Reference soil Costa Rica 12: Andosol

CR012

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 CR012: Andosols

Brief soil description: Very deep, well drained, brownish black over yellowish brown loamy soil. The upper 50 cm have a very high organic matter content. The soil has been formed in various superimposed volcanic ash deposits of the Turrialba volcano. The site has been used for many years for pasture, which has caused compaction of the upper 30 cm, as evidenced by slight mottling. At time of description, the land was being prepared for growing potatoes and later on beans, after which pasture will probably be reestablished. In the subsoil some very large pores are present, partly filled up which material from the A horizon.

 

Classification

WRB 2006WRB 1998
Umbric-Silandic- Andosol (Hyperdystric)Pachi-Silic- Andosol (Umbric Hyperdystric)
0-53 cmumbric horizon
53-150 cmcambic horizon
-andic
0-150 cmsilandic horizon
0-53 cmumbric horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Pachi-Umbric AndosolHumic Andosol
0-53 cmumbric A horizon
53-150 cmcambic B horizon
-andic
0-53 cmumbric A horizon
53-150 cmcambic B horizon
-exchange complex dominated by amorphous material
-thixotropy