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• 2.05.6 <br />occurred February 17, 1978, is for the period of record from 1934 through <br />1995 and is measured upstream of the Town of Somerset, CO. <br />As explained in Section 2.04.7, the Bowie No. 2 Mine is experiencing an <br />inflow of approximately 30 g.p.m. Discharge records for the fourth quarter <br />of 2002 indicate the mine water has a TDS of approximately 1500 mg/I <br />(Reference BRL's discharge monitoring reports for Pond C). For the <br />purposes of this PHC a worst case mine inflow/discharge of 175 g.p.m. is <br />utilized. This is significantly more discharge than is expected from the <br />combined flows from the B-Seam and D-Seam. <br />The average TDS measurement at the upstream North Fork of the Gunnison <br />River monitoring station for the baseline period (2002 AHR) is 130 mg/I. The <br />average iron measurementatthe upstream North Fork of the Gunnison River <br />monitoring station for the baseline period (2002 AHR) is 0.10 mg/I. The <br />maximum iron in the mine discharge is 0.35 mg/I based on an 3/21/03 lab <br />• report for the preparation of DMRs. The following tables present the <br />estimated affect the mine discharge will have on the quality of water in the <br />North Fork of the Gunnison River: <br />PHC North Fork of the Gunnsion River <br /> Flow m Flow cfs~ TDS m I Iron Trec, m /I <br />North Fork 11,220 25 130 0.10 <br />Mine Dischar e 175 0.39 1500 0.35 <br />Combined Flow 11,395 25.39 151 ~ 0.104 <br />Based upon the above calculations, the mine discharge into the North Fork <br />of the Gunnison River will not have a measurable impact on the TDS or total <br />recoverable iron in the river. <br />The pH of the North Fork of the Gunnison River varies from 7.5 to 8.8 <br />according to the 2002 AHR. The pH of the mine discharge water is in the 8.0 <br />range. Therefore, the mine discharge water should not adversely affect the <br />pH in the North Fork of the Gunnison River <br />n <br />ICJ <br />PR-08 2.05 - 73 - 07/03 <br />/~iPRovE~ <br />9/zs/o3 <br />