Reference soil Brazil 09: Ferralsol

BR009

Ferralsols occur in tropical and subtropical regions of the world, mainly on old and stable land surfaces.

Characteristics

Soils having a ferralic horizon (strongly weathered horizon with low-activity clays and very low amounts of weatherable minerals) between 25 and 200 cm from the soil surface. They lack a nitic horizon (a horizon with strongly developed, nut-shaped structure) and do not have a layer which fulfils the requirements of an argic horizon and which has, in the upper 30 cm, 10 percent or more water-dispersible clay.

Distribution of Ferralsols (rough estimation supplied by soilgrids)

 

Reference soil BR009: Ferralsols

Brief field description: Very deep, well drained, dark brown clay soil derived from basalt. The soil has a high organic matter content. From 50-100 cm depth onwards clay nodules (0.5-2 cm) of irregular shape, and white chalcedon in irregular concentric form. The soil is formed in saprolite of basalt of the 'Serra Geral' formation, Jurassic/Cretaceous. Soil cracks considerably when drying out. *) Brazilian classification: Latossolo Bruno Humico Distrofico. Reference soil BR 09 is comparable to soil profile 12 III RCC.

 

Classification

WRB 2006WRB 1998
Umbric- Ferralsol (Humic Alumic Clayic)Alumi-Umbrihumic- Ferralsol (Rhodic)
0-41 cmumbric horizon
16-250 cmferralic horizon
0-41 cmumbric horizon
16-250 cmferralic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Alumi-Humic FerralsolHumic Ferralsol
0-41 cmumbric A horizon
16-250 cmferralic B horizon
0-41 cmumbric A horizon
16-250 cmoxic B horizon

 

Local classification:Latossolo Bruno Húmico distrófico