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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2483
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dc.contributor.authorallD'Alessandro, W.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallBrusca, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallKyriakopoulos, K.; Department of Geology, University of Athens, Athens, Greece.en
dc.contributor.authorallRotolo, S.; Dipartimento di Chimica e Fisica della Terra ed Applicazioni (CFTA), University of Palermo, Palermo, Italy.en
dc.contributor.authorallMichas, G.; Department of Geology, University of Athens, Athens, Greece.en
dc.contributor.authorallMinio, M.; Dipartimento di Chimica e Fisica della Terra ed Applicazioni (CFTA), University of Palermo, Palermo, Italy.en
dc.contributor.authorallPapadakis, G.; Department of Geology, University of Athens, Athens, Greece.en
dc.date.accessioned2007-09-17T14:10:44Zen
dc.date.available2007-09-17T14:10:44Zen
dc.date.issued2006en
dc.identifier.urihttp://hdl.handle.net/2122/2483en
dc.description.abstractWe report first data on chemical composition of the gas emitted by the geothermal system of Sousaki, Greece. Gas manifestations display typical geothermal gas composition with CO2 as the main component and CH4 and H2S as minor species. Soil gas composition derives from the mixing of two end-members (atmospheric air and geothermal gas). Soil CO2 fluxes range from<2 to 33,400 g m 2 d 1. The estimated diffuse output of hydrothermal CO2, estimated for an area of 0.015 km2, is about 630 g s 1, while a tentative estimation of CH4 diffuse output gave a value of about 1.15 g s 1. Point sources accounted for lower flux values of 26 g s 1 of CO2, 0.1 g s 1 of CH4 and 0.02 g s 1 of H2S.en
dc.language.isoEnglishen
dc.publisher.nameAguen
dc.relation.ispartofGeoph. Res. Lett.en
dc.relation.ispartofseries/ 33 (2006)en
dc.subjectcarbon dioxideen
dc.subjectmethane emissionsen
dc.subjectgeothermal system,en
dc.titleDiffuse and focused carbon dioxide and methane emissions from the Sousaki geothermal system, Greeceen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumberL05307en
dc.subject.INGV03. Hydrosphere::03.04. Chemical and biological::03.04.06. Hydrothermal systemsen
dc.identifier.doi10.1029/2006GL025777en
dc.relation.referencesBender, M., and R. Conrad (1995), Effect of CH4 concentrations and soil conditions on the induction of CH4 oxidation activity, Soil Biol. Biochem., 27, 1517– 1527. Cardellini, C., G. Chiodini, and F. Frondini (2003), Application of stochastic simulation to CO2 flux from soil: Mapping and quantification of gas release, J. Geophys. Res., 108(B9), 2425, doi:10.1029/2002JB002165. Castaldi, S., and D. Tedesco (2005), Methane production and consumption in an active volcanic environment of Southern Italy, Chemosphere, 58, 131–139. Chiodini, G., R. Cioni, M. Guidi, B. Raco, and L. Marini (1998), Soil CO2 flux measurements in volcanic and geothermal areas, Appl. Geochem., 13, 543–552. Etiope, G., P. Beneduce, M. Calcara, P. Favali, F. Frugoni, M. Schiattarella, and G. Smriglio (1999), Structural pattern and CO2–CH4 degassing of Ustica Island, Southern Tyrrhenian basin, J. Volcanol. Geotherm. Res., 88, 291–304. Etiope, G., A. Caracausi, R. Favara, F. Italiano, and C. Baciu (2002), Methane emission from the mud volcanoes of Sicily (Italy), Geophys. Res. Lett., 29(8), 1215, doi:10.1029/2001GL014340. Fytikas, M., P. Dalambakis, V. Karkoulias, and D. Mendrinos (1995), Geothermal exploration and development activities in Greece during 1990–1994, paper presented at World Geothermal Congress 1995, Int. Geothermal Assoc., Rome. Hernandez, P. A., N. M. Perez, J. M. Salazar, S. Nakai, K. Notsu, and H. Wakita (1998), Diffuse emissions of carbon dioxide, methane and helium-3 from Teide volcano, Tenerife, Canary Island, Geophys. Res. Lett., 25, 3311 –3314. Kelepertsis, A., D. Alexakis, and I. Kita (2001), Environmental geochemistry of soils and waters of Susaki area, Korinthos, Greece, Environ. Geochem. Health, 23, 117–135. Kyriakopoulos, K., R. Kanakis-Sotiriou, and M. G. Stamatakis (1990), The authigenic minerals formed from volcanic emanations at Soussaki, West Attica peninsula, Greece, Can. Mineral., 28, 363–368. Lewicki, J. L., D. Bergfeld, C. Cardellini, G. Chiodini, D. Granieri, N. Varley, and C. Werner (2005), Comparative soil CO2 flux measurements and geostatistical estimation methods on Masaya volcano, Nicaragua, Bull. Volcanol., 68, 76– 90. Mo¨ rner, N. A., and G. Etiope (2002), Carbon degassing from the lithosphere, Global Planet. Change, 33, 185– 203. Pecoraino, G., L. Brusca, W. D’Alessandro, S. Giammanco, S. Inguaggiato, and M. Longo (2005), Total CO2 output from Ischia Island volcano (Italy), Geochem. J., 39, 451– 458. Pe-Piper, G., and K. Hatzipanagiotou (1997), The Pliocene volcanic rocks of Crommyonia, western Greece and their implications for the early evolution of the South Aegean arc, Geol. Mag., 134, 55–66. Stiros, S. C. (1995), The 1953 seismic surface fault: Implications for the modeling of Sousaki (Corinth area, Greece) geothermal field, J. Geodyn., 20, 167– 180. Vasarhelyi, A., I. Hunyadi, I. Csige, J. Hakl, E. Hertelendi, J. Borrosay, and K. Torkos (1997), Radon enriched deep earthgas upflow in a seismically active inhabited area, in Rare Gas Geochemistry: Applications in Earth and Environmental Sciences, edited by H. S. Virk, pp. 221– 235, Guru nanak Dev. Univ., Amritsar, India.en
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorD'Alessandro, W.en
dc.contributor.authorBrusca, L.en
dc.contributor.authorKyriakopoulos, K.en
dc.contributor.authorRotolo, S.en
dc.contributor.authorMichas, G.en
dc.contributor.authorMinio, M.en
dc.contributor.authorPapadakis, G.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentDepartment of Geology, University of Athens, Athens, Greece.en
dc.contributor.departmentDipartimento di Chimica e Fisica della Terra ed Applicazioni (CFTA), University of Palermo, Palermo, Italy.en
dc.contributor.departmentDepartment of Geology, University of Athens, Athens, Greece.en
dc.contributor.departmentDipartimento di Chimica e Fisica della Terra ed Applicazioni (CFTA), University of Palermo, Palermo, Italy.en
dc.contributor.departmentDepartment of Geology, University of Athens, Athens, Greece.en
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.deptUniversity of Athens, Dept. Geology and Geoenvironment, Greece-
crisitem.author.deptUniversità degli Studi di Palermo-
crisitem.author.deptUniversity of Athens, Dept. Geology and Geoenvironment-
crisitem.author.deptDipartimento di Chimica e Fisica della Terra ed Applicazioni (CFTA), University of Palermo, Palermo, Italy.-
crisitem.author.deptUniversity of Athens, Dept. Geology and Geoenvironment-
crisitem.author.orcid0000-0003-1724-0388-
crisitem.author.orcid0000-0002-6570-9673-
crisitem.author.orcid0000-0002-7498-4589-
crisitem.author.orcid0000-0001-7523-1338-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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