砂岩破坏过程能量释放及前兆特征Energy release and precursory characteristics during sandstone failure process
孔存芝,周智奇,孙涛,姜玉杰,南骁聪,朱星,曾鹏
摘要(Abstract):
岩体原始裂隙的扩展、贯通是导致岩体失稳破坏的重要原因。基于此,开展了含不同角度裂缝的细砂岩试验研究。采用MTS刚性压力机对其进行加载,利用声发射监测系统对加载全过程进行实时探测,对其损伤过程岩体耗散能、弹性应变能、损伤变量及声发射信号频率、能量特征及失稳破坏前兆信息进行研究。结果表明:(1)在耗散能的驱动下岩体发生损伤破坏,宏观裂纹的形成相比微裂纹的孕育、萌生需要更大的耗散能。在宏观裂纹形成时岩体储能能力丧失,弹性应变能急剧下降,损伤达到最大。(2)当细砂岩体产生小尺度损伤破裂时会伴随着高频、低能的声发射信号,当岩体裂纹扩展、贯通形成大尺度宏观裂纹时会伴随低频、高能的声发射信号产生。可将低频、高能的声发射信号作为岩体破坏的前兆信号。(3)声发射累积能量、声发射累积振铃计数的变异系数在细砂岩体临近破坏时具有响应特征,表现为变异系数的大幅突增,大幅突增点出现于岩石破坏时间的73%以上、破坏应力的60%以上,具有较好的时效性,且出现点大致位于弹性阶段末至不可逆的塑性变形阶段具有一定的物理意义,可将其变异系数产生明显增大作为岩体损伤破坏向失稳破坏转变的前兆信息。该研究可为隧道、采矿等变形历程短、突发性强的工程监测预警提供有益参考。
关键词(KeyWords): 能量释放;声发射;能量-频率特征;变异系数;前兆信息
基金项目(Foundation): 山东省交通运输厅科技计划(2019B38);; 四川省科技计划项目(2019YJ0534)
作者(Author): 孔存芝,周智奇,孙涛,姜玉杰,南骁聪,朱星,曾鹏
DOI: 10.13928/j.cnki.wrahe.2022.06.015
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