2008
DOI: 10.3133/sir20065008
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Environmental factors affecting mercury in Camp Far West Reservoir, California, 2001-03

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Cited by 4 publications
(11 citation statements)
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References 14 publications
(22 reference statements)
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“…For example, chlorophyll a concentrations in surface water were highest (mean value of 13 ± 5.4 mgÁL -1 ) in the fall and winter as water levels rose and lowest (3.5 ± 0.90 mgÁL -1 ) in the spring and summer as water levels declined. The peak in chlorophyll concentrations during fall of both years occurred at low water while the reservoir was thermally stratified (Alpers et al 2008) and was generally sustained as the reservoir filled. The development of the bloom prior to destratification was not expected, since algal blooms typically occur when nutrients are mixed from the deep portions of the reservoir into surface waters following destratification, particularly in oligotrophic systems such as CFWR (N:P ratios of 136 to 5191; Kuwabara et al 2003).…”
Section: Resultsmentioning
confidence: 99%
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“…For example, chlorophyll a concentrations in surface water were highest (mean value of 13 ± 5.4 mgÁL -1 ) in the fall and winter as water levels rose and lowest (3.5 ± 0.90 mgÁL -1 ) in the spring and summer as water levels declined. The peak in chlorophyll concentrations during fall of both years occurred at low water while the reservoir was thermally stratified (Alpers et al 2008) and was generally sustained as the reservoir filled. The development of the bloom prior to destratification was not expected, since algal blooms typically occur when nutrients are mixed from the deep portions of the reservoir into surface waters following destratification, particularly in oligotrophic systems such as CFWR (N:P ratios of 136 to 5191; Kuwabara et al 2003).…”
Section: Resultsmentioning
confidence: 99%
“…Total mercury concentrations in sediments from abandoned mine sites are as high as 45 000 mgÁg -1 (Alpers et al 2005b), whereas total mercury in sediments from CFWR range from about 0.3 to 1.0 mgÁg -1 dry weight (M. Marvin-DiPasquale, unpublished data). Mercury-contaminated sediment continues to be transported in the Bear River watershed and other Sierra Nevada watersheds affected by historical mining, especially during high-flow events (Alpers et al 2008). Three sites in CFWR located along a downstream gradient from the inflow at the Bear River arm to the outflow at the dam were sampled quarterly for 2 years (Fig.…”
Section: Site Descriptionmentioning
confidence: 99%
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“…The primary source of mercury to Camp Far West Reservoir is suspected to be transport of contaminated sediments from upstream reaches of the Bear River, especially during high-flow events (Kuwabara et al 2003;Alpers et al 2008). Historically, hundreds of gold mining operations occurred in the Bear River watershed upstream from the reservoir, each contributing to mercury loss during the gold-recovery process.…”
Section: Study Area and Methodsmentioning
confidence: 99%
“…Specific objectives were as follows: (1) determine if mercury concentrations varied spatially and temporally in selected fish species and (2) determine if mercury concentrations exceeded toxic threshold levels or related criteria for piscivorous fish and wildlife, and human consumers. The results were also intended to contribute towards a multidisciplinary federal investigation of mercury uptake and cycling within the reservoir, and help to identify mercury "hot spots" in the Bear-Yuba river watersheds for possible future remedial action (e.g., Kuwabara et al 2003;Alpers et al 2008;Stewart et al 2008).…”
Section: Introductionmentioning
confidence: 99%