Reference soil Cuba 18: Vertisol

CU018

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 CU018: Vertisols

Short field description: Very deep, moderately well to well drained, dark yellowish brown clay derived from alluvium. Small slickensides are present in the subsoil. Geology: Holocene silty clay and alluvials sands. Geomorphology: alluvial plain and terrace, eroded and hilly.

 

Classification

WRB 2006WRB 1998
Mollic- Vertisol (Calcaric Humic)Eutric- Vertisol
25-45 cmcambic horizon
45-115 cmvertic horizon
-calcaric
0-25 cmmollic horizon
25-45 cmcambic horizon
45-115 cmvertic horizon
-calcaric
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Molli-Eutric VertisolChromic Vertisol
0-25 cmmollic A horizon
25-150 cmcambic B horizon
- cmcambic B horizon
- cmmollic A horizon
-slickensides
-vertic
0-25 cmmollic A horizon
25-150 cmcambic B horizon
-slickensides
-vertic

 

Local classification:Aluvial diferenciado