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Alluvium, DCAL -02, did not exceed the TDS GWPOC standard, 3195 mg /1, but <br />did exceed the ambient -based iron standard. <br />In the Probable Hydrological Consequences (PHC, Tab 17) section of the <br />Seneca II -W Mine PAP, predictions were made as to the expected TDS <br />increases to be observed at various monitoring wells. The following <br />table outlines these predictions along with this year's observed average <br />values (annual average for bedrock wells, May - September average for <br />alluvial wells) . <br />Well Predicted TDS values (mg /1) <br />WHAL7 -2 1299 <br />WOV14 4385 <br />WOV17 4295 <br />WOV25 none <br />WW14 2630 <br />WW17 3002 <br />WW25 none <br />* indicates value above prediction <br />This year's average TDS (mg /1) <br />900 <br />3220 <br />6340* <br />1670 <br />5020* <br />650 <br />2840 <br />For Well Wadge Overburden WOV17, a value of 4295 mg /l was predicted, <br />while a value of 6340 mg /1 was observed in this year. The predicted <br />value for Well WOV17 was predicated on a 5.5% increase of the pre- mining <br />(prior to August 1990 for the central area) value of 4072 mg /1, which is <br />an average of several overburden wells. However, Well WOV17 exhibited a <br />pre- mining TDS average value of 8043 mg /1, while the next highest TDS <br />Wadge overburden well (WOV15) had a baseline TDS average of 3741 mg /1. <br />Well WOV17 also exhibited a high degree of baseline TDS variability <br />(min. = 6860, max. = 8586 mg /1). The TDS value in this year, 6340 mg /1, <br />was below the PHC prediction using the average baseline value (8043 + <br />5.5% = 8485 mg /1) , and is also below a 5.5% increase of the maximum <br />baseline TDS value (8586 + 5.5% = 9058 mg /1) . In 2008, 2009 and 2011, <br />unusually high TDS values (over 10,000 mg /1) were observed at this well. <br />These values were over the pre- mining average, 8043 mg /1, for this well. <br />The TDS value for this well in 2010, 2012, and 2013 dropped back down to <br />7 <br />