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2014-05-02_REPORT - M1974004
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2014-05-02_REPORT - M1974004
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Last modified
8/24/2016 5:43:44 PM
Creation date
5/6/2014 9:48:30 AM
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Template:
DRMS Permit Index
Permit No
M1974004
IBM Index Class Name
REPORT
Doc Date
5/2/2014
Doc Name
Stability analysis of spec agg quarry
From
Martin Marietta Materials
To
DRMS
Email Name
PSH
Media Type
D
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No
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Martin Marietta Materials <br />Spec -Agg 2014 Annual Report <br />According to the analysis method developed by Markland (1972), a wedge failure can occur when the <br />following criteria are satisfied: <br />1) The plunge of the lines of intersection is less than the dip of the slope face. <br />2) The plunge of the lines of intersection exceeds the angle of friction. <br />On the stereonets, Markland's criteria for wedge sliding are satisfied when the intersection of two <br />discontinuities plot within the critical zone. <br />6.4.1.3 Toppling Failure <br />Toppling failures can occur where planes share a similar dip direction to the slope face and where they <br />dip relatively steeply into the slope face. In our opinion, toppling failure is not likely to be associated with <br />large -scale instability on the scale of an entire mine highwall. Therefore, toppling was not considered in <br />our kinematic analysis. However, small -scale toppling failures are likely to occur locally at the site <br />contributing to localized rockfall. <br />6.4.2 East Walls <br />For the 2014 annual report, we analyzed two east wall orientations based on the locations shown in <br />Figure 2 and Table 2: East Walls 1 and 2 corresponds to the same wall location and orientation analyzed <br />in previous 2013 annual report. <br />The stereonet plot for East Wall 1 does not indicate the possibility of planar or wedge failure. <br />The stereonet plot for East Wall 2 shows one discontinuity intersection that falls within the failure <br />envelope, suggesting that wedge failure is kinematically possible for this slope orientation (Figure 8). The <br />intersecting set that may result in wedge failure includes joint P -5 and joint P -7. Planar failure is not <br />indicated in the stereonet plot for East Wall 1. <br />The development and size of these wedge failures will be controlled by the variability and limited lateral <br />extent of the discontinuities. Based on the 2014 data set, joint P -5 and joint P -7 have weak signatures <br />represented by relatively few measured orientations representing these features (Figure 6). As <br />excavation proceeds in the eastern walls, additional measurements are needed to refine the <br />representative discontinuity orientations of these joint and foliation sets in this area to evaluate their <br />potential to contribute to large -scale slope failure modes. <br />Our analysis indicates that potential planar and wedge failures may form in individual benches along the <br />eastern walls with near vertical faces during the temporary conditions prior to reclamation. <br />6.4.3 Northern Walls <br />For the 2014 annual report, we analyzed four northern wall orientations based on the locations shown in <br />Figure 2 and Table 2: Northeast Walls 1 through 3, and the Northwest Wall correspond to the same wall <br />locations and orientations analyzed in previous 2013 annual report. <br />March 31, 2014 Page 12 Lachel & Associates, Inc. <br />Project 13364013.00 02014 All Rights Reserved <br />
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