Reference soil Spain 03: Vertisol

ES003

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 ES003: Vertisols

Short field description: Deep imperfectly drained uniform reddish-brown clayey soil; Structure is strong angular blocky showing prominent slickenslides and wedgeshaped aggregates between 25-95 cm.. Deep wide cracks occur during dry season, and continu down to 90 cm, still being some 2 cm wide at 50 cm depth. * undulating landscape. ** observed watertable deeper than 150 cm.

 

Classification

WRB 2014 
Vertisol 
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Stagni-Calcic Vertisol inundicChromic Vertisol
- cmochric A horizon
-slickensides
-vertic
- cmcambic B horizon
- cmochric A horizon
-slickensides
-vertic

 

Local classification:Vertisuelo topomorfo