Reference soil Nigeria 15: Acrisol
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
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 2006 | WRB 1998 | ||||||||||||||||||
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Umbric-Gleyic- Acrisol (Albic Ferric Alumic Humic) | Umbri-Gleyic- Acrisol (Albic Humic) | ||||||||||||||||||
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FAO-UNESCO-ISRIC 1988 | FAO-UNESCO-ISRIC 1974 | ||||||||||||||||||
Umbri-Gleyic Acrisol inundic | Gleyic Acrisol | ||||||||||||||||||
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Local classification: | Obigwe Series |