Forms of hydrothermal and hydraulic flow in a homogeneous unconfined aquifer

Groundwater flow in an unconfined aquifer (a porous layer with an open top) can be driven either by hydraulic forces, i.e. the gradient of the water table, or by differences in the density of porewater due to thermal expansion and changes in salinity. In this study we assume that the salinity is con...

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Veröffentlicht in:	Geophysical journal international 2004-08, Vol.158 (2), p.785-797
Hauptverfasser:	Cserepes, László, Lenkey, László
Format:	Artikel
Sprache:	eng
Schlagworte:	anisotropy convection groundwater flow hydrology
Online-Zugang:	Volltext
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