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PERMFILE135052
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Last modified
8/24/2016 10:35:47 PM
Creation date
11/26/2007 3:02:37 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981010
IBM Index Class Name
Permit File
Doc Date
6/13/2002
Doc Name
2001 Annual Hydrologic Report
Section_Exhibit Name
Appendix W 2001 Report Section 2.5
Media Type
D
Archive
No
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3.0 GROUND-WATER QUALITY <br />Appendix B presents the ground-water quality data for the Trapper Mine. This <br />appendix tabulates ail of the historical data in Table B-1 and presents TDS and sulfate plots <br />versus lame to convey changes in the major constituent water quality. <br />Appendix B also presents the spring and seep water-quality data. Water quality <br />for the springs and seeps are included in this section because their source is ground water. <br />Section 3.7 presents a discussion of the spring and seep water-quality data. <br />3.1 TOTAL DISSOLVED SOLIDS (7'DS) <br />Figures B-1 through B-9 present plots of the TDS concentrations for the Trapper <br />Mine wells. The wells have been grouped together based on aquifers. Figure B-1 presents <br />the TDS concentrations for wells GF-1 and GF-2. Well GF-1 is completed in the 20 Mile <br />Sandstone, while GF-2 is completed in the U aquifer. The TDS in 20 Mile well GF-1 does <br />not show a consistent trend with time with typical TDS values being around 500 mg/I. TDS <br />concentrations in U aquifer well GF-2 gradually increased from 1992 through 1995 then <br />gradually decreased followed by fairly steady concentrations the last three years. <br />Figure B-2 presents the TDS concentrations versus time for three QR aquifer wells <br />GD-2, GD-3 and GE-1. Well GD-3 is a backfill well in the QR aquifer. TDS concentrations <br />were fairly steady for the last three years in well GD-3. The fluctuation in this backfill <br />aquifer is well within natural ranges and may be very similar to variations that would have <br />occurred in the QR aquifer at this location. Some of the TDS in the backfill aquifer may be <br />due to leaching from the backflll material. The TDS in this backfill aquifer is greater than it <br />is downgradient in the R Coal at GD-2. The TDS in well GD-Z was steady in 2001. The <br />3-1 <br />
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