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
Cutanic- Luvisol (Profondic Rhodic Colluvic) Rhodi-Profondic- Luvisol (Cutanic)
12-122 cm argic horizon
0-40 cm ochric horizon
12-122 cm argic horizon
FAO-UNESCO-ISRIC 1988 FAO-UNESCO-ISRIC 1974
OrthiChromic Luvisol Eutric Nitosol
0-40 cm ochric A horizon
12-122 cm argic B horizon
- fluvic property
0-40 cm ochric A horizon
12-160 cm argillic B horizon

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