“…It was first applied to tracer transport in saturated alluvial formations [Ahlstrom et al, 1977;Prickett et al, 1981], and then porous media of all types [Uffink, 1985;Kinzelbach, 1988;Cordes et al, 1991;Mahinthakumar and Valocchi, 1992;Tompson, 1993;Semra et al, 1993;LaBolle et al, 1996LaBolle et al, , 1998LaBolle et al, , 2000LaBolle and Fogg, 2001;Weissmann et al, 2002;Maxwell et al, 2007;Green, 2010] and extended to fractured rocks with matrix diffusion [Yamashita and Kimura, 1990;Wels et al, 1997;Liu et al, 2000;Tsang and Tsang, 2001;Roubinet et al, 2009Roubinet et al, , 2012.…”