SCIENTIFIC ABSTRACT SHAMRAY, E.F. - SHAMRAY, V.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001548310001-8
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 9, 2001
• Sequence Number: 1
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

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'Thy~;iologi-cal Pelattionsahip% betweer- Vitamins -", P, M eui,-~ fi4rerocorricaZ
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Pepart to be- presented at Medical Society of J. E. PUP ".M, Czecu,
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Ik. vat.. k,*-. chim. 1936.340 02(in Prtiviv
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Three phaws tif.. Aid vulm. we for nacd in plot u of

, Vas originally believed. Below 10% Li a jolitt vAll. ij
v o d Jorrued. The cornpd. Mfg, in. at Cift" without dn-ompti.
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iin Frrn,h e(jua. iti2rrim of the At. Li %vstctn
-at "-mirtactrif lo Ille If tjj,-rm4I Allff joirr,"Ill1c.
(a fal onalysm. The At uwd con%w.-Ij of 111P.41% At,
-%I and W113"j. Fv amf tht- I I wal III,
Wf1I~Xj1fftWd III&%. OR 1111V filitillhill Alld .41411111 Jklillt tO
the rXi4teme of 111, 1. AIH. prt-"~U-Iv imrstig.ted
hyA.Midler 1Z. MfJ,,:,Ukwm4e 13, 231(M-16it. A hithtt.,

unknown rute"ic betvr~n AIIA, I-j-phsw) and [.I I. 600
phawl. cormtpotutisix to 94 of. Li it 1711.6% it Oum"

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The song of alloys of Al wit!$ Mg and Cm in the field of
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'Tb, Axeirm of Mo7v of Allaisdalum with Zinc wist LiAlluum.
-I At Abild. N Ill: .1
allA F. 1. Mantra%, (I. 19U, lKinin.j. (21.104
,
itivestigateil the ;I&:,- haniviling pri,
hav" 00
ert oes at rt - -Ili and Oevat,d tell, lk-tAturtii of acries of it I uIll"llu it, Mile -lit Ill"",
00 Al.,v. taitanong the following ration of title to lithillill; IM ; 1, 37, 5: 1.
1:1!i: 1. 4:1. 1-11:1. 1:1-3. 1 A-2. Small Additions of lithillill ,in lead to
*0 it vinisideralilt- uvrva.-A, in the ap-hartivninir (if Alitininiurn title all"P. -00
I;rratvtt alwAute haritness (140-15k) Brinell) %aA attain(A b%- artilicially
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xiin, 20-413. litliturn U-54',
to-inj, the alloys: ilitic 26-75. lithium W25"u;
-
,, I-
64 .
ow Iti-mi. lithium (;P-ater joereentagir met%-&--* lit hardness due to
so w--iiuz am. however. prultord by small lithium additions tit lutIrr-tilic alloys
;::p to Wu zinu). while the greatmt lorrurritapm incruases are obtained at
00
1
gh lithium : mine rati(o. Thus. as the relative smomit of lithium increases =
so o the maxinium t-flects of natural and artificial ageitiv. are displacril in the
on-vtiun If dr,wasing ix-ret-litaLle of title -, lithium frion 12"', zinc [or
-1
00
lAry sli'lyi dow it to 3% title - lithium in the case of natural oig"sg. ur
i.i =
so, :
It -Ili ititic duton to 4",, iluir 1 lithium in the rase of artilit-itill agring.
1roo
00 4. 1 ii, grt-al,-t lio-n vntagr int-rra^- lit hoordnemot (about Nidr".) wat, obtained 6% -
; 00
Art.fi,t,ills ahwing the fulloisting alloys : title 2-SAI. lithium 1-50 (Briciell hartf z
00 r: zoo
WO'j7~1! ne- ^ft. or %~v
, ing title 1-32. lithimn 1-69 J-N-3); zill, 1-7.41. lithium
*to j. 2-24 (h2- 1); zin, it 72. lithinin 2-'-'.% (83-1.q. With incretioing lithinin : zoo..

00 rAtill. the quenching telilloi-ratain- for tho, talloys post, wip too 5go C..
ond the artificial lillcing tenlpemture from 75" to Mij, C. -.N. it. v.
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Psocrills A-C P&CORAMS mail
A
"On U* CwrWm-l&~dma of Ahmkima-Lithiss A11075. P. S. Moixecy
and F. 1. Shammy (Ittvat. Mad. Nawk S.S.S.R., 19W jKlAim-1. (6). 41D-
-resistance of a wries of aluminium-
410-11n RILMi3n.] The corrosion
lithium allova (0, 13-16 St.." s-f lithium) was Studied. Short-time laboratory -00
tk~t. in 0-5N-110 aml six-month tests, in Pu N*&Cl showed that the alloy
0 0 i-ontainiog 2 04 at..'!o of lithium is the most. eorrosion-Maistalit of all thI-
Alovs zatnimA. In order to explain this behaviour, all alloys were studied As**
1,-v & clectron-diffraction method. after annealing at 400' C. Onlythealloy
")-'ItALininS2-94at.-0* oflithium showed evidence of the presenct- ofa chemical
at the ou"
rfacr; the identity of this cornimund was not, however,
cilt'aEurishmi- 1'. K. not
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L L11FRATURE CLASSIFICATION
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Mechanical pr"erties of alloys of Al with Zo and Lo.
A. 11adaeva awl F. 1. Shainral. J. Appited Chrm.
00 S- S. R.) 16. IM-72119,P)WIlitfish 'lullsoaly)-1114.
o0 luthorit studied the Al-Zu-Li alioy sen" ill rriprct to -00
phr. and tech. properties. Alloy-. ill the teNtou of At .00
00 1
~1 ~.ln. have very zt~f niech. pI`Oj~f(iC%, V1IKViAllV
so after rolling and beat-treatment. Common resistimcc 1,, -00
~ra water decreawi with increaw of U tip t,o ipj~-Araiwr
J tit tw,,.ph*w ymetu after hivii the e-imAil- ,,
09 crtwle% a. the Al-1-1 side Of tilt W 41111111", IM1.
rhe stwy a( -I

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a t IQ It it it it it It 11 41"a r, 0" 0.
A1. L 01L1 4 1 j 1 1.a Pi.r4. A Y V IF AI AA K EL
00
11114 t, Alloys of Aluminjum wan ML~enmnm &W Lithium. T. A.
.00 1. Shmmir (1h.r. 11,skind. Khom.. till 1. 17, 2N, 241 Brit.
_TT7.-
Alinninolin rimizil-tion lithiull.
^Ihn. 114%log -1111-ith,us Iviog within the 0111111inilon did -Isitwo n-glon
00 van' I.- pn-.~A (it +~~ to the M41" Alm) PANI in ill, ?,tu, -04
j.-nitun- rmigr NWY41)1F'V. The merhanival pro1wrtiov of Aluminium-ning- 1_06
ll,tinm h1hinni all.-~vya (inAlp"ono f lithinin 3 .13"... nimxip~iwa : lithium up
l1v tx.t;g,r than th-OW (If Ow mm-spon4i;ng Almoinium -
1, 419-3 t 1) Rreonly oil
0
Inagn-itial all erv-have a op. gr. of2-49-2-71) and show eltingatioto 1,(0
::0 0
25 :11"" kith a tenAile twngto cof 2o-39 kg. Pi. win. afk,r haniening. The
n.,,itan". 1" M.A.Wat'r mrrnmi.m deen-Ames %ith incrt-minR lithium mment ill, A 0
t a tnagnerliunt : lithium ratio - 2-91, and then inerr",t beyond that of =0 0
g \~Zolllillill u uimjzm~iuln A1141VA; it decream-A under stn-m.
Z:e 0
00 -00
00
IF .40
t"tI -;e 0
-00
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-.00
A 4 S L Ae(TALIUPGKAL LITERIT601 CL&SSWKATICN
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lu U AT Z, LS* An I
it IT CO It OP ME K It R U K
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0
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as
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Mechanical properties of aluminurW
Al co(IIA1111111
Y
mapesium and Linc in the alaminum sotid-so ution field.

r. A. Kida"a and F. 1. Shaturil (lust. Gcn. and Inorg. -so
Chrin. Avad. .1ki.. Bull. -uad j,i. I -H-S.-S
Chs,,, -. Ink. 19-40, (1.11-1.4-Allov, Comg, :1 IX,
7
-00
, 1,-
`V1% -t Zol %%ith the %1g:Zn rmiVi varviog from 1: 12.
a*
Is. prol.-rti"
c
~t,tv prriml. and examd. for III
00 d artificiai tgiuK
vorrl.ion rr'b'tancr aftcr isatund ~,i
SLm Irmile streuxth, 4040 kg. tour ml. mm., Via% obt.iiiivd
00 11, .1loy, Contg. (Mg + Z11) VVith Nlx:Z1% TAIII.. =so
00 I.-twmit 1:5.4 and 1:1. '66 ividiLatcd that itictea-ttl
'Ircorth 1%~' cauwd not oilly by ppt[1. of NlKzt12 pll.t" a
00 but al,o by Al..Nljt,Zu4. vit: alloy, tuttim Kid g.xki rV -
00 'i'talwe to Corroion in NCA watcr but wvre wri,iiiv,: t,,
-
when under ten-swo.
t4m~ion in %%aler valm)r :tt 7o-liml
Rathillawt
so

us

IV
-
0
,i n r,
0
0 a 0 0 a 0 0 0 0 0 0 0 0 0 0 0 0
0
0 0 0 0 0 a 0 0 a a!* 0 0 0 0 a 0

~ T ~ t, "7 T
z . ~"i , ,.! .
"Ternar:i System," Part I. MeGhod of Working wl-th
1, 1 th 1 ta. '-,Iinary Systems, I--,-vest4y,-t Akademii Nauk S~'~SR Otdeleniye iililLi~hes?-Jkh Nalak
(11,147) V!cl. kl PT lo5!/616
Translat-ion 22 Sej~ 5"

TiA
SP: I,
!Yaw/ChemistrY - Systems, Termary Jan/Feb 1948
Chemistry - Therml Analysis
"Ternary System, Aluminum - Magnesium - Lithium,
Part II: Diagrams Showing Composition of Sub-
eidiary Gross Sections," F. I. Shamray, Inst of
Gen and Inorg Chem, Acad Sc-' USSR, 14 pp
"Iz Ak Nauk SSSR, Otdel Khim, Nauk" No 1-PA3-q~-
Subsidiary cross sections of ternary system alundnun-
magneaium-lithium studied by methods of thermal
analysis and microstructure, and photographs of
resultant diagram included.
we 66T32
r

"Ternary cy-tcm.," Part !I!. Bescr!~A'Or- CIP
and
Fro~:ection of L-I,uidiu; Curfa-t. JsoUerir,3 at
Al-adem, i i SSSR Otdelen 'Lye
a r, d (D-f ':ryst-al I li,.ation. I- Ya
2 1
NO.
Tranz,l' 2- -'e? :,4

ZELIKMAN, A.N.~ SAMSONOV, G.V., KREYN, O.Ye.; STEPANOV, I.S., inzhoner,
retsenzent-, TANANAYEV, I.V., retsenzent; POGODIN, S.A., professor,
doktor, zaaluzhennyy deyatell nauk-i i tekhniki, reteenzent; ROJE,
YeJe., professor, doktor, retsenzbnt, ABRIKOSOT, N.Kh, doktor
khimicheskikh nauk, retaenzent; SF-OMY. F.I., doktor khimicheakikh
4, " ~- Rr "
nauk. retsenzent; MOROZOV, I.S.. VINO(FaX khimicheakikh nauk,
retsenzent; BOOM, Te.A., kandidat khtmicheskikh nauk, retabnze-at;
NIKOLAYXV, N.S.. kandidat khImIcheskikh nauk, retsenzent; ZVORYKIN,
L.Ya, kandidat khimicheakikh nauk. retsenzent; BASHILOVA, N.L.
kandid-at khimicheek.kh nauk, retsenzent-, VYSOTSKAYA, V.N., redaktor;
'KARAYEVA, O.M., redaktorZ ATTOPOVICH, M.K., tekhnicheakiy redaktor
[Metallurgy of rare metals] Metallurgiia redkikh metallov. Moskva,
Goa. nauchno-takhn. izd-vo lit-ry po chernoi i tevetnoi metallurgii,
1954. 414 p. (MLRA 7:9)
1. Chlen-korregpondent Akademif nauk SSSR (for TanaWev)
(Metals, Rare-Metallurgy)

SHAMM, F. I.; KRYIOVA, Ye.Ya.
Aging of Rig - Zn - Li systen alloys on an --'A,-Dhass base. Trudy Inst.met.
no-3:218-244 158. OGRA 12:3)
(Magnf3sium-zinc-lithium alloys) (Phase rule and equilibriun)
(Metals, Effect of temperature on)

SHAIRff, F.I.; KIffLOVA, Ye.Ya.
Mutual solubility of zinc and lithium in magnesium. in the solid state
sit various temperatures. Trudy Inst.mot. n0-3:231-237 '58-
(MIR& 12:3)
(Solutions, Solid) (Systems (Chemistry))
=n~s ma vow= or um vmW (vz Ume) or tbe ImUtEt
UNd A2 bq%o Dbualwuua lwutww is. " awwr) atelm 31
SwAft" M Obt4awwo &MUVIAFAI =tau and GLUP, M& "Icachomical
w1b"s at lowastl4stun. am or the steal" Put"B to the reaectu'l of
SUNWOMU"Or as V10004ty " other abecWterlauce of b1wt On
Mogo MAU08UM In MUU, awkbg or mtaU An to ewws"W, 41MUMMOW
ewe 1A
Or MtSIA OL V631=6 Umg&Mt~. for MWWrIM
mdlstw~ wd far 4ewmialac t1w -1time point or u." ~x
M~# ~9%'Ml ~P~ W&U%Ul - it"I" &RtMUIUKU~ TJ7 UP
rofeven"S. wrUad, -d a4ft of, allap. gock be" Is SONOWNj.& by

PHASE I BOOK EXPLOITATION sov/5747
Vsesoyuznoye soveshchaniye po redkim shchelochnym. elementam. 1st,
Novosibirsk, 1958.
Redkiye shchelochnyye elementy; sbornik dokladov soveshchaniya po
kb-imii, tekhnologii i analiticheskoy khimli redkikh shchelochnykh
elementov, 27-31 yanvarya 1958 g. (Rare Alkali Elements; Col-
1ection of Reports of the Conference on the Chemistry, Technology,
and Analytical Chemistry of Rare Alkali Elements, Held 27-31 1
January, ig,--8) Novosibirsk, Izd-vo Sibirakogo otd. AN SSSR, 196o.
99 p. 1-1000 copies printed.
Sponsoring Agency; Akademiya nauk SSSR, Sibirskoye otdeleniye.
K!', _U
Amiko-m-etall rgicheskiy Institut.
ReEp. Ed.: T. V. Zabolotskiy, Candidate of Technical Sciences;
Members of Editorial Board- A. S. Mikulinskiy, Professor, Doctor
of Technical 3oience;s, A. T. Logvinenko, Candidate of Technical
Sciences, F. F. Barkova, Candidate of Chemical Sciences; Ed.:
V. M. Bushuyeva~ Tech. Ed.: A. F. Mazurova.
Card 1/5

Rare'Alkall Elemants. Collection (Cont.) so,~/5747
PURFOSE : VU5, book is J-ntended for chemical engineers and tech- -
nicians working in metallurgical and mining operations and
related enterpris~en.
00-VERAC-F.: 'T'A"',~e collection contains reports which deal with the
physical and analytical ohemistry of rare alkali elements and
their c~cmpound5 and their reactions with mineral ores and salts.
Methods of extraction and modern analytical tee'lllniques and
equipment are also diseussed. No personalitle5 are mentioned.
Rr:f,-renc-e,1 ac(;cApany Individual articles.
TABIa. (.,F 01,R-ITENTS-
Urazc-v, 0. G. [.r"eceazed IT. V. P'Iyushchev.. Yu. P. SJ.rp.::. ov,, and I. V.
3hakh-io (Moskcrakly in~st~-Itut tonkoy khimicheskoy telchnologii im.
Mv. I Lomono-5ova - Mo::,;,sc-,vr Tnstitutc- of Fine ChemJ.-,a--, 'T"eahnology
i-meni M. V. Lomoz.-o~-:-ovj. High-Temperature Modtfication of SpodLmere 5
Plyushchev-, V. Ye. [Moiicow Institute of Fine Chemical '-':echnology
Card 2/5

Rare Alkali Elements; Collection (Cont.) SOV/5747
Imeni Lomonosov]. Physicochemical Investigation of the Process
of the Interaction of Spondumene With Sulfates of Alkali Metals 15
Shamray, F.-I. and T. F. Fedorov. (Institut metallurgli im.
--B-dyR_ov__W_S~9SR - Institute of Metallurgy imeni Raykov AS USSR].
Thermodynamics of the Vacuum-Thermal Method of Obtaining Lithium 25
Klinayev, V. M. [Gosudarstvennyy institut redkikh i malykhm,-vwtallov-
State Institute of Rare and Minor Metals]. The Interaction of
Lithium With N-1,trogen 31
Petrov, Ye. S. [Sibirzkoye otdeleniye AN SSSR - Siberian Divi-
sion of the AS USSR]. Some Relationships in the Interaction
of Salts of Alkali Metals With Silica And Alumina and Proper-
ties of the Products Formed 43
Logvinenko, A. T. and G, D. Uryvayeva [Khimiko-metallurgi-
cheskly institut Sibirskogo otdeleniya AN SSSR - Institute of
Chemical Metallurgy of the Siberian Department of the Academy
Card 3/5

Ra're Alkali Elements; Collection (Cont.) SOV/5747
of Sciences USSR). Binding Building Material From Industrial
Wastes 51
Poluektov, N S and M. P. Nikonova. [Institut obshchey i
neorganiches6y*ulmli AN Ukrainskoy SSR - Institute of General
and Inorganic Chemistry of the Academy of Sciences Ukrainskaya
SSR). Use of Photometry-of-Flame Methods in Analyzing Ores
and Salts of Rare Alkali Metals 63
Zak, B. M. [Irkutskly in3titut redkikh metallov - Irkutsk
Inatitute of Rare Metalij. Methods of Determining Rare
Elements 71
Zakhariya, N. F. and Ts. A. Leyderman, [Institut ob-~-ilchey :1
neorganicheskoy Uimil A~! SSSR - Institute of General'*and
Inorganic Chemistry of the Academy of Sciences USSR]. Methods
olf Quantitative Spectral Determination of Rare Alkali Metals
in Ores and Evaluation of the Impurity Content in Ore Prep-
aratlons 75
C,-~ rd 4A

Rare Alkali Elements; Collection (cont.) SOV/5747
Koz1ov, A. S. [Khimicheskiy fakulltet Moskovskogo gosudarstven-
nokpuniversiteta - Chemistry Department of Moscow State University).
A New (Turbidimetric) Method of Determining Small Amounts of
Cesium With the Aid of Cesium and Cadmium Ferrocyanides 79
Galkina, N. K., and M. M. Senyavin [Institut geokhimii i
analiticheskoy kh'L,.nii AN SSSR - Institute of Geochemistry
and Analytical Chemistry of the Academy of Sciences USSR]
Chromatographic Separation of Mixtures of Alkali Metals 87
Zabrodin, N. I., A. A. Nechayeva, and T. V. Korobochkina
[VBesoyuznyy nauchno-lssledovatellakiy institut galurgii - All-
Union Scientific Research Institute of Halurgy]. The Content
of Rare Alkali Elements in Natural Salts of the Soviet Union
and Prospects of Its Utilization in Industry 97
AVAILABLE: Library of Congress (QP 172.A4V8)
JA/rsm./jw
Card 5/5 11-27-6i

67835
/Y. 1~2 0 0 SOV/180-59-6-13/31
AUTHORS: Dokukina, N.V., Polyakova, M.D., and,Shamray, F.I.
(Moscow)
~1- NbSi Sys teM AUoys
TITLE: Several Properties of the WS12 2-
PERIODICALs Izvestiya Akademii nauk SSSR,Otdeleniye tekhnicheskikh
nauk,Metallurgiya i toplivo,1959,Nr 6,pp 102-109 (USSR)
ABSTRACTt Alloys were prepared from powders containing 99.2% Nb7
99.7% W and 99.13% Si. Mixtures containing 23-37% Si)
1.2-76% W and 0.1~-62% Nb were prepared by hot pressingt
followed by are melting. The final compositions are
given in Table 1. Microsections were repared in the
cast stats and after 360 hours at 1000 9C followed by a
Slow (-001. Alloys containing less than 59.2% NbSi2
were ti,,o phased and greater than 59.2% N-,5i2 single
phased. The primary crystals of alloys on the WS12 side
had a long columnar-type structure, with thin films of
the second phase in the grain boundary. In the alloys
lying on the NbS12 side, the primary crystals were more
rounded. The alloys containing 29.3% NbSi2 had
Card approximately equal amounts of both phases. The heat
1/3 treatment coarsened the structuro of the alloys and
decreased the quantity of second phase in alloys

67835
sov/18o-59-6-13/31
Several Properties of the WS12 - NbSi2 System Alloys
containing up to 1.9% NbSi2. The microhardness of the
WSi phase was 1255-1280 kj/mm2. The microhardness of
100% NbSi2 was 1038 and fell to 780 kg/mm.2 with a
decrease to 71% NbS12 in the alloy. Further decreases in
NbSi2 content led to an increase in microhardness. The
Vickers hardness increased from 723 to 840 kg/mm'2 with
increase in NbSi2 content from 0.7 to 65%. Further
increases in NbS12 content gave a curve similar to, that
for microhardness. X-ray investigations showed only
NbSi2 content. The lattice parameter decreased with
increase Of WSi2 from 1.6 to 28.7%. The porosity of the
alloys varied from 1 to 7%. The electrical resistance
was found and calculated for zero porosity. The
resistance increases from 17.4 to 148.9 micro ohm/cm with
increase in NbS content from 0 to 48.5%. It then fell
to 23.2 micro =cm in the 98.4% NbSi2 alloy. The high
temperature strength at 1100 and 1200 OC in air gave poor
results. The oxide layer formed on the alloys is porous
Card and does not protect them from further oxidation.
2'13 Table 4 gives the melting points of various Aloys. An
equilibrium diagram was drawn from the above results

673' 5
SOV/180-59-6-13/31
Sieveral Properties of the T;I-,)i2 - NbLSi2 SYStGnI
(Fi-~ 7). The !'[Si2 - NbSi2 section of the W - Si - Nb
ternary system is pseudobinary. There is a uride range
of solid sz~Ditions Of IlSi2 in NbSi2, and eutectic at
about 29% NbSio.
There are 7 figures, 4 tables and 15 references, of
which 7 are German, IF English, 3 Savlot and 1 French.
SUBMITTED: July 20, 1959
Card 3/3

S1081 /62 /000/004/003/08 7
B1 491B 101
A UT HO R S'hamray P. I Ped orov T. F.
T
TITA.,Cj, The thermodynamics, of the vacuum-thermal method of preparing
littlium
PERIODICALI Referativnyy zhurnal. Khimiya, no. 4t 1962v 51, abstract
4-B337 (Sb. "Redk. shchelochn. elementy". Novosibirsk, Sib.
otd. AN SSSR, 1960, 25-29)
is
TEXT: The effusion method was used to study the equilibria in silico-
thermal reduction of lithium oxide in the presence and in the absence of
Dacilm oxide And in alumo-thermal reduction of lithium aluoinate.
Mineralogical analysis of briquet scraps
took place during the reduction-
2Li20 + Si + 2CaO = 4Li(gas) + Ca
4Li20 + 3i 4Li(gas) + Li4sio 4
card 1/2
showed that the following reactions
2 sio4(1);
(2);
25
3 0

S/081/62/000/004/003/087
Thz4! thc-ruiodynamics ol" the vacuum-thermal - B149/B101
-I'Li O-Al 0 2AI = 61,i(gav) +' 4A1 0 (3).
2 3
The experimental data were used to calculate the equations for the
dependence of '15he isobar potential on the temperature for reactions (1),
(2), and (3).
ZAZ,*o - -20c,',900 + 70-6T; 167000 - 115.6T; 312820 - 129-75 T.
The values of the isobar potentials of the entropy and enthalpy for the
formation of lithium oxide, lithium orthosilicate and lithium aluminat~~ we e
calculated from these data. LAbstracter's note: Complete translation./
Card 2/-2
0

ILI%
S-/5oq/6o/ooo/oO4/017/024
E021JI/E.106
AUTHORS. Shnmrav- F,I. . and Krylovia, Ye.Yau
TITLE~ The Mutual Solubility of Zinc and L-f-hilum in the
P-Phase of the ',,Ig-Zn--Li System in the Solid State
PERIODICAL~ Akademiya nauk SSS11. Institut metallurgii,
Trudy, No~ 4, 1960~ Metallu-rgiya, metallovedeniye,
fiziko-khimichesklye r,-.etody issledovaniya, pp.200-207
T EXT The solubility of zinc and lithium was investigated
in five sections:
I Mg: Lx 71~29 Zn - Li. ~ .1
1I Mg - Li 71-~29 Zn, L1 = 3 2
III Mg: Li 69.,31 ZncLj, = 1A
IV Nilg-,Li 67-33 ZnAi. = 2-3
V Mg -1.1 Li, 671,37; Z-n..Li = 17 ' 83
98-95',0* Li, 99 ~ 991" Zn and 99,91~~ Mg were used. The main method of
I ri 0
Investigation was by microstructural analysis,
In section 1, the limiting solubility in the P-phase by micro-
structural analysis corresponded to 375 OC and 16,8 weight 0/-0' zinc.
At 330 OC, zinc 'goes into so.lutaon, at 300 OC about 110/0'~
Card 1/ 2

S/509,,-'6o/ooo/oo4/ol7/o24
E021/E106
The Mlutual Solubility of Zinc and Lithium in the P-phase of the
I
Mg---Zn-Li System in the Solid State
"I
and at 250 OC about 7,0 The hardness increased with increase in
zinc up to 16.80/0' and then remained constant.
In section II the limiting solubiliLy from microstructural analysis
corresponded to 370 OC and 17~.' zinc, The solubi-lity at 350, 330,
290, 250 and 150 OC was 16, ih, 10.5, 7.5 arid 2.4 weight 0,1. zinc
respectively. The hardness of alloys in this section increased to
16.8% zinc and ttieti. remained constant,
In section III microstructural analysis showed that the limiting
solubility corresponded to 360 OC and 19 wel-ght % zinc. At 350,
250 and 150 OC, the solubility was 17; 6~7 arid 20% zinc,
respectively. The hardness increased up to 18,4cj~,, zinc.
In section IV the microstructural analysis showed that the 'Limiting
solubility corresponded to 385 OC and 19,27 weight P% zinc. The
solubility at 550 and 300 OC Was about .17 and 15'/'0' zinc,
In section V the limiting solubility corresponded to 320 OC and
18 -i-reigi-it ,"*) zinc,
There are 2 figures and 2 tzible5~
Card 2/2

S/509/60/000/004/018/024
EC)21/Eio6
AUT1101-IS: Shamray, F.I., and Krylova. Ye-Ya.
TITLE - Ageing of Alloys of the ~-Phase in the Mg-Zn-Li
Syst em
PERIODICAL; Akadepii~,a nauk SS31-U, 11IStIAUt metallurgii.
Trudy, No. 4, 1960, 'NatalLurgiya, tiietallovedeniye,
fiziko-khimicheskiye metody issledovaniya- pp.208-213
TF-XT. Ageing was studied at 125, 100. 750C and room
temperature, using the following seetions~
I INS -. Li = 71.29 Z11-1'i = 4'A'
Ii Mg~Li = 7i~29 ZniLl = 3:2
III Mg Li = 69-.31 Zn-L-L = 1,1
IV 'Mg Li = 67-33 Zn,Li = 2,-13
V Mg~Li = 67,35 Zn-Li = '1-7~83
At 125 OC there was a particularly marked -increase in the hardness
of the alloy from section I containing 16-6,,0,- zinc and 9-070%
lithium. After 3.15 hours an increase of 15 units on the Rocku-ell
C scale was observed, Alloys from this secLLon containing 3.31.
6.49 or 9.53,;t) zinc aged to a lesser degree and more slowly.
Card 1/'i

5/5oq/6o/ooo/oo4/o18/024
Eo2i/E.to6
Ageing of Alloys of the P-Phose in the Mg-Zn--L.i System
A similar ageing process was observed in 5ections II, III and IV.
In section II a maximum increase in hardness was observed with the
alloy containing 15,430,0' zinc and 9-840,'J lithium after 3-15 hours-
At 100 OC all the alloys were suscept-ible to ageing. The
character of' ageing was similar to that observed at 125 OC.
Alloys from sections I and III aged to a f.,rreater degree than the
others. In section 1. the maximuni increase in hardness was
9 units for the alloy containing 12.4'71,'& z.inc and 9,4io,. lithium
after one hour. At 70 OC All the alloys aged to a lesser degree
than at the higher temperatures. The alloys of the lost two
sections gave a maximum increase of hardness of 4
Natural ageing at room temperature -was carried out for daysz
Alloys of all the sections aged very slowly and the maximum
increase in hardness ,-.,as 4 - 7 units after 3 - 5 days. Ageing
practically ceased after 10 days. The corrosion resistance of
the alloys was also tested by immersion in a 3c,", solution of
common salt. Alloys of sections I and II containing 12~67 and
16.6,,,V! zinc had low resistance (1,,reight loss of Ill and 17.26 mg/cm2
Card 2/3

8963- 6
S/5oq/6o/ooo/oo4/ol8/024
E021/Elo6
Ageing of Alloys of the P-Phase in the NLIg-Zn-Li System
per day). Alloys of sections V and III containing 3-31, 6.49
and 6.67% zinc were relatively resistant (1.34, 4.15 and 6.91
mg/CM2 weight loss per day), but had lower hardness figures.
Alloys of section IV containing 10.080% zinc had good resistance
(6-31 mg/cm2 per day) and medium hardness, The lithium used
in the investigations contained 0.5%' sodium and 0.2% potassium
which may have affected the properties.
There aro I Zigure and 1 table.
Card 3/3

'KALININA, A~A., Sff_kMRAT, -!?j
veicochemieal investigation of the section,
Ph. sic - B4'G of the system
Ei - B - G. Trudy last.oet. n0-5:151-155 60. (MIRA 13.6)
(Silicon carbldej
(Boron carbide)
(Powder metallurgy)

.w
. BDOEM, TF. ;-SHANRAY, F.I.
Reaction equilibrium of lithium oxide reduction by the thermodynamics
of silicon in presence of calcium cxide. Trudy Inat.,met. no.5:
!62-165 i60. (WRA 13-6)
(Lithium)
(Silicon)
(Vacuum metallurgy)

86697
S/180/60/-000/006/007/030
E193/E335
AUTAORS Fedorov, T.F. and S ray,
11111~4 I I ~F- I ~-
TITLE. Refining of Metallic Lithium
PERIODICALI Izvestiya Akademii nauk SSS.,R, Otdeleniye
tekhnicheskikh nauk, Metallurgiya i toplivo,,
1960, No. 6, PP. 56 - 6o
TEXT; Having derived an ejcpression describing the variation
of the composition of the liquj-d and vapour phases of an ideal
liquid solution during the distillation process, the present
authors used it to construct thtretical curves which, for the
case of lithium containing its hief impurities, illustrate
how the composition of the residue and condensate should vary
in relation to the ratio between the weight of the condensate
(and residue) and the initial weight of the metal distilled.
These theoretical predictions were checked experimentally on
lithium containing 0.6% sodium and 0.04% potassium. In the
Pirst series of experiments simple distillation was studied under
various conditions of temperature, partial pressure of sodium
mnd vaquum employed, The results were disappointing in that,
Card 1/2

6o/oo0/00 007/030
tJL93/E335
Reflnlmg of MetAllic Lithium
irrespective of the conditions employed, it was found impossible
to reduce the content of the impurities below 0.1%. In the
next series of eXperiments, distillation with fractional
condensation in a'horizontal Column was employed. Vacuum of
5 to 6-x 10-4 Ulm Hg Ues used and the distillation process was
carried out at 700-80~ 'C. Under these conditions the fraction
condensed at 300-'400 1C contained."Iess than 0.01% sodium and
potassium. However~, no reduction in the manganese content was
attained by this method. Best results were obtained when
distillation was carried out in a' bubble-cap plate fractionating
column. This method reduced.the impurity content in the
starting material t~o les8 than 0.01%. There are 3 figures,
7 tables and 7 references-, Soviet and I non-Soviet.
~51)'BMITTED zApt'i.1 J., 1960
card '2/2

90 0 (4) 68120_
5M SOV/78-5-1 39/45
AUTHORS: Fedorov, T. F.1 Shamray, F. I., Nisellson, L. A.,
Petrusevich, I. -V-.--- - -"r . ..... 1-
TITLE: On the Production of Elementary Boron
PERIODICAL: Zhurnal neorganicheskoy khimiiq 1960, Vol 5, 11r 1,
pp 226-228 (VSSR)
ABSTRACT: After giving a survey of publications with reference to a paper
by F. I. Shamray and V. I. Xikheyev (Ref 6), the authors mention
that commercial boron has a purity of about 90%. Boron with a
higher degree of purity (~91%) is produced only in small
quantities. The author 's attempted to obtain pure boron by re-
ducing B01 3 with Zh. Thermodynamic investigation of this re-
action (Table, Fig 1) indicates that it may be carried out
within a wide temperature range. As boron chloride reacts SlGW3y
even with liquid zinc, Zn was evaporated in a device schemaiical-
ly represented in figure 2. The reaction took place in a
quartz tube heated to 10000. It was stopped as soon as the
cts (Figs 3,4).
tube was.,oompletely-fil:Lecl.with the reaction produ
Card 1/2 The latter were decomposed.in~o B, Zn, and ZnCl in quartz
2- . -

681 go
SOV/78-5-1-39/45
Qn the Production of Elementary Boron
ampoules by distillation at 10000. The boron, the purity of
which is not given, contained impurities of Fe, k1n, Zn, Al,
and Si. There are 4 figures, 1 table, and 16 references,
3 of which are Soviet. q1
SUBMITTED: May 31, 1959
Ca,rd 2/2

83126
S/078/60/005/009/009/017
BO15/Bo64
AUTHOR3, Charkashina; N. V., Nedumov, N. A., Shamray, F.
TITLED tem '~itaniu omium
Some Data on Alloys of the Sys m - Ar Iroll,
PERIODICAL Zhurnal ne 'organichesko,.- lchMii, 1960i Vol, 5. No 9.
pp~ 2025-2031
TEXT: ThR DhaSe diagram of the ternary system Ti-Cr-B was inve3tigated;
first, the nross sections Cr-Ti2B and Cr-TiB2 were studied (Tables 1. 29
composition of ;he mixtures). The samples were produced by mixing and melic
ing the powders and were investigated both metallographioally and with
respect to microhardness (on the nNT-3 (PMT-3) device), while the alloy,;
Cr-T12B were thermally analyzed with a device described in Refs. 10, 11.
~ha'se transformations were recorded by a differential thermometer (Fig.
while temperature was optically measured in an electric furnace (Fig. 2),
Figs, 3 and 4 show the microstructure photographs of some alloys, the dala
of the microhardness of the phases are given in Tables 3 and 4. At 20 a~%
Card 1/2

831-26
Some Data on Alloys of the System S/078/60/00511009/009/017
Titanium - Chromium - Boron B015/Bo6A
Ti B or TJB, a eutectic occurs in the structure of the alloyc An ln~rease
2 e
of the Ti2B or TiB2 content to more than 20 at% leads to the formation of
e~n..'n2
an excessive boride phase whose microhardness is between 1300 and 2070k
depending on the boron content, The reaults of thermal analysis sho-A that
apparently a ternary eutectic occurn in the system Ti-Cr-B whose formalion
temperature lies somewhat over 13000Cc Its composition could not be statedi
it is- however, very likely to lie in the range of 70 at% Gr and 30 at'lo
TiB . There are 6 figures, 4 tables, and 11 references: 3 Soviet, 5 US,
2
1 Germart, I British, and I Danish,
SUBMITTED.- June 20, 1959
Card 2/2

DOKUKINAJ, N.V.; �MIRAY,_F.,I
Phase equilibrium in the system W - A - Si and certain allov
properties. Porosh. met. 2 no.6:32-41 R-D 162. (NMA 15:12)
1. Institut metaUurgii Imeni A.A.Baykova AN SSSR.
(Tungsten-niobium-silicon alloys.-Metallography)
(Phase rule and equilibrium)

FMOROV. T.F.; -NMUMOV, N.A~; POLYAKOVil, M.D~; BRAMBAY,, F.I.
JData, on the ternary system titanium - boroja - chromium. Porosh. met.
Z no.6:42-49 N-D 162. (MIRA 15:12)
11. Institut, metallurgii imeni Baykova AN SSSR.
(Titanium-boron-chromium alloys-Metallography)
(Powder metallurgy)

'.7
S/03.0,/62/035/005/002/015
D204/D307
.4sellson, L. A., Petrusevich, I. V, Shamray, F. I.
and Fedorov, T. F.
Predaration of elemental boron by reductiOZZ Of its
halides with hydrogen
10 D I CI'l ZhUrnall prix"ladnoy khimii, v~ 35.)190'2, 984-989
T',-,e oresent ~-.,ork was carried out U
-to supplement ex4sting da-
-4 on
U~ . ` elemental B. Puri'ied BC1 BI and
-a on th-e )repara o. L 3) BBr,, . 3
H'.) aere used under anhydrous condiT. ions. The reactor consisted of a
c,,~art-_ tube erclosing a -jair of Mo electrodes connected by a Ta
U
w~:re 100 x 5 x 0.10 mm, on which the 3 was de osited. Temperatures
%,are varied from 800 to 14000C and the molar NX 3 ):(H2 ) ratios,
11
k1r.), were made 1:3-25. The interactions took place over 1.7 - 8
.'o-rs. The raze Of B deposition increased rapidly with temperature
fL " V U
and te-ded to be highe-- I'or lower ii. For BBr 3/H2 mixtures the
Card '11/2

-a 4 o.,- -7' e e,~, e In -, a I t
e ~:a I c)
c"'/O~-if)/'0-2/'03~c,/OC,5/002/0^1 5
D204/D307
- I
-ds o~' 3 4ncreased -cron--3106 at 80000 to --50~5 at 1300'C,
a -1 0 S I'lidebendent1v of n. Por a given -I,--emnPr,14.-IIT-P t1hp ratp of 3
increased 'n 'he order BC1 < BBr < BI Be-ween 800 and
9;~J'00C brolan, friable deposi-lu-s of amor;hous A werYobtauined for all
3-L-Ie-4ied, I -n B3r
'A r0, ,H mixtures. At hioher temperatures and n,
11,--a~Dhite 3
33 wa8 oroduced. and "me-allic" crystalline boron
Si-
oz-red at and abovf~ 120000 with 3 or less moles H le BBr
2/mo 3'
of for--ation of each 11"orm of B are bGi--;eved uo exis
t
and 31 -,H systems. There are 6 f-J'aures and 1 table.
2 3 2
January 25, 1961
I~ard 2/2

N. V. a SHAMRAY F. I.
DOKUKRIA) Y p
WOUNWA-MOW!
I~ivestigating the tAnmai7 system tungsten - niobium - silicon.
Trac'~v Inst. met. no.123132-W 163. (MIRA 16:6)
tTimff-sten-niobium-sili con alloys--MetaUography)
~Ph,se rule and equilibrim)

L 248oo-65 om
ACCESSIM
NRI
AT4046000
.
ENCU)SURES01.
-

fin -
/.7W w

Av

10
AV

A N
A
-C -
phase diagram for Cr-B alloys

_L___326?2-66__ EWT(m)/EVwTW/ETI IJP(c) -JD/WW/JG/WB/GD
ACC NR. AT6013571 (N) SOURCE CODE:
UR/0000/65/000/000/0421/0428
AUTHOR: Cherkashina., -N.V.; redorov, T. F..; Shamray, F. 1. -1 -i
4
ORG: Institute of Metallurgy im. Baykov (Institut metallurgii)
TITLE: The xj=onium-vanadium-boron pystem
il ;Lj -~' I
SOURCE: AN MrSSR. Institut problem materialovedeniya. Vysokotemperaturnyye neorga-
nichaskiye soyedineni.ya (High temperature inorganic compounds). Kiev, Naukova dumka,
1965, 421-428
TOPIC TAGS: zirconium, vanadium, boron, boride
0;[1jD09r41^'V
ABSTRACT: The phase structure and oxidation susceptibility of the binary sections,
ZrB2-VB2 and Zr-VB2, of the Zr-V-B system were investigated by x-ray, microhardness,
and gravimetric techniques. The individual diborides were prepared by fusion in a Tan
man furnace in a hydrogen atmosphere of the oxides and carbides according to formulas:
V,O, + BjC + 4C 2VB, + 5C0;
2Zr% + BC + 3C 2ZrBjj + 4CO.
The intercomponent molar ratio varied fron 1:9 to 9:1 in the case of the ZrB2-VB sys-
tem and from 1:19 to 19:1 for the Zr-VB2 system. For all the ratios, the ZrB2.-VBI sys
1/2

L 32672-66
ACC NRt AT6013571
tem was found to be a true two-phase one. After oxidation U hour heating in oxygen
at 12000C) the ZrB2-VB2 samples gained 0.5-2.0 weight due to the predominant formation
of Zr02- It was found that ZrB2 contributed to greater oxidation stability of the
ZrB2-VB2 alloys. It was found that Zr-VB2 alloys containing more than 50 mol % Zr had
a face-centered lattice with a=4.618 kx (where lkx=1/1.00202 A]. Alloys containing 80
and 90 mol % Z--- had a cubic face-centered lattice with a=4.63 kx. When subjected to
oxidation at 12000C all samples of the Zr-VB2 system corroded throughout and turned in-
to powder. Orig. art. has: 1 figure, 6 tables, 2 formulas.
SUB CODE: 1l/ SUBM DATE: 03Julfi5/ ORIG REF: 003/ OTH REF: 008
Card 2/2

SHRAYMAN,L.I.; SHAMRAY,G.A.
Discussing the duration of boring and blasting work in explod-
ing blast hole VV charges of increased diameter. U901' 30
n,3.4:12-15 Ap '55. (mLRA 8:6)
1. VNIIOVShS
(Coal mines and mining) (Blasting)

1-9AXYKAT, B.Z., dotsont; VINNIK. I.Y., inzh.; KARASIK, I.B., kand.
tekhm.nauk; TROFIMOV, V.P., gornyy inzh.; VOVK. A.A.. gornyy
inzh.; SHAMRAY, G.A.
Response to I.B.Detiatov's article "Evaluating tho Pfficiency
o9 explosivos." Ugoll 35 no-3:58-61 Mr '60.
MRA :L3:6)
1. Gosudarstvennyy nauchno-teklinicbesk-ly komitet USSR.
(for Zrofimov and Vovk"
(Coal mines and m-in)Ing-Explosives)

SE~--H-IAY, T.. A.
IITO -*L,',Ie ~4-uentlian of Acemulation of Terri:~ n.-as !-'a.-erial 4ri ' rth 'aucasus during the
,e 1 t, - 40 V
la)r., Dept. n-;-nera-lo,-~j ~. Rostov
I i,.,
~- , - P Era, " Toll. 0, 25, ' 0 - 7, 1939. -
Univ. A-r,,. V. 'i-'olotov, -1939--

S T '
Z, -- . r~ . f ---l C, - XItl or
, k ~, i
See: SED =rISKI-1, 1. D.
SedletsIdy, 1. D. and Sharway, I. A. - '31,5neralogy of the Sulin-
skdy fire cla;tsju Uchen. zapiski (Rost. rVD gos. im-t in.
1-folot"Ova), Vol- XI, 1948, P. 21-35 - Bibliog: 14 itemw
SO; U-31,566) 1.5 I-Lawch. 5.~, (Letopils 'Zh-Lum.-a lrwlffi Statey, iTa, 14, 1949).

YLA
-1-d,AY, I. A.
5
Shamray, 1. A. "Sketch of the natural 'building stone deposits of the Illsko-
Kholmskiy zone in the Northern Caucasus," Uchen. za.dski (Rost. n/D gos. un-t im.
l."olotova), Vol. XI, 1948, p. 73-84
SO: 10-3566, 14131-larch, 531Letopis tZhurnal Inykh Statey, No. 14, 1949).

SHAKRAY, I.A.
Paleogeaic glauconites in region of Stalingrad city as an example of
marine allochtonoua ore formation. DALAN SSBR 96 n0-3:621-624 my '54.
(MMA 7: 6)
' -Pred5tayleno akademikom H.H.Strakhavym.
(Staling,rad rmgion-GIR-twouito) (Glaiwonite-Stalingrad region)

c v
j6,~Irlineralogicat characteristics of quaternary loess loarn,
and their marine analogs in the Lower Don and Volga
Basins. 1. A. Shaniraiwand S. Ya. Orckhov../ Dnklady
Aknd. Nauk S.S.S. R. 85. ~ 17- '_!i1(I952)_-The petr~gmphic P
character of %videspread Inc-- deposits in S. Russia is given
bv a surprising abunflanee of light and heavy mineral., at
relatively unstable Inincr-als, e.g. the Cztsily Weathering felds-
pars (15 to 20% in light fractiotis), mica, chnicedony, glau-
conite, calcite, diatontaccous earth, hesides quartz. In the -
heavy fractions nre ilinvoite, less magnetite, Imeoxene,
Fe-0, hydrates, epidote. zoisfte, rlinozoisitc, fuWtcr par-
ticularly choracteristic. green and basaltic lioniblende. but
t-.ireactinoliteatititreiiiolite. l-"rii(lotein(tairpliit)oletiiiiier-
-,its occnr in larger atnts. in the tiorth-south direction of the C
deposition in the loess, but quartz, garnet, kyanitc, staurolit~t,
and sillinianite decrease. Below the loess occur refl-colored
clavish rocks, which (liff,-r from the loess especially by their
lo%v conteriLs of feld-par; epidote, amphibole, and pvroxene-s
are absent, irlicreas zircon, rutile, kyanite, and stattrolite are
distinctly enriched. Between the lorss loams and these red
rocks are brownish transitionz.1 linrizons which combine the
characteristice, of both. The older (Upper-Tertiary and
Palaeogenir) sediments also (to not contain amphiboles and
garoct,butsoniefeldspar. All these sedintents are typically
terrigenous (continental). but analogous loesslike rocks
occtir in the hasin of the Caspian Sea. of Old-Tertiary origin,
and in bed,.; of IM in. thickness. They are liclitic or psurini-_
initiv. tind siallific in client. char-arter. The fluirtz-feldspar
content may be 15 to 20%, and chalcedony and inicas are
also abundant. fit their heavy fractiotiq, epidote and
aniphiboles are characteristic, but black, bamltic horn-
blende is absent. 'rite partial or complete disappearance of
unstable minerals by weathering and inech. decay is observed
in the alluvions. There is a close analogy of these tonrine
layers, especially in the varieties of the Bakit and Khazaura
region with true loess. W. Eitel

~t 15-57-4-4830
Translat-ion L;"Zzopt-~ Referativnvy zliurnal, Geologiya, 1957, Nr 4,
P 11^4 WSMR)
AUTHOR,. Shantray, 1.. A.
TTTLE.a iviechanical Sorting Action of the ... Sea,as .a F.%ctor of
Se'dimmt Ace'umulation (Mekhanicheska'ya sortiruyushchaya deyatell
noi
W moryakak.faktor morskogo rudqS*op1eniya)
PERIODICAL: Vopr. mineralogii osadoch. obrazovaniy. Kn. 3-4.
Llvov., Llvovsk. in-t, 1956, pp 121-131
ABSTRACT: The formation of marine sedimentary deposits is
associated with hvdrochemical and hydrodynamic
processes. The latter process is highly important:
the author believes that the conditions of deposition
of a number of marine accumulations of limon'ite,
5iderite, bauxite, glauconite, etc., and the structu-
ral and textural characteristics of the ores indicate
Card 11/2 their allochthonpus nature6 The translocation of

Mechanicall So)--tlag Act-ion of thc- Sea Oont. ~ 15-57-4-4830
sediments accumulated or, the bottom of the sea and the mechanical
sorting associated therewith are important and necessary for for-
mation of such deposits. These processes occur on a large scale.
Lake iron ore deposits are a typical example of the concentration
of sediments as a result of mechanical sorting and displacement on
the bottom of a basin under the action of hydrodynamic forces.
Diager~esis plays an important part. The action of diagenesis con-
sists basically in structural alteration of sediment (as, for
instance, consolidation of ore depositions) which promotes the
processes of aorting and enrichment of ore material.
Card, 2/2 S. I. B.

OR M OV6 S.Yag SHAMRAY, I.A.
~ - ,-- N ~~ ', ~ ~. , Y,.,*e~
Tertiary phosphorites of the eastern Donets Basin and their petro-
graphic charrcterlsUcs. Dokl. AN SSSR 106 no-3-529-532 Ja '56.
(mLRK 9:6)
1.'Rostovskiy n-.,x Donu gosudarstvenn" universitet imeni V.H.Molutova.
I'redaqtavleno ;W..mdemikom N.M.Strakhovym.
(Donets lllauin--Apatite)

.SffAIARAY, I.A.z LAZAEGIVA, Te.P,
Palaogenic Coccolithophoridap and their Stratigraphic importance.
Dokl.Alv' SSSR -108 no.41.711-714 Je 156. (MLRA 9:9)
!.Rostovskiy, gosudarstvennyy universitet imeni V.M.Molotova.
Rred5tavleno aludemikon N.M.Strakhovym.
~Coccolithophoridae, Fossil)

AUTHOR SHAMRA'Y, I.A.,CR6KHOV, Sla. 2o-i-48/64
TITLE Th`e_M`oi,_olit41_cly Plastical Fhoophoritt Ores at the Periphery the South-
Eastern Donets- 'oasin: the Deposit Near Nesve(~ayev. O~
fPL!1stmo__=.ot_itN.ye fce:R)ribwyye rudy na periferii yugovo3tachnogo Donbassa
('119 five tnyev&,oye mostoromhdonlye) - Russian)
PERIODICAL 10gkiady hKademij Nauk 55571t, 1957, Vol 114, Nr 1, Pp 176 -179 (U.S.S.R.)
,kBSTRACT During the course of recent geological invest.igations in the above area,the
monolithicly plastical type of the phosphoritt ore was found.Examination
of the ore led to the important conclusion thaL this kind of ore is of rela-
tively high quality.Further explorations of the area have already been de-
cided, It is assumed that there exist in the southeastern Donets Bassin
many inore such deposits - not only in areq of Nesvetayev.
(I Drawlng, 1 chart, references' G.I.Bushinski,Izv.An.SSR,ser.geol.Nr 1,1954
D.T.Afasiliev) Izv. Donsk.Politekhn1nst. 4k 11, 1915, S.Y.Orekhov,DAN lo6,
'Ir 3s 1956)~
ASSOCIATION No',; Givtgn.
PRESENTED 5Z
SU8MITTLD
AVAILA3LE Librawy of Congrtace
Card 1/1

XTHTYR- ,;h V. It f-MVj/-,o-12v-4-5? 1'67

TITLW-: Th- Minez- loan-:.-, i~r, Con et 3. t iom-- o' Form a E i on o~ ~hn D a rk-

orchl iner-ij.opii- unloviya f ormiro-
Tron Cres of"
14 -nskil,-h rud)
1 boklady AVCicmii ri-mk 1`5~i, Vol Nr 4, pp-9711--S78

A 3'-1 TR 4 C- T Ariong Oie or-f-, of the Kerch'(Kerchenskiy)p the
oxide-ox~dc- lariet.- io Ti-ont advanced in

i;F-ve:--lopinc~nt. The two other type-j: the, brown one aind th
U
Ore occur frequ(-.,ntly, znd, exactly i~- p-1a.4 in-,
j- k, - - us oxide-
are :i h~-rogenic Trodification of the firct. The ferro
oxide ores have h-.aen little investigated, as usually they
i-,re cover-ed b1, a con5:idvruI-I.- layer of sedi-ents. Only re-
ci?ntly n(-.w ore of this -,ort was extracted in the Kanysh-Burullskaya
depression. in it~- fresh state th- -re is d~-rk
nlmoot black.
,
It ra,~Idly oxi.di-es -:;hen exposed to air, turiinE green, then
.Kreenish-brown, and finally brown. These ores contafn t-i-,o
br,slc 8trurtural and mineralogical components: iron oxilde.
toolite, pea ore end lumps of anIcnomrn com-
Card 1`4 i-n-t a 7rf--n f-,=oic oxide cement mass. The s+rudure

;)G-V/2o- 120-4-52/67

Th,i
-.tinn -
to' ~Or:,,at c- Park.-'
-4: 0 OIL' Green Iron Ores
of Kerch,
c;,' thx- s;: orz~t- is o-f a t-f-pical coli tic nature. The qubstance
nf' formati,)ns con2ist2 primarily of ircn hydroxide
ner*, 1-1~1ogo~.-.t l- i i. C, r,;oethite, more rarely lepidocroti te.
--t the run-oxi-de ag;-aomerationo contain
of' 1--am- ~a'erial and frc~cuent,r 14ne terri-

a fti%-. 1[i:rcrE~ the coliteil are replaced by
1: 1 t 'fie E7 ,irfacv, for-ilng a nar.-,---.- ceam. C~n firct
tKh- c",Q :i4cal oomoos-it.-on of mineral dops
ngr~%e z-th Thai
.L oi the cementin,- rriass "Table 1~. The ee-
l, I -
ment e..-::,entially i:3 L- solid voll,~-)idal pseudosolution of cha-
moetly _F f, zebille-like colloid mass. riNic, probleui
of - coi-,unon gerierat io
n of the oxide- and the L'PrrOLIS OYide
n i'~r r: J, n orcs represents considerairls -diffi.-
OZ., t i The amrjun', of or.-anic sub~-tanc-_-- nre~Fent _r: the ore

..eis not ~e T-F F I
tc transform the -ntir huize i,,~~se- of
i-rar! o,.-IdIR raate~rial -into a felrrous o::i-de st~-,te. -it onl:.- sul'-
fie;~ld to --n~-Lve th~? redu2t'on of easily reducilill 4 0,,. 0. i e
und.- -,'j,& forniat -ion of oh-amoisite, that -!~: to say cf
10'st's of tron
M c
.xide
vrhich
enetrnted t-
e fine
. .
,
. p
,
quprtz-Jirk;_- ore sub strate, As r-,~!gards the st-~po of f c:,:-ma t i on
"ard 2 i
'he ore deposits
it c-an be maintained, that in -o-r'icuiar

~OV/1'1`0-1 _90-14 -52/67
,1111f-- 3-irlert-, .1 Ogy lmd Olp !'o-nl it or,- of i,ormat i u of the "ark-Oreen Iron (ores
of ~irrch t
their hip" concentration is due to the ictivity of tile ~Iurf.
There sire 2 figurea, I table, and 12 refereaces, it of
-e!uch are lioviet.
A,3,z "ClAUTION: Lift' v0rcit,~t
N~ kh vi e c de y of
..;Ciaencez-:-) USA
S, TUB .11 1 ri"T"K Z" January
1. Tran ores-Geo'Iogy 2. Iron ores--Properties 3. Iron ores
S t, -L
uottura" analysis, 4, Ir~on ores-44aterials
;,.rd 3/3

4 SOV,1;:2-59_2-~~/32
1
5
AUTITO~~; Shamray, I. A.
TITLE: Petro--rachical Peculiarities and Conditions of the Formation
U- -
of Deposits of the Northern Part of the Maykop Basin (Petro-
graficheskiyeosobennosti i usloviya formirovaniya osadkov
ze,u'ernoy chasti AaykQpskog.o basseyna)
PEFLICDICAL; lzvestlya vyaghik-h tichebiiykh zivedeiiiy. lieftl i
1959, ':r ?, ,)P 3 - 8 (M3P)
A B S-.1 C 11 1r. the South of the European par%' of the USLSE Iaar.e areas
are made up of mighty deposits of the Maykop series. In
the South at!d Southeast they border on the northern foot-
hills of the Caucasus ran.-e. In the Southv-reot they comprise
a considerable part of Transcaucasia. In the North the
masses, more closely studied in the present article, reach
up to the !,,-wer part of the Don and Vo~_-tochny,r DonbLsa.In
the Northeast typical Maykcp sediments com..rise Yuzhnyye
Yer-eiii and Nizhnelye Pova1zhiye. Further to the East and
arc to bo 'Lou,,,.d ai.alogous formations to the
Card 1/4 Maykop series of siimilar a0a, are in the main represented

Pe"ro-re.T~,hical Peculiarities and Conditions of the Sc~111,')~~2-5,-i-2-3/32
Formation of Dezosil's; of tha Northern Part of t',re "Taykan Basin
b,,.r ;continental facies. They extend to Priarallye. The ab-
.-enc,e of some horizons of the lower ffeoseL,c points to a
considerable interruption of the post Maykop period. it
seema thaAw for a lorq~er period of the upper Maykop continen-
.,a! conditions prevailed, Possibly, the same conditions
also nrevailed all- th~~, be~~ niiin- of the ',aykop a- . This is
i
to be seen clearly from the fact that the masses in t-'-,e
northern part, of the basin are relatively depressed (Table 1),
- (, Ii -s due to -the abseace of lo,.~.rer and upper horizons.
L
h
A very typica.1 characteristic of tile ITayltzop mass of the
wrth-ern part of the basin, as well as of t-he southern reGions,
i it 1:."s h'iSh percenta,-_,e of or~,,-nic materials and iron
oul-fid-a_~ (rnelnicoiritej marcasite, and pyrites) to be found
4
, th--2 rocks. In son-a layers of the northern section of "-e
~.a4ykop series these materials are often to be found in
wrnour,4- otlletween 10-30 percent. As to their oroanic material
cont-ents 111,aykop deposits a-re quite distinct from r,~cent
iea and IaEor,-~i muds -which rarely contain more than 1.5-2
of these Sthidies of tfie orGanic material containeCL
Card 21/4

Petrographical Peculiarities and Conditions of the SOV/152-55-2-3/32
Pori:,Oation of Der;os':_ts of t~-.e Northern Fart of the "aykop Basin
In Yiaykop rocks have sho-jr. that it is mainly of thle type
o:r bz7orn coal humua and is represented either by finely
-d-ispe.-se material penet-atin-r- the clay mass, or by brown
coal mud. The brow-n-Ish black, chocolate brown coloring of
tb~e ijtaykop rocks is. due tQ brown coal naterial and finely
di:~peroed -m-asses of iron sul.-L'ide minerals. In some places
~~maller cuantities of biturninous material can be found. The
.ncrease in organic and iron sul'ide materials to be noted
n the nor'hern sections of the mass su--ests that it comes
froim the exte-,ided peat - moor area of the humus region
north a.-,.d northeast of the 'Jaykop sediments of more recent
times. It can be assumed rather safely that the ';.aykop
socliments of the northern part of the :;'aykop basin are of
t.he same au:~ as the coal-bearin--~- scdiments of a .-iide strip
ol' t-ho wastern and sout1lorn Priur-111ye. reGard to
-,revalen-4- f-',,urin- t-.,- of t1le I.:ayhop
`-tributJ n of coal
be c--id t*at `i-:~
ass can - f. Lk
na r i a Ii the iaycr~-~ of --orilcF ~--nd its percentages
in aom;-, .;-a-yer2 point to thw-i fact the ~:ay.--c-. Oasln 7'as
Card 01'ten 41"'1 co'urse ol' its u-,~ ---nd its

Petrr,.-raThical Peculiarities and Canditionz r,'L the SO-1.1/152-c9-2-7/32
Formation of Dapu.-its of the Northern Pa-rt. of thf~ :.'ay,~op Bassin
si,.:o varied. D11rirv, 130MC pcriodo thic Maykop banin rece(led
fa-r to the South and was in the North replaced by a semi-
contine:.tal sea- moor area. Thus the sediments carried down
from, the North could during -come periods penetrat(-. rather
far into the South; the th'Lcl-noss of the sediment in tl~e
South thus areatly increased, but the sediments retained their
mineralogical oh~aracter, Tllhe-rn are 2 tables -and 11 Soviet
-e-
-'el,eLOCS.
.
AS30CIA`OTC~! I jj03tCVS-,-4
State Univer-
S UP M 1112. -a' D 3. i(958
C a -T- d 4 /4

SfWMAY, I.A.,
Textural and oine.-alogical types of Tertiary quartz sands in the
eastern DDnpts Basin and thei.~.-5tratigraphic position. Uch. &ap.
2 (MIRA 14: 1)
.RGU 440~46 159t
(Donets Zasin~-Sand)
(M-natu Bgsinm--Gmloa, Stratigraphic)

SIIAMRAY* ll,,A~sb ORIEMV,
I
Uaw pVloojp-hgt"3 C-colurrmic~e, im the i,'rcjtAcoo;R, and lower-Paleogene
~a-dimm"s in Thai" -%laJA &%sin, (.;.f tho Nol-thern Caucasus. Uch. zap.
9
2GU 44;1-6-5-1-10 95CII. (MIRA 14: 1)
Cllcla~m ihilay VINDrt'hovr.

50) Radu szhe-vr, V_ SOV/20-124-4-49167
'UT~IORSI- L+
T
-ITLE. CIauconite FrDm the Cratacp.=; Sediments of the Belaya -River in
the Northeni Caucaalis (Glaukonit iz melovykh otlozheniy r, Beloy
na Severnom lkavkaze)
PERIODICAL: Doklady A',kademii nauk SSSR, 1959, Vol 124, Nr 4, pp 900-902 (USSR)
ABSTRACT; Ln the region mentioned -above a =istan-t aorizon of glauconitic,
aands and sandstones in the Lower Cretaceous (Aptian) can be ob-
served in many places~ On the Belaya river it attains a thickness
of 15 m and is charaQterized by a high glauconitic concentration
which often attains a percentage of 050-75 %~, The respective strata
are described herq, They contain also fine intermediate strata and
-Dizarre dendroid sider-ite concretions which are probably pseudo-
Morphs of wood reamants. -;7;hich- also contain glauconitic inclusions,
The glauconite grains are green,, ball-shaped. or elliptical, slightly
transparen-t; only a" the edges and their size varies between extreme-
ly small dimensions and 0.6-0.7 mm, In polarized light there appears
a typical aggregate extiaction with double light refraction. '1)_mblz?
shows the chemical composition of glauconite and the crystallo-
chemical foxmula is very approximate to that mentioned in
Card 1/3 zeference 2. The numnerical (ch_is'_1-?v-DY koeffitsient) Of

SOV/20-124-4-49/67
clauconite Frov. t-he CretaceQus R4vo:,- in the Northern
Caucasuu
011-it.1-onn a:n the torahedrQL gizi.-,unta that of aluminum in the
oi~i,ahedra 0-~t, Pzrt of the s-i-I-Jocz. ia replaced in the tetrahedra
by alumi-num, Gslauconite 4&,~ 5imilar tv the oeladoniteu (Ref 2) due to
a rathe- high of -i-Iran i-n the u-1-tahedra.1 layqrs. Table 2-
presents the rad'!.ometfis measure-m-ents and the compari-oon between tirm
and- tha D-ebye electronograms -of eaftiez dPs-.x,-'Lhe,! (Refs 1,2,3.5) -glauco-
nite5. Tf...-,, thermal cur-ve of heating (Fig I. ,) ~--tdicated two marked
eadothermic intermiesion2 (ostanovka)*as bel'n,- characteristic of
sta-nda--d glaucon-ites. ice. at 190 bly '-Qs--t of the hygroscopir- water
and at ~75`3 by separation of the --~onstitlation watex., Up t::~ m0,3
:!. water are separated (Fig 2), up t-~ 400' the water loss is
about 4 P
insigni-f-4cant., The largest amount of wati-r is seDarated between 400
and 6000, At 7000 debYdration has 1r,airtually been completed. The
lots-,- loss of viater to 0, % appToxamakely, The glauconit-e
eeposits within the cat-,hmen--- area of the Belaya river may have been
built up in the area of an extremely ahallow body of water near the
ohore, which is.confirmed by a h.-Igh conten'- of organic substances
~as Weil as tree-like 5iderit-ic paeudo-morphs, A high content of oxide
iron ia eviderv7e of the smal"I dept.h in which the delDc-,sits were
Card are regarded, as uc.,-~,.zulstions in the upper shelf

SO'll/20-124-4-49/67
t~~ Yror. tho C-re ta ceous aed i iners ts of th-e Be' aya- Z-U ver in 'the Northern
area (Ref 1). Glaucouite waa formed b- hydrochemical synthesis
during the earliest stage of diagenesis when the reductive reactions
had not yet attained the climax. Subsequently, siderite was produced
s~hen the decomposition of organic substances increased-and the re-
ductive processes nad attained the climax. Thus, siderite was formed
in a later adage of diageneeia (Ref3 7,S). Aa the glauconitic
mterial in weakly 3orted, it is syngerietiQ-autochthonous. A certain
displacement -and sorting within the intermediate s,trata most abun-
dant in Slauconite seems to be possible (Ref Q), Ihere is no doubt
about the great practical importance of the above -mentioned deposits,
There are 2 figures, 2 tablea, and 18Q reierences, 9 of which are
Sovio t -
ASSOCIAT1011,1z Rostovskiy-na-Donu gosudarstvennyj univeraitet
I
kRostov-zria-Donu State University)
PRESENTED. October 11, 1958, by 13, M., Stra-khov,
SUMUTTED& October 9, 11956
Card 31',~

SHAMRAY, I:A., KUBETSKIY, N.L,
7 -
Organogenic phosphate oreq in the northern part of the Maikop
Basin arid the conclitions of their follmlation. Dokl, AN SSSR 135
no.5:IM9-,1222 D 160.* (ML9A 13:12)
1. Rostovsklj~~na-Donu gosudaretvennyy universitet. Predstavleno
-'k M.Strakhovym.
,widemtkom So, -
(Maikop-Phosphates)

BLINOV,p Yl.!.X,c QIEEFOV~. S.Yo,.- Sfw.TIY, !,A.
~ I
Gjazzot pla-;ceT in-Tmp-se. Priroda cO no.8-.109-IG9 Ag 161. (MIRA 14:7)
1, aggtovakU7~!=~cinu goaudarstvenn~q v-mlvvrait~t.
. Miapso rogion-Gar-not)

Some foms of Upper Glre,~aceous- and Pal.oogene coccoliths and
Discoasteridae in the southern- part of the Russian Platfom.
Tz-v. 1"-9. ucheb. %,Av.; geol. i rqzv, 6 no.4.27-40 Ap 163.
2 (miRA -L6- 6)
L Rosta7skdy, osudarstvemVy universitet.
. ~ I
Ftwaian Platf OM-COCCO hs
(Illuo.gian Platform-Discomn aridam-)

5111C18OUS rOZkj f7CM the scutheastem,
and ttie oordttiona Rz;ve-rning the----'r fol-m5t.-Ifm.
-pol. -I-k=~ no~2;19-11 !,'Jz.-.Ap 16c (M::,l 8
c

3HAN~U!Yt P.P~, KOIPTET-OVA, S,N.
0
Wn ere -
Xi .1ogical and stmetural-petrogranhic Lypes and areas of
J10esa-type roAs in the Io-ger Don Valley, southern Yergeni Hills,
0
Lmd morth-arn C7.1,5caucasia, Kom- chetv. per. no.30:10C-110 165.
(MIRI 19:2)

L 36942-66
ACC NR: AP6020966 SOURCE i: UR/0226/66/000/006/0088/009
AUT11OR; Dokukina, N. V.; Shamray, F. I.'
ORG. Institute of ~~-_tallurgy im A. A. Baykov (Lnst-itut metal-lurgii)
TITLE: Oxidation resistance of tungsten silicide.-niobium silicide alloys
SOURCE: ~roshkovaya metallurgiya, no. 6, 1966, 88-91
TOPIC TAGS: tungsten silicide, niobium silicide, tungsten silicide allov. niobium
silicide containing alloy, alloy oxidation, oxidation
,-USTRACT: A series of tungsten-silicen-niobium alloys with compositions rres-
ponding to WS12-NbSi2 and W Si -Nb Si sections were tested for oxidation6ehavior
jr 3,t 5 3
at 1000, 1100 and 1200C in a w h an eXPOSLre time of 5 hr. It was found that the
knallz~~ed conpcnenLz (silicides) in both'tle 1Zi?-NtSi2 and W5S13-NbSSi3 systems are not oxida-
tion resistant even at 1000C. The addition of a second component improves oxidation
resistance in both systems. In the WSi2-NbSi. system, the lowest weight gain
(10 mg/cm) in 5 hr at 1000C was shown by alloy containing 19.9% niobium. Under the
same conditions, unalloyed NbSi2 had a weight gain of 20 mg/cm2, and unalloyed WSi2
gained 160 mg/cm2 in 3.5 hr. In the WbS13-Nb5si, system, z!lloy containing 32.5%
niobium had the highest oxidation resistance. its weight gain in 5 hr tests at 1000C
was 10 mg/cm~ compared to 110 mg/cm2 for Nb5si, and 140 mg/cm~ for W5si3,, the latter
in 1.6 hr. Orig. art. has: 6 figures. (DVI
SUB .('ODE:.,3.-1/ SUBM DATE: 161-far66/ ORIG REF: 003/ OTH REF: 002/ ATD PRESS:543,

Y-ARVITSKIY., M.P.) inzh.; SHANdUY, L.N., inzh.
Use of bentonite clays in the constraction of seepage preventing facings
in irrigation canals. Gidr.i mel. 13 no.7:29-34 Jl '61.
(NBA 14:7)
1. Sredazgiprovodkhlopok.
-(Irrigation canals and flumes) (Bentonite) (Seepage)

ASATURrAN, jk.Sb,,., kand.tekbn.nank; SHMEUZ. N.I.. 'Lnzh.
Forced quasi-harmonic Vibrations of piston pump valves. Izv.
v,7s.ucheb.zav~, energ- 3 no.6:145-153 Je 16o.
(MIRA 13:6)
1. Bashkirskiy, nauchno-isqledovatellskiy institut po pererabotka
nefti. Predstavlena kafedroy transporta i khraneniya nefti i
gazr
, -4 Ufimskogo neftyanogo instituta.
(Pumping machinery--Vibration)

SHAMRAY, N.M,
Determining the speed ot a valve at the time of its seating. Trudy
IIIITransrieft' no.1:315-332 161. (NIRA 16:5)
(Reciprocating pumps) (Valves) -

514AK'~AY3
-3 N.M.
~
Operation of the valven of a platoa p-ower pump. Trudy
Bashfill NIP no,62259-P66 163. (MIPA 17g5)

1, silutwx, P's.
2. USSR (600)
4. Technology
7, Electri"ic tion of collective farm work* Kiev, Gostlekhi dat, USSR 10,52
9. Monthly List of Russian Accessions,Library of Congress,February,1953.Unclassified.

112-3-558i
TranSlation from: Referativnyy Zhurnal, Elektrotekhnika, 19575
N r (USSR)
AUTHOR; Shamray, P. A.
INTLE: Power TransmisBion from High-Power SYstems (Peredache
energii ot moshchnykh energosistem)
PERIODICAL. 14ekhaniz,sil"sk. gospodarstva, 1956, Nr 5, pp. 24-25
Mrainlan SSR)
ABSTRACT, Bibliographic entry.
card 1/1
1~

SHAMAY)I.F.L-assistent
Developnent of connective tissue in a wound. Sbornauoh.trud.
Vin.der.med.inst. 18 no.1%137-155 158. (MIn 16:2)
1. Xafedra gistolo li 1 embriologii (zav. kafedroy doktor med.nauk,
prof. I.V, AlmawovvRnnitskogo, gosudarstvennogo medit4nskogo
Ustituta.
(WOUNDS) (CORNBMIVE TISSUES)

SHAMRAY, F.F., assistent
Pal-ticipation of vjunerary iafiltrate eolls in the development of
collagen T:fbers. Sbor..nauch.-trud.Vin.der.med.Wt. 18 no.18156-
3.64, '58. (MM 16-.2)
1~ Ka:esdra gistuologii i embriologii (zav. kafedroy doktor med.
nauk, prof. 1.V. Almawr) Vinnitgkogo gosudarst7ennogo medi-
tsinakogo instituta.
(WOUNDS) (COLLAON)

IS119MAY, F.F., assistent
Changes in vulnerary infiltrate cells cultivaed in a colloid
bag within the organism,, Sbor.trud.Vin.der.med.inst. 18 no,,2*.
40-45 '58. (MIRA 16.-2)
L Kafedra, gistologii i embriologii (zav. kafedroy doktor med.naukq
prof. I.V. Almaz-ov) Vimitskogo gosiAdarstvennogo meditsinekogo
ustituta.
(WOUNDS) (CONVECTIVE TISSUES) (TISSUE CULTURE)

YUFA, Ye.Ye.; SHA?-!RAY, T.V.
Work of the nurse in the prevention of poliomyelitis. Med.
sestra no.6:52-53 Je 162. 0,1IRA 15:8)
1. Iz detskogo poliklinicheskogo otdeleniya 4-y bollnitsy Llvova.
(POLIOMYELITIS--PREVENTION) (NURSES AND NUKiING)

SHAMR,AY,V., inzhener
The machine-tractor station assists collective farms in con-
struction work. Sell.stroi.10 no.6:4-5 Je'55.
(MLRA 8:10)
1. Nachallnik stroitellno-montazhnogo otryada Kryukovskoy
mashinnotraktornoy stantsii Moskovskoy oblasti
(Machine-tractor stations)

ACC NR% AP7002403
SOURCE CODE: UR/0363/66/002/012/2156/2161
AbTHOR: Alekseyevskiy, N. Ye.; Ageyev, N. V.; Shamray, V. F.
~ORG: Institute of Metallurgy im. A. A. Baykov Academy of Sciences SSSR (Institut
.metallurgii Akademii Nauk SSSR)
:'."ITLE: The critical temperature of the transition to the superconducting state of
i
!the B-Phase in the Nb-Sn-Al-Ge system
~SOURCE: AN SSSR. Izvestiya. Neorganicheskiye materialy, v. 2, no. 12, 1966,
:2156-2161
~TOPIC TAGS; niobium tin allay, aluminum containing alloyo germanium containing
:alloy, superconducti~g alloy arr,~~ion-trans-i-t4on-.temperatureg-&Uoy,-transi-
tA.4m temperature
IAB&TRAcT;
elements were levitation melted from 99.8Z-pure niobium and 99.999Z-pure
aluminumi tin and*germanium, homogenized at 600C for 250 hr and water
quenched. Nb Sn, Nb Al and Nb Ge compounds were found to have a temperature
3 3 3
of transition to the superconducting state (Ted of 18.1, 17.4 and 7.1K,
respectively. With increasing Sn content*in alloys of the pseudobinary
Nb Sn-Nb Al section, T
3 3 cr gradually decreased, reached a mini-t- at the Sn:A1
ratio of 1:1, and gradually increased again with a further increase in the
Sn content. In alloys of the Nb3Su-Nb3Ge section, T dropped sharply with
cr
Card 1/3
Beta-alloy's of the Nb-Sn-Al-re system with various contents of the alloying

ACC NRt AP7002403
an increase of Nb3Ge content to about 70%, and then remained almost constant.
With small increases in the Ge content of alloys along the Nb3Al-Nb3Ge
I section, T slightly increased to a maximum in an alloy with a 4:1 Al:Ge
ratio, andelhen decreased continuously with'increasing Ge content. The

ACC NR: APT002403
composition dependence of T in the Nb3Sn-Nb3Al-Nb3Ge section is shown
cr
in Fig. 1. Ihe critical temperature Tcr was also found to increase with the
increasing degree of ordering of the investigated alloys. In the Nb-Sn-Al-Cie
system, the value of Tcf appears to be determined mainly by the.density of
at the Fermi our ace. Orig. -ait- hiii....7-Tigures.,
;.SUB CODE: 11, 20/ SUBM DAM ogmar66/ ORIG R17: O-OT/ OTH REF: 008/
i ATD PRESS: 5113