Reference soil Mali 04: Luvisol

ML004

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 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.

 

Classification

WRB 2006WRB 1998
Vertic- Luvisol (Hypereutric Hyperochric)Hyperochri-Vertic- Luvisol
14-135 cmvertic horizon
14-135 cmargic horizon
-aridic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Aridi-Vertic Luvisol takyricHaplic Xerosol
0-14 cmochric A horizon
14-135 cmargic B horizon
-vertic
0-14 cmochric A horizon
14-135 cmcambic B horizon
-aridic moisture regime

 

Local classification:Sol sodique