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.

 

Classification

WRB 2006WRB 1998
Stagnic- Luvisol (Ferric Rhodic)Rhodi-Endostagnic- Luvisol
55-87 cmargic horizon
87-115 cmplinthic horizon
87-115stagnic colour pattern
87-115reducing conditions
0-35 cmochric horizon
55-87 cmargic horizon
87-115 cmplinthic horizon
87-115 cmferric horizon
87-115stagnic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Plinthi-Ferric LuvisolLuvic Xerosol
0-35 cmochric A horizon
55-87 cmargic B horizon
87-115plinthite
0-35 cmochric A horizon
55-87 cmargillic B horizon
87-115plinthite