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溶解有机质对三峡水库消落带重金属吸附解吸行为的影响。

Effect of dissolved organic matters on adsorption and desorption behavior of heavy metals in a water-level-fluctuation zone of the Three Gorges Reservoir, China.

机构信息

College of Resources and Environment, Chengdu University of Information Technology, Chengdu, Sichuan, 610225, China; Key Laboratory of the Three Gorges Reservoir Region's Eco-Environments of MOE, Chongqing University, Chongqing, 400045, China.

College of Chemical and Environmental Engineering, Chongqing Three Gorges University, Wanzhou, Chongqing, 404000, China.

出版信息

Ecotoxicol Environ Saf. 2019 Dec 15;185:109695. doi: 10.1016/j.ecoenv.2019.109695. Epub 2019 Sep 29.

Abstract

Operation of recession and inundation in Three Gorges Reservoir (TGR) revealed a potential contribution to the migration of heavy metals in soil and fluvial systems, thus led to negative ecological impacts. The work herein investigated the concentration and speciation of three typical heavy metals (Cd, Cr and Cu) in a water-level-fluctuation zone of TGR, as well as simulated the adsorption and desorption behavior of heavy metals on soils, which aimed at elucidating the fate of heavy metals in this special area. Field investigation revealed that water level fluctuation greatly enabled the migration of heavy metals to inner or upper soil layers. Laboratory experiments showed that adsorption of Cd(II) was a chemical process and dissolved organic matters (DOM) in soils strengthened the combination of Cd(II) to soil surface which inhibited the desorption process. Cr(VI) was physically adsorbed and readily to be desorbed. DOM enabled deposition of Cr(VI) in soils. Cation exchange was dominate mechanism in Cu(II) adsorption process, whereas DOM presented positive effects on desorption of Cu(II). The results presented in this study would provide basic theory for scientific research in TGR.

摘要

三峡水库的蓄水和放水运行揭示了其对土壤和河流系统中重金属迁移的潜在贡献,从而导致了负面的生态影响。本研究调查了三峡水库水位波动区三种典型重金属(Cd、Cr 和 Cu)的浓度和形态,模拟了重金属在土壤上的吸附和解吸行为,旨在阐明重金属在这一特殊区域的归宿。野外调查表明,水位波动极大地促进了重金属向内部或上层土壤的迁移。实验室实验表明,Cd(II)的吸附是一个化学过程,土壤中的溶解有机质(DOM)加强了 Cd(II)与土壤表面的结合,抑制了解吸过程。Cr(VI)是被物理吸附的,容易被解吸。DOM 促进了 Cr(VI)在土壤中的沉积。Cu(II)吸附过程中,阳离子交换是主要机制,而 DOM 对 Cu(II)的解吸有积极影响。本研究的结果将为三峡水库的科学研究提供基础理论。

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