The vibrational spectroscopy of H-2, N-2, CO and NO adsorbed on the zeolite
ferrierite is described. The spectral modifications induced by the adsorpt
ion process on the protonic form are compared with those observed on the al
kaline-exchanged forms. Different environments of Bronsted sites and of alk
aline counterions in ferrierite are evidenced, which differ in the local el
ectric field associated with the cationic species. These different environm
ents are associated with the cation locations in the channels and cavities.
In particular, ions located in the 10-membered ring channels are more avai
lable for the interaction with CO, N-2 and H-2, while ions in the cages for
m weaker adducts. On passing from lithium-, to sodium- and to potassium-exc
hanged samples; the local fields probed by H-2, N-2 and CO are increasingly
dependent upon the distribution of the ions in the framework. In K-ferrier
ite the interaction cannot be solely described in terms of 1:1 K+/B (B=N-2,
CO) adducts. As far as H-ferrierite is concerned, it is inferred from the
observed shift of the v(OH) mode upon interaction with H-2, N-2 and CO that
the bridged strong acid groups show an acid strength very similar to that
observed for H-ZSM-5, H-mordenite and H-Beta. (C) 2000 Elsevier Science B.V
. All rights reserved.