SCIENTIFIC ABSTRACT VLADIMIROV, L.V. - VLADIMIROV, O.A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001860210017-5
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: March 14, 2001
• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

VIADIMIIW.. L.V., red.
me thods of chemical analysis in basic chemistr-yj Iz
metodov khimicheskogo analiza v osnovnoi khimii. Moskvaj,
Laboratoriia nauchno-tekhn.informatsiij, 1961. 58 P.
(MM 15:8)
(Chemistx7, Analytical)

VLADIKROV, L.V.; SHULIGINA, M.N.
Rapid complexometric method for determining phosphoric acid in
defluorinated phos hate, determination of sulfate ion in super-
phosphate. CTrudyj NIUIF no.164:51-52 159. (KRA 15:5)
(Phosphoric acid) (Titration)

VLADIMIOV, Leonid Vladimirovich; YIYACHKO, An4rey Borisovich;
---- ------------- A.S., t~khn. red.
(The father of machinfoslOtets maBhin; rasekazy o stankakh. Mo-
skva, Izd-vo "Znanie," 1962. 53 p. (Novoe v zhizni.. nauke,
tekhtike. IV Seriia: Tekhnika, no.15) (MIRA 15:9)
(Machine tools)

vIADIMIROV, Leonid V24dimirovich; FEDCIMO, V.., red.; BUGROVA, A. y
-- -
(Roads to the invisible treasurelDorogi, k nezrimomu kladu.
Moskvaj, Molodaia g;rardiia, 1962. 226 p. (MIRA 15:9)
(Electric power--Research)

VLADIMIROVs Mo
Shortcomings of the 'Rekord" and NStart-3w television receivern.
Radio no. 11:48 N 160. (KM 14:1)
(Television-Receivers and reception)

VLADMIROV, 14.
Mias.ind. SSSR 34 no-3:45-46
Wking of sheep pelts. 1 163.
(MIRA 16:7)
1. Kiyevskiy myabokombinat.

~ 9 makhanik-nastavnik,- dDVOAUVYKHq V.; KHOZEp A.v kand.
tekhn.nauk
Cool-Lng external frames of self-dIeving doors of the 1".V-5 boi?er
Rech. transp. 20 no. 2:" F 16i. (MIRA 1412)
(Boilers j, Marine)

,VLADIMIROV, 14. (g.Kursk)
Factnry is being built quicklyA*nd efficiently. Prom.koop. 13
no.8:26 Ag 159 (MIRA 12:12)
(Kursk-:!Cleaning and dyoing industry)

V'r
-Zli- 14. A. VLADEVIROV
V-1, and
VoL,dushnye woruzheniia G-rmanLt; t3tortia, taklinika, kadny,
sovr&ninnoe sostoianie., mmozhosti. lloskva, ~~os. voen. izd-vo,
1935. 164~3 p., illus., plabns, tables, riaps.
Titl,5 tr.: The Air Force of Germany; history, tec"lique, cadris,
recent conditions and potenti.*1 development.
UCA35-133M
3:): Atronautical Scis~nces and Aviation in the Soviet Union, Library of
Congress, 1955.

_4 A
BURUW. 1~3. voyeainthener 3 ranga; 7LADIMIROV, M.A.; TZpLINSKly, B.L.,
general-mayor aviataii, radakto-r;-!Y-Itkllbkytv-,n~~ir-.-i., mayor, redaktor;
DOZIMT, I.M., tekhnicheakiy redaktor.
[Military aircraft of the U.S.S.R.] Voonnys samolety SSSR. Mook7a,
Voennoe Izd-vo Narodnogo komiseariata oborony SSSR, 1940. 39 p.
[Microfilm] (MLRA 7:11)
1. Russia (1923- U.S.S.R.) Armiya. Tlpravlenlye voyeano-vosdush-
nykh oil.
(Lirplanes--Recognition)

V) ~p, leks,,Ievich
.Ljjj1-t,rjV j-qjj a
frhe air fieet -~'f n c e
u loilsid (SDrp-vochnye- Sv
Vozdushnyi r1o'
~ I I sk-v,- '-)S 71 Z' "o ta
datq~ Pod red. E. G. . '.' '. *'j- - 1 "-V
1936- 199 P- illus-, tables, diaCrs.
Folded rAn in pocket. DTZ: 'uG,(j35-PTj'55
ost c5t-H
SO: ansportation nm: C,7,ua-.uvLjct1tio1-.'~' P, P'-iblloj~rauhy) 'Abrfiry of Con:ycss
,ient, i,ashlnCton 1952-,
Refererce Departr y unclasoMed

VULDIFIROV) HIM~IL AL,'K5 ~11 I C; i.
Vozdushnyi flot Pol'shi (spravochnyn svederiia). Pod redaktsiei
E. G. Biddem. -:'oskvi, '~os. voen. izal-vo, 1936. 199 p., illus.,
maps, tables, diagrs.
Title tr.: The air fleet of Poland. A m2nual.
UG635-PTv'55
SO: Aeronautical Sciences and '.viation in tho- Soviet Union, Library oP
Congress, 1955.

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61,1111. Ills HE I IF
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12
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33M

VIADjBIROV, M.P., Eng.; SE1,121OV, G. N., Eng.
Bearings (Machinery)
Ways of saving metal in forging shops of bearing plants. Vest. mash,
32j, No. 4, 1952.
Monthly Jjpt SLf Russian AccessioRM,
Library of Uongueos, Cctober 1952, UNCLASSIFIED.

VLADIMIROV, M.I. (Baku)
- .Mll %
Green saund. Zdoroy's 4 no.4:16-17 Ap 158. (KIRA 11:4)
(BAM-DESORM101)

VLADIMIRDV*, N.K.
Organization, reglmen, treatment, and care in pediatric tubercu-
lous sanatoria. Mad. seetra, 14oskva no. 6:27-31 June 1952.
(CLKL 2-2:3)
1. Head Physician at Children's Tuberculosis Sanatorium. Xalakhov-
ka Station, Moscow Oblast.

VLADIMIROV,_.M.Z,__Cselo Vcherayshe Zhitomirskoy qblasti)
How to 'tring medical care closer to thp rural population.
Felld. i akush. 27 no.1:50-52 Ja 162. (14IRA 15:3)
(MEDICINE, RURAL)

Y N.
of
V,

VIADIMIROVO 11. - " ---
The AN-14 Vmlka aircraft, -Istecky obzor 7 no.2.,4&49
P 163.

VLADIMIROV N -)
Behind the averages. Grazhd.av. 15 no.1001 0 158. (MIRA 11:11)
(Airports)
I

sov/84-58-lo-41/54
AUTHOR.- Vladimirov, N.
TITLEI."~71~ving for Average Figures (Za srednimi tsiframi)
PERIODICAL: Grazhdanekaya aviatsiya, 1948, Nr 10, p 31 (USSR)
ABSTRACT: The author desn.ribes conditions at the Kiyev airport on
1 September 1.958, when the 8-ytionth trwisportation plan appeared
overfulfilled. Ai~tually, however, the first two quarters of 1958
had shown a lass in i*.,ome because of inadequate organization,
and only the seasonal rush during the summer months had made up
for the deficit. In t.be meantime the influx of passenger traffic
had over-taxed airport fa;,531t1e)L~., planes had been running off
schedule .1 and the line's reputation had (%.onsequently been impaired.
The author advosates a stabilization of year-round traffic by
appropriate measures. There Is 1 photograph.
Card 1/1

VLADIKIROV N
The An-:L4 airplane called "Booff. Grazhd. av. 19 no.11:22-13
N 162,, (NIRA 16:1)
(Airplanes)

I. VLADIY1ROvg N.
2. US33R (600)
4. Borunova, Tonta
7. Girl crew chief. Ifol. kolkh. 20, no. 2, 1953.
Mav 1953. Unclassified.
9. Monthly List of Russian Accessions, Library of Congress,

VIADMIROV, if.
Machinery - Models
Creations of young masters, Tekh. ~-olod. 21, No. ). -1953
Nonthly List of Russian Lweessto s ry of Congress, June 1953, Uncl.
TL_, Librr -

B/684/62/000/011/002/002
D036/Dl!4
AUTHOR: Vladimirov, N.
TITLE: The An-14 "Pchelka" aircraft
PERIODICALt Grazhdanskaya aviatsiya, no. 11, 1962, 12-13
TEXT: The AH -14 (An-14) "Pahelkall multipurpose aircraft is de-
scribed. Both passenger and agricultural versioni are available.. The pas-
senger version can seat 7 passe-Zers, has a cruising speed of 190-210 km/hr,
and a range of 600 km. It is primarily designed for routes up to 200 km,
where it can take 9 passengers or a load of 720 kg. With full tanks and a
commercial load of 550 kg,the range can be increased to 720 km. The An-14
is 11-04 m long, 4.25 m high and.has a wing span of 22 m. It has two AM -14
n-.k(AI-14RF) air-cooled radial piston engines developing a total of 600 h.p.
r
The aircraft can fly horizontally on one engine, has a take-off run og 60-
90 m, a landing run of 70-110 m, and a landing speed of 65 km/hr. It can
,land on dirt, sand or snow landing stripe. Ito operating costs are 3-4
times less than those of the MW-l (Mi-1) and MA-4 (Mi-4) helicopters.
There are 2 figures.
Card 1/1

VLADIMIROV, 11.
Outstanding leader. Mast.ugl. 9 no.10:29 0160. (MIRA 31:10)
(Vakhrusbov, Vaailii Vasillevich, 1902-1947)

BOYTSOV, IG., irizh.; XQIHIROV,-N-, inzh.; GROMOV, M., Inzh.
Thorough study of piloting. Rech. transp. 21 no.5:48-49 )kf
162. (AURA 15:5)
(Pilots and pilotage)

VOLIFOSONP S.I.; VLADIMIROV, N.A.
Organize the production of converter-steel articles. Standarti-
zateiis, 26 no.6s52 Je 162. (KRA 15:7)
(Bessemer process)

VIADIMIROV, N.A.
It is necessary to train specialists in standardization.
Standartizatsile, 29 no.7:59-60 Jl 165. (MIRA 18:11)
1. Glavnyy inzh. prwjekta otdela standartizateii Gosudarst-
vennogo naucbno-isi3ledovatellskogo i proyektnogo instituta
neftyanogo mashi-nootroyeniya.

VLADIMIROV, N.A.
Delivery of large chemical equipment. Standartizataiia 28
no.1:54, J& 164. (MIRA 17:1)

VLADIMIROV, N.A., Inzh.
Quality of petrochemical equipment is lowered. Standartizatsiia 29
no.1:14-15 Ja 165. (KMA 18:4)
1. Gosudarstvennyy nauchno-issledovatellskiy i proyektnyy institut
nefteyanogo mashinostroyeniya.

VIADIMIROVO N.A., inzhanarl KAZHINSKIT, B.B.. kandidat fiziko-matematicho-
Improving the production quality in the hydraulic machinery industry.
Standartizatsiia. no.6:66-67 N-D 1560' (MLRA 10:1)
I
1. TSentrallnoye konstruktorskoys byuro gidromashinostsoya.
(Hydraulic machinery-Standards)

V,LADIMIROV,--N.A.
Specifications for the presentation of mechanical drawings are
not needed. Standartizatalia 26 no.8j56-57 Ag f62.
(Mechanical drawing-Standards) (MIRA l5s8)

1, 27dj7_66 EWT(d)/EfiT(M)/EWP(c)/EiVP(v)/T/EWP(t)/EWP(k)/EWP(h)/EVIP(l)
AR6009951 SOURCE CODEs -UR/0137/65/OC
IJP(C) JD
AUTHORSs Vladimirov, N. F.; Galkin, K. F.; Solntsevp_Yu, F. 24
TITLEt Development of programmed electrical operating conditions for the smelting Of
steel in an arc furnace in connection with automation of the process
SOURM Ref. zh. J&Aallurgiya, Abe# 12V347
W SOURCVt Elektrotermiya. Nauchno-tekhn. ob.p vYP- 44, 1965, 64-67
TOPIC TAGS: steel, steel industry, are furnace, smelting furnacpj computer program-
ming, computer/ VU-5086 computer
ABSTRAM A technique is presented for formulating a computer program based on the
electrical operating conditions corresponding to the most economical conversion of I
ton of steel. On the basis of the characteristics of 400 emeltings of various steel
types in a furnace of 3-ton nominal capacityf the correlation dependences of the
furnace operation characteristics--the specific smelting period Ir.and the opecific
electrical power consumption W--on the mean active power P were found in the form
W-A2+BP+CJ'.',
where A,, B1, 01, A2, and C are the coefficients of the regression equation*
D2' 2 1
Calculations of the most economical power permit values.to be determined for the
duration and mean active power for partioular,stages of the smelting period$
Card 1/2 um 669.187t621.365.2

L 27417-66
ACC NRt AR6009951
0 ti - 0 minp P, 1360 kw; 2) t2 40 mint P, 1750 kw; 3) t3 15 minp P3 1500
kw. The calculated values cem be specified an program data for the computer VU-5066a
It is found thatt for oxidized carbon content of 0.30--0-50% and moret the economical
power is independent (with sufficient accuracy) of the oxidized carbon content.
5 figures, I tablo. kIz, RZh Elektroteldmo) (Translation of abstraot)
SUB CODEs 11V,Qq
Card

VLADDUROVP N. M.
263.48 Primeneniye szhatogo vozdukha dlya borlb.; 8 zavisaniyem topliva v Lunkerath,
Zlektr stantali, 1949, No. 8, s. 59.
SO: LETOPIS' NO. 35, 1949

N. I'!
VLADI~11101!) I ~.
Problem of the Ori~?In of Elf,er 41.~Durxlo in "',le -i-&.le Re-yi-,n F~twe,.r the Volu,,~ r~ T:r,21
(resume In Yjzakhatani) Izv. 'd' Yj--z. ser. vfol., 3,21, "'o 1', '1953
I'-c-14,
Critical survey of the literatilre on the origin of Raer mounds. The author
considers that these relief forns, which are Oistributed over n terriroty ad-
joining the delta of the Ural Yivt--i- from the northwest, verc :ormed no a result
of the cunulative action of erosion by vnter currents (in their jiLripheral part
,~-)f the (I~eltas). and by po3itive tect--)n.,.c iur)vemrnts. (FiZhGeol, Yo 1, 1954)
SO: W-31128, 11 Jan 55

VLIMIS2 11VII 1 1.7. Y.
WSR/Hisoallansous Archaeology
,cam 1A I Pub, 123 - 10/13
Authm- - I Fedint -No- Fe,, and Yjadivitat N. M.
Title- Archaeological -finds.in tho-ragion- between, the-.Volga- and the Ural
PerlOdIcal i Vest. AN Kaz, 5Mj 11/2p 75-81j, Feb 1954
Abstract I In the raglan between the Volga and the Ural,, which is flooded in the
opringtimo# there is a slightly higher and &iar area in which relies
of an ancient civilization war(s found, A study of thisse, with a view
to datemining their origin anti date,, lad to the conclusion that the
region was inhabited from the Neolithic era up to the middle of the
fIxet millenium A. Do Illustrations; map.
Institution t
Submitted t

VLADIMIROV. N.M., kandidat goologomineralogichaskikh nauk.
I
Formation of underground waters of Naryn send massife. Vast. AN
Kazakh.SM 11 n0-5:80-84 Mr 154. (MLRA 7:7)
(Naryn sands# Xazakhetan-Water, Underground)
(Water, Underground-laryn sands, Xazakhstan)

10 USSR/Soil Science. Tillage. Land Reclamation, Erosion. J-5
Abe Jour: Ref Zhur-Diol., No 6, 1958, 24825.
Author Uspanov, U.U.; Soko~ov, A.A.; Vjad~
Inst
Title The Soil-Reclamation Character of Lands of the Northern
Precaspia.
Orig Pub: Tr. In-ta pochvoved. AN MzSSR, 1956, 4, 231-241.
Abstract: The character of the lands is listed from the stand-
point of their fitness for irrigated agriculture.
In the Volga-Urals interriver territory, southward
of 490 N. lat., the authors discern the following
soil-reclamation groups of lands. 1. Lands suitable
for irrigated agriculture with the observance of
measures against secondary salinity (light-chestnut
and brown solonetz soils). 2. Soils suitable for
Card 1/3
62

USSR/Soil Science. Tillage. Land Reclamtion. Erosion. J-5
Abs Jour: Ref Zhur-Diol., No 6, 1958, 24825.
ture, possessing high water permeability and in-
clined to deflation). 6. Non-saline soilis of the
old delta of the Urals region. 7. Lands riot suit-
able for irrigated agriculture without fUrLdamental
land-reclamtions, or totally unsuitable (seaside
salt-marshes and seaside mrsh soils).
Card 3/3
63

BOCHKAREV, V.P... kand. geol.-miner. nauk; NIKITINA, L.G... kand.
geol.-miner. naulc; SHAPIRO, S.M., kand. geol.-ininer.
nauk; EYDR-110VA, N.M., at. inzh.; GOLObORODIX0, G.L., inzh.;
PERLIK., G.P.J. inzh.; BAINDALETOV, S.E., kand. geol.-Yiner.
nauk; VLADIMIROV N 14 kand. geol-miner. nauk; SIDYKOV,
A.M., kand. geol.-miner. nauk; MAJYSHEV, Ye.G., ml. nauchn.
sotr.,- BERKALIYEV, N.A., st. inzh.; EYDINOV, Yu.I., at. inzh.;
Y1UKHAY,EDZHAN0Vp S.M.., kand. geol.-miner. nauk; ISfiBAYEV, T.T.,
st. inzh.; MOTOV, Yu.A., inzh.; KOLOTILIN, N.F., kand. geol.-
miner. nauk; LAPIDUS, Zh.D., inzli.,- SHOYMANOVA, M.M., inzh.;
YARF1TM'v r.c%, Jnzh.: BAT?TrT-d---N1ARN1 A.V., kaxdo.miner.
nauk,. (deceased) I MAKMYW
Vp-B.P.p st. inzh.; SATPAYEV, Kole,
akade.mikp;,glav.,!.red.[deceased]; HED0YEV-,cATS., otv. red.;
D14ITROVSKIY, V:I., red.; SMIDJOV, I.S., red.; BRAILOVSKAYA,
M.Ya., red.; KOROLEVA, N.N., red.
[Irtysh-Karaganda Canal; engineering geological ccnditions]
Kanal, Irtysh - Karaganda; inzheneirno-geologicheBkie usloviia.
Alma-Ata, Nauka, 1965. 169 p. (MIRA 18:5)
MV~-cnrd)

VLADINIROV, N.M.
1- 1 -, -
Subsoil waterB in the plains of northeastern Xasakhotan as the seat
available source of a vater supply for nev state farms. Vest.AN
Kazakh,SSR 12 24,7:60-74 J1 156, (Kuu 9:9)
l.Predstavlana akademikom AN &wSSR U.M.Akhmedeaftsym.
(Uzakhatan--Water, Underground)

VI-DIFIR07, -
&I --r. ---.
Fo-at-len of undercroind t-XI"or in the plairs of the
interfluve. Izv,- AN Kazalch. SSR. Sgr.,-e,)I. no.l.:63-74 1-1,01.
OIIR~. 1,.: in 'I,
(Irtysh Valley-Water, Underground)

LI, A.B.
Traditional meetings. Test.AN Kazakb.SSR 16 ao#6.84
Je 160. OCIU 13:7)
(Geology)

POPOV, Viktor Mikhaylovichl DAVYDOVA, Iraida Vasillyevna; VLADIMIROV, N.M.,
red.; VORONINy K.P., tekhn. red@ - -- - --
[Burning of lignite with a high moisture content in the furnaces of
steam boilers] Szhiganie vysokovlazhnykh burykh uglei v topkakh
parovykh kotlov. Moskvaj Gos. energ. izd-vo, 1960. 143 P.
(MIRA Il+:9)
(Lignito) (Furnaces)
I.

VLADIHIROV, N.M., kand. geol.-mineral. nauk
Conjunction of the Ishim and Nura Rivers. Vest. AN Kazakh.
SSR 20 no*6t67-69 Je 164 (MIRA 18:1)

Calculations in the weaving indust-y. ,Iosl-.vp-, Gos. Te,.,I,n. izd-vo, 1924. 1;-'
(A. Serija 2. Fabochaia biblicteka, no. X-2)
Yudin TS1451.V86
1. Textile industry end fabrics - Russia.
2. Weaving - Tables and ready-reckoners.

VLADIMIROV, N- M.
32471. Eksploatatsiya kotlov vysokogo davleniya Shmidt-Gartman. j3lektr. staltsii,
1949, No. 10, 9. 60-~62.
SO: Letopis' Zhumallnykh Statey. Vol. 50, Moskva, 1949

283h6
DorbbA s korroziyey vos du shrrykh 1~)d-~.n-yevatyelyey (-;z ino!~tr. 0.-),Y;; el*~eKtr. -7rlan--~':~
191A9, No ), S. 61-62
So: Letop-13 No. 34

VLALDIMIROV) V.M.j, kand.goologo-mineralogicheskikh nauk-; SYDYKOV, Zh.,
---k~h, ~.ge~logo-mineralogicheskikh nauk; 1-11UKHAMEDZWOV, S.M.,
kaM.goologo.-minera.logicheakikh nauk
'Underground waters of the continental Oligocene in the jurgay
trough and northern Kazakhstan. Sbor.nauch.trud,KazQ4I no.18:
92-101 159. 1 (19M 15:2)
(KazakhsULn,-Water,, Underground)~
.A -

ki6"
POTAPOV, A.A.; VLADIMIROV NX.
Devices for the automatic triggerin of traps and for fractional
gadfly count. Med.paraz.i paraz.bol. no.ltl0c)-110 162.
(14IRA 15:5)
1. Iz entomologicheskogo otdela (zav. - prof.. V.N. Beklemishev)
Instituta meditsinskoy parazitologii i tropicheskoy meditsiny
imeni Ye.I. Martsinovskogo (dir. - prof. P.G. Sergiyev) Mitisterstva
zdravookhranoniya SSSR.
(ENTOMOLOGY-EQUIPIENT A11D STIPPLIES) (HORSEFLIES)

VLADIMIROV, N.P.; KAIJMEIIKOV, II.L.; RA.SSOKAMUN, G.I.; SKUGAREVSKAYA, O.A.
-NONOW.
Experimental studies of the phenomena of electromagnetic field for-w--tion
in a multilayered medium. Izv.AN SSSR Ser.ge ofiz.no.6:708-711 Je 156.
(HLRA 9--q)
1.Akademiya nauk SSSR, Geofizicheskiy institut.
(Terrestrial electricitv)

_17-
AUTHOR: Vladimirov, N. P.
49-9-11/13
TITLE: On certain results of electric prospecting work on an
intersected relief. (0 nekotorykll rezulltatakh
elektrorazvedochnykh rabot na peresechennom rellyefe).
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya Geofizichesicaya,
1957, No.9, PP-1185-1188 (USSR)
ABSTRACT: During a number of years the author of this paper carried
out investigations in mountain regions with the aim of
finding concealed fractures passing predominantly along the
valleys of ravines and consisting of various rocks of
a resistance higher or lower than that of the surrounding
medium. The work was carried out by three-electrode test
equipment, the dimensions of which were commensurate with
the width of the non-uniformity of the ground surface.
The geological interpretation of the obtained results
involved considerable difficulty due to the strong
distorting influence of the relief. Therefore, special
experiments were made on models applicable to concrete
geological and topographical conditions and the results of
these investigations tire described in this paper. The
experimental work was carried out on a section at which the
"~Pdfd 1/3 profiling instrument did not show sharp chani~es of the

49-9-11/13
On certain results of electric prospecting work on an intersected
relief.
apparent electric resistance. On this section models were
built of valleys of various cross sections; along the
valleys vertical seams were placed at various depths made
of materials possessing a low and a very high resistance;
as seams of high resistance,recesses of 2 to 4 m length,
0.2 m width and 1.0 m height were used which were covered
by planks and a layer of earth. As material for the seams
of low resistance, a clayey mixture and pieces of iron
were used as fillers of recesses of the above given
dimensions. The results of the investigations are plotted
in the graphs, Figs. 1-5. These show that in spite of the
complicated shape of the graphs,use of combined profiling
on an intersected relief can yield good results.
Particularly it can be assumed that fixing of maximum
resistivity values in the deepest sections of the
Earth's surface by Aans of three-electrode test set-ups
of small dimensions can be used as an indication of
presence of bodies of high resistance. The position of a
seam of low resistance is determined from the point of
intersection of the curves of combined profiling in the
same way as on a level surface. The results indicate that
Card it is necessary to take into consideration in the

49-9-11/13
On certain results of electric prospecting work on an intersected
relief.
interpretation of graphs not only the characteristic
points but the general character of the ? curves since
taking into consideration of only the chaActeristic
points may lead to a reduction of the usefulness of the
electric method of prospecting. Acknowledgments are
made to'A. N. Tikhonov for his assistance in carrying
out the work.
There are 5 figures and 1 Slavic reference.
SUBMITTED: April 7, 1956.
ASSOCIATION: Ac.Sc. U.S.S.R. Institute of Physics of the Earth.
(Akademiya Nauk SSSR Institut Fiziki Zemli),
AVAILABLE: Library of CongreBs
Card 3/3

I
PH= I BOOK UPWITATION SOV/3502
Akademiya naak SSSR. Institat fiziki zemli
..Metodicheakiye isoledovaniya po gravirazvedke i elaktrorazvedke v Zapadnoy Sibirl.
(Systematic Studies bn Gravitational and Electric Prospecting in Western Siberia)
Moscow,, Izd-vo AN SSSR,, 1959. 59 P. (Series: ItsTrady, Wo. 4) Errata slip
inserted. 1,400 copies printed.
Ed.: A.G. Kalashnikov, Professor; Ed. of Publishing House: Ye.B. Kuznetsova;
Tech. Ed.: Yu.V. Rylina.
POPOSE: The publication is Intended for geophysicists and geologists.. particularly
for those interested in the geological structux*e of Western Siberia from the
point of view of oil and natural gas deposits.
COVERAM This is a symposium of four articles published by the Institute of
PhyBics of the Earth of the AcadenW of Sciences JSSR. The articles deal mainly
with geological prospecting in Western Siberia for oil and natural gas by using
geophysical,methods, such as electrical sounding and investigation of gravita-
tional fielct. References (all Soviet) am given at the end of each article.
Card 1/2

Studies on Method (Cont.)
TANZ OF CONT
SOV/3502
Kalashnikov., A.G. Invastig&tjons Performed by the Eastern Oil
and Natural Gas Expedition in Western Siberia 3
Ohneyersonj, B.L. Investigation of the Gravitational Field of Siberia 8
Enenshteyn, B.S. Long Direct-CUrreat Electrical Soundings by the
Potentionetric Method 22
Vladimirov N.P. Possibilities of Application of the Electric
~L
If ~spec~-iiQ 14-e-t-hod under the Local Conditions of Western Siberia
AVAILUM: Library of Congress
Card 2/2 Tm/ms
5-13-60

66237
S/049/59/000/12/019/027
3.91000 E03?-/E391-
AUTHORS: Vladirairov, N.P and N:Lkiforova, N.N.
TITLE: On the Spectrum 6 ariationn in the Natural Electro-
tic Field of the Earth \-/
PERIODICAL: Izvestiya Akademii nauk SSSR, Seriya geofizicheskaya,
1959, Nr 12, pp 1867 - 1869 (USSR)
ABSTRACT: As a part of the IGY programme the Institute of Physics
of the Earth of the Ac.3c.rJSSR has been engaged in
studying on a large scalc variations in the natural
electromagnetic field of the Earth. The present paper
reports results obtained between 1957 and 1-958 in the
frequency interval 0.3 -- 100 C/S- It wa.-:, found that-,
1) the terrestrial electromagnetic field in this
frequency range has a continuous frequency spectrum;
2) the frequency distribution (luring different times of
day as observed in the Rylsk region of the Kursk district
remained practically the same;
3) the intensity of the variation5 depends both on the
frequency and the time of day. At lwwrer frequencies the
Cardl/2 amplitudes are greater and the Intensity of the variations

-J7
5/049/59/000/12/019/o27
E 0 3 ~-'/ E-*, 9 1
on the Spectrum of Variations it, tile NEktural Zlectromaznetic Field
of the Earth
is slightly greater during tbe day than during the night;
I
11) the average amplititdo of the hor:Lzont."I components
of the electric field was found to be 0.1 mMun. Th o
amplitudes of the magnetic field component are of the
order of 10 ..7_10-8Oe. The presence in the electromagneti-.
field of practically all the frequencies in the region
0.3-100 C/8 confirms the usefulness of the magnetG-
electric method of prosperting using the natural variable
terrestrial magnetic field.
There are 4 figures and 3 Soviet-references,
ASSOCIATION., Akademiya nauk SSFR Institut fizi.ki Zemli
(Institute of Physics of the Earth, Ac.,Sc.USSR)
SUBMITTED: May-ch 30, 1959
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S/049/60/000/01/017/027
E201/B191
AUTHOR: Vladimirov, N.P.-
TITLE: The Possibility of Using the Natural Terrestrial
Electromagnetic Field for Geological Prospecting
PERIODICAL& Izvestiya Akademii nauk SSSR, Seriya. geofizicheskaya,
1960, No 19 PP 139-14-1
TEXTs In 1950 A.N. Tikhonov showed theoretically that it is
possible to*use variations of the natural terrestrial electro-
magnetic field for studies of the electrical properties of deep
layers of the earth's crust (Ref 1). In 1953 Tikhonov's Ideas
were further developed by Cagniard (Ref 2) who pointed out the high
resolving power of the magnetoelectric method. In later work It
was shown that this method can be used to study the geoelectric
s,ections of the portions of the crust under &~ layer with an
infinitely high resistance (Ref 3). The theoretical ideas were
confirmed experimeltally only for very low frequencies (below
0.1 cls, Ref 1+). To find whether h1gher frequencies of the natural
field can be used, a station was developed at the Institute of
Physics of the Earth, Academy of Sclences, USSR. Development began
Card 113

S/049/60/000/01/017/027
R201/E191
The Possibility of Using the Natural Terrestrial Electromagnetit-%
Field for Geological Prospecting
in 1956, and first prototypes were tested under field conditions in
1958. The station consists of three amplifiers, one standard
oscillator and an oscillograph POB-12. The amplifying part consists
of a preamplifier and three channels with filters for three
frequency rangess 0.3-10, 10-100 and 100-1000 c/s. The intrinsic
noise level is not greater than )+ VV. The amplified signals are
fed to a galvanometer GB-IV and recorded by the oscillograph POB-12
on a film moving at the rate of 12-1500 mm/see. Investigations were
carried out in the Ryllsk region of Kursk Province on sand clay
deposits with a crystalline substrate at a, depth of 500 m. This
substrate has, for practical purposesq an infinitely high electrical
resistance. The horizontal components of the electric fields
(Bx~ F7) were recorded by means of electrodes along lines oriented
respectively in the northern and eastern directions. Induction
coils constructed by V.A. Troitskaya and L.N. Baranskiy were used as
pickups for the horizontal components of the magnetic field, Hx
and Hy. The frequency response of these coils is shown In Fig 1.
Card 2/3

S/049/60/000/01/017/027
E201/E191
The Possibility of Using the Natural Terrestrial Electromagnetic
Field for Geological Prospecting
The largest number of electromagnetic oscillations was recorded at
frequencies of 6-8 and 70-80 c/s. The apparent impedancg, ()K,
was found from: n 11~
9K = (1/5f)(Ex/Hy)". DR. = 1/5f (EY/HX-J'-~ (a.)
1~
where f is the frequency. Although the accuracy was not high,
(� 50% for 9K) the values of oy, (Fig 2) gave the depth of the'
crystalline substrate as 450 mj this agrees quite well with 500 m
found by other methods. The results obtained show great promise,
provided the apparatus (especially the magnet.1c, pickup ccils) ale
improved. Lcknowledgements are made to A.N. Tikhonov and k.I.
Zaborovskiy for their help.
There are 2 figures and 4 referencess 3 Soviet and 1 English.
ASSOCIATIONs Akademiyanauk SSSR, Institut fiziki zemli
(Institute of Physics of the Earth, Acad.Sci. USSR)
SUBMITTED: June 20, 19 59
Card 3/3

ajq/0
-)5()IL
S/649/60/000/011/005/012
j, 2,17 1 ~"l
-UT11uh.-A Yladijull-ov, N. P., ItIld 11'011~.1111.ov' hl~ V.,
TITLE: On the resolving power of the magneto-telluric method
PERIODICAL: Akademiya nauk SSSH. Izvestiya. Seriya geofizicheakaya,
no. 11, 1960) 1598-1600
TEXT: The authors investigate theoretical possibilities of using the
magneto-telluric method, based on geomagnetic pulsations, when studying
geological profiles consisting of three layers of thickness h,, h 21 h3
C- and resistivity The authors develop a for-
P I P2f P3 ~ C~o 0
mula for calculating apparent-resiStiTity curves
1 + 2e-p (A cos - B sin + (A 2 + B2 213 (6)
PT/Pl 1-2e_~(Acos -Bain +(A 2 + B2) e-2
Card l/#
_~7

2~5.04
S/049/60/000/011/005/012
On the resolving..~ D247/D305
and give some examples of graphs by different parameters (Fig. 2, Fig~ 3)~
~k 7. P 2/ P, = 2A; 4.0 and v ~ h 2/h, - 1.0; 2.0; 3.0; M; 9.0 . Every
cu rv,- P T corresponds to the ratio 19PT IP1 - 1 g J_T where T--
period of oscillation by constant parameters ~k and v of the geological
cross section, A comparison with the curves obtained by vertical electri-
cal sounding is given in Fig. 3. Interpretation of the field data matches
the experimental curve (apparent-resistivity vs period) with a stan-
dardized theoretical curve of the same nature. The displacement of the ~'Y
0 point of the standard curve from the abscissa corresponds to the resis-
tivity of the first layer and from the ordinate with the value 1i I/ '/F1 .
After calculating the longitudinal conductivity S I of the first layer,
the conductivity of the second layer can be computed according to the
formula S 2 ~ SI' V/P_ where P_ and 1i -- moduli of theoretical curve,
Depth of the third layer can be computed according to the formula
Card 24-3

On the resolving...
2~504
S/049/60/000/011/005/012
D247/D305
H - h1 + h2 ' h1 + P02 a The authors conclude that magneto- tel luric
sounding is advantageous only if the layers are of sufficient thickness.
There are 4 figures and 2 Soviet-bloc references.
ASSOCIATION: Akademiya, nauk SSS119 inatitut fiziki zemli (Academy of
Scienceaq Institute of Physics of the Earth)
SUBMITTEDt May 69 1960
Fig. 2. Graphs of magneto-telluric sounding PT' Pallet A - 2 - 00
Fig. 3. Curves of magneto-telluric sounding and of vertical electrical
sounding. Pallet A - 4 - CX3
Card 3/0

AUTHORS:
TITLE:
PERIODICAL:
2~2 1
0
sl16qAfl 00/007/079/149
D228/D307
An, V. A.0 Vladimirov, N. P.0 Yermolenko, Yu. A. and
$tation for measuring variations of the earth's na-
tural electromagnetic field in the range 0.5-1000 c/o
Referativnyy zhurnal, Geofizika, no. 7, 1962, 34j ab-
stract 7A221 (V sb. Vopr. teorii i praktiki elektro-.
metrii, M., AN SSSR, 1961, 56-68)
TEXT: Equipment with a low noise level has been created to measure
electromagnetic field variations with an amplitude to 10 P_v in the
magnetotelluric method. The station's frequency range of 0.5 -
1000 ols is broken into three bandB-.'0.5 - 10, 10 - 100, and 100
1000 c/s. The frequency characteristic of each band is flat. The
amplifiers of each channel are charged by nOb-42(POB-12) loop-os-
cillograph galvanometers. Three components -- the horizontal and
the vertical for the magnetic field, and the horizontal for the
-electrib field -- can be recorded simultaneously. The oscillograph's
Card 1/2

S/169/62/000/007/079/149
Station for measuring D228/D307
sensitivity is not below 20 mm//Iv on each band. There are tube am-
olifiers with a set of filterB and output attenuators that weaken
!he signal by'100-fold. Provision is made for the possibility of
visually controlling the signal from the scale of a H-ZY (1-1-24)
ammeter. In the station there is a low-frequency calibration 6ene-
rator, permitting the supply to the amplifiers' inputs of sinusoi-
dal voltage, of a definite amplitude and frequency. The results of
testing the station in different areas confirm that for proepe,;t-
ing purposes it is expedient to study the natural electromagn Ac
field in the range 0.5 - 1000 ols. Z Abstracterts note: Complr~te
translation--7
7-
Gard 2/2,

L
7'~L /0 D226YD306
AUTHORS: Vladimirov, N.P., and Nikiforova, N.N.
TITLE: A method of interpreting curves of magnet6-telluric
sounding
PERIODICAL: Akademiya nauk SSSR. Seriya geofizicheskaya. Izvestiya,
no. 1y 1961# 111 - 113
TEXT: A number of investigations into the development of a magne-
to-telluric method of prospecting based on variations in the na-
tural electric field of the Earth h,ave recently been carried outs
A method of magneto-telluric profiling, developed by M.N. Berdi-
chevskiy (Refo 1: Teoreticheskiye predposylki magnitotelluriches-
kogo profiliroveniya, Izv- Akad. Nauk*SSSRj ser. Geofiz., No. 7,
1.959)j has been introduced, in which field vartations with a fre-
quency of less than o.1 hertz are used for studying the relief of
the buried basement at depths of several kilometers. The develop-
ment of a method of magneto-telluric sounding using frequencies
23459
S/04 61/000/001/004/008
Card 1/6

23459
S/049/61/000/001/004/006
A method of interpreting ... D226/D306
above 0.1 hertz and permitting both the study of the basement and
the differentiation of the overlying sedimentary rocks is of much
interest. This type of work entails considerable difficulties of
an equ*4mental and procedural charactero In the last two years de-
finite success lias been achieved in developing a method of magneto-
telluric sounding at the Institut fiziki.zemli AN SSSR (Institute
of Physics of the Earth AS USSR) and the first experimental curves
have been obtained, In this connection a procedure for interpret-
ing experimental data became necessary, and the authors describe
in detail this method where the determination of profile parame-
ters is based on the comparison of experimental curves for the
apparent resistance ,p and the impedance phases e with the corres-
ponding theoretical carves. Each theoretical curve corresponds to
th, dependence of 19 PT/Pl or 6 on 1g Vf for the two constant pro-
file parameters g and D. The curves for the same values of 44,(or
,0) are usually placed on a single form, the parameter v(or~k)
being indicated on the corresponding curve. The experimental cur-
ves are constructed on the same scale as the theoretical curves,
Card 2/6

23459
S/049/61/000/00li/004/008
A method of interpreting
lg P,, or 6 being plotted on the Y-axis and 1g, On.- 46. X-axi a. ~j
Such a construction enables the same interpretation procedures em-
ployed in the method of direct ourrentresistanoe to be utilized.
When interpreting the magneto-telluric sounding cu.-ves the questi-
on of the rational selection of the point of origin of the theore-
tical pallets is a basic matter of principle. It is expedient to
choose the position of the point of origin in such a way that the
upper layer parameters may be directly determined during the in-
terpretationt as is the case in the method of direct current re-
sistancep a fact which a number of authors have failed to take in-
to account. Some research workers choose as -the cross a point on
the X-axis where the ooordinate of T = 6#4 seconds -- the Point A
of Le Oagniard (Ref. 31 Basic theory of the magneto-tellurio me-
thod of geophysical prospecting Geophys.p 18t No. 31 1953). This
is to some extent justifiable since all two-layer curves of a
differing modulus intersect at the given point. Three-layer curves
with a small modulus for v# howeverp do not pass through Point At
so there are insufficient grounds for plaoing the oroas at this
Oard 316

23459
8/049/61/000/001/004/008
A method of interpreting at, D226/D306-
point if one takes into account that first layer parameters can
only be indirectly found by means of this point after certain calcu-
lations. The authors explain their method of interpreting P,, (ap-
parent resistance) curves, then interpret such a curve obtained in
1959 on the northern rim of the Dnepr-Donets basin. Pig* 3 repre-
sents the comparison of an experimental and theoretical curve (,a=
- 3s j = 4). The geology of the study area comprises Pre-CambriEn
metamorphic and sedimentary rocks omurring at.e. depth of about 900
m and sedimentary rocks largely consisting of argillaceous and are-
naceous formations. According to the data of vertical electric
sounding two electric horizons are distinguished in the sedimenta-
ry complex with resistances P, = 30 and P2 = 50 ohm.m. The results
of this interpretation of the curve are in good agreement witb geo-
logic and geophysical notions on the structure of the study area,
and corroborate theoretical considerations about the possible use
of variations in the natural electromagnetic 'field of the Earth
with freauencies above 0.5 hertz for geologic prospecting. There
Card 4/~,

23459
S/049/61/000/001/004/008
A method of interpreting ... D226/D306
are 3 figures and 4 references: 3 Soviet-bloc and 1 non-Soviet-
bloc. The reference to the English-language publication reads as
follows: L. Cagniardq Basic theory of the magneto-telluric method
of geophysical prospecting. Geophys., 18, No. 3, 1953.
ASSOCIATION: Akademiya Nauk SSSR, institut fiziki zemli (Academy
of Sciences USSR, Institute of Physics of the Earth)
SUBMITTED: June 299 1960
Card 5/6

KOWAKOV P M.V. VIADIM.IROV N.P.
Equivalency of magnetotelluric sounding curves. IZV&M. SSS'-R-
Ser. geofiz. no.4:541+-552 AP 161o (MIRA 14:3)
1. Institut, fiziki Zemij.AN SSSR.
(Electromagnetic prospecting)

30281
S/049/61/000/011/003/005
3 D239/D303
AUTHORS: V1 ~ov' N. P., and ~-n, V. A.
TITLE: On methods of processing geomagnetic oscillograms
PERIODICAL: Akademiya nauk SSSR. Izvestiya. Seriya geofiziches-
kaya, no. 11, 1961, 1649-1654
TEXT: This article is a discursive commentary, pointing out some
of the difficulties and pleading for more work to be done. Basic--
ally the problem is to determine the effective electrical impedance
of the earth at the station along two directions at right angles,
defined by
PT = 7f
Ex 2 2
f
H yl f PT f I HX1
(1)
where PT is in ohm.m., Ex, E y are in mV/km and H x, Hy are inrunits.
Card 1/ 3

30281
S/04 61/000/011/003/005
On methods of processing D239YD303
The processing of the oscillograms from the four (or five, if the
vertical component be measured as well) receivers involves determlln-
ing the frequencies and amplitudes of correlated trains of oscilla-
tions. The authors favor the use of arithmetic mean amplitudes ra-
ther than maximum excursions. One source of error is the assumption
that the voltage picked up from the geoelectromagnetic field is 14L-.
nearly proportional to the length of 'the receiving horizontal aer~__.
al. Data are given to illustrate a case where this is not so - pre-
sumably due to a local inhomogeneity in the surface layers. Another
source of error is the uncertainty in the frequency, which may
amount to +- '10%. Improvements in the apparatus are called for here.
Since the Horizontal geoelectromagnetic field is often elliptically
polarized, the use of a smoothed ellipse drawn through the pointo
constructed from the observations leads to greater precision. What
is suggested is that the major and minor axes of this ellipse are
used as axes of reference and the impedances ZaV Zb defined by
Ea /Ha and Eb/Hb determined separately for each observation. The
mean value of __ can be quite a precise measure. Its dependence
YZaZb
Card 2/3

On methods of processing
30231
S/04 61/000/011/003/00,:
D239YD303
upon frequency (the range under consideration is from 0.5 -- 100
c1s) can be usefully studied.' There are 6 figures, 1 table and
Soviet-bloc references.
ASSOCIATION: Akademiya nauk SSSR, Institut fiziki zemli (Academy
of Sciences of the USSR, Institute of Physics of the
Earth)
SUBMITTED: February 21, 1961
Card 3/3

S11691631000100110551062
2'18/D307
AUTHORS: Vladimirov, N.P. and An, V.A.
TITLE: The magnetotelluric method of prospecting
PERIODICAL: Referativnyy zhurnal, Geofizika, no. 1, 1963, 30,
abstract M62 (Razvedka i okhrana nedr, 1962, no@
6, 34-37)
TEXT: Brief information is given about (1) an apparatus
J for studying variations in the electromagnetic field of the earth
in the frequency range 0.5 - 1000 cps, -(2) field detectors (elec-
trodes and coils with ferrite or permalloy cores), (3) the field
frequency spectrum, (4) the dependence of variations on the geolog-
ical structure of the locality, and (5) the accuracy of the measure-*
ments. Two magnetotelluric soundings are reported,for the Dneper-
Donets basin together with their interpretation and an example of
a record of the variation.
Z-Abstracter's note: Complete translationj
Card-

VLALDIHIROV# W.P.; UZYKENOVA, V. G.
Strueture of the earth's natural electromagnetic field in the
freveray ranke of P*5-100 o.p.s. Izve'AN SSSR* Ser*geofize
no.lPt1368-1374 0 162%6 (MIRA 16:2)
1* Ustitut, fiziki Zmli AN SSSR.
(MaOetiamv Terrestrial) (Earth cmTental

8/049/62/000/011/006/oo6
S.W/O D200308
-AUT11ORt Vladimirovt N.P.
TITLEs Induction magnetometers used in studies of
the terrestrial magnetic field
PERIODICAL: Akademiya liauk SSSR. Izve8tiya. Seriya geo-
fizicheskaya, no. lit 1962, 1645 - 1650
TEXT: Magnetometers intended for recording micro-
variations of the terrestrial field (0.1 - 100 c/o, intensities
down to 10-31) are described. Each magnetometer consisted of
five Plexiglas formers of 17 cm diameter wound with 100 000 -
500 000 turns of wire and placed in a.cylindrical casing. The
cores were either ferrite rods (1 x 2 x 10 cm) or Permalloy
sheets of type H - 791M (N - 79NN). Different magnetometers
with separate amplifiers (flat frequency response) were used
for the 0.1 - 10 and 10 - 100 c/i ranges. Field tests carried
out in 1960-61 showed that a magnetometer with 140tooo turns was
suitable for the iO - 100.c/o range, while for 0-5 - 10 0/8 a
Card 1/2

KOLMAKOV, M.V.; VLADIMIROV, N.P.
Equivalence limits of curves of magnetotelluric profilinsIr
Razved.i okh.nedr. 28 no.llt53-55 N 162. (MIRA 15:12)
1. Institut fiziki Zemli J6N SSSR.
(Electromagnetic prospecting)

-VLADIMIRCIV) N. F.; KRYIPI, S. 1-1.
Characteristics of the m1crowriations of
magnetic field. Izv. AN SSSR. zer. geofiz.
a natural electro-
no.6:872-882 Je 164.
(MIIIA 17-7)
1. InBtitut fizikt Zemli &N SSSR.

ACCESSION NR: AP4041181 8/0049/64/000/006/0872/0882
AUTHOR: Vladimirov, N. P., Kry*lov, S. M.
TITLE: Characteristics of the microvariations of the natural electromagnetic field
SOURCE: AN SSSR. Izv. Soriya geofizichoskaya, no. 6, 1964, 872-882
TOPIC TAGS: geology, goologichl prospecting, geoelectrio prospecting, magnototelluric
prospecting, natural electromagnetic field, gooelectricity
ABSTRACT: 71ils article gives the charactorititica of the cakthlu natural cloctrornagnelic
field In the range 0.3-100 cps on the basis of investigations rdade in 1958-19G2 by the
Institut fizild Zerni AN SSSR (Institute of Geophysics). The chlaracterlstic microvariations
of the natural field with a frequency of 0. 3-2. 0 and 6-10 cpsare those which are usually used
for the solution of problems In structural geology; the following conclusions were therefore
drawn for this range. The strength of the clectric field is highly dopendent qn the geoolectric
profile: the greater the rosistivIty of the rocka inaking up the profile, tho higher the
amplitude of the electric field. During field work carried out under varlous geological and
geophysical conditions, the authors recorded a change In the mean amplitude of the field
Card 1/2

ACCESSION NR: AP4041181
In the range from 6 to 10 cps which amounted to two orders of magnitude (from 0. 045 to
5. 0 mv/km). No clear dependence of the strength of the horizontal component of the
magnetic field H on the character of the geoelectric.profilo was discovered. The mean 1
strength ll In the range 6-10 cps was everywhere 0. 007 Y. The strength of the components
of the electromagnetic field is dependent on frequency. In the range 0. 3- 10 cps an in- i
crease in frequency Is accompanied by a decrease In field intensity. The components of the
electromagnetic field in the range 0. 3-Z. 0 cps-have a phase shift which is not constant in
time, this being evidence of the complex character of polarization of the electromagnetic
wave. The great scattering in the Impedance values can be attributed to the fact that in th~
processing of magnetotelluric oscillograms it Is customary to use formulas which do not
take Into account the peculiarities of the structure of the natural field under specific
geological conditions. Orig. art. has: 1 formula, 6 figures and 3 tables.
ASSOCIATION: Institut fizild Zemi, Akadomiya nauk BSSR (Institute of Geophyal
Cal
MR Academy of Sciences)
SUBbUTTEDt 01JUI63 ENCL-. 00
SUB CODE: ES Wo RE r SM. 00
5 OTHERt 007
2/2
C-ard

VLADIFJROV, Rikolay Petrovich; ST-CHEFErOV, Ivan Alekqeyevich;
BELOGLAZOV., Vasiliy Ivanovich; PUSHKAREV, Leonid Vasillyevich;
. h 0 In A
ZERNOV, S.A., Imb., retrement; AGUO"', '.D., kap'tan,
retsenzent; FIATLIN, A.A.,kapitan, retnen7ent; ~AKULPN, ?.F.,
kapitan, retsenzent; MOSUU, S.V., kapitan-nastavrik,
retsenzent; POFOCHKIN, Ye.14., red.; MAICWSHINA, A.N., red.
[Special sailing directions for the Volga-Kama and Don River
basins; Moscow Canal, Volga River from the Ivankovo Hydraulic
Development Complex to Bertyull, Kama F4 ver from the city of
Perm to its estuary, Vol-a-Don Canal, T31mlyansk Reservoir, and
the Don River from the TJ_ml~yansk Rensei4oir to the city of
Rostov] Spetslotsiia Vo1zhsko-Kamskogo i Donskogo basseinov; ka-
nal im. Moskvy, r. Volga ot Ivan1kovskogo gidrouzla do nas.
p. Bertiull, r. Kama ot g. Perm' do ustlia, Volgo-Donskoi kanal
im. V.I.Lenina, TSimlianskoe vodokhranilishche i r. Don ot
TSimlianskogo vodokhranilishcha do g.Rostov. Moskva, Trm sport,
1964. 288 p. (MIRA 17:10)

VIAD114IROV N,P.
'Ajnq characteristics of c-' t~,-.e -at--Lral e2ectrorag-
netic field of the earth. Izv. AN SS.3R, F.l,.,. teem. no.6:67-90 165.
(ITMA 18:7)
1. Institut fiziki Zeruli AN SSSR.

L,-6CV4
-65
3
JACCESSION UR: APS018289
found that the varlitlon T-,Y s, r with changes in the horizontal
rrckq, such

jkQW=j, N. F.,u ANO V. A.
MU-NWM&
Magnetotelluric method of prospecting. Razved. i okh. nedr 28
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----- -
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ifii
S/169/62/000/001/067/083
D228/D302
AUTHORS: Alltshjler, V. M. and Ylad -
__ -J-m~ _O- A ~-
TITLE: Calculating the semidiurnal tide (M 2) in the Baffin
Sea and the Davies Strait by G. V. Polukarov's metbod
PERIODICAL: Referativnyy zhurnal, Geofizika, no. 1, 1962, 11-18j
abstract M06 (Tr. Gos. okeanogr. in-ta, no. 6~,
19619 112-117)
TEXT: The calculation was made for 39 points on a square grid
with a side length of 60 miles. The map of the cotidal hours agr~-~es
well with similar, previously constructed maps. This area's semi-
diurnal waves are formed not only by the Atlantic tidal wave but
are even induced, too, by the wave from the Arctic Ocean. Shore
reflection has a great influence on the propagation of the M -9
wave. In the narrow part of the Davies Strait the wave's velocity
diminishes markedly, but its amplitude grows considerably. In the
north of the Baffin Sea the wave's amplitude also increases in
Card 1/2