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使用数值算法和随机算法的耦合方案模拟多孔介质中铵和铬的传输。

Simulation of ammonium and chromium transport in porous media using coupling scheme of a numerical algorithm and a stochastic algorithm.

作者信息

Palanichamy Jegathambal, Schüttrumpf Holger, Köngeter Jürgen, Becker Torsten, Palani Sundarambal

机构信息

Institute of Hydraulic Engineering and Water Resources Management, RWTH Aachen University, Aachen 52056, Germany.

出版信息

Water Sci Technol. 2009;59(8):1577-84. doi: 10.2166/wst.2009.159.

Abstract

The migration of the species of chromium and ammonium in groundwater and their effective remediation depend on the various hydro-geological characteristics of the system. The computational modeling of the reactive transport problems is one of the most preferred tools for field engineers in groundwater studies to make decision in pollution abatement. The analytical models are less modular in nature with low computational demand where the modification is difficult during the formulation of different reactive systems. Numerical models provide more detailed information with high computational demand. Coupling of linear partial differential Equations (PDE) for the transport step with a non-linear system of ordinary differential equations (ODE) for the reactive step is the usual mode of solving a kinetically controlled reactive transport equation. This assumption is not appropriate for a system with low concentration of species such as chromium. Such reaction systems can be simulated using a stochastic algorithm. In this paper, a finite difference scheme coupled with a stochastic algorithm for the simulation of the transport of ammonium and chromium in subsurface media has been detailed.

摘要

铬和铵在地下水中的迁移及其有效修复取决于系统的各种水文地质特征。反应输运问题的计算建模是地下水研究领域工程师在污染治理决策中最常用的工具之一。解析模型本质上模块化程度较低,计算需求也较低,在构建不同反应系统时难以修改。数值模型能提供更详细的信息,但计算需求较高。将传输步骤的线性偏微分方程(PDE)与反应步骤的非线性常微分方程组(ODE)耦合是求解动力学控制反应输运方程的常用方式。这种假设不适用于铬等低浓度物质的系统。此类反应系统可使用随机算法进行模拟。本文详细介绍了一种结合随机算法的有限差分格式,用于模拟铵和铬在地下介质中的传输。

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