Reference soil Kenya 02: 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 KE002: Andosols
A dark volcanic soil (turning to dark brown/dark reddish brown in Bb horizons) with common very fine pores below 17 cm, with a texture changing from silt loam to silty clay loam in 3 lower horizons. Due to its very high CEC (72) and its high percentage of nutrients and organic matter the soil can be considered very suitable for agricultural use.