“…The main characteristics of the soil are its advanced degree of weathering and high contents of iron oxides (greater than 180 g kg À1 ), aluminium, 1:1 clay minerals (kaolinite) and quartz (Reatto et al, 2008), which are characterised by low-activity clay, little differentiation among horizons, and a strong and well developed microgranular structure comprising angular and subangular microaggregates (Reatto et al, 2009;Brossard et al, 2012). These microaggregates are organised into micropeds that are smaller than 1 mm, with a porous massive structure according to Volland-Tuduri et al (2005).…”