Search results for " Volcano"

showing 10 items of 131 documents

Plants as biomonitors for volcanic emissions

2014

Biomonitoring techniques have been widely used in environmental studies to monitor anthropogenic pollutant. Recently such techniques have been applied also to ascertain the impact of contaminants naturally released by volcanic activity. In the present study a biomonitoring surveys has been performed in many different active volcanic systems: Mt. Etna and Vulcano (Italy), Nisyros (Greece), Nyiragongo (DRC), Masaya (Nicaragua), Gorely (Kamchatka, Russia). We sampled leaves of different species Betulla aethnensis, Pinus nigra, Populus tremula, Senecio aethnensis and Rumex aethnensis on Etna, Cistus creticus and salvifolius on Vulcano and Nisyros, Senecio ssp. on Nyiragongo, a Fern on Masaya an…

Biomonitors Volcanoes Trace elements
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The 2007 eruption of Stromboli volcano: Insights from real-time measurement of the volcanic gas plume CO2/SO2 ratio

2009

Abstract The recent eruption of Stromboli in February–April 2007 offered a unique chance to test our current understanding of processes driving the transition from ordinary (persistent Strombolian) to effusive activity, and the ability of instrumental geophysical and geochemical networks to interpret and predict these events. Here, we report on the results of two years of in-situ sensing of the CO 2 /SO 2 ratio in Stromboli's volcanic gas plume, in the attempt to put constraints on the trigger mechanisms and dynamics of the eruption. We show that large variations of the plume CO 2 /SO 2 ratio (range, 0.9–26) preceded the onset of the eruption (since December 2007), interrupting a period of …

Convectiongeographygeography.geographical_feature_categorystromboli volcanoStrombolian eruptionPlumeGeophysicsEffusive eruptionVolcanoGeochemistry and PetrologyMagmaSaturation (chemistry)GeologySeismologyJournal of Volcanology and Geothermal Research
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Estudio Hidrogeoquimico De Las Áreas Termales Del Complejo Volcánico Copahue-Caviahue

2016

Hydrogeochemical study on Thermal areas of the Copahue-Caviahue Volcanic Complex The hydrothermal system hosted in the Copahue- Caviahue Volcanic Complex consists of different geothermal areas around the Copahue volcano, whose last eruptive cycle started on December 22 of 2012. This work presents new data from the samplings of November 2012 and march 2013 in Las Maquinas, Las Maquinitas, villa de Copahue and Chancho-Có areas. These acid-sulfate and steam heated waters, presented changes in their SO4-2 concentrations, especially in Las Maquinas and Las Maquinitas areas. Meanwhile, SO4-2/Cl- ratios presented a strong decrease in the samples from November 2012, regarding the samples from 2013.…

Copahue volcano hydrothermal system water geochemistry REE volcano riskSettore GEO/08 - Geochimica E Vulcanologia
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Insights Into the Mechanisms of Phreatic Eruptions From Continuous High Frequency Volcanic Gas Monitoring: Rincón de la Vieja Volcano, Costa Rica

2019

OVSICORI Understanding the trigger mechanisms of phreatic eruptions is key to mitigating the effects of these hazardous but poorly forecastable volcanic events. It has recently been established that high-rate volcanic gas observations are potentially very suitable to identifying the source processes driving phreatic eruptions, and to eventually detecting precursory changes prior to individual phreatic blasts. In February-May 2017, we deployed a Multi-GAS instrument to continuously monitor gas concentrations in the crater lake plume of Rincón de la Vieja, a remote and poorly monitored active volcano in Costa Rica, site of frequent phreatic/phreatomagmatic eruptions. Forty-two phreatic/phreat…

Costa RicaVOLCANOES010504 meteorology & atmospheric sciencesGeochemistryGASES010502 geochemistry & geophysics01 natural sciencesVOLCANIC ERUPTIONSHydrothermal circulationVolcanic GasesTURRIALBA VOLCANO NATIONAL PARK (COSTA RICA)Crater lakePhreatomagmatic eruptioneventERUPCIONES VOLCÁNICASPARQUE NACIONAL VOLCÁN TURRIALBA (COSTA RICA)lcsh:ScienceRincón de la ViejaVolcanic gasesPhreatic0105 earth and related environmental sciencesevent.disaster_typegeographygeography.geographical_feature_categoryPhreatic eruptionPlumeVolcanoVOLCANEScrater lakesCrater lakeGeneral Earth and Planetary Scienceslcsh:QPhreatic eruptionMulti-GASGeologyFrontiers in Earth Science
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Development and application of active and passive DOAS instrumentation for the remote sensing measurement of volcanic gas emissions and continuous ge…

2011

DOASdegassing volcanoevolcanic gaSettore GEO/08 - Geochimica E Vulcanologia
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Active alkaline traps to determine acidic-gas ratios in volcanic plumes: Sampling techniques and analytical methods

2014

In situ measurements have been the basis for monitoring volcanic gas emissions for many years and—being complemented by remote sensing techniques—still play an important role to date. Con- cerning in situ techniques for sampling a dilute plume, an increase in accuracy and a reduction of detection limits are still necessary for most gases (e.g., CO2, SO2, HCl, HF, HBr, HI). In this work, the Raschig-Tube tech- nique (RT) is modified and utilized for application on volcanic plumes. The theoretical and experimental absorption properties of the RT and the Drechsel bottle (DB) setups are characterized and both are applied simultaneously to the well-established Filter packs technique (FP) in the …

Detection limitgeographyAnalytegeography.geographical_feature_categoryalkaline traps plume sampling sulfur and halogen Etna volcanoDifferential optical absorption spectroscopyIon chromatographyMineralogySettore GEO/08 - Geochimica E VulcanologiaPlumeGeophysicsVolcanoGeochemistry and PetrologyAbsorption (electromagnetic radiation)Inductively coupled plasma mass spectrometryGeologyGeochemistry, Geophysics, Geosystems
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Carbon dioxide diffuse emission and thermal energy release from hydrothermal systems at Copahue-Caviahue Volcanic Complex (Argentina)

2015

Fil: Chiodini, Giovanni. Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna. Bologna, Italia. Fil: Cardellini, Carlo. Università degli Studi di Perugia, Dipartimento di Fisica e Geologia. Perugia, Italy. Fil: Lamberti, María C. Universidad de Buenos Aires. Instituto de Estudios Andinos. Buenos Aires, Argentina. Fil: Agusto, Mariano. Universidad de Buenos Aires. Instituto de Estudios Andinos. Buenos Aires, Argentina. Fil: Caselli, Alberto Tomás Universidad Nacional de Río Negro. Instituto de Investigación en Paleobiología y Geología. Río Negro. Argentina. Fil: Liccioli, Caterina. Universidad de Buenos Aires. Instituto de Estudios Andinos. Buenos Aires, Argentina. Fil: Tambure…

Earth scienceGeochemistrychemistry.chemical_elementThermal energyCO2 DIFFUSETHERMAL ENERGYHydrothermal circulationCiencias de la Tierra y relacionadas con el Medio AmbienteCopahue Volcano CO2 Diffuse Degasingchemistry.chemical_compoundVulcanologíaGeochemistry and PetrologyCalderaCaviahue Calderageographygeography.geographical_feature_categorybusiness.industryFumaroleCopahue Volcano CO2 diffuse degasingSettore GEO/08 - Geochimica E VulcanologiaGeophysicschemistryVolcanoCAVIAHUE CALDERASoil waterCarbon dioxideCaviahue Caldera Copahue Volcano CO2 diffuse degasing Thermal energyCOPAHUE VOLCANObusinessCO2 fluxCarbonThermal energyGeologyCIENCIAS NATURALES Y EXACTAS
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Gradual caldera collapse at Bardarbunga volcano, Iceland, regulated by lateral magma outflow

2016

Large volcanic eruptions on Earth commonly occur with a collapse of the roof of a crustal magma reservoir, forming a caldera. Only a few such collapses occur per century, and the lack of detailed observations has obscured insight into the mechanical interplay between collapse and eruption.We usemultiparameter geophysical and geochemical data to show that the 110-square kilometer and 65-meter-deep collapse of Bárdarbunga caldera in 2014–2015 was initiated through withdrawal of magma, and lateral migration through a 48-kilometers-long dike, from a 12-kilometers deep reservoir. Interaction between the pressure exerted by the subsiding reservoir roof and the physical properties of the subsurfac…

EldgosLateral eruption010504 meteorology & atmospheric sciencesLavaÖskjugosHraunrennsli010502 geochemistry & geophysics01 natural sciences[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryCalderaComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryMultidisciplinaryGlacier DynamicsResurgent domeMedicine (all)Complex volcanoLateral Magma Flow16. Peace & justiceCaldera collapseDense-rock equivalentBárðarbungaVolcano13. Climate actionEruptionMagmaGeologySeismology
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The contingent equilibrium during imbalanced volcano tourism demand through fee estimation: An empirical analysis of tourism in Mt. Etna

2022

Volcanic sites can be considered strategic areas for conservation and protection policies, but such policies may involve considerable costs However, not only are volcanic sites often integral to the tourism industry and, hence, of potential significant benefit to local economies in general; entrance fee income from tourists can also contribute to management and conservation costs in particular. Nevertheless, seasonal variations in tourism demand, resulting in over-and under-tourism situations, may impact on both the level of income generated as well as on the sustainability of sites Therefore, based on a case study of Mt Etna in Italy, this study considers establishing appropriate entry fee…

Environmental EngineeringItalyVolcanic sites contingent valuation volcano tourism Over-tourism Economic equilibrium Mt. EtnaN832Costs and Cost AnalysisIncomeN831General MedicineManagement Monitoring Policy and LawSettore SECS-P/06 - Economia ApplicataWaste Management and DisposalTourism
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Emission of bromine and iodine from Mount Etna volcano

2005

Constraining fluxes of volcanic bromine and iodine to the atmosphere is important given the significant role these species play in ozone depletion. However, very few such measurements have been made hitherto, such that global volcanic fluxes are poorly constrained. Here we extend the data set of volcanic Br and I degassing by reporting the first measurements of bromine and iodine emissions from Mount Etna. These data were obtained using filter packs and contemporaneous ultraviolet spectroscopic SO2 flux measurements, resulting in time-averaged emission rates of 0.7 kt yr-1 and 0.01 kt yr-1 for Br and I, respectively, from April to October 2004, from which we estimate global Br and I fluxes …

Etna volcano
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