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 2006WRB 1998
Endoleptic-Cutanic- Luvisol (Clayic)Cutani-Endoleptic- Luvisol
23-55 cmargic horizon
-continuous rock
0-23 cmochric horizon
23-55 cmargic horizon
-continuous hard rock
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Haplic Luvisol lithicOrthic Luvisol lithic
0-23 cmochric A horizon
23-55 cmargic B horizon
-continuous hard rock
0-23 cmochric A horizon

 

Local classification:Brunosol subéutrico lúvico ArFr