Quantitative data obtained by thermal analysis proved to be consistent
with the stoichiometry expected for incorporation of indium(I) ions i
nto Y zeolite by reductive solid-state ion exchange upon treatment of
ground In2O3/NH4NaY mixtures in a hydrogen atmosphere at temperatures
of 620-760 K. Detailed information on the complex process was obtained
by IR spectroscopy. Both high frequency (HF) and low frequency (LF) h
ydroxyl groups are involved in the solid-state ion-exchange process, t
he HF ones showing higher reactivity. Reoxidation of the formed indium
(I) lattice cations was found to proceed at relatively low temperature
s (300-400 K) and to result, dependent on the excess of hydroxyl group
s over In+ lattice cations, in the formation of In3+ and/or cationic I
n(III) species comprising 'extra-framework oxygen'. The cationic indiu
m species obtained after reduction and reoxidation were characterized
by their interaction with pyridine applied as probe molecule. Adsorpti
on of water on the cationic indium(III) species results in the formati
on of Bronsted-acid sites (Zn(OH)(2)(+)) the acid strength of which is
significantly weaker than that of 'bridged' hydroxyls. The reduction/
reoxidation cycle proved to be fully reversible.