Reference soil Nicaragua 06: Andosol

NI006

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 NI006: Andosols

Deep, well drained, black to dark brown loamy to sandy loam soil developed from volcanic ejecta, derived from unconsolidated pyroclastic materials (ash, lapilli). The soil contains few manganiferous concretions, is friable, moderately structured and highly porous and permeable. A recent profile (A-Bw-C) is found upon a buried profile (2Ab-2Bb-R) derived from older pyroclastic materials. The profile forms part of the NIC05 to NIC09 toposequence.

 

Classification

WRB 2006WRB 1998
Mollic-Vitric- AndosolMolli-Vitric- Andosol
0-55 cmmollic horizon
-vitric
0-55 cmmollic horizon
0-78 cmvitric horizon
33-55 cmcambic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Molli-Vitric AndosolMollic Andosol
0-55 cmmollic A horizon
33-55 cmcambic B horizon
- cmcambic B horizon
- cmmollic A horizon
-andic
0-55 cmmollic A horizon
33-55 cmcambic B horizon
-exchange complex dominated by amorphous material

 

Local classification:Nindiri Series