Reference soil Spain 18: Vertisol

ES018

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 ES018: Vertisols

The profile consists of two parts: a colluvial upper part which merges via a transitional zone (at 52 cm) into a red clay. The colluvial part shows a yellowish red, fine textured surface soil, overlying a dark reddish brown, fine textured sub soil with moderate structure and showing many intersecting slickensides. A soft calcic horizon, which includes many clay nodules and occasional slickensides, forms the upper part of the red clay. At a depth of 115 cm it changes in a heavy, well structured clay with gley phenomena and prominent slickensides.

 

Classification

WRB 2014 
Vertisol 
FAO-UNESCO-ISRIC 1974 
Chromic Vertisol  
  
- cmcalcic horizon
- cmochric A horizon
-slickensides
-weatherable minerals