SCIENTIFIC ABSTRACT SHMERLING, ZH.G. - SHMIDOV, F.I.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001549730011-0
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 23, 2000
• Sequence Number: 11
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

39233
S/218/62/027/003/005/005
1018/1218
AUTHOR: Shmerling. Zh. G. and Bass, 1. A.
TITLE: Amino acid activating enzymes and transfer-rna in Escherichia coli
PERIODICAL: Biokhimiya, v. 27, no. 3, 1962, 502-511
TEXT: The problem is whether E. coli cells infected with T, phage retaiti their amino acid activating en-
zymes and the transfer-RNA or whether the s-RNA formed prior to phage infection is capable of binding
the activated amino acids. In the experiments, lysates of E. coli spheroplasti were used. Amino acid activation
was ascertained by the hydroxamate formed. s-RNA activity was determined by the use of labelled amino
acid and isolation of s-RNA-amino acid complex. It was shown that duing phage infection, the enzymes
%khich catalyze the formation of amino acyl-adenylates are fully active, i e. they are not affected by phage
infection. The activity of enzymes catalyzing the transfer of activated amino acids to s-RNA as well as the
activity of s-RNA (the capacity to bind amino acids) are not affected by infection with T.) phage. The
authors conclude that in the synthesis of phage protein participate an-Lino . cid activating enzymes and s-RNA
of E. coli formed prior to phage infection. There are 3 tables and 2 figures.
ASSOCIATION: Institut atomoni e'nergii im. 1. V. Kurchatova Akaderiii nauk SSSR, Moscow (Institute
of Atomic Energy im. 1. V. Kurchatov. Academy of Siences USSR)
SUBMITTED- December 7, 1961
Card 1/1

il- L(, -Ull,-- -; i, Y
.-, i o i . ;~' I ri u . I :

SOURCE CODEt U
795/059/001/0033/0056
AUTHOR: Shmerling, Zh. G. (Moscow)
..ORG, none
TITLE: Heterc-seneity of DRA'and its biological significance
(0
SOURCE: Uspekhi sovremennoy biologii, ve 59, no. 1. 1965, 33-56
TOPIC TAGS* DNA, genetics, RNA, protein, biologic metabolism, chertdcal composition
ABSTRACT: The current view of the metabolic stability'and fun'c-
-tional homogeneity of,DIJA In cells except at the time of repli-
cation of chromosomes is not supported by recent experimental
data. These data indicate that there are.functional differences
In Intracellular DNA. One may differentiate between two types of
DNA molecules: those of DNA with genetic activi-;y that is capable
of transmitting genetic Information and those of DNA with metabo-
.,.L-lc actIvIty, i.e., of DNA that synthesizes the Anformation RNA
svihiah effects the synthesis of specific pro-Ceins and determines
thcIr structure, In the majority r-.' cases both '..'unctions are
carried out by the same DNA molecules, but In some specific casesi
.the t"o types of DNA are distinct. No correlation between this
Card

2/-;r-1-1-4~
ACC NR. AP6015548
ioahomoge:io I ty of DNA and Its observed physico-cliemical-and chem-i
hetcrogeneity has yet been established, but the fact that
Is a heterogeneity of DNA 'i-iith respect to 'biological func-
...I
~_4ons, physical properties, and chemical composition (in some
cases possibly only-because of differences In the degre6 of poly-,
merization) ic demonstrated by many experimental resulta. The DRA
po.lym.crization tests were carried out b~ 0. B. Astaurova. Orig. art. has: 2 filrares
5Pk_S7
-SUB CODE: o6, 07
/ SUB14 DATE: none / ORIG REF: 032 / OTH REFt 115

SH~RR'nSTM, -S.A. (L'vov)
Use of 71-1 readily fusible porcelain mterIal for the
of crowns.. StoTnatologlia 38 no.5:71 S-0 1!9. (MIR-k 13:3)
(DMISTRT-CERAMICS)

Sll~~V'R, S., karid. fiziko-m%tEm. nauk
Jet streamS and aviation. Fryl. ro--. lo' no.Y.-2P-29
o 165. (M!---A 18: 12)

SHM--,TBR, S.M.
Chlorine content in the water of clouds in connection with their
microstructure. Trudy TSAO no.9:3-6o '52. (MIRA 11:6)
(Chlorine) (CloudE)

SI-ME,TER, S.M. (Editor)
flarious Procedural 13roolems of Aerologiral Measurements7, Trudy Tsentrall n
Aerologicheskoy 0.)servator-ii (Works of the Central Aer6logical Observatory),
No 12, 1953, Leningrad (ETiTtor: S.14. Shmeter, Candidate of Physicomathematical
Sciences).

SHNETER, S.M., POIMOVSKIY, V.N.
Influence of the density of air on the readingi3 of fan anemometers.
Trudy TSAO no.12:18-26 ' 53. (MIRA 12t1)
(Anemometer)

ETER S. /v1.
'FE-DOROV, Yeja., profasa-; PREDTECHENSKII', P.P.; EUCHINSKIL LY'ro.;
SEYANINGV, G.T., BOSHM, L.V.; ALT-SOT, B.P.; PIRYUKOV,,
N.N.: GALITSOV, A.P.; GRIGORIYET, A.A., ak--demi-k; BYGERSON, M.S.,
MURET07, N.S.; KHROMOT, S.F.; BOGDANOV, P.N.; LEM:DKY-,
A.N.: SOKOLOV, V.N.; YANISEWISKIY, ru,D.; SAMOYLEITKO, V.S.; USMA-
NOV, R.F.; CHUBUKOV, L.A.; TROT.59NKO, S.Y--I~, VANGENGEYM, G.U.;
SOKOLOV, I-F.; SMO, B.I.; TEIW-KCj'Tv;,, N.S.; !SAYET, E.A.; DMITRIYEV9
A.A., M~UYUGIN, Ye..A.-, LINM4AA, Ye.K.-, -R&FOUNIKOVA, S~A.; RAKIPO-
VA, L.R.; POKROVS.ISAYA, T.V.; BAG-DA.-SARYA3, A.B.; ORLOVA, V.V.; RU-
BINSHTEYN, U.S., prrifea~~-~:c~; MIT-EVSKIT, V.Y-a.; SHCHERBAKOVA, Yeja.;
BOCHKOV, A.P.; ANAPOLISKAYA, Me.; ILTI-JAYEVA, A.V..- UTESHEY, A.S.;
RUDN9VA, A.V.; RTJIEITKC, A.I.; ZOLOWK7, M.A., NERSE-SYAN, A.G.,
MIMYII)V, A.N.; GAVRI-LOV, V.A.; TSOMAYL, T.I.; DLPYATKOVA, A~M.;
ZAVAR-INA, M.V., SHMETM, -S.M.*, BUDYKO, K.I., prcfessor.
Dis~~-uz3to:a ~;f i-LaS ".-kn the f~.Ym of
stale arA rxrh---d-A Infcrzo
sb--r.GUGHS na.3 (MIRA 8:3)
Almiamli r-auk SSSR (f.,r, F6d,-. 2. Gia-ms5,
r
gecfizicfteska5-~. Lm. A.I.TI-sykt~;-a Pradtechanski7,
Leabeds-v, Yanishevskiy-, isaye-, OZ-137a, Rubir~-
shteyn, BLdyk..?. Sh--h6TTbako-;-a , jkvaprI7skay-z., Du--ay-e-.a, Rvdneva,Gamri-iov,
Zavarin-L). Ula-aiask...y gidrometeorologiche-
sk-17
'Cm
t - -1-Jr-o-ed .-;m r-ex' card)

YEWROV, Ys.Yz;., pr,~fess.;7~.- PREDT-ECHENSKITT. P.P.,, a-~.a
Diac-,zss-lo,-- of f*116 rSPCT;~, "he f-%rm of Eof the cu-nvin`l-
ataLs and met~--.da )f de-:-;3l' It]. Inf;:;i;m.
sbc-r. GTnMS (Carli NIRA 8-3)
4. -,?t!-niev:~ st~ia (for Selyaninov, Rudenk,~,).
-d
5. Kls-icv~~dGic (for
ski - goaudarstz-ann;q, jzzjgerslt8i. 1m. ~I.V.1omoncao7a (fc,-:- A-*Iao,91).
y L - -
Minmisters~q~c, putry soot.Lhnhenlya SSSR (for 8. Inall-
tut ge:,&iafii Ak-ademii nai-JL -SSSR (for Gailtsov, 9. Geo-
fizichaskay-a kcmisslpa Vssso3uzncgo geograficheskogo obahchestva (fcr
Eygensor-). 10. Minllatevstr-,~: i slektr.,)promyshlennc-slU
SSSR (for Muret--r). leninomdtki7 gposudarat~vennY7 universitet im.
A.A.Zhdano-Ta (for .12. TSdatralInyy
Skiy arkhl- (fc.:, Zolc-lvarev). !_-,. Gr,-
sucla.r.i'r-irenn;F.w iualit7x~, (for Samcylenkc.). l4r. TSen-
trallwy (fc..r Uaaa-n--:,-Y, Sap-l',Yhalk-,-,-;-a). 15. Inatitut
geografili AkEulemii nwA SSSR I TSra-%s-.."l tt-~Ntj- instltu~ kuyori-~jlcgll (fvr
Chabuk~,-T) . 16. inst."out imen!
Yalt~L (f:~r TxrJsaLk~,). --'7.
nE:x~-. caz,,~~\

FEDOROV, Ye.Ya., PREDT-ECHENSK7'j, P.P,,, -m-nd
Discussi!:t. cl ~-he (In the f~,,,mm --f f-A-F -~iie c-ar-ren~,
state r4f resew-ch --.,2.-,! cil de-,,ed-~- ng i Al
.L- ~pi - .-, .
I mf c rm . sbor . GUGNS no . _3 (MBA 8:3
18. Dallnevostv--h,~,y7 gidzr-~meteorologichs-
sld.Y- imstit-ut (for lq~ Irist.It-a'I i geogTafil AX-.-
demii nauk Lltriv-sk..i7 SSR (P~-,-, Sty-t.-)~ 120~ Rr;si~~.-3k-oe u;~--avlenie
gidrometaluzhbjr Ui~r Ternik--a). 21. Morzkf.~y gidrofiz!sha2-Aiy Inati-
tut Akadamii nauk- SSSR (fc:r Dvll~rl'yrsq). vseszoyus-~:v itnatitut
rastenlyGv-cd3,~--.a (for Malyugin). 23. Akadc-miya nauk Estonskoy SSR
(for Liedemaa). 24. Akademiya n--uk AM-Emok-o-y' SSR (f,~r Bagdasary-an).
25. Leningri-Askiy gldrometeorol-ogi~~heakiy InBldtul; (for Mile-rakiy.).
(Continued on next caiA)

YEDOROV, Ye.Ye., profesicr; PMTECHENSKIY, P-P,,, nnd Cltheni.
Discussion of the repor:, (it the fcIrm Df debateE)' lof the ---jz-rent atat-s
climatological research and dF of d6---6iplng it]. lnfcrm.sb~~r.
GUGMS no." 14- 26
If -154 194. (14ISA 8:3)
26. Goaudarst-7ennyy gidrologichesldy instituk (for Bocbkov). 27. Ka-
zakhaki,y naucYne-iss'Led-:;-,a"~-ellskiv gicIr.-meta6rAcgicheskiy. institut
(Ifor Uteshev). 28. Upravlenie gidromets'-whb7 Armyansk3y SSR (f-,~r Nev-
sesyan). 29. lirsningradak-,y's upra-71arniya gidrcmet-sluzhby (for Mikhaylov,
Dev-yatkova) - 30. Tbilisskiy gosudarslivennyy universitet (for Tsomaya).
31. TSentrallnaya aerologicheakaya obser-a-toriya (for Shmeter).
(Climatology)

124-58-9-10067
Translation from: Referati%-ryy zhurnal, Mekhanika, 1958, Nr 9, p 90 (USSR)
AUTHOR: Slime ter_-S-v~-_-
T rr LE: Random Errors in the Measurement of the Air Temperature and
Pressure in the Free Atmosphere by Means of Commutator --switch
Type Radiosondes (Sluchaynyye oshihki izmereniya (emperatury
i davleniya ,ozdukha ,, svohodnoy atmosfere s pomoshch'y - greben-
chatykli radiozondo~)
PERIODICAL- Tr. Tsentr. aerolog. obser-..-. , 1954, Nr 13, pp 46 59
ABSTRACT: A description of the methodology and results of laboratory
and field investigations of the random errors incurred in measure-
ments of the pressure and temperature in the free atmosphere b.;
means of propeller -driven pulse -transmitting, commutator --switch-
type radiosondes RZ-043M and RZ -049. In either type of radio-
sonde the mdgnitude of the random errors in the determination
of the pressure and the elevation are virtually identical; errors
in the temperature measurement for the RZ-049 appeared to be
somewhat smaller than for the RZ-043M. In general, the errors
increase with elevation. For the radiosonde RZ-049 the rnagni~
tude of the Drobabld random errors in the temperature measure-
Card 112 ments does not exceed 0. 40 for the lower troposphere and 0. 70

124-58-9-10067
Random Errors in the Measurement of the Air Temperature (cont. I
for elevations of the order of 16 km. The macnitude of the probable random
0
error in pressure measurements is limited by an absolute value of 4 mb at
all elevations up to 16 km.
V. S. Khokhalin
1. Aii-Temperature 2. Tempera ture--Measuremenl, 3. Air--Pressure
4. Pressure--Measurement 5. Radiosondes--Applications
Card Z/Z

124-58--9-10066
Translation from: Referativnyy zhurnaL, Mekhanika, 1958, Nr 9, p 90 (USSR)
AUTHOR: Shmeter. S. M.
TITLE- Inertial Errors in the Measurement of Air Temperature by Means
of Radiosondes (Inert~~ionnyye oshibki v izmerenii temperatury
-,-ozdukha- s pornoshch'yu radiozondov)
PERIODICAL: Tr, Tsentr. aerol. observ. , 1954, Nr 13, pp 60-73
ABSTRACT: Upon examination of the physical meaning of the concept of an
nertial error" and derivation of a calculation formula therefor
based on the hydrodynamic theory of heat exchange, it is shown
that the inertial error_~ encountered in RAOBS are large in com-
parison with the errorS incurred in aircraft-meteorograph
soundings and that they become even more pronounced in the
presence of intense temperature inversions in the free atmosphere.
Laboratory tests with radiosondes RZ-043M and RZ-049 are des-
cribed; the latter model is the current standard observational-
network instrument throughout the USSR. It is established that for
the usual density of the surface air and the usual speed of the ven-
tilating flow, which is 5 m/sec, the inertia coefficient for the
Card 1/2 RZ-043M is 0.32 minand for the RZ-049 0.24 min. Inthe

124 - 5 8 -9 - 10061)
Inertial Errors in the Measurement of Air Temperature (cont. )
conclusions it is noted that the inertia coefficient is inversely proportional to
the heat-transfer coefficient, that it decreases with elevation, and that the
relationship of the inertia coefficient with the rate of climb of the radiosonde
is consistent with the relationship between that quantity and the air density.
The aboveindicated laws go,(,erning the changes of the radiosonde- inertia coeffi-
cients permit in a number of cases the determination of cbrrections which
serve to refine the results of radiosonde observations.
V. S. Khokhalin
1. Air--Temperature 2. Temperature-44easurement 3. Radiosondes--Applications
4. Heat transfer--Theory
Card 2.12

SMETER, S, M, FCKRCVSKIY, V. I.
"Radiation Errors of the uomb-Type Radiosonde," Trudy Ts 0
No 14, 1955

SHMETERO S.M.; SM, G,N,
Blectrometeorograph for observations by airplanes. Trudv TSLO not'22:
3-8 '57. (MIU 11: 4)
(Meteorological instruments) (Aerona-utics in meteorology)

SHMETER, S.M.
Motion of soundirL- balloons in accelerated air currents. Trudy TSLO
no;22:17-21 157. (XML 11:4)
(Balloons, Sounding)

- SHMZM Sjj--~ '
Accuracy in calculating Richardson numbers using data for winds from
pilot-balloon observations. Trudy TSAO n0,22:32-34 157.(xIBA 11:4)
(Atmosphere, Upper)

PINUS, N.Z.; SHMRM, S.M.
Some characteristics of atmospheric turbulence oVer mountain
regions. Trudy TSLO no.24:3-11 '58. 1(MIRA 12:1)
(Atmospheric turbulence)

SHKE-M, S.M.
Passage of air currents around mountains. Trudy TSAO no.24:16-31
158. (MIRA 12:1)
~Mount4i~s)
(Winds)

34126
S/124/62/000/001/030/046
D237/D304
AUTHORS: Pinus, N. Z., and Shmeter, S. Ill.
TITLE; Results of investigating atmospheric turbulence
in the Central Aerological Observatory
PERIODICAL: Referativnyy zhurnal, Mekhanika, no. 1, 1962,
95, abstract 1B653 (Tr. Tsentr. aerol. observ.,
1959, no. 26, 6-16)
TEXT: The results are presented of investigations of wind
changes at various altitudes, structure of air streams, turbulent
oscillations of various sizes, up,.-,,ard motion over plain and moun-
tairious regions and stream regions, performed at the Central
Aerological Observatory together with other scientific and experi-
mental establishments durina the last few years. Of many conclu-
r ta
sions appearing in the work, the following are given here:
(1) Mean quadratic variance of the horizontal 'c~'omponent of the
-.-Ir,nd velocity vector over the time intervals up to 12 hours is
Card 11/2

34126
S/124/62/000/001/030/046
Results of investigating ... D237/D304
C~
higher8 (a) in the colder half-year; (b) in latitudes moderate
in comparison with the South of the USSR. The maximum is reached
near -the tropopause, (2) Velocity of vertical streams (w) in
'301"' of c.
asea maintains its sign over a 2 - 3 mi-n. period. Momen-
tary values of w reached 50 cm/sec. in 80% of flights. The
-Iiiaracter of distribution of w with the amplitude depends on
the general synoptic process and on the local conditions. (3)
"he number and magnitude of the overloads both increase with 4n-
L
crease of the intensity of turbulence. Zones of turbulence
appearing most often are those of a thickness of 300 - 600 m.
~,4 Advection of cold favors the development of turbulence of
oscillations of dimensions comparable with dimensions of air-
planes. (5) Rough air in the vicinity of mountain ridges is
determined by -the character of streamlining. 30 references.
1'r-Abstracterlo note: Complete translation.2
Card 212

PAKHOmOV, L. A. ; Slh-!-"2,ETt, S. 14. ; SHUR, G. N.
--j--
The Im-Drovpd EM TSAO airplane alectrometenrograpb. Trudy TSAO
no.11:61p-?i 15.q. (MIRA 12:9)
(Retporological instruments)

M81UNW, Vadim Dmitriyovich; SHMETER, S.M., otv.red.; BLD414IKOV,
L.V., red.; ZARKH. I.M., takhn.red.
(Ageoatrophic deviationa of wind and astatic phenomena in the
atmosphere] Otkloneniia vetra ot gradientnogo i iavleniia
nestatichnosti v atmosfere. Moskva, Gidrometeor.izd-vo, 1960.
93 P. (MIRA 13:10)
(Winds)

PAKHOMOV, Leonid Afanaslyevich; PI1RJ5, Noun Zinovyevich;,~g~X~ZER,---
Solomon Moisey evich; K01TILETKO, V.S., red.; ZARKH, I.M.,
- ------------------
tekhn.re
[Aeorological research on the variability of the atmospheric
refraction coefficient for ultrashort radio waves] Aerologi-
cheskie issledovaniia izmenchivosti koeffitsienta prelomleniia
atmoBfery dlia ul'trakorotkikh radiovoln. Moskva, Gidrometear.
izd-vo, 1960. 101 -P. (MIRA 14:1)
(microwaves) (Refraction)

S/ 1 2/00,01W) 1 /')-j3//n,!6
D2-377ID)04
t; C'
2-
1" 1 12 L Turbulence in the clouds of the upper tropo-
sphere
PERIODIC_;'~L: Referativnyy zhurnal, Mekhanika, no. 1, 1962~
96, abstract 1B661 (Tr. Tsentr. aerol. observ.,
1960, no. 34, 52-58)
TEXT-~ Some results are considered of exDerimental investiga-
tions into bumping of airplanes within the clouds at altitudes
of 8 - 113 km. The materials used were obtained during experi-
mental test-flights under the auspices of the Central Aerological
Observatory and State NII GVF on the plane TIJ-104 (TU-104) in
August and September, 1959, in East Siberia and in the Far East.
Pressure and temperature variations of air were recorded by means
of the electrometeorograph :)M-LLAO (EM-TsAO) installed in the
plane together with +.~rbulence recorders. During the flights,
Card 1/2

, SHMETER, S.M.
High cumlus clouds. Trudy TSAO no.35:3-20 160. (MIRA 131: 11)
(Cloud physics)

PtU.SE 1 BOON EX'PLOITATION, SOV/5852
Porov~!-.ov, Alekjandr MoisoLpwich, Ivan Ivanovich G-,Iy%,oronr;kiy, Yeliz-avc--ta
Gcrywanovila Zak, Vadim Vladimirovich Kostarev, III ya Pavlovich '--I:i7.in,
Yuvgc!ri' yevich 1%,linervin, Aleksandr Khristoforovich Khrgian, and
SoInmon ',.10I"!3cye,.7'.ch Sh er
-Cizi',~a ablak.ov (Cloud Physics) Leningrad, Gidrometcoizdat, 1061. 458 p.
5006 copics printed.
Eld. (Titic page): A. Kh. Khrgtian; Ed. : -V. S, Protopopov; Tech. Ed.
M. 1. Braynina and 0. G. Vladimirov.
PURPOSE: This book is intended for meteorqlogists and for specialists in fore-
catitin, sf~rvice and aviation.
CQIV'LI',AGE: The book describes modern me;hods of studying the development,
structure and ori~fin of clouds. Special attention has been gtven to the forma-
Card itio

clicud Physics
SOV/5852
ti-ri mirroncopic clernents in clouds. Tlv~ rn;icroscopic propertiv of
rlw:ds w,- al~icj studied in detail. Their posittion in space, motion, as as
lh'~w connt:ctioll with thertzicid-irmmic structure of the utruosphere, general
ca-culAic-"l, cyric,nic nctivitv, ~tc. av,! Flviim~ in cleuds is
E d':L:;c Or- pl-~i`i,-atioa ~wi s,,(,:l!n-
!j- 11 1.
It. M. Uorov~loiv, V. Ye. Al'nurviri,
Ch.
VI, by A. Kh. Khi-~-mn;
and S. 'I. ShIlle"or: Ch. Ili. V, and
C~i. jV, by A. Mi. Ki-irgian and S. At. Shin.-ter; Ch. V11, byYe. G. Zfuk;
cii. vili. 1)v A. M. r1orovikov; Ch. IX, by j. P. Mazin; Ch. X, by 1. 1. Gay-
~'orcm:~!~ly; Ch. XT, by V. V. Kostarvv, V. Ye. 'Nlinervin and A. Kh. Khr'_ian.
The 1'. T. and A. "I. Ilaranov. Ther,2 are 632 refer-
,-n,f-,: 27-1 'E'nglish, 254 Soviet, 71 German, 30 French, 2 llun.qtrian and
I Iltilish.
Card 2110

KALIIIOVSKIY, Aleksandr Bolealavovich; PINUS, Naum Zinov'yevich. Pri-
nimal uchastiyv--MZ7-&IT-&rF-r-, STEPANMiKO) V.D.j. otv, red.;
ZAEIODSKIY, G.M., otv. red.; VLASOVA, Yu.V., red.; BRAYNINA,
M.I., tekhn. red.
[Aerology] Aerologiia. Leningrad, Gidrometeor. izd-vo. Pt.l.
[14ethods of aerological measurerents] Metody aerologicheskikh
imerenii. 1961. 517 p. (MIRA 15:2)
(Meteorology-Observations)

Samm, S.M I
I
Features of a wind field ct the edges of Gb capillatus. Meteor,
i gidrol. no.11:20-Z7 N 162, (MIM 15:12)
1. TSentraltnaya aerolo ic#idikaya observatoriya.
fzds-)

PHASE I BOOK EXPLOITATIOIT SOV/6115
Pinus, N. Z., ed.
Atmosfernaya turbulentnost', vyzyvayushchaya boltanku samoletov
(Atmospheric Turbulence Causing Airplane Bumps). Moscow
Gidrometeoi.zdat, 1962. 166 p. Errata slip inserted. 1400
copies printed.
Sponsoring Agency: Glavnoye upravleniyegidrometeorologicheskoy
sluzhby pri Sovete Ministrov SSSR. Tsentralinaya aerologi-
cheskaya observatoriya. Ed.: L. V. Blinnikov; Tech. Ed.: I. M.
Zarkh.
PURPOSE: The book is intended for meteorological and aerodynamics
specialists and for persons connected with the organization
and supervision of aircraft flights.
COVERAGE: This book describes the effect of turbulent air on the
stability of an aircraft in flight.
Card 1//4

Atmospheric Turbulence Causing Airplane Bumps SOV/6115
TABLE OF CONTENTS [Abridged]:
PART 1. P_TNUS, N. Z., AND~S -~.,M.. -SHMiT ER
TURBULENT AIR AFFECTING AIRCRAFT-FL~IGHT_.
Foreword 3
Ch. 1. Some Aspects of the Theory of Free Air Turbu-
lence 5
Ch. II. Turbulence Causing Bumping of Aircraft 35
Ch. !I!. Turbulence in Jet Streams 57
Ch. IV. Physical and Meteorological Characteristics
of Cumulonimbus Clouds 78
Ch. V. Vertical Motion and Turbulence in Cumulonimbus
and Cirrus Clouds 97
Card 2/ 4

Atmospheric Turbulence Causing Airplane Bumps
Bibliography
PART II. RESHETOV, V. D. THE PHYSICAL BASIS FOR CHANGE
IN THE LIFT OF AN AIRFOIL IN A VARIABLE LIGHT TURBULENT
FLOW AND MODEL OF TURBULENT AIR CAUSING BUMPING OF AIR-
CRAFT.
This section (pp. 121-164) describes the theory
of gust loads and bumping, the relation of lift
to the intensity of light turbulence, the effect
on aircraft of passage from a laminar flow zone
to a turbulent zone and back, and the relation-
ship between the intensity of bumping and atmos-
pheric zones.
Results
Conclusions
SOV16115
115
121
161
163
Card 3/4

Atmo3pheric Turbulence Causing Airplane Bumps SOV/6115
Bibliography 164
AVAIL-AB,'.'F- Library of ","ongress
SUBJECT: Aerospace
AD/d~/jw
Card 4/4 1/6/63

T . !1.
)i,
I.; V(,
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RE`llCi I ?,(-j I. P, 0 1 . p I . I L
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e of cwnulonirnlruo, c loud
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.IllU 17:10)

ISA "If4~ S
Ab- Nr. 981-3 3 June
CONFERENCE AT CENTRAL AEROLOGICA L OBSERVATORY (USSR)
Meteorologiya i gidrologiya, no. 3, 1963, 60. S/050/63/000/004/0021002
The followina7 are among the reports presented at a recent session of the
Scientific Council of the Central Aerological Observatory: 1) N. Z. Pinus --
an experimental investigation of the wind field at altitude*s Qf 7 to 11 km,
certain peculiarities of the mesostructure of.the wind field, and the statisti-
cal characteristics of horizontal and veritical wind fluctuations in the j e t
stream zone in different regions of the European USSR and Siberia; 2) S. M.
Shniater -- the process of cumulonimbus cloud development and a pro~_os_ed
model of the structure of the fields of meteorological elements near the up-
per third of such clouds at different stages of development; 3) V. D. Reshetov --
the use of hydrodynamic equations for determining the interdependence of
ageostrophic, nonstatic, and nonstationary atmospheric motions and a more
Card 1/2

An Nr - 981-3 3 Juae
CONFERUCE AT CENTRAL AEROLOGICAI [Contd] S/050/63/000/004/002/002
accurate form proposed for writing such eq.u-ations; 4) 1. F. Kvaratskheliya --
conditions for the formation of sharp chengeEl of vertical w*ind shear in t he
upper half of the troposphere over the Transcaucasus; 5) A. I. Ivanovskiy
and A. I. Repnev -- the hydrodynamics of the upper atmosphere, taking into
account the chemical reactions occurring under solar influence; 6) V. V.
Kostarev, A. M. Borovikov, and A. B. Shupyatskiy -- certain radar criteria
for identifying the hail content of clouds and criteria for evaluating the effect
of cloud modification; and 7) A. G. Gorelik -- certaip rjesults of radar inves-
Tigations of the wind field at altitudes of 50 to 700 m. [ET]
Card 2/2

ACCESSION IM: AT4011396
S/2789/63/000/047/0055/0062
AUTHOR: Reshchikova, A. A.; Silayeva, V. I.; Shmicter, S. M.
TITLEt Growth of cumulonimbus clouds aad.characteristies of the temperature field
above them in the upper troposphere and in tho tropopauso zone
SOURCE: Tsentrallaaya aerologicheskaya observatoriya. Trudy*, no. 47; 1963.
Fizika oblakov, 55-62
TOPIC TAGS: meteorology, atmospheric convection, cloud, cunmlonimbus cloud, tro-
popause, troposphere, temperature field, upper troposphere, air temperature,
stratosphere, lower stratosphere
ABSTRACT: An investigation of the fields of meteorological elements near the
upper part of 94 cup-mlonimbus clouds was made by the Tsentrallnaya-aerolooicheska-
ya observatoriya (Central Aerological Observatory) in:1959-1961. A TU-104 flying
laboratory was used; it carried an electrometeorograph, apparatus for.measurement,
of turbulence and a Doppler set for determination of wind velocity and direction.
The flights were made in the Soviet Far East and European Russia. Emphasis is on
the rate of growth of cilmillonimbuaLclouds at heights of 8-12 km. At the time of
strong convection these clouds can penetrate into the tropopause layer and even
i to t' lower stratosphere. In the tropopause zone the rate of growth of clouds

ACCESSION NR: AT4011396
sometimes exceeds 1 meter/second. Air temperature directly over 'he tops of cuma-
lonimbus can differ by several degrees from its values in the zone outside the
clouds. The temperature is lower over growing clouds than in the surrofinding at-
mosphere but over cumulonimbus whose growth is terminating the temperature is
higher than in the surrounding atmosphere. Typical examples of these changes are
shown in Enclosures. Orig. art. has: 3 figures and 4 tables.
ASSOCIATION: TSENMALINAYA AMOLOGICHESKM OBSERVATORM (Central Aerological
Observatory)
SUBMITTED: 00 DATE ACQ: 24Feb64 ENCL: 03
SUB CODE: AS kO'REF-SOV: 603 U-MER: 003
2/5 -
Card

ACCESSION NR: AT4o45515 5/2789/64/o00/053/0054/0078
AUTHOR: Shmeter,.S.. M.
TITLE: Stages of development of cumulonimbus clouds and characteristics of the dis-
tribution of meteorological parameters In the cloud zone
SOURCE: Tsentral'naya aerologicheskaya observatorlya. Trudy*, no. 53, 1964.
Dinamika atmosfery* (Atmospheric dynamics), 54-78
TOPIC TAGS: meteorology, cloud dynamics, clotid, cumulonimbus cloud, cloud turbu~
lence, atmospheric turbulence
ABSTRACT: Data are presented on the structure of the fields of temperature, wind,
vertical movements and turbulence in a zone of cumulus clouds at different stages
of their development. It is shown that each of these stages corresponds to a speci-
fic character of distribution of meteorological elements in the cloud zone. The
lifetime of cumulonimbus clouds can be divided into stages of growth, maturity and
dissipation. Each of these stages corresponds to a specific variety of Cb. The
character of distribution of temperature, wind, vertical movements, turbulence and
other atmospheric characteristics in a Cb zone Is dependent on the stage of cloud
development. Cumulonimbus clouds In the stage of active development always have
the.form Cb caiv. In this period the mean rate of growth of their tops M is
C.rd 1/3

ACCESSION NR: AT4o45515
usually 0.2-0.5 m/sec, in some cases up to 2 m/sec, although In certain intervals
of time W can considerably exceed this value. The upward growth of Cb calv is al-
most never acc(Ynp3nied by an expansion of the top. The rate of change of its linear
dimensions rarely exceeds 0.6 kin/min. In individual cases in a period of growth of
Cb calv there is even a decrease in the diameter of the top, apparently associated
with its erosion. With a transition to the mature stage there is a rapid horizon-
tal spread of the cloud top with a velocity up to 1.2-1.6 km/min. At the same time
the velocity of upward cloud development is decreased by a factor of several times.
A cumulonimbus cloud passes Into the form Cb calv - Cb Inc, characterized by the
presence of individual domelike formations above the anvil. At the end or the
mature stage of development the dome above the anvil becomes fiat, the cloud
assumes the form Cb inc and upward growth stops. In the stage of dissipation cumu-
loninibus clouds most commonly have the form Cb inc. They settle with a velocity
attaining I m/sec. The total or partial ' dissipation of the liquid-drop part of Cb
precedes the settling of the top. Horizontal spread of the cloud top ceases and the
diarieter of the upper part or Cb gradually decreases due to the evaporation of cry-
stals. If Cb have small horizontal dimensions, the Intensity of convection is
51,1011, the wind in the atmosphere is weak and its horizontal gradients are small,
transition of a cloud into the mature stage occurs without formation of an anvil.
in this case the cloud maintains the form Cb calv in all three stages. Within the
_tOP5 of cumulonimbus clouds there are zones with a width of from 200 in to 1.5-2 kin
1:.

ACCESSION NR: ATh045515
within which the air Is In a state of permanent rising or descent with a velocity
attaining 20-30 m/sec. Within Cb calv ascending currents predominate. In Cb calv
- Cb inc there are local zones with ascending and descending movements. in Cb Inc,
especially in the dissipation stage, the air Is descending almost everywhere. The
air temperature within ascending and descending currents differs from its value
outside them. In growing clouds the ascending currents are most frequently warmer
than the surroUnding air. Descending currents In all stages of development of Cb,
and ascending currents In the mature stage, are usually cold. Ascending currents
arc observed over the tops of Cb calv and the domes of Cb caIv-Cb Inc (in 72% of
all cases). Descending air with a velocity of 4-6 m/sec is almost always observed
along the lateral bounda*ries of Cb. Ascending movements are observed only near Cb
ca1v in a narrow zone directly adjacent to the cloud boundary. The abovementioned
facts represent only part of the numerous conclusions presented. "The author
wishes to thank M. M. Kulik, V. S. Aleksandrov and A. F. Yepishev, specialists at
the GosNII GVF, and test pilot A. A. Krestenko, without whose assistance this work
could not have been done." Orig. art. has: 7 figures and 9 tables.
ASSOCIATION: Tsentral'naya aerologicheskaya observatoriya (Central Aerological
Observatory)
SUBMITTED: 00 00 SUB CODE: ES
Cor~--3/3 NO REF SOV: 008 OTHER: 007

ACCESSION NR: AT4045516 S/2789/64/000/053/0091/0100
AUTIIOR: Reshchikova, A.A., Silayeva, V.I., Shmeter..S.M.
TITLE: Turbulence causing aircraft bumping In a zone of cumulonimbus clouds
SOURCE: Tsentral'naya acrologicheskaya observatorlya. Trudy*, no. 53, 1964.
Dinamika atmosfery* (Atmosp!.eric dynamics), 91-100
turbulence, cloud, cumulus;
TOPIC TAGS: meteorology, atmospheria turbulence, aircraft
cloud, cumulonimbus cloud, aviation meteorology
ABSTRACT: On the basis of data obtained in special flight Investigations of atmospheric
turbulence causing the bumping of aircraft in a zone of Cb clouds the authors present
data on the frequency and intensity of bumping (aircraft turbulence) of jet aircraft near.
the tops of Cb and to some extent within them. They discuss the effect of wind flow around
Cb on the structure of zones of aircraft turbulence near these clouds. The following
conclusions are drawn: 1. Within the tops of Cb, In the layer up to 500 m beneath their
upper boundary, aircraft turbulence of some duration is virtually always observed. In
clouds which have ceased their upward growth the intensiV of such turbulence is not
113
Card

ACCESSION NR: AT4045516
more moderate. Only in extremely rare cases Is the overload Increment as much as
0. 5-0.8 g. In the tops of upward developing clouds the turbulence Is manifestcd as
sharp upward and downward thrusts. The intensity of bumping can be very strong with
overload increments reaching up to + lg and even somewhat greater. 2. During flight
within the tops of growing Cb an aircraft experiences transverse horizontal overloads
which "shove" It from side to side. In many cases there is also a long-period Ipitching".
3. Flight over Cb at a distance of more than 200 m above the cloud boundary are
virtually free of turbulence. 4. Over Cb, turbulent zones are encountered in the direction
of the wind vector more frequently than over sectors situated perpendicular to the wind.
These zones are situated not only over the cloud, but also extend 5-10 km to one side.
The horizontal extent of turbulent zones is 33-50% smaller alongside developing clouds
than alongside fully developed clouds. 5. In approximately 80% of the cases the turbulent
zones over Cb are continuous, but in 20% of the cases they have a discontinuous character,
with calm zones between the turbulent sectors. The latter is observed only alongside Cb i
calv and Cb calv - Cb Inc. 6. The turbulent zones near the upper third of Cb are some-
times asymmetrical relative to the direction of the wind vector. On the leeward side of
Card 2,13

.ACCESSION NR: AT4045516
the cloud these zones are more elongated horfzontally and the Intensity of turbulence is
maximum. In many cases (especially beyond the leeward boundary of Cb), there is a
second region of high turbulence at a distance of several kilometers from the turbulent
zone adjacent to the cloud. Ilia region can persist for 15-20 minutes, almost without
changing in size of intensity. "In conclusion, the authors wish to thank M. M. Kulik and
V.S. AlcksandroV, their colleagues at the GosNH GVF, for organizing and carrying out
the aircraft Investigations." Orig. art. has: 2 figures and 5 tables.
ASSOCIATION: Tsentrallnaya aerologipheskaya observatoriya (Central
Acrological Observatory)
SUBMITTED: 00 ENCL: 00 SUB CODE: E
NO REF SOV: 004 OTHER: 001
,Card 3/3

RESHCHIKOVA,, A.A.; SILAYEVA, V.I.; SHMETER, S.M.
Growth of cumulonimbus and the characteristics of the overlying
temperature field in the upper troposphere and in the troporause
zone. Trudy TSAO no-47:55-62 163. (MIRA 16:12)

CHISTYAKOV, A. F~, MI. V, ORLOVA, Ye.14. ; GLAZOVA, O.P.
PED7. L.A., ABRAMOVICH,, K.G.?, POPOVA,
T.,P,,:; I-LMEYEV, L.T. BACHU11111A., A.A.; LEIZEE;IAI F.V.,
PESKO-11, B,.Ye,-. aoli~XqOV-, N.N.; VOLEVAKHA,N.M.; PMLKO,
I.G.; PETTIENKO Ir - "~MVUENK0. I.V.-. PINITS, R'Z.;
S24EMR, SJI,, T.F.; MITUDIA, L.S.; BELISKAYA,
taiio'lm,: red.~ ZVEREVA, N.I., nauchn. red..~
K!TIlGA!'-QKJV-'A, V.14- nalichn. red.; IMTSALOVA, A.N.~ nauchn.
ed,; ':7' TI:F uchz~, red.;
SAGATOVSKI~Y, N.V.,
na
otv, red., -ilCVSKAYA, A. D...
[Marrua~ :31--r~i-4-range weathez~ ~tingj ?,ukovodstvo
po hr: t7o,-~Ib--ym prognozam pcp~~.-, rin,,. Gidro-
~' ad
meteor P'.2~ lzd.'), Yj"
(MIRA .18:8)
1. rMo::,-,,au, 'I'So-iitrai'nyy im3titut pwgiozov~

red
LN Ya.
o,i ia. e n n";r r a-d C. i d e o z, d a 2
31~O

_L 25575.
Z-'T (I) AGO (yd---- -------
AM6006946
Monograph
UR/
Pinus, Naum Zinql~~yeyich; Shmeter, Solomon Moiseyevich'
Aerology. pt. 2: Physics of -the free atmosphere (Aerologiya. ch. 2: Fizika svobodnoy
atmosfery) Leningrad, Gidrometeoizdat, 1965. 230 p. illus., biblio. 500O.copies
printed.
TOPIC TAGS: atmospheric physics, atmospheric circulation, cloud cover, aerothermody-i
namics, aeromechanics
PURPOSE AND COVERAGE: This monograph is Part II of the textbook by A. B. Kalia2nki
y
and N. Z. Pinus, entitled'Aerology, Physics of the free atmosphere, which gives a-;
systematic outline of contemporary data-on the composition of air and its changes
with altitude, on radiation and the heat balance of the upper atmosphere, on space
and time changes of atmospheric pressure and air density, on the dynamics of the
atmosphere and turbulent motion, on clouds at various altitudes and on cloud modi-
fication methoils. The book is intended as a textbook for students of hydrometeoro-
logical institutes and universities. It will also be u3eful.to specialists in the
field of atmospheric physics, aviationi rocketry, etc.
.TABLE OF CONTENTS [abridged]:.
Foreword 3
Card 1/2 UDGs 551.510.536

L 25575-66
ACC NR: AM6006946
Introduction -- 5
Ch. I. Gaseous composition of the earth's atmosphere
Ch. II. Radiation regime of the free atmosphere -- 53
Ch. III. Thermal regime of the free atmosphere -- 75
Ch. IV.- Air nressure and denaftv at variniin Altittiden

ACC NR:
AP603/,029 SOURCE CODE: UR/0050/66/000/010/0007/0013
AUTHORS: Shmoter, S. M. (Candidate of physico-mathematical sciences); Silayeva,* V. 1.
ORG: Central Aerological Obzervatory (Tsentrallnaya aorologicheskaya observatoriya)
TITLE: Vertical currents within cumulonimbus clouds
SOURCE: Meteorologiya i gidrologiya, no. 10, 1966, 7-13
TOPIG TAGS: atmospheric cloud, atmospheric turbulence, air nuiss
ABSTRACT: Durinr, the interval 1959-65, the TsA0, jointly with Gos1JIIGA and GGO, made I
a stud-i of the temperature, wind, and vortica'-movemont field.,; in the Cb zone. A
TU-104~ airplane, set up as a laboratory with special apparatus, was used to make
698 series of measurements in 294 different Cb cloud zones. Most flights were made
at heights from 7 to 11 km, and most turns were made several hundred meters within
the cloud, maximum penetration being about 1000 m. The vertical component of air
velocity was computed by means of data supplied from measuremonts of overloading and
shift of the planets center of gravity. The most intense vertical movements were most!
I frequently observed near the center of the cloud (laterally) and betw9en the center l-
and the top (vertically). Downdrafts were found to be 20-39,9 weaker than updrafts
at all stages of cloud development. No more than 10
-12 zones of large-scale down-
drafts were generally observed, and these occupied no more than 30-50% of the total
Card 1/2 UDC: 551.558.1

ACC NMP6034768 SOURCE 6 ODE:
AUTHOR: Shmeter, S. M.
------ ---- --
,ORG: Central Aerological Observatory (Tsentraltnaya aerologicheskaya
,observatoriya)
TITLE: Interaction of cumulonimbus clouds with the wind field
SOURGE: AN SSSR. Izvestiya. Fizilca atmosfery I okeana, V. 2, no. 10,
:1966, 1026-1032
TOPIC TAGS:'Lywind field, azFw~~ cloud, atmospheric mesometeorologyj
1dynamic meteoroloo,,y, atmospheric turbulence, "& CAI.~
The mesostruct -ure of the wind field, vertidal air currents,
temperatures, and turbulence near and inside cumulonimbus
clouds (Cb) were investigated in 1959-1965 at heights of.
3-12 km from a specially equipped Tu-104B airplane. Per-
sonnel from the central Aerological Observatory, the
GosNIIGA, the State Geophysical Observatory, and the Central.
Institute of Forecasts participated in the work. Wind di-;
rections and speeds were measured with airborne Doppler
equipment Vertical wind gusto were computed from data on
Card 1/5 UDC:r-51-558:551-576

ACC Nk P6034768
accelerations and changes in the pitch of the airplane,
which was equipped with thermographs ind.%barographs, elec-
tric field strength recorders, radar, and other instruments.
Visual observations were supplemented photographically and
by radar scope. A total of 698 series of measurements were
taken in and near 294 cumulonimbus clouds &t heights of
1.5-12 km over European USSR, the Soviet Far East, and
Central Asia. About 30% were storm clouds and the others
produced showers. This article deals with the interaction
of these clouds with the surrounding atmospherep and prob-
lems that relate to the development of convection near such
clouds.
Empirical data showed that a marked difference exists
between the value of the vertical wind velocity gradient
inside clouds more than 10 km across and that outside the
clouds; on the average, the ratio is 0.3-0.7. Changes in
the wind speed and direction near such clouds as compared
with values far away from the clouds are noticeable at die-
tances 1-1.5 times the diameter of the cloud and in a
layer 500-1000 m above. It was found that the change in
speed near the top of a Cb cloud reached 10-15 m/sec at
times and the difference in direction 40-50% The fev
wind measurements taken near cloud bases indicated that.
changes in wind speeds and directions were about the same
as above the clouds.
Card

ACC NR-AP6 )034768
An analysis of data from measurements taken in 50
passes across the tops of Cb clouds showed that, other
conditions being equal, the absolute values of wind spee
and directions increased with increasing vertical wind
gradients in the surrounding atmosphere, the.turbulence
coefficient k, and the maan velocity of medium-scale (cc
vective) vertical currents inside cumulonimbus clouda.
Wind speeds usually increase near Cb clouds, at times
by 1.5-2 times. The magnitude and sign of the change in
wind direction differ at varying dialinces from the tops
of Cb clouds. Radial air currents flowing into and t of
Cb clouds probably play a large part in the changes in wind
direction observed near Cb clouds.
The divergence of the wind (Div c) about the' edges of.
Cb clouds was calculated from data from 43 series of =ea-
surements. The absolute value of Div c in the top third of
a Cb cloud, measured in squares of 5 x 5.km, waa found to
vary from 4 x 10-4 to 8 x.10-2 sec-1. Div c. around the
base of a Cb cloud was calculated for only six series of
measuraments, where it was found to range from 7 X 10-4 to
9 x 10-3 GQc-I (thus, approximately the same, as near the
cloud top). Thus, Div c is 100-1000 timso greater near
Cb clouds than in the frontal
of nontropical cyclones.
zones
LC-Ed3Z5

Acc_~ik,_AP6034768
Varying values of Div c about a cloud caused forced verti-
cal cuirents of different sign where speeda are 1-2 m/sac
in some regions. As a rule, rising or verv slowly descend-
ing currents are observed on the windward uide of Cb clouds
and relatively strong descending currents on the downwind
side. Rising currents in front of the cloud top and de-
acending currents behind it produce an anomalously cold
region in front of the top of a Cb cloud and an anomalously
cold air region behind it. Relatively waris regions were
observed behind well-developed Cb clouds and an anomalously
cold region often formed behind rapidly growing incipient
Cb clouds.
Since Cb clouds are--s-urrounded by divergence and con-
vergence zones, vertical currents of dynamic origin occur
which produce fluctuations in the atmospheric pressure.
The formula for computing this pressure indicates that it
increases in proportion to the horizontal dimensions of a
cloud and the dynamic affect is more noticeable beside
large clouds (the differences in pressure Ap, are about
0.2-0.5 mb). The development of convection may be strength-
ened or weakened by 'the considerable-vertinal pressure
gradients that may be produced here.
Card 4/5-

72.
S,~-.ielltific InL;ti-tuto for --:~iculturc:-
Cos -0~ of cucll:~.)Urs
7--., U-c cf 7'
,,ouscs and :' cCs
Oni -- IU-,- --ul.
-4-
1~57, i1c) 2, 2-1-24.
Trhc. ~-btdl-- cucu:~!)(,r.3 !--,f --mrhctin;-- -.-n'turit.-, it is
Lloo7.; II)c visit& y -1 b
suff i c 7 c U U ccs
al~cl im --nder to obtain a Cma-Gor -:70iri. -41, so,~O, it
i-,r o lnc-,-c,~sc t.],o r:Lr,.bcr( 'U
is necessa- :f lc~(!s G 40-
56. The use ~if tan~inE; j-.,CrcasL--l visitatio-D's to the
f lowers by !05 cal~~ th C! cuclal)cr C-U) was -*r-,crcascd
by 731"
c,,

MITSYK, A. I SIDE, YSSER , M.
Letts start the attack with joint forces, Okhr. truda i sots. strakh.
5 no.8:8-12 Ag 162. 04IRA 15:7)
1. Predsedatell komissii okhrany truda shakhtennogo komiteta shakhty
NO-5 kombinata "Vorkutugoll" (for Mitsl-y). 2. Zamestitelt predsedatelya
komissii sotsiallnogo strakhovaniya shakhtennogo komiteta kombinata
"Vorkutugoll" (for Shmeysser).
(Vorku-ta-Coal mines and mining-Hygienic aspects)

CZP-CHOSLOVAKUL/Cultivated Plants - Fodder. bi.
Abs Jour : Ref Zhur - Biol., No 4, 11058, 1568o
Author : A. Shmid
Inst
Title : Remarks on the Seda Sowinr, of Red Clover.
(Zametki o posevakh klenera krasnogo na semena).
Or i C; Pub : Socialist. zemed., 1956, 6, No 18, no&li i i
Xistract : No abstract,
V4
Card 1/1

'URCHENKO, V.G.; TAUBE, A.M., prof. [deceased]; NWIROV, I.A.; SWID,
V.A.; M-OHOZOVSKIY, N.G., kapitan dallnego plav?niya kofffr--
- a'
a miral, red.; BORISOV, V.V., red.; BALASHOVA, M.V., red.-
leksikograf; MILDNIKOVA, N.D., red.-leksikogra:C; SAVIN, B.V.,
led.-leksik-ograf; KUZIMIN, I.F., tekhn. red.
[English-liussian navnl dictionary. Approzimate*.LY 40, 000 words
and rhrases]Anglo-russkii voenno-morskoi slova:,-'. Pod red. U.G.
Morozovskogo. Okolo 40,000 slov i sochetanii. Moskva, Voenizdat
1962. 8,51 P. (MIRA 15:12)
(Naval art and science-Dictionarieo)
(English language Dictionaries-Russian)

S/564/61/003/000/002/029
D258/D304
AUTHORS: Shmid Y. ' Kvapil, Y., Myl, Y., and Sholts, Z.
~~Czechosiovak Socialist Republic)
TITLE: The influence of supersaturation on the formation of
parasitic crystals
SOURCE: Akademiya nauk SSSR. Institut kristallografii. Rost
kristallov, v. 3, 1961, 273-277
TEXT: This paper is the first of a series concenied with the factors
influencing crystal growth, especially in chemical technological pro-
cssses. The authors deter-mined the lower limit of the metastable region
for the supersaturated solutions of monoamn,onium phosphate (W), di-
potassium (d)-tartrate (DFT), potassium alum, and Seignette's salt. This
limit was set in a dynamic process I)y recording the solution temperature
at which the first crystals were formed. The temperature of saturation
was retLd at the time at which the neighborhood of the first formed crys-
tal was optically homogeneous. The apparatus is shown in Fig. 1. A
Card 1/4

S1564j'611003100010021029
The influence of... D258/1)304
powerful light source situated opposite the observing stereo-microscope
emits parallel rays across the plexiglass containers Another light
source, at 900 from the first one, illuminates a small section of the
bottom and traps each c-rystal as it comes down. The microscope is simul-
taneously focused onto tbeilluminated part of the bottom and on part of
the parallel rays, Salts of analytical grade were used and the results
checked against those obtained with optically pare solutions. The latter
were made by partly dissolving crystals with the aid of steam, draining
the resulting solution, and then distilling water into the container in
order to dissolve the remainder of the crystals. This final solutiong
saturated at 550C, remained stable for 20 hours at C0C. The lower limit
of the metastable region was found -to be a function of overheating.
Lovered curves of temperature v. concentration resulted for increasingly
higher overheating. These curves were approximately parallel with the
curve of solubility for overheating periods of I hour. Thus, when over-
heating by 300C, the temperature of crystallization of DPT was lowered by
0 0
100C and that of AIAP by 15 C; that of0Seignette's salt was lowered by
18 C and that of potassium alum by 30 C. There are 6 figures and 9
Card 2,47

The influence of...
S156 4JOl/003/000/002/029
D258/D304
referencest 1 Soviet-bloc and 8 non--Soviet-bloc. The references to the
English-language publications read as fallowss R. P. Rastogi, J. Amer.
Chem. Soc., 3129, 1952; B. S. Strikantan, J. Indian Chem. Soc., 29, 674j
1952; A. Seidell, Solubilities, I. N. Y., 1953, p. 101; Huai Ting Hsli,
L. Warren, McCabe, Ind. Engng. Chem., 26, 1201, 1934.
ASSOCIATIONs Department of Physical Chemistry, Chemical Technological
College, Pardubice; Institute of Mineral Research
Card 314,

UZHOKI, M. [Uzsoky, M.1; SIR=G, I., [2!Ldeg, 1.1
Cross talk i-R pulsp~-pooition modulation sptems. Acta techn
Hung 42 no. 1/3:791% 1163.
1. Budapeshtskiy zavod tekludki sv;yazi*
~o.

j
ACC MR7 A1,6 CZ/0043/667006/(50f/6(54j~((j654.
033605 SOURCE CODE:
4~
AUTHOR: Simek, Ivan--Shimek, T. (Engineer; Candidate of sciences; Bratislava); ~Z
Smid, Jaroslav--Shmid Ya (Engineer; Bratislava)
_- ~t- -!' )3
ORG: [Simek] Department of Organic Technology, Slovak Technical Universit
Bratislava (Katedra organickej technologie Slovenskej vysokej skoly techni
(Smid] Slovak Petroleum n.p., Bratislava (Slovnaft, n.p.)
TITLE: influence of atacticity and crystallinity upon the dynamic and mechanical
properties of polypropylene(
SOURCE: Chemicke zvesti, no. 1, 1966, 43-54
TOPIC TAGS: polypropylene plastic, crystalline polymer, mechanical property
ABSTRACT: The dynamic and mechanical properties of polylxropylene determined by the
method of free torsional vibrations are related to the de-nsimetric and extraction
data of polypropylene characteristic for its atacticity and crystallinity. Orig.
art. has: 6 figures and 2 tables. [JFRS: 34,8051
SUB CODE: 11, 20 / SUBM DATE: 23Jul65 / ORIG REF: 003 / SOV REF: 001
Card 1/1

ZISMAN, N.A., inzhener; POPOVA, N.E., inzhener; SHMIDELI, A.A., Inzhener;
YARTSEV. G.Ye., inzhener. -
VS-3 apparatus for compositing steel circuits. Vest.sviazi 16 no-5:
5-7 Je '56. (MLRA 9:8)
(Telephone--Apparatus and supplies)

ZISMAN, N.A., inzhener; POPOVA, N.E., inzhencr; SHMIDEL', A.A., inzhener;
YARTSEV, G.Ya., inzhener. -
VS-3 apparatus for composing stool circuits. Vest.sviazi 16 ne.7:
11-13 Jl 156. (Telegrat)h linma) (MIRA 9:9)

SOV/111_59__~~_8A7
G (5)
AUTHOR, Muradyan, A~G., Candidate of Technical Sciences, Chief;
Shyr,tidell, A.A. Eag'L neer, Chief Designer,
TITLE: Individual Tone Am lifier (ITU) (Individuallny,; tonall-
ny-y usilitell (ITU~)
PERIODICAL: Vestnik svyazi, 1959, Nr 2, pp 10-12 (USSR)
ABSTRACT: The article discusses the technical specifications of
the amplifier as a whole, and describes its separate
component parts. The ITU amplif-.er is designed to
complement the SUTU type amplifier, already in use, and
the two types are basically similar in respect to oper-
ating frequency range, amplifying capabilities, and
possibilities for equalizing arrangements in operation,
in corresponding types of circui-ts, although the ITU
contains but one equalizer, which is changeable. The
ITU is intended for use in a variety of operating con-
ditions, and is therefore to be produced in several
models: for 4-conductor cable circuits the ITU-1 (way
Card 1/4 stations) and ITU-4 (terminal stations); for connection

Individual Tone Amplifier (ITU) SOV/111-59-2-8/,27
into steel and copper air circuits, the ITU-2; for use
in bi-metallic circuits and with PRVPM cable with con-
ductors 1.2 mm in diameter, the ITU-3; for organiza--
tion of auxiliary communications-along cable circuits,
the ITU-5 and ITU-6. The ITU contains equipment for
induction, and tone calling.. On 4-conductor circuits
the tone call equipment can be used for sending dis-
tance-dialing pulses. The author describes the system
provided for correction of amplitude-frequency distor-
tion,, accomplished by four different equalizing cir-
cuits in the amplifier. The amplifier element is a
three-stage transistor unit, usin=7. PlV triodes in the
first two stages, with grounded emitters, which cir-
cuit gives the greatest power amplification. The
final stage uses a P'r_- with grounded base, to decrease
non-linear distortion and stabilize output resistance.
The author notes that the triode types Pl, P~ - 00 i* ( X) -'~ + 00
or 2.) (x) < + oo f+ (X) > - CD
or 3.) f+(x)> - co Y+(X)< + M
or 4.) f (x)> - aD -f-(x)