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3. Site NPDES 004 and 005 <br /> NPDES discharge points 004 and 005 (Permit No. CO-0000213; see <br /> Appendix 7-6) are located within the East Return Ditch drainage <br /> along the central southwest edge of the scraper area as shown <br /> on Exhibit 1. To date, neither of these discharge points have been <br /> known to discharge. Discharge monitoring reports for the past <br /> three quarters of 1986 are provided in Appendix C. Because the <br /> present storage capacity and spillway configuration of the ponds <br /> are inadequate (see Appendix 7-1 of the Nucla Mine Permit <br /> Revision) , these ponds have been redesigned. Up until and upon <br /> reconstruction, these ponds will continue to be monitored for flow <br /> and quality according to the requirements of the NPDES permit. <br /> 4. Site SW-N3 <br /> Site SW-N3 is located on Tuttle Draw downstream of mining as <br /> shown on Exhibit 1. Flow and quality data have routinely been <br /> collected from this site since April 1980; these data are presented <br /> in Appendix B and statistically summarized in Table 7. A <br /> hydrograph constructed from monthly instantaneous flow measurements <br /> is shown in Figure 4. A trilinear plot of the major ions is <br /> depicted in Figure 2. <br /> As previously described, flow at this site is artificially <br /> controlled for most of the year from irrigation return flow <br /> from the Second Park lateral irrigation ditch. According to <br /> the hydrograph depicted in Figure 4, flow during the summer months <br /> is generally between 2.0 and 7.0 cfs, falling to a baseflow during <br /> the winter and early spring of less than 1.0 cfs. As can be seen <br /> from Figure 5, during the summer a substantial portion of the flow <br /> at this site is contributed by flow from the West Return Ditch as <br /> monitored at the NPDES 001 discharge point. <br /> Because site SW-N3 is located downgradient of mining, a <br /> resultant diminution in water quality is expected and evident. <br /> Prior to mining, water quality at this location on Tuttle Draw <br /> was probably similar to that of present day water quality at <br /> 22 <br />