SCIENTIFIC ABSTRACT AVERYANOV, A. G. - AVERYANOV, S. F.
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Deep oeismic sounding...
22423
S/Oz-,0/61/000/002/001/012
D2427001
Kurillskoy ostrovnoy dugi i prilegayushchikh uchastkov Tikhogo
okeana podannym glubinnop seysmicheskogo zondirovaniya (Some
Results of the Study of Crustal Structure in the Kurile Island
Are and Adjoining Parts of the Pacific Ocean from the Data of
Deep Seismic Sounding) Izv. AN SSSR, ser. geol., No. 1, 1961)
has
already indicated that the.crust is of the..continental type-,
In
the continental-type.hodographs the arrival times of the PO, P*
and P.waves are at a maximum, the transit time of the P waves
being 18 - 19 sec. There are two forms of hodograph; one repre-
sents-a three-layer crust.(sediments - 'granite'-'basalt') for
the region near Kamchatka and Sakhalin, while the other corres-
ponds to a granite.crust (with local basalt layers) in the
north
of -the: Okhotsk Sea. Ac*cording to,the velocity-depth curves
the
continental -type crust, whose thickness throughout the study
area
may vary from 20 to 30 kai, includes thick or thin sedimentary
layers. Oceanic-type hod.ographs cover areas approximately out-
lined by the 5 Ian isobath. The arrival time of the P* and P
waves
Card 6/11
S/04 9/61/000/00 2/00 1/0 1:2,
Deep seismic sounding... P242/D:501 V~O-
r
Fig. 9. e.C' dy--
Principal
hodo;-,;raph
types. is-
1-continental
2-oce anic 4,P-'O P
3-in-temediate -a 0 CN
striations
-m areas
deno
where there
are different
t-y~.)ea of hodo- A
graph waves;
Type 3. charac,
teri::ts hodo-
graphs for the
B
ring and
e
Okhotsk Seas 0"
P~
Ca:rd 9A1 753 /117. '01
...
Dclep seismic sounding...
22423
S/049/61/000/002/001/ol.;?
D242/D.301
is at a minimum and t~e transit t'iMe' for. the latter waves is
1' 14 sec. The presenctt bf a thin basal:t crust'with a
thickness
02 about 5 - 12 Ian may be inf erred f rqm. the observational
data.
The intermcdiate-type-b.odographs are representative of the
south..
ern part of the Okhotsk Sea and the neighborhood of~ the
Komandor-
sliiyc Islands. They art! distinguished by, the existence of V*
and.
P waves and by the large area in which waves of the first type
w0re recorded; the tranait time of the P waves is 15 - 17 sec.
The velocity-depth curves rdsemble those for the continental-
type
czvs-L in abyssal parts of the Okhotsk Sea, where the sediment
thickness appears to be considerable,.and those for the oceanic-
type crust in the Ber~ng Sea. The authors cone]: ude by stating
that a-composite interpretation of the data of deep seismic
sounding and of gravimetric, acromagnetic and'geologic observa-
tiona in this region will be made subsequently which may
possibly
expose the patterns of development of crustal atructure and also
clarify the conditions and sequence of transition from one type
Card 10/11
2 242 W-A
S/049/61/000/002/001/012
D242/D301
Deep oeismic sounding...
of crustal structure to another. In addition, they emphasize
the
desirability of comparing.their data with those from other
global
zones.- There are 13 figiares and 12 references: 10 Soviet-bloc
and 2 noni.-Soviet-blac.. The references to the
EngLisli-language
publications read.as foll.ows:.R. W. Reitt - Seismic-rcfraction
studies of the Pacific Ocean Basin, p. 1. Crustal thickness of
the ceintral.equatorial-Peicific, Bull. Geol..Soc. Amer., 67,
No.12,
1956; M. Talwani, G. H. Sutton and J. L. Worzel - A crustal
section
acroas-the Puerto Rico Trench, J. Geophys. Roes., 64, No. 10,
1959.
ASSOCIATION: Akademiya n.auk SSSR, instit-ut fizikJ' zemli
(Institute
of Physics of the Earth, AS USSR)
SUBMITED: July 24, 1960
Card 11/11.
-0 F,,,YT (i)/nre--AFFTc/EsD--~3-TF
ACCE; BSION NR: Ap3owcO s/oo4,o/6:5/ooo/orI)6/o33q/o
AiMOR: XvaMn,- ~--; -Am nQv. A. -G--
TIM, : Seismic wave modeliag vith two-dimonsional perfol.,ated nc-dels in
layered
nonh=oaeneous vxdia
SOUXM: A14 SSSR. Izv. Ser. j-,eofizicheskayza, no. 6, 196:), 83-ol-5-o6
TOM . TAGS: - neismic. modelirig, -two-diT-ensional perforatcd -model-I -
saismic
wave propaGation
\7'
MSTIMM Experiments modeling ha-ve beert carrica out on
tn-dimensional perforaterl iro6els of nonhomo,geneous, laycred-homo,-encous, ana
1;%ye:.,cd-nonho-,.oGcneous mcdbk. Wo-dirnnsional inotlels for ronhonDgeneo,.~-,
vitre designed oyi the basis tDf the exTeri-mentally derived zelatioiship
'cctween
wave velocity and. the diarve-ter of the holes cut in a 2-=i durabxAn ~;Ihcet
forialng
a tr4.~,,uigular grid. In modeling a horiogencouD half-spnee i~, was fourd tbat
thl.
dIve','Gence ftn-ation inclex n for a direct lDn(,,itvtUnal wave P va-.-icd
'bot-wreen 0.5
wid :,-5 vhen zz)urcv nnd rec(tiver wre loc--ated on a fr--e in the t.,Ir,!c..
dj,r2llsional Mofte.1, this wo,.11d corresponel to a variatioz, of n frz:!.-.1
I to 21. 7i-,
Card
L ICIAG-63
ACCE:SSION IvRs. AP3002023
attemun-tion patterns of head. and refractcd waves varied; the hend
waves sbcved
Tapl,d attenuat.ion, and the refracted vaves attenuated rather
alowly with in-
creexin,g, disUice even at srall velocity gradients. To (>vcrco-,c!
the n-- Sc -
lutton of waves cauacd by lonj~-period oscillatIons, it ii; sugf
sted '.h-- vi -,
I t~e n. dc
'rand trnnsducers be devolopM which would produce a pulse ran~;in-
fron 2 to 20
u
microseconds. Orig. art. ',iExs: 16 fipgures, 4 tables, and 8
forz:lulas.
ASSMIATION: Akadermiya nauk SSSR. Inst-itut fiziki Zemll!. !:caderw
ot Sciencep
A
=1- Insti th
SUBM D: OTAug62 DAME ACQ: 16jul63 EITL: 00
SUB COW: 00 NO M. F SOV: Oll OTIM-R: 000
li, 1 1 k-A 'k,
j0mde-n, Lya nAu), SSSR. Inotitut flziki zc.,all im. 0. lu. 511imilta
q,-opieb printad. Rasponnible editorvi 1. Gallperin, 1. P. Kosm-Inskayal
Rdilor of the piblinhInp ho:)iiai S. Ilz r, -,:p k 1.7 1 T tnc 'in 17,11
c~ d I t or Li T a V
ILR)( I , I . 3 .~ . , . o I -.c.. ~ r- .,IV A
a-P 97 A 07S -,n r fnrri 3 C5~ 7je ', -.I f~ -~, T~ j7 m F,,R 0
icii I
rear, ocesn, s6ismic wnvB
PU RPOS! MxTD If' iNg Inv )V, 19 -Tibis mo-Mr-.-Mr)b iB dffVCII-E'd
qtL)r',IAA 11V A&
a Dn ine n i t
r, 6raA n K.Q m.- h~ t L, Ia
I-V e s, I
tlf ividual chaptara, althouili n1l are davoto-%d to a ainRlo probler-3
urld am
Card V4
~Z
LP
L~ Liii t z 1 A i'~ '~o
I I I i I t..,$ r
. I ~ ,
A, . ,-
,; 1~ -'i P, ! F's
alTmil 020
t
" " I x
Eli
OLMV, Nikolav Mikha7lovi,:h,- AVIRI TANOV I AWN
redaktoz; PXRMINOV, S.V.,
radaktor; GINULDOYBU, %8KnnICnOGKi7 redaktor
[Storage of petroleun, petroleum products aid gas]
Khranente nafti,
nefteproduktov i gwine Leningrad, Goo. nauchno-takchn.
tad-vo neftiancil
i gorno-toplivnol 1-Lt-r7, 1954. 617 p. (MLRA 8:4)
(Petiroleum-4horage) (Petroleum products--Storage)
(Gas. Natura:.L--Storage)
AVE11TANOV, A.G.
Necessity of reduchA: air samples from industrial
'buildings to the
average level@ Gig@ I sane 21 no.9:93 S 156. (MIRA
9910)
(AIR--ANALYSIS;)
A13RITANOV, A.G.; GRIMITLIII, M.I.
Dust collectors used in surface grinding. Stan.i
Instr. 28 no.4:
18-39 Ap 157. (KLRA 10:5)
(Dast collectors) (Grinding and polishing)
i,.r nit ljrtriAl p-n-niren !'('11itted Ify several
k HAT
1 1: V'I ~k t
AVEROYMOV. Aloksay Grigorlyevioh; GRINITIM, Rikhail
:[osifovich, IOFIRDT.
Germn Abramovich; r=OV, Petr Arkad'yevich, ILLITZOM, Taygemly
Kiprmiolij XLTACHKO, L.S., )atnd. tekhn. nauk, ipets. red.;
RAKUrt
I S, 1,, takhri, red,
[Angineering practices In studying ventilation installations
in
industry] Nauohno-takhnioheskii opyt issledovwdia
ventiliatsiannVkh
ustanovok v pronWiblennosti. [Moskva] 1zd-vo VTsM Profizdat,
1909'
165 P. (KIRA 1117)
(Yaotories-Hoating and ventilation)
TIMOFEYEVAp Oltga Nikolayeirna; BLITMM., Yovgoniy
Mikhtyloviob;
IOFINOV, German Abramovich; AMrfANOV,_A.G._t
s~petsred*;
DENISOVAj I.S,, red.; KOROLO'fA7V--N-.b-.V-
ek6-.iid-.j
(local exhaust ventilation in electric welding
ohops)
Mestmia vytiathnaia ventiliatniia pri
elektroinrarocbMkh
rabotakhs Mookup Profisdatj, 1961, 139 pe (KEPA 150)
Electric welding-Safety meavurea)
Motories-Haating and ventilation)
AVERIYANOV, A.G., kand.toklin.nauk; ELITMIAN, Ye.M.,,
k&md.tekhn,.nauk; VEKSMI,
G.S.,, inzh.
Results of the investigation of ventilating sys'~ems for
the brush
painting of compartmentao Sudostroenie 28 no-5::51-55 MY
'62.
(Ships-Painting) (MIRA 15:7)
,~WRRITANOV, A.P.; STAKOM:IT, A.Te., red.; KOVSHOVA, O.H.,
red.izd-va;
, 0.6.0 taklm.red,
[Model of the A-1 glider] Modell planer& A-1. Nahkva. X-vo
kulltury RSFSR. Isd-vo 'IDetsidi air", 1959. 1 fold. (Pri-
lozhenle k shurnalit OlUnyi tekhnik," no-709))
(miRA 14a)
1. TSentrallneya stantsiya iunykh takhnikov, Noccow.
(Gliders (Aeronautics)--Kodels)
. I ; . , .1 ; I - , I I , - * . . ~ I I . " . . , I ~ I ~ I I '- - - I . - " , :
- z . . . I I .
I I
AVIMITANOV, B.
On a return vielt. Sov.profsoiusy 4 no.8:85-87 Ag 056.(MLRA 9:10)
(Scotland--Relat Ions (General) with Russia) (Ruvela-Relat tons (Genne-
ral) with ScotlFmd)
AVER'YANOV, B.
Sidestepping vital. problems. Sov. profsoiuzy 18
no.21:43-41, N '&!. (NIRA 15:11)
1. Zavoduyusheldy mezhdunarodnym,otdo1om
Vsosciyuznogo
tsontrallno o soveta professioriallnykh soyuzov,
fGroat Britain--Trade unions-Congrcissas)
AMIYANOV, G.B.
A simple transformer of a single-phase current in,:o a
three-phase
current. Politekh.obuch. no.11:75-76 N 157. (MIRA
10:10)
(Electric transformers)
AVIR'YANOV. G.B. (g. Kirovogmd)
Three-phase generatora used for&wnstrations. Politakhocibuch,
no.io:47-48 0 1511. (MIRA lifil)
(Blectric gerieratore-Design and construction)
AVERIYANOV, G,B.
Two devices for the subject "Atomic structure"~ Fiz.,r
shkole 20
no.1:78-80 JA-F 'El. (MIRA 14:10)
1. 27-ya arednyaya ohkola., Kirovograd.
(Nuclear physics---Study and teaching)
AVEEIYANOV, G.P.; GAVRILOV, N.,M.; SHALINCA-, i.l.'.
Des:gn relationsh- ps for a double-helix wave gu~.de.
Usicorritell. r:o.;,:
92-CA) '64. (!.IlTjt 18:2)
HIMITANDV G.V. (g. Kirovograd, USSR).
Demonstration model of the asynchronous motor ani~
electric
motor. Fis. v shkolo 16 no.6:53-54 N-D 156. (MM %12)
(Blectric motors, Induction)
(Zlectric meterm)
"IliAMANOV, 1.
-1,
AV'-"H'YANOV, 1. C.: "On Irmrularities in the operati,n, c7
tunriel cume
coversoll 'jin jlivljo~r !-,jacition USSR. Moscow Inst of
Chemical -Iachine JuildinF. :,'ios(!owp 1956.
(JissertatJon for the Dac,re~, of Canci,iate in Scienc~.s)
Technical
Sco: Knizhnaya Letopis', No. 18,, 19~6
v c- q, ytl N 0 \/, I - C--,-
Pon I POK 1"WITArm WV/3922
V#,7WdnO, Ivu Petravichp lysin Orlprlyevich Averlyarx"s
Vladiuir Sevemvich
Qxrokhor,v Anatolly Widmimovich Gorshkow, Mi-en-a"'mAl'yevich
Zakhanwt,
&A likola), Uspawich'relxMin
Hasbiny i apperaty ustanmik r"delenlys Yoz&Wa metodam glubokoV
othlesMeirlys;
titles kons-truktsiy (Machinery and Apparatus for Air
Separation by Low-Tempirstare
Refrigerationj Atlas of Designs) Xoscowt Xmsbgizp 1569. 189 p,
Irrate, slip
Inserted. 5,,000 copies printed.
Zd.* I.P. VtjyWcin,, Doctor of Technical Sciencest, ftofe-ssor;
Revievers: I.K.
i0 r., Candidate of Technical Science9j, and M.P, Ulkov.0
Doctor of
Technical Sciences, ft)fessor; Ede.: PX lonov; ftgineer, B.N.
Bol'shabyr,
an& W.B. Usperevich; Managing Zd. for Catalogs and Alb=s: K,A.
Ponomwevn,,
lr4o.werj Tech. Bd.: A.14. Tikhanar.
PURPOM Tlds atlas is intenAed as a design marmal far students
of schools of
higher ttichnidal education, and can be used by planning and
design offlems and
scientifte research iiistitutes in the stmv of problem of
low-temperatur?
refrigerst--on and the use of orMn as a wants of raising
inftstrial ont-pat.
Card-a-42
10(2) '
SOV/64-59-3-14/24
A17711,01ISt
Averlyanov I. G. ,
Candidate of Technical Sciences,
.' I -- '
-
-
~
ikaelrr
o
,L. S., Candidate of Technical Sciences
TITLEt
Conditions for
Regular Work with Cupola Bottoms
(Unloviya ravnomernoy raboty
kolpachkovykh tarelok)
PERIODICAM
Hbimicheskaya
promyshlennostil 1959P Hr 3v PP 64-79 (USSR)
ABSTRACTz
In
recent times several papers on the conditions necessary for
a
regular effervescence in columns with bottoms have been
examined (Refs 1-5, 8-12), and among other things it is
stated
that an increase of the gas supply changes the
irregular
offervegeence into a regular one by using the whole
bottom
area, The investigation results are given with regard
to the
reasons for an irregular action of cupola bottoms and
the
conditions for a regular effervescence vhich took place
in the
air - water oystem. The experiments were carried out
on a urtit
specially devigned, where canal bottoms (CB) and
bottoms with
round cupolav (BC) were examined, as well as
(CB) of a
fraotioning (solumn for pyrogaaes deaignc-d
according to the
standards of the NIIkhimmash (Ref 6). lit
the case of the (PC)
Card 1/2
the experiments proved that the
observal;ions described in
Cisuditlone for Regular Work with Cupola Bottoms
SOV/64-59-3-14/24
publications (Refs 10-12) Nero right, in the case of the (CB)
a different character of irregularity wNa observed. A sketch
of a (CB) is given (Fig 3) and the ooourring irregular
effervescence is explained by this sket*h. An analogy is
stated between the character of the function of the relative
specific weight of the gas emulsion, the speed of the gas
stream and the height of the liquid layer in (BC) and the grid
bottoms. The derivation of the equation (15) is given for
em ting the gas speed at which a regular eff ervescence of the
(BClain Initiated. Together with the explanations of the
reasons
for an irregular effervescence an the b3ttome it is mentiomed
that the supposition (Refs 10-12) of &,promoted overrunning to
wrong. Finally some calculation examples and the corresponding
data are given by means of a (CB) of a -water cooling scrubber
f the oxygen plant BR-5, There are 8 figures and 12 refer.
:
ncest 9 of 'which &re Soviet.
CILrd 2/2
WYUKIN~ I,P.; A P-444,; UVAIIOVA, A.P.; Prinimali
ucbwtiyv.-
DOLG A.A.; C LEFKOVA, A.A.
Continuous method of the production of ammonium
bicarbonate
Khim.prom. no,10:ir23-728 0 162* (RIRA 15:12i
(Amoniumcarbonate)
AVBRITANOV, I.I., insh.
' Industrial methods of produaing sanitary engineering
fittings.
Tr&nop. strot. 8 no,9:17 1 S 158. OaRk 11:10)
- 3
ipe
R
AVERIYANOV, I.I.
Construction of preftbricated reinforced concrete wator
towers.
Vod. i. son. tekh, no.1:5- ja 'Al. (MIRA 1419)
?Water towers)
v
AVEWYANOV, I.-I-.-,-.inzh.
Joinivir 4.11in vipeq :In sanitary enpinevrinF
operstiont. knt. i
!; P.. t I 'I . (MIRA 14:10)
.F. rab. v stro'A. 23 no.10:2-5-26 0
1. Orgtransstroy. N
(Pipe Jointso
2551,0
S/089'/61/011/'005/005/017
C-9 41, B102/P!04
ATITHORS: Serov, V. I., Peroshivkin, V. A., Andreye,~, M. F.,
Averlyanov, I. K.
TITLEt Investigation of the Be9(d,t)Be8 reaction
PSRIODICAL: Atomnaya ener-giya, v. 11, no- 59 1961, 440 - 442
TEXT: The authors measured the diffe 6ential. triton
Froduction cross
section at an angle of emission of 17 and an angular
diatribution betwoon
0 for E" -
0 and 150 1.125 - 3.8 Mev. The deuterons accelerated by an
2
electrostatic generator hit the beryllium target of 100 - 150
jAg/cM which
was placed in the center of a magnetic spectrometer iith
inhomogeneous
field. This spectrometer analyzed the emitted tritons with
energiell lip 1.0
Et - 5.4 Mev. Faster tritons were slowed down by a foil. k
t.~in CvI
cryetal with a photomultiplier served as a particle detector.
A 50-charincil
pulte-height analyzer recc,rded the momentum spectrum of the
particles, The
differential triton production cross section as a furction of
E d showed it
small resonance peak at E d, , 1-37 Mev and a marked or.e at
Ed '2.85 Mev.
Care. 1/3
lnvosti~,mtion of the,
L
295)0
S/Oaq ~61/011/005/' 005/0 17
'41t
B 102~ )4
E
6
Do (n, (0: " C!
B09(p,n)119
Ile9(d,t)Be8
10(a,n)C"
res'
2,6
2,3
2-33
2:75
E
,43
Results indicate that the confilaration
of the compound nuclreus correspondo to
the system "initial excited nuclCUB -& 411-
cident particle". Ttie authors thank
te,". of V. A. Ivanov as well as
V. V. Kuzyanov for aFaistance, There are
5 fi(~,-urerj, 1 table, and 6 references:
1309(p,y)B"
8
1309(d,t)Be
:30(a,n)Cl'
3.14
3.10
3.08
,04
1 Soviet and , non-S)viel. The four no:)l
recent references to
publicntions read its follows: R. Smither.
1'hys. Rev., j_01, 196 (1957); IL'. Ju::ic,
Phys Rev., 98, 85 (1955); R. Heft,
Libby- I'llys,
11,
lZov, ,100, 799 (1955~1 F. Ajzenberg-Selove, T. Lauritser.
No, 1 1 (1959).
!.;-JB:'lTTI:D: "Ay 5, 1(961
d
AVICRITANOVA I.M.
Mineralogy of the processes of beryl alteration.
Mat. po mfr?..
Koll, poluost. 2tV*0-142 162. (MM. 1614)
(Kola Nninvula-Beryl)
AV07.'YfJtOV) I. P.
"Extraction of Construction Sand," Y~,ol!, No. 2, 19h8. Engr.
Construction
of' "Yagunovskoy' Mine., Kemercvo.
t
Air-
4. Coal Fines and Nining
7. Lxperien,.e in fil"inr cave-in3 occurinF d~irin~ minim, !dth
sMe7.12 in winter,
Uf,-ol-' 2", no. 3, 1953-
9. Monthly List of Russian Accessions, Library of Congress, "Irly
1953. Unclassified.
AVIIRITANOV,I.P.
"I"
The quality of bulkheads. Ugol' 30 no.9:38-40 Sl,;5.
(KIRA 8:12)
1. Kusbasspetstrest
(Coal mines and mini W -Safety measures)
AVIRIYAWVI IIP.
Device for catching and removing unwashable
Inpurities
from slurry (hydraulic stone remover). Ugol' 31
n0-1:
39 Ja 156. (KIRA 9:4)
l.Kasbasepetstrest.
(Kuznetsk Basin--H*draulic mining)
LVERMNOV., I.P.
Rocks of the "gro-n tuff" typo in the northeastern pnrt
of Kmachir
Island. Trudy Si_,kh. kompl.nauch.-iss3. List. All S!,SR
no.10:76-82 161.
U"M 15:6)
WwAshir Island-Volcanic ash, tuff., otc.)
U832
S/561)/62/000/011;,'003/011
12 1001,14101
AUTHORS AvQr I tan_oy~_I_. _P., Kaeatkin, A. M., Li.venteov, A.V.s
Markov, M. N.,
Merson, Ya. I., Sliamilev, M. R., Shervirzkiy, V. Ye.
TITUs The measurement of Earth's thermal radiation into space
during the
total eclipse of February 15, 1961, from e4 altitude geophysical
automatic station
SOURCEt Akademiya nauk SSSR. Iskusstvennyye*sputniki Zeimli. no.
14, 1962,
49 - 56
T To improve calculational methods of determinir4; radiation of the
atmollphere at high altitudes, -the study of optical propertios of
its upper
layers, using the measurements of its thermal radiation, is
nec;easary, These
studies have been conduoted in the USSR since 1958 by means of
altitude geophys-
Ical rockets. The article describes one of these experiments
performed during
the total solar eclipse of February.15, 1961, in the middle part
of the Buropean
part of the USSR. The general scheme of the experiment is
:,hown~in Figure I imel
the block-diagram of the device mounted on an alt4tude geoplVeical
automatic.:
Card 1/4
The measurement of Earth' s therTial ...
Figure 1. The scheme of an
experiment
Legend: I - Altitude geo-
physical automatic stationj
2 - rocorder of Earth's
radiation; 3 - area on the
Earth whose radiation is being
measured; 4 - belt of total
eclipse phase; 5 - band of
sca=Lng; 6 lunar umbra.
Card 3/4
SNC/6Z/000/014/003/011
AOOI/AlO1
AYER I y ANOV 1- 1 . p
"Cocarde" formationis in hydrothermally altered rccks in the
central crater of the Eb)ko Volcano. Izv. AN SSSR.Ser. eol. 28
no.5182-88 My 163. IMIRA 17W
1. Sakhalinskiy komplekanyy nauchno-isoledovatellskiy institut
Sibirskogo otdolenlym AN SSSR.
Ak~,-A~IYANOIIJ 1.11.
Sn1fur-containing varJoty of pr pyl.it!ze,~ r
~:ks 1i; Fura-Rushir
Island (Kurile lsl.andEi). Jzv. AN M)I'-
Sor.teol. 29 no. 2 -
101-IM F 164, (M':RA 17: 5)
1. Laboratoriya viilkaiiologii Sakhalinskoro
komp'-whoriogo
instAtkita .1.1ildrskogo WIolezilya
fill SS~',!, Ii
., puselok Novo.-Alokoandrovik, Sakhalin.
hVERIYANOV, I.P.
Alimits of altered rocks in the Vernadskii Range of' Pammushur
Wand (Kitrile Islands). Geol. rud. raestorozh. 7 nc-.2slO2-106
Mr-Ap 165. (MIRA 180)
1. Sakhalinakiy komplO:snyy nauchno-lasledovatel'Aiy institut Sibirgkogo
otdolenipt AN S99R.
I;j p
c;:
S/181/62/004,/006/022/051
B100112
AUTHORS: Baryshov, N. E'.. , # and Aver'yanov, 1. S.
T:TLE: Photoelectric propertivs of tirt4ficial PI~S single
crystals
Fizika tverdol;o tela, v. 4, no. 6, 1962, 11)21)-1526
-AZXT: The photoelectron.~en.,tic -:?ffect and the
phot,-coiiduction of
artificial p- and n-type PbS single crystals with carrier
concentrations
of 8-10 16- 8-10 18 cm-3were investi6ated. The
photoelectromagnetic effect
was measured in fields of up to 15,000 oe, and its temperature
depenience
'was determined by means of a special. cryostat. The
measurements were mado
in liquid nitroeen vaDor. The photoconduction was d6termined
in tile
modulated light (390 cps)' (:f an incandescent lamp (300 vv).
The carrier
lifetime was found to be ict-7-lo-10 sec. For samples with a
carrier
concentration