Reference soil Zambia 03: Acrisol
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
Reference soil ZM003: Acrisols
FAO - medium textured - No oxic horizon because of (1) too high CEC, (2) too high water dispersible clay in subsoil. - Textural analyses indicate : Argillic B horizon. LOCATION: 2.5 km W of Kiwambe Mission along Mbala-Kiwambe road. Termite mounds average base diameter 8 m, distance 80 m; reddish colour. HUMAN INFLUENCE: Ploughing, indicated by abrupt boundary at 25 cm.