Reference soil Kenya 02: Andosol

KE002

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 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.

 

Classification

WRB 2006WRB 1998
Mollic-Silandic-Vitric- Andosol (Calcaric Siltic)Molli-Vitric- Andosol (Calcaric)
0-41 cmmollic horizon
0-49calcaric
0-75vitric
75-140andic
0-41 cmmollic horizon
0-41 cmvitric horizon
75-140 cmandic horizon
0-41calcaric
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Silti-Mollic AndosolMollic Andosol
0-41 cmmollic A horizon
0-140andic / strongly humic
0-41 cmmollic A horizon
-exchange complex dominated by amorphous material