SCIENTIFIC ABSTRACT YEFREMOV, G. D. - YEFREMOV, G. V.

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CIA-RDP86-00513R001962410017-0
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December 31, 1967
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SCIENTIFIC ABSTRACT
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Exam YEFREMOV, G.D., 4ots. Value of the coefficient of rock hardness from the Yoly-n coal deposit. Ugoll Ukr. 3 no.8:16-18 Ag '59. (MIRA 12:12) l.Kiyevski7 politakhnichookiy Institut. Ormov-Volyn Basin-Coal) ORMEMMI =2. M M; Mk~Eaa_- EIRMIM IIMPI-T, YEFRDIOV, G.D., kand.tel.-n.nauk --------------------------- Shaft equipment during the reorganization of deep Donets 2asin mines. Ugoll Mr. no.6:8-10 Je 160. WjiA 13:7) 1. Kiyevskiy politekhnichesl-JV institut. (Donets Baoin-Coal mines and mining) (Shaft sinking) NAM EM af-M-1 Lal". Ala KHARCHFNKO., M.I.; .?FRMOVL G._D,,, kand,,tekhn.naqk Development and timbering of cleep, mines in the Donats Basin. Ugoll Ukr. 5 no-4:8-9 AP 161. (KM 14:4) 1e Glavnyy inzh.tresta Makeyeirghakhtostroy (for Kharchenko). (Donets Basin-Coal mines and mining) _K~FkKM.L aqrg4 Dmitriyevich; HOCHERGA, N.T...~red.; KHIVORUCHKOtP., tekhn. rW. [Working coal seams,at great depths]Razrabotka ugolInykh plastov na bol'shikh glubinakh. Kiev, Goatekhizdat USSR, 1962. 143 P. (MIPA 16:3) (Coal mines and mining) TIKHONOVp Mikhail Yegorovich, kand. tekhn. nauk;jLEfM!jqV,_S!.D!..,_ kand. tekhn. nauk, retsenzent; KOCHERGA, II.T., 4pzh., red.izd-va; SHAFETA, S.M., tekhn. red. (Means of controlling roofs]Sposoby upravleniia krovlai. Kiev, Goatekhizdat USSR, 1962. 150 P. (MIRA 16:3) (Mine timbering) ME m- ?~FREMOV,.-G.D-.-O,-.knd. tekhn. nauk Hypothesis of sudden rock outburists in deep mine workings. Ugoll Ukr. 10 no. 1:48-50 Ja 166, (MIRA 18:12) 1. Kiyevskiy politekhnichesk-iy Jimtitut. TROFIM3V, Vladimir Petrovich; WREMQV, G.D,., kand. tekhn. nauk, ratsenzent; A.%NINA, G.P.(Afonina, H.P.], red. izd-va; STARODUB, T.O., tekhn. red.; SHLMA, S,M., tekhn. red. (Ways of developing the coal industry of the Ukrainian S.S.R.) Shliakhi rozvytku vuhillnoi proinyslovosti URSR. Kyiv, Derzh. vyd-vo tekhn. lit-ry URSR, 1963. 110 p. (MIRA 16:3) (Ukraine-Coal mines and mining) YEFREWOV, G, D., kand. tekhn. nauk ----------- Injection and auction ventilation of deep mines. Ugoll Ukr. 7 no.4110-13 Ap 163. (MIRA 26:4) 1. Uyevskiy politekhnicheakly infititut. (Donets Basin-Hina ventilation) ') Ri PrI, k Kfj , r . p.; y, pp, (;. k,. L~ ,jV, S'ho,--k valles In m!Aiils. lzv. vy~-. uc~ieb. z&v.,- ~:L-. no./,!72-74 164 (KLPA I. Pookovokoya lrf,,-ii Baunmna. L o81? FdT (1) IJP (c GG Wo-oW~%1-65-V66l/o1561 Ioi~ ACC NR: A ~M75 SOURCE CODE: t AUTHOR: Yefrewya_ Go -Z~* ISO ORG: RadioRhYoUP-WWuts,,Pf the Gorlk~z State University (R diofizicheskiy institut. Gor1.kovBKogo-go1uaArszvFM6go universiteta) TITLE: Symmetry relations for the cross susceptibility tensor SOURCE: Zhurnal eksperimentallnoy i teoreticheskoy fiziki, v. 51, no. 1, 1966, 156-164 TOPIC TAGS: susceptibility tennor, quantum theory, perturbation theory, nonlinear of- fect, correlation function ABSTRACT:''Some general properties of the cross susceptibility,with account of spatial dispersion,.,, are considered on the basis of the spectral representation, for a close qua um-mec9anical system cted upon by an external field. The motion of th system under the action of the field is described by a density matrix, the equation for which is solved by time-dependent perturbation theory. Rymmetry relations that are general- izations of the Onsager reciprocity relations for the linear susceptibility are derived f~rom the invariance of the equations of motion with respect to time reversal. The con- nection between the nonlinear response and -the fluctuations of quantities corresponding to the dynamical variables in the unperturbed syrtem is established in general form. The cross susceptibility of the system characterizes the nonlinear response-to a mono- chromatic field. Some of the general properties which follow from the definition of the cross susceptibility and its spectral representation and which are independent ot Card 3/2 Rz Ap6o24875 the specific form of the Hamiltonian of the system are given. The connection between the nonlinear response of the system to an external perturbation and the fluctuation of three quantitities in a state of thermodynamic equilibrium is established, in anal-, ogy with the relation between the linear susceptibility and the fluctuations in an un- perturbed system (the Callen-Welton theorem or the fluctuation-dissipation theorem). It is also noted that the fluctuations in a system in the presence of external fields can also be expressed in terms of the correlation functions derived (luring the course of the analysis. The author thanks V. M. Payn for a discuadon of the problem treatei in this work and for very valuable remarks. Orig. art. has: 37 formulas. SUB CODE: 20/ SUBM DATE; 21Dec65/ ORIG REF: 008/ OM MF: 009 2 not GLLVATSKIY, S.M.; YXYREMOV, G.K. - ---.OWbWAWAWWp$qF. Bruption of Sarychev Peak in November, 1946. Biul.Vulk.sta. no.13: 8-12 148. (MLBA 9:11) (Barychey Peak) T To a e a e S e 0 0 a e a 6 0 0 0 a 0 0,0 a 0 0 0 a a 0 0 0 0 0 9 9 0 9 9 0 0 to 0 & * e 0 0 0 *Itf-*- -0 46 46 16.6 H-JU-11-a-M -111-39 M A. VP A 6-C 0 G-H- X L- 0 Of 0-ft I I T-W " ! I - - 0 -1-- - 'ST-CM a n A of 0 1 4 . I AT too' A.,G go. "NoM 1111outs A00011 to,019 1,411"IALS ."I 004 r a get eat Oft see 646 it go L Vag (W IC A nee ist'ibre 110113-15 (1932).-Kyanite occurs In Ow Urah 002 and Karlfia In UAS.R. The are contains 60 tow 62"' MA and 30 to 330' Replacing quant by add.4 Ofb -10 0 kyanite Improved t Zitjof the porcelain. Kyanitor 0 sti 6uwdaboforsupqmfnwtor Pso *111111 700 go. 0 06. W00 00- r00 00- 00 IN14*3 "I. coot Gag 0 Of I a 4 to or I A f a o A A % , , " . I I A I A 11 1 t 0 Do Of K .19 11"r1U11*4 ad oft 0 a 0 0 0 0 0 9 0 0 0 0 , 0 0 0 9 0 9 9 * 9 * 9 go 0 r 00 'e4e, rd,-= 0 a 0 0 0 410 0 of 0 0 0 0 0 rw 0 0 0 0 0 0 9 0 0 0 0 9~6,94 - oil or. OA 0 ea gas - 04b 0 so. 0 0. 00- 00- - W V tr cr 6 Cy mr 4 KV fo me 4 to 6 ~ 6 a fF 9 0 a v a 0 0 go 0 go o" a 0 0 0 0 * 40 0, 0 0 00 0, 0 & a _440 *9 * 0 WN't V STO TIFI-F-A t AT a 161 AXO WD tIlIll 12.0 filer i ..ft A~ ~1. AUjWV4 1"19 Vale L., ii1d KWAb=dl4 V- 0. 111CULY ALV- IAL$ W US MMUFACMX 011 POT$ FOR mmTlmo orncm. cLmm - KersoiL i &04N 10 112113-18 (1934).-The conduslorm of sludin are as Milows: (1), The Introdwtion of finely cround kyanite into the asix for glamamelting " commiderably increasto the resistance of the pots to the attack of the gissa,melt. (2) The most. efffvtiyt nwthod wim that afmingprotectlyr k-rxnitecmtx an the in4de of the pot.-* (3) The thernaal stalpility at the, pots is Vcally jmrcm.%cdwbm u&X a dcow lining on a, porousbody. (4) Refrodaryclay with a high iron content may be uwd for the production of the pot bedy without affectitig the quality of the Slam. provided that-it is "uted with a ProteclivT layrr. 9'1 1_9 0 W, 0 0001901kagir Ole 0 0 0 0 0 0 9 0 9, 0 0 0 0 0 0 00000000 9 0 0 0 0*0 0 00 0 o' 00 0 m IN TV T A 1 -4- r1r-T-T-V'-a 44 a It " U It 0 0 0 0 0 0 0 0 0 0 0 0 6~6 0 0 j '000 0 ~ 0 0 0 j a a All 0 a 0 0 0 4` 0 0 1 11 11 u 11 1. R ji M v v it m A hi 12 a P 4, 41 4s a Q 0 s T V A.A 011 LV '.1 1 4 0 1 s 4 00 A -90 90 A UNN Ng hwo all-bo" -00 Os A: 'W malkhm Now flame (I xum&wn. Timiaozw 13-18 - 1034 Tbl rmdts of ;i0dirs Allared U= that: (1) Th J . ,, ou of fludy d kranits l ' hm- i l e nto the tnilt for nie t o ng pots Y 11 the tb. stsimismv of Pou to the attack of tit 11 9 , 1 4" 1001t. (2) The usant 5MCt1vQ Method wma tht ol " P"Htvtivv hyanitit C4*10 on th4 Ill" Of th ~Z ~ -00 e Pot (3 ) tbttuW It 11A of the pots Is pratly jnctft~4 h'" a &.. I= '(. -00 04 Y , us"' ON A P-Olls tmdY. (4) Refro=ct clay with a high ifou COGItUt C" 1, md fm ,he &action ( h "60 =00 0 t e put body with-t aff_.dm ths q"Uty of the " 00 a PF~W", tb,!i It W -led with a pcotcvllvv ldyvr, =00 00 00 4 00 00 h! :,Zee zoo too to 0 Olt.. $1-1 too 9 AV -0 St, . , . o u tv to 1.9 6C 9 0 R a it 91 V 04 0 4 W W 1 13 4 3 4 ff.". A. o o 0 0 0 00 0 to 0 goo o 0 0 a-00-9 egoo 00 0 q *;o a 0 o 0 o o 0 0 0 go 00 4~ a a 0 cc 0 0 0 0 0 a 0 a 9 0-0 0 0-f -* *-*T# 6COPO W--4 -0 N ALM M Oft 43 TVITI 6 !J- 0 48 -4, ty CA 0 a n 1 , , I , . l 1l -9 3-P Wife lop A.0 itit rJ161101 r 0. L ~A- A : 00"uPwy S M404105).-An W" con- 11AYWW- rentrate of kyanite *Wd kith sinterins clay was IQ at v o titi ( the r P H 14 Th b t h C i o *A i a ir . . e u on o arge was . . comp c 1j so 01% kyanite and 40% cLw. A satisfactory product was A beginning of deformation under load was 00 *ft at 1425". and tht water absorption. The faing v00 0 temper ture vttmt therefore beAtigher than cone 14. : Kyanit shotdd be finely ground (n 3 mm.) and the firing 00 09-- of kyaulte must be done in, kyanite iaggers at the tempera. 00 0 ture of firing of the fi nished proeuct. Kyunite masws can be used as protecti ve coutinjea. The clay content in 1, the masses should he lowered. :06. 41. 410. : Go- 144445 At GOT 40% a, ; a, a It K 0 0 0 0 0 0 0 6 9 0 0 e a 0 0 0 0 0 a 0 * * 0 0 0 0 00 0* -SW-40cit -amitit 041 V n J. IN, .0 0 0 * 0 0 0 * 0 0 a 0 0 0 0 0 0.0 0 0 0 0 esesooo Ole'* 0000 a 00 0 0 as 90 : Goa G~fA W-S, -. *004646400*000 Sol$ 1 0 W fl 12 11 m Is U I I a a JR4 9IS 34 16 v 4 a 41 a AS 0 Oka IA 1 4, I-Ij 8, m r 4 J- 4 1. J It -fi- ot 4 ---- -- job pot-colsts S-6 P6101441.16 mail oot 00 00 a 0 at 41 Comak Pal po OIWXPOFW.4. no. 1. 33. 100 MM CUbe dmm -of VIM thtWxh a Pmvkin man derresied the makure content :,a 1*-- -004 I hr.; the cuad. then dtaramed greatly. BIVIIII-Wts cmN be obtained by adding ekorolytepi -110ciallY NaCl, the mpoisturt. content being thus tvducW to about "0%. wee P. R. F4#,fanaw*v =so :OW too 2 goo no* see woo CIO* AL A S a - S L A SITALLUINGICAL LITINATUNII CLASSIFKATICIN INS* N.SAI: sojamo .1. Ole miuricootj fliAll 601 Q-- Ift 9 1 V, I ZIA Etu a AV po .1 "1 a, a, ; ; I X, a, .1 11" ;11 ; I,, ; a L I a ad 0.4 0 104 OT11,41 0 0 0 4 : I a 4 1 ;'a 0 0 of Oie 0 0 00 9 * 4 0 0 : 0 0 0 0 0 Gig 0 0 9 0 0 0 0 9 0 a 0 9 0 0 a 41:1: 0 0 0 4 * 0 0 6 a is -----Mrv'3A ~Ivl:) W419 7,Mims Tit-Wtv Kati, 1'.11ani'Efreiitor, Rr L.7 KI) 1111017% A NIMI~ ItIMI-GRADH CnRAMIE TI "t: .,kaya Lah.. 5, -1114 1101 1274-75 (111.1n).-Thr molerl. - olitnint(I by 6311191 njumina a- the funtinmental raw- material (mutformed ItIto; cortindurn cry--tals. The ware k prepared by casting and' firiag, to coalpletc shitcring in r1ectr1ral and oil furmices at, "about 17M*. Tile %ititcrijig Is ninde poqsIble by nclfli~g.ll to 21A ofalknlinc earth %alts or other ininernli7crs fneill ing the formn(loo of cry%tals at lower temperatures. TiW materinl i% unctl for prcpnrinl, high -tvfractory crticibles,j electric fitritace Whes-uld flictmocc)UPIC till;eq. It hnia,* 7 qp 4 -*-" qqvj,:&s-A -4~ R it ~ Is It u U U 0 16 v -0 -W-Q-41 Al It 46 U-M,M ON too ssp ol~p , 061