Trimetallic oxyhydroxides as active sites for large-current-density alkaline oxygen evolution and overall water splitting

• DOI: 10.1016/j.jmst.2021.08.083
• Publication Date: 2021-11-09T16:12:52Z
• Authors: Lei Chen; Yunpeng Wang; Xin Zhao; Yuchao Wang; Qian Li; Qichen Wang; Yougen Tang; Yongpeng Lei
• Keywords: Oxygen evolution; Overpotential; Alkaline earth metal

Abstract Earth-abundant electrocatalysts for large-current-density water splitting under alkaline condition are desirable. Oxygen evolution reaction, which is a bottleneck of the overall water splitting, faces the problems of complicated reconstruction and deficiency in rational design of active sites. Herein, we report a series of transition metal chalcogenides for alkaline OER. Among them, FeCoNi(S) displayed a low overpotential of 293 mV to deliver a current density of 500 mA cm−2, which is in the top level of non-precious metal based OER electrocatalysts. A combination of (ex) in situ characterizations and DFT calculation shows that Ni(Fe,Co) trimetallic oxyhydroxides were the active sites for highly-efficient OER. Furthermore, for FeCoNi(S), when used as a bifunctional catalyst for water splitting, it only required a cell voltage of 1.84 V to deliver ∼500 mA cm−2 with extraordinary long-term stability over 2000 h. This work provides the comprehension of high-efficiency, robust catalysts for OER and overall water splitting at large current densities in alkaline media.