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Last modified
8/11/2009 11:32:57 AM
Creation date
8/10/2009 4:56:06 PM
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UCREFRP
UCREFRP Catalog Number
9343
Author
Greve, A. I., N. E. Spahr, P. C. Van Metre and J. T. Wilson.
Title
Identification of Water-Quality Trends Using Sediment Cores from Dillon Reservoir, Summit County, Colorado.
USFW Year
2001.
USFW - Doc Type
Denver.
Copyright Material
NO
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<br />incoming total load left in the reservoir. Copper, <br />iron, manganese, molybdenum, and zinc were <br />analyzed for total (unfiltered) concentration, which <br />allowed the percentage of the overall load occurring <br />in the dissolved phase to be determined (table 6). <br />In the case of copper, iron, and zinc, the entering <br />load had a smaller dissolved percentage than the <br />exiting load. It is likely much of the incoming copper <br />and iron was in the suspended phase and was depos- <br />ited on the reservoir bottom by settling. Manganese <br />showed a decrease and zinc did not show a large <br />increase in dissolved-percentage exiting the reservoir, <br />implying that geochemical processes in addition to <br />sedimentation are acting to contribute loads to Dillon <br />Reservoir. <br />From the load calculations, the stream contrib- <br />uting the largest amount of a given element was <br />identified. Tenmile Creek, which accounts for about <br /> <br />37 percent of the total water inflow, delivered the <br />largest loads of aluminum, barium, and, as one would <br />expect, molybdenum. The Blue River contributed no <br />more than one-third of any trace-element load entering <br />the reservoir, less than the portion of the flow contrib- <br />uted (35 percent of inflow) to the reservoir. The Snake <br />River, generating 28 percent of the total inflow, <br />contributed most of the copper, manganese, and <br />zinc loads. <br />Those streams delivering the largest loads <br />of trace elements to the reservoir also had higher <br />streambed-sediment concentrations, with the excep- <br />tion of barium. The barium load delivered by the <br />Snake River was smaller than the barium loads carried <br />by the Blue River and Tenmile Creek; however, the <br />streambed-sediment concentration of barium was <br />highest in the Snake River. <br /> <br />Table 4. Results of Kendall's tau calculations relating trace-element concentrations to core depth in core DNL, collected <br />August 1997 <br /> <br />[Ilg/g. micrograms per gram; %. percentage; n. not applicable; value is based on the large sample size approximation described in Helsel and Hirsch (1993)] <br /> <br />Element Units Tau p-value Trend <br />Aluminum % 0.099 0.576 No <br />Arsenic Ilg/g 0.111 0.529 No <br />Barium Ilg/g -0.006 1.000 No <br />Cadmium Ilg/ g -0.637 0.000 Yes <br />Calcium % -0.158 0.363 No <br />Chromium Ilg/g 0.333 0.050 No <br />Cobalt Ilg/g 0.287 0.093 No <br />Copper Ilg/g 0.509 0.003 Yes <br />Iron % 0.345 0.042 Yes <br />Lead Ilg/g -0.053 0.780 No <br />Lithium Ilg/g 0.439 0.010 Yes <br />Magnesium % -0.018 0.944 No <br />Manganese Ilg/g 0.228 0.184 No <br />Mercury Ilg/ g -0.380 0.025 Yes <br />Nickel Ilg/g 0.544 0.001 Yes <br />Potassium % 0.170 0.327 No <br />Scandium Ilg/g 0.357 0.036 Yes <br />Silicon % 0.135 0.442 No <br />Sodium % 0.123 0.484 No <br />Strontium Ilg/g 0.006 1.000 No <br />Titanium % 0.673 0.000 Yes <br />Vanadium Ilg/ g 0.626 0.000 Yes <br />Zinc Ilg/g 0.298 0.080 No <br /> <br />Direction <br /> <br />Upward over time <br /> <br />Downward over time <br />Downward over time <br /> <br />Downward over time <br /> <br />Upward over time <br />Downward over time <br /> <br />Downward over time <br /> <br />Downward over time <br />Downward over time <br /> <br />IDENTIFICATION OF WATER-QUALITY TRENDS 15 <br />
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