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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >The development of a multi-surface soil speciation model for Cd (II) and Pb (II): Comparison of two approaches for metal adsorption to clay fractions
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The development of a multi-surface soil speciation model for Cd (II) and Pb (II): Comparison of two approaches for metal adsorption to clay fractions

机译:Cd(II)和Pb(II)的多表面土壤形态模型的开发:两种金属吸附粘土组分的方法的比较

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摘要

The mobility of toxic metals in soils or sediments is of great concern to scientists and environmentalists since it directly affects the bioavailability of metals and their movement to surface and ground waters. In this study, a multi-surface soil speciation model for Cd (II) and Pb (II) was developed to predict the partition of metals on various soil solid components (e.g. soil organic matter (SOM), oxide mineral, and clay mineral). In previous study, the sorption of metal cations on SOM and oxide minerals has been evaluated by thermodynamically based surface complexation model. However, metal binding to soil clay fractions was normally treated in a simplistic manner: only cation exchange reactions were considered and exchange coefficient was assumed unity. In this study, the binding of metals onto clays was described by a two-site surface sorption model (a basal surface site and an edge site). The model was checked by predicting the adsorption behavior of Cd (II) and Pb (II) onto three selected Chinese soils as a function of pH and ionic strengths. Results showed that the proposed model more accurately predicted the metal adsorption on soils under studied condition, especially in low ionic strength condition, suggesting that adsorption of metals to soil clay fractions need to be considered more carefully when modeling the partition of trace elements in soils. The developed soil speciation model will be useful when evaluating the movement and bioavailability of toxic metals in soil environment.
机译:有毒金属在土壤或沉积物中的迁移率受到科学家和环保主义者的极大关注,因为它直接影响金属的生物利用度及其向地表水和地下水的迁移。在这项研究中,建立了Cd(II)和Pb(II)的多表面土壤形态模型,以预测金属在各种土壤固体成分(例如土壤有机质(SOM),氧化物矿物和粘土矿物)中的分配。在以前的研究中,已经通过基于热力学的表面络合模型评估了金属阳离子在SOM和氧化物矿物上的吸附。然而,通常以简单的方式处理金属与土壤黏土组分的结合:仅考虑阳离子交换反应,并且假定交换系数统一。在这项研究中,通过两点表面吸附模型(基础表面点和边缘点)描述了金属与粘土的结合。通过预测Cd(II)和Pb(II)在三种选定的中国土壤上的吸附行为作为pH和离子强度的函数来检验模型。结果表明,在研究条件下,特别是在低离子强度条件下,该模型可以更准确地预测金属对土壤的吸附,这表明在对土壤中痕量元素的分配进行建模时,应更仔细地考虑金属对土壤黏土组分的吸附。建立的土壤形态模型在评估土壤环境中有毒金属的迁移和生物利用度时将非常有用。

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