溶解
氧还原
氧气
化学
氧还原反应
还原(数学)
无机化学
电化学
电极
物理化学
有机化学
几何学
数学
作者
Angus Pedersen,Kavita Kumar,Yu-Ping Ku,Vincent Martin,Laëtitia Dubau,Keyla Teixeira Santos,Jesús Barrio,Viktoriia A. Saveleva,Pieter Glatzel,Vinod K. Paidi,Xiaoyan Li,Andreas Hutzler,Maria‐Magdalena Titirici,Antoine Bonnefont,Serhiy Cherevko,Ifan E. L. Stephens,Frédéric Maillard
摘要
consumption and therefore pH increase (pH = 8-9) within the bulk Fe-N-C layer facilitate precipitation of Fe cations. This work provides a unified view on the Fe dissolution degradation mechanism for a model Fe-N-C in both high-throughput flow cell and practical operating GDE conditions, underscoring the crucial role of local pH in regulating the stability of the active sites.
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