Reference soil Indonesia 29: Andosol
The original forest has been cleared, at present fallow land with abundant ferns. At some distance of site low level arable farming, mainly horticulture. All horizons have clearly a low bulk density. In the BA horizon the soil colours change gradually from the colours of the A and the B horizon. From 80 to 108 the profile consists of a serise of thin horizons which are influenced by redox processes. It has been described as Bs(80-90) and Bg?(90-108) horizons. The Bg? itself can be subdivided in very thin layers: Bg(90-100) 10YR4/4, clay loam, Bh(100-103) 5YR2.5/2, loamy sand (buried A horizon?) and Bs(103-108) 2.5YR4/8, loamy sand. The sequence of these thin layers varies locally, its genesis is not clear. Roots are concentrated in coarse channels in the Bg and C horizons. The C horizons have a sandy texture, the sand consists mainly of translucent fragments, probably volcanic glass. Penetrometer readings: A 1.6, BA 1.0, Bw 2.6, Bs 3.0-5.0, Bg 1.8, C 2.0, and Cr 5 or more kg/cm2.
WRB 2006:
Folic Silandic Andosol(Acroxic Hyperdystric) | |
0-16 cm | folic horizon |
16-79 cm | cambic horizon |
andic properties |
FAO-UNESCO-ISRIC 1988: |
FAO-UNESCO 1974: |
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Other classification
USDA-NRCS (1999) |
Acrudoxic Ultic | Hapludand |
USDA-SCS (1975) |
Acrudoxic Ultic | Dystrandept | medial | isohyperthermic |
Classification (other) |
Podsolik Coklat |
Deep, well drained, dark yellowish brown, clay loam. Very dark coloured humus rich topsoil, the brown subsoil is thixotrophe, the light coloured tuff subsoil starts at about 90 cm. |
Sumatra, Taput, Harian Boho, 2.1km W of Tele (west side bridge left)