail growth, si-,:e of its
particles, time of cloud's existence necessary for
precipitation) on velocity of ascending currents.
237T51

USSR/Meteorology - Simmer Precipi- Jul 52,
tation
"Theory of Aestival Precipitations," N. S. Shishkin,
Cand Phys-Math Sci, Leningrad Main 6dophys; Gbs imeni
Voyeykov
"Meteorol i Gidrol" No 7, PP 17-22
Outlines theory of processes occurring in an aq
cloud with an even, continuously rising flow.
States that although this theory is not yet ccir-
plet-. it nevertheless allows one to clarify the
basic phys haracteristics of processes of formation
230T82
of pptns, Brief,2y discusses role of appearance of hard
spherical particles in the initial cloud Finds
investigations of arbitrarily shaped ice particles
within the cloud are more complex, but the govern-
ing laws in this case do not differ essentially from
the previous ones.
W
E-4
PL.
230T82

USSR/Geophysics - Hydrometeors Jan/Feb 53
"Some Physical Laws Governing Phase Conversions of
Hy~rometeors," N. S. Shishkin, Main Geophys Olas
"Iz Ak Nauk SSSR, Ser Geofiz" No 1, PP 78-82
Discusses quant laws governing processes of melting
and freezing of hydrometeors originating during
diffusion transfer of water vapor from particles
to the medium surrounding them. The author finds
the value of the melting threshold of ice particles
and freezing threshold of water drops for abso-
lutely dry air. Thanks N. P. Tverskaya, V. D.
Tret'yakov and V. Ya. Nikandrov.
F.A 2
241T37

PHASE I TREASURE ISLAND BIBLIOGRAPHICAL REPORT AID 450 - I
BOOK Call No.: QC921.S47
Author: SHISHKIN, N. S.
Full Title: CLOUDS, PRECIPITATION AND THUNDERSTORM ELECTRICITY
Transliterated Title: Oblaka, osadki i grozovoye elektrichestvo
Publishing Data
Originating Agency: None
Publishing House: State Publishing House of Technical and
Theoretical Literature
Date: 1954 No. pp.: 280 No. of copies; 4,ooo
Editorial Staff: None
Text Data
Coverage: This is a study of physical phenomena occuring in clouds and
leading to the formation of precipitation and thunderstorm electricity,
and an account of the principles of the quantitative theory of these
phenomena. The author examines the investigations of foreign scien-
tists. The author expresses the opinion that Soviet investigations
are frequently ignored by foreign scientists. The introduction pre-
sents a short historical sketch of the development of this branch of
meteorology. Names of Russian and foreign scientists, descriptions
of their methods of investigation and instruments and accounts of
their observations (with date and place) are scattered through the
book.
1/2

Oblaka , osadki i grozovoye elekt--ichestvo AID 450 - I
Th e book is provided with illustrations, tables and charts.
TABLE OF CONTENTS PAGES
I ntroduction 5-11
Ch. I General Information on Clouds and Precipitation 12-60
Ch. II Modern Methods of Investigation of Clouds and
Precipitation 61-8o
Ch. III Structure of Clouds 81-102
Ch. IV Laboratory Investigations of Processes Leading
to Precipitation 103-127
Ch. V Condensation Growth of Cloud Particles 128-159
Ch. VI Coagulation Growth of Cloud Particles 160-179
Ch. VII Phase Transformations of Hydrometeors 18o-197
Ch. VIII Fundamentals of the Theory of Summer Precipitation 198-235
Ch~ IX Electric Structure of Clouds 236-256
Ch. X Fundamentals of the Theory of Thunderstorm
Electricity 257-273
Purpose: The monograph is intended for meteorologists and geophysicists,
scientific workers., teachers in universities and technical schools and
graduate students
Facilities: None
No. of Russian and Slavic References: Total 156, 93 Russian
Available: Library of Congress.
2/2

'S HI S y A,/ /V, Y. Y,
Tiss-R/1-leteorology - Rain
Card 1/1 Pub. 86 - 15/37
Authqrs ! Shishkin, N. S.
Title : Dimensions of rain drops
Periodical : Priroda 43/10, 90-92, Oct 1954
Abstract : Methods of measuring the sizes of rain drops are described and explanations
are given for the difference in size. The formation of hail is also dealt
with. Two Russian references (1953 and 1954). Graphs.
Institution :
Submitted :

SHEMKIN, N. S. and BUDnOVA, Ye. P.
"Computations of the Quantity of Condensed Moisture in Convective Clouds;'.
Trudy Gl. geofiz. observ., No 47, pp 49-52, 1954.
A method for calculating the water capacity with the aid of the
aerological diagram is proposed by the author. From the diagram is
found the change in specific humidity of saturated air during ascent
along the wet adiabat. This change represents the ouantity of mois-
ture (in grams per kilogram) which can be condensed in a given layer.
The possible water content (in grams per cubic meter) is found by
division of the amount of the change in humidity into the density of
air. Since the water content depends upon the height of the base and
upon the temperature at the level of the cloud base, such computations
are carried out for various initial conditions.
The water content of clouds at first increases with altitude, and
then decreases the faster the lower the temperature of the cloud base;
here the dependence of water content on temperature of the lower base
is practically linear. Theactual water conttnt of clouds can deviate
from the computed in consequence of deviation of the vertical tempera-
ture gradient in a cloW from the wet-adiabatic, the evaporation of
drops from the cloud's periphery, md the displacement of cloud masses
1/2

of various density,,md also in consequence of the fall of cloud parti-
cles and precipitat4 on. The latter three factore can substantially
change the magnitude of the computed water content. The largest ratio
of computed and actual water contnes evidently can be observed in the
central portion of rapidly developing convective clouds.
(RZhGeol, No 9, 1955)
SO: Sum No 884, 9 Apr 1956
2/2

:ilT.-,T`!:TT 1., T;
'-J~-_Ieous Clouds in t'lle of Lcialn,rad"
1;7, 1954, 53-5'
or 5 n
)e uresent o:' t-wc 'li~;hts in ne Ler.~ngrad re, I
--)12 fcr t'le stud,. of c~ouecus clcuds tllaalz ~L.,c intense
5~ i c,--7 clcu-ly slrzst~-i-as of tllern-.al -fronts t"a-'t 1n-
-7. tk c -a cor,.! inr', t1l,e didt.-rilbution the abst~ncc of ice
7,7~d ~=VC~t.4 Of ~_ ClOlldV 57_~-Ste::! Of a COld --F'rCnt. CC:---
nt -rec-T.Dite.-
t,'~-. e c, 7, b I c"' -fall-o-at o f s u ff I c, i e t, t 1 v -2nse
C LoM.5. Tho Fizes of the rain drops neex the
earth reached '0.7-t).~) 1~*-m wli,-7i *' li.-~ i." %,- w' : *:v~ -l', -i vms of th2- order
of' :mm/hcur. 'VIdi'ional ;nvesti,-ation o' 'Ps clouds in January 1950
onfirmz -'Ih-c no,lsibilit~.- of he Tall-ott, of pz-~c-T)Itaticns In the fluid
-..,in',~-r NZIlGeol, No 9~ 1955)

V C 1: 0 t! J 3 Z' ~Ui r C f t
G. sr, r -,,r r3,1 j t ze o c u..-
j U 0 E~ wo :,,ete.- r
v.- r -"CLI! ve luc r C!"
L.Ijnnj

SHISHKIN, N. S.
"Data of Certain Measurements of the Size of Drops of Storm and Shower Rains".
Trudy G1. Geof'kz. Observ., No 47, PP 94-95, 1954.
Results of systematic measurements of the sizes of raindrops, which were
carried out in 1952-1953 in Leningrad, are briefly expounded. Under investigation
were 16 storm rains and 45 showers without thunderstorm phenomena. The
measurements were conducted by the filter paper method. Comparing the size distribution
of the drops for storm and shower rains the author arrives at the conclusion that
storm rains differ sharply according to total spectrum from nonstorm rains.
The mean value of the maximum radius of drops for storm rains according ot
1952 data amounts to 1.5 mm and for shower rains it amounts to 1.0 mm; corresponding
values obtained in 1953 are 1.8 and 1.2 mm. The maximum size of drops in storm
rains is 2.6 mm. It is confirmed that out of 4,204 drops in storm rains the radius
of only 10 drops exceeded 1.5 mm. Hence in the author's opinion it follows that there
are no grounds for condisering that the Gezekhus effcat plays the main role in the
development of storm phenomena. RZhGeiol, No 11, 1955)
SO: Sum No 884, 9 Apr 1956

SHISHKIN, N.S.
Effect of size distribution of cloud particles on the size of rain
drops. Trudy GGO no-54:78-80 '55. (MIRA 9:8)
(Drops) (Rain and rainfall)

SHISHKIN, N.S.
Using the layer method for forecasting the vertical force of
convective clouds. Trudy GGO no-54:96-102 '55. (MLRA 9:8)
(Glouds) (Atmospheric temperature)

SHIISHKIN, II.&. .. ~ .
Study of sky condition" producing precipitation in the form of
snow. Trudy GGO no.57:111-112 '56. (MIRA 10:1)
(Snow) (Clouds)

SHISHKIN. N.-S.
Some results of sttid7ln.- storm and rain clouds. Trud7 GGO no.63:3-21
856. 10:5)
(Clouds)

NI!WfDROV, V.Ya., kand.fiz.-mat.nauk, red.; SHISHKIN N.S doktor fiz.-mat.
nauk, red.; SHMIN, K.S., doktor z.-mat.nauk, red.; SOIOOVIYEV,
V.A., kand.fiz.-mat.nauk, red.; PISAREVSKAYA, V.I., red.;
SOLOVEYCHIK, I.A., tekhn.red.
[Investigations of clouds, precipitation, and thudnerstorm
electricity] Iseledovanie oblakov, osadkov i grozovogo elektri-
chestva; sbornik dok'-'adov V Mezhvedomatvennoi konferenteii po
voprosam Issledovantia oblakov, osadkov i grozovogo elektrichostva.
Leningrad, Gidrometeor. izd-vo, 1957. 214 p. (MIRA 11:6)
1. Russia (1923- U.S.S.R.) Glavnoye upravlenlye gidro-
meteorologicheakoy sluzhby.
(Clouds) (Atmospheric electricity)
(Precipitation (Meteorology))

SHISHKIN, N.S.
'7
~ed Vctin!gtZQerstorms and showers by layer method. Meteor. i
gidrol. no.8:14-20 Ag 157. (MLRA 10:8)
(Thunderstorms) (Weather forecasting)

AUTHOR Shishkin, N. S. 36-74-2/5
TITLE: Mechanism of Hail Formation (0 mek-hanizme obrazovaniya
grada)
PERIODICAL: Trudy Glavnoy eofizicheskoy observatorii, 1957, Nr 74,
pp 32-40 1USYSRj
ABSTRACT: The author reviews the available information on hail
formation during hailstorms when rapidly ascending
currents of air are present (or actually induce the
storm) and when raindrops become ice pellets (at temper-
atures below freezing). The author explains how the
embryo of the future hailstone grows to a size of 40-50
microns and how the element of diffusion in water vapor
stops playing its decisive role in the-growth of the
pellet. It is the coagulation of independent pellets
that accounts for their consequent development into a
visible hailstone; some of the hailstones grow to a size
30 centimeters in diameter and weigh 10 kilograms.
The relationship between the diameter of the hailstone
Card 1/2 and the velocity of ascending air currents Is examined.

AUVI'OH:
Khmalstdze, k',,
50-1-25/26
I
TITLE: The Scleritij-." )f Thi'lisi Sc~enttifiz- Research
o 7 -e-Fe -or-57 o t- %
Institute for Hyrr y iiauclin ya
sessiya TI)iliss"-.o,-o NIGMI)
PERIODICAL: ';-!eteorolo,-,iya -i Gidrolotriya, 195,5, Nr I ,pp. 66-67 (US-SR)
ABSTRACT-. In 11a,
1957 this institute held its fourth scientific
session, where 16 lectures devoted to various branches
of the hydro-ieteorolo,,-ical science were held~ Under the
conditiono of Transcaucasia the problem of the forecast
of thunderstorms is of great practical importance, there-
fore special attention was paid to the lecture by Guniya,
S. U. on t-e method of forecasting thunderstorms under
the mountainous conditions of Transcaucasia and the
lecture by_q~ ~ , (Main Geophysical Observatory)
on the topic of the forecast of thunderstorm-processes
according to the method of layers. Papinashvili, K. I.,
Napetvaridze, Ye. A~ and Lomina-dze, V. P. dealt with the
2roblemo of the investiration and subdivision of the air-
and turbulence-currents above Transcaucasia.
Vorontsov, P. A. reported on some peculiarities of the
Card 1/2 temperature- and wind-conditions above the lake Sevan.

The Scientific Sessic-ri of' Tbilisi St-iectiftc- Feselaxah 50-1-25/ b
Institute for Hydrometeorolojy~
I. F., Tsutskiridze, A. Ya. and Kurdiani,
I. G, (Stpte University Tbilissi) renorted on the results
of their works in the field of the aeroclimatic
characteristic of th~: frce atmosphere, on the analytical
raethod of the treatritent of observation,- -:,ith Dilnt balloons
and distribution of clouds in Georgia.
Chirrikadze, G. I. and Gi.-ineyshvili, V. 11i. el-.u.Lained the
scherae of the radiation method of plottine the slipperiness
of ice in Transcaucasia and the cha:racteristic of slush
and its distribution in Transcaucasia. Khmaladze, G. N.,
Tsomaya, V. Sh, and Poklepa, V. F. repuxted on the duration
of the vernal-aestival floods in the rivers of Trans-
caucasia and on the method of their calculation as zell as
on the method of the determination of the water supplies
in the snow according to given records of snow routes.
Tsertsvadze, Sh. I. held a lecture on the method of fore-
casting the main phenophases of grapes in GeorpjA,
Svanidze, V, Fc - on the characteristic of-the ai~ro-
meteorolooical conditions of the cultivation of potatoes,
various conditions of the cultivati-- of notatoes, various
Card 2/2 terms for planting in the low grounds of valleys of EastGecrg"
AVAILAELE: Library of Congree.-
1. Weather forecasting 2. Meteorology

3(9) PHASE I BOOK EXPLOITATION SOV/2268
Glavnaya geofizicheskaya observatoriya
Voprosy fiziki atmosfery (Problems in Physics of the Atmosphere) Leningrad,
Gidrometeoizdat, 1959. 74 p. (Series: Itsi Trudy, vyp. 82) Errata
slip inserted. 1,250 copies printed.
Sponsoring Agencys Glavnoye upravleniye gidrometeorologicheskoy sluzhby pri
Sovete Ministrov SSSR.
Ed. (Title page): N. S. Shishkin, Doctor of Physical and Mathematical
Sciences; Ed. (Insid-e'~ook): T. V. Ushakova; Tech. Ed.z M. I. Braynina.
PURPOSEt This issue of the Observatory's Transactions is intended for students
ancl teachers of-dynomtic'-Imeteorology as well as for professionals in the
field.
COVERAGEt This collection of articles is mainly concerned with the results
of investigations on the physics of the atmosphere carried out in'1956-57
at the GGO, Division for the Physics of Free Atmosphere. The authors
discuss the development (formation) and disintegration of co.pvective clouds
Card 1/3

Problems In Physics (Cont.)
SOV/2268
and the relationship between the cloud structure and aircraft icing. A
new method of affecting supercooled clouds is described. One article
is devoted to an analysis of the frontal structure of anticyclones.
References accompany each article.
TABLE OF CONTENTS:
Shishkin, N. S. Growth and Disintegration jispersio2n of Convective Clouds
---uu-r-i-ngNon-stable Stratification of the Atmosphere 3
Vasillchenko, I. V. Computation of the Characteristics of Convective
Cloud Flow 22
Zavarina, M. V. Phase Structure of Clouds and Aircraft Icing 26
The article analyzes the results of observations made at Shosseynaya
near Leningrad and at Arkhangel'sk for the purpose of establishing the
effect of meteorolo'gical conditions on aircraft icing. The probability
of icing as a function of cloud forms Is presented in several graphs.
Card 2/3

PHASE I BOOK EXPLOITATION SOV/4643
Leningrad. Glavnaya geofizicheskaya observatoriya
Voprosy fiziki oblakov i aktivnykh vozdeystviy (Problems in the Physics of t,'louds
and Active Modification~) Leningrad, Gidrcmeteoizdat, 1960. 93 P- (ijeries:
Its: Tru&y, vyp. 104) 1,000 copies printed.
Spc-~Lsoring Agencies: Glavnaya geofizicheska~a observatoriya imeni A.I. Voye-ykova;
Glavnoye upravleniye gidrcmeteorologicheskoy sluzhby pri Savete Ministrov SSSR.
Ed. (Title page): N.S. Shishkin, Doctor of Physics and Mathematics; Ed? (Inside
book)~ L.P. Zhd&i6~i-,-Te'c-h-. Ed.: A.R. Sergeyev.
PURPOSE: This collection of articles,is intend~a for sAentific workers in
meteorology and for graduate students in fyc"rometeorological institutes.
COVE-RAGE: This issue of the Transactions of the Main Geophysical Observatory con-
t.~dns articles dealing with problems of cloud,formation and microstructure.'and
with methods of active modification of clouds and fog. Instr=ents used in
cloud investigation aredescribed, and the use of electronic computers for the
(---dt~

PHASE I BOOK EXPLOITATION SOV/4173
SOV/2-S-102
Ieningrad. Glavnaya geofizicheskaya observatoriya
Voprosy fiziki oblakov Problems in the Physics of Clouds) Leningrad, Gidrometeoiz-
dat, 196o., lo2 p. ~Series-. Its: Trudy, n'p. 102). Errata slip inserted. 1,,150
copies printed.
Additional Sponsoring Agency: USW. Glavnoye upravleniya gidrometeorologicheskoy
sluzhby. Ed. (Title page): N. S. Shishkin., Doctor of Physics and Mathematics;
Ed. (Inside book): V. S. Protop~j(~~,---jiiiL Ed.: M. 1. Braynina.
PURPOSE: The publication is intended for the scientific workers in meteorology and
aerology, as well as for graduate students in these fields.
COVERA0: This is a collection of 6 articles published as No. 102 of the Transac-
tions of the Main Geophysical Observatory imeni A. I. Voyeykov and deaaing with
the physics of clouds. Individual articles axe concerned with convective clouds
and their radar characteristics., the microstructure of supercooled clouds,
radar chaxacteristics of thunderstorms, and the problem of the optimum radio wave
for detection of cloud systems and precipitation. Fleferences accompany each
article.
Caxd V2

sl~s 1~1 jj-, -N. -3-
Wo6i
(531 / 6Z/000112(o/002/004
3_~ o 1053/Z 253
AUTHORS i Gromova, T.N., lCraslkov, P.H., Lenshin, V.T., Ilikandrova,.
0.T., Khimch M A., Shishkin, N.S.
TWILEt Experiments on the application of Pb12 In water solution
to amperooolod clouds
i SOUPCE:' Leningrad. Glavnaya geofizicheakaya obserVatorlya. Trudy.'
no. 106, 1q62. Voprosy fIziki oblakov I aktivnykh
vozdystviy, 1C-21
TM -. Cloudc or mists nro tronted with a combustible water solution
;-Of PhIn sprayed out of an air-plane nt a pressure of 5-4 atmosphere
throart-i i3pra-rnro comprising 32 nozzles 1.2 mm in diameter. The
effoot has bn,3n observed from an altitude of 0.5-1.0 km over the
upper cloud limit. In olimulus clouds with a vertical capacity bf
2 km and over, precipitntiona hnve been obtained below -70G* Com-
-pact strato-cumulne clouds with a capacity of 200-460 m were dIn-
aipated below -150C. At - -291G both the PbZ
_2 solution and the
later itself produce cloud dissipation-, There Is I table.
Caird 1/1