Cobalt (Co)‐based oxides show promising activity as precious metal‐free catalysts for the oxygen evolution reaction in proton exchange membrane water electrolysis, but the dissolution of Co has limited the durability of Co 3 O 4 at industrially relevant current densities. This work demonstrates that cation in an octahedral coordination environment accounts for the oxygen evolution activity. Using a mixed inverse‐normal phase spinel Co x Ga (3‐ x ) O 4 as a proof‐of‐concept example, the designed Co 2+ ‐O‐Co 3+ motifs in octahedral sites trigger oxygen evolution through a kinetically favorable radical coupling pathway. Furthermore, lattice oxygen exchange, a leading factor in catalyst structural degradation for normal Co 3 O 4 , is suppressed, as evidenced by isotopic labeling experiments and theoretical calculations. With the optimized catalyst, Co 1.8 Ga 1.2 O 4 , an overpotential of 310 mV at 10 mA cm −2 is reported, with stable operation at 200 mA cm −2 for 200 h in a three‐electrode setup, and a proton exchange membrane electrolyzer operating at 200 mA cm −2 for 450 h.
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Zhou et al. (2024) studied this question.
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