Search results for "volcan"

showing 10 items of 899 documents

Recent advances in ground-based ultraviolet remote sensing of volcanic SO2 fluxes

2011

Measurements of volcanic SO2 emission rates have been the mainstay of remote-sensing volcanic gas geochemistry for almost four decades, and they have contributed significantly to our understanding of volcanic systems and their impact upon the atmosphere. The last ten years have brought step-change improvements in the instrumentation applied to these observations, which began with the application of miniature ultraviolet spectrometers that were deployed in scanning and traverse configurations, with differential optical absorption spectroscopy evaluation routines. This study catalogs the more recent empirical developments, including: ultraviolet cameras; wide-angle field-of-view differential …

event.disaster_typegeographygeography.geographical_feature_categorySpectrometerEarth scienceDifferential optical absorption spectroscopylcsh:QC801-809Volcanologylcsh:QC851-999Volcanology Volcanic Gases Volcano monitoring Volcanic effects upon atmosphere Atmospheric instruments and techniques.Volcanic GasesAtmospherelcsh:Geophysics. Cosmic physicsGeophysicsVolcanoRemote sensing (archaeology)Radiative transfereventlcsh:Meteorology. ClimatologyGeologyRemote sensingAnnals of Geophysics
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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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First multi-GAS based characterisation of the Boiling Lake volcanic gas (Dominica, Lesser Antilles)

2013

We used a Multi-component Gas Analyser System (Multi-GAS) to measure, for the very first time, the composition (H2O, CO2, H2S, SO2) of the volcanic gas plume issuing from the Boiling Lake, a vigorously degassing, hot (T ~ 80-90°C) volcanic lake in Dominica, West Indies. The Multi-GAS captured in-plume concentrations of H2O, CO2 and H2S were well above those typical of ambient atmosphere, while no volcanic SO2 was detected (<0.05 ppm). These were used to derive the Boiling Lake plume characteristic ratios of CO2/H2S (5.2±0.4) and H2O/CO2 (31.4±6). Assuming that other volcanic gas species (e.g., HCl, CO, H2, N2, etc.) are absent in the plume, we recalculated a (air-free) composition fo…

event.disaster_typegeographygeography.geographical_feature_categorylcsh:QC801-809GeochemistryInstruments and techniquesGases Volcano monitoringlcsh:QC851-999Geochemical dataFumarolePlumeVolcanic GasesAtmospherelcsh:Geophysics. Cosmic physicsGeophysicsVolcano13. Climate actionBoilingeventlcsh:Meteorology. ClimatologyGas compositionGeomorphologyData scrubbingGeologyVolcanic riskAnnals of Geophysics
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. New ground-based lidar enables volcanic CO2 flux measurements

2015

AbstractThere have been substantial advances in the ability to monitor the activity of hazardous volcanoes in recent decades. However, obtaining early warning of eruptions remains challenging, because the patterns and consequences of volcanic unrests are both complex and nonlinear. Measuring volcanic gases has long been a key aspect of volcano monitoring since these mobile fluids should reach the surface long before the magma. There has been considerable progress in methods for remote and in-situ gas sensing, but measuring the flux of volcanic CO2—the most reliable gas precursor to an eruption—has remained a challenge. Here we report on the first direct quantitative measurements of the volc…

event.disaster_typevolcanic gasegeographyMultidisciplinarygeography.geographical_feature_categoryFluxCO2 flux; volcanic gases; lidarArticleFumaroleDialVolcanic GasesLidarVolcanoTemporal resolutionMagmaeventCO2 fluxlidarGeologySeismology
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Os, Sr, Nd, Pb, O isotope and trace element data from the Ferrar flood basalts, antarctica: evidence for an enriched subcontinental lithospheric sour…

1996

Os, Sr, Nd, Pb and O isotopes and trace element data are reported for basaltic andesite and andesite whole rocks and, in part, for selected mineral separates from the Jurassic Ferrar flood basalt province. Radiogenic Sr (> 0.709), unradiogenic Nd (εNd= −3 to −5), and radiogenic Pb isotopes, as well as low Nb/La ratios of 0.4 – 0.6 and Nb/La ratios between 0.45 and 0.6 are found for all rocks including our most primitive sample (Mg# = 71.9). This indicates involvement of either continental crust or enriched lithospheric mantle in magma genesis. 187Re/188Os correlates strongly with 187Os/188Os, with an age of 172 ± 5 Ma, in agreement with published Arsingle bondAr data. Initial 187Os/188Os of…

flood basalts010504 meteorology & atmospheric sciencesGeochemistryFerrar Group551010502 geochemistry & geophysics01 natural sciencesMantle (geology)magma contaminationBasaltic andesite[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/PlanetologyGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryEarth and Planetary Sciences (miscellaneous)[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology0105 earth and related environmental sciencesgeochemistryPeridotiteBasaltAndesiteContinental crustTrace elementGeophysics13. Climate actionSpace and Planetary ScienceFlood basaltFerrar Group; flood basalts; magma contamination; geochemistryGeology
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Constraints on mantle source and interactions from He-Sr isotope variation in Italian Plio-Quaternary volcanism.

2008

[1] Helium isotope ratios of olivine and pyroxene phenocrysts from Plio-Quaternary volcanic rocks from southern Italy (seven Aeolian Islands, Mt. Vulture, Etna, Ustica, and Pantelleria) range from 2.3 to 7.1 Ra. Importantly, the phenocryst 3He/4He correlate well with whole rock Sr isotopic composition (0.70309– 0.70711), reflecting the mixing of two sources. A significant contribution of He from crustal contamination is recorded only occasionally (e.g., pyroxenes from Vulcano). When merged with data from the Roman Comagmatic Province, a remarkably strong near-linear He-Sr isotope correlation is apparent. The general northward decrease in 3He/4He corresponds to an increase in 87Sr/86Sr (and …

fluid inclusionheliumstrontiumitalian volcanism.Settore GEO/08 - Geochimica E Vulcanologia
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The heterogeneity of the Mexican lithospheric mantle: Clues from noble gas and CO2 isotopes in fluid inclusions

2022

The abundance of mantle-derived rocks and lavas, in combination with its tectonic evolution, render Mexico a perfect laboratory to investigate the chemical and the isotopic heterogeneity of the lithospheric mantle. New data on the composition of noble gases and CO2in Mexican mantle xenoliths and lavas is reported. Our samples consist of six ultramafic nodules from the Durango Volcanic Field (DVF) and the San Quintin Volcanic Field (SQVF), monogenetic complexes belonging to the Mexican Basin and Range province; and four lavas from the Sierra Chichinautzin (SCN), a Quaternary monogenetic volcanic field located in the Mexican volcanic arc. Ne and Ar isotopes in fluid inclusions reveal mixing b…

fluid inclusionnoble gas isotopesnoble gas isotopecarbon recyclingCO2 isotopeBasin and Range provincefluid inclusionsarc lavasGeneral Earth and Planetary SciencesTrans‐mexican Volcanic BeltCO2arc lavaMexican mantle xenolithsisotopesMexican mantle xenolith
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Insights on Hydrothermal‐Magmatic Interactions and Eruptive Processes at Poás Volcano (Costa Rica) From High‐Frequency Gas Monitoring and Drone Measu…

2019

Texto completo del documento Identification of unambiguous signals of volcanic unrest is crucial in hazard assessment. Processes leading to phreatic and phreatomagmatic eruptions remain poorly understood, inhibiting effective eruption forecasting. Our 5‐year gas record from Poás volcano, combined with geophysical data, reveals systematic behavior associated with hydrothermal‐magmatic eruptions. Three eruptive episodes are covered, each with distinct geochemical and geophysical characteristics. Periods with larger eruptions tend to be associated with stronger excursions in monitoring data, particularly in SO2/CO2 and SO2 flux. The explosive 2017 phreatomagmatic eruption was the largest erupt…

gas monitoringVOLCANOESGeochemistryPARQUE NACIONAL VOLCAN POAS (COSTA RICA)Hydrothermal circulationVOLCANIC ERUPTIONSphreatomagmatic eruptionsCrater lakePhreatomagmatic eruptionphreatic eruptionGEOLOGYPOAS VOLCANO NATIONAL PARK (COSTA RICA)geographyeruption triggeringgeography.geographical_feature_categorygeophysicGEOLOGÍADroneGas monitoringPhreatic eruptioncrater lakeGeophysicsVolcanoVOLCANESERUPCIONES VOLCANICASGeneral Earth and Planetary SciencesGeology
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Volcanic gas monitoring of quiescent volcanoes using permanent Multi-GAS networks

2014

The Multi-component Gas Analyzer System (Multi-GAS) has recently consolidated as a standard technique for the nearly real-time in-situ observation of major volcanogenic components (H2O, CO2, SO2, H2S,H2) in volcanic gas plumes. The Multi-GAS has been initially operated at open-vent volcanoes, where it has revealed ideal for long-term continuous observations at for instance Etna and Stromboli volcanoes in Italy, therein paving the way to the acquisition of unprecedentedly long and continuous volcanic gas time-series. We here initially review the present state of the expanding network of permanent Multi-GAS instruments, now covering about 10 volcanoes worldwide. We then specifically focus on …

gas monitoringvolcanic degassingSettore GEO/08 - Geochimica E Vulcanologia
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