Static lattice computer modelling techniques are applied to investigate the
framework and extra-framework cation distribution in clinoptilolite/heulan
dite zeolitic materials. The results emphasise the close coupling between t
he framework Al distribution and the location of the extra-framework cation
s. In the majority of the polymorphs, Al is predicted to be preferentially
localised at the T2 and T3 crystallographic sites. Extra-framework cation d
istributions are often controlled by a strong driving force for the locatio
n of Ca2+ close to Al-rich regions. Cation-cation repulsion also play a sub
stantial role in controlling the position of extra-framework cations. We fi
nd significant differences in both the distribution of Al in the framework
and in the location and distribution of the extra-framework cations dependi
ng on the exact composition of the heulandite-structured material considere
d.