Reference soil Botswana 04: Calcisol

BW004

Calcisols occur in regions with distinct dry seasons, as well as in dry areas where carbonate-rich groundwater comes near the surface.

Characteristics

Soils having a (petro-)calcic horizon (horizon with accumulation of secondary calcium carbonates). In addition, they have no diagnostic horizons other than an ochric or cambic horizon, a calcareous argic horizon, or a gypsic horizon beneath a petrocalcic horizon.

Distribution of Calcisols (rough estimation supplied by soilgrids)

 

Reference soil BW004: Calcisols

LOCATION: 200 m West of main road to Gabarone VEGETATION: Acacia Mixed Woodland with A.nigerescens and A.totrilis BRIEF PROFILE DESCRIPTION: A moderatley deep, well drained, dark reddish brown snady clay loam with an epipedon of sandy loam texture, horizonation is gradual to clear, weak fine sub-angular blocky structure is confined to the top 33 cm. The soil reaction is slightly acid but becomes neutral to moderately alkaline in the subsoil. MORPHOLOGY: B1 Very fine and fine gravel increasing with depth. C Also pinkish white parts (5YR8/2, dry). The horizon has an appearance of weathered calcrete rock with granitic matrix; very hard (dry) but in some parts soft.

 

Classification

WRB 2006WRB 1998
Luvic-Petric- Calcisol (Chromic)Luvi-Endopetric- Calcisol
10-91 cmargic horizon
91-100 cmpetrocalcic horizon
0-10 cmochric horizon
10-91 cmargic horizon
91-100 cmpetrocalcic horizon
FAO-UNESCO-ISRIC 1988FAO-UNESCO-ISRIC 1974
Chromi-Petric CalcisolCalcic Xerosol petrocalcic
0-10 cmochric A horizon
10-91 cmargic B horizon
91-100 cmpetrocalcic horizon
-fluvic
0-10 cmochric A horizon
10-91 cmargillic B horizon
91-100 cmpetrocalcic horizon