The methanol-to-olefin (MTO) process
allows the conversion of methanol/dimethyl
ether into olefins on acidic zeolites via the so-called hydrocarbon
pool mechanism. However, the site and mechanism of formation of the
first carbon–carbon bond are still a matter of debate. Here,
we show that the Lewis acidic Al sites on the 110 facet of γ-Al2O3 can readily activate dimethyl ether to yield
CH4, alkenes, and surface formate species according to
spectroscopic studies combined with a computational approach. The
carbon–carbon forming step as well as the formation of methane
and surface formate involves a transient oxonium ion intermediate,
generated by a hydrogen transfer between surface methoxy species and
coordinated methanol on adjacent Al sites. These results indicate
that extra framework Al centers in acidic zeolites, which are associated
with alumina, can play a key role in the formation of the first carbon–carbon
bond, the initiation step of the industrial MTO process