塔菲尔方程
析氧
化学
过电位
赤铁矿
无机化学
氧化物
电催化剂
分解水
磁铁矿
催化作用
化学工程
氧化铁
电化学
矿物学
物理化学
电极
光催化
有机化学
工程类
作者
Wai Ling Kwong,Cheng Choo Lee,Andrey Shchukarev,Erik Björn,Johannes Messinger
标识
DOI:10.1016/j.jcat.2018.06.018
摘要
Stable and efficient oxygen evolution reaction (OER) catalysts for the oxidation of water to dioxygen in highly acidic media are currently limited to expensive noble metal (Ir and Ru) oxides since presently known OER catalysts made of inexpensive earth-abundant materials generally suffer anodic corrosion at low pH. In this study, we report that a mixed-polymorph film comprising maghemite and hematite, prepared using spray pyrolysis deposition followed by low-temperature annealing, showed a sustained OER rate (>24 h) corresponding to a current density of 10 mA cm−2 at an initial overpotential of 650 mV, with a Tafel slope of only 56 mV dec−1 and near-100% Faradaic efficiency in 0.5 M H2SO4 (pH 0.3). This performance is remarkable, since iron (III) oxide films comprising only maghemite were found to exhibit a comparable intrinsic activity, but considerably lower stability for OER, while films of pure hematite were OER-inactive. These results are explained by the differences in the polymorph crystal structures, which cause different electrical conductivity and surface interactions with water molecules and protons. Our findings not only reveal the potential of iron (III) oxide as acid-stable OER catalyst, but also highlight the important yet hitherto largely unexplored effect of crystal polymorphism on electrocatalytic OER performance.
科研通智能强力驱动
Strongly Powered by AbleSci AI