SCIENTIFIC ABSTRACT FEDOROVA, M.N. - FEDOROVA, ZH.S.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R002200810005-3
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 17, 2001
• Sequence Number: 5
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

USSR
FEDOROVA) M. N.j et al., Fazavyy Khimicheskiy Analiz Mid Chernylth ~Letallov i
,
Produktoy ikh Pererabotki Nedra" Publishing House, 1971~, 169 pp
Iron minerals and ores 19
A brief review of methods of phase analysis of iron ores 23
Determination of ore and silicateiron 21;
,
Determination of magnetite 36
Determination of the magnetite chemical composition 50
Determination of iron hydroxides 53
.,Determination of siderite 55
Determination of Hematite 59

Determination of the sulfur mineral forms ,
60
s
Determination of cobalt and nickel forms.in iron ore 63
,
Determination of the forms of phosphorus 65
Determination of bi- -and trivalent iron in products yith

high concentration of sulfides 66
Chapter II. Phaso analysis of pelletized products prepared from iron ore
concentrates of diffem-nt compoBitions 69
Formation of minerals in the charge during pelletizing process and
and firing of pellets 70
Synthesis of minerals present in the pelletized products 72
4/6

.. ........ .. ......
USSR
FEDOROVA M. N., et al., Fazovyy Khimicheskiy- Analiz Rud Chernykh Metallov i
Produktov ikh Pererabotki, "Nedra" Publishing House, 1972, 160 pp
Determination of calcium ancl iron oxide forms in pelletized
products prepared from ore concentrates of a simple composition 73
Phase analysis of highly-basic agglomerates 78
Determination of mineral forms in pelletized products prepared from
ore concentrates of complex composition 80
Chapter III. Phase analysis of titanium ores
Titanium minerals and ores 84
Determination of the mineral forms of titanium 86
Study of the forms of iron, titanium, vanadium, and of other
elements in titanium-1mgnetite and ilmenite-magnetite types of
ores 97
Determination of grain sizes of ilmenite in titanomlagnetite 100
Chapter IV. Phase analysis of manganese ores in products of their
treatment
Manganese ores and minerals 103
Reviev of methods of phase analysis of nanganese ores 105
Determ ination- of mineml fams of manganese in carb onate and
mixed ores 110
5/6
95

USSR
FEDORaVA, M. N., et al., Fazovyy Khimicheskiy Analiz Rid Chernykh Metallovi
Produktov ikh Pererabotki, "Nedra" Publishing, House, lSqP- 160 pp
Analysis of oxide ores
121
Analysis of firing products 123
Determination of phosphorus forms in manganese ores 324
Determination of chemical and molecular,composition of
carbonate manganese complexes 134
Chapter V. Phase analysis of chromium ores 140
Chapter,VI. Determination of free and bound silicic acid 14,6
Methods of determining quartz 147
Determination of opal 153
Determination of sizes of quartz particles 154
References 155

616

DATE--04DEC70
012 UNCLASSIFIED
-rITLE--BISINFECTION OF FODDER GRASS SEEDS -U-
:-.-AUTHOR-(02)-KALASHNIKOV# K.YA.t FEDOROVAt.M.No
10
...COUNTRY OF -INFO--USSR
,SOURCE-KHIM. SEL. KHOZ. 1970, 8(4)r 284-6
PUBL ISHEO ------- 70
SUBJECT AREAS--AGRICULTUREs,61OLOGICAL AND MEDICAL SCIFNCF~
l'OPIC TAGS--AGRICULTURE CROP SEED, FUNGICIDE
'CONTROL MARKING--NO PESTRICTIONS
DOCUMENT CLASS--UNCLASSIFIED
-PROXY FICHE NO- --FD70/605002/CO7 STEP NO--UR /0394 7i"l 1008 1410?
clfzc

UNCLASSI FIEO
-2/2 012
CIRC ACCESSION NO--AP0139433
G13-0- ABSTRACT. IN FIELD EXPI.S., 0 R Y S Ef D
'C _T~
~~WITH GRANOSAN (1) AND 50PEIZCENT r ii I R Ali I I Il I MM E 0 1 A'T E L Y: OR 9 "10 NO
BEFORE SOWING STIMULATING THE GROwTH A N D DE.VELOP14ENT OF MEADrI'vi
CHAR0 GR
.(FESTUCA PRATENSIS), TALL FESCUE (F. ARUNDINACEAls I)R;, A'S
IF A C X4
JDACTYLIS GLOMERATA), CANARY GRASS (PHALARIS CANARIENSIS), ANI 1j
..FOXTAIL (ALOPECURUS PRATENSIS). THE SEED YIELDS OF ORCHAJ-,f) 1-julss,
,.CANARY GRASSi AND MEADOW FOXTAIL 14ERE HIGHER WITH I I, WHEREAS THOSE Il-
I HIGHEiR I I"i I.
MEADOW-FESCUE AND KENTUCKY BLUEGRASS (POA PRATENSIS~
-1 AND It 1440 THE SAME EFFET OIN THE SEED YIELD OF T1,40111Y (PHLEUM
PRATENSE). EARLY SEED DRESSING OLD NOT DECREASE- Tlj,c-_ GEIRMINAfING
.-CAPACITY OF THE FODDER GRASS SEEos, THE RECOMMFNDED 00 SES ARE 1.-1. 5 G
AND 3 G-KG SEEDS FOR I AND FACILI;rY, NAUCH.- I SSL ED.
[It RESP.
,:--BAZA VIZRI PUSHKINO, USSR.

L12 018 UNCLASSIFIED PROCESSING DATE--20NOV70
TITLE--POSSIBLE KECCNSTRUCTIGN OF CHROMATIN AFTER DISSOCIATION IN SALT
a
SLLUTICNS -U-
ALTHOR-(Q2)-ASbMARIN, I.P.w FEDOROVAt N.A.
~'CCIJNTRY OF INFC--USSR
::SOURCE--TSI'rCLOGIYA 197 0, 12-(3), 338-42
-CATE PLELISHLO ------- 70
~SUBJECJ AREAS--alOLOGICAL ANG MEDICAL SCIENCES
.TCPIC TAGS-Clif(OMATINt RAT# LIVER#-DNAr DIALYSISr PROTEIN
UNTROL MARKING--NO RESTRICTIONS
OCCUMENT CLASS--UNCLASSIFIED
PROXY REEL/FRAMC---3002/042(j SUP
CIRC ACCESSIL',\ NC*--,61'l0127997

I Im n "nil 6
-ESS ING OAT;7--2()NOV70
2/2 018 UNCLASSI HED F ROG
:C-IRC ACCESSICN NO--AP0127997
-:-A6STP-ACT/EXTRACT--(U) GP-0- A3STRACT. FRACTIONS GF 130 f1i i,.IATIVF 040
-4 VER AFTER ULTRASONIC
-RECCNSTRUCTED CHROMAII, ISOLATED FROM RAT11
TRr-A-,T,4t-NT IiERE FRACTIUNATED GN ASEPHADLX G-200 CCI-WIN. PROTEIN
DISSOCN. FRCM NATIVE CHRUVAUN GCCURRED IN 2 . 51M NACL PROT E IN
-.RECCM8Ij\-ATI0N WITH DNA WAS ACCOMPLISHED BY MEANS OF Srr-PWISE DIALYSIS.
'CPROTEIN CONTENT AND OPTICAL ABSORPTIOW AT 230 AiND Z60 I-IMU
BLITH PFCSPI.
WERE THE SAME IN FRACTIGN OF hATIVE AND RECCNSTRUCTED CHROMATIN,
FACILITY: DIEP. 810CHE.M.s, LENINGRAD UNIV.? LENINGR4D, USSR.

Molecular Biology
USSR VDC 578,058.4:547.963.3
A., and LONSKIY, A. V.
"The Use of Ultrasound to Obtain Chromatin Fractions"
Leningrad, Vestnik Leningradskogo Universiteta, No 9, Bioiogiya, to 2, 1970,
pp 146-149
Abstract: Study of the distribution of various proteins along thu D",'A helix, and
evaluation of the specific functions of proteins in speciil'C SeCLIGIls of DNA,
are required to explain the significance of the different J!TCU-Pli Of proLet-ns in
the emerging blue-print of chromatin activity. Difficultj-., r~
ei a -se in Lhe prep-
aration of samples for such a study because of the presence of protooiytic
enzymes. Preparations of chromatin from mice livers ,,iLh a proLei-11: D"I'A ratio
of 2.4:1 were dissolved in 0.01 M tris buffer at pli 8, and -.ubjecLed to ultra-
sonic vibrations in a nitrogen atmosphere at a frequency of I and
intensity of 10 VolL/cm2 for 30 min. Chromatin obtained in this :,.-,anner vzas
fractionated on Sephadex columns. The gel flil t ration, method was usec co de-
ternine the molecular weight of the fractions. The data obLainc:d indic,-ice the
formation of DNA-protein complexes, winich differ in tneir compo;ii,,J~on tt~ro7.i
similar complexes of native chromaLin. it was concluded thaL th,~ ci,romi.-ILIII
proteins do not possess a pronounced affinity for specific section!, (it the DNA
helix.
'jJ4 1~
.1 - RIV, H.M.1 MH IM I! I@ IN III ;I.r 11021111 1111111111L R11111t '11.119111-M!

1/2 020 UNCLASSI F [ED PpocussOlc rwp---o~OCT703
i,TITLE--EMISSlCjN HEIGHT DISTkIt-AUTIONS OV CERTAIN AUROAAL f:0qN", ON HIGH
'~' LATITUDES -U_
'AUTHOR--FF00R9VAs N.I.
_CnUNTRY OF 114FO--USSR
5(-,lURLE--RAZUEL IV, P0LY;%,RNYYE SIYA.NIYA I SVECHCNIYE N 0 1 t., 1.. 5'14 E3A 197J,
14R PP 42-49
tuATE PUELISHED ------- 70
~SUBJFCT AREAS--ATMOSPHERIC SCIENCES
TOPIC TAG,S--AUR ORA* OXYGENt RAOIATION INTENSITY, GEOGRAPHIC LAT[T11DE
CDNTi~ll 14ARKING--NO RESTRICTIONS
DOCUMENT CLASS--UNCLASSIFIED
PROXY 1,EfL/1-RAfAlF--1994/')1I3 STEP N11--UR /330 7/ 70 /OX/ )1.1/ 034 t'04'~i
CIRC ACCESSli)NI N(J--AP0Itf#50')

77~
020 LINC LASS I F I ED PROCESSING DATE-02UCT70
CIRC ACCESSION Ntl--AP0114504
-AiSSTk'ACT/fXTR-AC-T--(U) GP-o- ABSTRACT. HEIGHT- DISTR[E)JTl0.\' IF E41SSITYN
INTENSITY-WAS DETERMINED IN 4 NUMBER OF DISCRETE FQRliS OF AUR,04-AE. 1 1%,
ORDINARY AURORAE THE HEIGHT VARIATIONS OF THE INTENSITY OF GRFEN ATIMI--
~OXYGEN LINF' AkE SIMILAR TO THOSE OF 1PGN SUB2 AND ING~, 'b" P-4,1'4F
POSITIVE MOLECULAR BANDS. hOWEVERP IN THE'd TYPE AURIPAE WHIC-4 qAVE A
BUTTOM RED EDGE THE RATIO I SUB5577(01),I SU8(A.5)1,PG% SJB2 IS SOMF
-:LOWER, (SIMILAP TO 7-9) THAN 1.4 ORDINARY AURORAE OF ~HA, ;;.A, H5, 4~B* R A~~F)
OTHER TYPES.(WHERE IT IS APPROXIMATELY 10-12) WHILE~ AT THE BOTTO'4
~~UF'THE DEFOCUSED RAYS WITHOUT ANY SHARP LOWER BOUNDARY AND 1.4 SOME OTHFR
FOPMS,THIS RATIO COMES UP TO OVER 20. THE INTENSITY OF T4E REn OXYGEN
LINE IS-CONSIOERABLY INCRLASEU WITH HEIGHT. THERATIO I SUB5577rl
SUB6300 INDIFFERENT FORMS OF AURORAE VARIED FROM 0.1 TO 8.0.
UNCLASSIFIED
---wlwrm

... .................. ....
P EMI
Acc. Nr.: j;,P0042Yj0_
Ref. 417
Studv of Geoactive corpiiscli~3 and Phatoelectrons
(Abstract: "Study of Geoactive Corpuscles and Photoelectroas Or. t";L.'
'Kosmos-261' Satelli e," by in, Y . 1. - -
t ~~Iyu~,qva, M..,.L. Brag Ga
perin, V. A. _gJXdv.5hev, N. V. Dzhord.-hip.. G. N K4k:1,11,70,
' _' ' - - - _Z jAt~kn, .!I .._ ft,-.-.,. ! - I.-
R. A. *~d~,~~zhkin, ~k, XkL. 'I- Pq!~or-nnE~V. - V_ . ~:_ --.
_ __ _K_ Y
Fedorova, Yu. P. Shilyayev, F. K. Shuyskaya and R. V. Shulenil".1.1; Mosicow,
Kor,micFtc-ski-ye-ts-s!Z~'dov,iniya,-V-ol*-Vlll,-I,o 1, 1970, pp ld4-ij6'j__
The'artificial earth satellite "Konmos-261" wati u,,Ld il~ a GLUI:1-
low-energy gcoactive corpuscles and fresh phot.oclectrons and zh.eir
action with the earth's upper atmosphere. The Gatellita w.;i On
.10 December 1968. Orbital inclinat"on t -o the equator was 7l'*, sa for
a raZacively long time it moved airost along a tangent alonG -,h,!
zone over the Soviet Far North, making it possible to increase cha
of simultancour, measurements from the satellite and from ground aI.!;,,.-va-
tories. T'he storage regiv4 made ft possible to extend cont.~nuouj
ments for periods of several -evolutions. Including passes over :h,~ auroral
zones in the Arctic and Antarctic and over the polar caps as farr 4S in-
variant geomagnetic latitudes 82-85*. Durin% the initial perlod thf-
satellite apogee was at 670 km and Perigee wis ac 217 km, but It flnij:y
J
T

. .............. . .....
A200425AL
burnt up upon entering Into the dense ~Iayars of the atmosphere .,;n !2
y 1969 after making 857 revolutions of the earth. The expurltzon:
ruar
insted 53 days. The orbit was such that in the northern hemisphere m!,Edia
aad hi~"h laticudes the satellite mived below or close to the
the ForeCion so that ionospheric e2ectron density along, Its
and its variations could be determined in a nwmber of regions on the
oi measure-mencs by ground ionospheric stations. The period af.thd
ment included both quiez ~~ezlods and those with strong
experiment was conduczed under the "Program of Cooperation Ama.~g Soc'~a'.~sc
Countries in -he Field of Space Research and Peaceful Use af Scpace.":
Oround me-asurementa %.,.Lre made in Bulgaria, Hungary, East Ga:inanv,
Rumania, USSq and Czechoslovakia. Observatories and apec-al
atationn in the USSR participated! in Yakutia, the Far North,; Meria, "n-d
middlc- la;itudej. The ijrticle cited belov is divided intu four parr*-.
DescriptiGn of Ex?crizznt; 2) Measurement of Low-Energy Eloctroas; 3)
aurejaent of Low -Zn%!r.-j Tons; 4) Xcasurenento of Charged Particles Wit.-I
intemediate aad High Energies. PartG 2)-4) are esaenttall')r
articlei and are abstracted separately.
13760552

6
Ace. Nr.: Ref. C :ode -
M e a s u r ee n r-, o fLow-Energy 'electrons
nergy Flectrons," by
(Abstract: "Measurement of Low-E ~(U
V. 2 zt
qzhio, 1. D. Ivanoy, 1. P.