Dynamic acoustic emission source localization and damage evolution analysis of rock under compressive loading

Longjun Dong , Shen Zhang , Longbin Yang , Daoyuan Sun , Jianqing Xiao , Hongwei Wang
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Abstract

Understanding the dynamic damage evolution of rock is crucial for ensuring underground engineering stability. However, traditional acoustic emission (AE) source localization methods that rely on pre-measured velocity models introduce significant errors under heterogeneous media evolution. This study uses a self-developed AE monitoring system to investigate dynamic AE source localization and damage evolution in rock subjected to compressive loading. AE sensors captured spatiotemporal acoustic signals while velocity field inversion was performed by traveltime tomography to track crack propagation across four loading stages: crack closure, elastic deformation, stable crack propagation, and unstable crack propagation. Results, as visualized in Section 4, demonstrate that the velocity field increases dominantly during the initial stages, then exhibits localized attenuation as damage accumulates. A velocity-free localization method simultaneously solves for event locations and effective velocities, eliminates dependence on pre-measured velocity models, and achieves high-precision AE localization. The deduced localization results align with the X-shaped shear failure pattern of the specimen. This combined localization and tomography approach provides a reliable tool for real-time characterization of rock damage evolution, advancing fracture mechanism analysis and engineering monitoring under complex conditions.
岩石压缩加载下动态声发射源定位与损伤演化分析
了解岩石的动态损伤演化过程对保证地下工程的稳定性至关重要。然而,传统的声发射(AE)震源定位方法依赖于预测速度模型,在非均质介质演化条件下存在较大误差。利用自主开发的声发射监测系统,研究岩石在压缩载荷作用下声发射源的动态定位和损伤演化过程。声发射传感器捕获时空声信号,同时通过行时断层扫描进行速度场反演,跟踪裂纹在四个加载阶段的扩展:裂纹闭合、弹性变形、稳定裂纹扩展和不稳定裂纹扩展。结果,如第4节所示,表明速度场在初始阶段主要增加,然后随着损伤的积累呈现局部衰减。无速度定位方法同时求解了事件位置和有效速度,消除了对预测速度模型的依赖,实现了高精度声发射定位。推导出的局部化结果与试件的x形剪切破坏模式一致。这种结合了定位和层析成像的方法为岩石损伤演化的实时表征提供了可靠的工具,推进了复杂条件下的断裂机制分析和工程监测。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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