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不同来源腐殖酸、腐殖质和干酪根对六价铬的吸附、还原和络合的机理及多步动力学模型。

Mechanism and multi-step kinetic modelling of Cr(VI) adsorption, reduction and complexation by humic acid, humin and kerogen from different sources.

机构信息

Beijing Key Laboratory of Water Resources and Environmental Engineering, China University of Geosciences, Beijing, 100083, China.

Department of Water and Sanitation, University of Cape Coast, Cape Coast, Ghana.

出版信息

Environ Sci Pollut Res Int. 2021 Aug;28(29):38985-39000. doi: 10.1007/s11356-021-13519-z. Epub 2021 Mar 20.

Abstract

Humin (HM) and kerogen (KG) are widespread in soils and sediments, which have strong retention effects on the migration and transformation of Cr(VI) in subsurface environment. Previous studies mainly focused on the interaction between Cr(VI) and soluble organic matter, such as humic acid (HA); however, the adsorption and reduction mechanism for Cr(VI) by insoluble HM and KG are still unclear, the processes of which might be quite different from HA due to their different sources and humification degrees. Consequently, in this study, HA, HM and KG extracted from different sources were used to explore the adsorption, reduction and complexation mechanisms of Cr(VI) in soils and sediments, based on which a multi-step kinetic model of Cr(VI) was carried out. According to the results, the retention of Cr(VI) by humus was found to obey a coupling mechanism of "adsorption-reduction-complexation", where Cr(VI) adsorption was by complexation with carboxylic groups by ligand exchange. The phenolic and hydroxylic groups were determined to be the main electron donor for Cr(VI) reduction. Notably, the Cr(III) produced was found to be adsorbed on the surface of humus by complexation on phenolic and hydroxylic groups, and the excesses were released into the liquid phase after the saturation of complexation sites. Based on the revealed mechanism, a multi-step kinetic model for simultaneously describing Cr(VI) adsorption and reduction and behaviour of Cr(III) was proposed producing a better fitting performance (R ≥ 0.984) than the first-order and second-order kinetic models (R ≤ 0.84 and 0.87, respectively) and hence could provide more factual understanding of Cr(VI) transformation in soils and sediments enriched in various types of humus.

摘要

腐殖质(HM)和干酪根(KG)广泛存在于土壤和沉积物中,对地下环境中六价铬(Cr(VI))的迁移转化具有很强的保留作用。先前的研究主要集中在 Cr(VI)与可溶性有机质,如腐殖酸(HA)的相互作用上;然而,由于来源和腐殖化程度不同,不溶性 HM 和 KG 对 Cr(VI)的吸附和还原机制仍不清楚,其过程可能与 HA 有很大不同。因此,本研究采用不同来源提取的 HA、HM 和 KG,探索了 Cr(VI)在土壤和沉积物中的吸附、还原和络合机制,并在此基础上建立了 Cr(VI)的多步动力学模型。结果表明,腐殖质对 Cr(VI)的保留遵循“吸附-还原-络合”的耦合机制,Cr(VI)的吸附是通过配体交换与羧酸基团络合。酚基和羟基被确定为 Cr(VI)还原的主要电子供体。值得注意的是,生成的 Cr(III)通过与酚基和羟基络合被吸附在腐殖质表面,当络合位点饱和后,多余的 Cr(III)被释放到液相中。基于揭示的机制,提出了一个同时描述 Cr(VI)吸附和还原以及 Cr(III)行为的多步动力学模型,其拟合性能(R≥0.984)优于一级和二级动力学模型(R≤0.84 和 0.87),从而可以更深入地了解富含各种类型腐殖质的土壤和沉积物中 Cr(VI)的转化。

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