Reference soil India 05: 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 IN005: Cambisols
A moderately deep, well drained brown soil with a silty loam texture, derived from weathered biotite schist and granite gneiss, situated in the southern foothills of the Himalayas. The upper part of the soil is most likely of colluvial origin. In the lower brown and gray mottles appear along the root channels, grading into whitish silt coatings. Soil reaction is neutral near the surface, becoming acid in the subsoil. Organic carbon content of the topsoil is high.