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Dynamic response of rock mass during split Hopkinson pressure bar test: numerical simulation utilizing distinct element method

机译:霍普金森压杆试验中岩体的动力响应:采用离散元法的数值模拟

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摘要

Dynamic responses of rock mass subject to high strain rate loadings by Split Hopkinson PressurernBar (SHPB) tests were analyzed utilizing distinct element method in the present paper. In order to investigaternthe discontinuum of the rock mass, a numerical SHPB test model based on two-dimensional ParticlernFlow Code (PFC2D) was established. Two approaches with regular and random assemblies for incident andrntransmitted bars were compared to account for dispersion caused by inertial effect. Additionally, the relationshipsrnbetween strain rate and peak strength were studied and the rate-sensitive behaviors were analyzed. Therndistinct element method implemented in Particle Flow Code provides an effective approach to observe microcracksrnevolution, failure process and stress wave propagation; this model also can be extended to higher strainrnrate tests such as more than 103, 104 and so on. Furthermore, the effects of joint parameters such as locations,rndirections, contact areas, as well as stiffness, are investigated and attempts are made to shed light on macroresponsernwith respect to discontinuum of rock mass, the results identify that the joints are closely related tornfailure modes, stress wave propagation and dynamic response of rock mass.
机译:本文采用离散元分析方法,通过Split Hopkinson PressurernBar(SHPB)试验对岩体在高应变速率荷载下的动力响应进行了分析。为了研究岩体的不连续性,建立了基于二维粒子流码(PFC2D)的SHPB数值试验模型。比较了入射棒和透射棒的两种常规和随机装配方法,以解决惯性效应引起的色散。此外,研究了应变速率和峰值强度之间的关系,并分析了速率敏感行为。 《粒子流法》中实现的“独特元素法”为观察微裂纹的演化,破坏过程和应力波的传播提供了一种有效的方法。该模型还可以扩展到更高的应变率测试,例如超过103、104等。此外,研究了节理参数(如位置,方向,接触面积以及刚度)的影响,并尝试揭示了与岩体不连续性有关的宏观响应,结果表明节理与节理模式密切相关。 ,应力波的传播和岩体的动力响应。

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  • 来源
  • 会议地点 Wuhan(CN)
  • 作者

    X. F. Li; H.B. Li; J.C. Li; X. Xia;

  • 作者单位

    Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, China;

    Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, China;

    Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, China;

    Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan, China;

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  • 正文语种 eng
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