Rasgos hidrogeoquímicos de las aguas termales en los acuíferos carbonatados del Bajo Andarax (Almería)

摘要: The carbonate aquifers of the Lower Andarax is a significant geothermal anomaly, as evidenced by high temperature spring waters (22 - 40 OC). most saline (2000 3000 mg.L-1) correspond to Deep Aquifer; which presents sodium chloride sulphate facies, while least (500 mg.L-1), with magnesium calcite bicarbonate type, are found in some sectors Carbonate Aquifer. Aquifer having less and directly associated more rapid flows can thus be identified. In Aquifer, situation complex, tense thermal anomaly area acts conjunction influence evaporitic materials long residence time groundwater; factors tend produce concentrations boron and lithium.