Reference soil Colombia 12: Andosol
Andosols occur throughout the world where volcanic activity is common, especially in the circum-Pacific region and along the mid-Atlantic Ridge.
Characteristics
Soils with a vitric or andic horizon (slightly to moderately weathered horizons in pyroclastic deposits dominated by short-range-order minerals, notably allophane and imogolite) starting within 25 cm from the soil surface. In addition, they may have a histic, fulvic, melanic, mollic, umbric, ochric, duric, or cambic horizon. Other diagnostic horizons (unless buried deeper than 50 cm by volcanic deposits) are absent.
Reference soil CO012: Andosols
PARENT ROCK: Ejecta of Galeras volcano. CLIMATE: The climate may vary considerably over short distances because of varied topography. Calhoen (1971) gives the following information on general climate variations in the Pasto area: altitude (m) rainfall (mm) temperature (Celsius) 3100 9-12 2750 781 13 2670 700 13 1400 1392 20 ( 0 2849 26 ) VEGETATION AND LAND USE: In the surroundings also maize, potatoes, onions, Eucalyptus and Pinus. The original vegetation (bosque humido montano (secco) bayo) has been cleared. ADDITIONAL NOTES ON PROFILE DESCRIPTION: Ah1 - reaction to NaF = 10; also many coarse roots; Ah2 - mottles occur along rootchannels; also many coarse roots; reaction to NaF = 10; lower boundary in places clear; AC - reaction to NaF = 10; C1 - reaction to NaF = 9.8; C2 - depth C2 may attain 15 m; little evidence of fauna activity in the soil; some tubules; pH relatively high because of lower elevation, less rain and higher temperature; * volcanic glass determination is preliminary and needs minerological confirmation, the term is used to describe the quantity of visible minerals in the soil in general.