SCIENTIFIC ABSTRACT LIVSHITS, L. D. - LIVSHITS, L. S.
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Collection:
Document Number (FOIA) /ESDN (CREST):
CIA-RDP86-00513R000930310006-9
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RIF
Original Classification:
S
Document Page Count:
100
Document Creation Date:
November 2, 2016
Document Release Date:
June 20, 2000
Sequence Number:
6
Case Number:
Publication Date:
December 31, 1967
Content Type:
SCIENTIFIC ABSTRACT
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CIA-RDP86-00513R000930310006-9.pdf | 4.25 MB |
Body:
S/207/62/000/005/003/012
Determination of the phase ... B108/BI86
SUBMITTED: July 11, 1962
Legend to Table 7: (1) pt kg/cm 2 ; (2) graphite
Pb AgCI
T
20-1231C 17-132'C 21-131, 1, 23-110 ~133
; 25-RA)l Ila 0,21
c
I DO 25 .115 02 40 40 40
5000 80 -21 25 20 88 D 32 38
10000 71 -56 21 9 85 122 27 46
15000 58 -74 15 1 80 32 22 62
110000
2 44 -73 8
-2
74 58 24
S6
2.W 45 -55. -5 -2 69 22 12.55
")0 37 -20. 1 3 62 1
Card 2/2
LIVSHITS, L.D.; GENSHAFT, Yu*S,; MARKOV, V.K.
-Diagram of state of cerium in the range 20 to 3500C at
pressures up to 80.103 Kgo/=2. Zhur. e~p. i teor.
fiz. 43 no.4:1262-1267 0*162. (MIRA 15:11)
1. Institut, kbimicheakoy fizJJd AN SSSR.
(Phase rule t a uilibirum)
(Ce 1:3
(High-pressure research)
-LIVSHITS, L.D.; MARTYNOV, Ye.D.
Laboratory apparatus for compressing liquids at pressures up to
20 kat. Prib. i tekh, eksp. 8 no.3:161-164 MY-Je 163.
(MIRA 16 19)
1. Institut khimicheskoy fiziki AN SSSR.
(High-pressure research-Equipment and supplies)
EWP(q) 9
/EW(m)/1W--t.McASD-JD
-ACCESSION NR: AP3001209 S/0078/63/008[006/1302/1306
AUTHOR: Li shits, L. D.; Genshaft, Yu. S.; Ryabinin, Yu. N 0
TITLE: Phase diagram of crystal hydrates MgSO sub 4 at high pressures
SOURCE: Murnal neorganicheskoy khimii, v. 8, no. 6, 1963. 1302-1306
TOPIC TAGS: phase diagram, crystal hydrates of MgSo sub 4, polymorphic transition,
phase-transitionse MgSO sub 4
ABSTRACT: A phase diagram of the crystal hydrates of MgSO sub 4 was constructed
from measurements obtained by the "piston displacement" method; data was obtained
at 20 degrees by volume compressibility of salts which were previously dehydrated
at 200 degrees. A polymorphic transition in the region of 4500 kg/sq.cm. pressure
was discovered. The phase transition in the crystalline hydrates is sensitive to
the quantity of water of crystalli*zation; by decreasing the content of bonded
water, the discontinuities in the volume upon compression are blurred, down to a
complete disappearance of separate transitions. There is a limit in the piston
displacement method above which the liberated water interferes with the measure-
ment of-change in volume decrease with pressure. Actual crystalline conditions
of the salt under pressure can be studied by X-rays, but it may be assumed that
Card 1/2
L 10660-63
ACCESSIO14 NR. AP3001209
significant volume change with-the transitions indicates important structural
changes in the material. Orig.. art. has: 3 figures.
ASSOCIATION: Institut khimichoskoy fiziki Akademii nauk SSSR (Institute of chea",
cal.Physics, Academy of Scienceg SSSR). Institut fiz!Lki Zemli Akademii nauk SSSR
(Institute of Earth Physics, AcadezW- of Sciences SSSR)
SU%aTTED. 28May62 DATE ACQD: 0lJul63 ENCL: 00
SUB CODE: 00 NO REF SOV: 004 OTHER: 003
kes/~-
Card 2/2
I&ABININ, Yu.N.; PETROV, V.P.; MARKOV, V.K.; LIVSIJITS, L.D.; DELITSIN, I.S.
Additional data on the conditions governing the formation of the dense
modifications of silica at high pressures and temperatures. Izv. AN
SSSR.Ser.geol. 28 no.8:3-10 Ag 163. (MIRA 17:2)
1. Institut fiziki Zemli AN SSSR i Institut geologii rudnykh mesto-
rozhdeniy, petrografii, mineralogii i geokhimii AN SSSR, Moskva.
i~ACCESSION NRt AP4025911 8/0056/64/046/603/0821/0824
AUTHORS: Livshits, L. D.1 Genshaft, Yu. S.
TITLEz Nonlinear dependence of the magnetic transformation tempera-
tures of two invar alloys on the hydrostatic pressure
SOURCE: Zhurnal eksperimentallnoy i teoraticheakoy fiziki, v. 46*
no. 3,-1964, 821-824'
TOPIC TAGS: Curie temperature, magnetic transformation temperature,
phase transition, second order phase trdnaition, invare coelinvare
elinvar, Curie temperature pressure dependence, high pressure ferro-i
magnetic transformation, ferromagnetic transformation
ABSTRACT: The pressure dependence of the Curie temperature of the
elinvar and coelinvar alloys was studied at prebsureb up to 20 kbar
as part of an investigation of second-order phase transitions under
pressure. The relation I
P1.
Card
ACCESSION NR: AP4025911
Op- 8 ap - bp2,
temperiture ot magnetic' transformation at pressure p, 8~n~.
P
temperature,la and b -- consj:ants) is found to-bold for both alloys.
Although suc%i a nonlinear relation follows from the theory, previous
experiments yielded only linear relations, probably owing to the
smallness of
~the range of variation of the pressures employed and in
some cases tq, the smallness of the effect itself. A tentative value
11
dE)/dR = 3--3.5 X 10 deg/cm is obtained for both alloys (R -- in-
ter~tomic radlus,on the order of 2.5 "The material for the
samples was giaciouily furnished by G. 1. Katayev, to whom the
authors are deeply grateful. They also thank Yu. N. Ryabinin and
R.'Z'. Levitin'for i0terest in this work." Orig. art. hast 3 figures,
4 formulas, and 1 table.
card 2/~
ACCESSION NR: AP4025911
.MSOCIATION: Institut fiziki zemli AN SSSR (Institute of Physics
of the Earth, AN SSSR)
SUBMITTED: 14Aug63' DATE ACQ: 16Apr64 ENCL: 01
SUB-OODE.- PH NO REF SOV: 006 OTHERt 001
Card
ACCESSION NR: AP4010755 S/OOeO/64/154/001/008610087
AUTHOR: Livshits, L. D.; Ryabinin, Yu._ N.;..Beresnev, B. I.; Marty*nov,
Ye. D.
TITLE: A new relationship between the elastic limit and pressure
,SOURCE: AN SSSR. Doklady*, v. 154, no. 1, 1964, 86-87
TOPIC TAGS: elastic limit, high pressure metallurgy, axial tension of materi-
als, rate of deformation
ABSTRACT: The authors have investigated the elastic limits of va:r1ous steels
and of brass under high pressure. The ir method of investigation differs from
that previously used by a very high rate of deformation. The elastic limit E
(the natural logarithm of the ratio of areas of the specimen cross sections be-
fore and after rupture) was measured as a function of pressure p. In the pre-
vious work (mainly by Bridgman), a proportionality between E and p has been
Card 1/2
ACCESSION NR: AP4010755
found in many metals and alloys. It is shown in the present work, that in some
materials there is a relationship of a new type between E and p. At lower pres-
sures, there is almost no effect of p on E. The rate of axial deformation has
no effect on the dependence of the elastic limit on pressure. Orig. art. has:
2 figures.
ASSOCIATION: Institut fiziki Zemll im 0. Yu. Shmidta Akademil Nauk SSSR
(Institute for the Earth Physics).
-SUBMITTED: 05Apr63 DATE ACQ: 1GFeb64 ENCL: 00
SUB CODE: PH, ML NO REP SOV: 003 OTHER: 001
Card 2/2
7
I-A. -i Ai.f ~rTMI
A 9, F T ''--1'i r7 T TI-e a~-thors r e v! e tv tlzq- regulf-C of aa exporlmeriBA studv of the plastic deforma-
Tno~ v fll(~n
pres5urocz :twi 11) tt~( n v(' s t.
4,,, r t,,. p il 1.11 1j-n V f rV' "Vcts !p
=m-K ex
samples of quartz moncoryst.-da a, auperhigit Pressures amd- Mg-t- flemperaturbs (above
L 25621-65
T AP4049998
ACCESSION Nl":
';",,o lof,rmation, wil',,'-~in ri (rw, c,inin!cx. ir. ~w
de-ve'ops for thia most part- etuner parmim ir, mu piiuuQu, ,,
()r- perpenclicidar to it. "The mjthor:~ to thane 1. Lukin ,md V- F. Cherny*shcv
4 sh(
S 11 (Institute of
~'.SS'OC;"ATTION: institut fiziki Zemli AIN S-S Plivsics of the Farth. A"
Ths-Mut geologii. rudnv*kh mcgtorazlideniy, petrografft, mincvalmo-i 1 geo~ldulxrail. AN -131:1illt,
the Geolo p _~lineralo and Geochem
Moscow fLnstitutc of of Ore Deposits, Petrogra hy, - -gy
'EID: ~"51vlarf^)4 FN (7 1,
T- T
m! t-
K
firgh
'.~,S 1UN NF: AP5005241
AUTHOR, Livshits,,L, D.; Ryabinin, Yu. N.; Beresnev, 1j. I .
TITLE: Effect of pressure on the ductiliLyof metals
SOURUF: Zhu,:nal tekhnicheskoy fiziki, v. 35, no.2, 1965, 348-354
TOPIC TAGS: chromium chromium ductility, hydrostatic pressure, ductility pressure
dependence 4
16
ABSTRACT: To determine the effect of high hydrostatic pressure on the ductility of
metals, specimens of pure forged claroriium were subjected to tensile tests at ambient
IlvdrostaLtC pressures of up to 19,000 kR/mm~. 'I"he curves of the ultimate deformation-
pressure dependence showed that pressures of up t,, ~000-',')Wj ~P-';Trm'- ;ave iiLtle or
no effect on the ultimate elongation, but with a further increaqe in t6e pressure
the elongation sharply increases. An analysis of the resuAL.3 shvwed that sirallar
behavior 1.9 exhibited by a number of other brittle and low-ductilitV metals. The
metal giatn size appears to have no clalfect on the ~-p dcq)endence. This indicates
t~-- major role of the condition of grAins and the ie(nndiry tmportance of graiii
boundaries. Top~-tatnamore exact evaluation of the effect of individual deformaLion-
pressure factors, further investigacion is requireud. 01rig. aLt. has: 6 f1rures.
C.,d '/ 2 [HS)
L 27188-65
ACCESSION NR: AP5005241
ASSOCIATION: Institut fiziki 4emli im. 0. Yu. Shmidta All SSSR, mosc- (Institute
of -21lysies of the Earth, AN SSSR)
SUBMITTED: 09Kar64 ENCL: K, SUB CODE: MM
NO REF SOV: 003 OTHER: C02 ATD PRESS! 3191
Pill
Q
1, 41068-65 EITr(jn)/EVP(t)/EWP(b) IJP (c JD/JG
AC=-SION NF: AP50104.96 LM/0056/65/048/004/1050/1053
AWHOR: Livshits, L. D.; Gensh&ft, Yu. S.
J-
'71-_F~ '~-hift c-f Curie temT)erature of gadoliniumm, under hydraulic compression up to
f na r
SOURCE : ZhurnL-LI eksperimente-l'noy i teoreticheskoy fiziki, v. 48, no. 4, 1965,
1050-1053
TOPTC TArS: getdolinium permeability, gadoliniumm Curie point, gadolinium perme-
ability pressure shift, gadolinium Curie temperature shift
IrISTRACT: The pressure dependence Of permeability v- plotted at a constant tem-
~;A R ~'requency of 500 cps mnd effe_,;-tivt~ f'oll intensli'y 91' The
aj~pii~-A 'hr-,)Qgn EL Si Iv~- 'n- I" im ~" +" -1
-- i: +
me r; 9 w- r- mi in i a,. rr) 1 y C 7-~, 9 tnP MI- 3- ~:7 -M
a&- ri i im wn n
e"eriment di dnot exceed 0.5.w.1C. The pressure dependence curve of the Curie
~-LF Dif-Aled on the bexi~ of twelve independent determl ations f tb p
n o e ressure
-ni - t~e specimen 7hanizei A+,i+~, ~kF3 -xpected thin
Card 1/2
L 41068-65
ACCESSION 11R: LP5010496
curve wess a jtraight line with a proportionality factor of 1.34 J_ 0.06 degrees per
S r. 7,,e mean deviation of the e)cperimenta.1 points from the 3trai0t 111ne was
-mporEture and 0.6 Icbar !- prp!~~-~r- A i
'!~'haz pr)-,.39,,ire range -f the
4 1 9t)4 Al 87) w as nc,,. e -rig art. !_,Ets
FP!
__titUt--_fiZ-ikL zinLl i -Alkedemil- mauk SM
ASSOCIATIM! R (Inst.-itute of Physica of
Ins
the Earth, Academy of Rcience!,SSSR)
SUB CODE: 5~~ E m
T-: Cjqiov,64 :n
SOV: 005 CITHEP: 007 ATD FRESS; 3232
Card
, ; 'f , / , '~ Pf-4 :P(C)
an i T s-et, P;C 'I /~R 'ff. P
)/T/E P~ h)/Eff A(d "Kff
ACCIESS'1011' TUB:
AP50115 30
e_fy_f3 I its BLei~esaev, 13. 1-i
AUTHOR: I
6'h pro ssure
x -Ie '0 fit%
SOURCF: A14 S3SR- Do?lw~y, V, 1b1, n~c 1,~ 7
bismuth alloy, tin contaiping alloy, p-ijny
P
s,j t i It F re lat i onsh i p, bri tt lenes s, luct i i i ty
B1,kary Bi-Sn alloy cn-.AaJni;-~,, '.0 at'~r 1?1, --r 'dt'er
te47
fnatura-l-ly Fr L
-LUP ~~t-30-0--350 Ag cMT- t~he-aff~oj-fr act re7,Vag -b-ritl~j-
-vt- p -rei. -vu~r4e t-he rue-ture- became r-wre-7 -and-mejwc~--duati-le -.I ".the
,fVr,--ner increase-i -6 -
ncreased, the elongratJori CLACd
11.400-1=00 kg/cm2 ange the alloy ductility Gharply I reach-
in vressure
ari-I the r,2duction of area vg,-, 99.9%. With !~~ furthfir in
a) ductiiity derre-t-s-ed, pass,~A ;at,R
increw~ed ag&A.i to the oecond mriximum qt 9
pr%cti'2~.tlly to zero in the 11,000-11,500 k6/crl 2 I-angre With an increar-e ii,
2. lie elongation again increased and
presoiire frovt 12,000 to 18,000-20,000 kg/cj,- I t,
0,000 kg/, ~Iity dropped rain
tne fracture became ductile, while above-, ? - -Tr"2 tjIC -jIICt,
Card 1/2
11, 49-284-.65
1ACCESSIONT NR: AP5011530
and the f*racture became brittle. Thus, the experimental results revealed a new
ph~n,.rierian-the existence of prf-ssure ranges with'n which -, material can have a
or P- --ower ductility. It, i3 '-1j!; S '1z-S'- -iated
pe-ii-ritief~ of the p, T-diagram of the ailoy. -jrig. ar.. has: L- figures .
ASSOCIAMON: Institut fiziki zemli im. 0. Yu. Shffidta Akademii nauk SSSR
(Institute oLl Physics of the Earth, Acadevj of Sciences SSSB)
SUB:-~:7-17ED: noct64 ENCL: 00 SUB CODE: W~
UO REF SW: 008
OITER: 004 ATD p,,Rt-,S 4005
Card 2/2
M
M
L 34oo-66 EPA (s) -2/E~IT(m)/EVIP(w)/EPF(c)/EPF(n) -2/T/~WPM/EdF(b)
ACCESSION NR:': AP5024209 UR/0020/65/164/003/0541/0544
Beresnov, B, 1a; Genshaft, Yu. Sop- Ryabinin, Yu# No
"UTHORSi Livshits, L, Do;
3,3
TITLE: Change in strength of several substances in the region of polymorphic
3)
transitions under pressure
SOURCE: AN SSSR. Doklady, v. 164, no. 3, 1965, 541-544
TOPIC TAGS: polymorphic transition, rubidium chloride, silver nitrate, limestone,
calcium carbonata
ABSTRACT: The effect of pressure on RbCl, Ad103, and limestone was studied. The
investigation is an extension, of previous work on Bi-Sn alloys published by the
authors (DAN, 161, 5, 1965). Axial compression of specimens was determined at
high hydrostatic pressures. The specimens were of cylindrical shape, 8-10 mm in
diameter, and had a length-to -diameter ratio of 1 to 1.5. PhotographB of the
deformed samples are presented and stress-strain curves are shown graphica y
(see Fig. 1 on the Enclosure). It is conel 'uded that pressure affects the strength
of different materials differently during polymorphic transitions. Thus t =e
I'Gsisttance to compression of RbCl increases with pressure, that of limestone
Card 1/3
L 34oo-66
C SION NRt AP5024209
id is
F
increases alvo, but more slowly, and that of AgN03 shows a decrease with increase
of pressure. Orig, art. has.- Ygraphs and 1 photograph.
ASSOCIATION% Institut fiziki Zeml:L im. 0* Yu. Shmidtaj Akademii nauk SSSR
(Institute oil' Geophysicap Academy of Sciences,SSSR)
SUBD=TED: OlFeb65 ENCLt 01 SUB COM SS
NO W SOV3 003 OTHER-. 001
RUMRP'J~-~A' 4E
L 4oo-66
- -3~ _ _ _ __ -______- _ _ _ I - ---T
.0 ENCLOSURE3 01
A.CCESST N NR: AP50242og
kj~/iftM2
70
to- z0 IL
e ~14~D
'ZO
fdo 'C Ow
Ell
19
:3 alto 0 v0
43,
43
43 U)
5 to i0 JOI-1010 10!
Fig. 1. Dependence of reduced stress on pressure for constant residual.
deformation const,). a- RbCIiI 3%j 2 10%j
A
b- Ag1t 2%;
'03: 1 2%,- 1 2 10.%,- imestom
2 5%; 3 0%
I-VIRKOV) V.K.; LIVSHITS, L.D.; DL1,1TSINY J.O".; !,,YABIIIII,',
Cornersicns In metasillcate under high ~~ressures and
TemperaT",Ires. Izv. :If SZSP.. S:er. geol. 30 nc.7:-"IE-4) .71 16f.
IFA 18; 7)
1. institut fiziki- Zemli AN SSSRJ i Institut geologi-i rudnyl:h
mestirc-zhderdy, petroFrafii, r--neralogil i geokh-,,mil All SSSFF',
Moskva.
LUISSITIT3, T_ G., -rn,-,r. Cand. -eclh. `cd.
Dissertf-, t Jon: "Theoretical and Experinental 3,ibstantlation of tl'e CocLin-'- ~'F-Ics of
J '.
Rabb-ts B-83, B-H and E-T D.:rnF, 7s,='Ir All-Urion S.-I Res 7-.st ol
4, into I -
Mechanization and Electrificstion of AFrIculture - I Jul 47.
SO: Vechernvaya-MosIrva, Jul, Y.147 (Project #17836)
TT
Doe
Steel, Chromium-Nickel
Steel, Structural
'Uw-Alloy Structural Steel," L. G. Livehits,
Cand Tech Sol, 0. A.. TorpftnOTO, Engr, ToNlICherflEr,
4 pp
"Stall" No 12
Some alloy structural stools (in particular,
thome containing molybdomim) can be success-
fully replaced In many cases by proposed lov-
alloy steels of low chromium and nickel content.
Tncludes nine die one microphotograph, and
Uroo Itablesi
LIVS'lITS, L. G.
0 metodakh powjsheniia iznosos*uoikosti detale-- tral