Reference soil Zambia 04: Ferralsol

ZM004

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 ZM004: Ferralsols

REFERENCES: Van Sleen L.A., 1978. Detailed soil survey of the Uningi seed potato area (and two soils studied in Kleynhans' farm), Northern Province. Soil Survey Report no. 60, Soil Survey Unit, Kasama. (profile K-1, p. 27-28, and Appendix 4, Brief petrographic description of rock sample K-1). PARENT MATERIAL: brief petrographic description of rock sample K-1: Dolerite. A typical fine grained ophitic texture of augite and labradorite plagioclase - with scattered skeletal opaques. The two major minerals show retrogression in patches to amphibole and kaolinite. (Source: Laboratory report, Geological Survey Department of Zambia. 29 October 1976, by J. Tether, mineralogist).

 

Classification

WRB 2006 
Vetic- Ferralsol (Hyperdystric Clayic Rhodic) 
12-150 cmferralic horizon
 
12-150 cmferralic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Veti-Ferralic CambisolOrthic Ferralsol
0-12 cmochric A horizon
12-150 cmcambic B horizon
-ferralic
0-12 cmochric A horizon
12-150 cmoxic B horizon

 

Local classification:Malashi clay