Item talk:Q238890
From geokb
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"abstract": "The Cinnabar and Fern mine sites in central Idaho are primary source areas for elevated mercury and arsenic entering the South\nFork of the Salmon River, which provides critical spawning habitat for bull trout and Chinook salmon. Mercury mineralization is\nhosted by carbonate rocks, which generate waters dominated by Ca2+ and HCO3\n- at pH 7 to 9. A synoptic sampling was\nconducted on headwater tributaries to determine geologic background concentrations and quantify trace metal concentrations in\nstream water associated with historical mining. Geologic background concentrations in unfiltered Cinnabar Creek water were 8 -\n14 ng Hg L-1 and 4.8 - 9.5 \u00b5g As L-1. Immediately downstream from the mine site, concentrations increased to 257 ng Hg L-1\nand 20.6 \u00b5g As L-1. Groundwater inflow diluted these concentrations by approximately half before the confluence of Cinnabar\nCreek with Sugar Creek. As expected, mercury and arsenic concentrations increased downstream in Sugar Creek below the\nconfluence with Cinnabar Creek. However, the final downstream reach on Sugar Creek showed an increase in unfiltered\nmercury, methylmercury, and iron concentrations relative to the upstream reach. This increase is associated with historical\nmining activity in a mineralized area of carbonate rock that intersects the reach.",
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