Reference soil Nigeria 22: Acrisol

NG022

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 NG022: Acrisols

BRIEF CHARACTERIZATION OF THE SOIL: Very deep, moderately well drained brown to red sandy clay loam derived from acidic schist; with moderate mottling in the subsoil.

 

Classification

WRB 2006WRB 1998
Haplic- Acrisol (Alumic Hyperdystric Profondic Chromic)Alumi-Profondic- Acrisol (Hyperdystric Chromic)
15-197 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Chromi-Haplic AcrisolFerric Acrisol
0-15 cmochric A horizon
15-197 cmargic B horizon
0-15 cmochric A horizon
15-197 cmargillic B horizon
-ferric

 

Local classification:Etionni Series