SCIENTIFIC ABSTRACT SINITSIN,V.I. - SINITSY*N, V.V.
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CIA-RDP86-00513R001550810005-6
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RIF
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S
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100
Document Creation Date:
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Publication Date:
December 31, 1967
Content Type:
SCIENTIFIC ABSTRACT
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Body:
Application of High-intensity Radiation Sources S/170/6U/0U-x/U2;25/026
in Industry B000005
organisms, ecbnomic problems with respect to processing methods by means of
radiation, etc. were dealt with,
I/
Card 3/3
NISIMICH, A.I.;,SINITSIN, V.I.
Using radioisotopeS in solving the problem of increasing the
durability of machine parts and mechanisms. Inzh.-fizahur.
no.3.1:113-3.19 N 160. (KERA 13: 11)
(PAdiolobtopeo-Industrial applications)
S/170/60/003/011/015/016
BO19/BO56
AUTHORS, Nisnevich, A,. I.., Sinitsyn, V,, 1,,
TITLE, The Use of Radioactive isoL,~ResliTor the Purpose of Solving
the Problem of Increasing the Servioe Life of Machine Parts
and Mechanisms
PERIODICAL: Inzhenerno.,,fizicheskiy zhuraal, 1960, Vol. 3, No. 11,
PP- 113-119
TEXT. 1n the introduction., the use cf radioactive elements as indicators
for near is discussed in a general manner. In this connection, the activa-
tion of the parts investigated is described as an essential problem, i.e.,
irradiation in an atomic reactor and the applying of radioactive substances
onto the surfaces under investigation. The advantages of an irradiation in
a reactor are compensated by the disadvantages of the change of various
physico-mechanical properties of the material under investigation. This
method is only very little used in the USSR, The difficulties in the case
of the second aforementioned method oonsist in the fact that the radio-
active elements, which are used for this purpcse in form of alloys vith
Card 41/2
The Use of Radioactive Isctopes for the 5/170/60/003/011/015/016
Purpose of Solving the Problem of Increasing B019/BO56
the Service Life of Machine Parts and Mechanisms
59 60 65
Fe CO or Zn have a low activity and that the production of equal
c,r similar alloys with these elements is difficult. Another fact of
great importance is t%e quantitative measurement cf the radioactive
particles, ;hich is most.1y carried out with scin~tillation counters. As an 60
example, aii investigation of the operation conditions of a tractor
motcr with respect to the wear of piston rings is dealt with. A scheme
c-f the experimental setup is shown; the coniac'. surfaces were activated
ty mRans of a C060 and Za,65-containing alloy, It is found that at a defi-
nite number of rotations of the crankshaft wear is the greatest. The in-
irestigation --,f the wear of further motors is partly dealt with, several
details are briefly discussed., and finally, testing in practical operation
is described as an especial advantage. From the investigation of a tractor
of the type F~'~,54 (DT--54) the results obtained are shown in a diagram.
Piston rings show the greatest wear among all parts investigated. There
are 4 figures and 10 Soviet referenoea~
SUBMITTED-, February 8, 1960
Card 2/2
21.6loo,21-7100 77257
SW/89-8-2-22/30
AUTHORS: Sinitsin, V. I., Grafov, G. I.
TITLE: Conference on the Application of Powerful Radiation
Sources In Industry and Especially in Chemical Processes
PERIODICAL: Atomnaya energiya, 1960, Vol 8, Nr 2, pp 164-167 (USSR)
ABSTRACT: The conference was held in Warsaw September 8-12, 1959.
More than 200 representatives from 27 countries were
present. The representatives of Canada reported on the
radiation source and construction of the irradiation unit
for irradiation of potatoes. The use of a powerful
irradiation unit with cobalt 60 as the radiation source
_Ln the rubber and plastics industry was reported by
representatives of Czechoslovakia. Several reports were
devoted to methods of calculating and designing irradia-
tion units for use in the chemical industry (De.-mark,
Hungary, USSR, France). The outstanding reports of the
representatives of the U.S. were: G. Silverman, on the
Card 1/3 11~pe of )2 -radiation of fission products in textile and
Con1'erence on the Application of Powerful 77257
Radiation Sources In Industry and Especially SOV/89-8-2-22/3()
in Chemical Processes
Card 2/3
plastics industries; D. George and D. Gregory, on the
-/ -unit of the research center of the Australian Atomic
Energy Commission; Oz. Oster, on "The Role of Electron
Excitation in the Chemical Effect of Irradiation on
Plastics"; J. Sederland and A. Allen, on radiolysis of
pentane in the crystal lattice of hydrated synthetic
ziolites; E. Taylor, on the effect of Y-radiation
on the ac'~ivity of catalysts; A. Hengl~'in, on synthesis
of nitric compounds by the reaction of free radicals
with nitroc~en oxide; E. Pollard and U. Gild, on inacti-
~iation curves for certain plants, animals, and bacteriolog-
ical viruses; Ch. Artandi, on sterilization of phar-
maceuticals and hospital equipment with ionizing
radiation; P. Ebersold, on main types of industrial
application of radiation in the U.S. and future plans
for the use of radiation. Several studies conducted at
Brookhaven and Oak Ridge National Laboratories were also
reported. The reports presented by representatives of
Japan are: S. Onisi, on measurerments of spectra of the
Conference on the Application of Powerful 77257
Radiation Sources In Industry and Especially sov/89-8-2-22/30
in Chemical Processes
electron spin resonance of Y -irradiated polymers;
M. Matsumoto, on the effect of radiation on polyvinyl
alcohol; S. Okamura, on polymerization of vinylacetate
in an aqueou mediLUn Linder the effect of -Y -radiation.
The Soviet reportb mentioned are: A. K. Bi!eger, on the
principle and general characteristic of indium-gallium
irradiator using short-life isotopes; S. S. Medvedeva,
A. D. AbIcina, and P. M. Khomikovskiy, on radiation poly-
merization of ethylene in gaseous phase of organic
solvents. The other reports noted are: S. Pinner (U.K.),
on synthesis of polyvinyl chloride with copolymer chains
cross-linked with allyl bonds; F. Dalton and R. Robetson
(U.K.), on graft-polymerization of polyacrylonitrile and
dimethylsiloxane caused by -y-radiation; H. Heins and
B. Dere (Belgium), on the effect of -radiation on
polyethylacrylate of' various molecular weights; F. Trenar
and Verrie (France), on the effect of radiation on the
reaction of chlorine with one of its liquid derivatives;
F. Balestic and M. Maga (France), on the effect of rad-Ja-
Card 3/3 tion on synthesis of some dyes.
AUTHORSa
TITLEs
64238
S/089/60/009/004/018/020
B006/BO70
Lokhanin, G. N., Sinitsyn, V. I.
New Hermetic Chambers for Working With a- and P-kctive
Subs ces /7
PERIODICALi Atomnaya energiya, 196o, Vol. 9, No,. 4, pp. 344 - 347
TEXT: The authors give a detailed description of the chamber 1K,
14)K
(1KNZh), mass-produced in the USSR, in which it is possible to work with
a- and P-active substances. In this chamber, which has one working place,
it is possible to work at high temperatures, and o with acids and
lyes. (A similar chamber of the type 2KH)K (UM)Irith two working places
is shown in Figs. 4 and 5). The chamber is-m-alle-of 3 mm. thick stainless
steel, and is 2320 mm high, 875 mm broad, and, including the antechimber,
1270 mm long. The hermetically sealed space in the chamber is 0.4 m . The
chamber itself stands on a foundation made of carbon steel. Figs. 1 and 2
show the front and the back of the chamber, Chambers of this type are
produced with one or two antechambers which are used for introducing and
removing the radioactive materials, the vessels, reagents, etc. The
Card 1/2
84238
New Hermetic Chambers for Working With a- and S/089/60/009/004/016/020
P-Acti-,e Substances B006/BO70
inside of the chamber is lighted with a three-tube lamp (45 w) of the
type CZC-45 (SDS-45). For protection against radioactive aerosols, gases9
and other substances in the air, the chamber is equipped with a special
two-stage filter system, which is described. A receptacle is inserted in
the foundation of the chamter (Fig. 2) to receive solid contaminated waste
matter. The solid radioacti~;e waste matter is packed inside the chamber
in a plastic material and sealed hermetically. It then comes to the
receptacle which is put on a small hand-cart (Figs. 2 and 3). This process
is described in detail. The waste container is made of carbon stee and
has a capacity of 10 liters, A container of the type 10KEOC!MhO_ 6.s
used for contaminated water and liquids. It is described in the preceding
paper on a wash cabinet (pp. 341 - 3449 Fig~ 3)~ It is briefly described
also here. There are 5 figures.
Card 2/2
PWROY, N.A., red.; PETRENK0, L,I., red.; SATITSKIY, P.S.. red.;-%U"TAU&
red.; KCLOTYRKIN, Yo.M., red,: SYR03, N.P.. red.; RONK,
R.F.. red.; AB7YSMN. P.I.j red.; VARTAZQ0T.:S.Ya., red.;
ZAYTSKY, A.I., red.; ZNZYULINSKIT. T.M., red.; ZEDGINIMS, G.L.,
red.; KARTYNKIN, F.P.. red.; ROGACHET. V.I., red.; MATINSKIY.
A.N.. red.; LRYINA. Te.S., vedushchiy red.; TITSDYA, B.F.,
vedushchiy red.; PERSHINA, Ye.G., veduBhchly red.; IONEW. A.G..
vedushchiy red.; ZARMSKAYA, A.I., vedushchiy red.; MUKHIKA, B.A.,
tekhn.red.
ETransactions of the Conference on the Introduction of Radioactive
Isotopes and Nuclear Radiation into the National Sconomy of the
U.S.S.R.] Trudy Teesoiuznogo soveshchonlia po vnedreniiu radio-
aktivnykh izotopov i iadern~kh izluchenii v narodnoe khozialstvo
SSSR. Pod red. N.A.Petroirs, L.I.Petreako i P.S.Sevitakogo.
Moskva, Goo.nauchno-tekhn.izd-vo neft. i gorno-toplivnoi lit-ry.
Vol.l. (General aspects of isotope applications. Instruments
with sources of radioactive radiation. Radiation chemistry.
Chemical and petroleum refining industry]
(Continued on next card)
PETROY. N.A.---(continued) Card 2.
Obahchie voprosy primeneniia Izotopov. Pribory s istochnikami
radioaktivnykh isluchanii. Radiatsionnnia khimiig. Khimi-
cheskaia I nefteperersbatyvaiushchnia promyshlennost'. 1961.
340 p. Tol.2. [Construction and the industry of construction
materials. Light Industry. Food industry and agriculture.
Kadicinel Stroital'stvo I promyshlennoot' stroitellnykh mate-
rialov. Legkaia prorqshlennost'. Pishchmvaia promyshlennost'
sellskoe khoxisistvo. Keditsina. 1961. 267 P- (KIRA, 14:4)
1. Ysesoyuznoys soveshchaniya po vnedreniyu radioaktivnykh
12OtOpOV i'yadsrnykh-iz1uch9niy v narodnoye khozyaystvo SSSR.
Riga, 196o.
(Radioisotopes) (Radiation)
SINITSYNq V.I.~-ALAYABIYKV, A.F., red.; VLASOVA, F.A., tekhn. red.
[Radiactive cobalt] Radioaktivnyi koballt-,- Moskvaq Goo.izdvo Iit-
ry v oblasti atomnoi nauki i tekhniki, 1961. 56 p. (NM 1426)
(Cobalt-Isotopss~
LOKHANIN, G.N.;-Sll -N3 V.I.; SHTANI, A.B.; VATVEYEVA, M., red.; BOKSHA,
VITSY
R.V.JP red.; MAiH-i,-Ye.i., tekhn. red.
[Protective equipment and devices for working with radioactive
substances) Zashchitnoe oborudovanie i prisposobleniia dlia raboty
a radioaktivnym- veohchostvami. Moskva, Goa. izd-vo lit-ry v oblasti
atonmoi nauki i tekhniki, 1961. 129 p. (MIRA 14:11)
(Radiation protection)
R168/B160
AUTHORS: Sinitsyn, V. I., Shtan', A. S.
TITLE: Appliances and apparatus based on the use of radioactive
isotopes for the control and regulationof technological
processes in the chemical industry
PERIODICAL;' Referativnyy zhurnal. Khimiya, no. 10, t962, 357-358,
abstract 101177 (Vestn. tekhn. i ekon. inform. N.-i. in-t
tekhn.-ekon. issled. Gos. kom-ta Sov. Min. SSSR po, khimii,
no. 5, 1961, 35-P)
TEXT: Mass-produced Soviet appliances of interest t1o the chemical
industry are briefly described, together with some planned for
mass-production in 1961. 1. A level indicator for the interface between,
two media. C060 radiator, -amma-rays, activity 0-5-60 mg-equiv radium
("Kalugapribor" Factory). 2. Level regulator-indicator with pneumatic
outlet P'~71-1 (RUP-1), made at the same factory. 3. A series of relay-type
appliances, made at the Talinn Plant, based on the SPA-1i (URAP) electronic
relay unit: level recorder for measuring vessels, with an accuracy of
Card 1/3
S/081/62/000/010/049/085
Appliances and apparatus based... B168/B180
2 mm: maximum level recorder P7-Y-4 (RPRU-4), accuracy t 5 cm; device
?V~-A (RK-4) for regulating the filling of containers on a conveyor, a
tracking level-gage SP-6-A (UR-6-A) for storage tanks; c;ntinuous
density gage 7c:t,~'-2 (PZhR-2), range 1-1-5 9/cm 3, error 0.5
4. Ionization gage ',/."-,7,A (MIR-3A) for inactive gases and.steam, range
0.01-10 mm Eg error � 5~o, alpha-particle source Pu 239 ("Kalugapribor"
.Faz;tory). 5. Non-contact device (BIV) for weighing sheet materials
in the course of manufacture, range 200-800 g/m2, error � 5 ~-, source
Tl') 04. *6. Gage for measuring deviation of sheet thickness from a
2
standard (URIT-1), range 50-500 9/m error + 3 ~,, beta-radiation,
consistine of 5 units. 7. One- or two-level regulator AF7Y (ARPU) for
the interface between two media, difference in densities 10 and 90 ~-'
operating time 10 secp error 1 40 mmp model .---3P (V-3G) (Talinn Factory).
8. ,-thickness gage -DTT-(BTP) for coatings (varnish, paints,
electroplating, etc.), range - a few mg/cm 2 , accuracy + 2 ~~, source
T1 204 , 120 po (Talinn Factory). 9. Pulp d4naity gage VMT (IPP), range
Card 2/3
Appliances ano apparatus based ...
S/081/62/000/010/049/085
B168/B180-
1.0-1.5 and 1.6-2.1 g/CM3, error 1-5 ~~t gamma-radiation source Cs137,
50 mg-equiv. The following are being developed: 10. PcAtassium
ccncentration gage (RKK-B-1) for measuring thei4ntensity of
40
inherent radiation of K , range 0-20 cl', error t 1.5 2p_*,.(In-t avtomatiki
USSR (Institute of Automation U,krSSR)). 11. Densitomlov for liquids
3
-7--7-5,4 (PZhR-5.4)f range 0.1 to 0.6 9/cm , error 1 21%;
- gamma-radiation
T_
source Cs137 (NIITeplopribor). 12. Liquid analyzer (RAZh~l) for
determining the concentration of one of the components of a binary
rKixture, source Sr9o.(OKBA).
(for atmospheric air), range
14. Level indicator compressed
accuracy �10- mm, source Co6o
translation.-!
13- Ionization methanometer TM-4 (TM-4)
0-5 %, error 1 0.2 %, iource - tritium.
j
cylinder gas ~1`-3 (1U-3), portable,
1 mg-equiv. [Abstracter's dotes Complete
Card 3/3
e.~U_-z
16
S/089/61/010/004/027/027
B102/B205
AUTHORS: Lokhanin, G. N., Sinitsyn, V. I.
TITLE: New universal chamber for handling a-, P-, and y-active
materials
PERIODICAL: Atomnaya energiya, v. 10, no. 4, 1961, 420-421
TEXT: A brief description is given of a new Russian universal chamber
designed for handling hot substances. It consists of two chambers, one of
type 1-KHK (1-KNZh) and the other of type KW (KSh), which are connected by
a pre-chamber. The first chamber is used to handle a- and P-active
materials, while the second one serves for work with 7-active materials of
UP to 50 mg-equiv. Ra; it has a biological shield. The first chamber has
a volume of 0.4 m3, and the second chamber has one of 0.6 m3. Air can be
fully exchanged 25 times per hour. The filter areas of the two chambers
2
are 0.11 and 0.25 m , respectively. Dimensions of the universal chamber:
2970m 2560X 2320 mm; weight: 5700 kg (450 kg +5250 kg). The 1-01"Uh
chamber has already been described in Ref. 1 (Lokhanin, Sinitsyn.
Card 1/2
22622
S/089/61/010/004/027/027
New universal chamber ... B102/B205
Atomnaya energiya, 9, vyp. 4, str 344 (1960)). Radioactive material is
transferred from one chamber into the other through the pre-chamber. The
KSh chamber is equipped with manipulators of the type MIIA-05 (MShL-05), an
instrument box, daylight lamps, a manometer of the type THM-890 (TNM-890),
two-stage filters, several vessels and containers, power supply lines,
pipes for hot and cold water, sewers, and waste cans. The KSh chamber has
a size of 1700x 2540x 2485 mm. Its biological shield consists of cast-
iron plates having a thickness of 100 mm (front), 80 mm (sides and bottom),
and 50 mm (top, back, and in between), and of several lead glasses (total
thickness: 150 mm). The base of the chamber is made of carbon steel and
has a size of 1700-v 980 X940 mm. The two-stage filter used for air
cleanina consists of a glass fabric 200 mm thick and four layers of the
fabrictrin-15-1,7 (FPP-15-1.7). The filter cleans 25 m3 of air per hour.
The pre-chamber is made of stainless steel of the type 1X18H9T (1Kh18N9T)
and 450x 706-x732 mm. large. The operating part of the chamber is made of
stainless steel 3 mm thick and has a size of 900x 706 x725 mm. The waste
containers are of the type 10 KWO(10 KZhO). There are 2 figures and
2 Soviet-bloc references.
Card 2/2
-26687
3/056J61/041/005/002/038
.2.2 B104/B108
AUTHORS: Klebanov, Yu. D., Sinitsyn, V. I.
TITLE: Injection of plasma from a strong pulsed discharge into a
vacuum
PERIODICAL: Zhurnal eksperimentallnoy i teoreticheskoy fiziki, v. 41,
no. 5(11), 1961, 1340-1346
TEXT: The authors describe experiments carried out with two plaama injec-
tion devices: a small and a bigger one (Figs. 1 and 2). The bigger
device in difference from the smaller has two diaphragms with apertures of
5 and 10 mm separating the observation chamber from the discharge chamber.
The injection of plasma from a strong pulsed discharge into hydrogen
(0.1-1.0 mm Hg) was studied. The capacitance of the discharge circuit of
the small device was 40 gF, the voltage was 20-30 kv and the maximum
discharge current was 400 ka. The capacitance of the discharge circuit of
the bigger device was 60 RF, the voltage was 30-40 kv, and the maximum
discharge current was 500 ka. The plasma parameters at different injector
conditions were determined photoelectrically together with a temperature-
Card 1/4
26667
S/056/61/041/005/002/038
Injection of plasma from a ... B104/B108
scan. It is Rhown that plasma is ejected in two opposite directions along
the discharge axis. The plasma was injected in single pulses (2-5 gaec).
The pinches were 30-40 cm long. By means of photoelectric and calorimetric
methods the total number of particles injected by one pulse was determined.
The density and velogity of the plasma were estimated too. The authors
obtained: N = 8-101 ; n = 6_1o13 cm-3; vz = 2.8-1o7 cm/sec. N. V.
Filippov (D. P. Petrov, N. V. Filippov et al., Fizika plazmy i problema
upr. termoyadernykb. reaktsiy (Plasma Physics and Problems of Thermo-
nuclear Reactions), V. 4, Izd. AN SSSR, 1958, P- 170) is mentioned. The
authors thank Academician L. A. Artsimovich and S. Yu. Luklyanov for
discussion of results, M. A. Savenkov and V. S. Shumanov for assistance.
There are 8 figures, 2 tables, and 19 references: 10 Soviet and 9 non-
Soviet. The 3 most recent references to English-language publications read
as follows: F. H. Coensgen, A. E. Sherman, W. E. Nexsen, Phys. Fluids,
765, 196o; F. R. Scott, R. F. Wenzel, Phys. Rev., 119, 1187, 1960; J.
Marschall, Phys. Fluids, 1, 134, 1960.
SUBMITTED: March 21, 1961
Card 2/4
',I. E,
Industrial h-Igh-powtr radiation sources. Atom. energ, 16 no.l:
83-84 Ja 164. (MIRA 17:2)
SINITSYN, V.I.
Use of r--radiographic control methods In certain countries -
members of the Council of Economic Cooperation. Atom. enarg.
16 no.2.,174--176 F 164. (MIRA 17:3)
SINITSYN, V.I.
Use of radioisAopes in the metal Industries of certain*countries,
memberq,,of the~Council of Economic Cooperation. Atom energ. 16
no-3:21%282 gr 164. (MIRA 1713)
S.I.; STNITSYN, V.'I--.
Use of nuclear geophysical. methods in the search, prospecting, and
working of mineral deposits. Atom. energ. IS n0.1:81-84 Ja 165.
M
W~ 18;2)
SJNITSYN, V.I.
New saritar-f --u-',.es for the organization and control of high-
powr isotcpe p2nnts. Atom. energ. 18 no.4:435--436 Ap 165,
(MIRA 1884)
ya.
o o
L 52955-65 ---NT(J)/EPF(n)-2/-.-&WG(=)/EPA(W)-2- -PZ-6/PO-4/Pab-lo/P:L-4.1l.IJP~o
iff;tAT
'ACCESSION NRt AP5010500 tW0056/65j048j00k/1vW1 I.
AUMOR: Osovets, Be No; Sinitsyn, V. I.
6
TITLEt Dynimid -stitbill-sation of a- sma-vinch --- ---
SOURCEt Zhurnal eksperimentallnoy I. teoreticheZ fiziki, V4 48# nos 49 19651
1071-10T6
TOPIC TAGSt plasmi pinch, dynamic stabilAzation, plame stability,, high frequency
plasm stabilization
ABSTRAM Experixents are described, In vh1ch.qzam1e stabilization of apinch
onwing-ourrents -up-to-105--k-has -been -dbitemd,- ft a 639eri,
_lqdrogku -p4s** The,
mental apparatus Is shown In the - fteloture-and- congrists --of7iC main: dig--
charge circuit and a stabilizing circuit. The parameters of the main circuit hre
Cl - 30--&5 pFq U - 5-10 kVp and T - 20--2k jisec. The discharge chamber is filled
with hydrogen to a pressure 0.05-0.1 mm Hg. The stabilizing circuit im made up of
six axial :opper rods insvlALted from the electrodes and ftom the pla-, comj~rising
an inductive load fed from a capaoitor bank controUed by a Yacma trigger whose
operation can be shifted rel&tiye to the initiation Of the mAin diachUge br
Card 1/3
ACCESSION NR: AP5010500 ENCLOSUM-0
1/3
C
ard 3_j
. . ..........
L 45105-66 LWT(1) 1JP(c) AT
ACC NR, AP6024866- soUR`CE O-ODE: Wdb-567 051/001/ T7009"f-
ALIPHOR: Pavlov, Ye. I.; Sinitsyn, V. I.
ORG: none
TITLE: Inhibition of instabilities in a D-Irasma column
SOURCE: Zhurnal eksperimental'noy i teoreticheskoy fiziki, v. 51, no. 1, 1966, 87-94
TOPIC TAGS: plasma column, plasma instability, plasma stability
ABSTRACT: It is shown experimentally that under certain conditions a straight plasma
column carrying a current of 100-120 kA can be stabilized by busbare employing a
rapidly varying magnetic field. The stabilizing contour consists of six busbars
arranged symmetrically on the outer surface of the discharge chamber., vhich has a
diameter of 20 cm. The conclusion regarding the stabilization effect is draun on the
basis of data obtained by streak photography of the radiation, magnetic probe
measurements , and recordings IV a magnetic element of the amount of energy* escaping to
the chamber walls. Orig. art. has: 6 figures. [CS]
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0-0o,000000 4040006i
USW/Geolomy Apr 1947
CHINA/Geology
"Structurral end Orographicel Scheme of the Chinese
Tien-Shan," V. M. Sinitsyn, 6 pp
"Izv Ak NaWk Ser Geol" No 4
Study of the Tien-sban, showing that most olf the
ridges chawn in topographical ma-ps are not ia-
dependent units but parts of eleven larger ridges
eeperated by mountainous depressions. The author
names and Identifies these eleven ridges.
17T58
MW 1947
Sediment,
00m the Quaternary. 11story of Tarim Depression,"
V.
X. Sinitayn, 11 pp
"Byull Moskov Obah lop Pri, Nova Ser, Mel Geol"
Vol IXII, 10 3
Jurassic form of relief continued their developent,
into the Pleistocene era. During this time the Tarim
depression included only the lutcharskly and Jarkend
Basins. ClImste nipre huald then the contemporary one.
Author describe* various sediments of the period, and
their geological 6bamps. lhwlng the last zillenium
the surface dischorgp of rivers decreased; ground
LC 49T33
UMM/Geology (Contd) Xar 1947
vaters sunk to greater depth; forests of the Ttrim
Plain perished; and sands covered settlements in-
habited betveen the 3d and 7th centuries. Gives lo-
cation and types of soils of the period.
LC
StratIrleatIM
%&or-Tag Folds in the Tarts Settled Haself)'" Vi
sudtayn, 4 pp
OD& Akad, Nauk SM, Nova Ser" Vol LVIII, no 3
MIRSer-Tag Mountain Range located In western part at
the Tarim depression in sandy wastes of Tokla-Mokom.
SUMsyn describes -sqw ipological details of wS
ratorest first directed to this range after 3. M.
P1,Wievallskly conducted study of the eastern ez&'.ot
reage, in vicinity of Ihotan-Darl Ri-ver Delta. ftb-.
m1tted by Academician V. A. Obrucbev, 26 Apr 1947.
SIJT 1TSYN, V. M.
RA 4-1T4-1
USSR/Geology Jan
"The History of the Tarim Settled Massive," V. M.
Sinitsyn, 131 pp
"Izv Akad Nauk E�SSR, Bar Geol" No 1
The Tarim settled massive is the western fragment of
the Chinese platform, which settled during the period
of the Yenisian movement. Discusses history of the
development of the Tarim massive and also shows how
its development parallelled the development of some
settled regions in China.
to
Some Basic Problems of Geosynclines," A. V. Peyve, V. M. Siritsyn
IIIZ Ak Nauk SSSR, Scr Geol" ITO 4, pp 28-52
From lon:r personal !rvesti-,ation-c in Central Asia, Kazak-listan, Urals an~d Caucasus, authors
develop new ideas orl.-in, develooment, and structure of 7co-synclines and platforms.
13crore Uri! -er-Prnteruzo.ic ern ther dovel-med ,i continental. shell,
11panniatform," common for future geosynclines and platforms. At 1-,,eginning ofera, after
sharp chan~-e in evolution of -all geological processes, geosynclinal stage of development.
of earth's structure began. Consi-9ted of several qualitatively liffferent stiges. Discusses
general characteristics of stacTes of development of.-posynclinal regions.
PA 162T43
SINITSTN. V.M.
-- The geotectonic factor in ihe change in cllmte.of Centr&I Asia,
Biul. KOIP. Otd. geol. 24 no.5:3-12 049. (NM 11:5)
(Asia, Central--Climate)
IN V.
USSR/ Geology
Card 1/1 Pub. 46 - 3/24
Authors
Title
I Sinitsyn. V. M.
I Geological history of the Lobnorsk plain and the Lob Nor Lake
Periodical I 17,v. AN SSSR. Ser. geolo 6, 30-42, Nov-Dee 1954
Abstract I Using the data of various Investigations the author presents a brief
history on the development of the Lob Nor plain and he arrivea at the
conclusion that the episodical dispalcements of the Lob Nor Lake are
explained by tectonic motions which appear non-uniform in various
parts of the Tarimsic depression. The Lob Nor plain is situated at
the eastern tip of the Tarimsk depression running along the western
regions of Central Asia. Twenty-one iefereacess 11 USSR; 1 Frenchl
2 Swedish; 3 Germanj 2 English and 2 Chinese (1878-1951). maps.
Institution t
Submitted & February 17. 1954
/V
WSIR/Geology Volcanoes
Card 1/1 Pub. 86 - 17/46
Authors i Sinitoyn, V. M., Dre GeologicalJ&.eralogical Soi.
Title New knowledge about an active volcano in Central Asia
Periodical I Friroda, 43/9, 89-90,, Sep 1954
Abstract I The t4ndency of volcanoes to be located near coastlines or
island groups is noted., so that inland volcanoes constitute
objects of special interest. The finding of a new active
volcano in the Kunlun Mountains north of Tibet is reported
confirming the collateral evidence of subterranean activity
in that region. Map.
Institution 3
Submitted I *gas*
SINITSYN, V.M.
~
General tectonic system of the great Asian upland. Biul.KOIP.Otd.geol.
30 no.2:51-65 Mr-Ap 155. (Mtn 8: 8)
(Himalays, mountains)
SINITSYN, V.K.
General physical geographical survey of the Imuchow-Almse-Ats,
railroad region (within the borders of the Chinese People's
Republic). Izv.Tss~.geeg.ob-v& 87 n9-6;505-515 N-D '53.
(MU 9:3)
(Chtna-Physical geography)
SINITSYN, V.M.
-
Tectonic origin of the lunlum range. Dokl.AN SSSR 106 no.5:901-903
7 '56. OWU 9:7)
l.Laboratoriya geologii uglya Akademii nauk SSSR.Prodstayleno akademi-
kom V.A.Obruchevym.
(Kunlun--Geology, Structural)
SINITSYN, Vasiliy Mikhaylav,ich; OBRUCHEY, V.A. [deceased], akademik,
n nyy , r- MERG S
e .___'4VANOV, A.Kh., otvetstvennyy red.; A OV
G.G., red.izd-va; GUSEVA, I., tek-hn.red.
[The Turfan-Kham Depression and the Gashun Gobi; geological
reconnaissance of 19521 Turfan-Khamiiskain Ypadinn i Gashunl-
skain Gobi; geologicheskie rekognostairovki 1952 goda. Moskva,
Izd-vo Akad. nauk SSSR, 1957. 106 p. (MIRA 11:1)
(Gobi--Geology)
SINITSYR, Vasiliy Mikhayloviq4; ORRUCHEV, V.A.. akademik. otvetstvennyy
Aah., otvatstvennyy red.; GAIAJSHKO,
Ya.A.. red.izd-ve.
[11orthwestern part of Tarim Basin; a geological study] Severo-
zapedneia chast' Tarimskogo basesins; geologicheskii ocherk.
Moskva, Izd-vo Akad.neuk SSSR, 1957. 248 p. (MVU 11:3)
(TarimSasin-Geology)
ittj !.ioit - Sinitsyn, V.M. 10-58-3-5/29
TITLEt Geographical Observations in R1gbo.~jftjiaft Regions of Central Asia
(Geogrsficheskiye nab1yu&xdya'v vysokoy Azii)
PEKODICALt Izvestiya Akademii Nauk SSSR, Seriya Geograficheskaya, 1958,
Nr 3, pp 37 - 47 (USSR)
ABSTRACT; In summer 1956ja team of geologists from the Geological Insti-
tute of the Chinese People's Republic Academy of Sciences cross-
ed High Asia (a territory of 2,500,000 square kilometers in
Central Asia including the Highland of Tibet surrounded by the
mountain chains of Kun'lun' and the Himalayas) along the recent-
ly built Tsinkhay-Tibet highway. The only Soviet participant
was the author of this article, V.M. Sinitsyn, who gives a de-
tailed description of his observations. The author subdivides
his article into the following parts; 1) the latest orographic-
al structure of nigh Asia, 2) climate, 3) the hydrographic net-
work, 4) glaciations. There are 4 maps and 10 references, 6 of
which are Soviet, 3-English and 1 German.
ASSOCIATION, Laboratoriya geologii uglya Akademii Nauk SSSR (Laboratory for
the Geology of Coal at the AS UM)
AVAILABLE: Library of Congress
Card 1/1 1. Geology - Asia
~UTHO H: Sinitsyn, NX. nnd "initsyn, V.'-' 11-5R-4-1/16
TITLE: Tyanl-'3han'. Major Tectonic Elements (Tyan;-`~han.~, ~1-vneyshiye
elementy tektoniki)
PERTUICAL: Izvestiya Akademii Mauk SSSR, Seriya Geologicheskaya, 1958Ar 4,
P? 3-17 (USSR)
ABSTRACT: Tyan'-Shan', one of the largest mountain systems of Asia, is a
huge Paleozoic folding formation, composed of a lnrge number of
separate tectonic zones, differing in age, structure, deposits,
and magmatic occurences. The zoning of its tectonics is ex-
pressed in the in.terlocation of structures of Caledonian and
Hercynian stages. The caledonites form one fully separated
belt which can be 6raced along the whole length of the range,
The hercynites form two belts - scuthern and northern - which
border the Caledonian body. The structure of caledonites is
very complicated and has been insufficiently studied,. Generally
speaking, the whole system of the Lower-Paleozoic folding., with
the fragments of pre-Paleozoic structures and large reF:ions of
expansion of epi-Caledonian Fiddle-Ppliozoic formations, are
attached to the caledonites. --he relative importance of fraC-
ments of Pre-Cambrian structure in the Caledonian otructu.-e was
Card 1/3 taken by one of the authors (Ref, 14), as A criterion for sub-
Tyan'-3hanl. MnJor Tectonic Flements
11-5,Q-4-1/16
dividing the Caledonian folding zone into three parts: the
Yaratau-Talass, Sussamyr and Narat regions. A special feature
of the stratigraphic columnar section of the folding zone is
a large expanse of thick Lower-Paleozoic strata, an imrortant
development of pre-Cambrian strata and secondarily important
Viddle-Paleozoic r!eposits. In the Lower-Paleozoic strata-,all
the Cambrign and '. -;rdovician formations are found, represented
mostly by terrigenous deposits and to a lesser part - by car-
bonaceoun Fnd .olcnnopenous rocks. The magmatism of the cale-
donites -",- exhibited 1)y the domination of granitoids and by
the rarity of basic and ultra-basic intrusions, The hercynites,
which form two belts - southern and northern - represent a
complex of usually small folding zones of various age. nll Plong
the Viddle and Uprer Paleozoic. There are three distinct age-
groups: early hercynites formed during the Silurian and early
Devonian periods; middle hercynites - of Lower and Middle Car-
boniferous periods and late hercynites - of Upper Carboniferous
and Permian periods. The northern Hercynian belt is .-mainly
in China. Only the Djungarian (Dzhupgarskiy) Alatau ran;re of
mountains belongs to the USSR. The'folding structure of its
central Part belongs to the oldest formations. It is formed
Card 2/3 by thick sand-shistous strata of Devonian age, The southern
TyanI-,.,h--n'. ".njor Tectonic Elements
11 -V-1-1/16
belt of the Hercyni;;n folding zone Ire;,ins --t q,2n,-4 meridian
and extends to the west for 2,CCIC km, reaching the r'yzyl-Kum
plain, Tt is formed '~y hercynites of three age --roups (as
.-bove). The early hercynites extend alone, the southern ranges
of Tyan'-Shanl from t~ie Lob-Nor lake to the IFer!T.In ranE-e. The
middle hercynites form the Chatkal and Kavak zones and the
zone of elevated foot-hills of the northern slopei3 of the
Altay range. The Chatkal zone includes the Chatkal, Pskem,
partly Ugan, .,'.toynak and Fereanian mountain "ranges. The
Yavak zone includes the structures of mountains in the middle
part of the *,,.,qryn Piver. The late hercynites in the southern
branch of TyPnI-Shan' form the South-Giscar, Surrietash, Yara-
Chatyr, Varzhan-tau - Xuramin, Dzhamandnvan and Aksay (l.aydan-
Tne~') zones, formed in the Upper-Carboni.ferous and Permian
periods. The authors describe in detail all these zonec-~.
Therewe 1 man and 15 Soviet references.
ASSOCIA-IO,",: Lenineradskiy posudarstvennyy universitet, Lahoratoriya feologii
uglya AN SS'~-,R (The Leningrqd State University, Lpboratory of
CoaJ 5eology of the AS USSR)
SUBVTTT'FD: August ip,1957
I
Card 3/3 1 G-oloGry - Asis
AUTHOR: Sinitsyn, 11JA SOV/12-90-6-3/23
.0"Sr' ~
,,l.fTLE: evelopment of the ideas of Academician V.A. Obruchev
in the Recent investigations of Central Asia(Razvitiye idey.
akad, V.,A, Obrucheva v noveyshikh issledovaniyakh tsentrall
noy Azii)
PERIODICAL: Izvestlya Vsesoyuznogo geograficheskogo obshchestva, 1958,
Vol 90, Nr 6, PP 521 - 530 (USSR)
ABSTRACT: This article is based on ideas formulated by the late Aca-
demician V, A. Obruchev who indicated ways of solving
problems of the geology and &reo,-raphy of Central Asia. The
article deals with two main problems to which Obruchev de-
voted much attention, i,e. the origin of loess, and recent
movements of the Earth crust. Obruchev propounded the the-
ory of the eolian origin of Central Asiatic loess and he
considered that loess layers are dissimilar with respect
to their composition, structure, occurrence and origin.
They can be divided into two categories: typical loess, i.e,
unstratified formations originating from dust deposits,
transported by winds from deserts; and loess-like strati-
Card 1/3 fied layers, deuosited by water, He assumed that loess
SOV/12-90-6-3/23
The Development of the ideas of Academician V.,A,. Obruchev in the Recent
Investigations of Central Asia
was accumulated during the placiation epoch and that the
transformation of loess into loess-like layers was caused
by the subsequent humidification of the climate in connec-
tion with recent movements. There exist three types of
loess: loess of mountainous areas, highland loess and loess
in alluvial plains. These types are analyzed and the con-
elusion-is made that in mountainous areas eclian loess is
prevalent, that the occurrence of proluvial-alluvial loess
is developed in high-lands and is also prevalent in the
Tarim Plain, Loess accumulation was a continuous process
which took place during an extended period cf the Quater-
nary, and in some regions is still going on. The second
problem treated by Obruchev was the recent movement of the
Earth crust occurring in the Neocene and Quaternary epochs.
He proved that these movements have a considerable effect
on the development of the actual Earth relief, which can be
particularly well observed in the Central Asiatic region.
He proved furthermore that recent movements affect the cha-
Card 2/3 racter and structure of the hydro-geographical network, sub-
SOV/12-90-6-3/23
The Development of the Ideas of Academician V,A. Obruchev in the Recent
-Investigations of Central Asia
terrestrial water movements, the climate and the development
of organic life, These theories were confirmed by the lat-
est investigations. Obruchev;s theories on the movement
of the Earth crust explain the tectonic nature and morpho-
logj of Central Asiatic mountains, There are 1 map and 10
references, 9 of which are Soviet and 1 German.
Card 3/3
SIMITSYN, Vasiliy Mikhaylovich-. ZABIROV, B.Sh., red.; LAVRWIMA,
To.Y.. red,j 1"'OUSTSKIT, G.W.,7red.kart; NOGINA. N.I.,
tokho.rod,
(Central Asia] ?Sontrallnaia Asiia. Noskva, Gos.izd-ve
geogr.lit-ry, 1959. 454,po. (MIRA 12:7)
(Asia, Central--Physical geography)
3(5)
AUTHOR:
SOV/20-125-6
Sinifsya*.Y, -43/61
TITLE: Mongolian-Siberian Anticyclone and the Regional Zonality of
Eolian Deposits of Central Asia (Mongolo-sibirskiy antitsik-
lon i regionalInaya zonallnost' eolovykh otlozheniy Tsentra!4-
noy Azii)
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 125, Nr 6, PP 1326-1328
(USSR)
ABSTRACT: The Mongolian-Siberian maximum forms in the winter the baric
main centre of Eurasia. It is formed in consequence of an
extremely intense cooling and condensation of the air over
East Siberia and North Mongolia. The known maximum pressure
on the whole globe is bound to this region: Irkutsk 810 mm.
Furthermore~ an extremely intense anticyclone air circulation
(like in the title) is related to this maximum which propagates
over Central Asia and South-East Europe. The masses of dense,
dry, and cold air formed in the above-mentioned region become
mobile in the peripheral regions and flow to the regions
with lower pressure, The main current flows to Central Asia
where the air over the deserts is especially heated and thin.
The low Khangay chain as well as the eastern Altay spurs are
Card 1/4 easily passed. So this air appears in the Gobi plains and
Mongolian-Siberian Anticyclone and the Regional Zonality SOV/20-125..6-43/61
of Solian Deposits of Central Asia
dries and cools them in the extreme. The anticyclone which is
only 3,000 m high is now almost turned aside by the chains
of the Kuenl-lun' and Nan'shan' (6,000m and more) into the
latitudinal direction (the depressions of the 40th parallel)g
partly towards the east - towards Ala8han' and Ordos, partly
towards the west - to the Tarim basin. Thisenticyclone is
destroyed in springg in summer, however, the air over the
Central Aaiatic, deserts is heated. A region of low pressure
is formed into which currents of humid air penetrate from the
Atlantic and Pacific. The air loses, howev3r, almost its entire
humidity on the exterior slopes of the border mountains.
Over the Gobi the resultant dry marine air masses assume
quickly the properties of local air. Thus, dry continental
air is preserved during the whole year over Central Asia.
This is the reason of the maximum degree of aridity of its
climate. The processes of denudation are very weak here in
consequence of the few water courses, they almost stop.
Winds are, however, very strong and frequents They are able
to do geological work. Not solidified and weakly cemented
Card 2/4 sediments are blown away.. sands whirled up, loess dust clouds
Mongolian-Siberian Anticyclone and the Regional SOV/20-i25-6-43/61
Zonality of Eolian Deposits of Central Asia
blown up, and even parent rocks corroded. Therefore the
quaternary envelope consists mainly of formations of eolian
origin. This work is, however, done by the air currents related
to the afore-mentioned anticyclone. This is shown by the zonal
distribution of eolian deposits. They lack in the North
Mongolia which lies in the region of the formation of the
anticyclone and has therefore no considerable atmospheric
movements. The air masses in the lake plains of West Mongolia
and in the East Gobi depression become more and more mobile
till they have assumed the physical properties of local air
and the winds die down. Figure I shows the zones. A small
belt of sand deserts exists in the north where the anticyclone
is formed. Vast desert plateaus of stones - hammadas - lie
in the following zone where the wind attains its maxi
intensity. A broad belt of the southern sand deserts:
Takla-Makan, Dzosotyn-Elisu (Dzungaria) and Badanchzhareng
(Alagchan') lies on the further way of the anticyclone
current. Here the wind is not able to move the sand so that
it is accumulated in gigantic quantities. These deserts are
Card 3/4 followed up by an accumulation zone of eolian loess:
Mongolian-Siberian Anticyclone and the Regional SOV/20,-125-6--43/61
Zonality of Eolian Deposits of Central Asia
the northern slope of Kuen'lun1v Eaut-Kan'su platform,
North Shensi, etc. The dunes reflect the direction of the
anticyclone. Finally, it was detected tbatthe Mongolo-
Sibirskiy anticyclone existed during the whole postgla3ial
period, i.e. 12-15,000 years. There is 1 figure.
T
ASSOCIATION.i "aboratoriya goologii uglya Akademii nauk SSSR (Laboratory
of Coal Geology of the Academy cf Sciences, USSR)
PRESENTED: November 28, 1958, by D. V. Nalivkin. Academician
SUBMITTED: November 279 1958
Card 4/4
SINITSYN. Nikolay Kikhaylovich [deceased]; ZIjjZMV.M., prof., oty.
red.; KUMUMO-MMMAY, A.D., red.; OGM, V.N.. red.;
PORSOMKOV, G.S.. red.; MAMA, T.I., red.; VOCLAGINA.
S.D.. tekhn.red.
[Tectonics of mountains forming the borders of Fergana] Tektonika
gornogo obramleniia Pergany. Leningrad. Isd-vo Leningr.univ
196o. 218 p. (KERA 14:1)
(Fergana-Geology, Structural)
SINITSYN, Y.M.
Some characteristics of the distribution of Tertiary coal areas
in Eurasia. Trudy Labe geol. ugle no.10.-245-254 160.
(MIU 13:9)
(Burope-Coal geology) (Asia-Coal geology)
SINITSY -3th" daktor geol.-miner.nauk, otv.red.; KULIKGV, M.V., red.
2~~Y ~N
izd-va5 A:-,()!IS, R.A., tekhn.red.
LHistory of the lower ~bsozoic coal accumulation in Kazakhstan*
Part 2] Istoriia Nizhnemezozoiskogo uglenakopleniia v Kazakh tane.
Part 2. Moskva, Izd-vo Akad,nauk SSSR, 1961. 252 p. 53 plates.
(Akadeniia nauk SSSR. Laboratoriia geologii uglia, Trudyt no.13).
MIRA 15310
(Kazakhstan---Coal geology)
SiNITSYN, Vasiliy I-likhaylovich; LAVROV, V.V., doktor geol.-m-ineral.
nauk, otv. red.; SMIGER, I.A., red. izd-va; FRIOGRADOVA, Ei.F.,
tekhn. red.
[Paleogeography of Asia]Paleogeografiia Azii. Moskva, Izd-vo
Akad. nauk SSSR, 1962. 266 p. (MIRA 16:1)
(Asia--PaleogeograpIV)
RUK11114, Lev Dorioovich; doktor gcol.-iidnor. nauk,
retsenzent; RUMINA, Ye.V., kand. geol.-rdner. nauk, red.;
TOKAREVA., T.N., ved. red.; SMOVOVA, I.M., tekhn. red.
[Fundamentals of general paleogeogrcpby]Osnovy obsbehei pa-
leogeografti. Izd.2., perer. i dop. Pod red. E.V.Rukbinoi.
Leningrad, Gostoptekhizdat, 1962. 628 p. (WRA .15:11)
(Paleogeography)
BALASHOV, Z.G.; VRUBU-VSKIY, M.I.; LEVEDEV, V.I.; SINITSYN, V.M.
Seventieth birthday of S.S.Ku7netmov. Yest.IDU 18 no.6s5-7
163, (KM 16:4)
(Kuznetsov, Sergei Sergeovich, 1892-) d.
t
KUZNETSOV, S.S.,- IEBEDEV, V.I.-, ~_~~NgN,_V.M
The most important scientific problem. VeBt.IDU 18 no.W-11
163. (KIRA 1624)
(GeologT) .
T
SI~qTSPIJ V.M.
"The Kunlun and the Tarim.,
Reviewed by V.M. Sinitsyn.
JI-A 162
&ZL--Landforms) (Tarim
(Chohou
w edited by E.M. 14urzaev, Chshou Li-eing.
Izv. Vses. Cefr,. ob-va 94 no.4:354-356
(MIRA 15:9)
valley) (Murzaev, E.M.)
,Li -*sang)
S.PLTSYN, V.N.
One characteristi of the geologiCP-l 5trUCW-re of Asia. Trudy
Gool. muz. Aff SSSR no.14:170-176 163. (MIRA 17:11)
VOLKOVA, I.B.; NALIVKIN, D.V.; SLATVINSKAYA, Ye.A.; BOGOMAZOV, V.M.;
GAVRILOVA, 0.1.; GUREVICH, A.B.; MUDROV, A.M.; NIKOLISKIY, V.M.;
OSHURKOVA, M.V.; PETRENKO, A.A.; POGREBITSKIY, Ye.O.; RITENBERG,
M.I.; BOCHKOVSKIY, F.A.; KIM, N.G.; LUSHCHIKHIN, G.M.; LYUBER,
A.A.; MAJWDONTSOVO A.V.; SENDERZON, SINITSYN.Jm'i SHORIN,
V.P.; BELYANKIN, L.F.; VALITS, I.E.; VLASOV, V.M.,* ISHINA" T.A.;
KONIVETS, V.I.; MARKOVICH, U.N.; MDKRINSKIY, V.V.; PROSVIRTAKOVA,
Z.P.; RADCHENKO, O.A.; SEMERIKOV, A.A.; FADDEYEVA, Z.I.; BUTOVA,
Ye.P.; VERBITSKAYA, Z.I.; DZENS-LITOVSKAYA, O.A.; DUBARI, G.P.;
IVANOVP N.V.,- KARPOV, N.F.; KOLESNIKOV, Ch.M.; NEFEDIYEV, L.P.;
POPOV, G.G.; SHTFJeEL', B.M.; KIUUOV, V.V.; I;VROVP V.V.;
SALINIKOV, B.A.; MDNAKHOVA, L.P.[deceased]; MURATOV. M.V.;
GOBSKIY, I.I., glav. red.; GUSEV, A.I., red.; MOLCHANOV, I.I.,
red.; TYZHNOV, A.V., red.;,SRABAROV, N.V., red.; TAVORSKIY, V.I.,
red.; -REYMRT, L.A., red.izd-va; ZAMARAYEVA, R.A., tekhn. red
(Atlas of maps of coal deposits of the U.S.S.R.]Atlas kart ugle-
nakopleniia na territorii SSSR. Glaw. red. I.I.Gorskii. Zan.
glav. red. V.V.Mokrinskii. Chleny red. kollegii: F.A.Bochkovokly
i dr. Moskva, Izd-vo Akad. nauk SSSR, 1962. 17 p.
(MIRA 16:3)
1. Akademiya nauk SSSR. Laboratoriya geologii uglya. 2. Chlen-
korrespondent Akademii nauk SSSR (for Muratov).
(Coal geology-Maps)
V, M.
of fioll.sr epergy ir deve )V,,
T=~,
14
At
MATROSOV, P. So; SINITSYN, V. M,
A new land mark in the geological study of Mongolia&
Izv,AV SSSR, Sergeol, 29 no. 1:1-10-11-1 Ja #64, (MIRA 17:5)
SINITSYN p V.11-1.
Fundamental investigation of t~e Up,,Pr Y-aleozoic in Central Asia.
Vest. ICI:, 19 n0.18:127-129 164. (MIRA 17:11)
VORONTSOV, Valentin Viadindi-ovich; SINITSYN, V.1--,, geol.-
m1ner. nauk,prof.j ~ I .
[Stnicture and conditlons governing the formation of Lower
Mesozoic coal measures in the Karaganda Basin] Stroenie i
us.lovJJ.a obrazovanila rd.zhnemezozoLskoi uglanosnoi tolshchi
KaragRtAinakogo bnssninki. Ylosl-nqv N-9tikag 1,965. 139 p.
(MIRA 18:3)
SINITSYN, V.M.
Long-period changes of geological processes as revealed by a
study in Asia. Vast. LGU 19 no.2425-3L 164 (MIM 18.-l)
L711 2'
Om"Ma 18::Io)
SINITSYN, Vas:lliy MikW1.4svI,-,rq SKORYNINA, rei.
Paleo climatology of Eurasia] Dre,,nle klimaty Eirfazi.f..
Le.mingrad, Izd-7o Leningr, univ. Pt.--,. 1965. `Q5
(MIRA M22)
INSNRS~
I- ".Y/ -rS "V V. 'P.
E:? / BRUSOV, ~.L; PIMYGIN, N.3 ; SIVITSYN. V.P.; VISHNYAKOV, V.N., re-
daktor; PITROVA, M.D.: te*ftVrftW""6daktor.
[Air raid and chemical warfare defense) Protivovosdushnaia i
protivokhimicheskais. zashchita. Moskva, Dobrovollnoo ob-vo so-
detstviia arnii. aviataii i flotu. 1952. 111 p. (Microfilm]
(Air defenses) (MLB& 7:11)
BRMOV, I.I.; PIMLIGIN, N.S., SINIT
P,.;,..KUROGHKIN, F., redaktor;
MARMO, V., tekhnich re dator.
[Defense against air bombardments and chemical warfare. Translated
from the Fbassian] PrOtYPOTitrianyi i protykhimichnyi zakhyst. Pe-
reklad z roeiialkoi. J~ylv, Derzhavne vyd-vo tekhnichnoi lit-ry
URSR, 1953. 108 P- (MIRA 8:2)
(Air defenses) (Chemical warfare--Safety measures)
SiLITS'Ill) V. P.) ijitusov, 1. 1. and PERELIGIN, N. S.
IlAnti-Aircraft and Anti-Chemical Defense," Kiev, 1955
kandidat takhnicheskikh nauk; KALOV. N.F., kandidat tekhai-
cheskikh asuk; MANDRAZHITSKIY, M.N.; BORKMOVA, Y.D.; IAVROTSKIT.
X.F.. redaktor; DZHATIYBV. S.G.. tekhnichaskiy redaktor
(Local air defense; textbook for secondary schools and pedagogical
schools] Mestnaia protivovozdushnaia oborona; ucbebnoe posobie dlia
arednikh shkol i podagogicheskikh uchiliahch. Pod red. Sinitsyna.
Moskva. Goa. uchebao-pedagog. izd-vo Ministerstva prosveshcheniia
RSFSR, 1956. 150 P- [Microfilm] (MLRA 9:12)
(Air defenses)
MOSKALRY, V.D.. re(laktor; I YN V.P., redaktor; TERTYCHNYY, A.B.,
p
Za'!'
redaktor; XANZVSXATA. M.D~~me
M.D., r'∨ XARYAKIRA, M.S., tekhatcheekly
radaktor
Obnual on local air defensel Uchabnos posoble po WYO. Pod obshchat
red. V.D.Koskaleva. V.P.Stultsyno, A.S.Tertychnogo. Kooky&, Isd-v
DOSW. 1956. 222 p. [Microfilm] (NLRA 10:4;
i. Veasoyuzaoye dobrovollnoye obahchestvo sodaystviya armil.
fivtatsii I flotu.
(Air defauses)
PHASE I BOOK EXPLOITATION 1132
Levin, M.Ye-J. Kalinin.. G.A.J Mandrazhitskiy, M.N.,- Sinitsyn, V.P. and
Fedorov, V.I.
Zashchita ot sredstv massovogo, porazheniya (Defense Against Weapons of mass
Destruction) Moscow, Uchpedgiz, 1958. 181 p. 100,000 copies printed.
Eds. (Title page): Sinshchyn, V.P. Candidate of Technical Sciences and Kalinin, G.A.
Ed. (Inside book): Lavrovskiy, K.F.; Tech. Ed:Natapov, M.I.
PURPOSE: This book-is intended for public instructors of the PVO DOSAAF
(Antiaircraft Defense Unit of the All-Union Volunt" Society for the
Promotion of-the Army, Aviatipn and Navy).
COVERAGE: This book includes general information on atcmicl chemical aud "bacteri-
ological weapons and measures for individual ard collec+ive protection from them.
The various-mxthors contributed to the text as follows.* M.Ye. Levin wrote Chap-
ters 1,2,3,4 4nd.6; M.N. Mandrazhii~kiy,__' Chapters 7,8 and-9; G.A. Nalinin -
Chapter 10; V.P. Sinitsyn-Chapters 11, 12, and 14; and V.I, Fedorov -Chapter 5.
Card l/ 3
PtNITSVN
PLUR I BOOK S07/4103
levins Noisey Yevoeyevich., Georgly Andreyevich Nslininy Mikhail, Zkolayevich
amdrazhitakiyj, Valentin Petrovich Sinitsyn., and Valeriy Ivanovich Fedorow
Zeshchita at sredstv massovago porazhaniya (Protection Against Means of Nion
Destruction) 2ad ed. Moscowj, Uchpodglzp 1960. IT6 P. 509000 copies
printed.
General Zd,: V. P. Sinit"n. Candidate of Technical Sciences., and G. A.
Mialinin. Rd.: A. A. Korotk1y; Tech. 19d.: R. V. Tsyno.
PURPOSZ: This book is intended for the public instructors of M
DOSAAF (Air Defence Organization under the All-Union Voluntary Society
for- the Promotion of the Arwyj, Aviation and Navy).
COWARAGE: 2he book gives ftmdamental information an atomIc,, Chemical., and
bacteriological vespons and on means of individual and collective
protection. It states that the jxroblem bas been studied sufficiently
and that at the present time adequate means of protection exist for a
vell-organized and trained populdtidn. . No personalities are a, z"1 I d.
There are no references.
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Protection Against Means of Hms Destruction SW/4103
Ch. 9. Tasks and Organization of the local Air Defense Belative to
Dwellings.9 ft-tablishments., Institutions, and State and Collective
Forms, Rules of Conduct and Action for the ftialstion According
to the Signals of the local Air Defense 103
Ch. 16. Reconnaissance of StrlWwn Areas 3-10
Ch. 3.1. Imergency and Beseming OWations In Stricken Are" 130
Ch. 12. Fire Prevention Meammes; Ibetinguishing Fims in Progress and
Breaking Out 336
Ch. 13. Methods and Means of Decontanination; Degamming and Diminfectlon 145
Ch. 3.4. Daties of Personnel of Self-Defense Group Responding to Signals
Given by the local Air Defense 266
AVAEMIX: Library of Congress (IM926.IJ8 19(36)
Ac/rn/ee
Card 3/& 8-25-6o
L 3261.0-66 EWTO
;,CC -NII: AT6011924 SOUHCE CODE: Ult/0000/66/000/000/0028/0031
AUT11011: Sinitsyn, V. S. (Novosibirsk); Senin, A.G. (Novosibirsk)
011G:
TITLE: The synthesis of measuring information systems for the extrapolation of random
uniform fields
SOURCE: Vsesoyuznaya konferentsiya po avtomaticheskomu kontrolyu i metodain elektri-
cheskildi izmereniy, 5th. Avtomaticheskiy kontroll I metody elektricheskikh tzmereniy;'.
trudy konferentsli, t* * eritellnyye informatsionnyye sistemy. Ustroystva avtomati-
cheskogo kontrolya. Elektrl eskiye izmereniya neelektricheskikh velichin (Automatic
control and electrical measurfqg techniques; transactions of the confere , v. 2: Information
measurement systerns. Automatic control devices. Electrical measurements of non-
electrical quantities). Novosibirsk, lzd-vo Nauka, 1966, 28-31
TOPIC TAGS: information processing, mea: optimal control, automatic
control theory
ABSTRACT: Arbitrary dynamical systems are usually under the Influence of random inter-
actions, and thus during the analysis and synthesis of measuring systems it Ip natural to
Ipply statistical methods. Methods developed by the theory of random functions seem to be
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SIRITSYN, V. V.
Sinitsyn, V. V.
"The biological activity of ultraviolet rays which have passed through light
clothing fabrics." State Order of Lenin Inst for the Advanced Training of
Physicians imeni S. M. Kirov. Leningrad, 1956. (Dissertation for the
Degree of CancUdate in Medical Sciences).
KnizhnaZa letopis,
M. 21, ly5b. Moscow*
U'-)SR / Gonaral and -pacialized Zooloeyl InsOctsi The P
Biological '-'othod for the Control of Harmful
Insocts and --.oarids.
Abs Jour: Raf Zhur-Biol., No 13, 1958, 59237.
.A.uthor Stativkin, V. G., Paregonchenko, B. I.,
Sinitsyn, V. V.
Inst t given.
Title Our E-othod of icttling the Psoudaphycus malinus.
Grig Pub: Zashchita rast. ot vredit. i bolcznoy, 1957,
No 4, 43-44.
kbstract: Tho propagation of the Comstock itiealybug is
chacked by the presence in her colonies of
35-50-A mwmaies with the Pseudaphyci inalini.
The yiald of M from the soil by Lianual labor is
about 10 thousand H a day per man. It is increased
tenfold throuch the attraction of !,-.- from the mass,
Card 1/2
MARGOLIS, S.Ya.., inzh.; SINITSYN, V.V., inzh.
Determining the least radii for turning and the width of the
"clearance corridor" when transporting large art0ifte.
Prom. stroi. 39 no.11:42-44 161. (MIRA 14:12)
(Concrete products)
(Transportation., Automotive)
GOREUX2 L.L.; KOVALISKIY, N.Go; PODOORM, I.M.; SINIT87Np V.V*
Study of the escape of plams. through the magnetic gaps of
traps vith a field intmenirying toward the periphery* Bokle
AN SSSR 147 no.3t576-579 N 162. (NW 15tl2)
1, Predetavleno akademikom L*Ao Artsimovichame
(Plasma (Ionized Ones)) (Magnetic fields)
42220
S/057/62/032/011/014/014
B104/B102
AUTHORS: Gorelik, L. L., and Sinitsyn, V. V.
TITLE: The separate measurement of energy losses from a plasma due
to radiation and through particles.
PERIODICAL: Zhurnal tekhnicheskoy,fiziki, v. 32, no. 11, 1962,-14o6-140d
TEXT: According to the estimates of V. I. Kogan, a 1 cm layer of hydrogen
at a pressure of ---0-1 mm Hg absorbs practically no radiation from a
plasma, whereas it completely absorbs particles having energies between
50 and 100 ev. Here preliminary results of eiperiments are given in
which this effect is used for separately measuring the energy spectrum
of the radiation and of the particles, with the help of a bolometer and
a gas filter. The experiments were carried out with a toroidal discharge
chamber of type "Beta": inner diameter of the discharge chamber 21.6 cm,
longitudinal field RZ a 600 oersteds, maximum discharge current_65 ka,
intensity of the eddy electric field - 4v/cmp pressure (3-4)-io 3 mm Hg,
discharge time rvO.8 msec. The measuring chamber (Fig. 1) is an aluminum
box in the form of & cone enclosing the bolometer. The bolometer is
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S/057/62/032/011/014/014
The separate measurement of ... B104/B102
mounted on the end of a movable copper rod enabling it to be moved along
the axis of the chamber. If E b is the energy striking a unit area of the
bolometer, and E0 the energy striking unit area of the chamber walls, the
energy Zk which is incident on the chamber wall is given by Ek W k(R)E b(R)'
where k(R) is a factor which takes account of the solid angle between the
bolomever surface and the plasma, and R is the distance between the
center of the discharge chamber and the bolometer. Information about the
energy loss caused by the particles (E p) is obtained from the dependence
of E k/Eo on R (Fig. 3). After two days of vacuum treatment Ep is found
to be after three days '~:V4054. There are 3 figures.
SUBMITTED: January 29, 1962 (initially)
March 19, 1962 (after revision)
Fig. 1. (a) Measuring chamber. (b) slit of the measuring chamber.
Fig. 3. E relative a (Ek/Ed-100% as a function of R. Legend: (1) After
two days of vacuum treatment, (2) after three days of vacuum treatment.
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I
ACCESSION NR: AT4025318 S/0000/63/000/000/0270/0273
AUTHORS: Gorelik, L. L.; Kovallskiy, N. 0.1 Podgorny*y, I. X.1
Sinitsy*n. V. V.
TITLE: Investigation of plasma in an "Orekh* magnetic trap with the
aid of special bolometers
SOURCE: Diagnostika plazmy*_(Plasma diagnostics); &b. statey.
Moscow, Gosatomizdat, 1963, 270-273
TOPIC TAGS: plasma magnetic field, magnetic-mirror, plasma con-
finement, bolometer, tbin film
A13STRACT: The spatial and time distributions of beat flow from the
wall of a magnetic-trap vacuum chamber with a field that increases
towards the periphery were investigated to ascertain the influence
of the region near the point of zero fiela in' the escape of chaFged
particles at low plasma concent~rations, and also the character of
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ACCESSION NR: AT4025318
time variation of the width of an annular magnetic slot. Several
specially developed bismuth bolometers were used to measure the heat
flow from an "Orekh" magnetic trap. The bolometer constructions
are described. Measurements of the magnetic gap have shown that
the width of the gz~p is larger at small values of the magnetic field,
and the experimentally observed broadening of the magnetic gap can
be sufficiently well explained by classical diffusi.on. The escape
of plasma particles was-measured by introducing a metallic cylinder
into the trap and measuring the heat escaping through the magnetic
gaps with germanium boromieters. In the case of the first configura-
tion of the magnetic field in the trap it was found that the par-
ticle escape from the system is due to loss of the adiabatic invari-,
ant on entering the region of weak magnetic field near the,center,
whereas in the case of the second configuration the plasma is essen-
tially concentrated in the region of the weak magnetic field near
the center. Thin film bolometers were also used to measure the oz-
cape.of heat from the trap for plasma of high density (~101 .4 cz~-3)
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ACCESSION NR; AT4025318
and low density (10 12 cm-3 The escape times were found to be
60-70 and 150-200 microseconds, respectively. The bolometers
described can be used to solve various problems in plasma physics.
orig. art. has: 2 figures.
ASSOCIATION: None
SUBMITTED: 190ct63 DATE ACQ:' 16Apr64 ZKCLs 02
SUB CODE: ME NR REP SOV& 004 OTHER& 000
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ACCESSION NR.- AT4025318
m
CEO
Magnetic field configuratiom in the 10rekhe trap
INCU)SURE: C)l
card 4/5
1 2 3
11C AM*
Construction of bisinuth bolometers
frame-, 2 - oxidized-aluminum folLl, 3thermoresistance of
lead-bismuth alloy, 4 silver lose,&
ACCESSION NR: AP4020580
S/0057/64/034/003/0505/0508
AUq.IIOR: Gorelik, L. L. ; Sinitsy*n,--V.V.
TITLE: New three-layer bolometers for measuring energy losses in plasmas
SOURCE: Zhurnal tollchnichaskoy fiziki, v.34, no.3, 1964, 505-508
TOPIC TAGS: bolometer, three-layer bolometer, high time resolution bolometer, plas-
ma, plasma energy loss, plasma energy loss measurement
ABSTRACT: This paper describes three types of bolometer having sensitivities from
10-4 to 10-6 joule/cm2 and resolving times of the order of one microsecond. These
bolometers are refinements of the three-layer lo-3 joule/cm2 10-microsec bolometers'
described in detail in an accompanying paper (L.L.Gorelik, ZhTF,34,Ko.3,496,l964'-
see Abstract AP4020579). 1) A bismuth--aluminum oxide--aluminum bolometer is des-
cribed which has an equilibration time of less than 2 microsee and an electrical
time constant (RC product) of about one microsec. This bolometer differs from those
described in the accompanying paper chiefly in size (the presi.-At bolometer measures
3 x 0.7 cm2) and in the care with which the components were desiocated at various
stages olk construction. 2) A germanium--aluminum oxide--aluminum bolometer Is des'
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ACC.NR: AP4020580
cribed which has jL .;e,-.sitivity of 10-5 to 10-ra Joule/=2. The electi-ical time con-
stant is negligible, but the equilibration time is about 40 microsec. The oxide
coated aluminwa foil (oxide layer 5 microns thick) was prepared as described in the
accompanying paper. The germanium thermal sensitive element was vacuum deposited fcr
10 to 15 minutt?s at 12000C and 3 x 10-4 mm 11g. It is believed that batter and more
consistent results can be obtained by depositing under a higher vacuum. The resis-
tance of the germanium bolometer varies with the surrounding gas pressure. This does
not affect its usefulness for the contemplated plasma measurements (see accompanyirg
article cited above). 3) A bismuth--colladion--silver bolometer is described which
an electrical time constant of.about 1~
has a sensitivity of 10-5 to 10-6 joule/cn2
microsec, and an equilibration time of less than 0.1 microsec.-The bolometer-was v~
constructed on a 7 x 15 x 0.7 mm3 oxidized dural frame having a 5 x 10 mm2 opening.:
one side of which was chamfered. A co-1-Ic-iion film 0.2 to 0.3 microrsthick was de-
posited on this frame by a process that is not described. A 0.1 micron silver film
was vacuum deposited on the side of the collodion film facing the chamfered side of
the frame. This serves as the heat collector..The Bi-Pb (0.6% Pb) thermal element
was vacuum deposited on the other side of the collodion film. "In conclusion the
authors express their gratitude to I.IC.Kikoin for his interest in the work.and for
2/3
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ACC.NR. AP4020580
valuable advice, to V.Xh.Volkov for his interest and assistance in the work, to V.I.
Nikolayev for his skillful assistance in constructing the bolmoters, and to P.N.
Orlov for assistance in mastering the technique of preparing the collodion film."
Orig.art.has: 4 figures.
ASSOCIATIOX: none
SUBMITTED: 2aApr63 DATE ACQ: 32Mar64 UNCL: 00
SUB CODE: PH, SD NR REP SOV; 003 OlAM: 000
3/3
Card
GORELIK,, L.L.; HEDKOBORODYr, YU.N.j SINITSYN, V.V.
Effoct of a magnetic field an the heat conductivity of gaBes
with nonspherical molecules. Zhur. eksp. i toor. fis. 49
no.2:161-765 P 165. (Min 181 U)
I
ACCESSION NR: AP4012573 S/0056/64/046/001/0401/0402
'AUTHORS: Gorelik, L. L.; Sinitsy*n, V. V.
TITLE: Influence of a magnetic field on the thermal conductivity
of gases with nonspherical molecules
SOURCE: Zhurnal eksper. i teoret. fiz., v. 46,.no. 1, 1964, 401-402:
TOZIC TAGS: nitrogen molecule, paramagnetic gas, diatomic gas, non-
spherical molecule, thermal conductivity, effect of magnetic field,,
effective magnetic moment, nuclear magnetic moment, Senftleben ef-
fect, rotational magnetic moment, viscosity
ABSTRACT: Preliminary results of an investigation of the influence
of a magnetic field on the thermal conductivity,of N2 are reported.
The apparatus used is similar to-the oxygen gas analyzer with mag-
netic field described by L. L. Gorelik (ZhTF v. 33, no. 12, 1963).
Cord
ACCESSION NR: AP4012573
The change of the thermal conductivity could be judged from the
bridge unbalance upon application of the magnetic field. The mea-
surements were in fields.up to 340 Oe at a pressure of 3.5 x 10-2 mm
Hg.' The plot of the relative change (AXA) of the thermal conduc-
tivity against H/p (H -- magnetic field, p -- pressure) shows simi-
larity to both the plot of viscosity vs. H/p (J. J. Beenakker et al,
Phys. Lett. v. 2, 5, 1962'j and to the corresponding plot for oxygen
(E. Rieger, Ann. d. Phys. v. 31, 453, 1938), but there is a slight
discrepancy between the effective magnetic moment of the nitrogen
molecule and that calculated on the basis of the experiment. This
suggests that the effect observed in nitrogen is due to rotational
as well as to-nucle'ar magnetic moments. More accurate measurements
on nitrogen and other gases are planned. "The authors are grateful
to I. X. Kikoin,'Yu. H. Xacian. A. A. Sazy*kin, and L. A. Maksimov
for valuable discussions and advice, to V. Xh- Volkov for interest
and help, and to V. 1. Nikolayev for constant help in making the in-
strumentr and measurements. The authors are also grateful to L. D.
Card 2/4
ACCESSION NR: AP4012573
Pugikov (de ceased) for valuable discussions and advice." Orig. art. has:
2 figums.
ASSOCIATIONt None
SUBMITTED: 07Sep63 DATE: ACQ: 2GFeb64 ENCIt 01
SUB CODE: PH NO REP SOV: 002 OTHER: 006
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