“…The physical processes such as advection, dispersion, diffusion, straining and physical filtration, adsorption and biological processes such as growth/ decay processes and include active adhesion/detachment, survival and chemotaxis are strongly affected on biocolloid transport in saturated and unsaturated porous media. Although there is a substantial body of published research on biocolloidal transport in the subsurface, much of it focuses on transport in the saturated zone (e. g. Bales et al 1989;Chu et al 2000;Chu et al 2001;Fontes et al 1991;Harvey 1997;Hornberger et al 1992;McCarthy and McKay 2004;McKay et al 1993;Sen and Khilar 2006;Sen and Khilar 2009;Sen et al 2004) rather than on transport in the unsaturated vadoze zone. In the unsaturated porous media, the additional mechanisms (compared with saturated zone) for colloid transport are reported as: colloid captured at the liquid-gas interface (Crist et al 2004;2005;Gao et al 2008;Zevi et al 2005), colloid capture due to straining (Wan and Tokunaga 1997;Bradford et al 2006, colloid captured at solid-liquid-gas interface (Williams and Berg 1992;Abdel-Fattah and El-Genk 1998;Sirivithayapakorn and Keller 2003;Lazouskaya and Jin 2006) and colloid storage in immobile zone (Cherrey et al 2003;Gamerdinger and Kaplan 2001;Gao et al 2006), respectively.…”