Reference soil Uruguay 04: Regosol
Regosols are found in areas where soil has been eroded to the extent that the underlying unconsolidated materials come near to the surface, or where soil formation has not played an important role, e.g. in desert regions. The name comes from the greek 'rhegos' :blanket meaning young soils on weathering materials.
Characteristics
Soils in medium and fine textured materials, having no distinctive horizons other than an ochric horizon at the surface.
Reference soil UY004: Regosols
DRAINAGE PATTERN: coarse dendrite DOMINANT SPECIES: trachypogon montufari, paspalum notatum, andropogon ternatus, richardia humistrata, cyperus spp., axonopus affinis, axonopus argentinus spp. MORPHOLOGY: C Weathered rock, banded with alterated black minerals on the surface of which clay (10YR6/3) is found (unlcear whether the clay is formed in situ or illuviated). Probably biotite is alterated to vermiculite. Colours (dry) also 7.5YR5/8 and 10YR7/6
Classification
WRB 2006 | WRB 1998 | ||||||||
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Epileptic- Regosol (Humic Eutric) | Humi-Epileptic- Regosol (Eutric) | ||||||||
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FAO-UNESCO-ISRIC 1988 | FAO-UNESCO-ISRIC 1974 | ||||||||
Humi-Dystric Regosol lithic | Dystric Regosol lithic | ||||||||
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Local classification: | Brunosol subéutrico háplico |