Reference soil Ghana 04: Acrisol

GH004

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 GH004: Acrisols

Acrisol

 

Classification

WRB 2006WRB 1998
Pisoplinthic- Acrisol (Profondic Clayic Rhodic)Ferri-Profondic- Acrisol (Hyperdystric Chromic)
18-37 cmpisoplinthic horizon
37-220 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Chromi-Ferric Acrisol petroferricFerric Acrisol petroferric
0-18 cmochric A horizon
18-37 cmcambic B horizon
37-220 cmargic B horizon
-ferric
0-18 cmochric A horizon
18-37 cmcambic B horizon
37-220 cmargillic B horizon
-ferric

 

Local classification:Forest Ochrosol, Bekwai series