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.