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Subsurface A-site vacancy activates lattice oxygen in perovskite ferrites for methane anaerobic oxidation to syngas

Tuning the oxygen activity in perovskite oxides (ABO 3 ) is promising to surmount the trade-off between activity and selectivity in redox reactions. However, this remains challenging due to the limited understanding in its activation mechanism. Herein, we propose the discovery that generating subsur...

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Published in:Nature communications 2024-06, Vol.15 (1), p.5422-11, Article 5422
Main Authors: He, Jiahui, Wang, Tengjiao, Bi, Xueqian, Tian, Yubo, Huang, Chuande, Xu, Weibin, Hu, Yue, Wang, Zhen, Jiang, Bo, Gao, Yuming, Zhu, Yanyan, Wang, Xiaodong
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Language:English
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Summary:Tuning the oxygen activity in perovskite oxides (ABO 3 ) is promising to surmount the trade-off between activity and selectivity in redox reactions. However, this remains challenging due to the limited understanding in its activation mechanism. Herein, we propose the discovery that generating subsurface A-site cation (La sub. ) vacancy beneath surface Fe-O layer greatly improved the oxygen activity in LaFeO 3 , rendering enhanced methane conversion that is 2.9-fold higher than stoichiometric LaFeO 3 while maintaining high syngas selectivity of 98% in anaerobic oxidation. Experimental and theoretical studies reveal that absence of La sub. -O interaction lowered the electron density over oxygen and improved the oxygen mobility, which reduced the barrier for C-H bond cleavage and promoted the oxidation of C-atom, substantially boosting methane-to-syngas conversion. This discovery highlights the importance of A-site cations in modulating electronic state of oxygen, which is fundamentally different from the traditional scheme that mainly credits the redox activity to B-site cations and can pave a new avenue for designing prospective redox catalysts. Tuning the oxygen activity in perovskite oxides (ABO 3 ) holds great potential for overcoming the trade-off between activity and selectivity in redox reactions. This paper highlights how A-site cations influence the electronic state of oxygen and how subsurface A-site vacancies enhance oxygen activity for improved methane conversion.
ISSN:2041-1723
2041-1723
DOI:10.1038/s41467-024-49776-y