Reference soil South Africa 09: Vertisol

ZA009

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 ZA009: Vertisols

BRIEF CHARACTERIZATION OF THE SOIL: A very dark brown to black clayey profile showing pronounced intersecting slickensides in the lower part. The soil is non calcareous throughout. MICRO RELIEF: irregular polygonal pattern (diameter 30-40cm) of cracks ADDITIONAL NOTES ON PROFILE DESCRIPTION: AC - few continuous slickensides in the upper part, continuous slickensides increasing in number with depth and intersecting.

 

Classification

WRB 2006 
Grumic- Vertisol (Eutric) 
35-120 cmvertic horizon
 
35-120 cmvertic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Chromi-Eutric VertisolChromic Vertisol
0-35 cmochric A horizon
35-120 cmcambic B horizon
-slickensides
-vertic
0-35 cmochric A horizon
35-120 cmcambic B horizon
-slickensides
-vertic

 

Local classification:Arcadia Form