Reference soil France 02: Umbrisol

FR002

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)
Leaflet | ISRIC

 

Reference soil FR002: Umbrisols

LOCATION: Maps - Topographical map 1:25000; sheet Gérardmer No. 7-8 map coordinates: 358 N/ 951.5 E PARENT MATERIAL: Biotite granite (Acc. geol. map of France, scale 1:80000; sheet 85, ed.1939: Y1a, granite and biotite, poor on muscovite, also porphyroides and locally amphiboles). VEGETATION: coverage(%) trees 75 herbs & grasses 95

 

Classification

WRB 2006WRB 1998
Cambic- Umbrisol (Humic Alumic Chromic)Humic- Umbrisol
1-23 cmumbric horizon
23-66 cmcambic horizon
1-23 cmumbric horizon
23-66 cmcambic horizon
-strongly humic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Alumi-Humic CambisolHumic Cambisol
1-23 cmumbric A horizon
23-66 cmcambic B horizon
-strongly humic
1-23 cmumbric A horizon
23-66 cmcambic B horizon

 

Local classification:Sol ocre podzolique