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Numerical Methods for Nonequilibrium Solute Transport with First-Order Decay and Zero-Order Production

机译:一阶衰变零阶非平衡溶质运移的数值方法

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Solute transport in the subsurface is often considered to be a nonequilibrium process. Nonequilibrium during transport of solutes in porous medium has been categorized as either transportrelated or sorption-related. For steady state flow in a homogeneous soil and assuming a linear sorption process, we will consider advection-diffusionadsorption equations. In this paper, numerical methods are considered for the mathematical model for steady state flow in a homogeneous soil with a linear sorption process. The modified upwind finite difference method is adopted to approximate the concentration in mobile regions and immobile regions. Optimal order l2-error estimate is derived. Numerical results are supplied to justify the theoretical work.
机译:地下的溶质运移通常被认为是一个非平衡过程。溶质在多孔介质中运输过程中的非平衡被分类为与运输有关或与吸附有关。对于均质土壤中的稳态流动并假设线性吸附过程,我们将考虑对流-扩散-吸附方程。本文考虑了采用线性吸附过程的均质土中稳态流数学模型的数值方法。采用改进的迎风有限差分法来近似移动区域和非移动区域的浓度。得出最佳阶l2-误差估计。提供数值结果证明理论工作是正确的。

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