Reference soil Kenya 39: Andosol

KE039

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 KE039: Andosols

In the profile is at 75cm a stoneline of weathered lapilli. Slides: 10.010 - 10.014 of profile, vegetation and site. The former crater appears as an "vlei" along the road a bit further on the track.

 

Classification

WRB 2006WRB 1998
Silandic- Andosol (Hyperdystric Siltic Novic)Hyperdystri-Silic- Andosol
8-113 cmcambic horizon
-andic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Humi-Haplic AndosolOchric Andosol
0-8 cmochric A horizon
8-113 cmcambic B horizon
-andic
-strongly humic
0-8 cmochric A horizon
8-113 cmcambic B horizon
-exchange complex dominated by amorphous material