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REP32189
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Last modified
8/25/2016 12:08:19 AM
Creation date
11/27/2007 6:09:25 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1982056
IBM Index Class Name
Report
Doc Date
2/1/1988
Doc Name
1987 ANNUAL HYDROLOGIC REPORT 1987 WATER YEAR
Annual Report Year
1987
Permit Index Doc Type
HYDROLOGY REPORT
Media Type
D
Archive
No
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1 <br />The water quality data for the Twentymile Sandstone wells is summarized on <br />' Tables 5 to 7. The data does not indicate any trends that appears related <br />to the underground mining. Both wells have a field conductivity level of <br />' approximately 850 umhos/cm. This is within the range expected for the <br />unaffected aquifer. The data does not indicate any significant changes jn <br />the trace metal concentrations. The water in well 006-82-48A is mixed tyke <br />with no dominant cation and sulphate as the dominant anion. <br />The water quality data for the Wadge Overburden aquifer wells is summarized <br />on Tables 8 to 12. A plot of dissolved solids is presented on Figure 7. <br />' The plot does not indicate any trends that appear related to the underground <br />mining. Due to the collapsed casing in well 006-82-48 the recent water <br />' quality data is suspect. The water is a sodium-sulphate; the data does not <br />indicate any significant changes in the trace metals concentrations. <br />' Alluvium <br />' Sediments in the Foidel Creek valley up and downstream of the portal area <br />are monitored. Also, the sediments in the Fish Creek valley within <br />t Twentymile Park are monitored. Four wells completed in the Foidel Creek <br />alluvium are monitored. Five wells completed in the Fish Creek alluvium are <br />' monitored. <br /> Water Levels - The plots of the historic water levels in three Foidel Creek <br />' alluvial wells are presented on Figures 8 to 10. A plot of the historic <br /> water levels in some of the Fish Creek Wells is presented on Figure 11. The <br />t water levels in the wells show the typical seasonal pattern of relatively <br /> rapid increase and decline due to spring runoff. <br />1 <br /> <br />1 <br /> <br /> <br />While the seasonal variation in water levels in the Foidel Creek alluvium is <br />readily apparent, no impact from the underground mining is evident. The <br />average water levels in the three wells, adjusted for differences in spring <br />runoff, has not changed since monitoring began in 1979. Since the <br />underground mining has not yet approached Fish Creek, no Impacts are <br />likely. The Fish Creek water level data is presented for baseline purposes <br />only. <br />' -4- <br />
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