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2007-11-23_HYDROLOGY - M1977300 (9)
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2007-11-23_HYDROLOGY - M1977300 (9)
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Last modified
8/24/2016 3:18:41 PM
Creation date
11/5/2010 12:03:28 PM
Metadata
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Template:
DRMS Permit Index
Permit No
M1977300
IBM Index Class Name
HYDROLOGY
Doc Date
11/23/2007
Doc Name
Hydro Eval- Vol. II- Ap. G- Sump Shut-Down Data
From
Cotter and Whetsone
To
DRMS
Permit Index Doc Type
Hydrology Report
Email Name
DB2
Media Type
D
Archive
No
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Appendix G - Sump Shutdown Test Methods and Results 7 <br />• <br />• <br />mine site and 2 cfs near Ralston Reservoirs. Well MW-9 was pumped at 15 gpm, which represents 14% <br />of the average sump pumping rate for March and 8% of the average sump pumping rate for April. <br />'Water quality field parameters (temperature, pH, and conductivity) were measured around the clock at 11 <br />stations in Ralston Creek, and samples were collected for laboratory analysis of uranium. The data are <br />presented in Table 4. pH measurements declined slightly over the duration of the shutdown test (Figure 6). <br />'When plotted spatially (Figure 7), pH shows a slight increase with distance downstream. The stream <br />standard for pH in this stream segment is 6.5 to 9.0, and the only samples that fell outside this range were <br />collected near midnight on April 1, and are believed to be related to an instrument calibration error. <br />Although conductivity values increased during the course of the shutdown test (Figure 8), the increases <br />were the same at each station downstream of the D001 discharge point and were attributable to changes in <br />'the flow rate and concentration of the water treatment plant discharge (Figure 9) rather than input from the <br />alluvium downstream. Conductivity did not increase with distance downstream (Figure 10), except 2 miles <br />downstream at station SW-LLHG, which showed variable trends. <br />Uranium concentrations increased slightly over the duration of the test (Figure 11) and with distance <br />downstream (Figure 12). Uranium values increased from about 0.5 ppb (0.0005 mg/L) above the mine to <br />approximately 1.4 ppb (0.0014 mg/L) downstream of the facility, at station SW-BPL. <br />Uranium concentrations in the discharge water averaged 1.7 ppb (0.0017 mg/L) during this period, and the <br />average flow from the water treatment plant was 200 gpm (0.44 cfs). A mixing calculation was performed <br />using these concentrations and the flow rates from the water treatment plant and in Ralston Creek, <br />according to the following formula: <br />Cds - <br />Cu -Fu + Cwt - Fwr <br />Fu + Fwt <br />Where: Cds = downstream concentration of uranium <br />Cu = upstream concentration of uranium <br />Cwt = concentration of uranium in water treatment plant discharge <br />F„ = upstream flow rate (calculated as total flow minus Fw ) <br />FWt = discharge flow rate from water treatment plant <br />The mixing calculation results (Table 3) indicate that the loading from the water treatment plant would <br />raise uranium concentrations by only 0.11 to 0.27 ppb (0.00011 to 0.00027 mg/L). Since the observed <br />increase was on the order of 0.9 ppb (0.0009 mg/L), the remainder of the loading was likely derived from <br />the alluvium. The loading from the alluvium appeared to increase toward teen o the pumping (and <br />sump shut-down) test, when the sumps had been shut down for a total of 7 days. <br />Uranium concentrations in Ralston Creek also increased beyond the property line, and averaged 2.7 ppb <br />0.0027 mg/L) at the ong ake Head Gate (station SW-LLHG). The increase in uranium below the <br />property line is believed to be the result of natural uranium input after the water leaves the mine property, <br />in part because the. Schwartz trend intersects Ralston Creek downstream of the Schwartzwalder Mine. <br />• ° Ralston Creek flow near the mine site is based on staff gage readings for station SW-BPL. <br />s Ralston Creek flow near Ralston Reservoir is based on Denver Water records. <br />4109B.071109 Whetstone Associates
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