Reference soil Kenya 26: Nitisol

KE026

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 KE026: Nitisols

A very deep, red, fine clayey soil, with a good structure and high biological activity, formed by weathering of andesite (?) rock. Fine and very fine grass roots are well distributed throughout the profile up to a depth of 400 cm. Many small soft manganese concretions between 205-210 cm occur. Below 270 cm there are continuous ferro-manganese coatings increasing with depth. This is the most important soil series of the area.

 

Classification

WRB 2006WRB 1998
Umbric-Acric- Nitisol (Humic)Humi-Umbric- Nitisol (Dystric)
0-79 cmumbric horizon
79-270 cmnitic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Umbri-Humic NitisolHumic Nitosol
0-79 cmumbric A horizon
40-270 cmargic B horizon
-nitic
-strongly humic
0-79 cmumbric A horizon
40-270 cmargillic B horizon

 

Local classification:Magombo series