Reference soil Kenya 66: Vertisol

KE066

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 KE066: Vertisols

The profile is an intergrade towards a vertic cambisol. No tuff in situ appears! Acacia drenpanolobium is a typical Vertisol shrub. Slides: 10,242 - 10,247.

 

Classification

WRB 2006WRB 1998
calcic horizon- Vertisol (Pellic)Pelli-calcic horizon- Vertisol
15-64 cmvertic horizon
-secondary carbonates
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Calcic Vertisol gilgaiPellic Vertisol
0-15 cmochric A horizon
15-64 cmcambic B horizon
-slickensides
-soft powdery lime
0-15 cmochric A horizon
15-64 cmcambic B horizon
-gilgai microrelief
-slickensides