SCIENTIFIC ABSTRACT VETISKA, A. - VETLUGINA, K.F.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001859620016-3
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 1, 2001
• Sequence Number: 16
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

VETISKA, Aloe., doc.0 inz., dr.; SVBJCkR, Ari
Problem of verifying hardness testers. But liety-26 nc,.9:664-666
1, V~soke*uceni technickes Brno.

OBRLZ) LT., l.nza,, C.Sc.; VETISKA, A.,-inz., dr.. C.Sc.
'Now-methods for determining the elastic constants of
materials. Strojirenstvi X no.10:7$8-.773 10 0 162.
Is St4it-ni vvzl-.u=y ustav tepelne teohniky, Praha (for 013raz).
2. Vyooke uceni technicke, Brno (for Vetiska).

VETISKA, A.; TILL', A.
Contribution to the study on a dynamic impact test.
P. 37. (WNICKE LISTY.) (Brno, Czechoslavakia) Vol, 13,, No. 1. Jan. 1958
SO: Monthly Index of East European Accession (EEAI) LC. Vol. 7, No. 5, May 1958

-AUTHOR: Vetii.~ka, Aleg, Docent Ing. Dr. CZECH/34-59-1-6/28
TITLE: Contribution to the Study of the Defomation of
Spheroidal Cast Iron and of Soft Steel,. (PHspgvek ke
studiu. deformace tvarn(f litiny a m6kke' oceli)
PERIODICAL: Hutnick4 Listy, 1959, Nr 1, pp 30-38 (Czechoslovakia)
ABSTRACT; The micro-Btructure of the spher0.dal iron selected for
the tests consisted of a ferritic baset with inclusions
of spheroidal graphite of a regular shape with rare
occurrence ofislandsof partly globular pearlite. The
COMPOBition of this iron was: 3.24% C1 2.7% Sit 0.64% Mn.
0.099% P, 0.00?% S and 0.043% Ms. For comparison tests
were also made on a standard structural rimming steel
(CSN '11 341) the micro-structure of which contains
small quantities of pearlite embedded between the grains
of the basic ferritiC structure with a carbon content
varying between 0.08 and 0,10%, The process of
defoniation was studied on cylindri.cal specimens
10 mm dia,, 15 mm high which were upset with a slowly
increasing force or by impact, The loading speed was
selected to correspond to the speed of shaping by
Card 1/4 pressing and forging. Static upsetting was effected b
Y

07,ECII/34-59-1-6/28
Contribution to the Study of the Deformation of Spheroidal
Cast Iron eLbd of' Soft Steel
means of a universal Amsler machine which enabled
changing the loading speed within the range 0.7 to
47 mn,/see. Upsetting by impact was effected by means
of a special pendulum hammer with piezo-electric and
photc-electric recording apparatus; the speed of loading
varied between 0.5 and 5 m/sec. The hammer was
adjusted so as to enable impact compression tests to be
carried out, A special device on the-hammer enabled
deteimination of the reaction energy due to elastic
defoxmation of the specimen; the values of the energy
required for elastic and plastic deformations during
the first, second third fourth and fifth impacts are
entered in Table i, p 32! The progress of the plastic
defoimation of the Spheroidal iron as well as of the
soft steel during tne impact tests (five impacts) are
graphed in Fig 6 whilst the increase in the energy
required f03~ producing elaotic deformation is graphed
in Fig ?. The changes in the micro-structure and in
Card 2/4 the sub-microstructure during deformation were also/
~17

CZECH/34-59-1-6/28
Contribution to the Study of the Deformation of Spheroidal Cast
Iron and of Soft Steel
studied and some of the changes are illustrated by the
microstructure photographs reproduced in Figs 9-12.
According to micro-hardness measurements, static
deformation of spheroidal iron and soft steel brings
about a considerably more intensive hardening of the
ferritic grains than equivalent impact-produced
defozmation (see Table 3). Electron-microscope studies
yield;.ed further information which is discussed. The
influence of repeated static loading and a combination
of static and impact loading were also tested and the
relevant final deformations are entered in Table 4, p 36.
Compared with soft steel, the ductility of spheroidal
iron is smaller. At high reductionsunfavourable
structural transformations occur which may cause failure.
However small reduction are not dangerous for ferritic
spheroiaal iron because they do not damage the structure;
for such small reductions the forces need to to only
slightly higher than for soft steel. The overall elastic
properties of the spheroidal iron do not chango as a
Card 3/4 result of the shaping and the material retains a high
V

CZECH/34-59-1-6/28
Contribution to the Study of the Deformation of Spheroidal Cast
Iron and of Soft Steel
reeistance to impact loading. In the case of very large
reductions, the presence of spheroidal graphite brings
about a stress state which differs from that pertaini
to mild steel and causes fracture. It was found that if
preliminary deformation of' spheroidal iron and of steel
is effected by impact loading, further static deforma-
tion can be achieved more easily and with smaller
forces than can be achieved if the preliminary deforma-
tion to the same degree of reduction would be effected
by slow (static) loading. This feature can have very
usefUl practical applications.
There are 22 figures, 4 tables and 21 references,
7 of which are Czech, 6 English, 3 Soviet and 5 German.
ASSOCIATION: V& Brno LI-11
SUBMITTED: September 17, 1958
Card 4/4

VETISK1110 A.
International eeminar on superoonip. defectoscopy in Stary "im-okovec.,
Hut listy 16 no.!:.64-66 Ja 161.

PUNICOCIIAR Z.., im; KRUTIM., F. p inz,; HM- K, A.: VETISKA ~.
.9 - I :~~
Inform.tions on metallur&7. But listy 16 no.l-.68-72 Ja 161.

IVETISKA, A.
I "Thaoretical principles of founding" by Josef Pribyl. Reviewed
by A..Vetiska. Slevarenstvi 10 no.?:Z78 J1 162.

VETISKA, Alets; HERRON, Vladimir
Problems of the movement of molding mixtures in high pressure
moleLing. Slavarenstvi 12 no.11%431-435 N 164.

doe. dr. inz. GSc.
Effect of the gas flushing -' malt on the gray cast iron
quality. SlavArenstvi 13 to.'It8-14 Ja 165.
1. Chair of Founding of the Higher School of Technology,
Brno,

VETISKAI Also
Vew trends it evaluation of the quality of grey iron castings.
Slevarenstvi, 10 hoJt85-90 Mr 1W.
1. Vysoke uceni technickes katedra slevarenstvip Brno,

-2/612/010/001/002
Z/032/C
El6o/E435
AUTHORS: Obraz, J., Engineer, Candidate of Sciences,
Vetiskaj A. Doctor Candidaie of Sciences
Engineer,
,TITLE: New methods for the determination'of elastic moduli
[E, G and the Poisson's ratio3.of materials
".PERIODICAL: Strojfrenstv:r, v.12, no.10, 1962, 768-773
TEXT: A new method, using ultrasonic. pulses* is described which
is suitable not only for homogeneous bilt. also heterogeneous
materials, the latter category being represented by cast iron.
In suitable cases this method can be applied to finished machine
components, One of the advantages is that7standard equipment,
normally uned for detecting defects inside a material, is employed.
Large samples are more silitable; in oases of small samples or at
elevated temperatures distance 'bars are useo. Final computations
of elastic moduli and Poisson's ratio are based on the equations
where these constants are expressed in terms,of density and
longitudinal and transverse velocities of propagation of ultrasonic
waves.' These velocities are determined as follows: pulses are
sent longitudinally or tj~ainsversely through the sample and the
Card 1/3

KMA
Z/032/62/012/010/001/0b2
New-methods for the deteir6nation ... E16o/E*435
original pulijes as well h's their reflections are displayed on the
screen of tho standard equipment for detecting'faults in mater *ials..
-Y
Propagation velocity can'be determined either directly from such a
recording, provided an accurate time base in available, or by
comparison with some medium of known ultrasonic velocity. In
cases where transverse velocity cannot be determined directly, use
is made of transformatioft of longitudinal into transverse waves,
Samples of special shape"4an sometime's be made (semi-circular
section) which facilitate such determination. In cases where
special or suitable sampll'es Cannot be made, surface ' waves are
measured inittead of trariaverse ones (e.g. in sheet metal). Sharp
edged obstacles are lightly pressed on the surface of the material
at suitable intervals apart and at right anglem to the path of the
ultrasonic surface wave." The relation in given expressing the
surface ultrasonic wave Yelocity in terms of Poisson's ratio and
the transverse velocity. In the case of circular bars both
longitudinal and transver*e velocities are obtained simultaneously.
Due to a certain amount of divergence in the init lakting
longitudinal beame a part or it rails an the c:rlindrical portion
Card 9/3

Z/032/62/012/010/001/002
New methods ror the determination E16o/E435
and proceeds at an angle across the bar as a transverse pulse.
This can be separated on the display screen from tho-longitudinal
pulse since it takes longer to travel the length of the bar.
The authors have carried out comparison tests using eleven samples
1.-'of cast iron of varied quality and the roso nance-method for
checking the ultrasonic wave method. Generally, the results
agreed within + 7%- Calculation procedure for the moduli is
given for ono 3f the samples. There erre 9,figurea and 2 tables.
ASSOCIATIONS.-"SVTT, Prague (01braz-, J.)
VUT , Brno (Vetiika
4rd 3/3

Z/034/61/000/001/016/021
E073/E535
AUTHOR: Vetiska, A.
TITLE: titir-nitional Seminar on Ultrasonic Defectoscop Held
at Stary Smokovec
PERIODICAL: Hutnickle' listy.,, 1961, No.1, pp.64-66
TEXT: 'The seminar was held on November 14-26, 1960 in
Stary Smokovec on ultrasonic defectoscopy. The first part of the
seminar was Iintended as a basic study of new ultrasonic defectoscopy
methods, the physical nature and applications in research and
industry. The second part was devoted primarily to papers by
foreign guests and discussions. Only people with long experience
in the field with university or sub-university education were
invited. There were about 40 participants. In his first paper,
Dipl.Phys. Ha:as Ulrich Richter of the K, Liebknecht Works
Magdeburg, East Germany,.-dealt with the introduction of ultrasonic
testing for quality control of crankshafts in East German- (instead
of the hitherto applied magnetic tests); the sensitivity of these
instruments is such that slag inclusions above 2 mm can be detected.
It was proved conclusively that the ultrasonic indications are fully
in agreement withreality. In a second paper, H. Richter dealt
Card 1/3

Z/034/61/000/001/016/021
E073/E535
International Seminaron Ultrasonic Defectoscopy Held at Stary
Smokovee
with the possibility of using plane waves for automatic testing of
sheets. In his first paper, Dipl. met. Gerhard Scholz (Zentrale
ftir Prdf- und Entwickellungsstelle des Verkehrwesens - Brandenburg/
Kirchm6ser) pointed out the possibilities of application of ultra-
sonic tests in locomotives. In his second paper, he dealt with
testing locomotive axles and shafts. Ing..jolfgang Zellmann and
Ing. Heins Thorwirti (Oberste Bergbeh8rde der DDR - Institut ftir
Grlibansicherheit Materiel und Seilprilfstelle - Ijeipzig) presented
papers on testing weld seams. Some statistical data on
instruments used in East Germany are given.
Representgtives of MTS (Mr. Danda), CDS (Ing.Prudk- and Mr. Tryta)
y
and UDS MSK(Docent Vetina) were invited to the international part
of the seminar, which was directed by Engineer Medek (Dom techniky
Bratislava). It was agreed that personnel for defectoscopy work
should be basically trained in accordance with the following three
categories:
1) Training to the highest degree by meana'of a 2-semester post-
graduate study at VUT FS,Brno.
Card 2/3

Z/034/61/000/001/016/'021
E073/E535
International Seminar on Ultrasonic Defectoscopy Held at Stary
Smokovec
2) Decent;alizead four week training courses, organized by the
CDS at SVUMT (directov. Engineer Prlw).
~3) International seminar and days for exchanging experience in
defectoscopy to be organized by Dom techniky, Bratislava jointly
with 6SAV.
The training of auxiliary personnel should be the responsibility
of each works,
Card 3/3

Z"1151", A.
Ultlmai~ fatigue of materials and its damping 1,-y intentive surface rolling. p. 648.
HMNICKE LISTY. Vol. 11, no. 11, Nov. 1956
Brno,, Gzechoslovakia
SOURCEs East European Lists (EEAL )Library of
Gongress, Vol. 6, ',to. 1, January 1957
8

A
"Use of Control ty X-Pays in IletallurEy" p. a, (hTTINTY, Vol. 3, no. 4,
Apr. 1953, Praha, Czechoslovakia).
SOt Montb-ly List of East European Accessions, W, Vol. 2, No. 11, Nov. 1953, Uncl.

VMSKAO A.
Katejkat B. I Morevus, J- Effect of rolling on the fatigue 11mit
in alternating torsion* p., 752*
STROJIRENSTVI, Prague, VOL 40 no. lot oat. 1954.
SO: Monthly Ust Of East European Aacessions , (EEAL) , Lc, Vol. 5, No. 6,
June 1956, Uncl.

VETISKA,, A.
Contribution tA3 the study of spheroidal cast-iron and mild-steel de-
formation. p. 30.
HUTNICKE LISTY, (Ministerstvo hutniho pr%uWslu a rundnych dolu a
Caskoslovenska vedecka spoleenost pro hutnietvi a slevarenstvi)
Brno, Czechoslovakia, Vol. 11j, No. 1, Jan. 1959.
Monthly TAst of East European Accession,, (EMI),, LC, Vol. 8,, No. 12.. Dec. 1959.
Uncl.
SI

VETISFA, A.
"The 'Janak' CircvLlar Slide Rule System; For Calculating t~:e Heating Porter of
Fuels, the Amount of Air andCombustion Proft-ts of Technical Fuels" p. 85"
(HUTNIK, Vol. 3, M. 4, Apr. 1953, Praha, Czechoslovakia).
SO: Monthly List of East European Accessions, LO, Vol. 2, No. U, Nov. 1953, Uncl.

DAVID, I.; VETISKA, A.
Inter-national Congress or Foutding in Vienna. Slev&renstvi
9 no.32:485-492 D 161.

Usti**" Fellow 7166040'
llj&l. L No. 11, ISO-233).
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for 4m~A-WAIIns Ammlysio. litul roe flaw dau,441o" In f.#A

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. VETISKA, Ales, doe. inz. dr.
Nondestructive control of castings. Tech praca -16 no. 6s
451-453 Je 164.
I ~
'.1 .1;1 1

.--,-VETISKA, kleel KOLBINGER, Zdenek
New testing method for verification of gray cast iron quality
in castings. Slavarenstvi 11 no.6:221-226 Je 163.
1. Kittedra, slevarenstvi, Vysoke uceni tecbnickep Brno; Zavody
na rrrobu. kulickovych Iozicek, Brno - Lisen.

VETISKA, Ales
Measuring the danping capacity of gray cast, irhff. Slevarenstvi
12 no.6;213-216 Je 164.

I "'- ---
- VETMOV, V"K.
Introduction of the A=ir cork %ree. Bot. zbur. 50 no.2:123~-126 Ja
165. (MIRA 28:3) 1

VETHES, Janos
"Spark machining" by Roth, Kaldos,, Kovacs. Reviewed by JiLnos
Votkes. Gepgyartastechn 2 no-5:178 My 162.
1. "Gapgyartautechnologiall ozerkeazto bizottsagi tagja.

SERENSEN, Bergey VladWrovich; GIATSINTOV, Yevgeniv Valentinovich;
KOGAYLIV, Vladimir PetravicbI STEPHOV, Hildiail NikItovIcbj
PeLnimali uchastiyes BALIZW.;XIY, F.Kq BORODIN., N.A.j PIKIN
I.:Cpj IVANOV,, G.T.; ZASLAVSK3.-Y, B,V,, kand.tekhn.nauk, rtd.s
-90-TIKI A.Ya., te~ft.red.
[Structural strength of airplane alloys] 116natruktsionnnia
pr3chnost' aviatsionnykh splavorv. Moskva, Goa.nauchno-tokhn.
iad-vo obor., 1962. 100 P. (Moscow, Aviatsionnyi tekhnologicheski
inatitut. Trudy, no.54). (MIRA l6s2)
4kluminum aLloys-Testing)

,'Academy jul 49
of Sciences
Electric Power Stations
ver Engineers, Iaureateo of the Stalin Prizeu
-P
_t ]A~LVX OEaDTZ Ivo
UN 1~ okolov-Andronov, Chief Engr,- ORGRES (State
Sf 0
r Orgm and Rationalization of Rayon Power
Ations and Networks), W. S. Vetkin and F. M.
4#rgeyev, ORGRES engineers, an& I. K. Gizhirov
Y
r,,~Ier Shop Fare--an, Thermoelec Sta No Kazan,
~re awarded Stalin Prize for 1948 for developing
04 introducing a method of coal combustion
51/49T1
/Academy of Sciences (Contd) jul 49
ling slag '-- 'liquid for=. M. V. 1-U.1kin,
lef KuvbyBhev Elec Power- Plant,, S. V. Val'ohak.
J,
struction engineer, "Energodetall" factory, and i
W. Manuylov and S. D. Xuchkin, ORGRES engineers,
e awarded Stalin prize for developing and
~troducing aD autcmatic feed regulator for steem
Alers. Collective of workers, Cen Aero-Hydro-
c Inott and A. M. Xamarov, ORGIM engin er,
awarded Stalin prize for developing an& In-
ing new types of ccia-LrIfugal blowera'..
GL.1 Acum
E-

ACC NRI AP6035886 (A) SOURCE CODES UR/0413/66/000jO201012710127
INVENTOR: Smirnov, A. K..
ORG: none
TITLE., Device for measuring roll angle. Class'42, No. 187324
SOURCE: Izabretertiya, 'promystilennyye obraztsy, tovarnyye znaki,. no. 20, 1966, 127
TOPIC TAGS: aircraft control equipment, aircraft maneuver, aircraft stability,
A.LL t-Laf t ins trumen tation, aircraft roll indicator,
ABSTRACT: An Author Certificate has been issued for a device for measuring roll
angle. It contains mechanical-to-electrical transducers and a device which sets on
the transducers (transforms the roll angle into a pressure on the transdLkcers). To
increase sensitivity, the transducer actuating device is in the form of d calibrated
metal sphere located on a heat-treated, polished platform, the degree of freedom of
which'is limited by stop screws. It is firmly secured with flixiblej prestreseed
armat on each of which are fixed two strain gages connected by a bridge circuit.
Orig. art* hast I figure. JWA-981
SUB CODES 01/ SUBH DAM 02Aug65/
Card JZJ UDCt 528.52.716o4

AVDEYEVA, A.P.. lnzh.; META, G.I., inzh.
Distortion of the aample of combaotion products after the
determination of oxygen using VTI and ORSA apparatus.
Tep-.oenergetika 11 no.5:93-94 MY'64. (MIRA 17:5)

ZVORYKIN, IL.Ya.; VETKIMA, L.S.
Solubility isotherm of the system RbH2PO4 - H20 at 25 . Zhw,.ueo
khJz. 6 no.3-1:2572-2575 961. (MM 14:101
lo Institut obahchey i neorganicheskoy kbimil imeni N.S.Kurnakova
AN SSSR.
(Rubidium phosphate) (Ammonium phosphate) (Solubility)

STARODUOTSEVA, A.I.; VETKM, Ye.Ae; KMOVICH, V.L.
Respiration Intensity In sunflover isseds as a function of oil
content* BiAhimezerna n0-5:256-262 f6O. (MM 14:5)
1. 14bakovskiy tekhnologicheaki5r institut pishchevoy proxqzhlennooti,
(Sunflower seeds) (Plants-Respiration)

MIKOV,
--------------
"Iars
Gas, Vrolt- 8 n0-11

-,COP- F. --- --- -- - - - - ---- - --- - - -
P - --- --I
"Remarks on J. Houdek and M. Oppelt's Article 11reatment of flaw Iron
after Tappinj for Recovery of Vanadium. 11 P. 610,
(HUTNIKE LIM, Vol. 9, No. 10, Oct. 1954, drno, Czechoslovakia)
SO: Monthly List of East European Accessions, (EEAL), LC, Vol. Jj
No. 5, May 1955,.Uncl.

VIMUU -esenIYSvn8- agronom-eadovod; KALINIKA, G., red.;
Ar, -I.- :'W~ ,-.,,.,.Vera A.
EAltmi distances] Altaiskle dalle Moskva* Izd-vo TeX TUSK
*Molodaie grardiiao" 1959. 286 p, I (KM 13:2)
(Altai Territory-Description and traTel)

V74ELTIMI, Vera Arsenlyeva; MIATNA, 0. reda.ktor; P3rROVA,]P,. tskhni-
creW,F'r"9Mfbr. ---
[Trips through Crimea] Krymskle puteshostviia. Moskva, IzC-vo
TsK VTJCS-'4 "Molodaia gvardita," 1955. 389 P. (Geog.nauchno-,
khudoz:,,i. serits, "Hasha rodina") (I-ILRA 8:8)
(Crimea--Description and travel)

VETLEA, Vera Arsenlyema; Kll:,?LvAi,,'--SKAIZA, S.N., red.
.-.
(Once again pro3p--cting] 1 sncrre- Moskva,,
- i
Rosslia, 1964. 157 p. (KIRA 1"

YFDI."A 3ec 6 Vol-13/1 Internal Med.- Jan 59-
A caso, i~- th-so.-ribed tir .1-1 it our of the heart in a fernalv patient aged 41,
with a typical clinical pfi-ture (if left atrioventrkmar stenosix with increasing
manifeMationi or cardlovasrular instirricirncy. Active cardint: and antirheumatic
therapy had n,) effect and the patlPnt died with signs of progressive cardiat: fail-
urv. At autopsy a myxonta was found to be growtng from the left atrium on a
slender stalk, The tumour resembled a bunch of krapes and descended through
lite atrinventricular aperture into the left ventrit-le. Its dimensions were 4 x 5 x 8
cm. The tumour firmly plugged the at r Invent ricula r aperture which during tire
gave the clinkat picture of stenosis or this aperture. In addition there was hyper-
trophy of the right ventricle, dilatation of the left atrium, pulmonary oedema and
nutineg liver. (S)

UWR / Phar4acology and Tcmicology. Chemotherapeutic Agents. V-10
Antimalarial, Agents.
Abu Joiw :Ref. Zhur - Biologiya,, No 17.. 19581 No- 80715
Author :Vetloy, F. I.
Inst :Not given
Title :On the problem of the &dicinal Effect of Bibumal
Orig Pub :&d. parazitol. i parazitarn, bolezni, 1958) 27,, No 1, 107
Abstract :BiWM1 (I) was used in 65 patients with three-day mala ia,
in 6 with tropical mal ia, and in 1 with a mixed fom.,
according to the usual method. Iateral effects were not
observed. I cut shcrt attacks in a majority of the patients
with administration during an attack and in the period
betveen them, and caused the disappearance of the excitcr
from the WD(A in 100% of +,~ cases in the first days of
treatment* The influence of a 0.1% solution of I on Pe
relictum (concentration of 1., 1:3000) in the course of
Card 1/2
46

f-
Therapeutic action of biguml. Med.Paraz. i paraz.bol. 27 n0-1:107
Ja-1 138, . 01MA 11:4)
1. Is goopitallnoy terapevtichookoy kliniki Yoroneshokogo gosudar-
etvonnogo meditainskogo imtitua (dire institata - prof. V.P.Jladush-
kevich, save klinikoy - prof. V.S.Nesterov)
(PAWMINN)

Vetlovl, F. I. "Treatment of Nalaria with Bigumal." V oronezh State d inst, Voronezh..
1955 (Dissertation for the Degree of ~.wdilate in lledi~:al S~:ient!ei)
SO: Knizimaya Letopis', Ila. 24, Moscow, Jun 55, Pp 9l-lj4

'-1VM5&QVVm&WkwAwAkd1dat maditsinakikh nw,
Cardiac zyxoma causing insufficient blood circulation. Tracb. dolo.
no.1:85 JAL 157 (KEJU 10: 4)
1. 0ospital"naya torapovtichookaya klinika (save-prof. V.S, Westerov)
. Vorceash okogo maditainskogo Instituta.
(HEART--TMMS) (BLOOD--CIRCULATION, DISMDJRS OIP)

"Fronto'genesis and Conversion of Ifigh-Altitude DEformation
Fields." Thesis J,'or degree ~if Cand. Physiccumthemz-tical
Sci. Sub. /+ Oct ~,% Central Inst of Weatier Forecasting.
Sumary 82, 18 Due 52, Dissertatiov:-t Presented
For Degrees in S dence and Engine-~ring in ~bscaw in
;2~2, Frma Yj%Wirn7ay& Moskva, Jaat-Dec 1949

VLTLOV, IVAN PAVWVlCll 7N/5
623.452
J5
VEnov. IVAN PAVLOVICH
CSADKI KHOLODNYKH FRONTOV V TSKWntAL'NOY CHASTI YEVROPEYSKOY ITRRIROTII USSR V
TEFLCYE VREMYL GODA (SETTLID.G OF COLD FRONTS IN TU CENTRAL PART QF' EUROPEAN
TERRITORY OF USSR IN THE WARM SEASM, BY) 1. P. VE`fLOV I N. V. ENK
ISMGRAD, GIDRCHETEOIZDAT, 1955.
63 (1) P,. MAPS, TABLES.
BIBLIOCalPHY: P. (64)
AT HEAD OF TITLE: LENINGRAD.
TSENTRALINYY INSTITUT PROGNOZOll.

T 1- r Vi - - I-, t~"-
PHASE I BOOK EXPLOITATION 421
Leningrad. TsentralInyy institut prognozov
Voprosy sinopticheskoy meteorologii (Problems in Synoptical
Meteorology) Moscow, Gidrometeoizdat Moskovskoye otdelniye,
1957. 121) p. (Its: Trudy, vyp. 611 1,300 copies printed.
Ed. (title page): Uspenskiy, B.D.; Ed. (inside book): Sadovskiy,
V.N.; Tech. Ed.: Zarkh, I.M.
The article examines a series of problems which might possibly
offer some explanation as to the evolution of cyclones and
Card 1/~
2~-

Problems in Synoptical Meteorology
421
and anticyclones; these problems are still unsolved, despite the
abundance of theoretcial and empirical date. One of these problems
Is the effect of thermobaric field structures on the origin of the
cyclone and anticyclon6, and also on the process of cooling and
warming air by advection. The author analyzes the results of 110
observed cyclones and 82 anticyclones and discusses: (1) The
geostrophic wind velocity along the isobaric levels of 700, 500,
and 300 millibars and the horizontal temperature gradients at
the 500 millibar level in the area of cyclones and anticyclones
over thEarcentral, cold, and warm sections; (2) the advection
of vortices at 700,500,and 300 mb isobaric levels and advective
changes of temperature in the 500-1000 mb'layers over the central
section of cyclones and anticyclones; (3) the changes in the
turbulent a1r movement and their dependence on elevation in the
near-surface layer of the cyclonic area; (4) the changes in the
mean temperature at 500-1000, 300-500, and 200-300 mb levels In
the process of development of cyclones and anticyclones; andfima-
ly (3) the changes in baric.pressures observed during a 12-hour
interval. .411 the points cusidered may facilitate forecasting.
Card 2/7

30)
AUTHOR: Vetlovj 10 P. SOV/50-59-5-2/22
TITLEi Method of Determining Local Changes in Pressure With
the Help of Wind Data (Sposob opredeleniya lokal 'nykh
izmeneniy davleniya a pomoshchlyu dannykh o retre)
PERIODICALi Meteorologiya i gidrologiya, 1959, Nr 5, PP 9-17 (USSR)
ABSTRACTs The task of determining the velocity and acceleration in
the local change of the geopotentials of isobaric areas is
solved here in a manner that differa somewhat from the
methods usually employed. The terms with the vertical
velocity are maintained in the equations of motion, and the
contribution oi the adv ection of the eddy of velocity is
determined with partial use of the hypothesis on the
quasigeostrophic state. In spite of thisp the formulas
obtained for the velocity and acceleration of the change in
geopotential show a comparatively simple form, and are
convenient for qualitative analyses and quantitative
calculatione. They do not contain derivations of a higher
order. The comparatively simple form is attained by use of
the properties of multiple integrals (Hof 09 and by using
Card 1/3 wind data. In the formula for the velocity of the change in

Method of Determining Local Changes irt Pressure With SOV/50-59-5-2/22
the Help of Wind Data
Card 2/3
the geopotential H, the calculation of wind derivations is
eliminated. The dynamical, statical and continuity equations
in hydrodynamics are used as starting equations in the
x, y, pj t coordinate aystem. From these, formula (10) is
derived for The first summand standing under the
integral consists of the product of the absolute eddy of
velocity and the radial component of wind velocity. The
second summand standini.; under the integral consists of
the product of the vertical velocity and the change of the
tangential component of the wind velocity with height.
This second summa I is the consequence of a consideration
of the terms with the vertical velocity in the starting
dynamical equations. The first summand considers the total
effect of the eddy and of the divergence factors. The amount
and sign of the contributions of the individual summands to
the change in the Seopotential R are discussed here in
detail. Formula (17) is derived from formula (10). Only its
3rd term contains derivations of 2nd order. There are no

Method of Determining Local Changes in Pressure With SOT/50-59-5-2/22
the Help cif Wind Data
wind derivations. Calculating can be carried out in
different ways. Such a method ie explained here. The daily
forecast, howeverprequires a consideration of acceleration.
It can be realized by differentiating formula (10) with
respect to time. Formula (21) is obtained ani written down
in polar coordinates representing a relatively simple
expression. It contains only the lot derivations of the
wind and of the geopotential. A calculation of the lot
derivations of the wind can be avoided by replacing the
vertical component of the eddy of velocity by &H. There
are i figure and 8 referencest 7 of which are Soviet.
Card

67173
SOT/50-60-1-6/20
AUTHORs 'retloy, I. P.
TITLEs On the Computation of Derivatives of Meteorological
i9lements
PERIODICALs 11steorologiya i gidrologiya, 1960, Hr 1, pp 29 - 33 (USSR)
ABSTRACTs In practice, the derivatives of meteorological elements
are computed as ratiosof end differences. The aim here is
-that of selecting a not large distance range. Doubts con-
,:erning the possibility of computing such derivatives,
-and especially the divergence velocity according to the
wind data, as are expressed by a number of meteorologists,
,ar* unjustified (Ref 1). One may always assume such a
:rang* in which the wind increase is larger than the change
of wind in consequence of casual fluctuations. A small
11ind increase will characterize small divergence values.
Thereforet it cannot be an obstacle in the approximate
ievaluation of divergence values. The probable error due
to disordered fluctuations of wind velocity can be con-
aiderably lowered if a larger number of wind date. is made
ties of for computing the derivatives. Formulas (2) may
be applied here. They describe the relationship between
bard 1/3 -the partial derivativeb of function f(X,Y) versus x and y,
1.)

SOV/50-60-1-6/20
On the Computation of Derivatives of Meteorological Elements
and the partial derivatives of this function versus two
othor directions a and n which are perpendicular with respect
to each othar. In those cases where the derivatives are not
computed for one point only but for several points, it is
expodient to use a quadratic network (Fig 1). It is shown
beret how the derivatives 2~f and ') f
3-x 5Y
may be computed from 8, 12, and 24 points of this quadratic
network. The formulas can also be obtained with the aid of the
method of oomputin the gradients by R. E. Soloveychik and
Mo 11[. Yudin''(Ref 31 (based on the method of least
squxtreb). The a6curacy when computing the two mentioned
der!Lvativea"from 8 points is increased as compared to the
simplified method from 4 points (the method used in practice)
by '1.6fold. In the case of a oalculation from 12 points it
is '..noreased by 2.3fold, ard from 24 points by almost 4fold.
In order to be able to utiliztt the formulas given here for
the calculation of the wind derivatives and particularly for
the calculation of the velocity divergence and the velocity
Card 2/3 curl, charts are drawn for the wind components u and v. On

67173
SOV/50-60-1-6/20
On the Computation of Derivatives of Meteorclogical Elements
the strength of the calculation made here for this purpose it
in shown that the calculation of the velocity divergence con-
sists-in determining the mean value of the radial velocity com-
ponent. The calculation of the velocity curlp on the other
hand# consists in determining the tangential wind velocity com-
ponent along a certain circle with the radius R and a central
point in the spot selected for the calculation. Ifthw-abvolute
geopotential field is used in the calculation of the velocity
curl, one obtains formula (17). The latter yields the simpli-
fied relation between the change with time of the velocity
curl and the change with time of the absolute geopotential in
the cantral point. There are 3 figures and 3 Soviet references.
Card 3/3

VNTWY I.P.
ConWing local pressure changes from wind data. Trudy ?SIP no#106:
115-119 160. (KIRA 13:12)
(Atmospheric preseare) (Winds)

VETIOV. -1.L
Evolutiou of boric formationA in the trornmj#ere. Trudy TSIP no.not
51-69 162. (Cyclones) (MM 14:6)

BIURTSLT., A. IVETWV,Jj~-
r-
.-I...Restorettion of the geopotential field according to the wind field and
-,of the wind field according to the vortex and divergence. Meteor.
i gidrol. 110.5s8-16 My 162. (MIM 15:6)
(Atmospheric pressure) (winds)

Hap of mmerical prediction of wind in the free atmoopherse
Katear.i gidrol. no.1123-11 F 162. (NEU,15112)
1. TSentralln7y institut pmgnozoy*
(winds)

BF.LOV, Pavel Nikolayevich. Ptininali uchastiye: BELLIWA, N.N.,-
-VETUIV.. I.P.; BURTSEV, A.I.; BEMIKAYA, L.L.., red.;
tekbn. red.
[Praotical methods for numerical weather forecasting]
Prakticheskie metody chislemop prognoza po od Lenin-
grad., Gidrometeoizdat, 1963. 257 p. 16:12)
Olumerical weather forecasting)

ACCESSION IM AT4017170 S/2546/63/000/126/0046/0055
AUTUOR; Burtsov, A. r.; vetiov, i. P.
TITLE: Datemination, of the paths of air particles using electronic computers
SOMICE: Moscow. Teentraltny*y institut prognaxpY. Trudy*, no. 128, 1963.
Voprosy* kratkosrochny*kh progaozov pagody* (Prob'lems of short-rsmge weather
forecasting). k6-55
TOPIC TAGS; misteorology, weather forecasting, wind, short-range forecasting,
air particle, air particle path
ABSTRACT: The synoptic method for deteemination of the paths of air particles,
used currently by the Soviet meteorological service and described in full in the
Maaval on Short-Range Weather Forecastin4, is reviewed concisely, with emphasis
on the shortcomings of the method. It involves only an approximate allowance for.
changes of the wind And geopotential fields with time, provides only a rough idea
of the actual movement of a particle and the error, significant at beat, is the
greater the loi4sr the period for vhich the particle path is determined*aad the
more rapid is the change of the wind field with time. Improvements ver* not '
feasible while manual computations were necessary; electronic computers now make
Caid 11A~

ACCESSION Na: AT4017170
lit possible to obtain a relatively precis* datorminatioxi and forecast. A com-
puter of small capacity can calculate tbe movement of a relativoly large number
,of particles for a period of several days in a few minutes. Tho formulas used
in the old method are given, with necessary modifications. A 01fral-II0 computer
was used in datermining air particle paths at the 700-mb surface; data for a 12-
hour period ot obser7ations was used, with air particle position determined in
geographic coordinates. A total of 96 particles were traced. Me data fed to
tho computer Ancluded u and v wind data at 510 points in a grid or geopotential
data at 612 pi)int's. Fig. 1 of Enclosure shows a chart of air particle paths
for a 24-hour period computed from geopotential data for three imccessive.peri-
ods of observation. Air particle paths can be predicted by thin method provided
there already is a wind or geopotential forecast. An experimental forecast is
:,described. Orig, art. has; 16 formulas, 3 figures andl table*
ASSOCIATION: Taentral'W institut projnozov (Central Institutti of Forecasts)
SM%IXTTED: 01) ENCL: 01
DATE ACQ: 24Feb64
SUB CODE: AS NO MW sovs 001 OMMI 000
6a--rd

ACCESSI04N NR: A74017171 S/2546/63/000/128/0056/0063
AUTHOR: Burtsev, A. L; Vetlov, L P.
TITLE: Computation of components of wind divergence from the geostrophic
SOURCE: Moscow.
Tsentraltny*y institut prognozov. Trudy*, no. 128, 1963. Voprosy*
kratk-oorochv*kh prognozov pogocly* (Problems of sbort~-range weather forecasting),
SG-63.
TOPIC TAGS: meteorology, geostrophLc wind, wind, atmospheric geopotential, atmospheric
pressure field, weather forecasting, short-range weather forecasting, wind diver nce
ge
ABSTRACT: Formulas have been derived for calculation of the components of wind
divergence from the geostrophic. For computations with these formulas it is necessary to
bave data on wind only for the Isobaric surface for which the computations are made. The,:
values of wind divergence from the geostrophic, computed by the method proposed in the
article, agree with theoretical estimates In order of value and with the actual diurnal wind
variabiUty. The mOLethod is simple and electronic computers of relatively sraall capacity
can be used. The following are the equations for computation of the components of wind
Card

ACCESSION NR-. AT4017171
divergence from the geostraphio. The horizontal components of the wind vector are
represented in the form,
+V
H
6H
where 1 Wy and Sx-are the horizontal components of the geostrophic wind and ul
and v' are the compments of wind divergence from the geostrophic. Thenulandvlat
each moment of time can be determined from the system of equations
+ g(H.1)
+
+
Y
(2)
7x
The first of these equations Is derived if u and v are replaced In the
expression for borl-
zontal
divergence by their values from (1). The second equation of system (2) Is the

ACCESSION NR: JLT4017171
balance equation, written in somewhat different form. If u' and v1 are represented in the
form of the sum of the potential and solenoidal components, that is, if it is assumed
all +
ay J7 (3)
V +dY
X
by solving the equations
01 LH "at 61A.
Ay= D + A at
(ay ax -TX TY)
ou)'+ 2 "u .0u] Q!'
Px),+ liy ay
it is possible to,#.%~ermine andIT6', and therefore ul'and v1 from given values of the
horizontal complonOnts of wind and geopotential. Formulas (3), (4) and (6) were used to,
compute the values, u' and v1 at the 700-mb level at 0300 hours on 1, 2, 30 4 and 5 February
.--at-285 points of.a square grid; points'were spaced 300 km apart. Computations were made
Card. 3/4

ACCESSION NR: AT4017171
on a "Ural-111 electronic computer at the Institute of Pbysics of the Atmosphere. -The com-,
Ponents u' and v1 (if wind divergence from the geostrophic computed using formulas (3) - (5)':
are smaller than the corresponding values determined by subtraction from the components
of the actual wind of the components of Its geostrophic approximation and correspond to
theoretical estimates of the order of their value and actual wind variability. Orig. art.
has: 9 formulas, I table and 3 figures.
ASSOCIATION. Ts~ntrallnyy institut prognozov (Central Institute of Forecasts)
SUBMITTED: 00 DATE ACQ: 24Feb64 ENCL: 00
SUB CODE: AS NO REF SOV: 015 GTHEIL. 001
4/4

KONDRATIM, K.Ya., doktor fiz.-mat. nauk# prof.; KROSHKIllp M.G.,
kami. fiz.-mat. nauk; MORACHEIVSKIY, V.G.t kand.
mat,, nauk; FEDOROV, Ye.K.,, akademik,, red.,,,VETLOV, J.P.,
kand. fiz.-mat. nauk, otv. red.; DOYKOVA,g.'d'.`,-'i4d.
[Ow planet from space; an album of photographs] Nasha
planeta iz kosmosa; allbom fotografii* Laningrado Gldro-
metiaoizdat, 1961,. 50 P. (141IRA 18:2)

-lilt,
Tf
/En
!v (,I
--CIO
"rudy. 165, vcqwooY
v) 29-36
i a- _S L -I
L~ T- f I
SS

L 61407.6-5
wrlu

Rv SOV 1 003
- NN 1
11, OR
R1
1
-,
,

4 b

ACC NRi AP6018679
ftk-, - - /6 11()()0100c1 IrQ201'
SOORCE GGDr. U11 50 5 oc)26
AUTHORt Vetlov 0 Po (Candidate of physloorzthematical, sciences-)-; G e 11dy , V. L
-$Y vs
- .
-
-
o-
il
did
11
C
d
t
f
k
a
e o
an
at
o
i
(Candi
f
comathematical acionces); Ter-4-12r
aryants,
6 Yo, (
P1
p
plWaicomathomatIciLl sciences), Guseva
1 - L, tl*t Dornbkovslemiya, Ta, Ps, qrxLratlyov, K, Ys
- &

(Professor)j Hordbom V. (Doot;_r__~
R
0
7 7
~ l

Sol-2,Wj4GnGGWA, -005er-VaT.
-7 Stata-Unim sAfty- adaretvonra-utalmrsitat)---World-lidtoorological----
sit jLe ~ gos
9r
Hirovoy~mteorologiaheiskly toontr)
2ITLE t -Exporierice in analyzing tho-infrared, go ofal-oud-cover-obtained-by the'-
motoorologioal vatellito Qatua_j
V
SOURCE# Moteorologiya. i gidrologiyat no* 9, ,L965, 2o.26
TOPIC TAGS: -neteorologio vatelAlto, cloud colmr , satellito data anal;rsis, sAtellite
photography, IR,photogrophy
_ABSTRArT, This irticle presents esults of a comparative Analysis of
Pe r
ord in~ry te.oroloaica data on cloud cover obtained usin,,;
~the satellitc Nimbus L 1he article in accompanied by reproductions of
two flimbus infrared cloUd Iriageg obtained tit raidnight on 2 and 6 Sep-
tember 1964 over the Soviet Union. Much of tho information is such as
containedin recent articles on the Nimbus photos published in the Ameri-'
-can presh, bUt of dourse the photographs are 6ompared with goviet meteoro"
1/2 55W2W5L#5_0_Z,_36_2.,2

44:1
L 29145-66
ACC NR. -
logical data for the photographed area.,- rt1was fotind 'that the principal,
difficulties involved in recognition of the character-of cloud cover
'from the photog;raphs is that they show only relatively large details
and the smaller details, often important in interpretation, cannot be
:seen. The following-tentative conclusions are drawn: 1. Thd infra::ed
I ormativa
Aimage obtained from a satellite gives a iwre complete and in(
,picture of cloud cover distribution thatt a synoptic map. The photographs,
even for a regIoti with a dense network of meteorological 'stations, make
it possible to refind the distribution oE-cloud cover-,over the earth's
1 -2. -- In -some C
isurfact. -'cases data.-oit-the tadiitioh balin e can b6 used to
aid interpret%too Of_ satellite OrIgd ---- h4av- I'Aguies GM
r;
I tablos, LJPR�/
SUB CODFt 04o 221 14' SUM DAM 23Apr65
-2/9
T--,

28�38-66 (1 )/FC~#SS-2 17/9V
Acc tmt Ar661800- SOLMU, CODPA UR 00
50
A11TIK)Rs Votlov, Is P, (Cwvdidate of physical aM mathamtical ociences)
OpleAT so (Gidromotoorclogichaskly
ORG I lit romote IXA ion'-iric Research
L U
n;F
,7
nralcimo- as V r
gIg S~
TITU-',t Interpretation and wtoorological use of satellite information
SOURCS I tleteoralogiya i gidrologlyat no. 4, 1-966, 41-44
TOrTC TAGSt satellite data analysis, mteorologic satellite, cyclone, symptia
mtnoro.l.o17, atmospheric geopotentle-1, atmo3piwric vim
'Tt Th
-ABSTRAC is Is a reviiw of the current status or progress on the inter-
pretation and, meteorological use of satellito data ~O Soviet papers
are cited. 1he paper is a bAef summary of a repoi-V-`presented at the
Seventeenth Eession of the 161-10 Executive Committee. Rnphasis is on work
at, the World Meteorological Center at Hoscow, .here a special section has
been establiobed for carrying out such otudies, The day-to-day use of ~
satellite data on cloud cover is done at, the World Meteorological Center.'
in coUaborn, tion with the Central --T-nstjtmtq- oi 7 ~~ Qtqd It was begun
ime(Liately after initiation of the transmission or eatellite data rrom
Ahe United Staten, 7he contents of each of the cited papers are givens
For examplo,, in one or the cited papers. it is ahown that oatellito data
on cloud covor can be used in reconstructing the eynoptic situation*
1/2 UDCt
__�Xk~35L __7 362.2
_5A

L 26638-66
ACC NRt AP601 IWO
4ho pooition of cyclones c(m be determined# the fields of vertical move-,
mentso geopotenUal of Isobaric aurfaces ard wind can be reconstructed,
and the character of the temperature stratification of the atmosphere
can be dotenained., Other papors are cited Which doscribe3 the methodei
which can be used; for Increasing the accuracy of interpretation# etek
.,Thus,, each of tho papers cited wA siumri-,,,ed in this review,, in the
authorto opinionj represento a major contribution to progress In the
field of oatellite meteorology,* TM37
SUB CODSt 041 22 SUFm I)ATE Ihons ORIG Un 030--
C
otd

ACC NRt
AP7002137 SOURCE CODEt UR/0050/66/000/012/0003/0009
1, (Candidate of physico-mthezatical sciences); jf&t
AUTHORS: Burtsev, A. _Xpyg 1. P.I
-sico-mathematical sciences); Dudn-tkovp V. N.j oft~% i
(Candidate of phy
ORG: Hydrometeorological Scientific Research Center of the SSSR
(GidromotoorologJ.choskiy nauclino-issledovatellakiy toontr SSSR)
TME: 1%1niya-Ill transmits images of the earth from outer apace
SOURM Meteorologiya I gi4rologiya, no, 32# 1966p 3-9
TOPIC TAGS: meteorologic satellite, tv canera, cloud formation, earth planot,
wca-thor r-ap / Mlolniya-I meteorologic satellite
ABSTRACT: The authors discuss the television images of the earth, transmittod from
the llolniya-I satellite. The cameras were mounted on the outside of the housing of
the satellite and had interchangeable objectives. Those tolovision cameras permitted,
photographing in the yoUow-red region of -the spectrum, which increased the quality
of the images of clouds and the earth's surface. Photographs taken at 1500 hra
Moscow time on 30 May 1966 at an altitude of 30 000-40 000 km are shown. Anal7ols
of the television photographs shows a number of structural poculiarition of largo
cloud formations that determine the weather over a large territory, Orig, art, has:
2 photographs and 1 map.
SUB CODE: 0. 0 / SUBM DATE: 19Aug66

USSR/G~nera% Problems of Pathology - Comparative Oncology. U-3
Tumors of Man.
Abs Jour Ref Zhur - Biol., No 16, 1958, 75516
Author Vatlov, P.I.
Inst
Title Myxoma of the Heart as a Cause of Blood Circulation Insuf-
ficiency.
Orig Pub Vrachabn. delo, 1957, No 1, 85-86
Abstract A patient was adrdtted to the clinic with a diagnosis of
rheumation, stenosis of left oatiun venosumo carainc fi-
brillation, focal nophritie, cardiac cirrhosis of the li-
ver, thrombophlebitio of lover extremities. On the 88th
day after admission to the clinic, the patient diedo
Autopsy disclosed that the clinical picture of a left a-
tric-ventricular ostium vos conditioned by the presence
of a tumor 4 x 5 x 8 one in size, vhich grew from the loft
atrim through the atric-ventricular ostium into the loft
Card 1/1 ventricle and blocked this ostium. Ye*A* Skvirskaya.
3.7

nc,.
0 P I C'-r, S ba- a ke
~XWRLACT This Author CertLficnto pro2entn a dial: brakG for wheeled ruichines
en-
to the jl-ivo (s-,)e F.t,,-. I cn
-thf-1-

j-
RE-
jP
Card 2/31

-0-
Fig.
central solaT' gea--;

VXTLUGIN,-A,A. .
Ostoosynthesis of some diaphyseal fractures. Ortop.travm. i protez.
18 no.4:52-53 -Tl-Ag '57. (MIRA lltl) *
1. It kafedr7 goopitallnoy khirurgii (zavo - profe V.M.Ball)
Astrakhariskogo meditsinskogo instituta i khirurgicheskogo otdele-
niya gorodskoy klinicheskoy bollnitay (glavnyy vrach - V.K.Rodionov)
(FRACTURES, surg.
osteosyntheois of diaphyseal fract.)

_M=L, =A -AhWANkV^
U
0Gt6OG3'nth60I9 Of 8 closed fracture of the femur complicated by local
fibrousi dysplasia. Ortop., travm. i protez. 18 no.2154-55 Xr-Ap 157.
(MIRA 10:8)
le Is'kafedry goopitalluoy khirurgil (save - prof. V.K.Ball) Astra-
khanakogo maditainakogo instituts i Gorodekoy klinicheakoy bolluitey
g. Astrakhani (glaynyy vrach - V.X.Rodionov)
(mim-nACTURN)

BURAVKOV, Boris Fedoravich; VETLUGO, Aleksay Favlovich; TSVETKOV,B.,
red.
(Scouts of the plant; from the work practice of party and state
control groups and posts in the Sebryakovo Cement Plant] Dozor-
nye zavoda; iz opyta raboty grupp i postov sodeistviia partiino-
gosudarstvennomu kontroliuna Sebriakovskom tsementnom zavode.
Volgogradp Nizbuo-Volzhokoe knizhnoe izd-vop 1964. 34 p.
(MIRA 18:3)

VMMGIV, _ B. V. G.A. SAVENM
IPacks for Transportation of Wounded .-
VoyMO-MWITSINSM ZHURNAL (MIlita" Medical Journal), no. 2, February 1955,p. 74

15-57-2-1224
Translation from: Referativnyy zhurnal, IGeologiya, 1957, Nr 2,
p 5 (USSR)
AUTHORS: Ifudin, I. A., Vetluginj L. Go
TITLE: Additions to the Exhibits of theUral Geological Museum
(Novyye popolneniya eksponatov Urallskogo geologi-
cheskogo muzeya)
PERIODICAL: Irr. Sverdl. gorn. in-ta, 1956, Nr 26, pp 146-153
ABSTRACT: The summer of 1955 represents the 18th year of existance
of the Ural Geological Museum, which is one of the
largest in out country. It contains about 25 000
specimens representing minerals, ores, rocks and fossils
of the Ural district. In recent years the museum
obtained over 1 500 new specimens, many of which are
rare and extremely interesting. The article contains
a tabular list of new mineral specimens.
Card 1/1 G. I.. D.

.Y]~TLVGIII, F.G.: inzIl.; BURINIASHFV, F.G., red.; 3YTVYUK, G.I.,
red.
(Reconditioning dEmxAged motor-vehiclo fromos by oloctric
welding] Vosstanovlenie povrt3zhdrjnnykh avtomobillnykh ram
elektrod-agovoi. svarkoi. Alma-Ata) Kazakhskii nauchno-
losl. i proektMI in-t avtumobIlInogo truaisp., 1961s 33 P.
(MLLA 18s5)

VETLUGIN, V.
Unravelled tangle. lUn.nat. no.5;24-26 161. (MIRA 14:4)
(Ioosyatino, -Sugar beets)

vvrmu, V.
Triumpb of Academician Luklianenko. IUn. nat. no.12:11 D 161.
(MIRA 15:11
(Wheat breeding)

YL, TLUGLIM. V.
Crop on untilled land* lUn.nat. no.2:21-24 7 159.
(nU 12: 1)
(Transcaucasia--Wheat)

VETLUGIN, V.
"Bird conversations" by Pavel Barto. Reviewed by V. Vetluf,in. On.
nat. no-1:34 Ja '62. (MIRA 15:1)
(Bird song) (Barto, Pavel)

VBTLUG111, Vladimir.
1--mm"Ns"
Corr, marchos north. Wn.nat. no.7:13-15 JI
(Corn Walze)-Yarietles)
I
'5?. k ~ vu 10- 8)

kand. tekhn. nauk, dotsent
VETLUGIN, Te.M., inzh.; URMANOV,, R.N..,
SmA)oth voltage regulation of power transformters Under load
conditions by means of saturation choke coils. Trudy Ural.
eloktromekh. inst. inzh. zhel. dor. transp. no-5:44-55 162.
(MIRA 17:8)

VETLUGINA, K.F.
Diagnosis of present-day typbold fever. Zhur, mikrobiol. opid. i
in=.. 32 no.601-54 Je 161. (MIRA .1515)
1. 12, Astrakhanskogo moditsinskogo institute.
.(TYPHOID FEVFR)

VETLUGINA, K. F.9 CAND MED SC19 "EARLY DIAGNOSIS OF
TYPHO-PAAATYPHOID DISEASES UNDER POLYCLINIC C-ONDITIONS,"
IVANOVOI, 1960. (IVANOVO STATE MED INST), (KL,, 3-6it230).
398

VETLUGUIA, K.F.; USIMIOVA, A.V.; KOLIYAKOVA, T.A.
Liver abscesses of amebic etioldgy. Kaz.med. zhur. no-5:68-70
S-0163 (MMA 16:12)
1. Kafedra infektsionnykh bolezney (zav. - dotsent A.P.
Vozzybayeva) Astrakhanskogo meditsinskogo instituta i Infek-
tsionne.ya bollnitsa, imeni prof. Bekhtereva (glavnyy vrach
V.I.Gentbitskiy) Astrakhanl.

MLUGINA~ K.F.
Diagnoois of present-day mild forms of typhoid fever. Kas.mad.
zinw. no.lt60-62 Ta-F'61 (MIRA 16-11)
1. Kafedra infektsionnykh bolezney (aav.-dota. A.P.Vonhrjeva)
Astrakhanskogo meditsinskogo instituta.

- VATEUGIVA
phoumothyphus as a masked form of typhoid fever..Vrach,604 80,7:
695-697 JI 159. (MIRA 12:12)
1. Wedra. infektaionnykh boleznev (xav, - dotsent A.P. Toxxbayeva)
AstraCkhaustogo meditsinskogo instituta.
(TYPHOID 73v ) (PM;UMNIA)

AP6031636- -_ ~~ - _I ~ -_ -- -- -- -- - -UR/0297/66/6!f/6-0-9fd-846-/-0-64-j--7
---SOURCE -COD
AUTHOR: Ferdinand, Ya.. M.; Redechkina, Z. P.; Vozzhayeva, A. P.; Vetlugina, K. F.;
Vevyur, N. A.; ZhigUl'13kay~, 1. F. Borodzdenko, T. F.
.1
ORG: Rostov-na Donu Scientific Research Institute of Epidemiology, Microbiology,
and Hygiene (Rostovskiy--na-Donu nauchno-insledovatel'skiy institut epidemi.ologii,
microbiologii i gigiyeny); Department of Infectious Diseases, Astrakhan Medical
Institute (kafedra infektsionnykh bolezney Astrakhanskogo meditsinskogo instituta);'
Department of Infectious Diseases, Saratov Medical Institute (kafedra infektsionnykh
bolezney Saratovskogo neditsinskogo instituta); Hospital No. 10, Volgograd (bol'nitsa
No. 10)
TITLE: Antibiotic therapy and chronic typhoid fever carriers
SOURCE: Antibiotiki, v. 11, no. 9, 1966, 840-843
TOPIC TAGS: typhoid fever, typhoid carrier, antibiotic 4&mewpy, infective diseas
ABSTACT: Antibiotic- treatment does not eliminate all typhoid carriers#
but the treatment is justified since the highest percent of
carriers wai found among untreated patients. Administration
of antibiotics until the third week of convalescence sharply
reduces the number of carriers. (WA-50; CBE No* 12]
SUB CODE: 06/ SUBM DArE., 05Nov65/ ORIG REF: 008/ OTH REF: 001/
Card. 1/1 UDC: 616.927-085.779.931-07:616-008.97 (Bac. typhi)