Search results for "Geogenic"

showing 9 items of 9 documents

Selenium mobilization in soils due to volcanic derived acid rain: An example from Mt Etna volcano, Sicily

2011

International audience; The significant amounts of selenium (Se) emitted by volcanoes may have important impact on human health due to the narrow range between nutrition requirement and toxic effects for living organisms upon Se exposure. Although soils play a key role in determining the level in food and water and thereby human health, little is known about the behaviour of Se in volcanic soils. In this work we evaluated the Se release during rainwater–soil interaction under controlled conditions using soils collected on the flanks of Etna volcano and synthetic rain. Selenium concentrations in soil leachate solutions displayed a spatial distribution, which cannot be explained by plume depo…

010504 meteorology & atmospheric sciencesSelenium; Volcanic soils; Geogenic; Volcanoes; Contamination; GroundwaterSelenium; Volcanic soils; Geogenic; Volcanoes; Contamination; Groundwaterchemistry.chemical_element[SDU.STU]Sciences of the Universe [physics]/Earth SciencesVolcanoe010502 geochemistry & geophysics01 natural sciencesSelenateVolcanic soilchemistry.chemical_compoundSeleniumContaminationGeochemistry and PetrologySelenium acid rain soilsGeogenicChemical compositionGroundwater0105 earth and related environmental sciencesgeographyGroundwaterSeleniumgeography.geographical_feature_categoryGeologySettore GEO/08 - Geochimica E VulcanologiaDeposition (aerosol physics)chemistryVolcano13. Climate action[SDU]Sciences of the Universe [physics]Environmental chemistrySoil waterAcid rainGeologyGroundwaterSelenium
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Geogenic carbon transport through karst hydrosystems of Greece

2022

The Earth C-cycle is complex, where endogenic and exogenic sources are interconnected, operating in a multiple spatial and temporal scale (Lee et al., 2019). Non-volcanic CO2 degassing from active tectonic structures is one of the less defined components of this cycle (Frondini et al, 2019). Carbon mass-balance (Chiodini et al., 2000) is a useful tool to quantify the geogenic carbon output from regional karst hydrosystems. This approach has been demonstrated for central Italy and may be valid also for Greece, due to the similar geodynamic settings. Deep degassing in Greece has been ascertained mainly at hydrothermal and volcanic areas, but the impact of geogenic CO2 released by active tecto…

Geogenic carbon karst hydrosystems GreeceSettore GEO/08 - Geochimica E VulcanologiaGoldschmidt2022 abstracts
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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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Geogenic element behaviour in soil-rainwater interaction at Mt Etna, Sicily: preliminary results

2008

Active volcanoes emit considerable amounts of contaminants such as As, Se and V. Previous studies have shown that the volcanic activity at Mt Etna (Sicily) has a strong influence on local rainwater compositions. However to date, the behaviour of trace elements in the soils around Mt Etna is poorly understood. 4-hr batch experiments have been performed with 1:5 soil solutions of air-dried soil (fraction <2 mm) and synthetic (acid) rainwater (using either deionized water with a pH of ~6 or a ~500 ppm of sulphuric acid solution with a pH of ~2). In general trace element concentrations are more enriched in soil solutions with low pH (e.g. enrichment factor (EF) acid compared to neutral soil sol…

Geogenic element Etna soil-rainwater interaction
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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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Origin of the geogenic gases and preliminary estimation of the carbon release of Greece

2019

Volatiles are transported from the deep crust or mantle to the surface in geodynamically active areas where seismic, volcanic and geothermal activity is present; the circulation of hydrothermal fluids in the crust is enhanced. In such areas, faults may act as preferential pathways for advective gas-carrying fluid transport. Towards the surface, pressure decrease allows the gases to escape from the fluids into soil gas and eventually into the atmosphere (King, 1986). The migration of carbon-bearing crustal and mantle fluids contributes to Earth’s carbon cycle (Berner &amp; Kothavala 2001). However, till now, the mechanisms, magnitudes and time variations of carbon transfer from depth to the …

Greece geogenic gases carbon dioxideSettore GEO/08 - Geochimica E Vulcanologia
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Duvalo “Volcano” (North Macedonia): A Purely Tectonic‐Related CO 2 Degassing System

2022

Duvalo “volcano” is a site of anomalous geogenic degassing close to Ohrid (North Macedonia) not related to volcanic activity, despite its name. CO2 flux measurements made with the accumulation chamber (321 sites over ∼50,000 m2) showed fluxes up to nearly 60,000 g m-2 d-1, sustaining a total output of ∼67 t d-1. Soil gas samples were taken at 50 cm depth from sites with high CO2 fluxes and analyzed for their chemical and isotope composition. The gas is mainly composed by CO2 (&gt; 90%) with significant concentrations of H2S (up to 0.55 %) and CH4 (up to 0.32 %). The isotope compositions of He (R/RA 0.10) and of CO2 (δ13C ∼0‰) exclude significant mantle contribution, while δ13C-CH4 (∼ -35‰) …

Tectonic degassing carbon dioxide carbon cycleGeophysicsGeochemistry and Petrologystable isotopestotal CO2 outputC-cyclegas geochemistrygeogenic degassingSettore GEO/08 - Geochimica E VulcanologiaGeochemistry, Geophysics, Geosystems
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Geogenic degassing from active tectonic areas of the Balkan Peninsula

2021

During the last decades, great interest of the scientific community has been addressed to the estimation of geogenic Carbon degassing from tectonically active areas (Tamburello et al., 2018). Due to its high solubility in water, CO2 can be dissolved, transported and released to the atmosphere by groundwater. The quantity released by such process is probably of the same order of magnitude as that directly emitted from active volcanoes. The quantification of this contribution has a substantial implication for the modelling of the global atmospheric carbon cycle. The Balkan peninsula, one of the geodynamically most active regions in Europe, is characterized by intense geogenic degassing. Until…

geogenic degassing Carbon dioxide Helium Methane Balkan PeninsulaSettore GEO/08 - Geochimica E Vulcanologia
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Gas geochemistry and CO2 output estimation at the island of Milos, Greece

2018

Abstract Twenty gas samples have been collected from the natural gas manifestations of Milos Island, the majority of which is found underwater along its coast. Furthermore, three anomalous degassing fumarolic areas (Kalamos, Paleochori and Adamas) have been recognized on-land. Almost all the gases are CO2-dominated with CO2 ranging from 88 to 99% vol for the samples taken underwater, while the on-land manifestations show a wider range (15–98%) due to air contamination. Methane reaches up to 1.0% vol, H2 up to 3.2% vol and H2S up to 3.5% vol indicating a hydrothermal origin of the gases. The isotope composition of He points out to mantle contributions up to 45%, while the C-isotope compositi…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesVolcanic arcStable isotope ratioGeochemistry010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationMantle (geology)MethaneSettore GEO/08 - Geochimica E Vulcanologiachemistry.chemical_compoundGeophysicsHydrothermal gases Stable isotopes Geogenic degassing Carbon dioxideVolcanochemistryGeochemistry and PetrologyCarbon dioxideGeothermal gradientGeology0105 earth and related environmental sciencesJournal of Volcanology and Geothermal Research
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