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REP31413
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Last modified
8/25/2016 12:07:26 AM
Creation date
11/27/2007 5:55:13 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1982056
IBM Index Class Name
Report
Doc Date
2/7/1991
Doc Name
1990 ANNUAL HYDROLOGIC REPORT 1990 WATER YEAR PART 1
Annual Report Year
1990
Permit Index Doc Type
HYDROLOGY REPORT
Media Type
D
Archive
No
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increase and decline due to spring runoff. In addition they show the general decline in water <br />levels due to the relatively low runoff since 1987. <br />While the seasonal variation in water levels in the Foidel Creek alluvium is readily apparent, no <br />impact from the underground mining is evident. The average water levels in the three wells, <br />adjusted for differences in spring runoff, has not changed since monitoring began in 1979. The <br />Fish Creek alluvium water level data for the wells upstream of the tipple is presented for <br />baseline purposes only. The water level data for the Fish Creek alluvium wells do not show any <br />impact from the activities at the tipple or the Fish Creek Borehole. <br />Water Quality - The water quality data is summarized in Tables 14 to 19 for the Foidel Creek <br />wells and Tables 20 to 29 for the Fish Creek wells. The historic electrical conductivity <br />concentrations for the Foidel Creek wells are plotted on Figure 20. Seasonal variation occurs <br />in the wells, this is due to flushing effect of the relatively low dissolved solids surface water <br />which recharges the alluvial aquifers during spring runoff. There was a small increase in the <br />average salt content of the water in the 1988 and 1989 water years. This is probably due to the <br />relatively low runoff which has continued since 1987. <br />The water quality data for the Fish Creek Alluvial wells near the Fish Creek Borehole do not <br />indicate any impact from the discharge (Figure 54). The water quality in the Foidel Creek <br />alluvial wells upstream and downstream of the underground mine discharge similar. No impact <br />from the discharge is evident. The water is asodium-sulphate type. No increase in metal <br />concentrations was observed. <br />The historic field conductivity data for the alluvial wells near the tipple are presented on Figure <br />23. They show some indication of seasonal variation with higher levels in the winter and <br />decreasing levels following spring runoff. The data does not indicate any significant change in <br />water quality from previous years. <br />-5- <br />
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