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West Elk Mine <br />and from 100 to 250 feet wide above the chain pillars. This zone, is located approximately <br />above the edges of the panels or slightly outside the panel boundaries and above the center of the <br />chain pillazs, unless adown-slope component of movement occurs on steep slopes in addition to <br />the differential tilt component. Cracks tend to be more common and more permanent in zones <br />above mine boundaries, barrier pillazs, and unyielding chain pillars. Any surface or neaz-surface <br />water that might be present in this zone has a higher probability of being impacted than that <br />occumng in the centers of the panels. <br />Angle of Major Influence <br />The angle of major influence, (3, (also called angle of influence of the point of evaluation) is <br />defined by Peng (1992, p. 11) "... as the angle between the horizontal and the line <br />connecting the inflection point and the edge of the radius of major influence." The radius <br />of major influence (r) is therefore the horizontal distance from the vertical projection of the <br />inflection point to the point of maximum subsidence and the limit of subsidence (See <br />Exhibit 60B, Figure 3). The angle of major influence is used for computer modeling by the <br />influence function method. In the B Seam mining at West Elk Mine, the angle of major <br />influence ranges (from a horizontal reference) from about 70 to 80 degrees. For E Seam <br />mining in the South of Divide mining area, the angle of major influence is also expected to <br />range from 70 to 80 degrees, which was used for the computer modeling described below. <br />The angle of major influence may also be referenced to the vertical, as has been done for <br />the break angle and angle of draw. The angle of major influence (from a vertical <br />reference) is roughly equal to the angle of draw, and is therefore predicted to range from <br />10 to 20 degrees. <br />Relation Between Dynamic and Final Subsidence Deformations <br />Maximum dynamic tilt (change of slope) and horizontal tensile and compressive strain are <br />reportedly less above longwall mining panels than are the final tilt and strain values at <br />panel boundaries. Dynamic tilt and strain decrease, relative to final tilt and strain, as the <br />rate of face advance increases. <br />Dynamic tilt and strain reportedly decrease with increasing speed of longwall coal <br />extraction (Peng 1992, p. 20-21). Based on observations in a West Virginia coal mine: <br />1. Maximum dynamic tilt decreased by an average of 42 percent (from 0.0024 to 0.0014) as <br />the mining face rate of movement increased from 10 ft/day to 40 ft/day; dynamic tilt, <br />therefore, decreased by 14 percent as the face rate of movement increased by 30 ft/day. <br />2. Maximum dynamic tensile strain decreased by an average of 22.5 percent (from 0.0031 <br />to 0.0024) as the mining face velocity increased from 10 ft/day to 40 ft/ day; dynamic <br />horizontal tensile strain decreased by 7.S percent as the face increased by 30 ft/day. <br />C~ <br />2.05-121 Revised November 1004 PR70 <br />