“…These types of data are typically based on standard grain sieve analysis of soil samples, yielding a discrete representation of the curves by measuring selected particle diameters which, in turn, correspond to quantiles of the particle-size curve. The information can then be employed to classify soil types [e.g., Riva et al (2006) and references therein], to infer hydraulic parameters such as porosity and hydraulic conductivity [e.g., amongst others, Lemke and Abriola (2003); Riva et al (2006Riva et al ( , 2008Riva et al ( , 2010; Bianchi et al (2011);Tong et al (2010); Barahona-Palomo et al (2011) and references therein], or, in the presence of inorganic compounds, to provide estimates of the porous medium sorption capacity [e.g., Hu et al (2004) and references therein].…”