首页> 外文会议>International Groundwater Symposium 2002; Mar 25-28, 2002; Berkeley, California >3-D Groundwater Flow Modeling For the Oak RidgeReservation (ORR): Finite-Volume Method on AnUnstructured Grid System
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3-D Groundwater Flow Modeling For the Oak RidgeReservation (ORR): Finite-Volume Method on AnUnstructured Grid System

机译:橡树岭保护区(ORR)的3D地下水流建模:非结构网格系统上的有限体积方法

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In the design of in-situ bioremediation schemes, the flow near injection andrnextraction wells and recirculation units must be well understood. We describe arncomputationally efficient 3-dimensional finite-volume model for groundwater flow in arnheterogeneous layered anisotropic porous medium with dipping beds. This algorithm isrndeveloped applying the cell-centered finite volume method on an unstructured triangularrngrid system with fully implicit time discretization. According to the real hydrogeologicrnconditions of the Oak Ridge Reservation (ORR), we focus on aquifer layers with a 450rndip. The hydraulic conductivity is isotropic on a plane parallel to the layers, while thernthird principal axis, the one with the lowest value, is normal to the layers. The domain isrndiscretized into parallel dipping layers and each layer is discretized into triangles, thernsame at every level. The triangles are chosen using Delaunay triangulation techniques.rnThe use of triangles and adaptive technique makes this scheme more flexible and able tornaccurately represent a domain with wells and other geometric complexities. In thisrnscheme the total flux crossing each interface between neighboring control volume isrnapproximated by a one-point integration rule based on the specific discharge at thernmidpoint. At wells, realistic boundary conditions are used. Hydraulic conductivities arernderived from well tests using inverse methods. We show the flow regime near wells.
机译:在原位生物修复方案的设计中,必须充分了解注入井和萃取井以及再循环单元附近的流量。我们描述了非均质层状各向异性各向异性多孔介质中地下水流动的反算有效三维有限体积模型。该算法是基于单元为中心的有限体积方法在具有完全隐式时间离散化的非结构三角网格系统上开发的。根据橡树岭保留区(ORR)的实际水文地质条件,我们集中研究450ndip的含水层。在平行于各层的平面上,水力传导率是各向同性的,而第三主轴(最小值)是垂直于各层的。磁畴被离散为平行的浸入层,每一层被离散为三角形,每一层都相同。使用Delaunay三角剖分技术选择三角形。使用三角形和自适应技术使该方案更加灵活,能够准确地表示具有井和其他几何复杂性的区域。在该方案中,基于中点处的特定放电,通过单点积分法则可以近似通过相邻控制体积之间的每个界面的总通量。在井中,使用实际边界条件。使用反演方法从试井中得出水力传导率。我们显示了井附近的流动状态。

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