4.8 Article

Revealing Active Sites and Reaction Pathways in Methane Non-Oxidative Coupling over Iron-Containing Zeolites

Journal

Publisher

WILEY-V C H VERLAG GMBH
DOI: 10.1002/anie.202306196

Keywords

C-C Coupling; Iron; Methane; Non-Oxidative; Zeolites

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Non-oxidative coupling of methane enables the direct production of ethylene from natural gas. By using siliceous [Fe]zeolites with MFI and CHA topologies, high selectivity to ethylene and ethane (>90% for MFI and >99% for CHA) was achieved. Deactivated [Fe]zeolites can be regenerated by burning coke in air. In situ X-ray absorption spectroscopy and photoelectron photoion coincidence spectroscopy were employed to investigate the reaction mechanism, revealing the formation of methyl radicals as intermediates and proposing a reaction network leading to polyaromatic species over [Fe]MFI.
Non-oxidative coupling of methane is a promising route to obtain ethylene directly from natural gas. We synthesized siliceous [Fe]zeolites with MFI and CHA topologies and found that they display high selectivity (>90 % for MFI and >99 % for CHA) to ethylene and ethane among gas-phase products. Deactivated [Fe]zeolites can be regenerated by burning coke in air. In situ X-ray absorption spectroscopy demonstrates that the isolated Fe3+ centers in zeolite framework of fresh catalysts are reduced during the reaction to the active sites, including Fe2+ species and Fe (oxy)carbides dispersed in zeolite pores. Photoelectron photoion coincidence spectroscopy results show that methyl radicals are the reaction intermediates formed upon methane activation. Ethane is formed by methyl radical coupling, followed by its dehydrogenation to ethylene. Based on the observation of intermediates including allene, vinylacetylene, 1,3-butadiene, 2-butyne, and cyclopentadiene over [Fe]MFI, a reaction network is proposed leading to polyaromatic species. Such reaction intermediates are not observed over the small-pore [Fe]CHA, where ethylene and ethane are the only gas-phase products.

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