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both during periods of irrigation and no irrigation. The mean TDS levels measured at <br /> GW-N4 during periods of irrigation and no irrigation are 6,684 and 6,836 mg/l , <br /> respectively. Schoeller diagrams, representing mean milliequivalent values for the two <br /> above-referenced time periods, are presented on Figure 7-3. Ions accounting for the slight <br /> TDS increase during periods of no irrigation are calcium, bicarbonate and chloride. <br /> A range in pH values from 6.7 to 7.3 have been measured at Wells GW-N4 and N4R. The mean <br /> pH for Well GW-N4 is 6.83. <br /> There is a limited amount of seasonal variability in the water chemistry of Wells GW-N4 <br /> and N4R. In comparing spring chemistry versus fall chemistry, alkalinity, bicarbonate pH <br /> and TDS tend to decrease and chloride and calcium tend to increase in the fall . <br /> A summary of the ranges in concentration for trace elements sampled at Wells GW-N4 and N4R <br /> is presented in Table 7-8. Well GW-N4 water exceeds the CWQCC agricultural standard for <br /> manganese and Well GW-N4R water exceeds the cadmium and manganese standards. Both wells <br /> yield water that exceeds the livestock drinking water limits for magnesium and TDS (Table <br /> 7-9). Measurable trace metal concentrations at the two sites include boron, fluoride, <br /> iron, manganese, cadmium, copper, nitrate and zinc. <br /> Four wells (GW-N1, GW-N3, GW-N5 and GW-N6) are used to monitor the underburden ground <br /> water quality at the Nucla mining area. Statistical summaries of the water analyses <br /> performed on water sampled from these wells are presented in Tables 7-12 through 7-15. <br /> Trilinear diagrams representing analyses performed during periods of irrigation and no <br /> irrigation are presented in Appendix 7-3. The individual water quality analyses for the <br /> underburden aquifer wells are presented in Appendix 7-4. The well locations are shown on <br /> Exhibit 7-1. <br /> The four underburden monitoring wells exhibit three water types during periods of <br /> irrigation. Wells GW-N1 and GW-N3 have a calcium magnesium sulfate type water, well GW-N5 <br /> has a magnesium sodium sulfate type water, and Well GW-N6 has a magnesium calcium sulfate <br /> water type. During periods of no irrigation, only well GW-N5 changes in water type to a <br /> magnesium sodium calcium sulfate water type. <br /> Only small changes in TDS occur when comparing samples obtained during irrigation versus <br /> non-irrigation periods. Wells GW-N1 and GW-N6 increase in TDS while Wells GW-N3 and GW-N5 <br /> 7-39 Revised 04/11/88 <br />