Reference soil Brazil 01: Lixisol

BR001
Distribution of Lixisols (rough estimation supplied by soilgrids)

Deep, moderately well drained, red clay soil derived from gneiss; having a yellowish brown, porous massive, sandy (clay) loam topsoil. The B horizons show a multicolouring aspect due to grey and brown coatings of illuvial clay from upper horizons, in the C horizons this is caused by weathering minerals. The B horizons may have a limited permeability resulting in a temporary saturation of (A and) E horizon with lateral transport of moisture towards the valley. *) Brazilian classification: Podzolico Vermelho Amarelo abrupto Tb alico. Drainage pattern: dendritic; often presence of flat depressions without clear streamlines. Vegetation coverage: 5% shrubs; 20% herbs; 50% grasses; 25% bare soil (the original vegetation was a tropical forest). Limitations in land use: a. slope too steep for mechanization. b. rootability and possibilities for tillage suboptimal. c. risk of erosion. Reference soil BR 01 is comparable to soil profiel RJ 2 II RCC.

Classification

WRB 2006

Cutanic-Vetic Lixisol (Albic Clayic Chromic)  
14-38 cm albic horizon
38-100 cm argic horizon

WRB 1998

Veti-Albic Lixisol (Abruptic Chromic)  
0-14 cm ochric horizon
14-38 cm albic horizon
38-100 cm argic horizon

FAO-UNESCO-ISRIC 1988

Chromi-Haplic Lixisol  
0-14 cm ochric A horizon
14-38 cm albic E horizon
38-100 cm argic B horizon

FAO-UNESCO-ISRIC 1974

Ferric Luvisol  
0-14 cm ochric A horizon
14-38 cm albic E horizon
38-100 cm argillic B horizon
- ferric

Local classification

Classification information Podzólico Vermelho-Amarelo abrupto Tb álico
Other classification
USDA-NRCS (1999) Typic Kanhaplustalf
USDA-SCS (1975) Typic Paleustalf ustic fine-loamy kaolinitic isohyperthermic
Location: 

Rio de Janeiro, Itaguaí