Search results for " Clay mineralogy"

showing 2 items of 2 documents

Soil development on sediments and evaporites of the Messinian crisis

2020

Abstract Vast areas in the Mediterranean are characterised by evaporite deposits of the Messinian crises (c. 6–5.3 Ma BP). During this period, large deposits were built up in shallow lagoon-like systems and are now found in southern Italy, Albania, Cyprus and Turkey. So far, soil formation on evaporites has been studied predominantly in subarid to arid environments. Although the formation of soils has received new significance, little is known about the evolutional trajectories on evaporites of the Mediterranean. We therefore studied soil formation in the Caltanissetta basin (Sicily) where evaporites are most widespread. The lithologies included the sequence: marine clay deposits, laminated…

010504 meteorology & atmospheric sciencesEvaporite1904 Earth-Surface ProcessesGeochemistryEarthWeathering04 agricultural and veterinary sciences01 natural sciencesDiagenesis10122 Institute of GeographyPedogenesisSurface ProcessesSettore AGR/14 - PedologiaSoil formation Evaporites Clay mineralogy Weathering Diatomite Stable isotopes CarbonatesLeaching (pedology)Marl040103 agronomy & agriculture0401 agriculture forestry and fisheriesKaoliniteAridisol910 Geography & travelGeology0105 earth and related environmental sciencesEarth-Surface Processes
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Origin of clay minerals in soils on pyroclastic deposits in the island of Lipari (Italy)

2005

The island of Lipari (Italy) is characterized by calc-alkaline to potassic volcanism and a Mediterranean-type climate. The mineralogical and chemical features of two different soil profiles with ages of 92,000 and 10,000–40,000 y, respectively, have been investigated. There were no Andisols, but Vitric and Vertic Cambisols have developed at both sites. Although the morphology of the soils was similar, remarkable differences in the clay mineralogy between the two sites were observed. The site with the Vitric Cambisol was associated with the weathering sequence: glass → halloysite → kaolinite or interstratified kaolinite-2:1 clay minerals. Both sites had smectite in the clay fraction and, to …

CambisolGeochemistrySoil ScienceMineralogyWeatheringAndisols geochemistry montmorillonite glasses kaolinite sheet silicates Italy Cambisols clay mineralogy Europe silicates soils halloysite Lipari Islands clay minerals igneous rocks Lipari Island smectite metasomatism weathering Sicily Italy volcanic rocks Southern Europeengineering.materialHalloysitechemistry.chemical_compoundMontmorillonitechemistrySettore AGR/14 - PedologiaGeochemistry and PetrologySoil waterEarth and Planetary Sciences (miscellaneous)engineeringSoil horizonKaoliniteClay mineralsGeologyWater Science and Technologyclays and clay minerals
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