SCIENTIFIC ABSTRACT KARTSEVA, ALEKSANDRA VASILYEVNA - KARSVLIN, M.

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• Collection: Scientific Abstracts
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• Release Decision: RIF
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• Document Creation Date: November 2, 2016
• Document Release Date: June 13, 2000
• Sequence Number: 7
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

ABYZBAYEV,, Ismail Ibragimovich; SATTAROV, lla~sm Murtazov-1ch; KAMS~M4,
-Aleksandra YA2jjjy.Qyna; ORLOV, V.S. red.; MAKLAKOVA, L.F.,
ved. red.; POLOSINA, A.S., tekbn. r5d. 9
(Using solution gas drive in developing oil fields as
exemplified by the Ishimbay oil fields]Razrabotka neftiaMkh
mestorozMenii pri rezhize rastvorennogo gaza. nn primere
Ishimbaiskikh xestorozhdenii nefti. Moskva, Gostoptekhiz~lats
1962.(,151 P. (KIRA 15: 11)
shimbay region-Oil reservoir engineering)

KART,SEVA, A.V.; CHIRIXOV, L.I.
Economic efficiency in the use of various wthods for stimulating
the recovery of oil in the Arlan field. Nefteprom. delo no. 3:
22-25 164. (I-11MI 17: 5)
1. TSekh nauchno-issladovatellskikh i proizvodstvennykh rabot
neftepromyslovogo upravleniya "Arlanneft".

TSYRLINA, V.B.; KARTSZTA, G.N.
Stratigraphy, petrography, facies, and oil and gas-bearing prospects
of Devonian sediments in the Kuznei;sk Basin. Avtoref. nauch. trud.
VNIGRI no.17:155-169 156. 04IRA 11:6)
(Kuznetsk Baoin--Petrol(jum geology)
(Kuznetsk Basin--Gas, Ritural--Geology)

.KARTSEVA, G.H.
I
Newiata. on the age of the Barzaa series. Trud7 VNIGRI no.
95:141-146 '56. (MLRA 9:12)
(G"olof7, Stratigraphic)
l-'

KARTSEVA. G.N..LTSYRLINA, Y.B.
Stratigraphy of Devonian deposits in the Kuznetsk Basin.
Trady -164 156.
. VMGRI no-95:147 (W.RA 9:12)
(Kuznetsk Basin-Geology, Stratigraphic)

SHULtGIIIA, N-I-; K&RTSEVA, G.R.
Results of the conference on completing and reflning generalized
and correlatinp. stratigraphic scales of the V-,t Siberian Plikin.
Infombiul, VIIGA no.19t5-7 160. (IURA 11-12)
(West Siberian plaiD-Geolegyp Stratigraphic)

PUK, P.S.; KARTSEVA G N
Prospecting outlook for petroleum in the lower Yenisey River
area. Inform.biul.NIIGA no.16:22-29 '59. (MIRA 15:3)
(Yenisey Valley--Petroleum geology)

SIDOROVA, N.G.; YJI-R"EVA, I-I-_
Cycloalkylation of aromatic compounds. Part 22; Alkylation of
toluene and mesitylene by cyclohexar,ol. Zhur.ob.khim. 32
no.9:9785-2789 S 162. (MIRA 15:9)
1. Tashkentskiy gosudarstwnnyy universitet i-meni V.I. lenina.
(Toluene) (Mesitylene) (Cyclohexanol)

YATSE'NKO, X'.A.; GUTSALYUK, V.G., KAfCr,'-'FVI, 1.1.
Solubility of netroleum resins in acetone. Trudy Inst. khim. nauk
An Kazakh. SSR 11--151-155 161,. (MIRA 17:11)

KARTSEVA, M. V.
Analysis of crude tall oil. V. D. Khudovekov and M. V. Kartseva. Zhur. Priklnd,
Khim. (J. Applied Chem.) 23, 428-31(1950).-Use of'76~6~1~ applied methods for
tall oil analysis without detn. of petr. ether Insol. matter leads to erroneous
interpretations, since the specimen may contain varying amts. of oxidized sub-
stanees, The amt. of rosin acids in all specimens examd is
variable and is always larger when the detn. is made by volumetric method without sepn.
of petr. other insolubles than when It is mnde gravimetrically.
insolubles may range from 8.8 to 16.5%. Correspondingly, such volumetric method will
give low fatty acid value, especially when rosin acid level is high. The sum of
neutral bodies, petr.ether insolubles, and rosin and fatty acids is never 100 '00. The
petr. ether insolubles form, even after removal from the original sample, in the
course of analysis (during sapon.) largely at the expense of the rosin acids. Hence,
they are oxidation products of rosin acids. G.M. KosOlapoff

K19 it T5 V)9 1-n
-110tised for Wrisadlsig*e yield of Id Oil. V, D. Khudo-
vekow and M. V. K"va. fiewuh, Ptow. 23, No. 2.
30-2(lOW).-A& W-"ildn Method for the recovery of
tall oil from sulfate black liquor (1) is described and a koni-
;wis,tm o various methods of tall od re.-overy is made. In
dctg. the"a oil In 1. 60 cc. I Is dectstatid. with 30% H*SO.
mid the residue is, filtered jusit washed vilb IW. drW, and
exid. with toluene, the toluene is mpd,., anti the residue 14
estd. with EIjO. and dr1ed to consit, wrt. The pe&. ether
MAY.,411WHI.Orit.1salsodetil. Thellf"Aractioncif
i the samples of I tt%ted ranged from 4.2,to 15.6 S./L. and the
vieresixinding pett. ether-sol. tractiots 3.2 to 111.4 C./l.
Three methods of tall oil sepn. are stuilled; air flutation by
treatment of the warm I with regulated do" of air, coolifix
the I from 741 to 400. and letting the R stand 48 br*. The
total FtO-sol. fraction removed from the I by the 3 methotis
As and 72.6-12.4%, rr,p,. anti the Intal
vir, ether fraction removed is 93.8-74.7, 41.5-57.7. anti
resp. The total petr. ether fraction of the I
removed by the floistion metbod is indepenAlent A the
oritinAl conen. in the 1. In Mill ttiaLS Of the flotAtiOn
ethod. the concit. of the Ft,06". fnction is reduccif from
8 to 10-11, g./l. for coned. I and frinis 5-6 to 2,5-2.H it-A.
or dil. 1. The mott favorable re4ults obtained are a rctlue-
ion of Fti(JLsol. fraction frMn 4.0 in :.'-2L5 g.A. for I front
he w4.Zr~ unit from 8-10 to 3,5 g./1 (or I front the rvAlx~
torf,, results which can be duplicated only by letting the I
land More than 100 bri., and reprejenting an increase In
all oil recovery of 15-20 if./ton of 1pulp. The higher tie-
~Ce of tall all removal facilitates evalin'of the 1.
Iohn lAke Kravi

1. YMOVEKOV, V. D. ; KARTS--- M. V.
1
2/ ussR (6oo)
4. Ilk-alias - ILmay-sis
7. Deterndning the amount of sulphate soap in 'black liquor. Bum. proru, 27, lio. 10, 1952
9. Monthly List of Russian Accessions, Library of Congress, -1953. Unclassified.

ntifie ReSeRrCh IPStit' 'Ite Of 7'01deMi01OCY allid
KA,RTSr,"v'A, It. V. and Yu. V. FOzlpv (Sciel ~L
Hygiene of tile Red Ar;v)
IfLetermination of Fer,,vntative Activity of t4e Pancreas and Its F~,eparation in the
Practice of Production of Tryptic Hydrolysates"
for determination of the quantity of fereentative preparation necessary to
obtain hydrolysates
(from. Alt"NOTATIMS OF THE ARTICUS SUDIMTED TO IRE EDTIORIAL 01111FICE)
Zhurnall krobiologii, Epidemiologii i Lp:unobiolo ii , No 6, pp 78-79, 1945
(Trans V831 (partial) by L. Lulich)

KARTaVA, O.P.; LYCHAK,.P.P.; SMI"OVA, T.Y.; WARIXOV. G.M., dotsent,
iiu-chnyy red.
(Bibliography of scientific works by niamobers of the Smolensk
State Medical Institute, 1920-19591 Ilibliograftia nBuchnykh
rabot sotrudnikov Smolenakogo Gosudorsitvennogo meditsinskogo
instituta, 1920-1959 gg. Smolensk, 15,60. 310 P.
(MIU 14:4)
1. Smolensk. Smolenskiy Gosuderetvenny7 maditsinakiy institnt.
2. Sotrudniki biblioteki Smolonskogo G-offudarstvennogo moditainakogo
institute (for Kartseva. Lychak, Smirnova). 3. Direktor Smolensko.-o
Gosudarstvennogo maditainskogo institute (for Starikov).
(BIBLIOGRAPHT-MMICINE)

KARTS-E-VA, V. D.
261T33
USSR/dhemist"rY - Antibiotics Jan/Fed 52
"Physicoebemical Methods for Determining Antibiotics;
1. Colorimetric Method for the Quantitative Deter-
mination of Streptomycin," Ye.M. Sevitskaya and-'V.D.
Kartsevay~-All-Union Sci-Res Inst for Penicillin and
other Antibiotics, Moscow
zhur Anal Khim, vol 8, No 1, pp 46-49
Developed a two-variant colorirztr"Lc method for detg
streptomycin -with a high specificity and sensitivity.
With this method, they could det streptomycin both in
commercial prepns and in semi-finished industrial
products down to the culture mediwa.
261T33

.TSEVA V D
~"39v. Phpfqo-dwmfcg methods of determining antibiotics. 1.
filopietli -tining streptomycla. E. M. SaOtskaya
.94 for detern
and J~, D. Har"eva, (J. aptal. Chem.. USSR, 1953. 8. 4"9).-
--Streptam)WO-IT-Mir medium gives with 2 : 4-diuitrophmyl-
hydrazino iL y4l)ow hydrazone; the excew 0i tile orange Coloured
Tangent Is extracted lvith butyl acetate ?.nd the absorptio-a of the
aq. solution containing the proAct of the reaction is imasured at
4300 A. by means of lk dificAntial photoelectric coloritneter. A
similar reaction is given by D-mannosido-streptomycin which
%ijually uccoMpanies strept6mycin. ' Offierwise the reaction is
r-pedlie forstrcptomycin in an unpurifle~l preparation.
G. S. Smuji.

"
Ir
i
v
~4
R

,q
X. M. Savitsl;aya, S. P. *uns
A. A. Korobitskay4.- mnd V. D. Kartteva (Ail-Unkin Sel.
:
Kkimr
Rewmrch last. AnOwdes, 6.rcow ~.Rr. A114J.

( M 1224-7. 4-*Au4.-Ck4tu,:V.S.S-R. 10. 113-14(lesni
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ls
,
,
t.
I
rd lo:CCOSOU
Ro"ld-Mc(!otiAAckinethod(C-4,44,27Wi)I
modifications wbich improved its acmrscy. * To PSI.-P, th'!
reagerit dimlve 0.1 g, of 2rithranone In 100 nL'ouned,
li
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rtiter %vllkb It V tcody for uw~ After adtitt, of the t
the snalyzee, who. themixt. showd be kept W =10C -
,
~
HO for 6 ntin.
This is to develop the max. color fal
eusity,
Heating for a shorter petiod,or over 6 min. affects tile color
advetsely. TIv- pToccAure of atialysis is given. !3y this
M.-edure devbtion did not exceed a

q,j

Ind

I
14

KARTMA, V.D.; BRUNS, BeP,
Physico and chemical methods for the
Phrt 5: Iffect of various factors oi
of streptomycin with the maltol meth)d.
5-0 158.
deterviination of antibiotice.
the accitracy of determination
Antibiotiki 3 no-5:39-44
(KIRL 12:11)
1. Vaesayusnyy nsuchno-isaledovatellski7
(STILWTUMIII. determ.
maltol method off. of
accuracy (Ruse)
inatitut antibiotikov.
various factori on

XARTSEVA, V.,D.; BWNS, B.P.
Physicochemical methods for the determination of antibiotics. Report
N6.10t Determination of polymyxin in a culture medium. Antibiotiki 4
no.5t45-48 S-0 159. (MIRA 13:2)
1. Vessoyuznyy, nauchno-Issledovatel'skiy institut antibiotikov.
. (ARrIBIOTICS ches.)

KkRTSEVAv V.D.; GREKUIAYEVA, Yu.S.; KORCHAGIN, V.B.; BRUNS, B.P.
Determination of streptomycin a culture solutions obtained from an
enriched medium. Antibiotiki 5 no~4:50-53 R-Ag '60. (MIRA 13:9)
1. Voesoyuznyy nauchno-issledovatellskiy institut antibiotikov.
(STREPTOMYCIN)

KARTSEVA, V.D.; BRUNS) B.F.
A new variation of the method for determining polymixin
in culture fluids. Med. prom. 15 no.6:49-50 Je '61. (MIRA 15:3)
1. Vvesoyuznyy nauchno-issledovatel'skiy institut antibiotikov.
(POL=IN)

KARTSEA, F-1 -
718'
-a--d7 ElrY.X, M. Y.
KAM` n , ,
On hyr c- and anox; a of the Rrocardium. IIId cum:.,iunicatil~nl ::;~:T erim'-ints ,-.,ith KC GN Klinitche-
ska,,,,a '~"editsina 1947, 25/2 (35-40)
In jreviolis exrerimmts it was shown that hy-c:ria and finoxia of the myocardium had
a most marked infllience on the R wive. In varioUS, OXI el'imonLs oil 1,,zolated ani.iial hearts it
,,.ias found hy Konig ind others thA in anaurobic co.riditions (N or If atizosphere) the T-er-
fused huart may beaL for so ;e time withour oxyF t 11
,en, f or one ht.ur in i lon,~ er. The same
exrerim;antal cindition is realixed by intoxication of the heart vrith KCIN vhich in con-
centrations of 0.001 N does not interfere wi.th dehydrase (Belitzev.). TI-As explains
-,rhy no ir.-.mediate death of ti!~~sues follows this -ode of intoxication. In ex-eriments on
do,?s electrocardiogra,,ns were co-mtlared before an. after the introduction off 70 mgm KCM
into the Ar,:~ulation. Very definite changes o~~curred in th-e R and T waves, q becoming much
lower an~i T hi,gher.
This comfirms the impression that the R wave is cincerned writh tile oxygen-Consuning
chemical proces:-. of Lhe metabolisn of the heart an-i the T wave aith the anaerobic
processes. Low volta:,e ofthe R wave is seen in Ififection, anae-mia, diffuse myocardial
sclerosis, myxoedema, and all conditions where o_xygen consumption of the heart Muscle
may be presumed to be low. Higgh T vraves we-e seen in stenocardia, in convalescesce
from typ'hoid fever, etc. This illustrates conditions where, as a result of .;erious
da.ma:le to the heart m~iscle, anaerobic rrocesses are intensified. In the - ormal E. C. G., R
and ~ may e_crre.-,s tWO j1hases of' the metabolic procens in the the former the aero-
bic and the latter the anaerobic phase.
Van der -Iolen - Terwolde (See. VI)
SD: Jection ii jol. _?-~.'o. j!-12

KARTSIVA, Ts.P9, kandidat maditainakikh naxtk,- SHARIKOVA, A.I.
Iffect of tooth extraction on coronary circulation. Klin. mod*
32 no.10:66-71 0 154. (MLRA 8:1)
1. Is kliniki vnutrennikh bolezney (6ir. zasluzhennyy deryatell
nauki. prof. N.YatArlyer) Leningradskago meditsinskogo stomatologi-
cheskogo instituta.
(MTR RMACTION,
off. on coronary circ.)
(HEART, blood supply,
coronary circ., eff. of teeth extraction)

KARTSEVA, Ye.P.
Role of exacerbation of the rheimAtic process (in.particular
andooarditis) in the development of' cardiovascular insiiffielency
in patients with va.1vular defects of the heart of 1,heumatic
etiology Trudy 1,SGN1 48:54-61 159. (MIRA 27,s2)
iRHMIATIC HEART DISEASE) (HEART FAILURL)

KOSHKIN, K.- KATSIGRAS, G.; SERGEYEV, A.j, YAKUBOV, Kh.
Assembly of the reductor and front axle by the selective trial-and-
error method. Avt.transp. 41 no.11:26-30 N 163. (MIRA 16:12)

PALMV, V.G., inzh.1 KkRTSIN,, N.A., inzh.
Technical centers in plants. NTI io.1103 164.
(MJRA 18sl)
1. Byuro tekhnicheskoy i~formatsii Mebfallno-derevoobrabatuvayush,2hego
kombinata imeni Yermanat g. Volgograd. (for Paleyev) 2. Rjuro tekhniche-
skoy informatsii zavoda "Krannyy Oktyabr'" g. Volgograd (for Kartsin).

KISELEV. A.A., inzh.; LAPSHOVA,
uchastiye: KMTAKRINA,
ZHELMEVAO O*S., inzh.
Smelting roller-bearing
gas and fuel oil [with
Ja '58.
M.P.; KULIKOVA, M.N.: V rAbote Drinimali
S.Z., lnzh.; EARTSIN, Yu.A., inzh.
steel i-n &aid furnaces using natural
summary in English]. Stall 18 no.1:35-40
(MIRA 11:1)
1.Zavod "Krasnyy Oktyabrl" (for Kij3elev, lepshova, Kul'kova).
(Smelting) (Bearing, metals)

KARTSITAME, A.1.1 CKEWHAVA. A-M-
Ibthod~ for measuring temperature gradients and the humidity of
the lowest atmospheric layer. Trwly Inst. geofiz. AN Grus. SSR
16-.Z39-243 '57- (MIRA lli6l
(Atmospheric temperature) (Humidity)

SOV/49-59-2-11/25
AUTHORS:Balabanova, V. N., Bibilashvili, N. Sh., Kartsivadze A. Iol
Kiryukhin, B. V. and Sulakvelid2,e, G. K.
TITLE: Experiments on the Stimulation of Cumulus Clouds in the
Alazani Valley (Opyty po vozdeystviyu na kuchevuyu oblachnost'
v Alazanskoy doline)
PERIODICAL: Izvestiya kkademii nauk SSSR, Seriya geofizicheskaya,
1959, Nr 2, PD 262-275 (USSR)
ABSTRACT: The Alazani valley (Fig 1) is often affected by the hail
from the cumulus cloud developing over the Caucasus Mountains.
In an attempt to prevent the hail falling on the valley, ex-
periments on affecting the hail formations by means of artifi-
cial stimulation were carried out in 1956 by the~Institute of
Applied Physics, Academy of Sciences, USSR, in conjunction with
the Institute ot Geophysics of the Georgian SSR and. the Faculty
of Physics of Leningrad University. A me-thod of generating
silver iodide smoke from -round level was used because seeding
from aircraft proved to be too difficult in this mountainous
area (the circle in Fig 1). The smoke was produced from red
phosphorus which reached the cloud in 5 to 10 minutes. It
was found tftat the best results were obtained where the ratio
of silver iodide to phosphorus was 1-2. The amount 3f 2 k-
Card 1/~ f silver iodide gave a full crystallization of 1 km of cioud

SOV/49-59-2-11/25
Experiments on the Stimulation of Cumulus Clouds in the Alazani
Valley
at the temperatures -5 to -100C. The effect of sunlight in
these circumstances was found to be negligible. The weather
conditions were forecast the evening before the day of the
ekperij4ents. The air lift was checked by means of the pilot
balloons each time the smoke was produced. The formation of
the nucleus in the cumulus cloud was followed on the radar
screen and at the same time it was filmed. The height of
the cloud was measured with theodolites, The results are
presented in -the form of a Table on pp 26t~ and 265, The
data given are (from left to right). date, experiment number,
place of experiment, amount of reagent in kg, time and
heia"ht of the isotherms 00 and 6oC, time and height of cloud
top, zone number and time of nuclei formation, remarks on
visual observations, The remarks are as follows:
Experiment Nr 1 - precipitation at 15.30 hours from the cloud
spot where smoke entered - then cloud dispersed;
2 - cloud dispersed at 14.20 hours,
3 - no results observed,
4 - cloud subsided between 14- and 15 hours.
Card 2/5
SOV/49-59-2-11/25
Experiments on -the Stimulation of Cumulus Clou%~Is in the Alazari
Valley
5 cloud breaking and dispersing, formation Of Cryf3tallic
forms.
6 cloud dispersed during first 30 minutes.
7 no results observed.
8 first raindro-ps from the affected spot at 13.4-0 hours
followed by hail and rain at 14 hours.
first raindrops from the affected spot, rain started
17.20 hours.
10- cloud breaking at the affected spot.
11- hail at 10.20 hours.
12- weak rain at 13.41; hours, followed i~y cloud dispersing
acove place of experiment.
17- a weak preeipitation at l1,,:35 tc 11.40 becoming intensive
at 12.2c from affected spot.
The locations of the cloud nucleus for various dates are shown
in Figs 2". 7~, 9 and 10. they photographs of the sraoke from
some e:qperiments are. shown in Figs 3, 4, 6, 8 and 11. The
following 3onclusions were mad.E!, based on ~he experiments:
1) The success in some cases suggests the possibility of
rain stiuulatioa by seeding them 2ilver iodide into cloud
Card 3/5 composed cf super-c,,coled drops at certain weather conditions.

SOV/49-59-2-11/25
Experiments on the Stimulation of Cumulus Clouds in the Alazari
Valley
2) In order to ascer-l-ain the results, the analysis of the
ctomplex data of the pb~isi-al nanditions of th-? oloud (such
as stratification (f the. atinos;-)here., 4.-he cloud energy, visual
observation or, cloud formation and precipitations. radar
observation ~~f nuclei,) etc) sliould be made,
The 7.haraz-!--:Prist-Li~ feature of the formation o-P the arti-
--nuc!.Ei by means of smoke is their lower height (1-5
to 2 lu-ii) in -,iDmpa-ison with the natural conditions,
A3 tha 6rLoking is -not always practicable,
some other
methods cf ~.'-nud stimulation should be investi-ated (from
P1101, ballcons eto),
5) The vital moment c-f affe-Itir.4- the cloud is when it reaches
the re,':zion of --5 to -10c'G, Hol.~;=-ver., because of the very high
speed of hail formation (20 moment can be easily
misjudged. Therefore, in cr."Ler to p-nevent this, an investiga-
tion of a PoSsibility of ~Iie aiz- layer szimulation should be
quarried out.
6) The expei-im.--nte on com'bllstiaa with red -phosphorus show that
Card 4/5

SOV/49-59-2-11/25
Experiments on the Stimulation of Cum-alus Clouds in the Alazani
Valley
a method of determination of tho action of hydroscopic matter
on a warm part of the cloud should be investigated.
?) It is important to obtain more data on the necessary amount
of the active chemioals which can be applied for cloud stimu-
lation, There are 11 figures, I table and 5 references; 1 of
the references is Soviet and 4 are English.
ASSOCIATION: Akademiya nauk SSSR, Institut prikladnoy -eofiziki
0
(Academy of Sciences USSR, Institute of Applied Geophysics)
SUBMITTED: January 20, 1958.
Card 5/5

KARTSIVADZE, A.I.
Determination of the angle at which the Hun's ra7s strike
an inclined surface. Soob.AN Gruz.SSR 22 no.1:25-31 Ja 159.
(MIR& 12:5)
1. AN GruzSSR, Institut goofiziki, Tbilisi. Predstavleno
akademikon To.K.Kharadze.
(Solar radiation)

AKSENOV, M. Ya.; VERNIDUB, I. I.; KMTSIVADZE, A. I.; OKUDZHAVA, A. M.;
FLAUDR, N. 0.; SHISHMINTsW-r.-r;
.9
Study of the ice-forming activity of silver iodide aerosol
generated in the burning process of pyrotechnical compositions.
Trudy Inst. geofiz. AN Gruz. SSR 20:197-20 162.
tMIRA 16: 1)
(Silver iodide) (Atmospheric nucleation)

CIABARASHVILI, T.G.; KARTSIVADZE, A.I.
Freezing of droplets of aqueous solutions of salts. Scob. All Gruz.
SSR 36 no.1:61-67 0 164. (UIRA 18: 3)
i
~. institut geofiziki All Gruzinskoy SSR, Tbilisi. Subuiitted April
16, 1964.

-
~iir*ed~*Aui kb*"~ -
- :'itallization. Orig., art~~hast-.5
tddemhi,ya UsAk~'-tiuilmk
cei -

qi-

~__4T, 16229-66 W/Ima_ nN
ACC NRt AR5016458
ion /006AO62IB4?62
5
55 .509.6
SOURCE: Bef zho' GleofizDat, Abs. A63M
AUMOR: Vernidub, 1-1-;-Mirtaivadze. A.I. KizIrlya, B.I.; T!!!butin_j R.A
TM12: A method for the introduction of reagents into clouds with th3vuse of
aviation
CITKDSOLMCE: Tr. Vses* soveshchaniya p2 aktivno vozdeyetv:Lyam na, grado proteessy,
~__.TbjUsi* 190 162-192
TOPIC TAGS: atmospheric cloud, cloud-seeding, lalimate control
TRAMIATION; A method is-proposed for the introduction of iceforming aerosol sub-
stances into overcooled clouds by firing into them from an airplane using an autowti.*,.
mul#barrel mount firing.specih anti-hail cartridges. The cartridges "teclinic..
cha*ge ignites at a proper point in-thetrajectory and causes a trace of-active smoke:
io form. The firing device is a 24-barrel block, consisting of six 4-barrel itaits.
e anti-hail cartridge is described, and a formula given for an effective Nroted
T
h a;!ic
compound to be used in it. The above method of introducing reagents was used to
feet the heavy cumul6us clouds In the Alazanskeya valley, during the period 1958 to
1962. The tests gave positive results. Similfx methods may be used for the introdue-r
Card I OL2

1 -1
l:A:rl:-3T7AT,,,E, C.. -N.
23923; IL4-7-ifSFT-MZ, G. 11. Rosheniye Zadaya-i FopereclrmoEo Udara S Uch.,Aon
"g,~--""n Defoinnatsiy. Tmidy Tb-M5. !:7-Tik Inzl,-,--,-,crov Z','..-D.
1 -t! ~ - I. I
Transporta E-1. Lenina, VYP. 20, ig4g, S. .5-21. - BiblioE-y: 15 '."AZ7v'.
SO: Letojas, llilo- 32, 19119.

KARTSIVADZE, G.N.
% ---- aaa3ie
Problem of impact on a system with one degree of freedomlin
Georgian with summary in Russian]. Trudy Inst. stroi. dela
AN Cruz. SSR 4:97-110 '53. (MIRA 9:10)
(Impact)

1956. Rev.

-~--voe-f
aiderAtion of Icval I& ditcussed, 6e Ftoblem btins
;,Cd RO I !.,of the'Timashado typc.
b
ij. mpaccIO&
at,-. lit: frec =Cffla-
d6dof, -AY atwchez!
to" In thig regard, the displacing Impact force Ind internid
energy factott "y be tepfetetitEd as tbae hmcdo m in tip! f~cit
jorm,
-i ii7t~*AI1d:cinIj cht f., -,I ie Ciad

f r* -with Plutol-'aagreg'i ~f ftecdo=, -
Y.'Yst
-
-
Sy Au try 5 zoly. E'ned-id
ids
T

RMOMMMIN MORI

K&R
.!PTSI -%tv,-kandidat tekhnicheakikh rauk (TbiliBi); 4VITSABILIZE, 0.,
I..
kandidat tokhnicheskikh nauk (Thilisi).
Using high-atrongth rteel in reinforcing lightweigbt cpncrnte
building elements. Gor. i sell. ctrot. no.2:,O,-Irj F '57.
(Lightweight concrete) (Retinforced concrete) (MIRk 10:6)

97-10-5/14
AU TH 0 R: KartSivadze, G. N., Candidate of Mechanical Sciences.
TITLE: Increase Of' Coefficient of Deformation of R inforced
E
Con,'rete ,leweiiu-B TJnder x-colongeu -o-ding. ~O lcoeffi-
tsi7ente vozrastan17a progitov Izgibayemykh zhelezobe-
tonnYkh eler,,ien'%,*ov pri dlitellnom de,.!-stvii nagruEki).
FERIODICAL:Beton i Zhelezobeton, 1957, 'Nr.10. pp. 402 - 403.(USSR).
ABSTRACT: Tile recently published "Norns and Technical Data for it
Desi,gnine Concrete and Reinforced Concrete Constructions
(Ni '17) 123-5-5), analyses In detail the publication "Build-
inU Nor,-,is and 'Regulations Calculations of stresses of
bent reinforced concrete structures are based on the
theory developed by Prof. V. I. Llurashev (in collaboration
with Ya. M. Neinirovski) in TsI-TIPS. The effect of pro-
longed loading is Ce- reti al fo
,iven in NiTU. Theo C rmulae
and examples of calculations are presented. Table Cives
border values of coefficier..,t for a rectan6ular section.
There are four Husnian RefGrences.
AVAILABLE Library of Congreos.
Card 1/1 1. Reinforced concrete-Deformation 2. Reinforced concrete
structures-Design

ZATRIMS , X-irisk Sensonovich; KARTSITADZE, Georgiy Hikolayevich;
LbR~KIPAIIIDZE, R.S., dotsent, red.: JIBRAMISHMr. T'.'A., red.
izd-va; ZHIVIDZE, D.I., tekhn.red.
[Strength and dynamics of structuroal Ustoichivost' i dinamika
sooruzhenii. Tbilisi, Goe.izd-vo lichebno-pedagog.lit-ry 18TSodna,"
19419. 318 P. (MIRA 13:3)
(Striletures, Theory of)

KARTSIVADZE, G.N.
Role of various normal componenta in processeS of free vi-
brations of elastic gystemq. Trudy Inat.stroi.dela AN Gruz.
SSR. 7:61-78 '59, (MIRA 13:5)
(Vibration) (Ilastic rods and wires)

M'92SIVADZE,-G-U-,-kiLnd.takhn.nauk; KVITSARID2M, O.L. kand.tnkhn.
nauk; UMTHWTA. Te.S., kand.tekhn.nauk; GVELESIAM, L.O.,
kand.takhn.nauk
Effect of temperature and moisture conditions on the increase
of deflections in bent reinforced concrete construction ele-
ments subjected to long-time I(xtda. Bet.i zhal.-bet. no.1:
27-31 Ja 16o. (14IRk 13:5)
(Strains and stresses).

3L-~:)W
3 73o0
AU+HOR-.
TITLE:
S/169/62,/000/002/020/01'cn
D228/D301
KaESA"agK#*.~_
The role of separate normal components in the process
of seismic oscillations of complex systems
PERIODICAL: Referativnyy zhurnal, Geoj'izika, no. 2, 1962, 19, ab.-,
stract 2A138 (Soobshch. All GruzSSR, 25, no. 6, 1960,
723-730)
TEXT: For structures with many degree13 of freedom the problem of
determining seismic actions is solved by breaking down seismic os-
cillations according to their normal components; this enables the
maximum values of the inertias to be ascertained for each of -IV-he
oscillatory forms. Determination of the calculated values of seis-
mic forces meets difficulties of a principle and a technical na-
ture in view of the fact that spectral analysis does not yield in-
formation about the phases of normal o:3cillations and about the
comparative role of each of the normal components. The analogy of
the behavior of any normal coordinate and the correspondIng linear
Card 1/2

S/101 62./000/002/020/072
The role of separate D228YD301
oscillator is incomplete.. since the dependence of the inertias Of
the normal components on the natural oscillation period is not ex-
pressed by the spectral curve of the cited accelerations. The non-
correspondence is due to the disregarding of the oscillatory formFi
which determine the coefficients of resolution when the function is
presented as a series for the normal components. It is concluded
that the relative role of individual normal. components depends on
the properties of a structure. Therefore the number cf oscillatcry
forms taken into account in the calculation should be established
separately for each specific system. In the case of the slow con-
vergence of the series, representing the resolutlon of the full
maximum inertia for the oacillatory forms, the summation becomes;
difficult. In this instance it is expedient to give preference -.-
another method, which considers the seismic forces for each of the
oscillatory forms as an independently calculated case. Z_-Abstra:-.-_
ter's note: Complete translation.-7
Card 2/2

12, 00-U.,
AUTHOR:
TITLE:
PERIODICAL:
!i/169/62/000/009/014/120
.0228/D307
Kartsivadze, G. N.
Seismic inertia distribution down a building
Referativnyy zhurnal, Geofizika, no. 9, 19629 21, abr
stract 9A135 (Tr..Gruz. polit'ekhn. in-t, no-~ 5 (76),
1961, 47-52)
.TE'XT: The author studies the distribution of seismic forces, down
a pivot, which is fastened at one end and has distributed masses.
The distribution of seismic forces is compared according to-the
static theory, the USSR's standards (CHZ-51 (SN 8-57)), and the
Californian building code. The static theory considers seismic
forces as being uniformly dietributed down a pivot; in the SN 8-57
standards and the Californian'code seismic forces are taken as
.equal to zero at the pivot's base. While solving the problem ma-
thematically by the method of Fourier for an arbitrary moment of
time, a sufficient number of terms Must be retained in the formula
of expansion. The practice of considering just one term, i.e. of
Card 1/2

S/169/62/000/009/014/120
Seismic inertia distribution ... D228/D307
the fundamental tone's vibrations, when determining.seismic for-
ces has been insufficiently substantiated. The maximum value 'of
seismic forces can be found only on the basis of analysis for a
specific seismic movement. Z-Abstracter's note: Complete transla-
tion.-7
Gard 2/2

KARTSIVADZE, GJL4 MEDVEDEV, S.V.; NAPETVAIUMZEp Sh.G.; ZAVRIYEV, K.S.,
red.; DUZIMVICH, S.Tu., red.; BUDARINA, E.M., red. izd-va;
GGLIBERG, T.M., tekhn. red.
(Earthquakeproof construction abroeLd]Seismostoikoe stroitelletvo
za rubezhom; po materialam. Vtoroi irsemirnoi konferert sii po
seismostoikomu stroitellstvu v 1960 g. v g. Tokio. Pod ob-
shchei red. K.S.Zavrieva i S.N.Dusiinkevicha. Moskva, Gosetroi-
izdat, 1962. 223 P. (MIRA 161l)
(Earthquakes and building)

KARTS IVADZE, G. 11.
The distribution of seismic forces of inertia along the
height of a structure. Trudy GPI [Gruz.] no.5:47-52
161. (MIRA 15:12)
(Earthquakes and building)

KARTSIVADZE, G-bN-, kand. tekhn. nauk
Experimental data on the dynamic characteristics of arched
spans of reinforced concrete bridges. Bet. I zhel.-bet.
no.11013-515 N 161. (MIRA 16:8)
(Bridges, Concrete)

KARTSIVADVE, G.N.; BYUSp I.Ye.; DMINCRARADZE, D.I.
Now experimental data on the dynamic parametere of reinforced
concrete arched bridges. Trudy OPI [Gruz.] nc-7:55-60 f63.
(14IRA 18:6)

KARTSIVADZE) GIN.
Longitudinal seismic -ibrations of girder bridRes with rigid supports
on a pliable foundation, Trudy Inat, stroi.makh. i seism. AN Gruz. SSR
92183-188 163. (MIRA 17122)

~, q.j~ I- k.und. Lekhn. na-uk i ", ti; : ;:, .1 ~
SiYAW .1.
-LUd - -
ULteral ueiwnic vibratiorm, of' girdf-7-r ". - -- - -1 t=rr,
,I- U, +. 16:-'1
-,ooruzh, no.13:95 9' 1 ~ "

KARTSIVAME, G~N.
Free lateral vibrations of contlnuoun-beam bridges. Trudy
Inst. stroi. makh. i seism. AN Gruz. 10:199-204 '64.
(MIRk 18:11)

TTAWAM, G.K.
Now location data of epicenters and hypocenters of Caucasian earth-
quakes. Tru4 Inst. goof-is. 4N Gruz. 'SSR 16-.163-175 157.
(Cau,oasus-Ilartliquake a) (1(1:iA IV6)

IOSELIANI, M.S.; KARTSIVADSE, G.Ye.
----------
Seismogeological structure of the Akhalkalaki upland and some adjacent
regions. Trudy Inst. geofis. AN Gruz. SSR 18:81-89 160.
(MIRA 13:10)
(Akhalkalaki Region-Soismolog5r)

S/169/61/000/009/014/056
D228/D304
AUTHORSt loseliani, 1W. S., and K-artsivadze,-G. Ye.
TI TLE The question of the aeiamo-geologic structure of the
Akhalkalak highlands and some adjacent areas
MIODICAL: Referativnyy zhurnalo Geofizika, no. 99 1961, 19,
abstract 9A151 (Geopizikis institutis shromebi.
Sakartvelos SSIL Metaniyerebata Akademia, Tr. In-ta
geofiz. AN GruzSSR, 18,, 1959 1960 9 81-89)
TEXT: The general geologic structure of the Akhalkalak region and
adjacent areas is exposed, and seismologic data are given for this
territory. The epi- and hypocenters of earthquakes are determined from
G. K. Tvaltvadze's hodographs. Comparison of seismologic and geologic
data provides the basis for drawing the conclusion that there is no
seismo-genetic connection between the Akbalkalak highlands and the Kazbek
area. The foci of strong earthquakes are related to the boundaries of
tectonic units (Artya,-Somkhit block, Aftharo-Trialet fold-system, and the
Card 1/2

S/169/61/000/009/014/056
The question of the ... D228/D304
Georgian block). The seismo-goologic structure of the Akhalkalak high-
lands is related to the seisno-geology of Turtsiya. Their intensive
seismicity is, in the opinion of the authors, caused by recent volcanic
movements. As is known, the Akhalkalak highlands were a stable part of
the crust throughout the Alpine orogenetic-cycle, whereas intensive tec-
tonic movements took place in their adjacent areas. Towards the end of
the Neogene the picture changeds intensive tectonic movements began-
in consequence of which the dismemberment of the crystalline basement
into small blocks took place--and tectonic fractures, to which the earth-
quake foci are also confined, were formed. The results obtained by
abyssal seismic sounding and other geophysical methods will have great
significance for the deeper study of the seismo-geologic structure of
the Akhalkalak highlands. fAbstrhcter's note% Complete translation.3
Card 2/2

KARTSIWZ13, 2.N.
Functions represented in -che form ar a potential. Trudy Vych.
tsentr. AN Gruz. SSR 4a!9-28 164 (MIRA 17W

h N?
Nti %V 61t- 4 E 1-
Karcivadze, 1. N., Andlivedelid2e, B. V. On an inversion
formula. Swb~teniya Mad. Nauk W-1-tizill. SSR, 10,
587--591 (1949). * (Russian)
h%tjie"t141L1 Reviows 1, 2, - - 'he simph: closcil, silit;j1~1y slIjIlt,111
Let Ch (k
-itivo --
vole 14 N60 8 cUrves, exterior it) each other and with a I xjN di"Cl
Sept* 1953 51L I on each; C= ECk; it is assimied that 1111 poilli (if
itcC111110lation of tilt! 'w(plent.l. C,, C.!, - - - b(.111111"s lot C;
is givell by 0:s-v2Vi, %vli(
-r.-.% k -tit %ifarramj It i:i
tile lVilgill I)( CI. Lv[ '00 P)--,tIj) (III -A Y 4. (1 1
L
To

Ma.therm-bloal Reviews
Vol, 14 No* 8
Sept. 1953
Analysi.a
k-kitreivailm.LN On the behavior of an Integral of Cauchy
type nqar the ends of the path of Int-e-g-7i'lilo-n. Akad.
Nauli