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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...

詳細記述

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書誌詳細
出版年:Proc Math Phys Eng Sci
主要な著者: Cooper, L. J., Daly, K. R., Hallett, P. D., Naveed, M., Koebernick, N., Bengough, A. G., George, T. S., Roose, T.
フォーマット: Artigo
言語:Inglês
出版事項: The Royal Society Publishing 2017
主題:
オンライン・アクセス: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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