Reference soil Indonesia 14: Stagnosol
Stagnosols are often related to Luvisols and occur for the greater part in humid and perhumid temperate regions in West and Central Europe, North America, Australia and Argentina.
Characteristics
Soils having within 50 cm of the soil surface reducing conditions (soil conditions with low redox potential (negative logarithm of the hydrogen potential (rH) and presence of free iron (Fe2+) on freshly broken surfaces) and in 50% of the layer a stagnic colour pattern (strong mottling of soils in such a pattern that peds surfaces are lighter (at least one Munsell value) and paler (at least one chroma) than ped interiors, which are more reddish and brighter (at least one chroma)). The stagnic color pattern develops under temporarily saturation of a perched water table from surface water, long enough to allow reducing conditions to arise. The topsoil can be bleached and concretions can occur in the subsoil. They develop often in slowly permeable, unconsolidated materials of various origins.
Reference soil ID014: Stagnosols
PHYSIOGRAPHY: Dissected upper remnants of Pudjon intervolcanic plain. Eroded upper terrace of Kali Konto and its tributaries. Single slope of 8% with human constructed level bench terraces. PARENT MATERIAL: 0-50 cm: slope wash of reworked volcanic ash of intermediate and basic composition. 50+ cm: truncated volcanic tuff profile, built up during at least two major eruption cycles. HYDROLOGY: Moderately well to well drained; moderately slow permeability due to puddled ABg-horizon; medium runoff; occasionally flooded in rainy season by overland flow. LAND USE AND VEGETATION: Cultivation of rainfed annual foodcrops (maize, cassava, grain legumes) and vegetables on level bench terraces with supplementary irrigation in the dry season. Untill recently, water supply was sufficient to grow wetland rice as well. Whole area is cleared of its natural vegetation. ADDITIONAL NOTES ON PROFILE DESCRIPTION: Ap - continuously rejuvinated by slope wash material and deposits from irrigation water. ABg - compacted with broken thin FeMn-coatings on ped faces; caused by puddling praticed in wetland rice cropping. Bg1 - manganiferous ped coatings. Bg2 - accumulation of translocated organic-rich topsoil material at the lithological discontinuity towards weathered volcanic tuff; most of the interpedal void space is completely filled with organic-rich fine material. 2Bwg - relatively high clay contents due to weathering and transformation of primary constituents. 2Bwg3 - transitional towards the little altered tuff deposits that make up the 2BC-horizon. REFERENCES: - J.L. Tersteeg, 1987: "A study on the genesis of soils derived from volcanic material in the Malang area, East Java, Indonesia".
Classification
WRB 2006 | |||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Haplic- Stagnosol (Eutric) | |||||||||||||||
| |||||||||||||||
| |||||||||||||||
FAO-UNESCO-ISRIC 1988 | FAO-UNESCO-ISRIC 1974 | ||||||||||||||
Stagni-Gleyic Cambisol | Eutric Gleysol | ||||||||||||||
|
|
Local classification: | Kambisol Eutrik (PPT-Bogor, 1981) |