0000000000283212

AUTHOR

Antonella Bertagnini

showing 5 related works from this author

Magma and volatile supply to post-collapse volcanism and block resurgence in Siwi caldera (Tanna Island, Vanuatu arc)

2011

Siwi caldera, in the Vanuatu arc (Tanna island), is a rare volcanic complex where both persistent eruptive activity (Yasur volcano) and rapid block resurgence (Yenkahe horst) can be investigated simultaneously during a post-caldera stage. Here we provide new constraints on the feeding system of this volcanic complex, based on a detailed study of the petrology, geochemistry and volatile content of Yasur-Siwi bulk-rocks and melt inclusions, combined with measurements of the chemical composition and mass fluxes of Yasur volcanic gases. Major and trace element analyses of Yasur-Siwi volcanic rocks, together with literature data for other volcanic centers, point to a single magmatic series and p…

blockEarth scienceAndesiteYasur magmatic degassingvolcano thermal budgetVanuatu arcGeochemistryPyroclastic rockVolcanologyVolcanismmelt inclusionsBlock (meteorology)volatilesGeophysicsGeochemistry and PetrologyresurgentMagma[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyCalderagas fluxes[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentYasurGeologyMelt inclusions
researchProduct

A model of degassing for Stromboli volcano

2010

International audience; A better understanding of degassing processes at open-vent basaltic volcanoes requires collection of new datasets of H2O–CO2–SO2 volcanic gas plume compositions, which acquisition has long been hampered by technical limitations. Here, we use the MultiGAS technique to provide the best-documented record of gas plume discharges from Stromboli volcano to date. We show that Stromboli's gases are dominated by H2O (48–98 mol%; mean, 80%), and by CO2 (2–50 mol%; mean, 17%) and SO2 (0.2–14 mol%; mean, 3%). The significant temporal variability in our dataset reflects the dynamic nature of degassing process during Strombolian activity; which we explore by interpreting our gas m…

volcanic gase010504 meteorology & atmospheric sciencesEarth science010502 geochemistry & geophysics01 natural sciencesVolcanic Gasesvolcanic degassing; Stromboli; volcanic gases; CO2 fluxingGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)eventStromboliPetrology0105 earth and related environmental sciencesBasaltevent.disaster_typegeographygeography.geographical_feature_categoryStrombolian eruptionSettore GEO/08 - Geochimica E VulcanologiaPlumeGeophysicsVolcanovolcanic gases13. Climate actionSpace and Planetary ScienceMagmaCO2 fluxingInclusion (mineral)[SDU.OTHER]Sciences of the Universe [physics]/OtherSaturation (chemistry)volcanic degassingGeologyEarth and Planetary Science Letters
researchProduct

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
researchProduct

Prodigious emission rates and magma degassing budget of major, trace and radioactive volatile species from Ambrym basaltic volcano, Vanuatu island Arc

2016

Abstract Ambrym volcano, in the Vanuatu arc, is one of the most active volcanoes of the Southwest Pacific region, where persistent lava lake and/or Strombolian activity sustains voluminous gas plume emissions. Here we report on the first comprehensive budget for the discharge of major, minor, trace and radioactive volatile species from Ambrym volcano, as well as the first data for volatiles dissolved in its basaltic magma (olivine-hosted melt inclusions). In situ MultiGAS analysis of H 2 O, CO 2 , SO 2 and H 2 S in crater rim emissions, coupled with filter-pack determination of SO 2 , halogens, stable and radioactive metals demonstrates a common magmatic source for volcanic gases emitted by…

010504 meteorology & atmospheric sciencesLavaGeochemistryMineralogy[SDU.STU]Sciences of the Universe [physics]/Earth SciencesAmbrymVolatile fluxes010502 geochemistry & geophysics01 natural sciencesVolcanic GasesMagma reservoirVanuatuVolatile fluxeGeochemistry and PetrologyCalderaeventGeophysicComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesMelt inclusionsBasaltevent.disaster_typegeographygeography.geographical_feature_categoryMagma degassing budgetStrombolian eruptionGeophysicsVolcano13. Climate actionIsland arcRadioactive disequilibriaGeology
researchProduct

Scavenging of sulphur, halogens and trace metals by volcanic ash: The 2010 Eyjafjallajökull eruption

2013

The Eyjafjallajökull volcanic eruption in 2010 released considerable amounts of ash into the high troposphere-low stratosphere, leading to unprecedented disruption of air traffic over Europe. The role of such fine-grained tephra in adsorbing, and therefore rapidly scavenging, volcanogenic volatile elements such as sulphur and halogens, is explored here. We report on results (major to trace element chemistry) of leaching experiments carried out on 20 volcanic ash samples, taken from the deposits of the main phases of the eruption (March–April 2010), or directly while falling (5–9 May 2010). Ash leachate solutions from Eyjafjallajökull are dominated – among cations – by Ca and Na, and display…

Mineralogyexplosive volcanismvolcanic eruptionVolcanic GasesGeochemistry and Petrologyddc:550eventTrace metalVOLCANIC ASHmonitoring systemTephraVolatilesScavengingevent.disaster_typeVulcanian eruptionplumeChemistrystratosphere-troposphere interactionTrace elementtephrahalogentrace metalexplosive volcanism; VOLCANIC ASH; EyjafjallajökullEyjafjallajökullsulfurEnvironmental chemistryvolcanic gasVolcanic ashGeochimica et Cosmochimica Acta
researchProduct