Numerical solution of Richards' equation of water flow by generalized finite differences

被引:30
|
作者
Chavez-Negrete, C. [2 ]
Dominguez-Mota, F. J. [1 ]
Santana-Quinteros, D. [1 ]
机构
[1] Univ Michoacana, Fac Ciencias Fis Matemat, Morelia, Michoacan, Mexico
[2] Univ Michoacana, Fac Ingn Civil, Morelia, Michoacan, Mexico
关键词
Richards equation; Linearization schemes; Generalized finite differences; Iterative methods; Flow in porous media; POROUS-MEDIA; HYDRAULIC CONDUCTIVITY; CONSTITUTIVE MODEL; UNSATURATED FLOW; SUCTION; SOILS;
D O I
10.1016/j.compgeo.2018.05.003
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
Richards equation is a degenerate elliptic parabolic nonlinear expression which models flow in unsaturated porous media. Due to its importance in engineering, a number of linearization schemes for approximating its solution have been proposed. Among the more efficient are combinations of Newtonian iterations for the spatial discretization using finite elements, and an implicit 0-method for the time integration. However, when the finite element formulation is used, numerical oscillations near the infiltration front are presented. To overcome this problem, this paper presents a novel generalized finite differences scheme and an adaptive step size Crank-Nicolson method, which can be applied for solving Richards' equation on nonrectangular structured grids. The proposed method is tested on an illustrative numerical example on a road embankment and the results are compared with a finite element method solution.
引用
收藏
页码:168 / 175
页数:8
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