Reference soil Kenya 34: Andosol

KE034

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 KE034: Andosols

The spot around the pit is cultivated with maize, beans and partly abondoned (fallow?) with grasses and bushes, conspicuously with ferns. Also pyrethrum is grown. Even in the Bu1 horizon few carbonized materials are seen, suggesting some disturbances. Rootings frequent to the bottom of BA. Geology: basalt, basaltic conglomerates and volcanic ash. Climate: Rel. Hum.(%) - relative humidity 0600 GMT, first row Rel. Hum.(%) - relative humidity 1200 GMT, second row Slides: 10248 - 10251, Landscape, profile, landuse. Literature: Oswago, O. 1975. Soils of the Gituamba Experimental Farm, Soil Unit, NAL, Nairobi. Hirose, S. ed.1987. Agriculture and Soils in Kenya. Nihon University, Tokyo, Japan. Chapter B1, B2, B3, page 88 - 129.

 

Classification

WRB 2006WRB 1998
Silandic-Aluandic- Andosol (Hyperdystric)Hyperdystri-Silic- Andosol
16-130 cmcambic horizon
-andic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Humi-Haplic AndosolOchric Andosol
0-16 cmochric A horizon
16-130 cmcambic B horizon
-andic
-strongly humic
0-16 cmochric A horizon
16-130 cmcambic B horizon
-exchange complex dominated by amorphous material
-high organic matter content in B horizon