Through
synthesizing Ln2Zr2O7 and
LnAlO3 (Ln = La, Nd, Sm) catalysts, the origin of active
sites for oxidative coupling of methane (OCM) on A2B2O7 fluorite and ABO3 perovskite compounds
has been compared and elucidated. Ln2Zr2O7 catalysts show much better reaction performance than the
respective LnAlO3 catalysts at low temperatures (500–600
°C), but the difference will be mitigated significantly above
600 °C. The reaction performance ranks in the order of La2Zr2O7 > Nd2Zr2O7 > Sm2Zr2O7 >
LaAlO3 > NdAlO3 > SmAlO3. It
is revealed that
the unit cell free volume (V
f) plays an
important role in affecting the catalytic activity, and the Ln2Zr2O7 catalysts with a disordered defect
fluorite phase have inherent oxygen vacancies, which can directly
activate gas-phase O2 molecules to generate OCM reactive
O2
– anions. However, the oxygen vacancies
of LnAlO3 with a perovskite structure can only be generated
by lattice distortion/transformation above 600 °C. Moreover,
Ln2Zr2O7 fluorites have weaker B–O
bonds than LnAlO3 perovskites, thus making it easier to
generate surface vacancies as well as active O2
– sites. The surface alkalinity is intimately relevant to the active
oxygen species, which act together to decide the OCM performance on
both types of catalysts. Indeed, this explains that LnAlO3 catalysts show much worse performance than Ln2Zr2O7 catalysts below 600 °C, which will be evidently
improved at elevated temperatures due to phase transformation.