Search results for "Degas"

showing 10 items of 124 documents

Forecasting Etnean eruptions by real-time observations of volcanic gas composition.

2007

It is generally accepted but not experimentally proven that a quantitative prediction of volcanic eruptions is possible from the evaluation of volcanic gas data. By discussing the results of two years of real-time observation of H2O, CO2 and SO2 in volcanic gases from Mt. Etna volcano, we unambiguously demonstrate that increasing CO2/SO2 ratios can allow detecting the pre-eruptive degassing of uprising magmas. Quantitative modeling by the use of a saturation model allows us to relate the pre-eruptive increases of the CO2/SO2 ratio to the refilling of Etna’s shallow conduits with CO2-rich deep-reservoir magmas, leading to pressurization and eruption triggering. The advent of real-time observ…

Etna volcanovolcanic degassingvolcanic emissions of CO2 and SO2
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Halogen (Cl, F) release during explosive, effusive, and intrusive phases of the 2011 rhyolitic eruption at Cordón Caulle volcano (Chile)

2019

We investigate sulphur, chlorine and fluorine release during explosive, effusive and intrusive phases of the 2011 Cordon Caulle eruption, with a focus on halogen devolatilization. Petrological analysis shows halogen release to have been promoted by isobaric crystallization in slowly-cooled magma that was emplaced in a lava flow and sub-vent intrusion. Fluorine in particular mobilized only after extensive groundmass crystallization and incipient devitrification. By 2017, the gas emitted from vent-proximal fumaroles had hydrothermal compositions, with HCl/HF ratios decreasing with decreasing temperature. We estimate that the eruption could eventually emit up to 0.84 Mt of SO2, 6.3 Mt of HCl, …

Explosive materialLavaGeochemistryrhyolitevolatile budgetvolatileHydrothermal circulationGeochemistry and PetrologyRhyolitehalogensEarth and Planetary Sciences (miscellaneous)QE1-996.5geographygeography.geographical_feature_categoryChemistrydegassingGeologyhalogenFumarolevolatilesGeophysicsDevitrificationVolcanoCordón CaulleMagmaPuyehue
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New record in the Mediterranean Sea of unusual skin colouration in the black-bellied anglerfishLophius budegassaSpinola, 1807

2010

FisheryMediterranean seaAnglerfishSettore BIO/05 - ZoologiaLophius budegassa skin pigmentation Mediterranean SeaAquatic ScienceBiologybiology.organism_classificationLophius budegassaJournal of Applied Ichthyology
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Demethanization of aqueous anaerobic effluents using a polydimethylsiloxane membrane module: Mass transfer, fouling and feasibility

2017

Abstract The performance, fouling and feasibility of a polydimethylsiloxane hollow fibre membrane module for in situ methane degasification from the effluent of an Expanded Granular Sludge Bed anaerobic reactor has been investigated. Experiments at different operational conditions were carried out (liquid flow, sweep gas flow and vacuum pressure) with maximum removal efficiency (77%) at lowest flow-rate (0.4 L h−1), highest vacuum gauge pressure (−800 mbar) and liquid flowing in lumen side. Mass transport analysis denoted a considerably higher methane transfer than that predicted (attributed to liquid oversaturation). An enhancement factor for liquid phase has been proposed to correlate the…

FoulingGasos d'efecte hivernacleMembrane foulingEnergy balanceEnvironmental engineeringFiltration and Separation02 engineering and technology010501 environmental sciences021001 nanoscience & nanotechnology01 natural sciencesMethaneAnalytical Chemistrychemistry.chemical_compoundMembranechemistryChemical engineeringDegasificationMass transfer0210 nano-technologyEffluent0105 earth and related environmental sciences
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Diffuse soil gas emissions of gaseous elemental mercury (GEM) from hydrothermal-volcanic systems: An innovative approach by using the static closed-c…

2016

This study was aimed to test a new methodological approach to carry out measurements of gaseous elemental mercury (GEM) diffusively emitted from soils in hydrothermal-volcanic environments. This method was based on the use of a static closed-chamber (SCC) in combination with a Lumex® RA-915M analyzer that provides GEM measurements in a wide range of concentrations (from 2 to 50,000 ng m-3). Gas samples were collected at fixed time intervals from the SCC positioned on the ground (time-series samples). The Lumex® inlet port was equipped with a three-way Teflon valve allowing the free entrance of air through a carbon trap, in order to: (i) prevent disturbance to the Lumex® operative flow rate …

GEM flux Diffuse soil degassing Air pollutant Hydrothermal gas010504 meteorology & atmospheric sciencesCalibration curveMineralogychemistry.chemical_elementGEM flux010502 geochemistry & geophysics01 natural sciencesImpact craterGeochemistry and PetrologyEnvironmental Chemistry0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorySoil gasAir pollutantHydrothermal gasDiffuse soil degassingInletPollutionSettore GEO/08 - Geochimica E VulcanologiaVolumetric flow rateMercury (element)chemistryContour lineSoil waterFluid geochemistryApplied Geochemistry
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First characterization of Gamkonora gas emission, North Maluku, East Indonesia

2020

Gamkonora is an active volcano capable of intense manifestations that regularly forced thousands of inhabitants to flee their villages. The most extreme eruption, in 1673, was a VEI 5 event that induced pitch-dark environment over the region. Paradoxically, little is known about Gamkonora volcano and here we present the first gas measurement results obtained in September 2018 using a MultiGAS and a scanning DOAS. Results highlight a relatively small but magmatic gas with a CO2/ST of 3.5, in the range of high-temperature gas emissions from Indonesian volcanoes and H2O/SO2, CO2/SO2, H2S/SO2, and H2/SO2 ratios of 135, 5.6, 0.6, and 0.2, respectively. The daily gas emission budget corresponds t…

Gamkonora volcanogeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesAndesiteGas emission budgetGeochemistryMagmatic degassingGas emissions010502 geochemistry & geophysics01 natural sciencesGamkonora volcano Gas emission budget Magmatic degassingBasaltic andesiteVolcanoGeochemistry and Petrology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologySedimentology[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentGeology0105 earth and related environmental sciences
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Hydrothermal fluid venting in the offshore sector of Campi Flegrei caldera: A geochemical, geophysical, and volcanological study

2016

The ongoing unrest at the Campi Flegrei caldera (CFc) in southern Italy is prompting exploration of its poorly studied offshore sector. We report on a multidisciplinary investigation of the Secca delle Fumose (SdF), a submarine relief known since antiquity as the largest degassing structure of the offshore sector of CFc. We combined high-resolution morphobathymetric and seismostratigraphic data with onshore geological information to propose that the present-day SdF morphology and structure developed during the initial stages of the last CFc eruption at Monte Nuovo in AD 1538. We suggest that the SdF relief stands on the eastern uplifted border of a N-S-trending graben-like structure formed …

Geochemistry and PetrologySettore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaVertical profile pH CO2Campi Flegreisubmarine ventCO2 degassingGeophysicSecca delle FumoseSettore GEO/08 - Geochimica E Vulcanologia
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Estimation of the geogenic carbon degassing of Greece

2019

Abstract Greece belongs to the most geodynamically active regions of the world and as such it has to be considered an area of intense geogenic degassing. Here we review all the papers already published in the scientific literature on both the geochemistry of gas manifestations and the CO2 and CH4 release, in an attempt to obtain the first nationwide inventory of the natural output of these carbon gases in Greece. The best studied and most exhaling area is the South Aegean Active Volcanic Arc (SAAVA), which releases more than 1.3 × 105 tons of CO2 per year. Continental Greece, on the contrary, is much less studied but may release CO2 in the same order of magnitude in its eastern-central and …

Geogenic degassinggeographygeography.geographical_feature_categoryGas geochemistryVolcanic arcEarth sciencechemistry.chemical_element010501 environmental sciences010502 geochemistry & geophysics01 natural sciencesPollutionMethaneSettore GEO/08 - Geochimica E VulcanologiaAtmospherechemistry.chemical_compoundCarbon dioxidechemistryGeochemistry and PetrologyCarbon dioxideEnvironmental ChemistryEnvironmental scienceMethaneCarbon0105 earth and related environmental sciencesApplied Geochemistry
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Shallow Sea Gas Manifestations in the Aegean Sea (Greece) as Natural Analogs to Study Ocean Acidification: First Catalog and Geochemical Characteriza…

2022

The concepts of CO2 emission, global warming, climate change, and their environmental impacts are of utmost importance for the understanding and protection of the ecosystems. Among the natural sources of gases into the atmosphere, the contribution of geogenic sources plays a crucial role. However, while subaerial emissions are widely studied, submarine outgassing is not yet well understood. In this study, we review and catalog 122 literature and unpublished data of submarine emissions distributed in ten coastal areas of the Aegean Sea. This catalog includes descriptions of the degassing vents through in situ observations, their chemical and isotopic compositions, and flux estimations. Tempe…

Global and Planetary ChangeScienceQGeneral. Including nature conservation geographical distributionOcean EngineeringQH1-199.5Aquatic ScienceCO2 emissionsOceanographyenvironmental impactgas fluxgeogenic degassingCO2 emissionGreek Islandsubmarine gas ventsGreek IslandsWater Science and Technology
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Carbon dioxide degassing from Tuscany and Northern Latium (Italy)

2008

Abstract The CO 2 degassing process from a large area on the Tyrrhenian side of central Italy, probably related to the input into the upper crust of mantle fluids, was investigated in detail through the geochemical study of gas emissions and groundwater. Mass-balance calculations and carbon isotopes show that over 50% of the inorganic carbon in regional groundwater is derived from a deep source highlighting gas−liquid separation processes at depth. The deep carbonate−evaporite regional aquifer acts as the main CO 2 reservoir and when total pressure of the reservoir fluid exceeds hydrostatic pressure, a free gas phase separates from the parent liquid and escapes toward the surface generating…

Global and Planetary Changegeographygeography.geographical_feature_categoryHydrostatic pressureMineralogycarbon dioxideAquiferOceanographyMantle (geology)Hydrothermal circulationchemistry.chemical_compoundEarth degassing; carbon dioxide; CO2 flux; groundwaterchemistryTotal inorganic carbonIsotopes of carbonCarbon dioxidegroundwaterEarth degassingCO2 degassingCO2 fluxGroundwaterGeology
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