Reference soil Costa Rica 08: Ferralsol

CR008

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 CR008: Ferralsols

Brief soil description: very deep, well drained, brown clay soil, strongly acid and having a very low sum of exchangeable bases. Parent material is of fluvio-laharic origin. The original texture is not known. Composition parent material is probably andesitic. The pan has a black color and occurs at about 140cm depth. Actual classification: FAO (1988): Haplic Ferralsol USDA (1992): Andic Haploperox

 

Classification

WRB 2006WRB 1998
Haplic- Ferralsol (Alumic Clayic Rhodic)Rhodi-Alumic- Ferralsol
15-140 cmferralic horizon
0-15 cmochric horizon
15-140 cmferralic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Rhodi-Ferralic CambisolRhodic Ferralsol
0-15 cmochric A horizon
15-140 cmcambic B horizon
-ferralic
0-15 cmochric A horizon
15-140 cmoxic B horizon

 

Local classification:Suelo Neguev