SCIENTIFIC ABSTRACT LEBEDEV, T.A. - LEBEDEV, V.A.

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December 31, 1967
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SCIENTIFIC ABSTRACT
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ACC NR: AT6008673 formulae Nom = const, at I collst, NIP=const, at. a=const. Log c versus log Np and log t versus log N curves were obtained for all three specimens over a temperature range of 300--800C. The results show that the strength of these heat-roBistant materials under cyclic loading dep6ds first on the nature and intensity of structural changes in the metal during the test and, second, on the duration of the therml. stresses. The largest effect of the variable temperature parameters on the fatigue strength of the metals w4a observed in the temperature regime where noticeable structural processes were absent. Orig. art. hast 4 tablesq 2 formulasand I figure. SUB CODE: 11, 13/ SUBM DATE: 19AU965 2/2 ACC NRtAT7005723 soURcE--coDE:- AUTH?R: Lebede,,@@ Korneyev,, N. I.; 14arients,, T, K,; Kalugin,, V.F., Kr u. N, up n, ORO: none PITLE: Technology of production and properties of high-strength steel 3trip SOURCE: Leningrad. Politelchnicheskiy institut. Trudy. no. 267, 1966p lvtomatizatsiy i tekhnol.ogiya.mashinostroyeniya (Automation and tech- aology in the machinery industry), 15-21 roPIC TAGS: stainles3 steel, high strength steelj steel-atrip, 64pi-@ g PI volling, s*AV mechanical property, roII44g--#eeJmaI-* y/2KI.15N5 43 steel USTRAMA technology for industrial production of Iligh-SLrength steel strip has beenI, developed. The technology utilizes the strain hardening of austenitic- martensitic type steels in Lhermomechanical treatment done with Lhe use of rolling stands with multiple rollers of relatively small diameter and large supporting rollers. Iligh-strength SLrip, 0.165 min thick, was produced by rolling with an 80Z reductio'n Uhl%5AM stainless steel containing (%): 0.24 C, 0.80 Si, 0.80 Fln, 14.50 Cr, 4.0 Ni, 2.8 M and 0.06 N2. A partial transformation of austenite into martensite occurred in steel during Card 1 UDC: none k@C NR,AT7005723 rolling, while a reverse transformation occurred wf6 tempering, probably because of nitrogen diffusion in the a-phase. A relatively'low (1.85.104 kg/mm2) modulus of the normal elasticity can be nyplained by a high degree of strain hardening. A teusile strength of about 272, 280 and 290 kg/mm2 was obtained with 'aging at -200, +100 and 395'C, respectively, at an almost constant elongation of 0.75% in the -200--+300*C range. Nontempered and tempered (regardless of the conditions) speriTrens had a .0.98-0.99 ratio of (0.2) yield strength to tensile strength. Transverse specimens had a slightly higher tensile strength than the longitudinal. .The metal also had a low stress sensitivity factor of 1.07 and 1.17 for .longitudinal and transverse sper.1mens, reqpm-tively. The best strength characteristics were obtained with aging at 395%. Subzero treatment to bring about the y-a phase transformation was unsuccessful, probably because of the stabilization of austenite. The ductility (the elongation-to- hardness ratio) was constant for all aging condttions up to 450*C. The fatigue strength, determined on the basis of 106 cycles, was 90 kglmm2. Orig. art. has: 6 figures.. [HSI SUB CODE! 11:13/ SUBM DATE: none/ ATD PRESS.- 5117 Card2/2 ACC NR- AT7005725 SOUdCE CODE: UR/256@/6@/060/26@/0026/00@, AU11HORS: Gorbakon', A. A.; Lebedev, T. A.; Marinets, T. K. ORG: none TITLE: Possible ways for increasing the fatigue strength of heat-resistant alloys SOURCE: Leningrad. Politekhnicheskiy institut. Trudy. no. 267, 1966. Avtomatizatsiya i tekhnologiya mashinostroyeniya (Automation and technology in the machinery industry), 26-31 TOPIC TAGS: heat resistant alloy, metal property, high temperature fatigue, fatigue It' strength/ EI867 heat resistant alloy, E1437B heat resistant alloy ABSTRACT: The effects of thermomechanical treatments on the fatigue strength of heat:1 resistant alloys EI867 and E1437B were investigated. The initial heat treatment consisted of quenching from 12200, air cooling, aging for 8 hours at 950C, air cooling@ (for EI8067) and quenching from 1080C, air cooling, and aging at 700C for 16 hours i followed by air cooling (for E1437B). Fatigue curves for BIS67 alloy after 6 differ- ent types of thermomechanical treatment are presented and compared with the untreated behavior. Fatigue curves for alloy E1437B are presented for the untreated metal and for one type of thermomechanical treatment. After a discussion of the structural i effects of the treatments (sample micrographs are presented), it is concluded that thermomechanical treatment increases the fatigue strength of dispersion hardening Card 1 ACC NR: AT7005725 -alloys only when the plastic deformation temperature during the hot working is belo-zi the aging temperature of the alloy. Repeated thermomechanical treatment is even more effective (below the aging temperature). Orig. art. has: 7 figures, 1 table, and 1 formula. SUB CODE: 13/ SUBM DATE: none/ ORIG REP: 009 Card k3 is. i P -p Tea Ad ii r 'Val 4 Jig 4U.;(11.1 U gig ail J.: iv*t I- "Ili ' ' -' On the nature of the Cbarnygov magnetic anomaly. Dop. A@ URSR no.5:475-478;'56. (MLRA 10:2) 1. Inatitut geologicbnikh nauk Akademii nauk URSR. Predstavlano akademikom Akadamii nauk USSR V.Gt Bondarchukom. @4 (Ukraine--Magnetism, Terrestrial) LEBEDW. T,S.; KRAVETSI, V.V. ... P.To Pasallalkyi, outstanding scientist and geophysicist of the latter part of the 19th century. Geol.zhur. 16 no-2:78-79 '56. (MLRA 9:9) (Pawalletkyl, Pavel Tymofiio*ycb, 1871-1956) ISBEDIV T iS_ wwok. c ;t of the Dnieper- n the "TectOni G.M. Riabukhiuls art'cle 0 1 @i no.1:78-7 r:c Donets.Dopressiour'- Gool.nafti I Stijictural) (ftiOer Jovland.--GbOILI*Y, tural) (Donets B68ju_-GeologY. Stl L V BONMRENKO, B.V. (Minsk); LIBEIZV, T.S. (Kiyev) P.T. Pasallskii and his contribution to geophysics. Vop.let.est, i tekh. no.5:182-187 157. (MIRA 11:2) (Pasallskii, Pavel Timofeevich, 1871-1900) LIBED Density characteristics of the geological cross section of the Pripet Depression. PrIkI. geofiz. no.16.-200-209 '57. (HLRA 10:8) (Pripet Marshes--Geology. Stratigraphic) All-Ukrainian conference on preparations for the International Geophysical Year. Goo'. zhur. 17 no.2:93-94 '57. (MLRA 10:11) (International Geophysical Year, 195?-1958) IRBIKDBV . T.S. Gonference of Ukrqiniqn participants In the InternAtIonal Geophysical Tear. Visnyk AN URSR 28 no-5:65-66 MY 157. (MLRA 10:7) (Ukraine-International GeODhysical Year, 1957-1958) LEB-Off, T. S. .I- - - , . Geological interpretation of gravitational anomalies in the Pripet fault. Sov. geol. no.61:101-111 157. (MIRA 11:4). 1. Institut goologicheakAkh nauk USSR. (Pripet Talley-Gravity) - ------ 6-5656 sSM 39- -1' 959, jIr 6, t 4 ,,f ot, mom r t4 J.S S) @cx se r all -.,4 @jssyL. - .. ,f g;e,r - pr @of-.rp a I.Ort 0 -fie e p VI 5'i@' -_ TrI - 31 qer o5t_ cl a P @W, _@Y.g -"- --vat- oi, Boed or-, A ?rWY ell, _rj &I)il al f O-rm - ttle 00106 0- 0 ot -jars-, .je5 vs V - -1:,, - IDO@a, , &j.1 '.."k V.Iq r j J'a, 5 Irv), G'V ?L CIIS - v as all AIf se er. to 5 0,- ve., Clot 5@er.ce - ;, @ psi. PrT4 v 1/3 WI/I69-59-6-56,56 The Gravitationa.1 and Magnetic Ar-cmalle-S of the Pripyat' Depr-=s_=ion and Tha�z- Cor-r-6ction-With the Geological Structure 3 arbonate -sulfate strata of the upper Davonian fozrmatlor@ nc - + 0A g1cm a The first two are. --ore clear and and Permian deposits (A6 - + 0.2 g/om3). cons i's-t:%.nt in respect to their area (M.Geof iz, 1958, 1411 . Tqle fa.:@tovs causing the, anoma-ly of the gravitation field have been determinsd., a) chanxr-5 Ir. the'surface relief of the Pre-Cambrian, b) the norru-nifor-mity of the mate--i&I composition (and also the density) of the Pra-CambrJ_an rock.5; 0.) S4 vun;arai- moxThological peculiarities and changes in the lithology of Paleozoic depcsits. m.."le factors influencing the magnetic field a:ra, a) nonuniformity of +-)-.a material corvpo@_itioxi of' the Pre-Cambrian formation@ b) the sprpd of granitoid rooks, in Y the lower parts of the depression ( X ava- P@,, 300 - 10 -- C,'--;SM); c) the Dresencl- of *,;abbro-type rocks in the outcrot*)3 Of ih; foundation. (-k - 5,500clo-6 I yer d) the intrusion of effusives into the sedimentary itratum, o--igin-at--Ing from deep-seated fractures ( Xaver ~ 6000,,10-6 CGSM). The sedimentary deposit-13 detected in the depression'are pra,-tically non-magnstic. There are ,wo cle&r-17. defined zones of faults limiting the depression Jr the ror-th xnd saith. The tectonic border with the Dnapr-Donets &@Pres:3ion has been traced, The nature of the Chernigov anomaly has been clvxa@3terized (RZhGieof@z, 1957, Ca--,d 2/3 3(W/16q -59 -6 -56-16 The Gravitational and Magnetic Anomalies of the PrIpyal'-I Depressior. and Tnelr- Connection With the Geological Struoture 9918), '11-be difference in +.he struature of t1he gravitational and magnzti,@ anoMal4e:E of the Pripyat' and the Dnepr.-Donatz depr-a3iors a-re @onn--@@ted W-Itn the differences in the geological stvuct*dr8 of tb@, afor@!Mantiored rigions@ this way, the Pripyat' depression may be conslde-zsd as an ind@@Dendent zeo- str,ioturai element ir. the body of the Russian platform. 'Mrie tQ@atc@nicz of' tta se-@,6nd-ord,sr structlixes are diecussed in de4-ail, The IrIpjat' depreszIon 15 a grabe-m-like IYeeiTing of a series of large bloc@kF of th8 Prs-O%mbr@ar, bass to a eor-:@Iderablle dgp+-)i (up to 4.5 - 5@O Lan) @ *T-%--'s base criglna4@ed ir- tt6 M@Iddle- Devonian period or In the lower Paleozoic era, Bib!, 1.9 titles., (Ir-t nau7k AN USSR - in-sti-bate of Geological Sclsrv@-7)@: of thri AS,, UkrS3R) @-S, Lsbsd@@7 Card 313 Studying t@e density of Phleozoia deposits In the Aripet depression. TTudy lust. geol. nauk AIT URM Ser. geofis. no.2:138-151 '58. (MML 11W I's Institut geologicheskikh nauk AN USM (Pripet Valley-Geology, Stratigraphic) LIMM7, T.S. --, ,r,vr- In memory of Otto lUllevich Shmidt. Trudy Inst, geol. nauk AN URSR. Ser. geofiz. no.2:20(@-203 '58. 1 . (MIRA 11:6) (Shmidt, Otto IUllevich, 1891-1956) B1 D17 v 26-58-5-18/57 AUTHOR: 4aae-p-nMe @s' Candidate of Geological and Mineralogical TITLE: On the Causes of'the Chernigov Force@of-gravitation Anomaly,(O prichinakh.Chernigovskoy anomalii sily tyazhesti) PERIODICAL: Priroda, 1958, Nr 5, PP 79-81 (USSR) ABSTRACT: The hypotheses offered by V.S. Zavistovskiy, S.I. Subbotin, V.A. Sellskiy, and I.A. Balabushevich, in order to explain the Chernigov gravitation anomaly, did not explain the phenomsnon satisfactorily and were too much concerned with causes that had occurred at great depths within the earth. Recent drilling and rock sample analysises from depths between 1,587 and 2,751 m revealed that ground magma in pre-Cambrian periods had been thrown up through cracks and fissures, whereby effusive rock was intermingled with sedi- mentary rock. This process had also continued through the Upper Cambrian period and this brought about-the summariz- ing effect of a gravitation anomaly. Card 1/2 There is one schematic map and 5 Soviet references. On the Causea of the Chernigov Force-of-gravitation.Anon4ly 26-58-5-18/57 ASSOCIATION: In3titut geologicheskikh nauk Akademii nauk Ukrainskoy SSF, Kiyev (Institute of Geological Sciences of the Ukrainian SSR Academy of Sciences@, Kiyev) AVAILABLE: Library of Congress Card 2/2 1. Gravity - Measurement 2. Gravitation anomaly - Analysis 3. Chernigov force-of-gravitation anomaly 4T / _. /-@@ - /-.- / , SOV-21-58-8-16/27 AUTF'RS: Bondarchuk, V.G., f4ember of the AS UkrSSR, Xondrachjk, V.Yu., Krutikhovskaya, Z,A., Lebedev T S jllikhaylova, IN.P., and Sollogub, V.B. TITLE: Hypsometric Chart of the Surface of the Precambrian Foundation of the UkrSSR and Some Adjacent Areas (Skhema gipsometrii poverkhnosti dokembriyskogo fundsmenta USSR i nekotorykh sopredellnykh territoriy) PERIODICAL: Dopovidi Akademii nauk Ukrainslkoi RSR, 1958, Nr 8, pp 863-866 (USSR) ABSTRACT: The old charts of the Precambrian foundation within the Ukraine compiled by A.D. Arkhangel'skiy (Ref. 1) and other investigators, of which the most detailed is the chart by E.E. Fotiadi (Ref. 15) are mostly obsolete and do not correspond to the present level of the geologico-geophysical knowledge of the Ukraine terri- tory. Making use of charts compiled by F.A. Rudenko, G.M. Kozlovskaya, V.T. Syabryay, K.M. Varava, R.I. Andreyeva for individual regions and based on the results of electroeurveys by V.I. Klushin, gravimetric investigations by S.I. Subotin and prospecting drilling, in 1957 the authors compiled a hypso- Card 112 metric chart of the surface of the Precambrian crystalline SOV-21-58-8-16/27 Hypsometric Chart of the Surface of the Precambrian Foundation o-l' the UkrSSR and Some Adjacent Areas foundation of the Ukrainian SSR and certain adjacent areas on a scale of 1 : 750,000. The contemporary surface of the Pre- cambrian foundation has a peculisrly disjointed relief which in its fundamental features accords with the features of the tectonic structure of the areas considered. There is 1 geological chart and 16 Soviet referen6es. ASSOCIATION: Institut geologicheskikh nauk AN UkrSSR (Institute of Geo- logical Sciences of the AS UkrSSR) SUBMITTED: March 16, 1958 NOTE: Russian title and Russian names of individuals and institutions appearing in this article have been used in the transliteration. 1. Geology--USSR 2. Geophysics--USSR, Card 2/2 BERUDSWA, It.G. C-Bernedellm, LAQ; LFIBIM, T.S. [Lebediev, T.S.] Rocks of the crystalline foandation of the NarovIya area (Pripet Depression). Geol.zhur. 18 no.5:47-54 '58. (MM 12:1) metamorphic) (bkrovlya region-Rocks, Crystalline and IXBHDEV, T.S. [Iobediev, T.S.], kand.geol.nauk; PANCHEITKO, D.Yu. [Panchenko, D.IU.], kand.geol.nauk Some results of work of the scientific geological "Wednesdays." Visnyk All URSR 29 no.2:62-66 F 158. (MIRA 11:4) (Uk-raine--Geological research) LEBEDEV9-T.S. [Lebediev, T.S.], kand. geol.-mineral. nauk. Second all-Ukrainlan conference of the participants of the International Geophysical Year. Visnyk All UM 29 noo'3:56-62 Mr '58. (MIRA 110) (International Geophysical Year, 1957-1958) M V, T.S. [Lebedievy T.S.],kandogeol.-min.nauk Research by Ukrainian scientists on aspects of the program of the International Geophysical Tear. Vienyk AN URSR 29 no.12: 36-45 D '58. (MIR& 12:1) (Ukraine--International Geophysical Tear, 1957-1958) ill, kana. geol.-mineral. nauk. Gauses of the Chermigov gravity anomaly. Priroda 47 no-5:79-81 Yq 158, (MIU 1115) 1. Institut geologicheakikh nauk AS USSR, Kiev, (Chernigov Province-Gravity) BONDARCHTJK, V.G.; SOLLOGUB, Y.B.; ICOIIDRAC=, V.Tu.; ICMIKHOVSKAYA, Z.A.; IKBIMV, T.S.; MIKffAYLOVA, H.P. Surface relief of the pre-Cambrian crystalline foundation in the Ukrainian and Koldavian S.S.R. Sov.geol. 2 no.1:41-55 Ja '59. .(MIRA 12:4) 1. Institut geoloecheBkikh nauk AN USSR. (Ukraine--Geology, Structural) (Moldavia--Geolog3r, Structural) l,k;RWI%V, T.S. [Labediev, T.S.J, kcand. peol.-min. nauk; ]@@.VETS, V.V. CXravotsl , 'V.V.1, kand. geol.-min. nauk Geophynical research in Hungary. Visn.7k. AIT URSII @O no.8:60--@6 Ag ,59. MIRA 13: 1) (Hungary-Goophysica) LEBEDEV, T.S.; SOLLOGUB, V.B. Contribution of Ukrainian scientists t6 research completed under the ogram of International Geophysical Year. Mezhdunar. geofiz. god rKiev] no.2:3-31 160. (MIRI 14; 1) 1. Institute of Geological Science of the Academy of Science of the Ukrainian S.S.R. (Ukraine-Geophysical research) AUTHORS., TITLE% A 23 2/A 029 Lebedyev, T.S.j Krnjtykh,:,vs'ka, Z.O. On the Future Ways of tt,.P. D-vei-)pmen@ c)f !_'-,'_NphyEic @ in the Soviet Union [A Report Based on the Mi _.C--ia-LT-0T-7t7 vs,@-Es-yuzna heofizychna konferentslya (All-Union Gecphysical Conference)! PERITODICAL9. Dopovidi Akademiyl nalak Ukrayin@,'koyl F[SR, 1960, Nc,@ -," rZ_.387 - 391 TM- The Vsesoyuzna heofizychna konfer-antsiya (A '.1-Union neopfty3ical Cx@- ference) was held in Leningrad In 1959, it was dedicated ',: a w1de range of problems of prospecting geophysics: n,:-w trends In the metliodz_ of prospecting various minerals, like non-ferrous and rare wRtals, deve",.-.pment. of modern geo- physical equipment, rational m-it-hods of Int@_-@@z-_tlng the roasuits @f geophysl@-al investigations, new data on the geologica" structure of var-tous regions, et'@. All problems were discussed on plenary s@@ssions and in f:ur ss,7,;ti7ns (S"rUctural, geophysics, mining geophysics, gecphysi,:al equipment, and dev!,_@e design, and in- dustrial geophysics). The conference was opened by ProfeSsor V.V. Fedyn5@kyy, Head of the Viddil heofizyky. Min-laterstva hecloh-yi t.;. rolhorcny nadr 5MR7 'T7--- partment of Geophysics of the Ministry of Geca._@Ey and Minera:. Dep@@_zit P_rotc-+Ic-n Card 1/8 A232/029 On the Futuxe Waye of the Deevelopment of UnIon [A Report Baeed on the Mat.= *ria-.E: cP Iya (All-,Union Geophysical Conference)] Pr.@)spe::tIng Ge-physi-Is In the Soviet the VEie_z-_.yiizna heofizychna konferents., Of thr-, TIWR). In his report V.V. Fedynstkyy e1ucida7;,=d thc- prc6pects of -t-he de- velopment of geophysical prospecting methodi, as well as td-;e developmew. of tri= prospecting of minerai. depcsits fcr the perl:;d 1959 - 1965. !he plenar-y heard the following reports: A.!. Zaboravz;kyy, Fr,:@fes.@:Cr sf the Moscow Univer sit on "The Present@ State and the Ways of ,he Developmen*@ --f EngineerIng f2ec- physics", M.I. Sofroncv of the Vsesoyuznrr Lnst.ytut me+--_@dyky I tekhnikv heofiz., (All-Union instii@ut.e of the Meth.)ds and Techn ue of Ge - ye'r.noyl rozvidk-y - 1@ITR '_ iq ophyelcal Prospecting -- VITR) on "New Ways of the Llevelopment of Sear' -h-and-Fro- specting Geophysics"; 1@.O. A-.dr-ftX!,-,v of the Lc-ninhrad--5kyy hirny,:;hy-y Inc-tytut (Leningrad inEtItUte of WP'ng) an 'Certain Problems and Visl-.as of the D-velop- ment of Structural Geopryej7:_:Y@ , Professor of fhe L@-ningrad instl- tute of Mining on "The '*,., albilities of Insreaiiing the Efficiens-y of the @erc- -name-tCe'Method During i Mapping and SearChing for Mineral Deposits", 0 Z. Tuniff=v pf the .vod "Geologorazver1ka", Leningrad (Plant "Geologorazwdkd', Leningrad) "On the Tendency of the DeQip,:.-, and Productton of 11':@_6_-pFy_z.,,-rS_! Equip- men+", and others,. Apart frnm th_lz, -07e conclusive pl.ena@ry zessisn6 -of the Card 2/8 -n S/021/60/000/003/008/010 A232/AO29 On the Future Ways of the Development ion [A Report Based on the Materials (All-Uftion Geophysical Conference)] of Prospecting Geophysics In the SovieL Un- of the Vsesoyuzna heofizychna konferent--lya ference heard the report by H.I. Pptrashen' of the Leningrad Universit "On the Vistas of Applying the Dynamic Theory of Selsmic"Wave Propagation In the Seismo- graphic Geophysical Exploration"; Yu.A. IDikhof of the Kazan' University on "Tibe Tectonic Phenomena and Their Causes and ON. Mukhin of the Trest "UkrhvefIz- rozv:Ldka" (Trus t "Ukrheofizrozvidkalf) on The State and Development of the Geo- physical Service in the Ukraine". In his report on the new trends in the search- -and-prospecting geophysics, M.I. $ofronov presented interesting data on the de- sign of modern geophysical equipment in anumber of scientific research insti- IV/ tutes: the All-Union Institute of Methods and Technique of Geophysical Prospect- the Instytut fizyky zemli AN SRSR (Institute of the Physics of the Earth, AS USSR), and the Instytut avtomatyky AN URSR (Institute of Automation, AS Ukr- SSR). The report by Prdfessor B.O. Andryevey dealt with certain Important prob- lems and vistas of the development of structural geophysics (the study of the abysmal structure of*the earthts crust, the search for oil- and gas-bearing structures, etc). I.H. Klushin of the Leningrad Institute of Mining read a re- Port "On the Problem of Rating the Stratification Depth of a Crystalline Sub- Card 3/8 S/021/6o/ooo/oo3/oo8/o1o A232/AO29 On the Future Ways of the Development of Prospecting Geophysics in the SovietTh- -ion [A Report Based on the Materials of the Vsesoyuzna heofizy2hna konferentsiya (All-Union Geophysical Conference)] structure According to the Calculations of the Gravitational and@g@aet @-oma_ lies Under the Conditions of the Sout-h-East of the Russian Plateau". The seetton of mining geophysics heard 18 reports dedicated -1-o the development of theore'tical argumentations and to new methods and equipment for searching ore bodies under various geological conditions. Some of thesse reports are3 "The Increase in the Dept,h.of Investigations in Mining Geophysics" by A.H. Tarkhov, Professor of the Moskovdk heolohorozviduval'nyy instytut (Moscow Geological Prospecting InEti- . yy k tute); "The Methods and Equipment of Prospecting Blind Mining Structures Frcm Boreholes by Using the Method of Radioscopy" by I@a&_E2pov of the All-Unicki In- stitute of the Methods and Technique of Ge*phys4cal PrnF:penting (Leningrad); "The Experience Gathered in Applying High-Frequenc smographic Geophysical Exploration Under the Conditions of the Ukrainian urystaiiine Shield"'by iL @B.' Solohub of the Instytut heolohichny@h nauk AN URSR (Institute of Geolo", AS UkrSSR) and "On the Application of`Qtravity Prospecting at Ore Deposits" by a.H. UspensI)Wy. The reports by the workers of the All-Union Institute of Methods and Technique of Geophysical Prospecting (Leningrad), sucb as V-V, Polikarpoeb- Card 4/8 3/021/6o/or/j-/o-,j3/oo8/o i o A232/AO29 On the Future Ways of the Development of Prospecting Geophysics in the Sovie,,k;n- ion [A Report Based on the Materials of the Vsesoyuzna heofizychna konferen-@s_iya (All-Union Geophysical Conference)] kin, M.A. Lapp, M.M. Yermolayev, D.V@ Palf'yerov, A.H. Sen1ko and others were de- dicated to the methods of geochemical investigations when searching for gold ore, copper and nickel and rare metal deposits. The reports by A.H. Hramakov and V.S. Hlebovstka of the All-Union Institute of Methods and Technique of Geophysical Prospecting (Leningrad) investigated the problems which refer to the utilization of the emanation and gas survey when searching for ore deposits. B.M. Yanovsl- kyy, Professor of the Leningrad University, Z.O. Krutykhovs?ka of t-he-In-s-titu-te of Geological Sciences, AS UkrSSR, and F.M. Yefimoy of the Vsesoyuznyy naukovo- doslidnyy heolohorozviduval'nyv naftovyy instytuil- (All-Union Scientific Research Geological-Prospecting Petroleum Institute, Moscow) dedicated their rep!@rts to ti-B elucidation of the problems of%@a@is@mand paleomagrietism of rocks. The re- port of Z.O. Krutykhovslka,(Kiyev), was entitled "The Distribution of the Surplus ,Ymagnetization in Rocks of the Iron Ore Formation of the UkrSSR (On the Example of the Kremenchug Deposit) it . Vei-,tinteresting were the reports I'The Equipment and Methods of Conducting an Aerc@-'Electroprospecting' by M.M. Shuval-SerEXev v of the All-Union Institute of Methods and Technique of Geophysical Prospecting Card 5/8 S/0-21/60/000/003/008/010 A232/AO29 On the Future Ways of the Development of Prospecting Geophysics in the SovietUn- ion [A Report Based on the Materials of the Vsesoyuzna heofizycbna konferentslya (All-Union Geophysical Conference)] (Leningrad) and "The Experience Gathered in Applying High-Frequency Electro-Pro- specting cn the Deposits of Altay and Kareliya" by S.N. Shey-toman of the AII-Un- Ion Institute cf Methcds and Technique of Geophysical Prospecting (Leningrad.". A total of 14 reports was heard by the section of structural geophysics-z I'The Structure of -rhe Crystalline Envelope of the Earth as it Appears Ac- cording to Geophysical Data" by R.M. Demetelka. "Th;& Causes and the Mechanism of the Formation of Depressions of the Earth' rust" by 8.1. Subotir-,,, IrThe Ex- perience of the Regional Geophysical Work Done on the Example of Ust.'.-Urt" by Yu.M. Hrachov and others. A number of reports were dedicat-ed to the seismogmrh- ic investigations, particularly to the results of deep soundings 11 a on -he R (Yu.M. Hodin "Regional omplex Investigation Q@S A!- ek@_yeyev "On the Nature of the Bas@,c Deep Waves Recorded by the H3-Z Me-thod"') and to other new modifications of the'@elsmcgrapb.,- geophysical c-xp1_Lraticn. A 5,9- ries of reports heard by the above-mentioned secT.Ion dealt with new methods of mathematical interpretation and geological explanation of res-alts of gravinstric and magnetometric investigations. A special section di_,cus3ed. tne problem_@ C'f Caid 6/8 - ;01 S/O2j/60/0C;O/C'03/CC-0/ A232/AO'2-9 S Y C GecPvlys' .1r,eve p,,ospecting; 1z ycbna D, -Lopment 0 =oyuzn13- 've is vse- Future Ways Or the a d I no P- nd On the S,C). pid ubn Based On the e en1-1- r ion Fepr . sical Con (11 rr@pcr I tie of Gt.@!.- and e o P Mr -1 type -1jnjon G nt arid -e Q ,,pt,,y-jcaj_ equIPme j TnSt 4. . M d design'nl; 6'. of the All , ,@w III A. petro-v 8,11 RepOr u mov I d) lead cn a e ectin Pquipmen.-- "eropl-9-n' n L -Y 'Leningra .ts -,f I pro ros - r"l- le"l- @-VO- r@osc PVIYSica Ite 5- DmaTP rD, of'y,lertrO- cot -\@ I Dple t co_np ,tion in geo' opment ationits Its Iati@izl weromcl@ -ismo- q deve-1. -I ogging s n,w ot t-d on rc-N nt a- or depOs -II)Pmp t -ial e grad) repov -, a new Type - _ Ij.,e -"' f indu54- oil vecting .-I rje%, 0 heard t a-ila section (t4o .,t for PrO- were 9.1-=o -bile equiPme eqlipmen, - -ad -rebvodo,@ @-\ 4:rje rospecting VC - d and automo rti waz DM- ta :)nant mag;netoP I of 5 reP@ Ports by tr- an t.nta the rei Very r-lear-res( t A were cidat.ed the presen -n ju quipm@- * @ial S"Ophy-, 1.u+ r- aphic e I Interest ) whi ch e industi: -C ad Inst ' -- Of specia (Moscow., -Len!-116 14 at al eoplly54-Cs' 14 DaYDER-v- 1@ or methOds Of +hr-- )r V of t-le h., Rsprc- profess( for . ,one sGary an by na= d the rut:,@,,,-. nf . - 1-0 tne repo ' f. feren of Con ways .rp. a 'ion of the IQ. 0 we te e 5 In' "Trie, Determine" :)le 'Ind the plenary r'K BGVehl J_@@ & on It rfhe final f rm Field Around tile onditiOns he Thermal C duction Of Card I On the F-uture Ways Of the DevelOPment Of Prospect, on [A Report Baz 1/0 alrolo 1A11-Un4 A23;@IAO29 On Geoph on @;e @Iatertalsof the Vses 4. Ing Geophysics In t@h. Sovie, y.ical Conference)] OYuzna hc-ofjzYch11a. i yur- unan"rno"IY Passed a re ntq geophysics in the SOvIet-lutiOn aimed at the future t Union w4thin thL devej@:PmEnf coming SovlEt S-&ven- ' - -'rcsPect.1.9 Y-@ar P-,.an. Card 8/8 S/16 62/000/002/003/072 D228YD301 AUTHOR.- Le-bedev. T. S. TITLE. 4th AlIL-Ukrainian Conference of participants of the International Geophysical Year and International Gec- physical Collaboration of 1959 PERIODICALg Referativnyy zhurnal, Geofizika, no. 2, 1962, 3, ab- stract 2A5 (Mezhdunar. geofiz. god, Inform. "byUi.1, no. 1.961, 3-7) TEM- On January 25-28, 1960, in Kiyev there was a conference a', which the results of research fulfilled by Ukranian solientific cr- ganizations were presented. The work of the Poltavskaya grav-,me-- tricheskaya observatoriya AN UkrSSR (Poltava Gravimetri,--- Observa.- tory, Academy of Sciences, UkrSSR) was described in the report of its dire-3tor, Z. N. Aksentlireva. Extensive observations on the 15- t.itudinal variations of the town of Poltava were made in ac,=d- ar-Ce with the IGY-IGC program. Experimental work on the study of polar movement. from contemporary latitudinal and azimuthal cbser-- Card 1/3 3/169/62/000/002/0071/07.2 4th All-Ukrainian D228/D301 vations has been carried out. Investigations of earth tides have been considerably expanded. V. P. Tsesevich, the director cf zhe Astronomicheskaya observatoriya Odesskogo universiteta (AstroncmL_ Observatory of Odessa University), spoke on the questicn, --f melec.- fj@l research and supplied the main results of research in this I eid. A series of papers was devoted to the problem of "solar asti-::.tyll. V. A. Chegoryan and V. M. Zhebko (Kafedra radiotekhniki Khar@k,_-rs- kog,j politekhnicheBkogo instituta (Department of Radio Engineering, Kharlkov Polytechnic Institute)) reported on an investigatic'n of the horizontal movements of ionization irregularities in the lcr,.C. 3,)here. The ratee and directions of drift cf ionization r J t IL _L L `e-s were studied Jn the ionosphere's F- and E.--i.ayer-q.. N, N@ Ye- ryushev (Krymskaya astrofiz-ir-heskaya observatoriya AN SSSP (C-2-- mean Astrophysical Observatory, Academy of Sciences, USSR') hvj@ studied the change in the parameter of (Nlvl. rf @ri the 4ono@phere'!_: lower layers at the time of solar flare.9,, It was es-lab-112hed thaT: the changes in the parameter of (N/V) eff differ for differeril@ fre- quencies a-V the time of sudden disturbancea. A. S. Dvoryash-*Ln Car,,'- 2/3 S/16 62/000/002/003/072 4th All.-Ukrahian ... D228YD304 (Crimean Astrophysical Observatory, Academy of Sciences, USSR) --n,.- vestigated the relation of short-period variations of the geomag- netic field to solar and ionosperic corpuscular radiation. M. V. Stovas' paper, which broached the subject of the forinatkion of abyssal planetary fractures in the crust, provoked much di:-_I,_-LLSsior.. @ Abstracter's note: Complete translation ._/' Card 3/-,' LITErEV, T.S. [Lebediev., T.S.1; SOBAKART, G.T. [Sobakar, H.T.] Recent data on the block structure of the Kallmius-Mius interfluve. Dop.AIT URSR no.6:783-786 f6l. (MIRA 14;6) 1. Institut geologicheskikh nauk AN USSR. Predstavleno akademikom AN USSR V. G. Bondarchukom. (Azov Sea region-Geology, Structural) 1-:3BE D TEVj_ _TS@ Some results of research under the program of the Internatfonal Geophvsical Year in the Ukraine. 'Mezhdunar. geofiz. god no.9:54- 58 161. (LIkraine-Geophysical research) (MIRI 14;3) LEBEDEV, T.S. [T-ebediev, T.S.],- SOBAKARI, G.T. (Sobakar, H.T.] Tectonics of the northeastern Azov Sea Region by geophysical data, Dop. All TJRSR no.10:1341-1345 t6l. (MIRA 1J.-M) 1. Institut geofiziki All USSR. Predstavleno akademikom AN USSR V.G.Bondarchukom fBondardbuk, V.H.j (Azov Sea Region-Goology,, Structural) .UBEDEV., T.S. (Lebediev, T.S.1; SOBAKARI, G.T. (Sobakar, H.T@] I? Surface rOlief of Pre-Cretaceou3 rocks in the northeastern part of the Sea of Azov region. Dop. AN URSR no.11:1512-1515 161. (MA 16:7) 1. Inatitut gapfi-zlkl AN UkrSSR. Prodatavleno akademikom AN UkrSSR V.G.Bonclarchukom (Bondarchuk, V.H.]. (Azov Sea region-Geology, Structural) LEDEDEV, T.S. [Lebediev, T.S.1; SORAKARI, G.T. [Sobakar, H.T.] Some recent data on the density of sedimentary rocks in the southern outskirts of the Donets Basin. Dop. AN URSR no.12: 1601-1605 161. (MIRA 16:11) 1. Institut geofiziki AN UkrSSR. Predstavleno akademikom AN UkrSSR S.I. Subbotinym. LEBEDEV, Taras-.,Sergeyevich; SOBAKARI, Grigoriy Timofeyevich; SUBBOTIN, 'YUK) Ye.I., -red.; RAMLIVA, akademik, otv. red.; ANT01% N.P., tekhn. red. [Tectonics of the northeastern Azov Sea region; based on geopbysical data]Tektonika severo-vostochnogo PriazovIia; po danrym geofizicheskikh issledovanii. Kiev, lzd--.-o Akad. nauk USSR, 1962. 82 p. (MIRA 15:10) 1. Akademiya. nauk Ukrainskoy SM (for Subbotin). (Azov Sea region-Geology, Structural) LEBEDEV. T.S,j SOBAKARI, G,T. Some characteristics of the tectonics of the northeastern part of the Azov Sea region, based on geophysical data. Geofiz.sbor. no.1:11-23 162. (MIRA 16:3) 1. Institut geofiziki AN UkrSSR. (Azov Sea region-Geology, Structural) LEB9DEV T S.; SOBAKARI, G.T.; OROVETSKIY, Yu.P.; BOLYUBAKH, K.A. Geologic structure of the conjugated zone of Pokrovo-Kireevskiy and Tellmanovo blocks in the northeastern part of the ;@zov Sea region. Geofiz.6bor. no.1:32-36 162. (MIRA 116@-3) 1. Institut geofiziki AN UkrSSR. (Azov Sea region--Geology, Structural) LEBEDEV T,.q- [Lebediev., T.S.]; SOBAKARI., G.T. (Sobakar, H.T.]; OROVETSKIY, YUOP, [Orovetalkyi, IU.P.]; BOILYUBAKH, K.A. Recent data on the geological structure of the zone of unction of the Pokrovo-Kireyevo and Tellmanovo blocka northeaotern part of the region of the Sea of Azov). i Dop. All URSR no.1:91-94 162. (KERA 15:2) 1. Inotitut, goofiziki-AN USSR. Predstavleno akademikom AN USSR V.G.Bondarchukom (Bondarchuk., V,H.J. (Donetsk Province-Geology., Structural) SOBAKOI) G.T.; T-FIRP EV, T.S. Taking into account the effect of relief in gravimetric studies in the mountain regions. Geofiz.abor. no.2:33-40 162. (MIRA 16:3) 1. Institut geofiziki M V@r$SR. ' (Ukraine-Gravity anom-q I i es) -- (Ukraine-Landforms) , .I..-., @v .. LEBaEV, T.S.; KORNIUTS, D.V. Experimental studies of physical properties of rocks subjected to high pressures and temperaturese Ceoriposbor, no.2:119-121 162. (MIU 16:3) 1. Institut geofiziki. AN UkrSSR. (Earth-Surface) LEBEIEV2 T.S. Conference of @eophysicists and astronomers of the Ukraine. Geofiz.- biul. no.12s97i-102 162. (NDU l6s5) .(Ukraine--Geophysica) (Ukraine--Aptronomy) KORNIYETS, Dar Vasillyevich; SUBBOTIN, S.I., akademik, oti,' red.; KHOZANET, S.Y., red.; TUIRBANOVA, N.A... tekhri. red, [Heat of the earth] Teplo Zemli. Kiev, Izd-vo AN Ukr.SSR, 1963. 63 P. (14IRA 16:11) 1. Akademiya nauk Ukr.SSR (for Subbotin). (Earth temperature) LZBEDEV, Taras Sergeye ,ZMDEV, Taras Ser_ y ViCh; SOBAKARI Grigoriy Timofeyevich; -ffffMTSM, Yurly Pavlovich; BOLYURAKH, Klavdiya Antonovna; SUBBDTIN, S.I., akadem4, otv. red.; MFIINIK@ A.F.,, red.izd-va; RAKHLINA, M.P., tekhn. red. (Tectonics,of the central part of the northern slope of the Crim*n Mountains and results of its studyingi based on geophysical and geological data) Taktonika tsentrall- noi chasti severnogo sklena Krymakikh gor i opy-t ea Izu- cheniia; po materialam geofizicheskikh i goologicheskikh Issledovanii. [By) T.S,Lebedev i dr. Kiev Izd-vo Akad. nauk USSR, 1963. 85 P. @mim 16:5) 1. Akademiya nauk Ukr.SSR (for Subbotin). (Crimean Mount*ain-Geology, Structural) ACCESSION NR: AT4016590 S/2819/63/000/004/0014/0018 AUTHOR: Lebedev. T. S. -. Korniyets, D. V. TITLE: Investigations of the earth's upper mantle In the SSSR SOURCE: AN UkrRSR. Inst. goofiz. Geoft. sb., no. 4(6), 1963. Kompleks. geofiz. issled. territor. Ukrainy* (Complex geophysical investigations of the Ukraine), 14-18 TOPIC TAGS: geology, upper mantle, geonomy, cosmogony, earth tide, silica, high pressure, geophysics, silicate, earth core, metallic state, helium, lithium, earthquake, surface wave, seismic wave, velocity profile, travel-time curve, seismology, seismic activity, magneto-telluric method, geomagnetism, magnetic field, earth crust, lava, vulcanism, tectonophysics, deep seismic sounding, Quaternary glaciation, eclogite, ultrabasite. ABSTRACT: A conference on the theme "The Earth's Upper Mantle" was held in Moscow durin- the period 24 January - 5 February 1963. A large number of the reports presented already have been published. Summaries of the following report@ are given in the con- ference report. V. V. Belousov -- development of a now earth science to be called geo- nomy. V. S. Safronov -- theory of the earth's formation by accumulation of solid particles and bodies. X. N. Pariyskiy -- study of the horizontal nonhomogeneities of ihe mantle on Card j/*' ACCESSION NR: AT4016590 the basis of earth tides. P. S. Mantveyev -- anomalies of tidal deformations of the earth's surface in the SSSR. V. A. Magnitskly and Yu. A. Meshcheryakov --recent vertical move- ments of the crust and their geophysical interpretation. Ye. A. Lyubimova, --heat flux on shields in a zone of recent movements. Yu. N. Ryabinin --influence of high pressure on certain properties of solid bodies. S. M. Stishov -- a rutile-like modification of silica and phase changes in the earth's interior. L. V. AlItshuller --shock compression of silicates and metals and possible composition of the earth's mantle and core. V. N. Zharkov and V. A. Kalinin --determination of the equations of state of rocks at high pressures. V. P. Trubitsyn and F. R. Ulinich -- possible pressures during the transition of helium and lithium into a metallic state. S. A. Fedotov -- new data on the upper mantle in the southern Kurile Islands. N. V. Kondorskaya - - earthquake distribution in the Kurile-Kamchatka are. Z. S. Ivanov and others -- use of surface waves for study of structure of the upper mantle. N. V. Shebalin -- the upper boundary of the layer of low velocities in the upper mantle. T. B. Yanovskaya and I. Ya. Azbell -- determination of the velocity profile of the earth's mantle from the travel-time curves of P waves. N. N. Matveyev and A. S. Alekseyev -- use of a computer to find variants of structure of the upper mantle best fitting travel-time curves for deep-focus earthquakes. V. P. Orlov -- anomalies of secular variation of seismic activity in Tadzhikistan and the East European Platform. A. N. Tikhonov and others -- electromagnetic parameters of the upper mantle as determined by the magneto- telluric method. V. I. Pochtarev importance of the mantle in studies of geomagnetism. Card 21A ;A_ @k@@44f ACCESSION NR: AT4016590 T. N. Simonenko -- the anomalous magnetic field of the SSSR. V. V. Belousov -- structure and development of the earth's crust and upper mantle. Yu. M. Sheymnan -- composition and origin of lavas and structure of the upper mantle in the North Atlantic regi6n. G. S. Gorshkov -- vulcanism and the upper mantle. N. I. Kbitrov -- the earth"s crust -- upper mantle transition zone. N. A. Belyayovstciy and V. V. Fedynskty -- study of great depths in the SSSR. Ye. M. Rudich -- structure and development of the earth's crust in East Asia. I. V. IAtvinenko -- structure of the earth's crust on the Baltic shield using deep seismic sounding data. M. V. Gzovskiy -- problems in tectonophysics, as- sociated with study of the upper mantle. G. Z. Gurariy and 1. A. Solov1yev -- structure of the crust and density of matter in the mantle. S. A. Ushakov -- isostatic state of regions of quaternary glaciation. G. D. Afanaslyev -- relationships between the upper mantle and, crust. N. P. Vasillkovskiy -- differentiation of matter and formation of the crust. 1. P. Kosminskaya -- stratification of the earth's crust as indicated by deep seismic sounding. G. B. Udintsev -- relief of the Pacific Ocean floor. V. I. Popov -- formations and rela- tionship to deep structure of the crust. G. S. Shteynberg and M. I. Zubin -- relationship between vulcanism and development of geological structures. I. A. Yefimov -- the eclogite formation of Northern and Southern Kazakhstan. S. V. Moskalev -- genesis of ultrabasite in relation to upper mantle processes. Orig. art has: no graphics. ASSOCIATION: Institut geofizild AN UkTSSR (Geophysics Institute, AN UkrSSR) Card LEBMVP T.S.; SOBAKARI, G.T.1 CROVETSKIY YU.?I Physical properties, composition., and age of crystalline shales, sandstones, and spilite-type rocks in the northeastern Azov Sea region. Geofiz. abor. no-4:19-27 163. (MIRA 16:9) 1. Institut geofiziki AV UkrSSR. ACCESSION NR: AT4016591 S/2819/63/000/004/0112/0123- AUTHOR: Lebedev, T. S.; Kornlyets, D. V. TITLE: optimum pressure and temperature values (or investigation of the physical parameters of matter in the earth crust SOURCE: AN UkrRSR. Inst. Geofiz. Geofiz. sb., no. 4(6), 1963. Kompleks. Geofiz. issled. territor. Ukrainy* (Complex geophysical Investigations of the Ukraine). 112-123 TOPIC TAGS: geology, geophysics, earth crust, rock, high temperature geophysics, high pressure geophysics, Moho ABSTRACT: The Laboratoriya vy*sokikh davleniy instituta fiziki Zemli AN SSSR (High Pressure Laboratory, Institute'of Geophysics, AN SSSR) has studied the physi- cal properties of certain rocks at pressures up to 5,000 atmospheres and In some cases at temperatures up to l,OOOC; still higher pressures are being used at the present time. The Institut geokhimii I analiticheskoy khimii- im. akad. 1. V. Vernadskogo AN SSSR-(Institute of Geochemistry and Analytical Chemistry) is syste- matically studying geochemical processes at 3,000-5,000 atmospheres and 500-),OOOC. other institutes of the SSSR Academy of Sciences have developed apparatus for re- search at 30,000-40,000 atmospheres and 1,500-2000C. An attempt is made to esti- Card 1/2 ,ACCESSION NR: AT4016591 mate the range of temperatures and pressures which are pertinent for study of the earth's deep structure so that apparatus can be designed to meet these requirements. A review of the literature on pressures at great depths indicates that at 40 kilo- meters the mean maximum pressure is more than 15,500 kg/cm2 and hydrostatic pressure at the same depth somewhat exceeds 11,000 kg/cm2. Experiments at 15,000 kg/cm2 ap-: proximate conditions near the Mohorovicic discontinuity; experiments with a hydro- static.pressure of about 20,000 kg/cm2 approximate conditions below this discon- tinuity (where the Moho lies at a depth of 45-50 km)- Postu]@ted temperatures at various depths are reviewed. Special attention is given to shield areas, since the', authors have a particular interest in the Ukrainian shield. At depths of 30 km temperatures range from about 600C to as much as 1,000C in special cases. it is concluded that laboratory studies of the behavior of rocks at high pressures and temperatures should be formulated to consider pressures of )5,000-20,000 kg/cm2 and;@ temperatures of 500-1,000C. Initial efforts should be 'limited to 15,000 kg/cm2; as experience is accumulated the experimental temperatures can be increased. However, in designing apparatus the need for ultimately making investigations at 20,000 kg/cm2 must be given serious consideration. Orig. art. has; 2 formulas and 2 tables. ASSOCIATION: INSTITUT GEOFIZIKI AN UKRSSR (Geo h ics Institute AN U%ir SSR) SUBMITTED: OlMar63 DATE ACQ: 11094 MCI.: 0 JUB CO0j- AS NO REF SOV: 000 OTHER,..-, 000 LEBSDEVY T.S. [Lebediev, T.3.]; SOBA:@ARI, ""F.T. [Solbaknx, O."W"ITSKIYY ---'-Ttr.11.@(Orovets1kyi, IU.11.j; DOLYUBA'Zi, K.A. I New data on the tectonics of the central :jart of the northern slope of the CrLman Mountains on the bacis of the raterials of geophysical studies. Dop. 10i UR3111 no-3:3'86-30,0 163. C-:11--ck 17:10) 1. Institut ;cofizild A:, Ukr3.'@.L'. J-rad:3tavleno alzademikwia All S.I. Subbotinym. P -fUBAKii, '@-" 13BEDEV the Craimea. lg the and 9 u r, 18,6) Uk lllstltut L 2/996-66 EVIA(h)/EWT(l) GW ACC NRt AT6005987 (N) SOURCE CODE: UR/3169/65/000/001/0087/0105 AUTHOR: , Lebedev, T S...'_(,Candidate of, geological-mineral sciences); Shaporak,_V. I.; Savenko, B. Ya. ORG:- none TITLE.- Physical properties of bottom deposits in the equatorial belt of the Atlantic Ocean SOURCE: AN UkrSSR. Geofizicheskiy sbornik, no. 1(12), 196Si Stroyeniye zemnoy kory L fizicheskiye svoystva gornykh porad (Structure (if the earth's crust and physical pro- perties of rocks), 87-105 TOPIC TAGS: ocean dynamics, longitudinal wave, shock wave propagation ocean property ABSTRACT: Elastic, electriizal, and magnetic properties of samples collected during the XV voyage of the Mikhail 4omonosov research vessel in the western Atlantic are in- vestigated. Using the formula E 0 -0) Vu I/Al +00 -@d) and certain corrections (taking into consideration the finite dimensions of the me- dium) the propagation velozities of longitudinal waves (V were evaluated, where VLj Card 1/2 27996--66 ACC NRs AT6005987 is the velocity of propagation of longitudinal waves in an infinite medium, 9 is' Young's modulus, p is the sample density, and a is the Poisson coefficient. The elec- .trical resistivity of the sample was investigated using the formula LO st and some additional concepts where R. is the resistivity of the sample, R is the re- sistivity of both the sample and the solution, L is the distance between two elec- trodes, I is the sample length and S1 is the cross section of the solution colwnn. The measurement apparatus consisted of 2 electrodes and used an alternating current of 1000 cps. Magnetic susceptibilities of all collected samples were investigated by using a balanced H-shaped magnetic bridge as a pickup. The data show that 1) longi- tudinal (PL) waves of samples saturated with ocean ifater have a propagation velocity.. of 1300-1600 misec and that the propagation velocities for grayish ooze, white ooze and yellowish foraminiferalooze are 1580, 1510 and 1450 m/sec, respectively; 2) the resistivities of bottom deposits in the western equatorial belt of the Atlantic are dependent mainly on the lithologic and mechanical properties of the deposits varying from 0.5-0.9 A. The foraminiferal ooze, however, has resistivities up to 90; 3) the magnetic susceptibilities of the bottom deposits vary from 1-40-10-6 CGSH; and 4) the vibratory motions of the ship affect the reliability of seismic evaluations. Orig. art. has: 2 tables, 7 figures. SUB CODE: 08/- SUBM DATE:;' 29Aug64/ ORIG REF: 010/ OTH REFI# 012 Card 2/2 ACC NRt AT6034513 AUTHOR: Lebedev, T. S.; Bolyubakh, K. A. ORG: none 1'5 5 SOURCE CODE: UR/0000/66/000/000/0147/0 TITLE: Structure of the Earth's crust in the Crimea Mountains and the Black Sea basin according to data from gravimetric investigations SOURCE: AN SSSR. Otdeleniye nauk o Zemle. Nauchnyy sovet po kompleksnym issledo- vantyam zemnoy kory i verkhney mantii. Glubinnoye stroyeniye Kavkaza (Abyssal structure of the Caucasus). Moscow, Izd-vo Nauka, 1966, 147-155 i-ji,LC TAGS: riv%G,ovicic discontinuity, earth gravity, earth crust, granitic layer, bas%'tic layer, ABSTRACT: The correlation of available data on the structure of the Earth's crust in the Crimean Mountains and the Black Sea basin made it possible to compile a I generalized gravity-anomaly map (not given in the test) for this region. In the area of the Black Sea, a large, positive anomaly, 10-35-km wide, extending over * significant part of the Crimean meganticlinorium is superposed on * background of a smoothly varying gravity field. A region characterized by some- what reduced gravity values borders the positive anomaly field of the Crimean Mountains from the side of the Black Sea. Two very intense positive gravity anomalies- are found in the central part of the Black Sea. The deep-seismic-sounding and .gravity.data were utilized in preparing 3 cross sections of the Earth's crust. ACC NR: AT6034513 Qualitative calculations indicate that the intense positive gravity anomalies of the western Caucasus Crimea and the Island of Cyprus are associated with either an upwarping of the basaltic layer or with an intrusion of a body of basic and ultra- basic rocks into the upper layers of the Earth's crust. Orig. art. has: 4 figures. [WA-7941 SUB CODE: 08/ SUBM DATE: 26Feb66/ ORIG REF: 030/ OTH REF: 005/ I;MDEV. V.. kapilau dal'negO pivvaniYa gtion in the , and carr7ing Out nav' Xpe"rience in preparing ot. no.6:7-9 je '59. t Of the Aretics Morefl (141RA 12: 9) eastern Par on) (Aictic regiona-Navigat' SOV/137-58- I I -Z2191 Translation from: Referativnyy zhurndl. Metallurgiya, 1958, Nr 11, p 51 (USSR) AUTHOR: .. Lebedev, V. TITLE: Technological Progress and Rise in Labor Productivity in the USSR Copper Industry (Tekhnicheskiy progress i povyshenive proizvoditel' nosti truda v mednoy promyshlennosti SSSR) PERIODICAL: [ Uch. zap. I Akad, obshchest@,, nauk, 1958, Nr 32, pp 70 -105 ABSTRACT: An examination is made of the significance of technological progress, and in particular of the mechanization and automation of production, the introduction of the latest equipment and advanced processes, and also of replacement and modernization of outdated equipment for the purpose of attain;ng d higher level of and a rapid rise in labor productivity in the copper industry. A. P, Card 1/1 AUTHOR: lebedev., V., Engineer 84-12-29/49 TITLE: Starting the Engines of the Tu-104 in Winter (0sobennosti zapuska dvigateley TU-104 zimoy) PERIODICAL: Grazhdanskaya aviatsiya, 3.957, Nr 12, p 18 (USSR) ABSTRACT: The author discusses different factors which determine the behavior of engines at low ambient temperatures, such as the fuel ignition delay in the turbostarter and the engine, and the following flame-up of the accumulated fuel. Methods of preheating the starter according to the prevailing conditions are described. Another major factor affecting the start of the engines is the viscosity of the lubricant and hydraulic drive oil, which increases considerably not only with lowering temperature, but also with its time in use. AVAILABLE: Library of Congress Card 1/1 LIEBLeDEV, V., kand. me(j. rauk; KII ", I'; J, 4. kosr,. 47 (eKsLr. Iyp. Silence. B.*, !,@',BFVN, V. , . Ijigh-quality tir95 for motor vehicles. 17-18 ja 165. I I @,.,t. r2@,Isp@ 0 no.- I 18- 3) 1. Yaroslavskiy shinnyy zav0d- SOV/84--758-90-33/51 AUTHOR: Lebedev. V_P Enginee-_ TITLE: Tune-up of Tu-104 Eri@,ines (0sobennost-i otladki dviga- teley sawoleta Tu-104) PERIODICAL: Grazhdanskaya avia"Islya, 1958, Nr 9 pp 28-29 (USSR) ABSTRACT: Tune-up of turbojet engines of Tu-104 airliners has become necessary as a part of aircraft maintenance. This applies especially to the starting and pick-up phases of engine operation. The tune-up consists, In the main, in Improving the runup time of the engine. The article serves as a provisional instruction for engine maintenance personnel of airports and mainte- nance workshops. The main concern of the author is how to avoid compressor stalling in the initial, and overheatinn- of the exhaust jet in the later phase of the runuD. Three -raphs accompany the text. Card 1/i LEBEDFV., V.@-- Fertilizers go to the fields. Mest.promA khud.promys. 2 no.3:22 Mr 161. (MEU 14: 4) 1. Zamestitell nachallnika oblastnogo upravleniya mestnoy promyshlennosti, Kaluga. (Phosphate industry) LEBEDFV@ V-p podpolkovnik Demonstration of methods is the most important factor. Voen.vest. 40 no.10:51-52 0 160. (Military education) (MM 14:5) L 52-136-6-5- - EWT(m)/&IA(h) Pab 39/061@ AZ=3S1CCf FMt AP5013220 UR/O36T/65/ooi/o(*/o6 -5 AUM(Rit Apalin V-4 Grltayuk@ ?&"tikov I 1,ell-edle-11 11=, Neutron emission fr= fragments of t?33 -"5 in taer- 4 fission SGUECE: Yaderanya fizika, v. 1, no. 4, 1965t 639@-646 M, neutron TOPIC TMS; nuclear fission, thermal neutron fission, figsio iLgLagLe emission, symmetric fission ABSTMCT: This is a continuation of earlier meas=ements (ZhM Y. 43, 329, 2053, 1962; Nucl. Phys. v. 38, 193, 1962 and v. 41p 92, 1963; ZhETF v. 46, 1197, 1964) of the total n=-ber of neutrons emtted by fragments as a function of their mass ratio: In the Present work the authors measured the ne-eron (--aiasion from fragments of i U233, U235, and PU239 sepwated by an improved tecbniW.!e, and discuss the accuracy of the informtion-obtained. The experimental technique was the ssme an in the earlier work, with the fragment mass de-ten-Anation made by means of a double-grid ionization t-b er and a liquid-organia aciatillator neutron detectore To assess Cnrd 1/2 L52736-65 ACCESSION ZIR: AP5013110 the reliability of the information obtained in the wIrmetric- fission region, the experimental mass distribution was comared with the results of radiochemical stu- dies (J. Katcoff, Nucleonics V. 18, No. U, 201, 1960). Good agreeneat with these data was found everywhere exceprt in the --ju-matric-fission region, wh,@-re the present data lie sameiihat above the values of Katcoff. It is estimated that not mo-re tban4'. 3CF% and mare likely 15--20-,f, of the events in aymietric fission are spuriouz. An attermt is made to deduce a corTelation between the neutron emission da'a and the dynanics of the fission process at low emcit-ation energies. "The -a@.ztlljorI3 t1iink j. Milton for sending his t0bles, and B. Geylil an and V. S@ry-@Jn 'or Interesting' discussions." Orig. art. hast 6 fqufea I forlElara 0 ASSOCTAT1011s None SUEY..-LTTzD: i6oct.64 EINCL: 00 MM CODE: VP IM RU SOVI 005 7 LEBEDEV,-V.,,-inzh. Simplification of continuous beam calculations. Rech, transp. 21 no.3:39-42 Mr 162. (MIRA 15-4) (Beams and girders, Continuous) L 8�18-66 FSS-2/EWT-(l I/FS M-3 DD 1 ACC NR: AP5026191 -bkl-- 59/65/000/008/0027/0029 SOURCE CODE: 02 AUTHOR: Lebede _rl_ v.J L_(Candidate of medical sciences) ORG: None TITIE: IState of weightlessness Ik and the Ilend of the world" SOURCE: Nauka i teklmikaq noj@ 8,9 1965# 27-29 TOPIC TAGS: psychopathology# cerebral cortexs otolaryngologys weightlessnesss flight physiologys flight disorientation ABSTRACT: On the basis of increasing literatw-e datas the psychophysio- logical,reactions of individuals to a state of weightlessness have been' divided into three groups, The first group includes persons who experience no discomfortj maintain their work capacity# and enjoy freedom of movement, The second group includes persons who experience anxiety, discomforts and fear in the first 4 to 6 see of disorientation followed by a feeling of pleasant excitation and complete relaxation, The present article is primarily concerned with the third group which reacts violently by developing symptoms of seasickness or an Hend of the world" complex. In the latter case, the illusion of falling becomes very real and.the subject experiences anxiety# terror and grief for 1 to 2 minutes as he actually "sees" people dying,, buildings, d- t' 7jL7: L 8918-66 ACC NRs AP5026191 nature being destro7edo and the world literally coming to an end. This type of complex has been compared to Menlere's disease and Is attributed to a fLuietional disturbance of the brain as a result of a vestibular analyzer disorder. Weightlessness of the vestibular anal7zer otoliths affects the transmisqion of impulses to the brain, Disorientation produced by weightlessness also affects the nerve impulses transmitted from the skin surface, skeletal musclesp and cardiovascular system to the brain* When the brain is unable to Integrate and analyze properly these changed and sometimes distorted nerve impulses, there develops a psychophysiological reaction of the "end of the world" type. Psycho- physiological reaction differences of individuals to weightlessness are largely determined by auditory analyzer sensitivity and also sensitivity to physical strain, Orig, art, has: 4 figures, SUB CODE: 060 051 SUBM DAME: 00/ ORIG REF: 000/ OTH REF: 000 V WLC - No', 000254 SOURCE CODE: UR/0209/65/000/011/0027/003 AUTHOR: Kaslyan, I.; KoDanev. V.; Lebedev, V.; Khlebnikov, G.; Kolosov, 1. 7 ORG: none 69 TITLE: On an airplane in a state of Results or research SOURCE: Aviatsiya.i kosmonavtika, no. 11, 1965, 27-32 TOPIC TAGS: human physiology, space physiology, weightlessness, parabolic flight ABSTRACT: Cosmonaut training flights in aircraft equipped with a weightlessness tank are described. Some physiological parameters of the trainees during various stages of the flight are discussed. One series of tests performed on a dynamometer showed that, compared to horizontal flights, during weightlessness the amount of maximum muscular force which can be exerted is reduced by 6-12 kg for the right hand and 4-12 kg for the left hand. This decrease in muscular force is probably connected with the de- creased tonus of the skeletal muscles and functional changes in the central nervous system during weightlessness. The coordinograph, a device for measuring changes in fine coordination movements, recorded the total work time for each test, the number o errors, and the time of one movement. Although no disruption in coordination was ob- served when these tests were conducted during parabolic flight, most cosmonauts showed some lag in the speed of execution of motor acts. Orig. art. has: 2 figures. [JS]fl SUB CODE:- 06 SUBM DATE: none/ Card 161::- L 07850-67 M-JT(1)' SCTB DD ACC NRt --- AP 28039 SOURCE CODE: UR/0025/66/oOO/005/0111/0113i AUTHOR: Kuznetsov, 0. (Paychiatrirt); Lobodev V. (Candidate of medical aciencos) i-IRG: none )7 TITLE: Isolation /Y/ ISOURCE: Nauka i zhizn1.1 no, 5. 1966, 111-113 OPIC TAGS: isolation test, nervous system, psychologic stress, psychopathology -'BSIIRAGT: T.his popular article based on the 1iterature, discusses the phenomnenon o A' @ @Aallucinations reported by astronauts and experimental subjects under conditions of @rolonged isolation and lack of activity. To determine the nature of this phenomenonp Various experiments have been conducted in mockup space capsules and soundproor test bhambers with'the subject isolated from external stimuli. Some subjects lose their 6ense of time, some develop anxieties, and others experience delusions, illusions and hallucinations. These states in themselves are not symptomatic of mental disease as i@hey may appear in healthy individuals when some factor e.g. lighting, prevents Iaccurate, visual or auditory.perceptiono Various casas are cited, During prolonged periods of isolation the psychic state of the person is very important, particularly @atigue@ anxiety and fear, Another type of hallucination found to appear is 'pharacterized by visual and auditory mental images becoming so vivid that they become Card 112 @ACC NR' AP6028039 0 a reality for the subject. The vividness of the images is caused by the reduced @urdber of stimuli acting on the sensory organs. Under normal conditions the vividness Pf mental images (recollections,, wishes, ideas) is damped by numerous real stimuli paking the former appear-very pale and indistinct by comparison. The two different theories explaining the.-origin of hallucinations are not incompatible. With higher nervous system and brain disorders induced by prolonged isolation,, vivid mental images @ay become hallucinations;andj in tupli.,illusions and delusions may become hallucinations. Possibly, halluoination's found in mentalillnesses also have two ,6ifferent origins. Further study of the'problem is vital@for aviation and space travel as well as for persons-engaged in monotonous tasks under conditions of prolonged @solation. Orig. arte has&.: nones A SUB CODE-. 051 SUBM DATif',. none 2/2 N Serkini Lebedcv, Vith 'Ononovg I . . ter ogeTatID6 ra na stepanenk09 th -0 lievily-Developed Re.' -15 i regi8t ((),yt r,,,.,rabotk lodes E%perience5..onductOr TV ikovykll trl 0 @1_ --kh TITLE'. Lalainar Se m1c poluprovO611 n) 10 TSSK) ,,Iosvostnyk'Q niyej 1958, j1r 1, pp- se ,,aico,jductO_1' o5troje 1, ibor .1 t 0 11 , Of L Pr Lties are sl_O@'n Of hov ..@-jines. By meal c,jvel 1h is 6 pO13Bibil"' iculatinull schene Of vini(; . ter The umerical ca 11 the The re915 kB5TRkCT' C.4 ri, red - - to tr@e V L.0aes in isters pro', it 0" licatIon JOC, f 0,10vable reo - V 0- t" of its apP . Icoue co,'-e no possibill 'Unerica - jca t'n e tore ,,r.,Ler 'Clationed cn1j 11P n-'also B M I f", 1.) 0, 1 t left 0 'Int A)11t it brirlu'03 Cr, riu @@ svitc, ce e '_ec0(jer tri - lontr r a hbojirir'L@ chniciLl lock Is 01 nelb 3-te E: raw states radi 0 t 'h e -ers. Vne to 011ploy 6 of ,I -a i t n -100 for tae trig" Cd. - COMP iver. is US tD @iers -di .sed. It '1013t "al f tuninb e dise"10,itters for the , @.fnviier u - t, yLse @D. p a tra- I . common C- M 'th t the aid ` the e"tter triodes v1I ay %I i orrectOr In @jd ,,Ich connectIOn' r,_riember a2 c of fjT1 R_ card 1/9 as vlell ExPeri Wit], ",Les La,@in, Wit!' a jr ar Se..,ico' ed nduct-.r Tr- 20cles "O,@'13ter oDerati,,, be eacll,.d POL-ex, 171 t 1.f -1 C a. t i 1,11z)pt anplifIcat4.j4 cert,,,,, eve', of Pulce of, t ",a-!_eMe, t CU: all of 17!1 r,1 0 to ,': @j be re. 10 ic Z1. @7: t can are Sl a 'i c are 6 a Li brar f i -rat 7 14 rol@, Y Of con e 0:" O_*. th e Tri0cles-A Ic' 3 refererceq, PP11 catjon Card 2/2 MLIKdV., V.A.,, kand.tekhn.nauk; LZBEDENY V.A.; ARUTYUNYAN, inzh.; @AGARYSHLIVJ* D.F., in2ft. Experience-in the use of hydrocyclones for the P"ification of sun- flower-seed micellee MaBl.-zhir.prom. 29 no.1:27-30 Ja 163. (MIRA 16:2) 1. Krasnodarskiy inatitut pi3hehevoy promyshlennosti (for Easlikov.. Lebedev). 2. Zaporozhskiy maslozhirovoy kombinat (for Arutyunyan, Agaryahav). . (Oil induptries-Equipment and supplies) LEBEDEV, V.A. Effect of ecologic conditions on the resistance and susceptibility of cotton plants to pests and diseases. Vop. ekol. 7:95-96 162. (MIRA 16:5) 1. Sel'skokhozyaystvennyy institut, Samarkand. (Samarkand Province-Cotton-Diseass, and peat resistanFe) LEBEDEV, V.A., kand.biolog.nauk Oriental fruit moth. Zashch. rast. ot vred. i bol. 8 no.112:46 D 163. (14IRA 17:3) PoLYANsKly, Viktor Ivanovich; UEBEDEV, V. Gusev. Kaliningrad, Kaliningradskoe knizhnoe izd-vo, 1963. 50 P. (MIRA 17:4) : - @ @:@r r. , . - 1. LEBEDEV,.V., kand.med.nauk Adynamia in spaco flight. AvJ kown. 46 no.9t2L-24 5 163. (141RA 161lo) LEBEDEV,V., kand. med. nauk Man in weight'legaries--; !-n -@ -@- -.. ! I . I j -' - " @ _. I ---u- .- -.. - kosm. 4:7 no.9.,77-82 s t64 (IMU 17:8) 413-43-65 E E C-VE I11; )/EWT (d)Anc(,r)/E-----,T(1 I/EwPWA@Vm)/FS 1 '-2/ E PdTI/@Ro-4/Pe3?5@Pq-4/ fiR-. AP5002726 Fa q "P-e 2 764/060/0 /0015/0016 CarAidate of medical sciarvaes) The crew of an interp:@@e@taa a@cq- a-hip k-r-/ SOUFCR.- Nauka i ztdzn1, no. 12, 1964, 15-18 TOPIG TAGSz spacecraft, intarplanetary travel, payeboptWsioloGy, medical traiaing i.DS711ttiCT, - The problems concerning the peraonne! of a crew that mi.ght take t4ie long voyage -to Mars or Venus are examined. Many profesuions need to be represent,--A, since the ship will not carry one member of each profession required, each a!ztronaut aust be proficient in seve-7;d prnfessiorLq. It is supposed that such a n MUSt @, . nly -3 ay car-.y L-6 meo, some of whom it,"@rt bc eriGin4Ffers, but o e cerlal b doctor. In auch cramped quartars, @(;-mpatibilitY will be a vital facror. 7he .7 -n -m peditionz ane, frop; act, Lost.% ite@i 3everal -@pies of the problo, 1'rc,. P-v, tC315 that U16 coxmmudst peopia-@3, of LL,@tir -.0rale i'n Cormaun-istic up- I He tftini-cs tests be ar" better prepaxf@d t4i-u,, pooples, C @ Ow Plowever, ander siaulited ii-,tar-planotai-y It 14, nat enouPh to -,Bapoi-zd cifferently in msr,uly a person's abaracter--latica anii r--)5ponzas; Ie wnAy Cwd 112 L 41343-65 ACCESSWU XRx AP5W2726 different groups, It in beat that a group be m2de up of people not only bound togather by the current goal but by dooper and more sympathetic tias. The membors ,1-t he psychop4mialogically compatible. The xaln them3 of the author's discussion is tho aaed for doctor-astronauts, the need to train doctors for 5Lpecific purpoze, to tz-,-in them to operate -.Ln confined and inadequate quarter@-.. to obzervc4 people for emotional as wall as ph@rjical problem. The euthor considers the prob1sm of improving apparatuz in the spacecraft to make the doctor Is work as favorable as pazaible. Orig ga art* ha5t 2 figw,eat AS--MIATIONt nonp WBMITMC GO ENGL: 00 50 GCD& SVj; PH NO REF SOVz OW OTHER: 000 Card2/2 LEBEDEV, V. A., Cand Biol Sci -- (diss) "Susceptibility and resistance of cotton and other plants to injuries-i.*- (\ the spider mite .11 Samarkand, 1957. 16 pp (Min of Agr USSR, Uzbek Agr Inst im V. V. Kuybyshev), 100 copies (KL, 1-58, 117) _ 35 - ussR cultivatca Plant@-, Pi.--.*.nte, for Toclunic,7.1 U,,3@,, 14 oil pl,@nta, Plc@"-Its. Ab,i Jour Rof Zhur - Biol., No 6, 1958p No 34725 ,'%uthor Lebodav. 'I'Tot -,-ivon U Titl,) On tlio RoBis@,,_,nc(@, of Cottoli 111anto to Spider mites Orig Pub Sots. s. kl-i. Uzbckistana, 1957, lio 4, 22-24. Abstract Field conductod in 1955-56 with va- rious varictius of cotton plants hl-vo shown that thoso Dlants which cbsorbod ;.,T and P durin@, ViCir ontir-, vuL;::;tuation p_-riod ar, i_,,orc r@.sistax,'- to s@ider mites. Th_-@ yicld of th-- cotton olant in in Va@@3c arcas incr,@zs,@d bY 2.5 hwt pcr h@jct_,r_ SolClir _-S a rosult of th@) achicvcd throush of th,:@ li_,r.-@ful offocts of spider mites S-.--,irnov, USSR/Cultivated Plaits - Commiercial. Oil-Bearing. Sugar -Bearing. M Abs Jour : Ref 2-Mur Biol., No 12, 1958, 530697 Author : Lebedev, V,A Inst : Title The Effect of Biological Peculiarities of the Plairts and Ecological Factors on the Resistance of the Cotton Plant to Spider Mites. Orig Pub Xhlopkovodstvo, 1957, No 6, 4o-42 Abstract The cotton plant varieties which are condu-ive to mites are those in which the thickness of the lower epiderms aud of the spoii&y parenchyna of the leaf measures 129.6- 1-36-5 i.e., a thickness which does not exec-ea -the length of the piercing bristles of the mite. This per- raits the mite to feed oa tile c,--ntents of the chlorophyll- bearing palisade parenchym- The cotton plant varieties favorable to the ELito are also those -with a porous struc- ture of the leaf cells (8.2-9.8 cells per wAt of area Card 1/2 81 MI USSR/Cultivated-iPlailts - Cormercial. Oil-Bearing, Sugar-Bearing. M Abs Jour Ref Zhur Biol., No 12, 1958, 53697 neasurement in the microscopic objective); and varie- ties with 6.61-8-17 atm. osmotic pressure of the cell juice. Favorable ecological conditions for the develop- mi-it, of the plant and unfavorable conditons for the feeding and activity of the mite are created by the fol- lowing: the square-pocket placement of the plants; op- timum irrigation - 6 vegetation waterings of 900-1200 ,3/ha)applidation of 30% of the yearly rate of phospho- rus fertilizers with the first Up-dressing (during the 2-3 leaf stage) and the balance of phosphorus in subse- quent top-dressing. -- A.P. Adrianov %..ard 2/2 LIBIM, V.A. ...... stance to the damages by Tatranychus urticae Koch. Dokl. AN Uz, SSR no.6.-53-55 157. (MIRA 11:5) 1. InBtitut zoologii i parazitologii AN UzSSR. Predstavleno akademikom AN UzSSR V.V. Yeachoutovym. (Cotton-Disease and pests) 4 KLADOV, Hikolay Dmitriyevich; VLASOV, AlekBey Vladimirovich; LEBEDEV, V.A., red.; TIKHONOVA, I.M., tekhn.red. [Let's carry out the seven-year plan in five years; from the work practice of collective and state farms in Tolosovo District] Semiletku v piats let; iz opyta raboty kolkhozov i sovkhozov Volosovskogo raiona. Leningrad, Lenizdat. 1959. 92 p. (Volosovo District--Agriculture) (MIRA 13:7)