ORNL-1816 - the Molten Salt Energy Technologies Web Site
ORNL-1816 - the Molten Salt Energy Technologies Web Site
ORNL-1816 - the Molten Salt Energy Technologies Web Site
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ANP QUARTERLY PROGRESS REPORT<br />
whe<strong>the</strong>r a greater percentage of UF, could be<br />
reduced to UF, in NaF-LiF-KF (1 1.5-46.5-42.0<br />
mole %) at a lower temperature than previously<br />
used, a trial was made in nickel at 5OOOC. After<br />
2 hr of equilibration of <strong>the</strong> alkali fluoride with<br />
sufficient UF, to equal 25 wt % uranium as UF,<br />
and 100% excess uranium metal, <strong>the</strong> mixture could<br />
not be filtered, and no quadrivalent uranium was<br />
detectable by petrographic or x-ray analyses, Thus<br />
complete reduction of UF, to UF, was indicated.<br />
A similar experiment involved equilibrating <strong>the</strong><br />
NaF-LiF eutectic (40-60 mole %) in nickel for 2 hr<br />
5OC with added UF, and an excess of ura-<br />
nium metal. Chemical analysis revealed that<br />
all <strong>the</strong> uranium present after <strong>the</strong> test (25 wt %)<br />
was in <strong>the</strong> trivalent form. When <strong>the</strong> same type of<br />
experiment was carried out with <strong>the</strong> LiF-KF<br />
eutectic (50-50 mole %) at 6OO0C, only 60% of<br />
uranium was found to have been reduced. Thus<br />
KF appears to differ from NaF and LiF as a<br />
solvent for UF, and UF,.<br />
A trace of volatilized alkali metal was <strong>the</strong> only<br />
evidence of reduction when purified KF was heated<br />
at 9OOOC for 2 hr with finely divided uranium metal.<br />
A similar result was noted when NaF-KF-LiF<br />
(1 1.5-42.0-46.5 mole %) was heated to 7OOOC with<br />
uranium metal for 4 hr with gas stirring. Dispro-<br />
portionation of UF, is <strong>the</strong>refore seen as a reason-<br />
able explanation for <strong>the</strong> quadrivalent uranium found<br />
in UF,-KF mixtures. P<br />
Heating of high-purity UF, with <strong>the</strong> NaF-KF-LiF<br />
mixture at 8OOOC yielded material which, when<br />
filtered, was found to have 73% of <strong>the</strong> uranium in<br />
<strong>the</strong> filtrate, as well as all <strong>the</strong> uranium in <strong>the</strong><br />
residue, present as U3+. Evidence of slight vola-<br />
tilization of <strong>the</strong> alkali metal precludes a definite<br />
conclusion as to whe<strong>the</strong>r reduction of KF or dispro-<br />
portionation of UF, was responsible for <strong>the</strong> de-<br />
tected UF,; however, <strong>the</strong> presence of uranium<br />
metal also in <strong>the</strong> residue indicates strongly that<br />
some disproportionation took place.<br />
Electrochemistry of Fused <strong>Salt</strong>s<br />
L. E. Topol<br />
Materia Is Chemistry D ivi sion<br />
Decomposition potential measurements of molten<br />
KCI and of chromous and chromic chlorides dis-<br />
solved in KCI have been continued. These elec-<br />
trolyses, reported in Table 5.1, conclude, for <strong>the</strong><br />
present, <strong>the</strong> decomposition study in fused KCI.<br />
TABLE 5.1. DECOMPOSITION POTENTIALS OF VARIOUS CHLORIDES IN KCI AT'85O0C<br />
Anode: Carbon<br />
<strong>Salt</strong> in KCI*<br />
<strong>Salt</strong> Container Cathode Atmosphere E (observed) (v)<br />
(mole %)<br />
KCI** 100 Platinum Crucible He 3.25 to 3.30<br />
100 Platinum Crucible He 2.90 to 2.75<br />
CrCI, 3.0 Morganite A1203 Platinum He<br />
33.3 Morganite A1203 Nickel He<br />
0.55 to 0.65, 0.30 to 0.36, 0.90 to<br />
1-05, 1.65 to 1.80, 0<br />
1.60, 0.70 to 0.80, 1.25 to 1.35<br />
33.3 Morganite A1203 Platinum He 0.45 to 0.50, 1.04 to 1.15, 1.25,<br />
1.45, 1.57, 0<br />
33.3 Morganite Al2O3 Platinum<br />
H2<br />
0.98 to 1.03, 1.22<br />
3.0 Morganite A1203 Nickel<br />
H2<br />
1.06, 1.45 to 1.50, 1.75<br />
Morganite A1203 Nickel<br />
H2<br />
1.70 to 1.80, 1.15 to 1.25<br />
Morganite Al2O3 Nickel He 1.20 to 1.45<br />
Morganite A1203 Nickel He 1.16, 1.67 to 1.75, 1.35 to 1.65<br />
0.90 to 0.98<br />
P -<br />
These concentrations were made by mixing toge<strong>the</strong>r <strong>the</strong> appropriate weights of <strong>the</strong> salts.<br />
ade with a slotted Morganite crucible inserted between <strong>the</strong> two electrodes as a diaphragm.<br />
62 I<br />
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