SCIENTIFIC ABSTRACT BURYANOV, V. - BURYGIN, V.A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000307710011-1
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 12, 2000
• Sequence Number: 11
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

BUR I YANOV J, V.
High-frequency kitchen stove. ObBhchestv. pit no.9:63 S t61.
iMIRA 14A1)
(Great Britain--Stoves., Electric)

ANDREYEVI B.V.vARTEV.'YEV, S.P.; ARKHANGEL'ShY, V.M; AFANASIYEV, L.L.;
RABKOV, V.F.;*BRONSHTEIN, L.A.; BURICOV, M.S.; LUElANQY,--VA..,-
VARSHAVSKIY, I.L.; VELIKANOV, D.P.; VOINOV, A.H.; VYFdJBDV, D.N.;
DORMIDONTOV, A.V.; DIYACHKOV, A.K.; YEFREMOV, V.V.; ZHABIN, V.M.;
ZELENKOV~- G.I.; KALABUKROV, F.V.; KALISH, G.G.; KRAMAFMKO, G.V.;
KRASIKOV, S.M.; LAKHTIN, YU.M.;-MIMINp A.A.; ORLIN, A.S.; OSTROVSKIY,
N.B.; OSTROVTSOV, AA; RUBETS, D.A.; STEPANOV, Yu.A.; STECHKIN, B.S.;
KRACHATUROV, A.A.; KHOVAKH, M.S.; CRAROMISKIY, A..D.; SHARAPOV, K.A.
Nikolai Ro-novich Briling; obituary. Avt.transp. 39 no-4:57
Ap 161, (10A 14:5)
(Briling, Nikolai Ro-novich., 1876-1961)

KRASOVSKIY, S.S.; BURIYANOV, V.B.
Magnetic field of two vertical strata. Geofiz. sbor. no.7s86-91
164. (MIRA 17;U)
1, Institut geofiziki AN Ukx6SR.

KRASOVSKIY, S.S.1 BURIYANOV, V.B.
Usability of certain nomograms in magnetomatry. Geofiz. sbor. no.7:
97-104 164. (MIU 17;11)
1. Institut geofiziki AN UkrGSR.

11
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U
BTOYAJ.'W, V. F. -- " (;F TIIE i -1 f:F f I -,r i,'-,LL It.:; IN ;- , -rLL I N ~, ~," !. '. 1-1;r-
Ili 'rja: S*r,7,i::-n Tmj,, .-( MAY ;---- , I fl,-,~,rr: r1r L A i3: ~z J-~f f, I: f- N I ~-.w ~:
I rCl:t 11 r A I, ~'C I I ~101- I I I E-41 IIAL'I!-' It ( DI -- - EPTA7 I t)7! r,,,.P. -,I q- ,r- ~-;,;j-- I [~,, I c I ~i - I /. L.
~" C I 1:11CE)
I
50 : V~ctlFpw-yf-

if
LURI.Y.ANOV V. F.
.j
"Introduction to the metallurgy of cast iron and steel" B. G. Lebedev.
Reviewed by B. F. Burlyanov. Sov. kniga, Ao 8, 1952.

TATILOV. M.P.; RYBALICHMMO, A.M., inzhoner, retsenzent; BURIYANOT, T.F.,
inzhener, redaktor. _-O
[Lubrication of metallurgical plant eqaipment] Smaska matallurgi-
chaskogo oboradovanlia. Moskva, Goo. nauchno-takhn. isd-vo mashino-
strolt. i audostroit. lit-ry. 1954. 175 p. (MLRL 7:7)
(lubrication and lubricants) (Metal industries)

BJRYANgy,~Z, and KOIIOL:-,V, M.L.
UA manual on the designing of foundry worksho)-,s.',f Vestnik VZssh6y Shko&. Vol. 12,
No 4, T.p 59, 1954.
SO: D-81919, 25 Aug 1954.

BURIYAROV, T-,
~'
Wide-flange I beams rolled on rail mills (Troz: Jourlaal of the Iron
and Steel Institute, 1953, no-2, PP- 113-118). Abstracted bjr vo
Burlianov. Stall 15 no.1:92-94 Ja 155,, (MM 8:5)
(Steel, Structural) (Rolline-mill machinery)

SMIRNOV. V.V., dotsent; BMIYANDV, V.7e, kandidat tekhnichookikh nauko
"Mechanical eqmipment of rolling mills.8 A.A.Korolev, G.M.Nikol"
evakii. Reviewed by V.V.Smirnov, V-F.Bursianov. Stal' 15 no-31
286-287 14r 1550' OQU 8.5)
1. Hoskovskoys vysehsye takh-rdeheskoys uchilishche im. Bauman& (for
Smirnav)* Ze Vessoyusn" saoohnly politsktw4obsski7 institut (for
Burlyanov).
(Rolling-rell macblnarr) (Korolev, A.A,) (likolaevskii, G.M.)

RMIYANOY.V. kanclidat tekhnicheskikh nsm, .
"Precision rolling". A.P.Chekmarev. Reviewed by V.Barlyanov.
Stall 15 no.4:383-384 Ap '55. (miRA 8:6)
1. Ministerstvo tyashelogo mashinostroyeniya.
(Rolling (Metal work)) (Chekmarev,A.P.)

BURIYANOV,V., ref.
Planetary mills (From foreign periodicals). Stall 15 no.8:758-762
Ag'55- (YjaA 8:11)
(Rolling mills)
.0

BURIYANOV,V., ref.
,~,
Mechanical equipment of blooming mills (From: nStahl and Eisen."
G.Leder, no.8, 1953) Stal' 15 no.9:852-856 S'55- (KM 8:12)
(Bolling mills)

BURIYANOV, V,, referent.
r71,'.,--_ - ~ -, !I.--
Modern wide-strip reversing mills with furnace reelers.
Stall 15 no.11:1.047-1048 N '55. (MLRA 9:1)
(Rolling mills)

I
,~~~,Feferent.
Modern pipe-welding mills ("Iron and Steel Ingineer" no. 8, 1954).
stall 16 no.1:88-90 '56. MU 9:5)
(United States--glectric vjilding)

BIMIYANOV V.7 -AYISUMV, I.K,. inshener.,
OThe~1OW blooming-mill." A. A. Xorolev and others. Reviewed by V. F.
Burlianove' Stall 16 no.9:663 5 156, (MLEA 9:11)
1. Voesoyusnyy zaochnyy,politeMnioheskiy institut (for Burlyanov).
2. Hinisteretvo chernoy metallurei SSSR (for Antayferov).
(Rolling mills) (Korolev, A. A.) II

N6
From F~reign Metallurgical Literature. 381
PERIODICAL: "Stall" (Steel), 1957, No.4, PP- 378 - 384.
Temperatures and heat currents in the blast furnace
hearth. Review of literature on hearth cooling.
(4 references including I Russian).
By N. Leonidov. P-378.
A new continuous merchant mill.
(From Stahl u. Eisen, No.10, p.81, 1956).
By V. F. Burlyanov. P-384.
Automatic detection of defects during the production
of steel cables.
(From the Iron and Steel Engineer, 1956, No.2, p.187).
By A. B. Chelyustin. P-384.

BURIYANIOV, V.F.
BURIYANOV
New continuous rolling mill for small sections (from "Stdhl und Eisen,"
no. 10, 1956). Stall 17 no.4:384 Ap 157. (MLRA 10: 5 )
(Germany, East--Rolling mills)

BURIUNOV, V.P., kand,,takht.nauk; KOVALICV. V.N., inzh.
Continuous light-section rolling mill no. 250 at the Krivoy
Rog Plant. Biul. TSNIICM4 no.17:22-27 (325) 157. (MIRA 11:4)
(Krivoy Rog Basin--Rolling mille)

BURITANOV,- --referent
. -V.V
- '. ~N~'
New 255-tyPe light-section rolling mill. Biul.TSNIICHM no.17:57-58
(325) '57. (MIRA 11;4)
(Rolling mills)

BTJRIYANOVl V.F,, referent.
Continuous wire rolling mill in Niederrheinishche IlAte. Biul.
Tsmom no.21:6o 157. (MIRA 11:5)
(Germany, West-Rolling (Metalwork)) (Germany, West-wire)

BURIYANOV, T.F., kand. takhn.
. . ,
I- . .
Semicontinuous and combined mills need for rolling strips of medium
width, Biul, TSKIIGM no**22::25-33 157, (MOA 11:5)
(Rolling mills )

BELISKIY, B.S. [deceased]; BURIWOV. T.F.; VASILIW, Ye.P.; VITKM, B.Z.:
GAUAY, Th. S.; L-8Viif,-G. YU.M. 1. =YUSTKIN, A.B.;
ROKOTYAN, Te.S., red': ISTOMIN, A.19., rea.; 6z
red.;
NMPCKMSHCHIY, N.I., red. izd-va; KARASIV, A.I.,-,.tekhn. red.
[Ferrous metallurgy in capitalistic countries) Chernaia metallurgiia
kapitalisticheskikh atran, Ft.4.'[Folling mill production] Prokatuos
I trubnoe proizvodstvo. Bellskii, B.S. and othen, Moskva, Goo.
nauchno-tekhn. izd-7o lit-ry po chernoi i tovetnoi metallurgii.
1~58. 627 P. (MIR& 3-1:7)
I.- Moscow. TSentral'W nauchno-issledovatellskiy institut chernoy
metallurgii.
(Forgine) (Rolling (Metalwork)) (Pipe, Steel)

BURIYANOV, V.P., reforont.
1--- ,
M30-ornizing mills for acatinucnw large-utrip rolliTw. BiW.. TSNIIMM
158. (1w, ll:"-)
..0
(Rolling mills)

BURIYANOV. V.P., referent.
Universal light-sootion
158.

IBUR'YANOV, V.P., kand. tekhn. nauk.
Technology of rolling on blooming and slabbing mills in the United
States and Ganada. Blul. TSNII= n0.51-24-31 158. (MnA 145)
(United States-Rolling (Metalwork))
(Oanaft-Holling (Hotalwork))

BURIUNOT, V*P*, referent.
Development of the Gadsden (U.S.A.) plant. Blul. TSNIIGHM no.5:60
'58. (MIRA 110)
(United States-Steel industry',

XTAITAN079 V.7s,. kand. takhn. nauk; KOVAL3ffq V,N,p inzh,
~'. -,- zz,
Continucas wire-drawizg mill at the Irivol Rog Metallurgioal Plant.
Mule' TSNIIM no*6rI8-23 158, (MM 1195)
(Mrivoi Rog--Wire drawing)

BURIYANOTO: V.7., referent.
Wire mills at the Johnstown Plant* Biul. -TSNIIGHM no.1:53-55 158.
(United States-Rolling mills) (MIRA 11:5)

BURIYARQV
referent.
Combination mills for rolling narrow strips and wire. Biul. TSNIIOHM
n
o. (MIR& 11:5)
'6:59 158.
(Rolling Mills)

BURIYAHOV, V.P., referent
-
A-1; it. - I
- I -... ' 'n~ furnaces with parabolic crowns. Biul. TSIIIIGEIR no. 10:57-
59 158. (MIRA 11:7)
(Furnaces, Heating)

S OV/12 2-58-11-15/18
AUTHORS: _L~~Lil a~nov. V.F,.. Candidate of Techiii.-:-.al Sciences
~Cfierkasov. B.G-.7 Engineer
TITLE: Continuous Light Profile Rolling Mill 350 (1,Te-preryvnyy
melkosortnyy stan 35 0 )
PERIODICAL:Vestnik Mashinostroyeniya, 1958, lir 11, PP 79--84 (USSR)
ABSTRACT: The rolling mill. shown in plan in Fi.g.1 a-nd described
in detail is intended for round bar of 1G-30 mm
diameter, scfaare 'car 10.---70 mm. across, flat sections of
10-25 mm. width and 4-13 mm. thickness., equal angles
Nos.2-5 and strip between 50 x 1.9 a~d 200 x 6 mm,
all of carbon steel, Slabs of 80 x 60 and
106 x 106 mm. and about 9 a length are used. Of the
15 rolling stands, two in the roughing grcup and three
in the finishing group have -verti-z:al rolls,, the
remaining 10 haN-. horizontal rolls. The roughing
group contains 7 and the finishing group 8 stands.
The table lists the main data of all stands. A
horizontal working stand is shown in Fig.2 and a
Card 1/3 vertical working stand in Fig~3 (,:~ross-sact i on ) .

SN/1-22-58-11-15/18
Continuous Light Prof ile Roll-ing Mill 350
Siagle-d.rum. and. doiible-4,rum fly shears are installed
between the finishing rolling stand group and the
cooling unit. The single-dram shear mechanism shown
in Fig.4, consists of knives at the end of ro,--;kers
pivoted on the periphery of the rotating dium. The
rockers are separated by a spring but are brought
together under the action of electro-magaetically actuated
cams. TheRnives meet and cut the profile. The
transporting, cooling., straightening and storage
facilities are briefly described. Fig,q shows the round
bar calibrating schemes for diameters between 14 and
30 mm. Several faults revealed i-n servi,~e are
enumerated. The single drum shears requir-ed
strengthening of several components. The roller bed to
the cooler had to be abondoned owing to design faults.
The dropping of stock caused warping and the mill
could thereafter be used only for round bar and
similar products. Reliable sealing of the de-scaling
Card 2/3 water could not. be achie-ved in th-- working stand with

Continuous ILight Prof ile Rolling mill 350
SOV/122-5583-11-15/18
vertical rolls. Flames from the heating furnace had
to be held back by compressed air. The meean output
of the mill Jm 1957 was 53 tons per hour,,
`0
There are 5 illustrations and 1 table,
Card 3/3

B 0 vi V.
PHASE I BOOK EXPLOITATION SOV 471
. /5
Moscow. Vaesoyuznyy institut nauchnoy i tekhnicheskoy informatsii.
Prokatnyye stany. (Sbornik) 1 QMetal] Rolling Mills.[Collection] 1)
Moscow, 1959. 272 p. 2,000 copies printed.
Sponsoring Agencies: Gosudarstvennyy nauchno-tekhnicheskiy komitet
Soveta Ministrov SSSR. Akademiya nauk SSSR.
Ed.: Ye. S. Rokotyan, Doctor of Technical Sciences; Tech. Eds.: G. A.
Shevchenko and N. G. Goncharov.
PURPOSE: Thiscollection of articles is intended for technical
personnel in rolling mills, educational institutes, and design
offices.
COVERAGE: The collection contains articles dealing with the present
status of methods used in metal rolling. Attention is given to
the design and operation of sheet and planetary mills, electric
drives of equipment used in rolling shops, and instruments for
Card 1/3

(Metal) Rolling Mills (Cont.) sov/5471
measuring metal-rolling process parameters. D. P. Morozov,
Doctor of Technical Sciences, and I. S. Pobedin, Candidate of
Technical Sciences, edited some parts of the book. References
accompany each article. There are 131 references, Soviet and
non-Soviet.
TABLE OF CONTENTS:
Foreword 3
1. Rokotyan, Ye. S. [Doctor of Technical Seiences]. Modern
Sheet Mills 4
2. Bur2yanoy V. F. -e of Technical Sciences]. Plan-
[Candidat
Wary Mills 79
3. Filatov, A. S. [Candidate of Technical Sciences]. Modern
Electric Drive for the-Basic Equipment of Rolling Mills 126
Card 2/3

[Metal] Rolling Mill'B (Cont.) SOV/5471
4. Zhuravskiy, Yu. V. [Candidate of Technical Sciences]. Electric
Equipment for the Auxiliary Mechanisms of Rolling Mills 187
5. Meyerovich, I. M. (Candidate of Technical Sciences). In-
struments for Measuring the Force Parameters of Rolling
Mills 217
AVAILABLE. Library of Congrees (TS340.M-67)
Card 3/3
VK/wrc w
9.-lVil

K&SATKIN, Niko3ay I.Ivovich,-- BURIYANOV, IJ, red.; GOLYATKINA, A.Gi, red.
izd-va; KMIR4AN, M.R., tekhn. red.
[Assemblingp repairingg and greasing of metallurgical equipment]
Montazh remont i smazka metallurgicheskogo oborudovaniia. Moskva,
Gos. nauchno-tekbn. izd-vo lit-ry po chernoi i tovetnoi metallurgiip
1961. 337 PO (KM 14:7)
(Metanurgical plants-Equipment and supplies)

V.11.
DMI IL!;.;:cv YC , ~-ef'crcnt
Trcreasing the output of inflot curr, [from "Engineer," -.c.51,54,
29601. Diul. T, I-ICTI-;l no.5:5'C'-59 161.
(Great Dritain-Conveying :~.acliincxy)

BURIYANOV, Viktor Fomin.- ROKOTYAN, Yevgeniy Sergeyevich; GUREVICH,
Xz-rlbl"Ye-ffi~~v-!A; SONIKIN, M.A., red.; KISEIEVA, T.I.,
ATTOPOVICH, M.K., tekhn. red.
(Calculating the power of main drive motors for rolling mills]
Raschet moshchnosti dvigatelei glavrjylch privodov prokatnykh
stanov. Moskva., lletallurgizdat,, 1962. 360 p. (MIRA 15:6)
(Rolling'mills-Electric driving)

MAKOGON, Vladimir Gerasimavich; BUR' tor Fomigh; GOLYATKINAr
MLYA "OI-Yik n, -
A.G., red.isd-va; DOE~UZH-IFA-A-YA,-E.7.-,-I"el~rg-i*ed* -
[cOhtin-uous- hot' rol3ing miUs for 4de Wip] Nepreryvnye
shirokopolbanye stany gorinchei,prokatki. Moskva:, Metal-
lurgisdat, 1963. 216 p. (Rolling mills) (NMA 160)

C'mpounds of
Fln-' i7QV
77:7
FeQ,) on the ba,is of mn-t~irzsfrr studies, M K-

!-'y;,~;C:V. Y,
Dissertution* "Complex Corq,,oun't: c,f' r~;,--;: I-rl)~,
~;ith Ohl-7,r;,l:- of Cer'---2 71.er-nt.s.11 Gr.:,nu-l Gh~Am -ci inst of 'eneral
and Inorr..qnic Chemistr.v., Acr..(i Sci UkrEiininii S,~R,
I
-lawir,', Ehmlya, I;o,-cow, No. 16, Aug 54.)
4
60: 6UI. 393, 213 Fab 195~:~

i~
R~-F'g
N
I- ~~z

l
8 phughoru 0 iY VI(h
0
2
o
!
ta-
11
"ns e
1
1
The Systel =1
alatide alumfitunt chlotit)L (fertic chlodde)-nitrobetuene.
Zhar, O!"Ild".1
tvju,
FX1,1111NO. and Pck,~Alclt-llh\'O~
and m ~cr,vically. 71te addit.
I to it fiv-d arnt. tif AICI, or I-vCI., in KNO.- caus(A in
vach si-Stem a linear ri~c ill %p, coml. tiotil 1,04 Avas v(pral
ill moi. vwicn. to AIC4 or FvCjj. Vurthcr uddn. of PC4
mu'vil no sigilificallt changc in Sir. c"Ild. Crp ~.,Jylc Ill-
aht, indicatll tire btriliati'm of 11CLA.'ecl,
and I'C4.AICI.,. The :tpp:Lrtjit mol. %v(,, of
'0 7.5, rezvj), illilicated A
in PltNO~, M .7 and 20 '
(Ivgre of dissuen. pCj4.j.'c:Cj3 in Cill, nearly tire
tficomliml tool. Ayt.; the in PhNO.. is ImpAulalcit to
ions FcCh- or AICI, add PCIa H. %I.

MUM. YA.A.; BURIYANOV. Ya.B.
Complex compounds of phosphorus pentachloride with chlorides of
certain elements. Part 3. Study of the systemt PC15 -- HC' --
-- organic solvent. Zhur.ob.khIm. 26 no.4:1003-1009 4 '56.
Mu 9: 8)
1. Institut obehchey t neorgantcheBkoy khimii Akademii nauk
Ukrainskoy SSR.
(Phosphorus chlorides) (Acetonitrile) (Chlorides)

P- .44 (,J ~r4,
USSR/Inorganic Chemistry. Complex Compounds.
Abs Jour Ref Zhux - Khimiya, No. 8, 19577 26470.
~ anov, Ya.B.
Author P=
Inst
Title Complex Compounds of Pentachloride of
Phosphorus with Chlorides of Some Elements.
IV. System Phosphori;s Pentachloride - Tin
Chloride.
Orig Pub Zh. obshch. khimli, 1956, 26, No. 5, 1363 -
1367.
Abstract
Card 1/3
C
The system PCI SnCl)+ was studied by the
method of physic;,-chemical analysis. The
following was measured: the specific elec-
trical conductivity Kof PC15 4 SnCl)+ solu-
tions in nitrobenzene and acetonitrile at
25 and 450 as well as the viscosity 7 at 250
U k

USSR/Inorganic Chemistry. Complex Compounds. C
Abs Jour Ref Zhur - Khimiya, No. 8, 1957, 261+70.
and 1+50 and the depression of the freezing
point 4t of PC1 + SnCli+ solutions in nitro-
benzene. K of tke system PC1 - SnCl1+ -
solvent rises with the conc=ratioq of PC1
and attains the values of 4.0 x 10- mho pe~
cm in nitrobenzene solutions and 6.7 x 1o-3
mho per am in acetonitrile solutions at 250
and the moleoular ration PC15 : SnCl)+ of
about 2i further addition or PC1 increases
K litt e. There are a sharply expressed
maximum at PC : SnCl 2 and a deflection
at PC15 : SnC~ about I ~On the curve of the
dependence of te, on the composition at a
constant total molecular concentration of
PC15 -+-SnCl4- A minimum at 50 mol.% of PC15
and a maximum at 70 m01. % of PC15 were
Card 2/3

4
USSR/Inorganic Chemistry,, Complex Compounds. C
Abs Jour Ref Zhur - Khimiya, No. 8, 19579 26470.
revealed on the curve of the dependence of
I on the composition. A change in the course
of the 6t curve is also observed at PC19 :
SnCli+ - 2. The obtained results indicat the
existence of the complex compound 2PC'5,SnC3-4
(I) and, perhaps PClq.SnCli+ in the system.
The molecular weight 6f 260.2 was computed
for I by 4A at the concentration of 1.89%
by weight, which is three times less than the
theoretical; the author concludes on this
basis that I has the structure (PC11+)2(SnC'6)
and dissociates according to the scheme
2-
(PC14) 2(SnCl6) 2PC1~*- -t- SnCl,
See RZhKhim, 1957, 22632 for the part III.
Card 3/3

4~- . -' I - , . I I ~ . . . . . I . ..
-7 --,
4 ~' , 4 '. ! 9 11 ;~- - -
i : ' , , , !- 1 7

LA e-, -]A
5(1,4)
PHASE I BOOK EXPLOITATION sov/3413
Akademlya nauk Ukrainskoy SSR. Institut obshchey i neorganicheskoy
khimii I
Raboty po khimii rastvorov i kompleksnykh soyedineniy, vyp. 2
(capers on the Chemistry of Solutioiis and Complex Compounds,
Ne 2) Ki7ev, 1959. 229 p. Errata"alip inserted# 2,000
copies printed.
Resp. Ed.: Ya.A. Fialkov (Deceased) Corresponding Member,
Ukrainian SSR, Academy of Sciences; Ed. of Publishing House:
Z.S.'Pokrovskaya; Tech. Ed.: M.I. Yefimova.
PURPOSE: This book is intended for research scientists, teachers in
schools of higher education and technical schools, aspirants, and
.students of advanced chemistry courses.
COVERAGE: The c6llection contains 9 articles which review work
conducted at the Institute for General and Inorganic C4emlstry,
Ukrainian Academy of Scienceson electrolytic aqueous and
nonaqueous solutions, the chemistry of complex compounds,
Card 14

Papers on the Chemistry (Cont.)
SOV/3413
analytical chemistry, and fused electrolytes. The,collection
also contains an article entitled "Blectizoahemical Properties
of Al=um Halides In KonaqueQus Solutions", by V.A. Plotnikov
(Dece. ). Figures, tables and references accompany each
article. No personalitiei3 are mentioned.
j
TABLE OF'CONTENTS:
Flotnikov, V.A. Electrochemical Properties of Aluminum
Halides in Nonaqueous Solutions 3
Yakubson, 5.1. -Dependence of Decomposition Potentials of
Compounds of Aluminum Bromide With Metal Halides in
Nonaqueous Solutions as a Function of Concentration 72
Fialkov, Ya,A. (Deceaced), and Ya.B. Burlyanov. Phosphorous
Pentoxide As a Complex-forming Agent in-Ire-a-eni-dna With Metal
Chlorides 82
Fialkov, Ya.A. and Yu.P. Nazarenko. Study of Inorganic
Halides on the Basis of Isotope Exchange Reaetions n6
Card 2/3

Papets on the Chemistry (Cont.) SOV/3413
Sheka, Z.A., and YO.Ye. Kriss. Metal Xanthates 13 5
Sheka, I.A. Physicochemical Analysis of Solutions on
the Basis of Dielectric Properti6s 163
Babko; A...K., and T.Ye. Got 'man. Spectrophotometric Study
of Complexes of Low Stability During Complex Formation 186
,Babko,,*~,X and T N. Nazarchuk. Stiady of Metal Compounds
Dyed With anthroquinones,
.199
Markov, B.F. Electromotive Forces of Chemical Bonds With
Individual Fused Slats 216
AVAILABLE: Library of Congress
Card 3/3 TM/mAs
3-30-60

FIAIKOV, Ya.A. [deceased]; BURIYANOV, Ya.B.
Phosphorus pentacblorids as P- complex-form~ng agent in reactions
with metal chlorides. Rab.po kbim.rastv.i kompl.soed. no.2:
82-115 159. (NIRL 13:4)
(Phosphorus chloride) (Ghlorides)
(complex compounds)

BURIYANGV, Ya.B.; LAPA, V.A.
Nature of aqueous solutions of ammonia. Zhur.fiz.khim. 37 no.10:2357
o 63. (MRA 17;2)
1. Altayskiy sellskokhozyaystvennyy institut i Altaygkiy pol-itekhniches-
kly 1-nstitut imeni I.I.Polzunova.

PURIYANOVA, I.Z.,- FAVORSKAYA, I.I.A.
Origin of pjJjow lavas in the southern &ItnEPo
Iz-.AN SSSR Sor.goo-1.22-6 no.12:3-12 P 1161J. (I JIRA 14:12)
1. Institut geologli rudnykh mestorozhdaniy,. pettrografti.,
mineralogii i geokhimj.i AN SSSR, Moskvu.
(sikhote-Alin' Range--lava)

BERSENEV, I.I.; BURIYANCVA, I.Z.; YLASIYAN, Ye,D.;
Tuff lavas of the northern Sikhote-Alinl. Trudy Lab. vulk.
no.20:136-142 161. (MIRA 14:11)
1. Prilnorskup goologicheskoye upravlenip.
(Sikhote-Alin' Range--Volcanic ashp tuff, etc.)

3u
Burl ranov--., ~-f ncrThern
of thc vis'incvoy mc-untnills," Tru'ly korno-eol. in-to (i',-kcd. nL-uk Urallol-
b9-73 - Bilbl]cg: 9 itei-as
'C~: U-3851, 1c. (1,.atCn
0 jq 'ZIjUrI1,11 ljj-,~ICI~j 17 tatcy, '.o.

BURtYANTOVA, 'iv-. Z.
-A !APT85
Dis6usbes different forms of colored nepbelins:
gray, tink, dark brown, reddi6h brown with blue
gray streaks, and green., Gives reasons for varloW
Oolors,
1149T65

Perlodleal Dok. AN SSSR 98/2, 261-264, ~ep 11, 1954
.Abetract Scientific datElon the stru .cture and chemical composition of analcite
sedimentary rocks, found among concentrations of sedimentary phosphate
rocks -in the Tuvinsk autonomous region of the USSR, are presented.
Semi-quantitative spectral analysis showed that anal:ci'te contains
small amounts of Si, Al, Mg, Ca, Fe, Mn ' Ga, Ba and Na. Six USSR
references (1933-1953). Tables; drawing; illustrations.
Institution : All-Union Scientific Research Geological Institute
Presented by : Academician D. V. Nalivkin, June 5, 1954

d
6~- O'd LIP ------
FerrmAits. a new
KoTnkov. DdVady -graT.' amid A. 1.
Avii- $12-13 . -
(1) Is 1denticril with synthetic reSe.-
IU MthNb%nbk unit WI has tu - 4.79 A: ().M-- 6,
5.73 ~1: 0.02; 0.57 * 010 kX; opace groltp P~6m, or
P*n2. Synthetic VeSet has a slightly brger ccjl. I oc=s
in Middh- Derwian sediments of the Tuvu Autonontous,
Region; itfo~'=-VtrYsimPkPris=ticeMishwitbill0I
and 10111. striated p=lkl-to c. sometimes in intergrowth
twins. em&v- tq marcasite, or locltin.-ite. 71he sted-gray,
or tin-whitt cjjAnts ol about 0.1 nan. length we observed.
in the calmreous ce: ent of pDlymkt sandstonts; highly
brittk, hardness ".2, lust:r metal1k; clmvM pedect
paralkitoe. Worin reflected tight brom-antaw,rellection
powtr is bigh, bbrfringence wezk, but strongly anbotto*
with x, ish and Mae color tints between crossed nicols.
Fus. zakrcchezu. n-actions wet obtalmd for Fe mid Se,
forSomilTe. lislocaltyassood.lathesantistonewith
iat; and chaleopytite, locally it is changed by a reaction
on iw%hottopic red-brown colored raintral of very high.
r
f
a. and with a typk2l diamond lusW. Tht winerAl mn
casilyberokfustdVoith yst site.ete WV

15-57-5-6259
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 5,
p 81 (USSR)
AUTHOR: Burlyanova, Ye. Z.
TITLE: Authigenic Laumontite From the Middle Devonian
Sandstones of Tuva (Autigennyy lomontit iz srednedevon-
skikh peschanikov Tuvy)
PERIODICAL: Inform. sb. Vses. n.-i. geol. in-t. 1956, Nr 3,
pp 77-80
ABSTRACT: Laumontite has been discovereO in Middle Devonian
deposits of Tuva. With calcite, this mineral is
important as cement in the sandstones. The distri-
bution of the laumontite in the cement is spotty, The
mineral is white, rose, and brownish-red. Under the
microscope it is colorless or reddish-brown. Inclusions
of small flakes of hematite are observod in a variety of
laumontite that shows, under reflected light, a large
increase in the Intensity of reflection. The laumontite
Card 1/2 also contains numerous small liquid-filled bubbles.

Authigenic Laumontite From the Middle Devonian (Cont.
15-57-5-6259
The 2V is moderate, the interference color white, and the extinction
inclined (SpNg = 35o); Ng is 1.526 : 0.002, Np 1.513 0.002, and
Ng--Np = 0.013. Cleavage is well defined along (010); prismatic
cleavage is poorer. Tlae mineral forms a gell in HC1. An X-ray
pattern is given in the article for brick-red laumontite. The mineral
fills pore spaces between clestic grains of other minerals. It is
probable that an alumino-silica gel formed in the pore spaces in the
stage of early diagenesis. The gel absorbed Ca and Na, and sub-
sequent diagenesis led to its crystallization and to the formation
of laumontite.
Card 2/2 Ye. S. K.

15-57-2-1593
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 2,
pp 60-61 (USSR)
AUTHORS: Burtyanova, Ye. Z., Nekrasova, 0. 1., Khabakov, A. V.
TITLE: A-Petrographic and Mineralogic Description of the
Rocks in the Pre-Jurassic-Folded Basement of the
Eastern Trans-Ural Region, According to the Core of
the Tyument Exploratory Drill Hole 1-R (Petrografo-
mineralogicheskaya kharakteristika porod doyurskogo
skladchatogo fundamenta Vostochnogo Zaurallya po
kernu Tyumenskoy opornoy skvazhiny 1-k)
PERIODICAL: Materialy Vses. n.-i. geol. in-ta, 1956, Nr 8, pp 141-
'181
ABSTRACT: The general sequence of rocks.in the section of pre-
Jurassic folded basement is as follows: 1469.2 m to
1501 m (from the collar of the hole), basic volcanics;
1501 m to 1515 m, sedimentary rocks, alternations of
Card 1/6

15-57-2-1593
A Petrographic and Mineralogic Description of the Rocks (Cont.)
tuffs and mudstones; 1515 M to 1542.5 m, basic volcanics; 1542-4 M
to 1564 m, alternation of tuffs, mqdstones, and basic volcanics;
1564.8 m to 1714 M, basic volcanics; 1714 m to 1849.9 m, numerous
alternations of conglomerates, mudstones, tuffs, and other rocks;
1849.9 m to 1996 m, hypabyssal intrusions of gabbro-diabasez. The
tuffs occur between layers of flow rocks and in the upper part of
the red-bed series; tuffites are found in the red-bed series.-
Different types of sedimentary rocks are not equally abundant, tuffs
and mudstones being predominant and carbonate rocks being present
only in individual layers. Volcanic rocks are much more abundant
than sedimentary rocks and are found in the following depth inter;-.
vals: 1) diabase (labradorite) porphyrite at 1469.2 m to 1501 m;
2) olivine diabase at 1515 m to 1542 5 M; 3) the same at 1564.8 m to
1714 m; and 4) olivine gabbro-diabas; at 1849.9 m to 1996 m. The
flow rocks have the-followin mineral composition: plagioclase
(An52-68), locally andesine fin microscopic laths), highly altered;
olivine, containing approximately 15 to 20 percent Fa; monoclinic
Card 2/6

15-57-2-1593
A Petrographic and Mineralogic Description of the Rocks (Cont.)
pyroxene (pigeonite with a 2V of 400 to 500); and augite, with a
2V >500, hypersthene, basaltic hornblende, magnetite and ilmenite
(confined chiefly to the glassy groundmass), and apatite. The apa-
tite and magnetite are products of the late stages of crystallizaticn
of the magma. The hypabyssal rocks-are olivine gabbro-diabases,
consisting of plagioclase (Ay,~O, olivine with a-2V of 820
(corresponding to a content o to 34 percent Fa), pigeonite with
a 2V of 400 to 500 and cA Z = 380 to 450, and augite with a 2V of
500 to 640 and cA Z = 450-470 'titanaugite, hypersthene, magnetite,
ilmenite (in'tabular crystals~, apatite, and rutile. A table is
given to show the chemical compositions of the basic volcanics and
the olivine gabbro-diabases from the core of the Tyunen' exploratory
drill hole R-1. The paper contains a graph showing the-content of
minerals in-the heavy fractions of the sedimentary and of the vol-
canic rocks, lists the structural-textural and mineralogical charac-
teristics of the flows (in tabular form), and also furnishes
detailed optical descriptions of the plagioclases and pyroxenes of
Card 3/6

15-57-2-1593
A Petrographic and Mineralogic Description of the Rocks (Cont.)
the volcanic rocks. Descriptions are given for the individual
minerals in the sedimentary rocks of the pre-Jurassic folded base-
ment and the mineralogical characteristics of the series. The
process of authigenic mineral formation in the sedimentary rocks is
also described. The authors conclude by noting that all the sedi-
mentary rocks consist of a single complex of rock-forming clastic
minerals but that in predominance of minera--l associations three
series may be distinguished: amphibole-pyroxene, epidote, and garnet-
tourmaline-rutile-zircon. The provenance of the region during the
formation of the investigated series was the eastern slope of the
Urals. The lower part of the volcanic sequence contains thick ef-
fusives, divided into three lava flows (fissure eruptions). Later
volcanic activity was apparently of the central type. The volcanic
a~d hypabyssal rocks of the basement are similar to the traps of the
Siberian platform in mineralogy, chemical composition, and age.
Card 4/6

15-57-2-1593
A Petrographic and Mineralogic Description of the Rocks (Cont.)
Components 1 2 3 4
Si02 53-30 47.88 45.66 50-58
Ti02 0.93 1.19 0.73 1.83
A1203 15-40 17-14 16.o6 17-13
FeO 9.72 4.96 4.47 6.92
MnO 0.14 0.13 0.18 0.19
MgO 4.35 6.66 8.69 3.84
CaO 4.92 8.83 9.48 8.64
Na20 1.66 1.73 1.35 2.40
K20 0.78 0.71 0.53 1.33
P205 0.38 0.43 0.39 0.68
C02 2.45 none 0.28 0.40
Card 5/6

15-57-2-1593
A Petrographic and Mineralogic Description of the Rocks (Cont.)
Fe203 0.28 4.74 5.75 4.43
H20,+ 4.32 1.87 2.13 o.62
H20- 1.21 3.44 4.40 1.00
F 0.18 0.13 0.23 0.15
Total..' 100.02 99.89 100-33 100.11
O-Fz 0.08 0.05 0.10 0.06
Total 99-94 99-79 1 266.23 1 100-05
1) diabase porphyrite
1488 m; 2) olivine diabase
to 1534 m; 3) olivifie
to 1674 m; 4) olivine
to 1907 m.
Card 6/6
of unit VI, at depth interval of 1482 m to
of unit V, at depth interval of 1526 m
diabase of unit I, at depth interval of 1667 m
gabbro-diabase, at depth interval of 1906 m
S. P. B.

rlcroul~,h .-;, o.- Tr! ;. -
I I - I I -

KTAvy. %md I. Komkov A-h- Ich
Leningrad). - -r,.PlJki ;11,%,Y.-% Af,.f,al Oblx-
estw, 96, W2&-8(J957't---A natai"i mio~-rmi -3
_-no~-j with t~r.-Ilte J,'--,~

BURIYANOVA, Te.Z.
Mineralogy and geochemistry of cadmium in sedimentary rocks of Tuva.
Geokhimiia no.2:177-182 16o. (MIRA 13:6)
1. All-Union Scientific Research Institute of Geology. Leningrad.
(Tuva Autonomous Province--Rocks, Sedimentary)
(Cadmium)

BURIYAROVAJ, Ye. Z.
Analcime and sedimentary rocks containing zerlite in Ttrva.
Izv. AN SSSR. Ser. geol. 24 no.6:71-84 Jr 160. (KERA 14-.4)
1.--VAesoyuznyy nauchno-issledovatellskiy geologicheskiy institut,
(VSEGEI) Ministerstva geologii i okhrany nedr SSSR, La-ningrad.
(Tuva Autonomous Province-Analcite
(Tuva Autonomous Province-Zeolites)

S/00~/61/000/007/004/004
B103 B217
AUTHOR: Burlyanova, Ye. Z.
TITLE: Selenium content in sedimentary rocks of Tuva
PERIODICAL: Geokhimiya, no- 7, 1961, 623-629
TEXT: Selenium was proved in sedimentary rocks of Tuva by x-ray spectral
analysis in 1952. In 1953, Ye. I. Nefedov detected chalcomenite as
individual occurrence in Tuva. Only since 1955 it has been tried to
clarify the rules governing the selenium distribution in the mentioned
rocks. The author conducted tens of thousands of selenium determinations
by means of microchemical reaction, and developed methodical details of
selenometry which permit a simple semiquantitative determination of the
selenium content in the field as well as in sedimentary and other rocks
(Ref. 2: Ye. Z. Burlyanova, Mineralogicheskiy metod poiskov selena
(,N.Iineralogical method of selenium detection). Ekspressinformatsiya ONTI,
VIMS, 1957). She determines the selenium content in sedimentary rocks
from Middle Devonian (D2) up to recent rocks, and establishes a special
geochemical selenium province in Tuva. (A) The selenium distribution in
Card 1/ 6

S/007/61/000/007/004/004
Selenium content in sedimentary ... B103/B217
the terrigenic sediments of D2 is extremely irregular and cannot be
visually discerned in the rocks. Polymictic pink and pink-gray sandstones
with laumontite-calcite cement and green and brown siltstone fragments
contain selenium. According to their frequency, the selenium minerals
form the following series: (1) Ferroselite (most frequent), (2) claus-
thali~e and (3) cadmium selite (next in frequency), (4) stilleite (much
rarer and scarce), (5) selenium containing pyrite, (6) sphalerite,
(',) chalcopyrite, and (8) galenite. (5) - (8) are associated with all
other mentioned minerals. (B) The Upper Devonian sediments represented by
sandstones and conglomerates contain only very little selenium. only
individual samples contained up to 0.00410 selenium, Ferroselite was found
as scarce dissemination. (C) Also in Lower Carboniferous the Se content
is very low. Only individual layers of phosphate-tuff sandstones con-
tained several thousandths of percents. (D) Se traces up to 0.0005% were
found in Middle Jurassic in the sandstone of the Saldamskaya series.
(E) Recent sediments. The sediments of the Khadyn lake contained 0-0005~4
selenium. n-10-4% selenium was found in the soil around the town of Kyzyl.
Although polymetal and pyrite ores in Tuva contain sometimes up to 0.025%
Card 2/6

S/007/61/000/007/004/004
Selenium content in sedimentary B103/B217
selenium, no proper selenium mineralization could be established in them.
The author also characterizes selenium mineralization in the sediments of
Tuva.- Native selenium was found as (a) black, amorphous, and (b) red
crystalline variety. (a) forms fine crusts and earthy aggregates which
sometimes cover the grains of clastic material. Furthermore, thin coating's
were found on barite. Ferroselite was described by the author (with
A. I. Komkov, Ref. 1: Dokl. AN SSSR 105, 110.4, 1955), belongs to the
structural type of marcasite, and its x-ray structure is similar to that
of rammelsbergite (Ref. 12: G. Kullerud and G. Donney, Geochim et
Cosmochim. Acta 15, No. 1-2,1958). Ferroselite is Cisseminated as single
crystal in the cement of sandstone and often bound to the mentioned
siltstone fragments. As a rule, its crystals have no immediate contacts
to the selenides and sulfides occurring here. On the periphery, the
crystals are replaced by a red mineral which is assumed to belong to
native selenium. Clausthalite is also found in cement and its appearance
differs hardly from that of galena. A. I. Komkov studied the samples by
x-ray diffraction. The following parameter values were detected:
a0 : (6.11+0.01) kX; (6.110t0-003) U, and (6.12510.002) kX. Selenium is
partly replaced by sulfur. The lead selenides occupy an intermediate
Card 3/6

S/007/61/000/007/004/004
Selenium content in sedimentary B103/B217
position in the isomorphous series PbS- PbSe. Their formula can be
represented as Pb(Se 0.85, S0.15 ) and Pb (Se 0.93's 0.07 ). Cadmium selite
was characterized by the author (Ref. 4: Geokhimiya,No.2,1960). Its
4~
-Lormula corresponds to (Cd 0.091zno.,)(Seo. 64'So.16)' It belongs to the
wurtzite type. Compounds of an intermediary composition, in which the
lattice constant a gradually increases, exist between sphalerite and
stilleite. Their approximative formulas are: Zn (S 0.83' Se 0.17 ),
Zn (Se O-W S0.17 ), respectively. Blockite (penroseite) could not be
determined finally. It does not contain sulfur and belongs to the pyrite
type. a = (6~00�0.02) kX, Its formula corresponds to ASeV where A = Cu,
N-4, Co. The selenium-containing minerals of Tuva have a low sulfur content,
the weight ratio S : Se is, therefore,.low. It amounts to 0.24 UP to
1200, S : Se = 135, on an average. The selenium-containing sediments of
Tuva occupy a special position with respect to their ratio S : Se. The
author confirmed the opinion of V. M. Goldschmidt et al., according to
which iron bisulfide deposits are mostly poor in seleniumt The main mass
Card 4/6

S/007/61/0001/007/004/004
Selenium content in sedimentary ... B103/B217
of selenium is therefore not concentrated in pyrite. In Tuva, selenium
is only seldom accompanied by tellurium traces (up to 0.001%). The
author establishes that the formation of selenium-bearing horizons is
bound to take place under reducing conditions. The introduction of
selenium into the sediment took place under conditions of alkaline
reducing facies. Selenium mineralization is authigenic since it is bound
to the cement of sediments. Its formation is apparently bound to the
diagenesis of sediments. The formation of H 2S and H2Se was possible under
strongly reducing conditions of sedimetogenesis in bedded ground sediments,
thus forming selenides and sulfides of Fe, Pb, Cd, Zn and others. Conse-
quently, the selenium accumulation took place during the stage of sedi-
mentogenesis, whereas its mineral form developed during the diagenesis
stage. Sparse and fine dissemination of selenides indicates their sedi-
mentation from pore solutions. An old syngenetic or somewhat earlier
terrestrial volcanic activity is assumed to be the original selenium
source in the oldest sediments. It is also possible that individual
local selenium concentrations were formed by erosion of polymetal and
pyrite ore bodies which were on the continent denuded during D2* The
Card 5/6

S/007/61/000/007/004/004
Selenium content in sedimentary ... B103/B217
selenium-interspersed elastic material was accumulated afterwards. The
author mentions a paper by R. Gertsenberg, and the analysts A. F. Gri-
gorchuk and M. A. Andrianova. There are 3 figures and 13 references:
Soviet-bloc and 4 non-Soviet-bloc. The three references to English-
language publications read as follows: R. G. Coleman (Ref. 10: Amer.
Mineralogist 44, Nos.1-2, 1959); R. G. Coleman, M. Delevaux (Ref. 11:
Econ. Geol. 52, No. 5, 1957). Ref. 12 is given in the body of the ab-
stract.
ASSOCIATION: Vsesoyuznyy nauchno-issledovatellskiy geologicheskiy
institut, Leningrad (All-Union Geological Scientific
Research Institute, Leningrad)
Card 6/6

EGEW, L.Ye.; BURIYANOVA, ___
Prospecting methods, studying# and appraising of exogenous
deposits. Geol.mest.red.elem. no.11:88-101 162,, (MIRA 15:5)
(Selenium)

EGELIJ, L.Ye,,- BURIYANOVA, Ye,Z,,
Laboratory research methods. Geol.mest.red.elem. no.11:101-115
162. (14DU 15:5)
(Selenium-Analysis)

BURTYANOVA, Yr,.Z.; KASHENOVA, A.G.
Selenium content of*sedimentary rocks of the Lower Carboniferous
of the southern and northern Idnusinsk Depressions. Geol.i geofiz.
no -5:14-20 162. (MIRA 15:8)
1. Vsesoyuznyy nauchno-issledovatellskiy geologicheskiy institut,
Lenin,grad.
(Minusinsk Basin-Selenium)

S11691631000100110361062
D263/D307
AUTHORS; Egell, L.Ye. and Burlyanova, Ye.Z.
TITLE: Methods of prospecting, study, and estimation of
exogenic deposits of selenium
PERIODICAL: Referativnyy zhurnal, Geofizika, no. 1, 1963y 7p
abstract JD42 (In collection: Geol. mestorozhd.
redk. elementov. no. 11, M., Gosgeoltekhizdat, 1962g_~:t.-'
88-101)
TEXT: It is convenient to organize special prospecting of
exogenic deposits in conjunction with geological surveying on a
scale of 1:501000 or greater, and also during the search for other
useful mineral deposits, particularly those of uranium. In sedi-
mentary deposits selenium occurs predominantly in sand-schistose
layers, less frequently in limestones and phosphorites. The rocks
are studied by investipting sections transverse to the strike of
.-the strata. During this operation all lithological and stratigraph-
ical varieties of rocks are carefully inspected, taking samples 'by..
Card 1/3

Hethods of prospecting,
S/1.69/63/000/001./036/062-
D263/D307
.grooving, and in extreme cases, by picking up lumps of ore. The
shallow-water deposits of seas, lagoons, lakes an4 ancient rivers
are more promising. Bituminized limestones and carboniferous sandyl-
schist should be particularly carefully examined. The most promis-i
ing appear to be the sandy schists accumulating near active volcanic
regions. Since selenium is characteristically associated with uranli i
ium, vanadium, and molybdenum, the appearance of such minerals indi4
cates in most cases the presence of selenium in the given rocks.
Pyritic deposits contain as a rule sharply concentrated quantities
of selenium. It is particularly important to test iron caps for Sei.
In its usual sense metallometric sampling is not suitable for selen4:',,,.
ium, since the latter is not detectable by spectroscopic methods.
The prospecting is carried out with the aid of a special method,
selenometry, which comprises a series of operations including spec- I
ial sampling and estimation of selenium by dry microchemical tests..
Selenometry may be either qualitative or semi-quantitative. In
qualitative selenometry the element is detected by the usual method,
of sublimation in-a closed tube. The presence of 0.001% of Se may
be confirmed in this way. If selenium in the ore is not accompanied~~_'*.

Methods of prospecting,
S11691631000100110361062
D263/D307
a
by sulphide ulphur, or by arsenic, then the above method may give
a qualitative estimate of the Se content. Selenium-containing sam-1
plea are then subjected to chemical and mineralogical analysis to
establish the mineral composition and the selenium content. One of;
the promising methods of prospecting for selenium and uranium depo-;,
sits is the geobotanical method. The success of prospecting depends
on the depth of stratification and on the form in which the seleni
occurs. Although a large group of selenium-absorbing plants is
knoNm, their values as indicators is not uniform. Milk vetch is
generally accepted as an indicator. According to D.G. Kennon, prosi
pecting by plant-indicators is particularly effective if the concen
tration of selenium in the ground is about 0.0176, (U not below
0.0176) and if the depth of the ore deposit does not exceed 12 m.'
Of the geophysical methods, T -surveying and radiometry may be
used in prospecting for seleniferous deposits. The hydrochemical
method does not always yield positive results since the possibility
of confirming the presence of Se deposits in this way depends on
the Eh and pH of these weak rock solutions.
Z-Abatracter's note: Complete translation,2
rd

BURIYANOVA, Yelena Zakharoyna; FEDOROVA, L.N., red. izd-va; IVANOVA,
A.G., tekhn. red.
(Guide to uranium and thorium minerals) Opredelitell mine-
ralov urana i toriia. Moskva, Goageoltekhizd4t, 1963. 55 p.
(MIRA 16:8)
(Uranium) (Thorium) (Mineralogy, Determinative)

BURIYANOVA, Ye.'-7.; BAI,~ANOVA, Ye.N.- C. ~
-
. f,- 0 .
Authdr,enic hydrous rahiertd of titanium. uvanitiati) aild c"1101i'mt
close to brannerlte. Trudy VSEGM 96; U7"130 163.
(MIRA 17:9)

BUR'YATIOVA, Ye.Z.; KASHENOVA, A.G.
Using seTniquantitative selenium measurement. Razved. 1 okh.
nedr. 30 no.3:55-58 IL- 164 loo-I-)
1. Vsesoyuzn7y nauchno-issledovatellskiy geolcgichoski-,T insti-
tut,

o
BURIYANO',,"A -'~z,.-Z !.A_~q-TROKOVA, G.S.; SHITOV, V.A.
"'lanuramilit," a new mineral. Zap. Vses. min. ob-va 91,
no,.4.-437-443 165. (MIRA is 19)

BMANSKA, M.; SIROKY, J-
Statistical evaluation of the effoet of an active rest following farm work. 1~911
NMW ZAHRKNICNI LTTFMTURK. PRIRODNI VEDY, MATMATIKA. IQMff. (StatreL
knihovna CSR. Universitni kn:Lhovna v Praze)
Praha, Czechoslovakia
No. 4, 1958
Monthly list of East European Accessions (EZAI) W. VOL. 9'#- no. 1 January 1960
UndY.

- g4gAMHO- , --.'~-J.Gerasimov, I.P.); ZVONKOV, V.V.; BURIANOVSKI, M.S.
:~F
[Buryanovskiy. M. .]
Problem of the Danube River, and main problems of reclaiming
its delta and bank on the territory of the U.S.S.R. Analele
geol geogr 16 no.2sl27-133 Ap-Je '62.

lo BURYASHINA. V, - KHILKOP M.
2. USSR (600)
4. Bakiiig
7.~ Perfection of work methods and improvement of technical processes. Khol. Tekh. 29
no. 3, 1952
9. Monthly List of Russian Accessions, Library of Congress, January 1953. Unclassified.

KALLISTOVI P.L.; ZOKOV, D.A.; PROKOFIYEV, A.P.. Prinixali uchastiye:
BOGDANOV, F.M.; BORZUJi'OV, V.1-j.; BURYBLINI AY,)- DROZDOV) M.D.1
YEROFMV~ B.N.;KOMISSLROV, A.K.; KOGAN, I.D.; LYUB114OV, I.A.j
MI~1711 R.Ye.; ROKHLIN, M.I.j SERGEYEV, P.V.; SW-ENOV) A.D.j
FROLOV, V.V.; NWANOVA, G.F.., red. izd--va;- GERDIMKOJY&.B.~
tekhn. red.
(Instructions for appkving the classification of reserves to
primary gold deposits] Instruktsiia po primeneniiu klassifi-
kateii zapasov k korerj*rm mostorozhdeniiam zolota. Moskva,
Goa. nauchno-teklm.izd-vo lit-ry po geol. i okhrane nedr, 1955.
46 p. (14M 15:2)
1. Russia (1923- U.S.S.R.) Gosudarstvennaya komissiya po zapa-
Bam poleznylrb isko yenqkh.
rGuold ore s-Clagsif ication)

__~URYBLIN, AN.
Third Congreos of the Sc-1crtific and Tech,nlcal
Razved. i ok-h. nedr 30 no.4.59-6-1 A
p
MIR,~ 17 1-2)
1. TSentrallnyy komitet professional 'norp soytizii rabl),.-lilkh
geologorazvedochn.vlcli rabct.

\, \ , 1 ~,, -
BURYGIN, I.V., inzh.
-a.inking with use of local rock freezivg. Shakt. stroi, no.1:23-
25 '58. (MM 11t2)
(Shaft sinking) (Frozen ground)

RI,TRY.`,TN. V.A
w
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BurY,-in, V.A. "On some wajs of adapting plants to soil saltif ica Lion", Izvertiya Akad. nauk
UZSSR, 19: 3, No. 3, P. 3-16, (~tesume in U111:iCk) , - Hbliov: ab itens.
4 0
SO: U-3042, 11 March 53, (Letopis InykJi Statey, 14o. 9, 1949)

buRYGDv 2 7. A.
to 0
21874 _.tUHYGI~4,_�~_A. 0 ,oryshenii ooloustoychivo-Ai
vospitartaya. Doldat, -Amd. naul-, Uz SSR, 1949, "c!. 5, s. -
itt,-zyume na uzbek.
'jo: u
- Le~opis- Zhurn-al IrVich 3tatey, lo. 29; -roshra3 191~9

BURYG IN, V.A.
Certain ecologiaRl characteristics of the wormwood Artemisin terrRe
albae nnd the saltwort Snlsola rigida In connection with their cultiva-
tion. Trudy Inst.bot.AN Uz.SSR. n0-3:103-110 155. (KM Ida)
(Ust-Urt--Botany--&-ology) (Artemisin) (SRItwort)

ZLMOV, K.Z.; BURYGIN, V.A. -
Plant relicts of the Nura-Tau Range. Bot.zhur. 41 no.9:1331-1334
S 156. (MLRA 9: 11)
1. Institut botaniki Akademii nauk Uzbekskoy SSR, Tashkent.
(Nura-Tau-Botany)

MMYGIN, V.A.
Witter vegetation in the southern Xyzyl Kum. Izv.Aff Uz.SSR.
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(K= XUM--BOTANY)