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<br />.~ <br />r <br />above mentioned pump malfunction. <br />GENERAL COMMENTS <br />1) Although the water Level charts provided for each well and <br />mine discharge point are useful, the data for• each event are <br />needed in order to determine if water Ievel,s were measured <br />according to the schedule outlined in the monitoring plan and <br />to facilitate calculations of water level fluctuations. We <br />should request that the operator provide water Level data in <br />future submittals of AHR reports as well as ps-ovide the water <br />level data for all previous years of the permit. <br />2) Some of the water level charts include data points that are <br />off the scale of the chart. We may wish to request that the <br />operator include all data points on the water Level charts. <br />3) The wells used to monitor the Trout Creek Sandstone are <br />apparently both pumping wells. The practice of monitoring <br />water Levels in pumping wells is questionab.e, because the <br />water level around the outside of the pumping well is more <br />representative of the cone of depression around the well and <br />may bias an interpretation of the potentiometric surface and <br />ground water flow direction. In addition, 'the water level <br />measured in the well will be much lower than the head in the <br />surrounding aquifer, even in the cone of depression, as a <br />result of frictional losses. Therefore, we need to clarify <br />with the operator whether the pumps were turned off and water <br />levels allowed to equilibrate before water level measurements <br />were taken. If not, the water level data from these wells are <br />of questionable validity in the interpretation of the flow <br />regime and dewatering trends in the aquifer.. However, for <br />practical considerations, it may not be possible to suspend <br />pumping in these two wells. <br />4) The water quality data for bedrock wells appears to be <br />incomplete. The ground water monitoring plan in the permit <br />calls for a hydroxide analysis which was pfarformed on the <br />alluvial samples but not on the bedrock aquifers. We should <br />ask the operator why the hydroxide analysis was omitted from <br />the bedrock samples. <br />5) On Figure 14, there are no data to support th.e 6250' contour <br />or the right flank of the 6150' contour. I.n addition, the <br />placement of the 6200' contour appears to be slightly out of <br />proportion with regard to the data points. On Figure 23, <br />there are no data to support the 6122' contour. Although <br />these errors probably do not change the overall flow picture <br />presented on the maps, we may wish to caution the operator to <br />base maps prepared in future AHRs strictly on the data <br />available, so that it doesn't become an issue in the future. <br />