Reference soil South Africa 20: Umbrisol

ZA020

Umbrisols occur mainly in regions where precipitation exceeds considerably the evapotranspiration. They are dominantly associated with acid parent materials.

Characteristics

Soils having an umbric horizon (deep, brownish or blackish surface horizon with a significant accumulation of organic matter and low base saturation). They have no diagnostic horizons other than an anthropedogenic horizon less than 50 cm thick, or an albic or cambic horizon.

Distribution of Umbrisols (rough estimation supplied by soilgrids)

 

Reference soil ZA020: Umbrisols

Umbrisol

 

Classification

WRB 2006WRB 1998
Ferralic- Umbrisol (Humic Hyperdystric Clayic Chromic)Humic- Umbrisol
0-37 cmumbric horizon
-ferralic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Ferrali-Humic CambisolHumic Cambisol
0-37 cmumbric A horizon
-ferralic
0-37 cmumbric A horizon
-ferralic

 

Local classification:Hutton Form, Lillieburn Family