Reference soil Cuba 06: Vertisol

CU006

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 CU006: Vertisols

Short field description Deep, moderately well drained, brown clay, with large cracks at the surface. (Sub)angular blocky structure, slickensides and hard calcareous nodules. Geology: Middle Eocene, 'Vertientes' Formation: marls, sandstone, radiolaritas limestone. Geomorphology: Denudative erosive undulating plains. First ratoon: yield 51.4 ton/ha.

 

Classification

WRB 2006WRB 1998
Calcic-Stagnic- Vertisol (Albic)Calcic- Vertisol
20-55 cmalbic horizon
20-55 cmvertic horizon
55-170 cmcalcic horizon
-stagnic colour pattern
0-20 cmochric horizon
20-55 cmalbic horizon
20-55 cmvertic horizon
55-170 cmcalcic horizon
-secondary carbonates
-stagnic
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Albi-Calcic VertisolChromic Vertisol
0-20 cmochric A horizon
20-55 cmalbic E horizon
55-170 cmcalcic horizon
- cmcambic B horizon
-slickensides
-vertic
0-20 cmochric A horizon
20-55 cmalbic E horizon
55-170 cmcalcic horizon
- cmcambic B horizon
-vertic

 

Local classification:Pardo con carbonato plast.