Reference soil Democratic Republic of the Congo 02: Ferralsol
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.
Reference soil CD002: Ferralsols
WEATHER: Dry season, dry for at least two weeks. VEGETATION AND LAND USE: Hévéa from the 1930's, rejuvenated once (7 or 8 years ago). Tree rows, about 1m wide, clean, very few litter. MINERALOGY: Kaolinite, goethite, quartz. SURFACE DRAINAGE: dendritic, medium dense. ADDITIONAL NOTES ON PROFILE DESCRIPTION: O - fresh and decomposing organic matter and roots (many living). AB - cutans: matrans? - pores: also many micro to fine interstitial. B1 - cutans: bridges. - pores: also many micro to fine interstitial. - roots: also very few medium. B2 - cutans: bridges; contain iron oxides and hydroxides besides clay. B3 - cutans: bridges. Mottles from 12 to 154cm depth are possibly decomposing concretions. Structure from 12 to 94cm depth has a tendancy to porous massive; strong columnar when dry.