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| DOE-STD-3013-2004
comparable to those of pure oxides after calcination.
MIS elemental analysis on the 33 site materials studied to date shows only one of
these items has as-received chloride content above 20 wt%. In all cases, the
chloride ion content after 950oC calcination was reduced to less than 8 wt%. In
general, residual chloride salt is expected (and is observed) to be strongly
reduced by calcination, a factor which will restrict moisture uptake by chlorides
before packaging. Sodium and potassium chloride melt below the 950oC
calcination temperature and therefore relatively large particle sizes and low
surfaces areas are likely to result for these phases. A recent literature survey
indicates that these chlorides will not resorb water to an appreciable extent after
calcination unless quite high relative humidities are encountered [Smith et al.
1999].
Residual magnesium and calcium chlorides, on the other hand, can adsorb and
chemically bind as stoichiometric hydrates substantial amounts of water at much
known to partially or completely convert to their respective oxides when heated
in the presence of moisture, as confirmed by MIS elemental composition and x-
Unfortunately, magnesium and calcium chlorides also readily release water with
modest heating. At elevated temperature in sealed containers, this moisture
potentially could migrate to the plutonium oxide phase and physisorb as weakly
bound multiple layers, theoretically exceeding 0.5 wt% equivalent for the oxide
phase. This process, if it happens, likely would affect the equilibrium vapor
pressure of moisture over plutonium oxide, and possibly affect the radiolytic
behavior of the adsorbed water. Therefore, control of time and atmosphere
between calcination and packaging is strongly advised when handling plutonium
oxides containing magnesium and calcium chloride impurities to avoid the
potential for concentrating unacceptable levels of moistures on other phases, and
potential initiation of additional gas generation mechanisms. A survey of practical
experience in storing pyrochemical salts indicates that with reasonable
precautions, moisture readsorption should not pose a major issue [Tandon et al.
1999a].
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