Reference soil Gabon 01: Ferralsol

GA001

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 GA001: Ferralsols

A deep rooting (>180 cm) soil with many fine pores, derived from precambrian metamorphites (Leptynite); mineralogical features: kaolinite and goethite. Site situated in primary tropical forest with irregular forest floor and high biological activities (termites, earthworms, insects) and a thin (5mm) layer of decomposing litter. In the lower parts of the profile iron concretions appear; additional climate data: insolation (h).

 

Classification

WRB 2006WRB 1998
Haplic- Ferralsol (Hyperdystric Clayic Xanthic)Xanthi-Hyperdystric- Ferralsol
7-300 cmferralic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Dystri-Xanthic FerralsolXanthic Ferralsol
0-20 cmochric A horizon
7-300 cmferralic B horizon
0-20 cmochric A horizon
7-300 cmoxic B horizon

 

Local classification:Sol ferrallitique jaune, fortement désaturé, typique