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Richards Flow

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Part of the book series: Terrestrial Environmental Sciences ((TERENVSC))

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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References

  1. L.A. Richards. Capillary conduction of liquids through porous mediums. Physics A-J Gen. Appl. Phys., 1(1):318–333, 1931.

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  2. M.T. VanGenuchten and P.J. Wierenga. Mass-transfer studies in sorbing porous-media. 1. Analytical solutions. Soil Sci. Soc. Am. J., 40(4):473–480, 1976.

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  5. W.V. Abeele M.L. Wheeler and B.W. Burton. Geohydrology of bandelier tuff. Los Alamos National Laboratory report, LA-8962-MS, 1981.

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  6. H. S. Carslaw and J. C. Jaeger. Conduction of heat in solids. Oxford University Press, London, 2nd edition, 1959.

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Correspondence to Thomas Kalbacher .

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© 2015 Springer International Publishing Switzerland

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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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