Reference soil Indonesia 18: Andosol

ID018

Andosols occur throughout the world where volcanic activity is common, especially in the circum-Pacific region and along the mid-Atlantic Ridge.

Characteristics

Soils with a vitric or andic horizon (slightly to moderately weathered horizons in pyroclastic deposits dominated by short-range-order minerals, notably allophane and imogolite) starting within 25 cm from the soil surface. In addition, they may have a histic, fulvic, melanic, mollic, umbric, ochric, duric, or cambic horizon. Other diagnostic horizons (unless buried deeper than 50 cm by volcanic deposits) are absent.

Distribution of Andosols (rough estimation supplied by soilgrids)

 

Reference soil ID018: Andosols

PARENT MATERIAL: Intermediate (andesitic) volcanic ash strata (0-37 and 37-110 cm) over moderately weathered volcanic tuff (110+ cm). LAND USE AND VEGETATION: Coffee plantation (C. robusta) with Citrus spp. as shade trees. Remnants of primary forest in valleys and at remote places. REFERENCES: - Buurman, P. & De Vos, J.H., 1984. Land Evaluation for Agricultural Use of Aceh Utara and Aceh Tengah (DPA III), Sumatra, Indonesia. International Institute for Aerial Survey and Earth Sciences (ITC), Enschede, The Netherlands.

 

Classification

WRB 2006 
Umbric-Silandic- Andosol (Dystric Thixotropic Siltic) 
0-37 cmumbric horizon
48-125 cmcambic horizon
-andic
 
0-37 cmumbric horizon
48-125 cmcambic horizon
-andic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Humi-Umbric AndosolHumic Andosol
0-37 cmumbric A horizon
48-125 cmcambic B horizon
-andic
-smeary consistence
0-37 cmumbric A horizon
48-125 cmcambic B horizon
-exchange complex dominated by amorphous material

 

Local classification:Andosol Humik (PPT-Bogor 1981)