Locally conservative, stabilized finite element methods for variably saturated flow

被引:47
作者
Kees, C. E. [1 ]
Farthing, M. W. [1 ]
Dawson, C. N. [2 ]
机构
[1] USA, Coastal & Hydraul Lab, Engineer Res & Dev Ctr, Vicksburg, MS 39180 USA
[2] Univ Texas Austin, Ctr Subsurface Modeling, Inst Computat Engn & Sci, Austin, TX 78712 USA
基金
美国国家科学基金会;
关键词
Richards' equation; Finite element method; Multiscale stabilization; Local conservation;
D O I
10.1016/j.cma.2008.06.005
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Standard Galerkin finite element methods for variably saturated groundwater flow have several deficiencies. For instance, local oscillations can appear around sharp infiltration fronts without the use of mass-lumping, and velocity fields obtained from differentiation of pressure fields are discontinuous at element boundaries. Here, we consider conforming finite element discretizations based on a multiscale formulation along with recently developed, local postprocessing schemes. The resulting approach maintains the basic flexibility and appeal of traditional finite element methods, while controlling nonphysical oscillations and producing element-wise mass-conservative velocity fields. Accuracy and efficiency of the proposed schemes are evaluated through a series of steady-state and transient variably saturated groundwater flow problems in homogeneous as well as heterogeneous domains. The schemes are formulated for a generic nonlinear advection-diffusion equation and are thus applicable to many other flow models. (c) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:4610 / 4625
页数:16
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