SCIENTIFIC ABSTRACT SHUPPE, G.N. - SHUR, A.G.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001550220009-7
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 23, 2000
• Sequence Number: 9
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

. I --~ - I :IM-------,---- . -- .--
KAKHAROV, 0._; SHUPPE, G.N.
Determining the heat of adsorption of thor-Jum on tungsten
filaments as related to the method of filament processing.
Dokl. AN Uz. SSR 21 no. 11:24-26 164. (MIRA 18:12)
1. Tashkentskiy gosudarstvennyy universitet imeni Lenina.
Submitted August 1+, 1964.

L 3349-66
!A.16jMJE-S_SJ-1_M NR
'F3~
z 1. UR/O
AP5017284
;AUTHORS: Azizov,.U. Vj Shuppe,
TITLE: Emission and adso7tion characteristics of the faep.8 Of a
tungsten,single crystal
~b
1q, 55
-IFizika tverdogo tela, v. 7, no.
7, lq65, 1970-1973
:TOPIC TAGS: tungsten, electron emission, barium, adsorption, work
function
!ABSTRACT: The Richarson-line method was used to investigate all the-,.
faces of single-crystal tungsten of interest, namely (110.), (li2),
-function from ure tungsten anC_
(100), and (111). -The electron work p
from tungsten coated with barium, the average heats of adsorption of
barium near the saturation point of the mission current, and the con-
stants A (1 r) (A emission constant,r reflection co'efficient--ft',!--.-~
0 01
averaged over the electron energy) were,,measured for both pure surfa:ces_'.~*',,.'_
elin __7rn_-_-';~ 11'..
and for barium-coated surfaces... The*measurements:were mad the
strument shown in Fig. 1 of',the Enclosure-,:.in which*all-the electrodes
1/3
LC~!_~d

L 3349-66

ACCESSION NR: AP5017284

!were flat t o facilitate'the data reduction. All:the results are sumo'- __
marized in the table of the Enclosure*,. Differences between:theee ...

.results and --dis
those obtained by,-otbers are briefly, cussed .,,Orig.
r as.
5
figures.,1 formula., and.1-table.

SSOCIATION
vennyy~Universite _-_V9 -6
: Gosudarst t 'imp

~Vashkeii
TAnina
t

(Tashkent State Universi

SUBMITTED: 27NOv64~x-__ M CODE:

NR REF SOV: 006

Card 2/3

-66
L 3349
._------
ENCLoOS=.'
__

ACCESSION NR. AP5017284 -
-47

Emission and
ble 1
T ion characteristics
adsorpt
.
a

of the faces of tungsten

-T

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a/do
A0

.
09

4
.110
.
-112.
4. -005~'

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~..-100 :05.
4.5 4. 4".
4.4
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c-cr
3 ------------
i~l.--~-"-~~~,~~~~~PIMINRI ~~-_~.-~- ~Aov

AP5022719 SOURCE CODE: UR/0181/65/007/009/2759
AUTHOR: Aziz-ov, U. V.; Vakhidov, U. V.; Sultanov, V. M.; Sheynberg, B. N.- ShuDjk,,~S
G. N. 1, 55 Y 7. ST
ORG: -Tashkent State University im. V. 1. Lenin (Tashkentskiy gosudars -tvennyy univer-
sitet)
TITLE: Emission properties of a molybdenum single crystal
SOURCE: Fizika tverdogo tela, v. 7, no. 9, 1965, -4759-2762
TOPIC TAGS: single crystal, molybdenum, work function, electron emission
ABSTRACT: Richardson lines were pi Wed for measuring the work function of electrons
on the three main faces of a molybdenum single crystal: (110)i (100) and (M). In
addition to this, the work function of surface (13-1) was measured during vaporized
deposition of barium on this face. The methods used in preparation of the specimens
and making the measurements are described. Theequipment is described in other pa-
pers. Curves are given for in XIT2 as a function of 2rl for the three -fa---- studied.
The data obtained from these curves are used for calculating the work functions and
Richardson constants (see table)
C,,d 1/2

L 9204--tb
ACC NRs AP5022719
TABIX
Face ev Ao(l-r), a/deg2-CM2
(110) 5.10:k 0.05 270* 20
(100) 4.40 10.05 230* 20
(111) 4.151 0.05 140120
The method and formulas used for calculating the Richardson constants are described.
(III) a
It was found that the Ba-Mo cathode current is ;directly proportional to the
barium concentration. The work function in this case was found.to be.2.30 A 0.1 ev,
while the effective Richardson constant was 60 a/deg!2.CM2. Data desorption-
curves show that the mean heat of adsorption for barium on surface (111) of Molybdenum
is 3.90-4.00 ev. The results indicate that the contrast in the work function is
nearly as great in a molybdenum crystal as.in tungsten: A#= 4mar 4 min 1 ev. orig..
art. has.- 5 figures, I table.
SUB CODE: 20/ SUBM DATE: 09Apr65/ ORIG REF: 003/ OTH )WF: 000
Card

-'zzULT,kNOVI V.M,.~ *--"HU.!-I'~,q G.N.
Work function and heat of adsorption values of barium at
individual faces of a tungsten sinGle crystal. 1zv. AN Uz.-':SR.
Ser. fiz,=rnat. nauk 9 no.5-,49-53 165. (MIR4 18-11)
1. Tasbkentskdy gosudarstvennyy univer5itnt imer-I Lenin&.
:~MbmitLed December 25, jqU.

L )/EWT W /ETC (f /EPF (a)-;--2"W (MvTaWP(t)4Tr-(m)=A I-TP(r.)
ACC NRs AP5026347 JD/JG/AT SOURCE CODE: UIR/olb6/6.5/000/00.5/oi)49/0053
AUTHOR: Sultanov, V. M.; Phuppe, G. N.
ORG: -Tashkent State University im. V. I. Lenin (Tashkentskiy gosuniversitet)
TITLE: Work functions and.heats of adsoalion of barium on different faces of single-_:.,
crystal
tungsten
SOURCE: AN UzSSR. Izvestiya. Serl3m fiziko-matewnticheskikh nauk.. no .5j, 19 6.5
49-53
TOPIC TAGS: tungsten, barium., single c27stalp work functionp.thermionic emissionj,
.adsorption
ABSTRACT: The work ti
fu cr on was measured by the method of thermionic emission from
large single cx7 x.,,ng apparatus similar to that describedby the author earlier
s
tal
(RadiotekhnikEL I elektronika, v- 9., 317., 1964.. No. 2). The vorli functions obtained
were 4.40 � 0.03, 4.30 � 0.03, 4.53 � 0.05,, 4-76 � ox.5,, and-5-33 � 0.03 ev for the
faces (3-11).,.(116), (100), (3-12), and (110) respectively. The heats of adsorption of
barium were measured with the same apparatus, and the test ro'cedure Is described-The
average values for the beats of adsorption were 2.2 � 0.1j, 0-4 .5-0 � O-1P
4-7 � 0-1., and 3.6 � 0.1 ev for the faces (110)., (M), (100),p (111)j and (1i6). When -7
all the tungsten.faces were covered with bariump the vork runction,-*determined
Using the Richardson curve., was the same for all faces., 2.3 0.1'0-v. Orig. art. has&
6 figures and I formula..
25Dec64/ oR3x; Rzrt oc*/, o7H ww: 00.3
SUB CODE am DAP-
~~L ccird- -.Vi.

L -,:R098-&5 EI-IT (m)JEWP (t) -IJT-(c-)-- - JD/JG
A16008550 SOURCE CODE: UR/0166/66/QOO/001/0065/0068
,t~ 3
AUTHOR: Kakharov, 0.; Shuppe, G. N.
ORG: Tashkent State University im. V. 1. Lenin (Tashkentskiy gosuniversitat);
Bukhara Pedagogic Institute (Bukharskiy jiTi-nititut)
TITLEz Determination of the heat of adsorption of cesium on filamentary tungsten
depending on the method of filament treatment
SOURCE: AN UzSSR. Izvestiya. Seriya fiziko-matematicheakikh nauk, no. 1, 1966,
65-68
TOPIC TAGS: cesium, tungsten, adsorption
ABSTRACT: The problem investigated was the behavior of cesium on tungsten. For
this purpose, a study was made in a sealed devfte placed in a thermostat, in which,
various vapor pressures of cesium could be created, corresponding to a temperature;~--
range from -180 to +100C. All the basic'inputs of the device were fitted into
glass tubes, which were heated by small heaters on the outside to prevent the
precipitation of layers of cesium near the inputs an the inner surface of the
glass and the appearance of conductivity between the inputs. The vacuum in the
device with a frozen source of cesium was of the order of 10-9 mm Hg. The
Card 1/2
Car
I "LIMM" 11

T. rP f j' G
P n -21 EW r k/EW Ti r , I
ACC NRt AF6oo9688 SOURCE CODE: up/O:L81/66/008/003/09.36/0938
AUTHOR: DikQ_v%j__L__K.,; Pyt a YR.- G. N.~
ORG: Tashkent State UnivergLty_;W. V. 1. Lep~~(Tashkentskiy gosudarstvennyy uni-
versitet)
inale-crv-stal
_9f the (110) and (111) faces o
TITLE: Thermoelectr f G
t sten coated with a thorium film
un 11
T__
SOURCE. 4. 'Fizika' V
~verdogo t ela?, 8 no. 3, 1966, 936-936
TOPIC TAGS-. thermoelectr1c property, electron emission, tungsten, single crystal,
-work function, metal film, thorium, pressure effect
ABSTRACT: To check on the theoretical conclusions of E. P. Gyftopoulos and I. D..
-Levine (J. Appl. PhYs. v. 33, 67, 1962) that -work-function minima can appear on
thorium films only if deposited on the (110) face of tungsten, the authors
__ate'a in the temperature range 1300--1600K the variation of the emission current with
time following sputtering of thorium on the (110) and (111) faces of monoci-jstalline
strips of -tungsten. The crystals were prepared by a procedure described earlier
._(YN,~uch._'_tT_." Tasshke'nt. g*64. univ., vyp. 221, 123, 1963) and tested in a speciaLly
designeC1n6tr"um-e'n6 3-g-" 1). The -best results have shown that no minima of work
functions occurred for the (110) face at pressures 10-7~_10-9 mr,1 Hg, or for the (ill)
face at 10-8--10-9 mm Hg. The only work-function minima occurred for the (111) face
"when -the residual-gas pressure was k
pproximately 10-'7 mm Ng, and also during the ini-
tial stages of the test, in agreement with the earlier results. The work function
Card 1/2

ijp( --jD w
Jw
ACC NR: Ar-6012475 SOURCE CODE: uF/o18l/66/oo8/oo4/il4o/l146
AUTHOR: Protopopov, 0. D.; Mikheyeva, Ye. V.; Sheynberg, B. N.; Shuppe, G. N.
ORG: Tashkent State University (Tashkentskiy gosudarstvenTWy universitet)
TITLE: Emission parameters of tantalum and molyj~denuj~ single crystals Z
SOURCE: Fizika tverdogo tela, V. 8, noo*X, 1966, 1~4Y-1146
TOPIC TAGS: tantalum, molybdenum, crystal, electron emission, work function,
crystal lattice structure
ABSTRACT: This is a continuation of earlier work (FTT v. 7, 3759, 1965 and others)
devoted to the work function of electrons from different faces of single crystals of
,tungsten and molybdenum. The present investigation reports similar measurements with
large crystals of tantalum, accompanied by new measurements on molybdenum and com,-
paring the results and refining earlier data. Most measurements were made in a
cylindrical system of electrodes (Fig. 1), although some were made with a flat system
of electrodes used in the earlier experiments. The measurements were made by the
Richardson method. The values obtained for the work functions of molybdenum are
q)a.a.o - 5-00 � 0-05, (Pia-- = 4-55 � 0-05, 9,loo - 4.40 � 0.02, and (P111 = 4.10 � 0.02 ev.
The values for tantalum were %jo - 4.80 � 0.02, (ploo = 4-15 � 0.02, and cp1j, = 4*00
� 0.02 ev. The results for tungsten, molybdenum, and tantalum are tabulated and com-
pared, and some of the differences are discussed. It is concluded that for metals
with a body-ceiltered cubic lattice the average work function is closest to that in the
[1001 direction. The difference between the maximum and the minimum work function is
Card

ACC NR, A!16030026 SOURCE CODE: ua/oo2o/66/i6q/0O5/12O9/l2ll
AU-.IIOR*. Shuppe, ff. G.
ORG: none
TITLE: Kinetics of RNA synthesis in living cello
SOURCE: AN SSSR. Doklady, v. 169, no. 5. 1966, 1209-1211
TOPIC TAGS: bioeynthesis, RNA, RNS synthesis, in vivo synthesis
ABSTRACT:
-Total, newly synthesized, cellular RUA consists of a mix-
ture of -uanine-cytosine- and alanine-uracil-type RNA
molecules. The figures comvare theoretical and experi-
mental data an the change in t1he rel;tive amounts of
the types of RNA with time. These relationships can be
-
expressed machematically as shaVU Lbv-z, the agreement of
the theoretical and actual results. TWA-50; CBE X0.111
-SUB CODE: 06/-, SUBM DATE: 15Dec65/ OPIG REF: 0071 OTH REF: 001/
Card 1/1 UDC: 547.963.3

r". r . ;p p I-, I" i ;s~:z i " ~, L DI F! . E' .
- , - I - . - -
GVII~RYANT, K-G-7 p
syr- tj,,e ~ -' ~s c f AU-type RINIA in animal cel'Ls. Dcki. All SSSR 164
1 - ~L -
fic. 6: 14 13-IL, 16 0 165. O~ap-tt 18:10)
1. Subm.1tted 23, 1965.

SYTA-L-~t, *'-'-.F~- SHt--:;~; T' -,
ionization of iodine- a'-cms or- the surface of heated, tar-taltunn,
fiz --.O~ :52-5E ;61.
I ' I -L - - 6 Q (1,11MA 15:1)
Srodneazicl t:;I-iy gosudarstuvezinyy universitet ime-12i Lenina.
(Iodine) (Tantalum) (Tonization)

SMIA, Ye.P.; SHUPPE, N.G.
Measurement of the electrcmic emission with time frcm timgsten
wires calcinated by direct and alternating carrent. Izv.AV SSSR
Ser.fiz. 26 no.UtI3,49-1353 N 162. (MM 150-2)
(Thermionic emission)

SYTAYA, Ye.P.; SHUPPE, N.G.
Surface iznization of iodine and sodiiun on an incandescent
polycrystalline tantalum filament. Nauch. trudy TashGu no.221.
Fiz. nauki no.21:103-112 163. (MIRA 17:4)

-I'.G., SWPPE, T:.G.; IMUL'IIINSKAY~'i~, I.S.
P 4.
RNA synthesis in the presence of small doses of actinomycin.
Dokl. Ali' SSSR 160 no.6:3411-1423 F 165.
(MIRA 18:2)
1. Submitted May 9, 1964.

BABYUKJ, A.G.; MIKRAYLOV, G.D.; SHUPSHPANOV, P,I., red.; SERGEYEVA,
A.S.I. takhn. red.
[Using ultrasonic techniques for the formation of emulsions;
practical work in physics]Poluchenie emullsii pri pomoshchi
ul'trazvuka; praktikum po fizike. Pod red. Shushpanova, P.I.
M6skva, No.28. 1962. 17 p. (MIRA 16:3)
1. Moscow. Institut narodnogo khozyaystva,
(Ultrasonic waves-Industrial applications) (Emulsions)

NIKOLAYCHUK, K.L., iuzh.;,SHUPTA S.S - ELIMESOV, O.A., slesar'; ZFMR TSOV,
F.M., master; GOIVZ'~ v A.M., mashinist elektrovoza.
Workers of Barabinek train shed. Ilek. i tepl. tiaga no.11:32-34 N
157. (MLRA 10:11)
1. 3hrabinsk, elektroyoznoye depo, Omakaya doroga. 2. Korrespondent
gazety "Cmakiy zheleznodorozhnik"'(for Shupta).
(Railroads--Maintenance and repair)

SHU,iYATSKIY, A.B.
I - ~--vel6city and shape of water and rain drops, TruAy
TSAO no. 22-.73-88 157. (NM llx4)
(Drops-measurements)

- SHUPUTSKIY A.B,
7!nz;;P~ , - - ~
-''l -
Investigating precipitations by radar using the standard-target
method. Trudy TSAO no,'22::89-95 157. (KM- 11W
(Precipitation (Meteorology)) (Radar mateorolog7)

SHUPYATSKIY. A.B.
Radar technique of measuring the average size
of drops during heavy rainfalls. Trudy TSAO
(Radar metisorology) (Drops)
and concentration
no-20:58-66 '58.
(MIRL 12: 1)

SHUPYRTSKlY, A.B.
Photoimpact method of measuring the
Triuly TSAO no.20:88-94 '58.
(Drops--Photographic
epectriuq of raindrops.
(MIU 12: 1)
measurements)

SH=AT-cn.=, A. B., Cavdidate Phys-Math Sci (diss) -- "Long-distance measurement
of -the intensity of precipitation by the radar method". Leningrad, 1959. 9 -op
( NIELin Geophys Observatory im A, 1, Voyeykov), 120 copies (KL.,'No 22, 19591 109)

3(7) PHASE I BOOK M~PLOITATION SOV/3030
Leningrad. Tsentrallne-ya aerologicheskaya cibseinratoriya
Nekotoryye voprosy fiziki oblakov (Scme Problems in Cloud Physics)
Moscow, Gidrometeoizdat (otd.) 1959. 94 P. (Series: Its: Trudy,
VYP- 30) 650 copies printed.
9-ponsoring Agency: GlaYnQye 91drCMeteOrojQ8iCh-3skqy sluzhby.
Ed. (title page): A.M. Bororikova; Ed. (inside book): M.I. Sorokina;
Tech. Ed.: T. Zemtsova.
PURPOSE- This collection of articles is intended for meteorologists and geophys-
icists.
COVERAGE: This is a collection of seven articles on problems in cloud physics.
All articles were written between 1955-1958 but their publication wa3 .,rithheld for
technical reasons. Individual articles discuss the origin of-th,e subfroutal
section in warm front cloud systems,radar scattering by non-spherical particlers,
unipolar charges in aerosols and atmospheric electricityand the conditions of
Card 1/3

Some Problems in Cloud Physics
SOV/3030
ice crystal grovth in the free atmosphere. A base line theodolite method for
surveying clouds is described, and a 'ecimpound for obtaining replicas of cloud
elements discussed. References.accompany individual articles.
TABLE OF COWIENTS:
Tsito'vich, T.A. Formation of the Subfrontal Section of a Warm Front
Cloud System. 3
Shupyatslriy, A.B. Radar Scattering by Non-Spherical Particles 39
Reahetov, V.D. Analysis of Unipolar Charges in Aerosols 53
Reshetov, V.D. The Problem of Atmospheric Electricity and Aerokols 62
Britayev, A.S., and A.N. Korneyev. Coagulational Growth of Ice
Crystals 73'
Korneyev, A.N.,and B.N. Trubnikov. The Use of Crystal Replicas
in Investigating Cloud Elements 81
Card 2/3

SHUPYATSKIY, A.B.
Daterming the shape and velocity
gidrol. no.4:42-43 Ap '59.
(Drops) (Precipitation
of falling droplets. Meteor.
(MIRA 12:5)
(Meteorology))

-THOR: Shupyatskiy, A, B. /10-59-4-8/21
T 1'_P L Detm-,unin.-_ the Sh,-n. e. jrd Spc-_1 of F~,Plin,! Drops Nprr~del--Iiye formy
i skorosti padayushchik~-~ krip,311)
PERIODICAL: Meteoroloriya i f:idrologiya, 195, :--r 5, T-P 42-13 (USSTZ)
AB~WRACT: A plant mounted in the Tsentral~naya acrologicneskaya
observatoriya (Central Aerologicni Observatory) is described
here, and the results of the experiments for mon3uring the
shape and speed'of falling drops are given. The plant is
based on the induction principle (Ref 1). The further
devel(Ipment of - this pi~inciple ,.vade it possible to determine
not onl,' , the falling speed of the drops but also their shape
awl dimensions simultaneousi~-- w--th the speed. The receiving
part of the plant consisted of '~ onen rings of silver-plated
3-mm wirb which ivere placed on plexiglass insulators in an
earthed metalscreen. ~he diameter of the rings varied between
15 and 3 cm according to the senzibility required. The drop
carrying the electric charge flow ~hrou_-h the first ring and
induced on the conductor a pulse -.-,hich was conducted through
the screened cable to the in-,,ut of the four-stage pulse
Card 1/2 amDlifier., After the amnlification, the signal vias di-~rided up

.Determining the Shape and Speed of Falling 'Drops Is 10 7i/50-59--s- .121
into 2 canals. One was us~_-", for iricasur-In-g the s-Deed, _'-ae other
for photographing. The charged drop flying through did not only
give for measurin'- its flyin- sF~~!ed but controlled
atically the ignition of the illizminating lamp, the
autor - k,
short-termed light pulse of which --,ade it possible to
photogra-uh the drop at t;--, :z,.u:iient wher:_~ its -Plying _s
determined. - The plant ai~-o per~Attei n-tural sun:::,:!r rai-.ndro-pc
to be registered, The r.IeaF=ements aere in sum-ier 1PI;'.
in the District of the town. of Dolg--?rudny-y, ~.Iozcovr oblf-.St
The photos of the falling ~IroDs sho-a that big drops - bez-.-.-een
r = 1,5 ---ind 2,C mm - -lo not sho~~,r a z-,3heric~il sh-are in falling
as a rule. The amount of Cefor!--iation is determined by thr~
fallinE speed, the mass of the dron and the resistance
coefficient of the mediurr,, "here are 2 tfigures and 1 reference.
Card 2/2

SHUPYATSKIY, A.B.
---------------
T--
Scattoring of radio wave2 by nonspheriCal Darticles. Trudy MO
no.30:39-52 '59. (14IR& 12: 9)
(Radar meteorology) (Cloud physics)

PHASE I BOOK EXPLOITATION sov/5o83
Shupyatskiy, Arkadiy Borisovich
---------------
Radiolokatsionnoye izmereniye intensivnosti i nekotorykh drug1kh
kharakteristik osadkov (Radar Measurement of the Intensity of
Precipitations and of Some of Their Other Characteristics)
Moscow, Gidrometeoizdat, 1960. 118 p. 1,200 copies printed.
Sponsoring Agency: Glavnoye upravleniye gidrometeorologicheskoy
sluzhby pri Sovete ministrov SSSR. Tsentrallnaya aerologiches-
kaya observatoriya.
Ed. (Title page): V. V. Kostarev; Ed.: M. 1. Sorokina; Tech. Ed.:
T. Ye. Zemtsova.
PURPOSE: This book is intended for meteorologists, aerologists,
hydrologists and specialists in the application of radar in
meteorology.
COVERAGE: The book discusses the theoretical and experimental
bases for measuring macro- and microphysical characteristics
of precipitation by means of radar. Theoretical
Card V5-

Radar Measurement (cont.)
SOV/5083
developments, methods and instruments, and various precipltation
characteristics measured by means of radar are described. No
personalities are mentioned. There are 78 references: 43
Soviet, 30 English, and 5 German.
TABLE OF CONTENTS:
Foreword 3
Introduction 4
Ch. I. Theory of Radar Detection of Clouds and Precipitation
1. Elementary theory of radar detection 7
2. Theory of locating , atmospheric formations with radar.
Effective surface of spherical particles 11
Ch. II. Experimental Investigation of the Microstructure of
Liquid Precipitations
1. MeasurIng the rate of fall and investigating the form
of falling water and raIndrops 21
Card-~

.. SHUPYATSKIY, A.B.
-------
Possibility of estimating the water cohtent of clouds by the
minimal detectable ocho-signal. Trudy TSAO no-35:66-78 160-
(MIRA 13:11)
(Radar meteorology) (Cloud physics)

S/194/62/000/007/122/160
J D413/D308
AUTHORS: Gerzhenzon, Yu.1,1., and Shupyatskiyt A.Bt-
TITLE: The scattering of elliptically-polarized radio waves
by non-spherical particles in the atmosphere
PERIODICAL: Re-L-erativnyy zhurnal. Avtomatika i radioelektronika,
no. 7, 1962, abstract 7-7-36 m (Tr. Tsentr. aerol. ob-
serv.s_no. 36, 1961,102 -108)
A
TEXT: The paper considers the theoretical questions of using ellipT,
tically-polarized waves for the radar investigation of non-spheri-,,-
cal particles in clouds and precipitation. Water-and ice'particles_~
are represented approximately as ellipsoids of revolution. From a
General expression *for the echo signal from a collection of non-
spherical particles with elliptical polarization, the particular
gases follow the magnitude of radar scattering for circular and li-
near polarizationsv as a function of the form, orientation and phas-e
state of the particles. The advantages of using elliptically polaii-
zed radiation are demonstrated. It.foTlows from the calculations
that by varying the parameters of the polarization one radar can
Card 1/2

SHUEYATSKIY, A.B.; MORGUNOV, S.F.
Application of el2iptically polarized radio waves for studying clouds
and precipitatiorror,"Dokl. AN SSSR 140 no.3:591-,1;94 s 161.
(MIRA 14:9)
1. TSentral'naya aerologicheskaya.obserTatori7a. PrefttaVIOMO
akedemikam Ye.K. Fedorovym.
(Radar meteorology)

ACCESSIO,'LI N-11: A.T4011397 S/2789/63/000/047/0063/0084
AUTHOR: Minervin, V. Yo.; Shupyatskiy,.A. B.
TITLB: Radar method of determining the phase state of clouds and precipitation
SOURCE-: Tsentrallnaya aerologichaskaya observatoriya. Trudy*, no. 47, 1963.
Fizika oblakov, 63-84
TOPIC TAGS: clouds, precipitation, meteorology,,keteorological radar, phase
state, polarization, cloud particle, cloud physics, cumulonimbus cloud, nimbus
cloud, cloud modification, aircraft icing, aircraft sounding, radiosonde, lea
crystal, snow
ABSTIL4,CT: The Taentrallnaya aerologichoskaya bbservatoriya (Central Aerological
Observatory) has developed a method for determining the phase state of clouds
and precipitation which is based on the use of the dependence of the polarization
properties of scattering particles on their form. The observational apparatus is
described; the polarization apparatus is shown schematically in the Enclosure.
Methods and observation errors are discussed. A nil or of examples of the dis-
tribution of the phase state of cloud and precipitation particles in space and
time are given. The-experimental results are compared vith data obtained by air-
1/41
C=rd

ACCESSION NR: AT4011397
craft and radi6sonde soundings. This radar-4wthod makes it possible to evaluate
the shape of the particles forming the echo signal, thereby indicating phase
state. The crystallization level in cumulonimbus and nimbus clouds can be deter-:.
mined from the ground. Si'milarly, phase transition can be observed at the time ;
of artificial modification of the supercooled part of the cloud and zones of pos-_
sible aircraft icing can be determined. Areas between vater-drop and mixed
clouds which are filled with falling snov can be detected, which in impossible
with other radars. Ma layer of thawing and change of particle shape during
thawing can be determined. However, at this time only clouds and precipitation
situated directly over the station antenna can be investigated, but means for
increasing the potential of the apparatus are proposed. Orig. art. has: 7 fi-
gures, 7 formulas and 5 tables.
ASSOCIATION: Teentrallnaya aerologicheskaya, observatoriya (Centr&1 Aerological
Observatory)
SUBMITTED: 00 DATE ACQ: 24Feb64 ENCL: 02
SUB CODE;': AS NO REF SOV: 005 OTMM: 001
Card --3/4

ACCESSIM NR: AR4015468 S/Ol69/63/OOO/Ol2/BOO5/BOO5
SOURCE: RZh. Geofizika, Abs. 12B37
AUTHOR: Morgunov, B. P.; Trifonov, G. P.; Bhupyatskiy, A. B.
TITLE: Radar apparatus for polarization investigations of clouds and precipitations
CITED SOURCE: Tr. Tsentr. aerol. observ., vy*p. 48, 1963, lo6-lli
TOPIC TAGS: weather radar, echo-signals, polarizing converter, 3-cm radar meteoro~-
logical objects
TFANSLATION,: The apparatus is built on the base of a high-potential 3-cm radar
set. It has two zenith-pointing identical 3-cm antennas. One antenna is used for
transmitting and receiving the signal, the other for reception only. Echo-signals
from both antennas are fed into the input of the common receiver through a change-
over switch and an attenuator and then to the recording device. Conversion of
polarization is done in the first transceiving channel. The polarizing converter
is made in the form of a quarter-wavearray consisting of metallic plates mounted
on foam plastic. The array is located near the radiating horn and travels in the
direction of rotation. The action of such a converter is analogous to the action
of a quarter-wave optical plate. The apparatus makes it possible to analyze echo-
I. Card 1/2

ACCESSION NR: AR4015468 - - '-' - - --- - - ---- -
signals from different meteorological objeCtB at different altitudes in a wide
dynamic range. N. Zolotavina.
DATE ACQ: og.Tan64 SUB CODE: AS, PH ENCL: 00

MINERVIN, SHUPYATSKIY, A.B.
of mdar in determlning the phase stalte of clouds and
precipitation. Trudy 'TSAO no.47~63-81' 163. 2.~,j:2.jj-)

Sum- of -Lij~~zr, unr
congesmus cj-cu, , and L~A,
164.

'~IORGUITOV, S,11,; SIRWYA'-PSKIYv AeBs
Evaluation of tho affbotiveness of modifloation by the
polu-Ioation characteristics of a target vignale Tructr
T.SAO no.57:49-54 1646 (M PA 19 3 1)

ACC Mmi AR5012910 UR/O169/65/00O/0WBOY1/BO34
551-576
SOURCE: Ref. zh. Geofizika, Abs. 3B215
AUMOR: Boravilarr., A.M.; Kostarev, V.V.; ShupyatsISIX, A.B.
------------a
TITIB: Equipment and methods used in rad observations of the evolution of heavy
cumulous and cumulo-pluvial clouds ?r
CITED SOURCE: Tr. Vses. i3oveshchaniya Do aktivn. vozdeystviyam na grad. vrotBessy*
Thilisi 1964, 210-216
TOPIC TAGS: atmospheric cloud physics meteorologic radar,'rm~~'-C~'Servc~tr-qq
TIMNSIATION: A description is given of the equipment and methods used in radar ob-
c;ervat-'Lons for explorinG the evolution of,heavy cuinulous and cumulo-aimbus clouds
which have developed naturally and those affected by reactions, for detemining the
radar signals of hail clouds, and for determininS criteria in evaluating reaction ef-
fects. Specifications are Given for ra-dar station-- vh:Lch are intended to carry out
such observations. Some technical data on the radar station Which was used are given
Tkemethod of vertical profiles is considered to be the most efficient for conducting
radar observations. A circular observation vas used for evaluating the situation in
the observed region, the selection of the subject to be observed, and the determina-
rd 1,L2

T. I (,AI~6_AA
ACC NR: PE5012910
tion of the azimuth of the most intensive reflection zone. Quantitative measurements
were made by means of the iso-echo method,-with the help of a specially designed
calibrated attenuator. The initial profile of the observed hail center was done by a
fully cut-off attenuator, and the zone of the radar picture seen on the circular ob-
servation screen-was, in this case of a larger scale. Subsequently, the profiles
were repeated with a gradual-ly increasing attenuation until the fadIng picture vanish-
ed entirely from the screen. The picture on the screen was photographed with a movie
camera. The overlapping of the photographic series made it possible to obtain a to-
pography of the intensity of the reflected signal in the vertical profile, and based
on these data, it was possible to build the vertical profile of the radar's reflecting
ability Z. The value of the latter is the most reliable of the radar characteristics
of a hail center., because it is not affected by the parameter of the station, nor by
distance. An estimate was made of the possible Lmrrors due to the attenuation of the
radiowaves propagating in the observed precijpitation. A. Borovikov.
suB coDE: o4
CGj7r2j/2
d

Z EWT 11. FCC G 1.41 WR
A
7RI AR5o12916 169/65/boo/oo3
CE UR/0 A093/BO94
551-509.6
SOURCE: Ref. zh. Geofizika Abs. 3B564
AUTHOR: Bo*ravik(:)v A.M.'- Kostarey, V-V.; ShMjWx"14X~ AB.
TITIE: Results of radar observations of the evolution of heavy cumul ous and cumulo-
nimbus clouds un~pr the effect of artificial influence
C11MIr SOURCE: Tr. Vses. soveshchaniya Po aktivn. vozdeystviyam, na grad. Protsessyd
Tbilisi 217--Z3-~!-
TOPIC TAGS: atmospheric cloud, cloidphysics, meteorologic radar
4M.1962
TRANSIATION. On the basis of analyses of radar observations conductecl in (4 19
lition on.the evolut
by the Samsarskaya expec ion of cumulo-nimbus clouds,P,9~& e
nary radar signs were established regarding.the.,hail-carrying capacity of clouds.
in order to discover these signs, certain radarcharacteristics applicable to clouds
were used, namely: the range of the maximal radar reflection and its.position in the
cloud; the stratum of an increased.reflection. zone and its position in the cloud*
the alt:Ltudes of these zones and theJ-r characterlstle- temperatures. One should lexw;
vhen: 1) the range of'radar reflecti lo-9sm3'
pect a precipitation of hail onis,>
zone of increased reflection is in a minimal 3-3.5 km strata and is either sym....-.
C,l,d_l
12
L
'Card 2

SHUFY*ATSKIY, M.G. , podpolkovnik meditsinekoy sliazhby
-1 --- -1- -, -~- -,
Unusual case of botulism. Voen. mad. zhur. no.4:25-26 Ap '59.
(BOTULISM, case reports, (MIRA 12:8)
unusual case (Rua))

4N/5
856
.S5
Shupyk, P L
3os,,'ahnenWa okhorony zdDrovlya
v Ukraij-.)3Ikiy IISR (Accomplishments
in 'Public Health in the Ukraine)
K.vyiv, Derzhinedvydav, URSR, 1958.
723 P. ports., tables.
At head of title: Ukraine. MizOster-
stvo Zdravooldiraneniya.
Bibliografiya: p. 671-723

SHM. A.
Continuous flov heat treatment of steel plates. Stall 15 no.2:186-
187 F '55. -(KM 8:5 )
1. Giprostall.
(Plates, Iron and steel--Heat treatment)

SITUR A., inzbenor; 4A-RIYENGOF, G., inzhoner.
PrAcast reinforced concrete stairs made of large elements.
Stroi. riat., izdel. I konatr. 2 no.7:18-lq J1 '56. (XLRA 9:10)
(Stair building) (Precast concrete)

SHUR, A., inzh.
Mechanized
no.11:5 N
application of bituminous waterproofing. Stroitell
157. (MIRA 10:12)
(Waterproofing)
(Spraying and dusting equipment)

05934
9( SOV/107-59-7-37/42
AUTHOR. Shur., A., - Bornovolokov, E.
-----------
TITLE:: Intercom Circuits (A Review of Foreign Designs)
PERIODICAL- Radio., 1959, Nr 7. PP 55-58 (USSR)
ABSTRACT: The authors describe in detail an intercom device
without indicating its origin. They mention in this
connection that Soviet made intercom devices DKZ-40
and DKZ-70 have electronic commutators switching the
units automatically to transmission as soon as the
first word is spoken. The intercom device described
in this article is built of four tubes. There are
three DF 191 for which the Soviet lKlP tube is re-
commended. The DL 192 has the 2PlP as an equivalent.
An amplifier station used with intercom devices con-
sists of tubes, DC-11, one DF-11 and two DL-11. The
Russian equivalents of these tiYoes are lKlP, lKlP,
-!KlP. and 2PlP, respectively, Wiring and transformer
core data were also converted to Russian designations.
Card 1/1 There are 5 circuit diagrams.

9(2)
AUTHOR: Shur, A.
TITLE: A Noise Generator (Generator shuma)
PERIODICAL: Radio, 1959, Nr 4, pp 41 - 43 (USSR)
ABSTRACT: The author explains in general the origin of thermal
noise and describes a noise generator used for tuning
ultrashort-wave receivers and for establishing their
noise factor. Expecially when building receivers
working in the range of 144 me and higher, does the
determination of the noise factor become important.
The generator suggested by the author may be easily
built and consists of 4 DGTs-24 diodes in the rec-
tifier unit and one 2D2S diode in the noise genera-
tor section, as shown in Figure 2. This device may
be used for testing receivers working on frequencies
of up to 300 me. The author explains in detail the
technique of applying this noise generator. There are
3 circuits, 1 sketch, 1 graph, 1 block diagram, and
2 Soviet references.
Card 1/1

SHUR, k. ; 1101XMIT, E.
Intercommunication system using transistor amplifiers. Radio
no.2:50-51 F 160. (MIRR 13:5)
(Transistor amplifiers)
(Intercommunication systems)

SHUR,--A., inzh.
Tuning and testing of shortwave antennas. Radio no,2:48-.11 F
,61. (MIR-A 14: 9 )
(Radio, Shortwave--Aritennas)

AUTHORS:
TITLE:
22271
S/109/61/006/005/018/027
D201/D303
Shur, A.A.,
A method of measuring radio-waves phase fluctuations
in the study of long distance troT~oQnbp-ri^ wrnrc~aa+4-
-Jr.
PERIODICAL: Radiotekhnika i elektronika, v.- no. 5, 1961,
828 - 829
TEXT: The known methods of measuring the phase fluctuations of
radioWaves propagated in the troposphere, although presenting much
interest from the theoretical and practical,pointB of view, are
very compl-'cated and cumbersome. In the present short communicati-
on, the authors describe a simple method of measurement as based
on the Hyquist principle (Ref. 3: H. Hyquist, S. Brand, Bell Sys-
tem Techn. J., 1930, 9, 522). The block diagram of the measuring
installation is given in Pig. 1. The transmitting installations
consist of the transmitter 1, modulator 2 and filter-receiver 3.
The receiving end consists of the receiver 4, phase-meter 5 with
Card 1/5
_1/

22271
S/109/61/006/005/018/027
A method of measuring ... D201/D303
an oscilloscope 6 and the receiver-filter 7. The principle of
operation is as follows: At the tz-arismitting end of the.path under
investigation the filter receiver 3 receives the signal from an
independent transmitter 8. It amplifies only the carrier frequency
of thig signal and attenuates all the components of the spectrum.
The filter 3 is at the input of a frequency modulator 2 of trans-
mitter 1. At the receiving end the carrier is compared in phase
with the carrier of the-same station 8 at the output of the recei-
ver. The phase difference between the two waves depends, therefore,
only on the conditions of propagation along the path. According to
the Hyquist principle, the signal spectrum of the transmitter must
be much smaller than the pass-band of the whole installation. There
the phase difference rf of the signal going through the installa-
tion is
CP ~ (2 T (w
where n - the angular frequency of the modulating wave, and T(w) -
the group time delay at the carrier frequency w. It can be shown
Card 2A

22Z I-L
S/109/61/006/005/018/027
A method of measuring D201/D303
also that the time delay between two waves scattered or reflected
from the inhomogeneities spaced by.heights Ah is equal to
T(w) R 46 h
Rec
where R - -the length of the propagation path, Re - the effective
radius of Earth; c - velocity of light in free space (c = 3 . 105
km/sec). The above method has been applied at an experimental path
of tropospheric propagation with normal TR installations with
added filters and phasemeter. The length of the path was 300 km,
measurements were made at a carrier frequency of 1,000 mc/s. The
transmitter carrier was modulated � 2.5 mc/s at 50 c/s. The filter-
receiver had 3 stages of RP amplification using 6)kl'n (6ZhlP) val-
ves and a crystal filter with a pass-band of 80 c/s. There are 1
figure and 3 non-Soviet-bloc references. The references to the
English-language publications read as follows: J.W. Herbstreit,
M.C. Thompson, Measurements of the.phase of Radiowaves received
Card 3A

22271
S/10 61/006/005/018/027
A method of measuring D201YD303
over transmission path with electrical lengths
of atmospheric turbulence, Proc. I.R.E., 1955,
Deam, B.M. Fannin, Phase-difference variations
radio signals arriving at-spaced antennas, Pro,,.
10, 1 02 [Abstractor's note: Error in spelling
4
H. Hyquist, S. Brandt Bell System - Techn. J.,
SUBMITTED: February 16, 1960
varying as a result
43, 10, 1391; A.P.
in 9,350-megacycle
I.R.E. 1955 43t-
of word pace'l
S dj;
1930, 9, 5~2.
Card 4/5~
q

BO-;?I!OVOL.OKOV,, Eduard Favlovich; VEYDLQIIS, Avgust Yakubovich; ROMIOV,
Boris A2eksandrovich;,_SHUR, Anatoliy Abele-vich; SOBOLEVSKIY, A.G..,
red.- LARIONOV, G.Ye.,
3 t&!-Jm. red.
[Loudspeaker systems] Peregovornye ustroistva. Moskva Gosenergo-
izdat, 1962. 38 p. (Massovaia radiobiblioteka, no.431i
(MIRA 15:7)
(Intercommunication systems)

42275
s/8og/62/000/000/002/003
B192/E382
AUTHOR: Shur, A.A.
TITLE: A high-sensitivity instrument for measuring the strength
of UHF fields
SOURCE: Novyye razrabotki v oblasti kontr:ol1no-izmeritel'jjoy
apparatury; informatsionnyy sbornik. Ed. by
A.S. Vladimirov. Moscow, Svyazizdat, 1962, 16 - 21
T EX T The development of a high-sensitivity fleld-strength
meter was necessary in order to measure the field strengths on
radio-relaying links operating at decimetre wavelengths,since the
fields on such communications routes can be 50 - 90 db lower than
the free-space fields. The most rational-way of increasing the
sensitivity of a measuring receiver is'the narrowing of its
operating bandwidth, which is defined by (A.A. Kulikovskiy
Lineynyye kaskady radlopriyemnikov (Linear stages in radio-
amplifiers), Gosenergoizdat, 1958):
f = 2 f3+ 2VF(" 2 + (Y'r r_1 )2-
Card 1/4 1 . I

S/809/62/Ooo/ooo/oo2/603
A high-sensi-tivity E192/E,382
where /Af is the bandwidth of the recelver., Y.- and Y. are the
expected instability factors of the local oscillator and transmitter
frequencies, respectively, - fl- and f,n are the highest local
oscillator and transmitter frequencies, respectively, and f- is
the highest signal-fluctuation frequency4 Assuming that
fr = f I-\ = 2 000 Mc/s and yr = YrI = 10 f3 = 10 c.p.s. and the
noise figure of the receiver N = 25 , eq. (1) gives A'~f = 0.6 Mc/s,
if' the noise at the output of the receiver is
o.6 x io-13 W. The sensitivity can be improved by increasing the
-~t_ability of the local oscillator and the transmitter but this
approach is uneconomic. A different way of tackling the problem
is as follows. The receiver of the equipment has a narrow band-
width and it is periodically tuned to the transmitter frequency by
varying the local oscillator frequency by an amount /-^Nf 2
(see Fig. la). When the frequency difference between the local
oscillator and a signal is equal to the intermediate frequency of
C,-%rd. 2/4

A high-sensitivity ....
S/809/62/000/000/002/003
E192/E382
tile receiver, a pulse is produced at the output (Fig. IE) whose
amplitude is proportional to the level of the received signal.
The continuous signal received is therefore converted into discrete
pulses whose peak value is measured by a pe~ak-readlng voltmeter.,
The relationship between /-\-f, pulse duration -r- , Z!~f 2 and the
period of the modulation signal'of the local oscillator is:
Af
11,M Af
By combining
bandwidth can
becomes 3.47
constructed.
1 765 Mc/s, the
+ 1.5 Mc/s.
was 50 c.p.s.
was 27 INIc/s,
Card 3/4
(2)
this formula with Eq. (1), it is found that the
be reduced to about 3.5 kc/s and the output noise
x 10- 16 W. Equipment based on this principle was*
This covered the frequency range from 2 000 to
automatic detuning of the local oscillator being
The modulation frequency of the local oscillator
The first intermediate frequency of the receiver
while the sec-ond Intermedlate frequency was

s/8og/62/000/000/002/003
A high-sensitivity .... E192/E382
0.465 Mc/s. The operating bandwidth of the,second intermediate
frequency amplifier was 12.3 kc/s. The maximum sensitivity of the
system was better than 8.5 x 10-15 W (or 0.8 IiV across the input
impedance of 75 _--L ). The time constant of the capacitive circuit
of the peak voltage-detector was 16 ,Ls for charging and 0.14 sec
for discharging. The instrument was capable of following fading
phenomena occurring at frequencies not higher than 25 c-P.s.
There are 4 figures.
FiE. 1:
I T7, T,
M
2H
J �i1=L_j
IF amplifier output
voltage
~S = 181 011 1
Card 4/4 - 1%

ACCESSION NR: AP4042500 S/0106/64/000/007/0001/0012
AUTHM Kalinin, A. I.; Troitskiy, Vs Ao
TITLE: Statistical characteristic of a signal during long-range
propagation of ultrashort waves
SOURCE: Elektrosvyazl, no. 7, 1964, 1-12 z
TOPIC TAGS: tropospheric wave attenuation slow signal fading,
signal statistical characteristic, wide band transmission, spacial
correlation radius, frequency correlation radius, fading statistical
distribution
ABS.TRACT: The results are presented of an investigation of long-.
range tropospheric propagation. Measurements %;pre -ifiade' at
30-40-cm wavelengths along routes 159, 303, 44-8, 630' and 13U km
~~in le-ngth and at 8-9-cm wavelengthsalong routes 85, 105, and 303 kid
jf
in length. Receiver-tr,anamitter equipment and antennas used made
I:it possible to measure the attenuation factor V - -118 db for the
30-40-cm wavelength along the 730 km route and V - -106 db for the 8t*
9-cm wavelength along the 303 km route. Th' error of measuring..signal-
!level values did not exceed +1.3 db. -According to the exper ants,
1/2
Cor4
J,
Cor'7

KfiJ-11TIN, A~I.F, TPOITS-KiY, V.N.j SHUR, A.A.
Stativattial cba:ract-iristlcs of a signa! in long-dis-.,ance microwave prc--
pagation. Elektrosviazl 18 no.7sl-2-2- J'l '64. (MLRA 17.-10)

N;Zt
AM502T749 Monograph UR/
_Ar.narjq,_ 11. A.1 Vvedenskiy, B. A. Guayatin3kiy, I. A.; Igoshev, I.P.;
Kazalv v, L YK-.-; Kalin n A. .; -Wdi~arova, L. G.; Nem1-rdVdYXY;--A-.
-So-Tc- o-v7-A=..; Taraeov, --
-c~j 13 n
L I p., A:. ; T 7YA.; ol
Tashkov, P. S.; Ti o, rov, A.; Troitskiy, V. H. Fedorova, L. V.j
/I ---~y-~ S 17r1n,
_.-,Nj!jrn Shabe ni[Eo 7 K. V ; antrey,-R. A 'CA* X~!, j
Shur, A. A.;;YAkovlev, 0. 1 j KolcGov, H. A.1 Levii~.L. r.j LoO=Ian, . no
Upper tjrop~~a heric ProValrationlortg1raohOrt radio waves (Dallneye
tropo-BTernoye raup-r-ostraneniye ulltrakorotkikh radiovoln) Moscow,
Izd-vo "Sovetokoye radio", 1965, 414 P- illus., biblio. 4000
copies printed.
Y?OPIC TAGSt radio wave propagation, tropospheric radio wave, radio
-, communication, space communication,tropoBpheric scatter communicat-
~A Ion, signal processing, signal distortion, field theory
PURPOSE AND COVERAGE: This monograph Is Intended for specialists
working in the field of radiowave propagation, designers of long-
distance radio communication systems, and teachers and students of
the advanced coursea In schools of higher tech=tcal education.. The'
monograph contains, for the most part, heretofore unpublished
reoults or soviet experimental and theoretical investigations in the
field of long-distance tropospherio ultrashortwave propagation.
Card I An N'r UAC -
-2/-XP/ - Zy

&CC NR% AM5027749
Problems of investigating the troposphere by means of refracto-
meters, the mean level of signals, meteorological conditions and
topography, fluctuation of arrival angles and distortions of antenna"
directivity pattornptIoDaen In antenna gain, and quick and slow
fadinga of signal levels are discussed. The statistical character-
iatics of the signals at diversity reception in time, apace, fre-
quency and angle as well as the distortion of signals In the commun-
ication systems are also investigated. The long-distance propagat-
theory to analyzed, and the engineering method of calculating field
Intenalty at long-dintance tropospheric propagation is given, At -
present, there in no theory of Long-DIatance Tropospheric Propagat-
ion which can be applied effectively enough in practice. Thus, In
the Investigation of that propagation, considerable attention has
to be paid to experiments. The special characteriatics or geograph-
ical conditions of the territory involved should be taken into con-
sideration during the analysis of experimental data and in their
practical application because the conditions of propagation in
arctic and tropical climates differ from those existing over seas
and*continents. A considerable part of the monograph deals with
the investigatioreof long-distance tropospheric propagation carried
out over dry'land routes, 800 km long, In the central part of the
USSR under the general supervision of B. A. Vvedenskly and A* G.-
Arenberg (up-to 1957). V. 1. 31foroy Iniestigated problms Cori-
Card

AM5027749
nected. with distortions and fluctuations or signals*
rollow oach chapter.
TABLE OF COInMUS z
References
Foreword
Ch. 1. Radio Engineering Methods of Investigating the Troposphere
Diolectria Constant -- 5
Bibliography -- 16
Ph. 11. Results of Troposphere Dlelectric Constant Measurements 17
1. Relationship between the mean value of the air refraction Index
and altitude. Standard radio-atmosphere - 17
,2. Fluctuations or the air refraction index- -- 24
3. Some notIons on the troposphere model -- 43
Bibliography 45
Ch. 3:11. Average (mean) Signal Levels In Long Distance Tropospheric
Propagation or Ultrashort Waves ( LT. P - U S W) - 48

Qt
AOCC MR;
Ar,15027749
1. Equipment and measuring methods for the mean signal level 48
2. Signal attenuation function in LTP USW -- 54
3. Relationship between mean signal level and the distance 57
4. Relationship between mean signal level and the wavelength 63
5. Relationship of mean signal level and-the shadow angko.of both
transmitting and receiving antennas --1-.65
6. Diurnal and seasonal variations of mean signal level T2
Bibliography 75
'Ch-' IV. Effect of Air Refraction Index at the Earth Surface an the
I-loan Field Level in =P USW -- 77
1. Correlation of the mean field level with the air refraction
index at the Earth Surface. -- 77
2. Possibility of predicting field Intensity variations 81
Bibliography 86
Ch. V. Fluctuation of Radiawave Arrival Aggles and Instantaneous
Patterns of Antennas Directivities
1. Methods of measuring radiowave arrival anglear-and recording of
Instantaneous antenna directional patterns U9

Al-15027749
2. Fluctuation of radiowave, arrival angles in horizontal an4 vertical
planes -- 92
3. Instantaneous antenna directional patterns 92
Bibliography 102
Ch. V1. Louses in Antenna Gain of MP USW -- 103
1. Determination and methods of measuring loscen-in antenna gain 11
2. Experimental data on losses in antenna gain -- 108
3. Theoretical investigations on losses in antenna gain 114
Bibliography 120
Ch. V11. Theories of Long Distance Tropospheric Propagation of
USW -- 122
1. Introductory remarks 122
Bibliography 129
2. Theory of scattering radlowaves by tropospheric turbulent
nanhomogeneitLes 130
Cwd SAO

A145027749
Bibliography 150
3. Reflection of radiowaves from dielectric nonhomageneities of
definite dimensions - 151
Bibliography 171
4- Reflections of radiowaven from laminated tropospheric nonhomo-
gencities of random character -- IT2
~'Blbliography 179
Ch. VIII. Engineering Method of Deeign-Calculation of Field Xntensity
1 Attenuation -- 180 181
1. Basic rules of calculation method
2. Diffraction horizon ( a distance, beginning of which, the value
of the field intensity, calculated according to therdiffraotion
formulas is smaller than the measured intensity),, -" 162
3. Determination of field standard attenuation 82'.
4- Meteorological conditions correction 184 -
Local topography correction -- 185
Estimate of losses in antenna gain - 185
card

ACC NRi
IV-15OZr749
7. r3timato of fadings '186
Bibliography 188
.Ch. IX. Statistical Characteristics of the_Envelope, Phase and Fre-
quency of the Random Signal in IRP USW - 189
1. Statistical characteristics or atmosphere dielectric constant
siSnal components In IWP __ 189
2. Distribution-laws for the envelopes and phas e of varloun oignal
components -- 193
3. Distribution laws of sum-signal envelope
4-Nulti-dimenalonal distribution functions of instantaneous value
oe envelopes and phases of the spaced signals in minute Intervals
207
A5. Parameters of multi-dimensional amplitude and phase distribution
i functions of spaced signals -- 210
.,6. Statistical characteristics of instantaneous values of the en-
velopen of spaced signals in minute intervals -- 222
7. Statistical characteristics of Instantaneous values of spaced
signal phases In minute Intervals -- 239
8. Statistical characteristics of Instantaneous value of phase
first derivatives of spaced signals In minute Intervals -- 248

CC NRa
JNM5027749
;-9. Statistical characteristics or instantaneous values of the first
derivative of phase in minute Intervals -- 257
Bibliography -- 260
Q~. ,,X. Experimental Investigations of Rapid and Slow Fadinge in
IT W -- 262
IT us
1. Methods of measuring and processing experimental data -- 262
2. One-dimensional distribution functions of signal Instantaneous
values -- 264
3. One-dimensional distribution functions of signal averaged values-.
278
4. Period and frequency in rapid fluctuations of sigma envelope-283
Bibliography -- 287
Ch. XI. Experimental Investigation of Signal Statistical Character-
istics at Space, Frequency, Time and Angle Diversity Reoeptlon - 288
1. Space-dIversity reception -- 288
2. Frequency-dIversity reception -- 295
3. Time-diveraity reception -- 299
4. Frequency-time diversity reception -- 305
5* Angle-K11versity reception -- 30T
C.rd 8/10

ACC MRs M15027749
Bibliography -- 312
Ch. XII. Investigation of Amplitude-Frequency and Phase-Frequency
Signal Characteristics at LTP -- 314
1. measuring and processing methods of experimental data 314
2. Amplitude-frequency characteristics -- 321
3. Phace-frequency characteristics of LTP channel -- 325
4. Frequency characteristics of signal group time delay 334
Bibliography -- 350
Ch. XIII. Signal Distortion In LTP USW -- 351
1. Theoretical Investigation of distortions appearing in multi-
channel E74 LTP communication systems -- 352
2. Experimental Investigation of distortion In LTP -- 384
3. Distortions appearing during TV transmission over tropospheric
radio links -- 389
Bibliography -- 392
Appendl.x Automation of Signal Statistical Processing 394
1. Quantification of contInuous sIgnale and coding 395
2. Signal quantificatlon Instruments --.39T
c.,,d 9/lo

S:-iVR, A. A.
Crystallography; Magnetite
Zonal variation in the density of a maMetite crystal.
Doki, A!,f SSISR No. 6:977-979 F '52
Gorno-Geolo_-icheskiy Institut Ural Iskogo
Filiala Akademij Nauk SSSR
rcd. 21 Nov. 1951
SO'- Month List Of Russian Accessions, Library of Congress, July 1952 Uncl.

SHUR,A.B., inzhener
Problem of evaluating the distribution Of gas flow by the gas
temperature in the gas uptake. Stall 15 no.7:592-597 Jl 155.
(KLRA 8:9)
1. Yenakiyevskiy metallurgicheakiy zavod.
(Blast)

SOV/133-58-11-2/25
AUTHORS: Levin, L.Ya., Kuzlmin, I.A., Kaylov, V.D. and Shur -B-,---,
--Yu !~!~
TITLE: An Experience in the Operation of a Blast rnace with a
High Top Pressure of 1.5 atm (Opyt raboty dozennykh peche7
s davleniyem na koloshnike 1.5 atm)
PERIODICAL: Stal'. 1958, Nr 11, 964 - 968 (USSR)
ABSTRACT: The operation,rf Nrs 1 and 2 furnaces in the Cherepovets
Works under high top pressure varying up to 1.5 atm is
described. Furnaces operated on a 100% sinter burden of
a basicity CaO/SiO 2 = 1.13 - 1.15 producing foundry and
basic iron. Main operational indices are assembl ed in
Table 1 and mean monthly results for both furnaces in
Table 2. It is concluded that with increasing top pressure
by each 0.1 atm (within a range of 1.0 - 1-5 atm), the
output of furnaces increases on average by 1.91/o. This
increase in the output is due not only to increasing driving
rate but also due to a decrease in the coke rate. The
main factor which permitted decreasing the coke rate was
Card 1/2

SOV/133-58-11-2/25
An Experience in the Operation of a Blast Furnace with a High Top
Pressure of 1.5 atm
an increase in the blast temperature to 950 - 1 000 'C.
The latter was possible due to an increase in the top
pressure. There are 1 figure, 2 tables and 2 Soviet
references.
ASSOCIATION: Cherepovetskiy metallurgicheskiy zavod
(Cherepovets Metallurgical Works)
Card 2/2

SHUR, Aleksandr Borisovich; ITEKRASOV, I.A., inzh., red.; ROZENTSVEYGi-
Ya.D., red. izd-va; ETMSOS, I.M., tekhn. red.
[Smelting pig Iron -;rith a minimum consumption of coke] Vyplavka
chuguna s minimallnym raskhodom koksa. Moskva, Gos. nauchno-
tekhn. izd-vo lit-ry po, chernod. i tsvknoi metallurgiiq 1960. 51 p.
(Min 14:7)
(Cast iron-Metallurgy)

_s /V
3
QOvIi -r-o-i -4/~:,rj
AOTHORS: Yalctibtsiner, N. M. , Trelcalo, S. K. (Candidates of
Technical Sciences), and Shur, A. B. (Engineer)
TITLE: Physical Properties of Fluxed Sinter of the Cherepovets
Plant
PERIODICAL: Stall, 1960, Nr 1, pp 14-18 (USSR)
ABSTRACT: This is a study of sintering problems at the Cherepovets
Metallurgical Plant (Cherepovetskiy metallurgicheskiy
zavod). G F. Grlgorlyevykh, Ye. V. Nevmerzhitskiy,
V. M. Sholeninov, D. L. Grinberg, and E. Ye. Gutman
participated In the work.. The plant is producing
fluxed sinter from beneficiated Olenegorskiy (not
identified) iron deposits and from Pikalevo deposit
(Filcalevskoye mestorozhdeniye) of limestone. At some
periods the pyrite cindevs of plants near Moscow were
added to the char e of sintering plant. The Olenegorskiy
beneficiated ore ~by 1958 data) contains 60.1 to 60.7%
l.3% CaO. The lime-
Fe; 13.2 to 14.1% SiO,; and 1.1 to
Card 1/6 s
stone (amounting to 3 0 kg/ton of inter) contains

Physical Properties of Fluxed Sinter 7711113
of the Cherepovets Plant SOV/133-60-1-4/30
51.5 to 53% CaO; 1.5 to 4% of insoluble resid:-ze (1 to
2% SIO 2) ; and about 0.3% MgO. The determination of
bulk weight of fluxed sinter and the determination of
screen composition and the degree of crushing of sinter
during transportation are described. The Cherepovets
Plant, for the first time In the USSR, used a two-stage
screening of sinter returns. In addition to the regular
screening machines (in the unloading section of sinter-
ing machine), which screen the returns before loading
of sinter into cooler, the additional vibrating, screen-
ing machines for secondary screening of fines rafter
the cooler) are installed. The bulk weight of sinter
varies. It is due to the increase of the apparent
specific weight of sinter pellets with the decrease of
their size, as shown by the experimental data pre%riously
obtained by N. M. Yakubtsiner and Yu. P. Smirnov (see
Fig_ 2). For the study of screened fluxed sinter,
:',ainple~'- were taken t'rom the- conveyors.
The results
ar-- -iven in ~ig. 4. The Lests'show that the secondary
screening of rCtUrns is expedient. However, the con-
Card 2/6 secutive transportation and reloading of sinter results

Physical Properties of FILr-ced 3inter
of the Cherepovets Plant
ja
4-
2,9
77443
SOVI/1-313-60-1-4/30

-
b

Fig. 2. The relationship between the apparent specific
weight of sinter and the size of pellets: (a) sample
Card 3/6 Nr 1; (b) sample Nr 2; (c) true specific weight.

Physical Properties of Fluxed Sinter
of the Cherepovets Plant

4:' : 1V

O'S

:
t
1)
d

Pr ---------- ?1r-
77443
SOV/133-6o-1-4/30
Fig. 4. Change in composition of various fractions (from
0-3 to 0-10 MM) in the sinter, when screening with 2
Card 4/6 open sectIons ~a) and tot lly closed (b) screening
machines ksampIes I to IVI.

y,.; ea I Pvop,,,r1_ c)C FI::,.,.ed Si_r~te-
Ph i I 1
11~-7 Chi-
Card 5/6
4'3
4
SOVI/ 13 ~, -60 -(D
in "he formatlorl of,' The ef'te