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2008-01-16_APPLICATION CORRESPONDENCE - C2008086 (3)
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2008-01-16_APPLICATION CORRESPONDENCE - C2008086 (3)
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Last modified
8/24/2016 3:21:02 PM
Creation date
2/7/2008 3:18:14 PM
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Template:
DRMS Permit Index
Permit No
C2008086
IBM Index Class Name
Application Correspondence
Doc Date
1/16/2008
Doc Name
Preliminary Draft Environmental Impact Statement/Subsidence
Media Type
D
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DRAFT <br />gob until the sandstone suddenly breaks. This is particularly troublesome when the <br />longwall face roughly parallels awidely-spaced and persistent joint set. When the <br />shearer undercuts such a joint, the face supports can be subject to a sudden load <br />increase, i.e. a long line of joint blocks can suddenly be released. When a <br />moderately large rigid gateroad pillar is loaded by the abutment arch from mining of <br />the longwall panel on one side, considerable strain energy can be stored in the pillar. <br />The loading of the pillar will be rapidly doubled when the adjacent panel is mined <br />past the pillar on the other side. If the strength of the gateroad pillar is only <br />marginally strong enough to carry the arched load, the stored strain energy can be <br />suddenly released as a rib bump or outburst. It is necessary to achieve a balance <br />between a rigid gateroad pillar when the first panel passes and a pillar that will yield, <br />but not fail until the second panel has been mined well past the location. A barrier <br />pillar can be left between every set of two longwall panels. This practice can waste <br />part of the coal resource. A rigid barrier pillar between adjacent longwall panels can <br />induce higher tensile strains in the overlying ground surtace. Rigid barrier pillars are <br />normally designed to isolate panel groups and protect mains and submains and <br />bleeder rooms. Rigid barrier pillars can locally concentrate stresses in closely <br />overlying and underlying coal seams hindering their future mining. <br />For a given point of observation on the surface, the compression arch will have <br />dissipated when subsidence and surface strains have ceased. This, however, takes <br />time, potentially years for the differential stresses to decrease to a stable and <br />permanently supportable level. Active measurable surface subsidence will <br />temporarily decrease significantly when the given point is over a gateroad and <br />between 0.5 to 0.7 times the depth horizontally from any adjacent active longwall <br />panel face. If none of the gateroad pillars are rigid to the load applied when the first <br />adjacent panel passes, less subsidence will occur on the surface over the gateroad <br />when the adjacent longwall panel is mined. When the gateroad pillars yield, the <br />excess load they were unable to support will be transferred to the unmined coal in <br />the adjacent panel. The adjacent gob (collapsed immediate roof rock) will be more <br />uniformly if all the gateroad pillars yield when the first panel passes. However, when <br />the adjacent panel passes the yielded pillars major overburden loading must be <br />carried by the coal at the tailgate corner of the face, see Figure 2. Keeping the <br />tailgate entry open to ventilate the longwall become a serious problem. <br />4.0 GEOLOGIC FACTORS INFLUENCING SUBSIDENCE <br />It is extremely difficult to quantify the impact of geology on the extraction of coal and the <br />resulting subsidence of the ground surface. There are some obvious generalities that can be <br />stated with complete confidence, but predicting what will happen and where is fraught with risk. <br />The overall geology of the coal bearing Mesaverde Group is generally known, but the site <br />specific geologic conditions aren't fully understood because it is only possible to see outcrops, <br />the immediate roof and floor and the coal seam and the overburden lithology is changing. <br />Page 13 of 57 <br />
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