The system UO2-Eu2O3 at high temperatures

The system UO2-Eu2O3 at high temperatures

JOURNAL OF NUCLEAR THE SYSTEM L. N. General 21 (1967) 302-309. 0 MATERIALS GROSSMAN, J. E. Nuclear LEWIS Technology Pleasanton, Received ...

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JOURNAL

OF NUCLEAR

THE

SYSTEM

L. N. General

21 (1967) 302-309. 0

MATERIALS

GROSSMAN,

J. E.

Nuclear

LEWIS

Technology

Pleasanton, Received

Phase equilibria determined sphere

in the system

for high

by

thermal

ceramograpby.

analysis,

Extensive

in the fluorite

phase;

fluorite mole

X-ray

solubility Urania

% Eu01.5;

50” C. Lattice

the eutectic

temperature

been

observed

invariant

; a binary

temperature

the

compound

are reported

and phase.

region

are

and

W

has

and

binary

for the Eu303-W

system. Le diagremme

d’bquilibre

des phases a BtB determine

U03-Eu303

et en atmosphitre

neutre

diffraction

des

existe

une

solubiliti!

phase

rayons

fluorine

alors

et

importante qu’il

n’y

Die durch

Eu303 cubique

keit

entre les phases fluorine

pour

80 mole

eutectique

y.

est

de

von

Eu3O3

Uranoxid

sont sign&%

Phase

besteht

UO3 stabilise

Un eutectique

se

et I%303 monoclinique

et

pour

iiber

eine

LB temperature

variante berichtet.

Introduction

Europium oxide is being considered for use in fast reactors to control the increase in reactivity caused by water flooding in a steamcooled reactor that has high neutron leakage Ia). The effectiveness of europium as a thermal or epithermal poison to control routine flooding reactivities in mixed U-Pu oxide fuel has been demonstrated in a subcritical assembly lb). It is anticipated that, for power reactor use, the europium will be in solution in the oxide fuel which will be fabricated by conventional

in

und

Fiir

die

unterhalb

Lijslichkeit der

mit

Solidus-

der

zwischen

Das Soliduslinie postuliert.

Eu303

monoklinen

ca.

80 Mel liegt werden

und

y0 bei die

Liquidus-

Gleichgewichtswird

fiir

Es wurde

die eine

Eu303 und W beobachtet

Verbindung im

im

von UO3

das kubische und

Fluoritphase die

Seite

Temperatur

Grosse L&lich-

Fluoritphase;

Temperatur

angegeben.

binllre

der

keine

Eutektikum

europiumoxydreiche

Les

param&res

ein

Eu203-U02

Riintgenfeinstruktur-

Fluorit

eutektische

Wechselwirkung

System

stabilisiert

1885” C. Zwischen

diagramm

2125 + 50” C.

a 6th

binaire

cornpost

bestimmt.

besteht

featgestellt.

de

ELI 0,5 environ.

la rhgion

und inerte AtmosphLre

Analyse,

Eu3O3 wurde

temperaturen

dans

im

monoklinen

la

& 1885” C environ.

forme

thermische

de Eu303

thermiquo,

solubilit&

un

binaire

analyse und Keramographie

Gitterparameter,

L’oxyde

interaction

Eu303 et W:

Phasengleichgewichte

11

a aucune

Une

wurden fiir hohe Temperaturen

la

la

pour

d’europium. invariante

Des Cquilibres

sugg&&

Eu303-W.

c&amographie.

par l’analyse X

entre

Die EuO1,5. 2125 f 50” C.

aux hautes tempkratures

UO3 dans En303 monoclinique.

1.

observee

bis

pour lo systbme

en oxyde

fluorine.

sont

80

is 2125 &

temperatures

Eu303

riche

du solidus et du liquidus

la phase

du solidus

le systbme

are given for t’ho fluorite between

en dessous

pour

between

for the europia-rich

interaction

les temp&atures

donnkes

une tempkrature

at approximately

solidus

r@ticulaires, sont

Laboratory,

1966

cubic Eu303

Subsolidus postulated.

exists

of UO3 in mono-

liquidus temperatures equilibria

and

of Eu303

is formed

phases

parameters,

have been

Nucleon&s

USA

19 September

diffraction,

stabilizes

1885’ C. An eutectic and monoclinic

CO., AMSTERDAM

and D. M. ROONEY Department,

California,

and neutra,l atmo-

no solubility

clinic Eu303 was found. to about

Eu303-U03

temperature

PUBLISHINQ

UOZ-EuzOs AT HIGH TEMPERATURES

Company,

Electric

NORTH-HOLLAND

und

System

eine

binlire

Eu303-W

; in-

wird

hydrogen sintering. The existence of a large solubility for Euz03 in UOZ and the feasibility of homogenization by hydrogen sintering have been demonstrated 2). The fluorite structure of UOz tolerates large deviations from stoichiometric composition on both the anion- and cation-deficient sides. Hyperstoichiometry is readily produced at temperatures above about 300” C in mildly oxidizing environments. As the temperature is increased, the UOz+, phase boundary broadens by the dissolution of interstitial oxygen ; a 302

THE SYSTEM U02-Euz03 maximum

O-to-U ratio of about 2.26 at about

lo-l.5 atm oxygen and 1450” C has been reported 3). Hypostoichiometry is more difficult it requires temperatures above to produce, about 1600” C and low oxygen pressure. An O-to-U ratio of 1.88 has been reported 4) for Urania equilibrated

at 2400” C in hydrogen

(dew

303

AT HIGH TEMPERATURES after experimentally

establishing

the appropri-

ate calibration curve. It was inferred from weight loss data that no significant compositional changes occurred during sintering. Hot-pressing of blended powders was accomplished Hoyt 8).

in The

apparatus were

described performed

at The

the UOa-s phase reaches a limit of about UO1.65

specimens were held at 5000 psi for lo-20

min

at about 2500” C, ref. 5). Oxides of composition MO2 and of fluorite

at temperature. The hot-pressed pellets were generally crack-free and between 94 and 97 y0

type can dissolve large amounts of sesquioxides when the cations are of similar size. A composition limit of Mol.75 has been observed for these fluorite solutions with anion vacancies 6). At large vacancy concentrations, the vacancies in the fluorite structure can become ordered and form the closely related Type C rare earth (thallium oxide type) structure which is exhibited by most of the rare earth sesquioxides

dense. Previous experience with UOZ pressing has shown that the initially hyperstoichiometric powder is reduced to stoichiometric composition during this procedure. Carbon pickup was confined to the outer pellet surfaces which were cleaned by mild abrasion. The mixed oxide pellets were encapsulated in tungsten by inert arc welding in an argonfilled glove box. Each pellet was cored ultrasonically before welding to accommodate a tungsten tube down the center. A cross section of a specimen capsule after testing is shown in fig. 1.

- 40” C); the phase boundary

for

at low temperatures. Three oxides of europium have been reported 7) : Eu203 (monoclinic and body-centered cubic), EuO (face-centered cubic), and Eu304 (orthorhombic); the sesquioxide is the most stable. A fourth reported oxide, designated “Ortho I” has been identified 7) as the orthosilicate EuzSi04. The sesquioxide crystallizes in the Type C rare earth structure below about 1100” C and in the Type B (monoclinic) structure above 1100” C. The suboxides are difficult to form because of their relative instability and of the high volatility 7) of EuO. No analytically significant deviations in composition from the stoichiometric sesquioxide have been reported for monoclinic Euz03. 2. 2.1.

Experimental

procedure

SPECIMEN PREPARATION

Blended UOZ and Eu203 powders were consolidated by two techniques : hydrogen sintering of specimens containing less than 20 mole percent Eu01.5, and vacuum hot-pressing of the other specimens. Powder analyses and sintering details have been reported 2). The molar ratios were confirmed by X-ray fluorescent analysis

2.2.

1400” C in graphite

by

dies.

point about

1300” C and

the

pressings

THERMAL ANALYSIS

The encapsulated mixed oxide specimens were inductively heated in vacuum to obtain heating and cooling curves. The experimental equipment and procedure for thermal analysis are similar to those reported by Rupert 9). Vacuum is maintained at less than 5 x 10-S Torr during heating. The specimen temperature is measured independently of the temperature recording system by optical pyrometry. A manual brightness pyrometer is sighted on the blackbody hole. The pyrometer is frequently calibrated against an NBS secondary standard bulb between 900 and 2300” C. Temperature measurement above 2300” C is made by extrapolation of the correction curve for the pyrometer. Temperatures below 2300” C are accurate to well within & 1 %; the accuracy of temperatures reported between 2300 and 2600” C is believed to be within f lg y. ; between 2600 and 3000’ C, &- 2 o/o is estimated to be the

304

L. N. GROSSMAN.

J. E. LEWIS AND D. M. ROONEY can readily detect temperature than lo C at all temperatures. of the detector

changes of less The linear range

is shifted by the use of neutral

density filters. The response time of the detector is 0.1 set at the middle of the linear range and less than 0.01 set at the high intensity

end of

the linear range ; thermal analysis data were always taken between these limits. Each specimen was heated to above the liquidus several times. Thermal analysis data were obtained on heating and cooling above approximately 2000’ C ; a few samples were

Fig. 1. Cross so&on of UO&% mole o/0 Eu01.5 in tungsten capsule after thermal analysis.

maximum error. The brightness pyrometer readings are corrected for the fused silica window and prism in the light path. For very high temperatures, tungsten evaporation and deposition on the window can affect temperature measurement accuracy. A magnetically operated shutter minimizes this problem. An image of the blackbody tube is projected by a large objective lens onto a cadmium sulfide photoconductor detector. The blackbody image is enlarged to about 40 x so that it completely covers the 3” dia. detector. The detector resistance is monitored with a shielded drop across the dc circuit. The potential photoconductor is monitored, and its first and second time derivatives may be observed. The potential drop across the detector is approximately linear with temperature over about 400” C. Over the linear range, the sensitivity is about 0.15’ C/mV; thus, a millivolt recorder

examined at lower temperatures. Thermal analysis of the specimens resulted in two general types of observed heat effects: thermal arrests, and abrupt changes in slope of the cooling curve. The first type is observed at temperatures corresponding to invariant points (e.g., melting point and eutectic reaction); the second type is characteristic of simple phase boundaries where no reaction occurs. No special care was taken to equilibrate the thermal analysis specimens at any temperature before cooling ; the final cooling was accomplished by shutting off the induction heater while the specimen was between about 2000 and 2500” C. Two specimens (27.8 and 46.2 mole o/o EuOI.5) were equilibrated at 1600” C after melting in the thermal analysis apparatus; shutting off the power cooled these to less than 900” C in about 1 min.

2.3.

X-RAY ANALYSIS

After thermal analysis, the capsules were sectioned longitudinally as shown in fig. 1. One-half the specimen was removed from the tungsten container and crushed to not less than 200 mesh powders. The powders were analyzed by X-ray diffraction with the Debye-Scherrer and diffractometer techniques, employing the reNelson-Riley and sin20 extrapolations, The wavelengths used were spectively. CuK,, (1.54051 A) and CuK,, (1.54433 A). A weighted average CuK, (1.54178 A) was used for the powder camera method. The accuracy of lattice parameter measurement by the

THE

SYSTEM

UOs-EusOs

AT

method was zt 0.005 A; powder camera diffractometer measurements were accurate in most cases to f was

used

specimens

to

0.0003 A. X-ray confirm

containing

the

fluorescence

compositions

of

up to 66 mole o/o EuOi.5

HIGH

305

TEMPERATURES

one between

2650 and 2695’ C, and another

between 2730 and 2780” C. All specimens showed traces tungsten were

too

in the small

oxide to

phases.

measure

interaction

by the Debye-Scherrer

will be discussed separately.

2.4.

CERAMO~RAPHICANALYSIS

The longitudinally sectioned specimens were prepared for ceramography by grinding through 600 grit silicon carbide grinding paper and rough polishing on nylon polishing cloth charged with 6 and 3 pm diamond paste. Final polishing was accomplished with a thick slurry of Hz02 and Linde “B” (0.05 ,um AlaOs) on Buehler Texmet polishing cloth. Medium pressure was used to avoid excess relief between phases. A 1 to 2 min swab-etch with a 9 : 1 Hz02 :HzSOa solution was sufficient to etch grain boundaries and develop substructure. Dark field illumination was used extensively in determining the pattern and location of metallic tungsten inclusions within the structures of the oxide specimens is). The advantage of dark field over bright field is the ability to see below the polished surface of the oxide matrix and therefore see more clearly the distribution of the metallic inclusions. 3.

Results

A summary of the experimental data obtained by thermal analysis and X-ray diffraction is given in table 1. The two types of thermal effects observed have been abbreviated as follows: A change in slope in the cooling curve is noted by “S”, a thermal arrest is noted by “A”. As a result of gradients in the specimen capsules, a change in slope or an arrest is usually spread over a temperature range of 20 to 50’ C. For example, specimen 10 showed two changes in slope upon heating or cooling,

metallic

The

amounts

accurately

by

ceramographic or X-ray techniques ; X-ray fluorescent analysis of specimens 15 and 17 showed less than 5 o/o total tungsten in the oxide phases. Specimen 18 showed extensive

after thermal analysis. In the pure EuzOs, analysis showed prowhere ceramographic nounced phase segregation (due to reaction with the tungsten capsule), selected areas were scraped with a diamond stylus and analyzed technique.

of

between

pure EusOs and tungsten Ceramography

of

specimens containing up to 57.2 mole y. EuOi.5 showed single phase fluorite which appeared identical to pure UOs. Small metallic tungsten inclusions, similar to those seen lo) in pure UO2, were observed ; a possible trend towards more tungsten with greater EuzOs content was observed. Lattice parameters were obtained from powder films by a Nelson-Riley extrapolation of all diffraction lines with 28 falling above 100” C. For diffractometer scans, a sins0 extrapolation was used. The fluorite lattice parameter data in table 1 and some earlier data 2) are given in fig. 2. Monoclinic europia was observed as a major phase in specimens 15, 17, and 18; line-for-line comparison with the diffraction pattern published by Rau 11) showed near-perfect agreement within the experimental accuracy of the two studies. Body-centered cubic EuzOs was observed in specimens 15 and 17. Identification of the body-centered cubic phase required careful examination to confirm that it was not a second face-centered cubic phase; diffraction lines forbidden in face-centered cubic materials were present. The lattice parameters of the body-centered cubic phases were computed and found to differ significantly from those of pure EuzOs for which ii) ao= 10.869 + 0.003 A. Specimen 15 contained more of the bodycentered cubic phase than specimen 17. Specimen 18, pure Eu203 in tungsten, showed a very nonuniform phase distribution. Obvious reaction had occurred between the tungsten capsule and the oxide, and the reaction had not gone to completion. A mixed oxide structure

306

L.

N.

GROSSMAN,

5.4800

J.

E.

LEWIS

I

I

AND

D.

M.

I

I

ROONEY

I

I .~.

5.4700 !

5.46po

\ ~-

5.4500

-

5.4400

--

"'\,

L

\

;

I

F 2 5.4300 : 'Z -. 5.4200 --

\ 5.4100 -~

I

.... X. x. I... k.

5.4000

~~~

53900 0

I IO

I 20

I 30

I 40

E"O1.5 (Mob

Fig.

2.

Lattice

parameter

versus

composition

Specimen

wt% EuzO3

mole o/0

1

0

0

Not, analyzed

0

0

S, 2755-2787”

ao=5.4707

i

ao =5.4708

& 0.0002

5

7.4

S, about

Not

analyzed

7.4

S, 2760-2850”

C

Not

analyzed

5

15

21.2

S, 2720-2760”

C

Not

analyzed

s,

c

Not

analyzed

equilibrated 10 11

20 35.8

27.8 46.2

S, 2650-2695”

C C

Not

analyzed

46.5

57.2

13

56.6

66.7

15

70

78.2

80

18

100

86.0 100

Not

; at

Fluorite,

ao=5.4100 ao=5.403

S, 2460-2515”

C

Fluorite,

C

Weak

S, 2230-2270”

C

Fluorite,

s,

2350-2390”

C

Weak

trace

S, 2150-2200”

C

Major

monoclinic

2120-2135”

C

A 1870-1895” S,’ 2176-2225” A, 2104-2135” A, 2060-2092”

c C C C

24 S=change

trace

Strong

4

S, 2760-2810’

C

Not

6

8.8

S, 2741-2818”

C

Fluorite,

*

A trace

monoclinic

Euz03

Eu203

bee, ao=10.907

unidentified

Fluorite,

arrest.

EuzO3

5 0.001

Monoclinic Eu203 New fee phase ao=5.395

C

; A =thermel

k 0.001

f

Major monoclinic Euz03 Strong minor bee, ao=10.900

S, 2812-2884”

in slope

& 0.0009

monoclinic

ao=5.400

minor

3.0 6.0

2

0.0009

1600” C

Trace 19 22

f

analyzed

S, 2400-2430”

A, 17

ao=5.4363

0.0002

1600” C

S, 2730-2780” equilibrated 12

Fluorite,

; at

(A)

Fluorit,e,

5

27.8

2800” C

;

present*

Fluorite,

3

20

solutions.

X-ray Phases

C

2770-2795”

solid

da.ta

4

9

j-

fluorite

analysis?

2

1 70

1

of experimental

Thermal

EuO~.~

I 60

50

'I.1

for UOs-Eu01.5

TABLE Summary

I ...... x...................... r-

of W

phase.

ao=5.4660

f

0.005

+ 0.005

& 0.005 See text.

0.0003

analyzed

was found

ao=5.4599 in every

& 0.0003

specimen

examined.

THE

of

apparent

peritectic

UOs-EusOa

SYSTEM

origin

could

be

seen

AT

HIGH

307

TEMPERATURES

respectively.

Solidus and liquidus temperatures

along the tungsten capsule walls and in contact with the tungsten capillary; X-ray diffraction identified the two phases as monoclinic EuaOs

could not be resolved by thermal analysis for compositions rich in UOa. The position of the eutectic is not exactly known, but it must lie

and a new face-centered cubic phase which could not be identified. The new phase has a

between

lattice constant as = 5.395 f similar in structure

0.005 A and is very

of fig. 3 have been inferred

Away from the tungsten in specimen 18 had not

walls, the europia reacted with the

tungsten. A major phase of monoclinic EuzOs and a trace of an unidentified compound were the only phases detected. The diffraction pattern of the unidentified phase is shown in table 2. Ceramography showed this unidentified phase as small nonmetallic islands within the monoclinic EuaOs grains. This phase is dissolved by the HzOa-HaSO4 etchant. TABLE Diffraction

The

specimens

from

side

analysis

of

15 and 17, and from the known 14)

polymorphism

in EuzOs. The invariant temper-

ature observed at about 1885” C in specimen 15 has been interpreted as a peritectoid. (No thermal analysis of specimen 17 was performed below 2000” C.) The peritectoid composition has been estimated from ceramography as has the subsolidus fluorite phase boundary shown in fig. 3. The oxygen pressure dependence of the fluorite phase composition is indicated by

2

pattern of unindentified europium detected in specimen 18

d (8)

y0 Eu01.5.

Subsolidus equilibria on the europia-rich

and size to the compound

2CeO.2..YaOs.

readily

78.2 and 86.0 mole

equilibrated specimens 9 and 11 are represented by two crosses in the fluorite field of fig. 3.

Rel.

oxide

II

intensity

oI

2800

4.225

ww

3.319

MS

2.929

vvw-

2.545

VW

2.373

VW

2.075

M

2600

2400

1.724 Y

Thermal analysis of specimen 18 showed an arrest on heating through the range 2060 to 2090” C which lengthened on each subsequent heating or cooling. Heating above the arrest showed a wide melting region, but no value of the liquidus temperature was obtained. The capsule ruptured after about 15 min above 1800’ C and signs of liquid formation at 2090” C were observed.

r f ;

2200

E 2 2000

1800

1600

4.

Discussion

The data of table 1 have been used to construct the phase diagram shown in fig. 3. The melting points for UOZ and EusOa are those reported by Hausner 12) and Schneider Is),

0

uo2

Fig.

3.

Mol.

r.

UOz-EuOl.5 equilibrium phase high temperatures.

diagram

et

L.

308

oomparison

N.

GROSSMAN,

of this study

with

J.

the work

E.

LEWIS

of

Haug and Weigelis). They studied the UOs.sEusOs system under oxidizing conditions (air

AND

evidence

D.

31.

ROONEY

for only two cation species (Eufs and

sintering at 1100” C followed by an air quench) ;

Uf4) in the fluorite phase. The interaction observed between EusOs and tungsten in specimen 18 bears on the dis-

single

crepancies in reported melting points for EusO3.

phase

fluorite

was

observed

between

about 28 and 64 mole o/o EuOi.5. The fluorite

Wisnyi

phase lattice parameter varied linearly between 5.406 and 5.392 between 38 and 64 mole o/o

for the melting point as measured on a tungsten

EuOi.5 under their oxidizing conditions. The lower lattice parameter observed with increased oxygen content in the fluorite phase is consistent with similar observations on the UOs-UOs system 16) and the UOz-YsOa-UOs system 17). The fluorite phase in the UOs-UaOs-EuzOs system at high temperatures resembles the fluorite phase in the UO2-UsOs-YsOs system 17) in several respects. In both, the fluorite lattice parameter decreases with increasing oxygen content and with increasing lanthanide content. As the oxygen pressure is raised, the region of fluorite phase decreases in both ternaries and gives way to UOs.6 on the Urania-rich side. The linear dependence of lattice parameter with composition shown in fig. 2 is in accord with Vegard’s law as might be expected for random substitution of Eu+s for U+4, and for random anion vacancies. Similar linear behavior 18919) has been observed in the system YsOa-ThOs and LasOs-ThOs where the cations have only one valence and where anion vacancies account for charge neutrality 6). The nonlinear variation of lattice parameter with composition in the UOz-YsOs fluorite solutions has been interpreted by Roberts 6) as evidence of vacancy interaction. Roberts’ conclusion was based on the data of Ferguson and Fogg 20) who equilibrated their specimens with uranium metal at 950 to 1050” C for 2 to 3 days in evacuated vycor tubes. Similar attempts by Aitken 21) to equilibrate high yttria content Urania-yttria fluorite phase with uranium metal did not reach equilibrium after several weeks. Thus it is not clear whether the ordering of vacancies at low temperatures or the excess oxygen caused the nonlinear behavior observed in the YsOs-UOs system. The linear behavior shown in fig. 2 is interpreted as corroborative

and Pijanowski

reported

2050 f

30” C

strip heater 13). Their value is apparently a measure of the invariant temperature observed in specimen 18 for the W-Eu2O3 binary. The value of 2240 f 10” C reported by Schneider is) was obtained using an iridium crucible ; X-ray examination of the residue after melting revealed no new phases. Schneider’s value has been used in the construction of fig. 3, although it may represent an invariant (e.g., monotectic) in the EusOs-Ir system. Foex 22) has reported about 2330” C for the melting point of EusO3 ; his technique involved solar heating of the oxide in air in a crucible of nonmelted EusO3.

5.

Acknowledgments

Grateful acknowledgment is extended to R. M. Harrington, N. R. Mullison, and J. G. Wilson who aided in the fabrication of specimens and in thermal analysis. E. A. Aitken, D. L. Douglass and U. E. Wolff provided stimulating review and discussions. The U.S. Atomic Energy Commission graciously supplied the material from which specimens were fabricated.

References J. W. Hallam, R. K. Haling, P. Killian and G. T. Peterson,

Proc.

Conf.

Safety,

Fuels

Design in Large Fast Power Reactors, Ill.,

1965, Argonne

Report

ANL-‘7120

National

end

Core

Argonne,

Laboratory

(USA)

(1965)

E. Kiefhaber and K. Ott, ibid. H. W. Hill, J. E. Lewis and L. N. Grossman. General Electric Company (USA) Report GEAP5008 (Jan. 1966) T. L. Markin, L. E. J. Roberts

and A. Walter,

in Thermodynamics of Nuclear Materials (IAEA, Vienna, 1962) E. Aukrust, 1’. Forland and K. Hagemrtrk, ibid. E. A. Aitken, H. C. Brassfield and J. A. McGurty, ANS

Trans.

6, no. 1 (1963)

150

THE

5)

6)

UOs-EuzOs

SYSTEM

AT

HIGH

of the metal oxides, National Bureau of Standards

A. E. Martin and R. K. Edwards, J. Phys. Chem.

(USA)

69 (1965)

1788

L.

Robe&,

E.

J.

pounds,

in Nonstoichiometric

Advances

in Chemistry

Com-

14)

D.C.,

8)

Roy,

9

ref. no. AED-CONF-63-040-18

Press, New York,

W.

A.

(USA)

65

Rev.

Sci. Instr.

36 (1965)

1629

(1966),

Young

et al., North American Aviation NAA-SR-6765

17) S. Bartram, General

C. Rau,

General

DC 59-9-122

‘9

(1959).

Company

Also in ASTM

file of X-ray

diffraction

12)

H. Hausner,

J. Nucl.

13)

S. J. Schneider, Compilation of the melting points

15 (1965)

Juenke

Company

(1962) and E. (USA)

A.

Aitken,

Report

TM-

1964)

and R.

Mezger,

Z. Phys.

Chem.

201

268 Z. Anorg. Chem.

5

)

I. F. Ferguson and P. G. T. Fogg, J. Chem. Sot.

21)

E. A. Aitken, General Electric Company, Nuclear

(1957)

data.

Mat.

(rev.

265 (1951)

(USA) Card

F.

F. Hund and W. Diirrwachter,

9 20

Electric

E.

Electric

E. Hund (1952)

(USA) Report ORNL-

p. 249

J. Nucl. Mat. 9 (1963)

Report

63-7-14

G. 11’. Rupert,

Report

Chem.

355

1962)

U. E. Wolff and D. RI. Rooney, 19”’ Met,allographic Group Meeting (April 20-22, 1965) Oak

R.

10, 1963) p. 12 Phys.

204s

(Germany)

E. W. Hoyt, in Proc. Sec. Intern. Vacuum Congress, Washington, D.C., Oct. 1961, 2 (ed.

TM-1161

J.

1963)

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