SCIENTIFIC ABSTRACT KOYTYPIN, S.N. - KOLUSHKI, V.

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CIA-RDP86-00513R000824010017-8
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December 31, 1967
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SCIENTIFIC ABSTRACT
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KOLTYPIIIJ, S. IT. KWain., S. N. "BlectorMpechano-callbthenics for treatment of trawna of nerve trunks7? limbsp" "rudy Leningr. obl, gospitalya dlya lechenicy invalidov Otechestv. voyny,, LeniWadp 1948, p. 193-202 SO: U-3850o 16 June 53 (letopis t7,km)al Imm -5tatey, No- 5, 1949) GTR5PL Vol. 5-N0- Jan. 1952 (All-UnInn 3clentilic Research Institiste nf Gralogicat ProAprcting fnr oil). M 1~1'sc-very of Senaman (asqils in the western part of the -o,ifhcrn Vznba, 971-3 AkedemlYs Nsuko S.S.S alt DQkIsdy No tj I / . ~ Z-.-n - - KOLZ - . - - 16 d, . - An instance of malinformation in the growth of belemnites. Zzhagode Vsee.paleont.ob-va l4t2O7-212 153, (KM 8:3) (Belemnites) VTALOVA, R.I., redaktor; DROBYSHICV, D.V., redaktor; KOIMYPIN, S.N., redBktor; F;-'M MOISEYMO, V.S.. redaktor.- SAZOMOV, N.T., redek, r.- 610MVA. Te.l.. redaktor; WHCHURMINSMA, A.B., vedushchty redaktor; GNBRADIYEVA. I.M.. tekhnicheskiy redaktor [Proceedings of the All-Uaton Conference on the Development of a Uniform System of Stratigraphy of Kesozoic Deposits of the Russian Platform] Trudy YeascAuznogo soveshchanita po rasrabotlm unifitsirovan- noy ukhemy stratigrafii mezozoyakikhotlozhenty Rueskoy platforsq. Leningrad. Gos. nauchno-takhn. izd-vo neftianoi i gorno-toplivnoi lit-ry, Leningradekoe otd-nie. 1956. 383 Pe (KIRA 9:12) 1. Vaesoyuxnoye soveshchaniye po razrabotke unifitsirovannoy sch6my stratigrafti mesezoinkikh otlozhenti Rusekoy platformy, 1954. (Russian Platform-Geologyl Stratigraphic) - ___M KOLTTFIN S.N. ~ lower Cretaceous sediments in the southern part of the Emba oil region. Avtoref. nauch. trud. VITIGRI no.17:219-222 '56. (min 11:6) (Kazakhstan--Petroleum geology) AlIT0140, K.V.; AYZEIISHTADT, G.Ye.; GRACM, R.I.; DMMGALIYEV, T.N.; KOICYPIN S.R. "Oil-bearing strata of the DO& region mmd the,origin of oil pool#.* N,K.Chukeov. Reviewed by K.V-Axtexev and ethers. Neft.khez.34 a9.8:65' M 95 6. (Km 9:10) (Emba region--Petrolmm ge*loa) (Chukeev, N.M.) 'low" G.T*.-4,. red.; MKIKOVp SeTov I.N.0 tekhn.~ re4 [Upper Cretaceous aediments In the.Ural-lbba salt dong area auk . the southeastern UriT-wA'Xbgodxhar .reiLo"I verihnsmolovyS otlo- zhSnII& Vriaq-Ngftia~*'l AolI=oktwollnol'dblaitl W ~9 iugo-waftogo, Priwallia., ip*'*dzh V1 gr~A, 0~9. nonahn. tekh. Ind-va neft, I gorne-topU=7 lilie'4195274, 217 j; (lesivgrad. rassoXwo. wl neftlanol nauibiip-lealli tells~ll geologo-romedo0wvt In- stitut, Trudyq no.,i0q), NIM 13.16) lurol Amtmiz.k r*cIon--%ol*&) AYZENSHTADP, G.Ye.-A.; DNNMV, V.S.; KOINYPIN, S.H.; SOMDLOVA. Te.I. Oil and gas potentials of -the-s-o-'u--thern Zmba region and adjacent southern territories. Geol.nefti 2 no.9:19-25 S 158. (KIRA 11:10) Im l.VeasoMnyy neftyanoy nauchno-iseledovatellskiy geologo-ras"dochny7 inatitut. (Kazakhstan--Gas. lZatural-Geology) flottan of 6 ,-Won ," IMS1 WWI. DIP- 63 (gsw 9 60 '9". 7. 1 doolostle 64"t 04". ""1, 016" -ov a Ives roamIaLl 1 a4ttv4 .derat" to tegolt4 in UW JUGOAR VttrAod by 172 me ,.OACO 0 W. %% was c"t""Aas a pass" Y444 4 . t isaticas. goes,02 t* 13Ab- Wd OV94A .W, IA 640 bdivOl"S "t *tugo . Now- 4 32 1 tA so ' . r. .0 ito "t" '."t46 to P" "SUO, O"d 9 f."- 9""Ol saolw~ 'wflatoaml - ' a" vw CLataes ai 9-1 TrIggsto ago ".%lom ot the tm svgw of the I as K.V. "In . samood" It K Oos . 'b. 0.1a. Oad 1/2 .' I= of ,,too 0.". It. ow" " Is - croue .x I%" Oster,- C~Mf,,,Ws f= I.M. to the astmo cot AYZXMHTAM, G*Ye.-Aea, XDMITPIV, S.K.; TRIMHOV, VA. qTbctonic structure and historical development of the Caspian Lowland and adjacent reglons 1n,connection with gas and oil potentials* br M.P.Katakov and others. Revi.owed by GA-A. Alzenehtadt, SoNaKultypin, and H.K.Trifonov. Izv. Air 35SR. Ser. geol. 25 no.4-.109-112 Ap 16o, (NMA 13: 11) (Caspian lowland-Geolog5r, Structural) (Kazakov, M.P.) KOLTYPIN S*N. Lower Cretac.e.cus dedimats of the Caspian Lowland,, Trudy YNIGNI no.29~,40-68 vol.3 Ia, (MIRA 149" ( S~ian LoViand-Ge-ology# Stratigraphic) KOLTYPIN, S.N. Stratigraphic scale of the upper Cretaceous of the Russian Platform. Trudy VNIGNI no.29:67-7,1 (MIRA 14:9) 0' vol-3 161. (Russian Platform-Geology, Stratigraphic) KOIRYPIN, S.N.; SAFONOVA, V.S. Pyroclastic rocks in the Cretaceous sediments of the Caspian Lowland. Dokl. AN SSSR 161 no.6.-1416-1418 AP 165. (147RA 18s 5) 1. Vsesoyuznyy neftyanoy nauchno-issledovatellskiy Institut. Submitted December 2, 1964. AN ZZ -M mV RFSONANCE ENEN)Y 13T 71 gait Is kad V.M-Uor,z,.- 13 o 25 -Quili.r ~Aiel 1 I U-on 11A VOLKOT, Vovs; TORMINOW, P.Te.; KOLTYPIN, Te.A-.; SIDOWV, V.I.; YARIKOV, G.B. Study of the V--D rmwtion In the 0.20 to 1.75 Vay deuteron saar&7 rm%e. Atom energ. suppl, U0.5.&U-25 '57. (MIRA llg2) (Awlear reactionsl KOTL IN YE. A. slut u licit A I AN I, .11jilaiji; ill f a A a pA. lei Au - =I JjjA g ,3 gal gill 011, a a A a IV: 1; AUTHOR: Koltypin, Ye.A. Con'7E'77 TITLE: ~strucli'ion olf"7-Solid For an Electrostati-z 87177 S/l2o/6o/ooo/oo4/0l7/028 E032/E4i4 Deuterium and Tritium Targets Generator PERIODICAL: Pribory i tekhnika eksperimenta, 1960, No.4, pp.130-131 TEXT: Thin layers of titanium or zirconium deposited on a metallic base and saturated with deute-rium or tritium are widely used as targets In neutron-producing electrostatic generator-q. In ordbr to obtain large neutron flxxxes, the targets must withstand considerable ion currents. Thus, for example, the power dissipated in a target by a charged particle beam of 1-2 MeV at a beam current of 10 to 20 ILA is a few tens of watTs, Under su.-h conditions these targets must of ~course be cooled. Moreover, in order to reduce neutron scattering the construction should be as light as possible. The design described in the present paper is. illustrated in Fig.l. The molybdenum base I of ihe target, which is 0.3 mm thick and 14 mm In diamoter, forms the lid of the vacuum systems The system is sealed by a rubber gasket 2 and a light aluminum cover 3 - The target was cooled by directing a stream of water droplets 4 on to the outer face I of tha target.. Card 1/3 S/120/60/000/004/017/028 E032/E414 Construction of Solid Deuterium and Tritium Targets For an Electrostatic, Generator In this way, the amount of matter In the neighbourhood of the: target is practically unaltered. The focused beam 5 of accelerated ions was spread-out by a rotating magnetic field so that it covered most of the area of the targei. The author has used tritium targets with a Ti layer 0.5 ;m2 thick with a protonv mg/- beam of Lto 2.5 Mev. Experiments were :-,arriod out with beam A currents of 30 to 50 TLA. The power dissipated In the target reached up to 100 W. After (2-3) x W uA hr, the loss of tritium from the target did not exceed 20%. There are I figure and 2 Soviet references. SUBMITTED: May 30, 1959 Card 2/3 3360 S/058,`6 1/000/0 12/016/0 63 A056/AIOI 7, 0 AUTHORS% Koltypin, Ye.A., Yankov, G.B. TITIE: Elastic scattering of 400-Kav neutrons by Zn, Se, Zr,, Ub, Mo, Cd, In and Sn PERIODICALt Referativnyy zhur-nal. Fizika,, no.,12, 1961, 105, abstract 12B524 (Tr. Tashkentsk. konferentaii po mirn. ispollzovaniyu atomn. ener- gii, 1959, v. 1, Tashkent, AN Uz=, 1961, 61 - 64) z The differential cro.ss sections of ela3tic scattering of neu,~rons (from the T(p,n)He3 reaction) by Zn, Se, Zr, Nb, Mo, Cd. In and Sn were measured. Comparison- of the angular distributions shows that with increasing atomic weight of the target, the anisotropy of angular distribution at first grows weakly, but beginning with Zn it rises sharply: S (00)/Smin equals 3.3 for Zr (A~90), but 4.2 for Mo (A-96). This variatioir of angular distribution is consistent with the predictions of the optical model of the nucleus. [Abstracter's note: Complete translation) Card 1/1 33083 S/630'41/001/000/005/056 B1027B-136 AUTHORS: Koltypin, Ye. A., Yanikov, G. B. TITLE: Elastic scattering of 400-kev neutrons from Znp Se~ Zrq Nbq Mo, Cd, In, and Sn SOURCE: Tashkentskaya konferentsiya po mirnomy ispol'zovaniyu atomnoy energiia Tashkent, 1959. Trudy. v. 1. Tashkent, 19619 61-64 TEXT: The authors study the anisotropy in the angular distribution of elastically scattered neutrons. T(p,n)He3 reactions with Ep.~ 1300 kev and proton currents of up to 50 ga provided the neutrons. The target consisted of a titanium layer with tritium on a molybdenum base and was designed to operate for a long period without a decrease in the neutron yield. The neutrons scattered were recorded by a proportional counter via the recoil protons. The counter was paraffin screened from the primary neutron beam Cylindrical samples were used (6 em long and 0.9-2-3 cm in diamet;r) (equal to about 0.5 mean free paths of scattered neutrons). The differential elastic scattering cross section was Card 1/3 33083 s/63 61/001/000/005/056 Elastic scattering of 400-kev ... B102YB138 calculated from the relation d0) - (N-N, 2/N.R2 is the number .)-d A-F; N-Nb of counts at the angle 4, without background, No is the number of counts at 00 (without specimen)&Lt a distance R from the target; d is the distance between specimen and counter, A is the total number of nuclei in the specimenj,F is a geometry factor. The background counts ranged from 20% with sma q$ arid 65% with 1~ - 1500. The anglalar distribution was determined from 10 measurements between 20 and 1500- With,~