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<br />(/) 4 <br />0: <br />w <br />f- <br />W 6 <br />:; <br />>= <br />m 8 <br />() <br />~ <br />I 10 <br />f- <br />e.. <br />~ 12 <br />w <br />0: <br />o 14 <br />() <br /> <br />16 <br /> <br />18 <br /> <br />o <br /> <br /> <br /> <br />o <br /> <br />2 <br /> <br />4 <br /> <br />8 <br /> <br />10 <br /> <br />12 <br /> <br />14 <br /> <br />16 <br /> <br />18 <br /> <br />20 <br />o 500 1,000 1,500 2,000 <br />TOTAL PAH, IN <br />MICROGRAMS PER KILOGRAM <br /> <br />2 <br /> <br />o <br /> <br />2 <br /> <br />4 <br /> <br />(/) <br />0: <br />w <br />f- 6 <br />w <br />:; <br />~ 8 <br />w <br />() <br />~ 10 <br />I <br />f- <br />fu 12 <br />o <br />w <br />0: 14 <br />o <br />() <br /> <br />16 <br /> <br />18 <br /> <br />20 <br />o <br /> <br />RATIO OF 4- AND 5-RINGED COMPOUNDS <br />TO 2- AND 3-RINGED COMPOUNDS <br /> <br />2 <br /> <br /> <br />20 <br />o 2 468 <br />RATIO OF PHENANTHRENE TO ANTHRACENE <br /> <br /> <br />o <br /> <br />2 <br /> <br />4 <br /> <br />6 <br /> <br />8 <br /> <br />10 <br /> <br />12 <br /> <br />14 <br /> <br />16 <br /> <br />18 <br /> <br />o <br /> <br /> <br />2 <br /> <br />4 <br /> <br />6 <br /> <br />8 <br /> <br />10 <br /> <br />12 <br /> <br />14 <br /> <br />16 <br /> <br />18 <br /> <br />3 <br /> <br />20 <br />o 0,5 1.0 1.5 <br />RATIO OF FLUORANTHENE TO PYRENE <br /> <br />20 <br />o 200 400 600 <br />TOTAL COMBUSTION PAH, <br />IN MICROGRAMS PER KILOGRAM <br /> <br />Figure 3. Five polycyclic aromatic hydrocarbon components plotted against depth in core DLN. (The <br />ratio of 4- and 5-ringed compounds is commonly reported as 2- and 3-ringed compounds to 4- and <br />5-ringed compounds. The ratio was reversed in this figure in order to show all three ratios that relate <br />combustion- and noncombustion-derived compounds to be comparable.) <br /> <br />have decreased over time (table 4). The decrease in <br />trace-element concentrations over time may be due in <br />part to the decrease in active mining in the drainage <br />area and efforts to reclaim old mine sites. <br />Elements shown to increase over time were <br />cadmium and mercury. Cadmium can be associated <br />with mining but is typically found in zinc-ore minerals <br />(Hem, 1992). Zinc concentrations in the sediment <br />core did not show a trend, which indicates that <br />there may be a source of cadmium that is not mining <br />related. Cadmium is used in paint, plastics, ink, and <br />batteries. It also can enter the environment through the <br /> <br />combustion of fossil fuels (Hem, 1992). The increase <br />of cadmium concentrations in reservoir sediment may <br />be associated with the population increase and urban <br />development in the Dillon Reservoir watershed. <br />Mercury is a trace element commonly associ- <br />ated with coal-fired powerplant emissions and <br />waste incinerators. It can be regionally transported <br />and enter a watershed through atmospheric deposition <br />(U.S. Environmental Protection Agency, 1997). Low <br />concentrations of mercury were identified in snow- <br />pack samples collected in the region during 1999 <br />(Don Campbell, U.S. Geological Survey, written <br /> <br />12 Identification of Water-Quality Trends Using Sediment Cores from Dillon Reservoir, Summit County, Colorado <br />