“…The presence of preferential flow paths (PFP) affects soil water redistribution and results in quick catchment stormflow response and rapid transport of pollutants through the vadose zone (Alaoui et al, 2011;Sidle et al, 2000). Field investigations and modeling of water and tracer movement are important in studying numerous hydrological problems, including water resource contamination (Gödeke et al, 2006;Sudicky and Illman, 2011;Zheng et al, 2011), flood mitigation (Baker, 1987;Gubareva and Gartsman, 2010;Wood et al, 1990), and landslide initiation due to excess pore pressure generation (Iverson, 2000;Wilson et al, 2012). Usually the influence of PFP on mass transfer is determined experimentally by measuring water or tracer outflow from soil columns, lysimeters or in natural catchments (Everts and Kanwar, 1989;Ghodrati and Jury, 1992;Kung et al, 2000;Mallants et al, 1996;Tsuboyama et al, 1994;Vanderborght et al, 2000).…”