三轴加载和卸载条件下细粒花岗岩破坏过程中的特征应力和应变前兆信息

Zhen Peng , Xing Su , Yuda Chen , Jianqiang Xia , Diyuan Li
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引用次数: 0

摘要

在地下工程中,开挖产生的卸载效应可能会对周围岩体造成不可逆转的严重破坏。本文对细粒花岗岩进行了常规三轴压缩(CTC)试验和三轴卸载约束压力(TUCP)试验,以研究其在卸载作用下的三轴压缩破坏过程。在裂缝体积应变(CVS)法的基础上,提出了裂缝轴向应变(CAS)法和裂缝径向面积应变(CRAS)法,以识别岩石破坏过程中的破坏前兆信息(包括应力阈值和裂缝连通阶段起始点的轴向应变)。CTC 试验结果表明,CAS 法识别的稳定裂缝扩展应力 σsd、不稳定裂缝扩展应力 σusd 和裂缝连通应力 σct 分别为峰值应力的 6%、74%-84% 和 86%-97%。对于 TUCP 案例,随着约束压力的增加,应力阈值、破坏时的轴向压力和裂纹连通阶段开始时的轴向应变都在增加,而裂纹连通阶段与整个卸载阶段的时间比却在减小。这表明细粒花岗岩在高约束压力下容易产生更多裂缝并导致突然破坏。此外,这种新方法还证明,径向裂缝面积应变的导数从稳定到突然增大或减小的转变点被定义为岩石破坏的前兆点。裂缝连接阶段起点的轴向应变结果与 AE 方法预测的结果非常接近,β1 不超过 11%。
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Characteristic stress and strain precursor information for fine-grained granite during failure process under triaxial loading and unloading conditions

The unloading effect by excavation may cause irreversible and severe damage to the surrounding rock masses in underground engineering. In this paper, both conventional triaxial compression (CTC) tests and triaxial unloading confining pressure (TUCP) tests were conducted on fine-grained granite to study its triaxial compression failure processes due to unloading. Based on the crack volumetric strain (CVS) method, the crack axial strain (CAS) method and crack radial area strain (CRAS) method were proposed to identify the failure precursor information (including stress thresholds and axial strain at the initiation point of crack connectivity stage) during the rock failure processes. The results of the CTC tests show that the stable crack development stress σsd, unstable crack development stress σusd, and crack connectivity stress σct identified by the CAS method are 6%, 74%–84%, and 86%–97% of the peak stress, respectively. For the TUCP cases, as the confining pressure increases, the stress thresholds, axial pressure at failure and axial strain at the start of the crack connectivity stage increase, while the time ratio of the crack connectivity stage to the entire unloading stage decreases. This indicates that fine-grained granite is prone to generate more cracks and leads to fail suddenly under high confining pressure. Furthermore, this new method demonstrates that the point at which the derivative of the radial crack area strain transitions from stable to a sudden increase or decrease is defined as the precursor point of rock failure. The results of axial strain at the starting point of the crack connectivity stage are very close to those predicted by the AE method, with β1 no more than 11%.

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