SCIENTIFIC ABSTRACT V.L. DOBROVOLSKIY - V.V. DOBROVOLSKIY

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• Collection: Scientific Abstracts
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• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 13, 2000
• Sequence Number: 2
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

ww
S/040/60/024/005/024/028
0111/C222
On the Application of Complex Variables for a Plane Plastic
Deformation
Theorem 1: In order that the function F(z,z) defined by
(1-7) is real
it is necessary and sufficient that
z 2eiQ V e_'Q
-6,i2 -
is satisfied.
Theorem 2z The partial solution 9 = Q(Z'i) of (1.8)
containing no free
parameters determines the tension components up to the
constant hydro-
static pressure.
Theorem 33 In order that the tension function F is
biharmonic in the
plastic domain it'is necessary and sufficient that 0
satisfies the system
-62() 2g 2 2 0
(1-13) ; 2 _2 0, 2 0.
x ~-2 e
y )x ax 3cay
The class of solutions of (1-13) is not empty, e.g.
1) 0 - const, 2) 0 - -2 are tg ky/x) + const.
Some particular solutions of the(e~uilibrium conditione in
the plastic
domain are given, eag.: if 9 - 0 y then 9 - are s4n(Ay+B);
if 0-.-2,f +R(r)
flay-A 'J/4

87800
S/040/60,1024/005/C24/026
0111/C222
On the Application of Complex Variables for a Plane Plautic
Deformation
then 0 = -2%f +arc sin (a- b2
r
To the first case there corresponds the tension
distribution in a strip
comprbssed by rough plates. In the second case, for a = b =
0 one has
an axialsymmetric, tension field, for a - 1, b - 0 tho
state of stress
of a plastic wedge with a uniformly distributed load on the
lateral
areas, etc.
The author mentions L.A.Galin. There are 3 Soviet
-.,eferences.
Card 4/4

DOBROVOLISKIYI V.L. (Mookva)
Plane plastio deformation of snisotropic materiale.
Prikl. mat.
i mekh. 25 no,ltl69-173 Ja-F 161. (MIRA 14:6)
(Deformations(Mechanicli))
.-,- , t k11

KUPRADZE, Viktor Dmitriyevich; Dq~qyq~~'
_PKIY, V.L.., red.; AKSELIROD,
I.Sh., tekhn. red.
.[Method of the potential in the theory of
elasticity] Fletody
potentsiala v teovii uprugosti. Moskvap
Fizmatuiz, 1963.
472 p. (RIRA 16:12)
-- (Potential, Theory of) (Elasticity)

DOBROVOLISKIY, V.L. (Moskva)
Solution of certain problems on stress concentration in the theory
of elasticity. Inzh.zhur. 3 no.4t732-736 163. (MIRA 16:12)
1. Institut makhaniki AN SSSRO

DOBROVO.T.1iSKTY, V.I.. (~10!;]CVa)
,-~c-lution Gf a nnnlin,.~nr pro-blem of c" 'aree
i,lowing 4;; a -,hL!f t,
fur'na!-(.. 1r,zh.7,hur. 5 no..I~.1711-176 165.
('11TRA 18~4)

b 04914-67 M'(1)/5d(M'
AW - AP6028708
E
AUTHOR: Dobrovol'sTkyy, V. M.-Dobrovollskly, V. M.
ORG: Kiev State University im. T. H. Shevehenko (Kyyivslkyy
derzhuniver"t)
ley
TITLE: Surface magnetoconcentrattonal effects. 11. Inherently
conductive semiconductors
SOURCE: Ukrayinsqiyy fizychnyy zhurnal, v. 11, no. 8, 1966,
836-844
TOPIC TAGS: germanium semiconductor, space charge density,
electromagnetic field,
electron density 4k
ABSTRACT: The author)develops the theory of
magnetoconcentrational effects in an inherently
conductive semiconductor and sh(nvs that dependence of
characteristics of the surface space
charge region on electric and magnetic fields acting on the
specimen Is affected by variation In
electron-hole pair concentration at the boundary of this region
with no substantial change in
charge valu?4tself. The highest values of the effects studied
occur In semiconductors, i.e.,
.germanium,'~kaving carriers with long life and high mobility.
The basic characteristics of the
surface space charge region are calculated and the distribution
of charge carrier concentration
throughout the semiconductor mass and carrier distribution in
the surface space charge region
are determined. The calculations do not take Injection level or
mechwitem of carrier genera-

L o4914-67
ACC NRs AP6028708
tion at surface space charge boundary into consideration, but this
does not affect the validity of
the equations presented. An extensive definition Is given of
conditions under which the effect
of Lorentz forces Rnd of recombination on electron-hole
distribution in the surface space charge
region. The author thanks 0, B, Zints for discussing the work.
Orig. art. has: 26 formulas,
2 figures, and 2 tables.
SUB CODE: 12120L SUBM DATE: 2lJulr,6/ ORIG REF: 005/ OTH REF: 003

DOBROVOLISKIY, V-N-,. inzh.; LU7111, H.F., inzh.; S
MTS, I.L., inzh.
omA renaWa-6n-marine, power plants used on whalers.
Sudostroanie
24 no.9:40-42 S '58- (MIRA 11:11)
(varine engines) (Whalers)

STEKWV, V.7u.j ZOLOTAREVP T.L., prof., red.;
BURLAK, I.N., red.j
DOBROVOLISKIY, V.N.
[Eleotrifleation is the road to communism]
Elektrifikatsiia -
put' k koftnizmu. Moskvap lzd-vo "Sovetskaia
Rossiia," 1961.
88 p. (Bibliotachka "Nagliadnaia ta~siia,
propaganda i
khudozhestveWe oformleniel" no.6 (MIRA 15:2)
(Electrification

SOV-120-58-1-29/43
ATJTHOR:.DobJ~ovol'skiy. V. N.
TITLE: An Oscillographic Method for Determining the
Parameters of
0
the Characteristics of a Detector (Ostsillograficheskiy
metod opredeleniya parametrov khar~kteristiki deteictora)
PERIODICAL: Pribory i Tekhnika Eksperimenta, 1958, Nr 1,1
pp 123-124 (USSR)
ABSTRACT: The static characteristic of a -ermanium. detector
in the
0
forward direction can be described by the expression:
I - Is [exp cx (V - Ir) - . (1)
where I is the current to the detector, V is the
applied potential, r is the base resistance and the other
symbols are the parameters of the characteristics. If the
.current flowing through the detector is of the form
I =.I 0 exp(-kt) then the potential across the-detector can
be obtained from the follo-Ing expression:
I oe:cp(- kt) - Is [exp a (V - Ir) (2)
Card 1/5

SOV-120-58-1-29/43
An Oscillographic Method for Determining the Parameters of the
Characteristics of a Detector.
The values of V as a function of time may be divided into
three regions as follows: (I) IrA7 and dV 1 Here:
1 k
V - ln(I0/1 5 - t (4)
a OL .
(III) For large values of the current when Ir cannot be
neglected compared with V we have:
V ln(I /I LI: - t - I r exp(- kt) (5)
a 0 S OL 0
The three cases are illustrated in Fig.l. The graph of V
as a function of time is a straight line in region II and
curves off in regions I and III. The measurement of (x and
Card 2/5

SOV-120-58-1-29/43
An Oscillographic Method for Determining the Parameters ol
tb.e
Characteristics of a Detector.
Is was carried out by means of the circuit shown in Fig.2.
A symmetric rectangular voltage waveform having a frequency
of 50 c/s derived from an oscillator is applied through an
RC circuit to a detector d whose characteristics are to be
determined. Since the resistance R which is in series with
the detector is much larger than the forward resistance of
the detector, it follows that when the positive part of the
oscillator output is fed to the detector the current through
the latter is of the form I = I exp(-t/RC). The time con-
stant of the circuit was chosen ?o be much smaller than the
duration of the pulse which ensures full charging up of the
capacitance during the pulse and consequently a change in
the current through the detector from Io to zero. A diode
Card 3/5

SOV-120-58-1-29/43
An Oscillographic Method for Determining the Parameters of the
Characteristics of a Detector.
connected in parallel with the detector discharges the
capacitor C and the output caDacitance of the oscillator
at the end of the positive of tiLe cycle. The waveform of
the voltage across the detector was observed on an oscillo-
graph screen and the value of Io was so chosen that the
region III was absent and hence the values of Is could be
measured, using the formula:
is = 10/exp dVo
(6)
The values of I could be determined directly using a
s
scale attached to the screen of the oscillograph. A
typical oscillogram is shown in Fig-3. R. N. Bondarenko
Card 4/5

SOV-120-58-1-29/43
An Oscillographic Method for Determining the Parameters of the
Characteristics of a Detector.
is thanked for suggesting this problem and interest in the
work. There are 3 figures and 2 Soviet references.
ASSOCIATION: Kiyevskiy gosudarstvennyy universitet (Kiyev State
University)
SUBMITTED: June 24, 1957.
1. Detect6rs--Analysis 2. Germanium--Applications 3. Detectors
--Performance 4. Oscillographs--Applications 5. Mathematics
Card 5/5

I
W.DORWM,!8lI
4AWM
Diffusion and reicombination during the measurement of
drift mobility,
Pizetvaretela, I no*5:719-725 Pq 159. (MP.U 12:4)
1. Ityevskiv goeu&aretvwmyy universitet, im. T.G.
Shevchenko.
(Semiconductors)

IASHUM, VoYs, Clashkarlov,, V.IZI; 13ONMRMMDP R-N-
[Bondarenko, RAI;
DQAtO=~SXIT,-.V*N. [Dobrovollelkyip V.M.J; MWIN, G.P.
[Zubrin, H.P.1;
LITOVCII V.G: Dqtovehenko, STRIM, V-I-
Properties of germanium oontaining beryllium admixtures.
Ukr# fiso
zhur. 4 no.3:37P.-375 My-Je '59. (KMA 13:2)
1,liyevskiy, goeudarstvannyy universitet im. T.G.
Shevehenko.
(Germanium) (Beryllium)

LL
V. IV/
26599 S/185/60/005/003/005/020
Is D274/D303
AUTHOR: Dobrovollslk~y, V.1-1.
TITLE: Effect of the magnetic field on the flow of minority
carriers
PERIODICAL: Ukrayins'kyy fizychnyy zhurnal, v. 5, no. 3, 1960,
333-344 ,
TMCr: The problem is considered in the linear approximation
with
respect to carrier concentration, for a homogeneous specimen
under
isothermal conditions. Spherical energy zones are assumed. (In
the case of ellipsoidal energy zones, the theory yields a
qualita-
tive picture). The basic equation of motion of hole
concentration
is a_lj . - X - 1,v. ip (1)
;) t T e
where'V is the concentration, U - the lifetime of minority
holes,
jp - the density of the hole current, e - the electron charge.
An
Card 1/6

26590 S/185/60/005/003/005/020
Effect of the magnetic field... D274/D303
analogous equation can be set up for electrons. The
expression for
the density is given:
ip - ePPp8 - ~TFpVv + e1pp8 x H - kT-LpVv x H +
where + eKppH x (H x kt;H x (H x VV). (2)
P Po + V ; (3)
'U, 2e (2kT 2 L _xdx
)2
3 FM_ lie-xxdx; Li a 3jr-f MiX2e
T '~C_ x +
0 ~O
denotes mobilities, t - the free path, p. - the
thermal-equilib-
rium concentration of holes. Analogous expressions hold
for elec-
tron-current density. An n-type semiconductor is
considered. The
field H is assumed homogeneous and parallel to the z-axis.
Substi-
tuting (2) in (1), and neglecting second-order quantities,
one
obtains
C ard 2/6

26590 S/185/60/005/003/005/020
Effect of the magnetic field... D274/1)303
&*J-
+ ~P&o x R + !~ x (H x
V +

at

+ hz_ !~H2Ax,y)q, Ax,y
e
+
2
(6)

&Y2
ax

where
0 is the electric field in the
specimen before the
injec-
tion
of carriers. For the case H.LjO or
IjO QO being
the
elec-
trical-carrent density in the specimen),

Eq. (6)
reduces to

O-V
t =

~_V -V
+ i) aLV + i)y L2_V +
- VXV x
a2,j 2
D z _ .
I

(7)
a
Y
2
ay ax2 ay
r
az2

where
are the velocities of carrier transfer, and
vx and v

DX9 Dy
DZ -
y
diffusion coefficients;

Dx z D kT (- _ v u2) D
e ~P -Pn z
- kT-
- _ePP,
(10)
Eq. (7) describes the flow of carrier concentration which
can be
Card 3/6

20~91 S/185/60/005/003/005/020
Effect of the magnetic fie! d... D274/D303
characterized by the quantities ~Lx,~Ly, Dx, Dy, Dz. In the
follow-
ing, the value of these quantities in particular cases is
considered,
as well as their physical interpretation. Analytical
expressions
are obtained for these quantities in the case of weak and
strong
magnetic fields, and the power-law dependence of a free path
on vel-
ocity. For the case of the independence of a free-path,
graphs are
given of these quantities as functions of the magnetic field
(which
include also intermediate fields). Some of these graphs were
taken
from 0. Madelung (Ref. 10:. Z. f. Naturforsch. I 8a, 7919
1953).
Eq. (6) was obtained by neglecting second-order quantities;
this is
justified if the n-type semiconductor has a fairly high
conductivity.
1%rther, expressions are derived which hold for arbitrary
conducti-
vity. The physical interpretation of obtained formulas is
discussed.
The first term in the formulas for u Y] is due to the effect
of the
Lorentz force, the second - to the Ha - field 6 Oy* If the
latter
is zero# Jiy decreases. The magnetic field has no effect on
car-
riers which flow in the direction of the field, but it is
effective
Card 4/6

S/185/60/005/003/005/020
Effect of the magnetic A~e D274/D303
if the carriers flow perpendicular to the field. For
sufficiently
strong magnetic fields,)Ax changes sign, i.e. the minority
holes
flow in a direction opposite to the direction of the
electric cur-
rent. The sign-change of Px leads to the conclusion that for
strong avAgnetic fields the injection of minority carriers
causes a
reduction in conductivity. - This is in agreement with
results reach-
ed by other authors. Experimental determination of/Ax,/uy
DX9 Dyl
D is then made. Eq. (7) is considered for the case of a
;late in
t~e xy-plane and perpendicular magnetic field. It is found
that -
~L and D can be experimentally determined. The measurement
Of
in a small magnetic field in conjunction with Hall
measuremekts'Ir.
the determination of ", on a specimen whose shape ensures
OY - 0
with simultaneous measurement of Ax, make it possible to
determine
the Hall mobility of-minority carriers, as well as the
ratio of
Hall- to drift mobility; a correct measurement of this
ratio is
very important, and there are in literature no methods for
measuring
this ratio for minority carriers. The measurement of )A.
and D on
Card 5/6

26598 S/185/60/005/003/005/020
Effect of the mapetic. fie,ld6.. D274/D303
n-type germanium permits determining the concentration
ratios and
the mobilities of light and heavy minority holes. There are
5 fig-
ures and 22 references: 10 Soviet-bloc and 12
non-Soviet-bloc. The
4 most recent references to English-language publications
read as
follows: E.M. Conwell, Proc. IRE, 46, 1281, 1958; R.W.
Willardson,
T. Norman, A. Beer, Phys. Rev., 96, 1512, 1954; N. Harrick,
Phys.
Rev., 98, 1131, 1955; W. van Roosbroeck, J. Appl. Phys.,
26, 380,
1955.
ASSOCIATION: Kyyivslkyy derzhavnyy universytet im. T.G.
Shev-
chenka (Kiyev State University im. T.G. Shevchenko)
SUBMITTED: October 16, 1959
C ard 6/6

?3 8
S/182 /j 1/003/005/033/042
16 3r B108/B20.9
17
AUTHOR: Dobrovollskiyt V. N.
TITLEs Propiwation of excess carriers in an salisotrbpic cubic
crystal under lb-ar-actkun. of a magnetic field
PERIODICALs. Fizika tvaidogo, tela, v. 3p,no. ~,1'1961,..1.574 - 1580'
TEXT,. The author describes th6 propagation of excess carriers in a
ma " tic' field by-means of the phenomehologioal equAtions of a current
thMugh an anisotropic cubic orystal~ On the as.slim~ptio,n that in the
n-type
hample conoernedg the concentration of excess oarrivrs is low as
compared
to the ,eleotron~.oonoentration ( y,.~cn)j the linear approximation
may be
used. The phenomenolog;cal 'equation for the hole current in the case
P
of a gradient of the carrier concentration (Ref. 20: P. Seitz. Phys.
Rev
22, 372, 1950) h 9 the form
-CIL
jF CE -i- I&PxE X BPPEH2 T~R (E, H) -4- 8,,rE]
krt%~ LVv -I- %,,Vv X NP..vv~' TH (vvl H) gjrVvj.
Card 1/6

23328
8/181/61/003/005/033/042
Propagation
of.910889.'849 B108 B209
where,"p and are the oarri9i and the Hall mobility, respectively;
C PH . I
AP P v P.Pare phenomenological constantel Felated,to the a.onstants
of Seitz's paper as followsi
P 601
(2)
is,the conductivity of the samples; T is a tensor with the componen-ts
0
t COS( y"', H32 COS( 23) Cos (,^y3) (3)
M Cox (Z"'1") Cos HI, Cosx 2
YI
(^ ), ( ), ( "' e
X1 y1 x2)1,eto. are th ailgles between the coordinate axes and the
crystallographic axes L100], '010 , 1-0011. Taking the magnetic field-
H to be homogeneous-and orienteA in the direction of the Oz axis, the
equation of continuity yields
Card 2/6

23U8
811811611003100510331042
Propagation of excess... B108/B200
-14 (E,) 4. 1,090 X H I..H (E0 X H)
(5)
Dv
D. kr
--w-~PjHla i, AL
dxdy
Y, and pf 'denotes the electric
it, linear approximation-with respect to
fielt: in the sample before the introduction of excess carriers, and
j- is
their .lifetime. 'The first term in Eq.,(5) is'related to the carrier
drift,
and the cecond to diffusion. For the case of a.tranaverse magnetic
field
Hi J. J" current density in the aiampla) one'obtains
Eft ',rH'
as- o0 (7)
Eor Ea.,
Card 3/6-

233A
8/181/61/003/005/033/042
Propagation of exoessee.. B108/B209
and, with Eq. (5). the.foilowing expressions.for the carrier
propagation:
Ov av L
---V. vs, V. "Os
t
(8)
Vs
H-+-
(9)
0
For the case H.11 j one has
-11 Ok 4- tl,&Eo X H -I- PPEOW IPH (E,, X H)
(9a)
1 -4-8 PTEOI Dv -
D T..w
dxd.V
Card 4/6

23128
SliaIJ611003100510331042
Propagation of excess.... B108/B209
and
.0
E0, o4 Q P.H2 y.hl -4- B.Q,
oil
(7a)
=.-tat Eo.,--.
Ea;
v V V are the transfer velocities of concentration in the directions
Z_
9f the respective axesle may be considered-to be some effective
*X z
mobilities;'the'term D r describes the carrier diffusion:
Dv Br, Do, D,.!!!,-
Wr
t
',The author point3 out the possibility of experimentally
determining the
phenomenological parameters of theory. Professor V. I. Lyashenko is
thanked for his ielp and interest in this work. There Are 1 figure,
Card 5/6.

23126
S1181 61/003/005/033/042
Propagation of excess... B108/B209
1' table and 21'refetencesi 14 Soviet-bloo.and 7 m*on-Soviet-bloo.
ASSOCIATION: Kiyevskiy gosudarstvennyy univbrsitet imeni T.- G.
Shevchenko
(Kiyev State Univer'sity imeni T. G. Shevchenko)
SUBMITTEDt December 6, 1960
Card 6/6

7
AUTHORS:
TITLE:
PERIODICAL:
2M2
S/18 61/003/009/014/039
B102YB104
Dotrovollskiy, 7. N.,and Lyashenko, V. I.
Sbidy of the drift of the excess carriers in the magnetic
field
Fizika tverdogo tela, v. 3, no. 9, 1961, 2646-2658
TEXT: The propagation of an excel-, carrier concentration in
n-type and
p-type germanium located in a trwisverse magnetic field and
traversed by
current has been studied theorlitically and experimentally. Fig. 1
shows
the orientation of the field components on the specimen. Using
equations
given in UFZh, ~, 333, 1960 for the cases E . Eo and E - 0 (E0 -
oy 0y 0y oy
Hall field), the author derives expressions for the carrier
mobilities.
The carrier drift was experimentally studied by measuring the field
dependence of the quantities 11 /F. and ~0 /F, (relative hole
mobilities)
'~~x P py P
and the analog quantities for electrons. For a short time an
approximately
100-tLwide light line was projected to the germanium plate in
which the
carrier drift was studied. The carriers produced by this light line
Card 1/5

28082
S/1 61 /61/003/009/014/039
Study of the drift of the excess ... B102/B104
propagated and, after a certain time, reached the collector which
~Vas
located at the distance bx 0 from the light line. This time was
measured
first at H - 0 (t 0) and then at H / 0 (t 0 + tit) at constant
Eox . t0 and At
were measured at different numbers of electron-hole pairs.
Subsequently,
the authors extrapolated for zero. From the thus obtained values
to and Ato
0
the authors calculated the relative carrier mobility using the
relation
t0/(t0+ At0). ~:P ~ ([LJ P where tL, and pi
0 0 1 + I'L2p2)/(Pl + P2)
denote the mobilities and the concentrations of the light and
heavy holes.
To determine I /1-L. the light pulse was projected to the
specimen in aline
1'~y p
which is shown in Fig. lb and the distances by 012 and bx 0were
then
measured in which the maximum carrier concentrations were
observed after
the time t0 . kfter extrapolation for zero pair number the
relative mobility
0 f 0
was calculated by the relation IA.,' /t_i = by /26x0. Hence, the
otherwise
py p 0
equivalent methods differed in that in the first case time was
measured at
Card 2/5

2, 0.
S11811611003100910141039
Study of the drift of the excess ... B102/B104
constant distance, in the second, the, distance was measured at
constant
time. The practical measurements were made in two h-type and
one-p-type
germanium specimens. The results were in good agreement with the
theory.
Usi.ng these results the authors calculated r - P2 /p, and A1(2/P'l'
i.e.
equation
10 (yj) AK' (1211)
top"= A RP; FV=:__2V 1 A
9*1 IH2 91C 1 -#.- r 2PPH 2. (9)
16ci f6c' (-I-:~ 7r)
was solved graphically. The following values were obtained for the
rela-
tive Hall mobilities of the light and heavy carriers; -
H , 0: NHall/iyp -0.94; F .94. H - 3,000 oe : ~LiHall/xi = 1.03;
.aHall/Fp' = 1
)1, t 1.19; 11 - 1.76. In general, different values were
Mall/~ 2 - TpHal tp
obtained for Hall.mobility and drift mobility and if the mean free
path of
Card 3/5

28082 S11 81 /61/003/009/014/039
Study of the drift of the excess B102/B104
the carriers was independent of velocity their ratio was 1. 18
for light and
0.94 for heavy holes. Finally, the authors thank Yu. I, Gorkun
for dis-
cussions. There are 6 figures and 14 references: 8 Soviet and 6
non-
Soviet. The-three most receni references to English-language
publications
read as follows: E. Conwell. Proc. IRE, _4,.6, No. 6, 1958, B.
Abeles a.
S. 11eiboom. Phys. Rev., 22, 31, 1954- M. Prince. Phys. Rev. ,
92, 681, 19536
ASSOCIATION:. . Kiyevskiy gosudarstvennyy universitet im. T. 'G.
Shevchenko
(Kiyev State Univer'sity imeni 91. G. Shevchenko)
SUBMITTED: April 5, 1961
Legend to Pig. 1, a) arrangement for measuring I b) for
measuring 1.0
11~x py
_W.-ligl~t line; K - collector
Card 4/5

-DOBROVOLISKIY, V.N. I LMIENKO, V. I.
Determining the diffusion coefficient of current
carriers.
Prib. i tekh.eksp. 6 no.4:115423n-Ag 161. (MIRA
14:9)
1. Kiyevskiy gosudaratvewW universitat.
(Electric fields-Measurement)

S/181/62/004/002/003/051
B102/B136
AUTHOR: Dobrovollskiy, V. N.
TITLE: Photoelectric Hall effect and photoconductivity in a
magnetic field
PERIODICAL: Fizika tverdogo telat ve 4, no, 2, 1962, 329-335
TEXT: Photoelectric Hall effect and the photoconductivity of a
semicon-
ductor in a magnetic field are studied on the basis of the
kinetic
equation. A new galvanomagnetic effect is discussed that of
negative
photoconductivity in strong magnetic fields which was first
described by
the author together with V. I. Lyashenko (FTT, 3, 2646, 1961).
This
effect was also experimentally observed (DAN SSSR, 136, 329,
1961). An
n-type semiconductor plate with n ~> p is considered. It is
placed in a
0 0 1
magnetic, an electric and a light field (Fie. 1). A oonstant
current, I,
is assumed to pass through it. The ratios V x - AVx/V ox ,&R/R
0 and
V , AV /V are calculated for a piece of the specimen, bounded
by'
y Y oy
Card 1/0

Photoelectric Hall effect and...
X=+a and Y-+ b; R 0 is its resistance.
- , ~x px - ppyctg 9
vy -N ImC a
~j ?Abvotg 9 ~
vx v - 0 P
y IAnx
S/18 62/004/002/003/051
B102YB138
(2)
6N P
N R; No.- n w; bN Andw; AP - bpdw.
N 0 f
.0 0 W
g6
4-f0" tg It,,, - t~"~t
Paz R11Y tg 0,
tgo= E" LO
Pa.
are obtained with
(4)
Card 2/f

Photoelectric Hall effect and...
2; H,
PF P
L, lo:
0
J4221
S/181/62/004/002,/003/051
B102/B138
L.H,
fly
Kc- 9% 'OAf3e'rde
JrCS 1 9 -f-- Tj-
0
9-X A= 4eIj (t) -!~L; i 1, 2,
f6- 2
P=po-'-AP; n=no--i-An.
N0 .AN and AP are the numbers of equilibrium electrons, excess
free
electrons and holes, respectively, 9 is the Hall angle. The L
and K i
integrals are calculated for m i = 0 and high H (piH/c ~11).
Card 3/0

34221.
5/181/62/004/002/003/051
Photoelectric Hall effect and... B102/B138
LiH= VW
2 '0 e-Y11da
L'(T,) 2T, -t- 2 6T1 ell [1 - 41
o
cc
j 1 - T, -4- Tj'e7'E (-Ti),
& -4-
0
ID e--da; E, (-r)
J
0
Using these relations, the dependence of V y
2H2
!~c~ is determined for the case AN
16
(5)
X
r
Vy/W and of Vx VxId on
AP. The results are shown
in Fig. 2 for IA2 /'Mj = 8, P2/Pl - 0.02 and 1.-.n/1.,p - 2. For
-- ; 'M 2/v. -10 H 2. It may be seen that negative
1-1p= 2000 c see, 1-75*10
photoconductivity is to be expected if the H values are high
enough. For
Card 4/1 _~ I

3h221
S/181/62/004/bO2/003/051
Photoelectric Hall effect and... B102/13138
n-type Ge the reversal will occur at H >45,000 oe at room
temperature;
below this the critical H-value will also be lower. Similar
considera-
tions are made for weak fields jkill/c't 1. Professor V. I.
Lyashenko and
A. A. Ostroukhoy are thanked for discussions. There are 2
figures and
4 referencea: 3 Soviet and 1 non-Soviet. The reference to the
English-
language publication reads as follows: F. v.d. Maeson. Phil.
Res. Repts.,
jA, 107, 196o.
ASSOCIATION: Kiyevskiy gosudarstvennyy universitet im. T. G.
Shevchenko
(Kiyev State University imeni T. G. Shevchenko)
VO.
SUBMITTED: July 18, 1961
Fig. 1. Illuminated
part of specimen.
Card 51V
A~A 0
//%/
All
Y. I
H
( N illuminated
surface

h4135
8/181/62/004/010/019/063
2 1~ 61 B108/B104
AUTHORSt Dobrovol'skiy. V. N., and Gritsenko, Yu. 1.
TITLEt Use-of the Hall-current in investigating the scattering of
carriers in semiconductors
PERIODICkL: Fizika tverdogo tela, v. 4, no. io, 1962, 276o - 2769
TEM A method of measuring the Hall ourrbnt is proposed. In certain
bases such a method can be more useful than measurement of the Hall
emf as
it allows the carrier mobility to be'determined from the
resistivity of the
specimen. The Hall current can be written as-the ~um of a surface
and a
volume current. These two components can be 'determined
individually by
measuring the total Hall current and the conductivity as depending
on the
voltage applied to the specimen. From this dependence of the
conductivity
it is possible to find conditions under which no surface bending of
the
bands occurs. The surface conductivity is then zero, and the total
Hall
current equals its volume component. Such conditions can be realized
-surrounding the specimen with a protective ring. When this ring is
also
connected to the circuit it,.will act as the part carrying the
surface Hall
current, thus eliminating surface effects in the specimen. In this
way it
Card 1/2

sll8lV621004101010191063
Use of the Hall current ... B108/B104
is poseible,to examine the processes taking place,in the volume
alone. Hall
current measurements were made with cuprous oxide. It was possible
thus
to establish a relationship:between the carrier mobility and the
resistivity
of the specimens (Fig- 4), which could not be done from measurements
of the
Hall emf. There are 4 figures and 1 table.
ASSOCIATIONt Kiyevskiy goeudarstvennyy universi~tet im. T. G.
Shevchenko
(Kiyev State t.ni.vqsity imeni T. G,, Shevchenko)
,SUBMITTEDs May 18, 1962
Fig- 4- Hall mobility as a function .+f
too-
of resistivity.
Legends (1) mobility, determined,
from Hall current; (2)'mobility,
determined from-Hall e.m.fe'.
to to! to' to,

44138
5/i$1/62/bO4/010/025/064
BIOB/BI04
AUTHORs Dobrovol'iskiy, V.fN.:
TITLEi Study of the conductivity due to excess carriers in a
magnetic field
PERIODICALt Fizika tverdogo tela, Y. 49 no. 10t 1962, 28o6 - 2812
.TEXTs The conductivity due to the injection of excess carriers into
a
p-type*germanium was determined in dependence.on the inten ity of a!
"*a -
verse magnetic'fi'eld. The c4ange's in voltage drop along the specimen
when.
excess carriers wer.e introduced were measured.as AVO without a
magnetic
field and asAVH'.Jna magnetic field. The relative, 'change in
resistivity
measured was f6und to agree very well with-the theoretical formul's
_(1 + )AV /A%Q., where Q is the resistivity, ~tn and are the
Pln/~7p HQo
electron and hole mobilitiee (FTTo 49 329t 1962)6. At liquid oxygen
temper-
atureq the excess carrier conductivity was.found to reverse its sign
at a
field+strength of 4500 oe,.~qing negative frop that value of H ont
There
are 4 figures.
Card 1/2

B/161/62/004/010/025/064
Study of the conduollvity*d64~to.... B106/BI04
ASSOCIAT.IONs Kiyevskiy gosudarstvennyy univeraitet im. T. G.
Shevchenko
(Xiyev State tirfiveraity imeni T. dlv~'Shevchenko)
SUBYITTE~ I May, 2'-~, 196?

V;wH)
S/',85/62/007/003/012/015
D299/D301
AUTHORS: Karalinyk, S.M., Hurs'ka, A.P. and Dobrovol's1k;y V34
TITLE: Study of characteristic absorption of X-rays by ger-
manium-aluminum alloys
PERIODICAL: Ukrayins1kyy fizychnyy zhurnal, v. 7, no. 3, 1962,
327 - 330
TEXT: The position of the K-edge of absorption of Ge in
the investigated alloys was studied in comparison with its
position
in pure Ge. The Al-Ge alloys contained 1, 2, 3, 8, 27 and 96
atom. % Ge,
respectively. The displacement of the K-edge of absorption in
Al-Ge
and in pure Ge at high temperatures (400 - 4300C) was compared
with
izs position at room temperature. The tabulated values are the
aver-
age results of many repeated experiments. Thereby, the
thickness of
0
the absorbing layers varied,as well as the height and width of
the
diaphragm, the operating conditions of the X-ray tubesi and
the num-
ber of pulses. The shape of the K-edge was similar to that
obtained
Card 1/3

S/185/62/007/003/012/015
Study of characteristic D299/D301
by other investigators. It was found that at high
temperatures, the
K-edge of absorption of Ge was considerably shifted (about
6 ev.)
for low Ge concentrations (2 - 3 atom.%). No such shift was
observed
at room temperature. The X-edge shift at high temperatures
is rela-
ted to the complete dissolution of Ge in the solid
solution. It is
noted that the magnitude of the observed shift is greater
than that
of Ge02. The K-edge shift in the system Al-Ge is. explained
by a me-
chanism proposed in S.M. Karallnyk et. al (Ref.l: Ukr.
fizychn. zh.,
6, no. 1, 1961); thereby it is assumed that the
redistribution of
electrons of the Ge-atoms during its dissolution in Al,
takes place
at external orbits and the size of the Ge-atoms increases.
The pres-
ent study shows that the results obtained in Ref.1 (Op.
cit.) (with
Cu-Al and Zn-Al) are not accidental, but apply to various
systems.
The value of the obtained results would increase even
further, if
the X-ray investigations were extended to the spectra of
the solvent
(in the given case -- Al). There are 2 tables and 5
references: 4
Soviet-bloc and 1 non-Soviet-bloc.
Card 2/3

S/18 62/007/003/012/015
Study of characteristic ... D299YD301
ASSOCIATION: Kyyivalkyy derzhuniveraytet im. T.H. Shevchenka
(Kyyiv
State University im. T.H. Shevchenko).
SUBMITTEDa June 20, 1961
f
Card 3/3

DOEROVOLISKIY V.N.1 GRIMM, Yu.1.
Using Rill current in studying carrier scattering in
semi-
condue'.ors. Fiz.tver,tela 4 no.lOs2760-2769 0 162.
(MIRA 15:12)
1. Ylyevskiy gosudaretven universitet imeni Shevehenko.
(Hall effecTt (Semiconductors)

DOEROVOLISKITP V.N-.
Con,luctivity due to e=vzm cmAmm t carriers in a
magnetic field*
Fit.tver.tela 4 no.10:28OW12 0 16.2. (NUI 15S12)
I. Kiyevskiy Osudarstvenny7 universitet imeni
Shevchenko.
I
isemiconductors--gleotrio properties)
(Mapetio fields)

L h9O2" w(l) lip(c)
7- F~ - a r
method
SOURCE! Pizika tverdogo tela, V- 7, no- 3, 1965, 81.1-818
:M-4S -Isurface scattering, eurface Hnal. er-
feet, surface carrl'~Frdiiisit-y, surface Ran -mob1lity
'is 'vvc-te,! 4o e-n investigat'on of'
rent makes It possible to dete-Tmine the effectiYe Yi&--
surface carrier denaity, and consequently also the r,::- bendIng Of
bands. In addition, the autbzr8 meswired the ffurface and
dete=,ine~-d
C,,d 1/2

erman ilqlift7 45
of irtrbizic 1-z ium witn ro"' -F.
a,,s-ribed by Tu.
to that I
ex-perimentmllY mf--asured
4, 67.
tending
eru-
Ly,
State

r-OBF01MLISM. V.0. VoO.]
A - , .:, , -
Section of hli:,'-~-r-y Cf rath3rlt ' ,, L, a . J
. , (; t " -- . . - I ~ I
Congre.ss on the li;stcjv,~ of unid 0 ;'
(.1. 1 -1
AN URSH no.Pt1650 165. . :1.11. .19 - 11

M
DOBROVOLIMY, V.P. , podpolkovnik mad. aluzhby
Bandage for covering a burn surface. Voen.-med. zhur. no.8:84 Ag
,6o. (MI-RA 14:7)
(BUFM AND SCALDS) (BANDAGES AND BANDAGING) I

DUBROVOLISKIY. V.P.
Interpreting vertical electric curves obtained in
logging
permanently frozen ground.
Hauch.dokl.vye.shko1y-, geol.-
geog.nanld no.2:127-133 '59. (HIR& 12:8)
1. Hoskovokiy universitet, geologicheakiy
fakitl1tet, kafedra
morzlotovedeniya.
(Frozen ground) (Slentric logging)

S/16 62/000/006/009/093
70,0 D228YD304
AUTHORS: knanyan, A. A. and Dobrovollskiy, V. P.
TI~TL1,; Electroconductance of frozen rocks of a natural struc-
ture in the R. Salekhard area
PERIODICAL: Referativnyy zhurnal, Geofizika, no. 6, 1962, 8, ab-
stract 6-A39 (V sb. Merzlotn. issled., no. 1, 'THI. MGU,
1961, 216-226)
TEXT: Laboratory determinations were made for the electroconduc-
L,ance of specimens of frozen rocks of a natural structure and
mois-
ture. Comparison of the data of measurements, okained with the
application of alternating and direct current, shows that they
prac.uically coincide. It is established that ihe
electroconductance
of loose frozen rocks is largely determined by the water's bhase
composition. In the freezing of rocks the electroconduc"6,ance.de-
creases suddenly. It is noted that rocks of a similar genesis are
characterized by approximately identical electroconductivity va-
-lues. /-1,bstracter's note: Complete translation._7
Id
Card 1/1

S/169j62/000/011/004/077
D228/D307
AUTHOR: Dobrovol'skiy. V.P.
TITLE: Electric anisotropy of frozen rocks
PERIODICAL: Referativnyy zhurnal, Geofizika, no. 11, 1962, 13,
abstract 11A62 .(In collection: Merzlotu. issled.,
no. 2, 1.1., MGUI 1961, 157-164)
T=.r: For frozen rocks electric anisotropy may be caused
not only by their structure and texture, but also by their tempera-
ture and by the existence of a temperature gradient. The resisti-
vity of frozen rocks depends on their temperature, iciness and
con.-
position. The resistance of variably composed.layers changes
differ-
ently when the temperature changes. This involves the unique char-
acter of the change irith temperature of the anisotropy factor for
a
rock, formed of lamina of coarsely-dispersed (sands) and
finely-dis-
persed (loams) fractions. The anisotropy factor may increase, de-
crease, or remain constant in different neg#ive-temperature varia-
tion ranges. Maximum.valuqs of the anisotropy factor are noted if
Card 1/2

S/169j62/000/011/004/077
Electric anisotropy of frozen rocks D228/D307
the temperature of frozen rocks is from 0 to -20. Considerable
anisotropy factors are observed in the same way in areas of
ther-mo-
karst development. The second cause of anisotropy in a rock
is the
existence of a temperature gradient in it. The,dependence of
the
rock resistance on the temperature causes anisotropy at the
expense
of the temperature gradient in a rock that even has a
homogeneous
composition and moisture content. Studying anisotropy,
related to
a differing temperature and temperature gradient, and taking
into
account the patterns df its change must greatly increase the
preci-
sion of the quantitative interpretation of vertical electric
sound-
ing, carried out in environments where frozen rocks occur.
f-i~stracter's note: Complete translation 7
Card 2/2

S/109JOl/000/009/006/056
0 D228/D304
AUTHORSs Ananyan, A. A., and Dobrovollskiyt V. P.
TITLE- The electroconductivity of frozen rocks
PERIODICAL: Referativnyy zhurnalo Geofizika, no. 9,* 1961t 91
abstract OA74 (Geologiya i geofizika, no. 3, 1961,
96-103)
TEXT: Certain patterns are described for the variation of
electric
resistances of frozen rocks in relation to the phase
transformations of
water which take place in rocks on the change of the
temperature. Data
are cited on the influence of the structure of a frozen rock
on its
electric properties. The results of the experimental
investigations of
the change of the anisotropy coefficients of frozen layered
rocks in
relation to the temperature and the qualitative explanation
of this
phenomenon are given. fAbstracter's note: Complete
translationj
Card 1/1

DOBRMLISKIYO V. P,
'Using the resistance method in electric pro"ating
for hydraulic
engineering construction in permanent3y frozen
ground. Merzl.
isol. no.1:190-207 361. (MMA 16:1)
(Frozen ground) (Electric rompecting)
(Hydraul.ia struoturea3

ANANUN, A. A.i DOIBROVOLISIVY. V.. Ja-
Specdfic eleotric conduotivitv of frozen ground of natural
struo~ture from the SalekbkLrd region. Merzl. isel.
no.1-1216-226
161e (MMA .16:1)
(Salekhard region--yrosen ground-Electric properties)

DOBRgOVOQLkmiyp V.P.
Eleciril~e-nisotropy of frozen ground. MrsLisal.
no.2sl57-164
161 \\ I (MMA 16: 5)
616klmrd region-Frozen ground"Blectric pmperti~p)
P-1

DOBROVOLISKIY, V.P.
Characteristic "freezing" shape of curves in vertical
elec-
tric sounding. Merz1. issl, no.3z.198-203 163,
Electric prospecting in engineering geologir under
conditions
of the "uniform" distributian of permanevntly frozen
ground
in the region of the Usti Botuobiia water gauge
poirrts.of
the Vilyuy Hydroelectric Power Station. lbid.:204-214
Characteristics of the structure of the geoelectric
di-4 -4 -n
caused by the presence of permanently frozen grotmd;
. oelee-
tko sections of frozen ground. Ibid.:215-230
Principles of the regionalization of tlie area of the
distr5bu-
tion of permanently frozen ground for puqvsp- -*
I-4-f-
prospecting in hydraulic engineering. lbid.:231-235
(MIRA 17:6)

V.
TjSPR / General and 9pecial Zoology.
Insects.
Abs Jour: Ref Zhur-Biol., No 4, 1958, 16424
Author Kuperman F.M.
Inst : Not given
Title :On the Control of Swedish Fly Larvae on Corn.
(0 bor'be s lichinkami shvedskoi mukhi na kukur-
uze.)
Orig Pub: Selektsiya I semenovodstvo, 1957, No 1, 56
Abstract: More than 100 types and hybrids of corn
were in
the sown environs of Moscow at the end of May.
A suspension of 2 liters of [hexachlorancyclo-
hexane] HCCH (0-05 9 of 12% dust and 2.5 9 of
ammonium nitrate per I litre of water) was
introduced Into each group of plants June 13.
(3-4 plants). Although the experimental young
crops were greatly infested with larvae, the
Card 112
20

USSR .1 General and Special Zoology. Insects.
Abs Jour: Ref Zhur-Biol., No 4, 1958, 16424
Abstract: plants became better June 22, the leaves
restor-
ed their normal coloring, the fifth and sixth
leaves developed normally, the sixth and seventh
leaves opened up one to two days sooner, the plants
were stronger than the control plants, while all
the larvae in the plants died.
Card 2/2

:1 )", 1'1~ 70 L' t S';' i y ) V. v1
"Alluvial -,rounds anc~ L'h,3ir
ttilization as
Fountiations l'or 3t,runtur,is."
flor
of ~'an,'. 'A"cohnical Sci. Sub 23
Fay 49, :"~Oscow
Ordar of -Zh-- jabor -ngincering
Con-
struction Tnst imini V. hLivImshev.
3 unwrnar-v b2, 1b D)cc 52,
Dissmrtations
?rcs3nted for Degx,~es in Sciiinea
and z:,ngiTic6ring
in ll~loscow in 194,-. From
-V~~chernyaya Moskva,

DOBROVOL' SKIT, V. V. , inzh,
Selecting pressure of scavenging air for two-stroke
diesel engines
without pressure food. Iner,-omashinostroanie 6
no.4:21-23 Ap 160.
Piesel engines) . (YURA 13:8)

DORROVOLISKIY. V.V.. in&.,
Estimate calculation of the basic indices of
stroke diesel engina. Mergomashinostroenie
(Diesel tmiginee)
a supercbarged four-
7 nooll%21-24 11
(MIRA 14 11)

DOBROVOLISKIY, V.V.
Distribution of dispersed chemical elements between the
soil
forming rocks, soil, and vegetation in the Moscow
region. Nauch.
dokl. vys. shkoly; biol. nauki no.3:193-198 163. (MIRA
l6t9)
1. Rakomandovana kafedroy o*hchey fizicheskoy geografii
Moskovskogo
gosudarstvennogo ~qdagogicheskogo instituta im. Lenina.
Nytishchi District--Trace elements)

DOBROVOLVSKIY, V.V., k&nd. tekhn. nauk
-1 .-
Method of designing a pulp thickener in the
pipeline.
Nauoh. eoob. IGD 181182-186 163. (MMA 16:11)
t

DOBROVOLISKIY vo starshiy nauchnyy sotrudnik,
kand.tekhn.nauk
Experimental studies of new methods and equipment for
hydraulic
filling. Makh. i avtom. v gor. prom. n0.303-61 163.
(MIRA 16tlO)

DOBROVOLISKIY, VjA', prof., dOktor biolog. nauk
Toward com~uxism without crop losses. Zashch.
rast. ot vred.
i bol. 6 mo.10:6 0 161. (MIRA 16:6)
1. Moskovskiy goeudaretvannyy univerBitet.
(Plants, Protection of)

-1 - -
DOBROVOLISKIY, V.V.
Chemistry and geochemistr7 of soil. Khim. v shkole 18 no.4:
.7-14 Jl-Ag 163. (MIRA 17:1)

KRYLOV, V.F.; DQPROVOLISKIY,, V.V., kand. tekhn.
nauk
Coal mining with filling is a progressive method of
working thick steep sea;6e. U901' 38 no.121ll-l~-
163.
(MIRA DO)
1. Glavnyy inzh. kombinata Kusbassugolt (for
Kryluv).
2. Institut gornodo dela. im. A.A. Skochinskogo (for
Dobrovollskiy).

=1TANOV, v.N.; POPOVA. T.N.; KORINA, A.B., kandidat
geographichookikh
nauk, doteent (deasased]; STAROUBOYMU, R.A.;
DDBROVOL'Sxff, V-V.,
doteent, redaktor.
[General physical geography] Ubshchaia fisicheskaia
geograftia.
Moskva, lid-vo geodestchaskoi lit-ry. Pt 1. 1953, 394 p.
(MMA 7:5)
(Physical geography)

a-, G fu! for t. I cp

DOBROVOLISM, V.V. (Voronesh)
Eliminating the damage done br )mrst. Priroda 44
no.4:117 AP 155-,
(Lipetsk Province-Karst)(Reservoirs) (IM 8:4)

KIY_
0 V-0 L S' i
11-1 10 carbonsite zodules in Quaternary 16"m
Uski vsesoyus. Ari..161. 6;:Cmf1
% .-The ci
jbcxmm ft- -AM, '13(19 ) almreotn clays And
great central chernoman (black sell) area of S.
Rutsia. contain typically supergene caxbonate concretions
which do not abow any petrographic relation to the char
acter of the un0erlying rocks or to the them. compn, of the
ground waters. Sedimentary cla3tic qu.
artz; feldspar, and
-andalusite am often Included In the nodules. In their for-
mation all the elements have par"ted that am charaL
teristic for the soils; the microscopic stmeture Is that of
typically colleform materials, with characteristic- deskica-
tian cracka.,,The miueralogical compn. is rnther complex;
tht:e am fine-cryst. carbonate concretions which form the
chief mass.,' Many constituents are adsorbed, especially----
ihose elements which do not bclohg to the structure of the
carbonates but which am assood. In their them. nature the
carbonates hre Chiefly Cam and McCr4; - Fem Is usually
Inatt and there Is mom C&CO~ than MgC%.
very subord.
Extensive analytical and differential-thrrmal data are Ulvcu~
'An-ore-or -An
Wn of.'the th excluded-' the bonate
lei is
'portion of the nodWes and the-FICI-soi. ;~;~ with its
icharacterfstle ratios SiWAIA And A4(),/FeA mft" for
'lot" origin. 71e spectrochem. analysis showed Ti. Zr;
Ora
8r, Ba, V, Cr, Mn; trac" of Cu. V, Be. Ga, *; and Sn, Ph
but Cd, Zn, aN enti/ W. 1_91tel
-77

USSR/Cosmochemistry. geochemistry. Hydrochemistry. D
Abs Jour Ref Zhur Khimiya, No.' 81 1957, 26565.
Author Dobrovollskiy, V.V,
Inst
Title Concretions of Carbonates in Soils and Soil
Forming Rocks-in.:Cefitral Black Earth Region.
Orig Pub Pochvovedeniye, 1956t_No. 59 31 42.
Abstract CaC04 predominates MgC,O-A in the studied con-
cret ons and.the,amo~nt`of the insolubla
residue-increases in the. peripheral zones of
contretions.: Fe produces thin films of hy-
droxides covering fine grains of carbonates.
The chemical composition of concretions corres-
ponds to the composition*of the embedding rocks
somewhat enridhed with A120 and Fe203, Selec-
tive occlusion takes place In the process of
Card 1/2

DOBROVOLISKIY, V. V C d Geol-Min Sai -- (diss) "Mineralogy and
geochemistry
11
of neogenio formations 6 Quaternary deposits of the
ContrRl-Russian forestMEW&W
inol. n~
steppeSwv9&." Mos, 1957. of Geology and Mineral Conse USS
Ast of author's Iwor MV 114 titles)
All-Union Sci Res Inst of Mineral Raw Material VIMS), 125
copi761t(JKL, 45-57, Mrl--1111
Ir
-7-

AUTHOR: Dobrovollskiy, V.V. 5-3-22/37
TITLE: Mineralogy of Quaternary Sediments Hypergenesis (K
mineralogii
gipergeneza chetvertichnykh otlo7heniy)
PERIODICAL: Byulleten' Moskovskogo Obahchestva Ispytateley
Prirody, Otdel
Geologicheskiy, 1957, # 3, p 168 (USSR)
ABSTRACT: The hypergene transformation of surface sediments
proceeds not
only by the change in the outward appearance of a rock but
also
in destruction of some mineral forms and arising of others.
New forms are mostly originated by metasomatosis. The author
reviewed various mineralogical forms occurring among the
hyper-
gene minerals and noticed that mqtacolloid structures
prevail,
which indicates the extensive development of colloid
phenomena
in the process of hypergene mineralization. Insofar as hyper-
gene transformation of surface sediments is controlled to a
considerable degree by general geographical factors, the
minera-
logical composition of the new forms will have its
peculiarities
in every natural zone. This circumstance presents a certain
interest for paleography.
AVAILABLEt Library of Congress
Card 1/1

.MSR/Soil Science - Physical and Chemical Properties of Soil. i
Abs Jour : Ref Zhur Biol., No 19, 1958, 86768
Author : Dobrovollskiy, V.V.
Inst
Title : Disper;~e`Fi=~U`Iil Soil-Forming Rocks of the Central
Russian Forest-Steppe
Orig Pub ; Poelivovedeniye, 1957, No 6, 56-62
Abstract : A study vms made of the content of microelements in a
colloidal diapered fractimi of the soil-forming rocks of
the Central Russian forest-steppe and of neogenes (hard-
pans, lime nodules) separated from these rocks. The de-
termination of microelements vas made spectrally by a
ten-point scale of apectrogram line intensity. Micro-
elements are present in largest quantity in the ferrous,
manganese and carbonate neogenes; in sulfate and phos-
phate neogenes the quantity of microelements is drastically
diminished. The complex of minor elements typical of the
Card 1/2

-USSR/Soil Science - Physical and Cbemical Properties
of Soil.
Abs Jour Ref Zhur Biol., No 19, 1958, 86768
neogenes determined was established.
Bibliography lists 13 titles. -- N.V. Verigina
Card 2/2

DOBROVOLISKIY, V.V.
Phosphates from modern peat deposits in central Russian
forest
steppe areae* Trudy Min. mun, no.8:13h-140 157. (MIRA
110)
(Phosphate)

DOBROVOLISKIY, T.1 ---,
,,
itudFing now gypm formations from surface depoalts In the
steppes
of 3aropeav Russia. Tftdy Min. muz. no.8.-140-145 '57.
(Min llo)
(Gypsum)

DO oee (/0/- ,sx/ / V v". V~
'AUTHORt Dobrb4Wskiyq V,V. 132-12-10/12
TITLE: All-Union Interdepartmental Conference on the Study of the
ibat,drneaT - Period. (Vessoyusnoys moxhduvedometvannoys
soveshcha-
niye po'izucheniyu ohetyertiohnogo perioda)
PERIODICAL: Razvedka i okhrana nedrp 1957oA# 12, p 58-59 (USSR)
ABSTRACT: Initiated by the Ministry of Geology and Conservation
of Natural
Resources (Department of Geologo.,Geographic Sciences of the
Academy of Sciences USSR, Committee for the Study of the "tw'
arnary Period# the Institute of Geology andthe.Inatitute of
Geography of the Academy of Sciences USSR) a conference on the
study of the qLatpraary , Pariod was hold in Moskva in 1957-
200 lectures were held during the'conference which was attended
by 500 scientists from the USSR, the Chinese Peoples' Republic,
the German Democratic Republic, Czechoslovakia, Hungary,
Roumania,
Poland, Bulgaria. The main problems among numerous -othbks*dei1t
with during--the conference weres-
1. Denomination of the 'Qmternary Period and its lower bound-
ary.
2. Stratigraphic subdivision of the q*+,ex%jAry Period.
The conference was opened with lectures of V.I. Gramov, B.P.
Card 113 Grichuk, A.I. Moskvitin, E.V, Khantser and others which
dealt

132-12-10/12
All-Union Interdepartmental Conference on the Study of the
QA&te=ary Period
with point 1, whereby the use of the term "anthropogen" was
favored by the majority of partioipants beside the old term
"Qatar=17 Period". The second point.was discussed in numerous
plenary.and sub-committee sessions, I.I. Krasnoy
(VSEGEI)'olaim-
ed that the present state of atuftes enabled,the issue of an
outline map on deposits of the 'Osternary Period of. the,
scal.e
115,000#000. Speoial obarts of the qmternary layers of the
soales 1000,000 and ls2OOgOOO and larger were developed during
.the-past..years. -Coordination of surveying work was
recommended
as.well as complex prospecting-for the.purpose to discover
specific oharabter4stice of different formations. B.A,
Pedoro-.,
vich and others lectured on Qat6rnary- deposits of north ern
Kazakhatanj which are of great general importance for
geonarpho-
logio mapping. EfE, Milanovskiy lectured on voloanio ashen ,
found.in layers of the Qmternary Period in southern plains of.
the'USSR~ 1rhich are important inasmuch they are connected
with
Pliocene and anthropogen voloanization. of the Caucasus. N.A.
Belyayevskiyo member o 'f the board.of the Ministry of Geology
an4 Conservation of Natural Resources VPSR pointed out gross
Card 2/3 omissions-of.former,workg because basic geologic
questions of

132-12-10/12
All-Union Interdepartmental Conference on the Study of the
Qmternary Period
deposits of the Qaternary Period were viewed by th 'a
oonferenos
from different angles. Great interest was devoted to the study
of different angles.i The lebtures 6f S.S. Morozov and,the
Ace-
demioian I.1, Gerasimov on the subject of-ge,oohemistry of
Quat-
ernary deposits were of special interest for the national
econo-
my. It was decided to hold the next regional conference for
Kazakhstan and Central Asia in 1958, for the Ural and western
Siberia in 1959t and for eastern Siberia and the Far East in
1960. The next All-Union donference on the study of the Qmt-
ernary Period will be hold in 1960.
ASSOCIATIONs VIM$
AVAILABLE: Library of Congress
Card 3/3

USSR/Soil Science - Genesis and GeoGrraphy of SoilB~
J-1
Abs Jour : Ref Zhur - Bioi,,j No 9, 38983
Author : Dobrovolskiy, V.V.
Inst : All-Union Geographical Society.
Title : Relies of the Steppe System in the
Contemporary Zone
of Podzol - Foruation.
Orig Pub : Izv. Vaes. geogr. o-va,, 1957, 89, No 2,
157-159
Abstract : On the basis of a study of soil forming
rocks) the author
arrives to the conclusion that conditions close to
those
fo contemporary forest-steppo and steppe existed on
the
territory of the Ryazm, Tula, Kaluga and Bryansk
oblasts
in the first half of the 14urms. glacial period.
Card 1/1

BAZMOV, Ivan Ivanovich, inzh.; LEONMO, Ivan Abramovich,
inzh.; KHAR-
MEMO, Aleksey Kondratlyevich. kand.tekhn.nauk.
Prinimali uchastiye:
DOBROVOLIBRIT, V.V~jL kand.tekhn.nauk; BORODULIN,
K.Ta., inzh.; POPOV,
&.-A, z KHOLWOV, K., red.izd-ve; PROZORMICATA, V.L..
tekhn.
red.
[Coal mines and mining in the Chinese People's
Republic] UgolInaia
promyeblennost' Kitainkoi Narodnoi Respubliki. Moskva,
Goo.nauchno-
takhu.izd-vo lit-ry po gornomu delu Goagortekhizdat,
1959. 479 P.
(HIRA 13:2)
(China--Coal mines and mining)

3(8) SOY/7-59-2-13/14
AUTHOR: Dobrovollskiy, V. V.
TITLE: Characteristics of the Hypergeneads of Quaternary Sediments
in North Kazakhstan (K kharaktoriatike gipergeneza chet-
vertichn.vkh otlozheniy Sp7z,~rnogo Yazakhatana)
PBRIODICAL: Geokhimiya, 1959P Nr 21 PP 178-190 (USSR)
AiSTRACT: The region investigated extends between the Ishim and
Irtysh
rivers south of the latitude of W town of Petropavlovsk. At the
region's eetftml ducl vestern partAhe Sever o-Ka z akh skaya
hills.
The colloidal-disperse mass was subjected to a differential
thermoanalysis and chemical analysis. The following empirical
formula was found: 3.8 (Si,Ti)O 2-1.3 (AI,Fe )203* 0.4(mg,Ca)O.
.061 (K,Na )20.5.4 H20 . Debye diagrams mere made by G. A.
Sidorenko and the refractive index was determined. The greater
part of microelements is to be found in the colloidal-disperse
mass (Table 5, rig 6). The composition of hypergenous new
formations is dependent upon the type of landscape. In moun-
tainous wood-steppe regions new formations of carbonate pre-
vail, which often contain iron (Figs 1, 2, 3; analyses in
Card 1/2 table 1). In the moderately arid steppe gypsum is to be
found

SOV/7-59-2-13/14
Characteristics of the Hypergenesis of Quaternary Sediments
in North Kazakh-
stan
(Fig 3, analyses in table 3), in the arid steppes the per-
centage of new formations of chloride - sulfate is hi h ro
New formations of iron (Table 4) and manganese (Fig 5 are
rare. The distribution of microelements in new formations
was determined spectrographidally under the supervision of
A. K. Rusanov and by methods devised by him (Table 2). The
investigation showed that microelements are regularly dia-
tributed among the individual kinds of now formations. There
are 6 figures, 7 tables, and 15 references, 13 of which are
Soviet.
ASSOCIATION: Vseaoyuznyy institut minerallnogo syrlya,
Moskva
(All-Union Institute of Mineral Raw Materials, Moscow)
SUBMITTED: March 21, 1958
Card 2/2

3 (5), 3 (8), 17 (4)
AUTHOR: Dobrovollskiyp V. V. SOV/20-126-2-43/64
TITLE: Admixture Elements in Carbonate Concretions From
Quaternary
Deposits of the Arid Zone (Elementy-primesi v karbonatnykh
konkretsiyakh iz chetvertichnykh otlozheniy aridnoy zony)
PERIODICAL: Doklady Akademii nauk SSSRt 1959, Vol 126, Nr 2,
pp 382-384 (USSR)
ABSTRACT: The redistribution of substance in subserial
conditions
differs greatly from the diagenesis processes which under water-
occur above the sediment (Ref 1). The author carried out
comparative mineralogio-petrographic, chemical, and
spectroscopic investigations of 66 samples of the concretion
mentidned in the title, in order to explain the behavior of
small--alementg under subaerial conditions. These oonoretiohe
in the USSR miginate from the earth hypergenesis and are
also distributed over arid zones in many other land3 (Refs 2-8~
The author deliberately collected these samples of concretions
in places f ar away f rom any ore-depos' desert (South
Kazakhstan,
Soviet Central: Asia), steppe black-earth
territory, European'USSR). The analys&., witre made in the
Card 1/3 laboratories of the Mineralogichookiy muzey AN SSSR

Admixture Elements in Carbonate Concretions From
SOV/20-126-2-43/64
quaternary Deposits of the Arid Zone
Mineralogical Museum of the Aca&emy of Sciences, USSR)
alysist N. V. Voronkova), the Voronezh University (by P.V.
M
Yakshova) and the Ministerstvo geologii i okhrany nedr
Ministry for Geology and Protection of Mineral Resources)
M N. S. Valeyev). The results are given in figure 1. By
comparing them with the results of the spectral analyses of'
the quaternary deposits of the area concerned one may see that
not every small element common to bearing rocks (Nb, Hf)
exists
in carbonate concretions (Analogy in Re~ 13). As the applied
spectral analysis method yields no results as to the absolute
content-quantities of the small elements, their relative
contents can only be estimated from the quantity of the ratio
of the elements. By arithmetic means for elements, which
appear constantly or frequently in concretions and in
quaternary sediments, it was ascertained that the ratio is
constant. There is about 2-3.5 times more Sr accumulated in
concretions while, on the othw band, the (xntent of V, C~i,
Pb, Ni,.Co, -and
Ba decreases by a factor of 1.2-2.0 that of Ga by a factor
of 0-5. Cr remains nearly constant. The interrelations of the
Card 2/3 characteristic elements are also different in the
said

Admixture Elements in Carbonate Concretions From
Quaternary Deposits of the Arid Zone
SOV/20-126-2-43/64
conoretions and sediments ~AU9 2), Most of the small
elements occur in carbonate concretions in smaller
quantities than they do in rocks. The results obtained prove
a deviation in the small elements during the transformation,
under subaerial conditions, of the and zone. There are 2
tables and 13 references, 10 ctwhioh are Soviet'.
ASSOCIATION: Vaesoyuznyy institut mineralinogo syr1ya
(All-Union institute
of Mineral Raw Materials)
PRESENTED: February 4, 1959, by N. M. Strakhoy, Academician
SUBMITTED: January 21, 1959
Card 3/3

DOBROVOLISKIY, V.V.
~ ----iieroelements in some soi-Is and soil
'-fcwming rocks of
Kazakhstan. Pochvovedenie no.2:15-23 F 160. (MIRA
15:7)
1. Vaesoyuznyy institut mineralinogo syrtya.
(Kazikhatan-Trace elements)
(Soils-4nalysis)

__POBROVOLO SKIT, Y.T.
Blements occurring as impurities in gypsum
concretions from
middle and upper quaterairy'deposits of thearid
zone.
Gookhimiia n0.7:644-643 160. (HEU 13:11)
. (Kazakhstans-Q"sum) (Concretions)

DOBROVOLISKI'r V V
Hypergenetio mineralogy of Quaternary sediments in the
central
Russian forest steppe* Biul,,MDIP.Otdogeol. 35
no-4-.83-99 A-Ag
1w0 (KEM 14:4)
(Sediments (Geology)) (MWor&logy)

PIOTiOMYj Tladimir Vladialroviaht PODOBXDOt,,. H.S., prof.,
roteentont;
BOGONOL07, L.A., doteent, retsousentA,03113R, SoTu., dottor
goograf.
nauks retsousent; BLAGOVOLTIN, N.S*# IA~6hgq sotrudnik,
Moment;
BOGDANOVA, N,,K, nauohnyy notrudnik, retsonsent; DOSKAM, AGo
naiwhun notrudulk, retsousent; ZHIVAGO, A.V.,. nauchnyy
votrudnik,
reteenzente, RANTSHM, Te.Ya., nauehuyy sotrudnik.
rettenzent-, NIKOLAYST,
R.I., prof., rot sent out I _AWCff9j doteent, rateensentl
VOSMSINSKM B.S., red,; SHAMAROVA, T,~,, red,lad-va; PESTS,
B*Na,,,
takhn.red.
(Geomorphology and fundamentaU of geology] Goomorfqloglia a
oonovami
goologit, Riga, lzd-vo goodes,lit-ry, 1961, 283 p,
(MIRA 14'1?- If or Ullor).
1.1kahal'alk.otdola, geomorfologil Instituta geografli AT
SSSR
2 Mel omorfologii Instituta eografti AT SW (for Blagovolin,
Bogda-
u;va, Dosech, Zhivago, Rautoman)!
(Geomorphology) (Geology)

DOBROVOLISKIY, V.V.
Carbonate concretions in relict meadow soils in the
frouthern part
of the forest zone. Nauch. dokl. vys. shkoly; biol.
nauki no.3:
180-184 161. (14IRA 14:7)
1. Rekomendovans. kafedroy obahchey fizicheskoy
geografii Moskovskogo
gosudarstvemogo pedagogicheskogo institute. im.
V.I.Lenina.
(TARUSA REGION-CONCRETIONS) (C=ITE)

DOEROVOLISKIY, V.V.
The geomorphological control of the geochemistry of
the supergene
formations using the axample of Kazakhstan
pensplain. Izv. Ali
SSSR. Ser. geog. no.6:18-26 N-D 161&~ (MIRA 3.1+:12)
1. Moskavakiy gosudaratvennyy pedagogicheskiy
institut im.
V.1. Lenina.
(Kazakhstan-Rarth surface)
(Kazakhotan-Geochomistry)

DOBROVOLISK-IY, V.V.
New typomorphic formations in Quaternary
sediments in the
desert zonet of the U, S. S-,~ R. Pochvovedenie
no.10:44-58
o 161. 1 (MIRA 14:9)
1. Moskovskiy gosudarstvennyy pedagogicheskiy
institut imeni
V.I. Lenina.
(Geology, Stratigraphic)