Quasi‐steady flow in sloping aquifers

Author:

Akylas Evangelos1,Gravanis Elias1,Koussis Antonis D.23

Affiliation:

1. Department of Civil Engineering and GeomaticsCyprus University of TechnologyLimassol Cyprus

2. Institute for Environmental Research and Sustainable Development, National Observatory of AthensAthens Greece

3. Navarino Environmental ObservatoryMessinia Greece

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Reference34 articles.

1. Analytical solution of transient flow in a sloping soil layer with recharge

2. Ambroise B.(1988) Interactions eaux souterraines‐eaux de surface dans le bassin du Ringelbach a Soultzeren (hautes Vosges France): Role hydrologique des surfaces saturres (English abstract) inProceedings of Ystad Symposium on Interaction Between Groundwater and Surface Water edited by P. Dahlblom and G. Lindh pp.231–238 Dep. of Water Resour. Eng. Lurid Univ. Lund Sweden.

3. The structure of discharge-recession curves

4. Theoretical and conceptual models of subsurface hillslope flows

5. Essai sur la théorie des eaux courantes;Boussinesq J.;Mém. Acad. Sci. Inst. Fr.,1877

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