Reference soil Kenya 41: Acrisol

KE041

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 KE041: Acrisols

The site shall be cleared within a year and used for crops like bananas, taro/yam, vegetables. The edge of the forest is shifted 100m mountain upwards (political decision, 1985). The actual groundwater level is below 120cm. Slides: 10,015, 10,016 and 10,023 - 10,029, profile, landscape and landuse.

 

Classification

WRB 2006WRB 1998
Cutanic- Acrisol (Humic Epieutric Clayic Chromic)Chromi-Humic- Acrisol
12-120 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Humi-Haplic Acrisol phreaticHumic Acrisol phreatic
0-12 cmochric A horizon
12-120 cmargic B horizon
-strongly humic
0-12 cmochric A horizon
12-120 cmargillic B horizon
-high organic matter content in B horizon