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首页> 外文期刊>Arabian journal of geosciences >Study on dynamic mechanical properties of phosphate rock through experimental tests and mesoscale simulation
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Study on dynamic mechanical properties of phosphate rock through experimental tests and mesoscale simulation

机译:通过实验测试和Messcale模拟研究磷酸盐岩体动态力学性能研究

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摘要

Dynamic characteristics of rock masses are an important part of the safety and stability analysis in rock mass engineering. The split Hopkinson pressure bar (SHPB) tests on the phosphate rock in Yichang are conducted, combined with the Split-desktop digital image method and mesoscopic discrete element method (DEM). Both macroscopic and mesoscopic characteristics of the phosphate rock have been studied from such perspectives as stress and strain, fractal characteristics of fragment size, and the spatial and temporal evolution of cracks. The research results show that the dynamic strength of the phosphate rock presents obvious strain rate effect, but the dynamic elasticity modulus is not so sensitive to the strain rate. There is a great correlation between the failure degree of rock specimens and the strain rate. The fractal characteristics of specimen fragments can be used to quantitatively evaluate the rock failure degree under impact loading. According to the characteristics of crack propagation, the rock failure process under the impact can be divided into four stages, namely the elastic crack-free stage, the crack initiation stage, the rapid crack growth stage, and the slow crack development stage. Moreover, with the increase of impact loading, micro-cracks are activated in large quantities. The specimens gradually change from the local damage mode to the axial splitting failure mode and to the crushing failure mode, and in this process, the number of tensile cracks takes an absolute advantage compared with the number of shear cracks.
机译:岩体的动态特性是岩石群体安全性和稳定性分析的重要组成部分。对宜昌的磷酸盐岩石的分裂霍普金森压力棒(SHPB)试验,结合了分体式数字图像方法和介观离散元件方法(DEM)。已经从这种角度作为应力和应变,片段大小的分形特征以及裂缝的空间和时间演变来研究磷酸盐岩的宏观和介观特性。研究结果表明,磷酸盐的动态强度呈现明显的应变率效应,但动态弹性模量对应变率不太敏感。岩石标本的故障程度与应变率之间存在很大的相关性。样品片段的分形特征可用于定量评估冲击载荷下的岩石衰竭程度。根据裂纹传播的特点,抗冲击过程下的岩石破坏过程可分为四个阶段,即弹性裂缝阶段,裂纹起始阶段,快速裂纹生长阶段,以及缓慢的裂纹开发阶段。此外,随着冲击载荷的增加,微裂纹以大量激活。试样从局部损伤模式逐渐变化到轴向分离失效模式,并且在破碎失效模式下,并且在该过程中,与剪切裂缝的数量相比,拉伸裂缝的数量取得绝对优势。

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