Reference soil Botswana 03: Luvisol

BW003

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 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.

 

Classification

WRB 2006WRB 1998
Cutanic- Luvisol (Chromic)Cutani-Chromic- Luvisol
21-104 cmargic horizon
0-21 cmochric horizon
21-104 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Haplic LuvisolLuvic Yermosol phreatic
0-21 cmochric A horizon
21-104 cmargic B horizon
-fluvic
0-21 cmochric A horizon
21-104 cmargillic B horizon
47-104hydromorphic