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<br /> <br />SPOIL SPRING MONITORING <br />' A monitoring program was initiated in 1986 and will be conducted annually <br />until such time as the monitoring requirement is eliminated. As per the <br />' approved plan the annual mine wide survey is conducted during May, and <br /> springs are measured for flow and field parameters. If a spring is <br /> discharging 35 gallons per minute or greater then it will be monitored <br /> throughout the remainder of the year in accordance with the monitoring plan. <br />' Flows <br />The field data for the May 1988 spoil spring monitoring program is presented <br />on Table 49. A Plot of the historic flow data for Station 114 is presented <br /> on Figure 42. No significant spoil springs were observed at Mine 2. The <br />' flow data indicates that the spoil springs follow the same pattern a s the <br /> surface runoff: very low flow during most of the year and a very rapid <br />' increase in flow during the spring runoff followed by a moderately rapid <br /> decrease in flow. <br /> <br /> Water Quality <br /> <br /> <br /> <br />1 <br />1 <br /> <br /> <br /> <br />The summary of the May 1988 spoil spring field data is presented on Table <br />49. The surmnary of the water quality data for Station 114 is presented on <br />Tables 54 and 55. Additional spoil spring data for Mine 1 is presented on <br />Tables 50 and 51 for Mine 1 and Tables 52 and 53 for Mine 2. Plots of the <br />historic water quality data for Station 114 are presented on Figures 43 and <br />43A. The data indicates that while the field conductivity level of the Mine <br />1 spoils spring flow may approach 4600 umhos/cm the average value is <br />approximately 3300 umhos/cm during spring runoff. The average value is <br />higher due to low flow periods of the year. During the winter when Foidel <br />Creek is dominated by the spoil spring and underground mine discharges, the <br />Creek's dissolved solids level approaches that of the spoil springs. The <br />dissolved solids levels of Station 114 follows the same pattern as the creek <br />because they are both influenced by the same climatologic patterns. Other <br />' - 8 - <br />