SCIENTIFIC ABSTRACT MATVEYEVA, E.M. - MATVEYEVA, L.S.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001033010005-8
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 14, 2000
• Sequence Number: 5
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

81557
S/062/60/000/05/07/no8
B004/Bo66
AUTHORSs (Deoeased),-4ergeleva, Z, I , Zubkova Be 1,,
IDolgov, B.
mat evalm~E* Moo Voronkove, M'. G.
TITLEs Organosilicon Esterelof Oximos
PERIODICALs Izvestiya, Akademii nauk SSSR., Otdeleniye khimicheakikh
ng"k, 1960, No. 5, P- 951
TEXT: The authors report in a letter to the editor of this periodical
that they had been able to prepare the trialkyl silyl ester of aldoximes
and ketoximes in good 7iolds (50-80 Per cent). The synthesis was per-
formed within 5 h at room temperature by reaction of trialkyl chloro
silanes with the corresponding oximes in the presence of pyridine ac-
cording to the equation
R Siel + BON=C N ->R SiON=MR, -4- 0 H N.M. Physical constantL,
3 I_R" + C5H5 3 5 5
and analytical data will be published shortly. On hydrogenation of these
compounds on platinum at room temperature the O-W bond is separated.
Differently substituted amines, NR,v and trialkyl silanole are formed.
Card 1/2

81557
Organosilicon.W.ers of Oximea s/o62j6O/OOO/O5/07/0(-,f
B004/B066
The hydrolysis of 0-triethyl-silyl-propional(toxime by means of 5% HCI
occurs only to 50-60 per cent. The initial compoundq the oximeg hexa-
ethyl-dielloxene and a resin containing nitrogen were found in the
hydrolyzate, The infrared spectrum of all 0-trialkyl-silyloximes Pon,-
taina the characteristic frequency 1636-1640 om-1 which may probably be
assigned to the valence vibrations of the Cull bond.
ASSOCIATIOWs Institut khimii silikatov Akadomii nauk SSSR (Institute
of Silicate Chemistry of the Academy of Sciences, USSR).
Leningradskiy gosudarstvennyy universitet im. A. A.
Zhdanova (Leningrad State University imeni A. A. Zhdanov)
SUBMITTEDt February 29, 1960
Card 2/2

jqYEVA, E.T.,- OSOKINA, G.N..
MOIDCHNOVp G.V.;,M
Electronapetle field of a verticalmagnetic dipole over a two-
layered structured with a oteplike boundary, Uch. sap. LGU
no.286-.255-260 160. (MIRA 14:3)
(Zlectromagnatic prospecting)

MATVEYEVA, E.T.; TROITSKAYA V.A.
General laws governing the pearl-tirpe mode of oscillations.
Geomag. i aer. 5 no.6:1078-1084 N.-D 165.
(WRA 19: 1)
1. Institut fiziki Zemli Kq SSSR. Submitted August 3, 1964.

.L ~208h-66 &N(17
SOURCE CODE: UR/0387A6/000/001/0076/0079
AUTHOR: Troit-skaya, V. A.; Shchepeatnov., R. V.; Bollshakova, 0. .; MMaltveyeva, E.
ORG: Institute of Physics of the Earth, AN SSSIJ (In-stitut fiziki Zemli AN SSSR)
TITLE: Characteristic properties of rapid variations of the Earth's electromagnetic
field in the polar regions
W,
SOURCE., AN SSSR. Izvestiya. Fizika Zemli, no. 1, 1966, 76-79
TOPIC TAGS: electromagnetic terrestrial field, electromagnetic field variation,,
solar activity, pearl shaped variation, stable variation, polar region, magnetic
storm,irregular variation, aurora, magnetically coupled region, magnetic force
11ne, proton, solar cycle
ABSTRACT: Durine the IGY short-Deriod variation measurements of the
electromagnetic field in the polar regions of the Soviet Union were
cariied out at five Arctic stations (Kheys Island, Barentsburg, Cape
Chelyuskin, Tiksi Bay, and LovozerO and in Antarctica (Mirnyy
and Oazis). Analysis of data obtained showed that the properties of
thepolar regions are associated with the cycle of solar activity.
Especially rapid irregular variations of type Pil and the frequency
of excitation of pearl-shaped variations Pcl depend upon the solar
cycle. The daily rate of these variations differs from those at mid-
dle latitudes. Soviet observatories noted giant pulsations of types

L 42084-66
ACC NRs AP6003338
Pg and Lpc in the polar regions. Simultaneous excitations of stable
variations occur in the polar regions during equinoxes and very seldom
during solstices.
Regular stable variations are typical of polar and other latitudes.
Stable variations of type Lj)c occur mostly in the polar regions. their
vibrations last 3-7 min. This type of variation takes place in middle
latitudes only in magnetic storma, appearing mostly at noon. Rapid
irregular variations of type Pil occur with high intensity in the auroral
zone where their amplitude reaches hundreds of mv/km. The amplitude
of Pil variations diminishes rapidly- to the north and south of the auroral
zone, - This type of variation occurs before midnight and in the morning
bouts. The Pil -type variations are very much associated with auroras.
The appearance of these variations testifies to the development of auroral
processes in the upper atmosphere.,
Special interest was aroused by the pearl-shaped variations. Figure
1 shows this type of variation which was obtained on 6 August 1964 at
Tiksi Station. Long-term records at USSR observatories made it possible

L; - Lf- _IWSM~_
FACC NR.
AP6003338
Tiksi "t. 6 August 6)1
Fig. 1. Pearl-shaped magnetic vibrations
to conclude that the frequency of appearance of these variations increases
with the decrease of the latitude of the observation point. This kind of
variation occurs in magnetically coupled rcilions. The formation of pearl-
shaped variations is hypothesized to be a movement of accumulated par-
ticles around a magnetic force line. Traveling from one hemisphere to
the other along the force line between magnetically coupled points, the
particle cluster increases the intensity of the magnetic field in the di-
rection towards which the cluster moves while decreasing the magnetic
field intensity behind it. The increased, field causes intense vibrations
which form the pe-jxL Another hypothei;is explains this formation by
magnetohydrodynamic waves which propagate from one hemisphere to
the other.
Card

L -4208h-66
Experimental simultaneous obp.7 vations were carried out in two
magnetically coupled points, SPR~~In the USSR and on the French is-
1=d of Kergelen in the Indi~ean. Processing of recorded data led
to the following conclusions: 1) Maxima of individual pearls in opposite
hemispheres are shifted by a half-period. Periods of envelopes over the
pearls are preserved in both hemispheres, 2) No delay in phases was
observed when the movement was from east to west. 3) Periods of pearl
formation in coupled regions are equal. These data cannot be considered
as a support of either the first or the second hypothesis.
Orig. art. has: 3 figures. UTD PRESS: 4172-F]
SUB CODE: 08, 03 / DATE SUBM: OBApr64 / ORIG REF: 004 / OTH REF - 006
Card 4/4 af

AP6018919 SOURCE CODE: UR/0203/66/006/003/0533/05xfv
AUTHOR: Troitskaya. V. A. ; Boll-shakova .--0. V. ; Matveygya
ORG: Institute of Physics of the Earth, ffl; SSSR (Institut fiziki zemli AN SSSR)
TITLE: Sudden electromagnetic field variations~ as an indicator of the state of the
radiation belts and the mgpetS~pki~~ of the earth
WURCE: Geomagnetizm i aeronopniya, v. 6. no. 3, 1966, 533-540
C.
TOPIC TAGS. Vz=-A4+o, radiation belt, gecoagnetiss measurement, geomagnetic field
ABSTkACT:"Changes in the ;s1tion of the boundary between the magnetosphere and the
external radiation beltsbrought about by excited stable oscillations and intensity
changes in the belts as a function of excited irregular short-period oscillations,,
are investigated. The measurements were made by Electron-1, Electron-2, and Explorer-
-XII satellites. The data show that- 1) The boundary between the magnetosphere and th'
radiation belts fluctuates about its meai position ~,IOR e, where Re is the radius of
the earth; 2) Geomagnetic field oscillations of Pc4 type (50-150 sec) are observed
when the boundary is located at a distance of 10R e or more; 3) Geomagnetic field os-
cillations of Pc2 and P0 types (5-40 sec) appear when the boundary moves toward the
earth; 4) The extremum values of the boundary positions vary from 7.5 R e to 12.5 R e
UDC: 550.386

421ni-66
ACC NM AP6016919
Periods of stable oscillations (T) are proportional to R5, where R is a radius of
the magnetosphere; 6) The existence of stable oscillations (Pc) in the main storm
.phase may indicate that the comVression of the magnetosphere continues during this
phase; 7) Intensity changes in the radiation belts are closely connected with the in-
troduction of charged particles into the upp;tr Ltmospheric layers; and 8) The presence,1
of irregular short-pAgPiod oscillations of "pearl" type (Ptl) is connected with sharp",;
intensity changes in the radiation belts. Orig. art. has: 9 figures.
SUB CODE: 08,22/
ATO PRESS 1 5363
e_-
SLMM DATE: 14Aug6!,/ ORIG REr: ooe/ OTH REF: 005

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M A T-V f-
1. MIZEROVA, T. P. MATVFV-EVA. Y. A. KAZARINOV. V. P.
2. USSR (600)
4. mwlin-BalsV~~kiy Deposits
7. Report on the prospecting work at the Kraval'skiy section of the Balavskiy
Kwlin depoiets in 1940. (based on materials of B. N. Valukhov)
Izv. Glav. upr. geol. fon.-n4;47.
9. Monthly List of Russian Accessions, Library of bong-reess, Muah-122, Unclassified.

HATUMA, F. A.
Matveyeva, F.A. *Ceramic clays of Western Siberia," in symposium:
Syrlyevyyeresuray tonkokeram, prom-sti SSSR I Duti ikh ispoltzovaniya,
Moscow-Leningrad, 1948, P. 177-83
SO: U-2888. Letopis ZhurnalInykh Statey, No. 1. 1949

15-57-1-731
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 1,
p 116 (USSR)
AUTHORS: Nbtveyeva, F. A., Plekhanova, Ye. A.
TITLE: Acid-Resistant Ceramics From Siberian Raw Material
(Kislotoupornaya keramika iz sibirskogo syrlya)
PERIODICAL: Tr. khim-metallarg. in-ta. Zap-Sib. fil. AN SSSR,
1955, Nr 9, pp 3-17.
ABSTRACT: Experiments have been conducted to manufacture acid-
resistant and earthenware ceramic products from clays
of the Yevsinskoye-Dorogino mestorozhdeniye (deposit)
in the Novosibirskaya Oblast .. The variegated, light-
colored clays from the Dorogino part of the deposit
were used. The chief properties of these clays are
given-in the Table (in percent). The yield strength
during shearing of air dried material is 3.6 kg/cm2.
Caking occures at 11500 to 1~000. To obtain a ceramic
body with high density, acid-resistance, thermal
Card 1/~ stability, and mechanical strength, it is necessary to

15-57-1-731
Acid-Resistant Ceramics From Siberian Raw Uhterial (Cont.)
add to the Doroginskoye clays refractory, slightly sintered,
sufficiently plastic clays and feldspar as fluxing material; grog
must also be added. The author recommends the following proportions
for the paqte (in percent): light-colored Dorogino clays, 35 to
45; refractory, sintered, sufficiently plastic clay, 25; feldspar,
10 to 15; admixture (grog from the Dorogino clays, porcelain rubble,
etc.), 20 to 25. It is possible to Atain a variety of acid-
resistant ceramic products from this combinktion.
Chemical composition Fire-
resistance
S102 2 3 Fe203 CS Others 0C
68.22 19.42 3.45 0.60 0.83 4.64 1520
Card 2/3

15-57-1-731
Acid-Resistant Ceramics From Siberian Raw Wterial (Cont.)
Grain-size distribution
(fraction units in mm)

0.25 0.25-
0. - .02-
0.01- 5-
0.00 0.002 0.0005
0.05 .0.02 0.01 0.005 0.002 0.005
0.3 0,08 13.30 12.85 19.41 16.21 19.72 18.13
Card 3/3 S. P. Sh.

15-67-1-736
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 1,
pp 116-117 (USSR)
AUTHORS: W18tveyev Plekhanova, Ye. A.
TITLE: The Chemical Stability of Ceramic Tile From Clays in
the Doroginskoye Mestorozhdenlye (Deposit) in the
Novosibirskaya Oblast (Rhimicheakeya stoykost,
keramicheskikh plitok na osnove glin Doroginskogo
mestorozhdeniya Novosibirskoy oblesti)
PERIODICAL: Tr. khim-metallurg. in-ta. Zap-Sib. fil. AN SSSR,
1955, Nr 9, pp 19-36.
ABSTRACT: Studies of the chemical stability of acid-resistant
tile, obtained under laboratory conditions from the
clays of the Yevttinsko-Doroginskoye deposit in the
Novosibirskaya Oblast', have shown that these tiles
have a higher in'dex than tiles from the Shchekinskiy
zavod (factory). This fact is explained by a higher
Card 1/2 development of mullite and greater density In the body

15-57-1-736
The Chemical Stability of Ceramic Tile From Clays (Cort.)
of the tile made from the Doroginskoye clays. Of these tiles,
those with a water absorption less than two percent have a greater
--hemical stability than those with a water absorption in the inter-
val from two to four percent. The tile from the Dorokinskoye clays
may be used in the chemical industry for acid-resistant material.
Card 2/2 S. P. Sh.

WAM M-151=1 ~_M1W_1MMVM19'9111_ rw2rMfAMMY~R MM K&W,
0-) 1) T- (11 , r Y E 1) /A 1 F-:7- ,-I
USSR/Chemical Technology - Chemical Products and Their Application. Silicates,
Glass. Ceramics. Binders, 1-9
Abst Journal: Referat Zhur - Khimiya, No 19, 1956, 62314
Author: Matveyeva, F. A. Plekhanova, Ye. A.
Institutiont None
Title: Concerning the Use of Acid-Resistant Tile Made from Clays of
Doroginsk Deposit in Novosibirsk Oblast in the Chemical Industry
Original
Periodical: Tr. khim.-metallurg. in-ta Zap. Sib. fil. AN SSSR, 1955, No 9,
37-49
Abstract: Presentation of the results of tests of chemical stability of
ceramic tiles made from Doroginsk clay, under conditions of uti-
lization at a coke and chemicals plant. The procedure of testing
in production apparatus with exposure to various caustic media is
described. Tests over prolonged periods were made of tiles made
from Doroginsk clay having different density and water absorption
of