Exact closed-form solution of the two-dimensional Laplace Equation for Steady Groundwater flow with nonlinearized free-surface boundary condition
Steady groundwater flow with steep gradients of the phreatic surface can be described by the Laplace equation. Without employing either the Dupuit assumption nor any other linearization of the nonlinear free‐surface boundary condition, we develop for an aquifer of infinite horizontal extension the e...
Gespeichert in:
| Veröffentlicht in: | Water resources research 2000-07, Vol.36 (7), p.1975-1980 |
|---|---|
| Hauptverfasser: | , |
| Format: | Artikel |
| Sprache: | eng |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
Schreiben Sie den ersten Kommentar!