Reference soil Nicaragua 06: Andosol
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.
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.