单轴与双轴加载条件下裂隙砂岩破坏行为及前兆特征融合研究

Multimodal precursor signature integration with failure analysis for fractured sandstone under uniaxial and biaxial compression

  • 摘要: 为探究双裂隙岩石在不同应力条件下的破坏前兆特征,在立方体砂岩试件中预制裂隙,选择平行双裂隙和共线双裂隙两种构型. 分别对预制裂隙砂岩进行单轴和双轴压缩试验,利用声发射和数字图像技术分别对岩石内部裂隙发育信息和岩石表面变形信息进行监测. 借助声发射事件率函数和砂岩最大主应变场变化研究了砂岩的裂隙发育及破坏过程,结果显示砂岩呈现出渐进式破坏特征,破坏模式多是劈裂破坏占主导,并伴随压剪破坏,破坏形态多呈现出最大主应力方向的偏“I”型破坏,偶有呈现出“X”型破坏. 为了表征试样的破坏前兆信息,引入了纵向应变场变异系数和纵向应变场标准差描述岩石破坏前的DIC前兆信息,借助声发射振铃计数描述岩石破坏前的AE前兆信息. 借助熵权法,确定了AE前兆指标和DIC应变前兆指标的权重,得到了能反映岩石内部和表面信息的融合指标AD. 结果表明,融合指标的前兆预警效果在单轴加载情况下预警时间不具有明显优势,但具有较明显的前兆特征,而在双轴加载情况下,不仅具有预警时间的优势,还具有明显的前兆特征.

     

    Abstract: In this study, cracks were prefabricated in cubic sandstone specimens to investigate the precursor characteristics of fractured rocks under different stress conditions. Two forms of parallel and collinear cracks were made to represent different rock structural planes. Biaxial compression tests were conducted on prefabricated fractured sandstone under lateral pressures of 0, 5, and 10 MPa, respectively. Acoustic emission and digital imaging technologies were used to monitor the development of internal fractures and surface deformations of the rock. The development and process of rock fractures were studied using the acoustic emission event rate function and maximum principal strain field variation of sandstone. The results showed that sandstone exhibited progressive failure characteristics. The failure mode is mostly dominated by splitting failure, accompanied by compression shear failure, and the failure mode often presents a skewed “I” shape in the direction of the maximum principal stress, occasionally having an “X” shape. The confining pressure has a “reinforcing” effect on the strength of the rock, and as the confining pressure increases, the “reinforcing” effect becomes more significant; however, simultaneously, the stepwise trend of progressive rock failure decreases. In addition, a strong correlation exists between the acoustic emission event rate function and the variation of the principal strain field on the rock surface, and their joint analysis can effectively characterize the failure process of rocks. In the compaction stage, the acoustic emission event rate is extremely low. During the elastic and plastic stages, the acoustic emission event rate gradually increases and remains high. Notably, the primary strain field shows a trend of localization. In the failure stage, a localized band of the primary strain field is formed, and the acoustic emission event rate gradually and violently fluctuates. Along with the rapid development of rock fractures, the acoustic emission event rate suddenly increases. To characterize the precursor information of the sample, the coefficient variation (CV) and standard deviation (SD) of the longitudinal strain field were introduced to describe the precursor information of the digital image before rock failure, and the acoustic emission precursor information before rock failure was described using the acoustic emission ring count. Using the entropy weight method, the weights of the acoustic emission precursor and digital image strain precursor indices were determined, and a fusion index Acoustic emission and DIC (AD) that reflects the internal and surface information of the rock was obtained. The results showed that the fusion index does not have an advantage in warning time compared to the acoustic emission ringing count, longitudinal displacement field variation coefficient, and longitudinal displacement field variation SD, but exhibits more notable precursor characteristics under uniaxial loading. However, under biaxial loading, it has an advantage in warning time and exhibits more significant precursor characteristics. In engineering rock masses, rock failure is mostly in a state of biaxial stress. The findings of this study provide a reference for the selection of precursor parameters for engineering rock mass failure.

     

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