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Cadmium distribution coefficients 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 K-dm, equal to the equilibrium distribution coefficient K-d(eq) and estimated using the conventional batch technique, and the macropore distribution coefficient K-dM, estimated using the modified batch technique. It was found that the conventional approach (using the coefficient K-d(eq) 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 Jurova 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:矩阵分布系数K-dm等于平衡分布系数Kd(eq)并使用常规批处理技术估算;大孔分布系数K-dM使用改进的批处理技术进行估算。发现传统方法(仅使用系数Kd(eq))会低估在Kalinkovo的壤土中大孔中运输的Cd的渗透率约为255倍,而在壤土中的渗透率约为20倍与本研究中提出的方法相比,在马科夫(Macov)进行了实验,在朱罗瓦(Jurova)的粘土中进行了122次实验。

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