Reference soil Mali 04: Luvisol
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.
Reference soil ML004: Luvisols
See also data of unit TH4 in "Mali Land and Water Resources", 1983, PIRT, mapscale 1:500.000. *Monitoring of vegetation by PIRT in the period 1980-1986. At the moment of site description no grass cover present, nearly 100% bare soil. Classification:(ST) when not Natrargid than typic Halaquept;(FAO) when not Xerosol then orthic Solonetz. Angular blocks of the horizons deeper than 14cm have tilted pedfaces (shearplanes/vertic properties?). No meteostation with reliable data nearby the site; precipitation is approximately the average of data from Kogoni(48.5cm) and Niafunke(28.0cm), for other elements average values of the meteostations of Segou and Timbuctu should be taken.