Reference soil Namibia 06: Cambisol

NA006

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 NA006: Cambisols

Cambisol

 

Classification

WRB 2006WRB 1998
Fluvic- Cambisol (Calcaric Aridic Siltic)Calcari-Fluvic- Cambisol
18-110 cmcambic horizon
-calcaric
-fluvic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Fluvi-Haplic CalcisolCalcic Cambisol
0-18 cmochric A horizon
18-110 cmcambic B horizon
-soft powdery lime
0-18 cmochric A horizon
18-110 cmcambic B horizon
-soft powdery lime

 

Local classification:Dunkelbrauner, tiefgründiger, kalkhaltiger Talboden (Scholz, 1962)