Shuo Chen
;
Kaiqin Yue
;
Jiawei Shi
;
Zhicheng Zheng
;
Yuanqing He
;
Hao Wan
;
Gen Chen
;
Ning Zhang
;
Xiaohe Liu
;
Renzhi Ma
Description:
(abstract)Most nonoxide catalysts based on transition metal elements will inevitably change their primitive phases under anodicoxidation conditions in alkaline media. Establishing a relationship between the bulk phase and surface evolution is imperative toreveal the intrinsic catalytic active sites. In this work, it is demonstrated that the introduction of Fe facilitates the phase transition oforthorhombic CoSe2 into its cubic counterpart and then accelerates the Co−Fe hydroxide layer generation on the surface duringelectrocatalytic oxygen evolution reaction (OER). As a result, the Fe-doped cubic CoSe2 catalyst exhibits a significantly enhancedactivity with a considerable overpotential decrease of 79.9 and 66.9 mV to deliver 10 mA·cm−2 accompanied by a Tafel slope of 48.0mV·dec−1 toward OER when compared to orthorhombic CoSe2 and Fe-doped orthorhombic CoSe2, respectively. Density functionaltheory (DFT) calculations reveal that the introduction of Fe on the surface hydroxide layers will tune electron density around Coatoms and raise the d-band center. These findings will provide deep insights into the surface reconstitution of the OER electrocatalysts based on transition metal elements.
Rights:
This document is the Accepted Manuscript version of a Published Work that appeared in final form in Inorganic Chemistry, copyright © 2024 American Chemical Society after peer review and technical editing by the publisher. To access the final edited and published work see https://doi.org/10.1021/acs.inorgchem.4c00568
Keyword: Oxygen evolution reaction, Electrocatalysis
Date published: 2024-04-22
Publisher: American Chemical Society (ACS)
Journal:
Funding:
Manuscript type: Author's version (Accepted manuscript)
MDR DOI: https://doi.org/10.48505/nims.4540
First published URL: https://doi.org/10.1021/acs.inorgchem.4c00568
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Updated at: 2025-04-14 16:30:42 +0900
Published on MDR: 2025-04-14 14:56:25 +0900
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