SCIENTIFIC ABSTRACT SOBOTKIEWICZ, V. - SOBOVA, A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001651910013-4
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 26, 2000
• Sequence Number: 13
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

SOBOTKIEWICZ# V.
U.qo of calciwo carbide in cupola furnaces. Liver vest 11
no, 3s84-87 164.

STARK, St., 14Mr; SGBOTKOVA H KUDr
Glinical studies on reorganization and therapy of gestoses.
Cesk. gyn. 19 no3:172-179 NY '54.
1. DFK-III. porodnicka klinika KU. Prednosta: Prof. MUDr
R.Peter.
(PRBGMNCY TOXNKUS, prevention and control,
*organiz.)

SOBOTKOVA, Helena
Hemosalpinx after a fall in the gynasium in a case of internal
genital anomaly. Cask. gyn. 251391 no.1/2:106-107 Mr 160.
1. Katedra DrO porodnictvi, gynakologii dospelych a deti FDL.
KU Praha, vedouci katedry prof. MUDr. Rudolf Peter, Dr. Sc.
(!JTJRUS abnorm. )
(FALLOPIAN TURN, die. )

SOBOTKOVA.1 II.; KOVAR, J.; BUHA, K.
Data on the configuration of nitrogen containing compounds. Ft.
1. 17: Coll Cz chem 29 no.8:1898-1903 Ag 164
1. Institut far organische Chemie and Biochemie, Tschechoslo-
wakische Akademie der Wissenschaften, Prague (for Blaha). 2.
Spolana, Neratovice (for Sobotkova). 3. Laboratorium fur Mono-
sacharide, Technische Hochschule fur Chemie, Prague (for Kovar).

'C', ~' "~I
'1.; 1. Techni-~.,ka spo2upi-a-ca: SOBOTKOVA, J.; PAffiL, L.
ef--~'ect cf elevated bcdly temperature on the functions of
.? U i-
i1he respiratc-i-i system in c'flronic asthmatic bronchitis.
Bra'Lisl. lek. listy 45 nc.10.*593-597 31 My'65-
1. Fyziatricica klinika Lekars'kei fpkulty Uri-vrerzity Kc-merskeho
v Dratislave a Ilysk=y ustav pre fyzi-atriu, balneologi-a a kli-
matologiu v Bratislave (veduci: prof. MIUDr. J. Hensel).

MCCHIR, J.; Technicka. spolupraca: SOBOTKOVA, J.
Changes in the ventilation mechanism in bronchial asthma.
Bratisl. lek. listy 45 no.8:486-495 31 0 t65.
1. Ilyskumny ustav pre fyziatriu, balneologiu a klimatologiu,
pobocka v Bratislave (riaditel prof. KJDr. J. Hensel).

SVOBODA, Zdenek; SL)i3UTKOVA, Riroslava
An unusual case of intracardiac calcification, Cesk. rentgenol.
15 no./+:260-262 161.
1. 11 interni klinika fakulty detskeho lekarstvi, prednosta profi-
MDr. R. Foit Rtg-oddeleni nemocnice Bulovky, klinicke zakladny Usta,~u
pro doskolovani lekaru, prednosta ,FJDr. J. Slanina.
(Man DISEAS&S 'ease reports) (CALCIFICATION' case reports)

J1fM,'iNOVA, I.; SOB40TKOVA, M.; THSLEFF, S.; ZFL"IA, J.
AtroDhy in ske-le-tal muscles poisoned with 'bo-tul4n=- toxin.
Physiol. Fohemosl. 13 no.5:467-472 '64.
1. Institute of Physiology, Czechoslovak Academy of Sciences,
Prague, and Department of Pharmacology, University of Lund,
Sweden.

RU-;,V%IIA Chemical Technology. Food Industry H-28
Abs Jour Ref Zhur - Khim., No 12, 1958, No 41461
Author Sobotkove
Inst NOE-9-iv-en-~
Titlo Evaluation of Hogs in a Slaughter House
()rig Fub Socielist. zemed. 1956, 6, No. 15, 930-935.
Abstract A description is given for a feeding technique whereby one
can obtain hog carcasses with a large amount of lerd and a
sufficient amount of loan neati The evaluetion of hog
carcasses in a slaughter house is done by comparing the
sizes of the heads and legs, as well as comparing the ratio
of the weights of the meat parts to the lerd-ccnteining
ones. The determination is also made for water, proteins,
fats, inineral salts in the meat and lard.
Card 1/1

cZECHOSLOVAKIA/Farm Animalg. Swine Q-2
Abs Jour; Ref Zhur - Eioll~ ~!o, 22, 1958, 101152
Author Sobotkova, Olga
Inst
Title Utilizina the Results of Experimental Fattening
0
and Meat Productivity in Swine Breeding.
Orifz Pub: Nas chov, 10,57, Yo. 23, 637-640
Abstract: Fattening indicators of young stock arrived at
u
by being relate,-I to their make and female
parental lines (lenath of time needed to reach
a 100 kg live weightq average daily weight
gains, etc.) were compared to indicators of the
same animals, obtainea after they were slaugh-
tered (weight of the slaughtered animal, per-
centage of meaty parts, wei:r,rht of head, width
of sides, thickness of subcutaneous lard), as
Card 1/2

SOBOTKOWSP~X, Krystyna; 111CIAK, Miec~zyslaw
IlIxed Lumora treatfid ull tho SurgLcal. Clinic of Storri-tology
of the Silesian Acadery of Medicine in 7,abrza. Czag. stoyrI.C'.
18 no.8/9:1125-1130 Ag-3 165.
1. Z Kliniki Chirurgii Stomatologicznej Slaskiej AML w Zabrzu
(KierolA,dk: rjrof. dr. M. Jankowski) i z Zakladn Anatomij Pa'Lo-
logicznej Slaskiej AH w Zabrzu (Kierownik- prof. dr. T,!. "lepo-
lomski).

SOBOTKOWSKA, ',rystyna; POGORZELSKA-STRONCZAK, Bogna
,pilepsy as a cause of craniofacial fractures. Czas. stomat. 19
no.l.:47-50 Ja 1 60'.
1. Z Kliniki Chirurgii Stomatologicznej Slaskiej AM w Zabrzu
(Kierownik: prof. dr. M. Jankowski).

SOBOTKMISKI, Kazimierz
Disseminated ossification of the lung associated with mitral stemals.
Pol. tyg. lek. 17 no.8:302-305 19 F 162.
1. Z Zakladu Radiologii AM w Lodzi; kierownik-vacat; kurator: doe.
dr med. L. Mazurek.
(HMOSIDEROSIS compl) (LUNG DISEASES comp:L)
(MITRAL STENOSIS case reports)

- SOBQTKOWSKj,._qp~zira 'SKA, Irena
~iq-rz; KASPER
A case of Crouzon--Apert syndrome. pol, -yg. lek.. 22 no.23:914-917
4 Je 162.
1. Z Za?-Iadu Hadiologii AM w Lodzi; kierounik: vacat, Imrator-. doc.
dr mod. L.. Mazurek i z Zalcladu Ortodoncji AM w Lodzi; kierownik: doc.
d.r slom. 11. Kondrat-Wodzicka.
(HYPERMLORISM case ropurto)

SOBCYTKC)WSKI, Kazimierz; 6ZANILWSKI, Henryk
A case of myositis ossificans of non-traumatic origin. Polski
przegl. radiol. 26 no.2:117-121 162.
1. Z Zaldadu Radiologii A14 w Lodzi Kierownik - vacat; Kurator:
doc. dr mod. L. Mazurek i z Przychodni Medycyny Pracy dla m. Lodzi
Dyrelctor: dr K.Wosik. (MYOSITIS OSSIFIGAIIS radiog)

1 20 LAN D
1. - I
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Was

Ol.
bones P
Of'
C, J -1
164.
I JI-4
op- -
J,odzi,
jdu~rrlli

TRONCZYNSKAP Jadwiga; SOBOTKOWSKI-, Kazimiers
Anatomical conditions for the development of esophageal voice after
laryngectomy. Otolaryng. Pol. 19 no.2:215-220 165.
1. a' Kliniki Otolaryngologicznej Akademil Medycznej w Lodzi
(Kierownik: prof. dr. med. L. Radziminski) i z Zaklaft
Radiologii Akademil Medycznej w Lodzi (p.o. Kierownika: dr. med.
K. S-obotkowski).

rad,*,:rrrar)iiy in th;~ dlffer~,nllal d4 gnouls of nonv
18 nc.!1;923-?29 1 le
L..3 of L a I Ll , I e k .- J
Z Zakladu Radio lo~cril AM w Lodzi. (P.o. kierownik.- dr. med-
Subotkoviski) .

SOBOTKOWSKI.. Kazimierz; RECZYK, jullanna
'alue of .~ d4oio~ffical teSts In the dia~noais and d.ifferenti-ation
a
of pathological processes of the sallivary glands. Pol. przea J.
radiol. 29 no.3.257-265 MY-Je 165.
1. Z Zakladu Radiciogli AM w LodzL (p.o. Kiero-wn,.k: dr. ined.
K. Sobotko-vski) i z Klinilr--'; Chiriii-gii Szczekowo-Tw-"rzowej AM
w Lodzi (Kierowrik: doc. dr. mel-1. J. Pardach).

SOBOTKOWSKI, W.; POTYNSKI, J.
"Energetistic Measurements of a Carbide Furnace", p. 589, (PRZEMYSL CHEMICZNY,
Vol. 10, No. U, Dec. 1954, 1%%rszawa, Poland)
SO: Monthly List of East European Accessions, (EEAL), LC, Vol. I+, No. 5,
May 1955, Uncl.

SOBOTKOWSKI, Witold, mgr inz.; ZELKOWSKI, Jaaek, mgr inz.
__- - ------ -_ !. I
Needs of the power-producing plant itself as a factor shaping the
consumption of thermal power per unit in modern electric power
plants. Pt. 1. Energetyka Pol 16 no.11:329-331 N 162.

SOBOTKOWSKI, Witold, zigr inz.; ZELMISKI, Jacek., mgr inz,
-
Power station needs as a factor shaping tlie over all heat
consumption in modern power plants. It. 2. Energetyka Pol
16 no.12:358-361 D t62.

FOILWARCZNY, Czeslaw,, mgr inz.; SOBOTKOUSKI, ',.~itold, mgr inz.;
SUCHOU.B. Antoni, inz.
Methods of performing acceptance tests of themal eau4pment in -
power plants. Pt. 2. Ene~getyka Pol 18 no. !-(i.e.51tSUpP1-.Mu1
nauk techn energopomiar 10 no. 3t17-23 My 164-

FOLWARCZNY, Czeslaw, mgr inz.; ~qPgK_WSjj,_Wjto1d, mgr inz.; SUCHORAB,
Antoni, inz.
Reliability and safety testing of thermal inrtallations in
power stations. Pt.l. Fhergetyka Pol 18 no.3t&Wplement:
Energopomiar 10 no.2:14-16 Mr3k4
1. Pion CiepInyp Zaklad Badan i Pomiarow,, Warszawa.

EG.KSTEIN,Z; SACHA,A.; S0130TKS,W.; Urbanaki,T.
n---~r-i-d -
On preparatio properties of 1-cyclooctenylnitromethane. Bul
Ac Pol chim 6 no.10:621-624 158. (Eui 9:6)
1. Institute of Organic Synthesis, Polish Academy of Sciences.
Institute of Pharmacy, Warsaw. Presented by T.Urbanaki.
(Nitromethane) (Cyclooctene)
(Cyclooctanone) (Olefills)

L 32802-66 GIAF
ACC NRj AT6016646 SOURCE CODE: cz/2512/64/012/000/0177/0197
Alois;
AUTHOR: Pros, Zdenek; Sobotova, Carmen; Waniek.2 Ludvik; Pribyl,
27
1 ORG: none Al//
I
TITLE: The velocity distribution of elastic waves in the Pribram graywacke
SOURCE: Ceskoslovenska akademie ved. Geofysikalni ustav. Geofysikalni sbornik, v. 12,
1964, Prague, 1965, Prace, no. 196-214, 177-197
kkys"-"~
TOPIC TAGS:Ageology, electroacoustics, elastic oscillation, wave analyzer
ABSTRACT: The velocity of longitudinal elastic waves in the Pribram -graywacke was
measured in a continued study of uniformity in the mechanical vroverties ot.tte-m-chs-
Samples from a vertical section of the pit at depths down to 1400 m were tested. The
dependence of waves velocity on depth was determined by the electroacoustic method.
It was established that this dependence is continuous and has a local maximum at a
depth of 800-900 m. The change in the velocity gradient at this depth cannot be
explained entirely by "he change in deusity, or by the macroscopically noticeable
change in the composition of the rock. Rather, it shows a correlation with the
boundary (interface) between two geological structures which constitute the rock,
called the Sadecky and the Tremoshensky gray-wacke; the boundary layer is rich in
hematite. The geological characteristics of the rock are given. It is noted that
the depth dependence Av/AP for the given samples was obtained through measurements of
Card

FACC NR- AT6016646
dependence of elastic wave on one-sided pressure. In turn, these measurements have
demonstrated that the elastic anisotropy caused by the rock stratification and shown
in upper strata is diminishing with increased pressure, i.e., in line with the in-
creasing depth. The authors thank Doctor J, Vanek for valuable advice and sugges-
tions, Mrs. N. Pick, and Messrs. K. Lomecky. and R. Havlik for devoted help in tests
treating and evaluating measurement results. The paper was reviewed by-K. Pec.
Orig. art. has: 12 figures, 3 tables, and 1 formula. [KP]
SUB CODE: 08/ SUBM DATE: 24Mar64/ ORIG REF: 004/ OTH REF: o04,

_P;
0
wfcb B>41
13 Starij:' V;
Mad. Nau 12 of
imtris td= from the otit Siul-121,0e. imid-portfoasi
lord tb
e centrea cam at sped of umn!nlfe~ for Owtent
and A resulted W the following
of U, Pb.. Ra, Th X. and Ac
findings. In Cood. latson six the eAtrat of the 5
elements VM covat. throush 0 of tile Sodmen,
is, Ao. awl U de- J
*Ihht, whilaTh tind Pb Me,
In4leadnira leaching proem wh moved R& at hisher rate
thanU,ThjdrPb, GeaemllY.pd heralpar"Otallspect-
tnem tendeA to be hlzhtr to Th an's Pb than 6entral pads
and In the central portions the WU ratio vm 1.7 X 10
Ra tends,
Instead (it the nokmaffy expected 240 X 10 es, U or the
to migrate -to the environment more than doe
products of decompa. of actinouranium. -,The emanatlon
at parts of 'a
coeffs. of powders of all the specimens from a
specimen are of the w=- order of magnitudt. siftot d
1~eeomes Im lmpc:tant. Isotopic compn. of Pb from cim,
00d agreeg,
tCS g
tral, well-preserved. parts of specimens indica
ment W
ith tue local scol. Indkations of age; only PbOIM
ratio leads to some disagremments. Isotope distsibutl
an
'the outer portions of the *Nfiaieus Invariably gavu a highd
Indication of age tlian lud"ted by other methods, althe(
IM2,11/pl)" ratio tended to give lovy results of age estn.

mif~~ cr."n"Os!tIon in
irr:m n)ekii- Y

vc:r e-
a fitimace Tiw,vawrs C T
On IL '~Ad
I and Ph -urfac
'
tcscs 4110wed blat SO-f"'I"n of the, TIL, re
cavaed 'allIhnaticia tc-~-Tp~ Ow PI.P. rf

by of the all~vt~3. 'If)k dc-
Thc nzijAral Vfi(MIRA,~~ :,i n. i ft
with K Ii 1!
thd
not fruabanate it Nowpi,-,Ily. 'r
he. accurac"--of Jla

z I'llf. kotow~ propurtiaTIS foll-.1d vvue
W, bef. St"uber

--MEW
~us-wym

STARIK, I.Ye.; SOBOTO N.V.; LOVTSYUS, G.P.; AVDZEYKO, G.V.;
T,OvTsyug-, N.TOJ.&0-11& 11 !~',
Mods of lead occurrence in naturiil formations [with summary in
English]. Geokhimiia no.7:584-591 157. (MIRA 11:1)
1.Radiyevy7 institut AN SSSR, Leningrad.
(Lead)

SOBCGOVICH., E. V.,
"Certain Problems of the Geochemistry of Lead Isotopes," Leningrad, 1958-
(Dissertation presented and approved for the degree of Cand. Chem. Sci.)
(Radium Inst. im. V. G. Khlotin).

SOBOMVICH
1 .1 E. V.
Sobotovich., E. V.A. G. V. Avzdeyko, 0. 1. Lovtsyus, A. V. Ilc%etsris--Sublimation as a
Method for Deter7,iinir.- Isotcpe Contents of Lead.
t3
The Si:xth Session of the Committee for Determining the Absolute Age of Geologic
Formations at the Department of Geologic--Geographical Sciences (OGGN) of the
USSR Academy of Sciences it Sverdlovsk in May 1957
Izv. Ak Nauk SSSR, Ser. Geol., No. 1, 1958, P. 115-117 author FekiLrokaya, T. S.

SOBOTOVICH) E. V.,
Sobotovich, E. 71.3 G. V. Avzdeyko, G. I. Lovtsyus, A. V. Lovtsy-us - The Method of
Locatin,7 Lead in Radioactive Minerals.
The Sixth Session of the CommittEe for Determining the Absolute Age of Geologic Forn-
ations at the Department of Geologic-Geographical Sciences (OGGN) of the USSR Academy
of Sciences at Sverdlovsk in I-lay 1957
The Sixth Session of the Con-aittee for Determining the Absolute Age of Geologic
Formtiogs at the Department of Geologic-Geographical. Sciences (OGGN) of the
USSR Academy of Sciences at Sverdlovsk in May 1957.
Izv. Ak Nauk SSSR, Ser. Ceol., No, IL, 1958, P. 115-117 Buthor Pebarskays, T. B.

i V 4VVA
AUTHOR- Starik, I.Ye. and Sobotovich, E.V. 11-9-8/14
TITLE: Lead in Natural Formations and Its Isotopic Composition
(Svinets v prirodnykh obrazovaniyakh i yego izotopnyy sostav)
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya Geologicheakaya, 1957,
# 9, p 81-85 (USSR)
ABSTRACT: Lead in natural formations can occur in various forms. The
stability of lead forms with resiDect to different temperatures
and media is determined by their physico-chemical and minera-
logical properties. In order to learn the possibility of
fractionation of lead isotopes the authors carried out ex-
periments with pitchblende from Ioachimsthal, Caledonian
granite and a most ancient granite from Northern Karelia.
The results of these experiments were the following:
1. During the sublimation of lead from the pitchblende
in a hydrogen flow, the fractionation of different lead forms
takes place, which leads to the change of isotopic composit-
ion of leads precipitated at different temperattLres.
2. The shift of isotopic composition with temperature
increase is directed toward the relative increase of the
content of radiogenic lead.
Card 1/2 3. The investigation of other samples containing lead has

SOBOTOVICII, E. V. Cend Chcm Sci -- (diss) "Certnin problems of the geochemisti-f
of lead isotopes." Len, 1958. 22 pp (Radium Inst i-m V. G. Xhlopin, Acad Sci
USZ-)R), 150 copies (KL, 14-58, 110)
-18-

D C 0
ILI

STALIK, I-Ye.; SOBOTOVICH, E.V.; -LOVTSYUS, G.P.; NEsTEROV, V.p.
Radioactive control of pyrochemical means of quantitative extraction
of lead from natural formations. Trudy kom.aaal.khim. 9:341-348 '58.
(MIRA 11:11)
(Lead-Metallurg7) (Radioactive tracers)

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20.109 years) were found,
which are probably due to too low values of the uranium content
in these chondrites. The authors determined the contents of
these elements and carried out a mass-isotopic analysis of the
lead taken from the same meteorites. The lower values of the
age, which were due to the ratios FOPYU23~nd especially
Pb 2o6 /U 238, are within the error limits of the determination of
U and Pb(i 30%). The above discussions lead to the following
conclusion.-.Aor the investigated meteorites, the isotopic
composition of lead does not display any noticeable anomalies
and also the content of uranium and lead in them is
approximately constant. The''age of the meteorites deduced from
these experimental data agreeswith the modern hypotheses about
their age. The authors thank the Komitet po metearitam(Committee
for meteorites) which put the samples at their disposal, and
SOV/20-12373-11/54
For the chondrites Forest City (Forest Siti)
Card 3/4

On the Age of Meteorites
SOV/20-'123:-3*11/54
also'-B.. B. Piotrovskiy and S. I. Rudenko for their help,,
There are 1 figure, 2 tables, and 11 referbnees, 3 of whf6h
are Soviet.
ASSOCIATION: Radiyevyy institut Akademii nauk SSSR ( Radium Institute of the
Academy of Sciences, USSR)
SUBMITTED.- July 26, 1958
Card 4/4

STARIK, I.Ya.; SOBOTOVICH, E.V.; LOVTSIMS, G.P.; IC)VTSfTJS, A.V.; SRATS, M.M.
Determination of the lead content and of its isotope composition
In iron meteorites. Radiokhimiia 1 no.5:596-602 '59.
(MIRA 13:2)
(Lead--Analysis) (Meteorites)

3(5) S 071/1-1- 5 GO -9 - 9/18
AUT11ORS: Starik, I.Ye., Sobotoy4ch, E.V. and Shats 7- ?T
TITLE: On the Problem of 'he -,'.-ge o' Tektites
PETIIODICA-L: Izvest-iya Akademii nauk SSSR, Seriya geologi-
cheskaya, 1959, Nr 9, pp 90-91 (USSR)
ABSTRACT; The origin of tek-tites nas not yet been deter-
mined. Some geologists suppose that the tektites
are of cosmic origin. Their absolute age, deter-
mined by the K-24.r method bit E.K. G ling and
r
and 7.3x106
11-,.L. Yashchenko, is between l.7xlOj
years, that is considerably less than 'he absolute
age of stone meteorites. The authors determined
the age of a tektite by the lead method. Fre-
c)
that the tektite is of cosmic origin, the
sumin
authors fixed its age between 4.7x!09 and 3.'17X109
years. On the other haund, presuming that it is
of terrestrial oigin and 4s a product of rer-elt-
inrr of some sedimentary rocks, --u-id tak4n- 'he
C'ard
~ otope comiposJ 'ion of Tert4ary or Q~iaternary
f

T- i-Les
o the -e 0
e 1roblem
the tel4tite
of
a-,,ithOrS -pixed the E 6-
k, I "'T M j -, jj on aS-
t b O-o e ar s- s aj of a fe
_Q C, 71-US Sa- h,)rs, the
o bc e e !~t
6 ~ - - b
.amc e f"0., tvekt~tes origin~tEd ma-st
a will'il
s, 'I b s -fl".,ther V~-~ea,'ch
z - h re-
of cosmlr~ 0! -..r,
Ther e a
c e
-1110 1 e a -
V. P 11
J-
41- L 2,
S
UM
9
-IT T--7:),.
Card 2/2

3(l)
AUTHORS: Starik, 1. Ye., Corresponding Member, SOV/20-128-4-14/65
AS USSR, Sobotovich, Lovtsyus, G.. P., Shats, M. 11.,
Lovt syus,
TITLE:. Isotopic Composition of Lead in Iron Meteorites
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 128, Nr 4, pp 688-690
USSR
ABSTRACT: C. Patterson et al. (Refs 1,3) found the same composition
with respect to lead isotopes in 3 different meteorites,
i.e. Pb 204 1; Pb2o6 9.5; Pb207 10.4; Pb208 29-5. His data are
in good accordance with the theoretically predicted isotopic
composition of lead in iron meteorites. Several authors
theoretically computed the isotopic composition of the original
lead, extrapolating back into the past (4-5 billion years) the
change in the isotopic composition of the lead of varying age
found in ore. The values obtained in this way are close to
those established experimentally by Patterson. The authors
intended to carry out a close investigation of the problem
mentioned in the title. They first examined the lead content
of the Sikhote-Alin' and Chinge meteorites (I. Ye. Starik,
Card 1/4

Isotopic Composition of Lead in Iron Meteorites SOV/20-128-4-14/65
E. V. Sobotovich, G. P. Lovtsyus, Ref 2). The lead content
of theee~wteorites in the metallic phase is less by at least
one order of magnitude than that published by Patterson for
7
the Canon Diavolo meteorite (3.7-10- g1g). The isotopic
composition of the troili-te and of the metallic phase of the
Sikhote-Alin' meteorite are entirely different from the
Patterson data. Because of this discrepancy the authors
analyzed the meteorites examined by Patterson. The meteorite
samples were chemically separated and the lead was pyro-
chemically removed (E. V. Sobotovich, Ref 4). Table 1: degree
of impurity of the meteorite caused by foreign lead. This
impurity caused by foreign lead is only 10-24%. Assuming that
iron meteorites contain original lead, the impurity by ordi=7
lead must be at least ioMlo of its cosmic content. These'-
experiments confirmed the results obtained on content and
isotopic composition of the lead in the analyzed iron meteor-
ites and they made possible to introduce a correction for
the foreign-lead impurity. Table 2 contains data on the iso-
topic composition of the lead in 3 iron meteorites and the
Card 2/4 troilites contained in them. According to it the composition

isotopIc ComDosition of Lead in Iron Meteorites SOV/20-128-4-14/65
of the Sikhote-Alin' and Hanbury meteorites is the usual
and the isotopic composition of the lead in the ore is
analoguous to an age of several hundreds of millions of
years. The results obtained by the authors are factually
valid for the lead contained in the iron meteorite and they
cannot be explained by impurities caused by ordinary lead
during the analysis. According to the results of the present
paper the meteorites have no common genesis in spite of the
generally accepted theory. Possibly some of them do not
belong to our solar system or they were formed under con-
ditions when lead originating from radioactive processes
was already present. These meteorites therefore cannot be
as old as was previously assumed. if these meteorites do
not originate from our solar system, nothing precise can
be said about them. If they come from our solar system they
have developed 400-500 millions of years ago. The authors
express their acknowledgements to the Komitet po meteoritam
AN SSSR (Committee for Meteorites of the AS USSR) and the
Estonskiy geologicheskiy institut (Estonian Geological
Institute) for putting at their disposal the meteorite samples.
Card 3/4 There are 2 tables and 4 references, 2 of which are Soviet,

Isotopic Composition of Lead in Iron Meteorites SOV/20-128-4-14/65
ASSOCIATI01T: Radiyevyy institut im. V. G. Kh1opina Akademii nauk SSSR
(Radium Institute imeni V. G. Khlopin of the Academy of
Sciences, USSR)
SUBMITTED: July 6, 1959.
Card 4/4

KASHTAN, M.S.; SOBOTOVICH, B.V.; KPWPIN&, T.N.
Raising the sensitivity of the isotopic spectral analvsis
of lead. Opt.i spek-tr. 8 no.1:23-26 A 16o.
(MM 13:7)
(Lead-Spectra)

STARIK, I.Ye.; SOBOTOVICH, E.V.; SHATS, M.M.
Using the lead-isotope method in determining the age of
meteorites. Mateoritika no.18:8P.-91 160.
Mqk 13:5)
(Meteorites--Age) (Lead--Isotopes)
COMAM ?We coU~Alcu ct 26 ortla*z an Prcb2fts Le m,etewitles 1=1~& the
?Mwact1me Oe the JUgm Xct*orlUc Caaf*r*w* vUeh too% plac-o la xtmc~,
_Xano 3 - 5, IrA. In intradwtory aft1cle revl~ re-ent Vrogmas in t!w rIvIA.
ve4u-%Lftr1y tn the matter of det.mWag the ap of seteoritos. 1*Uv1&L%1
artI.I.0 di.russ tb* fan, rhysical ml eh~lcxl proprtles, ad me vfxwtr~
it.$.. 11W "tor Vneentod by ft.tars to 4rurwal Ar-b ee..ulus to d1s-
-elod. V-4. rws-k~ d"crlbts th* theary mad %di4c" "w~u-stjq.. r=
daterwinlog tht distribut1m a' ==v in the stam;tom 4~&zg 1~ ~Uvs*%_
=-4y -UC164.
Ror*_~7 S uc, IndivI&MI ax

STARIK, I.Ye.; SOBOTOVICH, E.V.; 10VTSTUS, G.P.
.1 t~
Determining the lead content of iron meteorites. Meteoritika no.19:
loo-loz t6o. (MIRA 13:11)
(Meteorites-Analysis) (lead)

5/020/60/134/003/006/020
B019/B06O
AUTHORS: Starik, I. Ye., Corresponding Member of the AS USSR,
S F, V., Lovtsyus, G. P., Shatsz M. M.,
Lovtsyus, A. V.
TITLE: Lead and Its Isotopic Composition in Iron Meteorites
PERIODICAL: Doklady Akademii nauk SSSR, 1960, Vol. 134, No. 3,
pp. 555 - 556
TEXT: By way of introduction the authors refer to their discovery
(Ref. 1) that meteorites contain lead with various isotopic compositions
The present article deals with the investigation of all main groups of
iron meteorites (octahedrites of various structure, hexahedrites, and
ataxites). From two to three quantitative analyses were made on all of
the 12 meteorites investigated, and the isotopic composition of lead
was determined at the same time. The results tabulated in Table 1 show
that in the majority of these meteorites the isotopic composition of
lead corresponds to that of terrestrial lead. No intermediate isotopic
composition of lead was discovered. Judging from their composition, the
Card 1/4

Lead and Its Isotopic Composition in Iron S/020/60/134/003/006/020
Meteorites Boig/Bo6o
12 meteorites can be classified into two groups. The first comprises
four meteorites of the same isotopic composition of lead as was first
ascertained by Patterson (Ref. 2) and later by the authors themselves.
These meteorites are octahedrites of various structures and contain
1 *'2-10-7 g Pb'per gram. The second group comprises the remaining eight
meteorites containing lead with an isotopic composition corresponding
to terrestrial lead of various ages. All principal meteoritic groups ar~/
represented here. All hexahedrites and ataxites thus belong to that
group which contains lead in terrestrial isotopic composition. In them)
the lead concentration lies at the lower distribution limit of
2 - 4'10 -8 g Pb per gram. The same lead content was established for
coarsely structured octahedrites. A lead content of 2-10-7 g Pb per gram
was found for medium-structured octahedrites. The first group did not
exhibit any marked inhomogeneity in the lead distribution, while the
inhomogeneous lead distribution in the second group accounted for dif-
ficulties encountered in the determination of the lead content. There
are cases in which meteoritic surface zones contain more or less lead
Card 2/4

Lead and Its Isotopic Composition in Iron S/020/60/134/003/006/020
04
Meteorites B 9/Bo6o
than the core. Closer studies are required to explain this. No relation-
ship was established between the lead content and the isotopic composi-
tion on the one hand, and the type and structure of iron meteorites on
the other. Reference is made to the one to two times larger lead content
in troilite inclusions as compared with the content in the iron-nickel
phase. Indications regarding the formation of iron meteorites were in-
ferred from the existence of the two groups. The conclusion is drawn
from the existence of two analogous groups in stony meteorites that the
analogous groups originate from a parental body. The authors thank
L. G. Kvash and A. A. Yavnel' for their valuable advice. They further
thank the komitet po meteoritam AN SSSR (committee on Meteorites of the
AS USSR); the komitet po meteoritam AN BSSR (Committee on Meteorites of
the AS BSSR), the Tartusskiy geologicheskiy muzey (Tartu Geological
Museum) , and the Deningmadskiy gornyy muzey (Leningrad Mining Museum)
There are 1 table and 5 references: 3 Soviet and 2 British.
Card 3/4

Lead and Its Isotopic Composition in Iron S/020/60/134/003/006/020
Meteorites B019/BO60
ASSOCIATION: Radiyevyy institut im. V. G. Khlopina Akademii nauk SSSR
(Radium Institute imeni V. G~ Khlopin_of the Academy o
Sciences USSR)
SUBMITTED: June 4, 1960
v
Card 4/4

STkRIK, I,Ye,~ SOBOTOVICH, E,V.; LOVTISYUS, G.P.
Pyrochemical methods for lead separation from natural formations.
Blul.Kom.po opr.abs.vozr.geo1.form. no.4:114-127 161. WIRA 15:1)
(Lead)

5/081/62//000/005/019/1-,2
B158/3110
S o- o t o v i c h
E. V., Lovtsyus, A. V., Leont
V.
-0 a~ of lo-ms of lea'
o
saurna 1062. 11q, albzt~act
f -,~ ra t i 1. M-iimiya_, no. 5, ~/
51317 (Bvul. jo opredeleni-yu absolyutn. vozrasta -e01.
lrorrmatsiy, ;',N 5~31, no. 4, 1061, 128 - 17j)
~7 7 ril mr;`hod of hi-h tr_-,.~n~rature sublimation of lead is used 'or
Z t U d vof t1ne fcr.-,.s in ::hic'r~ P) is found ir natural formations (Rzh Kqir.1,
Yraction~.I sublimation of Pb in liranium pitch v;as c&vciedl
1 ' ?,~1;)77~-
U . C in. a cvtrr.~_nt of N. (purified of 0 by passing throug!-. CuO at
cl-~:' -, 70-0 2 C,
5000C~. Under those conditions, only PbS is sublimated. At 000 0C the
1 0
mixture of residual PbS ard metallic Pb may be sublimated; at 1200 0 the
.-esidual motallic Pb is sublimated as -.%,ell as -oart of the PbSrj 4? which is
,~,oiwcrt~_d to PbO. AfteZ- driving, off 'the Pb in a current of N 21 -whon its
Cari 1/2

STARIK, I.Ye.; SOBOTOVICH, E.V.. LOVTSYUS, G.P.; SHATS, M.M.; LOVTSYUS, A.V.
Isotopic constitution of lead in iron meteorites. Meteoritika no.20:
103-113 161. (KMA 14:5)
(Meteorites) (Lead-Isotopes)

STARIK, I.Ye.; SOBOTOVICH, E.V.; SHATS, M.M.; LOVTSYUS, G.P.
1.
Uranium and lead in tektites. MoteoritU4 no.20-,204-207
(Tektite) (Lead) (Uranium)
161.
(MM 14:5)

STARIK, I.Ye.; SOBOTOVICH, E.V.
Age of meteoritic bodies and the Earth, based on radioactivity.
Izv.All SSSR. Ser.geol.26 no.10:72-83 0 161. (MIRA 14:9)
1. Radiyevyy institut AN SSSR, Leningrad.
(Earth-age) N~teorites)

S/026/62/000/005/004/010
D036/Dll3
AUTHORS: Starik, I.Ye., Corresponding Ilember (see Association) and
S-obotovich, E.V., Candidate of Chemical Sciences (Leningrad)
TITLE: The age of the Earth
PERIODICAL: Priroda, no. 5, 1962, 75-80
TEXT: This is a popular description of inethods of determining the age
of the Earth, particularly radioactive methods based on the contents of
radioactive decay products, such as lead and strontium, in rock and meteor
samples. The authors themselves analyzed 14 iron meteorites, 5 of which
contained lead of the same isotopic composition as found in the "Devil's
Canyon" meteorite, while in 9 this content corresponded to that of terres-
trial mineral lead tens to hundreds of millions of years old. The Yardymly
(Azerbaydzhan) meteorite is said to belong to the latter group of meteorites.
Fig-ures given for the Earth's age tally with those generally accepted.
ASSOCIATIONt AN SSSR (Starik)
Card 1/1

S/169/62/000/012/004/095
D228/D307
luf HOR, S "jobotovich, 7..V. and Grashcherdko, S.11.
TITIL Question of the possibility of determining the a6e
of rocks from their uranium, thorium, and lead iso-
tope content
IC 1962 9-10,
P
M -DICAL: '~Cfcrativnyy zhurnal, G.eofizik,a, no. 12,
abstract 12A77 (3yul. Komis. po opredeleniyu. absoly-
utn. vozrasta geol. formatsiy, Ui SSSR, no. 5, 1962,
63-71)
T~Z',IT: The isotopic composition of lead is determined by
the correlation of prirnary lead, -,)resent in a rock from its crystal-
lization, and radioactive lead, which has accumulated during the
life of the rock. '~Ihc age of a series of rocic samples can be as-
certained from its known concentration of uranium, thorium, and
lead isotopes. Sucin determinations are feasible if the isotopic
composition of primary lcad is the same in all samples, the ratio
of lead to uranium and thorium differs in different samples, and
Card 1/2

S/1169/62/000/012/004/093
of the possibility ... D228/D307
the lead-uraniun mad lead-thorium ratios have not changed during
C)
the life of -the snriTpIc-P at the expense of additions or los:3es of
parent elez~ients or their dccay products. Systems of cquations,
including those for the arre of a rock and the isotope conLent of
primary lead, are COIII.T)ilCd from the uranium, thorium, and lead
isotope concentrations measured in the samples. The solution of
the system of equations is possible by graphical tactl~ods aneL allows
tlie age to L'c ascertained -Erom. 3 independent correlations tolgether
with the isotopic com,)osition o-f primary lead. Graphical methods
are suggested for processing th2 analytical data and for establish-
in,; the a-'e of: a rocl-, in which there has bee-a one alteration in
part of the lead-uranium ratio (loss or addition of lead or uran-
iurm), and the time of t-his alteration. The e---perimental precision,
the aze of a rock-, the lead-uranium ratio in it, and other ifactors
govern the possibilitv of age cici.1culation i any Darticular method.
Z--Ibstracter's ncte: Com.-ilete translation
Card 2/2

STOUK, 1.F., SOBOTIOVICH E V. SHATZ, M.M., LOIFTZUS, G.P.
Uraniur. and lead in the "Tectites."
"MF,TF-ORJTKA" (-%'OtOorJ te a-Stud leg)
11comittee-g-rl of us no. 20 - 1961, sponsored I.- the
---CA3t'8ox'itIO the Soviot Academy of Soiences - Yozrcl- 1961,
pagest and contaJnIng Collectod Works("Trudyn) of the
Organizet' bY tha !2~t~of the Soviet Aeadeav and
Held in KIF.V 01, 2-4 june 0.

STARIK, I.Ye.; LOVTSYUS, G.P.; SOBOTOVICH, E.V.; GRASHCHENKO, S.M.;
SHATS, M.M.; LOVTSYUS, A.V.- -
Isotopic composition of lead in meteorites in connection with their
origin. Biul.Kom.po opr.abs.vozr.geol.form. no.5tl2-25 162.
(KRA 15:11)
(Meteorites) (Lead-Isotopes)

STARIK, I.Ye.; VOROBIYEV, G.G.; SOBOTOVICH, E.V.; SHATS, M.M.;
GRASHCHENKO, S.M.
Origin and age of tektites. Biul.Kom.po opr.abs.vozr.geol.form.
no.5:26-34 162. (MIRA 15-11)
(Tektite) (Lead-Isotopes)

S/534/62/000/022/001/002
1033/1240
AWHORS: StarikiI.Ye., Sobotovich, E., Shats,-M.M. Rnd
Crashen !o, 36F.
TITLE; The orib,,in of tektites
SOURICE: Ak-ademiyla nauk SSSR, Komit.et po meteoritam.
Peteoritika. no. 22. Moscow, 1962, 97-103
TEXT: The data:on concentration of'U and Pb, and the
isotopic composition of the latter, for 7-samples of tektites,
were treated mathemat'Ically in order tb determine their age and
possible origin. A few different methods show that the age of
tektites is practicnAy equal to zero. The isochrone equations
balculated by the least squares method
Card 1/2

5/007/63/000/003/001/003
4;
Sobotov
AUTHOR: Starik~ I. Ye., S i ch5 E. V., Shats, M. M.
TITLEt On the problem of origin of meteorites and tectites
PERIODICAL: Geokhimiya., no, 3., 1963y 245-253
lrar.-
TEXT: Article considers experiments in deternirdng the time of formation of,
ious stages of meteoritic bodies by use of the isotope of lead content. Differ-
ences in amounts of lead isotones detected in two groups of meteorites all(wed con-, I.,
struction of isochrones Yrith coordinates of Pb207/Pb2O4, Pb206 pb204. The tangents'-,'
of isochrone angle of inclination pernt-tted estimation of the time required to
solidate the meteoritic body depending upon differentiation time of the silicate
and metallic phases. Equations for the isochrones are: Group I (containing pri-
mary lead)-
207/pb2O4 2o6/pb2O4
Pb 3.32 + 0.75 Pb (a)
Group II.- (containing more radioactive lead)
pb206/Pb204
pb207/pb2O4 9.31 4- 0.36 (b)
In spilt-i of this., the considerable error of equation (a) and present state of
Card I of 2

S10071631000100310011003
On the problem of ori&"...
kmowledge of the composition and structure of meteorites do not allow firmly. estab-
lishing genetic connections between stone and iron meteorites.
Concluded that in spite of further studies showing the abandance of ur,
thoriwa, lead, and lead isotopes in tectites their relatively young age doe& not
contradict the cosmic or mixed theory of tect-iAe origin.
Card 2 of 2

SOBOTOVIC11, EN.; GRASHCHENKO, S.M,,; LOVTSYTJ,3, AN.
Isotopic composition of lead in the oldest rocks. Radlokhimi-ia 5
no.2:157-160 163. (MIRA 16:10)

STARIK., I.Ye.; SOBOTOVIGIH, E. V. ,
Geochemistry of lead isotopes. Izv. AN SSSR. Ser.geol. 28
no-3:40-53 Mr 163. (KMA 16:2)
1. Radiyevyy institut, imeni V.G. Khlopina, Len~ngrad.
(Lea4lipotopes)

_S~QBPTOVICH, Ej.; GRASWHENKO, S.M.; ALEKSANDRUK, V.M.; SHATS, M.M.
Determining the age of ancient rocks by the lead-isochronous
and isotope-spectrum strontium methods. Izv. AN SSSR. Ser.
geol. 28 no-10:3-14 0 .163. (MIRA 16:11)
1. Radiyevyy institut imeni V.T. Khlopina, Ioningrad.

n; i(X'l C,
vl,A(A. opr. abq. vazr. geol. obr. ra. :,~~7 `1. 64'

SOWTOVICH$ ~,.V,..; WVTSYUS, G.P.; LOMYUS, AN.
New data on the content and isotopic composition of lead
in stone meteorites. Meteoritika no.24:29-33 164.
(MIRA 17:5)

EWG (v)/EWA(d)/EEC-4/FEC W Pe-5/Pae-2 AF#O/
L 10669-65 rdT(1)/EWT(M)/
r -AFWL/ASD (f -2/DIAAP GW
ACCESSION NR: AT4047021 S/2534/64/000/025/0040/0074
AUTHOR: Sobotovich
fTITLE: Radiogenic and cosmog2nic Is a L meteorites and cosmochronology
SOURCE- AN WSR. Nowitet po meteoritam. Meteoritika, no. 25, 1964, 40-74
TOPIC T`AGS- meteorite, radlogenic Isotope, cosmogenic Isotope, cosmochronology,
meteor matter'!
ABSTRACT: The elemental and Isotopic composition of meteorites gives an indication of.
the processes which cosmic matter has experienced from the time of development of the
nuclei of the elements to the time of the falling of the meteorites on the earth. In each of
the life stages of meteor matter, there was formation or redistribution of radioactive,
radiogenic, cosmogenic and stable isotopes. Almost the full range of half-life periods
of radioactive Isotopes, from 28 days to 4.3-1010 years, makes it possible to define
certain stages in the history of meteor matter and evaluate their intensity. This re(luires
a study of the distribution of a number of Isotopes, clarification of the way in which they
were formed, and comparison of data on different isotopic relations. This has been done
in this lengthy paper, making it possible for the author to propose the following stages in
the history of meteor matter. 12-4.7 billion years ago: Formation of the nuclei of
Card 1/3

L lo669-65
AT4047021
ACCESSION NI
elements by discrete nueleosynthesis. The synthesis of the greater part of the heavy
elements ended.. approximately six billion years ago. 4.7-4.5 billion years ago: Conso
dation of small bodies of asteroidal size and their rapid heating due to short-lived
0-
radioactivity oMer a period of several (up to 20) million years after the end of nucle
I synthesis. In this same period there was a separation of these bodies Into silicate and
metal-lie phased and thermal disintegration. 4.5-3.6 billion years ago: Formation of a
secondary planetary body (not more than 1-2 lunar radil) from the products of decay of
the primary
bodies and primary cosmic dust. 3.6-0.5 billion years ago: Gradual heating
and differentiation of this body and destruction. 11 there were two secondary bodies they
could have suffered destruction upon converging (attainment of the Roche limit). 2.3-0.01
billion years ago. Breakup of bodies of asteroidal size and beginnin of the time of
exposition. "In conclusion, the author wishes to express deep appreciation to his teacher,
the lateZXE~~ Corresponding Member AN SSSR, for valuable advice,
Academician V. G. Fesenkov, Doctor Ye. L. Krinov. Doctor B. Yu. IBvin, G. G.
ynel for detailed discussion of this paper at the Eleventh
VoroVyov and A. A. Ya
-*W-also to his Immediate-assoclates Ma__
Meteorite rence in Leningrad (194~2) M
::-Shats. G. P. javtmms and &- 74 Qrashcih~ ' - took part In developing
Who the t
hypotheses". Orig. art. has: 13 table and 9 fi
a gums.
2/3

AFANAS I YLV, G. D. ; SHCHERBAKOV, D. I.; SEMENPIKO, N.P. ; SOBOTOV I CH, E.V.;
Pl,"KARSKAYA, T.B.
Iosif Evseevich Starik, 1902-1964; obituary. Izv. AN SSSR. Ser.
geol. 29 no.10:122-124 0 164. OMIRA 17:111)

--- SOBOTOVICH, E.V.; G-R~Z-Fv--HENKO, S,kj.
lootlope coTposition of recent leads as a criLe--on of --he age of'
isolated igneous rock samples. Izv. AN SSSR. Ser.Geol. 30 no.4:3,
9 Ap '65. (NEI: RA 18: 4)
1. Radiyevyy institut im. V.G.alopina, Leningrad.

SOBOTOVIGH,.,Ivaa DmItrie ' h; SOBOTOVICH, Yevdokiya Pavlovna; SYTIN, P.V.
' -, ' 'IV, 0`~
-kokt6r~iii6A6hg;-ikR nauk, nauchny7 redak-tor; FEDYAYEVA, N.A.,
redaktor izdatelletva; OASHAYA, A-K.. tekhnicheskiy redalctor
[Moscow from the dock of a motorship; a guidebook] Moskva a borta
teplokhoda; putevoditell. Moskva. Rechnoi transport, 1955. 214 p.
(Moscow-Description) (MI3A 9:10)

SOWTOVICH Ivan Dmitriyovich; SOBOTOVIGH, Yevdokiya Pavlovna; LOPATIN, P.I.,
==-::-~tor; ROKANOVSKIT, I.S., redaktor; IrIDTATBVA, N.A., redaktor
isdatellstys; KRASNATA, A.K., takhnichaskiy redaktor
[Moscow from the deck of motor ship; a guidebook] Moskva a borta
toplokhoda; putevoditell. lzd. 2-oe. Moskva. lad-vo *Rechnoi
transport.* 1956. 259 p. (MIRA 9:9)
(Moscow-Description)

SSOBOTOVICIL. Ivan Dmitriyevich; SOBOTOVICH, Yevdokiya Pavlovna;
ZAREYEV, G.S., retsenzent; FEDYAT&VA, N.A., red.izd-va;
BODROVA, V.A., tekhn.red.
[Down the Moscow canal; a guidebook] Po kanalu imeni Moskvy;
putevoditel'. Moskva, Izd-vo "Rechnoi transport,* 1959. 86 p.
(HOBcow Canal--Guidebooks) (MIRA 12:10)

_YJLH,_-Iv%an--DF.a_trj4Myich; SOBOTOVICH, Yevdokiya Pavlov-na;
_�gIMTD U
SOKOLOVSKIY, Yu.Ye., retsenzent; IVSEIN, Ye.A., retsenzent,
TYUKAVIE, I.N., red. izd-va; BODROVA, V.A., tekhn. red.
[Along the Moscow Canal] Po kanalu imeni Moskvy. Moskva, Izd-
vo "Rechnoi transport," 1962. 123 p. (MIRA 15:5)
(Moscow Canal region--Guidebooks)

'JOBOTOViCil, 11Y.
,hir iri
to the assistant's :blc?~ Vnwrnrit~ifll,i~ zi,lir~ 1- nf) 5: -1-75

SOBOTOVICH, Ivan Dmitrieyvich; SOBOTOVIGH, Yevdok-iya Paylovna; BYTIN, P.V.
koktor istorichaskikh nauk,' nauchh~i~~igd'7ifktbt',--M'fATIVA, N.A.,
redaktor izdatellstva; KRASNATA, A.K., tekhaicheakiy redaktor
[Moscow from the dock of a motorship; a guidebook] Moskva a borta
teplokhoda; putevoditell. Moskva, Rechnoi transport, 1955. 214 p.
(Moscow--Description) (MIJU 9:10)

SOBOTOVICH. Ivan Dmitriyevich; 4QE2Z2VIGHA_Yevdokiya Favlovna; LOPATIN, P.I.,
redaktor; ROKANOVSKIY, I.S., redaktor; FADYAYNVA, N.A.. redaktor
isdat6l'Btva; KRASNATA, A.K.. tekhnicheskiv redaktor
[Moscow from the deck of motor ship; a guidebook] Moskva 9 borta
teplokhoda; putevoditell. lzd. 2-oo. Koskva, lad-vo "Rechnol.
transport," 1956. 259 P- Nmh 9:9)
(Moscow--Description)

SOBOTOVICH, Ivan Dmitriyevich; SOBOTOVICH, Yevdokiya Payl-ayna;
ZAREYEV, G.S., retsenzen ; T,-VA, N.A., red.izd-va;
BODROVA, V.A., tekhn.red.
[Down the Moscow canal; a guidebook] Po kanalu imeni Mosk7y;
putevoditell. Moskva, Izd-vo ORechnoi transport.' 1959. 86 p.
(Moscow Canal--Guidebooks) (MIRA 12:10)

SODOTUVIGII, Iven Di-nitriyovich; SOWTOVICII, Yovdokiya Pavloyna-i
SOKOLOVSKIY , Yu.Ye. , ireI`Fe_n_z_e_R_; -InIIIII , Ye' A. _ retsenzent;
TYUKAVIII, I.N., red. izd-va; BODROVA, V.A., tekhn. red.
[Along, the Moscow Canal] Po kanalu imeni Moskvy. Moskva, Izd-
vo "Rechnoi transport," 1962. 123 P. (MIRA 15:5)
(Moscow Canal region--Guidebooks)

SOBOVA, Alena, RNDr.
Body weight and height of infants under three years of age in Prague.
Cesk. pediat. 11 no-5:341-348 May 56.
1. Ustav pro peci o matku a dite v Praze -Podoli, nabr. K. Marxe c.
157 Redit;1: univ. prof. WDr. Jiri Trapl. nositel Radu republiky
Prednosta pediatrickeho vyzkumu: Doc. IMr. Kamil Kubat.
(BODY WEIGHT, in infant and child,
statist. in Inf. in Czech. (Cz))
(BODY HEIGHT, in infant and child,
same)

CZE-CHOSLOVAICIA/Humn and Animl Physiolo,,y. internal Secreuiml T-8
fibs Jour 11ef 7bur - Biol.) ijo 14, 1958, -,.o 65415
Author Hostoraska L.) Kottova Vi Sobova A.
Inst
Title A Comlarison of the Anabolic Effect of Testosterone anO.
MothyInnC-rostendliol on Proteins in Cases of Groirth Beta-rd-i-
tim-1 in Childhood.
Ori!--, Pub Vai.trini lol-arstvi, 1957, 3, 113 7, 620-630
Abstract 2, stucly was performed --)P- 83 cl.-;1(1-rcn whose ~Xovth was re-
uarOcd. F~)rty-nine chiWron rcccived 10-20 nG of methyl-
Uestosterme for a perioO. i)f t1wo months -with n subsequent
six-nonth interruption. The avera'-?c duratio-ii of treatmat
"as 31 years. The remain"P.- ch-;10,ren receiveO 25 ii~; o-f
racthyl-mid-rostencliol ~-cily until rcachinG the ossification, a.!-c-
level (-- lyear, on the avcra:~c). The Lxowth retardation in
the cliilclxcn was associat&. with hypopituitarism, Turner's
syndromc, cjhondroclystroj~hy aaO. other nausea. M)
Card 1/2

MECIR, M.; SOWVA, A.; HRUBCOVA, M.; KRF.TGOVA, M.
Physical condition & nutritional status of 0-3 year-old
children in the Pardubice region. Cas. lak. cask. 96 no.
24--~25:791-800 21 June 57.
1. Ustav pro pact o matku a dite Praha-Podoli, reditel prof.
dr. J. Trapl. vedouci pediatricksbo vyzkumm prof. dr. K. Kubat
Ustav organisace zdravotnictvi KU v Praze, prednosta prof. dr.
V. Prosek. M. M., Praha-Podoli, Nabr. K. Marxe 157.
(INFANT NUTRITION, statist.
in Czech. (Cz))
(CHILD
phys. cond. of Czech. child. (Cz))

SOROVA, A.,,Dr.
70th anniversary of the birth of MUDr. Iudmila Lukasova. Cesk. Tiedlat.
8 no.6:S47-549 5 July 58.
1. UPMD, Praha-Podoli.
(BIOGRAPHIES
Ink.asova, Ludmilla, biobibliog. (Gz))

BIAZEK, F.; HRUBCOVA, M.; KAPALIN, V.; ODGIMEWVA, Z.; PROKOPEC, M.; PROSEK, V.;
SOBOVA, A.
Examination, follow-im & assessment of nhysical growth & development.
Cesk..Pediat.-13 no.4t296-303 5 MaY 58.
1. F. B., Pfaha II, Ke Karlovu 2.
(GROWTH, in inf. & child
measurement (CZ))

SOBOYA,Alena
Comparison of graphic method fpr the investigation of child
development.up to 3 years of age. Gesk. pediat. 15 no.5:442-
447 Ky l6o.
1. Ustav pro peci o matku a ditev Praze-Podoli, reditel prof.
MUDr, Jiri Trapl, vedouci pediatrickeho vyzkumra NUDr. Urel
Polacek.
(GROWTH)

RAT-A , Karel, C.3c.;,SOBOVA,Alen~t.C. Se.; VAMTOVA, Jaroslava
Total consumption of oxygen in a case of late gestosis. Gesk.gyn.
25[391 no.7:521-528 S 160.
1. Ustav pro peci o matku. a dite v Praze-Podoli. reditel doe.
H.Vojta. zaslouzily lekar CSSR.
(PUGNANCT TOMIAS metab.)
(nSPIRATION in pregn. )