Reference soil Côte d'Ivoire 02: Acrisol

CI002

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 CI002: Acrisols

PARENT ROCK: Hard migmatite, rich in biotite; Precambrian Basement System. ADDITIONAL NOTES ON PROFILE DESCRIPTION: O - 2 to 3 leaves thick (rapidly decomposing). Ahcs - nodules: with black patina. Bcs1 - color interior concretions: 5YR3/2; nodules: with black patina. Bcs2 - nodules: with black patina. 2Bws - color interior concretions: 2.5YR4/6. Gravel: iron concretions up to 5cm in diameter, irregular.

 

Classification

WRB 2006WRB 1998
Pisoplinthic-Vetic- Acrisol (Hyperdystric Profondic Clayic)Veti-Pisoplinthic- Acrisol (Profondic Hyperdystric)
0-70 cmpisoplinthic horizon
10-150 cmargic horizon
40-150 cmferralic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Veti-Ferric Acrisol skeleticFerric Acrisol petric
0-10 cmochric A horizon
10-150 cmargic B horizon
40-150 cmferralic B horizon
-ferric
0-10 cmochric A horizon
10-150 cmargillic B horizon
40-150 cmoxic B horizon
-ferric

 

Local classification:Sol ferrallitique, see remarks