Reference soil Brazil 21: Luvisol

BR021

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 BR021: Luvisols

Moderately deep, well drained, brown clay soil derived from gneiss; topsoil in sandy loam, transition to weathered gneiss at 70cm depth. C-horizon: multicoloured banded rotten gneissrock. Stones at the soil surface and in the CB-horizon are rounded quartz stones with a desert varnish. Soil moisture regime is ustic bordering to Aridic. Landscape: moderately dissected denudational plain with a few inselbergs. Vegetation (Brasilian name): Caatinga Hiperxerofolia. Land use: near the site some arable farming, maize, cotton with supplementary irrigation. Additional information: SNLCS-Embrapa Boletim tecnico no 15. Slides no 9832, 9833.

 

Classification

WRB 2006WRB 1998
Haplic- Luvisol (Hypereutric Clayic Chromic)Chromic- Luvisol
27-70 cmargic horizon
0-27 cmochric horizon
27-70 cmargic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Chromic LuvisolChromic Luvisol
0-27 cmochric A horizon
27-70 cmargic B horizon
- cmargic B horizon
0-27 cmochric A horizon
27-70 cmargillic B horizon

 

Local classification:Bruno não cálcico