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Microcrack Growth Behavior and CWFS Criterion Parameters Optimization of Granite with PFC

机译:PFC花岗岩的微裂纹生长行为和CWFS准则参数优化

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Based on the physical and mechanical parameters obtained in laboratory tests, along with the section scanning of granite specimens, a microgeometric model of the granite particles was established in the Particle Flow Code (PFC) programs. The loading codes were programed and adjusted using the Fish language to simulate both uniaxial and triaxial compression tests. The micromechanical behavior and the evolution of cracks from the microcosm to the macrocosm of the granite were obtained under different loading conditions based on the complete stress-strain curves, Acoustic Emission (AE) monitoring results and crack number obtained from the tests, and PFC simulation. On this basis, the Cohesion Weakening and Friction Strengthening (CWFS) criterion model parameters of the granite were optimized and verified using the stress-strain curves, the relationship between the cracks, friction energy and plastic strain, and Fast Lagrangian Analysis of Continua simulation. The optimized CWFS criterion parameters of initial cohesion, residual cohesion, initial friction angle, and residual friction angle, as well as the critical plastic strain epsilon(p)(c) and epsilon(p)(f) of the granite, are 23 MPa, 4.3 MPa, 0 degrees, 46.3 degrees, 0.0015, and 0.0037, respectively. This provides a scientific basis for the establishment of a rock constitutive model during the transfer from open pit to underground mining in the Xingshan Iron Mine in China.
机译:基于在实验室测试中获得的物理和机械参数以及花岗岩试样的截面扫描,在“粒子流代码”(PFC)程序中建立了花岗岩颗粒的微观几何模型。使用Fish语言对加载代码进行编程和调整,以模拟单轴和三轴压缩测试。基于完整的应力-应变曲线,声发射(AE)监测结果和测试中的裂纹数以及PFC模拟,在不同的载荷条件下获得了花岗岩在微观和宏观上的微观力学行为和裂纹演变。 。在此基础上,利用应力-应变曲线,裂纹,摩擦能与塑性应变之间的关系以及Continua模拟的快速拉格朗日分析,优化并验证了花岗岩的内聚力弱化和摩擦增强(CWFS)准则模型参数。花岗岩的初始内聚力,残余内聚力,初始摩擦角和残余摩擦角以及花岗岩的临界塑性应变epsilon(p)(c)和epsilon(p)(f)的最佳CWFS准则参数为23 MPa分别为4.3 MPa,0度,46.3度,0.0015和0.0037。这为建立中国兴山铁矿从露天开采到地下开采的岩石本构模型提供了科学依据。

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