State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, 68 Jincheng Street, East Lake High-Tech Development Zone, Wuhan, Hubei 430078, China; Hubei Key Laboratory of Yangtze Catchment Environmental Aquatic Science, School of Environmental Studies, China University of Geosciences, 68 Jincheng Street, East Lake High-Tech Development Zone, Wuhan, Hubei 430078, China.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, 68 Jincheng Street, East Lake High-Tech Development Zone, Wuhan, Hubei 430078, China.
Water Res. 2023 Jul 15;240:120071. doi: 10.1016/j.watres.2023.120071. Epub 2023 May 13.
Hydroxyl radical (•OH) oxidation has been identified as a significant pathway for element cycling and contaminant removal in redox fluctuating environments. Fe(II) has been found to be the main electron contributor for •OH production. Despite the recognition of the mechanisms of •OH production from the oxidation of Fe(II) in soils/sediments by O2, the kinetic model about Fe(II) oxidation, •OH production and contaminant removal is not yet clear. To address this knowledge gap, we conducted a series of experiments to explore the variation of different Fe(II) species, •OH and trichloroethylene (TCE, a representative contaminant) during sediment oxygenation, followed by the development of a kinetic model. In this model, Fe(II) species in sediments was divided into three categories based on the sequential chemical extraction method: ion exchangeable Fe(II), surface-adsorbed Fe(II) and mineral structural Fe(II),. Results showed that the kinetic model accurately fitted the concentration time trajectories of different Fe(II) species, •OH and TCE in this study as well as in previous studies. Model analysis indicated that the relative contribution of surface-adsorbed Fe(II) and reactive mineral structural Fe(II) in •OH production was 16.4%-33.9% and 66.1%-83.6%, respectively. However, ion-exchangeable Fe(II) not only fails to contribute to •OH production but also reduces the •OH yield relative to H2O2 decomposition. Poorly reactive mineral structural Fe(II) can serve as an electron pool to regenerate these reactive Fe(II) and facilitate •OH production. Regarding TCE degradation, Fe(II) species plays a dual role in contributing to •OH production while competing with TCE for •OH consumption, with the quenching efficiency being related to their content and reactivity toward •OH. This kinetic model offers a practical approach to describing and predicting •OH production and associated environmental impacts at the oxic-anoxic interface.
羟基自由基(•OH)氧化已被确定为氧化还原波动环境中元素循环和污染物去除的重要途径。已经发现 Fe(II) 是产生•OH 的主要电子供体。尽管已经认识到 O2 氧化土壤/沉积物中的 Fe(II)产生•OH 的机制,但 Fe(II)氧化、•OH 产生和污染物去除的动力学模型尚不清楚。为了解决这一知识空白,我们进行了一系列实验,以探索沉积物充氧过程中不同 Fe(II)物种、•OH 和三氯乙烯(TCE,一种代表性污染物)的变化情况,随后建立了一个动力学模型。在该模型中,根据连续化学提取方法将沉积物中的 Fe(II)物种分为三类:离子交换态 Fe(II)、表面吸附态 Fe(II)和矿物结构态 Fe(II)。结果表明,该动力学模型准确拟合了本研究以及以前研究中不同 Fe(II)物种、•OH 和 TCE 的浓度时间轨迹。模型分析表明,表面吸附态 Fe(II)和反应性矿物结构态 Fe(II)在•OH 生成中的相对贡献分别为 16.4%-33.9%和 66.1%-83.6%。然而,离子交换态 Fe(II)不仅不能促进•OH 的生成,反而会降低相对于 H2O2 分解的•OH 产率。反应性差的矿物结构态 Fe(II)可以作为电子池,再生这些反应性 Fe(II)并促进•OH 的生成。对于 TCE 的降解,Fe(II)物种在促进•OH 生成的同时,与 TCE 竞争•OH 消耗,其猝灭效率与它们的含量和对•OH 的反应性有关。该动力学模型为描述和预测好氧-缺氧界面处•OH 的产生及其相关的环境影响提供了一种实用方法。