Reference soil Costa Rica 11: Andosol

CR011

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 CR011: Andosols

influenced by volcanic ashes. However, the first 35cm of the topsoil is strongly deviating from the buried A horizon, the latter having more convincing andic properties. High biological activity throughout the soil. Actual classification: FAO (1988): Umbric Andosol Soil Taxonomy (1992):Acrudoxic Melanudand

 

Classification

WRB 2006WRB 1998
Vitric- Andosol (Hyperdystric)Hyperdystri-Vitric- Andosol
25-56 cmcambic horizon
-vitric
0-25 cmochric horizon
25-113 cmvitric horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Haplic AndosolVitric Andosol
0-25 cmochric A horizon
25-56 cmcambic B horizon
-andic
0-25 cmochric A horizon
25-56 cmcambic B horizon
-exchange complex dominated by amorphous material
-thixotropy
-weatherable minerals

 

Local classification:Suelo Montelimar