Reference soil Nigeria 15: Acrisol

NG015

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 NG015: Acrisols

BRIEF CHARACTERIZATION OF THE SOIL: Very deep poorly to imperfectly drained, pale yellow sandy soil; derived from alluvium with a thick dark topsoil and strong mottling in the subsoil. PARENT MATERIAL: Derived from coastal plain sand.

 

Classification

WRB 2006WRB 1998
Umbric-Gleyic- Acrisol (Albic Ferric Alumic Humic)Umbri-Gleyic- Acrisol (Albic Humic)
25-55 cmalbic horizon
55-120 cmargic horizon
55-165 cmferric horizon
-gleyic colour pattern
-reducing conditions
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Umbri-Gleyic Acrisol inundicGleyic Acrisol
0-25 cmumbric A horizon
25-55 cmalbic E horizon
55-120 cmargic B horizon
-gleyic
0-25 cmumbric A horizon
25-55 cmalbic E horizon
55-120 cmargillic B horizon
-hydromorphic

 

Local classification:Obigwe Series