Reference soil Costa Rica 05: Andosol

CR005

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 CR005: Andosols

presence of cutans is not so convincing. Clay mineralogy: halloysite is a mixture of 0.7 and 1.0 nm material.

 

Classification

WRB 2006WRB 1998
Gleyic-Vitric- Andosol (Hypereutric Siltic)Humi-Vitric- Gleysol (Hypereutric)
7-106 cmcambic horizon
-gleyic colour pattern
-reducing conditions
-vitric
0-7 cmochric horizon
17-106 cmvitric horizon
7-106 cmcambic horizon
-strongly humic
-gleyic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Humi-Andic Gleysol inundicEutric Gleysol phreatic
0-7 cmochric A horizon
7-106 cmcambic B horizon
-andic
-strongly humic
0-7 cmochric A horizon
7-106 cmcambic B horizon
-hydromorphic