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污染土壤中锌的形态分析。

Speciation of zinc in contaminated soils.

作者信息

Stephan Chadi H, Courchesne François, Hendershot William H, McGrath Steve P, Chaudri Amar M, Sappin-Didier Valérie, Sauvé Sébastien

机构信息

Department of Chemistry, Université de Montréal, P.O. Box 6128, Centre-Ville, Montréal, QC H3C 3J7, Canada.

出版信息

Environ Pollut. 2008 Sep;155(2):208-16. doi: 10.1016/j.envpol.2007.12.006. Epub 2008 Jan 25.

Abstract

The chemical speciation of zinc in soil solutions is critical to the understanding of its bioavailability and potential toxic effects. We studied the speciation of Zn in soil solution extracts from 66 contaminated soils representative of a wide range of field conditions in both North America and Europe. Within this dataset, we evaluated the links among the dissolved concentrations of zinc and the speciation of Zn(2+), soil solution pH, total soil Zn, dissolved organic matter (DOM), soil organic matter (SOM) and the concentrations of different inorganic anions. The solid-liquid partitioning coefficient (K(d)) for Zn ranged from 17 to 13,100 L kg(-1) soil. The fraction of dissolved Zn bound to DOM varied from 60% to 98% and the soil solution free Zn(2+) varied from 40% to 60% of the labile Zn. Multiple regression equations to predict free Zn(2+), dissolved Zn and the solid-liquid partitioning of Zn are given for potential use in environmental fate modeling and risk assessment. The multiple regressions also highlight some of the most important soil properties controlling the solubility and chemical speciation of zinc in contaminated soils.

摘要

土壤溶液中锌的化学形态对于理解其生物有效性和潜在毒性作用至关重要。我们研究了来自北美和欧洲广泛田间条件下的66种污染土壤的土壤溶液提取物中锌的形态。在该数据集中,我们评估了锌的溶解浓度与Zn(2+)形态、土壤溶液pH值、土壤总锌、溶解有机物(DOM)、土壤有机物(SOM)以及不同无机阴离子浓度之间的联系。锌的固液分配系数(K(d))范围为17至13,100 L kg(-1)土壤。与DOM结合的溶解锌分数从60%到98%不等,土壤溶液中游离Zn(2+)占不稳定锌的40%至60%。给出了预测游离Zn(2+)、溶解锌和锌的固液分配的多元回归方程,可用于环境归宿建模和风险评估。多元回归还突出了一些控制污染土壤中锌溶解度和化学形态的最重要土壤性质。

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