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Water-rock interaction processes and uranium behaviour in El Berrocal granitic system (Centra! Spain)

dc.contributor.authorGómez, P.
dc.contributor.authorTurrero, J.
dc.contributor.authorPeña, J.
dc.contributor.authorGimeno, María J.
dc.contributor.authorCrespo, M. T.
dc.contributor.authorGordienko, F.
dc.contributor.authorMartínez, B.
dc.contributor.authorReyes, E.
dc.contributor.authorRivas, P.
dc.contributor.authorIvanovich, M.
dc.description.abstractThis work depicts a synthesis of the main water-rock interaction processes controlling the water chemistry in El Berrocal granitic pluton, emphasizing in the uranium geochemistry. An uranium-sulphide dyke controls the general characteristics of the system at the site scale. Dissolution/precipitation of calcite Is the m ost im p o rta n t process in the area. U ra n iu m concentration ranges from 4x10 ~9M to 8x10 ' 6M . Undersaturation with respect to most of uranium minerals occurs in the water. Adsorption processes can be considered as main mechanism of uranium retentionen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherEl Berrocal plutonen_US
dc.subject.otherWater-rock interactionen_US
dc.subject.otherUranium geochemistryen_US
dc.titleProcesos de interacción agua-roca y comportamiento del uranio en el sistema granítico de El Berrocal (España)en_US
dc.titleWater-rock interaction processes and uranium behaviour in El Berrocal granitic system (Centra! Spain)eng

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