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10             Energy, mine stability, mine


                                        seismicity and rockbursts




                                        10.1  Mechanical relevance of energy changes

                                        The discussion in preceding chapters was concerned with the design of single, or
                                        mechanically isolated, excavations in different types of rock media. In all cases, a
                                        design objective was to achieve a static stress distribution, or a set of static forces on
                                        discontinuity-defined internal surfaces, which could be sustained by the constituent
                                        elements of the rock mass. This approach would be completely satisfactory if rock-
                                        bursts and similar dynamic events did not need to be considered in underground
                                        excavation design, or if the stress concentrations which occur around openings were
                                        achieved in a pseudo-static way. Seismic events and rockbursts are a pervasive prob-
                                        lem in mines which operate at high extraction ratios, and involve release and trans-
                                        mission of energy from the zone of influence of mining. Furthermore, in metallifer-
                                        ous mining, the development of mine excavations, for both access and ore produc-
                                        tion, frequently involves near-instantaneous generation of segments of the excavation
                                        surface. As observed in Chapter 1, the development of an underground opening is
                                        mechanically equivalent to application of a set of tractions over a surface repre-
                                        senting the excavation boundary. Thus, typical excavation development practice is
                                        represented mechanically by the impulsive application of these surface forces in the
                                        rock medium.
                                          Seismicity is the sound of rock slipping or cracking. A seismic event is a sudden
                                        episode of radiation of acoustic energy in ground waves induced by discontinuity
                                        slip or rock material fracture. A rockburst is the sudden displacement of rock, under
                                        seismic impulse, in the boundary of an excavation, causing substantial damage to
                                        it. Both seismic events and rockbursts involve unstable energy changes in the host
                                        rock mass, suggesting that an examination of energy changes during mining is fun-
                                        damental to understanding of these phenomena. In conventional solid mechanics, it
                                        is well known that impulsive loading of a structural member or component results
                                        in transient stresses greater than the final static stresses, and that the most effective
                                        means of determining transient stresses and deformations under impulsive loading
                                        is by consideration of the energy changes to which the component is subjected. In
                                        fact, the amount of energy that a component can store or dissipate is frequently an
                                        important criterion in mechanical design. A component which is operationally subject
                                        to rapid loading must be constructed to a specification which reflects its duty as a
                                        transient energy absorber. In the mining context, it is reasonable to propose that rock
                                        around mine excavations will be subject, during development, to transient stresses
                                        exceeding the equilibrium static stresses, due to rapid application of surface tractions.
                                        It is thus inferred that both rockbursts and these transient effects may be best studied
                                        through methods which account for energy changes in the system.
                                          As observed later, energy changes in a mine domain arise from generation and
                                        displacement of excavation surfaces and energy redistribution accompanying seis-
                                        mic events. Because mine development practice frequently employs drill and blast


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