析氧
镍
催化作用
氧化还原
化学
动力学
无机化学
氧气
化学动力学
反应速率常数
反应速率
反应机理
半反应
光化学
电催化剂
电化学
活动站点
钴
过渡金属
分解水
材料科学
反应级数
反应中间体
作者
Yifeng Wang,Liam Peter Twight,Nicole Alessandra Saguì,Minkyoung Kwak,Shannon Wachter Boettcher,Benjamin Moss,Ifan E. L. Stephens,James Robert Durrant,Reshma R. Rao
出处
期刊:ACS Catalysis
[American Chemical Society]
日期:2026-03-19
卷期号:16 (7): 6749-6757
被引量:4
标识
DOI:10.1021/acscatal.5c09080
摘要
High Resolution Image Download MS PowerPoint Slide Ni x Fe 1– x O y H z is the state-of-the-art catalyst for the oxygen evolution reaction (OER) in alkaline water electrolyzers; however, understanding the impact of Fe on the active sites, reaction mechanism, and consequently intrinsic activity has been under intense debate. In this work, operando UV–vis spectroscopy was used to investigate Fe-free NiO x H y and NiO x H y with Fe selectively incorporated onto the surface. At oxygen-evolution potentials, similar oxidized nickel states were present before and after the Fe incorporation, with negligible changes in their redox potentials. However, the discharge kinetics of the Ni states show a substantial acceleration after the introduction of Fe, consistent with an increase in OER kinetics upon Fe incorporation and formation of active Ni–Fe species. Using optical spectroscopy, we determined the intrinsic reaction time constant per surface Fe site is <0.1 s, which is 2 orders of magnitude faster than Ni sites not in proximity to surface Fe sites (∼10 s), and also an order of magnitude faster than Ni sites in pure NiO x H y (∼1 s). Consequently, we propose that the OER occurs via charge accumulation primarily on Ni centers in these catalysts, followed by hole transport to the surface Fe species where oxygen evolution occurs.
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