SCIENTIFIC ABSTRACT ROMANYUK, N.A. - ROMANYUK, V.A.

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• Collection: Scientific Abstracts
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• Document Creation Date: November 2, 2016
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• Sequence Number: 19
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

L 00462417 EAT (I )1EV-rr (m)1F--VdP (t)/ETI IJP(C) JD/GG
MCC R AP'5024657 SOURCE CODO; ua/oo7o/66/bll/oo4/o6lo/o5l3
AUTHOR; Zholudov, I. S.; Romanyuk,
N. A.
t1vov State University Llvovslciy gosudars'Lovonnyy univorsitet);.Instituto of.
Crystallography- All SSSR - ii@`titut kristallografii AN SSSR)
TITLE: Diolactric .21@@rtios of clampod Rochollo-salt crystals
SOURCE: Kristallograftya, v. 11, no. 4, 1966, 6lo-613
IOPIC lj"GS: forrooloctric cry3tal, piozooloctric cijstal, oloctric hysteresis,
@'dioloctric.constant, pressure effect, Curia point, electric polarization
The authors report an investig tion of t the do struc' ro, the
ABSTRACT a maln L'u
loop, and the initial dielectric constant of Rochollo-salt r., 5 tals in
f
the region of the uppar Curio ton-porature for different degrees CA. conprossion, 6
the: samplos-The t a st. swbre made on suqaro polished plates with 450 X-ocut, moasur- d.w.:
i
ncr mm amplos were moasurod on a microscope stage in,
10 x 10 x@(O 4 -- 0-7) Tho s
U
47
a: thermostat oquippod with a dovico for simultaneous or successive comi;rass;.on CA.
porpond
crystals in two mut icular diroctions. This apparatus vas des-@
cribod1n, 'an oarlior.papor' (Krista,llog r&f iya v. 4, no. 5, 710~---717,119~9):.,Tii~,,,,:~l;;,-*,
Card'1/2
uw: 548.0:537-226

S/07o/6o/Oo5/oo6/005/009
E032/E314
AUTHORS'
Romanyuk, N.A. and Zheludev, I.S,
TITLE, PotarizatioW )f Rochelle Salt by Single-
I.A I JULI r-Lee tric 11ii Ises
PERIODICAL,, Kristallografiya, 1960, Vol. 5) No:. 6,
pp 4 911
90
TEXT: Abe- (Re f. 1) has described an. improved method for
recording the polarization of-Rochelle salt -and has studied
'processes occurring in t itne intervals of between 10.and
-12 sec. - The present.authors have extended the method so
that-it can be used to,study arization 'in
pol processes
Rochelle salt over time intervals of between.a, few tens
of seconds and.fractions of milliseconds. The modified
method is described as follows. Consider a fully polarized
specimen of an'X-section of a Rochelle salt-crysta.1 placed
in the extinguished position on the microscope st.age. I f,
the mutu ised
al disposition of the specimen and of the cro-s
Nicol prisms remains unaltert-d, then the intensity of
Card 1/6

S/07o/6o/oo5/oo6/005/009
E032/E314
Polarization of Rochelle Salt by Singie -shaped Electric
Pulses
vll] depend on th, dire@@tion of
leaving this sys tem i
polarization in the specimen. Di the case 0 f pa r t ia I
polar i za t ion. reversa 1. the. amount of light transmitted will
b e a f u n c tA on of the degree of' reversil. The , light @ beam
inc ident on the specimen was kept constant and both,the
current supplying,the microscope.lamp and the intensity
leaving the, mi.cros,-ope eyepiezefor a given polarization
statelwere stabilized.. Th e light beam,leaving. the eyepie@@e
was intercepted by the photocathode of a photomultiplier
(fEU-18) and th 'resulting signal was recorded-on
the screen. of an oscillograph (41-ji-I (ENO-I))@, Singl,2
Vr shaped electrical, Pulses 0:03-3 S.ec. tr_n_g@wcre applied
li r.izr (I
to the specimell from a pu,lse generater incorporating po
relay (Pi- 1 Longer pulses were-applied direzt ly@
te the specimen by switching en and oft' a battery..-
X-se,@,t ions o I' Roche I I e s al t erf? 4 tI ga I

a
C rd 2/6

S/07o/60/005/oo6/005/009
F,032/E3i4
Pala ri za t ion of Rochelle Salt by Single@shaped Electric-
Pulses
reversal time as a function of the pulse amplitude., and
the temperature dependence, of this function, are in good
qualitative agre ement with analogous curves obtained by
Pulvari and Kueb ler' in Refs.. 9' and 10 and by-Wieder-in
'Ref. 8, who used ordinary electrical methods. Well-defined
nonlinear and li near parts of these curves are observed
and the slope of the latter-is a function of temperature.,
@Fig. 2 shows.the dependence,of the polarization (photo-
current) on-the amplitude of the applied pulses (V/cm) for
different pulse lengths (I - 2 see, 2 - I sec. 3 - 0.4 sec,
4 o.15 sec, 5 - 0'07.sec-and 6 - 0.03 sec,, temperature
15 aC). Fi g. 3 -shows the reciprotal of the polarization
reversal t ime 1 /11:@ as a fumtion of the,pulse amplitude

8.8 oc" 2 0
@10.7 OCI 3 c., 4 ac
Card 4/6

211
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.
.
AUTHORS. T

TITLE:
Ij 0 r V a:-7.@
N

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Sal ,
tLons

ICAL
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71
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PERI
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ABSTRACT:
Shu I v@i s ic ti. Tec hn c a
%
L c
Phy
j
o i,
or
1
n' ndnutes
, a
o
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@
e
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'
.
l HO@IheLle
thors C
t
Th 3 a 1 t crystals into.
'
'
e au
axis.
, 4:::0
med unden
1-, 1.4 nm
0
.10 X 10 x 0. ;
he X a i Then, f. he I t ia e
to t r e c. i i..q e covered
,
with grlycerLn and at-,d those platles c h a. had
ains o t, b-
1 a rge c @(Iomc It
viere teStecl.

v I c e sh oa i n
10 by ti e de
1
8 + 0 0.
ti, . 1, wh ich has 'i
.
.
e
lever + Y.) I s- t o nset,,.-, transl@e-,,e to, !'.- 0, 11 OtI
er

i) L"I
-ibles t- I i e GIC J-e
nc
e t "J-f 0 r.
th-111 I t "-i'- - 0 'j,
@'
C ard 1/4 .
e
al te rn at e ly, '-@Jomg the thi@ y b b d: Z
.,
.

Study of the
4
/36,
Rochelle S6 1 f C vys t a o 0 Q
Structure Observationo
nx
@@le 011" a
the
loma In et":'LLOn-, n U@' o@' 0;-nn ro '@k 10 1-1 t o
C. On t' 1@ 0 1 an; I.J. m (1, -C @)y
Fri oupho Thus
e ow) le aw, Y 0
doma I r, areas Trie'as u -a n.
lCy of' ie dt k,_@ Co-vi- i o n b e
accurE f aol
'0' In Of ZT:reiz'.
exr)re;:l
tra In d I-le
Z;:
to whlch the orthovlhol'n'bie t@ 11 rn Into fliollocl-Inic
cQe - Lons t he - D I ate s
C Omp re s I rig, -a I e- r i a t y. J.,n
were turnel Lnt-o 0 1 0 r1l a- in
and -again in to lfsonodomz;in I.fq
en
disclosed that @Oads' 'he 10 l" s'tves'@ of
h,, e 1-he dorva Ln ttlucture
about 200 f:r:,/crre-. do not @m@f,
pplied for 2 to: hour@-, N e a the coercive-
even a
-0% d
stress change oC the 1", C.) w"ll'
dericribe-i b', Ci
"_j rof 0 .94
,2 J@nlil
'iT. J s
thic,k olate at 'J
and, t., the !,-;tt i.orl
1 U 10 r I L r 1 3@1 Ul I r@ @l
d 2/4 "a"L ici tr ti-e c a v f
Car

!@tudy of' the
U P I e-,-@oe I t - L.,: Po t ."a t, I or I of' 1,11-e-! i@

iochelle Salt.
Cryst-ai--,- to th-@ f tj
Structure Obs ervations
sidered In-,tend of' the coereLve stre@,,s. The @,.[)Pl- Lcat@on,.
. . . or electi-1.0 I'leic-1-1 or (,@ee Pig - 5) produced ,

ne ar ly pec, t; an-t-0 za r, hys t e i@e E, I rill e @ r,,,
oop I Yl at lonship
L
be tween t I ie r L p 1) 1. 1. e t, 'Y', o r
Y
E
lent electrlc Vield to the X 1-@
,
@y w
de-scrlbed by. Y heve e 1-1 the
2,
Y
piezoelectric- c,,on,-3tant ThCPe ave LIJ 1'iv ul,es; I table;
c e,
and 13 refever s, 83.Sovlot-, 2 anesse,
U.S., 2 Jap,
m@@,m The U . S r-eferences 11 H. 'vI iecie 1,, il. Appl.
pi-tys e2 4 413@--416 y , phys Rev

ASSOCIATION: Crystallographicall Institute of' the Academy of Sclences::@
of - the. USSR (Institut kvL3tallo gvl,,f'j.i AN S S "-dR
SUBMITTED: MctY 9, 19 59
Card 3/4

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ASSOCIATIOli:-:;~...16'~,VOVS~~~y..gq~,~idd
Univis re-fty) 9- ki tt'k.t,t.-, 'k,ri fiilt-@ I

S/07o/60/005/603/015/024M
E132/E.46o
AUTHORS, Romanyuk, N.A. and Zholudev, I.S.
@TITLE@ A Study of the.Slow Electrical Polarization Processes
in Roahelle Salt by Observations of the Domain Structure
PERIODICAL; Kristal.lografiya, 1960., V01@5, No.3t pp,403.-408
-TEXT, Pla@es of X-cut Rochelle salt about 10 x 20 x 1 mm were
s.11vered.. ex?-ept for an observation hole in each, and were
examxned with a polar-lzing microscope normal to their largesir
surfacss@ An electriz fi.eld.of.some 400 v/cm could be applied
parallel. to-the direction -of observation. measurements were made
t - alb ou t8 It was found that-the single domain statii-produce.d.
-by' the, field was rather unstable when the' field was..removed, The.
Stabil-ity ia le35 the smailer the initial domains" in these*cases
fields iakn or-der of magnitude greater than the coer-@ive field are
n5aded to produ,.e a single domain structure. The single domain
state @i,5 mos-stable if the majority of the initial domains were,lin
.t@e@ direc tion . chosen for polarization, The observation that the
crya-%al sooner- or later returns to its original domain configuration
,..-:"Indt@,ates the exseptional stability of.the latter, The change.:of.!_@
S with time of a growing component of a twin under.the action
Car d 1/2

8%91
xx
S/070/60/005/003/015/024/
E132/E46o
Study-of the Slow Ele,_@.rical Polar@ization Prosesses in Rochelle
Salt by Observations of-the Domain Structure
of a field whLch is near to _cosrt@ive field strength is approximately
des@_jr-ib&d by S kexp (. a/t) where t is the time since the
.-he field and a d n
application of epends on the field a d the
w seems to be applicable,over a
hisrvory of the.specimen, This la
e of field strengths. There is no, threshold: field,,
wide rang
c-The sm-allest field obserwed to produce a change is 20 Y./cm.
A crystal of Roshelle salt has. istic; of
a certain c;haracter
Avrem=-inberinsll. earlier statt5 of domain- structur't. With the growth
of the field strength the 5tabil-ity -of the polarized state in--reaset
arid this leads to the,growth of the coer-civity. . The abser-red
decrease in the coercl.vity onrepetition of the hy.steresis c;yccle
.indi@_atea that the.first in some measure produces condition3
facilitating repolarization of the domains -in succeeding cycles.
There are 3 figures and 9 refiirences@ 3 Soviet- 3 Japanese and
3 Engli sh.
,,-:AS.SOCIATION,, In5-titut krLstallografii AN SSSR
(Institute of Crystallograph'X. ASUSSR)
SUBMITrED Dr-ember 19@ 1959
Card 2/2 :.7@_

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x4o,rble arid ID in the nrottil tistne tirlRodiien ilie,tige -09
so of the fish. 'ibe content of 14 the licaul is nealy eqUAI .00
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Pl8ke I is VeVY CIOW to that Of reptiles And *MPilibiAns.
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approximating tha
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ROMAMYUK, N.
The infiuenid@ofthe anilblutics'of garlic on the actiAl

t
C
i
l Ab
t of proleolyfic enzymes of mail tpors of hi@pans at,
ex gnanttu
perimental animals, N. At.--ftotnati@,tik
ca
s
rac
hem
p R;1(110-011COL JuSt,. Kiev), Ukrain, Wokhiiil@ 4111ir. 24,'.
Nay 25) 53.6(Xin Rusikin, action of the atitibiotiC5
Biological Chemistry (1), of garlic are in@cstlgatcd' with Cathepshi (11) froixt humall
. tutilor (postoperative inatcr6l) atul allituat tuilmrs
cutnucous tumors of white mice).@ It cauFt,.i an increase Of
the free carboxyl groups of Lite tumor ttistte. thwi I'
crease or decrease of the activity of 11 undur the infla nce:of -
.1 catt be easily checked titrimetrically. 11 from li I's of.-
ac red- The llcjw@.
white mice and plain mice %v..; also coutim red- The
itig restilts ivere obtuined: The activity of the liver 11
increases in a in etard
alignant. growth. Thc I of garlic r
Or the activity of liver 11 of attituniq sufferhig front malig-,
'
-
itant growtIts, and retard it -it little in' licalthy aniinals.
The garlic I inhibit somewhat the 11.0f Malignant tuittors

of huni.
ans and nuhmils. In expts. in which r the tutnor-
ext. was fincly dispersed with garlic,, tumor devilopmek
%ras retarded. Weriter Jacob-2t

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Part Of the animals; when the tumoF.
X 2.5 em.'size, were subjected to x-ray irraclia-,

f
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OEM at the lomtion of the tumor with it daily dose 200.
'
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-

with the tumor but-upi
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(Uc1il6
S0V//7o-5'_1-25/30
AUTHORS: 3 1 v os t ro v,,,L, IM 1o!."-_1'nyuk N.A

TITLE: Effect of.the Exposure. o@ Tr1rly-cine Sulfate Grys tals
to Ultraviolet* Radiation on Their Ferroelectric
Brief Co
Properties. rrimunicationS
PERIODICAL; Krlatallc.@@raflya, 1960, Vol 5, Nr 1, pp 147-150
(USSR)
ABSTRACT: Radiation damage eff ect in Rochelle salt,and tri-
..glycine -7-ilfate has been known-. The authors
e
furthered the studies. Triglyclne oulfate plat a
.,
.
0-5@to 3.5 mm thick,,parallel to the cleavage
running i,orinal to the polar aXiu, became dull and
yellow aCter 20- to- 0-hr exposure to :ultraviolet
3
radiation emitted from quartz-mercury lamps
DRSh-100 and SVDSh_250., The hystereisis loops
became distorted as shown in Pig. 1- The exper@..Tentu
revealed that absorptulon In 0"-rmn-thick.,piates, decrea@e3
from nearly complete. for iovt -;nrave: ul traV lolet -rays,
Ca-rd 1/6 -to .5,(% a t. 250 ifil-L and te-) 40il for -:vriolet -rays with

Iv
(,L,yT; tI.-,tU itvavlolu t
1 - 2
/3

Ff VI@oc:le(@I
VIC

1100 11111, W th
1, V ray @I 250 MJL
-he fe
proved to-at'Vect. L. --vvoelectvic prope-Ptlea of
triglycIne OUl."dte to a gi,eater extent. The
,
radiation effect was not conVined to a surface:
layer as- two different experiments -verified.

l.adlation begun to alter ut
Ultravlolet ie hysteres
loop in about 115 oecoridoi Airther radiation d
ld
@
Ilot affect spontaheOU.'. polarization but. Increased
,
the coercive field and moved tile hy@ltercoi@ loop
along X axis until a new stlabl:e tate was achieved
C:@

after A months oU r
-adiation. The new state re-
mained stable even aftev
annealing above Unto Curie
,
point;- for 11 to 5 hr, or after keeping- the specimen
In a strong electric field. The expos!uru@ to
ultraviolet radiation proved to decrease the
dielectric sLisceptibilit'r of triglycirle Oulfate
f rorri 47' to .30 at 250 C -1/6 vs tc-mperature curves-.@::.@.

Ile Cur i
(FIC. 5) point W the applicability of
Weioo Law to both expo@ied ar-td iirtexpo,@ed 'q)ec-t
Card 3A
E I IMSE1112 I

-------------
Effecu of tflie E.,---poSL,.r - ft16
e of Tviglycine Sulfiat@._
Cryotals to Ultraviolet.Radiation on Their
15/3 P
S Wjf7, 0 -.1 2,
Ferroelectric Pror)erties.. Brief Co I
mmu n J_ ca, i on.,
S@,
of tr1glycine sulfate. Lx re':`
POSUre to radiatJon chanL
the slope of' the C- vs tlemperature- curve
-is@-ance,
and makes. the plates less elastic. For it
-13
3_@, decreases f rom 87 .16 lo to 84-95 x 16
rarn 71 lie .Piezoelec trio MOdUlLIS d de.creases
23
8 -8
f rorn 62.5 X 10- to 46.7 X 10 and 39.2 x 10
CGSE units after expoSUre to radiation
for 12
and 24 hr respectively. Me piezolelectric modulus
of an exposed specimen Increased, however, qo 05.5 X
x 10 CGSE units again aCter application of direct@,"
electric field. I. S. ZhelUdev Is acknowledged
for advice- I. V. Gavrilova for specimens,:and V.
N.
Varfolomeyeva for assistance. Theve are 5 figures
and-7 reCer.ence3, 5 Soviet, 1 Indian, I U.S.. The
U S. reference Is: A. G. Chynovieth,, P- s
nys. Rev
113.Y 159-166 (!95(-)).
(@ard 4/6

-@NEIHY L.S. KOFICTOTil I T@@.KAY A, O.L. M, I L' SHTEYN

rerel. a 1 c@-; d
kr, I, -VA. i nectiozli. sub iitute. Trudy Kiev.
lhir. 3:103-106, 161. nauch.-iEsl

I P A17:10)
,@J)Iastnapl th it t's I !van tya krovi.
ITI e

5-8-6-
01 /43
85-
-
1
ports, SaVLEI, A.,
R V Honcra---y 1,1aster of S
ili@ster of Sports
TITLE Delayed Group Jum?ing f --aa 'the Strxa-tosp7here- (G-rappoN-j-yol "-I
prjz-'ik-i iz strat, a . . .

PMODICAL 6, -I)p1
K@Jllyarodi--Y, 195', 7-19 OUSSIO

ABSr
PIWT: The -authors botli parachatists, distuss ye@ xrouj
- altitudes,, a quas 1 itarj t@rpe of X=c:I- mc-
frov, Wigh.
.
-)a- Its
quired urtle,--lax- i-,:, xce c.:'. ter I.,.-ch - =C'Atti- m,--m ra v e,
the Soviet rec o-,--d im. the- s*..' ons
::*ing 0' 1957

for the nee; interna;bioaa- ery@ inc-IuFW@ thle eboice o? tile
I c ont
Sohoi im-It'-seater turlbo-je- TiLa-aei cw,)do e of
02 15,0100 to 14 ;300.mlcte:@s. Seve---al tcs-*- fjii@s Tre--- mv2e avA
atteiatior- -..ms clct@l ne.
rient. The cuntaoia@i- jmv.) :aeLyiet 2:Lsc.,x=r- in J7a-.ro:r o
eolvii,:
,
the "gernoshl-Mil! Clctiixn@; incluil-,e- taLn -irool
or si-'-'- jeLmey undervear -,io::,2 unrlez. a y:ei-3r,-=a aui U, Yre- rhich
the usual -fl-,..ring corit-12"t @rcs S*@')"c:L21- equt-,'-peat Lmcluc@eci P.-

tez-y- to heat -tL,-- &riac3 c-f t@iie helmet dm.-@ag the .-rec
o
at
fall a hit-I attached -to -6-1:le iirrne.-3s coataim-@@ the
Card

3,-
Lue','e
De-layed Group j'j=o Pron the S@
ing
of
0 to-I Tlu'@
instrwient for recoreUng the jurp, =-O- an mvA,;!r. it.
110 ?evson,
panachute, clotaing end s-)ecial e,,.tuiWent .ras 5; hc:. 'ralc"' the
=uie-
inost impor-tant itejas upre the clofw-J."! .'Z:'Unt; axne, ae a. !-, c 1
re fL:"'t'
met. Five test M&Tita i re.Luv,'.c f@:r_c 5 ;r;. to
-0
5,000 in. flight -'M' 6 Lade @A`Zlhout an oxyg@-a a,@tfi t r; adw, r'.; 'Urte u.-ganf-1w.
higher altitudes; 30 uinuter, irero o--,c s:I. 5,0CC) u. -wr_O, t, u duscon' i.,wde 11-tt, a
nt 11 - . ."
speed of 55 to 65 Lq./uec. Uie secor.O. fli@-@xt, at 12,-NO x. IMI, .-)rC3SU=e
clothing and 7 ,uiM, ent, e@.x__-A 1-@=' e "*w-= _-teo t!-Ie
ftL11 er
hermet'L-_ heliaev trLc -oaraclnitistz ordina.--y -wilic-', Scrue
Sy
relievecIL presware on the ca-- druris &i=L-qj the gt@,-c fa.LL itu
to hold the nos . ar to -v4_@x@ wzeait o-.f t!le ra c 0
e d. also @e 3-u:@t,';ce. pai.
etc. Altit&_es we-2e Epa-diml-ly -to :u. @'.nlie -21rst jlar-)-7
made from an altitude o-rl 1,500 r-., the --P--ee lastia,-, 20 seconds. ::a.
quent flights paracluxtuists ball ee- out ki CO-1 ec@ul-ritzit at 4)0000 vit:i a
j.1inse IM-.4hts. estAt'hTishee, triat Vie he:,Tintic heln eq Ulnc@i
free fall of '(00 m. r
txcco-ptecl ;Anc-i It
some modification, The mcdified equipment wan h
made b=leathing easier and- wuLuld 'T., 1 COLI '.i*-' C!13TCUtS i:'-% frCe
I-ot-ect the face __Cr
1,1,, JJJM7@; planc
falls. - The entire group partic:1jr-tedl. :Ln t-1-he thi--O- t--ain-L,
climbed to its uw. to 2)('10- !.1. whe@:e -jt@k_
xiJum altita(le, then d=up-wd v
Hermetic helmets Were worn, and the glaus L't 4%011ecc eii not. f013 ove:4. Cont:-01,
2/4

Delayed Group Jumping from the Stratosphere 85-58-6-21/43
of the'body In the pressure suit was much more difficult; movements were impeded
and the to be dfie to the
parachutist's,hands almost immobilized. This appeared
asymmetry of the clothing outfit. The third jump confirmed the advantages of-
the hermetic helmet, leaving open the problem as to whether it should be kept on,
until landing or removed'once the parachute was opened. Some of the parachutists
maintained that the helmet prevented proper gaging of distance to the ground... It
was finally decided toremove the glass immediately upon opening the parachutei
since if the parachutist landed on his side, the air hose might becomelblocked and
.,stop the oxygen flow. Hermetic helmets were worn on all subsequent flights. On
20 August 1957, a record delayed jump was made from an altitude of,15,383 m- by
honorary Master of Sports N. Nikitin; on 21 August, the group,-consisting of
N. P. Zhukov, A. VanyarkhoY V. Petrenko, Ye.,Andreyev, P. Is 'hchenko, and
V.- Romanyuk jumped from an altitude of 14,811 m.,'vith a free fall of 14 1045 m.'
setting a new All-Union and world record, Parachutes remained unopened for 4
minutes.. The entire group landed within a radius of 600 to 700*m- from the des-
ignated area marked by a white cross measuring 5 x 80 m. The jump reaffirmed that:i.,"-1,
maintenance of-body control was much more difficult in a pressure outfit and that.
when parachutists succeeded in ettaining the proper balance after bailing out,
Card 3/4

Delayed Grazzp Jxnping from. the St:@P_tos]@iere_ 21/413
the he2zet-
Iftey were not always eCole to maiatell-la it. It fa7,-ther establisheCIL that
made the parr-chutist underestimB&.e the distance fraa the ground, because the sen-
/01 to 2.WO m. A, szeciall somd
se:Uon of spead in falling wez felt only,e. 1 o,
sigaeling device timed for:an altit-j.Oe 0@ 1,500 m-, wz theref,_xc-_ used. t:) !--A-
dicete the wpprop-ch, to the gro-ar-d. The @ first del-Ved night J=2? vas made
fr-= an a1titude of:14,332 m.J. ou 27 A%Ktst (19571 by N. Kikiitiu,'G. Nikolayev,
-L-sa OrieatattmWas emmlicate
ye. Andx-eyev, P. Ishchenko, and the 2 autho in -b:@C
w lig4ts and are g---een an& i&fte f LarhUght w= used to sigm lie i2ace of I=dJ-v,
The night Jimp,established that stranger ashUghta wei-encedea -4th Oi4ceec-4wol
U
lights. The free fe.11 lasted'ebomat 4 mizates and covered- 13,543 m. The gr
'ae 'a *get,
2.9ad-ed witLhin aradius of 300 to 4W m. k ia one case vk@.tdu 100 M.
personeaities mentioned. included B. Ecb_--ik-or, X. Fedorov, A. Shishkov,
V. Zhitnik. There are 2 ybotographs showing pa@.v_a:rxtists P. Ishchenko and-
N. P. Zhukov in pressure outfits.,
t
j =Ping-ussft
c er,,, 4/4

fj
49-12-15/16
Dissertations Defended in the Scientific Council of the Institute of
__qj the Earth, Institute of Physics of the Atmospher-e-a-in-d-
-Institute of Applied Geophysics,Ac. Sc. USSR,during the First
Semester of 1957. (Lv. Ako-t- P-J", S5S.@, See_ rL 1'15 7, p
V.A. Romanyuk Determination of the Gravity Forces on the Sea
b tHe Pendulum Method (Opredelenlye, tyazhesti na more mayatnik-
ovyM sposobom) - Candidate dissertation'. Opponents: Doctor
of Physico-Mathematical Sciences I.D.-Zhongolovich, Doctor.of
Physico-Mathematical Sciences V.V. Fedynski
y,.Candidate of
Phystco-Mathematical-Sciences N.N. Pariyskiy. May 31 1957.
The author attempted to makea more.exact'analysis of the move-
ment of a pendulum on a mobile support with the aim of deriving
more accurate formulae.and developing methods for the calculation
of.the action of acceleration and inclination-of the base of the
pendulum. The dalculation-of this action is precisely the .most
important and least clear problem in the theory of the measure-
ment of gravity forces on sea.
The author obtained a formula for the correctiQn of the inclina-
tion and acceleration of the support in the observed value-of
gravity.force which is valid for accelerations below 50 91.,
Card The.mainterms of this rp-Lation.correspond to the corrections,
12/21, of Brown, but there is' some divergence In the terms

49-12-15/16
Dissertations Defended ill'the Scientific Council of the Institute of
-Physics of the Earth, Institute of Physics of the Atmosphere and
Institute.of Applied GeophjfsicsAc.Sc. USSR during the First
Semester of 1957.
which depend on the periods of oscillations.of the pendulum and
the accelerations. In many cases, these:terms.can be dis-
regarded., The problem was formulated and solved of determining
'the accelerations and the'inclinations of the mounting by means.
of inclination-meters and accelero-meters. Attention is drawn
,to the erroneous nature of the view relating to.the, compensation-
:of the@term'
durinE: the observation time (!Z vertical-
-0
acceleration component of the mounting inan absolute system of::
co-ordinates). Under certain unfavourable ponditions, partic-
ularly during,@ob,servations in submarines, z can be consider-
ably.larger than the value of other correction factors.of the
second order. For reducing'the influence of the term 2!
0
the author proposed to* ine re ase th.e number@of measurements...
at various sections,of.th fi-im, during determination of th
e e
average period of'the pendulum; for this purpose it is jaecessary.--:1-1@1
to carry out recordingsat the beginning and at the end of.
bservations at high-speed of movement of the-film for durations@
Cardl3/22

49-12-15/16
Dissertations Defended in the Scientific.Council of the Institute of
-Physics of the Earth, Institute,of Physics of the Atmosphere and
Institute of Applied Geophysics,Ac.Sc. during the.First,
Semester of 1957.
of 4 - 6 minutes. The advantage was emphasised of constructing
@pendulum instruments in a cardan suspension with a minimum
natural frequency. , It is not advisable to apply a damping.
device.of the cardan suspension, which is linked with the, ship.
Methods were-develo-oed and investigated of evaluating the
recordings of inclination-meters and accelero-imters for obtain-
correction for the inclination and.the acceleration and
appropriate calculations were made based on materials collected
by marine gravimetric expeditions. It is concluded that it is
in principle.possible to,effect pendulum measurements on surface
ships provided that the,acceleration of the ship is below 20* gl;
at larger accelerati -ons, considerable.difficulties occur.
associated with the determination of the accelerations and
inclinations.
(;ard 14/21
Z@

AUTHOR: Romanyuk, V. A. 49-3-6/16
TITLE.-, Pendulum method of gravity measurements at sea, I..
(Opredeleniye sily tyazhesti na more mayatunixovym sposobom.I.)
PERIODICAL: "Izvestiya Akademii Nauk, Seriya.Geofizicheskaya"
(Bulletin of the Ac.Sc., Geophysics Series), 1957, No-3,
(U.S.S.R.)
ABSTRACT: The author derives, from the general theorems of
theoretical mechanics, the exact differential equation of the.
movement of a pendulum, on a base with six-degrees of freedom.
In.para.1 the differential equations@are derived of the
movement of a Dendulum on a base which moves arbitrarily,
eqs.(13), P.3",; it is thereby assumed that a physical
pendulum rotates about a mobile axis OA in such a way that
its rotation axis always coincides with the base, Fig.l,p.342.
in para. 2 the orientation oftlie base in space is discussed
and the coefficients b occurring in eq.(13), are
-the basis ik' of simple ge metrical considera-
determined on 0
In para-3 the exact differential equation of the
Dendulum movement is transformedlinto an approximate equation
by expanding into a series and retaining the terms up to and
including the fourth degree. The differential equations of
the movement of a horizontal elastic pendulum are also given.,

0THOR: Kirillov, F.A. 49-3-15/16
TITLE: Conference of junior research workers,@engineers and
aspirants-of the Institute of the Physics of the Earth
Ac.Sc., U.S.S.R. (Konferentsiya mladshikh nauchnykh
sotrudnikov, inzhenerov i aspirantov Institutaliziki
Zemli AN SSSR).
PERIODICAL: "Izvestlya Akademii Nauk, Seriya Geofizicheskayall
(Bulletin of the Ac.Sc.,:Geophysies Series), 1957, No.3,
PP-411-415 (U.S.S.R.)
ABSTRACT: The conference was held on December 24-26
1956,9 21 papers
'were read relating to work completed in 1955 and 1956.
In this report the-contents of the individual papers are
briefly summarised.
V. A. Romanyuk read a paper on.determining the force of
--gF-R@vy @6@n sea; it is stated.that other authors did
not take into consideration the rotation of the base when
'lating the differential equations of the penddlum.
formu.
@movements andt therefore, he derived formulae in which thiP
@rotation is taken into,consideration and,which are,
convenient for practical utilisation,
Card 1/4 A. V. RyLkoy read a paper on measuring the energy flow of
seismic waves. He. obtained several recordings of the

49-3-15/16
Conference of,junior research workers, enE;ineers and
@aspirants of the Institute of the Physics of the Earth,
Ac.Sc., U.S.S.R. (Cont.)
energy of seismic waves and evaluated the energy of earth-.
quakes comparing the results with,values calculated by
means of a formula which is in use.
avesti
V. A..Smirnov discussed his i gations with optical.
instruments.for measuring the seismic inclination proposed
by G. A * Gamburtsev.
I. Reysner read a paper on,"New movement of the Alay
depression and the mountains surrounding it".
N.. N. Leonov read a paper on the present structure of the
Pamir-Alay region and comparison of its structure with the-
seismicity.
S.-V. Vinogradov read a paper on acoustical observations
in (coal) mine workings and he concluded that such acous-
tical observations are of interest from the point of view
of investigating physical processes.taking place in
Oa@d 2,4 earthquake, foci.
V. I. Myachkin read thepaper "Study of the stress state. of-@.
a massive under.mine working,conditions.by means of ultra-7
sonics.

49-3-1546
Conference of junior research workers, engineers and
aspirants of the Institute of the Physics of the Earth,
Ac.Sc., U.S.S.R. (Cont.)
I. S. Tomashevskaya read the paper "On the problem of
investigationof che shear modulus of rock specimens under
conditions of high-pressures from all sides".
G.. I..Silayeva read a paper on investigating the propagation
lastic waves in rods and plates.
The paper of V. S. Isayev was devoted to the study of
distortions,of the wave-pattern in the case of grouping of
seismographs (explosions) in seismic prospecting.
S-A. Fedotov read a paper on the kinematic and dynamic
features of waves.refracted at curvilinear boundaries.
n d@pole lectromagnetic sounding.
Ye. V. Rybakova read a paper o e
0. M. Barsukov re.Td--tJfd Tz@7p__&F Certain problems of the
method of measurement in an elliptical polarised.electro.-
magnetic field".
-the paper "Diffraction of electro
B P. Dlyakonov read
magnetic waves on spherical inclusions in.a two-layer medium".
I. I. Rokityanskiy read a paper on the study of.the induced
polarisation in ion conducting@rocks.
Caxd A. S. Bollshakov read the paper "Magnetic stability of rocks".
3/4
S. Taychinov-read the paper, "Magnetic properties of
sedimentary rocks in strong.m.agnetic fields".

Yk4lv
V
AUTHOR: Romanyuk, V. A.
49-4-5/23

TITLE: ' -h a. b e
_:_D@eeriination of the:gravity'force on e se y th
pendulum method. Part II,
(Opredeleniye sily tyazhesti na more mayataikovym,
sposobom.,II.)
Ak d N
a emii, auk, Seriya Geofizicheskaya,
PERIODICAL: Izvestiya
,
,
1957,' No.4, pp-.45847O @,(USSR),@
ABSTRACT: In Part .,I'of,.this paper (Ref.4) -the dif f erenbial.'equation
was derived':'of:-the moveme'nt@of a fictitious pendulum,
Eq: (1) i p.4580' , :It. Was,'assumedth6t -in this oqua,tion''

smalL
orientation@.an les of,the base (%, P,7 y_and (p) ar e
9,
valuesof the first order and all the terms, incluling

that.of
n
the fourth,order, were m6intai ed., In this,
1
paper an evaluation is made of.the influence of the
disturbing-terms of the differential equation of. the. .
movement of"a~'fic-6iti.o,us:pendul-dm,on its average period.@@z'@;..-...@
For the observed values of the gravity force the second'.

r ctions u e nsl
order cor e @d e to th influence of fhelinatid
and the accelerations.of the-base are determined as

well as corrections for the non-isochronous nature of:@t e
h
ndulum.and amplitude corrections., The results obt' d
'pe
aine
..Card 1/2 .
by the autho'r'bf this paper.are then c ompar ed with the

-O'VIL@9_59-2-20125
AUTHOR: Romanyuk., V@ A.
TITLE: On Perturbations ofthe Force of Gravity by the Atmosphere
(O:Vozmushcheniyakh sily tyazhest:*L atmosferoy)
PERIODICAL: Izvesti-ya A-kademii nauk SSSR, Seriya geofizicheskayaj
P 320 (USSR)
1-959@ Nr 2@
ABSTRACT- Precision of measurements of variations of the force -of
,,o,,ravity at agiven point has been considerably increased in-.
recent. years. The number of observations of such variations:
has also.increased. To use the data obtained by observation,
it is necessary to be able to exclude a large number of
perturbatin- factors in order to.obtain-the correct value of
S, not
-the -ravily,, One of such pert rbating factor , which i
U u s
allowed for at present- is the attraction of the atmosphere.
Simple calculations-show that variations of this attraction
may reach values comDarable with tile 'magnitude of attraction@:
by the moon and thesun. Because of the smallness of the
attraction due to alt.-mosphere and to simplify further dis-1
cussion, the author assumes the earth to be a sphere, of,radius'@..
-Card 1/5

SOV/49-59-2-20/25
On Perturbations of tiie Force of Gravity by the Atmosphere
R Effect of attraction due to the atmosphere on the
gravity was considered at a point k , which is at a he ight
H above sea level.: Attraction of the.whole terrestrial
atmosphere at point k can be divided into two parts:
1) attraction due to the layer between the earth's surface
and a sphere of radius: R +-H whose centre coincides with,
-the earth's centre; 2) attraction due to the atmospheric
layer outside thesphere of radius R -L@ H . Attraction. of
-be reg with sufficient accuracy
the former+layer may garded,
As bein- constant and directed towards-the earth's centre.l,`;,':@@
0
This attraction can be added to the attraction by the earth'.,:
as a whole-and need not be considered any further. Attrac 't -'7
ion of the latter (external) part.of the atmosphere at the
point A will be equal to zero only when the atmosphereas@@:-:@,;
not perturbed i.e, when the density of the.atmosphere is
constant. Conversely, if-the atmosphere is perturbed, then
its attraction is not equal to zero. The author discu.7sses":.+I@, I
the following simple case of a perturbed state of ti:Le atmo 5
7:
_Ohere7 which is of practical interest, and calculates.the
atmospheric attraction at the point A .',The author assumes:.
Iregion bounded by a-circle ofl.--
'he atmospherie pressure in a 0 J
C+ d 2/5 radius r with its centre at the point ..A at a height of
ar

SOV/49-59-2-20/-5
On Perturbations of the Force of Gravity bby the Atmosphere
The
H above sea level, to be constant and equal to. PA
-s
atmospheric pressure at all other points on,the.earth*
surface is also assumed to be constant; and equal to p
0
Since the area of tiieformer region-is considerably smaller.,
the area of the latter region, then the change
than in.
the
ra-essure near@the point A does not in practice affect U
PO The author assumes, fherefore, that P can.,
0
be equated to the normal atmospheric.pressure at the hei-ht:..-,
H above,sea level, Using a formula for attraction by a,
r 4
unit s-ohe @-,al layer and a unit plane layer, the author
f ind sattraction at the point A due to condensed atmosphqre.,,.,:,
to be eTual to -
Ag 21(f p (p -pA) =.-O-000568(PA-Po)m'l.l'9als
0
Where is the density of mercury, f is the attraction..'.
constant and -p is,pressure in m-ra Hg. If r-" 10 h where'':
s th h
-d atmosp eric layer.
h i e height of the perturbe
Card 3/5

SOV/L@9-59-2-20/25
On Pertu bations of the Force of Gravity by the Atmosphere
r
error in determination of A -, from Eq (1) does not exceed
5116 (Re f 1), which is quite sufficient for practical appli-
ns. Co-rectionto the observed value of the force of
catio
gravity is then equal to:
+0.000568( p )milligals. (2
PA 0
Assuming 760 mm H,-3 to be the normal' the author
pressure,
-ectiDns given in U wo
calculated a set of cori the 'able belo
P @M -
9 P
01
L
A A- mi
milli-als Iligals
700 -0-034
760 0
-006
710 -0,026 770 +0.
720 -0,023 780 :+0 *011,
730, -0-017 790. +0.:Ol?
740 -0.0111 800
+0.023
7 50 -0.006
.Card'.4/5,:
L @0

PHASE I BOOK EXPLOITATION sov/3681

Akademlya nauk SSSR. Inatitut riziki zooLL
Voproay Instrumtntal-noy gravlmetril'. fabornlkl (?roblema or
Instrument Gravlisatry; Collection of Articles) Moscow
6
12d-vo AN SSSR. 1959, 76 p. (Sort*&: Its: , Trudy. No.
/175/)
-
t*d..
Errata slip Lnuort*d. 1,500 copies PrTn
Ed.t Yu. D. Bulanzho, Doctor or Physical and Mathematical 3cl*ncts;
Ed. or Publishing House:, V.0. 5erlLgautj Tech. Ed.; Yu.V.
Rylina.
PUR POSX; This publLcation 13 Intended for geophysicists. physicists,
h7drographsrs@ goodestat,s. and '"'Vig"Gra.

COVERAGE: This in a collection or eight articles dealing with grayl-
metric Instruments used In oceanographic Investigations. Do-
so
riptiona or the Instrumento.and data an test results are given.
No personalities are mentioned. References appear at the and of
some of the articles.
Popov, LT, Quartz Cravloeter for obabrvAtlona on the Ocean. 32"-'.
.
A dencriptlon Is given of a quArt.- 9rAvIx*ter rof now
photographic recording or the readings.
design with
Strong damp ng Of. Its elastic systnas makes observations
,
possible wnile movi" If the Instrum,snt Is Installed In a
global.
'U for Recording Incline and
SukhOdOI1sk&X_Y_V, Instrument RN
In Orevinetric Determinations On the Ocean 42
In addition to the recording or Incline and accol-sratIon..
the instrument makes galvanomatrtc@rscording or YLbratLons
which are converted into electrical OaCIII&tIonarrby means
or suitable tranamitters. Data obtAinftd during expeditions
to determine the nature of vibrations, Inclines and &CCajerb-
cIons acting an the 4acks of a dlesel-alectrIc ship and the
expedition vessel!"Mikhall Iomonowov" are promented.
-'BulanzD1_1@_R, Vibration of the Support of Quartz Gravlmetera
fth-gorizontal Torsion Wire 54
Effect of Support Vibration& on the
List ion wlod 61
K I y_y,.A_ Gravity Dots rmination by P@an,a of a
Z
u@

.
r
,11..r an a Moving Base 68
l
Berazin EaL.. and V.A. 99ZLYA=V-- xomogroms for the
;iiU@OJtlon of Cof-ri-et-Inns for A.plitd.. -eisp-vrature.
Depth Of Sub"ralon and Satv8s Effect and for the Determination
A of the Coefficient or Vibration Or the,Support In Pendulum
Observation. on the Ocean 72

AVAILABLEt Library of Congre as

MITHOR ream Ellen
TITM Chronicle
7Z-77
VzRIDDICLL: Goodoziya i k.rtacr-flya. 19-,0, *to. 0. pp.
TEXT: Froo U^y 10-14, 1960 the sheatoya 'U-.hduvsd"3tvonc,@ye
r-in.trii (3i.th
o,
h1hanI o
,
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:
0 . .1 1 In Moscow. It ... ... e-od by the
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tota Cood-li I goofittki Akadeiit nauk SSG?.
....;Vioni
Geodesy of the C,,..ittoa a a.od.ey and G..phy.icm or th. jW.Iiy of
ScIn to# USSR) and the Aer.4ravinetrichtakaym laboratorlyA lnoti%ut@
fiaikl Ze.li A.% 33SI (Laboratory for Aoro,;ravizatry or -r-,p
Ph *its of the Earth of the &S U3SR). 216 ropr*sertA,i'.. of "4
rg Part I.- thin cozf proJ,Ietio.
r ... @cb C.ntorv' and on trotloh
Int"It Lane .4 ri.nismtlann of the kk-d-tiya n-.V. SSnR
.

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'3 Mai). lkad.cli nauk Ukr.lh,kay, lr..Insk,j. LIIto,s1,.y i
&3.rbsydsh..Akr S3R (Ac.d.zleo of Sclobc-a of the
crulla.kAya. Litovtkwya, and Aterbayilhanckaya 23h),
vig.hogo i erednego srttsial4togo obrazovaulyn 3:':;*1 (@Iini5try of al-r4:@ "I
an4 Secondary Special Education at thn =Sa).
khrany nedr "3SR (2inistry of Cooloo and Frot4rvition of @'in4-4
M.Urc.4), I.Cit't Stan d.rtor, =4r I 1tj#r1twl'Nykh p@rjb.r- p.-4
ministraw SSZR (CoroIitto@ on 3-mftdards. !Zvmsuras, and Una.urini,
I stru met. of th council of Lzint...re '--R) "I V-1
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err* 0 iut-rhed In r-,;.ur or @uL@Iltt@t
for publication by 1.0.,; th- era by 1

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Card 316
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Chroniol.
(L@lnigr.j St't. L. A. P.1k, about Th vrr,@ref
sl., I Z4 ym M,;my or Z. tomi nI ne
Gr. I.
,'r' "s'i @@T _ . J@ Ib-t
of-Ane @hd Int,,r;'@l' 'f
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j7%@ELLJjLj@@@ otar
aLorin Crust In in* Antarctica A.-co r-`@
Ant:'rt4.-. ."t :to . L@@- (UjjAjj:,' AP.k.
about the @lrepLratL m and Use a mvil,tric ixport*;, Thv, racim-nd.tion.
91 an by the Ccnf.r.ne. are m.tioned..Pro- Apr 1 1 1 5 22 90
Scl4ntifla and TochnItal Conference of the 7jorkers of the
ti.L.-i the tht ll-oy. T
_qA - - pr-l.lipl. ;li@-
Iakhritmy n.4r pri Sovqtt 111nietrov Ukratnokay- -SR Wlxiln Admiristration
Ir Gooloo and 1'rome"a-ion at 91noral Basourttv of the @Guncil
Ul.imt:r,. trKr%tn.k.%yft SSl') vito held In Artozovsk. Therv, the *tk ofllh.
t.p.;r o-g-l-t1a and ark ,r t,., organization. at h.
GI ."ooltg1ja USIR (Wavj;**loj:ly* Ukr=) and the introduction of
Card 416
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d 1 the ft-t s jr-ho-ire, the
_,.:vqr. yoars. F
o-inj drk-tacks -* pointed I.- _ -thads 4r. too
and the 9*olQicd, orgm-.1-4% ions are Inau!ficlontly
equipped ith n.. s;V.rttu.g In gool.gie.1 the ..r..
photographs and tooirapMe pl@nn-avuilmltje on a lar@@ #*@I& - not
sufficlomilly v-d. -.filv state Is -;1albel by tnorriclett tw@;mlcll
dlrt..tjtqn;JIaeftipi..% -.0chni-I and t@terl.l a.p;ly, by . I.-.k or
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in r.
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this situ,tion. F@r Im,-xi,log or the -rk,r@ th-
Corif:r.no. s.ggv..*d t. c.n@- scientific and onf-n
atrp ar Intervals. For,tnprovlng irformation an, f*r the oi%!@A711 f
ta
P-1.
Imard of -ho ;ro-nt ;erle,lical .%I ackrd
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Card 5/6
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41

@98 W, Rem VVS 4,KWF= w 349 um rffi @ @. @--.

(Graltimetry

L 35897-66 EWT (I
ACC NRt AT6006260 SOURCE CODE: UR/0000/65/000/000/0026/0071
AUTHOR: Romanyuk, V.-A.
ORG: None
TITLE4- The de e of the cooscillation oI the sLand of a_pgndUju"k
t rmination
soucr.: AN ssSR.- Institut fiziki Zeml Apparatura i metody morskikh gravi-
metricheskikh nablyudeniy (Apparatus and methods of marine gravimetric observations).@
Moscow, Izd-vo Nauka 1965, 26-71
IOPIC TAGS: gravimeter, pendulum mechanics, mechanical vibration, vibration
analysis,:gravitation effect, friction
ly
ABSTRACT: For the relative'determination of ravitational'forc in modern pendulum
cievices the co-oscillation of the stand is usually determined using the resonance
method. Of the two pendulums used, the amplitude of one is assumed absolute zero,
a reqULrement which may not always be easy to satisfy. The present article develop$
a more accurate solution of the cooscillation problem which takes into account the'
friction-forces-acting on the two pendulums used in the resonance approach. The,
general relationships*are derived and the arbitrary constants of integration are
h
determined. The determination of the oscillation.of the stand from the relations ips
of amplitudes of the two pendulums is described and the simplest case of co-
o5c illation determination is discussed. A-detailed discussion is given of some
otI.-.er special cases. This comprehensive paper concludes with.a description-Of the',.

@4
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9mv
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Aeano-@:a,s;
ar
t-ions,.-, exp
kx@ll- tion, A
fjiiK16, di

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