208
J.H. Kwak et al. / Journal of Catalysis 287 (2012) 203–209
Following the hydrothermal aging at 800 °C, significant differ-
ences in the H2-TPR patterns were observed, as shown in Fig. 8.
For Cu-Y, sharp peaks at 275 and 295 °C are attributed to the
reduction of bulk-like CuO structures formed during the total
collapse of the zeolite structure. For Cu-beta, two broad reduction
peaks are now present at 305 and 670 °C. As most of the zeolite
structure was still intact after the hydrothermal aging, these H2-
TPR features may still be attributed to the reduction of Cu2+ and
Cu+ ions. Over Cu-ZSM-5, a sharp reduction peak at 270 °C for
bulk-like CuO is observed, as well as broad peaks at 280 and
470 °C, similar to those for Cu-beta. In trying to rationalize these
changes, a couple of points are likely to be relevant. First, prior lit-
erature has reported that H2-TPR reduction peaks are shifted to
higher temperatures when the ion exchange level of Cu is de-
creased [18]. Furthermore, the NMR results described above indi-
cate a moderate loss of Cu ions from the ion exchange sites for
both Cu-beta and Cu-ZSM-5 catalysts with a subsequent formation
of new Cu-aluminum-oxygen complexes where Cu strongly inter-
acts with the Al ions, therefore rendering the 27Al NMR peaks asso-
ciated with these new complexes ‘‘invisible’’ in the spectra. Thus,
the observed shift in peak temperatures and reduction in peak
intensities may represent the reduced occupancy of the zeolite
ion exchange sites by Cu and/or the reduction of Cu ions in the
newly formed Cu-AlOx species.
Fig. 7. H2-TPR profiles of fresh prepared Cu/zeolites; Cu-beta (black), Cu-ZSM-5
(blue), Cu-SSZ-13 (red), and CuY (green). (For interpretation of the references to
color in this figure legend, the reader is referred to the web version of this article.)
Recently, it was reported that there are several exchange sites in-
side chabazite (CHA) zeolites available for Cu ions [17]. Among
them, it has been proposed that Cu cations can occupy two of these
sites: ‘‘site I,’’ located inside the CHA cavity, and ‘‘site IV,’’ inside the
eight-membered ring connecting the CHA cavities. Note that site I
is similar to the exchange sites inside the sodalite cage of FAU zeo-
lite where the Cu2+ to Cu+ reduction has been proposed to occur at
ꢀ300 °C. Based on these previous assignments, it seems reasonable
to propose that the prominent H2-TPR peak at 230 °C is due to the
reduction of Cu2+ to Cu+ at the IV site, while the broad shoulder
peak is perhaps due to Cu2+ to Cu+ reduction for Cu ions at site I.
However, these assignments must be considered as tentative at
best at this point, as they contradict the conclusion of Fickel and
Lobo [7], who proposed the presence of Cu ions exclusively in
one type of cationic positions. Current studies in our laboratory
are aimed solely at understanding the locations of Cu ions in our
in-house synthesized SSZ-13 sample.
On the other hand, for Cu-SSZ-13, Fig. 8 shows that the reduc-
tion peak at 230 °C is still present and that the broad shoulder at
ꢀ300 °C has increased after hydrothermal aging. Furthermore, we
find that essentially the same amount of H2 is consumed for both
the fresh and aged Cu-SSZ-13 samples, suggesting relatively small
changes in the distribution of Cu ions between the likely two zeo-
lytic sites in SSZ-13. This result is consistent with the small ob-
served changes in both the solid state 27Al NMR spectra and SCR
activity for Cu-SSZ-13 catalysts after hydrothermal aging.
Considering the changes observed in 27Al NMR and H2-TPR, it is
likely that some of the Cu2+ ions in aged Cu-ZSM-5 and Cu-beta are
still located in ion exchange positions within zeolite structure and,
thus, responsible for the SCR activity albeit severely suppressed.
On the other hand, both aged Cu-ZSM-5 and Cu-beta exhibited rel-
atively good NOx reduction activity at higher temperatures. Re-
cently, we demonstrated that isolated Cu species on
c-alumina
can be effective in NH3 SCR [19]. The somewhat different struc-
tures for Cu species in these alumina supported catalysts and Cu
ions exchanged into zeolites likely explain the considerable differ-
ences in the optimum temperature ranges for NH3 SCR activity for
these two types of catalysts. Based on these recent results, we pro-
pose that new Cu/AlOx structures that form upon hydrothermal
aging and which exhibit strong interactions between Al ions and
paramagnetic Cu are, at least partially, responsible for the mainte-
nance of higher temperature NH3 SCR activity. Such Cu/AlOx struc-
tures may be thought of as small, isolated Cu-aluminate-like
species which remain dispersed in the intact zeolite channels of
the hydrothermally aged Cu-ZSM-5 and Cu-beta catalysts.
4. Conclusions
The effects of hydrothermal aging on the materials properties
and NH3 SCR activity of Cu-ZSM-5, Cu-BEA, Cu-Y, and Cu-SSZ-13
catalysts were studied here. After hydrothermal treatment at
800 °C for 16 h, Cu-SSZ-13 was found to show essentially no
change in NOx reduction activity, while Cu-Y completely lost its
NH3 SCR activity. Both Cu-ZSM-5 and Cu-BEA were found to lose
NOx reduction activity primarily at low temperatures (<350 °C).
In the presence of equimolar amounts of NO and NO2 in the feed
gas, significant amounts of N2O were produced over the aged Cu-
ZSM-5 and Cu-BEA at all temperatures.
Fig. 8. H2-TPR profiles of Cu/zeolites after hydrothermal aging; Cu-beta (black), Cu-
ZSM-5 (blue), Cu-SSZ-13 (red), and CuY (green). (For interpretation of the
references to colour in this figure legend, the reader is referred to the web version
of this article.)