Reference soil Nicaragua 08: Andosol

NI008

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 NI008: Andosols

Deep, well drained, (dark) reddish brown clay to silty clay soil developed from alluvium, derived from consolidated pyroclastic materials. The soil contains few pyroclastic fragments, is friable, strongly to moderately structured, moderately to slowly permeable and moderately porous. This well developed soil shows differentiation in color and texture (illuvial Bt horizon). The profile forms part of the NIC05 to NIC09 toposequence. NIC08 ("red soils") and NIC09 ("black soils") are both found at short distances in an irregular pattern, in consequence of differences in drainage conditions (well c.q. imperfectly drained).

 

Classification

WRB 2006WRB 1998
Mollic-Vitric- Andosol (Clayic)Molli-Vitric- Andosol
0-33 cmmollic horizon
33-75 cmcambic horizon
-vertic
-vitric
0-116 cmvitric horizon
0-33 cmmollic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Andi-Haplic PhaeozemHaplic Phaeozem
0-33 cmmollic A horizon
15-75 cmcambic B horizon
- cmargic B horizon
- cmochric A horizon
0-33 cmmollic A horizon
15-75 cmcambic B horizon
- cmargillic B horizon
- cmochric A horizon