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9       Excavation design in


                                        blocky rock




                                        9.1  Design factors

                                        A blocky or block-jointed rock mass presents a more complex design problem than the
                                        cases considered previously. The complexity arises from either the number (greater
                                        than two) of joint sets which define the degree of discontinuity of the medium, or the
                                        presence of a discrete structural feature transgressing such a simply jointed system
                                        as a cross-jointed, stratified mass. The condition that arises in these types of rock
                                        masses is the generation of discrete rock blocks, of various geometries defined by
                                        the natural fracture surfaces and the excavation surface, as illustrated in the simple
                                        schematic of Figure 9.1. Because the blocks exist in the immediate boundary of an
                                        excavation whose surface has been subject to the removal of support forces by the
                                        mining operation, uncontrolled displacement of a single block or collapse of the block
                                        assembly is possible in the prevailing gravitational and local stress fields.
                                          The issues to consider in the design of an opening in a blocky medium are a natural
                                        extension of those proposed for the structurally simpler media considered previously.
                                        That is, it is necessary initially to determine the likelihood of induced fracture in the
                                        rock mass, in the total stress field after mining. For continuous features, such as faults
                                        or bedding planes which persist over dimensions exceeding those of the excavation,
                                        it is necessary to examine the possibility and consequences of slip under excessive
                                        shear stress. Also, since joints have effectively zero tensile strength, a jointed rock
                                        mass is unequivocally a no-tension medium. Any part of a jointed or blocky medium
                                        which is notionally subject to tensile stress will, in practice, de-stress. The process
                                        of de-stressing a discontinuum implies loss of control, and possibly local collapse of

              Figure 9.1  Generation of a discrete
              prism in the crown of an excavation
              by the surfaces of defined geological
              features and the excavation boundary.





















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