Reference soil Kenya 23: Luvisol

KE023

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 KE023: Luvisols

A deep-rooting (125-180 cm), ill-sorted sandy soil of a dry and hot climate with small clay bands at 250 cm and a gravelly layer at 270 cm. Inside growing season the soil gets flooded 3 or 4 times and offers very extensive grazing land for animals; also many large krotovinas; vegetation: accacia sp., indigofera sp.

 

Classification

WRB 2006WRB 1998
Cutanic- Luvisol (Hypereutric Profondic)Cutani-Profondic- Luvisol
65-170 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Haplic LuvisolLuvic Xerosol
0-45 cmochric A horizon
65-170 cmargic B horizon
0-45 cmochric A horizon
65-170 cmargillic B horizon
-aridic moisture regime