Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7159
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dc.contributor.authorallD'Alessandro, W.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallBellomo, S.; 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.authorallKarakazanis, S.; University of Patras, Dept. Geology, Greeceen
dc.contributor.authorallKyriakopoulos, K.; University of Athens, Dept. Geology and Geoenvironment, Greeceen
dc.contributor.authorallLiotta, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.editorallLambrakis, N.; University of Patras, Dept. of Geology, Greeceen
dc.contributor.editorallStournaras, G.; University of Athens, Dept. of Geology and Geoenvironment, Greeceen
dc.contributor.editorallKatsanou, K.; University of Patras, Dept of Geology, Greeceen
dc.date.accessioned2011-10-17T06:33:06Zen
dc.date.available2011-10-17T06:33:06Zen
dc.date.issued2011en
dc.identifier.isbn978-3-642-24075-1en
dc.identifier.urihttp://hdl.handle.net/2122/7159en
dc.description.abstractGas and water samples were collected at CO2-rich wells in the plain of Florina (N. Greece). Chemical and isotopic composition of the analysed gases reveals their main crustal origin even if a small but significant contribution of mantle derived gases can be recognized. As a consequence of CO2 dissolution, HCO3- is always the main dissolved anion while cationic composition allows us to distinguish at least two main groups characterized by Na or Ca as dominant dissolved cations. The water-rock interaction is strongly enhanced by the dissolution of CO2 and the consequent lowering of pH. Such a process increases the mobility of some trace elements whose concentrations very often exceed UE drinking water limits. This study confirms that the Florina basin represents a good natural analogue of carbon storage systems and underscores the fact that possible deterioration of water quality due to CO2 leaks of the reservoirs must be carefully taken in account.en
dc.language.isoEnglishen
dc.publisher.nameSpringer-Verlagen
dc.relation.ispartofAdvances in the Research of Aquatic Environment - vol. 2en
dc.subjectGroundwateren
dc.subjectWater qualityen
dc.subjectcarbon dioxideen
dc.subjecttrace elementsen
dc.titleThe impact on water quality of the high carbon dioxide contents of the groundwater in the area of Florina (N. Greece)en
dc.typebook chapteren
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber135-143en
dc.subject.INGV03. Hydrosphere::03.02. Hydrology::03.02.03. Groundwater processesen
dc.subject.INGV03. Hydrosphere::03.02. Hydrology::03.02.04. Measurements and monitoringen
dc.subject.INGV03. Hydrosphere::03.04. Chemical and biological::03.04.03. Chemistry of watersen
dc.subject.INGV03. Hydrosphere::03.04. Chemical and biological::03.04.05. Gasesen
dc.description.obiettivoSpecifico4.5. Studi sul degassamento naturale e sui gas petroliferien
dc.description.fulltextreserveden
dc.contributor.authorD'Alessandro, W.en
dc.contributor.authorBellomo, S.en
dc.contributor.authorBrusca, L.en
dc.contributor.authorKarakazanis, S.en
dc.contributor.authorKyriakopoulos, K.en
dc.contributor.authorLiotta, M.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.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentUniversity of Patras, Dept. Geology, Greeceen
dc.contributor.departmentUniversity of Athens, Dept. Geology and Geoenvironment, Greeceen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.editorLambrakis, N.en
dc.contributor.editorStournaras, G.en
dc.contributor.editorKatsanou, K.en
dc.contributor.editordepartmentUniversity of Patras, Dept. of Geology, Greeceen
dc.contributor.editordepartmentUniversity of Athens, Dept. of Geology and Geoenvironment, Greeceen
dc.contributor.editordepartmentUniversity of Patras, Dept of Geology, Greeceen
item.openairetypebook chapter-
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.deptUniversity of Patras, Greece-
crisitem.author.deptUniversity of Athens, Dept. Geology and Geoenvironment, Greece-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italia-
crisitem.author.orcid0000-0003-1724-0388-
crisitem.author.orcid0000-0002-6570-9673-
crisitem.author.orcid0000-0002-7498-4589-
crisitem.author.orcid0000-0002-7203-1565-
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.parent03. Hydrosphere-
crisitem.classification.parent03. Hydrosphere-
crisitem.classification.parent03. Hydrosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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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