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PERMFILE111626
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PERMFILE111626
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Last modified
8/24/2016 10:08:07 PM
Creation date
11/24/2007 8:47:23 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981010
IBM Index Class Name
Permit File
Doc Date
3/16/1994
Doc Name
1993 Annual Hydrologic Report
Section_Exhibit Name
Appendix W 1993 Report Section 2.5
Media Type
D
Archive
No
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typically a good indicator of the TDS and in turn a good indicator • <br />of some major constituents. The first series of pages in Table B-1 <br />of Appendix B presents the TDS, conductivity, and sum of major <br />constituents (DSSUM) for each Well along with several other <br />parameters. DSSUM was calculated by adding the concentrations of <br />major cations and the major anions, except for one-half of the <br />bicarbonate which is not added because this concentration is <br />evaporated during the measurement of TDS. This allows a comparison <br />of TDS and DSSUM, which is a good check on the TDS and major <br />constituent measurements. The first series of parameters presented <br />in Table B-1 also includes values of the charge balance (BALNC) of <br />the major constituents. BALNC is calculated as the difference of <br />cations to anions in meq/1 divided by their sum times 100. BALNC <br />is also a good indicator of accuracy of major constituents and <br />values between -10 and 10 are considered good. The TDS <br />concentrations from the Trapper Mine ground-water quality generally <br />compared favorably to the corresponding conductivity values. <br />3.3 pH <br />Field pH is an important parameter to monitor because some <br />coal spoils have the potential to increase acidity of the ground <br />water which increases the mobility of most heavy metals. A pH of <br />less than 5 would generally be needed to greatly increase the <br />mobility of most heavy metals. <br />Available pH data is tabulated in Table B-1 of Appendix B. <br />Field pH has varied from 6.6 to 6.8 in 1993 for water from well <br />3-8 <br />
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