Reference soil Côte d'Ivoire 01: Acrisol

CI001

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 CI001: Acrisols

Extremely deep, somewhat excessively drained, red, very gravelly clay soil derived from Precambrian migmatites. The forest surface has a very thin, rapidly decomposing, litter layer and a what irregular surface. PARENT ROCK: Hard, rich in biotite, with a high mineralogical content of kaolinite, iron and aluminium (hydr-)oxides. Precambrian basement system. ADDITIONAL NOTES ON PROFILE DESCRIPTION: O - 3 to 4 types of leaves, various stages of decomposition; Gravel: concretions, ironstone; from 0-70cm angular; from 70cm+ spherical.

 

Classification

WRB 2006WRB 1998
Pisoplinthic-Vetic- Acrisol (Hyperdystric Profondic Clayic)Veti-Pisoplinthic- Acrisol (Profondic Hyperdystric)
0-100 cmpisoplinthic horizon
50-160 cmferralic horizon
7-160 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Veti-Ferric Acrisol skeleticOrthic Ferralsol petric
0-7 cmochric A horizon
50-160 cmferralic B horizon
7-160 cmargic B horizon
-ferric
0-7 cmochric A horizon
7-160 cmoxic B horizon
-ferric

 

Local classification:Sol ferrallitique