0000000000679207

AUTHOR

C. Minopoli

showing 3 related works from this author

Escalating CO2 degassing at the Pisciarelli fumarolic system, and implications for the ongoing Campi Flegrei unrest

2019

Abstract This short communication aims at providing an updated report on degassing activity and ground deformation variations observed during the ongoing (2012–2019) Campi Flegrei caldera unrest, with a particular focus on Pisciarelli, currently its most active fumarolic field. We show that the CO2 flux from the main Pisciarelli fumarolic vent (referred as “Soffione”) has increased by a factor > 3 since 2012, reaching in 2018–2019 levels (>600 tons/day) that are comparable to those typical of a medium-sized erupting arc volcano. A substantial widening of the degassing vents and bubbling pools, and a further increase in CO2 concentrations in ambient air (up to 6000 ppm), have also been detec…

event.disaster_typegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesCo2 fluxInduced seismicityUnrest010502 geochemistry & geophysics01 natural sciencesGas monitoringAmbient airVolcanic GasesGeophysicsVolcanoGeochemistry and PetrologyCalderaeventvolcanic gases Campi FlegreiPetrologyGeology0105 earth and related environmental sciences
researchProduct

First simultaneous mercury and major volatiles characterization of atmospheric hydrothermal emissions at the Pisciarelli's fumarolic system (Campi Fl…

2020

Abstract Hydrothermal systems with active surface expressions are important natural source of atmospheric mercury. Here we report on the first simultaneous assessment of gaseous elemental mercury (GEM) and major volatiles (H2S and CO2) fluxes from the fumarolic system of Pisciarelli, currently the most active at the Campi Flegrei caldera (CFc), Naples (Italy). This was achieved via a GPS-synchronized Lumex and MultiGAS survey which extends similar investigations reported elsewhere. GEM concentrations measured in the fumarolic emissions were consistently above background air level close to the degassing area (mean ~ 8 ± 3 ng m−3 on average) and ranged up to 12,000 ng m−3. Our data evidenced …

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesMineralogychemistry.chemical_elementAtmospheric dispersion modeling010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationFumarolePlumeMercury (element)GeophysicsFlux (metallurgy)VolcanochemistryGeochemistry and PetrologyCalderaGeology0105 earth and related environmental sciencesJournal of Volcanology and Geothermal Research
researchProduct

Evidence of a recent input of magmatic gases into the quiescent volcanic edifice of Panarea, Aeolian Islands, Italy

2004

- Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Vesuviano, Naples, Italy. - Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Palermo, Palermo, Italy. - Dipartimento Chimica e Fisica della Terra ed Applicazioni, Palermo, Italy.

geographyPaleontologyGeophysicsgeography.geographical_feature_categoryMediterranean seaVolcanoImpact craterGeneral Earth and Planetary SciencesAeolian processesGeologySeismologyWest mediterraneanGeophysical Research Letters
researchProduct