Reference soil India 12: Vertisol

IN012

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 IN012: Vertisols

Deep, imperfectly drained, very dark grayish brown clayey soil derived from basalt with deep, wide cracks during the dry season, gilgai surface features, prominent slickensides and accumulation of calcium carbonates. The profile is located on level land with gradual slope (0-1%) towards the east.

 

Classification

WRB 2014 
Vertisol 
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Orthi-Calcic Vertisol gilgaiChromic Vertisol
- cmcalcic horizon
- cmcambic B horizon
- cmochric A horizon
-slickensides
- cmcalcic horizon
- cmcambic B horizon
- cmochric A horizon
-gilgai microrelief
-slickensides

 

Local classification:Medium black soil