Reference soil Colombia 09: 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 CO009: Acrisols
PHYSIOGRAPHY: Local relief: 100 m. CLIMATE: Available climatic data of the Araracuara area are incomplete. The rainfall is estimated between 3000-3500 mm/year (closer to 3000 mm) with a minimum in January between 150-200 mm (closer to 150 mm). A maximum is recorded in July between 200-250 mm (closer to 250 mm). The evaporation is estimated to be about half of the precipitation, e.g. about 1600 mm/year. The relative humidity is more than 75% with a minimum in January and February. VEGETATION AND LAND USE: Area was cleared from tropical rainforest 50 years ago and was put under pasture; extensive grazing. PARENT MATERIAL: Precambrian. EROSION: Severe in places.