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- Language
- English
- Conflict of Interest
- In relation to this article, we declare that there is no conflict of interest.
- Publication history
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Received April 13, 2026
Accepted June 15, 2026
Available online October 25, 2026
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This is an Open-Access article distributed under the terms of the Creative Commons Attribution Non-Commercial License (http://creativecommons.org/licenses/bync/3.0) which permits
unrestricted non-commercial use, distribution, and reproduction in any medium, provided the original work is properly cited.
Most Cited
Post-Plasma Catalytic Partial Oxidation of Methane to Light Oxygenates Over Cu- and Ag-Modified CHA Zeolites
https://doi.org/10.1007/s11814-026-00776-2
Abstract
Selective oxidation of methane to light oxygenates under mild conditions remains challenging because thermal activation
commonly leads to deep oxidation and carbon deposition. Here, a post-plasma catalysis (PPC) system integrating dielectric
barrier discharge (DBD) plasma with Cu- and Ag-exchanged CHA-type zeolites, SAPO-34 and SSZ-13, enabled roomtemperature
conversion of methane to methanol and other oxygenates. Structural characterization confirmed that the CHA
framework was largely preserved after metal exchange, with Cu species finely dispersed within the zeolite matrix, whereas
Ag species were located mainly on the external surface. Under mild plasma conditions, CHA-based supports outperformed
MFI- and BEA-type zeolites, giving higher selectivity toward oxygenates, including methanol and formaldehyde, together
with lower coke formation, underscoring the role of zeolite confinement. Among the catalysts examined, Cu/SAPO-34 and
Cu/SSZ-13 showed the best balance of methane conversion and oxygenate selectivity, and maintained performance over
five consecutive short-term cycles. The introduction of Ag further shifted the product distribution from methanol toward
formaldehyde. These findings identify Cu- and Ag-supported CHA zeolites as promising catalysts for energy-efficient
plasma-assisted methane upgrading and highlight the combined importance of zeolite confinement and metal identity in
governing oxygenate distribution.

