SCIENTIFIC ABSTRACT VORONCA, A. - VORONEL, A.V.

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• Collection: Scientific Abstracts
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• Sequence Number: 5
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

'0/6"01 1/(,)11/()PI/001
A~031JAJ~6,
AUTHOR: Voronea, A., Erigineer
TITLE: The application'stage of geophysical methods in!drilling holes for
C I f c6al de4
the exploration and determination of the r serveso posits
in the USSR
PERIODICAL: Revista, Minelor, v. 11, no. 11, 1960, 561 5d
TEXT: The USSR widely uses the geophysical sampling.for'thelexplo:i,ation of-
coal deposits, performing yearly more than 3-1 million geophysicaj. samp',Ungs.~ The
drilled holes are examined by electric and radioactive sampiing uAd many samp les
are extracted by the sidewall sampler for the determinati6nillof tl~e strL'itigraphi-
cal columns and detection' of coal. The used electric samplio
g methods are: ap-
p-af ent resistivity (M), self -potential (PS), gradient Is,elf-potentia-, pro-
of!
ducea ,potential (VP), bridge r6sistance (MC), eleotric~curre~ts (1'X), and sliding
contacts (MSC). Tho radioactive sampling methods are:, natti~al g"a (GC), neu-
tron-gamma (NGC) and gamma-gamma (GGC). The aoil samples ar~ tak4n:wWL the side-
wall sampler, which extracts 20 samples In one operation. T6e volume of a sample
varies between 1 5 cu cm. Geophysical research conducted at a scale of 1 200
Card 1/ 6

10166101 Vol 1/001/001
The application stage of geop~4sical methods ... A231^1~61.
serves for the detection of coal, completion of the a~d
lithological horizonting of the profile. Geophysical resei~~h co~duote;'I at a iscale
of 1 : 50 serves for the determination of thickness and struoture,'of co&I striLta.
Electric sampling methods are used for the study of coal d4~68italia whI.ch the
alectric parameters of the coal are clearly distinguished from thatiof rahe other
rocks, or rocks of similar parameters, but of on-important 4uantity. '.The de ti"-
tion of coal is accomplished by the KS and TX 'tethods, and 'for details the VP and
PS methods are used. An accurate quantit4tive interpretation is iccomplished by
the PS gradient method. Coals of high resistivity, i.e., th~ majority of the
deposits of Donbas, Kuzbas, Pechora Basin, Karaganda, Lvov-Volyn,~Sakbalin IsIwid,
etc., as well as the anthracite coal deposit of the Donets 16sin aria de-;ected by
these methods. The radioactive methods combined with.electric methods' utre used
for the detection of mineral coal and lignite deposits with 'a high eleal-.ric resis-
tivity, and lignite deposlts~ vdth a high content of ash. Tfte used radioactive
mathods are GC, NGC and GGC, The latter method was introduced b5r!the-U,3SR in 1955,
s-4piying at present the best results in the detectiort'of the co~is in lr:Lllir4;
holes.' For-details, the'radiciactive methods are cowpleted~by KS and PS'electrdc
measuring, rOely by TK and gradient.PS methods. The~coal~dieposits.of Xizelo and
Chelyabinsk, as well as some deoosits'of the Moscow basin Aria exam'ined Oy radio-
Card 2/ 6

10/60/011/011/001 /001
The application stage of geophysical methods..,. A231/A126:
active methods whereas the coal deposits of the Western Urals; some sections of
the Donets and Moscow basins and of the Tomi-Usink Region iniftzbds~are detectod
by the combiadd.method. The use of a complex geophysical pr~oess,'expan,'ed by
L
the sidewall sampling method, guarantees the identirication,of the coal.strata,
determination of their thickness, structure and depth. Corrolati6n profiles don-
structed on the bases of geophysical diagrams also permit,in many!casecithe de-
termination of tectonic disturbances, their character and tk~ syn&4ymi,,~Jlltion of
the coal strata. The comparing studies proved that the geophysictil sw!ipling for
tiae determination of thickness, structure and,location depth is more atf urat th
lc e an
the-mechanic sampling, In coal basins where the use of geophysical me~ljhods is
more advanced, the qualitative determination of the coals by geophysiif:al methods
is at least as accurate as the determination by mining work'; Inthe U!M, the
evaluation of the thickness of the coal strata Is astimated!with an av;~rage error
of minus 18% to the real thickness. In some deposits thesellsubestimatLons varge
up to 55% (Pechora Basin). In some coal basins (Pechora, S~utheL~n Yakutia and
Kusnetsk), the coal re.9;erves are calculated only on the basis of ~results supplied
by the geophysical sampling. Based on the practical Importance ~f lthe-geophtrsical
sampling, the State Commission of Reserves of the USSR has ~,erjtabltzhedl.c "Utiliza-
tion Conditions of geophysical sampling data for the calculation: oE coal reserres"
Card 3/ 6

R~Oio/66/pii/Dii/ooi/boi
The application stage of geophysical methods 31/A126'
A2
The State Commission determines that in case the geophysicallsampling fulfills
the respective conditions, it should be consid6recl'as a basic method for the de-
termination of the necessary indexes for the calculation of:,the co'iLl re3erves.
With regard to the importance and accuracy,the inveatigation"of coal deposits by
geophysical methods in the USSR presents three categories; De~oaits where
the use of geophysical methods is more advanced, obtaining by t hem: E) detection
of thickness, structure and location depth of ooal strata; ~nd b)'
qualitative pa-
rameters of the coals. 2 - Deposits where the use of geophjaicall methods supplies
with accuracy: a) detection of the thickness structVre andilodaiion depth of coal
deposits; and b) quality parameters; they are obtained by analyz.ivig the samples
taken with the sidewall sampler; 3 - Deposits where the Us :6 of geophivaical nothods
Is not sufficiently developed and no accurate data on the,deteotion oJ.' thickness,
structure and depth of strata can be given. But also in:this situat:Lon, evezy
drilling hole is geophysically sampled. The,results obtained accor4tag to point
1 and 2, serve for the calculation of the coal rederves. da thvbasls of the re-
sults obtained, a method for the application:of datasupplied by,geophysical sampl-
Ing f9r the calculation of coal reserves has been worked out. In Bep.tember 1958,
Mi S. Speranskiy forwarded to the Coal and Bitumenous Slate.Section r,f the Commls-
sion of Geological Experts at the State Commission of Reserves, his report: "Pos-
Card 4/6

B/010/66/01 1/011/ool/001
The application stage of geophysical methods ... A~31/AI26
sibilities and Conditions for the Use of Ge6physical Samplink Dat~ in~t-he Cal6ula-
tion of Explored Coal Reserves". On the basis of this report, the State Commis-
sion of Reserves worked out and approved on November 15, 1956: "Application Con-
ditions of Geophysical Sampling Data in the Calculation of~d6al Reserves". The
standards include the use of geophysical sampling procedures~and the qualities
which have to be fulfilled, as follows: The geophysical sa~pling:ia a basic
method for the determination of some of the quantitative parameters of the coal
in beds where the geophysical method proved to be: equal, or~ superior totthe
mechanical sampling. In certain conditions it permits the:identitication of the
presence of coal strata and the determination of the thickness, structure and
location depth. The application degree of the data is determined;by the parti-
cularities of the physical properties of the coals and rocksi,in iheir-beddingn
and roofings; by the indices characterizing the thickness, structure and
qualities of the coal; and by the accuracy of the results obtain6 ,d by geophysical
sampling. The degree of accuracy is determined by ,,omparati~e studies between
the results of the geophysical and mechanical samplIngs and ~f the mining works.
The obligatory conrlitions for the use of data,obtained by gel6physical nvasurLngs
on thickness, structure and "batImetry" of the srata are des,~ribed. The advanta-
ges'of the geophysical sampling.against the mechanical sampling are., reduction
of the costs by 30 - 50% per linoar meter; d6ubling of the drilling speed; high
card 5/ 6

8/010/66/011/011/001/001
The application stage of geophysical methods A2jI/W6:
geological results and complete stratigraphioicolumns;: 6imole!'emtminati6ji
MO
of the geophysical graphs. Oh the basis of the Soviet results, the aw;hor rerom-
mends the intensification of the applicati,)n of geophysical mothodLs in Rumania:
Exchange of experience with,the USSR and o1her socialist coUntrie$ sh,~i.ild be,
carried out. There are 2 tables and 6 Sovtet-bloc refereiicipts.
card 616

VORONCA, A.
Application of geophysical measurements in1wells for co~-
purposeso p. 63o
REVISTA MINEWR, (Ministorul Minelor, Ministerul Industoei ?113t:~olului si
Chimioix Directia Exploaturilor Minim ai Amciatis Stiiipittfl~m a
Inginerilor ei Tahnicienilor din Homina) gumirostif fkiot6jat iVJ14 loy
no. 2,, Feb* 1959.
Monthly List of East European Accessions (LTAI) IG, V01,118~ n6-7, July 19159
Uncl&

V011011CA, A.
Results obtained in the WT10ration of coal, deposity l~ by means of boring with the
application of geophysical methods. p. 4Qj4
REVISTA MINELOR. (Ministerul. MInelorg:Mini.asterial ln~wtaIJ4 Petrolulul si
Chirdei, Directia. Exploatarilor Miniere si Asociatia,!:StUn;Ufica a Inginerilor
si Tehnicierdlor din Rorrdnia) &acuresti, Rtwmnia. Vol. 10. no. 10, Oct. 1959
Monthly list of East European Accessions (EEU)~ LC Vol. 9,,! no. 2, Feb.' 196o
Uncl,

-VORONCAP -A4-J--CONSTNNTINESCUP-Mo-
Character of the slide prism under conditions of the sp&ce problim, Wbo'n
narrow faces are subjected to earth pressure. p. 205
REV=A CONSTRUCTULOR SI A NATERLUMIt DE CONSTRUCTIL (AsocUtia Stintifica
a Inginerilor si Tehnicienilor din Rominia ei. Ministerul ConstrWitilloir si
al Materialelor do Constructil) Dxurestis Rumania.' Vol, 10.9 No$. 4, 4ril 1958
'Monthly List of Fast European Accessions (EFAI) Le. Vol. 9., No., 20 Feb. 196o
Uncl.

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14,
ORMEMO-i A.N.-.--1nzhene_r.
Installing fireproof partitions in oable,tu=qj.*~
~of operating
electric power plants. Zlek.sta. 25 no.8:50-51 7:9)
lectria power plants--Fires and fire prevenii0n);

BRODSKIY, V.B.; BEIITSKIY, B.M.; Tq~~NGMV. A.T.; KONYAKRIN, H.V.;
STAROSTIN, YU.N.
Radio sounding of a plasma moving inversely to the electrodynamie
acceleration in a coaxial.accelerator. Zhur takh. fiz. 33
no.4t426-428 Ap 163. (KIRA 160)
(Oscillography) (Plasma (Ionized Cases))

VUIONCHEV, Tildion Aleksandravichl IVAbUSUO, NoD., red,;'~ SnS".jKOj% A.A.0
CIVulse thyratrocol Impullonye tiratromy. Moskva, Uv-ro
"Sovetskoe radio,!' 1958. 163 p&- (MIRA 11:4)
OIIHI IJ[ III I" I'll"] lll`F"!11 1

PMUH I BOCK wwiwioir. 593
Voronchavp Tild= tacksaitdrovich
Mqp-xlIsnM tiratroay (Pulse nWmtrons)'. Kancow.# U4,-V~o "S6ywtskoye radio".
1958. 163 p. Nmiber of coldeo printed wt given.
FA. Ivanushko hnikor
N. D.; Tech. Ed.: Sven j Ae A*
FJMSE: TIds monograph Is addressed to those e& In the design of vari-
Otto installations in vldch julse tbyratrons me Used' Vell as to
designers engaged In the develo;ment of Vxlse
COMME: The monograph is concerned vith the design aad operatIN; speeifi-
cations of pulse thyratrons. 7he book contoAm data [~ ion re;wearch done on
various physical processes and can be divided Into t~xee oiections: 1)
physical processes takLng place in the thymtrcm dur4%g the pr%nanduction
pext of the period; 2) physical processes taking pla6e.durlng the con-
duction part of the period; 3) physical pmesseB tddng pleee dudng the
Postconduction period. Some special problems aaooci~ted with tkAyratron,
operation are discussed as well 3s pulse-thyratron mi=facbving tech~e.
Tae Mrasent vork also deals vith the results of resesith Cli the I*qsical
Card If5

Base Thyratrons
!;93
prooesses takJn place in thymtronsjo obtained in, davd.O;Men~ of the 1950
model Mll-130/10 high-frequency pulse tkyratron. Md~ thMttron las a. new
firing system which ensures high firing stabilityp short chsa-ge-baildap time,
and operates at a pase repetition rate of up to 30.,000 aps,~ The following
Soviet-produced equipment is discussed: the W11-3573,,' W11-50/5 end
Mll-130/10 thyratrons and the MII-3/1 Pulse tbyratrou~ eal of then developed
by the author; the type 25-1 single beam oscilloscope; the MI-2 thyratron.,
mentioned as the first pulse thyratron. to be dimlopecl iu. that Soviet Ubion;
thyratrou
the TG32-260/12 ; the Ml-0.3/12 tbymtron (MUed with lan7ton);
and the MZ-0.1/1.3 thymtron. Scue of these thMtroas are iv=erated in a
table with additional variants of the Mn type. The author expresses thanks
to Ptoffessor I. L. Kaganar for the supervision of the vo*j to Ya, B, Itsothi.,
Doctor of Technical Sciences for valuable suggestions in reviewing the
script, and to Rnaln ers M. V. Dmitriyeva and-L. 1. Fre3fterg~for their help.
!Mere are 23 Saviet references (including.1 translation)., 1 German., and 12
RnOl sb.
Card 2/ 5

Ch. I. General Introduction to Palse Tbyratrms
1.1. Des4m and some characteristics of page thymt, 7
1-2- Operating principle and operating characteristics of:
phase thyratrons 10
1.3. Technical requirements orf pilse thyratrms and some
of their parameters
19
Ch. II. Physical Phenomena In Aaoe Tbyratrons In the Pre-
conduction Part of the Period
2.1, Beale concepts of the theory of dischazge in
bot-cathode ionic instruments 24
2.2. Experimental research on disabarge bmUdup in pttlne
thymtrms
32
Card

Palse Thyratrons 593
A. Process of dioebarge bWl&p 33
B. Firing stability 58
C* Increasing Tiring stability 62
Ch. MEI. Pbysical Phencomms In False Tbymtrms in the~~iCmdaaltion
Part of the Period
3,1, Palse voltage dxW and volt-=pere characterlibic 64
3.2. OxMe-eathode slvxklng 84
3*3e Voltage drop in electric discharge narrowings !ad 6=' PI) 92
Ch. IV. Fbysical Plumomma in Rase Thyntrcm in the PojOt_
disebarge Part of the Period,
4.1. Wonization ;rocess and parameters denoting the fM-
que=y cb&Twteristics; of pulse tbymt;rcm 98
4.2. ConcUtions g1ving rise to seconditry, firinp a" the
of gad cirmdt parembers on frequency chamateristios of
pulse thyratrons.,
3.04
Card 4/5

GRWBMHCHIKOV, D. -, VOIDN' 10IMN A&, gvardti.P~Ilcov~dk, redaktcr;
GMHIKIID, G.V':!mr 0 or.;~Z, XDVA, T.F., tisk~n.lchetskiy- redaktor.
[Gunniryg, and rasoureefuluess In warfarel Toenuals'! khItp'ont' I
smetka. 3-s lad-dinAva. Voon.ted-vo Ministerst i5~ ol orbiXr SE
)SR
YL
1955. 66 p. [Microfilm] OLLRL 8110)
(Tactics)
111111 14

KlJRBnu'YF,V, G.U.; KONOVATA
The performance of flotation machines. Vvivet. Mt. 39 no, 12-r
23-24 D 165 (VTRT. 19 T'L)

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-WN
Kt]fZB"-'TIYEVP G.1'4.; KONOVALOV, M.I.; VOjOhlQjjKjjj,j G.A.; BIWA, S.L.
Industrial testing of sodium cyanide as a aubLrj'..!tut'e'fwrjr blalk
cyanide. T.Svet. met. 38 no.9:25-26 S 165.
(M I RA 13:12)
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AUTHOR: Vorenchikhin, 16. D.; dsk!j, E. A. Fak, i d t~!d
'ORG:- Institute of Physics of Metal S-. AN SSU (Idstl t1ult A~ilii
TITLE Superpaiamiagnetismin _c~,steeka~i v
SOURCE: Fizika metallo7 i metallovedenlye, v. 20, no U,
_TOPM,~AGS: austenitic steel, paramagnet.ism, magnetization~
netic-momenti-metal physical.property, 'Metal ph4sics
'q q, L;
21,
'ABSTRACT: -S!;Me aramaVwti~m wms studied i ild, .50K
n 40Kh2N2O..a
-steels in.-order to determine the average mag
neRc mcments, and
al ferromagnetic ordering regions,.(clusta~rs netiziki6n!
for,constant magnetic~fields and~sitrong4 changing cread', saln
mm (diameter) and 10 M (length) '.The data, shoiiod. illat ~the p
.-of the magnetization , curlms 0 colvespondl6g. to the ~aluei~ of t
~;tensitic trans formatictign t~csa a-teela can be 4eac:ribca by
UD6 9
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ACC NRt -AF6023111 Wultut; (;Uij!s.. UICIVb-.0100tue..Lluvjfv,#)Ofv"j.
AIMIORs, Voronchikhin,,_ FaIddov, I. G.- 7
0RG1 Instituta of Pbysics of Metals, MI SSSR (Institut fidk~/Mtallov, Wit)
it Determining the latent heat of martennito conversi6n1inducod in steel by a
magnetic, field
SOURCE:*-Fiz1ka motanov i meta11ovoden1,w,'-v. 21, no. 3,j966, 436JA1
'TOPIC TAGSv magnetic effecti martensitic transformation, cionstaht =gnotio field,.
-alcal stool, high teq)ilZ rature phopownon
pulsed magnetic fie3d, calorimetry, ni 3
MSTUCT. The *authors study the thermal Phenomena vhich~'accompany marten-
site-conversion induced by a magnetic field in stools. "Alie stwly coarirmo
Ahe &evioualy known fact of stepwise forioation of isolated nuirtensi Le
6dievand indicates that a sitailar mechanism of martansite conversiun
taken pi ace Fegardless of the physical causes underlying'the r-4 ,.onver-
'ail n. ~
D Atm h d is proposed for determining the latent heat of, rtonsito
conversiAu: to the effect of the magnetic field in 40Kh2W20 ad
'581CHNSSM steels. The chemical composition of these std'ela is given in
-,,the table below. . It is, shown that both pulsed and const4113t M0.0110tiIC
may' Iftitiato thix convorsion. The -advantages a, t110 PI-6poised
'method for determining the latent heat of austenite-to-martensite can-
.,Version in a magnetic field are discussed in comparison with the calori-
metric method,

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Voronchikhin, S. L ft Oa regastrovaterostomytil Ti-udy Mdiustituta
(IzSe- goso meds in-t(s Vol. M, 1949, p. 294-90;
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SO: U-38500 16 June 53, (Letopis, fZb=nal Imth haten No- 5,o M9)'

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XOIUYINKO, D.G.0 to)an'tchaft-7y radaktor
[The-~61gA flotilla In the areat Patriotic War) warbskaia voennaia
flotillia v Velikoi Otechestvonnoi voine. Moskva 0Yoe*.~Izil-vo
Hinisterstva vooruzhannykh oil SSSR, 1947. 39 Poll [Xi6roftlm]
L ~(MMA 9:10
1. Russia (1923- U.S.S.R.) Armiya. Upravlonive Mor:skikh 311.
Fo21tichookoye upravleniye.
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