The effects of the Si --> Al substitution on the structure of the siliceous
framework and the structure and vibrational properties of Bronsted acid si
tes in mordenite have been studied using density-functional theory, both in
the local-density approximation and including generalized gradient correct
ions to the exchange-correlation functional. The substitution induces a sub
stantial local deformation of the polytetrahedral geometry of pure-silica m
ordenite. Also the counterions have a strong influence on the geometry of t
he framework. Protonation of bridging (Si)-O-(Al) oxygen atoms is accompani
ed by a further local distortion of the structure. Changes in the bond leng
ths remain well localized to the nearest neighborhood of the perturbation c
enter; O-H stretching frequencies of acidic protons were calculated in both
harmonic and anharmonic approximations, indicating a rather complex relati
onship among stability, frequencies, and local environment of the Bronsted
acid sites.