The Variability of Fluorine Concentration in the Essentuki Mineral Water Field and its Relationship with Hydrogeological Conditions
摘要
Abstract
The fluorine content in the waters of four aquifers of the Essentuki mineral water field (Danian–Selandian, Cenomanian–Maastrichtian, Aptian–Lower Albian, and Tithonian–Valanginian) is determined. The possibility of regulating the fluorine content in extracted mineral water by changing the intensity of well operation is shown.