Reference soil Turkey 07: Luvisol

TR007

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 TR007: Luvisols

STONINESS: Rounded basaltic fresh bombs. CRACKS: 4 to 7cm wide and 20 to 25cm deep. ADDITIONAL NOTES ON PROFILE DESCRIPTION: Ap - many gravels, stones, boulders. B12 - also slickensides: shining surfaces with angle of 45°. B12Ca - also slickensides: shining surfaces with angle of 45°. B22Ca - also slickensides: shining surfaces with angle of 45°. B3 - slickensides: with angle of 45°.

 

Classification

WRB 2014 
Luvisol 
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Vertic LuvisolVertic Luvisol
- cmargic B horizon
- cmochric A horizon
-vertic
- cmargillic B horizon
- cmochric A horizon
-vertic

 

Local classification:Reddish Brown Mediterranean Soil