Reference soil Indonesia 40: Umbrisol

ID040

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 ID040: Umbrisols

PARENT MATERIAL: sapric/mucky sand, covered by peat. ADDITIONAL NOTES ON PROFILE DESCRIPTION: Ap - structure form 1 breaks into weak fine crumb to subangular blocky structure. Bw - mucky texture. C1 - very few medium roots, mucky texture. C2 - quartz.

 

Classification

WRB 2006 
Haplic- Umbrisol (Humic Hyperdystric Pachic) 
0-120 cmumbric horizon
 
0-120 cmumbric horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Pachi-Humic Cambisol phreaticHumic Cambisol phreatic
0-120 cmumbric A horizon
0-120 cmumbric A horizon

 

Local classification:Organosol Saprik