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2017-03-15_REPORT - C1981010
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2017-03-15_REPORT - C1981010
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Last modified
3/22/2017 7:39:06 AM
Creation date
3/16/2017 7:31:43 AM
Metadata
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DRMS Permit Index
Permit No
C1981010
IBM Index Class Name
Report
Doc Date
3/15/2017
Doc Name
Annual Hydrology Report
From
Trapper Mining Inc
To
DRMS
Annual Report Year
2016
Permit Index Doc Type
Hydrology Report
Email Name
RAR
DIH
Media Type
D
Archive
No
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Figure B-2 also presents a group of four QR wells. Well GF -11 is an equivalent QR aquifer <br />well in the backfill. The 2016 TDS concentrations were fairly steady in backfill well GF -11 and is <br />below its peak in 2001 and 2002. Concentrations in the QR aquifer are monitored downgradient at <br />well GF -6 and have shown no influence from the upgradient mining, except for a very slight overall <br />increasing trend. These small changes are well within natural variations. Figure B-2 also presents <br />the IDS concentrations for QR wells GP -5 and GLEV-1. TDS concentrations in well GP -5 were <br />steady in 2016 while a slightly smaller concentration was observed in new well GLEV-1. <br />Figure B-3 presents the TDS concentrations for three KLM aquifer wells. The data for <br />well GP4 is presented in red square on Figure B-3 with steady values in 2016. The concentrations <br />are overall similar to values for the last several years. TDS concentrations for two of the eastern <br />KLM wells, GP -2 and GP -8, are also shown on this figure with concentrations generally between 700 <br />and 800 mg/l. Variable TDS concentrations that are overall steady have been observed in these two <br />wells for the last several years. <br />Figures B4 presents the TDS concentrations versus time for the M aquifer wells. The TDS <br />in M aquifer well GF4 had gradually increased in concentrations with time but has been fairly <br />steady for the last several years. The small changes are well within natural fluctuations in this well <br />but could be due to upgradient mining. TDS concentration in backfill well GF -5 is slightly greater <br />but is still well within the natural range for the M aquifer. Significantly higher TDS values have <br />been observed in backfill well GF -7 with the concentrations in the last nineteen years being between <br />the lower levels prior to this period and the maximum historical values from this well. TDS values <br />in this backfill aquifer will likely fluctuate until they decline to a value similar to the M aquifer in <br />this area. <br />Trapper Mining Company 3-2 <br />2016 Annual Report <br />
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