Finite difference solution of the agricultural drainage Boussinesq equation with variable drainable porosity subject to a fractal radiation boundary condition.

Subsurface drainage systems are used to control the depth of the water table and to reduce or prevent soil salinity. Generally, the flow of the groundwater is studied with the Bousssinesq equation, whose analytical solutions are obtained assuming that aquifer transmissivity and drainable porosity ar...

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Bibliographic Details
Main Authors: Carlos Chávez, Carlos Fuentes, Manuel Zavala
Format: Article
Language:Spanish
Published: Instituto Mexicano de Tecnología del Agua 2010-11-01
Series:Tecnología y ciencias del agua
Subjects:
Online Access:http://www.revistatyca.org.mx/ojs/index.php/tyca/article/view/74