SCIENTIFIC ABSTRACT TKACHENKO. A.S. - TKACHENKO, D.F.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001755920003-9
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: July 16, 2001
• Sequence Number: 3
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

S/148/60/000/008/005/018
Determination of Efforts in Cold Rolling With Tension A161/AO29
duced from Koroleves work (Ref- 3) to simplify the formula. Experiments have
been cArried out with a continuous three-stand cold strip mill at the tin sheet
shop of the "Zaporozhstal"' works. The mill has a bobbin type uncoiler and a
coiler with a 500-mm diameter drum. Tension is used between the stands by loop-
ers as well as between stand and coiler. Metal pressure on the rolls was meas-
ured byresistance dynamometers with pickups. Comparison of the calculated and
experimental results proves that the formulae have given sufficiently accurate
data. Korolevis formulae gave too low values. The results of the work are re-
commended for calculation and designing of rolling mills with minimum weight, as
well as for calculating the optimum rolling process technology. There are 5 f1g-
ures and 7 Soviet references.
ASSOCIATION: Dnepropetrovskiy metallurgicheskiy institut (Dnepropetrovsk Met-
allurgical Institute)
SUBMITTED: June 26, 1959
Card 2/2

KOZHEVNIKOV, S-H- CKOzheynikov, S.M.] (Dnepropetrovsk); TKACHEiKO, A.S.
(Daepropetrovsk)
Automatic regulation of the thickness of strips on
continuous rolling mills. Pryk:l.mekh. 6 no-3:335-337
160. (MIU 13: 8)
1. Dnepropetrovskiy metallurgicheakiy institut.
(Automatic control) (Rolling mills)

J-7
S
/ 37/62/000/005/061/150
A0061AI01
AUTFOR: Tkachenko, A. S.,
TITLE: Investigating deformation of metal during the rolling of thin strips
PERIODICAL: Referativnyy zhurnal, Metallurgiya, no. 5, 1962, 2-3, abstract 5D11
("Nauchn. zap. Dnepropetr. un-t", 1961, V. 55, 39-48)
TEXT- Theoretical and experimental investigations were made of the deforma-
tion of metals during the rolling of thin strips with active rolls and front and
rear tension. As a result, It was established that the problem of investigating
metal deformatioreduring the rolling of thin sheets and strips can be reduced to
one-dimensional problem of plasticity; approximate equations of equilibrium and
plasticity can be used if Fk/Fc > 4. On the basis of experimental data on the
strengthening of rolled metal, it is necessary to take into account the law of
metal -itreng then ing during rolling. For the steel sheets and strips the-follow-
Ing law of metal strengthening during the rolling procann can bo. lired: 6~3 -
(0- + 1) - eO.577x, where 6'. is the yield limit; 6.1 Is the yield limit after
5
rolling In the stand. When determining metal pressure on the rol-Is in stand 3
Card 1/2

Investigating deformation of metal ...
,9/137/62/000/005/061/150
A000101.
and the following stands of-continuous rolling mills, and after a given number of,
passes on reversing mills, the law of metal strengthening can be used in the form
of a straight line for the whole deformation zone.
K. Ursova
[Abstracter's note: Complete translation]
Card 2/2

KOZHEVNIKGV, S.N.; SKICHKO, P.Ya., kand.tekhn.nauk; LENSKIY, A.N., inzh.;
TKAGHENKO A S inzh.
investigating the 950 blooming mill at the Dzerzhinskii plant
by experimental and ana.Lyt,.Leal meant, no with he.Lp of an
electron model. Trudy Inst.chern.met.AN URSR 16,37-55 162.
(MIRA 15:12)
1. Chlen-korrespondent AN UkrSSR (for Kozhevnikov).
(Dneprodzerzhinsk-Rolling mills-Testing)
(Electronic analog computers)

KOZHEVNIKOV, S.N.; SKICHKO, P.Ya., kand.tekhn.nauk;.TUIffAW__A.S-, inzh.
Dynamics of electromechanical systems with flexible couplings.
Trudy Inst.chern.met.AN URSR 16:56-65 162. (KIRA 15:12)
1. Chlen-korrespondent AN Uk26SR (for Kozhevnikov).
(Rolling mills)

KOZHEVNIKOV, S.N.; TKACHENKO, A.S... inzh.; SKICHKO, P.Ya.,, kand.tekhn.
nauk ------------
Experimental investigation of the performance of continuous
three-high rolling mills. Trudy Inst.chern.met.AN URSR
16454-160 162. (MIRA 15:12)
1. Ghlen-~Orrespondent AN UkrSSR (for Kozhevnikov)a
(Rolling mills-Testing)

KLIMKOVSKIYY B.M.; TKACHENKO, A.S.
Improving the tranBMiSSiOn of rolls on cold rolling pipe
mills. Metallurg 9 no.406-37 Ap t64. (MIRA 170)
1. Institut chernoy metallurgil AN Ukr6SR.

XLDIKDVSW# B,M.; TXArodEXK--'I, A.3,
InvostIgating tho perfoxmnee of a dial-feed wroban1sm
on cold pipe rolling nills. Met. i gornorud. prom*
no.6:34-36 N-D 165. (HM 18:12)

4 pe r o r. -ar

-- '___AP66358 - - - -Oj~ ----
Acc NR 19 SOURCE Coff.. /61~f:~/66/OOC~/02C~fddi~/66iS~i'I
INVENTOR: Klimkovskiy, B. M.; Tkacheako, A. S.; Bondarenko, A. G.; Stepanov, 1. V.
ORG: None
TITLE: A device for balancing forces of inertia. Class 7, No. 186952
SOURCE: Izobreteniya, promyshlennyye obraztsy, tovarnyye znaki, no. 20, 1966, 19
TOPIC TAGS: rolling mill, cold rolling, pneumatic aervomechanism
ABSTRACT: This Author's Certificate introduces: 1. A device for balancing the
forces of inertia generated during reciprocating motion of the stand in a cold-rol-
ling tube mill. The unit contains compensating pneumatic cylinders with pistons.
The initial pressure is automatically controlled with renpect to the rate of rolling.
The installation is equipped with a centrifugal pressure regulator connected to the
drive shaft of the stand. 'rhe regulator valve connects the compensating cylinders to
the air line. 2. A modification of this device in which the make-up feed to the com-
pensating cylinders is simplified and made more reliable by elongating the piston
slides which act as the make-up valve and equipping them with ports which connect the
cylinder cavities to the make-up line.
Card
621.771.o6-755-589.4

ACC NR, AP6035819
1--drive shaft of the stand; 2-centrifugal pressure regulfitor; 3-valve; 4-compen-
sating cylinders; 5-air 'Ine; 6-pistan slide-, 7-porta; 8---cylinder cavities;
9--make-up line
suB com 13/ suBm DATE: o4sep65
Card 21

PHASE I BOOK EXPLOITATION SOV/5973
Rayev-Bogoalovskiy, Boris Sergeyevich, Georgiy Ivanovich Glushkov,_Andrey
-Stepanovich Tkachenko, Aleksandr Vasillyevich Mikhaylovp Leon Ivanovich Manvelov,
Mt~ayva~novc ~o ;Rhov, Ivan Nikolayevich Tolmachevp and Fedor Iosifovich
Ruban
Zhsstkiye pokrytiya aerodromov (Hard Surface Covers of Airfields) Moscow,
Avtotransizdat, 1961. 321 p. 2000 copies printed.
E4.: B.iS. Deberdeyev; Tech. Ed.: Ye. N. Galaktionova.
PURPOSE: This book is intended for technical personnel and may prove useful to
students at technical schools.
COVERAGE3 The book discusses the properties, characteristic features., and con-
struction of runways, taxiways., stands for airplanes, and platforms for passen-
gers to be used in the various climatic 4nd geological regions of the USSR. The
following are reviewed: specifications of materials, modern airfield-surface
covers (one- and two-layer concrete, ferroconcrete, prestressed, monolithic, and
Card 1/#

Hard Surface Covers of Airfields SOV/5973
prefabricated), construction methods, and methods of designing all types of
covers. Calculation techniques are given for facilitating the design process.
The particular results obtained from the development of well-designed structures
have been generalized and are presented together with.a summary of the scientific
investigation on which this development is based. B. S. Rayev-Bogoslovskiy,
Candidate of Technical Sciences,wrote the foreword and sections 20 to 34 36 to 391
4_1+ to 47; G. I. Glushkov, Doctor of Technical Scienceso 8 to 12, 40, 4X, 43, 48-50Y
53, 54; A. S. TkachenIko, Candidate of Technical Sciences, 32 to 35; L. 1. Manvelov,
Candidate of Technical Sciences U; A. V. Mikhaylov, Candidate of Tech-
,, 3 to 7, 51, ?1
nical Sciences, 14, 15; N. I. Volokhov, Candidate of Technical Sciences, 16 to 18,
42, 56; 1. N. Tolmachev, Candidate of Technical Sciences, 13, 15, and pages 290,
291s 301, 302,, F. I. Rfiban, Candidate of Technical Sciences~ lc~. Sections 1 and 2
were written by G. 1. Glushkov together with A. V. Mikhaylov . The general scien-
tifi,c editing was carried out by. K. S. Makeyev, B. S. Rayev- Bogoslovskiy, and 1. .1.
Manvelov. There are 66 references, all Soviet.
Card 21#

PUSHKARI, Arnolld Ignatlyevichi-TKACEENKO,_ A.S. , red.; I-OWSHKINA, L.I. 9
tekbn. red.
[Kurile Islands] Ostrova Kurillskie. IUzhno-Sakhalinak, Sakhalin-
s%oe knizhnoe izd-vot 1960. 174 P. (MIRA 24:7)
(Kurile Islands-Description and travel)

ANANIYEV, M.G.; GORBOVITSKIY, Ye.B.; KOZLOV, Yu.G.; GOWDINA, B.G.;
KASHCHEVSKAYA, L.A.; LEVITSKAYA, L.A.; IVANOVA, L.N.; SUPKO,
N.S.; TKACHENKO, A.S.; UNIK, V.I.
------
Study of and experience in the use of the Soviet artificial
kidney apparatus. Sov.med. 26 no.7:15-20 Jl 162. (MIRA 15:11)
1. Iz Nauchno-issledovatel'Bkogo instituta eksperimentallnoy
khirurgicheskoy apparatury i Instrwnentov (dir. M.G.Ananlyev).
(KIDNEYS, ARTIFICIAL)

4.T-.- inshener (at. Kary); BELENIKIY, A.D., inzhener (St.
Xary); KOLOSOV, B.A., Inzhener (at. Xary)
Xethod of heating exciter windings and the main generator of
diesel locbmotives. Zhal.dor.tranap. 37 no-7:79-80 JI 156.
(KLRA 9:8)
(Diesel locomotive&)

"cc 3 e

AIEKSEYEVA, A.M.; TKACHEVKD, A.V.
Testicular synthesis of creatine. Vop. med. kchim. 7 no.3:1,24-325
my-je 161. (KIRA 15:3)
1. Iz kafedry biokhimii Kalininskogo meditainskogo instituta.
(TESTICIE) (CREATUM)

ZAMIAROU, AN.; TYURLIKOVA, L.P.; M~CIMNKO, A.V.
Content of nucleic acids; a3corbic acid and scme phosphoruB
compounds in guinea pigs during -the reparative ragenemtion
of skeletal muse2es. Vop. mod. Whim. 7 no.6:608-614 N.-D 161.
(Iff-W, 15:3)
y, "Academician I.P.
1. Chairs of Biology and Biochomistr,
Pavlov" First Medical Inatitute, Leniwgra!.
(MUSCIE) (NMIZIG AOIDS)
(ASCORBIC ACID) (EICSPHORUS C(14POUBDS)

TJCACHENkO A V
Detsmininj the coefficient of turbulent viscosity in stmosDheric
boundary layers. Trudy GGO no.60:53-59 156. (KMA 10:7)
(Boundary layer) (Atmospheria turbulence)

36-57-69-4/16
AUTHOR: Tkachenko, A. V.
T=: Convection and Its ApplJo-a:tion to I.3zal Forecast-ing (0 moshchnosti
konvektsii i yeye ispollzovanii pri lokallnZrkh pr~gnozakh)
PERIODICAL: Trudy Glp-vroy geafizicheskoy observatorii1191,57,
Nr 69, pp 36-4o (rjwR)
ABSTRAM. The author refers to "power of oon,,ection" (E) as the volume of work
performed by air masses per imit of time (t) in a colum-a of air at altitude h and
a unit cross-section. In order to calculate val-m-a(P), the rate of change in :Ehe
kinetic energy of convective movement must first be established. This coeffi-
cient it, in turn, closely related to the coefficient of turbulence, since the
theory of turbulence can also be applied to convective movements (changes). Ex-
periments have proven that the turbulence cc-efficient ie greater (and hence con-
vection is stronger) over hilly surfaces than over plains. Mw%hematlcal studies
are offered to calculate the power of convection using date from aerological (wind
and temperature) observations and to deduce the ratio between c.,)Avection intensity
in the morning and maximum daily intensity. A practical forw:aa is given to cal-
culate the power of ccnvecticni after zolving the aforemerr"Jiowd questions. The
author refers to D. L. Taykhtmanln mthod of calculAting the force of convection,
Card 1/2

Convection and Its Applica;Uon to Local (Cont.) 36-5T-69-4116
and also to M. P. Churinava's method of calculating the turbi-,ler-ce coefficient.
The relevant observational data vere supplied by Ye. S. Selezneva. There are
4 Soviet references.
AVAILABLE: Library of Cougreas
Card 2/2

3, TO ad;
89075
S/169/60oo/boi/boi/bii
AOO5/AOO1
Translation from: Referativnyy zhurnal, Geofizika, 1961, No. 1, pp. 110-41, # 1B353
AUTHOR: Tkachenko,_A--I-
TITLE: The Problem of the Effect of Catabatic Motions on the Convection
Development in the Atmosphere
PERIODICAL: "Nauchn, zap, Ltvovsk s.-kh. in-t, 1958, Vol. 8, pp. 205-213
TEXT: Some considerations are presented on the analysis methods of the
development conditions of,atmospheric convection; the author takes into account
the existence of both anabatic and catabatic air motions, but horizontal motions
are neglected, It is shorn that the conditions of vertical stability are deter-
mined in all these methods by the comparison of the actual temperature gradient
with the value ~ 0 = A I ? It + X T ', where ? "I ~ " are the dry- and moist-
adiabatic lapse rates respectiv2y, and ~ and X2 are the weight factorsY which
satisfy the normalization conditions I + ~,2 - I and are determined in different
ways in the various methods. Tn particular', in the layer method the cloudiness n
(the fraction of the clouded sky) becomes identical with the value A2- This
Card 1/2

89075
S/16g/Wow/bo 1/to i/3 11
A005/AOOl
The Problem of the Effect of Catabatic Motions on the Convection Development in
the Atmosphere
concept isfundamentally criticized. Reasoning shows that n4:~:,, ~2 only when it is
small and when the clouds occur near the zenith. If an intense convection takes
place, one can assume a direct relation between n an~ X1. The investigation
showed that although n can differ considerably from 1 at any individual period,
but then n changes with time, as a rule, towards the value of A, observed.
L. Gandin
Translator's note: This is the full translation of the original Russian abstract.
Card 2/2

AUTHOR: Tkachenko, A. V, SOV150- 5 8-9- 5/19
TITLE: Exploitation of the Stratification-Method for the Forecast
of Convective Clouds, Downpours and Thunderstorms (Ispoll-
zovaniye metoda sloya dlya prognoza konvektivnoy oblachno!~ti,
livney i groz)
PERIODICAL: Meteorologiya i gidrologiya, 1958, Nr 9, pp. 24 - 27 (USSR)
ABSTRACT: The scheme of the formation of convection which was
discussed in several papers (Refs 1-9) accor'ding to the
stratification method makes it possible to determine the
dependence between the vertical thickness of convective
clouds and the extent of the surface covered by these
clouds. The knowledge of this dependence was used for the
forecast of clouds (Refs 1,5,6). The author deals with
some problems of practical exploitation of the mentioned
method of forecasting as is known the instability of
temperature stratification of air is the most important
factor to determine the formation of convection. The
conditions of stability of the atmosphere in vertical
Card 1/4 direction which are offered by the stratification method

Exploitation of the Stratification-Method for the SOV/'JO-58-9-5/19
Forecast of Convective Clouds, Downpou.,z and Thunderotorms
in the case of a wet-adia %tic rise of a small volume
of air by a dry-adiabatic 'alling medium may be described in
the following way: An air ayer with a temperature
gradient y is either constaitly or inconstantly or
indifferentl~stratified if
sb (1), where sb denotes the so-called "amount of
convective clouds."
7 '_ 7B (2) where 7 denotes the actual temperature gradient.,
7C - 7B
YC the dry-adiabatic temperature gradient and y B the wet-
adiabatic temperature gradienti which characterizes the
change of temperature in a rising volume of the saturated
air with respect to which the state of equilibrium of the
stratum concerned is determined. In case the air volume
rose up to an altitude h from the condensation altitude
and passed a number of strata with different y-values
Card 2/4 the right part of the criterion (1) has to have a formula

Exploitation of the Stratification-Method for the 307/50-58-9-~-/19
Forecast of Convective Clouds, Downpours and Thunderatorza
which after integration runs as follows
TB(h) - T(h)
11(h) TB(h) - TC(h) W.This formula contains only
temperature values of the altitude h which may easily
be obtained from an aerological diagram (Ref 7). In
formula (4) only temperature values in an altitude h are
contained. If an emagram shows curves which are usually
plotted in connection with the setting up of a convection
forecast, i,.e,.: a) the stratification curve and b) the
curve describing the state of the rising air volume,
(e.g.referred to the timne of the climax in the formation of
convection), then t-e curve b) is represented by a drfty-
adiabatic up to the condensation altitude and by a wet-
adiabate above it. Now the author completes: I) the already
plotted dry-adiabate higher up to the sounding peak altitude,
II) plots the isobar p(h)= const, which corresro.ids to
Card 3/4 the altitude -H which is to be determined for p (h). H

Exploitation of the Stratification-Yethod for the 3OV/'::o-=8-q-=/1q
Forecast of Convective Clouds, Downpours and T-understor=s
is the highest possible altitude, which may be reached
by a rising air volume in t,,!e case of a given stratifi-
cation (or the height of the cloud). The smaller 7 the
higher will be H. The temperatures in the points of inter-
section between the mentioned isobars and the dry-adiabates
and the stratification curve and the wet-adiabate will
Tepiment TC(h): T(h) and T B(h), respectiYely. Thus the
data for.the computation of 4(h) are obtained according
to formula (4). The computation according to the "in--
struction" (Ref 1) takes 20-25 minutes) whereas the here
sug6ested method takes 2-3 minutes. There are 1 figure
and 9 references, 0' of which are Soviet.
Card 4/4

3
AUTHOR:
TITLE-.
Tkachenka, A.V~
S/169/61/0001/0! I/Ca 5
D228/D304
Analysis of the hodograph of the wind veloc.1ty in
the atmosphere7s boundary layer
PERIODICAL: Referatlvnyy zhurnal.9 Geofizikag no. 11, )96;.
abstract 11B237 (Tr. Ukr. n.-i. gidrometeorril, In -,R,
no, 20, 19609 '5 - 13)
TEXT: Taking for the turbulence coefficient (k) the breaking m-.ode!
(k is the graded function of the altitude in the near-surface iay=-r
and the constant value above it), the author writes out a soiutLori
for the system of equations establishing movements for It'he layer
enclosed between the upper borders of the atmosphere's near-8urfa.,.~-
and boundary layers. Under the influence of the thermal hetelyog-~.nt-.
ty of the atmosphere along a horizontal line the horizontal pr,~Ss,j
re gradient changes with altitude; an analysis of the solulli;_-n .!3
given for the case when the pressure gradient is a linear tun,_,t-on
)f -he a'titude. The formulas for the wl2id-velocity component-_:~ are
Oard 1/2

S/169/61/000, ~D
Analyais of the hodograph of the ... D228/D304
then reduced to a form convenient- for constructing a nomogram. Ca.-
ulating +.he parameter8 of the problem (the horlzontal tempet-a-11-jrF
gradient, the coeffic-ient of turbulence, etc.) was
filied by means of an arrangemeat. cons-Lsting of
mend. for conatructing a theore-ilcal hodograph and a nomogram
anallyzing the emp.,ilcal hodograph, (Abstractoris note,. Compj'et~-
0 a r d 2) /' 2

TKACHENKo A.V.
n~~- of a generalized
Method of determining the parameters -95-98 161
exponential lawa Trudy %rITIGAI no,. 26. (14IRL 15:2)
(Winds)

TKACHENKO. A.V.
Determining the cOsffj"ent of turbulence in the uts-tio. r
na, y
horizcntally heteroganeous boundary layer of the atwsphers.
Trudy UkrNIGMI no#4&45-51 165, (MIRA 18s8)

ALEKSEYEVA, AJI.~ TKACILFI'IFO,
jr, caused by cxp~-rz,--,-ntal
Preventive acLion of vi, o,2:39-42 ~,--Ap 165.
Z.IC)I.. 4eksp. terap. 9 n
chronic hypoxia. Pat- (MIRA 18-5)
1, Kafedra biokh!-mtJ- -~ajininskcgo mccli.t.sinskogo Instituta.

KLIMKOVSKIY, B.M.; MAT-KIN, A.S.; T HENKOY A.S.
Modernization 6f the fastening of rolls on mills for the cold
rolling of pipe, Metallurg 9 no.lD28 N 164.
(MIRA 18:2)

OV
f air

c r7p. 'Z' I MriF
7'', (7t-- I z A
p
of the atmosphe-e
CITED SOURCE: Tr. (Per, n.-I. gidrometeoral. in-ta, vy*p. 31, L962, 48-53
V)PIC TAGS w iid, velocit,~, anno3pheric b~-indarv layer-, geostr--.,phic
7'-
ccid 1

ACCESS 'LON A R
of the casps is It POSsible tt2 "se hjs merho' and in the davt "me in s unyre
r when

GAL&MIY, H.m.; MACHMIKO, A.T.
Experimee in detemining the coerfjojent of turbulmoe j.
the boundu7 layer of the al~wophs-ja based on data of uppey,
Wind's Soundbg in o?---,e po:Lni. T~rmdS' no,,3603-39rO
(MIRA 1-,&7)

C"
-- 61 :J .1 7, A T
AUT 110 RKerirtanci-tiova, A. R. llrachec.~-o A.
TITLE: Inureetigation of the wind velocity profile in the lowar 2-m
layer of the vir
SOURCE: K i v a,-r, rain3k L y n ~ u c ',-~ ri o - 'L i so va c it 1 ' s k ii d rome C a o r-
ologicheokiy institut. I ru dy k , no, . 4 1 ; 19 6 4Vaprosy" taplovago t
faaaa (Problems of heat and water balance), 116-125
lvodnogo ba
TOPIC TACS., wind velocftvyj"~Vartical wind velocity, verticzl wind
.velocity profile, atmospheric boundary layer,'boundary-Layer wind
velocity
ABSTRACT: The effect of height, t,~mperature stratification, and the
uneeriving surface on the vertical profile of aeteorotogical elements
t9 In dett!rminflow, the ,rqr~ical turbulent flow of aubstances
in tho gurface. boundary of (-')c atai-aphere. An analyais is made
t q - t i C a 1 'j I rl d- ve 1n rc Files recorded in tne 0-2-m )aver
,jn(i-,- 4e rer.- ra t ure-i , ri z P o n c o t-. (I i t i a n -1 2 6 1 n v e rj I o n a
C a r d I

.L 10,L-U-65
ACCESSION MR: AT4046361
dg
and 93 stable). It ts demonstrated that when pronounced temperature
,strati.fications occur, the relationship between the wind profile
and height is much more complex than is indicated by generalixed
logarithmic, pover, exponeritiai, ,r iniversal laws on the measure-
m e n t om- t e o ro g i i" r I R h a a 13
iASSOCIATION: Ukrainakiy aauchno-isalsebvatel'skiy gidrometeoncylogichasidT
;ingtitat (Ukrain5an 5,cientitic Reeear-~71-
Card 212

TKACHENKO, A.V&
Method of determination of the content of blood In organs
and tissues. Vop. ined. khim. 9 no.101-76 Ja-F 163.
(MIRA
1. Kafedra biokhimil Kalininskogo gosudarstvennogo medit-
ninskogo institutao
17t6)

TKAGHENKO, A.V.
Deiermination of the parameters of the vertical wind
profile in the lowest layer of the atmosphere. Trudy GGO
no.l":22-27 163. (MIRA 17:6)

LAYKH24.U1, D.L.; ORLF11KOt L.R.; TKACHENKO, A.V.
Dispersion of the turbulence energy in the lowest layer
of the atmosphere. Trudy GGO no.144:28-33 163.
(MIRA 17:6)

ORLENKO, L.R.; TKACHENKO, A.V.
Some results of processing and analyzing gradient observa-
tions in the lowest atmospheric layer. Trudy GGO no.144:11-
21 163. (MIRA 17:6)

GALADZHIY, N.M.; MELENTIYEVA, I.I.; TKACHENKO, A.V.
Determination of the height of the boundary layer of the
atmosphere by different methods. Trudy GGO no.144-.96-101
163. (MIRA 17: 6)

TKACHENKO., A.VI.; VOLEVAKHA, N.M.; "ZHIY, N.M.
Analysis of the hodograph of wind velocity in the boundary
layer of the atmosphere. Trudy UkrNIGMI no-31:48-53 162.
(MIRA 16:11)

ACCESSION NR: AT4028748
S/2531/63/000/1"/0096/0101
AUTHOR: Galadzhiy, N. M.; Melent'yeva, I. I.; Tkachenko, A. V.
TITLE: Determining the altitude of the atmospheric boundary layer by'various
methods
,.SOURCE: Leningrad. 01. geofiz. observ. i. Ukr. n.-i. gidrometeorol. inst. Trudy*,
no. 144/40, 1963. Fizika pogranichnogo sloya atmosfery* (physics of the atmospheric
boundary layer); Dneprovskaya expeditsiya GGO i'UkrNIGMI, 96-101
TOPXC TAGS: boundary layor, temparatura sounding, wind sounding, Dnieper expedition,
wind profile
~.ABSTRACT: In this paper the authors present results of determining the altituda of!
i. i
"the boundary layer of the atmosphere according to temperature and wind sounding
1~data during the Dnieper expedition. Formulas are derived which enabled the authors
to plot the altitude dependence of the dynamic boundary layer on an x-value. The
haracteristics of the atmospheric boundary layer, according to the Dnieper expedi-;,
c
.tion of 1961, are given in a table. The around-tbe-clock change of,the boundary
layer is plotted according to the derived formulas and is compared with the
C6-r8. 1/2

ACCESSION NR: AT4028748
experimental data. Orig. art. has: 2 figures, 2 tables and 11 formulas.
ASSOCIATION: Leningradskaya glavna geofizicheskaya observatoriya (Principle
Geophysical Observatory of Leningrad)
SUBMITTED: 00 DATE ACQ: 164pr64 ENCL: 00
:SUB CODE: AS, HH NO REF SOV: 004 OTHER: 000
CcWd 2/2
...............
-----------------------

TKAGHENKO, A. V.
Determination of the coefficient of turbulence in the
surface layer of the atmosphere. Trudy UkrNIGMI no.31:
36-39 162.
Determination of the coefficients of turbulent viscosity
in the boundary layer of the atmosphere. 40-47
(MIRA 16:11)

ACCESSION NR: AT4018985 S/2599/63/000/036/0033/0039
AUTHOR: Galadzhiy, N. M. ; Tkachenko,, A. V.
TITLE: Experience in determining the turbulence coefficient in the atmospheric boundary
layer on the basis of data from wind sounding at a single station
-1. gidrometeor. institut. Trudy*, no. 36, 1963. Voprosy*
SOURCE: Mev. Ukr. n.
fiziki at3nosfery* (Problems in atmospheric physics), 33-39
TOPIC TAGS: meteorology, turbulence coefficient, atmospheric turbulence, wind, weather
forecasting
ABSTRACT: The method for determining the turbulence coefficient k in the atmospheric
boundary layer on the basis of data from wind sounding at a single station has been described
earlier (Tr. UkrNIGMI, No. 31, 1962). Investigations were made at Krivoy Rog in the
winter of 1961 to determine the validity of the method. Empirical data indicate that begin-
ning at some height h (100-200 m above tho earth's surface) the turbulence coefficient
changes little with height z. For z>/ h it is assumed that k(z) = const. Undor these con-
ditions and assuming that the velocity of the geostrophic wind and acceleration are linear
functions of height, the method proceeds on the basis of Laykhtman's equations of motion:
a co-s S I ~ L;) !-(A. +zBy)
'V.
Cord 1/3

ACCESSION NR: AT4018985
Where u, v are wind velocity components, AX) Ayj Bxj B~l CXJ C y are unknown constant
t
values, functions of velocity of the geostrophic wind at he earth's surface, characteristics
Of the thermal wind; -A is a value related to the turbulence coefficient by the relation
6; sin Cip
k (2)
A 2
wherew is the angular velocity of the earth's rotation, ~O is latitude of the place. The prob-
lem of determination of k requires finding of A. Two computation schemes from the earlier
paper are presented, of which one is not recommended, and a new scheme presented; both
are suitable for determiningA and k. A total of 228 soundings were made; a wind velocity
hodograph and a graph of the sums of distances between points were constructed for each
case. Only 75 cases satisfied the criteria set by the authors. The value'X was determined
in each case using the three computation schemes presented. The determined turbulence
coefficient ranged from 1 to 50 M?-/sec. Changes of k are caused primarily by its depen-
dence on the velocity V of the geostrophic wind and the vertical temperature gradientT
Orig. art. has: 15 formulas, 3 figures and 1 table.
CO rd 2/3

'ACCESSION NR: AT4018985
ASSOCIATION: Ukrainskiy nauchno-issledovatellsldy gidrometeorologicheskiy Institlit,
Kiev (Ukrainian Hydrometeorological Scientific Research Institute)
SUBMITTED: 00
DATE ACQ: 27Mar64 ENCL: 00
NO REP SOV: 006 OTHER: 000
CGrd 3/3

ACCESSION ',17R: AT4028738 S/2531163/000/144/CG2210027
AMMOR: Tkachenko, A. V.
TITLE: Determining the parameters of the vertical wind profile in the surface layer
of the atmosphere
SOURCE: Leningrad. Gl. geofiz. observ. i Ukr. n.-i. gidrometeorol. inst. Trudy*,
no. 144/40, 1963. Fizika pogranichnogo sloya atmosfery* (physics of the atmospheric
boundary layer) ;'Dneprovskaya expeditsiya GGO i UkrNIGNMI, 22-27
TOPIC TAGS: wind profile, surface layer, exponential law, Dnieper expedition
ABSTRACT: In this paper the author describes the method of determining the parameters
of the vertical wind profile in the surface layer of the atmosphere, approximated by
the generalized exponenz;ial law. The analysis of the Dnieper expedition gradient
observations has confirmed that the distribution of wind velocity u and the surface
14yer of the atmosphere can be approximated with,sufficient accuracy by the &xponen-
'.,,a
3' 1 function of the altitude z which expresses the known generalized exponential
t
law of D.1. Laykht-an
U
U Z ZC (Z Z0)
'1/2 1 0
C.rd,

ACCESSION NR:' AT4028738-
or z
u - u, (2)
where u1 is the wind velocity at a certain fixied altitude zl, c is the stability
parameter, ZO is the roughness parameter. Through a series of-mathematical argu-
ments, the author defines the various parameters of the wind profile and presents
them in graphs. A comparison of the values of the stability parameter is presented
in a table. There is basis to recommend the described method of determining the
param'eter of the wind profile-for practical use in the analysis of gradient obser-
vations of the surface layer. Orig. art. has; I table, 3 figures, and 21 formulas.
ASSOCIATION: Leningradskaya glavna geofizicheskaya observatoriya, (Principle
Geophysical Observatory of Leningrad)
SUBMITTED: 00 DATE ACQ: 16Apr64 ENCL: 00
SUB CODE: AS, YM NO REP SOV: 001 OTHER: 000
Card 2/2

ACCESSION NR: AT4028737 S/2531/63/00011"/0011/0021
AUTHOR: Orlenko, L. R.; Tkachenko, A. V.
TIME: Some results, of the processing and analysis of gradient observations in the
surface layer of the atmosphere
SOURCE: Leningrad. Gl. geofiz. observ. i Mr. n.-i. gidrometeorol. inst. Trudy*,
no. 144/40, 1963. Fizika pogranichnogo sloya atmosfery* (physics of the atmospheric
boundary layer); Dneprovskaya expeditsiya. GGO i UkrNICMI, 11-21
TOPIC TAGS: gradient observation, atmospheric sutface layer, turbulence, wind
profile, heat flow, moiqture flow, energy balance
ABSTRACT: The authors examined the results of processing and analysis of gradient
.observations in the surface layer: wind profile parameters, components of the
I
erjergy balance of turbulence, and the turbulent flows of heat and humidity. ~Pradient
observations, conducted during the Dnieper expedition, on wind velocity, air
temperature and humidity, enabled them to produce vertical profiles of these meteor-
ological elements and, after appropriate processing of the data, to obtain important'
characteristics of the surface layer as the coefficient of turbulence, the components
of the energy balance of turbulence, and the turbulent flow of heat and humidity.
Card 1/2

ACCESSIO' N IM: AT4028737
The method of determining the parameters of vertical wind profile, in order to cal-
culate the magnitudes of the above mentioned componentu is described. The turbulent
flow of heat and moisture are presented in graphs. Toward the end of the period
an evaporation decrease and an increase in the turbulent flow of heat is observed.
However, an increase in evaporation is sometimes observed. Through a series of
mathematical arguments, the authors derive the components of the energy balance of
the turbulence; these ari plotted in graphs. Orig. art. has: 6 figures and 22
formulas.
ASSOCIMON: Leningradakaya glavna geofizicheskaya observatoriya (Principle
Geophysical Observatory of Leningrad)
SUBMITTED: 00 DATE ACQ: 16Apr64 ENCL: 00
SUB CODE:, AS NO REP SOV: 006 OTHER: 000
Card, 2/2

VOLKOVITSKIY., G.I., dotsentp kand. tekhn. nauk; PISHCHIKOV, G.P., inzh,;
YUFEROVY V.M., dotsent, kand. tekhn. nauk; DZYUBA, M.I., inzh.;
SAY, IT.F., inzh.; Prinimali. uchastiye: SURZHIKOV, V.A., inzh.;
KOVALEVAJ, A,D,, inzh.; TKACHENKO, A.V,,, inzh.; KIRVALIDZE, H.S.,
inzh.; GLADKIKH, D.V., 'rrizE.'j 'YES-A-ULOV, A.T., inzh.
Characteristiou of producing large-diameter pipe of Khl8Nl2M2T
0
steal. Stall 22 no.6:532-535 Je 162, (MIRA 16:7)
1. Yuzhnotrtidnyy zavod (for Surzhikov, Kovaleva, Tkachenko,
Kirvalidze, Gladkikh Yesaulov),
(Pipe., Steel~ (Rolling(Metalwork))

S/599/C-2/OW/031/003/006
A0661A,126
-AUTHOR., Wachenh~o----A-_
TITLE, A contribution to the problem of determining the coefficient of
turbulence In a ground layer of the atmosphere
SOURCE: Kl~ev. Ukrainskly nauchno-issledovatelLskly gidrometeorologiche-
skiy institut. Trudy, no- 31, 1962. Voprosy fiziki atmosfery, 36
39
TER. Investigations by D.L.Laykhtman have Bhown that in a ground layer
of the atmosphere the coefficientof turbulence k varier, with height according to
the law.
k ki
ZI
~hero k, is the value of k at a height zj, and e is the parameter of stability.
ki is given-by
26
%2u, E.- ZI
0
k (2)
_)2 (ze z I-;
Card 1/2

-3/599/( J103110031006
A contribution to the problem of determining ..... Ao66/A126
where vt - 0-38 is a universal constant, zc; is the parameter of roughness, and
Ui is.the wind velocity on the level zj. A very simple method is proposed for,
calculating 9 and k1. Equations (1) and (2) are transformed into
X2 + er 2
k1f
P
and
k - k, z (12)
1 ZO I
where k' is referred to z I m; r- f (no, 6) n' n
1 0 Tj p
Ul The ca IIculation of kj requires the knowledge of I E p.. r. a and
7- n~)
z1. The method suggested here is based on a graphic evaluation of.wind-velocity
measurements at various heights, using the function
p (ui ul) f (nj, S). (13)
There are 3 figures.
Card 2/2

3/599/62/000/031/004/006
A0661AI26
AUTHOR: Tkachenko, A.V.
TITLEt Determination of the coefficient of turbulent viscosity in a bound-
~ary layer of the atmosphere
SOURCE., Kiyev. Ukrainskiy nauchno-ii3sledovatellskiy gidrometeorologiche-
skiy institut. Trudy, no. 31, 1962. Voprosy fiziki atmosfery, 40
47
TEXT: An attempt is made to determine the coefficient of turbulence k
without using charts. or apecial means. The a%athor proceeds from the fact that
from an altitude h (100 - 150 m) above ground upward the coefficient of turbu-
lent viscosity remains constant. Hence, k (z) - const for h,4 z 4-- H, where
H is the height of the boundary layer. The equations of motion in z 4 h 4 H
have the form
du
Tt k
z2 + IV Pax
dv 12v .1
Ft k . .... lu -
2
Card 1/4 dz 9 Y

S/599/62/000/031/004/006
Determination of the coefficients of .... Ao66/A126
For the case of a steady flow and if and are linear functions of z,
ax ay
the equations of motion can be written as
U. e- (C x Cos X z + C,,5in ?,z) (Ay + zBy)
(2)
v e- %Z (C y Cos z CX sin Z) + (Ax + ZBX)
where
(3)
"A X, BX,yl and Cx,y are constants. The following problem is now to be solved:
~If T~e vertical wind velocity distribution is given in the form of a hodograph,
ich is assumed to satisfy Equations (2), then it is possible -- determine k
A Wo
from The equations of motion are represanted in the form
u CO (1 - e". %z1 Cos ZIB~r (6)
%2I
V, CO e sin z' z Bx
where XZO
90 C e (7)
Card 2/4

S/599/62/000/031/004/006
Determination of the coeffici(~nt of A066IA126
..by a transformation of coordinates. Here, ut u U0, vy , v - VO, Zr Z
z0; UO and. vo. are the wind velocities at the height zo. Three points of
the hodograph (Fig. 1) are chosen and expressed by the following equations:

--VIP
P 12 +
q~
n
2 12 t2
..
W'U -
+ V

8)
q
2 2 2
+ (v.' vi,
r, (U. U')
Sn ~is given by
sn CO (I (n, A),
where
_V(X" nX,)2 + /y
n., nyl)2
n
n
Xn 0- cos An
e sin An
Yn
Card 3/4

TKACffENKO, A.Yed,-, inzh.
Machines for planting and harvesting sugar beets. Mashinostroenie
no.2:93-98 Mr-Ap '62. (MIRA 15:4)
1. Ukrsel'khoztekhnika.
(Sugar beets--Ifarvesting)
(Planters (Agricultural machinery))

TKA.CHEjNKn,, A.Ye.. inzh.
Speed up the development of more efficient agricultu--al machinery.
Mashinostroenie no-3:87-89 My~Je 162. (MML 15:7)
1. Ukrsellkhoztekhnika.
(Agricultural machineryk---Technological innovations)

TKAGHE-IIKO-,,-A-Ie~Be7--lefi.moyieh; KARPE11KO, Sergey Aleksandrovich;
'~ORONEZHSKIY, V.I., inzh., retsenzent; PILIPENKO, Yu.P.,
inzh., red.; GOnOSTAYPOLISKAYA, M.S., tekhn. red.
(Machines for the over-all mechanization of field crop cultiva-
tion] Mashiny dlia kompleksnoi mekhanizatsii rabot v polevod-
Ave. Yoskva, Gos. nauchno-tekhn.izd-vo mashinostroit. lit- P
1961. 128 p. (11TRA 15-27
(Farm mechanization)

TKACIEUKO, A.Yo., rod.; 'MIEUU, S.I., red.; KAVIMIlWIIKO, L.A.,
-zh. -'. a VIM. ra d.
[Inventions and improvements in a-Ticultural machinery;
a collootlon of Ukraininn invontore nnd innovntorol Izobro-
teniia i usovershonstvovanila v sellokokhozinistvonnoi
tolclinike; abornik predlozhenil izobretatolei i ratsionili-
zatorov Ukrniny. Kiev, Goe.izd-vo sellkhoz.lit-ry. No.2.
1958. 295 P. (MIM 12: 10)
1. Nachallnik Upravloniya novoy teklmiki i izobretntellstvn
Ministerstva sellsko.-o khozynystva USSR (for Tkachenko).
(Agricultural machinery)

TKACHENKO, Aleksey Yefimovioh.[Tkachenko. O.IU.]..iuzh.; NATANZON, I.I.,
------- -;.-.. kanditekhn.nauk, otv.red.; GURWO,.V.A, (Hurenko, Y.Aj, red.
(Mechanization and electrification of agriculture in the
Ukraine during the seven-year plan] Makhanizataiia i elektry-
fikatsiia sillslkoho hospodarstva Ukrainy v semyrichchi. Kyiv,
1960. 39 P. (TovBryetvo dlia poshyrannia politychafth I nauko-
vykh znan' Ukrainalkoi RSR. Ser.6, no.8). (MIRA 13:7)
(Ukraine--]Zlectricity in agriculture)
(Ukraine--Farm mechanization)

, - I 1 1, ,
. - . iL. ~ . ) . - .1
1 -1 12
mect-.anizatim c1f fe~rL-i lizer !'a-,h-,nostrcenfe --~.3: -`~
'11---Je tAi ( ~, !.-~ 1 ,, : I I "
,j

MiCHEtIKO, B,.; ISAKOV, V.
Increasing the reliabllit,-- of -'U-he 1'stvorll-type 2cc~-.-,-cr-by--adar
Sta'Ldon, *ior- -"lot 21 no,9:20-21 3 161~
(llu~dar in navigution)

TKiWENKO, b.
Moving as entire building from one place to another. p. 26.
(Izgradnja, Vol. 11, No. 2, Feb. 1957, Beograd, Yugoslavia)
SO: Monthly List of Fast European Accessions (EPAL) Lc. Vol. 6, No. 8, Aug 1957, Uncl.

LETEDFS'S, V.A.~ TKA`-'dEN-K0-, B.,I.
Tr,atrr.,,n,, OIL* ilare'lip in rl.,~-j.~Idren. Ta,zn. !:,.~:d.
iz 4afedry go~.piLF,~ ~n)y khl.r,u-!-gi i.
~zav. - prof. 11.Z. lllouakov'
Tadzi-O-Kskogo illStit,LlLa Alinetai Abual-i

comb :r,,td tre a c-~ ~i f, T.C. a L o~ - Ir;-'I I y.-iF. ;,;a I-J. 0
ric,(193 2,r, Karen. Pr li,-iy Ta.-; ra" .n,- t. 51,
WHIA 1.7~8)
A Z kali--,iry g
j, kafedry b. (Zaj. dokt.r)r nae~i. nallk
B.h. fia~thmawvl% .k-venno&-, uied-Lts-,risk~,go ins"ILYIa
imera Abua!L

IMSHNIKOV. A.P*;.
Technic of preparing a capron net for alloplast7. Zdrav. Tadzh. 6
no.6.-40-43 159. (MMA 13:4)
1. 1z kafedry gospitalluoy khirurgii Nav. - prof. N.Z. Monakov)
Stalinabadskogo medinstituta im. Abuali ibni Sino.
("WN-THERUZUTIC USM) (PLASTIO MWXRY)

TKAGWIMIM, B. 1.
Analysis of the meebanIms of decrease in arterial pressure
in myocardial ischemia. Kardiologiia 4 no-4:16-23 JI-Ag7l 64
1. Otdel obahchay fiziologii imeni K.M. Bykova (zav. - prof.
A.T. Rikklt) Instituta eksperimentallnoy meditain7 (direktoi-
deystvitelinyy chlen AMN SSSR prof. D.A. Biryukov) AMN SSSR,
teningrad. Submitted September 24, 1962.

TKAGRENKO, B.I.
Reflex changes in brain blood sun-ply reBulting from action on
coronary vessels. Fiziol.zhur. 50 no-4t487-495 Ap 164. (MIRA 1824)
1. Otdal obshche7 fiziologii imeni akademika K.M.Bykova
Instituta eksperimentallnoy meditsiny AMN SSSR, Leningrad.

TKAC Of BeIa
- _j=
Characteristics of the reflexes from the endocardial recep-
tore Of the right half of the heart; problems of the existence
of the Bainbridge reflex. Dokl. AN SSSR 154 no.4:994-997
F 164. (MIRA 17:3)
1. Institut eksperimentalinoy meditsiny AMN SSSR. Predstavleno
akademikom. N.N. Anichkovym.

AUTHOR: Tkachenko, B. I. 2o-119-3-63/65

TITLEi . . . . ............ _,
Modification of the Cardiac Output and the Indices of the
Vascular Tonus in Experimental Hypertension (0b izmerariyakh
minutnogo ob"yema serdtsa i pokazateley tonusa sosudov pri
eksperimentallnoy gipertenzii)
PERIODICALs Doklady Akademii Nauk SSSR, 1958, Vol- 119, Nr 3,
pp. 617-62o (USSR)
ABSTRACTs It is generally recognized that in the mechanism of the con-
tinuously raised blood pressure (illness of hypertonia) the
tonus increase of the arterioles with a subsequent (seconda-
ry) reduction of activity of the heart is determinative (Ref
1-3)- But a very divergent course is also possible (Ref 5-7,
9-11). At the same time the author investigated the cardiac
output and the systolic volume of the heart together with the
vascular tonus in the formation and development of anvarying
modifications of the blood pressure with 6 dogs which had a
pituitrin, renal- and reflexo6enous experimental hypertension.
1. Experimental series . It Yras ascertained at 3 dogs that the
modifications of the vasculai*onue and of the activity of the
Card 1/3 heart with continuous rise of the blood pressure under the.in-

. Modification of the Cardiac Output and the Indices of the 2o-119-3-63/65
Vascular Tonus in Experimental Hypertension
fluence of an introduction of pituitrin lasting for a long
time (Ref 14) can be different. II. Experimental series. After
a considerably long time after the standardization of the blood
pressure a renal hypertension was caused in the same dogs by
ex5lantation of both kidneys under the skin of the back (Ref
15 . The modifications of the heart and the vessels were of
difforent kind with ainglo animalo. III. Experimental series.
At 3 dogs, which already had an experimental "reflexogenous"
hypertension, experiments with introduction of hexone or in-
crepArle were carried out. On the basis of the results the
author comes to the following conclusions: 1) The rise of
blood pressure in an experimental hypertension with dogs apart
from the modification of the vascular tonus can be condition-
ed by the modification of the cardiac output as well as of the
systolic volume. 2) The amount of the rise of blood pressure
is predominantly cbpendent from the degree of modification or
from the tonus of the vessels or from the cardiac output or
from both of these functions. 3) The reduction of the blood
pressure by application of hexone is mainly accomplished at
the expense of reduced cardiac output and of the systolic volu-
meme of the heart. When introducing hypotomic GASK this takes
Card 2/3 place at the expense of the tonus reduction.

Modification of thepardiac Output and thepndices of the 2o-119-3-63/65
.Vascular Tonus in Experimental Hypertension
Therefore it has to be taken into consideration which funct-
ional parts of the cardiac vascular system are of higher
importance in the actual continuous rise of the blood preasu-
re. There are 3 figures and 15 references, 13 of which are
Soviet.
ASSOCIATION: Institut eksperimentallnoy meditsiny Akademii meditsinskikh nauk
SSSR (Institute for Experimental Medicine of the Academy of
Medical Sciences of the USSR)
PRESENTED: December 4, 1957, by K. M. Bykov, Member, Academy of Sciences
USSR
SUBMITTEDt November 28, 1957
AVAILABLE: Library of Congress
Card 3/3

_
Characti3riotien of corwriar-I Fiziol, zhur. 49
no.11:1360L-1368 N 163. (IIIRA 17.8)
1. Otdel obslichey fiziologii ilneni akadwaika K.M. aykova
Instituta eksi.,erimentallnoy mieditsiny X-~l SSSR, Leningrad.

FACERPTA Y'.-DICA See 2 Vol 12/1 Physiology Jan 59
30.
RPLATIONS1111' BFTWFEN CARDIAC AND VASCULAR FUNCTIONS IN
AL-1-FRED BI.(X)D PRESSURF IXVELS
Tkilr'rhenko Ii, 1. Lah. or Cir(ulation and Hemp_ Dept, of('e?Wral
llhy~rbl_ Inst. of Exp. %led., I.vningrad
(348-355) Graphs 4
Arterial and venous bluod pressuve. vasckilar toite, determined by Arinchin's
I)Ioudless method (Fiziol. Zh, SSSI( 195.1, 40, 480),cardiac output and stroke
volunic detertnined by the acetylene method of Grollman-Snurnov were investigat-
ed in dogs with arterial hypertension, produced by dailv pituitrin injection over a
period uf 3 to 4 weeks. The rise of blood pressure depends on increased cardiac
output. as well as on a rise of vascular tone. Without change in cardiac output
blood pressure increases moderately only, or may even be lowered, due to .1 de-
'crease in cardiac output. The increased blood pressure can be lowered by hexo-
nium duc to reduced cardiac output or by hypotonin due to reduced vascular tone.
Simonson - Minneapolis, Minn.

TEA CHMKO, B. I.
Functional relation between cardiac and vasculBr activities In dogs
with altered blood pressure levels. Fiziol.zhur. 44 no.4:34*8-355
AP 158. (MIRA 11:4)
1, Laboratoriya kravoobrashchenlya I dykhantya Otdela obahchey
fiziologii Instituta eksperimentallnoy meditsiny A1,411 SSSR,
Leningrad.
(BLOOD PRESSURE, physiology
off. of variations on heart funct. & vase. tone in dogs
(Rua))
(HEART, physiology
output & stroke volume, off. of variations In blood
pressure in dogs (Rua))
(BLOOD VESSELS, physiolcM7
tone, off. of variations in blood pressure in dogs (Rua))

TKACHENKO, B.I.
Reflexes from the angioreceptors of the extremity. Fiziol.
zhur. 1+8 no.4:480-485 Ap 162. (MIRA 15:6)
1. From K.M. Bykov's Laboratory for General Physiology,
Institute of Experimental Medicine.. Leningrad.
(EXTREMITIES (ANAT%[Y)--BLOQD SUPPLY)
(RE FLEXES) (IORT)

TKACHEIZO... B. I. . -
Changes in the cardiac output and vascular tonue in experimental
hypertension, Dokl, Alf SSBR 119 no-3:617-62o Kr 158. (KIRA 11:6)
1.Institut eksperimentallnov meditsin7 AMN SSSR. Predstavleno
akademikom K.M. Bykovy-m.
(HMRT111SION) (CARDIOVASCULAR SYSTEM)

TKACIiP.-KO, j.I., cand Vied 3ci -- (diss) 110n t*V-
functional interrelations of wie volume of
heart and tontis of' Lhe blood ve,.sels in sUend-I
51
changes in the level of arterial prettiure in dogs
,.,,,ith ex.rerimental ftyrertension." Len, 1T)'11, 17 pt)
(Acad Med 6ci USSTZ. Inst of Ex nerimental t.'ed;cine.
1- A
Laboratory of Blood ~,irculation and &es iration)
20() =lies M, 29-58, 1~8)
- 132 -

TEACH.E.NKO, B. 1.
Kethod of determining cardiac output in doga. Fiziol.zhur. 45
no,1:114-116 Ja '59. (MIRA 12:2)
1. From the Laboratory of circulation and respiratiolL department
ip
of general phvsiolog7. Institute of Experimental Medicine, Leningrad.
(ERART, phy8iol.
minute volume, determ. In dogs (Rug))

TKACBU,,IKO,, B.I.
Analysis of reflex changes in the cardiovascalar syste-m. during
the stimulation of pe-ricardial chemorecep't',ors. Report no.2z
Role of the heart and different vascular areas in the origi-
nation of pressor reaction. Biul.eksp.biol. i med.55 no.1:
1-2-17 ja'63. (14IIL4 16:7)
1. Iz laboratorii obshchey fiziologii imeni, K.M.Bykova (zav.
prof. A.V.Rikklt) Instituta eksperimentallnoy meditsiny (dir.
deystvitellnyy chlen A14N 88SR D.A.Biryukov) AMN SSSR, Lenin-
grad. Fredat~~Iena deystvitellnym chlenom Al-91 SSSR P. S.
Kupalovyia.
(NICOTINE-PHYSIOLOGICAL EFFECT)
(PERICARDIU14 INNERVATION) (BLOOD PRESSURE)

TUCHENK0. D. I.
Correlation of depres3or and rre-sr,.- react,4~,-v 5rr~djce`
acetylcholine. Diu!. eksp, b~'o_!. *L med. 556 D
(1,111RA I 1': 1.1 )
1. Otdel obshchey fiziol-()Fii imen-I Rykova (zav. prof. A.V.
RIVk1') Instittita akspor'Lmontal'noy moditsiny (dir. - deyst-
vitellnyy chlen ALTI SSSR prof. D.A. Biryukov') Aill'! SSSR, Lenin-
grad.

TKACHENK09 B.S.; DEREGA9 E.V. (g.Kupyanksy f1ar1kovskoy oblasti)
Assistance from the medical school to public health organs as
one of the forms of relating teaching to daily life. Felld.
i akush. 26 no. 1:54,56 Ja 161. (MIRA 14:2)
(PUBLIC HEALTH)

TrACHINO jjtL._WKIN, M.I.; DIMOKIDOT, r.K.; TAXAR, V,A.; GROZDIIoOV, A.L.;
Te.Lo'; STRIMOV, S.A.
aeolegy of the northern part of the Central Siberian Fateau.
Trudy Wanch.-isel. inst. geol. Arkt. 81:133~-242 157. (MM' 11:5)
1. Sot-rudniki inptituta geologii Arktiki.
(Central Siberian Platean--4eology)

TIACIMIKO, B.V., kand.gool.-minerfil.nauk, nauchnyy rod.; DIA15W. G.&..
-a hohiy red.; GBIRIADIMA. I.M.. tekhn.red.
[Stratigraphy of Sinian and Canbrian sediments in the north-
eastern part of the Siberian Platform] Stratigrafiia siniiskikh
i kembriiskikh otlozhenii severo-voBtoka Sibirskoi platformy.
Leningrad, Gos.nauch.-takhn.izd-vo neft. i gorno-toplivnoi lit-ry.
Leningradskoe otd-nie, 1959. 210 p.' (Leningradl.Nauchno-iseledovatell-
skii institut geologii Arktiki Trudy, vol.101) (IMU 1228)
(Siberian Platform--Geology, Stratigraphic)

1,11%RKOV,F.G. and UU.CHEITKO, B.V.
"Paleozoic of the Smriet Arctic. "
re.port presented at the First International Symposium on Arctic Geology, Calgary, Canada,
11-13 Jan 196o.

-V al 1, t-.:,
Lower
Iji
r i a r d
'71' , I
v "j
N7,
t L
k I

GORPSETEYN, D.K.; GUDKOV, A.A.; KOSOLAPOV, A.I.; LEYFTISIG, A.V.;
MELINIKOV, V.I-'.; MOKSHATTS7E, K.B.; FRADKD1, G.S.; UE-KiSM,
N.V.; TROFMIUK, A.A., akademik, nauchn. red. vyp.; ftOZ'rTGV,
I.S., glav. red.; KOBEELYATSKIY, I.A., zam. glav. red.;
SHATALOV, Ye.G.,, z.--. glav. red.; BONDARFNKO, V.I., red.;
GRIEIiERG, G.A., red.; YEIDVSKIKH, V.V., red.; RUSANOV, B.S.,
red.; M01OV, G.T., red.; TKACHUKO, D.V., red.; KALADTAROV,
A.P., red.izd-va; GUMA, A.P7.--,f-Ah6-.--f6d.
[Basic stages of the geological development and prospects for
finding oil and gas in the Yakut A.S.S.R.] Osnovnye otapy geo-
logicheskogo razvitiia i perspektivy neftegazonosnosti IAkut-
skoi ASSR. [By] D.K.Gornshtein i dr. Moskva, Izd-vo All SSSR
10,63. 238 P. (MIRA 16:12)
(Yakutia--Petroleum geology)
(Yakutia-Gas, Natural-Geology)

USSR/Forestry - Forest Culturesh K-5
Abs JoDr: Ref Zhur - Biol., No 19, 1956$ 86889
Author : Tkact4ZS~qj,A*__V.
Inst i Ukrainian Scientific-research Institute of
Forest Management and Agricultural Forest
limelioration
Title The Dependence of Oak Growth on tho Number of
Oaks and on Their Distribution in Plots
Orig Pub- Nauchn, Tr.-Ukr. n,-i. in-t, les. kh-va I agro-
lesomelior., 1956, vyp. 18) 67-70
Abstract: In the experimental sections established in 1950
in the Trostyanetskoy forest (Ulcrainian SSR)., the
effect of group distribution and plant-Ing density
in holes on the growth of oak was explored. During
the four years up to the installation of the cultu-
ros, cultivated crops were raised in the uprooted
clearing. In the first vegetative period, the oak
Card 1/2

USSR/Forestry - Forest Cultures K-5
Abs Jour: Ref Zhur - Bibl,i No 19, 1958o 86889
Lbstract: grew equally well in all variations of the
experiment in row and bunch plantings and in
holes. Beginning with the third year.. the
planted oak grew beat in the row cultures. In
the clusters, the oak grew better when 10 acorns
were placed in the spot, worse when the sowing
was denser. Under the conditions of the left-
bank forest-steppe of the Ukrainian-SSR.0 mixed
row cultures of oak are recomraended, the mixture
being made up of pure rows., rings or squares. --
L. S. Lesina.
Card 2/2
28

ANGARSKAIA., M.A. [Anharalka, M.A.]; BEZRUK, P.I. (Bezruk, P.H.h TYrACHOKO. D.A.
Pharmacological propertlen of the card-Jac glycoside A.,
Farmatsev.zhur. 20 no.1:77--79 165. (1.9 RA 18! 10)
1. Laboratorip sksperimentallnov farmakologil Khnrlkovskogo
nauchne-issledovatel'sko~,,o ICnimik(,--farmatsevtic-.he5lcogo instituta.

LESIK, Boris Vasillyevich; TKACHMO, Dmitriy Filippovich
(Hemp grower's handbook] Spravochnilc konoplevoda. 2., perer. i
dop. 12d. Moskva, Goe.12d-vo selickokhoz.lit-ry, 1958. 191 P.
- (Hemp) (MIRA 12:4)