Reference soil Nigeria 20: Acrisol

NG020

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 NG020: Acrisols

BRIEF CHARACTERIZATION OF THE SOIL: Very deep, well drained reddish sandy clay derived from sandstone, with strong mottling and many horizontal tubular pores in the subsoil. Profile extends down to 390 cm.

 

Classification

WRB 2006WRB 1998
Vetic- Acrisol (Alumic Profondic Clayic Rhodic)Profondi-Vetic- Acrisol (Alumic Rhodic)
20-268 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Chromi-Haplic AcrisolFerric Acrisol
0-20 cmochric A horizon
20-268 cmargic B horizon
0-20 cmochric A horizon
20-268 cmargillic B horizon
-ferric

 

Local classification:Owode Series