首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >The influence of loading conditions on fracture initiation, propagation, and interaction in rocks with veins: Results from a comparative Discrete Element Method study
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The influence of loading conditions on fracture initiation, propagation, and interaction in rocks with veins: Results from a comparative Discrete Element Method study

机译:加载条件对岩石与静脉的破裂萌生,扩展和相互作用的影响:比较离散元方法研究的结果

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We present the results of a comparative study of loading conditions on the interactions between extension fractures and veins. We model the fracture behavior of brittle discrete element materials each containing a tabular vein body of variable orientation and strength in two different loading conditions. The first is uniaxial tension, applied with servo-controlled sidewalls. The second is a boudinage boundary condition in which a tensile triaxial stress state is induced in the brittle model volume by quasi-viscous extensional deformation in the adjacent layers. Most of the fracture- vein interactions observed in uniaxial tension also exists in boudinage boundary conditions. However, the importance of each interaction mechanism for a given configuration of relative strength and misorientation of the vein may differ according to the loading mechanism. Nucleation and internal deflection is under both boundary conditions the dominating fracture-vein interaction style in weak veins. In uniaxial tension models, strong veins tend to alter the fracture path by external deflection, while under boudinage loading these veins are more likely overcome by the fracture step over mechanism. Dynamic bifurcation of fractures was observed in uniaxial tension models but never for boudinage boundary conditions. This is because the acceleration of fracture tips in these conditions is suppressed by interaction with distributed fractures as well as viscous damping by the neighboring layers.
机译:我们介绍了拉伸条件与延伸静脉之间相互作用的加载条件的比较研究结果。我们对脆性离散元素材料的断裂行为进行建模,每种材料在两个不同的载荷条件下均包含具有可变方向和强度的板状静脉体。第一个是单轴张力,施加有伺服控制的侧壁。第二个是布德纳吉边界条件,其中在脆性模型体积中,由于相邻层中的准粘性拉伸变形而诱发了拉伸三轴应力状态。在单轴拉力中观察到的大多数断裂-静脉相互作用也存在于土脉边界条件中。但是,每种交互作用机制对于给定的相对强度和静脉错位配置的重要性可能会因加载机制而异。在两种边界条件下,成核和内部挠度都是弱静脉中主要的骨折-静脉相互作用方式。在单轴拉伸模型中,强静脉趋于通过外部挠曲改变骨折路径,而在腹股沟载荷下,这些静脉更有可能通过骨折越过机制克服。在单轴拉力模型中观察到了裂缝的动态分叉,但在杜邦边界条件下从未观察到。这是因为在这些条件下,由于与分布裂缝的相互作用以及相邻层的粘性阻尼,裂缝尖端的加速度得到了抑制。

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