SCIENTIFIC ABSTRACT BEZRUKOV, G.N. - BEZRUKOV, V.I.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000205210013-7
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 8, 2000
• Sequence Number: 13
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

BF-7RUKOV, G.N.
Basic characteristics cyf the distribuUon of
talcite deposits
in the Mlass talobearing region. Zakonom, razm.
polezn,
iskop. 6.,,568--585 '62, (MIRA 16-~6)
Institiat geologii rudnykh rjestorothdaniy
petrografii,
iunemlogli i geokhimii Ali SSSR,
(Miass region-Ta1c)

BMUKOV-1- G.S.
loather and footwear Industries during the sixth
five-year plan.
Log.prom. 16 no.5:1-5 NY 156. (MLEA 9 -. 8)
1. Zaaestitell Kluletra logkoy pronyahlonnosti S M .
(Shoa industry) (Leather industry)

BEZRUKOV, Grigoriy Somenovich; LYUBICH, Kikhqil
Galileyevich; VARSHAVSKATA.
. - - ~- ~ ~- ~ -'rgd'o ;~ VAMM, M. T. , tekhn. red.
(Now developments in the technolo&y of molding footwear
uppers]
Novoe v takhnologii fotmovaniia varkha obuvi. Moskva,
Gos.nauchno-
tekhn.izd-vo lit-ry po legkoi promyshl., 1958. 150 P.
(MIRA 12-10)
(Shoo manufacture)

BEZRUKOV, G.S.
Clothing industrv in Moscow Province after the
reorganization of
management. Shvein. prom. no.2:18-19 Mr-Ap '59.
(MIRA 12:6)
l.Nachallnik Upravlanira shveynoy promyahlennosti
Mosobliepolkoma.
(Moscow Province--Clothing industry-Management)

S ____ ~ so Moskva)
Clothing factories of Moscow Provinces in the first
year of the
seven-year plan. Shysin.prom. no-4:8-11 Ji-Ag 160.
(MIRA 14:3)
(Moscow Provinoe-Zlothing industry)

RMUKOV9 G.S. (Moskva)
Double level conveyer with vertical encloaure.
Shvein.prom. no./+:25-27
JI-Ag 160. (MU 14:3)
(Clothing industry-Equipment and supplies)

8/121/63/000/001/004/014
A004/A126
AUTHORS:. Baranov, V.N., Zakharov, Yu.Ye., Molseyev, V.Ye.,
Bezrukov, I.M.
TITLE: Chip-breaking In turning ductile metals
PERIODICALt Stanki 'I inistrusienti no. 1, 19630 14 1.6
TEM. Scientific. workers of the MVTU. im. Baiman have carried
out investl-
gations under production conditions to study the efficiency of
various methods
of chip-breaking.and of removing-ohips 'from the cutting zone
in turning highly
ductile meta2s. These tests proved the possibility. of
obtaining a reliable
breaking of chips over a wide range of cutting conditions, the
required finish
of the machined surface and an appropriate tool life by using
the hydraulic
Br-2 (VO-2) vibrating saddle. Moreover, the tests showed.that
vibrating sad-
dles with electromagnetic and eleotrodynamio valve driven are
suited bent for
operation in a frequency range of 25 -, loo cps, while .3rBC -1
(BGVS-1) vibrat-
ing saddles whose control valvesare driven by an electric motor
are most expe-
diently used in a,lower frequency range of 0.5 - 25 -cps. The
authors present a
detailed. description of the. design.featurea, tedhilological.
parameters and opera-
Card 1/2

S/121/63/000/,DOI/004/014
Chip-~-breaking in turning.duatile metals AOD4/A126
tional behavior of vibrating saddles, taking Into accc~znt
different turning con-
ditions. The operational tests with vib 'rating saddles provVd
that the reduction
In power required for cutting is,fully compensated by.the
power required by the
hydraulic system. The use.of low-frequency vibrating saddles
in turning highly
ductile metals ensures a reliable 'breaking of cl-Lips,. it
aurfttoe -finish of'at -lewt
class 6, an Ine'rease.in tool life by a factor of 1-5-ano,a
reduction in cutting
power of up to 65%, while the..vibrations have no negative
effect on the lathe..
There are 4 figureq and I table.-,
qaFd 2/2

ZOLOTAVIN., V.L.; BUKRE-YEEV, Yu.F.; TOLSTOV,
L.K.;-,H.FIZRUKGV, I.Ya.
Photometric determination of soditm in pure vanadium
pentoxide.
Zhur. prIkI. "ktr. 2 no.5t461-462 My 165. (MIRA 18:7)

ZOLOTAVIN, V.L.; BEZRUKOV, I. Ya.; SANNIKOVp Yu. I.
State of hexavalent uranium and pentavalent vanadium in
water-
ammonia solutions. Zhur.neorg. khim. 6 no.3-.581-586 Mr
161.
(MIRA 24:3)
1. Urallskiy politekhnicheakiy institut imeni S. M. Kirova.
. TUra3Tbw compounds)
(Vanadbm compounds)

SANNIKOV, Yu.I.; WLOTAVIN, V.L.;-BEZRUKOV, I.Ya. -
Hydrolysis of pentavalent vanadium compounds.
Zhur.neorg.khim.
8 no.4:923-933 Ap 163. (MIM 16:3)
(Vanadium compounds) (Hydrolysis)

~~7-
USSR/Nuclear Fhysics C-5
Abs Jour Referat Zhur - Fizikay No 5) 19571 11239
Author Bezrukov, L.S., Panov, D.A., Timoshuk, D.V.
Inst Not Given
Title Dependence of the Transverse Cross Section of
the
Reaction L17 (d, p) Li8 on the Deuteron Energy in the
Interval 1.1 -- 4 Mev.
Orig Pub Atom. energiya., 1956, No 4, 149-150
Abstract A measurement was made of the excitation
function of the
reaction M7 (d, p) L18 for 4.o-� 0.05 Mev deuterons
from the 70 cm. cyclotron of the Academy of Sciences,
USSR. The yield of the reaction was determined from
the
(3 activity of the Li8. The multiply-repeating cycle
of
measurements consisted of exposing the target during
one
second, interruption (one second), and counting the
Card 1/2

USSR/Nuclear Physics C-5
Abe Jour Ref Zhur - Fizika, No 5, 1957, 11239
activity of the Li8 for three seconds.
The excitation curve obtained has rAxi at deuteron
energies of 2.0, 2.5 and 3.7 Mev, corresponding to the
levels of the internediate Be9 nucleus with energieg
18.3,
18.7 and 19.6 Mev. Data on the existence of the Be;'
le-
vel with an energy 18-3 Mev coincidg with the results
of
investigations of the M7 (d, n) Be reaction.
(Referat Zhur Fizika, 1955, 24o63)
Card 2/2

THE QM-j�LC_-110N FOR THE RLACTION L11 0,32)
.A.$ A Y*UN('TIO'i*OF0EUTERO-,' i -Y? - -K
R.-E R 1; TSIX RA-NC
1.1-4 UEY L. 5. Bezrukov, D. A: ~Zri
X-R-,n7c- ETiv 4 W9-1011SBC).
Datiturons frorn a ' O-cm cyclomm were uf.~--d to r,*W, y tha
,mactlork The trw.D ~~-actlvv fcor vj~o nuactlt)-,i
1;bowa msonances ai den. orf?n er,-r-le5 of 2.0, 2,5. arJ 3.7
Mov.

BUMMOV, M.N.. insh.
Investigating the wharf wall in the river port at
Gorkiv. Rech.
trausp. 17 no. 7:39-41 Jl 158. (MIRA 11:8)
(Gorkty-Wharves-Testing)

BIZRUKOV, B.; VIKOLAYIV, L.
Overhauling engines. Ayt. transp. 36 no.10:21 0 '58.
kMIRA 13:1)
kMotortrucks--Jngines--Maintenance and repair)

PROSHIN, A.S., inzhener; BZZRUKOV, N.G., lji-~ener.
Increasing the load lifting capacity of gentry
cranes. Elek.sta.
28 no.8:59-60 Ag '57. (MIRA 10*10)
(Cranes, derricks, etc.)

"The effect of various factors on the
follJctLlar content
Kazakh fine-wooled sheep." Min Higher
Education USSR.
imeni S. M. Kirov. Alma-Ata, 1956.
(DISSERTATION For
Candidate in BIOLOCUCAL SCIENCE)
Kr,izhnaya letopis,
No 31, 51- 3 10c w

I(e) VA)
15A~00 )
USSR/Human and Animal Physiology - Reproduction. R-9
Abs Jour Referat Zhur - Biol., No 16, 1957) 71051 D-
Author Besrukov, N.I.
Inst I
Title The Influence of Different Factors on the
Follicle
Maturation and Fertility of Kazakh Fine Wooled Sheep
Orig Pub Avtoref. diss. kand. biol. a. Kazakhsk.
Alma-Ata, 1956
Abstract No abstract.
Card 1/1 - 6o -

BRURUKOV, Nikolay Vasillyevich; MUTSU, P.V., red.;
GL-B..&SIPOVA,
- I : wabidwaim
(Analysis of the economic operations of building
organizations]
Analis khozisistvennoi doiatellnosti stroitellnoi
organizatsii.
Koskva. Gosplanisdat, 1959. 155 P. (KIRA 13:1)
kGonstruction industry)

BEZRUKOV, O.F.; NERONOV, Yu.I.
Pulse generator for spin echo observation. Prib. i
tekh. eksp.
8 no.3tlOO-103 My--Te 163. (K[RA 16:9)
1. Leningradskiy gosudarstvemtyy universitet.
(Oscillators, Electric)

TEFIMOV, A.S., lcand.med.muk; BEZRITKOV O-V-. ordinator;
FIRUS, L.Ye., ordluator;
p --- F
YIWIMOVA, Te.l. (Krasnoyarok7-
Condition of the higher nervouB activity in endemic goiter.
Probl.endok. i P~orm- 5 no.3:43-50 Ny-Je '59. (14M& 12:9)
1. Iz kafedry Krasnoyarokogo maditainskogo instituta (zav.
-
prof.A.T.Fahonik).
(GOIM, physiol.
0ndemic, higher nerv. activity (-Rua))
(CENTRAL NERVOUS SYSTEM, phyniol.
higher nerv. activity in endemic goiter (Rus))

L 10100;;.,63 Wr ( 1 B DS - -A F FfD
ACCESSION NR: AP3002729 3/0120,/63/000/003/0100/0103
AUMOR: Bezrukov, 0. F.; Neronov, Yu. 1.
TITLE: Pulse generator for observation of spin echo
SOLMCE: Pribory i tekhniks -eksperimenta, no, 3, 1963, 100-103
TOPIC TAGS; spin-echo observations, pulse generator., rectangular
pulse
combinations, relaxation time
ABSTWACT: The pulse generator generates five different rectangular
pulse
sequences corresponding to five basic methods of observation of
spin echo. The
generator provides output pulses with an amplitude up to 40 v.,
rise and decay
times of approximately 0.1 microsec.. and smoothly variable pulse
duration of
2-200 ndcrosec. Relaxation time can be varied within 0.03 and 15
sec. Selection
of a desired pulse combination is accomplished by means of a
five-position
function switch. The following p-alse combinations can be obtained
from. the
generator: 1) sequence of two pulses of 90 end 180 derees, 2) two
90-degree
pulses, 3) tbree pulses of 180, 90, and 180 degrees, 4 a pulse
sequence where
the first pulse is 90 degrees and the other two are 180-degree
pulses, and 5) t.11z
90-degree pulses. 1~y varyim the parameters of',the circuit the
genpr~ator could7c.
Cord
---------- ......... --- ......

BEZRUKOV, O.F.; WKS, M.F.; NERONOV, YU.1.
Proton relaxation in solutions of ternary butyl
alcohol - water.
Ukr- fiz. zhur. 9 n0.-4:457-458 Ap 164. (MIRA 17:8)
1. Leningradakiy gosudarstvennyy universitet,

SAPOZENIKOV, Dzitriy Gavrilovich; TTSZTX'IN&,
HkRM ATZW-qAMROVNA;
BEZHMV P.A. otv.red.; BIMTAKOVA, Te.T.,
red.izd-va;
VOIKOVA, V.V., takhn.red.
[Recent sediments of lake Issyk-Rull and its
bays] Sovromennye
o9adki ozera Impyk-Rull i ego salivoy. Moskva,
Izd-vo Akad.
nauk SSSR. 1960. 159 p . (Akademiia nauk SSSR.
Institut
geologii rudzWkh mostorosbdenil, petrografii,
mineralogii i
gookhimii. Trudy. U0.36).
(lawyk-gull, lAke-Sedinente(Geology))

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I-IN 11tv ILI-it 1" Ilk- mi valw1v 1,A OwIlik all 'v
~J.q The
lit.41.114-K% Aild IN
r

li.1 .. 11 1 Ili 11 11V It .1. tllll All, 1- All 1"14 1 Wki SO
1, .1111
air of gl'Af 1,1111h fit,- thl.nit, luk".
a lit lite
ix-m-nisse .4 A1.4t. still Irvik,

W~Il it., 1--f. 1 A I..!, I
At-' C111tj .111,
,%i4lvs, Nikin-faltvwAlIv the given lbaulkilv~
are Chatacirl -

., 1 f;7*-*. "_ I
1.1
y4d III, On ps_lh~ .4 4"ll'us"AhIr clyNt. and MIAMI
;

IIIA IIV 111111,J1 glaV 11111 X IAV A1111y'll tiNit It
...
imt4l, .4 ihr 04,Aostr Itimp idAphimri. cryt. ilia.,Ixor

it attj
j.-j1.jj Amami* ht,jraf#~, Thr ird

U U &V .0 is tw 0 At I' is
lit 5 jj a 3 1 IF
is A, Is

0 904 01110 0 9 0 0 0 0 41111 0 0 0 0 0 0

00
to
00
00
"I", ,1,y 'Vic, ""'t M., m.."it.
dilpilitits In the taststs pan of the Turpi depromm"
Ald. No, 151,
J 42tof FuSit,li. Vg 4,1 IiKtO,. Nuttivt tout twit wr drilmn %
""Vexpl,vt if tit tit,- Ioa~t-l thr A%lut-Tasly-Tufgal River,
all"I At%Al%k f4vtot, %ttualril in flit- area of a VAwt dr
ple""I 811tithmg in a ttUtht-tti ditwitithn. T1w g"4.
tructurr of th'. q1tit,"It. flit- rsktbkw*,d
mirfjkv ttx-k% A flit, I twitwi%ull %law tit dw
figlualk"l, It'"Iff atihill flit, 1.1.1 .4 Vniwv
klftmtp l:1 *tOlOll'it t6yk AtUl CLOY uhalr,~
lifillir tilt' CAtlitilitit,1441% tk-Ixbmt% wr jutamir %italm
:;'x.InA1t1L`,A41ltA lid%% t-WhAing 101~ it[ lVAtJ%i1V-, OhbVh
mmily fiitm ladhititt, flit I'mital I'dulaWk lmrkft 1.~
U
thr zwk 1yjw with a tallut th'ittit-1 twim-ilitic 1dructutc.
Stvctal utk1w.. pailing iniow cakh othut, cast fir lim-
1109111shi'll. lilt, 10-t %uhll
twuvilr% til fitw pw4mv Milli I I t 111, -0.
Nwirs us flit, Vall1tv full V I~
Villujim-I m4t.-tsal ",Ijmtjlm~ VtlV 111414. li-ml, d.
IftKiti. (if 414-11% 1~.Iill,b 14'.." istr it" I,---
picnily --- A -heit, %mcwtv lif tiakattir mt fitsittl
I &IN.it, I [it- chwl I'llt'l-irnt if fill, mr, I, AIA 01
ine,tent in thr ccAloidal ftstin and ItAtilt, a- thr tf%..l
p6bmw 1,'Vtiw Oxick.im. pfv.~lit its thr liatil -4 lint. 'mc
wid henwitc 411(l TiO, 1, in Or I"ITIS tit lllt~h. ~ IN .
I- fire"Pit'llt All A MCCII. Mlltltl%t~ 11-JAII. q AN A
C4144dAl t'll"tt 1NWt11kJ- %fill flit 44V Nlikt%V 'nAIVW% 41111
ii-ttvaph, air rl..-ra S4%tl,` It'GIVUCc~. Milk-
dlelldilbl" Of tht IOUIL111411`111 PR" Of 1111141 MOKOW bman
A. K. ftchmiw. 11'sj 4. . lifItIff Fligh'It. tilt U tit
Itrormt, mitirialitigle gnu[ chcul COMI"T 4 9-1 %ASWIV
.4 haumic. "i Ill., ji-Ijim - J.-A 11W .-I,kf flick-
f1*111,119 cill-l~ "I Itic ttltl%nl~ dIV Alli-111-0c , A10 f. -
m410411,01 and hytifuttyllotc A)AVIllt)
Kyliwm "it Al sulfstrit (altunir ault ,I hi-lt;
mallet Im4ttortitont. -
Th~
IM Tit Ii FrTIw Miilrs mc 1-111 it, I b,
larpmf laut,itc driftwit% arc foutlit m div I INt kivtf hamn
30 40 km Ittutt fix- Tulm Cttv, I-ifiv is 4-tent-.
ChAt. Mane
0
0
00
of
00
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00
00
00

0900600000000000000069 ass a 000006000
I loss 7111 9 10"ull-millmlylstpallanisis At D lies J9 m it v
13 to is a v is A, a V Q a a 're
-2-11 Ill a I I m -0M tz L A A k A 7 s a -L- L-,~u
-00
the ArtistakimAn bedded phosphorites of the western
blopoulthe Urole. 11. 1 l1r,111hov 410 1 NI
I .I*%. NJ. /RIF lr,vllirl A 'N -N N ~
No. 142. K2411011 linxll-hl(Ml"~. I'llo-ph4tv 1- 4
00 c YbIs in emnlin. ftfun 15 to 31,~~ IY I& *A% 1114111& 11,
so :4aves tht-w were altmVide lim"tan, tm,l- c,mas. -00
mit of file dri-lits t,
0 1"(),. owing to the dri tIr
0 J. S. 1-11~
06
90
00
66
09 a
00
Oe
00
00

j

:
A16.1LA
EAVALLURWAL LITERAIL411 CLASIMPICATIC).

It

I#icg,) .10
owl as(

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:
a 0 0 vg

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IF
qqA[A,, ". A, I ~ h. I 1 -9 A - A - 1. -m- vi;LA I I -AA a Q up
III A.0 IND (1101pt
00 PROCIIIII ..* PROVIIII41 INDI.
go
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KIA-b I IL I A t 0 . a -A-j-
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GimilitJ11171-no'll. Ctinvahl.
96 c 1 1. K.""kv, .1 Chem. Ind
1, S. S. R., is N., ji,:1
.11 116A Kalsk.111, id. -41-1. If %1. 1.
:40
00
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A I a. I L A 84TALLUOSICAL LIT911ATI.Ot C ASWICATON 9.1
L
111,01A.. --- - -1- - ~ -, - -- -.- --:,- _= -
1o-
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as
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MIALL~AL LrMAIWA CLAOWKA"10 9 moo
- -- - ---- -~ 1 10*
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r
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4;
t, lid] More

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'
.

too

It -D

00

of

*4
Colowd Smumpkim, of, .too. 11. L. Belt-

_00

00 It

Comilpt. rowd. S. 24, 282-4
fukov.
-
w
t
h
l
f

1.0*

V
e
u
t
tlff;jV)jjn Englilb).-latrow nielalodmPhims o

pakozoic phumpbaie
beds in con-I ith Cawonialk

00
Illauite. obwaved at "A-Tau, So,
K"Alibstall. Ird to a

00
r!
Oulwe study of the j*tnoulenon, invul%ing it dq-tadt-d pol.

.

ing condilkins anti of the tneta-

"
lemetip'lon of the U

-00
00
tes into Allatitr btils. There
moildhidan w tits
-r
Ei

moo
so 3
tbal theintal "101
v,
l
due reasual to
d

ammipamied by an admixt. of volatile cou'Putwilts cante

00
it
intrusion. The metaillorphian tnvulves coin-
hy
:i

90

c ruction of the phosphorite crystals. The P.O.
d
e
WRIC
d i
3

0

ll
70 An
thcapatite ~,Vvr AnlUUU1J 1021.
"t"Itrat of
xwd
AAl
$w
2
i

:

zoo
00
-
rtrums,
rc
p

i.oe

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'1369

foe

001

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age

1
id
LITC TWE CL.Suo Two

00

I'll I Oft,

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T Aft I

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it t I

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:

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o

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so-'

G-Itskal lar"Opdo" of Atdnd&n phosphocites in

m"Um d""
of Ural atio"ULAS. 1'. 1., nctruli",r.

*02

JRJJ. FfrjdiW$
11110(t0fidlilkid0f TV. S. S. It.)

1.0

140. 16-24; Kkitm.
Riffral. Zkssr- MD. NO. 1.
ifi
Ai
7
h
i
A

24r.--T
Att-
e strat
rl
tt
37
ed upper
C. A. 33,
Age phospborites forin a stratigraphiattly comm. horizon,

IlIm"horitrs are %itusted insinly in thc outcrup~ of the

0

rtvf limeptours. Pho6phate-bessing fortnalions arc al-

00.

Isslung the UmAka river. Thopiw-

ago
viod

vfalirk~ pho,pholitrs

hised linleton". The phenphorit, t,pjcw$l1 ch,111,

Soo

matior
drptKitss formed in the shallow (but far t"novvd
i
l
(
O
i
f
h
i
1

40
90 .3

t~
mtlrotl
mut t
w
le U
1wilm o
e Shure) toile,
"g (o t
x

nd benthic (anna and to the ptclency of Ityritc. it. t-oo,jtj
-

09"

*I
VVX that the phiMphol'it" Were 10"110 With 'Ail iuMl1fiC1VHC%'

ZOO

Sol

of 0, whk-h tuakes tiscut 4fullar w the U-Ity Mountain
-
t O
l
~

itiou
w
ii
%tvt
hollphuritm Adc-wdptkmollithok4it
P

Artinskian format4mb their stratigruphy and a inicto-
;i
i
Ch

em.
ven.
%.tWkvl d"-ription
plimphorittt ate g

analymm of 3 t)Vcs of phoitphorite, and 5
invotuplete analy-

es of daknuitized fiturmone, tinterbeddell
with ph,^-

phstr,,) are given. W. R. Ifetin

a S A - S L A

41TALLOCKAL LITIOATURI CLASSOICAY100

.
-_

Iwo

--

smiciij .11 ONT aft

fib U 1, to Ll;;

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;

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.
I
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4
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r Ga It I I_u 1
I W, I M, P.PC av

Call,. 'It I I- III t I"

depolaitat in the
phcamphaI-b,,ri,,g

00
At"'t

H. J0, -1:11 Ill"I Ill fill.

00
dljk-ll~ at K41a.-I*"j,
11111t. c%I'j' all ,,I, ..-I ...

'Aln,f) III ph"qI1141".

dvjxa~its. formed by file %jolop.1g, all tile t,fgigctIfItI%
Illat_

Cut%. with %ett watrar twin& th- wmm III dor

'd flat.
III,, _'Imv If Ow I..
66 8::

v,fiv, %alh Itwx I:I:Is'
"

:fit
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A S as . S L AITALLU*GKAL LITIESOLOOR
CLASSWK&T'0

1

It 0"
t

oil all a"(

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3--,-.1r
q I i
1
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0 0 0 0 0 0
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:.

MIN W, U-1

Dr.
Dilss, "r a-~ "L
TUn 47.
SO:

P. L.
USSR/Goophysice - Sons 11 Jul 53
"New Data on the Geological Structure of.Far
Eastern
Seas,"'P. L. Bezrykov and G. B. Udintsev, Inst of
Oceanology, Acad Sci USSR
DAN SSSR, Vol 91, No 2, PP 359-362
State that new data obtained from investigation
con-
ducted by the Inst of Oceanology in the far eastern
seas permits one to look deeper into the history of
their development and gives interesting material
for
studying the formation of island are groups in the
Pacific Ocean. Presented by Aced D. S. Belyankin
11 May 53-
276T57

V110itorn Aeposits of the Xurile-Kamebatkit trenth. r7r._'
Sezxulcov.
7r=M(M5).-Amoufz the s~atlms of the 66ttorn drpmits-
are the river; that are nutnemuq in KQn,vitatlut and less
so in the Kuriles. The tertigerlous matcAd delivered by
the rivers is mostly insol, Another sourm are the products
r,,' volcanle eruptionis that are mvept into the ocean
follow-
Ing theabra5ion of theconit by the%va"s.
%m weeds Varrinii6tz and Forris) which have inorg. matter
attached to their holdfaas arid are cartird far Into the
sea by
currents are another contributing factor. The most irri-
t source are the volentioes, both surface and sub-.
ng e- 0a ids.
i~66dl' tho5colj1palla~idtfi- Alentianis '
Tuxaaz~liei, solfatarals, and )lot springs, are probably
re
r1ponsible for the presence of Si(~, nod Organi5ms
!that Artilize the mint~al% present in the occan for AtIct
structum Diso colluibute to tht formation, of c1cpaillo.
',Tmp. and chem. conditionq prevent the txcumulation of
~CRCO, but favor the formati,)a of diatom.R. The types of
deposits present at the bottom can be roughly classific-d
as:
,(It gravel, (") sand, plain or confg. small anits. of Fe,
Q10,
at SiOi, (3) shellfish remaini, (4) silts, (5) mud. Gravel
In, the Kuriler consis-ti In the main of aridc3:trs,,
hasalts,
'PMbyritel, dacites, and various tuligenic stra;a, much
less
frequently of granitt-3. granodiorites, and atgi)itev. The
,c*mpn. of gr&Tel in I,:) nichatka Is in ore varied.
Alongwith
tifusive and pyroclastic format;uns intrusive and metamc)T
phcalr shales are found also. A thararteristk feature is
the presemce of many lime-absculaing organistas- hydro
coraIlines, bal id Mat, and crinoidq. Tire smids
am 2,
in t1m, K.U. consist 7-u-ta6mlastq. atigite, bvtrersthene,
it? 301no Oaces of pitmice~ n~rai
~netite, titaniurn*~ziztrnaite,
and other rate minerals. The MO~ is verv, iron
V20. 0107o. Shrli5sh use found in thc !ita zurrl around
the Wzaid Khartimkotan (Pirclr. 47in-:4y'.
- ZZ,
balanidiandgasttoilOds). Tile client. cwnjn:t.,)(
thealel~T'itrs
\-ariei with their distance front tite surface, front
io.s~ to
'6.421,,; SiO.. 4.07 to 2X),1% Fe, amj O~i7 to
Clicin. examn. of the cl.,ty deln,S; Yldded thc foliowing,
data dcl)cndin.- on their disUnce ir~':t' ~Uhe surface-
3.26% SiO, 4.F~3.5213% re, and I.W-0.0% Mo. Fe and
hfn make file depo4its rLp;wt,-.r dark bo,,-.r,. illicl
\-.c, .!"d
Pale brown when dry. Ostrournov (C.A. 47, IQ-)k) ?*-,.
COVezed the presencc of llydrottoilite az!d Ills, the
L-ate.,
at the very bottom of t1le trenel!. The prescnee of H-.5 is
probably due to mduction of sulfate; r., , r,sLot oi mlcrr-
~!Ploi;ic pmcrrj~cs taking place a t~e boltora, A, 9. N-

USSR/ Geoltsy
Card IP Pub. 22 - 32/45
Authors I Bezrukovt P. L.
Title i Distribution of organic substances in Okbotak 6ea
sedimentatione
hriDdicAl I Dck. AN SSSR 103/2j, 287-29D..,Jul ll.. 1955
Abstract I Geological data are presented on the origin and
distribution of organic
substances in the xedimentatione of the Okhotsk Sea. Twelve
roferences:
10 USSR; I USA and 1 Germ. (1934-1955). Table; diagram.
Institution : Acad. of So., USSR, Tnet.,of Oceanology
Presented by: Academician S. 1. Mironovo April 3-1, 1955

D "rbu"03 d rixte Of se'dIrtientlitlan at
silica silts Ln the
is an -ov.
of Mhiltsli 1). L Beiruk PokVjV., M- Nduk
S'S'S'R. 103, 4~3449WVF--~Tnlcroils "'ilts Are
I% file-
spread avet tile bottom of tile Ilt-rhig Fra.
aild tile Sta of
OkliMA-; of the 1--ittknow "V1.;fc tntv'h lowt,
In
Ali thigen ic
~byleac7bingtvitbab%~%'nICO,soin.
Withividevari.itionOn
the single samples, the av. content in
amthionic SiO. %vas
1).r)", ill e4t ds 4.11- Cl-lyry ~iilv~ illay
in coarrs. alruritei I "' I ,
contain upto4!V-- anu
of the dcCp-Sk'a sediments in 'he western parts
of the 17;e_~ of
olihot~k Ure )v wer In SiOt 05-22%). 'Tile IP'W
C~Ment in
soi, SiOl ob,,ttvrd in sands is cmiktil by
nrcc.~-,jry ~picvfat
of spongr-i, Authigmic SiO. Is typical of the
pelific-cul-
loi&lfr-,Lctiottsaftlit!smmlitnetit!i.
gregates In the silis,tre highly porous (vol.
weight in tile dry'
state below 1.0'. cvcn down to 0.4), their
outside is colored
deep brown by Ma% hydtates (cf. A. 11. Zhuze,
Dok!ady
Akad, Ncuk 8,S.51R. 93. 127-30(1954)). A map
gives dict
regional d1litribution of the Si0j sedinicuts,
sho-'ting them
particularly enriched in the central parts
(deep-sea waters)
of the StA of Okhotsk. Tile hisliest production
of phyto-
plankton with Diatoninceae. however, 1i
obsen-ed lit the
litoral rr
I
gicim. The diakoinatwus silt5 form only the
upper
laytrs oft fit sea-bottom sediments; the
content ofauthigettic'
liatts thtv hnvt a thickiii-i (if tit., in the.
t.*ntral reglorl~
only of 20 cin- to I III, The ra'dilorlitti of
lilt 111111i (Irl'trg-
slon (ca,-t of Knnirbatkn), however, i;how much
highet
cumulations of 6i0- s-dim~nts, nd hichu
conciis. fit A0.
SlOg. thati lit the northern parts of the West
Pacific fx-,aa.
The rate qf sc(linivitillon of the atiffilgenle
SVI- ii Calcil. it.
tilt! order of magnitude of 10 to 25and I tc,
;!."' -!I. I)rr INA) 901
Yeats, Its tile 1(;Wer And upper limits,
evi,icutlY, "olcallic-
facies tend,.q to increase the rates. W. 1" -te

BEZRURM, P.L.; UDINTSW. G.B.
...
The northern end of the Hawaiian submarine ridge.
Dokl.AN SSSR
103 no,6:1077-1080 Ag 155. (MW 9-1)
1. Institut okesnologil Akadeeli nauk SSSR.
Predstavleno akademi-
kom D.I.Shcherbakorym.
(Havallan Islands --Geology)

DOLGOPOLOV, N.N. , redaktor; BUSHINSKIT, G.I.,
redaktor;
GIMMILlnROB, BWeK..,Nr6ftdZor; IVANCY, A.A., radaktor;
STRAKSDV, N.K..
akademik, otyetatyannyy redektor; FISENKO, I.A.,
redaktor; ASTROV,
A.V., redaktor lzdatellstva; AUZAN, N.P.,
takhnirheskiy redaktor
[Problems in the geology of agronomic minerals]
Voprosy geologii
agranoutchaskikh rule Moskva, 1956. 239 P- (MLRA 9:11)
1. *4mdemiya nauk SSSR.Otdolentys
goologo-geografichaskikh nauk
(Geology, Scohomic) (fertilizers and manures)

BE L
i1j"J40111 BtZRUKOV p,L... QSTROUKHOV, B.A., PA - 2922
.11,TU On Phosphorus Distribution in the sediments of the
Okhotsk Sea.
(0 raBpredelenii fosfora v osadkakh Okhotskogo moraya -Russian)
Y&RIODICAL Doklidy Akademli-Nauk ziba, 1957, Vol 113, Nr 1, pp
142-145, (U.8.0.R.)
Received 6/1957 Reviewed 7/1951
ABSTRACT Inorder ~o explain some qu"tions concerning the origin
of phosphorites
it is necessary "' know ~the rules governing phosphorus
distribution in'
the sediments of recent se". In contrast to other seas
the,Pacific has
scarcely been ifivestiggt!dIn this respect,
Conside.rablwquantities of
material of soil sedimeats was investigated which had been
collected by
the ship "Vityazll-in the North Western Pacific"s The close
connection of
the Okhot4sk Sea*with the Pacific', the perietration of
phosphorus -rich
abyasal-waters from this ocean, the high productivity of its
plankton,
the variety.of geblogical struct~ure and of the petrogra~hic
composition
of the surrounding continent, a*ell~as the existence of
upper-teriary
phosphorites on Sakhalin render this investigation important.
15o sta-
tionson theground were investigated with respect to
surface-samples,
(2-5 cm) and a chart (illustration 1) was made. This chart
shows that
there are two teritories with a relatively high
phosphorus-content.
1) A continental shoal in the nothern part of the sea and 2)
the Kam-
chatka- and Kuril Isles shoal. In the former region the coastal
zone
has less phosphorus(0,07-0,40/0) than the middle parts of the
shoal
Card 1/2 (opl2-o,150/o)- In the latter region the highest
phosphorus-content is

FA - 2922
On Phosphous Distribution in iho Uediments of the Okhotsk Sea.
found in the sand of the shore (o,O-o.~350/o) and it becomes
less
nearer the sea. In East of Sakhalin the phosphorus-content
increases
again, not on the shore itself,(0,02-6,040/o) but somewhat
moreto the
East in the Der7ugin depression (o,o6-o,o7O/o). Summary.
Phosphorus-
distribution in the sediments of the Okhotska Sea is on
thewhole
governed by the same rules that Strakhovp N.M.,found to exist
for,a
number of other watersi The phosphorus-compounds come into the
Okhotsk
sea as solid phase with,denudition- and abrasion products of
the continent
and partljr perhaps with products of volcanic activity.
(1 ill.,13 citations from published works).
A.IsSOCIATION OceanogrAphical Institute of the Academy of
Science of the U.S.S.R.
(Institut oksamlogil Akadsai Nauk SW
YRRMITED BY bTRAKHOV& WoMe, Member of the Academy.
bUBLITTM 12.11.19$6.
AVAILABLE Library 6f Congress.
Card 2/2

20-2-42/60
-AUTHOR: ko v, P. L.
TITLEt On Dee;nmter Deposits of the Idzu-Bonin, Marianas,
and
Ryukyu Ocean Depressions (0b osadkakh glubokovodnykh okeani-
cheskikh vpadin Idzu-Boninskoy, Tdarianskoy --; Ryukyu)
PERIODICAL- Doklady Akademii Nauk SSSR, 1957, Vol. 114, Nr
2, D.P.387-390
(USSR)
ABSTRAM So far, the deposits of the above oceanic
depressions have
been studbd very little. In connection with the beginning
of the investigations of the oceanic depression in the
Northern Pacific, the necessity was felt to examine also
some depressions in the Northwestern Pacific~ The sharp
oceanic depression East of the island chains of Idzu and
Bonin was now given the name of these islands. This depres-
sion has a meridional couve and its greatest depth is
9764.m. In 1955, its southern part was explored by a team
using the ship "Vit-_vaz". The 'Ldzu-Bonin depression ends
at
the latitude of the satbernmost Bonin island. Further south,
Card 1/5 opposite of the Volcano Islands, af ter a f oro of
a depth of

20-2-42160
On Deepwater Deposits of the Idzu-Bonin, Marianas,and
Ryukyu Ocean De-
pressions
only 100 m, this depression is continued by another, which
in its northern part may be called the Mariana depression.
Its almost flat bottom reaches a depth of 7800 m, and it
has steep slopes. The Ryukyu depression runs east of the
Ryukyu Islands. Its greatest depths: 7300 - 7500 m, south
of the Okinawa Islands. In the distribution of the sediments
of all three depressions, some characteristic features were
discerned: In the upper part of their slopes, different car-
bonate sediments are deposited. Below 4500 - 5000 m there is
virtually no carbonate in the sediments. In the lower parts
of the slopes and at the bottom brown (oxidized) clayey
clays
of the type of the "red clay" are deposited. Among them,
also grey clays of the reducing zone are found on the Idzu-
-Bonin and of the Ryukyu depressions. Everywhere on the bot,
tom of the depressions there can be found scattered lumps
of an older clay which have probably come here as result
of' landslides. The formation by landslides, probably accom-
panied by turbidity currents, as also confirmed by the
distri-
bution of water turbidity. For their examim tion, a new
method was devised at the "Vit-yaz" and used. In the upper
Card 2/5 water layers, the turbidity everywhere had a
pale-brovni

20-2-42/60
bn- -Deepwater Deposits of the Idzu-Bonin, Marianas,and
Ryukyu Ocean De-
pressions
color, whereas in the Idzu-Bonin and in the Mariana depres-
sions it was green. (3 samples, depth between 6000 and 7000
M).
The turbidity of the water was strongly increased. As those
layers of thewater which are close to the bottom are rell
aired, it can not be assumed that the change in color is
connected with secondary processes of the oxide compounds of
iron in the sediment material sinking to the bottom. It is
more probable that "green" tubidity is supplied from the
slopes. As result of the above-mentioned processes, further-
more as result of the complicated nature of the structure
of the depressions and of the water dynamicp at steep slopes,
the sedimentation in the deep-water depressions is irreeu-
lar. There exist many places at the bottom of the depressions
where no recent sediments are found. Pyroclastic material is
found here very frequently. Also submarine volcanic activity
was observed. Examination of the material collected made
it possible to distinguish between at least three different
Card 3/5 types of layer structure of bottom sediments:

20-2-42/60
On Deepwater Deposits of the Idzu-Bonin, Idarianas,and
Ryukyu. Ocean De-
pressions
1) Microstructure of layers of the solid clays (lumps at
the bottom of the depressions) up to twenty layers in
1 c in.
2) MacroBtructure of the layers widely obsorved - cauned
by alternation of clayey clays and pyroclastic materialt
aleurites, and less frequently sand and rubble. Sometimes
the thickness of the layers is rhythmical, and it
fluctuates between several millimeters and several centime-
ters. It is possibly caused by the periodicity of submarine
quakes and of eruptions.
3) Structure characterized by alternation in vertical di-
rection, sometimes by alternating layers of clays, colored
by ferric and ferrous oxide, and by manganese and man.-anous
oxide. This structure is connected with diagenetic
processes,
and as far as material is concerned it is controlled by
the tempi of sedimentation as well as by the supply of
organic material. There are 12 references, 7 of whidi are
Slavic.
Card 4/5

20-2-42/60
.Oh 'Deepwater Deposits of the Idzu-Bonin, Marianas,and
Ryukyu Ocean De-
pressions
ASSOCIATIONs Institute -oF Oceanology, AS USSR
(Institut okeanologii Akademii nauk SSSR)
PRESENTEDs November 24, 1956, by N. M. Strakhov, Member of
the Academy
SUBMITTEDs September 29, 1956
AVAILABLE: Library of Congress
Card 5/5

20-5-34/48
AUTHORSt
Bezru
Boychenko, I. G. Zhiva-o, A. V. , Zenkevicii,
U

N. Le Kanayev, V. F. and Udintsev, G. B.
TITLEt
New Data on the
Rules Governing tho Morphology of Submarine Relief

Olovyye dannyye
o zakonomernostyakh stroyeniya. podvodnot,o relyefa)
Q
PERIODICALs
Doklady AN SSSR, 1957, Vol. 116, Nr 5, PP- 841 - 844
(USSR)
ABSTRACTs
The cooperation of the two institutesgiven under
"association"

facilitated the obtaining of the characteristic of
some outlines

of the morphology of the submarine relief, together
with the results

of foreign expeditions. These outlines were
formerly either not

to a great extent known or subestimated.
Conceptions of the borders

of greatest morphological areas or of
the forms of first order like

the submaTine margins of the
continents, the zone of the conti-

nental slope, and of the ocean
gulf ("lozhe okeanall) could be de-

fined exactly; furthermore the
rules governing the order of the

great relief forms (forms of
second order), as well as the cha-

racter of the connections in
the order of smaller forms could be

explained. In the coastal zone
and in the shallow water zone the

bottom of the sea is nearly
everywhere levelled and slopes towe-rds

the sea extremely softly.
This bottom area is bordered by a bend of
Card 1/4
the bottom,
towards the sea. Behind it the bottom changes into a

20-5-34/48
New Data on the Rules Governing the Morphology of Submarine
Relief
0
more articulated area. This threshold does not lie deeper than
300
m, on an average.of.130 m. The levelled area is towards the sea
replaced by either the area of the submarine mar,,-,in of the
cortin-
ent or by the zone of the continental slope. The latter has con-
siderable inclinations as well as a very complicated relief. The
origin of the levelled area of the bottom in shallow water is to
be assumed to be in connection with the abrasion-accumulative
levelling processes. The surfaces of the submarine margins of the
continents often cover larg areas in comparatively shallow places
of the ocean. As a rule they continue the coastal plains of the
continent. Their breadth ant dopth vary in vast borders; single
sections lie in a depth of from 1000 to 1500 M. Up to now the
tech-
nical terms: continental abyss and continental si,elf were not
used
precisely enough. The expression continental slope does not re-
flect precisely the fundamental traits of the transition zone
from
the continental area to the ocean "sprout" (11lozha okeanov"). It
would be more precise to call it "zone of the conTinental slope".
Examples for a very complicated and a more simple structure are
given. The upper margin of the zone of the continental slope cor-
responds either to the exterior margin of the levolled area of
the
coast-near shallow water or to the exterior marj;in of the
submarine
Card 2/4 marginal zone of the continent. Sometimes there are
also compara-

20-5-34/48
New Data on tho Rules Governing the Morphology of Submarine
Relief
tively steept steps. In such cnsee one can speak of a takin.-
part
of the continental marginal zone in the development of the Zone
of
the continental slope. The lower margin of the zone of the
conti-
nental slope is rather clearly characterized by a bend of the
bot-
tom area in the transitiontDthe ocean sprout or by a still
sharper
bend in the transition to the flat bottom area of the oceanic
deep
sea channelswhich in many regions are bound to the lower part of
the continental slope. The ocean sprout is characterized by a
Ereat.
variety of forms and relief typest elevations, mountain ridoges,
and single mountains occur frequentV. The great relief fonis (of
second order) are distributed in all parts of the oceanic
bottom.
It is difficult to observe the continuations of ~he great relief
forms of the continent in the levelled part of the coast, they
are, however, better marked in the zone of the continental
slope.
In several cases a connection between the relief forms of the
zone
of the continental slope and those of the ocean sprout becomes
vi-
sible. Towards the land they are only seldom continued on the
con-
tinental margin. The great variety of the small -round relief
forms
can be comprised in 3 groups: 1.) a relief in which the traits
of
Card 3/4 the original relief are long time conserved which is
covered by a

20-5-34/48
Pew D4ta on the Rules Governing the Morphology of Submarine
hei-Lel
sedimentary cover of the same thickness. 2.) the levelling relief
the original unevenness of which is filled in ; the thicknes3 of
the sediments increases here in the depressions, and 3.) a level-
led relief in which the sediments cover all unevenness of the ori-
ginal reliefj in the depressions the layers are much thicker and
broken at the elevations. There are 7 references, 4 of which are
Slavic.
ASSOCIATIONt Institute for Oceanology, Institute for GeoGraphy AN
VS6R
(Institut okeanologii, Institut geografti Akademii nauk SSSR)
PRESENTED: Jday 13, 1957, by I. P. Gerasimov, Academician
SUBMITTED: June 11, 1957
AVAILABLE: Library of Congress
Card 4/4

baAiuK9V, P. 1.
Recent Exploration of Bottom Deposits in Far Eatern Seas anJ the
Northwestern Part
of the Pacific. The Article Reports on the character and the main
mineralogical Constituents
of botton depos-its. and or the use of echo meters. The
distribution of carbonate deposits
and the availablelity cf certain elements, such as phosphorus,
vanadium., titanium, etc., Is
discussed.
10"KK oceanograp
Iiic Research of the Northwestern Ptirt uf the Pacific Ocean
Moscow, izd-vo AN SSSR, 1958, 148 p. Its: Trudy-, t.2.
This collection of articles reports the results of observations
made in the Pacific
by the Institute of Oceanology of the Academy of Sciences, USSR. In
1949, the Institute
launched a systematic five-year program of scientific exploration
of certain hydrographic
peculiarities of the Soviet Pacific Area. The operations were
carried out as a "Complex
Oceanographic Expedition," using the Motorboat Vityaz' as its bas.
The Expedition warked
in collaboration with the Hydrographic Institute of the Soviet Navy
(W15), the Pacific
Institute of Piscatology and Oceanography, ans dome 4-0 other
instittutes of the Academy of
Sciences. Between 1949 and 1954, 18 trips were made, covering about
130,000 miles. Among
the subtects of direct concern were: Meteorology, hydrology,
oceanography, hydrochemistry,
sedimentation, geography of the littoral, geology and contours of
the sea bottom, fauna,
plankton, microbiology, and gravimetry. Twenty-eight authors
contributed to the collection
j17
which consists of 27 articles. There are: 6 gables, 23 diagr-ams, 3
_'Ustrations (Photo-
graphs of the littoral), 4 maps. There are no references.

BEZRUKOV. P.L.; ZE113VICH, N.L.; KAMM, V.F.; UDINTSRV,
G.B.
Submarine mountains of tbo Kurille Islands. TriiV
Lab.vulk. no.13'.71-88
1 58. (MIRA 12:3)
Murille Islands--Ocean bottom)

IC,
(ins4u-.
Ud

?I tlic Int.".

BEZRUKOV. P.L.
Oceanographic investigutions in the northwestern
part of
the Pacific Ocean, August-October 1954. Trudy
Inst.okean.
16:70-97 '59- (MM 13:3)
(Pacific Ocean--Oceanographic research)

P. L.
Oceanographic investigations in the northwestern part of
the Pacific Ocean, September-November 1955 Trudy lnst.
okean. 16:131-157 159. iMIRA 130)
(Pacific Ocean--Oceanographic research)

Bottom sediments in tb
36:169-1~10 '59.
(Kurile
n Kurile area. Trudy Inst.okean,
(MIRA 15:4)
region-Deep-sea deposits)

V r~ Z-.
PHASE I BOOK EXPLOITATIO' SOV/5331
International Geological Congress. 21st, I-openhagen, 1960.
Morskaya geologiya (Marine Geology Moscow, Izd-vo AN SSSR,
1960.
205 p. 2,500 copies rinted. ~Serles: Doklady sovetskikh
geologovs problems, 10~
Editorial Board: P. L. Bezrukov, Reap. Ed.; A. V. Zhivago,
V. P.
Zenkovich and 0, B. Udintsev; Ed. of Publishing House: V. S.
Sheynman; Tech. Ed.: V. Karpov.
PURPOSE: This book is intended for geologists and
oceanographers.
COVERAGE: The book contains 18 articles representing the
reports
given by Soviet geologists at the 21st. International
Geological
Congress. Individual articles deal with the bottom
topography,
sedimentation, and tectonics of Oceans (Western Pacific and
Southern Indian), as well as the geomorphology and
tectonics of
the Black and Cas
,pian Seas and Soviet sectors of the Baltic,
An English r4sume accompanies each article. No
personalities
Card I/P
12-11

-, BEZRUKOV,___P..-L..,; LISITSYN,
Classification
3213-14 6o.

BBMIOV. P.L.
Bottom sediments of the Sea of Okhotsk. Trudy
Inst.okean,
32;15-95 160. (MIRA 13:6)
(Okhotsk, Sea of--Deep-sea deposits)

-BEZRUKOV, P.L.; PETELIN, V.P.
Manual for the collection and preliminary processing
of marine
sediment samples. Trudy Inst. okean. 44:81-111 160.
(MIRA 14:2)
(Deep-sea deposits)

SWAROV, Y.N., doktor-geogr.nnukp otv.red,!_I~~~oktor
pmol.-mineral.nouk, red.; LOUGINOT, V.T., kand.geograf.nauk,
red.;
R WAOVUATA, N.A., kand.gsotr#f`.naukq red.; PANFILOVA, B.G.;
kand.geograf.nsuk, rea.; K021YANINOT, M.I.,
kand.geograf.nauk, red.;
PWJVIN, V.I,, red.; TUGARINOT. D.N., red.izd-va; NOVICHKOVA,
D.N.,
tekhn.red.
[Basic geological and hydrological features of the Sea of
Japan)
Oanovnys cherty geologii i gidrelogii IAponskogo moria.
Moskva,
1961. 223 p. (Km 14:3)
1. Akademiya nauk SSSR. Institut oksanologii.
(Japan, Sea of-Submarine geology)
(Japan, Sea of--Hydrology)'

MDRUSOV9 Niko3mq Ivanovichp alcademik (deceas9d)l
SHkTSKIYp N.S.# skademikv
glav. red. [domased]; SECEMAKOVp D.I.9 aimdemikp glav.
redo )P-
EM9 R.L.9 otv. r*d.j-B=UMDVq POL42-redol DAVITASH=-q
L.Sh.9 red.;
DOLGOPOLOVp N.N.'q red.; 'v . I i .9 rea.; MINM9 V.V.g
red.;
NEVZSSKUAv L.A.t red.;-ZZRZ3[Np A.G.0 redq TANSMNt A.~*g
akademikp
red.1 POLINOVAp T.P.9 tekbn. red.
[Selected workel Isbranays tru4. Mookwav Isd-vo Akad.
nauk SSSIR.
Vol.l. 1961. 73.0 p9 (paleontology) (MM 3.418)

Fqw a"bmitted for them 10" Felfic SCIGI-
COnC"$fi, H-02211, R&Wdt 21 'ag-
6 3-P 1961.
ArAPC'/A, G_ V.,
All from the Inctitute t Azed-,r or !; t
vr, usz;.!
botton relier or the r,.lifil ~- A t.
t *I " (S */:.A)
r_.t.,t,-. of A-t-v Or ::?1e.- tr~_R
Kletoph-e rl.hes of the their
111.C)
-at"t-Itt
r of 0-10,;/
t
AVU:7-~iV,T. D. (r. bl-!, "t UkVs, 1.),
Inetitute Or C~ioc/ of C-e repostt.,
end G.-hel.try - (Title of ";- I.
bl~~rred; f.11.4-.z I,
"Y-Ximte t1t1e) - "YA:_h7y"I,5mi_?~,*
jay'r
and rographim date," 'r=.C)
I&LUM14 -L. K_ 1-6t4tute of z4rth ph,~-m
1-1 0. Y~. sch-Adt -
~r~ charelter of streAsea wA mT--m -n
the foci if the
PmetfLc ela=lc -.e~ (sectioz V:-,.C.2)
--tit,t. ..- zoalGimr, "On the P-,fic
orie.- 3f
the A-rhlzh~lleaa f=lly- 11T.C)
Y.;rt.X St.t. Ur.1-r.-Ity - "On the
he,.'. ;-e....
In the veterj7oe the Fir Se- (sect_,~
vjj.B)
1-t - -on the tr-fi-ti-
f
pl-k-on the P-1r.: dr-Ift -4 1. -he
-11I.C)
z:XXICY.-Y. ,T_ =d 1-ti-tute of Emh
'le'a
0. TU. Blhlld* - " G-t--L- -1 ;. of the
Oby.3.1 IO~r ... Ii. of
the ... of J.;.Z, 7=.C.2)
WPTXAY77~a~j!- Ilat-ute Or Oca~~Il&r -
*Aze,~Uamil~ of quid
"A berk teeth st the we= n-r- (Setti.o.
--p=1 'P,L_z=tit,~t* or 0ce=l,'.oCf
se-l-entaton
end Via geol-odicaa hIstc-f of the C~-Ak
so&* (Svc-ion val.c.1-)
-A"
27-=, r- 4-L ;4317MO-A' P-1 72~-_ 1 V'
P-1 -4 r~-TL_A-Po
Ill, A, arid lletmrze of Get-lorl -
'so- epee.-fic, ,..t-x 1. .he
Ii.t.-Ib=I.. or bye.,a
pejea -I-, (A--Ph-lpc-:.)* 111.C)
-,.- I . - IoOtit~t. .., - %e., ch-t. of
eOtIdI 11"..
end the ch-ter of tLe- ;h--= - %he
?--If.-c -.~ceao' (rection
Imatt.
.ut,
of GeamoLoMr -The distrLb~uon af --he
blo- In the
F.,Ifs. OIe-- (Section. 11I.C)
IOatttutc of C-Io~ F:eploltntilon of
Combunti-ble
Mtao,ia.l. ~Ihv &1&eace'Lz cha~ez I=
bGttc= -iilent. from
the central paurt of the
lartitMe of G~Iccf - -SelilIntttir. ead
the regul
'arl
ties in the dlstrlbirtt~m of ll-ne-I
re-n-ej in the j:cOAyr..IL-1
bestr.m of the Tertia-1 ;,rind In th~
area, of -d the
sakhl.. 1.1-d" (S.I.L.. Vl-.c)
7V_VjM.A,Y__, wA_ZAT7Z7~,_ji:_._P.
Il.atit~te of 0-.oloc/ -
"30m chemLc&l fenturc3 of zedll-ts =~.
&ro-.1 -1-Ions r-catlaZ
the lat ter in the Puciric (=terLaZA Of
the morth.,catert,
VLI.C.l)
VM=_j_A., Toetitute Of Q!e=zIo*7/ - 'A
stuly of eq-tor"al
curr.m. I. the -.ter. P-If.~' (S-til-
VIL.B)
=d I-stitu-c of Ott,_noloc, -
-The !.rentio. or Ir =-.e, In the
r.:2m!1em ;=- or the pacim-
Co.-
IA. ,Z lnatit~-te of Gc-XcCj - 'The
rcZionz of forlation
A tra,nmItI** lou-I. .1 ant I-ly.I..- In
the northern prt or the
Pncifl~ Oe- (3-ti- VII.A)

STRAKHOV, F.M., akcadenik, red.; ~'BZ"U"OV.- P.L. .
red.; YABLOKOV, V.S..,
red.; NOSGV, G.I., red. izd-va, BRUMLSY V,V.,
tekhn. red.;
THECUIROVA., S.G., tekhn. red.
[ibecent sediments of seas and ozeans; transactions
of a
conference held on May 24-27, 196C! Sovremennye
osadki Morei
i okeanov'. trudy soveshchaniia 2,4-27 maia 1960~
Moskva, Tzd-vo
Akad.nauk SSSR, 1961* 644 po (M]RA 15:1
1. Akadem-Lya naak SSSR. Komissiya po osadochnym
rodam.
2. Geologicheakiy institut AN SSSR (for Strakho-vT.
3. Institut
okeanologii AN SSSR (for Bezrukov).
(Submarine geoiogy)

BFZRUKOV, P.L.
Exploration of the Indian Ocean during the 33rd cruise
of the
research ship "Vitiaz.11 Okeanologiia 1 no.4:745-7 161.
1 _53
(MIRA 14:11)
(Indian Ocean--Oceanographic research)

DOGORM, V.G.; BEZRUKOV, F.L., prof.
to I
Vitiaz"' in the Indian Ocean. Priroda 50 no.10:8?-lrC
n 161.
('MRA 14:9)
1. Institut okeanolouii AN SSSR (Moskva). 2.
Ohlen-korrt-Fpondent
AN SSSR (for Bovorov).
(Indian Ocean--Oceanograpbic researcb)

S/020/61/139/001/018/018
B103/B229
AUTHORS: Bezrukov. P, L., Zatonskiy, L. K~, and Sergeyev, 1. V.
TITLE: Afanasly Nikitin - Mountain in the Indian Ocean
PERIODICAL- Akademiya nauk SSSR. Doklady, v. 159. no. 1, 1961,
19~1, - 202
TEXT: The 31 St expedition on board the vessel "Vityaz"
discoveredan under-
sea mountain range, extending in a depth of 4500 - 4700 m for about
150 miles
south of Ceylon, in the north-western part of the Indian-Australian
ocean
basin, in Decem)'~erj 1959, Above,there is a high seamount, The
3~rd expedi-
tion of the "Vityaz" carried out an echo sounding of the searijount
on
January 9, 1()61. It was sug~~ested to name the mountain after the
first
Russian who traveled to India, Afaragiy Nikitin. In the course of
echo
sounding the area of the seamount, was traversed in different
directions, arid
-11, 'r'ig. 1).
two new minimum depth of 1666 and 1549 . respectively were found k.
The position of the ship during echo sounding*;Aas jeteratined by
tne usual
navigation methods: by astronomical observations arid calculations.
The
astronoz.-.ical determination was carried out at rtation no. 490(
'?, 3 miles
south-west of the summit of the mountain. This determinati--n
cerved as end
Card 1/6

5/020/6111/1 7~-/001/0 15/018
Afanasiy Pikitin - Mlountain ... B 10 z,/'B229
point of the calculation based on the observation from stbtion
no. 4908, and
as initial point of the calculation of station no, 4910, The
coordination
of measurements and the transcription of the recordings on a
scale of
1 : 125,000 were carried out by L., P~ Nasvr'. The echo sounding
was, carried
out in the deep-sea range echo sounder MC-?6H(IOS-2610. The
frequency of
the measurement amounted to 10 pulses/mi:n. 'The depths were
transcribed on
the map immediately from "lie echo-sourider record, The
coordination of' the
measurements was satisfactory. The data of echo sounding served
as a basis
for a bathymetric chart (Fig.)). Data obtained during the 1s t
voyage were
also used- As can be seen from Figs. 2 and ). the mountain,
according to
the morphology of its slopes.. constitutes a volcanic core.
Apart from the
Afanasiy Nikitin mountain there are many other summits in this
mountain range
with minimum depths of: 2500, 2892, 3050, and 3230 m. At the
southern slope
of the range there is a deep gully which, at a depth of 4880 m
has a flat
b3ttom 7 - 8 miles wide. South of it there is an elevation of an
average
aepth of 4300 m. The width of the mountain ran6e is not yet
known, As a
result of the bathymetric chart and the analysis of the depth
distribution
outside the map limits, the authors consider the mountain range
to extend
from west-noTth-west to east-south-east for at least 300 miles.
Future
Card 2/6

S/020/61/139/001/018/018

Afanasiy Nikitin Yountain... B103/B229

'Y
T'.

investigations
are to show,whether this assumption is correct.
A-sampling.

of the soil at
the slope of the Afanasiy Nikitin Mountain,
at a depth of

2380 m,. showed
a fine-grained globigerina ooze. A series
of pictures

showed a changing, spotlike distribution of ooze and hard
rocks. The

composition of
the rocks could not be determined. Ab a result
of the

analogy with other undersea volcanoes of the central part
of the ocean they:

are thoUght to
.
be basalt rocks. There are 3 figures.

ASSOCIATION:
Instibut oke&nologii
Akademii nauk SSSR (Insititute of

Oceanology of the Academy
of..Spiences USSR)

PRESENTED:
March 30, 1961 by A. L. Yanshin,
Academician

SUBMITTED:
March 2.6, 1961

e

.Card 3/6.

BEZRUKOV, P.L.
Irregular distribution of oceanic deep-sea sediments.
Okeanologiia
2 no.1:9-25 '62. (MIRA 15:2)
1. Institut okeanologii AN SSSR.
(Deep-sea deposits)

BEZRUKOV,, F.L.
Some problems concerning the zonality of sediment
formation in the
world ocean. Trudy Ckean.kom. 10 no.3-13-8 162. Ouu
15:3)
(Ocean) (Sedimentation and deposition)

BSXRLWVP P.L.; PETELIN, V.P.
Bottom sediments of deep-sea trenches in the western
part of the
Pacific Ocean. 'h-udy Okaau kom. 10 no.3:66-69 162.
(MIRA 15:3)
(Pacific Ocean-Deep-sea deposits)

BEZRUYOV,--k.L.. LISITSYN, A.P.; PETIELINJ.P,~,*
SKORZJYAKOVA,N.S.; AOIW-52TICH, E.A.
Map of the 2acific Ocean Sediments
Report submitted for the 13th General
Aseembly,IUGG,(Oceanography) Berkeley, California,
19-31 Aug 63

YABWKOVp V.S., oty. red.; ALEYRY.-F.L., red.;
SHMSOV, M.S.,
red.; SIIEVCHEZIKO, G.P., tekhn...Fed.
(Deltaic and shallow-water marine sediments]
Del'tovye i
melkovodno-mort3kie otlozheniia. Moskvnp Izd-vo
AN SSSRI
1963. 262 p. (MIRA 16:12)
1. Akademiya nauk SSSR. Komisaiya po osadochnym
porodam pri
otdelenii geolo o-geograficheakikh nauk.
?Sediments (Geology))

BEZRUKOV, P.L.
Study-of the Indian Ocean on the 35th trip of the
research ship
"Vitiazl."' Okeanologlia 3 no.3040-549 163. (MMA
16:8)
(Indian Oqwm-.Oeeanographic research)

BEZRIM011, P.L., doktor geol.-mineral.nauk
Research conducted by the ship "Vitiaz" on the program
of the
International Indian Ocean Expedition. Vest. AN SSSR
33 no.8s
96-104 Ag 163, (KRA 16:8)
(Indian Ocean--Oceanography)

BEZRUKOV,, P.L.
Distribution of ferromanganese nodules on the
Indian Ocean
bottom. Okeanologiia 2 no.611014-1019 162. (MIRA
17:2)
1. Institut okeanologii AN SSSR.

BEZRUKOVO P.L.; KANAYEV, V.F.
Basic characteristics of the bottom structure of
the
northeastern part of the Indian Ocean. Dokl. AN
SSM 153
no-4:926-929 D 163. (MIRA 17:1)
1. Institut okeanologii AN SSSR. Predatavleno
akademikom
A.L. Yanshinym.

tv
l3ccjlng~,, cii, the cf nr,~F:n-, and
'j D.01-6 j v.G.A.7Ti 1Q6", I t 's
kl:ln~iy sovetAikh gil-~Iogov, problemn 16) kmir.
j I -
1. Intornational Ge.31o,~iet.'
aelegat_iy;~.

BEZRUKOV, F.L.
Sediments in the northern and central parts of the
Indian Ocean.
Trudy Inst. okean. 64:182-201 164, (MIRA 17:7)

L 33164-6
EWT(l) OW

.
ACC NR, Ap6ol4282 01) SOURCE CODE: UR/0213/66/oo6/002/0261/0266

H
AUTHOR: Bezrukov, P. L.; ~~Lovl A. Ya.; Cherny8heva, V. I.

ORG:
Institute of Oceanology, AN SSSR (Institut okeanologii AN SSSR);
Radium Insti-

tute (Radiyevyy institut)

TITLE: Petrography and the
absolute age of the basalts on Indian Ocew-flD=

SOURCE:
Okeanologiya, v. 6, no. 2, 1966, 261-266

TOPIC TAGS: ocean
property, oceanographic expedition, oceanographic ship, basalt,

-
- -1
am petrography

ABSTRACT: Volcanic rock from the bottom of the
Indian Ocean was sampled during the

1959-1962 cruise of the
research vessel "Vityazl". Petrographic study of the samples

has
shown that in the most cases the rocks were olivine and
nonolivine basalts and

basalt glass (hyalobasalts). Chemical
analysis indicated that the part of the samples

is low-potassium
tholeitic basalt, and the other part is alkaline basalt. The K-

argon method was used to determine the absolute age of four
rockt samples from two

stations in the southern part of the
Ocean. Their age appeared to be about 60 million

yr,
correspondingtoLowerPaleogene (Eocene). Orig. art. has: 1 figure
and 2 tables.

(Based on authors' abstract.) [NTI

SUB CODE: 08/
SUBM DATE: 12jan66/ ORIG REF: 007/ OTH REF, 006/

1 Cord 1/1 UDC:
552.2/333.$(267) -

L 32201-66 EWT(1) GW
ACC NR. AP6Oo8O57 . I SOURCE CODEs UR/0020/66A66/004/096-V
AUTHOR: Chernysheva, V. Lj Bezrukavt P. L.
Offi: Thstitute of Oceenolou.AN SSM(Institut ;)koanologii AN SM)
TITIEt Serpentinites from the ridges of the Arabian-Indian Ridge
SOURM AN SSSR. Dokladyx v. 166s no. 4o 3.966, 961-964
MIPIC TAGS: underwater photographyj oceanographic expedition,
petrologyj, geochemistry,
oceanographic ship/Vitvam.oceanographic ship
i ;=RAM-Further subsita~tlafion has been found for the belief
that the under-
water mountain ranges in the various oceans of the world quite
universally
consist of ultrabasic rocks. On the 33rd voyage of the Soviet
research
ship "Vityaz" in 1960-1961, 27 bedrock samples were dredged from
the
sea bottom close to the central Arabian-Indian Ridge (Carlsberg
Ridge)
(5c2418" N and 62'0815" E). These specimens varied in size from
2 to
6 cm, were thinly coated with Iron and magnesium oxides, and had
angular facets. This latter fact, in conjunction with underwater
photo-
graphs, has been accepted as evidence that they represent
fragments of
bedrock which had fallen from the steep slopes of the underwater
ridge
to form talus deposits on the ocean bottom (at a depth of 1920
m). Chemical
and petrographic analyses.of these specimens made by the
Institute of the
i Card 1/3 UDCi (;9;2.M

L 322ol-66
~~`_C Wt
:.~'Ifolugy of Ore Deposits, Petrography, Mineralogy, and
Geochemistry
Academy of Sciences USSR showed that four of the samples were
L,-wk-gray basalts and twenty-three were green-gray serpentinites.
Thin-section examination revealed that the basalts consisted of
L'i Igloclase phenocrysts, monoclinic pyroxene, individual grains
of olivine,
an ore mineral in an intersertal mass. The olivine had been almost
npletely replaced by green-gray chlorite-type minerals. One speci-
'ner
yielded the following chemical analysis:
SiOl 49,10 NO 6,95 NIO 2,63
TiOt 1,5f MnO 0,25 KjO 0,20
All% 16,80 hIgO 7,19 IJj0* 0,60
Fej0p 2,95 C_%0 11,35 11%0- 0.5A
09,97%
~-Phe content of K20, N20, mil T'02 was relatively low and
generally re-
sembled that of specimens described by Wiseman, which were also
collected in the Indian Ocean, and by Engel, obtained from the
Mid-Atlan-
tic Ridge area.
Card

32201-66
ACC NR, AP6008057
The s6rpentinites consisted mostly of several different types of
ser-
Tentine with small grains of talc, individual grains of chrome
spinels,
Iqnd very small particles of magnetite, repl aced in places by
iron hydrox-
iide.- These rocks were classified as chrysotile-antigorite
apoharz-
burgites. Chemical ainalyses yielded the following r .eBuIts
Slot
40.52
FeO 1,43
NasO 0,38
TiOt
0,20
MnO 0,48
X.10 0,12
Also,
'
3,64
NIgO33,68
11,0- 1,40
Fesoe
0.63
CeO (1,45
11,0+11,41

100,0%
Serpentinites similar to these and the peridotites from the rift
zones*
of the Nlid-AtIantic. Ridge, have been dated as being older than
the basalts
of these regions, and Hess suggested that they represent rist-s on
the
mantle's surface. This'papei, was presented 15y D.S. K6r~hin6kij'
A'ademicianp
c
1j Oc--t-o,b-e-r 196'5'-+ Origo arts hass 2 figarese L&Bt v* 2a no*
smDATij: -,oeoct65 / omo Rms ooo / oTH mws oo5
SIM CODE.: OB 17
Card -3/.1

ANDRUSOV, Nikolay lvmiovich, akademik
(3861-1924); SHCHERBIKOV,
D.I., akademik~ glav. red.; YPNSIHN, A.L.,
akademik,
gIfiv. red.; ZEkEUCH. L.A... otv.
red.;..~EZRUKOV, P.L.,
otv. red.
(Selected works] lzbrannye trudy. Moskva,
fauka. Vol-4
1965. 402 p. (MIRA J-8.Ir")

1, Bezrukov, P.P.
2, USSR (6oo)
4. ARIENIA - PHOSPRATES
7. Paleozoic phosphorities of Armenia and the NakhIchevan'
A.S.S.R. (Abstract.)
Izv. Glav. upr. geol. fon. no. 2. 1947.
9. Monthly LIZ_+- 2_f Russian Accession;. Library of
Congress. March 1053 Unclassified

BABUS11KINi, 14.1'. ; MIPEOVA, V.S. ; BEZIRIUKOV)
V.A. -P 9 V.1~1.
Removal of sulfil- compounda from fuel gameo in a
flu;dized
bed of cinder at high tomperatureq. Izv. vyv.
uche). zav. ;
khim. i khim. tekh. 7 no.3:445-149 164.
17:10)
1. Ivanovskiy khimiko-teklinologiche ski y
dnsti,,ut,--'.-,afedr'I
kh3n-lcheskogo Rjash-inostroyeniya.

BEZRUKOV, V.I., starsbiy prepodavatel'
Determining the hollow champfer of a helical
gear-wheel tooth
shaped with a rack. I&v.vys.ucheb.zav.; mashinostr.
no.7:169-176
,61. (MIRA 14:9)
1. Chelyabin3kiy politekhnicheskiy institut.
(Gearing, Spiral)

EEZRUKOV9 V.I., aspirant
~ 1. -
---atnvolute gear transmission composed of bevel gear
wbeels having
arbitrary axis positions. Izv.vya.ucheb.zav.;
mashinostr. no.6:
40-50 163. (MIRA 16:10)
1. Chelybinskiy politekhnichoskiy institut.

BF_7RUKOV,, V. 1. (Cheiyabinsk)
Some problems of the geometry of bevel gears compcsed of
-Involute
straight bev-el gear wheels. ~Iashinovcdenie nc.4,":5-63
165.
(MIRA 18 a 8)

L;17091-63 E"(q)AWT(m)ADS AFFMASD-3 RM/JD
~ACCESSION Nft: AP3004694 S/0189/63/000/004/0065/0066
!AUTHORS: Bezrukov, V. I.; Lapitskiy, A.,V_t; Vlasov, L. 0.
.TITLE: R.~Ction 0 potassium metaniobate with the salts of some
metals
SOURCE: Moscow. Universitet. Vestnik. Seriya II. Khimiya, no. 4,
1903, 65-66
TO?1C TAGS: potassium metaniobate, sodium hydroxide, solubility,
complex forimatio4
salts of metals
A~STRACT: The reaction between potassium metaniobate and-the
salts of heavy
.metals, as well as the solubility of the resulting product in
cacess of KNb031
were studied by the nephelometric, potentiometric, and
conductivity techniques.
In view of the high pH of KNO solutions, parallel tests were
conducted with
The concentration of ~, 0 solutions were 0.1-0.001 normal) that
of the
heavy metal salts 0.05-0.0005 ngrnial. In all tests the KNbO
solutions were
added to those of the heav metals. Salts of dibasici 2 Pb formed
comoounds
Cu an
'which were soluble in excess XNb0 and FOH. The color of the
kk"b03 pric com-
pound differed from that of the ohginal cupric salt, and the
soluticoun remained
clear after a 32-time dilution. Ferric and ceric salts, as well
as those of Yg
and Cd. formed flocculent compounds insoluble in excess KNb03 or
KOH. The salts
bard
_-1/2

L 17091-63
'.ACCMION NR- AP3004694
~.of Zn, Al, and trivalent Cr produced compounds insoluble in
excess KNbO but
3
soluMe in excess KOH. fhe Zn and Al precipitates were white, and
the one with
lCr was green. The latter dissolved in excess KNb03, but further
addition of it
resulte ecip tio
in r ital n. Ferrous, cereous and rmnganous salts, as well as
'of CoMd Ni ~'Iformed compounds that were soluble only in excess
KNbO The solu-
A- 3'
tions were all colored. The formation of complex is suggested.
Orig. art.
has: I table.
!~A!ZOCIATION. Moskovskiy universitet, Kafedra radiokhimii (Moscow
University,
:,De
partruent of Radiochemistry)
--SUBMITTEED: 15Feb62 DATE ACQ: 06Sep63 ENCL: 00
~I;SUB CODE: CH NO REF SOV; 002 OTHER: 002
Card 2/2

LAFITSK-TY, A.V.; BEZRUKOV, V.I.; VLASOV, L.G.
Interaction of potassium tantalate with salts of
certain metals.
Vest. Mosk. un. Ser. 2: Khim. 18 no.502-33 S-0 163.
(MIRA 16:11)
1. Kafedra radiokhimii Moskovskogo universiteta.

LAPITSKIY, A.V.;_P~PRUKOV, Vj.; VLASOV, L.G.
Soluble niobates of some transition metals.
1zv.vys.ucheb.zav.;
khim. i khim.tekh. 7 no.2:175-179 164-
(MIRA 18:4)
1. Kafedra radiokhimii Moskovskogo gosudarstvernogo
universiteta.

ACCESSION NR: AP40129TI 3/0020/1b4/1!)4/OO4/O8W/O8TO
AUTHORS: Lapitsklys A-V.; Vlasovs L.G.; Bszx-iixov,, V.I.
TITLE: Production of het*roniobates of certain transition metals
SOURCE: AN SSSR. DDklady*,.v. 154, no. 41, 19b4# WS-UTO
TOPIC TAGS: heteronlobate, potassium cerous n1obate, potassium
cuprous n1obate, potassium ferrous n1obate,# potassium nickelous
niobate, potassium cobaltous niobatet nepholometry,.optical
spectrap
electrophoresis, molecular electroconductivity, anion mobility,
anion diameter
ABSTRACT: The reactions or aqueous solutions of potassium
metanio-
bate with transition metals salts Pb (n), Cr (III) salts
which are soluble in excess potassium n1obate and NDH; Ma
(II).. Fe
(II), Co, NXI and Ce (III) salts which are soluble In excess
potas-
sium metaniobate but-insoluble In MDH) and the chemical and
physical
properties of the products were studied. Nephelometric observa-
tions indicated that precipitates were formed with equivalent
amounts
Ca,d 1/3

ACCESSION NR: AP40129T1
of reactants: at 1:2 metaltnioblum ratio for divalent and 1:3
ratio
for trivalent metals. 7hese precipitates dissolve with excess
pre-
cipitant to form clear colored solutions (except for.Pbs which
in
colorless). The formation of hetero was further confirmed
from their optical spectra and-from electrophoresis studies In
which
the metal ions migrated to the anode Indicating they became
part of
the negatively charged particle. The following compounds were
ob-
tained:
]K4 EFe Nb03 4 (OH)21 11H20
K4 ECO N __ 4 (0H)21 :lOH2O
K4 C Ni N:4- OH
ON) 0
r4 CO 2 2
K4 Cu NbOq)4(011) 2%00
xi.t ce Nbop2(0'04.J'5%O
The maxijml- molecular electric conductivity of solutions of
the
last three compounds,, and the nobility and the
offective*anion dia-
meters were determined. Orig. art. baas 2 tables.