Item talk:Q72162
From geokb
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"name": "Dissolved cadmium, zinc, and lead loads from ground-water seepage into the South Fork Coeur d'Alene River system, northern Idaho, 1999",
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"abstract": "The valley of the South Fork Coeur d\u2019Alene\nRiver and some of its tributaries have been heavily\nimpacted by the dispersion of metal-enriched\nmaterials from the Coeur d\u2019Alene mining district\nsince 1884. The valley floor, including the unconsolidated\nvalley-fill/flood-plain aquifers, is a major\nholding area for mine tailings. The U.S. Geological\nSurvey, in cooperation with the U.S. Environmental\nProtection Agency, characterized groundwater\nand surface-water relations for parts of the\nSouth Fork Coeur d\u2019Alene River Basin and quantified\nthe loading of dissolved metals into the South\nFork Coeur d\u2019Alene River system from groundwater\nseepage. This information can be used to\ndetermine the effects of dissolved metal from\nground-water seepage on the river system and to\nevaluate the necessity and feasibility of remediation\nalong gaining reaches. This study defines a\nfield approach that can be repeated during and\nafter the implementation of remediation solutions\nto measure the effectiveness of these efforts in\nreducing loading to streams.\nThe study area includes three reaches along\nthe South Fork Coeur d\u2019Alene River valley in the\nCoeur d\u2019Alene mining district in central Shoshone\nCounty, northern Idaho: a 3.3-mile reach of Canyon\nCreek at Woodland Park, a 4.8-mile reach\nof the South Fork Coeur d\u2019Alene River near\nOsburn, and a 6.5-mile reach of the South Fork\nCoeur d\u2019Alene River near Kellogg and Smelterville.\nSeepage studies were conducted during July\n27\u201329; September 17\u201319; and October 15\u201317,\n1999. Each seepage study was conducted over a\n3-day period, during which each station was measured\non a daily basis for streamflow, and waterquality\nsamples were collected. The consecutiveday\napproach allowed for an evaluation of variability\nin streamflow gains and losses and metal loading\nthat resulted from changing hydrologic\nconditions.\nDuring the July, September, and October\nseepage studies, ground-water seepage was the\npredominant source for gains in dissolved cadmium\nand zinc loads in the three study reaches,\nwhereas tributary inflow loads were a minor\nsource. The overall average net gain in dissolved\nzinc load from ground-water seepage into the\nSouth Fork Coeur d\u2019Alene River near Kellogg and\nSmelterville was about 730 pounds per day, compared\nwith the net gains in Canyon Creek at Woodland\nPark and the South Fork Coeur d\u2019Alene River\nnear Osburn, which were roughly similar at 150\nand 218 pounds per day, respectively. The net gain\nin dissolved cadmium load from ground-water\nseepage into the three river reaches was about two\norders of magnitude less than the gain in dissolved\nzinc.\nOn the South Fork Coeur d\u2019Alene River study\nreaches near Osburn and near Kellogg and Smelterville,\nno pattern associated with an increase or\ndecrease in dissolved lead load along gaining or\nlosing subreaches was recognizable. Canyon Creek\nat Woodland Park was the only study reach where\nground-water seepage contributed appreciably to\nthe dissolved lead load; the average net gain was\n1.5 pounds per day.\nThe average dissolved lead loads leaving\nSouth Fork Coeur d\u2019Alene River study reaches (corrected for tributary inflow along the study\nreaches) near Osburn and near Kellogg and\nSmelterville were 1.4 and 0.8 pounds per day less,\nrespectively, than the loads entering the study\nreaches. The decrease in dissolved lead could be\nthe result of lead adsorbing onto organic and inorganic\nsediment surfaces and (or) coprecipitating\nwith iron and manganese oxides. These forms of\nlead likely will be resuspended into the water column\nat high flows.",
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"name": "Barton, Gary J. gbarton@usgs.gov",
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