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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 Jwly of 1986 (see <br />Appendix 7-S). 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 14.4 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 />