SCIENTIFIC ABSTRACT FILIPPOV, YE. - FILIPPOV, YU.F.
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100
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December 31, 1967
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SCIENTIFIC ABSTRACT
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KOPIYNV, S.
TA-UMOV J4 , kandidat tokhnichvrkikh nauk.
Institute for innovators in Gorkiy. Stroltell 2 no.4-5:28 Ap-Hy 156.
(MIRA 10t1)
1. Predeedatell soveta instituta novatorov, Gorlkly (for Yilippor)o
(Gortkiy-Building tradeo-Study and tbaching)
.-.I- -kJ,
107-57-IL-51/60
AUTHOR: Dugin, B, and Filippavp Yee
TITLE: International Show of Radio Equipment (Mezhdurarodnaya vystavka radioapparatury)
PERIODICAL: Radio, 1957, Nr .1, PP 55-57 (USM)
ABSTRACT: The 3rd International Show of Radio Equipment took place in Lyublyana, (Yugoslavia)
in August 1956. The following countries displayed their exhibits: USSR, Yugoslavia,
East Germany, West Germany, England, France, Austria, Holland, and Italy. The Soviet
Union displayed the following equipment: "Rossiyu," "Lyuks," and "Kontsert" radio-
phonograph combinations; "Latviya," "Melodiya," "Baykal," "Rodina," "Turist," and
"Nov"' radio receivers; "Yantarl P" "Mir," 117jiWk," 11soyuz,11 11Prizyv,11 and "Rekord"
TV sets; 11EG-211 electric phonograph; TGK-3 thermo-electric generator for supplying-
battery radio receivers. A number of defects and constructional drawbacks of the
Soviet equipment are*lieted in the article. A feir items of equipment displayed by
East Germany, West Germany, Austria, England, ani Yugoslavia are described.
There are 6 figures in the article,
AVAILABLE: Library of Congress
Card 1/1
I" LW~$6, 7A -T,
FILIPPOV, Ye.
School of Gorkiy construction workers. VTO no.3.,52-53
Mr 159. 14IRA 12:6)
1. Rabotnik kafedrv stroitallnom *Proizvodetva Gortkovskogo
Anxhan.qrno atioltillacgo. inatituta-,
(Go~kiy-Zulldiug kesearch)
FILIPPCV~ ~~ohiy ohtuiuan.
Requirements of the navigation spaco on seagoing ships. More flot 22
no.7,33-34 n 262e. (MIU 15:7)
le Parckhod wBbUmyskx' SakWilinskoilb parokhodatvas
(Ship hand" ig-Equipmeu-mA supplies)
A
P, ql.--
LASKORIII, B.N.; SKOROVAROV, D.I.; FILIPPOV, Ye.A.; SHILIN, A.L.
Mixtures of mono- and di(2,4-Oathyl-l-octyl) methyl phosphonates
as extrac'tants. Radiokhimiia'5 -no,,I+t424-428 #63. (MM 16:10)
(Ph6sphonic acid) (4ctraction (Chemistry))
S-4-3622-1;,5
ACCF;~SIOM NTR AP5017002 UR/01H/65/007/003/0356/0357
'-42~ 61:546. 791. 6:661. 718. 14-661. 713, 2
A TT'ru"In - T -.4 9k In. ft. N. F111ppoy Yej ki Goncharanko, G, 1, - Scvortsov N
V.
U'- Ex-irac-lon of U~ftwum rM from aarbmte soltitions: hy quafewnitry phosWmatum anj
arsonJum bases
SOURCE: Radiokh1m1ya, v. 7, no. 3, 190, 366457
TOMC TAG-S-. itranfuns extra'&,Ion,'*ph'oephoftittm-*ba'se, arsonluin base, hYdroxYquinoUne
A I'Cr il A ('T. T, deterTdne the effect of the concentration of cartonate tons and nature of
-Ir~-ction of uranium VVD. the authors tested hoqpi),)niu!n :;qits
The
-~Tli-L~m saltz [R4As] ~C! ~ I orgapjr p!jg.,;r- nn-q)!;t(,f3 --I a
a.- ~e r -ia ry bat: e in ch loroio ~m or bu ty i e,, n,~ , K vi- ~ - , -t:: ~ ; "
1 )~ M aqueous solutions of urafflum contaNng 0. 1 N1 ammnni-um
a-ii1irl onrhonatp. were emidoved. The axtracti( n wa,;. -,qr,led ~~v
-rmhIned aqueous --rd r~rgan4- pl,:i- I u m
--Yr-,-ounda ~nve practlealiv the garnp. Rxrrnv--iv( nrocpr-ie, -rw aului-
:YquinoLine causea the distriDUtiOn MUO L(-) t~e FDU,
~,unds. It Is concluded that the extractirn of urswum ~~T) from carbcnate
card 1/9
L 03622 55
I ACCESSION NEt., APS017002
by the -hosphordum and argenfam oompounds is rather ineffective owing to a. decreas(i
in tion coefficient caused by a;i appreciabb! sollibilfiv of the complex in the
th--'--Aribution ratio blu-
1!,Wa
by G, in, Kaway nd r%,
all um a ad arsottium bases were synthesised
Orii-. .rt. hEs: 3 figures and 4 formulas.
A&iCCLATIO 4: None
SUBTfUTTED. 23Dec63 ENCL: 00 SUB CODE: 'YC
1' -
0 FLE F SOT: 000 07HER. 007
N
C.,d 2 /21,
INS-I
INITYP ~-IiMlfl
MITI,
W- USS"k.
gig~
SOV/124-57-7-7890
TranslatLon from: Referativnyy zhurnal. Mekhanika, 1957, Nr 7, p 61 (USSR)
AUTHORS: Vyzgo, M. S., Filippov, Ye. G.
TITLE: The Spreading of a Jet and the Erosion of Loose Soil (Rastekaniye
strui i razmyv nesvyaznogo grunta)
PERIODICAL: Izv. AN UzSSR, 1956, Nr 5, pp 45-56
ABSTRACT: Certain aspects of the phenomenon of spreading of a non-free sub-
merged jet and the erosion of loose soil are clarified. A description
of experiments is given on the vertical flow of a rectangular water
jet in a medium consisting of water'and sand in suspension which has
been displaced from'~the bottom of a flume by the action of the jet. The
dynamics of the formation of the erosion crater were studied. It was
established that after a certain period of time the depth.,of the crater
and its form become stabilized and 'a definite portion of the sand re-
mains in a constant state of suspension. It is pointed out that an arti-
ficial change in the density of -~he medium accomplished by means of
adding sand to the erosion crater or by siphoning off the suspended
sand in a corresponding decrease or increase in the depth of the crater
Card 1/2 up to a definite stable value. Various aspects of the motion of the
The Spreading of a Jet and the Erosion of Loose Soil
SOV/124- 57-7-7890
seepage flow in the non--eroded soil.are studied, as well as the pressure disLribu-,
tion along 'he contour of the crater. The values of the coefficient K in the formula
of M. S. Vyzgo for the depth of erosion
CL5 O.Z5
t qO E(I
are calculated by means of experimentally-obtained data. The values of K obtained:
for one and the same type of soil ranged from 2 to 5. According to the author these
values indicate that the depth of erosion depends upon the hydrodynamic characteris--
tics of the jet and the degree of freedom for its spreading and the quantity and size
of the particles of the suspended medium, but not. on the properties of the soil gen-
erally evaluated by the permissible flow velocity. The formulas of G, V. Vostrzh4E:Iii
were used for an approximate evaluation of pressure at the bottom of the crater.
These tormulas correspond to those of the free, turbulent. submerged jets (RZh -
Mekh., 1956, abstract 4550). in the first formula on page 46 of the article a i.cfar
vo has been inadvertently left out in the numerator. Bibliography: 11 references.
A, G. Chanishvili
Card 2/2
RI
7111PPOT. Ye.G., aspirant
state of research on certain problems of multistage
water intake. Trudy SANIIRI no. 104:81-90 159. (MMA 14:1)
1. Sredneaziatskiy r-muchno-ineledovatellskLy Inetitut irrigateii.
(Eydraulic engineering)
mj; --gn.
F-,
MWE
- I.: , -- - . ", I
- fi- ~ - 1,4- -"ll
MOH-M
-1 ; -, ~ M,
i'M MM
~M -, i -
FILIPFCV, Ye. M*
FILIPPOV., Ye. H. -"On the Method of Gana-Gam-Electric Core SamPIW (OOK)
(Theory and Experiment)." Min Higler Education USSR* Moscow, 1955,
(Dissertation for the Degree of Candiditte in Technical Sciences).
So.: Knizhnaya Litopial, No. 79 1956.
-%j A---
FILIPPOv: E. 1.,I.
"Gamma-Gamma Survey," 'Utilization of Radioactive Isotopes & Emanations in the
Petroleum Industry, (Symposium), Min. Petroleum Industry USSRP 1957.
Results of the Joint Session of the Todnical Council of ~Un. of the Petroleum
Industry USSR and Soviet Sci. and Techncal Association, Moscow 14-19 Mar 1956.
pgq
U`
Nu -10
11 11-1/1;4711, /10. 1 /,/1
'i
FILIPPOV 'Ye.K,
Theory of gams-gamm logging. PrIkl. geofiz, no,17:231-264 '57,
(KIRA 11:2)
(Nuclear geophysics) (Gams, rays)
Wi-tq Zaporozhetu, V. M. "Application of Charged Particle Accelarator:3 in
Borehole SurVeying by Radioactive Logging."
oo': "all
"Investigation of the Diffused. Sjr-ctrurl of Gamna- Radiation in Rocks of
Different Mineralogical Composition and Densities."
p. -~-i6 In 'book AwIled GeovhNSIOD, Collection of Articles, No. 2,9 Vlowev.,
(;o8tOVWWzftt,j Z58* 153*7-- -
Tbi articles are d**oW to a disc-ussion of methods of interpreting vuleop
tAps W electrima lop, methods of determining the Vorogity., rermesbility;, MR
apecifla surface che teristics ot water bearing rocks, and methods of determining
the #iT!ical properties of sidements anI the chamteristice of vin-lous "IcaL
para-metirs. A denarlytion of piezoelectric pressure recorders used in selumic
explamUou is also given.
~u V611,
-g
1420--
IVY"
ZAPOROZUTS, v.m.; ramwe Ye.m.
Use of particle accelerators in radioactive well logging. Prikl-
geofiz. no.20:234-258 158- (MM 11:11)
(oil well logging, radiation)
R MRS.
Ail
rb
Ila
j.i33
jA .3 JA 11%121911,149 !p I
t.;
31.
I J
P1 ;U21 2
jvi- J, , &I .
Ras J3 a ILj
.0 ]!lull
.IP aaI
11 ,
1). u,
A .4 A v1 1;11
%4i1 I
oil a a
3(5) SOV/132-59-9-7/113
AUTHORS: Filippov, Ye.M. and Kuznetsov, G.A.
TITLE:: Determining the Density of Rocks and Ores in Out-
croppings and Mining Sites by the Dispersed Gamma-
Radiation Method
PERIOX CAL: Razvedka i okhrima nedr, 1959, Nr 9, PP 38-40 (USS11)
ABSTRACT: The authors propose the application of the method of
dispersed gamma--radiation to determine the density of
rocks or ores on the spot. Experiments made vrith
samples show large discrepancies due to changes in
humidity and the rock structures when the samples
were taken. For this purpose, a light LM gamma-
densitometer was developed by Ye.M. Filippov and A.G.
Khryapin. It 16 equipped with an electromechanical
EMS meter which registers up to 100 imp/second. To
increase the sensitivity of the densitometer, the EMS
meter was replaced by a self-discharging halogenous
STS-1 meter. A "Kachall SG-7 stabilizer was included
Card 113, in the high voltage net for the delivery of a 380 v
SOV/132-59-9-7/13
Determining the Density of Rocks and Ores in Outcroppings and
Mining Sites by the Dispersed Gamma-Radiation Method
current to this meter. As sources of gamma-radiation,
a radium standEa-d Nr 5 (Em = 0.68 mev) and a cobELlt
source (Em - 1.25 mev) with a 0.5 micro-curie activity
were used. The volume of the intensity of radiation
I dispersed by the rock is calculated from the formula
I = I p - Infl - (IV - Inf2)
where Ip is the intensity above the investigated
rock; IV - the intensity in the air; Infl - the in-
tensity above the investigated rock without the
source and Inf2 the intensity in the air without the
source. If the investigated rocks have a low inten-
Card 2/3 sity, then the -values Infl and Inf2 are identical
SOV/132-59-9-7/13
Determining the Density of Rocks and Ores in Outcroppings and
Minine; Sites by the Dispersed Gamma-Radiation Method
and the radiation'intensity can be calculated from
the formula I = I - I Experimental investigations
p V C)
were carried out on rocks with densities varying from
0.46 up to 7.8 gr/cu cm. The results received in
units related to the density of the surrounding medium
are shown (Figure 2). The intensity of dispersed
gamma-radiation in water was taken as a standard for
the curve. It was found that the intensity of dis-
persed gamma-radiation in rocks of low density in-
creases along with the increase of rock density to
a certain maximum point which depends on the initial
energy of gamma-quants. There is 1 graph, 1 table
and 3 Soviet references.
ASSOCIATION: Institut geologii i geofiziki Sibirskogo otdeleniya AN
SSSR (Institute of Geology and Geophysics of the Si-
berian Section of the AS USSR)
Card 3/3
av A A g
.1a
Jul
v
44 up
31 4s
IL
lit
a Im 'r. lei*
k.--
Theoz7 of the photoneutron methods for studying rocks and ores.
Geol. i geofis. uo.6;94-105 160. (KIRA 13:9)
1. Institut geologii i IgeofisW Sibirskogo otdoleniya AN SSSR.
(Prospecting-Geopbysical methods)
V, ye~
Studying -the thiaknesb of layers in connection with the use of the
scattered-gamma-radiation method, Geolo i geofiz. U00:103-108 160.
(MIRA 13:9)
1. Institut geolo1ii i geofiziki Sibirskogo otdelsuiya AN SSSR.
(Ore deposits (Arospecting-Geophysical methods)
Mug-
q'.q,
ggi
FILDIPOT, Te.M.
-----------------
Use of the group method ol,' neutron density distribution In lnvest:L-
gating highly~-&bsorbent rocks intersected by the b02-ehole. Frikl.
geofis* U00271201-211 0604, MU 13:12)
(Wiosciiive prospecting)
T5
M
i,-; r7
, ra
I 17!lil~,110 R*P
A gE kv-z ~ot~
4Z
KOP"YEV., Sergey Ivanoviahj FILIPPOV'Yovgeniy kjikhayjovich,-_
14YAGKOV, MAO red,
(Volunteer institute of invento.ra and builders] Obahcheatvan-
ryi institut novatorov-i3troitelei. 14oskva., Izd-vo VTsSPSI
Profizdat, 1961. 52 p. (Building) (MIRA 1511) .
FILIPPOV., Ye.Ma; KUZNETSOV., GA.
I
Selecting the optiam design of a gammaj-donsitometers , Geol, i geofl2r,
no. lsl.13-n5 161* . (MIU 14:5)
lt Inatitut geologii,.i geofiziki Sibirskogo otdeleniya AN SSSRt
Novosibirsk@
(Donsitometera)
B/169/61/000/011/028/0155
D228/D304
AUTHORS; Polakq 1.B.j Pilippov. Ye.M.9 Kuz'netsovg G.A., and
ZhavoronkovP V~-Ia..
TITLE: Investigating the spectrum of dispersed gamma-radia-
tion in conformity with the solution of certain geo-
physical problems,
PERIODIOALt Referativnyy zhurnall Geofizika, no. 119 19619 34-35~
abstract 11A306 (G'eologiya i geofizika, no. 39 19619
111 - 115)
TEXT: Experiments are described on the study of the spectrum of
disperaed y-radiation; these were carried out with the aim of cla-
rifying the Possibilities of th Tethod of dispersed y-radiation
(DGR)o'The isotopes 0060 and CeT3 were used. A luminescent counter
with a cryetal of CeI (Ti) and a PD~-29 (FEU-29) photomultipl-. L e r
were enployed as an indicator. A 100-channel analyzer of the "Rlidu-
ga" type was used. The source-and indicator of the radiation were
placed in a lead shield at a distance of 7 cm from each other- The
depth-Potential of the investigation was ascertained in plexiglass,
Oard 1/3
8/169/61/000/011/028/065
Investigating the spectrum of D228/D304
gla6s and iron. The spectra obtained in these media are giveno It
was established that the increase in the density of the medium and
in its effective atomic number leads to the decrease in the depth-
potential of the investigation, The increase in the energy of the
sourco of the I-quanta from 0.661 m.e,,v, to 1.25 m.e,v. for a 7 cm
probe results in practically no change in the depth-potential of
the investigation. The recording of the maximum of the equi-librium
spectrum of the dispersed T-radlation in place of the recording of
the integral rate of counting is recommended when working with a
7 om pzobe~ this leads on an average to a 25 % increase in the depth
--potential. The dependence of the measurement results on the change
in the rock density in the interval 0.4 - 7o8 g/OM3 was investiga-
tedo I't was established that the increase in the energy of the sour-
ce of 'Ohe y-quanta results in the increase sensitivity of the me-
thod to changes in the rock density* It is shown that the presence
of small impurities of the heavy element (Pb) in the sand leads to
the she.rlp change in the spectrum of the dispersed T-radiation~ and
that the method's sensitivity to the content of the heavy element
In -the K-jump region is higher compared with the integral. In the
Card 2/3
S/16 6-1/000/011/028/065
Investigating the spectrum of ... D22SYD304
author's opinion the measurements of the differential and integral
rates of counting should be combined when determining the density,
of rocks and studying the content of heavy elements in them by the
methad of dispersed y-radiationg (Abstractor's note: Complete trans-
lationi.
Card 3/3
_-AFF
'L-.19OL8-53 M(lVEWWAPP', W/A~D-TVCZ
~PHASE -1 BOOK EXPLOITATION 1130V/1528,52~
F111ppov. Yevgen~Z,Mikhaylovich
Prikladnaya yadernaya geofizika; primeneniye, istoohnikov yadernogo
v geologil I geofizike (ADDlied Nuclear Geophveicsi.,
the Application of Sourcou or Atomic ation In geology and I
Geophysics) Mosoowo.Izd-vo AN SSSRj, 1962, .579 p. Errata slip-
Inserted, - b00 oopleis printed.
,;Iponsoring alney: demildL gvuk'SSSR, Sibiriske-ye otdelenlyj. In-!
stitut glologil: i-geq~fizlki,
14. (Title page)l Lo S. Polllko Doator.of Phyaics'and Mathematicaj,
Resp. Ed.: 'E. Z. Potladiji'cCorre-sponding Member, Academy of sel-Z
enoes USSR; Ed. of - Publiolting Housei V, .'M, Keder; Tech, Ede*:
T. A, Fru3akova And Ye, V, Dlakuni,
MRPOSE:. This book Is intended for geophysicists imd geologists,
as well as for engineers and technicians: working in the
field of applied nuclear geophysics,
Cbxd 01
WOOM
19048-63
Applied Nuolear,Geophysion; the Application 9jr-(Cont.) SOV16285.-
--COMAGE: 1he book contains a review of nuclear geophysics ~ethc6~.
through 1960, Various' methods based on the utilization of exter-'~
nal nuclear radiation sources In-geophysios and geology aria in-
vestigated, The following personalities are mentiondd: _Pji. A..:
Oubemanj coworkers of the Xnstltute of Reolosty and
_Xa, Bespal
Pex!glopment of Mineral F110 12- 1. i&M_qqKa -o
P.--M. Srebrodollsifty., and Yu.._a.-S=eleviqh; A,Y_a. Te P men,-w
ber of the Institute of Potroohemlbaj Synthesis of the Aeade
--Solences-US ; V S A. Kantor, Referenops accompany.
.t--I.-Baranov,
Individual chapters. k
TABLE OF CCNMT4 (Abridgeals'
3',
-Pieftoe
Introduction
/K
'Card I
- ----- ------ so- -- -- --- -- -
mummNlys V.V. (Moskva); fFILIPFOIr,-V W .(Moskva)
Rxperimental investigation cof light-ocattering phenonmm In laminar ,
and turbulent fluid flows. Izi.AN SSSR.Otd.tekh.nauk.MekhA mashina,str.
no.6tlO-16 N-D 162. (MIRA 15%32),
(Light--Scatt4dring) (Laminar. flow) (Turbulence)
POLAK.9 L. S.; FILIPFOVP Ye. M.; KMNMOV, G. Aj ZHAVORONKOV) V. Ya.
Concerning the remarks of S, G. Troitskii, and V. L. Shashkin
in "Goologiia i geofizikaw no. 7p 1962, Geol., i geofiz. no.9:
125-126 162. (MIRA 15--10)
Rocks-Density) Okmma-raY sPectrometry)
roitskii, S. G.) (Shashkit, V. L.)
R
URVARINt G.B.; ZHAVORONKOV, V.Ya.; FILIPPOV, Ye.M.; BORISOV, V.B.;
HELIK-STEPANOV, YU-G- 0"Wav'"W-ft
Determining the'density of the flow of a mineral suspension during
ore dressing on shaking troughs, using a source of gamma rays.
TSvet. met. 36 no.70-10 J:L 163. (MIRA 16:8)
(Ore dressing) (Suspensiotin (Chemistr7)--~-Density)
(Gamma rays-Industrial applications)
ciw
R~QW--V94NMIV
L 163A3_65 EwF(e)/Ew(M)/DIP(t)/EWP(b) Pq_4 IJP(a)1FSD(t)1Mj)(gs)1g.A.
A %~Q16TRIA M,/! -9 D a 5 JDZ
ACCES310H W4.1 S103.,
%6/64/(W/008/0020/0020
AWHCO: Ostavoy, I* T-; 11ilipport. Td. K4WAAr-O
TITIX: Use of nuclear methods for auto=ition of the procesa of sorting ores froll
_gold ore deposits
SOURIIIE: Tavetn1ya metallyt-aa., 8 t1964, 20,-
TOPIC' TAGSI ng, -gol
-ingineeri d, kadustrial stutomation, radiation,inatiament
ri- Ii7_ - __ 1. 1: - - - - ~ 71k
IC
Y
i , t
6-Redaar~CW~ e -of Tin has nvefs igat
ran Le riiv-al- nati W. A
Ing- i6f --- tho-pro
radicratric methols of autut(W cess,
btained f:rom Krasnoyargkiy Kray. rA miaeralogical campoGition, tle 041C mass
0
consists oT Vhyllitized achists., pIWLlites., and vein quartz-~~Gold ir-, chiefly f
assc,-;jP_te(i vith sulfides aneL quartz, and with schists-Eo-a rr"ich learer degree,
The radjausetric method of autornating the sor+,J-rkg process ie based on
sevet:.ral phenomene. observed idien gamma rEqs or elementary particleti interact,
witit matter; att(nuation of the beam of the penetrating Canaa racLation,
saw.-terine; of the latter, mad thu'phenomeam of induced activity.
A Eitudy, oi.1' the chemical compositaon and physical propertie*i of the on
-And rock catablifshed that the Separatiai oll' the ore from, the rock is possible
'113
L U~
I :MR:
Ail AP5002052
J,
if- ome in m--Ae of the value of tht indulled activity uhich arises ac a result, of
irrtiiiation of the material (ore or rock) by a XLeutron fliix-
Since the gold content of the orfr in minute, a-ad the half-11fe of the
radioactive isotope AI-1198 is 2-7 days, 'the direat separation of the ore and
rOCA. In a fl.O'W by Means of th's metal ditl not secm possible.
To solve this problento other clements weiv ,Ised
nucirmr character-'
JG'Llcc- me(t the$e recluiremeatst name-1,Y, alurdnuai, Which has a rejaijv---~v high I
activatiori capajity.
In order to detemine the -poasib:Llil.7 of aeparating, ore rind rock by the
mietjod of induced activity based on alwtinum, a calculation was car-ried out for
th-e ea=le! under investi tion (irradi=ion tim used vas ! sec. and the film
density 108 neutronarcm2-sec) which showed a difference in the 1-nduced ac-
tiv-1ty of the schists, quartz, and conc:retions. In order to r:heck calculated
'dat3 on tle possibility of separating sl:hints from quartt and concretions, ex-
perim-nts on samplea of the ore and rec'c wtire car-ter! oiil. ir I~he ictlvatiniz =-t
i --tutie of 5e-)logy and GeopbYGLC-13. Acaden-,.r (if ~S~-
Prvatm~nt of the experi=ental da% produced vulues arf averag-, 13Tx--cific
ac-UIVI,~ICII for quartzj, concretions, and dark and gr%r schist-5, whLai ahow-ed thnt
Cas4l 2,13
g a
WVc
HIM
L 1.6313-65
AMMON NR: AP5002052
fdT different--min,era.logical groupaj---thoediffererae, in specific induce& aetivif4,
is relativ e-ly. g;eat; thusp ' quartz -and concretiom used for further cmirichment -T -7
hwre- an activity that is 2 to 4 times (to high av that of the schists.
The possibility of neparating ore from Uie rocr, by uGing sly!ctra of in-
ducced aclAwity in the region of soft ffmmm radiation wIth an enerf7r tip t-o I
MeV VaG kLISO checked.
Jknalysts of the data obtained a-imted that the resolving p-:)----r of the
r',-.-t-rr_Tr4!tric risthod was greater thar. that of the measurep-ni- -)I' t),n
ioc'uced activity. Thus, Ulic recording of soft Mdintion in the rej;iom of 1 tri
charinels gives a 6- to 3-fold difference in -~he induced activit:, of quartz
~kn, --n,7--etions vith schiste, against a 3-to 2--'old differene- ii 'h- -Ftse of
E reco.tIng, the integral induced activity.
Die calcidated and experimental investigatimis which were CUrried out
shcfwed the flundoxaental feasibility of separatix4~ ore from the rock of the i
gold-ore deposit by use of the induacd-clativity method.
ASISOCIATION: none
SUBMITUM: 00 ENCIL: 00 SUB CODE: GO# NP
NO PXF SIN. 000 OTIEER! OW JPRA
Card 3/3
V -
figr
N' .42;
- ME 19 M00,1~9-1, -'M' IR
;
7. 7--
-4
L 5 8 5 B3 E.64P( )/FMT( TJP(C) JD
A C r. P; S I C. IN qR: AP5019017 UR/0286j65/000/--'2/0042/0f:42
550.835
.AUTHOR: rilippov, Ye. H.; Vakhtin B. IS.; Rusptyev, 11. G.
TTT!;'- A device for determining the Molsture Content of or-es which '-,:)ntain borcm.
.Cla!;.; '41, No. 171937
ISOURM: Byulleten' izobre~eniy i tovarrykh znalcoV, no. 12, 1965, 42
TOPr-' TAGS: mining engineering, ore, moisture me&;urement
This- Author's Certifi-Cate, in-noduces a 4e-ice for detaimin,Az the moisture
---s which contain boron. T'ie unit con--.al:ns a neulron sr-ur-e, dete-or
t
~-r\-en for shielding the de:ector frorn t~e n1i
e - -. ,a Im-ul-rons which are sensitive to the conten-: c,f bor--~n in '~-)e Accuracy
,S 4mpr--~,voe- and single valued readings ire obtained by using an iadicator which is
activated by slow neutrons which are not semsitive to boron.
ASSMATION: none
ISLIEKTIVED.- 109ar64 ENCZ: 01 SEO CODE: E4NP!
C0111 1/2 110 REP SM. 000 OTM2: 000
~98 3-6"
ACCESSION NR: AP5019017
Card 2/2
ACMSSI-V NR: APS019018 LR/0286/651000/012/004,1/0043
550.835
AU'HOR: Varvarin, G. D.; Zhavoronkov, V. Ya FilipZZZ'L
A levice for simultaneously dotemining the --ni5l--r-
iii natural deposit5. ~:lass 21, No. 1-1-?39
S
Sj'~:RICE: Byulleten' izobreteniy i tovarnykb makov, r1o.
k 12, 196!), 43
TiM:I~' 'FACS: molsture measurementl orf., scjntillatiqp--q_9uq~-e.K_ .41
Ayi\ 7*
ABSIRACT: This Author's Cert ficate introduces a device for siuultaneouslv dt!ter-
mining t~e moisture content ana volmetric weight of :)res ir naitural dep,:?sIts. The
contains a radiation source, a scintillati.)n courter, a shielJ for pro-
lec~ing he counter from the radiatio-i source* a cadm~:um screen and -a measumr.-ent
cir-uit. The device is designed for usinst a single s-int I E;- 1*2gis-
~-c,~t-ervd garnma rays which inlicate the --,roluriotri- and
-,i- rnn capture gama radiatici where -,he theima I r--,!; e '~ e
--fern of f~e ores. For thii purpose -,tie -S Sur-
-ance
q
Carcl 1/3
58985-65
ACCESSim if Apsoiwii-
ASSOCIA11ON: none
SI.BMITTED: 28Feb64 MCL: D I
NC PE7 sov: ooo
OTHER: coo
m Com: UP
Cai d 2/,4
AC:ESSio-N HR. APS019018
EINCLOSUREi oi
L
lCm-d 3
imon=
l?II-10 ~M I
9
I.I.H.",i -1
VAKIII'llip B.S.; ZRAVORONKOV, V.Ya.; FILIPPOV, Ye.M.
Using the SRP-2 radiomelter for solvIng certain practical
problems in geology. N.zved. i okh. nedr 31 n0-1:40-1+4
A t65. (MIRA 18:3)
1. Sibirskoye otdeleniye AN SSSR.
VAMM-Nk YO.M.
Do+
,e--n.natlor, of the Migh content of boron In po
viler samples
by tha neutron--neut.rori :method.' Geol. i geofiz. no.4~155-157 '65,,
(MIRA 1.,1,,8)
1. hn' tut geolcgil. i jgsofizl~l S~bIrskogo otidele.-II.Ya AN SSSR,
Ncv,~aib-'Irsk.
'NS:
2~!!ANORONKOV, V.Ya.; FILIFFOV., le.,~.
. ying rocks and orer! d4.f,- *
Problem of classJg I iering
in normal physical properties. T3vot. wiet. -18 ,,
My 165. (.,f,rIR-' 33:6)"
FILIPPOV) Y66140
-1--w- I....... :.,;~.,.
Possibility of aerlial proopecting for mineralE with a generator of
-,,wirmm. Geol. i gettiz. no.2,IVI-122 165. (MMA l8s9)
1, lustitut geologli i geofiziki Sibirskogo otdelenlya AN SSSJI,
Novosibirsk.
Z4"(lRONxOv,,,V4Ya~; FILIPP(MI YG*M0
0
Determination of boron content in rocks by recording garma radicition
from the B10 (p,(f,) reaction. Geol. i geofiz. no.7:101-103 165.
(MIM 18:9)
1. Institut geologii i geoflziki Sibirskogo otdelenlya AN SSSR,
Novosibirsk.
VAKETINY B.S.Y FILIPPOV, YO.M,,
Neutron-neutron profiling in determining boron original rock
outcropi Geol. i goofis. no.lOtl32-135 v64. (MIRA 181l:2)
1. Inatitut geologii i goofiziki Sibirskogo otdeleniya AN S3.511,
Norooiblroke Submitted January 25, 1965.
W-4
ACC NRt AP7013162 SOURCE CODE: UR/0210/66/000/009/0094/0102
AUTHOR; Filippov, Ye. I.I..--Philippov, E. M.; 1havoronkov, V. Ya.
ORG, Institute of Geology and Geophysics, Siberian Department, AN SSSR,
Novosibirsk (Institut geologil I geofiziki Sibirskogo otdolonlya AN SSSR)
TITLE: Possibility of using electronic accelerators In truck and helicopter
surveys
SOURCE: Goologlya I geofizika, rto. 9, 1966, 94-102
TOPIC TAGS':electron accelerator, gamma radiation, geologic Instrument,
geologic survey, photoneutron, geologic research facility, stratigraphic
mapping, prospecting, helicopter I MI-6 helicopter
SUB CODE: 08,20,01
ABSTRACT:. The author discusses the possibilities for using electronic
accelerators as sources.of powerful gamma radiation for doterming the presence
of a nua-ber of kinds of minerals by the photoneutron method. Computations are
presented showing that nuclear technology now can be employed on land or fr(:"
the air for both geological mapping and determining the rock content of beryllium,
deuterium, lithium) carbon, thorlum and uranium. The Institute of Nuclear Fhysics
of the Siberian Department of the Academy of Sciences, for example, has deval-
oped an electron accelerator weighing 1.2 tons that can be used aboard
Card 1/2 --....-..UDC: 550.835
4Z
-P.
A
ACC NRj AP7013162
a helicopter employed for geological prospecting work. A MI-6 helicopter
with a load-liftin,o capacity of 10-12 tons can be used. This craft can lift
up to 8 tons on a cable to heights of 25-50 m. The helicopter carriers
recording apparatus and a current source for operation of the accelerator.
The crev Is protected by lead shieldin- ireighing about 1 ton. Therefore, the
total wel.nht of the apparatus on the cable is 4-5 tons. The control panel,
recording system and computer waigh not more than 1-2 tons. It is reccm-
mended that helicopters bareplaced by less expensive dirigibles. Prospecting
for beryllium (for example) can be carried out from a height of about 50 m
and its clarko can be determined with sufficient accuracy from a height of
25 m. The doses of radiation at the surface are entirel harmless. Orig. art.
has: 1 figure,'9 formulas and 16,tables. EMS: 40,10J6
2/2
ACC NR: A1470070-14 SOURCE CODE: UR/9-003/67/000/052/01DO5/0005
AU11,H01". _r'i.11Q_P_0_V_._YL.(D0ctor of goo-minuralogy, Head of Laboratory) (11ovo,3ibirs;')
ONG! Labt clear Geopliysics o Instituto of Geology and Geophysics of
Sil,crian Bratich Academy of Sciences, SSSRfLaboratoriya yadernoy gcofiziki Instituta
geologii i geofiziki, Sibirskogo otaeleniya Akaaemii nauk SSSR)
TITLE: The atom, geology, and millions (A discussion of the intelligent!
,use of new achievements in 8;eophyvics]
,SOURCE: Izvestiya, no 1-6
52, 2 Mar 67o P- 5, cola
~TOPIC TAGS: x ray analysis,.geophysies
ABSTRACT:Filippo'v, -Doctor of Geclogical-Min*eralogicai Sciences and head of the
nuclear geophysics laboratories of the Institute of Geology and Geo ysics
(Siberian Department of the'Academy-of Sciences USSR) wAtes that n'aclear
geophysics methods are being introduced at too slow apace. The-edit-ors of
.".Izvestiya" agree with F-ilippov and comment pro and con on the performancesi
nf various ministries. [NC]
09//
SUB CODE: SUBM DATE: none/ ATD PRESS: 5116
IVANOV, Turiy Vladimirovich, kand.tekhn.nsuk; PrinimalLuchastiye:
ALAKSEW, N. I., inzh.; -YILIZMYe
,N., makhanik; AMITPOT,
G.F., mak-hainik. 'BOMILIN, A.P., red.; NIXOLATIVA, L.K.,
tekhn.red,
(Maintenance of the steering gear and pin couplings in a motor
vehicle] Proverka tekhnicheakogo sostoianiia rulevogo upravle-
nila i sbkvornevykh soadinenii aytomobilai. Moskva, Avtotransizdat,
1960. 33L P. (MIRA 13:11)
(Motor vehicles--Kaintenance and repair)
FILIPPOV YQYAeR"k&R;.%jc
(safety marnial-for the oper'ators of roadconcrete-
machinery ftuishing) Pairdatka po tekhnike bezopasnosti
dlia mashinistov dorozhnykh betonootdelochrWkh mashln.
Moskva,, Str0iizdat, 1965. 17 p. (MIRA 19:1)
s/18o/62/000/006/0,01/022,
2193/E383
AUTHORS: Vertman, A.A*, Samarin# A.M, and ~1"RP_Qx,_
(Moscow)
TITLE.i Viscosity and electrical conductivity of liquid
nickel-carbon alloys
J~
PERIODICAL: Akademiya nauk SSSR. IZvestiya. Otdaleniye
telchnich.eskikh nauk.- Metallurgiya i toplivo
no. 6, 1.962,.37'- 42
TEXT: in continuation of an earlier work (Izv. AN SSSR, OTNI
Metallurgiya i toplivo, 1960, no. 6, 162-167) the authors ha-a
determined the concientration-dependence of viscosity and elec-',,
trical c-onductivity of liquid nickel-carbon alloys in the 0-2*3%.;,~~
carbon range., The results -are reprodaced in Fig. 4, where.the
viscosity (-~, contistokesl and electrical resistivity
of the -all oyd- -i-ndic'
pera ures ated by eacli curve are plotted,.,-,,,
against th(i carbon content (CI wt9%) of the alloy* Since it had-,.
been shown earlier (V.M. Glazov, A.A. Vertman - Sb. Stroyaniye i"e_~
as
svoystv zhidkikh matallov (Symposium. Structure and properti
of liquid metals), Izd-vo AN SSSR, 1960, 124-137) that the vis-~
cosl tr.4sotherms of eutectiferous systems passed through a
Ca d
r
S/180/62/000/006/001/022
-E383
Viscosity and E193/
minimum at the eutecticcomposition (1. e. in ~he alloy in which
the relatively weaker forces binding dissimilar atoms pradominated~,....._-.`:t
the curves reproduced in Fig. 1k indicated that the Ni-C eutectic'
was formed at 1-35% against, the published Yalue of 2o0-2..5% C'. Tho
constitution diagram of theNio-C system was therefore reinvostigated
by thermal and metallographic analysis; ' the results showed that
the eutectic was, in fact,:formed at approximately 1-3-1.4% C _:-q
It was concludpdt consequently, that the minima on the viscosity`..1:~-,,.:,-J
and electricalZ-'resistivity isotherms were associated with the fact
that the short-range ordorinherent in solid eutectic alloy4 w
retained on melting; increasing the concentration of either Ni
J~
or C in the alloy brought about an increase in the proportion of
the relatively stronger forces between'similar atoms which, in
turn, increased the viscosity of the alloy. The existence of'
viscosity hysteresis was also established. This effect -was
attributed to the-existence of microscopic arrays of C atoms in
the alloy; these~dissolved partially on melting, as a,result of
which their size during 'subsequent cooling was smaller' than during-.
heating,. this dif f erenco being reflected in the viscosity of . the;,
-'in the concentration-*'
alloy* The presence of a.shatrp minimum
-Card. 2,4
AMR
M'
P _ 5, Vt
S/180/62/Ooo/oo6/001/022
~Viscosity and Z193/E383
dependence of the activation energy for the viscous flow of Ni C
alloys.was also'attributed to the~effect'.of microscopic arrays of
C atoms~ The~,concentration"dependeftce of the ratio
TB
(where and. PTB denote,'respectively;-resistivity of the
the liquid and solid states at the:eutectic tem
allay in perature)
'was also determined. The value o
f ~)4k. practically constant
In the hypo-eutc-sotict-alloyst increased sharply -in the hyper-
eutectic range. This effect was attributed to partial dissolutioni
'The, general cone usion was-:
of the carbon micro-arrays on melting.
formation of earbon micro-arrays wao-a property common.
to -all three systems of the Ni-C iystem which represent *a limiting
case of microheterogeneous 'eutectic afloys, w*th pro~perties
approaching those of a colloidal s0iiLtion'. There' are 7 figures*
SUBMITTED: May 8 1~ 1962
-Card 3/4.
s/iLBo/62/00 0/006/OCII/022
ViscOSit y and EJ.9~/E383
V.
C-07
zzs
Os
/so
ISSO.
p L
10
44.
Card 4/4
UP,
M
VER24ANO A.,Aoj*, SAKARINO A.M.j FILIPPOV Yej,
PMA diagrami of ii - C. DAL IN SM 10 no.2:142-34,) A '63.
(MIRL 16s2)
lo Imstitut metallur i im, A#A. Daykova. 2. Wen-korrmpondent
AN SWR (for Samarinf.
(Nickel-carbon alloym)
ACCESSION NR: AP4022716- S/0020/64/155/002/0323/0325
AUTHOR: Vertman, A.A.; Samarin, A. M. (Corresponding member);
Filippov, Ye.S.
TITLE: The density of iron, nickel and cAalt in solid and liquid
state.
SOURCE: AN SSSR. Doklady*, V. 155, no. 2. 1964, 323-325
TOPIC TAGS: iron,*'cobait, nickel, density, solid state, liquid'state,~
fusion temperature, temperature density function, activation energy,
fluidity density function, structure stability, interatomic distance
ABSTRACT: The densities of iron, nickel and cobalt were determined*
by the "large drop" method (V.N. Yermenko, Yu.V. Naydich, Fiz. met.
=e,~alloved., No.-6, 883 (1961)) to obtain more accurate data than
pre-sently available'(fig. 1). It is proposed that the increase in
density in the proximiVy of the fusion temperatures of the metals is
caused by the evolu:tion of gases oxf fusion. The temperature-density
function of the mqtals in the liquid state, calculated for the equa-
~iofi .4 V A expWRT)., where B is the energy of activation, is shown
,~.;.,d 1/4,
.,ACCESSION NR: AP4022716.
in fig. 2. The break in the curve for Fe is caused by a transition
t~d: the gamma-iron ',st-rudture' The tluidi density relationship
according to the fprmul:a i~~ - a -b/ VZ density I a and b are
dbnstants) is a straight line function. The deviation (fig. 3)
!chows the structures d6:hot remain., constant and is associate'd with the
atoms aligning to ~he dtructure of ithe solid phase.,: Calculations
vi6re made to show that'the structure of Ni is the most stable with
r'6spect to temperature,change. Interatomic distances wore calculated.
froi the densities'for,Ni, Co, and Fe in the liquid state. Orig.
art. has: 2 tables, 3 figures and 4 equations.
ASSOCIATION: Institut*'metall%irgii im. A. A. Baykova (Listitute of
Metallurgy)
SUBMITTED; 150ct,63 DATE ACQ: O8Apr64
SUB CODE?: KIL NR REF.SOV: 005
CPrd 2/4'
FILIPPOV, Ye.S'.; VERTMAN, A.A.; SAMARIN, A.M.
Apparatus for measuring the density and surface tension of
iron melts.- Zav, lab, 30..no.5.-620-621- 164. (MIRA 17:5)
1. Institut".weth.1lurgii Imeni Baykova.
VERTNAN, A.A.; FILIPPOV, Ye.S.; SAMARRI, A.M.
-
Density of iron alloys with carbon in solid and liquid states.
Izvo vyoo uohebe mv*; chern. met* 7 no#M9-23 164
(MRA 17t8)
1. Institut metallurgii im. Baykova,
4W 04(
3A -7-
94 _W '-:!;/01,,48/64/ow/(07/ca62/oi64
ACCESSION NR:_' NWATWAN
.,AUTHOR., 7,
7-_
_7 !r
ME lh-
_jtatea
_2111 _S' _LuLd
SOURCE: IVUZ. _Gherna'a v!qWl~trgiygj1jtq* -7,19641 16a-164
loy'~~:*o alloy-, tic ltit~5' _1
TOPIC TAGS- obAtbase al e arbon'containing
-Metal ~P#0~1;6et-y
t h t iiidAA4. 1*4rVA A 4-
..Abe raatj.
Ln oteentx4tt n derandenee
id Co-C aud Ni-C alloys. Ln th liquid
. I e and Golid otates, since
density if; directly related to the. changle in the rtructure of e. solution.
Density pc4ythertrus were plotued, and then used to plot Isatterms for -.he
l(YY)-_17rA-) C, C rwige and to deteiTdre U~e inrLuence! 3f carbon on tile V011jr-
chan%-'- ta'e-inr, place on mltinr,. In the range of Low con--entrat ions (approx-
i"atelY O-Xv, in the Ni-C allcryr e-nd I.YoG irA tht., Co-C PULrj), dIssolixtion
of carbon oharply Increases decompression of the 1;olution, i.e., in the
allws studied, the bondlug forces tetween like particles sw-uass those
men LwUk law should
betve e odes), so that positive deviations :F'rom Raoult I
be exp-r~-cted in Iii-C and Co-C alloys. However, Eut carbon concentrationr> be-
low 0.9rf,, alidit tidgative deviatiods' are obverved In the Iii-C system which,
i Card 1/2
L 16006-65
ACCESSION I(R, AV500194~`.~
at "nigh concentrations,, become pronauimed"positivo deviettions. Eutectic,
Ni-C al-l(Yjs are characterized Py only a Slight invivaite in lien'tity V41th i _n
c-irbon content, aa ia the Fa-C eutectic. Thic, appcars to uc ciue ~_o
the thei-riaL stability of large eutectic, "colonied, and indicates the preser-
vation of ghort-rGnge order in the ettte-.tic m1t tip to about N 000C.
Ori,~. art. has 3 figures.
ASSOCIATION: Institut metanurgii itt. Baykova trustitute of Metallurgy)
SUBMITTED: 20.Kar64 LUCL- 00 SREI CODE: IV,
VER7MAN, A.A..; IVOOV, D.P.; SAMARIN, FILIKOV, Ye.S.
Changing the dennity of liquid caut iron by iscithermal holdina.
a
Lit.proizv. no.10:30-32 0 t64. (MIRA 18:41)
FILIPPOV, Ye.S.; VERTMAN, A.A.
Connection between volumetric charscteristies of molten iron
and "critical concentrations." Izv. vys. ucheb. zav.; chern.
met. 8 no.5:5-8 165. (MIRA 18:5)
1. Institut metallurgii imeni Bay1cova, 14oskva.
FT1,!FPQVY Ye.s.,. SklifjRIN) A.M.
Do-termining tho sborle-range c-rd-ir otru-.turt of 'j.'quid birary a*11,-78.
Dokl. All SSSR 165 no,1285--9,7 N 165. (MIRA 18t1O)
1. Tnotitut matalltir,i- 1-m. A.A.Baykrva. 2. Wlan-karrispondont
P11 SSSR (for SamarM--
FILIPPOV
Determining t~e coordination number of liquid metals by
their temperature relation to density. Izv. vys. ucheb.
zav.; chern. met. 8 no.11:103-109 165. (MIRA 18:11)
1. Institut metallurgii im. A.A. Baykovi.
VA T (m) /T /EW P (t JDANIM,
AM-N-R, AP5028575 SMCS CO-99:~Mt/0148/65/000/011/0103/0109,
AUTHOR:. Filippov,.Ye. S.-
lur (I~a.ititut metallurgii im. A.
ORG: A. -A Bat* Ai. Bsykov~
Institute of Meta~ ff. .
.~TITLE: Determining the coordination number of molten metalAi'lecording to the
temperature-dependence of density
SOURCE:- IVUZ.,Chernaya, metallurgtya, no. 11, 1965, 103-109
TOPIC TZGS: molten metal, 4.*mFd*swa4atF*umberr, fluid density, temperature
dependence
ABSTRACT: It,is shown that.the coordination number z of molten metal can essentially
be determined according the ideal volume Vo at O*K. Vo itself represents Ithe -sum of
the voltnne at atoms V and free volume V , and it can be determined by extraipo-
at
lating thd volume of molten metal at meltINS point to O*K. For molten iro-a the thus
obtained., V. of the "y"-structure of short-range order is less than the V of the 1160-
structure, which. corresiponds -to the theoretically expected increase of c2ordination
number from 8 to 12 with.heating at 17004C. It can be shown that the extrapolation
of the volume of molten metal to OOK indeed completely-accounts for the entire free
volume due to thermal expansion (Pig. 1). Ifp in sccotdance with the malting points
of specific metals, the absolute values of chanile in density during malting,
Cmd 1/3 ....ULIC: 669-154:541,12-
o
4-1 ';
VW" i~
_-13
ACC NRt 8575,
"A d (d d are plotted along ithe ordinate on assuming that
melt. solid liquid t
melt.
th weight of -the- atoms -,of all the 9 6d from Oi
e _ _ ----metals.. is,Identical. (I.e. on plottin
for convenience),.and.if in accordance with the temperature dependence *I* density
(Ad 1A T) to me, + 50*CP the thus adjusted values of density of the molten metal at
to
melting point are extrapolated toVK1 it will be noteld that Ihese valuet are roughly
divisible into two groups: with denso packing (z = 12) and if h logse packing (z - 0.
4t q
Thus, for molten iron-there exist~twa short-range struc 'tureel d&Wionally denoted -
by 4" (z - 8) and 11-y" (z - 12) (cf* Fig. I again). An, onalysia of the findings on
21 metals -gives reason to believe that.the following two tendencies for structure-
-formation exist in mol en megals: 1) preservation of directional bonds conditioned
by the overlapping of p9 or d orbitals (a ftf 8); 2) complete spherical sumetry of
the atoms (z %~:t 12). The intermediate values of z apparently are conditioned either by
the thermal expansion of the melt or by the partial preservation of directional bonds*
Orig. art. has: 5 figures, 1 table,_8 formulas,:_- __7
SUB CODE,t 11, 20/ SUBM D&TS: l4jun65/ ORIG REP: 010! OTH REF.- 002
L-99rd 3/3
7--iUU 4"T TRNFt-'M,
T~
15255-66 'En(m)/EPF(n)-2/T/1~qP(tgEN IJP(C) ID %1i
5/ oj~
ACC NR: AP 027841D UR/0026/65 (0085/0087
5
iAUTHOR: Fili~po:v,'Ye. S.; Samarin, A. (Corresponding member AN SSS*~.
ORG: Institute of Metallurgy im. A. A. Baykoy (Institut metallu'rgil)
TITLE: An. estimated phort ram older strugture in liquid binary metal alloys
1965, 85-87
SOURCk: AN SSSR. Doklady, v. 165, no. 1,
1 TOPIC TAG&- liquid naetal, ir6n alloy grain structure
Is quitew
ABSTRACT: -Whereas -theJocal order.- structure of.pure- i-11 known,
this is 'not the case with liquid alloys.:, However, the coordination number characterizing
the local order of atoms may be estimated, as in the case of liquid metals, from the
temperature dependence of the liquid tdloy density. The present analysis to carried out
on the basis of data pul?Hshed earlier. It is summarized in Fig. 1. Elements which
widen or stabilize the A or d' regions of solid iron solutions stabilize in liquid solutions
the local order structures > (Coordination number t- 8) and (a. n.
respectively. Orig. art. has: 3 figures.
SUB CODE: 11 SUBM DATE: - - 14Jun65 ORIG REF: 006
Card 1/2 UDC; 669.14:669.15
15255-66
-'ACC NR; APS027840
Fig. I., - The determination of the short
Irange'order structures of liquid-all
oys 41
-of Iron. Compl4o'otabilization .40 >~.
of the locaIA)rder structurei -a Fe -Cr
~Fe_Aj.
Fe~M - e 6~
b, Fe-Si; d
Fe-V; f - Fe-S. :C.otnp eto at ili.zation
I 01b
of the > structure: g - Fe-PT;
6Q
RA
-V
Unit for the ramote control of.fuel-distribution pumps Tram
i khran, nafti i nefteprod. no.51,18-20 165. (MI4 lg:lo5*
1. Proyektno-konatruktorskoye byuro Volgo-Ilyatakogo so-weta
narodnogo khoz),aystva.
Kl
FILIPPOV, Yu.
Yor a unified procedure in 4isability a;valuation. Okh.truda I.
sots.strakh* no.1:58 Ja 160* (MIRA 13:5)
1. DDverennyy vrach Tullekogo obleovprofa.
(Tula-Disabilfty evaluation)
~ 1-L7, -~ -,
1: -T~ 4~-
1
FILIPPO7, Yu.,inzh.
man at he blast farnace. Izobr.i rate. no.10:14-16 o,6o.(miiu i3tio)
1. Zavod "Serp i molot",".
(Blast furnaces)
T~=~,Mm Mom
KT
BUKKAN M.; FILIPPOV, Yu.~; TARASOVA., I., inzh.
Wd assembly of-large-panal buildings. Zhil. stroi. no.12:
13-15 162. (HIRA 16:1)
L Giavnyy inzh. SU Montuhshilstroy tresta AltaysvinotBatroy
(for Bul~~O. 2. kachallnik"ekspe-rimantalino-konstruktorskogo
otdala SU Montazhzhilstroy -trestd AltayBvinetastroy(for Filippov).
Wat'-Kamenogorsk-Apartment houses)
(Frecait concrete construction)
E C ( k2 /T/E 1,'4!Pk i
7M (e) /ETTW,~I-
ACC 12V7'ffM 9
71% AP6U_
SOURCE CODE
~AUTHOR; -Filippov, u. ~Engineer)
ORG, none
TITLE; Lasers
SOURCE: VDNKh SSSR. 1nformatsionn byulleten, no. 4, 1966, 7-9
Yy
TOPIC TAGS:- laser, solid state laseri siwiconductor laser, medical laser
ABSTRACT: A.review is presented of several types of"Soviet solid-state lasers wLth
liquid oxygen.(90K) or liquid neon (20K),cooling. Emission powers of the ordet, of
units of watts were obtained in the cw mode. Pulses.with several.gigawatta of
power with a duration of several secondsMire obtained with a..r!Lby,,rraser (beam diver-
gence approximately 0.5*.). . Lasers whoije,'active medium A glass doped -with rare-'.
earth elements ire advantageous inthat any form can be given to the glass and the
active medium can have the proper di r, nsions for obtaining optimum efficiency. BOrium
glass doped with &rivalent neoYAiu6 is one of the most suitable. 'Emission was ob-
tained at 10,200 A in lithiu.m-~magni?sium-s,.Iumino-silic:ate glass doped withjtterbium;
___lasers usin- laments ~containing
atoms of europium as the active medium. The laser was pumped by an ultraviolet
flash bulb. The activ a medium of plastic* lasers can be in the form of.rods or,iv,
Card 1/2
-&--- ; W, -, -. 1, - -, -.: . , - ~ ~ 4 ., , .
"- - ~,- "Vi jgg~~l "o, ;, , I
: , , - 'j -, ~~, , " : -
:... I' A 'iR:--%,'t , - ;~ ':
- -, -, zK, ~R!4M1 - , --. -. - e . .-. .
i - , V - - ~
. , r~ , ? ~;PW P~ Wrll - .. . , - I
IYL'V,' VasiliyYIAdimiioiicI(; GUYNER. Leonid Karlovich, NOVIMY,
Solomon Mikhaylovich; MAKAROVA, Nina Arkedlyevna; STUKAIA)VA, Antonina
Ivanovw, TABASOV,Viktor Konstantinovich, FILITPMjurIy-.AI*"ndre-----
vich- PMOVA, T.G.; APANABOYEV. V.V., reC.;-CABRoDINA, A.A., tekbne
red.
[High-frequency switches; training tables) Kommutatsionnys apparaty
vyiokogo napriazhenita; uchebrqe tablitay. Mosk-va, Gos. ene rg. izd-
VO, 1957. 43 p, and 15 plates (in portfolio) (MIRA 11:3)
(Electric zwit~hgear)
AFINOGENOV., L.P.; BAKAL,, Me!.~ILIP~~ YU.A.
Milliken vacuum capacitor4 'Part 2, Radlotekh. I e1ektron-6
n0.4:642-.648 Ap 161. (MIRA 1-40)
(Electric capacitors)
21-2LIOD 32010
S/089/62/012/001/013/019
B102/B138
AUTHORS: Druskina, L. S., Dmitriyeva, T. G. , allgRgy. Yu. A.
TITLE: Improvements in the photographic method of personnel
monitoring
PERIODICAL: Atomnaya energiya, v. 1.2, no. 1, 1962, 57-58
TEXT: The possibilities of extending the range of applicability of the
photographic method of radiation monitoring was studied, using films of the
type Pelffre4 XX (Rentgen XX) with sensitivity of 25-30 reciprocal r.
This type has a lower limit of - 0-05 r, which corresponds to three days
maximum permissible dose,, and an upper limit of 2.5-3 r. Attempts were
made to extend this range in both directions by chemical intensifying and
thinning the negatives with the aim of changing the optical density, first
of the previously exposed and then of the developed X-ray films. The films
were exposed to Ra 228 radiation and developed in metol-hydroquinone. The
darkened film was then treated with a proportional clearing agent:
potassium ferrocyanide with sodium thiasulfate. Density was measured with
a photoelectrioal densitometer 03-10 (DYE-10) in dependence on the
Card 1/2
32010
3/089/62/012/001/013/019
Improvements in the photographic ... B102/B138
irradiation dose. The measurements were plotted for different concentra-
tions of potassium ferrocyanide: 50, 25, 50 and 50 9/1 and 9, 18, 18 and
27 min, respectively. Before clearing the darkening-versus-dose curve
was so steep that accurate measuring was only possible up to 2.5 r. After
clearing, the curves were bent, so that Etccuracy could be extended to
50 r. A concentration of 50 9--/l (27 min) was found to be bests
The negatives were intensified in quinone thiosulfate. From the
darkening-versus-dose curves it can be seen that intensification shifts
the lower limit to -0.01 r. For clearirg and intensification the films
must lie uniform and have received similar photographic pretreatment.
There are 2 figures, 1 table, and 2 Soviet references.
Card 2/2
FILIPPOV, Yu.A.
Milliken vacuum capacitor. Part 3. Radlotekh. J. elaktron. 8
no.8tl466-1470 Ag 063. (MIRA 16s8)
(Condensers (Electricity))
ACCESSION NR: AP4013.5h2 S/0181/64/006/002/0649/0650
AUTHOR: Fil ov, Yus A.
TITLE: Statistics of secondary ele6tron emission of glass
SOURCE. Fizika tvardogo telai ve- 6, no* 2) 1964.. 649-65o
TOPIC TAGS: electron emission, silicate glass,, MIllikan vacuum capacitor,, secon-
dary electron emission coefficient, Poisson formiiLa
ABSTRACT: The emission characteristics 01%
silicate glass were investigated.,
using a Millikan vacuum capacitor* Tho glass, in the form of fine spheres
obtained by blowing FXound glass through a gas flame, was placed in an e3ectrostat-I
ic injector (a chamber directly beneath the botton plate of the capacitor). A
voltage pulse of "p to 7 kv and several railliseconds long applied to the injector
introduced the glass particles into the capacittor., Measuremonts were made for
three values of priptary electron energy: 100, 3'C),, acid 500 ev. The 350-ev energy
is approximately that corresponding to the maximal value of the secondary electron
omission coefficient (sooo), The data woro plottcd tomethor with tho probability
distributions from the Poisson. formula for the particular values of seec. The
Card 1/2
oassio NR: AM13542
author thanks L. No Dobretsov for his guidance. Orig. art. hast 1 diagrame,
ASSOCIATION.- Fiziko-tekhnicheskiy institut imeni A. F. loffe M SSSR Leningrad
(Physical and Technical Institute AN SSSR)
SUBMTED: .12Dec63 DATE ACQ: 03,viar64'14 EXCL: 00
SUB CODE: PH NO REF SOV: 003 OTHM: 000
KOROBOCHKI21, B.I.; FILIPPOV, Yu.A.; DITKIN, V.A.v profop otv* red.;
ORIMA , -1717"w"
,, -
[Tables of modified Whittaker functions) Tablitsy modifitsi-
4
rovanriykh funktsli Uittekera. Moskv&, Vyshisliteltnyi tsentr
AN SSSR, 1965. 321 P. IMIRA 180)
-:L-2~5474-77.:- -EWT(1)/EWi(M)
ACC NR: AP6009678 SOURCE CODE: UP/018jX/OW003/0877/0882
YU
AUTHOM Lig A,
loffe AN SSSR, Le ibo-
ORG:, sicotechni al Ins e-im. A& Fo~
tekhnicheskiy institut AN SSSR3
TITLE: Statistics of secondary electron enissioa of4aLckel and _jMrj_
& no. 3; 196
SOURCE: Fizika tverdogo, te3Ap.v 6:8TT 882 ldl
TAGS: secondary electron emilisionj Iron, statistic analyaiv# electron
nattering
ABSTRAM. The author investigated the statistics of pecondary electron emission froi
particles of nickel and iron susp'ended in the electric field in vacuumj, using, a
method described by him earlier.(Radiotekhn..i elektron. v. 8p - 1466, 1963). 7he ex-
periments. consisted of irradiating the particleivith a weak beam of electraneLfremL
a-gun and determining the net charge of-the ouslension.by measuring the-ci%rrent.it
produces in a capacitor..' 'The reaultS of the experiments have SholM.that at low L
primary-electron energies the secondary electronemIssion obeys Poisson-law statis-
ties but deviates from the latter with Increasirig energy. This deviation i6 attri---,
buted to scattering of the primary -electronaLby:the target material. An approxjxate.- :4
is derived for the secondarya. emission 1wobability, distribution to.fit the
experimental data, *The author thanks the supezirisor of this work L. N, Dobretagy;Jor
continuous.interest and valuable hints. Orig. ewt, 'has 5 figures -and 10 fOrMIAS. A,
20/ BUM IATE
SUB CODE.- O6Aug65/ MIG WW: 0091 OM REF: 006
C. d
SOV/109-59-4-2-10/27
AUTHOR:
TITIE: Amplification of the Space--Charge Waves in an Electron
Beam Moving With a Veriablet Velocity Along the Channels
in a Lossy Medium (Usileniye voln plotnosti zaryada pri
dvizhenii puchka elexuronoir a peremennoy skorostlyu
po kanalam v srede, obladayushchey omicheskimi poteryami)
PE,RIODICAL:Radiotekhnika i Elektronika, 1959,--~Vo'l 4, Nr 2,
(Uso 13 N
pp 228-232 QXLJ
ABSTRACT: An electron beam, having a variable velocity vo(x),
passes through a medium whose conductivity is o and
permittivity s. 'The aleCt3?ons are assumed to be
moving along channels having small transverse cross
sections. The parameters e, ~i and a and the medium are
constant. The~convection ourrent (Ref 5) is given by:
I = IS + dE
where is is the electron beam current density, while the
other component denotes the, induced current density;
'r is the electric field vector. If the problem is
assumed to be imidimensional, the--following equations
Card 1/4
SOV/109-59--4-2-10/27
Amplification of the Space.-Charge Waves in an Electron Beam Movivg
With a Variable Velocity Along the Channels in a Lossy Medium
have to be solved:
.dv +., dv e (2)
aT aR E
dis + dns 0
U 7
dE- 4)T (is + cE) (3)
TE ~-- - 6
If v and n are a~prox:imated by Eq (4) then Eq (3) can be
written as Eq (5 where Z(.x) is defined by Eq (6) and (7).
.If the velocity is an exponential function of x, Eq (5)
can be written as Eq (8). Consequently the expression
for is(x) which satisfies Eq (6) and (85 and the
boundary conditions of Eq (9), is given by Eq (10).
If a = o and c4- = o, this is in the foim of Eq (11)9
which is similar to the expressions given by-Rydbeck
Card 2/4 (Ref 6 and 7) and by Birdsall (Ref 4 and 5).
SOV/109-59-47g-10/27
Amplification of the Space-Charge Waves in an Electron Beam Moving
with a Variable Velocity Along the C,'iu=els in a Lossy Medium
The amplification of the system at the output, that is
for x = f,, is defined by'.Eq (12). If the modulus of the
amplification coefficient is denoted by p and its
argument by q2 the values of p and q can be found for
various special cases. In articular for 0 ~> 1,
p and q are given by Eq (163 and (17) respectively,19).
while f or c~, = o, p and q. are given by Eq (18) or
The dependence of p on frequency, the conduc-civity uf
the medium and the delay coefficient of the electron
beam is illustrated in the figures a. 6 and b on
page 232. The gTaphs were evaluated for s - 1
go = 17
0.15, uo = 4.05 :i 109 cm/seCl .2 X' 109/sec7l
and p0 = 1. The author expresses his gratitude to
Card 3/4
SOV/109-59-4-2-10/27
Amplification of the Space-Charge Waves in an Electron Beam Moving
With a Variable Velocity Along the Ohannels in a Lossy Medium
Professor V.L.Geiman for discussing the problem.
There is 1 figure and 8 references of which 2 are Soviet,
English and. .1 French.
ASSOCIATIOIT:Institut RadAfiziki i Elektroniki AN,USSR (Institute
of Radio Physics and.Electronics of the,AS UkrSSR)
SU~IqITTED: 23rd May 1957
Card 4/4
N,
M.
SOV/109-59-4-2-11/27
AUTHOR: :11~lippovj YU-F.
TITLE: Motion of an Electron BOam, Having a Periodically
Varying Velocity Along the Ohannels in a lossy Medium
(Dvizheniye puchka elekf;ronov s periodicheski
menyayushcheysya skorostlyu. po kanalam v srede,
obladayushchey omicheskimi poteryami)
PERIODICAL:Radiotekhaika i Elektro;aika, 1959, Vol 4, Nr 2,
pp 233-240 (USSR)
ABSTRACT: This work can be regarded as an extension and
continuation of the author's preceding article (see the
present issue of the Journal pp 228-232). Again, it is
assumed that the medium is lossy and that the electrons
move along the channels having small tran'sverse
dimensions. The election velocities are periodic
functions of the co-ordinates. It is also assumed that
the signals are comparatively small. and that the
problem is, therefore, unidimenaional. If the thermal
velocities of 'the electrons can be neglected, the
problem can be solved by employing the differential
Card 1/5
SOV/109-59-4-2-11/27
Motion of-an Electron Beam HavinE; a Periodically Varying Velocity
Along the Channels in a Lossy Medium
e q:aat ion: v_0 Sa2
ouo
Z11W - [j(vv) j _- I W = 0 (1)
VO VO vNi -- i-Q;r
0
where Z(x) is defined by 'the second eauation on -o 23~
If the change in the beam velocity Is periodic, as def ned by
Eq (2)2 Eq (1) can 'be written as Eq (3). In the region
where 0-1, Eq (3) can be solved approximately and its
solution is given by.Eq (4), where U and, V are defined
by Eq (5); the constants C, and C2 can be found from the
boundary conditions. The amplification coefficient of
the system is defined. by Eq (7), which for the case of
the boundary conditions expressed by Eq (6)t is in the
form of Eq (8). The solution of Eq (3) can be also in
the form of a modulated travelling wave, as expressed
by Eq (14), where f (3r.) is a periodic function which is
given by Eq (15). The condition of existence of this.
type of solution is expressed by the scattering matrix
Card 2/5 given by Eq (16). If the thermal velocities vT and
SOV/109-59-4-2-11/27
Motion of an Electron Beam Having a Periodically Varying Velocity
Along the Channels in a Lossy bledium.
the electrons are taken into account, the system is
described by Eq (22). This can be written as Eq (23),
which is similar to Eq (3) except that 0 is replaced.
by 01 and h is replaced by hi, The problem can also be
analysed by employl-ag the MaRviell equations and the
kinetic equation of the system and finding their
simultaneous solution. In this case, the electron beam
is assumed. to be propagating in a cylindrical waveguide
and the system is represented by Eq (26), where v is
the velocity of the electron beam, F is the distribution
function for the beam and cro is the potential of an
external stationaiV- field. 'The scattering equation of
the system can be obtained by employing the method
described. in Ref ?. The final formula is then in the
form of Eq (2?)~ where 20 is the plasma frequency,
kl is a quantity to be deteimined from the boundary
conditions at the walls of the waveguide, n = 41ja/aw
and p0 is thd propagation constant at q = o. If it is
assumed that the v-cLlues of pO are given by Eq (29), the
Card 3/5 amplification coefficients X can be expressed by
SOV/109-59-4-2-11/27
Motion of an Electron Beam Having a Periodically Varying Velocity
Along the Channels in a-Lossy Medium
Eq (30) and. (31). From these, it follows that the
presence of the thermal electron velocities does not
interfere with the generation and amplification of
high-frequeney sigaals for q = 0. The effect of the
periodic velocity variation, that is q