Reference soil Kenya 05: Andosol

KE005

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 KE005: Andosols

A reddish soil of volcanic ejecta with high porosity throughout the profile and a 5 cm layer (A0) of not decomposed organic matter. The texture of this well drained soil changes from silty clay to clay below 17 cm.

 

Classification

WRB 2006WRB 1998
Aluandic-Vitric- Andosol (Hyperdystric Clayic)Dystri-Vitric- Andosol
22-166 cmcambic horizon
-vitric
-andic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Humi-Vitric AndosolHumic Andosol
0-55 cmochric A horizon
17-166 cmcambic B horizon
-andic
-strongly humic
0-55 cmochric A horizon
17-166 cmcambic B horizon
-exchange complex dominated by amorphous material