SCIENTIFIC ABSTRACT OVCHINNIKOV, G. V. - OVCHINNIKOV, I. YE.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001238610016-3
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: January 3, 2017
• Document Release Date: June 21, 2000
• Sequence Number: 16
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

GIGAURI, V.S.; OVCHINNIKOV, G.S.; MURDASOVA, I.V.
Clinical and experimental experience in the use of the RN-59
respiratory apparatus. Trudy I-go MMI 331226-231 '64.
(14IRA 18: 3)

G.S.
r-'. irical' use cf' - a: para '.Ls ror &rtl' '.' cia -' F,,- .:7c nar),
1, r
vei-.1.1-ation. Nov. mea. -.ei:.,.. -c,.?:-",-FC , I .
, I., .- ~,~ , " : '.

TIKMLNSKIY, I.N.; PAVLOV, P.D. I-R-0-Alm
Stratigranby of Artian and Kunpur deposite In their taperinr-iut
zone (northeaste-n Totarstan). Dokl. AN SM 140 no.1:207-210
5-0 161. (MIRA 14:9)
1. Geoloro-poiskovaya kontora tresta "TatneftegaTra7vedka"
Predstavleno akademikom D.V.Nalivkinym.
(Tatar A.S.S.R.--GeoloF7, Stratirraphic)

VARIDIA)MMV. I.A.; SULIKIN. I.G.; OVCRIIJIIIKDV, G.Ye.
Rotating block with a red. Rate. I izebr.prodl.v strol.ne.124:24-27
'55. (Hoisting machinery) MaA 9:7)

GONCHAREVSKIY, Ya.A.; ANTIPIN, V.G.; PKIUNNIKOV, G.Ye.; KOZHANOV, M.G.
Operation of high-capacity open-hearth furnaces vith single-
channel ports. Stall 22 no.8:705-709 Ag 162. (MIM 15:7)
1. Magnitogorskiy met&Uurgieheskiy kombinat.
(Open-hearth furnaces)

OVCHINNIKOV, G.Ye.
~
Some characteristics of steel smelting in open-hearth furnaces.
Notallurg se.5:11-13 My 156. kKLVA 9:9)
l.Nachallaik @many martenevokoge teekha No-3 Magnitegorskoro
metallurgichookege ke,ibinata.
(Famitogorsk--Open-hearth process)

'IV I
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, I I I . t-- : ii . . ', - - i 7 1 1~j , " . i v I . .
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A .., . .~ '! . p j - . ; , , a o r * ' I .I I .II I , ~ .
. : : 3- " " - , ~ 3, , - , ;~ , I . ". I r. ,

Omir4l"IKOV, I.
Let us carry out t~e seven-year plan of road construction in fivo
yeam Avt.dor. 25 no.3:4 Mr '62. (MIRA 15:3~
1. ZaveduyusYchiy rayonnym dorozhnyt otdPlom Talovskof-o rayona,
Voronez~sk:)y ablasti.
(Talovaya reCion--Road construction)

KOMMOV, V.V., karid.sellskokhoz. nauk; PETRENKO, A.T.; OVCHINNIKOV, I.A.
Components of grass mixtures for slopes. Zenledelie 25 nc.12:
26-30 D 163. (MA 17:4)
1. Inatitut sellskogo khozyaystva TSantrallno-chernozemnoy polosy
imeni V.V.Dokuchayeva.

KC 7 t. L . rid -y. 1.
r1a
~31 A-T~ y I) Al V
a r,,-- t: f.8 IR dy
nka.y
j :r-, ~r-, E a, e r. I'a t-
cstest e r,ly t ::, " u, a Lo lift
T3 ntra-11n,;- r n,- z ar,,- e- n z 1, 9

Polosy Am. V T K I na", a
2.
~qa (fcr hr.ar),i v). rr~;%. pura.t -1:
I r, s t Se 3 1 S k g -~ k 1,-) '1 -'A n
PC I -, V V . -,,, a7j 7 U V F f. a ~l
goz~.Sk,r" "'ki f'rit-, ne z s K r -rl o v

MECHEV, V.V.; OVCHINNIKOV, I.F.; NIKOLAYENKO, V.N.
Service life of converter linings during the smelting of
high-grade copper-nickel mttee. TSvet. not. )8 no.11:75-77
N 165. (MIRA 18:11)

1. OVCHIMKOV, 1. 1.
2. USSR 600
4* Poultz7 Houses and Equipment
7. Idghting chicken houses at night, Fltitseyodetvo, No. 9, 1952.
9. Monthly Ust of Russian Accessions, Library of Congress, April 1953, Uncl,

OVCHINNIKM. I.F.
4---. -
Piston vater s"pler and results of its use in studying the VA
cycle of the bottom layer of vater is "Inok Reservoir. Tmdy
probl, i tom. soy. no.7:140-143 '57. (KM 10-.4)
(kbinsk Reservoir-Water-Analysis) (Gass@)

OVCHMIKOV, I.I.
Dw7ice for the fixation and traction of the testis in its
forced descent into the scrotmo Urologiia no.5tO-U 162.
(KIRA 15:12)
(TESTICIS.-ARRORKITM AIND DEFOWITINS)

OVCHINNIKOV. I.I.
Useful poster on poultry faraing. Ptitseyodstvo 9 no.2:42
1 '59. (MIRA 12:3)
(Duck@)

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1-- , I
I- - - LL 4- Lj:-~
.. I
, , -N
I - I

1. OVCHINEKOV, 1. K.
2. USSR 600
h. Prospecting - GeoptWeical. Mothods
7, Disturtance of a field of constant current by conductors located in a non-
homogeneous seWspace, Izv. AN SSSF. Ser. geofis, No. 1, 1953.
9. Monthly List of Russian Accessions, Library of Congress, April 1953, Uncl.

nD - 1 -(o6
USSR/Geophysics - Electrical conductivity -'I f T :,~' 'I
Card 1/1 : Pub. 45-6/12
Author : Dvchinnikov, I. K., and Kilyukova, G. G.
Title : Effectiv: :77trical-conductivity of medium with inclusions
Periodical : Izv. AN SSSR, Ser. geofiz., 57-59, Jan-Feb 1955
Abstract : The authors describe an experimental verification of the theoretical
formulas for the electrical conductivity of a medium with inclusions
in the form of ellipsoids. The results of the experiments agree with
the theoretical computations. Three references; e.g. I. K. Ovchin-
nikov, "Theory of the effective electrical conductivity, magnetic
permeability, dielectric constant of a medium possessing foreign in-
clusions," Trudy Voesoyuzn. in-ta razyedochnoy geofiziki, Wo 3, 1950.
Institution : Sverdlovsk Mining Institute Im. V. V. Vakhrushev
Submitted : June 27, 1953

,rans'lation from: Referstlvnyy zhurnal, '.~eoioglya, 'A9t-, 'ir
p 161 (USSR)
AUTHOR: Ovchinnikov, :. K.
TITLE: Shielding Influence of the Outer Layer of Eartrls '~r,;st
in Electrical Explor ation for Ore Deposits (Ekraniru-
yushcheye vliyaniye poverkhnostno go sloya zemnoy Kory
pri ele'Ktrorazvedke rudnykh mesto rozhdeniy)
A BS 7RA C 7: P I t1logropq.1c on I, ry or, t I-,o ou thor ' !j 11 s3orta r, ",r
the deFree of Doctor of Physical and Matriematical
Sciences, Tresented to tne --,e--"iz . AN 333111
(-,eophysical Ing'.4 t,. te of tte AS U33R), M--sc::w-
Sverdlovsk,
ASSOCIATION -,eof I z. I n-t AN 33SR (Geophys Ica 1 1 ns t'. ta to .)!' t:,e
AS USSR
Card 1/1

NV V
AUTHOR: Ovehinnikov, I. K.
49-4-6/213
TITLE: Electric prospectin6 of pyrite deposits located undf-r i:.
absorbing surface layer. (Elektrorazvedka kol c
zalezhey pod pogloshchayushchim poverkhnostn.Tm 3loyem
PERIODICAL: Izvestiya Akadeiaii Nbukv Serlyti Geofizicheskaya,
1957, No.4, pp.471-478 (US3R)
ABSTRACT: Ajialysis of curves of vert,~W4,,goundinC and of otner
ob*ervations enables c6zk~.'Aj1:dnii'"on the presence of
surface layer of a certain thickness above the entire
paleozoic rocks of the Eastern slopes of the Urals, wiicn
contain pyr4p deposits. In recent years new seams of
paleozoic ore bearing rocks were detected which are
parallel to and east of the earlier known seam. The new
deposits are covered by mezo-cainozoic deposits of a
thickness of several tens of metres which represent a
considerable screen, makinE prospecting for ores under-
neath them difficult. In this paper the screeninE affect
of the surface layer of ore deposits is investiLated ~.-nd
an effective method is described for loc,-,tine deposits
hidden underneath the screenini layer and results of
C,
field measurements with the new method ere described.
C&rd 1/6The non-uniformity of the surface layer in Lhe verLic~~l

49-4-c-/2 3
Electric prospecting of pyrite deposits located under an
absorbinE surface layer.
of the Dotential of the secondary field to that of the
primary field, is influenced by anomalies which: depend
on the relative gradient in the epicentre of the
anomalies and can be measured. The relative E;radient
produced by a conductor in the field of a linear electr3d(~
will change aE a function of the depth and dimensions of
the conductor and the thickness and electric conductivity
of the surface layer. Data on the relative gradient
show that for each method of electric prospectinE thorf,
is a threshold value at which the anomalies cannot be
detected satisfactorily by the given method and this
enables evaluation of the prospecting potentialities of
the individual methods. The threshold value can be
determined for any type of field but it was (onsidered
more convenient to determine it in the field of a linear
electrode. On the basis of earlier obtained solutions
(Ref.2), the potential of the primary and of the secondary
fields are calculated for a linear electrode of the lent~th
2& - 20 with an ideally conductinG sphere and disc as
disturbin& bodies. The relative gradient in the epicentre
Card 3/6 of the anomaly proved to be twice as hi6h for the sphere

49-4-6/23
Electric prospectin6 of pyrite deposits located under an
absorbing surface layer.
beinG mearured alon6 ~he profile which was perpendiculax
to the electrodes and passing throu6rh the epicentre of
the disc. At one half of the profile the field was
normal, whilst at the other half it was anomalous. From
the measure:2t-nts in points symmetrical relative to the
centre of the profile the gradient of the secondary field
can be calculated and then the relative gradient
determined. The thus obtained data are given in Table 3,
p.474. The errors were of the order of 10%. The
threshold value for the method of isolines is assiLued at
28% (Ref.2). The extensive use and the relative
effectiveness of the method of isolines in prospecting
for pyrite deposits in the Urals is attributed to the
large threshold values; only intensive anomalies from
large and shallow conducting substances are detected and
under favourable geological conditions ore deposits can
be detected with a hi0i degree of probability. For
detecting localised conducting bodies located under n
screening layer, it is necessary to use methods which are
characterised by a low sensitivity to surface non-
Card 5/6 uniformities and a high sensitivity to conductinE bodies

SoV/ 169-59-2 -
Translation from- Referativnyy zhurn&1, Geofitika, 1959, Mr 2, P 32 (USSR)
AUTHOR: Orv&1nnikov, K.
T=. The Dlsturb~Ln~e ~)f a Magnetic Pleld of Low Frequ.~kr-v by an 11daally
ConductLng Ellipacid
PEPjODI-'AL: Tr. _a~ ~�rn 1957, Nr 30. pp 4
ABSIRACr Me solution of .he pr.:.bl-em on the d1st.,urtince cf an alternating magne*1z
fleld by ar idea'-ly ocndu--tixg ellIpsold IP not suttabl~q for ca-I.-ulalicn.5.
thIs solution is Cited in 11.he The author puts a more simple
problem of. f!-ndirg tht d1sturbarc,9 at a lc-w frequoncy --f the fit-,J. To-
theory of 'I,,@ fleld of dly-ect curr~-r'- I!! applied Icir Its ;c1tjtio!-
The 5olu!lon Is glvsn in thn form of a table of th-!~ ocimponent.~, of Int-knsity
of the ee-crIdi3zy Tagnetic fleld for the casA cf a oondu~tl-njz
ellipsoid, - a vary t-tin diek- The solutions obtained area ut.:1,1ztd for t-ha-7
amparipcon of the. &nomalles Nom th.,~ Insulator &nd the -~ondlj~tor whtin 'Prv
a.re exilted Herea. the ipdu,~ttve 6xcitation of the leader
bel~-omes 'Ike to tne g&1venic excitation 6( the Ln-culato: The 7onclusl,)n is
Card 1/2 obtalned QLat the, ancca:y for c~f lickometric form I-z grrat.e, for

I A
AU-IhOR: Ovchin :i,~ V, 1. K.
TITLE: A '2~.,-~r
.7 f J i., - i e E- Lr
,)dn)e" .'-troinocc, rzar2)ttazaa.
NauA
ABSTRAM: T.,,
w.
la.rd 112

A Theory , f3 11 e e
latter for a run6o- f .-a 1 L. c, f r, 112, iI
1 table and 6 ref-re.. - i, -,f wl~ic- 1, ~.re R,;., s -au
English.
ASSOCIATIiIi: Sverdlov Uiiiii.
SU13MITTED: March ;'3,
AVAILABLE: Libra.-~- -~f
jard 212

Di D, f e ri led zi ';,o 3 1 e i f ic
L. t, I I I! Phys I C-,:~ o f P,~~ r t.'i , Acad,- o f 3c i-
(D at v .9
ovete 1.'.
r I A2,
D T 'jU,
Izv(- A.,.Pademll Na,,,
1-1.1 T T -I t-~ If f,~-d f :)r
D-,( 1 i n:, i r i I ri f I --i, - it
.16 -U7,j r
viLy-iniye pov,.
kory pri r -,iedicc- rudiVich
J: -Y -n~ - Dr, R~,, 1.1', Y P. B u 1, 1 tie v i i.
T. i I A.- Pin Di Ma il B , 149. y a n C V
-7" - v The n i ',ased
--tri:: met. f pyr t - dppc3di,~ aij..
U osi,,s ar- lo-1-.-1--~
r- 1-,-T-1 r; . which inflapri(.e:
-Iacl P:ir' ~ -UI,3rlj 1 t5 :- ~rl,
~Le furila-enta.

4
ssertit- )Ls Defer. ~.;F- 6- 1 t- ,I-, If ~(~ cr)u-r,- - , of
f PrIj E; C S :) f t* t (, L A-ad(t7,y ~,f Sclenres U33R.
4nfluerices -f -!71, nonuniformities is investigated na-nely.
the screenine., infllence of the surface lajer of t~.e Earth's
H~ a nevi f tt-, iroblem * - -v I vir,;-
molyi,,,Is h-ivc- a low sensi~lvlty tc the surfa,-.e =-
anifor-aitie- ind a hict sensitivity t( c,)nducTing bodie,,
lo,-ated nt IeT),:hs These ;.-,(t~iods are matorialised by
usii.g spec"ril' current feediiit,cirraiLst-G the semispace w~.ich
r,,~zlnp, the concentratl~)n of the current in the
a.,,' reducinE 1' at- the surface where the field
~bs-rv,.,L- :arried ci-,it The reduction in tli!~ :,nc~n-
Ih- -,iT-renr is aci-~ieved by -=.,,ensatinr, the f~;-id
:f cf electrodes with the field of other
,-rDundinw eliz-,rodes (compensation method). Field investi-
.;atID-Is h-ilfe shown that by m.,ans of this -.ieth-)d ore bodi.,s
I "is(
w1iich cannot be detected by the Ii t I )n
-,thDd
i r, ~, vs K aj a "T(-,-hnJque of Analysis of the Dyna~qic
!-,T --)pr-.-* los if 3.).a- SeI3.,iiic Waves" (Met,)dika allaliza dilla-
--v,ystv nekotorykh seysinichesirikh voln).
-s S -3
landidat--- D..,-s. r1ation 0j.),_,,unerI Dr. P,~,y -1.1,i L , . c . Yu. V.
d 5 R 1 7 r, 12 3~- . K, 1, Ugurtsov, January 10,

11 -4- 5'-3-d4 - 17/ 1
D Is sert a I- i-,ns Def, :.,(-I a, t~.e Sc' F-r.-,if Cc i--f
~;f rllysllc~- of ll,,~-- A,:ademY ~f 3--'Ler,~es US-SR
-,bser-vations,
t ,v, d arp bided ).-, 1.11P '"',eorrtical
I .- * ly-naml- c',luir -A c -, r I o t I C 6 -) f i3c 1 1 l at
of ttif- or o~ tl-,e source (for i,,-
f- nir.at i):-, of the 2r,,,rFy th(, char;,ct-rlst~~c )f
'
I IP
~.:-:i!3 ~Of tda:-]pinj, )f iomlc wav,,,-,,
-r -,vt, -d %Le asymptot ic rej,r,?se,.-Lt-
i : s t i ~7~1
)n of of t Le refloctEd, refraot-d a..d ~f
ne Incir. f~,r a :Lultilayer medium obtained by G. 1.
-a ~- n~-. r, at a distance from 1~he
i -) n * j f
3,'s thr- -Jritial ex t p i
Tl,~ sr rclal, iJL.z: have been transf )r--,ie~ i.
e --'-v 5 -.' z a I i n t e r p r e t an
f t fo I nw, fu,-~torL, i- lnve3ti-,Lito---,
radiatim, -- --I,L
r r. the ~eo
C- n t f r ~rw )n rr f I t i j!.
a n, i
T f I v i:i
r- rar f.L th, -;I~apu, of eib:3tl-- D.-;C111
A' I r, ~tie of the dic,. lacc-nents
F f a-,i f Aandarrl lt

4 )-C)1-1-14-11711;~~
Disserti-,:
1-..Ysic:- rf -e
shown th-,,~ in t i- c full I n te r nL I re'lecti-)-i th-

r, ter' F` i + 7
I . -,
-7 1 t )n and r f r -3 c *, ~on A
1~,ti In,- theoret ical s~,i -r 'if*
of re f t -d ~ij; 0 M~l i r4 Wa v r, S ,A~,:iuiii, I on.'.
perrai t I 1:1-ating certain clyr-i'amic
f e at ur(-- s f wav,~s without p1c.,Uting theoretical
ueis--ioi~ru=. 'Cu t aralysiT;g standard curves. Tiie
dzyna.mi- arc, investiv-ated of lonCi~-udinal wave's wt~ch
re cril.'~-al i,nfles. The cal--ulat4 :):-,s
r e
f-: a wa,`,2 L-f t~i~i, ratioE cf the sDeed ant the
b-,un(:ar-
y. It was estab
lishe,~ tt,,;it an.~rle-- at~-ve the critical, the
inten-~it,~ ~7-. ~~:,?s ard additional phabe silifts occur which
3re r. I it, th~-- 1iff,-rence in the time of passage.
F,-)r larl,-~- i the shape of the disc Incements chan-
3. rrof i1- Thai a dis~-urba-nce of the

V~,? *he:iretical esults are in
r
;,Ath aata of A, M,
--n fiel,!
seismic prospectin7 work in
L

as Ir
investi'lated of the free sur-
Card 4/5

4 )-58-4-17/18
Dissert at I o~:-- D, f ( n-'ed a' -~e 3-- ii,-. fi~- Jo,.~nc, il o f the
Phj-3ics Df thin Ea.-h of U,;.3 R
fa,,(- Dn SI wave,:-: (I . e. t~e infl-ionce, on
t hn i r -- 1, -1. and 'h, rati of the dls,~lacement
!LnEles It was found
that th"s I -iy-i f 1 i~~n the observed fluctua-
t n. S , I., ~- ~ 'I
cf nearby earthquakes. A
t -c ~-n 1 -'if i -n !;y m-an.~: Gf Ln Plectrinic computer
via3 evolv, f hc irterforen o of '-dimonsional waves whizh
are reppat.- .1 ~i-n! in the lajered medium.
In t e r f r,-, T-. - ~, 1 1, lat !,)n,,: lhavc- been calculated which occur
i,-.,-n. e -~f a .Ian(, 1 - ngitudinal wave on to trie
*,wc sarfa-- layers About 450 thc-)re-1Jca:
.3 e i s:-- i- am e -u r,% t 1-,i I a t- res,)Iv~nF- p:)wt--r .-,f t.1.
--s9lbilities 'ndlcat-d u'
,
f
.~.e surface layers by
o
1. Sclentifi:7 rep;i-t,.q---'JSSR GaophYsi'~3--ISSR
Car,J L)/~

OTCHMINT, I.X. [(>rchywvkov. 1.K.); ZINCHWMD, N.S. [Zinchanko, M.S.]
Vibrating scand method for investigating ailsymtrioal electron
be&= . Ukr. fis. shur. 4 no.21219-228 Nr-Ap 159.
(KIM 13:1)
1.1ustitut radlofisiki i elektroniki AN USSR i lhar'kovskiy gosudar-
stvswsyy univerettet In. Gor'kago.
(Blectron beams)

81115
S/142/60/000/01/007/022
3 / 4- 0 E140/E463
AUTHORS: Zinchenko, N.S. and Ovchinnikov, I.K.

TITLE: Experimental Study of the Passage of an Electron Beam
Through a Magnetic Undulator
PERIODICAL: Izvestlya vysshikh uchebnykh zavedenly, Radiotekhnika,
196o, Nr 1. pp 69-76 (USSR)
ABSTRACT: This study was undertaken for three reasons. Firstly,
the nonrelativistic, electron beam in passage through the
magnetic undulator may be a model for a relativistic
beam. Secondly, radiation of very short waves may be
obtained. Thirdly, periodic magnetic fields permit
increasing the stability of electron motion with beam
fo:using. The principal difficulty in obtaining
appreciable radiation powers ip such systems is the
difficulty of passing the beam through the magnetic
undulator. In previous experiments, the beam transmission
factor was less than 10%. Since the power is proportional
to the square of the current, the radiated power was only
1% of the maximum possible. The work described in this
article was carried out in 1956 and 1957 in the Institute
Card 1/3 of Radio Engineering and Electronics of the Ukrainian

81115
S/142/6o/ooo/ol/007/022
E-140/E463
Experimental Study of the Passage of an Electron Beam Through a
Magnetic Undulator
Academy of Sciences. The electron optical system is
fairly evident from the figures. The system consisted
of an electron gun, accelerating diaphragm, magnetic
focus coil, magnetic undulator and collector. The
cathode gave a current density of 180 A/cm2 in pulse
conditions. Armco iron was used for the undulator.
The collector was water-cooled. The field distribution
of the undulator was first found approximately by an
electrolytic tank. The actual distribution was measured
in the final undulator using a laboratory magnetometer
with a needle I mm long and 0.4 an thick. The field
distribution is shown in Fig 5. The projection of the
beam on the plane of symmetry has almost a sinusoidal
character. Further, an analysis of the beam stability
is given employing the theory of Mathieu equations.
Experiments were carried out using a tube with glass
envelope. The total beam length was 200 to 230 mm.
Three undulators of length 12 mm, 7.6 mm and b.8 mm were
Card 2/3 used. Beam currents up to 30 mA were used with almost 1<

8 i 11.5
S/ 142/60/ooo/ol/007/022
E14o/E463
Experiment&l Study of the Passage of an Electron Beam Through a
Magnetic Undulator
100% transmission. This was maintained for relativ-,I~,,
long periods (tip to three hours) without requiring
voltage entry angle or other adjustment. The onl)-
critical factor was the exact location of the tube with
respect to the plane of symmetry of the undulator
magnetic field. There are 7 figures and 10 references.
5 of which are Soviet, 3 English and 2 French.
SUBMITTED. June 20, 1959
Card 3/3

OVCHINNIKOV, I.K., prof.; Eh1XIH, V.A., insh.; TSAPLIM. A.A., insh
- Cd-wi~wedij
Investigating the vatting by mercury of platinum and it@ &11079-
Isv.vys.uch*b.s&v.; gor.shur. no.1:144-148 160.
(MINA 13 t6)
1. Sverdlovskiy gorzWy inmtitut iment T.T.Taichrusheva.
Rokomendovana kafedroy flalki.
(Platinum) (Surface chemistry)

L 34414-66
ACC Hko AT6022229 BOUNCE CODE: UHr0_b_0_0TW6_d_6_/_0_6_dj6b_ "76-01
AUTRONs Kukush, V. D.; Oychlamikov, If K 4-ozear, !A. PA', Zhllkov,
V. 9.1 Pas*ehnIk, Ve fjj"1090A.-O-We IL910211LOW0 To Me
0301 none
.1"Velt Device for measuring deviation@ In the power level
_4MA
SOUIRCSt voesoyusnaya asuchsaya 80981749 josTyasbehelfisys Dayu radlo
226" x96 radialimer6blYs DOILIAdY. Moscow, 1966, T-ly-
TOPIC TAGBt power mete4 electric measuring measurement, generator
ABSTRACTs A device for measuring the outpni power of uhf generators-is
describeA. The device operates on the principle of a balanced static
calorimeter used for precise power measurements In the centimeter ant
aIllIuet*r rangea. The system Incorporates a balanced static calorie-
*ter and a measuring block. ?be balanced calorimeter consists of two-
Id9otleal coaxial load*# I.e.9 an bt load sod a compensate& load. D-e.1
beaters are incorporated directly In the load** The measuring block-~f-~'
consists of three basic sectionst a &-a amplitiorg a measuring cire4io
&ad stabilized power supply sources, fte folloviag data were obtained
In experineste with the device which ebaracterise Its erricleacyt
voltage standing wave ratIo of the terminal section to practically

GVCHINNIKOV, I.K.
[Lectures for a ~-(jurse In "Field; "..r peoptynl-
------tor.9] Lektsii j,o kursu "Tocrlia polia" dlia geofizii,. )v-
razve,'chikov. Sverdlovsk, Sverdlovskil gormyi in-t Lm. V.%'.
Vakhrushava. Pt.2. 100 . 133 p. (mIhA 1-~19)

BURROYS VbA.; -WLHIMIxQVj-I.x,-
Structural characteristics of sonal currents and meridional
circulation of vatera in the central part of the Pacific Ocean during
the winter of the Northern Hemisphere. Trudy Inst.okean. 40:93-
1017 160. (KIRA 14:8)
(Pacific Ocean--Ocean currents)

BURKOV, V.A.; ARSENIYEV, V.S.; OVCHINNIKOV, I.M.
The concept of northern and southern tropical fronte in the ocean.
2rdbIwt.okean. 40:108-120 160. (MIRA 14:8)
(Pacific Ocean.-Oceanography)

BURKOV, V.A.j OYCHIMMOVs. LH-
Investigation of equatorial currents north of IfOw 0111 a- 7rudy
Inst.oksan. 40sl2l-134 160. (KIRA 14:8)
(Pacific Ocoanp--Ocean currents)

i(OZLYANINOV, M.V.; OVCHINNIKOV, I.M.
Relationship between the transparency of water and currents In the
northeastern part of the Pacific OCean. Trudy Inst.okean. 45:102-
112 161. (KRA 1~:2)
(Pacific Ocean--Ocean currents) (Sea water--Uptical properti-s)

OVCHINNIKOV, I.M.; PLAKH111, ie.A.
Distribution of the Atlantic and Levantine waters in the
Mediterranean Sea. Okeanologii-i 3 no.4:642-652 163.
(MIRA 16:11)
1. Institut okeanologii AN SSSR.

NRs AP5009498 6/0030/65/000/003/Ca2g/0150
AUTHORSt Vlaggrafty, A. P. (Academician)i (~Sr~a~-v 1. P. (Academician)l
Ten-.hin, A. L. (AcadomIcLin)i �.hcharbokov A_D-. I.
-~Arn'i"Mtcian); Sndovnkly, M. A. (6,,rroaponding memb., AN SSSR Akhwd1snrjG;.-
(AcadnrdolAn AN XA~7,-,R L. P. (Candidate of p1qatco-am them tioal
- )I Za~taqv'
ncl"nonn)l
TITLEt Development of earth nciencei In Central Asia and In Kasaidistan (Results
of a field trip or the Dopartownt. of Earth Scienoes)
SOURCE- Ali S-1,SR. Vostnik, no. 3, 1965, 128-150
70PTC TAGSi rq~nctlvity, goochom! Fj try. ~~geochronolog teal problem, geochronology,
,:-iodnay, goofTrnj*q, geological survey, GI~OIOBY, geomacnetials, goophysical Won-
pocting, goophyelcal research, goorhyalas
AW;TRV7: 7tio Prosidlum of the Acadeu7 of Sciancest SSSR hoard the report of
scade-Icinn A. P. Vinogrodov, secretary of the Department of FArth Science*, at
thO B-salon hold on January 13. The speaker presented the results of the deFarV-
ment'i trip (Oct. 1-1.1, 1964), organised br the Acadval" of Sclonose of-
Kavi~ikstan, Kirghlviya, Tedabikistan, Torkamistan, and labskistan, am aw
ce'd 1/5

L 4034n-Ac
ACCESSION NR i AP5009498
Stnti Geological CornIttoo Entnbliahlria direct relations with the sjNve t
ncAdonion van thn immodlate roal or the trip. The symposium on 0~10molooA -(hold
!n Tanhkort,) was roportod on by M. A. Sadovakly. Tho problew In Lh!r. -old were
!ntn Uirea ~,rvupmi 1) Intarnml it-ructure of tho earth'@ cru-i Ad
:;-bism9% i-y rigntlo rovoalo,l by daLa obLnInod by d1frerant brrinchns of tho geo-
v -Invc,); ) relntinn among difrortmt earthquaktj sourensi 3) protection of thn
rind natAnnn; -onor~r rrom mnrthqunke dnmire. It ~m recomended that
a apoc!.%, nerv!ce) doalln:7 wt.h 1.1in norLh,junk- for-cnotm be nre.,nnized. Anhieve-
mmts of !h" aympo3ium on rydrolojD ~-rq reported by U. ?1. Akh-iodanrln. D. 1.
K-id-11n 04)tcow Univorolty) pres,,ntod a pn,-,o,- on f-he Irminare and renewal or
ri %m.l wr.Lqr. U. M. Akli,jednefin spoke on the stu4y of artesian basins In
RaxskhuLan. N. A. Kermanrin (U-sbqk in3titute or Ity-Iroloa and Enfilaeoring Goology)
d1sensood the prlnclpnl problaro of theoretical hydrology. Zh, 3, Sadykov
(Acado3q of Sciences, Kazakh S5R) spoke on the seepage effect of underground
brines and its meamine In the interpretation of oro-formistion processes. 01 As.
Ysvlyanov presented an engineer ing-geological mp of the arid Uzbekistan. V1, Gj
'Gefurov discussad Irrigation principles and the forecast of b7drogeodynande
proceo-~.-m ts' ing place in the irrigatad areas. A,_ Lj,-X- spoke an utilisation
o1 aruml~a waters. 5. k. Toytoviev. recomem6ed tM orgamisation of a speelan"d
servic* for the isetwe. 7be pogm*lml proUsam In
Card 2/5

ACQ~'ZTON MRi 05"49S
Central knia were discu3ned at three interrelated geographic oymposla hold in
Tnahknnt, AahkhRhid, and at Unin-Ata. rho first dealt with the geographical
aspoc-t, or irrigation in Central Aninj the second with the problems of desert
coon'tiont and the bulldinr or Uio Kara Kum canali the third with the regulation
or gIncier Paltin(- in tho mountains or Control Asia. Of special interest wns the
!1sciission or tho rittur-P rnt.n or the Aral 5on. Two opposite opinions were pro-
riont,Idt V. L. Shit Its -,,tntod that increased itne of river waters for Irrigation
,Bill cnune a co~.plato drylrZ up of the son. L. V. Dunin-Barkovskiy drew attention
~,, the r"cant r*.ia or the wntor leve"i in the sea, explal" It by the peculiar-
'Aion of witor -.--kn::pirnion b7 difforunt ty"a of vogetatione Fa Fe DQTjW
".owevor, nxplainA tho pnrndox by the water supply at the river sources at the
arvi 'yun'-Shan' divide. The results or the three aessions were
by Academician 1. P. Garealmr. Academician A. L. Tonahln reported
on the mn1n session of the Earth Sciences Department in Alma-Ata. R. A. 130rukayvv,
A. X. Knyupov, G. F. Lynpichavp and L. _A. MircahnIchankc, reported on the strwtural
.nd Apping of eastern Kazakhstan. G. B. Zblllmkiy discupood
problerm In theoretical mad experimental aineralogy.
- A. K. Kayupov spoke on the
relation of endog*ne mtaUogezW to the deep structure of the crust. 1. P.
_99yokh-Ankly reported on iron and wiWanese deposits Ln Samakhatan. Zk. a.
andykov rAd* a qwmtltetlvv emolutlon of artoolan voters in the artesian bm&Jjwv
cmd )/5

ACCESSION kRi AP5009498
oolinn ann1s, and deltaic deposits of this region. M. I. Varentoov described
oil pro,3pects in southeas'.orn Kazakhaton. This topic was discussed In rreator
detail In tho prpor by P. Ya. Avrov, M. 1. Varentacy, V. 1. DIL=r anti A. B. Li.
Goophynicn] research In Kaznkhst-nn wan dooerlhod by A. T. Androyev, M. J. Morozov,
V. V. Pridava, and V. 1. Gol'd3hmit. The session an the probloms of ore genesis
van hall !n Frunze, and It3 rmilLg were reported by Academician D. I. Shcherbakov.
F. N. .-h,61i-av and A. 1. ' i,7-iHn,,v disriu,sol the application of now precise methods
In 900'r`7- V. T. -url,n. r-i;x,rted on his study of regional ronchomiatry In the
nccumulnt4nn and localixntion of' Lv-rcury orp. M. N. klltgnuzon criticized the
pqper of F. 1. Vol'fson on thn theory of formition and distribution of endogeno
are deposits. V. 1. Knauf and Ye. 1. ZubLsov presented a structural map of
northern Kirghiziya. A. 2. Ronov spoke on the origin of ores In sedimentary and
extrusive rocks of Tyan'-;han'. A, U. Abdu-118yev formulated principal conditions
for bauxite formntion. G. 1. PoyydQv discussed the polymetallic region of Holds-
tau. A Dzhumallylv spoke on the structure of ores in Dzhorgalan. Academician
__, Puyve reported the results of the Dushanbe session at which Academician
A_. V
D. q. Korzhinskiy discumated p-it-mgmatio processes. IM, V, Ris I;kqnko spoke
uu seismic act.4vity s~d tho onergy of earthquakes. jAJ6_ffiVaWv amd B, A.
-Zakbar--r *-. .1nea6ed the possible conneatlom betwese geoebealeal processes and
zoauamg Zekbarvv spoke " @@Lamle PBXs. V._JLAaMW dUembimW preMeem
CWd 4/5 1

L 4qjisn-65
AGGFZSION NRo AP5009498
irolnted to the study of vaismic proceasos. The session in Ashkhnbnd was reported
'by L.-P. L,31tjov, candidnte of phyalco-mOonntical sciences. It star -i vith
tho p~rqr or H. A. Sndo-.-kiy who doacribed the problem of earthquake acenting.
r. r. ~'nlir-ykov and A. A.-Dzr~bayov promantod now Infnrmation on the deep structure
;(.r Wr-.tnrn TurkrLonintnn. L. 11. Sntrnov doncrihni the general structural history
ltd th~ Alrlan-41irdilnyan nobila Vw.,It nnd the adjacent trnnsition zofw. 1. M.
,(-vchirn11-iv roportod to .he rrosIdDua the rosults of W4 Tashkent session 6)
wtilch V. V. Dolonsov preae,at-d tho paror "Earth crust and the upp9r-Mahtlo"of
lcontin,riLa.* A,- dincuncod thn origin of natural sulfur. A.-A.
),alnkhov drjncritw~d the PjtnllnFanic pocallarition and typos or the Uzbek ore@.
-7H.-D. Vol'fnon, V. G. Gourlkovets, and A_P~Jhyaloyokiy analyzed the application,
of roo"11CMIcal and goophloical methods to explore tion.NYThe Presidium of the
an W
,Acaun,, or sc, ces 51 approy" the work ttW Depaits"'as o1 "r1h gel""
praeontod its resolutions, and expressed Its graUtaft to Asaftnl*Us A. IN
Vinogradov, the mrstary of the D*WtMI�Ikt, WId t0 00 11111111M at VIS W901hift-
tion comitteee
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ACC NRt A117004094 (N) SOURCE CODE: UR/0169/66/000/012/VO07/VO07
AUTHOR:' Ovehinnikov, 1. M.
TITLE: Comparative evaluation of several methods of studying sea currents
(using the Mediterranean as an example)
SOURCE: Ref. zh. Geofizika. Abs. 12V45
REF SOURCE: Sb. 2-y Mezhdunar. okeanogr. kongress, 1966. Tezisy dokl.
M. , Nauka, 1966. 294-295
TOPIC TAGS: ocean dynamics, ocean current, hydrographic survey / M-editerranead
Sea
ABSTRACT: A study was made of data obtained instrumentally in the faLl of
1963 at 22 buoy stations located in the eastern part of the Mediterranean Sea.
Weak mass transport in the abyssal layers made it possible to identify a slow-
moving layer (1000 m). from which sufficiently reliable data were obtained at
32 drift stations on the current in the baroclinal layer, by using the Markarov-
Nansen dissimilarity method. Two methods used to make the determinations
showed satisfactory accord. Other methods used showed that when the proper
Cwd V-?- UDC: 551, J6, 085

ACt N% AR7004094
zero or cutoff surface near the lower boundary of the thermocline is selected, the
dynamic method will satisfactoril reflect actual water circulation and give a
y
correct representation of the vertical structure of ihe current (129 hydrologicalI
stations). The "nucleus" method provides only a very general picture of
horizontal water transport and greatly distorts the picture of the vertical
structure of the current. Isolines showing the location of water mass "nuclei"
are a better index of circulation. The isopicnal method and current charts,
based on ship drift, yield and equally rough approximation. The conclusion is
reached that in the Mediterranean, the almost stable circulation is well
reflected in the calculations of geostrophic currents. )Translation of abstract)
[DW
SUB CODE: 08/
~Cor#_ 2/2

GURLTICH9'M.G.; KRAVTSOV, S.S.; OVCHINNIKQV,-I-M.; SURKOV, V.N.
Re4ent data on the concentration of some trace elements in natural
buses and waters of the Northern Caucasus. Tr-ady MM no.4,6:92--97
,60. (MIU 1413.)
(Caucasuag Northern-Htneral waters)
(Caucasus, Northern%-Zas, Natural) (Trace elements)

AUTHORS: Gurevich, M. G., ovchinnikov, 1. M. 20-119-5--49/59
TITLE: A Short Description of Natural Waters In the Region of the
Tyrnyauzakoye Ore Deposit (Kratkaya kharakteriatika prircdnykh
vod rayona Tyrnyauzskogo rudnogo mestorozhdoniya)
PERIODICAL: Doklady Akademii Nauk SSSR, 1958, Vol- 118, Nr 5,
pp. 1021-1024 (USSR)
ABSTRACT: This ore deposit is located on the upper Baksan river in the
depression area of the Tyrnyauz-Tau chain In the region of the
Ellbrus mountain at an altitude of from 2ooo to 3058 m. The ore
deposit, being of a scarn - type is linked with a regional teco
tonic zone, which is represented by a narrow strip of metamor-
phosed and strongly d13located Palasoz:)ic and Lower Jurassic
rocks, which are wedged in betweeL old crystalline slates in the
shape of tectonic fragements. In the near vicinity of the El'bru3
aerated water springs are very frequent. The springs in the via
cinity of the mentioned ore deposit are interesting in various
a3pects. The rock around the ore deposit hardly contains ground
water down to great depths because they are drained by the Baksan
Card 113 river and several brooks to a deep level. Fissure water was only

k Short Description of Natural Waters in the Region 20-118-5-49/59
of the TyrrWauzskoye Ore Deposit
found to a considerable extent at the horizon 2312 m (from the
zone of the central disruption). Later on from 5 to 6 wells of
such water in the granite'and the greatest water supply in drill
holes in scarns of ore and marble were found. Gas escape has ne-
ver before been observed here. The here discovered springs apper,
tain to the bicarbonate-aodium or potassium type with a minerali-
zation below I g/liter. Table 1 gives analyses of several fresh
water nprings, of wator frnm the mines and or the ininfiral water@
of the said district. The mineral water from the structural tirill
tiole no. 1.014 (at a dopth of 12no m) in espe(-tally intorestIng from
the cheral,-al point of view. Within the range of from zero to 764,3
m neither water nor gas were met with. Between 764,1 and 834 m
ga3 and mineral water appeared. Clay solution was edected to a
height of 0,5 m. The gas separated from the solution in form of
numerous small bubbles, which burnt on the surface. Gas separation
and the ejection of the solution were irregular and occurred by
jerks, as if pulsating. UP to 83,80/o of Hydrogen were found in
a gas sample. After 1.8 days this content dropped to 10/o. The
initially low content of CO2(6,80/o) later on increased to 95,550/o
Card 213 and above. A sample of absolutely clear water was analyzed and

A Short Description of Natural Waters in the Region 20-118-5-49/59
of the Tyrnyauzekoye ore Deposit
the results were compiled In table 2. The content of tne
following specific components In increased in the drill
hole no. 104: C021 H2S1 Li, Fe, J, F, HW2 and H2Sio 3*
The mineralization is relatively high - 13,1 g/liter. The
water is carbonic, containing chloride, hydrocarbonate and
sodium, and contains an excessively high amount of lithi-am
(28o,8 mg/1-iter) which constitutes rare case.
There are 2 tables, and 1 reference, 1 of which is Soviet.
ASSOCIATION: Institut geologii rudnykh mestorozlidenty, petrogr&fii,
mineralogii I geokhimii kkademii nauk SSSR (Institute for
the Geology of Ore Deposits, Petrography, Mineralogy and
Geochemistry AS USSR)
PRESENTED: June 2o, 1957, by D. 1. Shcherbakov, Academician.
SUBMITTED: June 15, 1957.
Card 313

S/054/60/000/004/014/015
B004/BO56
AUTHORS: Grechishkin, V. S.,( Ovehinnikov, I. K.
TITLE: Device for Studying Nuclear Quadrupole Resonance in Nitrogen
Compounds
PERIODICAL: Vestnik Leningradskogo univeraiteta. Seriya fiziki i khimii,
196o, No. 4, pp. 126-129
TEXT: A simple device for studying the nuclear quadrupole resonance lines
of N14 is described. The circuit of the Franklin generator is shown in
Fig. 2. The sample is introduced into the well-screened coil L, (volume,
3
2.3 am ; inductivity, 20 microhenries). The total capacitance of the cir-
cuit at 3.3 No/sec is 140 micromicrofarads. The capacitor C 2 serves for
the rough adjustment of the generator frequency between 2 - 4 Me/sec. The
rotor of C3 is driven by a Warren motor (frequency change, 1-5 kc/sec-min).
Resonance is studied by means of Zeeman modulation (40 cps). Other parts
of the device are a ~P-10 (ZG-10) audio-frequency generator, a low-
frequency amplifier (I : 1000) with 6)Kln (6ZhIP) tubes, a phase detector,
Card 1/3

11) :Z.
70
$/054/60/000/004/014/015

_1P B004/BO56

11 00ROM Wpmv
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5000 or Cl 400AW R1 306M 6M OR .

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Card 3/3

L
GURVICH, M.G.; OV INKIIEOV
Helium in the natural gas streams of the Urup copper-pyrite beds.
Dokl. AN SSSR. 118 no.4:771-773 7 '58. (MIRA 11:4)
1.Predstavleno Akademikom D.I. Shcherbakovym.
(Urup--Gas. Natural)
(Gases, Rare)
00 t
0000 - 0;Oir"m

GUTMVICH. M.G.; Q-tCHINNIPO-V-L-1---M'
Brief characteristics of natural waters in the region of the
TyrrW-Auz or@ deposit. Dokl.AN SSSR 118 W-5:1021-1024 F 958.
(MINA 12 t 1)
1. Institut geologit rudnykh mostoroshdanty. petrograffl.
atneralogit I gookhtnti AN SSSR. Predstavleno aitadamthmm D.I.
Shcherbakov3rm.
(Tyrny-Auz Range-Mineral waters)

GUREVICH, M.G.; KATS, G.V.; OVCHIMIKOV9 I.M.; SAUKOV, A.A.
ftterials on geochemical characteristics of natural gasee associated
with ore deposits of the Caucasus. Trudy IGEM no.46:83-91 160.
(MM 1491)
(Ore deposits) (Caueasus-Gas, Natural)

GRICHISKIB, Y.S.; OYCHIUNIKOV, I.M.
Instrument for the investigation of nuclear quadrupole resonance
in nitrogen compounds [with sumisary in English]. Yost. LOU 15
no.22:126-129 160. (KIRA 13:11)
(Nitrogen magnetic resonance) (Nitrogen compounds--Spectra)

AUTHORSi Gurevich, M. G., Ovehirinikov, I. M. 4C '- I
TITLEt On Helium in the Natural Gas Jets of the Urup Copper-Pyrite
Beds (0 gelii v prirodnykh gazovykh struyakh Urupskogo medno-
kolchedannogo mestorozhdeniya)
PERIODICALt Doklady kkademii Nauk SSSR, 1958, Vol. 118, Nr 4,
(USSR)
ABSTRACTs These gas jets in the ore regions of Kavkaz have never been
investigated. The gas occurrence mentioned in the t:tle was
discovered in 1955 - 1956 together with compressed water in
the boreholes. The above mentioned ore bed is in the upper
part of the drainage area of the Urup river in the fcothil;s
of the main ridge of Kavkaz. 3 complexes of sedimentary and
oodimentary-voloanogenic rocks take part in the geol(.gical
strucvure it 1) the oldest middle-paleozoic, mostly vreen rocks
which are to a great extent dislocated and only in small sect-
ions exposed by erosional 2) a mass of red lcwer-Pernian sedi-
ments, dislocated to a small extent, in a vast area; 3) almost
horizontal, normally sedimented Jurassic rooks which are stra-
tified in the middle part of the ragion with a diatinct ntra-
C ard 1/4 tigraphic discordance on 1) and 2). The tectonics of t1,@

P0-111'_ (-~~
On Helium in the Natural Gas Jets of the Urup Copper-Pyrite
freely escaping gases and those solved in water. The
of Urup are chemically to be counted among the hydrocaruor-
and mixed nitrogen-hydrocarbon-gases. Carbonic acid e.t-.er
lacks completely or is present in very small quantities. ~iyrir~,-
gen sulfide is assumed to have been present in great :uantit-
iea at the beginning, in the samples taken from sources f:ow-
ing for longer time, however, hydrogen sulfide was detected
only in quantities below 0,01%. The solved gases show a;:r~Dxi-
mat sly the same composition, except oxygen which m j.-ht have
beeZ dragged from the air. Heavy hydrocarbons almost Iack- -(-,m-
pletely in freely liberated gases (table 2). The hydroc~,7: T.S
are here connected with the metamorphism of the rocks, n,t
with the oil formation processes. Table 3 shows the ans,IYSIS
of rare gases in the freely escaping gases. The hel-un :.-
tent is high (0,4%). The distribution area of helium is -er-
haps greater here. The age of the gases with reference to
helium and argon was determined as middle-Paleozoic w~.irn
corresponds to the formation time of the chalcoFyrite bed.
These latter are assumed to be in connection with the ~Q,,dr-
thermal activity and with the magnetic cycles of the 31i,'_s-
kaya (Sudetic) phase of the Gertsinskaya (Hercynian:
Card 3/4 period which took place between lower- and middle-

.. 1-1~i
I ;i

SOLOLOV, V.A., otv.red.; SAUKOV, A.A., red.; OYCHIIINIKOV. 1.M., red.;
KUMSTSOV, S.I., prof., red.; AL?,KSNYkI;'OFI'.A.,' prof.b red.; G3039KTAN.
A.A.. kand.geol.-mineralog.nauk, red.; , GIIMSKIT. G.A.. kand.
goologo-mineralog.n.quk. red.
(Geochomical methods of oil and gas prospecting; studies of the
conference on geochemical methods] Gookhimicheskie metody poiskov
neftianykh I gazovykh mostorozhdenii; trudy soveshchaniin po geo-
khinichesicim metodam. Moskva. aprell 1958 g. (MIRA 12:12)
1. Akademiya nauk S&SR. Institut geologil i raornbotki gorjruchikh
iskopayemykh. 2. Chlon-korrespondent AN SSSR (for Saukov).
(Geochomical prospecting) (Oil fields) Otis, Nntural)

LIVSHITS, U.N., inzh.; OVCHJNNIKOV, I.N., inah.; PINSON, I.I., inzh.
Pneumoolectromagnotic loader of sheet steel. Sudoatroonle 29
no.5s49-51 Mq 163. (MIRA 16:9)
(Shoot steel) (Materials handling)

OTCHMIEN, I.N., Inthener: PWROV, N.I.. inthener.
Installing the steering g*ap of a tanker afloat. Sudoetreente 22
no.4:29-32 Ap 156. (mw 9:9)
(Steering gear) (Tank vessels)

LiRZEEZI'AE, Yu-iy 11,11,ydovich; I.L., inch.,
j
I I. , ~ I., -, ~ zh. , r--tsenzent; ALEK. V , I".1. I
red.; ~-~,d.
,'C-untinucu. :'low Ili,, li, ~.hu rminufartu:-e )f rinc-
--ings I I o toe hna I it , .1 n, irt 1 zvoto% I en-! in f I r-nt. (-v ~ k 1- -
L,ning-ra , .3xi,ij
. I f.c i -

OVCHIVNIKOV, _;van,,jjAko:~ayqyIgh,
inzh.; OMATTSO. , B.M. ,
RUBASHKII", R.A., inzh.,
nauchn. rod.; NIKITITA,
tekhn. nauk, red.
Prinimal uchastiye YAKUSHIN, 1.A.,
kand. -ekhn. nauk, retsenzent;
retsenzent;
red.; ALEKSAIDROV, A.V.,
(Ship systems and pipelines; arrarigemen't, manufacturp am. in-
stallation] Sudovyc vistemy i truboprovody; ustroitotvo, izFt--
tovlenie i montazh. Landrgrac, Sudostroenle, 196,.. 310 v.
(NIRA 18: 3)

% . . . I. - .I I I . .11.0 . ". * .
- .. *.:- - , . . I F-
- , I , ':' .
~ (":.. - . . .

KOR"YXV. V.M.. OVCHINNIYOV, I.P* (Leningrad)
Hisotry of the origin of the individual first-aid-kIt, Yel'd. I
a)msh. 21 no.lOt27-30 0 158 (MIRA Dill)
(BANDAGES AND BAIDAGING)

YEDIGILROV, S.G.1 RA$HCNBMN, NI.Ye.; OCMNRKOV, I.S.
Cunplete mechanization of major repaire of pipelines. Soft.
khoz. 40 no.10-.55-62 0 162. NnA 1617)
(Pipelines--Maintenance and repair)

ACCESSION MR% AP4013319 3/0020/64/154/003VO523/0526
AUTHORSt OwohUmIkovs 1.3.j Suvorov,, O.D.
Mul Transformation of the Direchlet Integral and space mapping
SOMEs AN MR. DoIaW. v. 154,, no. 3,, 19b4,, 523-526
TOM TAOS: Direohi*t Integral., DJLr*Ch]Lot Integral transformation,
-space mapping,, three dimensional mppUW,, conformal owing" topol-
ogy,, fundamental sequenc*,, Cauc1hy sequence
ABSMCT: The inequality exprossing the length and area principle
has found wide application is the theory or plane PPUW (con-
formalp quasi-oonformal, and the more general ones). Thu inequai-
ityp as well as a number or its mcodirioations,, can be obtained by
simple tranvtossations of the Direablet integral for a plane repre-
sentafton. If the problem, is to find a class of representations,, a
GIAMB Of admissible OWLINS and the roUtIve d1stanees introduced
by cow4at1bilitys then the p&vU of bovWW" agreement with the
topological representation Y.1f Av Y 46 3 con be refteed to
cwa W3

ACCZSUOK MRs AP4013319
prove that, with a direct and :inverse representation T and T-1
Cauchy sequence will turn into the funda~mental. This problm is
aut9matically solved if it Is possible to f1nd the functions ~0,
(OL ) and so that 0
j o' 1-0 with at -Oa and such that
T1 IPA W. e) I < fi, IT (x,), r (e) I < q, IPA W, r) I
for any points x~,, x"-C- A which are sufficiently close with respect
to P. . This was expanded to apply to three dimensional mpping.
The wmained classes of representation@ Include the class or q-
quamiconformal mappings, translating the dmains Inzo domains with
a bounded vol uime . The classes of the D and A d cima Ins can be ex-
panded by means of Introducing a spherical mistric, defining the r*-
latlv* distances by this mtr1c and azaalnlng the spherical analogy
of the Dirochlot Integral. Thle method can pemit simiplification
even in an n-dlmenslonal case. Orig. art. haso 8 equations.
A330CIATION: Towskly gosudarstvonny*y univereltet In. V.V.
CWd

ACCUSION MR: AP4013319
Mayby*sbeva (Towsk State University)
9 Oll ffTTZDl 3*A%103 DATE A04% 9bFobb4 NMI 00
SIM 00=2 M NO RV 3"1 002 OTM 1 001
cwd 3/3

YEDIGAROV, S.G.; LEVENTSOV, A.N.; KRUGLOV, A.N.; RASI"CHEPKII,', K.Ye.;
OwIrIfIrIKOV, I.S.
Mechanization of the packaging of solid petroleLm bitumens.
Neft. khoz. 40 no.4:60--65 Ap 162. W1RA 15:k",
(Bitumen;
(Packaging machinery)

R 'PS', - ',, ~. .,- - ; Bi-- H;ti_K~y , V. L. , "7" -:I .. , I ...
06--: cor,b_ned - -i.7' '.,: -e - ',*,~ft. ~!.Cr- - - -
,I ., F k x, - -, .. .

1~
OVCH: 11.111. : XOVI; .0.
Me trl c pro pe r t I e s (, f ma pi I ng a-, -,, , n1. iqr,., . bo~ . '.
161 no.3t526-529 Rr 165. Y. :. - -1 .
1. Tomskiy goBudarltvenrLTy i,ni - .,.*,. m.
Submitted Octcher -,. 19t,4.

CVCHINNIKCIV, I.S.; SUVOROV, G.D.
Trawfoiimtlons of the Dirichlet inLagral and mapJnev
in space. Sib. mat. zhur. 6 no.6tl292-1314 N-D 'b5.
(MIFLA 18:12)

ACC NRo AP6014527 SOURCE COM Ull/0199/65/006/006/1292/1314
AUTHORSt Ovehinnikov, I. S.; Suvorov, G. D.
ORGi none
TITLEi Dirichlet-integral transforms and thrge-dimensional mappings
SOURCEi Sibirskiy matematicheskiy zhurnal, v. 6, no. 6, 1965, 1292-1314
TOPIC TAGS: integral transform, mapping, conformal mapping, partial derivative,
bounded function, Euclidean space, vector function, continuous function D,,el cNi.E r
Pfflo& Ofn
ABSMCT: Proofs of theorems axmounced earlier (I. S. Ovchinnikov and G. D. Suvorov.
Preobrazovaniya integrals, Dirikhle i proatranstvennyye otobrazheniya,Doklady Jkk. nauk
SM , 154, No- 3 (1964), 523-526) are given. The principal theorem of the method is
expressed by the inequality
dr < M,1 D,.. .) < Mj D),
r
where M9 (SR)i and Or- U It is shown that for all values of r, the
. -
integral A(/, x)ds
Cor'd 1/2 UDCi 517-54

- --.777T~~
8 DIAFWL/
(t),/ -Peb
BVIVIVEX
JP 0,
-NIL
-,ACCP-MN AP5qO0653 8/0181/64/000/012/3669/3576
uvfok._~~ A. it Ovchlmikov, 1. Vi'-
A
ec
St trio dipole echo in pgaMMMetto so n ast2me
Fisika tverdogo tela, v. 60 no#, 12, 1064_1669-8676
-r 1*xatLon',,' paranagiketlvz~; pav&magnatic
petrib'dipol h6
0 ec , a
A' It'l
BSTA&CV,' s shown that it s
(W)'Cobo In sub-
_o sib e to_e=It
ectric dipole
Ch4aramagni6tic impurity faomis occupy a position in, the.lattice which Is not
ifiveksion beiter for the, Immediate surroundint. .. Tho ED echo is d Ao the coherent
mbtWu-'o'tt'he'eifect of E13 the
moments-of aramagne c- atoms and is die electric analog
.0 Mag
f netic pole (span) coho.- The calculatio
n of the ED eoho sigdalsis carried out by
b6i
roc e similar tq ftt used by the authors earlier (FTT, Y. 6, 23641, 190) for the
p
SOAY of the effwt of ED Induction xpresgtons are derivod.for the ED echo signil from
601 on configur on
harm o ions with electr aU d7 In a tetrahedral-crystal ficidt -'Unlike spin
CaM -

OVCHINNIKOV, I.V.
Nature of the magnetic developiment of the hydrogen bond in aqueous
solutions of vanadyl salts. Zhur.strukt.khis. 4 no.3:448-449
IV-Je 163. (MIRA 16:6)
1. Institut organicheakoy Wail Kazanskogo filiala AN SM,
Kam 1.
(Hydrogen bonding) (Vanndium salts)
(Rleotron paramWetic resonanee and relaxation)

V 1555b,43
'ACCESSIM NRI AP~W_Vft
Om I A *'-d k- -6 Y_
-)*tU*q!r*1ftxmL4o0 of Im 0041.0-,
telij,~v, 5i 307-2093
~N
I. iyd'i ~-l A tit
1~natlon Hrjdltord an orbi
t4vttl Co.. Interattion
7,
MRAOTt"-~ Thi:,Ouu6r,~- itats of 4.'basle"I"bentem of'relazatlon In
tmpups, ~6t,trandtlon elewntes *Wrodu2flti~wof orlRto a . I a lo I +
f 0 potion be vp ng o
iiiii): io~a-,.ty i6mal~'vibrations of-,ths surr "'dirl, ione,, -49raidre tbat-the mDdtila-:
by to%mr' al 'vi bratt In Abe lattice is 11
UOA~6f-,;~qrbltal- movement of an ele6tron tiem
A~Vi!d 6umb6ld sm also, in covalent corpotmdol ha:ccnrdder9 It necessary to redeterrdne'
,,the operstor o --orbit-srin interact2on, since the electron now belongs not, to the
7.-~ _,,~centr,4-~ loin bint Ao group 85 in Wholej L As avcnaeournes of the changelln operator'
In the character of.the wave- functiont the mzktr$W alevents of..the orbit-lettice t
uqni-~:pf -A~bq ftirkulmr Woment and' of, ipin-oitdt'lutt-.aitlon-(contnined in
c
04~ieral`. rApressl one for prdbe~d li ty o f q4i I' Wee tranaltions) also change.
V-1
-1,N) Zllt-~L7

~4)tvt *ith- ipir6#V --lialklAfto wve ftinotdon of a
in'.00 Albell to oc*p -the probAM 11 ty of, Spi'l.-rhmcm --ti-maltl ons for #M oet&)M&Rli
te_
'h ~000 Mr- -6tC. Gleetrpr Rd 91Ferie'rel'oryelusion; Is the*, the trenidtion
'P
)v 16tile W. co-yeent bmil.in .-Ikecomrarded by on. Inereass In time 6r Spin-lattlee
LOXAlo~'*' '.wft author tharjkb~$ A. Alitakuler for eettlngidp the~prablem and for,!
art. heav-1 f
or
It Wv;~"-UO argitnicheakoy.Atdidi lii~#A
M
Km #At* of Onle
'-Sel
IMCU (W.
r . 4,1
IS
0-,t
A~
~:7L

KESSEL', A.R.; OVCHINNIKOV, 1.V.
Effect of electric dipole induction in electron resonance. Fiz.
twer. tela 5 no.8t2364-2365 Ag 163. (MIRA 160)
1. Fiziko-tekhnicheskly institut AN 3SSR, Kazan'.
(Dipole moments)
(Paramagnetic resonance and relaxation)

M~J1111-iKovp I.V.
Effect of L--e type of cov-dent Do-.d or, '.~.e spin-lattice relaxation
of an oc'~~iodru-' co-,plex with one magnetic el-!ctron. Fiz. tver.
tela 5 no.7:1887-1893 Jl 163. (AII". :
1. ln3,.i'-ut orgaii~choakoy khimii k. SSSI~, Kazan'.
(Chem~'cal bondB)

OVCHINNIKOV, I.V.
Stark effect and spin-phonon interaction in paramagnetic crista-1B.
Piz. tver. tela 4 no.6:1597-1600 Je 062. (~aRA 16:5)
1. Institut organicheakoy khimii AN SSSR Kazan'.
(Stark effect) (Nuclear spine (Parasagneti5m)

OVCHINNIXOV
Spin-lattice relaxation in X3(Co, Fe) (CN)6. Flz.tyer.tela 4
no.lOs2750-2754 0 062. OGRA 15:12)
1. Institut organIcheekoy kh1mII AN SSSR, Kazan*.
(Potassium ferricyanide)
(Paramagnetic resonance and relaxation)

A'll
3108/3104
AUTHORt Ovchinnikov, 1. V#
TITLEs Spin-lattict relaxation in X 5(Colp*)(CN)6
PERIODICALs Fisika tverdogo t*lat v. 4, no. 1*0, 1962, 2750 - 2754
TEXTs K (Co.Fe)(GN)6 crystals can be used In paramagnetic amplifiers
(masers). The abnormal magnetic properties of the iron in the compound
K3Fe(GN )6 are therefore of interest. According to B. Bleaney and
M. 0. M. O'Brien (Proce Phys. Soo.* 9699 i2i6q 1956), the sixfold degenerate
molecular orbit splits up Into three Kraaere doublets under the action of,
a strong crystal field. A magnetic fiold.oplits up the doublets into two
levels. With the aid of perturbation thtoryt tho transition probabilities
within on* pair of levels or& calculated from relaxation parameters, both
for direct processes and for Ramon scattering of phonons. The resulting
expressions
Card 1/3
2/101/62/004/010/017/065
','his result calcul-Ved
smwmw~ 'a greater thqyj that

8/18 62/004/010/017/063
Spin-lattice relaxation... B106YB104
indicated by the experimental data, either because the approximation of
the strong crystal fields cannot be applied to oompounde with covalent
bonds, or because the group Fe(CN)J- form a stable complex which interacts
weakly with the remaining lattice.
ASSOCIATIONs Institut organicheakoy khimii AN SSSR Kazan' (Institute of
Organic Chemistry?AS USSR, Kazan')
SUBMITTEDs Ray 11, 1962
Card 3/3

I/is 62/004/010/oi7/063
DIOSYS104
AUTHORI Ovchinnikov, I. V.
TITLEs Spin-lattice relaxation in K3(CO'Fe)(CN)6
PERIODICALs Fizika tverdogo tela, v. 4, no. 10, 1962, 2750 - 2754
TEM K 5(Co,Fe )(CN)6 crystals can be used in paramagnetic amplifiers
(masers). The abnormal magnetic properties of the iror. in the compound
K3Fe(CN )6 are therefore of interest. According to B. Bleaney and
M. C. M. O'Brien (Proc. Ms. Soc., B69, 1216, 1956), the sixfold degenerate
molecular orbit split& up into three Kramer@ doublets under the action of
a strong crystal field. A magnetic field.splits up the doublets into two
levels. With the aid of perturbation theory, the transition probabilities
within one pair of levels are calculated from relaxation parameters, both
for direct processes and for Raman scattering of phonons. The resulting
expressions
Card 1/3

Spin-lattice relaxation...
5/181/62/004/010/017/063
B100104
M' WR2~4T [ L' '-"7 (9,'T' -#- PT- -+- 20 (y.' - T'Pr -0-
SCOVI 2
-+- 2 (#1 --#- 27a') 72.72
F11
AR) 361,4AIR4 (3a' -4-- bl) (9a' + b2) Is,
4, 2SPOOO
it
AV
elp dv.
tip
(2)
are determined only by the properties of symmetry of the system. Here R
is the equilibrium distance Fe-C, d is the crystal density, v the sounG
velocity in the crystal; the parameters a and b are determined accorcinw
to Van Vleck (J. Chem. Phys., 7, 72, 1939) 4 3 and q 6 are the normal vibla-
tions of the octahedral complex. The apin-lattice relaxation time calculated
therefrom is'rl. 2300T + 630T9 for T