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Modeling Solute Transport in Volcanic Ash Soils with CationExchange and Anion Retardation

机译:利用阳离子交换和阴离子迟滞模拟火山灰土壤中的溶质运移

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摘要

Groundwater under agricultural lands is often contaminated by nitrate. In southern Japan, aquifers are covered by volcanic ash soils that can leach nitrate to the groundwater. In this study, column experiments using two volcanic ash soils (Kuroboku and Akahoya) were carried out. A mixed solution of KNO_3 and K_2SO_4 was used in the leaching experiments. Based on the experiments, a reactive transport model was developed using the Constrained Interpolation Profile method for ion transport and used to calculate chemical equilibrium for the cation exchange reactions. Anion adsorption was modeled by retardation in the numerical model. The developed simulation model results were compared to results obtained by the reactive transport model PHAST. The developed model was shown to quite well reproduce general characteristics of the experimental results. Also, the developed model results agreed well with results from PHAST. Slight discrepancy between observed and calculated breakthrough curves was probably caused by ignoring the kinetic reaction in the model calculations.
机译:农业土地下的地下水经常被硝酸盐污染。在日本南部,含水层被火山灰土壤覆盖,可以将硝酸盐渗入地下水。在这项研究中,进行了使用两种火山灰土壤(Kuroboku和Akahoya)的柱试验。 KNO_3和K_2SO_4的混合溶液用于浸出实验。在实验的基础上,使用约束插值曲线方法开发了一种用于离子迁移的反应性迁移模型,并用于计算阳离子交换反应的化学平衡。通过在数值模型中的延迟来模拟阴离子吸附。将开发的仿真模型结果与通过反应输运模型PHAST获得的结果进行比较。所开发的模型显示出很好的再现了实验结果的一般特征。而且,开发的模型结果与PHAST的结果非常吻合。观察到的和计算出的突破曲线之间的细微差异可能是由于忽略了模型计算中的动力学反应。

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