Unconfined Flow through Porous Media Using B-Spline Boundary Elements
The boundary element method (BEM) is now established as a suitable and efficient technique for the analysis of ground-water flow problems. However, as in other discretization procedures, inaccuracies can be introduced as a result of the lack of derivative continuity between adjacent elements. Contin...
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Veröffentlicht in: | Journal of hydraulic engineering (New York, N.Y.) N.Y.), 1991-11, Vol.117 (11), p.1479-1494 |
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container_title | Journal of hydraulic engineering (New York, N.Y.) |
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creator | Cabral, Jaime J. S. P Wrobel, Luiz C |
description | The boundary element method (BEM) is now established as a suitable and efficient technique for the analysis of ground-water flow problems. However, as in other discretization procedures, inaccuracies can be introduced as a result of the lack of derivative continuity between adjacent elements. Continuity of the derivatives of the main variable is important to obtain a good representation of moving boundaries with iterative or time-marching schemes. A recently developed BEM formulation, using cubic B-splines, provides as much as C2 continuity between adjacent elements. This formulation is applied in herein to steady-state and transient unconfined flow in homogeneous and nonhomogeneous media. |
doi_str_mv | 10.1061/(ASCE)0733-9429(1991)117:11(1479) |
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source | American Society of Civil Engineers:NESLI2:Journals:2014 |
subjects | Boundaries Boundary element method Formulations Iterative methods TECHNICAL PAPERS |
title | Unconfined Flow through Porous Media Using B-Spline Boundary Elements |
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