Am3+ and Eu3+/alkali cation exchange selectivity was studied on mordenite a
nd zeolite L at 25 to 60 degreesC to examine the effect of their openings o
f ion-exchange sites. The corrected selectivity coefficient at the infinite
simal exchange increased in the order of Eu3+ < Am3+ on mordenite and Am3< Eu3+ On zeolite L. The selectivity reversal did not reflect the effect of
the ionic form, but reflected the dimension of the opening of the ion-exch
ange site and charge of trivalent cations, since the crystal ionic radii of
alkali cations were much smaller than the openings of these zeolites (7-8
Angstrom).