SCIENTIFIC ABSTRACT ZHELTOV, YU.P. - ZHELTUKHIN, D.V.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R002064710009-2
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: March 20, 2001
• Sequence Number: 9
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

m ---

Avnm
PA 3090
TIM: W bf_palolatinj ihO Dimensimm 6f t 116suro
i~ of i L4ir'bibil
'Whibb is Voiikia by his B ght abbut by roulic
Aii4e-- (Ob oancra p-riblizhenam metode rudho tremb *4-
Dbrazu7twhohikhoya,pri.,giar&vUaheskom msryve plastap Russian)
PMODIOAL-., SSSR Otdel.Tekhne-1957o~Vo t Mr 3',pp 00-482
1 V
Revievedt 711957
ABSTRM i:r-f4irthet'-d~v*lt~'novit.1-6f, the calculation, method proposed by-, the
i~ithdr-'Aw Ii V'"- iiiitlUfi 4NAuk. MR jOtde1.Takhn.1q55o4r.5'-:is,-
i 1 6d~ ~%,x z..
6escirib *i nlhie-first~ bbapter. the - general. conditions: and the do-,
termining,~of-- Wi boixndary displacesents, of a horixontal fissure am
dismased* It is taim, for granted Ahat I on the bour4aries. of the
'eflisure a~ normal stress, . 1. trib
mits wM&- is din , uted, evoor0ing -to...the
'.3AW--f the -mdamge6- space a ~sto6te- of, stress Is present, wfdch
-to dtie.,to,:-the Tock.pressure, qH =;y(H is the weigbA 4 the
'r9ok, HAn the stratification depth of the Uyer, The f "sure plane
M to the laze z m 0. The perpendicular boundary shifts
oorrespo Al
Of-the fivaure W(j at z a O.under the influence of the stresses
are
asiuxed no that w (r) - 0 in located everjwhere outside of the
fisure, a prb am of zdxed boundary conditions In converted
" a.ard 1/2 to one with bwogeneous boundary oonditions. The Istress r) in

i

.- 1 11"', -:'.:
I . ( ~`~ H ~,
III! i i I fl fl, -41 -Til llili ! ~ IT I'M

SOV/24-38-11-11/42
-AUTHORS: Dorozhkin, V. S., Zheltov, Yu. V. and Zheltov, Yu. P.
(Moscow)
-TITLE: On the Movement of a Mixture, of Liquid with Sand in the
Well and in the Crack During Hydraulic Fracture of an
. ,Oil Bearing Stratum (0 dvizhenii smesi zhidkosti s
skvazhtne i treshchine pri gidravlicheBkom
peskom v
.
razryve neftenosnogo plasta)
MRIODICAL: Izvestiya Akademii Nauk SSSR, Otdeleniye Tekhnicheskikh
-42 (USSR)
Nauk, 1958s Kril, pp,37
ABSTRACT: In,the.process of hydraulic breaking up of an oil bearing
stratum sand.penetrates into the cracks which form in the
rocks and the penetrated Band prevents the closing
together of these.rocks when the liquid pressure is
reduced, Until-the sand reaches the crack it has to
travel a considerable distance along the vertical tube.
Therefore, for selecting a rational technology.of the
proc6ss of breaking up a stratum it is important.to know
the hydro-mechanical picture of motion of a mixture of
.,~ .liquid with sand, both along thecrack and in the vertical
tube. Special experiments were carried out to verify
Cardl/2 whether available relations are applicable for such

SOV/21+7-58:- I- I 11L2
ind
-On the Movement of a-Mixture,of Liquid with Safid in,t e
in'the Crack During Hydraulic Fracture of an Oil Bearing Stratum
coarsely disperse suspensions as mixtures of liquid and
sand; the experimental set-up is shown diagrammatically
in the sketch,.Fig.l. . The basic liquid used in the,
experiments was glycerine and for obtaining various
viscosities the glycerine was diluted with water;
furthermore, sulphite-alcohol distillery refuse was used,
.~which is frequently applied in the oil industry as a
liquid forbreaking up strata. As sand, quartz sand
with the fractions 0.6-0.85 mm was used and in some of~
..the,experiments sand of other fractions was used,
~Curves calculated on the basis of the relations expressed
by Bqs.(2.1), (2.8) and (2.11) are plotted in the graphl
Fig.6; in the same graph the values determined in the,
here described experiments are also plotted
There are'6 figures and 1 Soviet reference.
ASSOCIATION: Institut nefti AN SSSR (Oil Research Institute.Ac.Sc,MM)
SUBMITTED: May 9t 1958
Card 2/2

KRYLOV, A.P.J. red.; AFANASIYEVAP A.V0. kand. tekhn.nauk.9 red.;
BrPTsOV, Yu.F., doktor tekhn. nauks red.; BRISY&UN, A.A.,
red. kand.: tekhn. nauk; BUCHIII, A. 11. kand ekon. nauk,
r a -A S 0)
e i; VIRNOVSKIYJ 0.t$
'doktor tekhn. nauk, profs) red
MV 17,
karA. tekhn. nauk red.; MAKSIYlOV VI.I.p
..Rdnde.geolo- red., URKOVSKIY, G.E., inzh.,
red.; MELII(-PASHAXEVjV.:##,rtd6ktor geol.-miner. nauk, red.;
NIKOlAYEVSKIYtILM., uviwr ekon. nauk, profs red.;
kand. geols-miner, nauk, red.,,
PIL-ATOVS.KIY, V.P.0 doktor fiz.-mat. nauk, red.; ROZErIllatu,
~M.D.y doktor tekhn. -nauko reda; SMONOVj S.V,j kando teklm,
naukp red-,
jPetroleum production; theory and practice. 196' yearbook]
Dobycha nefti,- teoriia i praktika. Ezhegodnik 1963. Moskva,
Nedra, 1964. 302 P. WIRA 17:9)
1. Chlen-korrespondent AN S&gR (for Krylov). 2. Vaesoyuznyy
neftegazovyy nauchno-iBaledovatellskiy institut (for Nelik-
Pashayev Rozenberg). 3. Institut mekhaiiki A14 SSSR (for
Nikolayevskiy).

:11,
Im.

i

I . I
~- - ill -t I I I IT I
i. . I
i I i I , I ~4 04, ". i I
t I I

- - ---- ---------
Simulatin tIIC process@** D234/D303
9.
ter a a
note: Gornoye davlordye 4 %ountain preasuir if; also posa-
-Ibicy, t:- the length of the cracki t.the indican. H and 1.1 refer to-
tdral conditiona and modol~conditionn re On tho basis
..na spectively.
_of thin equation the authors concludq that if! linear d~mcnsions of
:th of the natural dimensions (eo
the model,are.taken to be 1/100
the le gth of the crack) , and E,', Eli#' IM qHt the processes of
crack expansion in nature and on. the- model wi 11 be similar only if
.7 :7 the-.product of the fl(w-and the:viacosity-off the liquid in the
The exper
~model in; l/L 0,00 000 of. that in nature. imental realiza-
,at,
:7: tion of.this'is very difficult.;~'The opinion of the.authors.is t1
rom.
a' aimplir' t4ay . is to diminish the Young modulu ..of ~ the matei Lal f
ellt-l which th lead to a do-
ainode I of the stratum-Lo made, Thi a will
crease in.tho mine pressure.in,the model which in also.advantageoua.
or xperiment. On the basis of this reasoning the authors
the.c
f
describe an experilmontal installation, developed by them for invostL-
i5ating tho.pro.cesses of hydraulic,stratum.breaking. The principtL
part ot.the* inataiiation.is~a block made,of porous white-rubber
:.,which se'rvive'as tho'model,of'the elastic porous-mad 52'-)
ium (44
'--.Card.- 2/3:

'
t1 i/0.5a
24/6
1/000/069/94

a
mul ting the .
, proces GO'0
D234P303

I
2
m)' Sor~e.
,provislonal ata
d obtained,

n thi's inatal
d o not a V-ee c
rwith,
the 'corresponding.data,of ,.,.,,*~,~.,.,.,
'',
tha natural cortditions
~
L Abetr4cter S t
notevOompiete..trarislation'-7 ,
,

U. PI

4

diiid

i t .
i
'I'lif"1111 ~ 11"I"I ill 1111-~ilfllf;
; ~t 1~
t t W -

I'll:i-3.1; If 1.1111 EN'll 1i: 1,11111. 11, ll 111" 1 li 111

1 1 , % . -
: 3:.,~
.1i :iP I

~ hi. 7

=_WRQzmaTTO v:~m Ovii-juivi-imfurm Yuk* AVOSW
Motion of sixture of liquid &n&,m&nd In a well and In a crack
during hydraulic fracture of an oil-bearing stratum. rzy, Ax
41_QQ'D '14,A 4-." , -.-I. -. 11.107-h-3 V sea BUTW 101.1~

SOV/24-58-11-11/42
AUTHORS: Dorozhkin, V. B., Zheltov, Yu. V. and Zheltov, Yu.
.(Moscow) ............ ....... ....................
TITLE: On the Movement-of a Mixture of Liquid with Sand in the
Well and, in the, Crack During Hydraulic Fracture of an
Oil Bearing.Stratum (0 dvizhenii smesi zhidkosti s
peekom v.skvazhlne i treshchine pri gidravlicheskom
razryve neftenoenogo plasta),
PERIODI(,IAL:.Izvestiya Akademii Nauk SSSR Otdeleniye Tekhnicheskikh
Nauk, 1958, Nr 11, PP 37-42 (593R):
ABSTRACT: In the process of hydraul~.c breaking up of an oil bearing
stratum sand.penetrates in-uo.the cracks which'form.in the
rocks and the penetrated sand prevents the closing
together of these rocks when-the liquid pressure is
reduced. Until the sand reaches the crack it has to
travel a considerable distance along the vertical tube.
Therefore for selecting a rational technology of the
process of breaking.up a stratum it is important to know
the hydro-mechanical picture of motion of a mixture of
liquid with sand, both along the crack and in the vertical
tube. Special experiments were carried out to verify
Cardl/2 whether available relations are applicable for such

BOY/24-58-11 I/A2
On the Movement of a, Mixture of Liquid with Sand iii the _~C~Yfr and
in the Crack During.Hydraulic Fraeture-of an Oil Bearing Stratum
coarsely disperse,suspensions as mixtures of liquid and
sand; the experimental set-up is shown diagrammatically
in the sketch, Fig.l. The basic liquid used in the
experiments was glycerine and for obtaining varlous
viscosities the glycerine was diluted with water;
furthermore, sulphite-alcohol distillery refuse was used,
which is frequently applied in the oil industry as a
liquid.for breaking up strata. , As sand, quartz sand
with the fractions 0.6-0.85 mm was used and in some of
the experiments.sand of other fractions was used.
Curves calculated on the basis of the relations expressed
by Eqs.(2.1)-i (2.8) and (2.11) are plotted in the graph,
Fig.6;' in the aame graph the values determined ;Ln the
here described experiments are also plotted.
There are 6 figures and I Soviet reference.
Ac.Se.WM)
ASSOCIATION. Institut nefti AN SSSR (Oil Research Institute,
-SUBMITTED: May 99 1958
Card 2/2

S
/124/61/000/009/041/058

M MORS Zheltov, Yi~&P~ and Zhaltov, Yu. V.,
TITLE. Simulating the ~roceas of expansion of cracks duririg
hydraulic;br aking of a stratum
112, RIODICAL: Referativnyy.-zhur na I.- Mekhariika, no. 9 1961. 18
*
abstract 9 V154 (Neft., hh-vo, 1961, no. 1, 34 395

0 acks
A W~.' approach t' simutating expansion oZ.cr
duri the
n9 hydra U b ing of a stratum -is :described. Inw au-

u re ak
,P
thors: an
aly ween par=cters characterizing:t..-
ze the,qe ation bet
-6
devetopment one. and -on a model.and
of a crack in natural, cohditi
come to the xelation,
fill
(9p
H 7q
v;here 0 is
' the flovi 'of the'liquid; the viscosity of the liquid.,
,
:
-

E
the Young
pressure Abstrac 7"
he
14odulus of -t
rock, q. the mine

tard 1/3

-S/124/.61/000/009/041/058

~Simulating,the D234/D2;03
Process***

ter. G rnoy
snote: 6 e davlen ye: Itaountain prea sure" is also poes-
_Ib 7 the lengths f the cr 'kj,,.thc indices-H and 1-1 refer to
nat raliconditions and model.conditiono:respectively. On the b asi a

-of this equation the authors concltdq that ons of
no ar dimens!
model are taken to be 1/100.~th of.tho natural dim6sions (eOge
' 'the length of the crack) and k, F-11P qM qjj 0 the proceaces of
-expantsion in nature and onthe mo
crack do: wili be similar only if
the Product o:C the f low and the viscosity of the liquid in the
".7 ''model is 11110OOtOOO of that in nature.. The experiniental realiza-.i
.., ._,t:
1 ,
tion 01
I'this Is,very difficult. 'The opinion of the authors, is that'
' ,,
'
a simpler way ~ is , to diminish,the.-Young modulus of the material from' ..-
_This will lead to a'do-

whicl
the model of the stratum-is made.
crease -in-the mine pressure'in,the model which is also.advantageous
for the . experiment. .0n,.the bas is of this reasoning the authors
wdescribe~'an~experimental inatallation, developed by them.for invest-
d
igating .,the-- processed of hy raulic atratua breaking. The principal,
part, of -the inat a block
allationi made -.of porous white -rubber
which sdrves.:as the.model.. of the elastic:'p~=ous'medium 1 52:,,
2, 3_

the,pro'ceso M234/03-03

2 b ained'
cra Sonic. provisiona. data i~~o t
on this' installation)
do not agreavith,tho corrdsponding datalof the natural,- conditions i
s.note': COMP16te-,.tranulation'7

ar

;~Z

POTAPOV, N.P.; ZHELT G-P.
Temperature~coefficients of quality factor measurep. Im. tekh.
nool$521-55 A 164. (MIRA I?tll)

Authors
Periodical I Vest. AN
Abstract
submil~ted .......

ACC NR: AP6012080 SOURCE CODE: UR/0062/65 93 81''
AUTHOR: Sonyavina, L. Bo; Sheynker, Mi. N.; zheltoval V. N.; Dombrovski& A* va;
Shevchuk, 11. lei Kabachnik, M* I,) Ma8tryWMVa-j T. A01 W-1011"va, T. A.
ORO: Institute of the Chemistry of Natural Compounds AN SS811 (Institut khimii
prirodnykh soyedlneniY WN SSSR)
TITLE: Infrared spectra of arglaethyleiietriphenylphoi)phorance and their salts
SOURCE; AN SSSR. Izvestiya. Seriya khimicheskaya, no. 5P 1965, 895-898
TOPIC TAGS: IR spectrum, organic salt, organic phosphorous compound, electron donor
cyclic group
intensities of the carbonyl absorption in the infrared
ABSTRACT: The integral
~spcctra of itroylmothylenctriplianylphosphoranes (in which the carbonyl group in
~bonded to a phenyl ring) and their salts were mcaoured. The data were considered
from tho atandpoint of electron donor and electron accaptor properties of the
phosphorus atomand the aromatic rings or tho aroyl group,,nu well as the influence
of subntituent6 in the aromatic ring on the absorption intonsity. The addition of
~an aromatic group to the carbonyl in phosphoranes led to a decrease in the frequency,
and intennity-of the valence vibration or the carbonyl group in compariuon with the
corresponding aliphatic derivatives, evidently an a result of the functioning of
the aromatic ring as an electron acceptor, competine with the carbonyl group for
.,electrons from the qtrong.4~ctron-donor phoaPhorub atom. The frequency and in-
UDC: 543
QEd 1/2
L

I - - -

FRIDLYANDER,,I.N.; RCHANOVAO 0..A,j ARCILVOIA0 Z.N.; GUnJYxV4 1.1.1
DRONOVA, PETROVAp A.A.; BYCHXOVAt Z.S,; Prinimali
achastiyes F%IINII X.M.; LEBEDEVA, W.S.; REZNIKj P.O.;
AVMINA, H.;.ZHELTOVSK=,..,L.S.;.,,VOROBIYEV, Yu.A.;
TIURINI N.M.,
Manufacture and investigation of semifinished products from
high-strength and heat-renistant VAD23 aluminum alloys.

Country 1 T
Catogory I Emen and pzinal Mwelology, Circulation
Abs. Jour, f ]Ref Zhur 3101')k' 2, 3.959S No. 8W7
Zhelyazkov D. A rgt~'. ai, A. Mkoloy,,A.; XhznkoYa,,A; Chu-
Mums o*YjD; Ignatcna,11 Mikolova M., Midehey
, T.
) P
Titlo "
The ffect of the Bulgarian Synthetic Estrogenic Prep&-
ration "Utestrol" ori Blood Pe saws.
Orig Pub. Irv. Ota. bio.1, I med. muki. Bolg, AN. S6ro eksperlm.
b1ol. I med.~ 19570 Ito. lp 47--55
Abatract VitestrolIvas Injected in doses of 0.51 1.3 and

Into normal, atropinized, vagotomized and. do-
5 mglkg
cerebrate cats, as vell as intocats vith carotid
sinumes removed. Vitestrol lovered blood pressure by I
16--35$ (depending upon the dose) vithin 72--395 seeonds.~
There vere no substantial differences betveen tbe'normal
and the operated animals. It In suggested that vitestro
acts directly upon the smooth muscle elements of-the
vessel val-Is.--S.B.Stafanov.

dard:

'I .,
11;1'llit,lll'l~:,I.!",I,Iil,i,g,lfl,,~,~'~
;. I il !IV :
: i
I I

EASSR/Chemistry - Food
Card JA I Pub. 86, 15/46
Authors I Zheltukhin, D. V., Crdi. Tech. SA.
Title
Periodical t Priroda 43/9# 8546P Sep 1954
Abatract j The article explains the process of producing xyloino Prcan
vegetable mAteriol and then converting thin into tril.oxyglittaric
acid, which is used extensively by ba-kers ruid Ifound to be far
more economical than lemon juice.
Institution I Leningrad, Order Lenin Wood Technology Aced. inj S. M. Kirov
Submitted I ....0

o R.1 . g!
- ~ wi t! i ~!, U I A .111 %;.. *;
T'll-Alz I .

1 -1

!HV:r

137-58-4-7717
Translation from: Referatlynyy,zhurnal, Metallurgiya, 1958, Nr 4, p.194 (USSR)
AUTHORS: Ipat' yev, V. V. ,-Zheltukhin, D. V. Kleymtnova, Lf 1.
TITLE: The Kinetics of Copper Scaling by Atmospheric Oxygen and Sulfur.
Dioxideat Elevated Temperatures (0 kinctike okalin 'oobrazova'-
niya medi A kislorodom vozdukha i sernistym gazom pri vysdkikh
teinperaturakh)
PERIODICAL: Byul- nauchno-tekhn. inform. po rezulltatam nauchno- is sled..,
rabot. Leningri lesotekhn. akad. 1957, Nr,47, pp 22-26
ABSTRACT: Intermittent weighing is used to study oxidation (0) processes
occurring.in Cu in air and in SO? during a five-hour period at 700,
and 900*C. It is shown that the 0 process follows a parabolic
law and that the 0 rate of Cu in SO is lower than in air, and that
this difference increases with rise in temperature. In both cases,
the scale consists. chiefly of the CujO phase. Constants for the
rate. of scale formation in the media and at the temperatures and
holding times investigated have, been calculated.
0. M.
Card 1/1 Copper-Oxidation-Analysis