Soil Water Retention and Hydraulic Conductivity fitting
This web app implements key water retention models along with our recently proposed Inverse Laplace Transform (ILT) model (Cardinali et al., 2024; Cardinali et al., 2025) for fitting your data. The ILT model has proven effective in capturing complex, multi-modal soil porosity structures, providing a continuous spectrum of pore size distributions. In addition, we have extended our approach to explore both Multi-Exponential and Multi-Gaussian models:
where \(\omega\) is the amplitude and \(h_0\) its respective characteristic matric potential, which are physically interpreted as the amount of pores that empty at that suction head. Based on the ILT-Gaussian approach and using cappilary bundle model, the closed-form equation to unsaturated hydraulic conductivity for ILT-gauss is
where \(K_s\) is the saturated hydraulic conductivity, and \(\ell\), \(\beta\), and \(q\) are fitting parameters of the \(K(h)\) function. For all models, the hydraulic conductivity was obtained using general capillary bundle model equation:
where \(K_s\), \(\ell\), \(\beta\), and \(q\) are fitting parameters, with \(\ell = 0.5\), \(\beta = 1\), and \(q = 2\) when fixed (Mualem).
More details are available in our papers (see citation). Please remember to cite our work if you use this webapp.
Questions? Watch the tutorial video: https://www.youtube.com/watch?v=UKdAfjYKiS4Supporters
M. C. B. Cardinali, G. V. Von Atzingen, T. B. Moraes
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