Reference soil South Africa 03: Umbrisol

ZA003

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 ZA003: Umbrisols

LAND USE AND VEGETATION: Forest was planted 20 years ago. Human influence: superficial soil management. ADDITIONAL NOTES ON PROFILE DESCRIPTION: R - Pinkish grey mudstone, continuous.

 

Classification

WRB 2006 
Cambic-Ferralic- Umbrisol (Humic Hyperdystric Chromic) 
0-40 cmumbric horizon
40-82 cmcambic horizon
-ferralic
 
0-40 cmumbric horizon
40-82 cmcambic horizon
-ferralic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Ferrali-Humic CambisolHumic Cambisol
0-40 cmumbric A horizon
40-82 cmcambic B horizon
0-40 cmumbric A horizon
40-82 cmcambic B horizon
-ferralic

 

Local classification:Clovelly Form