Reference soil Iceland 04: Andosol

IS004

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 IS004: Andosols

Classification

WRB 2006WRB 1998
Histic-Fulvic-Silandic- Andosol (Dystric Turbic Drainic)Fulvi-Silic- Andosol (Thaptohistic Dystric)
0-55 cmfulvic horizon
60-95 cmhistic horizon
-organic
-andic
0-55 cmfulvic horizon
0-60 cmsilandic horizon
60-95 cmhistic horizon
-organic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Endohisti-Umbric AndosolHumic Andosol
0-55 cmumbric A horizon
60-95 cmhistic H horizon
-andic
0-55 cmumbric A horizon
-exchange complex dominated by amorphous material
No data for this profile