Comparación de tres métodos de infiltración utilizados para el cálculo del balance hídrico del suelo, en la Cuenca del río Suquiapa, El Salvador

Autor: Alvarado Batres, Cesar, Barahona-Palomo, Marco

Publikováno v: UNED Research Journal; Vol. 9 No. 1 (2017); 23-33
UNED Research Journal; Vol. 9 Núm. 1 (2017); 23-33
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Water infiltration in the soil has a fundamental role in the hydrological cycle. Depending on geological conditions, it can remain in the soil as moisture, drain as subsurface flow and emerge as an ephemeral; or recharge the aquifer, among others. We

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______3056::f23027020faaf3b0fff6b615d88d0a0d
https://revistas.uned.ac.cr/index.php/cuadernos/article/view/1674