Search results for "Hydrothermal system"

showing 10 items of 22 documents

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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The role of the aquifer in soil CO2 degassing in volcanic peripheral areas: A case study of Stromboli Island (Italy)

2017

Abstract The peripheral area of Stromboli Island, Italy, named “Scari”, was continuously studied between January 2009 and December 2010. Data on soil CO 2 flux and the partial pressure of CO 2 (pCO 2 ) in equilibrium with the thermal aquifer linked to the magmatic system are presented. Soil CO 2 fluxes range from 20 to 370 g m − 2  d − 1 and have been strongly affected by soil temperature variations. Soil CO 2 flux data were filtered with respect to the soil temperature and the calculated values, called “residuals”, were considered to detect changes induced by the magmatic system. The pCO 2 values change in a wide range from 0.03 to 0.6 (atm), showing rapid variations. The results of this s…

Hydrologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciences2GeologySoil scienceAquiferin waterPartial pressure010502 geochemistry & geophysics01 natural sciencesfluxVolcano-hydrothermal systemSoil temperatureFlux (metallurgy)VolcanoGeochemistry and PetrologypCOMagmaSoil COGeologyGas-water interaction0105 earth and related environmental sciencesChemical Geology
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Chemical and isotopic characterization of Ischia hydrothermal system: an interpretative model of fluids circulation

2009

Ischia hydrothermal systemsthermal groundwatersSettore GEO/08 - Geochimica E Vulcanologia
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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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Geochemistry of Zr, Hf and REE in extreme water environments: hyperacid, hyper saline and lake waters in hydrothermal systems

This PhD thesis concerns the geochemistry of Zr, Hf and REE in extreme water environments characterized by a wide spectrum of chemical physical-parameters and compositions. The investigations were carried out in hypersaline waters covering a wide range of Eh values along Dead Sea Fault (Israel), in hyperacid waters circulating in Nevado del Ruiz volcano-hydrothermal system (Colombia) and in CO2-rich waters belonging to the Pantelleria volcano-hydrothermal system (Italy), including the alkaline lake “Specchio di Venere” formed within a calderic depression. The wide spectrum of chemical-physical conditions and various water chemical compositions interacting with different solid phases allowed…

Rare Earth Elements; Zirconium; Hafnium; Hydrothermal systems; Extreme water environmentsHydrothermal systemExtreme water environmentsZirconiumHafniumRare Earth ElementSettore GEO/08 - Geochimica E Vulcanologia
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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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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

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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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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Hydrothermal circulation on Ischia Island (Southern Italy), revealed by an integrated geochemical, geophysical and geological approach

2011

Volcano-hosted hydrothermal systems are complex geological objects, whose thorough characterisation requires extensive and interdisciplinary work. Indeed, even thought geological, geochemical and geophysical observations offer highly significant but independent information, only an integrated multidisciplinary approach can yield a comprehensive characterisation of the chemical/physical structure of hydrothermal systems. Notwithstanding the extensive application of geological, geochemical and geophysical techniques in geothermal research, there are only a few examples in the literature of concurrent use of the three techniques [Finizola et al., 2002; Zlotnicki et al., 2009]; these studies ov…

fluid geochemistryhydrothermal systemresurgent caldera.TEMERTIschiaSettore GEO/08 - Geochimica E Vulcanologia
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