SCIENTIFIC ABSTRACT SOLOVYEV, V.A. - SOLOVYEV, V.A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001652320009-3
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 25, 2000
• Sequence Number: 9
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

4. Irrigation
7. Experience with sprJng flood irrigation of meadows and aruble lands beyond the
Volga. Gidr. i rel. 5 no.2, 1953
9. Monthly List of Russian Accessions, Library of Congress, June 1953. Unclassified.

1. 3OLCV I YEV 0 V. A.
2. USSR (600)
4* Irrigation - Caspian Depression
7. Irrigation cycle for natural madows in local storage basins of the
Caspian Depression, Gidr. 1. mel., 5. no. 3. 1953,
9. Monthl List of Russian Accessions, Library of Congress, April - 1953, Uncl.

PXTROV, Yevgenir GrigorlyeTich; aQjQ*AUVV,4.&.jjCH9RNYKH. A.A.; ORLOVA.
V.P., redaktor; GURIVICH, M.M., tekhnicheskiy redaktor.
LSnov water irrigation and the accumulation of zoistureJ Liummos
oroshenie i vlagonakoplanis, Moskva, Goe.izd-vo selikhos.lit-r.V,
1956. 165 p. (irrigation) (MMA losO

50101PYEV, V.A.., _,kand. sel't~oPiozyay5tvennykh nauk
Increased production by urinf, irrippation in tl)e trans-Volga ref-ion.
Zemledelle 23 no.11:1(--19 N' ' 61 - (KIRA 34-11)
(Volga Valley--Irrigation farming)

SrT,OV,YEV 11ari. na)lk (Saratf),/)
p P. . . A
Irrigate,J Ian-Is am ar- irucrtant nource fcr increasing, meat prr,div!tion
In the Volga rmg1on. (Adr. i mel. 14 n,~~;7:62-63 J1 162.(MIRA 1712)

ACC NR' AM018526 SOURCE CODE: UR/O1f3l/66/OOV/0.)6/1683/*
AMOR: Lyubov, B. Ya.; Solcrytyeyj V. A.
ORG: Central Scientific-Research institute of Ferrous Metallurgy im. 1. P. BardIng
Moscow TTsenGillnyy nauchno-issiedovatel'okly Institut oernoy met allurgii)
TITLE: Kinetics of disintegration of dislocation cracks on the polygonal walls of
edge dislocations 6
SOLJRCE: Mika tverdogo tela, yo 8. not 6, 1966p 3683-1689
TOPIC TAGS: crystal dislocation phenomenonp crystal defect, crack propagation, meta-
stable state, surface property, relaxation process, brittlenessy hardening
ABSTRACT; The authors analyze the decay of metastable dislocation cracks on poly-
gonal walls of edge dislocations, the decay being the result of diffusion orver the
surface of the crack. It Is pointed out In the Introduction that formation of dis-
locations along one side of a crack is energetically favored and that the diffusion
on the surface of the crack is the mor6 l1kely mechanism of disappearance of disloca'-
tion cracks at low temperatures. The time evolution of the diffusion of the atoms
over the surface of the crack from the base of the crackp which is under compressionp
into the mouth of the crack, which is under tension, is described and the dislocation
distribution produced during such an evolution is calculated. The decrease in volum
accumpanying the crack disintegration Is also calculated an well an the relaxation
times characterizing the process. It Is concluded that dislocation cracks should

SOWV 'TV, V. A.
Method of determination of the resistance of Mycobacterium tubercu-
losis to antibiotics. Probl. tubork., Kookv& no. 3:31-33 NW-Jww
1952. (CLHL 22:4)
1. Of the bacteriological Laboratory (Scleatific Supavisor - Prof#
P. N. Kashkin). Lezdagrad Institute for Surgical ftberculoste (Direc-
tor -- Prof. P. G. Kornev, Active Meniber AN U831). 1

y
SOW',"wV, V.A., Ved ZS4i -- (diss) ninturcostal
:Mbple-iral ~-!vastr.esi--, in lung, operations." 1/.,n, I,)
iA-
It) pp ("First Lon ','td Im-A.- im Acad f, i~-.iar I.F. ?nvlov) 2(Y,)
cro (?I, I..j>)
- 12,11 -

SOL'UVIYEV. V.A.
Uperimental data on the use of Intercostal anesthesia in
surgery of organs of the thoracic cavity* Vest,khiro 82
no.4:85-90 Ap 159. (MIRA 12:6)
1. Is gospitallnoy khirurgicheskoy kliniki (say. - prof.F.G.
Up,lov) I kafedry operativnoy khtrurgit I topograficheskoy
anatomit (say. - prof.M.A.Srosell) 1-go Leningradskogo medit-
sinskogo Inst. im.I.F.ftylova (Leningrad, ul,L*Tolutogot 6/8)o
(LOCAL ANEbTHNSIA) (CWT-SURGERT)

SOLOVITXV, V.A.
Operation on the lungs vith the application of intercostal subpleural
anesthesia. Vest.khir. 83 no.8tll5-121 Ag '59. (mm Ila)
1. Is gospital'noy khtrurgichookoy kliniki (sav. - prof. F.O. uglor)
I-go Leningradskogo maditainskogo instituta Im. almd. I.P. Favlova).
Adres avtorat LenInKrad, ul. L. Tolstogo, d.6/8, goopitaltnayn khirur-
gicbeekaya klinika 1-go Leningradskogo weditainakogo Institute. it.
1.P. Favlova.
(LUNGS surg.)
(ANESTHISIA, LOCAL)

SOLOVIYEV, V. A.
Drug resistance of mycobacteria tuberculosis !n osteoarticular
tuberculosis. Probl. tub. no.2:91-93 W. (MM 15:2)
1. ZZ Loningradekogo nauchno-isoledovatel Iskago instituta khirur-
gicheskogo tuberkuleza (dir. - deyetvitelln7y chlen AKU SLSR
prof. P. G. Kornev)
(DRUGS-PHYSIOLOGICAL EFFECT)
(MYCOBACTERIUM TUBERCULOS15)

SOLOVIrEv, V. A., k&nd. biologicheakikh nauk
SIgnificance of specific allergy in the pathogoneele of tubercu-
lools. Probl. tub. 40 no.4:65-71 162. (MM 15:6)
1. Is Laningradekogo nauchno-issledovatellakogo inatituta khirur-
gichaskogo tubarkulaza Wir. - prof. D. K. Khokhlov, nauch"y
rukovoditell - deystritelOW chlen AM SSSR prof. P. G. Korney)
(TUBERCULORIS) (ALLERGY)

U)V, -?-TY T%
SO v IrAl v n.
um/metemologicea iResearch Jkr 191q,
*Contencrary Viewpoints m the Formation of Rain,,
V. A. S*lovlyev, 5 pp
*Prirode No 2
Discusses the formation of.preolp Itat1ca an a result
of the formatice of Ice putioles In clouds and sup-
plants Xens~ls theory that raln Is caused primrily
ty means of water-bearIng clouds. Soloylyev discusses
both Findelasnstheory of the formtIm of rain out
at Cumilo-ninbus and Beriherms theory of the forms-
Man of rain " a result of clouds generated at the
d1vislan ot two air masees.
3VI&

Sam-fiv, 'I. A .
Meteorology - Biography
Nikolay Nikolayevich Kalitino Met. i gidrolt No. 3. 1949.
MDnthl List of RussilmWeegsionap Library of Congress,, November 1952, UNMASSIFIED.

SOWVtTL'V, V,A,
MMWMUMIAF~ -I
A.I.Voeikoy and current problems of climatology; material$ of the
meeting of the scientific council of the gain Geophysical Observa-
tory devoted to the memory of A.I.Voolkov. Izv.A?I SSSR Seregeofize
no.6:739-743 Je 156. WRA 9:9)
(Toeikov, Aleksandr Ivanovich, 1842-1016)

36-58-5/12
ALY00R., Soloylyev, V. A.
TITLE: A Method for Measuring the Sizes and Charges of Fog Droplets
(0b odnom metode imereniy zaryadov I ramnerov kapell tumanov)
PERIODICAL~ Trud Glavnoy geofiziebeekoy observatorii, 1956, nr 58,
a
pp 31-41 (USSZ
ABSTRACT: The author describes a device, essentially an ultramicroscope,
developed by a group of Soviet scientists for measuring the sizes and
charges of fog droplets. The instrument operates on the principle that
a freely falling charged fog droplet moves along a zigzag-shaped path
within an electrical field, constant in size but varying In direction,
The vertical and horizontal components of the speed of the moving
droplet may be determined by the length, amplitude, and period of the
zigzag, and its radius and charge, respectively, by the magnitudes of
the vertical and horizontal components of Its rate of speed. The
instrument de3cribed is a model perfected by the author and his asso-
ciates In 19514, and to based on an instrument built in the workshops of
the Main Geophysical Observatory in 1948. Its design was developed
Card 112

NINANDROY, V.Ta., kand.fizo-mtonauk, red*; SHISHKIII, U.S., doktor fis.-Mat.
nauk, red.; SHMIN, K.S., doktor fiz.-mat,nauk, red.; SOUNITRY,
V.A. kand,fite-matenauk, red.; PISARNYSXhTA, V.I., red.;
1=73YOHIK, A.A., takhn.red.
(Investigations of clouds, precipitation, and thudnerstorm
nloctricity] Inoledovanie oblakov, osadkov t grozovogo elektri-
chestva; sbornik dokladov Y Mezhvedometvennot konferentsit po
voprosam iseledovaniia oblakov, osadkov i grozovogo elektrichostvae
leningrad, Gidrometeor, izd-vo, 1957* 214 Ps (MIRA 11:6)
1. Ruasia (1923- U.S.S.R.) Glaynoye upravlaniye Cidro-
mateorologicbeekoy eluzhby.
(Clouds) (Atmogpherie electricity)
(Precipitatiou (Meteorology))

GANDIN, L.S.; DUBOV, A.S.; 50 'YxV- T, .
In the Toelkov Main Geophysical Observatory. Meteor. I g1drol.
no.8:70-72 Ag 157. (Meteorology) (KLRA 100)

SOLOVIUV, V.A., kitadidat fi-siko-mtemAtichookikh nouk.
What Is *loctroolinate? Ppirods 46 no.6:73-76 Jo 157. (RUA ln:7)
1. GlAwneya goofixichoskmyA obserratorlyA im. A.1. Voyoftows.Loal.-od
(.1.6.iosphorle eloctricity) (Air, lonlood)

VIKHOTY.B. L.G.; 501DVtv.ZV, V.A.
I
Role of electric charge In the coagulation of fog Aroplets. Trudy
GN no.73:116-122 158. MU 11:9)
(Atmospheric slactricitr) (Yog)

XMH(YrXIM, I.G., S-OLOVITXV, T-A,
XlectrIcal characteristics of th4 atmooptaro during fo so Trudy
Goo no.97:63-86 160. (NLRA 13Z
(Atmospheric electricity) (Yoe)

s/196/62/000/022/005/007
E194/EI55
AUTklullb: Makhotkin, L.G., and bolovlyev, V.A.
TITLEi ChArACtpristics oV the atmosphere during
Fog
FERIODICALs 1(e1*#-rntivnyy zhurnal, ElektratekhnikA i energetika,
iio.22, 1902, 29, abstract 22 E 199. (In collection:
'11.4sled. oblakov, osadkov i grozovogo elektrichestvall
(linvestigations of cloudst-precipitation and
ntmospheric electricity'), Moscow, AN SSSR, 1961,
,219-Z24).
TEXT: In fog, when the electrical properties of the
atmosphere are significantly Jifferent from normal# the potential
gradient Ls greater, the air conductivity in much reduced and the
concentration ot light ions is lower. Until rocently, few detailed
results of observations made during fog have been available.
The --ilgnii',icance of' theoretical calculations made in the
Labo.,storiya nerozoley (Aerosol Laboratory) of the riziko-
khimicheskiy iiistitut imeni Karpova (Physicochemical. Institute
iment Knrl)uv) twenty years ago was recently evaluated and the
Card 1/2

Electrical characteri-stics ot the ... S/190/b2/000/022/005/007
E 194./E 135
conclusions previotisly obtained were repeated lit a number of works.
The impo*rtniice ot the formulae is not tkint they replace measurements
by calculations, I)ut that they serve to check the correctness and
completeness o! (Iv.,4crJption u1 inicro-processes in fog, and
establish general aisemmukenta and relationghipb between the various
characteristics. The meteorological characteri.-otic of" visibility
rang,e may be associated with the atmospheric electrical character-
istic of' light ion concentration. Experimental data concerning
the chargeti on fitie drt~.pb of' tog are in good agreement with
experimental resiilta ineastired in cloudn on the mountain Elbruss by
a completely dit"rerent method. 9 references.
TAbstractor's note;
Complete translation.
Card 2/2

ACCESSION NR: AT4030534
AUTHOR: Solovyov, V. A.
5/0000/63/000/000/0115/0122
TITLE: On the possibility and perspective of providing storm activity Information
to operational service for aviation
SOURCE: Nauchnayo konferentelya po aviatoionnoy matearologil. Moscow 1960.
Naterialy*. Moscow, Gidrometeoizdat, 1963, 115-122
TOPIC TAGS; storm center, lightning, cathode direction finder, air temperature,
meteorological observatory, upper atmosphere, cloud
AIMMACT: 71tis paper Is one of 13 previously unpublished reports of the 40 papers
given at the Nauchnaya konferentsiya po voprosam aviatsionnoy meteorologii (scien-
tific conference on problems of aviation meteorology) that was held In June and July
of 1960 in Moscow at the Glavnoye upravleniye gidrometeorologicheskoy sluzhby* SSSR.
'nie author stated that danger to aircraft from storm activity still exists. A graph
was presented showing the number of aircraft destroyed by lightning. Of those
catastrophes, more than half occurred at altitudes of 3-4 km with air temperatures
of about 00. Maps were presented showing storm center locations at particular times,
in Europe, the Middle East, and the Far Seat. Stom activity data from various
Cardl/2

SOIXIYEV, V.A.
*The significance of atmospheric electricity wasurement.0
Report submitted to the Third Intl. Confe on Atmos heric and Space
Electricity,, Montreauxt Switserland ;Z 1963

SKLY AAOV, V.M., otv. red.; GhIBANOV, h.N., red.; EURCIATSEV, A.M.,
red.; POGOSYAN, Kh.P., red.; PROTOPOFOV, V.S., red.; HUHN,
G.V., red.; SOKOLOV, A.A., red.; SOLOVIME V.A., red.;
USNUOV, I.F., red.; ZhDAII'OVA, L. red.; RUMOVA, G.Ya.,
red.; CHEFELKINA, L.A., red.; KOLESOVA, Z.H., takhn.red.
[Man and the elements; hydrometeorologic desk cnlendar for
1964] Chelovek i otikhIla; nastol'rWi gidroineteorologicheakii
kalandnrl 1961,. Leningrad, Gidroreteorologichookoe Izd-vo,
1903. 154 1). (MIHA 17t2)

AP5025706 SOURCE COLES UR/0286/65/000/018/0057/0057
AUTHORSs Konovalov,, Yo. A.; PlosbehansgZ* L, M,j Solcylyev, V, As
W
ORGs none
TITUS A device for checking radiation motors, Class 22t No, 17,4729
SOURCES Byulletent isobroteniy i tovarrykh smkovs no. Is# 1965# 57
TOPIC TAWS radiation monitor,, radiometryj, radiowtorp filter, mercury
ABSTRACTS This 1uthor Certificate presents a device for checking radiationboterso
It contains a radiation source, a shielded housing vith a collimated channel, an
attenuating filter mochani me for moving and fixing the position of the source, and
an effective area (see Fig. 1). To siWlify the design, increase the measurement
range,, and reduce the checking timej a liquid metal (osg,o Rg) is used as the
attenuating filter. The radiation source in placed directly inside the filter and
can be moved,
Cord 1/12 M 621,03945

Fit, 1, 1 - Radiation source;
2 - shielded houmiftl
3 - l1quid-ontal. attonmting
filterl J# - mechamisa for wring
source; 5 - mocham"a for fixing
source; 6 - effective arsa;
7 - sensing 92amA of radiation
meters
Orig. art, hass 1 figure,
SUB COMs IS/ SUBM DAM Mipr64

1, lzu-(X-00 . r'WT t 11 / lr,t;u UW
NR, AT5028-6-65 SOURCE COM UVi6-A_/6_576bo/oiq/C_1 _I/Ifi 9 5
AMORt $olov'Yev# V, As
ORGt Far Vastern Soiantific w_ch_Aydrmdeoro1ojri6i1
(DallnevostochMy nauohno-iseledovatellskiy gidrometeorologlobookiy institut)
TITLEs Thund2retors a2tky-ity in the Par Fast
%M%0
SOURCEs Vladivostok. Dallnevostochnyy naucbno-tooledovatellskiy gidroustooralogicho-
skiy inatitut. Trudyp no. 19, 1965. Toprosy acrologii I sinoptichookoy notoorologii
(Problems in aerology and synoptic neteorology)p 191-195
TOPIC TAM diurnal variationg -thunderstorme storm# climatology, atmospheric
disturbance# marine meteorology
ABSTRACTs Thunderstorm activity was characterized on the basis of direction finding
observations, The study covered the period 1961-1962 for the area 30--55 N, li5-150
El and was an extension of similar studios conducted in European Russia. The thunder-
storm activity was studied for its annual and daily variations. Over land there wart
no thunderstorms from December through Februaz7q and 84% of the storm occurred from
June through September. At seag atom occurred each month@ with the maximum of a Ion
axtrane variation in the fs,11-winter. A maximam daily &otivity was observed over the
land In the evening. The observition region was divided lato four seations for etud$-
in# the duration of the storm period and the number of dare with thumderstormse une
CAWd

NRI AT5M8665
area# entirely over landq showed a typical continental pattern and gave good agrooment
between the direction-finding oboar, time and weather station roportse 14m arms had
a mixed land-sea surface pattern and showed an intermediate thunderstorm pattern*
Here correlation between the two "a of data was poor due to the limited weather
reporting system. The fourth artat entirely over waterp showed a typical marine
thunderstorm pattern and sooomnted for half of the stom-Uvedift oesters, of the,
entire region. This moth" in equally valid over land md sea. Ortgo arte hase I
fi6we and 4 tables.
ago OOIAI 04/ SM DAM noms/ CRIG Wo 002

Eli', T
ACC NR, AP60IB660 SOURCE COIZe UR/0D0/65/CV0/O3D/0O32;66j
AUTTIORt Solovo (Candidate of physicomathematical sciences)
ORGs Main Geophysical Observatory(alavnaya geoflzichaskaya obsopyatorJLya)
TITIZt Diurnal and annual variation of thunderstorm activi in the ljorth 03,antic
and the seas.of Western Europa and the Far East
=RCES Motcarologiyaj gidr*logIM nos 30# 2965,# 32-34
TOPIC TAGSt d:btrnal variationp storm
AD the basis of an analysi 19 of __ data from the network of stations
.15'rlela(t"Britain and the Soviet Union for direction-finding of atmos-
.pherics, for the years 1961-1963 this article gives the distribution
(diurnal and annual) of thunderstorms for the region from 350 to 700 11
and from 301 W to 300 E, the Norwegian Sea. North Sea, Baltic Sea and
-Mediterranean Sea and the North Atlantic, and 250 to 600 N from 1201
to 1530 E, the Sea of Okliptak, Sea of Japan, Yellow Sea and East China
Sea and part of the Pacific Ocean. For the different seas of western
,Europe there is a different annual variation of thunderstorm activity.'
Tor example, for the Norwegian Sea and the Northeastern Atlantic the
maximum thunderstorm activity occurs In the cold half of the year, In
the Norwegian Sea area 85% of all thunderstorms occur from October
through March, and In the Northeastern Atlantic -- 70%. The mean an-
r.,A' 1/2 UDOt 55le5h,21

ACC NR, WwWo
egian Sea is 7 per 100,000 km2'
nual number of thunderstorms for the Norw
whereas for the some area of the Northeastern Atlantic there are 100,
over the North Sea -- 170, and over the Mediterranean -- 600. In the
4editerranean area the distribution of thunderstorms is almost uniform
throughout the year. Over the Sea of Okhotsk, on the other hand, thun-
derstorm activity is confined to the warm months of the year; thunder-
storm activity is 25 leas frequent than over the North Sea, which can
be attributed to the presence of the cold Kurile Current. Although that
Sea of Japan in at the same latitude as the Mediterranean its thunder-
storm activity Is different: the distribution Is not uniform and thun-
derstorms occur almost four times less frequently. In the Pacific area
.the activity resembles that of the Atlantic, probably due to accumula-
tion of hent by Lhe world ocean and the same mechanism of its distribu-,
tion during the year at!the same latitudes. Similar comparisons are
made for the diurnal distribution. For those seas where the surround-A
ing land exerts a great-influence there to a diurnal variation of thun-
derstorms. Seas that adjoin the ocean feel no such Influence. Or1g, ajrto
hafis 4 tables*- rJPRS7
SUB 0=& 04 8UBHtl1kT31 02Feb65 OriM MW 1 002 OM MWI 004
2/2

SOLOVIYEV, V.I.
Flastle InterseLion ot vananclop witb #dge dimlocatleas In
the onntinuil theor
VY r. Fli. met, i motalloved. 20 n0-0634-
636 0 165, ( ma RA 3. 8 g *" j )
1, Ingtitut wtalloyedarilp t fifiki. motallov i 'M;"ntrall-
ny-y inortitut c1mmay mat-aDvriv!
imeni %Peilirdin%.

7. 1%.
solol:,ly-y '! A. "on tf--,~ r-o"nier of the causns of castration of rares (sic)", TruJly
Zhitomirsk. s. -kh. in-tq , Vol. 111, 1949, p. 91-06.
1
SN IT-4630, V lppt. 51t (1ptorir Inurnal Inykh Rnt-y, N'O. 23, 1949).
a

CAT

jOUR. I RZhPlol, No. 3. 1959~ ao.12061

T I T ~.Ill nc,., r,i, j;r,.,)t,Jn llw-,n the
liter.-anp of -,.'arly I*rt~urity In ~igsa
0 R I G PU J. ltli-ut:hn. 11-r. lr,-t, lr)57,, 1-2

"T; -,11,'T -vt on 3 f~rnla,
ct* t-, I-rj-~I
loc-,il browl_~ rl

F' of nvotein,,

cnn ,,I tut,,, --j ()o porpent, wria juicy feedis 'I?- por-
the rvion's nutritive. valua; 'rhn plg-

the _(I rx-tu-) vmvp~- corro s pondl. nj~ly
2n U -

7 3 76 of' tin'
20 arid ).6 it
,-,rour-, 39., 784, 311 bald 6.;~. At tho nZe of ono
m`

SOLOVIYKV, V. A. ~~ Doe Agr Sci -- (dies) "Biology of the early maturing
methods
of hogs and of modifying it." Moo, 1959* 33 pp (Min of Agr RSFSR.
Mos Vat Aced), 160 copies (KL, 46-59, 138)
YS
-46-

. :. ~ I I . I . I .~!* ~ 'I I . I - - I - I
. , ; 1: i " . . I I -. .
I I I I ~ I , . I - i - i , ,~ i; : , ~- 1, ~~ 1. 1,
, Z, : - .1 1 ~ 11 i 'A', ~ : , I
: I I
a" -, ",-, -, -v )

Vlktol. Aleki-yeov i ch
"The Bioloey or the F.-irly 1-flatu ration or Pirs and Methods of
Alterin.- It";
dissort4ktion for the degree of Doctor of Agricultural Sciences
(aw&rdsd b7 the TimirYasev ASAWItural AcadaVj, 1962)
(IwO9tlYa Tiftdr~"MkOY $01OAWdwlM$tvftvW Akadedip MO"Owjv No. 2p
1963p pp 232-236,

L 24486-65 E~IT(-l)/EWG('f)/FEC(t)/EEC(b)-2/FCC
ACCESSION NR: AT5002954
Pe-5 RB/aW/WS
S/2531/64/000/163/O(Y76/0086
4
AUMOR: Soloy'vey. V.A.
TITLE: Thunderstorm a6tivity over the European part of the SSSR
SOURCE: Leningrad. Glavnayj -gbofizicheakaya observatoriya. Trudy, no. 163, 1964.
Voprosy klimatografil (ProbleTs In -climatography), 76-86
TOPIC TAGS: thunderstorm, climatography, lightning, atmospheric turbulence,
meteoroloxical radar
ABSTRACT: For the purposeof obtaining data on thunderstorms- in areas without
meteorological stations a network of stations has been established for the radio direction
finding pf atmospherics\ ociated with thunderstorm activity. This network covers
virtuall the entire area of the Soviet Union and certain parts of foreign couzitries adjacent
to the SR. Such observations have been made since 1957. This work has yielded a
o
mass fdata on thunderstorm distribution and Intensity (observations are made eight times
daily). -Tho study was based on st;~tjons located in the European SSSR and Central Asia,
supplemonted by data from similar stations In Great Britain, and tht-i compared with
data from meteorological stations. All observations were averaged for 5-degree grid
squares. Tables were prepared for the number of thunderstorms, number of days
Card 1/4
'.7 T.,

L 24486-65
ACCESSION NR: AT5002954
with thunderstorms and duration of thunderstorms for each grid square. Data were
analyzed for the Juno-August period for the area from 45 to 65*N and from 25 to GVE.
There was good agreement with available data from the British s stem. Figures I and 2
y
of the Enclosure show the maps of thunderstorm activity for the summers of 1960 and
1961; these differ greatly. The regional differences and change in pattern between the
two years are discussed, although no generalization's can be drawn from such limited
data. However, such maps are superior to those compiled from meteorological data
because data are used for areas where no meteorological Infor7nation Is available.
Diurnal variation of thunderstorm activity was also analyzed. Orig. art. has: I formula,
4 figures and 5 tables.
ASSOCIATION: Glavnaya, geofizicheakaya observatoriya,' Leningrad (Main geophysical
observato
SUBMITTED: 00 ENCL: 02 SUB CODE: ES
NO REF SOVt 003 OTHER: 004
Card 2/4

L 24486-65
ACCESSION NR: AT5002954
0
ovo~
p
00
02 00
091
02
r?
ICA*
ors
nV. l.--Thunders
Card 3/4

L 24486-65
ACCESMON NR: AT5002954
Fig. 2. lbunderstorm distribution over gu-ra;,~
Card 4/4
('450
ISO,
'-ISO
no-August 1901.

SOLMIYE'4', V.A.
Causes of the discrolan-,y between attoal;herl-os and wiather
,.-cmditions. Trudy GGO no.157.*73-75 164 (HIPA 1728)

L 217 99-65 i~~ITT(D/FCC AGD(a)-5/AFWL/SSD/AFETR/RAEH(&)/RASK(i)/RALN(J)/
BSD(c)/63D(gs)/r,SD(t) GW
!.R: ~?5 GC1815 SIC,03016510001CO210301C~35
0115;r
Soloviyov, (Candidato of.pbycico-='-.ha=tIcal sciencoc)
V.
-4 Dotorrin in~! O;orr, activity fron direction -;f inding data on atzotphorics
'M=': Motooroloeiya I gidrololiya, no. 1, 1965j. 30-35
'-'TIC TAGSs atmospherics, direction findin,,;
data from European stations for 1960 and 1961. Anot-hor r-ap showing atorm cor-to.-D
can: 1/2
tatal land curface, and those aro insufficiant tor\"prodic' r ato- I -) dic--o
Vin yg, -~or -re
Z~cn~z at son thoy are uneloss. The nothod of dotor"--)Inr' diroction of 4nUrosphor-
41
ics is uniquo and nay bo used for distancoz up to covoral thowanj kil=ators,
Tho SSS U
R has 15 stations for atrosphorles observation, arranrcd in throc rrourc:
Zuropc3n,-Contral ~;ian, and Far Eastern. Tho direction of atr4aphcrico Is deter-
r..'nod by sinultaneouz obscrvation at thro6 or four points. Thur. far, irXor=tion
on stmosphorics has boon usod only for refining, the position of fronts, for
zainini; somo idea of atom conditionc in re,-
& ,ions without imathar stations, and
tho lil-c. Tho author attempts to uso such data for dollneating tho charactoriz-
tics of storn, activity. Maps of atom activity vero prepared on tho basis of
IM -1 PA 4 vort sman
CT.- Tho data from synoptic charts reprozent, porcont-i,-,o o!'

L 21799-65
ACC-~'c'ZION MR: AP5001815
0- the basis of AUk)spherics- vms alno'preparrod. Thi3 =p shoix that t~:a daily -
behavior of different centers distributed along lines of latitude v_-ioc, Ivat !x
almost identical along moridians. It can bo observed that storm cj"xi:nuro nirr!.vo
earlior toward tho cast. On continents, in ganoral, the storxr,-aativiV~ zx%i_-.urj
arrive in 12-15 hours. This is apparently duo to earlier heating of -a land.
1ho larger the number of water bodies in a region, the later the arriv-al 0., t~-.o
r.axir.xr,a, coming as late as 18-21 hours. The author concludas that eata on direc-
tion of atrosphorics may more completely describo storm activity than data of
weather stations. It in oanecialiy important to note that these dafa por-t,.1'. foro-
---casting -for- the--ocean and
tablei.
A.SSOCIATION: Glavnaya geofizicheskaya observateriya (qh1ef Geophys cal g1morva-
tory)
31"IM,17TED3 04Fob64 ZNCL: 00
5UB GODE't ES 1110 RL? SOV: 003 O'Mra: 000
Card 2/2

20~
w mew -10- -AM --W. i-
Aiii.T"A PO
ISS.A. Ilk a
" MP
I In MA a "
The PAM, MW the lnteo*y of The nhm Ed bfto b
11M.M ad a livitak callet ms wh m a rmdwwtgf
'W. *W*j. The tbi. Law&* 1 .4 l1w Olmajobilis
'*'7*,'ZT IN,
Larw all
intavAll 40 ale med bum is .%JAM, -
C at dw am. wd the abwtmkm reiril, -1
all
to%
at a
with a mut
.X 2A. C .
4.11, 40.1
UM. 0.43. 901, TOM. 40.91; #`QlY-
ul, 7117IRL O.Mll' 0'3:k. QJ3; bi"N" IN (adleni"a
leap. - "*) JA 2.4. 3.1. -. 3,9. PWS of klg a - A
fum o1 Ng , on V~ 1w ra4m &W bituimn. Iml Or
dimime*m- ed CMVO* toTho Tisisof IP lw thrl PATVW-

V. A.
USSR/Physics - Ultrasonic in Liquids May 53
"Absorption of Ultrasonics Waves in Liquids and the
Molecular Mechanism of Volume Viscosity," I.G.
Mikhailov and.A.A. SolovIyev
Usp Fiz Nauk, Vol 50, No 1, PP 3-50
S
Study of theory of "-T)er-Strokes" absorption coeff
ultrasonic waves in liq-uil- inlli::ates tfi4t moic~.-ular
mechanism of vol viscosity is not yet clarified.
Further development of theory of structural relaxation
would be very useful (see J.J. Markham et al. Rev
Mod Phys. 23, 353 (1951)).
261T100

MIKHATLOV, I.G.; SOLOVIYXV, V.A.
Use of compound piezoelectric vibrators for studying the mechanical
properties of polymers. Mmst.zhur.l n0-4:3103-347 O-D 155.(KLAA qs2)
I.Lentngradskiy ordona Lonins, gesudarstvannyy univorsitot Imeni
A.A.Zhdaneva.
(Oscillators, Crystal) (Polymers and polymerization)

A'sc nE rdEORT OF IME Ul"MMU Irk]
Val. 2, No. 3, 2'-p540 (1054). In Russian,
The ultraswic intc-r1tvroetcr is widely u~," for ttm measure.
ment of use ctn be
extended to the meaiurd-
went (d the aboorptlon coaft-Watx, praNtd-
ipg absorption to not great. The author puts forward a new compu-
lational formula to be applied to the interfarometer mozirArtments
in order to obtalri the absorption coefficients. C.R.S.Manders

USSR/Acoustics - ultrasonics.. J-4
Abst Journal: Referat Zhur - Fizika, No 12, 1956, 35565
Author: Solov'yev., V. A., MikbAylov., I. G.
Institution: Lentngrad University, Leningrad, USSR
Title: On the Theory of the Composite Piezoelectric Vibrator
Original
Periodical: Izv. AN SSSRJ, ser. fiz., 1956, 20, No 2, 261-267
Abstract: Description of a method df investigating the mechanictl prc er-
ties of high polymers ovir a wide frequency rang( (10 10T
cycles) with the aid of a composite piezoelectric vibrator. A
bar made of the investigated material is glued to the piezoelec-
tric bar in which oscillations of the required type are excited.
The resonant frequency and the Q of the composite vibrator are
then measured. The contribution of the piezoerystal to the pLra-
meters of the composite vibrator can be readily elimimted. The
theory of the composite-vibrator is analyzed and equations are
derived for calculating the complex modulus of elasticity of the
Card 1/2
US84/AcouBtice - Ultrasonics, j_4
Abst J(xirnalt Referat Zhur - %?'UikaP No 12) 1956t 35565
Abstract: investigated substance for the following 3 types Qf load of the
Piezocrystal: load on one sidej the lengths of the piezocrystal
and of the specimen are chosen &ribtrarily.
2 equal *Pecimens of arbitrary lengths, L*ad symmetrical
Load on one side
the length of the specimen is so chosen that its resonant . but
quencY is approximately the Game as the frequency of t fre-
A comparison is made of the 3 variants he crystal.
$ principally from the
Point Of view Of their use for the investigation of mechanical
properties (modulus of elasticity and absorption coefficient)
of high polymers.
Card 2/2

StOd" P(Aymers,"
,qlte vlbrW.
prei,.nite,3 a", thF-~ Semirar On MYS'", Al~p1l.catirn ~jf Ultras, -,.-.n,l '21-26
cic t
en.! ngrad -

L JL 6, U'- .1 iii, o L,-,e propeities of polyetiAyiene
and ol paraffin by a composite vibrator method. (Issle-
dovaniye izekhanichoskikh svoystv polietilens. i parafina
miet-odom sostavnogo vibratora.)
P!~IdOLDICAL: "A
kuuticheskiy Zhurnal" (Journal of Acoustics)
1957
l
,
0
Vol. III, No. 1, pp- 65 - 73, (U.S.S.R.)
AB,-~'~iLl.(;T: Meauurument of the dynamic Young modulus
E = El + iE"
(where El represents elasticity and the imaginary part I"
represents the energy loss) in polymers by the composite
vibiutor method has been described in their earlier works by
the authors 1), 2). The sample of material umder test in
the foiti of a rod, is attached to the surface of an axially
vibrating rod of piezo-electric material, The self-resonant
frequency and mechanical losses in the sample an then
deteivilned from the change in the resonant frequoney of the
uquivalent resistance of tile vibrator. If resonant frequencias
both of the piozo-clectric rod and of the sample are nearly
equal, a sample rod of a smaller dianter than that of quartz
uLay be used 1), which permits wider application of the mothoa,
namely, for testing materials with low sound speed and high
~otjoos. In the present article, the method is applied to the
Card 1/3 hivestigation of mechanical properties of polyethylene and
i~araffin (used for condGnsers filling, mean molecular, Oryo-
sopic in benzole weight 490) in a wide temperature rango,

Lnvu-,ti -utioi, iiiLUo Ltie- mechanical properties of polyethylene
and of parafLn by a composite vib*r"Icitor method, (cont.)
o" 46-1-8/20
-165 to + 90 ,, in- ;-*,~,ic.-4 the 3uund velocity drops to the
ordur of 250 ra/sec- Ueazur~-;zents were made at 40 Ot W-5t
.. s in a thormostatically-contro led (to
75.0 and 100.3 i
within 0.1 0 .3 0~ arabience, The self-resonant frequencies
of sainplus wer-,- within 10,~~ of the frequency of the quartz.
Results are u~; graphs of Ell S" and of the
loo-Arithnic. as functions of the temperature.
C) A peculiarity of Lila curves of temperature dependence of
the sound veloci%,, both o-f polythene and paraffin is a very
ra-.)id fall of tha velocity with temperature. Curves for E'.
(enei-,~;y losse;;-t) shew 2 distinct broad maxima. Although their
positicnin, is riot accurately determined and the temperature
interval rath~ar narro-;., it can be reasonably firmly established
11-hat t!jQE;U maxima, -.r4rhan frequency is inci-aased, tend to shift
towa:L'd-, the Iiiji temteratuie re6ion, which implies that they
are of rulaxation oiltdn. 1,;omlyarison with dielectric
m-uasuru.L-.,eiAs zho-vs- that the form of rulaxation spectra in both
cases, differs, thou~;h the positioning regions coincide very
well. I-To dispei,sion can be observed, which cannot be explained
from t1l.-c I)oinU of view of relaxation theorj. The results for
Card 2/3 polD~ethylene are lart;ely in accordance with results obtained
by others. Proia t-;~--oretical considerations, a third maximum
sho-old be expected for E" in the investigated temperature

111 v,; ;t i-ItAOn i1'60 Wiv lacci"anical propeities of poiyt~'-h lane
and of' jitraffin by a compoelte vibrator Laethod46ii2g
ranUe, but it ik; pi:obably Lnasked by the too small vu~u2e of
the Investigated moduli.
5 graphs aie included. There aie 1C references, of which 7
are Russian.
ASSOCIATION: Deningrad State University (leningradskiy Gosudarstvennyy
Universitet. )
SUBMIYLO: Mlay 10, 1956.
AVAIIABIX:
Card 3/3

r771 V cn nd Sci
t 0d of
Of
C; t7,-,,,, 011 n, c z oe r; r I c v b r o r. e: n 9 ton C-rdcr of
z
1'. in. t t Uldv -nov. Plivric:,-

AUTHOR;3: Mikhaylov, I.G., Sn.11011ro'l- Syrnikov, Y,.,. P.
TITIZ- T~~- Main Probl- C
"a 1 r A c o u
Zhurnal, 1953, Vol 14, Jr
U-3), "R
AB3TRA'_'T: V-do is a roview of the Pr~-,-zent utat,.~ of ._~C3.
Both We~A~~-cr, atid Ru~'I_Aan wor'.: is In vicw of tll-~
r,7A,-..,tivc 3i~aAiciUy of uItrasonic Lho vclo~Atj of
:3_)j,-,d h,,.,.s b-,~cn g.-.ej.~;-ured in a v,~!rj lar,'e nu.-~b.ir of
Z-,f! vel)city lv,s been correlated with variou3
;iicro~;c,:)pic pro-.,e_rti,2-o of liquids and varir,)w~ e-.-,.Arico.1
!,,-.v~~ `,r!en ~,u ;--~_ted. kaong thre -e rulf,-, i-,i tlv~ _)nc
U.) Rau, Ti~.e -gint Dat that; in their opini:)n
rule doc-~; not sum:.iarise any special nolecialar LiezhiMion.
Tjhis is ~,h6vvn above ull bj the apiroxim-nte nature of thia
I-esult and.'its limited ramp of ap-Aicability. The correct
vIraj of devc1opin- tI:cor:_-IU-ica-l acou:;tico would be
r;a1culate zho coit:,rcsjibi!itj anC~ lienec the volocity of
u!" r A.
.11:-ut h~~r than t-o try and find a thoorotical foundation
f3r Rao'o 11:)viever? a.; is well tInia ij-. verj
-i-Llicult --nd kv-,3 r.,ot -is pit b,-,cn dot-,c. ottc~:ints havo
1/3 11 ~o calculate tllr~ velocit.7 of sound dire-tiy from

)V-11 G-1; -l/ I
I c -.-, rl -I ~,-, ra (it :!f'.; ar, 7 ) but 1 nattc---lptn
L,1(2 v,Aoc~Yty obtain;~6 not- a 3olutlon of tho
r;quat;on b)AL by ailnj.: vur-/
ul,, t, -Dnf, give the riF:ht ord -,r tho
C al U
v,-,iocit.7 of s~)Lmd but, they are quit-1- ur.',,~Ieos in ~llrovidinj;
iii1L"rjr-.aa~Q-ic)n !xi t1v! act;i~,,l ~;truczure j,L' th,:., Part1,:izlar liquid.
R,A Llv~orj poirl.-s to a --orinc-etiur b'~tvUc"i volume
procej.~e.,, .1-o F--j,.,*L1ibri.,aT..
irrevercibie 11
Some -)n this been done bj 3thevs
(R.-,,f~-15 rmd l?). In th---, author!.~' opinim, t1heory
i;-;vcj lmq :,D"At cnrre~,-t ~Ivsical pictur(, of th-) --~~r~uctura of
i i UnfDrt-anitely, at tha pral-eiit Li.mr-, ';he anthem-atical
UJ ~~f thi-,, "heory is n3tt .;ufJ.'icie,)1:1j d,,--r~Aoped. Tale
ai~vAovm--~nt of ill
3 )l 27,1
to t;.
of
i t iin Wo-ld be :,f A-,ij3r valw,, in the
Lhe
revie-vt t,-l as to, are

T i r Ac 0, !,-!tic,;
Lho ~n I., Cw- L'I~
e
)l 11 U A'2 6L .)Ut 11-hat ill :_l~iny on '.;0(;
.1;ound, in liquids tho iAersit"r of
i.-u'-on into accr;owat. 01. V,.r~ Dth~"r xamq(~. it h been
Lh'Lt tlit~ coeffici'
ent ,)f ab3arpt.,
uo-,; ue~venu' -.)n '0io i.-tensitj ,~vcrk P)r rolati.vL~'L,/ low
L ud Al 0 "IX'.) 'I'll 2. 2 -, n t a 11 n Llh .3 ~: a in 'w Z;f
of altras,-??i5a 1L,2 lj':~ carriod out in .1
,Aul r
.7 ranro. Zi-o =t) n') fii-urus
57
26 av,) ".)vieto
tot (Lcnini;ra,~i
';~'atc univc-'rsity)
1~:t.~-nbor lit, 11
" ") 57 -
1. Acoustico 2. Smmd--VelociLy 3. Liquils-Acoustic properties

It UT"70 H o I
T T"'L Tiv., Dyn-~-,ic Vfscoo.-lnotic Pronort;-,~i,-.- if of
2r,1
-~,ure ;:!v
1958, Nr 4,
In n.-Pition to pr~~vlou.-
..V"l A"rlft:',on ar,7
or the lynrv;!lc Younj7ls mnliilw-, !,-n! intoi.
wit in on,~, 7.iorr~ of
a-H thr,:?o liff,~rornt of
'h
Tho -r.~tho-l of co,i-o:3ite piczoiilqctri,~
ri I --k t o [.!I ;v, m z7 I o ye Th u rv o r t h t 4) r, i -P u re
of jowil volocity c, !-~ccurtic X
rm
5 Ic c Io e n, r o i v ,n witliin tht) t-,r-iner-!ttru~ of fro7
C iin to rv~nrl-- --iOllinz- -,hg wilu-.~o of c in
I , :)ont
aro "lrtn ~,l The ~nrif~ctinyi on v-lo,~lty
-h

Thn D-.-n.-!.iic 7i:-.coelastic Pro,p~rti;.1-3 of Polyothylr~nv? of 5 - -1 -4/17
L --v :1 r7, 11 r -:~
curve3 1% th ! rc,,,:,ion or ths! law-te -r)-?rallirr~ loi i fa
rior~, pronount-c-! excopt in one, 'br: '
f I c ) oa.lI he poak
t
it:-'Af is Thp ,3o~~onl lo3- '-Oilcll, 1.,i
no!tr roo-1 to--):)eratur-~, i -i sh ;~f tn.,' to.vrtrl ; 11 lj~h t,~ i:, !ra-
i i r s ( u x ce 1) t it n th-i c no c o f p b r i t t 1. -) :-a npl o';' Ic nqu r - -1 r?-,l to
ci~vrl,~rl , iit rit d, M.,rQnt frequencl~::.s ~,Jo to loo kc/aec) Ath
a O'l-In!') of PE how tho2 f roqi.~Tincv I t o f the I n-a- tp'ip-
. 1~ y ! :-, or ll;ho o !or '-'
r;itur.., 1c,os pca'~ ~act~vation (.,n.:?ri- ! r I
but no lisperzion of c is ob-ierv--A. Lo-r-prassura
liffer.-, from -.,ulyethyl-le by th,?
Inv of rn-,-zificatlon of chaino ~th-! nunVir of !7roup:7
CH3 por loo -'roup!) C"12 ir. lo-,~,,(!r by - ti-niroii ;n iow -
r-n,l by th~-? correspo-t!ini7lv
A e -r -o of qr:,,~,t,illinlty !7o-~')o J n,-,nin3t 5o-ro ' If cry3t,11li-
-lity to accorlinj to lonnity). In this o~()-,n,~,ction
to co-npoirf.- Vv? 'ynn-i'c -irop-~rtl,?3 of
lo-.-,,- ure poly~3tliylonc!.
I ut by ntvn,~roun author:3 nt
o
G~irl 2
2), 150-1500 c 'R,~ fn - 1-5 In

0 ~To-1 54-1-4/17
'"he Dynrimic Visco,)1-;ttir of Polyot,)~yl ,!'a ' ,
works the resonanco -.1ethod -,v~n onployei *n 1. frequency .7ns
x) f i(~-l tor-other with ti-,ipqratur~2). In the work ~!Ref.,-,)
,!.-.rrto1 out nt 2 kc, alio thoi dielectric losn-7-,; on thry
rr,~,pv.micy of' foria 1,5 TLIO lo Po -ro lnvo~ittf-!,' -A. Tho
low-tirrmour!'! polyethylnn,~ invociti,rrnto(I ).(-iro wn.., proitweel
tiy :jairp and '~121. The author thanks tknlreyovn for
tho -n-1 valu2s pInced r,t hii ft3pooal (thf.1 latter
ar,p-arin.1- Ln tho 4 f-'rat coltrina of the table). The vvipln
of low-7)res3ure pol:.~,ethylene - 2 ani low- Pressure poly~vly-
ind been previously m-ozifD7atel, (Rif.1)
is nn inlu-itri!O. proluct of th~_) Cfvr%~.c-il Kombinnt in Okhta.
Tho author '.h-n"-,i Yc. Kh. GolIC-r-M for t1v,, mrinnlos in-i
for bein- to!,,. th-_~ir molec-al-~r ani he also thvnks
1. G. '.Aknailov for vRluibl(, r~elv;cq !7'v,m. 71v3ro j,.ri I
I table, anJ ~, r~f,~r 2 of .7hich nre SInvIc.
15, 1957
VA ILA 7-1 T. 1,11irary of Conf-rens
C-,r,! 3/5 1. Polyethylene-Properties-Analysis

4`4 ( 1 ) 86/46-5-3-28/32
AUTHORs Soloviyev, V.A.
TITIEs On the Allowance for Reflection at the Radiator In the Theory of an
Ultrasonic Interforomotor (0b uchoto otraihonlys nA isluebatel* v
toorii ul'trezvukovogo, intorformotra)
PERIODICALs Akustichoskiy shurnal, 1959, Vol 6, Nr 3, p 382 (USSR)
ABSTRACTs V. 11gunas and 3. Jaronis (Rof 1) state that Ibbbard's intorfermotor
theory (Ref 2) is in error since Hubbard asamme that the secondary maves
are totally reflected from the radiator surface. The author points out
that when secondary waves are reflected froa a radiating surface its
vibrational velocity V is altered. Consequently either a now expression
for this velocity should be used or additional pressure, wMch would
need to be applioi to the radiating surface to keep its vibrational
velocity equal to Ila original value V, shimmU. be Includod In the
expression for the totAl pressure on the radiating surface. Both
Ga rd 1 these alternatives Are O%iv&l~at to An &sSmption that the secondary
waves are totally reflected fron the radiating surface, Hubbardes for=l&
is also confirmed by an exact solution of the interf9ranoter probleis
given by Mason (Rof 3) And S010v'Y*T And MikbAylov (Rof 4). There are
5 references, 2 of ihich are Soviet, 2 English And I other.
ASSOGIATIONsLoningradakiy gosudarstvannyy universitot (Leningrad State University)

S/081/60/000/007/012/C)12
AOO6/AOO1
Translation from: Referatlvr,.yy zhurnall, KnImilya, 19050, No. 7. P. 623, # 29428
AUTHOR: Solovtyev, V. A.
TITLEs The Use of a Composite Fiezo^-lootrIc VIbrator for Invest1gating
the Me~hanlcal Properties of Polymers 1
PERIODICAL- Tr. Seminara pa f iz. I priment-miyu, ul I trazyuka, rlsvjasheh. paWati
prof. S. Ya. Sokolova, Leningrad, 1958, pp. 10- ?
1,472
TEXT: Sound velo-zity &,.d the reactive portion of the speo~fi~~ ar';"Stic
Impedance (depo~nding on t,,~mperatuire) in polynAthy-'-met:-AC-Vlat81(I) wo~re
mpasured for the purposi of zhecking the appl!:-abl-11ty of lln'jar approximat-'on
wl,en analyzing a composilte piezoelsotrlc vibrator of variable o.ross sectIM.Ceses
wi-e studied when the seotions of the rod of I and of the plezi-quartz rcd
we.ra equal and when they were diffirent.. Tli-e mtbthod of meazur~-=ent and lh,,~
lu -1 1 A )lei 4 Z'
,~al~-ulatlonal formulae were d,~s,,rlbed 'In ar. ar'.L,'-& p t 'i RF-M1 1956
No. 8, # 22 568. !t. Is shown that when the natural frAqu^.11i!t-s of I a:-'kd Lhe
piazo-quartz rod ar-i 4-hq samq, th,:~ lln-~ar apprix!matlon is just1fled wlth the
Card 112

81/60/000/007/012/0 12
A004-IAOOI
The Use of a Composit~! PInoq1eotrIc Vibrator fmr 1rvestIlgating the Mechanical
Prcpsrtles of Polymwrs
d& leg 4'
boundary cndltlon.- th-~ equality cf tvctal for:es actirg on the bown r
th-? rcids. LLnear approximation dot3 riot. provIdq for a suffIcient aocuracy In
t
,he case of a t~ompcsite vlbrat- with rcAs of mrlablo cr,~-sp seAlons, 11f ti-,q
rf,sonance fr4quencIA3 of thi dn not apprca.-*h th4 )p,?ratl-ng fraqwtncy of
4 A. I
~he Nlbrator. It is ~on.~-udo~d *.hat tt.4 method ~&n bA usal ford thq
stjdZ,r of polvme-r-s !" tte Patnral fr4qijqro~ix,*s ar~! Aqua! wid *
~4 ,iat It is
practl,-;ally th~-. only mql.hod In a tr-ij*utm~~y rw,,ge of I - 0 cycles.
T. Khazanc,.ri--h
Translator's note.- This is tt~4 full of t)-,~- orfglnea thA'selan
abatra:~t.
Ca.--I 2/2

26396
B/046/61/007/003/002/004
3104/B201
AUTHURi Solov'YOV, V. 'k.
TITI,'"": Relaxation of exoitaticn of molecular vibration levels
FERIODICALs Akusticherk-U zhurnal, v. 79 no* 3. 1961, 337 - 344
TEXT: The establishment of energy equilibrium between the degrees of freedom
of translation and tho degreon of freedom of inner -4lecular vibrations When
taking an excitation of higher lcvols into account ie dascribed by a large
ntLmber of relaxation ti=es. I Tb calculats tham, it is nocassary to introduce
lfg,-Aneralizod coordinates" in %hich the oyatem of oquatiens of excitation
reactions is split into independant equations. If the probability of trans-
itions betv,~en the levels has the same 41'orm as that of dipole tranjitions with
e=ission, this problem can be solved. 'The preseat papar offers an exact
solution for isothermal relaxation and a solution in acoustic approximation
for relaxation at a variable temperature. If n II ne n 39 0660 MolecU700 Of a
gas or a liquid are in vibrational states with the energy levels Op big 2bV,
3hVj **of the equation of excitation raaction can be written as
Card 1/4

26396
8/046J61/007/003/002/004
Relaxation of excitation 060 B104/B201
DO CIO
0 3, ....
n a a,,nk
kao kao
k4.j k+j
To solve the problemg the "geno.-alized coordinates" zust than be found as
i M
lin'ear combinations of the "natural coordinates" ne all of which obey the
x - Se) (m ~ 19 21 39 ... ) by Mantiollshtam and Loontovich.
Here# denotes the equilibriuz value of displace2ent I being tho
fm Im
rolaxation. time of aucix displacement. 7his equation can be oasily solved if
extornal conditions (such as temperature) aro constent* In this cormeetion,
the number of "generalized coordinates" equals the number of indepenlent
variables which describe the eyatem, 7hia number Is irdnitely large in the
present caae# and so is the number of relaxation times* If only exoitatic.--s
of the first vibration level are taken into account in the simplified theoryby
Kneser (Ann- PhYs-, 19339 L6P 5t 337) and Rutgers (Anne Physep 19339 -169 5t
Card 2/4

26396
S/046/61/007/003/002/004
Relaxation of excitation ... B-404/B201
350), only one relaxation time will be found in the experiment. These
circumstances are examined more closely, and the coefficients ajk derived
by L. Landau and Ye. Teller (Phys. Z. Bowietunion, 1936, '0, 1, 34) and by
R. N. Schwartz et al. (J. Chem. Phys., 1952s 20, 10, 1591 - 1599) are shown
to deviate appreciably. The author's calculations are based upon the model
by Landau and Teller. For (1), equation
f1j ~jB-&(J*1)AJ n +Jkn,_,+(J+I)Bnj+l (J-1s2,3; ... ) (5) is formulatedt
j 0 .
which obtains In generalized coordinateal the form
m oc~
Z ml -A _5~ ji n , and, in natural
m k-1 k1(m-k)1 J-k k1(j-R11 j
coordinates the form
C~O k
n . 2- (_,)J4k k1 2 )(1 A k-m ~., From these
j k-,j M-~ mi (K-M) 13-A
37 k--j I!
equatione, equations of the form (2) with relaxation timee'r m a 1/m(B-A)
Card 3/4

26396
S/046/61/007/003/002/004
Relaxation of excitation ... B104/B2011
are obtained for each ~M* The equations obtained here allow problems of
isothermal reiazation to bo solved. The Boltzmann distribution Is dis-
cussed for an example. The application of results to the solution of
arountic problems in dealt with next. The coefficients A and B In (5) are
not constant In this case. The sound-wave amplitudes are assumed to be
"mall, which permits (5) to be linearized. The representation of the
relaxation equation in diagonal form is given in the appendix. 1. G.
Mikhaylor is thanked for his advice, and A. G. Vlasov for a consultation.
There are 6 references; 2 Soviet-bloc, and 4 non-Soviet.-bloc~ The
references to Englli3h-language publications read as followst R, N.
Schnartz et al., Calculation of vibrational relaxation times in gases. J.
Chem- PnYs-, 195?, ?20, 10, 1591 - 1599; E. W. Motrollg K. E* Shuler. Stud-
lea in nonequilibrium rate processes. 1, The relaxation of a system of
harmcni-, oscillators. J. Chem. Phys., 1957# 26, 3, 454 - 464.
ASSOCIATIONt Leningradskiy gosudarstvennyy universitet (Leningrad State
University)
SUBMITTED~ November 17t 1960
Card 414

SOLOVIYEV, V.A.
"Absorption and dispersion of ultrasonic waveB" by K. F. Herzfeld,
T. A. Litovitz. Reviewed by V. A. SolovIev. Akust, zhur, 7
no.1:120-121 161. (MIM 1,414)
(Ultrasonic waves)
(Herzfeld, X.F.) (Litovitz,, T. A.)

S/043/62/000/000/005/010
D207fD300
;O*L-I.i ), 1AI.Ya. , Iali'.-.Iiov, !,.I:. .~nd ~;olov'ycv, V.A.
of the absor-ption of ultrasound in polymer
soll. L 2. Olis
-AroyetAy'! i lizicheskiye svoy~-tva veshchestva v
L
..L.idl:on :;or-toyanii; naterialy IV soveshch. ljo.probl.
zhid:.ollo so.,.t. -eshchesiva, v Kiyeve 1959 g. Kiev,
;.icv. Univ., 1962, 85-91.
-~x.-~erincixtal results for the absorption oZ ultrn-
:-,owit, in soLitiont; in benzenc (3 - 3.51; conc.) are
accuunt(itl ~-oz- by tl-%-''ollowing model. -Pol er molecules are repre-
yn
';CnL'ed ')y elastic innersed in continuous viscous nedium.
.~Lc Tilat-.1cill.-s c-:-.cciitc ; cments and assurv- various bent-
rownian riov
,tiha,jcs. Van dcr Wa,~J.s interactions (and dipole interactions in
Volar iolyucro) ixtween the filaments make them behave as a network
joined 'by Van der Waaln bonds. -riction with the solvent and betueen.
the individual segincutS o.7- the neighboring polymer filaments are
Card 1/2

S/B43/61/Ooo/ooo/oos/oia-
Theory of the t~)sorption ... D207/J308
'111ollod A-or. of the viscosity is included 6y assutiing
;I II(ItIrly cowAivious of reliwation tinen. This Tiodel ac-
cowAL.,; or (1) the lacl~ o," correlation ~~twecn the viscosity and
tiw absor,,tiozi con'icirnt of ultrasound in a polymer nolution,
2) thn re(biction of tlv~ ratio (YIV2 (oL, is the absorption coeffi-
cicnt and, 'v i3 tho ~-rnqUICIUCY) vith increase of the ultrasound
frcquency, awl 3) th ,rcwersibIc changes of structure appearing at
high sound intensitios. Thr~ theory is presented as a physical des-
cri-,ition of tae vic-ch-luiLmn, i-,volv(,d, vith a minimum of mathematical
trcatra(,-at. Tliere are 2 figu~cs and 1 table.
Institut w1sol:onolelculyarny1ch soyedineniy AM SbSR
Unstitiitc o~: High Molecular Compounds, AS USSR)
Card 2/2

SOLOV I YEV, V. ~A.
Relaxation of intermolecular oscillations in gases and 11 ulds.
Ukr. fiz. zhur. 7 no.8:854-M S 162. = 16s1)
1. Leningradakiy universitet.
(Molecules) (Oscillations) (Quantum theory)

MIKHAYLOVj, I.G.; SAVINA.. L.I.; SOLOVIYEV V#A*j SYROVA, M.N.
~ P
Absorption of ultrasonic waves in t.~diokols. Akust. zhuro 9 no#4:
460-465 Y639 ("IRA 17:3)
1. Leningradskly gosudarstvennyy universitet.

S/04 63/009/001/013/026
B104YB186
AUT111ORi Solovlyev, V. A.
TITLF; Adiabatic relaxation in a system of harmonic oscillatcre
Ak-,j3ticheakiy zhurnal, v. 9, no. 1, 1963, 72 - 75
A.
M-AT: flaking use of formulas and results of previous papers (V. A. solov~evt
Akust. zh., 1961, 7, 5, 337 - 344; A. I. Osipov, Dokl. AN SSSR, 1960, 130,
3. 523 - 525) the Osipov equation is solved without restrictions. The
spectrum of relaxation time for the adiabatic process of establishin6 an
equilibrium in the energy distribution on the molecule vibration levels is
calculated. In this calculation, energy transfer between the oscillating
a.-,.d the progressive degrees of freedom and between the excited states
(resonance transfer) of different molecules are assumed. The transformation
to nor.-.;al coordinates defined in the previous papers has the same form as
is obtained with isothermal relaxation in a system without resonance trans-
fc.r. The natural acoustically active coordinate is the number of
vibrational quanta in the system.
ASSOCIATIONt Leningradskiy gosudarstvennyy universitet (Leningrad State
University)

(WENT (OVEPT (c )/Epp (n) -21vdp( jvvi6 (b.)
_q ~_46v, E4T -4f
,ru-4 (c) w/M4
ACCESSION la AM5001446 BMK EXPID rrATXaf S/
Syrut
M~Khjtylov I or' 01.ggInvich; qo ~Vlld A a ot kov. luri
Pavlov,ich,
,-,u3Ar acoustical -v0
Principles of,moler L0m%cr,7.m6lekuly;&rnor akustiki)# Moscow# Izd
"Nauka". 1964, 514 p. illus.0 biblio.p index. 4g5OQ copies printed,
iTOPIC TAGSs acousticap sound vavep thermodynamicap relaxation process,, polyrors
sound - absorption,,- acoustic-
TABLE OF CONTEWS (abridged)s
Fbreiord -- 9
Introduction-n
Part 1. Use, of acoustic methods to study equIlibrium propeAies of aul~dtnnoeg
Cho I* 'Th=7 of sound propagation,
Cho 11. Speed of sound and struotvve of &.aubst4=*.v Gaseli
Cho Me Speed of sound and structure of *abstanceso Liquids and aolide"-,69
Cho IV. Soood of sound in mixtures and solutions - 121
Part 2. U311 'Of acoustic rethods to study nov-oquiUbritm properties of a
Substance
Card

AC=1011, NR AM50MIM
1Ch* V, Sound ways absorption '163
Ch. VI. Fhenominological roUntion theory 202
Ch, V11. Jonaral thermodynamic thoory of relaxation proceflaes In a sound inve
(the theory of L. 1. Mandollshtan and Me A* Loontoovich) - 236
C*h, V111* Chemical relaxation - 283
Che IX, Exoitation of oscillatory degrees of freed= of molecules 3U
Ch., X, Relmtion processes in gases - 330
Ch. X1. Relaxation processes in liquid -0 365
Ch. XII, Relaxation In vol. meas and low-molecule solids
Bibllographr - L83
Subjeot index . 511
S*JBKrr=s 22jul64 SM Cam I OP
NO RU SM 1 215 OTHMI W
Card' 2/2

L 5o67-66-~W(m)/EFF,(o)/EWP(J)/T/E*oiA(h)/V;IA(l) , lm~d/Mt
WC7,r-9R--AP5O22645 UR/0089/65/019/002/OP01/0203
539ol6.07
AUTTIOR: Konovalov, Ye A.; Ploshchanskiy# L. ~ff;-Llovljavt V, A.
TITLE: The Use Of polyethylene pipes in pipelines of dosimetrio air
sampling system W-,!r Y
ZZ5
SOURGS: Atomnaya energiya, vs 19, no* 2, 19659 201-203
TOPIC TAGS: nuclear reactor, atomic energy plant equipment, air
pollution control
ABSTRACT: The radioaotive-air samplers are usually equipped with pipe4ft
lines made of aluminum or stainlos tool pipes. The possibility or
their replacement by non-corrosivekolyethylone pipes is discussed.
The authors describe their exper ents with the polyethyline pipes bav-
,ing a 20 mm diameter and 4 mm wall thickness. The results of their i
tests showed that the polyethylene pipes could be used at temperatures
up to 60 C. pressures up to 3 kg/sq cm and rarefactions of 600 mm 11ge
At the beginning of 1962t the air sampling pipelines of the VVR-M
reactor were equipped with polyethylene pipes and tubes, Their total
length was about 3000 m, No trouble wee experienced during two years
Cord 1/2
4 t.3,
v9 6 16

-L-5067-66
AP" NR- AP5022645
of operation of this stetionary dosimeter system at tha,ph-valcotechni--l
oal Institute im. A. F. loffe of the $33H Academy of Golenoes, Orige
art@ has: 1 photo showing the.mounted pipes,
ASSOCIATION: none
m

A- CC) DE: UR/0126/66/0'-12/006/0665/0870
AUT11011: 11. Y.-L.; Soluv'Ycv, V. A.
M F
ORG: TsN11ChEM T im. 1. P. Bardin
TITLE: Calculating the diffusion growth rate of a pore under the action of applied stresses
SOURCE.: Fizika metallov i metallovedeniye, v. 22, no. 6, 1966, 865-870
TOPIC TAGS: diffusion, porosity, polycrystal, crystal vacancy, plastic deformation, metal
grain structure
ABSTRACT: It is experimentally knowii (Rozenbcrg, V. M.,et al. FMM, 19G6, 22, 438) that
the application of relatively small stresses at high temperatures causes the growth of macros-
copic pores at the grain boundaries of Cu polycryst;ils, chiefly owing, to the diffusion of vacan-
cies from the material to the pore. Two possible interpretations of this process are analyzed:
1) diffusion of vacancies into the pore because they attaln their equilibrium concentration ear-
lier at the surface of the pore than in the material; and 2) vacancy supersaturaUon of the ma-
terial owing to plastic deformation. The kinetics of pore growth in the presence of applied
stresses is analyzed and it is shown that changes in equilibri= concentraUou owing to elastic

ACC NRt AP7002737
stresses alone are not enough to assure the observed gromh rate of the pore. PlasUc d 0.0
formation, on the other hand, leads to an increase in the concentration of vacancies in the
material, thus leading to an excess concentration of vacancies and hence interpretation
appears to be more probable: supersaturation with vacancies of the material owing to plastic
deformation is responsible for pore grow-th. It Is worth noting that even a small increase in
the diffusion coefficient D can markedly reduce the extent of vacancy supersaturation needed
to cause pore groN%th. At the same time, plastic deformation can markedly affect D. Thus the 1,
above interpretation accounts for the experimenta.Uy observed growth rates in the presence of
a reasonably moderate degree of supersaturation. In the general case, parUcularly during the
initial stage of the process (small pores), allowance must also be made for the additional
transport of vacancies along the grain boundaries of the polycrystal. Orig. art. has: 27 for-
mulas.
SUB CODE: 11 20/ SUBM DATE: 07Apr66/ ORIG REF: 009/ OTH REF. 001
L_qp_rd_2/2

V.A.
Ictural. position of the Chirkovskaya Dopreszion in the Cenortl
oyatem of dopresnions or the Iiinusinak intemontano trough. Geol.
i geofiz. no.]-1:49-56 160. (KII-I 14:2)
1. Imstitut goologii i !;eofiziki Sibirskogo otd-oleniya All SWR9 Novo-
sibirsk.
(Minusinsk Basin-Geologyp Structural)

PARFENOV, L.M.; SOLOV'YEV, V.A.; BOROVINOV, A.M.
TecLonic terminalopy. Geol. I geofiz. no-9:118-123 '61.
(MIRA 14tll)
1. Institut Fcolofii i gpofizlki Sibirskogo 3tJelenlya xN SSSR,
Novosibirsk.
(Geology, Struct.;ral--Terminolory)

. "I-,V ' "' ~ - %F 9V . A.
Genetic relationship between ~Jle Cnnazcic and Mesozoic troughs in
westerr Transbaikalia and the fault systems of different &fee. Gaol.
i geofiz. no.409-87 163. OURA 16:10)
1, Institut geologii I geofizlkl. 031birskogo otdeleniya AN SM,
Novosibirsk.

KOSYGIN, Yu.A.; VAN.IYAN, A.L.; SOLOVIYEV, V.A.; KURIN, Ye.P.
Recent data on the deep-seated structure of the Lake Baikal region.
Dokl. AN SSSR 151 no.5tll62-1163 Ag 163. (MIRA 109)
1. Institut geologii i geoflaiki Sibirskogo otdoleniya AN SSSR.
2. Chlen-korrespondent AN SSSR (for Kosygin).
(Baikal Lake region-Electromagnetic prospecting)

~, 11; V' Yt-z,., V.A. ;, , I..; A , ij. . .
v
Reviews and discwssions. Izv. AN SSSII. Ser. geol. 30 no.!*~: -
11P-126 Je 165. (1,41M 18:61;
1. Tnstitut geologil i geofizlki Sibirskogo otdeleniya All SSS.R,
Novonibirsk (for Solovlvtv). 2. Klyevskiy gosudarstvennyy uni-
versitet, Klyev (for E~nor).

".,i
Th!.,rderstorm activlt,7 In ti-c-, rt-glcn of the northeastern Atlantic
and iestern F.Lrope ~,:i data on atre--apherl.-as Trudy GGGO
nri.177:31-36 165. (YJRA 18 18)

KIKHNOp N.P.; SULWYEV, V.A.
Tectonle conditiore goveming the assoclatlon of Mceotole
formations In western Tranabalkalla. Geol, I goofla, no.10!
45-54 165. (MIRA l8il2)
1. rnstitut geoiogii i geofialki Slbdrokogo otdoleniya, AN
SWR, Novosibirsk. Submitted March 16, 1964.

SPUY"ITEV, II.A.
Diunderstorm activity of the Far Eeat. Trudy Dallnevont. ItITG?!l
no. l9rI91-195 165 (1417A 191l)

I"
A F V i AS I 'ff- I, Y~- I. r I i~ASIH A REN , A, 4K, 1, 1JASHARI NAt N.P. -, VC., )TH. C:.A, YEVY
V.,i.; K!lASll,lYlKOV. B.N., cta. n3d.: L.M.p Otv. red.
on toctoniq ternlqolngy. Part 3..Tec4.,onlc3 and its ilvision.
Ire-i3 -..n qtructtwal goalogy.) Materialy ro taktcnicheakoi terminologil.
Novon.lbirsk. Yt. 3. Tektonika i eo rul-icly. Terminy strukturnol gr-)10-
gLi. 1964. 255 P. (its Tridy, no.34) (MIRA 19t4)
. if%

SOLOV-11zv,-Viktor-Andj~e~eyichI tokar-rastochnik; BASTOV~ Viktor
Fedorovich~ inzh.; KOVALIZZIN, F.F.j red.; WANOVA, N.N.,
tokhn. red.
(Manufacture and introduction of multiparrose attachments for
machining compound parts] Izgotovlenie i vnedrenie universall-
nykh prisposoblenii dlia obrabotki slozhrqkb detalei. Mosk%aj
ProftekhIzdat,, 1961. 47 p. (MIRA 15:6)
(Machine tools.-Attachments)

V.Yo.; PA' A.11.j SOLOV"?,`V, V.A*; ; -'jOV A*Ie
PAOSHKOV
Selection of the optimum magnitude of the prea,.,-,,re area In NSh-,32 and
ITSh-46 gear pumps. Trakt. i sellkhozmash. 32 no.6sl4-15 Je 162.
(MIRA 15.6)
1. Moskovskiy zavod gidroagregatave
(Tractors-Equipment and supplies)

OSNAS. Ytt,v.; SOLOVIMY
- i _ig~
Repairing plane-parallel and measurtne rods. Ise. takh. w.4:39-42
jl-j~g 137. (XM 10:8)
(Ideights and =^sure a-Rapairt ng)

SOWTITLT. V.A.
I&PPIDg-lu of plane-wallel and seasures. Ismetekhe
no.4:1-4 Ap 160. (Kim 13: 8)
(I*Wb masuroment)

25(6) S/028/60/000/03/020/029
D041/Doo6
AUTHOR: Solov'Yev. V.A.
bwfioww"- W, ~dr*WP*r4Y"~-_
TITLEj Devices forAheckin;Nart Dimensions During the Machining
Process on Surface-Grindi Machines
1-f
PERIODICALi Standartizatsiyao l960pNNr 3t pp 48-49 (USSR)
ABSTRACT: The Komitet standartov, mer i izaeritellnykh priborov
(Committee of Standards, Measures, and Measuring Instru-
-ments) has approved the "GOST 9376-60" standard for devices
checking the dimensions of parts being machined on surfsev
grinding machines. The standard fixes 3 types of device:
for automatic, semi-automatic, and visual checking. For
automatic and semi-automatic checking, the use of in-
ductive electric contact or pneumatic pickups is foreseen.
In the case of visual checking the devices m&y be equipped
with tooth-lover measuring heads, dial indicators, or
special built-in meters. The new standard obliges machine
Card 112 building plants to raise the accuracy of surfaco-grinding

S/028/60/000/03/020/029
D041/DO06
Devicea for Checking Part Dimensions During the Machining Process on
Surface Grinding Machines
machineaq and instrument plants to supply the metal
working industry with high-stability devices*
Card 2/2

SOLOVIMj V,.A,o _
Rulerfor accurate measurement of external angles, Standartizataiia
25 no. 5:55-56 My 161. - (KLRA 14 t 5)
(Rulers (Instruments))

SOLOV'YF,V, V. A.
Cand Biol Sci - (diss) "Fffect of Cl- and S04-- ions on the
nitrogen metabolism of glycophytes and halophytes." Rostov-
na-Don, 1961. 16 pp; (Rostov State Univ); Ir.-O copies; price
not given; (XLI 6-61 sup, 209)

BARYSIINIKOV, F.A.j SOIDVITEVJ,-,V.A.j KOVRIZMYKH, Tu,P,
Interrelation between the petrographic and mineral ccuposition and
the germanium content of some kinds of coal. Trudy last. gor. dola.
Sib. otd. AN SM no.3:252-265 160. (Nnu 14:4)
(Coal-Inalysis) (Germanium-Analysis)

USM/Biology - Botany
Card 1/1 1 Pub. 22 - 44A6
Authors I Solovyev, V. A.
Title I Effect of volatile phytoncides on the germination of pollen
Periodical Dok. AN SSSR 97/4,, 741 - 744, Aug 1,, 1954
Abstract I The effect of volatile phytoncides on the germination of alfalfa
pollen, is explained. Four USSR references (1946-1951). Tables.
Institution t The A. M. Gorkiy State Universityx Molotov
Presented by: Academician A. L. Kursanov, March 22j 1954