SCIENTIFIC ABSTRACT VASSOYEVICH, N.B. - VASULIN, M.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001859020009-7
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 1, 2001
• Sequence Number: 9
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

VASSOYEVIGH N.B.- EJVAGILEVA, Y.S.
Content of aul,ochthonrus bitutflnold in scils and the deLect~'r-ri c.-f
the prtsonce in them of petroleum allochtbcn bituminoldc. Trudy
VNIGRI no,227 GeuKhlm.sbor. ni).9%132-160 164.
(MIRA 1311)

r
SOEDIDT, T. A.; T. P.1 VABSOIP~MNXs__;~.j ARTONOV, P. L.; CRUGGRITICT, 0. 0.
a& Ozary, Y. P.
'ImIgmtIon prootte"s of G" wA OU, Moir In6wity and DireotionstUt;r."
Abstract. The article gives a description of the processes Goo arutrWisrs observed on various levels of a section orJ
of migration of oil and got, their intensity and dirsidion In surface layers above oil and gas pools le3fiFy to the
In various stages of the existence of sedimentary rocks. vertical migration of goots and to continuous processes of
In the early stages of the fo(moNon of sedimentary rocks dissemination ol"all and gas pools.
the processes of migration cause a removal of excess gases Dillusion coofficients.1% for various types of rocks studied
Into aqueous medium and Into the almosphoris at well
-
vary between 10-1 104 It ec. In Nome cases one can
'l'
as a primary accumulation of free gases in sediments and .S
observe the dying of diffu of the low valves of D.
their solutions in underground waters. At " D * equal to 10-1 - 1; stinstse,- the clitsomin,36on of
During oil and got accumulation and the formation of goo pools by othlionstry diffusion alone is so great that
their deposits the following processes play the main parts their preservation within geologic time can be explained
transfer of oil in a dissolved stale both In compressed ga. he unsteadiness of the process and by the phenomena
by
ses and in the water, a removal of dissolved got and oil :
of he dying cut of the diffusion reducing put losses as
components from the water, condensation of liquid hydro. well as bry the recent, Iwo geologic sense, formation of
carbons from gases of decreasing temperature and pressu. those pools or by a conotinuout replacement of the gas
re and then oil and goo buo),ancy in porous waterbesciring due to Ito Inflow front deeper bedo.
beds and rack MOIL
The oil and goo pool formed undergo dissemination due Considering " problem of the time of the formal*,vit of

to oho processes of filtrations, cfilfvs;on as well as due to got accumulations one should take Into account ticif only

the solution and removal of out end oil by the water sur. the ago of a frop but also the amounts of poodble goo
losteit

rounding their pools. i .
The processes of 111froficin core, found to be most Intensive
duritio loodonic shIfto and they'con asm the clostioulng
9f a pool within a short period all timet.
U WWJIL
Fmarwt
"I*= Cw6ro"
,
ropwt to U nvwtud f4w MW O ,
I
ig.m% jvm n63
------------

VASSOYEWICH. N.B.
V.I.Vernadakii's concept of petroleva origin. Sov.geol. 6 n0.3:25-42
Mr 163. (MIRA 16:3)
1. Vaesoyuznyy neftyano3r.-,,chno-issiedovateliskiy geologirazvedochnyy
patitut. - (Petroleum geology)

vjssel~MCH , i. B.
Role of organic matterr-in tfie natural histor7 of petroleum
in the light of Academician V.I. Vernadskii's concept. Geol.
nefti. i gaza 7 no.3349-52 Mr '63. (XIM 16:4)
1. Voesoyuznyy neftyanoy nauchno-issledovatel'okly geologo-
razvedoohnyy institut.
(Petrol*.= geoloR7) (Organic matter)

- .. 1, . I ~ I
vl~- ". ~. , .1. -.
"Origin, evolution and urimar:.: ff' mi--i-coll."
report submitted for 22rid Sess, Intl GeoLogical Cong, flew Ll+-~,2 r"4.

VASSOYL710H, N.B.; BiZHEEV, P.M.
C-igin of block breccia and conglomerates in the
flysch of the eastern slope of the Central Urals. Lip. i jr--I.
( !,1 .7 IZ.4 -: ~ - "- )
iskop. no.6:74-82 N-D 164. - -

VASSOYEVICH, N.B.
~,ontribution of A.D. Arkhangellskil to the development of the
problem of oil formation. Vest. Moak. un. Ser. 4: Geol. 20
no.4%5-15 Jl-Ag 165. (MIV 18:9)

A
ATA
u~'Uctm ratuto intcdec-,ram. Ilk-- ASAI'lmy 61
grvips was aadic-d by tlio us,~ o1 41kAn~.
.~d SCW hydmlysic Th. jonZ f;:.th~d JRzz
711M Chrm. Ilay-nai. W5.1, 71. 843) Y'XI It.,und
tLvLluo far thm3 purptr~r.,
to 4"kahne t.-,Jluzn yfacts with KCI, r:ld 015
cxcess oll cpanidd ii de'triplavi by WlZttOfl WM*
with dipFenyLutxtzrj-m " imh.,,at~t.
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add --r;d thm hixi-ated ~,itef
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c!-tc'i eotolndiv ',:!or, to pr-rjer!t'
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ry
: CZ,gC11O, SLOVAKIA
:Laboratory P -,lipment. Tn3trumntao lfb,.7.Lr
lk
Ab3.
1959, :in. 1
Au ~ha r
T.1 t ir
Orl:*.
A); tj L re. Camago to tho rubber tubtriC. All ratert3 ~re
Cont'd equ.Lpped 1.1th clectronagnetic or mechanin.&I
nl;ters, noc~-s 11ith sections for the introdUc-
tion of 1-he rourent, uni sta*,jdard
or olectrodes.- 7. Knesslova

CZECH03LOVAKIA
KOLINSKY J1 VA3TA, M; CHROMECEK, R; BOHI)ANECKYS M
1. Research Institute of Chemical Technology, Usti nad
LAben - (kor ?)s P. Research Institute of Synthetic
Resins and Lacquerso Pardubici - (for ?),(Present
address of Chromeeek and Bohdanecky; Institute of
Maoromolecular Chemistrys CzeohoslovAk Academy of
3oiences, Prague)
Prague,, Collection Qf C;ecbosloyak Chemical Coigmul3ioatiorm,
No 7# July 1966, pp 2714-2726
*Kinetics of the etherification of phenol alcohols..Pa'rt. Is
Effect of structure of the phenol alcohol on the rate of
ether1ficatlon9w

I ~1762 -6~
Fr-4/Fir-4/Pt.10 WV/MM
ACCESSION RK: AP40147851
AUTHOR4 Zvonar. V. (Craduate engineer) ; V~aata, M. (Otdduate engineeir)
TITLE: Surface .phenomena at the glassfiber-resiAnterfaces in reinfor--,ed lam-
inates
SOURCE: Plaste und Kautschuks v, 11, no@ tO. 1964# S91-594
TOPIC TAGS: fiberglass, glass plastic, reinforced laminate, glass resin inter-
face, polyester mechanical property, polyester gvelling, polyester adhes a
ABSTRACT: nle machenical propertier, of glassfiber-reiftforced laminsited of P017--
eater resin are determined by the coaditione at the interface of tFe adhealve
d" fi_ler a~ vt�Li as 1-v the qoecific :~ropertf-~s -f the reoipective ruteridis. Thim!
weebanical properties are generally adversely affected hy water to e, consider-
able degree. The,,clianges, however, are 5--,,stly raverelble. Veriations in the
beadLng~.tcen8thearud- the elacticity nodtilus ara markedly dap*fident on the vary-
ing anoDunts of vater that "n-,trate th., 1&mirate. This reigeol the kiuastion of
hov such larg-2 amounts of water get in, PolveRter resin taket lip ai)proatmately
0.05% to, at a marimm, 0.11 wisture, vhich wculd hardly be onougY. to change
its properties to any noticeable extent. The surface of the glasir ti re cks
Card 1/3

L 31762-65
ACCESSMH NR.: AP4047851

'
up a layer of wator, several hundred colecules thick, equNtlent to ajtprozizate-~
.
1y 0.5 to 11 of the regin we"ght. Therefore, the "at plausibic explanation
for the uptake ~,f Rignificant ;1rrK-.nts nf water ir, to be found in the Mcro-
C 17 'A C k -.1 r - z IV~ v T- -i n ri H, T e n th,~ nntf~ r I a 1 , ne rt, I ntj I tr I v 9 ince
Ma ny -1 h~ J. L e Wr,r,-!- qn m