SCIENTIFIC ABSTRACT KHALEVIN, N.I. - KHALFAN, YU.A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000721710017-5
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 17, 2001
• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

Mum, H. 1.
--"W -------- WA-114
111mit!.ng Velocities for c,rtaII2 types Of bedrock in
Xxv-AN SSSR-Ser.goofix.120.2.,165-17.1 7 156o the Turgay- Gates.
(KMA 9:7)
1-Urallski.v filial Akademi, 4Auk 3
Turgay Gates-Geolo..1 331t Gorno-goologichooki, ingtitut.
PhYsical methods)
Structural)(Turgv'GataB--Prospecting--Gea-

KHALIVIN, N. I.
, 7
Natimating the accuracy of Interpretation of data of the refracted
vaves method, IzvsAN SSSR.Ser.geofiz. no.8:912-919 Ag 156.
(MIJU 10: 1)
1. Ural'skiy filial Akademii nauk SSSR, Gorno-goologicheakiy indti-
tut. (Saismometry)

KffAIXJ11j. II.I.
~ !~~-~~"`~, r
e-,~ Using the correlation method of refracted waves in prospec~jng from
and eXploration of c 1 deposits - w
0a on the eastern slopes of the Ural
Mountains. Trudy, Gor.-geol,
(Ural Mountains-'nst- no-30:116-120 157. (MIRA 11:7)
Coal) (Seism
,ic w,,,es)

KRAIEVIII, 71.1.
Seismic observation methods used in borehole drilling. Razved.
i prom. geofiz. no.2:85-87 '57. (MIRA 11:4)
(seismic waves) (Borings)

SOV/ 124-58-10-11459
Translation from: Referativnyy zhurnal, Mekhanika, 1958, Nr 10, p 108 (USSR)
AUTHOR: Kh al..eYin,-N-.1-z- - -
TITLE: Results of Seismic Core Sampling by Rates of Propagation of Elas-
tic Waves at Given Intervals (Rezul'taty seysmokarotazha interval'-
nykh skorostey rasprostraneniya uprugikh voln)
PERIODICAL: Tr. Gorno-geol. in-ta. Urallskiy fil. AN SSSR, 1957, Nr 30,
pp 111-115
ABSTRACT: A brief description of a test model of a portable equipment for the
determination of the rates of propagation of elastic waves in wells
at given intervals is presented.
Reviewer's name not given
Card 1/ 1

124-58-9-10437
Translation from: Referativnyy zhurnal, Mckhanika, 1958, Nr 9, p 146 (USSR)
AUTHOR: Khalevin, N. 1.
TITLE: On the Speed of Propagation of Elastic Waves in Sedimentary
Rocks (0 skorosti rasprostraneniya uprugikh voln v osadochnykh
porodakh)
PERIODICAL: Tr. Gornogeol. in-ta. Ural' skiy f i1. AN SSSR, 1957, Nr 30,
pp 121-132
ABSTRACT: Bibliographic entry
1. Waves--Propagation 2. Rocks--Wave transmission
Card 1/1
asuring the velocity of elastic wave propagation in conditions
of natural rook formation. Trudy Gor.-geol. lnqt. no.30:133-141
(MITIA 1l:'/)
(Seismic waves)
~g,

HA (_
20-1-23/54
AUHHOR: Khalevin, N. I.
TITLE: On the Interval Logging of Accoustic Waves
(K intervallnomu karottazhu akusticheskikh voln)
PERIODICALt Doklady Akadeniii Nauk. SSSR, 1957, Vol. 115, Nr 1, pp. 89 - 90
(USSR)
ABSTRACT: First the disadvantages of the procesies used hitherto are point-
ed out. The author used for his accoustio investigations an
apparatus with the following characteristiost The emitter of
electromagnetic waves mounted in the gap supplies a sound speot-
rum of the impulses to be investigated and just thereby makes
easier the extrapolation of the data obtained on the seismic
proupocting in the field. 2.) The interval of the investityation
extends to from 5 - 10 km which decreases false anomalies.
3.) The great reproduceability of the impulses emitted makes
possible a great use of the dynamic characteristics of elastic
waves- 4-) A non-screened standard logging cable is used.
5.) The mcaouremento were carriea out at such points where the
distance between them is uauallt equal to the interval between
emitter and seismic receiver.
After this the ncherie of the apparatus for the interval logging
Card 1/3 of waves is described. The intensity as well as the character
On the Interval Logging of Accoustic Waves 20-1-23/54
of the registration of elastic waves depend greatly on Ceologic
conditions. With various degrees of dependability we can differ
up to four types of waves which can be brought into connection
with transversal waves, longitudinal waves, shock waves (or
Lamb waves) and SH-waves. A diagram shows the registration on
a band. The results of the elaboration of these data are also
shown in a diagram. One can only get a general idea of the in-
tensive wave with the velocity of from 550 - 700 m/sec. The
velocity o-1 this wave increases rather quickly with the depth.
According t., the velocity of the shock wave (Lamb wave) one'
differs-betv en four layers which correlate with the character
of the curva )f apparent specific electric resistances. In the
case of slate, and sandstones the intensity of the Lamb-wave
depends greatl) on the rocks being present in the cross section.
The elastic wave, -tre sometimes absorbed by the porousity of
the rocks. There a, 2 figures and 2 Slavic references.
Card 2/3

49-58-3-12/19
AUTHOR: Khalevin N I
TITM: On logging by interval pulsed sound waves.
(Ob impulisnom intervallnom zvukovom karottazhe).
FERIODICAL: Izvestiya Akademii Nauk SSSR Seri7a Geofizicheskaya,
19587 Nr- 3, pp. 379-386 (TJSSR3.
ABSTRACT: The methods'of seismic investigation used at present are
sufficiently accurate for determining the average speeds
but they do not permit a sufficiently detailed sub-division
of the cross section as regards the elastic properties.
Such sub-division would not only improve interpretation of
the results but it may also increase appreciably the
effectiveness of the logging itself. If the differentiation
of the individual sections as regards their elastic
properties is detailed enough, it would be posEible to
elucidate the follovinG problems: determination of the
thickness of reflecting and refracting horizons;
determination of the peculiarities of waves which are
refracted and reflected from horizons of variouo thick-
nesses; a clearer separation of porosity differences in
formationsl etc. Although the possibility and the
necessity of detailed sub-division of sections of wells
Card 1/4 as regards elastic properties was mentioned many years
jo
h 11

49-58-3-12/19
On loSging by interval pulsed sound waves.
ago, there has been no appropriate apparatus for doing so.
In recent years apparatus has been developed and tested
which permits differentiation of sections of wells by
means of ultrasonics (Refs-3-7). In 1953 the author
carried out a small volume of measurements in wells by
means of a probe consisting of an electromaEnetic
transmitter of elastic waves and of a seisuic receiver
which are located at a certain distance from each other.
In spite of the fact that the receiver was of a low
frequency, had a na row passband and the apparatus iaad a
low overall sensitivity, satisfactory results were obhained.
In particular, a relation was established between the
intensity and the elastic wave and the structural features
of the cross section. In this paper a brief description
and test results are given for the equipment which has
been used by the author recently for pulsed acoustic
observations. The equipment enables characterizinG a
considerable volume of the investigated formations,
reducing thereby the influence of the well walls and local
non-characteristic non-uniformities. The investigations
Card 2/4 are effected at frequencies which are relatively near to

49-58-3-12/19
On logging by interval pulsed sound waves.
the ordinary seismic frequencies and it is, therefore,
possible to interpolate the detected relations for
field surveying. However, the fact -that the frequency
is somewhat higher than that used for ordinary seismic
prospecting improves the detailed classification of the
cuts as compared to ordinary seismic logging. A good
reproduceability of the shape and intensity of the
3xcited pulse enables utilising the dynamic properties
of the waves. In the measurements an ordinary logging
cable is used. The wave relations change considerably
depending on the physical-geological structure of the
cross section; in various intervals with a non-uniform
degree of reliability up to five types of waves could
be distinguished: longitudinal, transverse, Lamb vave,
"water" wave and wave of a speed of the order of 500 to
800 m1sec. The conditions of separation of theoe
waves and the characteristics of some of them approach
t1loGe obtained by other authors using ultrasonic logging.
There are 4 figures and 10 references, 7 of which are
Riissian, 3 English.
Card 3/4

49-58-3-12/19
On logging by interval pulsed sound waves.
SUBMITTED: May 27, 1957.
ASSOCOIATION: Ac.Sc. USSR, Ural Branch, MininE;-GeoloGical Institute.
(Akademi a Nauk SSSR Ural'Bkiy Filial. Gorno-Geologicheskiy
InstituT
AVAILAP,L:-,,: Library of Congress.
Card 4/4
~2

KMI-IMIN,
BOtimating rock PoroaIt7 by sonic well
Prom. gaofiz~oino*30:3-9 159. measurements. Razved. i
(MIRA 12:12)
1 well logging) (Ultrasonic teatime)

KHAL"'Mis N.I.
Structuro of tho Urain in 1' ;1A of data. ~,~Ov.
geol. 3 no. 12:22-32 D
1. Institut Georizild
(Ural Structurd)

IXUMINt N-L; BARYKINt D.D.
Instillation for acoustic inve0tigationo in boreholes. Jzy. AN
SWR* Sero geofix. nools6g-78 ja t61& (MIR& 3411)
lo Akademiya nauk SUR.p UrallskiT filialp Institut geOfiSW.
(Seismic prospecting)

KHALEVIN., N.I.; BUNIKOV., A*M,
Mobile SSP-3j, seismic station. Geol. i geofiz. no.12:124-128 16o.
I@ Institut 900fiziki Ural'skogo filiala AN SSSR (MIRA 14:5)
.9 Sverdlovsk.
(Seismic prospecting-Equipment and supplies)

S/-169/61/000/011/016/065
D228/D304
AUTHORS3 Khalevins--ffj," and Bun1kov9 A.M.
TITLE; A portable CCTI-14 (SSP-14) seismic station
PERIODICAL: Referativnyy zhurnal, Geofizika, no. 11, 1961, 21v
abstract 11A192 (Geologiya i geofizika, no, 312. 1960,
124 - 128)
TEXT; A portable 14 channel station, intended for solving problems
of economic geology and for parametric measurements in the basic
Kmnp (KMPV) method, was de,4koped. The station!s gross weight is 150
.Kg.*Compactness is achieved by decreasing the number of channel
and by altering the amplifier's, circuit. Three-cascade resistive
amplifiers are applied to 62xln.(6ZhlP) and 6H3F( (6N3P) finger-
lamps with a transformer inlet and outlet. The essential feature is
the use of dual T-shaped RC-filters giving a set of resonance cha-
racteristics on frequencies of 25p 40p 60p and 80 c/s at a sharD-
ness of 25 db/octave for the right section and 8 db/octa7e for !he
left section. There is also open filtration with a pass band of
20 - 2000 c/8. The voltage amplification is 150,000. The current
Card 112

S/874/62/000/002/011/019
D218/D308
Khalevin. N. I
T ITLE: Tectonic disturbances of the banement in the Trans -
ural' region according to geophysical G'ata
S G U DIG Z Akademzya naxdc SSSR. Ural'Gl,.iy filial. Institut po-
fiziki. Trudy. no. 2, 1962. Geofizichcskiy sbornik,
no. 3, 1962, 211-219
Gravimetric and aerial -magne tic survcy data for the
Traasural' region aere used to construct a maD showin- tlic C'Jis-3osi-
tion of the axes of Ag and AT anomalies, Tne ma,) is rc~,jro,'uc,-(!
a-,~. an attempt is made to account for the change in t',-e -intC:,.z;ity
nnd co--figuration WE the anomalies in terma of the position of tl-.e
oasement below the surface. Three groups of irregularities in the
basemerit were discoveredi some of them have '~,een )artia'lly
'Dy foological data. It it sug-ested that Sucl" ric"101"S !7.aV
-,i' v F :5
uitable for ore, coal, oil and ga;: -
Card 1/1

KHAIEVIN, N.I.; YUNUSOV, F.F.
Using the elastic waves from comercial, blasting
in the Urals for sounding the earth's core. Izv.
AN SSSR. Ser. geofiz. no.11:1567-103 N 162. (MIRA 15:11)
1. Urallskiy filial NI SSSR, Institut geofiziki.
0
(Ural Mo=taina-Winkth-Internal structure)
(Elastic waves) (Blasting)

I
KHAISM, Mi.; MALUMOV, A.A.
Regional seismic studies conducted in the Urals in connection
with extra-deep drilling* Izv, AN SSSR* Serageofiv. no.lt49-
57 ;a 163. (MIRA 16:2)
lo Institut, geofiziki Ural-skogo filiala AN SSSR i Sverdlmkiy
gornyy institut,
(Ural Mountainsm-Seismic prospecting)

ACCESSION NR: AP4023371
3/0049/6h/000/002/017bl0l$3
AbTHOR: Klmlevin, N. 1.
TITLE: The physical properties of rocks md rook complexes at the Krasnouralsk
intersection of the Lower Tagil symlinorium of the'Urals
SOURCE: AN SSSR. Izv. Seriya geofizichaskaya, no. 2,-1964p 174-183
TOPIC TAGSi physical property, rocks, magnetic property., electrical property,,
seismic velocity, density~ borehole, drill hole, synclinori~m, geophysical
examination, W022 log, teophyVical logs velocity log
ABSTRACT: The author has examined the magnetic, density,, velocity, and electrical,
properties of rocks from a number of drill holes. The elastic-wave velocity ranges
rather widely through short depth intervals. For the sedimentary rocks (mainly
limestones and conglomerates), however, it is generally 5900-6000 m/see, and for
volcanics and volcanic-sedimentary rocks (lavas, tuff-conglomerates., etc.) it. is
5WO-5600 m1sec. Velocity logs divide the sections into two layers: from 50 to
410 ra the velocity averages 53h0 m/sec, and below this the average is 5800 M/sec.
In the zone of deformed rocks the velocity is but 4400 m/sec. A refracting sur-
face at about 470 m proved to be the base of a distinctive weathering zone; it is
not a separate formation. The most promising technique for deciphering this part
Card 1/2

ACCMION NR: AP4023371
of the synclinorium is seismic reflection; especially with high-frequency waves,
The Tura series is characterized by a linear increase in density with depth, oven
in places where it is overlain by older rocks A similar rela"ionship is observod
for a number of other formations. The lower layers of the Tura series differ more
from the upper layers than they do from the underlying Imennaya series. In inter-
preting gravity anomaLies., therefore, one must keep in mind that the gravity affect;
will be dub chiefly to the first boundary and 'not to the transition between the'-
two. Density measurements show complex trends; and these variations must be con-
sidered carefully when structure is interpreted on the basis of gravity studies*
Magnetic and electrical properties of greenstones may be used for subdividing
drill-hole sections. Magnetic measurements permit recognition of the base of the
Tura series,, and electrical measurements permit this series to be subdivided.
Orig. art. has: 3 figures and 2 tables.
ASSOCWION: Akademiya'nauk SSSR Urallskiy filial Institut geofiziki (Academy Of
Sciences SSSR, Ural Braach, Institute of Geophysics)
SUBMaTTED: 2&'-Iar63 DATE AOQs Mar64 EWLI 00
SUB CODE: AS NO REP SOV% 025 OTISR:' 000
4-,d 2/2

KHALEVTN, N.I.; TAVRIN, I.F.
Subhorizontal stratification of the upper part of the earth's
crust in the Urals. Izv. AN SSSR. Fiz. zer.. no.3:61-64 165.
(MIRA 18-7)
1. Institut, geofiziki Uraltskogo filial& AN SSSR.

F-
L IU546 EIVT(1) GW
IACCESSION HR: AT5022651 UR/874/65/000/003/000*015'
W
1AUTFOR! Bulaahevich, Yu. Eh levin ;, ,
LL~R. mojLey!~,vj N~; Kuznetsov A. A. -'
__X. ; R_Ao_ -_ _Xllt -
q f,#t ;!;1' .4 Y, 5 1,44. 61
iTITLE: Selection of a site in -the Urals for sinking a
~SOURCE: AN SSSR. Ural'skly filial. Institut geofiziki. Trudy. no. 3, 1965.
lGeofizicbeakiy sbcraik, no. 4: Metodicheakiye voprosy rudnoy geofiziki Urala (Geo-
iphysical papers, no. 4: Methodological problems of mining geophysics of the Urals),
13-15
TOPIC TAGS: superdeep drilling, Moho discontinuity, Conrad discontinuity, gravity
survey, seismic survey, seismic profile, aeromagaetic survey, magnetic survey, earth
~crust
ABSTRACT: Since 1961, severat Soviet scientific organizations have carried out Inves-
tigations in the'Ural 14blintains to determine the optimum location for drilling a
superdeep borehole. The arqa covered extended along the range from 51*201 to 58*40r,
Let. The announced purposes of these Ltudies, both of scientific and industrial,
jimport, were as follows* 1) thickness, composition, and stratigraphic sequence of
_~geological formatjlons-, 2) nature of the geosynclinal sediment-" granitic treositiorl
zone; 3) thickness and romposition of the "granitic" layer; 4) nature of the "grdn~.
C,ard 1/2
-2

7
-2-44,66- -6 ]4'_
ACC NRi AP60131 SOURCE CODE: UR/0387/66/000/004/0036/0044
AUTHORt Khalevin, N* I#,vq_r_UzhinLn. V. S.; Rybalka. V. M,; Nezo enova,
.K. At.; CbWd&kd!Jf4-`L-0~'_N4
ORGI Institute of Geophvsics, Ural Branch, Academy of Sciences SSSR
(Institut geofizLkis Urallskiy filial, Akademiya nauk SSSR)
TITLE: Results of deep seismic soundini ), of the earth's crust in the
central Urals
SOURCEs AH SSSR, Izvestiya. Fizika Zemli, no. 4, 1966, 36-44
TOPIC TAGS1 deep seismic sounding, seismic profile, seismic discon-
tinuity, deep drilling, Hoho discontinuity
ABSTRACT: In 1962-1964,the Bizhenovsk Geophysical Expedition of the
Ural Geological Administration of the Main Geological Administration
of the RSFSR and the Institute of Geophysics of the Ural Branch of the
Academy of Sciences SSSR carried out deep seismic soundings (GSZ)
along a 450-km, east-west profile across the Urals between Krasnotifimal
on Lhe west and Tyumen 6n the east* Both the GSZ and KMPV (longitu-
dinal wave correlation) methods were used. In the GSZ operations$ six
shot points, spaced about 100 km apart with travel times of 300 km,
were supplemented in the Asbest region by quarry exp losions detonated-
Card 1 / 2 UDC: 550.830550.311

botJ t
ce d a-
sp a opet
t points# ofq tions
.1hree sho -2 in the
_~o tt,
.1sed 30160 sts f
date ss-~ aces a
hkp6- -13163 GSZ Shot0*50 V'%* 'I 'Were for dista Vere
CC the of Va thoc ?.-~2 raPhs
Vit I t i1ne a 0?v e 'Was Iseigimo% the
taneoilsly tCfLve the a a Ce 6 between
art Vith Used to altr tiork jere dig the
t meats this ats ta h 100 0 Ves in
ap TU h I on %er Tt 'Wit ted Va three 110b0
1.06 e 91 for spa a it a C and
,;tongs 00 %T 09 1. -- 1. 20 0 and T ct%xst tark a the
and 10-~ tea pp e T rap
litth Sy 100 WA 9 of 3-0-049 eflec'in the b3seTftea seisimos
th s1l 'Coups Of T eiss the t the
less 0 % rotIps tinu Ities at te-91 is of thS the 140h0
4 t ere d 9 t
e 'Main 0 the %ta Nn al y 1, lay tha luate
atra S J'K a dtsco of i a
roulps - urfaG06 t deft"ed. tle.
', laan t-jrev th 0rs e-4 a ti0%
4,2 e( S beir, elec
tin? X- 'ad upy s tooal
cr%lat), tloin r Lt-blOclt StVU 'the' au
t'he a alue to addit
lowe be -T%Jst 13rals - 4 that re an
ttutItty the the ,rest whe
that zed by M Eau of ero%Vkend ,, area
dtscoa O'Wed rter aundeT betn% d T 6,,, prese"t
data 9 rhara aq at 9 - la an itogro 3
to - 4 a doq,4 ('study ag~3ra I --ti a 7-11 d in has% JBILI
%is t t. '- this the -agil art.
Cr tiaut I Va. in ovete
atsron sined avillin% in the L aisr- Orig.
data obt deep rtaill . ve locity 'ainedo
the tte for espe 00 talse obt VLS? I eol
.1"e 13 be Tua * the 70-- il~ht be
r
'Cott e -6 A0 'Deg
on for Of 5~
e I. %na a de V 0 O?LIG
st%A a 26D Gc6hI
,J 'Are$@
S,U,a GODS% % q?1"7
CL"-
JD 'P?Lv' S
---rrcr~nios copes to measure ultrasonic
t experiments cases
ii Ural region. During the
e velocities were observed to
-C ropy were noted in which th To
-*rd
? y depending upon wave incidence and direction of transmission.
raphic analyses were made of three
M,-~I,, n the cause of this phenomenon, petrog n
major rock groups: 1) rocks with a schistose texture and a lepidoblastic or gra 0
blastic structure; 2) rocks with a schistose texture and a fibrogranoblastic and
porphyroblastic structure; and 3) rocks with a massive texture and a heteroblastic,
Card__ 1/2__
UDC! 550.834:550.311

ACC NR, -
AF6036363
granoblastic, blastogranitic, or blastopsammitic structure. Rocks of group I were
characterized by the greatest anomalies in velocity anisotropy. Velocities along
the plane of schisotosity (average,4340 m/sec) were 3-5 times greater than trans-
verse waves. In the case of rocks of group 2, elastic-wave propagation velocity
along the plane of shcistosity (average 5400 m/sec) -was about twice that of trans-
verse waves. In the case of group 3, velocity anisotropy did not exceed 30%, and
the average wave velocity is 4700 m/sec. Thus, the propagation velocity of ultra-
sonic longitudinal elastic waves was found to be greatly dependent on the texture
and structure of the particular-rock and on the quantitative ratio of mineral grains
of different forms (isometric, lamellar, prismatic). Orig. art. has: 5 figures.
SUB CODE: 08/ SUBM DATE: 08Ju165/ ORIG REF: 002/ ATD PRESS: 5108
LCard_ 2/2

I WMV
PUTILOVA, A.Tol KHALEVIN VA.-'
J-1
Carrying capacity of electric power transmission lines wIth
wavelength compensition. Trudy Transp.-energ, inst. Sib, o+.d.
IN SSSR no.11:105-120 160. (MIM 1416)
(Electric power distribution)

JaikuwIll, V.K.
Dynamic stability of half-wave tuned power transmission lines.
Trudy Transp, enarg. inst. Sib. otd. AN SSSR no.14:67-74 162.
(MIRA 16:,))
(Electric power distribution)

-~ ~i "%M~17 T PI , V . '~ ,
Cporat..".or of' ~ half-w!t-p~ tuned lLno W"A; I'.
-,.,: 1, ... I
'y 'I *' ? - " 1) r,. f;.*:.r3
rachi ne o . Trudy Sib. n,,,t-,.,ch .-issl o Irist . -:?, :",*,..I;,, I (,I
I . cy I I ~
( m, 1 -1 1! 1;,, : 5 ) I

L ztt~(30-00
ACC NRz AP6016981 SOURCE CODE: UR/0281/65/000/004/0011/00'.8
AUTHOR: -01shevskiy, 0. V. (Novosibirsk'/;V' Samorodovj G. I. (Novoriibirsk)
yhajevjn,_V_..Y,._ (NovoAibir_Sk)____
-_-Oituf- one
TITLt: Q aasistationary -solution -of-a- transient-process-in
SOURCE: AN SSSR. Izvestiya. Energetika i transport, no. 4, 1965,,11-18
TOPIC TAGSs electric power tranamietsion, mathematie op6rator
ABSTRACT: - On the basis of a solution for the equations of along line in the
form of DtAlembert, the operator method is used to produce asolution for the.
equations of a transient process in individual sectors,of time in the form OZI
a functional dependence on the parameters of the electrical transmissiono
!current or voltage in the stationary regime and the number of the bection.*,
The advantage of the suggested method are especiaUy great in the case of
-number of time seetbre less than ten'. Orig. art. has: 15 formulas, 2 tijures,-
and 1 table. [JPRS]
SUB COM 10, 12 SUBM DATE: 2lSep64 allG REF: 001 SOV RZF'- 003
Card K_Y/0~ UDC, 621-3.051.025.2_
J/

TURMITAUB, H.S., professor; EX&MIM, G.L.
k,
Therapy of pulmonary abscess. Klin.med. 31 no.10:88 0 '53. (MIRA 6:11)
1. Is propedevtichookoy terepevticheskoy kliniki (zaveduyushchiy - professor
M.S.Tiirkelltaub) Arkhangel'skogo meditainakogo instituta i Bollnitey vodnikov
im. Semashka. (14mgs-Abscess)

j~~ R4 e- KI IV t? Cr - 14 -
1~,'-FR'Medicine _- *pertension FD-1758
Pub 1111-5/15
iiuthor : Khalevina G. L.
Title : The effect of a low calorie diet on hypertension crises
Periodical : Vop. pit., 24-26, Jan/j?eb 1955
Abstract : Putting patients on a diet of raw vegetables, apples, watermelons, compote,
or milk for 1-2 days lowered the cerebral blood pressure to a significant
degree. Such symptoms as headaches, inzomia, vomiting and nausia, dis-
appeared. No references.
Institution; Propuedeutic Therapeutic Clinic (Read-Professor M, S. Turkelltaub)
Archangellsk Medical Institute
Submitted : - -

AUTAMRS: Zimin,!.A. and Khalevina, 14.B. SOV-132-58-8-cJ/16
------ -1
TITLE: utilization of Kagnetometric Data for the Evaluation of Fro-
spective Reserves of Eagnetite Ore Deposits (0b ispol,zovanii
magnitometricheskikh dannykh pri otsenke perspektivnykh za-
pasov magnetitovykh meBtorozhdeniy)
PERIODICAL: Razvedka i okhrana nedr, 1958, Pr 8, pp 19-21 (USSR)
ABSTRACT: The authors compare the results obtained by geologists con-
cerned with the evaluation of prospective reserves of the
Kustanay contact-metosomatic deposits of magnetites after
seven years of prospecting operations with the results ob-
tained long ago by the magnetometric survey of the more im-
portant deposits of the Kustanay region. The interpreta-
tion of the magnetic anomalies of these deposits was made
by the method of selection according to the nomogram of D.S.
L'ikov and with the help of the bilogarithmic nomograms of
V.A. Bugaylo. The authors calculated the Yurzhunkullskoye de-
posit's reserves at 100,000,000 tons while other geologists
calculated the reserves at 77,000,000 tons with the north-
Card 1/2 western part not yet assessed. The reserves of the Sokolovskoye

SOV-132-58-8-5/16
Utilization of Magna tome tric Data for the Evnluntion of Prospective Reserves
of Magnetite Ore Deposits
deponit were estimated by Ye.,"I. Viahnyakova by the maeneto-
metric method as 410,000,000 tons and according to test
drilling operations they viere estimated as'471,600,000 tons.
This means that the difference in caai&tion by botl_~A%
thods is less than 1%. The Sarba, anT the Kachar-, depo-
sits showed almost the same correlation. The authors find
that the magnetometric method can be used for the calcula-
tion of reserves of magnetite ores. There are 3 tables.
A215CCIATION: Uralgeofiztrest (Ural GeophysicaI Trust)
1. Magnetite--Abundance 2. Magnetite--Economic aspects
3. Magnetite--USSR 4. Mathematics--Applications
Card 212

~ I ;-~- I'-! ~ - V7
"Froblem of ti,e Yeasuren-mt of f.Ye Tem-,eralure tind Purddity at 1.ow Altitudes,"
Yeteorol. i gi-Irologlya, I!o 9, 1953, pp 47-49
The author points to the extreme necessity f'--r the m-anlza'ion of aerological
otservations at low altitudes (up to 100-150 mters) for the solution of a nurber of
ir..!-.ortant'r.rollems of weather forecastin,-. In*rartJcular, he notes the recessity for the
construction of a lightened meteorograph which can be lifted in the envelope of an ordinary
pilot talloon. (RZhGeol, No 5, 1954)
,SO: Sum No. 5(8, 6 Jul 55

Subject USSR/Meteorology and Hydrology
Card 1/1 Pub. 71-a - 8/23
Author Khalevitskiy, Z. Z.
AID P 1434
Title Unused possibilities for the accounting of space
distribution of cloudiness
Periodical Met. i gidro., 1, 32-33, Ja - F 1955
Abstract Out of three methods of recording cloudines:
1) by the nephascope, 2) by airplane sounding of the
atmosphere, and 3) from observations from airplanes on
routine flights, the last method is emphasized. It is
of essential practical value in ascertaining the r.4ea
of cloudiness, its volume, and the amount of
precipitation it releases in different layers. "'Mis is
important in the synoptic analysis and in forecasting.
Two Russian references.
Institution: Main Administration of the Hydrometeorological Service
at the Council of Ministers of the USSR
Submitted No date

MYSKOVA, N.M.; TGMA, O.F.; FECHKIN, K.P.; KHALEVSKAYAj S.I.;
GOLISKAYA, I.F.; NEPOROUNTY, P.S.,-!;-d,.--;--N*,O--V--I-T~kly,.-L.M.,
nauchn. red.; GORDEYEV, P.A., red.; GOLIBERG, T.M., tekhn.
red.
(Album of new construction equipment; recommended for use]
Allbom novoi stroitellnoi tekbniki, rekomenduemoi k vnedre-
niiu. Moskva, Goastroiizdat. No.2. (Construction of power
engineering structures, Electrical engineering structures]
Energeticheskoe stroitel'stvo. Elektrotekhnicheskie raboty.
1963 111 P. (MIRA 16:10)
iPower engineering) (Hydraulic structures)

MALEVSKIY, B.M. dotaant (Rostov-na-Donu)
W--WlfWp-" . --
,. ~Congenital heRrt defects, Vrach,delo no,3:283-284 Mr'58 (MM 11:5)
1, Kafedra dingnostiki vnutrennikhbolezney (zav. - prof.'
B.N. MikhFqlov) Rostovokogo meditninskogo instituta.
(HEART-ABNORMITIMS AND DXFORMITIES)

S/180/60/000/03/025/030
F.R?A~F-3(1?
AUTHORS6, Kravchanko, V.S. and Khaleyev, oscow)
I 7"awm"
TITLE- Some Relationships ir; ~the 77flammability of Explo3ive
Mixtures of Saturated Hydrocarbons with Air
PERIODICAL: Izvestiya Akademil nauk SSSR, Otdeleniye telchnicheskikh
nauk, Metallurgiya i toplivo, 1960, Nr 3, pp 133-139 (USSR)
ABSTRACT: The relationships described in the paper were found during
the authors' investigations on spark safe currents in
electrical circuits in an explosive atmosphere of multi-
component mixtures of hydrocarbons of CnH2n4.,,2 series.
Ort the basis of their own experiments and with two and
multi-component mixtures of alkane series and literatur
data, tile authors established that the most dangerou5 )c
concentrations of hydrocarbons in air are inversely
proportional to the square roots of their specific (or
molecular) concentrations. Similar relationships were
found to hold in respect of minimal current which on
breaking of the circuit would ignite such mixtures. Thus,
a direct rel.ationship exists between the most dangerous
concentrati.ons of hydrocarbon-air explosive mixtures%and
Cardl/3 minimal igniting currents. Using this relationship one can

s/18o/60/000/03/025/03o
Eq~l~f3japl
Some Relationships in the Inflammabill osive Mixtures of
Saturated Hydrocarbons with Air
determine the most dangerous concentrations of any
explosive mixture, lower and upper explosive limits and
safe currents on the basis of the same data for methane.
A comparison of calculated and determined most dangerous
of alkane-air explosive mixtures and their
concentrations
dependence on the specific gravity of the explosive
component are given in Table 1 and Figure 1; the dependence
of igniting currents for gas and vapour air mixtures of
saturated hydrocarbons on their specific gravijy Table 2
and Figure 2 (probability of ignition p = 10- contacts
from steel wire 0.35 mm, in dia); the dependence of minimal
igniting currents on the dangerous concentration of
explosive component - Figure 3; the dependence of the
probability of ignition of various hydrocarbon-air mixture5
by circuit-breaking currents -- Figure 4; the probability
of the appearance of a mixture of hydrocarbons of various
specific gravities for a mine, situated in a neighbourhood
of oil-bearing strata - Figure 5. It is concluded that
CardV3 the relationships established can be used for calculating

s/i8o/60/000/03/025/030
Some Relationships in the lnflammabiliJO71~Ej~;losive Mixtures of
y 0
Saturated Hydrocarbons with Air
minimum Igniting and permissible currents and for the VC
evaluation of spark safety of electrical circuits on
chemical, petroleum and mining industries susceptible to
explosions. There are 5 figures, 2 tables and
6 references, 3 of which are Soviet and 3 English.
SUBKITTED: October 20, 1959
Card 3/3

Coll'?
.1 Of bIlUd.Li-
, , ,-lri co-U el jiroi.
7 no. 1:4
-5 JR-F'lc)5;?.
1"'Onthly Aut )f fius3im-n Accessions, Library of Con.,,reju, July 195,~. UnclaL;Afied.
IN 1
-K~,g

KHALEYEVA, L.D* [Kha-Ileieva L.D.]
Renal blood flow in experimental hypertension Of central nervous
System origin due to "Severing" of higher nervous activity.
FiziOl-zhur.1Ukr-) 9 no.1:123-125 Ja-F 163.
I. Kafedra normal Inoy, f iziologli (MIRA 1815)
instituta. Kharikovskogo meditsinskogo

SIMUTIVA, Ye.K., KATOROVA, M.A.,
,(gpkva)
Zffect of novoembichine on the course of the Arthus-Zakharoy
phenomenon and on anaphylactic shock [with summaz7 in English).
Patefisiol.' i ekspe'tergpe' 2 noe'5129-34 S-0 158 (HDd 11:12)
l' Is laboratorii okeperimentallnoy khisloterapH (saw. - chlon-
~;rrespondent AMV SSSR prof, LoYs Larionov) Institutr keperimentalluoy
pntologii I teiapti raka ANN SSSR;
(ALLUGY.'expero
anapbylactic shock & Arthus phenonmenon, off* of
N-Bis (2--chloroothyl-2-propylamine hydrochloride (Rue))
(NITROGN MUSTANDARDS. off;
N-ble (2-chloroetbyl,2-propylamine hydrocbloride,
on exper. ansphylactic shock & Arthus pehnomenon (Rue))

MIALVEYEVA. T.G.
7
r e-m- - bf hYPerPlasia of the mammary glands [with summary
in English]. Proble'endok. i gorm. 4 no.4:93-97 JI-A 158
&MA 11:30)
10 Ix laboratorii gormonoterapii (zav. - krana.biologicheakikh
nauk N.I. Lazarev) Instituta eksperimentallnoy patologli i terapil
raka AMU SSSR (dir, - chlen-korrespondent AM SSSR prof. HoN. Blokh1n).
(BREASTo dis
hyperpl:Bia, induction with ostrogen & pituitary
suspension in rats (Rua))
(ESMOGFXS, eff ,
induction of breast hyperplasia. with pituitai7 suspension
in rats (Run))
(PITUITARY GLAIM, physiol.
induction of breast hyperplasia with estrogens in
rats (Rua))

KIIALEMAP TOG,
y~of--t or-action of a numbor of antitumor preparations on cultureis
of human tumors. Biul. ekap. biol. i med. 49 no.1:9~-98 A 160.
(MIRA 13:7)
1. 12 laboratofti eksperimentallnoy khimloterapii (zav. - chlen-korres-
pondent AHN SSSR prof. L.F, Larionov) Instituta eksperimentalinoy
i klinicheakoy onkologii (dir. - oblen-korrespondent AMN SSSR prof.
N.N.Blokhin) AMN SSSR, Moskva. Predstavlens. deystv. chlenom AMN
SSSR A.D. Timofeyevsklm.
(C)IICER)

PRESNOV, M.A.; KHALEYEVA, T.G.
Cytological and cy-tochemical changes in a culture of cells of the
HeLa strain following the action of sarcolysine. Arkh.anat., gist i
embr. 43 no.7:51-59 JI 162. (MIRA 15:9)
1. Laboratoriya eksperimentallnoy khimioterapii opukholey (zav. -
chlen-korrespondent AHN SSSR prof. L.F.Larionov) Instituta
eksperimentallnoy i klinicheskoy onkologil AMN SSSR. Adres
avtorov: MoSkva, I-110, 3-ya Meshchanskaya ul., 61/2, korp. 9,
Institut eksperimentalIncy i klinicheskoy onkologii AMN SSSR,
(SARCOLYSINE) (CANCER RESEARCH)

KHALEYEVA) Z.N.p kand.sellskoklioz.nauk
Pea diseases in tho northwestern zone, Zashch. raot. ot vred. i bol.
8 no.705-36 Jl 163* (MIRA 16:9)
1. Pushkinskaya baza Voesoyuznogo inatituta zashchity rasteniy.

I I
A*13.; V0h0flKl"VP.,!!, L.V.; Giti-AKTIONOVA, N.M,
rjecobamical charactarlBtica of the organic lisseminated matter in
rocka of the Kazan stage In the VyatkB dinjocation zone and the
ad.facent rart of the Tatar Arch. Geokhimila no.12-1293-11298 D 1(4.
(MIRA 18:8)

Nam
M.Mialezov.
Vliiamie forry profilia i tolshchiny lopasti na kharakteristiku vinta. ;-Ioskva, 1932.
23 P., tables, diagrs. (TSAGI. Trudy, no. 129)
Summary in Englishe
Title tr.: Effect of profile shape and blade thic~mess on propeller characteristics.
QA911-M65 no.129
SO: Aeronautical Sciences and Aviation in the Soviet Union, Library of Congress,
1955

oz I 1IL-111i, G. 1. Jand -D.V.- KfMi,"ZOV.
DiagranoW dlia proektirovaniia vozduBhnykh vintov s profiliami VS-2. I-bskva, 1933.
30 P., tables, diagrs. (TSAGI. Trudy, no. 137)
Summary in English.
Title tr.: Diagrams for the design of propellers with VS-2 sections.
QA911.165 no-137
SO: Aeronautical Sciences and Aviation in the Soviet Union, Library of Congress,
1955

D.V.
Issledovanie raboty vinta s izmni0aermyT, v polete shagon.
diagrB. (TSAGI
- Trudy, no.174) "~Oskva, 1934, 27 P., tables,
Summary in English.
Bibliographical footnotes.
Title tr.: Investigation of controllable pitch propellers.
QA9ll-Y65 no-386
so; Aeronautical Sciences and Aviation in the Soviet Union) Library of Congress,
1955

C3TC3LA~I'SFII, 1.7. 2nd D.V. FHALEZCV.
Vizzi:,-mce vML-Ae'vi~Aa I s2nnleta. Moskva, 1935. 129 P., iliUs., t.-,ules, di2E-rs.
(TIVI. Trudv, no, 213)
if~ Zili-lish.
Bibliographical factn-tes.
Title tr.: Interfevence -,f Propeller and aircr2A cvqpwients.
QA911-M65 ng. 213
SO: lercnautical Sciences 2nd Avi2tlon in the Soviet 'Union, Libr:,ry of Congress,
1955

OSTOSLAVSKIIJ I.V.-, and D.-V. MALEZOV
Kharaketristika trekhlopastnykh metallichesklkh vintov TSAGI 3SIN-1 i 3314V-2.
,Nbskva, 1936. 34 P., illus., diagrs. (TSAGI. Trudy, no. 300)
Summary in English.
Bibliographical footnotes.
Title tr.: Characteristics of the CAM three-blade metal propellers 3SIN-2.
QA911. A65 no-300
SO: Aeronautical Sciences and Aviation in the Soviet Union, Library of Congress,
1955

OSTOSLAVSKII~ I.V., and D.V. KHALEZOV
Kharak-teristiki vintovykh profilei tipa Klark-Y. Moskva, 1937. 22 p., tables,
diagrs. (TSAGI. Tekhnicheskie zametki, no. 154)
Title tr.: Oharacteristics of the Clark-Y propeller sections.
TL570. M6 no-154
SO: Aeronautical Sciences and aviation in the Soviet Union, Library of Congress,
1955

KIIAL'.1- D. V.
K voprosu 0300snYkh Vintaldi. Moskva, 1939. 15 P-, illus., diagrs. (TSAGI. Trudy,
no.3R6)
Title tr.: Problems Or co-axial propellers.
QA911.Y65 n0-386
SO: Aeronautical Sciences and Aviation in the Soviet Union, Librar7 of Concress,
1955

KhaE~
Science (Field of Aerodynamics)
Concerning-aerodynamics of aircraft propellers,
Soviet Source: N: Stalinskiy Sokol, Moscow, 16 June 145
Abstracted in USAF "Treasure Island" Report No. 59885, on file in Library of Congress,
Air Infomation Division.

SM/84-58-12-42/54
AVMOR: Khalezov., D.., Doctor of Technical Sciences
TITLE: In the rerefrant of Soviet Aviation Sdience (V exangwde Sovetakoy
aviatsionnoy nauki)
FMODIM: Grazhdanskays axiatsiyaj, 1958., fir 12.. PP 29-30 (USM)
ABSMUCT; The author gives a brief description of the establishment of the
Tsentrallnyy aero-gidrodinamicheskiy institutp TsAGI (Central
Institute of Aera- dd H~drodynamits) forty years ago. The
construction of its laboratoriesj, provided with the latest equip-
menty including the superior T-1-2 wind tunnel, the largest of
its kind at the tims# was completed in 1927. A second working
section of the tunnel had an 8-sided cross sectionvith an inner
diameter of 6 meters where full-scale fuselages and propellers
were tested. A water tank, 200 z. longp 32 xvide,, and 6 m.deep,
Was built to test hydroplane models. A special laboratory for
investigating hydraulic zachinery,, a wind power laboratory., a
laboratory for the study of aviation engLnes.. and many devices
for testing aircraft aa helicopter propellers and autogiros were
constructed,, in addition to numerous other installations and devices.
Card 1/2
mnT,&L equipinent, num ji-t-u-sm-
studied wriation materials aud constructiOU in the field Of hydrodynamic
A.1q. Trpol,,3v headed the group de&Ung with exPeriwntal aircraft construe
tionp g.lidersp aerial sleds, and cutters. In this V=P vere 63-60
A.A. Arkhangel'sklY., V-M- PetlyakOy, P-()' Sukhoy$ and A-M' Cheremukhin.
V.p. Vetch-inkin worked in flight dYnWics.9 along with B.N. Yurlyev and
G.Kh. Sablydn. When the need arose to build new, more "Odern labora-
tories., a new TaWl was established late in 1935 on an enoxmous tract of
lmd near MOSCOV. The insta3-Wion of large vind tunnels to handle fALU-
scale aircraft and propellero was c6mpleted in 1939. Several a- or let-
boratories were added later. Vjhjs was, established a well equipped n
scientific aviation center. In the last few years TsWI has devoted cc
siderable attention to the study of passengrr aircraft with POWerftl
turbopz enginesp and to patting the finishing touches to their paver
units. There is I PhotograPh.
Card 2/2

KH~Lmov, L.S.
Suction underclearer systems for spinning machines, IZV.
"kh-t8lcBt- Prom. no-5:133-138 164. VYS.Ucheb.zav.;
1e Tvanovskiy takatillnyy institut imeni %4.V.Fr=ze. (MIRA 28il)

COUtr4hy U&SR
CATWORY i Cultivated Plants. Cereals. M
ABS, JOUR. RZhBiol, 1 ?10- 2]) .1955, No. 1046-34
AUT14OR P-rokoahov , V . it. ,
TNST. Molotov Agricultural Institute
TITLE VRCime Frobloms of Agricultural TechniqueS In the Cultivation
of Corn.
ORIG. 1"U13. Tr. Molotovak. a.-kh. In-to 1957* 15. 13-29
ABsTR-AcT The chief trend in the 4ultivation of corn in Wostern Ural
(results of the experiments at Molotov Agricoltural Insti-
tute and generalized conclusions from the wide production
experiAmce of kolkhozes) abould ehould be toward Its -
planting for sillage, Plantings for grain do not pay for
themselves. The following mid-seaaon and late maturing
varieties are rocommended for cultivation- Sterling,
Osetinakaya belayazubividuays, Krasnodarskaya 1/40,.
Odeaskaya 10 and the ea'rly maturing - VoronozhakaYa 76,
Cardt 1/2

KiftLEZOV, N.A., Cand Agr Sci -- (di,-~
IT thod:
j e cultivatim-
corn under condi,,ions of eermskaya Oblast.,, ferTif 19~9, 23 Pp
(Idn of Agr sci RSF-SIZ. p-rmi State Agr Inst ij-.1 Aca '-'~
rifilidcian
D.N. Pryanishnikov) 15o Coj)icS M, 34-59, lio
- 74 -

tuti(jilc

~
,77 77
USSR~L.Q themati cs
ca
rd 1/1
Author I Khalezo jj~
Title s. Automorphisms of matrix semi-groups
Periodical I Dokl. AN SSSR, 96, Ed. 2, 245 - 248, Vay 1954
Abstract 2 Report deals izj Fr, automorph isms. Automorphisms of the P'n E:roup
of all nonspecific matrices with elements from the F group are al-
ready known. Automorphisms of the Fr semi-t-roup are much simpler.
Each of the autotnorphism3 of the semi-kroup FS has a certain form.
Two references; 1 USSR 1953-
Institution S State Pedagogical Institute, Ivanov
Submitted I Presented by Academician A. N. Kolmogvrov, March 19, 1954,
March 19, 1954

_ PkUZOV-j-Ye,-Aj'(I:vanova)
i~
Automorphisma ar primitive quasi groups. Hat.abor. 0 no.3-.329-342
Mr 161. t OHIRA 34:3)
(Gro-Opat Theory of)
,?.* 1-11,

SOKOWV J, V.F.P kand-tekhn.nauk; IMALEZOVA
M.I., inzh. J, 91drobiolog; I:RAIMOVAP
Uo'ng
microctrainers. Vod.i san.tekh. no.1026_9
(Water-PUrlflcation)
162,
(MM .159-12)

XHALEZOVAO Ye-B.; NAZARENKO, I.I.
Bastnaesite of the Vishnevyye Mountains. Trud
kristalokhim-red.elem.(Vno.2:99-101 159. y lnst.min~p eeokhim.j
ishnevyye Mountains--Bastnaesite) MIRA 15'4)

YESIKOU.. Ye.M.; MTJKHITDINOV, G.N.; KHAUZOVA, Ye.B.
Characteristics of the chemical and mineralogical composition of
alkali rObka in the Viehnevyye Mountains, Trudy Inst. min., gookhim. 7
i kristallokhim. red. elem. no, 3z127-1" 159. (MIRA 1435)
(ViohnevM Mountains-Rocks,, Igneous-Analysis)

BOGDATIOVA, V-I-; MUMVITSKAYAp G.K.; ]~~ NOVA , Ye . B. ---
Determination of rare earths in zircons. Trudy IG124 no. 64.
Metod. khim. anal. min. no.1:95-97 161. (MIRA 14:7)
Rare earth-Analysin)
trcon)

S/081/62/000/001/016/067
B156/B101
AUTHORS: Bogdnnovag Ve I., Muravitskaya, G. N., KiMlezova, Ye. B.
TITLE: Determination of rare earth elements in zircons
PERIODICAL: Reforativnyy zhurnal. Khimiya, no. 1, 1062, 143, abstract
1D68 (Tr. In-ta -,eol. rudn. mestorozlid., petrogr.1
mineralor,ii i beokhimii.AN MSR, no. 64, 1961, 95-97)
TEXT: It has been established that the classical method (precipitation in
fluoride or oxalate form) does not always reveal