SCIENTIFIC ABSTRACT SEMENOV, YE.I. - SEMENOW, YE.I.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001547820017-6
• 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

SOV/122-59-4-15/28
Refinement of the Pattern of the Deformation Core a.nd Determination
of the Force in Die Stamping
of the deformation core by this procedure presented no
further difficulties. The relative thicknesses of
deformation zones were plotted against the relative
diameters of the forging (Figs 5 and 6). The thickness
of the first zone at half the forging radius differed
little from combined axial thicknesses of the first and
second zones. The thickness of the deformation zones at
half the radius away from the axis was also plotted and
found, like the thickness along the axis, to increase
progressively with the ratio of the diameter to the flash
thickness. The thickness along the axis of the
deformation zone did not vanish even at small diameter/
flash thickness ratios. When these ratios were about 20,
the ratio of deformation zone thickness to flash thickness
was about 3.5. The diameter/flash thickitess ratio also
affects the pattern of the deformation zone. At a ratio
of 3, the deformation zone is a bi-coneave lens. At large
ratios, the "lens" becomes bi-convex. The usual
Card 3/4 analytical solution for the deformation zone assumes this
to be conical or a stepped profile. A better solution

SOV/122-59-~-15/28
Refinement of the Pattern of the Deformation Core and Determination
of the Force in Die Stamping
assumes an elliptical shape. With the help of simplifying
assumption (plane strain), the forging pressures are
obtained by analysis. For forgings which. are round or
nearly round in planform, the equilibrium equations are
used in spherical coordinates when the deformation is
axially symmetrical. The analysis of this case is also
treated
There & 11 figures, 2 tables and 8 Soviet references.
Card 4/1+

PHASE I
'MOSCOW- VY&BhOYO toWmIchaskore uchlllohch.
ItashIny I tokhnologiy& obrabotki motallov davionlyem; sbornik 3tatey
(KAchInary and Procesaea for tht Pre30-working 3f K2t&.1s; Collec-
tion of Articles) Moacow, M"hgiz 1960. 246 p. (Serle3z its:
Trudy, Tn. 98 Errata slip Inserted. 3,500 copies printed,
Doctor of Toonical Sciences, Professor.; Ed. Of
ld-~.bl going Rouse. O.V. Q))dFrnyAk; Tech. Mi T.F.LZ--xolo~aj
KanagIng Ed. for Literature on Heavy MAchino Xjnufacturlln~ (Hashaiz):
S.Ta. Gollovin. Engineer.
PURPOM This collection of articles Is Intended for wzr~Lero In
scientific reaearch Institutions and In d-4e-fcrglnz shops, and
for engineering students.
COVERAOE: The book contains papers from the Department or Machtnes
and Processes for the Press~rkirj of Mlat-L- of the r.?-J (Moscow
Highs r Technical Scho2l imeni N.E. Bawman). The pi;e--3 deal x1th
theoretical and PrActics.2 aspects of metal prcsrvced=Z and vith
the theory and practice of furging =achine and press M-SIgn.
These papers data with machine hydraulics (selection of drives
Promises. pressure In cylinders). A design or a hydraulic power-
.0frow type 4preas-ha=merl, whIch can woric si a P~G.
or foidLng press, is Presented, Problems of the ttAcry or plastic
deformation in forging. upsetting and forming A" Jac &nalrod.
27 reference cardo (Non. 33 to 49J a--* appended to caz;.I&in problems
pertaining to the state of strong or plastically do fa.--*d metal,
Those cards are the continuation 0 presented In collection
I "No
No. 79 of the MTU, 1957.' No personalities ars mentiomed. Rafer-
once: accompany =*at of the articles.
T 0 Mna:
Candidats-6f
g3gmenov. Yo. vrnp-gillet Into the Container Of A IAr9* FOrlzcat&l
=RydraurIlOTExtruslon) Press (Certificate of Tnvantorship No. 113281
N
dated 4-4-581 58
XTA"k,o Engineer. Wavo Transmission of Energy 63
On Certain Kethode of Obtaining POOstin Mfcrzl~g
Yorooo 78
irjdg~.no"v 3 F , Inginsor. Selection of nuld Prevouro Im Dazl&nlnZ
gem
r . ;~~;
Zjmjb1-,'A.j., Lndy_$-jV_tZLn8hjbCjLndld&t tior Technical 3ejences.
lIzation of the Effo*tiV"&P&4ItY of r2ot (Power) r~" 101
U
ti
.proosso
liatieIC.I., Doctor of Technical 5016MOG, Professor- VAchanice of
plastically Deformed BOdIOG 12T
.1q22y___jV_A., Doctor or Technical ,or. .."mine-
I RI-nJ=
%ion or Hole Sizes in Burring EHOll..1 . lind'rial'al 136
~~~LDoator of Technical S6i~nQG2,oPr0f*`oOr- On the Prob-
pe of the Focus of Dofomat, During ForGINg in Dios
With Outter. 141
4pynorvo Myeglj ..Can4id.- Of Technical 3.1.noesp Decant. ftrgl"g
o, Bearings on Upsotters In a 147
sliding Die With Upsetting During Piercing
auelich ;,Zngiooor. Analysis Of Processes of AxILl3j SY=13-
PrIz MAi 0 ---- IT4 -
L-rFM-11On OL-9011 w Bodies
Attmayev _A.D., Candidate of Technical Sciences. EMerintant&I Invootl-
zation of Various Xothods of Shoot-Hatal POrMing 203
Candidate of Technical ScieT-063. History or the
-D"Olopment of the Soviet Proanforcins Industry 208
_ZjMja-A,j-(PAItor) . Reference Cards on the Theori or PI&AtI0
Defomatlanz;CLrdo 33-49- 217
AVAILABLEs Library or Congress
Card 5/5

v x
P. -4
~q sr r
8
Q A
43 a
o3
,7,8o
UA ~-u
3 1.9 F 3 t r ~fi
431 4
Ir
19
Ito

SDMTOV, Ye.l., dotsent, kand.tekhn.nauk
.Drop forging in the United States. Vest.mash. 40 no-7:75-80 JI
,6o. (MIRA 13:7)
(United States-Forging)

L -25'
L53~~
A
ON-
cql4psi

~7 I'll. V.
h ~!;- ~ -: k, ji VV.E.; 'E'4ENOV Ye.TO), E,':('HEf-,f3lfllAj
.1- 0.;- , - I -, ~, . L . , 1.
Huz 'ma Alle'k-seevich Vlasov, Ic.105-10,64.; obituary. Ce0khimiia
no.12tl332-1333 D 164s (%I-TRA 18-8)

unnog0room 010FAM
L- P077h-66 JDIHW
I ALL NKIAXG004681 SOURCE CODE: UR/018255796M io/don/dois
AUTHOR: Skorodumov, 61 A. Semenov, Ye. I.
ORG: none
TITLE: Investigation of deformed state during the sectiohal-dia,forgi f disks
SOURCE: Kuzuechno-shtampovechnoye proizvodstvo, no. 10, 1965, 11-15
TOPIC TAGS: plastic deformation, sectional die, die, iron, lead
ABSTRACT: The results of a study of the deformed state of sectionally forged disks
as compared with the deformed state of disks subjected to'conventional upsetting by!~
means of plane-parallel tools are presented. Armco-iron and lead blanks were used
The lead blanks were deformed in a 50-ton press and the amco-iron blanks, in a*1330-,
ton press. In the simulating experiments with the composite: lead blanks soldered with:
Wood's alloy, deformed state tras investigated with the aid of a coordinate grid,
(with 2x2 mm squares) plotted in the vertical diamettal plane of oneof the halves
of the blank. The blank wav deformed to the desired degree of deformation in twin-
section die, first by the c~'hntral section and then by the outer section. After this
the blank was split into two halves. The coordinate grid before and after the defor-
mation was measured with the aid of a microscope and photographed. The actual degree
of deformation in various parts of the diametral cross sectional area of the forg-
ings was determined according to the changes in the coordinate grid. On. thin basis,
Card 1 /2 Mr? 671 _QA1L

Ion 11 1 .
T, 2o!74-66
ACC NR: AP6004681
.curves of the distribution of actual degree.'of deformation.for forgings obtained:by
Bectional forging were plotted and were found to,resemble the curves for forgings
obtained by conventional upsetting. The only difference is that in sectional forging
the maximal actual degrees of deformation in the central zone lie below the horizon-,
tal line dividing the forging into two halves by height, whereas in conventional
upsetting these degrees lie either along or somewhat above this line. Subsequent
experiments with hot forging of armco iron also showed that the distribution of
actual degrees of deformation in sectional forging was roughly the-same as in can-
ventional upsetting. In-general, the sectional-die f i of disks is less ti
I ng
consuming than their upsetting and a.source and imprfedg macro- and'inicrostructural
n
of the material; this was confirmed by the strength nd plasticity tests of disks
obtained by both methods. Orig. art. has: 0 figures and 2 tables.
SUB CODU 11, 13, 20/ SUBM DATE: none/ ORIG REF: 003/ OTH REP: 000
Vub
Card 212

NISHKOV) ~.B.; SALDADIJZ, K.M.; ~',F,,%ENOVA, Ye.I.; PUCUHKOVA, I.A.
Anion ext-namae hizh-~asiclty ra-2mbranes of a heterogeneous
type. Plast. mas~iy no.11,39-43 165. (MIRA 18!12)

FILYAND, M.A.; SEMOVA, Ye.l.; POGODIR, S.A., zaalushennyy deyatell
nauki i P'izd4ssor, doktor, retsenzent; K9YERSON, G.A.,
professor, doktor, laureat Stalinakoy premii; SAMONOV, G.V.,
redaktor; KAMAYNVA, O.M., redaktor; MIKHAY10YA, V.V., tekhni-
cheskiy redaktor.
(Properties of rare elements; handbook] Svoistva redkikh elemeatov;
spravochnik. Moskva, Goo. nauchno-tekhn. izd-vo lit-ry po che:moi
i tovetuoi metallurgii, 1953- 414 p. (XLRk 7:11)
(Chemical elements)

86892
S/056/60/039/005/oo6/orli
? el 113'Vj115',1'j B029/BO77
AUTHORS: Avvakumov, V. I., Gariflyanov, S. S., =WW* i_sa~
TITLE: Electron Paramagnetic Resonance and Paramagnetic. Relaxa-
tion in Liquid and Undercooled Solutions of Ti+++ Salta
PERIODICAL: Zhurnal eksperimentallnoy i teoreticheskoy fizik:i, 1960..
Vol. .79, No. 5(11), pp. 1215 - 1220
TEXT: The authors detected an electron paramagnetic resonance in
liquid solutions of TiCl 6H 0 in glycerin and alcohol and also in under-
0 3 2 0
cooled solutions at 77 and 200 K at frequencies of 300 and 9640 mega-
cycles. Moreoverg they studied pyridine complexes of Ti+++, ard also
specimens of silicate glass and boron glass which contained titanium
compounds. The shape o1 the resonance lines obtained from poly-crystal-
line specimens is determined mainly by the anisotropy of the g-factor,
Table 1 shows how the line width AH depends on the concentration of
Ti+++ in different solvents.
Card 1/5

86892
Electron Paramagnetic Resonance and B/056/60/039/005/Co6/051
Paramagnetic Relaxation in Livid and B029/BO77
Undercooled Solutions of Ti++ Salts
Concentration 811, Oe
of the solvent 0
in moles/1 77'K 200 K 295
Concentration Oe
of the Solvent
in moles/1 77 K 2DOOK72,a;7K
Glycerin solution TiCl--6H 0 11 Alcohol solution TiCl 611 0
2 3 2
2 54 60 63
1 32 35
0-5 35 20
0.5 17 18 - 0.25 27 10
0.25 14 17 10 0.1 17 10
0.1 13 16 10 0.05 16 10
0.01 13
16
16 10 0.01 i 10
The intensity of electron paramagnetic resonance decreases considerab-
ly during the transition from an undercooled state into a liqu:.,d state.
For undercooled solutions of TiCI 3' 6H 20 the line of electron paramag=
netic resonance is very asymmetric and shows a second unresolved
Card 2/5

86892
Electron Paramagnetic Resonance and SP054_/6G/039/CG5/0G6/C5_
Paramagnetic Relaxation in Livid and B029/BO77
Undercooled Solutions of Ti++ Salts
absorption maximum. For V - 9460 Mc/sec Table 2 is valid;
gil OL geff When the temperature of the under-
cooled solution rises, the width of
770 K 290'K the line and the asymmetry of the
- 1i
id
h
th
d
en
curves
e
ecrease; w
ju
Glycerin solution of TiCl '6H 0
2 state is reached, the lines are sym-
3 metric and narrow. At -400 0K the f-
1.99 1.93 1,95 quency dependence vanishes. In paral-

Alcohol solution of TiCl_,6H 0 lel fields,, an absorption T"(H)
s
2 exists at 300 megacycles in a 2
2.00 1.90 1.94 solution of TiCl 3* 6H20 in glycerin
at 770K, which is caused by spin r elaxation, At a double dilution of
this solution, the intensity of ab sorption is nearly zero. More de-
tails are given. AH for curves of electron paramagnetic resonance in
c6acentrated glycerin and alcohol solutions is caused by magnetic di-
pole-dipole interaction. In dilute solutions, the line width which is
Card 3/5

86892
Electron Paramagnetic ReFonance and S/056/60/039/005/Do6/'c,';-
Paramagnetic Relaxation in Liquid and 3029/3077
Undercooled Solutions of Ti.. Salts
independent of the concentration, is due to the anisotropy of the g-fac~-
tor and the contribution of the magnetic moments from protons of sur-
rounding molecules. The spin-lattice relaxation contributes toLH ac-
cording to f 1/y, . The transition from the undercooled solu-
tion to the liquid state influences the motion which causes a decrease
of the line width. At 9460 megacycles, the shape of the curves for
electron paramagnetic resonance is typical of ions with a strong iso-
tropic g-factor. The shift of spin-spin relaxation toward lowerfrcquen-
cies with a decrease in concentration indicates an increase of the
spin-lattice relaxation time Q1. This was explained by the th-3-rinal re-,
servoirs of N. Bloembergen and S. Wang. The absence of electron para-
magnetic resonance in silicate and boron glass indicates the presence
of tetravalent titanium in these types of glass. The authors thank
B. M. Kozyrev for a discussion of the results, and Yu. M. Ryzhmanov
for assistance in experiments. There are 1 table and 17 referen:es:
5 Soviet and 12 US~
Card 4/5

86892
Electron Paramagnetic Resonance and S/056/60/039/005/Oo6/051
Paramagnetic Relaxation in Livid and B029/BO77
Undercooled Solutions of Ti++ Salts
ASSOCIATION: Kazanskiy filial Akademii nauk 53SR (Kazan' Branch
of the Academy of Sciences USSR)
SUBMITTED: June 17, 196o
Card 5/5

25698 S/181/61/003/007/020/023
B104/B203
AUTHORSs Avvakumov, V. I., Gariftyanov, N. S., Salikhov, S. G., and
Semenova, Ye. 1.
TITLEt Paramagnetic resonance in TiCl *6H 0 and Ti 4)3* 4H20
layers 3 2 2 (SO
FERIODICALt Fizika tverdogo tela, v. 3, no. 7, 1961, 2111 - 2114
k _, 11, 1215~ 1960), the authors had
TEXT: In a previous paper /ZhETF, 2
studied the paramagnetic resonance absorption of TiCl 3' 6H20 and
Ti 2(30 4)3' 4H20 salts dissolved in glycerin and alcohol at T = 770, 2000,
and 3000K. They had found an anisotropy of the g-factor. Here, they
report on experiments with powdery (fine-crystalline) specimens. The ex__~_
periments were made at 9594 Me/see and 270 Mo/sec at 770 and 2000K, with
the same salts as indicated above and with specimens in which these salts
were dissolved in diamagnetic Al salts at ratios of TisAl - 1:10 and
TiiAl = 1000. The results shown in Fig. la reveal that the g-factor
of Ti3+ is anisotropic at 770K; 91 . 1.91 and g2 ' 1.84. On heating,
Card 1/4

25698 5/181/61/003/007/020/023
Paramagnetic resonance... B104/B203
this line becomes symmetrical, and disappears completely above 2000K.
Between T - 770K and a temperature T up , the form of this line is temper-
ature dependent. T up is supposed at 100 - 1200K. At T = 2000K, the line
is symmetrical, the g-factor is 1.91tO.02, and the half-width of the line
&H = 376 oersteds. At 270 Mc/sec, this line is symmetrical at T - 770K,
and the half-width is 81 oersteds. The dissolved specimens (1000) have,
at the higher frequency at 770K, in contrast to the undissolved specimens,
a symmetrical line with g eff, 1.91tO.02 at a width 4H - 203 oersteds. At
270 Mc/sec, this line is narrower (4H = 38 oersteds). With further dilu-
tion of the solution, g eff and the line width remain constant. g eff
= 1.91tO.02 was determined on Ti 2(SO4)3* 4H2 0 at the higher frequency at
770K (undissolved specimen). Here, the line is symmetrical, the width is
209 oersteds (Fig. 2a). Also here, the line width does not depend on
temperature in a certain temperature range. T up is estimated with 2000K.
Above this temperature, this line becomes wider and disappears. In con-
trast to the above-mentioned chloride, the line width is almost equal at
Card 2/ 4

-25698 S/1-81/6*1/003/007/020/0-23 i
Paramagnetic resonance.... B104/B203
both frequencies. In the solutiah 100, the line width is 147 oerpteds:
at the higher frequency, and 26-5 oersteds at the lower one. In a dis-
cussion of the results, it is',stated that the line width at the higher
frequency is determined by the anisotropy of the g-faqtor. The symmetry.
of lines of dissolved specimens at higher frequencies-is explained by_
inhomogeneities of the intercrystalline field. The authors conclude that',
the line width of the undissolved specimens is determined by inagnetic
dipole-dipole interactions. The dependendo of the line width on' the con-'
centration of magnetic paiticles is given as a proof. Since the paramag*-,,.
netic resonance absorption can be observed at 770K and overt the-authors . I !
conclude that the lower orbital triplet of Ti3+, which in the ground state
.is- in a field with cubic symmetry, is strongly split by fields of lowe*r
symmetry. If,.the T13+ ion is in an octahedral environment, the crystal
field c~n have no axial symmetry but only trigonal symmetry. It is also
possible that the Ti3+ ion is ih.a tetrahedral environment. The autlio'rs
thank S. A. AlItshuler and B. M1. Kozyrev for a discussion of the results..
There are 2 figures and 4 references: 1 Soviet-bloc and 3 non-Soviet-bloc.
ASSOCIATION: Kazanskiy filial AN SSSR (Kazan' Branch of the AS USSR)
Kazanskiy gosudarstvennyy universitet im. V. I. Ully;ahova.-L
Card 3/4

698-
S7,81/61/003/007/020/C,2.3'.
Paramagnetic resonance... B104/B203.:
Lenina (Kazan' State University imeni V. I.-UllyanoV-Lenin).
SVBMITTED: January 7, 1961 (initially)v
February 27, 1961 (after revision)
Fig. 1-Curves for the paramagnetic hg.' 2s Curves for the pari-
resonance absorDtion of undissolved magnetic resonance absbrption'
TiCl 3' 6H 20. of undisscf1ved Ti2(SO A'4H2 O~
Legendj (a) 9594 Me/sec; (b) 270 Mc/sec. Legend as in Fig. 1.
A
q, 9Z
a
Card 4/4
2_

AVVAKUMOV, V.I.; GARIFIYANOV, N.S.; SEICNOVA.) Ye.l.
Electron paramagnetic resonance in trivalent titanium halides.
Fiz.'met. i metal-loved. 12 no.4:624 0 161. (MIW- 14,: 11)
1. Kazanskiy filial AH SSSR.
(Titanium halides)

S/056/61/041/002/003/028
B102/B205
AUTHORS: Gariflyanov, N. S., Semenova, Ye-.- I.
TITLE: Hyperfine structure of electron paramagnetic resonance
lines in subcooled solutions of Ti... salts
PERIODICAL: Zhurnal eksperimentallnoy i teoreticheskoy fiziki, V- 41,
no. 2 (8), 1961, 337 - 339
TEXT: Following a series of publications (ZhETF, _12, 1215, 1960; ZhETFj,
.a, 1551, 1959, e&c.) the authors report on investigations of the hyper-
fine structure of epr lines in liquid and subcooled solutions of Ti 2(S0 1~) 3~
enriched in T147 and T149 to 43-3 and 71-5%, respectively. Measuremento
in liquid alcoholic and glycerin solutions of Ti +++ were made at
%0 - 9430 Mclsec and T - 295 0K, and in subcooled glycerin solutions at
'J - 450 - 270 Me/sec and T - 770K. The solutions had concentrations of
Card 1/ 3

2 71-1 E ED
B/056/61/041/002/003/028
Hyperfine structure ofOOG B102/B205
-0-05 mole/l. The measuring technique has been dascribed earlier. At
9430 Me/sec and 770K it was not possible to achieve resolution of the
hyperfine structure in subcooled glycerin solutionsg since the absorption
lines were broad and the splitting constants small. At V- 450 Me/see,
however, resolution could be achieved in the presence of strong magnetic
fields. At this frequency and at a temperature of 77 0K, the hyperfine
structure of epr lines of the 47 Ti +++ solution consisted of five peaks
(cf. Fig. 1a), which indicates that the nuclear spin, I, of this ion equals
5/2. The hyperfine splitting constant A is~ 30 oe, and can be determined
from the resolution of the hyperfine-structural peaks. AtV - 450 M'-'/sec
and T - 77 0K, the 49Ti ... ion in a subcooled glycerin solution exhibits
seven peaks (Fig. 1b). Acoordingly, the nuclear spin I amounts to 7/2 and
~1-30 oe. 1. At 9430 Mc/sec and T - 2950K, the hyperfine structure of the epr
lines of Ti49 in an alcoholic Ti 2(s0 4)3 solution will not be resolved. Thet
Card 2/3

27162
S/056/61/041/002/003/028
Hyperfine structure of.ee B102/32105
epr line consists of two components, one broad and the other narrow. A
graphical analysis showed the hyperfine splitting constant to be ja~02 oe.
In liquid solutions jaj= (A+2B)/3- By s.ubstituting the values of A and B
obtained from the data on the hyperfine structure into the last-mentioned
formula, one findsjaj;~;11 oe. (IBI-2 oe). There are 1 figure and 7 refer-
ences: 5 Soviet and 2 non-Soviet. The two references to English-language
publications read as follows% R. ff. Sands. PhYB. Rev. 12y 1292, 1955; C. D.
Jeffries. Phys. Rev. ~2, 12629 1953-
ASSOCIATION: Kazanskiy filial Akademli nauk SSSR tkazanf Branch of the
Academy of Sciences USSR)
SUBMITTED: March 8, 1961
Card 3/3

GARIF'YANOV, N.S.-; SEMENOVA, Ye.l.
Paramagnetic electron resonance in some aqueous complexes of Tj3+
salts. Dokl. All SSSIR 140 no.1:157-158 S-0 161. (MIRA 14:9)
1. Fiziko-tekhnicheskiy institut Kazanskogo filiala AN SSSR.
Predstavlano akademikom A.Ye.Arbuzovym.
(Titanium compounds--Spectra)

SEMENOVA, Ye.l.
Some comvounds of trivalent titanium and their paramagnetic
resonance. Dokl. AIN SSSR 143 no.6:1365-1369 Ap '62.
(MIRA 15:4)
1. Fiziko-tekhnicheskiy institut Kazanskogo filiala AN SSSR.
Predstavleno akademikom A.'-,'e.Arbuzovym.
(Titanium compoun4a)
(Paramagnotic resonance and relaxation)

S/020/62/147/002/012/021
I;106/B101
AUTHORS: Gariflyanov, N. S, Kozyrevp B. M, Semenovi, Ye. I.
TITLE: Electron paramagnetic resonance in compounds of bivalent
silver
PERIODICAL: Akademiya nauk SSSR.. I)oklady, v. 147, no. 2, 1962,-365-367
TEXT: The e. p. r. spectra of some compounds of bivalent silver were
studied in order to confirm experimentally the strong covalent bond between
silver and the ligands which has been postulated by K. D. Bowers (Proc.
Phys. Soc. A, 66, 666 (1953)) for [Ag(Py)41 S208 , and to ascertain the strong
exchange interactions between the 4d-electrons; which are expected in
analogy to Cu Ii compounds. Results: Fine crystalline Ag(c 5K5N),,S208 (A)
showed at 450 Mcps and 77 0K a peak with g - 2.15, crff - 26 oerst.' Thisp and
also the independence of the coefficient of paramagnetic susceptibility
tY~_;ofl'ai0-indicate an exchange interaction between the 4d electrons. At
9320 MCP8, 77 and 295 0K a line with g,, - 2.17+0.01, gi - 2.08+0.01 was
Card 1/2

KUCHERYAVENKO,- N.S.; SEMENOVA, Ye.I.
Rate of* nuclear relaxation as dependent on the symmetry of the T13f
complex in aqueous solutions. Dokl. AN SSSR 152 no.3:662-664 S
163. (MIRA 16:12)
1. Kazanskiy pedagogicheskiy institut i Fiziko-tekhnicheskiy institut
Kazanskogo filiala AN SSSR. Preds7tavleno akademikom A.Ye.
Arbuzovym.

USSR/Cosmochemistry. Geoch:amistry. Hjdrochemi.stry. D
Abs Jour : Referat. Zhurnal Khimiya.. No 6, 1957; 18903.
Author : Ye.I. Semenov.
Inst : --- - -
Title Soconite in Alkaline Pe~Vnatites.
Orig Pub S~rmposium Kora v,-, Ivyotr_J':.va,1iy~t., V~jp. 2, M. , AN SSS-R,.
1956, 1,,;9-183.
Abstract Soconite was discovered in pegmatites of the Lovo-
zerskiy railge (Kola peninsula). Its monominer-al secre-
t.Lons connected with the oxidation of sphalerite at-
~ain the dimensions of 50 x 30 em. The results of
chemical, sp-ectral, thermt~l, X-ray, chromatographic,
microscopic and electron-microscopic analyses are cit-
ed. Chemical composition (in %): Si02 35-10, Al
203
0.401 Fe 0 0.04, ZJ1O _35-74~ M90 2.38, MnO traces,
2 0+0-100)
CV.0 r_.03) 8rO 0.2'9, N.-tS_0.25; K20 0.14, H2
6.20, H20- 10.77, total 99.34. La, Pb, Cu and Be were
~:tdd.,:tioiially disco-.-ered by spectral analysis. The
Card 1/2 -15 -
Abs Jour Referat. Zhurnal Kbiml~a, No 6.1 1957, 18903.

USSR/ Coamochr--mistry. Geochemistry., Hydrochemistry
Abs Jour Referat a-ur - Khimiya., No 4, 1957, 11512
2,,!P'-; AI,O 1.68; 1,00; Fe
3 304 5-h4; 13-15; MnO 27.65; 23.6o; MgO 2.9 18;
1.6~jl cao 3.6o; 1.145; BaO, not determined; 0.32; K20 4-38; 5.63; NA20
2.14; 2.14; H20+' (11 &) 3.84; 3.90, ~20- 1.08; 0.80; F 1.22; not determi-
ned; sum 100.49; loo.2.8. In addition were determined: by roentgenospec-
tral method 1% Sr, 0.4' Rb, 0.1~ Ce and 0.1%-Nd; by spectral mathod veak
I"
lines of Be, Zn, Ga and Tat Crystallochemical formulas according to two
P-rAlys"s; ~KO.64 Na 0.104.12 ("n.69Feo .47 M90-51 CaO.44) 4 ll(Til.00
Zr 0407 NbO-03)1.10 C"'3-75 Al 0.22 Ti 0-03- 014-7- (FlOH)2; ("0.83 NaO.47
Ba ~!Mn Fe MgO.28- Cao (TiO.90
0.01 1.21 2.28 1.19 .18.)3.93 '0.13)1-03
CS, 3,185 Al 0-14 Ti 0101014 -7 - (OH)2* One specific chemical analysis re-
2/3

USSF1 Coamochemistry. Geochemistry. 11~~rochemistry
Abs Jour -. Referat Zhur - Khimiya No 4, 1957, 1151-2
D.
realsa 4.35% NbI.30 - The. mineral has been named in honor of Soviet minsro.-
logists B.M. KuDl2tskiy and E.M. Bqnshtedt-Kupletskaya wbo were the first
to investigate Soviet astrophyllites.
tIp-
3/3

---------------
USSR1 Cosmochemistry. Geochemistry. Hydroc4emistry
Abs Jour Referat Zhur - Xhimiya, No 4, 1957, 11507
Author Semenov Ye..I., Bonshtedt-Kupletskaya E.M., Moleva V.A., Sludskaya N.N.
Inst -Ac-PI-em-To-F-Sciences USSR
Title Vinogradovite -- A New Mineral
Orig Pub Dokl. AN SSSR, 1956, 109, No 3, 617-620
Abstract In 12 pegmatite cores of Lovozersk and Khibiny Alkalin& massifs
(Xola peninsula) has been discovered 6 n6i 4neral -~; vih6gradovite,
named in honor of acaddmician'A.-P. Vinograd6y.'- The mfiieriLl is'pr6sent
in the forri-of finel~'acicular and-fin6ly fibrous formations up to 5
cm in size:
In contact-adjoiAing portions as fringes and psdudomor-
bhoses of ramsait6 and lampr6phillft6; iii-th6 defitral baxr~t, within ca-
vities-of dl~uaes of natrolite and arialcime;-oither associated'ainerals
of Pegmatite: aegirite,' nephelineP kidroc_liiieY' , eddialite,-a-patIite',' -po-
t Origin of vinogradovite is'hydxothdrmal.
lylithioni 8; neptunite etc'.
Syng6n~, ii monoclinic.' Coloration of aggreigatiils white' drysta16
J
alre colorl,~ss. Brittle, with uneven &iL6ture, perfect 616avage along
(010 Hardness (-~j 4, sp. gr. 2.878, 'in. p.,(--., 8o6O. Optically biaxial
1/2
D,

DUDYKINA. A.S.; SMMOV$ Is.I.
lovozero and Khi~imy massifs, a rare-metal biogeochemical region.
Tr~~ Inet. min., gookaim. i kristallokhim. red. slam no.1:35-37
'57. WU 11:6)
(rola Peninsula-Metale, Rare and minor)

SDMOTO re. 1.
Titanium and niobium oxides and hydroxides in the lovozero
alkaline Massif. Trudy Inst. min., geDIchim. i kristallokhim.
red, elem. no.1:41-59 157. (MIRA 11:6)
(Lovozero tundras-Metallic oxides)

Ien6opham in alkali pegmatites of the Kola Peninsula, Trudy Inst.
rft , gookhim. i kristallokhIm. red. elem. no.it6o-63 157.
(Kola Pbuinwala-le-mcophans) (MM 11:6)
(I'Sguatites)

sswov, Yo. I.
Gelbertrandite and spherob6rtrandite, new beryllium silicate
hydrates. Trudy Inot. min.,geokhim. i kristallokhim. red. elem.
no.1:64-69 157. (KIRA 11:6)
(IBertranaite) (Silicates)

SMONOV, Ye. I.
1480morphism and "camouflage" of rare earths [with summary in
Znglishl. Geokhimiia no.7:626-637 157. (MIRA 11:1)
l.Institut mineralogii, geakhimii i kristallokhimii redkikh
elementov AN SSSR, Moskva.
(Isomorphism) (Rare earths)

SHILIN, L.L.;SFIMOV, Ye.I.
7he beryllium minerals epididymite and andidymite in alkaline
pagmatites of the Kola Peninsula. Dokl. AM SSSR 112 no.2:325-328
Ja '57. (KIRA 10:4)
1. Institut geologii radnykh mestorozhdeniyc_petrografii, mineralogii
i geokhimii Akademii nauk SSSR. Predstavleno akademikom N. V.
Belovym.
(Kola Paninsula-Beryllium ores)

2,
20-5-52/6o
The First Find oiij~~~e U.S.S.R.
'..eervaya nakhodla. eTtidita v boyuze -Pussian)
PERNDic'.11 li, Do'-lady Akademii Nauk SSSR,1957,vol 114,17r 5,'J--, 11ol-11030I.S.S.R.)
A 3TST C T --loidite Na2Zr3i6O15-3H20 belonZa tothe rarost zkcon-nineral5-Un-
til recently it was only known from the basic pegmatites of South-
Greenland.The authors first discovered it in 1949 in the pegmatit-
es of the Lovozero-massif(of peninsula Kola).The so-called Titano-
elpidite fron the permatites of lChibiny (1926) proved to be a new
mineral -without rclation to elgilite.Elpidite occurs in the mentio-
ned. massif in the form of white radial accretions of long prismatic
crystals in the cavities of pink albite.The crystals are described
here.It is a biaxial mineral,soluble neither in HC1 nor in H2504
or ill-TO It is known that only one chemical analysis of the Gr
land 2p'idite was published (Lindstroem 1 .894), the second one is by
the third author from the Lovozero finding (1952).A eomparison of
the two analyses shows almost no differences-By spectral analysis:
H-afnium, beryllium,strontium,magnesiuL~l,manganese and yttrium was,
in addition, foLind in elpidite. The fairly high a 'ontent of niobium
in view of an almost cotaiplete absence of titanium is characteristic.
Thus,the possibility of an isomorphous replacement of zirconium by
niobium is confirmed.The results of thermal analysis indicate "zeo-
litic"characteT of the water in elpid-ite.It can,if made anhydrous,
Gard 1/2 absorb the .,.,atar.-_Por this rea-,on it would be more correct to write

AUTHORS: Semenov, Ye. I., Barinskiy, R. L. SOVI 7-58-4-4/13
TITLE: Peculiarities in the Content of Rare Earths in Minerals
(Osobennosti sostava redkikh zemell v mineralakh)
PERIODICAL: Geokhimiya, 1958, Nr 4, PP- 314 - 333 (USSR)
ABSTRACT: More than loo samples were investigated; they are from Ye. I.
Semenov, partly also from other geologists. Samples from
abroad were made available to G. P. Barsanov from the col-
lections of the Mineralogical Museum (Mineralogicheskiy
muzey AN SSSR). In the ~~ase of most minerals the sum of
oxides of the rare earths was separated by the analysts
A. V. Bykova, 0. F. Dorondova, M. Ye. Kazakova,, 11. V.
Kukharchik, I. S. Razina. The individual rare earths were
determined by X-ray spectral analysis by R. L. Barinskiy,
accuracy 5 - 7 %, sensitivity o,"! %. The results are given
in a great table.
In their paper the authors deal with the following sections:
a) The classification of the contents of rare earths. If
the contents of rare earths are plotted on a diagram and
Card 1/3 the points thus obtained are conne-.;ted the known toothed

30V1 7-58--4-4/13
Peculiarities in the Content of Rare Earths in Minerals
line is obtained; if, however, the even-numbered points and
the odd-numbered points are c~rnested, two sufficiently
simple curves with few maxima are obtained (usually from
1 - 2). These curves are given for a number of minerals.
The minerals are divided into th:ree types according to the
magnitude of the maximum.
b) Lanthanide couples. The ratio of the content of one of
the rare earths with even atomic number to the ratio of the
subsequent one is represented graphically.
c) On the classification of the rare earths. It is suggested
to draw the boundary line between cerium earths and yttrium.
oxides in mineralogical-geochemical respect between Tb and
Dy. Furthermore it is suggested to combine two elements in
one sub-group and to deno-be it according io the predominant
even-numbered element: Cezium group (Cep La), neodymium.
group (Nd, Pr)o samarium group (Sm, Eu), gadolinium. group
(Gd, Tb), dysprosium group (Dy, Ho), erbium group (Er, Tu);
and ytterbium. group (Yb, Lu). There are 5 figures, I table,
and 12 references, 4 of which are Soviet.
Card 2/3

sov/ 7-58-4--4/13
Peculiarities in the Content of Rare Earths in Minerals
ASSOCIATION: Institut mineralogii, geokhimii i kristallokhimii redkikh
elementov AN SSSR, Moskira
(Moscow Institute of Mineralogy, Geochemistry and Crystal
Chemistry of Rare Elemerts )AS USSR)
PRESENTED: November 6, 1957, at the Jubilee Meeting of the Scientist's
Council of the Institu,,_
SUBMITTED: December 28, 1957
1. Minerals--Analysis 2. Rare ear *th elements--Separation
3. Rare earth elements--Determination 4. X-ray spectroscopy
--Applications
Card 3/3

AUTH OR: -Semenov, Ye. I. SOV/7-58-5-6/15
TITLE: The Connection Between the Composition of Rare Earths and the
Composition and Structure of Minerals (Svyaz' sostava redkikh
zemell s sostavom i strukturay mineralov)
PERIODICAL- Geokhimiya, 1958, 11r 5, PP 452 - 461 (USSR)
ABSTRACT: This paper makes use of experimental results published already
earlier (Ref 1). Depending on-the crystal lattice the rare
earths enter the individual minerals in different quantities.
For their characterization the author uses diagrams in which
the percentage of the even lanthanides is entered. When the
points obtained this way are connected with one another a
curve is obtained which has characteristic maxima. Such curves
were plotted for bastnasite, monazite, euxenite, fergusonite,
zirconium, spessartin, sphene, orthite, pyrochlorine,uraninite,
"chinglusuite", and "churchite". According to the possibility
of the isomorphous penetration the author distinguishes
selective and complex minerals. According to the position of
the maxiLia different groups of selective minerals may be
distinguished: cerium selective minerals like monazite, bastna.-
Card 1/3 site, loparite etc., as well as the yttrium-selective euxenite,

The Connection Between the Composition of Rare SOV/7-58-5-6/15
Earths and the Composition and Structure of Minerals
chenotime etc. are wide spread; the gadol-inium selective
minerals are much rarer and they cannot be determined so
accurately. In minerals not belonging to the rare earth group
the composition of rare earths is determined by their closeness
of their ionic radii to the element being replaced. Thus, the
minerals of Sr, Ba, K are usually cerium-selective minerals
of Zr, Sc, Fe yttrium-selective minerals, and those of Ca-
complex minerals. The composition of TR may serve for diagnostical
purposesand for the identification of selective minerals. in
selective minerals the comrosition of TR is determined according
to the crystallochemical structure of minera~ls which limit
the isomorphism capacity, in complex minerals it is determined
according to the medium and the composition 6f TR in the
initial melt or solution. There are 1 figure and 9 references,
5 of which are Soviet.
ASSOCIATION: Institut mineralogii, geokhimii i kristallokhimii redkikh
elementov AN SSSRI Iloskva(Moscow Institute of the Mineralogy,
Geochemistry and Crystal Chemistry of Rare ElementsAS USSR)
Card 2/3

The Connection Between the Composition of Rare SOV/7-58-5-6/15
Earths and the Comnosition and Structure of .14-inerals
SUBMITTED: January 14, 1958
Card 3/3

SEMENOV, Ye.I.; KAZAKOVA, M.Ye.; SHOTOV, V.I.
"Seidozeritel" a new zircon mineral and other minerals of the woehlerite
group in alkali -pegmatites. Zap. Vses. min. ob-va 87 no-5:590-597
158. MRA 12:1)
(Zircon) (Woehlerite)

SEMENOV, Ye.l.
Rhaldophanite group minerals in alkaline massifs. Mat.po min.Koll
Poluost. 1:91-101 '59. (MIRA 15.,2j
(Kola Peninsula-Rhaldophanite)

SEMENOV, Ye.I.
Mineralogy of alkaline pegmatites in the Khibiny Mountains and
Lovozero Tundras. Mat.po min.Koll.poluost. 1:102-106 '59.
(MIRA 15-2)
(Kbibiny Viountains--Pegmatites)
(Lovozerolundras-Pegmatites)

SEMOV, Ye.I.
Zirconium content in titanl~ minerals. Trudy Inst.min., Feokhim.i
kristalokhim.red.elem. no.2:87-92 '59. (MIRA 15:4)
(Zir~conium) (Titanium)

SEMOV, Ye.I.
Isomorphous series "labuntsovit" - "nenadkevichit.11 Trudy
geokbim.i kristalokhim.red.elem. no.2:102-109 '59.
(Kola Poninsula--Y-inerals) (Isamorphism)
Inst.min.,
CURA 1~:4)

SEEMENOV, Ye.I.
Minerals of the montmorillonite groUD in alkali massifs. Trudy
Inst.min., geokbim.-i kristalokhim.red.elem. no.2:124-137 '591~o
(MIRA 15:4)
(Lovozero tundras--Montmorillonite)

SEMENOV, Ye.I.
Possible new rare earth fl.uocarbonate. Trudy Inst.min., geokbimA
kristalokhibi.red.elem. no-2:181-186 t59. (KRA 15:4)
(Kirghizistafi--Rare earth fluocarbonate)

SDMNOV. Ye.I.: SMA, I.D.
Geological age of the Iiovozero and other alkaline masnife of
the Kola Peninsula. Trudy IGEM no.28:138-141 159.
04M 13:4)
(Kola Peninsula--Rocks, Igneous)
(Goclogical time)

PHASE I BOOK EXPLOITATION SOV/5740
Akademiya nauk SSSR. Institut mineralogii, geokbimii i kristallokbimli redkikh
elementov
Voprosy mineralogii, geokh-1=1i i genezisa mestorozhdeniy redkikh elementor
(Problems in Mineralogy, Geochemistry, and Deposit Formation of Rare Elements)
Moscowj, Izd-vo AV SSSR, 1960. 253 N (Series: Its: Trudy, vyp. 4) Errata
printed on the inside of back cover. 2,200 copies printed.
Chief Ed.: K. A. Vlasov., Corresponding Member., Academy of Sciences USSR;
Resp. Ed.! V. V. Lyakhovich; Ed. of Publishing House: L. S. Tarasov;
Tech. Ed.: P. S. Kashina.
PURPOSE: This book is intended for geologists., mineralogists, and petrographers.
COVERAGE: This is a collection of 23 articles on the formation,, geology.,
mineralogy, petrography,, and geochemistry of deposits of rare elements in
Siberia and [Soviet) Central Asia. The distribution and characteristics of
rare elements faund in these areas as well as some quantitative and qualitat-
tive methods of investigating the rocks and minerals in which they are foundy
Card 1/6

Problems in Mineralogy (cont.)
SOV/5740
or with which they are associated., are discussed. Two articles present an economic
investigation of the possibilities of industrial extraction and uti-Uzation of
celenium, tellurium, and hafnium. No personalities are mentioned. Each article
is accompanied by references.
TABLE OF CONTENTS:
GEOCHM41STRY
Garmash, A. A. Peculiarities in the Distribution of Rare Elements
in Po;Lymetallie Deposits of the Zmeinogorsk Region of Rudnyy Altay 3
--Semenov, Ye. I. On the Content of Lithium and Rubidium in Minerals
~f--Alialinie`-Pegmatites of the Lovozerakiy Massif 20
Badalov, S. T.,, and S. Ra7matov. On the Geochemistry of Selenium and
Tellurium in the Ore Deposits of Almalyk 24
Gorokhova, V. N. On the Content of Rhenium in Molybdenites of the
Kadzb,aran Copper-Molybde Deposits 28
Card 216

Problems in Mineralogy (Cont.) SOV/5740
. RALOGY AND PWROMLAM
Yesikova, Ye. M... and 1. 1. Nazarenko. Pyrochlore of the Vishnevyye
Mountains, Its Paragenetic Associations,, and the Peculiarities of Its
Chemical Composition 33
Zhabin', A. G.P G. N. Mt1kh1tdinov., and M, Ye. Kazakova. Paragenetic
Associations of Accessory Minerals of Rare Elements in Exacontact
Fenitized Miascite Intrusive Rocks of the Vishnevyye Mountains 51
Zhab:Ln,, A. G. On the Separation Time of the Minerals Widbium, Zirconium,
and the Rare Earths in the'Granite Pegmatite of the Blyumovskaya Mine 74
Semenov, Ye. I. Gelzirconium in AlkaUne Pegmatites 85
Korldn, V. I., Yu. A. Pyatenko, and A. V. Bykova. On Britholite of the
Alkaline Rocks of SoutheAstern Tuva. 90
Card 3/ 6

Problems in Mineralogy (Cont.)
SO7/5T4O
Lyakhovichp V. V., and A, D. Chervinskaya. On the Character of the
Distribution of Accessory Minerals in Granite Massifs 94
Lyakhovich, V. V.., and V. I, Woneshnikova, On the Effect of Late
Proceeses on the Content of Accessory Minerals in Granitolds 3.10
Ivanov., V, V.,, and 0. Ye. Yushko-Zakharava. Discovery of Franakeite
in Yakatiya 131
Zuyev) Vo N,p and A. V. Kosterin. Yttrof1write From the Dapq#lto of
[Soviet] Central Asia 136
Podporinao Ye, K, Crystallographic Forms of Celestine From the
Gulisayekiye Deposits of Strontium in the Tadzhikokaya 00 139
WOLOGY AND =MIS OF THE DEPOSITS OF RARE EIMN
Kuzlmenkop M, V. Genetic Types of Deposits and Ore Manifestatione
of Riabium and TanWum 142
card 4/6

Problems in Mineralogy (Cont.) SOV/5740
Zhukova., A. S. On the Problem of Genetic Types of Germanium-Bearing
Deposits 17k
Tikhonenkov., I. P.,,and R. P. Tikhonenkova. Contact Rocks of the
Lovozerskiy Massifo Their Genesis and the Peculiarities of Distri-
bution in Them of Rare Metal Mineralization 185
Volochkovich, K. L. On the Pioblem. of the Structural Position of the
GornoaltayBkiy Rare Metal Province 203
METHODS OF INVESTIGATING ORES AND MINERAIS
Lebedeva., S. I. Rational Method of Quantitative Determination of
Disseminated Beryllium in Greisen Ores 209
Rodionov, D. A.j, S. F. Sobolev.,_B. P. Zo3.otarev,, and Ye. V. Vlasova.
On Accidental Errors of Quantitative Mineralogical Analysis of Ore
Sli s and Concentrates 214
Card 5/6

Problems In Mineralogy (Cont.) SOV/5740
Loginova,, L. A. Experiment in Measuring the Optical Constants of
Gdrmanite and Renierite 224
ECONCNICS OF RARE ELENOTS
Leksin, V, W, Prospects in the Industrial Extraction of SeUnium
and Telluriun From the Products of Copper-Molybdem~n Ore Processing 235
Kaganovich., S. Ya. 11afnium. (Economic Survey) 246
AVAILAWZ: Library of Congress
Card 616 Jk/dvm/nas
11-14-61

.-UMENOV, Y e. I. : BYKOVA, A. V.
Beryllooodalite. Dokl.AN SSSR 133 no-5:1191-1193 Ag '60.
(HlRh 13:8)
1. Institut mineralogii, geokhimii i kristallokhimii redkikh
elemontov Akademii nauk SSSR. Prodstavleno tdmd. E.V.Belovym.
(Lovozera Tundras--Soda'Lite)

BESPALMY I.D.; SE~SNOV, Ye.I.
Absolute age of the Lovozero and other alkaline massifs, in
the Kola Peninsula. Biul.Kom.po opr.abs.vozr.geol.j'orm. n0-4:
77-8o 161. (MIRA 15: 1)
(Kola Peoinsula-Rocks, Igneous)
(Geological time)

SEMENOV, Ye.I.; TIKHOIENKOV, I.P.
I
Low-temperature ramsayite. Trudy R-ZRE no.7:91-95 161.
(MIRA 16:11)

SF14ENOV, Ye*Io; KAZAKOVA, M.Yeo
Zirconium opals from alkali pagmatites. Trudy D-OU no.7:
96-99 161.
Hydrothorit- i- th,,~ pegmatitas of' I'll- llovozero ai-kz2i tun-
draf,. . ~ 323--IZ9 (MIRA 16:11)

S/020/61/136/004/025/026
B016/BO75
AUTHORS: Semenov, Ye. I., Khun Ven-sin, and Kapitonova, T. A.
TITLE; The New Mineral Baotite
PERIODICAL: Doklady Akademii nauk SSSR, 1961, Vol. 136, No- 4,
pp. 915-916
TEXT: The authors report on a new niobium mineral "baotitell (named after
the town of Baotou in Inner Mongolia). Basing on the authors' data
Pen Tsi-zhuy had already published brief information concerning this
subject (Ref. 1). Baotite forms isometric, sometimes rectangular
pornhyr.4tic crystals, 8-10 cm large, in white quartz. It has distinct
cleavage faces in two directions, a brownish-blaak color, and in small
splinters, it is transparent. Specific gravity d = 4.42 (theoretically
4-74). "..'-4crohardness 769 kg/mm2 (about 5.9 of the Mohs scale). Optically
monoaxial positive, Ne = 2.16, N = 1.94, Ne - No = 0.22. An intensive
pleochroism from black-brown (Ne~ to greenish-yellow (NO) is visible.
Extinction is diagonal with respect to the cleavage faces. V. I. Simonov
Card 1/5

The New Mineral Baotite
S/020/61/136/004/025/026
B016/BO75
of the Institut kristallografii AN SSSR (Institute of crystallography
AS USSR) has determined the dimensions of the tetragonal cell ao = 19.68;
Co = 5.88 A, co/ao = 0.312. Volume of the cell v = a2c = 2205A3. The space-
group is I 41/a. Table 1 contains data of the Debye powder pattern, taken
by analyst 11. G. Bataliyeva. Chemical analyses are summarized in Table 2.
Specimen no. 1, contained small quantities of albite and other minerals.
Sr, Mn, V, Cu, Sn, and Cr could be discovered in "baotite by spectrum
analysis (weak lines). The empirical formula Ba2Ti7NbSi4 028 C1 with a
weight per formula unit of 1575 was determined by chemical analysis. The
number of formula units in the unit cell amounts to z = 3-72;~4. The
formula is of the general type Ba(Ti,Nb)2 S'07 (z = 16). V. I. Simonov
(Ref. 3), for the first time, determined the crystalline structure of
baotite and found fourfold meta-silicate rings of silicon-oxygen
tetrahedra Si4012 in it, as well as chains of titanium-niobium octahedra.
In this structure, chlorine concentrates in large cavities. Ye. I.
Semenov and Chzhan Pey-shant (Ref. 2) recently have described a new
mineral bafertisite BaFe2TiSi209 occurring in the Chinese People's
Card 2/5

The Ne'w Mineral Baotite S/020/61/136/004/025/026
B016/BO75
Republic6 This mineral also oontains Cl and Yb. In it, like in baotite,
neither the compensation of the isomorphous substituiion of Ti by Nb, nor
the part played by Cl, are satisfactorily explained. In baotite,
subdtitution according to formula Nb5tcl---;?Ti4+ is most probable, since
the number of atoms of Nb and C1 are approximately equal. Jointly vith
baotite, albite, alkali-amphibole, Aegrinp, bastndsite, galenite, and
pyrite in small quantities occur in quartz veins. These hydrothermaL
quartz veins are deposited in quartzites not far from an alkali-
granosyenite massif. The authors assume that the formation of baotite as
well as of other minerals occurring there is connected with the-alkaline
metasomatosis. Table I gives the numerical values of the inierplanar
spacings of baotite which have been obtained by the Debye powder pattern
(analyst N. G. Bataliyeva). Table 2 contains the chemical analysis of
baotite (analysts T. A6 Kapitonova and A. V. Bycova). There are 2 tables
and 3 references: I Soviet.
PRESENTED: July 27, 1960, by N. V. Belov, Academician
SUBMITTED: July 27, 1960
Card 3/5

BY'020/61/136/004/025/026
B016/B075
I OdPA3Cq M J Odpawq M 2
A KomnOHeHTU

Dec. %
ISar. Kojmq. rpynnmposKa sec. % SIAT. KOAPM
slo, 14,t7 0,236 0,236 0,96 1 13,20 0.220
TIO, 29.33 0 367 33,65 0,421
NbiO3 11,50 0:087
1 0, 492 2. 00 1080 0,081
Fe2()3 3.07 0,M8 1:75 O.M2
A1203 1,62 0,032 "eAbl
CrIO3 0.05 -
mgo 0,20 0,00-1
cao 0,41 0,007 -
BaO 37,55 0,244 0, 261 1,06;z 1 38.60 0,251
KiO 0.13 0,003 -
Na2O 0,20 0,007
H.-O 0,52 0,058
2,01 0,057 2 17 0 065.
-O=CI2 0,45 - .0:50

1, cvmmo, 100.31
Card 4/5

S10201611136100410251026
Legend to Table 1: 1) ourrent number; 2) 1;
3) d, A.
LegeUd to Table 2: 1) componefitsl 2) SUM;
3~ sample no.. 1; 4) vt%; 5) numberof atomsi
6 group; 7) sample no. 2.
Card 5/5
n. n.
A n.n.
I d. A
1 8 3,55 11 3 .1,959
2 3 3,34 12 2 1,828
3 6 3,17 13 S. 1,775
4 8 2,89 14 .5 1716
5 5 2.77 15 4 1:35S
6 3 2,69 16 10 1,337
7 6 2,49 17 5 0,180
8 8 2.24 18 4 0,937
9 3 2,04 19 5 0,833
10 4 2,00

3 '
-
:

i

Kli(.'U)lXV-, V.ff~ B-`-PrlSFTl R~Ll
in, I,ho-phoxltea. (-~,,&Ap-lia no.'. 434-4.39 162.
(KIRA' 1 7 "1
1. In&ti4,iA,,-, ---f IJneralogy. Geochemistry mid Crystal Chealetri
Rare Mc~jcow.
."Fare ( Ilo-phaTI tes)

SEMENOV, Ye. I.
-------
group minerals in pegmatit8s of the Lorozero alIcaline
massif. Trudy INGRE no.9:36-54 162. (MIRA 16:1)
(Io6vozero Tundras-Apatite)
(Lovoze-o Tundras-Pegmatites)

SEMRIOV, Ye. I.
Hallocysite-kaolinite group minerals in alkaline massifs.
Trudy ]MOE no.9:67-82 1162. (MMA .16:1)
(Rallaysite) (Kaolinite)

SEMNOV, Ye. I.; TIFMONENKOV, I. P.
CatapleUte and hydrocataplelite of alkaline pegmatites.
Trudy IMGRE no,9-.88-93 162. (MIRA 16:1)
(Catapleiite) (Pegmatites)

S 1OV, Yeyge4iy, jy~aAq~yich;,.VLASOV, K.A., glav. red.;
GERASE-!OVSKIY, V.I.,, do'ktor geol.-min. nauk, otv.
red.; TARASOV, L.S., red.izd-va; FRUSAKOVA, T.A.,
tekhn. red.; RUSIKOVA, O.M., tekhn. red.
[Rare-earth mineralogy; mineralogy, genetic types of
mineralization and basic characteristics of the geo-
chemistry of rare-earth elements] Mineralogiia redkikh
zemell; mineraloglia, geneticheskie tipy mineralizatsii
i osnovrye cherty geokhimii redkozemeltnykh elementov.
Moskva, Izd-vo AN SSSR, 1963. 411 p. (141RA 17:2)
1.Chlen-korresporident P14 SSSR (for Vla5o-v).

SEMENOV, Yo.I.; KOCHEMASOV, G.G.; ITMOVA, A.V.
Zirkelite and rosenbushchite from contact-metasomatic rocXs in
the Lovozero Tundras. Trudy IMGRE no.15:106-109 t63.
(MM 16:11)

YAKOVLEVSKAYA, T.A.; SEPENOV, Yel.
Some new data on chkalovite. Trudy Min. muz. no.14:265-267 163.
(MM 16:10)
(Chkalovite)

-SE14ENOV.* YeOI0
Pyrophanite, franklinite, and tungsten, manganese containing
minerals in pegmatites of the Lovozero massif. Trudy 1MGRE
no.16:176-179 163. (MIRA 16:8)

SEMENOV, re 0 10 ~
Rare elements -'n hydroxides of alumin-um, iron, silicon.,
and manganese from the weat-hering surface and mineral
formations deposited by hydrothermal solutions in alkali
maBBifS. Trudy IMGRE no.17215-.32 163. (MM 3.63 12)

SE119NOV., Ye.I.; DUSMATOV, V.D.; SAIASONOVA, N.S.
Yttrium-bBryl.lium minerals of the datolite group. Kristallografiia
8 no-4:677-679 Jl-Ag 163. (I-EIRA 16:9)
1. Institut mineralogii, geokhimii., kristallakhimii redkikh -alemen-
tov.
(Datolite)

SEMENOV, Ye.I.; SPITSYN, A.N.; BUROVA, Z.N.
Hydropyrochlore from Lovozero alkaline massif. .Dokl. AN SSSR 150
no-5:1128-1130 Je 163. (MIRA 16:8)
1. Institut mineralogii, geokbimii i kristallokhimii redkikh
elementov. Predstavleno akademikom N.V.Belovym.
(Lovozero Tundras-Pyrochlore)

ACCESSIOA NRt AP400460f" S/0020/63/b53/004/0913/0915:
AUTHORt Dusmatovo V. D.; Yefimovj A, F.; Semenov, Ye. Is
TITLEs First find of stilwellite in the USSR
SOURCEt AN SSSR. Doklady*, v. 153, no. 4, 1963, 913-915
TOPIC TAGSt rare earth mineral, stilwellite, CeBSiOst rare earth
borosilicate, cerium borosilicate
ABSTRACT- In the USSR-, stilwellite was first discovered in the
pegmatites and hydrothermal veins associated with the alkatin*e
rocks of the Alaysk Range in Tadzhikistan and the Inaglinsk massif
in South Yakutia. In contrast to the Austral:Van variety, this
stilwellite has 'a fairly well-developed crystal form. The sizes
range from 5 x 1 cm for the Tadzhikistan' mineral to 0.3-x 0.1 cm for
the Yakutian. The crystals are a combination of a hexaRonal prism -
(1120)(# - 30% p - 0) and rhonbohedron (1011)(f - 0% p - 56*). The
chemical composition of the stilwellite found in the pure crystalline
state is very close to the formula CeBSiO5 Only a small substitu-
tion of the rare earths by thorium (up to i.8% Th02) can be observed.'
!Card 1/2

SEMENOV, Ye.I.
Calcium and sodium carbonate bydrates. Kristallografiia 9 no.l:
109-110 Ja-F 164. (MIRA 17:3)
1. Institut mineralogii, geokhimii i ktistallokhimii redkikh
elementov AN SSSR.

VLASOV, K.A., glav. red* [deceased].;-~OV.,
_je.l., doktor geol.-
"Y
min. nauk, otv. red.; TIKHONENKOVA, R.P.~ a6.~-geol.-min.
nauk,. otv. red.
(Mineralogy and genetic characteristics of alkali massifs]
Mineralogiia i geneticheskie osobennosti shchelochnykh mas-
sivov. Moskva, Nauka, 1964. 193 p. (MIRA 18:2)
1. Akademiya. nauk SSSR. Institut mineralogii, geokhimii i
kristallokhimii redkikh elementov. 2. Chlen-korrespondent
AN SSSR (for Vlasov).

in the lkili. pegniati -~es of the ' atr'm
S &--i1 regi on, Dckl I .1,SSR 16 1 1_1 07--1408 Ao 165. fMIRA
1 '18, 1)64.

SDENOV., Ye.I.; KATAYEVA, Z.T.; RUDNlTSKAYA, Ye.S.
New data on yttrotungstite. Dokl. AN SSSR 163 no.2:447-449 Jl 165.
(~UIA 18: 7)
1. Submitted January 22, 1965.

-~n U-;~-

SEEMENUI , Y9 J , ~ A P. ; DYKOV A I~,V~
,N,F~w Dckl. AN 163 n0.3-718-719 JI 165.
(MIRA 18!7)
.1. Institut =Japralogil, geAhiml! i kristallokhimii redkjkb elementov.
Submitted 38, --1%- 4.

ACC NR,"___AP7oo68oh_-'
!AUTHOR: S ov T. (Le*cturer,
!(Candidate of technical sciences)
Candidate of technical sciences); Skorodumov, S.*A.
~ORG: None
TITLE: Determining the forces of deformation for sectional stamping of discs
SOURCE: Vestnik mashinostroyeniya, no. 12, 1966, 51-55
TOPIC TAGS: metal deformation, turbine disc, metal stamping, stress distribution
ABSTRACT: Experiments are conducted at the Central Scientific Research Institute of
Machine Technology to determine the proper deformation forces and ratios between punch
diameters for two-section stamping of disc forgings. Lead specimens were used in a
die with angular pickups on a fifty-ton hydraulic press and in a die with Vire pickups
on a 400 ton hydraulic press. The ratios of the forging dimensions were DIM, 12,
18. Theoretical curves are proposed for the distribution of normal contact stresses
which agree satisfactorily with the experimental data for stress distribution during
operation with central and outside punches. The formulas derived on the basis of
these curves for determining the forces of deformation during operation with central
and outside punches give fairly accurate results. It was found that the optimum ratio
of the diameter of the outside punch to that of the central punch is not a constant
Card 1/2 um 621.73.043

ACC-NR, ~Ii-766
1.55 as assumed previously, but that it varies from 1.737 to 1.619 vi~h a change in
DIH from 6 to 18. Orig. art. has.: 7 figures, 1 table, 8 formulas.
SUB CODE: 13/ SUBM DATE: None/ ORIG. REF:' 006
2/2

KORDY"UKOV, Vr-.-Iljy 311,14ENOV, YeA., kand. tekhn.
rede
jv~fjl-,Jng largG forgings by the hammer forging method]
Olj),t izgo4.-ovlA-niAa krupn:yl-.h T kovok svoboduoi kovkoi.
Moskva,, Ma--hinostroenie, 1965. 191 P. (MIRA 18a12)

SEMENOV, Ye.i.
----------------
Effect of changes of temporary parameters on the operating precision
of amplitude-pulse telemetering systems. Izv.vya.ucheb.zav.;prib. 7
no.5:47-50 164. (MIRA 17:12)
1. Leningradskiy elektrolvekhnicheakiy institut imeni V.1011yanove.
(IAnina). Rekomendovano kafedroy elektroizmeritellnoy tekhniki.

52MENOV, Ye.I.; FRID, B.I.
[Telephorxyl Telefoniia. Moskva. Voeaizdat, 1954. 360 p.(KM 8:]D)

SEMOV, Ye.I.
Determining the required characteristics for acoustic noise
resistance in voice channels. Blektrosviaz' 11 no.10:50-56
0 157. (MI" 10:10)
(Telephone)

8 (2)
SOV/112-56-3-4509
Translation from: Referativnyy zhurnal. Elektrotekhnika, 1958, Nr 3, p 159 (USSR)
AUTHOR: Fremke, A. V., Semenov, Ye. I., and Zhilin, V. N.
TITMi Amplitude-Type Cyclic Telemeter (Amplitudnaya tsikliCheBkaya teleizmeritelInaya
sistema)
PERIODICAL- Izv. Leningr. elaktrotekhn. in-ta, 1957, Nr 29, pp.45-51
ABSTRACT: A multichannel telemeter is described that has time division of channels and
amplitude modulation in each of them. Block diagrams of the systems with electro-
mechanical and electron primary elements are presented, as well as Eimplified
circuit diagrams of indiviuual up-its. Basic error of the system (without the primary-
element error) is i 2 to 22j%.
V. A. K.
Card 1/1
USCOMM-DC-61,o57

AUTHOR; Zemenow, Ye. I. sovlo6-58-9-13/17
TITLE: e Mu-tual ~Conniectio`nbetween the Informational Capacity
of a Telephone Channel and Articulation (K voprc;su o
vzaimosvyazi mezhdu propusknoy sposobnostlyu telefonnogo
kanala i artikulyatslyey)
I V.
PERIODICAL: ElektrosvyazI, 1958,NNr 9, pp 73 - 71F (USSR)
ABSTRACT: The informational capacity of a communication channel is
the Piost general parameter since it characterises not only
the economic effectiveness bat also guarantees the highest
quality and greatest reliability. Although up to the
i)resent time an objective estimate of the naturalness of
human speech is riot possible, articulation has been the
subject of many studies. At the basis of the studies on
"readability" of speech is its representation by means of
additive formants A in a frequency band A F consisting of
n elementary bands Aflq M2 .......... Un- According
to Ref 1 the determination of A is that of finding the
probability of occurrence of a 2-dimensional random magni-
lulde (formant) in a region lying above the resulting
Card 1/3 (taking noise into account) threshold of audibility at the

sov/lo6-58-9-13/17
The Mutual Connection bet-weer, the Informational Capacity of a
Telephone Channel and Articulation
Card 2/3
output of the telephone charnel. From this point of view
the formal expressier, for A is that in (1) where the
component probabilities are summed. Since the energy
spectrum of speech and noise within the limits of the
elementary frequency bands car, be considered as smooth,
con'U-inuous and non-coherent, then express'ion (2) for
signal/noise ratio can be substituted into the known for-
rou
la for the capacity of a channel for a continuous sigral
avil).g a no
h n-uniform frequency distribution. This is done
in (3). Thus by comparing (1) and (3) it is possible to
see a complete analogy between A and the channel Capacity,
C, The author ha-- calculated A and C for an ordinary
urban teleDhone channel from measurements with the TAH-9
equipment in the frequency range 300 - 27)) c/s. For zero
line attenuation the charxiel capacity does not exceed
16~CCC binary uni~,s/sec and. for-a line attenuation of
2.5 nepers it does not exceed 5,000, The corresDondina.
values of articulation formant were 0.51 and 0-33 while
the syllabic formants were 311% and 60%. If perfect
1~

sov/lo6-58-9-13/17
1 c- L, -,'tual Connection between the Informational Capacity of a
Tl'~ie 4-tonig Channel and Articulation
re-sroduction is required (i. e A Q~l) then, in the given
r0d,--e i a chz~nrlel GO, c;citY of 377800 bits/see is needed
whicK requires a ~signal/noise ratio of
42 db. For a rcal tele--hone channel such a ratio is
1-1
not even possible under ordinary room-noise conditions.
In the above axam-,'lle the signal/noise ratios were 20 db
and 5 db respectively.
There is 1 Soviet reference.
SUBMITTED: ADril 24, 1958
Uard 3/3