On the proceeding of a saturation front under ponded conditions
The vertical infiltration of water is a variable saturated flow process until the soil under an inundated area is completely saturated. However, in several modelling studies that regard the river-aquifer interactions, the vertical infiltration under ponded conditions is modelled as a saturated soil...
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Autores principales: | , , , , |
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Lenguaje: | English |
Publicado: |
Universidad Católica de la Santísima Concepción
2013
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Acceso en línea: | http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-28132013000100003 |
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