Reference soil Kenya 42: Acrisol

KE042

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 KE042: Acrisols

Moderately deep, moderately well drained soil derived from volcanic breccia; with a thin, reddish brown, clay topsoil over a reddish brown, clay subsoil with a very gravelly layer between 50 and 60 cm. The soil is used for arable farming with bananas, taro and yams as main crops. The site is situated at the edge of the forest and arable land. At 80 cm depth mainly rounded stones and boulders occur. Slides: 10,015 - 10,016 and 10,030 - 10,034.

 

Classification

WRB 2006WRB 1998
Cutanic- Acrisol (Ruptic Humic Clayic Chromic)Chromi-Humic- Acrisol
15-50 cmargic horizon
-abrupt textural change
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Humi-Haplic Acrisol phreaticHumic Acrisol phreatic
0-15 cmochric A horizon
15-50 cmargic B horizon
-strongly humic
0-15 cmochric A horizon
15-50 cmargillic B horizon
-high organic matter content in B horizon