Evolución geoquímica de las aguas subterráneas en una cuenca sedimentaria semiárida: acuífero de Baza-Caniles, Granada, España

摘要: The physico-chemical data from the analysis of water Baza-Caniles detritic aquifer(Province Granada,Spain), was used to asses quality groundwater resources, and determine main geochemical process which are taking place in aquifer system. An incongruent dolomite dissolution identified unconfined sectors mio-pliocene a rise CO2 content can be observed, encourages carbonate dissolution. bicorbanate-sulfate character confined shallow is interpreted as result calcite precipitation, accompanied certain areas by halite slightly reducing medium. A reduction zone linked deep sector aquifer, under evaporite impermeable materials, analytical data. characteristics this brackish sulphate redox process.