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

机译:应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迁移

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The migration of the species of chromium and ammonium in groundwater and their effectivenremediation depend on the various hydro-geological characteristics of the system. Thencomputational modeling of the reactive transport problems is one of the most preferred tools fornfield engineers in groundwater studies to make decision in pollution abatement. The analyticalnmodels are less modular in nature with low computational demand where the modification isndifficult during the formulation of different reactive systems. Numerical models provide morendetailed information with high computational demand. Coupling of linear partial differentialnEquations (PDE) for the transport step with a non-linear system of ordinary differential equationsn(ODE) for the reactive step is the usual mode of solving a kinetically controlled reactive transportnequation. This assumption is not appropriate for a system with low concentration of species suchnas chromium. Such reaction systems can be simulated using a stochastic algorithm. In this paper,na finite difference scheme coupled with a stochastic algorithm for the simulation of the transportnof ammonium and chromium in subsurface media has been detailed.
机译:铬和铵离子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。然后,反应性运输问题的计算模型是地下水研究中非现场工程师在减少污染方面做出决策的最优选工具之一。解析模型本质上模块化程度较低,计算需求低,在此过程中,在制定不同的反应性系统时修改并不困难。数值模型提供了更多的详细信息,并具有很高的计算需求。输运步骤的线性偏微分方程(PDE)与反应步骤的非线性微分方程n(ODE)非线性系统的耦合是解决动力学控制的反应输运方程的常用模式。这种假设不适用于铬等物种浓度低的系统。可以使用随机算法来模拟这样的反应系统。本文详细介绍了一种有限差分格式,结合随机算法,用于模拟地下介质中铵和铬的迁移。

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