Abstract
Introduced by Richards [1], the Richards’ equation is used to mathematically describe water movement in the unsaturated zone. Theoretically, the equation is also a sort of simplification of the two-phase flow equations of water-air processes in porous media under the constant gas pressure condition.
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Kalbacher, T., Chen, X., Dai, Y., Hesser, J., Wang, X., Wang, W. (2015). Richards Flow. In: Kolditz, O., Shao, H., Wang, W., Bauer, S. (eds) Thermo-Hydro-Mechanical-Chemical Processes in Fractured Porous Media: Modelling and Benchmarking. Terrestrial Environmental Sciences. Springer, Cham. https://doi.org/10.1007/978-3-319-11894-9_4
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DOI: https://doi.org/10.1007/978-3-319-11894-9_4
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