“…In general, carbonate rocks are characterized as a more heterogeneous media than sandstone rocks and therefore require a longer time to reach the asymptotic regime. Recently, there have been extensive studies on pre-asymptotic dispersion in various porous media (Bijeljic et al, 2011(Bijeljic et al, , 2013aBijeljic et al, 2013b;Blunt et al, 2013;Mitchell et al, 2008;Scheven et al, 2007;Scheven et al, 2005). Most of these focused on velocities in the transition region or above is Fickian-like and predominately dictated by restricted diffusion (Bijeljic et al, 2004;Gist et al, 1990;Levy and Berkowitz, 2003;Sahimi, 1995).…”