Reference soil Indonesia 26: Phaeozem
Phaeozems occur all over the world, but especially on the more moist side of the steppe regions, bordering Chernozems.
Characteristics
Soils having a mollic horizon (deep, brownish or blackish surface horizon with a significant accumulation of organic matter and high base saturation); a base saturation of 50 percent or more between 25 and 100 cm from the soil surface; a calcium carbonate-free soil matrix at least to a depth of 100 cm from the soil surface, or to a contrasting layer between 25 and 100 cm; no diagnostic horizons other than an albic, argic, cambic or vertic horizon, or a petrocalcic horizon in the substratum.
Reference soil ID026: Phaeozems
PHYSIOGRAPHY: Piedmont landform at the lower northeastern slope of the Gunung Kawi volcano. Colluvial lower footslope at the transition towards Pudjon intervolcanic plain. Western valley side slope of one of the smaller tributaries of the Kali Konto. PARENT MATERIAL: Thick colluvial deposits of material derived from intermediate and basic volcanic ash. HYDROLOGY: Well drained, moderately permeable, medium runoff. The soil is occasionally flooded by overland flow. LAND USE AND VEGETATION: Cultivation of rainfed annual food crops (maize, cassava, grain legumes) and vegetables on graded benched fields. Locally small stands of bamboo. Whole area is cleared of its original vergetation.
Classification
WRB 2006 | |||||||||||
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Haplic- Phaeozem | |||||||||||
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FAO-UNESCO-ISRIC 1988 | FAO-UNESCO-ISRIC 1974 | ||||||||||
Orthi-Haplic Phaeozem | Haplic Phaeozem | ||||||||||
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Local classification: | Kambisol Eutrik (PPT-Bogor, 1981) |