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have been observed. Arsenic, cadmium, chromium, copper and lead concentrations have <br />been low with a few exceptions. Moybdenum, nickel and selenium concentrations have <br />stayed low, except for a slightly higher selenium value in well P-3. The recent radium 226 <br />values have been tow. The laboratory mistakeny missed the anaysis for phosphate and <br />phosphorus for a group of well samples. <br />3.6 SPRING AND SEEP WATER QUALITY <br />Table B-2 in Appendix B presents the water-quality data for the springs and seeps at <br />the Trapper Mine. The locations of the springs and seeps that were flowing in 2003 are <br />shown on Maps 2-1, 2-2 and 2-3. Row from the springs and seeps are shown on Table B- <br />2, which shows that East Pyeatt and Johnson springs exceeded 5 gpm in their discharge <br />rate in 2003. Water quality from the springs and seeps are similar to the ground-water <br />quality for the site. The TDS values from Johnson Gulch spring are much higher than the <br />remainder of the springs' water quality. Johnson springs' TDS is similar to that observed <br />from badffill well GF7. A substantial decline in TDS in the bacldill aquifer at well GF7 will <br />likey be necessary for the TDS concentrations in the Johnson Gulch spring to decline, An <br />increase in TDS concentrations was observed in the East Pyeatt Spring in 2000 with a fairly <br />similar value in 2003. The TDS for Fox Den Spring and Coyote for 2003 were similar to <br />values measured in 2002. <br /> <br />3-12 <br />