Search results for "Geothermal ga"

showing 2 items of 2 documents

Gas emissions and crustal deformation from the Krýsuvík high temperature geothermal system, Iceland

2020

Abstract The Krýsuvik volcanic system is located on the oblique spreading Reykjanes Peninsula, SW Iceland. Since early 2009 the region has been undergoing episodes of localized ground uplift and subsidence. From April–November 2013, we operated near-real time monitoring of gas emissions in Krýsuvik, using a Multi-component Gas Analyzer System (Multi-GAS), collecting data on gas composition from a fumarole (H2O, CO2, SO2, H2S). The dataset in this study, comprises a near-continuous gas composition time series, the quantification of diffuse CO2 gas flux, analytical results for direct samples of dry gas, seismic records, and GPS data. Gas emissions from the Krýsuvik geothermal system were exam…

Volcano monitoringgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeothermal gaVolcanic gaMineralogySubsidence (atmosphere)FluxCrustal deformation010502 geochemistry & geophysicsInlet01 natural sciencesGas analyzerFumaroleKrýsuvíkVolcanic CO2 fluxGeophysicsVolcanoGeochemistry and PetrologyGas compositionGeophysicGeothermal gradientGeology0105 earth and related environmental sciences
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Microbial methane oxidation leading to extreme isotopic fractionation in thermal springs of central Greece

2017

The Greek territory belongs to the geodynamically active Alpine-Himalayan orogenic belt. As such, it shows intense seismic activity, active volcanic systems and areas of enhanced geothermal fluxes. One of these areas is the Sperchios basin and the northern part of Evia island in central Greece, which present widespread thermal manifestations (D’Alessandro et al., 2014). Five of them with temperatures from 33 to 80°C present bubbling gases whose dominating species are either CO2 or N2. All gases contain from 27 to 4000 ppm of CH4. The isotopic composition of CH4 in these gases covers a wide range with δ13C values ranging from -21.7 to +16.9 ‰ and δ2H values ranging from -124 to +301 ‰. The h…

geothermal gases methanotrophy stable isotopes
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