The adsorption of pyridine as a probe molecule in the characterization
of Na-faujasites has been investigated with FT-Raman spectroscopy. It
appears that the interaction of pyridine is strongly affected by the
presence of adsorbed water within the zeolite structure. At pyridine c
overages around 180 mg/g of zeolite a signal at 998 cm-1 is observed,
attributed to pyridine adsorbed onto coordinated water. At higher cove
rages this signal decreases, whereas a band at slightly higher wavenum
ber arises due to the interaction with physisorbed water. At low cover
ages an increase in wavenumber is observed, assigned to pyridine adsor
ption on relatively more acidic OH sites or Na+ cations.