Reference soil Nicaragua 05: Andosol

NI005

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 NI005: Andosols

Shallow, young, (somewhat) excessively drained, black loamy sand soil developed from volcanic ejecta, derived from unconsolidated pyroclastic rock (ash, lapilli, volcanic bombs). The soil contains fresh pyroclastic fragments, is weakly structured, highly porous and highly erodable. At the surface an accumulation of about 2 cm of organic material is found. The densily closed natural vegetation prevents soil erosion. The profile forms part of the NIC05 to NIC09 toposequence.

 

Classification

WRB 2006WRB 1998
Mollic-Epileptic-Vitric- Andosol (Arenic)Molli-Vitric- Andosol (Epileptic)
0-30 cmmollic horizon
-continuous rock
-vitric
0-30 cmvitric horizon
0-30 cmmollic horizon
-continuous hard rock
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Molli-Vitric Andosol lithicMollic Andosol lithic
0-30 cmmollic A horizon
- cmmollic A horizon
-andic
-continuous hard rock
0-30 cmmollic A horizon
-exchange complex dominated by amorphous material