An Experimental Study of Effect of High Temperature on the Permeability Evolution and Failure Response of Granite Under
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ORIGINAL PAPER
An Experimental Study of Effect of High Temperature on the Permeability Evolution and Failure Response of Granite Under Triaxial Compression Sheng‑Qi Yang1 · Wen‑Ling Tian1 · Derek Elsworth2 · Jian‑Guo Wang1 · Li‑Feng Fan3 Received: 15 June 2019 / Accepted: 19 September 2019 © Springer-Verlag GmbH Austria, part of Springer Nature 2019
Abstract Granite is a viable host for deep nuclear waste disposal because its low permeability and high strength enable the stable and safe operation of the repository. We examined the evolution of the permeability and triaxial mechanical behaviour of granite after high-temperature treatment. First, the effect of the high temperature on the physical behaviour and permeability evolution of granite was analysed in detail. The mass, P-wave velocity, and thermal conductivity of granite decrease, but the volume increases with increasing temperature. The permeability of intact granite increases by four orders of magnitude as the cycled temperature increases from 25 to 800 °C. Subsequently, the effect of high temperature on the triaxial deformation and acoustic emission (AE) behaviour of granite was investigated. Under uniaxial compression at T ≤ 300 °C, the stress decreases before the peak strength is reached, corresponding to a significant AE event, which is due to the development of multiple splitting tensile fractures along the loading direction. At T ≥ 450 °C, AE event is observed once a minor stress is applied, which results from failure is controlled by thermally induced cracks. However, under triaxial compression, the temperature has little effect on the AE characteristics. The granite fails along the shear fracture plane, which becomes wider with increasing confining pressure. At T ≥ 600 °C, it is easier to form intragranular cracks and the stress quickly decreases after the peak strength is reached. The shear plane is smoother under high confining pressure. Third, the effect of high temperature on the peak strength and crack damage threshold of granite was further analysed. Generally, under uniaxial compression, the peak strength and crack damage threshold first remain relatively constant at T ≤ 300 °C, begin to decrease at T = 450 °C, and decrease more rapidly at T = 600 °C. The confining pressure notably reduces the effect of the temperature on the peak strength and crack damage threshold. Finally, the effect and mechanism of high temperature on the triaxial strength parameters of granite were further discussed. At T ≤ 300 °C, thermally induced cracks are not notable and the temperature has little effect on the strength. At 450 °C≤ T ≤ 600 °C, thermally induced cracks are more notable and the temperature has a significant effect on the strength behaviour. Because of the thermal stress released by thermal macrocrack formation, the continuous increase in the temperature has little impact on strength. Keywords Granite · High temperature · Permeability · Peak strength · Triaxial compression
* Sheng‑Qi Yang [email protected] 1
State Key Laboratory for Geomec
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