SCIENTIFIC ABSTRACT KRUCHINA, N.YE. - KRUCHININ, YU.D,

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000826710012-4
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: December 30, 2016
• Document Release Date: June 19, 2000
• Sequence Number: 12
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

TELIPUKHOVSKIYI V.B.; DMITIMIKO, T.A.; ZELE211M, I.Yo.; KOSTYAKOVA, G.K.;
RAMOWDIP B.P.1 BORISOV, Yu.S., otv. rod.;__ARqq11PA, li.Ye.,,rod.;
FEDOROV, A.G., red.; LYUBUSHKINA, To., red.; 7WOROVA, I., tekhn.
red.
[In the land of wide-open spaces and heroic deeds; youth in the
virgin lands] V kraiu prostorov i podvigov; molodezh na tsoline.
Sbornik dokumentov. Moskva, Izd-vo TsK VIXSH "Molodaia gvardiia)"
1962. 278 p. (MLiA 15:5)
(Agricultural laborers)

FUNSHTEYM, Ya.N.; 601UM, 13.1a.; r,hUCHINA S.K.
High-temperature natural-gas cementation. Avt.prom. 29 no.9:
41,42 S 163. (MM 16 19)
1. Kinakiy avtozavod. (Cementation (Metallurgy))

KRUCHIWAv V.
fters in a great interest in Pollsh export goods. Vnesh torg,
43 no.9tll,-12 163. iMIRA 16tlO)

-7 - -,T~ TV T' -'.--r-)77FT'P --7 rT
"Electromechanical Device for Computing the Mean Moments of the Passage of
Stars During Observations.," The International Association of Geodesy;
Abstracts of the Reports at the XI General Assembly of the International
Union of Geodesy and Geophysics, Moscow, Izd-vo AN SSSR, 1957, 63 P.
A Photoelectric amplifier makes it possible to measure the duration of two parts
of a contact (rectangular output signal) into which it is divided by a pulse from
a clock. Computing the moment of a star's passage is accomplished by a formula
given in the text. Observttions could also be conducted of high mgnitude stars
producing deformed edges of the contacts. Means of increasing the efficiency
of the device were also indicated.

e'7f
33-4-10/19
AUTHOR: Kruchinenko, V, G., Platonov, Yu. P. and Sukhov, V. B.
TITLE: An elec ronic mechanical device for determining the
mean moments Of stellar transits during observations.
(-Elektronno-mekhanicheskoye vychislitellnoye ustroystvo
dlya Doluchegiya dr momentov prokhozhdenly zvezd
BEII
vo vr%M i n
PERIODICAL: Astr asufty uraal, 1957, Vol. 34, No.4, pp.609-612
ABSTRACT; In the astrometrioal laboratory of the Pulkovo (USSR)
Observatory a device,was designed and constructed which
enables the evaluation of the mean moments of stellar
transits during observations by averaging the moments
of contacts of a photo-electric amplifier or a contact
micrometer. To increase the efficiency of the scheme,
an electro-mechanical calculator-printer was set up
and this transmits the values of T given by Equation 1
either to a printing device or a hole puncher. The
calculating block employs decatron trochotrons (type LP-4)
allows the results of observations to be reduced more
quickly.
There are 2 figures, no tables and no references.
SUBMITTED: December, 14, 1956.
Card 1/2

33-4-10/19
An electronic mechanical device for determining the mean moments
of stellar transits during observations.
ASSOCIATION: The Main Astronomical Observatory of the Academy
of Sciences of the USSR. (Glavneys Astronomicheskays
Observatoriya Akademii Nauk SSSR)
AVAILABLE: Library of Congress
uara 2/2

L1296
S/035/62/000/010/055/128
A00IIA101
AUTHOR: Benyukh, V.V, Gavlovskaya, A. A., Konopleva, V...P., Krivutsa, Yu.N.,
Kruchinenko, V. G., Sandakova, Ye. V., Terent'yeva, A. K.
TITLE: Photographic observations of meteors at.the observatory of the
Kiyev University in 1957
PERIODICAL: Referativnyy zhurnal, Astronomiyal Geodeziya, no. 10, 1962, 62,
abstract IOA459 (" b. rabot po Mezhdunar. geofiz. godu. Kiyevsk.
.S
un-t", 1961, no. 1, 3 - 15)
TEXT: Double photographic observations of meteors were conducted by means
of fixed four-camora (Dow= mm, F-250 mm) Installations during all clear moon-
less nights of the second half of 1957. A shutter rotating at a speed of 1,400
rpm was mounted in front of the cameras at one of the points. 141 meteors wbre
photographed, of which 14 from two points. The results of processing 10 meteors
.are presented in the article. The photographs were measured with a KjJM -3
(KIM-3) measuring machine. Five meteors were processed on a "Strela" computer,
the remaining ones - manually. Photographic photometry of the meteors was carried
Card 112

A/035/62/000/010/055/128
Photographic observations of meteors at the... AOO1/AlO1
out by relating to diurnal stellar trails, and for some of them. also
Ing to images of artificial meteors. The tables yield -the results of
Ing flight Instants (with an accuracy of 2 - 29 min), coordinates of
velocity and braking in the middle sectiori of the visible trajectory,
-atmospheric velocity, altitude of the start, maximum brightness and
visible trail. Stellar magnitudes, masses and corresponding densities
atmosphere are given for individual points of the trajectory. There are
ferences.
P. Babadihanov
(Abstracter's note; Complete translation]
by relat-
determIn-
radiants,
extra-
end of the
of the
8 re-
Card 2/2

--t -1
1j1273
S/035/62/ooo/olo/019/128
AOOI/AlOl
AUTHORSt Kruchinenko. V. G..Moyaya, R. I., Bayrachenko,.I. V.
TITLE: Radar observations of meteor streams
PERIODICAL: Referativnyy zhurnal, Astronomiya I Oeo~ezlya, no. 10, 1962, 41-42,,
abstract 10A307 ("Sb. ra~ot po Mezhdunar. geofiz. godu. Kiyevsk.
un-tto, 1961, no. 1, 26 - 36)
TEXT: The Klyev University conducted radar measurements of meteor numbers
on the 4-m wavelength from January 1, 1958, to December 1, 1959. 33, 670 meteors
wqre recorded during 6,4,90 hours of observations. Equipment characteristics are
!tj.follows: amitterls pulse power, 80 kw; pulse duration, 8jusec; frequency of
pulse repetition, 50 cpsireceiver sensitivity, 10*9v. The nine-element antenna
of;the "wave channel" typ'e at a height of 7 m over the ground surface is orient-
ed In east-west direc~tion. Reflected'signals were photorecorded on a film whose
mov'ement speed was 90 mm per hour.*For each meteor were determined the time of
appearance, distance and duration of reflection V. During the period of active
peteor streams, mass (m) distribution of meteoric bodies was obtained. The
I
ard 112

S/035/62/bW/010/019/128
Radar observations of meteor streams A0011A101
The relationT-- Aml.15 is assumed, where A Is a function of meteor velocity 'v.
The differential mass distribution of meteoric bodies is described by the re-
lation: N-m-s. The following dependence of meteor luminosity I on m, v and ze-
nith distance of the radiant zR is adopted: i-mOcosz, as well as the scale of
masses In which a +2m,86 meteor Is originated by a meteoric body with m-1 g,
v-10 km/sec and z R.0. A +2T4 meteor corresponds to duratlonT- 1 see. In the
GeminJistream, parameter a varies systematically during the visibility of the
stream. The values: 2.5; 2.2; 2.0; 1.7; 1.4 and 1.8 are obtained for the suc-
cessive nights of December 9 - 15. For the Arietid stream, the 4verage value
of a - 2.23. In the Perseid stream of 1958 the a-value changes from 1.83 on
August 6 - 8 to 1.65 on August 11 - 14. In the 1958 Orionid stream a - 1.80,
and in the 1958 Quadrantid stream e - 1.72, There are 8 references..
V. Lebedinets
[Abstracter's note: Complete translation]
Card 2/2

ACCESSION NR: AT4034464 S/3091/63/000/002/0040/0055,
AUTHOR: Noysya, A. I.; Kruchinanko, V. 0.1 Dayrachanko, 1. V.
TITLE: Influence of the directional diagram of an antenna on the observed mass
distribution of meteors
SOURCE: Klyev. Universitat. Sbornlk rabot po Mezhdunarodnomu geofizicheskom godu,
no. 2, 1963, 40-55
TOPIC TAGS: astronomy, meteor astronomy, meteor, antenna directionai'diagram,
meteor trail, meteor mass distribution
ABSTRACT: There are several methods for determining the exponents In the mass
distribution law for meteors when using data from radar observations. One of the
most common methods Is based on the measured distribution of the duration of radio
meteors. The derived theoretical expressions are correct only for the case of
reception of signals from a narrow sector of the directional diagram. in a real
case reception always -is from the entire region of the diagram and the amplifica-
tion factor of the antenna changes as a function of direction. in this article
the authors attempt to take Into account the Influence of the antenna directional
diagram In the vertical plane on the results of radar meteor observations. The
ar
cagiTh begins with a discussion of certain problems In the theory .of scattering

ACCE55ION NR: AT4034464
of radio waves on meteor trails and the method for selecting the range of electron
densities and masses; this entire section Is based almost entirely on non-Soviet
published sources. The authors present the derivation of the principal relations
required for solution of the.problem and discuss the method for processing data.
Solution of the problem required the introduction of many simplifying assumptions.
The problem Is limited to the Influence of the antenna directional diagram In the
vertical plane; the similar problem for the horizonpal plane will be considered In
a separate article. A final expression Is obtalne4 for the Integral law of mass
distribution of the recorded meteors with the lnflu'pnce of the directional diagram
taken into account. The problem also Involved a comparison for different antennas.
differing from one another In the form and degree of directivity. It was found
that the distribution of meteor bodies by mass differs when the Influence of the
directional diagram Is taken Into account from the distribution law actually ex-
isting in space. The difference Is particularly well-expre3sed in the region of
small masses. The influence of the form of the directional diagram Isralatively
small; this Influence also Is expressed most clearly In the region of small masses.,
Orig. art. has: 60 formulasg 12 figures and I table.
ASSOCIATION: Klyevskly universitat (Kiev University)
SUBMITTED: 00 DATE ACQt O7Kay64 ENCL: 00
Cord 2/2 SUB COOF: AA NO REF SOVI oo4 OTHER: 007

ACCESSION NRi AT4032228 8/3089/63/000/005/0293/0297
AVIMORs.-Kr"hineakol V.~qq_Noymys, R. I.; Bayrachoultog 1. V.
TITIZ: Determination of the true number of meteors using radar observation data
SOURCE: AN UkrSSR. Mexhduvedoestvonny*y geofisLcbeekly kouLtat. &ofislka L
astronomiya; informatsionny*y byullaten', no. 5. 1963, 293-297
TOPIC TAGS: meteor, meteor astronomy, astronomy, radar, antenna directional
diagram, upper atmosphere, radio meteor
ABSTRACT: In processing the radar observations of meteor activity It to necessary
to convert properly from the observed number of radar echoes to the true number
i of meteors for a certain sector of the sky. In this process it is necessary to
i take into account the influence of the three-dimensional form of the directional
j diagram of the radar antenna. In this paper the author cites the -?rincipal
formulas used in connection with radar observations of meteors and derives a
general expression for the integral distribution of meteor bodies by masses with
allowance for the influence of the directional diagram. The necessary formulas
are cited for conversion from the observed to the true number of radio meteors.
On the basis of the cited formulas, and with certain simplifying assumptions, it
Card 1/2

ACCESSION NR: AT40132228
is possible to determine the total increment of the earth's mass during a year
from the falling of meteor matter. The derived annual value is approximately
1,120 metric tons. Orig. art,hai: 22 formulas and I figure.
ASSOCIATION: AstronomLeheskaja obematorLya, KLyevskogo, gosudaretvannogo
universitsta, (Astronomica.1 Observatoryg Kiev State University)
SUN= Dt 00 DATE A0Qs 16Apr" INCL: 00
SUB COM A& 14D RJW SOVt 006 0TMMt 001
2/2

(I boil i es
IE

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GTIV-R k1 0 R F ~1910
C.,d 2 12
J~
Vt Al

MWCHININ. A.7.
Forestry survey map of the U.S.S.R. on a 42,500-000 scale. Bbor,
at. po kart, no.9:69-71 156. (KLRA 100)
(Forests and forestry-Aspal

%ol 'M
os
t 14
big

3(2)
AUTHORs
TITLEi
PERIODICAL:
ABSTRACT:
Card 1/3
soy/6-59-2-11/22
Kruchinin, A. F.
Region`a`r~~~egionallnyye karty;Jesov)
Geodeziya i kartografiya, 1959, Nr 2, PP 51-56 (USSR)
Previous forest maps of individual areas of the USSR were
schemea of low practical value. In recent years new forest Map
of some areas were drawn. In this connection it turned out to be
necessary to improve the method of compiling maps and to work
out them more in detail. At present, the following scales are
specified for regional forest maps: 1 t 200000 - 1 s 1000000;for
southern areas of the European part of the USSR.1 : 200000; for
Central Russia 1 : 300000 - 1 9 400000, for North Russia, Ural
and some southern areas of West Siberia 1 : 400000 - -1 : 500000,
for the northern area of West Siberia, the southern area of
East Siberia and the Far East 1 : 500000 - 1 : 750000- For
forest maps the same projection should be used as for topo-
graphical maps. Between the margin of the map and the border-
line of the area the following data must be entered: soil map,
table of wood resources arranged according to the various kinds
of trees, register of "leakhoz" (foreat industry establishments)$

Regional Forest Maps
soy/6-59-2-11/22
forester's districts, data on the volume of wood-cutting ac-
cording to kinds of trees. The following general geographical
data must be entereds continuously water-bearing rivers of a
length of more than 2 cm on the map scale, lakes and reservoirs
of more than 2 mm2 on the map scale. From among irrigation
channels only the main channels should be entered. In parched
areas all lakes should be entered with data on the chemical com-
position of water, and the map should contain wells and other
artificial buildings. In scarcely populated areas all populated
spots, even single buildings, buts, log cabins, hunting-boxes,
etc must be listed. Furthermore, all forest roads and paths
must be registered In scarcely populated areas. All forest sec-
tions of more than 1 am2 on the map scale, burnt areas, clear-
ings of more than 4 mm2 must be represented. In southern areas
where forests are scarce also woods of less than 4 he are to be
marked by one tree sign. All State nurseries, irrespective of
their size, all protective wood zones, all valuable woods, all
remnant kinds of trees should be registered. Furthermore, the
Card 2/3 maps should contain the administiation offices of forest eco-

Regional Forest Maps
sov/6-59-2-11/22
nomic districts and forestry trusts, the offices of all
forestry districts, transfer points, etc as well as the wood-
processing industries, forest research stations and those
lumber runs which are used also after work has been finished.
On floatable rivers the spots whore floating begins, the kind
of floating as well as the buildings, harbors, gratings for
floating logo, and transfer points should be listed. Also the
indices of wood resources (in cubic centimeters per I ha) must
be mentioned. The author describes the most useful method of
compiling the special distribution of details on the map devised
according to respective experience. There are 2 tables.
Card 3/3

Improving the performance of recording manometers. Knergetik
10 no.10s-U 0 162. (MIRA 15 -.12)
(Manomoter)

.KRUCHININO A.M.
Overall redesigning of raw coal feeding systems. Snergetik
11 no.10-9 Ja 163. (KMA 16i1)
(Boilers)

K%U,-HININ, A.M., msh-Inis"
T 15 '~d-
Duvice for scraping surfa~:ea. Er,~rgetlk 12
I'MIIA 17:4)

\1
L; I U 117 1 r- -I T- I
Milt f~,,

4L

ACC NRi a6o~7497 SOLMCE CODE: URI/Ol37/66/0OO/OO4/BO2O/BO2O
!ALMIOR: Kruchinin A. M.
ITITLE: Dynamics of a closed system for automatic control of electric-arc DC instal-
lations used in heating an intense stream of gas
SOURCE: Ref. zh. Metallurgiya, Abs. 4B127
i
IREF SOURCE: Elektrotermiya. & xuuchno tekhn. sb., vyp. 46, 1965, 45-49
C.TA S: automatic contr- electric arc, heqtjing C&^tz~
0 'r .1
ABSTRACT: A three-layer chani. model of the arc is used for studying the dynamics of
a closed automatic control system for regulating an electric-arc unit which heats
twisted stream of gas on 'direct current with stationary turbulence in the channel.
This model may be used on an anolog computer for simultaneous time solution of the
energy balance equation, the complete equation of the electrical circuit and the equa-
tion of motion with regard to nonstationary processes in the arc. Studies on the basig
of the proposed model showed that an automatic current stabilizer in combination with
a filter choke in the arc circuit provides stable arc combustion with delivery cbarac-
teristics and high quality stabilization of the electrical and thermodynamic heater
conditions even when there is no active resistance in the arc circuit. 3 illustra-
tione, bibliography of 11 titles. V. Pryanikova. [Translation of abstract]
SUB CODE: 09
1'enfol III n(It .
UDC: 669.621.365.5to5.011.66

~)revcrit'ltq, I,rrt!n lojues in t;,,~? trtr,,-,,,ortftton. Lvt- 42,

1. KRUCHINIM, 1. EKG.
2. ussR (6oo)
4s Building, adobe
7. Prom. experiments vith adobe. Bell. strol- 3 no, 3- 1947.
9. 12A= Lis& of AMI&A Accessions Library of Oongress, Karch 1953. Unclassified.

inth,
k-fficiency of basic trends in the modern! --t!on of wChins
tools. Vest. mnehinostr. no.5i?'---75 MY '64
(6A l7s6)
F

KRUCH I N N, I . A -z)
ffen',~, oo-n _-i dete.-m':'. r4 er.-I.-p- Of
"in moder-nizar.lon of equipment. prclzr"', 18
no.71,i7-38 .;1 164. ~~K-RA 17.9)

KRUCHIIIIN, I.G.
Measuring moments of journal-type friction-testing nachinep,,
Ilauch.-takh.Inform.blul. LPI no.11:96-102 158.
(MIRL 12:11)
(Friction--TestWO (Testing machines)

V..,-).; I'A"CUIT"IN, I.,*,.
between tie torue roller tltn loaci~
Neft. khoz. 39 no-9:7-12 ~ .61. (MIRA 15:1)
MrhWril I s)
. --:f z

DIYAKCVY B.F.; IMASHEV,, N.U.; KRUCHI.H.IN', K.V.j KOGAN, A.B.:
EZ140DEIIIYA113KIT WW~ V"-P.; TRIFONOV, N.K.
.0 V.V.; TO
CHMPANOV, V.11.; VYALOVA,, R.I.
Southern 14angyahlak is a large new oil-bearing region. Geol.
nef ti I gaza 5 no.12:4-11 D 161. (mm 2,4:n)
lo Voesoyuznyy nefteyanoy nauchno-inaledovateltakiy
goologorazvedocheakoys upravlemiye i trest Mangyahlakneftegazrazvedka.
(Mangy9hlak Peninsula-Oil fields)

SHVEDOV, G.V.; A.I.; CHIMNO K.1,1.
Current state of the geological and geophysical study of
the Mangyahlak Peninsula in connection with its gas and oil
potentials. Trudy VNIGRI no.21SS431-446 163.
(MIRA 17:3)

KRUCHINIHO K.V.
Now data on Maikop eediments in the scruthern Mangyohlak
Peninoula, Trudy VNIGRI no.220. Gool. abor. no.8:52-,64
163. (MIM 170)

VYALOVA, R.I.j DIYAKCV, B.F.; DWHLIV, N.U.; KOZ 'MODEM' YAHSKIY V.V.l
KRAYXV, P.I.; KRUCHININ, K.V.; TOKAREV, V.P.; TRIFONOV, K.K.;
CHEREPANOVp U.N.
Southern-Mangyahlak oil- and gaa-bearing region. Trudy VNIGRI
no.218:7-50 163. (MIRA 17:3)
ago

GeOlOgY and, Prospects for finding oil and gas in the Bekebash-
kudukakoye uplif t of the MwWahlak Peninsula. Trudy vNIrFa
no.186t286-306 161. (KRA 150)
(MwWahlak Peninsula-Petroleum geology)
(Mwwahlak Peninsula-Gas, Natural-Geology)

K1&'YS11EVp P.A.; KOZLOV, Ye.G.; EEDDZERTSEV, A.G.; VOLMUSKIY, D.Ya.;
GRACHEV, V.A.; 4RUCHDID1, M.I.; FILD"OLOV, K.N..; KHMMEN, A.I.;
ANDMEV, P.P.; OVOWILM, V.F.; CERSHAROV, S.V.; MAYEVA, A.P.)
red.; BALLOD, A.I., tekhn. red.; PEV22M, V.I., tekhn. red.
[Economic efficiency of mechanization in agriculture] Ekonomi-
cheskaia effektivnost' mokhanizatsii sellskogo khoziaistva. Ho-
skvaj Izd-vo sellkhoz,lit-ry, zhurnalov i plakatov 1961. 230 P.
I NIRA 15:5)
1. Vsesoyuzrqy nauchno-iseledovatel skiy institut ekonomiki
sel'skogo khozyaystva(for all except Pyla ova, Ballod, Pevzner).
(Yam mechanization~

KRUIC.HININ, M.S., otv# za vypuskj VOROTN1KOVA, L.F., tekhn. red.
(Regulations for -the factory repair of locomotives) Pravila za-
vodskogo remonta pamosov. Moakvn, Vass. lzdatellsko-poligr.
ob"odinenis M-va putei soobahcheniia, 1962. 350 p.
(MIRA 15:5)
1. Russia (1923- U.S.S.R.) Glavnoys upravionlye lokwotivnogo
khozyaystva.
(Locomotives-Maint,enance and repair)

MAECIEMKO, V.P., inzh.; BELKIV, M.N., inzh. (deceased); ZAVIYALOV,
G.R., inzh.; DZEAVOICHN, T.V., inzh.; CYETIZECV, _`~.F.j inzh.;
FOLYARCRUK, V.S., kand. tekhr. nauk; aUCHINII:, M.5.1 Inzh.;
AVDUKOVI M.I., inzh.; NELINIKOV, V.Ye., red.; ~ILVKDEVA, H.A.,
teldiri. red.
[Fanual for the locomotive encineer] Rukovodstvo parovoznoru
rashinistu. Izd.2., inpr. i dop. Pod obahchei red. V.S.
Moliarchuka. Moskva, Transtholdorizdat, 1963. 3F9 P.
(MIR.A 16:12)
1. Russia (1923- U.S.S.R.) Minister3tvo I:utey soobshchaniya.
(Locomotives--Handbooks, manuals, etc.)
Ti-

KRUCIIIIIIII, lj'.S.p inzh., otv. za vyp.; DAOZDOVA, lv',D.p tekhn. red.
[Regulations for the maintenance and repair of locomotivea
in depots. Superseding the regulations on the current repair,
maintenance and servicing of locomotives approved by the
Ministry of Railroad Transportation on March 8. 1957] Fravi-
la dopovskogo remonta i soderzhanlin parovozov. V otmenu
Pravil tekushchego remonta2 ukhoda i soder2haniia parovozov.,
utve.-zhdennykh MPS S/Ill 1957. Moskva, Transzholdorizdat
1963. 311 P. (HIRA 16:12~
1. Russia (1923- U.S.S.R.) Minifiterstvo putey f;oobnhcheniya.
(I,gcomotiveB-Maintenance and repair)
N

KRUCHISIN, N.V., tekhulk.
Improving the operation of single-process machines. Tekst.prom.
14 no-7:50 Jl 054. WaA 7:8)
1. Nachal$nlk teekha fabriki In. Lukina.
(Cotton machinery)

ACC NRI AN1013496 UR/0120/60/000/0011/0066/0067
AUTHOR: Klebanov. Yu.D.; Kruchinin, S.P,; Lozina. L.A.
ORG: Institute of Atomic Energy GKAU, Moscow (Institut atomnoy energii GXAE)
TITLE: Differential gas Carenkov counter
TOPIC TAGS: particle-veAwe:ity counter, Cerenkov veboa60y counter, mescn vellsoibi
lvdicaker, bubble chamber inshmamgnt. synchrotron.
) -----,,w --~-
ABSTRACT: This paper discusses the theory of operation, the construction and the re-1
sultS' of tests of a differential type compressed gas Cerenkov counter, used for
high energy particle velocity determination and counting. The counter was slated for
work with a godoscopic system (reported previously by L.I. Govor and Yu.0. Klebanov
at the Conference for high energy physics at Dubne in 1964) of a bubble chamber. The
particle velocity ~ to be determined is related to the easily neasureable angle of
the Cerenkov radiation ID, and the adjustable refractive index of the environment, n
.-
loglin soloda i piva; spetsiRllnyl k-i:,3. Mloskva., PI-
.1tichevula promyshImpost', e58 ~;- NIFLA 18:1)

SIIVYRYATICV, Ortgorty Konstantinovich; KLINOV , I.Ta.. rodaktor;
Xisgrlxv, V.S., redaktor; KLINOV, I.Ta., rodaktor; KZJCHIRIH,
V.I., re4aktar; POLTAKOV, X.A.. redaktor; SAGALAT977"0TV".,""'
rodaktor; ATZMISTiTAT, I.I., redaktor: KORMffIVA, V.I., tekh-
nicheekly redaktor
(Electrolytic-metal coatiDg for parts and articles for the
chemical industryl Ilaktrolitichookis metallicheskie pokry-
tila detalel I lzdelii v khimicheakoi promyeblennosti. Pod.
rod. I.IA.Kiinova. Moskva. Gne.nnuchno-takhnAzd-vo khimi-
cheakni lit-ry, 1955. 54 p. (Norroslia v khimiche8kikh prois-
vodstvakh i sposoby zaahchity, no.2) (KLRA 6:10)
(Electroplating)
VIR

YMOMOV, I.A.; XRUCEININ, V.L. redaktor; LITINSUT, V.D., redaktor;
SEPAX. xd:". "f9mm"W'skly redaktor I
Cftollte and ism use in the chemloal industry] ftolit I ago prine-
neale v khWchookoi promyehlonnosti. Pod red. V.1.1ruchinIna.
Moskva, Goo, nauchno-tekba. Isd-vo khim# lit-ry, 1936. 74 p.
(Korroziia v hisichaskikh prohvodstyakh t sposoby zashchity. no.6)
(pla-stics) (MT-RA 9:7)

, .-, ; I I
~ 1.j, , i, .. : ,
S14IRNOV, Y.K.1 WSMOSON. S.Kh.: ]MUCH INIR--,L I - - Fedakt or; VXKSM, A.A.,
redaktor; SH-PAX, Te.G.,tekhnTC-h-8s-kiy redaktor
(Chemical bases of "arzamit" coativig and lacquers with cold hardening
properties] Khtmicheski stoikie zamazki arzamit I laki kholodmogo
otverzhdantia. Pod red. V.1. Xruchinina. Moskvn. Oos. nauchno-tekhn.
ind-vo khim. lit-ry, 1957, 49 p. (KLRA 10:5)
(Ladquare and lacquering) (Corrosion and anticorrosives)

7-- T I
SMInOV, L.A.; kiIf:-'AIUZXN, A.V.; BAXLANOi. N.A.. red.; VOLCDIN, Y.Ye., red.;
KISHLEV. V.S., red.; "INOV, 1.Yn., red.;
SAGALAYBV, O.V,, red.; UDYMA, P.G., red,; AYZKNSHTAT, I.I., red.;
SHPAK, Ye.G., takhn.rod.
[Acldpr4)of* i-.nrnmtc chemIcnI apparntual KlitmichaskRia apparaturs
I-. kltilotc~dnornoi keramiki. Pod red.N.A.Baklanova. Moskva. Goa.
nauchno-te)-hn.izd-vo khIm.lit-ry, 1957. 164 p. (Korrosiia v khImi-
cheskikh prolzvodetvakh i SDOSoby znshchity, no.10) (MIRA 10:12)
(Chemical Appnrntus)

SMIRNOV. V.K.; VOVSHINA. U.S.; UWCHINIF, V.I., red. (deceased];
BNLIINIKATA, S.K., red.; KLffMff$'-'D.G.O' takhn.red.
(Impregnated graphite and its use in chemical industry)
Propitannyi grafit I ago primenenie v kh1micheekoi pro-
myshlonnouti. Pod red. T.I.Kruchinina. Moskva, Gos.nauchno-
tokhn.isd-vo khim.lit-ry, 1939, 67 P, (Korrostia v khIzi-
oheekikh proisvodetvakh i sposoby sashchity. no.12) (MIRA 12:7)
(Graphite) (Corrosion and anticorrosives)

BELETSKIYp ?,A., dote,, kand. fiz.-ratem.nauk; BIRKUI;, H.Ye..o inzh.;
KAZANOV, V.A. . Irzh.; KLYUSHB, S.M. , dots.; PVCHININ,, V.L. p.
inzh.; MARCHENKOV, Ya.P,, dote.; PISWEV, V.Stj inzh,;
RUTSKIY~ A.I., Inzh.; SOKOLOV, N.M., dots., kand. tekhn. nauk;
SOLUYANOV, L.N., insh.; SHKARBANCV, Petr Fedorovich, dots.,
kand. tekhn. nauk; PANCA', V.p red.; LUKASMICH, V., tekhn.red.
(Handbook for electricians) Spravochnik elektrika. Saratovp
Saratovskoe knizhnoe izd-vop 1963. 456 p. (MIRA 17:1)

SKOHEIXVJ, K.1s; JUIUCIIINIIII V.Pl
Suggestions deriving from the experience in the operation of
rectifying junction systems for a.c. and does currents,
Flek. I tepl. tiaga 7 no.9sl7-19 S t63. (MM 16:10)
1. Nachallnik sluzhby elektrifikatall i energoticheskogo
khozyaystya Snvero-Kavkazakoy dorogi (for Skobelev). 2. ZaTnesti-
telt nachallnika Tuapsinskogo uchastka energoznnbzhPniyn (for
Kruchini it) .

SKONIMNO K I. po, k Roa -(Rost,:) v- r, ! --'~ , ",
Reliable performance of the Inverter. 7hel. dor. tran3p. 47 nf).3:
49-52 Mr 165. NIRA 1815)
1. Nachaltnik sluzhby alektrifikatpii i energetichezkogo khozzyaystva
SoverL-Kavkazskoy dorogi (for Skobalev). 2. Zrunestitell n-achplInIka
Tuapsinakogo uchastka energosnRbzheniya Severo-Kavknzskt-y rtorogL
(for Kruchinin).

KRUCHINIMP ves,
KOans for reducing the cumbrousness and cost q or milled
Peat. Torf-prom. 34 no.1:16 '57. Of Accountin(MLfRA 1012)
1. Direk-tor Untesygkogo trofoprodpriyatlya.
(Peat lndustry%.-Accounting)

29A INS4T*,.N.G.; XRU~~CHIN SISKO, R.K.
-IN.-Tu.A
Snowstorm at the height of the sunmr. Probl*Arkto no.4:99-100
'58. (MIRL U: 12)
(Now Siberlaa Islands-Snow)
LE

VORONOV, P-S-6 kand.geologo-cineral.nauk; KMJCHININ. Yu.A., mladshi;y
nauchm7 sotrudnik
Brief plWalcogeographical oharacteristics of the region of the
Ismarey South Polar Station. Inform.biuI9Sov*&atark*oic8p*
no.120-9 159, i (KIBA 13:6)
1. Nsuchno-iseledoyst ell sidy Imstitut geologii Irktiki (for
Toronov)e 2* Arktiobaskly I antarkticheskiy nauchno-isaledovatell-
skly i titut (for Kruchinin),
(Usarey region, Antarctica-Pbysical go.ography)

~Ruafumlx. Yu.A.
Work and life at the lazarey Station. Inform.biul.Sovoantark.
ekep, no,14:35-36 160. (MIRA 13:6)
(lazarey Station, Antarctica)

1RUCHININ, Yu.A.
Ice ram. Inform. biul. Boy. antark oksp. no.20:52-53 160.
(Iazarev Xeglon, Antarctica-loeborge) (MIRA 13:9)
W.

KRUCHININ) YUOAO
Ice foundatlon.
160, .1nformf blul, SOV* &ntark. eksp, no. 24,63-4
(XDU -140)
(L""Ov OtatiOn., kltaretica-lcg)
Tii, -E
U

S/169/62/000/012/062/095
1)2-'18/1)307
,eX T1 Z.,, X'rucliinin, Yu.A.
1'reliminary results of scientific obrervations at
the La,.,,ircv 4',ntarctic station
:1 1 CD 1 C; 'jL .'efcrativilyy zhurn-al, Gco-A[Uziha, no. 12, 1962, 57,
abntract 123371 (In collection: 1-aterialy po xhtike
i ,ntrx'&-,ti'A!.c, no. 1, L., 1961, 47-49)
The notcorolofical conditions at St-n. Lazarcv, situ-
atcel on the Lazarev shcl.-~' -lacier (6905812113, 1205.514111E) arc out-
linecl. -~uturin (fropi mid-Acjbruary to tlir~ ~>cginning of is char-
actc:rizccl by the ,rzidual drop o-," the averzigc nonthly teitipcraturcs
from -3, -10 to _1.3 =d also by hurricanes. The avern,fe wind
volocity cquals 21.3 m/scc; there arc individual gusts of ul~ to
60 M/scc. GaIcs (15-20 n/.,;cc) and hurricatier. (40-50 m/sec) are fre -
queniC in wittter Way--'J'ept ember), the average i-imathly jcptct;i~xr t(m.-
.'ovci-
peraturc bcin;~ 27.80. Spring lasts fro-m Lctober I to I. ibcr 10.
The air tcr-q)cratum risca to -IG', the average wind velocity equals
Card 1/2

s0/169/62/000/012/062/095
19-rcliminary rc--ult-- J21231a307
11-13 n/scc, mad hurricnnos Lre rre. -.-ad clear weather, %-rith
an vxerare monthly tcm.;craturc of -6.7 al-ICI a vine velocity of
7.7 rI/rcc'*', prewilf; in the nutx~icr. Jud-ing from. the thichness 01.
the ,,early snow layers, tlie -mouvit o.~ -,)rcci,)ita-L4-on is 200-3.50 mm.
licr annim. , --tudy o)- thc tcrfi~);iraturc varizition in th.:2 surface
snow layer and, i-a a 37 m in de,)th? shous that the thickness
of the active layer cqu.,ls 14 m. 3clow this there is a 2-meter
layer oj*' constaat 'Com-cratures (-15.20). itill deeper the tempera-
turc increases by- 0.60 -.)cr meter.
C,~bstracter's note: ijon,pletc. trv.-ar'lation2
Card 2/2

KOWMITS, Ya.P.; KRUCHMIN,, Yu,A,
Dynamics of the shclf ice front in eastern Antarctica. fTobl
A.rkt..i Antarkt. no.9:67-71+ 161. (MIM, 15:1;
(Antarctic regions-Ice)

3/169
,/62/000/004/049/103
D228/D302
AUTHOR: Xruchinin, Yu. A.
TITLE: Morphology of the
Station Lazarev
shelf glacier in the vicinity of
PERIODICAL: Reforativnyy zhurnal, Geofizika, no. 4, 1962, 55, ab-
stract 4V323 (Inform. byul. Sov. an',arkt. ekspeditaii,
no. 26, 1961, 9-12)
TEXT: The morphology of the station's immediate environs waa stu-
died simultaneously with a visual survey of the part of the shelf
glacier on a scale of 1:50,000. A description is given of ice
banks, a glacial barrier, and the wavy surface L) the south of the
station. The most unique topographic form -- ice fissures, probably,V/
arisizig ac a result of tangential internal stresses in the body of
Uhe glacier and existing for a llong time thanks to the activity of
wind, carrying snow away from the fissure bottoms -- is described
in detail. The number of fissures to the south of the station ex-
-ceeds 30; their length varies from 10 to 500 m and their width from
Card 1/2

Morphology of the ... S/16 62/000/004/049/103
D228YD302
3 to 150 m; the height of the steep slope ranges from 1 to 22 m. 5
references. /-Abstracterts note: Complete translation--7
Card 2/2

MUC1111-1111, Yu,A., mladsiy nauchnyy sotrudnik
Dnamica of the snow surface on lazarev Shelf Ice, Inform, biul.
Sovo antarke ekap. no,270-8 161. (MLA 14:7)
1. Arktiohookiy i antar."Aichookly nauchno-looledovatel'Bkiy
institut.
lIzzarev Shelf Ice--Snos surveys)
MWOMM

,XRUCHIIIIII Yu.A.
Ll- ---- -- - - - -
Snow shavings. Tnfo=, biul, Sov. antark, ekap, no,27s45-46
161. (Antarotio regions--Snow) (MIRA 14:7)

3/169/62/000/005/055/093
D228/D307
n 1 rl 7
.,L
D~~'-~ITODICAL:
!~ruchiriiri, Yu. A.
A.
h, ransparen-.11 gale
Rcferativr,yy zhurnal,
stract 5B214 (Inform.
no. 28, 1961, 46-47)
Geofizika, no. 5, 1962, 31, ab-
byul. Sov. antarkt. ekspeditsii,
T -EX At the Lazarev Antarctic station the wind's strengthening is
usually accompanied by snow drifts and local snowstorms, and then
by Zone.ral snowstorms. In cdntrast to this, the wind's strengthen-
inc, to 20 ra/sec, with rusts of up to 25 - 30 -,Vsec on July 3, 1959,
o~,-.urred under conditions of the complete -absence of any znow mo-
veme-1t; this 13 explained by the thin ice crust situated at that
-4
or, the srow-cove,"s surface. It had been disturbed by the fol-
lowin- morning, and the strong wind was, as u3ual, accompanied b
L> -'batracter's note: Complete trar U
a severe snowstorm. slation.-Y
Card 1/1

S/169/62/000/004/059/103
D228/D302
AUTHORS: Voronov, P. S. and Xruchinipjt~. A.
TITLE: The finding of marine sediments on the surface of
the Lazarev shelf glacier
PERIODICAL: Referativnyy zhurnal, Geofizika, no. 4, 1962, 58, ab-
stract 4V343 (Inform. byul. Sov. antarkt.ekspeditsii,
no. 29, 1961, 22-26)
TEXT; The examination of one of the shelf glaciers near Stn, la-
zarev led to the discovery on the vertical surface of one of the
fissures in the glacier of shapeless dark spots with an area of
200 - 300 M2; these consisted of disseminations of shingle, silt,
and some organic remains in the ice. The study of their composi-
tion indicates that traces of chemical weathering processes are
practically absent in these remalne; and that bottom material
%..,hich belongs to the category of normal iceberg sediments, has
been found. The results of geologic and zoologic comparisons lead
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S/169/62/000/004/059/103
The finding of marine ... D228/D302
to the conclusion that recent marine sediments were encountered
oln the surface of the Lazarev shelf glacier; it is noted that this
kind of discovery also applies to other places in Artarctica. There
is some doubt about the hypothesis, according to which the con-
tinuous movement of the mass of the ice layers forming the shelf
glacier takes place upwards at the expense of freezing below and
the intensive melting and sublimation of ice from the glacier's
ul,per surface, since no bedding is observed among the organic and
the terrigenous inclusions. The assumption is made that it is poss-
ible for such inclusions to be formed at the expense of the arti-
culation of a whole row of icebergs, some of which could have been
inverted. 7 references. /-Abstracter's notes Complete translation-7
Card 2/2

S/10'9/62/000/004/058/103
D228/D302
AUTHOR: Kruchinin, Yu. A.
TITLE., Some data on the temperature regime of the Lazarev
shelf glacier
FERIODICAIT: Roferativnyy zhurnal, Geofizika, no. 4, 1962, 56, ab-
stract 4V342 (Inform. byul. Sov. antarkt. ekspeditsii,
no. 30, 19610 13-15)
T";'XT: Observations on the temperature regime of the onow-firn
stratum in a hole that was melted through and drilled thermally
were organized during the execution of glaciologic work at Stn.
Lazarev in the period from June to December, 1959. The hole, with
a-diameter of 6 cm and a depth of 37 m. was situated 10 km from the
base of 'the lazarev shelf glacier. After melting the hole its na- 1.1/
tural temperature was restored in 20 days. The measurements were
made by mercury inertia thermometers at the horizons: 2.5, 3.2, 5,
8, 10,12, 14, 169 20, 27, 32, and 37 m. Readingo were taken in
five-day periods. It was established as a result of the observa-
Card 1/2

Some data on ...
S/169/62/000/004/058/103
D228/D302
tions that the zone of seasonal temperature fluctuations stretches
to a depth of 14 m. The constant temperature observable at depths
of 14 - 16 m amounted to -15.20. This agrees well with the mean
yearly air temperature. At greater depths the temperature rises
evenly with a gradient of 0.0620 per meter, reaching -13.90 at a
depth of 37 m. The mean gradient, measured in a 100 m hole on the
Modheim glacier in 1950-1952, was about 0.0140. The anomaly which
is due to climatic warming and is almost absent on the temperature
curve of the Lazarev glacier, is well marked on the temperature
graph, constructed from these data. The rise of the temperature in
the shelf ice with depth is explained by the relatively high tem-
perature (-1.70) of the water masses underlying the glacier; the
divergence with the data on Modheim is explained by the fact that
the anomaly has had time to be smoothed out during the 8 years,
and also by the accumulation of a 5 m stratum of anow'on the La-
zarev shelf glacier in this period. /-Abstracter's notes Complete
translation,-7
Card 2/2

KWGHININ, Yu.A.,, mladshiy nauchnyy sotrudnik
The ice oltuation in the region around Lazarev Station in 1959.
InformobluleSov,antarkookep. no.31:26--30 161. OUPA 15 W
le Arkticheskiy i antarktictieskly nauchno-isoledovatellskiy institut.
(Lazarov region, Antarctica-Ice)

KRUCHININ, ru. A., mladshiy nauchnyy eotrudnik
Study of the stratigrapby of the upper layers of the firm
now cover of the Lasarev Shelf Ice. Inform. biul. Sov. antark.
ksp. no.32319-24 162. (NM 16:4)
:
1. irktichaskiy i antarktichookiy nauohno-issladavatellskiy
institut,
(Lasarev Shelf Ice--Snow)

KRUCHININ, Yu.A., mladshiy nauchnyy sotrudnik
Kicrorelief of the snow cover of Lazarev Shelf Iceo
Inform, biule Sov. antarke skep. no.33:27-31 162. (KERA 16:2)
1. Arktichaskiy i antarktiohaskiy rAuohno-isoledovatellskiy
inatitut.
(Lazarev Shelf Ice.-Snow)

KRUCHININ, TuAAA mladBhiv mmehnn fiotrudnik
Temperature condi-tiam in the active .1a7er of the anow formation
on the lazarev Sheir Ice. Inform. biu:L. Sov. antark. eksp.
n0.36:7-11 162. (MIRA 16:4)
1. Arktichaskiy I antarktiches-kiy nauchno-issledovatellskiy
institut.
(lasarev Shelf Ice--Snow)

iy Alskmandrollchl-ANDREYEVA, L.S., red.j USANOVA,
N.B., tekhn. red.
[Trip into the ice age) Puteshestvie v lednikovyi period.
Moskva, Izd.vo "Morskoi transport," 1963. 1U p.
(MIRA 16:7)
(Queen Maud Land)

KRUCHININ, Yu.A.
Practice of classifying Antarctic ice mhelves. Probl. Arkt. i
Antarkt. no.12:99-106 163. (MIRA 16:7)
(Antarctic regions--Ice)

KWICHININ, Yu.A., m1ndsidy nauchnyy sotrudnik; KOBTANTi, Ya.11., kand,
tekhn.nauk
Dynamics of the Trolltung Shelf Ice. Inform.biul.Sov.antark.eksp.
no-44149-52 163. (MIRA 17:4)
1. Arktichoskiy i antarkticheskly nnuchno-issledovatel'skiy

KRUCHININ, Yu.A.
Physicogeofraphical observatims m Kotellnyy Island (Tamp
Bay regim). Trudy AJLNII 2241119.3-165 163 (MIRA 18ol)
-P

KRUCHIN Yur Alek a ; GAKMI, Ya.Ya., doktor geogr.
nauk., r .) OKSENOVA, Ye.l., red.
[Shelf Ice of Queen Maud Land) Shellfovye ledniki Zemli
Korolevy Mod. Leningradp Gidrometeoizdat, 1965. 178 p.
WiLk 18:7)

IKRUCHININ~ Yu.A.
Praotice In the alaagification of the microrellef forms of the
snow surface of the Lazarev Shelf Ioe, Geoge abor. no,171
141-148 164. (MIRA 180)

ERVCIfMIN, Yu. v.: mmater Tech Sci (diss) -- "TMatlgntlon of the crystalli-
zation of Ural blant-furmce alag". Sverdlovak, 1958. 17 pp (M'-n Higher EAuc
USSF, Ural Polytech Inat Im S. M. Kirov), 11~O caplon (KL, m 1,)59, in6)
Ps,
4,

"Properties of Slag Melts and Their Castings" P. 1431
Transactions of the Fifth Conference on Experimental and Applied Mineralogy
and Petrography, Trudy ... Moscow, Izd-vo AN SSSR, 1956, 516pp.
reprints of reports presented at conf, held In Leningrad, 26-31 Mar 1956. The
purpose of the cunf. was to exchange information and eccrdinate the activities
in the fields of experimental and applied mineralogy and petregraphy, and to
stress the increasing complexity of practical problems.

AUTHOR: Kruchinin, Yu. D. SOY/156-58-1-4o/46
TITLE: Dependence of the Mechanical Strength of Slags on Their
Structure (0 zavisimosti mekhanicheskoy prochnosti shlakov
0t struktury)
PERIODICAL: Nauchnyye doklady vyeshey shkoly, Khimiya i khimicheskaya
tekhnologiya, 1958, Nr 1, pp. 164 - 167 (USSR)
ABSTRACT: Blast-furnace slag has lately been more and more used for
the production of various "stone"castinge (kamennoye litlye).
The dependence mentioned in the title has therefore gained not
only theoretical but also practical significance. There is
some disagreement of opinions represented in technical
literature (Refs 1-3). The author has investigated the in-
fluence of structure on the mechanical strength of castings
made of blaot-furnace slag from some metallurgical plants
in the Ural Mountains. Under such conditions as occur in the
production process of polygonal slag castingog i.ea# at
a comparatively low cooling rate of the melt, coarse-
crystalline porphyritic structures are formed in which the
Card 1/4 porphyry phenoorystg are formed by the melilite mineral

Dependence of the Mechanical Strength of Slags on SOVI 156-58-1-40/46
Their Structure
(Fig 1). The slag that was repeatedly molten in the ex-
perimento was cooled more rapidly so that the castings ob-
tained showed dendritio structures conBisting of melilite
skeleton crystals (Fig 2). These structures are of a greater
mechanical strength, as may be seen from table 1. Those
structures obtained at the same time that showed both of
the types mentioned take an intermediate position as regards
mechanical strength. With a longer crystallization time
of the castings showing dendritic structure# their mechanical
strength increases. This is due to the percentage of the
major constituent in the slag melilite (Table 2). kn ana-
logous dependence was established in testing the slag for
compression and tension. Those samples of each of the two
structure types that showed particular strength were examined
petrographically in order to establish the influence of
crystal size upon the strength of the castings. The strength
was found to be higher for a smaller crystal size. Figure 3
shows the porphyritic structure of a sample where the prisma-
tic melilite crystals are small (up to 0,35 x 0,15 mm). The
Card 2/4 compression strength of this sample was high, being 2970
iv

Dependence of the Mechanical Strength of Slags on sov,i56-58-1-40/46
Their Structure
kg/aqom. Figure 4 shows a dendritic structure of a laboratory
sample taken from the same slag where the bulk of melilite
skeleton crystals has up to 0,8 x 0,018 mm size. Its com-
pression strength wan 3700 kg/eqcm.There are 4 figures, 2 tables,
and 3 references, 2 of which are Soviet.
ASSOCIATION: Kafedra tekhnologii stekla i kerAmiki Ural'skogo politakhniches-
kogo instituta im.S.M.Kirnvs- (Chair of Glass and CerAmica
Technoln-1, mf the Urals Polytechnic Institute imeni S.H.Kirov)
SUBMITTED: October 79 1957
Card 3/4