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Fracture evolution during rockburst under true-triaxial loading using acoustic emission monitoring

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Abstract

This paper investigates the fracture evolution during rockbursts of granodiorite and basalt that appeared to be representatives of two different rockburst modes under true-triaxial loading using acoustic emission (AE) analysis. In the experiments, with the macroscale ejection and failure features captured and presented by the high-speed video imaging and failed specimens, the inside micro- or meso-scale fracturing was detected and analyzed in detail by AE in terms of intensity, temporal-spatial distribution, and mechanism. The experimental results and AE analyses show that the fracture evolution during rockburst (particularly in granodiorite) exhibits hierarchical characteristics: during early loading, small local microfractures developed progressively and stably mainly by tension and clustered preliminarily; around and after the point of the crack damage stress, large-scale fractures developed and coalesced rapidly and unstably with increasing shear mechanism, and nucleation zones significantly developed; upon rockburst failure, rocks near the free face buckled or fractured and ejected rapidly, and shear ruptures suddenly ran through. The findings help facilitate the rockburst prediction and control.

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This study is financially supported by the National Natural Science Foundation of China under Grant No. 51869003.

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Correspondence to Guoshao Su.

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Zhai, S., Su, G., Yin, S. et al. Fracture evolution during rockburst under true-triaxial loading using acoustic emission monitoring. Bull Eng Geol Environ 79, 4957–4974 (2020). https://doi.org/10.1007/s10064-020-01858-z

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  • DOI: https://doi.org/10.1007/s10064-020-01858-z

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