Abstract

Original abstract online at
https://link.springer.com/article/10.1007/s10653-026-03165-0

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 (?1?O and ?2H), 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.

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Data availability

The datasets generated and analysed during the current study are not publicly available due to restrictions related to institutional policy and regional confidentiality of groundwater well information, but they are available from the corresponding author on reasonable request.

References

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Acknowledgement

The authors would like to thank the Sistan and Baluchestan water and wastewater Co.

Funding

This work was supported by the Iran National Science Foundation (INSF) under Grant No. 4037853. No other funds, grants, or financial support were received for the preparation of this manuscript.

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Authors and Affiliations

Contributions

All authors contributed to the study conception and design. Material preparation, field sampling, laboratory analyses, data processing, hydrogeochemical modelling, and statistical computations were performed by **Reza Jahanshahi**, **Hafizeh Rigi Karvandari**, and **Sepideh Mali**. The first draft of the manuscript was written by **Reza Jahanshahi**, and all authors provided critical revisions and comments on previous versions of the manuscript. All authors read and approved the final manuscript.

Corresponding author

Correspondence to Reza Jahanshahi.

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Conflict of interest

The authors declare no conflict of interest.

Ethics approval

This study involved no human participants, animal subjects, or identifiable personal data. All groundwater sampling and field procedures complied with institutional and national guidelines. Ethics approval was not required, as the research was limited to environmental water sampling and chemical analysis.

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Not applicable. No human participants were involved in this study.

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Not applicable. The manuscript does not contain data from any individual person, images of human subjects, or identifiable personal information.