Reference soil Ecuador 03: 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.
EC03 is comparable to profile Ecuador 8 in part III: tour guide for Ecuador of the sixth international soil classification workshop (1984). The soil was redescribed and resampled by Kauffman and del Posso in April 1987; additionally two monoliths of 140cm length were taken. There are not sufficient temperature data available at the altitude of the site. When a correction of 6 degrees celsius per 1000 metre is applied on the data of Izobamba meteo station, the average annual temperature is around the limit of 8 degree celsius, hence mesic to frigid. If the frigid temperature regime is rejected the soil will key out as Dystrandept. The soil is a true volcanic ash soil except for the bulk density, which is slightly too high. If the bulk density criterion is strictly applied the soil will classify as Andic Humitropept(ST) and as humic Cambisol(FAO).
WRB 2006
Vitric Umbric Andosols (Endoskeletic ) |
0-92 | umbric horizon |
- | vitric horizon |
WRB 1998
Vitric Pachi Umbric Endoskeletic Andosols |
0-92 cm | vitric horizon |
0-92 cm | umbric horizon |
FAO-UNESCO-ISRIC 1974
Humic Andosols |
- | exchange complex dominated by amorphous material horizon |
- | smeary consistence horizon |
0-92 cm | umbric A horizon |
Local classification
Classification information | Suelo Negro Andino |
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USDA-SCS (1975) | Dystrandept udic loamy mixed isomesic |
Pinchincha, Quito, El Corazon vulcano