Reference soil Indonesia 11: Andosol

ID011

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 ID011: Andosols

LOCATION: In enclosure for weather station and pumphouse. LAND USE: at site grass, in the surroundings intensive vegetable production such as beans, cabbages, onions, carrots, corn, potatoes, etc. ADDITIONAL NOTES ON PROFILE DESCRIPTION: A11b - also many fine interstitial pores; A12b - also many fine interstitial pores; B2b - also many fine interstitial pores; all horizons are light weight and appear to have low bulk density. REFERENCES: - Chartres, C.J. & Van Reuler, H., 1985. Mineralogical changes with depth in a layered Andosol near Bandung, Java (Indonesia). Journal of Soil Science, vol. 36, pp 173 - 186.

 

Classification

WRB 2006 
Umbric-Hydric-Silandic- Andosol (Hyperdystric Thixotropic Siltic) 
0-162 cmumbric horizon
-andic
 
0-162 cmumbric horizon
-andic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Pachi-Umbric AndosolHumic Andosol
0-162 cmumbric A horizon
-andic
0-162 cmumbric A horizon
-exchange complex dominated by amorphous material