Reference soil Kenya 37: Andosol

KE037

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 KE037: Andosols

A very dark (10 YR 2/2 very dark brown to 10 YR 2/1 black) clayey-loamy soil of volcanic origin (tertiary volcanics covered by volcanic ashes) in a mountainous region with long steep slopes; a sticky and plastic consistence with many fine and medium pores throughout the profile.

 

Classification

WRB 2006WRB 1998
Mollic-Vitric- Andosol (Calcaric)Molli-Vitric- Andosol (Calcaric)
30-120 cmcambic horizon
-calcaric
-vitric
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Molli-Vitric AndosolMollic Andosol
0-30 cmmollic A horizon
30-120 cmcambic B horizon
-andic
-strongly humic
0-28 cmmollic A horizon
30-120 cmcambic B horizon
-exchange complex dominated by amorphous material