SCIENTIFIC ABSTRACT POPOVA, O.S. - POPOVA, S.M.
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December 31, 1967
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SCIENTIFIC ABSTRACT
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B/07 01034101110181024
B004YBO'64
AUTHORSs Sanzharovskiy, Ao.T. and Porova. 0-4 S. (Moscow)
TITLE: The Method of Investigating the Diffusion of Cathodically
Reduced Hydrogen Through Metals
PERIODICAL:- Zhurnal fizicheskoy-khimii,,1960,.Vol-,34, No.,11,
pp.12601-2602
TEXT: This paper-gives a report on diffusion measurements of cathodically
-redu.ced'hidrogen-through metal follsicarried out by two methods:
,a) diffusion through a metallic cathode foil into a space in-which the
pressure rise was measured with a gauge. b) Measurement of the sag h of
a cathode foil --isolated on one side-. The sag was caused by-hydrogen
diffusing into the fail. Iron and nickel foils (thickness, 50A) were used.
Depending on the center of gravity of the chu9ked foil and as a result of
tension, sag in the direction of the anode or in the opposite direction
occurs in case b at the same potentials-This joint action of mechanical
and diffubion'effects requires a careful interpretation of the experimental
data. There are 3 figures and 4 references: 2 Soviet.
Card 1/2
POPOVA, 0. S.: I-Iaster Chem Sci (diss) -- "Aspects of t:~e atr-,-,cr-fire anrl prr-P.---r-
ties of electrolytic precipitates of implicitly crystalline type". Moscow,
1959. 12 pp (Acad Sci USSR, Inst of Phys Chem), 150 copies (KL, No iL, 1959,
115)
-AUTNORS: Popova, 0. S. , Gorbunova,
TITLE: ---T1-.--e-S-6ructU-re and Some Pronerties of Electrolytic Manganese
(Stroyeniye i nekotoryye .9voystva elektrol-iticheskogo m-argantsa)
PERIODICAL: Zhurnal fizichoskoy khimii, 1958, Vol 32, Nr 9,
pp 2o2o - 2o28 (USSR)-
ABSTRACT: The electrolytic solution used contained manganese sulfate
and ammonium sulfate. An additional solution of the same
composition but with glycerin added vias also used. The
manganese deposit was investigated using the microzcope
(Fig 1), the electron microscope (Fig 2), and X-ray apparatus.
As the Debyograms show, the manganese deposits, and
especially those from the solutions containin,_r glycerin,
are almost amorDhic (Fig 6). After warming for a short
time at about 1200C the manganese appears to have 'the
strticture of a-Mn or y-"n in the X-ray studies. Whichever
modification appears is depprident upon the conditions of the
electrolysis. T*-,e hydrogen content of the electrolytic
deposit was also determined by using the apparatus shown 3
Card 1/2 in figure 3. The content was found to be between 5 and 8 cM,
S~ruc.Lu-re a--,d So-e of
7
Manganese
of hydrogen per gram of metal (Table). The greatest --art
of t-,e hydro6en escapes up to 12501", while the rest leaves
U'l - U
up to 3000C (Figs 4 and 5). This behavior differs from that
of electrol-.-tic nickel (Fig 5). By iisin~~ nn olnE;tic
c,rithodo tile Inner stre-i of tile maneanene wan, determined.
According to the ccrlditions of electrolysis this was
lound to be betwec--, 5 and 20 kg/MM2
il . There are 6 figures,
1 table, and 30 references, 9 of which are Soviet.
ASSOCIATION: Akade-miya naul. SSSH Institut fizicheskoy khimii, Moskva
(AS USSR, 1,10scow
Institute of Phycical Chem-istryl
SUBI-TITTED: April 4, 1957
Card 2/2
13 7 - 58 - 4 - 7 8 42
Translation from: Referarivny-v zhu_rn.L.
AUTHORS: Gorbunova, K. M. Popova 0. S. SLty-igina, A. A. Poluk.-- rov,
Yu.M.
T IT LE: Mechanism of Growth and Structure of Precipitates of Metals
Produced by Electrical Crystallization (Mekhanizm rosta i .5tro-
yeniye osadkov me talla, vozrikayushchikh pri elektrokristttlizat
sii)
PERIODICAL: V sb. : Rost kriStallov. Moscow. AN SSSR, 1957, pp 58-66
ABSTRACT: Certain principles of the growth on the cathode of an electro-
lytic cell of deposits (D) of metal in the form of dense coatings or
loose dendritic structures are examined. K. M. Gorbunova shows
that when s n lu crystals -ire tormed, an increase in current I re-
sults in the I ZS-K ratio remaining constant because of the increase
in the surface of growth. This latter results in ~ transition from
growth of the single crystal to the growth of multicrysLalline D (a
relatively high concentration of discharging ions occurs) or to a
growth of dendritic D (a low concentration of discharging ions).
Dense polycrystalline D grow when ZS-S is attained at the cathode.
Card 1/3 Subsequently, further increase in I can occur only when there is
137-58-4-7842
Mechanism of Growth and Structure (cont.
a drop in the concentration of ions at the cathode. At a given I, the ion concen-
tration at the cathode may prove to be close to zero: the maximum diffusion
current is attained (MDC). Powder D form upon electrocrystallization tinder
MDC conditions. The particles of the powder D are extremely fine dendrites,
the angles between the branches of which are determi,ned by the crystallogra-
phic nature of the metal. For Zn powder, the angle is 600. In (tense crystal-
line D the anisotropy of properties such as the magnetic, the linear compressi-
bility, resistivity, thermal expansion, resistance to corrosion, etc. , are de-
termined by texture (orientation of all the crystals of the D in a given crystal-
lographic direction). The authors hold that in the case of D with crystals above
a certain size and small internal stresses (IS), it is more accurate to regard
texture as "growth texture, " Texture comes into being as the result of com-
petition between crystals of different orientations, as the ionic building blocks
brought up to the growing crystals are put to use. The change in the texture
axis with change in the conditions of electrolysis is explained by the change in
the ratios of the growth rates in different directions. The unique adherence
of the texture of Zn and Cd D to a 6th-order axis [ 00011 c on application of
an alternating current, with the surfaces bounded not by apices but by the faces
of the base, may be explained in terms of the concepts developed by Kaishev
and Bliznakov. X-ray and magnetic studies have made it possible to determine
Card 2/3
137-58-4-7842
Mechanism of Growth and Structure (cont.
that IS anisotropy exists in Ni deposits, and also that the IS of Ni is not directly
reldted to the amount of occluded H2, Introduction of brightening tgents in Llie
buth leads to the formation of deposits not. hoving the definite clearly defined
boundaries characteristic of crystcils, nd the D consist of rounded forms.
0. P.
1. Cathodes-Deposits-Structural analysls 12
tural analysis
Card 3/3
05814
18M sOi/76-33-10-12/45
AUTHORS: Moiseyev, V. P., Popova, 0. S,
TITLE: X-Ray Analysis of Electrolytic Manganese Deposits
PERIODICAL: Zhurnal fizicheskoy khimii~ 1959s Vol 33, Nr 10, pp 2183--2189
(USSR)
ABSTRACT: Structural transformatiornin electrolytic manganese deposits
have been investigated little so far (Refs 4-9) though they are
of great scientific and practical interest. The structural
and phase transformations of electrolytic manganese deposits
occurring in vacuum heating were subjected to X-ray structural
analysis. The deposits were obtained from two baths of the
following composition: 1) 150 - 200 g1l of MnSO 4' 5H20+ 50 -
0 +
so
- 100 g/1 of (NH
and 2) 150 - 200 g11 of MnSO
' 5H
)
2
2
4
4
4
- 20 g1l of glycerin. The hydro:-
+ 50 - 100 g11 of (NH
30
)
2
4
4
gen separated by heating the sample (to 50, 80, 100, 125, 140,
200, 300, 500, and 700 C) mas determined in a vacuum device
(Ref 4). Kurdyumov's formula and a new equation for calculating
the lattice constants from radiographs (obtained for plane
Card 1/3 polycrystalline samples) were used for the purpose of choosing
0581L
SOV/76-33-10-12/45
X-Ray Analysis of Electrolytic Manganese Deposits
~he conditions of X-ray analysis. The radiographs (Fig 2)
resemble those of amorphous substances and exhibit a strongly
blurred diffusion line and a fairly large,background of in-
coherent scattering. Both allotropic variations, i.ea a-manga-
nese and y-manganese were obtainedq the latter in, a 10g deposit
on a silver base in bath (1). It is very unstable-and soon
passes over into the a-variation (after some hours). Data on
the variation in the crystal-lattice constants of %-manganese
(Table 1) indicate that different deposits (as to the content
in hydrogen and the kinetics of hydrogen separation in vacuum
heating) were obtained from the two baths. The.deposits may
be regarded as a solid solution of hydrogen in a~-manganese
(with strongly deformed crystal lattice). The afore-mentioned
amorphous structure is brought about by the large hydrogen
content in the crystal lattice. In vacuum heating, the solid
solution decomposes due to the separation of hydrogen and re-
duction of the crystal-lattice constant. The manganese deposits
were found to have an inhibitory effect on the decomposition
of austenite which occurs when the temperature of the samples
(1,080 C) slowly drops. Radiographs (made by A. T. Sanzharovokiy)
Card 2/3 of samples obtained by adding B02 to the solution indicate
POPOVA, O.V.
Use of intralaryngeal d'arson7alization in scleroma. Vest.oto-rin.
18 no.5:58-59 S-0 156. (MIRA 9:11)
1. Iz kliniki bolemey ukha. gorla i nosa (zav. - cloktor meditsinskikh
nauk Ye.U.Novak) Stanislavskogo meclitainakogo iustituta.
(IARYNX. die.
rhinoseleroma, ther., intralaryngeal d'arsonvalization)
61JIGTROTHIRAPY. in various die.
(r
d'arsonvalization, intralaryugeal. in rhinosoloroma of
larynx)
(RHINOSCIARONA, there
diarsonvalization, intralaryMeal, in rhinoseleroma of
larynx)
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ACCESSION NR: AP4038605 S/0108/64/019/005/0078/0079
AUTHOR: Blokh, E. L. (Active member). _.~qpvov._Q. ,V., (Active member)
TITLE: Nonoptimality of cyclic codes which correct single and detect double
:errors
SOURCE: Radiotekhnika, v. 19, no. 5, 1964, 78-79
TOPIC TAGS: code, cyclic code, error correcting code, error detecting code,
double error detecting code, binary code, Humming code
ABSTRACT: A Humming binary code with r - 3, 4. 5 ... check digits and With a
minimum distance d - 4, which has a length n is an optimum code. The
present article proves that: (1) no-cyclic code exists which would be equivalent to;
Hvmming's ~binary codes with d . 4; (2) no cyclic code exists with d >2 and r>3
check digits which would have a length n Orig. art. has: 2 formulas.
,ASSOCIATION: Nauchno-tekhnic~eskoye obahchestvo radiatekhniki i elektroevyamil
(Scientific and Technical Society of Radio Engineering an4',Electrocommunication) I
SUBMITTED: OZApr63 DATE ACQ: 09Jun64 ENCL: 00
SUB CODE: -A DP 2( t NO REF SOV: 001 OTHER: 001
!Card 1/1
SULTANDV, Z. A. ; BABATYWA, G. 1. ; POPOVA, 0. V.
Using spent acid for cleaning aromatic compounds. Azerb.
neft.khoz, 35 no.8:34 Ag '56. NLRA 9:10)
(Petroleum-Refining) (Aromatic compounds)
Levi. 0.
"hie laym. Smimov. and 0. V.
~Egnnvn- U.S.SR. 10S.9,37, june '215, Water-.-Ol.
Ilycok with a chain of --~4 C aturas or dicii etlier5 are 3daled
K. Jn a quantity ?_20 m1./1. of tvaulsiou along with gelatin-
Janning subitances. This procedure incrmses the streugth
;of the gelatin. Elasell
TIMOFEYEVk., A.V.II POPOVA, O.V.
Application of chemistry in footwear manufacture. Kozh.-obuv.
prom. 6 no.5tl3-14 My 164. (MIRA 17;12)
SMIRNOV, O.K.; LEVI, S.M.; RYBNIKOVA, A.I.; KORNEVA, E.D.;_POPOVA, O.V.
Hardening and plasticizing effect of water-soluble ethers
of hexamethylol melamine and some mono-, di- and triatomic
alcohols and polyglycerins. Part 1: Ethers of hexamethylol-
melamine and of mono-, di-, and triatomic alcohols and polyp
glycerins. Zhur. nauch. i prikl. fot. i kin. 8 no.6:401-404
N-D 163. (MIRA 17: 1)
1. Vsesoyuznyy nauchno-issledovatel'skiy kinofotoinstitut
(NIKFI) i Nauchno-issledovatel'skiy institut organicheskikh
poluproduktov i krasiteley (NIOPiK).
GHURAYEVA, A.M.; SHEBERSTOV, V.I.; POPOVA, O.V.
Effect of polyethylene glycol on the induction period and
subsequent speed of the photographic detrelopment. Zhur.nauch.
i prikl.fot. i kin. 9 no.23122-124 Xr-Ap 164. (MIRA 17:4)
1. Vsesoyuznyy nauchno-issledovatellski-y- kinofotoinstitut (NIKFI).
POPOVAY O.V.
Usually large choanal polyp. Zhur. ush. nos. i gorl. bol. 23.
no.2 -.79 Mr-Ap 163. (MIRA 16:8)
1. Iz kliniki bolezney ukha, gorla i nosa (zav. - doktor med.
nauk M.S.Yedved6vskiy) Ivano-Frankovskogo mditsinskogo insti-
tuta.
(NOM.,TUI-DI?S)
S.I.J. ; Vjj,7:~,':SKjY
L--VI Yu.B.; ICOGIRIEVA, S.N.; POPOVAJ, O.V.; V.,')--TEII-GVA, T.I,'.
Diffusion method of haardening emulsion layers. Zhur.nauch.i pril-1.
~ot. i kin. 7 no.3:161-168 ltr~-Je 162.
1. Vsesoyuzn3ry mauchno-iSL-1c-dovatel'skiy kinofotoinstitut (J~,JKFT) J
filial Vsesoyuznogo mauchno-is,-~Icdovatellskogo kinofotoinr;tituta,,
ShostIca.
(Photographic emit1sions)
LYUBIMOV, V.I.; KAGAll, Z.S.; V.ASILEYKO, M.A.; POPOVA, O.Ye.
Decomposition of volatile organic acids by microorganisms of
"active sludgell. Mikrobiologiia 32 no.4-700-702 Jl-Ag 163.
(MIRA l7x6)
1. LyuborotBkuyu laboraLurlya nauchno-it3oledovatallokogo otdola
tresta "Mosuchistvod.
YEGORGV, N.S.; POPOVA, O.Ye.; BITTEYEVA, MiB.; BULGAKOVA, V.G.; GOV-1AN, K.
Influence of the products of vital activity of bacteria an the
growth and antibiotic properties of various actinorjcetes. Mikro-
biologiia 29 no.2:269-275 Mr-Ap 160. (MIRA 14-7)
1. Biologo-pochvemyy fakulltet Moskovskogo gosudarstvennogo
universiteta. imeni M.V.Lomonosova.
(ACTINOMES) (9ACTERTA)
GOLUTVINA, L.F.,.kand. tekhn. nauk, PAVLOV, S.A., doktor tekIn. nauk;
IVANOVA, Ye.I., -nauchnyy zotrutink; POPOVA, P.A!, nauchnyy
sotrudnik; ZADVORNOV, V.P., nauchW-9-0'1~a-ar
Operational properties of fireproof coated materials. Nauch.-
issl. trudy VNIIPIK no.14,%83-92 163. (MIRA M12)
"UrT., G A
cun7ry
n
tlBtegory : or-entai.ion Indus ry
Ab3. Jour : Rei Zhu NO it.) 195Q,Nc 14 1::
Author : Uptl~rcrnN.
Instit-Ae :
Tilb-le : II-,Y IP e c 'a, o fCr;,.n~-. Prpssinr, in a Goritintioijf7 tIreFs
on the )Ila] i i-z of CopTizLr Distil late
()ri c- !~Jr)8, 7, '~O ~-;-I
b s r.; c t, The efl'eert ol (rra;- ~lre~zsint-- -Ir a contill1r.'U.13
,ress (t'.P.) cn Oic ciml-ity r~f copnv-c alcr*'01
has been inveizTigatedi. "I .it!, :-ncrr-!".Sel:l pr~-~:siircl!
;Llhn oor teri-t of. rnvtI,nn(~I in the dI ~i IA I 1A t,z"in-
-A
Thv~' fir-A ovtlp-t romle('Llor,
c, r
wit ~i r n f tn i r: 1) c, p c rr-. -a
r
Althoul-1- ne si-i-;iif'icvnt difformcp in 1A 'e c. t' c -
corycsitinn discovered, distillafe 1,
rlerivef! f'rcin Ihe mtst oT Che Pirst, nnd
IIP)
SNOPKOVAJ V.A.; POPOVA
Pathogenic staphylococcus carrier state among Foersonneel, rarturlents
and newborn infants in maternity homes Olos. 4 Wid 5) in Karaganda.
Antibiotiki 9 no.3:276-279 ?-x 164.
(MIRA 17:12)
1. K&fedra mikrobiologil (zav. - G.P.Mar) Karagandinskogo meditsinskogo
instituta, Karagandinskaya oblastnaya sanitarno-epidemiologicheskaya
stantsiya i laboratorlya stafilokokkovykh infek-tsiy (zav. - prof. B.V.
Voskresenskiy) TnstiLuta epidemiologii i mikrobiologii imeni N.F.Gamalei.
2~0182
S 76/61/035/009/00=)/015
A j /_9 j B1o6/B11O
AUTHORS: Andreyev, K. K., and Popova, P. P.
TITLEt Burning of pentaerythrytol tetranitrate
PERIODICALs Zhurnal fizicheskoy khimii, v. 35, no. 9, 1961, 1979 - 1984
TEXTt The authors explain the reasons for the different behavior during
burning of pentaerythrytol tetranitrate (PETN) as compared with other nitro
eaters similar with regard to composition and thermochemical characteristics,
The experiments were made on pressed specimens of PETN ( Y - 1. 25-1-30 9/cm)
at constant pressure in the pressure range of 16 - 750 atm. The expeximents
at high pressures were conducted by A. P. Glazkova. PETN is comparatively
stable to burning; only at a critical diameter of the charge d - 30 mm, it
burns under atmospheric pressure, The burning rate is only 0.023 g/CM2-sec.
(0.28 for nitroglycerine and 0.043 9/cm 2.sec for nitroglycol). Only at a
pressure of 16 atm steady burning sets in at room temperature and d - 6 mm.
The burning rate is here directly proportional to prensure, and at 10 atm
it has a value of roo.6 g/cm2-sec. For PETN the combustibility is, there-
fore, much lower than for nitro7glycerin or nitro-glycol, Nor do two
Card 1/4
27682
3/076/61/035/009/005/015
Burning of pentaerythrytol tetranitrate B1o6/B11O
the corresponding value for nitro-glycol. In conclusion, it may be said
that the peculiarities during the burning of PETN may be due to the fact
that PETN is solid at room temperature. The above-mentioned upper pres-
sure limit may be used for changing burning into explosion. When large
amounts of PETN are ignited and the pressure is then increased above the
upper critical value, the flame is extinguished, but the heated layer re-
mains and becomes even thicker since exothermic decomDosition in it is
maintained. Moreover, additional heating by the surroundings heated
during burning is also possible. Thus, a flare up of a high amount of
explosiVe may occur which may lead to an explosion, especially when the
PETN is in the form of a powder of low density, so that the hot combus-
tion products can penetrate into the interior of the powder. When PETN
burns in the molten state, marked pulsation appears at slightly increased
pressures (6 - 8 atm), which leads to a strong acceleration of the
burning. I. A. Tereshkin is mentioned. There are 3 figures, 1 table, and
3 Soviet references. The reference to the English-language publication
reads as follows: G. K. Adams a. G. W. Stocks, Pourth symposium on
combustion, The Williams and Wilkins Co., 1953, p. 239.
Card 3/4
POPGVAV P, 1),
Effectivenees of prb7entlon of nldphyloc6ccAl lnfoll-t~r;na In
parturient3 and newborn inf&nts by immunizatlor, with native
stapbylococcal toxold. "'bur. mik--,.A,!cl., PpId. i I=Un. 40
no.10j6.1-68 0 163. WIRA 17%6)
1. Iz sanitarnc-bakter.'t.,-;Logici-teskcy labore-torii Kdragandlns~oy
ablasti Kazakhskoy S5R I Instiilate. epi.-NimiologiJ J irdkrob1clogli
Imeni Gamalay AWI SSM.
APDREYEV, K.K.; POPOVA, P.P. (Moskva) -
Burning of pentaery-thritol tetranitrate. Zhur.fiz.khi"-. 35
no.9:1979-1984 161. (MIRA 14:10)
1. All SSSR., Institut khimichaskoy fiziki.
I(Pentaorythritol) (Combustlon)
85958
S1020160113'/C051'~35/ 35XY
BO 16330 5~
4
AUTHORS: Andreyev, K. K, and Popova, P. P.
TITLE: Combustibility of Protective Explosives---
PERIODICAL: Doklady Akademii nauk SSSR, 1960, Vol. 134, No. 5,
PP. 1142-1145
TEXT: The authors report on their investigations of the combustibility
of protective explosives which sometimes burn-up instead of exploding.
This combustion leads to an evolution of methane which when mixed with air
may take fire or explode. The combustibility is determined by critical
values of interrelated parameters. They are: 1) The minimum pressure,
2) the minimum temperature, and 3) the minimum diameter of the charge.
The authors deal with the critical diameter. Tho oxplosives Investigated
(density I - 1.3 g/cm3) were burned in a conical case (h = 5 cm) made of
three layers of glued Cellophane, or in a glass cone, both inside and
outside coated with perchloro vinyl varnish. The experiments were made at
100 - 120 atm. The change of the critical diameter with the change in
density, and the influence of the latter on the rate of combustion were
Card 1/3
85958
Combustibility of Protective -Explosives S/02O/6O/1'z/C0';/C35/C3_XX
BO16/BO54
determined. Table 1 shows the composition of the ammonites investigated
which contain no nitro ester. On the other hand, pobedite 1TY -2 (PU-2),
51T-i (VP-1), and S71-3 (VP-3) contains up to 9% of nitro ester mixture.
Fig. 1 shows the experimental fesults. Sence, the authors conclude that
the critical diameter of all explosives investigated (except for the
waterproof pobedite VP-3) lies between 7 and 13 mm at all densities and
at 100-120 atm. This value lies far below the usual measure of blasting
cartridges. The critical diameter of pobedites is smaller, but the com-
bustion rate is higher than that of ammonites, The latter also applies to
dynamites. The rate of combustion decreases with increasing density
(contrary to statements made for other explosives in Ref. 1). The critical
diameter -, as a rule, also decreases in spite of the decreasing combustion
rate. The authors assume here a considerable effect of the exothermic
reaction in the condensed phase on the flame propagation. The critical
diameter of pobedite VP-3 could not be reliably measured by means of the
method used by the authors. The combustibility of VP-3 proved to be much
higher than that of VP-1 at 100-120 atm. This is probably due to the
catalytic effect of the mineral components of admixtures added to the
saltpeter to make it waterproof. This catalytic effect is, however, not
Card 2/3
85956
Combustibility of Protective Explosives
B016/BO54
universal. The great difference between the combustibility of VP-1 and
VP-3 disappears at lower pressure (20 atm). The authors conclude that
the relation between the critical diameter in the mixtures investigated
and the combustion rate is more complicated than is generally assumed. The
authors' experiments were made with commercial substances. They showed
that the combustibility of the individual explosives used in coal mining
differs very much, especially at slightly increased pressure. The authors
recommend further investigations on this matter. A. P. Glazkova is
mentioned. There are 1 figure, 1 table, and 2 Soviet references.
ASSOCIATION: Institut khimicheskoy fiziki Akademii nauk SSSR (Institute
- of Chemical Physics of the Academy of Sciences U~SR)
PRESENTED: June 3, 1960, by V. N. Kondratlyev, Academician
SUBMITTED: June 3, 1960
Card 3/3
POPOVA. P.S.
Studring the nature of water aaturation in the Y-17azm Reservoir.
Vod. I Ban. takh. no.9:7-9 5 '58. (MITtA 11:10)
(Klyazm Reeervoir-Water-Pollution)
BUDAGOVA, G.G.; B=IAVICH, T.N.; POPOVA, P.S.
Role of helmintho and of intestinal protozoa in bacillar-y dyeentery. Ked.
paraz.i paraz.bol. no.4:351-353 Jl-Ag '53. (MTRA 6:q)
(Dysentery) (Worms. Intestinal and pa-rasitic)
BURAGOVA, G.G.; RUML&VICH, T.H.; POPOVA, P.S.
Work experience of the da7 hospital for the treatment of helzinthiasis.
Ked.parax.1 paraz.bol. no.6:551-553 &D '53. (XLRA 6:12)
1. Is Instituta malyarit i meditsinskoy parasitologii Hinisterstva
zdravookhranonlya FSM (direk-tor instituta S.N.Pb',,-.ovskiy).
(Worms, Intestinal and parasitic)
SADYKOV., -
Influence of light conditions on the for---ation of cotton fib--r.
Uzb.biol.zhur. 6 no./+:5-12162. WIRA 16:7)
1. Institut aeneUki i fiz-4ologii rasteni-7 AN UzSSR.
(COTTO1,,1 (PLAIMP EFFECT OF LIGHT OR)
YAZYKOV, P.P.; 'T2MSHENKO, M.A.; POPOVA, P.Ya.
Effect of the nutrient area and rate of fertilization on cottom-
yield. Izv. AN Uz. SSR no. 9:31-41 156. (NORA 14: 5)
(Cotton-Fertilizers and manures)
POPOVA., P. Ya.J Candidate Agric Sci (diss) -- "Changes in the quality off raw
cotton and fiber as a function of certain conditions of feeding the cotton".
Tashkent, 1959. 23 PP (Tashkent Agric Inst, Inst of the Genetics and Physiology
of Plants of the Acad Sci Uzbek SSR), 150 copies (KL, No 25y 1959, 137)
SMIRNOVI B.P.; POPOVA, R.A.; DANILOVA, G.P.; NISKANEN, R.A.
Paper chr2Tatography of bile acids In the form of methyl eaters
(R. COO.C14H 3) . Biokhimila 27 no.2:197-201 Mr-Ap 162. (NIRA 15:8)
1. Laboratory of Lipid Biochemistry, Biological Institute of the
Carelian Branch of Academy of Sciences of the U.S.S.R., Petrozavodsk.
(PAPER CHROMATOGRAPHY) (BILE ACIDS)
STU PAKOVA ) L. F. , inzh. ; -~'
,q~OVAJ ~R.A.
Earth roadbed made of opallm Ivt, 2p,
no.2:16-17 F 165. 18:6)
85615
6,1130
3, &-0-6-0
S/0;:O "G/Ooo '011/00~- '00=
B012/BO6'~
AUTHOR: Popova, R. K.
TITLE: Some Characteristics of Fog Formation in the Southeastern
European Part of the USSR
PERIODICAL; "Ieteorolol-i4ya i Eidrologiya, 1960, No. 11, pp. 29-31
TEXT: Da'a supplied by 27 weather stations during the years from 1946 to
1955 were used for clarifying 'the specific characteristics in fog
formation in the southeastern European part of the USSR. As many as 5852
cases of compact fog and 1275 cases of transparent fog -iere studied. All
fog formations were divided into four groups: advection fog, advection
radiation fog, radiation fog, and frontal fog. The following was
established on the basis of these investigations; Advection fog is
predominant over all the territory. Of all fog formations observed during
the past 10 years, 62A, were advection fog and 14% radiation fog, while
frontal and advection radiation fog constituted 12~/. each. According to
data by I~ V. Koshelenko (Ref. 2) on the central part of the European USSR,
Card 1/1-11
85615
Some Characteristics of Fog Formation in the S/050/60/000/011/003/005
Southeastern European Part of the USSR B012/BO63
advection fog is mainly observed at the western periphery of the
quasisteady anticyclcnes over southeast part of the USSR (32%) and, more
rarely, at the southern periDhery of the cyclones (27%o). About the same
data are supplied by N. V. Petrenko. A. A. Bachurina, and N. 11. Romanov
Oef. 4). In the territory concerned, mcst of the advection fog (787-) is
due to the clearly marked advection of the very warm and humid air masses
along the south and southeast cyclonic periphery. At the western periphery
of the quasisteady eastern anticyclones, however, only 2C~ of the total
adve~,--.ion fog is observed. In the southeastern part of the European USSR
a cloudiness reaching down to the ground as fog is observed so often that
a clear relationship is observable between days with compact fog and the
hei.-ht of the locality concerned above sea-level. As to its origin, this
fog may be advection, advection radiation, or frontal fog. This is
illustrated by the comparative data of two weather stations in the region
of Saratov: Saratov AMSG and Saratov City. The first is 160 m, and the
second 88 m, above sea-level. Twice as many foggy days (excepting those
with radiation fog) are observed in the first one. In 220 cases (44ci~'),
a cloudiness reaching down to the ground was recorded as fog near the
Card 2/3
85615
Some Characteristics of Fog Formation in the S/050/60/000/011/003/005
Southeastern European Part of the USSR B012/BO63
higher station. In 262 cases with fog simultaneously at both stations,
7776 of the fog first formed near the higher station and then dropped.
Similar conclusions were drawn by G. A. Ivanova at Dnepropetrovsk and
Podgornoye (Ref. 1). The correlation coefficient between the mean
multiannual number of days with compact fog, on the one hand, and the
sea-level, on the other, amounted to 0-767m calculated for 27 points.
HH_+ 200.
The regression equation reads: X = A , where x is the mean
8.6-
,,ultiannual number of foggy days, and H is the sea-level. The total
frequency of compact fog, as well as its duration and intensity decrease
from northwest toward southeast. Transparent fog is observed rather
seldom in the northwestern and western regions of the southeastern
European part of the USSR and much more frequently in the regions east
of the Volga river. In the former two regions, radiation fog was found to
predominate, while east of the Volga river the transparent fog consists
not only of radiation fog, but advection and frontal fog as well. There
are 4 Soviet references.
Card 3/3
KOKOTOV, Yu.A.; POPOVA, R.F~
Sorption of long-lived fission products by scils and clay min-
erals. Zhur.prikl.khim. 35, no.6-1242-1245 Je '62. (MIRA 15:7)
(Fission products) ("Joil absorption)
3/080/62/035/006/007/013
D204/D307
AUTHORS: Kokotov, Yu. A. and Popova, R. F.
TITLE; The sorption of long-life fission products by soil
and clay minerals
PERIODICAL: Zhurnal prikladnoy khimii, v. 35, no. 6, 1962,
1242-1245
TEXT: The sorption of 90 Sr' 137Cs and 144Ce on a variety of Soviet
soils and clays was studied in continuation of'earlier work, by
measuring the partition coefficient K defined as where P = am-
d
ount of the ion sorbed by 1 kg of soil or clay and C = amount of
the ion in solution, under equilibrium conditions. For 90Sr, the
dependence of Kd on the pH of soil suspension was found to be pro-
nounced but varied with the type of soil. Maximum sorption occurred
at pH 6 - 8 in soils where considerable substitution of Ca 2+ by A'
Card 1/ 3
S/080/62/035/006/007/013
The sorption of D204/D307
could, however, be considerably increased by adding salts to the
solution. There are 4 figures and 1 table.
6UBHITTED: May 23, 1961
Card 3/3
S/186/61/003/002/012/018
EIII/E452
AUTHORS: Kokotov, Yu.A., Ponova. R F and Urbanyuk, A.P.
TITLE: Sorption of long-life fission products by soils and clay
minerals
PERIODICAL: Radiokhimiya, 1961, Vol-3, No.2, pp.199-206
TEXT: The expansion of the atomic industry and power stations
And fall-out from atomic explosions makes the study of reaction of
fission products with soils important. The present work gives the
first results of an investigation of the most toxic fission
products, Sr90 and cs137, by some soils and clay minerals. The
distribution coefficient of the isotope between solid and liquid
phases Kd was taken to represent sorption. Kd = r/ci, where
r is the number of mols of solute sorbed on 1 kg of adsorbent and
Cl is the equilibrium concentration (mols/litre) in the solution
after sorption. The coefficient was found from the change in
activity of the solution on sorption, measurement after sorption
being measured on the liquid freed from solid by centrifuging.
The volume of solution was always 50 times the weight of sorbent.
Before measurement, solutions of Sr90 weru diluted with their own
volume of 1N HC1 to prevent sorption of Y by the glass and kept
Card 1/7
S/186/61/003/002/012/018
Sorption of long-life fission ... Elll/E452
for 14 days. Activity was then measured In special cells for
counting on liquid samples, a type CTC-6 (STS-6 counter being
used. Active solutions were prepared from a Sr;O solution of high
specific activity in 1 NHN03 with a salt content of 0.1 mg/mcurie
of chemical-reagent purity. The distribution coefficient was
measured for six samples of sails of different types: clayey
podzolic topsoil, grey soil, chestnut soil, leached black earth,
southern black earth and heavy black earth. From the results and
published data (Ref.l: V.bl.Klechkovskiy, L.N.Sokolova, G.N.
Tselishcheva, 5, 136. Atomizdat, M. (1959); Ref.2.
N.A.Timofeyeva, A.A.Titlyanova, Izv. AN SSSR, seriya biolog., 1,
111, (1959); Ref.3: J.R.McHenry, Soil Sci.Soc.Amer.Proc., 22, 6,
514 (1958)) it appears that, on the whole, the coefficient is
higher for soils with a high exchange capacity, determined in the
present work at pH =-6.4 (which is close to the pH of the
suspension of all but two of the test soils). The authors note
that the values of the coefficient (range 170 + 30 - 1150 + 140)
determined under their conditions determines tiie intensity-of
isotope migration in a soil with water. From the ion-exchange
equation (Ref.4: B.P.Nikollskiy, ZhNKh, 3, 1, 59 (1958)) the
Card 2/7
s/186/61/003/002/012/018
Sorption of long-life fission ... Elll/E452
distribution coefficient of Sr90 depends finally on that of the
macro-component present in the system. For soils this is usually
C&2+, and Fig.1 shows equilibrium values of Kd for Sr9o as a
function of the logarithm of Ca.2+ concentration in the original
solution for leached black earth (curve 1), southern black earth
(curve 2) and Ca'9+ as kaolin. Fig.2 shows Kd an a function of
the logarithm of ratio of the amount of calcium in the system to the
exchange capacity of the test sample for kaolin and leached black
earth (curves 1 and 2, respectively). Sorption of Sr90 could,
the results show, be reduced by adding a macrocomponent, in amounts
exceeding the exchange capacity of the soil, which competear with
SOO. The authors have studied-in this connection the nitrate@
of strontium, calcium, magnesium, potassium, ammonium and sodium,
this being the decreasing order of effectiveness. The authors
also show that washing of the root-bearing topsoils with salt V/
solutions would be~practicable only for soils of comparatively low
exchange capacity and with concentrations (of Ca2* or Mg2+) not
less than 0.01 N. The authors also studied-the effect of the pH
on Kd for their test soils and also kaolin and bentonite. The
Card 3/7
S/186/61/003/002/012/018
Sorption of long-life fission ... Elll/E452
results are shown in Fig-3 (curves 1 to 4 relate respectively to
heavy black earth, grey soil, kaolin and chestnut earth) and Fig.4
(bentonite and leached black earth represented by cur-ves 1 and 2,
respectively). These curves show the complexity of the processes
studied and the need-for choosing the right pH if soils and clays
are used for sorption of Sr90 from solutions. Dealing next with
cs137 whose known (Ref.1; V.M.Klechkovskiy, L.N.Sokolova,
G.N.Tselishchava. 5, 136. Atomizdat, M. (1959)1 Ref.5: D.W.Rodes,
Soil Sci. Soc. Amer. Proc., 21, 4, 389 (1957); Ref-71 A.A.Titlyanova,
N.k.Timofeyeva, Pochvovedeniye, 3, 86, (1959); Ref.9: T.D.Wright,
J.Monahan, UKAEA. Research group. Unclassified. AERE E/R 2707.
Harwell (1958)) strong sorption on soils and clay minerals the
Authors attribute to its fixation in the hexagonal voids in the
tetrahedral layer of the clay minerals. This effect has been
studied by other investigators (Ref.10: H.W. van der Marel, Soil Sci.
78, 3, 163 (1954); Ref.11: R.F.Reitemeier, Advances in agronomy, 3,
113 (1951); Ref.12: O.Ya.Samoylov. Khimich nauki, 4, Izd AN SSSR,
M, (1959)). The authors studied Cs137 from 0.01 and 0.1 N and
sometimes I N solutions of nitrates of various cations of the first
and second groups of the periodic table, ammonium nitrate and nitric
Card 4/7
IV
Sorption of long-life fission ...
S/186/61/003/002/012/018
E111/E452
acid, by'clayey podzolic soil, southern black earth and kaolin.
The order of decreasing effect on the distribution coefficient of.
.some ions tested is' Cs+,'Rb+I NH4',-K', H+. The results showed
that micro-quantities of caesium are fixed by soils (kaolin is less
effectiVe) and that therefore washing of the root layer of soil is
likely to have li.ttle effect.' There are ~ figures, 3 tables and
3.2 references:.5 Soviet-bloc and 7 non-Soviet-bloc. The four
most recent references toEnglish language-publications read as
follows; J.R.McHenry,.Soil Sci.Soc.Amer.Proc., 22, 6, 514 (1958);
D.W.Rodes, Soil Sci.Soc.Amer.Proc., 21, 4, j89 (1957);
W.E.Prout, soil Sci., 86, 1, 13 (1958); R.K.Schulz, R. Overstreet,
J.Barshad, Soil Sci.,' 89,.16, 1 (196o).
SUBMITTED: April i8, ig6o
Card 5/7
KOKOTOV, Yu. A.; POPOVA.,-R. F.
Sorption of long-lived.fission products by soils and clay
elements. Part, 3: Selectivity of soils and clays with respect
to Sr9O under various conditions. Radiokhimiia 4 no.3:328-331+
162a (MIRA, 15:10)
(Strontium-Isotopes) (Soil chemistry)
(Ion exchange)
s/186/62/oo4/003/012/022
E075/E436
AUTHORS: Kokotov, Yu..A., Popqv
TITLE: Sorption of long lived fission products by soils and
clay minerals. III. Selectivity of soils and clays
for Sr90 under different conditions
PERIODICAL: Radiokhimiya, v.4, no-3, 1962, 328-334
TEXT: The authors continued their study of the distribution of
coefficients of Sr90 between aqueous solutions and soils and
clays of the USSR. It was found that differences in the
dependence on pH of the distribution coefficients for the various
soils can be explained by their different contents of the 2+
macrocomponent (ion Ca2+). An increase in the'quantity of Ca
in a system leads to a lowering of the height of the maximum'of
the curve relating the distribution coefficient for Sr90 to pH
and shifts the maximum towards the higher values of pH.
Analogous changes occur when consecutive macrocomponent exchange
takes place for the series Na+ I ;Nlg2+, Ca2+' Sr2+, Ba2+* The
absence of full correlation between the,,values of distribution
coefficients for Sr90 with the exchange capacity of soils and,
Card 1/2
S/186/62,/004/003/012/022
Sorption of long lived fission ... E075/E436
also, changes of the coefficient during dilution of the soil
swspen8ioris is explained by the changes in the amount of macro-
component (Ca2,I) in a system at a constant exchange capacity of
the soil. The data obtained can be used to choose for a given
soil the.conditions giving the best selectivity towards micro-
quantities of Sr90. At p1l values close to neutral,-the best
selectivity is exhibited by the soils and clays that have the
maximum exchange capacity and contain the minimum quantity of
salts. Especially good sorbent under these conditions is the
Na-form obtained by washing out Ca2+ from a soil with an alkaline
NaCl solution, followed with water to pH = 6.5 to 7. For the
moderately alkaline media 11-forms of clays and black earth are
good sorbents for Sr90.- In alkaline media a clay mineral from
the vermiculite group Showed especially high selectivity for Sr90.
In acid media clays and soils are not suitable for the sorption
of Sr-90. There are 6 figures.
SUBMITTED: May 24, 1961
Card 2/2
s/.186/6~'/'004/002/009/010
C' 0 E075/El36
AUTHORS: Kokotov, Yu. A. , P2k0_'v~a_,__R,_F
Liu Ching Chih
and Mao Shih Ch I i
TITLE: Sorption of long-lived fission products by soils
and clay minerals, II. Sorption of 144Ce by soils
PERIODICAL: Radiokhimiya, vA, no.2, 1962, 227-228
TEXT: The authors investigated sorption of 144Ce by two
different soils: 1) Southern black earth, and 2) turf -
strongly podsol soil (podsol horizon) * The sorption from
aqueous solution of micro-quantities of 144Ce on these soils as
well as the sorption on ion-exchange resin K~(-2 (KU-2) from
0.001 N KN03 was investigated in relation to p1l. It was found
that 144ce is strongly sorbed by the resin in strongly acid
solutions and strongly sorbed by the soils in weakly acid
solutions. Sorption of 1114Ce was decreased considerably on all
5orbents in alkaline solutions The authors investigated also
the possibility of desorbing 144
Ce from the soils by treating
them with salt solutions, nitric acid and various complex-forming
Card 1/2
L 54462-65
ACCESSION MR: AT5013638
MUOOOO/65/000/000/0076/0079
541.i83:546.36:631.4+552.52+553.677
AUMR: Kokotov, Yu. A.; Popov&, R. F.
TTM: Radiachromatographic study of the sorption of trace amounts of Cs-137
by soils, clays, and micas
SOURCE: AN SSSR. Otdeleniye obahchey i tekhnicheskoy khimii. Radiokhimicheskiye
metody opredeleniya mikroelementov (Radiochemical methods for determining trace
elements); sbornik statey. Moscow, Izd-vo Hauka, 1965, 76-79
TOPIC TAGS: column chromatography, radiocesium sorption, radiocestum desorption,
soil column, clay~columnmica column, cesium fixation, isotope assimilation
ABSTRACT: The authors carried out radiochromatogtaphic experiments on the de-
sorption of cesitm-137 in order to shed awe light on the mechanism of sorption
of this isotop and clays. An analysis of the chromatograms obtained
showed that Caf3YY soils
is sorbed simittaneously by the two mechanisms of ton exchange
(with a relatively high selectivity of sorption) and fixation. The fraction of
C8137 fixed during sorption by various clays, clay minerals, micas, and soils was
determined. It was found that Cs137 is fixed most extensively on vermiculites
Card _1_/2
ACCESSMN M: ATS013638
(particularly on hydrobiotite) and black earth. The lavest fixation was obsyffed~l
on kaolinite and red earth. The ability of aoila to fix trace amounts of Ca
is not a function of the mechanical composition of the soil alone, since it is
also a function of the mineralogical compositions In the authors' view, dif-
ferences in the degree of fixation of trace amounts of C9137 are one of'the
reasons for differences in the assimilation of this isotope by plants on these
soils. Orig. art. hast 2 figures and 2 tables.
ASSOCTATION: None
SUBM=D* 13Feb63 ENCL: 00 SUB OODE: GCIIVP
NO REF S07: 004 0MR.. 007
KOKOTOV, Yu.A.; POPOVA, R.F. , URBANYUK, A.?.
Sorption of long-lived fission products by the soil and by clayey
minerals. Radiokhimiia 3 no. 2:199-206-16l. (MIRA 14-5)
(Strontium-isotopea) (Fission products)
(Cesium.-Isotopes)
CC NR: AP6032120 sou:,a coDE: ui,/0346/66/000/010/003010033
AUTHOR: Roslyakov, A. A.; Bisenov, K.;
Palichev, V.
_Z22ov,
Mukhamed'yarov, F. Sh.; Sal'nikov, F. Ye.
ORG: Alma-Ata Zootechnical-Veterinary Institute (Alma-Atinskiy zootekhnichesko-
Yeterinarnyy inst~itut)
TITLE: Problems in the epizoology and diagnosis of Rabies
SOURCE: Veterinariya, no. 10, 1966, 30-33
T071C TAGS: animal disease, infective disease, rabies, precipitation reaction,
diagnoGtic madicinQ, veterinary medicine
ABSTRACT: Rabies may be diagnosed rapidly using the precipitation reaction,
and preventive measures may therefore be undertaken in minimal
time. As rabies-antigen does not appear in equal quantities
in all parts of the brain, it is necessary to take samples from
all of them; studs of the spinal cord is particularly necessary.
In the Gur'yev and some other oblasts of Kazakhstan, Babes-
Negri bodies are found infrequently. Study of histological
sections also increases diagnostic accuracy, though care must
be taken not to mistake other inclusions for Babes-Negri bodies.
Card 1/2 UDC: 619:616.988.21-036.1-07(574.
ACC MR:
AP6032120
The seasonality of rabies (beginning in December, with highest'
incidence in January-April) in the Gur'yev oblast is of
epizoological interest. it is suggested that prophylactic.
I and preventive measures be undertaken in the fall. A table
shows the results of the authors' investigation using a diagnostic
complex including examination for Babes-Negri bodies, precipita-
tioa reaction, and bioassay. (WA-50; VCBB No. 121
SUB CODE:
06/ SUBM DATE: none/ ORIG REF. Oll/ OTH REF: 001/
C!:-d 2/2
'ACC NRi AP6032120 SOURCE CODE: UR/0346/66/000/010/0030/0033
AUTHOR: Roslyakov, A. A.; Bisenov, K.; Popova, R. G.; Palichev, V. M.;
1--Mukhamed'Tarov, F. Sh.; Sal*n:LTo-vF. 7C.
ORG: Alma-Ata Zootechnical-Veterinary Institute (Alma-Atinakiy zootekhnicheako-
veterinarnyy institut)
TITLE: Problems in the epizoology and diagnosis of Rabies
SOURCE: Veterinariya, no. 10, 1966, 30-33
TOTIC TAGS: animal disease, infective disease, rabies, precipitation reaction,
diagnostic medicine, veterinary medicine
ABSTRACr.. Rabies may be diagnosed rapidly using the precipitation reactions
and preventive measures may therefore be undertaken in minimal
time. As rabies-antigen does not appear in equal quantities
in all parts of the brain, it is necessary to take samples from
all of them; siud7y of the spinal cord is particularly necessary.
In,the Gur'yev and some other oblasts of Kazakhstan, Babes-
N
Legri bodies are found infrequently. Study of histological
sections also increases diagnostic accuracy, though care must
be.taken not to mistake other inclusions for Babes-Ne~gri bodies.
Card 1/2 UDC: 619:616.988-21-036.1-07(574.12).
L 54530-65 WMA99
!ACCESSION NR.- AR5014445 TJR/0169/65100(Y/00 5/B10 61BIO 6
551.675 (470..44/46)
SOURCE: Ref. rh. Geofizlka, Abs. 5B593
AUTHOR.- P-OPGVaR
TITLE: Conditions for the formaUon of advective fogs in the southeastom European part
of the &SSR
CITED SOURCE: Sb. 150 let Meteorol. observ. Kazansk. un-ta. Kazaal, Kazansk. un-t,
:1963, 80-84
TOPIC TAGS: fo ~(dvrective fog, climatology, af r mass
TRANSLATION: Advective fogs are the predominant type of fog in the southeastern European
part of the SSSR in the cold season of the year and develop during the cooling of warm and
moist air masses of Atlantic or Mediterranean origin. Synoptic conditions for the formation
of fogs and the characteristics of air masses were analyzed for the period from 1946
through 1955. In 43% of the cases advective fogs are the result of thermal advection and
the condensation of water vapor in the surface layer of the atmosphere; in the remaining
cases they are the result of lowering of clouds to the earth's surface. In the warm half-
year, advective fogs develop as a result of evaporation; they occur after the falling of rain
------------
ACCESSION NR: AR5014445
GELLER, L.I.; SAKAYEVA, S.Z.; MUSINA, S.S.; KOGM, Ya.D.; BEIO=EVA,
L.A.; OSTROVSKAYA, R.S.; VOU)KHO7, Ya.P.; LUKIYANOVA, Ye.S.;
POFO
IA,,~,~.; MOSKATELINIKOVA, Ye.V.
Effect of noise on arterial pressure; etiology of hypertension.
Ter. arkh. 35 no*7:83-86 J1163 (MIRA 17:1)
1. Iz kliniki ( zav. - qtarshiy nauclmyy sotrudnik L.I.Geller)
Ufimskogo nauchno-issledovatellskogo instituta gigiyeny i
profes.qi.onalinykh zabolevaniy ( dir. - kand. med. nauk G.M.
IlAhametova) -
-CAr P' aiec e -a e - KONDRA'-r'YEV, Ye.14.;
DF
V,
-RAS
FOK
A.; K YIN:; AY N
,liKLYLIt, T, 1 1'r-, nA.rvtj
. I -- KkN
0 1- ~ 1p,
L, V
ALUSEYEV,
y
n furmq::~t~q w"11
I i - c 11 -ILI 118,9 u.9ing rol'ormerrr,.
,j.i7,. prom, 9 nl).11,-14-17 164. (1,2RA
IVANOVA, V.N.; M1191AYLOVA, M. I.; POPOVA) R.S.
- ~ -
Inferaction of C/,, ~--ansaturated ketones with aliphatic orgar,6-
magnesium compcwids. Zhur. ob. khim. 34 no.9:3100,-3110 S 164.
(MIRA 17:11)
DROKOVA, I.G. Ifirokova., 'FUPIK,, N.D. [TLpykp N.D.]
"aratene in the &lg& lhLnallelli 6alina Teod. unds-' :Ine
conditiona of laboratory cultivation. Ukr. bot. zhur. 21
no.5T44-49 164a (MIRA 18.-2)
1. Otdal blokhlamii Tnstituta botanik-l' AN UkrSSR.
MAZIM, Ye.G.., kand.med.nauk; IMMUNNIKOVA, Ye.V.; 013UKIIOVSKAYA, L.T.;
FOPOVA, ft. V.
Child's body reaction to repeated injection of increased doses of
BCG vaccine b7 entereal method. Vop. epid. i klin. tub. 5:37-45
158, (MIRA 14:12)
(BCG-PHYSIOLOGICAL EFFEGT)
POPOVA, R.Ya.; PROTOPOPOVA, T.V.; VINOKLIROV, V.G.; SYOLDINCV, A.P.
Functional derivatives of malodnialdehyde and their reactions. Part
14: Condensation of some allyl halides with vinyl ether. Zhur.ob.khim.
34 no.1:114-119 Ja 164. (MjRA 17:3)
1. Institut farmakologii i khimioterapii AMN SSSR.
POPOVA, R-Yae-
. .
Some derivatives of N-toBylurea. Med.prom. 12 no.11.*19-20 N'58
(MMA 11:12)
l.' Inatitut ferinal-ologii i khimioterapii ANN SSSR;
(UREA)
MPMA, R. Ta.
Some derivativeg of az7,lsulfozqlurea. Ked.prom. 14 fto.6tl2-14
Je 060. (NMA 13:6)
1. Nauchno-lesledovateliekly institut farm"cologli i khimia-
terapli Akademii moditainskikh nauk SSSR.
(URM)
S~URNOVY B.P.; POPOVA, R.A.; NISKAIEN, R.A.
Qi=titative paper chromatography of higher fatty acids in the form
of methyl esters (R-C-00-CW3,. Biokhimiia 25 no.2:368-375 Mr-Ap
160. (MIRA 14--5)
1. Laboratoriya biokhimii lipidov Instituta blologii Karellskogo
filiala Akademi:L nauk SSSR, Petrozavodsk.
(ACIDS, FATTY) (PAPER CHROMATOGRAPHY)
Ii '. 'r '. - -
POPOVA, R. A.
"Results of Crossbreeding the Local Horse with the Trotter
in Kolkhozes within the Operational Area of the Cherepovets -State
Breeding Farm." Min Hi.--her Education USSR, Leningrad Agriculture Inst,
Leningrad, 1955. (Dissertation for the Degree of Candidate in Agricultural
Sciences)
SO- M-955,, 16 Feb 56
10
Fir
pp
IR
4 qm.!
Rpig;'R .gF i
6.- . x
fn
jE.
N-U-Na iq
2' 1 B
P r
A
EL
ai
POP~',V, S.A.; Gl,,L'F,'i,'!D, ,,.Ye.
Strr--tis,~2 prnerpte-d by surface 7rinding, of hard Rl'oyE -.~'
-'t,n.1 ',nFtr. "12 no.jl:-J5-3( !; "1 1 i
f~l-
(Grinding and poliFhing)
.11
POPOVA, S. A.
"A New Method in Stimulating the Action on the
Vessels of the Ratiha and Limb During Hypertonla,"
Vest. Oftalmol., 28, No. 2, 1949. Docent.
S/075/60/015/004/012/030/xx
B020/BO64
AUTHORS: Poluektov, N. S. and Popova, S. B.
TITLE- On the MuAual Influence of the Elements Upon the Intensity o.
Radiatiozil"in a Flame. Communication 2. Compounds Formed in
the Extinction ofvlCalcium and"bt,rontium Radiation With
Aluminum, Zirconium, and Uranium Salts
V1 I
PERIODICAL: Zhurnal analiticheskoy khimii, 1960, Vol, 15, No, 4,
pp. 437 - 442
TEXT: An extinguishing influence upon the radiation intensity of Ca and
Sr exert, apart from Al. mainly Zr, Be, V, Th, Ti, U, and Cr, which is
said to be due to the formation of compounds of the mixed oxides of these
elements, and the alkaline-earth metals in the flame, which reduces the
concentration of the atoms Ca and Sr in the gases of the flame and the
intensity of their radiation. By using two atomizers supplying one flame,
the authors showed that the most probable reason for the reduction of the
luminous power of Ca and Sr by Al salts is the formation of difficultly
volatile compounds of A120., CaO, and SrO in the flame at the moment of
Card 1/4
On the Mutual Influence of the Elements Upon S/075/'60/015/004/C;-,21~;,33C)/XX
the Intensity of Radiation in a Flame. B020/BO64
Communication 2. Compounds Formed in the Extinction of Calciii.-..
Strontium Radiation With Aluminum, Zirconium, and Uranium Salts
evaporation of one drop of aerosol of the analyzed solution, The luminous
power of Ca and Sr is not reduced if the aluminum salt is introduced into
the flame by a different atomizer. To investigate the composition of the
compounds forming between Ca (Sr) and Al, or other extinguishing elements,
the method of isomolar series according to Ostromyslenskiy-Job was used,
the reduction of the luminous power of the element in the flame being
chosen as characteristic value of the formation of the compound, The flame
spectrophotometer previously des 'bed which consists of a universal
monochromator o the YM-2 CUM-2 a photomultiplier of the types
S rtype,
~3Y-19 (FEU-1;,j Wnd ~3y-22 (FEU-22)?Za mirror galvanometer, and an
acetylene- and propane-butan~-air flame were applied. The mode of inter-
action between Ca and Sr salts, as well as Zr and U salts was photo-
metrically determined (Table 1). Table 2 shows the composition of the
solutions used to determine the composition of the Sr.-Zr compound, The
curve of the ratio between the atomic numbers of the metals in the
Sr-Zr compound is plotted (Pig.. 1) on the basis of the photometric
results; the photoelectric current is recorded in percent of the maximum
Card 2/4
On the Mutual Influence of the Liements Upon S/075/60/015/004/012/030/XX
the Intensity of Radiation in a Flame. B02O/BO64
Communication 2. Compounds Formed in the Extinction of ra':,_.a,;
Strontium Radiation With Aluminum, Zirconium, and Uranium Salts
as a function of concentration. Table 3 gives the calculation technique
for the Ca-Zr compounds with the help of various correction factors, Fig.3
gives the diagrams obtained from the composition of the compounds of Ca
and Sr with Al. The maximum in Pig~ 4 (as well as in Pigs. 1 and 2)
corresponds to a molar ratio of.Ca(Sr):Zr = 1:1 (for nitrates). Thus, the
compounds in the flame are likely to have the compositions CaZrO3 and
SrZrO 3' In CaCl2and zirconium solutions (Fig. 5) the maximum of the
curve lies, in the case of a propane-butane flame, at a ratio of CalZr-312,
where Ca3Zr207 is likely to be formed, while the curve shows no distinct
maximum in the case of the hotter acetylene flame. With Ca and U. com-
pounds of different compositions form, while with Sr and U, compounds
with a molar ratio of Sr:U - 3:2, but also 1:1 and 20 are formed
(Figs. 6,7). There are 7 figures, 3 tables, and 16 references: 5 Soviet,
1 Swedish, 4 German, 3 US, 1 Japanese, and 2 British.
Card 3/4
FOLUEUOV, N,S.; POPOVA, S.B.; OVCHAR, L.A.
Flame spectrophotometer with a spectrum recorder and its uses.
Zhur,anal,khim, 15 no.2:131-137 Mr-Ap 160. (MIRA 13-7)
1. Inatitut, obahchey i neorgenicheekoy khimii All USSR laboratorii
v odesse.
(Spectrophotometer) Mame--spectra)
S/075/6o/ol5/02/01/004
13005/BOO6
AUTHORS. Poluektov, N. S., Popova, S, B.,, Ovehar, L., A~
X
TITLE, A Recording Flame Spectrophotometerland Its Use
PERIODICAL. Zhurnal analiticheskoy khimii, 1960, Vol,, 15, No, 2,
pp. 131-137
TEXT: Flame spectrophotometers using monochromators of the type 711t-2
(UM-2) (Refs. 192) or attachments type C0-4 (SF-4) (Ref. 3) have ~several'
disadvantages for flame-photometric determination of elements in high
dilution which are described in thq introduction to the present paper,
In a pre-vious paperg (Refo 7)9 the authors described a recording
spectrophotometer with increased spectrum range for the determination of
certain rare-earth metals. In the present paperp an instrument of the
same type is applied for determining several other elements, Apparatus
applied and mode of operation are described in dete;il. The speo-tro-
photometer consists of a universal monoehromator type UM-2)
connected with a mechanism for turning the wave-length drum Mg. 1) and
Card 1/3
A Recording Flame Speotrophotometer
and Its Use
3/075/60/015/02/01/00/
B005/Boo6
great advantages over ordinary spectrophotometers, especially for the
determination of metals in presence of other elements with molecular
spectra or single lines in the spectrum regions at which the metals are
analyzed. There are 8 figures,, 3 tables, and 14 references, 6 of which
are Soviet.
ASSOCIATIONI Institut obahchey i neorganicheskoy khimii AN USSR,
laboratorit v Odesae (Institute of General- and Inorganic
Chemistry of the AS UkrSSR, Laboratories in Odessa)
SUBMITTED; February 21, 1059
Card 3/3
POLUXUOV' S.B.
Mutual influence of elements on the radiation inteasit7 4-n a
flame. Report Ifo.2: Compounds formed in the quenching of radia-
tion from calcium and strontium by salts of aluminum, zirconium,
and uranium. Zhur.anal.kbim. 15 ao.4,437-442 JI-Ag 160.
(MIRA. 13:9)
1. Institute of 4eneral and Inorganic Chemistry, Academy of
Sciences, Ukrattian S.S.R., Laboratories in Odessa.
(Calcium comDounda--Spectra)
(Strontium compounds--Spectra)
ZAVEIEVA, F.D., kand.mied.nauk; POFOVA, S.I.-L-kliniclieskiy ordinator
Comlination of peripheral tubercu-Ious 1)mphadenit.is and tula-renda
(notes from practice). Vop. epid. i klin. tub. 5:253-25,1 158.
NIU 14:12)
(LM-THATICS-TUBmcuLos is) (TUIAMAIA)
PCIPOVA) S -L.; Yt~.N.
Testing Sovlet s~-i-.hetic ~` berz. Tnudy -C, f 1.:2.
f r-I ~ A -:7. 0 )
-Ltl -LC.4j
0
GRIMICH. K.P.; ZHINKIN, D.Ta.; ZUBKOT, I.A.; POPOVA, S.L.; TOMOT, A.N.
Folymer naterials in the fishing indastryo Plastozaasy w .11-.18-19
160. (MIRA 13:12)
(Polyters) (Fishing-r-Implements and appliances)
PO-pm,t, S. ~U.
"Study of the Process of Deterioration of Net Materials." Sub 29 Jun 51, RL'oscow
Technical Inst ol~ the Fish Industry and Economy imeni A. 1. Riko:,an
Dissertations presented for science and engineerirk-, degrees in koscow during 1951.
SO: SUM. No. 480, 9 May 55
h-UKOIEVA, T.V., red.; PQTGVj',. S,R,, tekhn. red.
[Theory and design of linear acc6lerators]Teoriia i raschet
lineirykh uskoritelei; sbornik statei. Moskva. Gosatom-
izdato 1962. 347 P. (kRA 15:10)
1. Akademiya nauk URSR, Kiev. Fiziko-tekhnicbnyi instytut.
(Particle accelerators)
ROCHEV, N.W.y glav. red.; VAVIIDV,~F.P., red.; IMTELI E.I., red.; GORELIK,
A.I., red.; GUDIAN, I.S., red.; KUZNETSOV, G.U., red.; MVEDET, G.A.,
red.; MODYANOV, Ya.V., red.; PANTELEYEVA, A.A., red.; POLYAKOV, V.V.,
red.; POPOV,. S.A., red.; TOPOVA,_S.M., red.; RMEVSKIY, S.S., red.; RU-
DAKOV, S.V., red.;,SYUTIKIN, A.F., red.; USOV, A.I., red.; WITINOVA, I.K.,
red.; SHKILI, P.T., red.; CHEBYKIN, N.P., red.; MEZENTSEV, S.A... red.;
MOROZOV, V.S.,, red.; OPLESNIT, I.I., tekhn. red.
[Forty years of the Komi A.S.S.R., 1921-1961; studies on the cultural
and economic development of the Komi Republic]40 let Komi ASSR, 1921-
1961; ocherki o razvitii ekonomi I i kulltury Komi Respubliki. Syktyvka2*p
Komi knizhnoe izd-vo, 1961. 154 p. (MIRA 14:11)
(Komi A.S.S.R.--Economic conditions) (Komi A.S.S.R.-Culture)
H&WINSON, G.G.;_P0FOVA.__5-..M.
New Tertiary nollusks of the Baikal type from lake deposits of
southwestern Siberiae Faleontezhuro no.4:105-109 159.
OURA 13s6)
1. Baftallskaya limnologichaskaya stantsiya Tostochno-sibirskogo
filiala Akademii nauk SSSR*
(Omsk Frovince-Mollusks, Fogail)
POPOVA, S.M.
New Miocene lamellibranchiates frm Lake Baikal region.
Palsont. zhur. no.2:33-42 161. KERA 14:6)
1. Baykallakava atav,'--4-a AN SSSR.
(Polovinka Valley--Lamellibran~hiata, Foaail)
LOGAGHEV, N.&.,~, POPOVA, S.M,
Find of mcliuske of the genus Co37D--;cu:La in Quaternary deposits
of the Iake Baikal reaion., Dokl. AN SSSR J-43 no.l-.188-190
I'Lr 162. (IMIRA 1-:2)
1 .1
1. Voston.1-mo-Sibirskoy geologi~-,heskiy in3titut Sibirskogo
otdeleni7a AN SSSR, Predstavleno, akademikom A.L.Yanshin7m.
(Sulthpay Baybet R-3gion-Geology, Stratigraphic)
(lamel.-Libram,hiata, Fossil)
POPOVA) S.M.
Paleogene and Neogene .1'resh water imollusks in the southerr; part of
the Soviet Far East. Geol.i geofiz. no.7:50-63 163. (MIRA 16%10)
1. Limnologichoskiy Ingtitilt Siblr3kof-,o otflfilenf.pi AN 313,111t,
Listvennichnoye.
LOGACHEV, N.A.; POPOVA, S.M.
Fossil mollusks of the Bayanday series (Angara-Lona intervluve)
and the stratigraphy of Tertiary sediments in the1ake Baikal
region. Geol. i geofiz. no.8:26-37" '63. (KRA 16:10)
1. Institut, zemnoy kory Sibirskogo otdeleniya AN SSSR, Irkutsk i
Limnologicheskiy institut Sibirskogo otdeleniya AN SSSR,
s.Listvennichnoye.
(Baikal Lake region-%llusks, Fossil)
POPOVA, S.M.; SAICONOV, V.V.; MARTINSON9 G.G.
Bivalve mollusks of the marine families of Solenidae,
Mactridae, Cardiidae, and Aloididae in Cenozoic deposits of
the Baikal Lake Region. Dokl.AN SSSR 149 no.1:162-1(16 Mr "63.
(WRA 16:2)
1. Limnologicheskiy institut Sibirsk*o otdeleniya AN SSSR9
Gosudarstyennyy'treat po geologichaskim izyakaniyam na neft'
v Vostochnoy Sibiri i Geologicheskiy mu* Im. A.P.Karpinskogo
AN SSSR. Predstayleno akademikom N.M.StriLkbovym.
(Baikal Lake region-MA-lusks, Fossil)
POPOVA, S.M.
Study of the Paleogerie and Neogene fresh-water mollus-lics of
the Baikal Lake region and ~'he Sovie"t Far East. Trudy Lim.
inst. 4:151-271 164.
(MIRA 17:11)
LOGACHEV, N.A.;__EOPOYA
, S.M.:.
More about the find of Tertiary marine mollusks in the cis-Baikal
region. Izv. AN SSSR. Ser. geol. 30 no.8:118-120 Ag 165.
(MIRA 18:9)
1. Institut zemnoy kory Sibirskogo otdeleniya AN SSSR i
Limnologicheskiy institut Sibirskogo otdeleniya AN SSSR,
Irkutsk.
TURSUIP V.M.; CfEBOTAJtEVA, L.G.; FILWOVA, L.M.; PPPOVA, S.M.;
PPMB,UZHESNKIY, N.A.
Lipoic acid. Part 1: Synthesis of racemic lipoic-acid and
its derivatives. Z*mtr. ob6 khim. 34 no.110662-3664 N 164
(MIRA 18al)
1. Voesoyuznyy nauel-mo-isaledovatellskiy vitaminnyy institut.