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15             Longwall and caving mining


                                        methods




                                        15.1  Classification of longwall and caving mining methods

                                        The essential geomechanical features of longwall and caving methods of mining were
                                        outlined in Chapter 12. Longwall and caving methods are distinguished from other
                                        mining methods by the fact that the near-field rock undergoes large displacements
                                        so that mined voids become self-filling. In caving methods, the far-field rock may
                                        also undergo large displacements. In increasing order of magnitude of country rock
                                        displacement, and in decreasing order of strain energy stored in the near-field rock, the
                                        basic mining methods to be considered in the present category are longwall mining
                                        in hard rock, longwall coal mining, sublevel caving and block caving.
                                          In this chapter, the geomechanics issues involved in each of these methods of
                                        mining will be discussed in turn. If a relevant issue has been dealt with elsewhere, the
                                        discussion will not be repeated, but a cross reference will be given. One of the major
                                        geomechanics concerns in longwall and caving methods, mining-induced surface
                                        subsidence, will not be considered here, but will be the subject of Chapter 16.



                                        15.2 Longwall mining in hard rock

                                        15.2.1 Basic geomechanics considerations
                                        As was noted in section 12.4.6, longwall methods are used to mine narrow, flat-
                                        dipping, metalliferous orebodies of large areal extent. The near-field rock is usually
                                        strong, and mining often takes place at considerable depth where in situ stresses are
                                        high. The deep-level mines of South Africa provide the classic example of these
                                        conditions. The key elements of longwall mining in hard rock are illustrated in
                                        Figure 12.11. In the form of the method illustrated in Figure 12.11, it is likely that
                                        the down-dip spans of the longwalls would be limited by the use of regularly spaced
                                        strike pillars. Vieira et al. (2001) describe one such example in which the strike pillars
                                        are 40 m wide with a centre-to-centre spacing of 280 m. There are also a number of
                                        variants of the method in which dip pillars are used for regional support (see section
                                        15.2.2) and to bracket faults and dykes.
                                          The basic geomechanical objective of the mining and support systems used in
                                        this case is to preserve the pseudo-continuous behaviour of the near-field rock. This
                                        pseudo-continuous behaviour may be disturbed by two influences. First, natural or
                                        mining-induced discontinuities in the rock mass as illustrated in Figure 15.1 may
                                        isolate rock blocks that become free to fall from the hangingwall. This condition
                                        is exacerbated by the tendency for tensile boundary stresses to be induced in the
                                        near-field rock above the mined-out void. Structurally controlled instabilities and
                                        instabilities associated with mining induced fracturing in stope backs have long been
                                        experienced in the deep-level gold mines and the shallower platinum mines of South
                                        Africa (e.g. Heunis, 1980, Roberts and Urcan, 2002, Ryder and Jager, 2002, Stone,
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