Reference soil France 08: Luvisol

FR008

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 FR008: Luvisols

LOCATION: Premises of the École Nationale Superieure Agronomique. VEGETATION AND LAND USE: coverage(%) Trees 15 herbs & grasses 90 ADDITIONAL NOTES ON PROFILE DESCRIPTION: Ah1 - strong worm activity. Ah2 - strong worm activity. - pedotubules: some with dark brown (10YR3/3) coatings. AB - consisting of material from overlying and underlying material, mixed by fauna. - strong worm activity. - cutans: ferri-argillans. - high macro porosity. - pedotubules: filled with material from top soil. Bt1 - strong worm activity. - cutans: ferri-argillans. - high macro porosity. Bt2 - cutans: ferri-argillans. - high macro porosity. Ck1 - cutans: calcitans Ck2 - myselial carbonate. - veins and pockets of soft lime, horizontally oriented, decreasing with depth.

 

Classification

WRB 2006WRB 1998
Calcic-Cutanic- Luvisol (Siltic Chromic)Chromi-Hypocalcic- Luvisol (Cutanic)
25-77 cmargic horizon
77-138 cmcalcic horizon
0-40 cmochric horizon
25-77 cmargic horizon
77-138 cmcalcic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Silti-Calcic LuvisolCalcic Luvisol
0-40 cmochric A horizon
25-77 cmargic B horizon
77-138 cmcalcic horizon
0-40 cmochric A horizon
25-77 cmargillic B horizon
77-138 cmcalcic horizon

 

Local classification:Sol brun lessivé