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The selection of a procedure to determine when reclamation is adequate is <br />needed. The return of constituents in runoff water to premine levels is a <br />reasonable approach to determine when the mine area has been adequately_ <br />reclaimed. Generated sediment is likely to be the controlling constituent <br />r <br />because land stability will probably be the most difficult item in mine <br />reclamation. The present baseline data do not define the expected sediment <br />TSS or SS levels for different flood sizes. Additional baseline data are <br />being collected to define this relationship for the Trapper Mine. This <br />information should allow the determination when sediment (TSS or settleable <br />solid (SS)) values are representative of premine conditions for a particular <br />runoff event. Therefore, the return of surface runoff constituents to pre- <br />mine concentrations is proposed to govern when sediment ponds can be <br />removed. C~ '" U '~', ~(,o S . b`C~I~ <br />4.8.1.5 Operational Surface Water Quali <br />Numerous samples have been collected at the surface water monitoring sites <br />and a few analyses of the water in the settling ponds have been conducted. <br />Samples which were collected in 1977 or later are included in the operational <br />monitoring table. Table 2.7-18 gives the premine surface water quality. <br />Most of the drainages were not disturbed at the start of mining and therefore <br />some of the results presented in this section are baseline concentrations. <br />Table 4.8-8 gives concentrations for total suspended solids (TSS), total dis- <br />solved solids (TD S), conductivity, pH, total iron,~'[otal manganese and oil <br />and grease for the surface water sites. Map M3 ,~~hows the locations of the <br />surface water sites. Only a few samples in 1~9/~7~~~ere measured from sites S1, <br />S2, S3 and S4 because these are no[ in the (gcti``ve area. Numerous data are <br />given for the Johnson, No Name, Coyot~ and Buzzard Gulch sites. <br />~`\ <br />4-205 <br />