The rate and relative capacity of retention of Cr(III) and Hg(II) ions from
aqueous media in some synthetic (4A, 5A and NaX) and natural zeolites (cli
noptilolite, erionite and mordenite) has been studied. The exchange rate of
Cr(III) in the zeolites is controlled by the size of the pores and by the
exchange capacity of the materials, and the exchange rate of Hg(II) is main
ly controlled by the Si/AI ratio of the zeolites. The partial exchange of N
a+ for NH4+ in the NaX zeolite improves the exchange rate of Cr(III), but t
his exchange rate is not affected by the partial exchange of Na+ for La(III
), probably due to the La(III) ions being located in sites non accessible t
o Cr(III).