[Modelling of capillary hysteresis phenomena at unsaturated porous area by "Theorie des domaines"]

Lakhal, E.K.; Firdaouss, M.

[Modelling of capillary hysteresis phenomena at unsaturated porous area by "Theorie des domaines"]

1992

Lakhal, E.K. | Firdaouss, M. (Faculte des Sciences Semlalia, Marrakech (Maroc))

French. Lors d'un ecoulement diphasique en zone non saturee, la relation d'equilibre succin capillaire-teneur en eau est fortement affectee par l'hysteresis. Il se manifeste lors de la transition d'une phase de drainage a une phase d'imbibition et inversement. Il fait intervenir la non linearite dans l'equation d'infiltration transitoire.

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AGROVOC Keywords

drainage drenaje infiltration movimiento del agua en el suelo soil soil water movement suelo

Bibliographic information

Published in

Revue de la Faculte des Sciences Marrakech-Semlalia (Maroc)

Volume 272

Other Subjects

Infiltracion

Language

French

Note

4 figs. 7 ref. Resume (Fr)

Type

Conference; Summary

Conference

Hydrogeologie des Milieux Discontinus sous Climats Arides, Marrakech (Maroc), 22-25 Avr 1992

In AGRIS since: 1993-08-15

Format: AGRIS AP

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[Modelling of capillary hysteresis phenomena at unsaturated porous area by "Theorie des domaines"]

1992

AGROVOC Keywords

Bibliographic information