Reference soil Cuba 05: Ferralsol

CU005

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 CU005: Ferralsols

Short field description: Very deep, well drained, red clay. Diffuse horizon boundaries and moderately structured. From 3 meter starts the hard rock. The profile was studied and sampled after a heavy rainy season, which ended about 10 days ago. Geology: mid-low Miocene, Neogene Era. Guines Formation: biogenous limestone, detritic, dolomitics. Geomorphology: marine plain, abrasive and accumulative abrasive, slightly undulated and plain.

 

Classification

WRB 2006WRB 1998
Haplic- Ferralsol (Hypereutric Clayic Rhodic)Rhodi-Hypereutric- Ferralsol
27-170 cmferralic horizon
0-27 cmochric horizon
27-170 cmferralic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Eutri-Rhodic FerralsolRhodic Ferralsol
0-27 cmochric A horizon
27-170 cmferralic B horizon
- cmferralic B horizon
- cmochric A horizon
0-27 cmochric A horizon
27-170 cmoxic B horizon

 

Local classification:Ferralitico rojo típico