Reference soil Peru 10: Acrisol

PE010

Acrisols occur dominantly in the wetter parts of the tropics and subtropics and the warm temperate regions in relatively young landscapes.

Characteristics

Soils having an argic horizon (a subsurface horizon with distinct higher clay content than the overlying horizon), which has a cation exchange capacity of less than 24 cmolc per kg in some part, either starting within 100 cm from the soil surface, or within 200 cm from the soil surface if the argic horizon is overlain by loamy sand or coarser textures throughout. They have a base saturation (total amount of Ca, Mg, K and Na with respect to the cation exchange capacity) of less than 50 percent in the major part between 25 and 100 cm from the soil surface

Distribution of Acrisols (rough estimation supplied by soilgrids)

 

Reference soil PE010: Acrisols

Short field description A very deep, well drained, yellowish red and red clay. The soil is well structured and highly porous because of bio-activity. A thin leaf litter layer of aout 2 cm is present. The distinction between the soil horizons Bt1 to Bt4 are due to minor colour differences with gradual to diffuse boundaries. The soil site is located in 'Tierra Firme' i.e. terrain which is not flooded.

 

Classification

WRB 2006WRB 1998
Haplic- Acrisol (Alumic Profondic Clayic)Alumi-Profondic- Acrisol (Chromic)
38-150 cmargic horizon
0-25 cmochric horizon
38-150 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Alumi-Haplic AcrisolFerralic Cambisol
0-25 cmochric A horizon
38-150 cmargic B horizon
- cmochric A horizon
0-25 cmochric A horizon
25-150 cmcambic B horizon
-ferralic

 

Local classification:Suelo Carretera