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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Bibliografiske detaljer
Udgivet i:Proc Math Phys Eng Sci
Main Authors: Cooper, L. J., Daly, K. R., Hallett, P. D., Naveed, M., Koebernick, N., Bengough, A. G., George, T. S., Roose, T.
Format: Artigo
Sprog:Inglês
Udgivet: The Royal Society Publishing 2017
Fag:
Research Articles
Online adgang:https://ncbi.nlm.nih.gov/pmc/articles/PMC5719621/
https://ncbi.nlm.nih.gov/pubmed/29225490
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rspa.2017.0178
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