SCIENTIFIC ABSTRACT KVAPIL, M. - KVARATSHKELIYA, N. T.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000928310008-0
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 20, 2000
• Sequence Number: 8
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

KVAPIL,-,Mirzsla3r-
Colorimetric determination of phosporus In ferrovanadium. Rudy
10 no.6sSuppl.:Prace vyak ust no.5:33-34 Je 162.
1. Ustav pro vyzkum rud, Praha.

FAVLIKOVA, E. - KVAPIL M - WEISS, D.
~L~~
Chemical analysis of barite. Rudy 10 no. 4:Suppl-13-18. Ap 162.
1. Ustav pro vyzkum rud, Praha.

PAVLIKOVAJ, E.; KVAPIL, H.; WEISS, D.
Contribution ~o the chemical analyais of totrahodrite.
Rudy 11 no-31-Supple-i Price vyzkumnyoh ustavu no.2:9-23 Mr 163.
1. Ustav pro vyzkum rud, Praha.

KVAPILp Oldrich
higher labor productivity in agricultural production. Vestnik CSAZV
no.9:488-489 6o. (EW 10:3),
(Czechoslovakia--Agricultre)

KV-AP(L/ 0,
CZECHOSLOVAKIA
KVAPIL, 0., DVM
Louny
Prague, Veterinarstvi, No 3, 1963, pp 124-125
"Reminders to Designate Quality of Fork Fat."

KVAPIL Otakar MVDr.
. . . . . .~- -- P. ~- z - - , ~ , , '9
Methods of lard sampling for determining its use in maklng
products. Prum potravjin 15 no.11089 N 164.
1. Central State Institute of Veterinary Medicine, Meat
Department, Louny.

KVIPILt R.
"Calculating the Dynamic Effects of the Conic and Jaw-Crusher Operation." p. 109.
(Li!ftj Vol.lt ND.7,, Sept. 1953, Praha.)
Vol. 3. "o. 3.
SO: Lol.,,thly Li.-st of East Europ~,~an Acc*ssiors p ILibrary of Congri,3::,, 1~,-rch 195-1,5 Unci.

KVAIPILj R.
NPrineiples of Design for Ball Mills." p. 13 (RUDY, Vol. 2, No. 1, Jan. 1954) Praha,
Czechoslovakia
SO: Monthly List of East European Accessionop Library of Congress, Vol. 32 No. 41
April 1954. Unclassified.

KVAFIL, R.
"7undamentale of Compressors, DiesslIbtors, and Steam Engines." p. 101, Praha, Vol. 2, no.
4, Apr. 1954.
SO: East Suropean Accessions List, Vol. 3. No. 9, September 1954. Lib. of Congress

KVAPIL, R.
"Elements of turbine posor units." Technicka Fracap Pratiolava, Vol. 6) No. 1, Jan. 195/*,
p. 41.
SO: Eastern Elwopean Accessions List, Vol. 3, No. 11, Nov. 1954, L.G.

KVAPII,., R.
Methods for solvin,-,, problems of earth pressure. P. 146.
Surveys of boring systems in Czechoslovakia. P. 148.
R "raha
RUDYY . Vol. 3, no. 5, May 1955.
SO: Monthly List of East Euvopean Accession5) (EEPAL), LC, Vol. 4, no. 10, Oct. 1955.,
Uncl.

777

Kvapil, R.
Problems regarding the most advantageous construction of parabolic
underground vaults. p. 23. ILTMRSKE STAVBY. (Ydnist~trstvo
stavebnictvi) Praha. V01. 4, no. 1, Jan. 1956.
Source: EEAL IL Vol. 51 No. 10 Oct. 1956

KVAPIL, R.
Determination of natural vaults and the loose area over cavities caused by
mining. p. 105
RUDY Vol. 4, no. 4, Apr. 1956
Czechoslovakia
Source: EAST ELMLOPEAN LISTS Vol- 5, no. 7 July 1956

XVAPIL, Rudolf
Nove nazory v theorli horskych tiaku. a dulnich otresu. (New Theories on
Rock Pressure and Mine Earthquakes. lst ed. Germand and Russian sirmaries, illus.,
bibl.) Prague, SNTL, 1957. 132 p.
The study has three parts. It contains information on the results of the research
in the field of the Pressure of rocks, on their new theories and on earthquakes in
mines. It is an abridged version of a more extensive book to be published.
Bibliograficky katalog, GSR, Ceske knihy, No. 31. 10 Sept 57. p. 664-65.

KVAPIL, R.
A contribution to the basic research on earth pressure and mine quakes. Pe 730
(Uhli, Vol. 7, no. 3. Mar. 1957, Praha, C2echoslovakia.)
SO: Monthly List of East European Accessions (EEAL) LC. Vol. 6, no. 12, Dec. 1957.
Uncl.

KIAPIL3 R.
Crumbling of rocke from the point of vltw of potential enera. Pt. 1.
P. 285. (UHLI.) (Fraha, Czechoslovakia) Vol. 7, No. 9, Sept. 3-957
SO: MontUly index of East European Accession (LEAI) W. Vol. 7, No. 5, 1958

KVAPIL, RUDOLIF (Evapil, Rudolfj, doktot inzh. (Chakhoolovakiya).
1
M W- - 6 - t -
ine bump theory. Ugoll 33 no-5:46-413 My 158. (MIRA 11:5)
(Czechoslovakia--Subsidences (Earth movements))

KVAPILj R.
Problem of desiging storage bins for loose, loose, partly and
nonpourable materials. p. 392.,
-r-7MGETIKA, Praha, Czechoslovakia, Vol. 9. no. 8, Aug. 1959
Monthly list of East European Accessions. (EEAI) L-,, Vol. 8, No. 10
Oct- 1959
Uncl.

KVAPIL, R., dr., inz.; LU P K., inz.
Distribution of pressure in irregular experimental ores used for
crushing tests. Rudy 9 no.11:382-381+ N 161.
(Ores)

-FV~ ~ (Chekboslovatskaya Sotsialisticheskaya Respublika);
LTUPM.9 X. (Obekboslovatakaya Soteialisticheskays Respublika)
Distribation, ofotresses in irregularly shaped specimens in
determining 'thethardness of rocks under pressure. Ugol' 38
no.4958-60 Ap 63. (MIRA 16.*4)
(Rocks-Testing) (Strains and stresses)

Us:~c: To So d 1~.L
10a. vol.
Vol. 3, 1"). 3.
Slu: L.onthlv List of East Europcan Accessions ./Library of Com-,rcssP Larch 1954, Uncl-

JD/JG
L 26754-66 VVVT(m)/EWA(d)/EWP(t) IJP(G
ACC NRt AF6011471 smn cou: Wom/66/ou/ow/b289/0294
-AUMORb.- Timof V. A* DaVAIL, Y
ORG: Institute of CryAgLogmpb
yp (Institut kristallografii IM SSSR)
B: On the solubility and crystallizati of Y&U01i from solutions in melts of
TITL on
.PbO-B2% and PbO-B203-PbF2
SOURM: Xristanograflya,#, v. 31., no. 2., 1966, 289-294
TOPIC TAGS: garnetj, 'crystal powingp yttrium compound, aluminum compound, crystal-
lization , solubility, temperature dependence
~n
ABS7MCT: 2he authors investigated the solubility of theyt ~riuq-24,uqinum gtTneiln
low-volatility melts by a simple procedureo based on introducing a small p imer crys-
tal of the dissolved substance (Y,-.Al5Ol2) and checking whether the solution is under-
saturated or supersaturated by seeing.whether the primer melts or causes precipita-
tion of a larger crystal. The temperature dependence of the solubility is deter-
mined by the same m6thod. . The results show that in the same temperature region the
solubility of Y3AI5012 is higher in PbG-B203-PbF2 than in PbO-B~203. The method can
be used to grow Y&UsO,2 crystals with the aid of primers, to estimate approximately.
the ecrailibrium state of the system., and to outline the stable regions of crystal-
lization in,the7multl-~66zponiifit s~,stem Y2Q3-A3,20s-PbO-B2Q3-1IbF2. Related to this
procedure ii--a-ERNod dese id--for determining the saturation of the solution, con-
sisting of dropping a rod of Anum into the melt and drawing it. out so as to pro-
LS&rd 112 tw:

KVAPILI V.
Now construction of freight cars. p.21+2.
ZELENZNICNI DOPRAVA A TECHNIKA. (Ministerstvo dopravy)
Praha, Czechoslovakia
Vol.7, no. 8, 1959
Mnthly List of East European Accessions (EEAI) LC, Vol. 8, No. 11.
Nov. 1959
Uncl.

KVAPIL.. -V
- aclAy, inz.
Railroads and shippers. Doprava 7 no.2:99-100 165.

SOKOLP L.; KVAPIL, Z.; KAM, V.
Combining,the-gas chromatography and the absorption spectra methods
-for.the analysis of organic substances. Part 2: Identification of
htones, aromatic carbohydrates and nitriles in the extracts from
carbonization.benzons. Coll Cz Chan 26 no.9*.2278-2288 161.
1. Forachungsinstitut fur die chemische Ververtung der Kohle, Zaluzi
v Kmanych horach.
(Chemistry, Organic) (Chromatograpby-)
(Absorption spectra)

KUBICKA, Rudolf; P~AZ4,_Zdenek; SYKORA, Milan
'Pyrolysis of xylenols and tpr fraction. Chem pre 12 no.11: 598-601
N 162. -
1. Chemicke zavody CSSP, Zaluzi.

KVAPILEVI, A.I.v kand-6 sbl'khoz. nauk; SEREBRYAKOV9 K.M.v nauchnyy sotrud.;
DZKINA~_W.F., kand.-biblog, nauk; ZUSMANq N.S.9 kand. biolog. nauk;
LEPESHKINq V.I.-, haiic~lwy sotrud.; LEONTYUK9 S.V.p kand. veter. nauk;
GUSEVp S-A-9 k6md,, voter. nauk; DOBYCHINA9 I.P.p red.; FROKOFIYEVA.,
1S.N.P tekbn. red.
[Rabbit'rai9ing1'KrvMovodstvo. Moskva, Gos. izd-vo sellkhoj. lit-
ry, 1960. 311 P. (MIRA 14--9)
1e Sotrudnild Nauchn6-issledovatellskogo instituta pushnogo zvero-
vodstva i krolikovodstva (for all except Dobychina, Prokoflyeva).
(Rabbits)

I
PMWVICKY, Oldricb, Mr,,; KVAPILIK, Josef, MUC
Stperience with toxoplasmin test on the basis of allergometric
studies at the state psychiatric bospital at Kromeriz. Gas. lek.
cook. 44 no.34-35:933-937 26 Aug 55.
-1. Z neurologicke kliniky lekarske bygionicke fakulty Karlovy
university Praha, SFN Praha 111. Prednosta prof. Mr. Jan Sebek
Ze Statni psycbintricke locabny v Kroxerizi. Reditel Mr.
Antonin Pliskal.
(TOXOPLASMOSIS, diagnosis
toxoplasmit test, allergometric studies in mental
bosp. in Czech.)

KVAPILIK, Josef
------ ~ 11 1
The importance of Dr. Cenek Navrat for Yloravian psychiatry.
Cesk. psychiat. 57 no.6:402-404 161.
1. Psychiatricka ledobna v Kromerizi.
(BIOGWHIES) t~SYGHIATIIY)

KVAPILIK, Z.
Vasicek, Z. Installing AGY conductors using new installation materials. P. 389.
ELEKTROTECHNIK, Prague, Vol. 10, n--,. 12, Dec. 1955.
SO: Monthly List of Est European Accessions, (M~L), LC, Vol. 5, "to. 6- June 1956,
JJncl.

KVAPILIK~ Z.
Assembly of glass pipes in the inst,illation of electric systems. p.265-
(Pozemni Stavby, Vol. '~, No- 5, May 1957, Prava, Czechoslovakia)
SO: Monthly List of East European Accessions (EEAL) LC. Vol. 6, No. 9, Sept. 1957. Uncl.

KVAFlLIR, Z.; VA511-EK, Z.
~z_~
The development of clips to hold electric wiring conduits.
p. 230 (Elektrotechnik) Vol. 12, no. 7, JulY 1957 Fraha, Czechoslovakia
SO: :-C:EHLY 1.%IDEX CF EAST EtRICHIN ACCESSMIS (&IAI) LC, Vr,L. 7, no. 1, Jan. 195E

KVAPILIKI Z.; ELLINGER, K.
Pasting, a new method for fastening ele4etric installations in dwellJngs. p, 268.
POZEMNU STAVBY. (Ministerstvo stavebn ictvi) Praha, Czechoslovakia. Vokl. (7)
no. 5, (May) 1959
Monthly List of East Eurorean Accessions (EFA, LV' Vol. 8, no. 7t July 1959
Uncl. .

KVAPILIKOVA, K.
Surgical therapy of glaucoma with concentric narrowing of the
visual field. Cesk. oftal. 20 no.6:449-452 N 164.
1. Ocni klinika lekarske fakulty University J.E. Purkyne
v Brne, (prednosta prof. dr. J. Vanysek, DrSc).

KRLPILIKOVA, Kveta
Motility disorders in unilateral aphakis and their correction with
contact lenses. Cask. oftal. 18 no.3.-212-126 My 161.
1. Ocni. klinika University J. Ev. Purkyne v Brne, pre4. prof. dr.
Jan Venysek.'
(LENS CRYSTALLINE abnorm) (CONTACT LENSES)

KVAPILIKOVA, Kveta
Results of the surgical treatment of strabismus in adults. Cesk.
oftal. 18 no.2: 112 -115 Mr 162.
1. Ocni k3.inika University J. Ev. Purkyne v Brne, prednosta prof.
dr. Jan Vanysek. (STRABISMUS Ourg)

KVAPILIKOVA, Kveta
Binocular vision'following the implantation of intracameral lenses.
Cesk. oft-al 28 no.3t207-211 My 162.
1. ocni klinika University J. Ev. Purkyne v Brne, prednosta prof.
dr. Jan Vanysek.
(LENSES) (LENS CRYSTALLINE abnorm)

VANYSEK, J.y prof. dr,,Drqoo; XTAPILIKOVA, K.
Early and late experiences with intracameral. lenses. Cesk. oftal.
21 noe3&l59-166 MY 165
1. Ocni klinika lekarske fakulty University J.E. Purkyne v B-me
(predliesta: prof. dr. J. Vanyack, DrSe).

KVAPILOVAj A.
"Bulls and catle breeding."
p. 22 (Rolnicke Hlasy) No. 1, Jan. 1958
Prague, Czechoslovakia
SO: Monthly Index of East European Accessions (EEAI) W. Vol. 7, no. 4,
April 1958

KVAPI1A)VA, A.
Do ~-ou want more oork?
P. 20. (R101VICKE HL',SY) (Praha, Czechoslavakia) Vol. 11, No. 12, Jan. 1951J
SO.'- Monthly Index of East European Accessior (171EAI) L", Vol. 7, No. 5. May 1958

CZI~CHOSLOVAKIA
HANAKOVA, S., KVAPILOVA I. I-111NARIK, L: Physiological Institute
Medical Faculi~,-P-alla-c y-Miversity (Pysiologicky Ustav Lek.?&k6.
P.U.) Olomouc.
"Extension of Anesthesia Duration by Hyperventilation with Atmospher-
ic, Air."
Prague, Caskoslovonska F-ysiolorie, Vol 15, No 2, Feb 60', n 72.
Abstract: Use of an extension of anesthesia induced 13y thiopentuti&J.
after premedication with atropine-lobeline to influence CN5
activity is discussed. The extension of anesthesim is conn----,cted
to hyperventilation hypocapnia. It appears that the effect is due
to hypocapnoic vasoconstriction in the cerebrRl re7ion.
No references. Submitted at the "16 Days of Physiology" at
Kosice, 29 Sep 65-
1/1
pF,KAM, j.,. STEjsKAL, A.; KVAPILOVA, It.; technicke spoluprace VALKOVA, H.
A new method of preparing portussia vaccine. Cask. apidem. mikrob.
imin. 10 no.5-.314-322 8'a%61.
1. Ustav ser a ookovacich latek v Frazo,
(WHOOpING COUGH immmoi) (VACCINES)

--- --- ---

Oil, exe,-, of
c r

KVARTALINOV,- Ye-..V,.. - ~
Harmonic analysis of observation on tidal phenomena for a
period of many days. Okeanologiia 5 no.6:1070-1082 165.
(KRA 19: 1)
1. Kaliningradakoye otdolenivo Instituts. okeanologii Ali SSSR.
Submitted December 7, 1964.

KVARATSKHELIA, N.T.; GAMBASHIDZE, K.K.; DZHAKELI, M.Ye.
Effect of gramineous and leguminous grass mixtures and organic
fertilizers on the microbiological processes in subtropical
Podzolic soils. Soob. AN Gruz, SSR 29 no.1:73-8o ii 162.
(MIRA 18:5)
1. Inatitut pochvovedeniyaq agrokhimii i melioratsii, Tbilisi.
Submitted November 27, 1960.

S/032/60/026/05/17/o63
0715-6/0 B010/BO05
AUTHOR: ,4varatBkheli, Yu. K.
TITLE: Application of a Plasma Source to the Spectrum Analysis
of Slags
PERIODICAL: Zavodskaya laboratoriya, 1960p Vol. 26, No. 5, PP- 557-559
TEXT: A new light source known in publications under the designation of
"Plasmatron" was used in slag analysis. The device used (Fig. 1) is a
closed chamber into which gaseous argon is blown under pressure
(0-4-0.7 atm) through an opening in the bottom. The rod-shaped anode is
located in the chamber, and directed towards an opening in the side wall
of the chamber acting as a cathode. The plasma of the d.c. arc burning
between anode and cathode is blown by the gas pressure out through the
opening so that the greater part of the plasma is outside the Wiamber
forming a free flame. The latter is used as a light source for the
spectrograph having a temperature of 10,000 - 11pOO00 K. G. M. Gian-nini
(Ref. 1) attained temperatures up to 170,0000 K at higher current
Card 1/3

Application of a Plasma Source to the S/0~2/60/026/05/17/o63
Spectrum Analysis of Slags B010/BO05 -
intensities and gas pressures. In the present case, a special
construction of this light source (Fig- 3), as rell as correapondinC
anodes (Fig. 2), were chosenp and slag analyses carried out with three
variants of sample feeding: strewing of the sample powder into the
gas flow, pulverization of the sample solution, and complete evaporation
of the sample located in the anode. The last-mentioned variant proved to
be most convenient. The experiments were made with slag samples from the
arc furnace of the author's Association. The samples were analyzed in
the chemical laboratories of the zavod "Elektrostall" ("Elektrostall"
Works) and the author's Institute. A paste was prepared from the slag
powder, graphite, and cobalt oxide (1:2:1) with waterv and placed into
the opening of the anode. The "plasmatron" worked under the following
conditions: 20-22 a, pressure in the chamber 0-4-0-5 atm, electrode
gap 3mm, diameter of the cathode opening 1.6 mm. An ISP-22 spectrograp'-.
was used. A Table shows the analytical lines, Fig. 4 the calibration
diagrams. Line pairs with an exciting potential difference of 10-12 ev
may be used as analytical lines. There are 3 figures, 1 table, and 2
references, 1 of which is Soviet.
Card 2/3

,: 1.
Application of a Plasma Source to the S/032J60/026/05/17/063
Spectrum Analysis of Slags BO1O/BOO5
ASSOCIATION: TsentralInyy nauchno-iseledovatellakiy inatitut
tekhnologii i mashinostroyeniya (Central Scientific aK
Research Institute of Technology and Machine Construction)
Card 3/3

20771
S/05i/6i/olO/OO3/oo4/oio
5'S-9 0o E032/E514
AUTHORS: Korolev, F, A. and Kvaratskheli, Yu.K.
TITLEt The Plasmatron as a Light Source for Spectroscopic
Investigations
PERIODICAL: Optika i spektroskopiya, 1961, Vol.10, No.3, pp-398-4o2
TEXT: The plasmatron employed is shown schematically in
Fig.l. It takes the form of a closed chamber formed by metal
rings I and 2 and the insulator 3. The arc is excited
between the anode 5 and a graphite cathode 4 which is in the
form of a washer, When argon is introduced into the chamber at a
pressure of 0-3 to 0-5 atm, the discharge takes the form of the
jet 1, which in joined to the cathode by the thin conducting loop
11 and is surrounded by a corona made up of vapours of volatile
substances III. *A study was made of the possibility of exciting
a spectrum of high melting point materials and also materials which
are difficult to excite. The specimens to be investigated were
in the form of slag powders mixed with Co 0 and graphite powder.
These were inserted into the aperture in K; anode and the distance
between the electrodes was chosen to be 3 mm. The spectra were
Card 1/4

20771
The Plasmatron as a Light Source... 5/051/61/010/003/004/010
B032/E514
photographed in the 14Cn-A-2 USP-22) spectrograph. A detailed
description of the design of the plasmatron and its operation is
given in Ref.13. Figs. 2CLJ and show the external
characteristics of the discharge (a dependence of length t and
diameter d of the plasma on the current I at 0-7 atm and washer
diameter 1.6 mm; 6 - dependence of i and d on the diameter D
of the aperture in the washer at 20 A and 0.7 atm; 6 - dependence
of .9 on the pressure p. These graphs show that temperature
equilibrium exists throughout the plasmatron jet. The temperature
was measured using t1he FeI and FeIl lines for which the transition
probabilities have been given by N. N. Sobolev (Ref.14). It was
found that the temperature is very dependent on the gas pressure.
Inspection of Figs. 2 to 4 will indicate that the plasmatron can
be used for the spectral analysis of a wide class of high melting
point materials and, in particular, slags. The plasmatron can
also be used to determine the relative oscillator strengths.
There are 7 figures, 2 tables and 16 referencest 7 Soviet and
9 non-Soviet.
SUBMITTEDt May 5, 1960
Card 2/4

KAKABADZE, M.G.; LINDTROP, G..T.; BERNSHTEY14,-A.D.; KHORAVA, G.V.;
KVARATSKHELIYA9 G,M.
Role of farm animals in the tranqmipsion to human beings of lepto-
spirosis of serotype II in the Abkhazian A.S.S.R. Sbor. trud. Med.
nauch. ob-vo Abkh. 2:199-203 159. (1411HA 14: 10)
1. Iz leptospiroznogo otdoloniya (zav. M.G.Kakabadze) Respublilmnskoy
sanopidstantsii Ministerstva zdravookhraneniya Abkhazskoy ASSR (glav-nyy
vrach V.L*'Gvaliya) i Gadautskoy infektsionnoy bollnitey kglavnyy
vrach G.V.Khorava).
. (ABK W IA-, W TOSPIROSIS)
(ANIMALS AS CARUERS OF DISEASE)

-7 1-
XAVTARADU, X.N.; BXRI?SHTEYN, A.D.; KVARATSIMLIYA, G.Ya.
Sources of leptoopirosis in the Abkhazian A.S.S.R. Zhur.mikrobiol.
epid. i immun. 28 no.9:60-63 S 157. (MIRA 10:12)
1. Iz Sukhumskoy madiko-biologicheakoy stantsii AMN BSSR i Respubli-
kanakoy sanitarno-epidemiologicheskoy stantaii Abkhazako7 ASSR.
(IRPTOSPEROSIS, transmission,
carriers (Rus))

KAKABADZE, M.G.j BERMHTEYN, A.D.; KVARATSMIELIYA, G.ya.
Sources of leptospirosis in the Abkhazian A.S.S.R. Sbor. trud. Mod.
nauch. ob-vo Abkh. 2:189-197 159. (MIRA 14:10)
1. Iz leptospiroznogo otdeleniya (zav. MOG.Fakabadze) Respublikanskoy
sanepidstantaii Ministerstva zdravookhraneniya Abkhazskoy ASSR
(glavnyy vrach V.L.Gvaliya).
(ABEWIA-LEPTOSPIROSIS)

KVARATS!4~~4y*,_ 1071-:1
Problem on determining the tropopause. Meteor. i gidrol. Iko.6:
30-32 Ja 156. (MLRA 9:91',
(Atmosphere)

KVARATSKIELIYA, 1. F.
Kvaratskheliya, I. F., T-sutskirifte, A. Ya., ard Kurdiard, I. G.
(State University Thilissi), "The Results of Works in the field of the
Aeroclimatic Characteristic of the Free Atrosphere, on the Analytical
Method of the Treatrant of Observations with Pilot Balloons and Distribution
of Clouds in Georgia."
Report presented at the Scientific Session of Tbilisi Scientific Research
Institute for Hydrometeorology, May 1957. (Meteorologiya i Gidrologiya.
No. 1, 1958.)

KYARATSKMM, I.F.
on of oartain veteorologloal elements over Tifilso
Trudy Thil. NIGNI no~2tll,9-132 1570 (KM& n-.4)
(Tiflis-MlateoroloaY

50-58-4-5/26
AUTHORt F.
TITLEt The Characteristic Changes of Atmospheric Temperature Over
the Southern Areas of the Soviet Union in Altitudes of the
Annual Amplitude (Osobennosti izmeneniya s vysotoy godovoy
amplitudy temperatury vozdukha nadyuzhnymi rayonami SSSR)
PERIODICALs Meteorologiya i Gidrologiya, 1958, Pr 4, pr 21 - 23 (USSR)
ABSTRAM Table Nr I and Figure Nr 1 show the amplitudes of annual changes
in temperature in altitudes of from 0 to 15 km in Tbilisi,
Baku and Tashkent. These towns are nearly situated on the
same latitude but have a differentiated climate. Thereof in
an illustrative way result several peculiarities of the zonal
and vertical changes of these amplitudes. The amplitudes modi-
fy within wide limit on the surface of the earth. These facts
fall into line with the general climatic conditions of the
areas in question. From 4 km onwards the annual amplitudes
of the mentioned townq show fairly equal values. Moreoverg
the amplitudes in the lower atmospheric layers decrease with
the altitude. Tgen they increase gradually and reach maximum
Card 1/3 values (23 - 25 ) in altitudes of 10 km exceeding the values

50-58-4-5/26
The Characteristic Changes of Atmospheric Temperature Over the Southern
Areas of the Soviet Union in Altitudes of the Annual Amplitudes
on the ground. Higher than 10 km the amplitudes deorea8e rapid-
ly and oscillate in altitudes of 15 km betwebn 7 and 9 C. The
magnitude of the annual amplitude in the first kilometers is
strongly influenced by the surface of the earth. The magni-
tude of the amplitude is influenced by the temperatures of
the air masses prevailing during the hottest and coldest months.
The individual, periodical penetrations of relatively cold
masses of air in summer-time concern in general the lower and
middle layers of the air. The increase of the amplitude in
the lower half of the troposphere can be explained to a cer-
tain extent. Table Nr 2 shows the monthly changes of tem-
perature in the same altitudes for Tbilisi, Accordingly the
troposphere is rather intensively heated from April until
July and cools down in the second half of the year. Both
processes proceed according to individual altitude steps
and with a different intensity. Particular interest is fo-
cused on the fact that the farther layers of air are more
intensively heated from May until June and from June unt 1
July than the lower ones. According to the author's opinion
these facts play a greater part in heat supply because of
Card 2/3 advective-dynamic processes compared with the heat radiated

50--58-4-5/26
The Characteristic Changes of Atmospheric Temperature Over the Southern
Areas of the Soviet Union in Altitudes of the Annual Amplitudes
by the surface of the earth. During the summertime mainly
south-west winds blow over Tbilisi in altitudes of 3 - 4
and 8 - 9 km which carry considerable amounts of heat into
the upper half of the troposphere. The process of cooling
the troposphere sets in intensively from August until Sep-
tember but at first in the upper half.'This gives way to
the explanation of a rapid deterioration of the heat supply
from the earth and of the winds of this season. There are
1 figure, and 2 tables.
AVAILABLEs Library of Congress
1. Atmosphere - Temperature 2. Climate - Temperature factors
3. Climate - USSR
Card 3/3

S11691601000101110101016
AOO5/AOO1
Translation from: Referativnyy zhurnal, Geofizika, 1960, No. 11, pp. 124-125,
# 14161
AUTHOR:
TITLE:
KvaratskhelLya, I.F.
------- \rl
The Properties of the Temperature Conditions and the Local Circula-
tion of the Atmosphere Over Sukhumi
PERIODICAL: Tr. Thilissk. nri. gidrometeorol. in-ta, 1959, No. 4, pp. 93~111
TEXT: Investigation results of the temperature conditions are presented
according to radio-sounding data obtained in 1947-1953 and the wind conditions
from observations in the summer season in 1951-1954. The amplitudes of the an-
nual temperature fluctuations over Sukhumi, Tbilisi, Baku, and Tashkent show a
sharp distinction near the Earthis surface, vanishing at the altitude of 4 '.k-m.
The temperature distribution over the altitudes in winter and summer has no con-
siderable distinctions over Sukhumi, Tbilisi and Baku. The comparison of the
vertical temperature distribution in Sukhumi, Moscow, and Murmansk shows charac-
teristic properties in the meridional structure of the temperature field of the
atmosphere. Radiation inversions and others were observed in Sukhumi during the
Card 113

S11691601000101110101016
AOO5/AOO1
The Properties of the Temperature Conditions and the Local Circulation of the
Atmosphere Over Sukhumi
whole year. Tables are added on the frequency of the altitude of,the lower bound-
ary of inversions and thermal equalities, the days with inversions, their power
and ifitensity. The diurnal course of the temperature over Sukhumi is traced in
winter up to 1 km altitude, in autumn and summer up to 2-3 km. The orographic
propetties of the Sukhumi region cause breezes and mountain-valley winds. Either
wind blowing in the same direction, reverses its direction in the mornihg hours.
Thereby, thehigh frequency of calms in the morning hours (66%) is explainable,
which decreases by the evening down to 10% and increases anew in the later evening
hours. The diurnal course of wind direction is traced in summer up to altitudes
of 1 - 1.5 km. The frequency of the west wind changes in the ground layer from
I - 7% in the morning up to 20 - 60% by 17.00 hours; the east wind frequency de-
creases from 20 - 30% in the morning down to 3 - 5% in the evening. During 24
hours, the south-east wind predominates in the 1 - 3-km-layer, the west wind in
higher than 3 km.layer. The high frequency of the south-east and east winds is
caused by the deviation of the west current to the right by the Main Caucasus
ridge. This current deviated and directed along the ridge converges in the moun-
Card 2/3

S/169/60/000/011/010/016
A005/AO01
The Properties of the Temperature Conditions and the Local Circulation of the
Atmosphere Over Sukhumi
tain passes and furthers the orographic local pressure increase, giving thereby
rise to the inverse air diffluence. The average wind speeds up to 1 km altitude
increase in the day hours (from 5 to 17 hours). In the 1,5 - 4-km-layer, the
average wind speeds in daytime are lower than those in the morning. This is ex-
plai:nable by the turbulence developing in daytime at the mountain slopes, which
causes the inverse currents. V. Shtal'
Translator's note: This Is the full translation of the original Russian abstract.
Card 313

KVARATSMMITA, I.F.
Genesis of 'Laminnted structure of the tropopause. Trudy Tbil.N.IGM.
no.5:6Z-90 '59. MU 13:6)
(Tiflis--Atmospheric temp,)rature)

MUTSMMITA, I,F.
Pffect of the main Caucasian range on the temperature regime of the
free atmosphere over the central part of Transcaucasia. Trudy Tbil.
ITIGMI no-5:102-106 159. (MIRA 13:6)
(YAneralIny7e Vody-Atmos,:,herie temperature)
(Tiflis-Atmospheric temperature)

KVARATSKHELITA.- I,F.
--------
Characteristics of altitudinal variation of some meteorological
elements over Tiflis. Trudy Thil.NIGMI no.6:69-77 10.
(MIU 13:5)
(Tiflis region--Meteorology)

S/109 62/000/011/050/077
D228y,)307
AUTHOR: l(varatslcheliya, I.F.
~-aln Fcimiatic -fe
TITLE atures of the free atmosphere over
the Georgian SSR
PERIODICAL: Referativnyy zhurnal, Geofizika, no. 11, 1962, 76,
abstract 11B240 (Tr. Tbilissk. n.-i. gidrdmeteorol.
inLta, no. 10, 1962, 25--70)
TEXT: The author cxmines the temperature, pressure and
air humidity conditions according to radiosonde data for Suldiumi- in
1947-1952 and Tbilisi in 1933-1952 and the wind regime according to
pilot -balloon observations at Sukhumi,. Ba~umi, 1~utaisi wid Tbilisi.
The ground-surface temperature distribution caused by physico-geo-
graphic peculiarities of the Georgian SSR is distinguished by great
diversity, which becomes smoother from a height of 3-4 ku. In Jan-
uary the average ground-surface temperature varies from 5.90 at Suk-
humi to 1.20 in Tbilisi.' The temperature over both points reaches
-100 at a height of 3 1cm,.but falls to -540 at a height of 10 km.
Card 1/4

'3/169
0 /62/000/011/050/077
Main climatic features D228/D307
On the ground the mean July temperature is 23.80 at SW,:humi and
24.10 at Tbilisi. It equals -31.70 and -30.50 respectively at a
height of 10 Imi and -51.40 and -53.70 respectively at a height of
-)erature in January varies from_ 0
15 km. The minimum tem, 7 (Sukhuni)
to -140 (Tbilisi) on the ground and respectively from -590 to -650
at a height of 10 1cm. In July it varies from 140 to 160 on the
ground and -510 to -480 at a height of 10 1m. The amplitude of the
mean annual temperature changes from 17.9 0 at Sukhumi to 22.90 at
Tbilisi. The rai-ge diminishes with altitude in the first bottom
layers of the troposphere, then starts to increase, and reaches a
maximum at a height of 1.0 1cm. The vertical gradients and diurnal
variation of the temperature are considered, as is the temperature
difference in the free atmosphere and at alpine stations. The bot-
tom of the tropopause was defined by a vertical temperaturc gradient
equal to 0.200/100 m; the height, where isotherms of large thickness
begin was taken for its top. At Tbilisi the average height of the
bottom of the tropopause fluctuates from 10 km in January to 15.9 km
in july. Its actual values were observed at heights from, 7-8 to
17-18 km. The air pressure decreases with altitude by 9.0-9.5 mb
C ard 2A.

S/169
,/62/000/011/030/077
Main climatic features ... D228/D307
per 100 m in the layer up to 5 Ian, by 5.5 mb in the layer 5-10 Icm,
and by 3 mb in the layer 10-15 1Qn. The average pressure equals
537 mb at a height of 5 km, 259-261 mb at a height of 10 km, and
120 mb at a height of 15 km over Tbilisi. In July the average pres-
sure at heights of > I Ian is higher than in January. During the
year minimum specific humidity values are observed in January. The
4verage January specific humidity varies from 4.2 r/l-.g neai- SuIchumi,.
to 3.2 g/kg at Tbilisi on the ground and from 0.6 to 0.7 g/kg at a
height of 5 km. On the ground the average July specific humidity
changes from 14.3 (Suhhum:i) to 10.9 g/jcg (Tbilisi); at a height of
5 km it varies respectively from 2.9 to 2.6 g/kg. Near Sulthumi the
moisture saturation from the ground to a height of 4-5 km is higher
in summer than in winter. The effect of local winds that are obser-
ved in many Georgian districts is smoothed as one moves away from'
the ground and becomes scarcely noticeable at a height of 3-4 km.
Minds of the easterly quarter.prevail (70%)!to a height of 1.5-2.0 kn
in winter in the vicinity. of SuIchumi. The frequency cf westerly
winds increases in summer. Winds of the westerly-quarter prevail
from a height of 3-4 Ian. 'At a height of.S'km their frequency is
Card 3/4

S/149/62/000/011/050/077
Main climatic features D228/D307
7Vo in January and 74*X* in July. At Tbilisi north-westerly OP W;)
and south-easterly (- 30%) winds predominate to a height of 1.0-1.5
1%x in winter and smiter; above 2 Imi in winter and Lt IMI in _-urmer
strong winds ( >,, 30 M/sec) mainly have the directions of the N%rester-
ly quarter. In winter in the layer 0-1 km the average wind speed
reaches 5-8 M/sec, i.e. 2.5 times higher than-at Sukhumi. The
author reckons the observed maximum wind speeds (35 M/sec in winter
and So M/sec in sumer at Tbilisi at a height of 10 1m) to be too
low, since pilot balloons were launched at a weather-vane wind speed
of not more than 20 m/sec (at one of up to 24 M/sec at Rutaisi).
L Abstracter's note: Complete translationj
C ard 4/4!

AID Nr. 981-3 3 June
CONFERENCE AT CENTRAL AEROLOGICAL OBSERVATORY (USSR)
Meteorologiya i gidrologiya, no. 3, 1963, 60. S/050/63/000/004/002/002
The followina 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 altitudes qf 7 to 11 km,
certain peculiarities of the meBostructure 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.
Shmeter -- the process of cumulonimbus cloud development and a proposed
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

AW Nr. 981-3 3 J=8
COMMV= AT CENMAL AEROUGM= [Cont'd] S/050/63/000/0"/002/002
accurate form proposed for writing sueb'equationsj 4) 1. F. Kyaratskhell a --
conditions for the formation of sharp changeEl of vertical w.ind shear in th e
upper half of the troposphere over the Transcaucasus; 5) A. 1. 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. Shup'yatskiy -- certain radar criteria
for identifying the hail content of clouds and criteria for evaluating the effect
of cloud modification; and 7) A. G. Gorelik -- certain rjesults of radar inves-
tigations of the wind field at altitudes of 50 to 700 m. [ET]
Card 2/2

ACCESSION NR.- AR4015482
SOURM M. Geofiziks, Abs. 12BWO
AUTHORt Xvaratskheli ,.1. F.
YS
S/0169/63/000/012/MBB/BO88
TMZ: Influence of physico-geographic conditions in the Caucasus on the tempera-
ture regime of the free atmosphere
CIM SOURCE% Tr. 7Akavkazek. n.-I. giarometeorol. in-te... vy*p. ll., 196% 54-59
TOPIC TAGS: temperature regime,, free atmosphere,,. physico-geographic conditions,
atmospheric temperature sounding, air temperature) Kazakstan
TWSLhTION: It is shown that physico-geograFhic conditions in Kazakhstan have a
direct influence on the regime of air teiVerature in only the first lover kilometers.
This conclusion was made after a detailed consideration of the problem based on tem-
perature sounding of the atmosphere during Januar7 and JulY in 1953 and 3.954. At
high altitudesj, the atmosphere's temperature regime is determined by the general
circulation vhich is characteristic for this region. D. Yskovlev.
Das Am: o9jan64 MM COM: AS,, PH =M: 00
Cwd 1/1

ACCESSION NR: AR4015483
SOWM RZh. Geofizika, Abs. 12B461
AUTHOR: Xvaratak'hel:Lya,. -1.,.
8/0169/63/000/012/BO89/BO89
TITLE: Notes on climatic characteristics of the free atmosphere over the Armenian
SSR
CITED SOURCE, Tr. Zakavkazsk. n.-io gidrometeorol. in-ta, vy*p. 12, 1963, 21-42
TOPIC TAGS: climatic characteristics, free atmosphere, air temperature, wind
speeds, air pressure, tropospheric heating, stratospheric heating~ atmospheric
heating, orography, gradient temperature
TRANSIATION: Characteristics on the distribution of temperature, pressure, humidity
and wind over the Armenian SSR are given according to radiosonde data in Yerevan for
1949-1953 and pilot balloon observations for 1933-1935, 1937, and 1939-1952 in Yer-
evan and for 194~-1952 in Mazra. The mean air temperature at altitudes up to 15-km
has a well-expressed annual variation with a minimum at altitudes of 0-9 Im in
January, and higher in February; a maxim= up to an altitude of 4-km in July-August,
and higher in August. The Armenian highlands-'influence the temperature regime of
Card 1/3

ACCESSION NR: AR4015483
Yerevan- This influence can be traced in winter up to altitudes of 2-3 km, and in
summer up to 4-5 km. The difference in mean temperatures in January between Yere-
van and Tbilisi drops from -5-40 near the earth to -1-20 at an altitude of 134m, and
above this it fluctuates within small limits. In summer at altitudes of 1-2 -km in
Yerevan it, is 4-50 warmer than in Tbilisi, and in the layer between 6-10-km this
difference drops to 10. The process of heating in the troposphere and the lower
stratosphere begins with March but the increase in temperature occurs especially
rapidly from March to April (up to 3-km by 7-80, and above this by 3-60). Intense
atmospheric heating in July is noted, and in addition the atmospheric layers remote
from the earth are more intensely heated from May to July (at altitudes of 9-12-km
by 13-160) than the lower-lying layers (by 8-100). A similar phenomenon was noted
also over Tbilisi which was explained as due to advective factors. Atmospheric
cooling is especially noticeable in September and it begins with the upper tropos-
phere (at altitudes of 8-12-km by 6-70, and below this by 40). In the following ~
months the most.intense cooling is noted in the lower 3-km layer. Extremal. values
of temperature at an altitude of 5-km fluctuate from -380 to -90, and at 10-km,
from -640 to -210. The annual temperature amplitude i~ Yerevan is larger than at
other points where sounding was made in the Transcaucasus. Up to 4-km it decreases,
but above, it fluctuates from 1-20. In all points up to 5 _6-km the amplitude de-
creases, but thereafter up to 10-km it again increases. In the cold six months of
card 2/3

ACCESSION NR. ARW15483
the year, small vertical temperature gradients are noted in the lower 2-km layer,
which are caused by cooling of the lower layers and in the summer months from the
earth up to 4-5 km the man monthly gradients exceed the adiabatic moisture grad-
ients. The'tropopause height increases from 10-11 km in winter to 15-16 km in sum-
mer. The annual pressure variation corresponds to the temperature variation. The
annual pressure amplitude (from mean monthly data) decreases from 13 mb near the
surface of the earth to 6-7 ub in the 1.5-2.0 km layer and thereafter increases to
21-26 mb at aititudeB of 6-13 km. The variation of moisture content also corre-s-
ponds to the change in temperature. The specific humidity of the air up to 1-5-2.0
km slowly drops with altitude and above this the drop occurs rapidly. In winter
the relative humidity is higher than in summer. The annual range of mean monthly
values of relative humidity decrease from 30-40% in the lower 5-km layer to 20-30%
in the layer between 5-10 km# The influence of physico-geographic conditions on
the wind regime over Yerevan and Mazra in the winter months extends to an altitude
of 2-km and in summer up to 4-km (winds from southern and eastern directions pre-
dominate). Higher winds from the western quarter are most frequent. Minimum wind
speeds in the lower 2-km layer of the air are noted in winter in connection with
the stand-still of cold air. Maximum speeds in this layer are observed in July-
AusuBt during intensive development of mountain-valley circulation. In the 2-7
t km layer greatest speeds are noted in the cold half of the year. A. Buz.
DATE ACQ: o9jan64 SUB COLE: ABp PH ENCL: 00
Card 3/3

VARAT."MIdYl., '*,F,
JG-L atx.2~~atj and tbs c,mdi t, ~,nn ,,f thc, f cn7a I-fc n r..' En~-rp vt~-- ~,4 c a I
Aletirs of velnr-..-.ty ~m -,(!.,per ha-'d' --'L' thr- tr.~--osphe:,f- --irez,
Trantiraunasia. TI-idy MINIGIM!" I (4f,
(min 18~,Lc)

T UR/()16q/'65/0x/CK)-5'/B0j; 1/13 V; 2
551-557-5
SOURCE: Ref. zh. Geofizika.. Abs- 6B255
AUTHOR: Kvaratskh
TZ"VIE: Jet currents.and conaiticas.:Leading to the formation of vertical shifts in
-the troposphe ab nuscauctisia.
vind. velocities in the upper half of re ove Tra
4- CrM SOURCE -!kr. -52
'gidr6meteorol. in-ta vyy. 15(21), 1964, 21.
TOPIC TAM win d,, jet stream, wind wind velocity C'A"oj&Wr;e wrvev-r
MAMIATIOTI: After a year of.probing, statistical charazateristics wre obtained for
jet currents and vertical wind shifts above Thilis i. The maximum repetition of jet
fiows occurs at the end of summer and in autumn. The altitude of.the axis of a jet
above Transcaucasia is 11-12 km in summer, and 10 Im in winter; the velocity of the
wind is 40-42 m/sec in vinter, and in suzim.-r (July through September) it is 44-51 m/
see. The maximma velocities do not exceed 60 m1sec In January or 51 m1sec in Decemberl
The mulmum recurrences over Transcaucasia are registered for south-eastward cttrrenta, -
and tbe minimum for north-westward currents. Wo cantward currents were noted. The
It maximum recurrences of sharp vertical wind shifts occurred at the end of summer and
autwnn, i.e., during the period of max-Imign occurrences of jet flows. The average al-
Card I

ULM
L 16728-66
ACC _f4g: AR5016457 0
titude of the lower boundary of abarp positive.sbifts in winter was about 7 I= in
winter and 8-9-5 ka in summer. Wthe start of positive shifts, the avera,,~e al-----
is 2-3 km lower than the altitude of the jet axis., The average altitude of the jet
axis with a sbar_
'o positive shift is 9 I= in winter and 11 ka in summer; the average
ranp of the shift is 111-15 m1see per - 1 Im., The lover boundary of sharp positive
~bifts ir. most frequently found at levels from 6 to 11 1va. There are cases, occurring
either -in winter or in summer, when the boundary descends to 4-63 laa. In . smner it
may rise to 12-13 I=. Therefore,, planes flying above Transcaucasia are apt to en-
counter bumps within a wide range of altitudes. Sharp positive shifts begin at a
great variety of,vind velocities at their lover boundaries: Sharp shifts have been
registered at 3-10 M/sec., as well as at 30 m/sec. Negative shifts begin mostly at
arvitudes of 10-11 12a. In summer,, no sharp decrease in wind velocities is observed
be]/xr 12-13 1m. The folla4ing characteristics of both sharp positive s hifts and sharp
negativeshifts of over 25 M/Sec are described: The relation tothe altitude of the
jet., the average velocity of wind at the lover boundary, altitude of the lover bound-
ary, average velocity of the windin a jet flow., and the altitude of the tropopause.
It 1#as concluded that sharp vertical shifts axe observed not in the viciidty of the
jet axis altitude, but in the zones of frontal division. In order to judge the pos-
sible location nf the zone of great shifts, it, is sufficient to knov the spacial loca-
tion of troposjpheric fronts. The conditions leading to the formation of vertical
shifts are analogous to the-conaitions necessary for originating jet flows. In winterF
the basic factor in the formation of jet flows above Transcaueazia Ues in ineridional.
Card2lz
~7

ACC NL- AR50V~57
0
I procezaes and a vimultaheous flux of cold tawardc the southem parts o&" Che Et=i~ean
Terxitory'of the Soviet Union, vhicb =me great contrasts in temperatures (riaxL
at a 5 leme I) - In si r, the basic rt--Bon leading to the fmootion of jet 'flows
i atal
45 In the influx of tropical air=a the foxmtIon, of n IntittAinally locatol 'ro
al
zom,:Vhich sceetimes encire'Ims 'Lue wbole earth. In su=er., the greataut hori t
teq,-~ratuxre gra-dient, (I..214'/IW km) is, Imatc-a u% an altituile of 9-10 lan, Whiz re-
sults In a stsMere& increwe In vind mlocity. in the uppmr troposphere, the %Iorl-
zax"PaI gradients of tmagimamtaw an greater than in winter. "Ehis -pbenome-non ex-
plsiw the faiat that despi-te the average velocities above moatrato
Intituaes are encomteve& mm in summer than, in vinter. 25 references D% NmLov
SUB COOS.
OV
CWd '-4~
pg-
7

L 28487-66 EPF(hb-2jM(1)W% (m)"(f)IM(m) IJP(c) AT
A~C NRI'-.~AP6013136 SbURCE-CODE.- IIR/0057/66/036/OD4/0759/0762
[AT
yartskbavs,.I6F,,; Meladze,R,,D,; Khautiyev$E.Yu.; Reshchetnyak, N,G,
DRO: none
rmst on reasons for the4imitatio of the velocity of P~asr
n Wft In rail accelerators
SOME: Zhurnal tiskhnicheskoy.';izIki,* v. 36, no. 4, 1966, 759-762
fOPIC TAGS: plan" accelerator, plasma acceleration, rail accelerator, plasmold,
plasma un
9
TRACT It is suggested that the reason why the velocities of plastaoids in rail
ccelerators- are mare.than.an order.of magnitude lower than the possible stationary
rift velocities in the crossed fields is.that not'one plasmoid, but a chain of
uccessive
'plasmoidet is formed in 'the accelerator. Experimental,dato are reviewed
ich indicate that a number of plesmoids are in Tact produced; the failure to observe
Itiple plasmoid production in some experiments is ascribed to the complexity of the
enomena that can arise. The mechanism of multiple plasmoid production is discussed.
be,repeated breakdowns giving rise to the successive plasmoids reduce the applied
tential, limit the velocity of the plasmoids, and regulate the quantity of accel-
rated plasma4, It is argued that currents will circulate between the successive
I smoids of the chain, as a result of which most of the discharge current will be
la
.aarried by the first and last plasmoids of the chain and the intervening.ones will not
IUDC: 523a9
Card 1/2

KNARATSYMELIYA, 1.
"Determination of a rational type of primary unit for mountain rivers."
Dissertation for Candidate of Technical Sciences, Aeerbwjdzhan Institute, Baku,(AKII)
Subject: Hydroengineering building and construction
Gidrotekhnichesk2ye, stroitellstvo, 12, 1946.

USSR/Farm Animals - Silk-Worms. Q-9
Abs Jour : Ref Zhur - Biol-, No 1, 1958, 2697
Author : L. Kyaratsliya
Inat
Title A Determination of the Silk-Worm Egg Yield by the Average
Weight of the Cocoons.
Orig Pub Tr. Gruz. s-kh. in-ta, 1955, 42-43; 398-399
Abstract The higher is the average weight of the cocoons, the
higher is the fertility of the emerging femLles.
Card 1/1
KIVARATahELIYA, 14.3.
"Fias of Abldiaziya." Gand Biol Sci, Inst of Botany, Acad Sci Georgian
U
SSR, 27 Dec 54. (Ti, 17 Dee 51+)
Survey of Scientific and Technic&-l Dissertations Defended at USSR
Eigher Educational Institutions (12)
SO: SLm. No. 556, 24 Jun 55

, KVARATSKMITA, M. S.
Self-fertility and self-sterility in seedlings of certain faijoa
varieties. Agrobiologiis, no-5:782-785 S-0 160. (MIR& 13:10)
1. Sukhumakaya opytmya stantsiya aubtropichaskikh kulltur.
(Peijoa) (Fertilization of plants)

KVARATSKHELIYA, M.S.
BioloFy of the fertilization of pecan in humide subtropical areas.
Agrobiologiia no.1:151-154 Ja-F '62. (MIRA 15-3)
1. Sukhumskaya opytnaya stantsiya subtropicheskikh kulltur.
(Fertilization of plants) (Pecan)

f"~ M/!
DAVYDOV, F.G., kandidat ~el 'skokbo%yayatve-,wykh nauk; KVARATSKEMLIYA, M.T.,
I'mndidat nauk.
Using the Davy(lov universAl seed disinfector (PU-1) for conting
seeds vitq phosphobacterla. Dok'~-1knd.sellkhoz.22 na.5:44-43 157.
(miaA IC): 9)
1. VseacraziVy nauc'~-inr;-iseLeiovate'A.Iat:iy institut sellskokhozypystvennoy
,mL --obiz)logli. Pre,'Intavleno akRdemiko
m I.I.Samoylovym.
(Seeds) (Bacteria, Phosoborus)

KVARATSKHELIYA, M.T.
- bacterizing seeds with dry phoaphbrobacterin,
Trudy Vses. inst. sellkhoz. miktobiol. no.14:252-256 '58.
(MIRA 15:4)
(Bacteria, Phosphorus) (Boil inoculation)

KVARLTSMMLIYA, Mj.
Simultwrous treatment of seeds with phosphorobacterin and
disinfectitn with granooan. Zemledelie 24 no.7153-55
il 162. (MIRA 15:12)
1. Vaesopuznyy nauchno-iseledovateltakiy institut
sell skokhozyaystvemoy, mikrobiolog" -
(Seeds-Disinfoption) (Grawsan)-
(Baoterlaf Phosphorus)

-VARATF~~LIXA,-Nj~
Effectiveness of bacterial fertilizers& Mikrobiologiia 31 noopt
1102-n06 rv-D f62, (MIRA 16,3)
1e Teesoyuznyy nauchno-issledovatellskiy Imstitut sel'skokho-
zyaystyennoy mikrobiologii.
(SOIL INOCULATION)

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KVARATSEMLIA, '~. T.
Growth of sprouts on a lemon tree. Soob.AN Gruz.SSR 8 no*7:447-451
147, (MIR& 9:7)
l.Akademiya nauk Gruzinskoy SSR, Botanicheskiy institut, Tbilisi.
Pradatavleno chlenon-korragpondentom Akademii D.I.Soanovskim.
(Lemon)

RIAC of Olganti-minefal Compounds Ill Patuctute fouttation
of subtropical podralic soil Ab. In .
I'S V- 9
121% 10.41t till 10-1.- :11.91 (hg
h-11111)VO. did 11ol AM-1 ."I 'llmiull,' %Iwl', 1~.frnliwl
!rta'" '61. Me rmll* ill it, It 1-1 1 -JAI ; m hile
Will plIfting thev wl.t l1w -d aml I'mu'l l1w.l.
.. . .............. ..
1% ml 11M.H..1 9 114
",,VI %ill-, t, g . ,,I , I % Al't,
"Ollip ukhrls. did mAttlor I'mm k(A.I.- .4KAII-I ... 1',- 1-1
Owit pht. pwl~lll-
%I ii-Il

The in"bamism of structure formation with pertrinial
under conditions of the hurnid subtropics of the
Caticasiri X_ 1951.
,it" 1) 1 it ~a nmij,.m it,*,- zittictitral
I,. -id tv,t,l,t,jlII -11~ "till.
4 Ihe humid A], hare 1'. 1-- ., lugh
mic"-1 ritet tire -labilitv theii cImiluticA %ith t1w j..D,4ir,tl
-i1% It i. thm the varl I.- rt.
pl'ifilvil .41 Ille It'l.it of tile f"ttlialioll "f 'Xicillm.lin't.61
.(,e,-.fi, Al %. III I (Ittv .(,-I, I :I fit I Im JoIr N,().
11 S j - 414-

UARATSHMIYA, N. T.-, DZHUG-ELI, D.M.
Grasses -
Perennial grasses in humidp subtropical regions, Kom.baza. 3 No. 6, 1952
Montdhly List of Russian Accessions, Library of Cohkress, September 1952. UNCLASSIFIM.

1. XVARAT-9HKRI-IVA, H T., BERDZENSHVILIp L.I.
2. USSR (600)
4. Citrus Fruits
7. Intercropping a citrus orchard with perennial grasses. Sad i og. no. 11.
1952.
9. Monthl kLs_t q_f Rus�1 Accessions, Library of Congrass, March 1253, Unclassified.

I
PTARAT'SIMM YA, N. T.
Podzol
Effect of perennial grasses on the improvement of the Pir and water repims of podzolic
5oils in the subtropics, Dokl. Ak, ,,,ell khoz, 17, No. 6, 1952.
9. .7!,onthiv List of Russian Accessions, Librnr-v of C,,n~.--ress. Cetober 1952, TIM-

KVARATSnELIYA, N. T.
"Fodder-Grass Cultivation in Subtrapical Conditions of the kkhazian USSR." (Dissertation
for Degree of Doctor of Agricultural Sciences) Min Higher Education UISSR, Georgian
Order of Labor Red Banner Agricultural Inst. Tbilisi, 1955
SO: M-1036 2P ~~r 56