Reference soil Colombia 18: Acrisol

CO018

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 CO018: Acrisols

ADDITIONAL NOTES ON PROFILE DESCRIPTION: Ah - also many coarse roots; BC - from 105-110 cm in places gravelly sandy clay loam; C2 - 10R4/8, 2.5YR5/8, 7.5YR5/8 and 10YR7/2.

 

Classification

WRB 2006WRB 1998
Haplic- Acrisol (Alumic)Alumic- Acrisol
35-145 cmargic horizon
0-35 cmochric horizon
35-145 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Ferrali-Haplic AcrisolXanthic Ferralsol
0-35 cmochric A horizon
35-145 cmargic B horizon
- cmochric A horizon
-ferralic
0-59 cmochric A horizon
35-145 cmoxic B horizon