岩土力学 ›› 2024, Vol. 45 ›› Issue (5): 1284-1296.doi: 10.16285/j.rsm.2023.1610

• 基础理论与实验研究 • 上一篇    下一篇

裂隙砂岩应变场演化与超声时移衰减特征研究

张朝俊1,吴顺川1, 2, 3,储超群1,庞瑞1   

  1. 1. 北京科技大学 金属矿山高效开采与安全教育部重点实验室,北京 100083;2. 昆明理工大学 国土资源工程学院,云南 昆明 650093; 3. 自然资源部高原山地地质灾害预报预警与生态保护修复重点实验室,云南 昆明 650093
  • 收稿日期:2023-10-26 接受日期:2024-01-31 出版日期:2024-05-11 发布日期:2024-05-07
  • 通讯作者: 吴顺川,男,1969年生,博士,教授,主要从事岩土工程、采矿工程等方面的教学与研究工作。E-mail:wushunchuan@ustb.edu.cn
  • 作者简介:张朝俊,男,1994年生,博士研究生,主要从事岩石力学和声发射监测等方面的研究。E-mail:chaojun_ustb@163.com
  • 基金资助:
    国家自然科学基金(No. 51934003);云南省重大科技项目(No. 202202AG050014)

Strain field evolution and ultrasonic time-lapse attenuation characteristics of fractured sandstone

ZHANG Chao-jun1, WU Shun-chuan1, 2, 3, CHU Chao-qun1, PANG Rui1   

  1. 1. Key Laboratory of Ministry of Education for Efficient Mining and Safety of Metal Mine, University of Science and Technology Beijing, Beijing 100083, China; 2. Faculty of Land Resources Engineering, Kunming University of Science and Technology, Kunming, Yunnan 650093, China; 3. Key Laboratory of Geohazard Forecast and Geoecological Restoration in Plateau Mountainous Area, Ministry of Natural Resources of the People’s Republic of China, Kunming, Yunnan 650093, China
  • Received:2023-10-26 Accepted:2024-01-31 Online:2024-05-11 Published:2024-05-07
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (51934003) and the Yunnan Major Scientific and Technological Projects (202202AG050014).

摘要: 微裂纹萌生、扩展和聚结模式的识别是研究岩体灾害孕育演化过程的基础。为探究裂隙岩石微裂纹发育过程及机制,采用主动超声测量和数字图像相关(digital image correlation,简称DIC)技术同步监测单轴压缩下预制裂隙砂岩的损伤破裂过程,分析了表面应变场演化及超声衰减特征。结果表明:小倾角预制裂隙尖端的局部拉应力集中利于裂纹更早萌生;随裂隙倾角增加,预制裂隙试样由较为稳定的渐进性破裂转变为突发性破坏,其脆性特征也更明显,表面应变场可实时追踪裂纹的萌生和扩展。P波波速、振幅谱和超声振幅的衰减与微裂纹的发育和宏观裂纹的形成密切相关,可将超声波主频的明显衰减视为宏观裂纹形成的直接证据;不同射线路径P波速度及振幅衰减的差异,是轴向应力和预制裂隙诱导损伤累积各向异性的结果。此外,采用改进谱比法分析了超声衰减的时移特征,发现超声波衰减比P波波速对岩石介质中微裂纹的发育更敏感,进一步对比发现超声振幅、表面应变、P波波速对岩石损伤识别的敏感性依次降低。该研究结果表明,主动超声衰减和DIC表面应变同步监测是识别和量化岩石损伤和裂纹扩展先兆信息的有力工具。

关键词: 裂纹扩展, 主动超声监测, 衰减, 数字图像相关, 应变场演化

Abstract: Identification of microcrack initiation, propagation and coalescence patterns is fundamental to the study of the development and evolution process of rock mass disasters. In order to explore the development process and mechanism of microcrack in fractured rock, the active ultrasonic measurement and digital image correlation technology (DIC) were used to simultaneously monitor the damage and fracture process of sandstone containing prefabricated fissure under uniaxial compression, and the surface strain field evolution and ultrasonic attenuation characteristics were analyzed. The results show that the local tensile stress concentration at the tip of the prefabricated fissure with a small inclination angle is conducive to earlier crack initiation. As the fissure inclination angle increases, the specimen containing prefabricated fissure changes from a relatively stable progressive rupture to a sudden failure, and its brittleness characteristics become more obvious. The surface strain field can track the initiation and propagation of crack in real time. The attenuation of P-wave velocity, amplitude spectrum and ultrasonic amplitude is closely related to the development of microcracks and the formation of macrocracks. The obvious attenuation of dominant frequency of ultrasonic waves can be regarded as direct evidence for the formation of macrocracks. The differences in P-wave velocity and amplitude attenuation in different ray paths are the results of anisotropy in the accumulation of damage induced by axial stress and prefabricated fissure. In addition, the improved spectral ratio method was used to analyze the time-lapse characteristics of ultrasonic attenuation, and it was found that the ultrasonic attenuation is more sensitive to the development of microcracks in rock media than P-wave velocity does. Further comparison found that the sensitivity of ultrasonic amplitude, surface strain, and P-wave velocity to rock damage identification decreased in order. The results of this study demonstrate that the active ultrasonic attenuation and DIC surface strain simultaneous monitoring are powerful tools for identifying and quantifying precursor information of rock damage and crack propagation.

Key words: crack propagation, active ultrasonic monitoring, attenuation, digital image correlation (DIC), strain field evolution

中图分类号: TU 452
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