Reference soil Botswana 07: Luvisol
BW007
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 BW007: Luvisols
A moderately deep, moderately well drained reddish brown to yellowish red sandy loam with an apreciable amount of coarse fragments of a weak structural development and gradual horizonation, from 87 cm onwards underlain by a plinthite horizon in which coarse prominent red mottles occur from 87-100 cm.