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_19_ <br />The quantity of surface water will be impacted through evaporation of water in <br />the pit, in sediment ponds and through diminished spring flows during mining. <br />Following mining and reclamation, the surface water flow rate (quantity) will <br />approach pre-mining conditions. The impacts to surface water quantity will be <br />minor given the small drainage area involved, the minor spring flow <br />contribution, and the requirement to discharge waters from the ponds. <br />Ground water quantity will be impacted during mining through the mining of the <br />recharge areas of aquifers and through depletions of ground water storage <br />(lowering of existing ground water levels) in aquifers by mine induced pit <br />inflows. Water which would ordinarily recharge the strata upgradient of the <br />mine pit will be diverted into the pit during mining. The recharge area <br />within the permit area is minor in comparision with respect to the entire <br />recharge area of these aquifers up and down gradient of the mine. Ground <br />water currently stored within the aquifers will be depleted by ground water <br />flows from the aquifers into the pit (pit inflows) as the mining operation <br />moves down the dip of the coals. The applicant predicts a maximum inflow rate <br />of 200 gallons per minute which will lower water levels in the aquifers. <br />Following mining the pumpage of pit waters will cease and a spoil aquifer will <br />be established. This spoil aquifer will recharge the bedrock aquifers and <br />ground water levels within the aquifers will approach pre-mining levels. <br />The depletion of recharge will impact the quantity of discharges from springs <br />and seeps down gradient of the mine, during and for a short period after <br />mining. During mining, some of the ground water which is tributary to the <br />springs and seeps will enter the pit, depleting spring and seep flows. <br />Presently, springs and seeps from the aquifers in the permit and adjacent <br />areas are primarily discharging to the stream in Carbon Junction Canyon. <br />Thus, there will be a depletion of stream flows. However, pit inflow waters <br />will be discharged to the surface stream, and the overall impact to the <br />quantity of surface water during mining will be minimal. Following mining, <br />ground water levels will return to pre-mining levels. This will result in the <br />reestablishment of spring and seep flows consistent with pre-mine rates. <br />The mining and processing of coal at the Carbon Junction Mine will impact the <br />quality of both surface and ground waters during and after mining. Mining <br />will disrupt the natural soils and rock strata in the disturbed areas of the <br />mine operation. Disruption of soils and rock strata will increase the <br />exposure of previously unexposed materials to both surface and ground waters. <br />This exposure will result in increased leaching and weathering of these <br />materials, with a corresponding increase in suspended solid and dissolved <br />solid loads in surface waters and increased dissolved solid loads in ground <br />waters. <br />Suspended sediment levels will be minimized during mining by routing disturbed <br />drainages through sediment ponds. Sediment ponds will remain in place until <br />reclamation of the spoils and fill have been completed. <br />