Hydrogeochemical Signatures and Processes Influencing Mineral Waters at Furnas Volcano (São Miguel, Azores)
2025
Letícia Ferreira | José Virgílio Cruz | Fátima Viveiros | Nuno Durães | César Andrade | Carlos Almeida | Nuno Cabral | Rui Coutinho | José Francisco Santos
Furnas volcano, one of the three active central volcanoes of Sã:o Miguel (the Azores archipelago), hosts mineral waters with significant special variations, divided into hyperthermal (89.4&ndash:95.4 °:C), thermal (29.9&ndash:70.0 °:C), and cold (14.2&ndash:21.4 °:C) waters. Groundwaters are classified as Na-HCO3, with a neutral to slightly acidic pH, except one SO4-Na acidic sample. The major elements are primarily influenced by rock leaching and volcanic input, patterns also reflected in the trace elements, including the rare earth elements. The major cations, along with lithium, iron, aluminum, rubidium, and strontium, indicate the influence of water&ndash:rock interactions. Some samples depict a higher influence in this input, shown by the similar REE behavior between them and the local rock behavior. The volcanic input is distinguished into two environments: an acid sulfate boiling pool, formed by steam heating, and neutral HCO3-Cl waters, where bicarbonate-rich waters mix with a neutral chloride fluid from a deep reservoir. The deeper reservoir also provides boron, arsenic, antimony, and tungsten, also seemingly associated with a positive spike in europium due to rock dissolution at temperatures above 250 °:C or a reducing environment. This interpretation is corroborated by the stability of the strontium isotopes between samples.
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