Reference soil Kenya 32: Vertisol

KE032

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 KE032: Vertisols

A deep to very deep soil, poorly to imperfectly drained, olive gray to olive cracking clay; structure is strong very coarse columnar to angular blocky. Continuous thick pressure faces are found at an angle of 45 degrees; very sticky and plastic, firm when moist and very hard when dry. Secondary CaCO3 at B2 horizon. Roots are very few to few; vegetation: accacia sp, Thespetia danis

 

Classification

WRB 2006WRB 1998
Calcic-Mazic- Vertisol (Hyposodic)Mazi-calcic horizon- Vertisol (Hyposodic)
20-120 cmvertic horizon
-secondary carbonates
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Chromi-Calcic Vertisol sodicChromic Vertisol sodic
0-40 cmochric A horizon
20-120 cmcambic B horizon
-slickensides
-vertic
0-40 cmochric A horizon
20-120 cmcambic B horizon
-slickensides
-vertic