Reference soil China 36: Luvisol

CN036

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 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

 

Classification

WRB 2006WRB 1998
Cutanic- Luvisol (Siltic Chromic)Cutani-Chromic- Luvisol (Haplic)
17-105 cmargic horizon
0-17 cmochric horizon
17-105 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Silti-Chromic LuvisolChromic Luvisol
0-17 cmochric A horizon
17-105 cmargic B horizon
- cmargic B horizon
- cmochric A horizon
0-17 cmochric A horizon
17-105 cmargillic B horizon

 

Local classification:Argillic brown soil; Hapli-Ustic Argosol
Common name:Brown claypan soil