SCIENTIFIC ABSTRACT KOMAROV, O. - KOMAROV, S.G.

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• Collection: Scientific Abstracts
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• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

AN-UMAROV~ 0.
AUTHOR; Komarov, 0. 0 2 61/4 2
TITLE: Avtur-1 (Avtur-1)

PERIODICAL: Nauka i Zhizn'9 1957,A# 8. pp 48-49 (USSR)
ABSTRACT: The Institute for Au+nmation and Telemechanics of the USSR
Academy of Sciences has designed a contactleas automatic
level meter "ABTYP-11'- This device may be used for de-
termining the liquid level of reservoirs filled with oil, or
oil products, as well as various other organic compounds. The
device consists of two parts: an actuator (one-tube genera-
tor) and an indicator which are connected with each other by
two cables. The indicator also contains the power supply
unit which is connected with the acttator by means of one
cable. The other cable is used for transmitting the HF volt-
age from tht, actuator to the superheterodyne receiver with-.
in the indicator part. The actuator consists of a co-axial
cable section, shortened at the end, and is installed in the
reservoir of which the liquid level. is to be measuredo When
the device is switched on, resonance frequency oscillations
arise in the capacitance circuit which are transmiited by the
actuator to the receiver. By means of a tracking system
Card 1/2 the receiver is automatically tuned to the signals of the

Ov
valudW) 80. "1931).-Dwription of a 1.1-ton
qwU crytittil (kWh 3.8 m., diem. 1.6 ni.), from the ore
-,WPO*e of 11. 111"Pak-Dals (Ralkliash Steppe). Tke or-
-wrqnm in firipsk-Dab Is ebarazterbed by giant columnar
,kuru crrula throughout the mother rock. a weathefM
C.lemloet IS granite. The crystals are all white-milky,
with very abundAnt gas loclusioui. Columnar cryst.,14 )I
1 in. length and 2 m. diam. are not rate. Fuel
...........

..... . ..........................I................
USSR /Physical Chemistry. Crystpls. B-5
Abs Jour Ref Zhur - Khimiya,, No 8., 1957, 25081
Author A.L. Khodakov, M.L. Sholokhovoch, Yr.G. Fesenko, O.P. KcmarqX
Title Monocrystals of Strontium Titanite.
Orig Pub t Zh. tekhn. fiziki, 19569 26, No 11, 2505 - 2507
Abstract : The monocrystals of SrTiO (I) were prepared by crystalli-
zation 1) in a solution o? I in the melt of potassium fluo-
ride and, 2) in a solution of I in the melt of a mixture of
60 mol. % of Na2CO + 40 mol. % of K2CO 3* Crystals prepa-
red by the 1st meld are quite transparent, of light yellow
color and are confined within faces J100] , the edges being 1
mm long; the structure is that of perovskite with ideal cu-
cells; the refraction indet is 2*35, the x-ray density is
5.12, the picknometer density is about 5.0. Crystals prepa-
red by the 2nd method are less transparent of a smoky color,
the prevailing faces are ~1001 and ~li3 . and they contain up
to 0.7% of Fe; their x-ray density is 5.14. The dielectric
properties of both those kinds are scmewhat different.
Card 1/1

SENCHILO, N.P.; KOMAROV 0 F ~
Temperatures of cr7stallization of vein quartz in-rare-metal
stockworks; based on fracturing data. Trudy Inst.geol.nauk
AN Kazakh.SSR 6:210417 62. (MIRA 16:6)
(Kazakhstan--Quartz)
(Nazakhatan-Metals, Rare and minor)

KOMAROYP 0.11.1 PAPSHIN, A.Vo
Tempe'"aturea of the mine-ral formation of ;zaeolita ir, thri Karaoba
deposit acoording to thermal cracking data. Izv.MI &zr-,kP.S"'RO
Ser.gool-O' 22-no.5-.8247 8-0,465.
omw IR"2)
1. Tnatitut geologichaskikh nauk imeni KoI.Satpayeva, g.
Alm-'Attrm.

YORAPROV O.P.; PARSHIN, A.V.
--- ".1- -
Genetic characteristics in the formation of emeralds of the late
Hercynian massif in Kazakhstan. Trudy Inst.geol.nauk AN Kazakh.
SSR 7:327-3-45 163. (MM~ 17:9)

KMOKORMOV, D.N.; YERSHOVICH, A.N.; Prinimali uchastiye: FEDCHMO.,
A.M,; SHURUPOV, V.I.; BOLOTSKIY V D.- KCKAROV 0 S
ANDROSIK, Ye.l.; XUDI, V.I.; GALUSHRILI~-J-.1--~- -~",A.Nq
KROSENp R.I,; MURASHKOY O.A,
Technology of the production of gray cast iron in the mana-
faeture of tractor trucks. Lit. proizv. no.707-38 11 063.
(MIRA 17-- 1)
1. Nauchno-issledovateltakiy takhnologicheskiy institut
artomobillnoy prmyshlennosti (for all except Khudokormov).

KOHIROV, O.S., inzh.; MDOKORMOV, D.N., kand. te?1m. nauk
Effect of Sn, Sb, and Bi on the crystallization of magnesium
cast iron. Lit. proizv. no.1:36-37 Ja 166.
(1411u 19: 1)

Inz.h.;
of alminturl on th~
cast ion,
Lit. proizv,,' no.7i21~422-7- 165. (MIRA18,418)

BOBRYAKCVP G.I.; KOMROV~ O.S.
*draulic impact in foundry molds. Lit. proizv. no.6:-37-38
.To, - ~ 63 . (MIRA 16:7)
(rcunding)

RHUDOKOFMV, D.N.; KOMLROVL_~~
A,
CrystaUization of cast iron inoculated with ceriuml teUurlum,, apd
calcium, Litoproia, U0,021-23 AP 163, (MA IC:4-y
(Cut fior--=taUurgy) (CrystaUization)

KHUDOKORMOV,, D.N.; KOMAROVP O.S.
Characteristics of primary crystallization and the structure of
cast iron inoculated with rare metals. Metalloved. i tem. obr.
met. no.8t4.%4
1 WjAtW63. (MIRA 16slO) 1

220), 6(1)
SOV/178-58-7-7/24
AUTHORS: Lozhko, K., Guards Colonel; A2paxay,~. Guards Lieutenant,
Colonel; Lozhichevskiy, A., Guards Major
TITLE: The Radio Training (Area) is the Foundation of the Training-
Material Basis (Radiopoligon - osrova uchebno-materiallnoy
bazy)
PERIODICAL: Voyennyy svyazist, 10,58, Nr 7, pp 20 - 24 (USSR)
ABSTRACT: The authors describe the equipment and operating procedures
of a radio training (area) located about 10 km from the
permanent quarters-of a Signal Corps unit of the Soviet -
Army.. The radio-stations used for training are operated
from shelters and trenches. The-training ground is
operated from a central control point from which all radio
stations receive instructions. The switchboard used for
this purpose is shown.in Figure 1 and its circuit arrange-
ment in Figure 2. For creating combat-like conditions,
Card 1/2 a jamming transmitter is used, consisting of a SO-241

sov/178-58-7-7/24
The Radio Training (Area) is the Foundation of the Training-Material
Basis
master oscillator, a SO-257 power amplifier and a
SO-257 modulator. The soldiers undergoing training
are billeted at the training ground. ClaS8-rooms for
theoretical instructions are also available. There are
2 photographs and 2 circuit diagrams.
Card 2/2

XOKAROV, P., gl&YW inzhener,
Remoteheat control installation. Zhil.-kom. khos. 3 no.3:28-30 Nr 153.
I(NLU 635)
1. Mrasnopreenonskoys trazvavnoye depo. (Heating-Regulators)

KOMAROV, P.A.
Mining equipment manufactured by the 4shtym Machine Shop. Gore
zhur. no.8:43-" Ag 163. (~MIA 16:9)
1. Glavnyy konstruktor Kyshtymskogo mekhanicheekage zaveda.
(Kyshtym-Mining machinery)

'Lumbering
Speeding up the construction of rafts for the great construction projects of
communism. Les. prom. no. 5, 1952.
9. Monthly List of Russian Accessions, Library of Congress, August, 19524M. unclassified,

1. Eng.
2. ~600)
4. Lumbering-Pechora Valley
7. Tasks in the development of timber rafting in the Pechora basin. Les. prom.
13 no. 3 1953
9. MonthlY List of Russian Aecessions, Library of Congress, June 1953. Unclassifie d.

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The phase diagram OOL lw-melting mixtureso' II. The melting diagi-am of
oxygen-nitrogen and the phase diagram of nitr2gen-carbon monoxide. M.'Ruheman-
A.,,Likhter--a-n7EFP. Komarov. Physik. Z. So7j:"e-tunion 8, 326,-36(1935)j cf. C.A. 29$,
32'.-Measurements of sp. heat show that CO-N mixtsj form 2 complete series of
,,idxed crystals. The system O-N has a eutectic at 50-10K. and 23% by vol. of N.
The 0 lattice dissolves 16% N and the N lattice 69% 0. The heats of fusion of
the N-0 mixt. show a min. near the concn. of the satd. N crystal.
Morris Maskat

KUCHIM, Ta. (Chakhoolovabdya); AAR LKO, Ye.T.; MTASIWA. L.I.;
KOYAWT P N ; PROSIURNIN. K.A.
_E0
Dacomposition prodmate of phenol formed in the radiolysis
of benzene In aqueous solution, Wobl.fiz.khim. no.2:183-188
159. (MM 13:7)
1. Laboratorlys radiatsionnoy khimii Nauchno-iseledovatel'skogo
Miko-khimicbeekogo institute, imeni LeTaAarpovas
(Benzene) (Phenols)

L 8102-66 EWT(M /EWP(J)/EV1A(h)/EWA I
ACC NRt AP5026459 SOURCE CODE: UR-MiNT690-6-M-6516715 072
AUTHOR: Komarov 1~arelko, Ye. V.
(deceased) 0
ORG: Scientific Research Physico- chemical Institute im. L. Ya. Karpova
lNauchno-issl-edovatellskiy fiziko-khimicheskiy institutY-
TITLE: Radiochemical oxidation of butanol in aqueous solution at elevated tempera-
ture
SOURCE: Neftekhimiya, v. 5, no. 5, 1965, 715-720
TOPIC TAGS: aliphatic alcohol, gamma radiation, oxidation, oxidation kinetics'
ABSTRACT: Effects of temperature, solution concentratiqpd amma6O Co radia-
l , g
tion dosage ort the kinetics of the radiachemica %xidationloi aqueous solutions of
butanollwere investigated. Changing the alcohfli(concent ration from 0. 053. to 0. 76
ii~o__1/1 changed the oxidation product yield only 151/o. Increasing the reaction t6mp-
erature led to the development of chain oxidation reactions. At temperatures above
100 IC the chain reaction rate was only about an order less than in the oxidation of
pure alcohol. The induction period was somewhat longer and the reaction rate dur-
ing the induction period was. 2- 3 times less in the oxidation of aqueous solutions
than in the oxidation of pure alcohol, During the initial period the reaction rate waE
Card 1/2 UDC: 542.943+5 41.15:547. 264

I. - ";

77
L'8271,66 aff'(W/gEft RM
VAP5-0?6460 OURCE CODE: UR/026WV663T655767~j,TOK
S9
AUTHOR: Komarovs- P0 He
ORG; scientific-Research PhysicIochomical Inatitut im. L. Ya. Karpova
(Nauchno-isaledovatoltakry- fiziko-ida-Imixtieskly Enstitut)
0 pait-60 gaga radiati n on th kinetics
TITLE: Effec t of dose rate f olo 0 a
of the initial stage of radioche6le k1 -oxidap- ion-o--f buEanol In aqueous.
solution
SOURCE; NefteRhimiyal ve 5j no* 5P 1965P 721-724
T 0 P IC. - mos'i x1dation-kinetic
t
ABSTRACT:' ~.T:he 'e' f f e- 'a t' o_ 15 x l
f dose rate (4,2 x 10 to 4,0 0 e cm3 - a
-obtained by radiolysis of aqueousn-butano).
on the oxidatLon products
solutions .(0.981o1/1) was studied. The chain length ofthe reaction.,
products--is-approximatol7 proportional-to the reciprocal of-thesquare.
root-of the,initiation rato, Hance with a high rate the chains are
very short 'and with lower rates the.role of.products formed by chain,
-reactions increases, However,, the linear relationship between the
increase in dose rate and the accumulation of peroxides (formed by
chain growth) and of aldehydes and acids (formed by chain rupture)
Card 112,

KOMARMr . P; N.
Radiation-chemical oxidation of bitanol. Effect of butanol
concentration on the composition and yield of products.
Nef'uekhimiia 5 no.6:863-868 N-D 165. (MIRA 19:2)
1. Nauchno-issledovatellskly fiziko-khimicheskiy institut
imeni Karpova. Submitted Jan. 25, 1965.

SULTANOV, T.A.;JO!~~t,,.P. N.
RoUimg ooorse thredds with thread-roUing heads. Stan. i instr.
35 noo7sl+2-43 Jl 164.

ZYUZINP I.M.; KCMOV, P.S.
Tuportaht resouroes for increasing crop yields. Zashcb. rest.
ot vred. i bal. 6 no.10:8-9 0 '61. (MIRA 16:6)
1. Perv~y i6kretarl Kalacheyevskogo ravonnogo KOmiteta
Unuranistichaskoy partii Sovetskogo Soyusa (for Zyusin).
2, Ajroficm'p6 vashchits rastedy sel'skogo khozyaystva
Nalacheyevskogo rayons.IVoronezhskoy,oblasti (for Komarov).
(Kajach-Distriet(voroniazh Province)-Plantc,
Protection of)

xcmov F. S.
Highly opectal-ired unit. Zashch. rast. ot vred. i bol. 5
no.10:7 0 160o (HIM 16s 1)
1. Nachallnik otryada Kolacbeyovskoy rayormoy trnktornoy
stantaii po bor'be e vreditelywd i bolesnyami rasteniy.
Kalach Diatriet-Spraying and dusting in agriculture)
1ach District--Sugar beeta-Diseases and pesto)
t

11-il.5354-6 34T(l) aw
ACCNRt AR6001127_ SOURCS COM UR70_269/65/000/M9/0025jM25
SOU ICEs Rafe zhe Astronomiyas Abs. 9*51.235
AUTHORs Komarovt Pe so
TITLEs Electron densities in the atmospheres of "metallic" stars
REFERMED SOMFa Irv. Krymak. astrofis e observe 9 v. 339 1965p 273-278
TOPIC TAGSs star, electron density, rotation.. atmospughterep Balmer seriesp-hydrogan
line
TRANSLATION.- The electron densities no in the atmospheres of metallic and normal
stars of spectral classes A245 of the main sequence are compared. Spectrograms
with a dispersion of 150 A/= are~used. The values of ne are.determined from the Elm
rmmbers of the last observed Balmer lines.by means or the Inglis-Tel-ler formula.
In finding the numbers n., the dependence of the equivalent width upon the Une
number n was extrapolated to the zero value of We A correction for the rotation
of the star was introduced into the so-obtained values of %~ It was shown that
the electron densities in the atmospheres of metallAc stars agree,, on-the average,
with the electron densities in the-almospher6a of normal stars or the same spectral
class (as determined by tVdrogen lime), Bibliographl of 9 titleae Ae Kolesov
SUB CODEs 03
C'Urd lay. uDr. t 523,001

AUTHORS: Sokolov, G.A. and Komarov, P.V. SOV-11-58-8-"4/14
TITLE; Transformation of Ludvigite in the Magnetite Deposit Zhelez-
nyy Kryazh inthe Eastern Transbaykal Region (Izmeneniye
ludvigita na magnetitovom mestoroohdenii Zheleznyy Kryazh r
Vostochnom Zabaykallye)
PERIODICAL: Izvestiya Akademii nauk SSSR, Seriya Geologichoskayap 1958P
Nr 8, pp 27-37 (USSR)
ABSTRACT The autho3ndescribe ludwigite, associated with magnesium
skarno, as a late skarn mineral secreted metasomatically.
It is often found in the 6ontact-metasomatical "Zheleznyy
Kryazh" iron ore deposits. Zones of forsterite tikarns,
usually serpentinous and containing small quantities of mag-
nesium minerals, are the most favorable places for ludwigite.
The magnetite is often found in such skarns and even forms
magnetite ores. In places where ludwigite is formed, the mag-
netite usually fills the intervals between the priamatic rays
of ludwigite; some times its aggregates replace these rays.
This circumstance indicates that the magnetite was formed
after the ludwigite. In single sectors, iron sulfides, main-
- ly pyrrhotine, are also developed and belong to a later hydro-
Card 1/3 thermic stage. The rocks containing ludwigite are represented

SOY-11-58-a-3/14
Transformat,ion of Ludwigite in the Magnetite Deposit Zheleznyy Kryazh in
the Eastern Tranabaykal Region
by mineral associations with largely changing content of
waterless skarn minerals, ludwigite, magnetite, sulfides and
other secondary minerals. Sulfides are distributed in these
rocks irregularly. In zones with a high sulfide contents t-he
ludwigite undergoes many transformations, and samples taken
from various depths showed that they contain either thinly
dispersed pyrrhotin or colloidal sulfides of iron. As a rq-
sult of different laboratory research, it was found that the
higher the degree of transformation of the ludwigite, the
more boron it looses, even to such an extent that the 74jhelez-
nyy Kryazh deposit cannot be commercially exploited. It was
also found that the decomposition of the ludwigite is especial-
ly intensive in those parts of the deposit where the sulfide
.mineralizat'ion is more pronaiinced.
There are 7 photos and 3 tables.
SUBMITTEDi August 19, 1957
Card 2/3

SOV-11-58-8-3/14
Transformation of Ludwigite in the Magnetite Deposit Zheleznyy Kryazh in
the Eastern Transbaykal Region
ASSOCIATIONt Institut geolojii rudnykh mestorozhdeniy, petrografii, minera-
logii i geokbilmii AN S35R, ?Aoskva (Institute of Geology, Ore
Deposits,'Petro6raphy, Mineralogy and Geochemistry of AS
USSR, Moscow)
1. Ludwigite--Sources 2. Ludwigite--Properties 3. Ludwigite
---Availability
Card 3/3

KMAROV, P.V.; NAKTINAS, Ye.M.
I--
Fluorine, chlorine, and boron as elements-indicators in geochemic-al
prospecting. Geol. rud. mestorozh. 7 no.3:65-74 My~Je 165
(6A 1917)
1. inntitut geologii rudnykh mestorozhdeniy, petrografii,
mineralogii i geokhImU AN SSSR.

3(5)
SOV/11-59-5-7/14
Koma-rov, P.V.
TITLE: On the Connection Between the Formation of Magnesian
Ecarns and Gran-itization ( 0 svjazi obrazovaniya
mab-lezial"nylch skarnov s [;ranitizzatsiyey).
PERIODI-'VAL: Izvestiya AkadeLLli nauk SSSR, Seriya geologicheskaya
1959, Nr 51 pp 90-102 (USSR)
'iBSTILICT:
The Zheleznyy Krya.zh iron deposits in the Eastern
Transbaykalian region are of contact-metasomatic
origin. They are situated in the zone of contact
of Kutomara Variscian Granitoids with Lower-Pale-
ozoic sedimentary rocks. These Tmot-amorphized rocks
form residual block of different dimensions in the
upper part of the Granitoid iiiassif. Their lower
parts are composed of hornstones, maGnesia and
calcareous scarns and quartzites, and in their
upper parts, chloritized sandy-argillaceous slate.
Card 1/6 Granitoids have clear intrusive contacts with the

SOV/11-59-5-7/14
On the Co.-mection Between the Formation of Llragnesian Scarns and
Granitization
metamorphized sedimentary blocks. PTior to the meta-
morphizm, the lower parts Y:ere composed of sand-
stone, interbedded with sandy-arGillaceous and
carbonate-arGillaceous slate. ks a result of meta-
morphic and metasomatic process, these slates
and sandstones were transformed inLo various horn-
stones and quartzites. MoBt of the interbodded
ar-illaceous slate was transformed into magnesia
C
and calcareous scarns, which later were min-eralized.
The calcareous pyroxene-garnot scarns -,,rore of post-
magmatic origin. In some placcs, th--ay also re-
placed the magnesia scarns, provinG in that-way
to be of a later origin. In some places magnesia
scarns vere intersected by dykes of Granite-
aplites and diorite-porphyrites partly replaced
Card 2/Eb by minerals from calcareous scarns. Thus,-these

Sovil-C-9-C-7/11
11 -j 14
On (~'onnectio.-x Between the Formation of Marniosian 30.arni
and G--,--ixt.itization.
dykes were formed after the mamnesia scarns but
earlier than the calcareous scarns. The inj,?~ct-:Lo-a
of Granitoids is observed in maCne~3ia scarnr'~ ran,-d
in the diopside-plagiocla--tic rock.,, r;urrowLdlaz
the scarns. A distinct meta-comatic zonality i0i
the magnesia scarns surrounding the bybi~ld 6raArl-
toids is also observed; a granitoid dio-sido. oj,
diopside-spinel zone and a forsterite or 'Cor-
sterite-spinel zone. Granitoids in contact with
magnesia scarns have no traces of metasamatic -
changes, The author gives on (table 1) t1ie result
of the tmalysis of hybrid Cranitoids, shov-,,in~.7,
changes in their chemical composition occuring
in the interaction of granite magma t,,rith se~iiraen-
tary rocks. As to the process of granitization,
the author shares the vier., point of Academician
D.S. Korzhinskiy who considers the graniiji--at-ion
Card 1'-/6 process to be an infiltration-ol magmatiG re-

SOVI 1- 59-
On t1l,_~ Connection Between the Formation of Magnosian Scaras
place ment of enclosing rocks with "Uho f.Nrontiot~
of Gra-taitoids. The C;ranitizatlon -IM-4L,
Lorily occurs vrith an into rLlodiato, stago -if
diffusion or melting of enclosing rocks --and
summary composition of the neit equals the (,,u"-:,:?ct_Jc
composition for granitoids. One poculiarity of
granitization process is the formatio.-LL,
the magmatic stage of magnesia scarns of in.-
filtration type of Zheleznyy Kryazli deposiit~~.
The magmatic solutions of the infiltration ty~'le
conditioned the development of granitizatioA i)T--.j--
cess of dolomites and, as a result, alon,~; -.~-itlt
the formation in exocontacts of m-1--nesia sca--nns),
U
hybrid granitoids of increased basicity ~-rd alkali-
nity were formed in the endocotact zone of Granites.
Their increased alkalinity is connected in tulrds
case with the increased activity of alkal, in tho
Card 4/3 magmatic solutions as a consequence of its (alkali)

SOVIJJ-59-5-711L~
On the Connection Between the Formation of Lla-nesian Scarns and
Granitization.
inter,ae.tion with dolomites - rocks vrith a high
basic concentration. Such increase of alkalinity
permits the distin-,uishin~ of the magmatic in-
filtrational replacement (r-ranitization) from
U
the phenomenon of as-ilrdlation, which also occured
in some places of the Zheleznyy Yryazh deposits
and caused the formation Of Granit-oias of an
increased basicity. The author mentions the follow-
inG geoloGists in connection with t-his article:
I.I.A.Usov, V.A. Mlelioranskiy, V.N. Kozerenko, G.D.
Afanas'yev, IT.G. Sudovikov, N.M. Uspenskiy and
V.A. Zharikov. There are 4 photographs, 2 tables
9 graphs, 1 profil--i and 26 references, 20 of vhich
~.Iard 5/6 are Sovietq 5 American and 1 English.

SOV/11-59-5-7/14
On the Connoction Between the Formation of 11agne-r-Jan. Scarns and
Granitization.
ASSOCIATION: Institut geolog-ii rudnylch rez-lu-orozhdeniy, petro-
grafii, mineralog-ii icpo~:himii ,UT SSSR ( The In-
stitute of GeoloGy of .4dneral Deposits, Petro-
C-;rapby, Mineralo,-y arrid Geochemistry of the JIS
USSR, Lloscow)"
SUBLIIITTED: October 25 10,58
Card 6/6

ALIMBAYEVA, S.K.; ZINLYANAYA, G.P.; KOMAROV, P.V.; CMMVTAKOVA, G.P.
Spring excursions to the mountaina. Vch. zap. Kir. zben. ped. lost.
no. 4s153-216 159. (MMA 14:1)
(UrghtsIstan--School excursions) (Biology--Study and teaching)

KOMAROV~ P.V.
Magnosian skarns in the Teya, Geol. rud. mostorozh. no.2:n9-124
Mr-Ap 161. (MIR& 148 5)
1, Inatitut geologii rudnykh mestoroshdoniy.9 petrografii, mineralogii
i geakh4voli AN WSR,
(Kuznetsk A3.a-Tsu--SkLrns)

I
Studying some quantitative,indices of DNA-mediated transmission
of streptoaWcin resistivity in ataphylococci. Mikrobiologiia 31
no.3s454-458'Ylr-Je 162. (KIRA 15s12)
le Kirgisakly shenakly)pedogogicheekly inatitut, Frunze,'
(NUCLEIC ACIDS (STAPHYLOCOCCUS) (STREPTOMYCIN)

K%IAROV, P.V.
,,T
Specific activity of IUA obtained from transformed or adapted
staphylococcal cells. Mikrobiologiia 32 no.109-42 163
(MIRA 1713)
1. Kirgizskiy zhenskiy pedagogicheskiy institut, Frunze.

KOMAROV9 POVU
Geonhemical qpe'cialization of ore.-forming solutions of igneous
origin in relation to mineralizatLon (chlorine, fluorine and
boron). Geol. rud. mestorozh. 5 zio.6.-51-64 N-D'63.
(KMA I,I.35)
1. Institut geolngit rudnykh meotorozlidanly, potrografti,
mineralogii i geokhJirdi AN SSSR, Moskva.

20925
S/057/61/031/003/009/019
B125/B202
AUTHORS% Komarov, R. M. and Petrov, V. I.
TITLE: Study of a high-frequency discharge in a proton source
PERIODICALt Zhurnal takhnicheakoy fiziki, v. 31, no. 3P 1961, 321-326
TEM The authore,discusa.the effect.of.gas pressure in a high-frequency
proton source on the-temperature Te.of the electrons, the ionization
density ni of the.atomio-hydrogent the power W consumed by the discharge
and on the ion.current.IM emerging from the source. These high-frequenoy
discharges,were studied with-and-without application of a high-frequenoy
field. The change of ni and Te during the discharge as a function of gas
pressure was studied by optical methods. The ionization density (in
relative units) was determined by using the relation n oonst 9 (T
9 9 '
where 10 is the intensity of the line H 0 and C (T is a function of the
excitation cross section and of the ionization cross section of hydrogen as
well as of the energy distribution of the electrons in the discharge. The
Card 1/8

20925
S/057/61/o31/oo3/oo9/o19
Study of a high-frequenoy... B125/B202
absolute value of the power consumed by the discharge was not measured
but only the character of the change of this power as a function of the
gas pressure in the source with and without external magnetic field. The
experiments were made on a special vacuum stand. The experimental scheme
is shown in Fig. 1. The high-frequency discharge was excited by means of
a 25 me generator. The light which was produced during the discharge was
directed to a XC-55 (KS-55) spectrograph by means of a lens system. A
OY-25 (FEU-25) photomultiplier was directly connected behind the outlet
of the spectrograph. The ion current emerging from the source was
captured by a beam catcher. The external transverse magnetic field was
produced by means of an.NS electromagnet. All measurements were made with
reduced power of the generator. Fig- 3 illustrates the dependence of the
electron temperature on the pressure of hydrogen in the diacharge chamber.
Fig- 4 shows the dependence of the concentration of atomic hydrogen ions
on gas pressure. Fig. 5 shows the dependence of the power at the lateral
*all of the discharge chamber on the gas pressure; Fig. 6 shows the change
of the total current of hydrogen ions as a function of gas pressure if a
transverse magnetic field is applied. Fig- 7 illustrates the same as is
Card 2/8

Study of a high.-frequenoy.*6
20925
B/057/61/031/003/009/019
B125/B202
shown in Fig, 6, howeverl.wi-thout.external--magnatia.field. The results
of measurements may be sumaskrized.-as.followai 1) the temperature of the
electrons in a high-frequency discharge can be considerably reducedt
a)-with an increase in the gas pressure in the 's-ource; b) by the applica-
tion of an external transverse constant magnetic field, especially at
piessures below 35-40-10- 3 mm Hg; a).with.an.increasa-in the--generator
power. In the case studied here the elect-ron temperature was 6000-80000KI
25 the concentration of the atomic ions and the power-consumed..daringthe
discharge are a nonmonotonic function of.pressure. With.laaking-external
magnetic field and also with a longitudinal magnetic field,they have a
maximum at pressures of about 3-10-2 mm Rg. The application.of a trans-
verse magnetic field considerably increases the density of the-atomic
ions and the power required for the dischar e whose maxima.are shifted
toward lower pressures (15 to i8oo-3 mm Hgl. On the conditions described
the degree of ionization of the source was low; it amounted to lose than
one thousandth %. With ordinary conditions of operation of the source the
degree of ionization was by one order of magnitude higher. Also the
proton content in the ion beam is a nonmonatonic function of pressure,
Card 3/8

20925
S/057/61/031/003/009/019
Study of a high-frequency... B125/B202
where the maximum lies at about 2 -10-3 mm Hg. The optimum gas pressure
at which the current of atomic ions is the strongest is always lower than
that pressure at which the concentration of the atomic ions has a maximum
in the discharge. There are 7 figures, 1 table, and 5 references:
3 Soviet-bloc and 2 non-Soviet-bloc.
SUBMITTED: May 30, 1960
Card 4/8

-;,
s., pulpt-3kovnik, Ceroy vetskojr-
rMraim-Plificatiorl grazit harm. -our. Vcoriazh.
.,j.C 1'7,
,111 4 no. 10, 59 I'lly 161.. 1111'

NOMAROV, S.
I---_,
Conference on cooling furmoss. RIO no.9:54 8 '59.
04IM 13SI)
(Purnaces--Cooling)
W&

KOH&ROV. S.. insh.(Koskva)
Decisions taken should be carried out. NTO 2 no.2:34 7 160.
(MIRA 13:5)
(Power *vgineering)

-ARAV-- Sw insh.
So that the fuel.would not go up the chimney. NTO 2 no.11:26-27
h l6o. (MIR& 13:11)
1. Treat "Zaergocherviet.g
(Furnaces)

KOMAROV, S., Geroy Sovetakogo Soyuzaj, podpolkovnik
-- --------
Everything jj'jmpQrtaA+, if it concerno military discioUne.
Komm.Voorush.Sil 2 no.5t27-30 Mr 162. (MIRA 15:2)
(Ruasia-Air force)
(Military disoiipline)

KCWGV, S., podpolkoviaik.4 Geroy Sovetskogo ajyuza
F3ag crews should maintain order in the airfields. Komm.Vooruzha
Sil 3 no.19:60-63 0 162. (MIRA 15:9)
. (Russia-Air Force)

KOKLROV, S.A., inzhener; RA I a a$ -in-
Timber economy for 3-10 kilovolt networks.
I- - & fMr3aTW -I
Ilek.sta. 24 no.4:48-30 Ap t53.
(KUW4j-)
(Aloctric line#-Foles)-
I

KOLUROV, S. A.
Xortico-vic,3* ral Theory of th-- PathoEerasis of Ulcemus Disaases (Russian book by K. M.
F~rkov and 1. T. Kurtsin., publilshed in Mosem, 1Y49) EXTRACTs -According to the findings
of -~'. B. Popellskiy (1902, 1919), Bibel' (1908, 1913), and oden o (1910), it is namely
in the pyl6ric portion of the stomach that there are produced during digestion specific
hormones,, pylorin,, hystamin, substance "P"9 and pylorantrum-gastring possessing the
ability of stimulating the secretory calls of the fundal glands. These investigations
have been confirmed recently by Ae, M. Varob"711v (1935, 1937,9 1947)" S. A. KOMROV (19380,
1942), and others.
SOURCE': ClAs FDD U-35289 13 MV 1953t p 81, Restricted

6-58-2-10/21
AUTHORt Komarov, S. A*
TITLD: Distance.Nesswements-Along Routes of High-voltago Above-ground
Lines (Dallnomernyye izmereniya na trassakh vjsokovoiltnykh
vozdushnykh liniy elektroperodachi)
PERIODICAL: Geodeziya i Kartograftya, 195e, lir 21 PP. 38 - 41 (USSR)
ABSTRAM Up to now tape measure and levelling instrument have been used
for these purposes. The use of a range - finder - the tachy-
meter - was found rather inefficient arid it was used only on
difficult terrain (mountains). The author here demonstrates
that this opinion is not correct since in all cases the appli-
cation of the tachymeter guarantees sufficient correctness at
increased operation efficiency. In the case of measurements
of span widths up.to 200 m the maximum error limit of height
in the middle of the span width is beyond - 5 cm and of the
distance beyond - 1 cm. It is shown that this deviation can
be observed also by using the tachymeter. On the other hand
Card 1/2 the application of the tachymetxic method has the following

6-58-2-10/21
Distance Measurements Along Routes of High-voltage Above Ground Lines
advantages: the same,instrument can be used in plains and
mountains, only 5 men are necessary instead of '10, increase
of working productivity since no marching is necessary (which
takes 60 %6 of the working time), no cleaning of the levelling
plates from earth. Up to a voltage of 10 kV levelling auto-
matons can be used. They still have to be tested for higher
voltages.
1. Tran.smission linea-Zonstruetion 2. Range finders-
APPlications 3. Range finders.-Performance
Card 2/2

Tobacco Cuing
14. 1.1. Nadeyev and V. A. Gornyyls pamphlet "Curing barn for tobacco and mrkhorka"
(Sollkhongiz 1950) and plano for tobacco plants of the "SellkhozaturcipmkV in 1950. Tabak
k3 No. 4 1952.
9. Monthly List 2.f Russian Accessions, Library of Congress, October -195X, Uncl.
2

r, 7 '" :1
. I. I k' V , 0 . - -- - - - - - - - - - - - --- - ---- - - -- - - - - -- - -
'e"o:'lu I-Ov, - f 6
and Zhabrov, D. "The GhQnj;u in tho Vuluou of ftecorflud R-tiAitivity Taking,
Flacp in the Practice of Coring." Azerbaidzhanskoe lkftigno--~ Mhozlais~.vo, Baku, I-To. 10/11,
10135t pp. 20-32.

1. 10MAROV, S. Gt ALIPINO L. M.
2. USSR (600)
4. Prospecting - Geophysical Methods
7. Development cf the theory and mthod of interpretation of electro-core samplirg
diagrams. (Abstract) Izv.G3&v.upr.geo1.fon. No. 2 - 1947.
9. Monthly List of Russian Accessions, Library of Congres8, March 1953. Unclassified.

r,,OIQMV, S. G.
KOMAROV, S. G. -- "Core Sampling by Electrical PWans Based on the Resistance
I'lethod.11 Sub 13 Feb 52, Moscow Geological Prospecting Inst (Dissertation
fab theDegree of Doctor in Technical Sciences)
SO: Vechermaya Moskvaj, January-December 1952

K01-103V, S. G.
USSR/Geophysics - Prospecting
Sept/Oat 53
"Review of Symposiun 'Prospecting and Industrial Geophysics,", (A. G. Ivanovq reviewer)
Iz Ak Nauk SSSR, Ser Geofiz., No 5. pp 474-476
Favorably reviews the symposium, edited by V. V. Fedynskiyp entitled "Razvedochnaya I
promyslovaya geofizikall) No 4, Min Petrol Ind USSR, Glavneftgeofizika, Moscow,, 1952s 600
copiest price 1.50 rubies. Contributors were: I. K. Kupalov-Yaropolk, G. V. Bereza.. A. 1.
Slutskovskiy, B. S. Temkina, P. 1. Lukavchenko, 0. A. Shvank., N. A. Pertkov, S. G. Komarov,
I. Ye. Eydmanj L. M. Yesellson, and E. E. Fotiadi.
267T82

KUMCIL SOKMWV, N.N., and CHUMI, V.T.
"Carrying out of Electric Logging in Prescence of Strong Erratic GurreAs"
Prikl, Geofizika, 10, 1953~ 36-47
Ma-usurements of erratic currents were carried out in a well of the in-
dustrial district. The potential difference was taken between the surface
elebtrode and the electride sunken in the well. Ihe difference increases with
the depth and may rearh several volts. The distribution of -the difference
along the well axis probably depends on the specific resistivity of the layers.
(RZhFiz, No 10, 1955)

0 Y1
LITTINOT. S.Ta, j ARKHAROT. L.T. - KOKAROT .~. doktor geologo-mineralo-
gicheskikh nauk, retsenze0; WVINZ, Ye.G., rodaktor; POLOSINA.
A.S., tekhnicheskly redaktor
[Technical geopbjslesl Promplovala geofistka. Moskva, Go** -jauchno-
tekhn. Izd-vo neftl"ol I gorno-toplivnot lit-ry, 1954. 184 p.
(Geophysics) (mmA 7,tlo)
(I%Srole= geolov)

gak*w; RUBINKIN, L.A.: 5OZDWV, V.A.; YADDIMN-
KAMOV. 1W
ro, A.N.; IN, L.T., professor, daktor fiziko-'msteaatIcheBkIkh
nauk, redaktor [deceased]; PSWINA, Te.G., vedishchly ridaktor;
POZQS1U, A.S.. takhnichaskiy redaktor.
[General course In the geophysical methods of prospecting for petrol4rm
and gas deposits] Obobobli kurs gooliziche* Ikh metodor rasvodki neftia-
noth I gasovykh mestoroshdanii. Izd. 2-*, ispr. I dop. Moskva, Goo.
nauchno-ttktu. ix&vo neftianot I gorno-toplivnoi lit-ry, 1954. 457 p.
[Microfilm] (KLU 8:1)
(Petroleum geology) (Prospecting--Geophysical methods)

KOMAROV, S. G. and FEDYNSKIY, V. V.
"Geophysical Investigs;tion of Drill Holes in USSR" paper presented at Fourth World
Petroleum Congress, Rec- '55-
So: D407195
A-50226, 27 June 55

F=NSKIY, V,V,; KOMAMV, S.G.
[Geoph.vsical investigation of drill holes in the U.S.S.R.) Geo
fizicheskie Issledovanlia, skvashin v SSSR; doklady na IV
Mezhdunarodnom neftlanom kongresse v Rime. Moskva, Izd-vo Akademil
nauk SSSR, 1955. 23P. (MLRA 8:10)
(oil well logging)

KCIUMV, $or o GrIellyevich, doktor tekhnichoskikh nank, redaktor;
V%-r~~ilovich; BURSHTEYN, Iosif Hoiseyevich;
TARTSHIV. Boris Petrovich; PITHOVA, Te.A., reduktor; POWSINA.
A.S., takhnichaskly radaktor.
[Automat;c equipment for geop1qsicelexamination of oil wells]
Avtomaticbeeksia a-
Ppratura dlia geofizicheakikh iseledovanii v
akwazhinakh.Pod obshchqy red. S.G.Nomarova. Moskva. Gos.nauchno-
tekbn.izd-vo neftianot t gorno-toplivnoi lit-ry-, 1955- 337 P-
g:.i)
(Petroleum juduitry-Iquipment and sapplies)

0 M A 1\ 0 Vj 15, _6~
USM/Pbysics of the Sax-th - Geophysical Prosyecting., 0-5
Abet Journals Referat Zhur - Fizlka, No 12, 1956) 36494
Author: Kom ov, 3* G., Korshikov, V. N.
Institution: No~!B
Title: Conditions and &perience in Carrying Electrcmi` estigations
In Wells Drilled with Water,, In Regions of Bashi'* iya~'&nd Tatary
Original
Periodical: FAzved. I pramyal. geoflziks, 1955, No 14, W-51
Ahstractt When dri.11ing with water, large caverns are formed against the clays,
which makes it possible to move the geophysical Instruments. To
facilitate the love" and lifting of the instruments in the wellp
centering and sphericar bobs Were J*Ud. The latter til-ed ot&. to
be more effective. The great mineralization of the f lubUg water
reduces the differentiation of the resistance curves of the spon-
taneous polarization and of the neutron-gamm logging, and makes
it difficult to interpret them. The limiting thi*M-ess of the
strata, which can be separated on the diagram of the resistances
Card 1.12
USSR/PhYBICS Of the_Ear,~,h Geophysle
Abst TOUZmal: 'Referat Zhur - Flz:tka al Prospecting, 0_5
Abstract: and for which it , No 12, 1.956, 3649~
iDcreasee-frcm Is POssible to determine the I ec :c r istj ty
It -18 establisheo-1 to 0"5 m in fresh solut, -P if E as V1
pen' d- that when drilling v 'Lon" to 0-75 to 1-5 2.
etraticn into the strata is no Ith water the increase Of
investigations in the t 'very grtmt. The ge
OPbys:Lca.1
-acing the Water withWells is carried out
filled witll water. a clay solution. Pf"'Pa-14 after re-
among geoplW91cal- 't 18 reccmnended to When working with wells
and measuring Investigat-ims include mdioaCtive logging
with a -cavern et,(after lowering the core drill)
entire range of Ineasur r" and resistivity meter
measurement with a ement. When calrylng out BRZ over the
resistivity meter 18 made befO Z si c 7. the
Pletiom Of 161he operation Tj,. re jMd' '
carried acc()rd:img - 'ae Be t after ccm-
it to the GK gjc7PcT ion of the clay strata is
cavern ploti. of s~c curve and according to the
Card 2/2

PAVKOV. N-A-; KORSHIKOV. V.N.; KOWOV. S.G.. redaktor; TSATSIPAR. Te.B.,
vedushchly redaktor; teldmicheekLy redaktor
r
LInterpretation or radloaotive oil well coring diagrams,- provisional
instructionid Interprotataiia diagrams radioaktivnogo karottasha
skvazhin; vremennoe nastavlenie. Moskva. Goo. nauchno-takhn. Izd-vo
neftianoi t gorno-topllvnol llt-r:~, 1956. 56 P. (MM 9:8)
(Oil well logging. Phaiation)

15-57-8-11539
Translation from; Referativnyy zhurnall Geologiya, 1957, Nr 8,
p 208 (USSR)
AUTHOR: Komarov, 3, G,
TITLE- Determination of Rock Poros~ty According to Specific
Resistance (Opredeleniye poristosti porod po udellnomu.
soprotivleniyu)
PERIODICAL: Prikl. geofizika, 1956, Nr 14, pp 129-155
ABSTRACT: The starting point In determining the porosity of
rock according to its specific electrical resistance
(SER) is usually the value of the relative resistance
R, whLch represents the relation between the SER of the
rock and that of the water saturating it. Value R is
determined by the microsonde lateral electrical logging
and investigations of the strata into which the filtrate
of the clay suspension penetrates. In tl~.e latter case,
it is necessary to know not only the SER of the for-
mational water but that of the filtrate of the clay
Card 1/3 suspension. In determining the 3ER of the liquid
15-57-8-11539
Determination of Rock Porosity (Cont.)
saturating the zone-of penetration, it is necessary to introduco
corrections for the effect of the residual water or petroleum. The
correction factor for the eff ect of the residual water varies from
1.1 to 0.11, with a variation in the relation of SER of the filtrate
of clay suspension to that of the formational water ranging fram 0.1
to 100. The correction factor for the effect of-the residual
petroleum saturation varies from 1.2 to 4, depending on the proper-
ties of the trap and of the petroleum. Its most probable value is
1.6. To determine f from the v&lue R, curvas expressing the relation
R = 1/fm are used; Here m is the coefficient depending on the -
lithologic composition oTr the rock. The author presents such curves,
obtained by various investigators for elastic and carbonate rock in
various petroleum-bearing areas of the USSR and the USA. He notes
that the R',bf rock always decreases at the expe nse of the effect of
surfacFi conductivity where the SER of the waters filling the pores
is low (for nonargillaceous rock it exceeds 6 ohms; for argillaceous
rock it exceeds 4 ohms). Analysis of the errors in determining the
basic data shows that the total error,in determining f Is inversely
proportional to the value of f, and that for large values of f it
Card 2/3 -

V)
BASWKIN, Ivan Ivanayich;.LQRAQJ,.,S.3oq red.; DOBVNINA. N.P., vedushchty
red.; MUKHINA, B.A.. tekhn.red.
CStudy1nj wells by micrologging] Insladovanie okvazhin mikrosouftut.
Moskva, os.rAuchno-tekhnAzd-vo neft. i goruo-toplivnoi lit-ry,
1957- 47 Pe (MIRA 11:2)
(Prospecting-Geophys Ica 1 methods)

ZILITSKAN, Pinkhas Avrumovich; KOKAROV, S.1G. redaktor; DOBRYNINA, N.P.,
vedushchly- redak-tor; FOMINA, A.S6..-tekhnicheskly redaktor.
[Instruments for determining deflection of wells] Pribory dlia
opredeleniia iskrivleniia skyashin. Moskva, Goe.nauchno-tekhn.
izd-vo neft. i gorno-toplivnoi lit-ry, 1957. 85 p. (MIRA 10:11)
(Petroleum engineering--Nquipment and supplies)

EQUA104jerreg Gr!jor'&:vIehi ZAPCROZHKS, Y.N., kandidat takhalcheakikh
nauko ret"HINKII; vzvAwz&n, S.?., Inzhener, retsenzent; FGNZRAfiTS,
L.I.# Inzhesier, retsensent; PMBIXA. YeA., vedushchly rodalrtor;
FOLOSIA, A.$.. takhnicheekiy redaktor
(Technola of industrial geophysics] Takhatkik promyslovoi goofivikis'
Ixd, 2-ce, perere Moskva. Goo. nauchno-takhn. izd-vo neftianol I
gorno-topUvnoi lit-ry. 1957. 562 P. ("M 10'.1)
(Gsopbysics) (ProspectiW-ftophysical methods)

-and ZAPOROZHETS, V. M.
"Principal Objectives of the Radioactive Survey Method," Utilization of
Radioactive Isotopes & Emanations in the Petroleum Industry (Symposium),
Petroleum Industry USSR, 1957.
Results of the Joint Session of the Tbchnical Council of Min. of the Petroleum
Industry USSR and Soviet Sci. and Technical Association, Moscow 14-19 mar 1956.

1 1 SN, I
0 Al ~-K (1 -.0,
BOGDANOV, A.I.; XOMAROV, S.G.; FEDY14SK11Y, V.V.
Geophysical methods of prospecting for oil and gAs in the U.S.S.R.
Geol.nefti 1 no.11:13-30 N 157. (MIRA 10:9)
. (Proaneating-Geophysical methods)

KOZIUIROV, S. G.
With Keyvsar, Z. 1. "Permeability of oil Bearirg Strata Determined by
Specific Resi3tivitiea."
17Y In book 61affied Gooft1les; Collection of Articles,, no. Orp mw*ov
(;OUtOVWAA--ftt.- 195Up 2b7P-
"Phliso articles sre 00ncorwd vith the methodoloa of intmWeting the results of
-Asv1=tr:1OP selmdc Ond eUctrical vumeys,. Reviev the col ting pr rtles of
L lee cps
rocks on the. basis ef data obtained frcm resletowters and the appUention of ebarged
partlele necelemtors to vell logeng.

K%IAROV, S. G.
"Uze of Induced Potentials in Evaluating the Storing Properties of Strata"
P"kl"'Y' 9LOf"ika; 90'~Im~ 6UteYj, vYP. 21 (Applied rcopIxygics; CoUect:Lon, of
Articlea,, M~ 21) Mosem, Gostoptekbizdat, 1958- 22113.

ZOVAROT, S.G.; FMIKOT. M.A.
letter symbol@ used In applied geopbystc,s. Prikl. fizo
no,21:211-222 '58a .. Fa 12:1)
(Prospectine-Geophysical methods--Notailln)
I
k-.

14(5) SOV/19-59-5-155/~508
AUTHORS: Datskevichl, A.A., YeseVsonl L.M., Komarov, S.G.,
Pomerants', L.I., Shchukin, S.17 I - -----
TITLE: A Device for Geophysical Measurements in Bores
PERIODICAL: Byulleten' izobreteniy, 1959, Nr 5, P 36 (USSR)
ABSTRACT: Class 21
~, 30q1 Nr 95439 (433120/M-689 of 14 Aug 1950).
,
Dependen on luthor's Certificate Nr 81496. Submitted to
Gostekhnika USSR. The device works off a source of
d/c current and includes a pulsator and galvanometers
for recording KS - the resistance curve, and PS - the
spontaneous polarization. To make it possible to
regulate the KS and PS channels separately and indep-
endently, these channels are switched-in in parallel
and separated by filters according to Author's Certifi-
.cate Nr 81496. (2) Capacitors are used for shunting the
alvanometers to even out the current pulses in them.

To reduce the effect of interference - currents of
M
Card 1/2

SOV/19-59-5-155/308 1
A Device for Geophysical Measurements in Bores
commercial frequency and the effect of the current cir-
cuit on the measuring circuit. a pulsator with a syn-
chronous electricmotor and a reducer is used to enable
transition to be made from one fixed rotary speed to
another, lesser speed.
Card 2/2
A

14( 5) SOV/19-59-3-120/306
AUTHORS: Yaryshev, B.P. and Komarov, S.G.
TITLE: A Device for Simultaneously Measuring Several Pa-
rameters During Core-Sampling Operations Carried-
Out With a Single-Core Electric Cable
PERIODICAL: Byulleten' ._-zobre,teniy, 1959, Nr 3v P 133 ~(USSR)
ABSTRACT: Class 21g, 30 Nr 101497 (450669/MNP-1508 of
I
). Dependent on Author's Certifi-
8 December 19R
cate Nr 81492. Submitted to the Ministry of the
Petroleum Industry, USSR. This device is
equipped with a current distributor mounted in
the drifting instrument and controlling the cir-
,cuits of the current and measuring electrodes,
according to Author's Certificate Nr 81492. The
innovation is intended to separate the current
feeding the current-electrodes from the signals
taken from the MN measuring electordes. For
this purpose d/c. current is conducted from the
Card 1/2 surface to the drifting instrument. This

SOV/19-59-3"120/306
A Device for Simultaneously Measuring Several Parameters During,
Core-Sampling Operations Carried-Oiat With a Single-Core Electric
Cable
d/c current feeds an electric motor coupled with
the distributor and with a mechanical converter
for converting the d/c-current into a/c current.
The a/c current so obtained feeds the AB current-
electrodes. The a/c current, taken off the MN
measuring electrodes and amplitude modulated, is
transmitted to the surface for recording.
Card 2/2

SOV/19-58-11-223/549
AUTHORS: Polyakov, Ye.A., and Komarov, S.G..
TITLE: A Well Resistivimeter (Skvazhinnyy razistiiimetr)
PERIODICALt Byulleten' izobreteniy, 1958, Nr 11, P 52 (USSR)
ABSTRACT: Class 21g, 3091. Br 115891 (573062 of 13 May 1957)
1) A aell realstivimeter consisting of one current elec-
trode and two measuring eloctrodes. It is of a design
reducing the influence of the ambient medium on the results
of measurements; with one of the measuring electrodes
encompassing the other measuring electrode and the current
electrode and provided with apertures for inlet of liquid
into the instrument. 2) A design variation with one of
the measuring electrodes in the form of a balf-sphere with
perforations, encompassing two concentrical electrodes'-
the inner one being the second measuring eledtrode, and the
outer one the current electrode. 3) A design variation
Card,1/2 with one measuring electrode in the form of a spiral laid

SOV/19-58-11-223/549
( A Well Resistivimeter
into grooves on the cylindrical current electrode, and the
casing encompassing both and provided with lengthwise slots
forming the second measuring electrode.
Card 2/2

V . I.G.
_LIWVSIR, Z.I.; KOZINA, Z.K.; SKOBLIKOVA, G.I.; GUZANO A
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(2140tric prospecting)

FEDYNSKI:j V.V., doktor fiziko-matem. nauk., red.; SHIROKOV, A.S., red.; KO-
VALEVA, A.A... red.; GRATSIA11OVA, O.P.y naucbn. red.; BORISOV) A.A.
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red.; KUDYMOV, B.Ya., nauchn. red.; PETROV, L.V., muchrk.red*;,KOHA-
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FMNSKII., V.V., red.j. DAKENOV, V.N.9 ied.j VASILIYEV, V.G., red.~ MENOV.,
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(Oil well logging)

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hn
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(Calipers) (oil wells--Measurement)

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the reservoir propertiea of layers
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from the results
no-30195-213
(MRA 160)

JA ?. PETROSYAN, L.G.j PERIKOV, N.A.; FELIDMAN, I.I.;
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- KOMAROV, S.G.; KOTOV, P.T.
- -,
Determining the permeability of beda , form, induced potentleds,
Prikl. geofiz. no./,OzI63-17.1 164 - (m-IRA l8a)