“…We assume that the stochastic variability of subsurface porosity can be adequately captured by a Gaussian two-point geostatistical model. This assumption is generally considered to be valid for a given hydrogeological unit (e.g., Kelkar and Perez, 2002;Dafflon et al, 2009). For the parameterization of this model, we consider the so-called von Kármán autocorrelation function which, due to its versatility, has been used for a wide variety of research objectives, such as seafloor morphology quantification (e.g., Goff and Jordan, 1988), borehole data analysis (e.g., Dolan and Bean, 1997;Jones and Holliger, 1997), numerical simulations of wave propagation (e.g., Frankel and Clayton, 1986;Hartzell et al, 2010), and aquifer characterization (e.g., Tronicke and Holliger, 2005;Dafflon et al, 2009).…”