Fluid flow in porous media using image-based modelling to parametrize Richards' equation

The parameters in Richards' equation are usually calculated from experimentally measured values of the soil–water characteristic curve and saturated hydraulic conductivity. The complex pore structures that often occur in porous media complicate such parametrization due to hysteresis between wet...

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Detalles Bibliográficos
Autores principales: Cooper, L. J., Daly, K. R., Hallett, P. D., Naveed, M., Koebernick, N., Bengough, A. G., George, T. S., Roose, T.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: The Royal Society Publishing 2017
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5719621/
https://www.ncbi.nlm.nih.gov/pubmed/29225490
http://dx.doi.org/10.1098/rspa.2017.0178

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5719621/
https://www.ncbi.nlm.nih.gov/pubmed/29225490
http://dx.doi.org/10.1098/rspa.2017.0178

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