SCIENTIFIC ABSTRACT ZVEREVA, M.N. - ZVEREVA, V.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R002065710011-8
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 26, 2002
• Sequence Number: 11
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

ZVEMVA M. if.
Sipara-tion of zinc from cntions of nnnlYtic groups 11 Pnd III Using
anionites. *Ilav.lnb. 24 no.4:387-389 '58. (MIRA 11:4)
1. Loningrndakiy gooWnretvanny'y universitat im, A.A;* Zhdnnovn.
(Anions) (Zinc-Annlysta)

MORACHIVSKIY. YuiV.: ZVMVA. M.N.; KUZMCTSOVA, A.Ab~
Separating phosphate-ion from certain cations by means of
anion-exchanging substances. Zavalab. 22 no#10:1170-1171 '56.
(MLU 10:5)
Lleningradskijr gosudarstvannyy universitet4
(.Ions) (Phosphates)

XORACIWSKIT, Yu.V.; ZVEUVAO M.N.; ROINOVICH, R.Sh.
Now
Separation of lead from barium 'by means of anion-cichanging sub-
stances. Zav.lab. 22 no-5:541-543 036. (XLRL 0:8Y
1. Leningradskly goffudaretvannyy universitat.:
(Anions) (Barium) (Lead)

AUTHORS: Zvereva, Lf. N., Shibarov, V. N. 307/54- 59- t:-21- /25
TITLE: Separation of Zinc, Lead, and Copper:on an.Anion Exchange Resin
(Razdeleniye tainka, svintsa i medi na anionite)
PERIODICAL: Vestnik Leningradskogo universiteta. Seriya fiziki i khi'-~Iii'
1959, Nr 1, pp 145-148 (USSR)
ABSTRICT: It was the aim of this paper to find the conditions of the
separation of zinc from copper and lead by,means of the ion ex-
change method. Similar separations with different ion,exohangere
from the papers (Refs 1-5) are given. The.ion exchangers of the
type EDE-10, PE-9, and EDE-10-11P" viere used for the separation
of zinc from lead and copper. In a preliminary investigation it
was found that the ion exchangers EDE'10-11P" and PE-q~are better
suited for the separation. The quantitative Bepara-clon of. copper,
zinc, and lead was carried out as folloyrS.i ' 30 - 50 MI* Solution
was caused to flow through the Cl" ion exchanger, copper~vas
found partly in the filtrate., The residue wh:Lch remained in the
column was washed out with 80 ml 2 n MCI. Thp zinc was) then
washed out with 150 ml 0. 3 n HC1, and:; the lead which trao clef t in
the column was washed out with 200 ml water. The experimental
Card 1/2 results are given in table 11. The method is simpler if there are.

007/54-59-1-27/25
Separation of Zinc, Lead, and Copper an an Anion Er~hang~- Resin
only 2 components, e.g. lead and copper. Copper*i.9 washed out
with 2 n HC1 and zinc with water (experimental resultb of 4
samples in table 2).A separation of -vOry an'tall quantitios of
radioactive zinc froin greater quantities of copper and le'ad was
carried out as well by means of the above mentioned method
(Table 3), and good results were obtained.~Theauthors thank
professor Yu. V. Morachevskiy for valuable advice given for the
work under review. There are 1 figure, 3 tables, and 5 ref-
erences, 2 of which are Soviet.
SUBMITTED: October 26, 1957
Card 2/2
I Fin; Nih-0 ii PH;
dim q! i:t:1 1, 1 1! i

of Lrom fiarf VT-W Witt
X IT

AUTHOR: Zvereval Y.N. 32-24-4.-V67
TITLE: The Separation of Zinc and the Catiorm of. the 11. and III
Aralytical Groups by the Aid of AnioniteB (Otdelenive ts:Wca 0t
kationov 11 i III wali tic' heskikh grupp a powr3hohlyu =ionitov)
PERIODICAL: Zavoiskaya Laboratoriya, 1958, Vo2. 2J~, Ur 4,:PP- 367-389 (USSR)
ABSTRACT: Kraus and Moore (Ref already establiahtd the fact thatzina is
completely absorbed on the anionite "dalleiks-111. in the pretence of
2-1 hydrochloric acid, whereas in this wee tht- cations of, them III.
analytical group are absorbed in ve.-y smll quan~.ities or not. at
all. Kraus, Nelson and Smith (Ref 2) point to the fact that
daueks-1 does not absorb alkaline-earth jelemento , and theL B&MC VMS
found by Jentzsch and Froischer (Ref 3) In the case of the anionite
vofatit L-150 and calciin or magneii-im. 34-iller' and Hunter (Ref 4)
a,s zell as Amin and Farah (Ref 5) used anIerlite IRA-400 in chlorc-
form for the separation of zinc. Jenf zsch and Pawlik (Ref: 6)
showed tbat a maximum absorption 3f zind taken place in vof&tLt
L-150 in a 4_6n hyaroohiox-lc acid soluti.on. IrA a -previo-,~s vmrk
Card 1/2 (Ref 7) a method of separating zinc and nickel on the anionites

The Separation of Zinc and the Gations of the.II. 32-24-4-'2/6~
and III. Analytical Groups by the Aid of Anionites
FE-9,, PEK -aid TM was described. As the xe~ult o! ra number of e:F_
periment3 carried oi~t un,]Ier the aupcmisi(k~~ of Yu..V.Mor,%ohPvak1,
in which the ariioniteuPE-9, 'E'DE-10 and .4 M12-1.0-P of M.4sslan
origin were med, a proce,33 of analysin ~for the deterw-biatim
mertioned in the title J.9 described. In a.'Oolum, (I r= 0) v.1-W the
anionile EDE-10. P~ in chloreform., z4--to arA all catlo=i are ab_
sofaed from the test soltticnx contuaining rinc and the aitiona of
the IL and III. group. The cations a;m then washed azt with 2r.
hydrochloric acid, arA hereafter zino ixi eytracted with water. In
this manner it -4:s posr.:*Ible to sepamte oe-3-ci--ims rragneaim, and
other a.,Jmline-earth metalls f rom zinc in the rat-io Zn:MO-.-_1 0. 10 to
10: 1 , as well as iron, alumintim, chromdum., obba-1A, mz_lg;wnes e, and
nickel -Zn:Merl:l and Zn:A1:Cr-_-1:100G0:iOCOO to 1:100C00:1000004
Zinc was determined comple--tometrisally and in the last ;ase colori-
metz-1cally. Tabulated da+,a of the ~:esults Cotairied are giver..' There
are 6 tables, and 7 references, I of wlil&., is Soviet.
ASSOCIATION: Leningmdskly gosudarstvervW univerpitet im.A.A.Zhdanova,
(Leningrad State Urivemity inieni A.A.Zhrliziov) Z
1. Zinc--Separation 2. Zinc--Abuorption Tons--Gliemical effects
4. Alkaline earth metals--Separation
Card 2/2

ftL-STOLYAROV, K.P., red.; FEGER, D.P.,
red. izd-va; BELOGUROVA, I.A.p tekhn. red.
(Use of ion exchangers in analytical ahemistry] Prime'nenie
ionitov v analiticheskoi khi~ii; stenogramma. loktsii: prochitan-
noi Y LDNTP na kratko-orochnom seminare po met.0dam Udmicheakogo
analiza. Leningrad, Leningr. dom nauohno-tekhn. propagandy,
1963. 18 p. (KRA 16:6)
(Ion exchangers) (Chemistry, Analytical)

ZVMVA, M. V.
Recognition of properties through different modes of perception
[with summRry In Nnglish], Vap-,Paikhol. 4 no �318?48 MY-Je 158
(MIRA 11:8).
1. Institut teorii i istorii padagogiki APH MrSR, Moskva.
(PPAGEPTION)

BjDNIV)V, P. TRIMATSM S. I ZVIMVA, N.
Letter to the editors. Ognsupdry 22 no.3tl39-140 157*
(Refractory materials) (Nonferrous metajs--Ket~611urgr)

ZVERZVA, M.N.
Role of Russian physicians in the development of.the Method of sub-
cutaneous injections. Test. vener., Moskva no. 509-51, Sept-Oct 1952.~
(GIML 23:3)
1. Clinical Departmental Physician. 2. Of the Republic Skin-Vener-
eological Institute RMR (Acting Director - A. A. Kotdratlyeva),

ZVEREVAS N.A.; KALININAp V.A.
High temperature oil sterilizer* Med.prom, 16 no,4149 AP 162
(MIM 15:
1. Nauahno-losledovateliskiy institut eksperimentallnoy khirurgi-
ches~qy apparatury i instrumentov.
(STERILIZATION-EQUIPMENT AffD SUPPLIES)

kIlLIMMI, OROSHIN N.
_qj As AO
New method of producing 1,6-hexametkvlene-bis-(dlmethylamine).
Hed.prom. 13 no.7:46-49 Jl '59. (KM 12:10)
1. Leninegradoldy nanahno-i-saledovatellskiy inWtut antibiotikov.
I khimiko-farmatsevtichaskiy savod "Farmakon".
(DIIGTHYLAXIIIA)

GLADILIN, A.A.; GLUKHOT, D.S.; YWHIN, LAPIN, K.W."
WONOTA, A.S.; MARTYX07, U.K.; OHMM, MO.; KMALICHIKOV,
?.I.; POLYACHKIII, H.A.,red.; ASTMOV, V.P., tekbno rn4.
[Economy of Penza Province-, a statiatical collectionilffarodnoe
khoziaistvo Penzenskoi obloati; statisticheskii sborn1k. Penza,
1958. 190 P, (MIRA 11:11)
1. Penzennkaya oblast' . Statistiehealcoya iipravlsnijys.(f or all except
Hikhallchikov an~ Antonov),
~Peaza Province-statistics)

V03KRESENSKAYAP N.T.; _ZVII.Ej' LA,
Spectrochem1cal determination of gold in silicate riocks and
minerals. Zhur. anal. kh:Lm. 20 no.12sl288-1298 165.
JMIRA 18t12)
Is f/oskovskiy gosudaretvennyy universitet imeni M.Y. Low-anosova.
SuInItted May 15, 1964o

VOSKRESENSKAYA, N.T.; ZVEMA,_!L-F:l -11.
_YM", A
Geochemistry of copper in the Devonian and Carbonif6rouS
effusives of Karkalinsk District (central Kaza'khstan).
Vest.Mosk.un.Ser./+tGeol. 20 no.5:57-61 s-o 165.
(MIRA Mill)
1. Kafedra geokhimii Moskovskogo gosudarstvenn6go universiteta.
imp-moil! MIN 111EHI J,11111-1i, i

777777-7177--
CHISTYAKOV, A.D.; BTJRKGVA, 14.V. ORLOVA, Ye.Ml.; GIA7,OVA;, O*Rs~;
FED -p D.A.; M-MiJID M.Ye.- ABRAMQVICHo KA.!j PoFdVA,
T.P.; MAIVZYVI~ L.T.; BACHITRINA, A.A.; LEMMA, N,114';
PESKOV, B.Ye.; ROMOV9 VOIEVAKHAN.MO-10HUKO~
1,G.; PETRENKO.. 1.1 IT. J.V.. P11JUS.
SMETERV S.M. .11,102.AlEVA-, T.F. -MINNA,; L.,S f3E. Ll~%~YA
natichn. f6d
ILN4t nauctm, red.;
KURGAIISKAYA V,ki,, nalachn. red.,- I-ERTSALOVAi A.N..,nauchn.
red.; TOMMITA'TCH, L.V.,, nauch-~. red.; SAGATUSKM N.V...
otv. red.~ ROTIKOVSKAYA, A.B., red,
(Flanual o~' shor'll-range weather for,~: -3 t' ing
~'Ukowvlstvo
po knit~-x:rochrjym prognozam pogoa.v, Lelling"171111, Gidro-
meteol,-,dat. Pt 2. 17d.2. !965. at 1 j) 4
(~UHA 16;
1. Moscow. MentralliWy institut prognozorv.~

3/136/62/000/0()l/OOT/009
AQ51/Al26
AUIHORS. Krivunchenko, N.G.; Kolkhir, K.F.; 4vereva, N.I.j Dmitriyeva,
Ye.V.; Drugovskaya, M.N., Sokolov, S.A.
TITLE% The use of gas-producing resins in rubber rea:laimihS
PERIODICAL: Kauchuk i rezina, no. 1, 1962, 52 - 53
TEXTt The disadvantages of dry-distillation of pine tars, for use as
softeners in rubber reclaiming are non-uniformity and high cost. In the attempt
to find new resins for this purpose, gas-producing ones proved to be the most
successful. The Chekhov Rubber Reclaiming Plant developed the composition of a
resin and a technology of rubber reclaiming, using the product of the Izhevsk
Plant In 1958. This product has the following advantagesu 1) Uniformity in
group composition of the softener, leading to improved physico-mochanical prop-
erties of the reclaimed rubbers. 2) Reduced production cost of the reclaimed
rubber. 3) Increased capacity output of the refining rollers. 4) Increased ca-
pacity output of the autoclaves due to a shorter rubber devulcanization process.
5) Improved receiving and storage methods of the resin, eiliminating the use of
wooden barrels. The Chekhov Recovery Plant produced 6.5 thousand tons of re-
Card 1/2

SA38/6p,/boo/ooi/007/Oo9
The use of ga-c-producing resins in rubber reclaiming A051/A126
claimed rubber In 1959. In 1960, the Recovery Plant consumed 21000 tons of.res-
in. There is 1 table.
ASSOCIATION4 Chekhovskly regeneratnyy zavcd (Chekhov Recovery Plant)
Card 2/2
t A. it F,
4~iiilt~."ILT~4?14q,~i:-,4fs~-.ikila;i~Nd. d It Vr, j
U.41 11U.111T.311fill IM IMINAMMIMMUH114, if; .11 1 i;I:i
jj

13 -1- 19 5 8 - Z - ZZA-9-
Translation from: Refe ativ yy zhurnal, Metallurgiya,:1958, Nr 1, p 12 JUSSR)
AUTHOR: Zvereva, N.P.
TITLE: Synthesizing Heat-resistant Materials fCaibides, Nitrides; Borides,
Silicides, and Sulfides of the Metals of Groups IV, V, and VI I -
(Sintez tugoplavkikh materialov Ckarbidy, nitridy, boridy, silits,idy,
sul 'fidy perekhodnykh metallov -7
PERIODICAL: V sb.: Fiz. -khim. osnovy keramiki. Moscow_ Promstroy-
izdat, 1956, pp 325-348
ABSTRACT: A survey is made of the properties of superduty refractory
materials with fusion temperatures of 2. 000i - 4.0,001, and of.
methods of synthesizing them. The carbides possess the highest
temperature range; then come the nitrides, bori~es, silicides, and
sulfides. A system is described for fashioning products out of super-
duty refractory materials, and data are included.on the chemical and
physical properties of individual superduty refractories. The Author
cites some of the characteristics of the tect-tnology of producLs niade
of TiC, UN, ZrB2 Mos, , and ThS,
Bibliography: 56 reierence;. S. G.
Card 1/1
1. Refractory materials-Properties 2. Refractdry materials-SY;nthesis
3. Refractory materials-Temperature effects 4. Refractory materials
-Characteristics

AUTHOR ZVEMVA h*F
~
TITLE in
an han Sulphids.
20~-2-25/67
_
(0 sullfidakh lantana Russian)
PERIODICAL Doklady Akademii Nauk SSSR9 135T9 Vol 113p Nr 29 pp 333-3349
(U.S.S.S.R.)
Received 7/1957 Reviewed 8/1957
ABSTRACT, Apart from the polysulphides (L&S2) Ouly lanthanum sulph.ide L
263
:
is known, of whio*nly oontradicting partioulars concerning m I-
ting point and exterior appearance ara.ave,ilable. The m6nosulphi-
de that can be presumed,from the analogy'vith zorium sulphid! was
,produced by the authoress from mettaio lanthanum and lanthanum ni-
ng &a a-,datjrial that in highly
trate. It might become interest i
l
heat resistant and fire-proof. irst the nitirate was chlorinated
. The produced lanthanum tri-bhloride was then sul-
by means of CC1
4
phorated in the current of the dry H
S.
The sulphonation product
,
2
corresponded with 25,4% content of sulphur to the formula L&03-
It formed a non-eintered, crystallIne, v4ormilion powdero'Roasting
La2S tablets at 1700-18000 in a vacuum changes the ori'inil'
a-
oolo
r into a dark grey one. Here the content of oulphus wao
lower (22#37%) which pFoblably corresponds to a'solid splution
of L&2S3-La3S4- When beating the L&253-tableto up to 20000 they
melt and evaporate. Black crystals of hexagonal stru6ture.re-
mained in a small quantity on the lid of the iessel. Thei.were
Card 1/2 considered as L&2Q283. LaS is obtained by reduction of L42S3

On Lanthanum Sulphids.
with mettallic lanthanum by means of "impregnation". Tft-Itirrous
crucible made from lanthanum sulphide La was melted at a tempera-
ture of 1250-1600 The reaction product was &,gold-coloured.mat-
ter with 19,7~ content of'sulphur. The X-ray ploture of the p'ow-
der with lines that only belong to the oube-phase ehowed an iso-
structure with CeS. It crastallized was a granting of the;aommon
salt type- 9 the m1orostructure of the LaS is two-phaset large
oval yellow grains of L&S carry a light grey zone of lantharioxy
sulphide on their.borders. LaS-piecea do~not malt in a vacuum at
a temperature of 21000.(6 citations from publications).
ASSOCIATION
PRESENTED BY CHERNYAYEVq I.I.p Member of the kcadtmy,.
SUBMITTED
AVAILABLE Library of Congress.
Card 2/2

-Z vR-v IV.
Is
I' -fill

an

ANDREYENKOi G.V.,- ZVERffAt N.Ya.
Effect of phtnyllin on the thromboplastic activity and conceAration
of thrombotropinand proconvertin in the blood of white rats.
Vop.med.khim.' 6 no.4:182-385 Jl-Ag 160. (141RA 14 -.3)
1.,Laboratory for tho Study of,Physiology and Biochemistry of Blood
Coagulationg Biolo ical Faculiy, MOSCOW State University.
WICOAGUIAWS)

ZVM,'VA, O.S.
K. Holdhaus' "Traces of the Glacial period in the animal king-
dom of Europe." Izv. Komi. fil. Geog. ob-va SSSR no,S.-90-92
163. (MIRA 17:6)

AUTHORs Zverevat 0. So
TITLEi On the Genetic Boundary in a River Valley and its Role in
Hydrobiology (0 genatichookom rubezhe vdoline reki 2yego
znachenii v gidrobiologii).
PERIODICAL: Doklady AN SSSR9 19579 Vol. 114, Nr 6, pp. 1311-1314 (USSR)
ABSTRACTs The history of development of the dra 'inage.area of rivers
during the Quaternary is not always,duly -taken into account
in hydrobiological investigations. But this historical factor
may in many respects determine the conditions of the,drainage
area on which, in the end, the preaerit organic world;of waters
depends. This kind of dependences were detarmined by the.'author
in the Vychegda-river on both sides of the boundary of the
first Postmaximum glaciation by a comparison of hydrobiological
material (refernoes 30). The section inve stigated is ab'out
400 km long. In the point in which the above-mentioned bound-
ary crosses the river (district of the villages Ust'-Kulom-
-Derevyansk) the morphology of the valley. and the river bed is
considerably changed. Above Uatt-Kuiom (figure 1) the valley
is very wide and boggy. On the right side of the river a group
of lakes, representing relies of glacier-waters, lies in the
Card 1/4 bogs. Here the Vychegda is populated by a fairly well

e,
On the Genetic Boundary in a River Valley and its Role in 20-114-L-6-48/54"
Hydrobiology.
developed plankton and manyfold benthos. Mollusks, oligo-
chaetae, larvae of Tendipedidae live in the mud at the
bottom. In the microbenthos nematods axe predominant.,The
biomass of the benthos amounts to 1-12 9/M~~. Animal life is
especially rich in the thicket of aquatic plants. In old arms
of lakes the amynt of zooplankton at,tains 9.000.000 indi-
viduals per 1 m water.50% of the species of mollusks and
leeches known from the entire Komi regionlive here. Many
waters in their nature here approach,the stage of eutropbic
ponds. Below the boundary of glaciation t~e living world:
changes under the influence of the hjydrographio conditions of
the valley. The valley becomes narrower, the river bed becomes
youngert from a predominantly accumulative valley it becomes
one of erosion. The mud and the aqua 'tic vegetation disappeart
at the bottom sand, gravel and in place marbles are predom-
inant. For a stretch the river almost flows without anyregion
of inundation. The river forms meanders through the entire
width of the valley, Many tips of meanders are cut into,1he
terrace of "' pine groves. Here the mineralization of the
water, increased in the previously described section, de-
Card 2/4 creases, ail the river is mainly dependent on surface feeding.

on the Genetic Boundary in a-River Valley and its Role in 20-114,;~0/54
Hydrobiology.
The interrupted connection with the side lakes causea a
reaction tending to acidity and leads to OL general d;~atrophy
of the water. At the bottom mainly coarse-detritus-like peat
muds are deposited..The living worlCis poor here..In the
plankton diatoms and dasmids as well;,as rotifers are pre-
dominant. In the benthos - small laxvae of Tandipedidaep
oligochaetae and nematoda. The benthoe-biomass amounts to
fractions of a gram per 1 m2. The.old arms are chiefly in-
habited by river species. Centers of higher biological pro-
ductivity may-form in some places due to the accumulation of
organic detritus. The chief factora;inhibiting the,deve,lopment
of life here are the processes of erosion and accumulation,
whereby the river bad is constantly 4isplaced. But tho'changed
chemism, especially the disturbed:mineral nutritiont remains
the decisive factor. The region of the Vychegda became'un-
saturated in its stand of species after the withdraiwal~of the
Scandinavian glacier in the region.:of its deposits~ whereas
the stand of species above the glacier-boundary is sufficiently
manyfold. The wide part above Ust'~Kulom may be considered-a
peculiAr.region of refuge in which many faunal elements of the
Card 3/4 inteiglacial period were preserveL It is.true that from here

On the Genetic Boundary in a River Valley and its eole in 20-11-4-6-48/,54
Hydrobiology.
many species also.spread farther down the river, but.there
they occur in other numerical relations and excl usively in-
habit the waters of the region of inundation.
There are 1 figure.and 4 references, 3 of which are Slavic.
ASSOCIATION: Komi Branch of the AS USSR (Komi-filial Akademii -nauk SS SR).
PRESENTED: March 19, 1957, by Ye. N.. Pavlovskiyp Member of the~Acadepw.
SUBMITTED: March -6, 1957

Card 4/4

USSR / Gonoral Bioloc5y*' Gonoral HydrobioloGy.
Abg Jour Rof Zhur Biol,, No 19, 1958v iTo 85694
Author zVorciva
Inst Yo-' '* '~4ivon
Titlo Tho Gonatic Boundary in tho Rivor Volloy and
Ito Si-nificanoo In Hydrobio,loGy,
U.
Orig Pub Dolil. AN SSSRj 1957) 114, No. 61 1311-1314.
Abstract Fro:1 1939-1950 a hydrobioloL'rical:~ study was con-
ductod in tho VychoCsda Rivor. anal, tho rocorvoirs
of Ito rivor valloy on a 806tor ono portloh or
which flows throuOili tho torritory of tho first
Poatnaximal glaciation, tho ~ othor bolnG situatod
hi,3hor in tho rivcr bod boypnd tho limits of
dopoolta from, tho Gilaoiation, BOth soctorst
Gonotically difforont, Pro alloarly distinsuishod
In mcrpholoGy, hydrobiology, and hydrochonistry,
Card 1/2

ZMEVA O*S.
.New larval form of Tendipedidae (Diptera) from the Pechora River.
Int.obos-36 no.1:231-232 157, (MLHA 10:4)
1. Komi filial Adademil nauk SSSR, Syktyvkar.
(Pechora River-Chironomiaae) (Lexvae.)

V
ZV.l-
Kildedli icon

mum, 00- S.

L
as of
arvae of T6ndipedidas (Chironomidas) of plains rivers of the
guropean part of northern U.S.S.R. Trudy Gldrdblol.O-ya 5:264-274 1~3.
(KLRL 70)
1. Komi filial Akadexii uauk SSSR. (Diptera) Maryan)

mp P"a 0. S GETSER, M.V,; IZ"YUROVA, V.K.
8yatem or relic lakon lit tho
Dokl. AN SSSR 155 no. 3:677-679 kr 164. (MIRA 170)
1. Predstavleno akademikom Te.N.Pavlovskim.

USSR/General and Specialized Zoology - Insects. P.
Abs Jour : Ref Zhur - Biol,, No 6, 1958, 35142
Author : Zvereva, O.S.
Inst :
Title : A New Form of Tendipedidao (Diptera) Larval from the
Itchora River.
Orig Pub Entomol, obozreniye, 1957, 36, No 1, 231-232,
Abstract A New species of larva kanevi of Genus Tendipedidae, was
described,
Card.1/1

jjo2jhjX LUI 2L P31gilga Agcggai2DA, Llbrar7 of Oom&e~s, Dedgmter 19524i' Uncliessif iod.
~ !i : :
- t : - , :

SEKOLTAR, T.T.; ZVIRMVA 3 A
Late results of dental fillings. Stomatologii& no-613-7 11-D '54.
(KLRA 8-1)
1. ris kafedry terapevtIcheekoy stocatologil LeningriAnkago
meditsinskogo stonatologicheakogo instituta.
(INTAYS
follow up)

34504
S/169/62/000/002/042/072
D228/D301:
AUTHOR: Zverevil.... S__V_.
TITLE: Atmospheric transparency in the Arctic
PERIODICAL: Referativnyy zhurnal, Geofizika, no, 2, 1962, 29, ab.-
stract 2B225 (Tr. Arkt. I Antarkt. n.-i. in-ta, 229,
1961, 90-116)
TEXT: The atmosphere's transparency was ddt ermined from the data
of direct solar radiation measurements at eight polar statione, lo-
cated cn the territory from 69 to 800N and from 53 to 1790B an*d
having the longest series of observations (from 5 to 17 years),
and also from the data of drift-station observations. Many ofthe
direct solar radiation observations, made at different ele-vations
of the sung were processed by the graphical method of averaging.
The resulting mean-monthly values of the atmosph,eric transparency
coefficients are highest (0.816) In the winter months and lowest
(0.783) in the summer months, The yearly variation of the transpa-
rency for Arctic stations is analogous to that for more southerly
Card 1/3

B/16,9/62/000/002/042/072
Atmospheric transparency D228/D302
stations (Pavlovsk, Saratov, Karadag). The small range of the
transparency coefficient's yearly variation at Arctic stations in
comparison.with those outside the Arctic is explained both by the
decreased amplitude of the yearly variation of the water-vapor
content at the arctic stations and by the influence of condensa-
tional turbidity on the transparency coefficient. At the drifting
stations the transparency coefficients are somewhat smaller th,~,q
those at the polar stations (0.762 - 0.800).,No dependence of,the
atmospheric transparency on the geographic position of the;oboer-
vation point is observed in the cold half of the year; this rela-
tionship does occur in the warm half of the year, The transparency
increases with the increase of latitude to approximately 800H, but
it somewhat decreases in the area of drifting stations. A certain
decrease in the mean-yearly values of the transparency coefficient
in an esterly direction to noted in the zonal distributionjor Ar,,,-.
tic stations. The average value of the maximum transparency coef-
ficients at polar stations equals 0.830. As the mean transparency
coefficients obtained for a number of Arctip, stations differ little
between themselves, it is possible to use them for the characteri-
Card 2/3

B/169/62/000/002/042/072
Atmospheric transparency o4a D228/D301
stic of the average atmospheric transparency in different areas of
the Arctic. Z-Abetracterle.note: Complete translation.-7
Card 3/3

II.UTHOR:
TITLE
Zvereva, S. V.....
New integral atmospheric
S/169/62/000/006/062/0931
D228/D-304
eri ajC 8
tiransparency charact
'2141'IRIODICAL: Roferativnyy zhurnal, Geofizika~ no. 6, 1962, 27, ab-
stract 6B191 (V sb.,Aktinometriya.i atmosfern. optika,
L., G-Ldroneteoizdat, 1961, 168-171)
T--,'XT: A comparison is made of various new integ
gral atmospheric-
transparency characterislUics: The limiting transparency C;efficient.a
'Grooosed by Gullnitskiy (RZhGeofiz, no. 8, 19581 5847) and S. III.,
il..~zik (Me
r, toorol. i gidroligiya, inf sb. no. 5 1948) and Makhot-
kill's turbidity index (RZhGeofiz, no. 12, 1957: 10445~ with the
standard transparency coefficient, turbidity factor and C coeffi-
cient in Kastrov's formula. The comparison was made in two direc-
u -L
tions: 1) kccordin-rt, to z1he stability of each quantity's numerical
values when the atmosphere's mass changes, and the transparency is
fixed; 2) according to the range over which each of the transparency
-characteristics varies. The solar-radiation intensity averages, at'
Card 1.12

3/169/62/000/000'-1/062/093
i~ew in-wural atmospheric ... D228/ '304
th,e time of different masses and a variable degree'of atmospheric
transparency were used in zhe calculation, these values being ob-
ta-Lsned from the observations of Kalitin and Sivkov. KastrovIi; C'co-
and Mla'.Khotkinls turbidity index, and-then the turbidity
factor, are the most. sensitive to atmospheric 'trans .parency changes;
they are als,o the most stable in respect al' 'the change in the atmo-
spherelz mass. The limiting transparency coefficients have no ad-
o
vantages whatsoever over the other characteristics under condidera-
tilon. ~_Abstracterls note: Complete translation.
Gard 2/2

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L1111-17VIG., Yo R. it. A Z1,1101A T.M,, CA'e M' -,
I-ELMEV S.S.
Polv-merization of tetrahydroftirml ATI the y)rn,,,onr~ of antlvno~y
rentachlorlde and it.9 commpo=18. Vyookom. roud. 17 k1c).Q.,269-2174,
F 165. ("Alrd, Vi:3)
1. Fiziko-khimicheskiy institut imorli i Donetskiy
filial instituta khimicheskildi reektivcv I onobc c"histykh veahchestv.

LONGINOV# M.F.; ZVEREVA, V.A.
Preparation of thin plates for the studfof metals by meano'of
4 trausmission electron microscope. Zav.!~b. 21 no.5:559-561
161. (MIRA:14:5)
1. Chelyabinskly nauchno-issledovatellskiy~inati,tut metallurgii.
(Metallography)
(zlectron microscopy)

2h 358
3/032/61/027/005/004/017
5~S !) 0 B 11 9/B2 15.
AUTHORS: Longinov, M. F. and Zvereva, V. Ad
TITLE: Manufacture of thin foils for the e~.amination of metals
under a transmission electron microscope,
PERIODICAL: Zavodskaya laboratoriya, v. 27, no. la6l, 559-561
5,
TEXT: The authors have elaborated a new method of~manufacturing very thin
metal foils (thickness: 100 to 200 A) in which the structure of the mas-
sive initial sample is preserved. The foil is gradually reduced by'alec-
trolysis. During this process a layer of foreign metal is applied to one
side of the fail to ensure a constant and uniform current density'on the
surface of the foil and, thus, eliminate orrore caused by,irtegular reduc-
tion. The method was applied to carbon, structural, stainlesso and tranfl-
former steels. The foils obtained were examined under tbe)[1-3 (EM-3) electron
microscope. The foil is prepared as follows:A4C~20X? aim piece of the metal
to be studied is mechanically or chemically reducea to a thickness of
0.20 to 0.15 mm and then further reduced to 0.05 to 0.03 mm by electro-
Card 1/2

2hl
S/03Y61/05287/005/004/017
Manufacture of thin ... B119 B215
lytic polishing (for steels: an acetic acid chromium electrolyte is used
at 1.5 to 2-5 A). After washing in water and dryingt one'side of the fo il
isceated with a foreign metal by electrolysis or vacuum evaporationo When
choosing the metal, one has to consider thatthe latter can be chemically
removed without damaging the foil. For chromium anUchromium-nickel:.steels,
the authors used zinc or copper. A zinc layer has to be protected against
dissolution in the electrolyte by a thin paraffin layer. Under the,abovo
condit-ions the foil is then electrolytically reducea, on the bare side un-
til the foreign metal appears. For removing zinc a hot aqueous NaOH~solu-
tion is used, and for copper an aqueous or alcoholic JINO solution.2here
are 3 figures and 5 references: 4 Soviet-bloc and I non-Soviet-bloo.
ASSOCIATION: Chelyabinskiy nauchno-issledovatellskiy institut metallurgii
(Chelyabinsk Scientific Research Institute of Metallurgy)

ZVEREVA, Y.A.;.NIKOLISKIY, Yu.V., inzh.; SAYTANID1, L.D., teldm.red,
(Improvement of swamps and-mineral swampy soils; bibliography]
Meliorateiia bolot i minerallnykh zabolocheinnykh zemell; biblio-
graficheskii ukazatell. Koakva. Izd-vo 14-vn sell.khoz.RSFSR* ~
Pt.l. 1959. 1)0 p. Pt.2. 1959. 155 p, (HIRA~12:12)
1. Moscow. Gosudarstvannaya Inauchnnys bibliotaka. 2, Gosudarst-
vemuiya nauchnaya biblioteka (for Zvereva). ). Respublikenskiy .
gosudarstvennyy institut po proyektirovaniyu vodnkhozyaystvennogo
i meliorativnogo stroitelistva 1'Rosg1provoakhoz*,(.for Nikollakly).
(Bibliography-Drainago)
(Bibliograpby-Swamps)

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J.P.,kandidat tekhnichaskikh nauk.
Technique for determining the composition of protective oiide~
films resulting from electrochemical oxiae c6atir4 of steelvarei
.Trudy MVTU n0-36:62-66 '55. (HLRA 9-9)
(Oxidation, Slactrolytic)

z V-P,A V
',~rke, FleGtroplat.,ni and Metal Finishine
CLI E!;y V.
Sept. 1948, p. 591-592; Oct. 1948, p. 667-B68, 674.
ranslated from Zavodskaya

NINDLATEV, V.G.;
Ye.T.; ZIMINA, K.I.; POPOVAp memo
~500
Isolation of individual normal paraffin hydrocarbons from the, 200-3
fraction an obtained from Romashkin Devonian petroleum. Khim.i~tekh.
tol-no-3:11-17 Mr 156. (MMA 9:9).
(Hydrocarbons)

Let's prsi~re for tba.40th-emmyormary, of the Great October Ao'clallst
Revolution In the proper mnner. Blot. agitl~ vod. transp, no,6:3p.44
(ML~A- 10:4)
1. Agitator teplokhoda Oftrkmeuistan" raspiyokogo parokhodstva.
(Merchant warina')

z YER'Ev V, YA.
11/5
2 3 05
Artilleriy.--kaya insbriurental Maja Ra,.,vedka', Uchebnik Dlya' Ai-t~lloriyskAl%h'bcl,-~i.lishcl,.
(Artillery Reconnaisnace I ry) D.A PeIrgin, V. VA. ZU.1-W I V. IN. DA"IMN Yo.-.qkva,
Voyenizdat, 1956.
h83 p. illus., Dit,.C-rs.., Tables.
Bibliography: P. h78.

lyl, ~ vi
=
.V. Yu. T.
-----------
"Ohat the eagineer and repAIrman, chould read on boiler repair.
F,nergetik no.6:40 Je 05?. 10:7)
(I$ibliography-.Doilerfl-.':ointennn,.,o and.repair)

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ZORMSHCHIKOV, P.A., prof.; OBRAZTSOV, V.L*, assintent; ZVURNVA, M.Li
assisteat.
Results of vitaminizing pregnant cows and newborn,calves on the
OTrinaateat' let oktiabriam Collective Farm. Zhivotnovodetvo 19
no.12-68-70 D 157. (MIRA 10:12)
l.Troitakiy sooveterinarn inatitut,
(Calvels (Vitamins)

15-757-4,-4276
Translation from: Referativnyy zhurnal, Geologiya, 1957 Nr 4ffl~
p 33 (USSR)
AUTHOR: Zverevap 0# so
TITLE: Hydrographic Features of the Komi ASSR, and Their
Relation to its Quaternary History (Nek otoryye.osoben-
nosti gidrograficheskoy seti territoril Komi ASSR,v
svyazi s yeye chetvartichnoy is~oriyey)
PERIODICAL: Izv. Komi fil. Vses. georg. o-va, 1955, Nr 3, pp 11-16
APSTRACT: Bibliographic entry
Card 1/1

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USSR/Chemical Technology. Chemical Products and Their Application Food Industry,
1-28
Abst Journal; Referat Zhur - Khimiya, No 21 1957, 6585
Author: Zvereva, T. A.
Institution: None
Title: Study of the Suitability of Canker-Resistarit Varieties of Potatoes
for Drying
Original
Publication: Sad i ogorod, 1953, No 91 55-56
Abstract: No abstract

BCROWLINA, F.Z. WLOBATBVA, L*G,; ZVMWA, T,A*
Determination, of photosynthesis under f iald conditions. Trtdy Inst.
fiziol.rast. 10:250-256 155. A,: 9)
1. Kaf edra f lziologli rastenly HoskDvakogo goirAmrstvannogo univervitata
imeni M.V. Lomonosova. (Photosynthesis)

ZVEREVA, T.A.; TEPPER. R.Ya.; OGN.",A, R.I.
Preparing potatoes for drying. Kona. I ov. from. 13 no.4: 13,14
Ap 158, (HIM ll:'4)
1. TSentralInaya proizvodetvennoya laboratoriya pri Moskovskom
2avode pishchevykh konteentratov lfo.L
(Potatoes--Drying)

xAZImIRSKIY, Ta.M., starshiy nauchnyy ootrudaik; ZVEREVA, T.A,', starshik
nav,chnyy sotrudnlk; GRANOVSUTA, R.Ta. , mUdisfil-7 -natibEi~yy sotrWnik;
FrATIGORSKATA, T.Is, starehiy nauchny7 eotrudnik
Tachnical and economic offectivonoso of the stonm-beAting, and.,
mechanical methoda of preparing potatoeo for #ying.: Trudy VMXKOP
no.9:26-52 t59. (MIRA 14-I)i
(Pbtatoes-Rrying)

i
SOURCE: Ref. eh. Elektronlka I yeye primeneniyer Abs. 8A85
AUTHOR: Aleksand-vov, L. M.1 Mironoy, 9. M.1 Zvereva, T. 114
TITLE-. Investigation of tungsten rearystalUzation U quick eteotria heating
CITED SOURCE: Uch. zap. KbrdovsA un-t, vypo 56, 1964, 5~-,57
TOPIC TAGS: tungsten filament, tungsten, metal recrystallftAtio#, tainsile atr6r4;th,
annealing
TRANSLATION: Prior to annealing, the speciMns were aleaAdd by boiling in a 205~
solution of HaOH for 10 recrystallization process was studied by the
variation of the ultimatns;x Pth at room temperature with the annealing temperature
6 S termined on a FUE:9 iestin
and time.The ultimat -tre t as de _5~tensjle Mach 0. v')
For an annealing time of ',kO adLn, the final Fi~u-ii~-was
TCj and for 200 sea, 16DOC. Pmm the aboTe data,
about i45OC; for 10 min, almost 15,
a curve of pr imary-recrystalliration--acMIat Ion time vs. amneal3M, temperature roras
plotted. A metallographia method corroborated Ute fact that the, rec*stallisatlon
goes quicker with higher rates of heating. Bib 4.

ZVEREVA, T.S.
Foms of clayey fomations and'highly dispenod mJjierals in
turf-carbonaceous soils. Pochvovedenie no.11a,U-" 11 164
(MA 18:1)

ZVEMVA M. if.
Sipara-tion of zinc from cntions of nnnlYtic groups 11 Pnd III Using
anionites. *Ilav.lnb. 24 no.4:387-389 '58. (MIRA 11:4)
1. Loningrndakiy gooWnretvanny'y universitat im, A.A;* Zhdnnovn.
(Anions) (Zinc-Annlysta)

MORACHIVSKIY. YuiV.: ZVMVA. M.N.; KUZMCTSOVA, A.Ab~
Separating phosphate-ion from certain cations by means of
anion-exchanging substances. Zavalab. 22 no#10:1170-1171 '56.
(MLU 10:5)
Lleningradskijr gosudarstvannyy universitet4
(.Ions) (Phosphates)

XORACIWSKIT, Yu.V.; ZVEUVAO M.N.; ROINOVICH, R.Sh.
Now
Separation of lead from barium 'by means of anion-cichanging sub-
stances. Zav.lab. 22 no-5:541-543 036. (XLRL 0:8Y
1. Leningradskly goffudaretvannyy universitat.:
(Anions) (Barium) (Lead)

AUTHORS: Zvereva, Lf. N., Shibarov, V. N. 307/54- 59- t:-21- /25
TITLE: Separation of Zinc, Lead, and Copper:on an.Anion Exchange Resin
(Razdeleniye tainka, svintsa i medi na anionite)
PERIODICAL: Vestnik Leningradskogo universiteta. Seriya fiziki i khi'-~Iii'
1959, Nr 1, pp 145-148 (USSR)
ABSTRICT: It was the aim of this paper to find the conditions of the
separation of zinc from copper and lead by,means of the ion ex-
change method. Similar separations with different ion,exohangere
from the papers (Refs 1-5) are given. The.ion exchangers of the
type EDE-10, PE-9, and EDE-10-11P" viere used for the separation
of zinc from lead and copper. In a preliminary investigation it
was found that the ion exchangers EDE'10-11P" and PE-q~are better
suited for the separation. The quantitative Bepara-clon of. copper,
zinc, and lead was carried out as folloyrS.i ' 30 - 50 MI* Solution
was caused to flow through the Cl" ion exchanger, copper~vas
found partly in the filtrate., The residue wh:Lch remained in the
column was washed out with 80 ml 2 n MCI. Thp zinc was) then
washed out with 150 ml 0. 3 n HC1, and:; the lead which trao clef t in
the column was washed out with 200 ml water. The experimental
Card 1/2 results are given in table 11. The method is simpler if there are.

007/54-59-1-27/25
Separation of Zinc, Lead, and Copper an an Anion Er~hang~- Resin
only 2 components, e.g. lead and copper. Copper*i.9 washed out
with 2 n HC1 and zinc with water (experimental resultb of 4
samples in table 2).A separation of -vOry an'tall quantitios of
radioactive zinc froin greater quantities of copper and le'ad was
carried out as well by means of the above mentioned method
(Table 3), and good results were obtained.~Theauthors thank
professor Yu. V. Morachevskiy for valuable advice given for the
work under review. There are 1 figure, 3 tables, and 5 ref-
erences, 2 of which are Soviet.
SUBMITTED: October 26, 1957
Card 2/2
I Fin; Nih-0 ii PH;
dim q! i:t:1 1, 1 1! i

of Lrom fiarf VT-W Witt
X IT

AUTHOR: Zvereval Y.N. 32-24-4.-V67
TITLE: The Separation of Zinc and the Catiorm of. the 11. and III
Aralytical Groups by the Aid of AnioniteB (Otdelenive ts:Wca 0t
kationov 11 i III wali tic' heskikh grupp a powr3hohlyu =ionitov)
PERIODICAL: Zavoiskaya Laboratoriya, 1958, Vo2. 2J~, Ur 4,:PP- 367-389 (USSR)
ABSTRACT: Kraus and Moore (Ref already establiahtd the fact thatzina is
completely absorbed on the anionite "dalleiks-111. in the pretence of
2-1 hydrochloric acid, whereas in this wee tht- cations of, them III.
analytical group are absorbed in ve.-y smll quan~.ities or not. at
all. Kraus, Nelson and Smith (Ref 2) point to the fact that
daueks-1 does not absorb alkaline-earth jelemento , and theL B&MC VMS
found by Jentzsch and Froischer (Ref 3) In the case of the anionite
vofatit L-150 and calciin or magneii-im. 34-iller' and Hunter (Ref 4)
a,s zell as Amin and Farah (Ref 5) used anIerlite IRA-400 in chlorc-
form for the separation of zinc. Jenf zsch and Pawlik (Ref: 6)
showed tbat a maximum absorption 3f zind taken place in vof&tLt
L-150 in a 4_6n hyaroohiox-lc acid soluti.on. IrA a -previo-,~s vmrk
Card 1/2 (Ref 7) a method of separating zinc and nickel on the anionites

The Separation of Zinc and the Gations of the.II. 32-24-4-'2/6~
and III. Analytical Groups by the Aid of Anionites
FE-9,, PEK -aid TM was described. As the xe~ult o! ra number of e:F_
periment3 carried oi~t un,]Ier the aupcmisi(k~~ of Yu..V.Mor,%ohPvak1,
in which the ariioniteuPE-9, 'E'DE-10 and .4 M12-1.0-P of M.4sslan
origin were med, a proce,33 of analysin ~for the deterw-biatim
mertioned in the title J.9 described. In a.'Oolum, (I r= 0) v.1-W the
anionile EDE-10. P~ in chloreform., z4--to arA all catlo=i are ab_
sofaed from the test soltticnx contuaining rinc and the aitiona of
the IL and III. group. The cations a;m then washed azt with 2r.
hydrochloric acid, arA hereafter zino ixi eytracted with water. In
this manner it -4:s posr.:*Ible to sepamte oe-3-ci--ims rragneaim, and
other a.,Jmline-earth metalls f rom zinc in the rat-io Zn:MO-.-_1 0. 10 to
10: 1 , as well as iron, alumintim, chromdum., obba-1A, mz_lg;wnes e, and
nickel -Zn:Merl:l and Zn:A1:Cr-_-1:100G0:iOCOO to 1:100C00:1000004
Zinc was determined comple--tometrisally and in the last ;ase colori-
metz-1cally. Tabulated da+,a of the ~:esults Cotairied are giver..' There
are 6 tables, and 7 references, I of wlil&., is Soviet.
ASSOCIATION: Leningmdskly gosudarstvervW univerpitet im.A.A.Zhdanova,
(Leningrad State Urivemity inieni A.A.Zhrliziov) Z
1. Zinc--Separation 2. Zinc--Abuorption Tons--Gliemical effects
4. Alkaline earth metals--Separation
Card 2/2

ftL-STOLYAROV, K.P., red.; FEGER, D.P.,
red. izd-va; BELOGUROVA, I.A.p tekhn. red.
(Use of ion exchangers in analytical ahemistry] Prime'nenie
ionitov v analiticheskoi khi~ii; stenogramma. loktsii: prochitan-
noi Y LDNTP na kratko-orochnom seminare po met.0dam Udmicheakogo
analiza. Leningrad, Leningr. dom nauohno-tekhn. propagandy,
1963. 18 p. (KRA 16:6)
(Ion exchangers) (Chemistry, Analytical)

ZVMVA, M. V.
Recognition of properties through different modes of perception
[with summRry In Nnglish], Vap-,Paikhol. 4 no �318?48 MY-Je 158
(MIRA 11:8).
1. Institut teorii i istorii padagogiki APH MrSR, Moskva.
(PPAGEPTION)

BjDNIV)V, P. TRIMATSM S. I ZVIMVA, N.
Letter to the editors. Ognsupdry 22 no.3tl39-140 157*
(Refractory materials) (Nonferrous metajs--Ket~611urgr)

ZVERZVA, M.N.
Role of Russian physicians in the development of.the Method of sub-
cutaneous injections. Test. vener., Moskva no. 509-51, Sept-Oct 1952.~
(GIML 23:3)
1. Clinical Departmental Physician. 2. Of the Republic Skin-Vener-
eological Institute RMR (Acting Director - A. A. Kotdratlyeva),

ZVEREVAS N.A.; KALININAp V.A.
High temperature oil sterilizer* Med.prom, 16 no,4149 AP 162
(MIM 15:
1. Nauahno-losledovateliskiy institut eksperimentallnoy khirurgi-
ches~qy apparatury i instrumentov.
(STERILIZATION-EQUIPMENT AffD SUPPLIES)

kIlLIMMI, OROSHIN N.
_qj As AO
New method of producing 1,6-hexametkvlene-bis-(dlmethylamine).
Hed.prom. 13 no.7:46-49 Jl '59. (KM 12:10)
1. Leninegradoldy nanahno-i-saledovatellskiy inWtut antibiotikov.
I khimiko-farmatsevtichaskiy savod "Farmakon".
(DIIGTHYLAXIIIA)

GLADILIN, A.A.; GLUKHOT, D.S.; YWHIN, LAPIN, K.W."
WONOTA, A.S.; MARTYX07, U.K.; OHMM, MO.; KMALICHIKOV,
?.I.; POLYACHKIII, H.A.,red.; ASTMOV, V.P., tekbno rn4.
[Economy of Penza Province-, a statiatical collectionilffarodnoe
khoziaistvo Penzenskoi obloati; statisticheskii sborn1k. Penza,
1958. 190 P, (MIRA 11:11)
1. Penzennkaya oblast' . Statistiehealcoya iipravlsnijys.(f or all except
Hikhallchikov an~ Antonov),
~Peaza Province-statistics)

V03KRESENSKAYAP N.T.; _ZVII.Ej' LA,
Spectrochem1cal determination of gold in silicate riocks and
minerals. Zhur. anal. kh:Lm. 20 no.12sl288-1298 165.
JMIRA 18t12)
Is f/oskovskiy gosudaretvennyy universitet imeni M.Y. Low-anosova.
SuInItted May 15, 1964o

VOSKRESENSKAYA, N.T.; ZVEMA,_!L-F:l -11.
_YM", A
Geochemistry of copper in the Devonian and Carbonif6rouS
effusives of Karkalinsk District (central Kaza'khstan).
Vest.Mosk.un.Ser./+tGeol. 20 no.5:57-61 s-o 165.
(MIRA Mill)
1. Kafedra geokhimii Moskovskogo gosudarstvenn6go universiteta.
imp-moil! MIN 111EHI J,11111-1i, i

777777-7177--
CHISTYAKOV, A.D.; BTJRKGVA, 14.V. ORLOVA, Ye.Ml.; GIA7,OVA;, O*Rs~;
FED -p D.A.; M-MiJID M.Ye.- ABRAMQVICHo KA.!j PoFdVA,
T.P.; MAIVZYVI~ L.T.; BACHITRINA, A.A.; LEMMA, N,114';
PESKOV, B.Ye.; ROMOV9 VOIEVAKHAN.MO-10HUKO~
1,G.; PETRENKO.. 1.1 IT. J.V.. P11JUS.
SMETERV S.M. .11,102.AlEVA-, T.F. -MINNA,; L.,S f3E. Ll~%~YA
natichn. f6d
ILN4t nauctm, red.;
KURGAIISKAYA V,ki,, nalachn. red.,- I-ERTSALOVAi A.N..,nauchn.
red.; TOMMITA'TCH, L.V.,, nauch-~. red.; SAGATUSKM N.V...
otv. red.~ ROTIKOVSKAYA, A.B., red,
(Flanual o~' shor'll-range weather for,~: -3 t' ing
~'Ukowvlstvo
po knit~-x:rochrjym prognozam pogoa.v, Lelling"171111, Gidro-
meteol,-,dat. Pt 2. 17d.2. !965. at 1 j) 4
(~UHA 16;
1. Moscow. MentralliWy institut prognozorv.~

3/136/62/000/0()l/OOT/009
AQ51/Al26
AUIHORS. Krivunchenko, N.G.; Kolkhir, K.F.; 4vereva, N.I.j Dmitriyeva,
Ye.V.; Drugovskaya, M.N., Sokolov, S.A.
TITLE% The use of gas-producing resins in rubber rea:laimihS
PERIODICAL: Kauchuk i rezina, no. 1, 1962, 52 - 53
TEXTt The disadvantages of dry-distillation of pine tars, for use as
softeners in rubber reclaiming are non-uniformity and high cost. In the attempt
to find new resins for this purpose, gas-producing ones proved to be the most
successful. The Chekhov Rubber Reclaiming Plant developed the composition of a
resin and a technology of rubber reclaiming, using the product of the Izhevsk
Plant In 1958. This product has the following advantagesu 1) Uniformity in
group composition of the softener, leading to improved physico-mochanical prop-
erties of the reclaimed rubbers. 2) Reduced production cost of the reclaimed
rubber. 3) Increased capacity output of the refining rollers. 4) Increased ca-
pacity output of the autoclaves due to a shorter rubber devulcanization process.
5) Improved receiving and storage methods of the resin, eiliminating the use of
wooden barrels. The Chekhov Recovery Plant produced 6.5 thousand tons of re-
Card 1/2

SA38/6p,/boo/ooi/007/Oo9
The use of ga-c-producing resins in rubber reclaiming A051/A126
claimed rubber In 1959. In 1960, the Recovery Plant consumed 21000 tons of.res-
in. There is 1 table.
ASSOCIATION4 Chekhovskly regeneratnyy zavcd (Chekhov Recovery Plant)
Card 2/2
t A. it F,
4~iiilt~."ILT~4?14q,~i:-,4fs~-.ikila;i~Nd. d It Vr, j
U.41 11U.111T.311fill IM IMINAMMIMMUH114, if; .11 1 i;I:i
jj

13 -1- 19 5 8 - Z - ZZA-9-
Translation from: Refe ativ yy zhurnal, Metallurgiya,:1958, Nr 1, p 12 JUSSR)
AUTHOR: Zvereva, N.P.
TITLE: Synthesizing Heat-resistant Materials fCaibides, Nitrides; Borides,
Silicides, and Sulfides of the Metals of Groups IV, V, and VI I -
(Sintez tugoplavkikh materialov Ckarbidy, nitridy, boridy, silits,idy,
sul 'fidy perekhodnykh metallov -7
PERIODICAL: V sb.: Fiz. -khim. osnovy keramiki. Moscow_ Promstroy-
izdat, 1956, pp 325-348
ABSTRACT: A survey is made of the properties of superduty refractory
materials with fusion temperatures of 2. 000i - 4.0,001, and of.
methods of synthesizing them. The carbides possess the highest
temperature range; then come the nitrides, bori~es, silicides, and
sulfides. A system is described for fashioning products out of super-
duty refractory materials, and data are included.on the chemical and
physical properties of individual superduty refractories. The Author
cites some of the characteristics of the tect-tnology of producLs niade
of TiC, UN, ZrB2 Mos, , and ThS,
Bibliography: 56 reierence;. S. G.
Card 1/1
1. Refractory materials-Properties 2. Refractdry materials-SY;nthesis
3. Refractory materials-Temperature effects 4. Refractory materials
-Characteristics

AUTHOR ZVEMVA h*F
~
TITLE in
an han Sulphids.
20~-2-25/67
_
(0 sullfidakh lantana Russian)
PERIODICAL Doklady Akademii Nauk SSSR9 135T9 Vol 113p Nr 29 pp 333-3349
(U.S.S.S.R.)
Received 7/1957 Reviewed 8/1957
ABSTRACT, Apart from the polysulphides (L&S2) Ouly lanthanum sulph.ide L
263
:
is known, of whio*nly oontradicting partioulars concerning m I-
ting point and exterior appearance ara.ave,ilable. The m6nosulphi-
de that can be presumed,from the analogy'vith zorium sulphid! was
,produced by the authoress from mettaio lanthanum and lanthanum ni-
ng &a a-,datjrial that in highly
trate. It might become interest i
l
heat resistant and fire-proof. irst the nitirate was chlorinated
. The produced lanthanum tri-bhloride was then sul-
by means of CC1
4
phorated in the current of the dry H
S.
The sulphonation product
,
2
corresponded with 25,4% content of sulphur to the formula L&03-
It formed a non-eintered, crystallIne, v4ormilion powdero'Roasting
La2S tablets at 1700-18000 in a vacuum changes the ori'inil'
a-
oolo
r into a dark grey one. Here the content of oulphus wao
lower (22#37%) which pFoblably corresponds to a'solid splution
of L&2S3-La3S4- When beating the L&253-tableto up to 20000 they
melt and evaporate. Black crystals of hexagonal stru6ture.re-
mained in a small quantity on the lid of the iessel. Thei.were
Card 1/2 considered as L&2Q283. LaS is obtained by reduction of L42S3

On Lanthanum Sulphids.
with mettallic lanthanum by means of "impregnation". Tft-Itirrous
crucible made from lanthanum sulphide La was melted at a tempera-
ture of 1250-1600 The reaction product was &,gold-coloured.mat-
ter with 19,7~ content of'sulphur. The X-ray ploture of the p'ow-
der with lines that only belong to the oube-phase ehowed an iso-
structure with CeS. It crastallized was a granting of the;aommon
salt type- 9 the m1orostructure of the LaS is two-phaset large
oval yellow grains of L&S carry a light grey zone of lantharioxy
sulphide on their.borders. LaS-piecea do~not malt in a vacuum at
a temperature of 21000.(6 citations from publications).
ASSOCIATION
PRESENTED BY CHERNYAYEVq I.I.p Member of the kcadtmy,.
SUBMITTED
AVAILABLE Library of Congress.
Card 2/2

-Z vR-v IV.
Is
I' -fill

an

ANDREYENKOi G.V.,- ZVERffAt N.Ya.
Effect of phtnyllin on the thromboplastic activity and conceAration
of thrombotropinand proconvertin in the blood of white rats.
Vop.med.khim.' 6 no.4:182-385 Jl-Ag 160. (141RA 14 -.3)
1.,Laboratory for tho Study of,Physiology and Biochemistry of Blood
Coagulationg Biolo ical Faculiy, MOSCOW State University.
WICOAGUIAWS)

ZVM,'VA, O.S.
K. Holdhaus' "Traces of the Glacial period in the animal king-
dom of Europe." Izv. Komi. fil. Geog. ob-va SSSR no,S.-90-92
163. (MIRA 17:6)

AUTHORs Zverevat 0. So
TITLEi On the Genetic Boundary in a River Valley and its Role in
Hydrobiology (0 genatichookom rubezhe vdoline reki 2yego
znachenii v gidrobiologii).
PERIODICAL: Doklady AN SSSR9 19579 Vol. 114, Nr 6, pp. 1311-1314 (USSR)
ABSTRACTs The history of development of the dra 'inage.area of rivers
during the Quaternary is not always,duly -taken into account
in hydrobiological investigations. But this historical factor
may in many respects determine the conditions of the,drainage
area on which, in the end, the preaerit organic world;of waters
depends. This kind of dependences were detarmined by the.'author
in the Vychegda-river on both sides of the boundary of the
first Postmaximum glaciation by a comparison of hydrobiological
material (refernoes 30). The section inve stigated is ab'out
400 km long. In the point in which the above-mentioned bound-
ary crosses the river (district of the villages Ust'-Kulom-
-Derevyansk) the morphology of the valley. and the river bed is
considerably changed. Above Uatt-Kuiom (figure 1) the valley
is very wide and boggy. On the right side of the river a group
of lakes, representing relies of glacier-waters, lies in the
Card 1/4 bogs. Here the Vychegda is populated by a fairly well

e,
On the Genetic Boundary in a River Valley and its Role in 20-114-L-6-48/54"
Hydrobiology.
developed plankton and manyfold benthos. Mollusks, oligo-
chaetae, larvae of Tendipedidae live in the mud at the
bottom. In the microbenthos nematods axe predominant.,The
biomass of the benthos amounts to 1-12 9/M~~. Animal life is
especially rich in the thicket of aquatic plants. In old arms
of lakes the amynt of zooplankton at,tains 9.000.000 indi-
viduals per 1 m water.50% of the species of mollusks and
leeches known from the entire Komi regionlive here. Many
waters in their nature here approach,the stage of eutropbic
ponds. Below the boundary of glaciation t~e living world:
changes under the influence of the hjydrographio conditions of
the valley. The valley becomes narrower, the river bed becomes
youngert from a predominantly accumulative valley it becomes
one of erosion. The mud and the aqua 'tic vegetation disappeart
at the bottom sand, gravel and in place marbles are predom-
inant. For a stretch the river almost flows without anyregion
of inundation. The river forms meanders through the entire
width of the valley, Many tips of meanders are cut into,1he
terrace of "' pine groves. Here the mineralization of the
water, increased in the previously described section, de-
Card 2/4 creases, ail the river is mainly dependent on surface feeding.

on the Genetic Boundary in a-River Valley and its Role in 20-114,;~0/54
Hydrobiology.
The interrupted connection with the side lakes causea a
reaction tending to acidity and leads to OL general d;~atrophy
of the water. At the bottom mainly coarse-detritus-like peat
muds are deposited..The living worlCis poor here..In the
plankton diatoms and dasmids as well;,as rotifers are pre-
dominant. In the benthos - small laxvae of Tandipedidaep
oligochaetae and nematoda. The benthoe-biomass amounts to
fractions of a gram per 1 m2. The.old arms are chiefly in-
habited by river species. Centers of higher biological pro-
ductivity may-form in some places due to the accumulation of
organic detritus. The chief factora;inhibiting the,deve,lopment
of life here are the processes of erosion and accumulation,
whereby the river bad is constantly 4isplaced. But tho'changed
chemism, especially the disturbed:mineral nutritiont remains
the decisive factor. The region of the Vychegda became'un-
saturated in its stand of species after the withdraiwal~of the
Scandinavian glacier in the region.:of its deposits~ whereas
the stand of species above the glacier-boundary is sufficiently
manyfold. The wide part above Ust'~Kulom may be considered-a
peculiAr.region of refuge in which many faunal elements of the
Card 3/4 inteiglacial period were preserveL It is.true that from here

On the Genetic Boundary in a River Valley and its eole in 20-11-4-6-48/,54
Hydrobiology.
many species also.spread farther down the river, but.there
they occur in other numerical relations and excl usively in-
habit the waters of the region of inundation.
There are 1 figure.and 4 references, 3 of which are Slavic.
ASSOCIATION: Komi Branch of the AS USSR (Komi-filial Akademii -nauk SS SR).
PRESENTED: March 19, 1957, by Ye. N.. Pavlovskiyp Member of the~Acadepw.
SUBMITTED: March -6, 1957

Card 4/4

USSR / Gonoral Bioloc5y*' Gonoral HydrobioloGy.
Abg Jour Rof Zhur Biol,, No 19, 1958v iTo 85694
Author zVorciva
Inst Yo-' '* '~4ivon
Titlo Tho Gonatic Boundary in tho Rivor Volloy and
Ito Si-nificanoo In Hydrobio,loGy,
U.
Orig Pub Dolil. AN SSSRj 1957) 114, No. 61 1311-1314.
Abstract Fro:1 1939-1950 a hydrobioloL'rical:~ study was con-
ductod in tho VychoCsda Rivor. anal, tho rocorvoirs
of Ito rivor valloy on a 806tor ono portloh or
which flows throuOili tho torritory of tho first
Poatnaximal glaciation, tho ~ othor bolnG situatod
hi,3hor in tho rivcr bod boypnd tho limits of
dopoolta from, tho Gilaoiation, BOth soctorst
Gonotically difforont, Pro alloarly distinsuishod
In mcrpholoGy, hydrobiology, and hydrochonistry,
Card 1/2

ZMEVA O*S.
.New larval form of Tendipedidae (Diptera) from the Pechora River.
Int.obos-36 no.1:231-232 157, (MLHA 10:4)
1. Komi filial Adademil nauk SSSR, Syktyvkar.
(Pechora River-Chironomiaae) (Lexvae.)

V
ZV.l-
Kildedli icon

mum, 00- S.

L
as of
arvae of T6ndipedidas (Chironomidas) of plains rivers of the
guropean part of northern U.S.S.R. Trudy Gldrdblol.O-ya 5:264-274 1~3.
(KLRL 70)
1. Komi filial Akadexii uauk SSSR. (Diptera) Maryan)

mp P"a 0. S GETSER, M.V,; IZ"YUROVA, V.K.
8yatem or relic lakon lit tho
Dokl. AN SSSR 155 no. 3:677-679 kr 164. (MIRA 170)
1. Predstavleno akademikom Te.N.Pavlovskim.

USSR/General and Specialized Zoology - Insects. P.
Abs Jour : Ref Zhur - Biol,, No 6, 1958, 35142
Author : Zvereva, O.S.
Inst :
Title : A New Form of Tendipedidao (Diptera) Larval from the
Itchora River.
Orig Pub Entomol, obozreniye, 1957, 36, No 1, 231-232,
Abstract A New species of larva kanevi of Genus Tendipedidae, was
described,
Card.1/1

jjo2jhjX LUI 2L P31gilga Agcggai2DA, Llbrar7 of Oom&e~s, Dedgmter 19524i' Uncliessif iod.
~ !i : :
- t : - , :

SEKOLTAR, T.T.; ZVIRMVA 3 A
Late results of dental fillings. Stomatologii& no-613-7 11-D '54.
(KLRA 8-1)
1. ris kafedry terapevtIcheekoy stocatologil LeningriAnkago
meditsinskogo stonatologicheakogo instituta.
(INTAYS
follow up)

34504
S/169/62/000/002/042/072
D228/D301:
AUTHOR: Zverevil.... S__V_.
TITLE: Atmospheric transparency in the Arctic
PERIODICAL: Referativnyy zhurnal, Geofizika, no, 2, 1962, 29, ab.-
stract 2B225 (Tr. Arkt. I Antarkt. n.-i. in-ta, 229,
1961, 90-116)
TEXT: The atmosphere's transparency was ddt ermined from the data
of direct solar radiation measurements at eight polar statione, lo-
cated cn the territory from 69 to 800N and from 53 to 1790B an*d
having the longest series of observations (from 5 to 17 years),
and also from the data of drift-station observations. Many ofthe
direct solar radiation observations, made at different ele-vations
of the sung were processed by the graphical method of averaging.
The resulting mean-monthly values of the atmosph,eric transparency
coefficients are highest (0.816) In the winter months and lowest
(0.783) in the summer months, The yearly variation of the transpa-
rency for Arctic stations is analogous to that for more southerly
Card 1/3

B/16,9/62/000/002/042/072
Atmospheric transparency D228/D302
stations (Pavlovsk, Saratov, Karadag). The small range of the
transparency coefficient's yearly variation at Arctic stations in
comparison.with those outside the Arctic is explained both by the
decreased amplitude of the yearly variation of the water-vapor
content at the arctic stations and by the influence of condensa-
tional turbidity on the transparency coefficient. At the drifting
stations the transparency coefficients are somewhat smaller th,~,q
those at the polar stations (0.762 - 0.800).,No dependence of,the
atmospheric transparency on the geographic position of the;oboer-
vation point is observed in the cold half of the year; this rela-
tionship does occur in the warm half of the year, The transparency
increases with the increase of latitude to approximately 800H, but
it somewhat decreases in the area of drifting stations. A certain
decrease in the mean-yearly values of the transparency coefficient
in an esterly direction to noted in the zonal distributionjor Ar,,,-.
tic stations. The average value of the maximum transparency coef-
ficients at polar stations equals 0.830. As the mean transparency
coefficients obtained for a number of Arctip, stations differ little
between themselves, it is possible to use them for the characteri-
Card 2/3

B/169/62/000/002/042/072
Atmospheric transparency o4a D228/D301
stic of the average atmospheric transparency in different areas of
the Arctic. Z-Abetracterle.note: Complete translation.-7
Card 3/3

II.UTHOR:
TITLE
Zvereva, S. V.....
New integral atmospheric
S/169/62/000/006/062/0931
D228/D-304
eri ajC 8
tiransparency charact
'2141'IRIODICAL: Roferativnyy zhurnal, Geofizika~ no. 6, 1962, 27, ab-
stract 6B191 (V sb.,Aktinometriya.i atmosfern. optika,
L., G-Ldroneteoizdat, 1961, 168-171)
T--,'XT: A comparison is made of various new integ
gral atmospheric-
transparency characterislUics: The limiting transparency C;efficient.a
'Grooosed by Gullnitskiy (RZhGeofiz, no. 8, 19581 5847) and S. III.,
il..~zik (Me
r, toorol. i gidroligiya, inf sb. no. 5 1948) and Makhot-
kill's turbidity index (RZhGeofiz, no. 12, 1957: 10445~ with the
standard transparency coefficient, turbidity factor and C coeffi-
cient in Kastrov's formula. The comparison was made in two direc-
u -L
tions: 1) kccordin-rt, to z1he stability of each quantity's numerical
values when the atmosphere's mass changes, and the transparency is
fixed; 2) according to the range over which each of the transparency
-characteristics varies. The solar-radiation intensity averages, at'
Card 1.12

3/169/62/000/000'-1/062/093
i~ew in-wural atmospheric ... D228/ '304
th,e time of different masses and a variable degree'of atmospheric
transparency were used in zhe calculation, these values being ob-
ta-Lsned from the observations of Kalitin and Sivkov. KastrovIi; C'co-
and Mla'.Khotkinls turbidity index, and-then the turbidity
factor, are the most. sensitive to atmospheric 'trans .parency changes;
they are als,o the most stable in respect al' 'the change in the atmo-
spherelz mass. The limiting transparency coefficients have no ad-
o
vantages whatsoever over the other characteristics under condidera-
tilon. ~_Abstracterls note: Complete translation.
Gard 2/2

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L1111-17VIG., Yo R. it. A Z1,1101A T.M,, CA'e M' -,
I-ELMEV S.S.
Polv-merization of tetrahydroftirml ATI the y)rn,,,onr~ of antlvno~y
rentachlorlde and it.9 commpo=18. Vyookom. roud. 17 k1c).Q.,269-2174,
F 165. ("Alrd, Vi:3)
1. Fiziko-khimicheskiy institut imorli i Donetskiy
filial instituta khimicheskildi reektivcv I onobc c"histykh veahchestv.

LONGINOV# M.F.; ZVEREVA, V.A.
Preparation of thin plates for the studfof metals by meano'of
4 trausmission electron microscope. Zav.!~b. 21 no.5:559-561
161. (MIRA:14:5)
1. Chelyabinskly nauchno-issledovatellskiy~inati,tut metallurgii.
(Metallography)
(zlectron microscopy)

2h 358
3/032/61/027/005/004/017
5~S !) 0 B 11 9/B2 15.
AUTHORS: Longinov, M. F. and Zvereva, V. Ad
TITLE: Manufacture of thin foils for the e~.amination of metals
under a transmission electron microscope,
PERIODICAL: Zavodskaya laboratoriya, v. 27, no. la6l, 559-561
5,
TEXT: The authors have elaborated a new method of~manufacturing very thin
metal foils (thickness: 100 to 200 A) in which the structure of the mas-
sive initial sample is preserved. The foil is gradually reduced by'alec-
trolysis. During this process a layer of foreign metal is applied to one
side of the fail to ensure a constant and uniform current density'on the
surface of the foil and, thus, eliminate orrore caused by,irtegular reduc-
tion. The method was applied to carbon, structural, stainlesso and tranfl-
former steels. The foils obtained were examined under tbe)[1-3 (EM-3) electron
microscope. The foil is prepared as follows:A4C~20X? aim piece of the metal
to be studied is mechanically or chemically reducea to a thickness of
0.20 to 0.15 mm and then further reduced to 0.05 to 0.03 mm by electro-
Card 1/2

2hl
S/03Y61/05287/005/004/017
Manufacture of thin ... B119 B215
lytic polishing (for steels: an acetic acid chromium electrolyte is used
at 1.5 to 2-5 A). After washing in water and dryingt one'side of the fo il
isceated with a foreign metal by electrolysis or vacuum evaporationo When
choosing the metal, one has to consider thatthe latter can be chemically
removed without damaging the foil. For chromium anUchromium-nickel:.steels,
the authors used zinc or copper. A zinc layer has to be protected against
dissolution in the electrolyte by a thin paraffin layer. Under the,abovo
condit-ions the foil is then electrolytically reducea, on the bare side un-
til the foreign metal appears. For removing zinc a hot aqueous NaOH~solu-
tion is used, and for copper an aqueous or alcoholic JINO solution.2here
are 3 figures and 5 references: 4 Soviet-bloc and I non-Soviet-bloo.
ASSOCIATION: Chelyabinskiy nauchno-issledovatellskiy institut metallurgii
(Chelyabinsk Scientific Research Institute of Metallurgy)

ZVEREVA, Y.A.;.NIKOLISKIY, Yu.V., inzh.; SAYTANID1, L.D., teldm.red,
(Improvement of swamps and-mineral swampy soils; bibliography]
Meliorateiia bolot i minerallnykh zabolocheinnykh zemell; biblio-
graficheskii ukazatell. Koakva. Izd-vo 14-vn sell.khoz.RSFSR* ~
Pt.l. 1959. 1)0 p. Pt.2. 1959. 155 p, (HIRA~12:12)
1. Moscow. Gosudarstvannaya Inauchnnys bibliotaka. 2, Gosudarst-
vemuiya nauchnaya biblioteka (for Zvereva). ). Respublikenskiy .
gosudarstvennyy institut po proyektirovaniyu vodnkhozyaystvennogo
i meliorativnogo stroitelistva 1'Rosg1provoakhoz*,(.for Nikollakly).
(Bibliography-Drainago)
(Bibliograpby-Swamps)

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J.P.,kandidat tekhnichaskikh nauk.
Technique for determining the composition of protective oiide~
films resulting from electrochemical oxiae c6atir4 of steelvarei
.Trudy MVTU n0-36:62-66 '55. (HLRA 9-9)
(Oxidation, Slactrolytic)

z V-P,A V
',~rke, FleGtroplat.,ni and Metal Finishine
CLI E!;y V.
Sept. 1948, p. 591-592; Oct. 1948, p. 667-B68, 674.
ranslated from Zavodskaya

NINDLATEV, V.G.;
Ye.T.; ZIMINA, K.I.; POPOVAp memo
~500
Isolation of individual normal paraffin hydrocarbons from the, 200-3
fraction an obtained from Romashkin Devonian petroleum. Khim.i~tekh.
tol-no-3:11-17 Mr 156. (MMA 9:9).
(Hydrocarbons)

Let's prsi~re for tba.40th-emmyormary, of the Great October Ao'clallst
Revolution In the proper mnner. Blot. agitl~ vod. transp, no,6:3p.44
(ML~A- 10:4)
1. Agitator teplokhoda Oftrkmeuistan" raspiyokogo parokhodstva.
(Merchant warina')

z YER'Ev V, YA.
11/5
2 3 05
Artilleriy.--kaya insbriurental Maja Ra,.,vedka', Uchebnik Dlya' Ai-t~lloriyskAl%h'bcl,-~i.lishcl,.
(Artillery Reconnaisnace I ry) D.A PeIrgin, V. VA. ZU.1-W I V. IN. DA"IMN Yo.-.qkva,
Voyenizdat, 1956.
h83 p. illus., Dit,.C-rs.., Tables.
Bibliography: P. h78.

lyl, ~ vi
=
.V. Yu. T.
-----------
"Ohat the eagineer and repAIrman, chould read on boiler repair.
F,nergetik no.6:40 Je 05?. 10:7)
(I$ibliography-.Doilerfl-.':ointennn,.,o and.repair)

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Al -1 1~ . 1
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::~ V I-- ~ I I I . - I
ZORMSHCHIKOV, P.A., prof.; OBRAZTSOV, V.L*, assintent; ZVURNVA, M.Li
assisteat.
Results of vitaminizing pregnant cows and newborn,calves on the
OTrinaateat' let oktiabriam Collective Farm. Zhivotnovodetvo 19
no.12-68-70 D 157. (MIRA 10:12)
l.Troitakiy sooveterinarn inatitut,
(Calvels (Vitamins)

15-757-4,-4276
Translation from: Referativnyy zhurnal, Geologiya, 1957 Nr 4ffl~
p 33 (USSR)
AUTHOR: Zverevap 0# so
TITLE: Hydrographic Features of the Komi ASSR, and Their
Relation to its Quaternary History (Nek otoryye.osoben-
nosti gidrograficheskoy seti territoril Komi ASSR,v
svyazi s yeye chetvartichnoy is~oriyey)
PERIODICAL: Izv. Komi fil. Vses. georg. o-va, 1955, Nr 3, pp 11-16
APSTRACT: Bibliographic entry
Card 1/1

'
VE, E
VA) 7.
/7,
OOA

IrO=B b1fdOG. M.
sea It. No. 3, ",0q4
bAVO I"k kIM WidWJ rQ4
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00
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are*

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si
wo tOWA o0oxiv
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0 40,00* 0 0 Ole 00 Oe 13
I: :!:: : :

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proo
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U04 86 41
-rm Cofficass of Oamis 0 In
.
spimfirb, comMateri &It* bwas find peat Wait &r4di JW-

off cot4ing to riftmst*~-Dukiu.] The laswis of vitamin C did

8
0 not tweed 6-19% an wubi"~Obv veviLbIM with lintru
:
d
li
h
: an
coo
tte t
em wills sk.
he losses, reached Zt-13%
411

an coollft Then faith finster.i The Won" ofvilaosin C vm 44111

:0 1-28% oft keephalt the *v4"ables.ba tlw frostu 111111W.
Vetleftblefirmactowco"I wall 42,70 N&C1 u4s.;kvit :100
vm little of the* -41simin, C context. The losses *m
144-M-41% lifter,dtfroming and 7-M.1% after lallflat off
the defrosted Frown vegetables kom Itar
600
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!
sistenty of (ItA To
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d
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.
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4111~0 0-0 0 0 0 0-0 0-0 0- 9-0

USSR/Chemical Technology. Chemical Products and Their Application Food Industry,
1-28
Abst Journal; Referat Zhur - Khimiya, No 21 1957, 6585
Author: Zvereva, T. A.
Institution: None
Title: Study of the Suitability of Canker-Resistarit Varieties of Potatoes
for Drying
Original
Publication: Sad i ogorod, 1953, No 91 55-56
Abstract: No abstract

BCROWLINA, F.Z. WLOBATBVA, L*G,; ZVMWA, T,A*
Determination, of photosynthesis under f iald conditions. Trtdy Inst.
fiziol.rast. 10:250-256 155. A,: 9)
1. Kaf edra f lziologli rastenly HoskDvakogo goirAmrstvannogo univervitata
imeni M.V. Lomonosova. (Photosynthesis)

ZVEREVA, T.A.; TEPPER. R.Ya.; OGN.",A, R.I.
Preparing potatoes for drying. Kona. I ov. from. 13 no.4: 13,14
Ap 158, (HIM ll:'4)
1. TSentralInaya proizvodetvennoya laboratoriya pri Moskovskom
2avode pishchevykh konteentratov lfo.L
(Potatoes--Drying)

xAZImIRSKIY, Ta.M., starshiy nauchnyy ootrudaik; ZVEREVA, T.A,', starshik
nav,chnyy sotrudnlk; GRANOVSUTA, R.Ta. , mUdisfil-7 -natibEi~yy sotrWnik;
FrATIGORSKATA, T.Is, starehiy nauchny7 eotrudnik
Tachnical and economic offectivonoso of the stonm-beAting, and.,
mechanical methoda of preparing potatoeo for #ying.: Trudy VMXKOP
no.9:26-52 t59. (MIRA 14-I)i
(Pbtatoes-Rrying)

i
SOURCE: Ref. eh. Elektronlka I yeye primeneniyer Abs. 8A85
AUTHOR: Aleksand-vov, L. M.1 Mironoy, 9. M.1 Zvereva, T. 114
TITLE-. Investigation of tungsten rearystalUzation U quick eteotria heating
CITED SOURCE: Uch. zap. KbrdovsA un-t, vypo 56, 1964, 5~-,57
TOPIC TAGS: tungsten filament, tungsten, metal recrystallftAtio#, tainsile atr6r4;th,
annealing
TRANSLATION: Prior to annealing, the speciMns were aleaAdd by boiling in a 205~
solution of HaOH for 10 recrystallization process was studied by the
variation of the ultimatns;x Pth at room temperature with the annealing temperature
6 S termined on a FUE:9 iestin
and time.The ultimat -tre t as de _5~tensjle Mach 0. v')
For an annealing time of ',kO adLn, the final Fi~u-ii~-was
TCj and for 200 sea, 16DOC. Pmm the aboTe data,
about i45OC; for 10 min, almost 15,
a curve of pr imary-recrystalliration--acMIat Ion time vs. amneal3M, temperature roras
plotted. A metallographia method corroborated Ute fact that the, rec*stallisatlon
goes quicker with higher rates of heating. Bib 4.

ZVEREVA, T.S.
Foms of clayey fomations and'highly dispenod mJjierals in
turf-carbonaceous soils. Pochvovedenie no.11a,U-" 11 164
(MA 18:1)