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Release of Ni and Zn from Contaminated Floodplain Soils Under Saturated Flow Conditions

机译:饱和流条件下洪泛区土壤中镍和锌的释放

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摘要

As floodplain soils are often contaminated, we studied the release of trace metals from three topsoil horizons in column experiments with variable flow interruptions and flow velocities, compared it with that in batch leaching tests and evaluated the column data by inverse simulations. Only small proportions (<1%) of trace metals present in the neutral and humic soils were mobilised by the batch leaching tests and the column experiments. Release of Cr, Cu, Ni and Zn in the column experiments was rate-limited, as detected by increased concentrations after flow interruptions. A combination of linear equilibrium and non-equilibrium isotherms reflected the Ni and Zn elution data, with Zn release being slower. Simulated values for initially bound metals available for release are in the same order of magnitude as those determined by the batch leaching tests. However, the consistency of both experimental approaches decreases with increasing rate limitation, as detected here for Zn.
机译:由于洪泛区土壤经常被污染,我们在具有可变流动中断和流速的立柱实验中研究了三个表层土壤中微量金属的释放,并将其与分批浸出测试进行了比较,并通过逆模拟评估了立柱数据。通过分批浸出试验和色谱柱试验,仅中性和腐殖质土壤中存在的痕量金属只有一小部分(<1%)被动员。在色谱柱实验中,铬,铜,镍和锌的释放受到速率的限制,这是通过中断流动后浓度增加来检测的。线性平衡和非平衡等温线的结合反映了Ni和Zn的洗脱数据,而Zn的释放较慢。可用于释放的初始结合金属的模拟值与批量浸出试验确定的模拟值处于相同数量级。但是,这两种实验方法的一致性都随着速率限制的增加而降低,如此处针对Zn所检测到的。

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