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SCIENTIFIC ABSTRACT ANTIPINA, T.V. - ANTIPOV, I. T.

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December 31, 1967
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76-10-11/34 AUTHORSe Antipinap T.V., Isayev, OsV. TIT13i The Effect of the Composition of the Alumosilicate Catalysts on the Hydration of Diethyl Ether and Dehydration of Ethyl Al- cohol (Vliyaniye sostava alyumosilikatnykh katalizatorovx& re- aktaii Gidratatsii dietilovogo efira i dogidratataii etildvogo Gpirta) PERIODICALt Zhurnal Fixioheakoy Xhimii, 19571 Vol- 31, Nr 10, pp.2245-2252 (USSR) ABSTRACTs The dependence of the reaction volocitie3 in the case of the hydration of the diethyl other and of the dehydration of the ethyl alcohol on the concentration of OH-groupa at the surface of an alumosilicate catalyst and on aluminum oxide wag investi- gated here. The kinetics of the hydration of other and of the dehydration of ethyl alcohol at alumodlicates of different com- position and at types treated with lye solution was investi- gated at 400OC- It is shown that the degree of the transformatkin from other into ethylene is lower in the cage of the ether-hyd- ration-reaction by ev 1/3 than that of the transformation of Card 1/2 alcohol into ethylene in the dehydration of the alcohol. It was 76-10-11/34 The Zffect of the Composition of the Alumosilicate Catalysts on the Hydration of Diethyl Ether and Dehydration of Ethyl Alcohol ASSOCUTIONt SUBMITTEDe AVAILLBLIs found that in the hydration of other the ethylene separation does not increase considerably with the reduction of the alu- minum oxide pereentage, whereas it decreases linearly in the dehydration of alcohol. There are 13 figureat 2 tables, 7 Slavio references. Moscow State UniYersity Imeni M,Y9 Lomonosoy (Mookoyakiy goeudaretyennyy uniyeraitet imeni M.V. Lomonosova) July 11, 1956 Library of Congress Card 2/2 5(2) cr_r~8-2-26/35 AUT11ORi Antipina, T.V. -101;P1' I TITLEs Catalytic Activity of Alumosilicates Tr4-ated With Lye Solution. Report III (Kataliticheakaya aktivnont' alyumosilikatoy, obrabotannykh ahcholochlyu. Coobshchonlye 111) PERIODICALt Vestnik Yoskovakego Untv-.-,titeta.S-r",', matematiki- mckhanikip astronomii) fitiki, Wimii, 19-%8' N~ 2,pp 197-20~ (U33R) ABSTRAM In the preceding papers [Hof 112 jthe author ahowod that the alkali treatment of the alumooilicates leads to a utrong ae- crease of the ethylene development in the dehydration of the ethyl alcohol. Now she investigates whether this phenomenon is connected with a diminution of the specific surface. By measurings of the catalytic activity and of the ,%urfacoa it is proved that the phenomenon can be only explained by a chemical alteration of the surface. Some further questions in this connection are discussed. A method of V.T. Bykov LRof 41 was used* The author thanks Professor K#V. Topohiyeva for the interest in her present paper. There are 7 figures, 1 table, and 5 Soviet references. Card 1/2 1011 Catalytic Activity of Alumosilicates Treated With 0 /5r-r%6-2-26/35 .1 1 Lye Solution. Ropoit III ASSOCIATIOV's Kafedra fizioheskoy khimil (Chair of Physical Chemistry) SUBMITTEDi May 14# 1957 Card 2/2 "I, All TIT ~)J%S IntipintL,T.V. andNorkina,R.S. 0 OV/ 5~1-4- 25/ 31 '21 T LE t ~stfil-t' A'"ToO." Aatii W' V: c. 2tiall Feroortaga lu A m inium ~,ride (Katal5tif~hoskaya 6ktL-.ro.~11 alpmosilikatov malym protment.-qm PERIODICALz Vestnik !.,oskov --koKk> ki~LIIUS 1958, N'.r 4, ABSTRACT: iw.*,~ntigated ~.hr -,)f lix difforent 12 1 a t A, 0 content. 11. is lh:wn thtt .!,;! kinetit-i-] :,-' ~o:q&-ral 1-.r, t~yl &L-toh,,! is x1..,3 equatitn cf A.V.Frvr~ 71 t? t) ~-,ange of the alt~ohol in ethylene is mout irtmuilre fv.- R 5A Al ?0 content of the ~ntslyaer. Fc.~! a arao-kirL. rf a-umera the v lataly-i activity dearoaaeLl con-.-;int. It ia stated that tt,e ne. ~W) ei~,fr.^v) A~-C:jk tne ril! ~,i t:-3i io alraller Card 1/1 catalyliz- ActiNllt.~- 's t W ", t r, Small Purc-~-ntago cf than fo~,. ;l :(~v ~7~ "ir- q-ihoi-i V..,rk for 1!0!' A! SO C I A 'I 1CN! -.it or Ij- t AA i I f K 1 ',,,A t nly SUBME."CEDI :ulf-t Card 2/2 50) AUTHORS: Antipina.- Avdonina, Ye. N. SOV/76-33-1-32/45 T1TLEt The Influence of Boron Fluoride on the Catalytic Activity of Aluminum Oxide and Alumosilicates (Vliyaniye ftorietogo bora na katalitichonkulyu nktivnon't' nHsi alynnintya i alyumo- ai I tka tov) PERIODICALt Zhu rn-a i (Us:~,O ABSTRAM The 'Influence of boron fluoride on heterof;eneouc processes was investigated leas often than that on h6mogeneous procesoca (Ref 1). lt is known that DF 3 chemiaorbs irreversibly on Al 20 alumosilicate, and silica (;e] (Ref 4). The dehydration kinetics of alcohol and the crackinp, of are examined on samples of aluminum oxide (Jn,1uoLri;i1 A111)0 and alumosilicate catalyzers (n mixtur.- I ( '6 and Sio .(.,t-OC boron 2 (00)), which were treated with 1~t ~ fluoride was adsorbed on the catalyzer in the.reactor (in connection with a vacuum plant). The kinetic examinations were Card 1/3 carried out by a method already described (Ref 5). The results "o 1111,111olice of 1,01-on "'Noritle oil the :;UV/'76-33-1-32/45 Activity of Alwiinw Oxide and Alunovilicates obtv-4inod ~-oro elnborntod by uoin~-. th(.- equation by A. V. Front (,Iiof 6). i'lic zid;orptiozi of PA,3iiwrearjes the activity of Al 0 (;.,ig 0. n () with '-driorbed - +ow 2 3 1 2 3 ".3 , .3 an incronaed reaction velocity (it' the -.iurl'ac- rewctioii, i.,,& the proportional qunntity -%~ si,owu nn lnercrir,(? from. f-4 - 0.049 to 0-r~ - 0.070 (Fig 2). The activatioii of' Al 203 and alumooilicate by BF 3 for the cattilyciu of the dehydration kinetics of ethanol is thouj;ht ao being caused by the formation of a labile surface compound which in decomposed by the reaction products. The crack tecto of cumeno took place at a temperature of 4000C and during a poriod of 30 minutes. In this case, too, a sudden activity rice of the catalyzer, caused by a BF 3 treatment, is seen 4). Thin is especially true of aluminumoxido. Card 2/3 The Influence of Boron Fluoride on the SCV/76-33-1-32/45 Catalytic Activity of Aluminum Oxide and Alumosilicates The activating effect of BF 3 on alunocilicates wan alco observed by A. P. Ballod in the laboratory oV the Academician A, V. Topchiyev (~n-t nefti A". SSS!)(Inntitute of Petroleum, Academy of Sciences, U.;SR), (report on scientific research work of the Inctituto for the year 1955). in conclusion, gratitude is exprev-sed to 11rofessor K. V~ Topchlyeva. There are 8 fiCuren and 6 soviet A6SOCIATIONt Moskovakiy gosudarstvennyy univeraitet, in. 1-1. V. Lonolio!~Ova (Moscow State University imeni M. V. Lomonosov) SU1314IT I'LD: July 9, 1957 Card 3/3 S/195/60/001/003/013/013 B0021BO56 AUTHORS: Topchiyeva, K. V.,_Wjpj-naA__Z-_Y~, Li Khe-suyan' TITLE. The Effect of the Structural Porosity of Catalysts on Their Activity and the Kinetic Parameters of the Course of the Cracking Reaction PERIODICAL: Kinetika i kataliz, 1960, Vol. 1P No. 3, PP 471 - 477 TEXT: The effect of the sizeof poreo of an alumino silicate catalyst on the crwking reaction of cumene between 350 and 5000C was studied. A catalyst of the following composition was used: 12% A120 3 and 88% SiO21 The various sizes of pores between 12 and 115 A were obtained by re- placing the intermicellar water to a different degree by isobutyl alcohol. Isoamyl alcohol or cumene. Moreover, an industrially produced catalyst and a catalyst of the type Gudri (Goodry?) were studied., The structure of the samples was calculated from the adsorption isotherm of methanol vapor at 200C. The kinetic of the cracking reaction of cumene between 350 and 4750C Card 1/2 The Effect of the Structural Porosity of 8/195/60/001/003/013/013 Catalysts on Their Activity and the Kinetic D002/B050 Patameters of the Course of the Cracking Reaction . ~/ is described very well by the following equation by A~ V. Frost; V ln(1/1-y) - a 4. Pv y. v Is the volume rate of the addition ol the' initial m-iter a n mmoles7g~hj y is the degree of reaction; a in the apparent reaction rate constant in mmoles/g-hj 0 is a constant equal to unity. log a is a linear function of l/Tj the transition from the kinetic range to the diffusion range is manifested by a break of the curve This correspondd to a considerable chant;e of the activation enerey There are 9 figures. 2 tables and 15 references.; 13 Soviet, ASSOCIATION: Mookovskly gosudarstvennyy universitet (Moscow State University) SUBMtTTED: March 23, 1960 Card 21" 3/109160/000/002/002/006/XX B017/BO67 AUTHORS: Topdiiyeva, K. V., Antipina, T. V., and Khe-guyan' V TITLE: Effect of the Pore Radius and Other Structural Characteristics of Oxidic Catalysts on the Parameters of the Course of Heterogeneous Catalyti~: Proceseps. Communication 1. Productio! of Aluminum Silicate Catalysts With Different Structural Characteristics PERIODICAL: Vestnik Moskovskogo universiteta. Serlya 2, khtmiya, 1960, No. 2, pp. 13 - 21 TEXT: Aluminum silicate catelystalof equal chemical composition but different structural chaiacteristi a were produced in experimental series. The adsorption- and structural properties of the catalysts were studied in dependence on the degree of displacement of Intermicellar water by isobutyl alcohol and cumene. Intermicellar water was displaced by isobutyl, alcohol and oumene, in the apparatus shown In Fig.l. Aluminum silicate catalysts of the composition 12~ Al 203 and 88~ SiO 2 were Card 1/3 Effect of the Pore Radius and Other S/109/60/000/002/002/008/XX Structural Characteristics of Oxidic B017/Bo67 Catalysts on the Parameters of the Course of Heterogeneous Catalytic Processes. Communication 1. Production of Aluminum Silicate Catalysts With Different Structural Characteristics produced by the method of GrozNl,,rL (Groznyy Scientific Research Institute). The structural characteristics of aluminum silicate catalysts are gl7v-en in a Table. Two series of catalysts wore produced: 1) Series with the intermicellar water being displaced by butyl alcohol at 35, 51, 81, 95, 97, and 100%1 2) series with the intermicellar water being displaced by cumene at 34, 63, 90, and 96~. The adsorptive properties and structural characteristics of the catalysts produced were calculated from the iso- therms of adsorption of methyl alcohol vapor at 200C. Figs. 2 and 4 graphically show the adsorption Isotherms of methyl alcohol vapor, the distribution of pore volumes and pore radii, and the dependence of the structural characteristics on the degree of displacement of water in the catalysts of the first series. Figs. 5-7 show the same Curves for the*catalysts of the second series, in which water was displaced by cumene. It was observed that the chemical nature and properties of the organic solvents, which displace the water from the catalysts, influ- ence the structure of the catalysts. An aluminum silicate catalyst with Card 2/3 ARTIPINA, T.V. Irfect of changes in the chemical nature of on its catalytic activity. Vest. Hook un. ji-Aa 6o. L, lafedre. fishiahoskoy khimli Mookovskogo I (Alumina) the aluminum oxide surface Ser, 2t Khim- 15 no.413-11 (MIRA 1319) aniversitsta. TOPCIIIYEVA, K.V.; AhVIIINAO T.V~; Ll KIIE-SULIN,; LEONTIYEV, Ye.A. Formation of the porous atructuro of aluninosilicate catalysto subjected to the action of surface-active agonts. Yin.i kat. 2 no.6:887-893 11-D 161. (MIRA 14:12) 1. Hookovskiy gosudar3tvonnyy univoroitet imoni M.V. Lomonosovap kh W choskly fakulltot. (Alum1noollicatoo) (Surface-active agents) I- AnIPIKAO T,V.-j- CIMHEDNIX, Ye,Mo (Moskva) Surface chemical compounds of boron fluoride on &1umimm oxide am their role in catalysis* Part 2, Zhur. fiz. khin. 35 no. 0836- U1 AP 161. (MIRA 1415) 1. Moskovskiy gosudaretvannyy universitet, (Boron fluoride) (Alumina) (Catalysis) S/062/62/000/010/00 3/003 B144/BI86 AU NIORS: Nesmeyanov, A. N., Kritskaya, 1. 1., and Antipina, T. V. TITLE: Application of adsorption chromatoGraphy when working with ferrocene derivatives PERIODICAL: Akademiya nauk SSSR. Izvestiy,%. Otdeleniye khimicheskikh nauk, no. 10, 1962, 1777 - 1703, TEXT: The formation of keto groups on the central C atom was observed when chromatographinf, ferrocenes (P). More detailed studies were made of this phenomenon in aralkyl-PI, FICH 2Ar, and in ferrocenyl carbinols, FICII(OH)R (H being Ar, Alk), chromatographed on "chromatographic" AlI)O, (FOC7 2962-54 U 0 ST 2, 9 6 2 - 5 4p 11 6. 7 - 7 1 It 2 0 3,~', by weibht) and on and kOk (KSM) xilica gal in air. The acidity of the adoorbento was determined by It. A. Benesils method (J. Amer. Chem. Soc- 78, 5490 (1956)). Al 20 3:aralkyl-Fl yielded a distinct amount of keto derivatives; bonzyl-FI, for example, yielded -15'p" benzoyl-FI uftor 92 hre contact at room temperature. Alkyl-FO Card 1/3 S/062/62/000/010/003/003 Application of adsorptioneb. B144 B166 became oxidizad only in tritces, if at all. 4ith a contact time of 120 - 200 hre, the ferroconyl aryl carbinola FICH(OH)C 611 50 F, ~'CIIOIOC 611 5) 29 and FICH(OH)CH3 yi elded respectively 92, 76.8, and 34)~- Dehydration a. ~Iuo C in an N 2strean increased the catalytic activity of Al 20 3* The degree of oxidation decreased.when Al 203 had boun exposed to air or CO 2 for a considerable time, but reducing the contact tire of FIC112 C 6115from 90 to 4 hre increased the FICOC 6H5 yield from 13 to 72,,. when air or 02 wus blown throurh,.he adsorption column. There was no oxidation when Al 0 2 3 was treated with alkali. 41hon Fe had not been separated from 310 2' oxidation of alkyl and aralkyl-PI and of diferroconyl othanea easily occurred, forminj: forricinium cations of F1 derivatives with electron-donor cubstiltuents. Forrocanyl carbinols weru dieproportionated and otherifiod. This ruaction depended on the acidity of SiO54 1,11-di-(a-hydroxy benzyl)-F' was not disproportionated, but yielded 5516 of the internal ether besides small ounts of F(COC6H5)2 and ferrocinium cations. Polyaryl methyl Card 2;F5 Application of adsorption... S/062/62/000/010/003/003 B140186 carbinols yielded other under the same conditions. Benzhydrol for example, gave 41A of dibenzhydryl ether. The oxidations described are important especially for chromatographing small amounts. The conditions and results of 41 experiments are given in a table. Thera is i table. ASSOCIATION: Institut elementoorgunichookikh soyodineniy Akademji nauk SSSR (Institute of Elemental Organic Compounds of the Academy of Sciences USSR). Mo8kovakiy' gosudarstvonnyy universitet im. M. V. Lomonoeova .(Moscow State University imeni M. V. Lomonosov) SUBMITTED: March 26, 1962 Card 3/3 NESMEYANLN, A.N.; KRITSKAYA, I.I.; ANTIPMA, T.V. Use of adsorptica chromatogMhy In workAng with ferrocens derivaUveso Isve'AN =H*Otd*khim,,n&uk no.lOd777-1$ ,#3 0 162. (NIRA 15tlO) lo Institut elementoorganicheakikli soyedinsuiy AN SSR i Moskovskiy gosudarstvennyy universitat ime H.Y.Loozonosova* Verrocene) (Chromatographic analysis) V.A.; ANTIPINA, T*Ve Kinstia of cumno cracking on aluminum oxide activated with boron fluorlde. Kin* i kat, 4 no+-595-600 Jl-Ag 163, MRA 161l1) 1. Moskovskiy gosudarstvennyy universitet imeni Lomom)sova, khi- mich&skir fakulltst. CHENNOV, V.A I ~NTIIIINA T.V. Adsorption of benzene and mothsnol on fluorinm,*d Fklum1wir. oxile, Vest.?V)ok.un.Ser.2iKhlm. 20 no.3:23,17 MY-JP 065. (MIRA 180) 1. Morkovskiy univoraltet, kftfodra fitichmskey WmIlI, CHFMOV, V,A*j ANTIPIRA, T.Vs Aluminum fluoride as a catalyst for cracking of hydrocarbano. Xine i kat, 6 nos 6al134-U15 N-D 165 (MIRA 19ti) 1. Moskovskiy goorALretvmnyy universitat imeni Imononova, khtmicheekly fakulftete Submitted December 19, 1964, SWAYNTA. Te.S.; RtMU. T.M.; DMATKOTA, A.T.; DOLGAMIOY,T.I., starshiy nauchn" notrudnik; ANTIPINA, T.I.; ROGOYBKATA, Ts.O., red.; SlRalTV, A,V,, [Agrooliantio referenoe book on Pskov Provinool Agroklinnti- chaskii spravochnik po Pokovskoi oblasti. Leningrad, Gidromateor, lid-vot 1959. 138 P- (KIRA l3t2) 1. Leningrad. Oldromtoorologichookaya observatorlys. 2. Nachallnik sektore agrometprognosoy Severo-Upednogo upravlonlys gidromet- lushby (for Deryatkova). 3. Institut geografii AN SSSR (for Dolga- : hov). (Pskov Provinoo-Crope and ollwte) POPOVAr L.A.p insh.; ANTHIPA V I '; GIUMiOV, A.N. , starshiy inzh.; PERSHINAv M.P.t tekhn,; TMNIT414~9+-Aoq starnhly takhn.i ZARINApYe.S.; TUULYA- MSTSp KhJust inthsl XMIIA, L*A.t starehly insh.; KUZNETSOVq I.V,O red,j KYPRIp T.F"j red.1 SVITINAj A.A., red.; XOISEYEV, I.N., red.j FIAUM.M.Ye.9 tekbn, red: I [Hydrological yearbook Gidrologicheskil ezhogodnik. lieningradv Gidroveteor. iso-vo. 1957, Volel.lftsin of the Baltie Sea] Bassein BaltUskogo, moriao Nos*0-3. (Basins of the Oulf of Finland and the Oulf of Riga from the Russian-Finnish frontier to the northern watershed of the Salaca River] Basseiny Finokbgo i Rizhokogo zalivov ot gosudarstvonnoi granitay a Finliandi9i do severnogo vodorazdela r.Salatsa. Pod red. I.V.Kuznetoova i T.F.Sipro.-1961- 460 ' (MIRA 140) (Baltio Sea region-HydFo-logy) (Kama Valley-Hydrology) L 31810-66 E 4A" ( I -/0 ACC NR. SOUkF~ CODS j U~ 6~~1661oj61603764~5-11 AUL1101i Blitnyuk, No Kai Kolomiyotal A, Fee, KvAoha, Za Nol Lovokaya, Go Sol PF Antipina-1- Ta~# '97 0"(',-. All-Union Scientific it -osoarch Institute of Phyt9yathology (VaoaoyumVy TITLI,t DiallWl phouj~iltos and SOURC~-': Zhurnal obshchoy Idilmil, v. 36, no. 3, 1966, 475-)00 TOPTC 'AGS: orranic 1-4iot-,phorus compouivA, chortical reaction kinetics, toxicity, plant injiiry, ohartical :%)rnthosia, ester. Azootropic rLixturo A'56T,', Nt' i'% It vas foui-A that dial',qrl phosphltnz- ary.1 nonoa31vlpho5p%:1nitqs are pr'o~"Vicocl -In hi'711 yloiiis (al.Kmt quantitativo) ImInly,,irlont of th.) torporAttiro ot Which Atho reagents are mixod. and degree of removal of hyxiroi-en chloride fro--a Ui oreaction zone, by boiling the reaction mass, cont.ninint, the reaction prodticts of Alcohol,,% idth phosphorus trichlorldo or dichlorophosphinos, An astorification catalyst (such As sulfuric acid or p-toluenostilronic acii), and A Solvent. with atootropic distilIntion of --tor. A preliminary ostimate WAS nAde of the herbicidaVactivity or sone or the tqn compotuids uynthosized. I in the tosts the abovoground portion of the plants (the kidney benn An rA ty-dical dicot and the oat an A typical monocot) WAS sprayed with mulsions of, IUBOYO V.V.; ANTIPMA, TeJ.; CMIMMt, N.N. Temperature dependence of the mWnetostriction of certain ordering alloys* love vyea ucheb, sav; fit. no.149,51 163, (MIA 1695) 1. Lqbyohevskiy Industriallayy institut imani Kuybyphovao (Hapatoatriction) (Alloys) 1 41 - -- --VOROBIYICV,--B.-L~-.-ANTIPINA,-Z.A.,-rodiiktb7r--,-Al=SANMo v-, V.10, tekhnicheekly redaktor - (Transfer pictures (decalcomania)] Pereyodnys toobrathentia (dekslikomanita). Moskva. Oos. Isd-vo "Iskusetwo,* 1952. 106 p. [Microfilm] (KLRA 7tlO) (Decalcomania) NADZWIN, Th.; ANTIPOV. A. % --womstim Through the Island of Java. Tokrug eve%& no.8:25-32 Ag 053. (Iff-RA, 617) (Jays,-Daeoriptlon and travel) - ARPIPOV, A.,jDaster We use dismountablo dumping trays. Stroltell no.50-19 Ur '59. (141RA 1218) 1. Torkhno-P~rshainakty sayod thelosobatenrqkh konstruktaly I dotaloy. Sver4lovskogo noynarkhoza, (Loading oind unloading) AIMPOV, A.0 genorAl-mayor aviatail Laninist oontrol. in action. Takh. i vooruzh. no.3:4-5 Mr '(~4. Omlia 1,1:0 1. Zwootitell nachalItLika politichoskogo upravierdya Wlcrusskogo voyennogo okruga. us is 0 a 10-1.0 0, 114-j -4-1 $-1- 8 1 - 0 as let- 4"D 041 fools% wa bill PAid 0 c 10 eaql Ail Seep" *Wlellp 91111 a" "A As".# Iql 44!44 "Ulm (in (W PO MM III *M" Aq " %VI 0`1 a" 041 Ul 11 -qv= .41 a' "a 11%).114 0101 aRI P Wa "aawy at-al it so '1 0101 M."M 464 POIS&AWO JO A"P"p in Paul son gt=- M -1 P " 'I"- "P4-4 a 'am "11104 so "ISAM IM 049 1101116011 103uw 00 Zwll UVO 01 F"FWW P" r PUM 0 I"IM 01 to so- 14w^" &MOO19.6 4141 P" RIPM 0114014WAP 80" W11 o. M 9g Io -on- 40111 Is (M) VM*0111HWIMN%l ~) Is 19111 P" wul" P *1114111" "1 " (a) =%Xturfl p, 648 111$& OH311114 441 1" 1"&s .111M "Plao "I Olk"WIP, 190 M" 101cillmu v awil"ald A 00 q) Mq $11 P" sow" "W=P, "W"M so. so. to 066446 A.A,, Inzh.; WNW, V.G., kawl.teklin.niuk; MIESHCHENU), A.F., kani.tokhn.nauk Methods of calibrating propeller shafts. Sudostroanie 29 no.10s 64-66 0 163. (MIRA 1602) r., :t: ruL Y: r yu ...... ANTIFOY, A.I., kandidat tekhalcheskikh nauk. Xffect of lightweight passage@ on resistance to seepao In foundation eoile. Oldr.stroi. 25 no.9t48-51 0 156. (Km 9111) (Hydraulio ongineariftg) (Boll mechanics) SOV/98-r)9- I o- 10/20 10(i) AUT11ORs v A.I. Candidate or Technical Scienre.4 WWUOMI TITLEs The Selection of ft Itational Subterranean Contour for Concrete Dams on Sand Foundations PERIODICALt Gi (trot ekhn i cheskoye atroitel'stvog 19599 Nr 10, pp .16-40 (USSR) AJISTRACTs The article gives a brief account of a method developed for the cnIculation of subterranean contours or concrete constructions; this is normally a very complex question, but the inethod detcrib- ed here enables such problems as the weight of the construction, the coefficient of resistance to dislAncemont, coefficient (if ero- sion, filtration pressureq pressure on the rrest of the spillway, cost, etc.9 to be solved simultaneously. Tit? filtration count?r-- pressure V . 0) where p1. 61-2-3 is the area of the provisional lay~out of the counterpressure in the form of a trianglej is the volumetric weight or the water, Oe is the coefficient perrection or the filtration counterpressure lay-out (taken to be 1.50). The rela- Card 1/4 tion between V and Lite size of the subterranean contour is expres- SOy/98-59-10-10/20 The Selection or n Rational Subterranenu Contour for Concrete Dams on Sand Foun- dations sed thust nl1(1 + 0) S 1.5 (2) where 11 ic the pressure on the buildingt I in the length of the comtilever, B is the width of the dam, and n is the ordinate of filtration counterpressure directly behind the channel. The coef- ficient of the dam's safe resistance to diRplacement in determined according to the formula K W tG - W - W1 f, (3) C 1; N where EG in the sum of the forces acting downwards( W in the sus- pending forcef EN is the sum of the moving forces htrizontal), and f Is the coefficient of erosion of the concrete in the founda- tion. The depth of impervious deposits (T) should not be less than that dictnted by the formula S f 4 0.4 when 1 >/ 3, where S in the length of the channel and b in half the breadth of the dam baset Including the front part. By using Professor Ye.A. Zamarin's nomo- Card 21/4 grnph, shown in fig.21 we find the length of the channel S to be SOV/98-59-10-10/20 The Selection of a Rational Subterranean Contour for Concrete Damn on Sand Foun- dation& and the length of the front part of the dam to be L - b n blo S1 in the case of small-scale work the use of Professor P.F. Fillehakov's tables in recommended (Ref.5). From the compact graph, providing data concerning all the factors affecting the subterra- nean contour and their cost, the most suitable ce~bination may be chosen for all kinds of dame. Two sample calculations are given in the text# one with drainage, one without, and table 2 contains ft list of the pressures combining to form the quantity n and the. formulae for their calculation. By inserting the value of the act- ing forces into formula (3), we find n to be K +K A +K A A V 'I( EN+N., (7) 2 3 4 5 0 7 - I - f 0.7511(l + D) 12 Card 3/4 The cost of the variations In given in table 3, while fig.3 shows SOV/98-39-10-10/20 The Selection A' it Rational Svibterrwienn Contour for Concrete Dams on Sand Foun- dntians the combined graph for the different variations of the dimensions and cost. The conclusions drawn are that the method described pro- vides for greater rationalization and economy in all kinds of dams, but that In class I and 11 projects it should be supported by more careful calculations. There Ore 3 tables, .1 graphs, I diagram, and 5 Soviet referencesio Card 4/4 ANTIPOV, A.I., kand.tekhA.nauk Determining basic dimensions of ground profiles. Oidr.strol, (Dams) buttress dams with flat under- 30 no,7127-30 JI 160* (MM 13:7) ANTIFOY, A.M. OW" Conical vibrator sifter with production capacity of 15 cubic motors per hour. late. I Isobr. predl. v stroi. no,7026-29 153. OloveO (Band) . (MLRA 7ilO) wt " III If I fit v '"p 41A.-Mill - 600cows &40 CA APPARAIIIS FOR PIVRIFTIVO "3t2, VAPORS, AND LIQIADS. P. go Irsahow *ad A. K. Aajjpvw* INese lI#TTO. Doe. 4. 1911. Coastruetton details met 0* 00,1 0see 00 w w 860 1, 9 00, oo 0 9 ~16 g 400 1 off " 0 2 goo &$o tt a 04tattwSatat Imefilwat ct6twFICAVOR see goo -j~ u a " 0 goo 0 0 ANTIPOV; A.N. Complications arising in deep drilling beyond the Arctic Circle. Neft,khoze 43 noo4t63-66 Ap 165. (MIRA 1814) YIVCIRAFOVp Oeorgly Konstantinovichp prof*, doktor tekh&,rAukj IOSIIZVSK11p Ley lzralUvichp kand.takhassauk, dotoWl ALWANDROV, Anatour Vasillyevich, k".tekhz.nauk.. dotsent; D6W;4Xj Nikoiq NikoUqevioh, kwA.tokhn.n&uk# dotsent; I Up Genrikh Mikhvqlovich, iazb.; CHIRKOVv Vladilon Favladch, Lush* FrInimall uchastiyet RTBIWp V.,D.j Lash.; ANTIMT, KMOFANOV, Yu.Mej, inzbo,, rateementl KARM~I--i',A,, inzh.v rbd*l UMMO, L*A,p takhnoreds of the reinforcement [Prestressed bridge girders with stratOM before the concrete is placed] 'no napriashemWe balochrVe proletiWe stroenila mostov a napriasheniem armatury do betoniroyaniia. Mookvap Vass.isdatellsko-polUT.obPedinonis H-va putei ooobahcheniia, 1962, 282 p6 - (KtRA 15t4) I* Daystvitel'My chlon Akademli stroltelletva i arkhitektur7 Sam (for Yovgrafov). (Bridges, Concrete) (Prestressed concrete) YEVGRAFOV, G.K., prof.1 ANTIPOV, A.S., inah. oper'----~- -- Results of the ation o prestressed concrete bridges Put# i put.khos. 7 no.1200-31 163. iMIRA 16t12) KIIILlN5KlY, F.A.; LMSHFV, I.P.; LFbi;PMEU, 6.i~.; SFAMil"OVA, N.D.; DORIZO, A.F.; TEM-OVAYA, K.G.; AHMOV, A.S*j obahchestv. rod.; MAK, Yu.M., toklin. red, (Gorynchiy Klyuchl Gorlachli k1luche ltdo2,, 18pre i dop. [By) F.A.KiAlinskli i dr. Krannodarsko Krasnodarvkoe knizhnoe izd-vo, 1963. 84 p. (MlHA l7t2) 1. Glavnyy vrach vanntoriya No.", hurorta Garyachly K4uch) Kavkaz (for Lobodenko). 2. 'Anntorly No.1 Kurortn Goulxhly Klyuch, Knvkuz (for Sliavkwi(va#Tornov~)ytt).3#ZarastitalI glaviiugo vracha po maditninakoy chastl sanatoriya No.,' hurorta tioryachiy Kly-uch, Kavkaz (for Dorizo). IOSILWSKIT, L*I*, kandttekhnonauk, doteenti ANTIFOV, A.S., Inzh. Results of testing reinforced boundles vith NXIIII& anchor shoes for pulsating loads. Trudy KIIT no#126t68-8) 160. (HIIU 13: 10) (01rders-Testing) ANTIPOV, A.P., otv.red,; XALAGMUKOV, Y.P., takha.red. [Traffic regulations for care and pedestrians on streets of cities and communities, and on highways of Moscow Province] Pravila dvishemija transports i peshekhodov po uliteam gorodov, naselemVkh puxktov i dorogam Momkovskoi oblesti. Koakvn, Izd-vo *Koskovskais provda," 1959. 94 p. (MIRA 12:10) 1. Moscow (Province). Otdal Gosaytoinspektaii i bezopasnosti, dvishanlys. (Moscow Province--Traffic regulations) CdAoi. ;11.,. 'tae I Ity Timof eyev ich ; AIC POV Androy Yoe I lizemIch [ as :eased) W3A40Y. Ifiktor Ivanovi-.h; ITM =-!!ent; 5U4-Vi~. TO.64., WVAW~PV., r4ioktor JustalliM and servicinj se-uUhing and hackling devices In flex %t,d temp MLIIGI Ustroletvo i obolushivents mial'no-tropolInykh t ~wjeleprirotovktollzWkh agragatow l1nosayodov I oonlkozsv~uy. 4c,s'iya. Goo muahno-telchn.l.-A-vo H-va logkot )rL-.;iydhl. ~;L-h. 1957. .19 p. (tiax (Tot t I 1-i i i -A ry) SXXXMXNXO, N.A., doktor takha. "uIc: YURMY, V.N., insh.; SIMLIKOVSKIT, L.W., kand. tekhas nauk: ANTIPOT. A.Y., insh. 'Thermal calculation of boiler unitag(standard method). Roviewed by CA. Sessa4nka and othores Toploonergettko 5 no, 5:92-94 W 158. (MIRA llt7) I* Moskovskiy suargetichaskiy Institut, (Boilers-Tablem, calculations. etc.) ZANWIlt 79.1 ANTIFOV# B.1 XMSANOV, Sol KOLOKOLOVAq Hol M=j P.; SWILINIMA, NWTOV, T. p takhn.rod. (city or Orel) Oorod Orel. Orelp Orlovskoe knishnoe izd-vot 1958. 122 ps (KLU 1416) (Orel-4seaription) ANTIPOVO B. The general plan of Omsk. N& stroi.Ros. 3 no.9tlS-19 S 162* (MIM l5sl2) 1. Glay"y arkhitektor Ouka. (Omsk-City planning) ANTIAN, B. A. Antlp~ 11. A IfInvestIFation of Um wit,!!r nai,no-tic. Fell it oblata ;-M-PsAds of rotAtion arvJ slort. CY111;"iers in 'a, -miforzdy alternate fLeld," Trlidy Sib. fi:~.-tmWhn. in-ta) Issie p. ~321-31 SU: U-521il, 17 Deco-nber (Leto;As 'Vim-nal ln~;kh Staf'01~') ~O* '~~51 11,9101) ANTIPOV, B.V. Paeudomyxoma of the peritoneum. Trudy mol. nauch. notr. MCNIKI noell222-224 199 (MIRA 16oll) 1. Is pato-corfologicheakogo otdola (rukovoditel* prof. S.D. Vaynberg) Moakovakogo oblastnogo nauebno-lealedovatollakogo klinicheakogo inatitu+A imeni Vladimir8kogo, AMTIPOVf B.A,; ZUYXV, Wee I. EUMILN=O. P.N#; SONCHIXg T.Ke; YZMSHIN. '~'- - T.A. 2ransparenoy of a horizontal atmospheric layer In the range from 0.7 to 14 . Part lt Squipment ard measurement methods* Ivy. Yy%.ucheb.say,;fIs& no.2t103-110 1609 (HIMA 13t8) 1. Sibirskly fisiko-takhniohaskiy institut pri Tomakom gosuniversitste In. V*V.11uybyvh*Ya. (Atmosphere--Optical properties) 82331 (3.9000 s/i5q/6o/ooo/oVoll/05 3/ AUTHORSt Antilov, B.A.1 ZuYev. VJV , faaasnenko, E.F., Sonchik,--. Y ana- 1Fe3yuskqn_,_"6 TITLE: Transparency of the Horizontal Layer of the Atmosphere \Vin the Range or M.7-14 u. Part Lle Dependence of the Total Transparency of the Atmosphere in the Range 0-7-14 0 on the Thickness of the Precipitated Layer of Water PERIODICAL: Izvestiya vysshikh uchebnykh zavedoniy, Fizika, 1960, Nr 3, pp 72 - 75 (USSR) ABSTRACTt The authors made an attempt to determine an empirical relation between the magnitude of the reduced signal V (magnitude of the signal multiplied by a factor 42 /Sj:- Li being the distance between the emitter and the receivor, Sj heing the area of the emitter) and the air humidity which would show satisfactory agreement with experimental results obtained by the authors. As sources of infra-red radiation, four special emitters were used which were heated to 500 OC14", and placed at a distance of 1210, 3494, 6645 and 9855 m Cardl/4 from the receiving equipment. The experimental set-up, 82331 S/139/60/000/03/011/045 Transparency of the Horizontal Layer ofEM/11MI04sphere in the Range of 0.7-14 p. Part 11. Dependence of the Total Transparency of the Atmosphere in tits Range 0.7-14 p on the Thickness of the Precipitated Layer of Water tits method of carrying out the experiments and the processing of the results were the same as those described in an earlier communication (same journal, No 2, pp 105-110). The air humidity and the intensity of the signals were determined simultaneously. The partial pressure of water vapours was determined directly and then the thickness of the precipitated water layer wL was calculated, where w - the thickness of the precipitated layer of water in mm for I km and L - the distance in km between the emitter and a receiver. For detecting the relation between the air humidity and the magnitude of the signal only those measurements were taken into consideration which were carried out in the absence of any visible clouding of the atmosphere (mint, haze, fog, rain).Cra total of 811 determinations ~6nly 140 complied with this condition. The experiments Card2/4 were carried out during various days in March, April, 4-'* - - 6-2-33131 -- - - - - - -- - - - - - - S/139/60/000/03/011/045 Transparency or the Horizontal Layer ofEM/fUlosphere in the Range of 0.7-14 ji. Part 11. Dependence of the Total Transparency of the Atmosphere in the Range 0.7-14 'o on the Thickness of the Precipitation Layer of Water July, August, September, October and November, 1958 and encompassed a wide range of variation of air humidity; the value of w varied between 0.7 and 17 mm/km and the wL values varied between 0.8 and 167 mm. It was found that the magnitude of the reduced signal V is not a linear function of *4WL-7' (see plot, Figure 1) but it appears that the dependence can be better expressed by a linear dependence of Ig V an V -WL The following empirical relation was derived by the authors for the reduced signal V V a VO e - b ~fw-L (2) whereby V. is the magnitude of the reduced signal in the absence of water vapours in the air, b is a constant equalling in the given case 0.2319. Curves calculated according to this equation are in good Cand3/4 1, f ~' ~ - S/169/62/000/008/032/090 82-02VE392 AUTI'O*.13: Ant ipo I Zuyov, V.Yo. , 'AZohhanen!~o, P.N. , S iTi i1z, It. and Fedyushin, A.A. TITLE: and cortain results of studies or korizontal tr.inn )aroncy of the ati-iusphere' to long-wave raklia~ioll M.11OD1CAL: ;lefurativnyy z)iurnal, Gpofizilha, 110. 19Gz' 31, "butract 0132.32- M, tho sfarn. optilca' (Actinom, otry and atmosplieric o tics), Lanin~;rad, Gidromoteoizdat, 1961, 2-48 - 251) Tl~;--,r: The effect of t-nateorolo-icai conditions ol, the tranu- .)nrency I' Cie atmosphare to 1011'~;- ave radiation (0-7 - 14 over of 1.2, 3.5, 6.6 and 9.9 ]an was studied. n't notallic radicktors with alactrical heatinU were used a,4 -~ok re cc; of raLUation. A vacuum thermo-ale;aent with a vibro-converter a ;~c~kstiriw- aniplifier 23AM na' 0 (231,M) served as a receiver. A4c rocciv(~r was anced it, tiie rocus or a parabolic rairror. 3i::-ulta;-,eoualy ..*it*,i tho inoasure;aents at .111 four poitits Ule ciateorolo~;ical conditions wore also :-aensurod, ViZ. tem.;)erature (f Card 1/2 s1 169/6 2/ooo/oo%04/03 2/ogo Metaod.,~ and cortain results .... E2oL,/El-)9-,, the zli;-, :mllidit", wind and intollnity of -)I-Cci:dtatC- T% e retjtlltz-~ "; Cle in Lae for..% %)A~ radiatiua curves vs. (Ustance. The seasonal relation wit:% attelluntioll wlicA coillcidC3 with talc Periou or lli-%Ont absolki'le 11111-aidity wall f0tuid. A m'.mrp attenuatioji of ro(liation was obaerved u,) to 3.5 lua durin-t- the winter period, tLicii it decrcasm*., while the auia--.-.cr period a sharp attenuatioil was observod up to 665 Ian - Abstracter's noto: Co.-aploto translntion.-, 89693 S/139/61/000/001/001/018 E032/414 AUTHORSt ---Antipov B,A,, Zuyev, V.Ye., Kakhanenko, P.N., Sonchik! VA, and Fedyushin, A.A. TITLE., Transparency of the Horizontal Layer of the Atmosphere in the Region 0.7 to 14-0- 111. Dependence of the Total Transmission of the Atmosphere in the Region 0.7 to 14), on the Thickness of the Precipitated Layer of Water PERIODICAL: Izvestiya vy9shikh uchobnykh zavedeniy, Fizika, 1961, No.1, pp.17-19 TEXTz In previous papers (Refs.1 and 2) the present authors described an apparatus and a method of measurement of the transparency of the atmospheric layer next to the earth surface in the region 0.7 to 14 0 and for distances between 1.21 and 9.86 km The experimental material obtained was also reported. In the present paper additional data recently obtained are reported. As an approximation, the magnitude of the transmitted signal was described in Ref.2 by the exponential law V a vos -a -44' -L (I) Card 1/4 89693 S/139/61/000/ool/ooi/olB Transparency of the Horizontal ... E032/9414 where w in the thickness of the precipitated water in mm per km, L in the distance traversed by the radiation in km, a in a constant and. V, is the intensity in the absence of the absorbing medium. Eq (I was obtained empirically and gave a sufficiently good representation of the experimental results. This expression accounts for the absorption of the infrared radiation by water vapour only and does not take into account absorption by carbon dioxide or effects due to atmospheric turbidity. The criterion for the applicability of Eq.(l) is the linear dependence between 1S v and AqwL. The now data now reported are also well represented by Sq.(l) right up to wL a 90 mm. However,12P greater values of wL, the dependence between lg v and VW-L is no longer linear and in order to describe all the experimental data the following formula was employed V = c + k 1 + wL (2) where c and k are constants. This expression is also purely empirical and the criterion for its applicability is a linear Card 2/4 89693 S/139/61/000/001/001/018 Transparency or the Horizontal ... E032/z414 relation between v a~d (1 + wL)-l. Vig.2 shows the dependence or v on wL. During the measurements the sensitivity or the receiving apparatus was controlled by a 6 watt lamp at a distance of 5 M from the detector, It was found that the signal due to the lamp was very.dep*ndent on the humidity or the air. It is therefore pointed out that the use of a standard'source at a short distance from the receiver may introduce errors unless %corrections for the humidity are introduced. There are 2 figures Aand 2 Soviet references. ASSOCIATIONt Sibirskiy fiziko-tokhnicheakiy institut pri Tomskom gosuniversitete imeni V.V.Kuybysheva (Siberian Physicotechnical Institute of the Tomsk State University imeni V.V.Kuybyshev) .ISUBMITTEDs' February 13, 1960 Card 3/4 89693 S/139/61/000/001/001/018 Transparency of the Horizontal ... E032/E414 0 . v Jv - - 0 Fig.2. a .N 0 0 m Card 4/4 - W1 Pme. I .',3 v /FC C / -;'.-.C i - If G 1, ','7,R A15( 111 UTR, C-3 2 14 A V Y Kii Y'. TTTI.F: ';-IV A ppar a I. US for m~-a our i )g a tmospher I c t ranip.ir cncy in the ~nitaz eki re- -c fo r V, r ,v r, -I n, f pi- "ll 0 f,1 n i r a i od r ad int i or s ozin or opt. r a t ing with n i i or t ured co the, mmodnlijclon ficy,wi ev of Itho radi; t ion source . 7he c,", o, ho aarruv-hand am- COffj ~43 ACCESSION NR: ATUIL1177 ;)l if I C., can be cormccted to an e I --c t r,iv- ic co~nriit.,r imln,,., the circult of the WS-2 3evel"Pe" t,,r a n,i i oT,o); ph o r i c ve r - - s w,i t u z a I z lko i khn i clh- ft-*~ z I -Ij pr i T,,-rn ikon gosudar s tvenu)u.- 7 , c. ik S T a t v 1 niv --i r t sTal-IT rE,); 2 5 N ov 1 -4 NO REF SOV: 000 OTI I ER: 000 cnrd 2/3 Ti.: .' N.V., 'n'~ . x,tkini- firl.(A structures of 1,1116A woolle ;' v.6 i ~ ~ I , - ' " ' - - ' P-14 tp 104. , ~l I ;' , :' . -) ~ A17-11POVo B*V* Pathomorphological examination of the Hdry* arreated beart under conditions of experimental artificial circulation. Arkho pat. 22 no. 6t67-72 160. (VIIRA 14il) (PERFUSTON MW (HEMT)) 1 1, - . ANmov.-ILY.i GALTkIERIN, Yu.M.; Yr"WWOVA, 1:J1.; P.1U~;TGRONIN, S.Aj SM1RJ;OV8 YO.Ye. Restoration of cardiac activity aftor prolonged arrest and anemia of the heart in a surgically prepared experiments Vast, khir. 85 no. 7:9-17 Je 160, (MIRA 14i1) (HEART FAILURE) ANTIPOvf B. V.; GAWPERIN, Yu. M. (Moskva, ul. Vorovakogo, d. 26, kv. 14) Use of direct cardiac imemage for artificial blood circulation (experlmental-morphological data). Grud. kh1r. no.5152-58 '61. (MIRA 15:2) 1. Is nauchno-ekMmrimentallnogo t patomorfologichookogo oldela, (say. - prof. S. B. Vaynberg) Moskovskogo oblartnogo nauchno- isoledovatelIekogo klinicheekogo Inatituta imeni M. F. Vladimirskogo (dirt - saslushenM vrach RSFSR P. M. Leonenko) (tMART1 FAILURE) (RESUSCITATION) .,ANTIPOV, B.V.; GALIM-RIN, Yu.M.; Y-.;P,',:AKOVA, N.M.; PEMIZ ToliGN Il;, s.A.; SHM1OV, Ye.ye. i;ffOct Of Cw-dIOP109ic subetances " artificial blood circulation rol,-inos on tho routoration of hoart activity after prolonged tuiemia. Grud. kh1r. 2 no.4:106-113 JI-Ag 160. (MIZA 15:6) 1. Adres avtorov: 111-loakvu, 3-7a Vioalliclum3kaya, d*61/2p Moskovskiy oblantnoy nauchno-isslodovatallikily )d1nicheskiy institut inoni M.F. VladimtrskoGo. . (UMID-ClUGULATIOU, AFTIFICIALN (MWIT FAILURE) (CAMIAC RESUSCITATION) (CMI0V&;CUIAR. AGEIMS) VA)N-BFJIGP SOB* [deceased]; YUDINp Yu*091 ANTIPOVt B.V. e`"~ Leukemold reactions in tumor-like, diveaves. o klin Pate no.2t257.-262 t6l MIRA 6tl2) 1. Is paU logamorfologichookog;o otdola (save - prof* SOB* Vaynberg [decessed)) Moskovskogo oblastnogo nauchno-lealodo- vatellskogo kEmiaheskogo, inatit-dta. ineni Vladimirskogo. h , I 'N"ROV, 13.1%; N.M. (Moskva) Interrelations of local and general factors in the pathogenesis of a dynamic obstruction of the Intestines In peritonitis. Ar)di. pat. 27 no.304-60 165. (KIRA 18:5) 1. Nauchno-looledovatellekly Inatitut morfologil choloveka (dir. - chlen-korrespondont AM SSSR prof. A.P. Avtsyn) ON SSSR I 14oskov- skiy oblastnoy rutuchno-lasledovatellskiy klinIcheskiy institut Iment Vladimirskogo (dir. P.H. TAonenko). I I f 164, v n ~/ 01- . (I A,NTIPCVI , 3.A. HAI0KVj laul P.A. KWAM. Girookopichaskis aviatsionnyis pribory, Moskma,, 19/,0, Title tr.t Gyroscopic aircraft instruments. Nor 0 SOs Aeronautical Sciences and Aviation in the Soviet Union, Library of Congress, 1955 ANTIPOT, 0.1. -Bitumens In traps of the Siberian Platform. Boy. geol. n0.61:144-146 157. (XIM 11W 1. Ikepeditsiya Ministerstys, geologii I okhrarW nedr, g. Rudnogorsk. (Siberian Platform-4itumen) AUTHbRi Antipov, G.I. TITLE: Prospocting Characteristil.,-s c" Iron Ore Argara-Ilim Region (Poiskovy~e prizziaki mostorozhieniy v Ingaro.-Ilimskom reyonp) PERIODICALi Razvedka i okhrana nodr, 1958, ':r 7, PP 7 - Depcsitq 1r the -zhq1ezroru3nykh 1-4 (1L!,1,3R) ABSTRAM The author describes various characteriattos which could help to locale more iron ore deposits In the Angara-Ilim re- gion. This region, atill Insufficiently explored, has only 2 Iron ore depoitte which could be of commercial Importance, There are indicationa that more iron ore depogito can be found. In the last century, geologists discovered the con- nection of deposits with tectonic breaks and their location ovar the trappean intrusions, At n later date, other geo- logists (B.N. Artewyev, S,A. Doktorovich-Grebnitakly) con- firmed those findinge, -the author claegiflies these charac- terintica in separate groupst 1) lithologic-stratigraphic, characteristics - alfrost all depositi of the region are cor- nocteA with tuff breccia, Those fcrmationa are of pyro- clastic origin and, in contact with the ore bodips, they be- camo skarnnd; 2) structural-tectonic charactoris%ice - all Card 112 knowr are deposits are located on large fields formed by Prospecting Characteristics of Iron Ore Depopits 'In the Argara-llim Pegion. uniform mar!-argilscoous formations anti tire ipposited lkrri- zontally. In thi inmedints vicinity of the ore deposits these formations %r9 3lightly dislocated and broken Into separats blo:ks. The complicated structure of these hori- zontal layera indicates the poseibility of ore depositst mineralogle chareotorInttca - encloo-_~rg rocks are trana- formod into skarna in contact. with the ore bod%,. The larp- or the body, the larppr thf~ skarned surroundingst 4) geo- morphologic charecter'.!3tic% - tht Anga7s-llim region is an ancient plateau cut by large rivers, so that trap and mag- netite ore bodies alone form protruding bald mountains which must be studied carefully in cases whore theoe ore depobits are covered by a layer of alluvial sediments, they still form bed-like ,rotrAi4ione, wiich can be discovered in early spring or auttimn after ',he leaves have been she4. There are 6 Soviet references AZZ"CIATMI.- Vinisterstvo geologii I ckhrany notIr SSSR (11.1ristry of Geo- loey and Conservati on of !.An~~:!i.'. lie ^,urcas of the USUR)t I. Geology--USSR ~. Geopilysival Prcv;j;,~Ctln~ D. 4. Iron orn,,~.-.-Econo-rde aspects Card 712 AVT1"V. 0.1.; IVASHCHRWO. N.A. (deceased]: XORABZLINIXOYA, T.T,,* 16~_TUINv M#Xo, dotsont; X=XT5OT# G.A., dotsent; PIKARIN, P.M.; ROSUANOT, O.T.. dotsent; W%WOV, L.G.; CHEWIM51r, G.D., red*; TXALICH# S.Map red.; XMIN, B.S., red.ind-va; GUROTA, O.A., takhn6red. [Angers-Ilin Iron ore deposits of trap formation In the southern Siberion Platform] Angaro.-Illmskie sholexorudnys mestoroshdonita trappovol formtsil iushnoi chasti Sibirskoi platformy. Koskya, Gos.nauchno-takhn.lid-vo 11t-ry po geol. I okhrane nedr, 1960. R3 P. (MIRA 13:10) 1. Russia (1923- U.S.S.Ro) Ministerstyo geologil I okhrany nedr. 2. Geologi Irkutskogo geologicheakogo uprnvlonlya (for Antipove Iveshelonko, Korabelinikova, Pekarin, Strakhov). 3. Irkutskiy gornometallurgichaskiy Institut (for Kosyt;in, Roolyukov). 4. Ir- kutskiy gotudaretyannyy universitat (for Kutnotsov). 5. Glayn" insh. Irkutskogo goologichaskogo upravleniya (for Tkalich), (Angers-Ilim, region--Iron ores) AN?IPOT, 1. - ,-, Device on a cardignu-stitch knitting machine for reducing yarn, Prom.koop. uoel2t24 D 156o (XLRA IW) 1, Direktor fabriki no.22. (Knitting machines--Attachments) AIITIPOVj 1. On the threshold of 1962. MeBt.prom.i khud.promyo. 2 no.1:14-16 Ja 161. (MIRL 1414) 1. Direktor Hookovskoy shveyno-galantereynoy fnbriki Vo. 2. (Moscow-Clothing industry) M~ LLDSHS. Georgly Vladialrovich; C.IMNTSHRY. V.L. re4aktor; BOBURO , Te.56, takhnichoskiy redaktor [A production and financial plan for long hauls by railroads] Proievodstvanno-finansov7t. plan distantell putt# Moskya, Gose transpe thel-dor* iad-yo, 1956, 47 P (KLRI 100) (Ps ilroads-Kanagems N) )dvT-IP,0Y,1*A*. Operation costs should be reduced. Putt i put. khoz. no.4:31-3,1 Ap 159. (MIRA 13:3) (Railroade-Cost of operation) 7R-IT,.V,-F APTUPOV, I.A., insh. All divisions can and nut be profitable. Put' put.khoz. 4 no.2:3-5 7 160, (HIRA 1):5) (PAI Iroads- News went ) AKMVP I.A.1 inshe Constantly imroase the labor productivity,, Put' i putkhose 7 noel& 10-11 163 * (HIPA 160) (Ra.UroadA-IAbor productivity) ANTIPOV, I,A,s inzhe Now devolopenonts in tho detorminat,lon of labor productivity. Put, i put.khoz. 8 no.301-32 16/to OMRA 17%3) 1 Al,'T I I OV, 1vun Azitipovich; HADKIIIII, Alekastidr HodionovIch; SOAKA, XAM11 Grigorlyovich; I '-L'~KOVA, Lots'., red, F (D.-oriordes, organization and plunning of ruilroad tra,,-k aL,onotq) Flonomika) organitataila I plunlrovanle putevego khozininstva. Monkvrip Transport, 1964. 2~6 1~. (VUBA 17:9) ANTIPOV# L9A*j lnth,l LEZHEPEKOV, B.S., inth.1 STAVTSRV, B.N., irsh. Stleation of parameters for working unitts of a motor grader. Strol. i dor. mash. 8 not-12t4-5 D163 (14IRA 170) SAGATOVSKIY, V.N.1 Ah"rIPOVI, 1.0. (Tmsk) Correlation of the concepts *cause.* condition,* Ostiologyg and Opatbogenesis." Vest. AMN SSM 21 no.104-40 166. (HVU 1911) "~-,PVIYKV, P.Yo.-O. VTIPOVP I.K. Change in the group composition of humus or gray and light-gray forest soll.3 unler the influenco of cultivation. Nanch. doV-1. vys. shkoly; biol. nriuki no.1089-1,93 164. (MIRA 17t4) 1. Hekowndovnna kafedroy pcx!hvnvrA--nty1t Wskovikogo gowidarstver- nogo 11hiversitotrk im. M.Mnnonosova. KUROCIIKINO V.M.; ANTIPOVO lAt otv,,;*d.; ORWVAt I.A.0 red.; KORKINA, A.I.;, takhn6r*d* (Standard UNSM-2 programs of the Computer Center of the Academy of Sciences of the U.S.S.P41 Standartnye programV BBSM-2 Vychislitelf- nogo tsentra AN SSSR, Moskva, Vychislitellnyi tsentr AN SWR,, 1963, 11 P. (Akademiia nauk SSSR. Vychislitallnyi tsentr, Standar" I tipovye programmy BESM-2, no*6)o (MlRA 160) ANTIPOV, I.N.; PODrERYUGIN, V.D., otv.fed.; ORLOVA, I.A., red. (Use of gimpson's method in solving a definite integral] Vychislanie oprodelannogo integrale. metodam Simpson&. Moskva, Vychislitelinyl tsentr AN S-SSRO 1964. 9 p. (Akadsaiia nauk SSSR. Vychislitellnyi tsentr. Standartnya I tipovye programmy BESM-2, no.9). (KRA 17W BORISOVA, E,P,l ANTIPOV,.J.P., otv.red. (Subprogram of the iteration method for solving a general problem in linear programming) Podprogramma iteratsionnogo metoda resheniia obahchel sadachi Uneinogo programmiroyanila. Moskva, 1964. 40 p. (Akademila nauk SSSR. Vyohislitellnyi tsentr, StRndartnya prograz- my BESM-2, no.8). (MIRA 17W - 4^- - I FOGMEK, I.A.; ANTUOV I N., Otv.rnl., 131., - . . It-, A _ - X01KNAO A.!., t,1)khn.r#,I. [PrORram fcr cnIcul-tive oigt~nvnIlien nnti fAgo?nvvC",.CT-n ol .4 symmetrical mqtri) 1. Y-rorrunmk nobntvvnnykh _nnr n 1' .4 i sobntvonny~h ve~torov I!o:1v%q1i 10it)4. 23 p. (Andomita nsilik .3..',M. Vy-i .J's1j1kIIny', ~-nontr. . t tipovye projtrs~Ay no. -! " I n , . , U'l.)Y,ANOVA# T.Mj; AMIFUV# I.N.; CHIBraMp V.V.t otr. redo [I.Work at the control deek of tits BESM-~.' computerl programmer's hatAbookaj Rabot& m pulltm =H-2; posobie dlia pro(-a=istov, Moakvap 1965. 31 P. (Akademila nauk SSSR. Vychislitel nyi teentr. StarAartnr i tIpovyv progra=y Bel;M.Q,, no.10) (MIPA Ists) ACC NRt ")-~003062 SOUICS-COD:;:-U 00?3/67/033/=~1~014/0016 V AUTH01: 13olotsklyt D. P.; Antiloov, I, N.; Krylyuk, N, V. ORG! Chornovtsy State University (Chornovitskiy gosudarstvonnyy universitot) TITLSI Synthesis of single crystals and study of the SbI3-BiI3 system by using the 1 fusibility and electrical resistance mothods SGURCE., Lkrainskiy khimichoskly thurnal, v. 33, no. 11 1967, 14-16 TOPIC TAGGS: single crystal growing* antimony conowand$ bismuth compound, lodido, resistivity ABSMICTI SbIj and DIII single crystali were ioronarod from snectrosconically Duro Sb and BI And iodine by the Bridgman method in a vertical furnace with throe tommoraturo zones. 'I"he melting point diagrara of the Sb13-ftI3 system vas studied by plotting heating &n$ cooling curves. The diagram obtained (see Fig. 1) showed the 3ystom to be characterized by a tomploto solubility in both the liquid and solid state. The do- pandonce of the log of the resistivity on the reciprocal tomDerature -das found to be iinoar In SbI single crystals. The pro3ance or BiI3 changes this function con- pletalyt and ?he latter keeps changin'g with increasing Bi13 content. An isotherm of the resistivity of the SbI3;BiI3 system at 1000C showed a peak at 20 mole % KI3; this is attributed to a certain rderirig of the structure. Orig. art. hast 5 figures. Card 1/2, ACC NRs AP,7oo8o62 i Fi g. 1 t, %, , .-k 1. i SUB CODSt 0?/ SUBM DATSI Z)Jan65/ ORIG RSF:' 007/ OTH REF: 001 a j . 4 ANTIPOV, 1. T. Cand Teoh Sol -- (dine) ",We ~Ilverosl method of th? d=v ~t of serl&IARUvRmW photorraphs of 55 M fooAl A on a lilOpOscales" Moo, 1957. 25 pp (Yin of Higher FAjontion 115"IR. Mon Inst or Enrgineers of Geodesy, Aerial Motography, and Cartogre. j.,hy), 100 coplese (KLI 6-50, 1.00) AWNPOT9 lotel "pirant Processing of aerial photographic pictures by mans of transformation of projected bundles of rays, Trudy HIIGAIX no,29tlO9-144 157. (141RA 110) 1,Xafedra fotogrammetrit Moskovskogo institute, Inshenerov geodesil aerofotoogyawki I kartografil. (Aerial photograimtry)

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