Reference soil Indonesia 02: Cambisol
Cambisols occur mainly in the temperate and boreal regions of the world, where the soil’s parent material is still young or where low temperatures slow down the processes of soil formation.
Characteristics
Soils having either a cambic horizon (a horizon showing evidence of alteration with respect to the underlying material), or a mollic horizon overlying a subsoil, which has a base saturation of less than 50 percent in some part within 100 cm from the soil surface, or one of the following diagnostic horizons within the specified depth: an andic, vertic, or vitric horizon starting between 25 and 100 cm; a (petro-)plinthic or salic horizon starting between 50 and 100 cm, in absence of loamy sand or coarser textures above these horizons.
Reference soil ID002: Cambisols
CLASSIFICATION: The soil has more than 12kg/m² organic carbon between the mineral surface and a depth of 100cm. PHYSIOGRAPHY: Footslope area of Gunung Pangrango volcano. PARENT MATERIAL: Intermediate volcanic tuff. LAND USE AND VEGETATION: Abandoned rubber plantation. Rough grassland with some residual rubber trees. Whole area is cleared of its original vegetation and has been transformed into arable land, exclusive of some more remote places which are covered with secondary shrubs and trees. REFERENCES: - P. Buurman et al, 1980: "Red soils in Indonesia", pp. 24-47; Pudoc, Wageningen.