“…Even though model predictions can be strongly affected by the spatial variability of both hydraulic and biochemical properties [Rehfeldt et al, 1992;Miralles-Wilhelm and Gelhar, 1996;Miralles-Wilhelm et al, 1997;Cunningham and Fadel, 2007;Maxwell and Kastenberg, 1999;Maxwell et al, 2007], reactive transport codes based on Eulerian methods such as finite-difference or finite elements [e.g., Saaltink et al, 2004;Clement, 1997] still undergo computational burden and numerical problems when modeling strong heterogeneities and complex biochemical systems at high resolution. In this context, Particle Tracking Methods (PTMs) offer a convenient numerical solution particularly efficient in dealing with heterogeneities [e.g., Wen and GomezHernandez, 1996;LaBolle et al, 1996;Salamon et al, 2007;Riva et al, 2008] and a large variety of complex transport processes such as non-Fickian transport [Delay and Bodin, 2001;Cvetkovic and Haggerty, 2002;Berkowitz et al, 2006;Zhang and Benson, 2008;Dentz and Castro, 2009] and multiple porosity systems [Salamon et al, 2006b;Benson and Meerschaert, 2009;Tsang and Tsang, 2001;Huang et al, 2003;Willmann et al, 2013].…”