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PERMFILE126208
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PERMFILE126208
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Last modified
8/24/2016 10:23:28 PM
Creation date
11/25/2007 3:05:49 PM
Metadata
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Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
Permit File
Doc Date
6/24/2004
Section_Exhibit Name
Exhibit 07 NPDES Permit
Media Type
D
Archive
No
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Mountain Coal and Beaz Coal Water Quality Assessment CO-0038776 and CO-0044377 <br />The ambient water quality background concentrations used in the mass-balance equation account for <br />pollutants of concern contributed by upstream sources, and thus it was not necessary to model <br />upstream dischargers together with the Mountain Coal and Beaz Coal W WTFs when determining the <br />available assirilative capacities in the North Fork of the Gunnison River. Due to the distance <br />traveled, the significant dilution of the North Fork of the Gunnison River, and the changes in the <br />chazacteristics ofthe receiving stream, modeling downstream facilities in conjunctionwith Mountain <br />Coal and Beaz Coal WWTFs was not necessary. <br />Due to the low flow of zero, consideration of other sources when allocating assimilative capacities to <br />discharges to Sylvester Gulch, West Sylvester Gulch, the Dry Fork of Minnesota Creek and Lone <br />Pine Gulch was not necessarybecause the full assirilative capacities of these receiving streams aze <br />equal to the stream standards. <br />Based on available information, there is no indication that non-point sources were a significant <br />source of pollutants of concern. Thus, non-point sources were not considered in this assessment. <br />Chlorine: The mass-balance equation was used to determine the assimilative capacity for chlorine <br />for Outfa11004, which receives effluent from the domestic W WTF (Internal Outfa11007). There aze <br />no point sources dischazging total residual chlorine within one mile of the Mountain Coal W WTF <br />Outfa11004. Because chlorine is rapidly oxidized, in-stream levels of residual chlorine aze detected <br />only for a short distance below.a source. Ambient chlorine was therefore assumed to be zero. <br />Using theinass-balance equation provided in the beginning of Section N, the acute and chronic low ~ . <br />flows set out in Section III, the chlorine background concentration of zero as discussed above, and <br />the in-stream standards for chlorine shown in Section II, assimilative capacities for chlorine were <br />calculated. The effluent flow, Q1, reflects the design flow from Outfa11004 and Internal Outfa11007 <br />in the respective calculations. The data used and the resulting calculations ofthe allowable dischazge <br />concentration, MZ, aze set forth below. <br />7VnrtA Fnr4 nftho ('rrmnicnn Rivor <br />V <br />Parameter Q~ (cfs) QZ (cfs) Qe (cfs) M~ (mg/I) Ms (mg/!) Mz (mg/1) <br />Acute Chlorine 32 0.28 32.28 0 0.019 2.2 <br />Chronic Chlorine 43 0.28 43.28 0 0.011 1.7 <br />Outf_all 007 <br />Parameter Q ~ (cfs) Q Z (cfs) Q 3 (cfs) Mt (mg/1) M j (mg/1) Mz (mg/1) <br />Acute Chlorine 32 0.016 32.016 0 0.019 38 <br />Chronic Chlorine 43 0.016 43.016 0 0.011 30 <br />Fecal Coliform: There aze no point sources discharging fecal coliform within one mile of the <br />Mountain Coal WWTF Outfa11004. Thus, fecal coliform assimilative capacities for Outfall 004 <br />were evaluated sepazately. <br />Appendix A Page 14 of 20 Last Revised 3/912004 <br />
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