Direct methane conversion to methanol via chemical
looping using copper-exchanged zeolites has attracted considerable
attention during the last decades and is one of the most-actively
studied processes. Despite the significant progress that has been
made in the design of active systems and the elucidation of active
sites, the effects of zeolite topology and the structure of copper
species on the nature of the reaction products are yet unclear. Herein,
we show that oxygen-activated copper-exchanged zeolites of different
framework types, namely, MOR, MFI, BEA, and FAU, yield different products,
as detected by in situ Fourier-transform infrared
and nuclear magnetic resonance spectroscopy. Molecular methanol, methoxy
species, and dimethyl ether prevail at lower reaction temperatures
(<473–523 K), and CuI carbonyls and gaseous carbon
oxides were detected above 573 K. Methane coupling to C2 and C3 hydrocarbons was shown for the first time over
CuMOR, CuBEA, and CuFAU. The nature and relative fraction of formed
products strongly depend on the structure of the copper active sites,
which is governed by the topology of the zeolite host. Several pathways
of methane transformation over copper-exchanged zeolites are identified,
opening opportunities for tuning the properties of the materials to
achieve the best performance.