Reference soil Peru 09: Cambisol

PE009

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 PE009: Cambisols

Short field description A moderately deep, well drained, (dark) brown clay. The texture becomes more sandy in the subsoil. The soil site is located in 'Tierra firme', i.e. not flooded by rivers, on the summit of a hill along the road. The layers of parent material show an undulating arrangement. This and the irrgular texture with depth are indications that the parent material could also be an old alluvium.

 

Classification

WRB 2006WRB 1998
Haplic- Cambisol (Calcaric Ruptic Cp)Calcaric- Cambisol
2-107 cmcambic horizon
-calcaric
-lithological discontinuity
-secondary carbonates
0-2 cmochric horizon
2-107 cmcambic horizon
-calcaric
-secondary carbonates
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Calcaric CambisolEutric Cambisol
0-2 cmochric A horizon
2-107 cmcambic B horizon
- cmochric A horizon
-calcaric
-soft powdery lime
0-2 cmochric A horizon
2-107 cmcambic B horizon
-soft powdery lime