Reference soil China 44: Cambisol

CN044

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.

Distribution of Cambisols (rough estimation supplied by soilgrids)

 

Reference soil CN044: Cambisols

PROFILE DESCRIPTION : Very deep, well drained, reddish brown to red clay loam developed from alluvial deposits derived from sandstone. PARENT MATERIAL: The parent material at a depth of 370 cm consists of a 50 cm thick layer of gravel deposited by a side branch of the Lancang Jiang river (Me Kong). The river, at a distance of 100m from the roadcut where the profile was described, has formed a deep valley and runs actually 50 m lower than the profile is situated. Under the alluvial deposits another type of parent material is found, limestone/sandstone.

 

Classification

WRB 2006WRB 1998
Ferralic- Cambisol (Alumic Chromic)Chromi-Ferralic- Cambisol (Hyperdystric)
40-260 cmcambic horizon
-ferralic
0-98 cmochric horizon
40-260 cmcambic horizon
-ferralic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Alumi-Ferralic CambisolFerralic Cambisol
0-98 cmochric A horizon
- cmcambic B horizon
- cmochric A horizon
-ferralic
0-98 cmochric A horizon
98-260 cmcambic B horizon
-ferralic

 

Local classification:Haplic latosol; Hapli-Udic Ferrosol
Common name:Acid red clay