SCIENTIFIC ABSTRACT BEREZIN, V. M. - BEREZIN, Y. V.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000204820012-2
• Release Decision: RIFPUB
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: January 4, 2017
• Sequence Number: 12
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

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s/ ss/6 /ooo/oo2/oos/�

pressure field
A~TBORS: A problem of forecasting the at:,moepheriC

' ~tmospheric pre. s_ =~.~tem of hydro Y~ infinite as regards the
.... The Pr�%lem~_i~sas an ideal fluid,
TEXT: The. .~_n\ the comple~u ~J- the ai~ m~sse8 re m~inl2 .trdns~erre~
_ _-ordinate P~n~o ~--bere
approxim~xu ~

where '/~%etiO proces~. +.he ooordin~ !~c equations ~"---tion of the
as ~n a~-~ ' ~ss~ge ~u_~_. nf h~6~�~Yn~m~erential equ~ __ .~t~ins
(-~ V. Afte'~ a ~ -~ial s2s~'~-- - ~arti~X u~-- -.--m~tion, on~ ~-
~' lineari~ed, x~tem furnis~es.~.[.Oarson trans~u' -

, %oun~ ~' '_ from,.whiCn,'-- -
so%olev t~e , � ..~::

'~..(, ...',.

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',A prololem of forecasting the ..-

o~e o%~a~ne

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A problem of forecasting the ...

s/ eo/s2/ooo/oo2/oos/o,
B125/B102

X sin ~ sin ~ . ' .
~ ~ � ...... (12) with

oo

where X2= p2d2mn/kpt' 2+12,) wi~h ~2mn = '~~,., F(m2/L~) + ~2/L~]'
solution ~, o~taXnea ~ inverse ~aplaOe transformation, contains improper
. inte~als of Bessel functions with respeot to z, and of trigonometrie ~d
Bessel functions with respect to time. For a given time interval

The extensive

tara 3/4 - ..

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A ~roblem of forecasting the ... B125/B102

/Xt . t - to, this solution can be obtained with a wide ~tep and
electronic computers.

A$sOCIATION~
~ SUBNITTED:

!

Kafedra fiziki atmosfery (Department of Physics of the
Atmosphere)

May 22, 1961

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~umerieal ~al~alatian of the a~mospherio pressure fi~,~ using the
oc~.p~.e%e s~s%ma of hy~ro~amic equations. ~es~oHolkou~. ~ro3= .

1o ~afedra .fi~ztki a~mOs�ery ~skovskogo umiversitetao

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OF, SSZO zehoz z 7 s/o o.V6 /ooh/ooz/o z/oz 6

AUTHORS: B~ezin, V. M.; 8h~r~, ~u..

TITLE: Co~uting the ver~ic~ dietri~tion of at~pherio ozone

~UP~EI Oeomagneti~m ~ aero~a~ v. 2~ ~. 1~ 1~ ~1-~6

TOPIC TAGS: ,ozone, at.spirit ozone, vertic~ ~ibution, ~po~ere,
stratosphere, turh~ence coeffieient, antl~c~one, ~clone, ho~zont~ ozo~
gr~ient

~T~CTt The ~thors ~ve ~s~ the~ wo~ on average ve~ic~ ozone ~ributi~
above ~osa. The d~fgre~e sch~

(where [ a~ h represent steps of t~ ~'-~ cook.be, i a~ J, the coo~te
a~ time n~ber of the st~, ~ the ozone den~ty, D the coeffioient of t~b~ent
diffusion, w the ~e~c~ v~boity of the ~r~ a~ ~ - ~ ia a coefficien~ ~u~

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to the reciprocal value of t~e f~r half restoration of l~otochemieal equil~ztm)
satisfactorily describes P�asiBle ehan~ee in vertical o~r~e dircribution,
is confirmed particular~v by sample conputation of cec~ distribution with
zero initial distribution. The coefficient ~f turbulent diffusion in eon-
bination vith vertical velocity has a fundamental effect ca ~.lminution of
tOtal ozone content during ascending currents and c~ increase ~uring
scend~ing currents. C~nl~Atatiaas have sh~n that~ when there'ls no ver~lca~
velocity, diff~sion has no noticeable effect on tbs distribution of: ozone.
I'~en turbulence is insignificant in the tropoal~ere and lover stratosphere
durin~ ascendin~ movements, rye secondaA~ maximums of concentration appear
at l~l altitudes. These maximins fuse into c~e, weakl~ ~efined~ when tur-
bulence increases. Descending movements, especially ~urin~ increased
l~ulence, do not favor develolxnent of seeond~r~ maximt~s, The �
Pre~ence of ascendin~ and descen~in~ currents in cyclones aml anticyclones
lead~, to acc~nulation of oza~e ~ an~ decrease in ozone downward in the
cyol~ne. The re~er~ ia true in the ~ntl~yalone. ~1 ~ &~ve r~,e to & '
horizontal ozone ~m~lent over exten~ive re.~ona sn~ also to a ho~zontall
~rm~ent vith~n ind~ue~ Layere. 0r~. ar~. has: 2 figures, 2 ta~..le?,

Card ~'/~

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SUB 'CCI~E: AS. Pit NO I~F SOF:' 006 O2EER: 00~

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New metho~ for cl�terminin~ r�sidu~l w~te~ content in rock
samples, Trudyl~FlJlI no,2~128-131' ~57, (MI~A 12:1)
(Rocks--~nalysis)

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~ZIN,

� ev nethede for deternintn~ oil content in rock samples, Trady

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SOV/124-58-10-11337
Translation from: Referativnyy zhurnal, Mekhanika, 1958, Nr 10, p 92 (USSR)

AUTHOR:
TITLE:

Determination of the Amount of Oil Displaced by Water From
Cemented Rock Specimens (Opredeleniye nefteotdachi obraztsov
stsementirovannykh gornykh porod pti vytesnenii nefti vodoy)

PERIODICAL: Tr. Ufimsk. heft. n.-i. in-t, 1957, Nr Z, pp 140-154

ABSTRACT:

An account of methods and results of laboratory experiments on
the determination of the amount of oil displaced by water under pres-
sure. A great deal of attention is devoted to the Preparation and
mounting of specimens in various types of core-holders, as well as
to preparation of a special simulated petroleum. The amount of otis-
placed oil was determined by the volumetric method or by the method
of drying followed by a calorimetric analysis. The experimental re-
sults are arranged in form of tables and graphs representing the oil
yield as a function of the water/oil factor. Bibliography: 5 references.
M.V. Filinov

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B~EZIN, V. i~., Candidate Geolo~-~Lner&lo~ Sci (dias) -- "~t~s ~ de~-
ation ~ the c~acter~atics ~ t~ ~itial oil~-water ~t~ation ~d oil
yie~ off pr~ti~e r~k ~ t~ ~oni~ ~d C~bo~ferO~ dens,ts ~

~a~ 1~. ~ ~ (~n ~r ~ U~ ~she~ ~d~trial Inst ~ V. V.
~hev, ~a ~trole~ ~i Reo ~st ~I), ~ copies (~, ~ ~, 19~9s ~)

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~1o~1e~1oooloo~1o~281oo~3~,

AC~C;$SlON N~: ,~3009Z,87
AUT~0R: Berezin, V. M.

TI%E: One boungsry problem in atmospheric pressure �o~ecasttn~ accordin8 to a
complete system o� hydrodynamic eq~lo~
SO,CE: ~ ~sc~. Untv~rs~et. Veotnik. Seriya 3. FiEld, as~ron~lya, no.5, ,. '
1963, 28-33
.

~PIC T~S: press'~e, a~spheric press~e, ~ather forecasting, hy~od~Lcs,
hydrod~lc eq~cion, a~spheric d~tca~ wind, ~eos~rophic ~tnd, aco~Cic
vibra~ion, at~spheric c~ren~ air c~rent, ~teorolo~

~CT~ ~e d~elop~n~ of n~ ~hods of weather ~o~ecastt~ based on solution i .
o~ the system of i~i~ial eq~ions o[ a~sphe~ic d~ica rather than ~he
Cion of equa~io~ of ~eostrophtc wind Is ass~ ~reat ~orCance. ~e ~eneral
approach Zo ~he solution is a dtrec~ con,ink,ion and develo~nC of the n~ical ' '-
~chod o~ iorecas~t~ aa pro~aed by L. Rlch~on. A syste~ of hy~od~c
eq~io~ is' ~ed, and ~ i~lu~s acoustic vibra~io~, t~ vertical c~n~
of wind rellim, ~ ~ iolu~l~ o[ t~ p~blm should ~ appli~ble ~o f~e- ..

Co;d 1/~ ....................................................

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ACCESSIOH.HR: ~3009487

c~oCa of ueCeorie �ields hoed an equaCianl of h mechanics of �
liquid'. It &Isa takeo into account the vejt-eaot ~ranofer and ~rinse and ~nt~ial
condielono. Ic uoeo ~he system o� initial equations a~ :proposed by A. IP. Dyubyukl

~here u, v, v are c~o~nh8 o~ wind ve~i~ 8[o~ ~o xo yo
Coriolto~ p~am~er, goacceleration d~ to Sr~i~ ~,e~ul~ ~el~i~y o~ the
earthto rotation~ ~ sl8~ltu~, In pr~lo~ pa~rl ~ ~uk and ~sin, the

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: '!Card 3/4 '~. "

~CCI~SSION NR: AP3009487

~riple inte~;rals. The pr~ed~e f~ solution on an elec~roni~ c~uter pried to
, be rather c~plex. In thiu article the solution ia sought in zeneral fo~ for
mr~inal'p=oble~. ~e problem Is solved for d~iations st un~ functio
� the{~ vaXueo defi~la ~ the 8e~ral vest-east ~ano~er, ~e existence of ~a ~st- -
east:.~an~ter In tho ~ddle letitudeo and ouperpooition st the ~n~ on
~ 'basic cu~ent' ~e aoo~d. ~e solution ~s ~or a closed l~LCed vol~. [~e
', ~ield i8 calculated on an elec~onic c~uter ~ith a larse ~

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S~: DATE A~Q~ 08Nay63. KHCL:
SUB CODE~ HR~REF $OV~ O0 OTHK~**

~O~SIO~ 1~: AP30Og&87

and 2

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Calculation of the vertical distribution of atmospheric ozone.
Geomag. i aer, 4 no.1~131-136 Ja-F'64. (NRA 17:2)'

1. Fizi6hesk~y fakul~tet Moskovskogo gosudarstvennogo universlteta.

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KOVALI~O~ K.!. ~IN~ I,L,I BI~IN, V.M.~ ~ANTELEY~,

Incre~g the oil ~eld of ~s by ~Ject~g c~at~ water.
Neft. khoz. ~ no.ll~ N '~ (M'rRA 18~2)

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ACCESSION NTt: AP4033638 S/0188/64/000/002/0079/0081

AUTHOR: Bereztn, Y. M.

TITLE: No~linear boundary problem ~f foreoasting the field of atmospheric pressure for a
lira/ted spaoe

SOURCE: Moscow. Universitet. Vestnik.-Seriya Iii. Fizika, astronomiya~ no. 2, 1964,
TOPIC'TAGS: meteorology, weather forecasting, atmospher/c pressure

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ABSTRACT: In weather forecasting the central problem usually is precomputation of the
field of atmospher!c pressure. Two approaches usually are used for this purpose: the
Cauchy problem is solved for an unbounded space or a boundary problem is solved. In this
art/cle the boundary problem is solved for forecasting the field of atmospheric pressure,
using the full system of equations in hydrodynamics proposed by A. F. t~ubyuk (DAN SSSPb

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ACCESSION NB: AP4033558
12_.~3~ No.' 2, 1958).

{1)

where u, v, W are ~e wind velocl~ component, ; is aceeleraUon of ~a~,~= 2~ s~ ~
is the Coriolis force, ~ Is ~e ~l~ veloc~ of ~e e~'s ro~tion, ~ is la2~de. ~ ~e
loc~ problem It ia ~s~ed t~ = co~t. It ~so is ~e~ed that T = T' + To, where To
, , q = B + ~, where p is press~e, Po =
1000 mb, B Is ~e ~: co~t~t, A is ~e ~erm~ eq~v~ent o[ wor~ c2 - ~. ~en t = 0'

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ACCESSION Nit: AP4033638

System (1) can be reduced to ~n lntegro-dffferential system by its solution relative to u, v,
w, Q, expressing them through Fi. It As easy to show that system (1) can be reduced to the
equat/on
~ "1 c~ . 'o~'
1.t~'�
where ~are nonlinear terms. If it le assmed that c-~,0, equation (3) can be written

~'~;-'. ~" . (4)
and t~s equation wi, i ~, us~ for pr~oSUo pu~ses'[ *he ~r0blem of pre~oU.~ m~ n~,d
Q using equation (4) for an unbounded space already has been solved. However, computations
have shown that use of an unbounded region for forecasting leads to consid:~rahle complexit/es
when obtaining a solution on electronic computers.: Equation (4) therefore will be used for
'forecasting the field Q with boundary conditions. Due to the nonlinearity of the right-hand
side of equation (4) thq problem will bo solved numerically in time steps using initial data
for the field Q for twO'times of observation. It is assumed that the solution obtained ana-
lytically will be correct for each time step. The solution for each step is found by solution

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ACCESSION NB: AP4033638
i , ' : ;; .
of the linearized problem, using tho ~nethod'of separa~tom'of variables. The sOlution is
obtained, in a spectrum of harmonics; as a result of the no.~linear terms tho problem must
' be solved numericall~ ,with time stepS as:indicated. *~The:author thanks Professor
A..F. Dyubyuk for valuable advice and a~tontion to the wo~:k." Orig. art. has: 17 formulas.
ASSOCIATION: Kafe6ra flziki i atmosfer~*, Moskovskiy universitet (Department of Physics
and~ the Atmosphere, ,Moscow Unl~er,sity),i .~ :

SUBMITTED: 22Jan63
sUB CODE: F~

h ~

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DATE ACQ: 30 Apr64
NO REF SOV: .005 '

;r : l: :

.i

ENCL: 00

OTHER: 0,00

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~EREZIN, V.M., kand. f~l.-matem, nauk; SHAFRIN, Yu.A.

Some results of numerioal analysis of ~he vertical distribution of
ozone. Meteor. I gidrol, no.6~23-29 Je '65. (MIRA 18s5)

1. Moskovskiy gosudarstvennyy universi~et.

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BE]~EZIN,

Prof. A.F. Diubiuk. 1.895- ; on h~s 70th birthday.
Fiz. atm. i okeano 1 no.?~771-772 Jt '65.

Izv. AN SSSR
(nRA

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are solved by L~placa~arson transformations. Tho solutions turn out to be vari-
ous coabination: of influence (Green) functions which can be expressed in
of zero order Bessel functions and Struve functions. The behavior of the Green
functions is investigated by the numerical "step" m~thod for times up to 12 hours
and for 0 ~ r/~{ ~ 1 (r is the distance from the observation point, R is the gas
constant). To solve fei' the pressure fields, it is necessary to know either the
components of the initial Mind velocity and the temp:mature field, Or the initial
pressure function and its time derivative. The equilibrium of the pressure field
involve:~ an integral-differential equation and is solved by "time steps" in a
method eh:ilar to that used by I, A. Kibel' and i. F. Dyubyuk, The technique is
applicable to mountainous regions where there are large vertical ~inds, which
play a substantial role in determining orographic cyclogenesis. The author thanks
A.M 0bukhov. and A~ for their assistance, Orig, art, has: 2 figures
and 12 form~t~?r 4 ~,

ASSOCIATION: Moskovskiy gosudarstvennyy univereitet (Moscow State Univers~t~.)

SUB~AITTED: 20Jan65 ENCL: 00 SUB 00DE: ES, MA

NO REF SOV: 007 OTHER: O00
, _c_ ~_,.a_.. ~'~ ..........................................

� - : ..'- u': -..-_ ,

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~PIC TA~: meson ~, K m~son, pi
..... ~ KO and K~-meson~.~s ob-
. ~ the ~asse~
....... '~e value of the ~ffe~nce ......

KO_mesons ~ a ~ ~ ~2-~-- ~ ~he ~J.s of
aid of a m~tic ~ect~e~ ~'"' ~he ~e
~t~een its m~nt~ ~d the ~ction of ~e ~ ~ ~ gt~n, In ~1, 196

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- 'L 1962-66
iACCE5$IO~ NR: AT502#122

!S. Ya.'~ikitin fo~ ~ei~ ~te~st ~ the ~k, L. B. Ok~~ and I.

}the operation of the accele~tor~ ~d A,_~., ..~a,~oY, V. N,. H~ktZO~,
iV, ~. Kuz'~e~o~j ~d Yu. S, ~shnlkov fo~ ~etstance ~ setting up the'
i ~'~~i~ out the-~a'~t~;',, ~tg. a~t. ~s~. , fig--s,
~ ~S$IA~: hstitut teore.tiche~o~.i ek~rimen~ ~noy fizZ, ~stve~-

~~D. 16Ap~5 . -: ~C~. ~

ilo REF SOY: 005 OTHERt 005

212 '

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Short-range forecasting of the barie az~ kinematic fields off ~e
a~s~ere ~ the c~etq sys~m of ~uatio~ of h~rod~ics.
Izv. AN SS~. ~i,. atm. i okea= 1 no.81781-?~ A~.18,9)''--'
1. ~oskovs~ gosud~s~ ~versitet ~e~ M,V.~onoso~,

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Autokon: Vis~mevsk~ ~. Ye.; CaZan.l~.; S~M~_.?~. l~. A.; ~c~t~~
0~: none ~

~C ~: K ~son, ~ss s~ctr~et~, pi~, meson interaction

~CT: In vi~ of the discr~ncies b~ween the e~ent~ meas~ed ~ss ~f-
ferences of the ~ ~d ~ ~so~, the authors have meas~ed this ~ss di~erence ~ a
coherent regeneration meth~, ~sed on meas~eme~ of the dependence of the intensity
of the coher~ regulation of ~ mesons in a be~ of ~ mesons on the t~c~ess of
the r~enerator (co~er or al~). ~e ~r~nt ~s c~ied o~ ~ the I~F 7-'
G~ proton accele~tor (F~. 1). ~e meth~ ~d the ap~atus ~e brief~ described.
~e ~ mesons were r~i~ed ~ me~s of the ~ + ~+ + ~- de~ay with the aid of a
~etic s~ctr~er with scinti~tion c~ters ~d s~rk ch~bers. ~e distribu-
tions of the i~eraction ~e~s with res~ct to the ~sses of the dec~i~ ~icle
~d with respect to the ~e b~een its moment~ ~d pr~-be~ d~ectio~ ~e
give. A t~ of ~ coherent-regulated ~ mesons were fo~d ~ 375 t~c~. A
~ss di~ere~e of 0.82 i 0.14 (~vlc2), where vi' =.0.~ x ~-xo sec, ~s obtained.
~e ~strib~ion o~ the ~egiat~ ~ ~so~ ~ a ~ at 1.8 G~/c ~ ~
mo ze~ at 0.9 ~ ~ ~/c. ~s ~t ~ees we~ with those obta~ed ~ ~hers

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F/g. 1. ~:t~enta.l. setup, a-
Beam dtagram~ ~ -magnette spectro-
meter diagram (*F~e mmbers denote
lx~ttcle counters)o.

using similar methods. The authors thank A. I. Alikhano and S. Ya. ~iki~in ~or in,
terest in the work,_~~_and I. Yu. Kobzarev for discussions, ~
his crew for oper~2ing the accelerator, and ~'-l~as~ V N~_~Markizov, N~
V. F. St~ V. N. Xuz'menk?, and Yu. S. Oreshnikov for help with the appa-
and the measurements. Orig. art. has: ~ figures and 1 formula.

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8 (2)
AUTHORS:

TITLE:

PERIODI CAL:

ABSTRACT:

Card 1/4

Tayev, Ivan Sergeyevich, Candidate of SOV/161-58-4-13/28
Technical'SCiences, Docent, Berezin, Vladimlr Nikolayovich,
Senior~En~lnee~ ~

Experimental Examinations of the Processes During Extinguishing
a Free Alternating Current Arc (Eksperimental'noye issledovaniye
protsessov gasheniya svobodnoy elektricheskoy dugi peremennogo
toka) I

Nauchnyye doklady vysshey shk�!y. Elektromekhanika i
avtomatika, 1958, Nr 4~ pp 96-99 (USSR)

Some results of examinat~m~s, of the arc which forms on the
contacts o� a device during the switching-off of small current
intensities (5-130 a), at voltages of 127-700 v and a
frequency cfSO'c,are given here. These experiments were
carried out in the Laboratory for the Construction of
Electrical Apparatus of the MEI. The examinations were mainly
made to establish the conditions which are determined by
those parameters of the swi2ched-off circuit and the switched-
off apparatus, where the alternating current arc is extinguished
at the first zero crossing. The diagram shown on figure 1 was
used for measuring the burning time of the arc. Figure 2

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Experimental Examinations of the Processes
During Extinguishing a Free Alternating Current Arc

=ard

shows a diagram which gives the dependence obtained by
experiment of the critical characteristic frequency fo of
the circuit on the phase-shift angle ~ at constant voltage.
for various amperages of the switched-off current. These
curves enable~hoosing such parameter combinations for the
circuit to be switched-off, where the extinguishing of the
arc is guaranteed during a half period. Figure 3 shows the
diagram for the dependence of the number of re-strikings of
the arc in percent on the time of the contact o~ening t o
P
This curve is of a statistical character, having been obtained
through numerous experiments. Fromthe point of view of arc
extinguishing, the time of contact-opening t = ( ~ ), which
P
lies in the center of the half period, is most favorable. On
the other hand, the opening of the contacts at a time when
the current curve approaches zero9 eliminates almost entirely
the re-striking of the arc. The cathode oscillograms for the
returning voltage obtained during the tests, allow the
determination of the amplitude coefficient K . K represents
a a

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Experimental Examinations of'the Processes During
Extin~xishing a Free Alternating Current Arc

sov/~6~-58-4-~/28

� Card ~/4

the ratio between the maximum of the returning voltage and
the returning voltage with industrial frequency, If Xa and
the circuit parameters are known, the remaining resist~Ace
r of the arc column can be determined. Based on the
s
experiments by Professor O. B. Bron, it was found that for
guaranteeing the arc erasion at high amperages, it is
appropriate having not too great contact gaps. Besides, it
was established that it is ~lso appropriate for the
switching-off of low amperages to have small contact gaps,
which is illustrated on the diagram of figure 5. The
dependence of the initial strength of the gap on the
amperage to be 4witched'offp for various contact materials,
is shown in the form of.a curve on figure 6. The experiment
made here, showed that repeated zero crossings can occur
within the range of the examined ampera~es at a voltage of
220 v, provided a high characteristic frequency of the
circuit (some dozen kcycles) and a great amplitude coefficient
(1.~-2.0) exist, and contact materials with a small initial
stress (silver-graphite, silver-tungsten, copper) are used.

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Experimental Examinations of the Processes During
Extinguishing a Free Alternating Current Ara

SOV/16~-58-4-~/28

At voltages of ~80 v, currents below 10 a break at the first
interruption (copper contacts). There are 6 figures.

ASSOOIATION~

Kafedra elektzoapparatostroyeniya Moskovskogo
energetioheskogo instituta (Chair for the Construction of
Electrical APparatus at the Moscow Institute of Power
Engineering)

SUBMITTED: July 5, 1958

Card 4/4

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]~EVIN, A.A.} BEREZINz

Mechanized cutting of rolled paper and rolled cardboard. Med.prom.
16 no.4~42-44 Ap '62. (MIRA 15:8)

1. Medi~o-instrumental'nyy zav~d "Krasnogvardeyets".
(PAPER-CU'I~ING mCHI~) (MEDIAL TECHIqOI~DGY)

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BEII~IN~ �.Po' inshener~ ~0T0�e G.A., inshener.
~perience of the momt efficient lumber
5-1o ~ '5~.

NekJ~.trud. rab.? no.?:
(lg,l~. 6:7)
(~amber campm )

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BER~._~ Pavlovich; ZOTOV, Oeorgiy Aleksandrovieh;
'"~---~-HA~V, Stepan Alekseyevich; YE~0L~{, I.P., red.;
MYAKUSHK0, VoPo~ red,izd-va; KARLOVA, G.L., tekhn, red.
[Potentials for increasing labor productivity; from the
work practice of the 01enino Lumbering Camp] Rezervy ronta
proizvoditel'nosti truda; iz o~yta raboty 01eninskogo les-
promkhoza. Moskva~ Goslesbumizdat, 1963. T7 p.
(~A 16:12)
(Olenino (Kalinin Province))--Lumbering--Lab�r produktivity)

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~OV~

Appolinariy.3tepanovich~ ~H!~0, N.&.,ot~eredo ~ ~~V, P.P.,r~.;
~~V, G.'G~, r~,;~, L.F., r~. ~ ~IN, I.I., red. ~

.[~uction ~ use of soil concrete bl~ in t~ const~tion
of buiEi~e of few stories] ~oi~stvo i p~imene~l ~tobl~ov
v ~loetaz~ gtroiteleetve ~, 19~5. ~7 p. (~. Veesoluz-
~ ~uc~o-issl~ovatel's~i institut zolota i r~i~ ~t~l~v.
T~y. ~est~ stro~ter~, no.7) (a~

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red.; KAI~TBIIT, A.I., red.; ~ZiT.~TSOV, O.O., red.; ::~.TSUVEV, L.I~., red.
NUZHDIM, I.I., red,; FIRSOV, L.V., rod.; F0!'~Ei~iO. T.O., re~.;
..q~d{HNAtl0VICH, L.A.,

[Principles for makin~ geo~orpholo,~tcal prognosis maps of plae~ de-
posit s ] 0 print ~ipakh po~troenita ~olog~e~rf~logicheski~
no~;uykh 'tort roe~ypef, l~adau, 195~. ~ p. (~adau, Vsesotuzn~
n~uchno-issledovatei's~:ti iustitut zologa i redki~ metallov. T~y.
~olo~tia, no,37). (MI~
(Ore

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GAVRIEOV. Sergei IV~novich; 8HILO,,Ntl:ola.v Alekeeyevich~, otv. red.$ ~T~,
S,V., za,~.otv.red.; ~h~ROV,P.~., red'.; A~L~TSIN, F.R., red.;
B~IN, V.P., red.; ~I~, A.I., re~.; ~T~7, G.G., red.;
~~D~;, red.; ~Z~I~T, I.~., red.; FIRSOV, L.V., red.; ~t.?~ZO,
T.G., red.; ~~OVICN, L.A., red.

[Divisiou of t~,~ upper Iudi~ir~ Valley iuto t~ctonic region~] 0
te~ouichesko~ ralontro~'~ntt beeset~ vekhuego techentia r. Iudigtr~
~gadan, 1958. 17 p. (},[kTadan, Vsoaoluznyl naucbn,-issledovatel'skii
institut zolota i redkikh ~atallov. ~udy. Geologila, uo.~8).
(~i~ ~2:~)
(Indigir~ Valley--~olo~, Stm~ctm'al)

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"APPROVED FOR RELEASE: 06/08/2000 C1'A-RDP86-00513R000204820012-2

[Principles of the ore dressin~ process with uae of concentr;~tin~
tables] Osnovy proteesea obogashcbenila rud na konteentrateionnykh
etolakb. ~adan, 195~. 35 P. (~gmdan. Vsesoiuznyi naucbno-issledo-
vatel'skfi insti~ut zolota i redktkh ~etallov. ~rndy. Obogasbchenie
i mmtallur~ita, no.2?). (MIR~. 12:~)
(Ore dres~ing--E~ip~ent and supplies)

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[Structure, ~orpholo~y, and mineralization of the I~u~euskoye gold
depoeit] b'truk~u~a, ~rfolo~i~a, m~nera~o~i~a ~ or~euenie
skogo zoloto~dno~o ~storozhdenila. ~adau, 19~8. 71 p. (~a~,
Vsesoi,~i naucbno- tssledovatel's~i institut zolota i redki~
metallov. Tr~y, no,33)
(Teu~ke Valley~ld ores)

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[~LA_BIN, Ale!ssey II~loh;$1~ILO, N.A., otv.red.;~POT,~l.[~IN. S.V.;
AL~SA~ROV, P,P.;zam,o~v,red,; A~[~V, P.P., rec.; APV, L~TSIN,
"'~-OV.
F.R., re~.; ~FK0, T.~., re~'.$..BER~ZIN, ~.P., re~.; k~Z:: ,_~ . ~.~.,
,~d.; }~T~'~V, L.P., r~d.; ~Z~;'~T;I'jred;r FIRSOV, L.V., red.;
V~SH~, N.A., red.
[Umtor~ound waters i~ %he northeastern part of the U.S.S.R.] P~-
' zemiuye vody ~vero-Vo~%,oka SS~. ~adau, 1958. 85 p.
Vsesot~uyi na~hno-is~!'~dovatel'ekii iustttut zolota i redkikh uetal-
lov. T~v. M~rzlotovedeuie, uo.9). (MIRa 12:&)
(~assia, Northeru--Water, Under~ouud)
(~o~u ~roun,~)

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~fLOV. Fare! Ivaaov~ah~ ~J~, ~ee~gi~ Se~enov~ch~ SB/LO,

~.. ~z~~~.~ ~z~, ~.z.,~.; ~s~-

[F~t lifti~ by menns of e~tt~ ~hine~ in
p~e~ d~o~ts ~n the Northeaste~ U, 3.3,R,] VB~ to. or
~. 19~8. ~ p, (~n, Veesoi~ ~uc~issl~ovatel~-
e~i inetitut zolota I r~ met~lo~, T~y, Qo~ delo no,19)
(Soviet F~ ~8t--Oo~ ores) (P~t) (B~avating m~hiner~)

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SHILO,, Ntkol.ay Ale.~s~eyevioh; POTE~II~,, S.�.. sam. otv.red.; ALI~}~RO7. P.P.,
~~L ~S~N, F.~.~ E~~I~, V,P., red~: ~IN, A.I., red.
au~'~, ~.~., red., ~T~~ ~, I.I., red.~ ;
F~SOV, L.V., red.; ~0~ T~G., red;; ~~O?ICH, L~., red.
[So~ principles for c~ssif~g placer deposits] Nekotorye priutsi~
ross~nykb pr~iavlenii. ~gad~, 1~. 20 p. (~g~au, Vsesoi~u~
ua~huo-ts~ledovatel~ekii inat~tut zolota i redki~h ~etall~. ~y,
~ologita, no. 36). (~e ' (~ ~:$)
denosit s~Olaesificat ion )

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SHOROKHOV, Sergey Mikhaylovioh, prof., doktor tekhn, nauk;SBOROTSXIY,V.V.;
~BE~EZ~_~_~V.P., retsenzent; KUDRYASHL~, V.A., kand.
~~~"retsen~ent~ DIDXOVSKi~, D.Z.~ otv. red.~ KIT, I.X.,
red.izd-va; MAKSIMOVA, V.V., tekhn, red.

['Working placer deposits and the principles of planning] Ra~
rabotka rossypnykh mestoroahdenii' i osnovy proektirovaniia.
Moskva, Gosgortekhizdat, 1963. 764 p, (MIRA 16:10)

1. Zamestitel' predsedatelya Severo-Vostoohnogo sovnarkhosa
(for Berezin). 2. Irkutskiy politekhnicheskiy insti%u% (for
Kudryashev).
(Hydraulic mining)

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ANDRIANOV, Aleksandr Alekseyevieh; POTE~XIN, S.V., glavnyy red.;
� ~ATS~, L.P., zamestitel' glavnogo red.; S~L~HMAROVICH, L.A.,
red.;_BJ~~ red.; VESELOV, V,.V., red,; GOLAND~IY, D.B.,
red.;'~'DT~, V.G.,'re..d.; IGNATEt~O, M.A., red.; SHASHURA; M.V.,
red;; RIVKIN,. G.M. ~ red. ,' FIRSOV, .L.V., 'red.; b~.PE~EV, I.T. -

 'thods of analytic deoo~position of oassiterite and tin ores]
tody ana.liticheskogo razlozheniia kassiterit~ i rud olova.
Magadan, 1962. 14 p, (~gadan. Vsesoiuznyi nauchno-issledo-
vatel!skii i~stitut zolota i. redkikJl metallov. Trudy Obogashcheni~
i metallurgiia,, no.53). (MIRA 1657)
(~ssiterite--Analysis) (Tin oreS~Analysis)

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KASHTANOV, I.N., glav. red.; ~.,~J~..p., ired.; IOSIFOVICH,
N.L., red.; POT~,!KIN, S.V.s red.; SHILO, N.A.s doktor
geol.-m~er, nauk, prof., red.; FROLOVA, M.F.~ red.

[10 years of Magadzn Province] 10. let Ymgadanskoi oblasti.
Magadan, Magadanskoe knizhnoe izd-vo, 1963. 210 p.

1. DirektOr ko~Pleksnogo nauchno-issledovatel'sko�o insti-
tuta Sibirskogo otdeleniya AN SSSR (for Shilo). 2. Dire]trot
nauchno-issledovatel'skogo instituta zolota i redkikh me-
tallov (for Potemkin). 3. Sekretar' oblastnogo komiteta
KPSS (for Kashtanov).

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Results of the s~udy an the he~ of nu~g ~f~ts ~ ~-
lati~,~ ~ the~ ling c~diti~s. S~. z~. ~

(zav, - or~tsii z~avo~~i~ i istor~ mdi~y
~of. N.P. Fedora) T~o~ medits~sko~ ~sti~
(~r - p~f. Z.V. ~s~).

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TITLE8

PERIODICAL
ABSTRACT ~

Card

~J_~.~ GROSHEV,L.�., DI~AREV,V.S., PA - 2224
EOIAZAROV,H.B.~ KOHOLE�,E.N., ~ADEE�,�.~., NIEOLEYEV,YU.6.
The Spatial Distribution of the Folws of ~ -I~ys and of Slowed-
dOwn Neutrons in the Graphite. ColUmn of a Ph~sioal-Technical
Reactor. (ProstranStvennoye razpredeleniye potokov ~ -luohey
zamedlya)-u soohikh neytronov v ~rafitovoy kolonne reaktora HFT,
Russian).
Ato~naia Ener~iia, ~9~?, �ol ~, Nr ~, pp ~8 - ~22
This distribution was investi~ated in eprin~ 19~}. The results
obtained are suited also as experimental ~terial for controllin~
the theory as well as for the computation of the spatial dis-
tribution of ~ -rays and slowed down neutrons.
Experimental ~etails~ The thermal column (Rf ~Taphite) of this
reactor has a orose section of 100 x 100 om' and ~ lenEth of
~00 Omo This column ie separated from the active zone of the ap.
paratus by an 80 om thick ~aphite reflector and by a 4~ om thick
layer of a~r and the sidewalls ar~ surroundedby concrete. An
experimental channel leads alon~ ~he axis of the column, which
ie filled with ~Taphite rods. The indicators were irradiated ~n
the cavities of these 6raphite-rods. The development of the
density of thermal neutrons ~n ~raphite was measured by a

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Card z/~

~A - 2254
The Spatial Distribution of the Flows of ~ -Rays and of ~lowed-
down Neutrons in the Graphite Column of a Physical-Technical
I~eact or.
pros~ indicator. ~s an indicato~ of the reso~noe neutron,
Indi~ s~roun~ed by ca.iud, ~o1~ and Iodi~e ~ere used.
~easure~ents were o~rr~e~ out when reaoto~ operation ~d become
stea~' ~easur~n~ results of the spatial d~spers~on of the neutron
fl~es of ~fferent energies in ~r~phite ~re shoen in for~ of
d~a~r~. The neutron fl~ is di~n~shed much ~ore at the
~~ of.the ther~l column t~n at ~ts end. The c~es of the
reduction of the ncutron fl~es c~e noticeably ~t �
of ffro~ ~0 to ~80 ca. The fl~ee of the reso~nce neutro~
~nd of the fast neutro~ are exp�nent~al~ atten~ted. The course
of the o~ve of the ~ensity of thermal neutro~ is disoribe6
quite acc~ately By an exponential relation with the relaxation
leith L - 2~,g ~ O,~ cm. Also the decrease of the dosage of
~-r~s. in a ~aphite ool~ is shown in a
Diao~sion off the resulta~ In the asymptotio do.in spatial
ener~ distribution of the alowe~ down neutrons is deter~ne6
By that ener~'which oorreepon~ to ~xim~ saatteri~ leith.
At great diatanoea( ) ~80 om) the reso~noe neutro~ are
probably produ�ed by penetrati~ of fast neutron. The spatial

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The Spatial D~strlbutton of the Flows of ~ -Rays and of Slowed
down ~eutrons tn the ~raph~te Column of a PhyStoal~eohntoal
Reaotor.
distribution of fast neutrons then determines the spatial
tr~button of resonanoe neutrons. The experimental results
rained here are essentially
(5 illustrat~ons), a oonfirmation of the theory.

ASSOC~ATIONI

SUB~T~ED
AVAILABLE~
Card

~ot given.

Library of CongresS.

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~ximum-loa~ cycle l~ the electric ~rive of a~ ingot oar.
T~dy Ur~.polite~.~st. no.lOll~3 ,60, (~ ~3)
(~ (Met~work)) (Feed

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PAL'MBVs Ye.V.~prof., doktor tekhn.nauk; BEREZI~,Ye.N.; aspirant

Intensifying the operation of ingot cars. Trudy Ural.politekh.
inst. n0.101~6-12 ,60. (MIRA 14:3)
(Rolling (Metalwork)) (Feed mechanisms)

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. B~ZIN ~e Nos ~sho
New diagrams of high productivity ingot feede ~ U~I~,
~~. ia~t. ~o.~9~1~1 '~. (~ 16~1)

S~el i~ot~--~s~r~tion)

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S/00'~ 7/63/033/007/0788/0 794
i Ab'Tff0R: Bereztn, Yu.A.

TITLE: Normal oscillations of a plasma elll~?_2~d in a uniform =agnetic
field

SOUP~E: Zhurnal tekhnioheskoy ~iziki, vo33, no.7, 1963, 788-7~4

TOPIC TAGS: plasma osoillatlon~ ma~lO

~ST~T: Tho ~requency spect~
pl~sm~ in the shape of ~ elli~oid of revolutl~ located in a ~ifo~ ma$otic
field Parallel to the ~is of sy~etry is investilat~ by a ~th~ dovelo~d in
co~ection with ~erromaletic ~soaanoe by L.~.Walker (Phys.Eev ,105, 3~0, 195~
The p~asma elli~oid is ~Su~d to have a con '
~om the vacu~ by a sharp bo~d~ .... ~tant ~e~ity ~d to be sep~ated
electric tes ~ ..........
tic pro.rites et the plasna. ~e f~equency s~ctr~
is dlsc~sod in so~e detail, ~d its de~onco on the strength of the external
~gnetic field m~d on the sha~ o~ tho ellipsoid la ~llustrated wlth cu~es ~d

'Card 1/2

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ACCESSION Nil: AP3003946

~ha~ts, As t~ ~lllp=otd do~enora~ '
~n_t~o spa=ir=. A ~O~h cond,..~_TM a.dis=, threo ~onde=,~l _
a. I. haganov (Zh~.31 ~ ..... ,,ou~zon point ~O~d f ...... ~ points develo
nation o~ *~- .... � -~ --=~ i~2) is not obtai *-.~ ul=~ b~ V.G. Ba~ P'
no~-- ~i-'"'b ~screp~cy is offor~ ~ __--~ed. ~bs~racter,s no~ ..... Y~ar,
.. '---' Aruquenclus are ~+-,--~ - -~/ 'l'ne Uispersio- ........ '~' ,~o expia-

,~ .... ' ',~- ,,ugzocte~, "Ia ~--- .... z_..~ ~ae case in whi-~ ~ ....
~or suggestin- +~- ~ . -~,,-,usx~, Z express -,, ~-- --- -,,~ mo=ion
me to ex~lne ~.. ~ ",=.mpzc, for valuable a~vt~ -f_uuep ~atitude to M,I.

ASSOCIATION: nono
SUBMITTED: 22,Tu12,62
SOB CODE: P~{ M~f

DATE AOQ: 07Aug63

NO REF SOY: OOl

ENOL: O0

.o~a: 002

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crowave ~eld, skin e~fec~
m in a unifom longitudinal
~ST~ The in~o~c~l�n el ~ axially s~etric plas .... ~o~ic field is
m~gnetic field with an axially s~e~ric high tr~uency e~---
diS~ssed theoreti~llY- The hi~ ~r~uency field is assum~ to consla~ oI a longi-
tudinal ~gne~ic iield ~d a ~verse electric lield (ext~o~i~ wave), The
case of a longitudinal high ~requency elec~ric lield and an azimut~i ~otic
has been previo~lY disc~s~ by o~hers (H.A.Boot, S.A.SelI ~d R.B.R. She~by-Ha~
~.Elec.Contr. ~5,435,~58; E.S.~o~bel,Ib~d.5~435,1958)* The ~t~on o~ ~e ions and
oloctrons is s3~rat~ ~n~o a rapid compon~ hav~ ~e ~r~u~cY o~ ~e

'extr~Ox~dinax'y rave' .... : : i~-:~:

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ACC..~R: AP4020573,

of the alternating field. The syste~ Is described by the two-fluid hydrod~namic
~u~t~ons and ~ell's equators. ~n~tud~nal and t~nsve~e temper~ure~ and
pressures are d~st~n~sh~. In the "zeroth approxi~t~on", quas~eutral~ty ~s
sum~ a~ the non-l~near h~am~c te~ ~he'pressu~ ~d~ents~ and the
~o~es due to the magnetic comment of ~he ratable f~eld are neglectS. To these
zeroth app~xim~lon ~u~tio~ is ~dJo~n~ the sum of the "fi~t app~xl~t~on" eq-
uations of ~otion avora~ over a per~ of t~e high fr~u~cy f~eld. F~m ~he re-
sult~n~ ~uations ~he ~r~le velocities a~ two of the three components of the
te~2t~n~ ~eld are eliminate. ~o d~er~al ~uations a~ thus obta~n~ for t~
plasma density ~ the azimuthal electric ~eld as ~unct~o~ of the dist~ce from
the s~etry ~s. These ~uat~on~ we~ inte~rat~ n~erically for seve~l values
the parameters, a~ some o~' the results are present~ 6raph~cally. There are two
resonant frequ~c~es. For Sufficiently dele plas~s these fr~u~c~es a~ approx~-
~oly the LanguOr ~r~u~cy a~ the ~eometr~c me~ of the ~on and electra La.or
Zr~uenc~es. ~ the ~equency of the appli~l Z~eld ~s la.er ~an the ~e~ ~r
~r~uency, ~he plas~ deputy ~noreases and ";he alte~ ~eld deceases ~
to the sy~et~ ax~.:'~e ~the~tic~L s~pl~L~ti~ ~at ~ults

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ACC.NB. AP4020571 ' -,
frequency, the extrao.~Jinary wave penetrates the plasma. In this case the azimuthal
electric field amplitude is an oscillatory function of distance from the axis, and
the plasma density increases, with superposcd oscillatimns, as the distance from tbs �
axis is increased. The cr~terion for the validity of the approximations emplOyed is
that tho olect~n velocity bo small co.~lpnrod with the product of tho frequency
the applied field and a characteristic length which ~ay be either the skin penetra- -
lion depth or the wavelength. "In conclu~ion the authors express their gratitude to
R.A.Demirlchanov for his interest in the work and for discussi.ons." Orig.art.has:

20 formulas and 4 figures.

ASSOCIATION: none

SUB!IITTED: 3Llan63

SUB CODE: PH

I~T[; .'~Cq: 31~ar64
NR REF $0V~'003

ENCL~ O0

OT~R: 002

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CTA-RDP86-00513R000204820012-2

AU~Uem Be~esm, Vu.A.
.TITLES Low.froquen�F resomt ~oll~t~-'~ ~ ~~l plu~

l~ m t~t~ An the qmAstit~o

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,~equenole~ a~e e~mz~ote~sed by ~te~e~llal. ~e m~the "p~no~l" n~er~t~an, a~ ~e

~or ~x~ ~e el~t~ ~r r~u~o~ la ~uaX ~o ~e ~r z~noy, nM ae.

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BEREZIN~ ~u.A,; KARPMAN~ V.Io

Theory of nonsta~ionary waves of finite amplitudes in a rarefied
plasma. Zhur. eksp, i teor. fiz.: 46 no.5:1880-1890 My '64.
(~HA 17:6)
1, Novosibirsk~y gosudaratvennyy universitet.

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BEREZIN, Yu.A.

Lov-frequency natural oscillations of a plasma ellipsoid.
Zhtlr. tekh. fiz. 34 no.611124-1126 Je '64. (MIRA 17:9)

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. zpsoo~a~4 '~ '
:~-_...~.-- ..-:... .... .'!'-_'.~-___ c0Dm'.Ua/o~o?/es/ooo/oos/o-o-~-e~oo~-
AUTHOR:

ORG: none
TI'I%E: Waves of flnito amplitude in a hot~
so, cE: ...... .?, .
~.., --,,.,,~u �mr, muenesiioy Iizikt~ no, $, 1965, 26-32
TOPIC TAGS: ehock wave pr.opagation, high tern ratur
rarefied plasma ~,~,~/L.~,i ,. pe e pla5ma, low
'~ V ~.-,~/ ~,~ca~. ~ ~.~.~,. tempera,t~re plasma,

ABSTRACT: The autl~or studies the struclz~re of a plane shook wave o� a-rbitraz~, force propa-
gating in a hot rarefied pla.sma across a magnetic field. The problem of the Propagation of
unsteady waves of finite, but small ampli~de is examined under
_a.u.~or also considers waves of finite amplitude in a cop .... r.the, same conditions. The
,~ucn waves is i .,~ ,,.,,~_ .~._ _~_. .... �u rarei~eQ pin-ma. The profile of
caused _by__t?~ ~,, uommear and dispersion effects, the latter being
is used ~t~stan� o~ r.~e emmtion ~ -,.-- ........ P a A system of equations
~ ~-~,~n ~ me electron and ion components of plasma~ the
discontinuity equatio% and Maxwell equations. The plasma is a~m'ned to be quaslneutral.
The author introduces into the equation of motion the gas-kinetic pressure which
nature since the distribution of ions do~s no~ have s eric
thau~ 1L Z. Sa~levev and N ~ ~ .......... ph al s~nmetry. In ccnclusion~ author
--- ....... � ~u~9 ~or

Cm~ 1/2

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assistance In the numez, loal calculations, Orlg, ~t. has: 23 formulas. ~
SUB CODE: 20 / SUtLM DATF.: l�Jun65 / OHIG REF: 004

Card 2/2

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TITLE3 Finite ~plitude cylilgrlcal ,aves In r~reri~_~}sna.~..,, i,' //

SO~RCE~ Zhurnal prikladnoy mekb~i i ~k~iclmskoy ftziki, ~, ~, 196~s 116-118
TOPIC TAGS~ r~efi~ p~s~, cyli~rlc wave, mgnettc flebi, magnetic prevs~

~T~ The propagatio~ of ~stea~.c~lt~rtc ~avos 1~ r~efl~ cold p~s~
u~or a strong ~gnetic field is ~vestigated. The plas~ is assumed to be qu~i-
n~tr~, the gas d~c press~ is neglect~ in co~a~son to the m~netic
pres~e, ~d no cessions ~st betwe~ ~ic~s. At t~e ~ - O, the ~o~
cyli~o~ pl~ of radius "a" ~d de~ity ~ is ~bJect~ to strong magnetic
fie~ ~rect~ along i~s ~s. The re~ltt~displac~ent is descrl~ by a
s~ of five ~uations, t~ee descr~bi~ the pl~motion~ t~ee ~es ~d t~
desc~b~ the ~etic i~ucttcn. The ~~co~tio~ ~e ~ven by

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eh~e f(~) ts ~ Zlvo~ f~ctio~ of tt~. The ~olution is ob~in~ n~ca~y
~ ~e re,ts s~n ~c~ly. The f~ of the~e d~lct~ the pro~tion of

o~c~l~t~ c~ract~. The se~o~ sh~ the ~a~e profile~ at ~te~d~te times.
~ave front =ov~ at the ~ve~. Zn cou~u~o~ the ~thor t~ R~. ~%
em ~c~s~on~ ~d ~for helpt~ ~ th~ ~rtoal ~o~utatton~.

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~ NR, AP60090~6 sotmcz CODE: tm/o;o?/e6/ooo/ool/olo?/ozlo

AUTHOR: ~~oslbl~

ORG~ ~o~ .". .... , ~ ........ ~..-
T~LE: ~]lndrl~ wa~s p~~g a~oss a m~He ~d ~ a r~fied pl~ma
SO. CE: ~u~ P~~ me~i~ I ~Je~s~y fizl~, no. 1, 1966, 107-110

TOPIC TAGS: ~l~ie wave, pl~ma wave P~Hon,, 'pl~ma wave, r~fled pl~ma

~ACT- ~e profile of i
..... ~: ~~~. ~ .~ in a.r~fled ~ma is ~in~le
~o eo~ie~ presses: no~ ~st~g ~d "sme~ng,, ~e to ~ersion effect.
For waves prOP~a~g ae~ss a m~etic field in a cold r~fled pl~ma ~e dispe~ion law
is such ~at ~e ph~e veloeiW of sm~ ~ciHations deep,es ~ ~c~ff len~ of
wave. Such a ~s~rsion law lea~ to ~e possibfli~ of ~e e~n~ of s~o~ "com-
pression'' waves of f~i~ ~pli~de (isol~d ~d ~ri~c). ~me au~ors ~ve i~s~d
no~t~ion~ pl~e wa~s mov~g acres a m~e~e field ~ced ~ incre~in~ m~eSc
press~e on ~e pl~ma-vacum b~d~. ~e p~sent ~or ~lies nme~c~ ~a-
tion of ~e cor~spond~g e~on sys~m to ~e in~s~on of ~l~d~e~ waves
in a cold r~efied pl~ma acres a M~-in~i~ m~eflc field. ~e ~s~ ~e ~p~t
for e~erimen~ on r~id compassion of pl~ma col~ ~ a m~etic field ~r condi-
tio~ when ~e pl~ma m~ be co~i~d s~iden~ r~fled ~ descend ~ ~ M.

~/2

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ACC NR, AP6009056 --~
lskoltdsldy, R. Kb. Kurtmullayev, Yu. Ye. Neaterikhin, and A. G. Ponomarenko
(Eksperimenty po besstolknovitel'noy udarnoy volne v plasme. Zh. ekperim, i teor. flz.,
1964, vol. 46, No. 8). The author thanks~R. Z. $ de ev and N. N. Yanenko for valuable
consultations and discussions, as well as .~.._~..~_~ and ~. ~,~ ~ ~or assistance
in tho work. Orig. art. has: 2 figures and 9 formulas.

SUB CODE: 20 / SUBM DATE: 22Mar65 / ORIG REF: 004 / OTH REF: 003

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?IT[~: ?heo'r,~, of non~J, neaz, ~aves zn a plasaa

SOURCE: Zhurnal p~ikladnoy mekhanfki f tekhni~hes~oy ffzfkf, no. 2, 1966, 3-6

TOPIC TAGS: plasma physics, plasma magnetic �~uld~ ion, shock wave ~ elect~on~ plasma

ABSTP~CT: The authors study nonl[nea~ waves propagating across a magnetic field in a
cold rarefield quaslneu~al plasma consisting of electrons and two types of
Dispersion curves are g~ven for ~o~ ~pl[=ude ~aves ~n a three-component plasma (see
~=~gu~e ~). The 2o~e~ branch of ~e ~spe~s[on c~ve des~ibes ~n[[ne~ ~aves
[a~ve[y log velocities. As ~[oc~ty ~c~eases, the ~per b~nch o~ the' c~ve de-
scribes non~nea~ ~ave profiles. Elect~n vel~ ts dete~ined by d~ approxima-
tion. An ~p~ss[on ~s given ~ ~e velocity o[ an ~solated ~ave in ~e~s of the
m~ magnetic field in the'~. A f~ ~s given sho~ing this ~lationship ~ov
various ~lative ion concentrations (see Eig~e 2). ~ lo~e~ the concentration
~gh~ c~ponent ~ the pla~a the ~ate~ ~s the deviation ~ linearly. The lo~e~
wl~ l~t of the ~a~ ~s ~ual to the speed of sold and the uppe~ [~[~ is equal

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ACC

AP6013g15
0

Fig. 1.

Fig. 2.

to the phase velocity of Iow osciLlaKion a~ high frequencies, As ~he wave approaches
the upper 1Lmit the ligh~ component drops ouT. Dispersion effects which cornpensa~e
nonlinear spiraling appea~ a~ higher f~equencies due To electron inertia. The cri-
Tical velocity of ~he wave and ~he maximum magne'~ie field in ~he wave decPease with
the reduction in concentration of the light component. The ion energy in ~he wave is
estimated, I~ is shown ~ha~ li~h~ '~ons are accelerated in a direction perpendicular
~o the wave mo~ion when an Asola~ed w~ve passes 'through a three-componen~ plasma.

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ACC NR~ AP6013915 ~1

If friction be~een ~he plasma components is in~t-oduced in~o ~he o~iglnal calcula-
tions, the ~esul~ is a shock wave having an oscillator' s~:~uc~u~e with a steep fu'ont.
A p~ofile is g~ven fo~ such ~ w~ve (see figure 3).

lO~ig* a~z. has:
SUB CODE: 20/

Card

# figures, ~ formulas.

SUIt'4 DATE: 290et65/ ORIG P, EF: 003/ OTH KEF: 001

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ACC NR, AP6020�49 SOURCE CODE: UR/0414/66/000/001/0003/0028

AUTHOR: Berezin Yu. A, (Novosibirsk); _Kur~n~a~..Kh. (Novosibirsk);
Nesterikhin, Yum. Ye. (Novos~birsk) -

ORG: none

TITLE: Collisionless shock waves in a
SOURCE: ~izika gnrantya i ~zzyva, no. 1, 1966, 3-28

TOPIC TAGS: plasma shock wave, shock v~ave front, shock wave analysis, rarefied plasma,
shock wave structure

ABSTRACT: The author discusses the theory of the structure of shock waves, dispersion
effects, shock waves with an oscillatory structure, collisionless dissipation, shock waves
with an aperiodic profile, conditions for exciting waves, devices used to excite strong shock
waves, the basic method of plasma diagnosis, dynamics of cylindrical waves, and the structure
of a shock wave and physical phenomena at the front. The problem of shock waves includes a
wide scope of physical phenomena such as dispersion of plasma oscillations, microscopic in-
stabilities, collisionless dampingt and others. The interest shown in collisionless shock waves.
is to a considerable extent due to the fact that instabilities developing at the wave front and the

Card 1/2 UDC: 532.593+533.9.07

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L h09~-.66

ACC NR, AP6020549 C)
phenomenon of the So-Called "reversal" of strong shock waves can lead to au effectivo dissi-
� pation of energy and heating of plasma. The indicated phenomena are also of value for under-
standing processes occurl3ing in the interplanetary medium, for example the interac~on of the
solar wind with the geoma~netio field, UnfortunatelY~ the structure of a shock wave and its
~ Width has still not been tnvestiga~ed in space experiments, but apparently this will be done in
the near future owing to the increasing volume of work being performed on satellites and
rockets. Orig. art. has: 14 flgur.es and 11 formulas. . .... . . --
SUB CODE: 20/ SUBMDATE: 16De065/ ORIGREF: 021/ OTH REF: 017

Card

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ACC Ni, A~r000636 ~

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............... sou cs /oo;
.',."ACC NR, 6037086

ORG~ ~ovoB~b~rsk 6tats Un~~t~ (~ov~b~ ~8u~Btve~ ~r~te~)
~n pl~u ~d other ~spe~ive ~'
~:: ~ T~T~ ~ne~ evolution of ~st~b~ce~
' ~hu~ eksperi~nt~gn�~ i teo~t~cheeko~ ftz~t, ~. ~1, no. 5, 1966, 1557-
~ ~ S0UR~

~:.' ~,?'~ ~�,?' .~.
'::.:~C :TA~: ' pl~ma instabi~tY~f plume va~ P~Pa~at~On' plasm~ m~etic field,
~ ~. ~ on of e~lier vor~ {Z~TF ~. ~, 1~0, 1962), in vh~ch
~]']' hbo ~Bo~ V~ der~d for the c~e oz- ~a~f ~-~.~__ .~..~ 8~ ch~acteriatic .
:~ feat~ of ~ffe~nt t~es of ~ne BO~U~ ~n ~ l~m~ or ~ other dispe~ve
: descr~ the e~olution of n~e~ ~sturb~ces ~ . '
: ~'-~. ~ c~d~t~ for ~e dec~ ...... ~-- the Eo~eveg-~ Vr~e~
' of the ~8t~b~ceB'into ~o~ t~es off ~oLu-
~ ...... t rinciple lB l-O~a~e~ ~- .

 p~ned, ~o~ ~neF~ ~mpvv.-
. L o,d

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to the case vhen the solution conaists of ~n i~dtvi~ual j
articular attention is pa~_d ............... Vet of small ~plitudeS. t
P ....... ~ ~-~ a "tail" representing a x~xt~e~ w~v.. ~---_~ .._a_. -~ch the Initia~

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KOROTKEVI(]H, JLleksandr Timofeyev~ch; BEREZKIN, Yu.I., ~d.;
K~L~OVA, M.N.~ ~. ~-
[~ ~ttle ~ a~ ~rk ~ays ahead~ ~ ~st�~ of the
Miasnikov Car ~r Pl~t] V ~ia~ i t~de - ~zde ~ere~;
k isto~i ~ ~. ~asniko~. ~nsk, Izd-~ M-va ~sshe~,
s~nego spetsial'no~ i professional' nogo obmzo~ila ~R,
(MI~ 16,6)
1~2. ~ P' (~~il~ads--Cars)

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REVAZASIiVILI,B.I.I R.lqfl)IN, A.N.li.~_.~IN,
TeSt~. a eo~'r~ ~~r for the au~tic contr~ ~
~ o~r~. at ~ Teke~ ore d~ss~ pl~t. ~vet.met, 35'
no.~l~ D '~. (~ 16~2)
(Teke~s~ mc~e~) (Au~tic contel)

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BEREZIN, Yu.L., inzh.; DZYGALO, V.I., tnzh.
Automatic measurement of the quantity of solid substance in the
pulp. Mekh. i avtom, protzv. 18 no.9:l~ S '6A.
(MIR

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AUTHORS: , L.A.~ and~ ~ --~.r~-

TITLE: Influence of the Large Irregularities of the F2-1ayer
on its Radio Wave Reflection Coefficient (Vliyaniye
bol'shikh neodnorod~_o.stey sloYa F2 na koeffitsiyent
otrazheniya radiovoln)
'PERIODICAL: Radiotekhnika i Elektronika, 1957, Vol. II, Nc.lO, ~
pp. 125~- 1259 + I plate~BB~
ABSTRACT: A strict solution of the problem of the reflection of
radio waves from a horizontally non-homogeneous, ionospheric
layer is rather complicated, but it is possible to make a
quantitative estimate of the amplitude and phase of the ref-
lected wave by means of a comparatively simple theory. For
this purPose, it is assumed that the phase of the reflected
wave is determined by the length of the ray and the amplitude
is given by the curvature of the surface at the point of the
reflection. The reflecting surface is in the form of a sinus-
oidal cylinder, described by gq.(1) where h is the average
height of the reflecting surface, m is the amplitude or the
vertical dimensia~ of the irregularity, P = iht/z~ is the wave
number and /% is the horizontal dimension of the irregularity.
Under the above assumptions, it is shown that the change in
Cardl/~

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Influence of the Large Irre arities oI' ~ne l~ ~
Wave Reflection Coefficient.
the distance between the observation point and the reflection
point of the n-th ray at Z~rn = rn - h , is expressed by:
rn (2)
- = sin~ + � cos2

where ~ = p(x + xo) and ~ - aP2h � On the other hand, the
relative change in the amplitude of the reflected wave is
expressed by: 1
AZ -- _ .... (4)
i + sin
From Eqs. (2) and (~), it is possible to determine the phase
and'the amplitude of the field at the observation point~ The
amplitude of the second reflection is also of some interest, but
this can only be determined at the points wherelthe raddus of
curvature of the reflecting surface is ~ = +
Card 2/4 ap

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Influence of the Large irregularities of
Wave Reflection CoeEficient-
The above theory was checked experimentally by means of an
equipment which permitted the simultaneous measurement of the
phase and the amplitude of the primary and secondary reflected
signals. The amplitudes Could be measured with an accuracy of
about 10%, so that the reflection coefficient could be determined
with an accuracy of 20%. The experimental observations of the
two amplitudes and the p~se were recorded photographically that
, e anal.vsis of the above, it was found
(see Fig. F). ~.r�m-t~h~A o~litudes of the f~mb reflection and
89% of the maxima o~.
92% of the amplitude maxima of the secondary reflection coincided
with the maxima of the phase displacement. The calculated
reflection coefficient gives values ranging from 0.25 to 5.4.
Where the reflection coeffici, ent. was greater than unity~the
phase Var~n was a meximum (85~ of the cases). This seems to
indicate that such anomalous values of the coefficient are due
to- large irregularities. There are 5 figures and 5
references, i of which is Slavic.
ASSOCIATION: phYsiCs Faculty of the Moscow State University imeni
M.V, Lomonosov. (Fizicheskiy Fakul'tet Moskovsko~o
Card ~/$ gosudarstYenmmgo Universiteta im. M.V. Lomonosovaj

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Influence of the Le~rge Irregularities of
Waw,~ Reflection C�efficient.
~UB]~iTTED: July 5, 1956.
A~J~�LABIE: Library of ~Congress.

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}(6), )(v)
, AlY-PHORS:

TITLE

PERIODICAL:

ABSTRACT:

4/4

Gusev, V. D., Drachevs L. A., Mirkotan, S. F., ~erezin, Yu. V.,
Kiyanovskiy, M. P., Vinogradova, M. B., Gaylit,
The Structure and the Motions of Large-Scale inhomogeneities
in the Ionosphere Layer F2 (struktura i dvizheniya krupnykh
neodnorodnostey v ionosfernom sloye F2)
Doklady Akademii nauk SSSR, 1958, Vol 123, Nr 5, PP 817'82�
(USSR)
The authors invented anintegral phase method 'for the re-
cording of great inhomogeneities and their motions. This
methOd is free ,from the deficiencies of other methods and con-
sists of t~e recording of the variations of the Phase way
of the reflected signal. For small inhomogeneities, these
variations are of the order 2~, and for large-scale inh�m�-
geneities - of tho order 40 - 200 ~. This method has a high
precision (which amounts ~o dozens of meters) and a high re-
solving power. This permits the use of statistical methods
in the investigation o� large-scale inhomogenelt~- The
apparatus for the recordinK of phase variations consists

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The Structure and the Motions of Large-Scale Inhomogeneities in the
Ionosphere Layer F2
of receiving and transmitting ionosphere stations with phase
indicators and photoindicators. The phase variations are re-
corded on a cinematographic film. The authors Used 3 record-
in~ apparatus plac~ in 3 points of the Earth's surface, these
points formed a triangle of 30 - 40 km side length. In each
of these points the variations of the phase of the reflected
signal were recorded. In this way~ the authors found a regular
smooth curve for ~p(t) on which random-character variations
~ (t) (which are due to the presence of inhomogeneities and
their motions in the ionosphere) are sUperimposed. The term
~p(t) is due to the variation of the height distribution of
the ionization of the ionospheric layers from day to night.
A suitable utilization of the results permits a separation
of ~p and ~ . (These 2 quantities are not exactly defined
in this paper). An analysis of the behavior of ~ (t) gives
data concerning the dimensions, the shape, and the motions
of the inhomogeneities. The followin~ parameters were found:
Card 2/4 The velocity Vd of the horizontal drive in the ionosphere and

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80�/2o-12~-5-1}/5o
~he 'strUc%ure and the Motions of Large-Scale Inhomogeneities in the
Ionosphere Layer F2
its direction which is determined by the angle ~ the average
shape of the ionosphere inhomogeneities which is determined
by the "characteristic ellipse"; the radius of correlation
and the spatial dimensions of the inhomogeneities A j the
time of spreading Xc or the parameter of spreading 6 of the
inhomogeneities. By analysis of the variations of the phase
and o� the rate of phase variation the direction of the re-
flected radiowaves could be determined. The correlation func-
tions were calculated by means of an electronic computer
'' )be ty~e.,,Strela',. All.the above.discussed results concern

' - ' ' mos~ :f'z:ecluen+IY ~h~- ~,hiu~-a '8- -' 10 km/min are :f'oUnd~
-card 3/4 of Vd inore..::e only slightly from night to day. Because of

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SOV/2o-123-5-13/5o
The Structure and the Motions of Large-Scale Inhomogenoities in the
Ionosphere Layer F2

the presence of inhomogeneities in the ionosphere, the normal
to the front of'the reflected wave deviates from the vertical
direction. For 6 and xo the average values ~ ~ 0.3 (day) and
6 ~ 0.58 (night) and ~c were found. There are 1 figure, 1
table,and 6 references, 2 of which are Soviet.

ASSOCIATION: Moskovskiy gosuda~stvennyy univerSitet im. M. V. Lomonosova
(MoScow State University imeni M' V, Lomonosov)

PRESENTED: July 18, 1958, by N. N. Bogolyubov~ Academician

SUBMITTED: July 17, 1958

Care. 4/4

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