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residual discharge of shallow ground water from the irrigated fields above the site <br /> contributes some flow up through even January. During the irrigation period, measured <br /> flow ranged from .088 cfs (October) to 2.18 cfs (August). During periods of no <br /> irrigation, flow observations made at SW-N2 ranged from zero (February, March and early <br /> April) up to .031 cfs (January). <br /> SW-N107 is located about a mile and a half below SW-N101 on Calamity Draw (see Exhibit <br /> 7-1). Flow measurements have only periodically been collected at this site since July of <br /> 1986. A crest-stage gage has been installed at this site for the purpose of recording <br /> high water marks of large runoff events (rainfall or spring snowmelt runoff). These high <br /> water marks are used to determine the peak discharge of large runoff events using indirect <br /> discharge measurement techniques (see Tab 15, Hydrologic Monitoring Program). Since <br /> monitoring began (July, 1986), only four events have been calculated using indirect <br /> techniques: 1 ) 39 cfs, 11/11/86; 2) 35 cfs, 5/20/87; 3) 34 cfs, 6/22/87; and 4) 96 cfs, <br /> 8/27/87. The listed dates represent the respective visit dates that high water marks were <br /> measured at the crest gage. All events likely resulted from unusually intense summer <br /> thunderstorms, although no information of those particular storms was collected. <br /> Finally, Site SW-N103 is located downstream of SW-N107 on Calamity Draw (see Exhibit 7-1). <br /> Discharge has been measured at this site on a monthly basis since July of 1986 (see <br /> Appendix 7-5). As at the other sites established along Calamity, flow at SW-N103 is <br /> artifically controlled by irrigation, and to a lesser extent, by contributions from <br /> rainfall and snowmelt runoff, and even shallow ground water discharge. As shown in Table <br /> 7-42, measured discharge ranges from 3.36 cfs to 24.4 cfs during the irrigation season. <br /> For periods of no irrigation, flow measurements vary from 1.7 cfs up to 5.7 cfs. The <br /> highest discharge measured during the irrigation period was 24.4 cfs in July, and the <br /> lowest occurred in October (3.36 cfs). <br /> Streams - Water Quality. The following sections present discussions of water quality data <br /> collected at surface water monitoring sites established at both the Nucla Mine and Nucla <br /> East mining area. As in the previous section, discussions are grouped according to the <br /> drainage in which the sites have been located. All historic data (prior to January, 1988) <br /> for each site have been compiled and are presented as water quality reports in Appendix <br /> 7-7 and Appendix 7-9. Appendix 7-8 contains trilinear plots (Piper diagrams) of the <br /> distribution of major ions from all samples collected at each surface water site for both <br /> the irrigation and non-irrigation periods. The reader should refer to Exhibit 7-1 for <br /> locating surface water monitoring sites mentioned in the following sections. <br /> 7-122 Revised 04/11/88 <br />