Reference soil Gabon 06: Acrisol

GA006

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 GA006: Acrisols

An imperfectly drained soil, derived from cretaceous sediments. The primary tropical forest has been burnt and replaced by herbs and grasses with some cultivated plots in-between (manioc, bananas, plantain). In the upper 25 cm some charcoal particles appear. The Btg2 horizon contains some quartz grains (3mm); vegetation; Afromomum giganteum, Dicronopteris linearis, Musanga cecropioides.

 

Classification

WRB 2006WRB 1998
Gleyic-Cutanic- Acrisol (Alumic Epieutric Profondic)Profondi-Endogleyic- Acrisol (Alumic)
25-150 cmargic horizon
-reducing conditions
-gleyic colour pattern
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Alumi-Gleyic AcrisolGleyic Acrisol
0-6 cmochric A horizon
25-150 cmargic B horizon
-gleyic
0-6 cmochric A horizon
25-150 cmargillic B horizon
-hydromorphic

 

Local classification:Sol ferrallitique, fortement désaturé, apprauvi