Luvisols
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.
Luvisols occur mainly in temperate regions, particularly in areas with a Mediterranean-type of climate.
To the Luvisol Picture Gallery
© ISRIC - World Soil Information (2008)
Last update: 1/5/2006
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