SCIENTIFIC ABSTRACT DYAKINA, M.E. - DYAKONOV, F.V.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000411720001-5
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 22, 2000
• Sequence Number: 1
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

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Using KUM11's xothod A configurations are o=ml
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trigonal Priam having atoas above the controo of risht-englod tam,
symmetry DSh- 1194UC%200 tables show twu 7 and 9#0-bonds reap. can arlse
a in hyt,idizatlou& of a-, p-, d-, and In aU but on* case, f-oleatrona.
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ACC NR, AP6017302 QN-) F'OUPE
Ye.
AUTHORS: Volkenshteynp H. V.; Dyakina, V. P.; Novoselov, V. P~.; Start3ev, V.
0111G: Institute of Metal Physics, AN SSSR (Institut fiziki metallov AN SSSR)
TITLE: Peculiarities of the temperature dependence of electvic resiztivity of
dysprooium at low temperatures
SOURCE: Filka metallov i metallovedeniye, v. 21, no. 5, 1966, 674-677
TOPIC TAGS: dysprosium, electric resistivity, resistivity
CT 2jEif ieA
ABSTRA' : The electric resistivity of highly _ ysprosium (R 300KIRA,2X Z 105)
was measured over the temperature interval 1-5--300K to determine the magnetic
contribution to the electric resistivity as a function of temperature. The resistiv-
ity was measured on 10 x I x 0.5 mm strips made of distilled dysprosium using a
cryostat (R. V. Colvin and S. Arajs. Phys. stat. sol., 1964, 4, 73). The results ar(
shoA,m in Fig. 1. These results were found to agree well with the theoretical predic-
tions proposed by A. K. Mackintosh (Phys. Lett., 1963, 4, 140). This is demonstrated
in Fig. 2 which shows a comparison.
UDC: 539.292:537

L 40301-66
ACC NRt AP6017302
.Rr
V,61
!,2z

2

0 za
JOIS 1
0 ja /Go .150 zoo 2J0 W
Fig. 1. Electri6 resistivity'of Fig. 2. Low temperature electric resisiivity:
d~spr osium: 1 - total.resistiv- 0 experimental results; solid line - curve
ity; 2 - magnetic resistivity.
-
-
.
;T
m=aVe
P
, Yrith a/ROC 1.27 x 1074 degrees-2

A/k-- 30K;
dotted line
curve of T2 fur--.tion
having common point with experimental results at
T = 24K.
Orig. ext. has: 2 formulas and 3 figures.
Card 2/2/~?j-/" So CODE: 1,1Z SUBM DATE: 1OAug65j ORIG REF: 005/ OTH REF: 004
/0
3

NIKOLAYEV, R.I., AIMYUKHINA, T.D.; VXSELYY, V.A.;,_DYAKIVSKIY, S.I.
Line suspension insulators made of glass. Blektrichestvo no.2:
41-46 F 16o. (MIRA 13:5)
1. Llvovski politekhnicheskiy institut.
(Ely
ectric insulators and insulation)

NIKOLAyEV, N.A., kand.tekhn.nauk; JkRYUKHINA) T.D., kand.tekhn.nauk;
VZSELYY, V.A., inzh.; DYAKIVSKIY, S.I.
Hard-glass suspension insulators for areas
conducting percipitation. Elektrichestvo
1. L'vovskiy politekbpicheakiy institut.
We'etric insulAtors and insulation)
with electrically
no.lo:68 o 16o.
(MIRA 14:9)

ANDRYUKHIRA, T.D., DTAXIVSXIT, S.I.. NIKOLAYEV. N.A.
Tempering glass insulators. Stek. I ker. 17 no.6:25-28 Je 6o.
(KMA13:6)
(Electric insulators and iasulations--Testing)

NIKOLAYKV, N.A., kand.tekhn.nauk; ANDRYUKHINAJ, T.D., kand.tekhn.nauk;
VESELYYY V.A., Inzh.- DYAK I P S.I.
Features of tempered glass suspension insulators for electric
power transmiosion lines. Elek. sta. 31 no.U :64-70 D 160.
(MUIA 14: 5)
(Electric insulators and insulation)
(Eleotric lines-Overhead)

34159
s/196/62/000/0O2/Oo6/o2.3
014 E194/E155
AUTHORS: Nikolayev, N.A., Andryukhina, T.D., Veselyy, V_A.,
and Dyakivskiyj S.I.
TITLE: The manufacture of overhead-line suspension
insulators of hardened glass
PERIODICAL: Referativnyy zhurnal, Elektrotekhnika i energetika,
no,2, 1962, 6-7. abstract 2B 35. (Vestn.
elektroprom-sti, no.9, 1961, 54-56).
TEXT: The composition of glass used for insulators is given.
The glass is melted in a regenerative furnace burning natural gas,
with a flame shaped like a horseshoe. The amount of glass is
about 200 kg per m2 of furnace area, so that it was possible to
maintain a comparatively low temperature of 1410-1420 OC.
Appropriate quantities of hot glass are delivered to cast-iron
moulds for pressing. At this instant the temperature of the glass
is about 1020 OC. When the glass part of the insulator has been
pressed, the inner hollow of the head is of conical shape and is
then shaped by a special device. The time cycle for forming a
glass insulator part, including mould cooling time, is 1,5 min.
Card 1/2 x

34159
The manufacture of overhead-line .... s/196/62/000/002/Oo6/023
E194/EI55
Temperature equallsatlon and heating for hardening is carried out
in a conveyor furnace for 15 minutes with a gas temperature of
680 OC. The hot glass parts are then delivered for hardening to
air-cooled machines with eight spindles. After hardening, the
thermal resistance of hardened parts of insulator nc.-4.5 (PS-4,5)
increases from 35 OC (in the unfired condition) to 200 OC, and the
mechanical strength increases from 3.0-4.0 UP to 10 tons, It is
denied that slight damage to the surface layer of the hardened
glass leads to complete failure of the part. After hardening, the
glass parts are submitted to thermal shock tests with positive and
negative temperatures. insulator strings consisting of
18-22 units are subjected to a one-minute tensile load of 3-6 toils
(types PS-4.5 ; nCY-4.5 (PSU-4-5), ncr-4.5 (PSG--4-5).
5.5 tons for type n c-8-5 (PS-8.5)s and 7 tons for type ric-1-1
(PS-11), The insulators are then exposed for 3 minutes to a
continuous flow of sparks which do not form an arc. The
insulator fittings are 40-50% lighter than those for porcelain
insulators. 2 illustrations, 5 literature references.
Card 2/2 fAbstractor,s note: Complete translation.l.

NIKOLAYEV, N.A., kand.tekhn.nauk; ANDRYUKHINA, T.D., kand.tekh.nauk;
VESELYY, V.A., inzh.-, DYAKIVSKIY, S.I..,inzh.
Manufacture of hard-glass suspension insulators. Vest. elektroprom.
32 no.9:54-56 S '61. (MIRA 14:8)
(Electric lines--Overhead) (Electric insulators and insulation)

j, Loyn-bb
71: _ACt_NV_AP 6 0 15 4 4 9 N1 SOURCE CODE: UR/0181/66/008/005/134311350 -
AUTHOR: Dykman, I. M.; Tomchuk., P. M.
ORG: Institute of Semiconductors, AN UkrSSR, Kiey (Institut poluprovodnikov AN
UkrSSR); Institute of Physics, AN UkrSSR, Kiev (Institut fi"ziki AN UkrSSR)
TITLE: Function of electron distribution and mobility in polar semiconductors with a
nonparaholic dispersion law
SOURCE: Fizika tverdogo tela, v. 8, no. 5, 1966, 1343-1350
TOPIC TAGS: electron distribution, electron mobility, electron temperature
ABSTRACT: A donor-type polar semiconductor for which a nonparabolic dispersion law
holds is investigated. The interaction is considered between the conducting electrons'
and the polar lattice vibrations, whose energy quanta are constant h,,O~k& It
is assumed that the lattice temperature P0 -'o 0; it is shown that the "electron es-
cape" effect is removed if the effective mass of the electrons grows with energy C.
For fast electrons, c and the impulse p are relatedAy th pproximation c.-.Xp whert:
v < 4/3. With a dispersion law such as is valid foefInSb~Vhe electron temperature
increases monotonically with the function field. The-instability of the solution for
fields F > F* is removed, and thereby breakdown cannot occur. Conductivitv and mobi-
lity differ from those when dispersion follows a parabolic law. Mobility falls as the
Card 1/2

ACC NR: AP6015449
field intensifies because the mean electron mass increases with their temperature.
Curves are plotted for the dependence of the eleacron temperature in InSb and the re-
lative conductivity ou the strength of the applied field. Orig. art. has; 2 figures,.
33 formulas.
SUB CODE: 2010,/ SUBM DATE; 29Jul65/ ORIG REF: 006/ OTH REF: 004
nwm
Card 2/2

i IN ... . ...
ABLOV, A.V.; i.A.;
n-c aril j0 no.3:
of
6~8-635 165.

Q" -air" of day$ -d grog A
MAK"ININ Amn, A. K. DtAzomaxzo. 'i. J~abl..
9 1227-M OW) abdawled In Ckew-tesir.. 1942, '1
1 112004, Xhist. tral, Ziwr., 4 10170 (19IM-Tne fol-
lowing ure has been worked out for a rapid atudytis
of clays grog products for AW. TiOu and N4).
Fuw a with NtOll in a silver crucible. Leschthe
futed mass with water and allow to settle. Filter an ali-
qu--t. acidify the Altrate with MI. add a solution of
hydrozyquinoline In an amount sufficient for the maximum
content of A" and then add a solution of ClIsCOONa.
After some time heat the solution until It becomes cloudy.
make to a definite volume. filter and titrate the ex*vv
hydroxyqu,inofine In an aliquot with a solution of bromW
b"miste. adding this reagent in umne excess. and titrate
back ladometrically. Thus determine AIA. Filter the
remainder Of the master solution through the same filter
whk-h was used (or the solution of Alst)~. lXudvr Ti and
Fe oxides with HC3. Determine Fe suA Tl In aliquots.
As the calorimetric determination of Ti in a HCI solution
:nd in the presence of Fe is not reliable. repredpitate Ti
nd Fe with NIIjOH and disoolve the precipitate on the
filter with lfSO,. Determine TiO, In this solution colori-
metricall 'As Fe does not settle out m. pletely, add the
alkaline Ifirate to the solution obtained by di-Wving the
hydrusicim Determine FcA the Zimmerman-
Reinhardt method. The deviatiott7in the values of results
obtained by this method from thaw obtained by the ciasi-
Cal method is from -0.48 to +0.57% absolute for AIA.
an'l f.- -0.24 to +027% al;sWute for FeO, Ten
analyses can be made within 3.5 hr. An analyst with an
s"istant can make 4.10 to U) an&IYVVrcfnoalh.
.V + N1.110.

red*;
UVAROf,;SJP.g,~Ievvyy red,;-PWOV, A.So, red,; DP
GRCBMAW, S.M., red.; PWROVA, T.G., r;R.; KOLIWIKOV, F.M., red.;
KRUTOUS, V#P,, tekhn.red.
[Papers at a technical conference on design, construction, manu-
facture, and use of reinforcied concrete poles for electric trans-
mission lines and telephone communications, November 27-30, 19561
Materialy neuchno-takhnicheskoy konferentaii po proektriovantiu,
stroitelletvu, proizvodetvu i eke lustataii zholezobstonnvkh opor
lini.v elektroperedsohi i evyazi. EGroznyi] Chechano-Ingushokoa
knizhnae iad-va. 1957. 163 p. (MMA 1116)
1. Nauchno-tokhnicheakeya konferentsiya po proyektirovani,YU.
stroitelletvu. proizvodstvu i ekepluatataii shelezobetonnykh opoir
linii elektroperedschl i avyati. Grom ny ', 1956.
(Reinforced concrete construction) trIlectric llnes-ZJ~oles)

KAGAN. Ta.I., kand.fiz.-mat.nauk; KOVkLENKO, A.D.,inzh.; MUM, V.Z., lnzh.,
ROGDANOV, 0.1., inth..- ZUBARI. V.P., insh.; DOYAKONENEO, V.S., inzh./
Automatic measurement of shaft diametere during grinding. Vest.mash.
38 no.10:58-59 0 158. (MIRA 11:11)
(Thickness measurement)

LYUBGMROV, V, Ye., kand. med. nauk; AGARKOVA, S. V.,- DIYAKONENKO Ye. K.;
MATEYEVA, K. M.; PAVLOVA, 0. A.; SIROTA, G. M.; ~ Eff)Ts-,.:F. -Z. --- ---
Combined forms of pneumoconioses in patients with collagenoses.
Terap. arkh. no.9:95-101 161. (MIRA 15:2)
1. Iz Stalinakogo naucbno-isaledovatellskogo instituta, fiziologii
truda.
(LUNGS~DUST DISEASES) (COLLAGEN DISEASES)

D'YANONOV,A.; MANDRIKOY,V.
Cultural mass vork among students. SOV.-DrofsoiusY 3 no.9:52-54
S '55. (MIRA 8:12)
1. Predsedatell profkoma Urallskogo Politekhnicheakogo instituts.
imeni S.M.Kirova, Sverdlovsk (for Dlyakonov) 2. Zameatitell pred-
sedatelya pravleniya klubs. instituts (for Mandrikov)
(Sverdlovsk-Community tind school)

SIMUD, Fred. N.; KMILL, Anthony; SWWOV Yu.V. [translator]; DYAXO-
NOV.A.I.,Ctranislatorl: LYLTBIMOV,S.A. ttranslator]; VOLODejrjT'2,--sI'
fITOMtor]; RUSANOV.P.L. rodaktor;PAVLOV,V.S., redaktor; am-
RASD(OV,Ye.S.# takhaloheakiy redaktor
[Protection for people, buildings and equipment: from the atomic
bomb. Translated from the Inglish.] Protivoatownsia zashchita
liudei, zdanii i oborudovanita. Perevod. a angliiskogo W.V.Seme-
nova i dr. Moskva, izd-vo inostrannoi lit-ry, 1935. 292 P.
NLRA 9:3)
(Building, Dombproof) (Atcmic bomb--Safety measures)

DIYAKOIIOV, A.; BXIZBURG, Ye.
The papple's university is a source of knowledge. Stroitell
no.2:20-21 F 160. (MIRA 13:5)
1. Starshiy ins-moktor TSentrallnogo komiteta Profooyuza
rabochikh stroitelletva i promyshlennonti stroitellnykh
matorialoy (for D'yakonov).
(Building trades--Study and teaching)

04
VORONOV, F.D., prof.; DIYAKONOV, A.I., kand.tokhn.nauk; DIKSHTEYN, Ye.l., inzh.;
V.
TRIFONOVP V.V., inzh.; KAZAKOVJ, A.I.P inzh.; KOVALIK,
I.S., tekhnik.
Technological characteristics of Magnitogorsk Metallurgical Combine open-
hearth furnace operations using compressed air in the fuel spray. Stall
23 no.12:1088-1091 D 163. (MIRA 17:2)
1. Magnitogorskiy metallurgicheskiy kombinat i Magnitogorskiy gorno-
metallurgichaskiy institut.

VORONOV, F. D.; 41)YAKONOV, A. I.; LORIMIAN, V. V.
Oxidation nf the open-hearth furnace bath by - -e heart~-
atmosphere and Its effe,t on the indices of smelting. Izv.
vyx. ucheb. zav.; chern, met, 7 no.6:0-43 164. (MUU, 17:7)
1. Magnitogorskly gorziometaEurp-loheskly institut..
.1

BORUKAYEV, Ch.B.; DIYAKONOV, A.I.
Tuapse zone of lateral shifts (northwestern Cw easus). Dokl. AN
SSSR 155 no. 3:552-554 Mr 164. (MIRA 17:5)
i
1. Predstavleno akademikom V.I.Sm,irnovvm.

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LYPSONOV, A..:.
'r- 1-----.- --.1
"Investigation of Gas Movenent in Liquids on the Hydraulic 1-llodels,"
lecture given at the Fourth Conference on Steelmking, A,A. Baikov Institute of
I-Letallurgy, Moscow, July 1-6, 1957

0 r1WWW
T
137-1958-2-2426
Translation from. Referativnyy zhurnal, MetallUrgiya. 1958, N r 2, p 3 2. (USSR)
AUTHORS: Paliy, L.F., Gorin, V.K.. D'yalconov, A.I.
TITLE: The Productivity of Open-hearth Fui-naces as a Function of the
Values of the Parameters of the Bath (Proizvoditel'nost'
martenovskikh pechey v zavisimosti ot velichiny parametrov van,,)
PERIODICAL: V sb.: Fiz. -khim. osnovy proiz-va stali. Moscow, AN SSSR,
1957, pp4Z-60. Diskus., pp 160-187
ABSTRACT: A study of the performance of open-hearth furnaces of diverse
tonnages revealed that the total time to complete a heat, Z, is
expressed by the straight-line equation Z -- Y_ + K Hav ; the first
term, Z (the summation of the amounts of time needed for
preparatory servicing, charging, reduction, and tapping), is not
a function of the tonnage (T) of the furnace, but is determined
solely by the quality of the work-planning and the degree of mecha-
nization; the second term (the sum of the amounts of time needed
for melting and the "boil") is proportional to the mean depth of
the bath; moreover, the coefficient K is a function of thermal
and mechanical factors. An analysis of existing units of specific
Card 1 /Z productivity of open-hearth furnaces, i. e . , in terms of the yield,

1 -~7- 1958-2-242ri
The Productivity of Open-hearth Furnaces (cont. )
revealed their complicated dependence on the design and dimens-
ions of the baths. which makes these units unsuitable for comparing
the performances of open-hearth furnaces of equal tonnage. It was
found that the hourly productivity of open-hearth furnaces is pro-
portional to certain functions of their dimensions:
3 3
P -, M YTT and P r'-1 LYT;~ - S0
wherein S 0 is the area of the bath surface, P is the productivity
of the open-hearth furnace, and the coefficients M and L (which
are proportional to one another) are the absolute units of specific
productivity and are independent of the imensions of the furnaces.
The yield of steel, taken in units of T2%, which is called the
nominal working capacity of an open-hearth furnace, is determined
solely by the quality of work planning and the degree of mechaniz-.
ation. These findings have been verified by data obtained from
queationnaires covering 89 foreign and domestic furnaces of from
4 fq 32G tons.
Bibliography: 8 references. G.S.
Card 2/2 1. Furnaces-Production-Theor7 2. Melts-Xathematical analysia

137-1958-1-338
Translation from. Referativnyy zhurnal, Metallurgiya. 1958, Nr 1, p 52 (USSR)
AUTHORS- Agapov, V.F., Varshavskiy, A.P.. D'yakonov., A.T.
TITLE- A Study of the Sequence and Rate of fusion of the Free-flowing
Materials in a Basic Open Hearth Furnace (lzucheniye posledo-
vatel'nosti i skorosti plavleniya sypuchikh materialov v osnovnoy
martenovskoy pechi)
PERIODICAL: V sb.: Primeneniye radioaktivn. izotopov v che rnoy metallurgii
Chelyabinsk, Knigoizdat, 1957, pp 120-134
ABSTRACT: The sequence and rate of interaction of the ore and limestone
with pig iron in accordance with level and order of charging was
studied in seven b?,ats in 380-t open hearth furnaces by means of
isotopes p32, F~)"), and S35, imbedded in pieces of the lodse ma-
terials. Appearance of the isotopes in samplings of the metal and
slag indicated that the layer of material containing them had lique-
fied. Curves of the radioactivity of the metal and slag as the heat
progresses are adduced. It is noted that the deeper the layer of
free-flowing metals, the more time is required to fuse it. The
time required for the pig iron and ore to react diminishes as the
Card 1/2 amount of iron, the speed of charging, and the amount of light-

137-19~8-1-338
A Study of the Sequence and Rate of Fusion 11cont. ~
weight scrap increase. The mean fusion time of a single layer of
ore and limestone in proportion to their level in the bath is deter-
mined. A plot is adduced showing the relationship between the
tirne the isotopes appear in the samples and the depth at which
they are located. It is established that fusion time is lowest when
a single layer of ore is charged onto the hearth and the liniestone
is in the lowest possible position.
M Kh.
1. Open hearth furnaces--Performanc,&--Anidys:Ls 2. Iroz~-Produaticn
5. Phosphorus isotopes (Radioactive)-4plications 4. Fluorine
isotopes (Radioactive)-Applications 5, Sulfur isotopes (Itadio-
active)-&pplications
Card Z/Z

137-58-4-6668
Translation from: Referativnyy zhurnal, Metallurgiya, 1958, Nr 4. p 50 (USSR)
AUTHOR: D'yakonov, A. I.
TITLE: Variation in the Electrical Conductivity of Liquid Slags in the
Course of an Open Hearth Heat (Izmeneniye elektroprovodiiosti
zhidkikh shlakov v protsesse martenovskoy plavki)
PERIODICAL: V sb.: Fiz. -khim. osnovy proiz-va stali. Moscow, AN SSSR,
1957, pp 469-478. Di5kus. pp 505-512
ABSTRACT: A method for and the results of measurement of the electric-
al conductivity ~( of liquid slag in the course of an open hearth
furnace heat are presented. Measurement was by determination
of the resistance between two Fe electrodes immersed in the
slag. To determine the resistance of the slag skin formed on
the electrodes, additional measurements were made during 17"-
mersion of the electrodes in the metal. Xmeasurements were
made in four heats in 190 and 380 t basic open hearth furnaces.
Specimens of slag and metal were taken during the heats. It was
found that the of the slags varied in the 0.53-12.4 mho/cm range
The change in during the process of fusion parallels most
Card '112 closely the change in the values of the CaO/SiO2 and the

137-58-4-6668
Variation in the Electrical tcont, )
[CaO+(FeO)I/SiOZ ratio. The higher that ratio, the greater the ,"(' . It i'.;
noted that the rate of elimination of S from the open hearth bath incre,,-~e,
with increasing X-
Yu.Sh,
1, Metallurgy 2, Slags--Cord-ictivit,,--Meas,,irement 3. Kect--odes--Appli-
cations
Card Z/z

137-1958-3-4779
Translation from: Referativnyy zhurnal, Metallurgiya, 1958, Nr 3, p 46 (USSR)
AUTHORS: D'yakonov, A. I.:., Gorin, V. K.
P -_ - - -_ __
TITLE: A Rotary Spout for the Discharging of Metal From Large Open-
hearth Furnaces (Povorotnyy zhelob dlya vypuska metalla iz
bol'shegruznykh martenovskikh pechey)
PERIODICAL: Sb. nauchn. tr. Magnitogorskiy gorno-metallurg. in-t, 1957,
Nr 11, pp 70-76
ABSTRACT: The Magnitogorsk metallurgic combine developed a rotary
spout for large open-hearth furnaces, which enstires good control
over the filling of two ladles with metal and slag when the melt
is discharged, The spout is mounted on two supporting sections
set on rollers and may be rotated by means of a power drive froni
an electric winch. The lining of the spout interlinks with a trough
(approximately 400 mm long), attached to the mounting plate of
the discharge opening of the furnace.
V P,
Card 1/1

137-58-4-6687
Translation from: Referativnyy zhurnal, Metallurgiya, 1958, Nr 4, p 54 (USSR)
AUTHORS: Tuzankin, N. M., Gorin, V. K. . D'yakonov, A. 1.
TITLE. Car-bottom Slag Pockets for Rapid Slag Removal Regardless of
its State of Aggregation (Vydvizhnyyc shlakoviki dlya bystrogo
udaleniya shlaka pri lyaborn agregatnom sostoyanii)
PERIODICAL: Sb. nauchn. tr. Magnitogorskiy gornometallurg. in-t 1957,
Nr i1, pp 77-84
ABSTRACT: The design of car-bottom slag pockets for open-hearth furn-
aces developed by the Magnitogorsk gornornetallurg. in-t (Insti-
tute of Metallurgy and Mining) is described. The receiving ele-
ment (RE) in the form of a lined metal box is mounted on a car-
riage, and is rolled out by a crane onto the pouring platform.
The tops of the slag pockets rest on horizontal beams borne in
turn by metal columns fixed into the foundation. Reinforcing wed-
ges 50-80 mm high are provided between the carriage and the
RE. After they are pulled out by a crane, the RE, which has
fused to the roof of the slag pocket pulls away under the effect
of its own weight. The RE is calculated to take 250-270 heats.
Card 1/2 The weight of a full RE is 200-250 t. The force to roll it clear

137-58-4-6687
Car-bottom Stag Pocke~s (cont.
from the roof is 3-5 t and the time required for replLacement during repairs
when the furnace is shu* down, is 3-4 hours. For future open-hearth furn-
aces a sunken type of slag pocket is proposed with the RE removed to the
slag dump along inclined tunnttls below the pouring plai(oim. The benefits pro-
-1
v
ided by car-bottom slag pockets are: elimination of the need to drill and fire
charges to clean slag pocke,s. complete mechanization of slag removal elim-
ination of the partitions between gas and a.'-r slag pockets, and reciti(tion in
repair time and in open hearth furnace down time.
A.D.
1. Equipn,ent--Desig-t 2, Equiprr_,~ent--Operati_on 3. Slags--Re~aova-Pz7occesses
Card 212

P~11ko"wil,
137-58-5-9078
Translation from: Referativnyy zhurnal, Metallurgiya, 1958, Nr 5, p 47 (USSR)
AUTHORS: Perchatkin, P.N., D'Yakonov, A. I.
TITLE: Heat Absorption in the Hearth of an Open-hearth Furnace in the Course
of a Heat f 'Teplopoglo5hcheniye rnartenovskoy vanny po khodu
plavki)
PERIODICAL: Sb. nauchn. tr. Magnitogorskiy gornometallurg. in-t, 1957,
Nr 11, pp 85-92
ABSTRACT: Absolute heat absorption (HA) values were determined for in
the course of an open-hearth heat. The investigations were car-
ried out in an 185-ton gas-heated open-hearth furnace (OHF)
with carburization with tar. The heat flows (HF) were measured
by means of a calorimeter of VNIIT design. The HF's vary
sharply in the course of an open-hearth smelting-, the directflow,
passing from the flame to the hearth, varies more than the re-
turn flow from the hearth. A graph is presented showing the var-
iations of the direct FIF along the hearth. The absolute value of
the direct HF is greater at the end than it is at the midway point
in the scrap-charging process. The return HF remains practi-
Ca rd 112 cally constant throughout the length and width of the hearth.

137-58-5-9078
-lieat Absorption in the Hearth of an Open-hearth Furnace (cont.)
During the charging of scrap the HA varied from 340, 000 kcal/Irn2 at the
second opening to 140, 000 kcal/m2 at the fifth one, A similar nonUniformity
was observed in other stages of smelting also. The HF also varies from one
switching to another. The variations of the direct and return HF's in the
course of a smelting are shown in the form of a graph. The HA. which at the
time of charging of limestone amounted to 260-300 thousand kcal/M2, de-
creased to a value of'13,0-140 thousand kcal/m2 after the limestonie had been
heated for a period of 3-5 minutes. An analogous situation is observed in the
course of charging of Fe ore. After the introduction of the metal scrap charge
into the furnace, the HA amounted to 260-340 thousand kcal/m?-, but after 1.5
hrs of heating it dropped to a value of 140- 160 thousand kcal/mZ. At the end
of the smelting period and throughout the boiling stage, the HA diminishes
smoothly from 120-160, 000 to 30-50, 000 kcal/m2. The HA is also shown to
be a function of the combustion rate of C in the hearth. The HA, which prior
to the introduction of Fe-Mn into the hearth had a value of 90-120, 000
kcal/m?- (the hourly oxidation rate of C being equal to 0. 20-0.2556), is reduced
to a value of 40-55, 000 kcaI/m2 three to five minutes after the introduction of
the Fe-Mn.
1. Open hearth furnaces 2. Ifeat-Absoi-ption 3.
r:,A 10ri-
meter-Applications
Ca rd 2//Z

FBRCEEATKIII, P.N.; FATIOV, A.S.; BEZDEnZhNYKH, A.A.; BIGIMV. A.M.; IjbTIMIN, V.H.;
DIYAKOFOV, A.I.
Sulfur distribution between metal and slag during conversion
smelting of low-manganese pig iron. Izv. vys. uchab. zav*: chern.
met. no-1:33-40 160. (MIRA 13:1)
1.Magnitogorskiy gorno-metallurgicheskiy institut.
(Open-hearth process) ~Desulfuratlon)

VOHONITSYI'~, K.I., Icand. toklin. nau1c, red.; TIZITIGAUMil P.E., kand.
tekhn. nauk, red.; NADBAKH, M.P., red.; TANTSEV, A.A., slarshiy
nauchnyy sotr., red.; AffLWOV, S.A., kand. tekhn. nauk, red.;
ABILWOV, D.A., red.; BOGDANOV, II.I.f starshiy nauchnyy sotr.,
red.; VINOGOROV, G.K., kand. tekhn. nauk, red.; GAVRILOV, I.I.,
starshiy nauchn~y sotr., red., GUSARCHUK, D.E., starshiy nauchnyy
sotr., red.; 011YAKONOV, A.I., red.; ZAVIYALOV, M.A., kand. tekhn.
nauk, red.; URE starshiy nauchnyy sotr., red.;
KACIELKIII, L.I., starshiy nauchnyy sotr., red.; KISIIIIISKIY, H.I.,
kand. telchn. nauk, red.; KOLTUIIOV, B.Ya., starshiy nauchnyy :3otr.,
red.; OSIPOV, A.I., kand. tekhn. nauk, red.; SHINEV, I.S., kand.
ekon. nauk, red.,
[Materials of the enlarged session of the Scientific Council of
the Central Scientific Rezearch Institute for Mechanization and
Power Engineering in Lumbering on problems concerning power
engineering and the electrification of the lumber industry]
Materialy rasshirennoi sessii Uchenogo soveta TsNID.IE po voprosu
energetiki i elektrifikatsii lesnoi promyshlennosti. Nloskva,
1961. 75 p. (MIRA 15:4)
(Continued on next card)

VOROVITSYN, K.I.-(contimied) Card 2.
IMAmki.TSentrallmy nauchno-if3sledovatellakly institut me-
khanizatsii i energetiki lesnoy prowjshlennosti. 2. Nachallnik
TSentrallnogo byuro tekhnichaskoy informatsii lesnoy promyshlen-
nosti (for Radbakb). ). Direktor TSentrallnogo nauchno-
Issledovatel'skogo instituta mekhanizatsii i energetiki lesnoy
promyshlennosti (for Voronitsyn). 4. UcherVy sovet TSentrallnogo
nauchno-issledovatellskogo instituta mekhanizatsii i energetiki
lesmy promyshlennosti (for Dlyakonov)~ 5. Vachallnik otdeleniya,
energetiki i srodstv avtomatizatsii TSentrallnogo nauchno-
issledovatellskogo instituta mekhanizatsii i energetiki lesnoy
proir.shlennosti (for Zaretskiy).
(Lumbering) (Electric power)

ROSTOVTSEV, K.O.; VOSKRESENSKIY, I.A.; DIYAKONOV, A.I.
New data on the geology and gas and oil deposits of the eastern
regions of the Kuban. Trudy KF VNII no.6:38-66 161. (MIRA 15:2)
(Kuban--Petroleum geology) (Kuban--Gas, Natural..-Geology)

DIYAKONOV, A.I.
Geology and prospects for finding gas and oil in Tuapse District,
Krasnodar Territory. Trudy KF VNII no.6:67-go 161. (MIRA 15:2)
(Tuapse District--Petroleum geology)
(Tuapse District--Gas, Natural--Geology)

DIYAMONOVI A.I.; ROSTOUSEV, K.O.; VOSKREM-NSKIY) !.A.
New data on the geology of the Miadyzhensk and Shirvan-
Bozvodnenskiy ragiorwo Trudy KF VNII no.10:67-81 162*
(MBIA 15: 11)
(Caucasus-Geology)

VOSEMSENSKIY, !.A.; ROSTOVTSEVI K.O.; DIYAKONOV. A.I,
Geology of the I~axakayeVskoye field based on now data.
Trudy KF VNII n6.10.89-97 162. (MIU 15:11)
(Krasnodar Territory-Petroleum-deology)
(Krasnodar Territory-Gas, Natural-Geology)

DIYAKONOV, A.I.; MITIN, N.Ye.; SHELKOPLYAS, P.A.
I
P. Study of the Permian and Triassic sediments of the Belaya
Basin in the northwestern Caucasus. Trudy KF VNII
no.10:149-157 162. (MIRA 15:11)
(Belaya Valley (Krasnoclar Territory) G ology, Stratigraphic)

DIYAKONOV, A.I.; KOROTKOV, B.S.
--.- .
Geological structure and oil and gas potentials of the
southern slope of the northwestern Caucasus. Neftegaz.
geol. i geofiz. no-3:6-9 163. (MIRA 16:8)
1. Krasnodarskiy filial Vsesay-uznogo nauchno-issledovatell-
skogo neftegazovogo instituta.

GORLOVP S.I.; DIYAMRIOV, A.la
Prospecting for oil and gas in the maikop sediments of the
eastern Kuban. Neftega.27, geol. i geofiz. no.11a 6-8163
(MIRP 17:7)
1. Krasnodarakly filial Vsesoyumogo neftagazovogo nauulma -
isoledovatellakogo inatituta. '

GCRLOV,- S.I.; -L:)2R~
New data on the stracture,, and oil and goo potejitials of the
Armavir-NevinnomysEik region. Izve vysh, uchebo zava,, neftl i
gaz 6 no.3.9-13 963,. (MIRA 16:7)
1. Moskovskiy gosudarstvanayy universitet imeni Lomonosova
I Krasnodarski-y fili&L3 Yeasopmoga naftegavrrago nanchno-
isaledovatellskogo InAtit3ta.
(Russia., Southem-Petroleum Geology)
(Russia, Southem-Gaso Natural-Geology)

ALEMIN$ G.A.; GORIDV,
Determining the time-of the formation of gas pools. Geol.
nefti i gaza 7 nojt43~-49 Mr 163. (MIRA 16:4)
1. VsesqyuzMy nauchno-issledovatellskiy geologorazvedochMy
fieftyanoy institut, Mosk7a, i Krasnodarskiy filial Vsesoyuznogo
neftegazovogo nauchno-iseledovatellskogo instituta.
(Maikop region-Gas, Natural-Geology)

GORLOVI S.I.; DIYAKONOVP A.I.; NESTEROV, L.V.; SDKOLOV, P.N.
New gao-bearing area-1n the northern foothills of the Greater
Caucasus. Geol. neftl i gaza 7 no.5:39-43 MY 163
(MiiA 16:6)
1. Krasnodarakiy filial Vaesoyuznogo neftegazovogo nauchno-
itseledovateltakogo instituta, i Nauchno-promyslovoys upravledys
Kbadyshenneftt.
(Caueasus-Gas, Natural-Geology)

DIYANONOV, A.1,
lacies chara--:~trzristics of the Liver C-.e*,.ace(-)Us sed,'men'.G
.9 u+,hern slope of the nc;rthwaat,-,rn llauca3us -n
Prospects jlrr finding -.)i1 and gas. Izv.vys,llchj0b.Zu-l.:,
razv. 6 nc.11%73.-85 N 163.
1. Krasncdarsk'y f1lial Vse3-3y-..iznogo neftegazotrcg. rauciln
doW-,I'sk-,)go inutLtuta.

GORLOVP S.I.; DIYAXONOVJ, A.1e; ALEMS121, G.A.
New oil and gas bearing region In the eastern Kuban. Neftegaz.
geol. i geofiz. no.6:35-39 164. (MIRA -17:8)
1. Krasnodarskiy filial Vsesoyuznogo neftegazovogo nauelmo-
issledovatellskogo instituta, i Vsesoyuznyy nauchno-issledovatell-
skiy geologorazvedochnyy neftyanoy institut, Moskva.

D I YAKONOV A I
Prospects for finding oil and gas ir~ ~h,! Cret,~xeujs sedim-:,,r,'L-,O-
of the Black Sea region. Vest. Mosk. un. Ser. 4: Geol. 19 nc.',:
20-27 Ja-F 164. (MIFIA il~,:,- "
1. Kafedra geologii i geokhiviii goryuchikh iskopayeraykh Moskov-
skogo universiteta.

DIYAKONCV, A,1.
Geological prerequialtes for oil. and gas proopeel5ing anj prospecting
plan for the Black Sea region in Krasnodar -
lerritory. Geol. nefti. I
gaza 9 no.6:32-36 Je 165. (MIRA 18:8)
1. Krasnodarskiy filial Vsesoyuznogo neftegazavogo nauchno-
issledovateliskogo instituta.

RDSM, N.-IT. (Veterinary Doctor) and 21YA V -A-2. (Veterinary Technician,
JMM 7
B-Ehoumutets Veterinary Section, Dobrovsk District, Lipetsk Oblast'). (Abstracted
by NOSNDV, A. I.)
"Treatment of herpes tonsurans".....
Veterinariya, Vol- 39, no. 3, March 1962 pp. 32

'a
on r!
Ju ~'.MIRA MtO
I
K C Y. CZ,pi

-l.'Y~,4.,--,f4-'V', ~.j
'I t- --l * - . i . --, ,
I : .1 .. I . . .1 : ~ 11 t. " .. 0
8 -,, ') . ~ ~ 3 5.- "1 ~ 7 : :, j. , - . , -
-I I .! t1:

. D.I, -,
Principles of using amplitude and phase charActeristics of an
electromagnetic field in electrical prospecting. Izv.AN SSSR.
Ser.geofiz. no.100207-1210 0 1560* (MLHA 10:1)
1. Akademi7a nauk SSSR Geofizicheskiy institut.
(Prospecting-Geophysical methods)

WYAKONOV, B. P.
49-3-15/16
AUTHOR: Kirillov, F. A.
TITLE: Cbnference of junior research workers, engineers and
aspirants of the Institute of the Physics of the Earth,
Ac. Se., U.S.SR. (Konferentsiya mladshikh nauchnykh
sotrudnikov, inzhenerov i aspirantov Instituta Fiziki
Zemli AN SSSR).
PERIODICAL: "Izvesti-va Akademi'L Nauk. Seriva Geofizicheskaya"
(Bulletin of the Ac. Sc., Geophysics Series), 1957,
No. 3, pp. 411-415 (U.S.S.R.)
ABSTR.kCT: The conference was hela on December 24-26, 1956, 21
papers were read relating to work corip]-eted in 1955 and
1956. In this report the contents of the individual
papers are briefly summarised. B. P. D'yakonov read a
paper "diffraction of Electro-,',Lag'netic--'~Taves-on
Spherical Inclusions in a Two-Layex 1-ieedium:'.

f ~ K 0. % r4 o ~' t~" ; -
AUTHOR: D'yakonov, B. P.
49-6-12/21
TITLE: Nature of the electric currents of the Earth and their
investigation at the bottom of the ocean. (Priroda zemnykh
elektricheskikh tokov iikh issledovaniye na dne okeana).
PERIODICAL: "Izvestiya Akademii Nauk, Seriya Geofizicheskaya"
(Bulletin of the Ac.Sc., Geophysics Series), 1957, No.6,
pp. 800-802 (U.S.S.R.)
ABSTRACT: In spite of the fact that there is a great deal of work
published on the study of currents in the sea, the author
points out that most of the experimental work is extremely
superficial. Recording of the electric currents in the sea
by various authors was effected mainly by means of pick-ups
submerged to shallow depths around the shores and,so far,there
is no comparison between the electric currents in the sea
and on the land recorded simultaneously by means of identical
automatic recording apparatus. A further study of the
natural electric currents will have to be made at larger
depths and it will also be necessary to utilise the sea as a
screen for certain frequencies of the electromagnetic field
of external sources for the purpose of detecting the electro-
magnetic signals emanating from the depths of the Earth.'.It
Card 1/2 is shovin that at a depth of 2 km disturbances with periods.

49-6-12/21
Nature of the electric currents of U--he Earth and their
investigation at the bot-Gum of the ocean. (Cont.)
below 15 minutes will be appreciably weakened and this effect
can be utilised for attempting to record electromagnetic
disturbances of a new nature which so far have not been
studied. No new experimental data are given. In conclusion
the author outlines some of the problems, the answers to
which could be revealed by means of the electroma6uetic
disturbances with sources located inside the Earth: the very
fact of their existence will provide additional information
on the state and the structure of the internal regions of our
planet; if a correlation will be observed between the
recordings of currents at distant spots, there will be
adequate justification for the conclusion of the existence
of a unified system of currents which encompasses large
regions of the Earth; the seismic activity of the depth of
the Earth may cause so far unknown electromagnetic
disturbances which encOMDass limited regions and this would
be of great interest since it may permit solving the
difficult problem of forecasting earthquakes.
There are 1 table and 14 references, 10 of which are Slavic.
SUBMITTED: February 23, 1956.
ASSUCIATION: Institute of Physics of the Earth, Ac.Sc.USSR.
Cexd 2/2 (Akademiya Nauk SSSR Institut Fizilci Zemli).
AVAILABLE, Libroxy of Congress

Sj VILLIV.
AUThOR: D'yakonov
B. P
,
TITL-~: Diffraction of Electromacnotic Mavel,: by il C i rc, v, 1 a r
C,71-inder in a Uniform Half -Spw.-:_,
P.L,;1iIODICAL: Izv,_7!stiya A'r-.adem_J_J nau.-. 3SS11, S-,_*-11,-'~~--- ._-,z1.'-aYa,
pp 1332-134' (USSR)
lir 9
1959
,
,
ABSTRACT: The aim of the present io -.o Solv,_- t,- ~rotlem of trie
diffraction of electro.ja,_ neui.c waves i indrical
inclusion placed in a wiii'ori:i haif-S-Dace, TI-1 s- c- o I u 'U i o
is ex- ressed in a f orm ,vhich is. ili "~'a 11
calculations in connection wit", P, r 0.~ -p e C ?-- i f L~,
The problem is formulated in b1ri(,~
an a I Le rn, a cir.6 e I ectl-roma~..,nf-: i~.ic fd.L~ A d W
which is produced by a source p,iacc(i i1 nai.r or on L,-.,.
E arth' s surf ace. Unde _T~ 1.1i e Ea rS. ua- face -a ef tz; Is all
infinitely 10r-,,:, C311LidPjC,1l ia circular
crocs-section i,;hose w--is, is Pal-t'Lle-1 -.,o th-:~ surfoce, Ini" I El
Earth and the inclusion are loo',%e" lAv,,jii as un-:.form- a;nd
anisotropic. In oider to scimpl'if.. tlli:'-~ rLob l-~,, I-. is asca,,'~-d
that in rhe field produced 'by tr.v .-.. ~-ro iz~
component of U"he electric fie!Ld (Par.-.Li_C_-.L ~" C) _'_'1ji-
Card 1/4 the cylinder and coristarit aloii,,

Dif f r a ction cj _` E, lectrom a I. ne tic W a vez by a CIIIVC~, I !.ndc r11 C.
Unif orm Half -Space
to dt~t-~rlftirle the
race ~tnd also inside the
us;ed a-~, -- conductivit-.,,i of
a - radius '---iice
A
C'~rliuder to the Eart-11's surfrtce., 111-e
tfie earth and ai-Ir are, subscr-ipt,li 1
HL,li perii1eZibiliL. of t I I k2 i I: t~.~d I !1 1(1, 11t."d Q bt2 16
SlAme It is viell luiov..-ii (Ref 2) that a,_~ all ord1,;-_,,,rV
in Space, a monochromatic fi,~11.d
the %-,,ave equation -'-iv(,n by Eq (1),
2)112 1 - t-
e4w s the wave nui.,iber in the iedium.. The v~otor
potential A is L,-',ivf-,n by Ec,'(2), and
t~ie eiectric field axid -t-',,-e voctur pol~-_-t_`al b,~ C:~,,
since ir. the case under consiCeration div A =. 0,. 0 a
boundaries between media with d`z .41 f e r e n te c, t; r i. c a 1 -D r c-,, e r
ties there should be a continuous tan-entiall coMIDOP1.3nL C.11
both. electric a-rid magnetic fields. At: iufini,5,i, -.-In'-
diffracted field should obey the radia--,ior- In
V_
Card 2/1, this way the problem formulaCed above is reduced zo

Diffrac:.i o 7-i o lectromiagrietic 45vc'3 '!~Y
Uniform Half-Space
solution of -L~q (1) subj,~(-,t tLo n
bouDdaries,, ti,,e, pro-Durti"S 01'
~'O,e couditions ~it Ti,
0 r"-
'11C I
41--jon of ti,e Problem
of the vect-or poll-enti--,,! b,:,rh f o
ffrac~-2d. fields. F r O-m E o 0 "I'd
V~ i7
tl,,a~ for the z--compotient of tl~e. t, Z~ U
ri are of tl- ion,
o nd
i,,y
Lnr--'I-icatv..~3 the iiormal ~~o A'!
vect-or pate k,.- :_, ~'I
n' i als on e ith-~r Ld of
r)roblei~ is solved b7,,
.L,;ar~:,h-air bOUTidf~:iry ii: ropi.-~ic-2cj
.,,ad-iu-, R. so t,hat- the disiljjl,7~F! 0 i- %1. 1
T"-e problem, --is then reduced to t-'hiail- G C-.
-axes are parallel but do, no-F F, 2 c,
o f t hi s -p r o 1) 1 e::,, t;: e, r!-~ qu d s o lu o. r:
PUt'116- Ro.-? vo at co-istant ri,
U L
trair--,formed to polul, C-,,O-dlfl~ t",-,
V.7hich case the boiindai-y c6nditio,--,.~: 11 f
Ce,T.--i 3/4 by l,qs (8) and (c)). The 0 0 IU tj. Ti S V,

SOV ";Q
Dif If rac tion. of Z I ec"'Vorn, a, netic ""I a v~a Crclu
Uniform Half-S-oace
foi:in (;i' ~,eries (Eas, 104 11 =:1
obtaii---,,-~;.! from the bowidary T-
4~he ;n I--- ~,r. iu J, e a f - he
-1 f f rc.--,(I
u
surf callno S Lie I
is alterjd if
inLroduced by iche
iG is not diificiilt to e).ft-end 0 1 u i:.-''Dr,Ith, e
case where the iaai~not-ic f Leld if, ai:)11-- Ls
independent of z. Tliere arc I
ences, of which 3 are t:L-ans-lat-ion,-~ fro'm -,.i I -J zh
ASSOCIATIONt AlKad-lemiya nauV. SSSR.
(AS LISSR, Inst i t 11 t il' Ph-s i,_- -- of
SUBMITTED: Deceriber 1, 1956
Card 14/1,

Sc),114 G.- 5Q. - 11-E/28
AUTHOR: D'yakonov, B.P.
i
TITLE: Diffraction of Electromagnetic Waves by a Sphere
Placed in a Half-space
PERIODICAL: Izvestiya Akademii nauk SSSR Seriya geofizicheskaya,
1959, Nr 11, pp 1579-1590 (USSR5
ABSTRACT: The problem is solved for a sphere having an arbitrary
conductivity and placed in a conducting half-space with
a plane boundary. The solution is obtained in a form
convenient in low frequency electrical prospecting. The
corresponding problem for a cylindrical inclusion was
solved by the present author in Nr 9 (1959) of this
journal. The magnetic permeability is assumed to be the
same for the two media and the electromagnetic field is
-taken to be polarized so that there is only one
component of the electrical field. Maxwell's equations
are then solved subject to the usual boundary conditions,
namely, -that -the tangential components of the electrical
and magnetic fields are continuous across boundaries
and the radiation principle holds at infinity. The
wave equation for the problem is given by Eq (2) where
Card 1/3 U is the Hertz function defined by Eq (1) (Ref 3~. Since
VII,

~~jv/49-5c,-11-6/28
Diffraction of Electromagnetic Waves by a Sphere Placed in a
Half-space
there are three media (air, earth and the inclusion),
there are three functions U and these must satisfy
Eqs (2a), (2b) and (2B). The boundar-, ~r conditions (cf
Fig 1) are given by Eqs (3a) and(3b). Assuming that
the source is in the air, the solution is souEht in
the form of the series given by Eqs (6), (7) and (8)
and the coefficients are determined from the boundary
conditions. Formulae are obtained for the expansion
coefficients in the form of an infinite system of
algebraic equations. In the first approximation the
final solution takes into account the effect of
diffracted waves reflected from the boundary
of the half-space on the current distribution
both in the sphere and the adjoinin6 rc,Gions.
Thus the solution takes into account not only the
effect of the uniform half-space on the primary field
but also the effect of the interaction of the sphere
Card 2/3 with the "plane" boundary. There Lire 7 references, 6
V

A
SOV/49-59-11-6/28
Diffraction of Electromagnetic Waves by a Sphere Placed in a
Half-space
of which are Soviet (2 translations from English)
and 1 English, and I figure.
ASSOCIATION: Akademiya nauk SSSR, Institut fiziki Zemli
(Academy of Sciences USSR, Institute of Physics of
Earth)
SUBMITTED: January 25, 1957
Card 3/3

86313
3,91ao S/049/6O/0O0/OO7/oo4/oo9/xx
91 C1 700 E032/E3i4
AUTHOR: -D-1 Y-&kQ-nQ-v,-B-&-E-
TITLE: Asydiptotic Expressions for the Electromagnetic
04-1 Due to Cylindrical Inclusions
PERIODICAL: Izvestiya Akademii nauk SSSR, Seriya
geofizicheskaya, 1960, No. 7, PP. 954 - 958
TEXT: In order to investigate the principal features of
anomalous electromagnetic fields due to inclusions under the
Earth surface, it is frequently convenient to replace these
inclusions by simple geometrical forms, e.g. cylindrical
bodies. The present paper derives expressions for the
electromagnetic fields due to massive extended objects in
the form of right circular cylinders. Use is made of the
solutions obtained by the author in a previous paper
(Ref. 1) for the diffraction of electromagnetic waves by a
right circular cylinder in a half space. It is shown that
the vertical component of the anomalous magnetic field
decreases along the surface at least as 1/y3 while the
Card 1/3

86313
s/o4q/60/000/007/oo4/ooq/XX
E032/E314
Asymptotic Expressions for the Electromagnetic Fields Due
to Cylindrical Inclusions
electric component and the horizontal component of the
magnetic field decrease as 1/y - These results confirm
that it is useful to measure the horizontal components of
anomalous electromagnetic fields in searches for local
anomalies. It is also shown that the vertical component of
the anomalous%ij ~etiq field will be much stronger in regions
where there are considerable irregularities in the medium in
the horizontal directions and this is in agreement with
experimental data.
There-,are 3 references: 2 Soviet and I non-Soviet.
Card 2/3

86"
S/049/60/000/007/004/009/XX
E032/E314
Asymptotic Expressions for the Electromagnetic Fields Due to
Cylindrical Inclusions
ASSOCIATION; Akademiya nauk SSSR Institute fiziki Zemli
(Academy of Sciences of the USSR, Tns-~uta
of Physics ofthe q-th)
-E r
SUBMITTED: September 10, 1957
Card 3/3

DlYiKONM,- B.._.V. TIKHONOV~ A.N.0 IVANOVt A,O., and TROITSKAYA, V.A.
"Relationship Between Earth Currents and Earthuakes" Tr. Geofiz. in-'.,a AN SSSR,
No 25, 19549 181-191
A relationship between the propagation of seismic wzves and the ap-
pearance of an electromagnetic perturbation,, the so-cilled seismoelectric
effect is held possible, The effect originates in slow undulations of the
terrestrial core which may propagate as an elastic wave. The noticed coincidences
of seismic waves and electric perturbations indicate the ner-esit f recording
the slow motions of the terrestrial core. (RZhFiz, No 10, 19W 0

- I
Termicheskiye IssL.-davaniya Skvazhin R--~s;arcb on Cil By~7V- It'. Lkhnv
I D. 1. ';.,'Y-Akonov.
~51 P. lidacro., Tabil'J's.
IITA-.erw~,ural': r.
N/5
L~4-4
- Di

DAKMTOV, Vladimir Hikolayevich. professor; D'TAKONOV,D.I_., redaktor; PATRO_
VA,Ye.A.. redaktor; POLOSINA.A.B... 66%nl~hilkly~ daktor
(Interpretation of the results of geophysical studies of well pro-
files] InterprotatBiia rezulltatov goofizichookikh iseledovanii raz-
rezov ekvazhin. Hookva, Goo.nauchno-tekhn. izd-vo neftianoi i gorno-
toplivnoi lit-ry, 1955. 492 p. --- - [Album of charts for inter-
preting the results of well studies by resistance methods; an ap-
pendix) -- -- Allbom paletok dlia interpretateii rezulltatov issle-
dovaniia skvazhin me5odow soprotivlenii; prilozhenia. 17 graphs
(in portfolio) (KIRK 9:3)
(Prospecting--Geoph.voical methods)

D'YAKONOV. D.I., doteent.
- awskWAAW
Improving the interpretation and utilization of applied geophysical
data in the petroleum Industry. Trudy W no-15:5-12 '55.
(KM 9:8)
(Prospecting--Geophysical methods) (Petroleum engineering)

D I YAK0.*l0VP D. 1. Doe Geol-.Ilin Sci -- (disrs) "Thempl of' solvinG
T
geologiciA and petroi~-,imk-roblems.ll ?,ios, 1959. 30 pp Can n-C Higher Education
p
M;SR. laos Order of Labor Red !~t-nnor ly.i;;t of -try and Gas
ltin4W
Industry im. 1. 1% Gub*kin. Chair of likmk4 Geophysics), 150 copies (KL, .52-58, 99)

3(5)28(5) PHASE I BOOK EXPLOITATION SOV/1262
Dyakonov, Dmitriy Ivanovich
Geotermiya v neftyanoy geologii (Application of Geothermal Surveys in Petroleum
Geology) Moscow, Gostoptekhizdat, 1958. 276 p. 2,500 copies printed.
Ed.: Dakhnov, V-N.; Exec. Ed.: Dobrynina, N.P.; Tech. Ed.: Mukhina, E.A.
PURPOSE: This volume is intended for geologists, geophysicists, and petroleum
engineers and may also be used by students at petroleum institutes. As a
textbook it can be used as a guide in conducting and interpreting geothermal
surveys in mining and in the solution of hydrogeological or engineering-
geological problems. It is also useful in the study of the geothermal
characteristics of coal, salt and other mineral deposits.
COVERAGE: This work discusses the history of the geothermal method and evaluates
its scientific and practical value. It further describes the theoretical
principles, the methodology of exploration and the interpretative techniques
essential in geothermal borehole surveying. Particular attention is paid to
the geothermal surveying of oilvells. By collecting and interpreting a large
amount of basic field data, the author establishes the thermal characteristics
Card 116

Application of Geothermal Surveys in Petroleum (Cont.) SOV/1262
of many oil-bearing districts of the USSR. He also establishes basic relation-
shipsbetween the many factors bearing on the problems of exploration or ex-
ploitation of oil and gas producing fields. The author thanks Professor V.N.
Dakhnov for his assistance in editing the work. There are 48 figures, 24
tables and 224 references., of which 169 are Soviet, 50 English, 4 German, and
1 French.
Card 2A0_

Application of Geothermal Surveys in Petroleum (Cont.) SOV/1262
TABLE OF CONTENTS:
Introduction 3
Ch. 1. Brief Review of the Development of GeothermicB 5
Ch. II. Theoretical Basis of Geothermics 20
1. Thertral'regime in the 'surfac,6 and deep layers -of the earth's crust 20
2. Natural thermal field 28
Regional natural thermal field of the earth 28
Local natural thermal fields in the boreholes 40
Ca. III. Thermal Conditions in Boreholes and Problems of Conducting
Geothermal Investigations 45
Thermal conditions in boreholes 45
4. Preparation of boreholes for 93otherml surveys 66
5. Conditions for conducting geothermal surveys in boreholes 70
Use of various types of thermometers 70
Thermal inertia of the electric thermometers 73
2-.chnical conditions of recording and preparation of gaothermo-
grams (thermal graphs] 76
Card 3/6

Application, of Geothermal Surveys in Petroleum (Cont.) SOV/1262
Ch. IV. I-aterpetation of Geothermal Data 82
6. Thermsl -properties of rocks 82
Thermal resistivity, specific heat and conductivity of rocks
and their determination 82
7. Methodology in determining the gaothermal parameters 94
Determination of the geothermal gradient and the geothermal
%lotep" [depth increase per unit of temperature] 95
p! for the approximate determination of Beothermal
Special tachniji
gradients and steps" in boreholes with nonstabilized thermal
conditions 98
Determination of the thermal flow density 100
D,-termination of the temperature at a given depth 101
ComputAtion of results on geothermal state of boreholes 1W---
Cb. V. Utiliza;tion of Geothermal Data in Solving Problems in
Petroleum Geology 104
8. Study of geological cross sections of wells 1o4
Lithological-stratigraphic differentiation in oilwell cross-
sections accordJmg to geothermal findings 105
card 4/6

Application of Geothermal Surveys in Petroleum (Cont.) SOV/1262
9.
10.
Values of the geothermal gradient in lithologically homogeneous
intervals of cross sections for various regions of the USSR 2,29
clayey deposits 129
Sandy deposits 130
Carbonates -.30
lWdrochemical sediments 131
Magmtic and metamorphic rocks 1.31
Detecting mineralized horizons in the borehole cross-
sections IZ3
Petroliferous and gas-bearing horizons 133
Water-bearing horizons 139
Salt deposits and coal-bearing beds 141
Study of the geological structure of the explored regions 142
Correlation graphs --.43
Geothermal profiles 146
Geothermal maps 148
Application of geothermics in areal geological surveys 158
Application of geothermics in the hydrogeology of petroliferous
regions 16o
card 5/6

Applica-t-ion of Geotherml. Surveys in Petroleum (Cont.) SOV11262
11. Study of geological cross'-aections and tectonics of various
regions under permafrost conditions 170
Geophysical characteristics of the per oat zone 1,170
Yqpsometric relationship of the lower permafrost boundary
to the deep tectonics of explored regions 179
12. Analysis of geothermal characteristics for vario~ts regions of USSR 183
Conclusions 1'9-1
Lite-Latare 195
suppleme:Uts 2o4
AVAILABLE: Library of Congress MM/fal
3-6-59
card 616

Ll:v,)y
IS kit
A~44 i AA
o
Hs 4.
91
4 9 116 '3
In

D 1 YAKOMOV, D. I.
Geothermal investigations in &real geology and subsurface tectonics.
Geol. nefti i gaza 4 no.11:50-54 N 160. (MIRA 13:11)
1. Moakovskiy- institut neftekhimicheskoy i gazovo7 promyshlennosti
im. akademika Gubkina.
(Earth temperature)

DAKINOT, V.N.; KOBMOVA, Y.N.; PBOBERMIKOV, Y.F.; SINLOLISEMN; B.Yu.;
KMLIN, A.I.; POZIN, L.Z., DtYAKORDY D.I.- LATYSRVA, JLG.;
DD3WHIN, Y.M.; LARIOBOV, MIM, A.P.
Terminoloff and symbols used in applied geopbysice. Prikl. geofis.
no.27:223-235 160. (MIRA 13.12)
(Prospecting--Geophyaical methods)

VASILIYFV, Yu.M.; DIYAKONOV, D.I.; CIIARYGIN, M.M.
Most important physicnl parameters of the deer,3Catlad structures
of the Caspian Lowland. Trudy MINKHiGP no-43:178-191 163.
(141RA 17:4)

DVYAKOIT"V, D.I.
Some regularl"ies in the die-tribution of tIrp nat-u-nil thermaL
field and possibilities of using geother-my. Trud7 MINKOIGP
no. 50:~Z08-211, 161, (MLA 18a2)

ACC NRI AT6028387
AUT11OR: Dlyakonov, D. I.
ORG. none
SOURCE CODE: UR/0000/65/ooo/6oo/0267/0274
TITLE: Geothermal investigations in oil- end gas-bearing regions
SOURCE, International Geological Congress, 22d, New Delhi, 1964. Ge6~6yitheakiye
rezulltaty prikladnoy geofiziki (Geological results of applieO geophyaico');- doklady
sovo.takikh geologov, problema 2. Mo3cow, Izd-vo Nedra, 1965, 267-271,
TOPIC TAGS: gmlaRr, - geothermal exploration, Pei-idieum
prospecting, gas prospecting
ABSTRACT: In the present paper the possibilities of applying geothermial -.methods
in prospecting for oil and gas are analyzed. The use of these methods, ija bil- and
gas-bearing regions of the USSR and other countries made it possible to,-_.ejt Ablish
the:principal regularities in the distribution of the Earth's thermal f,i;~-Id based
on lithological, tectonic, and geohydrological factors. Geothermal prospe.c~ting
1 methods provide the solution of the following problem: a) determinatio"n-'of tempera-
tur~s and geothermal characteristics of subsurface formations,-b) locatiq~i of various
minerale by investigation of local thermal fields produced by exothermp~ and endo-
thermal processes; c)detection of inflows and annular circulation of wateri' water-
yieiding and water-absorbing formations, position and character is ti cs o~f cement
Pard I/

ACC NR, AT6028387
in the annular space; d) more exact definition of geological otructurC~f oil and gai
fields and study of deep-seated tectonics; e) study of geohydrologicalland f~rost
(in'permafrost areas) characteristics of oil and gas fields; f) controi*'*of' the
development of oil and gas fields. The most important trends of geothermal research
are as follows: a) development of theoretical basis of thermodynamics 'ania thermal
regime of the Earth's crust; b) systematic determinations of thermal p ioperties
of rocks and formation fluids; c) compilation of local and regional g66,i~~rmal
mapp; d) preparation of instructions for conducting geothermal investionfione in oil
P7
and gas fields.
SUB.CODE: OV SUBM DATE: o6jan65/ ORIG REF: oo4

L 05343-67
C NR, JW1
M~f (1) FDN/GW
SOURCE CODE: UR/0020/66/168/004/0871/
AUTHOR: Vasiltyev, Yu. It.; D'yakanov, ii. I.; Charygin, M. M.
Gas Industry Im.* I. M.
ORG: Moscow Institute of Petro !um Chem Gubkin
(MoskoVsMy insMut neftelchimichesEoy I gazovoy promyshiennosti)
TITLE: Temperatureof the deep layers of the Caspian Depression on the basis of data
from the Aral-Sor Superdeep Borehole
SOURCE: AN SSSR. Dolclady, v. 168, no. 4 1966, 871-873
TOPIC TAGS:
ABSTRACT:
geophysics. thennogram
i The authors present the first results of geothermal ihirestigatTfon6 madi,;
In the Aral-Sor superdeep borehole which is being drilled in the Caspian do-,
~Pression. The data are as follow.,
Depth,m T~mverature, OG
500 27
11000 40
2,000 56
3,000 71
4,000 87
5,000 123
C.,d 1/2 5,941 150
..g- r

L 053h3-67
ACC NR, AP7
The analysis of geothermograms revealed that the sedimentary complex In the
depression consists of deposits which differ in thermal properties; there are
many layers which differ In lithological composition and heat conductivity. This
paper gives full details on geothermal gradient for each of,the stratigraphic
com*ponents of the &~ologlcal~e
cross section. This pa er was presented by Academician
D. I. Shcherbakov on 6 January 1966. OPM 37,058
SUB CODE, 08 / SUBM DATE: 06 Jan 66
kh
Card 2/2

FAKASENKO) S.I., inzh.; SHCUKHRINA, B.G.J. Inzh.; AKSENOV,, V-;V.,, kMd*tekhn.
nauk;.D-IXAXQ,NQY-,,. ~Df. inzbr.; MMONOV) N.T... inzh.
Testing experimental oeetioup of the oupport of the AKD unit.
Ugoll, prom* no*6.*54P-57 A-P 162, (IURA 16J2)
1. Toretskiy-mashinootroitelinyy zavad (for Panasenko., Shcherbina).
2. Institut gornogo dela im. Skochinskogo-(for Aksenov, D-Iyakonov,
Mironov).
(Mine timbering-Testing)

AKSENOV, V.V., kand. tekhn, nauk, nauchnyy rukovod1tel';.P'_jAKQj~QY,
D.N., inzh.; MIRONOV, N.T., inzh.; YAKOVLEVA, L.A., red.;
69ASIMOV, V.F., tekhnolog I
[Optimian parameters of a system of working steep seams with
stoping machinery and the efficiency of mechanized mining)
OptimalInye parametry sistemy razrabotki krutykh plastov
ochistnymi agregataxi t effektivnost' agregatnoi vyemki;
kratkii, nauchnyi otchat. Moskva, AN SSSR, 1963. 46 p.
(MIRA 16:10)
1. Akademiya nauk SSSR. Laboratoriya podzemnoy razrabotki
ugollnykh mestorozhdeniy.
(Donets Basin-Coal mines and mining)

DIYAKONOV, D.N., inzh.
Basic parameters of a stope for the AKD unit. Nauch. soob IGD
2002-81 163. (iMk 16: 10)
(Donets Basin--Coal mining ruichinery)

SHAKHOT, A.A.; STARKOi SiAwi, KHAZANOV, V.S.;.DITAKONOV, F.S.
Spectral characteristics of plants. Bot.zhur. 44 no.12:1681-1693
D 159.- (MIRA 13:4)
1. Inatitut fixiologii raateniy AN SSSR, i Visesoyuzrqy nauchno-
iscledovatellskiy evototekhnichookiy institut, Moskva.
(Arctic regions-Leaves--Optical properties)

DI WOW, IF. V.
Economic Geography
Divnertation: "Geography of the Economy of Southwestern Yakutsk ASSR." Cand Geog
Sci, Moscow State Pedagogical Inst iment V. I. Lenin, 22 Mar 54. (Vecherayaya Moskva
MOSCOW, 13 Mar 54)
SO: SUM 213, 20 Sep 1954

D I.YAKONOV., P.V.; NALUACV, G.V.
"Economic and Geographic Characteristica of the Southwestern Part of the
Yakut A.S.S.R."
p. 6 Trudy Akad. Nauk SSSR, Yakutsk Filial, No. 1, 1956.