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Conventional and isotopic hydrogeochemistry of CO2-rich waters of Catalonia

dc.contributor.authorRedondo, R.
dc.contributor.authorYélamos, J. G.
dc.date.accessioned2015-02-11T12:32:25Z
dc.date.available2015-02-11T12:32:25Z
dc.date.issued1999
dc.identifier.urihttp://hdl.handle.net/10272/9878
dc.description.abstractConventional and isotopic hydrogeochemical techniques have been applied to a study of CO2-rich waters in the northeast of Catalonia. Two hydrogeochemical facies, a calcium-bicarbonate and another sodium-bicarbonate are clearly distinguished. The second one seems to be the result of evolution from the calcium facies. The tritium-ages support the previous division in two hydrogeochemical facies. Measurements of ,sO and deuterium ratio indicate that the carbonic waters have a meteoric origin. The i3C/12C ratio varied from -5,0 to -0,64 6°/œ showing a deep origin of COen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherGround wateren_US
dc.subject.otherCO2-rich watersen_US
dc.subject.otherHydrogeochemistryen_US
dc.subject.otherEnvironmental isotopesen_US
dc.subject.otherCataloniaen_US
dc.titleHidrogeoquímica convencional e isotópica de las aguas carbónicas de Cataluñaen_US
dc.titleConventional and isotopic hydrogeochemistry of CO2-rich waters of Cataloniaeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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