Reference soil Uruguay 05: Vertisol
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.
Reference soil UY005: Vertisols
GEOLOGICAL FORMATION: Libertad quarternary period MOISTURE: Soil is slightly dryer below 20 cm. SURFACE DRAINAGE: Coarse dendritic VEGETATION: (regional, local) Trees (1%, 1%); Herbs (20%, 19%); Grasses (29%, 80%); Bare ground (50%, -). Dominant species are Stipa charruana, Paspalum dilatatum, Bothriochloa laguroides, Eryngium horridum, Bacharis coridifolia, Stenotaphrum secunaatum. 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 2006 | WRB 1998 | ||||||||||||||||
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Grumic- Vertisol (Calcaric Humic Pellic) | Grumi-Pellic- Vertisol (Hypereutric) | ||||||||||||||||
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FAO-UNESCO-ISRIC 1988 | FAO-UNESCO-ISRIC 1974 | ||||||||||||||||
Pelli-Calcic Vertisol gilgai | Pellic Vertisol | ||||||||||||||||
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Local classification: | Vertisol ruptico |