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Gold Science and Technology ›› 2021, Vol. 29 ›› Issue (2): 208-217.doi: 10.11872/j.issn.1005-2518.2021.02.143

• Mining Technology and Mine Management • Previous Articles    

Particle Flow Simulation on Influence of Joint Roughness Coefficient on Stress Wave Propagation and Specimens Failure

Weihua WANG1(),Jie LUO1(),Tian LIU2,Zhenyu HAN3   

  1. 1.School of Resource and Safety Engineering,Central South University,Changsha 410083,Hunan,China
    2.City Investment & Operation Co. ,Ltd. ,of China Construction Third Engineering Bureau,Wuhan 430073,Hubei,China
    3.School of Civil Engineering,Southeast University,Nanjing 210096,Jiangsu,China
  • Received:2020-08-03 Revised:2020-10-15 Online:2021-04-30 Published:2021-05-28
  • Contact: Jie LUO E-mail:50973993@qq.com;954433950@qq.com

Abstract:

In order to study the effect of joint roughness coefficient(JRC) on stress wave propagation and the mechanism of failure of rough joint rock specimens under stress wave action,a numerical model of particle flow code in a split Hopkinson pressure bar(SHPB) system was established by using PFC2D,a numerical analysis software based on discrete element method. Based on the existing SHPB physical test,the microcosmic parameters of joint rock specimens were demarcated. By comparing the waveforms of incidence,transmission and reflection generated by physical test and numerical simulation,the microscopic parameters were adjusted until the waveforms were basically the same,so that the correctness of the numerical model was verified. The numerical model was used to study the influence of JRC on stress wave propagation under low impact load and the microcosmic crack propagation and failure mechanism of joint rock specimens with different morphology under high impact load. In addition,the stress balance at both ends of the specimen under low impact load was analyzed by using the stress balance factor and the stress variation with time at the incident end and transmission end of the specimen. The typical stages of stress change at both ends of joint rock specimen and complete specimen in numerical impact test were compared and analyzed to explain the delayed effect of stress wave on joint surface and the effect of joint roughness on the increase of stress at the incident end. The results show that the presence of joint surface can reduce the transmission coefficient of stress wave,and the larger the JRC value of joint rock specimen is,the smaller the transmission coefficient is,and the stronger the reflected wave of the joint surface is,the more obvious the effect of stress growth slowing down at the incident end of the specimen is. Under impact load,the crack initiation occurs at the joint surface and spread rapidly to the whole part of the specimen,especially the end surface of the specimen,most of the cracks are formed in the post-peak stage,and tensile cracks are dominant. The rougher the joint surface is,the lower the dynamic strength is,the more easily the specimen is destroyed and the more cracks are produced.

Key words: SHPB, PFC, numerical simulation, JRC, stress wave propagation, transmission coefficient

CLC Number: 

  • TU455

Fig.1

Particle flow model of SHPB system"

Table 1

Mesoscopic parameters of particle flow model of SHPB system"

参数数值参数数值
颗粒半径/mm0.9~3.0切向接触刚度/(N·m-12.45×1011
孔隙率0.12颗粒密度/(kg·m-37 894.7
法向接触刚度/(N·m-16.86×1011法/切向黏结强度/MPa1×10100

Fig.2

Comparison of incident wave between physical test and numerical simulation"

Table 2

Mesoscopic parameters of intact rock specimens model"

颗粒参数数值平行黏结参数数值
弹性模量/GPa8.0弹性模量/GPa8.0
刚度比2.0刚度比2.0
摩擦因数0.4法向强度/MPa60±5
最大半径/mm4.5切向强度/MPa48±5
最小半径/mm0.3半径乘数1.0
密度/(kg·m-32 710.4阻尼0.05

Fig.3

Comparison of the waveform results between the numerical and physical tests of intact rock specimens"

Table 3

Mesoscopic parameters of joint rock specimens model"

SJ模型参数数值
单位法向刚度/(GPa·m-11 000
单位切向刚度/(GPa·m-1500
摩擦因数0.5
抗拉强度、内聚力/MPa0

Fig.4

Comparison of the waveform results between the numerical and physical tests of joint rock specimens"

Fig.5

Particle flow model diagram of joint rock specimens with different JRC values"

Fig.6

Stress balance diagram at both ends of intact rock specimens and joint rock specimens"

Fig.7

Stress-time curves of intact rock specimens and different joint rock specimens"

Table 4

Transmission coefficient of joint rock specimens under numerical impact tests"

试样类别入射应力/MPa透射应力/MPa透射系数
完整试样52.1532.700.627
JRC4~652.1531.300.600
JRC8~1052.1531.020.595
JRC12~1452.1530.340.582
JRC16~1852.1529.200.560

Table 5

Statistics of crack number of joint rock specimens with different JRC values"

节理试样峰值裂纹数/个最终裂纹数/个
剪切裂纹张拉裂纹总裂纹剪切裂纹

张拉

裂纹

总裂纹
JRC4~61222053274121 6382 050
JRC8~101171622794221 7562 172
JRC12~141051592644361 7732 209
JRC16~18811121934561 9212 377

Fig.8

Variation diagram of stress and number of cracks of joint rock specimens versus time"

Fig.9

Cracks distribution and force chain diagram of joint rock specimens at different time"

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