Reference soil Brazil 27: Plinthosol
Plinthosols occur mainly in the moist tropical regions in low-lying positions where iron from the soil and adjacent uplands is accumulating.
Characteristics
Soils having either a petroplinthic horizon within 50 cm from the soil surface, or a plinthic horizon which either starts within 50 cm from the soil surface, or within 100 cm from the soil surface if it underlies an albic horizon or a horizon with stagnic properties.
Reference soil BR027: Plinthosol
Very deep, poorly drained grey claysoil derived from kaolinitic sediments; with a thick high organic matter containing topsoil and a strongly mottled subsoil. Effective soil depth depends on depth of water table which strongly fluctuates depending on the water level of the Formoso river. Vertical and especially lateral water transport in the subsoil is extremely fast because of very high permeability. The permeability of the subsoil is extremely high due to very high stable biopores. The pit wall shows a tongued character because of vertical filled up channels due to faunal activity, diameter about 2 to 4cm.
Classification: although derived from alluvial deposits the soil does not show sediment stratification anymore. It is assumed that the strongly mottled clay is plinthite, based on the observation that hard ironstone is protruding from banks of the nearby Formoso river.
The Koppen climate: Aw or Am. Original vegetation: semi-decidious forest or woodland.
Slides no 9891-9903.