Reference soil China 30: 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 CN030: Ferralsols
PROFILE DESCRIPTION : Deep, well drained, yellowish red clay derived from Quaternary red clay deposits. The topsoil has weakly to moderately developed (sub-)angular blocky structures while the subsoil is strong to very strong angular blocky. Organic carbon content is low and the soil reaction is strongly acid throughout. Dry soil breaks into enormous angular elements. PARENT MATERIAL: on a 20m higher plateau (distance 1km from site) 2-3m red Quaternary clay lies over an unconsolidated conglomerate. Slide nos. of the ISRIC collection: 13922-13928 (landscape, profile, profile details, vegetation, erosion features).