化学
选择性
催化作用
浸出(土壤学)
氧气
无机化学
氧化还原
抗氧化剂
铁蛋白
核化学
药物化学
有机化学
生物化学
土壤科学
环境科学
土壤水分
作者
Xuwen Cao,Caixia Zhu,Qing Hong,Xinghua Chen,Kaiyuan Wang,Yanfei Shen,Songqin Liu,Yuanjian Zhang
标识
DOI:10.1002/ange.202302463
摘要
Abstract Ascorbate (H2A) is a well‐known antioxidant to protect cellular components from free radical damage and has also emerged as a pro‐oxidant in cancer therapies. However, such “contradictory” mechanisms underlying H2A oxidation are not well understood. Herein, we report Fe leaching during catalytic H2A oxidation using an Fe−N−C nanozyme as a ferritin mimic and its influence on the selectivity of the oxygen reduction reaction (ORR). Owing to the heterogeneity, the Fe‐Nx sites in Fe−N−C primarily catalyzed H2A oxidation and 4 e− ORR via an iron‐oxo intermediate. Nonetheless, trace O2⋅− produced by marginal N−C sites through 2 e− ORR accumulated and attacked Fe‐Nx sites, leading to the linear leakage of unstable Fe ions up to 420 ppb when the H2A concentration increased to 2 mM. As a result, a substantial fraction (ca. 40 %) of the N−C sites on Fe−N−C were activated, and a new 2+2 e− ORR path was finally enabled, along with Fenton‐type H2A oxidation. Consequently, after Fe ions diffused into the bulk solution, the ORR at the N−C sites stopped at H2O2 production, which was the origin of the pro‐oxidant effect of H2A.
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