SCIENTIFIC ABSTRACT BADAKVA, V. A. - BADALOV, S. T.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000102920020-5
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 6, 2000
• Sequence Number: 20
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

EADAKVA, V.A. (Bolokbovskiy rayon Tullskoy oblasti)
Work experience of the Teplinskii Rural District Hospital. Sov.
med. 26 no.8:147-149 Ag t62. (MIRA 15-.10)
(BOLOKHOVO DISTRICT-MEDICINEY RURAL)

BAPAKVAJ V,;A,
Inducing the active members of the Red Cross Society to assist
the medical personnel in a rural area. Zdrav.Roa.Feder. 6
no.10:24-26 0 162. (MRA 16W
1, Glavnyy vrach Teplinskoy uchastkovoy bolinitsy Tul'skoy
oblasti. (TUIA PROVINCE-RYb CROSS)

RADAL, Jan, inz.
Hysteresis loop measuring instruient, Sdel tech 11 no,6-.216-217
Je 163.

BADAL, Jan, MUDr.
Therapeutic use of gas from mineral springs. Sborn. lek. 58 no.
1:1-24 Jan 55.
1. Z Ustswu Williama Harve7e ve Frantiskovych Laznicb prednosta
MTJDr. Jan Badal.
(GASIS.
from mineral spriW of Frantiskovy Lazne In Czech.,
tber. use (Cs))
(MI 5MUL WATER,
gas from mineral springs of Frantiskovy Lazne in Czech..
tber. use (Cz))

USSR/ Farm Animals. Small Horned Stock.
Abs Jour: Ref Zhur-Biol-, No 9, 1958, 40464.
Author Badalbay-ay
Inst Not g ven.
Title The Karakul Breeding Sovkhozes of Uzbekistan.
Orig Pub: Karakulevodstvo i zverovodstvo, 1957, No 5,
38-43.
Abstract: No abstract.
Card 1/1 38

BADALCFV . A. [- ,
FoUoving the path of technological progress. Radio no.10.,13-15
o 161. (MM 34:10)
1. Nachallnik Glavnogo radioupravleniya, chlen kollegii Mnisterstva.
m7azi, SSSR. .(Radio) (Television)

BADALOV, A.L.
Radio and television for the Soviet people, Vest.sviazi ;,I
m.10-.&.8 0 161. (km 14:.10)
1. Nachallnik Glavnogo radioapravlaniya 14insterstva svyazi
SSSR.
(Radio) (Television)

BAnAT.M.-A-.
Seen and heard on the earth. -Radio no.11: " N 162.
(MIRA 15:12)
1. Nachallnik Glavnogo radioupravleniya Ministerstva,
svyazi SSSR.
(Astronautics)

BADALOV,, A.L
C:r"Ii- .
Develop. and improve means of 4iLdio communications., televIvion broadcastI4
and radfo broAdcasting. Vest. pJazi 23 nol:3-4-Js:"63.(MIHA 16:1)
P
I* Nachallnik Glavnogo radioupravleniya Ydnisterstva. svyazi SSSR,
(Radio) (Television)

BADALOV,.A.L.
Prinliples of the distribution of the radio frequenev spectrum
and of the drafting of plans for different radio services.
Elektrqsvyaz'. 19 no-31l-12 Mr 165.
(MIRA .18:5)

~".. 'iL Pz-6/fab ijp(c~ ATIJD
q
~AGGESSION :NR: AP5011793 UR/0249/65/021/001/0014/0018~ Z---
1: 0
....AUTHORS:- Isken'der-zade,:Z. A.; Abdullayev, G. B.; Dzbafarova,
A.; BadaloV, A. Z.
rrT.rrrrr V Tnve5tic-a+ion of the tranaient characteristics of the re-
2
f e
c')TT -D (I LI:
AN Az-r'.SSF. Doklady, v.
T-OPIC TAGS: sili-on diode, pn .4unction. transient characteristic,
resistance,
ABSTFJoCT: TI-je autL-iors investigated the effe2t of reversal of the bias
cn pn .4,-:nctl~ns ottalne~! t-v aluminum in n-rI
zvers as wa,
tj
r-e o f e
r-p C.- r,%rj 01" the inverse resistance '!-,e T~ie experimenta'
paperp
Card

L 59487-65
ACCESSION NR: AP-5011-193
rF. 7-~e conn--ct-!~,n t-etween theFz- an,j lifeti 'Fiec-
-arri-s, In v~rivi~; P;~rts of the anri t-~e oulse du-:-atiorl I's
F-AM -n-a~
--e b,~ a'
-a s r&.-,t
-- 11 K" 1, p-
T.
NR REF SOV: 006 Or--L.MR: 003
Clara

BADALOV,,,,,E..,T., aspirart.
Froi-ongation of the residual acticn of aca-ric-fdes. Vet~li:~In-arlf--4
42 no.5sI02-103 ~tv 165. (MI-RA lF.6')
1. Tadzhikskiy nauchno-issledovateltskiy veterinannyy iwstib-d~.

BADALOV, F.; SHIRIMULOV, T.
Calculation of the effect of local tangential and normal loads on
an inhomogeneous plate fastened at the bottom. Vop vych. mat. i
tekh. no.3:3-16 164, WRA 18:0,)

ACC NR: AP6023882 SOURCE CODE: UR/Oiog/66/oil/007/1336/1337
AUTHOR:' Abdullayev, G. B.; Dzhafarova,- E. A.; Badalov, A. Z.
Iskender-zade, Z. A.; Chelnokov, V. Ye.
ORG: none
-TITLE: Reactive properties of reverse-biased sUicon p-n JunW~ons
SOURCE: Radiotekhnika i elektronika, v. 11. no. 7. 1966, 1336-1337
TOPIC TAGS: semiconductor device, pn junction
ABSTRACT: The reactive properties of low-volt (6 v breakdown) p-n junctions
made from n-Si with a resistivity of 0. 03-0.05 ohm. cm were investigated.
Measurements were made at temperatures of -196-130C and at frequencies of
0. 4-600 kc. Plots of junction capacitance vs. reverse bias at room temperature,
for'5-100-200-400-600-kc, are shown. In the far -from -breakdown region, the
Card I /Z
UDC: 539.293.011.41
-- --- ---- -

ACC NR: AP6023882
capacitance is independent of the small-signal frequency and-decreases when the
bias voltage increases, approximately as C - Urg-V . Ija the breakdown region, at
lower frequencies, the capacitance rapidly increases with the bias vol tage; at
higher frequencies, the capacitance drops to zero and turns into inductance. A
.physical explanation is offered. Orig. art. has. I figure.
SUB CODE: 09 SUBM DATE: 0 IApr65 ORIG REF; 003
Cord ?,/2

V j,
A'_'rH'_S51C'N' A!-' Q
UMR: : Badalov
:A _____A~, (Aspirant)-
TITLE: The effect of high-temperature thermomechanical treatment on the structure
and pronerties of chrome-silicon steel
~.":Rcy: Moscow. Institut inzhenerov zheleznodorozhnego transporta, Trudy, no.
pov,,-sheniva ?od,?izhnogo so~-tava 1
% 7 i~ F
Ma C t: i n e r vpartE,
TOPIC ',AC;S: automatic coupling, ther-momechanical treatment, austenitic steel,
c'.rome silicon steel, steel heat treatment, -tee! hardening, steel mechanical
property, cotter pin
ABSTRACT: The author calls attention to the great importance of incTeasiris the
stre-.i!th of rqilr,)ad ~utcrmatic couplinq mechanisms. particilarlv c" the draw voke
r w e , - I n r eE- e a - r--:c" atten-o':! !-~as F.'ve~' t-"
'~R( of -"'c
C e n a z ec. " -D tz n t ,wh i C ha vl.~'
e d ~ ae IT!-: this connec,, served e plast!c de-
t ernpe r i:~g. tnat if in
for-mation of the austenite is effected at Emperatures higher than that of recrys-
Card 1/3

A(USSICIN \R: AT5i-10i-~lli,
f%-l-Ilz ;c
a F. 7
.0 2.11-

L 41570-65
ACCESSION NR: AT5009616
c,il testlni~ were pr,~pared by izrindinc. This studv derronstrated that the
5 " a 1)1 ~ncrua~,(: mechanical P--~,c7-ec of c-irmne-s..Lco-, steE 15
ar.l. Ias: -" figures.
ASSOC'LMON- Vsesovuznyy nauchno-issledovatel'skiy institut inzhenerov zhelez-
lic Rese,arc stif-ite for
x0scow 'A! 1
S:" B~-. i~ :1,-; s"ll B CC' DF 1
1,10 REF SOV: 004 OTHER: 000
lfx-L-
co,d 3 /3
ow:55-13 MR Imm, NO

f -estu-r~ o'; )t ~,-uc t.
0 F; C, tw x"t.ernotioz-ozmego trani"rtq, Trud no
-a iz ov e
r dc
7- r --z t ic coup! ing, thermomechanical tredtment, aurtenilic rteel.,
5 s t e c 1 hea-E treatm,en, , !~IeC har6enlng, s~ce~ mechzn~cal
I ~T RA T h - a r C a 8 at ten' ion 1 0 '~e grr-a importance nc reas --g r~-
f - , e
re r a,: a cmll t Ic co,.,p! ~mg ;:,art ic- lar
-!It" ICA -,.a t Ylt- wh ic 1 1 C C.:-, o 0 a 5 t C d r 0 r -.,.a
"t, iu-- pi~ i ~f,;g . in thiv connection, it is observed that if tht plastic de-
~'or=~it ivIn of the susten I tc is effected at ~trm?er;j!ures higher zlian that oP recrv5 -
I , 3

T
a
a on. 5 r-,r oc- r- s i s CA I I ed ra t u r e th e cha n c a r es t men t
or,
L ,yublin Casting and Mechanical Plant). Diagrams illustrating the microstructure

-,a C 5 C, -

L 36290-" 90(m)/EWP(k)lg/AIP(W)JEWP(t)/~tI IJP(c) JDAW
ACC Nib ARGO04031 SOURCE Colz I UR/0M/65/00Q/009/0W8/0W9
AVMRs Badalov F6 A*
TrMs The Influmme Qt blo taqwetwo thermcmechanical tmetawt an tho struot4we
and propert1w of abrow-aillem stool
.30URMs W. sh. Hashloostroltellove materialy, konstrulftil I rasebet detalqW
nwhin. Gidralwivod, Abs. 9JA.61
MW SOLTMRI Tr* Hooko In-ta laske vb.-d. transp. vyp. 1989 19669 67-69
TOA6 TAWs stools, ty 37KhS steelt 380S stool
proper
A
ABSTRACTs This Is a at the results obtained In an lurestigation of the
a
Inf2aence of- 4 anleall under two regimen on the mchanical proper-
ties of Steels 370S 3M5* regimen ares 1) heating to 1150C9 holding for
3~.T M
]W :0 a 0~
~E_j ~_vI2~
2 hours v a 2-5 oll.quenchIM; 2) austan1te famation. at 900C for
nahing
30 mint 5-7 hamer blowsp and oil
4~~ 9 The specimens were forsind an wedges
of a tension clevis for an autawtJ tor. After quesiching, smealJ In am-
0 t
dwt.ed at 200, .3Ws, 4Wp 500p and 6=9 A graph describing the Influme of aneal-
q.rA
Ing temperature on MW st"I a 9 inolu&4. Thersomachwdeal treatoset of
the d"crlb*4 ragim signifiraw-l-Wi0ves the uschardeal WOPWties of cr-81 steel
Bibllograpw of 4 tluese lon of an abs
tftc&7
SUB CD]Xs U
CWA 2A UDG 1 66golS1251792-194

i~;". I )!V. 0 V
vi-:rt r-il pi~p
7,o
lit.

-- BA L-A LOV I 'F w G I
Some data on diurnal vertical miff-rations of the zooplankton in
the Caspian Sea. Izv., AN Azerb. SSSR. Ser. biol. i med. nauk
no. 6: 67-73 ~ 63. (MTRA 17 -~ 5)

2EV46 3adplov, X. I.
Izyskanie o-otitall nulch parametrov otdelontya i anay'd volnkon dlya polucheniYEE
ravnomerno,v grebennoy lenty. M., 1954. 10s. 21 am. (14--vo vYsts. obra
zovanlya SSSR. Moak. tekstilInvy In-t). 100 Ekz- BesDl. - (54-5~;720)

BADALOV, K. I., Aspirant
"An Investigation of the Optimal Parameters of Cutting and Joining
Thread for Obtaining Uniform Combed Ribbon." Cand Tech Sci, Moscow Textile
Inst, 30 Dee 54. (V142 22 Dee 54)
Survey of Scientific and Technical Dissertations Defended at USSR
Higher Educational Inttitutions (12)
SO: SiLm. No . 556, 21,. Jun 55

BADALOV, K.I.
V-- 'U14or shortcoming in the design of combing machines. Izv. vys.
ucheb. zav.; takh.tekst.Drom. no.2:80-86 '58. (MIRA 11:5)
1. Moskovskiy tekstilinyy institut.
(Combing machinen)

BADAWV. K.I., kand.tekhn.nauk
Investigating the process of separating and joining on combing
machines, Tekst.prou. 18 n0-12:32-36 D 158. (MIRA 11-.12)
(Combing machines)

BADALOV, K.L, kand. tekhn. naukp ispolnyayushobiy obyazanno!!t-l dot-3en'-l
Some regularities in the distribution of the harmonic yarn
unevenness in sateen fabrics. Tekst. prom. 24 no.10.-36-39
0 1 id". (KM 17g!2)
1. Moskovskiy tekstillnvy Institut.

B,U)ALMT, K.T., kand. t-ek*,,n. na,6:, ob-,a;rannos-,4 rj a - s enta
Increasing the efficiency in he utidjzatic
t. u - -'r, cf rf,bon ~ApFers.
MrF , I tj~ L- I
Tekst. Prom. 25 no.7:25-30 J-1 165. ll;_ -.-:b)
1, Mloskovskiy luckstillryy inatitul"

BADALOIT, L.T.
Synthesis of the mediator in the axonal endings of an adrenatic
neuron. Fiziols, zhur. 51 no.5g572-577 MY 165.
(11MA 18g6)
1. Kafedra normaltnoy, fiziologii I Meditsinskogo instituta imeni
Pavlova, Leningrad.

--- L 34738-66-----
ACC NR: AP6025124 SOURCE CODE:
AUTHOR: RndalDal- ~'-I-
ORG: Department of Normal Physiology, Firrst-Med,ical-Institute P. Pa-viov,
L-ingrad (Kafedra nonnaltnoy fiziologii I Meditsinskogo instituta)
TME: Mechanism of the restoration of the adrenergic mediator reserves in axonal
endings
SOURCE: Fiziologicheskiy zhurnal SSSR, v. 52, no. 1, 1966, 29-33
TOPIC TAGS: dog, nerve fiber, muscle physiology, hormone, gland, drug effect,
neurology, animal physiology, nervous system drug
ABSTRACT: Investigations wore conducted to determine the' possibility of the
'9 smooth
restoration of excitation transmission by thoAyBqa�Jw1ic norveh
muscle halted as a result of the exhaustion of mediator reserves in.the axonal
"ndings by the administration of resorpino and the extirpation of the substan-;
tia medullaris of the supraronals, and the possibility of the restoration of
the reserves by noradronalin. Male dogs were usod in the oyperiments. The
right suparenal gland and the substantia modullaris of the loft suprarenal
gland were removed. The sympathetic innervation of the musculus retractor
penis was used as the object of investigation. On the sixth day after tho
initial operation the abdominal cavity was opened and the sympathetic post-
-816
Card 1/2 UDC:, 612,

L 34738-66 -'
ACC NR: 06025124
ganglionic nerve stem in the area of the small pelvis was isolated. The
nerves of the stem were crossed and placed on platinum electrodes. The
abdominal cavity was then closed. A second incision was mado in the perinoum
and the tendinous end of the musculus retractor penis was exposed and connected
with a recorder of a ldz~ematogriph. Resorpine was introduced into 6ne of
'the arteries at the root of the Pohis. The experiments established that the
extirpation of the substatia modulaaris of the suprarenals and the administration'
of reserpine halts the process of the transmission of excitation from the
adronorgic nerve to the smooth muscle, probably as a result of the exhaustion
.of the mediatoi- reserves; synapti'c transmission is usually restored about four
hours after the administration of the reserpine; restroation of synaptic
transmission is provented by the protracted stimulation of the sympathetic
motor nerve following the administration of the resorpino; noradrenalin in
small doses does not hasten the restoration of the synaptic transtrission of
exitation; In large doses, however, it restores neuromuscular transmission
of excitation almost immediately after its administration; apparently.tho
.axonal endings are capable of absorbing and ut-ilizing noradrenalin as a
mediator when it i~ present in the blood in large concentrations.' C~,ig. art.-
has: 4 figures and 1 table. [JPRS)
SUB CODE: 06 / SUBM DATE: 060ct64 ORIG REF; 006 / OTH REF: 007
Ca

L 05620-67 EWT(1)/LWT(m)/T/EWP(t)/ETI IJP((-) JD/AT
ACC NRs AP6624V�1 SOUR6E CODE: &iVo iRV661 6a/ oft/
AUTHOR: Badalov, M. V.; 4ayev, M. A.
~_ bite "o~si
ORG: Inst cs, AN AzSSR, Baku (Institut fiziki AN AzSSR)
TITLE: Phenomenon of secondary tunneling in 2aSb
SOURCE: Fizika tverdogo tela, v. 8, no. 7,"T966, 2218-2221
TOPIC TAGS: gallium compound., antimonide, volt ampere characteristic, tunnel diode,
pn junction, temperature dependence, semiconductor research
ABSTRACT: The authors investigated the volt-ampere characteristics of tunnel junctions
produced with p-GaSb as the basis., at diff t temperatures, for the purpose of ex-
plaining the nature of t1he secondax7 pe on the volt-ampere characteristic. Inverted
dioden were produced from single-crvst GaSb doped with zinc. The p-n junctions
were produced by fusing an alloy of qb% Sn plus 2% Te in vacuum. The volt-ampere char-
acteristics were plotted at the different temperatures using direct current and a null
method. The secondar7 peaks were observed in the voltage range 0.28 - 0.32 v at room
teniperature and are attributed to the presence of deep levels in the semiconductor, t
cauped by uncontrolled impurities and defects and allowing the carriers to tunnel
through the p-n junction. The observed temperature dependence of the position of the
.secondary peaks is attributed to the temperature dependence of the injection currentp
o
and~not to a possible influence of the residual resistance of the diode. The author
thanks G. B. Abdullayev for interest in the work and valuable remarks. Orig. art. has:
3 figures and 9 formu_lAe.
!
SUB CODE: 20/ SUBM DATE: 2.lDec65/ oRi(; REF: ooi/ oTH REF: oo5
Card i / i 4!x!AL

GUSIKOV, V.V... kand, tekhno' nauk; KUZIMENKO, V.A.p inzh.;
BADALOV, M.M 'inzh.
Selectilig optiiar parameters
i sel1khozm&8h.,'133,nojlOxl-4
for wheeled tractors. Trakt.
0 163. (MIRA 17:1)
1. TSentrallnyy nauchno-issi6dovatellskiy institut
mekhanizatsii"i--4-16ktrifi)ti~ttli 601'akogo khozyaystva
nechernozemnoy zony

BADALOV.. M.M., inzh.
Effect of the distribution of the vertical load over the
axles of a wheeled tractor on its traction efficiency. Trakt.
i seltkhozmash. 33 no.110-11 N 163. WRA 17.-9)
1. TSentrallnyy nauchno-issledovatellskiy institut makhanizataii
i alektrifikataii sel'skogo khozyaystva nechernozemnoy zony SSSR.

LUKIYANCBENKO., A.A.; BADALOV M.Ye KOINCHIDI, Ye.K.
Influence of southwestprn win#s onthe appearance and.spread of
tularenia~ in. the focus of' ths' fon Deltd6. Zhur. mikrobiol e~id
A immin. 32 n'o',115:55-01~.MY 161'0 (MRA
11 IZ.Roqtovskoy-ob~as-bxioy odnitarno-'eyidemLologicheskoy stantsii.
(DON RIVER-,-DELTA-TUIAREMIA (WINDS)

V
PHASE I DCOX BYPLOITATION SC-v/5i.jo
I(on 'Cron tolya Po *m1morml ispolizovaniyu atomno.-
tno Twhkent, 1959.
'Ilrai;~ictiono of the TarbIcent Confervnce on t.~O- lo,~cefxil
"Oneray) v. 2. Ta.-,hkQnt, 1950.
Errata slip inserted. 1,500 copies printu~
Agency: Alcademiya na-uk Uzbelczkoy SSR.
n---*,ble Fd. : S. V. Starodubtccv, Acadeiracian, Pcadcmy of
-3 Uzbek SSR. Editorial Poard: A. A. .bdullaycv,
-.tc -hy.~Ics and M th:~matic,31 D. 1.1. Abdur-,--~,.lov, -!',~Ctor
o f ta
;-',odUcal SicIcnees; U. A. J"XIfLov, toadcmLiclan, of
-c ci,.3 U~~bedk SSR; A. A. Dorodulina, Candleate of Dlolo-icLl
V. 11. Ivashev; G. S. okra, ,)va; A. YO. Kiv; Ife. !I.
Candl-late of 2hy0icz arld :~Iathe-zitics; A. 2:
of *,;,,,dlcal Sciences; D. Niz,*hanov, Candid.~-.e of kcal
-~ponding -~7"~bcr, Acwlc~n cf E~,.-cncen
cnce~: A. S. Sadykov, Corre . . Y
Academy of Sciencoa Uzbek SSSIR; Yu. N. lli;,~--,-min,

Traw-actiona of the TaMikent (Cont. SOK/51110
Candidate of Phypics and Mathematics; Ya, Kh. Turakulov, Doctor
of Blological S~tiences. Ed.: R. I. Mhamidov; Tech. Ed. ; A. G.
Babalchanova.
?U%"~,SE The r_ublVaticn is intcndcd for saientific vrcrkora and
cnploy,~d In entei-jrl.7Len wzh-re radicactive 1cotopes
and nuc3ear radiation are used fcr ra.ssarch in goo-
lcgica:, and technological fields.
001irRAGE: ".M= collection of 133 articleB represnnts the second
vol,-,7.e of the ~?ran_a~tions of the Ta,-hkcnt Gon'ertntc on the
Pea~eful Uses of Atomic EnerGy. The individuai art'_,:Iez deal
vith a wide range of problem,3 in the field ef nuc-'o-a- radiation,
in--~Iudlng: product'-cn and che-,7deal analy!zzls of ra~lca,-tivc
isotcpe3! Inveatigation of the kinetics of chemical reactions
by rreans"of isotc-pes; application of spec--tral analy3i '7 for the
manufacturing of radioactive preparations; radloa:tiye methods
for determining the content-of elements in the rocka; and an
analysis of methods for obtaining pure substances. Certain
Card 2/20

Transactlcn3 of the Tachlccnt (cont.) SOV/5410
instrum-onta uoed, such as aiitomatlo rc,-ulatora, floimetorn,
level E~,_u5cs, and high-nencitiv ar-ria-rolays, are doscribed.
Ity r
No porcOnalities are mentioned. References follow individual
articlc3.
TABLE OF CONTENTS:
RADIOACTIVE ISOTOPES AIM YUCLEAR RADIATION
331 ENG11TEEZINM AIM GEOLOGY
Lobanov, Ye. 17. [Institut yadernoy fizilki UzSSR - Institute of
Nuclear Ph,,'rsiea AS UzSSR1. Application of Radioaetive Isotopes
and Nuclear Radiation in Uzbekistan
Talcuar, I..:M., and V. A. Yanuahkovakiy (Inatitut fizilti. All Latv
SSR - Institute of Phynica AS Latvian SSR]. Problems.of the
Typification of Automatic-Control Apparatus Based on the Use of
Radioactivo Isotopes
Card 3/20

Transcetions of the Tashkent (Cont.) SOV/5410
Crob-,r, A. 0. [Tocntrallnyy n.-i. Inatitut Rh-bp]cox:oY prony-
sliDnnooti - Ccntral Scientific Roncnzch institute of the Cotton
indu-stry). Ap~plication'.of the Radioaotivo laotopea In the
Cotton Indualvx-f
Srapcnya1*.1V,-], R. A. jVaeooyuz-iyy n.-i. inatitut mckhanizatoii
aolls]-.oLp Ichozyaystva - All-Union Solo'ntific Rez;oarc)i Inntituto
for tho :-chanization of P.5ricuiturol- Radioactlvc.4'-:~thoda In
Zvaluati,ig the Operational rranlitica of Lotor Oils and Kacanas
and M. M. llmminov [UzbL-It State Univeraity I-mcni
-A. -111ai-ol]. Attmuation of Ov.:,aa-Raya,by Wool and Cotton
Va,,mshtayn, B. I., A. n. DreSer, and N. P. SyrInaz
fi7iko-ti~ldinicheoldy institut im. L. Ya. Knxpova - llhyzico-
technical Scientific Research Inatitute imni. L. Ya. Xazipovl.
Dczlon of a Radiation-Chemical Plant Ulith a FdGh-Pcuor S~vxcc
of Gazma.,~-Radiation for Converting Benzene Into Fenol by Oxida-
tion
Card 7/20
73
84
68
go

BADALOV, N.; MUNINOV, M.
Attenuation of gamna rays by wool and cotton. Trudy Uzou
no.117:4.1-44 162, (MRA 16:7)
(Shielding (Radiation))

S/048/r2/026/008/015/028
B104/B102
AUTEORS: _L3adal.ov, N. B., Vasilenko, S. S. , Kaganskiy, 111. G. , and
Kkm_~nskiy, D. L.
110'+
TTLE; positron spectrum
Ag
PERIODICAL: Alkademiya nauk SSSR. Izvestiya. Seriya fizichaskaya, v, 26;
no. a, 1962,1042 - 1045
TIE";T: The positron 4peotruin was studied using a double-focusing ~-spectro-'~'
me ter ,,,hich gave a relsolving polier of 1 . 80 at a- solid angle of 1 .2~~ of 4 K.
The Arlio", ic
source wa!:~jsupplied by thermal-neutron irradiation from metall':
silver of natural iso_~opic composition. Sources nf M - and -6 mg/cm2
tliicknesses were used.~, The spectrum mainly 00n8ittS Of POSitrons produced
in internal conversions giving f-quantum pairs with energies of 1380, 14Cq
1500, and 1560 kev. In the hard part of the spectrum, it was possible to
separate out positrons derived from transitions at 1780 and 1930 kev.
Transitions with energies of 1650 and 1880 kev arc supposed. The multi-
plicities of the most important transitions were determined from the ratio
of the pair conversion coefficient to the electron-conversion coefficient
Card 1/f 2

3/048/62/026/008/015/028
110x-
Af, positron
spectrum .
B100102
(Table 2). it is proved that the 1597-kev transition d6tected-by the
authors occurs to the ground state. There are 2 figures and 2 tables.
A'-~SOCIATION: Fiziko-tekhnich eskiy institut im. A. F. Ioffe Akademii -nauk
3jSR (Ph3rs'lcote chnical Institute imeni A. F. Ioffe of the
Academj of Scie nces USSR)
Table 2.
r, x 10-
Et H2 Ea Mt M2
kfjV
Z-0-1 z - 81 Z-O 1 Z-84- Z-0
1380 1,95 0, 94' 0*1 0
1 0,34 19
0, 2A
0,07
1480 2,64 1,46 0,82-i ~.~0,60 0,2T 0,42 0,10,
,
1600 2,80 1156 0,90 OjOB ,
9148 '- ,
060 3,2 1.,92 1,12, 0,80 0,42 0. 8D 0.22
'
1780 4,80 3,40 2,00- 1,52 0.82 1,08' 0,60
t0.30 5,98 4,46 2,72 2,00 1,20.. 1.,56 0,80-
Card 2

S/056/63/044/001/006/067
BlOB/BIQO
AUTHORSt Badalov, N. B. S. S., Kaganskiy C G.,
Vasilenkq
KarAinskiy* D..L.s Nikitin: M. K.
182
TITLEt Positron decay of Re
'PERIODICALs Zhurnal tksperimentallnoy i teoreticheskoy fiziki, 'v- 44,
no. 1 1963 35- -~-'40
TEM Two.rhenium isomerewiih.the half lives of 13 and 64 hr were ob-
181 182
n
tained in the.reaction.Ta ((xi3n)Re after chemical processi g (purifi-'
cation)of the reaction product.: These two isomers show positron emission
during their Re 182 -4 W182 decay) with intensities of (v3-1073 and 500 -6
positrons per decay event, for the short and long-lived: isomer, rOspeqtiYe-,*.'
1y. Analysis.of the p-spectr'um-.of the short-lived.isomer'by means of a
Permi graph showed two branches of P+-deoay with threshold energies of
0+ 20-kev and the relative intensities of 0. -3 and
550 +20.kev and 174 6q.10
1.8010-3 182 182
posi-trons per decay event. The total energy of the Re . --*W
transition is 2860 20' kev. This p'ositrons are due mainly to internal
Card 1/2

182 S/056/63/044/001/006/667
Positron decay of Re B108/B!80..
with pair-production:during the electromagnetic transitions
182 +
accompanying the electron oapture in Re . The low A -d:eeay intensity
of the long-lived isomer is attributed to X-forbiddenness.. There are
5 figures..
ASSOCIATION: Fizikc-tekhniches.kiy institut im. A,. F. Ioffe Akademii nauk
SSSR (Physiootechnical Institute imeni A. F, Ioffe of.the
Aoadeny or Soi6ndes USSR)
SUBMITTED.: June 29,, 1-062-1
Card 2/2

BADALOV N B,,, VASILENX09 S.S.; KAGANSKIr, M.G.; KAKNSKIY, D.L.
Internal conversion with pair formation in B1-82 decay, Izv,
AN SSSR.Ser.fis. 27 no.22258-259 F 163. (KRA 16s2)
il
1. Fiziko-tekhnicheskly institut im. A.F.Ioffe AN 5M.
(Internal conversion (Nuclear pbyp.~cs))
(Bromine isotopes-Decay)

BADAIDVI N.B.; VASILENKO,,-,. S.S.; KAGkOKIY, M.G.; XAMINSKIT, D.L.
Internal conversion with--:paiT formation in As76. Izv.AN SSSR.
Ser.fiz. 27 noo2t260-262 F 163. (MIRk 16s2)
1. Fiziko-tekhnicheskiy institut AN SSSR.
(Internal conversion (Nuclear pbysics))
(Arsenic isoiopes--Decay)

ARDULLAYEV, I.K.; BADALOV, N.G.
Effect of the leaf quality of commercial mulberry varieties on the
yield and technological indices of cocoons, Dokl.AN Azerb.SSR
17 no.11:1065-1068 '61. OURA 15:2)
1. Azerbaydzhanskiy nauchno-issledovatellsiciy institut
shelkovodstva.
(Azerbaijan--14ulbarr7--Varieties)

BADAU37 v 2.A.
Combined method for determining optimum drilling systems.
Trudy Azerb. ind. inst. no-17'.83-92 157. (MIPLA 11:9)
(Oil well drilling)

BADAIDV, R.A.
Curve indicating change in mechanical speed of well sinking
and its analytic expression. Izv. vys. ucheb. zav.; neft' i
gaz no-l.51-55 '58. (MIRA 11:8)
l.Azerbaydzhanaki7 industriallnyy institut im. M. Azizbokova.
(Boring)

B&DALOV.. -RA.
Kinetics of rock destruction when using roller bits. Izv.vys.
ucheb,zav.; neft' i gaz 1 no-10:35-40 '58. (MIRL 12:4)
(Oil well drilling)

BADALOV,. ILAk, '-
Basic indicators characterizing drilling processes. Izv.vYm-
uchob.zav.; neft' i gag 1 no-12:35-39 '58. (miu 12:4)
1. A2erbaydzbanakiy Industrial'nyy inatitut im. M.Azizbekovat
.(Oil well drilling)

BADALOV, R. A.
Determining basic drilling indices. Izv. vys. ucheb. 7a7.; n-3ft'
t gaz no. 5:35-41 158. (VIIRA 11:8)
1. Az'eriaydzhanskiy industriallnyy institut im. M.Azizbekove,
(Boring)

BADAWV,_A,A,,,-,
Kinematics and dynamics of tricone bits. Izv. vys. ucheb. zav.;
neft I gas no,8:37-,40 138. (MIRA 11:10)
leAzerbaydshanskly industriallnyy institnt im. M. Azizbekova.
(Boring machinery)

--,. RADkWV, R.A.
1
Dynamic biting of a tricone bit into rocks. Izv. vya. ucheb.
zav.; neft' i gaz 2 no.5:31-36 '59., (MIRA 12:8)
l.AzerbEqdzhanskiy institut pefti i khimii im. M. Azizbekova.
(Boring machiner7-)

BADkWV, R.A.
Ivaluating the efficiency of the performance of three-roller bits.
Izv. vys. ucheb. zav.; neft' i gat 2 no.10:19-25 .'59.
(MIRA 13:2)
l.Azerbaydzhanskiy institut nefti i khimii im. M. Azizbekova.
(Boring machinery)

&QUVI R.A
Determination of the mechanical drilling rate in relation to
drilling parameters. Izv. vys. ucheb. zav.; neft' i gaz 3
no.1:43-48 160. (MIRA 14:10)
1. Azerbaydzhanskiy institut nefti i kbimii. im. M. Azisbakova.
(Oil well drilling)

BADALOV, R.A.-
Problems of the dynamic interaction of a bit and a rock. Izv. vys.
ucheb. zav.; neft' i gaz 4 no-5:31-38 '61. (MIRA 15:2)
1. Azerbaydzhanskiy institut nefti i khimii in. M.Azizbekova.
(Oil well drilling)

..,BA4 - IRADALOV, S.T.
- - _V
", 1,- -4 R.P.
,,,,W
- 7~
'040:0.
Some results of the study on bydrotherml chalcedony containing
magnetite. Trudy SAGU no-39:65-67 '53. (MMA 10:5)
(Chalcedony) (Magnetite)

KOLESNIKOVA T.I.; NAZAROVA, V.D.; BADALOV, S.A., RADIONOV, K.G.; OSTAPENKO,
Ye.h., LEONTIYEV, Yia.N.
Using modified starch in case of drilling in salt-bearing sediments
in eastern Turkmenistan. Burenle no,7:20-22 t64. (MIRA 18:5)
1. Vsesoyuznyy nauchno-issledovatellskiy institut burovoy tekhniki
i kontora razvedochnogo bureniya No.5 tresta "Tarkmenneftegazrazvedka"o

Chemical Abst.
V01. 48 No. 5
Mar. 10, 1954
Mineralogical and Geologioal Chemistry
investiption of S. T. Bada-
Doklady Ak#.9911.11114 ff'.
0=
--~~--A detailed investigation was made of garnet taken
from pegmatite veins, including a completi chem. analysis.
By disregarding negligible anits. of pyrope and grossularite,
it Is possible to consider the cmnpn. of the mineral on them
btasis of manganic-ferrous compds. A beating curve was
made, and it sbowed 2 clearly defined exothemic effects.
Bone, at 500*. corresponds to oxidation of ferrims oxide.
The other, at W, rtfm to oxidation of manganous oxide.
Another Indication of oxidation was that, during beating.
the color of the mineral chang"I (mm light rose to china-
jw3j - Cmj~.j -A N

11 S S R
()t tOuf-m2fine
7 71, A 1, t;,,

am. russe sninkral.) 80, 212-13(l Wil ).- flat h V-braring
minerals are olpwrv"I in the contstri Yone of ",,4rtz vChn
with black V-cmlff. llmirts-Irmliblor garn (elm*. (I $
Tourmaline In thin brown newfim d, 3AAM. neg.. malattial,
I - 1AM * 0,1103. a - 1.111H 1 0,101, ) -,v - 0.10,
%ifoug lilrochroissn: -Offown. a light-almli.h. Client.
41141)-Nis: Si(h 37.73, DkO, 804. AlAh .3]A%, %',0. 5.71;,
N140 8-1)(1, PeO 0,82, NmrO 1.70, KO O.M. CaO 2.14.
IGO 1.67. arml F 0.13. The Vj(h rrIplams AlAh; the z-uy
diAgrain ispructic-AllyWesilk-Al mithibitollordinary fournu-
line. (2) (1 lurutt. in 6odecalinfira of 1.5 to 2 unn. diam.. of
dAtk-Ktcvu color, with strong ronal stcucture: dArk pvcu iii
the central, newly rolorlc-~ in [lie exterior tp4rE3,. of. 3-Ni;
1 - 1.741. Chrin. anafy*k: !;i0, 3P.M. A10, 111.3P.
;. LX', Feel"), 3.13. Cr,(l. 1.01. C.() 31.9n,aml MXO 3.X)
4
mursixPluling to 60.41, g"Sularite, 15.10 V-Kamtt (CaNg-
Si.0n, %ith 311% V.0.1, 11.05 o-volK. 10.01 Asultuditv, vind
3.35 uvinuvile. Spectral analpis shmAccl that the tfArk-
green central parts are partic-uLirly high in V and Cr.
Both minerals originate (rcxn A courn. of V front the bar-
founding mintry ruck (horulds) under postmagatatic s4ga.
condition,. W. Vitt-1

BADALOV., S. T.; CHEBOTAREV., G. M.j AND DUSMATOV, S. S.
IrInfluence of Medium on the Composition and Form of Calcite Crystals.,"
Dokl. AN UzSSRs No 3s 39-43s 1953 (Utbekistani resume)
The authors have studied the various crystalline forms of calcites
which occur under various geological and physicochemical conditions from
one of the deposits of Central Asia. The composition of the studied
calcites, their coloro specific gravity are due, up to a certain extent.,
to the composition of the containing rocks in which the crystallization
of the mineral occurs. The form of the calcite crystals almost does not
depend on their composition, but, in considerable degree, is due to the
peculiarities of the chemism of the medium in which they are formed.
RZhGeol, No 1. 1955

t~~: 1 j~ ~- . 6
BADAWY, R.P".... BAMWV~, S.T.
-
e
Sore results of the study on hydrotherval chalcedony containing
magnetite. Trudy SAGU no-39:65-67 153. (NLRA 10:5)
(Chalcedony) (Magnetite)

BADAIA)V, S.T.; ISKiIIOV, M.
Form of occurence of copper in alunit4.' Trudy SAGU no.52:35-38
'54. (KLRA 10:5)
(Alunite)

VOROBIYEV, A. L., AND BADALOV, S. T.
Data on HemUWdrate
The authors distinguish the folla-ring genetic types of deposits of
hemihydrate, hemihydrates of sedimentary origin (in marine and lake-
brackish deposits); hemihydrates formed in soil imder desert conditions
in gypsum-thenardites, carbonate, and halide saliniferous crustations;
hemihydrates formed during the dehydration of gypsum on the surface
yields or under the action of sulfuric acid in sulfur deposits; hemI17-
drates formed during hydration of sedimentary or hydrothermal annydrite;
hemihydrates as intermediate variety in the transition of gypsum into
anhydrite at great depts. Deciphering of the Debye-grams and thermo-
grams of the hemi W rates Indicate the presence in them of admixtures of
gypsum and anhydrite. (RZhGeol. No. 5, 1955) Tr. S=dneaz. un-ta. Geol
n., hk.- 5, 1954, 29-34
SO: Stun. No. 744, 8 Dee 55 - Supplementary Survey of Soviet Scientific
Abstracts (17)

1,`Occurrence 61 drolhUtinal h
nadalf'v ntLin
S so Ccntzai ASN.
A
PC jar
paraget:e',,
phaltrite, 1)) r Nli I
-r,'tt: ell nnhy,l
Is Ob!,cMd ki vc-' COP3,rite g'J' I(e with tclurmalillc%
tilau t. "Is M whicl, t1)(' 114, lblarit'-' arld '~
Ile stAlfidt: - ! all Acif(v
S)'Cuite 11111ILT-111 V 15 dkIinctly old'.r
car hel
hav- clicuigt-d
PsIll't even li"Wil to deptil's of rit, 10
is i.-of"t DO In_ but tiliq 1,
e and Old), a ftw
are not Cluillifed t III. I., VIII. d"cl); tilt: glIr"i"
hIf
Yrite cry- S, le Suillevi"
9e kin how I,Ih h-'It rt-cidish
a p
I"I" er-f-l"Ma I r -10 I-t all.
I q "" OTI the
OP ka 3
t11
PU T1 (
0Intl 11
analpliq pI 11,570,
OkV V Mhatt,,lbli,
(p
4)00
z? Ba Cu. ],'a
So
trVice olp to-0'0'cZ)' Pb
S ra on the C, pyrite AN (about
I V-4
is hlgh"Iyt" Oe't, Of Pyrite a zil ge P.... -~,rp sluall Mnta-
on the w'restill.. gren 41WPJ'rit~e - Onflydrite
their al"S of t.." - ell t III the at I , or
dl~.Jr e anhydri ourmajille I 13'arite
41_ te Ve"'S and III, Observe
f d
is Oulid

W.0044 6
USSR/ Geo.Logy Central Asia
Pub 46 10/21
Authors a Badalov, S. T.
-Title
-Ww-iata about the hydrothermal anhydrite of Central Asia
Periodical t Izv. AN SSM. Ser. geol. 1, 114-117, Jran-Feb 1955
Abstract i The author pro sents da'ta obtained -from the study of anhydrites
in Central Asia, relating to their chemical composition, for which
he gives the results of the analysis of 9 specimens, the manne~r
in which the veins of the different minerals are arranged with
respect to each other, thedepths at which they are found, and
the relative order of their formation. Fourteen references: 13 USSR
and I USA (1935-1953)- Table.
~Vlstitution t
Submitted t Varch 10, 19-54

Vr

15-1957-3-3078
1
Translation from: Referativnyy zhurnal, Geologiya, 19517, Nr 3,
p 93 (USSR)
AUTHOR:
TITLE:
PERIODICAL:
ABSTRACT:
Card 1/2
Badalov, S. T.
The Origin of Calamine (0 gerTezise kalamina)
Zap. Uzbekist. otd. Vs9s. mineralog. o-va, 1955,
Nr 8, pp 161-165
During study of a polymetal deposit, it was dis-
covered that Zn occurs principally as calamine in
the zone of oxidation. The crystals have an
elongated tabular form and vary widely in size,
from 0.01 mm to 2 to 3 mm and even to 5 to 6 mm
in length, up to 3 to 4 mm in width, and up to 1
to 2 mm in thickness. Of the simple forms, the
pinacoids ZTOY and LZly, the prisms f3_027and
Z93117, the rhombic prism Jig, and the basal
pinacoid ZUO!7 were ident1fied. The calamine is

15-1957-10-14073
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 10,
p 109 (USSR)
AUTHOR: Badalov S. To
TITLE:. Some Results of the Study of Hydrothermal Helvite
(Nekotoryye rezul'taty izucheniya gidrotermallnogo
'
llvina)
ge
PERIODICAL: Zap. Uzbekist. otd. Vses. mineralog. o-va, 1956, Nap 10,
pp 59-67
ABSTRACT: The paper presents some of the results of the mineral-
geochemical investigations of helvite of hydxvthermal~_
origin. Six different types of helvite occurrences were
identified. 1) Polym6tal vein stockworks, consisting of
sphalerite, galena, and helvite. Very frequently the
helvite is included in coarse crystals of sphalerite. 2)
Quartz-helvite mineralization with pyrite, in zones of
crushing among the pblymetal ores. The helvite occurs
around ore fra-gments, which serve as centers
of crystal-
Card 1/2 ,
lization. Quartz mineralization occurred in several

15-195 7-10_1407~
Some Results of the Study of Hydrothermal Helvite
stages, the last of which is barren everywhere. 3) Calcite-
amethyst-helvite vein stockworks. The helvite forms bands be-
tween calcite and amethyst. This relationship indicates a sharp
change in the composition of the hydrothermal solutions; at this
stage it now contains sulphurous sulfur. 4) Helvite mineraliza-
~~on in tectonic zones containing tale. Here also the helvite
occurs in ore breccia, ce *mented by talc. The helvite crystals
have normal terminations and crumble easily. 5) quartz-ohalce-
dony-helvite mineralization in zones of crushing. The helvite
occurs in quartz, chalcedony, and tale. 6) HelVite mineraliza-
tion in chalcedonic forn~ations which contain almost all the ore
minerals characteristic of the polymetal mineralization. The
types of helvite occurrences listed are principally.4;qattpBuish-
ed by the accompanying minerals. They are all younger the
chief stage,of polymetal mineralization.
Card 2/2 K. N. Ryabicheya

7.-
USSR/ CoqmochemLLstry. GeocheM18try. Hydrochemistry
I
Abs Jour : Referat Zhur - Xhimiya, No 40 1957, 115o4
Author : Badalov S.T.
Inst : rmhtitute of Geology, Academy of Sciences Uzbek SSR
Title : Data on Geochemistry of Vanadium
Orig Pub Tr. In-ts, geol. AN UzSSR,, 1956, No lp-, 65-73
Abstract Spectral analyses were made of more than 34 specimens of minerals of
eruptdve and sedimentary-metamorphi.6 rocks of a Central Asian district.
The district is formed by a meta6orphic sandstone-shist Upper Silurian
series with faults of granitoidrocks of Varissian.gge. Coefficient of
Vconcentration (V content in granodiorites is taken as the unit) is wi-
thin the following limitsl in contacit-metamorphic rocks 10-500; grani-
tes, quartz-diorites, la~rophyres and others,/ 1-10; biotites 4 1-250;
im, covites 1-10, garnets, toiirmaliniis and-othei minerals 4 1-3000. The
principal source of V aie black quarti-graphite hornstones proauced as
a result of contact metasoliato's'Ls'from-sedime:ntary-bitumiiious vanadium
containing rocks~ Accumulation of V took place in'a reducing niedlum
during deposition of organic matterj~,vhich was converted into quartz-
1/2
D.

USSR/ Co~m6chemistry. Geochemistry. Hydrochemistry
Abs Jour : Referat Zhur - Xhimiya, No 4, 19,;6, 115o4
0
D.
graphite hormstone during subsequent processes of metamorphism. Almost
all the intrusion assimilated V is concentrated primarily in biotite and
partially in iiuscovite, and as a rule is not concentrated in any of the
subsequent pha,46s, except small hydrothermal Yeins, which contain at si-
tes of their, passage'through hornstone rare V-bearing minerals: roscoe-
lite, tourmiline, garnet etc.
2/2

T
15-57-7-9407
Translation from: -Referativnyy zhurnal, Geologiya, 1957, Nr 7,
pp 96-97 (USSR)
AUTHOR: Badalov,
TITLE: New Data on Thaumasite From Central Asia (Novyye
dannyye o taumasite iz Sredney Azii)
PERIODICAL: Tr. Sredneaz. un-ta, 1956, Nr 82, pp 19-24
ABSTRACT: The rare mineral thaumasite has been discovered in
lead-zinc deposits in the Kuraminskiy Mountains,
where it forms veins and networks in the host rocks.
Dark thaumasite of an earlier generation is cut by
veinlets of white thaumasite. The early thaumasite
is characterized by near-vein alteration and calcium
metasomatism, whereas the boundaries between the later
thaumasite and the host rock are sharp, and no meta-
somatism is present. The luster of the thaumasite is
Card 1/2 silky (in the fibrous varieties) to dull (in the fine-
I &

15-57-7-9407
New Data on Thaumasite (Cont.)
grained varieties). The hardness is 3, the specific gravity 1.901.
The indices of refraction are Ng 1.508 and Np 1.469. The chemical
composition is Si02 10.38 percent, CaO 26.40 percent, MgO 0.47 per-
cent, S03 12.55 percent, C02 7.33 percent, H20 42.87 percent. Two
effects are observed on the thermal curves: an endothermic effect
from between 800 and 1000 to 3000 (loss Bf water) and an exothermic
effect from between 6000 and 7000 to 800 (formation of Ca2SiO4).
Very weak exothermic effects on one thermal curve (at 8900 and 11200)
aj~e associated with the formation of free CaS94. The elimination
Of C02 occurs gradually and is not reflected in the thermal curves.
X-ray studies of thaumasite and its roasting by-products verified
the formation of Ca2SiO and CaS04. The author concludes that the
thaumasite is of hydrotkermal origin, with surface solutions con-
tributing in part. The presence of this mineral indicates the cul-
mination of an ore process the earlier stages of which should invari-
ably be accompanied by the separation of anhydrite and calcite.
Card 2/2 V. A. Voroblyeva

a&6 P. L. Prikhld 7-psii
hr- Omompd. a=d
tranu.
Ir thkkzrss are dc,
in the -c"d~"allthhr '3
Th thl=hOliti
1,11 14 06. Cc 5,?1. Fe
a disffict 10"
4 7g k, 70 49.

RADAIOV, B.T.
Study of tin-bearing garnet veins. Dokl. AN Uz. SSR n0-7:17-21
157. (MIRA 11:5)
I.Inatitut geologli AN UzSSR. Predstavleno akademikom AN UzSSR
A.S. Uklonskim.
(Garnet) (Tin ores)

BADAWV, S.T.; GOWVANOV, I.M,
Birunite, a new mineral in the thaumasite group. Dokl. AN Uz.
SSR no.12:17-21 157. (MMA 11:5)
l.Institut geologii AN UzSSR. Rredstavleno akad. AN UzSSR A.S.
Uklonskim.
Mbeldstan-Thaumasits)

RUUWV, S.T.
Paragenesis of sylvivits from the Almalyk Mountain. Uzb. gaol.
zhur. no.4:67-72 '58. ()URA 13:2)
I.Institut geologii AN Uzbekskoy SSR.
(Almalyk Mountain-Sylvinite)

BAMLOV, S.T.; RUDE&TOV, S.
, %. (Ionesis Of postorganic orthoclase m7stals, Dold~ AIF Ux, SSR no -5:
0
9-12 1580 (xm lit8)
s
is Institut.90010911 AN UESS, Predstavleno akadeldimm A]F UxSjM
AA. Uklonskin.
(Al.ml*--Peldepar)

IADALOV, B.T. __
Pyrochroite, zinc-bearing serpentine, and auophane from the
Alma~yk deposit (the Uzbek S.S.R.). Zap. Vsss. min. ob-va 87
no.6:698-701 '58. (MI]RA 12:3)
(Almalft region --Ore deposits)

AUTHORS: Badalov, S. T., Golovanov, 1. 1A., SOV/20-121-5-36/50
'-XFo_'zhatelev-, B. L.
TITLE",: A Monticellite Skarn From Central Asia (,',Iontichellitovyy
skarn iz Srodney Azii)
PER10DICAL: Doklady Akademii nauk SSSR, 1958, Vol. 121, Nr 5,
PP. 897-900 (USSR)
ABSTRACT: Idonticellite, sperrite, and melilite have been known in Cen-
tral Asia (3rednyaya Aziya) since 1950. The former forms in
all known cases both alone and also with the comDlex of its
paragenetic minerals (of the two last-mentioned ones) con-
siderable accumulations of metamorphosed minerals which are
bound to the contact zone between eruptive and carbonate
rocks. Table I shows the physical properties of monticellite
from Gavasay (Namangan area, Uzbek:.- SSR = Namanganskaya
oblast', Uzbekskaya SSR) and from Almalyk. The latter forms
small roundish grains of 0,1 to 1 mm of size, without crys-
't alline shape; the monticellite grains from Gavasay are an-
gular, of irregular shape, up to 0,1 mm of size. Table 2 shows
Card 1/3 chemical analyses with a conversion to mineral components to-

A i'Monticellite Skarn From Central Asia
Card 2/3
SOV/20-121-5-36/50
gether with comparing data from other sites. The first au-
thor took a radiogram in the Radiometric Latoratory of the
Institute of Geology of the AS, Uzbek'. SSR (Institut
geologii Akademii nauk UzbSSR). Table 3 shows the results of
his interpretation. They confirmed the composition of the min-
eral as monticellite from Almalyk. Moreover, sperrite is
found in the skarn from Gavasay. It forms crystals of 0,05 to
0,1 mm of size, of irregular shape, which develop at the cost
of the monticellite grains. The mineral of the melilite group
forms small angular crystals which often have an almost square
cross-section. The formation of the monticellite-skarn is
genetically bound to the contact-zone between eruptive rocks
of middle to basic composition and to dolomites (Almalyk) or
dollomitized lime (Gavasay). Here, like elsewhere, the process
has taken place under the participation of postmagmatic solu-
tions (Ref 6). It follows from table 4 that C02-gas escaped
during the formation of monticellite skarn and that kiesel-
guhr penetrated into the solution.
There are 4 figures, I table, and 12 references, 10 of which
are Soviet.

A Monticellite Skarn From Central Asia SJV/20-121-5-36/50
ASSCCII-:--j'N: Institut geologii Ak--demii nauk UzSSR Onstitute of Geolog,,-,
.11 . -6
A~'-', TJ z b e k *33R)
PIIE3~'NT-'-'D: April 9, 1Q58, By D. S. Korzhinskiy, Member, Academy of
Sciences, USSR
SU3MITTi*-.D-. April 5, 1958
Card -5/3

BADALOV, S.T.; RA.MY14VA, E.Ye.-, SUROVKIII, V.14.
Comparative method for obtaining thermograms. Uzbgeol.zhiir.
no..2:90-93 159. 14M 12:8)
1. Institut geologii AN UzSSR i SAIGIMS.
(Rocks--Thermal properties)

3(8) SOV/7-59-4-4/9
AUTHORS: Badalov, S. T., Yenikeyev, M. R.
TITM '_---0n-VFe ~Geochemistry of Cadmium in the Almalyk and Altyn-Topkan
Ore Deposits of Karamazar (K geokhimii kadmiya v Almalykskom
i Altyn-Topkanskom rudilykh polyakh Karamazara)
PERIODICAL: Geokhimiya, 1959, Nr 4, pp 328 - 335 (USSR)
ABSTRACT: The cadmium tenor were determined by V. A. Moskvitina, P. L~
Prikhidlko and V. V. Prasalova polarographically and chemi-
cally in the laboratory of the trust Uzgeolrazvedka, and
in the laboratory of the Institut geologii AN UzOSR (Institute
of Geology AS UzSSR). Further comparison values from other
deposits of the USSR and foreign countries were used. The in-
vestigations give the following data: Cadmium tenor in zinc
blendes of the copper-molybdenum mineralization of Almalyk
Table 1), cadmium tenor in zinc blendes of other deposits
Table 2), cadmium and iron tenor in zinc blendes in the
~
polymetallic mineralization of Zapadnyy Karamazar and com-
parison values from other districts of the USSR (Table 3);
cadmium tenor in tetrahedrites of Karamazar and Rudnyy Altay
Card 1/2 (Table 4), cadmium tenor in minerals of the oxidation zone

On the Geochemistry of Cadmium in the Almalyk and SOV/7-59-4-4/9
and Altyn-Topkan Ore Deposits of Karamazar
(Table 5). From this the following results.- Under hypogene
conditions cadmium is enriched in zinc blendes, leas in zinc
tetrahedrite; with decreasing temperature the cadmium tenor
of the zinc blendes increases. The cadmium tenor does not
depend there so much on the iron tenor of the zinc blendes
as on the type of the deposit and the paragenesis, The com-
paratively high cadmium tenor of the zinc tetrahedrite8 has
hitherto not been considered; an investigation of other sul-
fidic zinc ores, such as chalcopyrite, bornite, cnargite, and
others would be desirable in this connection. In the oxidation
zone cadmium is found in the smithsonite and in minute quan--
tities in the calcite. In other zinc minerals cadmium is
practically not found. There are 5 tables and 24 references,
20 of which are Soviet.
ASSOCIATION: Institut geologii AN UzSSR i Sredneaziatskiy gosudarstvennyy
universitet im. V. 1. Lenina (Institute of Geology AS UzSSR
and (Soviet)Central Asia State University im-eni V. 1. Lenin)
SUBMITTED: January 10, 1956
Card 2/2

KoRoLEv, A.V.; BADAWY, S.T.
-Primary zoning in the mineralization Of thb Almalyk ore deposit.
Geol. rud. mostorozh. no.5:31-38 S-0 '59. (MIRA 13:2)
l.Inatitut geologii AN UzSSR, Tashkent.
(Almalyk region--Ore deposits)

Comparative study of chalcopyrite and molybdenum from
Kara-Mazar ore deposits. Zap.Uz.otd.V9es.mln.ob-va
n6-13:52-61 159- (MIRA 13:7)
(Kara-liazar Mountains-Ghalcopyrite)
(Kara-Mazar Mountains-Molybdenum)

IV.
PHASE I BOOK EXFLOITATIOIN SOV/5740
Akademiya nauk SSSR. Institut mineralogii.. geokhimii i kristallokbimli redkikh
elementov
Voprosy mineralogii, geolchboli i genezisa mestorozhdeniy redkikh elementov
(Problems in Mineralogyj, Geochemistry., and Deposit Formation of Rare Elements)
Moscow, Izd-vo AN SSSR., 1960. 253 P. (Series: Its: Trudy., vyp. 4) Errata
printed on the inside of back cover. 2,200 copies printed.
Chief Ed.: K. A. Vlasov,, Corresponding Member, Academy of Sciences USSR;
Resp. Ed.: V. V. Lyakhovich; Ed. of Publishing House: L. S. Tarasov;
Tech. Ed.: P. S. Kashina.
PURPOSE: This book is intended for geologists., mineralogists., and petrographers.
COVERAGE: This is a collection of 23 articles on the formation,, geology.,
mineralogy., petrography, and geochemistry of deposits of rare elements in
Siberia and (Soviet] Central Asia, The distribution and characteristics of
rare elements found in these areas as well as some quantitative and qualitat-
tive methods of investiga;+.ing the rocks and minerals in which they are found,
Card 1/6

Problems in Mineralogy (Cont.)
SOV/5740
or vith vhich they are associated, are discussed. Two articles present an economic
investigation of the possibilities of industrial extraction and utilization of
celenium., tellurium., and hafnium. No personalities are mentioned. Each article
is accompanied by references.
TANZ OF COMUUS:
GEOCHEKL9TRY
Garmash.. A. A. Peculiarities in the Distribution of Rare Elements
in Polymetallic Deposits of the Zmeinogorsk Region of Rudnyy Altay 3
Semenov,, Ye. 1. On the Content of Lithium and Rubidium in Minerals
of Alkaline Pegmatites of the LovozersIdy Massif 20
Badalov., S, T.., and S. Ruzmatov. On the Geochemistry of Selenium and
Te . Ore Deposits of Almlyk 24
Gorokhova, V. N. On the Content of Rhenium in Molybdenites of the
Kadzb,aran Copper-Holybdenum Deposits 28
Card p/6

Problems in Mineralogy (Cont.) SOV/5740
MENERALOGr ARD FETROaRAPHY
Yeelkova., Ye. M.., and 1. 1. Nazarenko. Pyrochlore of the Vishnevyye
Xowtains,, Its Paragenetic Associations, and the Peculiarities of Its
Chemical Composition 33
Zhabin, A. G.., G. N. Mukh'tdinor., and M. Ye. Kazakova. Paragenetic
Associations of Accessory Minerals of Rare Elements in Exocontact
Fenitized Xiascite Intrusive Rocks of the Vishnevyye Mountains 51
Zhabin, A. G. On the Separation Time of the Minerals Niobium, Zirconium,
and the Rare Earths in the'Granite Pegmatite of the BlyumovalLaya. Mime 74
Semenov, Te. 1. Gelzircoauln in Alkaline Pegmatites 85
Mork'n. V. I.., Yu. A. Pyatenko., and A. V. Bykova. On Britholite of the
Alkaline Rocks of SoutheAstern Tuva 90
Card 3/ 6

Problems In Xineralogy (Cont.)
SOV/5740
LyakbovIch.9 V, V,t and A, D. Chervinskaya. On the Character of the
Distribution of Accessory Minerale In Granite Xassifs 94
Lyakhovich,, V, V,0 and V, 1, Noneshnikors, On the Effect of Late
Processes on the Content of Accessory Xinerals In Granitolds no
Ivanors V, V,j, and 0. Te, Yushko-Zakharova, Discovery of Francksits
in Yakatlya 131
Zuyev., V, R.,, an& A, V. Kosterias Yttrofluorite From tbo D~*I%~ of
[Soviet] Central Asia 136
Podporina;, Y*, K, Crystallagrapbic Form of Celestins From the
Oulisayakiye Deposits of Strontium In the TadzWkskays, 61IR 139
030LON AND OMM33 OF TM DEPOSITS OF RM ELM=
Ku ImMo X, V. Genetic Types of Deposits and Ore Manifestation@
of Nioblum and Tantalum 142
card 4/6