SCIENTIFIC ABSTRACT AVERKOV, S. I. - AVERYANOV, A. G.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000102610007-4
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 6, 2000
• Sequence Number: 7
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

06)162
soy-/~4 ly I-J&J6/28
Increasing the Gain of a Travolling-wave Tu e in e ransient
Regime
gain K depends orA the magnitude and sign of dJ/dt
It is greater than the stationary value Ko when the
derivative is positi-ve and less when it is negative. The
effect is independent of operating frequency but fallti
off with larger inputs~ For an actual inorease in
collector current of only 2011". the gain may be tempr1rarily
increased by a factor of 6 There are 3 fig-ures.
ASSOCIATION: Issledovatel9skiy radiofizicheskiy institut pri
Gorlkovskom universitete (Radiophysics Research Institute
of Gortkiy University)
smmirm: September 20T 1958
Card 2,12

06488
SOV/14
AurHORSt AverkoV, S.I9 and Ostrovskiy, L,A.
TITLE i i,
Me Prd~oig*tion- of Oscillations in Systems with
Time-Dependent Parameters (Rasprostraneniye
kolebaniy v sistemakh a parametrami, zavisyashchimi ot
vremeni)
PERIODICAL: Izvestiya vyxshikh uchobnykh zavedeniy,
Radiofizika,
1958, Nr 4, pp 46-51 (U-SSIft)
ABSTRACTs Previous studies of linear systems with variable
parameters have been made by various workers (Ref 1 ... 4).
The physical basis here has been a quasi-stationary
system whose dimensions are small compared with the
wavelength of oscillation. Distributed systems havo
been considered by Rytov (Ref 5) but the validity of'
the approximations used have not been examined very
closely. Some information on this latter point may be
elicited by using Poynting's theorem for a system in
which the permeability and permittivity depend on tirse
and on the coordinates (Eq 1). The present paper
Card 1,13 considers the propagation of a plane
electromagnetic

o6488
50V/141-58-4-4/26
The Propagation of Oscillations in Systems with Time-Dependent
Parameters
the action of varying the properties of the medium doet
work upon the wave and increases its energy. The mean
square value of power density in given by Eq (22) and
frequency by Eq (23). The distance traversed by the
wave-front in a time t is given by Eq (24). On the b&ivis
of experimental data on the rate at whieb the propertiets
of a medium can be changed with time (Ref 6), it appearst
reasonable to plan an experiment at radio frequencies
whereby the predicted change in power and frequency maty
be observed in Practice. There are 6 references, 5 of'
which are Soviet and 1 English.
ASSOCIATIONt Insledovatellskiy radiofizicheskiy inatitut pri
Gorlkovskom univeraitete (Radio-Physics Research
Institute of Gorkiy University)
SUBMITrED: 14th January 1958
Card 3/3

05483
SOV/J~J-2-2-8/22
AUTHORS: Averkov. and Stepanov,
TrrLB: --~~ave Propagation in the System with a Travelling
Parameter
PERIODICAL: Izvestiya vyisshikh uchabnykh zavedeniy, Radiofizilta,
1959, Vol 2, M, 2, pp 203 - 212 (USSR)
ABSTRACT: An exact analysis of the wave propagation, even in
comparatively simple systems with variable parameters,
presents considerable mathematical difficulties
(S.1. Averkov and Ostrovskiy, L.A. - Ref 4). Thus, for
a long line having characteristic parameters L and C.
which are functions of distance x and time t , the
basic rolation!%hips can be written as Eqs (1), where
V and I denote the voltage and the current in the line.
If it is assumod that L/C = const., Eqs (1) can be
written as:
Card 1,16

05483
sov/14l-2-2-8/22
Wave Propagation in the System with a Travelling Parameter
(V + VI) V-L'C (V
ax at[
a
(V - ei I =. --
fLC (V - ev
ax at ~ I
where In these equations it will be
assumed that the variable is \rLC=, n(x,t) . This function
is in the form of -
n = n(t - XA)
By introducing the notation of Eqs (5), Eqs (1) or (2) can
be written as Eqs (6). If q = t - x/a , the
characteristic equations of the system are written as Eils
Card2/6

05483
sov/14i-2-2-8/22
Wave Propagation in the System with a Travelling Parameter
expressed by the product of t%to different functions. The
instantaneous frequency in the line is given by:
U/W = tl(x, t) (22)
Eqs (15) are employed to investigate a particular case,
when the paramet-er n changes in accordance with
n(n) = n0(1 + m cosAyj) (25)
Here, two cases are possible: for a non-synchronous Wavo,
2 , 2 -tion
when b > 0 (see Eq 26), it is found that the func,
� is given by the second equation on p 208, where 9 is
defined by Eq (27). The dependence of I on x is
illustrated in Figure 1. For a synchronous wave
(b2 < c 2 the function j is given by the first equation
on p 209, where y is defined by Eq (29). When b = 0
I is given by Eq (31) and V is expressed by Eq (33).
Card4/6

05483
sov/14l-2-24/22
Wave Propagation in the System with a Travelling
Parameter
SU3MITTED: December 9, 1958
ca-:-d 6/6

3 3 S/141/59/002/05/004/0'-"6
AUTHORS- Averkov, S.I. and Ryadov, V.Ya. El?2/E382
y Means of Thermal
,rITLE: Indication of Infra-red Radiation B
Signnl-freckuoncy Tr.ansducers ~,S
PERIODICAL: Izvestiya vysshikh uchebnykh zavedeniy, Radiofizika,
Vol 2, Nr !;, pp 697 - 702 (USSR)
ABSTRACT: The transducers considered operate at wavelengths of
the order of 10 Ii and consist of a blackened film which
is heated by the measured radiation on one side; the
secondary radiation of the film, which issues from its
other side,, is detected by a sensitive photoresistor.
The problem consists of determining the threshold
sensitivity of such a transducer. The block schematic
of the system is shown in Figure 1. A signal of frequency
w is applied to the input I of the system. It passes
through a high-frequency filter 2 and enters into the
chamber 3 , which is filled with a substance which
absorbs tho energy of the electromagnetic radiation and
converts it into heat. The substance of the chamber is
heated to a temperature T and radiates a sig-nal of
Cardl/4

s/141/59/002/05/004/026
Indication of Infra-red Radiation bVWV%NA 82
of Thermal Sifriinl-
frequenc-.y Transducers
lf the chamber is cooled to a temperature T.' , Eq (1)
can be written as Eq (2). Since the temperature
difference W =,T - T' is small, Eq (2) can also be
0
written as Eq (3), where M(T01) is defined by Eq (4).
The time constant of the thermal indicator is defined
by Eq (5), whore c 0 is the overall thermal capacity
of the substance. Consequently, Eq (3) call be writton
as Eq (6). The signal-to-noise ratio at the output of
the filter 4 is defined by Eq (8). If the modulation
method of the reception of weak signal is employed, the
signal-to-noise ratio can be expressed by Eq (9), where
G is the noise factor and N is the so-called modulation
gain which is defined by Eq (10). The symbol A f ill
Eq (10) represents the bandwidth of the filter 4 and
&F is the bandwidth of the low-frequency filter of the
indicator 6 . Assuming that AT has a minimum value
Card3/4 when Eq (9) is equal to unity, the minimum distingu
is liable

S/141/60/003/02/025/025
AUTHORS3 Averkov, S.I. and Stepanov, N?J3/9314
TITLE% Letter to the Xditor
PERIODICALs Izvestiya v,faahikh uchabnykh zavodenby,
hadiotizika,
1960, Vol 3, Nr 2, P 344 (USSR)
ABSTILkM The Otbove authors point out an error in their
article*
publIshed in an. earlier issue of this journal
(Radiofizika, Vol 1, Nr 5-6, p 184, 19581. This
error was discovered by G.G. Solodarl (Moscow State
Univer3ity) who repeated the experiment mferred to
by the authors.
There is I Soviet reference.
SUBMIT,rEDs February 7, 1960
ASSOC,XXION: (Radioph)sica Reseirch Institute of Gorlkiy
Universi
.0
*[Entitled: Increasing the Gain of a Travel.ling-wave Tubd
in the Transient
Regime]
Card 1/1

86856
S/141/60/003/005/011/026
i3z)6 (a Iso / o v E192/E382
AUTHORS j AV rkXXA,Wj -bit and Khronopulo, Yu.G.
TITLE: Electromagneitic Waves in 1,ossy Systems with
Time-dependent Parameters
PERIODICAL; Izvestiya vysshikh uchebnykh zavedeniyo
Radiofizika, 1960, Vol. 3, No. 5, pp. 818 - 825
TExrs It is assumed that the permeability and permittivity
it mnd c of the medium are variable and that the medium does
not contain any charges or currents. The Maxwell equations
for the system can be written ass
6D
(I) rot B vi(t) -- I (III) div B = 0
at
aB
(11) rot D e(t)- (IV) div D - 0
at
whei, -e the vectors B and D and the magnetio-and
elet,tric-field vectors H and E are related byi
Card 1/7

B6856
s/141/60/003/005/011/026
E192/E382
I;Iectromngnetic Waves in Lossy Systems wilo Time-dependent
Parameters
(V) B = 4(t)H, (VI) D = c(t)E
on the waves of an ideally conducting metal wall, the
vectors
11 arid D satisfy the following boundary conditions:
(VII) Bna 0. (VIII) Dtan a0 .
The snlution of the abD%re equations is based on the method
of
the variables. Thus, it is assumed that B and D
can be expressed by Eqs. (1) and (2) where f and a are
certain non-dimensional functions of time, while the vectors
11aand Da are dependent on coordinates only. From the
zibove equations the relationship between Baand Dais
expressed by Eqs. (3) and (4). on the other hand, the
relationship between E) and f is expressed by Eqs. (5) and
1:6),
Card 2/7

86856
S/141/60/003/005/011/026
E192/E382
Electromagnetic Waves in Lossy Systems with Time-dependent
Parameters
where w is a certain constant and po and no are the
constants of free space,, The vectors B. and D. satisfy
the Maxwell equations and the boundary conditions with respect
to monochromatic oscillations of frequency wIn particular,.
At follows that Baobeys
&B + 11 C W2B - 0 (7)
a 0 0 .-&
where k is the wave number (defined by Eq. 8) and w is
given by Eq. (9), where c is the velocity of light in
Vacuum. The expression for E) can also be written as
I-',q. (10) so that the final expression for the function f(t)
).s in the form of Eq. (II)i a similar equation for 0(t) is
:Ln the form of Eq. (12). The energy carried by a wave is
oxyressed by the usual Poynting vector, which is given by
Card 3/7

W56
S/141/60/003/005/011/026
E192/E382
Eloctromagnetic waves in Lossy Systems with
Time-dependent
Parameters
Eq, (13). The above ;rormulae are used in the
investigation
of the propagation of waves in a simple dispersive
medium,
i.-?. a waveguide filled with a medium whose
permeability is
a function of time and F, is constant. Eq. (1) can now
be
wrLtten as Eq. (15), where c = k /c It is assumed that
PW varies in accordance withs
14(t) - (a - Pt)2
(16)
wh,ore a and 0 are constants. Consequently, depending
on the magnitude of the quantity R , which is
expressed by
Eq. (17), the solutions for f are in the form of Eqs.
(18),
(1)) and (20), where Q and F are constants, The case
represented by the Eqs. (18) is analysed in some
detail. it
is assumed that a TE M,n -wave propagates in the
waveguide.
The components of the vectors B a and D a are given by
Cerd 4/7

s/141/60/003/005/011/026
E192/E382
19loctromagnetic Waves in Lossy Systems with
Time-dependent
Parameters
Eqa. (21). 71hus, the component B z of the vector B is
given by Eq. (22). It is seen that this depends on three
"rbitrary constants h, Q and ~P and two integer variables
n and m . If it is assumed that for times less than zero
v(1.) = const, I - BZ component of the vector B can be
ex-.)ressed by Eq. (23). By considering the initial
conditions
at t = 0 , :It is pos:sible to determine the constants of
Eq.. (22). The final 1~xpression for B z is in the form
of
Eq. (29). From this It is seen that the field in the
waveguide
can be regarded as a ;superposition of two monochromatic
waves
whLch propagate in thia forward and reverse directions
with the
phase velocity defined by Eq~ (30), where W = P .
Under certain conditions, expressions for f ""and t can
be in the form of Eqs. (27a) and (28a), In this case, the
components of the Vectors 11 and E are given by
Card 5/7

86856
s/141./60/003/005/011/026
E192/E382
Electromagnetic Waves in Lossy Systems with
Time-dependent
Pa ramet era
Eqs. (33) and (34),, In this case, there exists only
one
nonmonochrontatic wave whose amplitude is
time-dependent.
It can easily be shown that the above approximate and
exact expressions fo-~ the field vectors can be
generalised
and extended to the propagation of several
monochromatic
waves. In particular, if there exists a modulated
three-
harmonic wave, the component E y is expressed by Eq.
(35),
where m is the modulation index and .0 is the
modulation
frequency. Fig. I shows the vector diagram of the
three
components of the modulated wave expressed by Eq.
(35).
By eamining Eq. (35) it is concluded that there exist
a
ntimber of cross-sections in the waveguide where
either
frequency-modulation or amplitude-modulation is
predominant.
If; is possible to determine the spatial period of
this
Card 6/7

86856
S/141/60/003/005/011/026
E192/E382
Electromagnetic Waves in Lossy Systems with
Time-dependent
Pitrameters
phenomenon. The authors express their gratitude to
A.V. Gaponov and N.G. Denisov for useful
discussions.
There are 1 figure and 9 referencess 2 English and
7 Soviet.
ASSOCIATION: Nauchno-isaledovatellskiy
radiofizicheskiy
institut pri Gor1kovskom universitete
(Scientific Research Radiophysics Institute
of Gorlkiy University)
SUBMITTED: March 16, 1960
Card 7/7

s/i2o/63/ooo/ool/025/072.
E032/9314
AvrHORS: Avorkov, S.I., Aniltin, V.I., Ryadov, V.Ya. and
I - -
Furashov, N.1
TrPLE; Vacuum spoctromptor.for the far infrared
PMIODICAL: Pribory i toldinika ekisperimenta, no. 1, 1963,
103 - 112
TEXT: A simple vacuui-,i spectromoter with metal mirrors is
described. It is suitable for the r4oigo 55 - 1200 it nnd can
bo
used for detert-Anation or wavolonguitt, opticni constants of
various materials, the emissivity of nources, Cie sensitivity
of
detectors, etc. It in similar to that described by Yoshinagq
ot
al (J. Opt. Soc. tuijorj,ca, 1958, 118, 315). The optical
system is
shown in Fig. 2-, in which JA is the source, M is the
modulator,
M I and L'~ 2 are outs, r1p is the receiver. The mirrors 3,
ana 3 are sphoric&3, (D = 30 cm, F = 20 cm); is a
9 34
spacrical mirror (D rr 20 cm, F = 15 cm) and are also
spierical (D = 31 cm, F 60 eat. and .3 are
3*
7 8
Card 1/3 1

s/i-no/63/000/001/025/072
Va-~uum spectrometer E032/C314
plane mirrors. A mercury quartz I)PK-11 (PIM-11) is used
as the source and the receiver is an optical acqustic
detector,
OIW~-2 (OAP-2), with tt working area of 7 x 7 t-,im- and a
I nim thick
cluartz windowq The modulator is a rotating disc with NaCl
s e,~.tors. The moduIntion frequency ia 9.6 c.p.s. The
bandwidth
of the tuned amplifiar is AF = 3.5 c.p.s. The resolution at
0*5 1
95, 125 and 127 it is quoted as: 1.1, 0.8 and 0.76 cm-
respectively. There tire 3 figuees %-,id I table.
AS50CIATION: Nauchno-isslodovatollskiy radio f izich askiy
institut GGU (Scientific Resoarch Radiophysics
In'stituto of !GU)
SWI-117TED: April 11, 1962
Card 2/3

Vacutint apoctromotor
Fig. 2:
S/120/63/000/001/025/074'1
E032/8314
Card 3/3

AVERKOV, S.I.; ANIKIN, V.I.; RYADOV, V.Ya.;
FURASHOV, R.I.
Astronomical station for observations in the far
infrared
spectral region, Astron. zhur. 41 no.39.542-545
W-Je 161,
(MIRA 17:6)

L&2245 -'5-/Pl - 4/.Pae - 2RA (DASNaM/
NNNIVEWOO
ACICESSION X.M. AP4040846 H/M33/W041/003/0542/0546
7ITLE: Ja-ustrmomical- ate tiDn for vbservadons In-ft of the eptctm~--
SCURCE.- AstronomicbesIdy zhu=al, v. 41, no. 3, 1984, 642-545
-q p ---f%r-lafr-ftr-qL
~w "tmomy, 13 IOUA arzn ~-Utg~ imp "vzo
rerim infrrmpdspectruin, ipactmaomw
A-70TRACT: AD astrommLeal station for nbnerv" in the far ldrured reglon of JIM
usod n YPs tv
spactrun to diiscx1bed. Wo i tation wai cu m eVO_A#on of ANMFl (1% 1
Thpgeneml appVaearaiwe-of the ntatirmto

.737-65
A oESMON NRi AP4040846
-too,
ftTvo the continuous npecL-um Di'the source. An e6olette grating ib
uosed an the i
di qV 0 roing:
Weltlent. Bcamiing of the spec bum is accomplishod by ttmdng the
echoleft, using a i
onitbronous ractor. Ile wea):Wpal dutect~d by the opticia ayBtem In
transmitted tx) the
mobliving-rooDitling apparatus. 1ho radialJon JiWicator uls-rd in this
umponent M &M
imbconcoustical detector with o iquartz window and a throobold
iseneltivity of V-15 x 10- 30w.
]Fuill details can cterning the apt UA-1 system are supnUed In the
text. PraUminary ta.,aLsi were!
inade under Isboratory condlftmB in the spectral ringe 140-1400 p.
Field tests in Ithf
1-1amllirs Rt Pn elDvation of 3, BED m were in the Ppectril region
300-1-101) p, and the ~gjv~r!tro-
!p-mns obtained at this timin wt re us~ed in determLning the windows
of nflative atmcupt 11ric
1rarir,parency in this r-,-.ng-,. Flq-,. 3 alf the Encllcrurt- sh-aws
the r-,c-,rd o;f Mgnals ?r-.-TT t".
BUO- JA UO p.
imn In MO r-OgLo.,-3 The mwma o1 tho curvo ooms d to tho abDo.-Puon
Nner.
of'o-M,
ter vapor An the atmoophive Itho upper ptirl- of the dialTam shows
their theor
Ruthc,ra thw* M. T. Gre]Nwa for her intivest
Aral diatrIbition) . "In -ew elusion, the
and vapport durin developmez I of ilia sLAtion. The authorn &1W thfmk
L V.- Monaloy jmd
1). k. Flmli-abuv for thoir us r3elpfition in U~-,q vasirn of Me
MHG-D~ P. A, 1)r
. . . . . . . . . . . . . . . .

A
8 6
Ai CMG RM AP404OB46
R!..i Alwribh i ri na-m gtm-,Zt VII 41.1 trz- ts --
paretuo and qA M".--Vv wbo pl~~ In I h a
txt hao
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AMCIATIVIN: nono
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NO REP SOVI 004 OTHES13 001
M.-M

AOCEMM Nil: "404080
ENCU61tRE: Oi

Card 4/6

L 8737-65
JA(!CESSION ?in: A13,1040840 ENCLO511PIE: 02
C-1
Aa,
Fig. 2.
7ig. 2~ R-Ow-ma-d-o 1-c-prosentabo-1--elf tile -P&Al fkYJ3tMU Of thO
aSt-IOnOMICal SWIM!
A 9; D - confocal parabolic mirrors; 'M - monocin-omator; 1 2-
par-idAle-
mi rronj; 3 4 - mi--rr,)rg; PTI - prism.-
Card 5/8

Fig. 3.
Cjxd 6/13, Rpectrum of elp-ml s froyn tho sun in flat) vu%ga 6W 1400 p

i
'_.AjJ=,W.j#ANIXnI, Y.:I; JRAvo_zHjvCTOvsXjY, D.M..
GAPOHOV, A-V.; ORMUFA,
M.T.; YERGAZOV, V.S.; LOPTM , V.A*; MIUM, M.A,; FLYAGIN,
V.A.
Diode oscillator notes source in the three-centimeter
band, Hadlotolhe
I elektron I noefl:71~-771 JS 156* (NUA 10: T)
(Pecillatore, Xlectron-bube-Noise)
(Vnve mides)

A P. 11-

IL
A. r. K~~

P- -.k- -M

AL a C-

Y.-A
10 AG Is 16c")
0.

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sm~ft" wo

rink omod"um Im. A. 1. Pwff (VMS)$ NWNWI
ftit*

I
LVEROCIN-11a, 31.1.V. Cand Geol-Einerdo "Ci -- ((ucs)
Mft6tlologlcjOA,- 00 1.3 I'Z
os
flubstmitiation of the.4dded Sella, slability of *p
conduit irl
ighor
v.-ater dmining sycterm.ll I.:os, 13pp (Vin of ilxxiik
:3dilcation USSR. I:cv
CWor of Lenin Q'tato Univ im 1-.V. Lomonosov). 100 copies
(lit 3~-58t 110).
- 10 -

J'ADIM, P.I.; AVIROOMallA, N.V.
~
Deformations of drainage canale in the Keshchere
Lowli-ad, their
nature and causeo. Vest. Hook. un. Ser. biol.,
pochv.,,96010,, 96009,
13 no. ItI51-161 158. (MIRA 11:7)
1. Hookovekiy gonudarstvanWy univarsitet, Kafedra
inshenarnor
geologil 1, gruntovedantya.
(Keshchore-Chnals)

AVRROCHKIKk, ?I.V.
Deformation of amndy slopne of 4rainage canals caused by filt&ration
pressure. Vast. Mosk. un. Ser. blol.. pochv.. geol., geoc- 13
no.2:2,01-210 158. (milLIL 11:9)
1. Moskovskiy gom. universitat, Kafodra inshanornoy goologil i
gruntovedeniya.
(Canals) (Water, Un~arground)

KOTSTM, B.D., kELnd.tsk1=.n%,ukj #VICROCHKINA, M.V.,
icand. gaol. -mineral. mauk:
Yormation of the secondaryetructure of subgrade soil.
Test. TS111
MPS 19 no.8t49-52 16o. (MIRA 13:12)
(SoLl mechanics) (Railroade-Track.)

ABAAHOVp L.T.; AVEROCHKINA H V. I
..' *&ww_j- ROCIIEROVAp N.D.; FILIPPOVA, L.S.
r
-vxn takhn.red,
ed.; VMP N*N*f
(Antibeaving measures on
railroade]ProtivopuchinrWe mero-
pftiatiia na tie,lezrjykh dorogakh. Mookvqp
Transzho3.dorizdtttq
1962. 22 p. (MIRA, 1501)
(Railroads--Maintenance and repair)
(So:Ll mechanic a-Re search)

AU"HKINAP M., kand,teologo-aineralogicheskikh nauk
Studying the off act of chomical additives on aoil heavii-ql*
Yeat.
TSNIIMPS 21 no.7:52-55 162. NMA 15:120
(Soil stabilifation)

AVERSHATYANJ T,,,A
lamprop"s in the Magri plutob. Izv. AN Arm. SM. Geol. j
geog. nauki 14 no.2:3-19 160, (MIR& 140)
1. Institut igoologichaskikh nauk AN Artqanskoy SSR.
(Magri District-lamphrophyres)

Av-r. h irl, 1 N.
Inv---wU--it1,)ri -)r tho. c,)nd1t!,)n,.., or, the
qfflciency o" In intchante-,1 Mil Ri-,hor
-it U) n U
n,, For Uic, 1.,.? r
1:ist. TP-nint-,nd, 19-36. (L ls~virt Aimi ry, .-f
In T-chalt-al .,ni-ences.
Knl-,hnava etrr'-
No 21, 1956. :'-

Pro'bless of the isparation process by mechanical classifiers.
Obog. rud 3 no.2:126-31 1 58. (IGRA 11:11)
(Separators(Machines)) (Ore dressing)

I - . - I ~ . ~ I, . , -11,1 ~- . ! . _0 . - ~ - -: -
- - . Mffmmms~
w9mmmP Elm
AVE-AL,11111, I.N.
Recovering the finer size classes in the olutriation fluid.
Oboe,.rul 3 no.41.21-22 '58. (MU 12:2)
(ore dressing)

AIT'.-.T)"YT~ ,
- fly --III ITT.M ) -.7. G, - -- - -
AI'JRSHlN, S.G.: POLYAK, I.I., redaktor.
[Shifting of rocks In underground mining] Sdvishenis gornykh
porod
pri podzamykh rasrabotkakh. Uoskva, Uglotakhisdat, 1947. 244 p
(5mbeldencen (Barth novements)) (MLRA 7;7)

Avershinp S. G. *Problems of lifting mined minerals"o (Report), Trudy
Soveaholuird.ya
po upravlaniyu gornym davloniyomi (1946), Moscow, 1948, p. 35-56.
SO: U-411, 17 July 53t (Letopia 'Zburnal Inykh Stat-ey, No. 20, 1949).

MaMines XOT h8
CoaLl
mini Methods
OCertain Problem of the Thoor7 of Rock
DIsloc&-
tion,w Prof S. G. A*ershin Dr Tech Sci,
I&ureate of Stalin Prize, R pp
%or Zhur" lo 3-1
DIscusses problem on coal formations,
connected
irith safe depth of shaft. Data reveals
surface
deformation related to geological and mine
operating conditions. Forsm1a discloses
that
40/49T67
/Mines (Contd) lov 48
the horizontal deformations decrease such
sooner than the settling, as depth of
shaft
increases. Gives tvo tables and graph of
observation.
kOA9T67

0 -1 ?
, " i . W :, 11,f, ()1)Jtc(1,ivc:; of t1le'. All-I'll; .11
S. I L"". 11, t I ti , ~c -Le."e 1.6 11~,r
-i_-. le".
11', Tru6y * 011, - . il-t,,~ l!"11 ~~, Vol. I., , I
p. 3-11r. . .0
SO: 12 Feb. 3, k'Leto.,11t Muriml Iny;:I, S~,ate.-, ',,0. o,

A. "A 311:1-i ry of th- rle..vlA!:
i nfl. jl'u:,.nct:, -)v,
bu-.~':r!., In 1;r)cc.;.'di:j-, 1~-)ri-"'Iltcl ;t Utz,", Trufly
Willa~' Vol. 15, I,V",
SO: 12 Prb. "~3, (betopls' Zhurml InyMi Statey, No. 2,

AMMINI S. G.
The extent of shifting in rock formstionn Leningrad,, Goo.
nauchno-tskhn. Isid-wo
lit-ry po chernol I tuvetnol ust4illirgit, 1950. 57 p.
52-19089
MOM

I I . . I . ~,-
uiffl~mium . .
Eurt~
InvestlEationa of t:~c Ul;eory )f displacement. 22, 1950.
9. Monthly List of Russian Accessions, Library of Congress, Octobor lq~;~, Uncl.

Profvs~-,!)r 1. Fakhurln anA ~;ovlet iflne nurvnying. (Trudy) VNI! 1 22, 1 50.
9. Monthly List of Russian Accessions, Library of Congress, )ctc)L(.,i- _194',
Uncl.

Role C., It ~5.~ a I,. se1u, A:'; to in, 0 tudyl"'ic he d is, r:. c;, s
ZI-rud'V17 V'~i' :, 22,
Monthly List of Russian Accessions, Library of CongreBs, Octnbcr -194, Uncl.
I-T

NEBO
A.
993. URTH SHM IN KLM KALB. Avershing-M. and Grigorley, S.K.
(Ugol(&;M, June 19520 1-10).
7his phenommon r4isembles wWlosions in the coal at do-ths of 200 m.
&M more, Suggestion* are made for preventing it. (L).

professor, doktor tekhnicheakikh nauk.
The greatest values for elements of a displacement
syncline, Trudy
VITIMI no.260-20 152. (14ML 80)
~Subsldencev (Narth movements))
I

AVERSHIN, S. G., Prof.
T!roblems concerning the trend in the examinatlon of rock
displacements. Ugoll
27 no. 9, 1952.
SOt MLRA. December 1952.

OKWCHRIK021 A.N., kandidat tekhnicheiakikh nauk, redELktor;
AVIRSHIN,
S.G. doktor tekhnichaskikh nauk.. professor, redakto"rM.,~wsay,
dok-tor tekhniclieskikh nauk, professor. reclaktor; 1W Ov.
G.R., kandidat tekhnJ:chq9ki1di nauk. redaktor; NIKIFMOV, B.T.,
doktor tekhnicheskikli nauk. professor, redaktor; RODKIVICH.
D.V.,
kandideA takhnicheakl-kh nauk, redaktor; TIHCFBM, i3.r., gorW
Inzhener. redaktor; SLOOROSOV, A.Klh., redaktor; SHPAK, Te.G.,
tekhnicheekly redaktor
(Studies In iurveyinij Issladovaul,4 po voprosam
marksheiderskoro
del&. Moskva,-Uglatskhizd&t. Ho. 27. 1953.'194 p. [Microfilm].
(KRA 8 :7)
1. Leningrad. VseeqjnLznyy nauchno-lowledovat all skly
marksbayder-
skly inatitut.
(Mine surveytig-)

.A9
r,orn,vy-9 raboty pod sooruzhonivami i vodo-jrtimami (Mining wndar
structures and bcAlms of
vat a r) Moskva. Ugletekhizdnts 1954-
322 p. illua.. diagra., tablef
731bliographic,tl footnotes.

AVF,RSHI tIRM Ga~rilovich; PANOV, A.D., rodaktor; SLAVOROSOV,
A.Kh.
Ali .- .tekhnichoskiy redaktor.
(Rock bursts] %rmVe udary. Moskva, Uglotekhiz4at, 1955. 233 P-,
(Mine socidonts) (MLRA 9:1)
Lzj W-11n, Wli~MIIL~~t;i~

FUMY; Vit,~714: LITVINNIUN, Y"thl-, KRMFj~ StAnIsIrm;
~iALUSTOUCE Antoni..
SHKLYARSKIY. H.F.., inthnnfr [Translator!: AYMSH-M. SO., rr,)"
?!r 5 or,,.
redr&tor-; SLAYCROSOV, A.Kh., rpdilltor; NOZOROTSKAYA, Y.L. .
tOkt-')I-
chookly redaktor.
[Froblome in calculrit Ing iturfftee disiplaeovents caused by
minvi work,
Trrtnslated frnm the Polish! Vopmey r^sehota eavi2henii
povvrikhnosti
pod. vltiantem gor-ny'di rattalsotok, Porovod 9 pollskogo
akogo, pod red.$ 4 ~ krarshina. Ilookyn. Got. nmichno-t
ekhnichaskom ild
vo lit-rzy po ugellnol premychl., 1956.63 P. (HLRA 9:5)
(Paland-F.arth movf-ments)

4T -
r L 1-15 5
JiBRimov, S.K., kand.tnkhn.iv,itj.-- S.G., prof., dcktor
tekhn.nauk;
AMMOSOV, I.r., dokl;or V.D.. inzha;
ANTROPOV, A.H., lmtli., iYANASOYEV, B.L., inth.; B'RGMAN,
TA.V.,
inch.; BLOCIA, Yo.Yo., im-.,h.-. TIOGACHEYA, Ye.g.. inch.;
BUKRINSKIT,V.A.,
Imnd.teklin.nauk; P.V., doktor geol.-min.nauk; VINOGRADOV,
B.G., Inch.; GOLUBRX, S.A., lnzh.; GORDIYNNKO, P.D.. inch.;
GUSEV, N.A.,
kand.tokhn.nauk; WOW1114. I.V.. kandqveol.-min.uauk;
KALMTKOV, G.S.,
inah.; KASAT001101i, V.I., dol-tor khtm.nauk; KOROLXV, I.Y."
inch.;
KOSTLIVTSICV, A.A., 11117-h., KHATKOVSKIY, L.F., lnzho;
KHASH)WINNIKOV, O.F.,
prof. doktor geol.---,a4.n.rv:ulr; bRIKUNOV, L.A., inth.;
LEVIT, D.Ye.. in3h.;
LISITSA, I.G.j kan~..tilklu,.naiik, WSHOKOV, V.A., inzho;
MATYNTEW. A.16,
dote., )mnd.geol.-vi',T,.tir:v*1:; HFJWISHVILI. G.Te..
iznh.-. MIRONOV. K.Y..
inch.; MOLCHANOV, I.I., " riih.; HAUHOVA, S.N., starshly
riauchayy sotritinik;
I=IPHWVI Y.Yo.g !.nrh,, PAVUW, F.r.. doktor tekhn.nauk-.
FANYUKOV. ?.N..
doktor geol.-min,wil; POPOV, Y.S.. inzh.; PYATLIN, M.P.,
ksnd.takhn*
nauk-, RASITOVSKIY, itirli.: ROMANOV. V.A., prof$, doktor
tekhn,
nauk-, RYZHOV, P.A., pref., doktor tekhn.nauk; SNLYI JTSKlY.
G.A., inilh.;
SPHRANSKIY, M.A., InOi.; TIRENTlYBY, Ye.V.. inch.; TAITOV,
N.G..doktor
khim.nauk; GOKARLY, I.T. , Itirh.; TROYAUSKIY, S.V9, prof,,
dokt,or goole-
minenauk; FEDDROY, P.D., dots., lmnd.tekhn.nauk-,F)ZCROV.
V.S., Inch.
(deceased]; KHCHBIll'OVS1,11'. A.S., prof., doktor
gool.-min.nauk; TROTAHOV-
SKIY, S.V., otvetutvnnvyy red.; TLRPIGORAY, A.M.. red.;
KRIKUNOV. L.A.,
red.; XURUSOV, I.A., red.; MIRONOV, X.V.. red. ;_AYERS HIN,
S.G.. red.;
BURTSEV, M.P., red.; VAS)WY1.7, P.V., red.;
MOLCHANo~;-T-J-.7,~R.;
RYZHOV, P.A., red.; BAIANDIN, V.V., Inzh., red.; BLOKH,
I.M., kand.
tokhn.nauk, red.; '.HVKRlll,';YJY, V.A., kand.tekhn.neuk.
red.; VOLKOV. K.Tu..
inzh., red.; VCROB'YEV, L.A.. lnzh., red.; ZVONARNV, K.A.,
prof. doktor
tokinnenauk, red, (Continued on tiert card)

ARRAMOV, U.Xo-- (continuiweO Ci ;-d
ZDANOVICH, V.G., joror.,col-tor tekhn.nauk,red.; IYAROY.
G.A.. doktcjr
gool.-min.nouk, rod.;: ):j-J,.PVAYIX. N.M., red.;
KORCTKOV, G.T., kand.geal.-
min.nauk, red.; KOWITOV, N.V.. kand.tokhn.nauk. red.;
MAKKAVEYEV. A.A..
doktor geol.-mln.uRuk. rcc.; OMELICIUMO,
A.N..kand.texhn.na-uk.red.;
SINDERZON. N.M., Im tid,,go vl.--min.nauk. red.; USIIAKOV,
I.S., dote., Imnd,,
takhn,nauk, red.; TATILOYOV, V.S..
kand.gool.-min.nauk.red.; :KOROLXVA,
T.I., red.izd-va.- *Qj;:RAJXIWA, Z.I., red.1zd-va;
PROZOROVSKAYA, Y.L.,
tokhn.red.-. NADRIJISKAYA. A.A.. tekhn.red.
(mining; an ancyc1q,tieji. )wndbook) Gornoe delo;
entaiklopedicheekii
apravochnik. Glav. ree, LJI.Terpigorev. Moskva.
Gos.iiauchno-tekhn.
izd-vo lit-r7 po t4rolly:cl promVehl. Vol.2. [Geology of'
coal depoette
and ourveying] GooLogiti. t4-ollnykh mostorozhdanti i
marksheiderskoe
delo. Redkolegiia t-cris !;.V.Troianskty. 1957. 646 p.
(MIIIA 11:5)
1. Ghlon-korres 01.1160. fidi SSM (for Karave ev)

AMISHIN, S.G., doktor takhnichaskikh nalik.
"T"
Rock b~umps &L their prevention. Besop. truda Y prom. 1
no.1:11-14
J& 157. (KLU Iw4)
(Mine accidents)
. I.' ~ - i, - - . , , . ~ 1. .. I . . .. I :, ~ I I I .~- !
-,;:" ;- ~ I I ~,,, ~ ~ 1.

AV ~jokt.tekhn.nauk; ANANIIN, G.P., dotsont, bind.takhr...
neuk; BARANOV, A.I,. doteent, inshe; BMMIN, A.Tess ins:h,;
BOMMARST, 4.0., kand.tekhn,nauk; BUTMICH, R,T,, imnd,t~khn,nsxik;
YXS=VGKIY, V.S., prof.,doktor tekhnnauk; VESKYr. Me, kand.
takhn.nauk-, TOLIKSAU, A.Va, kand.tokhn.nauk; GAHCAVI, S.N.,
k9nd.t9khn.nauk-, GORBACHEV. T.F.1 DAVIDTANTS, T.T.,
ksnd.tekhn,v,4iuk-,
DKITRITZV, M.F.. kand.takhn.nauk; DOBRDVOLISKIT, T.Y.,
tand,leklat,nauk;
DNALOT, kand.takhn.nauk; ZATTSEV, N.'A.; ZARANKIN, P.S., 1xish.;
2TYAGIN, P.2.,, dotsent, kand.takhn.nauk; ILISHTITV, A.M.,
kand.tvkhzi.
manir; XILTACM'LOT. A.P., doteent, kand.takhn.nauk; KIRICHENKO,
I.P.,
insh.; I:RUPIMIIKOV, G.A., k?nd.tekhn.nauk; KUZNITSOV, S.T.,
kand.,,
takhn.nauk; KlICHIRSKIT, L.V., kand.takhn.nauk; LINMCNAU', N.I.,
litzh.;
LIKOVICH, dolisent, lcand.takhn.nauk; LOKSHIN, B.I.S.,
kaEA.tskhn.z.siuk:
MURATOT, X.L.1, dotsent, kand.tekhn.nauk; MUCHNIX, V.S., prof.,
doktor taklin.nauk; NATDTSH, A.M., doteent, kand.tekhn.rauk; NMI-
SOVSKIT, Ta.l., prof., doktor takhn.nauk; NIKHAY]IV, G.L., insh.;
NUROK, G.A., prof., doktor takhn.nauk; OVINOV, K.I., irtsh,;
FORTNOV, A.A., Insh.; PRDSII~MIN, V.T., doteent,
):and.tcikhn.nsuk;
IRUIM. B.A.. insh.; SCITSItIT, I.P., kand.tekhn.,nauk; SMTSKITj
R.A.,
dotsent, kand.,tokhn.nauk; SOMOV, A.F.0 kand.te):hn.naiLki WHII
P.T.. iuzh.; GONIN. S.D., prof.; SMPLATOT. A*P,O prol'.v doktor
tekhn.nauk; TI:140513VICH,.Y.A., inzh.; FMAN, A.A., inish.;
CH"WAL,
N.A.1 SHAMOMYSTIR. L.G., doteent. kand.tekhn.nauk; TK3PICWPR&V.
A.M.,
glaynyy red.; LOZNEVA, A.A., red.; NIPMIN, I.F., red.;
OSTROVSIJ:Tq
S.B., 4ed.; FANOT, A.D., red.; GARIV, A.S.. rod.; SqMKOV, I.A.,
laontinued on next caril

AV36 IN, S.G.-(contivued) Card 2.
red.; AP3MANGIVSKIT S kand.takhn.nouk, red.; R12HIKOV.
lnsh.# red*; AUSHIN: ;,:,:: red.izd-va; KACHALKINA, Z.I., red.
AzA-va; PROZOPOVSXATA. Y.L., tokhn.red.-, HADBIHEKAYA, A.A.,
takhri.red.
[Mining; an encyclopedic handbook] Gornoe delo: entaiklopedicheekii
spravochnik. Glav. red. A.M. Terpigorey. Chleny glnverod,:
Rarabanov i dr. Vol.5 [Underground coal mining] Razrabotka
ugol'nykh mostorothdanii podzemnym sposobom. Moskva, Goo. nauchito-
tokhn.izd-vo 71it-Jry po ugollnol promyshl. 1958. 447 p.
(KIRIL 12:2)
1. Chlon-komispondent Akademli nauk SSSR (for Gorbachev.
ChinalwLl).
2. Chlen-korroopondent Ak-ademii nauk USSR (for Zayteev).
(Coal mines and mining)

AVIF-T-SHIN, Step-nn G. 1,1,eningrad)
"Empirical Data from Pock Pressure Research."
paper submitted at Intl.. Cong. on Book Pressures in mining,
Laipzig, cm ,
14-16 Oct 58.

AVERSHIN, B.G., prof., do'ktor takhn. nmuk,rad.;
BLOXHA,Ye.Te..gornVy inzh.,rOd.;
WA-9"JIURVICH, T.Y., gornyy insh..red.; KRIXUNOV, L.A.,gomyy
inzh.,rad.;
LISHUTIN, B.G.. gorayy insh.,red.; OaLOBLIN. D.N.. prof.,
doktor
tekhn. nauk,, riod.; OKIZIUHMO. A.K..kand. takhn, neuk, red.;
RYZHOV. P.A., p:rof..doktor takha. nouk.; GLAZZMAP. K.K..
Lash..red.;
XONSTANTINOTA, L.1f.,in2h.,rad.-, NIKITIUA, KJ1..1nrh.,rrd.-,
NOVOSELOVA. Yu. A..inzh.,red.;SM1GO. To. I.Jush.,red.;
fAKOV13f,
K.G.,Lnzh..red.~ RASHKOVSKIT, Y&.Z.,inth..red.; SMIKAICH.
A.M.,
red. izd-va,; BERLOV, A.P.,tekhn. red.; NADSINSEATA,
A.A.,tekhn, red.
(Transactions of' the All-Union Scientific and Technical
Conference
on Mine Surveying July 17-23, 19561 Trudy vessoiurnogo
nauchno-
takhnicheakogo toveshchania po markeheiderskomu delu 17-0
lulta
1956 g. Kooky*, Ugletekhizdat, 1958. 743 p. (MIRA ll:..L2)
1. Vessoyusnoys nsuchno-takhnichaskoye soveshchamiye po
morkshoyderskovu delu. 1956.
(Mine surveying)

Tt* L%tv"*tl*fAI F~k TMOVAM I% Maim Val bold Ilk
Lotv*14, 14-lb Oct, 1958.
sovirl 4fleptas worel
ftem" Ik"amb.,
run. & 0. "d xv"mn. it.
*4~%tvms cc Yxk rMours."
VAOMWOT, h. P. wA MANJUVORn, T- t- (ft~)
.Iftn.v~w* of PA*k fteopw* am, the Strwq% of NIMIN
comstrwtl- I. W. V.Wts
buts.
801 lkmm)oklmkq& Mi Im vmI.

a- ,y
J
t4
Ua
goo
0. -,.J
cx n
:_~
p 87
yjjij~ 0--a 11 '. ~; .3 1;
. i A. I : Js
171.
ONg: H j
Hall
a kj,
Sig

21

1 : .,
t v
4 A
V~q ..~
Iev

0
.7j

'

.11 Ilk

-

KUZMSOV. Osorgiy Nikoleyvvich; BUDIKOpAeripi
Nikolayev"l . ',
FIUIPOVA. Antonins Alskeandrovnal SM#TARSKIY.
Mechislay
]Psliksovioh; AVERSHIN, B.G., otv.red.; LOMILINA,
L.N.,
tekhn.red,
(Studying manVestations of rook pressure by means
of models)
Isuchente proAavlenii gornogo davleniis na
modeliakh. Xoskya,
Uglatekhisdat,, 1959. 282 p. (MIRA 12%8)
(Geological modeling)
(Sibaldences (Rarth movements))

XAUKOVSKIT, Dmitriy An%onovich, prof.. doktor
teklui.nauk; ATIMIN.
an, Osyrilov*ich prof , doktor takhn.tLnuk; BRUN 0
-*q
Anton nVwfAMRh. do;sent, kand.takhn.asuk; GMT, Mikhail
Iosifovich, dotment, kand.tekhn.nauk; ZDMOVICH.
Tyacheslay
Grigorlyevich, prof., doktor tekhn.nauk-, XROTOT,
Gavriil Alakneyeviah.
dotsent, kand.tekhn.nauk; LAVLOV, Vladimir Nikolayavioh,
kand.toldua.
naut; LZBOXV, Kirill Kikhayltvich. assistant; PTA%Di,
Kikhail
Petrovich, dotsent, kand.takhn.nauk; STWIN, Nikolay
Ivanovich,
assistant; ZU INSKIT. V.A., otv,red.; SLAVOROSOV, A.Kh.,
red.ind-ra;
ALADOTA, Ye.l., takhn.redge, KOROTANNOVA, Z.A.,
takhn.red,
[Mine surveying] Karkshaiderskoe delo. Moskva,
UglatekhIsdato
1959. 688 p. (HIRA 13:11)
(Kine surveying)

t0

AVERSHIN, S.G., prof., (Joktor tekhn.nauk
Determining the parameters of chamber mining.
13-24 '61.
(Mining engineering)
[Trudy] ~NDIJ no.401
(MIRA 14-32)
I

AVERSHIN-,,.S.G.; PETUYFIO'7, I.M.; ROZOV~ B.V.; BUDKOV, V.Ye.
Control of the harmful effects of bumps in the mines of the
U.S.S.R. fgoll 37 no.8:22-30 Ag 162. (MBA 150)
1. Vaesoyuzr4ry- nauchno-isaledovatel'skiy maLrkaheyderskiy insti-,;A
(for Averehinj Petukhov). 2. Oosudaratvennyy treat uqol'nykh
predpriyatiy Kizelevskogo rayona (for Rozov, Budkov).
(Mining engineering) (Rock pressure)

AVERSHIN, S.G., doktor tekhn.nauk
International Congress on Rock Pressure held in Paris. [Trudy]
VNIMI no.40t212-230 '61. (MIRA 111:1.2)
(Rock pressure--Congresses)

AVWRIN,SAv, doktor takhn, nauk, praf.
Conditions causing rook-%rate &ad problems In
studying theme
[Trudy] VNINI no.4813-9 162. (MIRA 16tO
1. Vaesoyuz"y nauebno-ionledovatellskiy
marksheyderskiy
institut.
(Roak bursts)

AVERSHIN, S.G., prof., doktor tekhn.nauk;
FTUXMV-~,:I-,*.,,~-'kand.tekhn.nauk
Study of bumpB and development of measures to co"+rol
against
their harmful effects in mines of the U.S.S.R. .[Trudy]
VNIMI
no.49%3-17 162. '(MIRA 17W
1. Vsesoyuznyy nauepno-issledovatel'skiy marksheyder5kiy
institut.

41VEISHIN STEPAN 0.
"F:4,Ating rock bursts in coal inines"
report to be submitted fc*r the third Int. Mining
Congress, Salzburg Austria,
15-21 Sep 63 k

AVETWIN9 S.0.1 P8TUKWV'j, T.M.
. ......................
Oftnditions of genesis of rockbur3ts and
precautions against
rockburst hazard,16
Report to ba submitted for the 4th Intl.
Conference on Strata
Control and Rock Machlinice Now York, 4-B May
1964,

BORISOV, Aleksey Alekseyevich, prof... doktor
tekhn. nauk; AVFRS1UN,
S.G., akademik,, retserizent; ZHUKOV, V.V.p kand.
tokhn,nauk,
otv.red.; S-1IRENSHY, HX.p rod.izd-va;
IL'INSKAYA, G.M.,
tekhn. red.
[Calculation of rock pressure in longwalls of
flat seams]
Raschety gornogo davlenlia v lavakh pologikh
plastov. Mo-
skva, Izd-vo "Nodra," 1964.. 277 p. (MIRA 17:4)
1. Akademiya navk hirgizakoy SSH (for Avershin).

S'. G. ~; 11-TOKHOV, 1. M. .: VIS, 1. A.
"Gebirgsschlage mid Mabnahmen zu ihrer Bekwapfwig. "
report submitted for Mtg of Intl Bureau of Rock Me~.-Iiwiios,
Leipzig, Nov 65.
UdSSR, Frunsc~ Akademie der Wissenschaften der KirgisiGchen
SSR; Leningrad VNIMI

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ACC N14 AP6024416
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SOURCE CODE: UR/0020/661169/001/0158/13161
AMOR: Avorson, A. E.; Barzykin, V. V.; Herzhanov, A. G.
ORG41 Aulitmte of Chemical Physics. Academy of Sciences-SSSP/
(Institut khimicheskoy
Akadenii nau -SSS-R7-
f isiLki
TIUX: Therml theory of of condensed substances
SOURCE.-, M SSSR. Doklady, v. 169, no. 1, 1966, 158-161
TOPIC TAGS: Ignition theory, condensed system, Ignition AjjW
4."
ABS7RACT: Generalized equations are derived for the ignition of
condensed systems
under various boundary conditions, I.e., at a constant surface
temperature, a constant
heat flux to the surface of the coui)ustible. and under the
conditions of Newtonian
heat-exchange on the surface of the condensed system. The numerical
solution of' the
derived system of equations on an electronic computer yielded a
generalized equation
for ralculating the ignition delay of condensed systems over a wide
range of param-
etens. Ignition parameters calculated by the proposed theory are in
good agreement
with both ptiblished theories and published. experimental data
obtained for the is,nitiOn
of roMliii~(V 1. Lisitskiy, A. G. Merzhanov, Nauchno-tekhnich.
problemy orenlya i
vzrYU-417 Ho. i965). 1he authors thank ZA
_,S. Andrianova for programming the elec-
tronic computer calculations Orig. art. has: lotable, 2 fi res and 6
foraulta.VS]
SUB GODS: 21/ SUBM DATE,: i7Sep6 / ORIG REF: 05/ On REF- 664/ ATD
PRESS-,~-,Otyj,
Cgrd 11 46____

8/598 ', 61/00/006/011/+
D228/D303
AUTHORSt Upkeep Ya.bbv Averteevaj K.N~, and Koptsevaq I.N.,
TITLEs Studying tho character of the process of condensation
of magnesium and magnesium chloride vapors formed
during the Tacuum separation of the reaction mass
SOURCE1 kkademiya nauk SSSR, I Otitutimetallurgii. Titan i
yego splavyc nou 6j, 19?4, Metallotermiya, i elektro-
khimiyaptitana, 60 - 83
TEXT ii The authors btudied the prooess of vacuum separation
under-
high revidual preosures which make possible the condensation of
big
anA HgO12 vapors in order to try and find a way of both reducing
the 11g loss and deoreasing tba oondeneer dimensions, Aooording to
D.S. Kamenstskaya (Rif. It Sb. Premjnoni~e vakuuma v metallurgii
(Applicatiou of the aouum in Motal urgy Izd. AN 86BRt 1958) and
others, this process has to be conduoted at a high temperature In
the oondenser zono .,-. with reeidual pronsures In ex,3eos of the
va-
lues corresponding to the tripbe-polat readingat A vapor-tenaior,
of
V/
Card 1/3

Study;xig the ter of the D 8,, D-3 0 3
sequ-mtly oblained by ra-,,3ing the temperatu,e in the
condenae~- zone
tc% 61530, u3thwagh this tended -11~) d;.miniah the raTe cf
Au'~itionctl exper-'men-.s, in whi;h the conionser i&mperutare
was
,-iL~d fror. "'.0 -1c q",O,), Indien'ted Ilia-, the :ate
separa-.ion ~!on;~--
d4;:r,-,Ii-.y decreases above t-e r'*.-'cal 4empo:.,,a**Ora of
6--00, The a-.i.-
thoro t1jus con,,Iude that applicaticn of the syntem deveaoped by
thom will enELbA'e the density of -the cond&nsu*.~: -to be
incr-:?ased by
approxiTuttel.y two-fold. There aare -- f1gurets, 22 tablec, and
3 Scvict-
refc-rencee.
card

S/ 598 '161/1000/006/012/034
D2457D303
AUTHORSt Upkeep Ya.M*f Averteeva, K.N., and Kopteevaq IoNa
TITLEs Testing solid absorbents for vapor removal in produc-
ing titanium sponge
SOURCE: Akadftya nauk SSSR. Institut metallu~,gii. Titan i
yego aplavys no* 6, 1961. Metallotermt~a i elektro-
khimiya titana, 84 - 87
TEXIN The authors point out the undesirable effects of water
and
HC1 vapor8 in the vacuum separation of the reaction products
of
magneciothermal reduction of TIC11, H01 vapors can be
effectively
removed by a freeqing t*ps using iquid N2p but this has
disadvan-
tagos in practice. ccordingly, the following possible
absorbents
wero tested by drawing through H01 vapor with a control
traps of
liquid NV Oa, Mg oxidesp MgOI?p Cap solid NaOllp silica-gel,
acti-
vated charcoal, Ti powder, heated to 80000. $atisfactory
absorption.
was observed with (1) a mixture of activated oharcoal and Ti
powder
heated to 8000C and (2) a mixture of solid NaOH and Ti
powder (800
'DO). There are _1 figure and 3 tables.
Card 1,11

C/ I 37A,-11OnQA)()6A 3-1/ 1 3
AO()6/A V I
Al-I'MYLS - IAPK-~r~, Ya. M., Avortneva, K. 11., Koptseva, t.
~1
7'1'-
LT--! ltijdIes on the mture of the loll pro(ezt:
-Ttelgllr-~~11417 i:;,'
maF,ne,,Ium chlorii~e vapors, developluj,
reacilon mass
;1E.F11CIDTICAL, Referativnyy zhurnal, Metallurglya, no. 6,
(In ccllection-, "Titan I yego splavy", no AN,
80 -
t E" T; 7he authors studi,,:~d the process of vacuum
separation Jn apparat.;
v;.Ith ,pper and luwer condensers under conditions of highor
re!:I~iual Pr,?S-,U19
mm Tig) -.-ihich make it possible that MIg and Mgcl 2 vapors
1,.t,
r. liquid phase. The apparatus with a lower condenser yieltis
q r
a more dense structure on accoiint of partial melting out and
r~onrlen~~jitjon Into it
liquid phase of ~jg(,12. The Mg vapors were condensed merely
to ft plhz~,-.se
?artlal condensfitLon of Mg vapors, at first to a liquid
phasv. 1~',
tmn fig restdual pressure in the apparatus, a nr c)5()CC Jn
1-!~C

1,tud I er, on the nature of
/()_37/ A
AC('161 A 11 D A'
:A-paratinri zone and .500C in the condensatLon_zone. The
volum(~tr', ., -)j' f i -
-)ndensate Is then equal to 1,20 - 1.24 gl,-m-). 'Die most
den~5, cc,rid ri.-,;i t
'1 .4 - 1.~i g/cO volumetrlc weight, was obtained when the
,!~!riser 1-mie was inaintained equal to the Mg melting p,-)inr.
V
Vc,rol)' vi~va
Cx-,,stracterls note., Complete translation]
ca-rd

L 23177-66
F
ACC Nit: AP6006711 SOURCE CODE% UR 0105/65/000/006/0045/CK)'
AUTHOR;r Avetisy 1,.Dzh., A. (Ciwd1date of technical sciences,
Moscow)j
.gertir,ov ~Dto t -of technical sciences, Professor, Moscow)
A. I c or
ORO: n,)nc
iTITLE: Optimal design of the valient-pole field structure of a
synchronous machIne
SOU11CE: ElektricheAVO, no. 6, 196% 45-50
TOP:[C TAGSi synchronous machimo, digital computer, computer
calculation, magnett".
field, electric field, e1ectrAc motor
'ABSIRA(IT:An improved method of designing the field structure of
a 7nchronous
machino on computer Is suggostod. The uptiinality criturion Is
expressed through 11
utLlity function H a Fo, where F is the magnotizing force required
to convey that
flivi, t~trough the all-gap and antattre, and to offsot tho
armature reaction. The
utility function Is max-Iiiiized An this form-. M - Fo(h1a, b,,)
with h., > 0, bm > 01
hera lin wid bm aro goometric paramotors. Tho PirictIon viocOmmli
L; ,~na(;ht by the
vadlent method which requirea Iteration operations on -,A digital
compliter
the programing Is featured). L3 a result of computer
cai.culations, formulas ar*
f
C-Alrd 1/ 2 UDOt 621-313-32%001.12

L 23177-66
AGO Wk AP6006711
Idevolopod for the maximim usoNl field mapetizing fore,-.i,
optlp.Al Width and
oplAna holght of the polo coro. DprOCn data fnr S, 16, 70, 60, and
90-kw
obtlb)~,,A Ulo ikb~~-qo fw-111")1wi bind prr~
covjjlu-~d (tabOat-cd). "OptArl"A flold Fn~.Iiwor
_pIkatilina, In tho Coniputiw Leooratoi (LT, on ik 131~,Se-M
compitor,"
.,Y,J~it -y , L I
Orig. art. hass 4 figures and 17 formulas.
SUB CCDE1 09 MJBH DkTE, OSJIM64 CRID FMI 002 OTH RKF1 OW
Card 2,(2

23573-6
ACG NKt AP6002598 A
SOURCE COM UR/0286/'65/Cx)0/023/0093/C(193
AUTHORS: Gasparyanp A. MG; Alcopyan,
ORGt none
ent. Class 81, No. 176821
TVLEt Chamber feeder for pr!j
_Ar4qsqort equipm
SOURC'Zi Byulleten' itobrateni3r i tovarnykh tnakov, no, 23, 1965~ 93
TOPIC TAGSo pneumatic device, pipeline xMPWM&-
ABSTRACT: This Author Certificate presents a chamber f(jedor for
pneumatic
transport equipment. The feelcir consists of a cylindrical chamber
in the lower
portion of which an annular p)rous duct is mounted, fooding
compreased air into
thv cylinder, The inlet and )f the material duct, whore mixing of
tho friable
mater-'~al with air occurs, is placed near thb duct (seo Fig,. 1),
To eliminate
sourc;is of caking of the fria~)le material and to uniformly
dischrrIge the cham0er
of fr.able matorial, the anxniLur porous duct is made of sectors
separated from
each c:ther, each of which is 4,.onnected through an inlot tube to a
common
conprossed air distributor of the plug type. The distributor plug
irbich rotaten
0 ard 1/2 UDC: 6211.867 82t621.86.067.2

L 0513-66.
ACC Nits AP6002598
Fig. 1* 1 cylindrical
chamberl 2 - sectors of
porous ducti 3 - inlet
end of material duot;
4 - inlet, tubc; 5 - common
compressed air, distributor;
-.z:. 6 plug.
proviles successive feed of conpressed air into each sector,*
Orig, art, hass I.
di,~gram.
SU73 CODEs 13/ SUBM DAT&s 27Jun64
Card 2/2

AVERIYANMO, A., Clewe'. trubcogo tsakM.
-, [ -W -A ,
Decision of a general meting. Soy. profsolusr 5 no,5:25 W
'57.
(Dnepropetrovsk--Pipe, Steel) (KLRL lOtO

AY!j!,,jAV,jU&, L,,~ ri a GLOTOV, Turiy Georgiyevich;
POPOV,
'RovII
Sernfim ko"natan ON HC.-l- NOV, V.M., red.; MARCHUKOVA,
M.G.,
0
red.t2d-vn; LAVPXIOVA, N.D., tokhn.red.
[Uso of Onnts-Enk-ashek VIII IhR 216/)10 engInse by the
Satonian
merchant marine] Opyt eksplustatsil dvigatelai
Gsnts-Indrashek
VIII IhR 2161)10 ir Estonskom parokhodetva. Moskva, Izd-vo
OMorskoi transpor';," 1959, 4) p. (MIRA 12:12)
(Estonia--Merchant marine)
(Kerins diesel engines)

22423
S/049/61/000/002/001/012
3,4060
D242/D301
AUTHORS: A 0
Veytaman, F. S., Gallperin, Ye. I.1
Zverev, S. It., Zayonchkovskiy, M. A., Kosminskaya,
1. P., Krakchina, R. M., Mikhota, G. G., and Tulina,
Yu. V.
TITLE: Deep seismic: sounding in the transitional zone between
the continent of Asia and the Pacific Ocean during
the International Geophysical Year
PERIODICAL: Akademiya-nauk SSSR. -Seriya geofizicheskaya.
Izvestiya, no 2, 1961,.169-184
TEXT: As part of the IGY program scientisto.of..the.Inatitut
fiziki zemli.AN SSSR (Iristitute.of Physics.of the Earth AS USSR)t
the Vaesoyuznyy nauchno-isaledovatellskiy institut.geofiziki
Ministerstva geologii.i okhrany..nedr.SSSR..(All-Utlion Scientific-
Research.of the Ministry.of Geology and Mineral..Itesources.of the
USSR) and.other.organizations.investigated.the.ci7ustaI structure
of the Okhotsk Sea by means of deep.seismic sounding. The area
Card l/ 11

22423-
S/049/61/000/002/001/012
r%
Deep seismic sounding... D242/ D3-01
was chosen since very little is known of the.nature of
the crust
in, such transitional zones between continents and
oceans. It is
separated from the Pacij!ic by the Kurile Island Arc
which is
bordered by a deep ocean containing seismologically
active zones
with deep foci,.and..larg(-.positive.gravity.anomalies.
The main
observations were.undertaken.along profiles-with lengths
of
about 8000-km, orientated.transversely to.the supposed
structures
of the study area, as described by Ye. 1. Gallperin, A.
V. Gorya-
chev and S. 11. Zverev Mef. 1: Issledovaniye zemnoy kary
v oblasti
perekhoda ot Aziatskogo kontinenta.k
Tikhomu-okeany.(Investigatio-n.
of the Crust in the.Aren of Transition between.the
Continent of
Asia and the Pacific,Occan) Sb. XII razdel programmy ISGG
(seysmo-
Logiya), No. 1. Izd. AN SSSRt 1958) and by V. G.
Vasillyev et al
MI. 2: Issledovaniye 2;emnoy kory v oblasti perekhoda ot
Aziats-
kogo kontinenta k Tikhoun okeany (Investigation of the
Crust in
the! Area of Transition between the Continent of Asia and
the
Pacific Ocean) Sb. "Seycmicheskiye issledovaniya v period
MGG"
Card 2A1

22413
S/049/61/000/002/001/012
D242/1)301
Deep seismic sounding...
No. 4, Izd. An SSSR, 1960).- The area near Iturup Island was also
investigated on,a special. grid. The data was collected by the
methDd of movable explosion points with.single-point.recording
at fixed stations; the details are given by Ye. I. Gallperin and
1. P. Kosminskaya.(Ref. 2;: Osobennosti.matodiki.g:Lubinnogo
seysinicheskogo. zondirovarLiya. na more. (Features of the
Hethod'of
Deep Seismic Sounding..at.Sea) Izv. AN SSSR,.Ser. geofiz., No. 7,
1958).-Use was also madd.of.the.results-of..exper:Lments
conducted
by G.. A. Gamburtsev.(Ref. 6:.O.glubinnom
seysmicheskom-zondirovanii.
zeimay kory.i nekot"ykh drugikh prilozheniyakh motodom.vysoko-
chuviltvitel.lnoy zapisi seyamicheakikh-kolebaniy.(Me.Deep
Seismic
Sounding.of the Crust.and.some.other Applications by-the Method
of Hi.ghly-.Sensitive,Recording..of.Seismic..Oscillations) Izbr.
tr.
Izd. Akad. Nauk SSSR 1960 ) and P. S. Veytsman.(Ref. 7: 0 resul
tai;"-.h rabot po glubinnowu seysmicheskomu zondirovaniyu zemnoy
kory v odnom iz gornykh rayonov Sredney Azii (Results of the Deep
Seismic-Sounding of the Crust in a ~Iountainous Diotrict of
Central
Card 3/11.

MEN
22423
S/049/61/000/002/001/012
D242/D301
Deep seismic sounding...
Asia) Stud, Geophys. et Geodaet., No. 2, 1958) in.continental
areas of the.Soviet Union.. In.contrast to foreigi-practice, it
was possible.by employing several recording.stations.on.the line
of observation.to obtain the types of time-travel.curves shown
in Fig. 2 during a single. boat journey.. Wave recordings were
alsomade on.the explosion vessel.-The bottom of.reflections
provided information-on the.depth of water and th(s.structure of
bottoin sediments in.accordance with the procedure.mentioned by
S. M. Zverev (Ref. 10: 0 stroyenii.osadochnoy.toliihehi.nekotorykh
uchastkov.Tilchogo okeana po dannym seysmicheskikh otYazhennykh
voln (Structure-of the Sediment Layer of Certain.1'arts of the
Pacific Ocean from the Data of.Reflected Seismic Waves) Izv.
IN SSSR, ser. geol., No. 2, 1960). The explosions; of charges
weighing.about loo.kg.were.recorded on a low-frequency seismic
device with a. filtration range of 0.7 - 15 hertz at distances of
up to 200 - 250 Ian on the sea and..100.- 150 km on the ocean. The
receivers consisted of hydrophones with cascade.intensification.
Card 4/11

Deep seistdc
sounding...
Fig. 1.
Examples of
hodograph
systems ob-
tained in the
Okhotsk Sea
6-11)
ane: Pacific
Ocean (6-0)
Card 5111
P
r. ~.,.;,lu cucTot rwrWmll, lway-lellsm-,
)Xomtom mope (M-5-17-mr
it lixom 01(calle
S/049/61/000/002/001/012
Z~~J242/D301

22423
S/045V61/000/002/001/03.2
D242/D301
Deep seismic sounding...
The waves were separated.and correlated by.recording their inten-
sity simultaneously with.. the. construction -of. the
hodographs-which
were set out in such ei way that the coordinate. origin
correaponded
to the position of the rdeording station, the time of
wave-arrival
being plotted over the positi6ns of the.explosion sites. Despite
the complexity of the retordings, 'especially in island. and
litto-c-al
areas, several types of waves-related to crustal discontinuitiesp
bottom sediments and the water layer were dist.~Inguished on the
sciamograms, including refracted longitudinal waves associated
with boundaries in the sediment layer (Psed) and the actual
crual:
(P(3 and P*) and with'the Mohorovicic discontinuity at the base
of!
the crust. Waves of Vhe first type have speeds of 5 lan/sec and.
were. observed near the Mriles and on most sea profiles. The
velocities of -the PO. and P* waves mainly recorded in island
areas
and near KanchatIc'a-a'r'e &..and 6.5, - 7.1an/sec respectively.
The
leading P waves refracted from the,llohorovicie.discontinuity
Card 6/11

22423
Deep i9eismic sounding...
S/049261/000/002/001/012
D242/D301
travel'at speeds of about 8.5 km/sec. Waves (PR) reflected from
the Mohorovicic and other discontinuities were also noted in
addition.to the refracted waves, although it was only possible
to diatinguish them with any clarity in certain regions -
mainly
the northern and central parts of the Okhotsk Sea, where their
amplitude is greater than that of the other wave-.types.
Analysis
of the hodographs discloses the existence of.three main
wave-types
defined by differences in the arrival and transit: time of the
waves,. by the areas where they were rec6rded and by the
presence
or absence of the PO and P* groups (Fig. 9). By plotting the
values for the relationship of the mean velocity v to the depth
h, three types of velocity cui-ves,corresponding to
continental-,
intermediate- and oceanic-type-hodographs were also.obtained.
Cont:inental-type.hodographs.ax-c characteristic of-large areas
in- the northern. and.central. parts of the Okhotsk Sea. and
in the
northern Kuriles, where.work by P. S. Veytsman et al (Ref. 11:
Nekotoryye rezulltaty izucheniya.stroyeniya zerinoy kory v
oblasti
Card 7/11