SCIENTIFIC ABSTRACT BARANOV, V. I. - BARANOV, V.I.

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• Collection: Scientific Abstracts
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• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

1_57 S~M 67913
44~T~ SOV/20 129-5-20/64.
AUTHORS: Baranov, V~. I~, Khristianov, V. K., Karasev, B. V.
TITLEo Photoneutronio Method of Determining the Concentration of
Deuterium in Natural Water
PERIODICAL: boklady Akademii nauk SSSR, 1959, Vol 129, lir 5,
PP 1035 - 1037 (USSR)
ABSTRACTs The usual method of determining the deuterium concentration
in water exhibits certain difficulties. They can be eliminated
by the here described method, when making use of the photo-
cleavage of heavy water (Refs 2,3). The deuterium concentra-
tion can be easily and quickly determined in water within an
accuracy of + 1 % by combining an adequately strong f-radia-
tion source ';ith an efficient method of neutron modefation
and recording. The water sample is irradiated by a,Lquanta
beam from Na 4. The neutron resulting due to the r tion
D2 (pn) Hi is recorded by appropriate counters. The thresh-
old of this reaction is 2.22 Mev, its cross section being
1.2.10-27 cm2 (Ref 4)- Under etandard conditions of measurement
the number of emitted neutrons is proportional to deuterium
Card 1/3. concentration in water. By determining the counting rate of

1. 7 ~ 13,
.1-hotoneutronic Method of Determining the Concentration SOV/20-129-5-20/64
of Deuterium in Natural Water
both a standard sample of water and the sample to be in-
vestigated, the deuterium concentration in the latter can be
easily calculated. The above method was experimentally
checked by the authors. Na24 served as -radiation source.
With itsoPradiation energy (2-76 Mev) ,felement Be only is
capable emitting neutrons under the action of hard r-quanta.
The (~,n)-reaction cross sections are approximately th6 same
for D20 and Be. Figure 1 shows the arrangement in which the
measurements were made. It consists of a cylindrical lead
block 1 which is bedded in a paraffin reflector 2. In the
middle of the block there is a roughly spherical container 3
with three tubes 4,5,6. 20 proportional counters 7 with B10-
concentrated boron fluoride are arranged in an annular spacing
of the lead. The radiation source 8 is situated in the center
of container 3. Due to the short lifetime of Na24 the authors
were forced to content themselves with the accuracy of
�2-5-1- 1-5% determined by a single calculation. Up to a D20
concentration of 0-1784% a linear dependence of the counting
rate on the deuterium content was determined (Fig 2,1). The
Card 2/3 error due to water contamination was determined. Such elements

Photoneutronio Method of Determining the Concentration
of Deuterium in Natural Water
67 9 13
SOV/20-129-5-20/64
as B,Cd, C1 are apt to distort the determination result.
Figure 2, 11, shows the results of such an experiment. Thus
C11 in an amount of 0.24~ causes the determination result
Of D20 to appear lower by 1%. Apart from Na24, Y88 might be
used for tht 4b:k>~4 purpose (T-105 days), but the required 24
amount should be larger by dozens of times as compared to Na
Natural isotope ThC'' (T1208) seems to be promising. Its an-
ceBtors RaTh (Th228) and MaThl(Ra228) have half-lives of
1.9 and 6-7 years respectively. The authors investigated the
applicability of RaTh. The preparation generates neutrons it-
self. Chemical purification reduced this emission to about
1/5. Another poseibility would be that of preparing metallic
99.9 - 99.99% pure thorium enriched by radio thorium. By pre-
liminary experiments the authors confirmed on principle the
determinability of deuterium in natural water within a high
accuracy. There are 2 figures and 6 references, 3 of which are
Soviet.
PRESENTEDi July 17, 1959, by A. P. Vinogradov, Academician
SUBMITTED; July 14, 1959
Card 3/3

STARIK, I.Ye., otv.red.; SHCHMAKOV, D.I., akademik, zamontitell otv.red.;
BAIMOV, V.I., prof., zamostitell otv.red.; WMTSKIY, N.S., aka-
demik, red.; POLKANOV, A.A., skademik, red.; VINOGRADOV, A.P..
akademik, red.; AFANASIYEV, S.D., red.; GFMING, E.K., prof., red.;
PEKARSKAYA, T.B., kand.geologo-mineral.nauk, red.; IVANOVO B.V.j
red.izd-va [deceased]; GUS-XVA, A.P., takhn.--ed.
Uransactions of the sixth session of the Committee on the Deter-
mination of the Absolute Chronology of Geolo.gical Formations,
May 22-27. 1957J Trudy shestoi sessii komisaii po opredoleniiu
absoliutnogo vozrasta geologicheskikh formataii; 22-27 maia 1957 9.
Moskva, 1960. 306 p. (MIRA 13:7)
1. Akademiya nauk SSSR. Komissiya po opredeliniyu absolyutnogo
vozrasta geologicheskikh formatsiy.
(Geological time)

STARIK, I.Ye., otv.red.; SHCIMUAKOV, D.I., akalemik, zame~3titell otv.
red.; BARANOV, V.I., prof.. zamestitW ;:-tv.red.-, VINOGRADOV, A.P.,
akademik, red.; POLKANOV, A.A., almdemik, red.; SHATSKIY, N.S.,
akademik, red.; AFANASIYEV, G.D.; GMING, E.K., prof., red.;
PELARSY-;~YA, T.B., knnd.gool.-miner.nauk, rod.; S11-1K.114, S.M., rod.
izd-va; MAKUNI, Ye.V., tekhn.red.
[Transactions of the Seventh on the Daterminstion of
the Absolute Chronology of Goolo.-Ical Foi:imllionz] Trudy Sedlmoi
sessii Komissil. po opredeleniiu absoll-atno-go vozrasta geologicheskikh
formatsii, B-12 maia 1956 g. Mosk-va, 1960. 432 p. I
kMIRA 13:6)
1. bkademiya nauk SSSR. Komissiya po opredelenay:i absolyutnogo voz-
rests geologicheskikh form3-tsiy. 2. Chleny-Irm.Tres-pondenty AN SSSR
(for Starik. Afanasyev).
(Geology, Stratigraphic)

S/00 60/000/006/001/010
B002YB067
AUTHORS: Baranov V, I Khristianov, V K. Karasev, B, V
TITLE. Neutron --borometr Prof 2_2 I'd? ly
PERIODICAL: Geokhimiya? 1960, No 6. P,) 490 497
TEXT: At the radiogeokhimicheskaya laboratoriya Instituta -eokhimii i
analiticheskoy khimii im. V, I, Vernadskogo Ali SSSR (Radiolilyeochemical
Laboratory of the I -ns-ti tute -- of Geochemistry and Analytical Chemistry
imeni V. 1. Vernadsk.iy AS USSR) -an instrument for neutron-burometric
profiling -Nas developed in the course of the last years. In principle
it consists of a sleigh (Fig.1) carrying a 5 cm llh2t-.k paraffin reflector
layer (3), a moderator (7) with the neutron source (8) and detectc)rs
with oriented action for neutrons and gamins. quanta., The first one (9)
is a proportionality coiniter in a boron- cadmium qcroen (11), the. second
(4) is a packet of Ur-6 STS-6 aloCen counters ~rotecteci by a load
coating (6), A small cadmium metal foil i~, placed b~~tvi-en thi, ~~ounters
The detectors are arranred symmetrical]", to thp 1-11(il'it-lon oource at, a
Card 11,3,~-

~5535
Neutron-borometr.ic Profiling
S/007/60/000/006/001/010
B002/'Bo67
distance of 38 cw, The apparatus is drawn by/a car at a apew.d of
6. 8 km/h; the car carries the r!' 14 SC-1 Yecorder N3th a polonium
,07
beryllium source with 0,8 1 1 n/sec 200 t~' 300 Irflp/se- could be
counted. The sensitivaty was experimentally examined between 0,01 and
O~15% B 20 ) "The range of detection reaches to ab(,~O- Ili '20 .1-m Chlorinp
is recorded as anomaly by the n.n probe i.e., 0.&'~ NaCl -C.-rrespond to
the effect of 0.01% B 203' The limit of boron detectior is 6% NaCl.
Disturbances due to uneven ground are unimp,-,rt,-int and ma,~. lie easily,
corrected, The practical " estng of the instrument provi~.d its superiori.
ty over recordings by means of individual test-s TherQ are 7 fiCures
and 10 Soviet references.
ASSOCIATION; Instit.lat t)-eokhimii i analiticheskoy I-hiniii irn
V. I Vornadskogo Mloqkva (1.1101-It-11"e of
AN SSSR; 1
Geochemist,ry and Analytical Choinst-ty imt~-,zli V~ 1~
Vernadskiy AS USSR. Moscow)
SUB14ITT ED April 7, 1960
Card 2/31~-

,BARA1iOV,.-V.I.; MISTIANOVA, L.A.
Concerning the notes by S.M. Graahchenko and othero on V.I.
3aranov and L.A. Xhristianova's article "Radioactivity of
waters in the Indian Ocoan.0 Geokhimita n0-7:651-652
,6o. (MIRA 13:11)
(Indian Ocean--Radicactive sustances)
(Grashchanko, S.M.)

.3a4LIO,V--Y,I.; KNORRE. K.G.
The first Soviet geochronological scale. Geokhimiia no-7:6(l
l6o. (MIPL,~ 13:11)
(Geological time)

i)r, -) 2 8 / D'5 o,17
AUTEORS Baranov, V. 1. and Vachnad:,e , Yu. A.
TITLE: Correlation of natural rad-,.o.ictive emunation.,; -ill "11C
air in rclat-ion to gcolo6,ic conditJons in Ui(, cx~-,Tlplc
of areas of cortlain crystalline and scdir.-ien'L1;ir-,. rock--,7,
PER10DICi~L:. Referativnyy zhurnal, Geofizika, no. 7, 1962,
abstract 7B99 (Tr. ln-ta -,eofiz. :~T~' Gruz 603R, 19
19601
TEXT: The content of the decay products of -cadon an,,i t.horo- i i i
air at a height of 1 Lind 4 m wa,-, i,,le-isured over ,;urfaces, 'v"ith a d 4
verse lithologic composition. The method of i-~ieasurement %,.,a.,; to (~x,-
pose a negatively charged wire, 10 m in lon,-th, for _-' huurs -~it the
same time of day. Re radia'Gion of the rOU31a Surface was deter-
mined simultaneously by means of a Pa-1 (RP-1) device. 6even
points were investigated in all. It was established as a reotilt
that the concentration of thoron decay prodticts corralEitr-~-, ,-;ell
_with th~e radioactivity of rocks ill the 1110,-ISUrement area. Viere is
Card 1/2

Correlation of' natural ... i).1-',`,3/ D'-~ 07
no such correlation for the (luc;,ty pro(luoto, of It i,-, i.m1)o,.,,.-,-
ible, to use the ~i,.T I licki Me t'-06 Uo 013 t ii:l: I iLo 4~- I, 10 11 u pe oi, t
radioactivity, since thc concentrat.ion
is averaged for aii itrea thut cmnoL bo coinp,,-ircii 1,o Lht~
ing off thoron. /-Abstracter', note; Complete
Card 212

BARANOV, V. I.; NOVITSKAYA. A. P.
Effect of moisture on emanation. hadiokhimlla 2 noolf:485-490
,6o. (MIRA 13:9)
(Radon) (Radioactive substances)

20622
A07 1
AUTHORS% Baran ov, V. 7 J,
-Yakovi-e-7, Y-,~,V,
TITLE. Radioautlva-.-n
Developmen-,
Kh:i:a.- r )g.
PERIODICALF Zhurnal
MendeLeye-rwL, i~-'10, N~,
TEM The rad,'oa,1-'".-.,a-:
1. - r
- . I---
" .1 ;
I ~ '. f -, -
riale ~n ~he

pure mate
It 14
highly sensitive, d e,~ c-.,- d r~S7P Maz- f x 1,
particles and '.he
its specificit~j
traces of thG

the more rec:ent air' .I cn if

R T
1 " R e f
13-15) whi,,,h
Card 1/10

2 ~-)6 2 2
AO: A,_;,_
Radioactiva' A.7-aly~
samples . By
Y
and purity t1he I I --~ o P, 7 ~t :7 a' tte
usual ca1cu!ati,.,.-. :~f
~d
leads to an estimat.ion q
according to the energi,~.~ -I 2M a Tje of
admixture preseDt i-.:
sections correspc-rd--.ng t~ d m", v--.7 Thr
measurement of the a7:e~, ~,17 p'r.
photopeak contou-c of tie '2a-F:-,*.a-,
gation does not en-ft -ft-a' it
completely de3ayz; by the Lmt~ e e a e -n a Mad~, gf-a'MA.-
G -,r L-,g -,v ithi[~
scintillation :3pp-.Y.. )!-C
-de ----!~.7 )f 6
problem. Referen 7. th
application of h, r a:: C e
conducted a
semiconductor --manuf act-rirg
Card 2/10

2 2
2 1
Radioactivatior.
mixture el
tion spectrometei. A q G 10 N
Y
tector and the 3,,-, i
rounded by a lea 1. i .1 T,,- f' Ir, 71 1 1 L 7 3 ltd t
50-chanziel .1
The analyzer -'I.c) baok-d -I I n
time, combined with a t. e
- o- 4 1
ray tube. R e,7~ E,
to obtain the npE 7
T- 1~ 11 7 ',I'e a, -7 C D Y
capacity. The 1,
The estimated Zn i- ~C- -3~ 7 0 llo p ard ga, -.:-m
2-3-10-7,,, -1 irn p
Fig. f -zh 'Ad e.
,r4 a'
Further work wao --ri n-,
processing of t~,-e f -
Znq Cu, As and S~ f I
(about 0.5 f e .7 ~7
Card 3/10

20~22
D I I ~D 2 1
1. 0 0~_
Rad i oac t iva t.. A-j a P- D e
salts of the a I
previously
Int" ~,I~,M-'
and ether. The wo~:~
num cases and i--radatc-
for 24--2B houre. .4 f e -:~i p.: f -i Tr, p Y
Na, the standsrd~. 7.-,. r, r 7. e e r
I 1::Ti e f. F.
analyzing thall' F,,- d f a
T1204 for 1:. Ej
med in the -F
~ ~.'j
level , about 40,~6 e Tt,-, h E I
Ye: _~:7 rer-ders th
X-ray emission wi4-~-. a.-
er s7gY n
analysis diffici~.,. for, -.rT 43 1 q a.- F4,s. '2 A~-,vs ~,h,~
---e I.:t' i!-- Th "v of the
spectra of two 4n a:~; L e r
_DW E (T
photopeak of As+S- s,
j7
Table 1 shows the no s, 1,,'i,, Cu Z-,-S*r, F_%d A~? ad-
mixtures in the i L;.i a, t e a.-, a i Y a I s4 the adiEix-
tures was carried ou.t t'~e t-le rh,-Yt.,)r;;ak+ heilghts of +VhE,
Card 4/10

RadiouctiW.tit-M A-7 P-i- T.
sample being analy..-.le-d End tl--3 m.")Mert
Correction for tlh-~ g and
w e r e m. e a s u r eY-.. dii 1 z n o. - 2 .Th e ~i .2 r% -t,-, C 0! i t f-t
was cz3 tima ted aftei ca-I nulatf t1hf- a~ ---lute mas s of th admiytu-t- . a 1 a 2
gives 'the re'-luit"'. of thn of ,f
carried out on tho jamma- ~~)c tr:,,:rPtr-r Y. I'l")"It in d-4,
cussi ng the futu:~E- P:: :,z~ tA cf I I-g the -,,FLd4 t2 on Trr-. thc,4 o'
ana lys i s th e ail th o:- t:.ra t of t:-,e d --' r-f 41 t i. ir. 11-C I ly iT~-~ i t -T h e
main difficulty g-,sn, as tti'- fact Ih;it zdh,~. act- -t-
ed with neutrons '~-eoTi~7 `~aelseivcs. _-,-s Eivcn a,:, an
example. Another 11-*.-, ;.,.
o th~? Sj7,-r-~ S It E,~ t ~- j! M
obtained in th~, -,ue t.:. w h 1' c!%
give a contin,.~ clu, t.- fl)~--,d diffi-
culty ii3 the (I :~tF-o "r, 1 - o
-I o- r 'a, e a t .,,n of
which are weak in
the main problerq
Card 5/10

2 ,,-,22
0 1 /A C,
Radioactival.; t
new effective m p t Y, i:.~ f h e i 1 r F, - M, 1
of admixtures from ',-he ',--M3ir, t t.~:_ mm, ical
purificatior i-i thi!4 case T-n)-it .7i;)t %p t-jo tho
of *he short-liv4.rb arti.i.,ity, 1,-*,,,t,, Vic.
lysis. By deve 10_4riZ
the t r 0,--, -,,y 1 6
0 7: P
a pp 1 i c ab 1 e f o _- an a I y L7,4- n g m, a ' -2 r i a h c E?. t e c T) t n s i -., e
gamma-emitters them~eiverj. It- i f,., - t",e a- c c;;: mm e d 1 d e c r e i ~i c t 1, c C, L, LTI p -
ton background by usintz mr~re 2e_-fecte3 %:,-pR-atuE-. Th& authors
have developed a one-eh~-,-sl,
automatic-, recordin of' ltl-lt~ h .9 C. 0 71 t E. 3 T
+
of the simult,,n&c-,..- '.r i7
,vith subseouent cou-nting, )f tll~~
ence scheme. A third f.!~ t`r~= T, r I ry z t -a I s r. e c -
I, A
trometer fr)r sign-1, f-' t
lessening the i Z~,) 1 2..:, -vit
necessity of dt-.velopin- iii. o r 's h:- r d
Card 6/1")

2o622
"/0(
7 /60/r
it-.0, 51 /A020
Radioactivation Analysis of Pure Materials and Proopects of -1 tz Development
isotopes. When investigating the admixtures of short-lived radioactivity,
the activation analysis should be carried out near the reactor for this
reason. The radio-chemical operations should be eliminated. Finally, the
authors suggest that in order to detect, certain elements by the activation
met'hod, it, would be most feasible to use fast neutron fluxes. in the case
of detecting Al and 17C ~tdmiytures, for example the reaction on fast ne-atronz
should be used: A127 I,- 24(n,p)Na24.
(n,,3Qj,a24 and Mg The reaction on neutrons
in the resonance ener,-y field might also prove useful in this connection.
A si~;nificant incroase in the monochromatic neutron flux would then be ncc-
essary .. The activation analysis method should be developed to,'.'ard a ccnl~
ant
miri:imum' loss in its performance and toward increasing its productivity. Auto-
:~_ation of nieasur~!,monti3 is sugCested, as wt~il as of tho ri~3ult procos3ing,
yieldinj I L,
; a conplet~:! analytical chart of the S,,mplo. This can De facilitated
by introducing into industry the activation netlhod of analysis of elements;
by the computine technique. There are f igures, , 2 tables and 23 re-
ferences: ~ Soviot, 14 English.
Card 7/10

L0622
SZ06316010051005ZC11ZC2!
A051/AO29
Radioactivation -'.nalysis of Pure 'Materials and Prospects of Its Development
CIRI
+.
cd
0
0 5
channel
Figure 1': Gamma-spectrum of an
activated sample of
Card 8/10 -9 ilicon.
too As' 557ka
cu~ Sb 55SvO
4-
to 50.
4.
r,
0
0 0 V to 30 WIWI-
Figure 2 channel
Gamma-3pectrum of two activated
samples of thallium

20622
/c,"
" /~ C)I/oc,.-, /00 5/0' /0~ 1
A 0:-, ','// ANQ
Radioactivation Anslysi-a. of P.2z-e F-:-pp:t4 -;~' -;:3 Dev,31opment,
Table Re~qul ti, -~f gt" y, .1 f
Sample Ni:-.
1 2, 9 0- 10-1
I C
I "D 3
4 4 10- 3 0 1 f3 1 10
Card 9/10

20622
.A.,c "I /A 0 2
Radioaotivat4
Table 2.~ R e,.~,u I f -i f
...... ~,,z ie "era
Sample No. 70
2
5 2, 6,
Card 10/10

BUUMV, V.I.; GORBUSHINA., L.V.
quantitative determination of lead and bismuth radioisotopes
in the air of mines. Atom.energ. 9 no-1:56-57 Jl ,6o.
(MIRA 13:7)
Ojead-Isotopes) (Bismuth-Isotopes)
(mine gases)

BARANOV, V,I~; CHEN' YUYoVL?Y [CHIen V-6-wil
Isolating radioactive calcium from mica for isotopic analysis
Zhur,anal,khims 15 no.2:163-165 Y&r-Ap 160. (MIRA i3:7)
1. Institut (-,eokhimii i analiticheskoy khimii im. V.I.Vornadskolplo
All SSSR-;- Moskva.
(Calcium--Isotopea) (MICA)

A
83671
S/048/60/024/009/004/01;
B01 5/'BOb_-')
AUTHORS: Ba r a n ov , V ~ I G r 0 m 0 v D_z' _he_1_e_E_0Y_,__ -BS ZY Q n & Q h Q n g
Bay, MalyshevA, T. V, Morozov, V. A. , Khot in, _B,_ A~_,__
Chumin, V, G~
TITLE; The New Isotopes Ir 184 and Pt187
71 __1 f
PERIODICAL: Izvestiya Akademii nauk SSSR. Seriya fizicneskaya, 1960,
Vol. 24, No. 9t PP- 1079 - 1082
TEXT: The spectrum of the conversion electrons of the iridium fraction was
analyzed by means of a P-spectrometer of the type Danish~ This fraction is
formed during the disintegration of gold bombarded with 660-Mev protons.
Radiochemically pure iridium without carriers was separated from a bombard-
ed gold plate weighing 1 2 g (Ref. 1). The spectrum of the Ir conversion
electrons showed some lines with a half-life of 3.1 0.3 hours. These were
identified as L-120; M-120; K-264; L-264; M-264; K-391 and L-391 transitions,.
Experimental data on these lines are collected in Table 1, The measured
iridium spectrum ~Series 1) is shown in Fig. la, part of which is shown in
a higher resolution in Fig. 1b. In addition, the L-., M-., and N-11ines of the
Card 113

1,,', 6 71
The New Isotopes Ir 184 and Pt187 s/048/60/024/009/004/015
BO13/Bo63
120-kev gamma transition were studied by means of a -spectrometer with
double focusing (of the type 7r-F2) and increased resolution (Ref. 2), The
data obtained are given in Table 2, They indicate that the observed gamma
transitions take place in the even-even osmium nucleus (Figs. 2 and 3). On
the strength of the data obtained, the authors suggest a decay scheme for
184
Ir (Fig. 4). In addition to the above-mentioned lines, the iri.dium
fraction contained numerous lines that belonged to other Ir isotopes~.
'186 185 188 187
Ir ' Ir , and Ir .Next, the determination of the half-life of Pt
is described. The half-life of this isotope was found to be 2.0 t 0.,4 hours.
For comparison, tile half-life of the well-known isotope Pt186 was determined.
Its half-life of 2.5 + 0-3 hours is in good agreement with the results of
Ref. 7. There are 4 figures, 2 tables, and 7 references-, 3 Soviet
Card 213

b3b7l
The New Isotopes Ir 184 and Pt lof",
s/o48/60/024/ooq/oo4/ol5
B013/B063
ASSOCIATION: Institut geokhimii i analitichesko.) khimii im, V.. I.
Vernadskogo Akademii nauk SSSR (Institute of Geochemistry and
Analytical Chemi5try imeni V. 1. Vernadakiv of the Academy of
Sciences USSR)
Obl'yedinennyy institut yadernykh issledovaniy (Joint Institute
of Nuclear Research)
Card 3/3

B.~RANOV, V.I. ; KNORU, K.G.
Yirst Soviet geochronological scale. Vent.0 SSSR 30 no.9:
102-103 5 160. (MI;iA 13:9)
(Geological time)

ZAYTSEVAp L.L.9 kand. khim. nauk; LEVSHINq B.V.;_BARANOVt V.I.p red.;
KHLOPINq N.G.v red.; KNYAZEV, G.A,q otv. red,;- -AROlip-G.-M. 9 red*
izd-va; BOCHEVERO V.T., tekhn. red.
[Letters from V.G.Khlopin to V.I.Vernadskii; 1916-19431 Pislma V.G.
Khlopina k V.I.Vernadskomu, 1916-191+3. Sost. L.L.Zaitseva i B.V.Lev-
shin. Pod obshchei red. V.I.Bartinova i W.G.Khlopina, 1961, 88
(MIRA U,:46
1. Akademiya nauk SSSR. Arkhiv.
(Khlopin, Vitalii Grigorlevich, 1890-1950)

1. J- ,9
KHLOPIN, Vitaliy Gcorp-1-7ovich W,9(~ T'50)- ZINTSEVA, L.L.;
LEVS11ill, '~'V. , IMIYAM, G.A., otv, red.; BAI'LANOV, V.I.,--.
- red.
[Letters vritten to V.I.Vernadskii, 10,16-19431Pis'na k V.I.
Vernedskomu, 1916-1943, Sost.: L.L.Zaitseva i B.Y.Levshin.
Pod obsbchei red. M.Baranova i N.G.Khlopina, VoOlknra,
Akad. nauk- 1961, 88 p. (M-iiA 15:9)
(Vernadskii, Vladinir Ivanovich, 186,1--1945)

3/007/61/000/002/001/004
B107/B217
AUTHORS: Baranov, V. I., Titayeva, N. A.
TITLE: Content of uranium, thorium, radium, and ionium in the
Quaternary deposits of the valley of the Lena river
PERIODICAL: Geokhimiya, no. 2, 1961, 110-114
TEXT: The content of uranium, thorium, radium, and ionium (Th 232 ) in young
and recent continental deposits at the Lena river was studied. The purpose
of the work was to clarify the migration of these elements and the problem
as to whether an absolute age determination with the aid of radioactive
methods is possible. In 1958, 25 samples of peat, recent mud, and sandy
loam have been collected; the larger part of the samples was from long fro-
zen soil. The investigation of the samples was conducted jointly by the
kafedra geokhimii (Department of Geochemistry)and the kafedra merzlotoveder.-
iya (Department of Permafrost Study); K. I. Smirnova took part in the chemi-
cal analyses. Uranium was determined by luminescence analysis according to
L. L. Leonova (Geokhimiya, no. 8, 1956), ionium according to L. A. Khristia-
nova, and radium and thorium were radiochemically determined. SiO 29 Cao,
Card 1/4

S/007/61/000/002/001/004
Content of uranium ... B107/B217
Fe20,, MnO, C02 , and the humus content were determined in the spektrokhimi-
cheskaya laboratoriya (Spectrochemical Laboratory). On the strength of
these analytical values, the samples can be divided into two groups: 1)
samples with more than 10% humus (11 samples): uranium 4.0 _ 15~O 10 g/g
(average 9 10- 6g1g); thorium 0.1 - 1.2 10- 5glg (average 0.5 10- 5g/g); ionium
0.5 - 4,1 10- 6(in equilibrium units) (average 1.5 10- 6g1g); radium
O~3 - 2z3 10 -6 g1g (in e uilibrium units) (average 1.2 10-6g1g); mean ratio
Th/U = 0.5; U/jo = 6; UNa = 8; Jo/Ra = 1.2. (11) Samples with 'Lower humus
content (14 samples): uranium 1.6 - 7.1 10- 6g1g (average 2.9 10- 6g1g);
thorium 0.7 -- 1.4 10-5g1g (average 1.0 10- 5g1g); ionium 1.6 - 3.9 10- 6 g1g
(in equilibrium units) (average 3.1 10- 6g/g); radium 2.0 .. 3.9 10- 6g/g
(in equilibrium units) (average 2.8 10- 6g1g); mean ratio Th//U = 3.4; U/10
0.95; U/Ra = 1.05; Io/Ra = 1.2. Summing up: The first group with more than
1W~ humus is enriched in uranium but poor in thorium, ionium, and radium;
Card 2/4

S/007/61/000/002/001/004
Content of uranium B107/B217
the radioactive equilibrium is considerably disturbed. The second group
with lesb than 1C~ humus has a content of uranium, thorium, ionium, and
radium that is about as high as the average content in sediments and soils;
the radioactive ratio between uranium and radium is, independently of the
age of the samples, not disturbed in contrast to the ratio uranium/ ionium,
The parallf:1 behavior of radium, thorium, and ionium indicates a joint mi-.
gration, most probably together with clastic and colloidal material. This
is also confirmed by the correlation to the silicon and calcium content. A
correlation to the iron and manganese content was not established. The
sediments studied may, in principle.be used for the absolute age determina-
tion by the ionium method, but further studies would be required. Professor
V. A. Kudryavtsev is thanked for his help in field and laboraty work,,
There are 1 figure, 1 table, and 14 references: 12 Soviet-bloc. The two
references to English language publications read as follows K. M. Strom,
Nature 162, no- 4128, 1948; R. F. Flint, Glacial and Pleistocene Geology,
N- Y~, 10/47c
Card 3/4

S/007/61/000/002/001/004
Content of uranium ... B107/B217
ASSOCIATION: Kafedra geokhimii Geologicheskogo fakul'teta Moskovskogo
gosudarstvennogo universiteta im. M. V. Lomonosova (Depart-
ment of Geochemistry of the Geological Division of Moscow
State University imeni M. V. Lomonosov)
SUBMITTED: July 14, 1960
Card 4/4

-BA4AN(N,-V.I-,-DU LETYANI [Tu Lieh-Vion)
Geochemistry of ur-anium and thorium in granite rocka of the
Kyzyltau Massif (central Kazakhstan). Geokhimiia no.12:1059-1067
161. (II-MRA 15:3)
1. Chair of Geochemistry, Lomonosov State University, Moscow.
(Kazakhstan-Uranium) (Kazakhstan-Thorium)

BakNOV ~_ '~. 1 1 - T'iTIORRE y K. G.
JAILge and evolution of mettioritic terrestrial natter in the
light cf recent resoarch. ~ika xio.21:15-31 161, (IMMI 14-:11)
(Meteorites--Age) (Earth--Age)

BAILANW, V.I.: KNORRE, K.Cr.
New dev,~-Iopment in determining the absolute reolopical age. Ves'"
AN SSSR 31 no-10:131-232 0 '61. (maA 14:9)
(Geological time-Congresses)

BARANOV, Vladimir Illicb; GORBUSHINA, Lyudmila ValontlnoNma; VORONOVA,
A.1cp reda; POPOVA, S~1-11., tokhn, red.
[Safety measures in uranium mines] Voprosy bezopasnosti v urano-
vykh rudnikakh. lloskva, Gosatomizdat, 1962. 185 P.
(MIRA 15:7)
(Uranium mines and mining-Safety ireasures)

S/169/6-2/000/011/003/077
D228/D307
,'JJT I IOR - -13aranov, V.I.
TITIL: The age of tile Earth
P"ERIODICAL: Referativ-nyy zhurnal, Goofizika, no. 3.1, 1962, 9,
abstract 11A42 (Byul. Komis. po oprodeleniyu absol-
yutn. vozrasta geol. formatsiy, 'd4 SSSI~, no. 5,
1962t 7)
TSX T Accordin,( to the data of O.Yu. Shraidt the primary
condensation took place 7 billion years ago. According to the data
of lead and other methods the age of the Larth is - 4.5 billion
years, i.e. the -"arth must 'Llave been formed in the period betl-ieen
4.5 billion years, ago and the time of nucleogenesis. The author
recommends that this circumstance should be taken into account when
formulating a theory for the Zarth's formation. The advantage of
considering jointly both the formation of chemical elements a-ad of
the solar system is also noted. When determining the scale of rock
ages, it is recommended that those figures which do not require the
Card 1/2

S/169/62/000/011/003/077
The age of the Earth D223/D307
introduction of serious errors, based as a rule on hypotheses,
should be taken into account. The practice of reckoning discordant
figures to be rejects and of not taking them into account is, in
the author's opinion, incorrect. Yk.i. Tugarinov is working on the
use of these figures for the purpose of exposing the causes of
cp
their discrepancy.
Z7Abstracter's note: Complete tra-nslatio,12
Card 2/2

i
-c n
o i: lent In ifl. arL t o
Al
Io
,71 r I~J, e

BARAYOV, V.I.; VILENSKIY, V.D.
Deter,unation of long-lived beta-particle radiators in
atmospheric fallout. Radiokhimia 4 no-4:7*.86-492 162.
(MIRA 15:11)
(Radioactive fallout)
(Beta rays)

L 1;. 79
5/186/62/0014/001i/004/004
E071/E333
AUT110i,'LS: i3aranoy. V-T- and Vilensltiy, V.D.
010
TlTLE: Precipitation of Ilb- froi-ii the atmosphere
F-Ei~IODICAL: Radioldiiiniyal v. 4t no. 4 t 1962, 49,-> - J.,C)G
TEXT: A determination of the interisity of the precipitation
of Fb 210 from the atmosphere i~as carried out using two vessels
containing sortie distilled water ~~6uz%tvd about 3 it, apart. I r-I
addition, the concentration of ~b in a number of samples of
rain and snow and samples of ice on aeroplanes, collected from
various points of the USSR, was dettrmined. 'rile fliethod used
for the separation of 11b 210 before its d ,etermination will be
described in a later communication. it was found that the
intensity of precipitation varied greatly but the mean value-s
were close to those calculated for a uniform distribution over
the northern hemi~ybere, or somewhat higher. The data obtained
indicated that Pb' could be an important component of the
natural radioactive background of the Earth surface. On the
basis of data on the content of Pb 21.0 in cloud droplets an
CArd 1/2

1-recipitation of ....
approximate estimation
from air by cloud drvj)Lct~j
cbud droplet.5 ab,5orbed
the surroxinding air.
S/186/62/004/004/004/001i
E071/E333
of the efficiency of the removal of Pb 210
11
was carried out. T1 119 in(112W(l that
% ronaiderable proporti. of Pb f rom
There aro It tables
SUBMITTLD: October 26, 1961
Card 2/2

BARANOV9, V.I.., prof.
Radioactivity and geology. Veat. AN SSSR 32 no.2:17-22
F 162. (111RA 15s2)
(Nuclear geophysics)

: . 'j )j
otv. red.; Zrm- otv-
red.;, ',itJIANOV, V.I., i;rof., zar.. otv. r-C-cl.;
rcel.; JULKAI"C"v, A.A., red.;
G.D., rcd.; MURG, E.K., 1;rof., rod.;
PEKARSKAYA, T.B.,,.kahd.-geo-I*-miner* nauk, red.; ARON, G.E.,
red. izd-va; GALIGPTOITA, L.M., teldm. red.
(Tranonctions of the Tonth Session of the Comnission on the
Doterviinp,tion of the Absolute Ago of Geological Formationsl
0
Jum 11-IC, Y,161ITrudy desiatoi .7~essii... ; 5-10 iiun:*L;~ 1961
1-fo'sIm%, Izet-vo Akad. nauk SSSR, 1962. 379 p. (VIRA 15:11~*
1. Ahademiya nau]c SSSR. Komssiya po opredeleniyu absolk-utnogo
vozi-astaLpologicheskikh formatsiy. 2. Chlen-korrespondent
Akadoinii nauk SSM (for Starik, Afanns'~.ev).
(Geological time)

V.I. RARANOV, L.I. lOfEISTTANOVA (USSR)
"Radioactivity of oceemic sedil:-)(nats."
Rep,)rt -Prest-nted -at the Conference on Che,,:~istry ,i' Eirth's Crust..
14-osoov,, 14-!,) Mar 63-

LAVRUKIIINA, AvLusta ',,orstantinoviia; ' ALT'I'SHn'!i - qar--arr- Via d~ONT-a;
-,-. - Cl ~71 . :~ro v
FAITLOTSKAYA, Farmi IlliLi-chrla; ') ' I , . f-, 0-, -
red.; E.S., red.; GUSEVA, A.P,., toklin. red.
[Radiochemical analysis] lladiokhimicheskii analiz. Mloskva,
~jt.) ~. (Yr-Lk 16.12)
17.d-vo Al: S&Sli, 196-31. 1 , I
)

BARMOV, V. 1., URUS, Ye. V.,, red KILIZ1117,TS(N, I. Vred,
TIMUlLiCV. V.V,, red , 7!'~!UjV~ Yl.:,., red,;
D.I.., red,,
[Interaction of the 9ciences in the study of the earthl
Vzaim.ode~stvie nauk pri -~michi---nii-
AN ISSSIR,

VlNCG,'-tAXV, A. P. , akademik, otv. red. ; BARANGV, V. 1. , red. ; BAf6UKGV,
V. L. , red. ; BEUS, A.A. , red. ; W-L-TASSRO-,--R-G. , red.;
GERASlMOVSKlY, V.I., red.; KORZHINSKIY, D.S., red.; RONOV,
A.B., red.;'TUGARINOV, A.I., red.; KHITAROV, N.I., red.;
SHCHERBINA, V.V.,, red.; TARASOV, L.S., red. izd-va; DOROKHINA,
I.N., tekhn. red.
[chemistry of the earth's cnist]Khimiia zemnoi kory; tnidy.
Moskva, Izd-vo Aknd.nauk. Vol.l. 1963. 430 P. (MIRA 16:3)
1. Geokhimichaskaya konferentsiya, posvyashchennaya stoletiyu
so dnya rozhdeniya Akademika V.I.Vernadsliogo, T-loscow,i963.
(Geochemistry)

BA~-~MOV, V.I.; SEADYUKOVA, A.S.; GORBUSEINA, L.V.; NAMOlr,
YEFRIKIDA, Z.11.; PANA,12111FOVA, red.
[Lpboratory work and problems in radiometry] Laboratornye
raboty i zadachi po radiometrii. Moskva, Atomizdat, 1964.
307 p. (MIRA 17:'~)

AFPIIIAS'Yl',V) G.D., otv. red.; BAR.4Nov, v.j., prof., zam. otv. red.;
SlICHERBAYOV, D.I., ~:'KacjeT~.ik, A.A., zA,:ademik.
red. [deceased]; STAAIK, rodiiktor ;
VINOGRADOV, A.F., akadeirilk, 'IFRLING, E.K., prof.,
red.; FEKARSKAYA, T.B., Rana. nauk, red.;
BORSUK, A.1,11... red.izd-va; SINKINA, G.S., tekhr. red.
[Iransactions of the Ilth session of the Cerixiission on the
Detormination of the Absolute Age oC Goololyic,,;l Fc;rmationq.,
May 12-27, 19631 Trudy o(~innzicitsatoi ,:e,,;sil ... ; 1-'--"7 r,"aifl
1963 g. Mobkva, Izd-vo All SSSR, 1963. 390 p.
-17:4)
1. Akademiya nauk SSE!. Komissiya ~o opre~e-leniyu --bsolyut-
nogo vozrasta geologicheskikh formatsiy. 2. Chlen-korrespon-
dent AN SS~R (for Afanaslyev, Starik).

iih~a;uv) V.I.; ~--JhOZOVA, N.G.; YU:.';~SEILVA, K.G.; GRIGORIYEV, G.I.
Geochemistry of some natural radioactive elements in soils. Pochvo-
vedenie no.8.11-20 Ag 163. (MMA 16:9)
1. Institut geokhimii i analiticheskoy khimii imeni Vernadskogo.

BARANOV, V.I., Prof.
A conference on geological time hald at Moscow. Vest. AN SSSR
33 no.9t89-90 S 163. (MIRA 16:9)
(Geological time)

BARANOV, V. I.; PAVLOTSKAYA, F. I.; TYURYUKANOVA, 'E. B.; et al
"Some Regularities of the Distribution and Migration of Radioactive Elements in
the Soi-l Stratum."
report submitted for 2nd Intl Conf, Peaceful Uses of Atomic Energy, Geneva,
31 Aug- 9 Sep 64.

BAIMOV, V.I., doktor fiz.-matem. nauk, otv. red.; K111TROV, L.M.,
red.
[Radioactive contmrination of seas and ocu-nnsl Radiw-3c-
tivnaia zagriamennost' morei i olceanov. MoAva, Izd-vo
"Nauka," 1961,. ~27~ 1). (MIUA 17- 5)
1. Akadeti-ya nauk SSSR. Okeanograficheskaya korissiya.
2. Institut geoklAmii i analiticheskoy khimii im. V.I.
Vernadskogo All SLZR (for Baranov, Khitrov).

BARANOV, V.I.; KHRISTIANOV, V-K.; YARASEV, B.V.; PANOV, G.I.
Neutron-boronometric sampling of outcrops and mine workings.
Izv. AN SSSR. Ser. geofiz. no.3:349-353 Mr 164.
(MIRA 17:1)
1. Institut geokhimii i analiticheskoy khiviii im. V.I
Vernadskogo AN SSSR.

T

5/00491
AGGESSION NRs AP4030336 (64/000/003/0349/0353
jx=RS1 Baranoyf Ve Iol Khristi&novp Ve Ko; Massy, Bo Vol Panoy# Go I*
TITM Hoasuring baron by, the neutron method in outerops and rdne worldage
SOURCEs AN SSM. Isv. Ser. soofis., no. 3# 1964, 349-353
!TOPIC TAGSt boron., neutron sonde.. neutron loggings SNW 5 counter
;ABSTRAM The authors describe a portable instrument used for boron detection and
Imeasurement by neutron bombardment and furnish results of field tests. To make
ithe instrument portable it was necessary to reduce the weight of current devices
!and., consequently., to reduce the power of the neutron source. The neutron
:retarder and reflector were combined in a single block. Sondes near the inversion
!value were employed,, and this required a minimal length of 40 cm. Shorter sondes
'were too insensitive* The first instrument constructed weighed 16.5 kg and was
tested in the field in 1960, A later model., tested for th3 present study., weigba
':but 8 kg. The instrument has three parts: 1) a retarder-reflector of 5-liter
,capacity; immersed in water; 2) a casette with two SM-5 counters it a P-shaped
!boron-oadmium shield; and 3) a panel with amplifier, discriminator, transmitter,
'.Card 1/2

1ACCESSION NR: Ap4o3O336
iactuator, generator, and rate counter. Sensitivity was found to be 0.01% B203 for
la 10% decline in counter rate. Results on surface rocks and in mine workings show
I
;the instrument to be satisfactory for rapid determination of boron mineralization
without selection of rock samples. Results of profiling and of laboratory tests
Ion the areas investigated are in good agreement. The Jnstrument is suitable for
iexposed or slightly covered rocks* Either continuous or isolated readings may be
made, and work may be carried out rapidlys permitting large areas to be covered
!quickly* Orig, site haBt 4 figures.
!ASSOGIATION: Akademiya nauk SM Institute gookhimii i analiticheskoy kbi-14 im,
IV& L Vernadskogo, (Acadermy of Soienoes S=j, Institute of Geochemistr7 and
Analytical Chemistry)
SUBMUTED a Via& DATE AGQt 29Apr64 EML: 00
SUB GODEs 93 ND R1W SM OD2 OTEM ODO
of*
...... .

ACC NR,
AP6033 173 SOUPICL' CODE: UR/0033/66/043/005/107411080
AUTHOR: Baranov, V. 1.
ORG: none
TITLE: Age of the Earth, heavy clements, and moicorites
SOURCE: Astronomichcskiy zhurnal, v. 43, no. 5, 1966, 1074-1080
TOPIC TAGS: meteorite, radioactive decay, earth, heavy e) em ents, earth age,
absolute age, uranium isotope, lead isotope
ABSTRACT: Results obtained on the absolute age of the Earth, the chemical
elements, and meteorites, using radioactive decay methods, are discussed. The
value of 4. 5* 109 years for the age of the Earth and the meteorites is considered
accurate if it is assumed 'hat both Nvere formed a' the same dime and from the
same protoplanetary material through the process oA'differentiation. The upper
limit of the Earth's age is found to correspond to that of the heavy chemical
elements; this was computed by comparing the present and initial ratios of
sotopes U235/U238
uranium i . The initial ratio, estimated empirically, was found
to be equal to not more than 1. 64; this corresponds to a uranium age of 6. 6' 109
Card 1/2
UDC: 523. 231
-Cord

BARANOVq V.I.; PAVLOTSYMA, F.I.; FFDOSFYFV, G.A.; TITRIT-KANOVA, F.B.;
RODTONOVA, L.M.; BABICHEVA, Ye.V.; ZATSEPITI.,, L.-I.; VOSTrKID7'11.)
Prinimali uchastiye: MICEL'YANOV, V.V.; BELYAY--7~'t, L.I.; "S.!.;
MODCHANOVA, I.V.
Di5tribution of Sr9O on the surfEce horizon of soils of the Soviet
Union during 1959-1960. Atom. energ. IS no.3:246-250 Mr 165.
(M1RA IS: 3)

T
,1A"^.?*.( 1! , . ., :,T-C70'J.~ , *.." .
Sl,o~-t-livinr, r-.f-(Ion d-'si.-Ae--ra',';(,,n in
~Victeor. 1 f- :~ . .( '.'T T ~~ ~ ( i - " )
. .-I P . ~ . . - ,

ACC NR,
A1,6033 173
S()URCII CODL!
AUTHOR: Baranov, V. I.
ORG: none
TITLE: Acyc of the Earth, heavy elements, and meteorites
SOURCE-': Astronoinichuskiy vhurnal, v. zl~, no. 5, 1966, 1074-1080
TOPIC TAGS: meteorite, radioactive dcca, , earth, heavy elements, earth age,
absolute age, uranium isotope, lead isotope
ABSTRACT: Results obtained on the absolute age of the Earth, the chemical
eloi-nents, and meteorites, using radioactive decay methods, are discussed. The
value of 4. 5- 109 years for the aue of the Earth and the meteorites is considered
accurate if it is assumed that both were formed at the sai-ne time and f-om the
same protoplanetary material through tile Process of diffel-cliLiation. The uppcr
limilt oil the Earth's a(fe is found to correspond to that of the heavy chemical
elements; this was computed by comparing the present and initial ratios Of
L k A
-U235/-U238. The initial ratio, estimated ernpir-ca"ly, was found
aranium isotopes L I
-Lo be equal to not more than 1. 64; 'this corresponds to a uranium age of 6. 6* 100-
Card 1 2 'UDC: 523. 231

ACC NR: APGO33173
years. The upper limit of the age of the Earth's crust is estimited ~7,s the time
necessary for radiogenic lead isotopes to reach their present concentration in the
Earth's crust. This time depends on the lead -to - uranium ratio, which -if taken as
33 (based on estimated abyssal rock age) indicates 7. 5- 109 years to be the upper
limit of the age of the Earth's crust. Recent. estimates of 6* 109 years and over,
therefore, for terrestrial rocks and meteorites are not considered unreasonable.
Oria. art. has: 2 figures. [Author's abstract] [SP]
SUB CODE: 08/ SUBM DATE: 11Jan66/ ORIG REF: 006/ OTH REF: 001/
C.,d 2 2

UAYANOV , '~ . .' ~ , P - (-, (I- , ~':! - , i, % ~ "
Gron ', ~,c. i r-n U -i li - I.",, p '71 ., I .
, I .. 1 .11 1,4 - '!~~ ": 1 , .; - 1-: :'',1"
- I(', c .
., r a r ~d i I ~ 4 rl(, " A I , ~( " 1 " L " ) -. 1; " ;1 ~~ : 11 ),

!- 4 -,. f - -- - - l7 7'
I ~ 3 - . -- .
-Cl - ; " 1 5 1 ~ ov I -,, ~ , "; , '. , I ~: ~ , ~~ i I ... I I . 'i .. 1. - . . . .

V.I., profesaor; AMZOV, A.Ta., skadamik. glavnyy radaktor; LIVA-
'7-AdVo.-N.A., professor, otvatstvennyy redaktor; RASSTRIGIN' M.A., tekh-
nichaskiy redaktor.
[Kuligaahl Kuligash. Izd-vo Kazanskogo filials, Akademii nauk S=,
1948. 72 P. (Akademiia nauk SSSR. Xazenokii filial, Kazan. Trudy.
Sariia biologichezkikh i sallskokhoziaistvennylch nauk, no.1)
(MLU 10: 2)
(Aktanysh District-Swamps)

7~ ': '~' 1.,~V ,'V . I
25440
,:)vye -liotsenovoy 71ory `rLe. ED'U!-n.
110. 11 S. '10-9,
SO: f I I I
30, l'ibb

RARA OV, V.I.
Forest history of the Volga-lama region. Izv.Kazan.fil.AN SM.Ser.
biol.i sellkhoz.nauk no.1:37-61 149. (MLRL 10:2)
(Volga Valley--Trees, Fossil)

ti R M Pi () V, V.
-P A 41P" j=
Prei,.aration of the products of reduction of carbon dioxide, labelled
with carbon 14"
I by the chloroplasts outside a cell. A. P. V-1nogradov, E. A. Boichenko;
an,d V. - -A '18, 32-- 7 44) 7937h.-
~ov, Doklady Akad. Naut S.S.S.R. 7-795l); cf. C.A.
C!-J, ro4vas~ white clover or primala, isolated from the cells, were examd. in C(),,,
labelled witli; C in t1ae preselice of 241- C) by ma.,iometric techi:ique. Control expts. w;Ji7
boiled ctloroplasts gave no C111 activity in the exts., but active cl,,loroplasts 6ave sig-
n1ficant activity'A and almost all activity was pptd. by Ba as a complex, which contains
O.,)c,'~ P and is free of N, consisting largely of carbo-hydrate-like materials, giving ~Lroilc
acid reaction, and other carboxylic acids. The latter increase in proportion oil cloudy
days, ti-,e former predominate in specimens taken on sunny days. In Prolonged expts. some
70% of the retain;d c14 is extractable with EtOll, in the ketose fractions. Thus, the
process of reduction procceds via carboxyl)c acids do not reduce Cu, then uronic
acids, then ketoses. G. M. Kosolapoff

BARA-MV, V.I., professor; KIMBERG, V.A.: redaktor; KRASHIMINNIKOVii, V.F.
--- rakhnicheakiy redaktor.
[What the Kaqrshin sandstones and the Yergeni Hills sand tell us;
the history of vegetation In the lower Volga Valley] 0 chem
govoriat peschaniki Kaqrshina I peski Ergenei; k istorii rastitel'-
nosti Nizhnego Povolozhlia. Stalingrad, Oblastnoe knigoizdatel'stvo
1952. 46 P. (MLRA 8:8)
(Volga Valley--Paleontology)

'-- BARASOV, V.I.: VASILsYZVA, I.M.
On the way to the utilization and reorganization of the vegetation
resources of the Tatar L.S.S.R. 1zv.X&zan.fil.AN SSM. Sar.biol.i
sel'khoz.nauk no-3:23-48 '5Z. (HuL 10-.2)
(Tatar A.S.S.R.-Botany, Economic)

BAPANOV, V. I.
"Steps in the Development of Flora and Vegetation of the USSR DurinE the Tertliar~7
Period, " Re-viewed b37 A. Kbriahtofo-vich, Bot. Zhur., 7, 1-1,o.4, 19':)22.

~,, .1 1. 1 . -Ii / I
BARANOV,V.1.
New fossil flora from ferruginuuB anndatone of the Yergeni series
discovered by V.A.Nikolsev. Izv.Kazan.fil.AN SSSR. Ser.geol.nnuk
no.2:27-36 154. (MLRA 8.11)
(Stalingrad Province--Paleobotany)

.,RARANOV, V.I. (,Kazan')
History of flora in the works of Kazan botanists. Uch.zap.Kaz.un.
115 no.10:70 '55. (MLRA 10:5)
(Kazan--Botanical research)

RARANOV, V.I.; MOKSHINA, O.M.
%Wm - , .
New species of the Paloozons flora of Kamyshin. Uch.zap.Kaz.un.
116 no.1:183-185 '55. (MLRA 10:5)
1.Kafedra sistematiki rastenly.
(Kamyshin district--Trees, Fossil)

BARANOV, V.I.
"Middle Miocene flora of Zaleacy near Wisnioviec" [in Polish]. Hanna
Gzaczettewa. Reviewed by V.I.Baraz*v. Bot.zhur.41 ite.2:280-281 F 156.
(MlaA 9:7)
l.Kazanskiy gesudarstvennyy universitet.
(Vishnovats region-Palsobotany) (Czcczettowa, Hanna)

BAR&NDV, V.I.; NIKOLAYEVA, O.G.
Fossil wood from the qpper Gretaceous deposits of the Yenisei
Ridge. Dokl.AN SSSR 107 no.1:125-127 Mr 156. (MIRA 9:7)
l.Kazanskiy goeudarstvennyv universitet imeni V.I.Ullyanova~
Lenina. Predatavleno akademikom V.N.Sukachevym.
(Yenisei Ridge--Trees, Yossil)

BAqANOV, V.I., professor.
Developmental stagon of the flora and vegetation of the U.S.S.R.
in the Tertiary poriod. Pt.4: Now materials on Tertiary flora.
Indexes of plant and animal names mentioned in the text. Uch.
zap.Kaz.un. 116 no-10:5-47 '56. (MLRA 10:3)
(Paleobotany, Stratirraphic)

AISKS YICV, Aleksey Mikhaylovich; GUSEV, Nikolay Alekseyevich;
doktor biologicheskikh nauk, otvetstvennyy redaktor: MAKAROVA, O.V.,
redaktor Izdatel'stva; POLYAKOVA, T-V., takhnicheskiy redaktor
CNffect of mineral nourishment on tho water balanca of plants]
Vliianie minerallnogo pitaniia na vodnyl reatenii. Moskva, I2d-vo
Akad.nauk SSSR. 195?. 223 P. (MLRA 1():B)
(Plants, Effect of minerals on)

BARANOV, V. 1.
Photography and drawing in a botaniE;t'E; work. Bot.zhur. 114
no.8:1117-1119 Ag '59- (MIU 13:2)
1. KazanBkiy gonudarstvannyy universitet im. V.I.Ullyanova-
Lenina.
(Botanical resoarch)

RARATIOV, V.I.; MIKMYLOVA, L.P.
Pal7nological characteristics of Pliocene sediments of the
Ik River in Menzelinsk District, Tatar A.S.S.R. UL
ugh. zap. Xaz.
un. 117 no.9:223-226 157. -(MRA 13:1)
l.Kazanski7 gosudarstvenn7y univerBitet im. V.I. Ullyanova-
Lenina. Kafedra sistematiki rasteniy.
(Ik Valley--Pollen, Fossil)

RARANOV,- Vladimir Isaakiyevich, prof.; YAKMOVSKAYA, T.A., red.,
SIDOROVA, V.I., red.izd-va; GRIGORCHUK, L.A.. takhn.red.
[Stages of the development of Tertiary flora and vegetation
in the U.S.S.R.] Etapy razvitiia flory i rastitel'nosti v
tratichnom poriode no territorii SSSR. Moskva, Gos.izd-vo
"Vysahaia Bhkolz," 1959. 363 P. (MI11A 13:4)
aloobotaay, Stratig-raphic)

ARISKINA, Pins. Petrovna; BAMOV, V.I., prof., red.; GAYFULLIN, Sh.A.,
red.; SEMENOV, Yu.1'.-,-t&kh-n-.---r-ed.
[Sedges of the Tatar A.S.S.R. (classifioation key)]Osokd Ta-
tarskoi ASSR (opredelitell); posobie d1la studentov universi-
tetov, pedagogicheskikh i sellskokhoziaistvemykh institutov,
uchitelei i kraevedov-liubitelei. Kazan?, Izd-vo Kazanskogo Univ.,
1961. 50 P. WIRA 15.6)
(Tatar A.S.S.R.-Sedges)

BARANOV, V.L$ prof*
New developments in the determination of absol-ute afe
Vest. AN SSSR 31 no.4:119-120 AP 161. '1 iRA 14:4)
(Geological time)
10~ - 4

Cv, V. I
.ccont "ind of upper Oli,-ocmc, fic);-i, 'n
Dokl. .d ~SST! 136 no. 3:678-67~ J:i 1!, :2)
iii,.eni V.I.
Lenina. Prodstav! cno al:1-o c:~ V. . -t
(4,11; ~ t" 11 lc~y 1 -11, - -~

BAPUNOV y V. 1. ; YA'IAYKII;, L. A.
Developuent of flora and v,;,.I~ctition during the Kinell time ill thEl
loj4or Kviia Wdloy. Probl. '?,)t. o:18-1'1~ 162. (MRA 16:5)
(Kwua Valley-Pale-botwtv 1, Stratigraphic)

BARANOV, V.I.
Studies -m linleofloristics and mi.cropnylcgeny at the N-1partment of
Plant Cla~qsificatdon of the Kazan State University. B.,~t,-zbur. 49
no.10A1524-1527 0 164. (MMH~ :L8,,I)
1. Kazanskiy gosudarstvennyy universitet imeni V,:.Ul'.v&ncva-Ttlnina,

1. -T

S/216/62/000/006/002,/002
Aoo4/'Ai27
AUTHORS: Gazenko, O.G., Limanskiy, Yu.P., Razumeyev, A.N., Izosimov, G.V.,
Darariov, V.I., Chicl-a(in, V.A., Gaydamakin, N.A.
TITIX: Method of registering the action potentials of neurons of vestibular
nuclei upon adequate stimulation of vestibular receptors In the cat
PMIODICAL: Akademiya nauk QSSSR. Izvestiya. Seriya biologicheskaya, no. 6,
1962, 925 - 928
TEX'T: The studies carried out were aimed at registering the action poten-
tials of individual neurons of vestibular nuclei, particularly of the Deuters nu-
cleus, during a motionless position of the animal and the reaction of these neu-
rons on a stimulation of the vestibular apparatlis during a vertical passive dis-
placement of the animal. The tests were conducted on 17 cats on which action po-
tentials of more than 500 neurons in the area of-vestibular nuclei were regis-
tered. The authors describe the test conditions and the special test stand on
which the animls were placed. The data obtained are being analyzed at present.
Of the action potentials of 500 neurons registered, 6 gr,ups of nerve cells were
Card 1/2

Method of registering the action potent-1als of .... A004/A 127
separated, which were grouped according to the following symptoms: 1) Increase
in the background rhythm in stimulating the receptors - 439 cells; 2) slowing
down of the background rhythm - 20; 3) increase in the background rhythm when
moving the platform downwards - 14; 14) increase in the background rhythm when
moving the platform upwards - 7; 5) neurons detecting the restoration of the
background rhythm after motion sickness - 70; 6) neurons not detecting the re-
storation of the background rhythm in the period after motion sickness - 397.
51 neurons did not show any response to the stimulation of receptors. There are
2 figures.
Card 2/2

ACCESSION NR: AT4o42653 S/OOOO/63/OO0/OO0/O056/OO6O
AUTHOR: Baranov, V. I.; Gyurdzhinn, A. A.; Lomova, M. A.; Radkevich, L. A.;
Tutochkina, L. T.; Fedorova, T. A.; Furayeva, L. P.; Khn*chev, S. S.; Artemlyeva,
N. S.
TITLE: The effect of gravit.-f on the development of organisms
SOURCE: Konferentsiya po aviat6ionnoy i kosmicheskoy meditsine, 1963.
Aviatsionnaya i kosmicheskaya meditsina (Aviation and space medicine); materialy*
konferentsii. MoGcow, 19063, 56-60
TOPIC TAGS: gravity, centrifuge, organism development, physiological function,
rat, chronic centrifugation, blood compouition, urine composition, Coriolis
acceleration
ABSTRACT: In this investigation, &-iranov and his co-workers designed a centrifuge
for small animals with an arm radiun of 135 cm which could be regulated to produce
artificial gravitational fields of from 4 to 5 g. The centrifuge was arranged
in such a way that the arms and cages at the end of the arms would simultaneously
rotate around their axes producing Coriolis accelerations. A single control panel
Card 113

ACCESSION NR: AT4042653
regulated the photography and illumination of cage interiors, automatic feeding
of the animals, and the revolving rate of the centrifuge. It was possible to
record five separate physiological functions from some specially prepared animals.
Experiments were conducted on white rats, commencing on the first day after birth
and continuing for 25 days. Litters consisting of 200 animals were divided into
experimental and control groups. All animals were born at approximately the
same time. Experimental animals were subjected to accelerations ranging from 1.5
to 3 g for periods of from it to 6 hours, 6 days per week. The weighing of all
animals took place every three days as did biochemical assays of the blood and
urine, tests of vestibular activity, and the determination of the time of sexual
maturity in female animals. At the termination of the experiment, a comparative
test of the response of both experimental and control animals to brief accelora-
tions of 5, 10 and 20 g was conducted. After 20--25 days, the body weight of
chronically centrifuged animals was 60--801% that of the controls. The composi-
tion of erjLhrocytes (89.6%), leukocyten (93.16), and hemoglobin (99.1%) in the
blood of experimental animals with respect to control animala reflected a
slii:-htly anemic condition. 'Uhile blood albumin in experimental animals was some-
'i.hCAL lower than in the controls, serum mucoid composition was higher, indicating
a ciiant-,c u" dycLrophic character. Urine nasaya of experimental animals showed
that Lkte av,-Ia uf Dicho-pooitive i;ubatance (48%), nitro,.-vil (6;1~0' creatino (31%),
I
card 215