Zusammenfassung
Thermales Tiefenwasser spiegelt die Herkunft, die Zirkulationsdauer und die Wechselwirkungen mit dem Umgebungsgestein wieder. Die meisten Tiefenwässer weisen eine erhöhte Mineralisation und Gasgehalte auf. Um Aussagen zu den Eigenschaften des geförderten Thermalwassers und den möglichen Auswirkungen zu treffen, ist die genaue Kenntnis der Inhaltsstoffe eine grundlegende Voraussetzung für den erfolgreichen Langzeitbetrieb der geothermischen Anlage.
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Stober, I., Bucher, K. (2012). Hydrochemische Untersuchungen. In: Geothermie. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-24331-8_14
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