SCIENTIFIC ABSTRACT SHCHERBAKOV, D.I. - SHCHERBAKOV, I.A.

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December 31, 1967
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SCIENTIFIC ABSTRACT
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SHCHERBAKOV,-D.I.., akademik# glav. red.; YEROFEYEV, B.N..* otv. red.; - imil'K.Ul, D.V., alrademik, red.; ALITGAUZ121, M.P., red.; DAFXF2711-, V.I., red.; YOZESOE, D.L.; LEVCIEUKO, S.V., red.; CHAYKCVSKIY, V.K., red.; ShErNlWi, V.S., red. izd-va; DOROUINA, I.1111.1 tekhn.red.; LAUT, V.G., tekhn.red. lGeochomistry, petrography, anet mineralogy of sedimentary formations] Geokhimiia, petrografiia i mineralogiia osadoch- nykh obrazovanii. Moskva, 1963. 457 P. (MIRA 16:12) (Rocks, Sedimentary) I-, D.!, ~r!7-r, th,~ hlnt,)ry " fh~~ for the Study of Productive Forca3 in RuEAA. Och.po ist.g~-ol.znap. no.1104-45 163. (MIRA 1647) (111~rnadskLi, '.11alimIr Ivanovich, 1863-1945) (Mines and mln.~!ral resomrnes) 611ckiil~IZLAKOVI D.I. 0. IU. S,.rrddtp the emin nt Sov--et geographer; on his 70th birthday. Vop. ist. est. i tekhe no.13:135-137 162. (YEIRA 16:5) (Shmidt, Crttlo Iu2levich. 1891-) SFIGHERB.kKOV, D.I., akademik Important source of itfe, Priroda 52 no.6:12-4-125 163. (AURA 16:6) (Water conservation) ~ - -W~Rg~ -PR I I I -~- . - ,- I ~~W* M-- SHCHERBAKOV, D.I., akademik Outstanling Soviet geologist and traveler. Priroda 52 no.10: 37-45 163. (MIRA 16:12) SIICIIERIIAKOVP [).I., akudemik V.A. Obruchev,, aninent scientist and explorer; on the 100th anniversary of his birth. Vest. AN SSSR 33 no.10:116-119 0 163. (MMA 16:11) FFDORCVICHY B.A.; -SHCHERBtIKOV, D,I. .q.E.Fersman, mineralogist, geochemist a-nd transformer of nature. Izv. All SSSR. Ser. geog. no.1-94-100 Ja-F 164. (MIRA 17:3) i,-; i~ -al forma-.`~n.; age forrifit,3111.. V, oic v aN P- ulk a1016,. znd i-od r~j i geo 1 c he Sk N, a ..s ona I I -,ly,,F '~ rami !,e t ~7,arj logov -,-ic ~Y~v-uza. dient, A.N ~,-SSR predsedatel' Komi5si. P,--~ ci-,reaelnnlyu ubr,Av,.2tnr.)~-tj v~z-asta ge,:)]ciz;:heSk.l!-,h f,~rrn-- Vj It ';ov , F'.A . ; I iF I,W], N.V. ; , F. I.; GENK IN, A. D. ; G1 t,;; 131111J; , A I.; U'UN, I- I.; K01",'llifISMY, D.S. ; SALTYKOVA, V.S. ; SAUKOV, A.A.; SOKOLk)V, G.A.; ~IIQIIERBAKOV, D.I.; SHADLU11, T.N. Konstantin Avtonomovich Nenadkevich, 1830-10/63; obitLany. Geol. mid. mestorozh. 6 no.1:123-125 ia-F 164. (MIRA 17: 11) SHCHERBAKOV, D., 1, , , akad,3,milk Italy through the e-yre3 of' a ~--eo?cgjst. ; -, In u _..6z "t-106 164. ~.-unA -L'I.-61 SHCFERBAYOV, D.I., akademik Tireless explorer oil the interior of" the earth. 'Priroda 52 no,11:45-46 163. (MILRA 17:1) :'~ . ~ l . , L,i:: I ; r l Y I V;iT~ !,I " " f! ; 1~ . , 1~ 1, ~:, , q 3 ! , '-'.!d . ;. ~. ~ -'. . , , 11 . : . , . W c- , -~ - I- ~! ;~ . -. -"Va I !,(; nm'.; 1 _,.I, t C, f a g : ~3 ', , , " r; - , .1 . I I ~ , "r , . . 11 - r ) I ZC' - v --' -'F-. , .1 ", ~. . I - P- . ~ , : L' DZEALAL3EKOVA, L.A., prof.; MtZILIN, prof., red.; ZU,-:-KOV, A.I., red.; KALEE.TNIK, S.V., prof., red.; KISELEV, Yu.N.J, red.; I:EVSKIY, V.V., red.; 0BRUCII-EV, S.V., prof., red.; ROMIN, L.Ye., doktor biol. nauk, red.; USFENSKIY, L.V., red.; SHCHERBAKOV, D.I., akadev:ik, red. [The globe, a Geograph7cal yearbook for children] Globus. [Geograficheskii ezhegodnik dlia detei.] Le- ningrad. Detskaia literatura, 1964. 333 p. (1'.IRA 18:1) 1. Chlen-korrespondent kkaderii pedagogicheskikh nauk (for Verzilin). 2. Chlen-korrespondent AN SSSR (for Kiselev, Rodin). 3. Prezident Vsesoyuznogo Geograficheskogo obshchestva (for Kiselev). SHCHERPAKOV, D,I,, akaieTik Lands r~-' anci--~nt 51, n,~.4.99-103 164. (MIRA 17:4) tjLk,)jzjy Sj!rgeyevich, akademiki KH'EaASK~ N.1 otv~ ad'-f,. ~ '. 2olia v~d r --I ak A akLciernak' za~7_ gj'av. rav- K -urly mo: -vF, Nauka Vol,, 3. -7 -k -ed WI-)! Jj lzbrannye t.i !1-),) -3' il.l.; ','jj(,jFHBhKOV, D.I.; [y, V i NT GENKIN, A.D.; %1 T .NJ C)G i j 10 rjV V.I.; VC)'"IFSUl, AT'l N AN K", T-. HC"l pf':17E. ',,',AN, A. I. ; FZKHARSKI Y, L MIN, L. I - F.K. 7 vc.; G-j S?ADL"N, N.; SE, A'0:!--an,'roVj--h Saukov, lq(D2-1,i64; obituary. Geol. rud. irestorozh. (MIRA 18%4) ia-F 165. - ::! 1: " ~: T~ * , r~' .... ... I-.-,.;,.. IF, ~'. - . , - - , : ~! t -' cn cf' n,-- - s + . , N S~SR 3 5 :n. tne :=--, -- (Mliallt. 18:10) - ~ n !- - r c C - - - - , - - n., :'. .. " . - ~:~ - , u BUGELISKIY, Yu.Yu.; VITOVSKAYA, I.V.; GODLEVSKIY, M.N.; ZVEREVA, Ye.A.; KORIN, I.Z.; NIKITINY K.K.; NTIKITINA, A.P.; FISE115KIY, G.V.; SAPOZHNIKOV, D.G.; SOKOLOV, G.A.; CHUMOV, F.V.; SHCEERBAKOV, D.I.; EDELISHTEYN, I.I.; YANITSKEY) A.A. Illia Isaakovich Ginzburg, 1882?-1965; obituary. Gool.rud.mestorozh. 7 no-4:109-110 Jl-Ag 165. (MIRA 18:8) H A 0, isoteric e 0 izc)tovjzl,)-' geolcgii. 0 c, 161 p. --o ZSS~~. Yomiss-ya po opredelEni -u. a5 A --ast;, 7r, ...,u-_o;.r, ,oz. F~e~ lo Z~ LAuNikK Hl , vii -jj jjy Vasipye-,lich; SlIGNWHAKOV, D.I. ,i ,'-, ,. akacemi I. ot" rerl.; SHOSKAWSWA, N.D., red. [On the shores and islands of Lake Baikall Po beregam. i ostrovam Baikala. Moskva, Nauka, 1965. 189 P. (MIRA 28:10) ANP'r,Ul',OV,. Nikolay Ivano-vi.-Ai, akademik (1861-192141,. ~SHCfEnAKOV, v. red.,- YANSHIN, A,L,, akademlk, ,1- akaderalk gla n ti v. red.; ZENTEVICH. L.,A,, )tv. red.- BEZPUFOV, F.L., Otv. red. [Selected works] Tzbrannve trudy, Moskval fauka. Vol..4 10~,5. 402 P. (MIRA 18!121 A Yp., re I., GLIJPUSHK !I,, FJI. red.; r tj E. F 1. . I SAv"SK Y kanrjr.-.,v~m,-~t c;F the man-,,,N~,~ure of wares and -,cables with rubber lnci.,, mal,~-ifiusl Us-,ver3henstvovanie proiz- I vods7va Prl*-v----4,-x i kalbele- s rezincivoi izoliatsiei; sbor- rik mater-nl-_ ;_ X.:~,slcva, Energiia. 196~', 263 P. (ML~A 18;8) scveshf~hamye po VI-Tr-EaLm Usl~~11fersheps'-:,-van-Lya prozvcdstva provodov i ka- beley s izolya-tsivey. I-Ith, Pe_reborv Rybinskiye, insti-cu-.' kabel2noy pro- nshte -0 yn VICOGhADOV, A.F., akadlemik; SADOVSKLY, M.A.; AKII'EDSAFIN, U.M., akademik; GERA~SIYIOV, 1.F., akademik; YANSHJN, A.L., akaderrik; SUCHERBAKOV, D.I.$ akadeizlk; A.V., akadernik; 1"A"ISEVY L.P., kand.fiz.- 1witem.nauk; OIjC'jjNI"TKOV, !.M. Devel-ument of earth sciences in Central Asia and Kazakhstan; results of t~e out-of-town session of the Department of Ea--th Sciences. Vest.AN SSSR 35 no.3:128-150 Mx 165. (MIRA 18:4) 1. Chien-korrespondent AN S-'-SIR (for Sadovskiy). 2. AN Kazakhskoy SSR (for Aklumedsafin). DZIIA!- A, L.A.; VERZILIN, i..M., prof., red.; '-ZT:jK('V, A.I., na-ulk, red.; KALESNIK, S.V., red.; KISELEV, Yu.!"..' NVIS-KIY, V.V., kerd. geogr. nauk, red.; '~'.T)IT' T V- Prof., red.; USFE17SKIv., L.V., doktor biol. nauk, lea.,* SHCHERBIAKV ?D.I., akadei~ik, red.; OBPUCM.I', S.V.,red.(deceased] [The Globe, 1965; geo~-raphical ,,-earbook for children] Globur, 11~65; geo~7raficheskii ezhegodnik dlia detei. Leningrad, Det-sk-al'a li- ter!~tura, 1965. 333 P. (I-IIHA -19: 1) -1. Chlen-korresiondent Akademli pedaf,oj~,icheskikh nauk (for Verzilin). 2. ChItan-korrespondent AM SSM (for Kalesnik, O'Oruchev). ~' "I" ;; 7-ft.)Ij . 'r. 9 a; 'r. ; : , t1j) F. "j, .11 " I I. I.. ij -, ~-( ;1,- .1. 1 ~. - ~ I .. riII!I,". - LUKI '7 1 - I . .9 (1 IFFTly F. 1, , d,~ktr- r gec~l. -A, I . - . Sclentific wcrk cf Pcademician lc-,flf Fedorkc,,ich GrIgcrIev. lzv. AN SSSR. 361-,~Tecl. 30 no.!-1:110-114 11 165, I. Cilu-n-korr,?,r~icndent AN SSSR (for ChUhrov). N~,H4 1s.12) SHCHER-3AKOV, F. Provide for safe operations of electric A-esaitin-E machiner7., Pozh.delo 6 no.2:3-5 F '60. OURA 13 5) 1. Ifachallnik Kuybyshevskoy pozharno-ispytatellnoy stantsii. (Petroleum refineriea--7ires and fire prevention) TSYPLYIIKOV, V.D., inzh.; SHCURBAKOV, P.A.. inzh.; GO-RFWV, L.M., inzh. Device for dribing spike nails by pressing. Suggested by V.D. TSyplenkov, F.A.Shcherbakov, L.M.Gorelov. Rats.i Izobr.predl. v stroi. no.13-07-88 159. (MIU, 13:6) 1. Pa materialam flormativno-issledovatellskoy stantsii pri treste, Pechorstroy Ministerstva transportnogo stroitel'stva SSSR, Komi ASSR, g.Pechora. (Nails and spikes) AU'211OR: Shcherbakov, F. A. TITLEs Some Conditions of the Concentration of Heavy t1inerals in Littoral Marine Alluvium (Nekotoryye usloviya kontsentratsii tyazhelykh mineralov v pribrezhnykh morskikh nanosakh) PERIODICALi Doklady AN SSSR, 1956, Vol. 116, 1Ir 2, pi). 364 - 366 (USSR) ABSTRACT- The author succeeded in proving a connection of these concentrations with the littoral sections characterized by a cert_ain dynamics in the alluvium along the shore of the Anadyrskiy gulf (Berirg Sea). Ile mineralo.-ically analyzed the alluvium-fraction 0,1 - 0,05 mm from certain depths (2-) m) in imme rsion-li quids. This fraction vras in bromofor..1 (specific gravity 2,9) SUbdivided into a heavy and a li-lit subfraction. The heavy fraction (avereee content 14,5 %) visa Microscopically investigated. A uniform complex of minerals was found to exist in the entire region inveoziga-ted. It containeds 1) weathered and opaque non-ore minerals, 2) opaque ore minerals, pyroxenes, 4) brown hornblende, 5) green hornblende, 6) epidote, 3 7 zircon, 8) apatite, 9) garnet, 10) chlorite, 11) sphene, 12) ru- ~ tile, 13) syllimanite, 14) zoisite, 15) staurolite, 16) leucoxene, 17) biotite and 18) disthene. Characteristic is the aLriost complete Card 1/3 absence of metamorphic rocks.The uniformity and the composition of 5 1;'0'0 Some Condition3 of th.E~ 11-irire k1lu- vi Um the matarial accordilIg to its hydraulic ~;iz~ takes pi.~,ce here at the bond of the Coastal line. Lar-er cr heavier parti-les ;-,rc- moved along the shore by the wave.3. Si%allcr an-11 1-J,,ht,--r are Wa."Ited dcan into tho dal;t1i. llk-aliiov j cticlni %ri,, alio under the influence of theoi! riotiono in O-c coastal zone. Bla8e,! on these facts the author formulates a .-eneral aentence as follcazl: The concentration of the especially heavy r:,LLterials in the litto:r.--.'-' alluvium takes rlace where selectivu processles accordir.- to th~3 hydraulic size are possible which ar--~ due to certain features of the dynamics of the shore. Thera a-ir-1 3 fi.r,urej, anj -9 references, all of ,,,hich art. SI-Lvi- ASSOCIATION: In3titute for AN USSR (Institut okeancluz,rii Akade~,ii nauk :3',33R) PRESENTED: April 0', 1~57, by D. I. Shcherbakov, SUBMITTED: April 2, 1957 AVAILABLE: Libri--ry of Con~,ress Card 3/3 A Study of the Concentration Processes of Heavy SOV/20-123-1-41/56 Minerals Relative to Exploration for Coastal Sea Ore Deposits structure of the mainland near the coast, i.e. the occurrence of rocks which contain the necessary components. B. The most essential question concerns the conditions of ccnr-entra- tion of large sand masses along the beach. As a result of longshore movement of the sand and other factors, a single area of sand accumulation may represent an entire accumulation zone having a complicated, polymorphic structure. This zone includes the recent depositional pattern and a number of relic bodies (above and below the water). Each of these bodies may be a deposit containing valuable minerals. C. The question of locating areas in which a concentration of heavy minerals is possible. The longshore movement of sand previously mentioned is accompanied by mechanical and mineral- ogical differentiation, which leads to the formation of placer deposits under definite conditions. This process is very complicated and manifold. In order to bring definite areas of concentration to light, a thorough analysis of the dynamics and morphology, as well as the entire development history of Card 2/4 the accumulation pattern concerned, is necessary. The authors A Study of the Concentration Processes of Heavy SOV/20-123-1-41/56 Minerals Relative to Exploration for Coastal Sea Ore Deposits illustrate the above statements with the examples of the Beringovo more (Bering Sea) (Fig 1) and the Black Sea (Figs 2 and 3). In the case of the Bering Sea, the concentration of heavy minerals results from a differentiation of alluvial particles, always according to their specific gravity. This process is a result of reworking along the coast by waves (eg. scouring), as well as on the coastal slope below sea level. Various morphological features, such as terraces on depositional patterns, spits, beach deposits, the borders of unconsolidated alluvium and residual soils, etc., may serve as indicators of such littoral processes. On the Black Sea a movement of alluvium along the coast was stopped at a bend in the shoreline. As a result of the accumulation and repeated reworking and a--jrasion, mechanically resistant grains are separated and concentrated on the beach (zircon, tourmaline, garnet, etc.(Fig 2)). The concentration of heavy minerals is especially intensive in the surf zone (Fig 3a). Primarily, the study of all varieties of accumulation condi- Card 3/4 tions for the heavy minerals will make possible the determina- A Study of the Concentration Processes of Heavy SOV/20-123-1-41/56 Minerals Relative to Exploration for Coastal Sea Ore Deposits tion of characteristic features for use in the exploration for coastal deposits. There are 3 figures and 6 Soviet ref6fince6'.' " ' - ; ' PRESENTED: June 13, 1958, by D. I. Shcherbakov. Academician SUBMITTED: may 31, 1958 Card 4/4 SHCM. BAKOV, F.A. Lithological investigation of beach drift in Anadyr Bay. Trudy Okean.kom. 4:31-43 159- (miRA 13:4) 1.1natitut okeanologii AN SSSR. (Anadyr Bay--Coasts) NL7ESSKIY, Ye.ff.;SHCfMBAKOV, F.A. History of the development of the Fhore of Tuapse B3y during the Litest transgression of the Black Sea. Trud7 Okeen.kom. 4:127-131 l5q. (MIRA 13:4) 1.Institut okeanoloeli AN SSSR (Tuapse Bay~-Coaat changes) SHCHERBAKOV, F~A,, History of the development of the northern and western coasts of the Sea of Azov with reference to the formation of coastal marine clacers, Trudy Okean.kom. 12:17-29 161. 04EU 15:1) 1. In,9titut okeanolopii AN SSSR. (Azov Sea region--Mines and mineral resources) (Azov, Sea of--Coast changes) SHCHERBkKOV, F.A. Some data on the postglacial transgression of the Bering Sea. Trudy Inst. okean. 4e:114-120 '61. (MIRA 15:1) (Bering Sea--Coast changes) 'IT i -D'iFDD".1, V.S.; DOU'r-CV, Yu.S.; qi~~HERB~YJV-,-F.;,. --- - Some features of coastal structure and development in the south of t~-p Elaritime Territor7f. Trudy Inst. okean. 48:121_14.~~ 1 61. ( 11-11 rL-', 15: 1 ) (Peter the Great Bay--Coast changes) IONIN, A.S.; SHCHERBAKOV, F.A. Stratification of littoral deposits in the eastern part of t?~e Black Sea. .1 Okeanologila 1 rin.5:8U-871 '61 . O-URA 15-.") 1. Institut okeanologii A' SSSR. (Black Sea--Sediments (Geology)) I- 61.i-(;ffLiWAiIOV.I P.A.; FAVLIDIS, Yu.A. Characteris-I'Acs of the dis-uribution of heavy minerals in the - 0 162. oastal zone. OP,,-canologiia 2 no.4-:151-663 (1-aU 15.7) -1 J. Listitut okeanologii AN SSSR. (Coasts) (Ydnerals) w SCERBAKOV., F.A. [Shcherlmkov, F.A,I; PAVLIDIS, I.A. ~.L 11 Characteristics of the heavy mineral repartition along the 11ttoral 0 area, Analele geol geogr 17 no.2:83-96 Ap-Je '63. SHCIERBAKOV, F.A.; I AVLI. ILS, Yu.A. Bedding o-f beach sediments. -lit. i pol. iskop. no.4: 80-87 .71-,'.g 164. 17:11) 1. Institut okeanologii AN S3SR, Moskva. AKSENOV, A.A.; IONIN, A.S.; SHCHERBAKOV, P.A. New data on the structure of strata of recent coastal deposits. Okeanologiia 4 no.5:842-849 164. (MIRA 18-1) 1. Institut okeanologij AN SSSR. ,-C "T R/0000/66/000/cia/0207/0229 A'". 00V/97 Ut AU'lliUl: Shcherbakov, F. A. GRG: none TITLE: Present sediment formation on the north coast of the Azov Sea SOMC---: A~i SSSR. Okeanograficheskaya komisgiya. Issledovaniya gidrodinamicheskikh i, r.orfodLnamicheskikh protsessov beregovoy zany morya (Studies of hydrodynamic and morp,hodynamic processes of the shoreline). Moscow, Izd-vo Nauka, 1966, 207-229 TOPIC TAGS: ocean dynamics, geomorphology A3371RACT: From 1959 to 1962 the Institute of Oceanology AN SSSR conducted investigations to compare the granulometric and mineralogical composition of sediments: :on the north coast of the Azov Sea. In this area the Azov Sea represents a shallow 'basin with rraximum depths of 15 m. The coastal waters are particularly shallow (7 to 8 rn) with s~~eop waves 2 to 2.5 m high and normal drifting of sediment. The greater part of the coastal sea bottom is covered with silt and crushed shells and the primary source of sediment formation is sand abrasion. Sediment samples and sediment cores .taK.n from the beach and underwater coastal waters were compared. The following granulometric and mineralogical composition was foundt Card 1/2 ACC NR: A17001797 Fraction, mm > 1 1-0-5 .5-.25 .25-A -1--05 Md So Heavy fraction Content of continental sands, % 19.2 31-2 33-5 13-9 2.20 -50 2.17 1.0 Content of underwater sands, % 20.0 11.4 23.4 44.8 5-31 -Z5 1.70 1.6 under-;ater sands of this area are on the whole finer in size, better graded and contain more heavy minerals. These differences are largely attributed to -waves acting! on the sea bottom. Drifting of sands and formation of sand bars are described. Orig.: art. has; 7 tables and 6 figures. SIM CODE: 08/ SUBM DATE: 17Apr66/ CRIG REF-. 008 Card-2/2 SHCHERBAKOV, G. Jew collective agreement has taken eftfect-. Mast.,agl. no-4:13 '59. (14IRA 12 :6) 1. Predeedatell shalchtkoma shakhty "Rw~nichnayal' kombinata Kizoluiml ' . (Coal mines anI mining) AUTHOR: Shcherbakov, G. 107-5 e-7-2C/47; TITLE: Ar. Electromagnetic Pla~,,i-detector (Elektrcmagnitnyy defek-~-Is- kop) PERIODICAL: Radio, 1956, Nr 7,, pp 27-20 (USSR) ABSTRACT: This is a device for detecting flaws and cracks in magnetic objects. it consists of a pick--,.zp, amplifie-r- limiter and grid-rectifier with e-'e?tronic stab11-izatiGn. Tt is fed from the '127v or 220-T grid with a consumption of 90 watts. The circuit d_4aEram is snown in Figure 1. Sinusoi.-al oscillat4-ons at a freqlzency of 1,150 cps are Eenerated by a triode and fed to -he magnetic indu,_.icr cof' of the pick-up. The pick-uP 's designed to react sh_arply t:~ a crack in the ferromagnetic object being tested, which causes a change in the magnetic field above the crack. There_ is an air gap of 1.5 mm between the pick-,-,- and the test :,b- ject so that the type oil surface has no ~:,ea. effect on the detection of crack. Secondary coils in the pick-up recGi-:2 an induced emf, modificd by any flaw that may be p-resent in the test object, and are fed back tr% the amplifier limiter. In the output circuit of the amplifier are the in,134-cating Car,~ 1112 irstru7ent-s - microammeter and neon -,ube - and a set o-" r r d Tii e ,u I ~;e a:_! I i~ ::,-I:- ~he c_- --nd de:~reases ~n f I i t a i e a e C 1-1 z d f e I i f I u Z S r r i ea C, n n ZI r i n E s S C 7 d 1. Fu I is c c i~ a 1. Ferromagnetic materials--inspection 2. Electromagrezic equipment--Appli.cations .Car SKIN MAKOV, Or.; SHBILKOVNIKOV, A. Key worke_rs -vere the smil of the s-irvey. Okhr.trda i sots. strakJi. no.1:25-28 Ja '59. (14IRL 12:2) 1. Predsedatel' obleov-profa, g.Brvansk (for Shcherbakov). 2. Glavnyy tekhnicheskiy inspektor oblsovprofa, g.3ryansk (for Shelkovnikov). (Bryansk Province--Industrial hygiene) YZRCHUK, V., slesar';RAZIKA.LOVp, V.I. slesar'; CHUFISTOVA, G. (g.Kostroma); .SHCHERBAKOV,-61.-(g.Vologda),~ On friends and comrades; readerif letters. Sov.profsoiuzy 7 no.g: 33-34 My 161. 1. (MIRA 14:10 1. PryadilInaya fabrika kombinata "Baltiyskaya manufaktura". g.Tallin (for Yarchuk). 2. Zavod imeni OktyabrIskoy revolyutskii, g.Lugansk (for Basikalov). (Trade unions) /JD, 1-210 S/l26/6o/oo9/o6/o16/O25 AUTHORS: Varich, N.I., Belousov, N.N~OKa/dEgRgherbakov, G.I. TITLE: Influence of Plastic Deforglationi"On the Structur and Properties of an'lAl-Mg'~I~klloy PERIODICALt Fizika metallov i metallovdeniye, 1960, Vol 9, Nr 6, pp 909 - 917 (USSR) ABSTRACT- The aim of the work described in this paper was to investigate the influence of plastic deformation of cast and hot-pressed specimens on the changes in the mechanical prop ties and in the sub-microstructurei'Yof a new alloy 1~~r8o-Xontaining 11.5of MgI 0.14% Be, 0.10' Ti, 0.1%` Zr, rest Grade AMOOO aluminium. Ingots of this alloy were produced in a 120 mm dia metal mould, applying by means of a piston a specific pressure of 1300 kg/cm 2 during the process of crystallisation. The thus-produced in-ots were heat-treated (soaked at 43,5 0C for 20 hours and subsequently quenched in hot ;-rater'). One batch of the specimens were investigated in the cast and heat-treated state, A part of another batch was subjected to cold- Cardl/3 working to the extent of 25, 50 and 75~o; a second part of this batch was subjected to hot pressing at 420 C +11" 80888 S/l26/6o/ooq/o6/ol6/O25 Influence of Plastic Deformation on thEeOWEUNar. and Propert�es of ail Al-Mg Alloy There are 9 figures, 3 tables and 4 references. 2 of which are German and 2 Soviet. ASSOCIATION: Dnepropetrovskiy gosudarstvennyy uni-versitet (Dnepropetrovsk State University) SUMMITTED- October 10, 1959 Card 3/3 ACCESSION NR: AT017178 the high-melting elements Be, Zr, Ti, and Mn, application of plunger pressure dur-4 ing crystallization decreased the differences In the permanent crystal lattice parameters and hardness at the center and edges of the ingot. Orig. art. has: 4 figures and 6 tables. ASSOCIATION: Fiz.-tekhn. Institut, AN BSSR. (institute of Physics and Technology,! AN BSSR). SUBMITTED: 19Apr63 DATE ACQ: 06Mar64 ENCL: 01 SUB CODE: MM NO REF SOV: o04 OTHER: 000 Card 2/3 s/1,;9/63/000/00-1/01.5/027 v_20;_/Z592 AUTHORS: Ueloti5ov N.Y., Varich, ".1, Krivusha Yu.V. And Sliclserbakov G.I. TITLE: Cortnin mtruettiral cliarac t criq ties rind propertiei of alloys crystallized under piaton prosstire PERIODICAL: Izvestiya vysshiklt uchabity!c1i zavedeniy, Fizilux, no-1, 196-31, 92-95 TEXT: The effect of piston pressure on the hardness, lattice parameter and size of the mosaic bloc%s in the alloys (AL8U) (11. 1% Mg, 0. 1,1~; Be and 0 - 1.5% Ti and Zr) , A41 I (AL2) (9.84/:'; Si and 0-175,' Fe), AL9 (-/.O~'O' Si, 0.27" rind 0.=~ Fe), and Mn rind 0.15;j' Fe) is discussed. a AL4 (9.3;~; Si, 0.32 Mg, 0.25;)1 The alloyA were crystallized under atmospheric pressiure and un er )iston oresstire; the last three rnnginL: froln 300 to 6ooo kg/cm nd the first on(- in the preti.4 tire. ra nge of 1650-9425 kg/cm-., Samples were cut out from the ingots radially and the Vickers -1) (TP). Tie X-ray hardnesi~ measured on a sclerometer type I lattice determination was carried. out in a camera type (KROS-1) xising copper radiation. The dimensions of the mosaic, ~j i Card 1/3 Certain stroctural characteri:~;tics S/139/63/000/001/015/027 S202/Z592 J blocks were determined from primn'r.,~- extinction and the intertsity of the interference maxima wa:t~ deterniined photographically. The ctions of the blocks irere calculated according to G.M.Voroblyev,' dititen, Method (Izv. AN SSSR, ser.fiz., 2.3,, no.5, 1.959) The hardness and attice parameter were dater-mined also foi- the trnnsitional zone. In the case of AL3U, the hardnes!:, did rat change along theedges of them ingot while it increased con'Tc-ritZ.1y in the center. With pressures in excess of 3000 kg/cm tha' Growth of hardness ceased. The experimental data shoured that 'crystallization under piston Pressure reduced the dintensions of the'coherent scattering regions Block vtere subdivid(!d nzio_;t vfrollgly at pressures up to 2500-3000 k /cm further increase of nre.-3suve did not affect their 9 a paramete:r' dintensions. The increazFe Of DrOSSUre reduced the lattic Particularly in the center iind in, the transitional zone, which was V~ nscribed to decrease of the magnesitim content in the a-solid solutioD. The increase of harrine.ss, in the center of the ingot was 1- by subdivision of the; m6saic blocks. However, sub.-- Z accompanied did not affe division of the bloc%s at the edges of the ingot ct the hardness. This was due to the (-ffect of thd distribution and j dimensions of the P-phnse particles. In the remaining three alloys, Card 1/3 Cc rti I. n i tmicturrt I cliarncteristic.-; 5/139/G3/000/001/015/027 E202/Z!592 th hardnesn increased contirmoitsly irith increasing pres-sure, with the exception of ALS), where the increase ceased in the pressure range of 500-1500 kg/cm2. The dizeRsions of the blocks within. the presriire ra.nge of 300-2000. lcg/cm- substantial1v decreased. It was not possible to observe the behavior oft Athe former at higher pressures since blocks c~maller than 10 cin had no effect on the intensity of the X-ray iziterference.- In AL2, AL9 and 2 AL4 the lattice parameter increased at the low presstire of--300 1q9&A 2 -1 gher pressure and then rapidly decreased at 1000 kg/cm 11i _t caused slight increase but in the region of 3000-60bu lcg/cm there: was no change in their parameter and its value was substantially the same as for pure alumin-Jum. These phenomena were explained by the general reduction of sollubility in solid solutions during; increased pressures. There are 5 figures and 2 tables. ASSOCIATION: Dnepropetrovskiy gosuniversitet imerli 300-letiya vassoyedineniya Ukrainy s Rossiyey (Dnepropetrovsk State University imeni 300-Years anniversary of union between the Ukraine and Russia~ SUBMITTED: October 30, 1961 Card 3/3 USSH/Dis,j-As,~s -f Farm Animal~; - Diseases Caused by Bacteria R-2 and F"angi . Abs Jc--)ur Ref Zhur - Biol., Mi 14, 1958, 64631 Author Lonshkov, G.A., Shcherbakov, G.P. Inst Title &,pur-iment in the Hypozrirmnuil.zation of Steers with Rreci- -pi'tated Antigen for the PLar-posc of the Production of Serum Againat Swine Erysipclas. Orig Pub Inform. byul. biol. prom-sti. 1-957, No 2, 17-19- Abstract No abstract. C,-,: d 1/1 S116,116110031001102010A2 B006/BO56 AUTFORS: Sokol'skaya, I. L. and Shcherbakov, G. P. TITLE: Study of the effects of a strong field in autoelectron emitters-cadmium sulfide crystals PERIODICAL: Fizika tverdogo tela, v. 3, no. 1, 1961, 167-175 TEXT: The authors set themselves the task of directly measuring the voltage drop occurring on a CdS emitter when taking off the autoemission current, in order to study the effect produced by voltage drop, and carrier g~~neration upon the autoelectron current. A study of the derendence of the volta-,e drop on the autoelectron-emission current flowing through th= emitter under various conditions (temoerature, exposure) permits not onlj a quantitative consideiation of the effect produced by voltage redistribu- tion uron the volt-amp6re characteristics of the autoelectr-Dn current, but supplies also data c:)ncerning the effect of a stron6 field in CdS. The voltage drop on the emitter -.,,as determined from 'the delay-curve threshold of the autoolectror cur-rent from tjie emitter to the collector, i.e., 'L.rom the positive pt-,tential on tLhe collector (with res'vct to t1he emizteP' 'it Card !/6 S1181161,11)0:~100110201042 Study of the effects of a strong... B006/BO5' 0 C~ which a current occurs in the collector circuit. The lcz~nd scheme of the experiments is shown in Fi,--. 1, the circuit diagram in Fig 2. Thi emitter was a 1-7 mm. long CdS crystal having a cross section of 0.~-O.i mr. , whiA had been subjected to electron bombardment and strong current -Dulses before the r.-,easurements. Investigation of the dependence of the voltage drop &Vk on the emitter uron the autoelectron current ia showed that in all cases tkVk increased monotonically with growing ia. The temperature and exposure effects do not change the curves, but only their position; thus, the &Vk values are hi--her in darkness than when exposed to light, and they are higher in Col. than in heat (measurements were carried out at room temperature and at the temperature of liquid nitrogen). The '&Vk values were about 100-250 v; some high-ohmic CdS crystals attained 500-600 v in darkness and at room temperature, and at nitrogen temperature they attained 2000 v and more. Also the ia dependence of the voltage drop between probe and the tip of the emitter showed the same (non-linear) shape. The voltage drop between probe and emitter base, hither, was found to increase linearly with ia (at 3000K); at 930K, also this curve had the usual ron-linear shape (steep rise at small ia values; quick flattening; at high ia values, ne.9rly linear course). At room temperature and in the dark, &V was also a linear k Card 2/6 S/18 61/001/001/020/042 Stud.,- of the efflt~ct o-f a strong ... 3006Y30506 function of the anode voltage. Furthermore, also the heating of the emitter by the autoelectron current was investigated. UP to ia = jo-7a, the emitter practically was riot heated at all, from 10- 7 to 10-6a quick heating to -1500C occurred, after which heating was slower up to 2000C and, finally, thermal equilibrium was established. An investigation of the effect produced by tlio voltage drop of the emitter upon the volt-amp6re charac- teristics of the autoelectron current showed that the latter was only slight. Th,~ lz.st part of the paper reports on the effect produced by a strong field in the emitter upon tile volt-amp6re characteristics in the case of exDosures of varying strength. The volt-ampe're characteristics are characterized by the following peculiarities; 1) all three have a break, whose position shifts with decreasing exposure toward lower current intensities; 2) xith increasing exposure, the current intensity grows; 3) the exTjosure dependence of the current decreases at Ki-h voltages. Al. I. Yelinson is mentioned. There are 10 fi&-ures and .0 references: 3 Soviet-bloc and 2 non-Soviet-bloc. Card 5/6 5/1 a 1 /6 1~`/00 1102 Q04 2 Study of the effect of a strong ... B0061B"~:-' ~'o ASSOCIATION: Fizicheskiy fakulltet Leningradskogo gosudarstvennogo un~verniteta (Division of Physics, Leningrad State Universi- ty) SUBMITTED: May 31, 1961 Card 4/6 33341 S//16 1/ 62/004/00 1/007/0-52 gl /a, B102/B1j;B 4/-3,, /-3 AUTHORS Sokol Iskaya, I- L.., and Shqherbak-ov,-G---P-., TITLE Exnerimental verification of the cause of nonlinearity of the voit-ampdre characteristics of autoelectronic current in CdS single crystals PERIODICAL% Fizika tverdozo tela, v. 4, no, 1, 19062, 44 - 51 TEXT: A method described by the authors in an earlier paper (FTT, 3, i674 19061) was used to demonstrate that the nonlinear increase in autoelectronic current observed with semiconductor emitters may be attributed to carrier multiplicatior, The volt-ampere characteristics can be divided into three sections- (1) strong fields, raDid increase of current, rate of increase inversely proportional to illumination intensity; (2) medium fields, straiEht sections, running in parallel for different illuminations; (3) weak fields, current drops with voltage,accelerating as illumination intensity increases, These three ranges were studied separately. In the first range it was found that the carrior concentration was independent of voltage up toAV k = 160 v, Below this, Ohm's law was valid; above it, Card I'L 1 /~3 S7181/0/'2/004/001/007/052 E.xperimental v"_rification of, B102/B138 however, the carrier concentration rose according to the law a(AVk-160) -3 " 1 -10 v Measurements of n/n and 4/1 in n = n0e a 4 0 0 deDendence on Ua (anodic voltage) confirmed the relation expected between field-.induced carrier concentration and autoelectronic current, and showed that the nonlinear increase of the current is really due to this eff ect In the ran,-e of medium fields the current was proportional to the illumination intensity Li i a = const L and to the carrier concentration n: ia = const n. In the ran.-e of weak fields Ohmis law is also val-:d and i 2 or the characteristics 1, 2, a ~ev`at`on from i /n, In the straii-ht course is; however, observed_ This deviation is explained as follows- Transition from the weak to the medium field ran-e parallel characteristics) occurs at anodic volta-es which increase with L~ At low Ua the autoelectronic current is almost inde-Dendent of L~ These facts can be explained on the assumption that the additional -growth of i a in the weak-field range is due to an increase of electron energy unde_~ the action of inner fields,, Since 41a is proportional to the electron concentr-~tion Card 2/3 33 3L -L S/181/62/004/00-1007/0q~2 Experimental verification of- B102/B-:38 near the surface, n = n oo ( C + 1) with C = F/4e(2nkT) n V-n n 00 1 00 00 is t~)(-, volume concentration, F is the external field streni~,th and ~' is the dielet!t.ric constant.. In ---jeak fields and with low electron zoncentra Lions, the illuminqtion-induced increase in concentration is coMpensated by a decrease in band inflection. 'Nith increasing internal fiel(i the electron gas is heated, no compensation occurs and the electrons can pass more easily throuah the barrier Boadening of t~e distribution function reaches a limit at AVk 15 - 20 v, therefore at medium field strengths i n, From LV 150 200 v carriers are generated by the strong inter- a" k = - nal fields, n increases exponentially with AV k and ia increases w,.th !/u more rapidly than exponentially. There a-re 9 figures and 4 references! 1~ 2 Soviet and 2 non-Soviet., The reference to the En-lsh-language publication reads as follows- R. Stratton., Proc, Phys, Soc., B68, 746, 1955, ASSOCIATION.- Leningrsdskiy gosudarstvennyy universitet (Leningrad State University) SUBMITTED; Card 3/.3 . July 6, 1961. 43126 S/1 a 1/62/00i~/O 1110261049 B1 25/B1 806 AUTF%-"RS: Novikov, B. V., Sokol'skaya, I. L., and Shcharbakov, G. P TITLF,: Fine structure of spectral dependence of the autoelectronic. emission from CdS -nonocrystals PEPIODICAL: Fi--ika Iverdo6o tela, v. 4, no. 11, 101~',2, 3240-3243 TEXT: -,he fine structure of the electron sp'ectra were studied in order to elucidate 3tructures which snow analogies to tr.e spectral distribution of piiotc,coro'iuctivity, also to obtain fiew data on autoelectrorLi4c emission, and ,X 4 t ,~ to co-,.pare the data I . those of photoconductivit In -.he experiments, a Y.-9 :,'diler-ty,pe electron j~,enerator with a vacuum of .1110 mm Hg was used. US Cfy3t,~i'L~3, i,.i.;,,surinE ;-C.5-0.01 imr.1, werf, us'ea as emitters with no special impuritics introduced. To restore the photosensitivity oC the cr tals which was lost at 4800C in 'he de6assing process they Y-ere bombarded with -electrons of 1.~ kev. For working at loY temperatures the thermal equilibrium of the crystal temperature was established at 85CK wish the aid of liquid nitroi.-en. Q A monochromator wit fi a dispersion Of 45 A/mm and a spectral slit of 2-6 . -was us,!d to illuminate the entize crystal Logether Card 1/4- S/ Fi ne st ucture of s:, ec t ral . . . B12 1 6b %ith tne conl~act L-:.e autoel,_lctfonic em-4ssiol- was -.L_-s,,:red with ar. electrometr-c a:.- L) 1f f . "'he a~_-tcemisSive current of t,-!,- o-der of i 0-12 to 1G_- -n~_ ~~bsor-,,tion e-e at 8"-- ~cr ~wc -it 01,4 eat ons C)" r s,_.z:cL o t:;,2 cr~ :t -;-,tails C-axi s. :,ese curves clearly r,21V~al ed :L i r L G f a'.; t -3 ee c t ro n ie at i s s J, o n *x i. c h c o r r e sn o a d t o -a x co r, absorpti or, ', i aus , 'out n- ere observed . To elim" nat.- ~~ossible exneri.:.ertal -~Ivrors, CaS cr-.Stals were studied in fi%rt. diff'~__-ent apparatus. It is conclud~~d -_'-.at tne c.-.a~~.-,er of t':,le abscrotior. is 4-e to tne specific -._-turt: -f autjelectron e::~issior, or, .--.ore :-r3 .--, aIb Ito t.--e ellectron bombar-47-nt and ~xc~-ssive '-_atine In 'he vacu-im. .Vr. tne ot'-er hard, receated bzm'-_ard%.t:nt did ~i-_-t c-anEe the i)ositions of tne c:.citon minima. Photoconductiv*t,, and autcelectronic emission sPectra studied on the same US crys'al i-_--ve,aled -:,uaiitative -,~reement but a very shdruly expressed xi- -t mum of tile :,-:-.(_1toconductJvit~- current. Autoelectron-c absorption maxima obtained unuer 2ertain conditions at A>t where no exciton lines exist, eage and w"-re or quenched by IR light. The appearance of Is attricuted to illumination and plate volta&e conditions. are ~,rov-*13.'onally explained 1,y the following hypothesis: Card 2i"i Fine structure of spt-ctral... 5/101/62/004/011/026/049 B1-25/Bia6 the ini,omot:eneity of conductivity resulting from the strung field effect is experienced by the emitter point earlier than by the rem-gainder of the cr -ence it Lzenerates a strong local field in certain parts of the crystal and consequently also a volume charge which is capable of Mating. ~ ma y occur i osc~ -L 'he electrooptical effect which n the region of a stronf, field (L. V. Keldysh. ZhETF, 34, 1138, 1958) may possibly cause tiit-- excitation of electrons by light with A~,-A edge' These'electrons may diffuse into other pt~rts oi' the crystal and may amplify the auto- electronic current. In this respect, the action of IR light is eaual to that of visible lie-'nt. Ts'-.e possibility of electrons being overheated in the strong field reClon and of non-equilibrium'electrons diffusing into adjacent parts of t*re crystal is not excluded.. There are 4 figures. ASSOCIATION: Lenirgradskiy Eosutiarstvennyy universitet (Leningrad State University.) SUBMITTED: June 26, 11962 Card 3/4 SHCHERBAKOV, G.P.; SOKOLISKAYA, I.L. Experimental study of the energy distribution of field emission electrons from CdS single crystals. Fiz.tver.tela 4 no.12:3526- 3536 D 162. (KRA 15:12) 1. Leningradskiy gosudarstvennyy universitet. (Field emission) (Cadmium sulfide crystals) RYBIYEV, Igor' Aleksandrovich, doktor tel-,hu- muk, prof.; FROVINTEYFVY I.V., kand. tekhr,. nauk, retsenzent; SHUMBAKOV, G.S... red. [Technology of waterproof materials] T-ekhnologiia gidro- izoliatsionnykh materialov. ,'oskva.. 1~;sshaia shkola, a964. 304 p. (MIRA 17:11) 1. Rukcvodi--,ell laboratorii gidroJ*Lzc1ya--,,sior-rWkh mate- rialov Vsesoyuznogo nauchno-issledovatellskogo instituta stroitellnr~kh materialov (for Provinte-vev). SH~- EINELI , Gec)rgiy Kbristianovich; KARNEYEV, V.A., red.; SHCFMR.BAKO`V, P.S'.-,_:~ed.; VORONINA, R.K.0 t9khn. red. - [Load-lifting machinery] Gruzopod"emnye mashiny. Moskva Vysshaia -hkola, 1963. 269 p. (MIRA 17:A C n nau k U *-'c isey .y ay :77 Vaod I 'yov -ich, rf :t~ I U~ ly rec, V. V. Ark' :'-,:k-.,a, 7: SHCHEUAKOV, G.V. Method of studying deep wells an the basis of speed of restoration of bottom hole pressure after cessation of wall pumping. Neft.khoz. 34 no-3:32-37 Mr '56. (MIaA 9:7) (Petroleum engineering) TRRBIN, F.A.; SHCHRRELKOV, G.V. ' - Analysis of methods for hydrodynamic studies of wells. Beft.kbbs. 35 no-3:22-30 Mr '57. NLRA 10:4) (Oil wells) (H7drodymamics) t4 cd SHCHERBAKOV, G.V. Hydrodynamic method for determining parameters of anisotropic layerg. Trudy VNII 12:272-280 '58. (MIU 12:3) (Oil reservoir engineering) SHCHERBAKOV, G.V. Calculations of well yields and importance of rock permeabilit7 based on oil-field hydrodynamic data. Trudy, U11 12:281-291 '58. (MIRA 12:3) (Oil reservoir engineering) AUZHOR: Shcherbakov, G, V. 93-58-3-12/17 TME: Some Factors Af feet,:Lng the Pressure Build-up Cu--ve of Wells Ope--ated W~.t~i Deep Well Pumps (Nekotor~-je faktory, vliyayushchiye na, khod krivoy vosstanovleniya urovm7ya (davieniya) v nasosnoy skvezhine) PERIODICAL: Neftyanoye khozyaystvo, 1958 SR) I Nr 3, pp 47-52 (US ABSTRACT: The author presents a quantitative evaluation of some factors which d.:~stort the pressure build-ixp curve of ve2_1 s cperated with deep well nums. This study is based on the works of C. Fasso [%f 1) an 'd A. L. Khayn [Ref 3, 4]. Fig. 1 presents a pressure build-upeurve in case of mamentar-y hall-ting of the deep well pump. Fig. 2 presents a test well surrounded by other wel 1 s. The data on the effect of sla:neound-lng wells on the rressure build-up c,02-ve of the test well is S--*-.-en in Tables 1-2 and graphically presented imm Fig~ 3-4. Pressure build-up curves for an isolated test well and for a test well surrounded by other wel-Is are pm-seated in FIg. 5. Me author analyzes the data on the pressure build---p cu---m with the atd of fornmlas. The author Card 1/2 Some Facto~~-s Affecting the aaflld~ixp (COM'. 93-58-~;-12/17 concl&r~z ULat the -valllles 2_rinn,~%-7, P_~; iii this sti-, wi fac ku e the UL il ~et analysis af pressrre build 11P F-j-,d '~_t Possible to COUTP-re the- oreeticE-ul res~~Llts with fi&2.0 2 tables, and rcfl-,r.-;.m(;~:.q of 3 ez-,-e Soviet and 2 ltaMan.. AVAnAMF,: Congxr.,ns Card 21/2 TIUBIN, F.A.; SFICHERBUOV, G.V. Simplified method for interpreting results of pressure rest-oration in wells taking into account fluid inflow, after their depletion. ITeft. khoz. 36 no-5:37-41 My 158. WIRA !1:6) (Oil fields) TREBIN. F.A.; SHCHERBAKOV, G.V. Instructions for using a simplified method for the interpretation of the results of uressure restoration in wells considering the fluid flow after the shutting in of the wells. Neft. khoz. 37 no.1:55-57 J.a '59. (MIRA 12:3) (Oil reservoir engineering) LI TUY-SHAN [Li Yung-shang]; SHCHERBAKOV, G.V. Determination of the parameters of a leyer based on flow test data obtained by the use of a logging cable. Nauch.-takh. sbor. po dob. nefti no-15:77-79 161. (MIRA 150) 1. Vsesoyuznyy neftegazovyy nauchno-issladovatellskiy institut. (Oil well logging) SHCHERBAKOV, G.V. Russian and foreign data on the use of formation testers. Nauch.-tekh. sbor. po dob. nefti no.15:86 161. (MJRA! 15:9) 1. Vsesoyuznyy neftegazovyy nauchno-issledovatellskiy institut. (Oil reservoir engineering) ZERCHANN-OV, Igor' Konstantinovich-; SHCHEWAKOV, G.V., red.; VO'~ONOVA, V.V.,, tekhn. red. - . - - -- --- ___ [The technique of investigating water-tappin wells opening up productive deposits in the Volga-Ural regioni 14etodika issledova- niia vodianykh skvazhin, vskryvshikh produktivnye otlozheniia na territorii Uralo-Povolzhlia. Moskva, Gostoptekhizdat,-1962. 77 p. WIRA 15:4) (Volga-Ural region-Oil field brines) STEFIN, I.G.; SHCHERBAKOV, G.V. More accurate data on the geology of the D II and D5V layers in the Sokolovogorsk field iMIuding the resuits of the hydrody- namic studies. Nauch.-tekh. sbor. po dob. nefti no.16:3-8 162. (MIRA 15-9) 1. Vaesoyuznyy neftegazovyy nauchno4saledovatellskiy institut. (Sokolovogorsk region-Petroleum geology) KOCHETOV, M.N.; SHCHERBAKOV, G.V.; FILIPPOV, A.N. Using various methods to determine the mean values of the para- meters of a layer. Trudy VNII no.36:188-197 '62. (MIRA 15:11) (Oil sands-Permeability) SHCHERRA.KOV, G.V. Determination of reservoir parameters based on well data obtained by the use of a tester. Nauch.-tekh. sbor. po dob. nefti no.21:67-72 '63. (MIRA 17-5) 1. Vsesoyuznyy neftegazovyy nauchno-issledovatellskiy institut. r on Tif I,,, HN , 1",11111 Andt-oyovi0i; ISIVAIHWAKOV) GemincHy vindimil-ovich; I YA-KO7.11,:V, Wisilly Favlotil0i NOCIIIIi~;"3111; (TnrrT0TI,, T.A., ved. red. [Iticiromachanicul metlic.A.-, f'or the sLudy of welh; aDd l"Yoro] "lid roinekhanicheskie metoi,,, jsslt-~dovaitlia jkvazhin i I-Int"tov. Voskva, Nedra, 1965- 275 1". (1-11RA 18:5) 'a n -, f z~ e -;f zcnal "Y c' PoroL:s cli ni-id i'low towar6 e'l-s. Nauch. tekh. sbor. pc dcb. 165. 18:9) .,;,ejo3,"uzr-tT rieftegazoi7y nauchno-issledavatellskiy institut. TREBIN, F-A.; SWIIERBAKDI. G.V. =r_resa methed for testing wells based on pressu_re build-up cur~ves. Neft. !,-hcz. 43 no.9.28-31 S 165. OKIRA 133-10) SHCHCRBMV, I. Building reads in Kazakhstan. Avt.d*r. 19 mo.2:-2 7 156. (Kazakhstan-Road construction) (mlaA 9:6) :,j nzh. I ror, . i, no - or .etal , W',W', ) N 165. I.A. Ya.; G Ye. OUDYREIT Mars ard a S-OP'- di,--,-onal p, Mi n n -steel: sec, -f coal. Trudy 1--jD no.S!31-38 (MT p -ng c _A 17, 11_1 MURA17KIN, B.N., 1-hnd. takhn. nauk; SHCfFRBAKOV5 I.A., inzh. VT-I puliVerized coal feeder for pressure operation. Energomashinostroenie 11 no.6-.12-15 Je 165. (MJRA 18:7) I . - (;1*1~',~ijjj,~)V I. ;L. , ~ IT A---;PT'~ T. T . .); . 'r . 2. -.s -,i (6no) 4. Sil!~-dorms 7. Se-navtt-ng sill~worm m-oths b-i sex -iith the ail of ,. serar,~tor levice.. Dost. v sel'khoz. 1952. n. ilontl'ilv List of ?u, !an Arnessions, Librar.~, of Congress, Anril 1953, unclasq. SHCHERBAYOV, I.A. Labor productivity in the tire Industry. Trudy LIBI 39-57 '59. (MIRA 12:11) (Tires, Rubber) .t . t 7. 3AICONOV, V.P.; S.Ilicmi,!L-:-i'C~uv, I.A. A method. of obtairing titarli= carbide parzs. Titan i ego splavy no.9,.274---977 163. (MIRA 16:9) (Titaniim founding) (Ceman-i,ntitjn (Metallurgy)) SHCMMAKOV, I.A. DECEASED 1961./1 c1959 SEE ILC CHEMISTRY