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Hydrogeochemistry and microbiology of Hervideros (C02-rich waters) in Campo de Calatrava (Ciudad Real)

dc.contributor.authorYélamos, J. G.
dc.contributor.authorRedondo, R.
dc.contributor.authorCastro, F. de
dc.contributor.authorGalván, A.
dc.contributor.authorMartínez Rubio, J.
dc.contributor.authorRuano, Patricia
dc.contributor.authorSenderos, A. J.
dc.contributor.authorViIIarroya, F. I.
dc.contributor.authorRebollo Ferreiro, Luis F.
dc.description.abstractCÓZ-rich springs and wells in the Campo de Calatrava commonly are named Hervideros. This .ground water is originated by deep circulation along the fractures of the paleozoic rocks of the area, with residence times longer than 15years. The hydrochemical facies is miked-catipn bicarbonate and is related to the extinct yolcanism 6f the area. It is a possibility that not all the Hervideros are originated from volcapic or . > magmatic C02. Bacterial evaluation indicates high values, but probably it is representative of the-biomass presence in the proper sampling point instead of the groundwater-microbiologyen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherC02-rich wateren_US
dc.subject.otherHydrogeochemistry groundwater microbiologyen_US
dc.subject.otherCampo de Calatravaen_US
dc.titleHidrogeoquímica y microbiología en Los Hervideros del Campo de Calatrava (Ciudad Real)en_US
dc.titleHydrogeochemistry and microbiology of Hervideros (C02-rich waters) in Campo de Calatrava (Ciudad Real)eng

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