ABSTRACTS OF ARTICLES FROM UNAVAILABLE SOVIET SCIENTIFIC AND TECHNICAL PERIODICALS

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• Sequence Number: 278
• Publication Date: January 11, 1955
• Content Type: REPORT

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REPORT
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DATE OF
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REPORT N0.
THIS IS UNEVALUATED INFORMATION
AASTRACTS OF ARTICLES FROM UNAYAILABLE
SOVIET SCIENTIFIC AND TECHNICAL PERIODICALS (G)
[Comment: This report presents abstracts take^ from Sssues of the
Soviet periodical Referativnyy Zhurnal published July-October 1954.
These abstracts are of articles originally published in Soviet scientific
and technical serial publlcations which are not known to be available out-
side the Soviet Orbit.
The foll.owing form is used for each abstract in this report:
General subJect, specific subJect (Soviet abstract number)
Name of unavailnble periodical, volume and/or issue number,
date, pages
Author. of article
Title of article {Language, if other than Russian)
Abridgment of abstract (Source)
The sources, indicated in parentheses at the end of each abstract,
are abbreviated as follows:
RZhAstr Moscow, Referativnyy 'Zhurnal -- Astronomiya i Geodeziya
RZhFiz bfoscow, Referativnyy 'Zhurnal -- Fizika
RZhKhim Moscow, Referativnyy Zhurnal ~~,,imiya
RZhMat Moscow, Referntivnyy Zhurnal -- D1~ntematika
RZhMekh Moscow, Referativnyy Zhurnal -- idekhanilc~j
50X1-HUM
CLASSIFICATION S_-E-r_R_R_T
CENTRAL INTELLIGENCE AGENCY
INFORMATION FROM
FOREIGN DOCUMENTS OR RADIO BROADCAS'T'S
COUNTRY USSR
SUBJECT Scientific - Astronomy, chemistry, geology,
HOW
PUBLISHED
WHERE
PUBLISHED
DATE
PUBLISHED
Monthly periodicals
Moscow
Jul-Oct 1951+
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Geodesy, Instruments (5G5G)
Sbornik Statey po Geodezii, No 5, 1953, 45-52
Skavronskiy, V. N.
Results of Study of Short-Period Errors in the M?~::ink of the Horizontal
Circle of the Optical Theodolites of the Plant "AeroaFOrribor" OT-02
No 9184, 9195
Test methods of short-period marks on the limb of the specified
theodolites, and the processing of measurements are described. Results
are tabulated and plotted. Actual errors are expected to exceed the
computed ones. (RZhAstr, No'9, 1954)
Geodesy, Theory of Errors (5052)
Sbornik Statey po Geodezii, No 4, 1953, 69-83
Uapenakiy, A. K.
Solution oP Equation of Errors by Means of the Least Maximum Deviation
Author derives his formula under assumption that the maximum deviation
of the function oP errors in absolute value does not exceed the maximum devi-
ation in absolute value. The abstracter is critical of this method. (RZhAstr,
No 9, 1954)
Geodesy, Aerial Survey (5019)
Sbornik Statev po Geodezii, No 5, 1953, 3-16
Konshin, M. D.; Orlov, V. K.~
Determination of Elements of Mutual Orientation From Pictures of a !?Sountsinous
Territory
A determination method of elements of mutual orientation of plctures is
outlined. The corrective terms for the formulas of mutual orientation elements
do not contain products of differences of longitudinal parallaxes and hence
the accuracy of determination is independent of the relief. (RZhAstr, No 9,
1954)
The Sun, Spectroscopic Study (4900)
Bull. AN Georgia 9SP. No 15, 1953, 170-260
Georgobinni, Sh. M.
Spectrohelioscopic Observations on the Mount Kanobili in the Years 1941-1944
Results of systematic observations of bright flocculi, filaments, and
prominences in H alpha light are published. These observations were carried
out by Sh. Chkhaidze, N. Georgobiani, T. Kochlashvili, K. Chuvayev, D. Khita-
rizhvili. (itZhAstr, No 9, 1954)
The Sun, Spectroscopic study (4899)
Izv. Krymskoy Astrofiz. Obaerv., 11, 1954, 102-128
Muetel, E. R.
The Mechanism of GLow of Hydrogen FLocculi
From continuations of previous investigations (ibid. 9 (1952)) author con-
cludes that the H lines delta, epsilon and zeta are not formed in the chromo-
sphere, but in more deeply located layers. The H alpha line is due to exci-
tation of H by electron impact in the chromosphere and to recombination of
protons with electrons. The decrement of Ba]fier lines in flocculi spGetra
and the Whirls around spots are analyzed. (RZhAStr, No 9, 1954)
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Stellar Astronomy, Dynamics of Stellar Systems (4892)
Publikateii Tartuakoy Astron. Obaerv., No 5, 1953, 332-368
Kuzmin, G. G.
Third Integral of Stellar Motion and Dynamics of the Stationary Ga1s,q
The introduction of a third integral, besides the familiar ones of energy
and areas,?is suggested. In the expression of this quadratic integral the first
two terms represent the sum of squares of angular momentc+ around txo mutuallar
perpendicular axes in the plane of the galakv, anr! the third term is of the
type of the energy integral along the z-axis. The author intends to continue
his theory. (RZhAstr, No 9, 1954)
Theoretical Astrophysics, Nex Stars (4868)
Izv. Glav. Astron. Observ AN Ukrainian SSR, I, 1953, 67-84
Gordeladze, Sh. G.
Dissipation of Maas During the Surge of Novae
The amount of matter e3ected during the surge of a Nova is analyzed.
Suggests new methods consisting in determination of density of the stellar
shell by the study of forbidden lines. Another method consists in the de-
terttination of density from the absolute intensities of the Balmer Lines.
(RZhAstr, No 9, 1954)
Astrophysics, Star Observation (4848)
Peremengyye Zvezdy, No 5, 1953, 344-345
Semakin, N. K.
MX Cygni
Analysis of photographs of the Moscox collection did not reveal a star
of 11m - 12m on the spot marked by Rosa. Therefore the existence of this
star is dubious. (RZhAstr, No 9, 1954)
Astrophysics, Star Observations (4847)
Peremennyye Zvezdy, No 5, 1953, 342-344
Martynov, D. Ya.
RS Vulpeculae
A reiterated aaalysie of minim of RS Vul is performed for a possibility
of rotation of its Line of apaides, evidenced by the shifting of the secondary
minima. No definite conclusions could be made. (RZhAatr, No 9, 1954)
Astrophysics, Star Gbservation (4846)
R:remerr~yye 'Zvezdy, No 5, 1953, 341-342
Tsesevich, V. P.
Y 548 Cygni
The brightness of Y 548 Cygni was established from 141 plates of Odessa
Observatory. The star was found to belong to the A1go1 type. (RZhAstr, No 5,
1954)
Astrophysics, Star Observation (4845)
Peremengyye Zvez~, No 5, 1953, 339-340
Eelsalu, Kh. T.
IX Cassiopei
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The brightness of the variable xas estimated from 64 plates obtained in
the period 1940-1953 .and 7 maxima were established. (RZhAstr, No 9, 1954)
Astrophysics, Star Observation
(4844)
Ebmsm~e Zvezd , No 5, 1953,
336-338
Batyrev, A. A.
BIi Vulpeculae
Evaluations of brightness were made from 116 visual observations in 1952
and two maxima were established. A ~ump_like variation of period between 1917-
1935 is possible or a long-period inequality with a 70-year long period.
(RZhAstr, fto 9, 1954)
Astrophysics, Star Observation (4843)
Peremennyye Zvezdy, No 5, 1953, 334-336
Kholopov, P, N
SPZ 918 Persei - a Variable of U Gemini Type Nith Large Amplitude or a Nova
Previous studies and 59 photoplates of rfoscox Observatory were analyzed.
The magnitude of the star could be established only on two negatives and it
was not found on the other plates. Therefore it seems to be either a Nova
or n variable with very large amplitude. (RZhpstr, No 9, 1954)
Astrophysics, Star Observations (4842)
Peremennyye Zvezdy, fto 5, 1953, 332-334
Solov~yev, A, V.
The Semiregular Variable RW Sct
Ten maxima of brightness of the star were established from 210 negatives
of Stalinabad Observatory of 1940-1952? Elements were corrected and oscillations
in brightness were noticed during the maxima and minima. (RZhAstr, No 9, 1954)
Astrophysics, Star Observation (4841)
Peremennyye Zvezdy, No 5, 1953, 330-332
Batyrev, A. A.
SZ Cemini
A total of 142 visual observations of the variable were processed in
1951-1952? The elements were corrected and the maxima established. (RZhAstr,
No 9, 1954)
Astrophysics, Star Observation (4840)
Peremennyye Zvezdy, No 5, 1953, 328-330
Solov'yev, A, V.
The Cepheid RY Canis Ms,joris
The brightness of the variable xas estimated from 116 photoplates of
Stalinabad Observatory obtained in the period 1938-1950. The normal maximum
of brightness was established. (RZhAstr, No 9, 1954)
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Astrophysics, Star Observation (4839)
Peremennyye Zvezdy, No 5, 1953, 326-328
Yefremov, Yu. I.
A New Cepheid AB Camelopard is
This star was found to have a long period. The computed elements are
presented. (RZhAstr, No 9, 1954)
Astrophysics, Star Observation (4838)
Peremennyye Zvezdv, No 5, 1953, 324-326
Lozinskiy, A. M.
Proper Motions oP Five Short-Period Cepheids
The proper motions of these stars were established from comparison of
photoplates made xith the big Moscox astrograph at a 15-year interval. Re-
duction from relative to absolute motion was processed by using tables by
P. P. Parenago. (RZhAstr, No 9, 1954)
Astrophysics, Star Observation (4837)
Peremennyye Zvezdy, No 5, 1953, 314-323
Yudkina, V. P.
Five Short-Period Cepheids
Reference stars, maps of surroundings, and luminosity curves are pre-
sented for the following stars: RS, TV, TW Tauri, RV Ursae Maoris. (RZhAstr,
No 9, 1954)
Astrophysics, Star Observations (4836)
Peremennyye Zvezdy, No 5, 1953, 303-313
Zakharov, G. P.
Results of observation of the following visual variables are presented:
T and beta Lyrae; RY sad TT Unicorni; SY, TW, TY Serpentis; RY Orionis; ST,
SX, TW, UY Pegasi; RS Persei. (RZhAstr, No 9, 1954)
Astrophysics, Star Observation (4835)
Byull. AN Georgia SSR, No 15, 1953, 3-15
Magalashvili, N. L.
Electrophotometry of Eclipsing Variable RX $er and RS Vul
The elements of RX $er were computed from observations under assumptions
of a circular orbit using the method of Piotrowski. The luminosity curve'
of RS Vul was solved under assumption of elliptic orbit. (RZhAatr, No 9,
1954)
Astrophysics, Star Observation (4834)
Izv. Krymskoy Astrofiz Observ., 11, 1954, 91-101
Nekrasova, S. V.
Photoelectric Observations of Delta Sct
The establishment of temperature variation of delta Sct was attempted
by observation of its irregular variation of brightness. A total of 160
observations are presented. The luminosity curve indicates nonetationary
processes in the stars atmosphere. The thermal oscillations xere estimated
within the limits of 200 to 500?. (RZhAstr, No 9, 1954)
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Astrophysics, Star Observation (4829)
Zzv. Krymakoy Ast~ofiz. Observ., 11, 1954, 74-80
Nikonova, Ye. K.
Photoelectric Magnitudes of Bright Reference Stars for Photometry of Planets
An accurate establishment of stellar magnitudes outside the atmosphere
under consideration oP light absorption by the terrestrial atmosphere was
processed. Stellar magnitudes defined by 0. Eggers (Astrn s. 7. 112, 141
(1950)) were used as reference points for oL?acrvar?ion. RZhAstr, No 9,
1954)
Astrophysics, Star Observation (4828)
Izv."Glav. Aatron. Observ. v Pulkovo, No 5, 1954, 31-86
Dadayev, A. N.
Study of Hot Supergianta in Systems of Eclipsing Binaries
Photometry oP continuous spectra of AO Casaiopei and beta Lyrae is
studied. Curves of brightness and of color are plotted using photoplates
of Stebbins and Gutnick. Elements of orbits are comput;d and hypotheses
of gaseous streams are discussed. (RZhAstr, No 9, 1954
Astrophysics, Aatrospectroacopy (4821)
Izv. Glav. Astron. Obaerv, v Pulkovo, No 4, 1953, 45-~
Mitrofanova, L. A.
Determination of Relative Numbers gf Fe II
The transition probabilities of Fe II were computed in the crave band
35G-46o millimicrons for 91 lines. The excitation method of the epectrtim
by ap electric spark is deecribed. The spark temperature was found from gf
Fe I data to be T 5800 ? 380?. (RZhAstr, No 9, 1954)
Hydrochemistry (21513)
Gidrokhim. Materiely, No 21, 1953, 121-134
Vorob~yev, N: I.
The Determination of the Total Mineral and Sulfate Ion Content in Natural
Water by Conductivity
Worked out a method for determining the above by the conductivity method.
Accuracy is snid to be good enough for practical purposes. (RZhXhim, ~, 1954)
Hydrochemistry (21515)
Gidrokhim. Materialy, No 20, 1953, 98-100
Shidlovskaya_p~,chinnikova, Yu. S.
The Preparation of Deoxygenated Water
Describes method of preparing dea,gHenated water by boiling with subsequent
cooling under carbon dioxide. (RZhKhim, 7, 1954)
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Measured the fluorine content in 183 sources of natural water in the
Kazakhstan region. (RZhI4iim, No 7,.1954)
$ydrochemietry (21518)
Gidrokhim. Msterialy, No 21, 1953, 19-23
Cherkinskiy, S. N.j Zaslavskaya Ye. M.; Mikhaylovskaya, L. A.; Khovanskaya, M. G.
Fluorine Contents oP Water Sources in the RSFSR
Investigated the fluorine content of 916 water"supply sources throughout
various places in the RSFSR. (RZktKhim, Ao 7, 1954
Hydrochemistry (21520)
Gidrokhim. Materiel , No 20, 1953, 18-21
Zenin, A. A.; Konovalov, G. S.
The Content of Arsenic, Boron, Bromine, Iodine, and Fluorine in the Waters
of the Kuban River
Measured the amount of the above substances in the Kuban River during
the period 1949_1950. (RZhKhim, No 7, 1954)
Hydrochemistry (21523)
Gidrokhim. Materialy, No 21, 1953, 3-9
Gololobov, Ya, K,
The Thickness of the Oxygen-Fjydrogen Sulfide Layer in the Black Sea
Measured the thickness of the above layer and prepared relief maps,
(RZhHhim, No T, 1954)
Hydrochemistry (21517)
Gidrokhim; Material , No 21, 1953, 24-29
Boguaevich, L. N.?
Fluorine in Kazakhstan Natural Waters
Hydrochemistry (21525)
Gidrokhim. Material, No 21, 1953, 10-18
Pirogova, M. V.
The Chemical Exchange Between the Bottom and the Water Layer of the Black Sea
Studied the chemical and biological composition of the bottom and of
the layer of water adjacent to it in order to investigate the exchange of
materlals. (RZhKhim, No 7, 1954)
Hydrochemistry (21526)
Gldrokhim. Material , No 21, 1953, 144-151
Bnkhman, V. I.; Prokof~yeva, Ye. F.
Dissolved Gases in Silt Deposits (Muds)
Worked out methods for determining the amounts of CO2i H2S, CH4, and N2
in silt deposits. (RZhKhim, No 7, 1954)
Medical (22013)
Za Sots. 2dravookhr. Yzbekistana, No 2, 1953, 29-33
Altman, B. M.
Vitamin C Level in the Blood and Its Extraction From the Urine of Generally
Healthy People Living Under Conditions Prevalent in Tashkent
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Determined the above and concluded that the average annual vitamin C
deficiency in the Tashkent area is 1770 milligrams, (RZhKhim, No 7, 1954)
Nutrition (22044)
Izv. AN Late, SSR, xo 3, 1953, 67-75
shmidt, A. A.
Protein-Vitamin Concentrates, Their Preparation and Place in the Nutrition
of Man
Presents data on the above new nutritional product and its sources of
preparation. Addition of the protein-vitamin concentrate to bread increases
its nutritional value and taste. (RZhithim, No 7, 1954)
Deposits of Useful Minerals (Nonmetallic), Bleaching Clays (570
Izv. AN Turkm. SSR, No 4, 1953, 75-79 )
Murav~yeva, M. Ya.
Dispersion of Clays and Clayey Soils in Turkmenistan
The clays and clayey soils of Turkmenistan, according to the data of
20 analyses of 13 exploited deposits, are characterized by the considerable
content of a clayey-muddy fraction with dimensions of the particles less than
10 microns, and by the predominance of fine dust-like and sandy-dusty particles.
(RZhGeol, 1, 1954)
Deposits of Useful Minerals (Nonmetallic), Clsy, Ceramic and Glass Materials (574)
izv. AN USSR, No 4, 1953, 114-127
Bezborodov, M. A., ldazo, E. E., and Zuyev, N. I.
Nature of Finely-Dispersed Part of Clays of Certain Deposits in Belorussian SSR
The authors investigated the clays of the Vidibor deposits in Pinsk oblast,
the Levaya Ruba deposits in Vitebsk oblast, and the Malinovka deposits in Brest
oblast. The chemical composition of the clays are glven in a table. (RZhGeol,
i, 1954)
Deposits of Combustible Minerals, Coal and Combustible Shales (594)'
izv. AN Uzb. SSR, No 3, 1953, 43-49
Chikryzov, G. S.
Problem of "rorecasting the Coal-Bearing Character of a Covered Region on the
Basis of a Structural-Phasal Analysis (resume in Uzbekistani)
In order to forecast the coal-bearing nature of a covered area one must
study the peculiarities of the ieological structure and the coal-bearing quality
of the productive strata in bordering well-uncovered regions, where the zoaallty
of its structure can be established. The author gives rive prospecting criteria
(indices) determining the position of the zones. Employing these indices one
can determine the expected thickness of the coal layers and their expanse.
(RZhGeol, L, 1954)
Deposits of Combustible tinerals, Geology of Coal Deposits (600)
Izv. pN Kaz. SSR Ser. geol., 121 No 16, 1953, 3_19
Lyuber, A. A.
Blain Types of Coal Formation in the Ifaraganda Coal Basin
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Deposits of Useful Minerals, Formation of De
Mineral Rocks (503) posits and ;enetic Connection
Geologichniy zh
Nikol~s~--'' 13, No 2, 1953, 1 with
Y, o. p, 9-31
Certain problems of the Genesis of Rydrothermal De
resume in Russian)
posits (Ukrainian, with
'The chemical composition of the containing rocks influences the com
and determines the metal-bearing quality of granitic
and belts are connected with definite t Position
intrusive complexes are characterized b~e8 of the conta~ingOrocks~ring zones
according to six schemes listed. 3' multiphasal Individual
(RZhGeol ~(;nvironmental) formation
, No 1, 1 4
Deposits of Useful binerals, Ores of Ferrous Metals (510)
Geologichni Zh 1
Belevtae~-' 3' rro 3, 1953, 3-14 (Ukrainian)
Genesis of Ya. M
Iron Ores of the Saksa~pn Region of Krivoy Rog
The formation of the ~aksagan iron ores was due to the action of three
successive genetically different processes: 1) sedimentar
iron with silicates; 2) enrichment of the rocks with iron under the influence
of plutonic thermal Y accumulation of
minerals with the forA.ationas' 3) separation of the silicates and iron ore
of hydrohematite. (RZhGeol, No 1, 1954)
Engineering Geolo
Geolo 11 )
rveyshtadt,pL.Iizh~~ cnggnee No 4Ge19531c60 6tudy of Natural processes (666
Problem of the 9
Engineering_Geolog cal Conditiong i^ CO?nection with the Evaluation of
are planned Regions where Rydrotechnical Structures
A brief survey is given of works devoted to the fracturin
is pointed out that the Literature contains very little on the
fracturing as connected with engineerin g of racks. It
Examples of the successful B-geological and Problem of ,
beyond the usual formal descriptionation of fractures are~drotechnical matters.
(RZhGeol, 2io l Presented, going
1954)
Engineering Geo1o
Materialy o Inzh~Geoloiiicring_Geological Study of Natural
Vas in, N. A. g NO 4, 1953, 133_135 processes (668)
Some Data on Flood-Erosion Phenomena iq the Southern Regions of the USSR
The author describes one of the floods that occurred in the southern
regions, of the USSR in July 1951, in which the width reached
tremendous quantities of clayey earth were washed awn
flood was only 1.5 hours. 500 meters and
the develo The author notes that the floods are 81on of the
pment of the relief of high mountains. (RZhGeol, No 1
factor in
, 1954)
dendronsring layers ` LIIB rockssubd coals indicate the presence
ferns, pter dos ends Karaga?'1, and Do1a op s in the main
notes the main P ~, and somew}~t rarer calamites.p The authorido-
the Karaganda coal bearinplants existing during the period of formation of
g strata. (RZhGeol, No 1, 1954)
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Engineering Geology, Engineering-Geological Investigation for Construction (672)
Materialy po inzh. geologic, No 4, 1953 (ido~cox), 148-154
Makeyev, Z. A.
Engineering-Geological Investigations of Bridge Crossings With Application of
ELectrical Prospecting
Vertical electrical sounding along the axis of bridge crossings over a
big river shored, without any drilling operations, that almost the entire
bottom of the river valley is built up of sandotones, but the slopes are
gabbrodiabasic. It is concluded that the use of electrical prospecting
methods in bridge building can decrease the amount of drilling. (RZhGeol,
No 1, 1954)
Engineering Geology, Engineering-Geological Investigations for Construction (673)
Materisly po inzh. geologic, No 4, 1953, 7-15
Xarpenko, F. A.
Problems in the Study of Engineering-Geological and Hydrogeological Conditions
for the Construction of Nonferrous Metallurgical Enterprises
Most of the nonferrous metallurgical enterprises are located in the southern
mountainous regions of the USSR, regions with sharply-cut relief and dry climate.
Procedures for engineering-geological investigations in these regions have been
weakly developed; the most important objects for study are the following six:
properties of mountain Loess, saline foundations, excavations, mud flows,
fracturing of rocks, charts. (RZhGcol, No 1, 1954)
Engineering Geology, General Problems (658)
Materialy po inzh. geologic, No 3, 1953, 7-9
Knrpenko, F. A.
Certain Results of the Engineering-Geological and Hydrogeological Operations of
the Affiliate to the State PLanning Institute for Nonferrous Metallurgical
Enterprises During 1951-1952
Methods of mathematical statistics were used to study the laxs governing
the various properties of loess rocks and to investigate the settling and
sagging properties of loess rocks steeped by craters of various compositions.
Complex field and laboratory studies on loess rocks were conducted in Central
Asia to establish the dependence of ^agging and settling of loess rocks upon
their genesis. (RZhGeol, No 1, 1954)
Engineering Geology, Ground Science (Foundations) (662)
Materinly po inzh. geologic, No 3, 1953, 108-120
Kriger, N. I., and Mosknlev, M. R.
Loess Rocks on Steep Slopes
The study of the deformations of loess rocks on steep slopes of mountains
is necessary for industrial, civil and hydraulic engineering constructions.
An important variety of loess rock deformation is "oplyvina," characterized by
the flowing consistency of the rock. Such "flows" in the Tien Shan comprise
only the soil cover or small layers (2-3 meters) on the slope. Hillside
channels, drainage ditches, and sealing of cracks in the soil are recommended
in the struggle against loess-rock flows. (RZhGeol, No 1, 1954)
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General Geology, Personalia (14)
Geologichniy zh., 13, No 4, 1953, 3-7
Rodionov, S. P.
Vladimir Afaoas'yevich Obruchev (Ukrainian)
Biography, occasioned by 90th birthday. (RZhGeol, No 1, 1954)
General Geology, Personalia (15)
Izv. AN Turkm. SSR, fto 3, 1953, 69-72
Babayev, A. G.
Academician Vladimir Afanas'yevich Obruchev
Biography, occasioned by 90th birthday. (RZhGeol, No 1, 1954)
General Geology, Personalia (16)
Vest An Kaz. SSR, No 10, 1953, 59-62
Satpayev, K. I.
Oldest of Soviet Geologists
Commemoration of the 90th birthday of Academician V. A. Obruchev.
(RZhGeol, No 1, 1954)
General Geology, Sessions and Conferences (28)
Izv. AN Uzb. SSR, No 3, 1953, 103-111
Popov, V. I.
Novosibirsk Conference on the Science of Geological Formations
(RZhGeol, No 1, 1954)
Geochemistry, Geochemistry of Natural Processes (B;ypergene Processes) (471)
Geologichniy zh., 13, No 3, 1953, 24-28
Bankovskiy, V. 0.
Condltiona Governing the Mineralogical and Chemical Concentration in the
Sediment-Forming Process of the Donets Productive Carboniferous (Ukrainian,
with Russian resume)
The author considers the displacement in mineralogical and chemical
concentrations during variations in environmental conditions o^ the example
of one of the repeating lithological complexes in the Donets productive layer,
Variation in tectonic conditions leads to increase i^ concentration of some
elements and to decrease in concentration of others. Specific cases are given
concerning Ca and Mg in C and carbonates. (RZhGeol, No 1, 1954)
Geochemistry, Distribution of Isotopes (465)
Dokl. AN Uzb. SSR, No 2, 1953, 12-16
Uklonskiy, A. S.
Preliminary Data on the Study of the Zeotopic Composition of the Surface
and Subterranean Waters of Central Asia
A study xas conducted on the isotopic composition of a great many waters
of Central Aaia by the densimetric aethod, carried out in the Institute of
Geochemistry and Analytical Chemistry, Academy of Sciences USSR. The total
density of the water, without separation into the isotopes H` and 018, was
determined relative to a stapdard, which was water taY.en from the Moscow
water supply. For the first time comparative data has been obtained on the
isotopic composition of Central Asian waters, which permits one to decide
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the following: the constancy of the isotopic composition of river grater along
the river course; the closeness of the isotopic composition of river waters of
Central Asia (Syr-Darya, Amu-Darya) to that of European Waters (Volga, Dnepr);
geological conditions governing the course of certain rivers and their origin
(;aountain, glacier, underground). These data will be utilized to clarify the
genesis of the waters. Also studied was the isotopic composition of rain and
snort water. The relative density of the latter xa= less than the density of
snosrsanddice~glac~rsthe density of waters of rivers which are fed by melting
(RZhGeol, No 1, 195.,)
Geography of the USSR, Central Asian Republics and Kazakhstan (1042)
Izv. AN Kaz. SSR, No 8, 1953, 105-106
Zenkova, V.
Ten Years Since the Discovery of Peak Pobeda [Victory] in Tien Shan Mountains
[No abstract given.] (RZhGeol, P!o 1, 1954)
Geography of the USSR, Central Asian Republics and Kazakhstan (1039)
Izv. AN Uzbek. SSR, No 3, 1953. 31-35
Kimberg, N. V.
Direction of Development of the Soil Cover of the Amu-Darya Delta (resume in
Uzbekiatani)
bottomhlandtdeltaisollshinrCentral As iah(VgeAer~vaaheme of evolution of the
,i~'a, 2!0 14, 1946) cannot completely be applied to the dev- e~lo v sov. pochvoveden
the Amu_Darya delta. IIe considers that the flooding must beptakenoiatoiaccount,
which is of significance in the exploitation of the Amu-Darya delta. (RZhGeol,
No 1, 1g54)
Geography of the USSR, Central Asian Republics and Kazakhstan (1037)
Les, kh-vo, No 11, 1953, 41-43
erez , I. Ye.
System oi' Forest Zones of Kazakhstan
The forests planted with seedlings from the state forest stock in Kazhakh-
stan (more than 26 million hectares), soxn over s territory of 2.7 million km2,
can be systematized according to the plant composition and general medium (soils,
relief, climate and other criteria) into ten zones: north stab-lent birches;
steppe forests of Kustanay and Aktyuba oblasts; forests of Knzhkkstan melko-
sopochnik; ribbon pines of Irtysh; A1tay forest; Tien Shan forest; tugay;
haloxylon; forests of Bostandyk region; fruit-tree forests of south Kazakhstan.
(RZhGeol, No 1, 1954)
Geology of Asia (Outside the USSR), Peoples Republic of China (1115)
17arod_nyy K1tay, No 1, 1954, 14-16
Syue I_yuan~ Rsueh I-yuan]
Administrative Stability of the Peoples Republic of China
[No abstract given.) (RZhGeol, No 1, 1954)
Geography of the USSR, Siberia and the Far East (1017)
Nauka~~ No 11, 1953, 21-22
Andreyev, 0. A.
Soviet Siberia (Ukrainian)
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Brief survey of the natural conditions and economy"~of Siberia.
(RZhGeo1, No'1, 1954)
Geology of the Quaternary Deposits, Loess and Loess Rocks (156)
Materialy po inzh, geologii, No 3, 1953, 56-68
I'yaskovakiy, B. V.
What Is Loess?
The author analyzes the Sdeas of L. S. Berg, who explained the origin
of loess from the viewpoint of soil-formation-processes and refuted the
aeolian theory. In the formation of loess two stages are distinguished:
accumulation of fine earth (the matrix of loess), and its process of loess
forming. The author's opinion is that loess is formed under the humus layer
of steppe soils and is a component part of their profile and that loess is
a lime melkozem [fine earth] of dust-like mechanical composition possessing
a number of characteristic signs. (RZhGeol, 1, 1954)
Geology of Quaternary Deposits, Loess and Loess Rocks (160)
MaterLsly po inzh. geologii, No 4, 1953, 154-158
Terebinskiy, Y. G.
Mountain Loess of Southeast Kazakhstan
The loesaea are distributed 400 to 500 meters in the foothills and
along the slopes of the mountainous massifs at a height of as much as 2400
meters. The thickness of the loess covering is from a fraction of a meter
to several dozen meters. _With increasing altitudes of the occurrence of
loesses the clayey content increases and the sandy content decreases. The
zonality of the loesses according to grnnulometric composition convinced
the author of their neolinn origin. (RZhGeol, 1, 1954)
Geology of Quaternary Deposits, Loess and Loess Rocks (161)
Materialy po inzh. geologii, .No 3, 1953,10-42~
Kriger, N. I.; Moekalev, M. R.
Loesses of Northern and Nestern~T'ie^ Shan Ranges
The author discusses the loesses and loess-like rocks of the following
rnngea: Kirgiz Ala-Tau, Talas Ala-Tau, Chatkal,.Kurama, Pskem, Ugam, and
Kara-Tau; also the loesses of the intermontane valley of the following rivers:
Chu, Arys, Chirchik, Angren, and Syr-Darya. The loesses are extensively dis-
tributed in the intermontane valleys and on the slopes of the mountains of
the west and north Tien Shnn ranges. Loess formation took place during the
entire quaternary period. (RZhGeol, No 1, 1954)
Geology of Quaternary Deposits, Loess and Loess Rocks (162)
Materialy po inzh. geologii, No 3, 1953, 125-126
Konanykhin, S. I.
Compressed Loess-type Rocks from Rudnyy Altay
The physical properties of the loess are: specific weight 2.73, volumetric
weight 1.85, porosity 32-3? Sharp predominance of a pgwdery fraction and
absence of a sandy fraction distinguish the described loess-type rocks from the
stony loess of Central Asia. (RZhGeo1, No 1, 1954)
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Geology of Quaternar% ])epoeite, Loose and Loess 34c 9 (163)
Izv AH Kaz SSR. aer. geol., 121, Mo 16, 1 53,
Koletilin, P. F.
Problem of the Genesis of Loess Rocks in the Foothills o? Zaili Als-Tau
The loess rocks Sn the northern foothills of Zaili Ala-Tau posses
various origins: fluvlsl-glaclnl, alluvial, proluv!ol, deluvial, ris~n ulth
TY.e fluvial-glaelalo1ndRoci;laQ ~~ sses cover great areas in comps
the others. (RZh.,e
( _:!?'+ )
gydrogeology, Generalrroblema nod Methods of Investignticns
a, 63-69
Izv. AR Azerb. SSR, t7o -, 1953,
Davydov, I. Ya? the RegL?w~ of Underground Waters (resr~c in Azerbaydzhnni)
Method for Study!np;
T?:e aut'r.or c?:os!~^'^ taE+t t?`1`-' 1nve~'.igation of the re:,ia.e of underground
waters sY,ould be cocdcet^9 ?:ith consideration for the entire ecmiex of cc:r"p11-
cnted neturai pro-:ersec, uhir_i:?.+uuld lead to a more rational explanation of
the regime na~j -~-?-~~ -- =hcdSCa1 setup of Lhe observational netuork. The
~? ,the uorks of pnrtiec not ~i;loying
author analyzes _::~. T.1'~ ~,.`ic.crcies -
each consideratl._ns. -.:n:c-:
Dolk. Ati Azerb. S.:R, :!=' ? ' - -
~
?r,=:1sr .. ~ h. ,;Lrnta .,. ?;:e C.. _ i'.., G11-
Tn:arazyan, .. F. nnd
~,t,. - DLnikoi.
Problem of tt:e ,i~+turc ef,.h,' .? ~'. ~`=
Bearing Re ion ..;:,.n-~~ .. ~-.,-. ,
^ical charar.L_rist!cs are ?:c^. cC
' ;hie raters
Br1?~f h! r ,, +1
~y a~!r ' ^ northanst +..erbayd7h~
the Crscpiaa ~ y,< ?i,_r:,, an are culfateless and a .:arn. :lth
of the LhL?.1 ...t..cn c.?_ V _-_.,.,'.ion of Lhe uaters ircret+.:~:; 3urln" the
`
~: + --,
a ealinL'y c;f . ;-`~?C' .^ the aster lroflles is 3lrected up?.rar~
proses', of _ :'e!tntloc. -?_- ;. the moving uaters !,, v,r '.ortuous.
r n" th ` ? : - r r ?,hC stet ircr?~a:;e~
Blom? th^ c, d ti1y ` _ _am?neralizatlon o -
jt haS bee. -52r.Ji..+._ ions increase and i?~~.. ..canc.
?~+;r dl?;, clot, s.^. r::, ..
in the- s.,.~ ;,a=~.
roieutc ('
i~ydro;;colo_y, Cn:;pia^ Pct _'~
Ati ^erb. SSR, he ~F, ..
~elarov,A-?`3 Tamruzyna, :;..F~' _ 13carir.~ R:+;lon
'aspian Petrolew~-
Layer 'r:,ter:> c: t!:c ::,!'t.~ ... .
(res+LTr: in \:.ertuy z =an1'i
;:iaycd by subtcrr:+^='an uu::era in the
'ihe author.. vin?'1.c -~_ ... ~- ...,,,-ton is eempor>ed of n cw:,:lex of
1'orcation of lctro_caa ;ci.c~tlta. .,.?-:,;an~?y-clayey lay^ra ^. the N,a!ko1, strata
mcsozoic and tc:?:inry ac;:.,
ere oii-bearing. The nerth?=a:,t. v'-s. e: :anticlinal fo'd to eceplicatred by the
195!+)
?~?~n,,.+ ~ ~rarec~rescions. (FZhI'>eol Yo 1,
presence of ;nrg'----.-_ -.
Mineralogy, General Problems (359) 11_1;6
Izv AN Arm SSR, fiz-mat. yeatesty? 1 tekh. nauki, 6, iio 4, 1953,
Vardanynnts, L. A.
Anomalous Qptlcnl Biaxial'Ch:racter cf Funerals
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The author concludes tktat a ~ .k
their physical ro sties alp: ~ ~?2` -"
Ib: ~lui?:?t thnt onepof tho .r?,,bt ` t cc' .. ' _th t ,
..u?iquated citaractcristics cf cams: ;ri?::, ,,e~; a` :? .Lo, y
.:otuality. (R;hGeol, No 1, 1;51;) ., ,. .' ,~ .
`teal norrs.
.ace the
? !ncrc to
aineraloy, Yiinerals and Groins of i:;r,_r.a;: ~~,a~.: ) ( ~
Gcolo,^,ichniy zh., 13, Ho 3, 153, ~~-`lt (U:.r ~::i . )
Dyaclchen}:o, 1?f. G.
i'in~'ins of ,:ccessor Darite in I'rivcr:.:..
The discovery oP ncc_ssor barite in th_ U:.r:iai?in c:?ystalline uu;;;i^
is o: .3reat interest fer mirerrlegist;. Ore oP tha firot to note r,?:o _
nt barite in thin region aas I. D. Ts "? -~t? '''`
_:ro?: ' 1?: (:;_nerc.lo'i^l:cs:ay sbornii:'
Lwov;;Y.oo i;eologichcsko?o cbshchcatva,
described in detail. - '"?~)? The ncs finds ?tre
ldineralo~r, btinerals and Groups of Efineruls (.ti;lc.t,.s) (!.?24)
Dokl. i:N Azcrb. SSR, 9, Iio 9, 1;53, 51'j-5=k
1Q:.ilifnzadc, Cit. Df.
I?tonothermite and Illite in the Jurassic Clays ,;; Nc r ~::.,,..: tern ;laerbayd zhln
(resume in Azerbaydzhani)
Information on the .aineralo~,ica1 ccnpositiun o. Ll.e Jure:;sic clays of
northeastern :lzerbnydzhan is presented. Te fraction :; than G.001 met of
I'?.;ur saaples o. cloy token frc:a various stratL,ruphic :orir.onc acre suL,jected
to thorou;;h investigation (optical, X-ray structur..1, t.h~.cal, chemical,
npcctrophote?.etric, physicochemical), establishin;; that the clays in the
Jurc.:..;ic deposit; of northeastern :;zerbaydzhan are ::onotacrr itcs and quunti-
tstively in_'erior 111ites. (R:;hGeol, Iio 1, i;>4)
Yctro;;ruphy of A:a~r,:atic and t?fetnmorphic Ro::_ Genr_r.a ircbl::rs (3Ck)
Izv. Ton?,tkoo politcl;lta in-ta, ~4, ;!n 1, ,~ ]Z_1+,