Reference soil South Africa 02: Ferralsol

ZA002

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 ZA002: Ferralsols

PARENT MATERIAL: Possibly with admixture of sandy material from Dwyka Glacial till.

 

Classification

WRB 2006 
Umbric-Posic-Gibbsic- Ferralsol (Humic Hyperdystric Clayic Chromic) 
75-125 cmferralic horizon
-geric
 
75-125 cmferralic horizon
-geric
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Ferrali-Humic CambisolHumic Ferralsol
0-30 cmumbric A horizon
30-120 cmcambic B horizon
-ferralic
0-30 cmumbric A horizon
30-75 cmcambic B horizon
75-120 cmoxic B horizon
-high organic matter content in B horizon

 

Local classification:Griffin Form, Woodstock Family