Adit Discharge Summary for the Elkhorn and Charter Oak Mines, MT
Figure 3—The Charter Oak adit and the recorder installed about
50
feet downstream. The pond is very toxic. Water from the
pond eventually runs into the creek below.
Figure 4—Discharge peaked at the Charter Oak lower adit from
April
to June 1999. These data suggest that the recharge
area
for this adit is localized
Field parameters such as temperature, pH (acidity), and specific conductivity generally show seasonal trends (figures 5a, 5b and 5c). Water temperature, for example, follows a seasonal trend, with diurnal fluctuations. In early February 1999, the discharge stream around the temperature probe froze completely, as indicated by the negative values. Overall, water quality appears to be best just before the spring melt and poorest during higher flows. The data are shown in table 1.
Figure 5a—The greatest fluctuation in temperature (figure 5a),
pH (figure 5b), and specific conductivity (figure
5c) at the
Charter Oak Mine coincided with seasonal changes in discharge;
the higher
the discharge, the higher the pH, and the
lower
the specific conductivity.
Figure 5b—Fluctuations in pH at the Charter Oak Mine
from July
1998 to June 2000.
Figure 5c—Fluctuations in specific conductivity at the Charter
Oak Mine from July 1998 to June 2000.
In the Charter Oak adit we discovered that the ground-water recharge and discharge system is localized in nature and could easily be controlled by ground source control methods. The water quality fluctuated throughout the year. A treatment process that was based on a single measurement at this site would probably have failed.
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