Reference soil Kenya 38: Andosol

KE038

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 KE038: Andosols

Brief soil description: Very deep, well drained soil derived from volcanic ejecta; with a thick,black, slightly gravelly silty clay topsoil over a dark yellowish brown to dark brown, silty clay subsoil which has continuous clay cutans. The soil is under natural vegetation with bamboo-hagiena forest. Parent material 1. 0 - 37 silty, 2. 37 - 53 sandy, 3. 53 - 130 silty, in the lower part lapilli occur, 4. 130 - + silty and stony. The profile observed is a roadcut, situated in Meru district. Slides of profile, vegetation and landscape: 10.005 - 10.009. Literature: Hirose S. ed. 1987. Agriculture and soils in Kenya. Nihon University, Tokyo, Japan. Chapter B1, B2, B3, page 88 - 129.

 

Classification

WRB 2006WRB 1998
Umbric-Silandic-Vitric- Andosol (Hyperdystric Siltic)Sili-Vitric- Andosol (Umbric Dystric)
0-39 cmumbric horizon
-andic
-vitric
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Humi-Umbric AndosolHumic Andosol
0-39 cmumbric A horizon
-andic
-strongly humic
0-39 cmumbric A horizon
-exchange complex dominated by amorphous material