SCIENTIFIC ABSTRACT RAKINA, V.P. - RAKITIN, G.A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001344110014-2
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: January 3, 2017
• Document Release Date: August 1, 2000
• Sequence Number: 14
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT


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RAKINT, VLAIII-11IR ALEKSX.-DROVICII.

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RAKIPOA, hh, . "ft. , Tro8 hin, Ya. E. and 5 alChz.U_IN.# K. i.

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Y7F-WROV, fe-Je., p-,cfus.-;j:r; I.Ye.;
SNUJi.-NOV, G.T., BOSM;r;, L.V.; ?IRYL7,7"
U.N.; GALITS07, A.P.; GRIGORITIZ7, A.A., a~--demik; ZP-5-Zli-zON, H.S.,
prcf~-Iaacz; MURETOV, N.S.; KHROM07, S.P.1 BWIDANOV, P.N.- LZEEW,
A.N.: SOKOLOV, V.N.; YANISHN7-SKXY, Yu.D.; SAMOYLENKO, V.S.; USYA-
ROV, R.F.; CHUBUKOV, L.A.; TROTSENKO, S.Ta.; VANGENGEYM, !'X.Ta.;
SOKOLOV, l.F.; STYRO, B.I.; TEM01011;~, II.S.; ISAYNT. B.A.; DKITRITW.
A.A.; M&LYUGIN, Ye.k.,-, LIND&U, Ye.K.; SAPOZE211KOVA, S.A.;%4Aw4k-j
POKROVSXAYA, T.V.; RAGDA.SARIA3, A.B.; ORIOTA, V.V.; RU-
Ys.S., prctesscir; MILEVSKIY, V.Yu.; SHCHERBAKOVA, Te.Ta.:
~BOCHKOV, A.P.; AILA.POLISKAYA, L.Ye.; DWIAYWk, A.V., UTESID;7, A.S.;
HUDIUIVA, A.V.; RTJIZITKO, A.I.; ZOLOTARZT, M.A.; IaRSESYAN, A.G.;
MIMYLOV, AeNs; GAVRIWV, V.A,; TSOMAYA, T.I., DEITYATKOVA, A.M.;
ZAVARINA, M.V.; :SHMETER, S.M.; BU]YfKO, K.I,, proftseor.
Diacassiom- of fbe zapor-i', (in the fcrm oll ~whe
State climatclo&1sal' ard m6tl--,;d-:t da'~-'-Cplag InfczZs
nc.3/4.26-'154 154.
(MIRA 8:3),
1. Chlan-kerrespondect, Akad6m14 na-t:k SSSR (11:~' Fed: r'- v 2. Glavmaya
geof izicheskayh obse-.va~%-ziyu -ix. A.I-T:eyk~~--.a (f iar Preltechanskir,
Lebedev, Yanishevskly-,, IsayeT, Rati-L-
shteyn, Budyko, Shchartakwr~L, ALap',--"6kay;-t, L~.!L-Iyeza, Rudce-ia,Gawriliciv
ZavaTina). Ukrainck"y
skV
rext

FEDDROV, Ye.N., pr-Dfetis~;,7; -rlrbDT--bCii:-;!iSK7
~7, P.P.,
Discussio-,- of ~he repc~r'... (.',- tLe 4"-,rx. L:1- the ~!nren,~
a ta to cl I matniv -I cal rag earc-1- and me -.d a ,f I a laf -~ I'M.
4: 2 6 :5 (MIRA 8: 3
aboro GUGMS iwo.) -13 4 4. (Cara 21
4* V,sesoyuzry7 institat, rasteriiev:4st,.7a. (for Ss17azirc~r, R-..idenk,)).
Bioklimaticbeskaya startblya- KIsIcndsk (for B-,shnc). 6. HoAk,-r-
s~iy gosudarstvauW tmiversV-ef ita. M.V.Iomcnc,-q0-ri (for Allsov).
Minlsterstvo putey aoob,~hchenlya SSSR (for Bizryukt~v). B. Irt.3ti-
tiat -Pargrafii Ak-ndemil nauir SSSR (for Gailtsov, G.-Igorlyer). 9. GOO-
fizichealcays komiqelra VeeooyuzrLt3go geografl-cheikogo obahchost-a (f 0.-
19ygen3on). 10, Minl3terst-m i eIektr--,PromyshIenn,-sti
SSSR (f or Kure-007). Ii g . Leningradeki7 gvsud.arsti-Gr-W universitet iz.
A.A.Zhdano-va (for Khromvv). 12. TSen',ra'.,'ry7
okiy arkUl-z (fzr Zzi`ctarev,'). 'A.3 e G,,~-
sudsrstvennv7 okeap-ografichoshI.T ins',Iit;~!', (ftv SBm%-7:!eDk,~)* 114. Wen-
txaI'z*,y instit'.1t pr~,Zaozo7 (I*cr U:3=a-,,-Y, 15. Instit-It,
geografli Akademii =jk SSSR. 'A. TSaLLtx;~".',:-yj- Ir~sI.It-ut. k-lirrr
-led Ir
Chubuk,:,v). 16 Nauchn.. '-s~ -- -qll~ ut Izen' Se:-en-rs,
Yalta (f~r

YEDOROV, Ye.Ye., PREITI-EMNSK."". P.P., A--A
Discussion of the r9port (In the form Qf debate,3) [tJ ttie c-arren'
state of cllmat,,)lngleal researcL and metho-l-s d' de-4elcp Ing it).
(RIBA 8
Inform.abor. GUGMS no.314:26-154 154. (Carl
18. Dallnevostochnyy glrlr(~mateorolcgiche,
zkiy institut (for Sokolov). 4-9. lustitu" geolcogil geograft I Aka-
demll nauk Llto7sklDy S.-*R (for Sty-r--,,). 20, Rost-o-Aoe upravlenio
g1drometsluzhby- (for TemnAn-m). 21. Mcrak~,7 g1drof izl~!lhaskly
tul, Akadem.,.i nauk 33SR (fcr Dmttrlyev). 2'?. Vaeg,~yuznyT Instit,1A
a ALadsmlya na
stenlye7td.3tva (for Entoaskoy S,%
r
(for Lledemaa). 24. Akademiya nauk Army3nrk(,-y SSR (for Bagdasarye
loningradskly giclrometeorologi~heskiy iW,-Iltul; (for Mile7aakiy).
(Continued on next card)

YEDOROV, Tajeol profesisolr; PRIOTECHENSKIY, P.P., find --trers.
Dlacmssion of the itpCor' (in tbs ftim of debatei) [of the 'aurrea". st-ats
cllmatolzgical reseatch and :LsLhcd; oll de7-a'irping It]. lrf,:rm.sl*x,
GUGMS no-3/4-26-154 154. (car"i, 4) (MA 8.'3)
260 Gosudars~~-vennyy gid-rol,%gichaskAy institut (for _Rochkov). 27. Xa-
Lakliskiy nauchac-issisio7atelleldy glclrometG,~r,~lcgicheskly Institut,
(for Uteshev). 28. Upra7leals gidrramets'lluhby- Armyamsk~5y SSE (f-., Ka-~-,w
ses7aa). 29. lent ng-adakV~s uprazlatlya gid-.-zmatsl.u2hty- (for- Mlkh_%j'loT,
Dev7atkova). 30. Tbilisakiy- gosudaystwermyy xiveraitet (for Tqcm&y_A).
31* t3entrallnapi aerol:,gichaskaya obssr--rato:,iya (for Sl=atez,).
(Climatolo&)

111-1-613
Summary translation from: lleferat~,-ri.y~- ZrL=-:jal, Gec, a, I qr~7
g
7.1 USSR)
AUTHOR: Rakipova, L. R.
TITIZ: Effect of Solar Activit-Y -on General Atmospheric Conditions
(Vozdeystviye solneahnoy aktivnos~i na obshchuyu tsir-In.1-
1yatziyu atmosrerj)
PERIODICAL: Tsirkulyar. Astron. observ. Llvovsk, un-ta 105, N*_' 32,
ppo 7-14
ABSTRACT: In order to explain atmospheric variations caused by solar
activity, it is necessaryto study the behavior of high
pressure subtropic. belts during the various solar phases.
This may be achieved by extending the contactme,,.hanism
existing between the various atmospheric layers to general
atmospheric cond-itions,through cyclonic and ant!,,yol 'onic
storms. When solar aotlvity is inez-eased the contaat
mechanism may cause a weakening in the high press"s sub-
tropic belt'; when solar activIty is decreased the retard-
ation,effect does not occur. These are the primary effects.
of the solar activity on general atmospheric conditions.
Card 1/2 The change in atmospheric angular vtlocity connectad with

14-1-613
Effect of Sclar Activity on Gcuneral Atmospheric Conditions. (k"ont.
these phenomena causes secondary effects, such as ohanges
in atmospheric conditions in the critical latitudes and
in the prIncipal frontal zones. The procession of solar
activity.phenomena 1.5 - 3.0 years in advance of the
extreme3 of an 11 year sun spot nycle may probably be
explained by the fact that the numberof sun spoto changes
:only in generai proportionately to the inten3ity of geo-
active formations.in the sun, i.e. flares and high temper-
ature chromospheric eru-ptions -sh i ch produce powe:-f ul ultra-
violet radiation.
A. T.
Card 2/2

Call Nr: QC 901.R3
AUTHOR: .~akipova, Larisa R.
TITLE: Thermal Conditions in the Atmosphere (Teplovoy rezhim
atmosfery)
PUB. DATA: Gidrometeorologicheskoye izdatel'stvo, Leningrad.
1957, 184 pp., 1700 copies
ORIC. AGENCY: None given*
EDITORS: Responsible Editor: Shekhter, F.N.; Editor:
Yasnogorodakays, N.M.; Tech. Ed.: Shumikhin, K.F.;
Correctors: 14amedova, V.V., andiftnts, S.A.
PftPOSE: This monograph is designed forscientific workers,,
physicists, mateorologists,.'climatologists, as well as
f or aspimnta and seniorstudents in hydrowteorolo&Lcal
institutes and geography and physics faculties of
universities,
Card 1/4

Call Nr: QC 901.R3
Thermal Conditions in the Atmosphpre (Cont..)
COVERAGE: The book covers the results of experimental and
theoretical studLeb in the common tendencies of thezual
conditions in the atmosphere in a basic investigation
of totil and:zonal 'atmospheric fields. It includes con-
sideration and analysis of the horizontal macro-transfer
(o derly and turbulent) of heat In-basic types of
r
climate. Modern concepts of thermal condition Ln~the
stratotphere and the relationshtp between the upper
layers of the atmosphere and the troposphere are covered
in detail. The annotation says that the mathematical part
of-~the'study,may be omitted by thi general reader.
Personalities'mentioned are! Kondrat'yev, Y.Ya.'
Shvets, M.Ye. and Yudin, M.I. There are 86 bibliographic
referencei, 41 of which are USSR, 28 English,
14 German, I French, 1 Chinese,and I Indian.
Card 2/4

Call Nr: QC 901.R3
Thermal Conditions in the Atmosphere (Cont.)
Ch. U. Zonal Thermal Field of the Atmosphere 85
Formulation of.the,problem and of its solution for
zonal'and non-zonal temperature distribution.in the
atmosphere 85
Selection of numerical,parameter values 105
Computation of the zonal distribution of temperature
and components ofthermal conditions in the
atmosphere. Analysis of results 119
Ch. 111. Thermal Advection in the Atmosphere. 139
Integral characteristics of thermal advection 139
Computing components of regulated advection.
Evaluating horizontal turbulent heat transfer 145
.Bibliography: 181
__-AMAILABLE.- Libr&ry.of Congress
!"M
=mum

124-58-9-10096
Transldtion frorn: Referativnyy zhurnal, Mekhanika, 1,958, Nr 9. p 96 (USSR)
AUTHOR:, Rakipova, L. P,
TITLE: i,h-e n ce of the Corpuscular Streams. on the High-attitude
Perturbations in the Atmosphere (VIiyaniye korpu5kulyarnykh
potokov ria dinamiche kiye vozm,i!;hcheniya v verkhney atmos-
fere)
PERIODICAL: V st). Fiz. solnechn. korpuskulyarn. I pot.okov i ikh vozdey-
stviye na verklinyuyu atmosferu Zemli. Moscow, AN SSSR,'957.
pp 273-91-75. dhsku_s. pp 275-276
ABSTRACT: Bibliogriphic entry
L. Atmsphere--Physichl properLier.
Card 1/1

AUTHOR: RakiP,)va, L. R. SOV/50-58-11-16/25
TITLE: Inve--ti-ation of the Transfer of the Moment of Motiai.
in the Atmosphere (Issledovaniya perenosa momenta kolichestva
dvizheniya v atmosfere)
PERIODICAL: MeteoroloCiya i gidrologiya, 1918, Ur 11, PP 56-61 (ussn)
ABSTRACT. In the last years special attention has been devoted abroad to
CP-rd I/ f4
the moment of motion was refuted in 1921 when A,, Defant
the study of the transfer of some physical characteristics of
the atmosphere (motion, whirlwinds,,temperalture, humidity, etc).
Many paper dealt with the aforesaid problem: on the one hand#
they are a contribution to the solution of the fundamental
problem of meteorology - the establishment of a proper theory of
general atmospheric circulution, on the other hand, a problem
of merely applied meteorology is discussed in them, i.e. the
devising of some ner methods of wind-area forecasts. The abso-
lute nature of the older view-- of the law of maintenance of
proved on the basis of the theory of turbulence that whirl-
winds of a diameter of about 1,000 km in the area of a hori-
zontal wind must manage a merldional transfer of temperature-
Therefore the question was raised whether a large-area

Investigation of the Transfer of the Moment of Motion S071/5-0-58-11-1 ;'2r
in the Atmosphere
turbulence of the atmosphere plays an important part in the
processe3oftotal circulation, Then e. 11, Blinova (Ref 1)
and IV Ye~ Kochin established by theoretical investigations
the rational prin--ilAes of the quantitative theory of total
atmospheric circulation: in the case of a given temperature
distribution in hydrodynamic equations also the turbulent
viscosity is.taken into account in addition to the forces of
the baric gradient and the force.of coriolis, Before dealing.
with,the papers explaining the mechanism,of large-area trans-
fer in the at-mosphere, the author initiates the reader in the
values of the deviation of meridional distribution of the
zonal wind on the level of the strongest winds (300-200 mb)
from the theoretical distribution which is determined by the
condition of the constant of the angular momentum I (Ref 39)-.
-Figure I shows the theoretical and observed winds of vario"
latitudes, Ground friction is the main mechanism which changes
the, angular momentum of various atmospheric zones4 Within the
trade-wind zone an unintnrrupted current of the an6-ular momen-
tum from low latitudes flows from the earth's surface in the.
Card 2/4 direction of the atmosphere. In order to obtain the balance

Investigation of' the Transfer of' the Moment of ;Motion 3OVhD-58-11-18/25
in the Atmosphere
of the an,-,ular momentum of the total atmosphere, the excess of
the molnf-ntum (from the low latitudes) must be returned to the
eartb's surface. Within temperate latitudes this occ uro in the
--one of,westerlies where the angular momentum flows off,. Since
the wind systems herein are not destroyed withinvarious lati-
ru -
Uudeu, there must be a horizontal current of theabsolute ang
lar momentum that flows from the tropic to higher latitudes
(Ref,.11)" The current of the anGular momentum through a certain
latitqde may take place in form.of 1) a turbulent transfer
exanange of masses of the same size which possess different
angular momenta.due to cyclones and anticyclones; 2) an order-
ly transfer of 'air masses with occurs in lower atmospheric
strata toward the equator and in upper strata toward the
pole due to a mean meridional circulation, In the last years
many scientists tried tc confirm the theory,of horizontal
turbulent mixture aco-ording to Rossby (Refs 35-36). The theo-
retical assumption of a mean meridional circulation in the
-subtropics makes it possibile to drar a very satisfactory balan-
:ce of the anm,,ltr momentum for the range of jet circulation.
Card 3/4 Riehl (Refs 39,40) arrives at th,~ conclusion (Fic 3) that, i r,

Invest ii_;-at ion of' the Transfer of the Moment off 5-3- 11 -1812
in the Atmosphere
winter the mean iell circulation is caused by th-~, common effect.
of -turbulent mixture and meridional circulation, The importancei
of the turbulent transfer increases with higher latitudes, On
the basis of various in'7eStigations Palmen (Ref 30) 3Uggested
a workin6, scheme of total circulation in the troposphere con-
siqzing of two cl-,.%sed meridional circles (Fig 4), In conne-~tion
with modern views of' total circulation the problem of the
fransformat-~vn of the energy of disorderly turbulent,large-
P - - - - - - - 4- V--

3(8) PHASE I BOOK MIPLOITATION SQV/2270
Glavnaya geofIzIcheskaya observatoriya
Voprosy ainoptichoskoy kllmatologil (FroblerA In Synopt1cCl1mato-
logy) Loningrad, Oldrometeoizdat, 1959. 105 P., (Seriess Its:
Trudy, v7p. 7) 1,100 copies printed.
Sponsoring Agency: Glavnoye upravleniye gidrometerologichookoy
sluzhby prI Sovete Ministrov SSSR.,
Ed. (Title page): T.V. Pokrovskaya,lCandidate of Geographical Sci-
ences; Ed. (Inside book): T.,V..Ushakova; Tech. Ed.: A. N.
Sergeyev.
PURPOSE: This Issue of the Observatory's,Traneactlone Is Intended for
meteorologists and climatologists.
COVERAGE: The authors are primarily concerned with the possi-
bility of using various monthly characterlsties of atmospheric
circulation In forecasting monthly Air temperature anomalies.
Card 1/3

Problems in Synoptic Climatology) SOV/2270
One of the articles.discusses~the inertia,of the temperature and,
its utilization In forecasting. Other articles are concerned
with the effects of solar activity on atmospheric circulation.
The last article Is devoted to the probability of cyclical regional
distribution of mean negative diurnal temperatures,, offering also
a synoptic and climatological analysis of the results obtained.
References accompany each article.
TABLE OF CONTENTS:
Pokrovskaya, T.V. Application of the Multi ple Correlation Method
to the Qualitative Rules of Long Range Weather For*casting
Voroblyeva, Ye.V. Forecasting the Sign (Negative or Positive] of
Mean Monthly Air Temperature Anomalies In the Southeastern Part
of European USSR 10
SpIrIna, L.P. Possibility of Forecasting the Inertial Monthly
Air Temperature Anomalies 32
Rakipova, L.R. Effect of Solar Activity an the General Atmos-
'-phii-ri~F- Cij~-diilat ion 40
Card-2/3

PHASE I BOOK EXPWITATIO.N S,71/4174
SOV/2-S-99
a ofizicheakaya observatorlys,
Leningrad. Glavnay ge
Voprosy chislennogo Irognoza.i teorii klimata, (Problems inIfuserical Weather
Forecasting and climatology)., r.,eningrad, Gidrameteoizdat, 19W. 129 P-
(Series: Its. Trudy, vyp. 99) Errata slip inserted. 1,000 copies printed.
Additional Sponsoring Agency: USSR. Glavnoye upravleniye gidrmeteorologicheskay
sluzhby,
Edso: M.Ye. Shvets, Do--tor of Playsice wAMathematicsp and M*I* Yudin, Doctor of.,
Physics and Mathematics; Ed. (inside book): T.V. Ushakova; Teche Ed.; N.V.
Volkove
PURPOSE: The publication is intended for specialists in the field of dynestle
synoptic meteorology and climatology,.as vell as for graduate students In
these fieldse
COVERAGE: This is a collection of 11 articles published as No., 99 of the Trans-
actions of the Main Geophysical Observatory intni. A.I. Voyeykov and dealing
Card

Problems in Numeri cal, Weather (cont.) SOV/4174
with new methods of numerical analysis prognosis. Individual articles an con-
cerned with contiguous problems of climatology: temperature anamalles in the
atmosphere, effeat of the heat of condensation on pressure changesp numerical
prognosis of.the pressure pattern affected byLorognphic factors,and the hydro-
dynamic theory.of frontal cyclogenesis. References accompany each article.
TABLE OF CONTEIITS:
Rakipova. L.R. Formation of the Mean Monthly Anomalies of Atmospheric
Kagany R.L, Calculating the Effect of the Condensation Heat Flow and of
-the Stratosphere on Change in the Pressure Pattern 15
Bdgdanova., N.P. Approximative Evaluation of the Effect-of Heat Released
by Condensation on the Change in Pressure Pattern Near the Ground 37-
W Sia-yuanl. Precise System of Calculating the Irregularities of
the Earth's irt 'TwiLerical Methods- of Forecac-ting 43
Card 2/k~~-
---------------

0/733/60/000/003-4/006/012
6
"WHO: Riikipo,.a, L.R.
'11,2 #--'f,!ct of unlar a tivity on the gene atmoupheric circulation
Lvov. Univt!n-itet. Astronomicheskiy sbornik, no. 3-4, 1Q,60, 102-108
41--.X7: The thi!orvitical of interactidn'mechanism between the vurioun
larcr-- Orl-~'.('-: powl, I rudy GGO no 28, 1951) shrws that enhanced
R.
in c-re,%3 n V.t-- baric 7rad.lents between~
-oAnr nct . vi ty, cyclones and anticyclcne3,
C13Ult-, in a co:~Ivarntivcly, !rort! d,~ v; i I a:,,, ed cycionic activity in the atmosphere. Jince
t~-,e authcr, conzidf-ru cyclonic an;.* a-.ticycloniic activi-ty to be of primary sirnificance
in tllhf~ tr~-ni of Vl~ r-.-w3rall circulation, it follow-a that enhanced 391ar
activity le,,W3 to wi incrcano~ llr. tl.,-~, intensity of the general circulation and, mainly,
in tho interlatitude #~xchn.-~-c or air lasses. There is 1 table.
T I 'civ. ry
Glavnnya reo:i'71 :;knya obserratoriya (Main Geophysical Observato
Card I'll

R
r
AFIIUVA, L. R. ; 3! HNEY Eli)V, -5. Y

. - ,.;, V 1; 1, -.1, . -.11 t; -;', !- -Y~. 'l- ~~ . , - --- - - -

T4y- A Y70 13 7 1-1. 9
SOURCE CODE: Uti/0050/66/000/001/0035/0037
AUTHOR: Rakipova, L. R. (Doctor of physiconathenatical sciences)
ORGI Main Geophysical Observatory (Glnvnnya geofizicheskaya observatorlya)
TITIXI Interaction between the upper and lower layers of the atmosphere
SOURCEI Meteorologlya I Sidrolo.-iya, no. 1. 1966, 35-37
TOPIC TAGS: upper atmosphere, troposphere, stratocphor*g atmospheric
c1rcutntion, solar activity, atmospheric turbulence$ atmospheric$
thermodynani cs
SUB. CODE: 04
esults'of he problem of
MSTR,~M The author preients the r solution of t
the influence of perturbation3 in the upper layers of the atmosphere
on the circulation of the troposphere. A definite region# the polar
areat is considered, and also a dofinito synoptiC situation; :the
spring reorganization of circulation in tho upper layers of the atmos-
phore, and also sudden stratospheric warmings. In the spring reorgani-
zation of circulation under tho influence of radiation heat fluxes
there is a replacement of winter cyclonic circulation by mirmer anti-
cyclonic circulation, At the time of stratospheric warnings there is
Card 1/2
UDC~J,551.513

ACC NR: A F? 0 1) 72 9
a stmilar reorganization' of circulation. The hypotheses proposed .17or
explainingthis phenomenon (advactive,, circulatory, etc.) are inade-
quato because rocket soundings in recent years have sho-.,m that wa.-m-
ings also involve the upper stratosphere and mesosphere. One-, three-
and four-layor models of the problea are considered& The conclusion
drw.n on the banis of the analysis and computations in this paper is
that the initial state of circulation in the considered problem in the
entire layer of the atmosphqre is dependenton heat.fluxes in th,6- -
lippeyjatma~.sphe.rP and solar acti~ty. Grig. art. has: 3 f Igures and 6
fomulas, 01FIRS: 34,59Y

A,-rIc Sc'
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pral, zc t conditirm3 Of sot~~rn

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s/i9b/62/000/oo6/ooq/oId
AUTIIOR: R
TITLL: A new 2800 2XIIJ regional power station
PkRIODICAL: Reterativnyy zhurnal, Licktroteklinika i energetika,
no.6, 1962. 21-22, cibstract 6 G1626 (Eicktr.
no.8, 1961, 6-13),
TLXT. in 196.L, construct ion wa sc omme nc e din the Central
Industrial Aie-jon of the USSR of a power station with an output
of 2400-2800 MW burning natural ,as with fuel,oil as a standby.
The first section of the power station, with in oLrtput of 1200 INU
will be equipped with turbo-generator units type k~',-300-240
(K-300--240) of the LM nd single pass boilers.of 950 tons per
'Z a
hour of stca*ci at 255 atm, and 585/570.0C, wade by the Works
3. Meni Ordzhonikidze, arid will be started up by 1965. Latero
units of 600 or 800 jnIW will be installed. The boilers are of the
two-frame type with inverted-U interconnection. The heating
surfaces are cleaned by shot-blasting and magnesite additive is
also used.~ The boiler efficiency is 9h4,(o for gas firing, and
92.85. for fuel oil. The corresponding flue gas temperatures are
Card 1/3

~S/196/62/000/006/009/01~
A new 20oo region. il. power station
133 and Vto OC. Deaerators are included in the thermal circuit
(a deacrating section is also provided in thecondenser). There
is no cross-connectio'n between units. The feed equipment
consists of one mainturbine-driven pump for full boiler rating,
one reserve electric pump for half boiler rating, and three drain
pumps rated at 16 atm head which deliver water from the
deaerators to the feed pump.. The high pressure feed is connccted'
to the higb pressure side of the -pump. To provide heat for space
heating, ventilation and hot water su Ipply the first three units
will.have indirect water heaters with an output of 15 (.1cal/hour
(one set is a standby). For the power station auxilliaries the
station-has two pressi.ire-reducing and de-superheating units,,
a m ir
each rated at 40/20 atin and,80 tons per hour. The ste, ains
for primary and reheat steant are made of pearlitic steel. The
main building is made of prefabricated reinforced concrete with
up to 6j~,'4 prefabrication. The turbo-alternators are installed
across the machine room, the span of which is,45 i:ietres.
'W sets-is 118 metres. It is
Spacing between centres of the 300 M
proposed to make the turbo-generator foundations and the omo4e
Card 2/3,

A new 2600 Did regional power station S/iq6/62/OOo/006/ooq/oIb
E1911/E134
stacks oil prefabricated reinforced concrete. The height of the
stacks is lbo fr. I.-later is supplied from a reservoir using a
direct flow circuit (with partial return if,water supply is
inadequa te It is proposed to start up the units by varying
stean, conditions; the turbine is run up to speed and loaded
Whils-t htd--~arl: is beinx raised in the boiler. The heat rate for
the 3(-)0 XV 2st"tS is 1630 kcal/k,",q).
~Abstracttjrfos rju t Complete. tram-sla Lion.
Card 3/3

167T22

M
- ---, -, ~. "I -. -I.."-..

ItAXITINi A i j ft dol

ii

Some Mineralogical an'. nemical
limits (in weight-percent): Si02 52-30--65-45; Al,,I03,9.20-14-35;
CaO 3.25--9-45; M90 .1-37--2.65- Fe 0 1.1--8-73; -K20 + 14a 0 1.45
2 3 2
---2.62- 10 0 23 2 The la
.45 c ys contain the followina minerals:
h - A -- a .1
ydromica ydrogoethite, quartz, calcite, do'omite, kaolinite,
nontronite and montmorillo.nit.e. The clays have,a rt~latively low
capacity for increase in volume, which is exi.laint--d by the mineral-
Ogical composition of the fine fractions.
Card 2/2 N., P. -Yeremeyev

ACCESSION NR; APS006022 9/0065/65/000/002/0033/0040
A~THOR.*: Vasserman, L. K.; Rakitin A. M.; Grinchishin, B. I#
TITLE: Automation of the process of compounding oils and its economic effectfive~
nsss
liv i masel, no. 2- 1965, 38-40
SOURCE:~ Khimiya i tekhnologiya, top
-1T0,PIC:TAGS: automation, oil,' petroleum, petroleum industry
ABSTi'.ACT: The Volpgrad Branch of the Special Design Office of the Academy of
Petzileura Sciences.togetber with the Volgograd Petroleum,Products Plant developed
cess 0
and tested under industrial conditions a plan for the automation of the pro
7-
- compounding oils (see 1ig. I of the.Enclosure) which provides for the automatic
regulation of the delivery of thecomponents and additive.' 'A diaphragm mixer was
used to achieve effective mixing of the components and complete diss'olution of the
additive. Before goin to the diaphragm mixer the oil is heated in an ordinary heat
9
exchanger. Dur,in'g the mixing process, samples of the oil mixture were taken at
hour and were checked for viscosity at a temperature:of 1000C. The
intervals of one
results of the tests showed that the system provides for consistent maintenance of

JM "Olmw
4 -
00-
09.4
Investleatlom of Gemstlemair neleum Pbses by the Method of so
'00
of Proportional Cmaters (haledeveale gemeticheaki evissanygM tolchkov
ustodom proportaloselloWk1h sabetehikov) by D SAItIn and G Steatkow
'90
2634" (1%8) -July 11' (In Russian) -00
00
The *x1stonce of damme streammi of mom-lonising particles producing -00
01MIUmmome nuclear disintegratio ms was diseamered Is the commle
radiation by Dabrotla ad TWr11m NO. 5
In the present we* this N I we@ studied at a
090
3860 m altltvd* wlfsb the a1A of a telssmore of four g rom re of
proportional eounters. The ealseldenoes ocepared were 1, 2, 3, 4
and 1, 2, 4. It was fbmd that In about 213 of all cases dischoirges
In 1, 2, A ware mot secoupenled by a discharge In 3. Various devices
alblitty
and modifications is the experimental sot up excluded the pes -90
of attributing the oboes I go -mom to the following spoW 1*9
extensive atmosiberle shows", narrow showers of relativistic ~300
particles with possible loalsettom fluctuations, strongly loalsing
maeone,
partIleas generated thftvgh miaelear, d1einterrations,. healk
olestrome or phe
wa that the particles
tome, It-wer.sho
,
-
1#6040 ;47
1 salacp .10 a.. oft A A 51 *W 0.. it.
1KX
U is oOU L51i 44 IN
I
OWQ
al
0 01 00 0 0 0 9
0 0

USSR/Fhysics Cosmic Rays
"Transitional Effect of Density in Flectron-Nuclear Showers," 14. 1. Podgoretskiy,
A. 1. Parchukov, D. F. Rakitin, Phys Inst lermi Lebedev, Acad Sci USSR
"Dok, Ak Nauk 555101 Vol L)D,.III No 4, pp 685-6-P8
Reveals "Transitional effect of Density". Appezrence of difference ~I~etween (a) the pro,
ability q2 of recording simultaneous creation of 2 showers fenerated by P particles
formed in previous shower and (b) the sum of the probabilities (2qI 'of recordirg 2
successive acts of shower fromation created by these 2 particles biat separately. Thi s
effect has also been considered by fl. C. Birger, V. 1. V-aksler, N. a. Dobrotill,
G. 1. Zatsepin, L. V. Kurnosova, A. L. Lyubimov, 1. L. Pozentall, and L. Kh. Eydus
(see "Zhur ~,'-ksper i Teoret Fiz" No 19, 826, 1949). Submitted 3 Jun 50 by. Acad C. V.
Skobelltsyn.
1761oh

S/120/62/000/001/ooh/061
E032/E514
AUTHORS: Devishev, %I.J., Rakitin, D.F. and 11yabikov, S.V.
TITLE: Some fe,
atures of particle track photography in
n1leoll
.connection with the.simult, measurement.of
momentum and ionization in large Wilson chambers
PE'RIODICAL: Pribory i tekhnika eksperimenta, no.i, 1962, 28-~32
TEXT; It is pointed out that the photography of Wilson
chamber tracks in the, GeV region leads to specific difficulties
and the a im of the present paper was to investigate the
possibili ties of tile drop-count method and to select the
optimum photographic systems for use with large Wilson chambers.
rhe experimental part of the work was carried.out with a
rectangular Wilson chamber (60 x 20 x 30 cm3),and a control'system
~Arhich selected relativistic ji-mesons travelling in the vertical
direcItion. Each track was photographed with two objectives on a
photographic film with a resolution of 90-100 lines/mm. The
chamber, was filled with a 1:8 argon-helium mixture to a total
pressure of 2.5 atm and a 1:4 alco~ol-water tqixture. Tile,
calculated drop (tensity was 28 cm- A determination was made of;
Card 1/2

Some features of. particle track s/l_n0/62/000/001/0(A/()6J
E032/E514-
-1) tile resolution of tile system, b), the dependence of tile rep4olu-
tion of drop images oil the magnification, C) depth of focus,
d) effect of under-development of the f-ilm, and e) specific
iorlisation. It is concluded that with a track widti, or atiout
_2 mm the Ionization density can be increased to 39 drops/cm or
more,since a reduction in the statistical error (foes not lead to
ncrease in tile error due to overlap so long as tile drops can
still be counted. Under these conditions tile simultaneous
measurement of momentum and ionization by the drop-count method
can be carried out up to a magnification ratio of about 10. With
Soviet objectives and films the minimum diameter ofdrop images
turns out to be 21-30~1,l. This may be reduced-to 20 g by under-
development. There are If figures.
ASSOCIATIONt. Fizicheskly institut AN SSSR
(Phynics Institute AS USSR)
SUBMIT'rED: May 20, ig6i
Card 2/2.

m

vi

RAUTIN, G. (g.Turln, italiya)

IDSPICHILE, Andrey Vasil'yevich; TERENTIYEV, Nikolay Konaantinovich;
TYUHIKOV, Aleksandr Ivanovich; RkITTIV-4G.A., retsenzent; 02EVIBLOVSM,
Ch.S., retsenzen-t; SHCF-%MBACFXVICH, G.S., retsenzent; XUSUOV.P.I., re-
tsenzent; SHIMINI.P.M., retsenzent; MO=,N.P.., retsenzent;
RESHMIIKOV, V.Yep retsenzent; PESKOVA,L.N.,red.; ZHDANOV..,P.A,,qred,;
MTROV, P.A., tekhn. red.
[Safety engineering arA industrial sanitation in railroad transportation;
handbook]Tekhnika bezopasnosti i proizvodstvennala sanitarila na zhelezno-~'
dorozhnom transporte; spravocbnaia kniga. Pod obshchei red. P.A.Zhdanova
Moskvap Vses.izdatellskcpoligr.ob"edinenle M--va putei soobshcheniia
1961., 455 p. MU 14:12~
(RA]ILROAD--SAFETY MEASURES) (jai LHOADS--SAN ITAT 1011)

im
BARANOV, L.A.: GORBATOV, V.I.; YXMINOV, D.V.-, TERKAKOV, Ya.I.:
PITERMOV, N.I.; RYLIVOV, A.U.; RYA=11TM, K.G.; TOROPOV, A.S.;
TSMLIN, G.1.;.TAROSUV,D.M., TRUBIN, V.A.. glmmy7 red.;
GRINITICK.
SOSHIN, A.Y., zom.glavnogo red.; RAKITIN, G.A., red..
G.B., red.; TEPIFANOVj S.P., red.-, UBUFWTTW, I.A., red.; KHOKRLOT.
B.A., red ; ZIMIN, P.A., red.; TABUINA. K.A., red.izd-va;
m-no, L:M.. tekhn.red.
(Manual on.accident pr6vention and industrial sanitation during
constr-action and repair operations] Sprovochnoe posobie po tekhnike
bazopsanosti I promsonitarii pri proirvodstve stroltellno-montash-
nykh robot. Pod red. G.A.Rakitins. Xoskva, Gos.izd-vo lit-ry po
stroit.. arkhit. I stroit.mterialemo 1961. 359~p-
(MIRA 14:4)
1. Akodemiya stroitellstva i arkhitektury SSSR. Institut orgeni-
za.teii. makhanizatsil i tekhnicheskoy pomoshchi stroital'stvue
(Construction industry-Hyglenic aspbets)

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