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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10653
DC FieldValueLanguage
dc.date.accessioned2017-12-13T13:14:54Zen
dc.date.available2017-12-13T13:14:54Zen
dc.date.issued2017en
dc.identifier.urihttp://hdl.handle.net/2122/10653en
dc.description.abstractThis study focuses on the interaction among deep volcanic/hydrothermal gases, groundwater and soil gases at Vulcano Island (Aeolian Archipelago, Italy). The chemical-physical parameters of the groundwater, the total dissolved inorganic carbon (TDIC) and the isotopic composition of the CO2 dissolved in groundwater are reported and discussed. Furthermore, a comparison between soil gases and groundwater indicates that groundwater and soil gases show the same qualitative information, giving a good overall picture of the main degassing zones of a volcanic system, whereas the soil gas discharge provides an evaluation of the mass released by the deep feeding system. This approach can be a useful tool both to characterize mixing and/or interaction processes among different sources and for a monitoring of degassing activity of a volcanic system.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofProcedia Earth and Planetary Scienceen
dc.relation.ispartofseries/17 (2017)en
dc.subjectSoil CO2 fluxen
dc.subjectDissolved gasesen
dc.subjectIsotope composition of CO2en
dc.subjectGroundwatersen
dc.subjectVulcano Islanden
dc.titleDissolved Carbon in Groundwater versus Gas Emissions from the Soil: The Two Sides of the Same Coinen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber116-119en
dc.subject.INGV03.02. Hydrologyen
dc.subject.INGV04.08. Volcanologyen
dc.identifier.doi10.1016/j.proeps.2016.12.021en
dc.relation.references1. Capasso G, Favara R, Francofonte S, Inguaggiato S. Chemical and isotopic variations in fumarolic discharge and thermal waters at Vulcano Island (Aeolian Islands, Italy) during 1996: evidence of resumed volcanic activity. J Volcanol Geoth Res 1999; 88(3), 167-175. 2. Capasso G, D’Alessandro W, Favara R, Inguaggiato S, Parello F. Interaction between the deep fluids and the shallow groundwaters on Vulcano island (Italy). J Volcanol Geoth Res 2001; 108, 187-198. 3. Favara R, Grassa F, Inguaggiato S, Pecoraino G, Capasso G. A simple method to determine the δ13C content of total dissolved inorganic carbon. Geofisica Internacional 2002; 41-3, 313-320. 4. Camarda M, Gurrieri S, and Valenza M. CO2 flux measurements in volcanic areas using the dynamic concentration method: Influence of soil permeability, J Geophys Res 2006; 111. 5. Di Martino RMR, Camarda M, Capasso G. In situ determination of the carbon isotopologues of the CO2 emitted by soils. In Rendiconti Online della Società Geologica Italiana; 2015, 35-2. p. 367. 6. Sommaruga C. Le ricerche geotermiche svolte a Vulcano negli anni '50. In Rendiconti della Società Italiana di Mineralogia e Petrologia; 1984. pp. 355-366. 7. Capasso G, Favara R, Inguaggiato S. Chemical features and isotopic gaseous manifestation on Vulcano Island (Aeolian Island): an interpretative model of fluid circulation. Geochim Cosmochim Acta 1997; 61, 3425-3442. 8. Capasso G, D’Alessandro W, Favara R, Inguaggiato S, Parello F. Kinetic isotope fractionation of CO2 carbon due to diffusion processes through the soil. Water-Rock Interaction 10. Swets & Zeitlinger, Lisse; 2001.en
dc.description.obiettivoSpecifico2V. Struttura e sistema di alimentazione dei vulcanien
dc.description.obiettivoSpecifico4V. Dinamica dei processi pre-eruttivien
dc.description.journalTypeN/A or not JCRen
dc.contributor.authorCapasso, Giorgioen
dc.contributor.authorDi Martino, Roberto M. R.en
dc.contributor.authorCamarda, Marcoen
dc.contributor.authorPrano, Vincenzoen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.orcid0000-0002-0890-7948-
crisitem.author.orcid0000-0001-6435-2759-
crisitem.author.orcid0000-0003-1527-7910-
crisitem.author.orcid0000-0003-3873-3720-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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