As has been proven earlier, ruthenium-containing NaHY zeolites are abl
e to catalyze the decomposition of ammonia at temperatures from 300 to
450 degrees C. In such catalysts, ruthenium cations are still present
, even after heat treatment in high vacuum at 400 degrees C; they can
be detected using ammonia and/or pyridine as probes for Fourier transf
orm IR spectroscopy. They reside both in supercages and in sodalite ca
ges. Various intermediates of the decomposition of the Ru(NH3)(6)NaY c
omplex on heat treatment in high vacuum were identified via in situ IR
spectroscopy; in particular, evidence for the formation of complexes
with nitrosyl ligands was obtained. It was shown that partially decomp
osed (deammoniated) Ru(NH3)(6)NaY complexes can be recovered to some e
xtent by readsorption of ammonia. Ruthenium-containing species were lo
calized either in the supercages or in the small cavities as shown by
LR spectroscopy employing ammonia and pyridine as probes, The acidic p
roperties of variously treated Ru(NH3)(6)NaY zeolites were characteriz
ed via temperature-programmed desorption (TPD) of ammonia, which was m
onitored by mass spectrometry. A strong interaction between ruthenium-
containing species and the zeolite framework, leading to a lack of ove
rtone and combination modes in the near infrared, is confirmed. Invest
igations of Ru(NH3)(6)NaY samples by X-ray photoelectron spectroscopy
under the same conditions as applied for IR and TPD studies revealed t
hat, at variance with the results usually obtained after heat treatmen
t of Ru(NH3)(6)NaY in high vacuum, no significant formation of rutheni
um metal species through autoreduction occurred. Rather, a particular
form of a cation-exchanged Ru, Na-Y zeolite was obtained. (C) 1997 Aca
demic Press.