SCIENTIFIC ABSTRACT KAGAN, P. - KAGAN, S.

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SCIENTIFIC ABSTRACT
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IKAGAN-, P.O.-Bej CAND PHYS-MATH SC.1 f"FuNCTIONAL SPACES C014- JUGATED WITH TM S, L. S013OLEV SPACEG AIID 114EIR APPLICATION TO BOUNDARY VALVE PROSLEM3 FOR DIFFERENTIAL EQUATIONS IN PAR- TIAL DERIVATIVES*" NOVOSIBIRSK9 1961o (ACAD -SCI USSR, Slat- RIAN DEPT. JOINT SCI COUNCIL FOR PHYS41ATH AND TECH SCIEIICE$). (KL-DVI 11-619 208). -12- I. lin(l, Kar :)I' ul-lothara,~.v on t.l;:3 J'rcvju,~nc;~ of' or-irr,~rx;~ in "wlliti Gor"..-. ln-ta domatolofji :L J K!Afudry iri. YJro-,,L~, I.-Oue 1"~) 1:--,264, IL) Anril 1953, (Lotci)is '~,',Iurnal ""f1d, LltLtv, '1949) A rill In, - I-- ~. I - - -i- ---- -- ---- .--1 1- 111 1-- -'11 !J '1 11 111 It o- -,! I Ili 11- L,-~~ 4!---!i1-.1 i . :--i,- - - .. a I --I- -.- - I , It 'LU lNot PHASE I BOOK Eamommou mt/4174 Leningrad. Glavnaya ge6fizicheskays observatoriya S01/2-8-99 Voprosy chislennogo Vrognoza i teorii k31mata (Problmms in Itumerical Weather Forec"ting and Clim ology). Leningrad, Gidrameteolzdat, 1959. 129 P- (Series: Its. Trudy, vyp. 99) Errata slip inserted. 1,000 copies printed. Additional Sponsoring Agency: USSR. Glamoye upravlenlye gidrameteorologicheskoy sluzhby.. Eds.s M.Ye. Shvets, Docto r of Physics andMatbemat1cs, aad M.1. Yudin, Doctor of Physics and Mathematics; Ed. (Inside book): T.V# Ushakova; Tech. Ed.: N.V. Volkov. PURPOSE: The publication is intended for specialists in the field of dynemic and synoptic meteorology and climatology, as vell as for graduate students in these fields. COVERAGE: This is a collection of 11 articles pubUohed as Noo 99 of the Trans- actions of the Main Geophysical Observatory imeni. A.I. VMneykov and dealing Card 1~ Pr~blems in Numerical Weather (Cont.) S(N/4174 with nev methods of numerical amLlysle prognosis. Individual articles are con- cerned with contiguous pmblemo of climatologyt temparatwe anomalies in J;he atmospbere, effect of the heat of condensation on premoure ebanges, numerl4al prognodis of.the pressure pattern affected by orograpble factors,and the hydro- dynamic theory of frontal cyclogenesis. References a"ampamy each article. TABLE OF CONTEM: Rakipova., L*R. Formation of the Mean Konthly Anomalies of Atmospheric Tswyerati~re 3 .R.L& Calculating the Effect of the Condensatton Heat Flow and of the Stratosphere an Change in the Pressure Pattern 15 Bcigdanovi, N.P. Approximative Evaluation of the Effect-of Rest Released by Condensation on the Change in Pressure Pattern Near the Ground 3T Du Sin-yuan'. More Precise System of Calculating the Irregulwities of the Earth's Surfeace in Numerical Methods of Forecasting 43 Card 2/3 Nil 3M 0711150-5~ - 2-4) 114' 5 AUTHOR: Kagan, R. L. TITLE: Influence of Condensation Heat Supply on the rrPossure ChanCe According to Time (Vliyariye kQnkn:3at*ior-,r--!,:h pritokov I.epla na izmenaniye dayleniya vo vremeni) PEPIODICAL: MeteoroloCiya i "idrole.-iyal 195); irr 24, m) 7-141 (USSR) A'93TRACT: In the article under review the change of the goopotential according to time is lnvesti~ated. Conoiduration is L~iven only to heat supplies caused by condens,,,tJ.Qn, -ahile heat supply lue to radiation is not taken into nocrjunt. 1'. 1. Yudip'B method (Ref 2) is used to determine the change in the reo- potential, both in the presence and absence of a cloud layer. For the heat oupply in layers I and III outside the clouds form-Lila (1) in used, and it is assumed that 9 - 0. Ipproxima- tion equation (3) is iiaed to determ:ive tha heat supply in cloud layer II. E is the heat supply due -to condennation for the mass unit per time unit in agitatood air. Formula (5) which is used to determine the geopotential in derived. Both the systrem of equations (10) for layers outside the clouds Card 1/3 and the system of equations (12) for the cloud layer can be SOV150-59-2-2125 Influence of Condensation Heat Supply on the Prej!!ure Chanj7e According to Time obtaine,d from this formula (5), The constantn contained in these equations are found by means of the boundary conditions (6) and (9). They are introduced into (10) and (12), &nd the problem posed is solved. A concrele case is then inves- t-.gated by way of evtnplo. On the grounds (,,,f the renults ob- tained the author concludes an followtv: 1) The influciice of heat supply due ti phase changes on the chitnfre in the geo- potential of isobaric areas at a considerable distance from the cloud in small. (Here and f,~irthir ohangas are dis- cuased in comparison with o1wingon in 4.-.loudloos atnosphere). The closer these isobaric areas appreach the clouds, 'the stronger becomes the influence. It is strongest at tile outer edges of the cloud. The signs differ at the different sides of the cloud. The influence is lowest in the center of the cloud. 2) If the isobaric areas are iinnediately above the clouds, the phase supply increases the geo:potential in the u,,)per part of the cloud in the case of heat advection, and decreases it in the case of coll advoction. For the levels of the lower part of the cloud and in the layer below the cloud phase supplies lower the greopotential in the case of Card 2/3 heat advection, and raise it in the case of cold advection. S07/5 0.- 5 3'- 2-2/2 5 Influence of Condensation Heat Supply on the Pressure Chani;e According to Time 3) If the isobaric areas of the layer art, situated above the cloud, the phase supply increases the goopotential in the upper Part of the cloud layer in the case of advection of cyclone eddies, and also in the case of cold advection. 4 The influence of heat advoction at different levels on the geopotential change exclusively due to heat supply through phase transformations can be compared, in the case of levels near the cloud boundaries .. to the influence of heat advection on the geopotential change in a cloudless atmosphere. The relative change of the influence of the eddy advection. due to phase supplies is not as great, but still considerable. The influence of heat advection and that of an eddy advection may have diffefent signs on different lovelm$ and may thus compensate each other. Thus, the influonce of heat supply due to condensation may vary according to -the distribution of heat and eddyadvection in space. The results obtained con- firmed the assumption of some scientists that the freeing of beat due to condensation may consierably add to the force of the cyclogenesis process. At the amme time the results per- mit numerical estimations of this effect. There are 1 figure, Card 3/3 1 table, and 6 references, 2 of which are Soviet. 31 ~614&4 0 S/050/60/000/05/01/020 BOO7/BO14 AUTHORt Kagan, Re L. ---------- TITLEs On the Influence of Heat Inflows During Condensation on the Vertical Air Currents in the Atmosphere PERIODICAM Meteorologiya i gidrologiya, 1960, No- 5~ PP. 3-10 TEM A method is given here for computing tk)oe instantaneous values of vertical velocity and of condensation in the\bloud Eroviding the cloud boundaries bj and b2 be known on the basis of a 9, en thermobaric field in the atmosphere. Formula (1~ is written down for computing the vertical velocities and is solved by means of the method suggested by M. I. Yudin (Ref. 2): formula (9). It can be seen therefrom that the vertical currents are safely determined in every point at given cloud b*undaries b, ana b2 by the heat advection- and whirl fields in the atmosphore. At b, - b2 the solution passes over into that for a cloudless atnosphore, which is also made use of in the practice. A comparison of the two aolutions reveals the followings clouds exert a considerable influence upon the vertical currents in the areas near the clouds. This influence is Card 1/3 On the Influence of Heat Inflows During S/050/60/000/05/01/020 Condensation on the Vertical Air Currents in 11007/B01ij the Atmosphere especially high in the cloud center. Clouds augment ttie innuence of the thermal factor M - RA T (R denotes the gas constant, AT is the heat advec- tion). The advection of the anticyclonic whirl promotes on a certain level the formation of positive 'W"-values, i.s. of descending current3 below this level and of rising currents above it. m-L ~1 is a quantity pb dt similar to that of the vertical velocity. p. is the standard pressure at sea level. The advection of cyclonic whirls exerts the opposite influence. By and large, the influence of the cloud consists in the air-engthening of the dynamic factor at the vertical passing through the respective point. The influence of vertical currents at the earth's surface decreases more slowly with increasing distance from the earth's surface in -the presence of a cloud, than occurs in a cloudless atmosphere. Conclusions given here are illustrated by Figs. 1 and 2. Thus, vertical curronts increase in the presence of a cloud in consequence of phase heat inflows (heat inflows in consequence of condensation in the time unit for the unit 4of mass of the shifting air (Ref. M according to their absolute magnitude., This increase Card 2/3 On the Influence of Heat Inflows During 8/050J60/000/05/01/020 Condensation on the Vertical Air Currents in B007/BO14 the Atmosphere is of the same order as the one at vertical currents in the respective thermobario field in a cloudless atmosphere. If the vsrticaLl currents in the atmosphere are known, also the amount of humidity oondtnued in the cloud can be computed from formula (14). It is shown by Fig~ 3 that the condensation of humidity is promoted by the following factorst heat advection at all levels above the respective point, low-toutporature ad- vection above the neighboring points, advection o;Uantlcyolonic whirl in the lower half of the troposphere and the advection 6 -1he"cyclonic whirl in the upper half of the troposphere. There are 3 figures and 3 references, 2 of which are Soviet. '~' 5,000 Card 3/3 LAYKIfTMAN, D.L.;_ KAGAIJ,R.L. Some problems associated vith Improvod organization of mow surveys. Trudy GOO no.108:3-18 '60. OURA 13: 11) (Snow surveys) I :V' I. U- ) .' - . L . C.JCL~'. f " -.- r,--.-, . 1 -1, t: 13 I f - - i "'A .". .14:--l'?i 1 - , I'. - . - ~.4: ~) (c 7.,~ - -11 KAGAN9 R.-L.9 GAND P"YO-MAT" 3911 "EFrF.(,-T OF UTRATIrl- CATION'-Sf--DYPAUICS Of LAROE-SCALE MOVEMENTS IN T"E ATMOS- PHERE," LENINORAD, 1961. (LENiNoRAo ORDER OF LENIN STAtE UNIV im A. A. ZHDANOV). (KLI 3-61, 203). 48 GANDIN, L.S.; RGAN, R~L. Accuracy of determining the mean depth of tho snow cover from discrate data, Trudy GGO no~2300-10 162a (MIRA 151?) I- (snow ourveye) ..r 1% 1k-. KAGAN, R.L. Calculation of some meteorological elements a.Uowlmg for flows of condensation heat in clouds. Trudy GGO no.12.li67--79 161. (MM 15.5) (Mteorology) - KAGARP R.L. Accuracy of extrapolating the depth of the snow coi-.r in time, Trudy GGO no.130:38-50 162. (MA 15t7) (Snow surveysO KAGAN R.L.; 1AUH71-LAN, D.L. Optimum snow surveying methods. Trudy GGO no. 112:78-86 163. (MIRA 17:5) GANDIN, L.S. ; KAGAN R L- Accuracy of determining the uiearj value from dBarste data. Trudy GGO no. 112:87-99 163. (MIRA 17.,5) ACC=~ION NR: APLO23380 5/0049/64/000/002/0302/030$, AUTHOR TITLE: Computation of the inertia of an instrument during matoorological. MO&MUS-0 ments SOUI~CE: Ali S33R. IzV,. Scriya geofizicheakayap no. 2, 19641 302-305 ,MPIC TAGS: inertia, meteorological meaurement, meteorological e3ment., inertial instrument., ineetia free instrument, averaging period ABSTMACT: It is possible to obtain average values of a matearological element r for the preceding period of time T (the averaging period) in the record it massure.-! ments are made with an inertia-,free irwtrwwnt, But such inal;ruments an very complex., and treatment of the records are very laboriouse Tho metoomlogical element may be expressed by J.P,e) d~,,,.. ACCESSION NR: AP4023380 where t is the instant of time corresponding to the and of the aver*&g period* Inertial instruments we tommonly used'in praotice, therefora, and UA turbul4ab pulsations in the meteorological values are smoothed, The corrospouding function for the inertial instrument is' where T0 is the time constant of the instrument. The task here is to a ompare values of fl and f2 and to/determine the conditions under which thade differ least from each other. In this process the author has considered evrors in me&- surement to be negligible. He has determined the mean square difference betwom the values (0). Limiting cases are examined for T = 0 and T -;~ cc . It becomes clear in this examination that one may chooso, for W TO; a viaue for the averaging period T that corresponds to a minimal value Of e. Computztions are made for several specific values,"'and it 18 concluded that the results indicate that for the broad class of meteorological elements the optimal period-of aywaging, Card ?_/3 ACC ESS-510,11 M: A?40233 80 is approximately 1.73 times the time constant of a linear instrument. "in conclusion., the author eVresses his thanks to L. L4: Braginskaya for liar part in mre,:ing the computations." Orig. art. hast I figur4, I tablej " 26 forvwUm. AIS30CIATION.- Glavnaya geofizioheskaya observatoriyu im. A. 1. VoYG5,4cova (Nain Geoy.mysioal Obsexrratuory) SUBI-ELT 'I'm -. 22JU6~ DATE AGQt 217W64 MIGL 1 00 SUB CODE; AS NO REF SOV: '004 OTHER:. 001 Card 3/3 &~CIAE Y R. L. ; %ljjTj:jj:C)V, , K . 'Ya . Mapiling of radiation mcalurnment:9 rrom or~tellites- Trudy GGO no.166:227-234 164. (, U I u, I,,-, : I I ) L 14022-66 E1Yrj1)LfFCC G11 ACC NRs AT6004187 AUTHOR: Braginskaya, Ka L. L R. L ORG: none I TITLE: Precision determination of mean values using instantimeoua readings ol~ in4 ir- tial devices SOURCE: Leningrad. Glavnaya geof izicheakaya o~seSKatqrty.4. Trudy, no. 174, i 1965. Metodika meteorologicheskikh nablyudeniy i obrabotki (Methodir of ileteorologWil observation and processing observation data), 3-20 TOPIC TAGS: meteorologic instrumentl meteorologic observatiwm, extror functloji, error correction, inertial equipment ABSTRACT: The authors examine th oblem dealing with the accuracy of subs.0tuting grg averaged values of meteorologipq ements for a certain t1to period using inst~tntaneous readings of inertial devices. It is shown that the optimum period of averagilig the readings for a linear device is approximately 1.7 t(mes grestor than the constitnt i4ne of the device. orig. art. has: 24 formulas and 9 tables. 111ased on author'll abstract], SUB CODE: 04/ SUBM DATE: none/ ORIG REF: 004/ Card L--L49Z1--f&' 514 1 U ;r all ACC NRs AT6004188 N SOURCE CODE: Ult/25~3l~105/(',100117410021/!OOA AUTHOR: KH ~,R.~L. ORG: none TITLE: Calculation of inertia of a device for teorologic mit4witr0oxints SOURCE: Leningrad. Glavnaya geofizicheskaygl obseygt9r Irrudy no. 174, 1965, Metodika meteorologicheskikh nabludeniy i obrabotki (Methods of meteorological! observation and processing observation data), 21-34 TOPIC TAGS: meteorologic instrument, meteorologic o"b rvatiom, error measureftntp, error correction, inertial equipment ABSTRACT: The author analyzes the problem of accuracy of reullngs ~of an inertial device which characterizes the instant and averaged values oT the m*asured maA.,nitVide. The effect of inertia on the correlative functions obtained bil, an watp-erimental methlod .is evaluated. Orig. art. has: 52 forumlas and 2 tables. (8-ased on author'o abstract]. SUB CODE: 04/ SUBM DATE: none/ ORIG REF: 005/ OTH REP., 001/ -Card 1 1, 1 1 j:, r I fl j,i ,l - ;-;- , t..' ati. - :,. 'r:-,'Y GC' I '~ 1 -1 'V) "o .4 ; ~lp , - ( I LAI 1. ~ 18 ) L 14217-66 EwT(1) w ACC NR: AT6004197 SOUPCE CODE: (JR/2 01/6 5/OOD/1711/01.4 0/0114 AUTHOR: Kagan, R. L. ORG: Main Geophysical ObservatorLL to atori- (Glavnaya Si izieliel kaya obt. irv ya) 4q, TITLE: Calculation of tbvimol lMxqs in the cl-ptidles-.t., atmosphere _rAdjalLoIL f SOURCE: Leningrad. Glavnaya.geofizicheskaya observatoriyai~ rruajf, no. 174, 1965 Metodika meteorologicheskikh nablyudeniy i obrabotki (Yatlields of~ mateorologica-1 fob- servation and processing observation data), 158-174 TOPIC TAGS: radiation intensity, heat radiation, ozone, Wimsphimic radiatlon q ABSTRACT: The author considers various proble-,ms involved In usitig computeVa fot calculating thermal radiation fluxes. It is found that XbjjdVat1j1v-Nii1isk tranEimis- sion functions give results practically identical to thase'of Sl!iikhkter fund'tiolds in calculating flows of ascending themal radiation in the cloidleop atmospheve without consideration to the presence of ozone. Accounting for tho' albedia of the ~~derlylng surface for thermal radiation introduces Blight correctionm into: the calcul.~tio~s Card V2 L U217.& ACC IIR: AT6004197 .which may be disregarded as a rule. Outgoing radiation flini iat tlic boundary ~af ~he atmosphere may be identified with the flow of asconding rad liat Lori' at. the 10Q mb lev- el within the limits of computational error. fn calculatiliji the iiscenang, vidia-' tion, data on standard isobaric surfaces may be used. When ~calctillcrting &84;anding and effective radiation, it is necessary to use data from porticti.1ar sounding pa-"nts. Random errors of 20-30% in determining the humidity at high,, leveip introducit! 'Comp-ar- atively low errors into the results of tho calculation. Thil reli*Ive humidity or downward dew point deficit may be extrapolated when there aive no iMita an th,i,- taimj.di- ty for these levels. The accuracy of flux calculations usiillig thl~ proposed iiatho~[ is comparatively low (relative errors of up to 5% are allowablil!). t1hill calculati.6na,may be made more accurate by taking account of the pmsence oil itiacne !arld the ground I.ev- el temperature discontin-eity.' Orig. art. has: I figure, 8~tabldsj, 23 forrilAas. SUB CODE: OB/ SUBM DATE: 00/ ORIG IMF: 003/ OTH REN ~105 Card 2/2 .. . ... .... KAGAIJ R. L. of dr~tr.rininirg thi nrivi ar~--crdlrjrf, to ttala of pol,,nr, Trudy G';O n-,,! 5.-!*;7--i~'~. 1~r, (MIRA. 1W) 1. Gl,,.t-vndia in. A.I.Vayeftova, Lanipgrad, t ,T -. '7 5 S - t) _7 -AzC-7qV- AT6029354 SOURCE CODBi UR/?53lA6/OcA)A91/C,035/d0h6 AUTHOR: Guahchinap M. V.; Kagan, R.-L. ~17 ORG: none TITLE: Statistical structure of a ecipitation field ;SOURCE: Leningrad. Glavnaya geofizichoskM observgt Trudyi, no. 191, 1966. iPrimeneniye statisticheskikh metodov v meteorologii (The application of statistical 6thods in meteorology)) 35-46 (fOPIC TAGS: practical meteorology, rain,, diurnal variation., otatistic analysisj Icorrelation statistics, error statistics., mean square error IABSTRACT: Tho statistical structure of the rainfall field in north-central regions of ~the SSSR is analysed and the data is used for evaluating the accuracy of rainfall :estimates avbraged over a given area* Correlation functions wore calculated for the ;amount of precipitation over short periods of time at two points under three variantsr'-1: 1for days of simultaneous precipitation at both stations, days ithen there was rain at !only one station, and regardless of the presence or absence of rain at either station* ;The precipitation field has a well defined statistical structure and correlation ibetween the amount of rain at different stations extends for considerable distancess IThe territory and especially the topography of the region very significantly affects Card 1/2 L 01867-67, ACC N1, S AT6029361 1253,1661ooOA911012210132 AUTHOR: Kagan, R. L. 01,10: none \rK TITLE: Reduction of motoordlogigpl elements over an area ,SOURCE: Leningrad. Glavnaya geofizichaskayA oboorntgriyao Trudyp no. 191., 1966. ~Primeneniye statisticheskikh metodov v meteorologii (The application of statistical .~nethods in meteorology), 122-132 PIC TAGS: meteorologyo weather forecasting., weather station, stom,, atmospheric vement., wind velocity., rain, statistic analysisj correlation statistics., probability,! ast square method STRACT: The author had concluded earlier that in problems of reducing meteorologi I ca ements values of measurements at the center of an area could be replaced by values -eraged over the area. The present work discusses the correlation between values of meteorological element at a point and averaged over an area and the greater ac=,acy it tainable by exchanging the latter not with measurements at the central point but vithL ta obtained by some method of averaging, considering the statistical behavior of the ement. The method of least squares is proposed for correcting data at individual ints. The regression equation is examined: f I (f r, where f 11, is 5 0 0 (r,5 ord - 1/3 1 ACC NR1 AT6029361 Ithe avbrage value of the element f over an area S, IT + C are the mean square 'deviations of the averaged and the point values, and P is tRe correlation coefficient I ibetweon the point and averaged values. Errors obtained by using th13 regression equation are significantly smaller than when using data for the point at the center of the square. For occasions where To ~ ?,, such as rainfall ocemrring over on17 a part of the area, the probability of simultaneous precipitation at different points is calculated and the proportional value for precipitation is assigned to the central points The specific reduction coefficient p can be deterodned by integrating 2 2 P v(lV-x2+y2 )dxdy.- (23) 2 T if the relationship between the distance 1 and the probability v(w1-th coordinates x,y) of precipitation at a certain point is known. Examination of earlier data showed p depends on the 2area but is essentially Independent of the shape of the area. For areas, over 10.,000 km I p - < 0.8; for 1000 la~l area p, 91 i.e.p on days when it is rainingl at the station the rainfall depth over the 1000 Weis only about 90% of that at the station. There is comparatively little difference in the duration and recurrence characteristics at individual points and over the territory for local phenomena such as radiation fogs and frosts. But the probabilities of advectiva phenonena, such as rain and thunderstorms# change rapidly* Models styllzing data of the phenomenon were used L L 0186.7-67- ACC NRs AT6029361 'in order to readily establish aquantitative relationship between probability icharactoristics of the phenomenon at an individual point and over an area# A simple ,Model with a minimum number of parameters was constructed to simulate thunderstorms. IVormulas were developed for approximating the average duration of the storm at a given point and over a given territoryp and for determining the number of stormy days over ~the territory, Assuming wind velocity of 36 km/hr the average duration t . in hourej of the storm in a territory of r kilometers radius is approximately tr - to + 0.035r. The developed equations are not applicable to largo torritorien and do not provide for differences between frontal and air mass storms. However.. the data obtained Alom. these calculations compared favorably with empirical calculations described in A* No ebedev's works* It is concluded that formulas of this type can be used to approxLmate the probability characteristics of advective type phenomena. Origo art. hast 33 equations, 2 figures and 2 tables@ COM 04,v 12/ SUEM DATEs none/ MIG REN 005 Card 3/3,t.Y-(-- III I It 119 N 11111 li.,I 111; 1111111 a in I ~ I~ I L 079,03-6,1 G, ACC N"' AT6029352 SOUICS7 CODE: UR/2531/66/0G0/19l/0018/GCJ2" _Ga.-din,_L. S.; Kagan, R. L. ORG: none T.-'LL'-: Approximation for characteristics of a statistical structuro SOURGE.- Leningrad. Glavnaya geofizichoskaya observatcriya. 'Trudy, no. l91.. 1966, T'r :1 -'eneniye ta'is'icheakikh matodov v metoorologii (The application of statistical Mathods in matoorology), 18-21 TOKC TAGS: meteorology, statistic analysis, interpolation, correlation function A 3 ZAIACT: Statistical characteriz;tics such as correlation ;.nd structural functions are iT-.,-,)O-,tint :Ln the theory of rando-a functions as applied to ine parareers of these characteristics are determined by tha statistical tr6atment, of t an experimental material. The authors doinionst-Aate, for a one-dimensional case ho~ polation for a -meteorolojical elo-mant can be mwade by uz:Lng measurements of Vais clement at equidistant points. The opti,=1 interpolation sugCest.,d by Gandin is used, or s al b_nsad on t"a mathod of least, squares. It is also sho,= that ' he data , tatistic 5tructure can be used for find4n" the formulas of optimal in-vtoggration; howavar, the construction of the correlation functions requires more detailed information than needed for t7he solution of a concrete Problem. Ori.,r. art. has: 13 equations. SUB COD-: 04: 12/ SUBX DATE: none/ ORIG REF: 002 --,A 'I h ,I , L 0769 b.,67 ACC NRt AT6029360 functions. Tabulations are given of the values of correlation fuctilon3 for exponential, structures, of the relationship between correlation functions of averaged and Point values ,, of normalizod correlation functions of point and averaged values and of normalized cross-correlation functions of averaged nzirl point valuesp of factors calculated for various structural parameters, and of deviat,4 on and Carl-elation of .averaged values for various structural parameters, By using, these tables the trans.-Ition from point value functions to correlation functionu of averaged values may be readily accomplished. This is illustrated by examples basiDd on previously p-Xb1ished data wherein comparisons of spatial correlation flLictions of total rainfall at individual point3 and averaged over a given area, or of the time correlation functions of rainfall per unit time and averaged over a longer period,, are graphically presented. The tabular data presented may be used in evaluatir.2', other aspects of statistical structures Orig. art. has: 17 tables, 5 figures and 57 equations. ,sn com o4, 12/ SUBM DATE: none/ ORIG REF: GOV OTH REF: 001 i Card 2/2 T f ACC NP. AT6529358 AUTHOR Ka an, R. L. ORG: none TI-ILE: Optimal formulas for numerical integTation of random functions of a sr)Ocial kind '30b-RCE: Lening-rad. Glavnaya gcofizi heskaya observatoriya. Trudy, no. 191, 1966. - - L. . c Frimeneniye sta,.is'vicheskikh matodov v mateorologii (The application of statistical Tmethods in meteorology), 77-85 TTOPIC TAGS: correlation function, least square method, -wind, atowspheric turbulence I iABSTRACT: The authors obtained formulas for num crical inte'-~,vzition:; of stationary !random ftlactions with a linearly docreaoing correlation functf.;on. The formulls arel I I optimal in the sense of the method of least squares. The case of exponential correlation function was treated by Candin, L. S., Soloveychik, Ro Zo (Zap. -Loningradskogo gornogo instituta, t. 43, vYP- 3, 19611)o The case of a linearly t, !docreasing correlation function is of practical importance, for in1vtance, at large-, I ianiplitude wind fluotuations for distances of about 1000 1w. Cwig. art. has: 2 tables ,and 35 equations. ~SUB CODE: 04, 12/ SUIN, DAM none/ ORIG REF: 002 SOURGE GODE: UR/2531/!;6/boo/i9iAO77/bo6" 1 r^,,j I A 44--' Of tlw M*a we lwateA lu the following saMis (Vw,.- eaa&lve copwlt;y of sodium oleate lelng usW- ak~ linity) tCUates Rat Xt' At Ce It 2&t 5.0. '80innitted 2 Oot 4-7.- SHIRNOVp A,; SILKIN, A. (Zhdanov); SHCMBAKOV, G.I._.KAGAN, S.; KOZWV, P. (g.Rovno) .... ... Readers relate, advise and criticize. Sov. profsoiusy 18 no.16t 34-35 Ag 162. (MIRA 15:8) 1. Chelyabinskiy metall4gicheskiy zavod (for Smirnov). 2. Sotrudnik Kostromokoy oblastnoy gaxety "Knanyy Sever", g. Vologda (for Shcherbakov). 3. Zaveduyunhehiy yuridicheakoy konsul'tataiyey Kostromakogo oblastnogo sovsts professionaltnykh soyusov, g. Vologda (for Kagan). 4. Noshtatnyy korroppondent shurnala "Sovetskiye profsoyusym (for Kozlov). (Vologda Province.-Employees, Dismissal of) (Rovno Province-Blodd donors) (Chelyabinsk-Steel industry-Tachnological Innovations) KAGAN, S., inzh. Testing a sealing paste. Mor. flot 25 no.11:30-31 N 165. (MIRA 18:11) r: 1'. r.-I 2f .-C3 'TI J 1,; 1'-. 1 3 a V Id 1: ~ KAGAN, S.A., kand. med. naak Rcperience In the study of the ultraMe struoft?e of human spermatozoa in oligovoospemia and necrospermis., tlrologila 28 no.504-38 S-0163 OURA 1!7 ZO 1. 1% urologicheskoy kliniki ( zav. - prof. H.11* Zhukova) Go- sudarstvermogo ordena Lenina ins-tituta usovershenstwoveniya vrachey imeni Kirova. KAGAN, S. A. Antitoxic liver fimction in surgical renal disoanes. Vast. khir. Grekova, Leningr. 71 no.4:8-11 1951 (OLML 21:1) 1. Of the Department of Urolog7 (Read - I. N. Shapiro). Leningrad Order of Lenin Institute for the Advamced Training of Physicians imeni S. M. Kirov. 11 IF. I 111~ I t I P I :F IN ~fi Mill PIIIIJ111111 I PI'dPIP Nrflp I volwl I, In I V I I I I I* Ail M. Hl Vill: I KAGM.,p S.A., kand.rod.nauk Uretarolryoloplasty of a single pyonophrotic kidney. Vwqt.khir. no.6:112-113 161. OURA 15:1) le 17. kliniki voyenno-morakay khirurgii (nach. - prar. A.A. Bochtrov) Voyenno-neditsinakoy ordena Leninn akiWomii imani Kirova i bollnitBy in. Uritakogo ( I vracb - D.A. Shushkov). (KIDIMYS.-DISEASES) %DNIE~SURGERY) (URETEM-SURGERY) '1]D/WWV% T AP6006725 SOME CODE: lfillbmA 11/0-07W AUTHCH: -TasinskVa, Go A. 1411 7 ORG.- none TITLE: Now refracbory materials for boiling zinc SOURCE: Lakokrasochnyye materialy i ikh primeneniye, no. 1, 1966, 73-79: TOPIC TAGS; refractory compound, corrosion resistance,, zinc, metal phoadaaL~_ metal grain structure,, protective coating A AWTRACT: Corrosion resistancek"to boilipg zinc and-zinc vapors of nuowcow-; jjgh-t~Mp~rature refractor materialsl2was tested-under laboratory and working conditions because of the failure of presently used xnate 'to withstand the sustained action of molten zinc at~boiling temperatum 'This problem ar,,)se, Lor Instance, in conreying,,~A_~Lu d t I I me a where thermocaiples, pipings, and electromagnetic pmum 0. have to be made of corrosion -resistant materials or coated with such materia", if they are to withstand continuous and prolonged use in contact with liquid metal at high temperature. The tests described in this article were conducted jointly by the Institute of the Scienmq;. MWd4x* _A~_ MSSR, and the lAoinuad 9-h.- UDC: 667.613 precisely develops new refractory materials which would meet the above requirements. Samples formed into crucibles or cylinders were first submitted to the action of molten zinc under laboratory conditions, andthen. to boiling zinc, contained in a muffle, for periods up to 12.5 days. The corrosion resistance of the samples was evaluated from visual and micrographic observations and changes in weight and dimensions. Some of the data are summarized in Table L The m~,qro-strVcturq_fnd properties o!,Ahe boride (TIB2, ZrB2. CrB 2, and W BS). _i2~ N 'ZrN, an5l'AIN),, Si3N4+SiC, jthe nitride (Ti__o BNC, and Si3N4 + BN samples did not change after Ney were exposed to the action of boiling zinc, Formation of a dense,, zinc -impregnated titanium* oxide crust on the TiB2 sample protected it from further corro- sion by oxygen present in the muffle atmosphere. The most corrosion- resistant carbide, fitanium carbide, displayed a change in struchire and decrease in mic.!ohardness. Refractory compounds of the nonmetallic type, AIN, BN, SIjNt(sicj, Si N 4 + SiC alloy, S13N4 + BN alloy, and BNC were singlp-d out for 3 practical applications as highly corrosion-resistant to aild barely wettable Card 2/1, > able 2. Experimental data of the C) n,R refractory samples In b;iling int at 9400C Z "0 Residence position specific Visual C)% Sample time in dm, th It I corvair. e v tio b e rr s r a n n cm o hr Titanium On the Insignificant boride 240 surface *0.02 slag adherence Zirconium Slag adherence borlde 180 #0.15 padi=W &bast Chromium borlde 120 +0.006 Tuagaten c3a4n surfbw, no borlde 168 Immersed -0.014 slag adherence Utsal,ua On the Unchang" c4rbide IM surface -O.Ok2 externally Zirconium 14w* Semple. Carbide 220 -3.8 lost strength Ckiradvis ft%le diamohied castide 24 in the malt "bdenum Donsiderable Caftids 168 +0.14 slag sticking' Tungsten axIde Ibl carbide 1414 Immersed -0.015 " Molybdenum on us - savOk vwraaw IlIeI11* 204 surface instable Tj: salon Iftaignifican-t attride he #0.02 vzlkce aMation A114com On the 81cmifican Nitride 20T& lFurrabe +G.= slag Silicon Thin cinder- 300 *0.041 like layer Box to visible Cattlatwo 2014 -0453 change Boron 91-dAcort over- C&AW&Aam 204 -0.026 zinc dei UI& s , qw able) 264 .0.008 a Q> L 42069-66 ACC t4R. AP65667-2-5 by molten zinc at boiling temperature. Moreover, these materials can easily be profiled into a -given--sbape mith the, help ot-wetal"Cuttilkif "Ols and are cheaper than the refractory compounds of the metallic type (compounds of the IV-VI group transition metals). 1'* Boron carbonitride, silicon carbonitride, and AIN refractcwy I CrB2, W2B5, TIN, 'materials of the nonmetallic type, TiB2, ZrB2, trN. and~conditional on an increase in thermal stability, MoSil mater- Ws of the metallic type may be recommended for use in contact with e molten and boiling. zinc. In view of the relatively high price of -th metiMc-type refractory compounds, their iise as protective coatings) was indicated; they may be conveniently sprayed on ceram.1c or tallic As by meam of plasma guns. Orig. &A - h'as-. 1 table. [FSBI produd v. 2, noo sUB C~I*j~ 11 SUBM DATE: none OTH RU 001 Fig 4A af KAGAN. S,G. WeAr resistance of D16.5/20--l diesals. Energ.biul.ne-7:1-4 JI 156. (Diesel engines) (MLRA 9;10) KAGAN S.G. Modernization of *Pionarg diasels. Inerg. blul. nool:t.-24-28 N 156. (Diesel engines) (MIA& 9:12) AID P - 2367 Subject USSR/Engineering Card 1/1 Pu b. 28 - 1/13 Author Kagan, S. Title Operation of the 2d - 16-5/20-1 engine with water- cooling loop system Periodical Energ. Byul 6, 1-3, Je 1955 Abstract In order to make it possible to operate the 2D - 16.5/20-1 diesel (50 HP and 750 rPm) in arid reg:'ons, i.e. with a closed circulating water system, the ~-80 tractor radiator and fan'driiien by'the KDM - 46 motor were utilized with success. A sketch of the Installation, a diagran of engine performance, and two tables with pertinent data are attached. Institution: None Submitted: No date 004 OOA 00 00 1 gig 004 00 oo'l ood, HLULIJ T-Vj 'r I- ii w a ~ ; A- 6 A 6r N S, L .00 00 !~Opo 406MISOW Ito Ayr (Sxftd. WAA v rwm 400 &66 sisal! goo goo ALLUMOKAL LITSINATtOll MASWICATWo A- SLA NNW %I. ilk S.Asse -,a['" .1. dft, oat it a lit amu i i 0 0 a 0 0 0 0 OR 0 0 0 0 0 0 0 * OR 1010 4-----OO*Ooooe%~000,00060001TO64000000ootoo*ooooe~2A also goo COO goo Ito Iz 40: ".40 as n4t ~1. :L 'I 40 0 0 0 0 OR 0 0 0 OR 0 0 OR 0 0 0 0 0 0 6 a a a 0 0 4 0 0 0 0 0 0 0 9 0 0 0 0 0 16 tilt 4 6 4 e A 4 0 it 0 00 0 0 0 41 0 40 0 tof to 0 , 4 L L a it If 6 1 1 1is A, lit Ill 9 1 & r 4 RN 6 x , 00 06 He"a tot 4949rolaws Lim cisewitntratio.010 Vill .00 Disiersaislad" of issalsolaidil % % .00 istiol 4 A-. I ~ " .1 ja ~ 4. 1.11#1 ' e " 1 AsIbirl, I . I Jq, .11,:P flo'.1 . l % VILIV 1ft ..IIIIAIIII, uOrd I'll life 'lei's W .1.411 will. ..I .*. '00 ICowls warylim withill WhIr 11111116. Its asialtillill 4411114'.. i 14 oil '.41111d. it I"Ill if 0, 0.1 aid. 0 1 1.11 1 , I-) ;.* 0 00 with Clio at Va 21111'. [lit witlis VAII4.4 11"Ilt Ola as 9 I%K-v uf I hc VO 41111141MM In - .1 I 1 I *o K 1, - 1, , 1-0 if ." . O lilt bliss 441..ts. III Cil last It It, lit IV~711 a,'91 W; -11 Ow Atli' -411-1111111 14"Willb : ,hr W41606M Willi list 1 lersol 110 If 2.4%v 111rilis o * 00 ::0 go 00 '00 woo Ll 00 # is 1 4 Liffil,aTOt 00 3 sea i.. .1. a.. ;.1 00 it _1i - Ir -1 1 F A 1,141911pt a 1 10, '1 -TI 'IF 1 u vt ;o if * 0 0 0 a 0 0 o o o 0, 1 O 0 0060 1T Oft It I I Ow Is 0 1 Iff . a I fill 600000000*1100 a It a 4 4041 o 0 o 0 0 0 0 0 0 0 9 a 0 0 0 4 0 0 0 0 6 0 0 0 0 0 0 0 O o 0 0 0;0 0 0 0 0 0 * 0 0 #* 0 0 0 0 & 0 0 0 0 ' ' N o " i 16 0 r* LAI) 6Z---4-L A F IU I & t t I t 19 dolorm"164 kill lAwrlwal"fillowi 14, L kiimlsw i ill I'llatiks KOM s-, whirr tIk- mial 44 H111111111 is, .I$ -fl., I- ON, I out 2- Sa, I-milml 11MI ihr Ill A I- IQ X Ili'l .,Ill ItIv" 0 'll.flult" .4 1, .111. '! A Ilk 1.41 I-Is 111-411 IN, 11111 8"it it It : :4.11.4111.4 'Alit, "III Ilk 1 .411. 1..$ ,It .1 ,, L. 6 -00 00 00 .06 0 .00 4.00 dig It A will use es 8 oil. I T, 'u too 0 0 0 0 0 0 0 0 441 -1-- - .. ,."i Illong, 14 1 v it ~ " PHASE I BOOK EXPLO=ATION 215 Pakidov, 15etr Aleksandrovich Novaya metodika rascheta tekhnolog:ichesklkh razmerov I dopuskov pri mekhanl- cheskoy obrabotke detaley (New Yethod of CalcuDding Tachnological Prr>.,ass Dimensions and Tolerances in Machining Parts) Ymcow, DULShgIz, 1956. 42 P. (Obwen tekhnieheskim. opytom) 6,500 copies printed. Reviewers: Zaretsk:Ly, A. R., lhgineer, and Kagan, S. L., Rugiuer, Tech. Ed.: Dagina, N. A*; Ed.-of the Vralo-Siberian r thgiz: Smntavov, X. I. PURPOSE: The booklet Is Intended for eng1maring and techalcal personnel. COVKRAM: The booklet describes the basic properties of 4imnsion ebalms emd. methods for chain solutions, characteristic features of a1loltances and tol- erances b6tween successive machining operations. A method lo g1m for cal- culating technological dimensions and tolerancet1nvolved in nachining parts. A nev method of calculating process dimensions measured from reference planes subject to further machining In presented and a new method of studying cmiplex dimension chains having practical applications in plants is given. Card 113 New Method of Calculating (Coat.) 21,-) Ptabl-ImtIon of the booklet was xecem"ended by the Owk Nlkzhime Building Institute and the Ural Branch of the Scientific and NcWc~al Society of Machine ladustry, There are 6 Soviet references. TAM OF C Foreword 3 Dimension Chadne 5 Basid definitions 5 Structure of dimension chain 6 Solution of dimension chains 9 Operating onchs-In 14 Order of calculations In s4ving dimnslon chains 15 interoperatimmi (Process) Allowances and Tolerances 16 Basle definitions 16 Interrelationship between interoperational. allowamees, toler"mes, and'dimensions 17 Methods of determining interoperational allowances 19 Card 2/3 89822 s/lio/61/000/002/009/009 9141000 (10'VW,0t?,1067) E194/E455 AUTHORS: Lavrinovich. L.L., Candidate of Technical Sciences, Barsukov, I.A., Engineer and Kagan, S.M., Engineer TITLE: Increasing the Accuracy of Measiire '0"".r tertain Parameters of Electrical Machines PERIODICAL: Vestnik elelitropromyshlennosti, 1961, No.2, pp.64-75 TEXT: There are numerous types of instrument for the measurement of the frequency, rotational speed and slip of electrical machines but their range of measurement is very restricted and they are not very accurate, For greater accuracy of measurement it is necessary to develop counter-type instruments which give a direct reading of the values to be meamsiured. With counter-type instruments, the accuracy of measurement of such magnitudes as frequency or speed is much higher. However, until recently, although methods existed, there were in fact no Instruments suitable for measurements at sonic frequency and high speeds, With the development of Soviet decatron lamps which can be used to count in the decimal system, it has become possible to make a fairly simple instrument for general use for the measurement of speed, frequency and slip. The use of decatrons Card 1/5 89832 S/110/61/000/002/009/009 Increasing the Accuracy ... E1911/E'155 sets no limits on the range of values to be measitred. The simplicity decatron circuitry and tile fact that direct readings; are obtained in the decinial sy.4tem is advantageous ill tile Aonic and infra-sonic frequency ranges, An instrument has been developed for the measurement of sonic frequency, speed arid slip of electric motors which can handle frequencies up to 20000 cycles, speeds up to 1200000 rpm in three ranges, and slip in a number of' ranges up to 0.000001%. In principle, the instrument consists of a photo- electronic signalling device and a decatron co4nter, with an appropriate supply source, The photo-clectronic signalling device converts light signals into voltage impulses which are ineasured by the counter. The principal components of the counter are the special gas-filled decatron lamps which count impulses in tile decimal system, The decatrons are described, along with their control circuit. They fulfil the role of a counting and memory device, The decatron counter is the fundamental part of the instrument; it consists of a counting-cliain and a time-chain, a n electronic switch and quartz oscillators of 10000 and 16666.6 c/s, The counting-chain comprises 6 decatrons which shine immediately opposite numbers on the front panel, The counting-chain is Card 2/5 89812 S/110/61/000/002/009/009 Increasing the Accuracy E194/E455 controlled by a rectangular switching impulse of positive polarity received from the electronic switch, In the abmence of a commutating impulse, the counting-chain blocks and input signals received from the former do not affect the countot,, The time- chain is identical with the counting-chain and im provided to increase the period of repetition of time signal4i. The signals applied to the time-chain are: from the quartz generators of 16666.6 c/s, for measuring speed; from the supply circuit of the induction motor, for measuring slip; from the quartz generator of 10000 cls, for measuring frequency, The electrical part of the photo-electronic signalling device consists of the following componentsl an incandescent lamp; a photo-electronic convertor based on a photo-electronic multiplier type 13y--31 (FEU-31)i an amplifier based on triode type 6HZr7 (6N2P), A ray of light from the lamp passes through an optical system on the rotating object and the reflected beam is picked up by the cathode cf the photo- electronic multiplier, which has eight emitters, At the moment of reflection of the light beam, a negative impulse is formed in the anode load of the photo-convertor and is applied to the amplifier triode, Under static conditions in the absence of an impulse Card 3/5 Increasing the Accuracy ... 89832 S/110/61/04)0/002/009/009 U194/E455 this triode is quiescent, The instrument as a whole consists of two units, the photo-electronic signalling device and the decmtri)n counter,._ The power supply is fitted below the decatron counter; the electronic switch, quartz generators and other equipment are in Lhe upper part, The instrument is simple to time, The accuracy of the instrument proper depends on the accuracy of adjustment or itts parts and in particular on the adjustment of the quartz oscillators, The inherent error of the instrument is analysed and ts shown to be the same as the frequency error of the quartz generator. Consequently, the inherent errors of the instrument when measuring frequency and speed are + 0,01%; When measuring slip the inherent error of the instrument 'is zero, as the source of time -signals is not the quartz generator but the motor supply circuit at the time Of measurement. As the counting method can only count whole numbers of impulses, errors can arise through failure to register fractions of a period, This error is analysed for two casen~ when it is positive and too many impulses are counted and when it is negative and too few are counted, The method of calculating the total error in particular cases is explained anti two numerical Card 4/5 IAVRINOVICH.9 L.L., kand.tekhn.nauk; BARSUKOVp IsAsp iKIZII*; KMA11', S.M., inxh. Increase in the precision of the measurements of certain parameters of electric machl ry. Vest.elektropram. 32 no.2t64-75 F 161. (14IRA 15:5) (Electric machinex7) (Mectric measurements) Ztudics in the Field of FomoloTics of the Cr..mphor .-roup. XIV. Cn rome 'low Ley.j-,jA41VCB of a-Isocar--phynylcre and on I ts tvro ncarcst homol. by N; r-,otkin and S. S. LKa.ran (p. F~O) SO: Journalof Gent-ra-I Ch~-mj.n (Zhurnal Cbrhchcl. KhAmJl) Vc,,Tumc 1i--, 12k, LU C'6W UUU4. ahxE~ MAN, S. S. Bonus system for engineering and technical personnel In plants of the chemical industry. Xhim.prom. no.2;97-98 Mr 136. (KLRA 9:8) (Chemical industries) (Bonus system) SEC-AL. A.Ya.j KAGAII, S.S., red.; SIIPAK, Ye.G., tekkin. redo [Ha.ndling of nitro and amino compounds] P=iatka po obra- ahcheniiu a nitro i aminoproduktami. Moskvao Govkhimizdat, 1961. 19 P. (MIR-A 15W (Nitro compounds) (Amino compounds) (CbM4 &Is--S&fety measures) DOBKIN, V.M.; KAGMT, S.Sq K.K. Automation of batch manufacturing procenses in the chemical induatry. Zhur.VKHO 6 no*5:559-563 16L (WRA 14:10) (Chemical industries) (Automatic control) Ka,.;an, S.S. "A complex o~' the .;ctLl#,,mr:nt of a rv.,jon, und Ilik! llmj.-.,-v-,erri(nt. of' conditions", (the or:_,anlzation and pro.ram of op.-ra'.ions of Uiv Kiev Inst-i::,te), Vracheb. delo, 1949, :;o. 1, para,Yai)ils 73-76. SO: U-30142), 11 Narc,'-l 53, (Letopis InyMi Statey, No. 9, NAGAN, S. S. ?A 48/49T59 mw wA' got.;. A* Medicine Social B$glene Meory of the Soviet Health Program," S. S. EWn, Prof.. Kiev, 4 pp "Sov Zdravookbran" No 2 Disagrees vith various parts of Prof.Batklol article. Questions Batkis' statement that social bygiene should be re-established as a separate subject for etudT. Criticizes Betkis statements on sanitation statifftice and on narging of social byglene services with taber- cqloaio and venereal disease. services K Aoki 1 5. 6. -657~ VeksamLrovich emashko, E-7c liiin/ Yat clbnrjtb (18-1,4- Ilikolay erillvy FuLb' D/-2 1949) vrachlob 101o, 10,49, No. 9, STB ")9-441 6, Foltr, KAGAN, S. S. USSR/Me%P-4-ne-Diagnosis, Quality JanlFeb 50 Hoopitalas Children's "Quality of Diagnostic Procedures in the Unified Children's Therapeutic Prophylactic Institutions," N. N. Sachuk, Chair of Orgn of Pub Health, Kiev Order of Labor Red Banner Mad Inst imieni Acad A. A. Bogomollte *Pediatriya* No 1. pp 50-55 Tabulates and discusses data on results of consolidation of childron's consulta- tions and p6lyclinics with children's departments and hospitals in Kiev. QLality of diagnosis has strongly improved. In the age group up to four quality is better than for group from four to 14. Chief, Chair of Orgn of Pub Health: Prof S. S. Kagan. PA 163T33 PTUKKA, M.V.. professor: XAOAN, S.S., doktor meditoinskM rA44, professor, Over-all morbidity regiRtration method of the MiAstry of Public Health of the U.S.S.R. Sov.sdray. 14 no.5:27-32 S-0 155. (MIJU M12) 1. Dayetvitel'My chlen AN QVSR, saslushenr" dayatell neuki USSR (VITAL STATISTIOSO morbidity registration in Russia) chleif-korrespokident AN SSR, (for Ptukha) system of ministry.of bealth XAGAN, B.S., professor (Kiyev) ?asks of sanitary and epidemic control stations In the control of tuberculosis, Gig* i sane 21 no* 9:51-54 5 156~ (Mija 9:10) 1. Is Kiyevskogo oblastnogo otdoleniya Toesoyasnogo nauchnogo obahchastva gigiyanistov. (TUB]IRCULOSIS, pray. and control in Russia, tanks of sanitary & spidemlol. stations) YCAGAN, B.S., prof. (Kiyev) `~~I;igllns of Soviet sanitAry orgnnizntion in the UkrAlte- motme features of its develooment. Gig. i san. 22 no.12:16-43 D '57 (SANITATION (MIRA 11:1) in Russia, develon. & organiz. (Rue) 11 '1 V I I I A q; 7! prof. (Kiyev) Petr Xvnnovich lurkin, the founder of Ruestan public health statistics. Vrachdelo to.91969-991 S158 (MM 11:10) (MMICAL STATISTICS) ( .1 E, PETR IVAROVICH, 1856-1934) KAGAN 0 B.S. prof Aleksandr Vasillevich Gliko,- one of the oldest Soriet sanitarjr plWaiciana. Gig. t san. 23 no.4:85 Ap 158. (HtRA 11-6) (OLIKO, ALIMSAER VASILINVICH, 1874-1956) *1 v; , 1 ` ,z .~z . I , -. , "Pro'bl,ms of stu,-Iy of nonulation irorlcd lity." ?.~ir.-ort itu th-:~ 13th '~Jl-Unlon I- or,~roq3s of 1. nildmioloj:As an-, Infectionists. 1959 BRUSHLINSKAYAp L.A.; MAZURv M.M., dotsent; RODOV, Ya.l., doteent; KAGANy S.S.v prof, "Critique of bourgeois theory and policy on population" by B.IA. Smulevich. Reviewed by L.A. Brushlinskaia and others. Sovo zdrav, 39 no,7:83-85 160. WIRA 13: 8) (POPULATION) (SMULEVICH9 B.IA.) KAGAN, S.S.p prof. (Kiyev) , 'I., - ,- " Modern meaning of the terms "morbidityk:and "diathemis".. Sovadrav. 19 no.10154-58 160, (KIRA 1411) (MEDICINFTEMINOWGY) KAGAN !i? NCritique of bourgeois population theories and policy" by B.IA, Smulevich. S.S, Kagan. Gig. i san. 25 no. 5:111-115 MY 160. (KIIU 13: 10) (MIOGRAPHY) (SMULEVICHp B,IA,) KALYUZHNYYO D.N., prof.;_KAGAN, S.S., prof. Exhibition which has gone dcim in the history of hygiene and public health; on the 50th anniversary of tho Dreadon International Hygiene Exhibition. Vrach. delo no.5:125-128 My 1629 (MIRA 15:6) 1. Chlen-korrespondent AMN SSSR (for Wyuzbnyy), (PUBLIC HEALTH-EXHIBITIONS) 1. 11-111111111 j'!j't�n, 111 1 -L 141 1' Ti -11Z :111; - I "I "I" ~uqp'j'' I I- -k~ t 11 I ;- ~ k%, 4 Eli 3 IT' l At%l 4 rr,-ltP~j V /JMR - I 'IF -li lapm,,.,Ilqg E Mm fflo"Hol W."IFIR jTpjjq~, qq A HdIffit ftLAI-l" 8' EU Y Q tk ~irv I k r,,r, 131AWSBYARG, P.I., Irandidat teMh-nicl:no;~ikh nauk; KAOAN, S.Ya.. iM71~ener. Induction motor Pitr, i-Diiase and short-CIrcuited vindings rn tzla rotor. Vest.slektroprom. 27 ao.^i;27-31 5 156. (M'.IAR.A 1(1:9) 1. Moskovskiy -inzhonerao-stroitelIrkyy Institut imeni V.V,KUybFzhG--a (for Krptyeberor.). 2. Kharlkcmakiy elaktratelthnuichenkly zeyod (for Yam). (Electric motors, Induotion) SOVI 112-58-1-570 Translation from: Referativnyy zhurnal, Elekirotekhnika, 1958, Dix 1, p 84 (USSR) AUTHOR: Maleva-iyy, A. I., Kagan, S. Ya., and Mayzlish, Ye. Ya. TITLE: Electrical Equipment 0~ffimersfbtE-Plamps for Artesian Wells (Elektrooborudovaniye pogruzhnykh elektronasosov d.111a axtezianskikh skvazhin) PERIODICAL: V sb.: Raboty M-va elektrotekhn. prom-4iti SSSR po mekhuniz. i avtomatiz. nar. kh-va, Moscow, 1956, pp 38-40 ABSTRACT: The Khar'kov plant KhEMZ manufactures immersible MAPZ electric motors Z, 5, 12, 35, and 60 kw, 380 v, for driving Immersible pumps intended for artesian wells with pure water (without mechanical or aggressive chemical impurities) with a temperature up to 200 C. Motor cooling and bearing lubrica- tion is effected by the water being pumped. Stator winding has vinyl insulation and is not sealed. Motor journals are of stainless steel pr-essed over the motor shaft; bearing bushings are made of textolite. A control station and PVVP cable are furnished with the motor. The control stationst for 35-- and 60-kw motors have a provision for connecting a float relay for automatic pumping. AVAILABLE: Library of Congress Card I / 1 1. Pumps--Control systems 2. Electric KAGAN, S.Ya. (4talinskaya oblast') Formllae of the roots of quadratic equations* Wto v shkole no* 3t61-62 HX-je 161. (MIRA 1435) (Equations, Quadratic) YE. U-.] :-,0- 72-7~- -C Translations "Case of Dislodgement of a Foreign Body in the Upper Part of the Esophagus of a Ton-Month Old Infant." Honored Dr. RSFSR, Cand. Med. Sai, Otorhinolaryngological Unit, 6th Gorlkiy Polyclinic KAGAN, S. Z. PLANOVSKIY, A. N. and KAGAN, S. Z. "Continuous 5ulfonation of Denzene,41 Al N. Planoyskly amd S. Z. Kagan, Promyshlennost Oiganicheskoy Khimii (USSR) 7: 2964304, 1930. Since we are not experts on the subject of sulfonation, it is difficult to evaluate the article. It contains a far more extensive theoretical study of the problem than any other found so far. Apparently the authors are acquointod only with the pilot plant operations and are fairly new to the field. The article makes no pretense to show knowledge of actual plant operations. Ix V 9-6 a- 0 W-m-4 a 0 0 a 0 W lvivvT-- 0 0 0 0 "0 0 0 too 0 0111fe 0 W, Off: 1ITO 0 0 41 0 0 0 o o 0 0 0 0 0 41 Q'0 *0000 Z ; - ;' A M, V 11 9) 11 0 It js At u a a 41 a 41 to 42* 7~O 0 00 A 0b 00 GOAI .00 .0 00 Now compoWdoam fw lu&gcbomk&l apprahm. A-1. Rychkov and & S. Kagan. Kkimukrikaya Prom- 1%4. 00 %10. 1, 19-2t.-41uhris wm MR& from a total. of vinYt Chloride min (U. dibitityl plilbolate 22 and emkitt 14% 0 .4mM WM Made at VWyl ChWW Milk 100, lWbGlji phthaUte 50. too 40 parts by wt. and Ca Mew - ate. These were resmitant to client. corrosion and were very scrykTable in chem. industrial &M. G&Aets vW age Of SOM- rubber a ve n*Ut&ni to W, d. be'Wnettlitts-,91YVTTWInflak.at temps,of -&Ildl aful under a *41c rapp 411 pr,"um. t)"&Ih a, prnm. uf,tllc 11111" art thrm, anif elletirlic" with jill.i, us,, 11, moo 00* 'q* =9 0 See =4-V 1111TALLOICK&L t1frOAT641 LAWFKA110% I U W 0 rv it 411 W It - u it Is If a KW a I doll, 0 0 0 0 0 0 0 41 0 0 0 fu Ilse a a a a 0:0 a 0 0 0 00*00 0 0 0 919 0 0 0 0 o o 0 0 0 0 0 0 0 #1 1 it M! - 1 it It-go 340, 1.1, 1 .,nfjmv.~- 5 go A ';j "olvir 0.0"11110 A led thruts4h bOldliad dall*, ls~t 90 - 611111110% do 6" d the bossivill, TjqW lilil ftaI_. wrJacity of VOW 18 tM 110111"Attir 0.1 Ol- Pat SOV-VOWly Of "S" /0 00 Continuous "C" (or the Pic4uttlest Of be aliens. Ito babbis cap spoillisom,11.4on. per sot. Umillortbearl III - I slid sob)"Wilkin in oin Iolwinittinst Pmr- ion -1111411 au 0 IlOck Add. A, N. IUw,,Ljj jUkd~j,Zit".1. Kksnl- C h-jkayu Proft. J944 N. 9 5 it) am niosim 1.6 lars. 71he Wlkguai~m inn be szedit cois- diti " V d l h . . , , 0 n to devin a ow 1-nArne a study wes "wlc "i 'be effect 14 1 -111 "L el3vi o or, u the *an s%qWrvd See sollMantion v%tits irmh the so. tit 1 P - IRIA,turr content *I the re. cycle- 4"d MHAM art& -A Contget Th U "to as Waste (w. of It4lift, ftft-1wWr. 41bi dMIC is HIM OAU 327 13 0 4 k l 1 . e nte Joe *0 -ullonalid." (ellbeciusen I ally dvid.) I% I - (1"Twx 24 ~ h 0 ) . . . irs.. rW.. #vm): , ; . 0.0m. 2.251 16. 0.11172. UJI; al. 0.945. 1.M. It appeals 'd - S d ercA ty the lif0covileat of the ": y,kJ 1.0ruse . Coilstructicsi of a 1 and gem i * that the app. abould vuluest oMilarviamc loaf-wisons rohLit Ill WetiOess 2-T of the rearlit I the coam & .60 .. p., s tbe ' W . "ILl -- of If-SU- in MW. 7u, said jr Is the com t f go . . pp. p 1%0 exiistamil to triol. %. wall tot 77.7. 81-0. 4117. 1 O,j so* ent o benzrac-Aillunic " am ftwouss in &be reactitas a " 26.3. An williontiou Mv- . 7 =00 product expretird in n". %. In an app. where the in. coming benzene vapor aft 2 i d i h 1 saw. IN which Hill" Is oil valml from 4 Mtervair .-ZW1 il CO 0 a nto t e 1&900 tbre"41111 It POICNIS plate. the lefp. V Tt rewtion is IMI, the ov. A tomma mgvlotar s" it imilaing *vkv into a m tor. - Omearto Is pentpud Orimt. s. qser we r of hvsh beasente Of 11-0 in the recYck Is 3.A%. end 11to beassi e is IvVir l l d A or fivele a tims-vtO of birmiorne con6tasku thrGughi a tru e A I wirs, k - 3.8. WbMthilgpp.jInithebub. 00 U'ag type wb"c tb b otlarkillAtike slid a Catubinsitka stsowit'.11M i g o4 , or "Witiorts ftnisin the mine. 90 a k - 2. In an app. vilinc the 2 phaws are brought into Walter. ftn d flat sapesIMMI-4 vatior Zvw. lv is kd into this sadamitur and the otbir pan Is Doom So* dkwtc=tget,k~U.W. The prWeffedcmdjLkmjj~Dr $u1. to"tiax benzene are: ternp ~ ISO no 4 ii thinatilh the bottom into& IS-10latir colons. The esittioa l' l r BOX l1lowe t % W% goo 2 . , c , recy% ng tinws t, 9 a ovistor clto a eni ove peadw in % g. catwuauav hom the 111111111111OW Into OW U44M Part of the . ' 1 1 vskmil, Flowing dowitioull. We Prollift loom With that beasene valitin so that When It resdam the $spowin 4 0 4111 g g i i l i hd o0 ; t riales t ftatic 'Rill n w balinani when tsth. Immardestl l ed notAins ossly 3-4% of Ism IUW)~. MA)-contandisa Leazene vagxn are witheleawn throislill the " al 00 fulfallallis " the Column, rhe vatiols Ilk" thil"66 a t condrinin and aviler Into a sillosslor 11heit this l4litall a LA s4TALLURGOCALLIT CLASSOKAVION : &$ natue mv. Tl* 14.0 it d1war" and tk Ildo am I* h a dj4 kt and tiolittaknor h2to the . d thtou b nz is a &. ij , .... ... e m ene p g TW villfgastion tiose in tur"t cundenwie v tot b i .0 0 . tew o e r such an spp. Is cale-1. to tv 1.5 hin. U. Haab ' lot T- A 1 11-.---.. - ............. j. A~ ~ 4% 1 . 'A L 1 4 1%d 0 Ole, IVCPIIR44 Haiti mull will !10 0 0 0 0 0 9 0 0 0 * 0 411 * 0 0 0 0 * * 0 0 0 0 00 0 OX - - - - AA - Amass sidilds dbas 0 sale.&-o' 0-4111' oe * 4111 111,10.10, -1 KASATKIII, A.G.; KLGAN, S.Z., redadtor; POGUDKIII, P.V., tm)dmicheskiy- re- daktor. (Basic processes and apparatus in chemical sngln9mAng)O3novrqe pro- tsessy i apparaty khimicheakoi tekhnologit. lzcl. 4-oe, perer. Mo- sk-vA. Gos. nauchno-tekhn. isd-vo khlmichaskoi lit-ry. 1948. 916 p. (Ghemical anj4,nenring) (MLRA 8:7) ix-ikN, 3. L. OrEanic h2-,,rn Tom,,-.erature thermoconauctarz-, ari ti-,,jir ujo in inciussixy ios- nouchro-tokhn. Jzd-vo lit-ry, IS~51. 171 1), ~ ~r I -~', I ) qD51 i - &-)-5 A KASATKIN, A.G., professor. doktor takhnichaskikh natk, re(Laktor; UMMIOT, V.A.. radaktor; IMAROT. V.T., rodaktor; KAGAS, S.Z., redaktar; LIMOY11, H.S., tekhnichaskiy rodaktor [Processes and apparatus used in chemical tochmology3 Protessay I apparaty khimichookol takhnologit; oboralk rOot. Pod red, A.0. Itasatkina. Hooky&, Goo, nauchno-tekhn. tzd-vo khImichookol lit-ry, 1953. 115 p. [Microfilm] (MIaA 7:10) 1. Russia (1923- UIS.Sala) HInIsteretwo kh-LmIchookoy promyshlon- nosti. (Chemistry. Technical) f-- , L41 i /77 A, j7 1-1 I Y IL E;- iv FLOOVSKIT, Aleksandr Ifikolayevich; RAUH, Vitaliy MaIrsimovIch: XWAN, Solomon Zakharovich; KUROCHKINA,H.I., reduktor; jRLU(H,TeI-Ir*-T" 121.4, IeMMelsl"aaktor (Processes and eqnipment in chemical tachnoloa] -Protuessy i appai-aty khinicheskoi tekhnologii. Moskva, Gos.naucaiao-tekhn. izd-vo khim.lit-ry. 1955. 580 p. (KUtA 9:3) (Chemical engineering--Apparatuo and supplies) XLGANO S.Z., kandidat tokhAichesklkh nauk. Hydrocyclones, their construction and design. Wnprom.no.6047- 357 6 '56. (mm 10.: P) (separators (Kachlues)) RUMMIDI/Chemical Technology - Chc!jiLcal Priducts and Their H-2 f,pplication - Processes and Apparatus for Ch~miical Technology. Abs Jour : Ref Zhur - Khiml-ya, NO 3, 1953, 8236 Author : rnst Titlo : Hydrucyclones, Their Construction and Desilgi# Orig Pub : An. Rom.-Sov. Mi!ta1urC;ie si constr, msini, 1957, 11, No 2, 67-09 Abstract : A translation; See RMICUri, 1957, 17907. Card 1/1