在Fe (II) - 酸盐复合物的氧化过程中,酸盐联体介导的活性氧物种的产生
Wei Yan1, Liying Wang1, Chuanyong Jing1
1State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Journal of hazardous materials
|September 5, 2024
概括
酸盐在铁 (Fe ((II)) 氧化过程中增强基 (•OH) 的产生,影响污染物降解. 这项研究揭示了酸盐如何影响环境环境中反应性氧物种的产生.
科学领域:
- 环境化学环境化学
- 地质化学 地质化学
- 降解氧化过程的过程.
背景情况:
- 铁矿物质氧化产生的反应性氧物种 (ROS) 生产对于铁氧化还原循环和有机污染物的命运至关重要.
- 在Fe(II) 氧化过程中影响ROS生成的环境因素在很大程度上被忽视了.
研究的目的:
- 调查酸盐在Fe (II) 氧化过程中增强基 (•OH) 生产中的作用.
- 阐明Fe(II) - 酸盐复合物影响ROS生成和氧激活通路的机制.
主要方法:
- 旋转陷电子旋转共振 (ESR) 实验用于检测OH基.
- 进行p-nitrophenol (PNP) 降解实验,以评估OH的形成.
- 量化PNP降解产品以确定O2激活通路.
- 对酸盐-铁的实验和理论研究 (II) 协调.
主要成果:
- 酸盐在Fe (II) 氧化 (5-50 mM) 时显著增强了OH的产生.
- 已经证明Fe (II) - 酸盐复合物可以促进OH生成.
- •OH形成主要是由连续一个电子O2的减少 (90.2-96.9%).
- 控制的Fe (II) /酸盐摩尔比率为超氧化物 (O2•−) 或OH生产的O2激活通路.
- 酸盐与Fe (II) 的协调起着双重作用:促进O2•−的形成和改变OH的形成路径.
结论:
- 像酸盐这样的天然氧离子在Fe的O2激活中起着重要作用.
- 了解这些机制为地下污染物的现场降解开辟了可能性.
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