236
A. Gannouni et al. / Journal of Catalysis 289 (2012) 227–237
spectra of the supports, namely ½Hꢃ22þ ꢁ ½6ð6 ꢀ MRÞꢃa2ꢀ; ½Hꢃ22þꢁ ½6ð6ꢀ
oxidation of Pd2+, three species are likely to exist, namely [PdO]2+
,
2ꢀ
2ꢀ
MRÞꢃ2bꢀ; ½Hꢃ22þ ꢁ ½8ð8 ꢀ MRÞꢃa and ½Hꢃ22þ ꢁ ½8ð8 ꢀ MRÞꢃb (Fig. 6a). On
the other hand, our simulations of the spectra corresponding to
the systems obtained when PdO2+ is deposited onto [8(8 ꢀ MR)]b,
[8(8 ꢀ MR)]a, [6(6 ꢀ MR)]b, and [6(6 ꢀ MR)]a show a good agree-
ment with the experimental spectra (Fig. 6b). Indeed, these bands
are associated with vibrational modes of PdO2+ in interaction with
[PdOH]2+, and [Pd(OH)2]2+ in 8-membered rings. Such 8-mem-
bered rings have already been invoked in Mordenite as the sites
for incorporating PdO [56]. In forthcoming contributions, we will
examine the reactivity of the oxidized species identified in the
present work for CH4 oxidation reactions and the effect of the Si/
Al molar ratio.
MS2ꢀ that at 630 cmꢀ1 to (PdO) and that at 274 cmꢀ1 to combina-
m
tions of PdO out-of-plane and in-plane bending modes coupled
with support modes. Hence, the band at 630 cmꢀ1 can be associ-
ated with the Raman active B1g vibrational modes of PdO [72].
The broadening of this band implies that the amorphous environ-
ment affects the vibrations as suggested by Demoulin et al. [72].
Moreover, among all the other Pd oxidized forms for which the
Raman spectra have been simulated, two, namely ½PdOHꢃ2þꢁ
Acknowledgments
The authors would like to thank G. Montagnac for Raman exper-
iments, Sandrine Denis-Quanquin for the solid-State NMR experi-
ments, and Lhoussain Khrouz for the ESR measurements. Grants
of computer time from Pole of numerical simulations (PSMN) in
Ecole Normale Supérieure de Lyon are gratefully acknowledged.
2ꢀ
½8ð8 ꢀ MRÞꢃb and ½PdðOHÞ2ꢃ2þ ꢁ ½8ð8 ꢀ MRÞꢃ2bꢀ, display spectra in
agreement with the experimental one. To summarize the results,
the simulated spectra of the three most likely structures are gath-
ered in Fig. 8 with the experimental one. The spectrum for
Appendix A. Supplementary material
Supplementary data associated with this article can be found, in
2ꢀ
½PdOꢃ2þ ꢁ ½8ð8 ꢀ MRÞꢃb differs from that shown in Fig. 6 by the
relative intensity of the peaks because the level of calculation is
different (B3LYP vs. B3LYP//PBE). The two peaks at 606 and
References
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390–386, and 281–270 cmꢀ1 and hence are in agreement with
the experimental data.
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a
[PdO]2+ oxo group. By comparison of the