Search results for "ISOTOPES"

showing 10 items of 1216 documents

Genesis of fumarolic emissions as inferred by isotope mass balances: CO 2 and water at Vulcano Island, Italy

2002

We have developed a quantitative model of CO2 and H2O isotopic mixing between magmatic and hydrothermal gases for the fumarolic emissions of the La Fossa crater (Vulcano Island, Italy). On the basis of isotope balance equations, the model takes into account the isotope equilibrium between H2O and CO2 and extends the recent model of chemical and energy two-end-member mixing by Nuccio et al. (1999). As a result, the H2O and CO2 content and the δD, δ18O, and δ13C isotope compositions for both magmatic and hydrothermal end-members have been assessed. Low contributions of meteoric steam, added at a shallow depth, have been also recognized and quantified in the fumaroles throughout the period fro…

Volcanic Gasesevent.disaster_typeMagmatic waterIsotope fractionationGeochemistry and PetrologyStable isotope ratioIsotope geochemistryGeochemistryeventFumaroleHydrothermal circulationGeologyIsotopes of oxygenGeochimica et Cosmochimica Acta
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Geochemistry and isotope composition (Sr, Pb, δ66Zn) of Vulcano fumaroles (Aeolian Islands, Italy)

2018

We present and discuss temperatures, major and trace element gas geochemistry, radiogenic isotopes (Pb, Sr) and the first Zn isotope data of fumarole condensates and altered rocks from the Vulcano fumarolic field. The fumaroles of the La Fossa cone, sampled on 5th May 2015, have temperatures ranging between 233 and 427 °C. They plot compositionally on the mixing trend between the magmatic and hydrothermal end-members defined by previous studies, but are strongly displaced towards the hydrothermal component. Correlations of radiogenic (Sr, Pb) and stable isotopes of Zn with δ13CCO2 and several trace elements of the fumarolic acid condensates support mixing between the above mentioned distinc…

Volcanic gase010504 meteorology & atmospheric sciencesVulcano IslandGeochemistryFumarole010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationRadiogenic isotopeGeochemistry and Petrologyddc:550Volcanic gasesRadiogenic isotopes0105 earth and related environmental sciencesZinc isotopegeographygeography.geographical_feature_categoryRadiogenic nuclideIsotopeStable isotope ratioTrace elementGeologyFumarolesAeolian IslandFumaroleEquilibrium fractionationAeolian IslandsVolcanic rockGeochemistryZinc isotopesGeology
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Isotopically (δ13C and δ18O) heavy volcanic plumes from Central Andean volcanoes: a field study

2017

International audience; Stable isotopes of carbon and oxygen in volcanic gases are key tracers of volatile transfer between Earth's interior and atmosphere. Although important, these data are available for few volcanoes because they have traditionally been difficult to obtain and are usually measured on gas samples collected from fumaroles. We present new field measurements of bulk plume composition and stable isotopes (δ13CCO2 and δ18OH2O+CO2) carried out at three northern Chilean volcanoes using MultiGAS and isotope ratio infrared spectroscopy. Carbon and oxygen in magmatic gas plumes of Lastarria and Isluga volcanoes have δ13C in CO2 of +0.76‰ to +0.77‰ (VPDB), similar to slab carbonate;…

Volcanic gase010504 meteorology & atmospheric sciencesδ18Oδ13CEarth scienceGeochemistry010502 geochemistry & geophysics01 natural sciencesVolcanic GasesIsotopic signatureGeochemistry and Petrology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyeventIsotope ratio infrared spectroscopy0105 earth and related environmental sciencesevent.disaster_typegeographygeography.geographical_feature_categoryStable isotope ratioCarbon isotopeδ18OFumaroleVolcanoIsotopes of carbon[SDU]Sciences of the Universe [physics]Kinetic fractionationGeology
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Natural and artificial radioactivity levels in Livingston Island (Antarctic regions).

1994

Radioactive contamination of the sea and land is due, on the one hand, to fallout from atmospheric atomic explosions since 1945, and, on the other, to emissions produced by nuclear and radioactive facilities. Given its geographic position far distant from the aforementioned main sources of radioactive contamination, Antarctica should have the lowest levels that can be measured on the Earth of artificial radionuclides in the various receptor media which are characteristic of the trophic chain. In the case of Antarctica, these are melt-water, sea-water, mosses, algae, and lichens. With the aim of contributing basic information on the radiation levels present in the Antarctic ecosystem, we hav…

Water Pollutants RadioactiveHealth Toxicology and MutagenesisPotassium RadioisotopesMineralogyInduced radioactivityAntarctic RegionsFresh WaterToxicologyTritiumRadioactive contaminationEcosystemSeawaterLichenShetlandRadionuclidegeographygeography.geographical_feature_categoryGeneral MedicinePollutionOceanographyArchipelagoStrontium RadioisotopesEnvironmental scienceUraniumEnvironmental PollutantsEnvironmental PollutionStrontium-90Bulletin of environmental contamination and toxicology
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Evolution of neodymium isotopic signature of seawater during the Late Cretaceous: implications for intermediate and deep circulation.

2016

20 pages; International audience; Neodymium isotopic compositions (εNd) have been largely used for the last fifty years as a tracer of past ocean circulation, and more intensively during the last decade to investigate ocean circulation during the Cretaceous period. Despite a growing set of data, circulation patterns still remain unclear during this period. In particular, the identification of the deep-water masses and their spatial extension within the different oceanic basins are poorly constrained. In this study we present new deep-water εNd data inferred from the Nd isotope composition of fish remains and Fe–Mn oxyhydroxide coatings on foraminifera tests, along with new εNd data of resid…

Water mass010504 meteorology & atmospheric sciences010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesCretaceousBottom waterPaleontologyOcean circulation[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry14. Life underwaterSouthern Ocean0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryNeodymium isotopesNorth Atlantic Deep WaterOcean currentAbyssal plainGeology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryCretaceousOceanography13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyThermohaline circulationOceanic basinGeology
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Water stable isotope data set in temperate, lowland catchment, two years of monthly observations, River Salaca, Latvia

2020

Highlights • Two years of monthly water stable isotope ratios from temperate lowland catchment. • Hourly water table, temperature and electrical conductivity monitoring. • Distinct isotope ratios for raised bog, groundwater and rivers.

Water tableEvaporationDrainage basinWater stable isotopesHydrogeologyGroundwater-surface water interactionlcsh:Computer applications to medicine. Medical informaticsCatchment03 medical and health sciences0302 clinical medicineparasitic diseasesTemperate climatePrecipitationlcsh:Science (General)030304 developmental biologyHydrology0303 health sciencesgeographyMultidisciplinarygeography.geographical_feature_categoryStable isotope ratioIsotope hydrologylcsh:R858-859.7Environmental scienceEarth and Planetary ScienceSurface water030217 neurology & neurosurgeryGroundwaterlcsh:Q1-390Data in Brief
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IBMF and IBFFM Approach to Nuclei in the A≃100 Region

1988

An overview of the calculations in IBFM and IBFFM for nuclei in the A ≃ 100 region is presented. The application to these nuclei with a complex structure including the rapid transition from spherical to deformed nuclear shapes provides a stringent test for the capacities of this theoretical approach. From the result of the studies of the heavy Yttrium isotopes and the N=59 isotones it is concluded that it can account for the basic structure and the phase transition in these nuclei.

Yttrium IsotopesPhysicsPhase transitionNuclear TheoryAtomic physicsNuclear Experiment
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A Neandertal dietary conundrum: Insights provided by tooth enamel Zn isotopes from Gabasa, Spain

2022

The characterization of Neandertals’ diets has mostly relied on nitrogen isotope analyses of bone and tooth collagen. However, few nitrogen isotope data have been recovered from bones or teeth from Iberia due to poor collagen preservation at Paleolithic sites in the region. Zinc isotopes have been shown to be a reliable method for reconstructing trophic levels in the absence of organic matter preservation. Here, we present the results of zinc (Zn), strontium (Sr), carbon (C), and oxygen (O) isotope and trace element ratio analysis measured in dental enamel on a Pleistocene food web in Gabasa, Spain, to characterize the diet and ecology of a Middle Paleolithic Neandertal individual. Based on…

Zinc isotope ratiosCarbon IsotopesMultidisciplinaryMiddle PaleolithicNitrogen IsotopesIberian NeandertalsCarnivoraHomininHome de NeandertalPrehistòriaCarnivoryCarbonDietTrace ElementsOxygenZincSpainStrontiumAnimalsZinc IsotopesCollagenDental EnamelToothNeanderthals
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Effect of cropping cycles and repeated herbicide applications on the degradation of diclofop-methyl, bentazone, diuron, isoproturon and pendimethalin…

2002

A greenhouse study was conducted to investigate the ability of four crops (wheat, corn, oilseed rape and soybean) to influence the degradation of bentazone, diclofop-methyl, diuron, isoproturon and pendimethalin in soil. The present study showed that microbial biomass-carbon was significantly higher in planted soils than in bulk soil, especially with wheat and corn, after several cropping cycles. The biomass in corn and soybean planted soils was adversely affected by bentazone but recovered after three cropping cycles. In wheat-planted soils, diclofop-methyl application resulted in persistent increase of the amount of microbial biomass. Bentazone did not show accelerated degradation even af…

[SDE] Environmental SciencesCrops Agricultural[SDV]Life Sciences [q-bio]Bulk soil010501 environmental sciencesBenzothiadiazinescomplex mixtures01 natural scienceschemistry.chemical_compoundSoilHalogenated Diphenyl EthersBiomassCarbon RadioisotopesComputingMilieux_MISCELLANEOUSSoil Microbiology0105 earth and related environmental sciences2. Zero hungerCambisolRhizosphereMethylurea CompoundsMineralsAniline CompoundsBacteriaChemistryHerbicidesPhenyl EthersPhenylurea Compoundsfungifood and beveragesAgriculture04 agricultural and veterinary sciencesGeneral MedicineMineralization (soil science)15. Life on landPesticideCarbon DioxideEnvironment Controlled[SDV] Life Sciences [q-bio]PendimethalinKineticsAgronomyInsect ScienceDiuronSoil water[SDE]Environmental Sciences040103 agronomy & agriculturePesticide degradation0401 agriculture forestry and fisheriesAgronomy and Crop SciencePest management science
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The transport history of two Saharan dust events archived in an Alpine ice core

2005

Mineral dust from the Saharan desert can be transported across the Mediterranean towards the Alpine region several times a year. When coinciding with snowfall, the dust can be deposited on Alpine glaciers and then appears as yellow or red layers in ice cores. Two such significant dust events were identified in an ice core drilled at the high-accumulation site Piz Zupó in the Swiss Alps (46°22' N, 9°55' E, 3850 m a.s.l.). From stable oxygen isotopes and major ion concentrations, the events were approximately dated as October and March 2000. In order to link the dust record in the ice core to the meteorological situation that led to the dust events, a novel methodology based on b…

[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereAtmospheric Sciencegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciences[SDU.OCEAN] Sciences of the Universe [physics]/Ocean AtmosphereGlacierMineral dustSnowAtmospheric sciences010502 geochemistry & geophysics01 natural sciencesIsotopes of oxygenlcsh:QC1-999Aerosollcsh:ChemistryDeposition (aerosol physics)Ice corelcsh:QD1-99913. Climate actionPaleoclimatologyGeologylcsh:Physics0105 earth and related environmental sciences
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