SCIENTIFIC ABSTRACT ORLENKO, G.P. - ORLICZ, M.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001238210006-8
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: January 3, 2017
• Document Release Date: June 21, 2000
• Sequence Number: 6
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

SOV/30-50-6o-5/10
AUTHOR: Laykhtman, D. L. and Orlenko, G. P.
TITLE: Intensity of Turbulent Exchange Over Water (Ob intensivnosti
turbulentnogo obmena nad vodnoy poverkhnost'yu)
PERIODICAL: Trudy Glavnoy geofizicheskoy obeervatorii, 1956, Nr 6o, Pp 51-52 (USSR)
ABSTRACT: An important indicator of turbulence over water surface is the ver-
tical coefficient of turbulenft which is a factor in all formulas for
cmputing thermal stromi, humidity, etc. This coefficient was cal-
culated fram parameters characterizing the distid-bution of diffusive
substances. The paxameters were secured in 54 experiments. The ar-
ticle contains 1 diagram. There are no references.
Card 1/1

075/007W
on
46t
N.; Orledco, C. pis sly so
Aurmit raddon

729U
-**twd.-fbr vulawkisift butadi~ ldtipl"l'mwAbbw.
Clan
&
.
-76
toOsimy md m* 14 MS 75
I~Jwt butadi~ sitrUe 24abbw syftbatle rd&w
701PICIIIAGS: im

DSTAMi, We i :ftr volowd buts"On
Af
ghwes cut -ties" SLOg
A" of M: accaell"re The
77-
-to redowd : %:*ihivmmVwtAW ty-ofAbs vulconi

*alsom as the a@-
usift ai'oompomd ot,usta3m idth"mmiable
082amter-

OMI :00
VA 0=1 W

go. Mr! oW 000 arm

ORIMMO, L.P.
"WAPnee of heat flow into the sail on ground surface te"ra-
ture. Meteor. I gidrol. W.7:30-32 JI '57. (aft lot8)
(soil te"rature)

.;()V/l 39 - t,_ ',//29
AU'PhORS: Orlenko, L.-P-. -and StanyuKovich, E,P,
.PlTa: Shock Waves in Solids (Udarnyye volny v tverd,/Ai,
Pr;rdOD1,~AL:Izvestiya Vysshik-h Uchebnykh Zavedeniy, Fizika.
19589 Nr 6, pp 14-24 (USSR)
A_,~-RAOT: A theory is presented of tue propagation of sY.,oc,~
waves in solids; a relation between instantaneous
pressure and deformation is deduced and tl-.e
corresponding wave and particle velocdties CDMPIAC-d
The basic equation of propagation in one dimension 13
au + ~~k 0, ~u ~V
at ah Ir-) h'Z~t
Here u denctes tht: particle velocity. v sp
volume (V 1/p., wilere density) and L tne
co-ordi-nate; t; and p denote time and pressun~
respectively WriTing a for tension and F tcr vol.-arue
strain (i..e . caangi.~ in voiume. per uni-c iriitiaI
the follow-,.ng relations are obtained:
a b, F- = E - vo
Ca rd 1 /4 VO

Shoc.K i~aves i-n Ll'olidsr
7,Cl-
Here vo sibui-fies the initai value ol ,r,
PO si fy the densities abso~.iate-q wi,11. ~r :,L-A
v = lxf~ and vo = I/f'o re.3pect-_vely 6 11 b q , 1 T, UI
.r,q (2) inio Eq (1) yields tiie following relai icu-
4U 200 do ;3E u, -A E r
.- = 'Jul
at 3h C_ Yh
If -Llie nelat:ion between a and ~ is kn-)v,,n iL
form. tl.Le!z~e ias'- E.,quat-ioi-s elia.,le trie shod-? w.-ge
velocity tc be deduced A relati,3n w1ii-A.
agi,eement witi. ex1,_)er_,.jiieni is:
CY Go z -A ( c - c 0 )7) (4)
Wrie re 00 E;C, are inltial values 01" 0~ E ar,,i A
re''-ated to -ciie elasti,_, pi-opt-r-tit:~s of tiie
shock-wave velocity ~., absocclated witi, tiiis rel:_:i
between a and is readily 61~o-,An to te ~-_p%-. -i 'by:
0
r7c
OTC
/% + 2
Ca rd 2 /4

Shock ,aves in -ciads
and the correspond,.n~; particie velccity w i~i
A
w F3_ I.
Po
Po to + F- 0
I P
ilhe theory is used to discuss tne case in wilict., tie
initial disturbance iies outside trLe medium, the exaia-,)Ie
caosen beijig tiiat of an explosive charge detonated aC
a he i ght At- a,bove a plane boundar-j of the mediam. e
pre s sure p, at any time, t after the explosion i.,.
case foiiows a power law given by
p PC Ir- -) 3n (1,29)
PH Po +
.-'ere P,, 1S -,:lie val~;.e of n - 0 and t 7 0
PC. and ii are eiapii-ical con:Aants and , is a
ci,aracteri~,ti.c time t/D wnei~(. ;) is ti-,,e detom',ion
velocl'.y Cno nuiueul,ui results are giveli L11
lard ~/4 with tais exam Ile bui. -it would presumaljiy 'L~e L-ie
P

Shocz ,ia,,-es in ~clid_2
to a "nl~clear jel,,_ce"
su-rfacel i,e I-ecry
-chickness d ana wa,ie S
of I ae
plar.te are discissed
referenct::
A
yssiieje
imen-i L~auinaru:, (Lc,:]~cuw
r~a ma n
SLJB~111",'ED: lbT.h Aprli 1'.-l:_36
i e T .)r, ac v e
t; -e,' ap 1--ed t,( a
re f ie ed f ro m r rie r--~ ar
is
Card 4/4

67~L
30U scv/i i
AUTHORt Orlenko, L.P.
TITLE: The P~opagation of a Plane Wave in a Plate of Finite Thicknees
PERIODICAL: Nauchnyye doklady vysshey ohkoly. Fiziko-matematicheskiye 11auki,
1959, Nr 1, PP 117-125 (U""R)
ABSTRACT: At first the author considers the propo6ation of a wave in a
hard half space on the free surface of which there acts an
instantaneous pressure which then decreases with time. The shift
of the particles is one-dimensional and takes place in the di-
rection of the wave motion. Wood Z_Ref 4-7 has given a numerica)
solution for the propa.-ation of such waves. The author gives the
analytic solution of the problem and solves the motion equation
in the region of the shock wave under corresponding boundary
conditions
(5) ) 2v a 2v + a2 (X)
Tt 2 1 Z~x2 1
S where the x-axis is the direction into the i-t~,rior of the semi,
Ca Card 1/ 2

ORL&KO, L.P.
Notion of a piston in the soil. Jkuch.dokl.vys.9hkoIy; fis.-mt.
nauki no-31105-110 '59- (MM 13:6)
1. Moskovskoye vyssheye tokhnicheakoye uchiliBhche imeni M.B.
-Baumans.
(Soil mechanics) Arplosives)

S/15 6o 00C1021101r,18
D012V2~
AUTHOR: Orlenko. L. P
TITLE: Recent Vertical Movements Of the Coasts of the -t'hite and
Barents Seas
PERIODICAL: Izvestiya vyashikh uchebnykh zavedeniy. Geodeziya i
aerofotos"yemka, 1960, No. 2, pp. 95-96
TEM In the investigation of the movgments of the earth crust on the
territory of the USSR, performed by the MIIGAiK (Moscow Institute of
Geodetic, Aerial Survey, and Cartographic Engineers),and the Institut
geografii AN SSSR (Geographical Institute of the A~ USSR), and oceano-
graphical organizations the determination of the spied of the movement
played an important part. There are already publications on this problem
in Soviet 1iterature,i-e-,conoaTdng the Baltic-, Black-, and Caspian Seas,
and the Sea of Azov, but not for the northern seas. For the observation
points at Mudlyug, Severodvinsk, Kem'-port, Soonovets, Barents-burg,
and Teriberka levelinga were carried out during at least ten years
(cf. Table 1). The values and their errors were treated by the method
r1ard 1/2

Recent Vertical Movements of the Coasts S/15 60/000/02/10/018
of the White and Barents Seas B012YB123
of least squares. From the data gained one can see that for both seas there
is a tendency to coastal depression which is stronger, however, for the
Barents Sea (0.1-0.3 cm/year). For the White Sea the speed of depression
of almost all points lies within the permissible limits. That means that
the White Sea is practically stable. The values given should be considered
to be approximate values, and additional material will be needed for a
final report. There is 1 Soviet reference.
SUBMITTED: July 6, 1959
Card 2/2

BUWAKOVA, A.A., ORT, 0, 16. P. . MOTOV, I. D.
Loosening stuc-.: drills without tearing off the pipe. Prikl- geofiz.
no.26:253-266 16o. ()aRA 13: 8)
(Oil well drillirigi

ORLUKO L. P.. kand. tekhn. nauk
Mode.linR at dytamic loadinR. 12v. v3ra. ucheb. &sr.; mashinostr.
no.7389-93 162. (MIRA 16:1)
1. Moskovskoye vyssheye tei-Judcheskoye uchilishche imeni
Baiman.g.
(Engineering models)

JD)W
y"'Ofo,' foftl= thin
Ifiiii6sti6~iniy-a

f_kC_C_NR, AM5611015
BOOK EXPIDTTATION
Orlenko, L.P. U11
Behavior of materials under IntcnGive dynamic loads (Povedeniye materialov pri
, (' I
intensivriykh d1naraicheakildi nii,,,rtL~.kii)(ii)-i~o-r,-c-ow-,-Izd-vo "14aGhinoutroyeniye," 1Y 'Al.
o166 p. illus., biblio. Errata slip inserted. 2,500 copies printed.
TOPIC TAGS: explosive forming, dynamic stress, spark shock wave, compression shock
wave, compressive stresa, mechanical engineering, solid mechanical property, mecharli-
gth metal
cal shock resistance, simulation, metal, metal physical property, high atren
PURPOSE AND COVERAGE: This book in concerned with the mechanical and physictl prop-
erties of materials under dynamic loads anq,shock conditions. T'he text presents
problems in shock-induced compreGGibility!of solids and change of mechanical proper-
ties of materials under dyna_mi_c_i&a__di_._It also contains problemsIof propagation of
stress vaves,in dense media, of deformation of thin-walled shells under dynamic loads
induced by electric sparks, explosives, or piston npacts, and of simulation under
dynamic load conditions. The book Is intended for specialists In dynamic technologi-
cal processes, such as explosive or electric spark forming, as well as for specialisti
concerned vith the dynamic strength of structures. The author thanks Kirill Petraddi
Stanyukovich for his advice and aid in the vork.
TALBIZ OF ODWTEM [abridged).
Card

ACC NRo AM5011015
Preface -- 3
Introduction -- 5
Ch. I. Mechanical properties of materials under dynamic loads -- 13
Ch. II. Dynamic compression of solids -- 38
Ch. III. Initial parameters of shock waves at, the boundary between two media 82
Ch. IV. Stress waves in dense media -- 98
Ch. V. Simulation under dynamic loads -- 130
Ch. VI. Dynamic deformation of thin walled shella -- 149
Bibliograyhy -- 162
SUB CODE: 20, 13/ SUR DATE: JlOctol/ O1UU IMT: 1W/ OM REF: 059
-Card 2/2

-L 4265-66 FSS-'2/EtIr (I)JEWP(m) jE.qr(m)4IqA(,d)JEWP(4) AJEC-S (L-1 4VJA(b)/.EVIA (r3
^CC NR9 027284,jjp (c)/*RpL ' VM/AT/RI4 SDURCB- COM UR/ID20q/65/OW/0D5/0130/01 I
AMORSt P. (Noscow); tar
Orlenko, L. I (Noscow)
C
Ms ]Me
TITLEt Computation of the onera of a shock wave in water
SOURCE: Zhurnal prikladnoy sekbazuki i tekhmicheekoy fisikil no. 5o 1965, 130-131
41-
TOPIC,,-TAM, shock wavep obock W&TO froot, shock wave prCphastiong shock mechanicap
F
wMlo *long mlosive, explosion offoott underwat;r ixplosion
'A%IMCT i The "orgy..of.an vnderwater sho*vsve ittemaing from an vaderwater explosi
to solved CANAM~"tion. of irreversible mechanical dissipation of onergy. The
shook is determined with the aid of the
of 'U an Underwater wave
qhock.adisbatioftecharge isentropest and the variation. 0f_ frontal pressure with
distalacee The t6til:vslue of irreversible energy lose zi+izL a shock ways from an
Orwater onion with spherical throw-crut of wtploolve material is given by
where the vait snorMr are to
looses o(P2) -i441
PA +:h
LCwd 1/3

L 9285-66
ACC NRs AP5027284
(see F. A. Bamp 1. P. StwWakovich, and B. I. Shekhter. Fixi!:& Vzryv Fi=atgiz,
Iq5,9). The qusntities p. and v. are the initial pressure and unit voluize of the water;
P2(r) and Y,(r) are the pressure and =it volume at the shock ways front; r is the
aDordizate of the shook wave front; and r is the throw-cut radius. The integral term
0
an is computed along the expausion isestropes of the water (as*
4w svolww vj, eorresponLing to the condition of Us water after cipumion to the
Tot"
essure p swr& is Us sum 'of _ the -epera of p@ bubble pulsation
PIVS, is as defined is ** machwima
The
1 + Z2 Where 11 "a" e" 12
vuerv compated IF Mpirloal means. Plots of the ratio 11/4 and 12/q (for peatolite)
ywou we wt- givom Am #iVft IW
Mot:
cmd

0

OPLE24YO, L. R.
OFLKNho, L. P.--"Analysis of the Basic Factors Determining the Pjai)-,
Oscillations in Teriperature of the Ground Layer of the Atmosphere."
Flain Administration of the Hydrometeorclogical Ser~-ice, Council of
Ministers USSIi. Main Geophysical Obser-vatory imeni A. 1. Voyeykov.
Leningrad, 191,'5. (Dissertation for the Degree of Candidate of
Physicomathematical 3ciences).
80; Knizhnaya Letopis' No. 2", 2 July ],)L'L'

02mra
ChwW of the thermodynamic state of the atmosphere. Trudy GGO
no-53:95-99 155. (KLBA 9: 8)
(Atmospheric temperature)

SOV/36-56-60-7/1-0
AUTHOR: Orlenko, L. R.
TITLE: Computing the Diurnal Rate of Shortwave Radiation on Clear Days
(K raschetu sutochnogo khoda korotkovolnovy radiatsii v yasnyye
dni)
PERIODICAL: Trudy Glavnoy geofizicheskoy observatorii, 1956, Nr 60, pp 6ri-66
(USSR)
ABSTRACT: In studying the diurbal variations in temperature an accurate eleva-
tion of the diurnal rate of shortwave radiation is of primary im-
portance and all losses in radiation should be accounted for. SolAr
radiation in the atmosphere is weakened through absorption IV awop; ozone,
water vapor and other components of dry air. Dispersion by dry air
and vapor together with scattering and diffusive reflec-;ion of sub-
stances suspended in the atmosphere(duot)are also contributing fogtors.
Theoretical computations and observations fom the basis for a new,
well founded nomogram. The article contains a supplement. There are
10 tables, 2 diagrams, and 7 references of which 5 are Soviet and
2 German.
Card 1/1

AUTHOR: Orlenko, L. R.
36-57 -69-1/)-6
TInZ: Evaluation of the Influenze of Daily Evaporation Rate on the Temp-
erature of Surface Soil and. Near-surface Air (Otseaka vliyaniya
autochnogo khoda. ispareniya na t~_mperatoru po-,rerkhnosti pochvy i
vozdukha)
PERIODICAL: Trudy Glavnoy geofizicheskoy obuervatorii,19,
Nr 69, pp 3-10 (USSR) 57
ABSTRACT: The author points out that in computing the 6,aily temperature rate for
the heat balance of surface soil, earlier researchers (such as A. A. DDrodnitsyn,
I. G. Lyutershteyn, and A. F. Chudrovskiy) failed to account for the heat spent
on evaporation. The present article suggests a method for determining such heat
losses, and in this way obtain a more accu-rate pictLre of tbee influence of evapor-
ation temperature. The author recalls a sLmilar attempt b,,r M. Ye. Shvets vho
bwjed his calculatioa on the coefficient of maximum specific humidity at the sur-
face of vater or moist soil. On the other hand the author of the present article
treats the phenomenon of evaporation as a fuaction related directly to surface soil
temperature. The necessary data for such a relationship were deduced from the re-
sults of observations at the KoltiLahi Station (near Leningrad), coaducted in the
Card 1/2

36-57-69-1/16
Evaluation of the Influence of Daily Evs porat .!on (Cont . )
swwr of 1950-Theinitial fujmnLL--j in determiniag dependen~'P of evaporation on
temperature is IE=IEO + bt-, where b is the coefficient cf change in the evaporation
rate resulting from a temperatu--re ciiange (the coefficiez~ 'being expressed in calories
per square centimeter per minute); t is the deviation of temperature from the mean
daily temperature; and LEO is the mean daily evaporation rate. Based on the know-
ledge of the parameter LE, the author develops a mathematical method to determine the
lose of heat required for evaporation. Among other data (such as the temperature of t
soil) the method also accounts for turbulent heat conductivity. in Section 3 of
the article the author verifies the results obtained, plotting two curves, one of
which reflects the heat lost during evaporation. The difference amountsto 4-6* Centi-
grade daytime and to -3 to -5* at night, when b = 0. Verification was also conduct-
ed at the above-mentioned station at Kol-.ushi. There am 4 figzu-es and 5 Soviet
references.
AVAIIA13LE: Library of Congress
Card 2/ 2

A- ~,' ~I ~ r"
PHASE I BOOK EXPLOITATION sov/4641
Leningrad. Glavnaya geofizicheskaya observatoriya
Voprosy fiziki prizennogo slo-va rozdukha (Problem in the Physics of the
Wear-Surface Air Layer) Leningrad, Gidrometeoizdat, 196o. 161 p.
(Series: Its: Trudy, vyp. 94) Errata slip inserted. 850 copies printed.
Sponsoring Agencies: Glavnaya geofizicheakaya observatoriya ineni A.I. Voyeykova;
Glaynoye upravleniye gidrometeorologicheskoy sluzhby pri Sovete Kinistrov
SSSR.
Ed. (Title page): D.L. Laykhtman, Doctor of Physics and Mathematics; Ed.
(Inside book): Yu.V. Vlasova; Tech. Ed.: N.V. Volkov.
PURPOSE: This publication is intended for meteorologists specializing in the
lower layers of the atL-osphare. It may also be of interest to agronomists,
construction engineers, and other specialists whose activities are influenced
by atmospheric conditions.
COVERAGE: This issue of the Transactions of the Rain Geophysical Observatory
contains 18 articles dealing mainly with problems of the physics of the !,oar-
surface air layer. Correlations between the surface wind and geostrophic
wind are examined and the results of both theoretical calculations and
Card 1/4

Problems in the Physics (Cont.) sov/4641
experimental investigations given. Individual articles analyze the
temperature regime of the active surface of soil and the factors determining
the thermal conditions of the boundary layer. Results of fog investigation
are presented in two articles. In addition, some problems of methods in
the experimental Investigation of the near-surface layer are eliicidnted. N,
personalities are mentioned. References follov each article.
TAEU OF CONTMS:
Laykht-n, D.L. Formulation of the Problem of the Stationary Structure
of the Boundary Layer
Tseytin, G.M., and L.R. Orlenk, Stationary Distribution of Wind, Tem-
perature, and ~urbu ient E~xchang~e in the Boundary Layer Under Different
States of Stability 8
Ariyell, N.Z., and L.A. Klyuchnilwva. Wind Under City Conditions 29
Klyuchnikova, L.A., and F.N. Shekhter. The Role of Radiant and Turbulent
Heat Exchange in the Formation of the Temperature Stratification in the
Boundary Layer 33
Card 2/4

Problems in the Physics (Cont.)
Ariyell, N.Z., and L.A. Klyuchnikova. Operational Method for
the Wind Profile in the Boundary Layer
Shekhter, F.N. Ground Freezing at a Given Temperature on the Active
Surface 42
Tseytin, O.Kh. Correlation Between the Temperatures of the Active Surface
and of the Air in an Instrument Shelter 62
D'yachkova, T.V., and N.V. Serova. Thermophysical Propertien of Snow 70
Martynov, G,A. Effect of Periodic Temperature Fluctuations on the Depth
of Ground Freezing 6o
Martynov, G,A, Results of the Cft:Lcultition of the '[bmjx!ziit%irf~ Flelii , f
Thuwing Ground Compared With Observational Data 19t
Timofeyev, N.A. New Method for un Approx1mate Cal:,ul.o '.crl and F.~
of Snow-Melting Intensity
Card 3/4

Problems in the Physics (~.ont.)
Timofeyev, N.A, Calculation of the Diurnal Variation of Temperature rind
of Snow Melting Intensity in the Spring Period
D'yachenko, T.F, Modeling the Diurnal Variations of Temperature in
Gandtn, L.S., and R.Z, Soloveychik
Into Accourt Horizontal Mixing
3n the Evaporation Theury, '~tking
Berlyand, M.Ye., and Kim Zin-Mun
tion Over Seas
On the Theory of Air I-"iss Transf-;rma-
Berlyand, M.Ye. Conditions for Fog Formation
Gracheva, V.P. Investigation of Fog-vormation Characteristics
Solomatina, I.I. Diurnal Variation of Absolute Humidity in the Near-
Surface Air Layer
AVAILABLE: Library of Congress
1-4()
156
Card 4/4 jA/dwm/sfm
2/1/61

ORLENKOY L.R.
Relationship between WindB near the ground mid the geoBtrOPhic vind-
Trudy GGO no-107:55-59 161. (KIRA 14:10)
(Winds)

OldENK09 k.R.; UTRIA, Z.M.
CalcuUtion of the accretion and thaving of old ice. Trudr GOO no.127/
112-3-15 162. (MIRA 15:7)
(Arctic regiom-Sea ice)

ACCESSION NR: AT4004709 S/2922/63/007/000/0045/0051
AUTHOR: Orlenko, L. R.
TrrLE: Determination of the vertical currents in the boundary layer from external
parameters
SOURCES: Wes. nauchn. meteorologich. soveshch. Trudy*, v. 7, Fizika prizemnogo
sloya. Leningrad, 1963, 45-51
TOPIC TAGS: meteorology, vertical air current, updraft, atmospheric boundary layer,
vertical current determination, atmospheric friction, wind, wind velocity, turbulence,
synoptic process, barometric pressure, Coriolis parameter, boundary layer structure,
temperature, temperature gradient, atmospheric turbulence
ABSTRACT: A method is described for determining vertical currents in the boundary layer
of the atmosphere. It is shown that the deb.-rmination of the vertical component of wind
velocity in this layer requires data on the distribution of its horizontal components. Two
approaches are given for determination of the vertical component, depending on how the
horizontal components are determined. Since one method requires a dense network of sta-
tions, emphasis is on the second approach, based on certain formulas for the distribution
of wind velocity and direction in the boundary layer. Two equations are given making it
wrible to determine the wind velocity profile if the turbulence coefficient in the boundary
1/2

ACCESSION NR: AT4004709
layer is known. The difficulty of determining this coefficient is overcome, and the problem
is solved for a specific stratification of the atmosphere. Wind velocity in the boundary layer
is determined from the known pressure field and the roughness of the underlying surface, so-
called external parameters. A simple expression is derived for the vertical component at
the upper limit of the boundary layer. A qualitative analysis has been made of the depend-
ence of vertical currents on the speed of the geostrophic wind and air stratification of the
boundary layer for a symmetric pressure formation assuming a constant turbulence coef-
ficient in the entire boundary layer. Such an analysis makes it possible to make quantitative
estimates of vertical currents in the boundary layer. Final formulas give the relationship
between the vertical component and the speed of the geostrophic wind and air stratification
in the boundary layer. Ile method was checked using data on the geostrophic wind and the
temperature gradient from synoptic charts. Solution of the formulated problem makes it
possible to predict, as well as determine, vertical currents, provided there is a forecast
of the pressure held. Orig. art. has: 24 formulas.
ASSOCIATION: Gla,~maya geofizicheskaya observatoriya (Main Geophysical Observatory)
SUBMITTED:00 DATE ACQ; 27Dec63 ENCL 00
SUB CODE: AS NO REF SOV: 003 OTHER: 000
Card 2/2

IAYKHTW, D.L.; ORIZNKO, L.R.
Program and methodE for ol-l-servationb r-iad(, during the
expedition. TrAy GGG 1 (YIRA 1-,' ;~-;

ACCESSZON XR: AT4028737 S/2531/63/000/1"/0011/0021
AUTHOR: Orlenko, L. R.; Tkachenko, A. V.
TITLE: Some results, of the processing and analysis of gradient observations in the
surface layer of the atmosphere
'SOURCE: Leningrad. G1- geofix. observ. i Mr. n.-i. gidrometeorol. inst. Trudy*,
ho. 144/40, 1963. Mike pogranichnogo, sloya atmosfery* (physics of the atmospheric
boundary layer); Dneprovskaya expeditsiya GGO 1, UkrNIGM,, 11-21
TOPIC TAGS: gradient observation, atmosphoric surface 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 surfice layer; winei profile parameters, components of the
t
e4argy balance of turbulence, anJ the turbulent flows of heat and humidity. Gradient
ob'Fervations , 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
chaiacteristics of the surface layer as the coefficient of turbulence. the components
of the energy baUnce of turbulence, and the turbulent flow of beat and humidity.
4qard .1/2

LAYYdf'iW, D.L.; ORLENKO, L.R.; TKACHENKO, A.V.
Diaperelon of the turtmlence energy in the loweBt layer
of the atmosphere. Truoy (W no.144t28-33 163.
(MIRA 17:6)

M
ACCESSION NR. ATT4028740 S/2531/63/000/144/0034/0047
AUTHOR: Orlenko,,_L.._R..
TITLE: On the ratio of the comianents of the energy balance of turbulence accordin,g
to experimental data
SOURCE: Leningrad. G1. geofiz. observ. i UAr. n.-i. gidrometeorol. inst. Trudy*,
no. 144/40, 1963. Fizika pogranichnogo sloya atmosfery* (physics of the atmospheric
boundary layer); Dneprovskaya expeditsiya GGO i UkrN11GMI, 34-47
TOPIC TAGS: energy balance, turbulence, gradient observation, aerostatic observa-
tion, pilot balloon observation, Makhtalinsk expedition, energy dis6ipation, boundary
layer, exponential law
ABSTRACT: In this paper the author examines the ratio between the components of the
energy balance of turbulence at --arious altitudes. Distribution of wind and tempera-
ture in the boundary layer is used for analysis according to materials of gradient,
aerostatic and pilot-balloon observatioa in the-MAIntalinsk expedition. Estimates
of the parameters 6 are given by considering the energy dissipation of turbulence
into heat within the boundary layer. Through a series of mathematical arguments,
the author derives formulas for the various parameters which are presented in tables
Cordl/2

ACCESSION NR; AT4028740
for various altitudes and times. He also studies the effect of atmospheric strati-
fication on the vertical profile of energy balance of turbulence. "ibis profile is
plotted in graphs for day and night times. Observations of the distribution of
temperature and wind for 13 hours were used for evaluating 6 during the day time.
6 was defined according to averaged data for h = 20 m and h 50 M, 7 - 0.98 0/100 m
a
and 7. = 0.60/100 m. Calculations have shown that for a re iable determination of
6 during the day, the distribution of the wind and temperature must be known in
the entire boundary layer. On the basis. of the presented analysis, however, it can
be assumed that the energy expenditure of turbulence on the operation of intersper-
sion for the boundary layer as a Vhole is small and therefore 6 must be assumed to
be somewhat less than unity (0.9-0.8). The value of 6 for day conditions must be
made more precise. For -night conditions the presented value of 6 is confirmed by
the data of the Dnieper expedition. Orig. art. has: 8 formulas, 3 figures, and
2 tables.
ASSOCIATION: Leningradakaya glavna geofizicheskaya observat"iya (Principle
Geophysical Observatory of Leningrad)
SM3'V"-=D: 00 DATE ACQ: 16Apr64 EXCL: 00
q'TR CODE: AS, MM NO REF SOV. 004 OMER: 000
Cord 2/2

; A Y K HT ~" 'I., , ; . . ; , ): - -'. I j .. .
. 11 1 , -,I -*' , ".. I- ., -. .., . . I - " ~, - ~. I -- - , ! - - I ( - , , . , ..
~- . des. ' 7- - . . ~ ~ :. . ~ -- - -

ACC NFZ- AT6021505 (h' SOURCE CODE: UR /2 5 31 6 6 /0 00 /0 187 / 00 13 /00 43
~AUTIIOR: Bortkovskiy, H. S.; Orlenko, L. It.; Toeytin, G. Kb.
1ORGi none k
TITLE: Calculation of wind and tangential stress above a water surface
SOURCE: Leningrad. Glavnaya geofizicheckaya observatoriya. Trudy,
no. 187, 1966. Fizika pogranichnogo sloya atmoafery (Physics of the
atmospheric boundary layer), 13-43
TO-,r! TAGS: micrometeorology, atmospheric tu-bulence, wind speed,
tangential stress, atmospheric boundary layez, near water boundary layer,
wind velocity, ocean dynamics, ocean current, surface tension
1ABSTRACT:
I
;-A oro(fedure is presented for calculating wind and tangential
Istress over the open sea using a ~,iven baric field and known
Itemperature stratification. The procedure is based on theoret-
.ical investigations made at the Department: of the Physics of
!the Boundary Layer, Main Geophysical Laboratory. Since the
roughness-of the water surface is regauded as known, the problem
is reduced to solving the usual equAtions of raotion for air
with a given horizontal.baric gradient over a moving surface
Card 1/4

Wft' NR1 Am,602156
_(ex,cept that the underlying surface is not motionless). Hor-
Jzontally homogeneous conditions are assumed. In selecting
boundary conditions, the presence of surface water currents
and the temperature stratification in the boundary layer are
(characterized by the difference between the water-surface
temperature and the air temperature at the upper limit of the
boundary layer. The influx of radiant heat is assumed to be
a linear function of height, a model in which there is~a
!Juinp at height h is accepted in determining the turbulence
1coefficient k, and the Laykhtman model is accepted in determin-
',.~ng wind velocity.
General solutions are obtained for the layers zo 1 z < h and
z > h. The solution for the first case is simplified so that
th; wind-velocity components are computed rapidly with auxiliary
tables and nomograms. A scheme is given for finding wind
velocity, tangential stress, the modulus of the wind velocity,
and the angle of "friction" at a height of about 10 m above
the sea. A simplified procedure is presented for calculating
wind velocity and tangential stress under equilibrium condi-
tions. The procad~sre was tested with limited experimental
data. The applicability of the procedure is discuesed, and
the errors-are estimated. For instance. with a time interval
of 2 hr, the error in the component of tba.tangential stress

ACC NRI AT6021505
T, X. 8% for V. - 15 -n/sec and AV9 5 m/6ec (the velocity of
t9a geostrophic wind ..tnd the jump n the geostrophic wind);
12% when AV 10 m/sec; errors of 1.2% and 20Z were noted
'1~0 x
in Toy under like coniitions. The error in the wind velocity
due to advection ahould not exceed 15Z. [WA-50; CBE No. ill
SUB CODE: 04/ SUBM DATE: none/ ORIG RIP.F: 018/ OTH REF: 012/
Card

ARANOVSXIY, N.G.; ORLIWKO. N.1.; SHTMIN. L.S.; 1YXWJSALIMKIY, A.M., doteent,
redaktor. vbww~~~
(Drafting In zowhine construction] Chertoshnoe khosialetvo v mushinostroenli.
leningrad, Nanchno-takhn. izd-vo mashinostrott. lit-ry Eleningradskoe otd-niel
1953. 103 P. MRA 6:10
(Machinery-Draving) (Drawing-room practice)

L 06456-67 94 (m)~Ee(j - IJP(c) _GGIM _Vo664_/oo
OD _66-
AC_C'__WR_-AP6o24546 (A) SOURCE C 66-8979/623V6o
Suroyegij~,,;~_
AUMOR: Berlyant, S. M.; Drozdav, V. Ye.; Finkel'. E. E.; Orlenko, P. A.;
L. M.; Breger, A. Kh.;, Karpov, V. L.;_Zorin,_V._7.
.ORG: none
/5'
iatioh cross linking of polyethylene insulation of cable pr(>-
.TITLE: large-scale rad
!ducts
SOURCE: Atomnaya energiya, v. 21, no. 1, 19,6, 64-66
:TOPIC TAGS: radiation chemistry, polyethylene, polymer cross linking, insulated wire,
!'electric cable/ KP gamma ray apparatusp
.ABSTRACT: In view of the many advantages resulting from the use of irradiated thermal-
ily stabilized polyethylgne as insulation in cables, the authors describe apparatus de-
veloped for the irradiation of such insulation, for use in geophysical cables for very
;deep weU drilling (o.d. 6.5 mm, length -9 weight --380 kg, volume - 400 1),
~capable of withstanding temperatures up to :MC and pressures higher than 300 atm.
The entire cable was wound on a drum and exposed to 7 raVation from Co6o (total
activity 180,000 g-equiv lent of radium) from the KP-200'.1hpparatus- Measures taken
,to ensure uniformity of ?he gamma radiation, which .T., -anTessential factor in the
success of the operation, are described. "Die required dose was 140 Mrad At
'a dose intensity of 63 r/see and an irradiation time of 610 hr, the productivity ;)f
the apparatus was 0 7 kg/hr and the efficiency -13%. The -uthors thank G. V. Liqoy
uDc: 621.039.55: 541-15
Card 1/2

L o6h56-6 7
ACC NRI AP6024546
for participating in the development of the %pparatur., and M. Ye. Yeroshav, M.
Larionov, L. K. Topil's Y!~. ~Dia~ov, and the late1w. X.-Kuznetsavjfor help
with the experiments. Orig. art. has: 3 figures.
SUB CODE- 07, 20/ sum DATF,- 16oct65/ ORIG REF: 007
2/2
Card

OR
Work of the polyclinic in the organization of medical service for
workers. Zdrav. Belor. 5 no.1:39-41 Ja 159. (MIRA 12:7)
1. Glavnyy vrach teentrallnoy polikliniki. Gomel'.
(GOKU~-INDUSTHUL MBEIGUM)

BONDARI, Nikolay Gerasimovich.. doktor tekhr. nauk.. prof.; KAZEY,
Igor' lvanvvi* kau4ir--ujkkmft*w7,-4AWJ3", Bernard
Falkovich, kand. tekhr. nrtak.~ KOVKIN, Turiy Georgiyevich,
kand. tekhn. nauk: dots~; Pr.1rilwal, uchantiyuj TUASPMO,
V.F., kand. tekhn. nauk: YkKOVLEV. G.N., kand. tekhn. nauk
dots.; DOROSHENKO, Ye.V., kand. tekhn. nauk; NEVZOROV,
I.N., inzh.; KONASHENKO. S.I., kand. takhn. nauk, dots.;
OUENKOI V.P., lnz~~,, KHOKIIWV A.A., kand. tekhn. nauk,
dots.; ZELEVICH, P,M.; kand. 'ekhn. nauk, red.
[Dyr-mics of railroLd Dinamika zheleznc-.dorozhnykh
mostov. [By] N.G.Otnda.- ! dr. Moskva, Transport, 19b5.
411 p. (MIRA 18:12)

SLYUSAREV, T.V.; CRLENKO, V.Ye.
Crope for a vinter green fodder plan. Zhivotnavodstvo
23 no.7:55 Jl 161. (MIRA 16:2)
1. Direktor Dinskogo ptitsesovkhoza, Krasnolarskogo
kraya (for Slyusarev). 2. Glajmyy hqr,,)nom Dinskogo
ptitsesovkhoza, Krasnodarskogo ~:raya ~fa- Orlenko).
(Poultry-Feeding and feedr-.)

'At
-;ADth4;-7:., ree,~ Thr ences'~
oe'USSR:refejr
r
Ap
hik

ORLIEW, Ye.G.
-
Anatomical structure and Physiological activity of the leaf
apparatus in (~isrcas pediumculata as affected by illumination.
Dokl.AN SWR 106 no.3:555-557 Ja 156. WaA 9:6)
l.Belorusekiy naxichno-iseledovatellskiy institut leanogo kho-
zyaystya.Gosell. Predstayleno akademikom T.N.Sukachevym.
(Oak) (Leaves)

ORLENKO - Ye, G.
Cytological inveeUgation ~)f the green-barked and gray-barked
&open form in the forests of 'White Russia. Sbor. nauch. rab.
Bel. otd. VBO no.3z1l)-,ll5 '61. (M UU, 14: 12 )
(White Rusgia, . -Aspen)

ORLENKO. Ye.G.
Valuable form of spruce (Picea excelss. var. acuminata Beck.) grow-
ing at the southera boundary of its range in the White Russian
S.S.R. Dokl.AN BM. 6 no.2:125-126 F 162. OMIRA 15:2)
1. Belorusskiy nauchno-isBledovatellskiy institut lesnogo
khozyaystva, Gomel'. Predstavleno akademikom AN BSSR I.D.
Yurkevichem.
(Brest Province--Spruce)

oillE.M., Ye.G.
-1 . - 'r
~,*Plerti,Dn Of jtjG!-.4,rj,,r :,-. !, ;.,.e for breed-'np, ;-l ric.:es de.,e . :' ,
on tho % ...... of '-.- - IKO *- ; ', : : 1 . N! 1 . C ~;
( , - ~ _4 -, -1 . '.
no. 7: 11 P- 1:'~' 't,5. A I - I

VORONOVv P.S.j KLIMOV, L.V.;- 0-,R-LE =..- t Ye,H,
Geological structure of Mount Brmn. Trudy NIIGA 113:98-122 160.
(MIRA 14:5)
(Brownp Mountq Antarctica-Petrology)

SIOBOIJSKOY, A.L., professor; GJAHTS, R.K., starchiy nuuckuiyy sotrudnik; BRUOITSY-
NA. M.P.; VMBITSKIY. V.P.; 02=KO. Yu.14.. direktor; OViIYMO. I.I., do-
tsent, dire)-tor.
Gertain data on the role of the cerebral cortex in the pathogenesis of re-
actions which occur following trunsfusion of different-type blood. Vest.
khIr. 73 no.4:9-13 JI-Ag '53. (KI," 6:8)
1. WrainRkiy nauchno-isaledovatellskiy institut perelivaniya krovi (for
Orlenko). 2. Mrainskiy institut usovershenstvovaniva vrachey (for Ovaiveji-
ko). (Blood--Trunsfusion) (Bruin)

XBAINSXATA-IGNATOTA. VA., professor; OMANKO, Tusk., stershly nauchnyv.
motrudnik-. CHIMNEO. K.1., star-S'W'baud lotrudnik
Cross reaction to Individual blood compatibility and Its role in
the detection of taosensitixotion of the recipient. Top.perel.krovt
4;89-96 255. (MIRA 9:12)
(BOOCS-42ANSMS ION)

C~PLRIKQ In-]L- starshiy nauchnvy sotrudnAk 0[har1kov, ul. Bassaynays. d.
15)
Bzperimatal and clinical use of chloride plans* in acute intestinal
obstruction. Mov.khir.orkh. no.2:7-11 Mr-Ap '57. (MLRA 10:8)
1. Ukrainskiy asuchno-imeledovatellakly institut perelivaniya krovi
i neotlozhnoy khirurgii
( 1NTIST INES- -WSTRUCT ION) (B1,OGD PLASKA SUBSTITUTIS)

-A
aRISHKO, ju.X,, starshly nauchnyy sotrudnik
New compound OChloride plasmsO " its use in several diseases re-
quiring surgery. Top.paral.krovi 4:192-212 155. (KIRA 9:12)
(BWO PIASNA SUBSTITUMS)

OMBNKO, Yu.N., sterehiy nauchnyysowudnik; KOZTRI. P.T., kandidat biologi-
-- ~ I-'- - - ~ 6bi4kM)VIauk
Role of *midget ampules* for t1w bactartological control of stored
blood and its componerits at various stages of preservation. Vop.
perel.krovi 4:231-241 955. (HLRA 9:12)
(BLOOD-COLLBOTION AND PRISMATION)
(IABORATORIES-INSTRMIITS AND APPARATUS)

ARLOZOROV. Z.G.. starohiy nauchnyv sotrudnik; ORIXNIO. Yu.M.. starshiy
nauchnyy sotrudnik; LEKABBY, S.A., vracE - --
New method of preparing serum from the blood of donors with conserva-
tion of the globular mass for transfusions. Yop.perel.krovi 4:259-
255 155. (KLRA 9:12)
(SIRUH) (COLIRCTION AIID PRNSIRRVATION)

EXCERM MMICA See 9/Vol 13/5 SURGMY XV 59
2695. A TRIAL OF CHLORIDE-PLASMA IN ACUTE INTESTINAL OBSTRUC-
TION. A CLINICAL AND EXPERIMENTAL STUDY (Russian text) -.Or -
__Lc_Qko Yu, M. - NOV.KHIR.ARKH. 1957, 2 (7-11)
Two prep%rations Of chloride -containing plasma no. I and no. 2, both containing
extra proteins in plasma, were suggested by the author in 1949. 1. v. administra-
tion of the preparation increases the blood concentration of chlorides and rapidly
abolishes hypoproteinaemia and hypochloraemia. Experimental results were favout -
able and clinical use (475 transfusions to 275 patients) showed that the preparation
accelerates disappearance of toxaemla while the increase of blood chlorides is
maintained for 6 - 10 days, (S)

'iRIA14KO, Yu.M., doteent
Use of chloride-treated plasma in acute intestinal obstruction in
experimental and clinical conditioas. Probl.gamet. i perel.1crovi 2
no-3:38-41 k-Je '57. (MLRA 10:8)
1. Iz UkrainBkogo nauchno-Isaledovatel'skogo institute parelivaniya
krovi I aeotlozhnoy khirurgil
(IR14TINAL OBSTMICTION, therapy,
blood plasma with chlorides in exper. & clin.
cases (RUB))
(BLOCD TRANSFUSION, in various diseases.
intestinal obstruct,,, chloride-treated plasma in exper.
& Olin. cases (Rug))
(OHIMiDIS,
blood plaamB treated with chloride@ in ther. of exper.
& clin. intestinal obstruct. (Rua))

ORMKO, YU.M.
"Ourrent problems in hematology and blood transfusion." Probl.gemat,
I perel.krovi I no.4!56-57 Jl-Ag'58 (MIRA 11:8)
(BWM)

ORLENKO, Yu. M., Doc Med Sci -- (diss) "Chloride plasma and its ap-
plication in complex therapy of acute blockage of the intestines.
(Experimental-clinical research)." Kbarlkov, 1960. 19 pp; (Kfiar,.eov
State Medical Inst); 250 copies; price not given; (KL, 1~-bO, 166)

ORLMZO,ju.K., daktor med.nauk; BRUSNITSINA, M.P.; BIRYUKOVA, S.D.
Imediate and late results o1,' different surgical interventionp
for perforating ulcers of the stomach and duodenum. Khirargiia
no.3:47-51 162. (MIRA 15:3)
1. In Ukrainskogo institute perelivaniya krovi i neotlozbnoy
khirurgii i kafedry obshchey khirurgii Kharlkovskogo meditsim-
skogo inatituta.
(PEPTIC ULCER) (STOMACH-SURGERY) (DUODH1&JM--S1JRGERY)

ORLEMO. Yu. M., doktor mod. nauk (Rharlkov, ul. Petrovskogo, d. 6,18,
k~. 15-T -
Perforating ulcers of the stomach and duodenum in elderly and
senile subjects. Vest. kh1r. no.4112-15 162. (MIRA 15:4)
1. Iz kliniki obahchey kbirurgii Kbarlkovskogo meditainokogo
Institute (rektor - doteent B. A. Zadorosb"y).
(PEPTIC ULCER)

ORLENKO, Yu.M., doktor med. nauk (Kharlkov, u1. Petrovskogo, d.6/8, kv.15,;
~ Ya.
P
Acute cholecystitis in aged and sen-'13 persons. Vest. khir-. 99 nc..l.':
125-127 0 162. (.'-!11.~A l-,:
1. Iz kliniki obshchey khirurgii (zav. - doktor med. nauk Yu..". Crienl,~ ,
lechebnogo fak-LI'teta Kharlkovskogo meditsinskago 4nstltuta (rektGr -
dotsent B.A. "adorozhnyy) na baze 11-y Kharlkovskoy gurodSkLly kll'lli-
cheskoy bollnitsy (glavnyy vrach - Ye.b. Guzhel).

CRIMUP Ye. K.
Min Higher Sducation UjSQ. Moscow Crder of LenLn and Crder of Ltor Banner
Higher Tecimic~,l --'chool imeni Fbuman. -,oscow
ORLENKCIV, Ye. K.:- "The effect of the ~l,hlity of' weld penetration or, tile strength
and plasticity of butt joints in autom.-tic flux welding." M. n higher Education Uo',,.R.
Moscow Order of Lenin Find Order of Iabor !ied BFnner Higher Technica. .-Ichool imeni
Faunuin. Msc:;cow, 1956. (Ldj:~,,rt,tj,, for -.',e De.;-ree ol -:-nddate *,.,. *Ica-I --- (:~ - - . "
SC: Knizhneya Leto~ip 1, No. 2' , 1 .'56

13 7- r)8 - 3 - r) 198
Translation from: Referativnyy z-iurnal, Metallurgiya, 1958, Nr 3, p 106 (USSR)
AUTHOR: Orlenkov, Ye. K.
TITLE: Vibration Strength of Welded Butt Joints with Defects Due to
Non-fusion (Vibratsionnaya prochricist' svarnykh stykov~-k':'.
soyedineniy s neprovarom)
PER10DICAL V sb. - Prochnoqt' i avtomatizatsiya svarki (MVTU, 71),
Mashgiz, 19'~T, pp 19-4~)
ABSTRACT~ The LT. of butt joints of low-carbon steel welded on both s,,des
and containing flaws caused by various degrees of incomplete
penetration was compared with the 15,w of identical, but deff-( t-
free joints. A limited(swwas determined for each series of
specimens on the basis of Zx,06 cycles with alternating tension
and pure bending alternating in sense. It is shown that under
both types of vibrational loading a welded seam obtained by
automatic two-sided welding with flux exhibits greater strength
than the parent metal. In all specimen,; exhibiting complete pen-
etration and free of other defects of the seam, the rupture oc-
curred in the parent metal far from the welded region.
Card I 1Z Under a pure bending load the presence of Lip to 25 percent of

13 7 - 5 8 - 3 - 5 19 8
Vibration Strength of Welded Butt Joints (cont
incomplete penetration has no effect whatsoever on tile vibrational strength
of the weld. At 40 percent incomplete penetration the 0.1 of the welded ioint
is 7 percent lower than that of the parent metal. A considerable decrea~se in
(5V,(29 percent) was observed at approximately ~iO percent of incomplete
penetration. Under a tensile load, incomplete penetration in welded butt
joints sharply reduces their 6W. Even the presence of 5-6 percent of incom-
plete penetration results in a 30 percent decrease in (YW. Not unlike a sharp
notch, the effect of stress concentrations created by incomplete penetration
is more pronounced at low stresses which approach the C7W. Parent metal
with transverse fibers exhibits a 0./ which is 14 percent lower than that of a
metal with longitudinal fibers.
N. T.
Card 2/2

KA , Fl~tnlm 11 tt,.4 , '.c,.! (,! -)ch . OW-i-~~ 1, t
a . T Eie c - um, a . Y . .-,: 7 ~ g
k -', "h(,rob A IP .4e
e ~ir, e z n
of or A. Ffl i JK, I e w

0 0 -110 0 are 0-6 6
0 0,0000000 0 0 4 4 0 0 0 0 w -
u is fill fill Its
IV a a b AS if a It At u 0 16 v a a a d, -W 41 a
A-A a A. a It It A 0 Q 0 04A b
00
-00
Aj -00
-00
00 a
00
004 Cd $mod "go 01 p" mA na4mm pladd6b -00
ee N.. bbwNW7- -J,-h9tt- t.96
C% l0j).-A disimwki-- Koo
It ye Lai. Cbm.
:
0 a =00
.';zoo
"MOO
see
w0 :zo 0
coo
too r - 0
U00
Alto SL 1141ALLUNGKat toll
"lug, C141111"1101 woo
t I WX'i goo
us -69 do , t- 9 g- I - 11 1 1 g- )
is . a 1. , wi
0 a it a a a q 0 4 a w 4
0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 st 0 0 0 o q
1166009,6 00000 0 iio a 0 - 00 : :t A
I --0000040000000000000es

le
?
It IT I.? r f.90.20 2 II6. l Ab
op so! *0 06,00
.
A-1L.A 6-M -1 AL A

P&OM519 AW O"flit-11 ..of. -4119
00
00
00
00 -00
*0
00 -00
90

008 -00
06.1 1 0 goo
zoo
I%J- (IrktallZandskupa Lob., IOU, a. '100
Tb,,tcch*,Ari. u.
di., ml.

00 a ToWn asmi photagmphe an given. -8. G. roo
.
0
I

SOO

11
00
W
0 0

0
:
:
0
.91ILLUI-LKA. LITEPATL411 CLASIMPICATION 9-1- MOO
woo

U a A, ~O IT
an 11 Iq a in A a n* 0
0 *wool# Code

0006000006*00090
O
O
O
1
0
: 0000 0 0 0 0 a 0 00 0 0 00
66096091096006006
d
b
S
O::: - -41 00000000000 0000

000
00A
00
00
00
00
000
00 1
a 0 is is is v avp 041 4 di 40 460
. a -4 1L
rodw
R. T.
6 L A MIT"t Ll"Mal"Off 4L&UWICAVMN
.00
see
1-00
qoo
!"Of
Ogg
woo
goo
so*
j"0
j age
V- ago
woo
a MI; J i a ; a ; ; 4-op'l "Jgmi str4o ",Iwo 9 a 0 0
0 0 0 6 0 0 0 0 0 0 0 c 0

loop
00
00
14,r
ffn gvm64 ,k IRON the cqmw.
Wa weft owipwition OW outUP4 ivopwike of do J8,14,11
siumi-vism4imm 4ypro of bigh-spmd otwk mid
lowbie 1&"Ww in Uw m stlard
7ximAtioll of staw
Row"m stfob of " tylv. ("M the polm View INAII of cutting
pnq*rLkv mobtl of muwmy tat &Wyir4 co"lumN.
77i;.SLA 'WI&LtWWIW
"SOW JOA Diem
;AJ
1000000
U
pea
"Oe
see
woo
see
sloo
V IN S 8 A 0 2 V 9
6,04ASID

go
go
416 ell
go
go
Pik~sz;d T. S4,rxim-skity"
(Vial, 1M.No,10-11,pit 84--M). ( V it
of shvi DNA (owitaining'eltabon 0.87%. silicon 4l-302%,, nlarigarmw
sulliltur (1-0160%, OKwilkhmna 0-016%, chroiniuin 1.51 ~ linif
nivitel (1-4149110 bad for Its object th" dekemittatioork of the optirfluill
1#111 film, awl a slotiv of ilk" offevi (of thiii 14,1111writ.
lin- still the . M.18 t,,.. on the hink-lolibillf %. now) hithilbown, an
41 " ill*, rfferl it( the troilwratorr on il.i.
merhanival ltrulvertivit. MitiOninin ooirfaiv hikphw~ %%is. .,bittill,41
bV #11killirbilIg f,,,, &,W)*r (!.. file bJkJdJl* tittlittif
1~,ftig that n-otintumilded ill tho A.M.N.T. (itow A.N.M.) standurtim
Vor ulaxitnunk dut:Mlity. the juenchilis tenilicrattin- mhould In,
lowemil to W V. wild the holding time tmbled. The hardnom
irrinitined unclistigM by tolikilmim at 'up W HAVC. slid it then
fell five Hoo-hwull C units on tenilwing as 211WC., Illistelluently
rrinaining un&vw-,Avd when the tempering trinlirmturr iiiiii $it.
rfrow4il up to 300- C., above which the hairditr4a again dev",awill
Foir inipmved ductility imprring should be voitilurtai at MWC
a 10 1 L MIALLUNGIC" LlT%RhTW!! ~LJ!~WKATSM
losawa:.,.,
GO 0 0 0 0 0 0 * 0 0 0 0 0 0 0 a
iW-M
i
0 0 1 w
-00
lee
-0 0
400
40
409
too
lee
too
too
410o
do*
400
00

a C a a 4 a
u X L a 0 pq a I I W 12 A a . .1?itufm
r ST a a 0 Vs
l

Is's
**
M 'Iffca a
"
WO APO 4y. C*D#NS V. 400u"

'T;x ..at. gamLs On
luismilwams 9 11 -6 9 9

r

d
ap ma!p
sq, jo tmmlmdawa jqj uo n (1" im s* mql no Waa
*s idoatu -iu4nuwuO9jvOm"jO"W)O"'"
my OWUPSY4 w
-
jew am" aqj u"MO (n envmwum Swuld4s"
vajiMoid Iviluwq
00
002 jaqglq v onwIM-ma lunu- &qm Mom Q%L Pma wa mp
002 muldaMs ~qj jo imm M uo suo"qys umqmm ap p P%w
0 4~1 11139JUQ9 sqj~ -pq" aq plow jumm Omm OR% pm" ORS (n lx-

so= -walpwva ul"aw
tUnlp-A JO V.(IgO '91 -0 PMM.UW F NU -a
'
-
-
w
4n.1 .1
E
m
I ; 000
0
'
St-0
r
p
IOU pip 1-" -0
%094
7. 0
0 *~
laryu 'UR40-M-0 usni"a 10/112 .0 womw 'Yowo-mo
Olg I
i
p 00
0* anamm %g9.0-09.0 uoqM :puWuw on oopiwduloo )0
0
s
00
0 4k. " 1
illtull Jluj.,Aqtqj aqj ujqjjA samej st" saM uO luessigan I
Ad o0
,
o Oid Q%L Mr-Oll 01
-1-ils P mt~ 10 ) (" t
e-
00 'I'lm) -.1 'N p MR w4 VOW" vp I I to "Pom
W
�
~ 0*
4
. q
*
pm P" pww =Pam p
A 000
100
00
*0
A

00
-
- 00
7
641
f #140
w A i roe
0000000000 00001
01
a 6 * 0 0 6 CD rv as rp rp a a a a is 0-0-0 0 0 0 0 0 #1

0
l
,
T
1 9 So is u isw5tr a Ill aAll vSO a 0 &1
,
IOU a 43 a age

A
0
0
.0.9-M
-voe
A c4pl" -
00, -- ps
00 A
l
0o'
00 ir I ......
l
Admim sawsmio ai
m
1"b..
1157 1

00 54 In It Itruw
1
vw1irfa
w II
, a
'rIwrt UFItt. .00

00 .00
0: 00

000 00

o: IS 09

00
see
'00
'go

'69
oes woe
too
w
AV
Rol ltall 41101 A I a ad 0 a Sir IN 9a
14wil ISO v
am,
it 01091 an
0 0 & &* * 0 0 * 0 * 0 0 0
4440000000006 0000000 00 0 ** 0 * 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0 0
of oiee 0 0 *Go 000 000000 006i

MARGOLIN. G.I., inshener; DIIOMDOVSKIY, B.A., inshener: ORMS, P.I.,
inshener.
Junction lines in shaped steel castings. Stal' 7 no.1:58-62
147. (KIRA 9:1)
I.Xirovskiy tavod.
(Steel c&Btings)

~sm= C006-- Rd/O-03465101310011000310006
alWoo"I Sp~
.of toebrAma a 614120) or"Y'

BWKHIN,- A.S.; BDRODZYUK,- G.G.; LESHCR1NSKIY, A.A.; OKSMARO, L.K.;
KOSMINSKIY, O.F.; MANUSHKIN, A.Ye.; MILEVSKIY, Yu.S.;
DRIATSKIY, N.M.; IrASIL'YEV, V.V.; LIVDVICH, A.A.;
OBUYEVSKIT M S j moicz P I. A. ; OKSIAN, A. K. ; KKEL G S -
1. M. ; VASIL I YEVp L. N. (deceas
GINTS, YU.K ';'VASIL'YEV, G.K.; LUGOVSKOY, N.Ye.; KlRILWV,
Ye.V.; STRUYKINA, N.S.; LEVINOV, X.G.;BLOKRIN, A.S., otv.
red.; GURIN, A.V., red.; SLUT'SKIN, A.A., tekhn. red.
(K-1920-frequency telephone aynbnj Siatema Yysokochas*tnogo
telefonirovaniia K-1920; infomatsi~innyi sbomii~. [By]A.S.Blokhin
i dr. Moskva, Sviazlizdat, 1962. -U9 p. (MIRA 16:4)
(Telephone)

~ -
Bolero rndio receiver. P.1'
RTIOAMATOR
Wargzawn, 'oland
Vol.9, no.1, J n. 1959
Mrnthly List of has' Eurcnerin Accessions n(-e-,[, -- j~- A -' - C, 'Vo-' .`~, no.4
.T-ne 1959
Uncl.

TEMIER, Jan, mgr Inz.; ORLEWICZ, Boleslaw, mg.- inz.
Selection -~ tole,-!Lnce --~f the components -f the heteradyre ci-rc~--4t
of superheterod.,ne receivers. Prace Inst. teletechn o rio,1:5'7-7o
162.
1. Zaklady Had"owe Im. M.Kasprzaka, W!irszawa.

MUT, Jan, ingr ir..-..; OPLi-wil-, bz~esldwp 1114.
Influence :A' c.---( u.", rstray --oipavItan-t- on the frprjupn:~y -.Firlj"Ft
ratio of radic, recei I rx1ti-ed in sf-ries. Frace. Inst
t-gletschr 7 w).4-49--,(' 16 ~A.

CRLEWICZ, Jan, mgr
Synthetic indexes of economic efficiency. Rudy i metale
6 n0.10&453-457 0 *61,

TFK,ER, j an, mlrr Inz, , F,v" -, ll t6
Ar'r cr t.-.6 f 6 ~ I;i:-e -L-v- ',-I- Er-lne -1 -~ 1 *.0 -: ..- . -i~
p,. I B': ,j ct ; - nj a I r , -~ 1 6 1 * P. C tin tj -% -, ... , 1. ' -! - . '4 * , '. -
p, , ' . r,.! .. -
1. Ilubralt-.eA MAY 2-1,

ORLEWICZ, Jan,,mgr; IWINSKI-WISNIOWSKI, Gerald
Mechanization of accoanting in nonferrous meta-Ilurgy. Rudy i motale
8 no.2:58-60 F 163.

Q=WICZI Jun, Mgr
Economic deveiopment aspects of th~- a0afer:~JUS Me";~Aro-~y ~~: . ~--
the 20 year perlod. Rudy i metcle 9 no. 7: 377 .38' J-' 164-
-L I
1. Virector for Eooru.:rii . irc-bl -.Tm, AstwciLOA-)n of No nf ~ r r', ., ; - i - ~,,
and Metallirgy, Katovi-;e.

cliJIT"Z 1 j arl y mgr
!,7-0: , ~m of . -p ',! j m ~, , ' r , - - I tl* ' - - ' ': ' . . - ~!- -1 ~
. - it. :1
71 1, -. .- *. 'T~ - - -. ;. , - -~ - -
ml.r.' np in.] me, ~' ` - ;l ~- , '- .- ~
"I mr 165,
1 if)

ORLIC, Djuro
Npidemics In Serbia in the first half of the 17th centa" as
reported by the Dubrovnik Government. Srpmkj arh. celok. lek.
84 no.4:543-549 Apr 56.
(HISTORT, 4EDICAL
epidemics In Serbia In 17th century (Ser))

ORLIC, Dj.
Dubrovnik reports about epidemics in Serbia in the second half of
XVII century. Srpski siph. colok. lek. 85 n0-3:366-372 gar 57.
(HPIDICKIOIOGT, hist.
epidemics in Serbia in XVII century (Ser))

VOTRUBA, Jaroslav, Inz.j ORLICEK, Wenak, dr. .^Sc.
Enterprise analyses of the effectiveness of ImprrL and
export. Podn org 18 no.l2t546-548 D 164.
1. Ministry of Foretp T-rade, Prague (for Vortuba)
Research Inatitute of Foreign Trade, Praipia tfor OrIIr-,i,I,.

FORM, Margit, dr.; ORLICSEK' J0280f
PunctiOnal tYP96 Of ths Hangariam country towns, Poldrajzi ort
12 no&2tl67-199 1163,
41
1

ORLIGSEK, J0Zsef
Gazetteer coral-iLing work of the Central Statistical
Office. Stat szemle 42 no.5:519-530 My 164.
1. Group Chief, Central Statistical Office.

au=r;gm at Me Imind, & 7
)iai4
-_ Ch"
-boa
St 'ti
of
Hin south fuld Am
w
j~.Cn x4fiwo
0' the Tatia dii ttio .vAor krch Is-situ&W,
ka wwdo a the r h
)i -whkh 4r*
erly wfW3 sirt'itim the In Ithe
thg d,'
tba. rid -the
w of -$Uri At lcis*wy
pas a
ca cr_qkidd_
observcd, we'to the -wA
phkdip,_
F*tda -an low
ir

ORLICZ. 14.
"Profeaeor XugAnius2 Ro-wr; nn obitnpryll. p.1, (GAZETA ~'ISRPWATCRA Vol. 7,
No. 2- 1peh. 1q54 IInrpzawa. PolAnd)
d-
SO: Monthly Met of 7--st Munnegn Acppsslons. ( Y-UL) .LC. Vol. 4. No. 4 .
IAW 1955. Uncl.