Sulfur geochemistry of hydrothermal waters in Yellowstone National Park: I. The origin of thiosulfate in hot spring waters

@inproceedings{MahadevaIyer1998SulfurGO,
  title={Sulfur geochemistry of hydrothermal waters in Yellowstone National Park: I. The origin of thiosulfate in hot spring waters},
  author={Y. MahadevaIyer and Jie Xu and A. P. Knight M.A. and Martin A. A. Schoonen and D. KenjiSatoPh. and Darrell Kirk Nordstrom and K. Mallika and Patrick N. Cunningham and J. W. and Robert Mason Ball},
  year={1998}
}
Thiosulfate (S2O3 ), polythionate (SxO6 ), dissolved sulfide (H2S), and sulfate (SO 4 ) concentrations in thirty-nine alkaline and acidic springs in Yellowstone National Park (YNP) were determined. The analyses were conducted on site, using ion chromatography for thiosulfate, polythionate, and sulfate, and using colorimetry for dissolved sulfide. Thiosulfate was detected at concentrations typically less than 2 mmol/L in neutral and alkaline chloride springs with low sulfate concentrations (Cl… CONTINUE READING
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