Search results for "PSU"

showing 10 items of 678 documents

New knowledge on the Monte Conca gypsum karst system (Central-western Sicily, Italy)

2011

The Monte Conca karst system is located in Central-Western Sicily, where Messinian evaporites are widespread. Here, the evaporites lie on lower Messinian-middle Serravallian clayey-marly-sandy deposits and are overlain locally by Pliocene marly limestones. These successions are affected by E-W, and to a lesser degree N-S and NW-SE, high-angle faults that have also produced lateral contacts between the gypsum units and the clayey-marly deposits. The cave passages reachaltogether about 2.4 km in lengthand 130 m in depth, and the system consists of a sink cave, a resurgence and a relict resurgence. At large scale it is characterized by superimposed levels of sub-horizontal galleries connected …

Gypsum karst system speleogenesis Monte Conca Sicilygeographygeography.geographical_feature_categoryEvaporiteLandformSettore GEO/04 - Geografia Fisica E GeomorfologiaEcological successionKarstDebrisSink (geography)PaleontologyCaveAlluviumGeomorphologyGeologyEarth-Surface ProcessesActa Carsologica
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Sistemi costruttivi tradizionali in gesso nell’architettura siciliana

2020

Chalks outcrops characterize all the central-western territory in Sicily. They are different in types and extension and tangibly mark the presence of the well-known sulphurus chalky series. In the same areas it is possible to see several traditional buildings built, even in their structures, using gypsum, an material which is unusual in other contexts. In some cases the chalk outcrop makes up even the base of a building. This text describes different kinds of walls, floors, vaults and flooring where gypsum is the main material.

Gypsum traditional buildings sicilian techniquesSettore ICAR/12 - Tecnologia Dell'Architettura
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Authigenic phase formation and microbial activity control Zr, Hf, and rare earth element distributions in deep-sea brine sediments

2014

Abstract. Sediments collected from hypersaline and anoxic deep-sea basins in the eastern Mediterranean (Thetis, Kryos, Medee, and Tyro) were characterised in terms of their mineralogical composition, the distributions of rare earth elements (REE), Zr, and Hf and their content of microbial DNA. We identified two major mineralogical fractions: one fraction of detritic origin was composed of quartz, gypsum, and low-Mg calcite bioclasts (with 0 < Mg < 0.07%) and another fraction of authigenic origin constituted of halite, dolomite, high-Mg calcite (with a Mg content of up to 22%) and rare bischofite and showed a textural evidence of microbial assemblages. We found that in the Medee and Ty…

Gypsum010504 meteorology & atmospheric sciencesSettore AGR/13 - Chimica AgrariaGeochemistrylcsh:LifeMineralogy[SDU.STU]Sciences of the Universe [physics]/Earth Sciencesengineering.material010502 geochemistry & geophysics01 natural sciencesDeep seachemistry.chemical_compoundlcsh:QH540-549.5Settore CHIM/01 - Chimica AnaliticaQuartzEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesgeochemistryCalciteRare-earth elementlcsh:QE1-996.5AuthigenicAnoxic watersSettore GEO/08 - Geochimica E Vulcanologialcsh:Geologylcsh:QH501-531chemistryengineeringCarbonatelcsh:EcologyGeology
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Electronic microdiffraction study of structural modifications resulting from the dehydration of gypsum. Prediction of the microstructure of resulting…

2001

Abstract Endothermic decomposition reactions (solid 1→solid 2+gas) generally affect only part of the inter-atomic bonds of the solid 1 structure. In consequence, the morphology and external dimensions of particles remain unchanged (the particles of solid 2 are referred to as pseudomorphs of those of solid 1). The gas release normally leads to a decrease of the molar volume of the precursor solid, resulting in cracking and formation of intra-particle porosity. This work deals with such a reaction: the dehydration of gypsum into sub-hydrated and anhydrous phases. Ultrathin (010) gypsum cleaved plates have been dehydrated under controlled conditions and studied by electron microdiffraction. Al…

GypsumChemistryGeneral Chemistryengineering.materialCondensed Matter PhysicsMicrostructureEndothermic processCrystallographyElectron diffractionChemical engineeringTransmission electron microscopyAnhydrousengineeringGeneral Materials SciencePorosityPseudomorphSolid State Ionics
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Geological development of a gypsum lake formed at the beginning of the 20th century in central Sicily, Italy: Integration of historical data with mod…

2006

A limnological investigation was carried out on the small, endorheic lake, called Lake Sfondato, located in central Sicily (Italy). All the aquatic environments in the central part of the island are rich in salt, with conductivity values above 5 mS cm−1, and are characterized by high alkalinity values and hard waters. In addition, due to intensive agriculture, many of these ecosystems have experienced a strong anthropogenic eutrophication over the last decades. In order to better understand the functioning of these peculiar environments, the morphology, hydrology, and geochemistry, as well as several selected physical and biological characteristics of Lake Sfondato, were studied in the year…

GypsumEcologyIntensive farmingAquatic ecosystemClimate changeengineering.materialOceanographyHydrology (agriculture)engineeringGeneral Earth and Planetary SciencesEcosystemPhysical geographyEutrophicationEcology Evolution Behavior and SystematicsGeologyGeneral Environmental ScienceTrophic levelChemistry and Ecology
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A new calcium sulfate hemi-hydrate

2010

Calcium sulfate hydrates receive significant attention due to numerous large scale industrial applications. There has been a long debate on the possible existence of two gypsum hemi-hydrate polymorphs, denoted alpha- and beta-CaSO(4).0.5H(2)O. In this work, a new crystal structure of calcium sulfate hemi-hydrates is presented, denoted beta-CaSO(4).0.5H(2)O. The structure was solved using powder neutron diffraction data, the space group is P3(1) and the unit cell in a hexagonal setting a = 6.9268(1), c = 12.7565(3) A. The structure has two calcium-oxygen coordination polyhedra: Ca1 is eight coordinated and has Ca-O bond lengths in the range 2.31(3) to 2.89(2) A and Ca2 is nine coordinated an…

GypsumHydrogen bondNeutron diffractionCrystal structureengineering.materialInorganic ChemistryBond lengthCrystallographychemistry.chemical_compoundchemistryengineeringMoleculeSulfateHydrate
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Successive alkalinity producing system for the treatment of acid sulphate soil runoff: preliminary results of a field trial

2005

A successive alkalinity producing system (SAPS) has been investigated as a potential passive treatment option for acid, metal containing runoff from acid sulphate soil. A pilot-scale system was installed at an agricultural land site in Rintala embankment area in mid-western Finland. The experimental layout consists of three parallel treatment units: two different SAPS cells and one limestone-filled cell for comparison of performance. The SAPS cells are composed of a bottom layer of limestone and a top layer of compost supplemented with sand. One of the SAPS cells contains sulphate-rich, waste gypsum mixed with the compost layer in order to enhance the metal reduction by sulphate reducing-ba…

GypsumNatural resource economicsAlkalinitychemistry.chemical_elementsuccessive alkalinity producing systemrautaManganeseengineering.materiallcsh:AgricultureMetalAluminiumlcsh:Agriculture (General)DrainagealumiiniSAPSCompostlcsh:Sacid sulphate soilsArticlesmangaanivedenkäsittelylcsh:S1-972chemistryhappamat sulfaattimaatvisual_artEnvironmental chemistryvisual_art.visual_art_mediumengineeringSurface runoffveden käsittelyFood Science
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The effects of anthropogenic particulate emissions on roadway dust and Nerium oleander leaves in Messina (Sicily, Italy)

2003

Complementary studies on the inorganic chemical composition of Nerium oleander leaves collected in the town of Messina (Sicily, Italy) and seven grain-size fractions of local roadway dust have been carried out. Data and maps are presented to show that the particulate matter present in the air of Messina contains trace elements significantly in excess with respect to the average continental earth crust. The anomalies follow the outline of the urban area, the highest concentrations of trace elements being observed where traffic density is highest. Chemical and isotopic analyses of both road dust and Nerium oleander leaves indicate that Pb contamination still characterizes roads with heavy tra…

GypsumNerium oleanderDust particlesPoison controlengineering.materialManagement Monitoring Policy and LawMetals HeavyNeriumHeavy trafficParticle SizeVehicle EmissionsInorganic ChemicalAir PollutantsEnvironmental engineeringPublic Health Environmental and Occupational HealthDustGeneral MedicineParticulatesSettore GEO/08 - Geochimica E VulcanologiaPlant LeavesMotor VehiclesItalyEnvironmental chemistryengineeringMicroscopy Electron ScanningEnvironmental scienceComposition (visual arts)GasesPorosity
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Formation of secondary carbonates and native sulphur in sulphate-rich Messinian strata, Sicily

2010

Abstract Microbially formed authigenic carbonates accompanied by native sulphur are present in the ‘Calcare Solfifero’ below a thick succession of gypsum deposited during the Messinian salinity crisis in Sicily. We sampled these carbonates and associated sulphur in five former sulphur mines to subject them to a detailed petrographic and geochemical study in order to explore their different modes of formation. Native sulphur formed in conjunction with microbial sulphate reduction, which is reflected in its depletion in 34S (δ34S values as low as − 2‰ vs. V-CDT) and an enrichment of 34S in the residual sulphate (δ34S values as high as + 61‰). The oxidation of organic matter by sulphate reduct…

GypsumSettore GEO/02 - Geologia Stratigrafica E Sedimentologica010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]StratigraphyAlkalinityGeochemistryCarbonate minerals[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]engineering.material010502 geochemistry & geophysics01 natural scienceschemistry.chemical_compoundδ34SMessinian salinity crisiSicilyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesSettore GEO/06 - MineralogiaAnhydriteGeologyAuthigenicSettore GEO/01 - Paleontologia E PaleoecologiaNative sulphurSettore GEO/08 - Geochimica E VulcanologiaDiagenesischemistry13. Climate actionengineeringCarbonateMicrobial sulphate reductionAuthigenic carbonateGeology
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Investigations of Surface Forces between Gypsum Microcrystals in Air Using Atomic Force Microscopy

2000

This article introduces a new approach to the study of the interactions between gypsum faces in air. We have mounted a gypsum crystal on the end of a microcantilever to measure local forces (van der Waals, capillary forces, electrostatic) directly between two crystals. A systematic study with respect to the orientation of crystalline faces, relative humidity, and the duration of contact between crystals improves the understanding of the mechanism involved in the hardening of plaster in air. In dry air, a physicochemical process of matter transfer is added to the van der Waals forces to ensure the cohesion. Others force measurements were performed by varying the shape of the contact (interac…

GypsumSiliconChemistryCapillary actionSurface forcechemistry.chemical_elementMineralogySurfaces and Interfacesengineering.materialCondensed Matter PhysicsCrystalsymbols.namesakeElectrochemistryengineeringsymbolsHardening (metallurgy)General Materials ScienceWettingvan der Waals forceComposite materialSpectroscopyLangmuir
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