Search results for "COMPOSITI"

showing 10 items of 2775 documents

Mercury gas emissions from La Soufrière Volcano, Guadeloupe Island (Lesser Antilles)

2009

Abstract Quantifying mercury (Hg) emissions from active volcanoes is of particular interest for better constraining the global cycle and environmental impact of this highly toxic element. Here we report on the abundance of total gaseous (TGM = Hg 0 (g)  + Hg II (g) ) and particulate (Hg (p) ) mercury in the summit gas emissions of La Soufriere andesitic volcano (Guadeloupe island, Lesser Antilles), where enhanced degassing of mixed hydrothermal-magmatic volatiles has been occurring since 1992 from the Southern summit crater. We demonstrate that Hg in volcanic plume occurs predominantly as gaseous mercury, with a mean TGM/Hg (p) mass ratio of ~ 63. Combining the mean TGM/H 2 S mass ratio of …

geographygeography.geographical_feature_categoryAndesitevolcanic plumeMineralogychemistry.chemical_elementGeologyMercuryParticulatesfumaroleAtmospheric sciencestrace metalFumaroleSettore GEO/08 - Geochimica E VulcanologiaPlumeMercury (element)Impact craterVolcanochemistryGeochemistry and Petrologyemission rate.gaseous and particulate mercuryChemical compositionGeologyChemical Geology
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Plume composition and volatile flux of Nyamulagira volcano, Democratic Republic of Congo, during birth and evolution of the lava lake, 2014-2015

2017

Very little is known about the volatile element makeup of the gaseous emissions of Nyamulagira volcano. This paper tries to fill this gap by reporting the first gas composition measurements of Nyamulagira’s volcanic plume since the onset of its lava lake activity at the end of 2014. Two field surveys were carried out on 1 November 2014, and 13–15 October 2015. We applied a broad toolbox of volcanic gas composition measurement techniques in order to geochemically characterize Nyamulagira’s plume. Nyamulagira is a significant emitter of SO2, and our measurements confirm this, as we recorded SO2 emissions of up to ~ 14 kt/d during the studied period. In contrast to neighbouring Nyiragongo volc…

geographygeography.geographical_feature_categoryBromine010504 meteorology & atmospheric sciencesHydrogenLavaFluxMineralogychemistry.chemical_elementNyamulagira Plume composition Total gas flux010502 geochemistry & geophysics01 natural sciencesPlumechemistry.chemical_compoundVolcanochemistryGeochemistry and PetrologyGas compositionHydrogen chlorideGeology0105 earth and related environmental sciences
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Multicopter measurements of volcanic gas emissions at Masaya (Nicaragua), Turrialba (Costa Rica) and Stromboli (Italy) volcanoes: Applications for vo…

2017

Abstract. Volcanoes are a natural source of several reactive gases (e.g. sulfur and halogen containing species), as well as non-reactive gases (e.g. carbon dioxide). Besides that, halogen chemistry in volcanic plumes might have important impacts on atmospheric chemistry, carbon to sulfur ratios and sulfur dioxide fluxes are important established parameters to gain information on subsurface processes. In this study we demonstrate the successful deployment of a multirotor UAV (quadcopter) system with custom-made lightweight payloads on board for the compositional analysis and gas flux estimation of volcanic plumes. The various applications and their potential with such new measurement strateg…

geographygeography.geographical_feature_categoryDifferential optical absorption spectroscopyMineralogychemistry.chemical_elementSulfurPlumechemistry.chemical_compoundFlux (metallurgy)VolcanochemistryAtmospheric chemistryGas compositionGeologySulfur dioxide
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Genesis and evolution of the fumaroles of vulcano (Aeolian Islands, Italy): a geochemical model

1981

A geochemical model explaining the presence of fumaroles having different gas composition and temperature at the top of the crater and along the northeastern coast of Vulcano island is proposed. A pressurized biphase (liquid-vapor) reservoir at the depth of about 2 km is hypothesized. Energy and mass balance sheets controlP-T conditions in the system.P-T must vary along a boiling curve of brine as liquid is present. The CO2 content in the steam is governed by the thermodynamic properties of the fluids in the H2-NaCl-CO2 system. On the assumption that oxygen fugacity in the system is between the HM-FMQ oxygen buffers, observed SO2/H2S, CO2/CO, CO/CH4 ratios in the fumarolic gases at the Foss…

geographygeography.geographical_feature_categoryEarth scienceGeochemistryAquiferFumaroleCO2 contentImpact craterVolcanoGeochemistry and PetrologyMineral redox bufferAeolian processesGas compositionGeologyBulletin Volcanologique
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Environmental Radioactivity and Volcanological Features of Three Islands of the Mediterranean Sea (Pantelleria, Ustica and Vulcano)

1996

Abstract The Mediterranean Sea is an area of great interest for its volcanic activities. This paper presents a comparative study of radiometric and chemical data regarding three volcanic islands located in southern Italy (Pantellena, Ustica, and Vulcano) characterized by different magmatic histories. Measurements of radionulide contents and chemical composition of rock samples belonging to the main lithologies present in the three islands were carried out the observed correlations among radiometric, chemical and mineralogical data reflect the differences in the volcanological genesis and suggest some hypotheses on the magmatic evolution.

geographygeography.geographical_feature_categoryEcologyLithologyEarth scienceVolcanic rockMediterranean seaVolcanoMagmatismGeneral Earth and Planetary SciencesEnvironmental radioactivityRadiometric datingChemical compositionEcology Evolution Behavior and SystematicsGeologyGeneral Environmental ScienceChemistry and Ecology
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A christmas gift: Signature of the 24th December 2018 eruption of Mt. Etna on the chemical composition of bulk deposition in eastern sicily

2020

The eruption of Mt. Etna which occurred on December 24th 2018 was characterized by strombolian activity and fire fountains, emitted by the New South-East Crater and along a fissure that propagated towards the SE. The influence of volcanic emissions on atmospheric deposition was clearly detectable at several kilometres from the source. Wet and dry (bulk) deposition samples were collected each month, through a network of eleven collectors, in the areas of Milazzo, and Priolo between June 2018 and June 2019. They were analysed for major ions and trace elements concentrations. The pH values range from 3.9 to 8.3, while the EC values range from 7 to 396 μS cm-1. An extensive neutralization of th…

geographygeography.geographical_feature_categoryGeochemistryGeology010502 geochemistry & geophysicsFluoride Rainwater Trace elements Volcanic emissions01 natural sciencesStrombolian eruptionSettore GEO/08 - Geochimica E Vulcanologiachemistry.chemical_compoundDeposition (aerosol physics)VolcanoImpact craterchemistryGeneral Earth and Planetary SciencesEnvironmental scienceSeawaterSulfateVolatilesChemical composition0105 earth and related environmental sciences
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Chemical and isotopic characterization of the gases of Mount Etna (Italy)

1997

Abstract In the period 1990–1995, 43 samples of dissolved gases in groundwaters (wells, springs and drainage galleries) and 64 samples of free gases (fumaroles, bubbling and soil gases) from the Mount Etna area were collected and analysed. Isotopic analyses were also carried out of both the carbon of the CO 2 in free gases and dissolved inorganic carbon (DIC) in the waters. The chemical composition of the gases depends on the relative abundances of three interacting components. These are gases of (1) atmospheric origin enriched in O 2 and N 2 , present almost exclusively in dissolved gases, (2) deep origin enriched in CO 2 , prevalent in the majority of cases, and (3) more superficial origi…

geographygeography.geographical_feature_categoryMineralogychemistry.chemical_elementNitrogenFumarolechemistry.chemical_compoundGeophysicsVolcanochemistryGeochemistry and PetrologyEnvironmental chemistryIsotope geochemistryDissolved organic carbonCarbon dioxideChemical compositionGroundwaterGeologyJournal of Volcanology and Geothermal Research
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Innovación y TIC en el paisaje sonoro de la música festera a través de la creación de musicomovigramas

2019

Este artículo es parte de un proyecto de investigación sobre el paisaje sonoro, la escucha y la creación y recreación de espacios de educación ambiental y musical. Consiste en una propuesta de creación y utilización de un recurso auditivo-didáctico e interactivo, el musicomovigrama o musicograma en movimiento, para trabajar la escucha y el desarrollo emocional mediante la Fiesta y la música de Moros y Cristianos de Alcoy y su paisaje sonoro. La gran potencialidad de este recurso deriva de su capacidad para ofrecer al alumnado un soporte visual atractivo sincronizado con la progresión de la música que escucha, de tal manera que ambos códigos avancen simultáneamente. El objetivo principal es …

geographygeography.geographical_feature_categoryMovement (music)media_common.quotation_subjectBandes (Música)General MedicineViolin musical stylesExpression (architecture)AestheticsPerceptionNatural (music)Active listeningSociologyComposition (language)Sound (geography)media_commonMúsica Ensenyament
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Minor and trace elements in olivines as probes into early igneous and mantle melting processes

2013

Abstract The trace element composition of olivine is a rapidly growing research area that has several applications of great potential. Mantle olivines can be distinguished from volcanic olivines by lower concentrations of Ca (

geographygeography.geographical_feature_categoryOlivine010504 meteorology & atmospheric sciencesContinental crustMantle metasomatismGeochemistryengineering.material010502 geochemistry & geophysics01 natural sciencesMantle (geology)Igneous rockGeophysicsVolcano13. Climate actionSpace and Planetary ScienceGeochemistry and PetrologyOceanic crustEarth and Planetary Sciences (miscellaneous)Trace element compositionengineeringGeology0105 earth and related environmental sciences
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Trace elements mobility in soils from the active hydrothermal area of Nisyros (Greece)

2014

Nisyros Island, Greece, is a stratovolcano known for its intense hydrothermal activity. On June 2013, during a multidisciplinary field campaign, soil samples were collected in the caldera area to determinate the main mineralogical paragenesis and to investigate the distribution of trace elements concentrations and the possible relationship to the contribution of deep originated fluids. Soil samples were analysed with XRD and for the chemical composition of their leachable (deionized water) and near total (microwave digestion) fraction both for major and trace elements. All data were compared to a local background soil. The results allow to divide the samples in 2 groups: Lakki Plain and Ste…

geographygeography.geographical_feature_categorySoil testvolatile elementslcsh:QC801-809Trace elementtrace elements Greece hydrothermal emissions biomonitoringMineralogyvolcanoeslcsh:QC851-999Hydrothermal circulationSettore GEO/08 - Geochimica E Vulcanologialcsh:Geophysics. Cosmic physicsGeophysicsVolcanoSoil waterCalderalcsh:Meteorology. ClimatologyVolatilesChemical compositionfumarolic gasesGeology
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