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2010-02-19_REPORT - C1980001 (4)
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2010-02-19_REPORT - C1980001 (4)
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Last modified
8/24/2016 3:59:51 PM
Creation date
2/19/2010 12:44:21 PM
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Template:
DRMS Permit Index
Permit No
C1980001
IBM Index Class Name
REPORT
Doc Date
2/19/2010
Doc Name
2009 Annual Hydrology Report
From
WWC Engineering
To
DRMS
Annual Report Year
2009
Permit Index Doc Type
Hydrology Report
Email Name
JDM
Media Type
D
Archive
No
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as found during baseline studies and previous years monitoring. The lowest specific conductivity <br />concentration in 2009 was recorded at monitoring site TR-A in June with a reading of 100 <br />umhos/cm @ 25 °C and the high was recorded at monitoring site TR-C in April with a reading of <br />1010 umhos/cm @ 25 °C. <br />3.3.5 Surface Water Total Dissolved Solids <br />Chart 6 shows total dissolved solids (TDS) concentrations for monitoring sites TR-A, TR-B, TR- <br />C and TR-D for the period of record. TDS concentrations in Trout Creek exhibit an expected <br />pattern. As stream flow passes the mine, TDS levels increase while adjacent to the mined areas <br />and then begin to decline downstream due to inflow from undisturbed lands below the active <br />mine. Peak TDS levels in Trout Creek adjacent to the mine occur in early spring prior to the <br />period of peak flow. This is caused by the spring runoff from the portion of the watershed in <br />which the Edna Mine is located. Although TDS concentrations in the mine runoff may be quite <br />high when compared to concentrations occurring above the mine, generally the mine runoff is <br />small relative to Trout Creek's total flow. Therefore, a significant increase in Trout Creek TDS <br />levels is observed only during the initial stages of spring runoff. A comparison of the TDS and <br />flow data indicate that TDS concentrations appear to be directly related to flow volume. <br />The dilution of TDS concentrations in downstream flow for the past decade has not been as <br />pronounced as in the previous decade. Beginning in 1990, mining and reclamation occurred in <br />close proximity to TR-C. As such, dilution of TDS concentrations probably occurs farther <br />downstream of TR-D as runoff from undisturbed areas enters into Trout Creek. Although <br />elevated TDS concentrations have moved downstream in conjunction with mining and <br />reclamation activities, all values for TDS are consistent with the probable hydrologic <br />consequences projections. TDS concentrations seem to have peaked during the 1996 sampling <br />season and have been steadily decreasing to the current year of sampling. TDS concentrations <br />exhibited the same trends in 2009 as found during previous years monitoring. The lowest TDS <br />concentration in 2009 was recorded at monitoring site TR-A in June with a value of 80 mg/L and <br />the high was recorded at monitoring site TR-C in April with a value of 740 mg/L. <br />3.3.6 Surface Water Calcium, Magnesium and Sodium <br />Charts 7, 8 and 9 show calcium, magnesium and sodium concentrations for monitoring sites TR- <br />A, TR-B, TR-C and TR-D for the period of record. Calcium is the dominant cation in Trout <br />Creek with magnesium and sodium occurring in lesser concentrations. While the relative <br />proportions of these parameters change slightly between the sampling points, all show peak <br />concentrations coinciding with spring runoff, as would be expected. As with TDS, all three <br />cations show general increases in concentration as the water passes the mine area. Additionally, <br />the relative proportion of each constituent remains constant to the other constituents. While <br />trends in their subsequent dilution downstream have yet to form a consistent pattern, little or no <br />dilution in any of the concentrations have occurred between sampling points TR-C and TR-D <br />since 1989. For the last decade, it is believed that this was due in part to the Moffat area mining <br />Page 6 <br />^?wWCENGINEERING
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