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Peabody Sage Creek Mining, LLC <br />Page 7 <br />12/14/2015 <br />• Water levels were not reported for well SW19 for <br />this water monitoring year. <br />-Water Quality: <br />• Temperature was not reported for Well COV 1 I <br />from the September, 2014 sampling event. <br />• Temperature was not reported for Well CW23 <br />from the September, 2014 sampling event. <br />Please provide the missing data or explain why the <br />required water level or water quality parameter was <br />not measured or reported. <br />17. Parameters to be <br />Volume 1, p. 2.04-105 <br />All required parameters were analyzed with the <br />analyzed in ground <br />of CDRMS mining <br />exceptions noted in Item No. 16 above. <br />water samples <br />permit C-2009-087 <br />18. Basic Standards for <br />CWQCC regulations <br />Seven groundwater wells exceeded the pH standard (8.5) <br />Ground Water <br />41.4 and 41.5 <br />in 2014. The baseline water quality for pH associated <br />with the seven groundwater wells exceeded the 8.5 <br />standard. Seven groundwater wells exceeded the <br />manganese standard (0.2 mg/1) in 2014. As mentioned in <br />the above item number 8 above, in soils with a high pH a <br />standard of 10 mg/1 would be more appropriate than the <br />0.2 mg/1. In 2014 no PSCM wells displayed a value <br />higher than 8.0 mg/1. Three wells exceeded the fluoride <br />standard (2.0 mg/1). The iron standard was exceeded at <br />alluvial well 71. The baseline conditions for all of the <br />above mentioned wells exceeded the basic standards for <br />groundwater prior to the issuance of C-2009-087. <br />19. Restoration of <br />CDRMS regulation <br />For the 2014 water year, water levels at all wells fell <br />ground recharge to <br />4.05.12(3) <br />within their historic ranges with no exceptions. All <br />approximate pre -mining <br />alluvial wells displayed seasonal water level fluctuations <br />rate <br />in response to periods of precipitation recharge. <br />Overburden and coal well water are fluctuating in <br />response to the precipitation recharge, induced ground <br />water flow to the reclaimed mine pits, and in some cases, <br />changes in reservoir water levels. <br />