Oxygen Splitting and Methane Oxidation over Fe-Mordenite: Insight by the Operando 2D COS UV-Vis-NIR-IR Approach

0583973 - ÚFCH JH 2025 RIV US eng J - Článek v odborném periodiku
Tarach, K. - Sobalska, J. - Held, A. - Dědeček, Jiří - Tabor, Edyta - Góra-Marek, K.
Oxygen Splitting and Methane Oxidation over Fe-Mordenite: Insight by the Operando 2D COS UV-Vis-NIR-IR Approach.
Journal of Physical Chemistry C. Roč. 128, č. 9 (2024), s. 3759-3769. ISSN 1932-7447. E-ISSN 1932-7455
Grant CEP: GA ČR GA22-06737S
Institucionální podpora: RVO:61388955
Klíčová slova: hydrogen-atom transfer * active-site * electronic-structure * bond activation * zeolites * identification * catalysts * dioxygen * acid * hydroxylation
Obor OECD: Physical chemistry
Impakt faktor: 3.7, rok: 2022
Způsob publikování: Open access

Activation of molecular oxygen and subsequent oxidation of methane over Fe sites in mordenite zeolites with different content of framework Al atoms were studied in the continuous regime at low temperatures. For this purpose, reactivity tests of methane oxidation by molecular oxygen over iron mordenite zeolites were combined with an operando 2D COS UV-vis-NIR-IR study to analyze the reaction pathway. The transmission spectra in the visible-NIR-IR range of investigated iron mordenites revealed the structural changes of Fe(II) after O2 treatment and the formation of the spectral features typical for alpha-O stabilized on iron. Mass spectrometry analysis of gaseous products of the simultaneous interaction of methane and oxygen with iron mordenite revealed the formation of methanol, water, carbon monoxide, and carbon dioxide. Moreover, operando 2D COS UV-vis-NIR-IR also evidenced the presence of formaldehyde, formate, carbon dioxide, and carbon monoxide as products of subsequent methanol oxidation. The differences in the reaction pathway of methane oxidation over Fe-mordenite compared to Fe-ferrierite and Fe-*BEA catalysts reflect unique properties of mordenite topology providing isolated alpha-oxygens in individual mordenite pockets, although formed by splitting of molecular oxygen by two cooperating iron ions and the nature of adsorption sites in the mordenite matrix.
Trvalý link: https://hdl.handle.net/11104/0351965