Search results for " Vulcano"

showing 10 items of 457 documents

Il risarcimento del danno ambientale da inquinamento: modelli di analisi geochimica valutazione monetaria di un eco-socio-sistema fluviale in Sicilia.

2014

danno ambientale sistema fluvialeSettore GEO/08 - Geochimica E Vulcanologia
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The use of shallow dripwater as an isotopic marker of seepage in karst areas: A comparison between Western Sicily (Italy) and the Harz Mountains (Ger…

2013

Abstract The isotopic signature of slow-flowing dripwater collected in caves located in Western Sicily (Italy) was determined for evaluating its possible use as an isotopic tracer of the local groundwater recharge. These spot measures were compared with a longer series of local rain and spring compositions and with other samples taken, under different hydrogeological conditions, in caves of the Harz Mountains (Northern Germany). The slow flowing dripwater from Sicily showed δ 18 O/δD ratios similar to those of local rain and groundwater, demonstrating that these three are all parent waters. A parallel similarity was found in the vertical isotopic gradient (Δδ 18 O) of the three groups of wa…

effective infiltration010504 meteorology & atmospheric sciencesSettore GEO/04 - Geografia Fisica E Geomorfologiaevapotranspirationisotopic composition010502 geochemistry & geophysics01 natural sciencesIsotopic signatureCaveGeochemistry and PetrologyspringwatercaveEnvironmental Chemistryrain0105 earth and related environmental sciencesHydrologygeographyHydrogeologygeography.geographical_feature_categorydripwaterGroundwater rechargeKarstPollution6. Clean waterSettore GEO/08 - Geochimica E VulcanologiaWater resourcesInfiltration (hydrology)GeologyGroundwaterApplied Geochemistry
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Exploring the explosive‐effusive transition using permanent ultra‐violet cameras

2017

Understanding the mechanisms that cause effusive eruptions is the key to mitigating their associated hazard. Here we combine results from permanent ultraviolet (UV) cameras, and from other geophysical observations (seismic very long period, thermal, and infrasonic activity), to characterize volcanic SO2 flux regime in the period prior, during, and after Stromboli's August–November 2014 effusive eruption. We show that, in the 2 months prior to effusion onset, the SO2 flux levels are 2 times average level. We explain this anomalously high SO2 regime as primarily determined by venting of rapidly rising, pressurized SO2-rich gas pockets produced by strombolian explosions being more frequent and…

effusive eruptionVolcanic degassingStrombolian activitySettore GEO/08 - Geochimica E Vulcanologia
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Degassing of halogens from basaltic volcanism: Insights from volcanic gas observations

2009

Abstract The currently available data set of S–Cl–F abundances in volcanic gas plumes and high-temperature fumarolic gas samples from basaltic volcanism is reviewed here in the attempt to derive constraints on the modes of halogen degassing from mafic silicate melts. Apart from large volcano-to-volcano variations, reflecting remarkable differences in volatile abundances in the source magmas, each of the explored volcanoes displays large changes of SO2/HCl and SO2/HF ratios with the style of volcanic activity, with HCl/HF staying fairly constant. Halogen abundances are low and SO2/HCl and SO2/HF are high when fresh (volatile-rich) magmas sustain degassing, as during explosive eruptions, at t…

event.disaster_typeBasaltgeographyExplosive eruptiongeography.geographical_feature_categoryhalogen degassingGeochemistryGeologyVolcanismSilicateSettore GEO/08 - Geochimica E VulcanologiaVolcanic Gaseschemistry.chemical_compoundchemistryVolcanoGeochemistry and PetrologyMagmaeventMaficGeologyChemical Geology
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Total volatile flux from Mount Etna

2008

[1] The Total Volatile (TV) flux from Mount Etna volcano has been characterised for the first time, by summing the simultaneously-evaluated fluxes of the three main volcanogenic volatiles: H2O, CO2 and SO2. SO2 flux was determined by routine DOAS traverse measurements, while H2O and CO2 were evaluated by scaling MultiGAS-sensed H2O/SO2 and CO2/SO2 plume ratios to the UV-sensed SO2 flux. The time-averaged TV flux from Etna is evaluated at ∼21,000 t·day−1, with a large fraction accounted for by H2O (∼13,000 t·day−1). H2O dominates (≥70%) the volatile budget during syn-eruptive degassing, while CO2 and H2O contribute equally to the TV flux during passive degassing. The CO2 flux was observed to…

event.disaster_typeBasaltgeographygeography.geographical_feature_categoryVOLCANIC IMPUT IN ATMOSPHERECo2 fluxGeophysicsAtmospheric sciencesPlumeSettore GEO/08 - Geochimica E VulcanologiaVolcanic GasesGeophysicsFlux (metallurgy)VolcanoTotal volatileGeneral Earth and Planetary ScienceseventGas compositionGeology
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The fumarolic CO2 output from Pico do Fogo volcano (Cape Verde)

2020

The Pico do Fogo volcano, in the Cape Verde Archipelago off the western coasts of Africa, has been the most active volcano in the Macaronesia region in the Central Atlantic, with at least 27 eruptions during the last 500 years. Between eruptions fumarolic activity has been persisting in its summit crater, but limited information exists for the chemistry and output of these gas emissions. Here, we use the results acquired during a field survey in February 2019 to quantify the quiescent summit fumaroles' volatile output for the first time. By combining measurements of the fumarole compositions (using both a portable Multi-GAS and direct sampling of the hottest fumarole) and of the SO2 flux (u…

event.disaster_typeCape VerdeCO2 outputgeographyGEO/07 - PETROLOGIA E PETROGRAFIAgeography.geographical_feature_categoryPico do Fogo volcanoDirect samplingGeochemistryCape Verde CO2 output Pico do Fogo volcano Volcani gasesFluxGeology010502 geochemistry & geophysics01 natural sciencesFumaroleVolcanic GasesCape verdeVolcani gaseVolcanoImpact craterGEO/08 - GEOCHIMICA E VULCANOLOGIAArchipelagoGeneral Earth and Planetary Sciencesevent0105 earth and related environmental sciencesItalian Journal of Geosciences
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Halogens in volcanic systems

2009

The transport, degassing and atmospheric release of halogens from active volcanism on Earth have been the 12 focus of increasing interest over the last few decades, and have recently been the subject of the 1st workshop 13 on “Halogens in volcanic systems and their environmental impacts” that was held in December of 2007 at 14 Yosemite Lodge in Yosemite National Park, California. As an introduction to this Chemical Geology special 15 issue, collecting contributions from many of the participants at the workshop, we review here recent 16 advances in this field, including experimental and theoretical investigations of halogen behaviour in volcanic 17 and related magmatic systems. We discuss pr…

event.disaster_typegeographygeography.geographical_feature_categoryEarth scienceGeochemistryGeologyCrustVolcanismHydrothermal circulationMantle (geology)Settore GEO/08 - Geochimica E VulcanologiaTroposphereVolcanic GasesHalogensVolcanoGeochemistry and PetrologyeventStratosphereGeology
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Unmanned aerial vehicle measurements of volcanic carbon dioxide fluxes

2008

[i] We report the first measurements of volcanic gases with an unmanned aerial vehicle (UAV). The data were collected at La Fossa crater, Vulcano, Italy, during April 2007, with a helicopter UAV of 3 kg payload, carrying an ultraviolet spectrometer for remotely sensing the SO 2 flux (8.5 Mg d- 1 ), and an infrared spectrometer, and electrochemical sensor assembly for measuring the plume CO 2 /SO 2 ratio; by multiplying these data we compute a CO 2 flux of 170 Mg d -1 . Given the deeper exsolution of carbon dioxide from magma, and its lower solubility in hydro-thermal systems, relative to SO 2 , the ability to remotely measure CO 2 fluxes is significant, with promise to provide more profound…

event.disaster_typegeographygeography.geographical_feature_categorySpectrometerMeteorologyAtmospheric sciencesPlumeSettore GEO/08 - Geochimica E VulcanologiaVolcanic GasesGeophysicsFlux (metallurgy)Impact craterVolcanoMagmaPanacheGeneral Earth and Planetary Scienceseventvolcano monitoring unmanned aerial vehicles volcanic gas monitoringGeology
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Gas hazard assessment at the Monticchio crater lakes of Mt. Vulture, a volcano in Southern Italy

2009

Geochemical investigations have shown that there is a considerable inflow of gas into both crater lakes of Monticchio, Southern Italy. These lakes are located in two maars that formed 140 000 years ago during Mt. Vulture volcanos last eruptive activity. Isotopic analyses suggest that CO2 and helium are of magmatic origin; the latter displays 3 He ⁄ 4 He isotope ratios similar to those measured in olivines of the maar ejecta. In spite of the fact that the amount of dissolved gases in the water is less than that found in Lake Nyos (Cameroon), both the results obtained and the historical reports studied indicate that these crater lakes could be highly hazardous sites, even though they are loca…

event.disaster_typegeographygeography.geographical_feature_categorybiologyGeochemistryGeologyHazard analysisSettore GEO/08 - Geochimica E VulcanologiaMaarGas hazard crater lake Mt. VultureVolcanic GasesVolcanoImpact craterCrater lakebiology.animaleventEjectaGeomorphologyGeologyVultureTerra Nova
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The Monticchio crater lakes: fluid geochemistry and circulation dynamics

2011

fluid geochemistryMonticchioSettore GEO/08 - Geochimica E Vulcanologia
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