1. 江西理工大学 资源与环境工程学院,江西,赣州,341000
2. 江西理工大学 江西省矿业工程重点实验室,江西,赣州,341000
3. 神华北电胜利能源有限公司,内蒙古 锡林浩特,026000
网络首发:2021-04-25,
纸质出版:2021
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赵奎, 冉珊瑚, 曾鹏, 等. 含水率对红砂岩特征应力及声发射特性的影响[J]. 岩土力学, 2021,42(4):899-908.
ZHAO Kui, RAN Shan-hu, ZENG Peng, et al. Effect of moisture content on characteristic stress and acoustic emission characteristics of red sandstone[J]. 2021, 42(4): 899-908.
赵奎, 冉珊瑚, 曾鹏, 等. 含水率对红砂岩特征应力及声发射特性的影响[J]. 岩土力学, 2021,42(4):899-908. DOI: 10.16285/j.rsm.2020.1201.
ZHAO Kui, RAN Shan-hu, ZENG Peng, et al. Effect of moisture content on characteristic stress and acoustic emission characteristics of red sandstone[J]. 2021, 42(4): 899-908. DOI: 10.16285/j.rsm.2020.1201.
为了探讨含水率对红砂岩特征应力及声发射响应特征的影响,利用RMT-150C岩石力学压力试验机和PCI-II AE win型声发射系统开展了不同含水率条件下红砂岩试件单轴压缩试验。对水侵蚀作用下红砂岩的物理力学参数及特征应力演化机制进行了分析,探究在不同含水率条件下声发射(宽、窄频带)时间序列模式的演化规律,同时基于累计声发射事件数与统计力学理论构建了红砂岩的损伤演化模型。试验结果表明:(1)P波波速随着含水率增加呈现先减小后增加的变化趋势,当含水饱和度达到临界值时,P波波速会降到最低值;(2)窄频带接收传感器接收的声发射信号与红砂岩内部颗粒间的摩擦作用息息相关,而宽频带接收传感器接收的声发射信号与红砂岩内部裂纹演化存在着内在联系;(3)水对声发射事件率(宽频带)在裂纹非稳定扩展阶段影响相对较为显著,对特征应力与强度的比值影响甚微,但对各阶段应变百分比作用效果相对较为明显,随着含水率的增加,红砂岩试件的失效模式由脆性破坏逐渐向延展性破坏转变;(4)随着含水率的增加,声发射事件率(窄频带)活跃期呈现后移的变化趋势,干燥、自然与饱和状态下岩石试件声发射模式分别为主震型、前震–主震–后震型和群震型;(5)基于声发射累计事件数(宽、窄频带)与统计力学理论构建的损伤演化模型可将不同含水率条件下红砂岩试件的损伤过程分为4个阶段:初始损伤阶段、损伤稳定发展阶段、损伤加速发展阶段及损伤破坏阶段。
In order to investigate the response law of moisture content to the characteristic stress and acoustic emission characteristics of red sandstone
the uniaxial compression tests of red sandstone under different moisture content conditions were conducted using RMT-150C rock mechanical pressure testing machine and PCI-Ⅱ AE win acoustic emission system. The physical and mechanical parameters and characteristic stress evolution mechanism of red sandstone under water erosion are analyzed
and the evolution law of acoustic emission (wide and narrow-band) time series mode under different moisture content conditions is also investigated. At the same time
the damage evolution model of red sandstone is constructed based on cumulative acoustic emission event number and statistical mechanics theory. The results show that: 1) The P-wave velocity decreases first and then increases with the increase of moisture content. When the water saturation reaches a critical value
the P-wave velocity will drop to the lowest value. 2) The acoustic emission signal received by the narrow-band receiving sensor is closely related to the friction between the particles in the red sandstone
and the acoustic emission signal received by the wide-band receiving sensor is intrinsically related to the evolution of the internal cracks in the red sandstone. 3) The moisture content has a significant effect on the acoustic emission event rate (wide-band) at the stage of unstable crack propagation
and has a minor effect on the ratio of characteristic stress to peak strength
but it has a relatively obvious effect on the strain percentage at each stage. With the increase of moisture content
the failure mode of red sandstone specimens gradually changes from brittle failure to ductile failure. 4) As the moisture content increases
a "backward" change trend can be observed for the active period of acoustic emission event rate (narrow-band)
and the acoustic emission modes of dry
natural
and saturated rock samples correspond to mass shocks
pre-main-later shocks and swarm shocks type
respectively. (5) According to the damage model based on the cumulative number of acoustic emission events (wide and narrow-band)
the damage process of red sandstone can be divided into four stages: initial damage stage
stable damage development stage
accelerated damage development stage and damage destruction stage.
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