SCIENTIFIC ABSTRACT PASECHNIK, I. I. - PASECHNIK, M. S.

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• Collection: Scientific Abstracts
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• Release Decision: RIF
• Original Classification: S
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• Document Creation Date: November 2, 2016
• Document Release Date: June 15, 2000
• Sequence Number: 5
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

PASECHNIK, I.I., inzh.
Investigation of stress-deforr-ed blocks of untouched ore in
chamber-mining systems. Izv. vys. ucheb. zav.; gor. zhur.
6 no.9:42-51 '63. (MIRA 17:1)
1. Moskovskiy Institut radioellektroniki I gornoy elektromekhaniki.
Rekomendovana kafedroy vysshey matematiki.

PASECHNIK, I.I.
Choice of D-rm-s3ib--e ~,r,srings ir ch.ri,--t*--r-Rxd pillar r-ining. VeFt.
I
All Kazakh.SSH 11) 0 r, 3. (MIRA 17; 1)

PASECHNIK, I.I.J. starshiy prepodavatell; HYBASOV, V.I., inzh.
Relationship between the shape of a lateral cross se-cf-ion of a
gallery and the state of stress and deformation in the massif.
Izv. vys. uch. zav.; gor. zhur. 5 no.6:22-27 '62. (MIRA 15:9)
1. Moskovskiy gornyy institut. Rekomendovana k&fedroy vysshoy
matematiki.
(Rock pressure)

PASECHNIK. I,. Kr,,
Ef'f-,.' o!' %-,'batn B, (F-p-.joxine) -,n -,r,,- bl-e et-nc-*'r~g -
t 10,-, -. f, I'J,,t~ jjw~r ~~fl a"'lle t-)rpftri"Tl#,Tltn,' herlitil-1,9 In doj,ll~
'7 ~& I
Farm. i tokq~ ~r- nc-t,~ ~ , 14 - rf) '0 (MI I RA 18,, ` )
1 . KsLf edra f a,-nak,: - ~g' I ! 2 a,,, - 1 1 -4 en t- N.F. Tka-kun)
pci-qk,~gc m~d~.,.5in3k3gc, -n,;t'.Tuta.

Ef fec of f 2 ar: on
Farm. ?8 ric;.IiIC5-l0'l Ja-F 'rj5.
IIMI!,2. I i - I,,
1. Kafedra farmakoloifil (Z8V. - VT'('f. N.P.FKilun) Te T-T; r I' 9~. 0~-
meditsinskoro

F.RTROVSKIY. G.A.; 4A.PADNYUK. V.I.j PASJ92HHIK- 1-Q,,..A3RZDA, A.Ys.;
LITYINCMX. N.V.
Cholegogue effect of 13upleurun exaltatum, Agrimonts aslatica,
leontopodium ochroleucum, and Veronica virginica. Farm. I toks. 20
no.1:75-77 Ja-F '57. (KLRA 10:7)
1. Lefedra farmakologii (rev. - prof. G.A.Petroveirty) Llvovskogo
moditsinakogo institute.
PILIART TRACT, effect of drugs on.
Agrimonia aslatica. Bupleurum exaltatum. leontopodium
ochroleucum, & Veronica virginica. cholagogue action kRus))

PASFMIK, I.Eh.
Choleretic action of vitamin P-active preparations. Vrach.delo
no.2:153-155 F 160. (MIRA 13:6)
1. Kafedra farmkologii (zav. - dotsent N.I. Skakun) Ternopol'-
okogo meditainakogo instituta.
(vrTAMNS-P) (LIM)

-a' ",*- 1-7A !,=ICA m,etc.Jan5S
".~J;4n '~sc.2 Vol.3-1/1 Physic-Bioche
S 4EC-h-, 11~-k" -4:11 -.-- - - ---
338. EFFECT OF THE PROPIONATE OF 4-PIIENYL!.1:2:5-TRIMETHYL-4-
PIPERIDINOL (PROXIEDOL) ON LIVER FUNCTION (Russian text).
Pasechnik 1. Kh. Dept. of Pharmacol., Lvev Med. Inst., Lvov.
T"MAXOM-1-TOKSIROL. 1957, 20/1 suppl. (22-23)
The effect of promedol on the volume and composition of bile was studied in dogs
with chronic bile fistula and the effect on tone of the sphincter of Oddi was studied
in acute experiments on anaesthetized cats. In a dose of 0.3 - I mg. jkg. promedol
caused a decrease in volume of bile secretion with an increase of the concentration
of bile salta, a decrease of cholesterol and a rise of the cholate-cholesterol ratio.
It slightly raised the tone of the sphincter of Oddi. Its effects on bile secretion
were more favourable than those of morphine. RaAkovd - Prague

Affect of promedol on liver function. Farm.1 toks. 19 supplement:
22-23 156. (MIRA 10:7)
1. Kafedre farmakologii (zav. - prof. Tu.A.Patrovskiy) Llvovskogo
maditainskogo institute
(ANALGESICS, effects.
4-phenyl-4-propoxy-1,2.5-trimetkiyl piperidine on liver
funct. (Rue))
(LIM. effect of drugs on,
4-phanyl-4-propoxy-1,2,5-trimethyI. piperidine (Rua))

Pgnovsny, G.A. [decensed]; SMUM, A.Ya.; PA.SNGHNIK, I.Kh.
lirfect of 11111thiol on the ci1olAJwuO function (if tile liver In ex-
nerimental (toxic) hepittitic. Farm. i toks. 22 no-3:274 RY-Je '59.
(SULPHYDRYL COMPOUNDS, eff. OCM 12:7)
2.3-dimercaptopropane sodium sulfonate on bile aacretion
in exper. toxic hepatitis (&19))
(B112,
secretion in exper. toxic .iepatitla, eff. of 2,3-dimercap-
topropane Bodlim sulfonate (Ibis))
(HLTATITIS, ex,)er.
eff. of Zj-diinercaptapropane nodium suLfanate on bile
necretion in toxic hepatitis (Hue))

S'KAYIN , N.P. ; i ;,~;: ( i1r: I ~~, ' . Kh.
144-r,chariissm r,,,' trii~ r~r.r- t . , 'I-- i r. ** a ,, -c, -, " - ~, .- -, 4 - -, .... ": ,1. ~ .1 1. ~. 1.
and r (i r- t i o on,. .Fa r rr. .",,, , , . , '~ , . 1: , , - ~.~r, 11 1 ".. .
1. Kafcdra far.,wkoiwi 4 Zav. - cr ~oj :. na-3: N.1 .
Tt~ rri.- ; c, , ' - r. ~ *, 6 i!,!~ ~ - j- .' ~- t j ', . t ~j .

a,O Y,5 c-,zl A// A~'
USSR Pharmacology and Toxicology--Med-leinal Plants V-5
Abs Jour: Hof Zhur-Biol., No 23, 1958~ 107341
Author : Petrovskiy, G. A., Zapadnyuk V. I., Pasechnik,
I. Kh., Sereda, A. Ya., Litvinchuk, M.-*V-.,------
Inst : Not given
Title On the Choleretic Action of Bupleurum Exaltatum,
Agrimonia Asiatica, Leontopodium Ochroleucum, and
Veronica Virginica
Orig Pub: Farmakol. i toksikologiya, 1957, 20, No 1, 75-77
Abstractt The choleretic action of Bupleurum exaltatum,
Agrimonia asiatica, Leontopodium ochroleucum, and
Veronica virginica was studied in dogs with gall
bladdex fistulas and ligated common gall ducts. It
was established that Bupleurum. exaltatum and Leonto-
Card 1/ 3
13

USoR / Fharmacology and Toxicology-Medicinal Plants V-5
Abs Jour: Ref Zhur-Biol, No 23, 19587 207341
44 to 45 milligrams per 100 [there is no indication
from which parts of the plants the infusions or
decoctions were prepared-editorl.
Card 3/3
14
SUKUN, N.F.0 dotsent; PABBOHNIK) I.Khei kandem'donauk
influence of adenosinetrilbosphoric 4cid and a muscular adenylic
preparation on the bil-9 secreting function of the liver. Vrach.
delo no,.21*56-58 F f61. (MIRA 14:1)
1. Kafedra farmakologii (zav. - dot:%ent !I.P.Skjr-~=) Ternopol'Skogo
moditsinskogo inBtituta.
(LIVER) (ADENOSINETH-2HOSPHORIC ACID)

USSR/Pharmacology. Toxicology. Aralgesics U-3
Ab
,~~ur : Ref Zhur-Biol., No ?, 1958, 32886
Author : Pazoohnik-_ . Kh.
Inst : 9o--t given J--n
Title : Effect of Promedol oil Hepatic Function
Orig Pub : Farmakol. i toksikologiya, 1956, (1957), Prilosh,
Sb. ref. , 2e"-,'3
Abstract : 11%vo dogs with chronic fistulas of the gall bladder
were administered Dromedol subcutaneously in doses
of 0.33 to 1 mg/kg. A decrease in the quantity of
bile and of cholesterine in the bile, an increase
in the concentration of bile salts, of bilirubine
in the the bile, of the specific weight of the bi-
le and of the coefficient of cholestorine-cholate
was noted. In acute experiments on 15 cats which
were anesthesized by urethan it was indicated that
Card 112

PAS EC I U I I K
Influence of phenatine or. biliation by the liver. Farm. i toks.
24 no.5:562-564 S-0 161. (MILA 14: 10)
1. Kafedra farmakologii (2av. - dotsent N.P.Skakun) Ternopol'skogo
gosudarstvennogo meditsinskogo instituta.
(PIW- NAT ME) (LIVE10 (BILE)

3ffect of promedol on aecretory and periodical motor activity of
jtc)i. Fiziol.zhur. [Ukr." ' no.):393-)07 My Je 159.
the atom j 5
(MIRA 12:10)
1. Vvivalkiy Tnedichniy inatitut, lutfedra farmakologit.
(PIYX11IDI1U,') (STOMC14)

PASECHNIK, I.Kh.; MERIKOVA, Yej.
Vitamin S as an antlcholoretic. Vop.,-)It. 18 no.5:39-42 S-0 159.
(MIRA 13:1)
1. Iz k-afedry farmlcologli (zav. - zasl=hennyy deyatel' nauki USSR
prof. Yu.A. Petrovskiy [dfjceasedl) Llvavskogo medltsinskogo Instituta
i kafedry farmak-ologli (zav. - dotsent N.P. Skakun) Ternopollskogo
meditsinskogo inatituta.
(VITAMIN B pharmacol.)
(BILLA.RT TRACT pharmacol.)

I I. I'lli.
Pasechnik, I. Fh. 117he of promodol." Llvov
St,ite ,' 'edic;tl Inst. Llvov, 1956. (Dis-ert-tion for
the DeF:ree of Candidate in !,,ed~c:,l Science)
3o: letolds', :k). 27, l~_'5u. 114-1 1 J; III.

PASEGMK, I.Kh.
Effect of noradrenalin od Od&'L'a sphincter tonus. Farm.i toks.
22 no.6:519-522 N-D 159. (MIRA 13:5)
1. Kafedra farmakologii Llvovskogo (zav. - zaeluzhennyy dayatell
naWd USSR prof. Tu.A. Petrovskiy [deceased]) I Ternopollskogo
(zav. - dotsent N.P. Skmkun) gosudaretvannykh meditinakikh insti-
tutov.
(BILE DUCTS pharmacol.)
(ARTEMOL)

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-7 5 . I
Wi A .9 -rawberry aF a c.'~c -ia7og-.Ie a Vo~ . ~i t. 23 n~. 5: 1--, c-- '--.
1. K),f(Arn ftwllvl~.oloj!'li (~,,Ilv. - 14,01'. ~"g k "
mpdAtf)Jri,qkopo Inutlulta.

I K , T . Kh. ."C' it . K
jr. r,
cIfe- si
Illf'-- -
d Tit-'
ka
fal-m-:-09.
gcjgu! !a 7". t

GAMBURTSEV, G.A.; RIZ "NICHMO, Yu.V.; rOMZON, I.S.; YRPIIIATIYRVA, A.M.;
PASXCWI~; KOSMINSKAYA, I-P.; XOUS, YO.V.; YIROFVZVA, A.A.,
fWnM-dr-. KISEI-XvA, A.A.. telthnicheskiy re4aktor
[correlation method of refra.:tod wavnn; mamml for seismological
engineers] Korreliatsionrkvi metod prolomlennykh voln; nikovodstvo
dlia Inzhenerov-seiRmorazvedchikov. ?Aosl-v&, Izd-vo Akad. nauk SSSR,
1952. 238 P. (Microfilm]. (MM 8:7)
1. Chlon-korrmspondent All SSSR (for Gamburtneiv).
(Seismom"try)

USSR/Geopbysics - Geophysical Prospecting Nov/Dec 50
Seismographs
"Vibration Platform for Studyine Seismographs Used
in Geophysical Prospecting," I. P. Pasechnik, Geopbys
lust, Aced Sci USSR
"It Ak Nauk SSSR, Ser Geograf i Geofiz" Vol XIV, No 6,
RP 514-530
Describes inertial vibration platform constructed
from design by Yu. V. Riznichenko for recording
;Muency and phase responses of modern vertical
Prospecting seismograpbs in frequency range 5 - 3,500
cps. Tested electrodynamic seismographs, and es-
tablIsbed. several resonances at high frequencies
M- 171T65
UM/Geophynice - Geophysical Prospecting Nov/Dec 50
(Contd)
caused by natural transverse oecillationa of flat
springs loaded by --cill at ends. Submitted by Aced
0. Tu. S=idt 10 Apr 50.
Am 171T65

UssR/Geophysics - Seismology Jan/Feb 52
"Procedure for Experimentally Studying Resonance
Phenomena In the Oscillatory System Soil-Seismo-
graph," 1. P. Pasechnik, Inst of Geophys, Acad
Sci USSR
"Iz Ak Nauk SSSR, Ser Geofiz" No 1, pp 21-34
Describes devised techniques applied to subject
study as well as procedure for processing of re-
sults. Cites examples of observed frequency and
phase resonance curves and of recorded natural
oscillations of the syntem "soil-seismogragill'"
obtained under various conditions.
205T39

USSR/Geophysies - Rego
oirge,Phenomepa in -May/Jun 52
elsmograph System
"Results of Experime!2tal Study of Resonance Fheav-
mena in the Oscillatory System Soil -Seismograph,"
I. P Faeecrni-m, Geophys In5t, AQad Sci USSR
"1z Ak Nauk SSSF, Ser Geuf iz" No 3, PP 34-51
Expounds results of an erpLl study of the dependence
of resonance properties of the oscillatory system
soil -seismograpt upon its parameters: velocity of
propagation of longitudinal wwves in soil and
soil's density, and wt and area of seismograph's
base. Presents data on influences of various
metbods of setting up a seismograph upon resonance
properties of the system soil -seismograph.
224T70
Indicates influence of phenomenon of resoanzce
in the system upon the character of seismic re-
cordings and upon resolving capacity of seismic
t.,A- lzd~icated various methods for setting up
seismographs for various surface conditions, under
which methods the resonance phenomena are absent Qr
weakly expressed. Submitted 30 Dec 51.
224T70

MWOeophysics - Seismology Sep/Oct 52
"Compmrison of Results of Theoretical and Experimental
Investigations of Resonance Phenomena in the System:
Soil -Se ismograp4 " I. P. Pasechnik., Geophys Inst,
Acad Sci USSR
01z Ak Nauk SSSR, Ser Geofiz" No 5, pp 25-46
Dependence of resonant properties of the oscillating
system: soil-seismograph on soil parameters, density
and velocity of propagation in the soil, and vt and
radius of seismograph base is investigated theoret-
Ically. Comparison of theoretical frequency and phase
22&62
resonance curves of the system with experimental ones,
obtained under various conditions, is drawn. Article
states that these curves agree satisfactorily. The
effect of resonance phenomena of the system an seizzic
recording is shown. Received 5 Jun 52.
P-2ft62

PASECHNiK, 1.41.
USSR/Geophymics - Froperties of Rocks FD-1191
Card 1/1 Pub. 45-2/8
Author : Karus, Ye. V., and Pasechnik, I. P.
Title : Study of the elastic and absorbing properties of rocks in their
natural surroundings by methods of selemoacoustics
Periodical : 12V. AN SSSR, ser. geofiz., no 6, 1954, PP 515-526
Abstract : The authors briefly describe the physical principles of their appa-
ratus, technology and method of field observations for determining
the elastic and absorbing properties of rocks in their natural sur-
roundings. Their method ic based on a study of the propagation in
rocks of elastic stationary sinueoldal oscillations with frequencies
from 50-100 to 3000-4000 cycles, which are excited by electrcmagnetic
or piezoelectric vibrators of low power (of the order of 50 v). using
this method they deter-mine the phase velocity of the propagation of
elastic stationary sinusoidal oscillations as well as the values of
the coefficients of amplitude absorption of these oscillations.
Institution : Geophysics Institute, Acad. Sci. USSR
Submitted : March 6, 1954

USSR/Geophysics - Physics of the Earth FD-1713
Card 1/1 : Pub. 45-1/12
Authors : Karus, Ye. V., and Pasechrjik, I. P.
Title : On the nature of elastic waves excited in real media by a harmonic
source
Periodical : Izv. AN SSSR, Ser. geofiz., 89-100, Mar-Apr 1955
Abstract : On the basis of an analysis of experinx!ntal materials obtained In various
to seismological conditions the authors examine the question of the nature
and properties of elastic oscillations excited in real media by a har-
monle source. They show that these oscillations have a complex character
and are the result of the 6uperposition of waves of various types -
longitudinal, transverse and surface waves. The longitudinal waves are
not predominant as regards intensity; the transverse or surface waves
turn out to be predominant.
Institution Geophysical institute, Academy of Sciences USSR
Submitted June 16, 1954

H`~ E0_ H IN I K 9 F - _P
USSR/Physics of the FArth - Gqnoral Problems, 0-1
Abet Journal: Referst Zhur - Firika, No 12, 1956, 36291
Authort Paseohnik, I. P.
Institution, Yone
Title: Azimuthal Four-Comporent Installation with Tnelined Seismographs
Original
Periodical. Tzv. AN SSSR, ser. peofiz., 1956, 'go 3, 295-2R9
Abstract: Description of an azinut'hal 4-componert installation w4-th inclined
seismogrrphs, !ntended for the recording of local earthquakes. The
installation was used in work of the Khaitsk epicentral zone of the
Gamak Oblast. The advantages of recording with 4-oomponent in-
stallation with 'nalined seismographs over recordinre obtained ve-th
ordinary 3-componert installations with 2 horizontal seismographs
and one verticel one are describnd.
Card 1/1

POSF-CHNIK, I-P
USBRIPhYSics of the Earth - Seismology, 0-3
Abut Journals Referat Zhur - Fizika, No 1~, 1956, 36360
Author: Ventskevicn, Ye. V., Pase*ik, I. P., Fedoseyenko, N. Ye.
Institutions None
Title: Application of a Driven Swe-ap in the Recording of Seismic
Vibrations
Original
Periodical; Izv. AD SSSR, Ser. Geefiz., 1956, No 5, 525-533
Abstracts Description of a method and apparatus for a multi-channel photo-
graphic recording of seismic vibrations, the time of arrival of
which is unknown beforehand, with the speed of the sweep being
capable of being raised to 50 MM/sec. The method is based on
using a driven sweep in the registers, automatically switched in
at the instant that the first pulse of a 4~Wation arrives at the
seiamogr*_
Card 1/1

PASBCHNIK, I.P.
Study of the seismic character of the Khalt epicentral zone.
Izv.AN SSF)R Ser.goofi2.no.12:1427-1438 '56. (MIRA 10:10)
1. AN SSE~t, Geofizicheakiy inetitut.
(D-ait--Seismology)

PASECHNIX. I.P.
,
Selecting optimum conditions for arranging selance.7stoho and wave-
generating appAratus in amismoaccaustics. Trudy Geofiz.no.35:159-
1?5 '56, (MLILA 10: 1)
(beismology)

C)s

49-1-13.."16
AUMORS: Pasechnik, I.P. and Pedoseyenko, 1q.Ye.
'P=: Electrodynamic Microbw-ograph with Galvanometer Recording
(Elektrodinemicheskiy Yiikrobarograf a gallvanometricheskoy
registratsiyey)
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya Geofi7icheskaya, 1958, Nr 1,
PP 121-130 (USSR)
ABSTRACT: A description is given of EL microbarograph which has been developed
by the authors of this paper and also of its calibration and examples
are given of recordings of microfluctuations of the atmospheric pressure
within a wide range of periods of 2-3 sec to lr--20 min. Furthermore,
.1
examples are given of the interrelations between such microfluctuations
and certain seiamic and meteorological phenomena. The microbarograph
is produced in two variants, in one of which the sensitive element is
an elastic membrane covering one of the waUs of the hollow hermetic
chamber, in the other the sensitive element consists of a conglomer-
ation of "vidi" boxes. The first-mentioned variant consists of a
hermetic chamber of 28 000 cm3 volume, one of the waUs of which is
covered by an elastic membrane of circular shape made of 0.1 mm thick
Card 112 phosphor bronze; at the centre of the membrane a light rod is fixed

AUTHOR: Pasechnik, I.P. 6OV/49- 58-91-8/ J4
TITLE: Sel-s-m-1-c-an-d-kerial Waves Origimted by Erupticri of
Volcano Bezymyannyy on March 30, 1956 (Seiamicheskiye i
vozdushnyye volny, voznik-sh--'ye pri izverzhenii vuikana
Bezymyannyy 30 marta 1956 g)
PERIODICAL: Izvestiya Akademii 1,iauk SSSR, Seriya Geofiz-;cheskaya,
1958, Nr 9, pp 1121 - l126 (USSR)
ABSTRACT: The volcano Bezymyannyy (Kamchatka) was considered as
extinct until 1955 wien, for the first time, some seismic
activities were reccraed. Later, on March 30, 1956, at
06.1.L hours GMT an energetic eruption took place, togethe:
with a local earthquake. The eruption, which had a
character of the stioLt detonation p.--oduced the aerial waves
which travel-'eu rouLd the 'earth. They vere recorded by
the seismic stations ol the USSR and abroad.
The seismic waves were &-'6o recorded. Table 1 was
compiled from these recordiri6s, one of which is shown in
Figure 1 (a - longitudinal wave registered at 2 250 km,
b - surface wave - 6 600 km). Tle exact position of both
the epicentre and tLe focus coul(i not be established
due to variouLi The ezijrgy (El, was
Uardl/3 calculz~ted from the formilla (1) ab 10 6 - 10 ~ orgs, Miicli

'30V/'49-P8-C~-841~c a 110
Seismic and Aerial Waves Orig_-~naTed ',-Jy Eruption 0tl~e
Bezymyanyy on March 30, 1956
represents the magnatude much hiEher than that cf the
strongest known elrup-Acn of Mikhara volcano (Japan) in
1953-1954. The data of the aerial waves, as registered by the
various stations, is given in Table 2. The travel of
the waves around the Ea--th and the position of some of
the observing staticas aTe shown in Figure 2. The
photographic copy of the recordings are shown in Figures
3 and 4. The charactertstic shape of the first wave was
recorded at every station (this shows a phase of
compression with gene_--aCl quasl-sinusoidal form). The
first half-period of the vib-ration was 8 min, while the
next one lasted 10-12 m,-n. The maximum air pressure was
250-300 bar. The ve'_o_,_'ty of wave travel was 295-333 m/sec.
The variations of vei:.city were caused by the
meteorological condit,-')ns.
The second wave, recorded at the distance of ',~ ~/50 km
was of a similar chtjraccer as the first. Its velocity
was 318 m/sec. The Ljj_jj,d WLI-1t) (1~jkrure 4e) al~3o of ~Iio
same character, had a Of 313 m/-gec. It was
established that a I-e;.;Iiar :character of the waves was
t,ard.2/3

SOV/49-58-9-8/14
Seismic and Aerial Waves uriginated by ErUDtion of the Voicanno
Bezym:ftnyy. on March 30, 1956
cau3Dd by the first abrupt discharge of gases.
The energy of the aerial waves was calculated by means of the
Whipple formula as being equal to 1023 ergs. When taking
this energy as being only 0.1 of that of the eruption, it
can be assumed that the latter was equal to an equivalent
of several tens of jaillion tons of TNT.
The aerial energy of the above and other eruptions could
be determined more closely if the observation stations sit-
uated in the active regions were equipped with mbre precise
microbarograzhF.
There are 4 iigures and 2 tables and 11 references, 6 of
which are Soviet, 4 English and 1 French.
ASSOCIATION: Akademiya nauk SSSR~Institut fiziki Zemli
(Ac. te. USSR, Institute of
SUBMITTED: March 61, 1957
-ard 3/3

f
MONAKHOV, F.I.; rASiCHNIK, I.F.; SHEBALIN, N.V., PODCILISKIY. A.D..
red.; YAMI, Ye.V., tokchn.red.
(Seismic and microseismic observations at Soviet stations
during the International Geophysical Year] Eeismichaskie
I mikrosaismicheakis rLabliudeniia na Bovetskikh stants~iakh
v period KGG. Moskva, Izd-vo AkBd.nauk SSSR, i959. 37 P.
(MIRA 12:7)
(International Geophysical Year, 1957-1958)
(Seismology--Observations)

L'-D'/04c)/59/000/03/014/019
AUTHOR: pasechnik, I. P.
TITIZ: Long-Period Air vlaves Occurring Befor) a Storm
PERIODICAL: Izvestiya Akademi-i nauk SSSR, Seriya geofizicheskaya,
1959, Nr 3, pp 4',11-4?5 (USSR)
ABSTRACT: This type of wave was.,pecorded by sensitive micro-
barographs at va.?ious',Qeism1 stations in USSR.
Examples of reccids are illustrated in Figs 1, 2 and
4. The periods of waNes were 4 to 12 minutes,
the maximum amplitudes were- 100 to 200 bars
(sometiaes 500-(500 bars) and the durations were
usitally 20 to 30 minutes (see T&ble on p 4?1),
These records caL, be compared with those of air waves
produced by the eruption cf the volcano Bezym-yanny
illustrated in Ftg 3. Fig 5 illustrates the vibrations
of the grouxid generated by air waves propagated in front
of a thunderstorm and recorded by a horizontal seismograph
Card 112 11--ype SGK),,designed by D. P. arnos, It is suggested

S/049/59/000/03,/014/019
Long--Period Air Waves Occ;-drring Before a Storm
that Im order to explain the nature c,f these air waves
y -- e ma t ir ccbserwatJons should be carried out by
more s-
M e. t e. 0 r c 1 C, g _~ F; t sTriere are 4 f -_'gures, 1 table and
8 r~-feren,_-ES. c,f whi-_Yi am Sc.viet, 3 English arid
Ge rir.,,a ii
ASSOCIATION: Ak-adem,.,ya nalUe. SSSR, T-ristitut fizi.k-. Zemli
(A-- Se--. IT'33SR, Institute of Physics of t-he Earth)
SUBMITTED: Ju.1y ~G, ',~.It?
Card 212

V/14 9- 59- 11 - I C'/
AMHUR, Pasechnik, I.-P.
PITLE: Aerial Waves Produced by the Gobi-Altity Earthquake
or., December 4, 1957
I-ERIuDI,2i,L: Izvestiya Akademii nauk SSSR, Seri.va geofizicheska,-:a
1959, Nr 11, pp 1687-1689 (USSR,i
ABS'Titii "f- The waves were recorded by the riicro--,aro~,,ra~;hs EDMB-1
and ED1113-II (described by Pasechnik i:1 Ref 7) the
,ensl:ivity of which was 2 and 7 bar/am/m respectively.
'hey wei~e placed at the epicent-ic distance of 4)6 -
~440 km (a temporary observation poinL). An example of'
Lhe oscillo6ram rE!Corded is reproducel in Fig 1. Tlie
dimes of wave gen(,!ration, as calculated by different
seismic stations, are given in Table 1. The entering
z~-Jmes recorded by the observatiDn point are Given in
Pable 2. The velocity of wave propa.L;ation was deteymizl,~,-,,
as VP = 320 m&ec. The energy -Nas calculated as 10 7 er
ie it was 10Y times less than that of seismic wave
There are 1 fif~ure, 2 tables and 11 references, 7 of
'N'r.ich are Soviet and 4 English.
Akademiya nauk SSSR, Institut fizil~i Zemli (Ac~jder-,,:y
uf Sciences USSR, Institute of PhysicF of Earth)
6'JBMiI-L-"~D March 11, 1959

S/04 9/59/000/12/0 16/021 7
E131/E391
AUTHORS: Pantighnil" I. P. and Fedoseyenko, N.Yo
TITLE: Experimen'ta'With the Improved iismog;rE~jphs , Types SVK
and SGK
PERIODICAL: Izvestiya Akademii nauk SSSR, Seriya geofizicheskaya,
1959, Nr 12, PP 1855 - i86o (USSR)
ABSTRACT: The seismographs 3VK and SGK, generally used in the USSR
for recording the longitudinal, tran.-jverse and surface
waves, are not sufficiently precise for recording weak
IV earthquakes of a magnitude m - 4 . The author, therefore,
-d`e`M1gn-`e`a7fFe new improved type:5 , SVK-M and SGE.-M, which
are illustrated in Figure 1. Their characteristics are
tabulated in Table 1. The constants of these new seismo-
graphs, as used at the stations of the Soviet zone of
the Antarctic, are given in Table 2 and Figure -. As an
example, the SVK-M seismograms. are compared with those
obtained with SVK (Figure 3), Figmre 4 shows an example
of the P-%fave obtained with the seismograph SVK-M at the
distance Aa = 2 650 Ian from an underground detonation
of 1 000 tons of explosives (M ~z 4 ) . Figures 5 and 6
Cardl/2 show seismograms of two earthquakes recorded by the

s/o49/5q/ooo/l:-'/016/027
E-131/E391
Experiments with the improved Seismographs, Types SV--k' and SGK
seismographs SVK (a) and SVK-M (6 and B).
There are 6 figures, 2 tables and 8 Soviet references.
ASSOCIATION: Akademiya nauk SSSR Institut l'iziki Zomli
(Institute of Physics of the Earth Ac.Sc., USSR)
SUBMITTED; April 1, 1959
Card 2/2

D 68160
AUTHORS: Ko~gan, S. D. 9 p
Sultanov. D.
TITLE: Difference in the Periods of jeismic '.1avog
in Underr-round Explosions and in Eiirthjliakos
PERIODICAL: Doklady Akadeinii ri,uk .33jR, Vol 1214, Nr 0
( TISSR)
A53T:~AC--: The a~it`-Iors ccmpure the da ti- on th a I re llo::l i nEL t, n,.-
seismic vibrations in explo.,jiono tnd in
equal intensity. On Dece!.,,be;* 1',), ~jt `-'U
time, 1000 tons cf amnqo!zitt~ w,-~re Lxplloded ~C k.:,
the -ailroad station of Ar.3' (Tu.~,hkent line)
~ = 69'0~1'02",99 E) for 3cientifi,; i~uri-oae---
fixed in a lepth of 40 m in LL SildI41t C!j"gjb,3r( 1,n
On ?9p 1959 510-J tons of ammonite Were -t
9.30 A. M. Greenwich time in t1io rayon of Pukrov;i~
( I = 60.20N1, A - 590,) E) "or th,~ 1~ur;.ooe of
river of, ~.ogether, I 1CC n. 1~: Ithu
were recoried ~y 1,r--A-b;,ri seisro.,3ral,hs -ed '--y
(3K) , by mor;~ sen3itivf, ,~,o-iernizztl
,ard 1/4

68160
DifferenQe in the Pprio~~3 -)1
r e Ex c i t d i ri U nde r r~ ro,,1 ril EY p I i. -.j n Lj ri ri d I n z - t h -1 ~Ia 1~ e.9
o ther i ns *,r-:::er. ts T!.e 1.re : or. * Ft~per i i ~i i:3ed
IT e as a re.apnts wi t~ ~E . In .~ e case -f in -I ergr- -n-~
M
all types of wtve3 't;,",'fl r-,-C ;h1ch ire c' ~'~ z
of earthquakes .-,'iLh their ~;ri6in In L.. jraijite la,er. ' :.e
stations with epicentral 1:,stances of ,q~ to k., t:.,
follo-.,.,ing front waves br,)kt~n 3n the brundaries of tiie
cru3t were recorded in the oxplosions: sodiner,,~r.., 1~,-r granit--
A
layer (P,S), !a-,,e,- - k)asz~lt 1a-.1er ~r, J ):"i"e
f
' and al so 3 '11. "LC e ,cave s ~ YH -I t - v
0 .'
Y
n
Rf,, f 1 ) rro Le a :-ez o~- t on the ~-ic oCrLphS Of V~, I -7.e SIC:
prod u(-, -ad b~,,, %eavy ~jx:- 1 o6 i c -i s a nd on the ~3 t r,,~ c e f :I.
crust in ( 3ov i e t ~, C e -i tr u 1 A-, i a t e T i c e:. I. ru I
tha.--, 1 1 OC ',-,n ~ i re c t I ongi tA 1 ni~! vav Ps i r e r -I;.
Waves 3, and a'Lsc s,-~rface rinves were
-ecorled vi~,ves ~-.re 7,!Ic)wr, in fij~u;-e I . A*~ ~ne
Ji3tance tirie period c-f the sArf~.~.a wave in c)r.-
times a-q 9:%all as the 1:Lriod o-' a sarface w%ve .,i
The "at,,ors u1sc lealt with eart,.qa,kei riei.r th~
Card 0/1-1 recor~e! a' *he ~;tation Fra-ie durin, the

68160
i~!"* c h j cc~'
Difference in Vie k'eriods o' Sel 3~li C
Are Excited in Under~5ro~.,nl Zxplo-~i:)nj znd in EarthqUil't?P,
Accorlingly, the -eriodq c' vol,im,~~ -.-aves 10 not or
de:~end on t~,e e~ic-?ntrai !i,;tance, on the Jai~th Lf
and on intensit," I,-, th~: case of !istanceq
100 to 1003 1,::,, ~eriD,15 cf the Lon-itJnul 7~ves
car~,~~i are C.6 to ?.0 sec, in eXV 1031 :~ns to 0 s~-c

, va v e!-. a ti -: e n t r.. 1
periods of trunsvpr, ill Partiiquuke
of up to 1,~CKi m ur~-, 'rom - 1 to al proximatel, 4 j-
3urface wves :-ecorl ~~ Ly ~ hrowl-I)and
3~~ the liff-re!,.-e in the i,eri.)ds of earthquake3
'
~
I'Ke
? - t
' I I t3- 9c :--
-rea t.
Re f
r0
i s th~
V
k (
~
.
-
:
.
.
,
I
~
~
surf .-c e wave ~ i n i on.Li mus t ftL.ve smal lur per,- -)d-,
of tne diffe-ence ir. reenter 1;.mensions tt.~,, ~Iurfz'ce
ear thqual, e c-,, ; rov i d i ng t ha t thtf pe i i ocis 0 f body
t ht- i r e ne r.~y E- r e e-i i n 'io th c a s c- s . T h i s ~ u n I - -i ~3 1 0 r. '.7C
firiiied b-,. otl-ier cor-,,iderutio,;s. The lata obtalnv-! r
a new o r i ter i on f or the 1,~Arj,-)6e of ~.l I ii rij, , i ~1'. i- ~j
betvo---en exploulonL; mnd earth juakes, Thero are 4 f 'r),j
4 references, 5 of -xhich Lire Soviet.
C
d
ar
3/4

68160
Difference in the Periods of Seismic Uav-~r, 1,11~11c.,j -3C,lj'20-' 21-?-,~-
Are Excited in Underground Explosions and. in .arthquakes
A 3,O)OC I A TI 0 N: Institut fiziki Zemli im. (,. Y-i ~hT~dt!i Akademil
(Institute of Ph,~sl-~s of tli,~ ---:urtn i
'M I - Yu.
Academy Cf 3ciencc-,,i of t'ie '!Jj~il
PH!~SFTNLD: 3eptember 16, 195~, b~y 'j, N, jozaenov, ;,cudp;~,ician
SUBI.'I'!'T--'D: 3eptember 16, 1959
,ard A,,I"4

q
_31~300
AUTHOR: Paeechnik, I.P.
26981 S/049/60/000/012/005/011
D214/D305
TITLEs On determining the attenuation parameters of P n and
S* waves
PERIODICALs Akademiya nauk SSSR. Izvestiy-s. Seriya geofizicheskaya,
no. 12, 19600 1740 - 1743
TEXTs The variation in the amplitude of i3eismic waves with the
epicentric distance is of major importance in detecting and iden-
tifying underground nuclear explosions. The attenuation properties
of these waves can be established experimentally from seismic ob-
servations obtained for nuclear explosions or ordinary "chemical"
explosions, since both types give rise to similar seismic records.
The present author makes use of data for the underground nuclear
explosions set off in the USA, and TNT explosions set off in the
USSR, to estimate the attenuation parameters of Pn and So waves.
The amplitude attenuation of longitudinal and transverse head wa-
Card 1/4

26981
13/049/60/000/012/005/011
On determining the attenuation ... :)214/D305
ves in a perfectly elastic medium can be represented by the formula
A 10-
27-
0
where Ai and A. are the amplitude at the) point of observation and a
point nearer the epicenter respectively,, and A i and 4-b are the
corresponding epicentric distances. Experimental and theoretical
work on the amplitude attenuation of head waves has shown that in a
real medium the vedation in the Eanplitule of head waves with the
epicentric distance may be represented by an expression of the form
A Ao e-M (A i-A0 (2)
i Li ) n
Ja 0
Card 2/4

26981
:3/049/60/000/012/005/011
On determining the attenuation D214/D305
According to I.S. Berzon (Ref. 5: Izv- AS SSSR, Ser. geofiz., No. 4,
1951) the average value of n approaches 2, the limiting values being
1.5 and 2.5. The present author finds that in the case of the 5 and
10, kiloton nuclear explosions (Romney, Ref. 2: J 0Geophys. Res., 64,
No. 10, 1959) and the TNT explosions reported in(Ref. 1: I.P. Pa-
sechnik, S.D. Kogan, D.D. Sultanov, and V.I. Tsibullskiy, Tr. In-ta
fiziki Zemlip AN SSSR, No. 15, 1960) the values of n and a are as
follows: For P. waves with periods betwcen 0.6 and 0.8 see the ave-
rage value of n is approximately 2.0 and the average value of a is
0.0022 km-1; for S* waves with periods bet Ieen 1.0 and 1.2 see the
values of n and a are -jl.7 and 0.0023 km- respectively. These va-
lues were determined by direct fit. of the theoretical curve to the
observed experimental curve and also by the method described by Yu.
V. Riznichenko (Ref. 6: Tr. Geofiz. In-ca AN SSSR, No. 35, 1956).
gree-
The two methods lead to values for n and a which are in close a
ment. The present paper is said to be a first attempt to use the me-_~_
thods developed for seismic prospecting in determining n and a for
Pn waves. In principle, the method may lead to more accurate values
Card 3/4

26981
S,/049/60/000/012/005/011
On determining the attenuation ... D214/D305
for a and n, e.g. when more
iable. The,7e are 1 figure,
and 3 non-Soviet-bloc. The
cations read as follows: C.
ves from underground nuclear
10, 1959; B. Gutenberg, Bull
C.F. Richter, Bull. Seism.
complete! experimental data become avai-
1 table and 7 references.- 4 Soviet-bloc
references to the English-layWage publi-
Romney, Amplitudes of seismic body wa-
explosions, J. Geophys. hee. 64, No.
Seism. Soc. j~mer., 35, No. 2, 1945;
Soc. Amer., 25, No. 1, 1935.
ASSOCIATION: Akademiya nauk SSSR, Institut fiziki Zemli (Academy
of Sciences USSR, Institute cf Physics of the Earth)
SUBMITTED: May 21, 1960
Card 4/4

32021
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60 2
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trinitrl)t

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T' r 7 ;,u
ex.
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T- e a 1, -
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7a ra
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320 1
S
e a u S S ~m S 7- Z_ 1 1.
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s am e f- n e r,-,,, I e v e s! C i 3 a e
r E. J e 2
ea
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~ac
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sc
r 9 c 1 CLed
are ess t~.Lin
of
wav et',,& max ml-~m M-,I e "I
af t-?rw,c i-ra I
a I e
an c e A
was c3n~,I~t~4 ~y Y', V f I C eY 7.
r:,- v m a C:
-ST
e x;~, c 30:
under,:7 n" e.;Zl n
r
r av
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'IS ll'~ a V e r 7~
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:.
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are
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'
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,
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-
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lu-,-. d e Y. t- o s 10 s
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- Am-li'~~des Of
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ls:
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7
Card /

Seismic observations...
22426
S/049/61/000/002/006/012
D242/D301
absence of nearby earthquakes, apart from sot-,ie oscillations recorded
in August 1958 which were t~.e probable result of various kinds of
ice movement. As has been noted by F. 1. Monakov, I. P. Pasechnik
and N. V. Sh,2balin (Ref. 2: Seysmicheskiye i milcroseysmiclieskiye
nablyudeniya na Sovetskikh star.tsiyak-h v period MGG (Seismic and
Microseismic Observations at Scviet Statioas Durling the IGY) Izd.
AN SSSR, 1959), a di-stinctive characteriszic of earthquakes
recorded at the Mirnyy station is the rather lar~;e period of the
body waves; over epicenter distances of 2000 3000 Im the P wave
has a period of 6 - 8 sec and the S wave of 9 13 sec. Ar-cord-ing
to the data of V. L. Belotelov, N. V. Kondorskaya and Ye. F. Savar-
enskiy (Ref. 3: Ob opredclenii energii uprugildi voln, porozhdayem-
ykh zemletryaseniyem, Izv. AN SSSR, ser. geofiz., 11o. 5, 1960) for
Pacific earthquakes recorded A. stations in the USSR on the same
apparatus, the respective periods for P and S waves are 4 - 5 sec
and 6 - 8 sec over epicenter distances of 20 to 800. These seismic
observations coiifirm. the geological views of P. S. Boronov (kef. 4:
\J\1
C ard 2A

2 242 11
S/049/61/000/00-?/006/012
D242/D301
Seismrc observations ...
Stru1tturnaya skhema intarktiki, Inform., byul*l.. Sov. Antark-, eksp.,
No. 1, 1958) concerning the existence of a g-..rdlc of Alpine folds
around the main East Aa-ttarctic Platform, since this zone coincides
with the areas of carthquake epicenters sh0lM in Fig. 3. Bu t
Boronov's opinion that active uplift is takir.g place along the
littoral zone of the platform is soinewhat of an enigma in view of
the lack of earthquakes in Zastern Antarctica durincy the last 3-1
years. The comparatively constant directions of the first P-%.Yave
movements indicate that tectonic processcs al,:)nrf the whole -irdle
of Alpine fold-structures are mainly ta1cing pLace in the same
direction. During three earthquakes in Novemi:)cr 1956, July 1958
and October 1954 one of the steeply-dipping nodal planes f6r the
P wave bad a latitudinal trend and the other a meridional trend.
T 11.
It would thus ao.)ear that the southern ide of' the latitudinally-
trendinrr fold-s ructurcs is rising, although cata from a greater
number of earth uakes are required to sl-:bstantiate this as rumm:) t ion.,.,,
Rayleigh and Loie waves recorded in 27 earthquakes were cori-Paried
with thc theoretical curve3 cited by F. F. Evison, C.
Card 3/6

22428
S/04S)/61/000/002/006/012
Seismic observations... D242/D301
Fig. 3. Epicenters of Antarcti
earthquakes with an indica-
tion of the magnitude of M
and the direction of the
first movement of the P
wave at Mirrnyy and Oazis
I - 4 < 1.1 < 5, 2_5 < M < 6,
3 - M > 6, 4 - 11 not knoi-m;
the first arrival of the P
wave corresponds to a wave
of compression (+) and to
a wave of rarefaction
Card 4/6

2 2 4? P
S/049/(1/000/002/006/012
D242/D301
Seismic observations ...
and R. H. Orr (Ref. 5: Thickness of the Earth's Crust in Antarctic,
Nature,.181, No 1, 1959) in order to deter,-nine the crustal struc-
ture of Antarctica. The theoretical and observational data for
waves of a group of 15 earthquakes with foci to the *north, west
and east of Mirnyy are given graphically. The scattering of the
Rayleigh and Love waves implies an oceanic-type crust with a
probable thickness of some 7 - 20 1cm in the area between the
earthquake foci and the recor(ling station. The waves of the
other group of earthquakes travelled beneath both land and sea
areas before reaching Mirnyy. The scattering of Rayleigh and
Love waves during their passage beneath land and sea areas is
also given graphically and would appear to suggest that the
waves passed through an oceanic-type crust with an approximate
thickness of 9 km and a continental-type crust with a thickness
of around 40 km. Thus, the obtained results indicate that
Eastern Antar(~tica is part of the whole Antar(LiC continent
while the cruatal structure of the area between the Axitarctide
and Alpide folds is typical of oceans. The authors conclude
Card 5/6

3
29579
014,40 000 ()()#1 Oft-
01
i"$, lilt I It
I c4 III :.fill I'loill I I % III" om J-ill
lilt I I It)1 4 It
rl'.xT This paper im im alitireiiintvil ver-Kion of otiv rvad at a met-ling
#)I the Council for ~-~ #)I If- III -iv It-fires USSI? if) Apt I I
I )Ili 1""perimi-11,ii rv kill v_-vot. flue to ntlElf-AT
v-, Ili)- fill, if Iwo 1(;I,lj 'i"Otyll th;lt Ifw
t-1.1 ~tc seiSMIC ";4vils fit th".-k, JIM,. Iv k1wilivi. to tic
I (.I,;Itefi i a va I ~t hirl I I;Ows I% i I h vt I., -I 'I c(. k I c I. he Fit I I o% I It tr I'Ifics (d
%lij%V.q van he rvicordetl Ili %kirf;wv and ;'lWo,;pht it wlt jual. v%ploslow"
fonci(urtmal and Iran,vcr-;v Imfj% ll-mites, Ili I'll, I'MI.
V,IN lilt 1- 11 1 % Ile I o V
(it
k

29579
fill) 61 mo (106 005 (111
Me- 02 1 H , 0306
i,, if 111, 1 e~ I I). Of A I km, it I too.-; phe I I ( are it , it r hic Lp - x I) I cr, I nns o 1 20
k- lot miiii tip to Nevej ill hisjultredis of kt I ome I t- r P; and megatoll expick."Ifilt-
hi~ d(- It, (I vd aI I ovi-ir Ili t, a I nbc , The p0411 I D o f I tic lcmv I ,
'11) 0 ep I I , ;11,
1- it-leimmed to within 11) ken frtim I he I tint , of ar f iikm I of 11 alld 1,
,I
V- It .~, At a retimber o f d I an I , t ij I i clus ~m;tjvr mirich it !~ t It I, t pi ( v tit E, I (I - it
I I 11 at 1 (11, (1 f I. he expfo~s (m I , ;I will c d I I I I %I I I PT-01) I I'M - I I till I
;I ! rpo I vnt I I v s Eric I v n c I fit, (I vriam I c p r opf P , of I h v ~ I I in I k t -, of v~
'I'll We fit I r K I 'I'S it S 411111111 It u 11 4- 11" 1 0 fA i'41V 1 4' 1 Witt kme f I , it I I I. x it I
1, Th I ~
.1. 1 hi, quemt ) nn (if I d,-nI I I N viiz trivic lear riplotizitimi.. ,~ ma t e I I ;I I ta
a mt bevi-I ptIfj I I sh'd Im I It b % I -% wid So v i !- I Ov I t- aa I I on~~ to tht, Coll-
n- orl thl. Interital t,,iial Ccint!-okof %m h-ar E%p1os,onI,. Thut-v at
gl) r e s a it d I I t I, I e I - ii, t-- 7 wil I , I Ail )( and I ii(iii-Sov let -1)10( . 'I tit
(me ..,- f I-I (.n( es o I he bil &r I , s if - I angti agt, ptib I I f, a I I 4m ~ re ad ns f v I I ou ,
i? I ( It I ('r- like I 'it v 4 ~m - 1~m - ~mvt , -25, no, 1 111115- B. Gutent)p I,
't, I SrA SoC Amer . '--1. 1,-,, 2 %nn . Gro I' I
1945: 11 Gtj I #-riberg , I Howc
I 19 5 F) C thmi-ec % I fit-ophi s He, . 6 .1 , n (, to- 19591,

~ 11111,`
S/04SIV62/000/011/001/006
D207/ D308
AUTHORi Pasechnik, I.P.
TITLEi Dependence of the seismic magnitlidp on the
seismoeeoloGical structural features in the
observation region
PERIODICAli Akademiya naul: S.j,';R. Izvestiya. ')eriya
(;eofizicheskaya, 1962, no. 11, 11)02-1515
T Go r re c t i o na 4 m(where m is t1141 seismic
magnitude of an earthquake or a similar disturbance) were cal-
culated for 55 Ljoviet seismic stations using the recordings of
eight American nuclear explosiona (ground, sealevel, and atmon-
pheric) carried out between February 28, 1954 and Atly 12, 1956,
at Narshall Islands. A correction A m for a particiular station
represented the difference between the value of m avEraged out
for 10 25 stations ~mav) and the value mst for that station:
M mst - m av . The direct longitudinal P waves (mainly the
Card, 112

S/D41)/62/'U(- C/C 11/0 C 1 / 00-6
Dependence of t.lie seismid D207/D508
vertical components) were recorded with seismographs of type C K
(6K), C K M iM), 0 K - 1-1 (YEG IK-,M). The values of m
were calculated from m - log (A/T) + q, where A is the crustal
displacement in microns, T is the period of the seismic waves in
seconds, and values of , were taken from the work of B. Gutennerp
and C.F. Richter (Annali di Geofisica, IX, no. 1, 1956). The
average corrections were: -0.2 for the Far Eastern stations,
- 0.1 for 61beria, - 0.1 for the Soviet Central Asia in its plateau
parts, and from - 0.1 to + 0.4 for the regions of the Soviet
Central Asia with sedimentary structure; all these corrections are
in units of m. The corrections m for various stations in the
USSR were essentially the same as the correction N M for the
same stations determined earlier from the surfrce waves generated
by the Kuri.lo-Kamchatka earthquakes; here m - 0.63 M + 2-5.
There are 3 fiCures and 3 tables.
ASSOCIATIUNs Aka(,emiya nauk 6SSH, Inatitut fiziki Zemli
(Academy of Scienc-es IJ66R, Institute of
PhYsics of the Earth)
SUBVJTTk,D: May 2, 1962
Card 2/2

L-244S,1-66 Ma(l) _Wkih) OW
JCC N~, A 09423 SOURCE CODE: M'0020/6r)/16B/006/1338/1341
AUTHOR: Fasechnik, 1. P.
ORG: Institute of Physics of the Earth im. 0. Yu. Shmidtj AcadMV of ScijRcg3 SSS
(Institut fiziki.Zemli Akademii nauk SSSR)
TITIt: Determination of frequency dependence of the absorption coefficient of longi-
seismic waves in the earth's mantle
V
SOURCE: AN SSSR. Doklady, v. 166, no. 6, 19BB, 1339-1341-
TOPIC TAGS: seismic wave, upper mantle,. abiorption coeffiaient, longitudinal wave
ABSTRACT: The amplitude spectra of F~ and P waves -as a fmiction of epicentral dis-
tances (a) were Investigated on the basis of seismic data obtained In the Soviet Unior
and the USA from nualear tests conducted in Nevada In 1956. In order to use a method
developed by Berzon, et al., (IM), the following assumptions were made: 1) the at-
tenuation of % and P waves due to absorption is expressed in terms of e-oh, wbere a
is the coefficient of absorption, frequency dependent-, 2) the soil and structure of
the earth's crust.at the points of observations having various epicentral distances
(A) are Identical; and 3) the absorption in the lower mantle may be characterized by
Card 1/2
UDC: 550.346

L 24481-66
ACC Nib APSOD9423
I
,the appreximate moan value of the coefficient of absorption (a) Independent of depth.
The spectra of Pn and P waves were calculated on a computer usir4g the parabolic Inter.
polation method for frequencies from hundredths of a hertS to 20-30 hertg. The data
abow that 1) the coefficients of absorption, a and sg, for the upper mantle and
P"
lower mantle,, are linear functions of ft%equencyq wbere o~ and a. pertain to the P "
and P waves,, respectively; 2) the values of absorption coefficients (V) and Q(wlv)
.for the Fn wave determined by various methods abow only wall differences: 3) the
values of tb Liabsorption coefficients for the F waves given In this Investigation are
apprculmate ir4g to velocity changes in the mantle as a ftmetion of depth; AL) the
study of the spectroi of P, PP& PbF., PXP$ and other wave I-Mos is necessary for the
evaluation of, the aNiarption coefficients of definite depth Intervals of the mantle;
and 5) the more precise evaluation of a values ft, 0*2 ft 0.05 cps frequencies re-
p
quires the study of meismograss obtained from higb frequency earth quakes. Presented
by Acadexlcian..D..'L, Sbr-berbakov on 9 June 1964, OrIgi art. has: 3 figures.
SUB COM: OB/ SM DATE: Wuns4i OPIC REF1 001/ OTH REN 006
Cwd 2/2
7

item. n~.
I A I 'T.- I, . , . .1
Inst: *1,~ fizi?,

PASECHNIE. I.P.
Science has proved that nuclear explosionB can be- detected wherev~~:.-
they tt..ke place. Priroda 51 no.7:3-12 JI 162. (YIRA 15:c')
(Atomic %,eapons-Te sting)

PASECIINIK, I.P.
Relationship beetween the seismic magnitude and vie
seismDtectonic features of the area of observation.
Izv. AN SSSR. Ser. pofiz. no.LI:1502-1513 N 162.
OGRA 15:11)
1. In3titut fiziki Zomli Ali SS3"R.
(Seismology)

ANDROSOV, B.I., kand.tekhn.nauk; BEGAGnYEN, T.A., inzh.; BERKOV, K.I.,
inzh.; BLINOV, I.S., kand.tokhn.nauk; BROYTRAN, A.A., kand.tekhn.
nauk; GPJTSAY, L.L., kand.teklLi.nauk; ZAVISHA, V.V., kand.tekhn.
nauk; KUNITSKIY, A.A., lnzh.; LFSHCHINSKIY, V.N., inzh.;
PASECHNIK., I.V., kand.tekhn.nauk; DUBCRAK, V.Kh., inzh., retsenzent;
FATOVP I.T., inzh.,, retsenzent; TU~N, I.D.0 inzh., retsenzent
[Manual for ship mechanics) Spravochnik sudovogo mekhanika.
Moskva, Transport, 1965. 832 p. (MIRA 18t12)

.%K ~ P ~" '.,
RFSHFTNYAY, V.S., dots-nt; PASI-CHNIK, I.Ya., veterin. vrach.; S~;' .... ' . ..1 . ,
veterin. vra,~.. - I
Preparation of teaser bulls. Voterinarila 41 no.1:71~-PO .-.h-
(MIPA lq;~~
1. Llvovskly zooveterinarnyy institut (for Reshetnyak).
2. Llvovskayn oblastnaye pollklinika (for Pasechn1k, ',~.nkarpv .

WBASOV, PLI., inzh.; PASECIINIK. I.Ye.. inzh.
Mechanical 014 shale dust spreader. Ugol' Ukr. 3 no.4:17-38
Ap 159. (14IRA 12:?)
(Coal m1non and mining-Rquipment and supplies)
(Minn dusts)

VOWDIN, V.Ts.: PAKHOHOV. N.M.; DMSHUNICH, Tu.V., PASECHNIK, L.A.;
BULHARIN, Te.V.; NOISETEVA, Te.l.. Prinimall uchastlye., GRISHIP,
M.Te., inzh.; PROTMATITM:ATA, Te.A.. lnzh., GOYRN, D.A., inzh.:
VINARSKIT, V.I., lnzh.; PLUTENKC. V.P.. inzh.. MOSHCHANSLIT.
B.A., nnuchnyy red.; TTAPKIN, B.G., red.izd-va; GURVIGH, E.A.,
red.12d-va; KKDVMV, L.Ta., takhn.red.
[Anticorrosive coatings for construction al9monts and appirntus;
handbook) Antikorroziinye pokrytila stroitellnykh konctruktail i
appnratury; spravochnoe pooobia. Hoalm, Goe.izd-vo lit-ry po
stroit., Arkhit. I atroit.mnterialam. 1959. 266 p. (MIRA 1):4)
1. Russia (1917- R.S.F.S.R.). Glavnoye uprovleniye po montazhu
tekhnologicheskogo oborudovaniya I proizvodBtvu montazhnykh robot.
2. Proyektno-konstruktorokoye byuro treptn Moi,trjzhkh1mznshchita
(for Volodin, Pakhomov, DeroBhkievich, Pasechnik, Bukhnrin, Moine-
yeva).
(Protective coatings) (Building m, terials)

VOLODIN, V.Ye.; EMSMVICH. Yuj.; PAUOMOV. N.M.; PASECANIK, K.A.;
BUKHARIN, Te.V.; MOISMVA, Ye.l. Prinimali uchaBtiye: UrSHIN.
N.Te., inztt.; FROTOSAVITSTAYA, Ye.A.. inih.; GoYiW, D.A., irizn.;
VINAIRSKIY, V.I., In2h.; PUTTKICO, V.P., lnzh.. MOSHCHANSKIT, N.A.,
nauchnyy red.; TYAPKIN, B.G., red.izd-va; GURVICH, E.A., red.izd-va;
KKDVMV, L.Ya., tekhn.red.
[Anticorrosive coatings for engineering structures and apparatus;
a marmal] Antikorroziinye pokrytiia stroitellnykh konstrukteii
i apparatury; sprovochnoo poBoble. Moskva, Gon.izd-vo lit-ry po
stroit.., arkhit. i strolt.materialam, 1959. 266 p. (MIFLA 12:8)
1. Russia (1917- R.S.F.S.R.) Hinisteretvo etraitel'stva. 2. Pro-
yektno-konstruktorsko.i,e byuro tresta HontazhkhiMZaBhchita (for Volo-
din, Dereshkovich. Palchomov. Pasechnik, Nkhatin, Noiaeyevn).
(Protective coatings) (Yactories-Equipment P)nd supplies)

se c

DA
F,PIIS,E G H /)/ / /~~, J- - D.
LONGINOV. V.V.; PASCHNIK. L.D.
-.- ...... , ... .
Principal laws of development of the profile of shingle beaches.
Trud.y Inst.okean. ?:135-153 153, (MLRA 7:3)
(Beaches)

qi j.
...... Td v ul -.1011 T-.q"Z-dq,j~ a rqS -qa P"
-I
'-T---T ZI .4. j
...... -qI 2.T.T.I~-i;P -j I wT-dd.
V 9 _ __::qql
P-pj- ~-TR-A 'To m,', A* dr RA
. ".T d .:1
(7-r q ) T: la
P.-
P*=;~:;?PATM,2TW.ft1-& q9
J. A4TT C- Ar&_Vff -i-A
19 "J'A
.Pz-
J. Is J. _7"q 1.1 a.- lab -3~
-(T~r RS
7ojT d 1 -q..Ia .-D J. P.., qz .. .3 d
-I-,
J.x q.4
qj. P_ (..7.-d
Td P
-91 -n
'T- 1- -1.2
q.M j. A...'a M.-di P_
A*T,(T-or R3
I. Q.11 d J* ... do T.,"a .,, I
~a Ail-.a .1 .111 I.._: - -bT-jwT1, ~v
A n O_W P.! u 7'.. , .q2 In ;. A.":TuTx
-ql AQ r=~Zp .,u Jzn",,
I.:::, (.CT - 6CCJ dd
'Q -N 't TOA -6W 7
O.T..A%:-dT2
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21 (7
AUT. HORS: c ~, I rY. L.
I TI, E'
'isma 0 3C In t rassc~~ piny- 4
11--'RIODI C-',L ~r~ t;~ n,,y i t eore t i c f
A3=~ C--: In the 'i :r severa 1 pape rs dea.. ne r.: s.,
aro d i F, c-~ ssed (Rji~f s- 1 1 ) . The objec t of t he pre sen t -aT ers
t~e investij_ation of interaction between the electron team an;
a plasma form;~j r.Jt-perdently. The experinental arrangement
L-Ssentially of a glasftube anJ an rittacn-i
piece containl4nE; a pr,-be. By means of a lq,.iid mer~'-.r~ -:~a t h~ j
an,-14 aspecial anode- system a plasma was producel &.ong the
in the mercury vap,~r, th(~ density of which amourted ',o
.C9 71
1-5-10 cm kmercury vapor pressure p :rr,.
An ox--ie cathode served as electron source. First, charac-
teristic all various (sinall) currents I e of the electror. beam
Card -~---as --,vestiEated; figure 2 shows the dependcnce C~
f -ne

sov,156 - 56-.,.' -0,'70
The Aronalou3 ScattPri rC ,f E! tj -trDn,, and the Excitation of Pla.,;r.-,a Os,~ I . ~it
7urren t or, - he ~-r- j tag e or the ana I yzer pr-
I - va'. ~r-s of 0.0~) - ma with an anode curren* of 0." a.
E ~,O,;, ~ - )0 r.-.m) . Plasma concentration was ?, ~ ' . " . '0
'he ~ si oi.s drawn f rcr-. he course of t ne c.. r Lz-,
Lhe.n m?na c f anoi-,.a , --,is s( at eri rig are di sc ;ss-d Th~ i n e 7 .
- ,I C)~ Nas f . rs ! c bserved by Langmui r (Ref " " , :- --,S: S* S
ci r,', e in the f a.- t ' 'hat u lec trons whi ch have pene t "a .1 r, C,
I'lasma partly have hirsh vellocitiQq). Figure '5 s~,I-ws ~-,e d
endcnce hk,. re'.u~ive quantity cf anomalously f it s
On t~O ~0,91t OT-1 Of Ov. probe (again for different T,, vzi-.
The ~f *~L, current is di~,- ;tri il;
fcr i . ff~?rent types of catholos tin i I i f f
curr~-n'--- and plasma densities I and 4,. . Th- f I W
lim , -I m
chapter discusses excitation and ext-nguishing ~f s m~ a
cillat.or,s occurring as a results of interaction ~ t
r. beam ani ~)-,(? plasma. Figure 4 sh:;ws t~,, srEtl . fl
,f at various I 41'd T. s
e
CPrd 2/4 1 13 rn~i, K - I.Ov. F,.k-,,~re ') shows oscl!

SO V.
The Anomalous Scatloi :f --1-ictrc, 9 tne Exci~'
d,~ 3 -, r, Lt v;iricus --va:ues ar.d
Fi6u rL 6 shows t Ke depondence of wave I engl r. an I s c
inter.sity on 1 ;in J f i gU r e 7 f J r, a' 1,) shcwq ti-.ea r. y
a
distr. t. )n cf csci ir. the eleo tror. n e a mt- on e
the plasma for various I a-values. In the fo: lowing, *he- f
t xorcA 13od by (kri (]X torrial [nit Kn e t' I Cflo A (Irl'ti"tol par'll:
to the electron boam is d1scuoned in short. FlKuro 8 Oh,)-W5 t he
dependence of the position of the oscillation zone and of tre
scattering zone on the wave length of the observed electr~-
magnetic oscillations (I increases linearly with-k.', fieure 9
shows the dependence of the position of the scattering z~r.e
A at 2 electron energies, E = 41 and 28 v. 11 also grows
1y with ek, the curve for greater E is somewhat steeper. Pgure
shows the same for ~,-values corresponding to a certain p--asma
concentration. A discussion of the results obtained shows that
the effects observed may be explained qualitative'-y Icy tree
fact that electrons are assumed to gather in clusters and that
C Fir d 3114 these clusters coherently interact with the plasma. The

SOV/~b ~6 -,; 1 0,~-10
The Anomalous Scattering of Electrons and the Excitation of Plasma C s c ' I '~'. * . - '. z
F,t,-; t ho r P, f . ria: Ily t ~ ank N. D. Morgu I , s f or 1,, rj,~ li:;,, I ,Iv :- .-, . * i .
T he r e are '0 f . 6,; r~~ s, 1 t ab'. e, arid ' ') ref ere r' ~~ ~. ~~"4- ~ w ~. . --. r.
are So,-iet.
ASSOCIA7'ION: I n 9 t i ! -.i * f 1, -, i k 41 Ak a d e m 11 n a u k U k r a Ji n a k c, y SS R ~'p 1-. y s '~ ':.:; -, " ! " -
of the Academy -f Sciences, Ukrainskayn SSR)
SUBMIT TED: 0': 1., --, be r " C!,"e
Card 4/4

3', 7 7
61-5-0
5/056/60/0,
B006/B07O
AUTHORS: Gabovic.-i, M. D., Pasechni-k- 1. Yazeva.- V ~_3
TITLE: DeteCtiDn of Ion Oscillationsl\in a Plasma
PERIODICAL: Zhurnal eksperirrental ' noy i teoret icheokoy f 1 z 1 k i
Vol. ~Ek, No. 1,1'0-1433
TEXT: Ion oscillations with a limiting frequency of fo
been known for electron beams with compensated space char,7e , 1~u t
not yet been found in the plasma of a gas Jischarge, It is ,r~ t~~e
present work that it is possible to make a diroct determination I- ~ze~f
sustaining ion oscillations in the plasma of a gas discharFe. The ex
perimental apparatus consists of a discharge tube in %hich t~~ere i.,i v Ir-
discharge in mercury vapor; the charge concentration in t~.e pl-Azima !~ t
varied by varying the discharge current. There are two probes in tht- li,;ma
one fixed and the other movable. Ti, distance between them couli be a.tc~rpl
from 0 to 1' mm The arrangement for the letec, ,ion of ion
described in brief. Essentially, it consistp, of. a pream-,,lifer, a su:er
heterodyne amplifier of' the typ(, vin 12m~lip 11 speci;ll three st~ir~p
Card 1/3 12

83577
Detection of Ion Oscillations in a Plasma S/056/6o/038/00',/010/'3;C'
B006/BO70
narrow-band amplifier, and a tube voltmeter. The sensitivity of the amp:i-
fying arrangement can r2ach - 2.10 a v, The results of measurement are sho-jin
in Fig. 2: With increasing discharge current 1, the voltage U.ut at the
output of the amplifier system increases, passes through a maximum. ;IrA *'ne:1
falls steeply. The position and the height of the signal peaks in the
Uout (I) diagram depend on the frequency f of the amplifier. Fig. 2 sh,-,'As
the characteristics for f = 1.6, 2, an 'd'2.4 Mc/sec. Fig. 5 shows the de-
pendence of the resonance currents on the potential of the probes for
6 f-values between 1.6 and 2.6 Mc/sec. Ires increases linearly with UT,robe'
and the greater f ihe greater is the slope of this straight line. (I res is
the I-value corresponding to the peak of Uout ). The follolhing relatio'n,
holds for the frequency of the ion oscillations: f - f0 /111ne 2X1,!,, 7kTe
where X is the wavelength. With this, the charge density in the Plasma 1~~
n - f2/(e2/RM - e 2f2 X21 nTe); (nexp ;7--- 1010 cm-3). It may be assumed tha
the probe selectively indicates oscillations with a wavelength that is
Card 2/3

83577
Detection of Ion Oscillations in a Plasma S/'O96/6O/O38/OO-,,'O1O,'3:3
B006/'BO7O
approximately equal to the radius of the ion layer surrounding the probe
Since the radius of the ion layer surrounding the probe increases with
increasing potential of the probe, n and I res must increase not only Aith
f but also with negative potential U probe of the Drobe, This is actually
2 ? 2
found to be so experimentally. It is also found that X < kTe /Mf . As a
practical example (corresponding to the experimental conditions), one nas
Xmax ~ 6~4-10'2 cm with To = 3.8-10 4 oK ani f = 2,10 6 cps. Such a thick
ness of the ion layer (- '~ max ) fairly agrees with theexperimental resilts
By extrapolating the curves shown in Fig. 3 for a zero potential of t.',e
probe, n 0 and Io res may be obtained; and also here theory and ex~~eriment
agree satisfactorily (Fit,. 4) It has, thus, been possible to lotect 1.,,
these experiments the OSCIllatiOnil Of ions and to verify formuln
qualitatively. V. D. Rutgayzer and K. 1. Kononenko are mentioned, Thert~ are
4 figures and 6 references: 1 Sov!.et, 4 US, and 1 Irish.
SUBMITTED: November 23, 1959
Card 3/3

20&68
S, 0--- C Do. 3
L I 04A,'B 2 0 4
AUTHORS: Gabovich, M 1~., Pasechnik, L. L , and Romanyuk, L. 1.
TITLE: The boundary o" a penetrating plasma anI plasma focus:~-.e-
PERIODICAL: Zhurnal tekhni:~neskoy fiziki, v '1, no. " 1961,
TEXT: The authors describe a probing method for determining the boundar
of a penetrating plasma "he experimental arrangement shown in F,~,~. ' c~r-
sists of a pulsed ion sour2e with electron oscillat:ons in a Magnt~tc
field. The dscharge curront attains 40 a, the on pulses have a rect-
angular shape, the pi;lse re~etiticn frequenc3 is ~O c~,s, aria tLe magnc-tlcc
field strength is about ~00 oeryt~_-ds The digci-.arges were Frodu--t ~n
hydrogen at a pres~rir- of - .'0 MM Hg Thu plasma coming fror. tnk2 nc'_~rce
Passes through an operiang :n an electrode (9), ar-,d reache3 a lens con-
sisting of two cylinde.-9 (1C)) Find 111) (inner diameter of th,~ cylinder:
120 mm; L = 120 mm; ddstancc AL: 20 mm). Electrode 111) ~.as a negat:ve
potential of U f) = ')0 kv rele-tive tj electrode (10). A beam catcher
prevents secondary electron emsjion from elt~ctrode ~ 'I ', )Probes I" tir-i-I
(8) could be shifted The a: ~ominC from the probes was amplf~t.-i
I s_gn
Card 7

120068
The boundary of a Fenetrat*njr 3/0 ~ 7,!61 j~O' I /OC !,'~j - ,'o
B104/B204
end fed intc a peak Feneratcr The output signal of this p-~ak g(-,neratrr
was conveyed to a recorder. wl:ero~y the spatial distribution of tl.e ;-rcr-
current could be r-corded, Fro-- the ax-'al and radial distribu*icrisol'
plasma parameters near the )penlng, Ahich are shown in FiEs. 4 aric,
it fo)low,,3 that an increase of the neVative potential of electrod(-
up to U0 . 50 kv prodj~-.q nr effect uyon the distribution of' th,2
parameters, At a ereater JiFtanc(~ from the opening, determinaton off tne
plasma parameters is mcre The authors conf'-,ned therriqf,"V,~~l I
determining the plasma ~,)uroary. tirid, for this purpose, they applied i~
potential cf 100 v to the jrcbe relative to electrodes (5) and ' 'q ) j-, r.
probP -urrent wan aatomati-,illy recordel In this way, a plasma ool.~nalar',
could be clearly deterwined. Th,s bcundary is at a distance of ab-,il,
10-15 mm from the opHn:n~7 anj mundfests itself in a cnariLce in the -~.l
of the probe current Up tD approximately 10 mm, tte probe current '-s
exponentially-, at larrer d- 'stances a greater drop occurs 1,FiC, 6 ,'- Ir~
this way, it is possib', to Jetprmine the plasma boundaries for vr'--q
conditions. As may he seen from a close study of the plasma boun,,ar,-C-S,
the shape and position of -it~ plasma boundary ch6nge with a chang'd -I
U.1 which is equa: to a change I p !he focusing properties of the, sys*~m
Card 2// 7

The boundary of a penetrating ...
5/05 61/oxi/ooi/c,,3/0!7
B104X204 /
If the plasma boundaries arc- simulated with metal electrodes of correspond-
ing configuration, it is possible, conditions being suitable, to constr~;ct
the ion trajectories (Fig. 9). From this figure it may be seen thtit b,,-
increasing the potential and extending the plasma boundhr.N', the ion currert
focused in the bean catchE?r may be increased. Fig. 10 graphically re.-rre-
sents the experim6ntal dependence of the ion current on tho- potential
u0. There are 12 figures, 1 table, and 7 references. 4 Soviet-bloo and
2 non-Soviet-bloc.
ASSOCIATION: Institut fiziki AN USSR Kiyev
(Institute of Physics AS Uki-SSR, Kiyev)
SUBMITTED: June 1, 1960
Card 3/ 7

27166
S/057/61/031/009/006./Si~
BlOAIB102
AUTHORS: Gabovich, M. D , Pasechnik, L L and Lozovaya, Ye. A
TITLE: Discharge of a plasma with high concentration of charged
particles into a vacuum
PERIODICAL: Zhurnal tekhnicheekoy f iziki . v.. 31, no . 9, 1961 , 1049- 1056
TEXT: The authors studied, by a probing method, the spatial distribution
of the parameters of a hydrogen plasma with high concentration of charged
particles (about 1015 om-3), The plasma was produced by a pulsed
disch.:rge, the amplitude of the discharge current being about 50 ka The
oscillation period was about 25 Peso, the battery of condensers had 90 Af
capacity, and was charged to 3 kv, The most important parts of the
experimental arrangement were the plasma source (discharge space with
3 electrodes) and the empty space beyond the hole in the lowest electrode
(cf. Fig. 1), where one or two probes could 2be shifted. All measurements
were made at a hydrogen pressure of 5.6 10 mm Hg in the source, and
about 10-5 mm Eg outside the source In all cases the oacillograms of
Card 1/6

271.6o
3/057/61/031/009/006/O,,,,
Discharge of a plasma with high, B104/'B102
the probe current were recorded together with those of the djeoharge
current. Some peculiarities turned up in the transition from ionic to
electronic current; in particular, a strong modulation of the electronic
current took place. Such a modulation was observed when the probe
exhibited a small positive potential with respect to electrode 2 (Fig 1)
Further, it was remarkable that the ionic current peak agreed almost
exactly in time with the discharge current peak, wh--Ie the electronic
current peak was considerably Bhiftedagainst the discharge current. This
is explained by the fa3t that the probe current depends not only on the
plasma concentration but also on the potential in %he probe space at the
given instant. After determining the probe characteristics, %he authors
determined the distributions of concentrations of charged particles, of
electron gas temperature, and of the space potential. Fig 9 shows
examples of radial distribution of the probe current for distances of the
probe from electrode 2 of 5, 10, and 20 mm. Results reveal that the
axial distribution of parameters is the same as in plasma with low
concentration of charged particles. The temperature gradient is here
lover than in plasma with low concentration of charged particles. In the
Card 2/6

271b6
S/057/61/031/009/006/01)
Discharge of a plasma Nith high B100102
anode cavity, the temperature of the electron gas (about 50,OOOOK) is
lover than in the cathode cavity (130,000-70,OOOOK) There are )figures
and 6 references: 6 Soviet and 1 non-Soviel The reference to the
English-language publication reads as follows; The Characteristics of
electrical discharges in magnetic fields. Edited by A Guthrie and
R. K. Walkering, N. Y~, 1949
ASSOCIATION: Institut fiziki AN USSR Kiyev (Physics Institute,
AS UkrSSR, Kiyev)
SUBMITTED: August 1, 19bo
Fig, 1~ Diagram of the experimental arrangement. Legend. 1,2, and
are electrodes; 4 is the outlet of the plasma source ( 3 mm diameter);
5 is the discharger; 7 and 8 are the probes; Cc is the capacity for
maintaining the probe potential; (A) is an amplifier, /B) an oaciiloscope
Fig 9. Spatial distribution of the plasma parameters Legend. (a)
Card 3/6

FASECOR, --L-L. [P&s:Lchnyk, L.L.]; KOZAK, O.V.
Study of the escape of charged particles from a plasma in a
magnetic field. Ukr.fiz.zhur. 7 no.lltl-165-1-171 N '62. (MIRA 15:12)
1. Institut :rizlki AN UkrSSR, Kiyev.
(:Plasma (Ionized gases)) (Magnetic fields)

ACCFSSION NR: AP4035699 S/0057/64/034/UO5/0873/OU78
AUT11011: Pasechnik, L.L.; Kozak, O.V.; Yagola, V.V.
TITLE- Magnetic confinemant of a dense current-carrying pl"inn
SOURCE: Zhurnal telchnicheskoy fiziki, v.34, no.5, 19G4, 073-878
TOPIC TAGS: plasma, plasma filament, dense plasma, plasma confinement, magnetic
plasma confinement, plasma diffusion, ambipolar diffusion, helium plasma
(1012 to 1014 cm-3)
ABSTRACT: Dense plasma filamento were formed in helium at pres-
stires from 0.1 to 0.01 mm 11g. The plasma filament cnrried n current with curront
density up to 103 A/cm2 and was located in a longitudinal magnetic field of 7 We
or less. The gas pressure and longitudinal magnritic field strength were varied, and
the radial density distribution in the plasma filament was measured. The density
distributions were compared with calculations based on ambipolar diffusion theory.
The diffusion theory accounted adequntely for the observations in magnetic fields
less than 3 k0a. The plasma f ilaments were formed in 8 tube 8 cm in ftwoder and 80 cm
long and cantaftdngShot tungsten cathode at one end and a cold anode at the othor.At
the beginning of the operating cycle, the cathode was overheated for a second or two

I
'ACCESSION XR: AP4035699
and a capacitor was discharged through the tube, thus producing a preliminary iorii-
,zation of the gas. A 5-milli.soc pulse was then applied to the mignat winding, pro-
;ducing the longitudinal magnetic field. After a dclny of I to 1.5 millisec, giving
,the magnetic field time to reach a nearly constant value, a 3-millisce rectangular
.pulse was applied to the discharge tube, producing the plasma filament. Into density
lof the plasma was determined with a Langmuir probe. There is same discussion of the
applicability of Bohm's formula to the present conditions, in which the ion Larmor
radius is less than the radius of the probe, but it is concluded that relative den-
sities in different parts of the plasma should be given with adequate accu Cy. 711(3
~
electron temperature was determined from the intensity ratio of lie II 4,,,r~ to lie
1 4713 R lines; it was found to be 5 cV, "to highent plactma density observed wnn
5 x 1014 cm-3, and the Ionization in said to have reached 100%. Tito plasma density
~decrcased rapidly with increasing distance from the axis of the tube; the rate of
decrease was greater for stronger magnetic fields. In a 4.4 kOe field the density
fell to half its axial value at 8 mm from the axis, and to ono-tenth its axial val-
ue at 23 mm. The steady-state relation between density and radius was calculitted
from the theory of ambipolar diffusionswith recombination taken Into account. Des-
solos equation of zero order is derived for the square of the density (this equntion
was also obtained by N.Rynn and N.D'Angello (Rov.Sci.Instr.31,1326,1960)) , and the
Cord
a/3

2t00
336b5
V.
AUTHORS: Pasechnik, M_-B., Pucherov, N, N., Totakly, T. A,, Chirk,-,,
TITLE: Scattering of medium-energy nucleons, and the optical mtAf.~, of tnr-
nucleus
PERIODICAL: Referativnyy zhurnal, Fizika, no. 12, 1(,161, 111, absTrart 12131,-Ai'.
("Tr. Tashkl?ntsk. konferentsil po mirn. lspol'zovanlyu ato=.
energii", 1959, v. 1, Tashkent, AN UzSSR, 1961, 103-107)
TFXT: There were investigated the angular distributions of 6.8-Mev
and 2.8-Mev neutrons elastically scattered by nuclei of B1, Pb, Sn, Cd, Ag, Zr,,
Cu, Ni, Co, Fe and Al and nuclei of Bi, Pb, Hg, Sb, Sn, Cd, Zn, Cu and Re
respectively. For medium-weight nuclei the angular distributions of elast!_-ail'y
scattered protons represented In the form IT (E))/6R(e) reveal a diffraction
structure which becomes disturbed on going to the lighter nuclei, The expe-1-
mental angular distribu'.,Ions of elastic scattering were compared with calcula-
tions carried out accoriling to the optical model of the nucleus. The
tions of neutrons scattered by Fe, Sn and B1 are not only in qualitative but
also in quantitative agreement with calculations based on the blurred-edge
Card 1/2

,FASECHNlK,--M.S.J, dokto:7 tekhn. nauk; ZHEL'VIS, A.I. kanc. , ekhr..
nauk; KORBUT, V.A.; FLATONOVA, SF:,21kll;A, 7
TSINTSIIJS, V.M. ; STRELE, L.A. , red.
(Manual on general chemistry
of analysisj Uchebnoe posobie
khimicheskim metodam analiza.
obshchei red. M.S.Pasechnika
Leningrad , 1c)65. 204 1,.
and physicochomieml methods
o obshchei khimil i fizil(o-
fijy', H.S.Pasechnik i dr. Yod
i A.I.Zhellvis (chFst' 1).
0" 1 RA 19: 1
1. Leningrad. Lesotekhnicheskayti akademiya.

PASHCHINIX, M.. B., Dr. Tech. Sol. (LIlss) "Inventic,,ation of iM'ect
of Nature nnd Physical-Meenarilcall Fropertlee of Luorlcnnte cr
Process of Plas".1c Deformation of Rolled Metal and Development
of Hign-efficient Technolo.,-Ical LuDrIcants for Cold hollln,- of
Thin-sf,eet Steel," Moscow, 1961, 1-6 pp (Moscow Petrol. En,;r. anC
-7as.Industry instiT.) 2?0 copies (KL 5upp 12-61, 2c~l).

PASECHNIK. H.S. [Panichnyk, M.S.J: KAMINSKIT, N.AjKan1nB'kyi, N.A.]
Investigating the effect of the compositiot of a cormercial lubricant
on the coefficient of erpansion in cold rolline of thin steel plates.
Dop. AN URSR no.1:4q-51 159. OAIRA 12:3)
1. Dnapropetrov3kly posudarstvenrjyy universitet. Predstavil akademik
Ali USSR A.P. Che".arev.
(Rollinp (Metalwork)) (Imbrication and lubricants)