SCIENTIFIC ABSTRACT LAKSHIN, A.P. - LAKTIONOV, A.M.

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December 31, 1967
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SCIENTIFIC ABSTRACT
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Foundry Machinery BOV/2300 18. Type 297 mobile sandslinger with removable bin 182 19. Types 772 and 774 mold-turning and drawing machines 199 E. Core-making machin s 20. Type 285 core blower 2o6 21. Type 287 core blower 21o P-2. Illype 288 core-mking Unit 218 23. Type D-12 four-station tux-ret-type core blower 231 24. Type M284 jolt core-making machine 235 F. Automated molding machines 25. Type 96220 automatic molding machine with the B.Z. Cheernyak system 243 G. General premises 26. Standard mechanization of auxiliary processes 250 27. Installation of a molding machine on a foundation 250 28. Regulations for starting, operation, and maintenance 250 Ch. III. Equipment in Cleaning and Shakeout Shops 1. Type 422 mechanical shakeout grate 252 2. Type 425 vibratory shakeout 254 Card 4/7 Foundry Machinery SOV12300 3. Types 33.1 and 313 tumbling barrels 257 4. TYPe 334M two-chamber double-nozzle shot blower 261 5. Types 392M and 393M shot-slinging machines 264 6- Type 323 semi-automatic shot-slinging machine 269 7. Type A53 shot-slinging cleaning table 285 8. Types 361M and 362 shot-blasting cleaning chambers 29o 9. Types 365, 367, and 861 shot-slinging cleaning chambers 307 Ch. IV. Centxifugal Machines I .L. Types Ts23B and Ts13 centrifugal machines 327 2. Type Ts61200 centrifugal turret-type machine 336 3. Types 541, 543m, 545, 545L, 547, 549, and 549L centrifugal machines for pipe casting 345 4. Type 563 centrifugal machine with vertical axis 364 Ch. V. Chill-casting Machines 1. Type K-21 chill-casting machine 369 2. Type X-13 tuarret-type chill-casting machine 370 Card 5/7 Foundry Machinerf SOV/2300 Ch. VI.' Diecasting Machines 1. Types 511, 512, and 513 diecasting machines 379 2. Types 515 and 517 diecasting maebines 396 Ch. VII. Shell-molding Machines 1. Type SKF-2M four-station turret-type shell-moldiag machine 4og 2. Type 832 turret-type shell-molding machine 415 3. Type 8,37 sheLL-molding machine 423 4. Type 873 she 2-1-core -making machine 437 Ch. VIII. Standard Plieumatic Devices for Air and Oil Distributior 1. Air-distributing valves 447 2. Khee- and hand-operated valves 449 3. Jolt valve 450 4. Automatic time valve 452 5. Automatic pressure valve 455 6. Vibrators 457 7. Pheumatic lubricators 458 8. Pheumatic flask clamps 46o Card 6/7 Fbimexy Machinery SOV12300 9. Peducing valve 46o 10. Bypass valve 462 11. M)ck valve 462 AVAn"Z: I&bmry of Congress GO/fal Card 7/7 10-20-59 CHERNOV, Yurly Ivanovieh; KIZIWV., Anatoliy Ivanavich;- IUMIN A.P., kand. tekhn. nauk., retsenzentj ZHUKOVj A.A.p kand. tekhn. . re..; IVANOVA., K.N., inzb.., red. izd-va,- SOXOIDVA, T.F., tekhn. red. [Handbook on foundry equipment) Spravochnik po liteinoi osnastke. Aoskva, Gos. nauchnc-tekhn. izd-vo mashinostroit. lit-ry, 1961. 406 p. (MIRA 14 - 11) (Foundries-Equipment and supplies) BERKOVICH, Ye.S.; NESVIZHSKIY,, O.A.; DAPMHINAO L.B.; LIMRMAN, V.I.; KWANOVA,, A.V.,- IAWHIH, S.VQ Determining relative wear resistance of deposits built-up by the T-590 electrode with various coating on the laboratory testing maohine "rotating bowl." Trenei izn.mash. no-15:31-46 162. OURA 15:4) (Metals-Testing) TRESHCHALIN, V.N., tekhnik; LIBERMAN, V.I., tekhnik; LAKSHIN, S-V. Gcopressed air blendingand conveying of charges for electrode coverings. Svar. proizv. noA:25-26 Ag 162. (MIRA 15'.11) 1. Pavshinskiy mekhanicheskiy za,vod. (Electrodes) (Pneumatic machinery) ziwTA, A.N.-,TA TRA, L*K* Application of dicoumarin in *6car4lAI-infarctions and in thromboses of peripheral - vessels. -11-ins ked; '~ Moskva 32: -1A 7,igA.29537. no k4 (CLML 24:1) 1. Of the Department of Hospital Therapy (Head Prof. A. L. Hyaqui- kov), Active Member AM MSR). USSR / Human and Animal Physiology (Norml and Pathological). T Blood. Abs jour ; Rof Zhur - BiOlogiYa, NO 13, 1958) no*' 60351 Author : Iakshi~ia K. Inat S~cok dical Institute Title :Estimation of Sclerosis in Large Vessels as Determined by the Propagation Rate of the Pulse Wove Orig Pub :Tr. 1-go Moak. mod. in-ta, 1956, 1, Uk-122 Abstract :In 34 hyportonsive patients (HP), in 28 with athoro- sclerotic aorta with a normal artorial pressure, in 45 (11P) with sclerotic aorta and in 54 normal people, the carotid and the femoral artery pulse was recorded (air trans- mission with photographic recording). The rate of propagation of the pulse wave in normal people is, on the average, 6-7, and in atherosclerotic ones - 9-7 per sec. In HP without atherosclerosis, the effect of increase in Card 1/2 USSR / Human and Aninal Physiology (Normal and PatholoSical). T Blood. Abs Jour Rof Zhur - Blologlya., No 13) 1958) No. 60351 prossumo upon the increased rate in the propagation of the pulse wave is insignificant. The increase in the rato of propagation of the pulse in the section of aorta-iliac arteryinEP indicated the combination of byjx3rtonsion with atherosclerosis of the aorta. -- M. G. Shrayber C ard 2 /2 6o LAKSHINA, Lr. K., Cand Ned Sc~ -- (diss) "Evaluation of Sclerosis - 0-h tLp ~sa4~ ed of wh&~ of the Pulse of Large Vessels AQaet - Spe Wave-" Mos, 1957. 8 pp (ist Mos Order of Lenin Medical Inst im I. M. Sechenov), 200 copies (KL, 47-57, 90) LAXSEINAt L.N.; SHLVEMV, V.N. Scientific economde conference. Vast. AN Kazakh. SSR. 21 no.gs 84-85 S 165, (MIRA 18t9) MARFEVICH.. A.V.; LAKSHTANOV, V.Z.; ljC1'B-YCFiIM, S.L. P,3t~ of hydrogen as gas ca:~-rjer -ir. 16-45ch.~trge dotectors. Zhur. prild.khim. 38 no.11:2459-2-64 N 16~:* (VIR.A 18:12) 1. Gusudarstvenn~7 iinstiLutu prikladnoy khimil. Subm~,tted September 6, 1963. IMS, Te.A.; KATSEV. I., redektor; LAKSUOVSWii, rodaktor; NATISSIN, Z., takhalchaskly redak - ---1 LPractical photography manual] rrakticheskee posobie po fotografii. Moskva, Iskusstvo. 1933. 247 p. WaA 7:7) (Photography-Handbooks, manuals, ate.) DORO-V=, Vitaliy Flitrofanovich; ISVD!, Venismin Yakovlevich. Prininali uchastiye.- YLUNIN. S.D.. ln2,b.; KONDRUSEV, V.S., inzb..L-L~AKWO~VSM ~A-Au kand. takhn. nauk., rateezzentl - SKUBACHEVSKIY, L.S., inzh.,, red.; SMIFRE, L.I.; red.; CIAMMEMA., LoAaj, teklmfk red. Mating ram-jet enginesj Ispytaniia vazdushno-resktivmykh avi- gatelei. Moskva.. Gos. naucbno-tekhn. izd-vo Oborongiz, 1961. 220 p. (Airplanes-Ram-jet engines) (MIRA .15:2) ZAKKARCIGHKO, D.D,dotseat, kandidat tekhnicbeckikh nauk-, ISAYEV, I.P., dotsent, Icandidat takhnichaskikh nank: KALININ. V.K.,iazhaner; KUSTITANOV. X.Ya.,dctsent, kandidat-takhtilchaskikh nauk; IAKSHTOVSXIY I.A.Aotsent, kandidat tekbnichaskikh nauk; rT-A.U.,proxessor, dox-tor tekWildhaskikh'nauk; ~X=Ll. Y.B., professor, doktor takhnichaskikh nauk; MIRONOV. K.i.,inzhener; MIKHAYLOV, N.M.,dotjient, Imndidat takligicheBUkh uauk; HAKHODKIN, M.D., doteent, kandidat tekhnichaskikh nauk; OZZ"IA)VSKIT. Ch.S., inzhener; OSIPOV, S.I.,inzhener; AOMASHKOV,--S.G.,lut.,hener; SOKQlOV, L S.,inzhener; FAMINSKIY, G.V..kandidat taltbnichaskikh nauk; S;~;SILLO, A.A.,inzhoner-, PHLYAKH-TO, P.N.,dotisent, kandidat taklmichaskikh nauk; BOVI, Ya.G.,kandidat tekhnicheskikh nauk, ratsem8nt; PERTSOVSKIY.-L.M.,insheier. retsenzent; ALEKSBYRY,.A.Ye.,professor, doktor takhnic~skikh nauk, retsenzent; BATALOV', N.M.,iwahaa6r, retsenzent;-VINFER , B.N.,inzhener. retsailient; G~UCHSVA. L.0.. kandidat takhnichaskikh nauk, reteenzent-, YBOOKIMOV, A.M., inzhener, rateenzent; KALININ, S.S.,iazheaer,~ratoenziqnt; TRAUTMAN, L.M.,kandidat takhniabaskikh nauk,retsenzapt; PTISNKOV, A.P.,inzhenar, retsenzent; GOKRBEWBIN, B.Tik.',k4adidst takhnichaskikh nauk. retsenzent; ILIIN,-I.P.,ipzhoner,.r6teausent; NAXHCDKIN. M.D.,dotsent. kendidat takhuicheta~i~ na*, istsenzent; TISHCEUKO, A.I.,otvetatvenn~7 redaktor; B*HNSHEIVICH., 1-;I., kandidat takhnicheskikb nauk, radaktor; ZONOXHOVICH,.A.Te.,dotsent kandidat takhaichaskikh nauk, redaktor; LUTSU10.1a.G., inzhaaar, radaktor; RWOZHIN, A.P..inzhener, redaktQr;.S33)OltO'?, R.I.$ inshener, radaktor; VARINA, G.P.,takhnich"kly radaktor (Continued on next,eard) ZAKHARCIMkO, D.D.---(continued) Card 2. (Toobnical manual for railroad workers] Tekbnichaskii spravochnik zheleznodorozhnika. Rod. kollogiia R.G. Granovsk-ii i c1r. Moskva, Goa. transp. zhel-dor. izd-vo. Vol. 9.[Blectric railroad rolling stock3 SlektropodviEhnoi aostav zheleznykh dorog. Otv. rod. toma A.I. Ti9hchenko. 1957. 652 p. WaA 10:4) 1. Oblen-korrespondent Akadamii nauk SSSR. (for Aleksayev) (Blectric railroads--Rolling i3tocl.) LAYISKIYP L. Treasures of the green no.6:54-55 A 161, (Reed virgrin lands, 11auk-a J zhiznl (1,'11, 14:7) -)roducts) LAKSKIYq L,j insh. Photosensitive glass. Nauka i shisn' 29 no.1103 X 162. (MIRA 161l) (Glass, Optical) TIP,.KTANCiVA, II.V. a SUfl r; 2 rG (141 ca:.-rying 1. Kumv, D.: LAKTAYEv, N. 2. LzsR (6oo) 4- Irrigation 7. Utilization of water on a consolidated collective farm with a new system or irrigation. Khlopkovodstvo No. 8, 1952. 9. Monthly List of Russian Accessions, Library of Congress, January 1953. Unclassified. P N. T. Experience of the Sverdlov kolkhoz in adopting a new irrigation system Tashkerr~ Gos. izd-vo UzSSR, 1953;7 36 p. LAKTAYEV$ N. T., Cand Tooh Sci (diss) "Llethods of improvin6 Kolkhoz use of viat-,r.11 Tashkent$ 1957, 26 pp (TashImnt !nstitute of Enjjnecrs of Irri-ation and Mechanization of Agriculture TIIIfISKh1a) 150 copies (HL, 36-57, 105) I i: - IARTAYEV, N.T. -, CIELYUKAROV, M.D. ~ Use of water on the 'Fakhtaarall' State Farm. Vop. gidr. no.10.-5-36 162. (MIRA 16:2) (nlich District-Cotton-Irrigation) LdKTAYEVAL-Aleksandra Mikhaylovua, starshays ptichni,ton; ZOLOTLTiauN, B.V., red.; TBRTYMNIX.-G--.E., red.; YA SKINA, Ye*A., tekhn.red. [For 170 eggs per layerl za 170 iaits ot nesushki. KuibyabBv, Kuibysb,avskoe knizhnoe izd-vo, 1960. 20 p. (MM 14:1) 1. Kolkhoz "Novoye Zavolzhlye" Privolzhakogo rayons (for Laktayeva). Ogge-Production) IJAMONOV, A.F. I Propertios of the sea ice. Transportation Institute devoted to the study of the North, No. 49. 1931. UKTICKOV, A. F. LAKTIONOV, A. F. ...Severnyi poUus; pod red. prof. V.IU. Vize. Arkhangellsk, Arkhangellskoe oblastnoe izd-vo., 1939. 233 P. Contents; --Pervye puteshestviia k pollusu. - Ekspeditsii, 1527-1937. -Vozdushnye ekspeditsii k Severnomu poLluou. -Tranwkticherkie perelety 1937 oda- - Poliarnaia stantsiia "Severnyi polius".- Kratkii fiziko-geografichaskii ocherk g' DLC 4tsentrallnogo Poliarnogo bassein3a -Glavneishaia literatura (p. 231v:ff3j) : G620. L3 )m SO: LC., Soviet Geography, Part 1, 1951, Uncl. LAKTIONOV, A. F. LAKTIONOV, A. F. Severnaia Zemlia; pod red. V.IU. Vize. Moskva, Izd-vo Glavsevmorput, 1946. 148 (4) p. (Poliarnaia bibliotekB.) "Biblioa,raficheskii ukazatell": D. 145-Z1-49 -7. DIC: G827.L3 So: LC, Soviet Geography, Part II, 1951/Unel,assified. URTIONOV, A.F. LAKTIONOV, A. F. 3 m i lius; ocherk istoril, puteshestvii k tsentru Arktiki J-od 'e IlY2 "v Y obshchei red. V.Iu. Vize skva, Izd-vo GlavsermorPuti, 1949. 394 P. "Glavneishaia 3-iteratural't P. 391-393. DLC: G620.L3 1949 SOt LC, Soviet Geography, Part 1., 1951,, Uncl. IAKTIONOY,,Ale* I ed rovich; FROWT, VYachesl&v Usillyevich;, --~~Cfml _1 ., r or; VOLKOVA, Ye.D.. tekhnichaskiy redaktor [0a floating ice] Na dreifuiushchikh 11dakh. Moskva, Izd-vo wHorskoi transport," 1955. 87 P. (MLIU 9: 8) (Arctic regions) Laktionov.9 Aleksandr Fedorovich shestviy k ,z-~ ;_-- Severn-~~Y- CFOs oc erMsWrii Pute ransportits Tsentru Arktikie Moskva) Izd-vo IlMorskoy T 1955-47, p. Illus.0 Diagrsop Ports*# maps.' 23 cm- Bibliography: po 440-C44 LAKTIONOV, ALEKSANDR FEWROVICH Recent Soviet Scientific Investigations in Translated by Kenneth R. Whiting. Maxwell Air Research Division, Research Studies Institute, IV., 104 P, Illus., Diagrs., Maps, Tables Research Study, AU-272-56-RS1 2B/4 621.12 .Lll the North Polar Regions, Force Base, Ala., Doementary 1956. (Air University Documentary Sumary of HIS Severnyy Polyus (The North Pole) Moscow, 1955. Bibliography: P. 101-104. LAKTIONOV, A.F. Battle-borne message from the icebreaker "Taymyr's Izv,Vsas. geog.ob-va 88 se.3:302 Ny-Je '56. (NM 9:9) (Ice-breaking vessels) 1AKIrIONOV, ALMANDR F-.!,POROVICII D/3 181.52 -L1 Yezhdunarodnyy geofizicheskiy god v Antarktike The International Geo-physical Year in the Antarctic Lanin- grad, Gimiz, 1957. 178 P- illus.$ Diagrs., maps, tables. 1AVP1VjJ()V, A],g$s LA0140VA, B.I., redaktor; SCJLIDV,6YCHIK, -;%.A., -TURYnitches y redektor LInternational Geophysical Year in the Antarctic] Mezhauuarodnyi gecfizicheskii god v Antarktike. leniagred. Gidrometeor.i2d-vo, 1957. 178 P- (MLHA 10:10) (International Ge hysical Year) (Antarctic regionel UKTIOMV, A.F.; SVAMOIIT'YEV, V-A- Aeronautics in Arctic oceanographic 19-31 157. (Arctic regions--Aeronautics (Oceanographic research) research. Probl. Arkt. no.2: . (MIRA 1;:.12) in geography) LAKTIOITOV) -A-F-p- --Kil-'Union Arctic Scientific Research Institute, Moscow 19561 "Arctic Ice Observational 14ethods," (English) 35 PP. u papertsubmitted-pat Arctic Sea Congerence, Easton, U3., 24-27 Feb 5" 14711 LLUIONOV, A.F.; SH&MONTITIV, V.A. Use of airplanes in oceanographic research in the Arctic. Biul..Okean.kom. no.2%65-74 '58. WU 12:5) (Arctic regions--Oceanographic research) (Aeronautics in geographY) LLITIOWV, A.F. Oceanographic research in the central Arctic. fiek. probl.i rez. okean. issl. no.1;17-19. 159. (MM 13.2) (Arctic Ocean--Ocesmographic research) LAKTIOMV,,_A..,_q_tarsbiy nauchnyy sotrudnik Outstanding Polar explorer and geographer. Mor.flot. 19 no.12:38-39 D 159. (MIRA 130) Is Arkticheakiy i Antarkticheskiy nauchno-iosledovatel'sldy institute (Vize, Vladimir Iurlevicb. 1886-1954) LAXTIONOT, Alaksandr,F-adorovi.ch; BUFIRNOV, V.F., red.; IVANOVA, Z.D., red.iz~-~va-, MEZINOV, M.M., red.izd-va; TIKHONOTA, Te..A., takhn.red. ENorth Pole] Savarnyi -polius. Moskva. Izd-vo "Morzkoi transport.' 196o. 524 p. (MIRA 13:6) (North Pole) GORDIMM, P.A.; LUMONOV, A.F. Main results ofArecent oceanographical studies in the Arctic Bain. Izv- AN SSSR- Ser-.1900g. no-5:22-33 B-0 160. (MIRA 13:10) (Arctic Ocean--Ooeanographio research) LAKTIONOV. A.F Effect of ice on tidal phenopena. Probl.Arkt.i Antarkt. no-5: 53-58 160. (MM 14:4) (Tides) (Sea ice) LAXTIONOV, A., starshiy nauchnyy sotrudnik Rctending the navigation season in ice-affected harbors. Kor. flot 20 no'M:40-41 N 160, (MA 13: 11) 1. Arkticheskiy i Anatarkticheskiv machno-issladovatellakly institut. (Ice on rivers, lakes, etc.) LAKTIONOV, A.F. First Interdepartmental Conference on Model Studies of Atmospheric and Hydrospheric Phenomena. Okeanologiia I no.5:924-0,26 '61. (MBA 15:3) (Meteorological research) (Hydrology--Research) LAKTIONOVO A.F. B.Franklin and some problems of oceanography. Okeanologiia 1 no.5:951-955 '61. (MIRA 15:3) (Franklin, Benjamin, i7p6-179o) (Gulf stream) LAKTIONOV, 'A.F. M.V.Lomonosov and geography; on the 250th anniversary of his birth. Izv. Vses. geog. ob-va 93 no.6:463 *-478 N-D '61. (YjfLn 15!1) (Geography) (Lomonosov, Mikhail l.'asil'evich, 1711-1765) LAKTIONOV, A.F. Academician Otto IUI'evich Scbmidt; on the 70th an:-Iversary of his birth. Izv. All SSSR. Ser. geog. no.2:95-103 Yx-Ap '62. (KRA 15:3) (Schmidt, Otto lUllevich, 1891-1956) IAUIONOV,v A-F. N.K.Knipovich,, his life and work; on the 100th anniversary of his birth. Okeanologiia 2 no,4:758-766 162. (MMA 25:7) (Knipavich., Nikolai 1411-hall vich., 1862-1939) - LAKTDMY,-A..,Z,- Drift meter designed by H.V.Isvekov. Ckeanologiia 2 no.'5:901-903 162o NIRA 15: 11) 1. JL-ktichookiy i antarkticheakiy nauchno-issledovatel-lakiy Institut. (Drift) -LAKTIONOV, A.F. (Leningrad) Calendar for nature lovers. Priroda 52 no.6:123-124 163. (KIRA 16:6) (Science-Miscellanea) LAKTIONOV. A.F. Arctic and Antarctic Museum. Probl. Arkt. i Antarkt. 119-126 163. (Leningrad--Art galleries and museums) no.12: (MM l6s7) LAKTIONOV., A.F.; ROMANOVICH, Z.S. Survey of literature on marine hydrologic and ice forecasts. Probl. Arkt. i Antarkt. no.13:137-144 163. (wm 16:9) (Bibliography-0--eanography) ME-RZLOV, Ye.; ZAVIYALOV, A.; LEBEDEV, N.; IAKTIONOV, A., gruppovoy . , 1, - - -- --'ik inzh.-elektromekbanik; VERIGO, A eRiViomex-Ram -Automatic control on ships. Mor. flot 23 no. 12:45 D 163. (MIRA 17:5) 1~'Nachallnik sluzhby sudovogo -khozyaystva Dunayskogo parokhodstva (for., Merzlov). 2. Nachallnik tekhnicheskogo otdela Dunayskogo parokhodstva (for Zavlyalov). 3.* Starshiy inzh. NIO Odesskogo -.vysshego inzhenernogo morskogo uc.hilishcha (for Lebedev). 4.-Dunaysko.ve parokhodstvo (for laktionov, Verigo). L A ~k or~ o v. A G USSR/Optics Physical Optics K-5 Abs Jour Referat Zhur Fizika, No 5, 1957, 12947 Author Levehin, V.L.' Laktionov, A.G. Inst Physics Institute, Academy of Sciences, USSR, Moscow State University USSR Title Absorption of Complex Molecules, Which are in a Metastable State. Orig Pub Dokl. AN SSSR, 19551 1o3, no 1, 61-64 Abstract Measurements were made of the absorption spectra of matas- table (triplet)'molecules of fluorescein in boric acid, also of estuline, roduline orange, acrydine yellow, and rivanol in sugar drops. The spectra were measured on a recording spectra photometer GOI, and with the aid of a UM-2 monochromator, with illundn ion by unmDdulated light 436 millimicrons). The investigated spectra are Card 1/2 L op, k t / I ?p PO ('~ 49-58-3-18/19 AUTHOR: Laktionov A. TITLE: The Distribution of Aerosol Particles in the Atmosrhere (Raspredeleniye chastits aerozolya v svobodnoy atmosfere) PERIODICAL:-Izvestiya Akademii Nauk SSSR, Seriya Geofiziches1caya, 19581 Nr 3, pp 419-421 (USSR) ABSTRACT: The study of the distribution of aerosol particles prov- ides an opportunity for consideri2--,', turbulent mixin,-, in the atmosDhere. Ho facts have previously been(riven in the literature on the quantity of large particles >41i) in the atmosphere, their dispersion with size and change of con- centration with height. The author mentions the vviork of Junge (on particles from 10-31, - 1N) and Gayvoronslo-iy on exy and the vior'21-. ponential decrease of particles with height, of Penndorf on the distribution of Mie particles in the troposphere. All this work refer-s to small particles Kloll), concentrations of thousands of particles Der GM and the results obtained indicate-a constant mixing coeffic- ient with height. Sinrortsov and Vullfson showed that the atmosphere is divided into layers: the lower convective Card 1/3 49-58-3-18/19 The Distribution of Aerosol Particles in the Atmosrhere. layer endo at 300 m whilst the upper extends from 300-1500 M. In the latter region, the average intensity of convective flow does not change with height. The author made his mea- surements along the route: Moscow-Leningrzid-Kiev-Krasnodai-- Baku-Tashkent and back. The apparatus is as follows: a stream of air flows through a capillary 1 mm in diameter. Particles in the air intersect a light beam at the focus of an ellipsoidal mirror. This scatters light which is cozeen- trated by the mirror onto a photomultiplier. The resultant imDulse is recorded either on a mechanical counter (giving. the number of impulses) or on an indicator giving the count- in- rate. The apparatus is attached to an aeroplane ahead of the propellors, in order to avoid disturbance of the air. It could record up to 400 particles/cc. Tests of the air were carried out for periods of 120 see every 10-15 Minutes; the number of particles and the volume of air (4-5 1) were recorded. The various channels of the recorder were arrann- Sed-so that the first counted all particles >41i, the second *V7.1ii and the fourth>%L. The following >5.51i, the third , preliminary results were obtained: (1) The concentratio-n of particles >41i depends on the physical geography of the 0 e-ion, e.g., in the morning, above the Central EuropeanpErt Card 21?F 0 0 - 49-5~-3-la/19 The Distribution of Aerosol Particles in the Atmosphere. of the USSR, at 1000 M, the count was 30 particles/1--itre;- in Central Asia 100-200 particles/litre, over extensive water surfaces 10 particles/litre; over the Caspian S~,,a 10- 15 particles/li.tre Emd above the Black Sea -15 particies/litre. In constant weather conditions and at constant time of the day, the particle concentration remains almost constant above similar types of country. (2) Results obtained in Tood wea- ther show that the atmosphere is divided into layers. The number of these, and their heights, can change - - ,,reatly. (3) It is calculated that the number of large ppxtic-les -.,)er cc diminishes with height quicker than the number of smail CD particles. Acknoveledgement is made to Corresponding Me-mber of the Academy of Sciences Ye. K. Fedorov who swcervised the work. There are 3 figures and 7 references, 5 Russian and 2 English. ASSOCIATION: Academy of Sciences of the USSR, Institute of A-.)plied Geophysics (Akademiya nauk SSSR , Institut prikladnoy ,eofiziki) SUBMITTED: July 24t 1957. AVAILABLE,: Library of Congress. Card SOV/49-59-11-14/28 AUTHOR: Laktionov, A. G. TITLE; An Automatic Continually Operating Apparatus for Determining the Natural Aerosol PERIODICAL: Izvestiya Akademii nauk SSSR Seriya geofizicheskaya, 1959, Nr 11, pp 1656-1664 (USSR5 ABSTRACT: The apparatus was designed for determining the particle concentration up to 1000 particles per cm of the aerosol, with particle diameters from 2 to 40 ji. The design of the apparatus is illustrated in Figs 1 and 2 where : 1 - lamp, 2 - condenser, 3 slit, 4 - lenses, 5 - mirror, 6 - aerosol stream, 7 light extinguisher, 8 - photocell, 9 - photo-multiplier. Two types of aerosol inlets employed are shown in Fig 4. The results obtained by the application of the apparatus are shown in Fig 5, where the data_are given for different temperatures (a - 00, b 220 VE - 450, 1 9001c3 - 1350C, e - theoretical calculation for Q 2 cm, sec W - type'a'(Fig 4) of inlet (curve 1) and Q = =3~see (curve 2)1 It was found that for the aerosol size d < 2N and wind speed u - 4 m/sec Card 1/2 with 200 fluctuations of its direction during one I/ '4 SOV/49-59-11-14/28 An Automatic Continually Operating Apparatus for Determining the Natural Aerosol minute, the coefficient of capture was K-~ .Z 0.7. Thanks are conveyed to L. M. Levin, Yu. V. Konyshev, V. G. Fruntikov and V. F. Struchev for their assistance. There are 5 figures and 7 references, 3 of which are Soviet and 4 English. ASSOCIATION: Akademiya nauk SSSR Institut prikladnoy geofiziki (Academy of Sciences U9SR, Institute of Applied Geophysics) V11" SUBMITTBD~ January 59 1959 Card 212 82,703 S/049/60/000/004/007/018 5_0010 E032/E514 AUTHOR: Laktionov, A. GA. TITLE: Results of Studies on Natural Aerosols over Different Regions of the USSR PERIODICAL: Izvestiya Akademii nauk SSSR, Seriya geofizicheakaya, / ig6o, No.4, PP-566-574 . q TEXT: The particles of natural aerosols which are present in the atmosphere during clear and cloudless days,when the humidi ty -is less than 100%, are normally solid. The instrument employed to study natural aerosols from an aeroplane in a free atmosphere was described by the present author in Ref.1 and is shown schematically in Fig.l. The~natural aerosols were studied during four summer expeditions. Measurements were made of the distri- bution of particles, both as regards their dimensions and their The results obtained are summarised in the table 9" FFf 7T?-7T--2-! af Raf ty rrah in a uniform air mass at altitudes or lob m or lilgiaev abov-4 & Uniform underlying surface during cloudless days is a definite characteristic of the atmosphere and does not change very much up to 100 km. There is a well defined dependence of the concentration Card 1/3 82703 s/o4g/60/000/004/007/018 E032/E514 Results of Studies on Natural Aerosols over Different Regions of the USSR of '!gigantic" particles (radii between 4 and 12 microns) on the character of the underlying surface. The mean concentration of particles.observed above snow and water is smaller by a factor of 100 as compared with the concentration above deserts and steppes. The size distribution of "gigantic" particles varies continuously during ascent from 100 to 1000 m. This variation is particular rapid during winter and summer (daytime) above water, and less rapid during summer (daytime) above deserts. The effective optical radius of large particles remains practically constant between 100 and 1000 m. This radius is found to lie between 0.08 and 0.14 it, depending on the type of the underlying surface. Heating of the air by these particles during daytime at 100 m above ground is 2 x 10-3 deg/hr and apparently has no appreciable effect on the heat transfer in the lower troposphere. It was found that the size distributions of particles could be described by expressions of the form Nr> r 0 = C X Card 2/3 r0 82703 s/o4g/60/000/004/007/018 E032/E514 Results of Studies on Natural Aerosols over Different Regioas of the USSR where c and x are constants. The present work was directed by Member-Correspondent of the Academy of Sciences of the USSR Ye. K. Fedorov. Acknowledgment is made to the following person for assistance: Yat I. Kogan, V. I. Kazas, V. G. Fruntikov, V. F. Struchev and Yu. V. Konyshev (Members of the Institute of Applied Geop ysics). There are 3 figures, 1 table and 6 references: 5 Soviet and I English. ASSOCIATION: Akademiya nauk SSSR Institut prikladnoy geofiziki (Academy of Sciences USSR, Institute of Applied Geophysics) SUBMITTED: August 20, 1959 Card 3/3 LAICTIONOV, A.G.; IXVIN, L.M. Comparative measurements of the concentration and function of particle distribution in water aerosols. Izv.AN SSSR.Ser. geofiz. no-7:1056-plO38 Jl 160~ OCMA 13:7) 1. Akademiya nauk SSSR, Institut prikladnoy geofiziki. (Gloud pbysics) LAKTIONOT, A.G. Verical distribution oi aerosol particle concentration mination of the coefficients of vertical motion in the atmosphere. Izv.AN SS�R.Ser.geofiz. no-9:1397-1406 1. Akademiya nauk SSSR, Institut prikladnoy geofiziki. (Cloud physics) and dater- free S 160. (MIRA 13:9) 8/020/60/133/04/23/031 BO19/BG6O AUTHOR: -Laktigao_V.L A. G. TITLEs The Determination of the Coefficient of Vertical Intermixing of Particles in the Free Atmospherp 1-Y PERIODICAL: Doklady Akademii nauk SSSR, 1960, Vol~ 133, 110. 4, PP. 838-840 TEXT: It *follows from the exponential equation (1) for the particle concentration, which is obtained from Fick's equation for the turbulent diffusions that the concentration of faster sinking particles decreases more rapidly with rising height than the concentration of slower sinking particles. Measurements matte by I. I. Gayvoronskiy and others showed, however (Ref. 2), that the concentration of Aytken condensation cores in the atmosphere decreases ir. the same way as the concentration of particles of the order of magnitude of I)A . This result contradicts the conclusions drawn from (1). With a view to clarifying this problem, concentration measurements of particles wtth an effective opl.ical radius of O.lAi and of large particles in the range of 10P N r > 3)A were carried out from Card 1/3 The Determination of the Coefficient of 5/02o/60/133/04/23/031 Vertical Intermixing of Particles in the B019/BO60 Free Atmosphere an H_R -14 (IL-14) airplane at altitudea of 100, 200, 3004 500, 750, 1000 m. and further every 500 m to 3000 m. Fig. I is a graphic representa- tion of changes in concentration of the aerosol with diameters of about 0 1A , 5/A, and 8p . It follows from the discussion of the turbulent diffusion coefficients cf the particles calculated on the strength of these measurement results that (1) is not suited for describing the con- centration distribution of large particles and all the more of Aytken condensation ccre8, The cause for this is found in the assumption made in the derivation of (1), namelyof t%e settling taking place under the action of the gravitational force. For this reason, formula (2) is suggested for the concentration distribution for particles, which takes account of the influence exerted by air motion in anticyclones. A new coefficient is used here for the turbulent intermixing of aerosol particleN which is calculated according to formula (3). The values of this oo- efficient ara in good)agreement with those obtained by D. L. Laykhtman's method (Refs- 5 and 0 ~ The author then discusses the difference between formulas (1) and (2) which basically consists in that (2) yields a particle distribution which is not dependent on the particle size, Card 2/3 The Determination of the Coefficient of S/020V60/133/04/23/031 Vertical Intermixing of Particles in the B019/ .060 Free Atmosphere provided that the Stokes settling velocity be considerably smaller than the air motion rate in an anticyclone. The author thanks Ye. K. Fedorov, Corresponding Member of the AS USSR, for his assistance. There are-f- figures and 6 references' 5 Soviet and I German. ASSOCIATION: Institut prikladnoy geofiziki Akademii nauk SSSR (Institute of Applied Geophysics of the Academy of Sciences, PRESENTEDs November 10, 1959, by A. A. Dorodnitsyn.. Academician SUBMITTED: November 9, 1959 Card '.,-,,"3 LAKTIONOV, A. G. Cand Phys-Math Sci I'diss) "Study of several characteristics k of ratural aerosol." Moscow, 1961. 10 pp; (Academy of Sciences USSR, Inst of Applied Geophysics"; 200 copies; price not given; (KLt 6-61 sup, 194) LAKTIONOV, A. G. Relation between the scattering of light in the free atmosphere and the vertical distribution of aerosols. Izv. AN SSSR. Ser. geoftz. no.6:953-957 Je 164.. (MIRA 17:7) Lu ih- h-silb*,xight. -scat,- oil, 01 f 1. f V00 rlw- ACC N& AP5(i26361 -UR/9,362/65/0 5 01/011/1212/121 W AUTHOR:, Kauas,' V~ 1~; Xon shev, Mr. V.; Laktionov,.A. G. ORG: Instit,*ute~ of Applied. Geophysics (:Institut prikladuoy geofizik TITLE: 0 nti 0 nuous airborne instrument for measuring the size and concentration of large drops in clouds SOUROE: AN SSSR. Izvestlya. Fizika atmosfery I okeana, v. 1, no. 11, 19651 12~12-12151 TOPIC S.~7 9 to aiher forecasting, mieteorolog instrument, atmospheric preolpitatibn- 11 XABSTRACT: ItJs known. that the, mostimporttint mechanism leading to the ~., growth of:-cloud d.rqps~.to-the size of rain diops is gravitational -,coagulation which leads. t.-V:a rapid g:rowth'of theArops If their ini- d1 -1 n .r tial - amete;r~ is greater, thane 50 M!03?o* 9. -The p esence in the clouds ~of~drops_.lartterlhan-50 microns also-determinea.:the possibility of the~developkent of precipitation, ~The~arttole presentsdetalls of an aircisft-4iounted instrument which .:permits -Teliable Asts, on the drops in' Iho':'~ at Ze ringe of 30 t - 150;M16ions in Aiametef. 0 A dia- gramaUc- ek6tdh o fi ~Ahei lutrum6nt Is Ishown -(Seel Fig. 1) - 1/3' Cbr&l I C "R9 AP 003247 aw AUTHOR. k SOURCEICOE., 31 -1:11 tionov UR/0020/65/165/006/1290/1 ,W ZZ.- PRG:. Jasiltut lied "C' e-of- 'Geo h sicP Inatit6t .~11.I - (.. Prildadnoy E: beterminatlon geofjZIk 0 1) f thec ancentratlon ofc SOURCE: - !R -clqu AN SSSR. : Dokla ds6 TOPjc TA6S. dY,IV. 1650 no. 6, 1965, 1290-1293 ~nucj meteorology# cloud physic eus, aerosol, at 8, atmospheric conden Mospheric aerosol, ABSTRACT: A particle sizing sation. condensation sation __ method has been developed for det nuclei In clouds) in. termining the CO-ncentrati the.:crltj~al , which is unique on of conden- 31ze for a a hat only thos to Investigate this c Oven-supersaturati. . e drops which exceed oncent n are considered, a PhOtOelectric:anal ration 0 The apparatus used cro s) f Yzer for measuring si f an isothermal diffusion chamber, 'of condensa n and:a zes of individual drops (down to 0.-1 mi_~ :_ tIO ive-channel electronic recorder. The apDaratus permits measureme- taneous determ L:tujc01.ei concentrations at supersaturatio~s of 0.1 t in of the total co nt the chamber . ncentration of drop 0 IZ and simu.1- Concentrations of s larger than 0.2 P grown 100 k~ fr 0.2, 0.3, and 0.5Z in rations of-O .1 condensation nuclei were Meas~ired at iupersatu field tests car'ried om Moscow in June -1964.. Resu out at a rurai-locality -including th Its obtain 0 .se of the aut .0 ed by different-investigators, Card' 2 br,.are presented .(see Fig At 04 supersaturation of UDC. 551.574.11 trationg once nuejej .66 n648 OadVOat' b tjoifts hP6003241 IF1.9p I. supetsoura in (DC low is dat -jod" 11V0 PeA. ordiAvl- to a acrovdius 4 Nee .1 dutinS method :3 ental. a contin- ten olatir ed by the 2 1 1964); C _. In r ..Proces, .3. 4 310-e , the same k --a io dat! .1.964;b DC to OUT june lts 0ktag 3 the resu . but ta aing ~tq~ t1yose, Of 2 i size C/ acr-Or Vffic'se. 3e~meutg as e droPS thOs 4_ordiu sieas.ur Uut Only sizei. seco 5*. into et 3e~ed_the Ista. e 43 ds- th Twome3 S, to Vielan . cent- % S__ tOjaciAe - ;ELIV30S Of 0.1 per Metbod .- Cation .11: ~it'h ro OSa,. ersatul ve lei for t a 6 11 'ire- agree jiuc d 11% talveA bf . rLsatioll jip gult, obtainea by e a factor 0a Of..coade an _lau v0ectra le re. bY a esp Australia r.ther thau t, bu, disagree Of, couaell, es _1U tiou Sp :deteTv's%A bag ,result spectra Discrep t do-of ~art- ljowever land - tt IOTIS- 'd 1WIC jaturatl 'it ~Ucla pis', t6ine es 0 TD TV e 0 P, -ob eat degrP ibed chiefly Ur Aif jet "u in the I asr-t 0031, OT e are ces 03. To," jal dif f eret' au651 01L 041 SUS card L 442?4-66 F,,,,tT(l ACC NRi AP6021464 A souRcu CODE: uR/o4l3/66,000/011/00811 /0084 INVENTOR: Laktionov. A. G. ORG: none ~0 TITLE: A photoelectric nephelometer. Class 42, No. 3.82362 /announced by Institute of Applied Geophysics (Institut prikladnoy geofiziki)7 - I SOURCE: Izobreteniya, promWshlerir*7e cbraztsy, tovarnyye znaki, no. 11, 19662 84 TOPIC TAGS: aerosol, atmospheric turbidity, particle sizing, meteorologic instrument, nephelometer, light scattering ABSTRACT: An Author Certificate has been issued for a p otoelectric nephelometer (see Fi g. I). It. is intended for recording the range o visi measuring v, Fig. 1. Photoelectric nepbelometer Card AMV 1 - Light source; 2 - system for observ ng the light scattering; 3 - device for extinguishing interfering light. 4 ACC NR, Am6o21464 the intensity of light scattering at an angle of, for example,450 to the direction' of illumination. Its measuring chamber is an open cylinder whic has facilities for: Wstructure and extinguishing interfering light to prevent disturbing the aerosl, for observations at any time of day and from moving vehicles. Orig. art. has: 1 figure. [F.01 suB com: o4/ SUBM DATE: 05Feb65/ L 07214~k7 EWT(1) ACC NR- AP6024432 SOURCE CODE: UR/0362/66/0021007/0766/0769 AUTHOR: Konyshev, Yu. V.; Laktionov, A. G. ORG: Institute of Applied Geophysics (Institut prikladnoy geofiziki) TITLE: Airborne photoelectric device for measuring cloud \drops SOURCE: AN SSSR. Izvestiya. Fizika atmosfery i okeana, v. 2, no. 7, 1966, 766-769 TOPIC TAGS: photoelectric detection equipment, measuring instrument, cloud physics ABSTRACT: This article describes a new airborne photoelectric cloud-drop measuring device which is based on a photoelectric nephelometer. The optical system of this device has an incandescent lamp which illuminates a diaDhragm with a square hole. In front of the diaphragm is a lens which projects the image of the filament onto the inlet of the objective lens. The objective projects a slit into the vicinity of the point of intersection of the optical axes of the condenser and microscope objective. The light scattered by the drops investigated is focused with a 3.7-fold magnification onto the plane of a diaphragm with a square opening by means of the microscope ob- jective situated at an angle of 90* to the axis of the condenser. The light passing through the opening in the diaphragm strikes a photomultiplier. The electrical im- pulse from the photomultiplier passes through an emitter follower and broad-band aw-- plifier to a multichannel electronic recorder. The instrument described permits mesa- G1 1/2 UDC: 551.508.765 L 07214-67 uring drops with a diameter greater than or equal to 25 p. At a flight speed of 70 m/sec the instrument can measure in one sec the drops in 500 cm3 of cloud. This volume marks the minimal concentration of drops at which the instrument can give statistically reliable results. Orig. art. has: 4 formulas and 2 figures. SUB CODE: 14,04/ SUBM DATE: lOJan66/ ORfG REF: 005 Card I -- T-AKTION017 --A-. Lm-j-- -- - ---- - - -- ---- - -- - I I LAKTIONOV) A. (Chief State VeterinEry inspector, "or accuracy 311c; hii?h quality of -.-,ork. So: Veterinariya; 23; 1; January 19h6; Lnel. TABCON 0 0 0 0 0 * 0 0 0 0 0 0 0 0 0 * * 0 0 0 4) 0 0 0 0 0 0 0 LSSR/Medicine - Veterin.- y Medicine Many 19117 Medicine - Encerhalomyeliti-c "Infectious Dicephtlomyelitis in Horsee," A. M. L--ktio-qov., 4 p-p "Veterintri-?t" No Lists doctors and their articles on the disease'. Among them axe F. Z. Amfite--trov on EM menin- Gitis, M. G. Nikitin, member of the educttiontl board for the Veterinary Institute ?~t Khar1kov on his observntion on epizootologieftl infectious encephilamyelitie and sever!!.l othcre. UKTIONOV, A. CM) "About the causes of infectious anemia of horses." SO: Vet 27 (2) 1950, p. 8 0 0 0 * 0 0 0 0 & * 40 0 0 0 0 0 9 0 0 0 0 0 0 0 0 0 0 * , A iq , ", Lt'r~-! : h.) ~~ Veteri.rzar.v !avs ard' Veterinar,'?code c-l" 'UhE USE11~ Kolkh. prcizv. 12 no, 1952 9. Monthi List of Russian Accessions, Library of Congress, 195T.- Uncl. LAKTI0:TC;V, A. 11-11. .,e Veterinary M dicine Problem of veterinary serivee in the consolidatej collective form. Veterinaria 29 No. 8 1952. Monthly List of Russian Accessions, Library of' Congress, Oct. 1952. Unclassified I LaTIO'.1-ov, ~.. 1%.. "Infectious Equine ;me-A&." Lr Vot Sc,-, All-Union Inst o1 Exmr-Jjrerta2 Veterinary Sci, loscow, 1953. (-RZ~Bial, Na 8, T-ec 54) Survey of Scientific anC- qechnica-1 -L.issertations --efen~-.e~ at USSR Highcr Educational Institutions (22) SO: Sun.. IN-0. 556~ 24 Jun 55 L,,~ K7_1ONC I/ 1 /1 - "91' Category: USSR /Diseases of Farm Animals - Diseases Caused by Bacte- V-2 ria and Fungi. Abs Jour: Ref Zhur-Biologiya, No 106, 1957, 72272 Author Laktionov A. M. Inst NoCgiven Title The Study of the Determination of the Properties of Experimental Allergenic Methods of Diagnosis of Epizootic Lymphangitis. Orig -?ub: Veterinaria, 1957, No , 72-79 Abstract: Two allergens (A), No 1 and No 2, prepared from one freshly cul- tured strain of Cryptococcus for the diagnosis of 1. epizootica (LE) in horses were tested in "W". A was tested on healthy hor- ses, those with LE, glanders, strangles and on "Malleinshchikakh" horses. The reaction towards No. 1 was determined by the thicken- ing of the skin fold, and towards A No. 2 by the area of svelling of the skin in 24, 48 and 72 hours. Positive reaction towards A No 1 in LE horses and mules was found. in 92.43 percent,doubtfLJ in 1.13 percent of the cases. In healthy horses 99.45 percent reacted negatively; the reaction was negative also in all animals with Card 112 -1- Category: USSR/ Diseases Caused b,j Bacteria and Fungi. V-2 Abs Jour: Ref Zhur-Biologiya, No 16, 1957) 72272 glanders or strangles which came from farms containing no LE. Similar results were obtained with the use of No. 2. For example, in 25 percent of horses which reacted towards A No. 1, and in 18.18 percent which reacted toward A No. 2, a general rise in temperature vas observed. A is recommended for use in the fight against LE in KNR- Card : 2/2 -2- Is iclul" il,,~~., 2~), 1o-3, 904