Reference soil Gabon 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 GA003: Acrisols
A well drained, deep rooting soil (125-180 cm), derived from precambrian material (schists and sanstone) that varies considerably in composition. On the surface there is a micro-relief of earthworm heaps (2 cm); in the B horizons common reddish yellowish to yellowish mottles appear. Particles of parent material can be found in Ah2, Bns and BC. Apart from patchy clay-iron cutans, clay-humus cutans and humus cutans cann be found in Bws and Bns. In these horizons there are tongues of organic material, filled in the space between the structural elements. The land is savannah, used for hunting and is mainly consisting of herbs and grasses with spots of dense forest; vegetation: pobeguinea sp., hymenocardia acida, palmyra sp.; additional climate data: insolation (h).