Reference soil Botswana 01: Luvisol
BW001
Distribution of Luvisols
A deep, moderately well drained profile with a topsoil of dark reddish brown sandy clay loam overlying a homogeneous dusky red clayey subsoil (underlain by very hard calcrete). Organic matter decreases irregularly and remains high with depth. Coarse mineral fragments of quartz and granite occur throughout the profile and increase with depth. Only a very few thin clay cutans are observed in thin sections. Kaolinite is the dominant clay mineral.
Classification
WRB 2006 | WRB 1998 | ||||||||||||
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Cutanic- Luvisol (Profondic Rhodic Colluvic) | Rhodi-Profondic- Luvisol (Cutanic) | ||||||||||||
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FAO-UNESCO-ISRIC 1988 | FAO-UNESCO-ISRIC 1974 | ||||||||||||
OrthiChromic Luvisol | Eutric Nitosol | ||||||||||||
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Local classification
Classification information | Tobela series |
Other classification
USDA-NRCS (1999) | Aridic Paleustalf ustic fine mixed hyperthermic |
USDA-SCS (1975) | Aridic Paleustalf ustic fine mixed hyperthermic |
Location:
Central Province, 6km SE of Shoshong, S of Serowe