Chang C M, Wang M K, Chang T W, Lin C, Chen Y R
Department of Agricultural Chemistry, National Taiwan University, Taipei, ROC.
Chemosphere. 2001 Jun;43(8):1133-9. doi: 10.1016/s0045-6535(00)00176-4.
The predictive accuracy of using the one-dimensional advection-dispersion equation to evaluate the fate and transport of solute in a soil column is usually dependent on the proper determination of chemical retardation factors. Typically, the distribution coefficient (Kd) obtained by fitting the linear sorption isotherm has been extensively used to consider general geochemical reactions on solute transport in a low-concentration range. However, the linear distribution coefficient cannot be adequately utilized to describe the solute fate at a higher concentration level. This study employed the nonlinear equilibrium-controlled sorption parameters to determine the retardation factor used in column leaching experiments. Copper and cadmium transportation in a lateritic silty-clay soil column was examined. Through the explicit finite-difference calculations with a third-order total-variation-diminishing (TVD) numerical solution scheme, all results of the theoretical copper and cadmium breakthrough curves (BTCs) simulated by using the Freundlich nonlinear retardation factors revealed good agreement with the experimental observations.
使用一维对流弥散方程来评估溶质在土柱中的迁移转化时,其预测准确性通常取决于对化学阻滞因子的恰当确定。通常,通过拟合线性吸附等温线得到的分配系数(Kd)已被广泛用于考虑低浓度范围内溶质运移过程中的一般地球化学反应。然而,线性分配系数不足以用于描述较高浓度水平下溶质的迁移转化情况。本研究采用非线性平衡控制吸附参数来确定柱淋溶实验中使用的阻滞因子。研究了红土粉质黏土柱中铜和镉的迁移情况。通过采用三阶总变差递减(TVD)数值求解方案进行显式有限差分计算,利用弗伦德利希非线性阻滞因子模拟得到的理论铜和镉突破曲线(BTCs)的所有结果与实验观测结果吻合良好。