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PERMFILE62071
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PERMFILE62071
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Last modified
8/24/2016 11:08:31 PM
Creation date
11/20/2007 7:25:49 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1982056
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Section_Exhibit Name
Exhibit 35 Backfill Hydrology Evaluation
Media Type
D
Archive
No
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• Underground mine discharge are currently averaging 102gpm (0.23 <br />cfs) and show little seasonal variation. Typical total dissolved <br />solids concentrations are about 2500 mg/1. Discharge rates to <br />Foidel Creek are anticipated to increase over the next few years <br />to about 300gpm by 1988. Solute concentrations are projected to <br />remain similar to present conditions. Once the Fish Creek shaft <br />is completed, which is projected to occur in 1988, most of the <br />additional inflows will be discharged to Fish Creek. Consequent- <br />ly, projected worst case flow rate and concentrations of the <br />underground mine discharge to Foidel Creek are assumed to be <br />300gpm (0.67 cfs) and 2500 mg/1 respectively. <br />The projected backfill discharges to Foidel Creek have been <br />discussed earlier. Solute concentrations of this discharge are <br />expected to be similar to Pond F Spring water quality in the <br />order of 4000 mg/1. <br />The salt load analysis was performed using data from CYCC site 69 <br />which is on Trout Creek downstream from Middle Creek. Data from <br />this site is assumed to represent conditions before significant <br />contributions from mine related discharges to Foidel Creek. The <br />data presented in Table 2 is taken from a report on cumulative <br />hydrologic impacts in the Twentymile Park Basin performed by <br />Kaman Tempo for the Office of Surface Mininq (OSM) in 1982. The <br />• projected increase in solute concentrations in Trout Creek during <br />low flow periods are based on the worst case assumptions that all <br />flow in Foidel Creek is from mine-related discharge and that no <br />flow occurs in Middle Creek upstream from the confluence with <br />Foidel Creek. The mass balance equations used are: <br />Ftd = Ftu + Fm + Fb <br />Ctd = (Ftu Ctu) + (Fm Cm) + (Fb Cb) <br />(Ftu + Fm + Fb) <br />Where: <br />Ftd = Flow rate of <br />Ftu Flow rate of <br />Fm = Flow rate of <br />Fb = Flow rate of <br />Ctd = concentration <br />Ctn = concentration <br />Cm =concentration <br />Cb = concentration <br />Trout Creek downstream <br />Trout Creek upstream <br />Foidel Creek mine discharges <br />Foidel Creek backfill discharges <br />on Trout Creek downstream <br />on Trout Creek upstream <br />of Foidel Creek mine discharges <br />of backfill discharge <br />The results of the analysis are presented in Table 3. It can be <br />seen that the contribution of solutes from the backfilled areas <br />• at the CYCC operations presently accounts for an increase of <br />about 57 mg/1 in Trout Creek under worst conditions. This <br />16 <br />
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