Reference soil Gabon 05: Plinthosol

GA005

Plinthosols occur mainly in the moist tropical regions in low-lying positions where iron from the soil and adjacent uplands is accumulating.

Characteristics

Soils having either a petroplinthic horizon within 50 cm from the soil surface, or a plinthic horizon which either starts within 50 cm from the soil surface, or within 100 cm from the soil surface if it underlies an albic horizon or a horizon with stagnic properties.

Distribution of Plinthosols (rough estimation supplied by soilgrids)

 

Reference soil GA005: Plinthosols

A well drained deep soil (125-180cm) on an erosional plain between two ridges (closed basin in karst landscape). The land is used for hunting and is burnt anually. There are charcoal fragments in upper horizon and about 10 % of organic matter in Bcs. With increasing depth the amount of ironstone (goethite) becomes dominant (up to stone and boulder size); vegetation: immenocardia; additional climatic information: insolation (hours).

 

Classification

WRB 2006WRB 1998
Acric-Pisoplinthic- Plinthosol (Hyperdystric Clayic)Hyperdystri-Pisoplinthic- Acrisol
25-100 cmargic horizon
50-100 cmpisoplinthic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Ferric Acrisol skeleticXanthic Ferralsol petric
0-22 cmochric A horizon
22-100 cmargic B horizon
0-22 cmochric A horizon
22-100 cmoxic B horizon

 

Local classification:Sol ferrallitique jaune, fortement désaturé