低温CO氧化对氧化表面的协同效应
Pablo G Lustemberg1, Chengwu Yang2,3, Yuemin Wang4
1Institute of Catalysis and Petrochemistry, CSIC, 28049 Madrid, Spain.
Journal of the American Chemical Society
|February 16, 2025
概括
地下氧气空缺导致二氧化 (CeO2) 的低温一氧化碳. 这些空隙迁移到表面,激活二氧化物 (O2) 并形成通过过氧途径促进二氧化碳生产的中间体.
科学领域:
- 表面科学
- 催化剂
- 计算化学
背景情况:
- 一氧化碳 (CO) 与活性氧化物 (O2) 在金属氧化物上产生二氧化碳的反应至关重要,但人们对其了解甚少.
- 在这个过程中氧气空位和活性氧的作用需要进一步阐明.
研究的目的:
- 在二氧化 (CeO2) 模型系统上研究低温CO氧化机制.
- 确定氧气空位和活性O2物种在CO氧化中的作用.
主要方法:
- 使用红外反射吸收光谱 (IRRAS) 来研究单晶CeO2的反应.
- 用自旋极化密度函数理论 (DFT) 的计算来探索反应机制和能量学.
主要成果:
- 暴露降低的CeO2到O2在80K并没有形成超氧或超氧物种.
- 在吸附的CO的存在下,发生了低温氧化,消耗了CO并氧化了CeO2基质.
- 发现氧气空隙从地下迁移到表面,激活O2并形成中间体.
结论:
- 提出了一种涉及地下氧空位迁移的新机制,用于低温CO氧化.
- 过氧介导途径被认为比碳酸盐途径在低温下更有利于CO氧化.
- 地下氧气空缺在CeO2上的O2激活和CO氧化中起着动态作用.
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