Fe/MFI catalysts prepared either by sublimation of FeCl3 onto H-MFI or by s
olid state ion exchange were characterized by XRD, FTIR, and ESR spectrosco
py. Ligated Fe3+ ions, such as (Fe(OH)(2))(+) or (Fe=O)(+) in distorted tet
rahedral coordination, multinuclear oxocations, such as (HO-Fe-O-FeOH)(2+),
and Fe2O3 oxide particles have been identified. Their relative abundances
depend on the Si/Al ratio and the Fe loading. Nitro and nitrate groups, ide
ntified by their FTIR bands, are formed upon exposing Fe/MFI with high Fe l
oading to N2O. These adsorption complexes are reduced with benzene at 200 d
egreesC but not at room temperature. Their reduction with CO occurs at a lo
wer temperature than that of the bridging oxygen. Exposure to N2O at 320 de
greesC and 0.5 kPa pumps 30% more active oxygen into Fe/MFI than calcinatio
n in O-2 of 100 kPa at 500 degreesC. Thermal decomposition releases NO and
O-2 at the same temperature. The catalytic decomposition rate of N2O to N-2
+ 1/2O(2) in diluted feed streams over Fe/MFI is first order in N2O. The r
ate constant is very low for samples with low Fe loading, but jumps to a mu
ch higher value for high Fe loadings, indicating the important role of mult
inuclear Fe clusters in accordance with recent EXAFS results. Stable isothe
rmal oscillations are observed with overexchanged Fe/MFI (Fe/Al = 1; Al/Si
= 1/14), in the presence of H2O vapor, showing that two different states of
catalytic activity exist. No oscillation is observed with a dry feed or ov
er Fe/MFI with low loading. (C) 2000 Academic Press.