1. Tracking high-valent surface iron species in the oxygen evolution reaction on cobalt iron (oxy)hydroxides
- Author
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Seunghwa Lee, Hao Ming Chen, You-Chiuan Chu, Aliki Moysiadou, and Xile Hu
- Subjects
ni ,nanosheets ,Hydrogen ,Inorganic chemistry ,chemistry.chemical_element ,02 engineering and technology ,010402 general chemistry ,electrocatalysts ,size ,01 natural sciences ,7. Clean energy ,catalysts ,Catalysis ,state ,symbols.namesake ,Environmental Chemistry ,biology ,Renewable Energy, Sustainability and the Environment ,Chemistry ,Oxygen evolution ,Active site ,021001 nanoscience & nanotechnology ,Pollution ,0104 chemical sciences ,water oxidation ,Nuclear Energy and Engineering ,13. Climate action ,biology.protein ,symbols ,identification ,Water splitting ,nanoparticles ,oxide ,Absorption (chemistry) ,0210 nano-technology ,Raman spectroscopy ,Cobalt - Abstract
The oxygen evolution reaction (OER) is the bottleneck reaction of water splitting, which can be used to generate green hydrogen from renewable electricity. Cobalt iron oxyhydroxides (CoFeOxHy) are among the most active OER catalysts in alkaline medium. However, the active sites of these catalysts remain unclear. Here we use operando ultraviolet-visible (UV-Vis), X-ray absorption, and Raman spectroscopy to reveal oxidations of both Fe and Co ions in CoFeOxHy during the OER. By analyzing samples with different Fe contents and thickness, we find that the concentration of Fe4+ species at the surface, but not the concentration of Co4+ in the bulk, scales with the catalytic activity. These results indicate an Fe4+-containing active site in CoFeOxHy.
- Published
- 2022
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