Reference soil Peru 12: Cambisol

PE012

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 PE012: Cambisols

A moist soil column (monolith) of 145cm shrinks after drying to a length of 138cm (5%)

 

Classification

WRB 2006WRB 1998
Endogleyic- Cambisol (Alumic Humic Clayic)Chromi-Gleyic- Cambisol (Dystric)
22-66 cmcambic horizon
-gleyic colour pattern
-stagnic colour pattern
-vertic
0-22 cmochric horizon
22-66 cmcambic horizon
-gleyic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Stagni-Gleyic AlisolGleyic Cambisol
0-22 cmochric A horizon
22-66 cmargic B horizon
-stagnic
0-22 cmochric A horizon
-hydromorphic

 

Local classification:Altura