Reference soil Kenya 12: Acrisol

KE012

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 KE012: Acrisols

A deep-rooting, porous, and well drained soil in undulating coastal uplands originating from coarse-grained sandstones (Shimba grit), with high biological activity and a very weak surface sealing. (R3 pg 205)

 

Classification

WRB 2006WRB 1998
Cutanic- Acrisol (Epieutric Profondic Chromic)Chromi-Profondic- Acrisol
15-220 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Chromi-Haplic AcrisolOrthic Acrisol
0-15 cmochric A horizon
15-220 cmargic B horizon
0-15 cmochric A horizon
15-220 cmargillic B horizon