Search results for "element"

showing 10 items of 13601 documents

Impact of basin burial and exhumation on Jurassic carbonates diagenesis on both sides of a thick clay barrier (Paris Basin, NE France).

2014

27 pages; International audience; Several diagenetic models have been proposed for Middle and Upper Jurassic carbonates of the eastern Paris Basin. The paragenetic sequences are compared in both aquifers to propose a diagenetic model for the Middle and Late Jurassic deposits as a whole. Petrographic (optical and cathodoluminescence microscopy), structural (fracture orientations) and geochemical (δ18O, δ13C, REE) studies were conducted to characterize diagenetic cements, with a focus on blocky calcite cements, and their connection with fracturation events. Four generations of blocky calcite (Cal1-Cal4) are identified. Cal1 and Cal2 are widespread in the dominantly grain-supported facies of t…

010504 meteorology & atmospheric sciencesEvaporiteCarbonateStratigraphyGeochemistryJurassic[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysicsOceanography01 natural sciencesDiagenesisPetrographyOxygen and carbon isotopesPaleontologychemistry.chemical_compoundParis Basin[ SDU.STU.MI ] Sciences of the Universe [physics]/Earth Sciences/MineralogyRare earth elements0105 earth and related environmental sciencesCalciteGeologyCementation (geology)6. Clean waterCretaceousDiagenesisGeophysicschemistry[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesEconomic GeologyPaleogeneGeology[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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The behaviour of zirconium, hafnium and rare earth elements during the crystallisation of halite and other salt minerals

2017

Abstract Halite crystals from Messinian and Tortonian evaporites from Sicily and Spain and current precipitated halite crystals and the relative parent brines (active evaporation systems) were investigated in order to evaluate the Zr, Hf and Rare Earth Element (REE) behaviour. Halite crystallisation from evaporating brines fractionates Zr, Hf and REE through a two-step process. During the first step, dissolved complexes of studied elements are scavenged onto the surfaces of crystallising halite. During the second step, elements are co-precipitated into the crystal lattice as it grows. The first step mechanism is determined by the dissolved REE speciation. In saltworks where carbonate-REE co…

010504 meteorology & atmospheric sciencesEvaporiteGeochemistryMineralogychemistry.chemical_elementengineering.material010502 geochemistry & geophysics01 natural sciencesGeochemistry and PetrologySettore CHIM/01 - Chimica AnaliticaZr/HfDissolution0105 earth and related environmental sciencesZirconiumRare-earth elementGeologyAuthigenicHaliteREESettore GEO/08 - Geochimica E VulcanologiaDiagenesisEvaporitechemistryengineeringHaliteSeawaterGeologyChemical Geology
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Zr/Hf ratio and REE behaviour: A coupled indication of lithogenic input in marginal basins and deep-sea brines

2019

Abstract The distribution of dissolved Zr, Hf and Rare Earth Elements (yttrium and lanthanides, hereafter referred to as REE) in the Eastern Mediterranean seawater column was measured in the Kryos basin to evaluate the lithogenic contribution from both Nile River and Sahara and Arabian desert dust. We found dissolved Zr/Hf ratios below the signature of crustal rocks and chondrites; a phenomenon likely driven by the dissolution of the Mn-rich coating of atmospheric dust particles delivered from the desert. In deeper waters, Zr/Hf ratios are clustered close to the signature of crustal rocks and chondrites according to the different Zr and Hf dissolved speciation. The Zr/Hf ratio observed in t…

010504 meteorology & atmospheric sciencesEvaporiteGeochemistrychemistry.chemical_elementYttrium010502 geochemistry & geophysicsOceanography01 natural sciencesDeep seaAnoxic watersWaves and shallow waterOceanographychemistryChondriteSeawaterZr/HfDissolutionGeology0105 earth and related environmental sciencesDeep Sea Research Part II: Topical Studies in Oceanography
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Intra- and inter-annual uranium concentration variability in a Belizean stalagmite controlled by prior aragonite precipitation: A new tool for recons…

2016

Aragonitic speleothems are increasingly utilised as palaeoclimate archives due to their amenability to high precision U–Th dating. Proxy records from fast-growing aragonitic stalagmites, precisely dated to annual timescales, can allow investigation of climatic events occurring on annual or even sub-annual timescales with minimal chronological uncertainty. However, the behaviour of many trace elements, such as uranium, in aragonitic speleothems has not thus far been as well constrained as in calcitic speleothems. Here, we use uranium concentration shifts measured across primary calcite-to-aragonite mineralogical transitions in speleothems to calculate the distribution coefficient of uranium …

010504 meteorology & atmospheric sciencesGeochemistryF700MineralogySpeleothemF800StalagmiteF600engineering.material010502 geochemistry & geophysics01 natural sciencesF900Geochemistry and PetrologymedicinePrecipitation0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryδ13CStable isotope ratioAragoniteTrace element15. Life on landSeasonalitymedicine.disease13. Climate actionengineeringGeologyGeochimica et Cosmochimica Acta
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Petrographic and geochemical characterization of the Middle‒Upper Jurassic Fe–Mn crusts and mineralizations from Monte Inici (north-western Sicily): …

2021

AbstractFe–Mn concretions and mineralizations, associated with condensed horizons and hardground, are significant archives in ancient carbonate rocks. Their petro-chemical study allows an assessment of the palaeoenvironmental context in which they were formed also connected to their biotic or abiotic origin. At the western side of the Monte Inici (Fornazzo section, north-western Sicily) a well exposed outcrop of condensed pelagic limestones (Rosso Ammonitico facies: Middle‒Upper Jurassic) is well-known and thoroughly studied. In this section, the base of the Rosso Ammonitico facies consists of a very condensed level rich in fossils with a variable thickness deposited from the early Bathonia…

010504 meteorology & atmospheric sciencesGeochemistrySettore GEO/07 - Petrologia E PetrografiaContext (language use)engineering.material010502 geochemistry & geophysicsCarbonate hardgrounds01 natural sciencesDiagenesisPetrographyTodorokiteIsotopes of carbonFe–Mn crusts Frutexites Microbial mediation Mineralogy Trace elements REE Stable isotope Growth rateFaciesengineeringGeneral Earth and Planetary SciencesCarbonate rockGeology0105 earth and related environmental sciences
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2021

Abstract Contaminated soils are lands in Europe deemed less favourable for conventional agriculture. To overcome the problem of their poor fertility, bio-fertilization could be a promising approach. Soil inoculation with a choice of biological species (e.g. earthworm, mycorrhizal fungi, diazotroph bacteria) can be performed in order to improve soil properties and promote nutrients recycling. However, questions arise concerning the dynamics of the contaminants in an inoculated soil. The aim of this study was to highlight the soil-plant-earthworm interactions in the case of a slightly contaminated soil. For this purpose, a pot experiment in controlled conditions was carried out during 2 month…

010504 meteorology & atmospheric sciencesHealth Toxicology and MutagenesisBiomass010501 environmental sciencesToxicologycomplex mixtures01 natural sciencesNutrient0105 earth and related environmental sciences2. Zero hungerbiologyChemistryEarthwormTrace elementfood and beveragesGeneral Medicine15. Life on landbiology.organism_classificationPollutionSoil contamination6. Clean waterBioavailability13. Climate actionEnvironmental chemistryBioaccumulationSoil waterEnvironmental Pollution
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Chronospeciation of uranium released in soil during a long-term DU shell weathering experiment.

2021

Corrosion process was investigated of depleted uranium (DU) ammunition fragments buried for three years in aerobic soils continuously irrigated with water. The continuing corrosion process was triggered through formation of soluble uranyl oxyhydrate phases such as metaschoepite and becquerelite, which were identified by micro-Raman and X-ray diffraction spectroscopy. The soil was not amended by phosphates and, therefore, no uranyl phosphates were found as corrosion products on the DU surfaces by X-ray photoelectron spectroscopy. A speciation modelling at high temporal sequence (chronospeciation approach) indicated that the abundant Fe oxyhydroxides in the soil immobilized the U(IV) released…

010504 meteorology & atmospheric sciencesHealth Toxicology and Mutagenesischemistry.chemical_elementWeathering010501 environmental sciences01 natural sciencesCorrosionFerrihydritechemistry.chemical_compoundPore water pressureSoilRadiation MonitoringEnvironmental ChemistrySoil Pollutants RadioactiveWaste Management and Disposal0105 earth and related environmental sciencesTotal organic carbonGeneral MedicineUraniumUranylPollutionCorrosionchemistryEnvironmental chemistrySoil waterUraniumJournal of environmental radioactivity
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ATR–FTIR Spectral Analysis and Soluble Components of PM10 And PM2.5 Particulate Matter over the Urban Area of Palermo (Italy) during Normal Days and …

2019

Several epidemiological studies have shown a close relationship between the mass of particulate matter (PM) and its effects on human health. This study reports the identification of inorganic and organic components by attenuated total reflectance-Fourier-transform infrared spectroscopy (ATR-FTIR) analysis in PM10 and PM2.5 filters collected from three air quality monitoring stations in the city of Palermo (Sicily, Italy) during non-Saharan dust events and Saharan events. It also provides information on the abundance and types of water-soluble species. ATR-FTIR analysis identified sulfate, ammonium, nitrate, and carbonate matter characterized by vibrational frequencies at 603, 615, 670, and …

010504 meteorology & atmospheric sciencesHealth Toxicology and Mutagenesissaharan dust eventsPM10 and PM2.5Infrared spectroscopychemistry.chemical_elementlcsh:Medicine[SDU.STU]Sciences of the Universe [physics]/Earth Sciencesionic soluble components010501 environmental sciencesMineral dust01 natural sciencesionic soluble componentSaharan dust eventPM<sub>10</sub> and PM<sub>2.5</sub>Absorbancechemistry.chemical_compound11. SustainabilitySulfate0105 earth and related environmental sciencesparticulate mattersirocco windsPM 10 and PM 2.5lcsh:RPublic Health Environmental and Occupational HealthSettore GEO/07 - Petrologia E PetrografiaParticulatesSettore GEO/08 - Geochimica E Vulcanologiachemistry13. Climate action[SDU]Sciences of the Universe [physics]Environmental chemistryCarbonateClay mineralsCarbonATR-FTIRInternational Journal of Environmental Research and Public Health
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Asynchronous changes of CO2, H2, and He concentrations in soil gases: A theoretical model and experimental results

2016

010504 meteorology & atmospheric sciencesHydrogenchemistry.chemical_elementSoil science010502 geochemistry & geophysics01 natural scienceschemistry.chemical_compoundGeophysicschemistrySpace and Planetary ScienceGeochemistry and PetrologyAsynchronous communicationCarbon dioxideEarth and Planetary Sciences (miscellaneous)GeologyHelium0105 earth and related environmental sciencesJournal of Geophysical Research: Solid Earth
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Lower mantle hydrogen partitioning between periclase and perovskite : a quantum chemical modelling

2016

Abstract Partitioning of hydrogen (often referred to as H2O) between periclase (pe) and perovskite (pvk) at lower mantle conditions (24–80 GPa) was investigated using quantum mechanics, equilibrium reaction thermodynamics and by monitoring two H-incorporation models. One of these (MSWV) was based on replacements provided by Mg2+ ↔ 2H+ and Si4+ ↔ 4H+; while the other (MSWA) relied upon substitutions in 2Mg2+ ↔ Al3+ + H+ and Si4+ ↔ Al3+ + H+. H2O partitioning in these phases was considered in the light of homogeneous (Bulk Silicate Earth; pvk: 75%–pe:16% model contents) and heterogeneous (Layered Mantle; pvk:78%–pe:14% modal contents) mantle geochemical models, which were configured for lower…

010504 meteorology & atmospheric sciencesHydrogenpericlaseAnalytical chemistrySocio-culturalechemistry.chemical_elementengineering.material010502 geochemistry & geophysics01 natural sciencesMantle (geology)chemistry.chemical_compoundGeochemistry and PetrologyOrganic chemistryH2O-partitioningperovskiteEquilibrium constant0105 earth and related environmental sciencesChemistryAb-initio calculationslowermantle; H2O-partitioning; periclase; perovskite.SilicatePartition coefficientlower mantleAnhydrousengineeringPericlaseChemical equilibriumlower mantle H2O-partitioning Ab-initio calculations periclase perovskite
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