SCIENTIFIC ABSTRACT KUZNETSOV, YU. N. - KUZNETSOV-FETISOV, L. I.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000928210020-7
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 20, 2000
• Sequence Number: 20
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

,-.,-X'UZNLPTSOV. TU,N.
Device for preparing powder samples for spectral analysis,
Zav.lab. 26 no.5s623 160, (MM 1317)
Is Irkutskiy cauchno-iseledovatel'shy institut redkikh
astallov.
(Speatrum analyste)

8/032/61/027/007/011/012
B1 1 O/B203-
AUTHOR: Kuznetsov, Yu. N.
TITLE: Automatic ?!ant for spectrum analysis of ores
PERIODICAL: Zavodskaya laboratoriya, v. 27, no. 7, 1961, 910-913
TEXT: Since the methods for pneumatic introduction of samples in the
electric are suggested by N. N. Semenov Ref. 4: Zavodskaya laboratorlya,
XXII, 4, 457 (1956))) and Gv I. Kibisov ~Ref- 5; Inzhenerno-fizichookiy
zhurnal, 2, 3, 68 (1959)) are difficult to automatizag the author
developed a chamber for the atomization (Fig. 1) as well as an automatlo
device for photographing the spectra. The horizontal disk I with chambers
on its periphery is used as magazine. I is fixed by nut 6 to shaft 3 with
flange 4 and screws 5 for horizontal adjustment of the disk. The inner
boring of the movable shaft 8 centers the latter with respect to pin 9. The
bearing ball 10 facilitates rotation. Nut 11 permits elqvation adjuatment
of the magazine by j 6 mm. The oonical nozzles 12 forming air jets are
fixed on the ring disk 14 by means of rubber sleeves 13; 14 closes the
chamber lid with a rubber gasket. Wing nuts on the pins 16 tighten the
Card 11T

8/03 61/027/007/011/012
Automatic plant for spectrum analysis B141OX203
disk. The rotation mechanism consits of a d-c magnet 18, a ratchet wheel
22, and a locator. Plunger 17 of the magnet is withdrawn to the initial
position after switching off spring 19 attached to guide 20. 20 prevents
horizontal rotation of 21. 22 has 30 tooth. The steel ball of locator 23
situated in tube 24 is pressed by a cylindrical steel spring adjustable by
Atop 25. When the ball enteri the Indentation of the gear wheel, it locks
chamber exactly below the arc space. The magnetic system of an electric
shaver or bell serves as vibrator. The operation is controlled by eleva-
tion adjustment. The arc tripod stands on an asbestos cement plate 26
which is connected with the rider by means of the vertical textolite board
27 (with window for the arc light) and steel pin 28. The electrodes 29 are
placed in the guide tubes 30, and are pressed by the springs 31 against the
fixing guide tube openings. For the electrode adjustment, plunger 32(with
the upper arm of the lever frame) of magnet 33 responds when the current is
switched on. Template 34 is introduced in 1he electrode gap. On further
rotation, the frame of Stop 35 lifts the springs 31 and releases the
electrodes. They are led from the guides to the template stop by means of
the springs 36. The analysis samples are filled into the cylindrical,
25 mm. high chambers (diameter 20 mm) with 0.2-0.5 mm thick elastic rubber
Card 2/7

8/032/61/02T/007/011/012
Automatic plant for spectrum analysis B1101,B203
diaphragm bottom. On top, the lid is provided with guide cone and nozzle 12.
Under the action of the vibrator, the chamber diaphragm form particle
suspensions blown out of the nozzles. The jet velocity is controlled by
the vibration number and nozzle diameter. The constant weight of samples
(1 5-10%) guarantees a regular supply of substance during the exposure time
of 20-30 sec. For samples with different physical properties (weight
difference !~ 20-2%), mixtures with finely ground fillers (buffer mixturO3)
are examined which do not separate according to the specific gravity with
sufficient degree of fineness. The grain size must be 300 mesh (particle
size - 0 being a quantity vohich depends on the specified value of the correct
and incorrect decisions. It is shown that decision-nuadng rule (2) will be independent of noiso
power If the following conditions are satisfied:
1n (3)
01
P2
2 2
Cr I 'Al. 0r2 P2 (4)
3A
.1card

L W25-67
kdC7146 AT6022373
Ws procedure also applies, moreorless, tD other o4paal classes, and parlicularlyto signals
with random phases as well as to signals with raWom amplitudes and phases. Orig. art. has:
14 formulas.
M CODE:,,. - 17,12/ SUBM DATEI,, O6Mar66/ ORIG PX- F-. 001,
Ccj 4A'
rd

ACC NRs A170021943 -QA) SOURCE CODB: UR/0188/66/000/002/0044/0051
AUTI 101(i
ORG: 1)QV0AMP-Y&1, A
TITLE: Investigation of.a. combinational parametric oscillation excitement
SOURCE: Moscow. Universitet. Vestnik. Seriya 111. Fizika, astronomiya, no.2, 1966,
45-51
TOPIC TAGS: paraTetric oscillation, parametric resonance, parametric equation
ABSTRACT: The author discusses combinational parametric excitation at a frequency
equal to half the sum of the two non-coruncrisur able simultaneous frequencies of the
driving voltaoc U(t) = p1coswlt 4 p7cos4~t (1). The system hehaviour is found to
be analogous to that having one para~ic ter 'osci llating at a frequency equal to the suffli
of the exciting frequencies. The analysis was substantiated by circuit experimenta-
tion over a wide range of the ratio of the two simultaneous exciting frequencie5WI/W2
Resonance curves, amplitude characteristics and excitation domains were determined.
The excitation areas had closed boundaries in the (p p ) plane. Author thanks prof.
V.V. Migulin for the suggestion of the topic and valulbie discussion. Orig. art. has
6 fi'gures, 7 formulas and I table.
SUB CODE: 09/ SUBM DATE: 220et64/ ORIG REP: 003/ OMi REF; 002
Card 1/1 UDC 621,372,061.310

KUMTSOV . Tu.F., Who
-memo"
Carrying out preparatory operations on the building site of an
Industrial plant in Kosoov. P&m. stroi. 38 no.11143-45 16o.
(MIRA 13:10)
(Moscow-7actories-Deeign and construction)
(Foundations)

KUZNETSOV, Tu.P., Insh.; JUKHTER, V.A., inzh.
Compaotness,indicator of a rolled layer, Strol. i dor. maah.
8 no.ll123-25 N 163. (MIRA l7tl)

Tv. j LHAYE, V.H.; VTLF=V~ N.G.
o -- ~-,e --- P'.
j.r~xluctlon of carbon disalfide from methane and sulfur in
the Ngh-texperature zone. Xhim. voloV. no,508-41 165.
(MM 18:10)
1. Hookovskly orders lanina khImikr-tekhno1ogI(,heskIy Institur.
lie. 1). 1. Mendeleyeva.

CHMOVt T.P. Iprof I KMNETSOV,, TuJ, lusb.
Automatic, control of-the quality of the compaction of eoila.,
gravel, slag$, 04`460alt concrete. Prom. stroi. 41 no-3-It
X~-42 N '63. (MIRA 17s2)
1. Moskovskiy insheyorno-IstroitelInyy institut in. Krqbysheva.
4"P

VIDINEYEV, Yu.D.; ZALIVADM, B.S.; KUZNF.TSOV, Yu.P.
. - -
Design of toothed rotary dynamometerse Priborostroenie
no.120-8 D163. (MIRA 1725)

VILESOVO N.G. [Vilietovp N.H.]; LEKAYE, V.M. [Lekae, v.m.]; KUMETSOV. Yu.P.
(Kuznietsc*, IU.P.1
Carbon dioWift content of sulfur dioxide and methane, Khim.pzam,
[Ukr.*] no,115-6 Ja-Mr 164, (MIRA 170)

TRUNKOVSKrY, Lazar' Yomallyanovich; JCU~NETSOVj_.X_W etrovich*~
J~~.~
PODGUZOV) H.I.p rod.j MRIKOVA, A.N., tokhn. rod.
(Automatic control cablesj manual on the installation and use of
control and special cables] Kaboli avtoratiki; spravochnik po
montazhu i okopluatatoii kontrollrqkh i spotnialfrWkh kaboleio
Mookva, Voonizdat, 1962. 365 P. (MIRA 15:6)
(,Electric cables) (Automatic control)

KUZNETSOV lu~jy Petrovich; BEWTSEFJWVETS V.V. nauchn. red. 1
;URA VA, N.N.,Aekhn. red.
[Meohanization of elootrical equipment installation] Me-
khanizataiia elektromontashnykh rabot. Moskva, Proftekhis-
dato 1963 119 P, (MIRA 16:8)
keotric power distribution)

~Tjzlc, I-30V Yu 11 - RA'3A'fK I tip A.G. - 1,EKAYI,;, '1.M. ; Yl-,'I.K ri;, ,,.u. ; vjix.,.,)(Yv,
P p
,004
Tlji~rmodynwrdcs of the high-tompertiture con,.croion of methane by
sulfur. Trudy MKHTI rio-47;80-85 164. (MIRA 18:9)
4
0

FTIESOV, N.G. ; KASATKIII, A.G. ; l,iKAYF-,, V.11. ; Kli, Yu.F.
Mechanism of the forirvLtlon of' virbor, aiar!ng tLu
redurtion of sulfurous anhydride by rjethana. Trudy '1KHT! no.47:86-
89 164. 18:,))

STEPANOVp VXI VAGAPOVA, T.I.1 KUZNETSOV, Ylr,S,
-.1- r -
Nterninatiaq- af-l-terminal aml n - widw Irr hog pVezro BickbIV41a
29 no.3029-133, MyrJe 164. (MIRA 1814)
1. Institut khiaii pr~rodnykh-sqyedtr~nty-Aft SSSR, Mo3kva.

KUZNETSOV YU-, Vo.) Cand Chem Sci,;
Ij (diss) "Study of
Distribution of dicelements in rine Demos~
LiE,1958;-APP with grat)hs (Radium Inst im V.0. Khlopin.
Acad Sci dr USSR) 120 copie:~ M, la-58, 119)

N
AUTHORS'. StarikJ, I. )e., Kuznetsov, X!L. V .
GraBhchenko, S. T._,7f'renk!tkh, M. S.
TITLE: On the Ionium blethod of Determining the Age of Marine
Sediments
(K voprosu ob ioniyevom metode opredeleniya vozrasta morskikh
osadkov)
PERIODICAL'. Geokhimiya, 1958, Nr 1, pp. 3-13 (USSR).
ABSTRACT! First the authors report on the research results which have
hitherto been obtained in this field. Then they describe their
own research methods and the process of analysis. Seven cores
from the marine bottom of the Indian and Pacific ocean were in-
vestigated. The content of Mn, Fe, Cao, Ra. Jol Th and U, and its~
alteration with increasing depth were represented graphically.
For most of the cores the obtained values for Ra, Th, Jo and U
are given another time in tables. According to the distribution
of the elements it can be distinguished between:
1) Nearsbore sediments (cores 2 and 3). The'distribution of ion
Card 113 nium and radium is difficult to be explained, they are not in the

On the lonium Method of Determining the Age of Marine 7-1-1/12
Sediments.
radioactive equilibrium. This is due to external influences.
2) Sediments if average kind (core 1). The distribution of
the two elements remains unclear, 'there is,, however, already
a connection in distribution.
3) Deep-sea sediments (cores 4, 5, and 7). The radium concens
tration is reduced with increasing depth; several maxima and
minima are explained by the changing conditions during sedimens
tation. Zhe vertical distribution of ionium corresponds completely
to that of radium.
Hence it can furthermore be concluded:
A migration of radium in sediments does not take place. The sedi-
mentation velocity in the marine regions of cores 4 and 5 changed
only to a little extent with the time. In all cores investigated
the concentration of uranium and thorium remains constant along the
core* In a series of cores there was an obvious connection between
the distribution of radium and ionium or, the one hand and calcium
on Uit othor hand.
There are 8 fieures, 5 tables, ami 1-1 references., 3 of whicb art!
Slavic.
Card 213

On the lonium Method of Determininp, the Age of Yarine Sediments 7-1-1/12
ASSOCIATION: Radium Institute imeni V. 0. Khlopin, AN USSR, Leningrad
(Radiyevyy institut im. V. 0. Khlopina AN SSSR, Leningrad).
SUBMITTED: July 22, 1957.
AVAILABLE: Library of Congress.
1. Sedimentation analysis
Card 3/3
2. lonium-Application

STARIK, I.Te,; VA,
Forms In which uranium and tborlum are found In bottom deposits
of the Antarctic Ocean. Rodiokhivnila I no-3:321-324 '59.
(HIRI, 12:10)
(uranium) (Thorium) (Antarctic Oceau--Deep sea deposits)

SOV/20-10-5-50/64
AUTHORS; Starik, I. Ye., Corresponding MemberAS USSR, Ku=A,0,0-x rulvoy
Nikolayevp Do Sop Login, V, Kol Lazarev, K* Po, Grashchenkop-
B. M.# Kolyadin# L. B.
TITLE: Distribution of Radio Elements. in the Sediments of the Black Sea'1_1~.
PERIODICAL: Doklady Akadeaii nauk SSSRg 19599 Vol 129, Nr 51 PP 1142-1145
(USSR)
ABSTRACT: The radioactivity of the sediments in the enclosed seas is al-
most uninveatigated. The Black Sea shows characteristic bydro-
logical and hydrochomioal oodditions. It is also intensively fed
with sedimentary material, For this reason its sedimentation
strongly differs from that in large oceani waters (Rat 5)- In
this connection the authors wanted to explain the influence of
these specific conditions on the sedimentation and.on the type
of distribution of the radio elements in.. the Black- Sea bottom -
sediments. The resultq achieved are not sufflcien.-L to draw final
conclusions.'For this reason only some assumptions'are expresi'ed.
The authors studied the vertical distribution.of uranium, radiump
ionixim, thoriumt iron, and calcium in a sediment core vMoh was
taken from the central part of.the Black 3ea from a depth of
2137 m- It was 227 am long and consisted mainly of grpy homo-
Card 1/3 geheous clay with 5 intermediate sand strata. The upper 18 cm

SOV/20-12M-50/64
Distribution of Radio Elements in the Sediments of the Black Sea
consisted of-extremely fine-disperse mud with thin sapropel in-
termediate stratao.Figure I shows the vertical distribution of
the above-mentioned elements in the core. Table 1'gives the oor-
responding figures* Prom theta data it iiay be concluded that
in the upper horisonq of the-core the radioactive equilibrium
in the*uranium series,is widely disturbed: the ionium doritent
is almost 4 times higher.-than the amoa corresponding to the
equilibrium with uraniumi the radium content, howevert oonati-
tutes only 1/4 'of this amount. The radium content in the water
'of Via Black Sea is only 15% of the equilibrium value of uranium
dissolved in the water. Thus the radium content in the sediment
is hardly one foupth of the amount which should be measured if
85% of the radium were spdimentated from the water. Assuming,that
no radium migration --tikes place in the ooree of marine sediments
(Ref 1) the disorepencyin the radium balanas in the water and
in the sediment of the Black Sea may-be explained by radium
,leaching from the sediment in ith upper layers. On the other
.hand, the upper horizons are considerably enriched with ionium,
and uranium. Their oontent.deoroaaaa downwards to 42-48 cm rapid-
ly and then practically ru*ne constant. Agoording to N4 Mo
Card 2/3 Strakhov more than 50% of CaCO7. were zedimentated by, joemioal'

SOV/20-129-5-50/64
Distribution of Radio Elements in the Sediments of the Black Sea
methods. The main bulk of iron, howevert is transported into the
deep-seated sediments with the river water. The authors conclude
therefrom that,the 4rtical CaCO,-distribution reflects the change
of the chemical conditions in th~ course, of time. Since Ve ver-:,
tical distribution of ionium and uranium agrees with of
GaCO3it indicates that the main amount of ionlun un!
was -separated from the solution. On the other 'land it may be
adnaluded from the parallel change in -the thorium content with L/
thpt of iron that the major part of thorium is of terrigenoua
origin. The authors calculated the rate of sedimentation in the
Black Sea from the data from table 1. It is 12-13 am within
thousand years. If it is however assumed.that in the horizon
100-106 am the equilibrium between ionium.and uranium is still
attained (Fig 2) the rate of sedimentation is only 0.4-0.5 am
per 1000 years. The problem as to which of the two values is,
correct has hitherto not been definitely solved. There are 2
figures, I table, and 6 references, 4 of which are Soviet.
SUBLIMED: August 22, 1959
Card 3/3

KOLYADIV, L.B.; HITOLAM, D.S.; GRAMIMIKO, S.M.;.KMMSOV. ru.V.;
Issarev, K*T.
Yorms of the occurrence of uranium in waters of the Black Sea,
I)okl.AN SSSR 132 no.4:915-917 Js 160. (MIRA 13:5)
1. Predstavleno akademikou N H.Strakhovym.
Olack Sea-UraniuD

GRASHOBENED, S.M.; EXOTAUT, D.8o; KOLTADIN, L.D.; XUZNJTSOV, ru.T.;
LAZU", L. F.
Radivx concentration in waters of the Black Be&* Dokl,AN SBSR
132 no-5111?1-1172 JO 160. (KVU 13:6)
(Black 8"--Udium)

PC
Jig
n
-lot
01 a
1
JA
E a gRai
'S' o.
Allj143;11 69
'511g! ij;IH ~,.
AiM
1."
10
2i
Asa
ILI
41 is

STARI..-, I.Ye.; 1lx,2.',,j.',C-,-l lu.V.~ 12-GEp
Certedn charaoteriatica of radiolonim dating. Radio!�i--Ia
3 no.4:49C-497 141. (111RA 14:7)
(Thorium-laotopon)

STARIK, I.Ye.; NIKOLAYEV, D.S.j KUWXXV, Yu.V.;,LEGIN, V.K.
Relationship botween the radioactivity of sediments in the Sea of
Azov and the Black Sea. Dokl. All SSSR 13~, no.2:456-459 Jl '61.
(MIRA 14:7)
1. Chlen-korrespondent AN SSSR (for Starik).
(Azov,, Sea of-Radioactive substances)
(Black Sea--lirflioactive DubDtancos)
(Deep-03a deposits)
I

ffL_ju ~V- LEGIN., V.K.
STARIKO I.Yeej NINDIAIEV, D.S.I_FENETS
Ra1ioutivity of sediments in the Black Sea, DOL AJI SM
139 no.6.-2456-21+99 Ag 161o (MIM 3.418)
2, Chlen-korreopondent AN SSSR (for Starik).
Black Sear-Sedimentition and deposition)
adioactive substances)
R

STARIK, I.Ye.; YZLIZAROVA, A.N.; KUZNETSMp Yu.V.
Determination of the age of ocearde deposits by the ionium-
protaotinium method, Radiokhimlia 5 no.2tl54-157 63.
(KCRA 16slo)

KUZNETSOV, Yu.V.1 LEGIN2 V.K.; SIMNMp Z.N.
Determination of ultrasmall quantities of uranium., radium, and
thorium isotopes in silicate materials taken from the same batch.
Radiokhimiia 5 no.2sl89-197 163, (MIRA 16slo)

KUZNL?SOV Yu.V.1 LEQ11i, V.K.j LISMIN, A,P,; SVIONYAX, Z.N.
I
Radioactivity of ocean suspensions, Part li Thorium isotopes
in ocean suspensions, Radiokhimiia 6 no.2t242-254 164.
(MIRA 17& 6)
li

TELIZAROVA, A.N.- KLIZHETSOV, Yu.V.
Determination of protactinium In weakly radioactive iilicate
materials. Radiokhimiia 6 no.3075-376 164. (MIRA 18;3)
.... ...... .

N - - - f
ACC NRi__AT6O1&228 1"' -2 0011: U"m~GOGGIGG/000/00010GO310007'T--
AUTHOR: Kuzneteov, Yu, V.
ORG: none
TITLE: A new waveguide line -tieaeuring method for deteimining the dielectric constants
of isolating film or sheet ma;orials
SOURCEt Vsesoyuznaya nauchnLya sessiya, poavyashchennaya Dnyu radio, 22d, 1966.
Sektsiya radioizmereniy. Doklady. Moscow, 1966, 3-7
TOPIC TAGS: dielectric property, dielectric,constant, electric measurement
ABSTRACT; The proposed method for measuring dielectric properties of thin samples
consists of placing them along the rectangular waveguide axis on one ofits wider
sides. The dielectric constant may be found if the dimensions of the waveguide are
known. However, the following values must be measured: the wavelength in the wave-
guide containing the sample, the wavelength when the sample is not there, and the
attenuation factor of the wave when the waveguide contains the sample. The latter
quantities may be measured by means of standing waves. This method also determines
the thickness of the dielectric materials as well as the dielectric constants of
constituent materials if the film or sheet is made from two materials with very
differeut dielectric constants. Orig. art. has: 5 formulas and 2 figures#
SUB CODE: 09/ SUBM DATE:. 19Har66/ ORIG REF: 006/ OTH REP: 001
Dqat4

)MNETSOV, Yu.V.,. inzh.; TARKUNOV, V.A.j, inzh.; OSIPOV# Yu.A.j, inzh.
Role of weakening of the Coal irAsoif strength under the
effect of water injection into the seam, in an increased labor
productivity, Ugoll 40 no,11156-57 165. (MIRA 18:1.1)
1. Fermskiy nauchno-issledovatel'skiy ugolln7y Institut.

E--
- - - -- - - - - ----
KUZNV,LISOV, Yu.Y.; RAPOPORT, S.R.
, W"W""
POPPIVgrammed unit of a temperature regulator.
no.6;27-28 Je 057.
(Thermostat)
Priborostroonle
(KLRA 10:7)

992-6 18 Juac
NILASURBIMENT OF T11 E' PHASE VELOCITY OF A SURFACE WAVE (USSR)
Kuihetsovi- Yu. V;--Izvestiya--vyss#ikh-uchabtiykh tavedenly.- Pribords-troyean
op
- S/146163/006/002/0011010-
v. 6; 6 ~ 3 8.
A rnetaod for the measurement of the delay of so-called "nat" and single har-
manic dQlay sy,~;,,Qms and associated test equipment has been developed by the
Lcnin,,,,rad Institute of Precision Mechanics and Optics. It is shown that the
dulay factor can be'determined if the phase velocity or phase wavelength of
clectrornagnetic oscillations propagating along the delay-system. and heir
V~:'.ocity anci wavelength in free space are known. The method presenreid is
basted on the utilization of the phase sensitivity properties of hybrid Tee and
cons4s-.s in measuring the phase velocity of a delayed wave by means of a
movable load. In the test setup described the shf amplitude modulated car-
r,'er is applied through a waveguide to the H-arm of a hybrid Tee and then,
_rc~- gh t'ne side arms, is transmitted to the short-circuited
waveguide and to the delay system, which Is terminated in a variable
Yr. order to determine phase velocity, changes in the linear displace-
mcnt of *Laa variable load, which correspond to a certain phase shift of a de-
layed wave reflected from the load. are measured. The phase shift is
Card 212

e.:--.-w'~'.~_..~-.'~ 0:1' PZUM V,"=X=Y [Ccat0d] 8/146/63/006/oWool/olo
-neasured by successive comparison of a measured phase of the delayed
wlnich is propagated twice along the system investigated, with the
ra--:i2:-~!nce phase cf the wave propagating in a short-circuited waveguide. If
) zis,_,L ~' re,,
, "I - 'locted wi.ves are coincident, then the basic portion of the
-cfiQ:cted waves of energy appear in the H-arm, but if the reflected wave
p1las.,s are shifted in respect to each other. the basic portion of the energy
app(_ars in the E arm of the Tee and consequently on the detector which
Lernalnates this arm. By taking readings of a distance corresponding to two
maxima or minima, the phase wavelength and, as a result, the rate
ti-, _~ phas c velocity of electromagnetic oscillations in a delay system can be
c~.:'.E;rrnined. Usina the device described, several delay systems were Inves-
A graph is included, which compares the predicted value of the de-
of the delay factor on the thickness of the dielectric layer with ex-
peri __tai resu.ts. This curve indicates that tha deviation of experimental
from a theoretical curve does not exceed + 1. 5% and total error of the
device is less than + 4-50/o. (GS)
Card 2/2

KUZNETSOV,,.js;..V,~
Measuring devices for the determination of dielectric permittivity
of insulation layers on metal surfaces, Izvsyyssucheb.zav,j pribo
6 no.6:10-14 163. (MIRA 17:3)
1. Leningradskiy institut tochnoy mekhaniki. i optiki.
Rekomendovana kafedroy radiotekhniki.

r. Y9. sTARix, Yu. v. xummov, Ye.p. Pmum, v.x. LEorN (usw
"Bom problem of the Woobadstry of radioactive isotopes."
Report presented at the Conference on Chemistry ot the tarth's crust,
Moscow, 14-19 Her 63.
`W~*6

I.L.p professor; MORGUNOV., G.A.., aspirantj KUZNETSOV, Tu,V.,
-aspirant
late results of palliative reoeotiono of the liver in alveolar
echinococcoois. Vsotokhir. no,545-50 162. (MMA 15:11)
1, Iz gospitallnoy kbirurgichaokoy kliniki (zavo - prof* I#L*
Bregadze) Novosibirokogo meditsinakogo inatitutao Adrea avto-
rovi Novosibirokp Kmanyy pr,j d,3., gospitallnaya khirurgiche-
skaya klimika.
(LIVMI-SURGM) (LIVER-HYDATIDS)

70 0
S/058/6SW/0O6/t2q/b4O
AOO5/AOOl
Translation from3 R~ferati~nyy zhurnal, Fizika, 196o, No. 6, p. 294, # 1492o
AUTHORs Kuznetsov,_~YU_V-,
TITLE: Controllable Punnel, Directivity Diagram of the Rod Antenna
PERIODICAL: Nauohn. tr,Leningr. in-t toohnoy mekhan. i optiki 1959, No. 29,
pp. 86-90 '
TEM The problem is considered of using a single conductor for forming
funnel directivity diagrams. An approximate formula is given for calculating the
directivity characteristics. Two possibilities of diagram control are mentioned:
by varying the conductor length or by varying the wavelength of the electromag-
netic oscillations. The operational principle and the design are described of
the wide-band transformer - the transition from the rectangular waveguide to the
coaxiil wavegulde exciting the single conductor. The experimental diagrams of a
cylindric rod of various length are presented. The high transmission factor of
the transition is noted in connection with small transformation losses.
N.N. Filippov
Translator's note: This is the full translation of the original Russian abstract.
Card 1/1

__ - F__
9 TUA... insh.
~ -.1 - Preliminary impregation of coal in mines during blasting, Besop,
tuda v prom. 2 no.ZA-5 7 1580 (MnA 1112)
1. Vostochn" naaahno-Iseledovatel'skly institut po bezqpaanosti
rabot v ornoy prourshlennosti.
10oal mines and mining--Safety wasuros) (Blasting)

KMV.TSOV, Y11.V.
Blasting hoins with water as means of Increasing the efficiency
and safety of blasting operations. U901' 34 no-3:48-49
Or 159, (HIRA 12:5)
1. *oatochM7 naucbno-looledovatel'skiy institut po bazopasnosti
rabot v gornoy prowyablennosti.
(Hining enginearing-Safety measures)

lUZIE3TSOV, T ir Yladimfr'b'-v'jch; ARKHIPOY, N.A., otv. red.; ZHUXOT, T.Y.,
'iu-r-2y- TI"'llmlrovz
, red, tekhu.red.
[Preliminary wetting of coal seams] 11redvaritaltnoo uvlazhnonis
ugollnykh plaiatov. Moskva; Goo.nauchno-tekhn.iod-vo lit-ry po
gorno?m delu, 1960, .56 p. (MIRA 14:3)
(Mue duste)
0

- ~qYt_.LutV,-CNavosibirok)
Preliminary moistening of coal in the block as a means for increasing
labor productivity. Ugoll 35 no. 4s17-20 Ap 160. (MIRA 14:4)
Coal mines and mining-Labor productivity) (Mine dust)

rJUIETSIOV, Yu,.V.
-
lAboratory Inveatigation of tho pulsoi method of Injecting water
Into a coal aeam. Nauch,o.. trudy Pei-mNIIJI no.6s203-12,14 164.
(MIRA 1812)

.EJZNETSOVI" Yu.V.j OSIPOV, Yu.A.; TARKHANIOV) V.A.
Efficiency of injecting water into a seam* Biul. tekho-ekon.
inform. Goo nauch.-inel. nauch. i tekh. inform. 17 no.9tlO-12
S 164 (MIRA 181l)

XUZRZTSOV, Yu.Ya.
Principles for compiling goomorphological maps of mountainous
region*. Geol.ebor,CLvorj no,2/31294-304 1569 KRA 10:3)
1. Vs Osoyuzzy7 asro geologicheekly trest. Hooky&.
(Physical geography) (Surfaces, Representation of)

1 0 VV, v
j
3(5) PHASE I BOOK EXPLOITATION SOV/1796
Moskovskoye obshchestvo ispytateley prirody. Geograficheskaya
sektsiya,
Regionallnoye karstovedeniye; trudy soveshchaniya po regionall..nomu
karstovedeniyu (RegionalStudy of Karst Phenomena; Papers of
the Meeting on the Regional Study of Karst Phenomena) Moscow,
1958. 79 p. 600 copies printed.
Additional Sponsoring Agency: Moskovskoye obshchestvo ispytateley
prirody, Redaktsionno-izdatellskiy sovet,
Ed.: (Title page): N.A. Ovozdetskiy, Professor; Ed. (Inside book):
G.N. Endellman
PURPOSE: This book is intended for geologists., hydrologists, specia-
lists in engineering geology, and speleologists.
COVERAGS: This collection of articles is badW mainly on reports
presented at a Conference on Regional Studies of Karst organized
by the Geographical Section of the Moscow Society of Naturalists
Card 1/3

Regional Study (Cont.)
SOV/1796
which took place on April 16.. 1958. The extensive karat phenomena
within the USSR, and their possible influence on d1mate and hydro-
logy, has m6rited extaidve , study by Soviet scientists, The influ-
enoe of biochemical processes on the formation of karst is noted.
Each article is accompanied by photographs, diagrams and biblio-
graphic references.
TABLE OF CONTHIMS:
From the Editor
3
Gvozdetskiy, N,A* Regional Studies of Xarht. Brief Review of
Latest Studies and Some Problems 4
Gvozdetakiy,p N,A,,t and AaI, Spiridonov, Latest Data on Karst
Phenomena in the Basin of the KlyazIma River'and the Oka-
Klyazlma Intbrfluve 15
Card 2/3

Regional Study (Conto) SOV/1796
Chikishev,, A.,G* Karat Formations In the Basin of the Chusovaya
River on the Western Slope of the Central Urals
Solov1yevj A.I, Karat Phenomena on the Eastern -Slope of* the
Southern Urals
Kuznetqovj_Yu*Ya6 Karat Caverns of the Utebay Traot (Southern
Ustyurt)
Nikollskaya, V.V. Observations of Some Karst and Pseudokars.
Formations In the Zeya River Basin
Sokolov,, D,S. Certain Characteristics in the Development of
Karat in One of the Regions of the Middle Course of the
Yangtze River (China)
Gvozdetskiy, N,A., and YaG. Mashbitse Some F'roblems of the
Yucatan Karst (Geomorphology., Water Supply'and Settlements)
AVAILABLE: ILtbrary of Congress (0601.16) MM/lsb
Card 3/3
29
1. .
39
49
53
61
71

KU7.IDV,SOV, Yu.Ta.
Modern glaciation of the southern Fergana Range Trudy, VAGT
no.4:66-78 1513. WRA 12:6)
(Fergana--Glacial epodh)

Note on the recent and old glaciation of the Turugart Pass,
Geol. abore [Lvov] no,5/6079-581 '58. (HIRA 12:10)
l.Vsesoyuzny7 aerogeologichookiy treat, Moskva.
(Turugart Pass--Glaciers)

MM I BOOK Eawrunw
SOV/3852
Akad-4ya nauk SSM. Laborstoriya aermetodov
Trudy, tom 8: Materialy VII Vsesoyuznogo aezhvedwstvennogo soveshchways
po aeros"yemke 25 noyabrya - 1 deMbrya 1956 g. (Naterials of the
7th All-Union Interdepartzental Conference on Aerial Surveying, 25
November-1 December 1956) Moscow, Gosgeoltekhizdat, 1959- 300 P-
5,000 copies printed.
Ed. of Publishing House: V. G. Filatov; Tez"i. Ed.: 0. A. Gurovaj
Editorial Comissiont N. 0. KallIp Corresponding Member) Academy of
Sciences USSR; A. A. Lopchevp V. P. Kiroshnichanko (Hoop. Ed.)p
and N. ff. Sokolov.
PURPOSE: This publication is intended for photogrammetrists, geologists,,
geographers., and other scientific and technical personnel concerned
with aerial photography.
COVERWE: This issue of the Transactions of the Laboratory of Aerial
Survey Methods contains the second put of materials presented at
the 7th All-Union Interdepartmental CoAference on Aerial Surveying
which took place in Leningrad, November 25 through December 1., 1956.
Card 1/ 10

Materials of the 7th All-Union (Cont.) SOV/3852
Articles treat problimm - dealing vith the execution and application
of aerial survey methods in geologicalp geomorphological, and geo-
physical Investigations. Special attention is directed to aerial
survey methods in.goological and geomorphological mapping and geo-
physical vork under different conditions. The, techniques of joint
airborne - magnetic prospecting and serial photography are described.
References accompany individual articles.
TAKE OF CONTEM:
Forevord 3
Lungerspuzen, Go Pej and V. P. Ponikarov (VAOT - Vassoyu=yy aeropa-
logichaskly trest - All-Union Trust for Aerial Oeological Sum "].
Su=w.ry Results of Applying Aeri&I-Ourvey Methods to Geological Re-
connaiasance of the UNRO Based on the Work of the All-Union Trust
for Aerial Geological Surveying 5
Miroshnichenkoj, V. P. ELaboratoriya aerowtodov AN SSSR - Laboratory of
Aerial 3urvey Methods, Academy of Sciences UM), Application of
Card 2/10

Materials of the 7th All-Union (Cont.) SOV/3852
Aerial-Survey Methods to Geological Reconnaissance 14
Ponikarov, V. P., and Yu. Ya. Kaznetsov [All-Union Trust for Aerial
Geological Surv*yingT_._1e_e'EL_fo-_FF_= the Application of Aerial-Survey
Methods to Integrated, Oeological Mapping of Certain Regions of
Soviet Central Asia 39
Miroahn:Lejhenko, V. F. (Laboratory of Aerial Survey Methods$ Ac&6W of
Sciences USSR]. Visual ObservationsYrom an Airplane in Geological
Exploration 45
Aristarkhova, L. B. [A3.1-Union Trust for Aerial Cleological Surveying).
Results From the Application of Aerial-Survey hathods to Integrated
Geological Surveying of Desert and Semi-Desert Areas Me" the
Caspian Sea 74
Maslyayev, 0. A. (Soyuzn*4a goologopoiskovaya kontors, - All-Union
Prospecting Office]. Tectonics of the Northeastern Part of the
Ponto-Casplan Area [Central Memych Lowland] According to Aerogeo-
morphological-Survey Data 84
Card 3/10

XUZNETSOV, Yu-.Ya.
G*Unr mid origin of the Velief Ur southeastern Fergana. Vop.geol.
rM.TianlAmia 2440 '160. - (KMA 15 13)
(ForgAwL.-Physical geography)

KU34ETSOV, Yu.Ya.
___I
Content of geological maps of closed territories. Sov.geol.
5 no-4:127-129 Ap 162. (MIU 15s4)
1. Aerogeologichaskaya ekspeditsiya.
(Geology-Maps)

-------------KUZNETSOV, Yu-.Y-a.-;-PjiUSOV-,--V,V-,-
Age of metamorphic and eruptive rocks in the nucleus of the Tuar-hyr
anticline. DokI. AN SSSR .142 no.3:647-649 Ja 162. (MIRA 15:1)
1. Aerogeologicheskaya ekspeditslya No.11 Vsesoyuznogo aerogeologicbe-
skogo tresta. Predstavleno akademikom A.L.Yanshinym.
(Tuar-Kyr region--Petrology)
S'.

WJZNETSOVP Yu.Ya.
Ohrinkage of glaciers in the hrgana Range. Izv, v7so ucheb,
Savoy geolo i razv. 6 no.jt145-147 Ap 163. (MIRA 16:6)
Is Trost "Aarogeologiyas.
Oergana-Glaciers)

KUZNETSOV, Yu.ya.; PRUSOV, V.V.; TUGOLESOV, D.A.
Tectonics and prospects for finding oil and gas in the Usturt.
Sov. geol. 6 no.10.-24-31 0 163. (MIRA 17:1)
1. Aerogeologicheskaya ekspeditsiya Geologicheskogo instituta
AN SSSR.

- KUZNETSOVf. ,Yu.Ya.,
Ustyurt as an exanple of a karat region in the deaert.
Trudy MOIP 1506-61 165. (KIPA 18s9)
%~x
4.

U KLEYNER, Yu.m.; V2Z1%S,,_Yu-_Ya-; SHOLJAHOV, V.V,
Kethoda for detailed structural and geological studies in Ustyurt.
Sov. geol. 8 no.3:107-110 165. (MIRA lh5)
1. Voesoyuznyy aerogeologicheakiy treat I Naucbno-iaaledovatell~kaya
laboratoriya geologicheskikh driteriyev otsenki perapektiv nef te-
gazonoonosti.

ARKIIIP OVt A.Ya., ALTAYETA, N.V,j BAYBULATOVAv Z.Ks; VISKOVSKIYq YU.A.;
GOLENKOVA, M.P.; KRAVCHENKO, M.F.; KUPRIN, P.M.; LEVIN, A.I.;
POLISSR, L.A.; SEHDV, V.N.; SYRNEV, I.P.; USHKO, K.A.;
SHOIDMOV, V.V.1 Prinimali uchastiyet RODIONOVA, M.K.; CHELITSOV,
Yu,G.; !nnT-8qL-xUj&.&-, kand. geograf. nauk, nauchnyy red,
[Geology and oil and gas potentials of the south of the U.S.S.R.;
Kara-Bogaz-Gol (Gulf) region (eastern part of the Middle Caspian
oil- and gas bearing basin).] Geologiia I neftegazonognost' iuga
SSSR; Prikarabozazle (vostochnaia chest' Srednakaspiiskogo nefte-
gazonosnogo basseina). Leningrad, Nedra, 1964. 300 p. (Trudy
Nauchno-issledovatel'skoy laboratorii geologicheskikh kriteriyev
oteenki perspektiv neftegazonasnosti no.12).

L 32180-66 EINT(l) IJP(c)
ACC NR: AP6013922 SOURCE CODE: UR/0207/66/000/00V00-41/0045
AUTHOR: Kuznetsov Yu Ye Syrovoy, V. A.010
t-lq
.ORG: none
JITLE: The solution of equations for aregular electrostatic beam4-assuming emis-
sion from an arbitrary surface
SOURCE: Zburnal prikladnoy meRhaniki Itekhnicheskoy fiziki, no. 2, 19G6, 41-45
TOPIC TAGS: electrostatics, dimensional flow, current density
ABSTRACT: An analytical solution is given for the equations for a regular clectro-i
static beam emitting from an arbitrary surface under conditions of full space chargeo.
~A regular beam is defined as one in which the generalited particle momentum is a
potential vector. It in assumed that the emitter is the coordinate surface x'1 =
const in the orLhoganal system xI (I a 1,2,3) and that the density of the emission
current J is a fixed function J(x2' X3). The solution Is given as aeries in x1 with
2 3
coef ficienv functions of xX - The first correction to the Child-Langmuir 3/2 la
is determined by -the sum of principal curvatures of the emitting Gurface with
Card 1/2 -A

L 3218o-66
'ACC NR: AP6013922
:respect to the expansion of an arc along the length of the xi axis which is orthogari-
al to the emitter. This solution can be used to determine the shape of a collectori
w
'hich will provide a given emission current density distribution at a given surface.
SUB CODE: 20/ SUBM DATE: 25Jul65j ORIG RE:r: 000/ OTH Rm 000
lard 2/2

GRODZOVSKIY. G.L. (Moskva)f KMNMSOV, Y-aje.
Gao-flow vortex-oooling chamber theory. Izv. AN SSSR Otd.tekh. nauk
no.10:112-118 0 154, (MIBA 8:3)
(Gas flow)(Vortex motion)(Refrigeration and refrigerating
machinery)

GRODZOVSXIY# G.L.1 KUZNETSOVj YU.Ye.1 TOKAREV, M.V.
Approximate calculation of axiayzwetric supersonic flove un4er
internal problem conditions. Prom.aerodin. no.24tl52-157 162.
(~qRA 160)
(Aerodynamics, Supersonic)

-GROD7,OVSKT, -G.L KURVM~Olr-- --KHUDTAKOV--G.Te. --(Mo-scow)I
"The gas dynamic theory of the flow of a fluid with varying phases."
report presented at the 2nd All-Union Congress on Theoretical and Applied
Mechanics.-Mosoow, 29 Jan - 5 Fab 64,

Yu.M., doktor tekhn. nauk; RUZHINSKIY, M.B., ~;nzh.; 'ZOWTANITSK IY,
MO., lnzb.; KUZNETSOV, Yu.Ye., In2h.
Mhatoring the productIon of pipe by Induction welding at. the
NovoBlbirsk metallurgical plant. Stal' 25 no.3t245-251 Mr 165.
(MIRA 18t/,)

DZHAVADOV, Ismail All ogly; SADMHOV, Thad Sadykh ogly; GUSLTAUVo
Mamed Gasan ogly, KUZN1TSOV Z.A.,_in2h.
Best foreman of the Azerbaijan Railroad. Put' i put.khos.
no.10:26-27 0 159. (MIRA 13t2)
1. NachaVnik Kirovobadekoy distantaii Azerbaydzhanskoy
dorogi (for Dshavadov). 2. Sekrstarl partorganizatuit Kirovobad-
akoy distantsil Aserbaydshanskoy dorogi(for Sadykhov).
3. Predeedatell meetkona Kirovobadekoy distantaii Aserbaydzhan-
skoy dorogi (for Guoeyuov). 4, Eirovobadukaya distanskoy
dorogi (for Kusnetsov).
(Aserbaijan-Railroads--Nmployees)

r. - - - . , , ji = ~ - s
27171 KUZI-IhT-c*OV, Z. I. Odnobarabannyje Lebodni na pof,,ruzke lesu. les. prom-stip
1949j, 110A., S.9-10.
SO: Letopist ZhurnalInykh Statcy, Vol. 36,1949

KTJZNETSOV-PETISOV, L.I., dotment
Productign of silicon tetrachloride under laboratory conditions*
Trudy MWI no,14:107-110 149, (MIU 12ill)
I.Kafedra tokhnologii neorgenioheskikh veshchestv Kazanskogo
khimiko-takhuologichaskogo instituta im. S.M. Kirova.
(Silicon chlorides)

KUZWSOV-MISOV, Lr.; JaUSUIT, B.B.
uoing wguesium perchlorato under laboratory conditions*
Trudy XMI no.15:62-64 150. (pubi. 1511 (MINA 12:12)
(Vagnesium perohlorateJ

KUZNETSOV-7ZTISOVj-L,I~; TUPILOVSKIT. N.N.
Laborator7 ultrasonic unit for physicochemical investigations. Trud~T
KWI no.17s63-68 152 (publ. '531. (MIRA 12:11)
(Ultrasonic testing)

)i - -,; - ~ ~; -
lie4tv of form tL M~T14 In the Wt-Im Uwc
,AAe
L I nif
I"MIC11511 frindiclom). z4fig'. prilhid. Kki.i. 25, 1311-13
52).-Tfit methf-gi. tr, KnI IntcrPretittion of expli.
M
teqQIt,q used by Gtifimm rc-A. 4Z, MIM). tire crittcW.
The imix. nil.-wilidity beat In the Itmary systern 1(,%0 - I
l1'%'0,,';0, com-sponds to the compri. 31IN0,4% (n%tc!1fd
Its value. accrxiling
to clctnt, by K, and K.-F., is equai to 137 cal. per C. of
mixt. Insuld of the 64 Col. " pmvimml3r r-potted,
Ifftimt

- - . .., . - ~ ~7 K: A - - -
rm~- - -
~ I ~ ~t
, , ~: -t

L-LE Tx-5
Ulf
VIM v
Wittig

SOV/78-3-10-4/35
AUTHORS: Kondratlyevg S. N., Kuznetsov-Petisov, L. 1.
TITLE: On the Production of Anhydrous Liquid Sulfur Trioxide in the
Laboratory (0 poluchenii bezvodnoy -.hidkoy trekhokisi sery v
laboratornykh usloviyakh)
PERIODICAL: Zhurnal neorganioheskoy khimii, 19581 Vol 3, Nr 10, pp 2240-2243
(USSR)
ABSTRACT: A simple method was described by which So 3 can be produced under
laboratory conditions. Impurities due to polymerized products
are avoided by this method. Moist SO 3 is produced by distil-
lation of sulfuric acid of 60%, while potassium dichromate is
added (for the oxidation of So 2)1 followed by distillation at
80-10000. An apparatus was described (Fig 1) by means of which
anhydrous 503 can be produced. The melting point of anhydrous
s03 is 16t79.� OtO20 which compares well with the value mentioned
in the reforences (16,80). The method described makes it poesible
Card 1/2 to produce 400-500 g of chemically pure sulfur trioxide in the

SOV/78-3-10-4/35
On the Production of Anhydrou~ Liquid Sulfur Trioxide in the Laboratory
laboratory, which polymerizes on standing at a temperature not
lower than 170C. The dehydration of 50 3 by means of phosphorus
pentoxide does not lead to a uniform product. Thepreparati.ons
obtained have different melting points. The temperature range
of the melting point depends on the method of dehydration and
the drying time. There are 1 figure and 11 references, 3 of
which are Soviet.
ASSOCIATION: Kazanskiy khimiko-tekhnologicheakiy institut im. s. kv. Kirova
(Kazan, institute of Chemical Technology imeni S. M. Kirov)
SUBMITTED., - July 17, 1957
Card 2/2