Reference soil Cuba 07: Ferralsol

CU007

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 CU007: Ferralsols

Short field description: Very deep, well drained, red clay. Well structured, with small iron concretions. Geology: Neogene Era. mid-higher Miocene. Guines Formation: clays, marl, limestones and dolomitic. Geomorphology: marine plains, abrasive and accumulative abrasive, undulated and nearly plain.

 

Classification

WRB 2006WRB 1998
Haplic- Ferralsol (Hypereutric Clayic)Hypereutric- Ferralsol
16-150 cmferralic horizon
0-16 cmochric horizon
16-150 cmferralic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Eutri-Haplic FerralsolOrthic Ferralsol
0-16 cmochric A horizon
16-150 cmferralic B horizon
- cmferralic B horizon
- cmochric A horizon
0-16 cmochric A horizon
16-150 cmoxic B horizon

 

Local classification:Ferralitico rojo tipico