Search results for "volcan"

showing 10 items of 899 documents

In situ quantification of the nitrogen content of olivine-hosted melt inclusions from Klyuchevskoy volcano (Kamchatka): Implications for nitrogen rec…

2021

International audience; Assessing the N content of arc magmas and their mantle source remains a challenge because the volatile element composition of melts and gases can be modified during magma ascent, storage, and eruption. Given that melt inclusions (MIs) in Mg-rich olivine represent the best proxies for primary arc melts, we applied, for the first time, an in situ high-resolution secondary ion mass spectrometry (SIMS) method to determine the N concentration in olivine-hosted MIs from Klyuchevskoy volcano in Kamchatka. To reverse the effects of post-entrapment modification processes (i.e., exsolution of volatiles into a fluid bubble), the MIs were partially to completely homogenized at h…

Klyuchevskoy volcano010504 meteorology & atmospheric sciencesNitrogenMineralogyvolatile recyclingengineering.material010502 geochemistry & geophysicsmelt inclusions01 natural sciencesMantle (geology)Geochemistry and Petrology0105 earth and related environmental sciencesMelt inclusionsgeographygeography.geographical_feature_categoryOlivineSubductionGeologyCrustVolcano13. Climate action[SDU]Sciences of the Universe [physics]MagmaMagmatismengineeringSIMSsubductionGeology
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Reply to the “Comment by Delmelle et al. (2013) on ‘Scavenging of sulfur, halogens and trace metals by volcanic ash: The 2010 Eyjafjallajökull erupti…

2014

Abstract With this short communication we address the principal issues raised by Delmelle et al. (2014) in relation to the work of Bagnato et al. (2013) concerning the 2010 eruption of Eyjafjallajokull, Iceland. The principal conclusions of the work of Bagnato et al. (2013) include the observation that protracted gas-aerosol interaction in the plume promotes selective leaching of cation species from ash, with alkalis and Ca (and, among trace elements, Zn and Cu) being more rapidly re-mobilized (and transferred to soluble surface salts) relative to more inert elements (Mg, Ti). They also observed that adsorption onto ash surfaces is a major atmospheric sink of volcanic acidic gases, with 282…

LEACHING OF ASHgeographygeography.geographical_feature_categoryChemistryMineralogychemistry.chemical_elementexplosive volcanismSulfurSettore GEO/08 - Geochimica E VulcanologiaPlumeexplosive volcanism; VOLCANIC ASH; EyjafjallajökullAdsorptionEyjafjallajökullVolcanoVOLCANIC ACID GASGeochemistry and PetrologyINTERACTION ASH-PLUMEHalogenddc:5502010 EYJAFJALLAJOKULL ERUPTIONSelective leachingVOLCANIC ASHScavengingVolcanic ashGeochimica et Cosmochimica Acta
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Hydromechanical behaviour of a volcanic ash

2013

This paper presents experimental analysis and numerical modelling aimed at improved understanding and prediction of the hydromechanical behaviour of volcanic ash at various states of saturation. Results from a comprehensive experimental programme are presented in order to characterise the response of the material in terms of matric suction and confining stress changes. The evolution of the yield stress at different suction levels has been quantified. The volumetric response with suction variations allowed the analysis of the collapse-upon-wetting behaviour. Water retention and permeability are also addressed. Tests results are used to calibrate a constitutive model based on the effective s…

Laboratory testPartial saturationEffective stressEarth and Planetary Sciences (miscellaneous)Constitutive relationGeotechnical engineeringSuctionGeotechnical Engineering and Engineering GeologySaturation (chemistry)Partial saturationGeologyCollapsed settlementVolcanic ashGéotechnique
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Yttrium and lanthanides in human lung fluids, probing the exposure to atmospheric fallout.

2011

International audience; Inhalation of airborne particles can produce crystallization of phosphatic microcrysts in intraaveolar areas of lungs, sometimes degenerating into pulmonary fibrosis. Results of this study indicate that these pathologies are induced by interactions between lung fluids and inhaled atmospheric dust in people exposed to volcanic dust ejected from Mount Etna in 2001. Here, the lung solid-liquid interaction is evaluated by the distribution of yttrium and lanthanides (YLn) in fluid bronchoalveolar lavages on selected individuals according the classical geochemical approaches. We found that shale-normalised patterns of yttrium and lanthanides have a 'V shaped' feature corre…

Lanthanide010504 meteorology & atmospheric sciencesHealth Toxicology and Mutagenesis550 - Earth sciences010501 environmental sciences01 natural sciencesLanthanoid Series ElementsACTIVATED COMPLEXMass SpectrometryHuman lungLanthanideELEMENTSYttrium RadioisotopesYttriumWaste Management and DisposalLungInhalation ExposureInhalationDendriform pulmonary ossificationSEAWATERPollutionmedicine.anatomical_structureItalyEnvironmental chemistryThermodynamicsBronchoalveolar Lavage FluidAlgorithmsBronchoalveolar lavageCHEMICAL-REACTIONSEnvironmental EngineeringChromatography Gas[SDU.STU]Sciences of the Universe [physics]/Earth Scienceschemistry.chemical_elementMineralogyVolcanic EruptionsWATERSmedicinebronchoalveaolar lavagesPARTICLESEnvironmental ChemistryHumansIn patientDISSOLUTION RATES0105 earth and related environmental sciencesRARE-EARTH PNEUMOCONIOSISPrecipitation (chemistry)YttriumEnvironmental ExposureAerosolSettore GEO/08 - Geochimica E VulcanologiachemistryModels ChemicalMedical geochemistry13. Climate actionMedical geochemistry; Lanthanide; bronchoalveaolar lavagesVolcanic ashVolcanic ash
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Volatiles in pantellerite magmas: A case study of the Green Tuff Plinian eruption (Island of Pantelleria, Italy)

2013

Abstract The Green Tuff (GT) Plinian eruption, the largest in magnitude at Pantelleria, erupted 3 to 7 km3 DRE of pantellerite magma and a small volume of trachyte. Fifty-nine anorthoclase-hosted melt inclusions from the two basal pumice members were analyzed by FT-IR spectroscopy in order to assess the pre-eruptive H2O content in the pantellerite melt. Microanalytical methods were used to determine major element, Cl, F and S contents. Melt inclusions and glassy groundmasses have a nearly homogeneous pantelleritic composition (peralkaline index = 1.9-2.2) and variable water contents ranging from 1.4 to as high as 4.2 wt %, i.e. much higher than the 1.4 wt % of earlier published studies. The…

LavaSettore GEO/07 - Petrologia E PetrografiaGeochemistryTrachyteMagma chamberStrombolian eruptionGeophysicsEffusive eruptionGeochemistry and PetrologyPumiceMagmaThe Green Tuff (GT) Plinian eruption the largest in magnitude at Pantelleria erupted 3 to 7 km 3 DRE of pantellerite magma and a small volume of trachyte. Fifty-nine anorthoclase-hosted melt inclusions from the two basal pumice members were analyzed by FT-IR spectroscopy in order to assess the pre-eruptive H2Ocontent in the pantellerite melt. Microanalytical methods were used to determine major element Cl F and S contents. Melt inclusions and glassy groundmasses have a nearly homogeneous pantelleritic composition (peralkaline index = 1.9-2.2) and variable water contents ranging from 1.4 to as high as 4.2 wt % i.e. much higher than the 1.4 wt % of earlier published studies. The chlorine content is constant at about 1 wt %. Combined Cl and H2O data were used to estimate a confining pressure of about 50 MPa (depth around 2-3 km) for the GT magma chamber. The chamber was characterized by a compositional zoning with a dominant pantellerite overlying a trachyte magma. Soon after the GT eruption intra-caldera volcanism was dominated by the eruption of voluminous trachyte lavaflows while pantellerite melt production resumed after about 20 ka with numerous low-volume mildly explosive (Strombolian) to effusive eruptions. Comparison with data from the literature reveals that despite the differentexplosivity the post-caldera Strombolian eruptions and the GT Plinian eruption were fed by pantelleritic magmas with similar water contents. Chlorine and CO2contents suggest that the young magma reservoirs feeding the Strombolian to effusive activity were deeper (h≥4.5 km) than the much larger (based on erupted volumes) magma chamber which fed the GT eruptionGeologyMelt inclusionsJournal of Volcanology and Geothermal Research
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Short-term occupations at high elevation during the Middle Paleolithic at Kalavan 2 (Republic of Armenia).

2021

The Armenian highlands encompasses rugged and environmentally diverse landscapes and is characterized by a mosaic of distinct ecological niches and large temperature gradients. Strong seasonal fluctuations in resource availability along topographic gradients likely prompted Pleistocene hominin groups to adapt by adjusting their mobility strategies. However, the role that elevated landscapes played in hunter-gatherer settlement systems during the Late Pleistocene (Middle Palaeolithic [MP]) remains poorly understood. At 1640 m above sea level, the MP site of Kalavan 2 (Armenia) is ideally positioned for testing hypotheses involving elevation-dependent seasonal mobility and subsistence strateg…

Lesser CaucasusTechnologyHominidsSteppeStratigraphySocial SciencesMarine and Aquatic Scienceshabitat selection010502 geochemistry & geophysics01 natural sciences[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMiddle Paleolithic0601 history and archaeologyHistory AncientSedimentary Geologyraw-materialMultidisciplinarygeography.geographical_feature_category060102 archaeologyEcologyFossilsAltitudeQRexplosive eruptionsHominidaeGeology06 humanities and the arts[SHS.GEO]Humanities and Social Sciences/GeographyArmeniaGeographyArchaeology[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphylanguageMedicineVolcanoesSeasonsPhysical AnthropologyGeghama highlandArtifactsResearch ArticleFreshwater EnvironmentsVolcanic GlassObsidianPleistocene[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryScience[SDE.MCG]Environmental Sciences/Global ChangesVolcanology930obsidian artifactsArchaic HumansRiversIgneous GeologyPaleoanthropologyAnimalsHumansHominins[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/HydrologyOccupations[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentSea level0105 earth and related environmental sciencesPetrologyEcological niche[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonicsvolcano Eastern AnatoliaArmenianEcology and Environmental SciencesSubsistence agricultureBiology and Life SciencesPaleontologyAquatic EnvironmentsBodies of Water900 Geschichte und Geografie::930 Geschichte des Altertums (bis ca. 499) Archäologie::930 Geschichte des Altertums bis ca. 499 Archäologie[SDE.ES]Environmental Sciences/Environmental and Societylanguage.human_languagewax n-alkanesPaleoanthropology[SHS.ENVIR]Humanities and Social Sciences/Environmental studiesAnthropologyEarth SciencesAnimal MigrationSedimentPloS one
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Trench-parallel spreading ridge subduction and its consequences for the geological evolution of the overriding plate: Insights from analogue models a…

2018

A series of 3-D asthenospheric-scale analogue models have been conducted in the laboratory in order to simulate the arrival of a spreading ridge at the trench and understand its effect on plate kinematics, slab geometry, and on the deformation of the overriding plate. These models are made of a two-layered linearly viscous system simulating the lithosphere and asthenosphere. We reproduce the progressive decrease in thickness of the oceanic lithosphere at the trench. We measure plate kinematics, slab geometry and upper plate deformation. Our experiments reveal that the subduction of a thinning plate beneath a freely moving overriding continent favors a decrease of the subduction velocity and…

Lithosphere010504 meteorology & atmospheric sciences010502 geochemistry & geophysicsGeociencias multidisciplinaria01 natural sciencesCiencias de la Tierra y relacionadas con el Medio AmbienteSUBDUCTIONAnalogue modelingLithosphereAsthenospherePatagoniaOceanic ridgeSouthernmost AndesANALOGUE MODELING0105 earth and related environmental sciencesEarth-Surface Processes[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/TectonicsgeographySLAB PULL FORCEgeography.geographical_feature_categoryVolcanic arcSubductionMid-ocean ridge[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/TectonicsSubductionLITHOSPHEREPATAGONIAGeophysicsRidgeTrenchSlabSOUTHERNMOST ANDESSlab pull forceOCEANIC RIDGEGeologySeismologyCIENCIAS NATURALES Y EXACTAS
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Degassing of gaseous (elemental and reactive) and particulate mercury from Mount Etna volcano (Southern Italy)

2007

Abstract There is an urgent need to better constrain the global rates of mercury degassing from natural sources, including active volcanoes. Hitherto, estimates of volcanic fluxes have been limited by the poorly determined speciation of Hg in volcanic emissions. Here, we present a systematic characterisation of mercury partitioning between gaseous (Hg(g)) and particulate (Hg(p)) forms in the volcanic plume of Mount Etna, the largest open-vent passively degassing volcano on Earth. We demonstrate that mercury transport is predominantly in the gas phase, with a mean Hg(p)/Hg(g) ratio of ∼0.01 by mass. We also present the first simultaneous measurement of divalent gaseous mercury ( Hg ( g ) II …

MERCUREAtmospheric Sciencegeographygeography.geographical_feature_categorychemistry.chemical_elementMineralogyVolcanismParticulatesHgMercury (element)PlumeFlux (metallurgy)chemistryVolcanoEnvironmental chemistryPanacheGeologyGeneral Environmental ScienceAtmospheric Environment
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Mercury and halogen emissions from Masaya and Telica volcanoes, Nicaragua

2008

We report measurements of Hg, SO2, and halogens (HCl, HBr, HI) in volcanic gases from Masaya volcano, Nicaragua, and gaseous SO2 and halogens from Telica volcano, Nicaragua. Mercury measurements were made with a Lumex 915+ portable mercury vapor analyzer and gold traps, while halogens, CO2 and S species were monitored with a portable multi gas sensor and filter packs. Lumex Hg concentrations in the plume were consistently above background and ranged up to 350 ng m-3. Hg/SO2 mass ratios measured with the real-time instruments ranged from 1.1 × 10-7 to 3.5 × 10-5 (mean 2 × 10-5). Total gaseous mercury (TGM) concentrations measured by gold trap ranged from 100 to 225 ng m-3. Reactive gaseous m…

MERCUREAtmospheric SciencemercuryAnalytical chemistrySoil Sciencechemistry.chemical_elementMineralogyvolcanoesAquatic ScienceOceanographyVolcanic Gaseschemistry.chemical_compoundFlux (metallurgy)Geochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)eventEarth-Surface ProcessesWater Science and Technologyevent.disaster_typeEcologyGeographyHydrogen bromidePaleontologyForestryFumaroleSettore GEO/08 - Geochimica E VulcanologiaMercury (element)PlumeEarth sciencesGeophysicschemistrySpace and Planetary ScienceHalogen
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Enhanced volcanic hot-spot detection using MODIS IR data: results from the MIROVA system

2015

We describe a new volcanic hotspot detection system, named Middle InfraRed Observation of Volcanic Activity (MIROVA), based on the analysis of infrared data acquired by the Moderate Resolution Imaging Spectroradiometer sensor (MODIS). MIROVA uses the middle infrared radiation (MIR), measured by MODIS, in order to detect and measure the heat radiation deriving from volcanic activity. The algorithm combines spectral and spatial principles, allowing the detection of heat sources from 1 megawatt (MW) to more than 10 gigawatt (GW). This provides a unique opportunity to: (i) recognize small-scale variations in thermal output that may precede the onset of effusive activity; (ii) track the advance …

MODIS automatic global detection of volcanic activitythermal anomaliesMODISHot spot detection system thermal anomalies MODIS MIROVAMIROVAHot spot detection system
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