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Título

Downward Infiltration - Estimation of S and K

AutorLatorre Garcés, Borja ; Moret-Fernández, David
Fecha de publicaciónoct-2016
EditorCSIC - Estación Experimental de Aula Dei (EEAD)
ResumenEstimation of soil soprtivity and hydraulic conductivity from cumulative infiltration data The sorptivity, S, and hydraulic conductivity, K, are estimated from the the inverse analysis of the full-time cumulative infiltration curve developed by Haverkamp et al. (1994) ,(Latorre et al. 2015). A procedure to detect and remove the effect of the contact sand layer and a sensitivity analysis using the water level measurement as uncertainty source (e.g. air-bubbling in the infiltrometer) are also included.
DescripciónThis calculation tool online is hosted on the following website: http://swi.csic.es/ More about it: https://digital.csic.es/handle/10261/157974 Creative Commons License Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0)
Versión del editorhttp://swi.csic.es/?page_id=5
URIhttp://hdl.handle.net/10261/157977
ReferenciasHaverkamp R, Ross PJ, Smettem KRJ, Parlange JY. 1994. Three dimensional analysis of infiltration from the disc infiltrometer. Part 2. Physically based infiltration equation. Water Resources Research 30: 2931-2935.
Latorre B, Peña, C, Lassabatere L, Angulo-Jaramillo R, Moret-Fernández D. 2015. Estimate of soil hydraulic properties from disc infiltrometer three-dimensional infiltration curve. Numerical analysis and field application. Journal of Hydrology 527: 1–12. http://digital.csic.es/handle/10261/89342
Latorre B, Moret-Fernández D. Soil and Water Infiltration [website]. https://digital.csic.es/handle/10261/157974
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