Reference soil Mali 03: 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 ML003: Luvisols
See also data of unit DA4 in "Mali Land and Water Resources" 1983, PIRT, mapscale 1:500.000 *Sols brun-rouges sub-arides de transition vers les ferrugineux. *Monitoring of vegetation by PIRT period 1980-1986. Landscape: eroded dunes, very weak undulating. Deeper subsoil is imperfectly drained. Geogenesis:probably cover sand over ancient alluvial plain (check with textural analysis and micromorphology). Groundwater in nearby wells at a depth of about 50 meters. No meteo station with reliable data nearby site; precipitation is approximately the average of data from Kogoni(54.2cm) and Niafunke(28,0cm), for other meteo elements the average values of the meteo stations of Segou and Timbuctu should be taken