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Medical Hydrology and Balneology: Environmental Aspects

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Therapeutic indications of the mineral waters of<br />

Galicia (NW Spain) according to their<br />

thermo-hydrogeological characteristics<br />

Juncosa R (1) , Mejide R (2) , Delgado J (1)<br />

(1) University of Coruña, Water engineering <strong>and</strong> the environment group (GEAMA), Spain<br />

(2) University of A Coruña, Departament of Medicine, A Coruña, Spain<br />

rmf@udc.es<br />

Introduction <strong>and</strong> Objectives<br />

The therapeutic properties of mineral waters from Galicia (NW Spain) are related<br />

to the chemical characteristics of the sources that outcrop in Galicia. The chemistry<br />

of the water is directly related to the geologic matrix by flowing <strong>and</strong> which is<br />

enriched mineralogically. Therefore, Galicia appears to be very rich in terms of<br />

exploitation, applications <strong>and</strong> using of different thermal, mineral-natural <strong>and</strong> mineral-medicinal<br />

resources.<br />

Galicia is one of a large outcrop dominated by igneous <strong>and</strong> metamorphic rocks<br />

called Hesperian Massif where there are many thermal manifestations. The<br />

groundwater flow can develop in very different time scales according to the hydrodynamic<br />

<strong>and</strong> geological characteristics. Groundwater dissolved minerals as they<br />

ascend to the surface.<br />

Materials <strong>and</strong> Methods<br />

Study of the hydrochemical situation of groundwater <strong>and</strong> mineral springs of Galicia<br />

regarding the common characteristics of Galician waters, the substrate geological<br />

outcrop, identifying physical <strong>and</strong> chemical parameters <strong>and</strong> therapeutic use<br />

Results<br />

Most of the groundwater flowing through silicate lithologies is medium <strong>and</strong><br />

coarse grain. They tend to be sodium/potasium bicarbonate. However, in some<br />

thermal source <strong>and</strong> source near the coast, the chlorinated component can be very<br />

important (e.g.: Thermal source of A Toxa, Caldas de Reis). The deepwater ascent<br />

through igneous <strong>and</strong> metamorphic rocks with sulphide content, (where conditions<br />

are anoxic) can cause sulfur sources on the surface (e.g.: Spa of Guitiriz, Baños da<br />

Brea, Termas de Cuntis) . The water passing through carbonate rocks (limestone<br />

<strong>and</strong> dolomite) causes water with calcium bicarbonate or calcium / magnesium<br />

chemism. There is also a characterization gaseous in some sources for the chemical<br />

imbalance of water with the carbonated rock (e.g.: Mondariz, Agua de Cabreiroá,<br />

Agua de Fonte Nova).<br />

Balnea 430<br />

ISBN: 978-84-669-1887-0<br />

978-84-669-3482-4<br />

2012, núm. 6, 430-431

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