Reference soil Ireland 11: Luvisol

IE011

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 IE011: Luvisols

Parent material: glacial till, predominantly limestone composition,with admixture of shales,sandstones and some vulcanic materials (Weichselian). Vegetation: abundant occurence of rushes. Profile: Mottling in top horizons concentrated along rootchannels Presence of illuvial B horizons below 23 cm indicated by grain size analysis and micromorphology.

 

Classification

WRB 1998 
Albi-Gleyic- Luvisol (Epidystric) 
  
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Albi-Gleyic LuvisolGleyic Luvisol

 

Local classification:Podzolic Gley, Howardstown Series