In the United States, almost 40% of the nation’s river length and lake area have mercury fish consumption advisories [1]. Discharge from abandoned mines is a primary source of mercury to California watersheds, where both mercury and gold were mined extensively [2]. We have characterized watershed impacts from historic mining operations and evaluated the effectiveness of mine site and stream restoration efforts [3-5]. However, even low mercury inputs from atmospheric deposition can pose an ecosystem threat because mercury is a bioaccumulative toxin. It is important to understand how this contaminant cycles through terrestrial watersheds and to identify the mechanisms driving biologic uptake [6]. We combine hydrology and geochemistry to study the effects of groundwater-surface water interaction on lacustrine and riparian mercury dynamics (e.g., hyporheic zone processes [7]) and apply geomorphologic tools to evaluate mercury-sediment interactions (e.g., transport distance, depositional environments, and time scales for sequestration and erosion). [7] Alley, W.M., R.W. Healy, J.W. LaBaugh, and T.E. Reilly, Flow and storage in groundwater systems. science, 2002. 296(5575): p. 1985-1990. |
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