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2016-01-07_PERMIT FILE - C2010089A (11)
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2016-01-07_PERMIT FILE - C2010089A (11)
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Last modified
1/31/2017 9:56:06 AM
Creation date
2/11/2016 10:27:49 AM
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DRMS Permit Index
Permit No
C2010089A
IBM Index Class Name
PERMIT FILE
Doc Date
1/7/2016
Doc Name
Protection of Hydrologic Balance
Section_Exhibit Name
Section 2.05.6(3)
Media Type
D
Archive
Yes
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over time. Six months prior to NI -IN Mine startup, monitoring of Spoil Spring #1, 001 discharge <br />site, and SW -N3 (on Tuttle Draw) will be resumed if at that time it has been suspended. The <br />approved "hydrologic monitoring plan" is described in Appendix 2.05.6(3)-3 at the end of this <br />section. <br />Impacts to receiving Waters — Meehan Draw <br />The Meehan Draw barrier pillar will serve as a dam of sorts (see discussion on "Spoil Water <br />Infiltration Into Low Wall" on page 23 above and Figure 2.05.6(3)-1) for water in the backfill of <br />the reclaimed pit. It is anticipated that water accumulating behind the low wall will eventually <br />issue as a "spoil spring", (Spoil Spring #4 (projected)). Based on the structure contour map (see <br />Map 2.04.6-1 in Section 2.04.6), the overburden depth, and the topography the expected location <br />of this spring is in the vicinity of NW 1/4, SW 1/4, NW 1/4 of Section 25, T. 17 N., R. 16 W., (see <br />SS #4 Map 2.04.7-1 in Section 2.04.7). There are two basic differences in the spoil water that <br />will eventually issue from Spoil Spring #4 (SS#4): <br />• The area north of Meehan Draw will be reclaimed as "dry land pasture" and will <br />not be affected by the percolation of irrigation water. Therefore, water entering <br />the pit will be the result of seepage from the bedrock zones (due to the low <br />annual precipitation and high evaporation rate very little precipitation remains for <br />percolation). <br />The quality of the water in the bedrock zones in the area north of Meehan Draw <br />is lower in TDS (see groundwater monitoring data in Appendix 2.04.7-1 of this <br />application) than the area north of the old highwall. <br />Unlike SS #1, SS #4 does not have an existing analogy to draw on or that has been previously <br />monitored and therefore flow and quality must be projected. The expected highwall seepage rate <br />is calculated by Q = (K, ft/day)(area, ft2)(gradient)(365days)/43,560ft3 to get acre -ft per year. <br />Hydraulic conductivity or K is different for each of the bed rock zones: OB = 2. 1, Coal = 0. 19, <br />and UB = 1.61, (see Tables 7-5 and 7-6 in Appendix 2.04.7-2 this application). Height of each of <br />the bedrock zones is also different: OB = 20.3 ft. during irrigation season and 14 ft during non - <br />irrigation season; Coal 6.Oft.; and UB 5.Oft. Gradient is estimated from the draw down (cone of <br />depression) around the old Peabody highwall at 0.053. The maximum highwall length from the <br />north and east high walls is 4005 ft. During irrigation season (165 days) it is projected that <br />maximum seepage into the pit will be: OB = 34.3 ac -re; Coal = 1.07 ac -ft; and UB = 7.77 ac -ft <br />for a total of 43.14 ac -ft, or about 59 gpm. During non -irrigation season (200 days) it is projected <br />that maximum seepage into the pit will be: OB = 28.7; Coal = 1.29; and UB = 9.41 for a total of <br />39.4 ac -ft or about 44.6 gpm. This is a total of about 82.6 ac -ft per year, not all of which will <br />accumulate to issue as a spoil spring. As noted above (see discussion of seepage into "low wall" <br />Section 2.05.6(3) Page 29 Sept. 2015 (TR -11) <br />
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