SCIENTIFIC ABSTRACT VVEDENSKAYA, M.V. - VVEDENSKIY, A.A.

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SCIENTIFIC ABSTRACT
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WEEi-p-l"13KAYA, 11. "1. VVFF---iE-!:SKAYA., 14. V.; "Deternination of thiacyarzites In thc -arine w~ a metlro~! of sUxlying the functiorzil state of the liver," Gorlk--*y, 1955. Glorlkiy 4 110 e .)Late MedicnI Inst imeni S. MI, Kirov. (Disnertation for the Dei,,rCC- of C.-IrAl- t of Medical Sciences) paa Letonis' No. 47, 19 Nbvenber 1955. Irbscow. SO. Lni2~L VVEDENSKAYA, N.A.; IODKO, V.K#; XONDORSKAYA, N&Vo; LANDYREVAY N-S-; ---"~M=NA, L.A.; SDOW, P.G.; TABULMCH, V.K. Bulletin of strong earthquakes In the U.S,S.R. In 1960. Trudy Inst. fiz. Zem. 28 Vop. inzhe seism. no.8:61-76 163. (MIRA 16:11) ".; DZHAITUZAKOV, K. D.; IODKO, V. K.; KONDORSKAYA, ff. V.; LANDYREVAJ. N. S.; HISHARINA, L. A.; SULTANOVA, Z. Z.; TSKWAYA.. A. D.; YURKMCH, 0, 1. Bunetin of strong earthquakes in the U.S.S.R. in 1959. Trudy Insto fix, Zeme not.2-2. Vop, insh. seism. no.7:3-24 162. (MIRA 15tlO) MmUquakes) VVEDEIISKAYA, N, A, General compilation of eeimic otatiotic3l data in oeiomic zoning of Contral Asia. Trudy Inst. fiz. Zem. no.22. Vop. inzh. oeism. no.7:25-45 -162. (MIRA 15:10) (Soviet Central Aoia-Seiamology) S/16 62/000/003/005/098 D228%)301 AUTHOR: Vvedenskaya, IT.A. TITLE: ~The question of using instrumental data on strong Cen- tral Asian earthquakes in seismic zoning PERIODICAL:' Referativnyy zhurnal, Geofizika, no. 3, 1962, 13, ab- stract 3A119 (Tr. In-ta fiz. Zemli, AN SSSR, no. 17 JsI7, 1961, 119-127) TEXT: A method'is proposed for construction of theoretical earth- quake isoscismals from the value of magnitude 14 with an account of the regional geologic structure. A map is constructed for,the iso- seisnals of Central Asian earthquakes with M,~4 1/2. It is s1rd%rni that the character of the disposition of the force isoseismals de- pends not only on the-focal depth, but also on the peculiarities of thexegional g6ologic structure. /-Abstracter's note: Complete tranalation,-7 Card 1/1 8151Y601000100810041031 D051 D113 AUT11ORt' Vvedenukayaq N.A. TITLE: Contribution to the question of using data on micro-earthquakes for problems of seismic zoning SOURCEi Kkademiya nauk SSSR. Sovet po, soysmologii. Byulleten" no. 8, Moscowq 1960.' Voprosy seyamicheskogo eayonirovainiya',3 60-66 TEXTs The author discusses the possibility of using data on observations of micro-earthquakes for seismic zoning purposes. Ad tLis possibility depends on the large-scale study of the complicated and varied association between strong-iLnd-micro-earthqaakeel.it,.io stated that at present only very general regularities' cin."~e discussed. -On a regional-basis the author describes this association with respect to Central-Aoia, us*ng for this purpose graphs and maps showing the epicenters of earthquakes and changes In seiomic acti- vity foryarious 'se-ismically active zones.. An analysis of one of the maps shows that areas where seismic activity is relatively more stable are char- acterized by an increased number of micro-earthquakes. On the basis of an analysis of -observations of mIcro-earthquaken in Central Asia for the 1950- Card 1/2 S/5l9j6O/OOO/OO8/OO4/031 Contribution to the question... D051/D113 56 periodt it can be said that in areas where strong earthquakes previously oaourred or occur tit present, the frequency of micro-earthquakes is relative- ly higber. "Increatied technical 'accuracy has made.-more accurate the delinea- tion of' seismic zones prone to strong earthquakes. Stationary seismic eta- tiohs.aan be used for zones of stable as 'ismio,activity, highly-sensitive ones..~~ for unotable zones. 'The former can.be used for determining the epicenters of'earthquakes with an error of only 15-20 km and observations made from these stations car. be used for compiling 115#000,000 seismic ioning maps* Observations of highly-sensitive stations can be used for larger scale seis- mic =ing maps* The author discusses in detail the possIbility of using ob- servations of micro-earthquakes for determining the recurrence of strong earthquakes and the maximum intensity of individual,areas,'stating that still more data is necessary for this possibility to be realized. The data of these-observatione, however, coupled with geological datap can be success- fully used for tbe delineation of individual oeismically-active zones. A.A. Fogel' and I.V. Gorbunova are mentioned in connection with the compilation of a seismic map. There are 5 figures and 2 Soviet-bloc references, ASSOCIATION: Inutitut fiziki Zemli AN SSSR (Institute of Physics of the Earth of the AS USSR) Card 2/2 S/261g/64/000/033/0124/0143 .,ACCESSION NR; A14045972 ',AUTHOR: Vvedenskayi~j Dzhanuzakov, K. D.; lodko, V. K.1 Kondorskaye, N. va; Irk.'( -i J rfavgdln~lclg; ~!s~prlnq, L. A.; ~natsakanyan, 0# K.; Ragimov. Sh. S.; Semenov, G. ;-TITLE:' 13yulleten' sIPWIth',zemletryasenly SSSR (Bulletin of the Strong Earth- quakes of the SSSR) for 1961 !SOURCE: AN SSSR. Institut fl;lki Zemll. Trudy*, no..33(200),'1964, Vopros 12 -1 3 ~~inzhenernoy seysmologil'i (Problr-ms of earthquake engineering), no. 9 4 "TOPIC TACS: geophysics, selsm.4~,logy, earthquake, earthquake focus, earthquake epicentet Ity seismicity earthquake Intens ABSTRACT: The " Bu I I et I n of the'Strong Earthquakes of the SSSW Is a periodic annual summary which simultaneously summarizes all fnstrumental and noninstrumen- tal data on the strong earthquakes (Ii > 4) occurring In the Soviet Unlon.The Dilletin ~-.contalns a catalogue of earthquakes (r~_eproduced In the paper for 1961 In the form ;:,of a lengthy table), a map of the epicenters and a brief description of the stron94 est earthquakes.-The catalogue Includes Instrumental data on the coordinates of the epIcenter, focal depth, magnitude M and the time of occurrence of earthquakes, taken from the Byulleten' setl seysmichesklkh . stantsh, SSSR (Bulletin of the Net- ~qoj~ %f Seismic Stations of the SSSR) arid,nonlnstrumentat data Information on Car r mown ACCESSION NR: AT4o45972 the sen5ed Intensity of earthquakes, received from reports submitted by local in-' habitants or from Investigations devoted to descriptions of the strongest earth- quakes. With the exception of the Kurile:-Kamchatka zone, In the catalogue there are data for all earthquakes with M >,4, and all earthquakes for which K was not determined but which were recorded t;y- seismic stations of the general type.as'. having epicentral distances greater than 1,000 km. Data for the Kurile-Kamchatka Include all earthquakes with H > 5'. A map Is presented In the pape'r which zone shows the location of the epicenters7of the earthquakes listed In the catalogue; _.,~_numbers on the map correspond to the numerical listing In the catalogue. In 1961 there ware 272 earthquakes in the SSSR with M > 4. Their distribution by regions and Intensitl is tabulated in the original t-ext. Fig. I of the Enclosure shows the value Y, ETh for Individual seismically active zones of the SSSR for 1961, computed using the formula-19 E .-1).8 + 1.5 M. Fig. 2 of the EnWsure shows the. 'o_change with time of the deviation from the mean annual-volue'p, El 2 for four sels-' micaW actlveoone!;. Along thi y-axis of the graph there i~ plotted the valuT ME - (2 E ZYnean and along the x-axis - time (1946-1961)., The value (E mean for each zone Is Indicated at the right of the graph., The authors go on to- describe briefly, but Individually, the most Important seismic phenomena occurring, In various regions oaf the SSSR In 1961. The annual publication of the Bulletin was begun in 1956 and until 1961 It was printed In the Trudy* Instituta FIzikI SSSR In the collection of articles Voprosy Inzhenernoy seysmologil C1, cro I 1 4 r ACCESSION NR-. AT4o4!;972 (Problems of Earthquake Engineering). Beginning with the Bulletin for 1962, the report will be published In annual numbers of Zemletryaseniyp SSSR, which will be a separate publication. Orig. art. has: 11 figures and 1-table. ASSOCIATION: Insti.t.ut fIzIkI-ZemII AN SSSR (institute of-Phylles of'the Earth, AN - SSSR) SUBMITUD: 00 ENCU 03 SUB'CODE., ES NO REF SOV: 004 .OTHER: OaO Card 3/6 ENCLOSUREI 02 ACCESSION NI,: AT4045972 Flg. 2. ova if~jv ""Pi 210 0. ljJ /if It- R RE card ACCUSION IfEt I AT045972 ZNCLOSUREj 03 Continuation of Fig. 2. -/I % opt 0 8 N a h Apo ,Erl/2 Change In JEI/2 an with ) An time 1946.1961,: 'a'- Far East; b Central Afla; c m Eaucasus; ,cl- Baykal. card 6/6 VVEDIENSIK,AYA, 11. A. N. A. --- "Investir,,,tion of the Plutanic of Central Asia." Sub 11 Jun.52,, Geop~rynics Innt, Acpd ~Sci lj=to a i c mna t, i cmn t i ca I (Dis-,, crta Lion for the Dof-rec of Cnndid-,ite -in Phy Scicnces). , - Vech(!rzinya Elos Janunry-Deccmber 19"2 50. kvn VV V4 P_w ?" A Y A, V1. A " USSR/aeophysice Seismology FD-11 Card 1/1 Pub..45-1/8 -Author Vvedenskaya, N. A, Title t Procedures and results of generalization of the observations by the uetvork of stationary seismic stations in Central Asia, 1950-53 Periodical t Izv. AN SSSR, ser. geofiz., No 6, 1954, pp 497-514 Abstract The author gives an account of observations of Central Asian seismic stations. Using charts of epicenters she draws a conclusion about a definite relationship between the distribution of earthquake centers and the geological structure of a region. Establishes a dependence in the distribution of centers of mild and severe earthquakes. Institution : Gecphysics Institute, Acad. Sci. USSR Submitted : May 4, '15954 USBR/Physics of the Earth - Seismoloa, 0-3 Abot Zcurnalg Referat Zhur - Fizika, No 12, 19561 36361 Authors Vvedenskaya, H. A. Institutions None 'title: Concerning the Accl=acy of Determining the Position of the Focus of an Earthquake Uning the Method of Intersections Original FeriodIcal: Tr..Gt3ofiz. in-ta .411 SSSHj 1955o No 30, 127-136 Abstracts A solution is obtained for the problem of estimating the accuracy of determination of the foci of earthquakes using intersections de- pending on the accuracy of reading the time difference in the ar- rival of the longitudinal (P) and tranevereo (8) waves and the relative positions of the stations. To derive the initial calcula- tion equations, the method of the time fields Is used with the followtug assumptiores the hodograph empl*yed is assumed accuratei the idiamtification of the waves was correetly madej the medium has a 3-layer composition -- granite, basalt., and ultrabasalt, Card V3 USM/PlVsics of the Earth - Issionoloa.. 0-3 Abst Jcn=a1z Referat Zhur - Fizika, No 12, 1956, 36361 Abstract: with horizontal separation boundarieaj the propagation velocities of the waves and the thicknesses of the layers used are in ac- cardance with the data of Ye. A. Rozova for central Asiaj the speed is assusted to vary linearly with depth in the ultrabaoalt. For the majority of seismic statione, the error in the determina- tion of the time t. - tp is approximately 41 sec. For earthquakes with normal depth of focuB the accuracy of determining t1te position of the epicenter and of the deptliof focus is greatest when Using tbi difference tff - tp . The egcenter can also be sufficiently accurately determined By Using ts* - tpi, but then considerable errors are possiblo in the determtoatirm of the depth. When de- termining the position of the epicenter of a deep earthquake, when the time difference of the arrival of the "direct" waves P and S Is used, It Is necessary to assign greater veight to the observa- tions frcm relatively remote stationo., while observations of nearby stations are emphasized in the determination of the depth of fQCus. As t1uy number of stations is Increased, the observations of which are uned, the errors in the determination of the position of the focus diminish. Calculatioms have shown that undAr the most Card 2/3 USSR/Pbysics of the Faarth - Seismology,, 0-3 Abst Jornmal: Referat Zhur - Fizika, No 12, 1956, 36361 Abstract: favorable placement of BtAtione located from 100 to 1,000 km avay from the epicenter., t7he position of the epicenter can be determined in the best case with ~b accurac of �10 km. In practically moot cases the error is greater than 110 km and in :Lndividual*casee it reaches 40-50 km. In the compilation of the maps of epicenters it ~s therefore necessary to estimate at least approximately the ac- curacy of the deteinination of thepoidtion of the foci, since othervise it will be difficult to conclude whether the particular foci'of -the earthquakes belong to any definite geological struc- tures. Card 3/3 fVS I< A Yn.) N. A, USSR/PJjyeics of the 4arth - Seismology, 0-3 Abst Joramalt Refazut Zhur - FizLka, No 12, J-56, 36363 Authors Vvedenskaya, N. A. Institutico: None Title: Concerning Reporting the Observations of the Stationary Seismics stationfefof central As�a Or:4;inal Perio~ticals Tr. Geofiz. in-ts, AN BSSRY 1955, No 30, 137-141 Abstract: A description of the procedure for determining the foci of earth- quakes vhen ccwpiling the bulletin of the stationary seismic stations of Central Asia. 1%4--plotting of the epicenter maps -- the second stage in theproceosing of the observations -- was discussed by the author earlier (Referat Zhur - Fizikaj 1955, 18124). Tm Central Asia, the Ustance between stations and epicenters does not exceed 600 km, and u3uaUy is not less than 100 km. For these conditions it is most :rational to determine the epicenters using the hyperbola or interaection methods (based on the use of the hodograph). The methcd Card 1/h, USSIt/Phyoice of tbAl EGrth - Beiazolov, 0-3 Abst journal: Reforat Zhur - Fizika., No 12, 1956., 36363 Abatract: of Intersection makes it possible to employ simultaneously ob- servations frcm nearby and remote stations; its principal short- coming Is the ne&I for study of the vayes of various types and this means that V; is neceoeary to employ for all of Central Asia one average hodograph (although the hodographs differ for different epioevtTal regions). The waves that are the most de- penclably identifi-nd are the F and T, or P and 9 at epi7central distamces A. that are less than 170 km. Th6 travel times of the and F waves are Wependent of the thickness of the earth's crust and at A < 5d they depend little on the depth of the foew, if the latter is lc~cated witb.Ln the earth's crust. Hodo- graplas of F and Uwayes in different regions diffe ittle from each other. This makes it possible to emplo, lerences the obSW-VatiOnS of stations at A< 170 J= (the difference in travel tine is less than 2 seconds). The dependable element of the hodoipraph of Central Asia is the appeaent velocity of the P wave (718-8-1 kolsec), diffracted by the lower surface of the earth's ,A*Ust. and arriving first at A > 200-250 km. Using the Instants aT-vt'dch the P waves arTive at A*7 200 km, It is possible to Card 2/4 USSR/Plwbics of the Earth - Sei8#409Y) 0-3 Abst Jciurnal: Referat Zhur - F12:�ka, No 12,-1956, 3063 Abstract: detexmine the epicenter by usljje,.-1~4e hyperbola method. Errors causi!& by inaccurate knovledgem*t'th) velocity in the granite laye:7 (from 5.5 Vr 6.0 IM/sec) vill. be insignificant. If one employs observati'O'Ds of stations in which the times of arrival of the first waves are close to each other, but which are lo- cated an the opposite sides of the epicenter, and if the speed Is tALken to be 5.8 kmisec. Under conditions prevailing in Central Asia it is advantaf .eoiis to employ methods based on the assumption that the hodograph'is a straight lina. The determi ation of the depth of the focw of tha earthquake using the Vadati method is possible mly for the small region in northern Tien Shan. The use of waves of the type pP,, BP, and oS is possible in rare cases. It Is. therefore possible to employ in practical cases only the methcd of intersectips, which requires a knowledge of the exoct W4*ra;hs for various depths of focvs. Tha depth is determined with relative accuracy only for foci under the 6arth's crust. In the presence of an FAve-mged hodograpb. for aU of Central Asia, it is necessary to confine oneself to an approximate estimate of the depth of focus. In the conclusion the author speaks of the Card 3/4 USSR/Physics of the Earth - Seismology, C-L Abst, Journal; Refetrat Zhur - Fizika, no 12, i956o 36363 Abstract: incompleteness of the datafgiven in the bulletins, and expresses ideas concerning the trendb3 of development of more accurate metbods for detennining the coordinates of the focus. card 4/4 VVIDINIZLYA.".. Isolating the wave sP in records representing deep-seated earth- ,quokos in Central Asia. Trudy Goofiz.inst. no.36:25-34 056. - (HLRA 9:8) (S-oviet Central Asia--Seismometry) SOVI 49 -58-11-13/18 AUTHOR: Vvedenskaya., N. A,. TITILE, RdiationiW.-P 1xi Time, tht., Yae-atlane In Sidsszl,~ Ac-tivity of Neighbouring Epicentric Regions (0 svyazi vo vremeni mezhdu izmeneniyem. seysmicheskoy aktivnosti blizko raspcilozhennykh epitsentral'nykh zon) PERIODICAL: I:zvestiya Akademii Nauk SSSR.. Seriya Geofizicheskaya, 1958, Nr 11, PP 1394-1398 and 2 inserts (USSR) AB,13TRACT: In order to establish a relationship between time and variations of seismic activities in various epicentric regions, an analysis of the earthquakes in Central Asia was made between 1950 and 1955,, Six regions of the highest activity were chogen (Fig.l) for which graphB were prepared, showIng the total en6rgy of elastic. waves and the nuiebor of ea.rt:aquakes oc^--,xr-ring in theoe regions during that time (Fig~2)~ The graphs weTe based on the logarithmic, scale acco.rding to the formula .1og 1-3 - 3.0 +- 1,7 M where E - energy in ergs,, M - intensity, From all the selected regions. only region IT was found to be suitable for detailed, It was divided Into two areas (A and B in investigatiq)i Fig,l) and cumulat.ive graphs of the r-!Iastio wave energy were made fo-r each of them, This type of graph is very Card 1/4 useful but does not always give an exact picture. Therefore, SOV/ 49-58,--11--13/18 MAbionship in I'Lua 11,;Avitu *1 of NeighbourJ-ng Epicentrie Region-o both logarithmic and cumulative graphs were considered, The analysis of graphs for two areas showed clearly that an in- crease of seismic energy o-11 one ,,aused a decrease of the other-, These examples are indicated in Fig,.3 by the arrows. In order to define the relationship between the variations of seismic activities in thA, differeat nreas situated still nearer each other, a detailed analysis was made for the Garm region. This region showed relatively high seismic activity in 1930 to 1955,, with t-1-he epicenUres positioned more exactly,, Fig.4 shows the map of tht% Garm region where the distribution of the epicentres of weak eart'hquakes (M - 39 3.5 and 4) is indicated together with the stronger earthquakes marked in points. Based on this dis-tribution, four areas were distin- guished which., duzing 1950-1955, ahowed the highest seismic activity (Fig'4). The aharacter of variations for each of these areas i; shown in Fig.,5.. whi~ch was prepared, taking into account all the earthquakes of M.:1~3, It can be seen Card 2/4 SUVI 4 ~~-58-11-13/18 Ri1%ti=9h1.p in Time tgWts-i-_t the in-StImde Aitivity crf 11,tai,eibexaring Epicentrie. RetlozA from thisgraph that an Increase of seismic activity in one area causes a decrease in the neighbouring areas. These cases are indicated in Fig.5 as dotted lines, In some iso- lated. cases where this relationship did not occur the ex- plana.tion could be found in the special geological structure. It WELS found that a generalisation. could be made that an increase of activity of one epicentre always causes a de- creaEie of others situated not further than 200-300 km away, This did not apply to the strong earthquakes which only caused some delay in. the accumulation of tension in the ad- jacent areas. In order to verJ17 the result -s obtained., the period of 1927-a'.949 for Central. Asia was investigated; but due to the inadoquate observations during that period, a detailed analysia could not be made, However, the Card 3/4 SOVI 4'9-58-11-13/18 A'alAicraship in TU4 Vsjghb6ui1n9 Epit6ntric Rajdcn-v inventigation did not contradict the results obtained for the period 1950-1955~ There are 5 figures and no references. ASSOCIATION: Akademiya nauk SSSP., Institute fiziki Zemli (Acad6M7 Of Sciences USSR, Institute of Physics of the Earth) SUBMITTED: June 26, 1957. Cwrd 4/4 Vy~,D~F IODKO, II.K.; KONDORSKAYA, !,,'.V.; L.A. ; flNATl;',AFJ-NYA.N) D.11,1. ; RAGINW, 5h.S.; SM-171NOV, P.G.; T13,'LLVIC 7.11. Bulle~ht ot powerful earLhouakes in tile U.S.S.R. during 1961. .1rudy In:,L. fiz. Zc-m. no,33. Vop. irz~a. sci!jrn. no.9:121~-143 W= otv. red.; KOIIDORSKAYA, N.11. j, otv. rod. (Earthquakes in the U.S.S.F. in 19621 Ze=letriaseniia v SSSR r 1962 godu, Moskva, Nauka., 1964. 153 p. (MJRA 18.-6) IT-MGOV-r-PN. [V"iuhov,, P.M.); GONCHAROV, K.S. bloncharov, K.S.1; M.23;,Tiyp V.S. Man~facturingo(- and p-sources for the graduation of dosi- metric apparatus. Lllc~. fiz. zhur. 6 no.2t284 Mr-4p 161. (IORA 14.6) 1. Fl.ziko-tekhnichoskiy institut AN TISSR. Alpba rayl) I ~ Beta rays suroment) (Radiation-Mea S/619/61/000/017/001/002 B' 239/D302 AUTHORS: Medvedev, S.V., Bune, V.I.9 Viredenakaya, N.A., Gay8kiy, V.N. Kirillova, I.V., Nerses~_,T,_f--L., Rii-A-1-c-henko, Yu.1f.2. Savarenskiyj B.F. and SOrBkiy, il.A. TITLEs Instructions for regional seil=0106iCal summaries SOURCB8 Akademi a nauk SSSR. Institut fiziki Z.emli. Trudy no. 17 (1M Moscow 1961. Voprosy inzhenernoy seysmologii no. 5, 128-145 TEXT: These instructions were confirmed by the director of the Institute of Geophysics AN SSSR, M.A. Sadovskiy, on Pebruary 27, 1961. Their objective is clearly to secure a uniform system of recording all seismological data pertinent to building construc- tion, obtained in future in the USSR. The instructions are divi- ded into six parts, containing 64 numbered articles, the follow.- ing being an indication of the scope of each part: 1) General Card 113 Instructions for regional ... S/619/61/000/017/001/002 Section. This defines the purpose and scope of the work. The seismological map of the USSR established in 1957 is being kept up to date by continuing observations. Its scale is 1 1 5.000,000. The maD is tc be used to make seiaiaolo6ical forecasts both for the epi-central zone and for the whole earth's surface. 2) Instru- mental data on earthquakes. This is defined as data obtained now from both fixed and expeditionary stations as opposed to the study of past earthquakes. Uethods of olassification by magnitude, precision of epicentral location and frequency of recurrence are defined. 3) Engineering seiBmology. Under this heading is defined the format of an atlas of strong earthquake with isoseis- mals. This should be on a scale of lt 1,000,000. It is alao hoped. to include data on. the energy density distribution of the frequency spectra. 4) Seismogeological data. Since some regulari- ty is discernible in the distribution of shocks, a 11seismotek- tonic" map should be a possibility. This would be particularly helpful in regions where seismological data up to this time are Card 2/3 S/6191'61/000/017/001/002 Instructions for regional vo. D2394)302 Bpa,ose. Gravitational data could also be useful here. 5) Proce- dtires f or mak".ng seismological summary rjaps and their dccumen-. -vation. These'are to be of two types, corresponding to 1 and 3. above., i.e. seismological maps and maps of iscseismals shcNing energy and attenuation ohara~.;teristics of the region. The way in which thesi:,, should be prepared is described in considerable detail, togetiaer with some guidance about what is envisaged for the seismolektonic maps. 6) Arrangem,ent, duration of -and parti- r;ipants inlhs fulfilmant of the project. The names and addres- ses of the participating institutions for each reGion are 0'4venrthe end of the first term will be at the -end of 1962. The map is expected from the AN SSSR (AS USSR) in 1963. There are 60 Soiiet-bloc referenceo Ca:-d 3/3 lit 'a go P. 'o .48 A VVIMSMYL-ILA.; KOMRSKAYA, N.V. Bulletin of strong earthquakes recorded in the U.S.S.R. in 1956. Trud~r Inst.fiz.zem. no.5:3-19 139. (MIR& 13; 6) (lbrthquakes) vv=HN3xkuo _-HAKO Time relation of changes in the seiaxic activit7 of near epicentral zones. Izv.AN SS67R.Ser.goofiz. no.11:1394-1398 K 158. .(MIRA 11:12) lo-LO SSSRjInatitut fiziki Zemli. (BarthcpuLkes) I UMNSKAYS, N.A.; YOGILI,-A.A. [deceased] I Kap shoving the epicenters of northern Tien Shan. Blul. Sov. po seis-m. no*3:106-117 157. (MIRA 11:5) (Tien Shan-Seismology-4taps) Vil,65,01F,P5k4M *A. 49-58-2-7/18 AUTHOR: Predenskaya IT.A. TIM: On Utilising Observations with Instruments of Weak- Earth- quakes during Seismic Zoning (Ob ispolIzovanii instrmmer- tal'ny1ch nablyudeniy nad slabyrii zemletryaseniyami pri seysmicheskom rayonirovanii) PERIODICAL: Izvestiya Alcademii Nauk S3SR, Sariya Goof 19513, Nr 2, pp.210-224 (USSR) ABSTRACT: On the basis of analysis of observations of turbulent seia-mic stations of earthquakos in Central Asia between 1950 and 1955 an attempt is made to establish the relation between the distribution of tremors of weak and stronn- ear-,;hquakes and to solve the problem on the possibilitly of utilising the territorial distribution of weak earthquakes in i3eismic zoning. Analysis of this data as well as the data ol stron--er earthquakes during earlier periods ---?Id of results Published by other Soviet authors leads to tne con- clusion that -there is a territorial linlk be-tween t'he dis- triloution of t'he Loei of weak earthqualces during recent yea:cs wit-h the distribution of foci of stronG, earthquakos u ove:r lon-ar -oeoiods. This pe:vmits utilising datua collect-ed Card 1/2 V FE D F_ IVS K P3 60-36-3110 AUTHOR: Vvedenskaya, N. A. TITLE: Separation of sF Waves in the.Recordings of Deep Earth- quakes in Central Asia (Vydeleniye volny oF na'zapisyakh glubokikh zemletryaseniy Sredney Azii) PERIODICAL: Trudy Geofizicheskogo institutal AN SSSR, 1956, Nr 36, pp. 25-34 (USSR) ABSTRACT: The author discusses the isolation of a reflected- diffracted sP wave in the recordings of deep earthquakes with small epicentral distances, and shows the possibil- ity and expediency of using an sP wave in determining the depth of an earthquake focus. D. P. Kirnos' apparatus was used in Interpreting the kinetic and dynamic charac- terlstics of waves. There are 7 figures, 1 table, and 6 references of which 5 are Russian and 1 English. AVAILABLE: Library of Congress Card 1/1 IVVVNNSKAYA, N. A. Usitig the data of waak earthquakes Ln probleas associated witb the establishment of seismic regiont. Biul, Sov. po saiRm. no.8:60766 160. (MIRA 13:10) 1. Institut fiziki Zemli AN 3SSR, (seismology) USSR*&thematics - Pedagogyo Olympiad Jal/Aug 52 "Mthematical Life in the.USSR-. 14th Moscow School Mathematical Olympiad," B. N. Delone, X. D. Vvedenskays. "Uspekh Matemat Wauk" Vol vn, No 4 (50), Pp 180- 184 'April 51 the Yoscov.Msth Soc together with the Moscow State U and Moscow City Div of Pub Educ con ducted.sub~ect olympiad of students of middle schools in Moscow (7-10 classes). Lectures were 'heard from: Prof kus'h^-irhp Act Mem, Acad.Ped Sci FWSRI Prof V. A. Yefremovich; Prof 225T69 Kosmq~~Mldy, Corr Mem., A2~~dt_Sci; Prof A. P. Yusbkevich; A. A.'Xronrod, Dr. Phys- Math Sci; Prof_!._,.Q_Ge3_itota, Corr Mem, -Acad-Sci WM; Prof P. X. Rashevskly; Prof A. Ta. Xhinchin, Corr Mei., Acaa Sci USSR; Prof Ya. S. Dubno'v; Prof A _'M. Lopshits; Prbf L. A. Lyustec-nik, Corr Mem A;ad Sci USSR; Prof A. G. Kurosb,, Prof V. V. Nemy- takiy; Prof P. S. Aleksandrov, Corr Mem,_Acad_Sci_ M-;,. Prof A-.-T-. 7h, Act'iiem, Acad-re& Acij~; pl~Ci-iim_13ii of docents and csndidates~ Zzemples of problems given the students are shown. Statistical results of solns.broken down by clas- ses of students. 2=69 UM/Mathematico Elliptic Equations 1 Aug 53 "A-Boundar'y-Value.Problem for Elliptic Equations That Degenerate on the Boundary of the Region," D. Vvedenskaya DAB*SSSR,, Vol 91, No 4., PP 711-714 -Acknowledges guidance.of her teacher 0. A. Oleynik. .Zab&blishes theorems,on tbO existen-ze) continuity and boundednees of the solutions to the foliowing eqs: L (u) ymu~,~uvv+au ibu tcu z 0, L-,Jul M Y% +u 4 jbu +cu = 0 ;,Witg the, boundary conditionsyll-Uff= a U'~~"'Au- f (x,y) on G, u(x,O) F(x) on-,-/G/(Pi) ; here V 272T64 &,btc-,A are functio'ni.of x,y and uV 5.s the derivative alone-, 'the. direction, Y(Xy).. ttesentud by Acad 1. 0. PiArevokly 6 Jun 53. 1461 nL~jjA Mathematics - Comp)titions - Moscow Fifteenth mathematical olympics for schools in Moscow. Usp. mat& nauk 7 no- 4, 1952. q RASIMVSKIT, P.E.; VVZIENSWA* N.D.; KOROLIE7, B.H. I?if teenth mathematical ol~vplad for t1ut schools of Moscow. Usp.mat.zauk. 8 no.4:,193-197 Jl-~Ag 053. jMLRA 6-8) (Moscow-Kathematics) (MathematicB-Moscow) 0t T tepon. ;0 9 l 14 (1953). "alpnj~ pf the fw-n au , gill , AU,+&(Z. Or Y)U -0. Y :;+~ +C(r ! -C -q 4" ay + - Ou, +6(r. Y4 , 4-C It viti - Cl. -I, are -oi-~ sid.. rril m a doinain D in the ialf -plane y > 6. l*hr voeffi,tevtf ar,~ a-&, cm~ I art A I yric tvi h -.6 0. m > Gj The ,+)~~,-d , ar, ~tfi f-rm ng oic 6,)ujidar, ( D are ii"-urred to -(insist ~f -vrrwww t,t ,he x axis and ertm. arcs r In the tipper i\all ~diztne .-ti~hug on thew selments. For such a 10main the boundiLry (riAlitions A Y Y) F. f w)-,rc , H A d!r(-x LIW~ makrng ~111 aCtite an Cie With thO InteflOr f,~---Tiai to r A 90, and Max (A (9, y)--C(x, y)) v Is similar to the behavior of dg/dO. The posai- bility of smooth solutions An.the whole range 0 s 3 s 2v is questioned. The nature of a singularity of the solutions obtained for the windward side of the cone-at --0 - w is -analyzed W:-.- Orig 0 arto-haer 3 figures-O 12 - formulas and 1 table.- ____ -[All] SUB CODE:- 20/ SUM DATE: -28Dec64/ ORIC REP:~ 003/ OTH REP: 003/, ATD-PRESS: 4 -1--card ___'2/2 7- 1~ M-M SOURCE CODE: UR/0421/66/000/005/0036/0040 AUTHOR: Vvedeaskaya, N. D. (Moscow) ORGI& TITLE: A note on three-dimensional laminar boundary layer on a blunt body SOURCE: AN 888R. Izvestiya. Mekhanika zhidkosti I galas nof 59 1966, 36-ho TOPXC TAGSs supersonic aerodynodas, laminar boundw7 layers'Navier stokes equations Prandtl boundary layer, ideal gas flow I .44iA1rVmc1 deal 'ABSTRACT. Prandtl's laminar boundary laye In a stesAy suRersonic flov of an I gad'past a blunt-nosed con at an angle or attack is considered in order to elucidate the behavior of the solutions of three-dimensional Prandtl equations. The eqiations are derived on the assumption that all flow paelameters in the boundary layer change slowly in directions tangential to the surfaceVof thet body. Thus, the existence of discontinuities in thi solutions of Prana=s equations points to the fact that those equations do not ade9justely describe the flow in the whole boundary layer. The solu- tion is sought by a Vinite-difference method. The pticuliarities of the solutions for the lea side of the balf-plane 0.- w, where 0 Is the angular coordinate, are Investi- gated. The results of numerical calculations of the flow past a-spherically blunted' I C"d 1/2 scone at X 4, To n 3000 m const, 200, a - 50, wid~Cp 0.014 Lre given. graphs and discussed., Orig. ixt. has: 5 figures and 8fontulas. .SUB CODE-v 20/ SWX DAM 28Fab66/ ORI(; P"I 005 VVEDENSKAYAI N. N. .1 "Application of the ?,(,ethcd of the End Differences for the Ccnstructi(;-n !:...P Generalized Solut:Lon5 of Nonlinear Equations." dissertation defended for the degree of Cand. of Phys-Math. Scl. at the Inst. of Mathematics im V. A. Steklov., Defense of Dissertations (Jan-jul 1957) Section of IIhynIc%1 Math. Scl, Vest. AN SSSR, v. 27, No. 12, 1957, pp. 108-9 VVEDENSKAYAO N. P. Cand. Tech... Sci. Dissertation; "Experimental Investigation of the Process of Yfichining Splined Shafts with Hob Cutters of Various Types." 3 Oct. 49 Moscow Order of Labor Red Banner Higher Technical School imeni 11. E. Br~ujran v so m0 S U Yn 7 1 KLOKOV, V. G. , VVEDE-MMAYA, IT, P, "The Formation of Re" Side Ant,,Ies In Villinp Slotting Toolso. Stanki I Instrumont, 10, No.. 7, 1939, 1-floscow Tool Plant, Znrinear. Report U-1505. 4 Oct 1951- 3/563/62/000/00.~1/004/004 DC41/1)113 L.X., and Vvedenskayat N.P. Candidates of Technical Sharnenint, and honinr of tools provided with hard-alloy plates diaTond wheels usin,f, ;-..T., C." Gosulartvenn777 I-o-Itot Zovettt IUnintrov SSSR no ai, -.o:natizatqiJ. i 'V.,3.esoyuznyy nauchno-insledlovatellskiy in.itrument:-I-nyy institut. Moscow, Mapbrizo 1961. o va Y.: tekhnolo,,.jy-A izp-ofovIeniya Instrumenta, 131-139 T.-. -he -ontains thf, rest,,lts of invertip-ationi carr~~Pd f;u~ b VNII Y ri"n, di'-)r1ovid whe~!Ia manuracturei at Uf-li.Ch3kiy cha~7ovoy ltavnd (Uplich Clock Plant) and NITalma7. 11,~ Well az nn qnaly:-,iz of non-Ooviet e ta on dia- mon,! -hoels. Thie purpo3e of the study w:ti to obtair. the optimur workin7 con_ ditions anl -r!(IUi.TIInc.-nt r-quirc-montn for r%tionally usini- diamond and to devolop a pro,-rpm "or f,. s(,r.,i-aijtvatIc machint. slisrp-n- Card 1/4 4' Sharp(min and honing of 0 /D!13 inf- and honinr cmttsr~,, nrovidi~d vrl~th hard-alln- pl%tes by -f-ann of diamord wheels. Diamond -xni7eln vilth thr, i~rit sizes -re recomnerided by th4? NIIalma~. 08-39-1-57 nor,-. 'or honinr tools with hay~-!Mcy ,~ , C. k (I M-10 /v;4 )4~28 (-M?O)j fJ14 (IM14), and P110 (V10); -ftheeln with FrIt s.Lzes of 150 i-nd 2.~G -1hould b,~ used for ~,n - - -~r rAD-r -~nll 8-gtb clas3 finirh Its i, 2769-5~' (GOST 2789-59), M40, M2---,~, I VLF I M14 for ',--llth finish ant]. VAO for 12-13th clans finish. V31! lin-i C;- .aine-d .. finish of VIO vrith wheels havin:- grit ni7.ei of 100 and I'io, -7 -1 follovir!j,v diamond conrertration valal-r, ii-avr, been accepted in induttrial prac-I ice:a 100-1,9 con ~-,nlvratior corresuc-i-Inr, to a diamond contont of 0 878 m =3; 50-:' connQntration correspoi..,.inf to a diamond con!--:n* of 0:4179 ZI/m--,J- an-i 5 -` on r-- pondinr to a dianond content of r-,cr::---md3 th. se at xht, witri 0. 21.9 T!~ - c;~- . q, t lined, aince excenniv, TAJ.~:! Z, 'fir -IJ)Qfj 1 -4~-, Card 2/4 Sharpening and honing of s## S/568/61/000/002/004/004 DOWD113 any bond. Thereforep the cross feed and longitudinal feed are chosen within a narrow range of values. NIIalmaz recommends a cross feed of 0-05 to 0.1 mm/double pass and a longitudinal food of 0-75 m/win. VNII recommends that the diamond wheels be fastened like the abrasivo wheels. The following per- centago coolant composition is recommended by the NlIalmaz norms trisodium phosphate - 0.60; vaseline oil - 0.05; borax - 0-30; calcined soda, 0.25; sodium nitrite - 0.10; water - 98.70. It is pointed out that Soviet machine- tools for sharpeningand honing tools by means of diamond wheels should be built, For the clock and instrument making industries, the C 194 (S194) machine tool should be used as basic design modelq and the 3P64 OA64) marhine tool for the medium-sine machine-building industry. Machine-tools for diamond sharponing and honing should have the following specificationst a cross feed of OAl to 0.2 mm/double pass, a shaft wobble of not more than 0.01 mmf a critical speed of 30 to 50 M/0009 and a longitudinal feed of 0*20 V/ to 0.60 m/min. A special installation (Fig. 5) is used for electromechanical sharpening. 'Thelatter reduces the diamond wear by 75%, There are 1 tablef 5 figures, and 1 Soviet-bloc reference. Card 3/4 Sharpohing and honing of S/56-/Ifl/000/002/004/004 j B0417DI'13 Fig- 5- Device for electro- mechanical sharpening. Legend: I - tank; 2 - brushes; .3- insulation; 4 - disk; 5 - diamond grain on the disk; 6 - instrument to be sharpened; 7 - nozzle; 0 - rectifier. :Card 4/4 3/121/631/000/0 1 10CY7101 4 A0O4/A126 AUTHORSi Degtjarenko, N.S., Vvedennkaya, N.11. TITLE: Tool grinding by reans of diamond wheels with bakelite and retallic hinders PERIODICAL; StankI iinstrument, no. 1, 1963# 26 - 30 TEXT% The authors report on Investigationr. of elastic grinding by means of diamond wheelt; with bakelite and metallic binders carried cnjt by VkT In con- nection with resoarch work on the automation and mechanivation of the grinding and dressing of outting tools with sintered carbide bits. As a result of these studies it wa's found thatthe elastic tool grinding with diamond wheels with bakelits binder makes it possible to increase the efficiency by a factor of 5 In comparison to gr;Lnding with rigid clamping of the tool. Optimum grJnding condi- tions are obtained at a wheel speed of 30 Wsec and a preasure of 3.0 kg/cn?, If wheels of A6 grain size W*A 5G% concentration are used-on machining areas of up to 0033 cm2. Diamond wheels with metallic binder of A5 - A6 grain size admit pressures In -the range of froin 7.3 11 kg/cfR2. To reduce clogging of the wheel Card ~1/2 6/221/63/000/001/007/014 To~l grin'dIng by means of &aAwawt whae2v with ..... A00VA126 Surface, wheels of 100% coneentrailon are rooommaded4 Under optinim conditions .of elastio grindlng, diAmWd wheelsvith metallic binders are 4- 5 times more efficient than those with bakelite hinder, while the same surface finish is ob- talned. For me6anizlng " automating tool-grinding processes, the elastic grinding with diamond wheels with bakwlIte or notalUe blyide.r is considerably more efficient than the present tochnoloo of Crinding wIth diamond Wheels, while a surface finish of at least class 9 cm be attalned. The model B 3 -80 (V3-80) grinder for-the dAamond grinding of 'cutting tools bags been 4esikned according to the principle'of elastlic griTkling. There are 9 figures. FETROSYAN.. L.K.., kand.tokhn.naukj kand.tekhn.nauk Grinding and lapping metal-cutting tools equipped vith hard- alloy tips by diamond wheels. Nov.tel:h.izg.instr. no.2:131- 139 161. (IffU 15:8) (Grinding and polishing) S/121/61/000/003/004/oo6 D04O/Dll2 AUTHORS: Petrosyan, L.K., and Vvedenskaya, N.P. TITLE: Sharpening and lapping carbide tools with diamond wheels PERIODICAL: Stanki i instrument, no-3, 1961, 28-31 TEXTs The article contains the results of experimental investigations made at VNII in order to establish optimum techological conditions for sharpening and lapping carbide tools with diamond wheels. References are made to fo- reign practide,-inclucling that of the Norton Company in the U.S. It is stated that the latest foreign trend is to use porous metal binders and a maximum wheel speed of 90 m/sec# and that in the USSR the application of diamond tool grinding in industry could result in high losses in view of tho narrow permissible feed limits*in diamond grinding and the consequences of wheel wobbling and improper dressing. The available Soviet tool grinders are not suitable for the use of diamond wheels. New grinding machine*de- signs will be developed during 1961, and modernized universal grinders may be used for the purpose meanwhile. The experimental data are given in as- tail and illustrated by graphs; recommendations for grinding and lapping Card 1/2 S/121/61/000/003/004/006 Sharpening and lapping carbide tools ..... D040/bll2 three carbide gradesp ~-~2 (VK2), -'-15K6 (Tl5K6) and 73OK4 (T30W are con- tained in a tab'.ee The following recommendations are made-.use of the organic7'.* l(Bl) b-Inder; different grain size(according to state standard numbers) for difforent carbide grades; different diamond concentrations bet- ween 25 and 100%; 1-2 liter/min coolant consumption; 0.01 mm cross feed of wheel per double run for all grades, in grinding and lapping; the use of paste consisting of two portions of vaselime to one portion of paraffin as a coolant in grinding VK2 and T15K6 carbide or lapping VK2 -xith wheels with a 50% diamond concentration. The following problems have yec to be solved before diamond whoels of Soviet make can ba used in in(~,_=Lryt 1) Pilot units of diamond grinding and lapping machines for carbides have to be producedl 2) The production technology of carbide tools with the use of diamond wheels must be standardiised (i.e. curface preparation for diamond grinding, allow- ancen, otoo)l 3) Production of diamond wheels on metallic binders must be started, for such wheels have a lower diamond consumption and higher produc- tivity than wheelo on organic binders. There are 7 figures, 1 table and 2 Soviet references. Card 2/2 IC/I ~-'// W .:' .11 ) VrXMMKA,YA, X.Te.; TOU)SYAMN, G.D.; MASIDVA, A.I.; RUNSOVA, N.A. "mm-WeAwl Organization of occupations for tuberculous patients. Probl. tuterk., Kooky,& No,6163-66 Nov-Deo 31. (CIML 2134) 1o 0 Irzannodar Scientif lc-Re search Institute of Tuberculosis (Director Prof@ A.L. Samoylovich)o im-nn. 40 17.6) 1. 1z !nstAI.,ut.,j I VVEDMKArA; 0.1. "The viralenco factor (H-orubstance) and the protective antibodies (M-antibodies) in streptococcal infections.* Report BubmitlAd to the Intl Congress for Microbiology Montrealj Carutda. 19-25 ;;9 1962 LYAMPERT, I..H.j VV NSKAYA, 0. 1. - Content of M-substance an one of the indexes of the virulence of streptooocoi of the A group isolated during acme strepto- coccal infections, Zhur. mikrobiol,l spid. i immun. 32 no.8t 43-48 Ag 161. (MIRA 15:7) 1, Iz Institute, epidemiologii i mikrobiologii imeni Gamalei AM9 SSSR. (STFXPTOCOCCAL INFECTIONS) LYAMPERT, I.M.j VVEDENSKAYA, 0.1. On tb~ question of obtaining the M-oubetance possessing antigenic properties from group A streptococci. J. hyg. epidem. 6 no.4:442- 449 1152. 1. Gwaaleya Institute of Epidemiology and Microbiology, Academy of Modical Sciences of USSR, Moscow. I (ST.FXPTbCOCCUS) (ANTIGENS) KOVAIZVA, Ye.V.; SHISHOVA, Ye.M.; VVEDEIISKAYA, 0.1. Role of streptococci In thes pathogenesis of rhawcatic fever. Vop. revm. 3 n0.4:3-8 G-D "3. (MIRA 17:2) 1. Iz kafedry dotskikh bolezney (zair. -doystvitollnyy chlen AMI SSSR prof. Yu.F. Dombrovskaya) I Moskovskogo ordcna Lenina meditsinskogo instituta imeni I.M. Sechenova i iz otdola streptokok- kovykh infektsiy (zav. - doktor rued. nauk I.M. Lyampert) Instituta epidemiologii i milcrobiologii imeni E.F. Gamalei (dir. - prof. P.A. Versbi-lova) AM .53SR, VVEDENSKAYA, 0., 1. Cand !.led Sci -- (diss) "kitibodles for various antiZen 0-4L I C- components of hemolytin, strelitococoh in anti streptooocew sermiss Mm, Isr,8. 9 vp (Acad Med Sci USSR. Inst of Epidennioloai wid Microbioloar L-1 Honored Acedemiainn N. F. Gamaley), 200 copies (KL, 13-58, 100) -98- VVEDENSKAYA, 0. L Detem. ination of H-antigens in antistreptococcal sera. Zhur. o1krobiol.epid. I immun.28 no.12:15-20 D '57. (MDU 11:4) 1. Iz Institutn epidemiologii I mikrobiologii iment, GAmRlei AMY SSSX. (STREPTOCTIOCUS, immunolog7, K-antigens in nnti-streptoc. Immune serA (RUB) (DOWUNS SHRUMS, isame) VVEMSKAYA,_.R.,I. Antigen characteristics of autoclaved cultures of group A otrep- tococei and oup antibodies in irmmine antistreptococcal eerums. lab. delo;8 ri.e.91 no.1239-44 Ja 163, (MIRA 16:5) 1, Otdal straptokokkovych infaktsiy (zav. I.M.Lyampert) Insti- tuta apidemologii i mikrobiologii imearN.r.r-m-lei (direktor prpf. P.A Vershilova) AMN SSSR. iSTHMOCOCCUS) (APTIGEFS AND ANTIBODIES) IMARMO. T.A.; VVKMSXAYA. T.Teo OWWRENWNR Exhaustive splitting of brown-coal humle acids by metallic sodium In 11(rald, ammonia. Do)d. AN SSSR 109 no.2:322-324 il #56. 1. Inaltut geryuchikh iskopayemykh akndenikou A.Y. Topchiyevymo (flumic naid) (KW 9: 10) Akademii nauk SSSR.Fradstiavleno (Lignite) 1~ . . I., . 1 1. ~ i - . . , , . ~ 11 . - ~ ~~ -I--- -, ;, ~. , . ~ . . I . , - . . - 11 : .. . I I -- - . 'z- - I '. . - . . . - - I ..: - I -", - ! !- - - a . 900" - . - I I FM flm' "m 6) ~M, EIISXATA. T KWARn T, A J-BI) BELICOVA) . A, Humic Acid Interaction of humic acids of mineral carbons with metallic sodium in liquid a=onia. Dokl. AN SSSR 86 no. 3, 1952. 9. Monthly List of Ibissian Accessions, Library of Cotigress, December 1952. Unclassified. JO 41, tiy sad leftwk via ty~l caorane imcdo%e, A. Vs. - Komkv. 1C. A. Asdriaow.' L- S. Ute&bent, suid T. E. Vredt Lko~ ly A ka. N4*k S.SS.R. 89, MIT= -Pawmmoe of dIO 0.9750, at* 1.4061, was (wtionated bF p 11, 40u1 I'o' Ca 1. sotn' at 231 Oman With to 4 & The oamrAic preuarts were detil. In tolutme by US' deal- -CoOty (111) Were Wcd. by is WW K, ArA the Intrinsic VL using the e4tmtlamn of lfuW'ns (CJ 36 5(076* - 17 09, R TDI d 114 0 0-6, --P)ef; q - v opec4Ar/4)atco - 0; V./Clo- /q/ + jvlks, iowfithl tite I and 2subscriptstefertosal, ,at and somte, nwatic pres- resp., c - onco., d m density, r - e I The follwLig mtilts an reported (frutcm no).,* - yle COU i#ezcy, M. K. resp., giv tn):- 1. 14.3%, etasth- 1.200,000, MOO, 0.479, OM; 2, M570, Plastic, 4M.000, 0.10. 0.475, 643; 3. 30.6%,; very glotk 144 000.0-4A 0.07, OM, 4,15.4%, vitmo liquid 7 000: 0.456. 0.40, - The uafnttIonztM sample had a woli wt. of, 74r In totuene &A in CC4. Tte rel:";on 1wtween IVI was 11 --12.16 X 10-4MO.". Being vC in kluene, If the m2ter4l larotly linear. but the vwiame in j shm", that the fractions difftr samr, in structure, and the swAlltr values *f K indicate th~tt the fta4diOnS at t(jWT( mot, wt. are mom branched. 11te velues of It are smAller th4o those obtained by Scott 'C-4 41 637i) wul mom in ac"id with thom expected by it "I', for Vis0oul liquMs Xftd PkLSAIC mAterials. John flowo.kAti- BELICULs Humic Acid Interaction of hunic acids of mineral carbons with metallic sodium in liquid ammonia. Dckl. All SSSR 86 no. 3, 1952 9. Monthl List of Russian Accessions, Library of Congress, December '2 195~ Uncl. 1.* KO.ROLFIV,. A... YA.',- ANrFYANOV,* K: A-.',' Trr-SqFIA,* L: S." r7nFNSKAYA' T. Eg 2. USSR (6oo) 4. High molecular weight compounds 7. Molecular weight and characteristic viscosity of fractions of polydimetlqlsiloxane, Dokl. AN SSSR 69 No. 1, 1953 9. Monthly List of Ru.sslan Accessions, Library of Congress, May 1953. Unclassified. 1. Xollofxv, A. Ya.,z I. ; VVE'DE-3XIYA, T. Ye 2, USSR (600) 4. Siloxanes 7. Molecular weight and characteristic viscosity of fractions of polydimethylsiloxane. Dokl. All SSM 119, No. 1, 1953. 9. Monthly.List of Russian Accessions, Library of Congress, May 1953. Unclassified. KuXW,R8NKo, i,.A.; Yvicaw-run, T.Te. Water soluble acids of solid mineral fuels. Pochvovedanie no.12.:51-58 D 159. (HIM 13: 4) 1. Inotitut goryuchikh iskopayerqkh Akademii nauk SSSR, (Peat) (qoal) (Acids, Organic) )IMRAREM, T.A.; VVEDEFSKf~TAA Complete decomposition of hunic acids by metallic sodium In liquid a=o:aia. Xhim.i tekh. topl, no*6:25-34 Je 156. (W-RA 9 19) .1 1,1natitut goryuchikh isk avemukh Akademii nauk SSSR. (Humic acicli 4 1 6 SodUm Interaction of humic aclils of mineral carbons with metallic sodium in liquid mmnia. Dokl. AN sssR 86, no. 3;, 1952. 9. Monthly List of Russian Accession!, Library of Congress, Decembtr 1952. UnclessifitkI. MMUUN09 T.A. (Moskva); VVEDENSKAYA T.Ye. (Mosk-va); =j GRIGORIYEVA, Ye.A. (Ko-oWa-T; -6AVELOYLY, A.S. (Moskva) Obtaining of organic acids from weathered.coal. Izv, AN SSSR,, Otdo tekh. nauko Met, i tople no,03.43-249 JI-Ag 161. (MnA 24:8) (Organic compounds) (Coal) VMMSKAYAp T.Ys. 4. Oxidation by oxygen in an alkaline isedium of veatbsrtd coal in varioue otages of metamorphism. Trudy IGI 21:3-15 10. (MIRA 16t 3-1) ITEDE-E-SKIYA, V. IN. Vved-7ns,kava. v. N. ,ft,,jto7ati, rcr-rc, of C,irrent -Itrenr`h 7,rd Time I- ():~Ivarlv Frcmsses." info rmat s I c, rn-.,,,r tek?lrdci.--;',i f- .- 1 4 1 1 1953, Er: V, Fall-M 214-27, Y . - .1 y 7;^~,,mflk M-fprr-nc;~ Tck,-,!cs'., ra~t;a 1 1 STANKOV, S.; TROFTMOV, V.; VVEPEYM=,-A.;. STIRIDOV, A., inzh. vodnogo transporta; CHERNOV,-g-.-, inzh. vodnogo transporta Improve the management of the consDlidated inland waterway network. Rech. transp. 24 no.10:1-3 165. (MIRA 18:12) 1. Nachallnik Glavnogo upravleniya rechnogo flota pri Sovete Ministrov KazSSR (for Stankov). 2. Na.challnik Kamskogo rechnogo parokhodstva. (for Trofimov). 1. Nachs.11nik Severnogo rechnogo parokb.odstva (for Vvedenakiy). D.WILEVSIKIY, Tiktor Tasillyevioh, akademik; SrAPUKHOT. T.I., prof.. doktor geol.-mineralog.nauk, retsenzent; PRUDBUSUT, G.A., prof., doktor skon.nauk. retsenzent; VVEDEN -, -.-$.,,Prof*$ %TT -A A doktor ietor.nauko retsenzent; WUMIKOT, e.A., red.; ARXH"- MIMIATA, H.S,, red,izd-va; YATUSMYN, Ye.B., tekhn.red. (Russian gold; history of its disoovery. and mining up to the middle of the 19th century] Rusakoe soloto; istoriia otkrytiia i dobyohi do serediny XIX v. KoBkva, Gos.nauohno-tekhn.izd-vo lit-ry po chernoi i tovetnoi motallurgli, 1959. 380 p NIRA 13:3) 1. AN USSR (for Danilevskiy). 2.lChlon.-korrespondent AN SSSR (for Prudenakiy). (Gold mines and mining) 4 TVIMENSKIY, Aleltsey Alekseyevich. %Wm- [Electricity in oux life] glaktrichost7o v nashei zhisni. Moskva, Goo. izd-vo tekhniko-tooret. lit-ry, 195). 63 p iMA 7:3) (Nauchno-populi.arnaia biblioteka, vyp. 16). (Electricity) 1 0 4 a it U U W is if is x of v a a x a A1111 ON us issralre of au a OC a I A -A A - I -A. 11 -J-k- P --V I j A 00 J, 00 91b T_ 00 J. G". Chm. (it. S. 14. RTI 11); d A. 25, =11-A study was made .-so 7 Wit 00 9 ot the tf,; of white P Into red whit, in the liqukl state, at temps. "locity of trim,form so 175-MOV. Impurities In wWe P catodyte the tranx(orma0m bt-tween 17&0 and ZVI% 00 therefore the white P was camfully pvfiW by distn. in roetw. in the Interval 175- 00 6; :0 2W the velocity coast. K Increases with time. the more in the lower W temp,. which Indicates that the reaction is outoestalytic at them tempq. Above 2M' the trangfor. matinet folilims the law of nwousmol. revirtiori. showletit a litonjenrotil; (non catalytic) reaction anti K rrinsins rmst. frestdiew of the length of time from the sidn 1`164 Is .00 vlarly true for tenips. sbutc.I(W. At highrr truilm jelsorr 4.1W) the rracli,vi ty becomes much higher and The transformation It accomi*njnl by a smaig see = so is evolution of best, the truip, ii" to 52LV-W)* and the prewrt reaches 42 min, At '00 still high" tevills, Or reactlin slows elown. This prculiar lehavlor Is attritmtrit to 00 the matener In the sawlaus Niaw of several kinds of molt of while 11 that rallidly reach 4*0 a state of ev"Ale equil. and tralet to form particks of felt Il- It L MAIN-OSKY 00 '00 sew a** .0 of 01910004 an Rv Nuft A :~o o 4 0-1 0 0 0 0 o * 0 0 o o ~o o 0 0 0 q o o o 0 0 0 o 0 o Ice 0 '00 00 boo 61146 i* 4.v its so p 0 UO n I a a; a * a I W is a 4 3 "1 9 00114 0 0 o 0 Zo 0 0 0 0 0 0 0 0 0 6 0 0 0 0 0 a 0 ~o o a 0 0 o o o 0 o o 0 o 0 0 0 o 0 Z a V -Irv ,~4v' itV 49, 0 0 0 0 ,-i ],!Mrs A a 6 it 1A o411 0 it w is, _A -j_ 1, As a - L_ .riot 1441t.ts- * A A CIO/ 0 far to do I U. sea TINS *w%dds 4d As C I cetrjys bf 44 sots. A, & V tM3 "m with rl &0& %7 bir It see f via, W, Witt affill, I'llicittiffill I .00 ee'l "j" the C.S." v fle of 'IT, ;;, 04 11 -lls;R I N of tot,. Cl god 100, so 00 8~ 00 t9 to CV- c:4 &So-$L 0'0 ILL 0 0 u it 1416 1; K 7'% 0 0 0 9