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 | |||||||
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Haplic- Umbrisol (Humic Hyperdystric Pachic) | |||||||
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FAO-UNESCO-ISRIC 1988 | FAO-UNESCO-ISRIC 1974 | ||||||
Pachi-Humic Cambisol phreatic | Humic Cambisol phreatic | ||||||
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Local classification: | Organosol Saprik |