Reference soil Kenya 57: Luvisol

KE057

Luvisols occur mainly in temperate regions, particularly in areas with a Mediterranean-type of climate.

Characteristics

Soils having an argic horizon (a subsurface horizon with a distinct higher clay content than the overlying horizon) with a cation exchange capacity equal to or more than 24 cmolc per kg clay throughout.

Distribution of Luvisols (rough estimation supplied by soilgrids)

 

Reference soil KE057: Luvisols

Crotovinas at 20cm and at 64 - 80cm. A broken petrocalcic at 130 - 150cm. Other landuse: small scale rainfed annual crops. Slides: 10,168 - 10,172 and 10,178 - 10,183.

 

Classification

WRB 2006WRB 1998
Cutanic- Luvisol (Ruptic Clayic Chromic)Cutani-Chromic- Luvisol
130-140 cmpetrocalcic horizon
8-64 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Petrocalci-Chromic LuvisolChromic Luvisol petrocalcic
0-20 cmochric A horizon
130-140 cmpetrocalcic horizon
8-64 cmargic B horizon
-calcareous
0-20 cmochric A horizon
130-140 cmpetrocalcic horizon
8-64 cmargillic B horizon