Reference soil Nigeria 16: Acrisol

NG016

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 NG016: Acrisols

BRIEF CHARACTERIZATION OF THE SOIL: Very deep, well drained, brown sandy clay, derived from coastal plain sand, with a thick dark brown topsoil and strong mottling in the subsoil. PARENT MATERIAL: Derived from coastal plain sand.

 

Classification

WRB 2006WRB 1998
Haplic- Acrisol (Alumic Chromic)Chromi-Alumic- Acrisol
10-120 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Haplic AcrisolFerric Acrisol
0-10 cmochric A horizon
10-120 cmargic B horizon
-ferric
0-10 cmochric A horizon
10-120 cmargillic B horizon
-ferric

 

Local classification:Elieta Series