循环冲击作用下高水压岩石动态强度的劣化特性

Study on dynamic strength degradation characteristics of rock under high water pressure and cyclic impact loading

  • 摘要: 深部高水压岩体工程涌突水灾害是水压力、地应力和多次爆破动载荷共同作用的结果。为研究高水压高应力岩石在多次爆破动载荷作用过程中的动态疲劳力学性能,采用自主研制的高水压高应力岩石动力学测试系统,对具有不同水压力和轴向静应力的红砂岩进行循环冲击试验,分析岩石动态应力-应变曲线形状演变、峰值应力劣化的规律,构建岩石动态峰值应力随水压力和轴向静应力变化的劣化模型。通过建立岩石动态峰值应力与平均应变率的经验关系,研究循环冲击过程中岩石动态峰值应力随应变率的劣化效应,探索高水压高应力岩石动态疲劳力学性能的劣化机理。研究结果表明,岩石动态峰值应力随循环冲击次数的增加呈指数函数下降。在相同水压力下,总循环冲击次数随轴向静应力的增大而减少;在相同轴向静应力下,总循环冲击次数随水压力的增大而增大。动态峰值应力和平均应变率呈负线性关系,动态峰值应力劣化系数的绝对值在水压力为定值时随轴向静应力的增大呈先增大后减小的趋势;固定轴向静应力时劣化系数的绝对值随水压力变化不明显。水压力在循环冲击荷载过程中主要表现为作用于裂隙尖端的“水楔效应”等弱化作用,以及外部压力水的束缚作用和Stefan效应、弯液面效应等共同组成的强化作用,2种作用共同影响岩石动态疲劳力学性能。

     

    Abstract: Water inrush disasters in deep rock mass engineering result from the coupled actions of hydrostatic pressure, in-situ stress, and repetitive dynamic loads from blasting. In order to study the dynamic fatigue mechanical properties of rock under these conditions, cyclic impact tests were performed on red sandstone with varying water pressures and axial static stresses using an independently developed high water pressure and high stress rock dynamics testing system. The evolution of dynamic stress-strain curves and the laws of peak stress degradation were analyzed, and a degradation model for the rock’s dynamic peak stress under hydro-mechanical coupling was constructed. By establishing an empirical relationship between the dynamic peak stress and the average strain rate, the study investigated the degradation effect of the peak stress on the strain rate during the cyclic impact process and explored the underlying degradation mechanisms. The results showed that the dynamic peak rock stress decreased exponentially with the number of cyclic impacts. At a constant water pressure, the total number of cyclic impacts was negatively correlated with the axial static stress; conversely, at a constant axial static stress, the total number of cyclic impacts increased with increasing water pressure. A negative linear correlation was observed between the dynamic peak stress and the average strain rate. The absolute value of the dynamic peak stress degradation coefficient initially increased and then decreased with axial static stress at a fixed water pressure, whereas it remained relatively insensitive to water pressure at a fixed axial static stress. During cyclic impact loading, water pressure primarily exerted weakening effects such as the “water wedge effect” at crack tips, as well as strengthening effects composed of the confining effect of external water pressure, the Stefan effect, and the Meniscus effect. The competition between these two effects collectively governed the dynamic fatigue mechanical properties of the rock.

     

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