“…S -soils are highly sandy, with very low profile water and evaporation; F -soils have very high clay content, highly mottled subsoils, with high profile water and evaporation; while T -soils are highly silty with the highest profile water content (Table 1). Soil types and its characteristics have been demonstrated to affect several processes in agroecosystems, such as the availability and supply of water to plants (Passioura, 1991), respiration and soil temperature (Koizumi et al, 1999), plant growth, vegetation cover and yield (Mako et al, 2008;Bestland et al, 2009;Genxu et al, 2009), the transfer and interaction of mineral nutrients (Echevarria et al, 2003;Matias et al, 2011), and the physical, chemical and biochemical properties of soils (Rhoton et al, 1993;Paz-Ferreiro et al, 2011), while higher soil sand content has been shown to improve AMF colonisation (Zaller et al, 2011).…”