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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 22, issue 2
Hydrol. Earth Syst. Sci., 22, 1193–1219, 2018
https://doi.org/10.5194/hess-22-1193-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 22, 1193–1219, 2018
https://doi.org/10.5194/hess-22-1193-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 12 Feb 2018

Research article | 12 Feb 2018

Parametric soil water retention models: a critical evaluation of expressions for the full moisture range

Raneem Madi et al.

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Cited articles

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Assouline, S. and Or, D.: Conceptual and parametric representation of soil hydraulic properties: a review, Vadose Zone J., 12, https://doi.org/10.2136/vzj2013.07.0121, 2013.
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Behrangi, A., Khakbaz, B., Vrugt, J. A., Duan, Q., and Sorooshian, S.: comment on “Dynamically dimensioned search algorithm for computationally efficient watershed model calibration” by Tolson, B.A., and Shoemaker, C. A., Water Resour. Res., 44, W12603, https://doi.org/10.1029/2007WR006429, 2008.
Bradley, R. S.: Polymolecular adsorbed films. Part I. The adsorption of argon on salt crystals at low temperatures, and the determination of surface fields, J. Chem. Soc. (Resumed), 1467–1474, https://doi.org/10.1039/JR9360001467, 1936.
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Water flows through soils with more difficulty when the soil is dried out. Scant rainfall in deserts may therefore result in a seemingly wet soil, but the water will often not penetrate deeply enough to replenish the groundwater. We compared the mathematical functions that describe how well different soils hold their water and found that only a few of them are realistic. The function one chooses to model the soil can have a large impact on the estimate of groundwater recharge.
Water flows through soils with more difficulty when the soil is dried out. Scant rainfall in...
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