Reference soil Colombia 06: Alisol
Alisols occur in the tropics and subtropics, and in the warm temperate regions of the world in relatively young landscapes. The high level of exchangeable aluminium in these soils is caused by rapid weathering of secondary high-activity clays such as vermiculite and smectite.
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 24 cmolc per kg clay or more, and which starts either 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 "alic" properties (high content of exchangeable aluminium) in the major part between 25 and 100 cm from the soil surface; moreover, only such diagnostic horizons as an ochric, albic, andic, ferric, nitic, plinthic, or vertic horizon are present.
Reference soil CO006: Alisols
PARENT MATERIAL: Tertiary unconsolidated sedimentary and volcanic rock. VEGETATION AND LAND USE: Tropical rainforest (bosque bajo, poco desarrollado sobre terrases con mal drenaje, presencia de cauces abandonados, sotobosque muy denso con abundancia de palmas, PRORADAM, 1979); at the end of the trail an area of about 100 ha has been cleared for cultivation. ADDITIONAL NOTES ON PROFILE DESCRIPTION: Bw2 - concretions: lithorelicts. BC1 - concretions: lithorelicts.