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(Table 5) and are also the same as those used in the water quality <br /> reports. The frequency column on Table 6 indicat es the number of <br /> exceedences out of the total number of samples (i.e., 112 indicates one <br /> exceedence out of two samples). Below is a summary of standards that <br /> were exceeded. Given in parenthesis is the source and use of each <br /> standard. <br /> <br />I <br />Parameter <br />Boron (CDOH, irrigation) <br />Chromium (CDOH, irrigation) <br />pH (CDOH, irrigation) <br />Iron (CDOH, irrigation) <br />Manganese (CDOH, irrigation) <br /># of We11s / # of Excursions <br />1/2 <br />1/1 <br />1/1 <br />3/5 <br />7/14 <br />In addition, a total of six samples (from WOV14, 16, 17 and WW14) had <br />cadmium values that were less than an elevated detection limit (30 ug/1 <br />vs. a normal detection limit of 3 ug/1), which was higher than the CDOH <br />standard of 10 ug/1. Likewise, the same samples had lead values that <br />were less than an elevated detection limit (200 ug/1 vs. a normal <br />detection limit of 20 ugJl), which was higher than the CDOH standard of <br />100 ug/l. The cause of these elevated detection limits was a decision by <br />the laboratory to dilute the samples prior to analyses in order to <br />reduce the effects of interferences (primarily, high salinity). <br />Elevated levels of iron may be attributed to natural {i.e., not mining <br />related) conditions, since elevated levels for that parameter are not <br />normally found in spoil wells at the adjacent Seneca II Mine. The two <br />bedrock wells (WW14 and WTC201) that often exhibit high levels may have <br />higher than usual concentrations of iron pyrite in the rock. Well WTC201 <br />(Trout Creek Sandstone, shop well) often displays high iron values, but <br />does not display an increasing trend. Wadge coal well WW14 started <br />displaying high iron values in 1998 and displays an increasing trend. <br />The high levels of iron displayed in the one alluvial well (WHAL7-2) may <br />be the result of organic matter and plant debris present in the alluvium <br />(Hem, 1989, Pg• 77)~ A11 wells with high iron values exist within the <br />Seneca II-W permit boundary. <br />