Abstract
Content of dissolved fluorides in the waters of 13 mud volcanoes of the Kerch-Taman region was determined: 0,13–2,00 mg/l with average value of 0,87 mg/l (n = 37). A fairly close correlation was established between the fluorine concentration and pH value (r = 0.80) in the absence of correlation with mineralization and content of components of the basic salt composition. It was suggested that the fluorine concentration in mud-volcano waters is controlled by the exchange reaction where et is content of adsorbed and structural fluorine (hydroxyl ions) in the clay minerals; F– et OH– is concentration of fluorides (hydroxyl ions) in the aqueous phase.
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