Reference soil Nicaragua 09: Vertisol
Vertisols occur dominantly in level landscapes under climates with a pronounced dry season. Vast areas are found in Australia, India, northeastern Africa (Sudan, Ethiopia), southern Latin America and the USA.
Characteristics
Soils having a vertic horizon (a clayey subsurface horizon with polished and grooved ped surfaces ("slickensides") or wedge-shaped or parallelepiped structural aggregates) within 100 cm from the soil surface. They have 30 percent or more clay in all horizons to a depth of 100 cm or more, or to a contrasting layer (lithic or paralithic contact, petrocalcic, petroduric or petrogypsic horizons, sedimentary discontinuity, etc.) between 50 and 100 cm, after the upper 20 cm have been mixed. In addition, Vertisols exhibit wide cracks, which open and close periodically.
Reference soil NI009: Vertisols
Moderately deep, imperfectly drained, very dark grey to black heavy clay developed from alluvium derived from tuff. The soil contains few pyroclastic fragments, is moderately to strongly structured (columnar) and moderately to slightly porous. This typical Vertisol with a very high clay content and poor internal drainage shows great problems in workability and management (central pivot irrigation system). This profile forms part of the NIC05 to NIC09 toposequence. NIC09 ("black soils") and NIC08 ("red soils") are both found at short distances in an irregular pattern, as a consequence of differences in drainage conditions (imperfectly c.q. well drained).