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王振伟, 马克, 田洪圆, 李全生. 煤岩体应力波传播规律及其影响因素的数值分析[J]. 煤炭科学技术, 2019, (6).
引用本文: 王振伟, 马克, 田洪圆, 李全生. 煤岩体应力波传播规律及其影响因素的数值分析[J]. 煤炭科学技术, 2019, (6).
WANG Zhenwei, MA Ke, TIAN Hongyuan, Li Quansheng. Numerical analysis of stress wave propagation law of coal and rockmass and its influencing factors[J]. COAL SCIENCE AND TECHNOLOGY, 2019, (6).
Citation: WANG Zhenwei, MA Ke, TIAN Hongyuan, Li Quansheng. Numerical analysis of stress wave propagation law of coal and rockmass and its influencing factors[J]. COAL SCIENCE AND TECHNOLOGY, 2019, (6).

煤岩体应力波传播规律及其影响因素的数值分析

Numerical analysis of stress wave propagation law of coal and rockmass and its influencing factors

  • 摘要: 大多数煤岩体存在不同程度的损伤,分布有大量裂隙,当应力波传播穿过裂隙时,会出现波速下降、能量衰减及时间延迟等现象。为了理清应力波通过煤岩体裂隙时间延迟的规律,并对其进行定量分析,反演煤岩体内部破坏程度,采用数值计算的方法,对应力波在含单个裂隙煤岩体内的传播规律进行了研究,分析了应力波过缝前、过缝中、过缝后的波形特征,和裂隙宽度、荷载参数及岩层参数对延时规律的影响。研究结果表明:应力波过缝延时与缝宽、密度和荷载周期等因素呈正相关,各因素的敏感性排序为:缝宽>弹性模量>岩层密度>荷载振幅>荷载周期。其中,缝宽引起的延迟时间是荷载周期的0.23倍。研究结果揭示了CDEM可以较好地模拟应力波在裂隙煤岩体内的传播规律。

     

    Abstract: Most of the rock masses have varying degrees of damage and there are a large number of cracks.When the stress waves propagate through the cracks, wave velocity, energy attenuation and time delay will occur.In order to clarify the time delay law of stress wave passing through the coal rock mass, and quantitatively analyze it, invert the internal damage degree of coal and rock mass, and use numerical calculation method to study the propagation law of stress wave in a single fractured coal rock.The waveform characteristics of the stress wave before, during and after the seam are analyzed, and the crack width, load parameters and delay parameters of the rock layer parameters are analyzed.The results showed that the stress wave time delay was positively related with the factors such as width, density and load cycle.The sensitivity order of the factors was:crack width>modulus of elasticity>rock density>load amplitude>load cycle.Among them, the delay time caused by crack width could be 0.23 times of the load cycle.The results reveal that the continuum-discontinuum element method program could well simulate the propagation of stress wave in the fractured rock.

     

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