Hidrogeoquímica convencional e isotópica de las aguas carbónicas de Cataluña

dc.contributor.author	Redondo, R.
dc.contributor.author	Yélamos, J. G.
dc.date.accessioned	2015-02-11T12:32:25Z
dc.date.available	2015-02-11T12:32:25Z
dc.date.issued	1999
dc.description.abstract	Conventional 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 CO	en_US
dc.identifier.uri	http://hdl.handle.net/10272/9878
dc.language.iso	spa	en_US
dc.publisher	Sociedad Geológica de España	en_US
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.accessRights	open access	en_US
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	Ground water	en_US
dc.subject.other	CO2-rich waters	en_US
dc.subject.other	Hydrogeochemistry	en_US
dc.subject.other	Environmental isotopes	en_US
dc.subject.other	Catalonia	en_US
dc.title	Hidrogeoquímica convencional e isotópica de las aguas carbónicas de Cataluña	en_US
dc.title	Conventional and isotopic hydrogeochemistry of CO2-rich waters of Catalonia	eng
dc.type	journal article	en_US
dspace.entity.type	Publication

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