SCIENTIFIC ABSTRACT YARGULYANTS, G.S. - YARIN, L.P.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001962120017-2
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 1, 2001
• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

YARGULOYA-NTS, G.S., inzh.
Centralize the supplying of glass plants with^polishing
materials, Stek, i ker. 21 no.709-40 JI 164.
(MIRA 17j1O)
1. Stekoltnyy zavod "Proletariy.11

8/057/62/032/007/010/013
B104/BI02
AUTHOR: Yarcyn, Ve SO
-i
TITLE: Laminar flow of a conducting liquid in a homopolar tube
PMODICAL, Zhurnal tekhnicheskoy fiziki, v. 32t no. 71 1962, 883-890
12EXT: The isothermal flow of an incompressible liquid in a homopolar tube
of finite-length (G. V-. Gordeyev, A. I. Gubanov, ZhTF, XXVIII, 9, 1958;
xxix, 6, 1959; M. F. Shirokov, Fizicheskiye *osnovy gazodinamiki, -
PhysiIcal bases of gasdynamics - Fizmatgiz, 1958) is studied here for the
case where the side walls play an important role and the Hartman number 11
in amall. This tube consists of two coaxial electrode cylinders. The
.,ends -of thio tuba aro.nealed by annular dieleatric caps. The space
S); betpeen the cylindorn iv filled with a liquid, Neglecting the axial
and radial velocity components, a systoln of-oqwtiona for the velocity
field is obtained in first approximation.by-expanijion wlt~h roupoot to-
H2 2
M2. For /4n < QgLI I V /_ QLI v and M2 < I,. it is shown that in f irut
1 0
approximation only,a.r.adial current appears, H, is a constant having
Card 1/2

S/05 621032100V0101013
Laminar flow of a conducting liquid ... B104YI3102
the dimension of a magnetic field etrengt~, L, is the charaotoriatio
axial length, V. aD q2/L in the characteristic velocityp L I is the
0 0
characteristio radial length. The radial velocity depends on the ratio
of the radlif the velocity maximum being nearer the inner electrode.
With ~ = rj/r2 (approximating to a tube of zero wall-thicknees) the
maximum shiftd towards the middle of the space between the electrodes. *
A coefficient of hydraulic resistance is introduced, and it is Bhown that
the effect ofthe end caps of the tube on this coefficient depends not
only on the height but also on the transverse dimensions of the tube.
There are 2 figures.
SUBMITTED:* April 21, 1960 (initially)
November 21, 1960 (after revision)
Card 2/2
-:77-

-L 17o4-66 94T (1) /iWT(m)/D[P.(V)/T/EWP (t) /EFI)-2 /EWP (b) IEWA (c) IJP(a) JD/4
ACCESSION NR: AP5021078 UR/0288/65/OGO/OO2/0103/0109
V, Y Y, Sir ~Yf Sir
AUTHOR: Drokin, A, I.; Sudakov, N. I.; Sidorov, F. K.; Yarichina, K.
TITLE: Magnetic crystallographic anisotropy and losses due to rotary hysteresis
In sin le crysta IT f cobalt Iron ktdtgf~,,
SOURCE: AN SSSR., Sibirskoye otdeleniye. Izvestlya. Seriya tekhnicheskikh
nauk; no. 2, 1965,--103-109
magnetic anisotropy, crystal anisotropy, magnetic hysteresis, sin-'
gle crystal, ferrite, cobalt alloy, iron alloy
ABSTRACT: Object of the study was investigation of thedtemerature dependence
of the aniso,tropic constants for single crystals of cobalt'& roWe rrite s over a
broad temperature interval, the effect, of thermomagnetic treatment on the curves'
for the mechanical moments, and losses due to rotary hysteresis. The samples
had the following composition: :Coo,p Feo,11 Feo, 04 (with 1. 2-1. 4 mole%
excess Iron). To eliminate internal stressed, the samples were annealed for 24
hours at 600C. with subsequent slow,cooling. The constants of magnetic cryitallo-t"
Card 1/3

L
ACCESSION NR: AP5021078
graphic anisotropy were determined by measuring the rotary_ mechanical moments'-,.
acting on the-sample in the field of a rotating electromagnet. Measurement error
id not. exceed 31o. Temp ature interval was from the temperature of"boiling
oxygen to.the Curie pointi,"Losses due to rotary hysteresis were determined by
planimetric measurement of the area between the curves for the mechanical mo
ments during forward and reverse rotation of the magnetic field in the plane.
Error -was 6- 81o. Magnetic sat
uration was determined by a ballistic method, and
the initial magnetic permeability by the resonance method at a frequency of 10
m
rgacycles. The first constant of magnetic crystallographic anisotropy for the
o
ferrites tested increases with a decrease in the temperature, at first slowly and
then, In the temperature interval 400-200K, rapidly, and then again slowly, alwar
remaining positive. At room temperature, it is equal to 2. 9. 100 erg/cm3; at i
the temperature of boiling oxygen it is 7. 46,106 erg/cm3. Thermomagnetic treat
ment of a sihgle crystal (heating from the temperature of boiling oxygen to room
temperature in a field of 10, 000 oersteds) causes inducod anisotropy. At room
temperatures and above, losses due to rotary hysteresis have normal character. 1
They increase. with an increase in the field, attain a maximum, and then decline
ard 2/3,
C

L 170
ACCESSION NR: AP5021078
to zero. 'At low temperatures, these losses are very great and do not completely
disappear even in a field of 40, 000 oersteds. As a result of thermornagnetic
treatment, losses due to rotary hysteresis decrease, their maximum shifts to the
side of high fields, and they disappear- in lowgr fields, "In conclu we expresiji!
our dee alinWf~
p indebtedness to-T. M. Perek and A.'A. Askochens f for furnishing'
us the samples of single crystal ferrites. " Orig, art, has: 3 formula3 and 6
figure.9,
ASSOCIATION- Institut fizikii. Sibirskogo otdeleniya AN SSSR, Institut tsvetnykh
metallov im. M.' I. Kalinina, Krasnoyarsk (Institute of Physics, Siberian Branch
AN SSSR M. L Kalinin Institute of Nonferrous Metals, Krasno
Y-Y,
ieb63
SUBMITTED: ior ENCL: 00 SUB CODE: SS
NR REF SOY: 005 OTHER: 014
Card
3/ 3

DROKINO A.1,; SUDAKOV, N.I.; SIDOROV, F.K.; YARICIIINA, K.V.
Magnetic crystallographic anisotropy and losses on rotatIonal
hystereeis in single crystals of cobalt ferrites. Izv. SO AN
SSSR no.6. Ser. tokh. nauk no.2:103-109 165.
(MIRA 18:11)
1, Institut fiziki Sibirskogo otdeleniya AN SSSR, i Institut
tsvetnykh metallov imeni M.I. Kalininav Krasnoyarsk.
LIE--

Neurology --Far
1475, PAT110MORPHOLOGY OF T1IF CENTRAL AND PER11111FRAL Nrltvous
SYSTEMS IN TOXIC FORMS OF EPIDEMIC HEPATITIS (BOTHIN'S Do-
EASE) AND IN ATROPHIC CIRRHOSIS OF THE LIVER (Russian text) -
Y a r I g I n N. E. Dept. of Pathol. Anat., Yaroslavl Med. Inst.. Yaroslavl -
ARKH.-FATO-C.7-1 955, 20/3 (21-29) Illus. 7
Changes in the central and peripheral nervous system were studied in 6 fatal comes
of apidemle hepatitis and in 0 cases of atrophic cirrhosis. Although only 4 of the
cases with liver cirrhosis had a history of recurrent jaundice, all were regarded
as having resulted from viral hepatitis. In both groups of cases the lesions of the
CNS were more pronounced than In the sympathetic and parasympathetic nervous
oyoteme; the most advanced neuronal dystrophy was found in the wall of the 3rd
ventricle, in the mAulls oblongate and in the subcortical nuclei. The glia was not
studied In detail. In acute hepatitis all lesions were more severe than In atrophic
cirrhosis.- Wilson -Dearborn, Mich. J~V, 8)
z d
V

MINI, 725
Organizatsiya i planiravaniye vlodoovoshchnykh predpriyati.Y (Organisation Y2
And Planning Of Fruit Arid Vegetable Enterprises) Moskva, Gostorgizdat, 1952.
240 p. illus., diagrs., tables.
-!A

YARIKHOVIGH. K., starshina averkharochnoy aluzbOy.
Roller pan. Tanklat no.5:30-51 Yv 158t, (MIRA :L1:0,)
r~A
(pans)

-sve--
~WICII 9 ~11- f 0 ~Iavs rkh srochnoy sluzhby
Portable apparatus for instruction in shooting, Voen, vest, 39
no. I:SM1 A 160.- 1 (Shooting, Military) (KERA 14:2)

15-57-5-5773
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 5,
p 9 (USSR)
AUTHOR: Ya ri k ov , G. M.
TITLE: Stratigraphy of the Upper Carboniferous Rocks in the
Bond of the Don (Strati rafiya varkhnekamennougoltnykh
otlozheniy Donskoy Lukil
PERIODICAL: Uch. zap. Stalingr. gos. pod. in-ta, 1955, Nr 4,
pp 171-177.
ABSTRACT;
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The author considers a new outline of the stratigraphy
of the Upper Carboniferous rocks in the bend of the
Don. The outline differs considerably from that of S.
V. Semikhatova ZP-oiski i razvedka gazovykh mestorozh-
deniy, Tr. VNII(YAZ'a, Gostoptekhizdat, 1951 (Exploration
and Prospecting for Gas Deposits, Transactions of the
All-Union Scientific Research Institute of the Gas
Industry, State Scientific and Technical Publishing
House of the Petroleum and Mineral-FUel Industry, 1951),7
-XIM
bN
vr~ S.

15-57-5-5773
Stratigraphy of the Upper Carboniferous Rocks (Cont.)
The lower boundary of the Kasimov series is drawn at the base of a
sequence of clays, containing pebbles of limestone, that rests on
the eroded surface of Myachkovo, limestones. This sequence is easily
recognized on drill-hole logs. The Kasimov series is divided into
three zones: 1) the Protriticites zone contains limestones (28 m
thick), subdivided in'to four units; LI) the Triticites montiparus zone
(37 m thick) has a lower unit of argillaceous dolomiFe-al-R-an upper
unit of aphanitic limestones; and 3) the Triticites arcticus and T.
acutus zone (47 m thick) is composed of argillaceoiis sandy r cks,_
dolomites, and limestones. The upper boundary of the Kasimov series
is placed at the base of the first clay unit. The Gshelian series
contains only the two lower zones. In the Triticites stuckenberai
zone (55 m thick) are found argillaceous rocks and imestones. The
Triticites jugulensis zone (0 to 18 m thick) is commonly eroded in
T upper part. The-total thickness of the Upper Carboniferous Is
180 m. The author presents a diagram comparing the sections of
Upper Carboniferous rocks of the bend of the Don according to him
and according to Semikhatova.
,Card 2/2 V. N. B.

15-1957-10-13549
Translation from#, Referativnyy zhurnal, Geologiya, 1957, Nr 10,
p 13 (USSR)
AUTHOR: Yarikov, G. M.
TITLE: Stratigraphy and Lithology of the Carboniferous Deposits
of the Interstream Area of the Kurtlak and Tsutskan
Rivers in the Western Part of the Stalingradekaya Oblast'
(Stratigrafiya i litologiya kamennougollnykh otiozheniy
mezhdurechlya Kurtlak i Tsutakan v predelakh zapadnQy
chasti Stalingradskoy oblasti)
PERIODICAL: 1Uch. zap. Stalingr'. goo. Ped. in-ta, 1955, 17r 5, pp
129-135
ABSTRACT: Drilling programs have uncovered Kashirskiyj Podollskiy,
and Myachkovskiy horizons of the Middle Carboniferous.
The Kashirskiy horizon consists of organic limestones
containing brachiopods and foraminifers. The Podolfskiy
horizon is composed of interstratified'units of lime-
stone, clay, and w- r1 in its. lower part (17 m). Round-
Card' 1/3 ing of brachiopod fragments and of foraminifers indicates

15-1957-10-13549
Stratigraphy and Lithology of the Carboniferous Deposits of the
Interstream Area of the Kurtlak and Tautskan Rivers in the Western
Part of the 3 tali ngradakaya Oblast'
carbonate unit of rocks.
Card 3/3 D. A. Timofeyev
e~ 1 7&

15-57-5-5772
Translation from; Referativnyy zhurnal, Geologiya, 1957, Nr 5,
p 9 (USSR)

AUTHOR:
Ya
.........
TITLE: New Data on the Stratigraphy of the Upper Carboniferous
Rocks in the Bend of the Don (Novyye dannyye o strati-
grefii verkhnekamennougollnykh otlozheniy Donskoy Luki)
PERIODICAL: Uch. zap. Saratovsk. un-ta, 1955, Vol 45, pp 27-30.
ABSTRACT: The author gives new data on the stratigraphy of the
Upper Carboniferous rocks in the bend of the Don,
reported on earlier (see abstract 5773). This infor-
mation Is supplementary only in presenting a log, the
maximums of which are in close agreement with the
lithologic subdivisions.
Card 1/1 V. N. B.

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Inge:

YARIKOV t G.M. , kand.geol.ofyo-.mineral.ogichot3kildi nauk.. dotsent
-----------
Conditlons of oedi.-ventation during the l(ijer Carbonifs...x-7as pnr.'-~J
west of the Volga in Stalingrad Province. Uch. zap. V01g.
goo, 1>3d, inst's no*10.93-120 '59. ('AIM 14 -. 11)
(Volgograd Province-Geology, Stratigraphle)
T V
v'U

.-YARIKOV, G.M. kand.geologo--rUm eralogicheakikh nauk, d6ts-eKft-
Bour&q between the Davanian and Carboniferous in the Volga
Valley portion of Stalingrad Province, Uch, zaps Volgo goa*
ped. inst. no.10321+2.,243 1459, (141PA 1/"-] 1)
(Volgograd Province-GeoLogy, Sixatipaphie)

Position of the boundary between the Devenian and Carboniferous
in the Volga Valley portion of Stalingrad Province. Trudy
VNIGNI no. 19:99-111 159. (MIRA 13:12)
(Stalingrad Province--Geology, Btratigraphic)

yARIKOV, G*M.; MEL'IIIKOVA, A,,S-; NIK'T'NAO G.Po
Carboniferous sediments in western. Stalingrad Province. Trudy
VIIIGIII no. 19:112-151 '59. 1 Stratigraphic) (14MA 13-.12)
(Stalingrad Province--Geology,

YARIKOV, G.M.
----------------
Carboniferous sediments in the lower Khoper Valley. Geol. nefti i
gaza 3 no.9:43-50 S 159. (MIRA 13:1)
le-Stalingradakiy podagogichaskiy institat.
(Khoper Yalley--Geology, Stratigraphic)

MOROZOII, N.S,j-XARLKOVj_ G.Ms
Carboniferous sediments in the Don-Northern Donets inteTnuvep
Uch.zap;SGU 65:29-38 159. (KMA 16:1)
(Don Valley-Coal geology)
(Severnyy Donets-Coal geology)

FPMADANOVA, E.A.; BERLIN, Yu.M.; ORLOVA, I.N.; FADEYEV, M.I.; CHERNOVA,
Ye.N.; YAPIKOV, G.M.
Carboniferous sediments of the western part of the northern
Caspian ol'- and gas-bearing basin. (Trudy] NILnefte aza
no.lOsl82-222 063. IMIRA 18t3)
1. Nauchno-issledovateliskaya laboratoriya geologicheakikh
kriteriyev oteenki perspektiv neftegazonasnosti; Volgogradskly
nauchno-Inaledovatellakly institut neftyanoy i gazovoy promyghlon-
nosti; Uizhnevolzhskiy nauchno-iseledovatellskiy inatitut geologii
i geofiziki i Kuy..b7shevskiy nauchno-issledovatellskiy institut
neftyanoy promyshl~nnosti.

YARIK0V$_.,G.M.j 314IRNOV, A-V-
ialeogeography and sadl7enLatlon in the Ba,-17 Vias ir the VOlea "a2ley
portion of Volgograd Province. Geol. nef U i gaza 9 no.9:3t--4-1 S 165.
IN

_Tn
YARILOV, A.; AKIMOV, D.
OMMIK4.
The party organization In the effort to Inprove the vaintenance
of airplanea. Grazhd.9v. 12 no-9:7-9 S '55. NLRA 10:?)
(Airolanes--Kaintenance and repair)
(Communist Party of the Soviet Union--Party vork)

YARILOV, .,A
FOr,jLuh prinoiple objectivityp efficisnoy. Grazhd. av. 20
at
lojlo~jj*o 16Y0, (MIRA 16.
-12)
1. Nitchalinik politicheakogo, otdela. Momkovskogo, territorial'-
nogo upravleniya Grazhdanskogo vozdushnogo flota,
p',
V2

A UTHOR: Yarilov, P. SOV-26-58-11-37/49
TITLE- Flowers Turning White (Pobeleniye tsvetkov)
PERIODICALt Priroda, 1958, Nr 11, P 114 (USSR)
ABSTRACTt While white flowers are found individually among plants with
otherwise colored flowers, the author discovered areas of
tens of square meters covered with Chamaenerium angustifolium,
Scop., Epilobium angustifolium L., Aconitum excelsum Rohl.,
Geranium silvaticum L. and Delphinium elatum L. blooming
white instead of red, blue, etc. in the Arkhangelfs~aya Ui~tl.
the author tentatively explains this phenomenon by the pre-
sence of large amounts of differently-colored blooming plants
and the calcareous ground.
ASSOCIATIONt Arkhangallakiy loeotokhn1ohaakiy inatitut im. V.V. Kuybyoheva
(The Arkhangellak Forestry Institute iment V.V. Kuybyshov)
1. Plant pigments--Chemical reactions
Card 1/1 r, A I I

-YAH I LOV -P-p -0ya
YARILOV. Pad.
r7i; I
Prol1ems of reforestation under conditions'of mechanized lumbering.
(N()Ptimal dimensions of falling areas under conditions of mechanized
lumbering.* Elaureat Stalluskoy premii,doktor sallskokhozysystyenuykh
nauk] Y.G.Hesterov, Reviewed by P#IA,IArIlov)- Les.prom. 14 no16:32
Ja 154. (mm 7:6)
(Nesterov. Y.G.) (Forests and forestry)
7Z

TARIIDT F~.IYa
loading packaged mine supports on open rnilwnY core. Mekh. trud. rab.
11 no*12,32 1), 157. (MIRA 11:3)
1. Limendskaya loll operevaloohnsyn baxa tresta Dvinosplav.
(Mine timbering) (Loading and unloading)

0 0 0 0 0 0 0 0 0 4 0 9 0 0
4 Ot 1-1 W Y'0~-J-1- L PA At 9 M Uj,I S A-f i;.t
YFIKILVV
The role of uthophille lichens in wastherfail aysticlime
b*4 rock. ff. A. Yariloina. Prde4y 1947,
-U~-AftfrTIW6UITrre%-lew t
33
6
gives snalytical data on 3 species of liche", &I well sm Of
:10 the rocks on which thew grow. namely amphlboli, granite,
mks schht. Lichens seem to concentrate in their Wits
fig
L *CTALt.(,&(.XAj LfjfIj&jL4t CLA%%I#6C&TfCW
11 17
S i-;~;-O 0 f I if 1W 'i
0 t? 0 to or d Is If R 9 of tt a a Ot OW n I
'j ell 40 0 0 0 0 0 0 0
4.~
So*
t:00

yliglLOV-9,
,~;yvnits minerak in the first stages of
sou Ysrilcya,.Trp~l 1"ArAtwevoco 14J1.
- 110211OW) --Thr trantlor-
in, V. V. IWAICA"lli-34
mation 0 the ruck Is laltlal~l by , rv.14biliAnient tot It.,(
lower forms of lotophytti. The metsmorph"of the nick
IrAding to the fortrution of high altitude (Northern Cau-
Icagus) mrsdow "Is 6 traccri. M. ll~h

P hylolltlwai ityaWlitatlan Irk the "0. H. A. ljtrll*vv&.
tj,.& v AW. xisk S.S.8,R. 83,
rueux 44 chtrixWm ag*l were round to ctmtt*W # few grilins
of cludcvdiony In the form of phylolitharian v~i~ with
oil l1w periphery th4n in the center*. The repults Ind"le
progremyc aging of the Phylolithadn" -ttru and crystn'
of its opaque immnpn. Specimens from chanotens have -r
grutnaly above lbore frnul primitive "Is show few
in-larters of such high a. Probably the cryan. dtws mot
bAll Ott the chour-losly stage; "Our gril"s Wrrr 6"111.1 111.11
slu~wvd qijimililkv charartethl", (1, hl. K'MkLjt%A

YARILOVA, Ye. A.
111,11iner.ilogiccl Coo,poettion of Clipricozemci Zoil of 3tcp.~e the
Influence on It of Artificitl Afforeftt!tton rind Gr1j,.V-Fiald Cro?; Po-
tation," VoproFy trnvopollnoy oistemy zemladollya, Vol 2, pp 20~-266, 1953
Study of the. ininerr-logical composition of cherrmzem rind of its con-
tinental rocke nnd cover elby, led the puthor to the followine concluEionc
concerning fractions jacre tht,n one mUcron; proce-.sea Coverninr_ wenth"ring
I)e proceed r.
of ~rimory Pdrierpls under rux)ijitione of the EmennayEa Step lowly,
and content of feldoijor over sail profile remrins unvhi,nj:ed; In the upper
horizon of the chernozem secondrry qunrtz rjeciumilptea bpct,utie of crysti.111-
yation of vilica of plant remBins; In thp soil are (jbcerved mincruls formied
In plants and called "bibliths" by the nuthor, which relikte to phytolithtrirje
t 10
of 1-rosses compoEed of opal, FAliceous rikelete of diptomsceous 'Igve. Ur -j~r
minerpl compounds close to ferr.ut; bf~ydejlitv tire obrei-ved In B Uff
dark--g,rey soil. (RZhGeol, No 4, 1955)
suln-.11TO. (381, 7 Oct 55P

YAMLOVA, Ye. A* and PARFENOVA, Te* I*
"Nattzria Geochemical Transforinations bf Some Elevient:;.," a paper presented at
the 6th International Soil Science Congress, Paris, 28 Aug to 8 Sep 56
Library Branch #5

to v /)) bw.
USSR/soil Science. Genesis and Geography of Soils.
Abs Jour: Referat Zh-Biol., No 6, 25 March, 1957, 2P-430
Author Yarilova, E.A.
Inst
Title The Mineralogical Study of Subalpine Chemozem, on Andesite-
Basalt (Armenia).
Orig Pub: V sb: Kora vivetrivaniya, 1956, No 2, M., AN SSSR, 45-6o
Abstract: Development of the s oil-forming process on andesite-basalts
under subalpine conditions of the Akhmangan Plateau is accom-
panied by a vigorous mechanical and chemical decomposition of
minerals of soil-forming beds. Volcanic glass almost totally
disappears from the upper soil layer. In the fine soil mass
of the upper layer, there remains--o1% of fresh and -5% of
considerably modified andesite-basalt fragments. In the first
stages of soil formation, a large role is played by bacteria
and lithophile lichens. As a result of bacterial activity, a
Card 1/2
1-2

USSR/Soil Science. Genesis and Geography of Soils. 1-2
Abs Jour: Referat Zh-Biol., No 6, 25 March, 1957, 22430
border of fine crystalline calcium carbonate forms in thepores
of andesite-basalt. As a result of lichen activity in the form
of film existing at the end pres of andesite-basalt, a clayey
sticky brownish-yellow mass is formed, which penetrates the
entire section of fine soil and exudes in its pure form in a
characteriatic flowing manner along fissures, root-paths and
pores. According to x-ray structural data and thermal analysis
of soil fractions,.e. 1 m, this new formation corresponds to the
mineral beidellite. A characteristic differential peculiarty ofo
its tbermogram is the absence of a third endothermal peak at 850
The new formations include also biolites - minerals originating
,within the plants which return to the soil upon their death. A
secondary idiomorphic quartz which was found in the chernozem
studied evidently was formed as a result of the soil formation
process. The rest of the minerals found in the studied chernozem
belong to the components of andesite-basalt lava of the Akhmangan
Plateau.
Card 2/2

PARMOTA, Ye.r.; TARMOVA, Ye.A.
Synthesis of allophanolds In laboratories under normal te Tature
and pressure [with summary In 3nglishl, Pochrovedents no.4:80-85
AP 157. (HULA 10: 7)
1. Pochvennyy institut im. V.V. Dokuchayeve Akademil. nank SSSR.
(Allophane) (Soil colloids)

I T
YMI ~O
GORUUM~, N#I*,__YA111g'1A.,,g,.A.
Physics and mineralogy of soils discussed at the Sixth
Congress of Soil 'Sciqatiste (International Society of
Soil Science, First bommission), Pochvovedenie no.2:
105-108 F (MMA 10:5)
.1. PachvenW institut im..V.V. Pokuchayeva Akademil nauk SSSRs
(Soil Physics)
-n

TARIWTA, Ye.A.; PARMOYA, Te.l.
Newll formed clay minerals In soils Lwith summary in Inglishj.
Pochvovedenie no.9:37-48 S 157. (MIRA 10:12)
1. Pochvennyy institut im. V.V.Dokuchayeva AN SSSR.
(Minerals in soil)
ML M--
7

PAMMOVA. YO.L.- YARMOVA, Ye.A.
Taoks and methods of the microscopic analysis of soil minerals.
Pochvovedenle no.IP:28-35 1) 10. (HIRA 1231)
1. Pochvennyy Inotitut Imeni V.7. DolLitchayeva AN SSSR,
(Minerals In %oil)
~M

Country : U~SR
Category : SQil Science. Physical and Chemical Proper-
ties of Soils,
Abs Jour : RZhBiolej No 6, 1959, No 24583
Author : Itarilova Yeo A*
Inst : USSR.
Title : Mineralogical Characteristics of Solonetz
Soils in the ChernoZem Zone,
Orig Pub : Tr, Pochv, in-ta AN SSSRI 19587 53, 131-142
Abstract : By the micromorphological method with the
aid of microscopic sections under a micro-
scope and by t-he method of mineralogical ana-
lysis in iunersion liquiasq two solonetz
soils -.Ln the chernozem zone, rep:.,esenting suc-
cessive f;tages of the solonetz dexrel-pmental
process. A= chernozan soil., vex-o studied, The
development of the solorietz process over the
Card :L/4

Cotvn.1;ry USSR
Category Soil Science. Physical and Chemical Proper-
ties of Soils*
Abs flour '.9zhBioi.i No 61 1959, No 24583
In-3;-
Titj;e
Orig Pub I
Abstvact chernozem soil brought about important chFLn-
ges of the mineralogical composition In 50
years, Gypsum and tonardito.appeared; the
soil became enriched with Ca in the micro-
crystalline form due to the migration of the
solutions to the surface horizons. The for-
mation of iron-manganese-humus concretions
Card 1 2/4
10

Country i US,5R
Category t Soil Science. Physical and Chemical Proper-
ties of Soils.
Abs Jour : RZhBiol., No 6, 1959, No 24583
Author
Inst
Title
Orig Pub
Abstract takes place with greater intensity, thanks to
IV-he periodic advent of anaerobic conditions;
a dispersion of the minerals is observed, par-
ticular*&'.y c)4&.* crystalline quartz; there appea-
~?ed the absent-in-the~-chernozem mobile collo-
morphic arail.Laeaous mineral, According to its
properties and chemical composition the latter
is closaly related to fe.-Ovous beydeilite. The
Card 3/4

Coun"X-v : USSR
Categ:'r7 : Soil Science* Physical and Chemical Proper-
ties of Soils,
A s R~ur : 'PZhB iol No 6, 1959, No 24583
Aut 0-
T itl e
Orig Pub
Abal'Aract migration of this mineral from the upper hori-
zons to the alInvial ones are noted. The mi-
gration is accomplished, it seems, in complex
with fulvic acids and mobile humous acids. Spe-
cific secondary argillaceous minerals7 inherent
to the solonetz-soll formation only$ were not
found. N, I, Bazilevich
Card 4/4
n

YMIOVA. Ye.A.; PAMNOVA, Te.l.
Studies on characteristics *f cla.7 minerals in soil colloids Cirith
summary In English], ']~ochvededenie no.2:75-79 7 159.'
(MIRA 12:3)
l.PochvenW institut imeni V.V. Dokuchayeva AN SSSR.
(Soil colloids) (Minerals in soil)

ROfM. A.A.-,-YARILOYA, Ye.A.i USIWSKAYA, I.M.
Genetic ebaracterietics of the dark-colored soils of large
depr"tionfi. Pochvovedenie n0.8$1-13 Ag 60.
4M 13--8)
1, Pochvenrq7 Institut im. T.T. Dokucha7eva Akademii nauk
SSSR.
(soils)

PARFEITOVA, TO.I..;---TARIIWVA, Ye.A.
lossivage and podzolization. Pochvovedenie n0.9,01-15 3 160.
(MIRA 13.:9)
1. Pochvenn" inotitut im. V.V. Dokuchayeva Akademii nauk SSSR.
(Podzol)

YARILOVA,
-1,20MOVA. Ye. 1.
Clay minerals of soil colloids. 1011. zhur. 22 no.2:237-242 Xr-AP
16o. (MIRL 13:8)
1. Pochvennnyy institut AN SSSR, Moskva.
(Colloids) (Clay)

PARFENOVA., Yelena Ivanovna;YARILOVA Yakaterina Ardenlyqvna;
AMTAYEV "-;--j otv. red
ANTIPOV-Y , I -i- -, =0 ..; PAVLOV, AJI..,
red. izd-va; HYLINA.. Yu.V.j, tekhn. red.
(Kineralogical invastigations in soil scioncal Mineralogichookio
issledovaniia v pochvovedenii. 14oskva) lzd-vo Akad. nauk S&;R,
1962. 203 p. (MMA 15:7)
I* Akademiya, nauk Tadzhikskoy SSR (for Antipov-Karatayev).
(Minerals in soil)

YARILOVA, Ye.A.
Micromorphology of soils in the Tergeni Hills. Pochvavedenia
no.203-39 F 163. (MIRA 16:3)
1. Pochvennyy inatitut imeni V.V.Dokuohayeva.
(iergeni Hilla-Soilp.)
-wp
--N

Ye.A.
Works in the field of soil micromorphologyj review of the work
of a symposium. Fochvpvedenie no.11:104~-1,10 N 163.
(MIRA 16:12)
1. Pochvennyy Institut imeni V.V. Dokuchayeva. -
-7-7777777

1.1 1 _ -f A
Problens of t1he ?,*h fn-,enla-,-Ima~
Soil Scientist-j. PoahvovadenI.A no.5a].01-106 My 165t
(MIRA --t8t5)

YARIN, - E.
PlyLng and hourly bouns wage system at Altai machinery
Ar
marrafacturing p1ants. Blul.nauch. inform.; trud i zar,
plata 3 no.1:37-41 160. (mm& 13:6)
(Altai Territory-Machinery industry)
(Kltai Territory--Bonus system)

ZICTOEMMN, V.; 'WIN. E.
Using an amateur notion-picture camera for the study of elezents
of operations of short-duration. Blul. nauch. inform.: tz-ad
i zar. Plata 3 no. lo:34_~7 16o. (MIRA 13:12)
(Motion pictures in industry) (Motion study)
Obtal cutting)

OR.
YARIN, E.
The bonus system should be operational. Sots.trud 5 no-3:123
Mr 16o. (MIRA 13:6)
1. Altayski7 nauchno-isoledovatel'skiy proyektno-tekhnologicheokiy
instltut.
(Altai Territory-Machinery Industry-Production standards)
(Bonus system)

YARIN, E.
Using group wage payment systems in the machinery manufacturing
plants of the Altai Economio Region. Biul. nauch. inform.; trud i
zar. Plata 4 no-9:39-41 161. (MIRA 15:1)
(Altai Territory--Wages--Machiner-y industry)

141ROSHNICHEIINOY S.; YARIN, B.
I
Methodology for determiaing the nwaber of adjusters of metal-
cutting equipment. Biul.nauch.infom.: trud i zar.plata 5
no.8:41-45 162. (141RA 15.-7)
(Rubtsov-sk.-Mbtal-cutting tools)

,YARINp 1.
Individual and group wage systems in machiner7 manufacturing.
-Sotsotrud 8-no.3.*73-76 Mr 163. (MIRA .16:3)
(Wageis-Macihinery industry workers)

YARIN, G., makhanik.
There must be no smote from factorychimneys. Prom.koop.no.11:6-7
N 156. (HLRL 9:12)
(Smoke prevention)

Al..jP(j
NKI 8r SOURCE CODE - W3_/O
6001840-0-"..- UR/6374/66/o 1166 0.51
AUTHOR: Yarin, t. I.,
-'-ORG, Experimental Institute of Industrial
. C-ntral Scientific Research and Planning
Stru tures. Moscow (Tsentrallnyy nauchno-isoledovatellskiy i proyektno-eksperimentall-
-__p)7_institut promyshlennykh zdaniy i sooruzheniy)
TITLE: Investigation of deformation properties of certain -el-aatic--r-e-fn-f6ra-6d-Dlastic
SOURCE: Mekbanika polimerov, no. 1, 1966, 43-51
TOPIC TAGS; polycrystalline film, crystal anisotropy, deformation rate, capronet
surfacetension, Poisson.coefficient
ABSTRACT: The article deals with an experimental investigatio"f the laws of de-
formation of elastic filmq~of plastics reinforced with sa pronel-Tabric. The experi-
ment showed that the Teforliations of these films cubjected to biaxial tension are
in close agreement vith Hook's law for anisotropic materials. Methods of experi-,
mental determination'of the Poisson ratio-of the material under study are presented.
Orig. art# has:- 6,f1gures, 13 formulas, and 4 tables. (Based on author's abstract.]
INT)
_M -CODE: llf_ SM DATE,: 22mar65/ ORIG REF: 007/ MH PXF: 001/
CWd uDel 676;.Lq.o24.4.62l.5
JM.

YARIN, L. P., ARTMM, L. Y.., VMISI L. A. , and MSHKAREV, B. P.
"Thermal Problems of a Boundary Layer at Heterogenoun and
Diffusive Combustion.11
Report submitted for the Conference on Heat and Mass Transfer,
Minsk, BSSR, June 1961.

ARTYUKH, L.Yu.; BULIS, L.; KASIIK=Vp V.P.; 7ARINj L.P.; ATENKOVp S.,
tekhn. red.
[Thermal boundary layer problems in the case of beterogenous and
diffusion combustion; Conference on Heat and Hass Transfer., Minsk,,
January 23-27, 19611 Teplovyo zadachl pogranichnogo sloia pri ge-
terop,ennom i diffuzionnom gorenii; soveahch6nie po teplo-i masso-
obmenu, g. Minsk, 23-27 ianvaria 1961 g. Hinsks, 1961. 18 p.
(M3RA 15:2)
(Boundary layer) (Combustion) (Thermodynamics)

S/124,/63/000/002/OL2/052
D234/1)303
-Ydrin I?
_7
~'Thermal c oriditions f --bu -7of-unmixed stases
o rning
'lm - -no. 2. 1963, 84,
PERIODICAI: Referativnyy zhurnal, Vekhanl.
abstract 2B561 (IZV. 437 X=SSR. Ser. energ. 1961,
'no. 1(19), 47-55 (Summary~in Kaz.))
TQIT: The author considers a diffusion flame front situated
in a plane turbulent boundary layer formed during mi,.ding of a fuel
stream with the oxidizer.. The front is assimied to be a surface of
weale. discontinuity. Tcrq)eratvrc and concentration of components of
the fuel -mixture have discontinuous derivatives on the flame- surfacq
corresponding to the velocity of the chemical reaction of burning,
wbdch in given as an Arrhanius function of the awrage temperature
and a linear function of the average concentration. Outside of the
front the author looks for a self-modeling solution of stationary
equations of momentwn, heat and mass transfer in.the turbulent iso-
baric bou-ndary layer of compresaible liquid for the averaged quanti-
ties. CriticaL conditionn of ignition and e!ctinction in the burning,
Card

3/124/63/000/002/012/0.52
Thermal conditions of burning ... D234/D308
front are obtained. The author considers the effdct of radiation
nditions, for which the con-
from, the flame front on the critical co
..ditions at the discontinuity were modified accordingly. In the pre-
Sellice- of I-Lbat losa by radiation the interruption of burning becomes
possible not only during the intensification or- the process but also
in the case of low intensity when the influence d heat loss increas-
es.
"~ibstractarls note: Complete translation

S/O 31 /62/000/004/001/001
B102/B104
AUTHORS; Yershin, Sh. A., Yarin, L. P.
TITLE: Aerodynamics of a turbulent diffusion flame yet in an
accompanying flow
PERIODICAL: Akademiya nauk Kazakhakoy SSR. Vestnik, no. 4, 1962,
46-51
TEXT: A nozzle system, consisting of honeycomb Input, diffuser, damping
chamber and nozzle chamber with a specially designed combustion chamber
was used.to study the behavior of a turbulent diffusion flame jet in a gas
flow whose flow rate in varied. In the combuction chamber two burners
are arranged oppositely; the "secondary" gas sprayed by the opposite
burner is mixed with the burning products thus forming the tnrbulent jet
outside the nozzle. The stability of the jet is achieved by an intense
preheating (13000K) of the gas mixture and by an annular stabilizer
placed in front of the nozzle. Pressure was measured in the jot by Pitol
tubes and MPZ (MPP) micromanometern, temperature with PtRh-Pt thermocouples
Card 1/2

S/031/62/000/004/001/001
Aerodynamics of a turbulent... B102/B104
Tr?-30-6 (PR-30-6). The operational characteristics of the apparatus
were determined carefully. They were used together with the p,t measuring
data to determine the aerodynamic structure of the flame and its
surrounding regions. The investigations showed that at any pressure of
the accompanying flow and different concentrations of the burning profile,
the excess momentum hac a maximum at the jet axis and decreases smoothly
in radial direction.. A minimum van observed*outside the flame front at
.'-he profiles of dynamic pressure. It is shifted with respect to the zone
of highest temperature., Both facts are explained by an asymmetry of the
boundary conditions for velocity and temperature. Special ex-periments
were made to study the effect of the rate of the accompanying flow on tile
aerodynamic structure of the jet. The temperature was found to decrease
nonlinearly with increasing flow rate, the flame length increased. In both
cases the curves become saturated at higher flow rates. The effects can
be explained within the framework of the general theory of free turbulence
in isobaric flow. There are 4 figures and I table.
Card 2/2
q~,Ta;l q-Z S( 2::- ir6cul bf, 4 -t

L 16735=a EPA(b)/EWT(I)/BDS AMCIASD Pd-4
S/124/63/000/004/022/064
AUTHOR t Yershin, She j Yarin,
A study in the aerojn2E4cs of turbulent diffusive flares of finite
dimension
PERIODICAL: Re.ferativnyy zhurnal, Melchanika,, no, 4j 1963., 95, abstract 4B655
(Izv; AN KazSSR. Sere energo, no. 1(21).. 1962,, 74-87)
TEXT: The study involves a thooratical computation and an experimental approach to
a turbulent diffusive gas flare. On the theoretical side, velocities, temperatures
and concentrations are calculated on the assiLnption of an infinitely great reaction
speed and identity of the mechanism of turbulent exchange of pu1so, heat and --ater-
ial within the flare and the free streanw. The com,-mtation is made by reduction to
the equivalent problem in thermal conductivity for a flare of finite diinension; the
dynamic problem is solved on the assumption of an unaltered field rho u sup 2. 11he
additional assumption of the constancy of the ratio of reduced coordinates (of the
type of "Prandtl's turbulence numbert') permits the use of a single empirical connec-
tion - the pattern of pressure along the flare axis - in transfer to plane surface.
Di the experimental porVLon of the study, results of measuring the profiles of the
pressure head and temperature within the flare upon burning of natural gas in aIr
Card 1/2
51.

L 1673 5-63
S/224/63/000/004/022/064
k study in
there is also a photograph of theflare. The experimental profiles are
co iled in conjunction with computations obtained rith the hydrointeGrator, and the
- qn. ,
satisfactory agreement is noted, as it also is for the computed and expertmental
values for maximun temperature for the f1mme front site. The feature vihich distin-
gudshes the study froin other investigations of the aerodynazdas of a gas diffusive
,-flare consists:in the fact of obtaining a continuous. picture of a flare of finite
d:Lnension with minimum of empirical.data; this was possible bedause of the use of
the equivalent problem from the theory of thermal conductivity. There is a bibli-
-9
-------- --
[AbstracterTs -note: Complete translation.]
-Card 2/2

YERSHIN, Sh.A.; YARIN, L.P .._(Alma-Ata)-.
"Diffusion flames in laminar and turbulent wake flows."
report pr esented at the 2nd All-UnIon Congr*ss on Theoretical and Applied
Mechanics, Moscow, 29 Jan 5 Feb 64.
- - - -- ------------
fA
A

i -.
Wd..W
I "
12, 1
I
1 4.-`
'T-' ,
FB T"
4
wi
~~Jm,
9
Mmi
I
POR
1.

MET
zoom
ALITAMV, D. X.; SAKUM, Z. D. I TAM, L. P.
'got shielding of iurfacos vith reguiar mcro-roughraie.*
repDrt vibuitted for 2nd =-Unloa Comf oc Rost Mass Trawf4r, KWk, 4-19
msy 1964.
?over Inst, A.M. K&OW.
7 7-.
Ed 1~1--l!a,-= L z~ L
y,

15Z

7117

"Transfer processes in turbulent jets in the presence of a highly intensive
chemical reaction."
report submitted for 2nd All-Union Conf on Heat & Mass Transfer, Minsk, 4-12
may 1964.
Power Inst, AS KazSSR.

PL
ACC.Mi AP5026026- SOURCE CODE- UR/0405/65/000/001/0052/0058
AUTHOR: Yer (Alma-AIA)
shin i Sh. A. Yarin L.P. (Alma-Ata)
ORG: None
TITLE: The calculation of diffusion combustion within a turbulent flow of compressible gas
SOURCE: Nauchno-tekbnlchesldye problemy gorenlya i vzryva, no. 1, 1965, 52-58
TOPIC TAGS: c Be
ombustlon4bl arch, compressible gas, gas flow, turbulent flow, subsonic
flow, supersonic. d_ow-,Wo_w velocity, combustion, combustion gLs dynamics, boundary layer
flow /,S
ABSTRACT: The combustion of gas In the turbulent boundary region was investigated by
numerous authors, but the studies were zoncerned mainly with flow at the currents low sub-
sonic velocities. However, there are grounds for assuming that combustion of unmixed gases
with high-velocity sub- and supersonic flow offer advantages over explosive Ignition of homo-
geneous mixtures. The present authors developed an approximate gas-dynamic method of
calculation of the combustion of unmixed gases in a plane-parallel boundary layer of high-
velocity flow, using the methods of the theory of turbulent jet flow of compressible gases.
The results obtained 1) describe the displacements of the flame front.as a function of the
velocity of the Incident flow; 2) show the distribution of the velocity, Mach number, thermo-
dynamic temperature, and damping temperature across the cross section of the boundary
Card
1/2

YENJ 10 1.:, 1 It, L. 11.
lAi0bu,lon burning in a 3=inar boundary layers X.-iucb,-t,3kb,j.-z-rb1,
gorei vzrpra PO-21101-105 '65,
(AURA 18:10)

75;f P -1K
.

S~Z

SUBHITTEDi 2 6 4
ENCL aa

8
ALIYAROV, B.K.; SAKIPOV, Z.; YARIN, L.P.
Some characteristics of flow along highly rough surfaces. Vest.
AN Kazakh SSR 21 no.4:80-84 Ap 165. (MIRA 180)

KONOPLYANIIIKOV, A.G.; KUDHYASHOV, Yu.B.; YAMODMIKO, S.P.
Regeneration efficiency in mice irradiated with W Me,., protons.
Dokl. AN SSSR 161 no.6:1448-1440 Ap 165. (I.IJRA I&II)
1. Moskovskiy gosudarstvennyy universitet i Institut giglyeny
truda i professionalInykh zabolevady AMN SSSR. Submitted Decertber 2,

L 23~81-66 Et-IT(1)/E',Vp(m)/EWT(m)/ETC(f)/EPF(n)-2/EWG(m)/EWA(d)/T/ETC(m)-6/ERA(l)
j'ACC NRI AT6006930 SOURCE CODE: UR/0000/6,5/000/000/0433/0440
Yarin., L. P.
AUTHOR: Alijarovi Bs K,; Sakipaj,
ORG- Power Inqtiiute,AN KszSSR-,,'Institut energetiki-AN KazSSR)-
TITLE: Jet shielding of su rfaces with regular macro-rougliness
SOURCE: Teplo- I messoperenos. t. II Toplo., J m Iassoperenos pri
----vzaimodeystvii- tel--a potoksmi -zhidkostey -i--gazov-- (Heat -and mass-transfer.
vi 2: Heat and mass transfer in the interaction of bodies with liquid
and gas flows). _14ins1c, Nauka i tokbnike, 1965, 03-hljo
TOPIC TAGS: gas jet, surface property, nozzle design,
/ made in a unit
ABSTRACT: Experiments with jets of transformer oV1wAr_10:_,
consistinC of a reservoirs a qp P bo (EcL_nozzle~' and a bollow brass
._.p a 1 1 qj~ P
rod with a diameter of 20 mm placed concontricol -_ with respect to tbo
nozzle. The jet isouod from an annular gap (5 mpl~ formed y the nozzle
and,tho rod. A study of 'the jur~g_dZmpmicg and beat transfer In an
axis-puictric-semi-Infinite airfjot wi:tb fully developed turbulent flow
conditions was carried out in a simila-r unit at various values of
initial velocity and excess tempersturo.,/Measurements were made of the
velocity distribution (air and oil JetsY/and of the temperature (air jet)
'~T

--L-23981-66
,ACC NR- AT6006930
qt different transverse cross sections. Regular micro-rougbness-was,
obtained-by-placir~g-steLI-tubds of.-different diameter on a smooth plate
tranaverpe to the flow. In those exporimontsj measurements were made of
the distribution of the total pressure, -the velocity, and the statiaticoll
pressure at different cross sections of the Job, Experimental results
are exhibited in a series of curves. It is dernonstrntod that, with a
somi-inflnito jet propogating 91ong a rjurfoco with raeulor mnoro-
roughness, the. maximum value of f riction at the wall exists at values of
the parameter R approximately equal to unity. It con be expooted that
the dependence of the beat transfer ooefficient.on N will be of on
analogous nature,- Orig, art* boa: 5 figures on&2 tables.
:H2
_EiIL

0
ACC NR, A116020555 SOURCE CODE: UR/0414/66/000/001/0079/0087.
AUTHOR: Vulis, L. A. (Alma-Ata); Yershin, Sh. A. (Alma-Ata); Yarin, L. P.
(Alma-AtaY-
ORG: none
TITLE: Calculation of a homogeneous turbulent gas flame
SOURCE: Fizika goreniya i vzryva, no. 1, 1966, 79-87
TOPIC TAGS: combustion, gas combustion, turbulent combustion,
ABSTRACT: An analysis was made of the combustion of a premixed stoichlometric gas
mixture which discharges into air or an inert gas. It was assumed that the reaction
rate is finite and the maximum temperature is at the flame front. Equations were
obtained for the combustion temperature and the location of the flame froat as a
function of the calorific value of the mixture and the initial flow velocity
(1-54.2 m/sec). Plots of the combustion efficiency as a function of the initial
gas flow velocity and the calorific value of the mixture showed that an increase
in the flow velocity and %decrease in the calorific value result in a decreasa in
the combustion efficiencYA As an example, the flame cone angle of a hydroci~rbon-
air mixture was calculated and verified by experiments in a Bunsen burner. A for-
Card* 1/2 UDC! 536.46+532.507

ACC NR, AP6020555
6
mula was also obtained for calculating the turbulent burning velocity as a function
of the.gas dynamic as well as the kinetic parameters. Orig. art. has: 15 for-
niulas and 6 figures. [PVI
SUB CODE: 21/ SUBM DATE: 27Jul65/ ORIG REF: 005/ OTH REF: 001/ ATD PRESS:

L-31 "Ut'i -oe) FVip W hqia' *Y; W
ArC717 rtiig-023749 SOURCE CODE: UR/3149/6u, )/003/Oio6/,3i,,-,
AUTHOR: Aliyarov, B. K.; Sakipov, Z..; Yarin, L. P!-
ORG: none
TITIE: Experimental study of the principles of the propaga.;ion of turbulent,
se=iconf ined jets, developing along smooth and tubular, flat surfaces,
SOURCE: Alma-Ata. Kazakhakiy nauchno-issledovatellskiy institut energetiki.
Problery teploenergetiki i prikladnoy tepl'of'i z-i'ki-," _n'o_-.__ 3','- 1966, 1o6_123
TOPIC TAGS: '~ir jet, aerodynamics,velocity profile, temperature profile, tubular
flat surface, smooth surface V%~V%Ae%n
ABSTRACT: Experimental studies were made of the aerodynamics and heat exchange
during the propagation of a semiconfined /air jet.along a smooth and a microrough
flat tubular surface (see Fig. 1) to determine the cooling effect of the air jet on
the surface. The temperatuvs and velocity profiles, friction coefficient, and the
jet cooling efficiency coefficient were mewured at temperaturm T = 300-650K,
u 14.5-29 m/sel!, u = 12.9-35.2 m/sec, b =
0 10 mm, with overheating parka-ters
T.,/To (2.00-3.00)0, concurrence parameters mu = u./uo (0.44-1.68), and head
pressure ratios m U2 = H./H (0-07-1-00). An analysis of the experimental data
indicates that the"aerodynagic and heat-exchange principles governing the flow of an!-
~i ~4

L 077 -4-66
ACC NRiAT6023749
a
1. Lq.:U.:
b
Fig,l. Flov-diagram, of a
CM-
semiconfired air jet in a
current flow.
a - Along a smooth surface;
b - along a microrough
(tubular) surface; b - widthi
of the jet exit noz&; t
temperature-, p-- den i
ty-,
u - velocity of the flow;
main flow; o-. -.jet.

L 38774-66
ACC. NRs 06023749
air jet alOpg a microrough surface in a concurrent flow are similar t'0 those
'characteristic; for the. boundary layer formed during the flow of a jet along a rough
plate. A similarity-in the velocity'and temperature profiles in various cross
sections of the jet',permits an approximate, semi-empirical calculation of its
parameters using the previously postulated theory of turbulent jets (Abramovich,
G. N. Teoriya t4rbulentrWkh strui. M., Fizmatizdat, 196o). Orig. aif;-has:
13 figures and 2,'tables. [PSI
SUB C61E: 20/ SUBM DATE: none/ ORI~ REF- 003/ OTH REF: 002
'Card' 3/3-4
Tt4%

L 08569-6-1 941(m~/OAT(1)/W(m) -VV-1JW1JWD1Y
ACC NR, AP'6-0-3-2-9-11-57 -s b U'R-'C-E'-C 0-D E' Ull/0031/66/000/-009/-004"8/0050
AUTHOR: Yershin, Sh, A*; Rybalqva., R. P,; Xaz~in, Le P._
ORO: none
TITLE: Calculation 'of a 4ffusion flame in the transient flow region
SOURCE: AN KazSSR. Vestnik, no. 9, 1966, 48-50
T*OPIC TAGS: combustion, diffusion flame, propulsion, combustion rate',
transient flowp flow velocityp turbulcnt flame
ABSTRACT: The length of diffusion flames in laminar flow regimes is
directly proportional to the/e;as flow velocity. With increasing flow
velocity, the flame becomes f~-r-bulent i-nd the regime is transient. At
high flow velocities, the flame is fully turbulent, and the length does
not depend on the flow velocity. The turbulent and laminar regimes
have been previously studied, but the transient regime, which involves
both molecular and turbulent transfer, has not yet been thoroughly
studied, In the present study, experiments in the tranqient regime
7~
were made with carbon monoxide and hydrogen combustionVa d the follow-
Ing formula was derived for calculating the flame length:
d
XT Re + Kir Re O~IRO
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ACC W AP6032975
let
2
-Fig. 1
Figs. 1 and 2. Comparison of calculated and experimental ro-
sults an the dependence of the flame length of the Reynolds
number
Fig. 1, Carbon monoxide; Remax - 3300; Recr - 2700;
kT - 1.115.10-3; a - 0,00018151,
Fig* 2 114drogen; Rem&X -'2700; RGcr *2700; kT - 0.3.10- 3
a - 03015
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ACC M AP6032975
where Sc is the schmid'tnumber; KT, empirical coefficient In the ex-
-pression for eddy diffusivity; If, flame length; d. burner diameter;
U,' gas"'floW Velo*city; allowing for the physico-;-chdmi-
cal properties of the gas; D, diffusivity; Res Reynolds number; and a
is given by
(Rema K, 5C 11
(where Remax the Reynolds number corresponding to the maximum flame
length); a can be determined experimentally. R* is given by
D,,"D,+(D,-Dje-*'R*,; where DMT is overall molecular-eddy diffusivity,,
DT*i6 thie"'66dy-di-Maivitys and DM is the molecular diffusivity, grige
arts has: 2 figures and 4 formulas. [WA No. 683
SUB.GODE: 21/ SUBM DATE: none OHIO REP: 008/ OTH REFs 003
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ACC NRt AM16609- SOURCE COD92 UR/017016610111005/0630/0633
AUTHOR: Vulis,_L._A.,* Yarin. L.171_
ORG: none
TITLEt Electric modeling of the combustion process by means of low-temperature plasma
SOURCE: Inzhenemo-fizitheakiy zhuinal, v. 11, no. 5. 1966, 630-633
TPPIC TAGS:--Acombustions gasc - - - - - - - - -
V1
e
ABSMCT: Direct experimental studies of an ytical solz&ns to conbustion
vt
rocesses are replete with difficulties. Thereforeo-tbe feasibility of electric
p
t
simulation of gas combustion processes has been'.investigated (see Figs. I and 2). Th
beat release in the flame is simulated by the'loule heat evolved by passage ~f
current through as $as which serves as themodeling substance. The electric currents
passing through the low-temperature plasm vast be sufficielitly small so that heat
release Is the only effect* Applied " wall as induced magnetic fields must be
absent. -An an~exs*le, the Ignition of a combustible mixture flowing along the plate
with and without allowance for combustion, Is conaldered* 'By this method using the
43
MCI 536446