Reference soil Kenya 27: Cambisol

KE027

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 KE027: Cambisols

A deep and brown soil derived from volcanic ashes (Holocene-Pleistocene) on quartzite rock (Bukoban system), situated between a rolling landscape on the western side and an almost flat surrounding to the east; area includes some ant hills.

 

Classification

WRB 2006WRB 1998
Haplic- Cambisol (Hypereutric Siltic)Hypereutric- Cambisol
10-114 cmcambic horizon
114-152 cmferric horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Eutric CambisolEutric Cambisol
0-10 cmochric A horizon
10-114 cmcambic B horizon
0-10 cmochric A horizon
10-114 cmcambic B horizon