SCIENTIFIC ABSTRACT BETSKIY, O. V. - BEUS, A. A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000205120017-3
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 8, 2000
• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

L 21846-66 EWA(h)/LW(I)
ACC NRt AP6010718 SOURCE CODE: UR/0142/66/009/1
AU111OR:- Lebedev, 1. V.; Betskiy, 0. Vs
311
ORG: none
TITLE: Increasing the gain of H-type microwave amplifiers
SOURCE: IVUZ. Radiotekhnika, v. 9, no. 1, 1966, 8-14
TOPIC TAGS: amplifier design, magnetron, platinotron
ABSTRACT: The author reviews the factors which determine the
efficiency of M-type
crossed-field microwave amplifiers, in particular the magnetron
configuration.
Efforts to increase gain are concentrated on lowering the minimum
input power required
to form cycloidal electron trajectories in the interelectrode
space. To increase
efficiency without sacrificing gain, special electrode
configurations must be resorted
to, two examples of which are shown schematically in Fig. 1. The
second.scheme, which
Card 1/2 UDC: 621.385633.24

L 21846-66
ilCycloidal Path
Fig. 1. M-amplifier variants
uses an impedance section on the cathode as well as on the anode,
is pyeferable for
its simpler design and also because it provides good suppression
of parasitic feedbac'
Though improved designs of the type suggested may not approach
the amplification
attainable by 0-type amplifiers, it should be possible to get
M-types up to a gain of
40-50 db. Orig. art. has: 4 figures and 8 formulas. [SH]
SUB CODE: 09, 17/ SUBM DATE: l3May65/ ORIG REF: 002/ OTH REF:
010/ ATD PRESE:
LI 2-1 '1
Card 2/2 not

L 3619746 EVIT(l)
ACC NR: AP601145Z SOURCE CODE: UR/Oiog/66/011/004/0709/0720
AUTHOR: Betskiy, 0. V.; Guttsayt, E. M.
ORG: none
TITLE: Balanced regenerative SHF amplifier
SOURCE: Radiotekhnika i elektronika, v. 11, no. 4, 1966, 709-720
TOPIC TAGS: SHF amplifier, regenerative amplifier, magnetron
amplifier,
waveguide filter
ABSTRACT: A slot -wave guide -b ridge balanced circuit
containing two regenerative
magnetron amplifiers is considered; the bridge separates input
and output signals.
Fundamental design formulas for matched- and unmatched -load
conditions are
developed. The effect of nonidentical amplifier characteristics
is explored, as is
the effect of slot-bridge imperfections (perfect directivity
but unequal power
r-A-rd 1/2 UDC: 621.385.66+621.385.64

L 36197-66
ACC NR: AP6011452
division, limited directivity). The effect of load mismatch on
the balanced -circuit
gain is investigated. Experimental amplitude, frequency, and
load characteristics
of a two pulsed -magnetron circuit measured at a 3-cm wavelength
are presented.
It is claimed that the balanced circuit, although having a 6-db
lower gaia, is
simpler and more reliable than the ferrite -circulator circuit.
The formulas
developed in the article are applicable to any balanced
regenerative amplifier.
The introduction of a phase shifter into one of the bridge arms
is recommended for
phase equalization of both amplifiers. "The authors wish to
thank I. V. Lebedev.
for initiating the work, and also NMI graduate students I.
Vaynberg and
S. Pervakov for their part in the investigations. " Orig. art.
has: 7 figures and
22 formulas.
SUB CODE: 09 SUBM DATE: 29Dec64 ORIG REF: 007 OTH REF: 002
Card Z/?.,.W

R3TS&BN, Tall.. redaktor; VODZINSKIT, V.V..
tekbnichaskiy reclaktor
[Time norms (standard) for repairing industrial
equipment. in the
oil Industry) Horsy vremeni (tipovye) na remont
tekhnologichaskogo
oborudovaniis w9lozhirovoi prozymblennosti,
Utworzhdeny prikazom
no.43 Glavraozhirmaslo ot 23 fevralia 1951 g. Moskva,
Poshche-
promizdat, 1952. 515 P. (MLRA 10:3)
1. laningrad. Vassoyusnyy aauchno-iseledovatellskiy
institut
shirov.
(Oil Inclustrise-Bluipment and supplies)

BETSOFEN, Ya.I., red.; KISINA, Ye.I., tekhn.red.
[Sabject plan for publications of the state
scientific and
technical publishing house "Pishchapromizdat' for
19591
Tematicheskii plan vypuska izdanii gosudarBtvennogo
nauchno-
tekhnichaskogo 12datel'stva OPishchepromizdat" na
1959 g.
Mosk-va, Pishchapromizdat, 1958. 16 p. (MIRA 12:8)
1. Russia (1923- U.S.S.R.) Vsesoyuznoye ob"yedineniya
knizhnoy
torgovli.
(Bibliotgraphy-Food industry)

BEETSRUM, S.
"on an Island of Peat," (Na Ostrove Bolchogo Uglya), by 11.
Sviridov, G. Va-ti-levoy
and S. Betsrum, Tekh. Molod., No. 12, 1953-
Abs. D21o896, 29/4/55

S/137/61/000/010/008/0%
A006/A101
A:"THORSt Bett, F., Khikmen, B. S., Uillis, G. M., Uormer, G. K.
TT=t Some-studies on obtaining-titanium by electrolysis of
molten salts
PF-910DICAL: Referativnyy zhurnal,.Metallurgiya, no. 10, 1961,
16, abstract
10G122 (V sb. "Izvlecheniye I ochistka redk. metallov", Moscow,
Atomizdat,, 196op- 466 -..482. Discussion, 482 - 489)
T-EXT This is a review of methods for obtaining Ti metal. The
most promis-
ing method is the production of high-purity Ti by electrolysis
of Ti chlorides,
dissolved in molten salts. TiC'3.oan be obtained by TiCl4
reduction by two moth-
&:iB. 1)~Out*ide the electrolytic bath. It is suggested to boil
TiC14 In a spe-
Plal apparatus in the presence of.H2,.where the rate of
obtaining TiCl 3 is propor-
tional to t e energy cmtsumed 2) In the electroly~*;, From all
the. known moth-
k th
ods of-reduoing TiC14 in the electrolyte, the most~expedient is
that of reduotdon
or, the cathode by electrolyti~qally deposited metal.
The.design of..a pyrext-glass
elsotrolyzer is described whilch can be used for small-scale
experiments) a large-
0-1se graphite electrolyzer is also desaribed. A
eutectia.mixture of,Li and K
c"onides., containing 60 mol. % LiCl; with 3500C melting pointj
is used as an elec-
-Card 1/2

S/137/61/000/010/008/056
Some'studive ion obtaining... A006/A101
tralyte., '7or large-scale electrolysis a eutectic mixture-of
Na'chlorides-(50
t'hol:. %)'and' Mg is most'suitable. A sstisfaotory 'deposit in
the form of coarse-,
un-tightly adhering dendrites, can be obtained-at medium
curront densities (50
100 amo/din2), high concentrations of TiCl and temperatures of
about 7500C. One
of -the basi3 pz~oblems is the -prodactibn o? &-dense cathode
deposit which'dan be
eas.-Ily-washe&off the electrolyte without noticeable
oxidation. `
L. Voroblyeva
LAbstracter's note: Complete translation]
Card 2/2

KLDO.'HEK, R. [Klimecek, R.); BETTE-L'GMO Ya.
[Bettelheim, J.),
Innovation in absorption technique; a colu= with
spiral
wire packing. Zhur. prikl. khim. 36 no.11:2432-2437
N 163.
(MIRA 17:1)
1. Nauchno-iseledovateliskiy institut
neorganicheskoy khimii,
Usti nad Labem.

3CLUI, Bohuslav, akademil.,, laureat statni. ceny;
YvITC, VI., inz.;
SVaWOVA, S., MlDr.; TUSL, M., I-Mr., C.Sc.; rLUA, Jan.;
MTEBILA, Jan, inz.; KLMECER, Rostiolav;
BIETITIHEIII-11 Jan, inz.;
HALA, Eduard, doc., inz... dr.; MR, L., inz.; KOMIK,
L.;
EMUS, Emorich, doc., inz., dr.; VWOIS013L, Jan., doc.,
inz., dr.;
NADENIK, 0., inz.; HRUDKA, 'J.; HOSTALEK, Zdenek,
iliz., dr.;
RADL, K. inz.; PEKABEK, U., Mr.; BLISTAN, J., inz.;
STO~LH. 0.
inz.
A national conference on protection against chwidcal
fumes
fron, electric )w at plants; a sumEa-j of reports.
Energetika Cz
11 no.2:109-111 F 161.

BETTELHEIM, J.
Basic relations for the calculation of spray
absorbers.
Chem prum 14 no.1:17-19 Ja'64-
1. Vyzkunny.untay anorganicke chemie, Usti naxi
Labem.

SKRIVAINEK9 J.; BZfTELHEJM, T.
Appro,'cimate solution or sh~,rL.,*.Una d'A'Nslon
In a Bphi--r.: a!
body. Ghem pruln 14 no.?.351-353 Ji 164.
1. Fesear,!h Institute of lnorgani~- Chemistry,
L13t-', nad labt~r-.

AUTHORS: Ergen, N.K., Briant, R.C., Weinberg, A.M., JCYT/
89-4-6-22/30
Bettis, B.S.
TITIZ: A Fluorine-Containing Fuel for High-Tempc)rature
Reactors
(Ftoristoye goryucheye dlys. vysokotemperaturzvkh
reaktorov)
FMODICAL: Atomooya energiyat 1958, Vol 4, Nr 6, pp 597-601
(USSR)
ABSTRACT: This ia a detailed review of 6 papers published
in Nual.Engng,
1957, Vol 2, pp 16, 298; Engineering, 1957, Vol 181+,
Nr 4783, P'- 604- Nuol. Soi. Enpg, 1957, Vol 2, pp 6, 826,
797, 804, 80. ~Reviewer- V.A.). There are 3 figures, 2
tables
and 6 references.
1. Reactors--Heat transfer 2. Fuels--Applications 3.
Fluorine
Card 1/1

BETTKHER, K, [Bottcher, X.]
Lecithin -vi tellin reaction in the species of
nonsporeforming
bacteria. Rikrobiologiia 32 no.3:!,19-424 ltr~-Je163
(MIM', 17:3)
1. Institut pochvovedeniya i pitaniya rasteniy,
Berlin, Ger-
manskaya Demol-raticheskaya ResIxiblika.

BETTLACH, Fr., MUDr.
Physician's tasks In physical education. Prakt.
lek.. Praha
35 no.14:329 20 July 55.
1. Vedouct lekar telovych, lek, poraduy pri OUNE
Usti nad
Orlici.
(PHYSICAL EDUCATION AND TRAINING
in Czech.. role of physician)
(PHYSICIANS
in Czech.. role in physical educ.)

The lubility of ~qbalt. f erroqapide in water
determined
y 3 so
b
pacific-conductivity mensuremen a of a onturAted
solu-
ti.. at W. Antogi Bcqio~kl, ~Vp ighj5zymaj~ski,
and
Teresa Betto ANW.-Torl ic- 33,
suiizniiair-y')*.-~~-My. of CojI?e(CN)j,
detd. by sp.-cuid. irmasurenwaits of the satd.
-oln. at 25', Is
2.F5 X 10-0 mcdes/l. A. KrevIeAWiil.I:.:

KIN, Zygmunt, dr. ins.; WORONIK, Genowefa, ins.;
BETTO, Teresa, mgr.
Application of carboxymetbyleallulose in the
production of
printing paper. Przegl papier 18 no.71215-218 JI
162.
1. Wloclawskie Zaklady Colulosowo-Papierniese,
Wloclawek.

ar" I-etts 1. "The -,lasticizt3'ion of hutadiene-
st-,,repe rUbber, tt In the s-.mposiuji:
T7,.-.,es+.J-r:ation in thr-, fiEdd
Of COI-inle.X-ITIOICCUlar compowids, Eoscow-Leningrad,
191,99 p.
-Tibliocr: 7 items
U-5`41, 17 December 1953, (Letovis Izhurnal Inyl-Ji
Etatey `.o. 26 IL,,1.9).

lasHOnflap o1 but&d'ene-.61yrene rubters.
lid 1L X.
Ffilichills i
PRIILr Aj)pi',LLN ',,-) VMIN.Al-,
ivs hr eaf-r ',-v thr rnmc, auZh!4-., 111`13-
A~ntej to flic t3ij? oil
Cc ----T- -
~etl c I jnurniu,
ri --min pn1in iis
P~~Pj. 19,50. 2D, 4S5-01.

BINT71 G. E.
"Yodification of structure and 'Properties of Divinylstyrol
Rubber in the Process
of its Plasticization." Sub 7 Ilay 51, Moscow Inst of Find
Chemical Technolof,7 imeni 14.
V. Lomonosov.
Dissertations presented for science and enraneering, degrees in
'Moscow during 1-51.
SO: Sum. No. 480, 9 May 55.

ANIYAHOVA, K.F.; W" a_la- ZHAKOVA, V.G.; KOXSXATA,
S.F.; KAMIN, B.K.;
PRISS, L.S.; HNZNIKOVSKIT, M.N.; COMKINA. L.A.; SHTM,
Te.B.
Structural and characteristic similarity of Soviet SO
polyusoprene
rubber and natural rubber. lauch.i rez.no.1:4-14 Ja
'57. (KM 10:2)
(Rubber--S~rnthetic)
.1 ~

31978
S/081/61/000/023/053/061
0 B106/B101
AUTHORS: B!tts~ G._ F,-, Gubenko, I. B., Karmin, B. K.,
Lukashevich, I. R,
Markova, L. M., Segalevich, A. Ye., Troitskaya, N. I.,
Chernozhukov, N. I., Guseva, V. I.
TITLE: Test of petroleum products as plasticizer fillers for
rubber
compounds from divinyl styrene rubber. Communication I
PERIODICAL: Referativnyy zhurnal. Khimiya, no. 23, 1961, 560,
abstract
23F346. (Tr. N.-i. in-ta shin. prom-sti, sb- 5, 1960, 5-20)
TEXT: For the purpose of examining the possibility of
enlarging the raw
material basis for the production of olefin rubber, a study
has been made
of the effect of paraffin-naphthene hydrocarbons (I) and
aromatics (II), vt/
isolated from different kinds of petroleum at different stages
of
processing, on the physicomechanical properties of standard
rubbers from
EVC-30A (SKS-30A). Addition of I and II in an amount of 35% to
a mixture
of rubber and softener deteriorates the physicomechanical
properties of
vulcanizates and enhances their elasticity. The tensile
strength of rubber
containing I drops from 274 (standard rubber) to 173 - 226
kgf/cm2 while
Card 1/2

31978
S/081/61/000/023/053/061
Test of petroleum products ... B106/B101
its tear resistance drops from 81 to 47 - 54 k~f/ m. The
tensile strength
of rubber containing II drops to 200 - 245 kgf cm and its tear
resistance
to 52 - 64 kgf/cm. The thermal stability and the bonding
strength of
doubled rubbers decrease substantially after vulcanization.
High-molecular
products of comparatively higher viscosity deteriorate the
strength
properties of rubber less than do low-molecular ones. A test
of 29 products,
obtained from differently processed petroleum asphalts,
deasphalted products,
distillates, and raffinates, have shown that the most
interesting of these
products are a deasphalted petroleum asphalt, the residual
high-viscosity
oil, a secondary raffinate, and an aviation tar. These
products ensure
satisfactory phygicomechanical DrODerties, elasticity, and
brittleness
temperature (-50 C) of vulcanizateg. I Abstracter's note:
Complete trans-
lation.
Card 2/2

1S/081/61/000/023/052/061
B106/B101
AUTHORS: Betts, G. E. Zhakova, V. G., Karmin, B. K.,
Strellnikova, 1".
P., Eytingon, 1. 1.
TITLE: Chemical mastication accelerators for natural and
synthetic
rubber and proSDOCtS Of their aDDlication
PERIODICAL: Referativnyy zhurnal. Khimiya, ro. 23, 1961, 559,
abstract
23'P544- (Tr. N.-i. in-ta shin. prom-sti, sb. 5. 1960, 27-55)
T E, XT :Numerous compounds have been examined, many of which
are vulcanizatkn
(1) was found to be the moat aci,,ve
accelerators, Dimethyl phenyl p-cresol I
chemical mastication accelerator for CtAC-30 (SKS-30) rubber.
In the
presence of 1.2 parts by weight of 1, mastication can be
carried out in
kettles within 30 to 50 min at 130 0C as agairst 70 min at 135
0C without 1.
A similar accelerating action is exerted by I on the
mastication of LL&H
(SY,N) and [t,0(SKI) rubber, but not on that of Hk (NX)
rubber. Active
mastication accelerators for NK rubber are Renacit II, IV, and
V
thiophPnol, zinc salt of pentachlorothiophenol, or
pentachlorothiophenol,
respectively),Vulkamel TBN (30% thio-o-naphthol and 67,~o
inert paraffin),
Card 1/2

S/081/061/000/023/0c52/06I
Chemical mastication accelerators... B106/13101
Peptone 65 (zinc salt of o-benzamidothiophenol), the zinc salt
of trichloro-
thiophenol, Peptone 22 (o,ol-dibenzamidodiphenyl disulfide),
and a-nitr--C-
naphthol. ".Then selecting mastication accelerators, it should
be hr)"!;v
in mind that Lhey are able to affect the scorrhinC of
compouridF~
--o the vulc~tnization and physicomechanical propertieF~ of
i'l.ifferent ways, depend2nj- on the type of riibber, filler.,
and other
ingredients. Of great importance are the cooling conditic)n~:%
of !!i,-:
masticated rubber. Scorching is frequently increased by waTer
permit mastication in closed rubber mixer,3 and i)renarit.:-i
()f' vomocoinds at the same time. Accelerators that arp
activ-~- ai. r~,? y
low temperatures, such as Renacit IV and Peptone 6c, are
rpquirj~-U' ~or t Inis
P u r p o -~,. e .[Abotracter's noip~ Comnlete tz-anF~ kit Ion
Card 2/2

S/136/60/000/005/007/012
A051 A029
AUTHORS: Be 41
tts, G.E,, Karmin, B.K , Eytingon, I.I., 'hakova, V.G.,
Strellnikova, N.P.
TITLEc The Mastiicalion~of Natural Rubbe \b, with
O-Benzamidothiophenol,
its Zinc Salt and 0,01 -Dibenzamidodiphenyldisulfide
PERIODICAL: Kauchuk i Rezina, 1960, No. 5, pp. 24 - 27
TEXT: After brief reference: to a previous article published in
"Kau-
chuk i Rezina", 1959, No. 8, p. 32 by the authors on the action
of thio-
phenols and their derivatives on the mastication of natural
rubber, they
point out that the present article deals with the results of an
investi-
gation of e-benzamidothiophenol, its zinc salt and o,ol
-dibenzamidothio-
phenyldisulfide (pepton 22). The method by which
o-benzamidothiophenol
was obtained is described. It is stated that the mechanism of
the reaction
has not yet been clarified. The structural formulae of the
reduction re-
action are given for o,ol - dibenzamidodiphenyldisulfide,
reduced to o-ben-
zamidothiophenol with sodium hydroxide and glucose., The
physical and
chemical properties of the obtained product are given: melting
point 101 -
M-A J/ 3

ip
S/138/60/000/005/007/012
A051/AO29
The Mastication of Natural Rubber with O-Benzamidothiophenol,its
Zinc Salt
and 0,01 -Dibenzamidodiphenyldisulfide
- 1030C, yield 75%. 0-benzamidothiophenol has a characteristic
odor, is
hardly soluble in water and dissolves well in hot alcohol, and
in acetone.
and chloroform when cold. The authors outline the procedilre for
obtaining
the zinc salt of the original product, and describe its chemical
and phy-
sical properties. It is pointed out that the salt obtained by
the given
method has similar properties as the imported salt. The activity
of the
benzamidothiophenol and its derivatives in mastication of rubber
was furth-
er studied under laboratory conditions. The details of the
investigation
are submitted whereby laboratory rollers and the Krupp-Gruzon
rubber mixer
were used. Various concentration of pepton 22 were applied and
the kine-
tics of the mastication at these concentrations can be seen in
Figure 1.
The obtained data reveal that the most active of the three
investigated
accelerators of mustication at the temperatures investigated,
was o-benzami-
dothiophenol. Pepton 22 seemed to be the least active in the
region where
the mastication effectiveness dropped with arl increase in the
temperature.
The zinc salt of o-benzamidothiophenol held an intermediate
position, In
Card 2/3

S/138/60/000/005/007/012
A051/AO29
The Mastication of Natural Rubber with O-Benzamidothiophenol,
its Zinc Salt
and 0,01 - Dibenzamidodiphenyldisulfide.
the temperature region where the mastication rate increases
with an in-
crease in the temperature, the activities of the disulfide and
the zinc
salt of o-benzamidothiophenol gradually approach each other,
The technolo-
gical and technical proberties of the masticated rubber
obtained by o-ben-
zamidothiophenol and its derivatives are/discussed. Pepton 22
is recommend--
ed for industrial use as an accelerator\v of mastication, in
addition to the
zinc salt of o-benzamidothiophenol * Both are only slightly
toxic and sta-
ble. The zinc salt is recommended for use at temperatures
below 130 0C, and
peptone 22 at temperatures above 130 0C. There are 5 figures
and 1 table.
ASSOCIATION: Nauchno-issledovatellskik institut shinnoy
promyshlennosti
(Scientific Research Institute of the Tire Industr
Card 3/3

S/138/60/000/011/005/010
A051AO29
AUTHORS: Eytingon, I.I., Karmin, B.K., Zhakova, V.G., Betts,
G.E.,
Kamenskaya, S.A.
TITLE: Mastication of Natural Rubber in the Presence of Para-
Tertiary Butylphonolmercaptane, Dimethylphenylparacresolmer-
captane, Their Zinc Salts and Disulfides
PERIODICAL: Kauchuk i rezina, 1960, No. 11, pp.21-24
TEXT: The results are given of work carried out on the
synthesis
and study of paratertiary butylphenol.mercaptane,
dimethylphenylparacresol-
mercaptane, their zinc salts and disulfides, as accelerators
of natural
rubber mastication. The method for producing the listed
accelerators is
outlined and a characteristic evaluation of these is given.
Corresponding
disulfides were used as the initial products for producing
substituted
arylmeroaptanes. Both products under investigation were
obtained by react-
ing sulfur monochloride with paratertiary butylphenol and
dimethylphenyl-
paracresol. The reaction is given as:
Card 1/to

S/138/60/000/011/005/010
A051/A029
Mastication of Natural Rubber in the Presence of
Para-Tertial-I Butylphen-
olmercaptane, Dimethylphenylparacresolmereaptane, Their
Zinc Salts and
Disulfides
2 + S2 C12 __V~ S + 2HCI; where R is the tertiary
butyl or dimethylbenzyl. The reaction was carried out in a
solution of
dichloroethane at its boiling point. Sulfur monochloride
was added gra-
dually, mixing for 2 hours. At the end of the reaction the
dichloroethalfe
was distilled off and the product obtained dried in a
vacuum at a tempera-
ture of 40-500C until a constant weight was achieved. The
disulfide
yields were 82 and 87% of the theoretical, respectively.
The obtained
products, which were resin-like substances, were subjected
to an elementary
analysis. The results were: for
Card 0_0
'7-

S/138/60/000/011/005/010
A051[AO29
Mastication of Natural Rubber in the Presence of Para-Tertiary
Butylphen-
olmercaptane, Dimethylphenylparacresolmercaptane, Their Zinc
Salts and
Disulfides
0 H S
C20H2602S2
calculated ................... 66.26 7.23 17.68
found 66.67 7.36 17.02
C 30E30 02S2 -
calculated ................... 74-07 6-17 13.16
found 74-40 5-99 12.81
The results showed that the synthesized substances correspond
to disulfide
of paratertiary butylphenol and disulfide
dimethylphanylparacresol. In
order to obtain corresponding mercaptanes from the disulfides
the reduc-
tion method was used with glucose and alkali hydroxide in an
alcohol-
aqueous medium (Ref-3). Results of an analysis of the zinc
content in the
zinc Balt of the corresponding mercaptane proved that sodium
mercaptide
and not phenolate is formed when reducing the disulfides with
glucose and
a calculated quantity of alkali hydroxide. The mercaptane
yield was 90 and
Card 311-G

S/138/60/000/011/005/010
A051/AO29
Mastication of Natural Rubber in the Presence of
Para-Tertiary Butylphen-
olmercaptane, Dimethylphenylparacresolmercaptane, Their
Zinc Salts and
Disulfides
97% of the theoretical, respectively. Zinc salts of the
paratertiary
butylphenolmereaptane and
dimethylphenylparacresolmercaptane were obtained
from the respective sodium mercaptides formed in the
process of the di-
sulfide reduction. The yield of the commercial product was
96% of the
theoretical. The zinc content for the C20 H2602S2 Zn was
calculated to be
15.2% and found experimentally as 14.7%. The authors point
out that they
were first to obtain the mercaptanes of the paratertiary
butylphenol and
dimethylphenylparacresol, their zinc salts and aiso
dimethylphenylpara-
cresol disulfide. A study was carried out of the action of
the parater-
tiary butylphenolmercaptane,
dimethylphenylparacresolmercaptans and their
derivatives on the mastication of natural rubber. Fig.1
shows the effect
of various doses of mastication accelerators on natural
rubber processing
on rollers, and Fig.2 the kinetics of mastication at
1000C. Data on the
effect of temperature on the mastication on rollers are
given in Fig.3.
The tested substances form the following decreasing series
according to
Card 4/It

S11 3816011000/011100 5/010
A051/AO29
Mastication of Natural Rubber in the Presence of Para-Tertiary
Butylphen-
olmercaptane, Dimethylphenylparacresolmercuptztnc, Their Zinc Salts
and
Disulfides
their effectiveness on the mastication process: paratertiary
butylphenol-
mercaptane, dimethylphenylparacresolmercapta-ie> zinc salts'>
disulfides.
The greater activity of the mercaptane as compared to the zinc
salts, etc.,
corresponds with data obtained previously by the authors in
studying tri-
chlorothiophenol, pentachlorothiophenol, orthobenzamide thiophen:)l
and
their derivatives (Ref.1,2). It was further found that the
mastication of
natural rubber in the presence of paratertiary
butylphenolmercap-bane,
ilimethylphenylparacresolmercap'l,ane, their zinc salts and
disulfAides is
hardly effective on the tendency of the breaker mixtures to
scorching, or
the vulcanization rate and ~hysico-mechunical properties of their
vul-
u
tanizates. The authors state in conclusion that for-industrial
application
nly the zinc salts of mercaptanies are of interest, since
mercartanes are
'toxic and easily decompose when stored, and the disulfides have-a
resin-
iike consistency. There are 3 sets of graphs, 1 table and 3
references:
2 Soviet and 1 German.
ASSOCIATION: Nauchrfo-issledovateltskiy institut shinnoy
promyshle.-L-iosti (Scien-
bard 51W tific Research Institute of the Tire Industry)

BRIMI, Istvan, dr.
Pathogenesis of leukoencephalitts basmorrhogica.
Orr. hetil. 96
no.6:164-166 6 SO 55.
1. A Fovarosi Ussoki utcat Korhas (igasgato:
Farlms Karoly dr.
candidatue) prosecturajanak kozlemenye.
(BRAIN. diseases,
leukoencephalitis hemorrhagics.)

EXCERM MMICA see.2 Vol.9/n Pb73i*1oj7,etc, Nw56
5104, 4BET&D-RIL and PARKAS K. FovArost Uzooki utacal
KOrhkz, Prosecturi.
W~Kftl. *Pancreds do nyllmirigy vizagilatok
kfsdrletes histamin aelh-
mdban do serum anaphylaxiftan. Studies on the
pancreas and
:alivary glands in experimental histamine asthma and
erum ana-)hyl axis ORV.HETIL. 1956,
97/11(294-297)lllus. 5
In guinea-pigs subjected to histamine asthma and
serum anaphylaxis, histological
changes similar to those in the dyscrina of Woe Mal
asthma in man were observed
in the bronchial system. pancreas and salivary
glands. The Identical dysfunctions
in the saliva-forming cells are ascribed to an
autonomic nervous disturbance.
Taking into consideration the tissue changes of
allergic nature observed in other
organs It is concluded that In both experimental and
human asthma a mechanism
involving the whole organism is involved. The attacks
of dyspnoea are due chiefly
to the bronchial dyscrinia.

E(CITTTA ',.'ZDICA Sea-13 V01.11/2 Dematology,etc-Feb57
464. BETLET11 1. and FODOR 1. IfauptsUldt. Uzsoki-titca
Krankenh., Budapest.
-7 ~er( i(!~),isozellul.Iii,enKret)s;trten der Haw. Ba sa
I cc I i cancers of
the ,;k in ACTA MORPILACAD. 'SCIE'NT. IRING. (MAipest)
1956, 6/3
(33~)-349) Tables I Illus. 8
Analysis of 787 basal cell carcinomas involving 70.5
patients. There were no re-
lations between tumour structure and localization in
different regions of tilt- body,
but for the internal ocular angle where the adenocystic
form is prevalent. Thore
was no conneution between clinical course and histological
type. in 2w7r. there w.IS
a direct relationship between tumours and epidermis
(speaks against Krompecher's
view). According to the authors, basal cell cancers are
initially rather uniforn-, in
morphology; the development of different types is
influenced by an inter-relation-
ship between stroma and parenchyma, and by secondary
degenerative provesses.
Basal cell carcinoma and its predominance in the face is
due to meteorological
and radioactive effects, but also to the presence of
embryonic branchial clefts.
Rezek - Miami, Fla. (V, 13, 16)

BETLERI, Istvan, dr.; PATAKY, Zsigmond, dr.
Came of polynuclear leukemia. Orv. hetil. 98
no.39:1087-1089
23 Sept 56.
1. A Fovarosi Uzsoki uteai Xorbas, Karoly, dr. az
orvostudomarvok
doktora) Prosecturajanak es a Budapesti OrvostudomarWi
Agyetem I.
sz. Sebeezeti Klinikajanak (igazgato: Hedri, Inclre,
dr. ee5ret. tanar)
kozlemenye.
(LIIUKDUA, MYELOCYTIC, case reports
granulocytic leukemia (Hun))

A,
MIRRI, Istvan; KOVO, letvan
Cortisone therapy of acute panoreatitleo Orv. hotil. 98
no.30-51:
1409-1410 15-22 Doe 57,
1. A Povarost Ussoki-utce.i. Korhas (igL%gLtot Ssauto
SLudar dr.) 1.69.
Sebesseti, Oestalyanak (foorvos: loves Istyan dr.)
kozlemenyo.
(PANOMIATIT159 ther,
cortisone (Ran))
WORTMONI, ther. use
panoreatitis (Hun))

BITIaRI 'Idtvaa Br
Generalized thromboangitis obl-ii6rane causing abdominal
crisis. OrT.
netil. 99 no.3:98-99 19 Jan 58.
1. A Povaroal Vzooki utcal EDrhas (Igazgato: Yarkas laroly dr.
&z
orvostudomanyok doktora) Prosecturajanak kozlemenye.
(TRWKBOANGITIS OBLIMA , compl.
&outo abdom. caused by generalized thromboangitis
obliterans, autopsy findings (Ehn))
(ABDUNIV, MUTS, stiol. & pathogen.
thromboangitte obliterans, generalized, autopsy findings
(Han))

BSTIARI, Istvan, Dr.; 'FARKAS, Karoly, Dr.; TANKA,
Dezoo, Dr.
Influencing experimental hiatamine asthma and ser=
anaphylaxis.
Orv. hetil. 99 no.21:713-715 25 WY 58.
1. Az Orsza~qos Rheum es Furdougyi Intezet (ignzgato:
Parkas Karoly
dr., az orvostudomanvok doktora) Korszovettani
J'aboratoriumanak so
az Uzsoki-utcai Korhaz (ignzrato: Szanto Sandor dr.) I.
sz. Sebeszeti
Osztal~vani4- (foorvos: koves Istvan dr. ) kozlemenye.
(ASTHXk, exper.
histamine-induced. influence of various chemicals in
guinea pigs (Hun))
(ALURGY, exper.
anaphylaxis, influence of various chemicals in guinea
pigs
(Hmn))

BODOKT, Gyorgy. Dr.; BNTIMI, Istvan, Dr.; FODOR,
Istvan. Dr.; BALKANY1,
Ivan, Dr.
Siderofibrosis lienis. Orv. hatil. 100 no.14:510-512 5
Apr 59.
1. Az Uzsoki-utcai korhas (ig. Szanto Sandor dr.) 1.
Bz. sebeszoti
oestalyanak (f oo: Koves Istvau dr. ) II. st.
belgyogyatizati oe&+Al-
yanak (foo.: Flamm Sandor dr.) es az ORM korszovettani
labora-
toriumnak (foo.: Farkas Karoly az orvostudomanyok
doktora) kozle-
menyo.
(SIDEROSIS, pathol.
siderofibrosis, histopathol. (Hun))
(SPIMN' die.
saw)

BITLXRI,IBtvan.d.r.; TANYA,Dozoo,dr.
Histological examination in experimental hypothermia.
Ory. hatil.
101 no.19-.667-670 8 W 060.
1. Orazagos Rheum es Furdougyi IntO26t, Sebeszeti
oaztaly es
Korbonstani oaztaly.
(HYPOTHMIA INIUCID exper. )

BETLERI . I.
Experimental investigations on so-called postoperative
disease. Acts.
chir. Acad. Sci. Hung. 3 no.1:85-95 162.
1. Chirurgische Abteiluni (Chefarst: Dr. T. Verebely)
und Prosektur
(Chefarzt: Dr. K. Farkas des Landesinstitutes fur
Reumatologie und
Balneologie, Budapest.
(SURGERY OPERATIVE compl)
(ADRENAL CORTEX HORMONES pharmacol)

BETLERI, Istvan, dr.
Steroids in surgical conditions. Magy. sebesz. 15
no.4:252-257 il 62.
(ADRENAL CORrEX HORMONES ther)
(SURGERY OPE RATIVF,)

t
I
r: r ~rl t ci ft I i t I "a 5 s lup to On-
uc ve i~ lin, t
ltil an, Vol 11
a 10
i~. in t F -.j r o c v r
-.4j 7 "L: t h i~ 1 IF- f I A
of
"15
oun -,atl cn

HUNOARY
BETLERI.-.15tvan.-Dr, KSRENYI, Karoly, Dr, LOVASZ,
Laszlo, Dr, YESZAROS,
Laszlo, Dr; National Institute of Rheumatology and
Balneolo.r-Y, Department
of Surgery (chief physician: VEREBELY, Tibor, Dr)
(Orszagos Reuma- es
Furdougyi Intezet, Sebeszeti Osztaly).
"Successful Resuscitation of Cardiac Arrest Following
Surgery."
Budapest, Orvosi Hetila_p, Vol 107, No 36, 4 Sep 66,
pages 1713-1714.
Abstract: [Authors' Hungarian summary] The successful
resuscitation of a
case oFeardiac arrest, by 100 minutes of manual, open
heart massage, is
reported. The arrest developed, for unclear reasons, in
a 22 year-old male
patient following surgery for a duodenal ulcer. 3
Hungarian, 4 Western
references.
1/1

BETUXER, Jaws., prof. (Murghit4i); TERM, Zoltan,,
prof. (Marghit&)
Solving some geometric problemb vith the aid of
complex ambers.
Gaz mat B 14 no.1:1-7 A 1190.

BETYAYEV., S. K. (Moscow)
"On the theory of magnetic deflection of gas from
wall of a conical
chamber; similarity compression of a conical piston"
report presented at the 2nd All-Union Congress on
Theoretical and AD lied
Mechanics, Moscow~ 29 Jan - 5 Feb 1964.

L 5532 xk EWA(c)IEWA(h) Pd-I/Pi-4
YA(d)/EWFCS'
ACCESSION NR- APSOID9393 S/020B/65/005/002/0274/0206
517.9:533.7
AUTHOR: Den~ayev, S. K. (Moscow)
TITLE: Self-similar separation of a gas from the surface of a
circular cone,or a
A
1wedge with attached shock wave
SOMCE: Zhurnal vycbislitellnoy matematiki I matewticheskoy fiziki, v.
5, no. 2, 1.
i-1965 _274-~286
TOPIC TAGS: gas dynamics, shock wave,-numerical method
ABSTRACT: Problems in the gas dynamics of jonical compression are
considered. The!
pressure on a piston and other functions are found from the law
defining-the ex-
patision pf the chamber. This'law is expressed in the form rj=
Etf(ej)] , wbere t
is time and rl and e2 are tba- polar coordinates of the piston.
Conical-compressionj
occurs in the limiting case when 3 +-. A shock wave is Introduced in
such coopres--
sion toward the apex of the conical chamber. A numerical solution is
carried out
for the resulting problem by the method of characteristics. Initial
conditions
are expressed by means of expansion in series, and a solution by
quadrature is
Card 1/2

- - - - - - - - - - -
L 55125-65
ACCESSION NR: AP5009393
given for the case when it.is possible. The Massau-Guderley method of
characteris
ties Is then applied to obtain a numerical solution of the partial
differential
equations. Estimates for the.applicability'of Guderley's method are
made for the
system in the presence of a shock wave. Orig. art. has: $2 formulas,
9 figures.
ASSOCIATION: none
SUBMITTED, 103un64 ENCL: 00 SUB CODE: GP, HA
NO REr SOV: 006 OTHER: 003
Card 2/2

BNTYGIN, K. 0 W-M
Computation of tvVorary-dimability relief for
workers and
employeen receivtng place rate pay. Okhr.truda i
sots. strakh.
no.5:64-66 N 158. (MIRIL 12:1)
(Insurance. Social)

USSqHw.i,-n cmd Physioloa. The Nervous Systen T-12
;~bs Jour Ref Zhur - Biol.) No 14, 1958, No 65747
uthor Bat-Wov
~nst
Title The Role of the Cutaneous Machanical ''malyzer in the
DeveloD-
,"ent of Ex-.3cri:--,ental Neurosis in the Dog
Ori g Pub : V sb.: Probl. sovreu. fiziol. nomi. i
-..iysh(!chu. sistcn.
Tbilisi. 'LN GruzSSR, 1956, 285-292
;ibstract : Ra-j3idly pro3ressing cxtenction of conditioned
reflexes wz~s
-Y
observed in three dobs in association with alternation
(without reinforce-ilent) of positive conditioned distant
stil~iuli (Ml2c)) 50 Watt bulb) worked up in response to
food
resinforcei.,ent. Extinction of the responses to
altcrnatin~,,
distmt (sound) and contact (touch) stimuli in thz~ presence
of the food roflex, or r~ltematin.; positive and Sicriiicina
torj distant stimuli in the presence of an electrodefensive
reflex, was accoupanied. by a reduction in salivation,
mc~infest,~tions of compensatory phase, Cmoralized
Card 1/2
125

B11111-f-UTBUYA, A. V# I - ..
------ ~--.
N.A.Tollskii, 1830-1891. Moskva, Gos.izd-vo med.lit-ry,
1953. 221 p.
(MIJu 6: 7 )
V. (Tollskii, Nikolai Alekseevich, 1830-1891)
1

BETYYEV, S.K. (Moskva)
Self-similar squeezing out of gas from the surface of
a circ-ular
cone or wedge with an additional shock wave. 7hur.
v.vc-. mat. i
mat. fiz. 5 no.2:274-286 Mr-Ap 165. (,Ii-L,'L!. 18:5)

G/030/62/002/007/004/004
;030/1230
AUTHORS: Betzel, M,., Hase, W., KleinetUck, K., and Tobisch, J.
TITLE: Measurement of the coherent scattering amplitudes
of Dysprosium and Tjulium for thermnl for thermal
neutrons
PERIODICAL: Physics, status solidi, V.2, no.7. 1b62. K164-K167
T3XT: The kno*'ledge of the nuclear scattering iron sections,
a prerequisite for the investigation of magnetic structures by means
of neutron diffraction, of 'rare earth is of interest in view of the.
increasing use of these elements for the development of magnetic
materials. In order to determine the coherent scattering amplitudes
of Dy and Tm, neutron diffraction diagrams 04 DY203 and Tm203 res-
pectively were obtained, with 1,197 1 OOM3 k1. Measurements
were standax*ized relative to a Nickel prepailation,using 4-,,k
Card 1/3

G/030/62/002/007/004/004
1030/1230
Measurement of the coherent scattering...
(13,2 1 0,2) barns for Ni. Atomic parameters and temperature factor
of DY20 and Tm 0 are assumed to be identical to the values publish-
ed for L20 (K2oeLer, Wollan and Wilkinson,-Phys. Rev., 110, 37,
(1958) ). ;rom the intensity of the 222 reflections values for the
coherent scatterin,~~ wuplitudes of 1,72 � 0,05 -10-3-2 cm for Dy and
0,69 � 0,02 - 10-14 cm for Tm are deduced. Structure factors cal-
culated with these values are compatible with those determined from
the intensities of the measured diffraction pattern. There are 2
tables and 2 figures.
ASSOCIATION: Zentralinstitut fUr Kernphysik, Bereich Reaktortechnik
und Neutrondnphysik, Rossendorf bei Dresden und
Institut fUr RUntgenkunde und Yfetallphysik der TU,
Dresden (Central Institute for'Nuclear Physics,
Depirtment Reactor Technique aiid Neutron Physics,
L-Card 2/3

G/030/62/002/007/004/004
1030/1230
Xeasurement of the coherent scattering...
Rossendorf near Dresden, and Institute for RBntgenology
and Metalphysics of the T.U.g Pread6n).
SMMITTED: June 12, 1962. VA

STANKOVIC, D., doe., dr.;
BEUC, M,,.,
Contribution to the study
19-26 162.
(OSTEOCHONDRITIS
(SalILUNAR BONE

11A.w-1j 1=1 'f I IA
1i ) Vi If-
BEM, V.A., KLIMOVA. X.N.
Remopoistic modifications in peptic ulcer befor and
following surpery.
Klin.med..Moskva 28 no-5:89 Kay 50. (CLIML 19:4)
1. Of the Leningrad Institute of Blood Transfusion
(Director -- V.V.
Kukharchik), Leningrad.

BEURAN, Ioan, ing.
Avoidance and removal of pebble deposits in
the cool4ng
system of internal combustion engines. Rev
transport 10
no-5:204-206-My 163.

PEURAJI,, N.
-- . .. ...... - -
SCIENCE
Periodicals: YEMOWGIA AFLICATA. Vol. 5, no. 5,
Sept./Oct. 1956
BRIMAN, 140. Problems of medical mptroloU-. p.
221
Monthly List of East European Accessions (EFAI)
LC, Vol. 8, No. 2,
February 1959, Unclass.

I T,,chiiology. Chemical Prodi!cts and H
Thcir Applications. Safzty and San-taticn.
f,.bs Jour: -','ef ?-hur-Iihimiya, 1959, Nlo 12256.
Author Riminiczanu., R.- Florescu, T.,- Arama 0.,-
T~estor., Aurelia; Vasiliu,
Inst Not qivsn.
Title On t'cic -1.')ror)hylaxis of Zinc Poisoning in
Polygraphic
-Enterpr is es .
CrIg Pub: Fed. interna, 1958, 10, hlr~ Z., 285-2091.
:.)stract: Methods are described for diagnosing zinc
,-)oison-
ing. Statistical data are cited on. the res-,ilts
of the medical examination of 173 workers of a
polygraphic enterprise. -- Z. J"haijqs%iy.
CE,rd 1/1
16

BEUS, A. A.
-Ii~blogioal ,Prospi;Ai~g-
Stratificatim
Minerals
jun 1948,
*Vertical Zonality of Pegmatites In Samples From a.
Pegmatite Field of Aksu-Pushtiry (Turkestan Ridge),"
A. A. Bms, 4 pp
*DOk Ak Rank SSER" Vol II, No 7
Briefs mineralogical findings in pegmatite veins in
subject area. Submitted Jkr 1948.
T6T48
PA7,-T48

1. 6E-US', A. A.; PETRCV, G. 1.
2. USSR (600)
4. Geolegy and Geography
7. T-heoreticnl Principles of the Science of Ore Deposits. By
I. I. Tanatar. (Kiev-Llvcv,
Incraine State Technical Press, 1950). Reviewed by A. A. Beus
and G. 1. retrov.
Sov. Kniga, No. 6, 1950. ----
9. IWReport U-3081, 16 Jan. 1953. Unclassified.

oplite-Re (uplPoitill ~~Wtids f pvgmptifts imllcae chew.
itittrac';(ins (4 tile Ilagalatic material Trith tile Countly
rock--, which are evident in the chtav. Werencez betwe"n
the centrd, and the salilzind patts of cumplex veirm of this"
type. D. studied these phenomena In the blSia-ternp. ptj~
matites in wica scilists r.1 the Turkestai chnins, xhich-w-C
typical graphic uartz-blotitt-wicrodine nxks, widt Lt-
granular magiij rotma oi sowedmeg on!v 3-cm. thicl-ueo,
with aciculex tourmaline. The granite iii(Abe: ruck of the
pegruatites Plows, with systemauc arproach to tht Vehl.
decrtasing rontents in green amphillo1c, and inerming cuo'
tents in tourmaline and musLovitc wbirb gtadually jep=
the biut!te. The aplitold zone shovrg strWngly 2 tenera-
tions of rr&roeline, and ftne-gnurular quartz repl;Ang 6e:
feldmar ivith microgTanitic intergrowthl (d both j?dvei-aU,.
ninA tlut-maline, and some abnandite. , The wie3 of cbew.
Of SaMP1*3 Pr Idt illeSe ZOlItS $br.W &.XtArRt
Linpuverisiment of the aplita;d margWal runts in Ve, PeA.
CELO, and Mg% but! a considerable incrtns, in K30, vrrath Is;
explutued 'y th~ musco*tizatiorl of tht dark bialte. Tite
oi a sviec, Of thin btclion-C

ic -[I ,cf, is f t I I e
nud the pq;matite, Oiolvs a stiong turichiullit !n Atg
al"I M4.11), t,f HlOallmratic inim-rals ill tilt- fzdbauds
ploper; All'! WillS Whidl LAVC lk ~11`01!gly (IC-
N"A.'J'wd aplitoid zont, ~llld we much l3iff,zoa tilt! 11LSS
t1m vcui tzck by all c-avirimwrit in bhtitu, t,,! irtnalhic
alln.--oulitc, alid evc'.n In:tgnetite. Thvie is a ~is
thict r0itim Lai~cvn the thic1m;s ~,f tilt oplitcid zones,
and tile collcil. ill ImInn'tcratic lllinfrll~ ill tilt!
11vi'lliatitc.,
vdrN. Thk 1',c,ulfirowd Lly tilt, liott. of
tA.Vlt ftk'IU tilt' SAINU I-J60t IlLid LV~ll dc-
ill thill-Ldioli analytk.. The o,ulflty Ndlkts 1kre
ill(' jjj(~Ve CTJljC1ltl1 ill iflLdiCl. 111111
ilIIjY.VL1i!,1lt~(j ill Nir niid
J~c tile nearer the !,ailipics ar~ it) 11;v cr-w:izt.
~~s',-,%t t~) tile
ap1it,,id salt,ands F,- atid N11, lm~ cu%'.~-fv A, bkit YjO
i~ tle.
cha,cd. in C'4111parioll with Old v,:i;-- I'v1:11:10itc, 311
rough
witfille: Fe wid Mg ruigroti, from t1w %r~llkts 011t0 tile
K:o fr.lni the purmutit(! onr, jb(: ~Vlkku.
W. tilel

Mepodwille and two now mut.
*fide frotia pogroadles. A, A, lirw- DrikWy
A W. Naildt
N.S.S.M. front the Turkei,
tan Ridge frMuently ctmWo plamphAte
minerd1s. The new
mineral% at-, found in
MUW.0Vilt-l)%k-Ttlrlillr JIVIIIIAtitr a
Kyrk-HuIALA. im.". with triphylitc.
arrojadite. and their
.illeration produrti. MAguesiophilite is
3(1%fn~ Fe. Nfc K 1,
P,(),, in utmoo-pitik-cgured SITKULAtiC
CFY'tA(A. The min.
ri-Al I, intimAtIrly inturtfrown Willi
ITiphylite. in biulitc
whist xenolilh% of the pegotatile- Pyrite,
chalcupyriie,
ant I pyrrhot ite wre oft tit includeti.
Thefictu,I: (Itilit,(Illili.
111V 01111111)A Ill
%%Itll ITilthylite i% ofil-will .1 1.1
111t. el."ItIA1,111 411.1 (11110:.
1%oth-liku arrmiaejorjil~. Willi 1111.
OtAractirli'lic ilial'.
I%%, voinvide in both inincrok. 6ut the
avotr bi-ectri,,t,
I'm and i rimp. I foirno ;tit auxle of:110
lit 45'. Magnv%inphifitc
I% 0111iCA11Y p0h., 2W 111 44 - 4M*; *~, )
- I -U; 0 -
1,7(ki: . - 1.41395. all :J:0.41111;
colurle., in thin section,
The ininer-A bt rather umilar to
graftonitc, but CAO 6
entirely absent, and Mgt) high; the
magnesiophilite is thus
the Afg analog of lith4hilite, Li(.Nftt.
Fc)PO.. The d-
%paciuss of the powdei diAV&m are given.
Matigamt-
lioniorkite ii a hypergenic metasomatic
product in the oxidA-
tinei zotie of the jOegmatites. The new
mineral is earthv,
,xtreiltely filic-cry-.1 ; the martgates
are lviukih %iolri III`
War. The it is Afk-An I fl~,; to 1 711, d.
~' IV, when beitni, the
lo~c. much 11,0 (8% britio, ~,l lr~ Al.,kr
11,01
I he ChCOll AlWyltill 19 in ligICCIltellf
Willi the k1-4111111 I I'C, NhO
110,311-0- W~ Fif'.1

;:7
Ll "S

Ne~. pts!bzte miptral- in pexpuatit" of the Tisrk-
Stim few Thdy Afixprv.ag VuL3ya

Akad. Nark -11i~nvllnc-,

e
,
111USCOVIt. 'o'd allAte trient pegmthes o( the Turke-:

stan ranges contuin iltyr1opinents of inttmting
mincrals.

Crystab of Uiphylite, Ituni I:yTk-Bu6k shuw vh~
Bnna~

10101, (OOLI, 1110h, 11201, 11011, 10211, of p9cul I
onal habit
11
excellent clmva
e
aralL ( evi t
D
3

.
.
.
;
g
p
and (010). poorpereltel (110). OptlcaUynej.,2VJO-.?Wd

PLme of the opticO urs is (Ift 6 a
,
700~LM
692
695
70D
~
1
1
1
708

-
-
-
.
.
.
y - 1.
.
; P - 1.
;
The Chem. analysb shows the compa. to be LINPO, 0%,i

LINInPO, 13%. mnd PwIniophilise (Mi.. Fe ' IdgmP04.5
-
f LJ
1)
i]ha'

,
,nnt o
24% This indicato the replace
(
q
+'
Felt by Al
The pegmatites thow lithlophilite in the:

.
g
cent, a! parts. assoed. vvith druvdandite, follovied by
a zcce
-of triphylitr, and this Trijiml liordered by akut-Tite
(.(,P:I-l
t

Cully neg.; -y - 1,733; a -- 1.714), which b chitil to
2t,

trosite on ctucks. The Complete mnluvil of !~-brinvs!

auctit th,! crystn. of ammdary Ll tvurnalli*-vi
Ahitized!

itone. Bbaial Mn apatite (with y LMD;

a - 1.678~
with the litb I'llite. -Iletem%ite IN
LI
l

O
i9r__
-
v0
.. AVWO&~~

tb~axld:iiliin lir - itet-w-lili" moval of LI from
tripfiy1ldiii ir.
3.410,2 - - % r, on pleochrolsin In brown-red colors;
optical ON lane (1 1, however, Is not replaced by-
heterosite, tit mains h. The chrm. Shows
lwtn'o~ , Mg 1.9470. 1 is a lieW iniuvral, ob-~
kerved in hitininte ' %Ttli with triphylite; color sal-
ITI-111-roqc, fnity luster, r Cleavage, tiften vilth
inchulonq,
of Plulfide-4. rurnis I lWl 10161. 11101. The regular (it.
tergriwthivitlittiphyllte il(iws (tit eros4
iectionsperpendicu.,
t-Ar to the prlsmmlc elmigmloit a ii-eudoltexaVital
network'
Avith laniellae hitem-cting nt 69", with Identical
orlentutlon
ond extinction In the lamellite 4 1. Mine of Optic axes Is
4100); optially .. 2 %, - the wite lilsectrix of I
ncludes an n. Of 30-45": -r - 1.712, # - 1.70d; a -
1.605. '17he x-ray data are oonitwhat different from tho4e
of graftonite (Nickel Plate). The chem. atinlysis zhows
MKO 0.50%. but "1 0.54% CaO. Arrojadite (11).
MgO-rich, I;; ob~.erved is charticteristic reaction thns
be-
tween triphylite and ulbite, minctlines lit
well-iltveloptd,
crystals with (1001, 0101, (1101; hardnats 5, c-,teellent
cleavage In one directinn, extinction nenrly parallel (2'
to
4" devitition); y - - 1.7".0; a - I.M; 2 V - 72'; wejk
Fleuchrolsm parallel y, dark-imvit parallel a, and h
somewhat
Irighttr green. The chon. analysis conx-5ponds to the
ratio (RO + R,O):(PO,) 3: 1. vridi 5.08%. NatO, and

J~
19. 6"S ~A
n. an mor-
-3 0. - R1.1( ),mt R1 O(PO.) b Chw In
e.P R1 "M e Mg,11D)r`
le ten tiv. f 'ola 2 N1n.Fe)PO..4 F
for the r
(POO7 kest= rMuct of H. Nin SVC) 1%
(-N1n.Fe)POt-2HjO, nud hin konhickilt. (Fc,N',n)
.31 '0,
are found in md-violet formsktiw)3 on Mphylite and
betero-
-site. The Mn strengite has tht cleavn 1) and (100)
of different qualities, hardness -1.8, a U;arpl
hroixmfn
violet-blue colors; rime lot the optic axes (I ); 2
V
42', optkxliy pos., strong dispaxsLin r >x; y -
1.740, a
1.710, 1108, The Mn koninckite forms clay-liki
vlolet-colored eggregatc% with ms 1.08-1.70,
strongly plea.
chroic, d. 2.05. It Is derived from heterailte by
simple by. I
dration. Palsitt, 2H4MnFe)4PO,),,3Ii%O. In changed
by I
oxidation to a mJxt. of manganite, wid Ma
strengite. whiel,
jn turn h changed by hydration tn Nin koainckite.
PeAvIte
(hureaulite) fonns red-colorml, rounded aggregates
In pan- i
Sencsi-, w:th tiipby)ite and black tourmaline;
optic-411Y I
neg., 2 V - 82*; -y - I iM: P - I.M5 ; a - 1.649.
Vas.
:hegyite, 4AIj03.3PO..30H,0- Sordonita MgO. A1,0j.-
P,06.9H,O, and evans3te,
'observed in the muscovile-microcline pegmatites in
WUAU
amylules surrounding triphylite and Mn konincUte
ne3ts. i
va,
,h gy1t; is den . vrWte, hardnL-. J; d. 1.90-1,02;
ho.
tropic. n IAW- 1.5W. C' oidonitt in xuall tabular
rzys.

tilIN is F":'ocd. IS-Ith V;Lqlleg)-itr; biw6d, POS.,
-f
tile
a 2 V ~ approx. W. Evansite N observed in
central patLi of !Ile alayl"(14fles, colloidal,
opal-like, wk)"C'
Ity exaltalldwitiolls of Pe,O)'A11101, etc.,
i~O)troplc, 1. strouly
varial& idth the Ve content, ficlin )AM to 1.492; d,
var-
IpMe between 1.85 unfl 1.93. W. Eltel

BFJ5, A. A.
=R/kinerala - Pesmatites Nov/Dec 51
"Zonation of Granitic Pegmatites," A. A. Beus
"Iz Ak Nauk SSSR, Ser Geol" No 6, pp B7-102
Beus classifies pegmatite zones in his descrip-
tion of zonation of granitic pegmatites and con-
cludes by agreeing with his predecessors that
pegmatites are products of magma crystn, en-
riched with volatile'components.
205T86

BEUS, A. A.
"The Isomorphism of Beryllium in Regard to Phenomena of Its
Dispersion and
Concentration," Dokl. AN SSSR, 90, No.3, pp 425-28, 1953
There is a connection between the phenomena of dispersion and
cone of Be
and the character of heterovalent isomorphism Which is detd by
the possibility of
isomorphic inclusion of Be in the lattices of rock-forming
silicates. The inclusion
of some cations (Ti, Ygj etc.) from other rocks in the process
of mineral formation
enhances the possibility of the inclusion of Be in the lattices
of rock-forming mine
and leads to a 5-to-10-fold increase of Be in the silicates of
skarns and pegmatites
of pure origin. Presented by Acad. D. S. Belyankin 23 Mar 53.
260T14

otighl of t1le zoning of jl~-cnlto
permatites. A - A, l3tv-~.
Orklally Akad. A'auk S.S.S.R. 97,
lijil-cial Crotip of (Ito mi"oditte mr-ul
zillit(e p, '-r
~' !'~ll le 111 ~ruj -- 1 1% 1; i ell - hows
t 1147 Sol I i1 I ~ trt I C t u I C Of K I a
ti i I Q
per'llilititri In geocral Ill tile :1
lltlye~ Of I I[
anii Ill
tolvOr. mincralizatimi. B. d(" iiot think-
Old magmExtIr
diftmut tit( loll Is the kadtor m lovilIN bi
dtlvrlVkM1g ;W41.13A.
the,n flom rtmiikh! Ou%plim, NO npraki of
thpir i~y
rlltc~ll" rrv'Nill, Tht Reol. laktOI5
luillig tlicst. 31iqcs are
tile ICvcI 0t tl;c Injection. the tectollic
c0:10itipilq 11:4iatll
tile illjLctioll alld crystn" and tit(, lomf
conditiom,
cold sixq d the Isegmalitc ImAks. B. duts.
zkl, Ott dvgice oi
tht Telntivr lirilits of the mmem ill the
different ancl
espuially the posribility oi the prntriiFion
of Volatilei I]' Ole
vertical direction of t~e pegmalite
injectivIlS. For CY.,01
011C of tile 35tilgrs it il showtt how
ffId-way tire riall-lo'.1 lit
-the mili'l lihme, hi I Ill g(aphic etk(Mttv
1wd
fridmat ixxll,~s, Ill It as mamive iWiodloc,
with bM,I, unit Rpoilumenc, and late
jwth:tic and
211115covitic crystim, ill In with massive
nuprtz (fly by'draly
sis), nod late ulbitization, Ricistm, gild
as
mphimittent phe"olmol. If Slam the NjuilIMA
a nag.
niatic dinn. lit the fillearting of Motility
(cf. CA. 39, 403P)
from Superaltical, In that of super- or
ultdin-rcrit, Sollm. of
tile livirtrothermal tvpe. W. INIA

C--

0
ctent of turn in
"ryllham
OvRehem"I distTibutina C:T
"
'I
Z
iM
~

a4
#Percnx
n u
itts A. A. 136
Vftd
dAd �. N. gSgOT1111A,
pYk
KkO
R 108-1I
d
I955
f
=

.
.
.
), c
y
A
N
W
5
i
~

G

e
WBernineraiarefoun Latl
C.A. 49, ll5lIg,-Typ
.1
lelate-
.Iua

,magm9tic pegmatites, as-soed. with feldspars and
micas

(musLovitc, lepidolite). The early stages of
matitiza-
'

ODA'ari I'sually low in Be (O-WDI
to 0-MM % , m graphic
m

iranilis with microcline. e.g. in the granites 0~ the
Shitomir-

Kirovograd w*--- in Ukraine. Beryllium is in
these early

pegruatite formations "captured" Irk the
feldspam, by a

coupled ionic replacement of the type
(K, Na) t +
0
':
R
1

.
by rare earth tlerutnt3l' + IBC()4)1-, or 'Ca" +
0
:

by2raitcarthelernLnts'~+(DcO,lo-. ~(beiocrcasingcon-

tents of the later pegmatitesof the "j)urcline" in
rare earths

are usually accompanied by the appearance
of Be in garnet,

spodu.nene, tourmaline, gilbertite.
apatite, muscoxite,

kpidulite, -with 0.('k)16 to 0.0126
% Be. In pneumatelyt-ic

p,egmafites, the contents in Be
ue particularly enriched, e.g.

in m3xgjr;te (0.43 to
0.67% Be), phlogopiti (0.025 to

0.00005-'~). and
typical Be minerals occur in such forma.

tions either
of contact-metasomatic and prieurnatolytic

type,
characterized by enrichnients In TI, Cr, Mg. which are

hoeign to the granitic pegmatites of the "pure fine,"
or with

high contents in F-,.e.g. in micas, with the
coupled ionic

replacements Sift + 2(0H)- by Be" + 2 F-.
With such

variable oin-litions of the enrichments in
Be. it is
dif-

fi~ult to det. a gcn~ral geochrm, distribution
cocil or Be.
7

A tolerable estn. I" pegmatites may be about 0,0020%
Be.

But this cocil. varies in rather wide limits for
peginatites

which we free from Tare earth minerals (not
albitized), peg-

matites with minerals contg. rare
earths, but no beryl. and

Pegmatite- w-th beryl concns.
of O.Oj jP 0.1%. or even 0,2

to .2.5% beryl. 'F-,,Eitel

V
Laboratoriya mineralojifi ge0kchildi-redki aLem
akademft nauk SSSSR* Predstavleno akadeMikom D. 1.
S1hCherb6kO-7YM-

azus,~-A'leksay Aleksandrovich, STE:-ANOV, I.S.,
redaktor; SMINNOVA. !-I-V.,
CHKINA. K.Y., tekhniche3kly redaktor.
[Beryllium; appraisal of deposits in prospecting]
Berillii; otseaka
nestorozhdenit pri polek&a 1 rarredkakh. Moskva,
Gou.nauchno-tokhn.
hd-vo lit-ry po geologti I okhrane nedr, 1956. 147 p.
(MLU 9:5)
(Beryllium)

'
,ft
im

..
Im
a
Ph -wry j Br im"n th..'j?4A

and propettits of its iin, were txattu~nu&

of berYlliuvot witb ~41ie*n bas bm-n proved pri-siible, en mndlu'lf,

that clec'-;-~Matic Cquilibrilml is ret fined (.1) in the
iv

by Avay el -a para-Het cwry h1to the strzcturt! of !~,-Nmt hisi,
'
!

it r,
.' C
V~'
,

ae.
, ill PIAM;)l mlin

b-,
in OIL nr.-i0q part, by rep', na ~S:O;)' [BeWiF.

tMassnitt, mus"Vi1r, phkg~p"-
Ynjy~anite, ~1"

Examples of ismtruuiural -*Scan~l;-nh-m of

wlih
silizues (wilkinite, ca int' C'-'Zeklittz'

thctrite, art
etc.), 'd bormliicate!i (homilitt:, darain; L-e 1;-

Ith bavem4c as an
riairipk' thL! PD~-Ability of a tiu

lainitai has Inn J~

14 ~;l I"T. 11
the ,1y-

I
.1.i,
- _-,
i
I

15-57-4-4594
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr
4,
pp 85-86 (USSR)
AUTHORS: BeusY A. A., Zalashkova, N. Ye.
TITLE: The Origin of the Sodium Variety of Beryl in Granite
Pegmatites (0 genezise nitriyevoy raznovidnosti berilla
v granitnykii pegmatitakh)
PERIODICAL: Mineralog. sb.-Llvovsk. geol. o-vo pri un-te,
1956,
Nr 10, pp 273-287.
ABSTRACT: Crystals and intergrowths of sodium beryl are most
common in partially albitized pegmatites. They are
characterized by tapered or acutely pyramidal features,
The tapered and pyramidal crystals are aggregates of
intimately intergrown individual crystals. In addition
to the massive varieties, 'Istuffed" crystals are widely
developed. The principal features of these "stuffed"
crystals are inclusions of albite, quartz, more rarely
muscovite, tourmaline, and microcline. The "stuffed"
Card 1/3 crystals are complex formations, consisting of a
number

15-57 -4 -4594
The Origin of the Sodium Variety of Beryl in Granite (Cont.)
of uniformly oriented, intimately intergrown individual
crystals of
distinctive tabular form. In all the deposits studied, the
tapered
sodium beryl is characteristic of an albite-replaced
complex that
formed In blocky-microcline or coarse-grained pegmatite
that consists
of pegmatoid.al segregations of potash feldspar and quartz.
When
albitization is superimposed on a zone of graphic pegmatite
or on
coarse-grained pegmatite of relict graphic structures,
11staffed"
tapered sodium beryl is formed rather than the massive
tapered
variety. Locally there is a gradual transition into a later
variety
consisting of thin prisms. The largest accumulations of the
11stuffed" beryl are found in pegmatoidal bodies where the
zone of
graphic or relict graphic pegmatite is immadiately next to
the
quartz-microcline core of the pegmatite or next to the zone
of
quartz-muscovite replacement it complex that surrounds the
core. In
the beryl-bearing zone, the stuffed" sodium berTl is
distributed
rather uniformly. Both the massive and "stuffed sodium
beryl are
probably of metasomatic origin. They formed by the
replacement of
microcline by the action of beryllium-bearing alkaline
solutions,
Card 2/3

15-5 7-4 -4594
The Origin of the Sodium Variety of Beryl in Granite (Cont.)
separated In the crystallization process from the residual
silica-
rich part of the pegmatitic melt-solation.
Card 3/3 G. A. G.

USSR/Cosmochemistry
A)
:3eochem stry. Hydrochemistry
Abs Jour Referat. Zhurnal Khim-iya., No 0, 1951, 18894
D
Author A.A. Beus. L.I. Sazhiiia
Inst
Title Concerning Berilli.um Colitents in Acid MaTnatic
Rocks.
Orig Pub. Dohl. AN SSSR, 1956, lo.), 140 4. 807-810.
.Abstract Berillium contents were 6pectroscopically
detemined
la 300 mean samples., individual specimens and rock
forming minerals from varous granite r-anges of USSR
(mean samples were prepared each from 15 to 30 separ-
ate samples taken wth in the limits of a ranSe)
Samples contajning less thaa 3 x 10-11% Be were ana-
ljzed us-ing, the Mori.n fluorcm-atrie method. Following
- 32 x 10-
limits were obtained for Eranite rocks: 2 4.
the mean value 5 x 10-4 exceeds the values obtained
by Goldschmidt (3-6 x ~)- 4) brid Sindell (3 x 10-4)
using a comparatiNrely small number of specimens. Dis-
tribution of Be in rock formLn-7 minerals (according
to 4 or 5 determinations in %~: feldspars I - 10
X 10-4, quartz < 2 x 10-~, micas and hornblende from
1 X 10-4 (biotite) to 5 x lo*3 (muscovite). Increased
Card 1/2 -7-

BEUS, A. A.
[Basic characteristics of beryllium geochemistry and
genetic
types of beryllium deposita; abiftrect of a dissertation
for the
degree of doctor of geological and mineralogical
sciences] 0snovve
cherty geokhtmii berillita i gensticbeskie tipy
berillievykh
mestorozhdanit; avtoreferat diesertatsii, Drodstavlennoi
na
soisksnie uchenoi stepeni doktora
geologo-mineralogicheskikh
nauk. Moskva, Akad. nauk SSSR, 1957. 38 p. (MIRA 11:11)
(Beryllium)

JI-
BEUS. A. A. Doo Geol-Min Sci -- (dies) "Basic features
of geochemistry of
C4-
beryllium,/and genetic ty es of beryllium deposits."
MOB, 1957. 40 pp
-I AL
(Aoad Sci USSR. Inst of/~ineralogyv Geochesnistryand
Crystallochemistry of
Rare Elements), 150 copies (KL, 42-57, 91)
-11-

BEUS, A.A.
IP-1
Concerning S.T. Badalov's article "Results of the
hydrothermal helvite." Izv. AN Uz. SSR. Ser. geol.
study of
no.2:85 157.
(MIRA 11:9)
(Helvite)

AUTHOR: Beus, A.A. 11-e-1/14
TITLE: Geochemistry of Beryllium in Granitic Pegmatites (K
geokhimii
berilliya v pranitnykh pegmatitakh)
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya
Geologicheskaya, 1957,
# 8, D 3-15 (USSR)
ABSTRACT: The author discusses some problems in geochemistry of
beryllium
in granitic pegmatites and distribution of beryllium in peg-
matite deposits. The author defines the concept of-"pegmatite
injection" as a series. of pegmatite formations of the same
age connected with the same pegmatite seat and occupying a
certain position in the tectonic structure of a region. In-
dividual pegmatite bodies of the injtotion can be either in-
terconnected or completely isolated along the vertical direction.
The horizontal zonation of & pegmatite field does not exist
by itself, but represents a reflection of the vertical zonat-
ion of a pegmatite injection. The character of the vertical
zonation is closely interconnected with the geologic position
of the pegmatite formations, the components of an injection,
This character of the vertical zonation is one of the main
factors which determine the distribution of rare-metnl minernl-
Card 1/4 ization, including beryllium within the boundaries of a
peg-

Geochemistry of Beryllium in Granitic Pegmatites 11-8-1/14
matite injection. Beryllium minerals do not occurv as a rule,
in the roots of the pegmatite injection. Beryl accumulations
are associated with the zones of block pegmatites (in small-
block pegmatites) and with the boundary zones of the block
quartz (in large-block and entirely differentiated
~egmatites~,
The concentration of the main beryllium mineral, beryl, in
the converted pegmatitea varies in wide ranges, sometimes up
to 0.6 to I %. The beryllium in a pegmatite injection is
accumulated in the well differentiated pegmatite bodies of
the middle horizon of the injection, and especially in the
upper horizons. A principal fattor which determines the
concentration of beryllium in pegmatites is the process of
crystallization differentiation, which is of special signific-
ance during the early phases of pegmatite origination. The
main assertions of the theory of phase crystallization are
as follows:
1. Pegmatites are formed as a result of the phase crystall-
ization of the pegmatite molten mass which is a product of a
normal granitic molten mass enriched with volatile substances.
2. The crystallization of the molten mass occurs in a
relatively closed system.
3. Phenomena of replacement, typical for pegmntites, are
Card 2/4 considered as results of interaction of the
paragenetic com-

Geochemiatry of Beryllium in Granitic Pegmatites 11-8-1/14
plexes of the primary crystallization with emanations (and
solutions) which separate from the pegmatite molten solution
in the process of its crystallization.
A scheme of the formation of granitic pegmatite zonation is
illustrated in Fig. 1 in the article which shows the follow-
ing 3 pha.ses: opigmatic, pneumato-magmatic, and
hydrothermal-
pneumatolytic phases. In the course of evolution of the peg-
matite process, the separation of beryllium occurs. One part
of beryllium, contained in the pegmatite molten solution, is
crystallized directly out of the residual silicate solution
(non-alkaline modification). The other part, by far the
greater one, in captured by the alkaline emanations and sol-
utions, migrates into various sections of the pegmatite body,
and precipitates into the solid phase as an alkaline modi-
fication of beryl. The author then discusses various possible
forms of beryllium migration. Studies of beryllium distribut-
ion in pegmatit*s resulted in the establishment of the 8ver-
age beryllium contents as being 0.002 ~6. It is observed
that beryllium occurs in a constant paragenesis with such
rare elements as niobium, tantalum, zirconium, which are
connected with the activity of alkaline emanations and solut-
Card 3/4 ions.

Geochemistry of Beryllium in Granitic Pegmatitos 11-8-1/14
The article contains 2 figures, I table and 18 references,
13 of which are Slavic.
AVAILABLEt Library of Congress
Card 4/4

BNJSO A.A.
Beryllian idocrame. Trudy Min. muz. no,8:25-28 '57.
(KIRA 110)
(Idocrane)

A U!T H OR
Bous, A. A. Soy 7-58-4-3/13

TITLE:
RA
The Ole of Complex Compounds in the Transport and Con-

centration of Rare Elements in Endogenous Solutions

(Roll
kompleksnykh soyedineniy v perenose i kontsentratsii

redkikh
elementov v endogennykh rastvorakh)
PERIODICAL:
Geokhimiya,
1958, Nr 4v PP- 307 - 313 (USSR)
ABSTRACT:
Complex compounds
influence the transport and the formation

of endogenous
minerals, above all in the case of the rare

elements which
are typically amphoteric (Be, Zr, Hf, 14b,

Ta, and others),
or very weak bases (Se, sE and others). in

the case of high
concentration of strong bases and acids

complex compounds
(acidocomplexes) are the most probable

form for these
elements, in aqueous as well as in supercri-

tical solution.
Fluorine, chlorine, (CO ), HCO - and above
'
L
A

h
a
all phosphate may be complex formers. S
mplex may

be decomposed by reaction of the dissociated ions
with

other components of the solution and by hydrolysis.
Elements

with similar chemical properties are sepaxated, if
the com-
Card 1/3
plexes are of different stability; on the
other hand che-

sovi 7-56-4-3/13
Thu RAOle of Complex Compounds in the Transport and
Concen~ration of Rare
Elements in Endogenous Solutions
mically different elements may precipitate together if the
acidocomplexes have a similar stability. Such a separation
is found in the case of columbium and tantalum, the rare
earths of the cerium- and yttrium Croup and some others; the
common precipitation of elements is illustrated by the
close paragenesis of beryllium, columbite, and cytblite (Be,
Nb, Zr), in granite pegmatites, of pyrochlorine and cir-
conium (Nbj Zr) in albitized alkaline rocks, of columbite
.-.nd circonium (ITh, Zr) in albitized granite porphyries etc.
Whether a further investigation of this problem is success-
ful depends on the fact that the complex compounds of the
rare elements are investigated experimentally and material
is collected on the composition of gaseous-liquid inclu-
sions in minerals of rare elements. There are 12Soviet.-
references.
ASSOCIATION: Institut mineralogii, geokhimii i kristallokhimii
redkikh
elementov AN SSSRj Moskva
(moscow Institute of Mineralogy, Geochemistry and Crystal
Card 2/3 Chemistry of Rare Elements AS USSR)

suv/ 7-50-4-3/13
The R81e of Complex Conpounds in the Transport and
Conoentration of Rare
Elements in Endogenous Solutions
SUBMITTED: April 11, 1958
1. Rare earth elements--Separation 2. Complex
compc~inds--Chemical
reactions 3. Solutions--Chemical properties
Card 3/3

Le
RUMANIA / Cosmochemistry, Geochemistry,
Hydrochemistry, D
Abs Jour: Ref Zhur-Khimiya, No 18, 1958, 60463.
Author
Inst
Title Geochemistry of Berillium.
Orig Pub: An. Rom.-Sov. Ser. geol.-geogr., 1958,
12, No 1,
W~-63 -
Abstract: Translation. See RZhKhim, 1958, 7427.
Card 1/1

BEUS, A. A. Doc Geol-Min Sci -- (dies) "Basic features of
the geochemistry of
berylliumsand the genetic types of beryllim deposits."
MDs, 1959. 40 pp;
1 sheet of tables (Aced Sci USSR. Inst of Mineralogy,
Geochemistry.and Crystal
- L ~s r-
Chemistry.of Rare-11mments), 250 copies = of authorts
works at end of text
/N
(15 titles) M. 52-59, 117)
-26-

BEUS, A.A.; STBPANOV. I.S.. nauchnyy red.; NEKRASOVA,
H.B., red.izd-ve;
--1VANOVA, A.G., takhn.red.
[Trabovaniia promyshlennosti k kacheotvu minerallnogo
eyriia;
spravochnik dlia geologov. Izd.2., parer. Moskva,
Gos.nauchno-
takhn.izd-vo lit-ry po geologii i okhrene nedr. No-36.
(Beryllium].
Berillii. Nauchn.red. I.S.Stepanov. 1959. 35 p.
(MIRA 13:7)
1. Moscow. Ysesoyuznyy nauchno-inaledovatellskiy
institut mine-
rallnogo syr1ya.
(Beryllium)

SIMETEVA, Nina Dmitriyevna;,J3EVq,, A.A,.-, doktor
ge ol. -mineral. nauk,
otv.red.; SDMIN. S.M., red.izd-va; KUZIMIN. I.F.,
tekhn.red.
(Mineralogy, types of depoBits, and baoic
geochemical charac-
teristics of selenium and tellurium] Kineralogiia,
tipy mesto-
rozhdenil i oanovnye cherty gookhimii selena i
tellura. Moskva,
Izd-vo Akad.nauk SSSR, 1959. 254 P. (MIRA 13:2)
(Selenium) (Tellurium)

,-,~7us, A.A.
Basic characteristics of the geochemistry of bezjllium
in the
hydrotbermal-pneumatoly-tic process. Trudy Inst.min.,
--eokhim.i
t
kristalokhim.red.elem. no-2:7-18 '59. (MIRA 15:4)
(Beryllium)

AUTHOR: Beus, A.. A., SOV/7-59-3-10/13
TITLE: Discussions (Diskussiya). On the Position of Alkali
Metals in the Structure of Beryl (0 polozhenii shchelochnykh
metallov v strukture berilla)
PERIODICAL: Geokhimiya, 1959, Nr 3. pp 278-281 (IISSR)
ABSTRACT: The position of alkalies in the lattice of beryl has
hitherto
not been explained. The alkali oxide content attains a
percentage of up to 7~23 %, Ingress into the channels of the
lattice and valence adjustment by aluminum in silicon position
(Ref 2) is not po3sible because in alkali beryls no increased
aluminum content is found, Replacement of 1 Be+ + by 2 Na+, K+ Li+
0
or Cs+ (Ref 3) is, seen from a crystallochemical point of view,
most improbable. To this the author expresses the opinion that
r:-.1ght-o-oordinated aluminum partly enters into the four-
coordinated beryllium places and that lithium and sodium take
the place.--.t -~;oordinated aluminum.; the other alkalies
entering the channels for value-adjustment. That Na in this
case may also enter for Al, may be seen f--ora the example of
Card 1/2 milarite, which has a similar struoture. For the purpose
of