Laserfiche WebLink
• <br />To: <br />Ryan Sweetwood and Kathy Welt <br />Mountain Coal Company, LLC <br />Via Email <br />Re: E -Seam Angle of Draw <br />MEMORANDUM <br />From: Wright Water Engineers, Inc. <br />Gary D. Witt, P.G., and Richard Dunrud, P.E. <br />Date: August 2, 2010 (Revised February 1, 2011) <br />During the latter half of 2009, Mountain Coal Company, LLC's (MCC) mining of the first E -seam <br />panel (Panel E -1) in the South of Divide mining area extended westward beyond the subsidence <br />monument grid established at the eastern end of this panel (Map B -1 of Appendix B in the Spring <br />2010 Subsidence and Geologic Field Observations report [Spring 2010 Report]). Survey data <br />collected prior to, during, and following mining beneath the area has been collected in a timely <br />manner as required by the permit. This data was included as Appendix B in the Spring 2010 Report <br />prepared by Wright Water Engineers, Inc. (WWE) in October 2010. <br />Subsidence monument grid data is useful in evaluation of many subsidence parameters including <br />displacement, tilt, strain, angle of draw, break angle, and angle of major influence. Of these, the <br />primary focus is generally given to the angle of draw because of the geometric considerations which <br />stem from this particular parameter (i.e., panel layout relative to features such as water resources <br />and geologic hazards). This memorandum lays out the specific calculations for angle of draw as <br />developed from data obtained as part of the subsidence monitoring program. <br />Figure 1 shows the location of the 124 subsidence monitoring grid monuments relative to longwall <br />panel E -1. Of particular interest in the subsidence grid survey data is the identification of the <br />subsidence trough boundary along each traverse. Monument locations with no discernable longwall <br />subsidence (approximate edge of subsidence trough) are listed in Table 1. <br />The angle of draw (T) is defined as the angle between the projection of a straight line from the coal <br />extraction boundary (i.e., edge of longwall panel) to the outer limit of the observed elevation change <br />caused by the longwall extraction and the vertical reference relative to this coal extraction boundary. <br />(see Figures A and B of Appendix A of the Spring 2010 Report). The calculation is relatively <br />simple, once the elevation change caused by the coal extraction panel is differentiated from the <br />influences of the surrounding chain pillars. Therefore, the trigonometric equation is as follows: <br />Wright Water Engineers, Inc., 2490 W. 26 Avenue, Ste. 100A, Denver, CO 80211 <br />Tel. 303/480 -1700; Fax. 303/480 -1020, e- mail:wwe @wrightwater.com <br />