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GENERAL47887
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Last modified
8/24/2016 8:23:22 PM
Creation date
11/23/2007 3:53:40 PM
Metadata
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Template:
DRMS Permit Index
Permit No
M1977378
IBM Index Class Name
General Documents
Doc Date
8/20/2003
Doc Name
Consent Decree Fourth Amendment
From
Sunnyside Gold Corp
To
DMG
Media Type
D
Archive
No
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APPENDIX A <br />Reference Water Quality <br />A-1 Definition of "Reference Water Quality" and "Project Period" <br />°`Reference water quality" is defined as the dissolved zinc (Zn) concentration and flow at <br />reference point A-72, the US Geological Survey's stream flow gage no. 09359020, Animas River <br />below Silverton, for the time period of September 5, 1991 to May 22, 1996. Measurements that <br />were taken on the same day or on consecutive da}~s were averaged to reduce the relative <br />importance of those measurements when using the data in statistical analysis. This set of 17 <br />flow/zinc pairs is termed the "baseline set". Tlris set of data defined reference water quality <br />against which later water quality will be compared. Both the raw data and the baseline data set <br />are presented below in Table A-] . <br />"Project period" is defined as the time period that begins with the closure of the valve at the <br />American Tunnel internal portal plug and the diversion of Cement Creelc into the American <br />Tum~el water treatment plant. The project period ends when there is final closure of the number <br />two bulkhead in the American Tunnel. <br />"Post project condition" is defined as the condition of water quality that is expected after the A- <br />list Projects have been completed; mine pool equilibrium has been reached; American Tunnel, <br />Terry Tunnel, the Mogul Mine and the Koehler mine have been plugged; and diversion and <br />treahnent of Cement Creek have ceased. <br />A-2 Relationship between flow and dissolved Zinc in the baseline set. <br />The high-mountain headwaters portion of a river such as the Animas is subject to seasonal <br />fluctuations in flow due to hydrologic response of the basin to climatic factors. In this basin, <br />stream flow and concentrations of dissolved metals are inversely related. At low flows <br />concentrations of metals are high, and at high flows concentrations are low, exhibiting a dilution <br />effect from snowmelt. Figure A-1 presents the baseline Zinc concentrations and streamflow at <br />A-72. <br />When compazing varying concentrations of dissolved metals in surface waters, standazd practice <br />is to adjust for the variation due to streamflow. This is an analytical technique used when <br />pollutant concentrations vary as a function of streamflow, as shown in Figure A-1. If the data set <br />consists of sanrples taken at a variety of streamflows, some or all of the concentration differences <br />could be due to differences in streamflow and not to changes in upstream inputs. By computing <br />a regression equation between concentration and streamflow, the effect of streamflow can be <br />"subtracted out." <br />Appendix A <br />232565 <br />
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