Alkali-metal aluminosilicates with the quartz, cristobalite and tridym
ite structures possess zeolitic behaviour when imperfectly crystallise
d. In aqueous solution these novel materials display a level of cation
exchange which is comparable with synthetic zeolites. In contrast, wh
en they are well crystallised these stuffed silica polymorphs, as they
are also known, do not possess this cation exchange behaviour. They c
an be prepared simply from clay minerals and have potential as inexpen
sive inorganic cation exchangers.