Reference soil Botswana 03: 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 BW003: Luvisols
GEOLOGY: Precambric rocks, mainly granites from the Mahalapye formation. LOCATION: 500 m South of the road to Bonwapitse MOISTURE: soil dry from 0 to 70 cm and slightly moist below VEGETATION: Acacia nigerescens, A. robusta, and Dichrostachys cenerea. HUMAN INFLUENCE: plough layer from 0-20 cm. BRIEF DESCRIPTION: A deep, moderately well drained sandy clay loam with a gley horizon commencing at 76 cm depth. Horizonation is gradual, structural development weak to absent. Weathered rock is encountered at 129 cm depth, while a plouth layer of a coarse sandy loam texture is present from 0-20 cm. The soil reaction is slightly acid from 0-104 cm and becomes neutral to mildly alkaline in the B3. MORPHOLOGY: Ap Few termine nests with 2 cm diameter. B21 Thin cutans in root and termine channels. B2g Coarse fragments increasing with depth. B2g Appreciable amount of coarse fragments and few small prominent reddish concretions in the lower part of the horizon. C Weathered rock with common distinct bluish black fine concretions.