Reference soil Cuba 12: Ferralsol

CU012

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 CU012: Ferralsols

Short field description: Very deep, well drained, strong brown, clay loam. Well structured, with diffuse boundaries, porous ferromanganese concretions. Geology: Jurasic higher, oxfordiano and tithoniano: limestones, marbles. Geomorphology: tectonic-lithological low mountain. The monolith was taken in a small area (40 cm x 40 cm), surrounded by coffee and degraded forest.

 

Classification

WRB 2006WRB 1998
Pisoplinthic- Ferralsol (Epidystric Xanthic)Xanthic- Ferralsol
21-160 cmferralic horizon
48-160 cmpisoplinthic horizon
0-48 cmochric horizon
48-160 cmferralic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Xanthi-Ferralic Cambisol skeleticXanthic Ferralsol petric
0-48 cmochric A horizon
48-160 cmcambic B horizon
- cmcambic B horizon
- cmochric A horizon
-ferralic
0-48 cmochric A horizon
48-160 cmoxic B horizon
-ferralic
-weatherable minerals

 

Local classification:Ferralitico rojo amarillo lix.