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Geochemical evolution of groundwaters in the southern edge of Sierra de Gádor (Almería)

dc.contributor.authorVallejos, Ángela
dc.contributor.authorPulido Bosch, Antonio
dc.contributor.authorSánchez Martos, Francisco
dc.contributor.authorGisbert, Josep
dc.contributor.authorMolina, Luis
dc.description.abstractThe study of the flow paths shows the different hydrogeochemical conditions of carbonate materials in the southern edge of Sierra de Gádor. The study and modelling have consisted on the comparison of the saturation indexes evolution along the supposed flow path and the calculation of the mass balance (dissolution-precipitation processes of different phases) among the different wells analysed. The combination between the calculations of the mass transfer and the groundwater flow time allows to establish the apparent velocity of dissolution with respect to several minerals (calcite, dolomite and gypsum)en_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherMass balanceen_US
dc.subject.otherFlow pathsen_US
dc.subject.otherIsotopic characteristicsen_US
dc.titleEvolución geoquímica de las aguas subterráneas en el borde meridional de la Sierra de Gádor (Almería)en_US
dc.titleGeochemical evolution of groundwaters in the southern edge of Sierra de Gádor (Almería)eng

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Atribución-NoComercial-SinDerivadas 3.0 España
Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 España

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