A new model has been developed for the estimation of structural acidit
y parameters and the acid amount of zeolites using valence electron de
nsity, atomic polarizability, and chemical composition. Based on this
model, the computed zeolite acidity has been compared with the data ob
tainable from Sanderson's electronegativity model and also with availa
ble experimental data. The general agreement between our calculated va
lues and those reported in the literature has been found to be very go
od in the case of mordenites. It has been established that electronega
tivity equalization (EE(q)) in zeolites could be equally explained via
the electronic polarization process governed by the proposed equation
: EE(q) = 1.67 alpha(p))(N-Q/alpha(Q))(N-R/alpha(R))](1/(p+q+r)), wher
e N is the valence electron density and a the atomic polarizabilities
of the constituting atoms expressed in the unit of volume, and p, q, r
are the number of atoms representing a molecule of general formula P(
p)O(q)R(r). The relative polarizing power of structures has also been
reported as a function of Al content. This means that increased bond p
olarization will result in enhanced acidic behavior of the protons upo
n interaction with basic substrate molecule. This is why relative pola
rizing powers, alpha'(p), are directly related to the Al content, the
acidity [H+], and shrinkage effect of bond lengths (D-t-0).