SSS
Soil System Sciences

Soils at Imaggeo: Gypsum concretions in a soil horizon

Antonio Jordán, University of Seville, Sevilla, Spain

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Most Gypsisols are formed when gypsum (calcium sulfate) from gypsiferous parent materials is dissolved and moves through soil water, precipitating in an accumulation soil horizons.
Triassic rock outcrops in almost all Andalusia consist mainly of red and variegated clays and in some cases by clays of different colors are known as the iridescent clays of the Triassic, or as variegated clays. Gypsum appears as chemical precipitation rocks formed by the accumulation of crystals of calcium sulfate which precipitated in lakes, lagoons, ponds or in the coastal plain. These sediments are the consequence of important arid conditions, since these salts require high concentrations to precipitate.
In arid areas or during the dry hot season of some climates, soil moisture moves up through capilars, a gypsic or petrogypsic horizon may be formed relatively near the surface. In arid regions with hot and dry summers, gypsum is dehydrated into a hemihydrate powder, which returns again to gypsum crystals during winter. Often, highly irregular gypsum crystals form thick compact crusts on the surface. Gypsum precipitates as fine crystals, white, powder in old root channels (gypsum pseudomycelia) or pockets, sand-sized crystals or strongly cemented petrogypsic horizons.

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Antonio Jordán is a Senior Lecturer at the University of Seville and coordinator of the MED Soil Research Group. Antonio’s research focusses on rainfall-induced soil erosion processes, the effects of wildfires on soil properties and soil degradation in Mediterranean areas. He is an active members of the Soil System Sciences (SSS) Division of the European Geosciences Union (EGU), which coordinates the scientific programme on soil sciences.