Extension of the Dupuit–Forchheimer Model for Non-Hydrostatic Flows in Unconfined Aquifers
The classical Dupuit–Forchheimer approach, commonly used in analysing unconfined groundwater-flow systems, relies on the assumption of a negligible vertical component of the flow. This approximation is valid only when the convergence of streamlines is very limited and the drawdown of the p...
| Main Author: | |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
MDPI AG
2018-06-01
|
| Series: | Fluids |
| Subjects: | |
| Online Access: | http://www.mdpi.com/2311-5521/3/2/42 |