Reference soil Uruguay 03: Luvisol
UY003
Luvisols occur mainly in temperate regions, particularly in areas with a Mediterranean-type of climate.
Characteristics
Soils having an argic horizon (a subsurface horizon with a distinct higher clay content than the overlying horizon) with a cation exchange capacity equal to or more than 24 cmolc per kg clay throughout.
Distribution of Luvisols (rough estimation supplied by soilgrids)
Reference soil UY003: Luvisols
HYDROLOGY: Moisture conditions: Deeper than 23 cm more wet. MORPHOLOGY: B2 10YR3/6-mottles are bigger and have orange boundaries at the bottom of the horizon C colour also 2.5YR5/8 and 5YR5/8 (both dry) pedotubules of organic matter abundant ferrogenous and quartzic concretions as well as contretions with black minerals and vermiculite
Classification
WRB 2006 | WRB 1998 | ||||||||||||
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Endoleptic-Cutanic- Luvisol (Clayic) | Cutani-Endoleptic- Luvisol | ||||||||||||
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FAO-UNESCO-ISRIC 1988 | FAO-UNESCO-ISRIC 1974 | ||||||||||||
Orthi-Haplic Luvisol lithic | Orthic Luvisol lithic | ||||||||||||
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Local classification: | Brunosol subéutrico lúvico ArFr |