Reference soil Colombia 14: Andosol

CO014

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.

Distribution of Andosols (rough estimation supplied by soilgrids)

 

Reference soil CO014: Andosols

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 ) PARENT MATERIAL: Partly consolidated volcanic ejecta of Quaternary age;

 

Classification

WRB 2006WRB 1998
Umbric-Hydric-Silandic- Andosol (Hyperdystric)Hydri-Silic- Andosol (Umbrihumic Hyperdystric)
0-68 cmumbric horizon
0-150 cmandic horizon
0-68 cmumbric horizon
-strongly humic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Pachi-Umbric AndosolHumic Andosol
0-68 cmumbric A horizon
- cmumbric A horizon
-andic
-strongly humic
0-68 cmumbric A horizon
-exchange complex dominated by amorphous material