Involvement
of suprafacial and intrafacial oxygen species in catalytic
combustion of methane over the (100) faceted cobalt spinel was systematically
examined as a function of temperature and CH4 conversion
(X
CH4
). The clear-cut Co3O4 nanocubes of uniform size were synthesized using
a hydrothermal method and characterized with XRD, RS, HR-TEM, XRF,
TPSR (CH4/16/18O2), and SSITKA (CH4/16/18O2) techniques. The experimental
results were corroborated by first-principles thermodynamic and DFT+U
molecular modeling, providing a rational framework for a detailed
understanding of the origin of a different redox comportment of the
catalyst with the varying temperature and its mechanistic implications.
Three temperature/conversion stages of the methane oxidation reaction
were distinguished, depending on involvement of the adsorbed or lattice
oxygen and the redox state of the catalyst. A stoichiometric (100)
surface region (300 °C < T < 450 °C, X
CH4
< 25%) is featured by the
dominant suprafacial (Langmuir–Hinshelwood) mechanism of methane
oxidation. A region of slightly defected surface (450 °C < T < 650 °C, 25% < X
CH4
< 80%), in which oxygen vacancies produced upon
CO2 and H2O release are virtually refilled by
dioxygen, is characterized by coexistence of the suprafacial (Langmuir–Hinshelwood)
and intrafacial (Mars–van Krevelen) mechanistic steps. In a
nonstoichiometric surface region (T > 650 °C, X
CH4
> 80%), the oxygen vacancies
are only partially refilled, the catalyst is significantly reduced,
and methane is combusted according to the Mars–van Krevelen
scheme. Molecular modeling revealed that the suprafacial Co–Oads adoxygen species are more active (ΔE
a = 0.83 eV) than the intrafacial Co–Osurf surface sites (ΔE
a = 1.11 eV)
in the CH4 oxidation. The (100) surface state diagrams
for the three distinguished conversion regions were constructed to
elucidate the catalyst thermodynamic behavior under those conditions.
It was shown that the activity of cobalt spinel is maintained by redox
autotuning of the catalyst and dynamic adjustment of uneven participation
of the suprafacial and intrafacial oxygen species in methane oxidation
to the actual reaction conditions. These factors have important structural
and mechanistic consequences for the catalytic CH4 combustion
on cobalt spinel and related systems, controlling not only the sustainable
versus the stoichiometric turnovers but also for the prevalence or
coexistence of the Langmuir–Hinshelwood and the Mars–van
Krevelen mechanisms with the reaction progress.