Geogenic fluoride enrichment in groundwater of a volcanic terrain: hydrogeochemical processes, exposure pathways, and human health risk assessment
摘要
Elevated fluoride in groundwater is increasingly recognized as a major geogenic and public health concern in volcanic terrains. In the Taftan volcanic region of southeastern Iran, fluoride concentrations ranged from 0.04 to 1.77 mg/L, with 43% of samples exceeding the WHO drinking-water guideline value (1.5 mg/L) and approximately 57% exceeding the regionally optimal concentration of 0.68 mg/L. A total of 28 water samples collected from rivers, wells, springs, and qanats were analyzed for major ions, physicochemical parameters, stable isotopes (δ1⁸O and δ2H), and fluoride-related health risk indicators. Hydrochemical facies evolved from Ca–HCO₃ waters toward Ca–Cl–SO4 and mixed types, reflecting progressive water–rock interaction and localized evaporative effects. Correlation analysis, ionic ratios, mineral saturation indices, and principal component analysis consistently indicate that fluoride mobilization is primarily controlled by silicate weathering processes, particularly the dissolution of fluoride-bearing aluminosilicate minerals such as biotite and muscovite, coupled with calcium removal through carbonate precipitation and ion exchange. Distinct relationships among Ca2+–F⁻, HCO₃⁻–F⁻, and SO42⁻–F⁻ suggest combined contributions from fluorite equilibrium, surface desorption mechanisms, and minor sulfate-associated fluoride phases. The fluoride–pH relationship exhibits a characteristic U-shaped trend, with minimum concentrations near neutral pH and enhanced solubility under both acidic and alkaline conditions. Stable isotope signatures differentiate meteoric recharge-dominated groundwater from surface waters affected by evaporation, supporting the interpretation of contrasting hydrogeochemical evolution pathways. Health risk assessment reveals elevated non-carcinogenic risk for children in approximately 38% of the samples, emphasizing the vulnerability of younger populations to chronic fluoride exposure. These findings highlight the critical role of volcanic lithology in governing fluoride enrichment and underscore the need for targeted groundwater management and health risk mitigation strategies in arid and semi-arid volcanic regions.