Reference soil Kenya 43: Acrisol

KE043

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 KE043: Acrisols

Potterie troughout the profile from 0 - 30cm. The site is fallow land used for grazing. The valley has a natural dam of phonolite at the outlet. Slides 10,035 - 10,039.

 

Classification

WRB 2006WRB 1998
Umbric-Gleyic-Cutanic- Acrisol (Alumic Humic Hyperdystric Clayic)Umbri-Endogleyic- Acrisol (Humic Alumic)
0-60 cmumbric horizon
5-75 cmargic horizon
-reducing conditions
-gleyic colour pattern
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Umbrihumi-Gleyic Acrisol phreaticGleyic Acrisol phreatic
0-60 cmumbric A horizon
5-75 cmargic B horizon
-gleyic
-strongly humic
0-60 cmumbric A horizon
5-75 cmargillic B horizon
-high organic matter content in B horizon
-hydromorphic