Laserfiche WebLink
this theory since the mine water which emerged from the slide in November had a <br />temperature in excess of 26 °C. The graphs presented in Appendix B show that measured <br />parameters are consistent with prior years results except for conductivity and temperature <br />discussed above. <br />AA-3 The 1996 AHR noted and increase in conductivity for well AA-3 (19461aboratory result <br />1,340 umhos/cm) and believe it to be a result of water infiltrating into well AA-3 from a <br />broken mine discharge line located upstream of the well. The 1996 report speculated that <br />future monitoring would show a steady decrease in conductivity. The field conductivity <br />was 1,120, 240 1,060 and 3,300 umhos/cm during the 1° , 2nd , 3rd and 4d' quarters <br />respectively. The lab conductivity for the 4'" quarter was 3,190. The conductivity did <br />show a decrease until the 4d' quarter which is attributed to a comment in the field notes <br />which indicate bottom mud was mixed with the water sample during bailing. <br /> <br /> <br />-3- <br />