Reference soil Greece 06: 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 GR006: Vertisols
Brief profile description: A dark brown clayey profile with weak blocky structure and pronounced slickensides thoughout the solum, overlying a strong brown calcareous clay with many carbonate concretions. The soil is under cultivation and regularly ploughed. Slickensides: distinct and prominent at 45 degrees in Ap, intersecting in AC1 In the Ac horizon occur "tongues" of organic matter from the A horizon In the Ck3 coatings of Manganese oxide(?) on cracks Attention: Exchangeable cations and CEC : pH=8.2 pH and EC measurements : 1:5 extract