My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
REP38147
DRMS
>
Back File Migration
>
Report
>
REP38147
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/25/2016 12:17:48 AM
Creation date
11/27/2007 7:59:40 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981034
IBM Index Class Name
Report
Doc Date
11/30/1996
Doc Name
1996 ANNUAL HYDROLOGIC REPORT
Annual Report Year
1996
Permit Index Doc Type
HYDROLOGY REPORT
Media Type
D
Archive
No
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
17
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
Red Canyon Mine - 1996 AHR Page 2 <br />`~`~~ ~'` ~`~'-~"' - ""' Total Dissolved Solids m Sodium Adso lion Ratio <br /> <br />~-~''*<=~~%-~<'?<<~i;:;;:,~ Measured Predicted Measured Predicted <br />U/S Wazd 9/94 60 214 0.67 0.90 <br />U/S Ward 9/95 66 214 0.67 0.90 <br />U/S Wazd 10/96 78 214 0.69 0.90 <br />D/S Ward 9/94 105 214 1.02 0.90 <br />D/S Ward 9/95 90 214 0.69 0.90 <br />D/S Ward 10/96 112 214 0.72 0.90 <br />This sampling confirms that the Red Canyon Mine has not had an adverse impact on the quality <br />of water in Ward Creek. <br />The hydrologic monitoring pmgram requires the sampling of springs SP-1 and SP-3 for flow, pH <br />and conductivity twice each year. This monitoring is done to determine if the quality of the <br />springs is impacted by water which could seep into the alluvium from the possibly flooded mine <br />workings. in May and September the conductivity of SP-1 was 830 and 780 uhmos/cm <br />respectively. Both values are higher than the historical average of 734 uhmos/cm but lower than <br />the historic high of 990 uhmos/cm. Tn May the conductivity of SP-3 was 620 uhmos/cm which <br />is higher than its historical average but less than the historical high of 666 uhmos/cm. in <br />September the wnductivity of SP-3 was 580 uhmos/cm which is less than its historical average <br />of 591 uhmos/cm and much less than the historic high of 666 uhmos/cm. The pH of the spring <br />water, both SP-1 and SP-3, is within an acceptable range. <br />The enclosed graph shows that the conductivity of spring SP-1 has consistently been below its <br />historic maximum during the period 1989 through 1995. For Spring SP-3, the enclosed graph <br />shows that its conductivity has consistently been above its historic average and below its historic <br />maximum except during 1993 when the measured conductivity of SP-3 was about 12% greater <br />than it historic maximum. <br />The hydrologic monitoring program provides for monitoring to determine if run-off from the <br />mine site has any impact on the water quality in the Carbon Ditch. SP-D is the upstream <br />monitoring point and SP-DA is the downstream monitoring point on the Carbon Ditch. SP-D is <br />located on the Carbon Ditch at a point that would not be impacted by surface run-off from the <br />mine site. SP-DA is located downstream on the Carbon Ditch at a point that could be impacted <br />• by surface run-off from the mine site. Both points are monitored during May and September for <br />field parameters and total suspended solids, (TSS). Tn May the TSS for SP-D and SP-DA was <br />
The URL can be used to link to this page
Your browser does not support the video tag.