Laserfiche WebLink
the conductivity of 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 average conductivity <br />of the water discharged from the mine and gob pile. Therefore, the conductivity of the <br />alluvial groundwater can only be improved by the combined discharge. <br />14000 <br />12000 <br />10000 <br />E <br />v <br />s 8000 <br />E <br />6000 <br />3 <br />L <br />C <br />O <br />U <br />4000 <br />2000 <br />0 <br />Monitoring Well GW -3 <br />N M V M (O r- CO O O N M V M (O � M O O N M V M (O r M M O <br />00 00 00 00 00 00 CO CO CO O O O O O O O O O O O O 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 C C C C C <br />7 7 7 7 7 7 7 7 7 7 7 7 7 7 7 7 7 3 3 3 3 3 3 3 3 3 3 7 7 7 <br />M M M M M M M M M M M M M M M M M 7 7 7 7 7 7 7 7 7 7 M M M <br />Date <br />—+—GW -3 Conductivity --W—GW-3 Baseline Combined Water Average <br />Appendix N — PR -02 - 5 - 10/10 <br />