Laserfiche WebLink
<br /> <br />SPOIL_SPRING MONITORING <br />' A spoil spring monitoring program was initiated in 1986 and will be <br />conducted annually until such time as the monitoring requirement is <br />' eliminated. As per the approved plan the annual mine wide survey is <br /> conducted during May, and springs will be measured for flow and field <br />' parameters. If a spring <br />th <br />it <br />ill b <br />it <br />d is discharging <br />th <br />h <br />t th 35 gallons per minute <br />i <br />d <br />f th <br />i or greater <br />d <br /> e mon <br />ore <br />en <br />w roug <br />ou <br />e rema <br />n <br />er o <br />e year <br />n accor <br />ance <br /> with the monitoring plan. <br />1 <br /> Flows <br />' The field data for the May 1989 spoll 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 as 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 />Water Quality <br />' The summary of the May 1989 spoil spring field data is presented on Table <br />49. The summary of the water quality data for Station 114 is presented on <br />fables 54 arrcl 55. Additional spoil spring data for Mine 1 is presented on <br />' Tables 50 arrd 51 for Mine 1 and Tahles 52 and 53 for Mine 2. Plots of the <br />Iristorfc water quality data for Station 114 are presented on Figures 43 and <br />44. 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 />apprnxirmtely 3400 nmhos/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 sluing and underground mine discharges, the <br />(:reek's dissolved solids level approaches drat 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. I <br /> <br />' - 8 - <br />