Reference soil Kenya 56: Vertisol

KE056

Vertisols occur dominantly in level landscapes under climates with a pronounced dry season. Vast areas are found in Australia, India, northeastern Africa (Sudan, Ethiopia), southern Latin America and the USA.

Characteristics

Soils having a vertic horizon (a clayey subsurface horizon with polished and grooved ped surfaces ("slickensides") or wedge-shaped or parallelepiped structural aggregates) within 100 cm from the soil surface. They have 30 percent or more clay in all horizons to a depth of 100 cm or more, or to a contrasting layer (lithic or paralithic contact, petrocalcic, petroduric or petrogypsic horizons, sedimentary discontinuity, etc.) between 50 and 100 cm, after the upper 20 cm have been mixed. In addition, Vertisols exhibit wide cracks, which open and close periodically.

Distribution of Vertisols (rough estimation supplied by soilgrids)

 

Reference soil KE056: Vertisols

Little soil fauna activity. The vegetation is cut over for charcoal production. Slides: 10,181 - 10,182 and 10,184 - 10,190.

 

Classification

WRB 2006WRB 1998
Haplic- Vertisol (Calcaric Hyposodic)Hyposodic- Vertisol
10-26 cmargic horizon
26-100 cmvertic horizon
-vertic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Calcari-Eutric Vertisol skeleticChromic Vertisol sodic
0-10 cmochric A horizon
10-100 cmargic B horizon
-calcaric
-slickensides
0-10 cmochric A horizon
10-100 cmargillic B horizon
-gilgai microrelief
-slickensides