Reference soil China 36: Luvisol
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.
Reference soil CN036: Luvisols
PROFILE DESCRIPTION : Deep, moderately well drained, light brown to yellowish brown silty clay loam derived from loess-like lacustrine deposits overlying red, very gravelly sandy clay loam. The dark yellowish brown to strong brown topsoil shows weakly developed crumb and platy structures and is low in organic carbon. The subsoil dominantly shows strongly developed prismatic and angular blocky structures. Soil reaction is neutral to slightly acid. CLIMATE: climatic data regarding sunshine hours per month: J 171.2 F 185.2 M 234.2 A 271.6 M 248.7 J 271.6 J 215.9 A 277.6 S 242.2 O 215.1 N 164.2 D 154.9 Year 2574.0