Reference soil Kenya 47: Nitisol

KE047

Nitisols occur mainly in the tropics and subtropics, as well as in areas with a Mediterranean type of climate. They are associated with basic rocks (e.g. basalts) or hard limestone or dolomite deposits.

Characteristics

Soils having a nitic horizon (a horizon with pronounced nut-shaped soil structure and significant amount of active iron) within 100 cm from the soil surface, and gradual to diffuse horizon boundaries between the surface and the underlying horizons. They do not have a ferric, plinthic or vertic horizon within 100 cm from the soil surface.

Distribution of Nitisols (rough estimation supplied by soilgrids)

 

Reference soil KE047: Nitisols

Brief soil description: Very deep, well drained soil derived from basic volcanic breccia; with a thin dark reddish brown, clay topsoil over a dark reddish brown clay subsoil with clay cutans. The soil is used for arable farming with crops as sweet potato and maize. Slides: 10,071 - 10,072.

 

Classification

WRB 2006WRB 1998
Lixic-Ferralic- Nitisol (Humic Eutric)Hyperferrali-Humic- Nitisol (Eutric)
18-150 cmnitic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Chromi-Haplic NitisolFerric Luvisol
0-18 cmochric A horizon
18-150 cmargic B horizon
-nitic
0-18 cmochric A horizon
18-150 cmargillic B horizon
-ferric