Abstract
The Kharaqan hot springs are located in the historic city of Abe-Garm, famous for its hot springs, in Qazvin province, in northwestern Iran. Thermal waters with temperatures ranging from 28.7 to 52 °C vary in chemical composition and TDS contents. Those waters generally are enriched in Na–Cl–HCO3 and suggest deep water circulation. Chemistry of all of the water samples are graphed in the Cl–SO4–HCO3 ternary diagram. There is a trend of mixing along a line of constituent proportions between recently recharged water and older water. The trend toward the chloride corner is mainly the result of contact in the subsurface with evaporite-bearing formations and/or mixing with brines. Relatively high concentrations of Na, Ca, K, Cl, and SO4 resulted from rock/water interactions. These hot spring waters show high concentrations of arsenic (0.14–0.95 mg L−1). The diffusion of As-bearing spring waters into shallow aquifers could contaminate the groundwater which is used for drinking purposes. Also discharges of this As-enriched water into streams and rivers could affect irrigated crops in downstream fields. In both cases, the health of local residents could be at risk.
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The authors would like to express their thanks to the Geological Survey of Iran and Shahid Beheshti University for providing the funds for this project.
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Yazdi, M., Taheri, M. & Navi, P. Environmental geochemistry and sources of natural arsenic in the Kharaqan hot springs, Qazvin, Iran. Environ Earth Sci 73, 5395–5404 (2015). https://doi.org/10.1007/s12665-014-3794-4
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DOI: https://doi.org/10.1007/s12665-014-3794-4