SCIENTIFIC ABSTRACT MAZILU, A. - MAZIN, YU.A.

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SCIENTIFIC ABSTRACT
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ZAGUMU I I. p dr.; SUCIU t 1. p dr. i -M-IZIL'ljA. . Cir . Observations on the incidence of arteria2 bypertenBim in a rum2 envirronwnt. Mad. intern. 14 no.2.*261-265 F 162. 1. Lucrare efec-tuata in clinica medicala Iq Cluj (director: acad. Aurel Moga). (HIPFMFMION StAtiStiCS) (FJIVIRONMM) (RURAL HEALTH) MAZIII., AlexarAM, ing. Economic calculation of the headwater channele. Enargetica Rum 11 no.7:3"-349 -T1 163. i 2 OS, beam WMpr ~mc," u i cl .............. & " The, sts f. ei edin n 6 dc5 : r;pans su -Monea on Col. MAS, --IMZLW,-Vicolae Tecbnlcal and organizable plan of action in Bmumian plants. Munca sindic 7 no.2:18-21 F 163. 1. Responsabil al comisAei pentru problemale intrecerii socialiste a comitetului sindidatului u-zinelor 00telul Rozu",-regiunea Banat. VdilA AnIMR126 Cattle. tist 2 - 7371 o 110 6 Author i : Baies, A.; AU4 1a" Inst _ _ : Timisoara ~Sstitute-~:qf. Agrqn~my Title , : The:~Jnfluence-.,of T~Ppqr4tur'e_.on.the.',Ud et, tke ' a-Pactor Rai sing.. ~ the -Perc entage o Yfit in the Hilkl*;.of~~-Oows..~ Orig Pub so Anuarul- lucrar,.,.vt11nt, Inst.',agr.6' Timi- n, soars,, BucureBti-o. 1957,., 221-237 Abstract 'm I 't ht in 'Inbrder_~to-.ralse the lkls fa con 6 cows, warm compresses were employed in one group, In another hot applications. Eighteen cows took part In the experiments, divided Into 3 groups, At the first stage the prepa- ration of the udder for milking consisted In Its being washed with water of the same temp- Cat'd ~'-!/2 nit 19 7Z rRUHANIA Prof Ch. LUPASCU, Or Aspasta BOSSIF-AGAVRILOAEI. DS"M"' ioj.gi.t~SKI. 'Dr Eugenla NECULICI-BALLIF, 1Dr Plereta CONSTANTINESCU Tr ISFAN, Or D. PETREA& Qr V. AZILU and Or V. ROHANI Institute "Or, I. Cantacusinot" Laboratory of Malaria and Pathogenic Proiozoa (Laborstorul do malarle s1 protozoare patogene) Center of Sanitation of Paludism (Centrul de Impoludare terapeutica) "Bercent". Hospital (Spitalul) "Ch. Marinescu" and Malaria Stations (Stattile do malarle.) "The Problem of Quartan Malaria and the Malaria Eradication Progran6l' Bucharest, Hicrobl" Is, Parazitologia, Epidemlololtia, Vol 8, No 2, mar-Apr 63; pp 99-112! I I Abstract [ Engl lab st-ary codified] i Quartan ma laria seoms'ospecka 11 v difficult to eradicate due to spontaneous recurrence of ancient infection and costa where parsoltemia Is so slight am to be virtually undiagnosable, caming transmission via transfused blood. in 1949, 215 of 50,ODD (0.4%) cases were quartanj 1960-1962, 71 of 1341 Craph, 2 tablenj 5 case reportal It Rmanian, 3 9owlet,1B Western references. Lin ffp Im ~-~ ': _- - - - -- , I a/ -- / UTP (b) Pz-6/Pr-4/Ps-h/Pu-4.i TJP(c) WIJDAPd i_. 1~ '- -- 7" - -- 1~ I- . :-~-APS-6099-44 i d7 .,~?,AMHOLINSKIY, F., kamd. med. nauk, pkkovnik weditsinskoy sluzhby; MAZIN, A., polkovnik maditsinskoy sluzhby Keep heart and nerves well in hab4g Kryl. rod. 14 no.5:34-36 163. 1411P+ , (MIRA 16:7) (Parachuting) WIZINq A.G. Speed up the' dobstruction of mines. Sov.shakht. 10 no.5:6-7 My 961. (MIRA 14:9) 1. Zanestitell nacballnika Glavnogo upravleniya ugollnoy, torfyanoy i slantsevoy promyshlennosti Vysshego soveta narodnogo kbozyaystva RSFSR. (Coal mines and mining) MAZIN9 A.G. ":!z Potentials for increasing the efficiency of capital investments in the coal industry. Shakht.stroi, 6 no.2:1-4 F 162. (MIRA 15:2) 1. Zamestitell nachallnika Glavnogo upravleniya ugollnoy, torfyanoy i slantsevoy promyshlennosti Vserossiyskogo Soveta Narodnogo Kbozyaystva. (Coal mines and mining-Finance) AGAMHANYAR.. N.A.; ZHAROV., SG.; KALINICHENKO, I.R.; KARPOVA, L.I.; KAPLAN, Ye.Ya.; KMNETSOV, A.G.; OSIPOVA, M.M.; MAZIN.. A.N.; SERGMNKO, A.V. -.1 ---- l.,----- Effect of various rates of decompression on the human bod Voen, med. 2-hur* no.lOt49-53 0 165. (MIRA l8tl7l WIN, A.P., kapitan. voyennyy letchik pervogo klassa First-class personal training. Vest.Vozd.Fl. no.8:42-44 Ag 160. (MIRA 13:9) (Flight training) man, B. Extracurricular conferences of students on educational topics. Prof.-takh.obr. 15 no.1:27 A '58- (HIU 11: 1) 1,Pomoshchnik direktora po dullturno-vospitatelinoy rabote tekhnicheskogo uchilishchs No.14 g. Moskyy. (Student activities) A-ft NOTER, lns;b.; GOLMIOVSUY, Yu.M.., inzb.l MAZIN,, B.A.3, inxb. Tbze*-Vbase bridge-typo transiotar frequency converter. SUktrotekbmika 34 nD.lOs64,-68 0 163a (KMA 16: 11) . it HAM, B.S.; PETUKHOV, LN.; KUROCHKIN, P.G. Use of periclase-apinel bricks in the regenwator checkerwork of open-hearth furnaces. Stall 21 no.8:699-700 Ag 161. (MIRLA 14:9) 1. Beloretskiy metallurgichookiy kombinat. (Open-hearth furnaces-Equipment and supplies) HOIII, I., inzhener. Ravine the construction of equipment for unloading grain from railroad cars. Nuk.-elev.prom. 21 no.12:6-9 D 155. (KM 9:4) I.M= Ikovskeye otdoleniye Promserneproyakta. (Grain-Transportati*n) (Loading and unloading) KAZIN. I., Inshener. i,tie,* -rar- Muk. _T s, of lowering the cost of elevator construction. -elev. prom. 23 no.8:13-16 Ag '57. (MIRA 10:11) 1. Zhar'kDvokaye otdolonlye Prousernoproyekt. (Grain elevators) (ConstruOtion Industry--Costs) KAZIN, I., I-nzh. - Pamphlet on the Installation of grain d;wts (*Construction and installation of grain ducts In elevators and grain dryers" by N.M. Tullchineldi. Reviewed by 1. Kazin). Kuk. elev. prom. 24 no.1:32-3 of cover Ja 158. (MIRA 11:2) (Grain elevators--Equipment and supplies) (Tullehinskii, N.M,) MAZIE, I., inzh. Introducing automatic unequal-arm scales at grain elevators. Muk, elev.prom. 26 no.7:14-15 JI '60. (MIRA 13:9) (Scales (Waighing instruments)) VW MA.ZIN I. inzh, Revise standards for planning grain elevators and grain receiving stations. Huk.-elev. prom, 27 no,4t28-29 Ap 161. (MIRA Ut7) (Grain elevators) cerning -the Fatigue of Metals. Metallurgical Abst. and kin W. ~V..k h*)?., Vol. 21 Apr. 195/+ 78. 12): Rumiall). Some Nublished empirical formulv for inten)reting fatigue (Wa are iscuseed. Properties of Metals Tben. oil t lie basis of a mi.. 10 physical model of the formation of printary fatigue crack,,!' file 'relatiTl A' = Nord(A - Aj b detluced for A -_ A, with AT-)- oo for . 0. In this expression, A is the amplitude of strew for racture after X cycles, a is the const. of proportionality in the equation dS = aSdA (where S is file general area of ck-avage in unit vol. for one rycle) and A, the critical value of A at which cleavage begins. Published experimental data for C and alloy steels agree well with this. fortnuts.-G. V. E. T. . . PAZINO I.F. CalcaUtion of the deposit of Trutly TBAO no.7a.39-0 152. (E~rgroue try) (Drops) 6 L, 3, 0 7 -"-) 3 0 3 drops on rouniL cylindriwa armeaces. (Miak 8:5) tz~ ~, 11 ~,J, -J~ j , KMIAN, A.Kh.; MAZIN, I.P. Computing the errors of aerial droplet samplers. Trudy TSAO no.12: 3-12 ' 53. (HIRk 12:1) (Meteorological instruments) firn Y-4 -4- ) /V, , -Z- , 'P. KERGIAN, A.11h.; WIN, I F. Analyzing methods for describing spectra of cloud particle dispersion. TrudyTSAO no.17:36-46 1 156. (ML'RA 10: 3) (CIOUIS-49'pectra) llkZI:T 1.3 I.P. C...nd 17fqo--katli Sci (diss) "Mysical principles in the iciriC-over of vroVMmr-&-Iven and jet-propblled airpLanas-ll (Ilbs., pifo. by USSIR Allcad scil 1957- 10 pp 22 cn. (1-11ain Gcc~-,hys Oil" - Cbserv ir~ A.I. Voyeylov) 120 copies (Y1, U-57, 96) 2 PHASE I BOOK EXPLOITATION 512 Mazin, 1. P. ................... Fizicheskiye oanovy obledenenlys samoletov (Physical Principles of Aircraft Icing) Moscow, Oidrometeoizdat, 1957. 119 p. 1,000 copies printed. Sponsoring Agencies: Glavnoye upravleniye gidrometeorologicheskoy sluzhby pri SoveteMinistrov SSSR, and Teentrallneya serologi- cheskaye observatoriya. Ed.: BoroVikov, A.M., Subbotins-, G.B.; Tech. Ed.: Zarkh, I.M. PURPOSE: This book is intended for meteorologists, synoptic forecasters, and aviation workers interested in aircraft icing phenomena in flight. COVERAGE: The author discusses the theoretical and experimental problems of aircraft icing in flight including the influence of physical Ca rd 1/1 '2 Physical Principles of Aircraft Icing 512 parameters of clouds and the Influence of the operating conditions of aircraft on icing Intensity. He considers theoretical problems of the flow of air containing suspended drops of water over various bodies.. and the role of heat transfer processes which diminish the intensity of aircraft Icing* The author states that the problem of icing changes constantly.and the prevention of icing takes new forms. Newly designed aircraft may be particularly susceptible to icing in some atmospheric conditions. The probability of icing is different for various types of aircraft. New problems arise,, for example,,the icing of helicopters and the internal icing of jet engines. On the problem of icing in supersonic flights, the author states that theoretical considerations provide answers to many important questions., e.g..,intensity of icing,, Its dependence on cloud structure, etc. The theory of supersonic air- craft Icing presented in this book Is based on the supposition that a substantial heat transfer to the interior surface of the airfoil takes place. This supposition is not based on concrete data and therefore cannot be considered absolutely exact* It is possible that in some Card 2/4 'r-> Physical Principles of.Aircraft Icing 512 unfavorable conditions an unexpected deposition of ice may occur. In spite of the apparent accuracy of the supposition of icing at supersonic speeds, the problem should be studied in special experiment- al flights. Basic results cited in this work were obtained in the cloud research laboratories of the TsAO (Central Aerological Observa- torY) in 1950-1956. V.F. Bonchkovskiy and N.V. Lebedev are mentioned as working on the icing problems of supersonic aircraft. Graphs and the corresponding 5 tables of values in the appendix are taken from Bergman's report published in NACA Rep. 1107., 1952. There are 83 references, 34 of them Soviet, 39 Englisho 4 German, and 6 translations into Russian. TABLE OF CONTENTS: Preface 4 Card 3/~ W, f. P. "on the icing et High-Speed Aircm-rt,," by I. P. MftzIU,, JGeteOr- ologiya I Gidrologjn, No 4, Apr 57, PP 3-8-- This article presents theoretical data, based on the literature, to show that, if the theory or the absence of beat loss Inside the ving of an aircraft is correct, no icing can occur at supersonic ve- locities, even in rare cases of flight in strongly supercooled clouds vith a below-freeziug temperature at the surface of the aircraft. It states that experiment must shov how accurate this conclusion is and bov accurate are the assumptions on vbich it in based. (U) /,A( /, /0 AUTHOR: Mazin, 1. P. 49-4-17/23 TITLE: Some problems of icing of propellor driven aircraft. (Nekotory7evoprosy obledeneniya vintomotornykh samoletov). PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya Geofizicheakaya, 1957, No.4, pp. 534-539 (USSR) ABSTRACT: In studying the icing of various parts of an aircraft, the microstructure of clouds and the problem of purifying air and various other problems, it is necessary to calculate thq probability of collision of aerosol particles with bodies of various shape (e.g. circular cylinders, wings and propellors, etc.) during their movement relative to the air. For calculatinG the degree of icing, it is necessary to know the coefficient of "encroachment" E of the winG profiles for given stream- lining conditions. The coefficient of "encroachment" A is defined as the ratio of the cross section of a flow tube (in the non-disturbed region), formed by the extreme trajectories of the aerosol particles which still collide with the body, to the "mid-ship" cross section of the body. Determination of A is reduced to finding the trajectories of the aerosol particles near the body, i.e. to integrating Card 1/4 the motion equations of these particles,written in the Some problems of icing of propellor driven aircraft. 49-4-17/23 L non-dimensional form, Eq.(l), P-534; th-s equation represents an inversion of a system Of non-linear differential equations of the second order for which only numerical integration is possible. The trajectory of the particles and, consequently, the value of A depends on two parameters p (inertia parameter of the drop) and Re (Reynolds number for a drop of the radius r and th.8 relative speed u ). For a number of cases and Re 0 values %re calculated by Bergrun, R.N. Ref.6). Bergrun and L, M. Levin paid particular l attention to determining the critical parameter of p at Which the drops do not collide with the body i e for P4g Per the coefficient E = 0. Bergrun publishLd*a graph of the dependence of Pcr for a symmetrical Zhukovskiy profile on the relative thickness of C and the coefficient of lift force C . Levin gave an analytical relation for p fo~ Zhukovskiy profiles in which the dependence no?ronly on 0 and C but also on the bending of the profile expressed iy the relative thickness f, are taken into consideration with Card 2/4 an accuracy up to the third order. In practice the .-0"0 Some problems of icing of propellor driven aircraft. 49-4-17/23 thickness of the icing on the critical point of the profile, determined by the local value of the "encroachment" coefficient E is of greater importance but very little data are avail9ble on this point. Data obtaine by L. M. Levin as well as the results of calculations effected by the Central Aerological Observatory (Tsentrallnaya Aerologicheskaya Observatoriya) and also E0 values for a 15% symmetrical Zhukovskiy profil.-, with a zero incidence angle (derived from the work of Bergrun) are entered in the graph, Fig.2. It can be seen that for p > 0.05 the influence of Re is relatively slight. Disregarding evaporation and heat 8xchange on the iced surface (which is permissible fgr speeds below 300 km/hr and an air temperature below -5"C) the intensity of icing at the nose of the profile can be calculated by means of Eq.(5), p.537. Some experimentally observed results confirm results calculated by means of Eq.(5). This is interpreted to mean that the conception of "integral coefficient of encroachment" and the here given methods of calculation express satisfactorily in the first approximation the phenomenon of icing of aircraft. There are 4 figures, 1 table and 8 references, 7 of which Card 3/4 are Slavic. . Some problems of icing of propellor driven aircraft. 49-4-17/23 SUBMITTED: November 11, 1956. ASSOCIATION: Central Aerological Observatory. (Tsentrallnaya Aerologicheskaya Observatoriya). AVAILABLE: Library of Congress. Card 4/4 SOV/169-59-7-7143 Translation from: Referativnyy zhurnal, Geofizika, 1959, Nr 7, p 97 (USSR) AUTHORS: Minervin, V.Ye., Mazin, I.P., Burkovskaya, S.N. TITLE.- Some New Data on the Liquid-Water Content in Clouds PERIODICAL: Tr. Tsentr. aerol. observ., 1958, Nr 19, pp 3 - 32 AMMACTt The data from observations of the liquid-water content in clouds are evaluated statistically; the observations were carried out in 12 points of aircraft sounding of the hydrometeorological service in 1956 and 1957, which were different in their geo- graphic position. The greatest number of observations were performed in stratified cumuli (1,625 observations of the total number 3,665). The methods applied to the evaluation of ob- servations and the quality of the materials collected are described in detail. Basing on the common considerations, the author obtains a semi-empirical formula connecting the liquid-water,content of the cloud with the temperature gradient and the altitude above the lower boundary of the cloud. Empirical Card 1/2 data on the dependence of the mean values of the liquid-water 60 SOV/169-59-7-7143 Some New-Data on the Liquid-Water Content in Clouds content on the temperature arid, moreover, data on the frequency of water content in clouds of different form in different temperature Intervals are presented. The data on the vertical gradient of water content aro Inter- preted empirically, and the connection of the water oon-%;ent with the alti- tude above the lower boundary is explained. A clear-cut connection of the average characteristics of the water content with the geographic position of the points has not been detected. I.P. Mazin Card 2/2 315000 SOV/169-59-5-4920 Translation fromi Referativnyy zhurmal, Geofizika, 1959, Nr 5, p 86 (USSR) AUTHOR- Mazin, I.P. TITLE-. On the Radio-Observation of Wind From A Moving Ship PERIODICAL: Tr. Tsentr, aerol. observ., 1958, Nr 24, pp 72 - 74 ABSTRACT. The observations of a pilot balloon from a moving ship by means of a locator stiffly connected with the ship's deck allow to obtain the coordinates of the pilot-balloon only relatively to the shipts deck varying continuously its orientation in space. The author developed in the article the correlations for the determination of the real location angle, the azimuth, the height of object, and of the horizontal distance of the pilot- balloon considering the motion and -the rolling of the ship. I.P. Mazin Card 1/1 IVANOVSKIY. A.IJ,,SZIN, I.P. --I Turbulent coagulation and its role in the Wovth of cloud droplets. Trudy TSAO nn.35:21-35 160. (MIRA 13:11) (Clodd physics) PAZIN, I.F. - SKO-SYNEVA, V.D. -ij--= ----I .- iForm of fall streaks, their representation on radar nephograms *nd relation with the microstructure of falling particles. Trudy TW no.35.-66-78 060. (MIRA 13:11) (Radar meteorology) (Cloud physics) M"qz/& ~0. PHASE 1 BOOK EXPLOITATION SOV/5852 Borovikov, Aleksandr Moiseyevich, Ivan Iva4ovich Gayvoronskiy, Yelizaveta Germanovna Zak, Vadim Vladimirovich Kqstarev, 111-ya Pavlovich Mazin, VkLdislav Yevgen' yevich Minervin, Aleks4ndr Khristoforovich Khrgian, and Solomon Moiseyevich Shmeter Fizika oblakov (Cloud Physics) Leningrad, Gidrometeoizdat, 1961. 458 p, 5000 copies printed. Ed. (Title page): A. n. Khrgian; Ed. : V. 4, Protopopov; Tech. Ed. M. I. Braynina and 0. G. Vladimirov. PURPOSE: This book is intended for meteorglogists and for specialists in fore- casting service and aviation. COVERAGE: The book describes modern methods of studying the development, structure and origin of clouds. Special attgntion has been given to the forma- Card lho Clo.ud Physics SOV/5852 tion of microscopic elements in clouds. T!)e macroscopic properties of clouds are also studied in detail. Their popition in space, motion, as well as their connection with thermodynamic struclure of the atMOBphere, general circulation, cyclonic activity, etc. are Invj!stigated. Flying in clouds is briefly discussed. One chapter deals with Cloud modification and seeding. The book is based on Soviet and non-Soviet sources. Ch. I was written by Ye. G. Zak and 1. P. Mazin; Ch. 11, by A. M. Borovikov, V. Ye. Minervin, A. Kh. Khrgian and S. M. Shmeter; Ch. 111, V, and VI, by A. Kh. Khrgian; Ch. IV, by A. Kh. Ehrgian and S. M. Shmipter; Ch. VII, by Ye. G. Zak; Ch. VUI, by A. M. Borovikov; Ch. IX, by 1. P. Mazin; Ch. X, by 1. 1. Gay - voronskiy; Ch. M, by V. V. Kostarev, V. Ye. Minervin and A. Kh. Khrgian. The authors thank L. T. Matveyev and A. M. Baranov. There are 632 refer- ences: 274 English, 254 Soviet, 71 Germarl, 30 French, 2 Hungarian and 1 Polish. Card 2 /10 42523 S/789/61/600/036/oOl/013 E032/E314 AUTHORS: Borovikov, A*M-j Mazin, I.P. and Nevzorov, A.N. TITLE: Some results of measurements of the size-distribution of large particles in clouds SOURCE: Tsentrallnaya aerologicheskaya observatoriya. Trudy. no. 56. moscow, 1961. Voprosy fiziki radiolokatsii oblakov, 3 - 13 TEXT: This paper reports an experimental study of the concen- tration and dimensions of large particles (radius > 75 u) in vari- ous types of cloud. The experiments were carried out with a speci- ally designed apparatus mounted on board an aircraft. The device was developed at TsAO by A.N. Nevzorov. brops entering the device pass through a standard light beam, which is continuously monitored by a photomultiplier. As soon as the particle enters the beam the Yhotomultiplier current drops and is transformed into a pulse which can he recorded either on a moving chart or with the aid of elec- tronic circuits. The geometry of the device is such that the air stream flowing through it is affected as little as possible by the instrument itself. The light beam passes through about 100 litres Card 1/3 S/789/61/000/036/oOl/013 Some results of .... E032/E314 of air per second at a flight velocity of 50 - 60 m/s. Thus, the cloud!-volume scan per minute is of the order of a few cubic metres.- The method, therefore, has clear advantages over the foil method described by Brown (Journ. of Met., v- 15, 1958). The first experi- ments were carried out in October/November, 1959, over an experi- mental meteorological polygon near Dnepropetrovsk. The device was .modernized in April, 1960, to include electronic counting devices ;so that particles in four adjustable size ranges could be recorded. ,The modernized device was used in April/May, 1960, near Villnyus, 'to determine the drop-size distribution. Altogether 446 determin- ations were made. Detailed results are reproduced in the form of numerical tables. It was found, in most cases, that the relation between the number of particles per unit radius range was an exponential function of the radiua. It was discovered that the presence of large particles in clouds was the rule rather than the exception. In a number of cases, it was possible to determine tne height at which large particles were no longer present and to com- pare this with the position of the lower boundaries of clouds. Such comparisons showed that large particles were found up to 100 - 200 m below the lower boundary of Ac and Cu clouds and I - 2 km .-.,-,Card 2/3 S/789/61/000/036/oOl/013 Some results of .... E032/E3i4 or more below As and Ns clouds. In fact, they appeared to be d\ the precipitation particles reaching the Earth. In isolated cases, ' large particles were recorded even above clouds. There are 1 figure and 7 tables. Card 3/3 s/o58/62/ooo/oo6/i 18/136 Ao62/Aioi AUTHORS: Borovikov, A. M., Kostarev, V. V., Mazin, I. P., Chernikov, A. A. TITLE: Relation between the magnitude of a radar signal reflected from a cloud and the cloud parameters PERIODICAL: Referativnyy zhurnal, Fizika, no. 6, 1962, 32, abstract 6Zh215 ("Tr. Tsentr. aerol. observ.", 1961, no. 36, 0 - 30) TEM The dependence of the intensity of a radar signal reflected from a cloud on the water abundance of the-cloud and other parameters is theoretically and experimentally examined. It is shown that the existing opinions on a de- finite relation between the Intensity of reflected signals and the cloud water abundance are not founded. On the basis of the reported results of experiments it Is maintained that the fundamental reflection of standard signals is condi- tioned by particles of a size > 200/u. [Abstracter's note: Complete translation] Yu. Mel'nikov Card 111 S/789/6i/000/036/oo5/013 E032/E414 AUTHORSt Mazin, I.P., Skosyrova, V.D. TITLE: On the size distribution function for cloud droplets SOURCE: TsentralInaya aerologicheskaya observatoriya. Trudy. no.36. Moscow, 1961. Voprosy fiziki radiolokatsii oblakov, 43-52 TEXT: L.M.Levin (Xzvestiya AN SSSR, seriya geofiz., no.10, 1958) has reported that the empirical data on droplet size distribution can be described by the so-called gamma-distribution n(r) = Araexp(-r/p) where a is a constant and A involves the incomplete gamma-function. However, he found that high values of a were necessary to account for 71% of all the data, while the results obtained at TsAO indicate that- a should be much smaller (2 instead of 8). The present work was undertaken in order to elucidate the reasons for this discrepancy. The new analysis was abased on airplane determinations carried out by TsAO in 1959. The reasons for the above discrepancy were found to be as follows. Levin's results were obtained with droplet traps located on the Earth's surface (Trudy Geofiz. in-ta AN SSSR, no,7A, 1954) and the Card 1/2 S/789/61/000/036/oo5/013 On the size distribution ... E032/E414 samples were collected from "compact" volumes of the order of 1 cm~ These droplets probably went through the same development process in the same part of the cloud. An examination of the Samma- distribution shows that such droplets would give rise to a high value for a because their radii are not very different and this was in fact observed experimentally. The TsAO results, on the other hand, were obtained with samples collected from volumes of the order of 1 to lo cn,3 with very small transverse cross-sections and length of several tens of metres. In the analysis of the data the final distribution function represented an average for different regions of a given cloud and also for different clouds. The average value of a was then found to be 2. Unless this averaging procedure is adopted much higher values of a are found to result. There are 1 figure and 4 tables. Card 2/2 DDROVIKOVp A,1j.; KOSTAREV, V.V,,; MAZINp I.P. Use of radar for studying the structure of clouds. Dokl. AN WIS-S" 140 no.31575-578 S 961. ~(MIRA 14:9) 1. TSentralInaya aerologicheskaya observatoriya. Predstavleno akademikom Ye.K.Fedorovym. (Radarl-leteorology) AUTHORs TITLEs PERTODICALs 8/050/62/000/005/001/001 D234,fD3DB Maz Second scientific conference of young specialists of the central aerological observatory Meteorologlya I gidrologiyaq no- 59 19629 61 TEXT: On February 12 and 13, the 2nd conference of young specialists took place at the Central Aerological Observatoryq where 13 lectures were hold. In the cowxunication of A.A. Cbernyakov, the results of an Investigation of physical nature and structure of di- electric inhomogeneities in the atmosphere causing radioechoeB of the. clear sky were given. The form of the ) am (closed volum- ee)9 their dimensions (hundreds of me;2Mhondoglinfeistipeersiod, (over 5-10 minutes) were established. High reflootivityp as well as high direc- tivity of reverse re-radiation led to the conoluslon that there are considerable gradients of dielectric permeability at the boundaries of the inhomogensIties, In a series of Investigations devoted to wind Card 1/3 S/05OJ62/000/005/DDI/001 Second scientific conference D234/b3os and turbuXence fields in the atmosphere (V.P. Belyayevq 11.K. Vinni- chenko, L,A, Pakhomov and V,D* Fatsayeva) those of L*A. Pakhomov oc- cupy an eminent place; he created am airoraft equipment for measur- ing the micro-structure of wind fields in clouds and outside then and obtained first data on the character of vertical and horizontal pul- sations of the wind in clouds of stratified formes as well as in those of convective development. M. Ya. Akeenov devoted his paper to electron microscope research of dispersion of ice-forming aerosols. A.I. Nevzo- rov reported oxi a device for measuring large particles in clouds and precipitations designed by him. in the lectures of O.K. Xostko, G.M. Martynkevich, A.V. Fedynakiy and A.P. Chishov the difficulties of mass spectrometric me&surements in the stratosphere were comprehensively treated and the methods of corresponding measurements were given a basis. Laboratory experiments showed that an omegatron with exhaust system and a tranBit time mass spectrometer can secure corresponding meaeurements at heights of 40 to 60 km and nor's If they are lifted. The possibilities of automatic processing of the date of rocket sound- ing of the atmosphere were discussed In the lecture of V.I. Koslov. Card 2/3 8/05OJ62/000/005/001/001 Second scientific conferetwe D234/D3W V.G. Kidiarove, devoted her co=unication to the wxiability of pres- sure and density fields in the free atmosphere. Abstractor's note: Essentially complete trarislation) Card 3/3 MA711,1; I.V, Method for evaluating the efficiency of thermal Wears with allowance for liquid water content and temperature of the clouds. Trud7 TSAO no.39:56--76 162. (MIRA 15-,6) (Air-planes- Ice prevention) (Clouds) I-C."ESSIC.-N 20.: Juk-011394 S/2789/63/000/047/0024/0032 AUMOU: Mazin, I. P. TITALE: "Age" of particles in stratiform clouds SOURCE: Teentral9noya aeralogichaskaye, obsorvatorlya. Trudy*, no. 47, 1963. Fizika ol)lskov, 24-32 TOPIC TAGS: meteorology, cloud particle, cloud, strat iform cloud, condensation nucleus, atmospheric turbulence, cloud boundary, droplet spectrum ABSTRACT. The age of individual droplets in a cloud can differ appreciably from the age of the cloud as a whole, robably as a result of turbulence. Mason's work on this problem is reviewed Ti. of met., 17, No. 4, ig6o, 459-468).. The author agrees, with Mason that the,agge of drops 13 determined by ;the turbulent mixing mechanism (in stratiform clouds) but points"out inaccuracies in formxxla_ tion of the,boundary conditions. It is impossible to accept Mason's conclusions because of his arbitrary assumption t"t all nuclei replacing.,drops perishing at the cloud boundaries are again propagated from the center of the cloud. The problem is reconsidered, assruning that drops which pass through the cloud bound- "y evaporate so rapidly that only condensation nuclei can penetrate into the I CDrC1 ACCESSION NE: AT4011394 cloud firom outside; the age of dro-os is doter='ined by the time of their single ~lifetime in thi cloud layer. A suitable equation is presented and solved for the concentration of particles pon~trating into a cloud in a-given period of time at a particialar cloud level at buy time. Expressions are derived for the dens-ity of the dura distribution and clistribution.of cloud particles by agesi that is, tion of their single lifetime in ;the cloud. The conditions of growth of particles entering a cloud through the lower boundary differ from those for particles entering through the upper boundary; their dimensions will differ even if they coincide in age. Appropriate formalas are presented for determination of the quantitiy of "upper" and ulover" particles. A graph can be constructed for .-finding, the deasit.*.of distribution of drops by ages different cloud heights. Orig. art. has: 16 for=tlas and 2 figures. f ASSOCIATION: TSENMIALINAU AERDLOGIC11ESSAYA OBSERVATORITA (Central Aerological Observatory) Summm: OD DATE ACQ: MM64 ENCL: 00 50 CODE. AS kw Mzzov. 603 02ala: 006 Card 2/2 GEYVANDOV, E. A.;-HA 1. P. I - Simple method for calculating the melting of hailstones during the fall. Trudy TSAO no. 51: 57-68 163. (MIRA .17:5) .77~77 k t a ze-41aftl M apa ze m e th U, - v imid qt- fT i -n AN ZS ~RR - Ar, b.:4, 1963) bar-- ed u ty'a b -droplets under variouB of n ldh,6tic ocpatioM desorib ng the Joint obilavlor Ja a] ~tl It ~turna out.-that-, in apite: of ups entlaHy different init I asouniptloi _j 9 ln~ 66 bf- pardele concentration -pow &r&6blelo-b4lilfi: Me ver a or. 6- Thfis 'w-- -a- s_e iftil j6ntally bb a arv 46d du rth obtady of the (11BUrbufti of exp -44~ '.r aba-'partic- 1e- forMffon. dloud partiale'size-distribution, stochastic th rqfndoi~. hum.1ditylielde ond . ensa.tionjp .ecipflatlo-n Iluclells eoryl I-lbo--,m7perimmiLd,da.t~--(A.M, Bofo,~rdkov Mazln,' A. N. Nevzorov, I P.- 3A ker. Jb-lidd --atm.'- i_ okcana- no '19,6%--indi te-that-thedistTibution -SUB: corw.::~ - ES I.T., DAVYDOV, Ya.A. Quick-catch draw-in collar chuck for lathes. M"hlnoBtroitall no.2t19 F 165. (MTRA 180) imp ij 31 31-j! 0j Ka.-F nschener-polkovnik. _nEiEU'XA__i On the problem of dry bomb-gpot photograpby. Vestjosd.Fl.34 no.12:8D-82 D 151. (KM 8:3) (Bombing, Aerial-Study and teaching) RAZINS 1111 0 Purifying the overhead of a -auolims stabilization ;~xoduct w-i+-)-, a monrethanolamine solution, Nefteper. i neftekhim. no.9;33-34 164. (;-mu 17;20) 1. Vigarskiy neftoperorabatyvayushchiy zavod. ~ . "r . - '~.l ( , -~ ~ -A, , Vy T F Di~ fj';,n trig J, c f, f, T riu, ri o , MAZIN. M.R. inzh. 0. Precision in the ai3sembly of reinforced concrete colwms of industrial buildings. Prom.stroi. 43 no.12:6-9 165. (MRA 18:12) Mm Z TN. , M. R. Standardizing molds for making precast concrete constructi'ans. Standartizatsiia 29 no. 11:39-41 N 165 (ITTRA 19:1) AT I with- a 4 laaum:~Ref 'Ut-- ___70 xide-~or -trip ion -of, Go 61~ssiui~phdsphate- Oium -hy.4ro of -:these~-__methods,-_ifit authors. describe a setup br uticiit-6~-z-mo-noethio~olbminqi now operatingat the- iLr id -f0 Y., The me. -prov e 6. - r mixing inoLmine'-solution - with the- initial'gas, -separation wt~, 1y -'k DEMIDOVIGH, V.N.; LL,'VGfll-,NYA, - Ilse of an electz-A-aminescent matrix screen. Geof-iz. pribo no. 12:107-112 162. (MIRA 17:5) 1. VI-101A. T-SLPENYUK, M.Y'.-,. [TSyper.1,J-, LEV V, F, _A7TN V, A., SUty V.B. Use r-f the naphthalene fract.ion in the prcduc,,.-.or, of wihydride. Khim. prom. O-D 16~.. (M:rpo T, 05069-67 EqT(m) J R/,G D A AT027933 SOURCE CODE: UR/0000/66/000/000/0170/0174 AUTHOR: Abagyan, A. A.; Belov, S. P.; Kazanskiy, Yu. A.; I ORG: None TITLE: Measurement and calculation of the coefficients of secondary gamma-radiation SOURCE: Voprosy fiziki zashchity reaktorov (Problems in physics of reactor sbieldin nborni-k stat-ey, no. 2. Moscow, Atomizdat, 1966, 170-1711 TOPIC TAGS: gamma radiation, neutron, radiation shielding, capture cross section ABSTRACT: The authors consider the coefficient of secondary emission 0 which expres- ses the ratio of the total number, dose or energy of capture y-quai,ta to the total num-i ber of neutrons emitted from a given shielding material. The general expression for j this coefficient is If OR, E) X,,., (E) nj (E) rs, Ej) d2dEdVds S(P (r,, Q, E) dQdEds where ID(r, 0, E) is the neutron flux at the point r in the unit energy interval at energy E and in the unit solid angle about the direction Q; Y,,., V(E) is the radiation capture cross section for neutrons of energy E; qj(E) is the yield of y-quanta of Card L 05069-67 ACC NRv A!ToUe-(Y_J_j energy Ej per capture of a single neutron with energy E; V(r, r,, E,) is the func- tion which gives the attenuLAon of the stream of I-quanta with energy Ej from the point of y-quantum production r to the points r, on the surface. A formula is derive( for the asymptotic value of 0 determined by the physical properties of the shielding material alone. A comparison of theoretical and experimental asymptotic values of B shows a systematic divergence by a factor of approximately 2.5, the theoretical data being overestimated. The reason for the divergence is assumed to be inaccurate deter- mination of neutron intensities at the boundary. In spite of the discrepancy between experimental and theoretical data, the nearly constant divergence obtained for various elements with large, small and moderate capture cross sections (tungsten, lead, iron and nickel) indicates that the proposed method may be used for calculating the asymp- totic values of 0 with an accuracy of 30% if a correction factor of 2.6 is used. The authors thank S. G. Tayn n and V. Ya' Pupko for interest in the work and useful re- marks. Orig. art. has: 3 figures, 6 formulas. SUB CODE: 18/ S70M DATE: 12Jan66/ ORIG REF: 003 Card WIN, Y.S.. inzh. (g. ZaporozbOye) .000~ ~Inves~~Igating graphic train sheets by analyzing the configuratio.-- of lines made by train runs. Vest. TSNII MPS no. 5:48-51 J1 158. (MIRA 11:8) (Railroads--Traffic) PERCHIK, V.P. ; MAZIN, V.S. Efficicincy of thL- trunfifer ,J Q~F.- approach tracka to the main rallrrm,in. dc,r. trP..,lr;p. 47 no.3:24-25 Mr 165. 1. Nachallnik s+.fintsii Mlokraya Fri ~nap.--vzJf -".Y drr,~gi (fnr- Perc-.ik.. 2. Starshiy inspektor ped"yezdnykh plitey Pridneprovskoy dor,-)gj (for Mazln~/. TSITSIN, N.V., akademik; CHERKASSKIY, Ye.S.; PROTSENKO, Ye.P.; MAZIN, V.v.,--- LYADOVA, G.L.; KILIMIX, Ye.Ye. Effect of the insecticidal and fungicidal repellent dust (IFRD-1) on cabbage clubroot. Dokl. AN SSSR 143 n0-4:972- 975 Ap 162. (MIRA 15:3) 1. Glavnjv botanicheskiy sad AN SSSR i Opytno-pokazatellny./ sovkhoz im. Mossoveta Lyuberetskogo rayons. Moskovskoy oblasti. (Clubroot) (Fungicides) MAZIN, V.V. Effect of boron and hydrGgEn peroxide on the inf-c * , k'n ; ~f cabbage with clubroot. Biul.. Glav. bot. sada no.56:7t-81 164. ( m -I, R'." 18 1. Clavnyy botanicheskiy sad AN SSSR. MAZIN V V - PERELIMAN, V.M., kand. med. nauk F,xcretory urography with compression in the diagnosis of diseases of the solitary kidney. Sov. med. 28 no.10:131- 134 0 165. (MIRA 18:11) 1. Brologicheskaya klinika (zav.- prof. I.P. Pogorelko 0 (deceased]) i 1-ya kafedra rentgenologii i radiologii (zav, prof. S.A. Reynberg) TSentrallnogo instituta usovershenstvovaniya vrachey na baze klinicheskoy ordena Lenina bollnitsy imeni Botkina, Moskva. MUIZiN V V Resection and cavernostony of a solitary tuberculous kidney. Urol. I nefr. no.2i27-30 165. 041RA l9gl) 1. Urologicheskaya klinika (zav. - prof.I.P.Pogorelko [deceased)) TSentrallnogo InstAtuta usoversheiistvovanlya vrachey, Moskva. KAZIN, T&A. Nottative d9vice for the ZD-7 type pressure costing machine. Llt.prolsv. no-5:29-30 V7 155. Mm 8:6) (Die east Ing; .r -P, AUTHOR: Mazin, Ya.L. 3 2 -12-6.35/ 71 TITLE: Short Reports (7) (Korotkiye soobshcheniya). PERIODICPL: Zavodskaya Laboratoriya, 1957, Vol. 23, Nr 12, pp. 1520-1520 (USSR) ABSTRACT: The author reports in this paper that in e. Soviet industrial plant, which is not mentioned here, a new hydraulic dynamometer was con- structea and introduced following a suggestion made by V.D.Shiroko- rad, which is described. It consists of a case which contains a plunger. This plunger is provided with a steel spiral which presses it in an upward direction. This motion is intercepted by means of a screw cap. Under this screw cap, %within the same space, a packing is provided (for the plunger) which consists of a metal ring with a leather coating. The free space in the case under the plunger is filled with oil. Here a pressure manometer is mounted. Pressure upon the external surface of the plvnger is transmitted to the oil below it and is indicated by means of a manometer. This device proved to be of use in connection with testing machines and presses. There is Card 1/2 1 figure. Short Reports ( 7) AVAIUBLE: Library of Congress " 2-12-63/ 71 Card 212 1. Dynamometer-Construction 2. Manometer-Pressure AUTHOR: Kazin, Ya.L. 32-12-64/71 TITLE, Short Reports (8) (Korotkiye soobshcheniya). FERIODICAL: Zavodskaya Labor-atoriya, '1957, Vol. 23, Nr 12, pp. 1521-1521 (USSR) ABSTRAZT: The author reports that in a Soviet plant, which is not inentioned here, two new kinds of quickly detachable screw clamps have been constructed and introduced. According to the attached dravring one of them, as usual, consists of a metal aro and a thrust bolt. A spherical support is provided as starting from the end of the are; the bolt has a straight impact surface and is provided with a per- cussion thread. Because of the backstroke, a safety look is pro- vided, which is released by pressing the vring of the half-winged nut. The second construction is similar to the one described above with the exception that here an ~~dditioaa_l adjustment on the thrust bolt is provided. In thia case the thrust bolt consists of trio parts: the one is similar to the one described above and is used for the definite adjustment of pressure. The other part of the bolt is a continuation of the first and has a screw box nut, which moves on Card 1/2 a projection of the bolt only around its axis and is further pro- Short Reports ( 8) 32-12-64/71 vided vrith an internal thread, to ~.Aiich corresponds the external thread on the first bolt. The box possesses a handle and a releasable looking device. This attadhement serves for the quicker aBjustinent as well as removing the sorew clamp. There is 1 figure. AVAILABLB; Library of Congress Card 2,12 1. C18mPs-Serew-Construction .7 141)11,11 1 ~~ I I /,;,I" .1/1-111~ -1 NAZIN, Ta.L. Centrifugal friction clutches used in screv cutting lathes. . Stan. I inatr. 28 no.12:36 D 157. (14IRA 10:12) (Lathes) (Clutches (Machinery)) 1;' ~' I ) , -. . ( I I - F Z_ I ' '. f).11 '~- . .- MAZ IN,, U11VII.-O --i - 11--Oiloo- Spacial self-centering lathe chucks vith radial and axial operations. Stan.i instr. 29 no.1:36 Ja '57. (KIRA 11:1) (Chucks) .-