Search results for "Mercury flux"

showing 3 items of 3 documents

Mercury emissions from soils and fumaroles of Nea Kameni volcanic centre, Santorini (Greece)

2013

There have been limited studies to date targeting mercury emissions from volcanic fumarolic systems, and no mercury flux data exist for soil or fumarolic emissions at Santorini volcanic complex, Greece. We present results from the first geochemical survey of Hg and major volatile (CO2, H2S, H2O and H-2) concentrations and fluxes in the fumarolic gases released by the volcanic/hydrothermal system of Nea Kameni islet; the active volcanic center of Santorini. These data were obtained using a portable mercury spectrometer (Lumex 915+) for gaseous elemental mercury (GEM) determination, and a Multi-component Gas Analyzer System (Multi-GAS) for major volatiles. Gaseous Elemental Mercury (GEM) conc…

010504 meteorology & atmospheric sciencesvolcanogenic mercury volcanic degassing Santorini mercury flux inventory trace metalsEarth sciencetrace metalsAir pollutionchemistry.chemical_element010502 geochemistry & geophysicsmedicine.disease_cause01 natural scienceschemistry.chemical_compoundGeochemistry and Petrologymercury flux inventorymedicinevolcanogenic mercuryAir quality index0105 earth and related environmental sciencesgeographySantorinigeography.geographical_feature_categoryFumaroleSettore GEO/08 - Geochimica E VulcanologiaMercury (element)GeophysicschemistryVolcano13. Climate actionEnvironmental chemistryCarbon dioxideSoil watervolcanic degassingGeologyGEOCHEMICAL JOURNAL
researchProduct

Mercury fluxes from volcanic and geothermal sources: an update

2014

We review the state of knowledge on global volcanogenic Hg emissions to the atmosphere and present new data from seven active volcanoes (Poás, Rincón de la Vieja, Turrialba, Aso, Mutnovsky, Gorely and Etna) and two geothermal fields (Las Pailas and Las Hornillas). The variability of Hg contents (c. 4–125 ng m−3) measured in gaseous emissions reflects the dynamic nature of volcanic plumes, where the abundances of volatiles are determined by the physical nature of degassing and variable air dilution. Based on our dataset and previous work, we propose that an average Hg/SO2 plume mass ratio of c. 7.8×10−6 (±1.5×10−6; 1 SE, n=13) is best representative of open-conduit quiescent degassing. Takin…

Mercury flux volcanoes budget geothermal areaSettore GEO/08 - Geochimica E Vulcanologia
researchProduct

First combined flux chamber survey of mercury and CO2 emissions from soil diffuse degassing at Solfatara of Pozzuoli crater, Campi Flegrei (Italy): M…

2014

Abstract There have been limited studies to date targeting gaseous elemental mercury (GEM) flux from soil emission in enriched volcanic substrates and its relation with CO 2 release and tectonic structures. In order to evaluate and understand the processes of soil–air exchanges involved at Solfatara of Pozzuoli volcano, the most active zone of Campi Flegrei caldera (Italy), an intensive field measurement survey has been achieved in September 2013 by using high-time resolution techniques. Soil–air exchange fluxes of GEM and CO 2 have been measured simultaneously at 116 points, widely distributed within the crater. Quantification of gas flux has been assessed by using field accumulation chamb…

mercury flux carbon dioxide soil degassinggeographygeography.geographical_feature_categorygenetic structuresMineralogychemistry.chemical_elementHydrothermal circulationMercury (element)Settore GEO/08 - Geochimica E VulcanologiaVolcanic mercurychemistry.chemical_compoundTectonicsGeophysicsFlux (metallurgy)chemistryImpact craterVolcanoCarbon dioxideGeochemistry and PetrologyCarbon dioxideCalderaSoil degassingMercury fluxSolfataraGeology
researchProduct