SCIENTIFIC ABSTRACT TYURMINA, L.O. - TYURINA, YE.V.

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• Collection: Scientific Abstracts
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• Document Page Count: 47
• Document Creation Date: November 2, 2016
• Document Release Date: August 31, 2001
• Sequence Number: 10
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

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S116916 1/000/'008/'043/'053
A006/AI01
AUTHORS, Ben'kova, N.P.,I_T_Yurmi~~L-O~-
TITIZ: Analytical concept of the geomagnetic field on the Soviet Union
territory for the 1958 -epoch
PMODICAL: Referativnyy zhurnal. Geofizika, no. 8, 1961, -34, abstract 8G240
("Geomagnetizm i aeronomiya7, 1961, v. 1, no. 1, 87 - 103)
TEXT; For the 1958 epoch, the geomagnetic field on the USSR territory is
represented with the aid of coefficients of expansion of the geomagnetic poten-
tial in series in spheric harmonies. The results are compared with charts. A
comparison is made of data pertaining to the East-Siberian zone of the global
anomaly for a series of epochs, and secular changes of this anomaly are discus-
sed. The authors' summary
[Abstracter's note: Complete translation]
Card 1/1

TnWM L. 0.) FRYAZINOV,, I. V... ZHUZGOV) L. X.: PUSHKOV~ N. V. DOLGINUV; S~,. 57.1.
"Sow of the Constant Geomagnetic Field Measurements Carried out
from Sputnik III over the TexTitor7 of the USSR"
Soviet Papers Presented at Plenary Meetings of Conmittee on Space Research
(COSPAR) arid Third International Space Synosium, Washington, D. C.,
23 APr - 9 May 62.

S/203/62/002/004/003/018
1046/1242
A Mr I ' 0 R Bent kovn P. . and Tyurraina, L. 0.
T rL LE Tho magnotic field of the equatorial current
?ERIODICAL: Geomgnetizm I. acronomiya, vo2, no.4, 1962, 635-641
TEXT: r.11ho authors cale)ilate tho Yr4agnetic field of the equatorial
current ring for any point on the surfade of the oarth asnuming
that the current flows along s surfqce shaped like the force lines
of the dipole field (r = a sin2l?) and positioned symmetricall-y
with respect to the oquator. Agreement between the theoretical re-
sults and the experimentnl latitude distribution of the geomagnetic
Dst variation is best obtained for* a current ring with a = gReprttL
2V). The mgnetie nonont
and for current density j = jr,(b + c cos ,
of the ring (cAlculated for the Tragnetic storyn of June 1, 1958),
.7.1 = (4-5).1025 CGSVI agrees with the results of other authors (Ref.
5: Z.H.Vest'n, The geomgnat'c field, its deacription and analy31S.
.!Isshington,'1947). (Ref. 9:'LS.I.Akasofu, S.Cain, and S.Chnpman.
Card 1/2

S/203/62/002/004/003/018
1046/1242
The rr-ignetic field of...
J.Geophys.'Res., 1061, 66, :~o..12, 4013-4026). The conclusion3 con-
firm the-hypothesis. thrt the extraionospheric current flows in two
radiation belts w1th a = 3-5 R (the outer belt) and a = 9-10 R (the
outermost, or third bait). ~_'here are 2 figures and 3 tables.
ASSOC,IATION: Institut zeinnogo magnetizma, ionosfery i rasproastra-
neniya radiovoln AN SSSR (Institute of Terrestrial
S
,Magnetism, the Ionosphere, Find Propagation of Radio
Waves, IM: USZ;'H)
SUMITTED: April 17, 1962
Card 2/2

ADAM, N.V.; BENIKOVA, N.P.; ORLOV, V.P.; OSIPGV, N.K.; WUPHINA, L.O.
Spherical analysis of the constant magnetic field for the epochs
1955 and 1958. Geomag. i aer. 2 no.5:949-962 S-0 162.
(MIRA 15:10)
1. Institut zemnogo magnetizma, ionosfery i rasprostraneniya
radiovoln Sibirskogo otdeleniya AN SSSR i Institut matematiki
s vychislitel'nym tsentrom Sibirskogo otdeleniya AN SSSR.
(Magnetism., Terrestrial)

4h449
S/203/62/002,/006/004/020
A160/A101
AUTHORS: Dolginov, Sh. Sh., Zhuzgov, L. N., Pushkov, N. V., Tyurmina, L. 0.$
Fryazinov, I. V.
TITLE: Some results of measuring the constant magnetic field of the Earth
with the third artificial sputnik of the Earth above the territory'
of the USSR
PERIODICAL: Geomagnetizm i aeronomiya, v. 2, n6. C., 1962, 1061 - 1075
TEXTs The author presents some results of measuring the constant magnetic
field of the Earth with the help of the third Soviet sputnik above the territory
of the USSR from May to June 1958. A brief descripti6n is given of the metro-
logical properties of the used equipment and of the method of eliminating mag-
netic board Poises from the sputnik magnetograms. It was determined that, the
deviation may be represented by three harmonics whose mean amplitude values
equal ITJM - 1,500, U2m = 500 and UF = 200 7. A comparison of the measured
values of the geomagnetic field intensities with the values of this intensity
Permitted to establish their agreement within the limits-of.0.1 - 1% above a
Card 1/2

S/203/6;~/002/006/004/020
Some results of measuring the ... A160/A1O1
major part of the USSR territoryi'including the Siberian world magnetic anomaly.
The conclusion is illustrated by a limited number of typical magnetograins ob-
tained on the segments of the trajectories traversing tho whole territory of
the USSR. The material yielded'by the magnetic investigations with the third
Soviet sputnik permits to fully determine the possibilities of carrying out sp~_
cial magnetic experiments. 1) The main harmonics of the Gaussian serie s can be
determined with a precision of 0.1%. 2) With the help of a long-lasting sputnik
the real existence of the exterior sources of the magnetic field has to be found
out, not taking into consideration the theoretical valuei of the field, computed
from the ground data. 3) Regular work should be done on the secular variation
of the geomagnetic field. 4) In order to obtain highly accurate data, the re-
quirements for the complex of auxiliary equipment should be deter-mined. There
are 12 figures and 1 table.
ASSOCIATIONt Institut zemnogo magnetizma, ionosfery i rasprostraneniya radiovoln
AN SSSR (Institute of Terrestrial Magnetism, Ionosphere and Radio
Wave Propagation, AS USSR)
SUBMITTM: July 10, 1962
Card 2/2

A, P,v.
ADAW,- N-.V-., BWO
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TrM-MU, L.O.
'CRIlculated magnatio field of
the ra~ th, (USSR)
report
ulullted for the 4t~ Internetione, 3pgc* Science SYEPONIUR (OOSPAR)
"Areev, 63

ADAM, N.V.; HENSIKOVA, N.P.; ORLOV, V.P.; OSIPOV, N.K.; TYURMINA, L.O.
Spherical analysis of the permanent geomagaetic field and
secular variation. Geomag. i aer. 3 no.2:336-353 Mr-Ap 163.
(KUU 17: 2)
1. Institut zemnogo magnetizma, ionosfery i rasprostraneniya
radiovoln AN SSSR i Institut matematiki s vychislitellnym
tsentrom Sibirskogo otdeleniya AN SSSR.

T L
ADAM, N.V,,- BENIKOVA, N.P.; ORLOV,, V.P.; OSIPCIV., N.K.; -.0.
Spherical %nalysp of the constant geomagnetic field for the period
195-5 through 1901. Ft. 2. Geomag. i aer. 3 no.l.-IZ-3.26 Ja-F 163.
(MI RA 16
I* Im titut zemnogo magnetizma, ionosfery i rasprostraneniya radiovoln
AN SSSR i Institut matematiki s vyphislitellnym tsentrom Sibirskogo
otdoleniya AN SSSR.
(Magnetism, Terrestrial)

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ADAM, N.V.; BENIKOV4, N.P.; ORWV, V.P.; OSIPOV, N.K.; TYUMCNA, L.O.
1--l"
Synthesis of the geomagnetic field according to the coefficients
of spherinal andlysis. Geomag. i aer. 4 no.1:151-160 Ja-F'64.
(MIRA 17:2)
1. Institut zemnogo magnetizma, ionosfery i rasprostraneniya
radiovoln AN SSSR i Institut matematiki a vychislitellnym
tsentrom Sibirskogo otdeleniya AN SSSR.

ACCESSION NR: AP4043254 8/0203/64iOO4/004/0748/0752
AUTHOR: Adam, N. V., Baulkova, N. P.,'Orlov, V. -P., Ov1pov, N. K. , Tyurm", L. OJ
TITLE: Analytical representation of secular variation
SOURCE: Geomagnetizm i aeronomiya, v. 4, no. 4, 1964, 748-762
TOPIC TAGS: geomagnetism, geomagnetic field, geomagnetic field secular variation,
secular variation
i. ABSTRACT: A study has been made showing that an analytical representation of the
.1 secular variation (SV) of the geomagnetic field based on six harmonics is adeqa;%te for
representation of world SV with the same degree of accurary as world maps of SV compiled
directly from observations at magnetic observatories; it is also shown that tho analydcal
method can be used for comp'lling maps of SV. The synthesis of SV maps was'accomplished
using a grid.with grid lines spaced 5* apart in longitude. The grid-Was somewhat more open'
to the south of 600S and to the north or 70*N. "The values S X and 9 Y were derived using the
1: mean coefficients Sgn m and 6 h. m, 'computed from S X and SY in order to exclude the
potential-free part. In accordance with the assumption of the existence of an.outer part
the values 4 Z were computed using S Jmn and S Kmn. The quality of the analytical maps
was judged by compilin mays of the dMerences between-the initha values SX, 4)r
T711

ACCESSION NR: "4043254
and S Z used for analysis and the values obtained as -a result of the synthesis. Figures I
2 the Enclosure show the IMMAN (Institute of Terrestrial Magnetism, the Iono-
s ar:f
d
an Radio Wave Propagation) maps of A S X and 4 S Y. The A values are given I
1
ip gammas; positive values arerepresented by solid and negative values by dashed isolines.
The ma2dmum discrepancies between the initial and new maps, +30Y , was in the southern
hemisphere; in the northern hemisphere theydid not exceed +10-Y . The discrepancies in
X, S Y and S Z on the IZMIRAN SV world maps do not have a regular pattern, except
that in the southern hemisphere A J* Y Is generally pegative. The values 44X'~nd A 4 Y
are of the order of +6Y and only in the south polar ca~ do they attain 40Y for 6 X and 20Y I
f6r SY. For A f ZDiere is an increase to +15), In the Atlantic and a sharp increase to 60Y
-in the high latitudes of the southern hemispKere. The IZMMIAN maps also were compared
~with the values SX, SY and SZ directly at 53 magnetic observatories; the mean discrep-
ancy for the three elements was �9T *. The analytical method is thus as accurate as graphic,
methods, but doeEi not involve thi'subjectivism. involved in use of the latter. However,
graphic and analytical methods could be combined; the first is beat for areas f6t which little
data Is available and the sqoond is best for characterizing regians of rapid sepular varia-
fiens. Orig. art. has-. 3 figures i~nd 2 tables.

ACCESSION NR: AP4043254.
ASSOCIATION. Institut zemnogo magnetizma, lonosfM i rasprostranonlya radiovol-n AN
SSSR (Institute of Terrestrial Magnetism, the Ionosphere and Radio Wave Propagation, AN
SSSR); Institutmatematiki a vy*chislitellnym tsentrom, 80 AN SSSR (Institute of Mathematics
and the Computation Center, SO AN SSSR)
SUBMITTED: 04Feb64 ENCL: 04
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ADAM, N.V.; OSIPOVY N.K.; TfUle-IINA L.O.- SILLYAKHTINA, A.P.
Spherical hanv)nIc anrilyals of thc. world vilrWWr, f("..
epoch. Goomag. i aer. 4 no.6:1-130-1131 N-D 164'
'PA 18.-l)
1. Institut zemnago magnetizma, ionosf,,,ry i rasprostranend.ya radiovolln
AN SSSR i Institut matematiki s vychislitellnym tsentrom SIbLrskego
otdeleniya AN SSSR.

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MIN

L 231~6-66 E',IT(1)/.FC( GW
Acc !.-: Ap6oo6677 SOURGE CODEs UR/0203/66/oo6/ool/oi7q/oi8i
AUTHORSt Benlkova,, N. P,; Adam, N. V.,- TVn-mina,,-L.
ORG: Institute of Terrestrial M etis . the lono Radic.
Waves AN SSSR (Inatitut zemnogo magnetizma, ionosfery i rasprostranerdya radiovoln
AN SSSR)
TITLEt On tho accuracy of analyzing worldwide njgRqtjq maps of 1960
SOUWEi Gaomagnatizm i aeronomiya., ve 6, no, 11 1966, 179-161
TOPIC TAGSz goomagnetic fieldt harmonic analysis, research ship
AB,STRACT: Distribution of total magnetic fiald was computed through coefficients
of spherical harmonic analyses for lV60* Different combinations of spherical-
harmonic coefficients were used to compute for each of the three rectangular
coordinates of the fioldi Theoretical values of the field were then computed
according to each set of coefficients. To evaluate the accuracy of this approach
by spherical harmonies, comparieons were made betwean the values obtained here
with values Uken from worldwide magnstic, maps for 1960. Checku were made or every
UDCt
550.389

L 23136-66
1 ACC h7tv AP6006677
50, Of at 150 of 16
itude and rigitude, Comparisons were also made with data from
~the~Zary* for the Pacificp Indian and Atlantic Ocean,3 for the period 1957-63,
:-,.I redu6ed-to-1960, Cheeks'were-made at 372 points, The theoretical values were
also compared with average values from magnetic obsf~rvatoSies. Variation in
field (for horizontal component) was computed to be 260 60 was meaeured as 2861
on the Zarya, and.290,y at land-observatories. The difference between computed
values and the Zarya values for the points of comparison are plotted on a world
mapp and isopleths of d:L-Cference are drawn. Orig, art. bass 1 figure and 1
tdble4
SUB COM OB/ SUBM DALTSt 06JtLl65/ ORIG REF# 001

L 07h9l-67 ga4iI.&s.
-f-AZM. AT 02101 ,
d6b . UKPO 004.
AUTHOR: Adam, N. V.: Bentkova. N. P.: Orlov. V. P.; TyygqLnq, L. 0.
ORG: none
TITLE, Calculation of the geomagnoti~ field strength based on the coefficients of
spherical analysis
SOURCE: A" ]Lij!L~kt4t fiziki Zemli. Nastoyashcheye i proahloye magnitnogo polya
. . _SSRt- -ii~W-
Zemli (The present and past of earth's magnetic field). Moscow, Xzd-vo Nauka,
1965, 33-41
TOPIC TAGS: geomagnetic field, geomagnetic measurement, magnetic field intensity,
cartography
ABSTRACT'* This article is devoted to a calculation of the geomagnetic field strength
bascd on the coefficients of spherical analynis in order to obtain information on the
distribution and character of the change of the geomagnetic field at various distances
from the earth's surface. The first step in this work was to determine the coeffi-
cient3 of a spherical harmonic series in order to calculate the geomagnetic field in
circumterrestrial space. The starting data were the magnetic charts of the IZMIRAN
and the British Admiralty for the 1955 epoch and the values of the magnetic elements-
at unevenly distributed discrete points. A subsequent synthesis of the field on the
carth's surface and its comparison with the starting data showed that the. beat repre-
Card 1.1

L
AT6021012
sentation of the field is given by the coefficients calculated with respect to world
charts. The elements X, Y, Z were calculated by the sum of the first six harmonics
for a network of points 50 with respect to latitude and 15* with respect to longitude.
The coefficients obtained from the IZMIRAN charts were used for further calculations.
It was found that spherical analysis carried out-for world magnetic charts gives an
analytical representation of the distribution of the field on the earth's surface with
the same degree of flatness and with the same errors as the world magnetic charts on
which the analysis was based. Spherical analysis offers a sufficiently simple and
easy'method of calculating the magnetic field and its gradients for large heights.
The absolute errors of calculation decrease with height in proportion to (R/r)3 or
even more quickly, but the relative errors remain constant or decrease slightly. Tak-
ing this into account, as well as the rapid decrease of old harmonics with height, the
authors assert that at large heights the series of spherical harmonics provide a high-
accuracy of approximating the magnetic field sufficient for various problems of inves-
tigating a constant field and for interpreting satellite observations. An analysis of
the 1955 IZMIRAN charts confirmed the systematic shift of the earth's magnetic center.
The theories of the origin of the geomagnetic field scarcely touched upon the problem
of the eccentricity of the field and the authors wish to call the very fact of eccen-
tricity and the systematic shift of the magnetic center to the attention of theore-
ticians. The representation of smoothed world charts by series of spherical harmonics,
up to the sixth order is not, in the opinion of the authors, the limit. of what spheri-I
cal analysis can' give. With a sufficiently large number of observations pertaining tol,
one epoch, a s&erical harmonic series can provide a more detailed pi,,.ture c--' the
Card

L 07'491-67-
CC NRo AT6021012
field and with fewer errors. Orig. art. has; 11 formulas, 3 tables, and 4 figures.
SUB CODEt 08/ SUBM DAM 2lSep65/ ORIG REP; 008/ OTH REV: 004

TYLYRINA., M. M.
4---
Physiological characteristics of plants in the Pamirs. Truc'~r
Bot. inst. AN Tadzh. SSR. 18:334-352 162.
(MIRA 161l)
(Pamirs-Plant physiology)

TYURMOKO, G.A,p kand.sellekokhoz,nauk
Harvesting, drying, and storing lupine seeds. Zemleaelle 6 no.8:
7"76 Ag 158. (Lupine) (MIRA 12:11)

BENIKOVA,
Analytical representation of the geomagnetic field on the territory
of the Saviet Union for the 1958 epoch. Geomag. i aer. I no.l:
87-103 Ja-F 161. (MIRA 14:7)
1. Institut zemnogo magnetizma, ionoefery I rasprostraneniya
radiovoln AN SSSR.
(14agnatism,, Terrestrial)

-Tr M OREZOVp V. Yo. N15
653.021
.Bl
Telegrafiya [Telegraphy, BY] I. Ya. Balagin, V. P. Papov, [11 V. Ye.
Pymmmorezov. Moskva, Trwnzheldorizdat, 1958.
462 V. illus.p Diagre.p Graphop Tables.
"Literatura". 'P. 449.

TYUF040REZQV,Yilftu-XevgrafcyvichI inzh.; KIRIIDV, Mikhail Mikhaylovich,,
'kand. tekhn. nauk; KOZWV, lev Nikolayevich, inzh.; MU41N, le.A.,
iand, tekbn. naukj retsenzont; POZDNYAKOV., L.G... inzh., retsenzent;
FELIDMAN, A.B.I. retsenze.ut; KAZAKOV, A.A., kand. tekhn.
naukp red.; MEDVEDEVA, M.A.# tekbno reds
(Electric power supply to railroad commmications,, apparatus and
aiitomatic'control., and remote control systems] Elektropitanie
ustroietv oviazi, avtomatiki i telemekhaniki na zheleznodorozhnom
treajz~orte. Mosk7a, Vae.s. izdatellsko-poligr. ob"edinenie M-va
patei soobshcheniiaj, 1961. 215 P. (MIRA .14:11)
(Electric power supply to apparatus)
(Railroads--Electric equipment)

V Lit
6(7) PHASE I BOOK EXPLOITATION SOV/1291
Balagin, Ivan Yakovlevich, Vadim Petrovich Popov
Yevgrafovich Tyurmorezov and Viktor
Telegrafiya kTeleg:raphy) Moscow, Tz-anszheldorizdat, 1958. 462 p.
7,000 copies printed.
Ed.: Stroganov, L.P., Engineer; Tech. Ed.: Khitrov, P.A.
PURPOSE: This book was approved by the Main Administration of Educa-
tional Institutions, USSR Ministry of Railroads, an a textbook for
students of railroad automation, telemechanics and communications.
It may also be used by engineers and technicians in these fields.
COVERAGE: The author describes fundamentals of the theory of tele-
graph communication and discusses the circuits and construction
details of telegraph apparatus used in railroad communications.
The author mentions A.D. Ignatlyev, L.N. Gurlyev, and G.P. Kozlov
as having.done -Q7ork on the multiplexing of telegraph circuits and
and radio channels in 1936. Also mentioned are Engiheers
Card 1/18

Telegraphy
SOV/1291
N.A. Volkov, N.G. Gagarin, and S.I. Chasovikov, who in 1935
developed the ST-35 start-stop equipment. I.Ya. Batlagin
wrote the Introduction and Chapters I through XIIII V.P. Popov
wrote Chapters XIV through XXII and Chapters XXVIIJ: and XXIX;
V. Ye. Tyurmorezov wrote Chapters XXIV through XXVI.I., There
are,18 references, all Soviet.
TABLE OF CONTENTS:
Introduction
3
PART I. GENERAL INFORMATION 6
Ch. I. Basic Concepts 6
1. Principle of telegraph communication 6
2. Telegraph codes 7
3. Basic methods of telegraphy 10
4. Classification of telegraph apparatus 14
5. Operating principle of uniform code apparatus ltz
6. Basic methods of correction
Card 2/18

-ness of the Act-*on of Fatty
tre
'IT' eoretiv'l Basis for incr,:ms-Ln.
-
Aci6s in the Flotation of 01-idized Ores.
report presented at the 'onference an .3enefication of llsoruL ',,lincral-ol oi,,-onsored
'L k'1 rI; -.ara,an6s, "lov rec U60.
by t~je Learned Comcil of the j, AS Balakhash./Y .. 29

SS'l,'P!/ ZaAh ks i B-13
emis rj. Surface Phenomena. Adsoi-ption.
/U'S ~Sll Ciiromatography. Ion 1-1-change.
Abs Jour : Ref Zhur - Eb-imiya, No 7, 1957, 22551.
Author : 1. 11. Plaksin, V- I. T~yurnikov.
Inst : Not Siver.
Title : Examination of Yaathogenate Fixation Stability on Chalcopyrite
Grain Surface.
Orig Pub : Izv. AIN USSR, Otd. Tekhn. N. 1956, No 8, 14o-142.
Abstract : The stability of a series of xanthogenates M on chalcopyrite
(I) Crain surface is examined by method of radioactive isotopes.
The determination of desorption of X was carried out by the way
of washing off in a special mixer of an average sample of
chalcopyrite concentrate obtained by flotation of the mixture
of I and quartz X marked s3p, and of pine oil in a lime inedium.
It is shown that the fixation X stability, insignificant at small
expenditures of X (25-50 9/0, grows with the increase of X ex-
penditure till 300g, and falls againct further increase of X
expenditure till 600 s/t. Tne comparison of desorption of dif-
ferent X from I surfaces showed that the desorption of ethyl X
is much faster that that of the butyl and isoamyl X.
Card 1/1 -196-

TTURIKOV, V.H., Inzh.-
... Undulating wearof rails and how to combat it. puto i t
khoz. no.10:33-35 0 '59. (MIR& 13-2T 1
1. Starshiy dorozbnyy master rel'soehlifovallnogo vagona,
Temingrad.
(Railroads--Rails)
(Railroada--Maintenance and repair)

TYURIHA. Te.V.
Biolog7 of flowering and seed maturation in the Moldavian dragonnead
(Dracocaphalum moldavica L.) Trudy, Bot. sada Zap.-Sib. fil. AN SSSR
2:19-23 '57. (MIRA 11:10)
('Dragonhead)

TYURIKA. Ye.V.
I., ..
........ _ii olog7 of germination in coriiAnder fruit. Trud7 Bot. oada Zap.-Sib.
f1l. ~AN SSSR no.2:41-" '57. (HIRA 11:10)
(Oortander) (Garmination)

17- ~. - ~ - -7
A -