Reference soil Indonesia 26: Phaeozem

ID026

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.

Distribution of Phaeozems (rough estimation supplied by soilgrids)

 

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 
Haplic- Phaeozem 
0-45 cmmollic horizon
45-139 cmcambic horizon
 
0-45 cmmollic horizon
45-139 cmcambic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Haplic PhaeozemHaplic Phaeozem
0-45 cmmollic A horizon
45-139 cmcambic B horizon
0-45 cmmollic A horizon
45-139 cmcambic B horizon

 

Local classification:Kambisol Eutrik (PPT-Bogor, 1981)