SCIENTIFIC ABSTRACT TARDY, V. - TAREYEV, B.M.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001755010006-6
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 26, 2002
• Sequence Number: 6
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

TARDY, V
chiat. 58 no.2:
On the 60th birtbdaY of Dr. Jan Dolezal. Cesk. psy
130-133 AP 162.
(BIOGRAPHIES)

PETROV, G.N.; ROZWM ID, V.Ta.; KAGANOV, I.L.; PETROV, I'I.;
STAROSKOLISKIT, W*A.! TARB B. M.
Vasilii Aleksandrovich IsNiurov. Ilelctriebeetvo no 7:93 JI
,6o. (Wiurov, Vasilii Aleksandrovieh, 1885-) iMIRA 13:8)

TARS, R.
I
'V4'. , ., . I on$. Gov.profootusir 5 no-1:
' for technological progr (WA IWO
46-50 J& '57.
1. Predsedatel' komiteta profOOYuz& rsdi0s&yOd& im6ni POPIYT&.
(Udio industry) (Trade unions)

A n-i~ it! ; ;
11
Adjustment of continental triangulation nets. In German.
P. 429 (Acts, Technica) ;---iid&pest, Fungary Vol. 16, no 3/4 1957
SO: 'Monthly Index of Est European Acessions (AZEI) Vol. 6, No. 11 November 1957

T Or
4-53
TARZE A A. I.
TcQdcolw
Remchlorcyclchelmme
Feb
'"Approminate Data on Investiestions of the Toxic
F6atures of TeabnIcal Mixture of Rezoichlorcylobommw
160mrsi, A. I. T&reeva,, 2 pp
Farmkol I Takalkol" Vol X, No 2
Experimental data leading to the conclusion that
dosee of 200 and 500 mMIgmm do not cauno any
changes in the bumn akin,
4"3

M, ~ H~p F, K-oaz
IM -sr T, --I*,- -1."I
'R
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. fie'lk
I al., - mal 7 .11,11
-- . ; , v-- Ij5, - -
ML
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ma - !E,. i- 'I" ma of, - lm~ OEM

TARELKIN, Konstantin Danilovich; SINEVNIKOVA, TS.B., red.; TSESffiiyBi,
-L-. IF. -
[Fur goods] pushno-mekhovye tovarY. Moskva, lzd-vo "Ekono-
mika," 1964. 195 P. (MM 17:6) 1

Yu.A#, inzh.; DOBROKHOTOV, V.I., in7h.; KISFLIGOF, M.L., kand.
BOYKOY ; pATyCHEN,, zh,; POGORELOV, B.F., in:zh.;
tekhn. nauk ,0, v.S., in
T~~N~.. , inzh.
Burning of lignite with a high moisture contents Elek- eta. 36
no.2:8-12 F 165. (MIRA 18:4)

RODZUrVICH, N.V., Inzh. (Kolonn&)LIALM~LKIN Yu.Vp inzh. (Kolama)
Coating with caprone of
Elek, i tepl. tiaga 6
the axle box supports of
no.lls1O N 062.-
(Diesel locomotives)
diesel locomotives,
OaRA 16ti)
.U.,

PUTILIN, V.N.9 inzh.; RODZEVICH, N.V., Inzh.; TAP.7LKIN, Yu.V., inzh.
Use of capron for the axle end thruBt bearings and bushings
of the spring suspension for locomotives. Trudy VNITI
no.19:214-223 164. (MIRA 18:3)

TMILov, A,S., inshener*
- - tomatio feed check Talves. Alsk.stao 28 no-1:77-79 Ja '57.
(KLRA 10:3)
(Boilers--saf0ty appliances)

5891 TIM IM.0, It. 1. 1.!,'etbdlka- i tekhnik-- opredeleniya kollchegtva pyll 7
vozdukhe. (metod. pialmo). tbilisi, gruza-eclCiz, 1954. ?Jss. s ill.
l6sm (nauch.- issled. irt-t glgiyeny truda I profzabolevanly im. n. i.
makhviladze m-v-n zdravookhraneniya er=. ssr), 2.000ela. beepl. -a vy.
u1mzan v kontse telmta.-na gruz. yaz.-
(55-JM) 614-71-074
SO: KnIzhmya Latopist, vol. 1,1955

I
. rm- mmmm-pml
1,

--. , - - assomm;
u. Imbn ,
om-t"mouff-i'mas
m

KA.OHABELI, M.Ye.. kand.madeneuk; 2ARMO, M.I., nauchnyy sotrudnik;
GNKBASHIDZE, G.K., klinich;;'s-L-TJv-*~-,4rnator
Sanitary and hygienic conditions of workers employed in spraying
citrus trees with octamethyl and mercaptophos. 01g. i son. 22 ho-7:
84-85 Jl '57. (MIRA 10:10)
1. Iz Institute gigiyany truda i professionallnykh zabolevaniy
Ministerstva sdravookhraneniya Gruzinskoy SSR.
(INSICTICIDIS, injurious effects,
phosphates, insprayIng citrus trees (Rua))
(PHOSPHATBS, injurious effects,
insecticides. inspreFing citrus trees (Rua))

GCGUADWp V.0 doktor khim.nauk, zasluzhannyy izobrotatell Gruzinskoy SO;
, TARENKOt M4. nauchnyy ootrudnik
Lighting without burning. Izobr. i rate. no.lOsl2-13 163.
(MIRA 17:2)
1. Institut prikladnoy khimii i alektrokhimii AN Gruzinskoy SSR'(for
Taranko).

SHVANGIRADZE; M.Di:;-TSKHfiDADZEq K.A.; TARENKOp M.I.,- GOGUADZEI V.P.
Increase of the sensitiveness of nitrogen detection by the
Lassaigne method. Zhur. anal. khim. 18 no.3.1:1399-1400 11 163.
(MIRA 17:1)
1. Institut prikladnoy khimii i elektrokhimii AN GruzSSR, Tbilisi.

%1.
~A~.
r GOGUADZE, V.P.; TARENKO,
Color reaction for thiocyanate alkyls and the synthesis of new
fluorescent dyes. Soob. AN Gruz. SSR 36 no.1:69-76 0 164.
(MIRA 18:3)
1, Institut prikladnoy khimii i elektrokhimii AN Gruzinskoy SSR.
Submitted March 6, 1964.

.66 EINA(h)/EWT(l)
M%.-- rim M'jVVVQP44 monograpa vat
Teenenko Zua Ilfinichna (Candidate of Technical. Sciences);
Troknimenko, YAroaldv Karpovich (Candidate of Technical Sciences)
1,.DelaX oystem$9~(Zamedlyayushchlye sistemy) Kiev, Izd-vo "Tekhnika"t
1965, 306 p, illus.,, biblio'. 6000 copies printed,
TOPIC TAGSt delay circuit# traveling wave., cavity resonator
PURPOSE AND COVERAUt This book is intended for the teohnical
personnel of industrial enterprises and design officeas and may
also be used by aspirants and students'in advanced courses of radio
engineering and radio electronic divisions of schools of higher
education, It describes the properties of delay systems in shf
-o ca--hode-ray tubes, using the extensive interaction of tho electron
beam with the traveling-wave field. General problems pertaining to
traveling-wave propagation in delayi-systems are described. The
electrodynamic characteristics of helical, pinj comb, and 1W11ped-
parameter delay systems and of cavity resonator circuits, as well aa
those of some special types of delay systems, are discussed.
Methods for theorical and experimental investigation of delay system
--'__-1-~d-meamw_ement of their basic parameters are presented,
21t372-
Card I/
uDo 6ei,,385.6:6

L 25799-66
ACC NRI AM6008542
OF CONTENTS.
:..-Foreword 5
Wave propagation in delay.systems 7
1. Conditions for delayed wave propagation 9
2. Basic theorems concerning fields in periodic structures 13
3, Dispersion charactei?isties -- 16
4. Field propagation in delay systems -- 23
5, Coupling impedance. Field propagation parameter .- 2T
6. Effect of delay system characteristics on traveling-wave and,
backward-wave tube operation -- 32
7, Delay system in charged-particle linear accelerators 36
2. Helical structure delay systems -39
--l.-Helically conductive cylinder -- 39
2, Tape helixes 45----
3. Coupling impedance -- 51
4, Multiconductor and modified helixes 56
Helix in dielectric and ferromagnetic media 60
Attenuation -- 63
-73o-Rod-delaysystems 67
Card 2/f_

L.2~799-66
ACC NR# M16008542
1 #Theory of multiconductor lines -- 69
2, Calculation of characteristic impedances -- 74
3, Pin comb -- 77
4* Ladder systems -- 79
86
Opposing pins made of large rods
Opposing pins as a multiconductor line 90
Y, Flat helix -- 98
U, Practical modifications of rod systems 100
440 Rib structure delay systems -- 109
1, Wave propagation above a comb structure 110
2. Complex comb systems -- 116
3. Axial symmetry rib structures -- 121
4. Opposing plates in a rectangular wavegulde 131
Lumped-parameter delay systems 138
I* Dispersion equations -- 139
2, Characteristic and coupling lmpedance~:-- 145
3. Ladder circuit delay lines -- 152
4, Iterated networks of coupled circuits 16i 175
.5* Iterated networks of bundle six-poles circuits

L 25799-66
AICC NRi A1460013542
6, Iterated networks of coupled resonators 184
1, Properties of coupled resonator circuits -- 186
2. Iterated networks of capacitive-coupled resonator circuits 195
3, Dispersion equations of inductive-coupled resonator circuits -200
4- Positive mutual-inductance resonator circuits 208
5, Negative mutual-inductance resonator circuits 220
6. Multistage septate waveguides -- 227
7, On the method of equivalent circuits -- 232
Special types of delAy.systems -- 236
1. Delay aystems with contactless components. -- 236
Delay systems with gradually changing parameters 1243
3, Dielectric delay systems* -- 248
4, Delay systems of traveling-wave cathode-ray tubes 253
5, Ring delay systems -- 255
8, Measure'ment of delay-system parameters -- 262
1, Methods of experimental investigation of delay systeas 262
2, Measurement of dispersion characteristics -- 264
3. Measurement of coupling Impedance 275
4, Measurement of cold loss -
5, Matching of delay systems L282h
Bibliography - 291
List of pritwi al ____ )1 16
Card OURM-DIT
Im
_4A,&ZUB WEs 5
22!i~51 (RIG Ws 165/ OTH W, 122

H..
TARENKOV, Ye.
6~
Tr,tp-rnrj,--';ional t(ri,--is= and tha of pa-~.~5--:-Zar -.eSs-alls.
Mor. ktfct 25 iio.8:40-41 A-c, 165. (MMA 18:8)
1. Kapi~,an teplokhoda "Fellks
..7'. a
IT I W I
III I ~ Eli I blMj I NVA um

AIL_(w NKI AT6022699 SOURCE CODE:' UR/0000/66/000/000/0334/0343 S/
AUTHOR: Thresenico V. P. 20
5 =Q--- 9,A/
ORG: none
TITLE:' Automatic ogtimization of several plants
SOURCE: Moscow. 'Anstitut avtomatilti I tolemekhaniki. Samoobuchayushchlyesya
avtomaticheskiye sistemy (Self-instructing automatic systems). Moscow, lzd-vo
Nauka, 1966, 334-343
TOPIC TAGS: optimal automatic control, queueing theory, approximate solution
ABSTRAM The aim of this paper is to determine probability distribution of states
of a system of n plants and m optimizers (M4n),,the aver-ige longth of a queue In a
servicing system under settled operating conditions, and 'the optimum number of opti-
mizers. The case considered Is one where the probability that an optimizer*-.rill find
an extremum in no more than k steps
j!'p (k) (I - P),p I - (I pyl
and distribution density of arriving'calfilimc6ming from eaiiii -plifi-Efor servicing
is
14 W U >0)1 (2)
CoDS
-Alb

4c

tU-3VX-n-IA% I LW.T; L4CUJNXI M~l IY- --' ---- ...... ~w ~~W--:~~
- . - I . - - .- I

BORTISHKO, 1,11o, ind BOKHOVMK, H-Ho, inzh.; FIDILIMAN- G,S,, Inzh.;
POZIN, Me, dnktor tekhn. nauk; TARAT, Moya., kAnd.tekhn, nauk.
Foam dust collectors used at thn &6i*ihtftftft1jA"t of the
"4patite"'Combine. Bbzop. truda, v prom. 2 no.2:9-11 7 158.
(KIRA 110)
1. rombinat "Apatit"' (for Borushko, Bokhovchuk, Pidellman). T. Ie-'
ningradskly tokhnologichfiekly institut im. lonsoveta (for Pozin,
Tarat)..
(Dast collectors)

USW/Medicine - Infectious Hepatitis Dec 53
"The Clinical Aspects, Prophylaxis, and Treatment
of Botkin's Disease in Hot Climates," Prof"E. M.
Tareyev, Active Mem, Acad of Xed Sci USSR, Moscow
Klin Med, Vol 31, No 12, PP 3-11
En=erates some of the achievements attained by
LTAR ~science in research on infectious hepatitis.
States that manifestations of this disease, In a
hot climate, may involve special types of liver
morbidity. Discusses transmission of the disease
by Inoculation. Advocates a wider use of anti-
qddemL- measures, and the use of specific
274T26
propbylaxis for this disease. Names as outstand-
Ing problems, the detn of the origin of Botkin's
disease and development of specific methods for its
treatment.

VAJIGUSICAU, Mi. Ya.; LyMBTMIY, Kh. Z.; T42y~.,G.A. __
hosphate insecticides. Gig. i
Working conditions in testing new p (141iiA 12:7)
..n. 24 no.5:12-17 My '59-
1. Is ljzbekskogo MuchnO-ilisledavatellskogo flanits'"090 'natituts"
(plJOSPHONS, POis. .in IndUBt. (RUBD
insecticides, pre.

TARVLPV. YE
Vnutrennis Bolezni (Internal Diseftses)
950 p. 6-00
SO: Your Coutin*nt Book Ljjgt, April 1954

PAVLOV# AqN.# otv, za vypusk; VOWDICHEVA, Y.N.; IVAMOVA, A.I.; KULAKOV,
I.N.; LYAKIMA, T.N.; KITOXINA, L.I.; P02MUTAXOTA. M.P.; RODI(NOTA.
L.I.; RCWHOVA, N.M.; SOPI17T, M.S.; CHICHKINA, A.A.; TRISCHMOYAO
Z.G.: BOGATYREV, P.P.; BROVKINA. A.1.; IVANOVA, L.D.; IVASMN,
G.A.; KAHNN, N.I.; LTSANOVA, L.A.; OZHBMITZVA, Z.I.; PAVLOVA.
T.I.; TTUTYUNOVA. V.1.; UNNITSINA, A.P.; ZHIVILIN, N.M.; AIJASHIGM,
M.P.; VINOGRABOV, V.I.; TZRIMIN, F.S.; KRAVCHENKO, Te.P.; LOVAGMA,
K.V.; MIKCLISKATA, V.S.; KAUOV, G.I.; MEGINA, A.V.; TA44M A V.-
KHCLINA, A.V.; BRYANSKIT, A.M.; BtMMISTROVA, V.D.; MIGORIMA. A.M.;
LUTSINKO, A.I.; CREOWA, Z.V.; TXPLINSATA, N.V.; FICCKTISTOVA, V.I.;
BUTORIN, I.M.; BOCHEARIVA, L.D.; BITMINA, V.A.; VETUSHICO. A.M.;
VIMTAM, A.A.; SORCKIN, B.S.: TbIDMO, L.T.; NIKOV, V.N.;
DUNNOV, D.I.; STEPANOVA, V.A.; KANYAKIN, V.I., red.; VAXHATOV. A.M.;
MAXAROTA, O.K., red.izd-va; PTATAKOVA, N.D.. takhn.red.
(Soviet agrimilture; a statistical mammll Sellekoe khosiaietvo
SM; statistichaskii sbornik. Moskva, 1960. 663 p. (KIRA 13:5)
I.-Russia (1923- U.S.S.R.) TSentrallnoye atatiaticheakoys uprav-
Ieniye. 2. Upravlenlye otatistiki sel'okogo khozyaystva Mntrall-
nogo statisticheskogo upravleniya SM (for all except Makarova,
Pyatakove). (Agriculture--Statistics)

TAUYEV, B,Aq r of
- long of the abOO111te current method to the stud
Some applicAt v.AIi SSSR Ser-960fisq no,71
level variations of 8, shallov s6a- 12 (KIRA 9:9)
813-82o il 156.
J.AkademiYa ua~k SSSR, Institut okeanolOglie
(ocean currents)

TAREYEVI B. A. Cand Phys-Math Sci -- (diss) "Certain Problems of
the Theory of Wind-Caused Fluctuations of the Level of Shallow-
Water Sea." MOB, 1957, !9 8 pp 20 cm. (Marihe Hydrophysical Inst,
Academy of Sciences USSR), 110 copies (KL, 27-57, 104)
- 9 -

49-58-5-4/'--
AUTHOR: Tareyev, B. A.
TITLE: Drift Curreits--i'-ff a Shallow Sea under the Inflaence of a
Wind Varying with Time (Dreyfovyye techeniya v melkovodnom
more pod deystviyem peremennogo vo vremeni vetra)
PERIODICAL: Iavestiya Akademii Nauk SSSR, Seriya Geofizicheskaya,
1958, Nr 5, PP 605-612 (USSR)
ABSTRACT: The importance of this problem arises in the following way.
In wide, but shallow reservoirs, e.g. Northern Caspian or
Azov Seas a period of time of the order of the natural oscilr-
-1-lations in the basin is required if a horizontal pressure
gradient and current gradient is to be built up. In the
case of an irregular, rapidly changing wind of the type often
found in practicelthe surface inclination will be small and,
hence, the gradi6nt component of the resulting current will
also be small compared with the drift component. This is
even more the case for local winds, e.g. in the region of the
Mangyshlak~--I_ peninsula;~t. Thus, in many instances, the current
which arises can be considered as purely due to dAft, This
is useful in ptactical cases, e.g. navigation,, where, other-
wise. a calculation must be based on t4e average wind field,
whiA may change. The development of drift currents in an
Card 1/9 infinitely deep homogeneous sea in the presence of Coriolis

11.9-58-5-4/15
Drift Currents in a Shallow Sea under the Influence of a Wind
Varying with Time.
forces and under the influence of a constant wind which
arises suddenly was first solved by Fredgollm (Ref.1). P.A.
Kitkin generalized this solution for a sea of finite depths
A further generalization to a non-stationary wind field would
lead to difficulties and, as V,, B. Shtokman and V. A- Tsikunov
(Ref.3) have shown, would not be of great interest, In deep
seas, the current is distinguished by its relative stability
and, hence, reacts less to a rapid change in wind field than
the current in a shallow sea. In a shallow sea, Coriolis
forces can be neglected in comparison with othe.~ forces; The
author considers an infinite sea of depth h over which, from
the time t = 0 , a spatially homogeneous wind blows. The
wind can change arbitrarily in magnitude and direction. Co-
ordinates are taken with x and y in the sea's surface and
z vertically downwards. Since the continuity condition
holds, only one horizontal direction (x) is considered.
Eq.(l) gives the equation of motion and Eq,,(2) the boundary
conditions.
IOU (Z)
7 4Z dluz
Card 2/9

49-58-5-4/15
Drift Currents in a Shallow Sea under the Influence of a Wind
Varying with Time.
Ou . T(t) at z -.0; u = 0 at z =--h; u --(z,o) - U (z) (2)
Tz' TO 0
u is the velocity component along the x-axis,-)(z) is the
kinematic coefficient of turbulent viscosity which, generally
steaking, depends on z I P is the constant density;
T Q is the tangential stress of the wind along the axis (a
given function of time which depends only on certain, very
general, conditions). Consider first the simplest case with
periodic boundary conditions which gives a closed solution,
V is taken to be constant and Eqs.(l) and (2) written in the
form Eqs.(3) and (4), where q(z.t) is a complex function,
the real part of which equals u(Z,t) . Substituting
tf(zlt) a e-iwtZ(z) , a differential equation is obtained
which is integrated in accordance with the boundary conditions
to give: TKZ~t) - e-iWt To sin y(h-z)
;W C 0 B YE,
Separating the real and imaginary parts of this expression,
Eq.(6) is obtained. In the case of an arbitrarily time-
Card 3/9 varying tangential stress, an elementary solution can be

49-58-5-4/15
Drift Currents in a Shallow Sea under the Influence of a Wind
Varying with Time.
obtained from Eq.(3). Flel'stad (Ref.4) and Khidaka (Ref.5)
have zhown that the result is Eq.(8). which changes into
Eq.(9) for T = const. A numerical example for a periodically
varying wind is given. The period of tangential stress
change -, - 2V x 104se--^J17.5 hourB. coefficient of turbulent
kinematic viscosity, -0 =50 cm 2/see. Taking the unit of
length to be 1 m and unit of time 10 4sec; 50, w = 1, and
a o.1 m7 Fig.1 shows the results obtained for the
velocity distribution with depth at different timeo. As can
be seen from Fig.l., in the layer from z -:0,46 h to the
bottom a counter-current is observed periodically, Observa-
tion of suitable velocity distributions in natural conditions
might lead to incorrect conclusions concerning the gradient
of these 'counter-currents, if the non-stationary wind field
is not considered. Eqs,(6) and (7) permit the calculation of
the stress at the bottom, Fig.2 shows the variation with
time of the tangential. wind stress at the surface and the
Card 4/9

49-58-5-4/15
Drift Currents in a Shallow Sea under the Influence of a Wind
Varying with Time.
tangential stress at the bottom, whilst Eq.(11) gives the
result based on the figures introduced above. Fig.2 and
Eq.(11) indicate that the greatest possible value of the
ratio Tbottom/Tsurface = 0,77 . However, Francls' (Ref.6)
experiments show -that this ratio does not exceed 0.03 in
practice. It is obviously necessary to take into account the
variation of 1) with depth. This is done by employing
Eq.(12) which gives a linear variation with depth to a small
distance from the bottom, characterized by the empirical para-
meter e . It can be considered that e is proportional to
the thickness o; the laminar layer - Flel'stad tAinks that
zlh^alO-'-- - 10--~' (Ref.7). Choice of this parameter becomes
more objective if it is assumed that the coefficient of tur-
bulent velocity near the bottom is equal to the coefficient
of normal molecular viscosity. In Eq.(12) ~o is the co-
efficient of turbulent viscosity at the surface. Hidaka
(Ref.8) considered the case of 'd varying with depth (with
e = 0) . The author now considers the case with non-
vanishing viscosity at the bottom. Eq.(l) is rewritten in
Card 5/9-the form Eq.(13) and the boundary conditions, Eq.(2) are

49-58-5-4/15
Drift Currents in a Shallow Sea under the Influence of a Wind
Varying with Time.
used with, u (z) -a 0 A solution of the form Eq.(14) is
looked for wTth the boundary and initial conditions Eq.(15)
and (16). This sives Eq.(17) in-to which the substitution
U = G(QF(z) is made. Changing the independent variable z
a differential equation for R is obtained wJth the bound-
ary conditions (Eq.20). The integral of this can be written
in the form Eq.(21), where Jo I N . correspond to the Bessel,
and Neumann functions of zero order and Yn is the root of
the transcendental equation (Eq.22). A general solution of
Eq.(17) by series is now sought, with change to a new
variable y . Employing formula (19) and the expression for
the Wronshian cvlindrical function of zero order, the co-
efficients C' and 0" in Eqs.(24) and (25) are defined,
n n
The boundary conditions (Eq.20) and an integral formula for
Z (any solution of Bessell~ equation ef zero order) are
n8w used to determine JjRnjj . Eq~(27) is now obtained
from Eqs.(23), (17), (18), (24) and (25), and is integrated.
Card 6/9

49-58-5-4/15
Drift Currents in a Shallow Sea under the Influence of a Wind
Varying with Time.
The final solution is found in the form of Eq.(29): all the
calculations can be carried out with the variable y , and
the change to z left until the final stage. If V 0 is
put equal to zero, as was done by Hidaka the solution is
made much simpler since the Neumann function disappears.
The solution can also be used for a viscosity coefficient
varying with time as in Eq.(30) - this gives Eq.(31). If
we assume the coefficient to be constant with time this
implies that turbulence is fully developed throughout all
the region. However, in a shallow sea, a non-stationary
wind, produces a turbulent viscosity varying with time.
Unfortunately, the time dependence cannot be determined
owing to the absence of data. In the case of a suddenly
arising wind which thergafter remains constant, it is natural
to use: f(t) = (1 _ e 0-5) in Eq.(30, where w(.>O) is a
parameter, characterizing, to a first approximation, the
development of turbulence in a sea under the influence of a
wind. Using this f(t) the exponential factor m (Eq.9),
characterizing the change of current velocity with time has
the form:
Card 7/9

49-58-5-4/15
Drift Currents in a Shallow Sea under the Influence of a Wind
Varying with Time. 2
2n + 1 W) ~t - -L (1 - e-wt
exp (- 1) ( 2 h - W I)]
for sufficiently large t t is approximates to:
I
exp 2n + 1 12 t
V--2h-- W
A~ ( 71)]
In other words, with a 10 increasing exponentially from
zero to a fixed value. a certain fixed velocity will be ob-
se-~ved at the moment 't1 + 1 whereas with constant
7
this value will be observed at 'ti In view of the
function used, the velocity at the start will increase
very rapidly with time? which seems to be confirmed by
Card 8/9

49-58-5-4/15
Drift Currents in a Shallow Sea under the Influence of a Wind
Varying with Time.
observations in the North Caspian. A more detailed estimate
cannot be made without more information on the function f(t)
There are 2 figures and 8 references, of which 3 are Soviet,
3 German and 2 English.
ASSOCTATION: Akademiya nauk SSSR, Institut okeanologii. (Academy of
Sciences, USSR, Institute of Oceanography)
SUBMITTED: February 212 1957.
1. Ocean currents--f4eteorological factors
Card 9/9

.#UTHOR: TareyevB..A. SOV/49-58-9-12/14
TITLE: Stationary Circulation due to Wind in a Square Basin of
Small Depth (Statsionarnyy vetrovoy nagon i tsirkulyat3jyp-
v Pryamougollnom basseyne maloy glubiny)
PERIODICAL: Izvestiya Akademii Vauk S,93R, Seriya Geofizicheskaya,
19581 Nr 91 pp 1139 - 111:4 (USSR)
ABSTRACT: It is shown in Ref 1 that if horizontal viscosity and non-
linear terms are ignored, the question of stationary wind
circulation in a shallow sea depends on the solution of the
equation:
(13 1 T
- curl
h
)x 7 ~) i)y h ay 2ji Z h
Z
where h(x, y) is the depth of the sea, T(x, y) is the
tangential stress of the wind on the surface, A is the
coefficient of vertical turbulent viscosity and ~ is
defined by the Eqs.(2). Eq.(I) has the boundary condition
Card 1/7 (3) on the contour r of the sea, i.e. the component of

SOV/49-58-9-12/14
Statibnary Circulation due to Wind in a Square Basin of Small
bepth
the total current norma.1 to the shore line equals zero.
Having solved Eq.(I) with this boundary condition, the
inclination and velocity components can be found from
Eqs.(4) and (5)-
Obviously, Eq.(l) has no significance for in
particular, the inclination of the level increases without
bound. This singularity is due to the fact that near
h -m#O , the perturbation of the level t , cannot be
considered small compared with h . in numerical integration,
this can, of cou-?,se, be avoided by assuming the coastline
to be a vertical step.
The present article considers a constant depth basin. For
small depths the Coriolis forces can be igriored. and,
hence, Eq.(13 reduces te:
h2
curiz T (6)
21L
One method of solving the equation has been given by
Leibenson (Ref 2), who assumed that the coefficients of
Card2/7 vertical and horizontal turbulent exchange were of the

*IEWA~-
SOV/49-58-9-12/14
Stationary Circulation due to Wind in a Square Basin of Small
Depth
same order.
The author assumes the X(x) Y(y) and separates the
variables. For a basin of width and length 2L , the
boundary conditions become
+ = 0 when x = 0, and y - + L
It is assumed first that the wind blows along the y-axis
and changes only along the x-axis Then:
TX = 0; curl z T % dTY(x)
dx
Assuming X proportional to sin Xn~ , gives Eq.(9).
Yn is then found from Eqs.(9) and (10) and, hence, the
general solution of (6), satisfying the conditions (8), has
the form (12). If the length 6f the basin along the
z-axis is very great (i.e. a canal), Eq.kl2) simplifies to
give (15) for the inclination of the level. Thus, the free
Card3/? surface has the form of a plane (an analogous result was

SOV/49-58-9-1 14
Stationary Circulation due to Wind in a Square Basin of Small
Depth
obtained by A.I. Felzenbaum (Ref 1)
The author next considers the general case (L 1-:'~c, The
centre of co-ordinates is now moved to the centre of the
basin (Figure 1) so that the boundary conditions become
Eq.~16). It can be seen from jsq.k7) that the solution will
depend on cos anx (where:
a. ly 2n + 1 for n = Oplp2.*.
2 * z
curl.2 is denoted by f(x~ y) and an equation, analogous
to (9), is obtained for YnW Integration of this gives
Eq.(18) for ~ :. It is next assumed that the circulation
can be expressed in the form:
TX -.4 aly + b, Ty = a2x + b2 (19)
so that: h2
Card4/7 21-L curlz T = const.

SOV/49-58-9-12/14
6-t6tionary Circulation due to vVind in a Square Basin of Small
Depth
This gives Eq.(20) for which can be rewritten in the
form (20a). It can be seen from Zqa. (6) and (16) that
horizontal circulation is absent, not onlj for a constant
wind but also when the field of the tangential wind stress
is variable but is a scalar potential.
The author next considers the case when T. = 0,
TY = ax + b (wind along the y-axis, the change in
tangential stress characterised by a). This can be
reduced, using Fqs.(20a) and (4), to an approximate
expressionr-*~aZ/O-w the inclination in a direction trans-
verse to the wind. This can be simplified further near
L if L > 2 since
ch nj1
~2
n
Ch _~l )jr L
Card5/? . [(!2

SOV/49-58-9-12/14
Stationary Circulation due to Wind in a Square Basin of Small
hbpth
It follows from the expressions for ~1~ /ax and 4) ~/r) 7
that, for 7 = 0 $ Sx = 0 and) for x = 01 Sy = 0 . The
difference is that, in the first case, both the total
current and the x component = 0 .
Figure 1 shcws diagramatically the general character of
the eiraulation corresponding to Eq.(20) for a2 = a
al = 0 . It can be seen that for a> 0, a cyclonic
circulation is obtained and with a < 0 an anticyclonic.
Circulation in an actual basin is, of course, more compli-
Cated than that described owing to the neglect of horizontal
turbulent viscosity in the above calculations. However,
the inclusion of this factor in the equations would lead to
excessive difficulty in solution.
Card 6/7

SOV/49-58-9-1.2/14
Stationary Circulation due to Wind in a Square Basin of Small
-Depth
There are 1 figure and 2 Soviet references.
ASSOCIATION: Akademiya nauk SSSR,Institut okeanologii
(Ac.Sc. USSR,Institute of Oceanology)
SUBMITTED: October 3, 195?
Card 7/7
0

ILA.
tu To-,O
Obn
co
wn

FED(MOV, y 0GOltov, V. G.
TARSM) B. A. I . M. and B
cwm and the Problem Of Waste Disposal Tbarain."
'The I)eptba of the 0
e,ientific Conference on the DiSPOOI Of
report Presented at the S) 16-21 November 1959-
Radioactive Waste',IMonac(i

3(9)-
AUTHOR: Tareyev, Be A.
SOY/20-127-5-19/58
TITLE: On Free-Convection in Deep-water Cayitiso of the Oceans
PERIODICAL: Dokla Akademii nauk SSSR2.1959, Vol 127, Nr 5, pp 1005-1008
(USSR~
ABSTRACT: In cooperation with the problem of.the sinking of radioactive
waste products of-the.atomic industry into the oceans., the
author investigates the posoibIlity of water circulation in
great depths. It follows from observations that a noticeable
superadiabatic temperature inorease oocurs with inareasing
depth.-This phenomenon in expliLined by geothermal heat suppliee.
Therefore, the entire depth muit be divIded into two layers
which are separated by that surfacav on which the gradient of
the potential temperature passes through zero. The lower layeri
in which the potential temperature increases W'Ath depths is
described as.convecti:ve layer by the author. Rayleigh (Ref 2)
already pointed oui that at..a certain value of the dimensionles3
parameter (Rayleigh number a) convection current's may occur In
a horizontal layer of water, which is heated from below. Aq
in the present case the rotation of the earth must be taken
Card 1/2 into account, the system of equations is written down for -the

SOV/20-127-5-19/58
On Free Convection in Deep-water Cavities of the Oceans
Coriolis forcea, and.the boundary conditions for the surface
separating the convective layer and the water masses on the
opposite aide, as well as the threqlolda of instability are
deduced. The values found show that-..:.lready at very small
negative superadiabatic temperature gradients (0.010 to 100 m),
the Rayleigh numbers are above the critical value, and that
convection must occur in spite of the stabilizing effect of the
rotation of the earth. There are 1 figure and 4 references,
1 of which is Soviet.
ASSOCIATION: Institut okeanologii Akademii nauk SSSR (Inatitute of oceanog-
raphy of the Academy of Sciences, USSR)
PRESENTED: April 30P 1959 by V. V. Shuleykin, Academician
SUBMITTED: April 309 1959
Card 2/2

S/010/(O/OOO/Grj4/002/C)OC,~')C(
AO53/AO26
AUTHORS: Bogorov, V.G.; Tareyev, B.A.
TITLE: Oceanic Depths and the Problem of Dumping Radioactive Waste
PERIODICAL: Izvestiya Akademii nauk SSSR, seriyakpegnficheskaya, 1960, No. 4,
PP. 3 - 10
TEXT: The authors refer to the recommendation given by V.G. Bogorov and
Ye.M. Kreps at the II International Conference on the Peaceful UtilizaTion of
Atomic Energy in Geneva in September 1958, to the effect that the dumping of ra-
dioactive waste in depths of the ocean should not be permitted. In this article
the authors furnish new proof in favor of their viewpoint based on the latest
observations made by Soviet and foreign oceanologists, in particular on the oc-
casion of the Danish expeditLon on the SS Galatea in 1952 and the Soviet expedi-
tion on the SS Vityazlin 1958. The article compares the 23 deepest depressions
In the Pacific, the Atlantic and the Indian Ocean, In indicating maximum depths
and their location. It also gives information on the prevailing temperatures as
various depths ranging from 0 to 10,000 m in different areas and at different
seasons. These temperatures even at maximum depths are subject to variations
Card 1/4

S/OlO/60/OO0/O04/oO2/orj6/Ta
A053/AO26
Oceanic Depths and the Problem of Dump.-Lng Radioactive Waste
which permits to conclude that nowhere the water Is stagnant but constantly ~n
the move, however slow this movement may be in certain places. The vertical
movement of the water in the depths of the hilippine and the Bougainville de-
pressions have been calculated as being 10-~=2/sec or about 30 - 50 m per an=T.
The speed of horizontal movement of ocean water as a rule exceeds by far that cf
vertical movement, particularly in the upper layers. The article refers to In-
vestigation5 carried out In recent years pertaining to depth circulations, men-
tioning the findings of Doctor Swallow and of Doctor Laugjiton. The article cites
a number of other phenomena, which all tend to prove the movement of water, re-
sulting in a continuous agitation and mixing process, which creates favorable
conditions to the development of life, even down to 'the greatest oceanic depths.
During deep-sea trawling of the Vityazlin 1958 in the Pacific, going down to a
depth of 10,700 m, the existence of fauna was revealed even in these ultraabys-
sal depths, consisting of sponges, worms, mollusea, etc, 'though in snall qiianti-
ties, because at a distance cf 10 km from the photosynthetizing layers only ve'ry
little food is brought down. Life in the mass of water Is in a state of corztAnt
migration. Even plankton covers considerable distances. Thn migration of ani-
Card 2/4

s/oio/6o/ooo/oo4/oo2/oo6/x)r
AO53/A026
Oceanic Depths and the Problem of Dumping Radioactive Waste
mals and biocirculation are a powerful means of transportation of all kinds of
substance Including absorbed radioactivity. Harley found that In a district
west of the Bikini Atoll radioactivity of plankton was 470 times greater than
elsewhere in the ocean. Japanese authors state that as a result of radioactive
fallout Infeoted fishes were found near the Marshall Islands, later on near the
Caroline Islands and further north near Taiwan and the Bonin Islas. Pishes
caught within a radius of 3,000 km of the district of Bikini had to be destnyed
on account of their radioactivity. This district being the spawning place of
tuna and swordfish, it is likely that its contamination by radioactive fall-out
will be of far-reaching consequences in the way of infected tunaflah, in which
connection the authors refer to the findings of the Japanese scientists Y. Miya-
ke and Y. Suguira. Interesting In this respect Is also the theory developed by
R.H. Ketchum and T.V. Bowen concerning the physical and biological transfer of
different substances, concluding that biological transfer often exceeds the role
of the physical mixing process. In respect to biocirculation a great deal of
research work remains yet to be done, especially in deep-water circulation, al-
though it is known that big plankton migrates in deep layers (down to 6 km).
Thus radioactive waste buried in the depth of the ocean, when dissolved will rise
Card 3/4

S/010/60/000/004/002/006/XX
A053/A026
Oceanic Depths and the Problems of Dumping Radioactive Waste
by means of physical as well as biological circulation and eventually endanger
the life of human beings. The theory that the radioactive substances after a
while will be dispersed and in a dissolved state mix with the entire mass of wa-
ter is ill founded. Water currents are localized and the same refers to blocir-
culation following a certain cycle. The authors agree with H.T. Dunster that
the disposal of radioactive wastes in coastal waters is highly dangerous, and so
is the dumping of such wastes in the depths of the ocean. Further investigation
and research work should clarify in particular, "The behaviour of radioactive
substances in the ocean." - "The accumulation of radioactive substances in marine
organisms and their tissues." - "The age of different layers of water and the
duration of a certain mass of water remaining in a given layer, types and speeds
of mixing processes." - "Speeds of vertical and horizontal circulations of dif-
ferent layers." - "Biocirculation, daily, seasonal, multiannual'.' - "Geo-chemical
factors influencing distribution of radioactive substances". There are 16 ref-
erences: 9 Soviet, 6 English and 1 Japanese.
ASSOCIATIONi Institut okeanologli AN SSSR (Institute of Oceanology, Academy of
Sciences, USSR)
Card 4/4

----
Theory of convection circulation in oceanic trenchea. Izv-
AN SSSR.Ser.geofis. no-7:1022-1029 JI 160.
(MIRL 13'17)
1. kkademiya nauk SSSEL, Institut okeanologii.
(Ocean currents) (Ocean bottom)

IVANOV9 lu.A.; TAREYW B.A.
Calomlating the vertical velocity saiRment of drift currento. Trudy
HGT 220-4.160, (MIRA 34:3)
(ocean currento)

---TAREM, -B.-A. s - And-KIMMI- - ---- --- -- - -
"Geostrophic currents in the JIntarctic sector of the Faefic.11
To be subudtted for the 10th Paoftc Science Congress, Honolulu, 21 &w. - 6 Sep 1961.
Irmt1tate of 00sanolog3re

NAUMOVJ, A.G.; ZEMOVA.9 V.V.; IVANOV, Yu.A.; T~IIEYIIV B.A-
Frontal zones and biog .eograjDhic division of the OuAwe waters
( 0 - 500M.) of the southeir'n..*part of the Pacific Ocean based on plankton.
Trudy Inst,okean- 58:54-6~ 162* 11 (MIRA 15:12)
(Pacific Oceqn-Plankton)

TAREYEV% B-.A-.-
Estimation of the nature of beat convection and turbulent beat
conduction as applied to the Antarctic circumpolar waters.
Okeanologiia 2 no-1:31-43 162. (BIRA 15:2)
1. Institut okeanologii AN SSSR.
(Antarctic regions--Ocean temperature)

TARETEV
Internal waves in an ocean inhomogsngoug with respect too density.
Pokle AN SSSR 149 no-43827-8V Ap f63.
(X*A 1683)
le- Institut oksanologii AN sssR. Predstavleno akademikom V. V.
Shuleykinym.
(Seawater-Density) (Waves)

TAREMp B.A.
.. Internal baroolinicn waves Jn
of the bottom and their affect
tion. Okeanologlia 1+ no.59915
t
'k
flowing around tho iTTe~kla.:~i ties j I
on protteses of sediment forma-
164 (MIPA 18al)

. TAREM, B.A.
Possibility of the formation of natural vertical convection in
acme regions of the Indian Ocean. Trudy Inat. oksan. 64.50 42
164. (MIRA 17 7 ~

TAREYEV B A.
Inter-Z! waves observable during the f'.Low around
the unevenressa3 of the floor and 'd,,eir influence on the
deposit-forming 1-.Tocesses In t1e c,-Fan. 5 no.";
451-51 165). (MIRA l8s4)
1. Institut okeanologii AN SSSR.

TAREYEV, 13,Ae
quasi-geostrophic Instability of ocean currenta. Dokl. All S313P. 162
no.104-77 My, t65. (MIRA 18:5)
1. Institut okeanologii AN SSSR. Submitted September 17, 1964.

ACC N" AR7004103 (N) SOURCE CODE: UR/0169/66/000/012/VO21/VO21
AUTHOR: Tareyev, B. A.
TITLE: Some consequences of the dyanmic instability of ocean currents
SOURCE: Ref. zh. Geofizika, Abs. 12V127
REF SOURCE: Sb. 2-y Mezhdunar. okeanogr. kongress, 1966. Tezisy dokl. M.,
Nauka, 1966, 368
TOPIC TAGS: ocean current, approximation method, perturbation, ocean current
instability
A13STRACT: The problem of the stability of geostrophic baroclinic zonal ocean
currents is studied with methods of approximation. The solution takes into account
the vertical shift of main current velocity, vert-Lcal motions, stratification, 13-effect,
inertial forces, and the horizontal eddy vis'cost'q. Internal waves were filtered by
introduction of a quasi-geostrophic approximation of the perturbation field. It is
shown that for the real values of oceanographic parameteri, the intense circulation
systems such as the Gulf Stream, Kuroshio, and trade wtnd'durrents are dynamically
Card 112 UDC: 551.465

ACC N" AR7004103
unstable, and, consequently, cannot be steady. Periods of unstable, large-scale
quasi -geostrophic perturbances occurring on the background of the main current
have a duration of several days to several weeks. These pex-iods are determined by
ithe natu! al dynamic structure of the current and do not depend on the action of
external factors (changes in tangential stress of the wind, influx of heat from the
atmosphere etc). The wavelength of the more unstable large-scale oceanic perturba-
itions is of the order of several hundred kilometers. The natural scale of horizontal
turbulences - must be accordingly of the same order. In connection with the
phenomena of instability, the possibility of forecasting time variations of ocean
currents is naturally reducecL However, some statistical characteristics of spectrall
function type can be calculated on the basis of the mean values of characteristic
quantities (shift of velocity, stratification etc). The absence of long series prevents
a comparison of calculations with observations. However, coordinated surveys in
the Gulf Stream region show that the calculations yield a* correct order of values.
Some evaluations show that unsteady increasing (and fading) perturbations play a
substantial role in the energy balance of the mean oceanic circulation. (Translation
of abstract] [DWI
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- -- TKR4vt - -
The prcduction of glass electric resistora,-Moskva, Goo. energ. izd-vo, 1944.
26 p. (50-44428)
TX2851.T38

T-A4-V , R~ R. - -- - - - --- --- - - -
I -- - - - - --- - --- - - - - -- -- -
Electrical engineering materials, Yoskva, Goa. energ. Izd-vo, 1946. 231 p. (50-19007) 1
TY,453.T3

TAREYEV, B.
Tarevev. B. M. defended his Doctor's dissertation in the Moscow Power
Engineering Institute im 11olotov, USSR, on 18 April 194,3, for the academic
degree of Doctor of Technical Sciences.
Dissertation: "Heat-Stable Electrical Insulation". Resume: Tareyev treated
factors affecting the heat stability of electrical insulation, the deter-
mination of beat stability of materials, and its dependence on chemical
composition, as well as problems related to thc- thc-rmal conductivity- of
insulation. He also cited the results of a number of his scientific research
works and new production developments dealing with concrete forms of
Insulatinm materials with relatively high heat stability: liquid and solid
organic materials, aluminum oxide insulation, asbestos materials, glass-
fiber materials, vitreous enamels, mica, and its substitutes.
Official Opponents: Profs. N. V. Aleksandrov, N. P. Bogoroditskiy (Doctors
of Technical Sciences); G. I. Skanavi, B. N. Gokhberg, (Doctors of
Physicomathematical Sciences).
SO: Elektrichestvo, No. 7, Moscow, Au,--,just 1953, pp 87-92 (W/201344, 16 Apr 54)

TAREYEVx B. M.
PA VIOT31
UM/Bleotri city
InSMlatICg VAteTIS16
Insulators
Mork of the All-Unioa Bureau of Vleotrlo Insul-
)Ation ta 1946-1947,* B. 9.~Threy6v, CajA Tech Solp
Sol Seq -Union Ba of Elso Insalation,, 1 p
All
Blaktriohestvo" No I
Bilefly touches on major achievements of subject
.barsaa for 1946-1947.
kAmi

TkRUN,, B. M. PA 4/%9 T22
"The Oldest Czechoslovakian Electrical Joaxnal,
Illaktrotsohnicky Obtor' (Ilootrioal Ememsering
Outline),* B. M# Tareyer, Cand Tech Solp S. P.
"Elaktrichostro" No 1
Coupliments subject journal for the high-level
technical information vh1oh it ban consistently coa-

TARKLEV, 13. M.
"Lectures on the 'Electrical Materials' Course" (Lektsii po kursu "Elenromaterialove-
deniye") No 3, Electrical Insulating Glasses, Editing and Publishing Division of VZEI
(All-Union Correspondence Pover Engineering Institute), 1949, 24 pp. I

TAP
. ~Ev I B . 'I,. .
_- I - - - - -- - -- - -- -- - - --- - -- - - - - - --- -- ---
personala, Electrical engineering materials, Izd. 3., perer. MoBkva, Gos. energ. izd-vo, 1941
232- p. (50-22181) 1
TK453.T3 1949

TNRIZEV, B_. 111. PA 35/4-9T27
-abin,
trigulation, 'Electrical
BiblioSraphy
"All-Union Scientifid-Tdohnical~_Congresi an'9180-
trical' Insulation" B. M. Tareyer, Dr Tech Sci) Secyj.
-Union Bu of Blec Insulation, 2 pp
"Elektrichestvo" No 1
Session was hold 4-8 Oct 48in LeniWad vith 389
engineers an& teachers partici~atiug. Ifift y-four~
i(eporte on el3otrical insulation problem were
submitted.
-few 35AM

TAREYEV9
TJW Electricity E]octric Power Publications Apr 49
glew Books on Pover Engineering" -1 p
YZIek Stants" No 4
Brief reviews includes N. K. Bodashkev's NBrmkdows in Stream Turbines and
Their Prevention," G. K. Zherbels"Teoting Asynchronous Motors After Repairs,"
T. A. Zikeyev and A. 1. Urelin's "Analysis of Pover Fuels," "Installation and
Operation of High-Preasure Boilers," edited by S. To. Fayerman and S. M.
Sbukher, NHandbook on Electrical Insulationt" edited by Yu. V. Koritakiy and
't. M. Tareyevs and F. A. Stupel's "Automatic and Protective Relays."
Ph 55/49T27

Xv 49
Currents, High-Frequer'OY
"R9719V of I. P. Berdinski'kh's Book., 'Kiln Dryimg'
and Bonding of Ligneous Materials In a Field of
Elgh-Prequency Carrentap'" B. M. Threyer, Dr Tech
Sol, Netushil, Cand Tech LlCi, DwOuL V- A-
Arkhangel,ekly, Engr, E. P. Parim, En9r, 1 P
Ollaktrichestvo" No 5
not, indoree raterial In this book., vhich
consists of three main parts: generators (elec-
tronic tubes, gaseous rectifiers, etc.), drying,
and bonding. Points out numerous deficiencies In
55/49T50
USSR/Engineering (Contd) May.49
author's analysis of his subject and lists examples
of glaring errors In text. Published by Goe-
telthizdat Ukraine, 1948, 120 pp, price 5 rubles.

USSR/Electricity - Insulation, Electric Jan 50
CNI Dielectrics
Beat-Resisting Porous Insulation, Prof B. M. Tare
Yev, Dr Tech Sci, Ya. M. Parnas, Cand Tech Sci, A3_1-
Union Corr Power Eng Inst, 5 PP
"Elektrichestvo" No 1
Notes advantages of nonimpregnateed inorganic fib'er
imulation in gaseous medium with high vorking tem-
perature and sharp temperature impulses. Deduces
formulas for breakdown voltage, dielectric constant,
and dielectric loss angle of glass fabric as temper-
ature varies. Gives results of experimental verifi-
cation of proposed formulas, confirming feasibility
USSR/Electricity - insulation, Electric Jan 50
(Contd)
of using nonimpregnated inorganic fibrous ma-
terials as heat-resistant electrical insula-
tion. Submitted 8 Jun 49.
157T22

-rf1RF_Ye-V, '&M -
PHASE x TRL43URE ISLAND BIBLIOGRAPHICAL REPORT AID 757 x
BOOK Call No.: AP630350
Author: TAREYEV, B. X.
Fall Title: ELECTRICAL ENGINEERING MATERIALS (Fourth Issue,
Reviewed)
Transliterated Title: Blektrotekhnichookiya materialy
PUBLISHING DATA
Originating Agency: None
Publishing House: State Power Engineering Publishing House!
Date: 1952 No. pp.: 288 No. of copies: 25,000
Editorial Staff: None
PURPOSE AND EVALUATION: This book is intended for workers In power
system plants and repair shops, and contains the description of
properties, grades, testing methods and treatment of materials
most frequently used in electrical engineering. The book's
value lies in its detailed description of many chemical compounds,
which by givin� their basic data and characteristics as estab-
lished by the GOST" standards, permits an insight into methods
used In Soviet power engineering.
TEXT DATA
Coveraget. The book is divided into 12 chapters, which give
1/10

Elektrotekhnicheskiye materialy AID 757 x
information on diel,~ctric materials In the first 8 chapters and
on conductors in the last four. For a more detailed account see
"Table of Contents".
Annotated Table of Contents Pages
Introduction 5-10
Ch. 1 General Information on Insulating Materials 11-21
Electric resistivity, dielectric constant, losses and
strength.
Ch. 2 Gaseous Insulating Materials 21-28
Air and various gases; The work of Professor B. M.
Ookhberg on "elegas" (gaseous SF6) is reported.
Ch. 3 Liqild Insulating Materials 28-66
Transformer oil: properties, datax testing, "GOST"
standard requirements, diagrams of testing equipment
(AMI-60 type), nitrogen treatment, description of various
regeneration devices with d4agrams .
Various liquid insulating materials: cable oil with
increased visco ity. Condenser oil: basic data according
to "GOST" stand:rds, "sovol" (diphonyl CIOH12) and
"sovtol" compounds developed by Professor Andrianov ac-
cording to technical specifications of the NKKhP.
2/10

Elektrotakhnicheakiye'materialy AID 757 - X
Pages
Ch. 4 Congealing Insulating Naterials 66-n6
Resins: thermoplastic and thermo jetting; colophony
(also used in oil varnish), "OOST" standard speciricationa;
ishellac (only imported); amber; phenolic resins: bakelite,
Iditol and "sovenit"(basic data attached)developed in the
USSR, used in the radio industry ; glyptal, nitrocellulose,
acetyl-cellulose, ethyl cellulose; vinyl group: poly-
chlorvinyl, perchlorvinyl; polysterene, congealed and
emulsion (developed by A. F. Ioffe according to All-Union
Technical Specifications of the MOP and used in radio
engineering, basic data given); polyethylene (basic data);
polylsobutylene (basic data); polymethylmetacrylate (used
for "organic glass"); polyvinylformal; polytetra-
fluorethylene (basic data); polyamide resins (including
a Soviet make: "Capron"); polysiloxen resin group
(developed by K. A. Andrianov and 0. 1. Gribanovaj.
Bitumen: artificial (oil) and mineral (stphalt "GOST"
standard data given.
Dr il (basic
aTing oil: Linseed oil, tung oil, castor o,
data
3/10

Blektrotekhnicheakiye materialy
AID 757 X
Wax: paraffin; ceresin ("GOST" standards); poly- Pages
chlornaphtalene (basic data); oleowax (developed by
N. A. Petrov and S. A. Deryabin from castor oil).
Solvents: (a table'listing formulae, standards and
properties, pp. 88-89).
I Varnish:' impregnAting-varnish (types and speci-
fidAtions'); enamel And'adhOsive varnish; oil varnish
(types and specifications); cellulose varnish (types
And diita); aniline-formaldehyde and semi-conducting
varnish.
Impregnating and filling compounds: quartz and
other compounds for bushin and cables (tables,
diagrams, "GOST" standarder.
Drying and impregnating Insulating materials:
diagrams of drying equipment. Research on effects of
moisture by Academician P. A. Rebinder, S.M. Lipatov;
research on electric properties of various types of
hygroscopic dielectrics by X. X. Mikhaylov; the book
Teorija auahki(Theory of Drying)by A. V. Lykov (1950)
is mentioned.
4/1o

Elaktrotekhnichookiya materisly AID 757 - X
Pages
Ch. 5 Fiber Bass Insulating Materials 116-136
Wood: vogerties and treatment, compounds with
nuralite ,( 5% NaP and 15% dinitrophenol).
Paper and cardboard: data and "OOST" standards for
paper Insulations of cables and capacitors, developed
by P. I. Gostev, T. P. Lazaranko, P. P. Bondarenko,
M. A. Antonov, B. I. Ushakov and K. I. Dobrynin in
1951; Mica tape ("Japanese paper") developed by I. V.
Bondarenko and K. D. Dwitriyev; glue paper ("GOST"
standards); cardboard ("GOST" otandardai.
Insulating fabrics "GOST" standards for rayon,
cotton and hemp; tapes, rubberized and tarred.
Non-varnish and varnish-treated insulating; basic
data; "GOST" standards.
Inorganic fibrous materials: asbestos, composition,
"GOST" standards, fiberglass, as developed by K. 0.
Chernyak, K. S. Aslanova, S. I. Ioffe "OOST" standards;
table with basic data and properties on p. 135.
Ch. 6 Plastic Materials 116-168
General information, composition and photo of 150 ton
hydraulic molding press. Methods of injecting, blowing,
5/ 10

Elektrotekhnicheakiye materialy AID 757 - X
Pages
and pressing with diagrams of equipment used.
Binders: bakelite type, "GOST" standards, types and
basic data.
Organic glass: plexiglass, basic data, used for high
frequency expulsion tube, diagram of RTO type.
Laminated.plastic materials: "Oetinax", new paper-
base material developed by N. I. Krestov, V. S. Kvashnin,
V. V. Kudryavtoev, V. B. Rekst, and 0. A. Butuzova, basic
data, types and "GOST" standards; cotton-base "textolite"
types, data and "GOST" standards; "glass textolite",
glass-base, data; plywood.
Plaotic flexible films; vinyl and polysterene (styro-
flex), basic data.
Rubber materials: natural and synthetic rubber
developed by I. L. Kondakov, S. V. Lebedev, N. D.Zelinskiy
and B. V. Byzov, types, basic data, and "GOST" standards.
Thiuram vulcanized rubber; ebonite, "GOST" standards,
table; asbocement, basic data; mloalex, basic data.
Ch. 7 Mineral Insulating Materials 168-IT9
Mica: Muscovite and phlogopite, properties, by M. X.
Mikhaylov, E. K. Lashev, K. A. Vodoplyanov, M.I. Mantrov).
6/jo

Elektrote.khnioheakiye materialy
AID 757 - x
Pages
Micanites, shape, components and basic dates "OOST"
standards.
Various mineral Insulating materials: marble, "OOST
standards; slate, basic data; talechlorite, basic data.
Ch. 8 Glass and Ceramics 179-214
Glass: components, properties,, typesy manufacturing,
use, basic data, table on p. 188.
Porcelain: manufacturing, basic data, types, testing,
"GOST" standards for pin type and suspension type
insulators (diagrams presented); oil circuit-breakers;
VN-35-K tpe; 110 kv transformer TFN type (diagrams
presented)
Various ceramics: Radio- and ultra-porcelain devel-
oped by N. F. Bogoroditakiy and I. D. Fridberg, basic
data listed. AluminoxIde basic data; steatiteceramics
based on T102 "Butil" (ticond T80, T60 and T150);
segnetoceramice (tibar), developed by B. M. Vul; vilyte
developed by V. I. Pruzhinina-Oranovskaya and L. I.
Ivanov used for grounding.
7/l0

TARDY, V
chiat. 58 no.2:
On the 60th birtbdaY of Dr. Jan Dolezal. Cesk. psy
130-133 AP 162.
(BIOGRAPHIES)

PETROV, G.N.; ROZWM ID, V.Ta.; KAGANOV, I.L.; PETROV, I'I.;
STAROSKOLISKIT, W*A.! TARB B. M.
Vasilii Aleksandrovich IsNiurov. Ilelctriebeetvo no 7:93 JI
,6o. (Wiurov, Vasilii Aleksandrovieh, 1885-) iMIRA 13:8)

TARS, R.
I
'V4'. , ., . I on$. Gov.profootusir 5 no-1:
' for technological progr (WA IWO
46-50 J& '57.
1. Predsedatel' komiteta profOOYuz& rsdi0s&yOd& im6ni POPIYT&.
(Udio industry) (Trade unions)

A n-i~ it! ; ;
11
Adjustment of continental triangulation nets. In German.
P. 429 (Acts, Technica) ;---iid&pest, Fungary Vol. 16, no 3/4 1957
SO: 'Monthly Index of Est European Acessions (AZEI) Vol. 6, No. 11 November 1957

T Or
4-53
TARZE A A. I.
TcQdcolw
Remchlorcyclchelmme
Feb
'"Approminate Data on Investiestions of the Toxic
F6atures of TeabnIcal Mixture of Rezoichlorcylobommw
160mrsi, A. I. T&reeva,, 2 pp
Farmkol I Takalkol" Vol X, No 2
Experimental data leading to the conclusion that
dosee of 200 and 500 mMIgmm do not cauno any
changes in the bumn akin,
4"3

M, ~ H~p F, K-oaz
IM -sr T, --I*,- -1."I
'R
z, Mlll
. fie'lk
I al., - mal 7 .11,11
-- . ; , v-- Ij5, - -
ML
"Ill I
M
ma - !E,. i- 'I" ma of, - lm~ OEM

TARELKIN, Konstantin Danilovich; SINEVNIKOVA, TS.B., red.; TSESffiiyBi,
-L-. IF. -
[Fur goods] pushno-mekhovye tovarY. Moskva, lzd-vo "Ekono-
mika," 1964. 195 P. (MM 17:6) 1

Yu.A#, inzh.; DOBROKHOTOV, V.I., in7h.; KISFLIGOF, M.L., kand.
BOYKOY ; pATyCHEN,, zh,; POGORELOV, B.F., in:zh.;
tekhn. nauk ,0, v.S., in
T~~N~.. , inzh.
Burning of lignite with a high moisture contents Elek- eta. 36
no.2:8-12 F 165. (MIRA 18:4)

RODZUrVICH, N.V., Inzh. (Kolonn&)LIALM~LKIN Yu.Vp inzh. (Kolama)
Coating with caprone of
Elek, i tepl. tiaga 6
the axle box supports of
no.lls1O N 062.-
(Diesel locomotives)
diesel locomotives,
OaRA 16ti)
.U.,

PUTILIN, V.N.9 inzh.; RODZEVICH, N.V., Inzh.; TAP.7LKIN, Yu.V., inzh.
Use of capron for the axle end thruBt bearings and bushings
of the spring suspension for locomotives. Trudy VNITI
no.19:214-223 164. (MIRA 18:3)

TMILov, A,S., inshener*
- - tomatio feed check Talves. Alsk.stao 28 no-1:77-79 Ja '57.
(KLRA 10:3)
(Boilers--saf0ty appliances)

5891 TIM IM.0, It. 1. 1.!,'etbdlka- i tekhnik-- opredeleniya kollchegtva pyll 7
vozdukhe. (metod. pialmo). tbilisi, gruza-eclCiz, 1954. ?Jss. s ill.
l6sm (nauch.- issled. irt-t glgiyeny truda I profzabolevanly im. n. i.
makhviladze m-v-n zdravookhraneniya er=. ssr), 2.000ela. beepl. -a vy.
u1mzan v kontse telmta.-na gruz. yaz.-
(55-JM) 614-71-074
SO: KnIzhmya Latopist, vol. 1,1955

I
. rm- mmmm-pml
1,

--. , - - assomm;
u. Imbn ,
om-t"mouff-i'mas
m

KA.OHABELI, M.Ye.. kand.madeneuk; 2ARMO, M.I., nauchnyy sotrudnik;
GNKBASHIDZE, G.K., klinich;;'s-L-TJv-*~-,4rnator
Sanitary and hygienic conditions of workers employed in spraying
citrus trees with octamethyl and mercaptophos. 01g. i son. 22 ho-7:
84-85 Jl '57. (MIRA 10:10)
1. Iz Institute gigiyany truda i professionallnykh zabolevaniy
Ministerstva sdravookhraneniya Gruzinskoy SSR.
(INSICTICIDIS, injurious effects,
phosphates, insprayIng citrus trees (Rua))
(PHOSPHATBS, injurious effects,
insecticides. inspreFing citrus trees (Rua))

GCGUADWp V.0 doktor khim.nauk, zasluzhannyy izobrotatell Gruzinskoy SO;
, TARENKOt M4. nauchnyy ootrudnik
Lighting without burning. Izobr. i rate. no.lOsl2-13 163.
(MIRA 17:2)
1. Institut prikladnoy khimii i alektrokhimii AN Gruzinskoy SSR'(for
Taranko).

SHVANGIRADZE; M.Di:;-TSKHfiDADZEq K.A.; TARENKOp M.I.,- GOGUADZEI V.P.
Increase of the sensitiveness of nitrogen detection by the
Lassaigne method. Zhur. anal. khim. 18 no.3.1:1399-1400 11 163.
(MIRA 17:1)
1. Institut prikladnoy khimii i elektrokhimii AN GruzSSR, Tbilisi.

%1.
~A~.
r GOGUADZE, V.P.; TARENKO,
Color reaction for thiocyanate alkyls and the synthesis of new
fluorescent dyes. Soob. AN Gruz. SSR 36 no.1:69-76 0 164.
(MIRA 18:3)
1, Institut prikladnoy khimii i elektrokhimii AN Gruzinskoy SSR.
Submitted March 6, 1964.

.66 EINA(h)/EWT(l)
M%.-- rim M'jVVVQP44 monograpa vat
Teenenko Zua Ilfinichna (Candidate of Technical. Sciences);
Troknimenko, YAroaldv Karpovich (Candidate of Technical Sciences)
1,.DelaX oystem$9~(Zamedlyayushchlye sistemy) Kiev, Izd-vo "Tekhnika"t
1965, 306 p, illus.,, biblio'. 6000 copies printed,
TOPIC TAGSt delay circuit# traveling wave., cavity resonator
PURPOSE AND COVERAUt This book is intended for the teohnical
personnel of industrial enterprises and design officeas and may
also be used by aspirants and students'in advanced courses of radio
engineering and radio electronic divisions of schools of higher
education, It describes the properties of delay systems in shf
-o ca--hode-ray tubes, using the extensive interaction of tho electron
beam with the traveling-wave field. General problems pertaining to
traveling-wave propagation in delayi-systems are described. The
electrodynamic characteristics of helical, pinj comb, and 1W11ped-
parameter delay systems and of cavity resonator circuits, as well aa
those of some special types of delay systems, are discussed.
Methods for theorical and experimental investigation of delay system
--'__-1-~d-meamw_ement of their basic parameters are presented,
21t372-
Card I/
uDo 6ei,,385.6:6

L 25799-66
ACC NRI AM6008542
OF CONTENTS.
:..-Foreword 5
Wave propagation in delay.systems 7
1. Conditions for delayed wave propagation 9
2. Basic theorems concerning fields in periodic structures 13
3, Dispersion charactei?isties -- 16
4. Field propagation in delay systems -- 23
5, Coupling impedance. Field propagation parameter .- 2T
6. Effect of delay system characteristics on traveling-wave and,
backward-wave tube operation -- 32
7, Delay system in charged-particle linear accelerators 36
2. Helical structure delay systems -39
--l.-Helically conductive cylinder -- 39
2, Tape helixes 45----
3. Coupling impedance -- 51
4, Multiconductor and modified helixes 56
Helix in dielectric and ferromagnetic media 60
Attenuation -- 63
-73o-Rod-delaysystems 67
Card 2/f_

L.2~799-66
ACC NR# M16008542
1 #Theory of multiconductor lines -- 69
2, Calculation of characteristic impedances -- 74
3, Pin comb -- 77
4* Ladder systems -- 79
86
Opposing pins made of large rods
Opposing pins as a multiconductor line 90
Y, Flat helix -- 98
U, Practical modifications of rod systems 100
440 Rib structure delay systems -- 109
1, Wave propagation above a comb structure 110
2. Complex comb systems -- 116
3. Axial symmetry rib structures -- 121
4. Opposing plates in a rectangular wavegulde 131
Lumped-parameter delay systems 138
I* Dispersion equations -- 139
2, Characteristic and coupling lmpedance~:-- 145
3. Ladder circuit delay lines -- 152
4, Iterated networks of coupled circuits 16i 175
.5* Iterated networks of bundle six-poles circuits

L 25799-66
AICC NRi A1460013542
6, Iterated networks of coupled resonators 184
1, Properties of coupled resonator circuits -- 186
2. Iterated networks of capacitive-coupled resonator circuits 195
3, Dispersion equations of inductive-coupled resonator circuits -200
4- Positive mutual-inductance resonator circuits 208
5, Negative mutual-inductance resonator circuits 220
6. Multistage septate waveguides -- 227
7, On the method of equivalent circuits -- 232
Special types of delAy.systems -- 236
1. Delay aystems with contactless components. -- 236
Delay systems with gradually changing parameters 1243
3, Dielectric delay systems* -- 248
4, Delay systems of traveling-wave cathode-ray tubes 253
5, Ring delay systems -- 255
8, Measure'ment of delay-system parameters -- 262
1, Methods of experimental investigation of delay systeas 262
2, Measurement of dispersion characteristics -- 264
3. Measurement of coupling Impedance 275
4, Measurement of cold loss -
5, Matching of delay systems L282h
Bibliography - 291
List of pritwi al ____ )1 16
Card OURM-DIT
Im
_4A,&ZUB WEs 5
22!i~51 (RIG Ws 165/ OTH W, 122

H..
TARENKOV, Ye.
6~
Tr,tp-rnrj,--';ional t(ri,--is= and tha of pa-~.~5--:-Zar -.eSs-alls.
Mor. ktfct 25 iio.8:40-41 A-c, 165. (MMA 18:8)
1. Kapi~,an teplokhoda "Fellks
..7'. a
IT I W I
III I ~ Eli I blMj I NVA um

AIL_(w NKI AT6022699 SOURCE CODE:' UR/0000/66/000/000/0334/0343 S/
AUTHOR: Thresenico V. P. 20
5 =Q--- 9,A/
ORG: none
TITLE:' Automatic ogtimization of several plants
SOURCE: Moscow. 'Anstitut avtomatilti I tolemekhaniki. Samoobuchayushchlyesya
avtomaticheskiye sistemy (Self-instructing automatic systems). Moscow, lzd-vo
Nauka, 1966, 334-343
TOPIC TAGS: optimal automatic control, queueing theory, approximate solution
ABSTRAM The aim of this paper is to determine probability distribution of states
of a system of n plants and m optimizers (M4n),,the aver-ige longth of a queue In a
servicing system under settled operating conditions, and 'the optimum number of opti-
mizers. The case considered Is one where the probability that an optimizer*-.rill find
an extremum in no more than k steps
j!'p (k) (I - P),p I - (I pyl
and distribution density of arriving'calfilimc6ming from eaiiii -plifi-Efor servicing
is
14 W U >0)1 (2)
CoDS
-Alb

4c

tU-3VX-n-IA% I LW.T; L4CUJNXI M~l IY- --' ---- ...... ~w ~~W--:~~
- . - I . - - .- I

BORTISHKO, 1,11o, ind BOKHOVMK, H-Ho, inzh.; FIDILIMAN- G,S,, Inzh.;
POZIN, Me, dnktor tekhn. nauk; TARAT, Moya., kAnd.tekhn, nauk.
Foam dust collectors used at thn &6i*ihtftftft1jA"t of the
"4patite"'Combine. Bbzop. truda, v prom. 2 no.2:9-11 7 158.
(KIRA 110)
1. rombinat "Apatit"' (for Borushko, Bokhovchuk, Pidellman). T. Ie-'
ningradskly tokhnologichfiekly institut im. lonsoveta (for Pozin,
Tarat)..
(Dast collectors)

USW/Medicine - Infectious Hepatitis Dec 53
"The Clinical Aspects, Prophylaxis, and Treatment
of Botkin's Disease in Hot Climates," Prof"E. M.
Tareyev, Active Mem, Acad of Xed Sci USSR, Moscow
Klin Med, Vol 31, No 12, PP 3-11
En=erates some of the achievements attained by
LTAR ~science in research on infectious hepatitis.
States that manifestations of this disease, In a
hot climate, may involve special types of liver
morbidity. Discusses transmission of the disease
by Inoculation. Advocates a wider use of anti-
qddemL- measures, and the use of specific
274T26
propbylaxis for this disease. Names as outstand-
Ing problems, the detn of the origin of Botkin's
disease and development of specific methods for its
treatment.

VAJIGUSICAU, Mi. Ya.; LyMBTMIY, Kh. Z.; T42y~.,G.A. __
hosphate insecticides. Gig. i
Working conditions in testing new p (141iiA 12:7)
..n. 24 no.5:12-17 My '59-
1. Is ljzbekskogo MuchnO-ilisledavatellskogo flanits'"090 'natituts"
(plJOSPHONS, POis. .in IndUBt. (RUBD
insecticides, pre.

TARVLPV. YE
Vnutrennis Bolezni (Internal Diseftses)
950 p. 6-00
SO: Your Coutin*nt Book Ljjgt, April 1954

PAVLOV# AqN.# otv, za vypusk; VOWDICHEVA, Y.N.; IVAMOVA, A.I.; KULAKOV,
I.N.; LYAKIMA, T.N.; KITOXINA, L.I.; P02MUTAXOTA. M.P.; RODI(NOTA.
L.I.; RCWHOVA, N.M.; SOPI17T, M.S.; CHICHKINA, A.A.; TRISCHMOYAO
Z.G.: BOGATYREV, P.P.; BROVKINA. A.1.; IVANOVA, L.D.; IVASMN,
G.A.; KAHNN, N.I.; LTSANOVA, L.A.; OZHBMITZVA, Z.I.; PAVLOVA.
T.I.; TTUTYUNOVA. V.1.; UNNITSINA, A.P.; ZHIVILIN, N.M.; AIJASHIGM,
M.P.; VINOGRABOV, V.I.; TZRIMIN, F.S.; KRAVCHENKO, Te.P.; LOVAGMA,
K.V.; MIKCLISKATA, V.S.; KAUOV, G.I.; MEGINA, A.V.; TA44M A V.-
KHCLINA, A.V.; BRYANSKIT, A.M.; BtMMISTROVA, V.D.; MIGORIMA. A.M.;
LUTSINKO, A.I.; CREOWA, Z.V.; TXPLINSATA, N.V.; FICCKTISTOVA, V.I.;
BUTORIN, I.M.; BOCHEARIVA, L.D.; BITMINA, V.A.; VETUSHICO. A.M.;
VIMTAM, A.A.; SORCKIN, B.S.: TbIDMO, L.T.; NIKOV, V.N.;
DUNNOV, D.I.; STEPANOVA, V.A.; KANYAKIN, V.I., red.; VAXHATOV. A.M.;
MAXAROTA, O.K., red.izd-va; PTATAKOVA, N.D.. takhn.red.
(Soviet agrimilture; a statistical mammll Sellekoe khosiaietvo
SM; statistichaskii sbornik. Moskva, 1960. 663 p. (KIRA 13:5)
I.-Russia (1923- U.S.S.R.) TSentrallnoye atatiaticheakoys uprav-
Ieniye. 2. Upravlenlye otatistiki sel'okogo khozyaystva Mntrall-
nogo statisticheskogo upravleniya SM (for all except Makarova,
Pyatakove). (Agriculture--Statistics)

TAUYEV, B,Aq r of
- long of the abOO111te current method to the stud
Some applicAt v.AIi SSSR Ser-960fisq no,71
level variations of 8, shallov s6a- 12 (KIRA 9:9)
813-82o il 156.
J.AkademiYa ua~k SSSR, Institut okeanolOglie
(ocean currents)

TAREYEVI B. A. Cand Phys-Math Sci -- (diss) "Certain Problems of
the Theory of Wind-Caused Fluctuations of the Level of Shallow-
Water Sea." MOB, 1957, !9 8 pp 20 cm. (Marihe Hydrophysical Inst,
Academy of Sciences USSR), 110 copies (KL, 27-57, 104)
- 9 -

49-58-5-4/'--
AUTHOR: Tareyev, B. A.
TITLE: Drift Curreits--i'-ff a Shallow Sea under the Inflaence of a
Wind Varying with Time (Dreyfovyye techeniya v melkovodnom
more pod deystviyem peremennogo vo vremeni vetra)
PERIODICAL: Iavestiya Akademii Nauk SSSR, Seriya Geofizicheskaya,
1958, Nr 5, PP 605-612 (USSR)
ABSTRACT: The importance of this problem arises in the following way.
In wide, but shallow reservoirs, e.g. Northern Caspian or
Azov Seas a period of time of the order of the natural oscilr-
-1-lations in the basin is required if a horizontal pressure
gradient and current gradient is to be built up. In the
case of an irregular, rapidly changing wind of the type often
found in practicelthe surface inclination will be small and,
hence, the gradi6nt component of the resulting current will
also be small compared with the drift component. This is
even more the case for local winds, e.g. in the region of the
Mangyshlak~--I_ peninsula;~t. Thus, in many instances, the current
which arises can be considered as purely due to dAft, This
is useful in ptactical cases, e.g. navigation,, where, other-
wise. a calculation must be based on t4e average wind field,
whiA may change. The development of drift currents in an
Card 1/9 infinitely deep homogeneous sea in the presence of Coriolis

11.9-58-5-4/15
Drift Currents in a Shallow Sea under the Influence of a Wind
Varying with Time.
forces and under the influence of a constant wind which
arises suddenly was first solved by Fredgollm (Ref.1). P.A.
Kitkin generalized this solution for a sea of finite depths
A further generalization to a non-stationary wind field would
lead to difficulties and, as V,, B. Shtokman and V. A- Tsikunov
(Ref.3) have shown, would not be of great interest, In deep
seas, the current is distinguished by its relative stability
and, hence, reacts less to a rapid change in wind field than
the current in a shallow sea. In a shallow sea, Coriolis
forces can be neglected in comparison with othe.~ forces; The
author considers an infinite sea of depth h over which, from
the time t = 0 , a spatially homogeneous wind blows. The
wind can change arbitrarily in magnitude and direction. Co-
ordinates are taken with x and y in the sea's surface and
z vertically downwards. Since the continuity condition
holds, only one horizontal direction (x) is considered.
Eq.(l) gives the equation of motion and Eq,,(2) the boundary
conditions.
IOU (Z)
7 4Z dluz
Card 2/9

49-58-5-4/15
Drift Currents in a Shallow Sea under the Influence of a Wind
Varying with Time.
Ou . T(t) at z -.0; u = 0 at z =--h; u --(z,o) - U (z) (2)
Tz' TO 0
u is the velocity component along the x-axis,-)(z) is the
kinematic coefficient of turbulent viscosity which, generally
steaking, depends on z I P is the constant density;
T Q is the tangential stress of the wind along the axis (a
given function of time which depends only on certain, very
general, conditions). Consider first the simplest case with
periodic boundary conditions which gives a closed solution,
V is taken to be constant and Eqs.(l) and (2) written in the
form Eqs.(3) and (4), where q(z.t) is a complex function,
the real part of which equals u(Z,t) . Substituting
tf(zlt) a e-iwtZ(z) , a differential equation is obtained
which is integrated in accordance with the boundary conditions
to give: TKZ~t) - e-iWt To sin y(h-z)
;W C 0 B YE,
Separating the real and imaginary parts of this expression,
Eq.(6) is obtained. In the case of an arbitrarily time-
Card 3/9 varying tangential stress, an elementary solution can be

49-58-5-4/15
Drift Currents in a Shallow Sea under the Influence of a Wind
Varying with Time.
obtained from Eq.(3). Flel'stad (Ref.4) and Khidaka (Ref.5)
have zhown that the result is Eq.(8). which changes into
Eq.(9) for T = const. A numerical example for a periodically
varying wind is given. The period of tangential stress
change -, - 2V x 104se--^J17.5 hourB. coefficient of turbulent
kinematic viscosity, -0 =50 cm 2/see. Taking the unit of
length to be 1 m and unit of time 10 4sec; 50, w = 1, and
a o.1 m7 Fig.1 shows the results obtained for the
velocity distribution with depth at different timeo. As can
be seen from Fig.l., in the layer from z -:0,46 h to the
bottom a counter-current is observed periodically, Observa-
tion of suitable velocity distributions in natural conditions
might lead to incorrect conclusions concerning the gradient
of these 'counter-currents, if the non-stationary wind field
is not considered. Eqs,(6) and (7) permit the calculation of
the stress at the bottom, Fig.2 shows the variation with
time of the tangential. wind stress at the surface and the
Card 4/9

49-58-5-4/15
Drift Currents in a Shallow Sea under the Influence of a Wind
Varying with Time.
tangential stress at the bottom, whilst Eq.(11) gives the
result based on the figures introduced above. Fig.2 and
Eq.(11) indicate that the greatest possible value of the
ratio Tbottom/Tsurface = 0,77 . However, Francls' (Ref.6)
experiments show -that this ratio does not exceed 0.03 in
practice. It is obviously necessary to take into account the
variation of 1) with depth. This is done by employing
Eq.(12) which gives a linear variation with depth to a small
distance from the bottom, characterized by the empirical para-
meter e . It can be considered that e is proportional to
the thickness o; the laminar layer - Flel'stad tAinks that
zlh^alO-'-- - 10--~' (Ref.7). Choice of this parameter becomes
more objective if it is assumed that the coefficient of tur-
bulent velocity near the bottom is equal to the coefficient
of normal molecular viscosity. In Eq.(12) ~o is the co-
efficient of turbulent viscosity at the surface. Hidaka
(Ref.8) considered the case of 'd varying with depth (with
e = 0) . The author now considers the case with non-
vanishing viscosity at the bottom. Eq.(l) is rewritten in
Card 5/9-the form Eq.(13) and the boundary conditions, Eq.(2) are

49-58-5-4/15
Drift Currents in a Shallow Sea under the Influence of a Wind
Varying with Time.
used with, u (z) -a 0 A solution of the form Eq.(14) is
looked for wTth the boundary and initial conditions Eq.(15)
and (16). This sives Eq.(17) in-to which the substitution
U = G(QF(z) is made. Changing the independent variable z
a differential equation for R is obtained wJth the bound-
ary conditions (Eq.20). The integral of this can be written
in the form Eq.(21), where Jo I N . correspond to the Bessel,
and Neumann functions of zero order and Yn is the root of
the transcendental equation (Eq.22). A general solution of
Eq.(17) by series is now sought, with change to a new
variable y . Employing formula (19) and the expression for
the Wronshian cvlindrical function of zero order, the co-
efficients C' and 0" in Eqs.(24) and (25) are defined,
n n
The boundary conditions (Eq.20) and an integral formula for
Z (any solution of Bessell~ equation ef zero order) are
n8w used to determine JjRnjj . Eq~(27) is now obtained
from Eqs.(23), (17), (18), (24) and (25), and is integrated.
Card 6/9

49-58-5-4/15
Drift Currents in a Shallow Sea under the Influence of a Wind
Varying with Time.
The final solution is found in the form of Eq.(29): all the
calculations can be carried out with the variable y , and
the change to z left until the final stage. If V 0 is
put equal to zero, as was done by Hidaka the solution is
made much simpler since the Neumann function disappears.
The solution can also be used for a viscosity coefficient
varying with time as in Eq.(30) - this gives Eq.(31). If
we assume the coefficient to be constant with time this
implies that turbulence is fully developed throughout all
the region. However, in a shallow sea, a non-stationary
wind, produces a turbulent viscosity varying with time.
Unfortunately, the time dependence cannot be determined
owing to the absence of data. In the case of a suddenly
arising wind which thergafter remains constant, it is natural
to use: f(t) = (1 _ e 0-5) in Eq.(30, where w(.>O) is a
parameter, characterizing, to a first approximation, the
development of turbulence in a sea under the influence of a
wind. Using this f(t) the exponential factor m (Eq.9),
characterizing the change of current velocity with time has
the form:
Card 7/9

49-58-5-4/15
Drift Currents in a Shallow Sea under the Influence of a Wind
Varying with Time. 2
2n + 1 W) ~t - -L (1 - e-wt
exp (- 1) ( 2 h - W I)]
for sufficiently large t t is approximates to:
I
exp 2n + 1 12 t
V--2h-- W
A~ ( 71)]
In other words, with a 10 increasing exponentially from
zero to a fixed value. a certain fixed velocity will be ob-
se-~ved at the moment 't1 + 1 whereas with constant
7
this value will be observed at 'ti In view of the
function used, the velocity at the start will increase
very rapidly with time? which seems to be confirmed by
Card 8/9

49-58-5-4/15
Drift Currents in a Shallow Sea under the Influence of a Wind
Varying with Time.
observations in the North Caspian. A more detailed estimate
cannot be made without more information on the function f(t)
There are 2 figures and 8 references, of which 3 are Soviet,
3 German and 2 English.
ASSOCTATION: Akademiya nauk SSSR, Institut okeanologii. (Academy of
Sciences, USSR, Institute of Oceanography)
SUBMITTED: February 212 1957.
1. Ocean currents--f4eteorological factors
Card 9/9

.#UTHOR: TareyevB..A. SOV/49-58-9-12/14
TITLE: Stationary Circulation due to Wind in a Square Basin of
Small Depth (Statsionarnyy vetrovoy nagon i tsirkulyat3jyp-
v Pryamougollnom basseyne maloy glubiny)
PERIODICAL: Izvestiya Akademii Vauk S,93R, Seriya Geofizicheskaya,
19581 Nr 91 pp 1139 - 111:4 (USSR)
ABSTRACT: It is shown in Ref 1 that if horizontal viscosity and non-
linear terms are ignored, the question of stationary wind
circulation in a shallow sea depends on the solution of the
equation:
(13 1 T
- curl
h
)x 7 ~) i)y h ay 2ji Z h
Z
where h(x, y) is the depth of the sea, T(x, y) is the
tangential stress of the wind on the surface, A is the
coefficient of vertical turbulent viscosity and ~ is
defined by the Eqs.(2). Eq.(I) has the boundary condition
Card 1/7 (3) on the contour r of the sea, i.e. the component of

SOV/49-58-9-12/14
Statibnary Circulation due to Wind in a Square Basin of Small
bepth
the total current norma.1 to the shore line equals zero.
Having solved Eq.(I) with this boundary condition, the
inclination and velocity components can be found from
Eqs.(4) and (5)-
Obviously, Eq.(l) has no significance for in
particular, the inclination of the level increases without
bound. This singularity is due to the fact that near
h -m#O , the perturbation of the level t , cannot be
considered small compared with h . in numerical integration,
this can, of cou-?,se, be avoided by assuming the coastline
to be a vertical step.
The present article considers a constant depth basin. For
small depths the Coriolis forces can be igriored. and,
hence, Eq.(13 reduces te:
h2
curiz T (6)
21L
One method of solving the equation has been given by
Leibenson (Ref 2), who assumed that the coefficients of
Card2/7 vertical and horizontal turbulent exchange were of the

*IEWA~-
SOV/49-58-9-12/14
Stationary Circulation due to Wind in a Square Basin of Small
Depth
same order.
The author assumes the X(x) Y(y) and separates the
variables. For a basin of width and length 2L , the
boundary conditions become
+ = 0 when x = 0, and y - + L
It is assumed first that the wind blows along the y-axis
and changes only along the x-axis Then:
TX = 0; curl z T % dTY(x)
dx
Assuming X proportional to sin Xn~ , gives Eq.(9).
Yn is then found from Eqs.(9) and (10) and, hence, the
general solution of (6), satisfying the conditions (8), has
the form (12). If the length 6f the basin along the
z-axis is very great (i.e. a canal), Eq.kl2) simplifies to
give (15) for the inclination of the level. Thus, the free
Card3/? surface has the form of a plane (an analogous result was

SOV/49-58-9-1 14
Stationary Circulation due to Wind in a Square Basin of Small
Depth
obtained by A.I. Felzenbaum (Ref 1)
The author next considers the general case (L 1-:'~c, The
centre of co-ordinates is now moved to the centre of the
basin (Figure 1) so that the boundary conditions become
Eq.~16). It can be seen from jsq.k7) that the solution will
depend on cos anx (where:
a. ly 2n + 1 for n = Oplp2.*.
2 * z
curl.2 is denoted by f(x~ y) and an equation, analogous
to (9), is obtained for YnW Integration of this gives
Eq.(18) for ~ :. It is next assumed that the circulation
can be expressed in the form:
TX -.4 aly + b, Ty = a2x + b2 (19)
so that: h2
Card4/7 21-L curlz T = const.

SOV/49-58-9-12/14
6-t6tionary Circulation due to vVind in a Square Basin of Small
Depth
This gives Eq.(20) for which can be rewritten in the
form (20a). It can be seen from Zqa. (6) and (16) that
horizontal circulation is absent, not onlj for a constant
wind but also when the field of the tangential wind stress
is variable but is a scalar potential.
The author next considers the case when T. = 0,
TY = ax + b (wind along the y-axis, the change in
tangential stress characterised by a). This can be
reduced, using Fqs.(20a) and (4), to an approximate
expressionr-*~aZ/O-w the inclination in a direction trans-
verse to the wind. This can be simplified further near
L if L > 2 since
ch nj1
~2
n
Ch _~l )jr L
Card5/? . [(!2

SOV/49-58-9-12/14
Stationary Circulation due to Wind in a Square Basin of Small
hbpth
It follows from the expressions for ~1~ /ax and 4) ~/r) 7
that, for 7 = 0 $ Sx = 0 and) for x = 01 Sy = 0 . The
difference is that, in the first case, both the total
current and the x component = 0 .
Figure 1 shcws diagramatically the general character of
the eiraulation corresponding to Eq.(20) for a2 = a
al = 0 . It can be seen that for a> 0, a cyclonic
circulation is obtained and with a < 0 an anticyclonic.
Circulation in an actual basin is, of course, more compli-
Cated than that described owing to the neglect of horizontal
turbulent viscosity in the above calculations. However,
the inclusion of this factor in the equations would lead to
excessive difficulty in solution.
Card 6/7

SOV/49-58-9-1.2/14
Stationary Circulation due to Wind in a Square Basin of Small
-Depth
There are 1 figure and 2 Soviet references.
ASSOCIATION: Akademiya nauk SSSR,Institut okeanologii
(Ac.Sc. USSR,Institute of Oceanology)
SUBMITTED: October 3, 195?
Card 7/7
0

ILA.
tu To-,O
Obn
co
wn

FED(MOV, y 0GOltov, V. G.
TARSM) B. A. I . M. and B
cwm and the Problem Of Waste Disposal Tbarain."
'The I)eptba of the 0
e,ientific Conference on the DiSPOOI Of
report Presented at the S) 16-21 November 1959-
Radioactive Waste',IMonac(i

3(9)-
AUTHOR: Tareyev, Be A.
SOY/20-127-5-19/58
TITLE: On Free-Convection in Deep-water Cayitiso of the Oceans
PERIODICAL: Dokla Akademii nauk SSSR2.1959, Vol 127, Nr 5, pp 1005-1008
(USSR~
ABSTRACT: In cooperation with the problem of.the sinking of radioactive
waste products of-the.atomic industry into the oceans., the
author investigates the posoibIlity of water circulation in
great depths. It follows from observations that a noticeable
superadiabatic temperature inorease oocurs with inareasing
depth.-This phenomenon in expliLined by geothermal heat suppliee.
Therefore, the entire depth muit be divIded into two layers
which are separated by that surfacav on which the gradient of
the potential temperature passes through zero. The lower layeri
in which the potential temperature increases W'Ath depths is
described as.convecti:ve layer by the author. Rayleigh (Ref 2)
already pointed oui that at..a certain value of the dimensionles3
parameter (Rayleigh number a) convection current's may occur In
a horizontal layer of water, which is heated from below. Aq
in the present case the rotation of the earth must be taken
Card 1/2 into account, the system of equations is written down for -the

SOV/20-127-5-19/58
On Free Convection in Deep-water Cavities of the Oceans
Coriolis forcea, and.the boundary conditions for the surface
separating the convective layer and the water masses on the
opposite aide, as well as the threqlolda of instability are
deduced. The values found show that-..:.lready at very small
negative superadiabatic temperature gradients (0.010 to 100 m),
the Rayleigh numbers are above the critical value, and that
convection must occur in spite of the stabilizing effect of the
rotation of the earth. There are 1 figure and 4 references,
1 of which is Soviet.
ASSOCIATION: Institut okeanologii Akademii nauk SSSR (Inatitute of oceanog-
raphy of the Academy of Sciences, USSR)
PRESENTED: April 30P 1959 by V. V. Shuleykin, Academician
SUBMITTED: April 309 1959
Card 2/2

S/010/(O/OOO/Grj4/002/C)OC,~')C(
AO53/AO26
AUTHORS: Bogorov, V.G.; Tareyev, B.A.
TITLE: Oceanic Depths and the Problem of Dumping Radioactive Waste
PERIODICAL: Izvestiya Akademii nauk SSSR, seriyakpegnficheskaya, 1960, No. 4,
PP. 3 - 10
TEXT: The authors refer to the recommendation given by V.G. Bogorov and
Ye.M. Kreps at the II International Conference on the Peaceful UtilizaTion of
Atomic Energy in Geneva in September 1958, to the effect that the dumping of ra-
dioactive waste in depths of the ocean should not be permitted. In this article
the authors furnish new proof in favor of their viewpoint based on the latest
observations made by Soviet and foreign oceanologists, in particular on the oc-
casion of the Danish expeditLon on the SS Galatea in 1952 and the Soviet expedi-
tion on the SS Vityazlin 1958. The article compares the 23 deepest depressions
In the Pacific, the Atlantic and the Indian Ocean, In indicating maximum depths
and their location. It also gives information on the prevailing temperatures as
various depths ranging from 0 to 10,000 m in different areas and at different
seasons. These temperatures even at maximum depths are subject to variations
Card 1/4

S/OlO/60/OO0/O04/oO2/orj6/Ta
A053/AO26
Oceanic Depths and the Problem of Dump.-Lng Radioactive Waste
which permits to conclude that nowhere the water Is stagnant but constantly ~n
the move, however slow this movement may be in certain places. The vertical
movement of the water in the depths of the hilippine and the Bougainville de-
pressions have been calculated as being 10-~=2/sec or about 30 - 50 m per an=T.
The speed of horizontal movement of ocean water as a rule exceeds by far that cf
vertical movement, particularly in the upper layers. The article refers to In-
vestigation5 carried out In recent years pertaining to depth circulations, men-
tioning the findings of Doctor Swallow and of Doctor Laugjiton. The article cites
a number of other phenomena, which all tend to prove the movement of water, re-
sulting in a continuous agitation and mixing process, which creates favorable
conditions to the development of life, even down to 'the greatest oceanic depths.
During deep-sea trawling of the Vityazlin 1958 in the Pacific, going down to a
depth of 10,700 m, the existence of fauna was revealed even in these ultraabys-
sal depths, consisting of sponges, worms, mollusea, etc, 'though in snall qiianti-
ties, because at a distance cf 10 km from the photosynthetizing layers only ve'ry
little food is brought down. Life in the mass of water Is in a state of corztAnt
migration. Even plankton covers considerable distances. Thn migration of ani-
Card 2/4

s/oio/6o/ooo/oo4/oo2/oo6/x)r
AO53/A026
Oceanic Depths and the Problem of Dumping Radioactive Waste
mals and biocirculation are a powerful means of transportation of all kinds of
substance Including absorbed radioactivity. Harley found that In a district
west of the Bikini Atoll radioactivity of plankton was 470 times greater than
elsewhere in the ocean. Japanese authors state that as a result of radioactive
fallout Infeoted fishes were found near the Marshall Islands, later on near the
Caroline Islands and further north near Taiwan and the Bonin Islas. Pishes
caught within a radius of 3,000 km of the district of Bikini had to be destnyed
on account of their radioactivity. This district being the spawning place of
tuna and swordfish, it is likely that its contamination by radioactive fall-out
will be of far-reaching consequences in the way of infected tunaflah, in which
connection the authors refer to the findings of the Japanese scientists Y. Miya-
ke and Y. Suguira. Interesting In this respect Is also the theory developed by
R.H. Ketchum and T.V. Bowen concerning the physical and biological transfer of
different substances, concluding that biological transfer often exceeds the role
of the physical mixing process. In respect to biocirculation a great deal of
research work remains yet to be done, especially in deep-water circulation, al-
though it is known that big plankton migrates in deep layers (down to 6 km).
Thus radioactive waste buried in the depth of the ocean, when dissolved will rise
Card 3/4

S/010/60/000/004/002/006/XX
A053/A026
Oceanic Depths and the Problems of Dumping Radioactive Waste
by means of physical as well as biological circulation and eventually endanger
the life of human beings. The theory that the radioactive substances after a
while will be dispersed and in a dissolved state mix with the entire mass of wa-
ter is ill founded. Water currents are localized and the same refers to blocir-
culation following a certain cycle. The authors agree with H.T. Dunster that
the disposal of radioactive wastes in coastal waters is highly dangerous, and so
is the dumping of such wastes in the depths of the ocean. Further investigation
and research work should clarify in particular, "The behaviour of radioactive
substances in the ocean." - "The accumulation of radioactive substances in marine
organisms and their tissues." - "The age of different layers of water and the
duration of a certain mass of water remaining in a given layer, types and speeds
of mixing processes." - "Speeds of vertical and horizontal circulations of dif-
ferent layers." - "Biocirculation, daily, seasonal, multiannual'.' - "Geo-chemical
factors influencing distribution of radioactive substances". There are 16 ref-
erences: 9 Soviet, 6 English and 1 Japanese.
ASSOCIATIONi Institut okeanologli AN SSSR (Institute of Oceanology, Academy of
Sciences, USSR)
Card 4/4

----
Theory of convection circulation in oceanic trenchea. Izv-
AN SSSR.Ser.geofis. no-7:1022-1029 JI 160.
(MIRL 13'17)
1. kkademiya nauk SSSEL, Institut okeanologii.
(Ocean currents) (Ocean bottom)

IVANOV9 lu.A.; TAREYW B.A.
Calomlating the vertical velocity saiRment of drift currento. Trudy
HGT 220-4.160, (MIRA 34:3)
(ocean currento)

---TAREM, -B.-A. s - And-KIMMI- - ---- --- -- - -
"Geostrophic currents in the JIntarctic sector of the Faefic.11
To be subudtted for the 10th Paoftc Science Congress, Honolulu, 21 &w. - 6 Sep 1961.
Irmt1tate of 00sanolog3re

NAUMOVJ, A.G.; ZEMOVA.9 V.V.; IVANOV, Yu.A.; T~IIEYIIV B.A-
Frontal zones and biog .eograjDhic division of the OuAwe waters
( 0 - 500M.) of the southeir'n..*part of the Pacific Ocean based on plankton.
Trudy Inst,okean- 58:54-6~ 162* 11 (MIRA 15:12)
(Pacific Oceqn-Plankton)

TAREYEV% B-.A-.-
Estimation of the nature of beat convection and turbulent beat
conduction as applied to the Antarctic circumpolar waters.
Okeanologiia 2 no-1:31-43 162. (BIRA 15:2)
1. Institut okeanologii AN SSSR.
(Antarctic regions--Ocean temperature)

TARETEV
Internal waves in an ocean inhomogsngoug with respect too density.
Pokle AN SSSR 149 no-43827-8V Ap f63.
(X*A 1683)
le- Institut oksanologii AN sssR. Predstavleno akademikom V. V.
Shuleykinym.
(Seawater-Density) (Waves)

TAREMp B.A.
.. Internal baroolinicn waves Jn
of the bottom and their affect
tion. Okeanologlia 1+ no.59915
t
'k
flowing around tho iTTe~kla.:~i ties j I
on protteses of sediment forma-
164 (MIPA 18al)

. TAREM, B.A.
Possibility of the formation of natural vertical convection in
acme regions of the Indian Ocean. Trudy Inat. oksan. 64.50 42
164. (MIRA 17 7 ~

TAREYEV B A.
Inter-Z! waves observable during the f'.Low around
the unevenressa3 of the floor and 'd,,eir influence on the
deposit-forming 1-.Tocesses In t1e c,-Fan. 5 no.";
451-51 165). (MIRA l8s4)
1. Institut okeanologii AN SSSR.

TAREYEV, 13,Ae
quasi-geostrophic Instability of ocean currenta. Dokl. All S313P. 162
no.104-77 My, t65. (MIRA 18:5)
1. Institut okeanologii AN SSSR. Submitted September 17, 1964.

ACC N" AR7004103 (N) SOURCE CODE: UR/0169/66/000/012/VO21/VO21
AUTHOR: Tareyev, B. A.
TITLE: Some consequences of the dyanmic instability of ocean currents
SOURCE: Ref. zh. Geofizika, Abs. 12V127
REF SOURCE: Sb. 2-y Mezhdunar. okeanogr. kongress, 1966. Tezisy dokl. M.,
Nauka, 1966, 368
TOPIC TAGS: ocean current, approximation method, perturbation, ocean current
instability
A13STRACT: The problem of the stability of geostrophic baroclinic zonal ocean
currents is studied with methods of approximation. The solution takes into account
the vertical shift of main current velocity, vert-Lcal motions, stratification, 13-effect,
inertial forces, and the horizontal eddy vis'cost'q. Internal waves were filtered by
introduction of a quasi-geostrophic approximation of the perturbation field. It is
shown that for the real values of oceanographic parameteri, the intense circulation
systems such as the Gulf Stream, Kuroshio, and trade wtnd'durrents are dynamically
Card 112 UDC: 551.465

ACC N" AR7004103
unstable, and, consequently, cannot be steady. Periods of unstable, large-scale
quasi -geostrophic perturbances occurring on the background of the main current
have a duration of several days to several weeks. These pex-iods are determined by
ithe natu! al dynamic structure of the current and do not depend on the action of
external factors (changes in tangential stress of the wind, influx of heat from the
atmosphere etc). The wavelength of the more unstable large-scale oceanic perturba-
itions is of the order of several hundred kilometers. The natural scale of horizontal
turbulences - must be accordingly of the same order. In connection with the
phenomena of instability, the possibility of forecasting time variations of ocean
currents is naturally reducecL However, some statistical characteristics of spectrall
function type can be calculated on the basis of the mean values of characteristic
quantities (shift of velocity, stratification etc). The absence of long series prevents
a comparison of calculations with observations. However, coordinated surveys in
the Gulf Stream region show that the calculations yield a* correct order of values.
Some evaluations show that unsteady increasing (and fading) perturbations play a
substantial role in the energy balance of the mean oceanic circulation. (Translation
of abstract] [DWI
SUB CODE:
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The prcduction of glass electric resistora,-Moskva, Goo. energ. izd-vo, 1944.
26 p. (50-44428)
TX2851.T38

T-A4-V , R~ R. - -- - - - --- --- - - -
I -- - - - - --- - --- - - - - -- -- -
Electrical engineering materials, Yoskva, Goa. energ. Izd-vo, 1946. 231 p. (50-19007) 1
TY,453.T3

TAREYEV, B.
Tarevev. B. M. defended his Doctor's dissertation in the Moscow Power
Engineering Institute im 11olotov, USSR, on 18 April 194,3, for the academic
degree of Doctor of Technical Sciences.
Dissertation: "Heat-Stable Electrical Insulation". Resume: Tareyev treated
factors affecting the heat stability of electrical insulation, the deter-
mination of beat stability of materials, and its dependence on chemical
composition, as well as problems related to thc- thc-rmal conductivity- of
insulation. He also cited the results of a number of his scientific research
works and new production developments dealing with concrete forms of
Insulatinm materials with relatively high heat stability: liquid and solid
organic materials, aluminum oxide insulation, asbestos materials, glass-
fiber materials, vitreous enamels, mica, and its substitutes.
Official Opponents: Profs. N. V. Aleksandrov, N. P. Bogoroditskiy (Doctors
of Technical Sciences); G. I. Skanavi, B. N. Gokhberg, (Doctors of
Physicomathematical Sciences).
SO: Elektrichestvo, No. 7, Moscow, Au,--,just 1953, pp 87-92 (W/201344, 16 Apr 54)

TAREYEVx B. M.
PA VIOT31
UM/Bleotri city
InSMlatICg VAteTIS16
Insulators
Mork of the All-Unioa Bureau of Vleotrlo Insul-
)Ation ta 1946-1947,* B. 9.~Threy6v, CajA Tech Solp
Sol Seq -Union Ba of Elso Insalation,, 1 p
All
Blaktriohestvo" No I
Bilefly touches on major achievements of subject
.barsaa for 1946-1947.
kAmi

TkRUN,, B. M. PA 4/%9 T22
"The Oldest Czechoslovakian Electrical Joaxnal,
Illaktrotsohnicky Obtor' (Ilootrioal Ememsering
Outline),* B. M# Tareyer, Cand Tech Solp S. P.
"Elaktrichostro" No 1
Coupliments subject journal for the high-level
technical information vh1oh it ban consistently coa-

TARKLEV, 13. M.
"Lectures on the 'Electrical Materials' Course" (Lektsii po kursu "Elenromaterialove-
deniye") No 3, Electrical Insulating Glasses, Editing and Publishing Division of VZEI
(All-Union Correspondence Pover Engineering Institute), 1949, 24 pp. I

TAP
. ~Ev I B . 'I,. .
_- I - - - - -- - -- - -- -- - - --- - -- - - - - - --- -- ---
personala, Electrical engineering materials, Izd. 3., perer. MoBkva, Gos. energ. izd-vo, 1941
232- p. (50-22181) 1
TK453.T3 1949

TNRIZEV, B_. 111. PA 35/4-9T27
-abin,
trigulation, 'Electrical
BiblioSraphy
"All-Union Scientifid-Tdohnical~_Congresi an'9180-
trical' Insulation" B. M. Tareyer, Dr Tech Sci) Secyj.
-Union Bu of Blec Insulation, 2 pp
"Elektrichestvo" No 1
Session was hold 4-8 Oct 48in LeniWad vith 389
engineers an& teachers partici~atiug. Ifift y-four~
i(eporte on el3otrical insulation problem were
submitted.
-few 35AM

TAREYEV9
TJW Electricity E]octric Power Publications Apr 49
glew Books on Pover Engineering" -1 p
YZIek Stants" No 4
Brief reviews includes N. K. Bodashkev's NBrmkdows in Stream Turbines and
Their Prevention," G. K. Zherbels"Teoting Asynchronous Motors After Repairs,"
T. A. Zikeyev and A. 1. Urelin's "Analysis of Pover Fuels," "Installation and
Operation of High-Preasure Boilers," edited by S. To. Fayerman and S. M.
Sbukher, NHandbook on Electrical Insulationt" edited by Yu. V. Koritakiy and
't. M. Tareyevs and F. A. Stupel's "Automatic and Protective Relays."
Ph 55/49T27

Xv 49
Currents, High-Frequer'OY
"R9719V of I. P. Berdinski'kh's Book., 'Kiln Dryimg'
and Bonding of Ligneous Materials In a Field of
Elgh-Prequency Carrentap'" B. M. Threyer, Dr Tech
Sol, Netushil, Cand Tech LlCi, DwOuL V- A-
Arkhangel,ekly, Engr, E. P. Parim, En9r, 1 P
Ollaktrichestvo" No 5
not, indoree raterial In this book., vhich
consists of three main parts: generators (elec-
tronic tubes, gaseous rectifiers, etc.), drying,
and bonding. Points out numerous deficiencies In
55/49T50
USSR/Engineering (Contd) May.49
author's analysis of his subject and lists examples
of glaring errors In text. Published by Goe-
telthizdat Ukraine, 1948, 120 pp, price 5 rubles.

USSR/Electricity - Insulation, Electric Jan 50
CNI Dielectrics
Beat-Resisting Porous Insulation, Prof B. M. Tare
Yev, Dr Tech Sci, Ya. M. Parnas, Cand Tech Sci, A3_1-
Union Corr Power Eng Inst, 5 PP
"Elektrichestvo" No 1
Notes advantages of nonimpregnateed inorganic fib'er
imulation in gaseous medium with high vorking tem-
perature and sharp temperature impulses. Deduces
formulas for breakdown voltage, dielectric constant,
and dielectric loss angle of glass fabric as temper-
ature varies. Gives results of experimental verifi-
cation of proposed formulas, confirming feasibility
USSR/Electricity - insulation, Electric Jan 50
(Contd)
of using nonimpregnated inorganic fibrous ma-
terials as heat-resistant electrical insula-
tion. Submitted 8 Jun 49.
157T22

-rf1RF_Ye-V, '&M -
PHASE x TRL43URE ISLAND BIBLIOGRAPHICAL REPORT AID 757 x
BOOK Call No.: AP630350
Author: TAREYEV, B. X.
Fall Title: ELECTRICAL ENGINEERING MATERIALS (Fourth Issue,
Reviewed)
Transliterated Title: Blektrotekhnichookiya materialy
PUBLISHING DATA
Originating Agency: None
Publishing House: State Power Engineering Publishing House!
Date: 1952 No. pp.: 288 No. of copies: 25,000
Editorial Staff: None
PURPOSE AND EVALUATION: This book is intended for workers In power
system plants and repair shops, and contains the description of
properties, grades, testing methods and treatment of materials
most frequently used in electrical engineering. The book's
value lies in its detailed description of many chemical compounds,
which by givin� their basic data and characteristics as estab-
lished by the GOST" standards, permits an insight into methods
used In Soviet power engineering.
TEXT DATA
Coveraget. The book is divided into 12 chapters, which give
1/10

Elektrotekhnicheskiye materialy AID 757 x
information on diel,~ctric materials In the first 8 chapters and
on conductors in the last four. For a more detailed account see
"Table of Contents".
Annotated Table of Contents Pages
Introduction 5-10
Ch. 1 General Information on Insulating Materials 11-21
Electric resistivity, dielectric constant, losses and
strength.
Ch. 2 Gaseous Insulating Materials 21-28
Air and various gases; The work of Professor B. M.
Ookhberg on "elegas" (gaseous SF6) is reported.
Ch. 3 Liqild Insulating Materials 28-66
Transformer oil: properties, datax testing, "GOST"
standard requirements, diagrams of testing equipment
(AMI-60 type), nitrogen treatment, description of various
regeneration devices with d4agrams .
Various liquid insulating materials: cable oil with
increased visco ity. Condenser oil: basic data according
to "GOST" stand:rds, "sovol" (diphonyl CIOH12) and
"sovtol" compounds developed by Professor Andrianov ac-
cording to technical specifications of the NKKhP.
2/10

Elektrotakhnicheakiye'materialy AID 757 - X
Pages
Ch. 4 Congealing Insulating Naterials 66-n6
Resins: thermoplastic and thermo jetting; colophony
(also used in oil varnish), "OOST" standard speciricationa;
ishellac (only imported); amber; phenolic resins: bakelite,
Iditol and "sovenit"(basic data attached)developed in the
USSR, used in the radio industry ; glyptal, nitrocellulose,
acetyl-cellulose, ethyl cellulose; vinyl group: poly-
chlorvinyl, perchlorvinyl; polysterene, congealed and
emulsion (developed by A. F. Ioffe according to All-Union
Technical Specifications of the MOP and used in radio
engineering, basic data given); polyethylene (basic data);
polylsobutylene (basic data); polymethylmetacrylate (used
for "organic glass"); polyvinylformal; polytetra-
fluorethylene (basic data); polyamide resins (including
a Soviet make: "Capron"); polysiloxen resin group
(developed by K. A. Andrianov and 0. 1. Gribanovaj.
Bitumen: artificial (oil) and mineral (stphalt "GOST"
standard data given.
Dr il (basic
aTing oil: Linseed oil, tung oil, castor o,
data
3/10

Blektrotekhnicheakiye materialy
AID 757 X
Wax: paraffin; ceresin ("GOST" standards); poly- Pages
chlornaphtalene (basic data); oleowax (developed by
N. A. Petrov and S. A. Deryabin from castor oil).
Solvents: (a table'listing formulae, standards and
properties, pp. 88-89).
I Varnish:' impregnAting-varnish (types and speci-
fidAtions'); enamel And'adhOsive varnish; oil varnish
(types and specifications); cellulose varnish (types
And diita); aniline-formaldehyde and semi-conducting
varnish.
Impregnating and filling compounds: quartz and
other compounds for bushin and cables (tables,
diagrams, "GOST" standarder.
Drying and impregnating Insulating materials:
diagrams of drying equipment. Research on effects of
moisture by Academician P. A. Rebinder, S.M. Lipatov;
research on electric properties of various types of
hygroscopic dielectrics by X. X. Mikhaylov; the book
Teorija auahki(Theory of Drying)by A. V. Lykov (1950)
is mentioned.
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Elaktrotekhnichookiya materisly AID 757 - X
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Ch. 5 Fiber Bass Insulating Materials 116-136
Wood: vogerties and treatment, compounds with
nuralite ,( 5% NaP and 15% dinitrophenol).
Paper and cardboard: data and "OOST" standards for
paper Insulations of cables and capacitors, developed
by P. I. Gostev, T. P. Lazaranko, P. P. Bondarenko,
M. A. Antonov, B. I. Ushakov and K. I. Dobrynin in
1951; Mica tape ("Japanese paper") developed by I. V.
Bondarenko and K. D. Dwitriyev; glue paper ("GOST"
standards); cardboard ("GOST" otandardai.
Insulating fabrics "GOST" standards for rayon,
cotton and hemp; tapes, rubberized and tarred.
Non-varnish and varnish-treated insulating; basic
data; "GOST" standards.
Inorganic fibrous materials: asbestos, composition,
"GOST" standards, fiberglass, as developed by K. 0.
Chernyak, K. S. Aslanova, S. I. Ioffe "OOST" standards;
table with basic data and properties on p. 135.
Ch. 6 Plastic Materials 116-168
General information, composition and photo of 150 ton
hydraulic molding press. Methods of injecting, blowing,
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Elektrotekhnicheakiye materialy AID 757 - X
Pages
and pressing with diagrams of equipment used.
Binders: bakelite type, "GOST" standards, types and
basic data.
Organic glass: plexiglass, basic data, used for high
frequency expulsion tube, diagram of RTO type.
Laminated.plastic materials: "Oetinax", new paper-
base material developed by N. I. Krestov, V. S. Kvashnin,
V. V. Kudryavtoev, V. B. Rekst, and 0. A. Butuzova, basic
data, types and "GOST" standards; cotton-base "textolite"
types, data and "GOST" standards; "glass textolite",
glass-base, data; plywood.
Plaotic flexible films; vinyl and polysterene (styro-
flex), basic data.
Rubber materials: natural and synthetic rubber
developed by I. L. Kondakov, S. V. Lebedev, N. D.Zelinskiy
and B. V. Byzov, types, basic data, and "GOST" standards.
Thiuram vulcanized rubber; ebonite, "GOST" standards,
table; asbocement, basic data; mloalex, basic data.
Ch. 7 Mineral Insulating Materials 168-IT9
Mica: Muscovite and phlogopite, properties, by M. X.
Mikhaylov, E. K. Lashev, K. A. Vodoplyanov, M.I. Mantrov).
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Elektrote.khnioheakiye materialy
AID 757 - x
Pages
Micanites, shape, components and basic dates "OOST"
standards.
Various mineral Insulating materials: marble, "OOST
standards; slate, basic data; talechlorite, basic data.
Ch. 8 Glass and Ceramics 179-214
Glass: components, properties,, typesy manufacturing,
use, basic data, table on p. 188.
Porcelain: manufacturing, basic data, types, testing,
"GOST" standards for pin type and suspension type
insulators (diagrams presented); oil circuit-breakers;
VN-35-K tpe; 110 kv transformer TFN type (diagrams
presented)
Various ceramics: Radio- and ultra-porcelain devel-
oped by N. F. Bogoroditakiy and I. D. Fridberg, basic
data listed. AluminoxIde basic data; steatiteceramics
based on T102 "Butil" (ticond T80, T60 and T150);
segnetoceramice (tibar), developed by B. M. Vul; vilyte
developed by V. I. Pruzhinina-Oranovskaya and L. I.
Ivanov used for grounding.
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