Analytical approximation to the solutions of Richards' equation with applications to infiltration, ponding, and time compression approximation
Identifieur interne : 00C460 ( Main/Curation ); précédent : 00C459; suivant : 00C461Analytical approximation to the solutions of Richards' equation with applications to infiltration, ponding, and time compression approximation
Auteurs : J.-Y. Parlange [États-Unis] ; W. L. Hogarth [Australie] ; D. A. Barry [Australie] ; M. B. Parlange [États-Unis] ; R. Haverkamp [France] ; P. J. Ross [Australie] ; T. S. Steenhuis [États-Unis] ; D. A. Dicarlo [États-Unis] ; G. Katul [États-Unis]Source :
- Advances in Water Resources [ 0309-1708 ] ; 1999.
Descripteurs français
- Pascal (Inist)
- Wicri :
- topic : Ressource en eau.
English descriptors
- KwdEn :
- Ampt model, Approximate ponding time, Average rainfall rate, Delta function, Elsevier science, Environmental engineering, Exact solution, Initial value, Linear soil, Moisture content, Other techniques, Parlange, Particular case, Particular value, Ponding, Ponding time, Porous media, Present method, Rainfall rate, Richards equation, Second term, Small amount, Surface water content, Time compression approximation, Water content, Water resour, Water resources, Western australia, climate modification, compression, hydraulic conductivity, infiltration, soil moisture, soils, solution, water resources.
- Teeft :
- Ampt model, Approximate ponding time, Average rainfall rate, Delta function, Elsevier science, Environmental engineering, Exact solution, Initial value, Linear soil, Moisture content, Other techniques, Parlange, Particular case, Particular value, Ponding, Ponding time, Porous media, Present method, Rainfall rate, Second term, Small amount, Surface water content, Time compression approximation, Water content, Water resour, Water resources, Western australia.
Abstract
Abstract: A recent approach to solve Richards' equation is further improved. This approach brings understanding into the physical processes of infiltration and ponding. In particular we apply it to analyze the standard hydrologic tool of Time Compression Approximation (TCA). We also suggest that the new approach provides a more reliable alternative to TCA, e.g. for predicting ponding time.
Url:
DOI: 10.1016/S0309-1708(99)00022-6
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ISTEX:4580DFD65D1DBE09ADAD84A5398812FD6E43244DLe document en format XML
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<front><div type="abstract" xml:lang="en">Abstract: A recent approach to solve Richards' equation is further improved. This approach brings understanding into the physical processes of infiltration and ponding. In particular we apply it to analyze the standard hydrologic tool of Time Compression Approximation (TCA). We also suggest that the new approach provides a more reliable alternative to TCA, e.g. for predicting ponding time.</div>
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<front><div type="abstract" xml:lang="en">A recent approach to solve Richards' equation is further improved. This approach brings understanding into the physical processes of infiltration and ponding. In particular we apply it to analyze the standard hydrologic tool of Time Compression Approximation (TCA). We also suggest that the new approach provides a more reliable alternative to TCA, e.g. for predicting ponding time.</div>
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<front><div type="abstract" xml:lang="en">Abstract: A recent approach to solve Richards' equation is further improved. This approach brings understanding into the physical processes of infiltration and ponding. In particular we apply it to analyze the standard hydrologic tool of Time Compression Approximation (TCA). We also suggest that the new approach provides a more reliable alternative to TCA, e.g. for predicting ponding time.</div>
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