SCIENTIFIC ABSTRACT KUZMENKO, M.D. - KUZMENKO, P.P.

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SCIENTIFIC ABSTRACT
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87977 S/049/60/000/010/012/014 E133/E4i4 Measurements of the Ionized Constituents of the Atmosphere During Anti-Cyclonic Conditions average distribution spectra for positive and negative ions at the heights where measurements were made (300 to 5000 m), The results obtained confirm those found in Ref.l. From these results correlations can be found between the characteristics of the ion spectra and, some of the meteGrological conditions. Thus, during an anti-cyclone, the number of light ions and the conductivity of the air both increase with height. When the relative humidity increases with height, the number of ions decreases or remains constant, There seems to be a slight tendency for the number of ions to vary with the vertical temperature gradient: In some cases, the number of ions does not increase monotonically with height but has a minimum at intermediate heights. It was found that, during the break-up of the anti-cyclone, the positive ion spectrum was different from the negative ion spectrum. The presence of two maxima in these curves is probably due to the presence of dust In the atmosphere. There are 10 figures and 4 Soviet references. Card 2/3 87977 S/049/60/000/010/012/014 E133/F,414 Measurements of the Ionized Constituents of the Atmosphere During Anti-Cyclonic Conditions ASSOCIATION: Akademiya nauk SSSR Inatitut prikladnoy goofiziki (Academy of Sciences USSR Institute of Applied Geophysics) SUBMITTED: February 20, 1960 Card 3/3 S7 3 32704 S/049/61/000/012/008/009 D207/D303 AUTHORS: Komarov, N.N. , Kuzlmenko -M-D~ and Seredkin, A.A, TITLEs A counter for atmospheric ions PERIODICAL: Akademiya nauk SSSR. Izvestiya. Sleriya geofizicheskaya, no. 12, 1961, 1675 1881 TEXTa The authors give design calculations and describe the construction of a portable counter which can be used for field work on atmospheric ions or for laboratory work in physical, medical and biologi..V~ cal applications. The design calculations followed the formulae derived earlier by V.N. Komarov and A.A. Seredkin (Ref. 7: IZV. AN SSSR, ser. geofiz., no. 11, 1960). The counter consisted of 4 main partst A blower. two measuring capacitors, a dynamic electrometer and a loop oscillograph,- The blower was the usual ventilating fan with airspeed controlled by an anemometer; if stabilized mains supply was used, no control of airspeed was necessary., The two capacitors had separate air oupplieg but a common electrical screen. One capacitor was designed for heavy ions: it had an Card 1/ 3 1112 j Oil S/049/61/000/012/008/009 A counter for D207/D303 outer high-voltage cylindrical electrode, an inner cylindrical collec., tor electrode connected to the electrometer, and a cylindrical guard ring, insulated from the collector electrode. The other capacitor --ja-q designed for 'Light ionsi it was similar to the heavy-ion capacitor b-it a thinner collector electrode and no guard ring., The collector ele-~,.ro- des of the two capacitors were interchangeable. The heavy-ion capacit-_ could be used for heavy ions and for slow ions of medium mass; the light- ion capacitor was meant for light ions and for fast ions of medium Mass. Inthis way the whole spectrum of ion masses and velocities could be c:~-- ered by the counter,. The electrometer, designed as )a, 9 .-3 (DE-.31 was cff the type described by H., Palevsky, R.K. Swank and R, Grenchik (Ref 4 8 , Rev. Sci, Instr,, 18, 1947); itasensitivity was of the order of 10 3-ale divisions per Volta The complete counter could be used as (1 an ion s-pe, ctrometer with collection of light ions by the guard ring in the heavy- -ion capacitor, (2.) an ion spectrometer of the type described by H. 13.. rael (Ref, 2. Gerl, Beitr. Geophys., 31, 1931; Atmosphdrische EIektrIz_-'_ tdt~ 1, Leipzig, 1957), when air is passed conse:~utively through the hea-4y- Card 213 32704 S/049/61/000/012/008/009 A counter for ... D207/D303 -ion and light-ion capacitor, (3) an ion spectrometer using the method of characteristics, described earlier by N.N. Komarov and A.A. Seredkin (Ref. 7: OP. cit.) The counter was tried successfully in atmospheric measurements on the ground and in aircraft, as well as in laboratory measurements. There are 6 figures and 8 refeiences: 5 Soviet-bloc and 3 non-Soviet-bloo. The reference to the English-language publication reads as follows: H. Palevsky, R.K. Swank and R. Grenchik, Rev. Sci. Instr., 18 (1947) [Abstractor's note: The initials in this reference were quot- ed wrongly in the Russian originald ASSOCIATION: Institut prikladnoy geofiziki, Akademiya nauk SSSR (Institute of Applied Geophysics, Academy of Sciences, USSR) SUBMITTEDt juiy 14, 1960 Card V3 OZIMEINKO, Mikhail Ivanovich;__SIVAKOV, Arkadiy Rafailovich; GOLIDIN, ------- 0- O.S., tekhn. red. (Transistorized d.c. converters] Poluprovodnikovye preo- brazovateli postoiannogo napriazheniia. Moskva,, Gos. ener izd-vo, 1961 134 p. (MIRA 15:310 ~Electric current converters) KUZIIINNKOi M, St Dissert9tiont Physiological Ifivestigation of the Vater Balance and Wintering of Ton in the Crimea." Cand Biol Sci, Inst of Plant Phye- iology imeni K. A. Timix7azev, Aced Sci USSR, 26 May 54. Vechernyaya Moskva, Moscow, 17 May 54 SO: SUM 284, 26 Nov 1954 Pultawt Pnwillne Cut- I Nu. 2, 1953. Monthly Lis'- .0~' RuGsian Acces~ians, Library of Congrc-,s, Jnrc "63. Uncl. SAMMY, I.Y., kandidat eel IskokhozyaystvenvVkh nauk; KUZKMO, K.Y. Agricultural measures in the spot planting of shelterbolts. Zeml#tdolie 4 no.11:119-121 N 156. KU lo . 2) 1. Direktor Veselo-Po-dolyanskoy opytno-colaktsionnoy stantaii. (Windbreaks, shelterbalts, etc.) U~ s3 9 Fl. Ya j "., o Kliz If ImonRo. NTSV,,- Yofimen'-.0, A.'V- T trni~ t Y oj, winter 7,hunt Se'uotiorl in : - c' l- St k Z t i dl za , - o on oi y a nz~ q , Plj~3 W11 G V. . . . k-Li kt,-.r?lzr, Z, I ~-,v 19 5 7 Duzing the lazt yeara rha vnl-jotlos Ve3e 1?9 ap vc-ra bred. whi.ch ar,~, .-c-i istimt to lo,9f ruot . - v in wtnLul't i"0 lodginf; and droug..'It o 11 plor.a j!j v"4~--I:q 1951-1 lie . JL -- ~-9 73selcnadolvanskayn 4149 Yielded 29.7 to 4--,,o anrpast3lng LL-aosr,.-t~rka by ',-10.8 aWt/lha~ Tr. 1";';5 6 'l-Rrikit-Y P10"U3 tt PrOdkl~~Od !?Lft.3r ')'-55 we-(L b.hw,.~ ral~.3-ov, *,~). /ha oil 1~. clover and . . l i.p D :L/;~ 17 ;CUz 'MY10 R _,- Experiment stAtion in the service of livestock rhiBern. Naukh i pered.op. v sallkhoz. 7 no-8:10-11 '57. (KMA 10:9) 1. Direktor P01tAvskoy sel.'skokhozysystvennoy opytnoy stnntaii. (Poltava Province--Stock and stockbreeding) KUZ I MEW I M. V. '-- ~C=fere=ceon =ncreasirg the productivity of natural lands and tho production of crops rich in proteins. zhur. 14 no,1:113-114 157s (Ukraine-Pastures and meadows) forage Ukr. bote OILRA 10:5) KMIMMO.. M. V., Candidate Agric Sci (dims) -- "Methods of selecting winter wheat at the Veselo-Pbdolywmk Experlmental-Selection Station". Klevs 1959- 17 PP (Min Agric Ukr SSR, Ukr Acad Agric Sci), 150 copies (KL, No 24, 1959, 145) ChMMOdM41M mWo. M. 7-Y~KU&*ijk2. ill:4_11 2. 767 741% Ill ill of 'ilk. twit., "'Ifolit, 1, Iiiii-flull, IvAllf, Alill ill Ill dcnm-. olml. or cltakvdigi like -IOCK"g,ites. Th, d, t., 2.247 and the lurdricss ll~ Optical con-fit. and chrin. compn. ave identical with those of the ordirwry milrolite Ori 1.4gs-11ASSI: rise dchydrati.-o tww and x-ray dia. gilunu are abo iticutit-al. The otrurst-mv of eltalivilony- Iike it Imlit, t. I lor .1111ift. and 11.4,111tallit, IvNiml. litt-3 i;,, the tionlact offoy.,ili. Willi Imlikili- Iic sit phirlint- syvaite, asiamd. with much (Icconal.l. iteph. .lite and frhispar. aegirite, and alkali amphillole. Th, 6uromilic laincrub (+ bergriwimile tkrivrd floill Itwk. iii,initc) irr viarichord Ili the tvittral Imns 4 11%, lngfiwit, vriit%, Tht- chAvilony-liki, maitilite ~, e%rj,hjljI%. d, posit,-l frum thi, slani, -hm - Oil- lwinulss- flut at mi,iticrably lovivr teml... aml ratlwr ~uddvnlv t rystd. W. PRO = .~ - ~-, r- ~, - -4~-t - W- U USSR/Minerals A~~ K-o MN. Card 1/1 Pub. 22 34/47 Kuji - - - -- -AtLtk merLko,, -M-.-V.j -and-Umtova.-M.-E, &eV`i-hi--'-'--- in 1ht'e'+A3-- Nriodical t Dok. 0 SSSR 100/6, 1159-1160, Feb 21, 1955 Abstract I The discovery of a new mineral of the alkali titanium and niobium silicate group is announced. The mineral was named "Nenadkevichit" in honor of the Soviet mineralogist-geochemist Konstantin Avtonomovich Nenadlk-evich, Member correspondent of the Academy of Sciences USSR. The formula of the new min- eral is; AB(Si20 2H20 where A = Ila, K, Cap TR9 Mnj Ba, Mg; and B Nb, Tip Fe. Foi;~ references: 2 USSR, 1 German and 1 English (1890-1946). Tables. Institution Presented by: Academician A. G. Betekhtin, December 16, 1954 KUZ I =No, N.V. 1 -1 ~.. - Maosification and genesis of al)mli pokmatites, Truidy Inst. min, geokhiv4 I kristallokhimt red, slam, uoj:l%~-154 157, (lovocaro tiandras-Pegma:titeo) (-Ku lito VLASOV, Kuz'ma Alekseyevich; MIM&O. MarjZa Vasillypvna; YESIKOYA, Yevdokiya Mikhaylovna; GEIIASIMOVSKIY, V.I.p GYE-677~eologo- mineralogicheskikh nauk, otv.red.; GODOVIKOVA. L.A., red.izd-va; MARUNI, Ye.Ve, tekhn.red.; ICA-SHINA, P.S., takhn.red. [Lovo2ero alkali massif; rocks, pegmatites, mineralogy, geo- chemistry, and genesis] Lov02erskii shchelochnoi massiv; porody, peLl2atity, minerelogiia, geokhimiia i genezis. Moskva, Izd-vo Akad.nauk SSSR, 1959. 623 P. (MIRA 12:12) (Lovozero Tundras--Rocks, Igneous) .KUZIMENKO, M.V.; KOZHPIIOV, S.I. "Karnasurtit," a new mineral. Trudy Inst.min., geokhim.i kristalokbim,- red.elem. no.2:95-98 159. (MIRA 15:4) (Minerals) S/015/60/000/009/002/005 A052/A129 AUTHOR: Kuz'menko, M. V. TITLE: Concerning the geochemistry of tantalum and niobium PERIODICAL: Referativnyy zhurmal.Geologiya, 1960, no. 9, 178, abstract 16966 (Tr. In-t miner&logii, geokhimii i kristallokhmii.. redk. elementov AN SSSR, 1959, no. 3, 3 - 25) TEXT: Ta and Nb are typical oxyphiles and in the processes of mineral formation they display a geochemical affinity to Fe, Mn, Ti, TR, U, Th, Zr, W, So, Bi, Sb, wizh which Ta and Nb form complex minerals or are contained in the minerals of these elements in the form of isomorphij admixtures. In the naturhl processes Ta and Nb accompany alkaline metals, in particular Na and Li. The similarity of orystallochemical and chemical properties of Ta, Nb and T1 cause an unlimited - isomorphism of these elefiients In the processes of mineral formation and a constan presence of Ta and Nb in Ti minerals. In the course of evolution of magma the concentration of Ta and Nb increases from ultrabasic rocks to acid and further to alkali ones. Kb prevails definitely over Ta in all types of rocks. The re- lation of Nb to'T& changes from 5 in some granite agglomerat6s to 17 in basic and ultrabasic rocks. Nephelinic syenites occupy an intermediate position. In all Card 1/2 S/015/60/000/009/002/005 Concerning the geochemistry of tantalum and niobium A052/A129 natural processes, with the exception of the granitic pegmatitic one, Ub prevails definitely over Ta. In the acid (granitic) group of rocks Ta and Ub are associated closely to Fe, Mn and to a lesser extent to Bi, Sb, W, Sn. With these elements - they form complex elements or are contained in their minerals. In the gramosyenit- ic complex Ta and Nb form complex minerals with Ti and TR of the yttric subgroup, with U and to a lesser degree with Th. The concentration of Ta and Nb in granitic and granosyenitic complexes Increases towards the end of the magmatic and pegmat- itic process and then decreases towards the end of the pneumatolyto-hydrothermal process. The concentration of Ta and Nb in alkaline agglomerates depends on the magmatic crystallization differentiation. In well-differentiated agglomerates with a high Ta and Nb content the bullt of these elements separates out in the magmatic process, then in the pegmatitic and pneumatolyto-hydrothermal process. In this case their concentration decreases gradually. In the alkaline ultrabasic complex in the magmatic and pegmatitic processes Ta and Nb are contained in small quantities in Ti and Fe minerals. At the end of the pneumatolyto-hydrothermal process the concentration of Ta and Nb in solutions increases. In the ultrabasic complex Ta and Nb do not form.their own minerals, but are bound 4M Ti and Fe miner- als in -the magmatic process. [Abstracterts notez Complete translation] Author's summary Card 2/2 t P= I EMMM-010 SW/5740 Akad=i7a nmik SSSH. Institut m1noralogii, geoWil-mli i kristallo'chlylli radkiklli ele=ntov Vopro-3, =tnnaralc_~ii, geol-him-li i Caar-ozzina matormbdanij re(EdIt7a elcromtav (Problarz in Nireralo~71, end r-j~oait For--ation of Rart3 I:Icz*-,ntt;) Koaccw, Tzd-vo JO MMM, 1560. 2,53 p. (I-Oricu: Itat Tmay, v7P. 4) Errata printed on the inside of back co-mr. 2,12,00 copies printcd. Chief Ed.: K. A. Tlwov, CorrcsjrndIv3 "Intor, Acadnw of Scioncea UM; Resp. Edo V. V. LyteEbovIchl Ed. of Nblichina Dbanot L. S. Ta=o-,r; Tech. Ed.t P. S. rawIdnn, Pu-,U~CSZ: This book is intended for raolo,-ists, rim- ralo_giata, and 1--trc,,3ral.~mrs.- CG1rI!ZV=-: This Is a collection of e-3 articles on tho for-altion, ecolc,-.7, mir-cralou, patroSr,-,rby, cna rco-Zar;iotry of dorosits, of rx-o cIc-=zt3 in Sitaria, end LSovietj Central Amia. ~:~o distribution and ebar-acturiatica of rare eler--nto found in tL--ca aroaa so voll as at= (ra=titative and qualitat- tivv- =thods of inventIZAirg the roclw and minerals in vhIch thay wv found, Card 116 Probln= In 111naraloay (Cont.) Z-1 or vith uhich tbay are ua Two artichr, inve3tiGation of the pozribilitiaa of extr=tioa =a r-unzatic-a C., Celeni,L=, tcUuri=, and hafnium. 1.0 Tzrvoarlitica are =ntic=d. Each articlo is accompanied by referoncea. TAIMTE OP CO.-.L-.aTS: Gar-x=h, A. A. Peculiorition in thc DistAL-ation of Raro Elcaints in Poly--taUic Dapoolto of th~ Z=inc~;orzk rc,,Ion of rmlmyy Alta-7 3 Sc=nov, Ya. 1. On the Content of Lithir- and lMabidi= in lUmrala of A31mline Pe_-=tites of the I:wsif* 20 I!,%dala7, S. T., and S. rw--mto7. On th3 Caochemistry of Seleni= and Telhirl= in tl,-- CTe Daposita of Al=lyk 21~ Goralthova, V. N. On the Content of Rhani= in Kalybdanitas of the -M!E;,NiFa-n--Co-]Fp~-I.to3,ybdonum Daposits 1 Card 2/6 Proble=3 In lUncraloGy (Cant.) V-7/5740 l==74f IM =:--L= You tova, Yo. M., and 1. 1. Mzzr-ronLo. ryrochlora of th-2 Vichnov7yo rzmtcins, ito rarnacnatic Ucoclaticna, =d tto Pocullarltica of Its C'---=ical Composition Zhabin, A. G., G. N. I 'In-Olltdinov, and 11. Ye. Pa=---zstIc I Ascociations of Accescory 1:1mrals o;? Px--o Mar-onts in M-mccntaot ren:Lti%ad r4macito Intrusive rool'a of th3 Viel=avy7e I'-Zztaiw Zhabin, A. 0. On the Separation Tirz of tho Mvnrals Moblum, Zircozitm, and the Rare Earths in tho , Grenito Pc,=atito of tba Blyumovahaya 111no Sem2nov, To. I. C;olzircozd= in AlLmline Paj;Matites Korkin, V. I., Yu. A. Pyaten!z, and k. V. Bykova. On Britholite of the Alkaline Rocks of Soutl=atern lx~avm 35 51 74 65 90 Card 3/ 6 P.-,a'o.Um in (Coat.) [^.-7/5740 V. V.,, =1 A, D, CLs--vL", .-Va, Cz Ctnmanztar e t:~3 LICIVrIbution Of Accolcorl in Ur-litl L-mlco V* V.p =A Vf 1. ca tta r-,ZCQ1. 0~1 L.-;1.2 ",-zcozc-oa on tL3 Ocztoat of Acz-.:=;7 .~~.orallaa in V. V., =d 0. To. el in lzezti7a A. V. Zoltazlus r.. t ra;:5 V. U., c:A- t3 c2 cco-40t] C"tzal Azin rc"!r-zinap '100 SO vz~=-a C., call:t!--3 7~;::3 tL3 cuuszpup DOV31to 02 CA.=Zti= i=, t::3 C=P.,= P-M =7313 U C-M =:7.3 C? 1-::%o 11. V C=Ztia Ty;~Qs ef r%:~=U3 CrA C.-g I:mz!9aitWjcm3 Cara 3-10 3,31 139 Frolalems in Ninoralosy (Cont.) -CiV5740 Zlm~ova, A. S. On the I-Irclole= of C--~mtic Types of C2rz.=I=-Z0=in&5 Deposits TiU,onenkov, 1. P.,And It. P. in-a=n%mra. Contact Rocks of tbo Lovozersidy Eansif, TraeIr Cenaoia ema t'--a Ftcullaritiaa of Distri- butiop in Them of Ram 11'--tal Umralization Volochkovich, K. L. On th3 Problen of the St tractural roiition of tha Gornoalta7aldy Rare 1:3tal Prminco G:.,zz Arm 141-a-deva, S. 1. Rational I 2tIv-PA of Quantitative Dator:--imtion of Diaceminatod Berjllli- in Grelcom Oros Podionov, D. A., S. F. Bobolov,,B. P. Zolotarov, and Yo. V. vlazam. On Accidental Errora of Quantitatiyo larnaraoaical Anal7sis of Oro 314 is and Concentrates 3 174 155 203 214 Card 516 P-.oblr,= In Zlincralogy (Cont.) Logirc;va, L. A. Expri=nt in ll%amrinG tZ7.o O~Ucal Constants of Qr.:mite and Renierite mC.-.i7CU3 4:7 L,eLsin, V..11. Frosracto in tb-- Indastrilml Z-traction of Scllmima and Telluriun P= tte Products of Ore Procagaing 23 5 KaSanovich, S. Ya. (Econo=ic Sur-.w) 2~6 AVAILA=: Library of Congress Card 616 KUZIMENKO, M.V. ------ - Role of micas in the process of tantalum concentration. Dokl- AN SSSR 140 no.6:1411-1414 0 '61. (MIRA 14:11) 1. Institut mineralogii, geokhimii i kristallokhimii redkikh elemen- tov AN SSSR. Predstavleno akademikom D.I.Shcherbakovym. (Tantalum) (Mica) KUZIMENKO, M.V. Distribution of tantalim and niobium in slightly differpntiated rare-metal granite p~-gmatites and their genetic characthristicB. (Hip-k it, 8) TTudy D40IN - I n!Z2MVKO M. V.; AKELIN, N.A.; SERDYUCHENKO, D.P., daktor geol.-miner. nauk, prof., otv. red. (Genesis of subalka-line granitoids tuiu albitites con- nected with them and the distribution of tantalum arxi niobium in tbeml Genezis subshchelochnykh grani-toidov i sviazanrqkh s nimi allbitav i zakonomernosti raspreds- lenila v nikh tantala i niobiia. Moskva., Naika, 1965. 119 P. (MIRA 18:6) v il KUZIMEVKO. N.D. __ Peribronchitis In children. Ped., akush. I gin. 20 no.5:24-27 '58. (KMA 13: 1) 1. Klinika fakulltetakoy pediatrii (zav. kafedroy - prof. T.G. Balaban) Kiyevskogo ordena. Trudovogo Krasnogo Zuameni meditsinskogo institute, im. eked. A.A. Bogomolitea (direktor - dots. I.P. Alekseyenko). (BRONCHIT I S) TOLOCHKOV, M., po1kovnik;_KUZ'MRNKO, As general-mayor tankovykb voyek; DVORTSOV, F., podpolkovaik; KOVALNV, F.. podpolkovaik; KOLJCSMIXOV. I., gvardii general-mayor; ROKAN01, M., polkovnik,- KALINOVSKIY. V.. polkovnik; BOZHKO, I., podpolkovnik; PAVLOVICH, A., podpolkovnik We discuss projects of now general Army regulations. Voen. vast. 38 no. 8:2-10 Ag 158. (MIRA 11:7) (Russia--Army--Regulations) 5(4) SOV/79-29-5-6/75 AUTHORS: Sumarokova, T.t Omarova, R., Kuzlmenko, N. TITLE: On the Interaction of Tin Chloride With Esters. 2. (0 vzaimodeyst- vii khlornogo olova so slozhnymi efirami. 2.) PERIODICAL: Zhurnal obshchey khimii, 1959, Vol 29, Nr 5, PP 1437 - 1442 (USSR) ABSTRACT: In the present paper the influence exercised by the length of the aliphatic alcohol radical upon the acid-basic properties of esters was investigated. Viscosity, density and electric conducti- vity of the systems SnCl 4 ___C113 COOC8H 17 and SnCl 4 -CH3 COOC16H 33 were investigated. The results obtained on the determination of the properties as well as the calculated temperature coefficients of the electric conductivity, the corrected conductivity and the constant B for thd system SnCl 4 - CH3C00C8H 17 which was in- vestigated at 25 and 50 0, are given in table 1. In figure 1 the diaGrams kEqw*'- composition are presented. By physico-chemical analysis it could be concluded that the components of the system react with one another, thus forming a complex compound Card 1/3 SnCl 4* 2CH3COOC8H 17' The system SnCl 4 -C113COOC16H 33 was in- On the Interaction of Tin Chloride With Eaters. 2. SOV/79-29-5-6/75 0 vestigated at 40, 50, 60 and 70 . The determination results are listed in tables 2 and 3, the calculated values of the corrected electric conductivity, the temperature coefficient of the con- ductivity and the constant B in table 4- The diagrams property composition can be seen in figure 2. On the strength of the physico-chemical analysis it could be concluded that a complex compound SnCl 4* 2CH3COOC1611 33 is formed in the system. It was separated in free state. Its melting point is 560. The electric conductivity in the system indicates the existence of this compound. Figure 3 compares the values of the electric conductive ty at 500 in the systems SnCl 4 - CH3COOC2H 5(Ref 4), SnC1 4 - CH3 COOC8H 17 and SnCl4 - CH3COOC16H 33* The value of the corrected conductivity of cetyl acetate solutions is seen to be far smaller than in octyl acetate and especially ethyl acetate solutions. This can be explaiped by the fact that the formation of the complex compounds SnCl 4.3RCOOR' is a secondary redox reaction. It proceeds via the stage of the formation of Card 2/3 complex acids SnCl 4* 2RCOOR' which become weaker on lengthening On the Interaction of Tin Chloride With Eaters. 2. SOY/79-29-5-6/75 of the radical. A similar rule was found in the systems formed from tin chloride and carboxylic acids (Refs 16,17). Thore are 3 figures, 4 tables, and 17 referancos, 13 of which are Soviet. ASSOCIATION: Institut khimicheskikh nau1c Akademii nauk Kazakhokoy SSR (Institute of Chemical Scioncoo of tho Acadomy of Sciences, Kazakhakaya SSIZ) SUBMITTED: April 18, 1958 Card 3/3 KUZIMEIFAOj N.D.t aspirant Diagnostic significance of the antistroptolysin reaction In t~wil- litiz.and rheumatic diseases. Fed., akush.. I gin. 22 no.6:7-.;9 160. WiA 34:10) 1. Kafedra fakulltetskoy pediatrii (zaveduyushchiy - prof. V.G. Balaban (Balaban, V.H.) Kiyevskogo ordens. Trudvogo Krasnogo Znameni meditsinskogo instituta Im.akad. Bol omolstsa (direktdr - dotsent I.P.Alekseyenko [Aleksieienko LF * jMMUMATIG FMR)' (TONSILS-DISFASES~ (ANTISTREPTOLYSINS) MOSHCHICH, P.S., kand.med.nauk~ MIKENKOp N.D. j aspirant; BLIlVDIAN, R.S., starshiy laborant Serological indexes (antistreptolysin-0 titer, antistreptoliyaluronidase and Gwreactive protein) is jbwamatic fever and chronic tonsillitis in children. Vop. okh. mat. i det. 6 no-508-43 38-.1+3 MY-161. (MIRA 14:10) 1. Iz kafedry fakulltetskoy pediatrii (zaveduyushchiy - prof. V.G. Balaban) Kiyevskogo ordena Trudovogo Krasnogo Znameni meditsinskogo instituta imeni akad. A.A.Bogomolltsa (direktor - dotsent V.D.Bratust). (AUUMATIC FEVER) (TONSILS-ZISFASE) (ANTIGENS VM PJITIBODIES) (BLOOD PROTEINS) BFZNGS, A.M., inzh.; KULAKOITSKIYY V.A., i,'.nzh., YUZIWNK(", N,G~ Self-propelled drop hammer for knocking out accrettons. Mekh..' avtom.prolzv. 17 no.11:26-27 N 163. (MIRA 17-4) GNEDOV, N.P.; -KUZI.MFNKO, N.K.; SKLYAR, P.T. - -"- - -------- Detemination of coal quality. Standardlzatsila 28 no-3; 28-31 Mr164. (MIRA 17:5) i KUZII.ENKO, N.M. Hydrochemical characteristics and regionalization of rivers and temporary currents of water in the Crimea. Gidrobiol. zhur. 1 no.2:15-21 165. (MILRA 18:6) 1. Institut gidrobiologii AN UkrSSR, Kiyev. L 10346-67 E.'WT(N/VdP(t)/~'4_ 1JP(cj JD 6'6 0007008/0055/0060 Xn Ni