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https://doi.org/10.1016/j.compgeo.2013.06.004
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Cite Journal: Computers and Geotechnics |  Publication Date: Jul 16, 2013 |
 Citations: 7 |
Affiliation: Soochow University, Yangtze Normal University
Abstract A generalized Boltzmann transform is introduced to convert the Richards’ equation into an ordinary differential equation, and an approximate solution for the moving wetted front of water transport in unsaturated soils is obtained. The developed theory is also valid for water transport in porous fabrics.
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