Search results for "Plume"

showing 8 items of 208 documents

The crater lake of Ilamatepec (Santa Ana) volcano, El Salvador: insights into lake gas composition and implications for monitoring

2019

We here present the first chemical characterization of the volcanic gas plume issuing from the Santa Ana crater lake, a hyper-acidic crater lake (pH of − 0.2 to 2.5) in north-western El Salvador. Our results, obtained during regular surveys in 2017 and 2018 using a Multi-GAS instrument, demonstrate a hydrous gas composition (H2O/SO2 ratios from 32 to 205) and SO2 as the main sulfur species (H2S/SO2 = 0.03–0.1). We also find that gas composition evolved during our investigated period, with the CO2/SO2 ratio decreasing by one order of magnitude from March 2017 (37.2 ± 9.7) to November 2018 (< 3). This compositional evolution toward more magmatic (SO2-rich) compositions is interpreted in the c…

ratio010504 meteorology & atmospheric sciences/SOGeochemistry2FluxContext (language use)010502 geochemistry & geophysics01 natural sciencesVolcanic gas plumeGeochemistry and PetrologyCrater lakeWet volcanoGas compositionPrecipitation0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryPlumeSanta Ana volcanoCOVolcanoVolume (thermodynamics)Crater lakeGas scrubbingGeologyMulti-GAS
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H2S fluxes from Mt. Etna, Stromboli and Vulcano (Italy) and implications for the global volcanic sulfur budget

2005

We present here new measurements of sulfur dioxide and hydrogen sulfide emissions from Vulcano, Etna, and Stromboli (Italy), made by direct sampling at vents and by filter pack and ultraviolet spectroscopy in downwind plumes. Measurements at the F0 and FA fumaroles on Vulcano yielded SO2/H2S molar ratios of 0.38 and 1.4, respectively, from which we estimate an H2S flux of 6 to 9 t · d 1 for the summit crater. For Mt. Etna and Stromboli, we found SO2/H2S molar ratios of 20 and 15, respectively, which combined with SO2 flux measurements, suggest H2S emission rates of 50 to 113 t · d 1 and 4 to 8 t · d 1, respectively. We observe that “source” and plume SO2/H2S ratios at Vulcano are similar, s…

sulfur chemistryvolcanic plume
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Plume composition changes during the birth of a new lava lake - Nyamulagira volcano, DR Congo

2016

Nyamulagira, in the Virunga Volcanic Province (VVP), Democratic Republic of Congo, is one of the most active volcanoes in Africa. The volcano is located about 25 km north-northwest of Lake Kivu in the Western Branch of the East African Rift System (EARS) with a distance of only 15 km to Nyiragongo, which is well known for its decades-old active lava lake. Nyamulagira is a shield volcano with a 3058 m high and 2000 m wide summit caldera. The volcano is characterized by frequent eruptions, which occur both from the summit crater and from the flanks (31 flank eruptions over the last 110 years). Due to the low viscosity lava, although significantly higher than the one of Nyiragongo, wide lava f…

volcanic emissions lava lake plume gases and particlesSettore GEO/08 - Geochimica E Vulcanologia
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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
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Emission of Bromine and Iodine from Mt. 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 flu…

volcanic plumebromine and iodine in volcanic gaseatmospheric composition and structure : volcanic effects volcanology : general or miscellaneousvolcanic degassinghalogen atmospheric chemistry
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Volcanic Plume CO2 Flux Measurements at Mount Etna by Mobile Differential Absorption Lidar

2017

Volcanic eruptions are often preceded by precursory increases in the volcanic carbon dioxide (CO2) flux. Unfortunately, the traditional techniques used to measure volcanic CO2 require near-vent, in situ plume measurements that are potentially hazardous for operators and expose instruments to extreme conditions. To overcome these limitations, the project BRIDGE (BRIDging the gap between Gas Emissions and geophysical observations at active volcanoes) received funding from the European Research Council, with the objective to develop a new generation of volcanic gas sensing instruments, including a novel DIAL-Lidar (Differential Absorption Light Detection and Ranging) for remote (e.g., distal) …

volcanic plumes010504 meteorology & atmospheric sciencesFlux010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesVolcanic plumeVolcanic CO2 fluxImpact craterDifferential Absorption Lidar (DIAL);Remote sensing;Volcanic CO2 flux;Volcanic plumesGas compositionDifferential Absorption Lidar (DIAL)0105 earth and related environmental sciencesRemote sensinggeographygeography.geographical_feature_categoryvolcanic plumes; volcanic CO<sub>2</sub> flux; remote sensing; Differential Absorption Lidar (DIAL)lcsh:QE1-996.5ElevationRemote sensingPlumelcsh:GeologyLidarVolcanoVolcanic plume13. Climate actionGeneral Earth and Planetary SciencesEarth and Planetary Sciences (all)GeologyGeosciences; Volume 7; Issue 1; Pages: 9
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Ultraviolet imaging of volcanic plumes: A new paradigm in volcanology

2017

Ultraviolet imaging has been applied in volcanology over the last ten years or so. This provides considerably higher temporal and spatial resolution volcanic gas emission rate data than available previously, enabling the volcanology community to investigate a range of far faster plume degassing processes than achievable hitherto. To date, this has covered rapid oscillations in passive degassing through conduits and lava lakes, as well as puffing and explosions, facilitating exciting connections to be made for the first time between previously rather separate sub-disciplines of volcanology. Firstly, there has been corroboration between geophysical and degassing datasets at ≈1 Hz, expeditin…

volcanic plumes010504 meteorology & atmospheric sciencesLavaEarth scienceFlow (psychology)010502 geochemistry & geophysicsmedicine.disease_cause01 natural sciencesVolcanic plumeInterdisciplinary volcanology; Ultraviolet cameras; Volcanic plumes; Earth and Planetary Sciences (all)medicineinterdisciplinary volcanology0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryultraviolet cameraslcsh:QE1-996.5Gas releaseVolcanologyGeophysicsPlumelcsh:GeologyDynamic modelsVolcano13. Climate actionGeneral Earth and Planetary SciencesEarth and Planetary Sciences (all)GeologyUltravioletUltraviolet camera
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Advances in Bromine Speciation in Volcanic Plumes

2018

Volcanoes are a significant halogen source to the atmosphere. After water, carbon dioxide and sulfur compounds, halogens are often the most abundant gases in volcanic plumes. In the past, less attention was given to the heavy halogens bromine and iodine. However, the discovery of bromine monoxide (BrO) in volcanic plumes led to new interest especially in volcanic bromine chemistry and its impact on atmospheric processes. The BrO detection came along with advances in volcanic remote sensing techniques, in particular, robust DOAS applications and the possibility of continuous measurements by automated instruments located at safe distances from the volcano. As one of the consequences, the volc…

volcanic plumesvolcanic halogen emissionsbromine explosionbromine speciationgas monitoringlcsh:Qlcsh:Scienceplume chemistryFrontiers in Earth Science
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