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首页> 外文期刊>Mathematical geology >Three-Dimensional Numerical Method of Moments for Linear Equilibrium-Adsorbing Solute Transport in Physically and Chemically Nonstationary Formations
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Three-Dimensional Numerical Method of Moments for Linear Equilibrium-Adsorbing Solute Transport in Physically and Chemically Nonstationary Formations

机译:物理和化学非平稳地层中线性平衡吸附溶质运移的矩量的三维数值方法

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摘要

A Lagrangian perturbation method is applied to develop a method of moments for reactive solute flux through a three-dimensional, nonstationary flow field. The flow nonstationarity may stem from medium nonstationarity, finite domain boundaries, and/or fluid pumping and injecting. The reactive solute flux is described as a space–time process where time refers to the solute flux breakthrough in a control plane at some distance downstream of the solute source and space refers to the transverse displacement distribution at the control plane. The analytically derived moments equations for solute transport in a nonstationary flow field are too complicated to solve analytically; therefore, a numerical finite difference method is implemented to obtain the solutions. This approach combines the stochastic model with the flexibility of the numerical method to boundary and initial conditions. The approach provides a tool to apply stochastic theory to reactive solute transport in complex subsurface environments. Several case studies have been conducted to investigate the influence of the physical and chemical heterogeneity of a medium on the reactive solute flux prediction in nonstationary flow field. It is found that both physical and chemical heterogeneity significantly affect solute transport behavior in a nonstationary flow field. The developed method is also applied to an environmental project for predicting solute flux in the saturated zone below the Yucca Mountain Project area, demonstrating the applicability of the method in practical environmental projects.
机译:拉格朗日摄动法被用于发展通过三维非平稳流场的反应性溶质通量的矩方法。流动非平稳性可能源于介质的非平稳性,有限域边界和/或流体泵送和注入。反应性溶质通量被描述为一个时空过程,其中时间是指溶质源下游一定距离处控制平面中的溶质通量突破,空间是指控制平面上的横向位移分布。非稳态流场中溶质运移的解析导出的矩方程太复杂而无法解析。因此,采用数值有限差分法获得解。这种方法将随机模型与数值方法的灵活性相结合,以处理边界条件和初始条件。该方法提供了将随机理论应用于复杂地下环境中反应性溶质运移的工具。已经进行了几个案例研究,以研究介质的物理和化学非均质性对非平稳流场中反应性溶质通量预测的影响。发现物理和化学异质性都显着影响非平稳流场中的溶质传输行为。所开发的方法还应用于环境项目中,以预测尤卡山项目区以下饱和带中的溶质通量,证明了该方法在实际环境项目中的适用性。

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