首页 | 本学科首页   官方微博 | 高级检索  
     


An adaptive time discretization of the classical and the dual porosity model of Richards’ equation
Authors:Michal Kurá  ?,Petr Mayer,Dagmar Trpko&scaron  ová  
Affiliation:a Czech University of Life Sciences Prague, Faculty of Environmental Sciences, Department of Water Resources and Environmental Modeling, Czech Republic
b Czech Technical University in Prague, Faculty of Civil Engineering, Department of Mathematics, Czech Republic
c Czech Technical University in Prague, Faculty of Civil Engineering, Department of Mechanics, Czech Republic
d Charles University in Prague, Faculty of Science, Institute of Hydrogeology, Engineering Geology and Applied Geophysics, Czech Republic
Abstract:This paper presents a numerical solution to the equations describing Darcian flow in a variably saturated porous medium—a classical Richards’ equation model Richards (1931) [1] and an extension of it that approximates the flow in media with preferential paths—a dual porosity model Gerke and van Genuchten (1993) [8]. A numerical solver to this problem, the DRUtES computer program, was developed and released during our investigation. A new technique which maintains an adaptive time step, defined here as the Retention Curve Zone Approach, was constructed and tested. The aim was to limit the error of a linear approximation to the time derivative part. Finally, parameter identification was performed in order to compare the behavior of the dual porosity model with data obtained from a non-homogenized fracture and matrix flow simulation experiment.
Keywords:Darcy&rsquo  s law   Variable saturation   Retention curve   Mass balance   Adaptive time discretization   Preferential flow   Homogenization   Parameter identification   Multi-objective evolutionary algorithm
本文献已被 ScienceDirect 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号