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PERMFILE52001
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Last modified
8/24/2016 10:55:56 PM
Creation date
11/20/2007 3:09:25 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
Permit File
Doc Date
6/2/2006
Section_Exhibit Name
Exhibit 60B Subsidence Evaluation for the South of Divide Mining Area
Media Type
D
Archive
No
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Subsidence Evaluation For <br />Exhibit 606 South of Divide Mining Area Page 31 <br /> <br />greater than the magnitudes of any recorded bump or rock burst), did not affect the Somerset <br />Mine. To the author's knowledge the Rulison nucleaz shot did not trigger any landslides or <br />rockfalls, nor did it impact reservoirs, ponds, or streams in the South of Divide area. <br />15.0 SUBSIDENCE CONTROL PLAN <br />Longwall mining is currently planned for extraction of the E Seam in the proposed South of <br />Divide mining area Although longwall mining may initially induce more caving and fracturing <br />of the roof rocks as compared to the room-and-pillaz method due to the complete removal of wal <br />in the panel, it offers the advantages of maxim?ing resource rewvery. The longwall method <br />also causes more uniform subsidence (full extraction of panel) and causes equilibrium wnditions <br />to be reached in a shorter period of time (i.e., there is no additional, lingering pillar crushing in <br />panels). As such, to the extent possible, the longwall panels should be located so that homers or <br />boundaries, particularly in low cover areas, are not under or within the angle of draw or <br />influence to sensitive renewable resource lands or existing occupied residential dwellings. <br />15.1 Anticipated Effects <br />Long-term impacts on the surface are predicted to be minimal above the longwall panels. The <br />few surface cracks over the mining panels that may occur are expected to close once the <br />• longwall face moves past the surface area of influence- Surface cracks present above the rigid <br />chain or homer pillars or mine boundaries may remain open for many years where permanent <br />tensile suains remain after mining is completed. However, at least several hundred feet of rock <br />will typically exist between any mine-induced surface fractures and the upper part of any mine- <br />induced fracnues above the caved zone in the mining panels. Therefore, from a practical <br />standpoint, no interconnection between the surface fractures and the mine workings is <br />anticipated. Again, under aworst-case scenario, if a surface fracture were to occur concurrently <br />within an area controlled by faults or bedrock lineaments, there could be interconnection <br />between adjacent sandstones. However, even under these conditions, the fractures would not <br />extend through the claystones and shales present in the overburden. <br />Minnesota Reservoir is located outside of the angle of mining influence of the nine projected <br />panels (panels El through E9) for the South of Divide mining area. The northwest comer of <br />panel E9, which is nearest to dre reservoir, is located 800 feet away. The angle of draw to this <br />nearest area of mining is 69 degrees. The angle is much greater than the maximum of 20 degrees <br />projected for the South of Divide mining area. This means that Minnesota Reservoir will not be <br />affected by longwall mining in projected panel E9. <br />15.2 Reduction Measut~es (Underground) <br />C~ <br />Underground measures that may be taken to reduce surface strains above the chain pillars could <br />include: (1) designing the pillars to yield and crush after mining (thus minimising humps in the <br />subsidence profile), and/or (2) planning a rapid and unifomt mining rate. Any plans to reduce <br />chain pillaz dimensions in order to reduce subsidence impacts must, of course, be balanced with <br />831-032.690 WnghtWaterEngineers, /nc. <br />
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