My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
REP10089
DRMS
>
Back File Migration
>
Report
>
REP10089
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 11:39:33 PM
Creation date
11/27/2007 12:18:44 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981022
IBM Index Class Name
Report
Doc Date
2/2/1996
Doc Name
1995 AHR
Annual Report Year
1995
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.
/
155
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
Sanborn Creek Mine 1995 Annual Hydrologic Report <br />Monitoring <br />The hydrologic monitoring parameters and the schedules for the <br />hydrologic monitoring program are presented in Appendix 1. The <br />parameters and schedule were changed during 1994 by Technical <br />Revision No. 20. <br />Field parameters for groundwater are depth to water level, pH, <br />conductivity, and temperature. Field parameters for surface water <br />are flow, pH, conductivity, and temperature. Equipment and methods <br />used to measure the field parameters include: <br />Depth to water level - A cable marked in increments is lowered into <br />the groundwater monitoring well until electrical continuity is <br />reached at the water surface. A tape measure is used to determine <br />distances between marked increments. <br />pH - A Cole Parmer pHTestr 2 pocket-size tester is used to measure <br />the pH of a water sample. Published specifications for the pHTestr <br />2 are range: pH -1.0 to 15.0, resolution: 0.1 pH, accuracy: +/- 0.1 <br />pH, automatic temperature compensation: 0 to 50 degrees C, <br />calibration points: 1, 2, or 3. The pH tester was calibrated prior <br />to sampling events using the 2 point method. The expected pH was <br />bracketed by the pH of the calibration solutions. In most cases <br />the pH tester was calibrated at 7 and 10 which brackets all of the <br />• current monitoring results. If an expected pH is less than 7, the <br />pH tester will be calibrated at 4 and 7. <br />Conductivity - Two Cole Parmer pocket-size testers with different <br />range capabilities are used to measure the conductivity of a water <br />sample. Published specifications for the TDSTestr 3 are range: 0 <br />to 1990 u5, resolution: 10 uS, accuracy: +/- 2$ full scale, <br />automatic temperature compensation: 0 to 50 degrees C, calibration <br />with standard solution. Published specifications for the TDSTestr <br />4 are range: 0 to 19.90 mS, resolution: 0.1 mS, accuracy: +/- 2$ <br />full scale, automatic temperature compensation: 0 to 50 degrees C, <br />calibration with standard solution. A single Cole Parmer TDSTestr <br />20 pocket-size tester with dual range capabilities may be <br />substituted for the TDSTestr 3 and/or the TDSTestr 4. Published <br />specifications for the TDSTestr 20 are range: 0 to 1990 uS with <br />resolution 10 u5 and 2.0 to 19.90 m5 with resolution 0.1 mS, <br />accuracy: +/- 2$ full scale, automatic temperature compensation: 0 <br />to 50 degrees C, calibration with standard solutions. The <br />conductivity testers were calibrated prior to sampling events with <br />calibration solutions in the expected range. <br />Temperature - A standard mercury thermometer which measures <br />temperature in degrees Celsius is used. <br />Flow - One of two methods is used to determine the flow at the <br />2 <br />C~ <br />
The URL can be used to link to this page
Your browser does not support the video tag.