Reference soil Spain 01: Luvisol

ES001

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 ES001: Luvisols

Short field description: Very deep, well drained, brown, coarse loamy profile. Structure of the top 30 cm is massive and moderate thereunder. The profile has a well developed textural B horizon with anbundant clayskins, mainly in the pores. * erosion. At site no evidence of erosion, however close to site places totally eroded by gully erosion. Gully during periods of high water. ** depth of water table > 150 cm.

 

Classification

WRB 2014 
Luvisol 
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Chromic LuvisolChromic Luvisol
- cmargic B horizon
- cmochric A horizon
- cmochric A horizon

 

Local classification:Tierra parda illimerizada