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
,
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on
oi
y a nz~
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Plj~3
W11
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. 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