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Numerical Modeling of Aquifer Radial Movement Caused by Groundwater Pumping

机译:地下水泵送引起的含水层径向运动的数值模拟

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The present investigation is to model aquifer radial movement toward a fully penetrating discharge well within a confined and non-leaky aquifer system. The governing equation for aquifer radial movement applied in the present paper reduces from a general governing equation for the three-dimensional land movement established by Li and Helm (2010). Numerical simulation is carried out with emphasis on radial movement using MATLAB. The numerical solution in terms of velocity and displacement fields are found based on a conceptual model that is incorporated with three different boundary conditions. In the present paper, aquifer's specific storage coefficient is not a constant but a variable that can be either a stress dependent or hydraulic head dependent so thatan exponential relation between the volume stress and strain is applied. Aquifer's velocity and displacement versus radial distance have been analyzed and discussed thoroughly for three different boundary conditions. The numerical solution of the linear model is noticed to be consistent with the analytic solution previously found by Li (2011). The results of the numerical modeling of the radial movement for a nonlinear aquifer system are similar to that of the vertical movement done by Li and Ding (2014).
机译:目前的研究是对在密闭且无泄漏的含水层系统内朝着完全穿透的排水井的含水层径向运动进行建模。 Li和Helm(2010)建立的三维陆地运动通用控制方程式简化了本文中所采用的含水层径向运动控制方程式。使用MATLAB进行数值模拟,重点是径向运动。基于概念模型找到了关于速度场和位移场的数值解,该概念模型结合了三种不同的边界条件。在本文中,含水层的比存储系数不是一个常数,而是一个可以随应力而定或与水头有关的变量,因此可以应用体积应力与应变之间的指数关系。对于三种不同的边界条件,已经对含水层的速度和位移与径向距离的关系进行了分析和讨论。注意到线性模型的数值解与先前由Li(2011)发现的解析解是一致的。非线性含水层系统径向运动数值模拟的结果与Li和Ding(2014)进行的垂直运动的数值模拟的结果相似。

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