Reference soil Peru 16: Luvisol

PE016

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 PE016: Luvisols

Short field description A moderately deep, well drained, dark brown clay loam. The deeper subsoil has a yellowish brown colour. Soil profile located in a man-made terrace with 5 to 8 % slope which is a mountainside with 30% slope. The mountainside whithout man-made terraces show an increase in its grade of erosion and some landslide. "Others" in the climate data refers to the cloud cover in eights.

 

Classification

WRB 2006WRB 1998
Escalic- Luvisol (Humic Hypereutric Chromic)Chromic- Luvisol
27-59 cmargic horizon
-colluvic
-calcaric
0-27 cmochric horizon
27-59 cmargic horizon
-calcaric
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Calcari-Chromic LuvisolEutric Cambisol
0-27 cmochric A horizon
27-59 cmargic B horizon
- cmochric A horizon
-calcaric
0-27 cmochric A horizon
27-49 cmcambic B horizon

 

Local classification:Suelo Tarata