Reference soil Brazil 14: Ferralsol

BR014

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 BR014: Ferralsols

Brief field description: Very deep, well drained, dusky red clay; weakly coherent porous massive subsoil. Infillings from deeper substrata are common in Bw1, caused by biological activity. Colour of the infillings 1.25 YR 4/6 to 8. Consistency Ah1, Ah2, AB is soft to slightly hard. The AB horizon from 20-38 cm shows relatively a much lower porosity than over- and underlying horizons. Physiography:*= very broad open V-valley. Soil aggradation: in nearby soil pit presence of thin layers of coarser fragments (sometimes lateritic) shows the colluvial processes. Photographs/slides no 9795-9798 *) Brazilian classification: Latossolo Vermelho-Escuro Distrofico.

 

Classification

WRB 2006WRB 1998
Vetic- Ferralsol (Humic Alumic Clayic)Veti-Humic- Ferralsol (Alumic Rhodic)
20-470 cmferralic horizon
0-38 cmochric horizon
20-470 cmferralic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Alumi-Rhodic FerralsolRhodic Ferralsol cerrado
0-38 cmochric A horizon
20-470 cmferralic B horizon
- cmferralic B horizon
0-38 cmochric A horizon
20-470 cmoxic B horizon

 

Local classification:Latossolo Vermelho-Escuro álico