Reference soil Ecuador 18: Andosol

EC018

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 EC018: Andosols

EC18 is comparable to profile Ecuador 1 in part III: tour guide for Ecuador of the sixth international soil classification workshop (1984). The profile has been resampled in Mau 1987 by G.del Posso, additionally two monoliths of 140cm length has been taken. The gravelly ash/pumice layer hampers rootdevelopment, however a few roots are visible below the gravel layer, hence effective soil depth is somewhat deeper than 75cm. The soil horizon just above the gravel layer has compacted, probably due to tillage practices.

 

Classification

WRB 2006WRB 1998
Mollic-Vitric- Andosol (Eutric)Pachi-Vitric- Andosol (Mollic Eutric)
0-73 cmmollic horizon
-vitric
0-73 cmmollic horizon
19-73 cmvitric horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Molli-Vitric AndosolMollic Andosol
0-73 cmmollic A horizon
-andic
0-73 cmmollic A horizon
-exchange complex dominated by amorphous material

 

Local classification:Suelo negro andino