Nature of the Surface Intermediates Formed from Methane on Cu-ZSM‑5 Zeolite: A Combined Solid-State Nuclear Magnetic Resonance and Density Functional Theory Study

The intermediates formed upon the interaction of methane with Cu-modified ZSM-5 zeolites (Cu/H-ZSM-5) have been analyzed with solid-state NMR spectroscopy and DFT methods. Methane activation by Cu/H-ZSM-5 zeolites gives rise to three distinct surface methoxy-like species (−O–CH3) detected by 13C MAS...

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Veröffentlicht in:Journal of physical chemistry. C 2020-03, Vol.124 (11), p.6242-6252
Hauptverfasser: Kolganov, Alexander A, Gabrienko, Anton A, Yashnik, Svetlana A, Pidko, Evgeny A, Stepanov, Alexander G
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Sprache:eng
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Zusammenfassung:The intermediates formed upon the interaction of methane with Cu-modified ZSM-5 zeolites (Cu/H-ZSM-5) have been analyzed with solid-state NMR spectroscopy and DFT methods. Methane activation by Cu/H-ZSM-5 zeolites gives rise to three distinct surface methoxy-like species (−O–CH3) detected by 13C MAS NMR spectroscopy with specific chemical shifts in the range of 53–63 ppm. DFT calculations on representative cluster models of different sites potentially present in Cu/H-ZSM-5 have been used to assign these signals to (i) methanol adsorbed on two neighboring Cu sites (Cu–(HOCH3)–Cu, 62.6 ppm), (ii) methanol adsorbed on zeolite Brønsted acid sites (52.9 ppm), and (iii) lattice-bound methoxy groups (Si–O­(CH3)–Al, 58.6). The formation of these methoxy-like intermediates depends on the Cu loading and, accordingly, the type of Cu species in the Cu/H-ZSM-5 zeolite. For the sample with low (0.1 wt %) Cu loading containing exclusively mononuclear isolated Cu species, only the intermediates ii and iii have been detected. The Cu-bound intermediate (i) is formed upon methane activation by multinuclear Cu sites featuring Cu–O–Cu bridging moieties present in the materials with relatively higher Cu loading (1.38 wt %). The presented results indicate that methane activation by Cu/H-ZSM-5 can be promoted by both mono- and multinuclear Cu species confined in the zeolite matrix.
ISSN:1932-7447
1932-7455
DOI:10.1021/acs.jpcc.0c00311