A phase field model of unsaturated flow
We present a phase field model of infiltration that explains the formation of gravity fingers during water infiltration in soil. The model is an extension of the traditional Richards equation, and it introduces a new term, a fourth-order derivative in space, but not a new parameter. We propose a sca...
| Autors principals: | , |
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| Altres autors: | |
| Format: | Article |
| Idioma: | en_US |
| Publicat: |
American Geophysical Union
2010
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| Accés en línia: | http://hdl.handle.net/1721.1/59996 https://orcid.org/0000-0002-7370-2332 https://orcid.org/0000-0003-3958-7382 |