The strain field development prior to failure of a uniaxially compressed marble plate with an inclined central slot is studied experimentally. The whole process of failure development of the specimen is directly monitored and photographed by back illumination. The displacement fields at different stages are recorded with the moire technique and corresponding strain fields are calculated. Test results show that when the specimen is loaded to a certain level, its strain will become concentrated in relatively narrow belts which are potential locations of the impending ultimate failure. The failure process can be roughly divided into five stages: (1) initiation and propagation of primary forward tensile cracks, also known as wing cracks, (2) initiation and propagation of secondary forward tensile cracks, (3) initiation and intensification of shear belts starting from the slot tips and extending in an “X” form toward the four comers of the specimen, (4) initiation and propagation of backward tensile cracks, and finally (5) the ultimate failure. The forward tensile cracks are similar to those previously described in the literature ∗∗ but the backward cracks run in an opposite direction. In this study, four types of ultimate failure are identified: (i) axial splitting along tensile cracks, (ii) shear fracture along shear belts having a similar trend as the slot, (iii) shear fracture along shear belts sub-conjugate to the slot, and (iv) various combinations of splitting and shear fracture. Specimens with infill mortar material in the slot are also tested, where it is found that the mortar suppresses axial splitting. The geophysical and seismological implications of the test result are also briefly discussed.
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