Reference soil Indonesia 36: Andosol
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.
Reference soil ID036: Andosols
PARENT MATERIAL: The soil parent material is an ash/lapilli layer of about 1 to 1.5 metre deposited on a man-made terrace. The time of deposition is unknown to the farmers of this area. LAND USE AND VEGETATION: Land use at the site is wooded fallow land with few crops like banana. Nearby site sawahs. Penetrometer readings: A 1, C2 4 to 5, B 2, C2 1.5, IIA 1.5 to 2, IIB 2 to 3 kg/cm2.