Page 391 - Rock Mechanics For Underground Mining
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FIELD OBSERVATIONS OF PILLAR PERFORMANCE


















              Figure 13.4 Redistribution of stress
              in the axial direction of a pillar accom-
              panying stope development.


                                          The structural response of a pillar to mining-induced load is determined by the rock
                                        material properties, the geological structure, the absolute and relative dimensions of
                                        the pillar and the nature of surface constraints applied to the pillar by the country
                                        rock. Three main modes of pillar behaviour under stresses approaching the rock mass
                                        strength have been recognised, which may be reproduced qualitatively by laboratory
                                        tests on model pillars in a displacement controlled testing machine. These failure
                                        modes are illustrated in Figure 13.5.
                                          In relatively massive rock, the most obvious sign of pillar stressing involves spalling
                                        from the pillar surfaces, as illustrated in Figure 13.5a. Fretting or necking of the pillar
                                        occurs. In a detailed study, Lunder and Pakalnis (1997) described the progressive
                                        stages of degradation of a pillar in terms of the modes of deformation represented
                                        in Figure 13.6. Although the initial signs of rock stress may be local shear failure,
                                        associated with the re-entrant geometry represented in Figure 13.6a, the formation
                                        of surface spalls illustrated in Figure 13.6b is a more extensive failure indicative of
                                        states of stress satisfying the conditions for fracture initiation and rock damage in
                                        a significant volume of the pillar. In this condition, the pillar is partially failed, but
                                        the core of the pillar is intact, in terms of the model of rock fracture and failure
                                        discussed in Chapter 4. Higher states of stress lead to damage accumulation through
                                        internal crack initiation and extension, and interaction of the network of cracks, as
                                        shown in Figure 13.6c. When friction between the fully developed crack population
                                        is fully mobilized, the pillar is at peak strength, and mechanically is at a state of
                                        failure, illustrated in Figure 13.6d. This model of the progressive evolution of pillar
                                        failure is consistent with the micromechanical modelling of pillar loading reported
                                        by Diederichs (2002), in which progressive crack formation and localisation of shear
                                        strain was observed.
                                          The effect of pillar relative dimensions on failure mode is illustrated in Figure 13.5b.
                                        For regularly jointed orebody rock, a high pillar height/width ratio may favour the
                                        formation of inclined shear fractures transecting the pillar. There are clearly kinematic
                                        factors promoting the development of penetrative, localised shear zones of this type.
                                        Their occurrence has been reproduced in model tests by Brown (1970), under the
                                        geometric conditions prescribed above.
                                          The third major mode of pillar response is expressed in an orebody with highly
                                        deformable planes of weakness forming the interfaces between the pillar and the
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