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Experimental Investigation on the Deformation, Strength, and Acoustic Emission Characteristics of Sandstone under True Triaxial Compression

机译:真三轴压缩作用下砂岩的变形,强度和声发射特性的实验研究

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The study of deformation, strength, and other mechanical characteristics of sandstone under true triaxial compression is significant for understanding failure mechanisms in rock and evaluating the stability of underground structures. Conventional and true triaxial compression tests for sandstone are conducted for different stress states in this study using the self-developed true triaxial electrohydraulic servo test system combined with acoustic emission (AE) testing. This study presents an in-depth and systematic investigation of deformation, strength, and AE characteristics. The results show significant differences in deformation, strength, and acoustic emission characteristics for the rock under conventional triaxial and true triaxial compression tests, respectively. The peak strength, axial strain, lateral strain, and incremental strain (in unstable crack growth stage) increase with increasing confining pressure under conventional triaxial compression, and the AE count gradually decreases while shear crack proportion gradually increases, indicating that increasing confining pressure gradually inhibits the shear slip effect along fractures, delays perforation of the rock shear fracture surface, and enhances the ability of the rock to withstand deformation and load. Under true triaxial compression, the peak strength increases and then decreases with increasing intermediate principal stress and the axial strain and lateral strain gradually decrease; besides, the lateral strain (expansion) of the rock is mainly in the minimum principal stress direction, and lateral expansion tends to decrease before increasing. AE events first weaken and then enhance with increasing , and the proportion of shear cracks increases first and then decreases, indicating that the confining pressure gradually changes from the shear slip effect that controls crack offset to the damage effect that promotes crack tension with increasing . In addition, the protective effect of confining pressure improves when increases.
机译:真正的三轴压缩作用下砂岩的变形,强度和其他力学特性的研究对于理解岩石的破坏机理和评估地下结构的稳定性具有重要意义。在这项研究中,使用自行开发的真三轴电液伺服测试系统与声发射(AE)测试相结合,针对不同的应力状态进行了常规和真三轴砂岩压缩测试。这项研究对变形,强度和AE特性进行了深入而系统的研究。结果表明,分别在常规三轴和真实三轴压缩试验下,岩石的变形,强度和声发射特性存在显着差异。在常规三轴压缩下,峰值强度,轴向应变,横向应变和增量应变(在不稳定的裂纹扩展阶段)随着围压的增加而增加,并且AE数量逐渐减少,而剪切裂纹比例逐渐增加,这表明围压的增加逐渐抑制了沿裂缝的剪切滑移效应,延迟了岩石剪切裂缝表面的射孔,并增强了岩石承受变形和载荷的能力。在真正的三轴压缩下,随着中间主应力的增加,峰值强度先增大后减小,轴向应变和横向应变逐渐减小。此外,岩石的侧向应变(膨胀)主要在最小主应力方向上,并且在增大之前,侧向膨胀趋于减小。 AE事件先减弱然后增强,然后增加,并且剪切裂缝的比例先增加然后减少,这表明围压从控制滑动偏移的剪切滑移效应逐渐变为增加裂缝应力的破坏效应。另外,围压的保护作用在增大时会提高。

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