Water table fluctuations due to canal seepage and time varying recharge

Transient water table variation in an unconfined horizontal aquifer, lying between two canals located at different elevations above the impermeable barrier and receiving time varying recharge, is predicted by obtaining an analytical solution to the linearized Boussinesq equation. The proposed soluti...

Ausführliche Beschreibung

Bibliographische Detailangaben

Veröffentlicht in:	Journal of hydrology (Amsterdam) 2001-04, Vol.244 (1), p.1-8
Hauptverfasser:	Upadhyaya, A, Chauhan, H.S
Format:	Artikel
Sprache:	eng
Schlagworte:	Boussinesq equation Canal seepage Earth sciences Earth, ocean, space Exact sciences and technology Hydrogeology Hydrology. Hydrogeology Recharge Unconfined aquifer Water table
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!