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REP50869
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REP50869
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Last modified
8/25/2016 12:55:45 AM
Creation date
11/27/2007 12:57:30 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981033
IBM Index Class Name
Report
Doc Date
4/30/1998
Doc Name
1997 ANNUAL HYDROLOGY REPORT
Annual Report Year
1997
Permit Index Doc Type
HYDROLOGY REPORT
Media Type
D
Archive
No
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GROUND WATER MONiTORTNG <br />Quarterly water samples are collected at monitoring wells AA-1 and AA-3 using a hand <br />bailer. The results of groundwater data collected during 1997 and pertinent water quality <br />parameters are found below. Depth to water is measured from the top of the steel casing on AA- <br />l and top of the 2-inch PVC pipe for AA-3. The location of the alluvial wells can be found on <br />map, "Figure I1", in Appendix A. Graphs and well completion diagrams are presented in <br />Appendix B. Laboratory reports are presented in Appendix C. <br />Monitoring well AA-1 was destroyed by the November 1997 slide and has not been <br />replaced. <br />Monitorine Well AA-1: <br />Quarter Date pH <br />su Temp °C Depth <br />feet Cond. <br />umhoslcm TDS <br />ppm Oil or <br />Grease <br />1" 3/31/97 7.3 10.2 9.54 2,400 1,210 None <br />2"d 5128197 7.3 17.5 7.5b 3,000 1,510 None <br />3rd 8/26/97 7.1 26.2 9.0 4,070 3,600 None <br />4d' 11/30/97 Destroyed by Slide <br />Monitorin¢ Well AA-3: <br />Quarter Date pH <br />su Temp °C Depth <br />feet Cond. <br />umhos/cm TDS <br />ppm Oil or <br />Grease <br />1" 3/31/97 7.8 4.2 8.48 1,120 560 None <br />2"d 5/28/97 8.1 10.3 5.76 240 120 None <br />and 8/26/97 7.3 17.8 7.78 1,060 -- None <br />4d' 11/30/97 7.8 8.6 7.98 3,300 1,660 None <br />Findings: <br />AA-1 No laboratory results are available for AA-1 since this well was destroyed in November <br />1997 and laboratory samples are typically collected in December. The field conductivity in <br />the well was 2,400, 3,000 and 4,070 umhos/cm during the 1" , 2"d and 3'd quarters <br />respectively. The 4070 umhos/cm value is a little high for this well and may have been <br />influenced by the pending mine water discharge discussed in the introduction. The <br />unusually high water temperature measured in the third quarter (26.2 °C) further supports <br />_2_ <br />
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