Laserfiche WebLink
relative iy low TDS value. This is rvhat one we u1C expect in an undisturbed drains ce in <br /> this area <br />Two <br />m <br />r <br />a <br />t an <br />l <br />d f <br />d COOK' <br />i <br />i <br />t T <br />bl <br />d <br />d <br />( <br /> , <br />p <br />ra <br />e <br />e <br />s a <br />yze <br />v <br />or excee <br />rece <br />ng s <br />ream stan <br />ar <br />s <br />see <br />a <br />e <br /> 21) even though no mining has occurred in this basin. P, high total copper concentration <br /> of 100 ug/1 exceeds the standard of 2Z ug/1, and a high total iro n value of 2.2C mg/1 <br /> exceeds the standard of 1.0 mg/1. This should be taken into consideration before <br /> evaluating future impacts on Bond Creek, and the existing impacts of Cow Camp Creek, <br />8. Little Grassy Creek Drainage <br />Three monitoring sites lie within the Little Grassy Creek drainage: surface water site <br />SW-S2-5 located in the southwest portion of the permit area, NPDES Discharge Point 002, <br />also known as the Wadge Impoundment, and NPDES Discharge Point 003, also known as the Shop <br />Reservoir or the Northwest Impoundment, located just north of the mine shop and facilities <br />area. <br />1. Surface Water Site SW-52-b <br /> Surface water site SW-S2-5 drains the upper reaches of Little Grassy Creek which is <br /> essentially undisturbed by mining, P.eview of the hydrograph of monthly flan readings <br /> shows less runoff in 1986 than in 1985. <br />i <br />f <br />9 The CSG data shays a peak flow of 5.8 cfs in the <br /> spr <br />ng o <br />1 <br />86, compared to a flow of 13 cfs in the spring of 1985. <br />Review of Table 16 shows water at this site Lo be a calcium/magnesium sulfate type water <br />I ~~ <br />with a relatively stable TDS (since 1981) that may vary in high water years. <br />2. NPDES 002 <br />Flow data presented in Table 22 and hydrographs (1981 to 1986 and 1986 alone) presented in <br />Appendix D, show a smaller peak runoff in 1986 than in 1985 for similar reasons as <br />discussed earlier at NPDES 004. Peak mean daily flow was 4.8 cfs on March 9, 1986, while <br />it was 10.5 cfs on April 9, 1985. Total discharge was 447 ac-ft in 1986, while it was 773 <br />ac-ft in 1985. <br />Review of Table 17 shows water at this site remaining a magnesium sulfate type water. <br />Flows display a relatively stable TDS (since 1981) that varies from high to low water <br />years. No excursions of NPDES effluent limits were observed here in 1966. <br />'s. NPDES 003 <br />Hydrographs presented in Appendix D show that flow has increased at this site since <br />46 <br />