“…As reported previously, soil has a stronger adsorption capacity for bacteria than sand, as it has smaller particles and contains more organic matter (Jdvan et al, 1991;Huysman and Verstraete, 1993). This is because the adsorption of microorganisms in soil involve not only physical processes, such as soil adsorption, retention and filtration, but also chemical factors, including electrostatic and the Van der Waals forces between microbial surfaces and soil colloids (Weiss et al, 1995;Rysz and Alvarez, 2006;Wu et al, 2013). Soil types, soil particle sizes, organic matter, microorganism motilities, as well as microorganism motilities and sizes, significantly influence equilibrium adsorption characteristics and coefficients in soil (Coffey et al, 2010;Gyrya et al, 2010;Schinner et al, 2010).…”