Reference soil Botswana 02: Vertisol

BW002

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

 

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 2006WRB 1998
Pellic-Grumic- Vertisol (Hyposodic)Grumi-Pellic- Vertisol (Hyposodic)
67-142 cmvertic horizon
0-33 cmochric horizon
67-142 cmvertic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
PelliEutric VertisolPellic Vertisol
0-33 cmochric A horizon
33-142 cmcambic B horizon
33-142slickensides property
0-33 cmmollic A horizon
33-142 cmcambic B horizon
33-142slickensides property

Local classification

Classification informationCPCS (1967): Manale series (deep vertic A)
Other classification
USDA-NRCS (1999Aridic Haplustert ustic fine montmorillonitic hyperthermic
USDA-SCS (1975)Aridic Pellustert ustic fine montmorillonitic hyperthermic
Location: 

6km SE of Shoshong, S of Serowe