Reference soil Uruguay 05: Vertisol

UY005

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 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 2006WRB 1998
Grumic- Vertisol (Calcaric Humic Pellic)Grumi-Pellic- Vertisol (Hypereutric)
33-102 cmvertic horizon
-calcaric
0-33 cmochric horizon
33-102 cmvertic horizon
-calcaric
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Pelli-Calcic Vertisol gilgaiPellic Vertisol
0-33 cmochric A horizon
33-102 cmcambic B horizon
-slickensides
-soft powdery lime
0-33 cmochric A horizon
-slickensides
-soft powdery lime

 

Local classification:Vertisol ruptico