“…In a Monte Carlo framework, heterogeneity of hydrogeologic properties is commonly characterized by the following two steps: (i) on the basis of a limited amount of direct measurements (i.e., hard data), multiple representations of aquifer properties are generated by means of the geostatistical techniques such as sequential Gaussian simulation (Deutsch and Journel, 1998), sequential indicator simulation (Gómez-Hernández and Srivastava, 1990), multiplepoint geostatistical approach (Strebelle, 2002;Mariethoz et al, 2010b) or other related methods; and then (ii) on the basis of indirect measurements such as piezometric head and concentration data, inverse modeling is utilized to reduce the uncertainty by integrating these data to better characterize the spatial variability of hydrogeologic properties (e.g. for an overview see Yeh, 1986;McLaughlin and Townley, 1996;Zimmerman et al, 1998;Carrera et al, 2005;Zhou et al, 2012b).…”