Reference soil Botswana 02: 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 BW002: Vertisol
PHYSICAL UNIT: Escarpment with colluvium in the north and floodplain in the south. A very dark grey, very thin clay topsoil overlying a deep homogeneous very dark grey to black clay. Structural elements and cracks are best developed in the top 67 cm. Soil reaction moderately to strongly alkaline.
Classification
WRB 2006 | WRB 1998 | ||||||||||||||
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Pellic-Grumic- Vertisol (Hyposodic) | Grumi-Pellic- Vertisol (Hyposodic) | ||||||||||||||
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FAO-UNESCO-ISRIC 1988 | FAO-UNESCO-ISRIC 1974 | ||||||||||||||
PelliEutric Vertisol | Pellic Vertisol | ||||||||||||||
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Local classification
Classification information | CPCS (1967): Manale series (deep vertic A) |
USDA-NRCS (1999 | Aridic Haplustert ustic fine montmorillonitic hyperthermic |
USDA-SCS (1975) | Aridic Pellustert ustic fine montmorillonitic hyperthermic |
6km SE of Shoshong, S of Serowe