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單軸與雙軸加載條件下裂隙砂巖破壞行為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: 為探究雙裂隙巖石在不同應力條件下的破壞前兆特征,在立方體砂巖試件中預制裂隙,選擇平行雙裂隙和共線雙裂隙兩種構型. 分別對預制裂隙砂巖進行單軸和雙軸壓縮試驗,利用聲發射和數字圖像技術分別對巖石內部裂隙發育信息和巖石表面變形信息進行監測. 借助聲發射事件率函數和砂巖最大主應變場變化研究了砂巖的裂隙發育及破壞過程,結果顯示砂巖呈現出漸進式破壞特征,破壞模式多是劈裂破壞占主導,并伴隨壓剪破壞,破壞形態多呈現出最大主應力方向的偏“I”型破壞,偶有呈現出“X”型破壞. 為了表征試樣的破壞前兆信息,引入了縱向應變場變異系數和縱向應變場標準差描述巖石破壞前的DIC前兆信息,借助聲發射振鈴計數描述巖石破壞前的AE前兆信息. 借助熵權法,確定了AE前兆指標和DIC應變前兆指標的權重,得到了能反映巖石內部和表面信息的融合指標AD. 結果表明,融合指標的前兆預警效果在單軸加載情況下預警時間不具有明顯優勢,但具有較明顯的前兆特征,而在雙軸加載情況下,不僅具有預警時間的優勢,還具有明顯的前兆特征.

     

    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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