SCIENTIFIC ABSTRACT BURTSEV, A.I. -

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000307710005-8
• Release Decision: RIF
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• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 12, 2000
• Sequence Number: 5
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

Met. i Gidro., 3, 8-15, My-je 1955
Card 2/2 Pub. 71-a - 2/26
AID P - 2492
perattire changes resulting from the vertical movement of
air. Adiabatic heating and cooling, together with ad-
vection, affect the structure of the pressure field on
different levels. Eight Russian references, 1940-1954.
Institution: None
Submitted : No date

124 -58-9 -10058
Translation from: Referativnyy zhurnal, Mekhanika, 1958, Nr 9, p 88 (USSR)
AUTHOR: Burtsev, A. 1.
TITLE: Elements of the Moisture Cycle Above the European Territory of
the USSR (Elementy vlagooborota na ye-,,ropeyskoy territorii SSSR)
PERIODICAL: Tr. Tsentr. in-ta progn07OV, 1955, Nr 38. pp 3-60
ABSTRACT: Bibliographic entry
1. Atmosphere--Moisture content 2. Meteorology--USSR
Card 1/1

BMSRV, A. I*
Evolution of precipitation in connection with the change of moiPture
content 5- the air and of vertical calocities in a cyclone. Meteor.
gidrol. no.1:9-12 Ja'56. (KiaA 9:6)
(Cyclones)

ASTAFENKOF P.D., kand.geograficheakikh neuk;-BUR
_=,,.,A. I., kan&.f iziko
matematichaskikh nauk; GUROV, V.P., kqnd.fiifi~--matematicheskikh
nauk; ZVEnV, A.S., k-and.fiziko-matematicheskikh-.nauk; ZVBYAN,,G.D.,
doktor geograficheskikh nauk; MINNA, L.B., kEknd.geograficheskikh neuk;
MCROZKIN, A.A., inrhener-mateorolog; RUPFRRT. L.L., kancl.geografiche-
skikh nauk; SIMGNYEV, B.M., inzhener-meteorolog; SAMOYLOV. A.I.,
kand.fiziko-matematicheskikh nauk; TUMTTI, Z.L., Imnd.geografiche-
skikh nauk; CHERIJUVA, V.F., starshiy nauchnyy sotrudnik; CHISTTAKOV,
A.D., kand.fiziko-matematicheskikh nauk; POGOSYAN, Kh.P., prof.,red.;
YASROGUROD5KAYA. M.M., red.; BRAYNINA, M.P., tekhn.re&.
[-'synoptic study atlas] Uchebnyi sinopticheBkii atlas. leningred,
Gidrometeor. izd-vo. Pt*2. (Sost. P.D.Astapenko i dr.) 1957.
90 fold. maps (in portfolio)_ _ _ (Practical recommendations
and assignments for students using the "Synoptic study atlas*
Metodicheakie rkomendataii i zedaniia dlia studentov k "Uchebnomu
sinopticbeekoma atlasu," chast' 2. Sost. A-S-Zverev. 1957. 87 P.
(MIRA 11-3)
1. TSentrallnyy Institut Drognozov (for Chernova)
(Climatology--Gharts, diagrams, etc.)

49 - 2 - 10/13
AUTHOR: Pogosyan, Kh.P. and.Burtsev, A.I.
TITLE*. Features in the evolution of the field of temperature,
humidity and pressure of the air in developing cyclons.
(Osobeni,isti evolyutsli poley temperatury, vlazhnosti I
davleniya Vozdukha v razvivayushchikhaya tsiklonakh).
PERIODICAL: Izvestlya Akademii Nauk, Seriya Geofizichesjaya,r1957,
No.2. pp. 245-254.
ABSTRACT: It is shown that the distribution of the changes of
these fields pass through three fundamental stages of
development. Particular attention is paid to clarifying
the means of advection and vertical movement in the
change of the thermal field of the cyclons. It was
established that, in addition to advection of cold air
masses, adiabatic drop of the air temperature in the
central and frontal parts of the cyclons plays an Im-
Card 1/5 portant role.

49 - 2 - 10/13
TITLE:
Card 2/5
Features in the evolution of the field of temperature,
humidity and pressure of the air in developing cyclons.
(Osobennisti evolyutsii poley temperatury, vlazhnosti
i davleniya vozdukha v razvivayushchiRrya tsiklonakh).
CalculationJs based on the selection of thirteen fixed
points, namely, the center of the cyclon and twelve
points distributed symmetrically relative to the center
at distances of 300 and 600 km respectively; for each
of these points the advective and the adiabatic changes
of the average temperature ofthe layer between the
surfaces of 500 and 1000 mb were calculated for every
twelve hours and the calculated values of the total
changes of the average tempeature of the layer were
compared with measured values. These values are
summarized for all the three stages in tables 1 - 3,
p.247. It is concluded that the schemes depicting the
structure of the pressure and temperature fields,
presented by N.L. Taborovskiy (1) for the various
stages of the life of the cyclons, adequatley represents
the entire process of cyclon development.

49 - 2 - 10/13
TITIE: Features in the evolution of the field of temperature,
humidity and pressure of the air in developing cyclons.
(Osobennosti evolyutsii poley temperatury, vlazhnosti
I davleniya vozdukha v razvivayushchikhsya tsiklonakh).
The structure of the thermobaric field In the system of
an extending cyclon is such that it brings about an
approach of cold and warm air masses and lead to an
increase in the horizontal temperature contrasts. With
a degree in development of the cyclon, the advection of
cold extends gradually to the front part of the cyclon
but the drop in temperature takes place not only where
the advection of cold has penetrated but in the entire
system of the cyclon. The calculations of adveqtive
and the adiabatic changes of temperature given here
indicate that adiabatic cooling of air, which is most
pronounced In the front and central parts of the cyclon,
plays an important role in filling the cyclon with cold
Card 3/5 air.

49 - 2 - 10/13
TITLE:
Card 4/5
Features in the evolution of the field of temperature,
humidity and pressure of the air in developing cyclons.
(Osobennosti evolyutsii paley temperatury, vlazhnosti
I davleniya vozdukha v razvivayushchikhsya tsiklonakh).
The general reduction in the air temperature takes place
simultaneously in the entire system of the cyclon but
the intensity of this distribution is unequal. For
stages of maximum cyclon development, the cooling of air
in the tail part is more intense than in other parts of
thecyclon owing to advection of cold which exceeds
adiC:)atic heating. In the front and the central parts,
the temperature decrease is due to adiabatic cooling,
the magnitude of which exceeds advective heating. This
non uniform reduction of temperatnre brings about a
conservation of a warm crest above the central part of
the cyclon, although even there the absolute value of
the temperature decreases. In addition to weal~enlng and
subsequently stopping the advection of cold in the tail
of the cyclon and its penetration Into the front part, a
more intense break up of the warm crest above the central
part of the cyclon takes place; in this process the
adiabatic cooling of air plays an important role in
addition to the advection of cold.

49 - 2 - 10/13
TITLE: Features in the evolution of the field of temperature,
humidity and pressure of the air in developing cyclons.
(Osobennosti evolyutsii poley temperatury, vlazhnosti
i davleniya vozdukha v razvivayushchikhsya tsiklonakh).
In a cyclon system the moisture field usually coincides
satisfactorily with temperature field and is subject to
analogous changes in its individual stages.
The text includes 3 tables and 11 diagrams. There are
7 references, all Slavic.
ASSOCIATION: Central Forecasting Institute (Tsentrallnyy institut
prognozov)
PRESENTED BY:
SUBMITTED: 11/22/55
AVAILABLE: Library of Congress
Card 5/5

BURTSEV, A.I.
- - a"
Considering the changes In vertical velocity with increasing
altitude in the calculation of adiabatie. temperature chaWs.
Moteor.,I g1drol. no.7:26-30 J1 157. Offa& 10:8)
'(Atmospheric temperature)

PWOSYAN, Xh~F.; B1~4SiV. A.
Conditi5g,for the forration of considerable
the southern part of Ifeatern Siberia. Trudy
(Siberia, Western--Precipitation
precipitations over
TSIP zio.60:51-64 '57.
(MIRA 11:3)
(Meteorology))

IBURTSEV, A.I.; POPOVA, T.P.
Comparative evalution of the accuracy of different methods
u9nd in computing vertical air velocities. Trudy TSIP no.772
71-81 '58. (14IRA 12:5)
(Metsoroiogy)

BURTSEV, A.I.
Method of computing vertical air velocities in calculating
altitudinal variations of vertical temperature radients.
Trudy TSIP no.77:82-102 ~58. qHIRA 3.2:5)
(meteorology)

: a U ~T_s C-~ V, (~ - I -
-17 (7) PHASE I BOOK MWITATION SOV/3029
Moscow. Tsentralinyy-inatitut prognozov
Voprosy sinopticheskoy meteorologii (Problems in Synoptic Meteorology) Moscow,,
Gidrometeoizdat (otd.) 1959. 62 p. (Series: Its: Trudy,, vn. 7a) 11100
copies prInted. -
Sponsoring Agency: USSR.Glavnoye upravleniye gidrometeorologicheskoy slnzhby.
Ed. (title page): B. D. UBpenskiy; Ed. (inside book)i -L. B. Blinnikov,
Tech. Ed.: T. Ye. Zemt,sova.
PURPOSE: This issue.-of the Institute's Transactions is intended for specialists
in meteorology.
COVERAGE: This collection of articles discusses problems in synoptic meteorology.
The first tvo articles deal with the formation and structure-of frontal clouds
in the Western Siberia and Ural Mountain area-. Other articles discuss upper-
level cyclonic and anticyclonic phenomena, the evolution of thermal fields,
and thermal convectioii'. References accompany each article.
Card 1/2

Problems in Synoptic Meteorology 807/3029
TAWZ OF CONTEINTS:
Sovetovay V. D. Microstructure of Frontal Clouds Over Western Siberia 3
Sovetova,, V. D. Effect of the Ural Mountain Range on-the Evolution of
Frontal Cloudiness 12
Gayevskayaj, 0. V. The Problem of Accounting for Aqceleration in
Diagnosing and Forecasting the Evolution of Upper-Level Cyclones and
Anticyclones 25
Burtdev,'A. I., and T. P. Popova. The Role of Orderly Vertical Move-
--___me_n_-Us_ and Advection in the Evolution'of ~bhe Thermal Field In Frontal
Zones 33
Pavlovskaya, A, A., Aerological Characteristics of Thermal Convection of
Varying Int(pnsity 44
AMIABLE: Library of Congress
I
Card 2/2 TM/mal
12-29-59

S/050/60/000/05/02/020
B007/BOi4
AUTHORS: Burtsev, A. I., 4eonov, W. G.
TITLEg Slope of the Spatial Axis ofl~aric Systems
PERIODICALB Meteorologiya i gidrologiya, 1960, No- 5, Pp- 11-16
TEXTs quantitative relations between the spatial axis slope of the baric
center and the characteristics of the thermobaric field are derived in
the paper under review. Formulas (1), (2), and (3) are written down for
the spatial axis of the baric systemy and therefrom, the differential
equationt, (11) are obtained for the position of the axis of the baric
system in the space. If there is fairly sufficient accuracy, the spatial
axis of baric systems between two main isobaric planes can be assumed to
be a straight line. Moreover the symmetry axes can be regarded as the
coordinate axes. Formula (13~ is obtained. It follows therefrom that the
shift of the center of baric systems at the upper level with respect to
the system center at the lower level can be determined by the following
4 factorss the horizontal temperature gradients (TX, TY), the thickness
Card 1/3

Slope of the Spatial Axis of Baric Systems S1050V6010001051021020
B007/BO14
of the isobaric layer (p - p0)9 the quantities H xx , Ryy , marking the
curvature of the isobaric plane, and pressure. With equal temperature
gradients, the slope of the axis will be the larger, the smaller the
curvature of the isobaric plane in the center of the baric system. Also
such factors are discussed as give rise to a reduction in the axial slope
of baric systems at various periods of development of such systems. For
an example, a description is given of the cyclone over the European part
of the USSR in the time from June 21 to 25, 1959. This example shows that
the most striking reduction in the axial slope occurred during the first
stage of the cyclonic development, at the time, before occlusion, at
which the temperature contrasts did not change appreciably in the cyclonic
center. Mention is made of the part played by curvature as one of the
factors determining the axial slope of baric systems, and an example is
offered to demonstrate this role with the comparison of the inclination
angles of cyclonic and anticyclonic axes. Moreover, the axial slope of a
baric system depends to a lar e extent on the pressure at the isobaric
planes investigated. Formula M) for the tangent of this inclination
angle is written down in this connection. It is shown that the shift of
Card 2/3

~lope.of the Spatial Axis of Baric Systems S/050/60/000/05/02/020
B007/BO14
the baric center with height does not rigorously proceed along the
horizontal temperature gradient, but may also run to the right or to the
left thereofs formula (15). It follows from this formula that there are
two cases only, in which the shift of the upper center with respect to
the lower occurs precisely along the horizontal temperature gradient.
These cases are (1) if n3a a Ryy , i.e. in the case of steep isobars, and
(2) if tany tanTI, i.e. if the direction of the isothermal lines
coincides wizh the direction of one of the symmetry axes of the barie
system. Magnitude and sign of the deviation of the axis of the baric
center from the direction of the horizontal temperature gradient are
determined by the direction of the iBothermal lines and by the H xx -to-H Yy
ratio. There is 1 figure.
Card 3/3

'EbRTSEV, A.I,
The system of numerical wind and geopotential forecasting in the
lower part of the trojosphere. Trudy TSIF noollO;32-41 16~-V.
(mud
(Weather forecasting)

BURTSEV, A.L; LEONOV, N.G.
Calculation of cyclone mvements based on the initial fields of
pressure and winds@ Trudy TSIP no.110:42-50 161. (IMA 14.-6)
(cyclones)

BURTSEV, A.1 ; VETLOV, I.P.
.Li
.,*.,.Restoration of the geopotential field according to the wind f eld and
,of tne wind field according to the vortex and divergence. Meteor.
i gidrol. no.5t.8-16 My 162. (MM4, 15:6)
(Atmospheric pressure) (Winds)

BURTSEV,- A.I.; VETLOV, I.P.
Map nf imaerical prediction of vind in the free ataosphere.
Meteor.i gidrol. no,*1123-11 Iq 162o (mk:15212)
1. TSentralln7y institut prognozov.
(Vinds)

BELOV,- Pavel Nikolayevich. Prinimali uchastiye: BELSMA, N.N.;
VETIDV' I.p:;.p_IIAT;OV) _Aj.; BELENIKAYA, L.L., red.;
BRAYNINA, 1.1 1 iL .- ~ -
) 'i~ red.
(Practical methods for numerical weather forecasting)
Prakticheskie metody chislennogo prognoza po ody Lenin-
grad, Gidror-eteoizdat, 1963. 257 P. M! 16:12)
(Numerical weather forecasting)

ACCESSION NR: AT4017170 S/2546/63/000/128/0046/0055
AUTHOR: Burtsev, A._I,-i Vetlov, I. P.
, -~ .~ , .;;!'~- -- - ~ I- 7
TITLE: Determination of the paths of air particle& using electronic computers
SOURCE: Moscov, Toontrallay*y institut pro nozov. Trudy*, no. 128, 1963-
Voprosy* kratkosrochny*kh prognozov pogody* NroUiems of shortrange weather
forecasting). 46-55
TOPIC TAGS: meteorology, weather forecasting, wind, short-rarge forecastingi.
air particle, air particle path
ABSTRA,CT: The synoptic method for determination of the paths of air particles,
used currently by the Soviet meteorological service and described in full in the
Manilal on Short-Range Weather Forecasting, is reviewed concisely, with emphasis
on the shortcomings of the method. It involves only an approximate allowance for,
changes of the wind and geopotential fields with time, provides only a rough idea
of the actual movement of a particle and the error, significant at best, is the
greater the longer the period for which the particle path is detemdued-and the
more rapid isthe change of the wind field with time. Improvements were not.
feasible while manual computations were necessary; electronic computers now mks
Caidi/$ 'I-

ACCESSION NB: AT4017170
:it possible to obtain a relatively precise determination' and forecast. A com-
putor of small capacity can calculate the movement of a relatively large number
of particles for a period of several days in a few minutes. The formulas used
in the old method are given, with necessary modifications. A "Ural-11" computer
was used in determining air particle paths at the 700-Mb surface; data for a 12-
hour period of observatione was used, with air particle position determined in
geographic coordinates. A total of 96 particles were traced. Me data fed to
the computer included u and v wind data at 510 points in a grid or geopotential
data at 612 point'a. Fig. 1 of Enclosure shows a chart of air particle paths
for a 24-hour period computed from geopotential data for three successive.peri-
ods of observation. Air particle paths can be predicted by this method provided
there already is a wind or geopotential forecast. An experimental forecast is
described. Orig. art. has; 16 formulas, 3 figures and'l table.
ASSOCIATION: Tsentral'3*7 institutprognozov (Central Institute of Forecasts)
SUBMITTED; 00 DATE ACQ: W064 ENCL. 01
SUB CODE: AS ~0' MW Sm. 001 OMM: 000
d

ACCESSION' NR: AT4017171 S/2546/63/000/128/0056/0063
AUTHOR: Burtsev, A. L; Vetlov, L P.
TITLE: Comoui-tafi6 of components of wind divergence from the geostrophic
SOURCE: Moscow. Tsentrallny*y institut prognozov. Trudy*, no. 128, 1963. Voprosy*
kratk-osrochny*kh prognozov pogody* (Problems of short~-range weather forecasting),
56-63.
TOPIC TAGS: meteorology, geostrophic wind, wind, atmospheric geopotential, atmospherio
pressure field, weather forecasting, short-range weather forecasting, wind divergence
ABSTRACT: Formulas have been derived for calculation of the components of wind
divergence from the geostrophic. For computations with these formulas it is necessary to
have data on wind only for the isobaric surface for which -the computations are made. The,
values of wind divergence from the geostrophic, computed by the method proposed in the
article, agree with theoretical estimates In order of value and with the actual diurnal wind
variability. The niethod is simple and electronic computers of relatively small capacity
can be used. The following are the equations for computatiou of the components of wind
03rdj/4

ACCESSION NR: AT4017171
divergence from the geostrophic. The horizontal components of the wind vector are
represented in the form
OH
V
H
f 6H
where 1 6 y and 67care the horizontal components of the geostrophic wind and ul
and v' are the components of wind divergence from the geostrophic. Then ul an~ V, at
each moment of time can be determined from the system of equations
+ +
Y Y
d V,
The first of these equations is derived if u and v are replaced in the expression for hori-
zontal divergence by their values from (1). The second equation of system (2) Is the
-0i 0 2/4

ACCESSION NR: AT4017171
balance equation, written in somewhat different form. If ul and v' are represented in the
form of the sum of the potential and solenoidal components, that Is, if it is assumed
Y + (3)
V
Y
by solving the equations
61 4) H "al 6H
D +
U13+ (~'-J)-'+ ')Y
Tx) ')Y 2
it is possible to determine and If and therefore ul and v' from given values of the
horizontal compron6nts of wind and geopotential. Formulas (3), (4) and (5) were used to,
compute the values ul and v' at the 700-mb level at 0300 hours on 1, 2, 3, 4 and 5 February
at-285 points o6a s'quaro grid; points'were spaced 300 Ian apart. Computations were made
Card, 3/4

ACCESSION NR,. AT4017171
on a "Ural-111 electronic computer at the Institute of Physics of tlie Atmosphere. - The com-,
ponents ul and v' of wind divergence from the geostrophic computed using formulas (3) - (5)
are smaller than the corresponding values determined by subtraction from the components
of the actual wind of the components of its geostropldc approximation and correspond to
theoretical estimates of the order of their value and actual wind variability. Orig. art.
has: 9 formulas, I table and 3 figures.
ASSOCIATION: Ta6ntrallnyy institut progaozov* (Central Institute of Forecasts)
SUBMITTED: 00 DATE ACQ: 24Feb64 ENCL: 00
SUB CODE: AS NO REP SOV: 015 OTHER: 001
4/4

,-be Siry T T-j d v
oniems in sateliiie
kcrv -~y -m e t e or c.L o g, i
~y
Card V2

-, -;ui-: -~-~T--Vnv tF-Prl'r . - - - -- 4.--"
1 11 '. . I
014 . . wDm:-----,---.:-.~:,
kTD PREss, 4055
-5i
_.. -

r
ft 1-66 M( 0- ''M
IiKs AT5024834
URA*3118/65/OW/OM/0041/0045
AUTHOR: ~Burtsev, A.I.
Arovoy meteorologicheskiy tsentr)
IDRr World meteorological center (V
TITLE: On the prediction of wind and_tesperature
SOURCE: Mirovoy meteorologicheskiy tsentr. Trudy, no. 6, 1965, Voprosy gidrodinami4..'
cheskogo kratkosrochnago prgnoza pogody i mezometeorologii (Problems in hydrodynamic
short-range weather forecasting and r4esometeorology), 41-45
TOPIC TAGS: veather forecasting, hyclrodynamic theory, wind, atmospheric
temperature, computer
ABSTRACT: Author notes present preoccupation with geopotential and wind prediction
methods, and difficulties in computer processing of massive simultaneous fields of
the above parameters plus temperature. He therefore develops a prediction method for
winds and temperatitre, avoiding consideration of geopotential as the predicted para-.
meter. By substitt!ting,:in the hydrodynamic.equations of motion and heat inflow, fi-
nite differences for the time derivatives, three equations are obtained - the pairs:
~(I),(4); (2), (5); and (3), (6). Addition of the continuity equation Z7) and the sta-
tics equation (8) completes his first round in the construction of a system of 5 equ&.
tions for the determination of the 5 unknown functions u,v,-r , H, & T. Here we denote
kl=l8t; k2w`g8t; I - Coriolis parameter St - time step; u0pVo, TO & u,v,T-magnitu-
I - - ___ - _UDC_* -None -

L 3.4o63-66-
ACC NR, AT5024834
des of horisontal wind components and temperature at the time moments t and t +h;
also~ y. and A( - dry adiabatic mid actual adiabatic vertical temperature_gr.a.dients,
and R - the gas constant. With M212 RITOA-T) P

12
P
g
the equations are:
aH
u - ktv k2
dH
-==
V4I
V+k,U+k27
-
Y
T - k3% T.,
0 duo duo + 'o -LUO-
4a UO (U WX +V0 d- OP
Y (4)

va~vo- (U0 avo VO + %D
Fx- + dy
J710 670
T, TO Uo -7x- + to -jy-I U,
(6)
-Tx- + -FY- 7 -F W
OH
T---KCW,
R
(8)
Com A/3

ACC NRt- ATS0.24834
0
By a series of dif f erentiation, eliminations, integrations and substitutions, three
final equations of a mutually related structure and of the same type are obtained for
the determination of intermidiate parameters 11, f, and 0 equationst(14); (15) ' and
the pair (20) & (21). The intermediate parameters are simply related to wind veloci-
ties and to temperature by the equation (11), below, and (3). The combination of the
(20) plus (21) pair (one equation) and ecuation (3) provides the final sytem for the
determination of T in the next time step.. Methods for the solution of the equations
of the type of (14) are well developed, Orig. art. has 21 formulas.
2
nil
+
A2
(2
jp. RUt .7 O)Ta era
+ (U,.+ klV.) I +k- 7~2 n12.
dy
2
+ inj A vF.,
M, +
(V. kla.) + t kl-OX
+ k2
02
C2 +M2A.C=='p"
(20)
t)OC + av RCU
-Yya- + k12 AT,. -(21)
ITO W -77
SUB CODE: SUM DATS:-.-~ OPJG REF: 035/
Card 3/3

ACC NRs
AP7002137 SOURCE CODE: UR/0050/66/000/012/0003/0009
AUTHORS: -JLqrtsevS A ~,_ (Candidate of physico-mathematical sciences); Vetlov, 1. P.
(Candidate of physico-mathematical sciences); Dudnikov, V, N,*) SonecWklrk 'DA,
ORIG: Hydromotoorological Scientific Research Center of the SSSR i
(Gidrometeorologichoskiy nauclino-issledovatellskiy tsentr SSSR)
TITIS: llblolniya-Ill transmits images of the earth from oater space
SOMICEs Matcorolosiya i gidraleglya, no. 12, 1966, 3-9
TOPIC TAGS: meteorologic satellite, tv camera, cloud formation, earth planet,
weather ri-,ap / I-,Iolniya-I meteorologic satellite
ABS11UGT: The authors discuss the television images of the earth, transmitted from
the 111olniya-I satellite. The cameras were mounted on the outside of the housing of
the satellite and had interchangeable objectives. These television cameras permitted'
photographing in the yellow-red region of the spectrum, which increased the quality
of the images of clouds and the earth's surface. Photographs taken at 1500 hrs
1 M'oscow time on 30 I-lay 1966 at an altitude of 30 000-40 000 km are shown. Anal7sis
of the television photographs shows a number of structural peculiarities of large s.
cloud formations that determine the weather over a large territory, Orig. art. ha
1 2 photographs and 1 map.
SUB CODE: 0 SUBM DATE: 19Aug66
i Card 1/1 UDC: 629.195.1:551.5

BURTSEV, A.I., star.shiy prepodavatel'
I-- -
Interaction of loose rocks and fencing supports. Izv. vys. ucheb.
zav.; gor. zhur. no.11:36-42 '61. (MIRA 15:1)
1. Kemerovskiy gornyy institut. Rekomendovana kafedroy razrabotki
poleznykb Iskopayemykh.
(Mine timbering) (Rock pressure)

BURTS vp A o. aspirant
Loads of rubbish on the suspension supports in pitching seams.
Bauch. trudy MGI no.38:n9-226 161. (MA 3-5:10)
(Iline timbering)

BURTSEV, A.I., aspirant
Theory of the movemeft of loose rocks in a mined-out area of
pitching seams and the interaction of them with flexible
movable supports. Nauchp trudy MGI no.38:191-201 161.
1
(MIRA 15:10)

BURTSEVjL_A~.I., inzh.
Load from loose rocks on suspension supports in steep seams,
Izv. vys. ucheb. zav.; gor. zhur. 5 no.3:40-45 162. (MIRA 15:7)
1. Kemerovskiy gornyy institut. Rekamendovana kafedroy
razrabotld mestorozhdeniV poleznykh iskopayemyIdi Nomerovskogo
gornogo instituta,
(Mine timbering)

OREKHOVSKIY, A.A., kand. tekhn. nauk; BURTSEV, A.I., kand. tekbn. nauk
Ways of raising laluor safety in the shield system of mining.
Bezop. truda v prom. 8 no.11:3-6 N 164. (MIRA 18-2)

BURTSXV, A.K., nauchnY7 sotrudnik; SHABANSKIY, V.P., kandidat fiziko-matematiche-
z-skikh nauk.
Into the depth of the atomic nucleus. Nauka i zhizn' 23 no.8:1-4 Ag
156. (MIRA 9:9)
1.Fizicheskiy institut Akademii nauk SSSR (for Bartsev)
(Nuclear physics)

-Pnl IA-RTICIAM A-

AUTHOR: Burtsev, A. K. and Kolomenskiy, A. A. 120-2-2/37
TITIR: On the oLeoi,~Yo ~a Circular Phasotron. (K Teorii
Koll-tsevogo Fazotrona.)
PERIODICAL- Pribory i Tekhnika -.Eksperimenta. 195?, No.2,
pp. 11 - 15 (ITSSR).
ABSTRACT: The strongly focussing accelerator with a magnetic field
constant in time (the circular phasotron) was first
suggested in 1953 by A. A. Kolomenskiy, V. A. Fet-akhov
and M. S. Piabinovich, (Refs. 1 and 2) then by K. R. Symon
in 1955 (Ref. 3). The particle dynamics in the circular
phasotron as compared with the well known strongly focussing
synchrophasotron (Ref. 4) exhibit several pecularities.
In the present article an analysis is made of certain
problems associated with the linear theory of betatron
oscillations in the circular phasotron. From the analysis
of the rnagnetic field of the phasotron the so called
"similarity condition" (Refs. 1 and 2) is defined as
R2/Rl = n2/nl (equation 4). This condition is met only
for a certain set of parameters, e.g. for a = 47V . it
is shown that the "similarity condition" restricts the
choice of the working point in the stable region, for given
Card 1/3 accelerator parameters. The peculiarity of the circular

On the Theory of a Circular Phasotron. 120--2-2/37
phasotron is the fact that conditions for r-(radial) and
z-(vertical) oscillations are not equally important, which
is due to the fact that the sector angles should not be
equal to each other. The mean radius of the magnetic
toroid increases to infinity for Vl::::e-y2 and in general
the stability region is assymmetrical with respect to 'the
bisector of the coordinate angle in the ol, a 2 plane.
The amplitude of the betatron particle oscillations is
characterised by the modulus of Flocquet function. It
can be seen from equations 7 and 8 that this amplitude
increases sharply when the working point approaches the
limit of the stability region ICOS ~L r, zl,-- 1. The number
~f
og
n can be inter-relatea by equation 9 where a 1 is the
c;_ordi-nate of the working point in the a 1 a 2 plane.
Only the case of parai~etric resonanzes is analysed. The
equation for the allowable mean-square values of the field
index n change, which leads to a resonant increase of the
amplituae is given, (equation 10), and their numerical
Card 2/3 values computed for N = 70 and n = 50. The relative
the periodicity elements N and the index
the field

On the Theory of a Circular Phasotron. 120-2-2/37
influence of "fringe" focussing and the influence of the
use of linear gaps and fringes is discussed. The shape
of the maE;netic field is considered and means of obtaining
the necessary con-figuration are discussed. One diagram
and two graphs are given. There are six references, four
of which are Slavic.
SUBMITTED: October, 2?, 1956.
Assov~~,J,ION-. Institute of Physics imeni P. N. Lebedev of the
Academy of Sciences of USSR. (Fisicheskiy Institut im.
P. N. 1j--bedev-a AN SSSR).
AVAILABLO: Library of Congress.
Card 3/3

r ,- ~ T~--\ I- -- 7- V) ~~,
LRYKIN, Ye.M.; BURTSEV, A.I.; D"UXIN, I.&; LICBEZV, A-11.; OXMI, L.B.
Conference on the physics of high-energy particles. Usp.fIz.nauk
61 no.1:103-128 Ja '57~ (WAL 10: 2)
.(Particles, Blemente47)
I

BIM,*,V.V.(trsns1atnr1.: SYROVATSKIY. S.I.. red.: BURTSET. A.K., red.;
SOKOLOVA, T.S., tekhn. red.
C.Nlectromagnatic structure of atoms and nucleons; a collection of
articlas][transiated from the English] Slaktromagnitnaia struktura
isder i nuklonov; abornik statei. Moskva, Izd-vo inostr. lit-ry,
1958. 2C4 p. (MIRA 11:11)
(Nuclear physics)

PIMYA. A.D. [transistor]; ZICLITM, G.I. [translator]; IX!-!.UMG.
I.Xh. [translator]; KONSTAYTINOV, O.Y. [translator];
SHUTIKO.A.T. [translator]; SLIVA,L.A., red.; =TS3V,.AI..KA,
red.; SOKOLOYA,T.S., tekJln.red.
[Deformation oi7 atomic nuclei; generalized nucleus model and
the Coulomb excitntion mettod. Articles trpnslsted from the
3uglishl Deformstaiia atomnykh War; obobahchennaia model'
iadra i matod kulonovskogo vozbunhdaniia. Sbornik Btatei.
Mosk-ya. Izd-vo inostr.lit-ry, 1958. 383 P. (MIRA 14-5)
(Nuclear shell theory) (Nuclei, Atomic)

MSTRIUS, P. [MattheWB, P.T.1; RITUS. V.I. [translator]; USACHXV, Yu.D.
[translator]; BURTSEV, A.K., red.; REZOUKHOVA, A.G., tekbn.red.
(The relativistic quantum theory of elementary particle inter-
actions] Reliativistakaia kvantovaia teoriia vzaimodeistvii
elementarnykh chastits. Hoskva, Izd-vo inostr.lit-ry, 1959.
184 pi ( anslated from the Enalish) - (KIRA 12:11)
Palicles, Zlementary) (Quantum theory)

IOM' V.A. [tranelatorl:' SHWUMIT. G.A., red.; BURTSM, A,K,, red.;
IMNrLLOT, B.I., tekhn.red..; POTMUKOVA,
-[Dielectric spectroscopy; recent atudiez on'the properties of
certain ferromagnetie samico Uotors and diAectrics: relax'stion.
processes, electric conductance, losses, and the role of structural
defects. Translated articles] Dielektriebeeksis ope'ktroskopila;
noveiahie iseledavaniia evoistv nakotarykh forromagrxitnykh polu-
provodnikov i dielaktrikov; re1aksst#'Ibnnye protsessy. elektropro-
vodnost', ppieri i roll defektoy struktury. Sbornik statei. Pod
red. G.A.Smolenikogo. Moskva, lzcl-vo inostr.lit-ry, 1960. 362 p.
AMIRA 14:4)
(Spectrum analysis) (Dielectrics) (Semiconductors)

., SHP
KOVRIZRIYKH, L.M. [translator]; RHZER, M.D. [translator] - IGEL I j
I.S.[translator]; RABINOVICH, M.S.,, red.; BURTSEV, A.K.-f-
red.; POTAPENKOVA, Ye.S.,, tekhn. red.
(Plamna physicu and mngnotolWdrodynamics) Fisika plamq i mag-
nitnaia gidrodinmnika; sbornik statei, 14oskva, Izd-vo inostr.
lit-ry 1961. 302 p. Translated articles. (MI.U 15:3)
tPlasm (Ionized gases)) (MagnotolWdrodynamics)

N.Mjtranslatorl; RUM )fl-P
NOVAKU, Vjllovacu, Valerl, prof.). Ot-'-IJANUt
red.;_ A.K'. , red.; GRUSHIN, A.V.) tekhn. rod.
[Introduction to electrodynamics] Vvedenie v elektrodinamiku.
Moskva, Izd-vo inostr. lit-ry, 1963. 303 p. (MIRA 17:1)
1. Chlen-korrespondent AN Run;ynskoy SSR (for Novaku).

GG
~%a_ ANA%,; z.w.K- 50 SOURCE CODE: UR/C)051/65/019/004/0469/0473
AUTHOR: Bolotovsk!y, B. M.; Burtsev, A. K.
ORG- none
TITLE: Radiation of charge passing over diffraction grating
SOURCE: Optika i spektroskopiya, v. 19, no. 4, 1965, 469-473
TOPIC TAGS diffraction grating, electron radiq4o~,- electromagpetic radiation
ABSTRACT: When a uniformly movlng~electjron passes over any periodic structure such as
a diffraction grating, an oriented electromagnetic radiation 31s emitted. This phenomenon
has practical applications in the generation of electromagnetic radiation over a wide fre-
quency range that is difficult to attain by other methods. To explain this radiation, the
authors consider a three-dimensional problem in the approximation of the scalar theory-of
diffraction. Formulas are derived for the fleld and intensity of radiation of a point dis-
charge and a planar modulated electron flux. It is shown that at small distances of the
moving source from the diffraction grating, the radiation during passage over an inhomo-
geneous surface is Identical to the radiation of a charge which moves in a vacuum and whose
li-Card 1/2. 535.23:539.124

BURTSEV, A.M.
-I-- - - I- . -----------
Experience in decreasing industrial traumatism at the Syas' Paper
and Rap Combine. Zdrav. Ros. Feder. 8 no.21.5-8 P163 -
(MIRA 17:3)
1. Institut organizatsii zdravookhraneniya i istorii meditsiny
imeni II.A. Semashko (dir. P.I.Kall-yu).

BEER=

BURTSW, A.N., akend.med.no~"T'r; PAPAZOV, Y.K.
Multiple giant cell xanthomatous granulomms of the tendons. Ortop.
travm. i protes. 18 no.6:47-48 11-D '57. (MIRA 11:4)
1. Iz goopitallnoy kbirurgichaskoy kliniki imeni prof. V.M.Bogo-
slavskogo (zav. - prof. R.V.Bogoelavskiy) Stalinakogo meditsinakogo
institute (dir. - dotsent A.M.Ganichkin)
(TwORS, dis.
giant-call xanthomatous granuloma)
(GILANUIA)Kk
giant-cell zanthometous granuloma of tendons)

BURTSICV, A. N. kand.medenauk-. FAFAZOV, F.K.
Neurinoma of the ratroparitoneal space compressing the ureter.
Urologiia 22 no.6:56-57 N-D '57. (MIRA 11:2)
1. 1z gospitalluoy khtrurgicheakoy kliniki imani V.H.Bogo5lavskogo
(zav. - Prof. M.Bogoslavskiy) Stalinakogo meditainskogo instituts
(RITROP"ONSAL SPACE. neoplasms
neurilemmome. causing compression of ureter)
(11WRIUMMOMA
retroperitoneal space, causing compression of ureter)
(URETIRS. die.
compression by neurilammoma of retroperitoneal space)

BMITSEV, A.N., kand.med.nauk (Stnlino, ul. Artema, d.84b, kv.16)
Two operations for removing needles from henrt muscles. Novekhir.
arkh. no.2*.B9 Mr-Ap 158 (MM 11:6)
1. GoupitalInaya khirurgicheakaya klinikEk (zav. - Drof. R.P.
BogoslAvskiy) Stanlinskogo meditsinskogo instituta.*
(EMT--P=,IGIi BODIES)

IBUIRTSEV, A.N., kand.med.nauk
Plastic surgery for defect of the cranial vault after excision of an
osteoma. Ortop., trav.i protez. 20 n0-10:75-76 0 159. (MIRA 13:2)
1. Iz gospitallnoy khirurgicbeskoy kliniki im. V.M. Bogoslavskogo
(zav. - doktor med.nauk prof. R.V. Bogoslavskiy) Stalinskogo medi-
tsinskogo instituta (dir. - dots. A.M. Ganichkin).
(MUU neoplasms)
(OSTEOMA surgery)

BURTSEV, -A.N., kand.med.-nauk
Decubitus ulcers of the small intestine caused by a catheter
used in feeding the patient following gastrectomy.-Vest.khir.
87 no.11:111-3-12 N 161. 1 (KMA 15:11)
1. Iz gospitallnoy khirurgichoskoy kliniki im. prof. V.M. IrOgo-
slavskogo (zav. - prof. R.V. Bogoslavakiy)'na baze klinicheskoy
bollnitsy Stalinskogo meditsinskogo institute.
(STOMACH-SURGERY) (INTESTRW-ULGERS)

BURTSEV, A.14., kand. med. nauk (Donetsk, ul. Artema., d.81+,kv.16)
Apparatus for the formation of esophageal anastomoses by means
of a mechanical two-row suture, Klin, khir, no.10.-80-81 0 162.
(MM 16:7)
1. Gospitallnaya khirurgicheskaya klinika imeni. prof. V.M. Bogo-
slavskogo (zav.- prof. R*V, Bogoalavskiy) Donetskogo moditsinskogo
instituta.
(SURGICAL INSTRUMENTS AND APPARATUS)
(ESOPHAGUS--SURGERY)

130BORITSKIY, F.M.; MROT , P.P.; BURTSIV, A.P.
.Diecussion of the artiols "Ways of mechanizing line work". Avtom..,
telem. i aviaz' no-3:40 Wr 157- (MLU 10:4)
1. Nachallnik otdola slushby signalizatsii i avyazi Yugo-Zapaduoy
dorogi (for Baboritakly). 2. Zlektromakhanik Moskovskoy distantsii
signalizatmii i avyazi Koskovsko-lursko-Doubasakoy dorigi (Kimble).
3. Starshiy inzhener Mookovsko-Smoleaskoy distantsii sigualizateii
I, svyazi Kalininskoy dorogi (for Burtmay).
(Alentric line*)

KULAW, V.N,; GRIIGORIYEVp Ye,A.; MRTSKVI B.V.
Founding the profiled part of idrboccmpressor rotors. Listoproiav.
no.11939-40 14 162. (MMA 15:32)
(impellers) (Founding)

BURTSEV. D.A.; GOLIDIN, B.H.
"'
Work of the Simferopol' Hydromateorological Bureau. MstoGr. I
gidrol. no.12-144 D '56. (MMA 10:1)
(Simforopol'-Metoorology)(Simferopoll--Hydrology)

SOV/169-59-7-7447
Translation from: Referativnyy zhurnal, Geofizika, 1959, Nr 7, p 140 (USSR)
AUTHOR: Burtsev, D.A.
IV
TITLE- Aurora Polaris in the Crimea
PERIODICAL- Izv. Krymsk. otd. Geogr. o-va USSR, 1958, Nr 5, pp 273 - 274
ABSTRACT- The author reports on the observations of intense aurora polaris
in 1957 in the night from 21 to 22 January in theyevpatoriya
region and on September 29 in the Kerch' region. During the
appearance of phenomenon of aurora polaris, a sharp deterioration
of the radio communications was recorded.
Card I/I

BURTSBV, D.A.; STIUZ)iKOVA. Ye.H.
r~ -
Some characteristics of and synaptic conditions for the formation
and disappearanco of the snow cover in the Crimean Mountains.
Trudy Uk-fNIGKI no.12:110-122 158. (MIRA 11:12)
(Crimean Mountains-Snow)

3 (7)
.&UTHOR: Burtsev, D. A. SOV/50-59-3-10/24
TITLE: Unusual Frosts o Crimea (Neobyohnyye zamorozk-4 v Krymu)
PERIODICAL: Meteorologiya i gidrologiya, 1959, NT 3, r 40 (USSR)
ABSTRACT: On June 7 - 9, 1958 the weather bename considerably colder on
Crimea. On June 7, the air temperature dropped by 10 to 120 com-
pared to-the preceding day. In the following days it became
still colder. During the night to June 8 frosts were observed
in the mountains at altitudes of 900 - 1200 m, and on June 95
frosts occurxedalso in a number of steppe- and promontory areas.
The strongest frosts were observed during the nigh'. to June 9.
In Voronki (steppe area) temperatures dropped to -0.20 during
that night, in Belogorsk (promontory area) to 00 and on the Ay-
-Petri mountain to -2.0 0. In a number of districts the fm'osts
caused considerable damage to agriculture (corn, grapes).
Card 1/1

3 (7)
AUTHORS: Burtsev, D. A., Belashchenko, N. A. SOV/50-59-8-9/19
TITLE: Thunderstorm With Snow -'.n the Crimea (Groza so snegom v Yrymu)
PERIODICAL: Meteorologiya i gidrologiya, 1959, Nr 8, P 32 (USSR)
A13STRACT: On January 12, 19590 the formation of cumulo--nimbus clouds ac-
companied by snowfall, which er, 'imes limited visi~Ility to
200-500 m, was observed for some hours in Simfero-uo2.'.The
shower clouds originated rapidly, and were destroyeu just as
rapidly. The interval between individual "charges" amounted to
30-35 minutes at the most. Thunder was heard some times at mid-
day. Precipitation fell in the form of a downpour-snowfall and
frozen-fog grains. Since the beginning of regular meteorological
observations in Simferopol! in 1891, a thunderstorm in January
was recorded only 3 times. The winter thunderstorms ':I the
Crimea were only observed at. the polar fronts at the outlet of
11 southern cyclones, and were accompanied by downpoum On
January 12y 1959, the Crimea and the adjoining area wer,3
In the reex 6f t-he le'px-ession, ir- fcraed.-l- Mnsses of
former aratic air. 2he data of the radio sounding in
Simferopollat 9-15 hours on that day showed a moist-labile state
Card 1/2 of the atmosphere in the layer of from 1090 to 3200 m. The pilot-

Thunderstorm With Bnow n the Crimea SOV/50-59-8-9/19
balloon data showed at 15 hours a "gap" on the wind vector in
the layer up to 1000 m; at an altitude of 400 m, the direction
was recorded with 3320, and the velocity with 6 m/sec, whereas 0
at an altitude of 1000 m the direction was determined with 261
and the velocity with 17 m/sec. Higher up, the wind changed
little with the altitude. To clarify the possibility of a for-
mation. of a turbulent mixture in the lower layers in the kind
shown.in paper (Ref 1), the thermal equivalent of the vertical
gradient of the wind vector was calculated, and the "thermody-
namic" curve was plotted. The result showed a dry-labile state
of the atmosphere in the layer of 0-700 m with a condensation
level at an altitude of 550 m, a moisture-neutral state in the
layer of 700-1090 m, and a moisture-labile state in the layer
from 1090 to 3200 m. Consequently, the great dynamic turbulence
in the lower kilometer could form a thrust sufficient to over-
come the labile state and to form the cumulo-nimbus clouds. The
intrusion of cold air aisturbed the day-temperature course, but
the moving air itself was heated in the day-hours which also
favored the formation of convection. South of Simferopol~ there
are the ~I ountains, and the current coming from north
had to undergo e.'risipg motion which also intensified convec-
Card 2/2 tion. There is 1 Soviet reference.

VAZHOV, Vasiliy Ivanovich. kand.geograf.nauk; BURTSET, Dmitriy Antonovich-
~7
ZHILUKOVA, 0., red.; ISUOVA, N., tekhn.r-e7~.--=-`
[Unseasonable frosts and their
Simferopol', Krymizdat, 1960.
(Crimea-Crops
(Crimea-Mrost
control] Zemorozki i borlba s nimi.
79 P. (MIRA 13:12)
end climate)
protection)

AUTHOR: Burtsev D. A.
TITLE:. A thunderstorm with snow
PERIODICAL: Refera'tivnyy zhurnal, Geofizika,
stract 7B249 (Izv. Krymsk.
no. 7, 19612 217-220)
S/16 62/000/007/107/149
D228YD307
no. 7, 1962, 47, ab-
otd. Geogr. o-va SSSR,
TEXT: An intramass thunderstorm, accompanied by showery snow and
soft hail, was observed-on January 12, 1959, at Simferopol' from
1306 hrs to 1316 hrs. The upper cloud boundary did not exceed 3 -
3.5 km during the thunderstorm. Intense Cb forma.tion and destruc-
tioTi and snow charges,.recurring every 30 - 35 minutes were noted
before the thunderstorm, in masses of f 'resh Arctic air coming
from the north-west. The vertical temperature gradient in the lay-
er 1 - 3 km, according to the data of soundin- at Simferopol' at
09 and 15 hra, reached 0.75 - 0.78 deg/100 m.oThe thermodynamic*
stratification curve, constructed with allowance for the thermal
equivalbnt of the wind velocity's vertical gradient, was charac-
Card 1/2

A thunderstorm with snow
S/169/62/000/007/'107/149
D228/D307
terized by dry instability to a height of 700 m, by moist indiffer-'
ent stratification in the layer 700 - 1090 m, and by moist insta-
bilit to a height of 3200 m. The wind veloc-ity was maximal (17
m/sec~ at a height of 1 km, and the wind direction changed from
3320 at a height of 400 m to 2500 at a height of 1500 m and more.
The intensity of Cb formation and of the thunderstorm near Simfe-
ropol' increased in connection with the genqsis of orographic ver-
tical movements in the airstream directed parallel to the m~dn
ridge of the Crimean Mountains. 2 references. /-Abstracter's.note:
Complete translation.-7
Card 2/2

GRECHISHNIKOV, Nikolay Pavlovich; BURTSEV, D.N.) retsenzent;
X11MOSOV, I. I. p doktor g eol -prof.) otv. red.
[Methods of studying the material composition of solid fuel
minerals] Metody issledovaniia veshchestvennogo sostava
tverdykh goriuchikh iskopaerykh. Moskva) Izd-vo "Nedra,"
1964. 214 p. (MIRA 17:5)

AMMOSOV, I.I., red.; BURTSEV, D.IL, red.; GORIYUNOV, S.V., red.;
GUSEVY A.I., red.; KbROTK(YV, G.V., red.; KOTLUKOV, V.A.p
red.; KUZNETSOV, LA red.; MIRONOV, K.V., red,;
, NEKIPELOV., V.Ye., red. ; P01101UREV,
MOLCHANOVI I.I., red:!
T.N., red.; POPOV, V.P.S red.; FROKHOROV, S.P., red;
SHROBOV, S.A.p red.; TYZE40VI AN., red.; SHABAROV, N.V.p
red.; YAVORSKIY, V.I.,q red.; BOBffSHEV, A.T.., red. toma;
VINOGRADOVp B.G.., red. toma; VOLKGV, K.Yu., zam. red. toma;
LUGOV071 G.Lp zam. red. toma; OGARKOV., V.S.,, rea. toma;
SIMONOV, AN.., red. tome; IZRAIISVA, G.A., red.izd-va;
IVANOVA, A.G., tekhn. red.
[Geology of coal and combustible shale deposits in the
U.S.S.R.]Geologiia mestorozhdenii uglia i goriuchikh slan-
tsev SSSR. Glav.red.I.I.Ammosov i dr. Moskva, Gosgeoltakh-
izdat. Vol.2. [Moscow Basin and other coal deposits in
central and eastern provinces of the European part ofthe
U.S.S.R.IPodmoskovrwi bassein i drugie mestorozhdeniia uglia
tsentral'rWkh i vostochnykh oblastei Evropeiskoi chasti
FWSR. 1962. 569 p. maps. (MIRA 15:9)
1. Russia (1923- U.S.S.R.)Ministerstvo geologii i okhrary
nedr.
(Coal geology)

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AUTHOR! Burtsev, D.N.; Molchanov, 1.1. 132-58-5-14/14
TITLE: Conference of Coal :~T-l ng Geologists and Coal Chemists
(Soveshchaniye geologov-uglerazvedchikov i uglekhimikov)
PERTODICALt Razvedka i Okhrana Nedrq 1958, Nr 5, pp 63-64 (USSR)
ABSTRACTt From 26 to 29 March 1958, a conference of Soviet coal-
prospecting geologists and coal chemists took place at VSEGEI
in Leningrad by order of the Minister of Geology and Conser-
vation of Mineral Resources of the USSR. Among the 200 spe-
cialists, there were 32 members of the Ekspertho-Geologi-
cheskiy Sovet (council of Geological Experts) and represen-
tatives uf the All-Union, RSFSR and UkrSSR State Plans, the
USSR AS, research institutes and universities. The conference
was devoted to two main themest 1) The results of studies of
the coal basins and deposits in the USSR, and the further
direction of geological prospecting from 1959 to 1965 and
2) The results and methods of studies for their complex
utilization. S.A. Skrobov of the Minist,.-rstvo geologii i
okhrany nedr SSSR (USSR Ministry of the Geology and Conser-
vation of blineral Aesources) and N.V. Shabarov of VSEGEI spoke
on the first theme. They pointed out that the USSR has 58%
C&rd 1/3 of the world,la coal deposits, and that the presently un-

Conference of Coal -prospecting Geologists and Coal Chemists 132-58-5-14/14
developed coal reserves exceed those to be opened between
1959 and 1965 by 3 times. The insufficient capacity of con-
centration plants makes the lack of ash coal for coking still
more acute. Increased prospecting for coking coal, mainly in
the Donets, Kuznetsk and Karaganda basins, will go on in the
new 7-year period. The second theme was introduced by I.I.
Ammosov of IGI of the AS USSR who stressed the need for a
practical knowledge of petrology in coal prospecting. Addi-
tional reports were presented by F.Ya. Saprykin of VSEGEI,
I.V. Shmanenkov of V11AS and V.M. Ratynskiy of IGI of the
AS SSSR. Critical remarks on faulty planning and errors in
methods were delivered by the Deputy President of GKZ, X.V.
Mironov. The editors of the indivi4ual volumes of "Geologiya
ugollnykh mestorozhdeniy" (Geo'Logy of Coal Deposits) made
brief statements. Volumes I - IV will be published by
1 December 1956, V - VII by 1 March 1959 and VIII by 1 June
1959.
Card 2/3

C.-.e;'-ren-2e of Geologists and Coat Chemists 132-58-4-14/14
Q! CC,hTIONt Minis tez I o' -,-a y ad SSSR (Ministry of Geology
end Com~,~~.-vation ~~f ML~Aral 3ourcoa of the USSR) Glavgeologiya
pi~--- &~-~ete Miulstz-ov P-SF5R ~Msln Geological .-Pros ating Adminle-
tration of the Covmw:il -.~-f Ministers of th-5 RSFW-
AW I TA P 12 - Ubvar), of CzaVsI-.t
Card --/3 1. Geochemistr7-Conference
TJSCOMM-DC-54817

~JOLGM-JGV, I.I.; SKROBOV, S.A., TYMNOV, A.V~
"Coal" by P.V.Vasillev. Reviewed by D.N.Burtuav anci otherq.
Sov.geol- 5 no.38157-160 Mr 162. (MINI "&5,!,1 )
(Coal) (Vasillev,. P.V.)

SKROBOV, S.A., glav. red.; TYZ11NOV, A.V., zam. glav. red.; SHABAROV,
N.V., zam. glav. red.; PJ'2/10SOV, I.I., redaktor;
red. V_URT6ET,_D
red.; IVAROV, G.A., red.; KORDTKUv, V.,
red.; KOTLUKOV, V.A., red.; KUZNETSOV, I.A., red.;
MIRONOV, K.V., redaktor; MOLC111ANOV, I.I., redaktor;
VZKI~ELOV, V.Ye., red.; PONOMAREV, T.N., red.; POPOV, V.S.,
red.; PROKHOROV, S.P.., red.; YAVORSKIY, V.I., red.; LAGUTINA,
V.V., red. toma; LEVENSHTEYN, M.L., red. toma; SHIROKOV, A.Z.,
red. toma; IZRAIIEVA, G.A., red.izd-va; KROTOVA, I.Ye., red.
izd-va; IVANOVA, A.G., tekhn. red.
[Geology of coal and combustible shale in the U.S.S.R.]Geologiia
mestorozhdenii uglia i goriuchikh slantsev SSSR. Glav. red. I.I.
Ammosov i dr. Moskva, Gosgeoltekhizdat. Vol.l.[Coal basins and
deposits in the south of the European part of the U.S.S.Si;Donets
Basin, Dnieper Basin,:Lvov-Volyn' Basin, deposits of the western
provinces of Moldavia and the Ukraine, White Russia, Trans-
caucasia and the Northern Caucasus] Ugollnye basseiny i mesto-
rozhdeniia iuga Evropeiskoi chasti SSSR; Donetskii bassein, Dnep-
rovskii bassein, Llvovsko-Volynskii bassein, mestorozhdeniia za-
padnykh oblastei U~ra:ltny i Moldavii, Belorussii, Severnogo Kav-
kaza i Zakavkazlia. 1963. 1210 p. (KTRA 17:3)
1. Russia (1923- U.S.S.R.) Gosudarstvennyy geologicheskiy komitet.

BU RTSEV, - D. B. ~-
Condensing K.V, Mironov'r, booR "Goological and irduot-rial ova-
luation of coal deposits". Razved. i okh. nedr 29 no.11:63-64
N 163. (IrLMA 17: 12)
1. Gosudarstvennyy geologicheskiy komitet SSSR.

AUTHOR: Burtsev, G.A. Sov/106-58-2-11/16
TITLE: Propagation of Pulses in Infinite Lines (Rasprostraneniye
impullsov v beskonechnykh liniyakh)
PERIODICAL: Elektrosvyazl, 1958, Nr 2, p ?4 (USSR)
ABSTRACT: If the frequency characteristicsof a communication line
are approximated by the expressions:
0 = 00 + bV_W (1)
cx = aw + b FW (2)
then, as has been shown by L.A. Zhekulin in his paper "Propaga-
tion of signals by coaxial cable" (Ref 1), the voltage produced
in an infinite line When a unit step of voltage is applied to
it can be represented as:
U(t1j ) = e-OOL 0 Wl
where t' = t - Z/v is the distance up to the point in the
line-,
Cardl/3 v is the velocity of propagation of the signal;

Propagation of Pulses in Infinite Lines Sov/106-58-2-11/16
x = bt /q-2t'
2
(x) = 2 e-z dz
ff ~
is the Gaussian integral, the value of ~aich can be found from
tables (e.g.I~ef 2).
The approximating expressions (1) and (2) reproduce comparatively
well the shape of the frequency characteristics of aerial lines
of copper (Figure 1) and of steel (Figure 2)(wire diameter 4 mm;
s8paration0between wires 60 cm; conditions: "summer - dry";
t = + 20 C). as well as symmetrical cable with styroflex-cord
insulation (conductor diameter 1.2 mm) (Figure 3). In the
diagrams, the solid lines show the actual characteristics con-
structed from data in Ref 3 and the dashed lines represent the
approximate expressions. The phase-frequency characteristics
have not been given for the present scale.
Therefore, the results of L.A. Zhekulin can be applied to the
Card2/3

Propagation of Pulses in Infinite Lines Sov/106-58-2-11/16
investigation of signal propagation not only in a coaxial
cable. Figures 1, 2 and 3 also show the shape of a rect-
angular pulse 20 4sec long at various points in the lines.
There are 3 figures and 3 Soviet references.
SUBMITTED: December 7, 1956
Card 3/3 1. Pulses--Propagation 2. Pulses--Mathematical analysis

BURTSEV, G.A.
Multiple unit magnetic probes. Defektoskopiia 1 no.4:23-32
165. (MIPA 18.,1-9)
1. Institut fiziki metallov AN SSSR.

Wl-.
U-AUMP-M-
TITLE: Inc reasing the selectivity of the ferroprobt examint C.,-. -f
p r o al u c t qfo7- ;urfac-r- defectp
"na C r
C ra, F, ~Iil: r! o,
ABSMACT: Th ree me th odE are desc ribed f or i nc reas i -Ii: he. 5 f-
fe r copr o~~f, s u,- ac e -nT)t -nj of tma
P4

Pjl~125~65-

ACCESSION NR; AF50182.3b

2) the readinp i,( a ~ez-er~ of sip Mans 0!
Tin

c1 v i w, ~i: F i a a i v reduceLz th e overai. IeVE-,

t: a r f., S!,

171 i k i I
4~% S S
; R
.
.
A N _SSS RR

FOUPrO
-SUB WDE !E:

Cord

BURTSETY G. A.
Quality critera of large-scale flaw detection. Defekto-
skopi.ia no. 5:74-83 f65 (IURA 19tl)
1. Institut fiziki metallov AN SSSR.

BURTSEV I A
Reproductive ability of the hybrid between sturgeon and sterlet.
Dokl. Mi SSSR. 144 no.6:1377-1379 Ja 162. (MM .15:6)
1. Saragovskoye otdeleniye Gosudarstvennogo nauchno-issledovatelf-
skogo institute. ozernogo i rechnogo rybnogo khozyaystva. Pres-
stavleno -.t!~ad. Ye.N,Pavlovskim. *
('Hybridization) (Sturgeons) (Reproduction)

BURTSICT, I.B.
Experimental study of oil recovery in water flood operations.
Trudy VNII n0.24:11-21 159- (MIU 13:5)
(Oil field flooding)

0, 1 c
uvrini- ~he o' f' oil 1;
L 1960, 16 ?p
~nFt itute of the Petrochem;,_-ai and Gas Iiiustm i, u lkin) L, 35-`0, 1-24)
cl
zw~

. BURTSEVO 1. 13.
Rat-ovary of oil flooded from a porous medi=. Neft. khoz. 39
no.3:51-54 Mr 161. (MIRA 16:7)
(Oil field flooding)

BURTSEV, I.B.
Flowing oil production in flooding oil from a porous medium under
laboratory conditions. Neft. khoz. 39 no.11:50-55 N 161.
(MIRA 14:12)
(Oil reservoir engineering)

BURTSEV, I.B.,
Experimental investigation of the oil yield and phaSe Dermeabilities in
water drive in a porous media. Izv.vys.ucheb.zav.; neft' i gaz '?
no.4:47-50 164. (MIRA 17:5)
1. Filial Ufimskogo neftyanogo instituta v gorode Oktyabrlskcun.

--BURTSEV, l..B.
Solution of the unidirreinsional problem of flooding putroleiLT. fram.
a porous medikxm. Izv. vys.ucheb.zav.; neft, i Igaz 6 no.11~67-70
163. M RA 17 % 9)
1. Filial Ufimskogo neftyanogo instituta, g. Okty7ibrlskiy, Bashkirskoy
ASSR.

A.P.
Hydraulic resistamce In fluid flow tLirough pipelines. Izv. vys.
ucheb. zav.; neft' i gaz 7 no.5*.-"'5---'S' 164. (IHIRA 17:9)
1. Ufillskly neftyanoy in."Litilt.

TELKOV, A.,--.; ITURTSEV, i.B.
I -
uallculaUng the wat-ories5 porJod cX thc- of c-12
wells with Lottom water. T-zv. vys. lucheb. 2av.; neft' -; gaz
7 no.8:47-52 164. Ourp-, 1.-, :101)
1. Ufjmski-y nelktyanoy invt,itut.

BURTSEV, I.B.; TELKOV, A.P.
--- . A I-
Determining the coefficient of hydraulic
fluid flow in pipelines. Izv. vys. ucheb.
no.3:81-84 165.
resistance in case of
zav.; neft' i gaz 8
(MIRA 18:5)
1. Ufimskiy neftyanoy institut.

BURTSEVY I.F.
The KR-2 coal mining combine. Biul.tekh.-ekcn.inform.Gos.nauch.-
issl.inst.nauch.i takh.inform. no.3:14-16 162. (MIRA 15%5)
(Coal mining machinery)