Reference soil Uruguay 06: Vertisol

UY006

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 UY006: Vertisols

GEOLOGICAL FORMATION: Libertad quaternary period SURFACE DRAINAGE: course dendritic MOISTURE: soil is slightly dryer below 20 cm VEGETATION: (regional,local) Trees (1%, 1%), herbs (20%, 19%), grasses (29%, 80%), bare ground (50%, -) Dominant species are Stipa carruana, Paspalum dilatatum, Bothriochola laguroides, Eryngium horridum, Bacharis coridifolia, Stenotaphrum secundatum. LITERATURE: Terzaghi, A. Características Físicas de los principales suelos agrícolas de Canelones-Montevideo. Technical Bulletin No. 8 part 1 and 2. Canelones-Montevideo soil chart (1:100.000)

 

Classification

WRB 2006WRB 1998
calcic horizon- Vertisol (Humic)calcic horizon- Vertisol
22-117 cmvertic horizon
76-101 cmcalcic horizon
0-22 cmochric horizon
22-117 cmvertic horizon
76-101 cmcalcic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Hyposodi-Calcic Vertisol gilgaiChromic Vertisol sodic
0-22 cmochric A horizon
22-117 cmcambic B horizon
76-101 cmcalcic horizon
-calcaric
-vertic
0-22 cmochric A horizon
76-101 cmcalcic horizon
-vertic

 

Local classification:Vertisol ruptico