SCIENTIFIC ABSTRACT FR:ZAYTSEVA, G.N. TO:ZAYTSEVA, A.K.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001964100013-6
• Release Decision: RIF
• Original Classification: U
• Document Page Count: 99
• Document Creation Date: November 2, 2016
• Sequence Number: 13
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTR

Biochemical changes in a d .. i31 ~~3 f B1 ~~~ 1 ~ -~ ~; .
soluble ones increase. High-molecular poky; :`-c,s~~iiates ~.re s,ssumed tc bra
reduced to low-molecular fragments t;~nd c~r~ci~orY:osphate to provide p.~osphortis
and energy for cell division. Phosp~iorit. ~.~t~~rs of sugar show no periodic
synthesis. Polysaccharide increased ex~c:~~-~r,f~ntial;ty~ Fhospholipids are
cyclically synthesized . N. D. Iyerusal ~ i, ; ~~ �i ,y, Corresponding blember AS US~>.t,,
is thanked for hire intlerest in the grork .i't~~'r~~ :are 4 figures and 1'~ refer-
ences: 4 Soviet rand 8non-Soviet. The r ,~n~,~-- most important refereneps to
English-language publications read sus fc~ _ oY;.; ; Raf n 4: Ao Campbell
Bacteriol. Rev. , 21 , 261 (1957 ); Fief ~, ` _ :? !i : Scherbaum, Ann %~ ~ '~
Acad, Sci., ~0, 565 (160). Ann,Rey-, R_i~r~~l r~t-~cl- aaittrr+~ t~, t:l-~~
accumulation a� a large quantity of mc-isture in the upper part uf'
the cloud and to the appearancw3 ~pf int:eneive showers. A c.l.aud
with t~ :'v g;~ves only s irery shcirt-duration and weak sl~owf.rh
mac ~r
Car'ci ;~d4
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AUTMORI5: Ribilas'.hvili, N.Sh. , Zaytst~va, A.t-i. , I~-uz'min, Yee. A. ,
I,apcheva, V. I~". , ordzhbniki.dzc, A._)-t.~ ~.~~nd
5ulakvelidze, G.K.
TIT1~1~.: Theory of the formation of large drop fractions in
thy: heavy radial cu,mulo-nimbus clouds, rand f`actc~rs
affecting these prpcea;ses
YER;IOUTCAL: Refl~ratavnyy xhurnal, Gsof.i~ika, no.ti, lt)6~, dU,
abstract $ D 550. (:Cn ttiecollect ion: "Tss l~:d.
oblakov, osadkov i grazovo,~o elektrichestva" ('Studies
oi' clouds, precipitations ~rrnd thunderstorm cX.ectricity' )
M. , AN 5558, lgbl, 3-6 ).
TEX'.C: Using observational data from the strato-cumulus, '~
cumulus and heavy cumulus clouds in the years 1y56-195$ in Trans- ~
~aurA~Ul~ and Caucasus, the growth of clouds' droplets was
calwul.at+cd according to the method of ~3auen and K.iryukhin, in
terms of the gravitational coagulation, assuming linear iricrea:~e
of the anabatic ve~,ocity w, with respect to the height z.
Card, ~./~
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m~
~:,1iL' IJZ~t,11Aft ~ F' ,.j ~
~-
oz o~~her sins farces ,~~ ' ,,� ,~()~.
t~.on o;f' drops, u On''.~t`a~-~h Ltcce~lc~i'a1;c; t;he ~'. ~-,_ ..
cloud. ~-~owever, n 'z~ uApclr p~.l,:r't o:~' t~, t;h~~~~ivcumu~lu ~~~il ~:c~ ;l ~ , ;.tiir�.
the cont:~ :~ i~; ~
.~~�_ a,~e Hers tl.at ~'--e spuds o.~' ~, e
of hai.~ foci ar r- are Y1eCESSar~z - ~~ tl: ::ic�~)s tr;~c_
tr e ..lcs;, ~resszr~~-~ ' ,l nor ~~~le a.dva:~e ~ ;~
e :eth.od o b afi, to =- ;,;~ r."'
* 4r i 1~ F~ ~ d r ~S ~ i:~ l,k' ~' ;; , sr-i X 1 A ~ ~ ~ ~ ~~'t~~ (_; ;`;, u
v ~l � ~. 0 c -i ''' y 4 ~.1 S o d ~; u :.. t.+. C+ _` ~ .;,.
c i ent ,., , 2 Q r r:,~
a; ending cur , .~ wareucti ~ ~, ~._ ~i Y~l`^::i-u ~.a5 c'~:-
Zi':e , u- ;per part, tian~.ch Y _
o�' ~~ cloud ~ -~recipitatior~ ; ~-, r~~~-~
pitation. The ar~ourlt oy ~ .~ccnain~ cuz~-re.lt veloc~.~,~.
oj' ;areci ~, ors tY~.e a� ' .. , , ~r ~osCt7L~iC
,,, too, a.sodic of ~.ect or r~;I~z
mulu:~ clo~zds depend
:cocesse5 canno`~ be avcrted ~~y the eA
__. p
C.~.rd 3~4 _. -
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Writ: ,~Ytfsica o~. ~ '~ccur~ul;,.~~.d dur~r~~ ~~l ~ ~ ~~ ~ , '` ~~,~~ ~~rt-~-`:~~9
~ 'Prx~ ~'E;~41~..`~a, 4 r ',7,i'7.Zl.w E'.;'.;)(;(X1 uy~3:-:~ , ,
j;~~.It`1 Gvd � a ~1~:: '.~ ~ ~ ~.}I.`ui�; ' ` .
.b CALL Y .a ~` ~ LI y ~ \~ y ~ ~.i V ~~V 3. /+, ~ 4~ k~ .L. V ~ I . .. - y .J �l J . r .. .J ... t.i .. ~ .r / � ~w
~ a +.
'~, ~ aca7. veloci~ie~, ar
,...r
' hard 2/~
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of c.~ d:l~ �r~ ut~ E;n'tS , , ~ ~ln~ ~t: o~ is c
� s;;cs, ., c , o f co,1c.~1`= , r~c~~,y~f ~Z
-~,-ro~~ � ~ o.~ o,~~~er dingy
~relo0y~y, d, Lhe Quc~~~�ne ~~ o,ant o~ ~
Sato arj:z
.~nacSti~, cloua
-~~~ic~~ c~~ulu~
r Ca~'a ~ ~ ~ -~~~

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50~1~2o-12P-~.~2Qj' ~.%
an the Influence Exerted by a V'ariatian of the Vert~.ca]. 7lind ~,'c;~ ,:,r_=;a,~:. ;,
tb;e Format~.an of ~,~ho~~r ~arar;i~jltati~on~ and ~Ia~.l
the ~sloud, hail may be prn~~ontorl ar at leae~a red~~cc~ct ; ~, ;~;;:
preventing a gravitatianwd~~~~enclont irzcreaec~ 1n ti1r, ';;,' '
If place and time of the c~ar~tez far~n~~tion rrer� iLnav~;~~ :, ;.
could be prevented Frith 4 to 10 kg of silver iodidE~. ,:,~_,:. �
these quantities a;re unknoign, an amount of $ilvor ie;li~~;~~
laxgE3r by tao or three orders is requixed for t~ai1 px~::,~,:� , .
There are 3 figure~e, 1 table, ~~nd Afi references, 3 of ~rp,~. �a,
are Soviet.
'~
,~-
,~5~30~aIATI4N: El'brusekaya ekspeditsiya ~[nstituta prikladnoy ~;eor""~:,;_!�-;
Akademii nauk SSSA
(N].brue Expedition o;~ the ~:n�titute of Ap~~lied Gao~,hysi{~~, t ;'
the Academy Qf 9oia~n~aee, U~{SH)
~'I?]sS~,NTED: Mar 25, 1959, by I~. ]!l. Peku,a, Academician
:~UDMXTTED: April 2b, 1959
hard ~~~
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~~~(/~~M~~~~j~~~1~~
Qn the Inflaenae ~xertad by a "V'ariatior~ of the gertical i-ind Component on
the Formation of Shower Precip;ttizt,~alns ~~nd HaSl
at 1~m from 10 to 37Q m~eec~~ primarily occurs in the olaud part
near the peak, i. o. at they origin of the descex~ing branch of
the hails done tra;~e-~tory .The authors ~rrite down a correspond-
ing formula for tlaa size ~-f the hail.etone. The ti;~e required
for an incxQase in ~khe hailstone largely depends an ID, and
varies between Zp and 7Q a~in. The definite size of the heil-
stones deper-ds bolt Tittle on the vertic~-1 thickness of the
aloud. Completely nEix reauilts sre obtained if the vmricctions
in the verfiical cc-mponent of the velocity of e,ix currant~~
Nith the altitude are taken into account. This permits, amonf~
other thine, the 3'o7.loeing, conclusions ; 1 } A large amount
of droplika Rater a.id hail. is piled up in the cloud part n.c~ar
the peak. 2) The ~,ni'luenee exerted by aurfa~;e-acta.ve and
hygro$copio $nbsta.ncea on the upper part oP the foz�ming ~:,dssy
cumulus does net n~ffer any positive effect Ftt m :n~sec
for stratocumuli, 5 m je�c fclx~ cumuli, and ~ C-i 5 r~~ssc t'or
massy cumuli. 3everi~l ~vfnd gusts attain velac~.t~.er~ of 25 :;'sec,
The velocity M' of v+;3rtica3. c.urrsnts ~vxt}ai c ~r~e c2~,~~*d irzcrea.se$
With rising altitudFr up to s, max~~t~am, ~ ~g in t:~~: tzk,p~;r pay
of the cloud, and teen r~ecraassu ~ap~.d~.~~. 2) 1'.he fol.~psx~t~tzre
of the cumulus during its fa~rrr~aticsn ~s higher by ~!.h~.1.C'' than
the te,aperatur� of i~ha surroundinFa medium at the same altitude,
LE~rd 1~Q During atabilisatior~ and decampoait~.on of the cumu].~za in the
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iJUs .1 1v~i,):a.i. tlt.: til.ka.1'a.~.()(1i1 ~.~1 iil.: i~).l,f; i 't.
~., 1:+'~31.U2'l.ri~:i.:il f?t",,,)z f,it'i,'trt.i'I'1 t ; , ,;.
,;'ar kilLVf1 ~]w~; 'r
.; ~ , .
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~av/58-5g~-d-1 ~r~'7w
Translated from: Referativnyy Zhurnal Fi21ka, 1958, lifr 8, p 221 (USSR)
AUTHOR; .Zaytseva,__~A..M.
TTTLEa The Determination of Critical 4+'avelengt~h of the Lower rf~~~e fo~t~ LJti~-
cymrr~e~;r~.~,a.l, n ~ u,~ t~t~cl ~~ ~ rir,`1h:~~~ec~ W~N+~~~i.i.~l~~a~
PERI4DxCAI~, itch, zap. Mock, gos. ped, in-ta, 195$, Vol 18$, pp 2O7w~1O
ABSTRACTS The author veri:l'ied experimentally the computational formulae obl;ained
tay A.Ya, Yashki~~- (RZhFiz, 1958,, Nr 3, 6,564) for the critical wavelength
of unsymmetrical. "tl " and " -~ '~-shaped waveguides, The measurements were
carried out on ~.~ 3.18 em wavelength, T;he necessary cross-section of the
waveguides was ~abtained with tl~ie aid of brass inserts , The agree~men~t
between the expailrimental and eomputatioa~al data, lies within the range of
measurement errci~rsw
T, F, Dobrovol'