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Cadmium distribution coefficeints and Cd transport in structured soils

机译:镉在结构化土壤中的分布系数和镉的迁移

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摘要

In the case of cadmium transport via soil macropores, the short-term duration of an interaction between the reactive solute in aqueous phase and soil, as well as cadmium precipitation or adsorption on particles 10–5 m should be taken into account. Two distribution coefficients are proposed for predicting the cadmium transport in a structured soil: the matrix distribution coefficient Kdm, equal to the equilibrium distribution coefficient Kdeq and estimated using the conventional batch technique, and the macropore distribution coefficient KdM, estimated using the modified batch technique. It was found that the conventional approach (using the coefficient Kdeq only) would underestimate a penetration of the part of Cd transported in the macropores about 255-times in the loamy-sand soil in Kalinkovo, 20-times in the loam soil in Macov, and 122-times in the clay soil in Jurová in comparison with the approach proposed in this study.
机译:在镉通过土壤大孔传输的情况下,应考虑到水相中的反应性溶质与土壤之间的相互作用的短期持续时间,以及镉的沉淀或在<10-5 m的颗粒上的吸附。提出了两种分布系数来预测结构化土壤中的镉迁移:使用常规分批技术估算的等于平衡分布系数Kdeq的基体分布系数Kdm,以及使用改进批处理技术估算的大孔分布系数KdM。发现传统方法(仅使用系数Kdeq)会低估Kalinkovo壤土中大孔中Cd渗透率的255倍,Macov壤土中Cd渗透率的20倍,与本研究中提出的方法相比,在Jurová的粘土中吸收了122倍。

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