SCIENTIFIC ABSTRACT VOSKRESNSKAYA, N.K. - VOSKRESENSKAYA, T.

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• Collection: Scientific Abstracts
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• Document Release Date: March 14, 2001
• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

L 10650-63
AC(;&SIOU M AP3001221
in several 6m sub 2 0 sub 3 malts were there new veak lines. Heat curves of
unfused mixtures of cryolite - .h sub 2 0 sub 3 irdicated an endothermic reaction
between components. 'Spectral catermination was carried out by V. L. Gintburg.
The participation of T. 1. KhrarLin in carrying cut the work is ackaawledged.
Orig. art. has: 4 tables and 4 Hjures.
ASSOCIATION: Institut obshchey i neorganicheskoy khimii. im. H. S. Kurnakova. Aka-
demii nauk SSSR (Inst-Ifute of General and Inorzanic Chemistry, Acatlemy of Sciences
_SSSR)
SUBMITTM M4ug62 DATE ACQD: OlJu163 EWL: 00
OTM-- 003
SUB-CODE: 00 140 1MF:S0V:: 006
Card 2/2

VOSKRESNSKAYA, N.K.; KRIVOVYAZOV., Ye.L.
Thermal effects of the exchange reactions of oalto con-taining
analogous ions with different charges. 7hureneorg,khim, 7 no,10s
2426-2433 0 162, (MIRA 15:10)
1. Institut obahechey i neorgaineheskoy kbi-14 imeni N.S.KurnWcova
AN SSSR,
(Ion exchange) (Thermochemistry)

YOSKRESIMSKAYI, N.K.: BUDOVA, G.P.
Reaction of 1&2(~ with alkali and alkaline earth chlorides. Zhur.
noorg.khim. 5 no.9:2051-2055 8 160. (HIRA 13: 11)
1. Institut obahchey I neorganichesko7 khimii iment N.S.Karnakova
Akademii nank SSSR.
(Vidbium oxide) (Alkali metal chlorides) (Alkaline earth chlorides)

SOKOLOVA, I.D.;-V~ ~KAY~ANA~.
Surface tension of fused salts. Part 2: Surface tension of the
- NaCl, X2SO4 - NaBr. Zhur.fizAhim. 36 no.5:
systems BaC121
955-961 Yq 62. (KRA 15:8)
1. Institut obshchey i neorganicheskoy khimii imeni Xurnakova,
AN SSSR.
(Fused salts) (Systems (Chemistry)) (Surface tension)

VOSKRESENSKAYA, N.K.
Problems and tanks of Soviet inorganic chemistry in connecticn
with the decisions of the 22nd Congress of the CPSU, Objectives
of the study of fused salts in thelight of the decisions of the
22nd Congress of the CPSU. Zhur.neorg.khim. 7 no.4:709-71.1
Ap 162. (MIRA 15:4)
(Salts) (Systems (Chemistry))

VOSKRESE14SKAYAO N.K.; BERULI, S.I.
Conversions Of C002o Hd203, Sm203 and their Interaction with fused
lithium and potassium chlorides and with sodium carbonate and
sodium sulfate. Zhur.neorg.khim. 7 no.4:850-855 Ap 162.
(?URA 15W
1. Institut obahchey I neorganicheskoy khimii AN SSSR.
(Rare earth oxides) (Salts)

37628
3/076/62/036/005/0'02/013
B1011B110
AUTHORS. Sokolova, 1. D., and Voskresenakaya, N. K.
TITLE: Surface tension of molten salts. 11. Surface tension of the
systems BaCl 2 - KaCl, K2so 4 - NaBr
PERIODICAL: Zhurnal fizicheakoy khimii, V- 36, no- 5t 1962, 955 - 961
TEXT: The applicability of V. K. Semenchenko's generalized moments theory
(?overkhnostnyye yavleniya v metallakh i splavakh (Surface phenomena in
metals and melts) Gostekhizdat. M., 1957) to melts of the systems BaG12
NaCl (I), and K2SO 4 - NaBr (II), has been investigated. Systems II was
compared with the data found by V. K. Semenchenko, L. P. Shikhobalova'(Zh.
fiz. khimii, 21, 613, 707, 1307, 1947) for the system Va2so 4 - KBr. The
polythcrms for the surface tension of both systems were taken by the
maximun, gas bubble pressure mQthod with rising molar parts of NaCl or NaBr,
respectively. The 9600C isotherm was plotted for system I, the 10700C
isotherm for II. The Guggenheim equation was found to hold for I, but II
showed a major deviation from the value calculated. M. A. Reshetnikov's Y
Card 1/3

S/076/62/036/005/002/013
Surface tension of molten... B101/BI10
additivity equation, however, holds for both systemst
6 - CF + (a - dj)x/Ex + K(I - x)], where a,, the surface tension of
1 2 a2.'s
the two pure salts, a that of the mixture containing x molarparts of the
second component. K is constant for the whole range x a 0 - 1. K - 0-74
for the 9600C isotherm of system I, K - 0-54 for system II (10700C).
Calculation of the adsorption of the surface-active comprnent by the Gibbs
equation gives an adsorption maximum of 17-10- 11 g-molb1cm2 corresponding
to 0.4 molar parts of NaCl for.I, and 13-10- 11 g-mole/cm2 corresponding to
0.35 molar parts of NaBr for II. The surface tension of the melts investi-
3ated obeys the generalized,moments theory of Semenchanko on the assump-
2+ 2- +
tion that the ions Ba and SO4 , not the ions BaCl and KSO 4P prevail in,
.the melt. The isotherms for the surface tension'of the two diagonal
cross erections of the mutual system Na, XIISO 4, Br intersoot in the point
corresponding to the equivalent component ratio. There are 3 figures and
2 tables. The most important English-language reference iss J. S. Feake,
R. Botwell, J. Amer. Chem. Soc-, 76, 2656, 1954.
Card 2/3

Surface tension ofp molten...
ASSOCIATION: Akademiya nauk SSSR,
khimii im. N. S. Xurnakova
Institute of General
N. S. Xurnakov)
SUBMITTED. July 8, 1960
S/076/62/036/005/002/013
BiOl/B110
Institut obshchey i neorganicheskoy
(Academy of Sciences USSR,
and Inorganic Chemistry imeni

BUDOVA, G.P.; VOSKRESENSKAYAp N.K.
Reaction of n1obium pentoxide with molten salts of some oxy acids.
Zhur.neorg.'kbim. 6 no.6:1369-1374 Je 161. (MIRA 14:11)
-(Niobium oxide) (Acids)

SOKOLOVA, I.D.; KRiVO11YAZOV, Yo.T,.; VOSKRETENSKAYA, N.K.
Surface tension of alkal-40. retqphosrhn*,Os and al~alir.13 ear#.? 17 '
metaphosphates. Zhur.naorg.khim. 8 no.12:2625-2630 D 163. (Y-fRA 1 :9)
1. Inotitut ob-shchey I naorganicheskoy khImil Imeni Kurnakova AN
SSSRI

VOSKRESENSKAYA, N.P., kand.biolog.nauk
On the..,way to artificial photosynthesis. Priroda 51 no.3s
103-104 Mr 162. 04IRA 150)
1. Institut fiviologii rasteniy im. K.A.Timiryazava PJI SSSR,
. I
Moskva.
(Calvin, Malvin, 1912-) (Photosynthesis)

TSELINIKER, Yu.L.; VOSKRESENSKAYA, N.P.; OSIPOVA, O.P.
Leonid Aleksandrovich Ivanov; obituarr. I:zv.AN SSSR.Ser.biol.27
no.4:651-652 Jl-A f62. (MIRA 15:9)
fIVANOV, LEONID ALEKSANDROVICH, 1871-1962)

VOSYMSENSKAYA, N. P. Card. Biolog. Lai.
Dissertation: "Concerning the Effect of Cations (Potassium, Calcium and
Sodium) on the IntenBity of Photosynthesis." Inst of Physiology 6-f Plants
imeni K. A. Timiryazev, 11 Apr 47.
SO: Vechernyaya Moskva, Apr, 1947 (Project #17836)

YOSKRUnSKATA, N. P.

M 78T48
um/wlains - Plante, Physiology 'tun 1946
Medicine - Light, Effects
"Nitrogen Supnly and the Light Adaptation of Plants,"
:W, 11, Vookresenskaya, A. A. Nloblparovlob, Inat of
Physiol of Plants imoni K. A. Timiryazov, Acad Sol
tMM, 4 pp
Dok Ak Nauk SWE" Vol LI, No
Conducted tests to determine methods to adapt plants
under conditions of dim light. Submitted
for grovtk
'by Aead N. A. Maksimov 9-Apr 1948.

efte'lufluence of, Nitrogenous' AlIfientat ion and- Light
an,the Accumulation of ~, Organic Matter and the A~sIity
of Chlorophyll A and B In Lettuce," N. P.~.Voskrssen-
vat Inst of plant Physiol Imeni K. A. Tlmla7azavp
AD*& - ft i UMv 3,3/4 IT,
Ak Nauk SSSR" Vol LXV.ns No 1
~~d cm compiled. data', aiitB6 r- bUii~F&C thit: Ch:angei
In tho nitrogen-f&6din~;-.Iiieil-.'yroducea--a 6h~-, in il~
portlon
t4 szount, of *x-
to 2.
nrAerate3j loisied7th6jamit'N' ice-Imbulati=, otiaL,
Organid "as, Vhl~i 6#C44Vt0`:"'
Phenomenon, Ia'liie to - ln~re&sed: -pbotosyntulsu in
weak light where nitrogen content is In=aaead.
Submitted by Acad N. -A. Maksimov 9 Nay 49.

of wzvo lentith of RAM on wbobydrate forma-
tion and protein facToation in ULO loaf IN 11 V k I
k PeAludy Add, NatAll
4MMIX. 'A k;t.7 t.. Minflolkit Limits
litur light Caused tiluch less w4ul Itiallirr lux-IlimilAtom Own
lite Ird light. r.j~kwlv 1"t .nn And .111111"wel,
hy'llate fic~lflllulalwll In all vales IAXK"l 1. Ill'bi twill illy
Matter tooth. alth-augh rM light via* inorr rfleclise chaij
Our. Cwn CIN %U1,14Y 044 a-III A and 1.1"Irill %Yllllk so I
was (wivil to tw 0 m-sondary neither Mile vv,* in,
light IlC418111 Al"0111 Any shrlidra"I t*440111 evrillissli;
in --ine.1VICT A 4lfVlltW V101 IAMWI%ni. lIrIkT jKlkleth Ayli-
Ific.1% v" invur only in the pmwrkcv of I&ACM.)nIfirtiv me.
firky, Llr. in ptirmilm Of CL)i, and is favor"I by bluir light. -
0. hf. K~12POIT

VOSYMMSKAYA, H. Pi
USSR/Biology - Photosynthesis 51
"Reduction of Nitrates in Leaves Under Various Con-
ditions of 112umination,~' N. P. Voskresenskaya~
lust of Plant Physiol izeni K. A. Timiryazev, Acad
Sci USSR
nDok Ak NaUk SSSp,, Vol JXXIX, No 1, PP 165-168
Sectiona from leaves of sunflower and corn were in-
filtrated vith 0.02 X KNO Expts on this material
showed that presence of Ca' is necessary for the re-
2
Cuation of NO in leaves, i.e., this process is con-
nectied with Uotosynthesis. The special qompa of -
light does not affect the reduction of 903, but the
,intensity of the light has a strong I'Afluence on It.
21026

VOUPEEIVISKAYA,
Photos,,mthesis
Effect of the spectral con.-osition of light an the projortlon of svbntances
formed during photosynthesis. Dokl. Ail SSSSR e6 no. 2, 1952.
December 1952, MCLASIFIED
Monthly List of Russian Xecessions, Library of onFress,
N

The efIrct at tondiions c1 Ulu.,%jr&jjn,,
'A !he pro tucfx 4 pho*--,ymiht-v'T
K, A
.4 47. =,:It. 49,
0
)'y
i'v
ltzh. btit -O-f o~ 0%- in.
ttlc I-Acin ~y 'thrs~% n.'% t~lm
--~m~ ~tcps stage%, ~d unly -t;c lattrr Staps,
are senmfti~ to tite Ep"tral camvm~ The acc%urmlation of
Protein matter, Q10(ralb tdcct~-d by t"Alh ands of the snee-
tram. is fa--A

--log wtit)K~Yi$- 110 PO
I
0
Chemical., Abst.
Vol- 48 No. 9
may io~ 1954
Biological Chemistry
ollopectral *1
C"MR-m~rn of
nt3kin-4). .1ii(q. Nrink S.3.5. R- 93 -'-1 T!
. I
47 12281X.-Fxpt%~ with 4tiliflower plolt4; c Iit, to CL
10M. in tire Preirn't. ~f light of dil'trefif
013rarterbtlci nre dt!%crjlx(L lit ill,! bt 1,Y) sr,7- 4 phrito.
%Y11theO4 04 IS f0iltiff [ArKO" ill ill-It Ire nd-
~ntbed by pmtrin% and ionAltickitigc mtto~riaLl;, in rtd
light this fraction of J)"birts fleclillrd nil louger light ex-
sure. Apparently the first few -sec. lerve to form car
of active groups of proteins. -hich con:
tinues until the capacItY of prottin 14 !tatd- The b-Onning
of vynthc5l'i Proper ir signified h'.. a ri-ie in total and t;rvr.-M'~-
ra,limidivity of protein, mare pronrinix-vt In binr, fli.trl in
red light. In red light (lit citrIvAydrate fraction exctiviq
that l(nined in blue IN Iaination after longer thtin W-SAT.
expet3urcs bX large inargin..

TOSKRESMiSnYA. IT.P.
Zffect of the light's spectral composition on the intensity of photo-
synthesis, Trudy Inst.f1zIol,rast, 10:129-138 155. (KLRA a: 9)
1. Inatitut fiziologii rasteniy Im. X,A. Timiryaseva Akademii mik SSSR.
(Photosynthesis)

ccitfs ,,*,a
dIt "f&mlla acids
Gluminxti"I
Rif act
bekd C
-12airm with izfi~, tly In tn=fk
in the bfuc,e N-
irm and ~ 41--
Vit-
ttt;o wim
-exp4trm ffulpil
fw Cie
th ed ifn --a." - ffiEy
"rhazy a llf f - - in tent
tivel v C', "Mitent in carlmoxylic c eta
e
.c I tip -tin'

all

A.A,p with ANDREMA) T.F., VOSKRESIOISKAYA) N.P.,
"Different Ways of TTansformation of Carbon Assimilated by Plants in
the Process of Photosynthesis,"
paper presented at Intl. Conf. an Uses of Radioisotopes in Scientific Research
(UNESCO) Paris, 9-20 Sept 1957

20-2-39160
AUTHORS:

1. P. 0 Zak I Ye # G.
!~ay
,
TITLEs On Oxygen Absorption by Plant Leaves in Various Spectral
Regions (0 pogloshcheniildsloroda liatlyami rasteniy v
raznykh uchastkakh spektra)
PERIODICALs Doklady Akademii Nauk SSSR, 1957s Vol- 114, Nr 2, PP- 375-378
(USSR)
ABSTRACTs Absorption of CO carbon into different organic compounds in
h
accordance w.Ith
e processes of photosynthesis is not equal
for the short-wave range and the long-wave range of the
spectrum of physiological radiation. Some indirect data aug-
gest as cause for this the change in the oxidation-reduction
regime of the photosynthesizing cells under different condi-
tions of exposure. The intensification of the synthesis of
albumen and of amino acids, the accumulation of oreanic acids
during experiments of long duration, and the shift of the
points of compensation of the photosynthesis into the direc-
tion of stronger exposure to light in the short-wave radia-
Card 1/4 tion range permit the assumption that under these conditions

20-2-39/60
On Oxygen Absorption by Plant Leaves in Various Spectral Regions
the intensification of the process of oxidation takes place
which can be connected with the activation of the absorption
of oxygen by the leaf. 'The paper under review describes an
attempt of directly measuring the velocity of absorption of
oxygen by the leaves under ahort-wave and long-wave radiationt
400 - 580 m ("blue light") and 580 - 700 m ("red light"). The
comparison of the activities of absorption was conducted
(also in darknegs) manometrically with the aid of the Warburg
apparatus at 25 . For purposes of a direct determination of
the velocity of absorption, the photosynthesis would have
to be eliminatedl such an elimination by application of
poisons has not been entirely successful. Therefore the
authors of the paper under review carried out their investi-
gations with ethiolated material as well as with such spots
of the plant forms that were free of chlorophyll. On basis
of the results obtained it is possible to speak of the
existence of differences in the oxidizing-reducing regime
of the leaves if they are exposed to long-wave or short-
-wave light. These differences manifested themselves as
different velocities of absorption of oxygen. It appears
Card 2/4 that the carotinoids and endoxidases (flavoproteins) as

20-2-39/60
On Oxygen Absorption by Plant Leaves in Various Spectral Regions
well as the cytochrome system were responsible for the increase
in absorption.:Although these results were obtained with
regard to partg-of leaves that were not green, this may
hold valid also for green leaves. Thus it can be assumed
that the intensification of the absorption of oxygen at
exposure to blue light is based on this photochemical re-
action, i.e. on the abcorpthn of light of this sector by the
photoactive ferments of the breathing systems, together with
the carotinoids. As results of the photochemical reaction
that yields additional energy to the above systems, they must
be activated . In the case investigated by the anthors of the
present paper, this circumstance probably favored the inten-
sification of absorption by the-cell both of the atmospheric
oxygen as well as of the oxygen produced during the process
of the photosynthesis. There are 1 figure, 4 tables, and
14 referencess 7 of which are Slavic.
Card 3/4

20-2-39/60
On Oxygen Absorption by Plant.Leaves in Various Spectral Regions
ASSOCIATIONs Institute ot Fisat Physiology im.' K. A. Timil-yazev, AS USSR
(Institut fiziologii rasteniy imeni X. A. Timiryazeva Aka-
demii nauk SSSR)
PRESENTEDI March 5, 1957, by A. L. Kursanov, A&j&mjcja~2
SUBMITTEDt March 5, 1957
AVAILABLEt Library of Conf;ress
Card 4/4

VOSMSENSKATA, W,P.; GRISHINA, G.S.
~PrNMm~oilthe prolonged action of different spectral components
of light on plants [with summary in Znglishl, FAziolo rast, 5 no*2:
147-155 Mr-AP 158. (MIRA 11:4)
I.Inatitut fiziologii rastaniy im. K.A,,Timiryazbva AN SSSR, Hoslcva.
(Planti. Iffect of light on)

A

17(4)
AUTHORSs Voskresenskaya, N. P., Crishina, G. S. SOY/20-12Z-2-64/71
TITLEt On the Effect of Intensity of Spectral Composition of
Radiation Upon Metabolism and Harvest (0 deystvii
intensivnosti i spektrallnogo soetava radiataii na obmen
veshchestv i urozhay)
PERIODICAL: Doklady Akademii nauk SSBR, 19591 Vol 124, Nr 2,
pp 469 - 472 (USSR)
ABSTRACTz The differences in the ways of assimilation of carbon forming
in the case of photosynthesis in different sections of the
spectrum have an influence upon the entire metabolism of
plants. Short-wave radiation favors the accumulation of
nitrogen compounds in the leaves. A similar phenomenon is
also observed in the case of a reduction of the light
intensity. It is therefore not certain which changes of
metabolism, among them of nitrogen metabolism, are specific
of light of different spectral composition and what phenomena
can be explained by the difference of intensity of light. Data
concerning this problem are extremely scarce (Refs 1-3). For
Card 1/3 the purpose of investigating the subject mentioned in the

On the Effect of Intensity of Spectral Composition SOV/20-124-2-64/71
of Radiation Upon Metabolism and Harvest
title the authors bred beans of the type triumph (Triumf)
in a dark room illuminated with 30 w luminescence lamps
with "red" and "blue" light (Table 1). After 20-25 days of
uninterrupted illumination the authors had to give up an
investigation because of the damage the plants had suffered
(Ref 4). Since that time the plants were not exposed to light
for 6 hours daily. Resultj the affections did no'more occur.
Blue light had a highly inhibiting effect upon the longitudinal
growth of the plants (Ref 3). The period of blossoming and
the duration were in the case of both colors of light mainly
due to the influence of the intensity of light. Blue light
had a much more favorable effect upon blossoming and the
harvest of legumes. No results were determined with respect
to the absolute quantity of the harvest since a part of the
legumes remained green (unr4e) under red and blue light.
Table 2 shows much more the relative rapidity of legume
formation. In the case of a high nitrogen content in the
leaves under 'both colors of light the percentage was higher
in the case of blue light (Table 3). The protein content in
Card 2/3 the leaves was in blue light always higher than in red light.

On the Effect of Intensity of Spectral Composition of SOV/20-124-2-64/71
Radiation Upon Metabolism and Harvest
In the case of red light it remained the same no matter
what light intensities were used, in blue light, however, it
dropped with the intensity being higher (data of references 1,
2t 5, 6.,tonfirmed). Table 4 gives the protein nitrogen content
in the seeds. Unexpectedly, the protein content was somewhat
lower under blue light than under red lamps. The activity of
the cytochrome system was higher in the case of leaves exposed
to blue light. The increased capacity of accumulation of the
nitrogen compounds and the protein synthesis lead to the
acceleration of ripening and a greater harvest of bean seeds.
The results are of interest for plant ecology, in particular
for the leaves of the lower stages. - There are 2 figures,
4 tables, and 11 references, 5 of which are Soviet.
ASSOCIATION: Institut fiziologii rasteniy im. K. A. Timiryazeva kkademii
nauk SSSR (Institute for Plant Physiology imeni K.A.Timiryazev
of the Academy of Sciences, USSR)
PRESENTEDt September 17, 1958, by A. L. Xursanov, Academician
SUBMITTED: September 6, 1958
Card 3/3

WSKRESM ISKAYA 14% P.
N.A. Timiriazev institute of Plant Phyniology, USSR Acade--q of
Sciences, Moscow.
"Effect of various rays of the visible part of the spectrum on oxygen consumption
by green and non-green leaves."
paper submitted for the Third Intl. Congress on Photobiology, Copenhagen, 31 July -
5 August 196o.

YOSMSENSKAYA, H.P.; GRISHINA, G.S.
Ox7gen absorption b7 green leaves as related to the intensit7
and spectral composition of light. Fiziol. rast. 7 no. 5:497-
506 160. (MIRA 13:10)
1. X.A. Timiriazev Institute of Plant Physiology, U.S.S.R.,
Acadeaq of Sciences, Moscow.
(Plants, Effect of light on)
(Plants--Reepiration)
lit
~N W, z M.

VOMRE3E'NSKALI~ N. P., (U3SR) C- t~ I S, 111 N A, (~-, S ,
"Reduction of C02 in Various Parts of the Spectrum
in the Presence of Certain Oxidizing Agents."
4
Report presented at the 5th Int'l. Bioche~.Lstry Congrasa,
1,103cowl 10-16 Aug 11~61.

S/026/61/000/004/001/002
A166/A127
AUTHOR: Voskresenskaya, Candidate of Biological
-B-Hences
TITLE: The Artificial Synthesis of Chlorophyll
PERIODICAL: Priroda, no. 4, 1961, 83-85
TEXT: The authors described the importance of chlorophyll
in photosynthesis and discuss the recent successful experiments on
synthesizing chlorophyll, carried out independently by teams of
American and Wast German scientists. In view of the uses of chloro-
phyll in medicine, and especially for the healing of wounds, syn-
thesis of chlorophyll-'on an industrial scale could do much to re-
duce the cost of the product. Furthermore, more light will be shed
on the mechanism of photosynthesis. Academician A.P. Vinograaov haS
demonstrated that the oxygen secreted by a plant in light origi-
nates from the decomposition of water into oxygen and hydroi6en with
the help of the energy of the light which the plant assimilates in
the presence of chlorophyll. The process is very involved and en-
Card 1/2

8/026/61/000/004/ool/oo2
The Artificial Synthesis of Chlorophyll A166/AI2'?
tails the participation of other highly-active substances in the
green leaf. Further experiments have shown that photosynthesis also
depends on the proper organization of the component substances in
space, ie., within the structure of the leaf. Chlorophyll is con-
tained in the leaf in the form of chloroplasts which also contain
active enzyme catalysts in a photoactive complex. The full struc-
ture of the chloroplast has not yet been completely studied, and
attempts to reproduce photosynthesis outside the leaf have failed.
Individual photosynthetic reactions have, however, been reproduced
in isolated chloroplasts exposed to light. Oxygen secretion has
been noted, but a corresponding absence of organic synthesis from
carbon dioxide. In other cases organic synthesis is present but
oxygen secretion not. There is 1 diagram.
ASSOCIATION: Institut fiziologii rasteniy im. K.A. Timiryazeva
AN SSSR (Institute of Plant Physiology im. K.A.
Timiryazev, AS USSR), Moscow.
Card 2/2

VOSKPMENSKAYA
Chlorella. PrirOda 50 no.7:3-19 ii 161. (KM 14.- 6)
1. InOtitut fiziOlOgii rasteaiy,ime Ki,TimiryazeVa AN SSSR.
(Algae)

VOSKRESENSKAYA, N.P.; GRISHIDIA, G.S.
- Significance of light in nitrite reduction in a green leaf. Fiziol.
rast. 9 no-1:7-15 162. (MIRA 15:3)
1. K.A.Tiiniriazev Institute of Plant Physiology, U.S.S.R. Academy
of Sciences, Moscow.
(Plants, Effect of light on) (Nitrogen metabolism)

S/020/62/144/004/023/024
B144/B138
AUTHORSt Voskresenskaya, N. P., and Grishina, 0. S.
TITLEt Photosynthetic competition between CO and some other
2
oxidizers in various spectral regions
PERIODICALs Akademiya nauk SSSR. Doklady, v. 144, no- 4, 1962, 922-9251~"
TFXTs The effect of oxidizers (sulfates$ nitratest nitrites) on photo-
synthesis was studied to elucidate the differences in assimilation of
CO in varions spectral regions. CO reduction is presumably effected by
2 2
a photochemical reducing agent (R). After complete-removal of H 0 from
2
the intercellular system in the dark photosynthesis was measureds (1) on
2
10 am segments of tobacco plants irradiated for 2 - 5min with Hg quartz
14
lamps and incandesoent,lamps in a chamber containing 1-5~ of C 0 and
2'
subsequently fixed in 85% ethanol. Irradiation was not strong enough to
bring about saturation photosynthesis. (2) Colorimetrically on undivided
Card,1/3

C.
J
S/020/62/144/004/023/024
Photosynthetic competition... B144/BI38
beet leaves exposed to ped or blue light of luminescent lamps. H 0
2
(controls) and solutions of the salts weru introduced into the leaves by
vacuum
infiltration. The inhibition of 0140 assimilation was independelt
2
:of osmotic effects and constant at concentrations of 0-0075 - 0.0025 M
for 110 ) and O.Ol'- 0.0025 M for 30 and NO 0 This is indicative of a
2 4 3
competition between CO and these oxidizers in the reduction process*
2
Short-wave light inhibited the photosynthesis to a greater'oxtent than
did long-wave light. When NO wads administered without preliminary
2
removal of H 0 from the intercellular systemp fixation was reduced after
2
4 min in blue light only. When NO was introduced into beet leaves
2
still conneAd with the plant after removal of H20 from the inter*-
cellular system within 1,5 hral photosynthesis remained unahanged in red:
light$ but was reduced to 70% in blue light'. This can be attributed
neither to the short time of action nor'Ao the absence of NO reduction
2
Ca
Card 2/3

VIYLI, Yu.A.,(Viil, J.); VOSKRESENSKAYA, N.P.
Pffect of light on the biosynthasio of tryptophan in the green
veedlinga of barley. Fiziol.rast. 12 no.6:990-997 N-D 165.
(MIRA IF.-32)
1, Inotitut ekaperimentallnoy biologii AN Estonakoy SSR I
Institut fiziologii rastenly imeni K.A.Timiryazova AN SSSR,
Moskva.'-Submitted February 8. 1965*

KUTY-LYRIN, V.M - VOSOMEIISKAYA, N.P.; ULUBEKOVA, M.V.; GR1SHINA, G.S.;
Effect of the spectral composition of light on the frac-
tionation of oxygen isotopes duritig its abBorption by water
plants. Fiziol. rast. 11 no.1:7-32 Ja-F 164.
I (MIRA 17:2)
1. Institut CG "imii, i analiticheskoy khimii imeni,
Vernadskogo AN SSSR i Institut fiziologii. rasteniy Imeni
K.A. Timiryazeva Akademii nauk SSSRv Moskva.

--7-A
VOSKEESENSKAYA) N. P.
"On the question of the absorption of oxygen by green plants in light."
paper preeented at 4th Intl Photobiology,Cong, Oxford) UK) 26-30 Jul 64.
Inst of Plant Physiology im K. A. Timiryazev) AS USSR, Moscow.

GRISHINAp G.S.; VOSKRESENSK~jAj_.,~!F,_.",. ~
I.-
Light dependence of oxygen absorption bv chloroplaste (Mahler
reaction). Dokl. AN SSSR 151 no.2%452-455 J1 1634 OURA 16:7)
1. Institut fiziologii raateniy im. K.A.Timiryazova AN SSSR.
Fredstavleno akaderaikom A.L.Kursanovym.
(Chromatophoresl (Plants, Effect of light on)
(Plants, 4iffect of oxygen on)

VOSKRESEISKAYA, N.P.; GRISHINA, G.S.
Some peculiarities of the absorption of oxygen by green leaves in
the light. Fiziol. rast, 8 no.6:726-733 162, (~aRA 16:7)
I, Timiriazov Institute of Plant Physiology, U.S.S.R. Academy
of Sciences,, Moscow, I
(Photosynthesis) (Plants-ReBpiration)

ma c v
" - ~g 14"R 1 21
W MR lax- I "'If
21110 ~V, R
1 ~Ri
MIN
air
wgtgv,
Ile

VOSKRESINSKAYA Natal Iya P911,
q)n; VICHIPORZOVICH, A.A., Prof.,
G.S... red.
.9
lPhotosynthesis and the spectral composition of light)
Fotosintez i apektrallrqi sostav sveta. Yoskvap I;auka,,
1965. 308 P. (M1111A 18:10)

ZVEFIVA, TV,, RINKIIIA, L.L.
Spectrochemical determination of gold in silicate razks and
minerals. Zhur. anal, khim. 20 no,1231288-1298 165.
(MIRA 19:12)
1. Moskovskiy gosudarstvennyy universAtet Imeni P,.V. Lomononova.
Submitted May 15, 1964a
.' : ---~ ... . ..
. ;; - ~ I I -j- -

VOSKRESENSKAYA.-H ;T,;.,TITKOVAO N,F,; SHULYAKOVSKAYAp N,S.; TSZINI TSUY-IN
Idan TS ui-yilig]
Geochemlatry of thallium,rubidium,, and 34thium in igneous processes
Gookhimiia no.3t249-258 162. (KM 15:4)
I.Department of Geochemistry of the Lomonosov State University,
Honcow.
(Cauaams, Northern-MetalB., Rare and minor) (Geochamistry)

VOSKESENSKAYA, tj.T.
Thalliur in oome hyx1rothermal depo3lto of thp Gr-,atler
0 f
rGeokhirda no.8t676-683 161, HRA 17:010)
1. Kafedra geokhimji Moskovskogo gosudarstvt~nrc,!() vlrilvr..rsitpta imrl
Lomonomova.

RAYEVSKAYA, E.S.; zHUX0 I.# red,; Vqs=SENSKAY~, T
-~. rN
NEZN"OV" V.,, MWshi7 re
d N CGINA
[Studies on the history of economic thought in Hungary)
Ochorki Istorii ekonomichoskoi qrsIl Vengrii. Moskva., Sot-
Bekgiz, 1962. 21.1 p. Translated from tho Rungirian.
(Huncary-Economica) (MIAA 150)

-I.. TUCHIRMY, Naum Vladimirovich;.LAVROY, Gle'b Alskeandrovich; ZAYTSL'V.
Nikolay Petrovich; XARATYGIN, A.H., doteent, kand.takhn.nauk,
retsenzent; VOSMSEWSKIT, M.N., inzh., red.; TAIROTA, A.L.,
1 1111, 1 - ----
red.izd-va; ., i'ekh~.red,
Dechnology of printing-machinery manufacture] Tekhnologiia
poligrafichookogo mashinostroeniia. Hoekva, Gos.nauchno-takhn.
izd-vo mashinostroit.1it-ry, 1960. 376 p. (14IU 13:7)
(Printing machinery and supplies)

VOSKMICISX&YA, NOT4t
Form in vhich uranium occurs in coals. Part 1: Ixtraction
of uranium from coal by various solvents. Izv. AN Kir. &%L
Ser. eat. i tekh. nauk 2 n0-5:49-56 1600 (MIRa 13:9)
(uranium)
IA -

VOSKRESENSKAYA,,N.T.; SOBOLEVAt DOT.
. I .. 1 .1 ''.. 1''. ~ - I
More on tbanium in manganese m1nemls, GeokhWia no. 3t276-278
161. " (KMA 14 t 4)
1. Mookovskiy goeudarotvannyy univeraitat im, M,V. Lomonoscrvap
Geologicheakiy fakulftetp k&fedra geokhimii.
0zheadinakiy-44mganese ores) (Thallium)

VGSEMMiSK&YA, N. T.
Form in vhich uranium occurs in c oale. Part 2: Reaction of
humia'acida with urnayl sAlts. Izv. AN Kir. SSR. Bor. eat.
i takh. nauk 2 n0-5:57-64 160. (MIRA 13:9)
(Uranyl salts) (Humio acid)

- V Pg~~~~T.
Thalliunt concentration in m4patic rocks of the Greater Caucasus and
some other regions of the UaS,S,R. Geokh'alls no.7&573-583 161,
(MMA 14: 4)
I,Chair of Geochemiotr7s M.V.Lomonosov State University., Moscov.
(Thallium) (Rockop Igneous)

.ii. -Y
A
I'VOSKRIBETSIATA, N#To; USEVIGH, T.D*
Occurrence of thallium in manganese minerals [with summar7 in Inglish],
Geokhimiia no.7:606-614 157. (MIRA 11:1)
l.Moskovskiy gosudaretvannyy universitet, kafedra.Gookhimii.
(Thallium) (Manganesi ores)

10
AUTHOR: Voukresen-ikaya, N.T. 32-24--)+-5/67
TITLE: The Colorimetric Determination of Thallium With BeLlliant Green
in Rocks and Ores (Koloe-metrioheakoye a ridalenlye talliva s
brillanto7ym zelen~m v porodakh I rad:khY '
PERIODICAL: Zavodskaya Laboratorl-ya, 1958, Vol. 24, Nr 4, PP- 395-398 (USSR)
ABSTRACT: The method of determination mentioned is based ~Ton, the reaction
between T2Br4 ancl the oation of brilliant green. The reaction is
very sensitive and the color obtained Is stable. It is possible
-to detemine the color intensity and the concentration of thallium
either photometrically or visually by means of a number of stan-
dard samples. Determination can be carried out with an accuracy of
3-5%, except in the c4ui of very low tballiim ooncentraticna when
the error limit rises up to 20%. The separation of the tballium
2-
complex from disturbing ar-lons such as SbOlzo Slffir6s SnC141
2- 2- 2- - 2- 2- 2- -
SnBr4 , H&Br4 , CdBr4 , C10 4 , Cr207 ' CrO4 ' W04 ' C" a1:3
Card 1/2 cations such as Fb, Fe, Zn, Cu, in the presence of which a

The Colorimetrio Determimtion of Thallium With 32-24-4-5/67
Brilliant Green in Rocks and Ores
slightly y,91lowish-green coloring is prod%tced, is carried out by
extraction with ether. Colorimatrization shoull be carried out in
a O.In hydroohlorlo acid medium as hydrobromio acid with time ra.-
acts with brilliant graen. By experiments carried out with radio-
active thallium~-204 it waa foun-3 that in black ash inore than lcr~
thallium volatilizes, whereas this is not the c,-ue ia the dcoom-
pouition with lVdrofluorlo acid, and that it is possible to separ-
ate lead from thallium in galenite in an acid midium as sulfate.
200 samplas with 1/100 000 end 111OCOe. thallium wrtre InTestigated
an3 no cor_a~_~3erable deviationz were notice3 in parallel determina-
tions. An exact process of analysis as well as tables showing ra-
sults are given. Thera are 3 tables, ani 7 references, r, of which
are Soviet.
ASSOCIATION: Moskovaldly gosudarstvenW unirersitet im. II.V.Lomonoso-ra
(Moscow State Uni-ter3ity imeni M.V.Lomonosov)
1. Rock---Analysis 2. Ores--Analysis 3. Thallium--Determination
4. Colorimetry--Applications
Card 2/2

VOSKMLEgKAyA,_jj~j ZVEREVA, N.F.; VEYMARN) A.B.
Geochemistry of copper in the Devortian and Carboniferous
effusives of Karkalinsk District (central Kazakhstan).
Vest.Mosk.un.Ser.40eol. 20 no*5*.57-61 S-0 165-
(MIRA 18:11)
1. Kafedra. geokhimii Moskovskogo gosudarstvennogo universiteta.

VOSKRFSEI;SKAYA,__N.T.; TIMOFF.YEVA, I.I.V.; TOPIGIAIIA, M.
Timllium in sw-e minerals and rocks of sedimentary gonosis.
Geokhimiia no.8M~-741 162. (MM 15:9)
1. Kafedra gookhimii Moskovskogo gosudaretvennogo
universiteta imeni. Lomonosova.
(Thallium)

S/007/61/000/007/002/004
B103/B217
AUTHOR: Voskresenskaya, N. T.
TITLE: Thallium content in magmatic rocks of the Greater Caucasus
and some other regions of the USSR'
PERIODICAL; Geokhimiya, no- 7, 1961, 573-583
TEXT: The author gives a critical revision and exact definition of data
on thallium distribution in magmatic rocks, as well as its behavior in
the magmatic process in the North Caucasus which looks back to a long-
lasting geological history. She regarded this study as necessary since
the problem of average thallium content in the individual eruptive types
has not yet been solved in spite of numerous publications. From a survey
of published data the author establishes considerable differences in the
knowledge of the thallium content in ultrabasic, basic, and intermediate
rocks. Besides magmatic complexes, she also studied the respective ore
occurrences. She devoted a special paper (Ref. 17: Geokhimiya, No.8,
1961) to the thallium content in hydrothermal deposits. The thallium
content was colorimetrically determined by means of brilliant green.
Card 1/5

s/oo7/61/000/007/002/004
Thallium content in magmatic rocks ... B103/B217
Weighed-in rock portions of 1 - 10 g were disintegrated by HF, and the
fluorides removed by evaporation with HC1. Disturbing elements were
separated from Tl: (1) in ultrabasic and basic rocks by extraction with
ether from a I N HBr solution (Ref. 3: N.T.Voskresenskaya, Zavodsk.
laboratoriya, 24,395,1958); (2) in intermediate and acid rocks by cementa-
tion on copper (Ref. 18: I.A.Blyum, Zavodsk.laboratoriya 23,283,1957)-
On the strength of data obtained, the author detects that the Tl distribu-
tion in magmatic rocks of the Greater Caucasus obeys one of the geo-
chemical basic laws for thallium: (A) Its content increases from ultra-
basic to basic and acid rocks. Serpentines with a TI content almost double
as high as in the basic rocks form an exception. The author explains this
by the peculiarities of serpentinization where thallium is introduced
which then localizes in sulfides. (B) The effusives are richer in Tl
as compared with their intrusive analogs. (C) The Tl content of the
Neogene intrusion in the region of Kavkazakiye Minerallnyye Vody is
increased (in agreement to statements made in Ref. 17). The T1 binding
to acid rocks is a consequence of its geochemical nature. The so-called
"northern" microcline (north of the Musht river)(TI content 1.1-10-4%)
and entirely or partly microclinized old granites (9.o-jo-4% TI) of the
Card 2/5

3/007/61/000/007/002/004
Thallium content in magmatic rocks ... B103/B217
main Caucasus range are relatively rich in thallium, and contain up to
four times as much as the initial biotite granites. Some thallium was
introduced into the former during potassium metasomatosis. The author
also found the average Tl content in acid rocks of the intrusive and
effusive facies of the Greater Caucasus to be 1.0,10-4%. The reason of
some contents above and below this average could not be thoroughly
clarified. The majority of rocks from other regions of the USSR and
from abroad analyzed for comparison had a Tl content similar to that of
the North Caucasus. Several rocks showed, however, a higher content
(from Ukraine-0 East Tranabaikalia, and Saxony). The higher Tl content of
the German granites (E. Preuss, Ref.14:ZB.Angew.Min-3,1940) is assumed
to be due to superimposed processes. The higher values of the Tl content
in the fundamental work by D.M. Shaw et al. (Ref. 2:Geochim.et Coamochim.
Acts, 2, No.2,1952) cannot be regarded as average data for acid rocks,
since they are derived from not quite representative rocks (granites from
Finland). From papers published after 1952 the author draws the conclusion
that her own data on the average Tl content are convincing. Finally, she
determined the Tl content in ultrabasic, intermediate, and alkaline rocks
from other regions of the USSR, and observed -that the Tl content in the
Card 3/5

S/007/61/000/007/002/004
Thallium content in magmatic rocks B103/B217
ultrabasic rocks is double as high as that of the data obtained by Shaw
(Ref. 2). She explains this by the serpentinization of some rocks, and
considers her own data not quite accurate and, therefore, not final. Also
in basic rocks the author obtained a higher Tl content than Shaw, whose
content, however, well agrees with that found by PreuBs. Gabbro amphibo-
lite had the highest Tl content. Alkaline rocks displayed -the moot con-
siderable deviation from the T1 values: G.e-jo-4~,,,(author) compared with
D.M. Shaw (Rof. 1): 1-4-10-41- and 3.6-jo-4/o, and B.I. Zlobin (Ref. 16:
Geokhimiya No -4". The author explains these deviations by
- 5, 1958) 1-9-10 i6
the different genesis and mineral composition of these rocks. In the
transition from ultrabasic to basic and acid rocks, the Tl content rises
gradually in contrast to the rapid change observed by Shaw. The author
explains this by the average thallium content in acid rocks determined by
Shaw which is too high. The author calculated the average Tl content in
the magmatic rocks of the Caucasus with 0,52-1o-4%, and of the USSR with
0.75-10-4% with respect to the territorial distribution according to
Ref. 21 (S.P. Solov'yev, Rasprostraneniye magmaticheskikh gornykh porod v
SSSR (Distribution of magmatic rocks in the USSR). Gosgeoltekhizdat, M.,
1952). She states that the average Tl content in the magmatic rocks of
Card 4/5

8/007/61/000/007/002/004
Thallium content in magmatic rocks B103/B217
the USSR is approximately half as high as that detected by Shaw for the
entire crust of the earth. According to her opinion, the T1 content in
acid rocks affects the average TI content in magmatic rocks. This is the
reason of the divergence between the author's data and those found by
Shaw. The author mentions papers byt V. V. Ivanov,L. V. Tauson and
No No Buzayev, A. M. Demin and Do No Khitarov, Lo No Kogarko, No V. Koro-
novskiy,_N. F, Titkovat No So Shulyakovskaya, and the analysts:
Su Shou-tlieal Chin Tsfui-ying, E. E. Senderov. Lo To Soboleva, L. No
Soboleva. There are 1 figures 7 tables) and 2L referenoest 14 3oviet-bloo
and 8 non-Soviet-bloo.
ASSOCIATION: Kafudra geokhimii, Moskovskiy gosuaarstvennyy universitet
im. M. V. Lomonosova (Department of Geochemistryt Moscow
State University imeni M. V. Lomonosov)
SUBMITTEDs January 9, 1961
Card 5/5

VOSKRESENSKAYA, N.T.; SU SHOU-TYAN' [Su Shou-tlien]
Geochemistr-f of alkaline elements and tballium in the )Ajsht granites
(Northern Caucasus). Geokhimiia no~6&5Ww507 161. (MIR? 34s6)
1. Department of Geochemistry M.V.Lomono3ov State University,
Moscow,
(Ki3ht Valley--Granite) (Thallium) (Alkali metals)

vommosKAYA, N.T.; KOROITOVSKIT# N.V.; TITKOVA, K-F-; SHULTXOVSKATA, N-S-
Alkali elements and thallium in effusive rocks of the Northern
Caucaous and their petrogenatic significance. 7est, Moak. =*
Ser. 4: Geole 15 noo4:21-28 A-Ag 16o. (MIRA 13:10)
1. Kafedra gedchimii Moskovskogo universiteta.
(Caucasus, Northern-Rocks, Igneous)

BORISHAIISKLYA. S.S.; VOSKRESENSKATA KARPOVA, I.S.
Mineral shape of thallium In spaleritex of the VerkbiVaya, Ivayea
deposit. Hauch.dokl.vys.ehkoly; geol.-nauki no.4:135-136 158.
(MIRA 12t6)
1. Moskovskiy universitet, geologichoskly fakulltet, kafedm
mineralogii I geokhtmii.
(Caucasus--Thallium) (Caucasus-Sphalerite)

3(8)
AUTHORt Voskresenskaya, N. T. SOV/7-59-6-2/17
TITLEi The Geochemistry of Thallium and Rubidium in Igneous Rocks
PERIODICALt Geokhimiya, 1959, Nr 6, pp 495 - 504 (USSR)
ABSTRACT: Ahrens suggested the Rb/Tl-ratio its geochemical indicator
(Refs 2 and 4). This ratio is, howev?r, not constant for an
intrusion for the binding of the T1 + is more polar and its
compounds are much more volatile than those of Rb +1, especial-
ly the halides (Table 7). An example for this are the rocks of
the younger magmatic core of Tyrny-Auz (Northern Caucasus). The
average chemical raomposition of the rocks according to Z. V.
Studenikova, S. P. Solo7lyev, and L. A. Vardanyants is given
(Table 2). Table I shows the Rb and TI-contents in the leuco-
cratic granitoids in porphjroid biotite granites (Eldzhurtu
granites) and in the liparites. The content in individual
minerals of biotite granites was also determined. The consider-
able change in the Rb/Tl-ratio due to lime contact (Table 3)
or subsequent hydrothermal effects is clearly observable. Fluc-
tuations in the Rb/Tl-ratio were also found in quartz albito-
phyrene of the Kvaisi (Gruzinakaya SSR)2ead zinc deposit
Card 1/2 (Table 4). L. N. Soboleva made a chemical and petrographical

The Geochemistry of Thallium and Rubidium in IgneOV.3 Rocks SOV/7-59-6-2/17
investigation. They are also due to a hydrothermal effect. In
the course of the investigation of old granitoids of Baksan
(Table 6) an import-hnt daviation from the rocks of the young
magmatic corawas found to exist. A distinction from the old
rocks of the G'Lavnyy khrebot in the oouth-weatern part of the
area of Tyrny-Auz is puasible with the aid of the Rb/Tl-ratio.
The author tharLka Z. V. Studeniko-va and G. Nesterenko for in-
vestigation material and advice with respect to geology and
petrography of T7rny-Auz, Corresponding Member AS USSR G. D.
Afanaslyev, N. V. Koronovskiy, and Ye. Ye. Milanovskiy for re-
vising the article and for Lheir notes. Papers by L. V. Tauson,
A. V. Pek, V. V. Lyakhovich, A. S. Povarennykh, L. 11. Kogarko
are mentioned. There are 7 tables arid 18 references, 12 of
which are Soviet.
ASSOCIATION: Kafedra geokhimii Moskovskogo gosudarstvennogo universiteta
im. M. V. Lomonosova (Chair of Geochemistry of Moscow State
University imeni M. V. Lomonosov)
SUBMITTED: December 16, 1958
Card 2/2

i41,

VOSUMFSSKAYA, N.T.
WA
determination of thpllium in rock-a and ores using
brilliant groan. Znv.lab. 24 no.4:395-398 1513. (MIRA 11:4)
1. Moskovskiy gosudaretvennyy univerRitat im. M.V. Lomonosovn#
(Thallium-Analysis) (Chemic*l tests and reAgents)
(Colorimetry)

- -1 01 W~cw.. ..U~ ~- .4:1".- .- ., - --

AUTHORS:
TITLE:
PERIODICAL:
ABSTRACT:
Card 1/2
'Voskresenskayal N. T., Karpoval S. 5011/7-'13-5
inerals of the Verkhnyaya Kvaysa(Tal!iY
Thallium in the Ore M ey KvayBY)
v rudnykh mineralakh Verkhn
Geokhimiyal 195', Nr 5, pp~ 435 - 440 (USSR )
The main orea of the Verkhnyaya Kvaysa are sphalerite and
galenite. A peculiarity of theoe deposits is that the
"collomorphic" structure is located above the crystalline
one; i e.that the minerals were separated from colloidal soltAion.
Calcite -is the accompanying mineral,
The authors determined the thallium content colorimetrically
with brilliant green in altogether 40 samples of sphaleritev
galenite~ marcasite, oxidized ore and concentrames(the results
are mentioned in table 1). The change of the thallium content
4
in galenite was investigated (partly also in sphalerite) ~n
the falling (Table 2) and the striking (Table 5) of the ore
body. Table 4 gives the results obtained in the inve3t~ga-ticn
of two cross-aections of the ore vein (3 analyses each).
The collomorDhic sphalerites and marcanites havc a hiZher
thallium content than crystallized lead glance (Diagram 1). This
I

Thallium in the Ore Minerals of the Verkhnyaya Kvaysa SO-1/7-58-5-4/15,
is explained by the separation from colloidal nolution: lead
glance crystallized and on this occasion purified from the
impurities carried along.
In sphalerite a special thallium mineral, the hutchinsonite,
occurs (Ref 9). The elements Pb, Cu, Ag, T1 forming this mineral
cannot substitute zinc isomorphically; they were also precipitated
with the zinc sulfide gel and then formed micro lnclu:3ions.
The thallium content and the content of arsenic - antimony in
galenite ,jhows a correlation (Fig 2). Therefore the following
compensation may be assumed: 2 Pb2+ ---~ Tl+ - AB+3 or
2 Pb 2+ -4 Tl+ - Sb3+. No bismuth is found in the galenites
of Verkhnyaya Y,,vaysa. There are 2 figures, 4 tables, and 9
references, 7 of which are Soviet.
ASSOCIATION: Moskovskiy gosudarstvennyy universitet im,M.V.Lomonoaova,
kafedra. Geokhimii (Moncow 2ate University imeni M.V.Lomonosov,
Chair of Geochemistry)
SUBMITTF": APrJ-1 25, 1958
Card 2/2

,SAMULYLOV, YOS.; VOSMENSKAYA, N.V.
Attraction type interaction potentials between X - KI CS -
Caq C - 0 atoms forming molecules in the ground state. Teplofiz.
vys. tomp. 3 no.3t376-380 Itr-Je 165. (MIRA 18:8)
I.EnergetIcheskly Institut imeni G.M. Krzhlzhanovskogo AN SSSR.

----------- - -----
(b) M
CC NRs- "(401908 UVO 04 510631666 51
'!~)
AUTHOR: Samuylov, Yej.; Voskrosensk'Mag.N.V
-G.H. Krzhizhanovski (Energeticheskly
ORG: Institute of Xnergetice Im.
Inatitut)-
TITLE: Reaction cross section of carbon and oxygen atoms
SOUROE: Toplofizika-Vookilch tempera tur, v.3, .no.6, 1965, 851-859
TOPIC--TAGS., particle cross section, carbon, oxygen
~ABSTRACT; The article presents the results of the calculation-of--l-8
tq-p-es-_-_of7re -ac ti~o_n-pot-e`fit1_alv_,fo-r_ -car b--o-n- amd_~~ __ on-atoms-- on erg1"-,to_-
--qx-yg . - - II IV
the- -.fuzid6mental---di6-d6ci-a-tlon limit*- Based -on data on the potentials,
calculations were made by kinetic theory of the effective reaction cross
sections of carbon and oxygen atoms for a from I to 3,1 less than or
equal to s, and for temperatures from 1000 to 10,OOOOK. Atoms of carbon
and oxygen can interact at various potentials corresponding to different
types of energy levels of the carbon monoxide molecule. The latter can
be determined according to the rules for combination of the orbital and
spin moments of the atoms, as well as by comparison of the electronic
configurations of the molecules. The article presents calculations of
18 different types of interaction in tabular form. It is concluded that,
-card 1/2 UDC:-532-186.3

ACC NRI AP6001908
the effective reaction cross sections of oxygOat.carbon, and nitrogen
atoms reacting with an oxygen atom Increase with a decrease in the atomio
number of the element since, with a decrease in the atomic number, the
mean radius of the electron shell Increases. Orig. art. has: 10 formula
2 figures, and 5 tables. i
SUB CODE: 20/ SUBM DATE: 061?eb65/ ORIG REPI, 005/ OTH REF: 023
caj,d 2/2

rL 43156-66 EWTW/E'4P(t_)/ETI IJP(c) JD/.Tcl/(;I) 16610001000T0-02-5[0-029
ACC NR: AT6oz2642 scuRcs coDst uR/OOOO
AUTHOR: Samuylovj, Yo. V.; Voskrosonskayap fie Ve
ORG: none
TITLE: Attractive-type interaction potentials between U-Li atoms in ground states
SOURCE: AN SSSR. Energeticheskiy institut. Issledovaniya po fizichoskoy gazodina-
mike (Studies of physical gas dynamics). Moscow, Izd-vo Haukay 1966, 23-29
TOPIC TAGS: lithium, ground state, potential energy lc~~"' %jrA
A13STRACT: A method is proposed for calculating the curves of attractive-type inter-
action potentials for the case where the rotational constant B. is expressed in the
form of a power series in (,r + 1/2) (whore v is the vibrational quantum nuriber) includ
ing the second p