氧化还原
化学
傅里叶变换离子回旋共振
反应性(心理学)
硫化地杆菌
转化(遗传学)
溶解有机碳
反应机理
生物转化
配体(生物化学)
分子
环境化学
还原电位
无机化学
地杆菌
氧化还原
质谱法
光化学
化学转化
作者
Xiangjun Meng,Jialin Chi,Mengmeng Yin,Shiyin Wu,Kai Liu,Xin Zhang,Kai Jiang,Christine V. Putnis,Xiaoxia Zhou,Liping Fang,Fangbai Li
标识
DOI:10.1021/acs.est.6c05728
摘要
Abstract Microbial respiration-triggered reductive transformation of dissolved organic matter (DOM) plays a central role in O2 activation and, consequently, As(III) oxidation under fluctuating hydrological conditions. However, the key DOM components and their molecular transformations associated with this electron-transfer process remain poorly resolved. Here, by integrating Fourier transform ion cyclotron resonance mass spectrometry with machine learning, we reveal that fulvic acid (FA), the predominant DOM fraction, undergoes selective molecular transformation by Geobacter sulfurreducens PCA, forming a reactive subpool that drives O2 activation and thereby enhances As(III) oxidation by approximately 2–10 fold. Reaction network analysis reveals that oxygen-rich aromatic precursors are preferentially transformed into more reduced intermediates through decarboxylation, dehydrogenation, and partial reduction pathways. These transformations collectively shift the molecular composition toward lower oxidation states and enhanced redox reactivity. Machine-learning analysis further identifies nitrogen- and sulfur-containing molecules with low oxidation states as the key components governing the overall redox activity of the system. These species represent a functionally distinct fraction of microbially transformed FA with enhanced electron-donating capacity. This study provides molecular-level insights into how microbial DOM transformation regulates O2 activation and As(III) oxidation, offering a mechanistic basis for predicting and manipulating redox reactivity in dynamic soil and sediment systems.
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