SCIENTIFIC ABSTRACT GAVRILOVA, A.YE. - GAVRILOVA, L.A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000514510009-6
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: July 19, 2001
• Sequence Number: 9
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

A process of thermal dealkylation... s/o65/62/000/004/001/004
E075/E136
pressure in benzene column 0.1-0.3 kg/cm2; temperature in
benzene column, top 87 OC, bottom 130 OC; pressure in the
recycle stock separation column 0.1-0.3 kg/cm2; temperature in
the recycle stock separation column, top 2600, bottom 304 'C;
molar ratio hydrogen/feedstock 4:1; space velocity of feed
4.0 h-1; consumption of hydrogen 2.10,~~ wt of feedstock; yield
of benzene 78.7ca wt of toluene. It was calculated that high
grade benzene produced by the.process from petroleum derived
toluene is considerably cheaper than that obtained currently in
the coking industry. It was established that thermal
dei.,iethylation of methyl naphthalenes (700 OC, 50 atm) gives
naphthalene with a yield of ca.50513' wt of fcedstocle after one
cycle. The most suitable raw materials for the process are
aromatic products obtained during reforming, pyrolysis and
catalytic cracking processes. It is expected that the dealkyla-
tion process will constitute an important source of benzene and
naphthalene for the Soviet petro-chemical industry.
There are 1 figure and i table.
Card 2/2

STERIN, Kh.Ye.; AIEKSAIIYAN, V.T.~ UKHOLIPT, S.A.; BRAGIN, O.V.:
__"YRIWVA.,_A_Y*..;_ZOTOVA, S.V.; LIBEF44AN, A.L.; MIKRAYIDVA, Ye9A.
SMIRNOVA,, E.N.; STERLIGOV., O.D.; KAZANSKIY, B.A.
Raman ~pactra of some tri- and-tetraalkylbenzones and condensed
aromatic hydrocarbons. Izv. AN SSSR. Otd.khim.nauk no.8-.1444-
1450 Ag 161. (MIRA 14.8)
1. Yxmissiya po spektroskopii AN SSSR i Inatitut organicheskoy
kh4mll im. N.D. Zelinskogo PIT SSSR.
(Benzene--Spectra)
(Hydrocarbong-,Spectra)

GONIKUMP M.G.; GAVRILOVA, A,Ye.; STERLIGOV, O.D.; HOUKOVA, M.I.
Thermal polymerization of pentenes at bIgh preBsureB. Izv.AN =R.
Otd.khim.nauk no.8:2,458-2463 Ag 162. (MIRA 15:8)
1. Institut arganicheskoy khimii im. N.D.Zelinskogo All &WR.
(Pentens) (Polymerization)

GONIKBRRG, M.G.; DCROGOCHINSKIY, A.Z.; MITROFANOV, M.G.; GAVRILOVA, A.Ye.;
DRONIN) A.F.; KUMIYANOV, V.A.; HAKARIYEV,
VOVK, L.M.
Thermal dealkylation of aromatic hydrocarbons. Khim.i tekh.topl.
i masel 7 no.4:11-15 Ap 162. (MIRA 15:4)
(Hydrocarbons) (Alkyl groups)

GONIKBERB., M.G.; DOROGOCHINSKIY, A.Z.; MITROFANOV, M.G.; GAVIPgA. A.Ye.;
KUPRIYANOVO V.A.; HD(HAYIWSKIY, V.K.; VOVKp L.M.
Homogenous demethylation of toluene. Report No.!. Basic indices
of the process at 750-790 C. Neftekhiziia 1 no-1:46-53 Ja-F
161. .,x (KERA 15:2)
1. Inatitut organichookoy khisli AN SSSR imeni N.D.Zelinskogo
i Groxnenskiy neftyanoy nauchno-inaledovatellskiy institute
(Toluene) (Methyl group)

GOITIKBERG, IM.G.; DOROGOOHINSKIY.0 A.Z.; 9#,YK~qVA,_.A.Ye.; KOMANENKOVA, R.A.;
MITROFANOV, M.G.; KUPRIYOOV, V.A.
Determination of the naphthalene and alkyl naphthalene content of
stocks and dealkylation products. Neftekhimiia 3 no.6-916-921 11-D
163. (1,11IRA 170)
1. Institut organicheskoy khimii AN SSSR im. N.D.Zelinskogo i
Groznenskiy neftyanoy nauchno-issledovatellskiy inatitut.

GONIKBERG, M.G.; GAVRlLOVA, A. Ye.; ALEKSEYEV, Ye.F.; KOMANLVKOVA, R.A.
Homogenous demethylation of methyl naphthenes. Neftekhimiia
4 no.2.- 252-256 Ri-Apt64 (MIRA 17:8)
19 Institut organicheskoy khimii AN SSSR iteni Zolinskogo

SOBOIEVA, R,G.j GAVRILOVA, B.K.
Study of synantrophic Mes on one of the animal farms of the
soutbern Maritime Territory and their control. Soob. DVFAN SSSR
no.18%107-112 163. (MIPA 17:11)
1. Dallnevostochnyy filial imerd Komarova Sibirskogo otdoleniya AN

TILICHMO, M.N.; SOBOIZVA, R.G.; DOMANYUK, T.M.1 GAVRILOVA, B,K,
kftw insecticides; nitrogen bases from polymethylenepolycyclohexanons
its inseaticides against flieo and horseflies. Sobb. DVFAN SSSR no.18s
113
-117 163. (MIRA 17111)
1. Dallrievustoohnyy filial issni Komarova Sibirskogo otdoleniya IN
SSSR,

60COIrTmal of Man
Gevrilova
23 (S), 143-140
am soln. 1 (10 to 12 ml) containing Uo, and 8 ral
!wnythydrazina sohl. (coocn.- not stated)
acidified-with- W are heated- for 15 mill. on a
' The = sWu
is diluted to 50 ral in a
"04 batb
.
.
tallbritted Auk and 10 all is extmcted with &m1
amoullts of ijoamyl ikohol until the last atrict Is
colourless. ~'Tha caimblued extracts an diluted -Rith
isatutyl skohol to 25 ml in a calibrated flask and
-electric
the , extinction is measured on a photo
(
cc eT with s.green filter. Thoccintento
Mo
-
6om me4ibration curve. Themethodcl

b the Ban. from a sample of steel is not
taining
0
described. Tungsten does not Interfere.
G. S. Small

L 18298-63 EWP(q)/EWT(m)/BDS . AFFTC/ASD/ESD--3 _~WMIM
i.&QCESSION NRA AP.3005OW
I AIVEORS I GQrnY*y, 0. -YA.1 asyrilava, Z. P.-
TITLEs Deteridning total rare earths in.the presence of larger amounts of other
I elements
SOVRCEs- rKrainakiy khimicheskiy zhurnal, v. 29, no. 8, 1963, 859-863
TOPIC TAGSt oxalatef oxalate precipitationp rare earth elements
ABSrRACTt A new modification of the oxalate precipitation method was developed
for the quantitative removal of rare earths from large amounts of.other elementat
with very littl ntamination by the latter, The solubilizing effect of the
oxalate f the admixed elements is removed by neutralizing the complexes
with CaCO A mechanism for the neutralization is proposed.. Orig. art. hast
21tables.3
ASSOCIATIONs Institut geologichookikh rsauk AN USSR ~Jnstitute of geological
sciences, Academy of sciences Ukrm),
Card 1/

n-
Ga-, a Drr
uchnoW.rc:_EAViM,OII.A F., inzh.-kHnik: A.i. inzh.-
'chim1k; LOGVTNA, USMM-EVA, L.A.1
khivilk; GUDJIEvIKO, L.F.1 inzh.; NAZAREVICH, Ye.S., I*t:,,,,I,.;
SI.-IKVARUK, R.N." (lr,.yovh, L.A., inzh.; B *A,;HM KOV'A'~~.G.
irmb.-geolo.g; POR-c"M, Ye.s.v Otv. MELINIK, A.F., r~d.
(Goosher,"stzy aii!*i Analytic cbernistry of rare-earth elements,
Ft.l. Accessor7r rar-e-e~a-th miner-alt; and el(ircnfx of c--rium
i-oup in the 'Ukrain.Tazi Cryi3tallinL. ~'hie-'.6' - nra-
sub~ k j
.Ut.-I rheckaia element,'v. Kiwv, tbaukova
ch: mke_ P L. I. ir,:,,Ci~;~7,~:me I I n3n, r., I i---! r!~, TY
-u
1 -10 j rod F. -.-py 11 lkrn i zis o:pr, k r 1 s f. t I I i c he .~ kooo v` 7',a.

DOBRYANSXIY, A.P.i,_aAVRMYA, Z.K.
Thersocatalytic conversions of hydrocarbons. Phxt 2. Conversions of
tertiary-butyl benzene. Zhur.ob.khis. 23 no-7:1118-1119 J1 153-
(MLRA 6'-7)
1. Kafedra takhnichookoy khisil lieningrMakogo Gosudarstvonnogo universi-
tot&. (Ikxtyl benz*ne) (Catalysis)

Nam: GAVRILOVA, R. S.
D19sertatIon: Map of the city of Lvov and its development
Degree: CaDd Tech Sci
O,5f-CIYA%C,D A7
Aff0tabien: Mm Higher Education Ukrainian SSR, Lvov Polytechnical
List
I Place: 1956, Lvov
Source: Knizbnaya latopis', No 4, 1957

3(2) SOV/6-59-7-17/25
AUTHOR:
TITLE: Soue Remarks on the Signs Agreed Upon for Topographic Plans
on the Scales of 10000, 1:2000,1:1000,1:500(liLsigkollko "zamechaniy
k usloVnym zrLakam dlya topograficheskikh planov masshtabov
1:5000, 1:2000, 1:1000 1 1:500)
PLRIODICAL: Geodeziya i kartografiya, 1959, Nr 7, PP 55 -57 (USSR)
ABSTRACTs The signs for topographic plans on the scales of 1:5000,
1:2000, 1:1000 and 1:500 have a number of essential short-
comings. Their use in the compilation of town plans is very
difficult in practice. In order to eliminate these shortcomings,
the table issued for these signs must be integrated by new
signs, and some of the signs available must be coordinated to
each other. All remarkB and integrations of the available signs
are shown in a table in figure 1. They are described here in
short. There is 1 figure.
Card 1/1

L.1145,-i~ --(,#)----E.WP(c-)/EWP~j)/EWP(k)/EWT(d-)/EaT(M)/-T-/EWP(1)/EWP(-v)----RM-
ACCESSION NR: AP5021996 UR/0286/65/000/014/0074/0074
678.058.3
678.065 .7,
AUTHOR: Gurlyanov, B. I.; Loshakevich, B. P.; Pinovski Gavr i
_, M - L *4 e-l-,
Yurlyev, S. I.- Pankov, A. A.; Mikushin N. S * Proselkova Ye P
I - =~~l L_~~
%k'k 0A -- (-'7,
TITLE: A semiautomatic transfer machine for refilling the molds in autoclave
tire v~tlcanization. Class 39, No. 172976
- 15 144
!SOURCE; 'Byulleten' izobrc--.eniy i tovarnykh znakov, no. 14, 1965, 74
ITOPIC TAGS: industrial automation ~vulcanization, rubber working machinery-
ABSTRACT: This Author's Certificate introduces a semiautomatic transfer machine
for refilling the molds in autoclave tire vulcanization. The machine is a closed
circular device with a centrally located automatic operator and devices for angu-
lar orientation of the molds as well as for opening and steam cleaning them. The
machine is designed for complete mechanization of the process of extracting the
tire from the mold after opening, regardless of whether the finished tire is in
the upper or lower half of the mold. The automatic extraction device is made in
the form of a bracket which rotates 6n a vertical axle. This bracket carries a
Card 1/3

L 145-66
ACCESSION NR: AP5021996
pair of horizontal discs which move in the vertical direction. These discs are
equipped with symmetrically telescoping clamps for grasping the tires from the
inside in the upper or lower position.
ASSOCIATION: none
ISUBMITTED: 160et6l ENCL: 01 SUB CODEt IE
NO REF SM 000 OFTHER: 000
~M213

L 1145-66 .-
ACCESS-ION NR:. APS021996
Card t

KOLOBIKIIIN, GAVRILOVA, F.K
Oxidative dehydrogenation of n-butenes to 1,3-butadiene on
bismuth-tungsten catalysts. Neftekhimiia 5 no.6:820-824 N-D 165.
(14IRA 19;2)
1. Nauc-Mo-issledovatellskly institut monomerov dlyp. sin'.eticheskogo
kauchuka. Submitted Jan. 1, 1965.

MCHNIKOV, Sergey VasilOyevich; GAVRILOVA, G., rod.; SWETA, S.,
tekhn.red. -
[Amdamutals of applied electronics] Oonovy tekhnichaskol
elektroniki. t1ov, Gos.isd-vo takhn.lit-ry USSR. Ft.l.
(Power engineering electronics] Vnergetichaskala elektroniks.
1959. 454 p. (MIRA 13-2)
(Power engineering) (Electronics)

BONMRIP Mikhnil Favlovich; GAVRILoVA, 0., redo; SWETA, s., tekhn.red,
(New trends in the design of mechanisms] Novoe v konstruiroTanil
makhanizmav. XLev, Goa.lzd-vo takhn.lit-ry USSR, 1960. 19.1 p.
(MIRA 13:9)
(Mechanical movements)

ACCESSION NRI~ AP3006534 S/0191/63/000/009/0017/0019
AUTHORI Itedvade:'va, P, A. Igy*bkina, 0*. Ya,,*, Duntovs, L. Kot
Gavr,~lovag Go A.1 davurLnajilkeK
TITLEt Selfo-extinguishin glass-ra'inforead elastics "ibased on
iyester re a 7
epoxy7po
SOURCE: Plasticheskiy massy*, no, 9, 1963. 17-19
TOPIC TAOS$ glass fabric reinforced plastic, binder unsaturated
polyester, unsaturated polyester resin, TKhP, ChF, AF, styrenated
polyester, epoxy resin, ED-5, ED-6, self-extinguishing$ chlorine--
containing polyestert chlorine-containing curing agent, reinforce-
mento. Patin weave glass fabric, glass fabric, ASTTM92-5-13-l',
ASTT(b)S2,-8/3, organ.osilicon finish, GVS-9 finish, coupling agent,
glass fabric lay-up, antimony oxide, mechanical strength, bending
strength, thermal stabilLty, moisture offeetv temperature effect$
moisture, temperature
Card 1/3

L 16199-63
ACCESSION M AP3006534
ABSTRAM Self-extinguishing-glass-fabric-reinforced plastics
have been prepared with mixtures of epoxy and unsaturated polyester
resins as binders. Self-extinguishing proper ties were imparted by
r
introducing chlorine.into the polyester (method unspecified) o by
usingla chEorine-zontaining curing agent (unspecified). Styrenated
MF,,~ChF,voi ED-6 epoxy resins, mixed in
r AKolyes tars and
varioui-ra ios_~`generally 2 parts polyester to 1 paqED-5), were
S 8/3
used as binders; satin-weave 1abrics ASTLW-S.2_5j.30~;ASTT(b)
or ASTT(b)S2-8/3 finished with the GVS-9:~organisilicon coupling
agent served as reLnforcementse The glass-fabric sheets were laid
up at right angles to each other to impart multidirectional streniph 4
to the plastic* 3.5-4.5% Sb20 was added to the binder. The re-.
sults of a study of the properties of the plastics,, given in the
form of tables, show that glass-fabric-reinforced plastics thus
prepared are self-extLnguLshing, They exhibit high mechanical
strength (bindLnC strength vB n 3800-4400 kg/cm2) and high thermal
stability. The strength of these plastics (especially of those
reinforced with A.STT(b)S2-8/3 GVS-9) drop only slightly under
the effect of moisture 3280-4200 kg m2)
(0B /C and temperatures
cjp to 6oc (0B - 3200 hOOO kg/cm2). Orig. art. has: 5tables.

ACC NRs
AR6035213 SOURCE CODE: UR/0274/66/000/008/A045/A045
AUTHOR: Gavrilova, G. 1.
TITLE: Distortions of the directivity pattern of receiving antennas along the
ionospheric scattering caused by the spatial incoherence of the field
SOURCE: Ref. zh. Hadlotekhnika i elektrosvyaz1, Abs. 8A333
REF SOURCE: Tr. uchebn. In-tov svyazi. Al-vo avyazi SSSR, vyp. 27, 1965,
17-25
TOPIC TAGS: radio antennas, receiving antennas, antenna directivity pattern,
directing pattern, ionospheric scattering
ABSTRACT: Equations*are derived for determining directivity patterns of
receiving antennas as a function of the degree of spatial incoherence of the field.
The presence of random fluctuations in the amplitude and of the field phase causes
expansion of the directivity pattern in comparison with that computed for a plane
wave. Various special cases are analyzed. Original -article has 4 figures and a
bibliography of 5 titles. [Translation -of abstract] [INT]
SUB CODE: 171
UMC: 621. 396. 671:621. 396. 228
Card 1

BAGRINGVSKAYA, G. P. and GAVRIL(YVA, G. L. (1-1-osccv)
"Programmins of a Trrknslation front Englinh to Ilucalan."
Theses. Conference on Machlne Translation, 15-21 May 19,1,8, AW-0 S Cc) W,

GAVRILOVAI i:.; DAVIDSON, S. B.; BUDUNOVA, A. A. SHIU-SHIIII, F.
The Organization of the Treatment of Children with Chronic Dysentery,"
Avtoreferdty Dokladov 19-y flauchnoy Sessii Saratovskogo Gosudarstvennogo Meditsin-
skogo Insti.tuta, Saratov, 1952, pp 237, 238.

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of 0 0 0 0 411 1 - 0 - v 9 -W -W
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.
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1.8
kswc degree than imthtax~.Ie With 84 ifecoraw J
Cetop

00 L.A.KlimovA. J. Appliol C".(U.S.S.R.) ILMM- .
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rtt&nt
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o
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60 14. atitot-lave at a const. Its pgrapin tlWflk) aim.) in the fittAllf, PCO)AFtYphl-H&OCIttene. (41.1 %flue Iwillydroan.
'

00 presence of the Nlmliv catalyst ptvpd. from MA by trmt-

* rhe YkId (it SicAidroplicnauthtittit was
thtacvnci.
Thitty~scvca
hi
her than that ot Site hydruafithraktrie
for 12
ownt with It, un.kc a pfv%surt o1 VV situ. at 430 . .
g
A
Gele a bm. Anthracene (11 it x.) was hydrmnated at 2M-3W', ~
frfervoc". It. Hydriders celantlieracerse and the MW
- - - '%)' anxt 4*-N fur 65 tuin. in the
mo -4o , a. o 24) , 4 10 ;. eletim of their famation. K. 1. Pruk"v(s. . 11,4~ L.~~ - 9

4 10 X. ,( the Nfwln cAmlyst, yielding 9,10-tMy- (in French .1 authi4ccut At 3M.
M=. (ruainly at 30D*); I 2.3.4-tcUaleydroare- 0 'he ",nditious being as jbio%v. yilded synt. o%:(Ah)dr%4n-
.
,

thractne. jym-ociahydroantlitactior (in. 73*) and pe It -vnc, b~~ 4~
Iltraccue and temyne. vctahydruArethra, M a
. j,
vctah
dro,anthracene inctravil witj
ield of uni
in
The
droanthracceir, depereding on the expel. conditions. .
y
y
y
a ~;j formation of V1,10-dihydroanthraccive proceeded with lowering o( the temp. The di. and toltraleydroanthracreet

3
great ravc at -101', but further hydrogenatim of the latter abo yielded untyin. octahydircianthraccur. Ill. The

composition of fitlWel produd fortfied toliertker with wis-
09 cuFnpd. required , hitticr temp. On the other haod~ the
d hydroanthirettene and isomerrization of-octaleydrawithra-
w hydrostuation of Item deriv. to tlw octithydride proceede
it was
with such caqc that in order to obtain the tettst deriv I citare. F. 1. Prokopeti. A.. V. Pavictilto and S. M. Bogu-
0 .
nccvs~ary to cut 4rmu the reaction time and the amt. of %Iavskaya. fba. 8W Stin French 846).-~-Xhc IjquW
catalyst. Th~ hydrogenation of octshydrowthraccric, in 9 Rroduct obtained from anthrAccut under the %anic, condi-
turn. Prm-"Ard "ry slowly and an iticit of temp. in- tiorts as before, contained syne. and onsym. octahyd~-
-cd the yicltlt,filiqui(i~whstanteb.290-3W'. The
ctt& theracent. petleydroanthractne.

"
product of mupk-te hydrurnatim of rentleractne: was per- and syrn. octaleydroplicnancluvac. TmAtruent of
cittic

hyAltuanthraLtat atut the alx)vv, liquid seebitance. Smi-
' sym. octiehydroanthrAccue in the preserkv and aliveice of
- h
h
d

n temp. in-
larily to anthraevne, incrm-w of .11i reactio ro-
e
cat4lyst di-witised that the catal st promotts t
y
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intleepteviousexpts. Twelvettfrtetwei. ly.
cat tireadocenalions of octAhYdroandaweaes, F. 1.
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(Wfl)Aq 'jl11z3j-4lbq 10 swol~puazi IMMA-16W qju.3i..j

SOWUH, M.N.; GAVIUIA)VA, 0-Te.; )MZHUTIVA, Te.A.; KOGAN, N.G.
Causes of'dark-colorad ammonium sulfate In by-product coke plants.
Koko I Wm. no-1:35-56 156. (NLRA 9:5)
1. Bagloyokly koksokhImicheekly sawod.
(Ammonium sulfate)

GAVRILOVA, G.Ye.
Methods for testing aromatic hydrocarbons. Standartizatsiia 27
no.909 S 163. (MM 16s10)

GAVRILOVAY I.A.
Effect o4,beryllium on calcium radiation in the air-acetylene
flame."Ihur. anal. khim. 18 no.11:1394-1396 N 163s
(MIRA 17;1)
.,V, . 1.7

ZHURAVIEV, G,I.; GAVR11A)VA, I.A.
Det-ermination of nodlum, potassium,, and calcium in uranium and
its compotxnds by flame photometry. Zhur. anal. khim. 19 no. 1:
54-58 164. (MIRA 17.,r,)

GLAZOVSKAYA, Mariya AllfredovnBp prof.; MAKUNBA, Aleksandra Aleksandrovna,
kand. geogr. nauk; PAVIMIKO, Irina Alekseyevna., kand. geogr. nauk;
BOZHKO2 Margarita Georgiyevna., starshiy laborant; 9ARILOVA.-Irina-
Favlovna,, nauch*y sotr.., laborant; GRUNVALID, V.P., retsenzent;
ZkSUKHIL, G.N., retsenzent; PERELOW, A.I., red.; FADEYEVA, I.I.,
red.; YERMAKOV, M.S., tekhn. red.
[Geochemistry of land forms and prospecting for minerals in the.
Southern Urals) Geokhimiia landshaftov i poiski polezzWkh -isko-'
paelaykh na. Bilmom Urale. Pod red.A.I.Perellinana. HoAvallid
vo Mosk.univ., 1961. 180 p. (M]RA .15t2)
1. Nachallnik Yuzhno-Urallskoy landshaftno-geokhimicheskoy ekspe-
ditsii geograficheskogo faku-11teta Moskovskogo gosudarstvemogo
universiteta (for Glazovskaya). 2. Yuzhno-Urallskoye geologiche-
skoye upravleniye Ministerstva geologii i okhrarkv nedr SSSR (for
Grunvalvd, Zasukh1n). (Ural I'otmtains-Geoehemichal prospecting)

PAVLENKO, I. A.;_GA)TILOVA IP,
Heavy metal content in friable sediments of the upper Tanalyk
Valley (Southern Urals)& VoPo gGoR* no.59:82-104 162,
(MIRA 16;1)
(Tanalyk Valley-Ore deposits)
(Tanalyk Valley-Geochemical prospecting)

MIGUNOVA, N.A.; GAVR11-OVA, I.P.
Inve!itigating the caunes of the InstabIlity (if the elenLrcdepoWed
gold-copper alloy from a neutral cyanic electrolyte. Zashch. met. I
no.5s521-524 S-0 165. (MIRA 18s9)
.. ~ 1. Inutilut chapovcy promysiZieruicsti.

GAVRILOTIA, I.P.
Some characteristics of trace element distribution in
undeveloped Chernozemlike soils of the Southern Urals.
Vest. Mosk. un. Ser. 5: Geog. 20 no.5:61-67 S-0 165.
(MIRA 18:12)
1. Kafedra geografii pochv i geokhimi-i landshaftov
Moskovs1fogo gosudarstvennogo universiteta. Submitted
February 1, 1964.

(6H Y-RMOV a
ot lacasuring inisaf2cial itueita in a cryztzl an a
1. V. C.AVl!U%%A ;%I111 F- 1". I-ItUt.
Truty hist. Krist., A A ad, ffiiuk -w
Lugv luchutt spar crymah (9 X ILI X
of )I,,I Ow facvs weleef-r-
it. Thil wo UtIC111111ol willl Oautbdilic lot-ws-
1-coly poli-Att.
III "I WO 0%. llwv(~vcr, x-ray it-sis .,f the
v vt)'A AI 111diemed (hat dt"L ilt ..oll.
vrror. Adc(lit,ar piv,-Nov it. latcr
'%itli. -circle

85872
3/0413/60/024/01 110081036
B006/BO56
AUTHORS: Yurin, V. A., Baberkin, A. S., Korniyenkc, E. N,
Gavril7v-a, I. V.
TITLE: The Action of x-R diationl\upon the Ferroelectric Properties
of ~-rj als
PERIODICAL: Izvestiya Akademii naul.SSSR. Seriya fizicheskaya, 1960,
Vol. 24, No. 11, pj. 1334 - 1336
TEXT: The present paper is a reproduction of a lecture delivered on the
3rd Conference on Ferroelectricit , which took place in Moscow from
January 25 to 30, 1960. The authors investigated the influences exerted
by y-radiation upon the properties of triglycine sulfate (TGS), taking
special account of the stabilization of the single-domain state. TGS
Y-cuts of different shape and size were investigated upon which silver
electrodes had been sputtered in vacuo. From the Co66 source the sample
received a dose rate of 235 r/sec. From an observation of the hysteresis
loops and their changes due to y-radiation above and below Curie point,
with and without external (variable or constant) electric field, the
Card 1A

85872
The Action of I-Radiation Upon the Ferro- S/048/60/024/01'/008/036
electric Properties of Triglycine Sulfate B006/BO56
Crystals
following conclusions could be drawn: 1) Under the influence of gamma
irradiation either stable polydomain states are formed in TGS crystals
(to which the double hysteresis corresponds), or single stable domain
states (to which the displaced hysteresis corresponds); this means that
that form of domain structure is "solidified", which existed during
irradiation and during holding time after irradiation at a temperature
below Curie point. 2) The stability of domain structures is explained
by the formation of "internal displacement fields" in the crystal, where
in polydomain samples the signs of "he "internal displacements" in
neighboring antiparallel domains are reversed, and in single-domain
samples these signs are then uniform in the whole sample. These displace-
ments are not formed immediately during irradiation, but in the course
of relaxation processes, above all during diffusion processes, due to
which the radiolysis products in the lattice are deposited at the places
of minimum energy. These places are interrelated with the existence of
a spontaneous polarization in the crystal (as well as with their direc-
tion). This conception corresponds in ferromagnetic materials to an
oriented ordering, which causes a uniaxial magnetic anisotropy, whose
Card 2/4

85872
Thd ActiQn of y-Radiation Upon the Ferro7 ~S/048/60/024/011/008/036
electric Properties of Triglycine Sulf ate Boo6/BO56
Crystals
ocqurrence is explained as a perminvar effect or magnetic aftereffect.
3)'The results obtained by the authors and their explanations agree with
the results obtained by the irradiation of TGS with X-ray- or ultra-
vi6let irradiation. The authors thank I. S. Zheludev, M. A. Proskurnin,
and 1. S. Rez.for their interest in.th~s paper. T e are I figur"li-and
7 3~eferences: 5 Soviet, I US, and 1 French.
ASJOCIATION,- Institut kristallografii Akademii nauk SSSR fInstitute of
CrystallograDhy of the Academy of Science's
�R
Caid 3/4.

EJ
J
85872
5/048/60/024/011/-006/036
B006A056
Legend to the Figure:
Hysteresis loop of TGS: a before.
irradiation; b - after an irradiation
6
-10 r; c - after irradiation
with 2
6
with 2.10 r, the irradiation taking
place while a field +E
> Esa*t was.
applied. E was maximally 2 kv/CR
at 50 cps; t 200C.
Figure
Card 4/4

50534
3/504J01/303/000/003/029
D228/D304
AUTHORS: Koldobakaya, M. F., and Gayrilova. L, V.
TITLEs Growth of large finite crystals of triglycin sulfate in
laboratory conditions
SOURCE: Akademiya nauk SSSR. Institut kristallografii. Rost
kristallov, V. 3, 19619 278-282
TEXT: The authors studied the growtb of triglycin sulfate crystals--
(Nil4CH 2COOH)3 If2so 4- from aqueous solutions in the temperature Interval
20 - 550 by the method of reversible mixing. Frevious work by E. A. Wood
et al shows that these crystals which structurally belong to the dihedral
axial class of monoclinic syngony possess strong segneto-electrical pro-
pertiess a high dielectric non-linearity, a highly rectangular hysteresis
loopy high piezoelectric modulig and a low dielectric permeability.
Other characteristics include the disappearance of spontaneous polariza-
0
tion above 470, the predominance of m' J101 and c 01) faces below 55 9 a
Card 1/3

Growth of large-.
30534
S/564 61/003/'000//003/029
D2 D304
Yn
perfect 010 cleavage, a segneto-electrical axis coincident with the polar
ax-i s L2s an axial bisector coincident with the %--axis, and a curie-point
of 47 - 40.30. In the experimental procedure followed by the authorsi
~ crystallizer-a sealed glass cylinder containing the crystal-carrier,
~ glass tube with a pivotal primer, with a saturated and purified solu.-
tion of triglycin sulfate--is placed in a sealed glass water-bath with
a thermos tat-overheated by 5P in comparison with the solution-mot-or,
heater, mixer and refrigerator. The optimum temperature for erystal-
growth is established visuallyt and stirring is commenced as soon as this
occurs, the growth rates &long the x-9 y- and z-axes being 5A, 7.3 and
1.9 mm/24 hours respectively. It is noted that large homogeneous crystals
cannot be grown in all cases owing to their high sensitivity to changes in
the degree of supersaturation and mixing of the solution which increase
the crystal complexity and the number of liquid inclusions dnd parasitic
growths. Wring unilateral rotation, a zone of weak mixing develops at
each acute angle, leading to the fonnation of inclusions on the crystal
faces; this does not happen, howeverg with reversible rotation. On adding
Card 2/3

Growth of large...
30534
S/564/61/00,3/000/003/029
D228/D304
H2so 41 the dimensions of the growing crystal become smallerl my further
increase in the acidity results in the meas-formation of parasitic crya-
tals, while a reduction in the pH alters the crystal's external appear-
ances the isometric form is replaced by an elongated shape. In conclusion
the authors assert that crystals weighing 1 kg can be grown by this mo-
thod. Acknowledgement is also made to Z. 1. Yoroblyeva and 1. S. Ruda
for their help in the experimental work. There are 5 figures and 5 re-
ferenc--as 1 Soviet-bloc and 4 non-Soviet-bloc. The references to the
English-language publications read as followss B. T. Matthias, G. E.
Miller, I. P. Remeika, Phys. Rev., 104, 1, 849, 1956; E. A. Wood, A. N~
Holden, Acta crystallogr., 10, 1459 1957; Bell Lab. Rec., 35, 7. 27lj
1957; 1. M. Dion, Acta crystallogr. 12, 259, 1959.
Card 3/3

30535
552D S/504JOI/003/000/004/029
53400 D228/D304
AUTHOPS: Kuznetsoval L. 1.9 and *Gavrilovag-I. V..-
TITLEs Laboratory method of growing pentnerythrite crystals
SOURCM Akp-demiya nauk SSSR. Institut kristallografii. Rost
kristallov, v. 3, 1961, 283-285
TEXT: rrevious attempts to prepare pentaerythrite crystals--used as
monochromators in X-ray analysis-have not met with much success, so the
authors studied the best method of growing these crystals from aqueous
solutions with a slowly decreasing temperature. ]Pentaerythrite,
C(CH2Off)v belongs to the tetragonal system and has the following charac-
teristiess an S2 space-groupf lattice parameters a = 6.10 � 0.02
4
e - 8.73 � 0.02 1; a density 1.417 /cm 3 a configuration of two
tetragonal tetrahedra with additional (001) and 00) faces; and (001);~ 410) and
~00)cleavages. The crystals were grown in the temperature range 80 - 92
Card 1/2

30535
3/564j6l/OO3/000/004/029
Laboratory method of... D228/D304
the crystallizer was a hermetically sealed Erlenmeyer flask, placed in a
thermostat with a contact thermometer, relay, mechanical mixer and refri-
gerator. Under static conditions, the primer was attached to the bottom
of the flask; for the dynamic set-up, either the some procedure was fol-
lowed or else the primer was fixed to the cover at the elongated end of
a rotating glass crystal-carrier. The static method is recommended in
view of the poor stability of pentaerythrite between 80 0 and 920 which im-
pedes the formation of large crystals. Pentaerythrite crystals are very
sensitive to temperature and supersaturation changess any inopportune
reduction of the temperature or increase of the supersatu ration, however
11 light, causes structural damage and the appearance of extra 001 faces.
Nevertheless, it is possible in a period of 10 days to grow crystals
t.
weighing 50 gy and the authors conclude that even larger crystals may be
obtained by using a crys tall izing-f 1 ask with a capacity in excess of
300 ml. There are 4 figures.
Card 2/2

30536
S/564J61/003/000/005/029
I;- 55W D228/D304
AUTHORs Gavrilovaq 1. V.
TITLE: Certain growth peculiarities of crystals of sorbite
hexa-acetate
SOURCEt Akademiya nauk SSSR. Institut kristallografii. Rost
kristallov, v. 39 1961, 286-289
TEXT: The author discusses the preparation and certain properties of
crystals of sorbite hexa~acetate-C 6a80 6(COCH 3),-on the basis of work
performed by L. 1. Gverdtsitele and herself. Sorbite hexa-acetate belongs
to the dihedral axial class of the monoclinic system and develops a con-
figu f the ~100! ~0013, (011), ~711) and ~1_01j' forms with t1001
dc6ation consisting o
an 010 cleavages; according to 1. S. Rez et al (Ref. 1t Sb. Rost krisial-
loT, Y, 19 Izd. AN SSSR# 1957), the unit-cell parameters for a, b and c
are 10.15 , 8,43 and 12.7 2 1 respectively f-Abstracterls notet 1110.1 5 " and
118A 311 appear erroneously in the text as 1110.1 5" and 118.4," _7, while
Card 1/3

30536
Certain growth...
S/564/61/00-3/000/005/029
D228/D304
P = 960 . The crystals were grown bys (a) pouring a purified ethyl
alcohol solution into a glass crystallizer glaced in a thermostat; (b)
initially maintaining the temperature at 68 for 20 - 30 min., followed
by its slow decrease to the crystallization point; (c) stirring the solu-
tion with a mixer (80 - 100 rev/min.) when the primer at the base of the
crystallizer acquired a glassy surface rafter one day); (d) very gradu-
ally decreasing the temperature--by 0.1 every 24 hours; (e) carefully
decanting the residual solution in a heated drying chamber; and (f) finally
cooling the crystallizer in a thermostat to room temperature at a rate of
0180/hr. Among the crystals thus obtained was one with a weight of
355 g, grown for 37 days at 48 - 560. Depending on the supersaturation
and purity of the solution, the growth rates along the x--, Y_ and z-
axes are 0.13 - Ool8j 2o0 - 2.7 and 0.2 - 0.5 mm/24 hours respectively.
The course of the crystallization is influenced 17 the rates of crystal
growth and cooling of the solution, by supersaturation changes, and by.
the presence of impurities; these cause the development of internal
stresses and hatchures on the(,Ojface, the complete cessation of crystal-
lization along the z-axis and in the~0011 direction, and the formation of
Card 2/3

3)536
S/564J61/003/000/005/029
Certain growth... D228/MO4
laminae on the[0011 face which grow into large plates accumulating on top
of each other. In conclusion, the author notes that crystals of sorbite
hexa-acetatep cut out along the cleavage, may be used as monochromators
of X-rays; their reflecting power is higher than that of pentaerythrite
crystals, and they are stable to the effect of X-rays. There are 6
figures and 2 references: 1 Soviet-bloc and I non-Soviet-bloc.
Card 3/3

L-0~/Iq V
S/564/61/003/000/006/029
D258/D304
AUTHORS: Nepomnyashchayap V. N., Shternherg, A. A., and
Garj';~ilova,_ I 1-..-V.
TITLE: A laboratory method for growing large, faceted crystals
and oriented blocks of lithium sulphate
SOURCE: Akademiya nauk SSSR. Institut kristallografii. Rost
kristallov, v. 3, 19619 290-295
TEXTs The authors' aim was to produce crystals of Li 2s0 4.H20 to be
used in manufacturing piezoelectricul transformers, as indicated by r. G.
Poldnyakov (Ref. Is Kris tall ograf iya, 19 29 228, 1956). Their work con-
fims the difficulties encountered in producing crystals sufficiently
large and homogeneous for that purpose; they found, however, that ori-
ented blocks, grown in forms, are easier to obtain. The production of
both crystals and blocks is described. (a) Crystals: A solution of
Li2SO4 (C.P. or F. A. grade; d - 1.213 - 1.214 ut room temperature) was
Card 1/3

S/564/01/003/000/006/029
A laboratory method... D258/D3O4
used, and 0.5 to 1-,5 g/lit of R2S04 were added to yield pH 4-5. The
crystal volume after n days, V , was found to be: V - kn ~! nb + C)
n lk 2 (-TO
where C is the initial length of the seed (in 4.,.m); b-the daily increase
in width (in em); k was 0.75 - 0.85 . The veight of the individual
crystal was G n - VDd , and the volume of condensate removed in n days
G .1000
was S where S is the solubility of Li 2S04 (in 9/1't) at
the temperature of crystallization. Imperfect or parasitic crystals were
trapped by the hole of the false bottom and did not interfere with the
principal crystals. A fresh solution was continuously added at the rate
at which condensate was removed. The growth proceeded at the rate of
b = 3 mm. Periods of 40 to 60 days were necessary to obtain crystals of
up to 400 g . Many crystals were lost due to cracks formed during the
process or while being removed from the support. Added HSO 4 enhanced
growth along the 11z" axis (identical with the axis of the branch), while
Card 2/3

S/564J61/003/000/006/029
A laboratory method... D258/11304
impeding growth along the "x" axis. (h) Blockst A static process
was employed. The rate of growth depended on the daily quantity of
condensate removedp Q, which was calculated as followst Q (in ml)
P-a-d-1000 f where P in the overall crystal surface (in Cm 2); a-
s
the rate of growth (in cm of gained he 'ight); d-the crystal density;
S-solubility of Li 2s0 4 at the working temperature (in g/lit). a "'
averaged 1.5 to 2.0 mm/day. This method is said to be less sensitive to
temperature fluctuations, but very pure solutions are required. Imper-
fect growth could be eliminated by lowering the respective beaker into
the colder zone at the bottom and dissolving its contents. There are 5
figures and 5 referencess I Soviet-bloc and 4 non-Soviet-bloc. The
references to the English-language publications read as follows-. R',
Bechm%nn, Piezoelectricity, London, 1957; R. Bechmanng Proc. Phys. Soc.?
65, 375-377, 1952; A. Robinson, Crystal Growth, Discuss. Farad. Soc.,
5, 314-319, 1949; 0. F. Tuttle, W. S. Twenhofel, Amer. Mineralogist, 31,
5699 1946.
Card 3/3

8/081/62/000/917/009/102;~.
B i 661B i e o
-i
AUTHORS: Nepomnyashchaya, V. K., Shternberg, A'. Aj~,. Gavrilova# I. V.
TITLE: Laboratory technique for growing large faceted,
orientated blocks of lithium sulfate

179 1962, 33-34, abstract:
PERIODICAL: Rcf,.;raLivnyy zhurnal. Khimiya, no'.
.
17D201 (In collectiofi: Rost kristallov. v. 3. 24,f AN SSSR,
,
1961, 290-295- Dinousa~f 501, 502)
TEXT: A laboratory technique has been developed for growing large
faceted cryotals and blooke of Li so H 0 (1) Pihich are important for
2
2 4
,
the production of piezoelectric transducers for varidus purposes. Fully
formed crystals were grown'at u constant temperature of-490 - 100 0 from
weakly acid solutions (PH 4-5 01 by means of a controlled flow A
-condensate with reversible rotation of the crystals. The influence of
temperature, the PH of the solution and the quality of the seed crystal
on the growth rate and'homogdneity of I crystals is discussed. Crystals
grown a"L 940C show no cracking'defects. When ori6ntated blocks are grown i
.,Card 1/2

the 80lUtion will be precipitated and will either be entrained by the
growing crystal or leave microPhannels in it. (Abstracte~rts note-
Complete translation.]
S10811621000101710091102
-Laboratory technique for growing ... B166/B180
molds, tht~ seed crystals are cut parallel to one of the slowly growing
facec of the I crystal and arranged strictly horizontally so as to co'ver
completely the bottom of the mold. The-growth rate is controlled by the
quantity of condensate poured in. The technique described is not
susceptible to temperature fluctuations and no further measures are
required to keep the crystallization pans at'a constant temperature.
It, is emuh..-sized that the solutioremust be pure, since the crystals are
grown under static conditions and any mechanical impurities present in
Card 212

SHEnALI, M.N., doktor geologo-mineralogicheskikla nauk;
GAVRIWVA, IOVO
Equilibrium e~-De of crystals allowing for volume free energy.
Rost krist. L:32-35 164. (MM 17!8)
1. Otvetstvennyy redaktor abornika "Rost kristallov" for
Sheftal').

GAVRIIOVA, I.V.; FUZNFTZI-(;V,!, L.~~
of c,.f
single cry?tade. Rc-A krist. 4.~8,5-88 16,4. (M-!~A rf,~8)
:11

L 21222-66 EWT(m)/EWP(t) IJP(C) JD
ACC NR: Ap6oo3B12 SOURCE CODE: UR/0191/66/003/00:L/0272/0274
,AUTHORS: Areflyev, 1. M.; 113azhulin, eased); Gavrilova,
(jec
71 Zheludev, I. S.
.ORG; Physics Institute im. P. N. Lebedev AN SSSR, Moscow
.(Fizicheskiy institut AN SSSR)
~,TITLE: Temperature dependence of the intensity of light scattering
~in oriented single crystals of KHPO and Rochelle salt
4
i'SOURCE.- Fizika tverdogo ted] _V. 9, no. 1, 1966, 272-274
iTOPIC TAGS: ferroelectric crystal, phase transition, light scatter-
:ing, temperature dependence, light polarization, elastic modulus,
'crystal lattice vibration, Curie point, paraelectricity, piezoelectric~
property
IABSTRACT: The purpose or the measurement of the temperature depend-
was to check whether the ferroelectric phase transition in these
;crystals is connected with instability of the crystal against optical
'lattice vibrations. The experiment was made with a spectrometer
Card 1/3

L 21222-66
0
ACC NR: AP6003812
.(DFS-12) whose output was photoelectrically recorded. The illumina-
.tor and the sample-cooling system are described elsewhere (A. V.
~Rakov, Tr. FIAN v. 27, ill, 1964). The investigated crystals were
,.transparent with cross sections 7.5 x 7.5 mm and lengths 20, 23, and
'149 mm. The Rochelle-salt crystals measured 7,5 X 7-5 X 30 mm. The
0
of scattering,was measured at the maximum of the Hg 4358 A
:line under smooth variation of the temperature. The results were
strongly dependent on the polarization, and in the case of one type
,of polarization the intensity of the scattered light had a variation
;similar to that of the reciprocal of the elastic constant. It is
concluded on this basis that the scattering is produced by anomalous
!acoustic vibrations. In the case of Rochelle salt, the effect is
iless pronounced in KH PO - and no increase in the scattering intensity!
i 2 4P
lis observed at the second Curie point. This indicates that the
Istructure of the Rochelle salt crystal is different in the two para-.
i
,lelectric phases. No low-frequency Raman scattering spectrum was ob-
iserved, and it is therefore deduced that the increase in the scat-
tering intensity of the Curie point is connected with the anomalous
behavior of the acoustic lattice vibrations. It is concluded on the
Card

L 21222-66
ACC NR: AP6003312
basis of these results and earlier data by the authors (FTT v. 7,
2413, 1965) that the ferroelectric phase transition in both salts is
due to the instability of the crystal against the acoustic and
optical vibrations of the lattice, which are interelated by the
piezoeffect. The authors thank G. P. Motulevich and D. G. Sannikov
for a useful discussion. Orig. art. has: 2 figures
iSUB CODE: 20/ SU13M DATE: 02Aug65/ ORIG REF: 00-5/ OTH REF: 003

GAVRI IDTA. K. : VAT)ISHTM, Ya.
Bw shonld the laboratory of a restaurant's trust be orjpn-
Is6d? Obahchenty.pit. no.12:26 D '59. (MIRA, 13:4)
1. Vachal'nik torgovo--roisvodetyannogo otdOlA Kishinevskop
tresta stolovykh i restoranov (for Gavrilova). '. Zaveduyueha-
ch.ly laboratorlyey Kishinevokogo tiesta (for Taynohteyn).
(Testi laboratories)
'IR;staurants, lunchrooms, ate.)

-
4

V_ r ~, 1 0 4 14 U f

we -4i Ion of iundsten mind callumblum In steel,
04mijill-4 and K. (), (:-1UdQU~ 7Aff"1011
-
C16
4~1VI W C."I be WIXI. by cil
-
1
f;-
-i1h thkcyAtute. diter rt,luctiou, vvvit 1
pkr(-=U
the p"imunced.31,1, Mo.
7
Mi. of 4 N II.SC4 Simi 10 tul. film (d. 1.
.). 0"111..
with a tew it of ft.%*Lh. tvap. to funtes, C-4. -111,
=
with&) mi. of
.O.and 6-it todit%nive mits. Xcuti-Ain
00 with 207V N4011 to chjudincts, beat to boiling. add v, 140 00
ful.'slacustu- NX011 coul a
l
k
hi
~fi

00 i A ill
e t
s
a 10 ml. aliquot - '
quiit awom, lu
NAOIfaxd2N)mI.,nvoI. Add2.hml.of2S7vSII.SNC.
fit. to W mi. with 10% SuCh. mix. and turAsurr the cnl,,(-
00 in a ccAuriowtirr against a standard. Towp.WandClw,
f
l
h
a Zoo
i
ter t
e w
ll I thin. by rAl tltl. fill)
Atovr) to
till 9. 44 N41". IhI I.,
-4) Hill. .1k] ffl-At jJW COW W411. With 51W 11191. Ill

OO

"Pt"TURIS %At%. Aod suctse fifter Iloptr pulp. Mwt -itimt -00
00 10 win. mul filtratim. wash the t. with 3.3 N I IS1 1,
Ill
t--ntx. 20 MI. 6% cualtirrom pet
. and then with 5,;
' Z

N11.011. Ash the filter. moisten the ash with co,,'
I e 0
IISO.. and low with G-1 S. KIISO., Txuch the collil',

010 a inch with 4 lit (k water and add 2% 1 ICI tot toul "4. .1
250-0W oil. Bod 0.5 hr. with imk)!r Itulp and filter 4
thcCW.W. Wash with dil. IICI and ignite tocun%t. too
Xf. KAKairm,11
two
too

L 4 I-LL- W SL too
lee
t
,
414
r 0 a q
1 1
1, 1, v M W
it 4 IN M It it I N 0 n 1
*
r,

0
0 * 0 0 *
00 see 00000 00
099
0 q;0 o goo o 0 009 00 0 0 6 * 0 0 04 06 of 000 00000 we 0 0 0

(3- IqvR 0 V/-3
Country USSR T
Catc,-ory: 2-Aman caiLl AnLzl PhysioloMr. Internal Secration.
Thyroid G)=d
Abs Jour: P=iol-, No 19, 1958, 88949
Author Gavrilova ' '
Inst i= aitc~cdInstitute
Title The HistopatholoGy of the Thyroid Gland in Chronic
Loss of 'Zile by the Organism.
Oria Pub: 5-Y Pavlovsk- sb. Tonski y ned. in-t, Tomsk, un-t,
1956, 49-51-~
Abstr-act: In doC;s with bill"ary fistulas a picture develops
within two to seven weeks similar to chanCes occur-
rina with colloid Goiter; varked dilatat-'on of the
fol.liculos of the thyroid gland (TG) by a thick
Card 1/2

GAVRILOVA, K. K., Cand Med Sci -- (diss) "HistoloFical chz~n6es
in the thyroid gland upon chronic loss of bile in dogs." Tomsk,
1060. 10 pp; (Tomskiy State Medical Inst); 200 copies; price not
given; (KL, 19-60, 138)

rr
,Mri!
Ell f
CIE' I Ell
rill A
;L;j ac fl-091H
gN
29 j 16
v , I '.,I -. I r-0-
- P ~ i ; I MY, P!5
FF I r a
trot
a j log rr
Pq INn.

KHLGPKOV, A.M.; S-TRNBA,, O.S.; FAVLITSKAYA, S-S-; GAVRIIIOVAi, K-K-;
KOROCMM, L.I.
Changes in the organs of horses used for the production of
serum Winst tick-borne encephalitis. Trudy TomNIIVS 21:
31-1-318 160. (MIRA 16:2)
1. Tomskiynauchno-isaledovateliskiy institut vaktsin i eyvorotok
i kafedra gistologii Tomakogo meditsinakogo instituta.
(34CEPHALITIS) (UBMATORY AWIMALS-DISWES) (SWN)

GAVRILOVA, K.K.
of,x-ray changes in joints of the hand in chingae
[with summary in Inglish]. Veat.rent. I red. 33 no-5967-72
S-0 '58 (MIRA n:11)
1. Is kafedry obehahey khirurgii (sav. -,Prof,. G.A. Orlov)
Arkhangel'skogo meditsinskogo inatituta.
(DIPLOCOCCUS, infect,
chingap joint din. in seal huntors (Rue))
(OCCUPATIONAL DISBASES,
chinga6 diplococcal Joint die. In-seal hunters (R"))
(JOINTS. dim.
chinga, diplococcal infect. in seal hunters (Rue))

G.!,.VPIL--,,V-,', K.Y., C--,:d tied Sci - (dis:,) HX-ray observation
of -~v ~!os, 1959, 13 PP (11.9in of Health USSR.
Central inst for the Advanced Irainimg of Physicians)
200 copies (KL, 35-59, 116)
56

GAVRILOVA, K-lavdiya mikhaylovnas dots.; STARICHKOV, M.S., red.;
MATTEMX-,X-. 7re d .
(X-rW picture of chinga] Rentgenologicheskaia kartina
chingi. Moskva, Izd-Vo "Meditsina," 1964. 50 p.
(MIRA 17:3)

VOROVOVJ, F.D.; TRIFONOV, A.G.; MUSID, S.Ye.; DM-HTEYN, Ye.1,; VALIPITERS, E.V.
SIIEGIREV, Yu.B.; AIMPIN, V.G.; Prinim~li uchasti~m: SHIRNOV, L.A.;
KAZAKOV, A.I.; 'YELIZAROV, A.G.; KULAKOV, A.M.; KOZHAIIOV, M.G.;
ZARZHITSKIY,, Yu.A.; ARTMIONOV, M.P.; GOLIDEYBERG, I.B.; ROMANOVp
V.M.; VOVIKOV, S.M.; MAYEVSKIY, A.B.; DMITRIYU, I.; MAMMA, M.;
BEREZOVOY, I.A.; ZUTS, K.A.; BADIN, S.N.; TAT-.'-.RIIITSEIr, G.;
MITROFANOV, N.G.; GAVRILOVA, K. .; IVAKOV, N.I.
Operating a 400-ten open-hearth furnace on casing-head gas.
Stall 20 no. 7:594,598 Jl 160. (MIRA 14:5)
(Open-hearth furnaces-Equipment and supplies)

,_GAPII_oOVA, K.N.; PTATHITSKATA, Te.N.
Work of the operative group in supplying agrometeorological infor-
mation during the harvesting campaign. Meteor. i gidrol. no.10:
40-41 0 160. (MIRA 13:10)
(Irkutsk Pfovince-Meteorology, Agricultural)

137-1958-3-4834
Translation from: Referativnyy zhurnal, Metallurgiya, 1958, Nr 3, p 55 (USSR)
AUTHORS: Benuni, A. Kh., Gavrilova, K.-Y--
TITLE: Methods for Consolidation of Progressive Operational Experience
ii. Industrial Copper-smelting Process Engineering (Metodika
9hobshcheniya peredovogo opyta raboty v apparatur.nykh
protsessakh medeplavillnoy promyshlennosti)
PERIODICAL: Tr. Ural' skogo politekhn. in-ta, 1957, Nr. 66, pp 4- 11
ABSTRACT: Material dealing with the operation of a reverberatory converter
at the Krasnoural copper smelting plant was studied and consolidated.
Best methods for the performance of laboY operations were evolved,
together with optimal regimes for the technological process. In
order to minimize Cu losses in escaping gases and waste slags,
special graphs were developed for the loading processes of the
reverberatory furnace (with appropriate allowances for the
temperature regimen in the zone of fusion, and for chemical
composition of cinder) as well as for the optimal conditions for
the pouring of the converter slag into the furnace, the settling
process of the bath, and the discharge of the waste slags..
Card 1/1 G. S.

GAVRILOVI, Kapitolina Vladimirovna; ZONOV, S.K., retsenzent;
MkUBISINUW,-S-.MF.,--r7&F.,--SYROHINA, M.M. , red. izd-vp-;
MALIKOVA, N.T., tekhn.red.
[BusineeB accounting in the workshops of copper smelting plantq]
Vnutritsekhovoi khosraschet na medeplavilInykh zavodakh.
Sverdlovsk, Metallurgisdat, 1963. 49 p. (MIRA 16:6)
(Copper industry-Finance)

GAVRILOVAP Kapitalina Vladimirovna; KOVALEVSKIY, H.A.r -ed.izd-va;
GINNURGY R.Ya.p tekhn. red.
(Busilless accounting is a means of mobilizing internal
potentials] KhoziaistvenrWi raschet - uslovie mobiliza-
tsii vnutrennikh rezervov. Moskva, Metallurgizdat, 1963.
29 Pe (MIRA 17:3)

WA

-,-GAVRILOVA,--k-A,-
Struitturs of high winter anticyclones in the Arctic. Probl.Arkt.
i Antarkt. a0.3:31-39 160. (MIRA 13:9)
(Arctic regions--Cycloaes)

S/169/61/000/010/025/053
D228/D304
AUTHOR: Gavrilova. L.-A.
TITLE: Some results of investigating the thermal structure of
Arctic anticyclones
PERIODICAL: Referativnyy zhurnal, Goofizika, ho. 10, 19619 29-30,
abstract 1OB204 (Tr. N.-i. in-ta aeroklimatol. no. 14,
1961, 76-83)
TEXT: The characteristics of the thermal conditions in different parts
(front, rear, central, right, left) of three groups of Arctic anti-
cyclones were determined from synoptic and aerologic maps and the data of
radioprobing in 1950 and 1954-1958: (1) strengthening anticyclones moving
north-eastwards over the eastern sector of Soviet Arctica; (2) strengthen-
ing anticyclones with little mobility; (3) disintegrating anticyclones
with little mobility. The pressure change was determined for a 12-hour
period in the central parts of anticyclones. The mean seasonal tempera-
Card 1/3

B/169/61/000/010/025/053
Some results of... D228/D304
tures at standard levels, certain characteristics of inversions and the
tropopause, and also the mean stratification curves were obtained for
different parts of each group of anticyclones. Temperature inversions in
the near-surface atmospheric layer were noted in all groups of anti-
cyclones in all seasons of the year. In moving anticyclanes In winter and
summer, the left parts are the coldest in the whole troposphere, the
right and rear parts being the waxmest. The temperature differences b8-
tween the opposite parts of anticyclones reach a maximum in winter (14
at the ground surface) and decrease at all altitudes towards the summer.
In summer, the maximum differences were observed at a height of 1. km,
where they amountrd to 60. The temperature differences decrease witk
0
s1titude and become close to 0 at the tropopausets lower boundairy. A~
the ground surface in immobile, strengthening anticyclones, the western
par-t-is coldest for the whole year. the southern part being coldest in
....3pring 4nd the eastern part in summer; the eastern part is warmest in
Winter, the southern I\qxt is warmest in summer, and the western par-, i-q
J' -)b'
warmest in spring. Temperature differences in. various parts o imm. 1-e
~Gard 2/3

Some results of...
S/169/61/000/610/025/053
D228/D304
anticyclones are less than in moving ones. The mean quadratic variability
of0the temperature abruptly increases above 8 km in winter and reaches
11 at a height of 16 km. The abrupt heating of the Arctic troposphere
and stratosphere is noted each winter. The intensity and duration of the
heating diminish from above downwards. Thus, in January 1958, over sta-
tion CrI-1 (SP-7) the temperature rise comprised 41 0 at the 30-mb level,
290 at the 200-mb level, and 5 0at.the 500-mb level. Heat advection in
the Arctic in winter is noted at the time of neridional forms of circula-
tion. Immobile Arctic anticyclones are divided into three groups in rela-
tion to the circulation conditions and heat advection in the troposphere
and stratosphere in winter. The characteristic peculiarities of each of
the groups of anticyclones are given together with their frequencies.
8 references. fAbstracter's note: Complete translation.-7
Card 3/3

AdMSSION NRt AR4008M 3/6~f9/63/000/011/tO24/D024
SOURCE: RZh. Geofizika., Abs.' 11'B149
A'UTHHOIR, Gavrilova, L. A.
TITM: The verticai"Vktent-of fronts in the central Arctic
CITED SOURCE: Sb. Probl. Arktiki i Antarktiki. VY*P. 13. L., Morsk. transport,
1963, 27-33
TOPIC TAGS: meteorology, Arctic front, ionospheric front, tropospheric front,
froetal heat transfer, Central Arctic front, frontal altitude, temperature
sounding, heat transfer
TRANSLATION: The author testsl the suppositionslof S.S. Gaygefov and V.I.
K~yezeva on tbe considerable vertical extent of Arctic fronts. From the data of
ground-level and high-altitude synoptic maps and temperature probes from drifting
stations for January-July 1955-1160, she constructs tables of the vertical extent.
of fronts and time sections. She concludes that the fronts in the Central Arctic
are in most cabes high. The shift of the warm fronts to the south and the cold
Card 1/2

ACCESSIOIN NR: AR4008216
fronts to the north leads to the intensive inter-latitudinal exchange in the
Central Arctic within the limits of the entire troposphere, and in a number of
cdses in the lower stratosphere. I. Dubina.
DATE ACQ: O9Dec63. SUB CODE: AS ENCL: 00
Caro 2/2

KIMNETISOV, A.V.; NIFASHEVA, I.F.; GAI~~k~ L.A.; DANIIMIA, V.V,.
Frontal sections in the Arctic Basin and their relationship
with the types of synoptic processes. Trudy AANII 255:192-
2 12 t 6.3, (MIRA 17:6)

qA~MILOVA) L.!*
Vertical extent, or thm pnessure systoms in the! !,r!-,tjA,, i~rcbl. rtrkt. 1.
AnUrk. nn.20.~31'-~.39 165. (ff,.TRA 19CLO)

L 2 892-65, EWT(1)/'FqC ~Gw
ACCESSION NR:. AT5002286 S/3116/64/266/000/0104/0118
AUTHOR,- G ilovs. L. A*
Tl=: Distribution of tropospheric let streaml'in the h1gh latitudes
SOURCE: Leningrad. Ar -kt-i-cheskiy:_L antarkticheskiy nauchno-issladovatellskiy in-
stitut. Trudy, v. 266. Meteorologicheskiye usloviya v Arktike v period14GG i
MGS; abornik statey (Meteorological conditions in the Arctic during the IGY and
IGC; collection of articles), 104-118
TOPIC TAGS: troposphere,, jet.streams Arctic meteorology, tropopause, wind velom
city
ABSTRAM In. this study, an attempt has'been made to investigate the geographi-
cal distribution of the frequency of jet streams with different velocities dur-
ing different seasons of the year on-the basis of actual wind observations at
polar and on drifting stations, Radiosonde observations at 36 Soviet and foreign
polar stations situated to the north of 60*N were used; these data covered the
period July 1957-December 1960. Also used were AT500 and AT300 charts for the
same period. . For the Central Arctic the data used were from Soviet and American
drifting stations (1955-1960); the longer observation series for the drifting
Card 1/4

L zox~8j2_65
ACCESSION NR: AT5002286
stations was necessitated by the small wmber of jet streams in that region, The
Central Arctic was divided into seven sectors for this purposes In this study a
tropospheric jet stream is defined as a strong air current with wind velocities
greater than 30 m/sec with the maximum velocity observed in the troposphere or
in the -tropopause layero The frequency of jet streams with wind velocities greab.
er than 30 and 45 m/see (in%) is shown in a series of four seasonal maps; Fig. I
of the Enclosure is an example, It is shown that a characteristic of the dis-
tribution of the frequency of high-latitude Jet streams in winter and in the
transitional seasons is the presence of meridionally elongated zones of high and
-low - f reque nay -va lues.--In- summer-the-frequency- dis tribut ion-has -a-- more -latitud-
inal character in comparison with the remaining seasons of the year. In regions
of high frequency jet streams are stronger and more stable in direction, than jet
streams in regions of low frequency. The direction. of jet streams in winter and
in the transitional seasons is characterized for the most part by meridional
components (50-70%); in summer, especially along the Arctic coast, it is charac-
terized mostly by westerly components, A series of five appendices give a great'.
volume of data on the areal and seasonal distribution of Arctic jet streams.
Orig. art. has: 6 figures and 6 tables.
Card 2/4

L 23892-65
ACCESSION NR: ATS002286 ENCLOSURE: 01
~13
P.2
IIH V1
VIA
Figure 1. Frequency of Jetatreams1n winter (November-March)-. 1) frequency
of wind velocities greater than 30 m/sec; 2) frequency of wind velocities great-
er than 45 m/sec; 3) aerological stations,
Card 4/4

GAVRIU)VA, Ij*A.
Characteristics of tropospheric jet strmms--a-t- high -latitudes.
Trudy AAIIII 273:100-131 ?65. (MIRA 18:6)

I il L. A.; D A'; 1-1 U) V A p V. 14. ; N'b-.0V A ~ .
11 1 N. V
Structure of fronts at, hi-f~h latlt-,.des. I-Ifeteor. is-tl. :~r-.9:

L 46320-66 EVrI (-1
ACIC NR: -,Tj/
6014569
SOIT-ICE COTIE: !F-,/0169/65/000/011/3055/bO55
AUTHOR: Ca,.r-4lova. L. 4.
Id
TITIL: The cliaractoris'kics of tropospheric jet strearris at high latitudes
SOURICE: Rof. zh. Geofizilm, Abs. M371
Ll~'7 SOMCE: Tr. Arkt. i antarkt. n.-i. in-ta, v. 273, 1965, 100-131
TO?T.I stroazi, Ixctic clin-ito wind velocity, atmospheric front, tropopauno.
A3,STPUCT: kn attempt is made (from data from r--d-io pilot observat-ions of 1."orth Pole
-ta~40r --1960) to
6- is in 1955-1960 and 35 Soviet and foreign polar stations in 1957
h
obt-oim not only the vertical characteristics of troposp oric jet streams but also
'he horizontal ones: 'lie =.dmum velocities of Uho jo~
streans are given in tho
A.0r.m of isotachs. The riinimi"- velocities are localized over Arctic Canada, Central
Arc'4ca, and Taimiir. increased velocities in -.lie irintor and fall are ditua'ed in
t--I9 region from the L-Itlantic and Pacific Oceans to the Polo and (in sprin,m and sum-
Mer) from tho continents of Eurono and Asia. 'I'lle nrcOominant velocities at the
center of the jot streanns are 301-40 m/sac. Transition from sr--mier to winter has
a2z--o--t no effect on velocit~Ir. The vortical stron-th of tho streams (30 M/sec:;
accord to isotach) ro-ardloss of tho time of yoar, is observed alonG tho ~--ctic
i I 1~ i-
coast (?rrcom 3.2 to 3.6 h-mi, and tho minimwm (fron, 2./, to 2.8 11m), in. the central
A--ctic. Z=ples of jet strear- In the .4--ct--c with a thiclmesa o-4., 10-15 11CM are
CCIM 1A UDG:- 551.557.5 J
GW

L 46320-66
ACC MR:
AI-76011,569
prvauented. The altitude charactoristic of ra%-a--.al winds is given: the hichost
=-xirwam winds, regardless of the season, are situitod alono the coast of Eurasia and
Alasim (S.4-9.2 Im); the lowest, abovo the Canadian Arctic Ax-chipelsGo and-tho
neighboring seas. The maps of the average altitude of the Maximum vinds in
L' I jot
sl-rex=s are in General agg-oor-ent with the maps of averago intomsiLy. The jot streamsi
of the Arctic Basin are lovor than those of the middle latitUdos; their ax'os are
within 7-9 I= (9-12 11--a in the middle latitudes). Low jot stream (in a layer of
1-3 laa~-which are connected with cold frontn are observed in 'the Arctic in the
'..'Lntor. The case of the low jot of 17-19 Fobruai-r 1959 is analyzed, but the recur-
--Once DCriod of low jets is only 1-2' of the total number of cases. As a rule, the
jet streans of the Arct, c basin are situatod in '.he warm air bolow the tropopause.
Regardless of the Arctic region, the axis of the jet is 1-1.5 km below ' e trope-
U - Uh
pause. In isolated cases, this differonce can reach 5 laa. D. Mlorozov ZTranslation
of ab--tracgt
SIM CODE: C/,
Card 2/2 -,a-7X-

wits
Of th
&noMS 32estum CONIPOU11 . U. Action of
gneidum brontide on init
ca jfp~vll, and
it =arl
Khinf.'20, 24 ~A47.
Pr". TR~l PDr with 26 1. C1fg:Ch1cCOgMe
from 13 1. Mg and 48 S.
(cf. above ref. for procedure) gave 54~5 g. fraction coti(C.
38% dimethylUoprolo.-ayk=01nol and 48% J-1rf1ky1-Z-PC11L2-
mro. b.W-133"; tIt* letter substance was Identified by the
ssmi"rbavm, m-."*. A higher boiling fraction (1) of
the rtaction Products, 113 X" was Also Obtabled, bg 103-4"..
-OC113feC11r-
do 0.0770, xV 1.4468; which is either AW,
CUftCLh Aft ot MOM& CIA C11.4fe CO, Ate, Tit rod-
uct rcdui(cd A hro. with aq. K%CO; rue Cliff. bill
(1cwtup 192--31.
which cocre3ponded to CithcS dAyl-l-eydo-
AgXOM-1-Oxf of $4.44riwak hexo-1-oxo); the
other product oUhydrolysV=*"XA*t r4, CIA101. bt 165-
60" (with a motio-Ag saltj the acid.
yields an oziw#. Wo form of which wcxe Isolated, m.
120-l' and lini. 114-18*; the JV* Wt of oxiTa gavelom Ag
gait, C~SHUO These mctions were similar to t me of
14 hro. with MOMMOH'
M1d of o6 O"Aucts m. 11242,50, which is dther'
tan 60
74akg=xtdW# or ti-djftteMy1-2j'
dkY1-J..5-cy4oAezm;;1Lw. ~ MfelIr from ~ 13 g. Vg aed
.54 g. HtBr with W11. Cff*;CUeCO.Me pvc 2 fraztfops:
the filwilani- colf,40, b.- 1W-29.- did O.&M til?
1.4=, sM4 the IM&W (vattip-G, qWA, bt
xV 1,4395. 'The laft" rcftxtd 4 hys. with ok,'KOH pvc
aaacid'T CO 1*,i~.W6".whkhan4ow44W-p*-e~
The resulu Indiczavd Oci
of d Wwchl,
5~rcA two
-S-tvel,~ Ze 2~,

5(2) SOV/63-4-1-22/31
AUTHORS: Vladimirovq A.M.f Vcl ovik . B, N1. , 0,;vri I ova, L,A. , Kameno takiy,
V.I.: Kroll, V.A.
TITLE: Continuous Method for Preparing Titanium Trichloride (Nepreryv-
nyy sposcb polucheniya trekhkhloristoge titana)
PERIODICAL: Khimicheskaya nauka i promyshlennost', 1959, Vol 4, Nr 1,
P 132 (USSR)
ABSTRACT: A laboratory device for the preparation of T 'C13 is described
here. It consists of an evaporating device (1)i a heater for
TiCl 4 vapors (2), an electric furnace (3), a cooler (4) and a
container (5). The method is based on the reduction of TIC14
by hydrogen at 820 - 8400C. The output of the device is 10 -
15 g per hour. The reaction proceeds at a considerable eXcess
of TiCi 4 (10 : 1 or 20 1 1) which prevents the formation of
TiCl The produced TiClm is 98% pure.
2*
There are; 1 diagram and 6 references,.2 of which are Soviet,
Card 1/2 2 American, 1 English and 1 German.

Continuous Method for Preparing Titanium Trichloride SOV/63-4-1-22/31
ASSOCIATION: Vsesoyuznyy nauchno-issledovatellskiy institut sinteticheskogo
kauchuka (All-Union Scientific Research Institute of Synthetic
Rubber)
SUBMITTED: June 23, 1958
Card 2/2

3/138/59/000/07/02/009
AUTHOF?3: Vladimirov, A. M , Gavrilova, L. A., Krol', V, A.
TMM. On the Synthesis of Trans-1.4-Polylsoprenel\
PERIODICAL: Kauchuk I Rezina, 1959, No. 7, pp. 6-7
TEXT: The authors show that a polymer containing as much as 97% links of
the trans-1.4-type polymers, can be obtained in the catalytic polymerization of
isoprene using triethylaluminum and titanium trichlorlde. It is also shown that
this polymer is Identical to the a-form of natural gutta percha, as far as its
elementary lattice parameters and its crystallizability are concerned. Accord-
ing to the authors, this was already accomplished in 1956 by G. Natta and co-
workers, as stated in Ref. 1. The present article reveals the experimenfal results
on the polymerization of isoprene with titanium trichloride and triethyl aluminum,
the latter acting as catalysts. These experiments are the continuation of work
published previously by 1. 1. Boldyreva and coworkers, and B. D. Babitskiy and
coworkers, Ref. 3, and 4. The relacement of the titanium tetrachloride with the
trichloride, yields the trans- 1. 4-conf igurationinstead of the Cis-1.4, as obtained
,~ for obtaining titanium trichloride is described briefly.
in Ref. 3. The metho
The triethyl aluminumlis a ready product produced by the NIIPP (Scientific
Card 1/2

On the Synthesis of Trans-1.4-Polyisoprene S/138/59/000/07/02/009
Research Institute of Polymerized Plastics). The experimental procedure has
already been outlined in Ref, 3. Table 1 gives the results of the experiments
under various conditions. It is seen that the yield of the polymer depends a
great deal on the -temperature, and that even at 1000C, the yield does not exceed
15 to 20%. This Is explained as most likely being due to the low solubility of
the polymer. The presence of the solvent and Its nature has little effect on the
process.and on the structure of the formed polymer. Table 2 gives the results-of
the obtained samples, as to their structure and properties. Data of natural
gutta percha are submitted for comparison. The somewhat lower stability of the
synthetic polyisoprene is explained by the different molecular-weight distr1bution
of the polymers, and also by the possible presence of certain deviations in the
structure. There are 2 tables, 5 references: 3 Soviet, 2 Fhglish,
ASSOCIATION.- Vsesoy-uznyy nauchno-issledova"ellskiyimtitut sin'teticheskogo
-kauchuka im. S. V. Lebedeva(All-Union Scientific Research
Institute of Synthetic Rubber im. S. V. Lebedev).
Card 2/2

KHROMOV-BORISOV, N.V.; GAVRILOYA, L.A.
P3TYlium compounds having active methyl groups. Part 1: Reactions
of 2-methyl-4,6-diphenyl pyrylium. ferrichloride and 1,2-dimethyl-4,
&-~diphenyl pyridinium iodide with benzaldehyde and p-dimethylsolb-
obenzaldehyde. Zhur.ob.k.him. 31 no.7:2192-2198 Jl 161. (MIO 14:7)
1. Institut eksperimentallnoy'meditsiny Akademil iteditainqkikh
nauk SSSR.
(Pyrylium compounds) (Pyridinium compounds)
(Benzaldeb$de)

KHROYLV-BORISOV, N.V.; GAVRILOVA L.A
Pyrylium compounds having active methyl groups. Part 2: Reaction
of 2-methyl-4,6-diphenylpyrylium chloride with diazo compounds.
Zhur. ob. khim. 32 no.1:86-89 Ja 162. (14IRA .15:2)
1. Institut eksperimentallnoy meditsiny AMN SSSR.
(Pyrylium compounds) (Diazo compounds)

KMCMOV-BCRISOV, N.V.; ~~VJULOVAI-L-_
Pyry.lium ccmpmnds having active methyl groupa. Part 3:
Structure of pyrylium aso cmpounds. Zhur.ob.khim. 32
no.10:323-1-3214 0 162. - (MIRA 15:1-1)
1. Institut eksperimentallnoy meditainy AMN SSSR.
(Aso compounds) (PIrylium compoinds)

A
ACC NR, AT6006699 SOURCE CODE: UR/2561/65/000/020/0031/0039
AUTHOR: Gavrldova, L. A.
ORG: none
TITLE: Vertical extent of pressure systems In the Arctic
SOURCE: Leningrad. Arkticheskiy i antarWches!dy auchno-IssIq ~oiktellskly institut.
Problemy ArktIkI I Antarktiki. Sbornik statey, no. 20, 1965, 31-39
TOPIC TAGS: arctic climate, cyclone, anticyclone, atmospheric circulation, atmospheric
interaction
ABSTRACT: The purpose of this work was to investigate the vertical extent of stationary and
moving pressure systems in the Arctic based on the data collected during 1955-1960. for this
purpose the author selected anticyclones that had been observed over the entire Arctic and
cyclones which had been observed over the central and eastern sectors of the Soviet Arctic.
Ile selected pressure formations were bounded by closed Isobars and had been traced on
charts foratleast 12 hr. A total of 644 anticyclones and 333 cyclones was selected. The authoz
divided the anticyclones Into four groups: 1) anticyclones moving over the eastern half of the
Arctic toward the east and northeast; their regions of formation are Siberia and the Chukoteldy
1/3 UDC: 551.558(985)