Search results for "Geochemistry"

showing 10 items of 2967 documents

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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A CO2-gas precursor to the March 2015 Villarrica volcano eruption

2017

We present here the first volcanic gas compositional time-series taken prior to a paroxysmal eruption of Villarrica volcano (Chile). Our gas plume observations were obtained using a fully autonomous Multi-component Gas Analyser System (Multi-GAS) in the 3 month-long phase of escalating volcanic activity that culminated into the 3 March 2015 paroxysm, the largest since 1985. Our results demonstrate a temporal evolution of volcanic plume composition, from low CO$_2$/SO$_2$ ratios (0.65-2.7) during November 2014-January 2015 to CO$_2$/SO$_2$ ratios up to ≈ 9 then after. The H$_2$O/CO$_2$ ratio simultaneously declined to <38 in the same temporal interval. We use results of volatile saturatio…

volcanic gaseGeochemistry and Petrologyvolcanic gasesVillarrica volcanolava lakelava lakesmulti-GASprecursor CO2/SO2variationGeophysicprecursor CO2/SO2 variations
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Sulfur Degassing From Steam-Heated Crater Lakes: El Chichón (Chiapas, Mexico) and Víti (Iceland)

2018

The composition of the gases released by El Chichón (Chiapas, Mexico) and Víti (Askja volcano, Iceland) volcanic lakes is examined by Multi-GAS for the first time. Our results demonstrate that H2S and SO2 are degassed by these pH 2–3 lakes. We find higher CO2/H2S and H2/H2S ratios in the lakes' emissions (31–5,685 and 0.6–35, respectively) than in the fumarolic gases feeding the lakes (13–33 and 0.08–0.5, respectively), evidencing that only a fraction (0.2–5.4% at El Chichón) of the H2S(g) contributed by the subaquatic fumaroles ultimately reaches the atmosphere. At El Chichón, we estimate a H2S output from the crater lake of 0.02–0.06 t/day. Curiously, SO2 is also detected at trace levels …

volcanic lake010504 meteorology & atmospheric sciencesGeochemistrychemistry.chemical_elementVíti010502 geochemistry & geophysicssulfur degassing01 natural sciencesSulfurEl ChichónGeophysicsImpact craterchemistryGeneral Earth and Planetary SciencesGeophysicEarth and Planetary Sciences (all)Multi-GASGeology0105 earth and related environmental sciencesGeophysical Research Letters
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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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Evolution of Seismicity During a Stalled Episode of Reawakening at Cayambe Volcano, Ecuador

2021

Cayambe Volcano is an ice-capped, 5,790 m high, andesitic-dacitic volcanic complex, located on the equator in the Eastern Cordillera of the Ecuadorian Andes. An eruption at Cayambe would pose considerable hazards to surrounding communities and a nationally significant agricultural industry. Although the only historically documented eruption was in 1785, it remains persistently restless and long-period (LP) seismicity has been consistently observed at the volcano for over 10 years. However, the sparse monitoring network, and complex interactions between the magmatic, hydrothermal, glacial, and tectonic systems, make unrest at Cayambe challenging to interpret. In June 2016 a seismic “crisis” …

volcano-tectonic interactionsgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesScienceEquatorQvolcano-glacier interactionsInduced seismicityFault (geology)010502 geochemistry & geophysics01 natural sciencesTectonicsVolcanoMagmavolcano-seismic swarmsGeneral Earth and Planetary SciencesGlacial periodlong-period seismicityVolcanic coneGeologySeismology0105 earth and related environmental sciencesvolcanic monitoringFrontiers in Earth Science
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Geochemical characterization of trace elements in thermomineral waters of Greece

2020

Trace elements have a fundamental role in natural and anthropogenic systems. In waters, they present a great variability of concentrations that mostly depends on the degree of gaswaterrock interactions and geochemical conditions such as pH, temperature, redox and/or exchange reactions, etc. Even though, they are present in very low contents in hostrocks, elevated concentrations in ground or surface waters may have a hazardous impact on human and animal health and thus, it is important to both quantify and try to understand their behaviour in natural systems. Here we present the results of about 300 cold and thermal mineral waters collected along the entire Hellenic territory. Physicochemica…

water geochemistry trace elements GreeceSettore GEO/08 - Geochimica E Vulcanologia
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X-ray tomographic method for measuring three-dimensional deformation and water content distribution in swelling clays

2015

A non-invasive method for simultaneous measurement of the 3D displacement field and the water content distribution of a wetted solid material is developed. The method is based on comparison of X-ray tomographic images of a material sample in the reference state and in the wetted and deformed state. The deformation and water content analyses were successfully compared with numerical results for a cylindrical rubber test sample under axial compression, and with gravimetric results from axially wetted and sliced cylindrical bentonite samples, respectively. The methods were applied in a 4D study (three spatial dimensions and time) of wetting and deformation of purified swelling bentonite doped …

water transportMaterials scienceDeformation (meteorology)swellingGeochemistry and PetrologybentoniittimedicineGeotechnical engineeringComposite materialta216Water contentwater contentWater transportta114vesikuljetusbentonitedeformationGeologyBentoniteDisplacement fieldGravimetric analysisWettingSwellingmedicine.symptomvesipitoisuusX-ray tomographyApplied Clay Science
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Mise en évidence d'un Sénonien gypseux sous la série phosphatée du bassin des Ouled Abdoun: un nouveau point de départ pour l'origine des zones déran…

2013

In the Ouled Abdoun sedimentary basin (Morocco), the phosphatic series is composed of regular interbedded phosphatic and marly limestone layers. Exploitation of the phosphate in some deposits in this basin collides frequently with problems bound to the existence, in the phosphatic series, of disturbed areas (sterile bodies) qualified as derangements by the mining engineers of the Office Cherifian Phosphate Group (OCP). Their presence in the phosphatic layers causes two kinds of problems: (1) since the whole phosphatic sequence is overlain by a Quaternary cover, we do not know their volume proportion in the phosphatic layers, and therefore the reserves estimations can be wrong (2) they are g…

zone dérangéeGeochemistryBoreholeMineralogyStructural basin[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphydisturbed areaGroup (stratigraphy)Khouribgasérie phosphatéeQE1-996.5geographygeography.geographical_feature_categorylcsh:QE1-996.5SénonienSenonianGeologyOuled Abdoun BasinPhosphatic seriesSedimentary basinkarstKarstgypsumDiagenesislcsh:GeologyMarocMoroccogypseQuaternaryGeology
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Journée Scientifique de l'Unité Mixte de Recherche Microbiologie des Sols - Géochimie des Interfaces Sol-Eau

2001

International audience; Sessions : CARBONE, GAZ À EFFET DE SERRE, PESTICIDES, ÉCOLOGIE MICROBIENNE, MÉTAUX ET QUALITÉ DES SOLS

écologie microbiennemétaux[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistrygaz à effet de serrepesticidesmicrobiologie[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistryqualité des sols
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