SCIENTIFIC ABSTRACT BETHER, G. - BETINA, V.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000205120015-5
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 8, 2000
• Sequence Number: 15
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

BETGEER, YE. K.
"Nm Data on the Collection "Turkestanakiy Sbornik*
Izv. AN U(s. SSR., No 3., 123-125,, 1953
"Turkestanskiy Sbornik" represents a symposium of monographs
and articles
relating to Central Asia in general and to Turkestanskiy Kray
in particular.
It is a unique collection of printed material clippings from
gazettes,,
journals, and books on prerevolutionary, Turkestan; it totals
594 volumes.,
of which 416 volumes gathered V. 1. Vezhov cover the years
1867-1887 and
the remaining volumes were prepared in 1907-1916 and 1939.
Howeverj, this
collection cannot pretend to be complete. (RZhGeol, No 3, 1954)
SO: W-31187., 8 Mar 55

BITHER, Georg Dr.
-- ; - ~ ~ .I --4
Practical manual for determination of chemical
composition of
water. Bibl.Hig.inst.Srbije no.3:1-81 '53.
(WATER,
determ. of chem.c6mposition, practical manual
(Sar))
(CHMICAL ANALTSIS
of water, practical usuml (Ser))

B!-ff i i G E. w Q141-- 5
7
.~ilmonar7 thrombombolism accord'-rig ti the
aiitops~ of
,ne of Pathological Ahatomy of the
of Medidne in Zabrze. ?at. Pol. 1.5 no.4t527-533 ~j
T. Z Zakladu Anatmit Patologlumej Slaskiej
Akadi-mi. Vecy~:~znnj
w Ziabrzu (Kierownllc: prof. dr. m~-,d. W%
Niepulomekl).

6ETHKal
On the action of promotors chemically related to e
car-
ri6r., Alfons L;rau5e. ennn lipthl-e- and Aniela C
lk6xvnq
Poznafi, Polandy.-IM5ffffOem. 32, 409-1 1958)
ig~ an summary); cf. C.A. 51, M .Ile in-
hibitors in the catalytV action of CuO on the=ecomp~.
Th~ action of Ain 2L7jn the catalytic jacStijyjj)jcf
MnO3 is
similar. The -Ei-gFacti%,ity-o-r"M-e-Ftr-nary
catalyst, com-
posed of Fe, Cu. and Mg hydroxides (Fe:Cu:Mg - 1:0.3:
0.22) (1), which is the ideal model of respiration
enzyme
(C-4. 33, 32837), Is increased upon addn. of
identical ions.
The content of a given compontilt does not play the
main
role in the activity. These facts indicate that an
exchange
reaction should take place even between identicalvoms
leading to active or inactive complex compds WO --f
acts
jj ?n I as a strong inhibitor in the HCOOR oxi&tan- '
.Tt not
in the HA decompa. On the other hand.Al++-' n-1hibits
the action of I In the Hj% decompn. but not
In_tFFHCOOR
, oxidation. A. KrcglewskL-
Y

!YETI, I~al, dr., a tudc,-.ianyo? kalirl -1 1
I N I _uu-- -
_ -
'.. .I~
Up-to-date rat-orial tostlin.g. Toc-.hnll:a r no.10:(.7
C, " 4.

BETIKOVY I., inzh.; ELIVZON, M., kand.tekhn.nauk
Agloporitoo used in rural construction. Sell. stroi.
Li.e.16) no.3:
24-25 Mr '62. (MIRA 15:7)
(Aggregates (Building materials))

TILINOV, A.M., inzh.; CIIERVOCHKIN-, O.A., inzh.;
RETIKOV, I.Ye., inzh.
Heat insulating blocks of agloporites. Stroi.mat. 8
no,1;27-.28
Ja 162. (~aRA 15:5)
(Insulating materials)

BETIKOV.,.. ~.Ye. , inzh.
Study of-the kinetics of liquid phase in the
production of
agloporites based on the electric conductivity of
clinkeri
charges. Stroi. mat. 9 no.6234-36 Je 163. (MIRA
17:81

ARKIIIPOV, N.I.; BETIKOV, I.Ye.
------------
Mixer-granulator of clay rav mater-lah? for the
production
O-P agloporite. Stroi. mat. U no. 12:31 D '65. (MIRA
18:,2)
I A~
1. OLiv-.nyy In",hewr Lah:)vator.ij strAtv]Inykh
matorialev
Nauchno.-Issiedovatellskogo Instituta sell3ko.go
6troitellstvr
(for Arkhipov). 2. Direktor Tuchkovskogo
eksperimentaitnogo
pi-edpriyatlya Vsesoyuznoao nauchno-issledavatellskogo
instituta
navykh stroitedInykh materialov Akademli stroitel'stva
i
arkbitaktury SSSR.

eer ~-'- /,,/ 9 - /!//, -
PHASE I TREASURE ISIAND BIBLIOGRAPHICAL REPORT AID 296 - I
BOOK
Author: BETIN B. M.
Full Title: ~4~~ANSMITTING EQUIPMENT
Transliterated Title: Radioperedayushchiye
Publishing Data
Originating Agency: None
Publishing House: State Publishing House
Date: 1951 No. pp.: "0
Editorial Staff
Call No.: AF545388
ustroystva
for Energetics
No. of copies: 10,000
Editor: S. S. Arshinov Tech. Ed.: None
Editor-in-Chief: None Appraisers: None
Others: The author aelmowledges the cooperation of B. A. Smirenin
and
S. S. Arshinov who wrote paragraphs 1-3p 7-2# 11-3, 15-4, P-2, the
text on thermal compensation, and in addition, developed the prob-
lems of energy relationships in connection with amplitude
modulation.
Appreolation is also expressed to the following instructors of the
Gorkiy Radio Tekhnikum: V. A. Alyavdin, V. A. Min1kov, A. Kh.
Khitrin,
L. A. 11-brugin, L. T. Shnudeyko, etc.
Text Data
Coverage: The text deals with the theory and analysis involved in
the design and
production of low- and medium-power transmitters. The discussion
in-
cludes a brief treatment of UBF and SH? oscillators with general
descrip-

Radioperadayushchiye ustroystva. AID 296 - I
tion of lighthouBe, reflex klystron, and magnetron tube
circuits.
The approach is theoretical and analytical, supplemented by
diagrams
and formulas. The basic aspects are illustrated in detail by
many
examples. The book is actually a survey and a deeper
exposition would
have required supplementary theoretical material.
TABLE OF CONTENTS- Chapter I Development of Radio Transmitting
Equipment.
2 Basic Theory of High-frequency Power Amplifiers.
3 Energy, Relationships in Power Amplifiers.
4 & 5 Circuits and Analysis of Power Amplifiers.
6 Parasities in Amplifiers.
7 Ultra-short Wave Power Amplifiers.
3 Output Transformers.
9 Intermediate-frequenoy Amplifiers.
10 & 11 Generators (Self-excited, Ultra-short Wave, etc.).
n 12 Frequency Stabilization.
"13,14 & 15 Amplitude Modulation. (Plate, Grid, etc.).
16 Frequency and Phase Modulation.
17 Radio Telegraphy.
18 Pulse Operation.
19 Problems.
2/3

BITIN. Boris.Kikh&ylovich;,KOKUSHKIN, A.A.. redaktor;
FMKIN, A.M..
-.- tekhnicheakiy r*daktor
[Radio transmitters; theory and practice]
Rodioperadaiushchle ustrel-
stva; teoriis, i raschet. Moskva. Gos. energ. izd-vo,
1956. 352 p.
(Radio-- Transmitters and transmission) (HIM. 1011)

L 2689-66 EVIT(d)
ACC NRt AN5019285 YmouWh URI
Betin, B.M. .2-7
Radio trdnsimittersq, theor-j and design (Radio-peredayushchiye
ustrovstva; tepriya i
rascnet) 3d ed., rev. and enl. bbscow, Izd-vo I'Vysshaya
shkola," 1965. 334p.
illus., biblio., tables. 37,000 copies printed.
7OPIC TAGS: radio commmication, radio engineering, radio
equipment, radio
transrdtter.
COVERA(Z AND PURPOSE: This is the third edition of a text book
approved by the
Ministry of Higher and Secondary Specializbd Education for use
at radio
engineering schools. qheoretical and design problems connected
with the
developrent and lot production of relatively low-powered
radio-transrdtting
equipment are discussed. Sections describing the circuits and
operations of
pulse transndtters and modulators, frequency and phase
modulation, anp1ifters
and ultrashortwave generators are extended to include
transistorized anplifiers,
generators, and circuits and the technical indices of
transniitters currently in
use. The author thm*s N.A. Fletisova, Ye. M. Moskalevskaya, D.B.
Malysheva and
I. Kulika for their assfs-tanoe.
TABIE OF CONTERIS:
Floreword - 3
1/7

L 26389-66
ACC NRs M5019285
an the'
Ch. I. Brief History of the Development Of. Radio 'h- Witting
Systems in
USSR - 5
1. Spark, arc, and machine radio transmitting system - 5'
2, Tube generators and transmitters - 8
Ch. 31. Theoretical Fundamentals of High-Frequency Tube Power
Amplifiers 13
1. Operational principle of H.F. power amplifiers - 13
2. Plate cu:rrent in power anplifters - 21
3.',, Power relationships in the plate circuit of a power
amplifier 28'
4. Dependence of amplifier 'power indices an the load resistance -
30
5. Conputation of optimum plate load resistance - 32
6. Currents and power indices In the circuits of ccntrol, screen,
and
suppressor grids - 33
Ch. III. HF Power Amplifier Circuits - 39
1. Single-cycle amplifiers with series and parallel supply of plate
circuits - 39
2. Control gria circuit diagram - 42
3. Screen and suppressor grid circuit diagram - 47
4. Heater circuit diagram - 49
5, Circuit diagram of amplifiers with tubes connected in parallel
and of
push-pull amplifiers - 53
6. Wide-band power amplifiers - 62
:crd 2/7

L ~6389-66
ACC NRs AM019285
7. Technical calculation of power anplifiers 65
Ch. IV. Transrdtter Output Anplifiers - 75
1. Circuit--(Iiagram of output anplifiers - 75
~2. Design of a sinple-diagram output anplifier - 81'
3. Desigr of a conplex-diagram output aWlifter - 85
4. Design of coirplex-diagr-am output aryplifler with a smothly
acIjustable hequency
range - 86
Tuning of an output anplifter - 92
Ch. V. Interrwdiate Transrdtter Anplifier 94
1. Fundarmntal frequency intermediate anplifiers 94
9. Buffer anplifier - 99
3. Ftequency rwltipliers - 102
Ch. VI. Ribe Oscillators - 107
1. Self-excitation of tube oscillators 107
2. Oscillation frequency - 1-10
3. Sofft and rigid self-excitatian conditions 111
4. Diagram of single-circuit three-point oscillators - 113
5. Desigi of a single-circuit oscillator - 117
6. Diagram of double-circuit three-point oscillators - 121
7. B.K. Shenbell oscillator circuit diagmin - 125
gqo 3/7

L 26389-66
ACC NRj
X15019285
Ch. VII. Frequency Control 132
1. Requiremnts for oscillation frequency control of a transidtter -
132
2, Basic sources of frequency instability - 133
3. Quartz-crystal frequency control - 136
4. Quartz-crystal oscillators 137
Ch. VIII. Prevention of Anplifter Self-Excitation -.144
1. Effect of plate-grid coupling capacity on anplifter operation -
144
2. Bonch-Bruyevich inverse network - 145
3. Neutrodyne effect - 141
Ch. IX. Transistorized Anplifters and Oscillators - 150
1. Char-acteristics and pararneters of a tradam u3,--d As an hf
poww aqvxiw
2. Operation of a power arrplifier using juncticn-type transi8t&at
mDderately high freqtencies - 153
3. Power anplifter operation at conparatively high. frequencies -
162
4. Transistorized oscillators - 169
Ch. X. Meter Wave Band Amplifiers and Oscillators 173
1. Peculiarities of ultrashortwave tube operation 173
2. Urtrashortwave oscillatory system - 176
3. Voter wave band anplifiers - 179
4. Voter Wave hand oscillators - 181
t Card 4/7

L 26389-66
ACC NRi - AM5019285
Ch. )a. Decimeter and Centimeter Wave Band Amplifiers and
Oscillators 191
1. Decimeter wave band amplifiers and oscillators using triode
tubes 191
2. Klystrm amplifiers and oscillators - 195
3- Magnetron oscillators - 205
4. Arrplifiers and oscillators using travelling wave and
backward'wave
tubes - 215
Ch. XII. Grid Amplitude Ybdulation - 224
1. General information on amplitude modulation - 224
2. kriplitude modulation methods - 227
3. Distortion caused by amplitude modulhtion - 228
4. Modulation characteristics - 230
5. Control grid bias modulation - 232
6.. ArrpMcation of modulated oscillations 241
7. Suppressor grid m)dulation - 244
Ch. EII. Amplitude Plate (Power) Modulation 249
1. Plate mdulation in amplifiers using trdode tubes - 249
2. Plate-screen modulation - 255
3. Modulator operation at plate and plate-screen mdulation - 259
4. Automatic plate modulation 260
card 5/7

26389-66
C NRt AM5019285
-Ch. XIV. Frequency and Phase Modulation -, 262
1. Bases of frequency and phase modulations - 262
2. Fzequency spectrum of freqtency-mDdulated oscillations 266
3. Reactance tube - 267
4. Phase modulation - 274
Ch. XV' Radio Telegr-aph Operation of Tr-ansirdtters - 281
1. ;eZ-ca Information on radiotelegraphy - 281
2. Arrplitude manipulation circuits - 282
3. Distortion of radiotelegr-aph-signal shape - 286
4.i* Frequency manipulation - 288
Ch. XVI. Pulse Operation of Transndtters - 290
1. Fbundations of pulse radio com=dcation - 290
2. Pulse operation of radar transrdtters 298
3. Pulse modulator - 300
4. Switches - 307
Ch. XVII. Current Radio Transmitters 313
1. Classification of tran5mitters and their technical
characteristics 313
2. Circuit-&agram of up-to-date transirdtters - 317
Bibliography - 328

L 26389-66
ACC NN
Appendix 1 - 330
Appendix 2 - 331
Appendix 3 - 332
Appendix 4 - 334
SUB COM: 17, 09/ SUBM DAM 15Feb65/ ORIG FEF: 03D

SOV/ 124-58-10-11336
Translation from: Referativnyy zhurnal, Mekhanika, 1958, Nr
10, p 92 (USSR)
AUTHORS: Notarov, V.D., Betin, D.I.
TITLE:~ Methods of Determination of the Permeability
Coefficient of Individ-
ual Water-bearing Horizons by Means of Evaluation of Total
Yield
of Wells Operating in the Krivoy Rog Basin (K metodile
opredeleniya
koeffitsiyenta fil'tratsii otdel'nykh vodonosnykh gorizontov
po surn-
marnym otkachkam iz skvazhin v usloviyakh
Krivorozhskogobasseyna)
PERIODICAL- Byul. nauchno-tekhn. inform. N.-i. gornortidn.
in-t, 1957, Nr 3,
pp 58-66
ABSTRACT: A presentation of methods for determining the
permeability coef-
ficients of individual water-bearing horizons exploited bv a
common
well without provisions for mutual insulation of reservoirs.
The
authors base their reasoning on the fact that natural aquifer
horizons
are completely isolated from each other by heavy, impervious
layers
and that the only hydraulic connection between them is that
provided
by the wells. The yield of a well is regarded to be
equivalent to the
algebraic surn of the yields of the separate horizons. In
their compu-
Card 1/2 tations the authors make use of Dupuy's equations.
The calculation

SOV/124- 58-10-11336
Methods of Determination of the Permeability Coefficient
(cont.)
equations are based upon the following conside rations: The
first equation ema-
nates from the condition that drilling operations are halted
and the resulting steady-
state water level is measured after penetration of each
water-bearing horizon. Two
other equations are set up on the basis of two separate
pumping operations with
different yield from the horizon being considered. After the
hydraulic character-
istics of a given horizon have been determined, the drilling
operations are contin-
ued until the next horizon is reached. Water level
measurements and the two sep-
arate pumping operations make it possible to obtain three
equations from which
the hydraulic characteristics of a given water-bearing horizon
may be determined.
An example is given showing the computation of the
permeability coefficient of
three separate water-bearing horizons.
V.A, Vasiliyev
Card 2/2

TOKil'AJYL;'V, G.V.; BETIN. D.I.
L~ualitative evaluation of Jointing for the
chnracterization of
the stability of rocks. Uzb.gool.zhur.no.3:43-46
160.
(14IIU% 13; 11)
1. Vseeoyuznrr nauchno-issledovatelskly
goologo-razvedochri5ry
inBtitut.
(Joints (Geology))

NATAROV, V.D.- -BFjTIV D I
Method of determining anticipated inflows into mine
openings and
open*pits with a calculation of drainage time under
conditions
of the Krivoy Rog Basin. _Sbor, nauch. trud. NIGRI
no.7:60-69
360. (14W 14:12)
(Krivoy Rog Basin-Mine drainage)
(Water., Underground)

BORISENKO, V.G.;
BELEVTSEV, Ta.N.; BE;YGULENKO, I.L.; 8=
GUBKINA, N.N.; DZHEDZALOV, A.T.; ZHILKINSKIT, Se Ly prof.,-
ZALATA, L.F.; KAZAK, V.M.; MALYUTIN, Ye.I.; MURONTSEVA,
Z.G.;
NATAROV, V.D., doktor geol.-miner. nauk: PANASENKO, V.N.;
PITADE, A.A.; RADUTSKAYA, P.D.; SLEKTOR , S.M.; SMIRNOV,
D.I.:
TOKHTUYEV, G.V., kand. geol.-min. nauk; FOMENKO, V.Yu.;
SLENZAK, 0.1., red.izd-va; MATVEYCM, A.A., tekhn. red.
[Methodological guide for the geological servioe for the
prospecting and mining of Krivoy Rog type deposits]
Metodiche-
skoe rukovodstvo dlia razvedochnoi i rudnichnoi
geologicheskoi
sluzhb
.y mestorozhdenii krivorozhskogo tips. Pod red. U.N.
B6Uvtseva. Kiev, Izd-vo AN USSR, 1963. 395 p.
(MIRA 16:12)
1. Krivoy Rog. Gornorudnyy institut. 2. Chlen-korrespondent
AN Ukr.SSR (for Belevtsev).
(Krivoy Rog Basin-Engineering geology)

SHAKHOV, A.I.; BXTIN, P.7a.; AFANASIYBVSKIY, Te.K.,
redaktor; KIYYAYEVA, G*A.,
reeaktor. -
(Laying out and marking off ships on the mold loft]
RazbiTka i razmatka
sudov no plaza. [Leningrad] Goa. izd-vo sudostroit.
lit-ry, 1953. 123 p.
(MM 7:6)
(Shipbuilding)

SHWHOT,'Aleksandr
Ivanovich;-,BBTIN. Pavel Yakovlevich; DCRMIDONTOV, Y.K.,
otvetetvenny3r red.; MOCHKINA. L.I., tekhn. red.
Daying wit and marking off shipa m the mold loft] Razbivka i
razmatka endov na plaza. Izd.2., inpr. i doN. Ieningrad, Gos.
soiuznoe izd-vo sudostrott. proaVshl., 1958. 152 p. (NM 11:7)
(Naval architecture)

BW IN, S.
Kachinery for the northwestern zone. Trakt. i
sellkhozaamb. 30
no. 12:20-24 D 060. (KIRA 13.12)
1. GlavVy lconstruktor Spetsiallnogo konstruktorskogo
byuro
Severo-zapada.
(Russia, Northeraveatern--Agricaltural machiner7)

BETIN, S.
Machinery developed by the Northwestern Main Machinery
Design
Bureau. Trakt. i sellkhomash. 32 no.10:37-38 0 162.
(MIRA 15*9)
1. Glavnyj konstruktor Glavnogo konstruktorskogo byuro
Severo-Zapada.
(Fertilizer spreaders) (Harvesting machinery)

IYEVINSH, Ya.K.; BETIN, I.I.; TKACHUKOV, V.7a.,
. . . . . .* KTAAS, V.
nauchn. r VA, I.B., md.
[Farm mechanization in the countries of the
northwestern
zone of Europe (Finland, Sweden, Denmark, -the
German
Democratic Republic)] Mekhanizatsiia sellskogo
khoziaistva
v stranakh Severo-Zapadnoi zony Evropy
(Finliandii -
Shvetsii - Danii - GDR); obzor. Moskva, 1963. 91
P. (Kom-
pleksnaia mekhanizatsiia i avtoTratizatsiia
predpriiatii.
Seriia 1-63) (MIRA 17:5)
1. Moscow. TSentral'W institut
nauchno-tekhnicheskoy in-
formatsii po avtomatizatsii i mashinostroyeniyu.

P~~Tl N, , S. G,
. Some problems of developmnnt In the design of miultip-irpose
agricultural loaders. Trakt. i sellkhoznmsh. no.2:18-19 F 165.
(MIRA 18:4)
1. Gosudarstvennoye spetsiallnoye konstruktorskoye byuro
Severo-
-. Zapada.

BEETIN) V. T., B. I., KJZ-1AYZV,, F. A., and
J,~~YKH, j- G.
"Moisture Control of a Furnace Charge by the
Neutrun riethod"
paper presented at the All-Union Seminar on the
Application of
Radioactive Isotopes in &I-leasurements and
Instrument Building,
Frunze (Kirgiz..33R), June 1961)
So: Atomnaya Energiy&., Vol 11, No 5, Nov 61) PP
468-470

IMMOR i ; M*JR&TIRINSKlY. S.V.; URLLOV. N.S.
wpw~--
Cbservation of wirine ice from skirplanes. Trudy GOIN
no.40:147-155
'57. . . I (-~Ce) (KMA 10: 7)

BETIN, V.V.
Ice conditions in the Baltic Sea region and its
approaches and per-
ennial variations of these conditions. Trudy GOIN
no,41:54-125 '57.
(MIRA 11;9)
(Baltic Sea--Ice and rivers, lakes, etc.)

3(9) 3071/'0-51 9-5-1, 5/22
AUTHORS: Betin, V. V., Zhadriaskiy, S. V., Uralov, N. 3".
TITLE:
~f ObservinE; laland Ice in the Sea L.-,,
1nstrum-_-,.'s

Frorr, ~,n ~ir,,)Iare (Sp,:).;~b
instrumentalInyki.

materilmv,,,ni 1fl-i v mc_-C~)
P1M I ODI
CAL:
Yi~tf,,orol:~giya i E;idr-,lo6iya, 19510, Nr 5, -eP
5,11-54 (USSR)
ABSTRACT:
in thc .3lystematic obs~_,rvation of
the ice cover i;:,, t'-.~-

Sc-i fron, an airplane, the aerial
protractor -xith

;-.,as mainly ,.,,Z;C!d (R;~f 11). 0.".1

the
basis of this instrument, a method for thIC Sl.~~'VCY Of 4-ce

fields in the sea from an airDlane was worked out. The ex-

per.ence of the last 3 years showed t*,-,at this method
-aarantee~

an accuracy aufficient for practical and scientific
-purposcs.

It 4S suggested here to apply ICh 4S method also to
the cbsc_-

~,ation cf ililand ice in the sea. The a,,)ria'L
protractcr h-as an

autc-matically adjusting perspective
zxtwork and rc~,r

ineaouring the vertical and horizon'al.
angl,~:-- Th-~ per-

mA ts measuring the linear elements and
tht,, uicments of area of

4~
Lhc inland ice visible at an angle of 30 to 74?0 in 4,-*,,v
per-
Card 1/3
spective. The measuring method is Qx~lained here
in short. if

S07/50-59 -5-151122
Method of O~serving the Inland Ice in the S~--a by
1nstr1.=_e,11ts From an
the airplane is drifted, $'he length of the Ice objc-ct can tt,
calculated by formula /1 Formula (2) is giver.. This is the
general form of the equation 'or calcu'ating the length +",e
ice object. The real flying spead, and the drift of the airplane
out of the course can be measured at the same time by ziaans of
the mentioned net-oork. The procedure is described in short. -
Measuring the surface position of ice formations is a little
more complicated. The projection of this *,,eight on a
horlzoi~tal
plane is measured from the airplane, and then the height is
determined by formula (3). The icebergs are usually located :In
clear weather. The shadow can then be measured, and the height
of the iceberg above the ,,rater level can be determined by
formula (4). The position of the iceberg with respect to "he
airplane can be determined by formula (5). - Reccmmendations
are given for determining the height of the iceberg if thio
shape of the iceberg is &3Ymmetric. The accuracy of the survcy-
ing methods given here is - as an exami:-,aticr, showed - ap-
proximately equal to the one attained i.-_ determining the
z~oz~itiorl
of a ship in the sea by the method of ---s~oticn to coa-t
stations. The mentioned instrument .%as u1so le2tod
Card 2/3 ing factory chimneys, lighthouses, rocks etc. These
tL!stt; al~,o

SOV/550-59-15 - 1.5/22
Method of Observing Inland Ice in the Sea by instruments
From an Airplane
confirmed the utility of this instrument for measuring
heights
from an airplane. There are 3 figures, 1 table, and 1
reference.
Ca-rd 3/3

BETIN, V.V.; PREOBRAZHRNSKIY, Yu.T.
Variation of ice conditions in the Baltic Sea and
the straits
of Denmark. Trudy GOIN n0-37:3-13 '59- (MM 13:4)
(Baltic Sea--Ice) (Oresund-Ice)

BETIN, V.V.; ZHADRINSKIT, S.V. [deceased]; URAWV,
N.S.
New methods for aerial observation of marine ice
conditions.
Trudy GOIN no.37:205-230 '59. (MIRA 13:4)
(Aeronautics in surveying) (Ice on rivers, lakes,
etc.)

BMIN, V.Y., starshiy nauchnyy sotrudnik; MOBRAZHBMIY,
Yu.V., otv.
red.; DVOSKIZA. N.B., red.; YASUOGCRODSKAYA, M.M., red.;
MAUX, M.Ta., tekhn.red.
[Ice atlas of the Baltic Sea and adjacent areas] Itlas
l1dov
Baltiiskogo moria I prilegaiushchikh raionov. Pod red.
IU.T.Pre-
obrazhonskogo. Leningrad, Gidrometeor.ind-vo. Pt.l.
[Baltic Be&,
The Gulf of Rigs, the Straits of Denmark, and the
adjacent part of
the North Sea] Baltiiskoe more. Rishakii zaliv, Datskie
prolivy i
prilegaiushchnia chant' Severnogo moria. 1960. 7 P.. 64
P.
(Kim 14:3)
1. Moscow. Gosudarst"nnyy okeanografichookly institut.
Lenin-
gradekoye otdolonlys. 2. Leningradskoye otdaleniye
Gosudaretvan-
nogo okeanograficheskogo institute (for Betin).
(Baltic Sea region-See'lce-Kaps)

BILTIN, V.V.; PMMAZBMISKIY, YU.V.
x
Investigation of ice on the Baltic Sea during the
International
Geophvsical Year. Trudy, GOIN no.46:115-119 '59.
(MIRA 13:5)
(Baltic Sea--Ice)

BSTINO Y.T.; PECOBRAZHINSKIT, Tu.V.;.SOLOV'7ZV, V.I.;
TASNOGORODSKAU,
N.M., red.; 3RAYNIXA, N.I., tekhn.red.
[Album of aerial photographs of different forms of ice
occurring in the sea] 111bom serofotoanimkov ledovykh
obrazovanii
na moriakh. Leningrad, Gidrometeor.izd-vo. 1960. 221 p.
WRA 13:6)
1. Moscow. Gosudaretvannyy okeazograficheskiy institut.
Lenin-
gradskoye otdoloniye. 2. Leningradskoye otdeleniye
Gosudarstvennogo
okeanograficheekogo institute (LO GOIN) Glavnogo
upravleniva gid-
rometeorologichookoy sluthby pri Sovete Kiniatrov SSSR
(for Betin).
(Sea ice-Pictorial works)
(Photographic Interpretation)

BETIN, V.V.; MOBUZHEMKIYp YU.V.
Use of radiopb#totelographic apparatus in operative
transmission of
the materials"of aerial oceanographic and ice
observations* Trudy
GOIN no.55:182-186 160. (MM 14M
(Radiotelegraph) (Oceanographic research) -

BETIN,,,.V.V.;-, MOBPAZHUSKIYO TA-Vp
Desiptegr atiow of: nea,,ice and4ts'95timatiop.. Trudy
GOIN no.55;
187-407 160 (M3RA 14:7)

BETIN, V.V.; SHIROKOV, K.P.
Detentiining the elements of ice drift in the sea
from the
airplane. Trudy GOIN no.63:64-77 161. (14IRA 14:8)
(Sea.ice) (Aerial photogra=etry)

~IETIN, V.V.; ZAYTSEV, A.P.
Characteristics of freezing of the Baltic Sea in
the winter
of 1959/60. Trudy GOIN no.63:78-89 161. (MIRA 14:8)
(Baltic Sea--Sea ice)

B1qIN Vasi -Ige 11 evich; PREOBIIAZI-:El-'SYJY
Yuriy Veniaminovich
,- -- liy g!y_ I
-Cdeceasedj; NEDOSHIV114A., T.G., red.; VOLKOV,
N.V., tekhn.
red.
[Severity of European winters and ice
conditions in the
Baltic Sea] Surovost' zim v Evrope i
ledovitost' Baltiki.
Leningrad Gidrometeoroizdat, 1962. 108 p. (MM
15:7)
Nurope-Winter) (Baltic Sea-Sea ice)

ACCESSION NR: AT4038922 5/2634/64/000/07110125/0140
AUTHOR: Betin, V. V.; Losev, S. M.; Shirokov, K. P.
TITLE: Aerial photography of marine ice floes
SOURCE: Moscow. Gosudarstvenny*y o)-,eanograficheskiy institut.
Trudy*, no. 71,
1964. Issledovaniye izmenchivost~ ledavitosti nekotory*kh morey
(Investigating
the variability in ice formation on some seas), 125-140
TOPIC TAGS: oceanography, drift ice,Ace floe, serial photography,
ice flow
photography, marine ice
ABSTRACT: This extensive article is in four parts. In the first
section, the
'authors discuss aerial photographic field work in general terms.
Cartographic
and reconnaissance factors are considered which must precede the
actual photo-
.1 graphic operations. Recommendations are given regarding the
linear value of
the base for various frame formatsP scale and camera types. Tack
length is also
considered for situations involving photography along the shore,
along the fast'
ice line (shore ice) and over open water. It is pointed out that
an extremely
desirable condition when selecting the routing is the possibility
of a two-way
connection or orientation of that routing with certain fixed
features (islands,
1/6
Card
.7,

ACCESkON NIR: AT4038922
capes, promontories, fast ice zone, etc.). The time intervals
between subsequent
,sorties are to be so scheduled that not leas than 50% of the
floating ice area re-
corded on the pictures of a preceding tack is represented on the
next succeeding
aerial photography routing. The use of the smallest possible scale
is recommended'~
and the reasons why, in aerial photographic work involving the
study of ice drift,.,
this scale should always be minimal for given resolution of the
equipment, cor-
,responding meteorological conditions and dimensions of the ice
floes to be photo.-
graphed are explained. The importance of parallel observations
over surface
currents in the gaps between floes is noted. Recommendations are
given with
respect to the depth of immersion of float buffers and the point
is made that
this depth should correspond to the thickness of the ice. The
authors note that
it is advisable to carry out aerial photography in parallel with
two cameras
capable of simultaneously photographing at two scales: I : 20,000
- 1 : 409000.
for the ice drift proper and 1 : 5,000 for the disposition of the
floats. The
second part of the article analyzes the results of the aerial
photography per-
formed in the Gulf of Finland in 1961. This material was broken
down into three
groups. The first group contains materials obtained in photo
passes made along
the coast or the edge of the fast ice (coast ice); the second
group contains
material from cantilever extensions; the third group contains the
material from
Card, 2/6

ACCESSION NR; AT4038922
cl-osed passes, resting at fixed reference points on both ends.
The data pro-
cessing of the information from all three groups is discussed in
this section.
The authors point out that the determination of the elements of
ice drift on
the basis of the materials of each of these groups is possible
through the use
Of graphic photo-triangulation. However, for the first group,
under certain
conditions, the problem may be simplified somewhat with no
appreciable loss of
accuracy in the results obtained. For this purpose, it is
sufficient to limit
oneself to the use of conventional photo.layouts (aerial mosaics,
in this case),
mounted from contact prints, without recourse to the plotting of
photo-triangu-
lation nets. Since the problem of the processing of aerial
photography material
on drift ice is of definite interest, the authors have considered
it necessary
to consider the peculiarities.of this problem in detail as they
apply to each of i
the three cases. The third section of the paper deals with method
accuracy. The
ice drifting elements, obtained as a result of the processing of
the material
for each of the three groups above,naturally contain errors.
Since the charac-
ter of these errors and their magnitude will be somewhat
different in each
separate case, the degree of accuracy in the results derived will
hIso be dif-
ferent. For all three processes, the accuracy in the
determination of the speed
and direction of the drift will increase as the route length
decreases, as the
I~1_duration of the time interval between sorties increases and
as the drift speeds
Card' 316

ACCESSION NR: AT4038922
increase. Since the speed of the drift is independent of
humain intervention,
in order to obtain drift material of given accuracy only the
first two elements
can be varied, It is not always possible to reduce the route
length, since
this is limited by the region under study. Consequently, all
other conditions
being equal, the accuracy of the derived information can be
enhanced solely by
increasing the time interval between contiguous tacks. The
problem is analyzed
mathematically in the article. In the example considered by
the authors (ex-
posure scale 1 : 20,000; base number 23 - 25; time between
sorties about I hour;
drift on the order of 0.5 km/hour) the errors in the center
section of the photo
passes were not more than 15% for the speed of drift, and not
more titan 10% for
the direction. The fourth and final section of the article
gives a detailed
description of the use of repetitive aerial photography for
the study of ice
drifting in Kursh Bay (Kurshkiy zaliv) and in the adjacent
area of the Baltic
Sea. The ice was photographed over the same routes which were
so layed out that
it was possible, at least along the edge of the picture, to
obtain an image of
the coastal strip of dry land. In this way, a point of
reference on the coast
line was provided for all pictures and the position of the
ice flows was strictly
coordinated on the basis of orientation markers on the shore.
This section is
supplemented with charts and maps. The data on ice drifting
obtained in this
Card'

ACCE~SION NR: AT4038922
operation make it possible to recommend the method for wide use
in the inves-
tigation of ice drifting both in open as well as in coastal
watcrs. The general
conclusions reached by the authors in this article can be
summarized as follows:
.1. The use of the method of repeated aerial photographic tacks
permits the estab-
lishment of the laws of ice drifting as a function of wind
conditions, while at the
same timgembracing all the varieties of ice encountered at sea.
2. Experience
I in the use of aerial photography for the study of ice drift
conditions makes it
possible to recommend this method for practical utilization. 3.
Aerial photo-
graphy operations can be carried out over routes enclosed between
two objects
on dry land, by cantilever extension routes or by routes running
along the coast
line or edge of the fast ice (coast ice). 4. The smallest scales
permissible
under the given weather conditions, flow dimensions and resolving
power of the
photographic equipment in use Aould be employed. 5. Before
photographing an
ice drift from the air, it is expedient to drop special floats
containing a charge
of fluorescent material in the intervals between the floes. In
this connection,
the exposure should be made on two scales: on a small scale for
the ice drift
proper, and on a larger scale for the disposition of the floating
markers. 6.
Meteorological conditions (cloud formation, visibility,
illumination) place the
same constraints on the use of aerial photography for the study
of ice drifting
as on its other applications. Problems relating to the accuracy
of the determin-
516
Cafd*

ACCESSION NR: AT4038922
ation of ice drift elements at sea by the method of vertical
aerial photography
require further development and refinements Orige art. has: 5
figures and 12
formulas. I
ASSOCIATION: Gosudarstvenny*y okeanograhcheskiy institut, Moscow
(State
Institute of Oceanography)
SUBMITTED: 00
SUB CODE: ES
DA72 ACQ: 04Jun64 ENCL: 00
NO REP SOV-. 005 OTHER; 000
Card-616

BETIN, V.V.
Periodical fluctuations in the ice conditiOn3 of
the Baltic
Sea. Trudy GOIN no.71:120-124 164. (MIRA 171l0)
I

BETIN. V.V.; IBSEV, S.M.; SHIROKOV, K.P.
Aerial phoix1raphic surveying of the drift of ice in
the sea.
I
Trudy GOBI no.71:125-140 164. 17:10)

SEVEROVA, Ye.Ya., kand. med. nauk; BETlN, Ye.M.
Dermatitis caused by aminazine in medical personnel.
Trudy 1-go
MMI 28:79-86 164. (MIRA 17:11)
1. Kafedra obshchey terapii. i nrofessi.onallnykh
zabolevaniy (zav.
- deystvitellnyy chlen AMN SOSSR prof. Ye.M. Tareyev)
sanitarno-
gigiyenicheskogo fakullteta 1-go Moskovskogo ordena
Lenina medi-
tsinskogo instituta imeni Sechenova.

BWIN,Yu.P., ref ,
Remote control equipment for astallogrsiphic
investigation of radio
active substances. Review of forei&m liternture by
lu.P.Batin.Zav.
lav.21 no.8:1011 155. (KL;FLA 8:11)
(Radioactive substances) (Metallography)

Category: USSR/Fitting Out of Laboratories.
Instruments, Their Theory, H.
Construction and Use.
Abs Jour: Referat Zhur-Khimiya, No 9. 1957) 31160
Author : Betin Yu. P.
Inst :-not given -
Title Increasing the Stability of Radiation Recording
by a Scintilla-
tion Counter.
Orig Pub: Pribory i tekhn. eksperimenta, 1956, No 1,
43-47
Abstract: A device is proposed which compensates,
automatically, the change
in amplification factor of a photomultiplier (PEM) by
changing
subsequent amplification of impulses. The equipment
consists of
a scintillation counter, cathode follower, first
amplifier with
controlled amplification factor, a second (linear)
amplifier,
amplitude descriminator, scaler and automatic
regulator. Impul-
ses of linear amplifier output reach the automatic
regulator
(which operates according to the principle of a
peak-reading
voltmeter) which controls both the amplification
factor of the
first amplifier and the actuation threshold of the
descriminator.
Card 1/2 -19-

SOV/120-58-6-12/32
AUTHOR: Betin, Yu. P.
TITLE: An Equipment for Determining the Correlation Function
During
the Recording of the Disintegrations (Ustroystvo dlya
opredeleniya funktsii korrelyatsii pri registratsii aktov
raspada)
PERIODICAL: Pribory i tekhnika eksperimenta, 1958, Nr 6, pp
68-?l
(USSR)
ABSTRACT: The equipment described
correlation function in the
kk = Ti]'; RiEk For
is capable of evaluating a
form
this purpose the time is divided
into 1) intervals. During each interval, n i disintegrations
of the ith type are recorded; simultaneously, nk disinteg-
rations of the kth type are registered and the product of
nink is evaluated. The equipment employs two counting de-
vices, type PS-10 000 and an instrument type PS-64, which
permit the direct determination of the number of intervals
)) and the total number of the disintegrations of the ith
type during )) intervals; similarly, the total number of
Card 1/2 the disintegrations of the kth type and of the product

SOV/120-58-6-12/32
An Equipment for Determining the Correlation Function
During the
Recor4ng of the Disintegrations
nin k over )) intervals is detarmined. From these measure-
ments it is Dossible to calculate ni n k and n ink
The intervals V can be changed from 0.08 to 20 see. The
rise time of one of the computing channels is 5 -4s, while
that of the second channel (which evaluates the product
n n ) is 120 As. A detailed circuit diagram of the equip-
M~n~ is given and its operation is described in some
detail,,
The paper contains 2 figures and 1 Soviet reference.
ASSOCIATION: Fizicheskiy institut AN SSSR (Physics
Institute of the
Academy of Sciences, USSR)
SUBMITTED: December 16, 1957,
Card 212

I I\J"
PHASE I BOOK E.TLOITATION nov/5410
lconeerentGlya po mirno,%u iopollzovanlyu atomnoy
cner,,Lii, Ta~!,'Ikent, 1959.
T-Ldy (Tra.~,-actions of the Tac;hkcnt Confcreiice on tho
Pon-ceful
U', r -1., 196o.
.3 of Allc~-ac L-acra) v. 2. Taolnllont, lzd-vo A I
449 p. Errata slip inserted. 1,500 copies printed.
Spen--oring AZ;cncy: Akadcmiya nauk Uz-bck.,,koy SSR.
Re2pc%n:I',)lc Ed. ; S. V. Starodubtoev, Academician,
txadcmy of
Uzbek SSR. Editorinl Board: A. A. AbG*ull;r,,~v, Can-
of I'llysics and Math~~alv'lcr,; D. I.% Abdur~--.ullov,
Doctor
Sciences; U. A. j%rifov, Acadci~Uclan, Ac-acziy of
'-nces Uzbek SSR; A. A. Borodulina, Candidate of
Dloio,7ical
S,:,ic-nce~i; V. 1-1. Ivashev; G. S. A. Ye. Kiv; Ye.
T,,'~)-,.1OV, Candidate of Phyaic3 and liathclaatico; A-
Nilrol~-yov,
-11daue of M~-dlcal Sciences Ni-hanov, Candfdlnte of
ch-Ical
an D.
C
S-lences; A. S. Sadykov, Correoponding 17crinber,
Acad.---my of Sciences
7 USSR, Ac--demician, Academy of Sciences Uzbek SSIR; Yu.
N. Talanin,

Tran~acticn5 of the Ta~hkent (Cont.) ' Z C, 7/54 10
C,.nd!Oate of Phyrics and Nathematic3; Ya. Kh. Turi~kulov.,
Doctor
(.,~ 1-31ulo~~Ical STticncon. Ed.: R. I. 12iw-ildov; Toch.
Ld.i A. G.
1'U7LTr--,I2 : The publi.:ation is intended for rci~,n"IfJC
wi,-,IrCrz3 and
cmplow~-d in ente,-pri~er, wa-re radioac-tivC
,mil nuclear ra4iaticn are used fc-r rc--iarch in rh-ml-ai,
Cc-o-
lce.ical, and t,,)chnological fields.
collection of 133 articlei rcpre-f~nI.-:1 the, noccnd
of the 7'ranL~aat-ionz of the TaZhIccnt Confercr(~,e on tl-le
F,;a.~ful Uocq of Atomlc. Fner:7. The indiviJual ar' ' dcal
vitl~ a ij~de range of probleTu; in the field cf UC'L~a-
radiation,
fn-~--,UdInS. prodt~ctlcn and chemzical aialy,~-!!; cf
raJioactive
--,~tcpc3, in,.m.,,itigation of the kinctic-3 c-f che-nical
-~a-,-ticrIS
by rcan:3 of inotcpcs, application of ---pe-:~tral for the
manufacturing of radioactive pro.-~,arat .ion P; rLUc--,:rive
nctl
for detemining the content of elc-ment.D in the rCc'A*,3; ZMd
ana~-ysis of methods for obtaining pure sabotanceu. Uertain
Card P/20

Tranzactions or the Ta--Iilcnt (cont.) 3011/5410
Jn~;traT-.2nto used, such as autcnatic re,-,,,.lators,
flo*,7zacterz,
C-m[;ca, end hi&i-ncnoltivity are d~~ocribcd.
N i
No are mentioned. Ruforences follow Individual
articlc,i.
TADLE OF CONTEITS:
RADIOACTIVE 130TOITS AMD NUCLEAR RADIATION
IN FDOIN-EI G AND GEOLOGY
Lobanov, Ye. M. [Institut yadornoy fiziki UzSSR - Institute of
Nuclear Physics AS UzSZR). Application of Radioactive lootopea
I I
and Nuclear Radiation in UzbekiGtan 7
Ta!:nar, 1. 1.1., and V. A. Yanushllcovskiy (Institut fizilki
All Latv
SISR - Inotitute of Physics AS Latvian SSR]. Probl=3 of the
Typification of Automatic-Control Apparatus Ba3cd on the Use of
RadioactivQ Isotopes 9
Card 3/20

Transactions of the Tashkent (Cont.) SOV/5410
III. Yu., and A. T. Lobadev (Inotituto of Nuclc~r.r
Phyzios
AS Uz33R]. A Unified Radioactive loodromic ReCulator
(U:11111) 29
Eoru.khov. 1". Yu. and B. K. I:al'trcv [Inotituto of
Nuclear
1'hy-,1co AS UzSSR1. M--perimental A;;plication of
tivity G.Im-,la-Relay 32 2
Detin, Ya. P., B. I. VerIchovaldy, 11. 0.
&!Icvin2!caya, and
[PizichenUY In3titut fulcadc.-mii nauk M,':"-
Phyoi,~s Inotitute IT, U32.11,3. 11--thoda for
Incroac-ing the %dcuxacy
of of Radioactive Radiation Flux 36
Snisarcnico, A.,, Z. Tarmova., Ye.
llc-,)Q-,,nyaahchiy, and V. 11~ovonoll-
nk
, iy [IN-mchno-isalodovatell okly inztItut Dhinnoy
nosti-Scicntiflic Research Institute of the Tire
Indaz-t;,-y].
Deteraiination of the Wear of Car Tirea by Neans of
lootopea
TLI'04 43
ArkhanEellukiy, A. A., and G. D. Latyahev (Itirtituto
of Nuclear
Card 5/20

S/12o/6o/ooo/oo6/O05/o45
1033, /jj E032/E51.4
AUTHORS: Verkhovskiy, B. I., Zelevinskaya, N.G.
and Yakushin, V. V.
TITLEz A Method for Increasing the Accuracy of Measurement of
the Intensity of Radioactive Emission
PERIODICAL: Pribory i tekhnika eksperimenta, 1960, No.6, pp.23-27
TEXT: The principle of the method is as follows. The
radiation detector is irradiated both by the radiation under
investigation (intensity n.) and the radiation from a standard
source (intensity r ). The total electrical signal produced in
the detector under Ne action of the two radiations is fed into a
common electronic device at the output of which two signals are
VK
separated out. The magnitude of one of them (U ) is proportional
to the sum of the two intensities and the magnitude of the second
(U2) is proportional to the standard intensity only. The signal
U,
is used to determine the intensity of the radiation under
investi-
gation, whilst the ignal U 2 is used in the automatic control of
the readings and th:ir correction. The automatic correction of
the readings is carried out by measuring the ratio U /U 2' In
order to be able to separate out the signals U 1 and 1~ 2 at the
Card V*4

S/12o/6o/ooo/oo6/005/o45
OF-4 6_300 (~2,P/6j/0a3.')j/jy) E032/E514
AUTHORSt Betin, Yu.P., Verkhovskiy, B. I., Zelevinskaya, N.G.
and Yakushin, V. V.
TITLEt A Method for Increasing the Accuracy of Measurement of
the Intensity of Radioactive Emission
PERIODICAL: Pribory i tekhnike eksperimenta, 1960, No.6, pp.23-27
TEXT: The principle of the method is as follows. The
radiation detector is irradiated both by the radiation under
investigation (intensity n.) pnd the radiation from a standard
Source (intensity z~). The total electrical signal produced in
the detector under t e action of the two radiations is fed into a
common electronic device at the output of which two signals are
Vr
separated out. The magnitude of one of them (U ) is proportional
to the sum of the two intensities and the magnitude of the second
(U2) is proportional to the standard intensity only. The signal
U 1
is used to determine the intensity of the radiation under
investi-
gation, whilst the signal U 2 is used in the automatic control of
the readings and their correction. The automatic correction of
the readings is carried out by measuring the ratio U /U 2' In
order to be able to separate out the signals U 1 lind 1~2 at the
Card I/A

86731
S/120/60/000/006/005/045
E032/E514
A Method for Increasing the Accuracy of Measurement of the
Intensity
of Radioactive Emission
output of the device, the magnitude of the control beam of
radiation
is periodically varied.'The block diagram of the instrument is
shown in Fig.l. The detector 1 is irradiated from the left by
the radiation under investigation and from below by the control
beam due to the additional source S k . The control beam is
modulated with a frequency w using a rotating absorber as shown
in Fig.l. If the intensity A the control beam follows the law
n = n 1 + sin w t-), then-the signal at the anode of the photo-
k(t) k(ar 0
multiplier across the load resistance of the ionization chamber
is
of the form U n UA + U k (1 + sin w 00. The constant component
U" + U I thus proportional to the sum of the two intensities,
while the :mplitude of the variable component U k is proportional
to the intensity of the control beam. The total signal U is fed
into a dynamic capacitor 2 in which it is transformed into an
alternating signal with a frequency w1>> wo and is then amplified
by the main amplifier 3. The amplifier is followed by a linear
detector 4 which produces at its output the constant voltage
C.ard 2/4

86731
S/120/6o/ooo/oo6/005/045
E032/E514
A Method for Increasing the Accuracy of Measurement of the
Intensity
of Radioactive Emission
U1 = (U W + Uk) kk11, where k is the product of the voltage
transformation coefficient of the dynamic capacitor a and the
amplification coefficient of the amplifier. 1, and ki is a
coefficient depending on the parameters of the detector. The
component of the signal having a frequency w 0 leaves the
detector
4 into the amplifier 5 which is followed by a further detector 6;
the latter :L-solates tka constant voltage U = U kk"k k where
2 k 1 H 21
k is the amplification coefficient of the amplifier 5 and k"
H I
and k 2 depend on the parameters of the detectors 4 and 6. The
voltages U 1 and U 2 are fed into the electronic potentiometer 7,
which is connected in such a way that its amplifier sees the
difference between U 1 and a fraction of U 2 'which is applied
to tie
rheochord of the potentiometer. The potentiometer is so arranged
that its indications satisfy the condition
U1 /U2= r/R = p
where R is the resistance of -the rheochord and r is~,- fraction
Card 3/4

86731
S/l2o/6o/ooo/oo6/O05/o45
E032/E514
A Method for Increasing the Accuracy of Measurement of the
Intensity
of Radioactive Emission
of this resistance which feeds the amplifier of the potentiometer.
The ratio r/R is shown directly by the potentiometer. It is shown
that changes in the parameters of the detector of the radiation,
the
dynamic capacitor and the main amplifier have no effect on the
measurements. Details are given of the basic circuits involved and
some experimental tests performed with the apparatus. There are
4 figures and 2 Soviet-references.
ASSOCIATION: Flzicheskiy institut AN SSSR (Physics Institute AS
USSR)
SUBMITTED: September 26, 1959
Card 4/4

S/903/62/000,/000/014/044
B102/B234
AUTHORS: Benetskiy,, B. A., Betin, Yu. P., Bukarev, V. A., Frank, I.
M.
--------------------
TilTLE; (nt)-c?rrelation in inelastic ocattering of 14-Mev neutrons
from ~I nuclei
S ID:UR C E, s. Yadernyye reakts3;.i pri malykh i srednikh
energiyakh; trudy
Vtoroy Vsesoyuznoy konferentsii, iyull 1960.g. Ed. by
A. S. Davydov and others. Moscow, Izd-vo AN SSSR, 1962,178-179
T~JXT: 14'Mev neutrons from a T3(d,n)He4 source were scattered from a
toroidal carbon scatterer; the x-rays were recorded by a NaI(Tl)
scintilla-
tion detector with (f,~)Y-29 (FEU-29) photonultiplier, the neutrons
by a stack
of plates of an organic scintillator separated by plexiglas and
connected
with an qq~-24 (FEU-24) multiplier. Also the recoil protons with
7 Yev,