“…Likewise, particle detachment and soil erosion is clearly a threshold process (Hicks et al, 2000;Salles et al, 2000;Hairsine et al, 2002;Shao et al, 2005;Maerker et al, 2008;Scherer, 2008;Ternat et al, 2008), which is controlled by rainfall intensity, shear stress due to overland flow and soil stability. Infiltration, vertical flow and transport of contaminants in field soils may be observed in two qualitatively different modes, namely in preferential pathways or in a slow form in the soil matrix continuum (Bouma, 1981;Beven and Germann, 1982;Edwards et al, 1989;Flury et al, 1994Flury et al, , 1996Stamm et al, 1998;Zehe and Flühler, 2001a, b;Vogel et al, 2005;McGrath et al, 2007). Lateral preferential flow in soil pipe systems, which crucially determines hillslope scale subsurface runoff generation, is intermittent and is likely to be a threshold phenomenon as well (Adams and Parkin, 2002;Buttle and McDonald, 2002;Negishi et al, 2007;Weiler and McDonnell, 2007).…”