Chinese Journal of Catalysis ›› 2025, Vol. 69: 185-192.DOI: 10.1016/S1872-2067(24)60161-0

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Mechanism of selective reduction of N2O by CO over Fe-β catalysts studied by in-situ/operando spectroscopy

Yucheng Qiana, Shunsaku Yasumurab, Ningqiang Zhanga, Akihiko Anzaia, Takashi Toyaoa, Ken-ichi Shimizua,*()   

  1. aInstitute for Catalysis, Hokkaido University, N-21, W-10, Sapporo 001-0021, Japan
    bInstitute of Industrial Science, The University of Tokyo, Komaba 4-6-1, Meguro, Tokyo 153-8505, Japan
  • Received:2024-09-13 Accepted:2024-10-08 Online:2025-02-18 Published:2025-02-10
  • Contact: 电子信箱: kshimizu@cat.hokudai.ac.jp (K. Shimizu).

Abstract:

Selective reduction of N2O by CO under excess O2 was effectively catalyzed by Fe(0.9 wt%)-exchanged β zeolite (Fe0.9β) in the temperature range of 250-500 °C. Kinetic experiments showed that the apparent activation energy for N2O reduction with CO was lower than that for the direct N2O decomposition, and the rate of N2O reduction with CO at 300 °C was 16 times higher than that for direct N2O decomposition. Reaction order analyses showed that CO and N2O were involved in the kinetically important step, while O2 was not involved in the important step. At 300 °C, the rate of CO oxidation with 0.1% N2O was two times higher than that of CO oxidation with 10% O2. This quantitatively demonstrates the preferential oxidation of CO by N2O under excess O2 over Fe0.9β. Operando/in-situ diffuse reflectance ultraviolet-visible spectroscopy showed a redox-based catalytic cycle; α-Fe-O species are reduced by CO to give CO2 and reduced Fe species, which are then re-oxidized by N2O to regenerate the α-Fe-O species. The initial rate for the regeneration of α-Fe-O species under 0.1% N2O was four times higher than that under 10% O2. This result shows quantitative evidence on the higher reactivity of N2O than O2 for the regeneration of α-Fe-O intermediates, providing a fundamental reason why the Fe0.9β catalyst selectively promotes the CO + N2O reaction under excess O2 rather than the undesired side reaction of CO + O2. The mechanistic model was verified by the results of in-situ Fe K-edge X-ray absorption spectroscopy.

Key words: Fe-exchanged zeolites, N2O, Selective catalytic reduction, In-situ ultraviolet-visible