Reference soil Botswana 06: Luvisol

BW006

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 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.

 

Classification

WRB 2006WRB 1998
Haplic- Luvisol (Profondic Chromic)Chromi-Profondic- Luvisol
33-122 cmargic horizon
0-33 cmochric horizon
33-122 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Chromic LuvisolLuvic Yermosol
0-33 cmochric A horizon
33-122 cmargic B horizon
0-33 cmochric A horizon
33-170 cmargillic B horizon
87-100plinthite
87-115hydromorphic