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PERMFILE45400
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PERMFILE45400
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Entry Properties
Last modified
8/24/2016 10:47:46 PM
Creation date
11/20/2007 12:20:32 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981022
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Doc Name
PREDICTED D SEAM LONGWALL SUBSIDENCE /ELK CREEK MINE ABEL 1998
From
Old Exhibit 2.05-E2 Part 6
Section_Exhibit Name
Exhibit 2.05-E8 Part 4
Media Type
D
Archive
No
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"D" Seam Longwall Subsidence Page 59 August 17, 1998 <br />flexure and associated extension of the ground surface may open as <br />• the result of longwall panel mining. Prediction of the maximum <br />horizontal compressive strain line is less important because <br />compression ridges represent only a minor hazard. <br />The maximum predicted vertical subsidence at the final <br />recovery room and starter room for each individual panel in each <br />panel group conservatively assumed that the gateroad pillar <br />crushing subsidence at the local depth was added to the single <br />panel subsidence at that depth. Table 13 presents the predicted <br />subsidence at the ends of each panel in each panel group. <br />Table 1 presented the maximum predicted worst-case subsidence <br />and horizontal strain at the critical locations alongside and at <br />the ends of the panel groups. The worst-case maximum predicted <br />horizontal tensile (+E) and compressive (-E) strains for each of <br />the five panel groups will result in observable subsidence effects. <br />The magnitude of the maximum predicted tensile strains would <br />result in tensile fractures at the ground surface. These fractures <br />will be most pronounced at the shallower southern end of the panel <br />groups. The absolute maximum predicted tensile strain is 59950µe, <br />at the southern end of Panel #7. The predicted open surface <br />fractures will approach 2-ft in width. Outside the southern panel <br />mining limits these open fractures may intercept seasonal runoff <br />• water and divert it toward the east or west, depending on the local <br />hillside slope direction. In effect, the east-west open surface <br />fractures will facilitate the flow of runoff toward the nearby <br />natural drainages. The predicted north-south open surface <br />fractures will tend to channel runoff water downslope, generally <br />toward the south. The channelization of the seasonal surface <br />runoff will tend to fill the open fractures and possibly <br />temporarily increase erosion along the subsidence fracture <br />channels. The impact should, however, be temporary as indicated by <br />the absence of any such subsidence induced drainage channel <br />diversions from the previous advance-and-retreat high-extraction <br />room-and-pillar mining. Advance and retreat room and pillar mining <br />at the shallow mining depths should have produced similarly high <br />horizontal ground surface strains. No open fractures produced by <br />shallow room and pillar mining are currently visible. The natural <br />vegetation has apparently thrived in the subsidence areas in the <br />past and should do the same in the future. <br />The predicted maximum worst-case compressive strains will <br />produce compression ridges at the ground surface within the <br />projected outlines of the panel groups, at the locations indicated <br />on the plates. The height of the worst case compression ridges, <br />less than 1-ft, in relation to the hillside slopes at the ground <br />surface should not impede the normal seasonal runoff. The absolute <br />• maximum predicted compression strain is 15750µe, also at the <br />southern end of Panel #7. <br />54 <br />
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