Reference soil Norway 03: Cambisol

NO003

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 NO003: Cambisols

Classification

WRB 1998 
Dystri-Fluvic- Cambisol 
  
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Fluvi-Dystric CambisolDystric Cambisol