The predictions of a previously developed small cluster model for boun
d Cu ions and their interactions with CO and NO in Cu-exchanged zeolit
es [Schneider, W.F.; Hass, K.C,; Ramprasad, R; Adams, J.B. J. Phys. Ch
em. 1996, 100, 6032] are compared to those of a series of larger, more
realistic cluster models. The hypothetical case of Cu-n+ (n = 0, 1, 2
) coordinated to a single framework oxygen atom, described in the simp
lest model as CuOH2n+, is first examined in detail. The larger cluster
s considered include explicit Si or Al tetrahedral sites and are termi
nated by either H or OH. For nominal Cu(0) and Cu(I) oxidation states,
the qualitative predictions of the original ''water-ligand'' model ar
e found to be extremely robust, as are quantitative aspects of CO and
NO binding. More pronounced differences between models are observed fo
r a nominal Cu(II) oxidation state, due primarily to the tendency of t
he zeolitic portions of the larger clusters to reduce the Cu. The coor
dination of Cu-n+ (n = 1, 2) to a more realistic 4-fold coordination s
ite model is similarly examined and compared to the results for Cu(OH2
)(4)(n+). Excellent agreement is obtained between the water-ligand and
cluster models for both Cu(I) and Cu(II) in this case. The results in
dicate that proper treatment of the local coordination environment of
a Cu ion exchanged into a zeolite is of greater importance for describ
ing chemistry on the Cu site than is use of a ''realistic'' model for
an individual bridge oxygen site. The implications of these results fo
r future modeling studies of Cu zeolites are discussed.