Reference soil South Africa 12: Umbrisol

ZA012

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 ZA012: Umbrisols

PARENT MATERIAL: Derived from weathered paleozoic rocks: Middle Ecca Sandstone. ADDITIONAL NOTES ON PROFILE DESCRIPTION: Ah1 - top 5 cm: strong very fine subangular blocky/crumb,friable. Ah2 - mottles: soft iron concretions. B1 - plinthite; iron concretions: black; also many small and large, soft/hard, irregular and spherical, dark red (10R3/6) when broken and moist, red (7.5YR4/8) when broken and dry, iron-manganese concretions. B2 -also common strong red (7.5YR4/6, when moist) and few black mottles.

 

Classification

WRB 2006WRB 1998
Cambic- Umbrisol (Humic Hyperdystric Clayic Chromic)Humi-Umbric- Plinthosol
0-45 cmumbric horizon
45-90 cmcambic horizon
90-120 cmplinthic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Plinthi-Humic CambisolHumic Cambisol
0-45 cmumbric A horizon
45-90 cmcambic B horizon
-plinthite
0-45 cmumbric A horizon
45-90 cmcambic B horizon
-plinthite

 

Local classification:Avalon Form, Woodburn Family