Reference soil Colombia 13: Andosol

CO013

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 CO013: 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 ) The site is influenced by cold wet winds blowing from the "Laguna la Cocha". LAND USE AND VEGETATION: Crops grown in vicinity are Eucalyptus and Pinus. ADDITIONAL NOTES ON PROFILE DESCRIPTION: BC - the mottles occur along rootchannels Bir - placic; acts as a pan and upholds water, resulting in seepage just above the horizon.

 

Classification

WRB 2006WRB 1998
Hydric-Silandic-Epivitric- Andosol (Hyperdystric Placic Thixotropic)Sili-Vitric- Andosol (Hydric Umbrihumic)
0-30 cmfolic horizon
30-78 cmumbric horizon
-vitric
-andic
0-30 cmvitric horizon
0-30 cmfolic horizon
30-78 cmumbric horizon
30-98 cmandic horizon
-strongly humic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Placi-Umbric AndosolHumic Andosol
0-78 cmumbric A horizon
-andic
-smeary consistence
0-78 cmumbric A horizon
-exchange complex dominated by amorphous material
-smeary consistence