Search results for "hydrothermal system"

showing 10 items of 22 documents

Discrimination between effects induced by microbial activity and water-rock interactions under hydrothermal conditions according to REE behaviour

2013

AbstractRare earth elements (REE) were investigated in siliceous stromatolites forming in the Specchio di Venere Lake on Pantelleria Island. Chondrite-normalised patterns show significant La enrichments and Eu depletions suggesting that fluids involved in stromatolite growth experienced strong rock-water interactions under hydrothermal conditions. At the same time, enrichments in heavy REE (HREE) with respect to intermediate REE (MREE) suggest that hydrothermal fluids interacted with microbial mats during deposition of the stromatolites. The above-mentioned features suggest that rock-water interactions and bacterial activity were simultaneously recorded in the REE patterns of stromatolites,…

Rare Earth ElementsbiologyRock-water interactionsStromatolites; Rare Earth Elements; Bacterial activity; Rock-water interactions Hydrothermal systemRare earthGeochemistryMineralogyEarth and Planetary Sciences(all)General Medicinebiology.organism_classificationHydrothermal circulationStromatoliteRare Earth ElementHydrothermal systemDeposition (aerosol physics)StromatolitesStromatoliteBacterial activityRock-water interactions Hydrothermal systemMicrobial matBacterial activityGeology
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The summit part of Mount Etna revealed by High Resolution DC Electrical Resistivity Tomography coupled with complementary geophysical and soil gas te…

2016

Between 25 June and 13 July 2015 a very deep ERT profile (Pole-Dipole configuration, 40m spacingbetween electrodes and a remote electrode located at ~10km from the acquisition points) has been performedin the framework of the “MED-SUV” Project. Self-potential, soil gas concentrations (CO2, 222Rn, 220Rn, He,H2 and CH4) and soil temperature measurements were coupled to the ERT profile with a spacing of 20m(except for Rn: 40m). The NE-SW profile crossed Etnas summit craters in the middle of the 5720m ERTtotal length. Six roll along protocols of . of the dispositive (600m out of 2520m tot) have been carried outand, for the first time, a high resolution DC ERT profile reached the noticeable inve…

Settore GEO/11 - Geofisica ApplicataHigh Resolution DC Electrical Resistivity Tomography soil gases hydrothermal systemSettore GEO/08 - Geochimica E Vulcanologia
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Hydrothermal methane fluxes from the soil at Lakki plain (Nisyros Island, Greece)

2013

Μετρήσεις φυσικής ροής μεθανίου και διοξειδίου του άνθρακα από το έδαφος πραγματοποιήθηκαν με τη μέθοδο συγκέντρωσης θαλάμου στην περιοχή Λακκί της Καλδέρας της Νισύρου, καλύπτοντας έκταση περίπου 0.06 km2 συμπεριλαμβάνοντας τις περιοχές Καμινάκια, Στέφανος και Αλέξανδρο όπου παρατηρείται έντονη ατμιδική δραστηριότητας. Οι τιμές ροής που μετρήθηκαν σε 77 σημεία κυμαίνονται από –3.4 μέχρι 1420 mg m-2 d-1 για το CH4 και από 0.1, μέχρι 383 g m-2 d-1 για το CO2. Στις τρεις ατμιδικές περιοχές παρουσιάζονται διαφορετικοί ρυθμοί διαφυγής μεθανίου, ιδίως στα Καμινάκια όπου προέκυψαν οι μεγαλύτερες τιμές ροής. Η εξερχόμενη ποσότητα μεθανίου εκτιμάται σε 0.01 t a-1 από μια έκταση περίπου 2500 m2 στον…

Διαφυγή μεθανίουΘάλαμος συγκέντρωσης010501 environmental sciences010502 geochemistry & geophysics01 natural sciencesMedicinal chemistryHydrothermal systemsMethane outputAccumulation chamberMaterials ChemistryΑπαέρωση εδάφουςSoil degassingΥδροθερμικά συστήματαGeomorphologyGeology0105 earth and related environmental sciencesΔελτίο της Ελληνικής Γεωλογικής Εταιρείας
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Methanotrophy in geothermal soils, an overlooked process: The example of Nisyros island (Greece)

2020

Abstract A multidisciplinary field campaign was carried out at Nisyros Island (Greece). Hydrothermal gases were sampled and analysed, and CH4 and CO2 fluxes from the soils were measured with the accumulation chamber method. The sampling area (Lakki plain) covers an area of about 0.08 km2, and includes the main fumarolic areas of Kaminakia, Stefanos, Ramos, Lofos and Phlegeton. Flux values measured at 130 sites range from −3.4 to 1420 mg m−2 d−1 for CH4 and from 0.1 to 383 g m−2 d−1 for CO2. The fumarolic areas show very different CH4 degassing patterns, Kaminakia showing the highest CH4 output values (about 0.8 t a−1 from an area of about 30,000 m2) and Phlegeton the lowest (about 0.01 t a−…

010504 meteorology & atmospheric sciencesSoil testMethanotrophy Soil degassing Hydrothermal systems Methane output Greenhouse gasesSampling (statistics)GeologySoil scienceMethanotrophy Soil degassing Hydrothermal systems Methane output Greenhouse gases010502 geochemistry & geophysics01 natural sciencesSettore GEO/08 - Geochimica E VulcanologiaFlux (metallurgy)Geochemistry and PetrologyChamber methodSoil waterGeothermal gradientGeologyField campaign0105 earth and related environmental sciencesChemical Geology
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The structure of a hydrothermal system from an integrated geochemical, geophysical and geological approach: the Ischia Island case study

2011

The complexity of volcano-hosted hydrothermal systems is such that thorough characterisation requires extensive and interdisciplinary work. We use here an integrated multidisciplinary approach, combining geological investigations with hydrogeochemical and soil degassing prospecting, and resistivity surveys, to provide a comprehensive characterisation of the shallow structure of the south-western Ischia’s hydrothermal system. We show that the investigated area is characterised by a structural setting that, although very complex, can be schematised in three sectors, namely the extra caldera sector (ECS), caldera floor sector (CFS), and resurgent caldera sector (RCS). This contrasted structura…

fluid geochemistryhydrothermal systemSettore GEO/11 - Geofisica ApplicataTEMresurgent calderaERTIschiaSettore GEO/08 - Geochimica E Vulcanologia
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First gas and thermal measurements at the frequently erupting Gamalama volcano (Indonesia) reveal a hydrothermally dominated magmatic system

2020

Abstract The first gas and thermal measurements at the summit of the Gamalama volcano indicate that the system is dominated by hydrothermal processes. This is highlighted by the prevalence of H2S over SO2 (H2S/SO2 = 2–8), a high CO2/SO2 ratio (76–201), and a low heat transfer (3.0 MW) to the surface. A relative variation in gas composition is observed along the degassing fracture zone, possibly due to partial S scrubbing. Despite this surface hydrothermal signature, the system exhibits high gas equilibrium temperatures (425–480 °C), indicating that fluids are not exclusively derived from a boiling hydrothermal aquifer, but also sourced by cooling and crystallizing basaltic magma at deep tha…

Basaltgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeochemistryDominated hydrothermal systemFracture zoneGeodynamicsGamalama volcano010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationPhreatic eruptionDominated hydrothermal system Gamalama volcano Pressure and tensile strengthGeophysicsVolcanoImpact craterPressure and tensile strength13. Climate actionGeochemistry and Petrology[SDU]Sciences of the Universe [physics]MagmaGeology0105 earth and related environmental sciences
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Short-period volcanic gas precursors to phreatic eruptions: Insights from Poás Volcano, Costa Rica

2016

Texto completo del documento Volcanic eruptions involving interaction with water are amongst the most violent and unpredictable geologic phenomena on Earth. Phreatic eruptions are exceptionally difficult to forecast by traditional geophysical techniques. Here we report on short-term precursory variations in gas emissions related to phreatic blasts at Poás volcano, Costa Rica, as measured with an in situ multiple gas analyzer that was deployed at the edge of the erupting lake. Gas emitted from this hyper-acid crater lake approaches magmatic values of SO2/CO21–6 days prior to eruption. The SO2flux derived from magmatic degassing through the lake is measureable by differential optical absorpti…

VOLCANOES010504 meteorology & atmospheric sciencesEarth scienceGeochemistry010502 geochemistry & geophysics7. Clean energy01 natural sciencesVOLCANIC ERUPTIONSHydrothermal circulationeruption precursorGeochemistry and PetrologyCrater lakePhreatomagmatic eruptionEarth and Planetary Sciences (miscellaneous)phreatic eruptionERUPCIONES VOLCÁNICASGEOLOGYGas compositionGeophysicPhreatic0105 earth and related environmental sciencesvolcanic lakegeographygeography.geographical_feature_categoryhydrothermal systemGEOLOGÍAvolcanic gaPARQUE NACIONAL VOLCÁN POÁS (COSTA RICA)Phreatic eruptionGeophysicsHeat fluxVolcano13. Climate actionSpace and Planetary ScienceVOLCANESPoás volcanovolcanic gasGeologyEarth and Planetary Science Letters
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Turmoil at Turrialba Volcano (Costa Rica): Degassing and eruptive processes inferred from high-frequency gas monitoring.

2016

Abstract Eruptive activity at Turrialba Volcano (Costa Rica) has escalated significantly since 2014, causing airport and school closures in the capital city of San José. Whether or not new magma is involved in the current unrest seems probable but remains a matter of debate as ash deposits are dominated by hydrothermal material. Here we use high‐frequency gas monitoring to track the behavior of the volcano between 2014 and 2015 and to decipher magmatic versus hydrothermal contributions to the eruptions. Pulses of deeply derived CO2‐rich gas (CO2/Stotal > 4.5) precede explosive activity, providing a clear precursor to eruptive periods that occurs up to 2 weeks before eruptions, which are acc…

Geologicalexplosive eruptionhydrothermal systemSubduction Zone ProcessesVolcanologyMarine Geology and GeophysicsVolcano Seismologyphreatomagmatic eruptionVolcano MonitoringVolcanic GasesGeochemistryTectonophysicsExplosive Volcanismphreatic eruptionChemistry and Physics of Minerals and Rocks/VolcanologyNatural HazardsSeismologyResearch ArticlesMineralogy and PetrologyResearch ArticleJournal of geophysical research. Solid earth
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Turmoil at Turrialba Volcano (Costa Rica): Degassing and eruptive processes inferred from high-frequency gas monitoring

2016

OVSICORI Eruptive activity at Turrialba Volcano (Costa Rica) has escalated significantly since 2014, causing airport and school closures in the capital city of San José. Whether or not new magma is involved in the current unrest seems probable but remains a matter of debate as ash deposits are dominated by hydrothermal material. Here we use high‐frequency gas monitoring to track the behavior of the volcano between 2014 and 2015 and to decipher magmatic versus hydrothermal contributions to the eruptions. Pulses of deeply derived CO2‐rich gas (CO2/Stotal > 4.5) precede explosive activity, providing a clear precursor to eruptive periods that occurs up to 2 weeks before eruptions, which are acc…

Volcanic gaseVolcano monitoringAtmospheric Scienceexplosive eruptionVOLCAN TURRIALBA (COSTA RICA)Soil ScienceSULFURAquatic ScienceOceanographyphreatomagmatic eruptionVOLCANIC ERUPTIONSHydrothermal systemGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)MAGMAphreatic eruptionAZUFRECOSTA RICAERUPCIONES VOLCÁNICASVOLCANIC ASHGeophysicWater Science and TechnologyCENIZA VOLCÁNICAPhreatomagmatic eruptionEcologyhydrothermal systemvolcano monitoringExplosive eruptionPaleontologyForestryTURRIALBA VOLCANO (COSTA RICA)volcanic gasesSpace and Planetary ScienceEarth-Surface ProcessePhreatic eruption
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A model for Ischia hydrothermal system: Evidences from the chemistry of thermal groundwaters.

2009

Abstract Ischia volcano, in Central Italy, has long been known for its copious surface hydrothermal manifestations, signs of a pervasive circulation of hot fluids in the subsurface. Because of the significant chemical heterogeneity of fumarolic gas discharges and hot spring discharges, evidences of a complex hydrothermal setting, a definite model of fluid circulation at depth is currently unavailable, in spite of the several previous efforts. Here, we report on the chemical and isotopic composition of 120 groundwater samples, collected during several sampling surveys from 2002 to 2007. The acquired data suggest that the composition of surface manifestations reflect contributions from meteor…

Hot springgeographygeography.geographical_feature_categoryischia volcano hydrothermal systemsGeochemistryTrachyteHydrothermal circulationGeophysicsOceanographyVolcanoGeochemistry and PetrologyMagmaMeteoric waterSeawaterGeologyThermal fluids
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