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Simulation of chromium transport in the unsaturated zone for predicting contaminant entries into the groundwater

机译:铬在非饱和带中的迁移模拟,以预测污染物进入地下水的情况

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Heavy metal contaminations in the top-soil layers can impose serious threats to groundwater quality. A seepage water prognosis of probable future contaminant entries at the groundwater surface has to take into account the emission characteristics of the source zone and the reactive transport of the contaminated leachate through the unsaturated zone. Here, a possible approach is presented, exemplarily for a site contaminated with chromium, encompassing batch elution experiments, unsaturated soil column leaching experiments with flow interruption, soil monolith lysimeter experiments, and numerical modeling of non-equilibrium solute transport. The prognosis provides a long-term prediction of Cr concentrations at the groundwater surface. It must be emphasized, that the modeling results are uncertain, because several of the parameters in the simulations can be determined only with significant errors. Additionally, the approach is not applicable routinely for every hazardous waste site. Our study reveals, however, that reactive contaminants can possibly reach the groundwater at hazardous concentrations within very short time.
机译:表层土壤中的重金属污染会严重威胁地下水质量。地下水未来可能进入污染物的渗水预后必须考虑到源区的排放特征和被污染的渗滤液通过非饱和区的反应性运输。这里,示例性地提出了一种被铬污染的地点的可行方法,包括分批洗脱实验,具有流动中断的非饱和土壤柱浸出实验,土壤整块溶渗仪实验以及非平衡溶质运移的数值模型。预后提供了地下水表面Cr浓度的长期预测。必须强调的是,建模结果是不确定的,因为只能以明显的误差确定模拟中的几个参数。另外,该方法不适用于每个危险废物场所。然而,我们的研究表明,反应性污染物可能会在很短的时间内以危险浓度到达地下水。

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