Reference soil Peru 22: Cambisol

PE022

Cambisols occur mainly in the temperate and boreal regions of the world, where the soil’s parent material is still young or where low temperatures slow down the processes of soil formation.

Characteristics

Soils having either a cambic horizon (a horizon showing evidence of alteration with respect to the underlying material), or a mollic horizon overlying a subsoil, which has a base saturation of less than 50 percent in some part within 100 cm from the soil surface, or one of the following diagnostic horizons within the specified depth: an andic, vertic, or vitric horizon starting between 25 and 100 cm; a (petro-)plinthic or salic horizon starting between 50 and 100 cm, in absence of loamy sand or coarser textures above these horizons.

Distribution of Cambisols (rough estimation supplied by soilgrids)

 

Reference soil PE022: Cambisols

Short field description A very deep, well drained dark reddish brown (clay) loam. The soil profile is located in a man-made terrace on a mountain slope, near to Pomacanchi lake. The man-made terraces are in ddifferent states of degradation.

 

Classification

WRB 2006WRB 1998
Haplic- Cambisol (Humic Hypereutric Chromic)Hypereutri-Chromic- Cambisol
18-108 cmcambic horizon
0-43 cmochric horizon
18-108 cmcambic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Chromic CambisolChromic Cambisol
0-43 cmochric A horizon
18-108 cmcambic B horizon
- cmochric A horizon
0-43 cmochric A horizon
18-108 cmcambic B horizon

 

Local classification:Suelo Pomacanchi