Molten salts containing fluoride ion react destructively with Zeolite
4A through a mechanism that is typical of fluoride reactions with oxyg
en-bearing ceramics such as silica. The resulting product is one that
no longer contains the molecular sieve framework and is therefore usel
ess as an ion-exchange medium. Variations in either the temperature be
tween 500 and 740 degrees C or in the fluoride/chloride concentration
ratio from 0.05 to 1.0 produced little improvement in the stability of
the zeolite framework with respect to fluoride ion attack. Other ion-
exchange media such as mica have been considered, but they should be e
qually affected by the fluoride ion. It was therefore determined that
the fluoride ion must first be removed from molten salt mixtures if al
uminosilicate zeolites are to be used as an ion-exchange media in cont
act with them. Gaseous SiCl4 has been found to remove fluoride ion in
molten salts to at least 0.1 mol % by the reaction: 2CaF(2) + SiCl4 =
2CaCl(2) + SiF4 up arrow. The efficiency of the process is largely det
ermined by the effectiveness of the gas\melt contact. Attractive featu
res of this reaction include ease of separation of unreacted SiCl4 fro
m SiF4 for eventual recycle of both.