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REP35532
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REP35532
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Entry Properties
Last modified
8/25/2016 12:12:51 AM
Creation date
11/27/2007 7:09:06 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981018
IBM Index Class Name
Report
Doc Date
2/1/1994
Doc Name
1993 AHR
Annual Report Year
1993
Permit Index Doc Type
HYDROLOGY REPORT
Media Type
D
Archive
No
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<br />' <br /> TABLE 2-1 <br /> SURFACE WATER QUALITY PARAMETERS <br /> AND <br /> ALLUVIAL MONITORING HOLE WATER QUALITY PARAMETERS <br />FIELD MEASUREMENTS 60RATORY ANALYSIS <br />Discharge Ammonia Potassium <br /> pH Bicarbonate Selenium, Total <br /> Specific Conductance Boron Sodium <br />' Temperature Calcium Sulfate <br /> Carbonate Totat Suspended Solids <br />' Chloride Total Dissolved Solids <br /> Copper, Total Total Volatile Solids <br /> Fluoride Sodium Adsorption Ratio <br />' Iron, Total <br /> Lead, Total <br />' Magnesium <br /> Manganese, Total <br /> Nickel, Total <br />' NiVate <br />are located near the bottom of the Coal and Siltstone Facies (middle zone). Water levels are <br />' measured quarterly in the sixteen groundwater monitoring holes. The water level is measured <br />monthly in Oi4L-5, and samples collected quarterly to analyze for the twenty two water quality <br />parameters listed in Table 2-1. <br />1 The alluvial monitoring hole, RM-1, was drilled east (downsVeam) of the pond for Refuse Disposal <br />Area 2/3 on September 28, 1989, The location of this hole is shown on Plate 1. This monitoring <br />' hole was drilled to fulfill a requirement of the mine permit. RM-1 was drilled to bedrock at a depth <br />of 32 feet. No water was encountered during drilling. The hole was drilled with seven-inch hollow <br />' flight augers and cased with perforated two-inch PVC pipe. The hole is monitored on a monthly <br />basis. No water has been detected in RM-1 to date. If detected, the water level will be measured <br />and samples collected quarterly to be analyzed for the parameters listed in Table 2-1. <br />' During October 1984, the Taylor Draw Reservoir tacitities were completed and the reservoir began <br />filling with water. The area around the alluvial groundwater holes has become a shallow water mud <br />4 <br />r <br />
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