基于Freundlich等温吸附参数的土壤-骨架和土壤-水重金属污染有限元模拟

Nguyen Van Hoang
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引用次数: 0

摘要

国际上的研究结果表明,未经处理的渗滤液中重金属含量较高,容易污染土壤和地下水环境,导致土壤和地下水中重金属含量增加。Freundlich等温吸附参数是土壤输入参数中必不可少的参数,用于模拟溶质进入土壤骨架和土壤孔隙水污染的运移。利用Freundlich等温线吸附参数在模型域内随空间和时间连续变化,对溶质在土壤骨架和孔隙水中的平流-弥散输运进行有限元模拟,可以准确地评估溶质在土壤骨架和孔隙水中的浓度。本章主要介绍了现有等温吸附理论的背景、Freundlich等温吸附在土壤骨架和土壤孔隙水污染中的适用性、Freundlich等温吸附参数的确定方法、一般用GW运动模拟HMs平流-弥散输移的有限元过程以及Freundlich等温吸附参数。实例研究模型已被证明。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Soil-Skeleton and Soil-Water Heavy Metal Contamination by Finite Element Modelling With Freundlich Isotherm Adsorption Parameters
World research results indicate that untreated leachate contains high contents of heavy metals (HM) that are likely to pollute the soil and groundwater (GW) environment and contribute to the increase of HMs in soil and GW. The Freundlich isotherm adsorption parameters are essential to soil input parameters for modelling of HMs’ transport to access the soil skeleton and soil pore water contamination by HMs. Finite element (FE) modelling of advection-dispersion transport of HMs by GW movement along with Freundlich isotherm adsorption parameters which continuously change with space in the model domain and with time is sophisticated to accurately evaluate the HMs’ concentrations in soil skeleton and pore water. The chapter describes the background of the existing isotherm adsorption theory, the adaptation of the Freundlich isotherm adsorption in the soil skeleton and soil pore water contamination by HMs, method of determination of the Freundlich isotherm adsorption parameters, the FE procedure of modelling of advection-dispersion transport of HMs by GW movement in general and along with Freundlich isotherm adsorption parameters in particular. A case study modelling has been demonstrated.
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