Page 224 - Rock Mechanics For Underground Mining
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EXCAVATION DESIGN IN MASSIVE ELASTIC ROCK






















              Figure 7.8 A flat-lying plane of
              weakness intersecting a circular exca-
              vation non-diametrically.
                                        The limiting condition for slip under this state of stress is
                                                                       =   n tan

                                        or, introducing equation 7.4,
                                                                                2
                                                              

 sin 
 cos 
 =   

 cos 
 tan          (7.5)
                                        or
                                                                    tan 
 = tan

                                          Thus if 
 =  , the condition for slip is satisfied on the plane of weakness. (This
                                        conclusion could have been established by noting that the resultant stress, in this case
                                          

 , is constrained to act within the angle   to the normal to the plane.) It is observed
                                        that the sense of slip, defined by the sense of the shear stress, involves outward
                                        displacement of the upper (hanging wall) surface of the fault relative to the lower
                                        surface. This implies boundary stresses lower than the elastic values in the crown of
                                        the opening. A prudent design response would anticipate the generation of subvertical
                                        tension fractures in the crown.
                                          The equilibrium state of stress at the boundary-plane of weakness intersection can
                                        be established from equation 7.5, which may be rewritten in the form

                                                                     sin(
 −  )
                                                                    

        = 0
                                                                       cos
                                        For 
 >  , this condition can be satisfied only if   

 = 0. Thus the regions near the
                                        intersection of the opening and the plane of weakness are either de-stressed, or at low
                                        confining stress. They may be expected to be areas from which loosening of rock may
                                        commence, and therefore deserve special attention in support design.

                                        Case 4.  (Figure 7.9) The problem illustrated in Figure 7.9a is introduced as a simple
                                        example of an arbitrarily inclined plane of weakness intersecting an opening. The
                                        far-field stresses are defined by components p (vertical) and 0.5p (horizontal). For
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