Search results for "COMPOUND"

showing 10 items of 35174 documents

Activity-composition relations for the calculation of partial melting equilibria in metabasic rocks

2020

A set of thermodynamic models is presented that, for the first time, allows partial melting equilibria to be calculated for metabasic rocks. The models consist of new activity–composition relations combined with end-member thermodynamic properties from the Holland & Powell dataset, version 6. They allow for forward modelling in the system Na (Formula presented.) O–CaO–K (Formula presented.) O–FeO–MgO–Al (Formula presented.) O (Formula presented.) –SiO (Formula presented.) –H (Formula presented.) O–TiO (Formula presented.) –Fe (Formula presented.) O (Formula presented.). In particular, new activity–composition relations are presented for silicate melt of broadly trondhjemitic–tonalitic compo…

010504 meteorology & atmospheric sciencesPartial meltingMineralogyThermodynamicsGeologyComposition (combinatorics)010502 geochemistry & geophysics01 natural sciencesSilicatechemistry.chemical_compoundchemistryGeochemistry and PetrologyTetrahedronGeologyMixing (physics)0105 earth and related environmental sciencesSolid solutionJournal of Metamorphic Geology
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Steroid Biomarkers Revisited - Improved Source Identification of Faecal Remains in Archaeological Soil Material.

2017

Steroids are used as faecal markers in environmental and in archaeological studies, because they provide insights into ancient agricultural practices and the former presence of animals. Up to now, steroid analyses could only identify and distinguish between herbivore, pig, and human faecal matter and their residues in soils and sediments. We hypothesized that a finer differentiation between faeces of different livestock animals could be achieved when the analyses of several steroids is combined (Δ5-sterols, 5α-stanols, 5β-stanols, epi-5β-stanols, stanones, and bile acids). We therefore reviewed the existing literature on various faecal steroids from livestock and humans and analysed faeces …

010504 meteorology & atmospheric sciencesPhysiologySwineSocial Scienceslcsh:MedicinePlant ScienceBreeding01 natural sciencesFecesSoilchemistry.chemical_compoundChenodeoxycholic acidMedicine and Health SciencesBilelcsh:ScienceMammalsMultidisciplinaryEcologyOrganic CompoundsGoatsAgricultureRuminantsBreedBody FluidsTrophic InteractionsCoprostanolChemistrySterolsArchaeologyCommunity EcologyPhysical SciencesVertebratesSteroidsLivestockDonkeyAnatomyResearch Article010506 paleontologyLivestockEquinesBiologyGas Chromatography-Mass SpectrometryBile Acids and SaltsGoosePlant-Animal Interactionsbiology.animalAnimalsHumansHerbivoryHorsesFeces0105 earth and related environmental sciencesHerbivorebusiness.industryPlant EcologyOrganic ChemistryEcology and Environmental Scienceslcsh:RChemical CompoundsOrganismsBiology and Life SciencesArchaeologychemistryAmnioteslcsh:QbusinessBiomarkersPLoS ONE
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Reactive oxygen species formed in aqueous mixtures of secondary organic aerosols and mineral dust influencing cloud chemistry and public health in th…

2017

Mineral dust and secondary organic aerosols (SOA) account for a major fraction of atmospheric particulate matter, affecting climate, air quality and public health. How mineral dust interacts with SOA to influence cloud chemistry and public health, however, is not well understood. Here, we investigated the formation of reactive oxygen species (ROS), which are key species of atmospheric and physiological chemistry, in aqueous mixtures of SOA and mineral dust by applying electron paramagnetic resonance (EPR) spectrometry in combination with a spin-trapping technique, liquid chromatography-tandem mass spectrometry (LC-MS/MS), and a kinetic model. We found that substantial amounts of ROS includi…

010504 meteorology & atmospheric sciencesRadicalInorganic chemistry010501 environmental sciencesMineral dustbehavioral disciplines and activities01 natural scienceschemistry.chemical_compoundKaolinitePhysical and Theoretical ChemistryIsoprene0105 earth and related environmental sciencesAerosolsAir PollutantsMineralsAqueous solutionAtmosphereWaterParticulatesDecompositionDeposition (aerosol physics)chemistryEnvironmental chemistryParticulate MatterPublic HealthReactive Oxygen SpeciesFaraday Discussions
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Titan's surface albedo variations over a Titan season from near-infrared CFHT/FTS spectra

2006

International audience; We have observed Titan in a series of campaigns from 1991 to 1996 with the Fourier Transform Spectrometer on the CFH telescope. The data acquired provide a lightcurve from the geometric albedos in the 0.9–View the MathML source spectral region. The 1991–1993 data were previously analyzed in Coustenis et al. [1995. Titan's surface: composition and variability from its near-infrared albedo. Icarus 118, 87–104] with a spherical particle code by McKay et al. [1989. The thermal structure of Titan's atmosphere. Icarus 80, 23–53]. We present here three new datasets from the 1994, 1995 and 1996 observations, with additional information from the 0.94-μm methane window on Tita…

010504 meteorology & atmospheric sciencesSatellitesCFHTAstrophysicsAtmospheric sciences01 natural sciencesMethaneAtmosphereMethane absorption coefficientssymbols.namesakechemistry.chemical_compoundNear-infraredPlanet0103 physical sciencesRadiative transfer010303 astronomy & astrophysicsSpectroscopy0105 earth and related environmental sciencesPhysicsAtmospheric methaneAstronomy and AstrophysicsTholinAlbedochemistry13. Climate actionSpace and Planetary SciencesymbolsTitan (rocket family)Titan
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Selenium mobilization in soils due to volcanic derived acid rain: An example from Mt Etna volcano, Sicily

2011

International audience; The significant amounts of selenium (Se) emitted by volcanoes may have important impact on human health due to the narrow range between nutrition requirement and toxic effects for living organisms upon Se exposure. Although soils play a key role in determining the level in food and water and thereby human health, little is known about the behaviour of Se in volcanic soils. In this work we evaluated the Se release during rainwater–soil interaction under controlled conditions using soils collected on the flanks of Etna volcano and synthetic rain. Selenium concentrations in soil leachate solutions displayed a spatial distribution, which cannot be explained by plume depo…

010504 meteorology & atmospheric sciencesSelenium; Volcanic soils; Geogenic; Volcanoes; Contamination; GroundwaterSelenium; Volcanic soils; Geogenic; Volcanoes; Contamination; Groundwaterchemistry.chemical_element[SDU.STU]Sciences of the Universe [physics]/Earth SciencesVolcanoe010502 geochemistry & geophysics01 natural sciencesSelenateVolcanic soilchemistry.chemical_compoundSeleniumContaminationGeochemistry and PetrologySelenium acid rain soilsGeogenicChemical compositionGroundwater0105 earth and related environmental sciencesgeographyGroundwaterSeleniumgeography.geographical_feature_categoryGeologySettore GEO/08 - Geochimica E VulcanologiaDeposition (aerosol physics)chemistryVolcano13. Climate action[SDU]Sciences of the Universe [physics]Environmental chemistrySoil waterAcid rainGeologyGroundwaterSelenium
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Eustasy and sea water Sr composition: application to high-resolution Sr-isotope stratigraphy of Miocene shallow-water carbonates

2007

Oceanic 87 Sr/ 86 Sr-isotope ratios are strongly influenced by rates of silicate weathering and therefore linked not only to glaciation but also to sea-level change. The present study combines analysis of sequence stratigraphy and basin architecture with Sr-isotope stratigraphy in Miocene shallow-water sediments in southern Portugal and Crete (Greece). The common method is to use smoothed global sea water Sr-isotope reference curves but here a different approach is chosen. Instead, measured Sr-isotope curves are correlated with unsmoothed reference curves by identification of similar fluctuations in the order of several 100 kyr. Transgressive intervals are characterized by increasing Sr-iso…

010504 meteorology & atmospheric sciencesStratigraphy550 - Earth sciencesGeologyWeathering010502 geochemistry & geophysics01 natural sciencesSilicateWaves and shallow waterPaleontologychemistry.chemical_compoundStratigraphychemistry13. Climate actionDeglaciationSequence stratigraphySedimentary rock14. Life underwaterChronostratigraphyGeology0105 earth and related environmental sciencesSedimentology
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Geodynamic control on carbonate diagenesis: Petrographic and isotopic investigation of the Upper Jurassic formations of the Paris Basin (France).

2007

23 pages; International audience; The Oxfordian and Kimmeridgian carbonates of the eastern edge of the Paris Basin display poor reservoir properties (Φb15% and Kb0.1 md). The petrographic investigation and the resultant paragenetic sequence show that this is due to extensive precipitation of 2 types of almost synchronous blocky LMC (Low Magnesian Calcite) cements during mesogenesis (burial). Stable isotope investigation of these non-recrystallized cements, through both microdrilling sampling and in-situ SIMS (Secondary IonMass Spectrometry) analysis, shows that they originated from slightly buffered meteoric fluids (−3‰SMOW to −8‰SMOW) flowing through the Malm carbonate aquifers of the east…

010504 meteorology & atmospheric sciencesStratigraphy[SDE.MCG]Environmental Sciences/Global ChangesCarbonates010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyBasin evolution01 natural sciencesUnconformityDiagenesisPetrographyPaleontologychemistry.chemical_compoundUnconformities[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryLower Cretaceous0105 earth and related environmental sciencesStable isotopesgeographygeography.geographical_feature_categoryGeologyMassif[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryCretaceousDiagenesis[ SDE.MCG ] Environmental Sciences/Global ChangesDenudationchemistry[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyMeteoric waterCarbonateGeology
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Children’s exposure to polycyclic aromatic hydrocarbons in the Valencian Region (Spain): Urinary levels, predictors of exposure and risk assessment

2021

Polycyclic aromatic hydrocarbons (PAHs) are pollutants that are released into the environment during incomplete combustion of organic matter and which can have a negative effect on human health. PAHs enter the human body mostly through ingestion of food or inhalation of tobacco smoke. The purpose of the present study is to evaluate the internal levels of PAHs that children living in the Valencian Region (Spain) are exposed to. In total, we measured eleven biomarkers of exposure to naphthalene, fluorene, phenanthrene, pyrene, and benzo(a)pyrene in the urine of 566 children aged 5-12. The analytical method was based on a liquid-liquid extraction of the PAH metabolites from the urine samples, …

010504 meteorology & atmospheric sciencesUrine010501 environmental sciencesFluoreneUrineRisk Assessment01 natural sciencesTobacco smokeReference valueschemistry.chemical_compoundEnvironmental healthBenzo(a)pyreneHumansMedicineIngestionGE1-350ChildChildren0105 earth and related environmental sciencesGeneral Environmental Sciencebusiness.industryPhenanthrenePolycyclic aromatic hydrocarbonsHuman biomonitoringEnvironmental scienceschemistrySpainPyreneEnvironmental PollutantsbusinessRisk assessmentBody mass indexBiomarkersEnvironment International
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Nitrogen broadening of SF6 transitions in the nu3 band

2001

Abstract Nitrogen induced pressure-broadened halfwidths of a number of ν3 transitions of SF6 are calculated using the complex Robert–Bonamy (CRB) formalism. The calculations are made at 200, 250, 296 and 350 K and the temperature dependence of the halfwidths are determined. The intermolecular potential is taken as a sum of the leading electrostatic and Lennard-Jones [6] , [7] , [8] , [9] , [10] , [11] , [12] atom–atom components. The dynamics of the collision process are correct to second order in time. The calculated halfwidths are used to simulate the ν3 spectrum, which is compared to a simulation made using the HITRAN96 halfwidths and measurements made at the Universite Pierre et Marie C…

010504 meteorology & atmospheric sciences[ PHYS.QPHY ] Physics [physics]/Quantum Physics [quant-ph]Organic Chemistrychemistry.chemical_elementSulfur hexafluoride01 natural sciencesNitrogenAnalytical ChemistryMarie curieInorganic ChemistrySulfur hexafluoridechemistry.chemical_compoundFormalism (philosophy of mathematics)chemistry[PHYS.QPHY]Physics [physics]/Quantum Physics [quant-ph]0103 physical sciencesIntermolecular potentialTemperature dependence of the halfwidthHalfwidthsAtomic physicsLine broadening010306 general physicsSpectroscopy0105 earth and related environmental sciences
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Chlorine Partitioning Between a Basaltic Melt and H2O-CO2 Fluids at Mount Etna

2009

Partitioning experiments between a basaltic melt from Mt. Etna and a low-density hydrous fluid or vapor containing H(2)O or H(2)O-CO(2) were performed at 1200-1260 degrees C, at pressures between 1 and 200 MPa, either near the nickel-nickel oxide (NNO) buffer or at two log units above it (NNO + 2), and with different chloride concentrations. Most of the experiments were done at chloride-brine-undersaturated conditions, although at the highest Cl concentrations explored brine saturation might have been reached. The average partition coefficients (D(Cl)(fluid/melt)) over the range of Cl concentrations were derived on a weight basis by plotting the calculated concentrations of Cl in the fluid …

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesOxideAnalytical chemistrychemistry.chemical_elementMineralogyBasaltic melt010502 geochemistry & geophysics01 natural sciencesChloridechemistry.chemical_compoundGeochemistry and PetrologyCl solubilityChlorinemedicine[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyFugacity0105 earth and related environmental sciencesBasalthalogen degassingGeologySilicateSettore GEO/08 - Geochimica E VulcanologiaPartition coefficientBrinechemistry13. Climate actionFluid/melt partitioningMount EtnaChlorineGeologymedicine.drug
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