褐铁矿
氧气
X射线吸收精细结构
催化作用
氧气储存
阿累尼乌斯方程
钙钛矿(结构)
扩展X射线吸收精细结构
化学
动力学
活化能
无机化学
材料科学
化学物理
物理化学
结晶学
吸收光谱法
光谱学
量子力学
物理
生物化学
有机化学
作者
Kazuki Tamai,Saburo Hosokawa,Kenya Onishi,Chikara Watanabe,Kazúo Kato,Hiroyuki Asakura,Kentaro Teramura,Tsunehiro Tanaka
出处
期刊:ACS Catalysis
[American Chemical Society]
日期:2020-01-22
卷期号:10 (4): 2528-2537
被引量:20
标识
DOI:10.1021/acscatal.9b03857
摘要
In situ observation is a powerful and interesting technique for the characterization of functional materials in their working states. In this study, we used in situ dispersive X-ray absorption fine structure (DXAFS) measurements to observe the lattice oxygen dynamics in SrFeO 3−δ and Sr 3 Fe 2 O 7−δ during NO oxidation. The white-line intensities of Sr K-edge XAFS reflect the concentration of oxygen vacancies, and the lattice oxygen dynamics during NO oxidation are observed. Using a kinetics model, the rate-determining step (RDS) for NO oxidation was found to be an oxygen migration step. The activation energy obtained from the Arrhenius plots for Sr 3 Fe 2 O 7−δ is much smaller than that obtained for SrFeO 3−δ . Sr 3 Fe 2 O 7−δ with a Ruddlesden–Popper-type layered perovskite can release oxygen with relatively small structural rearrangements. In contrast, SrFeO 3−δ requires a significant rearrangement of oxygen vacancies to form the brownmillerite phase and the transformation restricts the oxygen release rate. The oxygen storage profiles with O 2 also show that the RDS is the oxygen migration step, although the dissociative adsorption of O 2 suppresses oxygen storage at low temperatures. The lattice oxygen dynamics obtained from the DXAFS measurements, which cannot be obtained from steady-state kinetics experiments, reveal the importance of the perovskite structure for NO oxidation.
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