Reference soil Nigeria 12: Acrisol

NG012

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 NG012: Acrisols

Brief description of the profile: Deep, well drained, red sandy clay loam with an increase of clay with depth and a soft plinthic horizon from 64 cm onwards blocked by hard plinthite at 130 cm depth; horizontation is gradual, structural development is weak. Parent material: Migmatites and granites of the basement complex. Land use and vegetation: Pure Isoberlinia woodland, grasscover mainly consisting of Andropogon gayanus. Additional notes on profile description: B2t: Mottles distinct, black and yellowish. B3: Between 100 - 130 cm fairly hard plinthite; texture as indicated only in the softer parts of the horizon. "Rhodoxic" (USDA) tentative subgroup. Climate data source: Agroclimatological data Africa 1, FAO. Rome 1984.

 

Classification

WRB 2006WRB 1998
Plinthic-Cutanic- Acrisol (Epieutric Chromic)Chromi-Plinthic- Acrisol
100-130 cmpetroplinthic horizon
36-130 cmargic horizon
64-100 cmplinthic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Chromi-Plinthic AcrisolPlinthic Acrisol
0-16 cmochric A horizon
36-130 cmargic B horizon
-plinthite
0-16 cmochric A horizon
36-130 cmargillic B horizon
-plinthite

 

Local classification:Upper series Borgu Game Res.