Reference soil Peru 11: Ferralsol
Ferralsols occur in tropical and subtropical regions of the world, mainly on old and stable land surfaces.
Characteristics
Soils having a ferralic horizon (strongly weathered horizon with low-activity clays and very low amounts of weatherable minerals) between 25 and 200 cm from the soil surface. They lack a nitic horizon (a horizon with strongly developed, nut-shaped structure) and do not have a layer which fulfils the requirements of an argic horizon and which has, in the upper 30 cm, 10 percent or more water-dispersible clay.
Reference soil PE011: Ferralsols
Short field description A very deep, well drained, yellowish brown clay overlying a yellowish red clay. At a depth of about 20 cm are some rounded, partly broken gravel stones. The subsoil is strongly mottled and has iron concretions. The Bt1 horizon can be divided in two layers: from 64-78 cm with the maximum concentration of iron/manganese concretions and 78-100 cm with very few concentrations. The soil colour from 78 to 150 cm is heterogenous and consists of a mix of yellowish, brownish and reddish colours. This may be indicative for water saturation during some part of the year. The soil is located in 'Tierra firme', terrain not flooded by rivers, located in a high terrace. The rounded stones in the topsoil are indicating that the soil may also be derived from an old alluvium. The land has been cultivated for about 65 years, recently it is pasture land, which is burned each year in september. In the FAO 1988 classification the soil classifies as Haplic Lixisol. Because no cutans were observed in the field, no argillic horizon can be recognized in FAO (1974), therefore the soil classifies as Ferralic Cambisol.