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2015 | OriginalPaper | Chapter

4. Richards Flow

Authors : Thomas Kalbacher, Xi Chen, Ying Dai, Jürgen Hesser, Xuerui Wang, Wenqing Wang

Published in: Thermo-Hydro-Mechanical-Chemical Processes in Fractured Porous Media: Modelling and Benchmarking

Publisher: Springer International Publishing

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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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Literature
1.
go back to reference L.A. Richards. Capillary conduction of liquids through porous mediums. Physics A-J Gen. Appl. Phys., 1(1):318–333, 1931. L.A. Richards. Capillary conduction of liquids through porous mediums. Physics A-J Gen. Appl. Phys., 1(1):318–333, 1931.
2.
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3.
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go back to reference J.K. Zhou. Differential transformation and its applications for electrical circuits. Huazhong University Press, 1986. J.K. Zhou. Differential transformation and its applications for electrical circuits. Huazhong University Press, 1986.
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go back to reference W.V. Abeele M.L. Wheeler and B.W. Burton. Geohydrology of bandelier tuff. Los Alamos National Laboratory report, LA-8962-MS, 1981. 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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go back to reference H. S. Carslaw and J. C. Jaeger. Conduction of heat in solids. Oxford University Press, London, 2nd edition, 1959. H. S. Carslaw and J. C. Jaeger. Conduction of heat in solids. Oxford University Press, London, 2nd edition, 1959.
Metadata
Title
Richards Flow
Authors
Thomas Kalbacher
Xi Chen
Ying Dai
Jürgen Hesser
Xuerui Wang
Wenqing Wang
Copyright Year
2015
DOI
https://doi.org/10.1007/978-3-319-11894-9_4