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14000 <br />12000 <br />10000 <br />E <br />N <br />O <br />8000 <br />E <br />6000 <br />V <br />V <br />c <br />0 <br />U 4000 <br />conductivity of the combined discharge is less than the conductivity of <br />GW -3. The situation is the same at all of the groundwater monitoring <br />wells. The baseline conductivity of all of the GW wells exceeds the <br />average conductivity of the water discharged from the mine and gob pile. <br />Therefore, the conductivity of the alluvial groundwater can only be <br />improved by the combined discharge. The most recent data gathered for <br />GW -9 located immediately down gradient of the gob pile, is shown in <br />Appendix N. As concluded with GW -3, it is likely the combined water <br />discharge will only improve the conductivity of the alluvial groundwater. <br />Monitoring Well GW -3 <br />2000 - <br />0 <br />N O V O 0 h W M O N ch V O 0 r� O O O N M V � <br />a0 CO oD aD o0 N W c0 c0 O) O C) m O O1 6) m O O O O O O O O <br />C C C C C C C C C C C C C C C C C C C C C C C C C <br />7 7 7 7 7 7 7 7 7 7 7 7 7 7 7 7 7 7 7 7 7 7 7 7 7 <br />Date <br />—♦—GW-3 Conductivity f—GW-3 Baseline Combined Water Average <br />There is a field to the south and west of East Salt Creek, where the <br />landowner is attempting to raise hay. As explained earlier in this section, <br />and according to the Division's 1987 Material Damage guidelines, mine <br />discharge does not add salinity to the already high values, rather, can only <br />lower the salinity in SW -1 and GW -3 during the irrigation season. By <br />PR -02 2.06-5 10/12 <br />