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Investigations of Sediment-water Interactions in Western U.S. Water Bodies |
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BENTHIC
FLUX OF METALS AND NUTRIENTS PROJECT |
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Camp Far West Reservoir, CaliforniaIn the northwestern Sierra Nevada, the historic, routine use of mercury for processing gold ore had resulted in mercury contamination and bioaccumulation of methylmercury within major watersheds. Previous studies by the USGS scientists from the Caolifirnia District demonstrated that: (1) Sierra Nevada watersheds export mercury to the Bay-Delta via the Sacramento River, and (2) fish from five reservoirs in the Bear River, Deer Creek and South Yuba River watersheds (among the most intensely mined) have elevated tissue-concentrations of mercury (Mercury Contamination in California Fact Sheet). The evaluation and development of remedial actions, including Total Maximum Daily Load (TMDLs), within Sierra Nevada watersheds is highly dependent on our understanding of controls of methylmercury production, transport and bioaccumulation. The relative contributions of mercury and methylmercury loads from the Bear, Yuba, and Feather rivers are poorly known; present estimates are based on scanty data from inconsistent flow regimes. This study is part of a collaboration with the USGS California District and the California State Water Resources Control Board to identify and quantify factors regulating mercury methylation, demethylation, and bioaccumulation in Sierra Nevada watersheds. In part, initial, direct determinations of total methyl-mercury benthic flux are being determined to: (1) evaluate the potential importance of sediment-water interactions in Camp Far West Reservoir along the Bear River, relative to other sources and sinks within the watershed, and (2) to identify processes that may regulate the spatial and temporal variability of those benthic interactions. Related Publications: Sediment-Water
Interactions Affecting Dissolved-Mercury Distributions in Camp Far West
Reservoir, California Mercury Contamination from Historical
Gold Mining in California
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