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- Dupuit–Forchheimer_assumption abstract "The Dupuit–Forchheimer assumption holds that groundwater flows horizontally in an unconfined aquifer, and that the groundwater discharge is proportional to the saturated aquifer thickness. It was formulated by Jules Dupuit and Philipp Forchheimer in the late 1800s to simplify groundwater flow equations for analytical solutions.The Dupuit–Forchheimer approximation requires that the water table is relatively flat, and that the groundwater is hydrostatic (i.e., the equipotential lines are vertical):where is the vertical pressure gradient, is the specific weight, is the density of water, is the standard gravity, and is the vertical hydraulic gradient.".
- Dupuit–Forchheimer_assumption wikiPageID "8568920".
- Dupuit–Forchheimer_assumption wikiPageRevisionID "598720599".
- Dupuit–Forchheimer_assumption subject Category:Aquifers.
- Dupuit–Forchheimer_assumption subject Category:Hydraulic_engineering.
- Dupuit–Forchheimer_assumption subject Category:Hydrology.
- Dupuit–Forchheimer_assumption comment "The Dupuit–Forchheimer assumption holds that groundwater flows horizontally in an unconfined aquifer, and that the groundwater discharge is proportional to the saturated aquifer thickness.".
- Dupuit–Forchheimer_assumption label "Dupuit–Forchheimer assumption".
- Dupuit–Forchheimer_assumption sameAs Dupuit%E2%80%93Forchheimer_assumption.
- Dupuit–Forchheimer_assumption sameAs Q5316065.
- Dupuit–Forchheimer_assumption sameAs Q5316065.
- Dupuit–Forchheimer_assumption wasDerivedFrom Dupuit–Forchheimer_assumption?oldid=598720599.