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PERMFILE52847
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PERMFILE52847
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Entry Properties
Last modified
8/24/2016 10:56:29 PM
Creation date
11/20/2007 3:28:44 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981028
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Doc Name
GROUND-WATER RESOURCES STUDY
Section_Exhibit Name
ASH DISPOSAL PLANS APPENDIX A
Media Type
D
Archive
No
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38 <br />Using an average seam thickness of 5,86 ft, a trench width of 100 ft, <br />a coal density of 80 lbs/f t3, and a mean production rate of 510,000 tons/yr, <br />the rate at which the trench is extended is 50 ft/day, On the average, <br />the maximum length of open trench 'in Pit A will be 3000 ft, a length that <br />will be achieved in some 60 days, assuming the average conditions presented <br />above apply at the outset of mining. For the purposes of pit inflow <br />estimates, it is further assumed that overburden removal in Pit B is <br />initiated at the beginning of the second year and that the trench length <br />is extended at the rate of 50 ft/day. Under these conditions, the maximum <br />length of open trench at any time is 6000 ft. <br />Inflow to the pit will occur from both sides and the ends. However, <br />the area of aquifer exposed on the end of the trench is very small relative <br />to the area exposed on the lateral surfaces of the pit, and inflow from <br />the end of the trench was neglected, therefore. Depending upon the final <br />mining plan, there is one area in Pit A where the eastern extremity of <br />1 <br />the. pit may intersect the old stream deposits in Ennis Draw_ Potential <br />inflow for this case will be discussed subsequently. <br />Regardless of whether the aquifers are confined or unconfined <br />initially, the exposure of the aquifers in the pit will cause the aquifers <br />to become unconfined in the vicinity of the pit. Therefore, the aquifers <br />will respond according to a coefficient of storage (apparent specific <br />yield) characteristic of unconfined materials. Also, exposure of the <br />aquifers in the pit causes the boundary condition on the outflow face <br />of the aquifers to be that of atmospheric pressure. Because individual <br />aquifers in the overburden could not be identified, the interval extend- <br />ing from the bottom of the coal seam to the existing piezometric surface <br />was regarded as the initial saturated thickness. The saturated thickness <br />i <br />
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