Reference soil India 08: Vertisol

IN008

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 IN008: Vertisols

A deep, moderately well drained very dark grayish brown soil derived from basalt. Tap and fibrous roots are commonin the first two horizons and fibrous roots are present in the third and fourth horizons. Clay content increases with depth. The slope is 1 to 3% with slight erosion. Cycle of micro-high and micro-low has been observed in the moist subsurface horizons. Few concretions of manganese and iron oxides are present. Slickensides are present in all subsurface horizons. Internal drainage is moderate and few faint dark yellowish brown mottles can be observed in the lower subsoil.

 

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:Deep black soil