“…Studies have documented increased infiltration rates in buffers (Schmitt et al, 1999) due to improved soil porosity and hydraulic conductivity (Udawatta and Anderson, 2008;Kumar et al, 2011;Larson and Safferman, 2012). Seobi et al (2005) and Kumar et al (2012) determined that soil hydraulic conductivity values were four to 16 times higher in an agroforestry buffer than in the associated cropland or pasture. Reported trapping effectiveness values of upland and edge-of-field buffers vary widely among studies: from 41% to 100% for sediment and from 27% to 96% for total phosphorus (TP) (Dillaha et al, 1989;Daniels and Gilliam, 1996;Schmitt et al, 1999;Mayer et al, 1999;Lee et al, 2000;Blanco-Canqui et al, 2004;Vianello et al, 2005;Bhattarai et al, 2009;Caron et al, 2010;Al-wadaey et al, 2012).…”