SCIENTIFIC ABSTRACT FIUTOWSKI, J. - FIZDEL, YE.A.

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

FIUTOWSKI J.
Prophylaxis and treatment of alcoholism in Austria and Switzerland;
report from a stay for schooling. Neurol ndurochir psych 12 no.lo.152-
157 Ja-F 162
1. Panstwovy Szpital dla Nerwovo i Psychicznie, Chorych., Fruszkow.
D~Tektor: dr mod. P. Kaczanowaki.

PIUMTKI, Stanjolaw
F J
.conomic premises for feeding sugar-beet pulp Iii? fattening pigs,
Postepy nauk roin 12 no.1:93-106 Ja-F 165.
1. Institute of Agricultural Ecotomics, Varsaw.

1 4 1 6 1 4 1, 111 It U Is a
to v a 1- #8
'
'
Is T 49 Is
1
L
.
A it A_.R~ I .c0, PIPPM.- 5 4 l_
00-1 %in_

0

0 The nduoralooe Characteristic of this phosphates of MuSSIAG phosphate deposits
ja eftilection WM their avooomk UOU11011. 1) ti~ %, RUIANUV.

CA) Udobvirwit i trr*sA4i (FertiEzers and Yiellis) 10141~3v_ 141114V
deposits of Russian

0 41
00 to which Contain no apatite, as a nactelvi consist of kurskite (appamntly
P.111.111thh"Iname tit the giviicrument Kursk
where solur phosphate dtivosits are locatedl.
41111111,a I ~ f
z .
which Is optically inactive, anti staffelite, which In optically active anti well crysid.
hi
i
t
l
h
fi
l
t
ew wrrr, (
v
v
Chem, ano
yw" t
c
Oil the hasla tit micloscople ant
1wirograp
-
t
vi
l
n
itic
Th
6u
itt
la
t
I
sl
b
i
i
11)
d O
f

i
.
sau
auci
t
ic a
"
s
c
t
iucon
c
C
y an
% l
t
y
ly ; (
)
AW
L a
hos
hates which is not activv
t, kunkite
a chief mass of t n sand
l
Ill 1W
t
00
.
o
it ollp
y p
p
In rited light also belongs to hurskite, S-ime crystalline xtaftelite 14 found alon
ho
tion ex
IA
hav
shown that th
th
d
hat
s
V
t
Vth
kAt
i
I .

0* -
a
.
e
e
turI
c
e van
e
ege
c
n
sp
p
y p
amorphous kurskite it Just as good as kil. Ishosphair In both sand &ml IN)d culturt-s,
ll
of th
It
T
d
2 v
ti
ti
I
l
t
th
i
i
l
ff
li
.40
00 A
e si
um
s.
o
.
e
a
e
es o
ve mu
s" negat
y.
whi
e the sta
e
to g
p

00 phate, 3 kinds of extractors were used: (1) 2% citrice acid. (2) cittute buffer.mixt. suit
Five-g
samples'ol the
was 4
of the buffer mixts
0
buffer mist
The f
rtrot
(3) t
0
.
.
.
.
.
e
a
u
in s rotary
of the soltis
and Phaken foc 2 firs
hates were Witted with Wl cc
hos t
.
.
.
p
p
shakinit machine. then filtered and 11 was dctd by the f^rns method. The hunkar
I'hO*VlMte$ of" 1110fe U'lr. although the differtners between kunkite and stafftlite wi-ft too 0
21"t as clear-cut as In the Vegetation extits. S, jorre

e

SIVALI,1004KAL LITIMANXI CLASSIFICATION
114" $" too

As 1A An I I a ts, a 11 9 or 01 2

1 1 ~ In I a`
0 it I A
It

94

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L I I q . mk-
PIOCIIII,
00
00
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0 -00
"W SIMUlf deptegits Le Rugg&,
of 41 Fivx-x- mumend,maii "'.'w Isjoboft.
3S
04 a kitile (K'4A ltr~a)
"tiers are -1 a low OFA-le- IKII ther can be cowd. anj
to d cu"InIcIvidIllY. 0[her 'kPOlitil are too high in re 4,00
andl ca"ant be war" f" t
13 he Selin. of PAX .41 a =00
seml- A. A.
roe
00
COO
goo
jar
00
zoo
0
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.300
t:041
fiS4,%LA stIAMAGICAL UTINATLOR CtASSIFKATICIt
Too
It .11 17.1 dot .1'a&1 cim wvv 11, :10 -0
v -1, 0 d a I IN IN 9 a a 3 9 1 -MF
TO '1*0** 'a 1.19 0. 'r at, in Oct
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toeooooooooooevoooooo0000010004oototoooooooo0ou

0 0 0 0 0 0 0 Op 0 0 0 0 0 9 0 0 0 a opq ago 00 0 * 0 9 0 0 0 0 0
Y12121 ;334zs A)"ro'Jail 32 u lab Jok it 14 jo a it 1: 41 a a
I I A I A I I 1 19 11 11 11 SO 13 4 17 Is III x EO
C v I I L I T u pp tr 4 1..
0 : 4 CINUCOS
Aptite.dopoelts of the KbIbictian tutidras. M. 11,
Fi-z- Sri. 1".1. Fovtdji~"
7, 1,421IM11): cf. ('. U 31, 2117V. Ato act-mit .,( Ow
Kbibinian tutidra almlitt *it It 41- t q6tot, oft lot. lit ill, i
141 Inincrali C. A. Stll.-ortml
it rs*
roe
j
00 re so
00
g
00
so
OW
MITALLUROKAL L1711116TOI C~WIFICATICII to 0
A S a . i L A
it
-i to
u AT 40 1 4 a 0. 0 J; It Ai
Top rot too it w 44 110,11[1111111 "ttet It cc Mm n 4m 4;
to 9 0 0 0 0 0 0 0 0
4 o 0000 0000 0 0:0 9 of 0 0090 00 000 go 0 0

0-0-0-0- -0-6-0-0 ~701*7---js 0 0 v 0
0 0 0 0 0
A 4 1 - I t z m a (X w tuf AL-A 6 t I -,1,j k- A 4 a --&--L -T"
411
.Of
I
00
It. I Liv~rgjottml A. 1'. Sh,11,811. 1). S, :00
J. N&,. 1. Itit delk-tA tA vulcattle
Mitts the culwlit. of the phosphstris orldclin M-rum w C0411-
"Wrrially l"llwortsint clislaillittel. The 4MI. of AtItAlittil
so its thr Kliffitta del-401111 its fSt.f. at 2 billin" (tills rimfg. 430
millit'll 1,111-4 it( P.O., 'nic Alpatiff. 4"c lilies Ifilaillirlit sit
so #I,
09 Z:j stir KhsIv%L plailt Sivrit a ""IN rilliall. V4,1111. 30.A 31,
of 1141.16. '1 liv. "'we 1.1thIll, 1. list- 11-1 A. Irtilhirs., 1-4 doe
they call he inside Its yjehl (after an -041111. llillaswil) Is
0* w-plichte cm-rittrate for the prothictimi ill the sokidem W see
66 Al. Na Amd 11 still it( cement. W. R. Wills
see
00
see
so*
1111FALLURGICAL LtT[R&TIAE CLASSAFKATPON
t L .61
Joe
ILE la Al NJ
al 3 If I
It ff it e1 Kw A I CW 0
9 0 0 ; 0 '; 0 0 0 41 41 0 6 O's 0 r 94"i
~1800 : : : j : : : : : : : 0 0 0 * it : -0 so to; :16 0 0 f 0 0 0 41 ill 0 c 0 0 0 0 :1

I A I &A N LI M' Ff b

Genesis of wolfrunits deposits of Transbalkal i Siberia i.
*11.1'.FiMiknd.%I.D.I)ftrfitian, I'ItIeNw-Ifet,11.1938, .
rMCITIM. -The BrIukha and littkuka Wme de"it,
.1itualrd ammix 11-1 Middit- juralAiv xranad~wjt" .00
a
00 and quarts d1imites near the contact tone with Jurassic
clay slates and sandstones. The lomation of the ores is
00 the fault of six phasesof mineralization. ThcWmiu.W415,
00 J~ are wolframits and sheelite. Part of the (Itposits is ndw,
twin$ worked commercially, H. IN. Dankloff
00 =00

000

:
0

00 Ifi
00
so
5*0
Of j
00 1
2,00
so I
00
00 ago
t
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WOO
0
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AM S 9 U 0 r M too

0

T U ts 4,
if it Vic
0 0 0 0 0

06040000
1
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40

A
00
A
00
09
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so
41100-9
of a
00 W
OF 1
00
00
W!
a $1 $1 SO A
lkltw. Soark, Ins,
N. 1% M 1404"0 Kb'Pl. XIffirkst~
j~ KhjjAn *petite kpWtb all,
dhar, 1"Mont N,-, e
to contain 2 WWII India, Of "litt'
drsirvibird. The dePoll I is allpfiva. 21
jW,nA.UmHdWr%&- Thtay-litt),cullfrul
Am"04. '/s tit Ohs 41fix"Its VE'll""If Zp)% "0"' Th" out'
pill 611 the "limb 4.2 flikilsoll, tom .4,40 musiumilly, I'li.
cufk'IWI Itolmlik"t &petite cotwelitlate tolliefits :111.2%
11.0" Nelibefifir. a W"fir Pt4xlLkt ublailml fil onfirbilis
~the apatitet in umsed. rhe iteptidile ompmutrate "ni.
I Slus A p to 30, Kill 5-41, Na,(J 12-13 slid PAX 2.0
"jA I %TU WpIleble 6 AX).Um tual, The
i1j.1 T output al i is, lo,"CrShi (,u the tlkb;mn
lots of 11W avelist- Ch
inguntalm) 6 a chm=:Cic osuipit of dm cauplex
utiliLatim of taw tuaterial. Apatile yidds 11, F &tOd Farr
earths. A40#, a mixt. ol potash and vocta. ant! ctment evit
lit Wile ned by trimmiling nephrlite. The fm-rvn of the
1
ispetite lieds contain txr builit, hiah In xPlurne. Bunch-
let& the spilmor two P"WilmN 0 k"Wrutfate lich W 11101.
W. R. Henn
L::t L
-so
.0
0
-00
-00
mo*
MOO
moo
goo
goo
690
a
"1000
moo
woo
r
Its"
14,301hi WAR a..
00 T U At 00 All; W.,
it W I or S-
to 0 it a AM A I
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00000*ooooooo:p::: oooooo;ol:ov;o
as . .
0000000000000000040

00 0000 BEY I
i~
0
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off
O'c
:0 -
&AA

P9001116 A" PFC01111ts 1.01.

Th* comstradou of to %tyu Massif
.dh*RA. M-Irbo-
" 00

-00
Fri owl sJorldfuncka- (U. S.
71rams
271
V
%
en
*
.
.
.
y
I
Ree-1. Zkor. 1"0.
14A
3T-44
Kilm
No
IW9 00
.
.
.
.
.
,
No. I, 3s~Tbt titanomawtite pbbaw and brig uh- -Ge
ordinate pyrosmes an richest in P (the sampl- of the -00
sishwals contained an xv, of 0.4817* of P&% and the mm-
I
h .00
n t
e
hspmtI1eIM%oIPA). The PA content
ThelAcontent
=%tm(GWv$frocnO
IItoI
48%
see
.
.
.
inma ples contg. spatite was from 0.58 to 2.01% along the
XiM
=00
usl layers. The minerals of the Patyn tnab6if do
'
W
R
Her
n
concns
of a
titc
tain an
com
t
.
i
.
.
.
.
no
con
p
y
The Camook veleask rodo of tho Glabome district
,

VktWk. A. 13, Rdwards and W. Crawford. Proc. Rey.
Zoe
-311(1940).-Ilemiptive.
281
1

,e:
to

A I a. It. A WALUMCKAL LITtRATtOg CLA1104CATM too*
9 -1Q W-- of -sp
CRT 0#1
-US AV -10- It It
it 1 N 0

Fin-G, I.I. P.
"The Concentration of Phosphorus in the Patyn Massif (Mountainous S 'a Pi
M. P. ve
R. 'A. Matrirosynn, Trudv Nauch Inst Udobr I Inanktofung Im Ya. V. Sawylam, No 146,
pp 37-44, Khim Referat Zhur 1940, No 1. PP 38 (SEE: Inst. Insect/Amg. in Ya. V.
Sapoylov)
SO: U-237/49, 8 April 1949

FIVEGJ M. P.
11Xhibin Apatitep" S. I. Vollfkovich.4 M. P. Fiveg, and L. E. Berlin,
Nauch Inst Udobreniyam i Insektofuhgisidam Zhur 1919-39, pp 17-24
(1939), Khim Referat Zhur 1940, No 6, pp 86 (SEE: Inst. Insect/
Fungi. in Ya. V. Samoylov)
SO: U-237/49, 8 April 1949

FIVEG, M. P. and CHERNYr. L. 141.
"Requirements of Industry as to the Quality of Mineral Raw Yaterials.
Handbook for Geologists," Goz. i2d-vo geologizheskoy lit-ry Komiteta po delam
geologii pri SNK SSSR, No.22, 1947

Aug 48
Rook 'Salt:
Sedimentation.
':the Annual Cycle of Sed J To ntation of Rock Salt in
the Upper Ta- k Bed," M. P. Fiveg, All-Union Soi
Inst of Halurgy, 4 pp
"Dok Ak Nauk SSSR" Vol LXI, No 6
N Ckiose' this deposit because it does not uidergo any
intensive movement and recrystallization. Therefore
the salt structure is very close to its structure
when sedimentation took place. Proves that the group
of ''rbytbmica.ily constructed. streaks of rook salt in
the Upper M%msk deposite-we actuilly yearly *y~a.
SUbmitted by Acad D. S. Belyankin, 22
Jun 48.
35A9T69

FIVEG) M. P.
"An Estimate of the Duration of Various Saliferous Materials in
Fossils from Salt Depoetto.
report presented at the meeting of the Geochronological Commission, Dept.
Physical Geography, AU Geog. Society, 19!53.
(Izv. Vaesoyuznogo Geograficheskogo Obahchestva, No. 6, NOV/Dee 51).

r i-, - '--"! - -
71M.M.P.
I - *"Wwc~awll~-
Yormation of potassium salt deposits. Biul.KOIP. Otd.geolo 30
no-3:3-15 W-Je 55. (MIRA 8:10)
(Potassium salts)

15-57-8-11306
Translation from: Referativny zhurnal, Geologiya, 1957, Nr 8,
P 170 (USSRT
AUTHOR: Fiveg, M. P.
---------------
TITLE: Geological Study of Potassium Deposits (0 nekotorykh
zadachakh geologicheskogo izucheniya kaliynykh
mestorozhdeniy)
PERIODICAL: V sb: Vopr. geol. agron. rud. Moscow, AN SSSR, 1956,
PP 155-161
ABSTRACT: For production of potassium fertilizer, use is made
chiefly of s~lvite-containing rock (sylvinite and the
so-called solid salt) and of potassium chloride as a
waste product of carnallite rock used in the production
of magnesium. In addition, langbeinite-kainite rock
of the cis-Carpathian district is used directly as a
fertilizer. At the present time, a plan of treatment
Card 1/3 of the polyhalite ores has been developed to obtain

15-57-8-113o6
Geological Study of Potassium Deposits (Cont.)
potassium sulfate and potassium magnesium sulfate. In the Permian
salt-bearing formations, lar e quantities of polyhalite rock with
Eg
sylvinite have been found ZZhilyanskoye mestorozhdeniye (deposit)7.
Sylvinites with caliborite and hydroboracite of the Indyerskoye
uplifted region are of great scientific and practical interest. In
the cis-Carpathian district, the lenses of the potassium rock in the
section of the potassium-bearing strata are correlated with the
accurately determined stratigraphic levels of the potassium-bearing
series. The content of bromine or the location of nodules of po-
tassium minerals in the rock salt may be used as a prospecting
indicator of the potassium deposits. For prospectings of potassium
deposits, the Lower Cambrian salt-bearing formation of Eastern
Sibiria and Miocene Transcaucasia (Avanskaya) present the greatest
interest. A high content of bromine and the presence of sylvite
are observed in the rock salt of the Serego structure in the Komi
ASSR, but the conditions of deposit of the rock salt and the geo-
graphical position of the Seregovskaya structure and of structures
Card 2/3
"N'
~K t tf_

Geological Study of Potassium Deposits (Cont.)
15-57-8-11306
adjacent to it cause them to be poor prospects.
Card 313 V. P. Yeremeyev

15-57-8-11305
Translation from: Referativny zhurnal, Geologiya, 1957, Nr 8,
pp 169-170 TUSSR)
AUTHOR: Fiveg, M. P.
TITLE: Types of Halogenous Basins (Tipy solerodnykh
basseynov)
PERIODICAL: Tr. Vses. n.-i, in-ta galurgii, 1956, Nr 32, pp 102-
110
ABSTRACT: Until recently, the "bar" theory of Oxenius on the
accumulation of saline strata in the lagoons was
generally recognized. After Oxenius, it was supple-
mented by recognition of the part fla d by monsoons
?)ye
(Zimmerman), high tides ffillfrat ~.7, and seepage
through the sands in filling of the basin with sea
water. It was also supplemented by the explanation
of the phases of migration of the halogenous basins
Card 113 (Howers) with simultaneous existence of the connecting

'r,'-pe-s of' Halogenous Basins (Cont. )
15-55/7-8-11305
lagoons (Branson). The widespread nature of the processes of alter-
lation of the natural brine indicates that there is, in addition to
t1he two types of feeding of the halogenous basins mentioned above,
a third, mixed type, which in the past was most widespread. The
,jLrect connection of the halogenous basin with the sea is rather the
exception than the rule. Therefore, it J.5 impossible to consider
the term "lagoon" as synonymous with "saline," as do L. B. Rukhin,
A. B. Ronov, and V. Ye. Khain. In the lagoon deposits, gypsum and
carbonates usually predominate; this is associated with the unfavor-
able conditions for retention in them of the saline precipitates.
The thickness of the salt-bearing series bears evidence that they
were accumulated in the most mobile of the intensively deformed
sectors of the earth crust. The nonlagoonal halogenous basins have
a long term of life and considerably greater areas. These are the
basins on the marginal parts of the platforms and the foremost
flexures and should be considered a special type of halogenous basin.
Thus halogenous basins may be classed as: 1) marine halogenous
Card 2/3

Types of Halogenous Basins (Cont.) 15-57-8-11305
basins; 2) lagoon and other basins of the coastal area; and 3)
saline lakes, solonetzes, and other accumulations of salts under
continental conditions. However, marine halogenous basins (Miocene
basins of the Tyan-Shan and Kara-Bogaz-Gol depressions) may also
exist on the continent. The feeding of saline lakes may also be
accomplished in part at the expense of marine salts, as in the
compensation lakes on the margins of salt domes and the interduction
of marine salts by the wind.
Card 3/3 S. M. Korenevskiy

FIVEG, M.P.
--. -- I
Geological conditions of the sedime t&I7 t 0 in the origin of
salt-bearing formations. Vop.min.osad.obr. 3 4:235-240 156.
(MLRk 9:11)
1. Vessoyusnyy institut galurgit, Leningrad.
(Geology, Stratigraphic) (Salt)

FIVEG, M.P.
Of' "salt basiume Trudy VNIIG 32:102-110 156. (KIM 11: 1)
(Salt)
06
4
Q,

FIVZG, M.P.
7ormati*n and distribution of potassium deposits in salt formations.
;akenem. rasm. polezn. iak*P- 1:517-530 '58. (MIRA .12:3)
leVseeoyuzny3r nauchno-iseledovateltakir institut galurgii.
(Potassium)

FIVEG, M. P.9 Dow)GEOL ROD M I N*Mt 801 p"GEOLOGICAL CON-
DITION~OF ME SEDIMENTATION OF SALT-BEARING SERIES AND THEIR
- POTASSIUM HOR!ZONS." Moscowt 1961o (GEOL JNSTjACAD SCI USSR),
(KL-DV9 11-619 212).
-604-

YMG, M.P.
Facies serieo of halogen rocks and characteristics of the
distribution of their members. Zakon.razm.po1*zn.iskop. 3:167-
174 160, (MIRA 14:11)
1. Vsesoyuznyy institut galurgii.
(ftloidite)

KASHKAROV, O.D.; P3ZQ,-U.,Px; ORLOVA, Te.V., nauchn. red.;
CHERNOSVITOV, Yu.L., nauchn. red.j FEDOROVA, L.N.., red.
izd-va; IVAVCVA, A.G.9 tekhn. red.
(Industry's requirement as to the quality of mineral raw
materials] Trebovaniia promyshlennosti k kacheatvu mine-
rallnogo syrfia; spravochnik dlip eologov. Izd.2., perer.
Moskvaj, Gosgeoltekhizdat. tio.224 lPotassium and magnesian
salts) Kaliivje i magnezial'rWe soli. 1963. 54 p.
(MIRA 16.12)
1. Moscow. Vsesoyuzrj~ry nauchno-isaledovatel'skiy institut
minerallnogo syrtya.
(Potassium salts) (Magnesium oxide)

a pnf

., - .- ~~ " - :-I. - . , --- - - ---lcL.l;!;I4,4Xnle-zl-Qtz ...I
L - - - . -- - 1. , _ 7 - - -- - ~- - . ~ ~- I---- - - - - . ---. . . - ~ I- -- - ---, - , -

e: r. C n c
3 1 a 7rzz. or F

FIVEYSKAYA. A.A.
Importance of focal infection in the gallbladder and the
biliary ducts in pateints with infectiona nonapecific poly-
arthritisl*T&Wtherapy. Vop.kar..,fizioter. i lech. fiz.
k.ul't. 28 no.2:147-152 Mr-AP163. (MMA. 16:9)
14 Iz artrologicheskogo otdeleniya (ispolnyayushchiy obya-
zannosti, zaveduyushchego F.F.Lyudvinakaya) kliniki Tsentrall-
nogo instituta kurortologii i fizioterapii (dir. - kand.med.
nauk G.N.Pospelova)
(ARTHRITISY THEUMANOID)
(BILIARY TRACT-DISEASES) (BATHS. MOOR AND MD)

Epp-/BIP(
(p)/BR A Mi. CIA S. DPs-h/pc L/Pr-4 Mlfbrw
(m)/BDS
MCESSICIT ITR: AP3004576 8/0032/63/029/008/IM/lw7
,'AT
JMORI Fiveyakaysa A.,K~; Yakdvlav, S.-A.
TITIZ i A- met-hod for bonding optical crystal windm to lamps and vessels.
Re-
Port presented at a conference on spectroscopy held in Gorikiy frcm-5 to 3-2 J07
61)
;,19
ISOURGE: ZvLvOd8ImYa labomtorlya- v, 29, no. 8, 1963, 1007
TOM TAG3; spectroscopy, bOadW;- Vacum-tight bonding, gasket, fluoroplast-3s
polychlorotrifluoroethylene,, Kel-F., fluorite, lithium f lu6ride, ultraviolet
.light source OK-50 OX-50 heat-resistant adhesive
.ABSM.CT,. A method has- been proposed for the vacu=-tight bonding of a vindow
of crystalline material to a glass vessel for service in tbe -195 to +150C tem-
Perature range. A flat ring-type gasket ofE f luoroplast-3qpo3,vehlorotrifluo.-o-
,ethylene), pretreated with a solut/ion of sollum naphthale complex in tetra-
hydrofuran was bonded with OK-50ftedt-resistant adhesivO, tweea the window and
the vessel to compensate for the-Effe-i: ince in ~ther~mal exEpansion coefficient*
After bonding, the part Is held at 60-150C for 3 hr. The method has been tested
with fluorite and lithium fluoride vindows in vacutm ultraviolet Light sources.
Card 1/2

FIVjlSi~Zf,'~ -11-L 0
Logarifr chesk-iyo s razrc-.nyrai s-Uml-ani G-'-TI Ur-35', 1-
W! Lathcmatics in the U'SR, 1917-1947
edited by Jurosh, ,,.G.,
R shevsk-iT, r,
i-cSCOlll.,-LerZ,tv..-rad, 1948

Accidental woun d of the cervical segment of the thoracic duct,
Zhirurgiia no-5:72 W 154. OPA 7:7)
1. Is kblrurgicheakogo otdolonlya 1-y Koyrovskoy gorodskoy boll-
nitsyl Vlaasirskor oblasti.
(WOMS AND ISM119-
7-F
*thoracic duct,in surg.-of subazillary tumor)
(AXILLOLD.neoplasm.
Omg mxlll&ry, surgw, acoid. Inje of thoracic duct)
(BMXRT. OPMUIT."Bi complicitions,
#iW..of,thoracto duet in murk. of subaxillary tumor)
(THORACIC DUCT,-wounds and Injuries,
*in surg. of subaxillax7 tumor)

-- - -
Dissertation: "Thermophysical Basis for Elimination of Icing in Mine Workings."
Inst of Mining, Acad Sci USSR, 17 Oct 47.
SO: Vachernyaya Moskva, Oct~ 1,947 (Project #17836)

21 Mt 15 (9),
AUTHORSt Mokultakiy, ff. A.9 Lazurking Tu. Soq SOV/20-125-5-15/61
Fiveyakiy, M. B., Kozin, V. I.
TITLE: The Reversible Radiation-mechanical Effects in Polymers
(Obratimyye radiatsionno-mekhanioheakiye effekty v polimerakh)
PERIODICALt Doklady Akademii nauk SSSR, 1959, Vol 125, Nr 5,
pp 1007-1010 (USSR)
ABSTRACT: By the action of an ionizing radiation the mechanical
properties of polymers may be changed to a cons'Iderable
extent. The authors of the present paper investigated some
mechanical properties of polymers during irradiation. The
investigation was carried out in water-cooled vertical
channels. The fluxes of the neutrons and r-quanta, as well
as the energy dose absorbed by the samples were measured on
this occasion. Moreover, several simple devices for
measuring the mechanical characteristics of polymers under
irradiation were constructed, and, especially, a device for
recording the extension curves (6--E ) for use in a reactor
were reconstructed. The authors investigated polymers of
different radiation resistance and different character of the
Card 1/4 most important radio-chemical variations. By comparing the

The-Reversible Radiation-mechanical Effects in SOV/20-125-5-15/61
Polymers
mechanical properties of the aaiples located in the radiation
field with theproperties of or-ginal samples (and with
samples whichq though irradiatedg were tested after
irradiation) reversible radiation-mechanical"effects were
discovered. They are based upon a temporary reversible variation
of the mechanical properties of the polymers. This variation
occurs during irradiation and vanishes as soon as irradiation
ceases. The authors observed the following reversible
processes: 1 ) Decrease of the strength of polymethylmetacrylate.
2) Decrease of the limit of the enforced elasticity '~rB Of
polyvinyl chloride, 3) Increase of breaking elongations of
polyvinyl chloride. 4) Inoreas6 of rdaxation rate of the tensions
in the investigated substances. 5) Increase of the creep rate
of polyvinylchloride, polystyrene, teflon, and rubber. Points
2-5 are then discussed in detail; thus it was found that(r
B
decreases in the case of a dose rate of 46000 rad/see by -25 %
and increases approximately linearly with an increase of the
dose rate. After irradiation ceases, the reversible effect
Card 2/4 vanishes after less than 1 minute and only a remanent effect

The Reversible Radiation-mechanical Effects in SOV/20-125-5-15/61
Tolymers
remains. A table contains the values of creep rate under
various conditions. As a result of the irreversible
destruction effect, the creep rate increases. Also this effect
increases linearly with increasing dose rate. Me diagrams 3-4
show the considerable reversible change of creep rate caused
by the switching-on and -off of irradiation. The reversible
radiation-mechanical effects may be of physical and also of
chemical nature. The molecules excited by the ionizing
particles during the dissipation of energy "pass through"
states with weak excitations, which do not suffice for the
stripping-off of the chemical bonds, but which correspond
to local heating to high temperatures of short duration. This
may accelerate the relaxation processes and change several
properties of the substance. However, ilso a chemical
mechanaim.must be taken into account. To what extent it is
able to explain the ' reversible radiation-mechanical effects
can be explained only after further investigations. There are
4 figures, I table, and 2 Soviet references.
Card 3/4

S/190/60/002/01/13/021
B004/Bo6i
I, ;Zbo P12081
AUTHORS: Mokullskiy, M. A,, Lazurkin,-Yu. S., Fi-eyakiv, M.
Kozin, V. 1.
TITLE: Study of the Mechanical Properties of Polyme 3 During the
Process of IrradiationIIII Strength and Ultimate Forced
Elasticity of Solid Polymers During the Process of
Irradiation in a Nuclear Reactor
PERIODICAL: Vysokomolekulyarnyye soyedineniya, 1960, Vol, 2, No. i,
pp. 103-109
TEXT: The authors exposed polyvinylohloride (PVC) and polymethyl-
methaerylatel(PUNA) to irradiation in a B.BP(VVR) nuclear reactors
Data on the neutron beam are given in Table 1. The irradiation was
carried out with a dose of 469000 - 56,000 rad/sec at 20 - 600C in
vertical channels cooled with water. During irradiation, the strength
and ultimate forced elasticity of were d,!~terminqd with tho apparatus
illustrated in Fig. 2, and the creep by that in Fig, 1. Fig: 5 shows the
Card 1/2

Study of the Mechanical Properties of Polymers S/190/60/002/01/13/021
During the Process of Irradiation. 1. Strength B004/BO61
and Ultimate Forced Elasticity of Solid Polymers 8208 1
During the Process of Irradiation in a Nuclear
Reactor
dependence of the strength of PIMA an the integral dcae, Fig, 4, the
dependence of of with PVC on the integral dosa7 The deerease in cf is
almost proportional to the radiation intensity (Fig. 5). The irradiation
was interrupted by switching off the reactor, and it was seen that of
increase immediately about 25 - 30% (Fig, 6): The breaking length also
increased after switching-off of the irradiation (Table 2. Fig. 7)_
As well as the known irreversible processes, based on interlacing and
destruction, reversible processes also occar on irradiation There are
7 figures, 2 tableB, and 5 Soviet references,
SUBMITTED: October 15, 1959
Card 2/2

FIVEYSKIY, M.B.; LAZURKIN, Yu.S.; MOKULISKIY, 1A.A.
[Simple calorimetric method for measuring the absolute
energy dose received by substances situated in powerful
fields of ionizing radiations] Prostoi kalorimetricheskii
metod imereniia abooliutnoi energeticheskoi dozy, polucha-
emoi veshchestvami v moshchnykh poliakh ioniziruiushchikh
izluchenii. Moskva, In-t atomno4. energii, 1960. 10 p.
(MIRA 17:1)
,I

V&
S/190/60/002/01/14/021
P?84~B061
AUTHORS: Mokul'skiy, M. A., Lazurkin, Yu. S., Fiveyskiy, M. B.
-----------
TITLE: Investigation of the Mechanical Properties of EaLLM-erel
During the Process of Irradiation.111. Creep of Solid
Polymers and Rubbers During the Process of jrradLajAonj?
in a Nuclear Reactor
PERIODICAL: Vysokomolekulyarnyye soyedineniyR, 1960, Vol. 2, No~ 1.
pp. 110 - Ila
TEXT: The aim of this work was to establish changes In mechanical
properties which re-form after cessation of the irradiation. The method
of examination is described in Ref. 1. The authors examined the creep
rate in de.Dendence on the mechanical stress applied and the integral
dose. Fig, 1 shows the change in creep for unplasticized polyvinyl-
chloride at a radiation intensity of 46,000 rad/sec, a stress of
0-5 kp/mm2, and 520C. For comparison, data are given, that were obtained
from nonirradiated material, and material taken out of the radiation
Card 1/2
g~q
ir
r!J
" 100-

Investigation of the Mechanical Properties of S/190/60/002/01/14/021
Polymers During the Process of Irradiation. B004/B061
11. Creep of Solid Polymers and Rubbers During 82082
the Process of Irradiation in a Nuclear Reactor
field. Fig. 2 shows the same data for a stress of I kp/mm?. The time
dependence of creep is reproduced in Fig, .3. A Table gives the experi-
mental datao/The same experipents were carried out with "plasticized
polZatyre e,'Pplasticized PVCV(Fig. 4), vulcanized rubber from natural
rubber of the type HK~Fig- 5), from CKH-18 (SKN-18) nitrile
rubberlf(Fig. 6), and from polyisobutylene rubberL~Fig, 7)_ In all the
substances examined, the creep rate increased in bounds, and decreased
again when the radiation was switched off. This effect increased with
increasing irradiation intensil"y. A reversible change in the
relaxation rate was observed, The authors mention a pap4r by Yue S.
ZuYev (Ref. 4), thank N. V. Zvonov for making the experiments on the
reactor possible, and the mechanics 1. F. Yermakov and K. K. Shcherbo
for their collaboration, There are 7 figures, I table, and 6 Soviet
references,
SUBMITTED: Ootobor 19, 1960
Card 2/2

84236
S/089/60/009/004/016/020
B006/BO7O
o
AUTHORS: Fiveyaki , M. B.. Lazurkin, Yu~ S~. Mokullskiyq M, A.
TITLE: A Simple CqJorimetric Method of Measuring the Absolute
Energy DosdlReceived by Substances in Strong Fields of
Ionizing Radiation~
PERIODICAL: Atomnaya energiya, 1960, Vol. 9, No. 4, PP. 321 - 323
IMT.Tr - - ~. -A steady calorimetric method is used for measuring the
radiation energy received by a sample if the dose rate is not too high and
the effect of other energy-generating processes in the sample is
negligible. For intense irradiation (high dose rate), this method is not
applicable, particularly because the establishment of thermal equilibrium
takes too long a timel in this case, the sample is so strongly heated that
it either melts or disintegrates; at least the high absorbed integral dose
changes the structure and properties of the sample significantly. For this
reason, the authors of the present "Letter to the Editor" developed in
1957 a simple nonsteady calorimetric method which is suitable for studies
on reactors and other sources of strong radiation. The method has been
tested during the last few years. The principle of the method is as
follows. A sample for dose-measuring is placed at time t-0 in a radiation
Card 1/4

A Simple Calorimetric Method of Measuring the S/0819wol/009/004/016/020
Absolute Energy Dose Received by Substances in B006/BO70
Strong Fields of Ionizing Radiation
field which is homogeneous and constant within the sample, under such
conditions that the temperature at the center of the sample increases
linearly for a time T independently of the surrounding temperature. i is
proportional to the square of the characteristic sample dimension d and
inversely proportional to the coefficient of thermal diffusivity 1. There-
fore, dT/dt is a function of the dose rate and heat capacity of the
sample, and the dose rate can be calculated from the formula
P - 0.417 c(dT/dt)o. c is the specific heat of the sample material
(cal/g.degree); (dT/dt) 0 is measured in deg/hour, and P in Mrad/hour.
Polystyrene, polyethylene, silicone rubbe?. Teflon, molten quartz, etc.
were used for the dosimeter. The sample had a cylindrical form (30 mm
diameter and 50 mm height). This size has a T value of 2 - 3 minutes which
is required for the measurement of dT/dt (Fig. 1). In this time interval,
the mutual shielding of the parts of the sample may be neglected. Copper-
constantan thermocouples were used for the measurement of temperature. The
construction of the dosimeter is very simple (Fig. 2). All parts with the
exception of the thermocouple consist of nonactivizable materials. The
Card 2/4

84236
A Simple Calorimetric Method of Measuring the S/089/60/009/004/016/020
Absolute Energy Dose Received by Substances in B006/BO70
Strong Fields of Ionizing Radiation
whole instrument was inserted in a perpendicular hole in a reactor and
checked in a radiation-free zone before measurements were carried out. In
this manner, the dose rates for different substances were measured in the
holes*of the BBP (VVR) reactor. The error was 5 - 10%. Tig- 3 shows the
dietribut
,Aon of the dose r9te along a hole in this reactor for ol
ethylenek!'and quartz glass.VWith this method the anomalies of the T(t)
curves may'also/be found. Thus, for example, the T(t) curve of polytetra-
fluoroethylenellshows a sharp bend which.may ascribed to a phase trans-
formation due to irradiation (cf. Fig. 4). There are 4 figures and
4 references3 3 Soviet and 1 US.
SUBMITTED: April 14, 196o
Card 3A
_N'
-T I.? N
ME:,
'AN 114 ~' N

A Simple Calorimetric-Method Of Measuring th S1089 60/oog/004/016/02o
Absolute Energy Dose Received by Substances e 84236
Strong Fields Of Ionizing Radiation
in B006 2070
Card 4/4
specimen. 2 -, ther-
mOcOUple hot Junction.
3 - aluminum foil- 4
fleXible 811spender-ins4-
latop- 5 - thermocouple
cold JtIhntlon. 6 - ter-
minals connected to a
measuring instrument.

43247
8/844/'62/000/000/109/129
D4:08/D307
AUTHORS: Lazurkin, Yu. S., 14okullskiy, M. A. and Piveyskiy, M. B.
TITLE: Nature of the reversible acceleration of mechanical re-
laxation processes in polymers under irradiation
SOURCE; Trudy II Vseooyuznogo.sovealicnaniya po radiatsionnoy khi-,~
mii. Ed. by L. S. Polak. Moscow, Izd-vo AN SSSR; 1962,
638-641
TEXT: By "acceleration of mechanical relaxation processes" is un-
derstood a wide range of phenomena, including acceleration of stress
relaxation, acceleration of creep, and decrease of ultimate forced
elasticity. In the present work the authors studied the accelera-
tion of creep (-kH- 'If (SKN-18) nitrile rubber irradiated in a nuc-
lear reactor, this being a continuation of previous investigations,
with the difference that in the earlier work the effect of irradiat-
ing rigid polymers was studied. Samples of the test material were
stretched under constant load for 45 hours to attain equilibrium
deformationg almost all the deformation occurring during the first
~10 - 20 minutes; other samples were stretched for 16 mins. The
Card 112

.~ I S/84 62/000/000/109/129
Nature of the reversible D408YD307
stretched samples, still under load, ,.,ere irradiated at intensity
a L.
2 ~c 104 r d/sec, whereupon creep was initiated at the rate of
4 x 10-3 sec-1 in both 'cases. The results indicated that the acce-
leration of creep and relaxation in ro8ino was caused by rLIPIUM Of
lattice bonds, i.e. the so-called 'chemical' mechanism and not by
the "physical" mechanism (described in an earlier worO as is the
case when rigid polymers are irradiated. Efficiency of the destruc-
tion process was evaluated by the method of Tobolskiy ot al for
the analysis of chemical relaxation. By means of the kinetic theory
of resin elasticity an equation was derived rellating the rate of
creel) under irradiation to the number of bonds rupturing per second
in I cm3 of material. Substituting into this equation the experi-
mental data for 6KN-16 rubber, natural rubber and jolyisobutylene,
the numbers of bonds rupturing per 100 ev of absorbed energy were
estimated to be 3, 4, and 19 respectively. There is 1 figure.
ASSOCIATION: Institut atomno energii Ak SSSR (Institute of Atomic
Energy, AS USSR~
Card 2/2

FIVEYSKIY, Yu., kapitan dal9nego plavaniya
Against primitive methods and laxity. Mor. flot 22
no.3-1:10 N 162o (MIRA 15:12)
(Merchant marine)

83585
S/056/60/036/005/018/050
Boo6/BO70
A'UTHORSt Nemirovskiyt P. E.f FiveyskiZI Yu. D.
TITLE- The Effect of Coulomb Attraction on the Cross Section of
Anti-proton Absorption by Nuclei
71
PERIODICAL., Zhurnal eksperimentallif6y i teorbticheskoy fiziki, 1960,
- Vol. 38, No. 5, PP. 1486-1488
TEXT: As is known, the anti-nucleon - nucleus interaction cross section
is considerably larger than that of the interaction with protons or
neutrons.
qualitative theoretical explanation
of this effect can be givM
A
on the basis of the optical model. On account'of focusing of the
trajectories-of the anti-protone.by the Coulomb field of the nucle-as, the
cross section for absorption by th4 nucleus increases significantly for
anti-protons whose energies are comparable with the Coulomb energy at the
boundary of the nucleus. This focusing effect has been calculated here on
the basis of the optical model. These calculations are applicable to all
negatively charged# strongly absorbing particles, particularly when the
wavelengths X in the case of energies of the order of the Coulomb energy
Card 1/3

83585
The Effect of Coulomb Attraction on the Cross 8/056/60/038/005/018/050
Section of Anti-proton Absorption by Nuclei B006/BO70
V. at the boundary of the nucleus are small compared to the nuclear
radi - t / F~~V
us R i,~(R) O(R)V R,(P is the reduced mass of the particle
and the nucleus). A complex p'btential acts*on the anti-proton inside the
nucleus. In the present work both the attractive potential of the nucleus
negative real part of the o;mplex potential) and the.,repulsive potential
positive real part) are considered. Assuming the potential to be given by
~
W = j-Uo(1+ij 0!6r.L-R
-Ze2/r R.~- r , the anti-proton absorption cross sections are
calculated for the nuclei of C, Cu, and Pb at*0.5 Mev (Table 1); the
anti-neutron absorption oroas sections are also given for comparison
(Table 2). The results ares ax
Nucleus Uo (Me v] 1 _ C%'max[b] UO[Mev] 1 6m, C(n
12 c
C 33 ir 1 3.2 30 1 0.82 4
CU 63 38 E:3 11.2 30 2 1.12 10
Pb 208 43 46 k18 30 L- 3 2 V10
Card 2/3

63585
The Effect of Coulomb Attraction on the Cross S/056/60/036/005/016/050
Section of Anti-proton Absorption by Ruclei B006/BO70
(I gives the cont3~ibution-toithe cross section),P Due to Coulomb attrac-
tion, the anti-proton absorption cross sections for energies lower than
the Coulomb energy areA to 10 times as large as the'anti-neutron cross
sections for the same energy. There-are 2 tables and 4 references:
2 Soviet and 2 US.
SUBMITTED: August 129 1959
Card 3/3

FIVEYSKIY Yu.D.
Effect of: the refraction of an antiproton beam on the aboorPtion
cross section. Izv.vys.ucheb.zav.; fiz. no.3:76-79 161.
(MU 14:8)
1. ~bskovskiy inzhenerno-fizicheakiy institut.
(protons) (Nuclear reactions)

FIVUSEV, YU - D,
8/089/62/013/006/019/027
B102/B186
AUTHORSs G. T. and M. R.
TITLEs Nauchnaya koaf erentalya Uoskovokogo Inzhe,,or,,o-f izioheskogo
instituta (Scientific Conference of the Moscow Engineering
Physics InstitAte) 1962
PERIODICALs Atomnaya energiya, Y. 13t no. 6, 1962, 6o3 - 6o6
TEXTi The annual conference took place in May 1962 with more than 400
delegates participating. A review is given of these lectures that are
assumed to be of interest for the reader's of Atomnaya energiya. They are
followings A. I. Leypunskiy, future of fast reactors; A. A. Vasillyev,
design of accelerators for superhigh energies; I. Ya. Pomeranchuk,
analyticity, unitarity, and asymptotic behavior of strong interactions at
high energies; A. B. Migdalg.phenomenological theory for the many-body
problem; Yu. D. Fiv~eki deceleration of medium-energy antiprotons in
matter; Yu_._!-R. ~Kogan,"Ya:IA. Iosilevskiy, theory of the Osebauer effectl
M. I-. Ryazanov, theory of ionization looses in nonhomogeneou8 medium;
Yu. B. Ivanov, A. A. Rukhadze, h-f conductivity of-suberitical plasma;
Card 1/4

5/056/62/042/003/025/049
B102/B136
AUTHOR:
TITLE- Deceleration of antiprotons in matter
PERIODICAL: Zhurnal eksperimentallnoy i teor0tich_e0*skoy fiziki, v. 42,
no. 3, 196?,,,~49 - 602
TEXT: A theoretical investigation is given of antiproton deceleration in_
light elements, assuming that the atomic mass of the moderator is much
greater than that of the antiproton and that the antiproton enerEy E is
smaller than the jr 0 production threshold:
E Z E ?/2 , nl