Reference soil Botswana 06: Luvisol
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.
Reference soil BW006: Luvisols
LOCATION: 3 km South of the road to Mahalapye GEOLOGY: Undifferentiated granitic rocks from the basement complex with subordinate occurrence of dolerite. ROCK OUTCROPS: Marutlwe hill (doleritic sill) 1 km to the South VEGETATION: Combreapiculatum, Acacia nigerescens (on abandoned field) Acacia tortilis and Dichrostachys cinerea. MORPHOLOGY: B3 Coarse fragments increasing with depth C Extremely hard mottled granite BRIEF PROFILE DESCRIPTION: A deep, well drained, reddish brown coarse sandy loam with gradual horizonation and weak to none structural development. The soil reaction is slightly acid throughout.