SCIENTIFIC ABSTRACT SAMODUMSKAYA, YE.N. - SAMOLINA, N.L.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001446920020-3
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 25, 2000
• Sequence Number: 20
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

SAMODUMSKAYAY Ye.N.
Dynamics of development in children suffering from Down's disease.
Zhur.nevrA psikh. 62 no.7:1058-1061 162. (MM 15:9)
1. Moldavskaya respublikanskaya. psikhonevrologicheskaya, bollnitsa
No.1 (glavnyy vrach B.A.Morozov, nauchnyy rukovoditell - prof.
A.N.Molokhov).
(MENTAL DEFICIENCY) (CHILDREN--GROWTH)

SAM.ODUROV'. A.;
%0 si 11 tin the teaching staff of a technical school. STO 2 no.ll,,
Ig
50 N 60 (MIRA 13:11)
1. Uchenyy sekretarl soveta Nauchao-tekhnicheekogo obahchestva
tekhnikuma Ministerstva putey soobshcheni,,ra, g.Ordzhonikiclze.
(Ordzhonikid2e--Technical education)

SMCMO%T, 1). (Loningrad)
@,- - @,-
Screem for magnetic recorder heads. Radio no.8:36 Ag 156.
(Magnetie recorders and recording) (NLRA 9*.10)

107-57-1-43/60
AUTHOR: Samodurov, D. (Leningrad)
TITLE: A Stere6-_@Acoustic Outfit. An Exhibit at the 13th Radio Show (Akustichaskiy
agregat s ob"yemnym zvuchaniyem. Eksponat XIII radio vystavki)
PERIODICAL: Radio, 1957, Nr 1, pp 41-42 (USSR)
ABSTRACT: Nonuniform directivity of higher-pitch sounLs and other disadvantages of a
single-loudspeaker acoustic system are mentioned. A group of loudspeakers mounted an
the front as well as the sides of a cabinet produces an effect approaching stereophonic
sound. A 30- to 15,000-cps frequency range and other requirements are listed as nqcea.-
sary to obtain a natural sound from a given electronic-acoustic equipment. The outfit
built by the author comprises four loudspeakers: a woofer-tweeter combination mounted
in the front wall of the cabinet,-.and two other loudspebLkers mounted in the side walls.
In addition, there is a rectangular opening in the front wall designed to convey Imer
frequencies emitted by the woofer. The cabinet dimentions are 650 x 500 x 350 w. Its
wooden walls are 10-mm thick and it is lined on the inside with a sound absorbent. The
loudspeakers used in the outfit comprise one speaker from a "T-68911 or "Riga-100 re-
ceiver (Riga factory imeni Popov) and three IGD.-l speakers. A drawing of the cabinet,
circuit diagrams, construction aids, and alignment hints are supplied.
There are 4 figures in the article.
AVAILABLE: Library of Congress
Card 1/1

SAMODUROV, D. (g.Leningrad)
Simple amateur magnetic tape recorder. Radio no.2:30-32 F 61.
(MIRA 14-9)
(Magnetic recorders and recording)

SAMMLIKMp K. f1foginsk Moskovskoy pe.); FILATOV, K. (Borovichi
Novgorodskoy obl.); MALITSEV, V. (Minsk);-OAMODUROV, D,(Leningrad);
BOYKOV, K. (Kuybyshev); SMITSKIY, V. (Lonin-gr-ad-T-
Our New Year interviews. Radio no.l-.10-11 A 163. (MIRA 161l)
(Radio)

BORISOV, Yevgenly Georgiyevich; �AMODgBQY,-anitriy-_Vasillyevicb--
KOROLIKOV, V.G., red.; BULIDYAYEV, N.A.,rlekhn. red.
- . @_71
[Equipment for sound scoring of amateur film] Apparatura
dlia ozvuchivaniia liubitellskikh fillmov. Moskva, Gos-
energoizdat, 1963. 23 p. (Massovala radiobiblioteka,
no.461) (Amateur motion pictures) (MIRA 16:6)
(Sounds-Recording and reproducing)

1. SAYODUROV, M. A.
2. USSR 6oo
4. Moscow - Sub*qs
7. In accordance with Stalin's general plan; a new line of the Moscow Subway,
Gor. khoz. Mosk, 23, No. 12, 1949.
9. Monthly Itist af Russian Accessions, Library of Congress, April -1953, Uncl.

SAMOMPOV, V.
Physics - Study End T*Pching
Remprks on the Physics rianwal for ti-achars' colle-ges, F.',z. v elhkole, @,so. L, 1952.
Vonthly Li6t )f Hus.,;Ian Accfai;rlnns. Library of Cor-ress Yif.)v-.-.bei- Ig-2 UNCLA'Cl-F.12D.
t@

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Mineramp of refti,*'y WW in th
00 CSWAUM. P."n! Ir '"'d
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art T@
.@lniikkdy Akad@ 04, itri
(1949).-ReftadmY sh-l- in layers 5 to 4o In. thick are
found in the Kabardilik-AsserbOidshan SS.R. Thrf
hAVC faint points of IM-1710". only otte tit. POW

it. by therin.11
Me fractions firm than 2 P were exam
Inatyvimi: the brating curv" %how first a cousider-able endo-
00 thermic- vallect at it tirvood at fA114410% but no

00 o i,xiithermal effect alutirr INW. These clay -hales which
.ire completely %malosous to the fAmous Chillwiv-Var
clayti, in their chem. compit. are, brvau.,e of the all,,ence

Tical "monothemitei.- The
of the exothermic tiffect, I)
'
-Ae
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nd NO
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etween
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IT
I Scioncc. Soil Genesis and Geography.
uss-@t / so 1 6027.
@jiol. , J@o 2,
kbs @our; Zhul -
Author :.Samodurov ences, Academy. Of
Inst :I.n,sjjtZ[@@'6rdy6jogical Sc i
Sciences Ukrainian SSR, e Looss-forming
Title :The Geochemical Nature Of th
Process- Morfol.
uk AN USSR. Ser. 800
Orig Pub: Tr. In-ta geol. na 1957, vyp 131-144.
elletVertichn. geOl-s
oess of the the steppe rogiOns Of the
Abstract: In the 1 @csh_jy formed tYPO
Ukraine and Moldavia the f] iron montaorillonitev
morphological minerals are oot hills Of the
quartz and calcite. In the f regions Of
eastorn Carpathians and the northcrn : oethite,
the Russian plain there arc beidollito, 9
and hydrogoothite mincrals. Approaching the
Card 1/2
Aus J'Otir- Rof Zhur-Biol-, No 2, 1959, 60pri.
Abstract: mountainous districts, the calcium carbonate con-
tont in loess diminishes and the amount of clay
fraction incroases, whilo the porosity and sag-
ging of looss rocks decreases. kftor the loss
of calcium carbonate by loess rocks, boidellito
is synthesized which. decroases sharply the con-
tent of montmorillonito. In the steppes of the
southern districts of the Ukraine and Moldavia,
calcium plays a significant rolo in the stuctur-
al formation of soil bottoms, while boidollite
plays an important role in tho structural forma-
tion of soil bottoms in the StODPo regions of
the Russian plain. -- F. I. Shchorbak.
Card 2/2
2

--TE, TO-)
Avg 48
Refractory Clays
Ceramics
"The ICIallmnitic' Maracter of.Tisfr&0tOry CIAYS Of
the Uobkmskiy Deposits in Nortbern .C-=-eia,,* P. a.
Samodurory I. Ds Sed.10taki7j. Roetor/Don state u inexi
T.'X. Molotorx 2 pp
"Dok Ak Ikuk SM" Vol LTI, So 5 -
Gives Wmtiiw WA debyAration curves, plus a chemical
composition table, of dark-gray, brownish clay,, amd
light_gMy 014 from these dspomits.
24

SAMOVUROVI P. S.
Samogurov, P. S. "Mineralogical composition and physico-chemical properties of
the five clays of the Shisskiy site in the Northern Caucasus," Uchen. zapikki
(Rost. n/D gos. un-t im. Molotova), Issue 1, 1949, p. 177-27 -- Bibliog 20 iems
SO: U-3566, 15 March, 53 (Letopis 'Zhurnal lnykh Statay, No. 14, 1949).

t@
P:
0
9
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2
Tf)

LIJ
CI&Y alitierals in Sediments of the North COWASUS
Titan. 11. S. Ss 0'. NI- M.'Wov Alair Vniv,
Rcmu Akad. VSkk S-Ii.S.R. ed,
the witte-opread TitcRiLgri It:ptwr-
Jurassic) wdisitents a( the Kulxtn-F4hkAktm rivur reg"i. 3
priticipcd types 4A cLy MiUMAIS Aft tAkWMd, CUIX-CiAlly
coned. in the fin"t fmCti(M%,,, (sindkt th.411 1 0:01 kl.i-
finitc-rirh frictsims; (2@ bdtt)y@ite tvgu*s; (3) mmultiltv-
mitir, fly 1,11' 11MV-114ifil ill 11133. APIA. ThC thVIIII41 C&CtS
list (liffervill4ij Iti-mling curivro, and the i1rhydralitill vurv"
11to ill it (vill Alprellivilt with dleoe Chem.
'LuAly-m-is with it ctunputution of It* (mmuLts art Sivris his
r,,pfv.Wnt.&ti%*v tvjw@ ,I tile cL&y titimprA14. 'rhe c,xuv
fr4clii,114'.1 tile @Jinlvnts &trr 1'riswil.kIly tietrit..1
of mot. rueb And schims, rho frj,-.
tious (tracts 2 fit .500 is) Contain quartz, titicroeline. orlb,i-
cLase. uligocUse. athitr.and mk-j. sulmirdioult chak-alottv,
Calcite. gyp'llm. TtW hMVY (FIACt"I% -111t.kill tile 11%11.11 f's
atut At %Hitutr%, at avvv@micv imitrinak evirmili, mi-I
disAtite. %V VitO

c_X
"a Ou 0 hoollillif I to
:v SlAte I'lliv.. It'hill, V .11
A7:1111. While 111V ittill III(III01110titille A11A.&VI, V1111t.11114
vurk-ty ".I. i1clor'.1.41
k.0, a Ifew K -fire, %
i.1 tile N11,4111.41 .11illit'litAtY SiCtIV- (11161,16- 0114-MV110.
I! U-11tilliAl- 114014111%, *fill rAlVilt, OAVN. 414-1 1114111
[ht inineral 6a.-Aso-al. -Aith the wtutilitit Act-r-1gy 111111CFA6
;-f fine-stAined w4fisitents uf this kind. 'rise ItAt-tit"is
wli)%v 11.1 p gave the tylvit-al
it it lotit is coubithertim I cfTcvt4 at I III atul MW The r%sj.
thelinie IwAt eftert At .1111 and 41111' hs,Watri @nur cas.
.ah-tiour. und thr slight forAl ubviarplims at 3011' the
I'msence of smue itcoothite. The chem. analysi,, curre.
@Ilonds to the foonstula
lie lf,0 cimitent tif 'MIC-nunwthcrinite is hilgher than that
'if tile rortlinary (K) variorty %of the inintral The is iv( I 1w
1,11s, iliprigair,i i- 1 57, 1.1%). the Wirlmigs-no-ir al."st
so I rj;.1. W. Wirl

Ulawaisgical
ScdktskiF and P. S. %Modumv (RA&tav. State
Zdp&ki (NI&M. SW. rUve
mk*W.) 79. 137-41(1950)@-Tlw detu. of stilimentary
rocits is based on an acewate identification, of the clay
minersh espKially by the differential thertnal analysig,
for whiricharecteristicesRatplesaw given, whk halln", Ite.
"' tr mrmtmatillanite, sind monothertnite. front
diff"ent horilono. schists. slates at t1w N. Caucauts anti
the Don Basin. Ar. chem. formulas we giw" (or the
clay sal 711e Mpremacy of this metbod over the
palwastoia" detu. is dwe to the frewancy of W.
zM whkk we entirtly bicking faWls. It Is an important
supplement also to the inethnits of the heavy min"Jx.
W. Filef

15-57-2-1639
Translation from: Referativn zhurnal, Geologiya 1957, Nr 2,
p 70 (USSR@y
AUTHOR: Samodurov, P. S.
TITLE: and Origin of the Red-Brown Scythian
Clays of the Southern Ukraine (K mineralogii i
genezisu krasno-burykh skifskikh glin yuga Ukrainy)
PERIODICAL: V sb: Kora vyvetrivaniya, Nr 2, Moscow, AN SSSR,
1956, pp 216-234
ABSTRACT: The author has studied the Scythian clays in a number
of regions in the Ukraine and in the Rostov Oblast'.
The clay samples were studied in thin section. Each
sample was separated into size fractions. The
fraction >0.002 mm was studied in immersion oils.
Finer particles were examined in specially oriented
mounts as well as by thermal, dehydration, X-ray,
Card 1/2 organic dye, and chemical techniques. Field and

15-57-5-6370
Translalion from: Referativnyy zhurnal, Geologiya, 1957, Nr 5,
p 98 (USSR)
AUTHOR: Samodurov,
TITLE: A Loess Type of Weathering Crust on Tortonian Siltstones
in the Fore-Carpathian Region (Lessovyy tip kory vyve-
trivaniya na. alevroiitakh tortona. Predkarpatlya)
PERIODICAL: Uch. zap. Belorus. in-t, 1956, Vol 28, pp 197-222.
ABSTRACT: The Tortonian rocks studied are composed of dense
pelitic-psammitic and pelitic siltstones vdth sub-
ordinate quantities of sands and sandstones. The
siltstones are covered by a loess weathering crust in
which five zones are, distinguished. These zones reflect
different stages of weathering. The thickness of the
fourth zone does not exceed 4 m, but the first zone
locally reaches 15'@ in ttickness. During formation of
the loess (in a weakly alkaline*environment), pyrite,
siderite., feldspars, mica, and hydromica. were replaced
Card 1/3 by montmorillonite, quartz, and calcite. Calcium from

15-57-5-6370
A Loess Type of Weathering Crust on Tortonian Siltstones
carbonates of organic, chemical, and clastic origin was dissolved by
rain water containing C02- It migrated to the lower part of the
loess profile, where it formed concretions up to 18 cm across.
Later, the remaining CaCO,3 went into the subsoil layer during
formation of the soil. During study of the section, the following
additional systematic features were noted (from the base upward):
a decrease in the relative quantity of the fraction 0.01 mm to
0.001 nmi at the expense of the coarser fractions and partly of the
fraction < 0.001 mm; a general decrease in the bulk weight and a
decrease in porosity a decrease in plant remains from 2.54 (in
unaltered siltstones@ to 0.09 percent (fifth zone); in the fourth
zone there occurs a local increase in calcite content, in value of
pH (from 7.5 to 8), and in porosity. The chemical compositions of
the fraction 0.001 mm. of unaltered siltstone and of the typical
loess are, respectively (in percent): SiO 49 31 and 51.10, A1203
22.20 and 17.12, Fe203 6.03 and 8.32, FeO Y.28'and none, MgO 2.20
and 2.59, CaO 1.32 and 0.21, K20 2.65 and 1.94, NA20 0.43 and a
trace, H20+ 5.10 and 7.53, H20- 8.03 and 11.04; total 99.96 and
Card 2/3

15-57-5-6370
A Loess Type of Weathering Crust on Tortonian Siltstones (Cont.)
100.38. The author gives mechanical and mineral analyses, thermal
curves., and photomicrographs of the rocks.
Card 3/3 V. A. V.

SAVODUROVO P.S.; PYLILO, V.K.
.1
Mineralogy of Rissian-and Armian moraine loams in White Bussia.
Uch. zap. IAk. un. no.1:136-i66 '57. 1(MIRA 110)
(White Phasia-May)

DOILOV., A.N., kand. tek-hn. nauk; SAMODUROVt S.I., inzh.
Wider use of local materials in the,construction of lccal
roads. Avt. dor. 28 no.ltl6-17 Ja t65. (MIRA 180)

SAMODUROV. T., kand.tekhn.nauk
Joints of exterior keramzit-conerete wall panels. Zhil. stroi.
no.12:10-11 160.T (MIRA 13:U)
(Concrete'910s)

SAMODURGV,V.I.
Stratigraphy of Mena4oic deposits of the lower reaches of the
Syr Darya. Biul.NOIP. Otd.geol-30 no.3:39-56 MY-Je'55.
(KLRK 8:10)
(Syr Darya Valley--Geology, Stratigraphic)

L@)qAvpu pto V
SUBJECT: USSR/Geology 5-2-6/35
AUTHORS: Garetskiy, R.G;, Samodurov, V.I. and Yanshin, A.L.
TITLE: Pseudotectonic Di alo cations of the Karak Mound in the Northern
Kyzylkums and Some Other Points near the Aral Sea (Psavdotek-
tonicheskiye dialokataii bugra Karak v severny'kh Kyzylkumakh i
nekotorykh drugikh punktov Priarallya)
PERIODICAL: Byulleten' Moskovskogo Obahchestva. Impytateley Prirody, Otdel
Geologicheskiy, 1957, # 2, Pp 77-103 (USSR)
ABSTRACT: The Karak mound is located 120 km SSW of the railroad station
Dzhusaly in the northern part of the Kyzylkum desert. It in
about 2 km long and 0.5 km wide. Its height is 40 to 50 m above
the surrounding plain, and its maximum height reaches 147 m in
the NE part.
In the Karak mound is neither a dome-atructure nor a graben, as
was supposed by the earlier investigators. Dislocations observ-
ed in the stratification of the layers belong to-exodialocations
or pseudotectonic dislocations. They die out in the plastic
clays of the Upper Eocene and do not extent deeper than 175 m
Oax,j, :@/2 from the mound's top.

rN-2-6/35
TITLE: Paeudotectonic Dislocations of the Karak Mound in the Northern
Kyzylkume and Some Other Points near the Aral Sea (Psevdotek-
tonicheskiye dislokataii bugra Karak v severnykh Kyzylkumakh i
nekotorykh drugikh punktov Priarallya)
The stratigraphic cross section of the Karak mound is described
in detail. RockB composing it are of the Upper-Pliocene, Middle-
Upper Oligocene, marine Paleogene and marine Upper-Carboniferous
origin.
Analyzing the geological and prospecting data available, the
authors have drawn some conclutions as to the morphology and
mechanism of the formations of dislocations in the Karak mound.
The most probable cause of these dislocations was a landslide
which occurred during the Middle-Pliocene period.
This conclusion is confirmed by the comparative study of some
other pseudotectonic dislocations near the Aral Sea whose origin
was established aa being definitely of the landslide nature.
The article contains 2 geologic maps, 2 geologic cross sections,
1 photo and 1 table. The bibliography lists 17 Slavic references.
ASSOCIATION: Not indicated.
PRESENTED BY:
SUBMITTED: No date indicated
AVAILA@LE: At the Library of Congress.
Card 2/2

Tectonics of the North-Eastern Aral Regions 5-4-4/15
two such plates can be singled out: the Western Siberian and
the Turanskaya plates. In these plates there are lower re-
gions, areas of active sinking, and the regions of relative
height which separate the first ones. The lower regiQns are
called sineclises and the higher ones - anteclises. The re-
gion under investigation is located at the junction of various
large structures of the Turanskaya plate. Its central part
occupies an uplift, called Nizhne-Syrdarlinskoye (Lower Syr-
Darlya), which is peculiar in its morphology and development.
The author classifi6s all sediments which occur in the north-
eastern area adjacent to the Lral Sea into 3 structural
groups: The first structural group consists of the rocks
of Paleozoic and Lower Triassic ages which form the folded
foundation. The second group includes sediments of the
Rhaetian and Lower Jurassic stages, and the upper 3rd group
is made of the sediments from the Middle Jurassic to the
Quaternary systems. Paleozoic sediments outcrop only in the
north-eastern corner of this area. They are represented by
various series of the Cambrian, Ordovician and Devonian
systems. The author describes in detail existing notions on
the tectonics of the region under consideration. In order to
Card 2/4 clear up the present structure of the region, geologic and

Tectonics of the North-Eastern Aral Regions 5-4-4/15
structural maps of the area were compiled. The structural
map consisted of structure contour lines of the roof of
Cretaceous sediments, by using of the data obtained from about
300 wells drilled by various organizations. The structure of
the folded foundation was analyzed on the basis of the aero-
magnetic and gravimetric survey data, seismic profiles, and
cross-sections of deep wells. The conclusions drawn by the
author are represented by the scheme of the foundation
structure shown by Figure 2. The author singles out 5' zones
with different foundation character and describes them. Judg-
ing by the data of an aeromagnetic survey, magnetic anomalies
with meridional strikes should exist in thetwestern part of
the region. It is presumed that the zones of magnetic ano-
malies correspond to buried Hercynian structures of the Urals
folded system (Figure 2).* The Nizhne-Syrdarlinskoye uplift
separates large synclinal depressions of the plateau cover
and is located in the central part of the area under invest-
igation. This uplift began forming in the beginning of the
Paleogene period and the process of its relative lifting con-
tinued also in the Quaternary age. The modern structure of the
Nizhne-Syrdarlinskoye uplift is due to tectonic movements
Card 3/4 which took place before the origination of Middle Miocene

Tectonics of the North-Eastern Aral Regions 5-4-4/15
sediments.
The article contains 3 maps, 2 profiles and 37 Slavic refer-
ences.
AVAILABLE: Library of Congress
Card 4/4

AUTHOR& Bondareva, T.P. and Samodurov, V.I. 5-6-6/42
TITLEs New Strata of the Pliocene Deposits in the Eastern Part of
the Turgay Depression (0 novoy svite otlozheniy pliotsena
v vostochnoy chasti. Turgayskogo progiba)
PERIODICALt By-ulleten, Moskovskogo Obshchestva Ispytateley Prirody, Otdel
Geologicheskiy, 1957, # 6, PP 93-100 (USSR)
ABSTRACTs The author describes new strata of alluvial deposits, un-
known thus far, which occur in the low watershed between the
rivers of Kara-Turgay and Ulu-Zhilanchik in the eastern part
of the Turgay depression.
As these strata are more ancient than the valleys which,
according to V.A. Lindgollm and A.P. Sigov, existed already
in the Middle-Pliocene epoch, their age can thus-be determined
as Lower-Pliocene.
It is proposed to name these sl:rata the Katpagan suite
after Lake Katpagan located between the two above mentioned
rivers.
The author gives a detailed petrographic description of
the rocks and mineralogical composition of the sands building
the Katpagan suite.
Card 1/2 He concludes that the study of the composition and thickness

5-6-6/42
New Strata of the Pliocene Deposits in the Eastern Part of the Turgay
Depression.
of this suite are of a great practical importancey because
its sandy rocks are associated with occurrence of fresh
water.
The article contains 1 map, 2 tables, and 8 Russian refer-
ences,
kVLILLBLEt Library of Congress
Card 212

AUTHORs@ None Given 5-6-9/42
.ITLEs Chronicle of the Activity of the Geologic Section (Khronika
deyatellnosti geologicheskoy sektsii)
PERIODICALs By-ulletent Moskovskogo Obshche8tva Ispytat,eley Prirody, Otdol
Geologicheskiy, 1957, # 6, -- 115-118 (USSR)
ABSTRACTs The following reports were delivered in the Geologic Section
from 1 March to 4 June 1957:
L.I. Krasnyy on the "Mongolian-OkhOtsk Geosynalinal Region
and Its Place in the Structure of Eastern Asia"; A.A. Bogdanov,
M.V. Muratov and V. Ye. Khain on "Some.Problems in Geology of
Cz'schoslovakia According to Impressions fiom a Geological Ex-
cursion"; V.I. SamoduroX on "Tectonics of the North-Eastern
Region Near the Aral Sea"; V.S. Zhuravlev on"Tectonic Nature
of Regional Gravitational Peaks of the Caspian Sineclise";
N.F. Balukhovskiy on the "Nature (Theory) of Geologic Cycli-
city"; A.V. Soloviyev on "Genetic Types of Petroleum and Ori-
gination of Oil Deposits of North-Eastern Sakhalin"; G.I.
Makarychev on "Stratigraphy of Proterozoic and Lower-Palsozoic
Deposits of the Bol'shoy Karatau"; I.S. Chumakov on "New Data
on the Geologic Structure of the Leninogorsk Depression in the
Card 1/2 Rudnyy Altai"; G.P. Leonov on "Principal Problems in the Stra-

Chronicle of the Activity of the Geologic Section 5-6-9/42
tigraphy of the Palsogene of the Russian Plateau"; S.V. Semi-
khatova on "Some Problems in the Stratigraphy of the Lower
Part of the Lower-Carboniferous System"; S. Ye. Kolotukhina on
"Facies of the Lower-Carboniferous System in the Karataull;
V. Ye. Khain, S.L. Afanaslyev, Yu. K. Burlin, Ye. A. Gofman,
M.G. Lomize and V.G. Rikhter on "New Data on the Geology of
the North-Western Caucasus", and B.P. Zhizhchenko on a "Draft
of the Unified Stratigraphic Scheme of Paleogene and Neogene
Deposits".
AVAILABLE: Library of Congress
Card 2/2

SX.-ODUROV, V.I., Camd Ceol-ldn Sci-(diss) IlStrntigraphy and tectonics
I
al lye I it I,
of the north-castern Priar .1os,191:3. 22 pp
(Aend Sci USSR. 6eol Inst), 170 coPie2 OM130-581124)
3k11-

AUTHORS: Garetskiy, R. G., Samodurov, V. I., 2o-119-6-40/56
Yanshin, A. L. I
TITLEs The Marine Albian Deposits on the Western Shore of the
Aral Sea
(Morskiye allbskiye otlozheniya na zapadnom beregu
Aral 0skogo morya)
PERIODICALs Doklady Akademii jisuk SSSR, 1958, Vol- 119, Nr 6,
PP- 1195-1198 (USSR)
ABSTRACTt As is known, the shores of this sea nearly throughout
consist of Tertiary rocks. Only on places where the
sections of anticlinal stru,cture are interseuted by
the coastal steep slopes, in their lower part rocks of
the Cretaceous system occur- 3 of such places exists
on the northern shore of the Kulandy peninsula, on the
southern shore of the Tokmak-1ta peninsula and on the
eastern shore in the district of Cape Ak-Tum uk (wWhite
Nose") . The most ancient sediments in 11ulandy are to
be classified with the Middle 1lbian (Ref. 13). In
Card 1/3 Tokmak-Ata Senomanian exposures are known (Refs. 1, 2).

The Marine Albian Deposits on the Western Shore 2o-119-6-40/56
of the Aral Sea
On Cape Ak-Tumsuk Mesozoic layers were classified with
Upper Jurassic by an erraneous determination (Ref. 14).
A discussion on this subject is summarizeds Nobody
supposed the occurrence of more ancient rocks than Se-
nomanian on Cape Ak-Tumsuk9 even, in this place the
occurrence of Senomanian and Turonian was doubted
(Refs- 7, 9, 10, 13). The authors succeeded in clearing
the cause of such a differing criticism of the occurring
Cretaceous sediments; i. e. individual researchers saw
and investigated different places. The more ancient lay-
ers, however, northwards gradually emerge out of the
sea. The authors propose the name "Kassarminskaya Anti-
klinal" (according to the Kassarma well) for the anti-
clinal structure of Cape Ak-Tumsuk. It is not connected
with the Chushkakul'skaya anticlinal but separated from
it by a North-Ust'-Urt depression running in direction
of the width. The approximate sequence of the parcels
of Albian layers south of the Kassarma well (from top
to bottom). is mentioned. The exposed Albian sediments
Card 2/3 have a minimum thickness of.30 m. The discoverT of these

The Marine Albian Deposits on the Western Shore 2o-1 19-6-40156
of the Aral Sea
marine layers together with other analogous finds of re-
cent times on the western shore of the Aral Sea can change
the hitherto existing conceptions in the way that the Al-
bian sediments notanlyawof continental character (contrary
to Refs. 4, 13)- Consequently, the transgressions at cer-
tain moments widely advanced eastwards. This happened along
that westreastern downwarping, which, since the Upper Pa-
leozoic separates the fold system of the Ural from the
Herzynian formation from folds of the Srednyaya Aziya.
There are 1 figure and 14 references, 13 of which are
Soviet.
ASSOCIATIONt Geologicheskiy institut Lkademii nauk SSSR
(Geological Institute AS USSR)
PRESENTED: November 13, 1957, by N. S. Shatskiy, Member, Academy
of Sciences, USSR
SUBMITTEDi November 11, 1958 (misprint)
Card 3/3

GARETSKIY, R.G.; SAMODUROVI V.I..- YARSHIM, A.L., akademik.
Stratigraphy of upper Cretaceous deposits of the Kassarms,
anticline onthemestern shores of the Aral Sea. Dokl. AN SSSR
124 no.5:1109-1112 F '59. (MIRA 12:3)
l.Geologichaskiy institut AN SSSR.
(Kassarma region-Geology, Stratigraphic)

ZHURAVLEV, V.S.;..@@AMDDUROV, V.I*
Evidence of secondary, saline tectonics on the open domes of the
eastern part of the Caspian syneclise. Dokl.AN SSSR 132 no.4:
891-894 Je '60. (MIU 13:5)
1. Geologicheskiv institut Akademii nauk SSSR. Predstavleno
akademikom A.L.Yanshinym.
(Caspian Sea regiou--Salt domes)

MNDAMA, T.P.1 SAMODUROV, V.I.
Recent data on the stratigraphy of Paleogene deposits in the northern
part of the Aral Sea region. Dokl. AN SSSH 140 ro.3:635-637 5 161.
(MIRAL 14:9)
1. Geologicheskiy institut AN SSSR. Predstavleno akademikom A.L.
Yanshinym. (Aral'sk region--Geology, Stratigraphic)

BONDAREVA, r.p.; NEMOV, G.I.; SAMODUROVx V.I.
Ape of the Tas-Aran series in the northern part of the Aral Sea
region. DokI. All SSSR 140 no.4:892-894 0 161. (MIRA 14:9)
2. Geologicheskiy institut AN SSSR i Yjoskovskiy geologorazvedochnyy
institut im. S.Ordzhonikidze. Predstavleno akademikom A.L.
Yanshinym.
(Aral'sk region--Geology, Stratigraphic)

GARETSKIX, R.G.; KNIPPER, A.@.; SAMODUROV, V.I.
History of the development and spatial relationship of Faleozoie .
structures in the Kara-Tau and nu-Tau. Biul.140IP Otd-geol- 37
no.1:43-56 Ja-F 162. (MM 15:2)
(Kara-Tau--Geology., Stru#twal) (Uln-Tau-Geology, Structural)

BOLKHOVITINA, N.A.; KOTOVA, I.Z.; SAMODUROV9 V.I.; YAN TSZI-DUkN' (Yang Chi-
tuan] -
Stratigraphy of continental Cretaceous sediments of the lower
Syr Darya uplift (northeastern Aral Sea region). Dokl-. AN SSSR
152 no.2:392-395 S 163. (MIRA 16:11)
1. Geologicheskiy institut AN SSSR. Predstavleno akademikom
A.L. Yanshinym.

GARETSKIY, R.G.; SAMODUROV, V.I.; SHLEZINGF-R, A.Ye.; YANSHIN, A.L.
Tectonics of the platform mantle of the Turan Plateau. Trudy GIN no.92:
202-257 163. (MI RA 17 - 10)

r W Qc e 0 COMP X mercull
- --the doubleoalt 2JCCLHgChJfP.-:
halldim. Z. V. Zvonkova, V. V, zlamodurovt@ and Waim Is
And Cunk m
L. 0. Verontsova. Doklady 2=77MM 3.73.1t 1021 PhIc, with mov4unk, orthorhombic,
1115-18(1956).-In ClHgCNS the dissunce Hg-CJ Is giveq i tkm3, The cubic form has as - 5AI.* 0,01 A. with Might.-,
in the literature as 2.29 A., corresponding to a linear sp Indications for a tripling Of the penod, In the lolmr-sym-l
binding; in KitfgCi,.HO the distance Hg-CI Is gi7en as mewernadificatfims. The P(AA) and F(Ak) intensity an-7
2.42 A., and in the perovskite-Ure structure of Cilfg0l It alysis shows the-general fe;itnres of a p4trovsIdte structure,
with Cs+ In the of the curie, Hg in the center..
given as 2.72 A. The problem of the- ionic or mol. bonding
c C I pc, ft'l.. could he dMved only fro. th.:.-,
ty in thest complex salts. made a redetn. of the structure (WAIA). Th
WIC Improved accuracy necessary. 3C2HgCl,.H#O, has the method of differzz;tial series, with rounded max- for-Cl in the
electron d. projections In-t/tI& Lt. 2 atoins CIt
arthorhombic space group Dlc-Pbam, with Z = 4 mols,-, Lwmttd in Hgo-
at - 8.22, bo = 11.51, c4 - 8.90 A., all with :1:0.61 A. ae- Cis mals., and one In CJji In the salt C!s+Cl-, fit statistic:.'
kuracy. The x-ray d. is 3.38 g./ce. At. co6rdluates an, 4 distributions of the shares 2 X CIT/3 %Ed one Cl;/3. Ile
Iffin 4(e): 00s; 4 X11 and 4 Cli in 4(g): xyJ; 4 nand ccOrdinates for Clt are: 0.078, '/*; wid for Chi, 0, 'A;
4 R.in 4(h): xyl/s; 8 Clar in 8(1): zyz. Parameters r"If C, 0.922, 1/l, and 1/t, 0.078; for CJ& 1/1, 0; for CI1,_:'
were for Hg, 0, 0, OMO; for CIT, 0.768, 0.073, 0, for vl,012. Thed@stancesare: 2Hg--CJt - 9.29; 4Hg-CJn
1& 0.768, 0.046, O.bW; for Cl@u, 0.115, 0.181, 0.244; 2.70; 4 W--Cla - 3.82. and 8 Cs+@Cly - 3.84 A. The
sC
for kt, 0@31?9, 0.161, 0, for K,',, 0.399, 0.201, 0.5m. formula is therefure not CsHVC4,but C J.HgCls, with
interat. distances were: Mg-Clizr - 2.20 A.; 214g-Cl@ - covalent Hg-Cl bonds, and linear mois@ HgCIj, in complete -
2.92 A.,, 211g-OR - 3.13 A.*. 3Kt*-CtF - 3.05 to 3.25 -agreement with the caicn. of the intersity from the mal.
to 3.52 A.; K,*-Otit - 3.21 A., MOM (R - 0.13), not with th to h! FerovsHte model (R::
aKt-aff - 173*. From 0.20). Also Cs I (Au
Ka-Clit, - 3.27. A.; angle ClItt-lig-P-Int Ch)-(AuCI4)-(cI_RI1Iott-dP&uI
spectrometric measurements the Hg-CI covalent bond dis- Ing. C.A. 32, 7MR) has a cubic and a ktragonal modifica-
tance in ClHgCffs is 2.282 :1- 0.005A. (cf. Cordyand Shed- tion, the Ist structure with a statistical distribution in the
dan,' CA. 48, 4979f). The real formula is therefore that of cubes; -the tatter Is of the covalent typesimllzr to CsCI.HgCI2.'
ru

SAMODUROVA. Z.B. (Dnepropetrovsk)
I.. @__ -
Yrom experience of teaching algebra in the 6th and 7th grades.
Kat.v shkole no.2:40-4 Mr-Ap '57. WaA 10:5)
(Algebra--Study and teaching)

SOV/97-58-11-3/11
AUTHORS: Baytsur, A.I., Avotin, A.I., Bakal, M.Sh. and
Samofal S.F., Engineers
TITLE: Precast Reinforced Concrete Constructions Used for
Underground Sections of Industrial Buildings (Sbornyye
zhelezobetonnyye konstruktsii v podzemnykh kommil-n-1kats-
iyakh promyshlennykh sooruzheniy) '
PERIODICAL: Betan i Zhelezobeton, 1958, Nr 11, pp 414-41? (USSR)
ABSTRACT: At present precast reinforced concrete segments forming wells
are used for the underground parts of industrial buildings.
At the same time the construction serves as shuttering. The
excavating work and the sinking of the well is fully mechanised.
This type of construction is used in the underground parts of
the Stalinskiy metallurgicheskiy zavod (Stalin Metallurgical
Works) and Almaznyan kiy ferrosplavnyy zavod (Almaznyanwdy
Ferro-alloy Factoiy)and designed by the Giprostall Institute,
Khar1kov. Figure 1 shows cross-section and plan of the
underground part of the Stalin Metallurgical Factory. It has
A oylin *drical structure, 28 m deep and 25 m in diamter.
The segmental
Cardl/3

Reinforced Concrete Const
Sections of Industrial Buildings. ructions Used for Underground
slabs have thin reinforced concrete walls with flanges
on all sides and one rib in the centre. The circular
floor slabs serve as additional strutting for the well.
They are supported an columns so that no weight from the
^-'loors is transmitted onto the outer wall. The precast
reinforced concrete segments (Fig.3) have the following
dimensions: 3.13 x 0*99 x 0.65 m; weigh up to 3 t, and are
made of concrete mark 300 with welded mesh reinforcement.
The segments are calculated to withstand a maximilm loading
of 40 tons/M2. The wall of the segmental slab has a
thickness of 15 cm. The ribs are 15 x 65 mm ih cross
section. The slab of the segment is provided with 2
openings of 63.5 mm in diameter which are used for placing
the grout between the wall and the excavation. . The segments
are bolted together with bolts for which 41 mm diameter
openings are provided in the ribs. Waterproofing is
obtained by addition of 2% to 3% sodium aluminate to
this concrete back-filling. The latter has a thickness of
'Card 2/3 15 to 20 cm. Fig.4 illustrates the process of construction.

-Precast Reinforced Concrete Constructions Used for Underground
Sections of Industrial Buildings.
The ground is first excavated and an in _s itu reinforced
concrete wall is constructed. The segments are then
fixed to the underside of this retaining wall forming a
ring. Further segments are added as soon as the excavation
makes this possible. The construction of a skiphole for
the AbumyurJdy Ferro-Alloy factory is shown in Fig. 5.
Details of this underground structure are also given.
Advantages'of this construction consist in the possibility
of being able to use precast units, to mechanise all
labour, saving time, reduction in the volume of excavations
and a considerable saving.in reinforcement. There are
5 figures.
Card 3/3

VIASOV, H.I.; ZILIBARMAN, A.A.; POVER19M I.D.- SAMOYAL, S. , redaktor;
!=, = r &
VISMWSKIY, I.F., redaktor izdat@1,stva;'A-M3W, --;., tekhni-
cheskiy redaktor
[Rapid capital repairing of blast furnaaes] Skorostnoi kapitalInyi
remont domennoi pechi. KharIkov, Goa. nailchno-tekhn. izd-vo lit-ry
po chernoi i tavetnot metallurgii, 1952. 99 p. (Km 9:8)
(Blast furnaces)

BATTSUR, A.I., insh.; KULOINS, Yu.I., insh.; SLK07AL S To.
I .. P--
Water tower with precast reinforced concrete bearing slemnts,
Blulo' stroi, tekh' 15 no 4:18-21 Ap 1,18. 1(NIU lls5)
- 0 @ 0.
1. GlProstall.
(Wtor towers) (PrIocast concrete construction)

RAYTSUR, A.I., inzh.; UMM, S.V., inzh.
Using reinforced concrete in making foundations for plant equipment.
Stroit. prom. 36 no 6:22-26 Jo 158. (MIRA 11:6)
(]foundations) (St;el industry-Iquipment and supplies)

SAMarAL, T.S.
m
Using the biological test for rating the degree of atjospheric pmrity.
Gig. i san. 21 no.11:93t-94 N 156. (MLRA 10:2)
(AIR--ANALTSIS)

SLMOM, T.S.. assistent (StanislaY3
Iffect of manganese on the development of experimental goiter
induced by 6-methylthiouracil. Arobl.sidok.1 gorm. 5 no.6:
7-10 X-D 159. OCM 130)
1. Iz kafedry biokhlmii (zav. - doteent G.A. Babenko) Stanie-
lavs@kogo meditainskogo instituta.
(CHIOURACM rel.apdo.)
(GOITIM experj
(MANGARISM pharmacol.).

SAMOYAL T.S.
Influence of maganese on the thyroid gland of rate in iodine
Insufficiency. Vrach.delo no-3.*313 Ar 160. (Km 13:6)
1. Irafedra biokhisli (say. - dotment G.A. BabenkD) Stanislav-
skogo meditainskogo Instituta.
(M&NUMM-PHYSIOUGICAL WTWT) (TMOID "JM)
(IODINE IN THS BODY)

SAMOFAL) T.S.
Role of copper in the etiology of experimental goiter. Probl.
endok. i gorm. 7 no.1:42-46 161. (MM 14:3)
(GOITER) (COPPER METABOLISM)

SAMOFAL, T.S.
Iodine, copper and manganese content of the blood.. liver-and kidneys
in experimental hypothyroidism. Vop. med. khim. 7 no.W63-166
Mr-Ap 161, @Mff?A 14:6)
lo-Chair of Biochemistry, Stanislav Medical Institute.
(WPTHYROIDISM)' (IODINE METABOLISM)
(MINERAL RETABOLISM)

SAMOFAL, T.S.
Effect of lowered dietary manganese on the growth-and development
of rat offspring. Vop.pit. 20 no.2:44-47 Mr-Ap, 161. (MIRA 14:6)
1. Iz kafedry biokhimii (zav. - dotsent G.A.Babenko) Stanislavskogo
meditainskogo instituta,
(MANGANESF-PHYSIOLOGICAL EMCT) (GROWTH)

SAMOFAL, T.S.
Relation of the copper and manganese content in beans to their
color. Vop. pit. 22 no.6:70-74 N-D 163. -(MIRA 17:7)
1. Iz kafedry biokhimii (zav. - dotsent G.A. Babenko) Ivano-
Frankovskogo meditsinskogo instituta.

an! In7e,@tl.-tlon of a Tramiducer awl Tr-Insmitter
for Taiemet-@ring tre libtt-r Out put in Irri@cllttl)n Systems." Cand
Te,3h Sci, Ch-lfr o;@' Aut-lmaticq anrl Telempcn-tnics, Kii@v Order of Lomenin
Inst, Min HL-her E-luc-t@ )n USSR, 4
Polytechn, K,.v lq@)' . (KL' No 11,
1,*-, r
SO: Sum. No. 670, 29 Sep 55-SurveY of Scientific anri Technical Dis-
sertntinns De@ended -at USSR Higher Uducational Institutions (15)

K.G.
@Inatrunents for checking and telemetering water deliver7 in open
canals. Izv. KPI 2Z:119-135 157. (MIR& ll:Y)
(Blectronic measuremouts) (Irrigation canals and flume)

SAMOnLOV,
Palse frequency transmission equipment used in elemetering water
delivery in irrigation systems. Izv. KPI 22:136-145 157.(miRk n.-j)
(Telemetering) (Irrigation)

5A-MQFILav.-jio r, gor!"Ac-h, kand.takhn. sauk, crdtiL; -ZALESOV,O.A.,
kFmd.tekhn.xauk.retoexzezt; SAVCHEM,r. Ya,', inzh., red. Izd-va; SHAFETA,
S. M. , tekhn. red.
(Calculating machinee]Vychislitellnye ustrolstva. Klmn,Goatekh-
izdat USSR, 1963. 262 p. (KIRA 16:3)
(Electronic computers)

L 38714-M &ff (d)/DIP(l) LJP(c) BB/GG
ACC NRt - 014200 SOURCE CODE: DR1627IM-700070117BO20029
AUTHOR: Samofalov, K. 0.1 Skorobogattko, N. V.1 Tikhonov, V. A. 9k
L;
TITLE: Analog-to-digital converter 1Vj
SOURCE: Ref. zh. Avtomatika, telemekhanika i vychislitelinaya tekhnika, Abs. 11B235
REF SOURCE: Vestn. Kiyevsk. politekhn. in-t4. Ser. aytomatiki, elektropriborostr.
I radioelektron., no. 1, 1964, 123-136
TOPIC TAGS: analog digital converter, voltage digital converter
ABS12ACT: A voltage-to-digital converter is described which consists of these unitas
a voltage commutator, a summation amplifier, three level-quantizers, twelve
rectifiers, three 4-digit registers, two code-to-voltage converters, a voltage-sip
shaper, and a main-and-offset-pulse generator. The overal.1 static error of the
converter is 0.3A. Circuit diagrams of the principal units designed with electron
tubes and semiconductor devices are explained. The code-to-voltage converter,uses
a method of current summation in a matrix that comprises two resistor types. Six
figures. Bibliography of 3 titles. N. P. [Translation of abstract]
SUB CODE., 09
Card 1/1 UDC: 6BI-142.621

ACC'NR. AP7007533 SOURCE CODE: UR/0432/66/000/003/002o'/0027
AUTHOR: @@Ofalovjl K. G. (Candidate of technical sciences); Plakhotnyy, N. V.;
Lavrinenko, V.V-`@
ORG: none
TITLE: Piezoceranric memory element with three stable states
SOURCE: 1.1ekhanizatsiya i avtomatizatsiya upravleniya, no- 3, 1966, 26-27
TOPIC TAGS: piezoelectric ceramic, computer memory
SUB CODE: 09
ABSTRACT: The Xic7 Polytechnical Instituto i@- performing investigations on
olomonts -,,nd structuros based on piezoacramica. One such oloment in a
3_stablo-zta-".-o coranic memory element mado in the form of a rootanguinr plato
-Ath z P1rzc--j1ac'%,r4_c film. Two signals (ono AC and one DC control) are
appliod to th3 Clomont, so.that the 3 ct-cblo vtato3 consist of 2 with an
altornatin3 iiignai at the output of @ho oloment, the two being difforontiatad
by a phaso diff,-_:,onco of 180 dogrees, plus one with no signal at the output.
1Tosting of of this dovico aho-a that it his high charanotoristic atability
a,r,3r a -..i%d@- rango and high Tho authors foulid that 'it
is posoiblu tv- u,:,!!d _- no-mory =trix on -Uho b-:--An of thoso elemonte.
inwatiga-@"ono into r=r@ufaetaring,technology arA docign aro continuinz,
@Crig. art. has: 2 f1gures. EJPRS: 37,7571
Card UDC:- 681-14,2.656

SAMOFALOV,. N.,I.p inzh.-mekhanik; KULENZINA) I.T., red.
(Highly efficient use of machinery on state farms in
virgin lands] Vysokoproizvoditellnoe ispoltzovanie
tekhniki v tselinrjykh sovkhozakh. Moskva, Kolosp 1964.
127 p. (MIRA 18t2)

VLASHCHENKOJ, L.F.; NOVIKOV, V.M.; ZINOVIYEVA, M.M.; SIDOROVA, A.Ps;
KARDASHOVA, A.A.; KLEYMENOV, I.Ya.; KRASIIOPOLISKIY, N.M.
[deceased]; UJKASH, Te.G.; @@@OV, P Ye YASHINA,
0
Ye.I.; KULIKOV, P.I., dots., retsenze-IntIMKAROVA, T.I.,
I
kand. tekhn. nauk, retsenzent; MMEVBURG, A.N., spets. red.;
KOSSOVA, 0.14., red.; SOKOLOVA, I.A., tekhn.red.
[Handbook for the technologist of the fishing industry]
Spravochnik tekhnologa rybnoi promyshlennosti. Moskva, Fi-
shchepromizdat. Vol.l. 1963. 589 (MM 17:3)
1

SM40FALOV2 V. zasluzhenyy shakhter USSR
Toward new achievements. Sovshakht. 10 no.11:29 N 161.
(MIM 34:1.1)
1. Nachallnik shakhty No.1 "ISentrallng7e- tresta Krasnoameyskugolt.
.(Coa3. miners)

GCFMN, I.Ne, inzh.; SAMOFALOV, V.G., inzh.
System for protecting filter bases in desalting systems from
corrosion. Energetik 11 no.7:24-15 JI 163, (MIRA 16t8)
(Food-water purification)
. jj

SAYIOFALOV, V.Ye.
"TSentrallnaiall Mine No.1 celebrates its fiftietb anniversary.
Ugoll Ukr. 5 no.11:12-13 N 161. (MIRA 14:11)
1. Nachallnik shakhty No.1 "TSentrallnayall, Trest Krasnoarmeyskugoll.
(Donets Basin--Coal mines and mining)

SAMOFALOV.,-Y--,-T@@-
Miners of Krasnoarmeyskugoll Trust welcome the Miner's Day
with suitable achievements. Ugol' 37 no.8:1&19 Ag 162.
1 (KRA 15:9)
1. Upravlyayushchiy Krasnoarmyskim trestom ugollnykh
predpriyatiy Donbassa.
(Donets Basin-Coal mines and mining-Labor productivity)

lll@ lllt@altlon With 2 m-16 .4
,..z ric:@ 3 , J - - !, ;.

Cirelilar of the Astronomical Observatory (Cont. ) SOV/4758
function In a given Interval of argument change. Extensive tabular data are
ptvvided on photospheric and chromospheric activity for 1957. There are no
references.
TAME OF CONTENTS:
S%mofalova, T. A,., and K. V. Plenskaya. Photospheric and Chromospheric Solar
Activity From January 1 Through December 31., 1957, According to Observations
of the Rhar1kov Astrwomical Observatory 3
The authors present 5 tables of data. Table 1 contains data characteriz-
ing the general state of the photosphere; Table 2 shbws data characteriz-
Ing the active regions of the sun; Table 3 9Lves a list of intensive floe-
cull, not identical with observed sunspot graips (possibly associated
with sunspot groups on the concealed side of the sun)j Table 4 provides a
1fat of filaments and protuberances; and Table 5 gives a list of pro-
tuberances whose height exceeds 60 ". Universal time is used on all
tables. The photosphere was observed visually with a 4-inch retractor
and attached screen. The image of the sun on the screen was i5l M-
Areas of sunspots are measured in millionth parts of a hemisphere and cor-
rected for perspective distortion. Chromsphere observations vere made
photographically on a spectraheliograph. Observations were performed
card 2/3

CJ-rcular of die Aatronoml,@al Observatory (Cont. SOV/4758
by L. 1. Krisenko and V. A. Yezerskaya, R. M. Chirkova, and T. A. Samofalova.
No references are given.
Bazhenov, G. M. Correcting Orbital Elements of Minor Planet (52) Europa 72
Baz,benov, G. M. Correcting the Orbital Elements of Minor Planet (152)Atala 74
Ba-zhenov, G. M. Computational Plan to Find the Polynomial Which Asthe Best
Cbebyshev Approximation for a Given Ametion in a Given Interval of
Arg,i-ment Change 76
AVAILAHER: Library of Congress
A-dwm-fal
Card 3/3 1-27-61 *

SAMOFAIOTA, T.A. ; RINSIATA, I.V.
Aictivity of the iolar p'hotosphere and chromoirphere from January
1 to December 31, 1957t according to observations at the lhaikov
Astronomical 6beervatory..!PSir.Astron.obser.Mmr.un. no 22:3-71
16Q.- (Swi-@serwat ions) (min 13:7i

AUTHOR: Samogayev, V.S., Engineer 118-58-6-19/21
TITLE: "_@The @Manu@facture 'of Railroad Ties from Wood Waste in the GDR
(Izgotovieniye shpal iz drevesnykh otkhodov v GDR)
PERIODICAL: Mekhanizatsiya trudoydmkikh i tyazhglykh rabot, 1958, Nr 6,
PP 44-45 (USSR)
ABSTRACT: Abroad, railroad ties are manufactured from waste.supplied by
snw mills and the woodworking industry and by low-grade timber.
Composition ties are superior to those made of solid wood.
Since 1956, a tie plant in Klesterfelld produces 280,000 such
ties per year (approximately 1,000 ties a day). A detailed
description of the production method is given.
There are 2 diagrams.
1. Railroad ties--Sandwich construction

Ya., and Raqdcav, A.
ir-T --I-
i A
-n ne -oa@ o Vi4n@,
M.Uon @f @hr Z@n,

9ANOCONYAN, A. YA. Cand. Physicomath. Soi.
Dissertation:' w5olution of Problems on Vibrating Polyplanes and Cylinder in a
Supersonic how by the Method of Operational Oalculus.0 Moscow Order of lAnin State
U. imeni M: N. Lomonosov, 26 Jun. 191+7
SOi Vechern-vaya Moskva, Jun. 1947 (ProJect #17836)

SAMORYL, Jiri (Brno. Herudova 11.)
Emergency bandage for burns. Rozhl. chir. 37 no.6:3756-381 June 58.
1. KUNZ Brno, klinika plasticke chirargie, prednosta doc. Dr. V. Karfik.
(BURNS, ther.
emergency bandage for extensive burns (Cz))
(.UAMAGING AND MISSING,
me),

SAMOHYL) iiri
Indications and possibilities of free skin grafts instead of skin
flaps. Acta chir. orthop. trauma. Cech. 28 no.4:323-333 Ag 161.
1. Klinika plasticke chirurgie v Brne, prednosta. prof. MUDr.
Vaclav Karfik.
(SKIN TRANSPIANTATION)

SA140HYL J - RIEMLOVA, V.
Some improvements In the technic of dressing severe burns and
in preparation of granulation sites for transplantation. Rozhl.
chir. 40 no.12:776-781 16@,.
1. K.inike plasticke chirurgie v Brne, prednosta prof. MUDr.
V Karfik.
(BUMIS ther.) - (SKIN TRANSPLANTATION)

SAMOHYL, J.; RIEBLOVA, V.
Some improvements in the technique of dressing severe burns and in the
preparation of granulation surfaces for transplantation. Acts. chir.
plast. 4 no.1:8-17 162.
1. Clinic of Plastic Surgery, Brno (Czechoslovakia) Director: Prof.
V. Karfik.
(BURNS ther) (SKIN TRANSPLANTATION) (BANDAGES)

Sk"OHYL. J.
Prevention of the development of contracture and sear deformities in the
treatment of deep burns, Acta chir. orthop. traum. cech. 29 no.6:551-
558 D 162.
1. Klinika plasticke chirurgie lekarske fakulty University J.Ev.
Purkyne v Brne, prednosta prof. dr. V. Karfx'k.
(BURINS) . (CONTRACTURE )

v Brnr@

V.I.r,vGi-N,m,v# V*N*q Inzliti ;!@Illrjlrll, R.D.. inab,
4
V4,L,Ijwdzed trol-loy for romoviMi and rainmi-ting a -turbopr,=tor
roior* gliorgot,114, V, -,tt 166. ( twi!. 19: 1)

SAMOILJ., dr.; IONESCUE.,, ing.; ALEXANDROAIk, I., ing.
Manufacturing superphosphate from phosphorites in the Vietnam
Democratic Republic. Rev. chimie Min petr 12 no.9:512-519 S161

41LU=I, D md c.-u Ti i,;aa);
Gh. @V., prof. (Basau); 'FUNT-IADU, I.,
a@'s ai) ; DioLa: T, , pi ialeo
-of. (F -3u:,,r
Gl'ZLKllU-.ii,'U.1 D. L;icolae (Hirsmra, Dobruja.)i 1, (Fagara--)
G,qOZ--,,;3cu2 T., prof. (Arad)i STAN-0, I,". Oucureiil.i); ITEAC@U, N,, prof.
C ar vi i a o L--- r,
Exer,:@ises axid problerr.3 fcr r@ades 5-8. Gaz mat B 16 no.211@1-93
F 16-5.

SAMOIIA, I. ; POPA, I.
Chalcographic study of complex pyrite and copper ores from Lesul-Ursului ii.
P. 30.
REVISETA MINEDOR. (Ministerul Minelor,, Ministerul Industriei. Petrolului si
Chimiei., Directia FuVloatarilor Miniere si Asociatia Stiintifica a
Inginerilor si Tehnicienilor din Romina) Bucuresti, Rumania. Vol. 10,
no. 1, Jan. 1959.
Month3,y Idst of East European Accessions (EEAI) IC, Vol. 8., no. 7, July 1959
Uncl.

SOCOIY.SCUS M., prof.; BUTUOESOU, N.; POPESCU, Th.,-,-SAMOILA-, Lj
TEODORESCU, D.p, DRAGIIAO 14.
Contributions to the knowledge of stanni ercus mineral-izing in the
Bais. Borsa, Burlotia, ore. Rev min 13 no.-.,I:/+Al-* N 169.

14URESjWUp P*La, prof.; SAMOILAp Z.- PETRESCU, I's
Contributions to the knowledge of the chemical composition of hay
crops obtained from some mixtures of perennial grasses in the year
of sowingo Studii mat Timisoara 7 no.1/2:193-204 Ja-Je 160.
OMAT 10:4)
lo Comitetul de redactie, Studii si cereetari, Stiinte chimice, Baza
de cercetari stUntifice Timisoara (for Muresanu)o
(Grasses) (Hay) I

SAMOILA, Z
AGRICULTURE
Periodical: STUDII SI CERCETARI STIINTIFICE. SERIA STIINTE AGRICOLE
Vol. 4 no. 1/2, Jan./June 1957
SAMOILA, Z.; OPRIN,"C. Geobotanic study of the natural meadows in the
Districts of Timisoara, Jimbolia, and Sinnicol.au Mare (Region Timisoara)
and their state of productivity. p.69
Monthly List of East European Accessions (EEILT), LC, Vol. 8 No- 3,
March 1959, Unclass.

NURESANU, P. L.; SAMOIIA, Z.- FETRESCU., C.; STOIANOVICI,, V.; VIILEANU.,
Nicloeta
Chemical composition of hay 4arvest obtained in the second 7WW
after sowing., and various mixtures of perennial herbs, Note II.
Studii agr Timisoara 8 no.1/2:89-10) 161.
(Planto-Chemical @nslysis) (Hay)

eet @"et
GO'otry.- auxanim
Znrincer
A:-`.U:4t=i. Co3.-ctiva Pax-m (Conpoearla. Arricola Colact-va.), Puriam.
Prnbl"e Zon@olmlrm .11 Vrt@l.-re, !:a 6, @ug Mill
-iha lationzi orp:vnization or Ca=-znal Fa3turor =s tt*z Use of
th, I.-an Convo7or, Frihr--pnl Fams for Incressinr. ?odder
i.-Oductilon (Fron the Exparlonco of the Collective ?am or Faria=,
Banat .4criurw
5-DI" Z. C.-.Finaor3 IC.,h Expor1rantal Station (Statiuma
M.0 , X.,In.
W 1" t V. , i1npinocr , Ropional. Aoricultural. Section (Sectis
Arricala Rarionsia) , aaast. V

MURARIU., Adrian, ing.; �M4OJLESCY.),.Pijyiu,,,ing.
Calibration and rollin the profile for mine armature.
Metalurgia Rum 15 no-5:362-366 My 163.

SAMOILL, Z.A , GIRDA, T.B.; CONTREA, A.
:L.:=4w
Experimental results on the transformatLon of the Nardua otricta
L. association-by agrotechnical surface measures and radical
remaking. Studii core biol vegat 15 no.3:401-420 t63.
-1. Comunicare-prezentata, do I. Popescu-Zeletin., membru
corespondent al Academiei R. P. R.

C) -
V. G*; KWW- WV9 t.. 2.1 MWUMAv 0. 1.
S* OrddMikift Al,-Omim CWWWw-n@OUU"l
I"UtUAO (v"w&l=w4rl
tl*Mddl fustit" in. S. LvdvboaiU&w)q Hose" (for &U)
Yragw* CalleatAon of Cmadwalavak Chadgal CoammicattgM go 12#
r*c 19650 pp 4257-an.
lasidbaft" a" . Part 26& us""as ear"Iltlao of

SPOY49NKO, AIqksaTxIru (Samoilencop A. (Bukharest)
Internation@l cooperation of the railroads of the Rumanian
People's Republic. Zh6l.dor.transp. 10 no.12:31-33 D 161.
(MA 15:1)
1. Direktor Mezhdunarednogo qtdela Ministerstva-trinsporta
i svyazi Rumynskoy N-arodnoy Respubliki.
(Rumania-Railraods-International cooperation)

- SAMOMINA, F.L. - -.- - - -
Production of zymosan labeled with @-+. Med.rad. 6 no-3:80-81
161. (MIRA 34:5)
(WHOSAN)
I