My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
PERMFILE107193
DRMS
>
Back File Migration
>
Permit File
>
100000
>
PERMFILE107193
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 9:59:45 PM
Creation date
11/24/2007 2:51:47 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1982056A
IBM Index Class Name
Permit File
Doc Date
10/14/2007
Section_Exhibit Name
2.05.5 Postmining Land Uses
Media Type
D
Archive
Yes
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
115
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
(Trout Creek below Fish Creek) to perform a regression. Therefore. the flow at Sne 1005 was calculated by <br />adding the estimated natural flow from Fish Creek (Site 1003) to the measured discharge from Site 115 and the <br />estimated floe- from Trout Creek above Fish Creek (Sne 69). "fhe equations are shoero on Exhibit 50, Tables E50- <br />2 and E50-3 and Exhibit 49, Tabie E49-26 and the regression analyses and plots are shown in Exhibit 50 Figures <br />E50-2 and E50-3). Since it is difficult to accurately measure sulfate levels in the field, conductivity has been used <br />as the indicator parameter for sulfate. ]n Exhibit 32, at the Station 69 node, the dry season TDS and sulfate levels <br />were modeled to be 412 and 174 mg/I_ respectively. Using the conversion factor of 0.75, the TDS is equivalent to <br />a conductivity of 549 umhos/cm. The ratio of the sulfate to conductivity levels is estimated to he 0.32. The stream <br />standard of 250mg/L is therefore equivalent to a conductivity of 780 umhos/cm. <br />Summaries of possible results from the mass balance calculation are shoem in Exhibit 49, Tables E49-23 and E49- <br />24. Site 109 may be able to discharge at the maximum loading under all cases and at flow rates as low as 50% of <br />the mean flow rate. During periods where Site 109 cannot discharge, the flows will be diverted into the sump in <br />the WMD. As discussed above, thr sump will be drawn down during periods of high flow to compensate for when <br />Site 115 is pumped at less than 55-gpm and Site 109 discharge is diverted into the sump. <br />]t should be noted for the period of record before starting the underground mine (October 1980 to December 1984) <br />21% of the sulfate measurements exceeded 250 mg/L. This indicates that there are other sources of sulfate in the <br />system. To account for this, when the conductivity at Site 301 (Trout Creek above Middle Creek) equals or <br />exceeds 740 umhos/cm the discharge from Site 109 will cease. This level is 95% of the standard. <br />Lower Trout Creek -Below Fish Creek <br />The flow rate and water quality of Trout Creek below Fish Creek will be affected by the discharges from Site 109 <br />and Site ] 15. Based upon the TR-32 update to the original modeling, there is a potential for significant impacts to <br />the water quality in this reach. The modeling indicates that during low flaw periods the sulfate level may exceed <br />250 mg/L. The highest modeled SAR value was 2.4, indicating that there is no significant impact to the SAR <br />level. The highest modeled conductivity value was 964 umhos/cm, indicating that the changes will not <br />significantly impact irrigation use. Based upon the potential to exceed the sulfate concentration, TCC will commit <br />to maintaining the discharge rates from Site 109 and Site 115 at levels to prevent exceeding the standard. In <br />addition to any other required monitoring, TCC will monitor the flow rate and conductivity at Site 69 (Trout Creek <br />below Middle Creek), Site 115, and Site 109 weekly and the conductivity at Site 301 (Trout Creek above Middle <br />Creek) as described in the Fish Creek and Lower Trout Creek between Middle and Fish Creek discussions above. <br />In addition to any other monitoring requirements, the flow rate and conductivity at Si[e 1005 will be monitored <br />weekly when either Site 109 or 115 is discharging see Exhibit 14). The discharges from Site 115 and Site 109 will <br />be adjusted using the Excel© based "Mine Discharge Calculator" shown in Exhibit 49, Table E49-24. The flow <br />rate is calculated based upon the mass balance equation shown on this table. As indicted in the previous section, <br />flow rates in Trout Creek will be estimated based upon a regression relationship with the stream gaging station on <br />the Yampa River below Steamboat Springs. <br />Since it is difficult to accurately measure sulfate levels in the field, conductivity has been used as the indicator <br />parameter for sulfate. As described above, a conversion factor of 0.32 will be used for converting conductivity to <br />sulfate levels. <br />Summaries of possible results from the mass balance calculation are shown in Exhibit 49, Table E49-23 and E49- <br />24. Modeling indicates that Site 115 should be able to discharge at the maximum loading under all modeled cases <br />and at the modeled mean flow rate. Site 115 will not be discharged when the calculator or instream measurements <br />indicate that the sulfate standard will be exceeded. As discussed above, the sump will be drawn down during <br />periods of high flow to compensate when Site 115 is pumped at less than 55 gpm and Stte 109 is diverted into the <br />~ump. <br />TR 99-32 2.05-156 APPROtIg,'p FEB 0 S 2000 1/3/00 <br />
The URL can be used to link to this page
Your browser does not support the video tag.