Laserfiche WebLink
Water in Fish Creek could see a slight increase in sediment load as subsidence <br />creates slight changes to the stream channel gradient and minor erosion occurs at <br />the head cuts in the stream. This increase in sediment load is anticipated to be no <br />more than the sediment increase observed during spring runoff and after large <br />rainstorms. An increased sediment load was not detected during past subsidence <br />of Fish Creek, Foidel Creek, or Middle Creek. <br />No impact to groundwater quality is predicted. Ground water could flow between <br />aquifers through subsidence fractures. The Fish Creek alluvium and the <br />Twentymile Sandstone have the greatest potential for such interstitial flow, but the <br />stratigraphic separation of several hundred feet between the two units would <br />prevent any significant amount of flow between them. <br />Water quality impacts to the stream/alluvial aquifer system of Fish Creek could <br />result from two additional processes: mine water discharge through the Fish Creek <br />borehole or Fish Creek Vent Shaft during mining and contamination of tributary <br />ground water through seepage from the underground working's after mining has <br />ceased and the workings have flooded. Impacts from mine water discharge during <br />operation will be discussed first. <br />Originally, mine water discharge was projected to have an electrical conductivity <br />of 1 mmhos/cm at a projected discharge rate of 0.41 cfs. Actual data from <br />numerous years of operation reveal mine water discharge values of approximately <br />0.20 cfs but an electrical conductivity of nearly 3 mmhos/cm. Discharge and <br />conductivity in this range would cause a measurable increase in salinity <br />downstream on Fish Creek. Stream flow modeling conducted during the CHIA <br />produced EC values in the area of .750 mmhos/cm, given a conservative TDS/EC <br />ratio of .8, for areas downstream of the Fish Creek dewatering borehole. Electrical <br />conductivity values at this level would not materially damage crop production <br />from either flood irrigation or sub-irrigation. <br />As was the case on Trout Creek, the majority of the plant species identified in <br />surveys conducted by the applicant and summarized in the supplemental package <br />of September 22, 1986, are rated moderately tolerant to salinity. Only 3.7% of the <br />relative vegetative cover on Fish Creek was made up of moderately sensitive <br />species. No production sampling was conducted on Fish Creek, and so a ratio of <br />4.5 obtained from sampled fields at the Foidel Creek/Middle Creek confluence was <br />used to convert relative cover of 3.7% to assumed relative production of 16.6% for <br />moderately sensitive species. <br />Cover and productivity data were collected in 1997 in and adjacent to the Fish <br />Creek AVF. AVF species are dominated by Smooth bromegrass, Kentucky <br />bluegrass, Common yarrow, sage, Artemesia cana, and Timothy. <br />Projected Fish Creek water quality for flood irrigation is conservatively estimated <br />at 0.9 mmhos/cm electrical conductivity. Projected root zone soil salinity would <br />be less than 1.5 mmhos/cm and therefore no decrease in crop production would <br />Foidel Creek Mine 41 June 4, 2010