Laserfiche WebLink
Permit C-81-071 1996 Annual Hydrology Report <br />of 1995 were sustained throughout 1996. Lastly, TDS values beyond the previously <br />' established maximum were recorded in November, March, and August (Table 12). All values <br />for well 006-AW-2 during 1996 occurred within previously established ranges (Table 13). <br />SPOILS <br />Five wells (001-SP-6, 001-SP-7, 026-SP-1, 026-SP-2, and 026-SP-3) are monitored in the <br />spoils on a quarterly basis for water levels and field parameters. They are located at Mine 1 <br />and Eckman Park and were installed in 1985 and 1986. Three of these wells (026-SP-1, 026- <br />SP-2, and 026-SP-3) require semi-annual water quality sampling as well. Sampling <br />requirements were completed at these wells during 1996 with the exception that the second <br />required water quality samples were not obtained until November, 1996. ~-~-a r,.,b/,~,... <br />The plots of the historic water levels in the spoil wells are presented on Figures 24, 26, 28, 30, <br />and 31. The water levels normally have a similar pattern to the alluvial wells: they respond <br />rapidly to the spring runoff and then decline rapidly in the summer. Wells 026-SP-1 and 026- <br />SP-3 have on occasion been dry by the fall, although this has not happened since 1988. Water <br />levels in these wells closely mirror the pattern of the spoil spring discharges discussed <br />elsewhere in the report. Wells 001-SP-6 and 001-SP-7 reflect fluctuation in the spoil aquifer <br />water table attributable to pumping activities associated with the adjacent Foidel Creek Mine. <br />Water quality data for wells 026-SP-1, 2, and 3 are summarized in Tables 14, 15, and 16 for the <br />1996 water year. Tables 14a through 16a provide period of record statistical summaries of <br />collected water quality data at each site. Figures 25, 27, and 29 provide graphical <br />representations of TDS concentrations recorded at each site. TDS values in wells 026-SP-1 <br />• and 2 were observed to be elevated in the spring during the period of significant recharge to the <br />spoils aquifer. TDS levels were then observed to drop off later in the year. The opposite <br />pattern was evident at well 026-SP-3 with TDS levels observed to increase during the latter part <br />of the year and decrease during the spring runoff period. <br />Monitored water quality parameters at these wells during 1996 returned values within previously <br />established ranges with the following exceptions. Anew maximum field conductivity was <br />recorded in April at well 026-SP-1 along with new maximum TDS, SAR, and nitrate as N values. <br />Well 026-SP-2 returned a new maximum value for pH in November of 1995. Subsequent <br />measurements returned to typical levels. New maximum values for field and lab conductivity, <br />TDS, and nitrate as N were recorded in April. Anew maximum value for dissolved selenium <br />comprises the only atypical value returned for well 026-SP-3 during 1996. This value was <br />reported for April and is only 1 ug/I higher than the previous maximum. <br />In general, the spoil groundwater has comparable dissolved solids concentrations to most of the <br />spoil spring discharge, but much higher values than in the background bedrock ground water. <br />Much of spoil ground water is acalcium-sulfate type with relatively high bicarbonate and low <br />SAR. Spring 114, located just downgradient from wells 001-SP-6 and 001-SP-7, typically <br />exhibits higher sodium and sulfate levels than other spoil springs. The water quality data for <br />spoil wells does not indicate any significant changes in trace metals concentrations have <br />occurred over time. <br />SURFACE WATER MONITORING <br />• Foidel Creek: Four surface flow monitoring sites on Foidel Creek in the vicinity of the CYCC <br />mined areas and facilities areas are utilized. Site 14 provides data from the undisturbed <br />I\DOCUMENTWHR\ECKMAN1EP96TE%T.DOC 03/26/97 Page 5 <br />