Reference soil Costa Rica 07: Andosol

CR007

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 CR007: Andosols

Brief soil description: Moderately deep, well drained, dark brown to brown loamy over sandy soil, well structured. On the boundary of Ah1 to Ah2 a 'panlike structure' is found altough no compaction was found. The structure can be recognized as a grey band with rust coloured edges. Abundant soil fauna: ants, earthworms, termites, jumptails, beetles. Actual classification: FAO (1988): Umbric Andosol USDA (1992): Acrudoxic Hapludand

 

Classification

WRB 2006WRB 1998
Umbric-Aluandic-Vitric- Andosol (Dystric)Pachi-Vitric- Andosol (Umbric Dystric)
0-80 cmumbric horizon
-andic
-vitric
0-80 cmandic horizon
0-80 cmumbric horizon
80-135 cmvitric horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Umbric AndosolHumic Andosol
0-80 cmumbric A horizon
-andic
0-80 cmumbric A horizon
-exchange complex dominated by amorphous material

 

Local classification:Suelo Los Diamantes