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A Microstructure-Based Model to Characterize Micromechanical Parameters Controlling Compressive and Tensile Failure in Crystallized Rock

机译:基于微结构的模型,表征结晶岩中压缩和拉伸破坏的微机械参数

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摘要

A discrete element model is proposed to examine rock strength and failure. The model is implemented by UDEC which is developed for this purpose. The material is represented as a collection of irregular-sized deformable particles interacting at their cohesive boundaries. The interface between two adjacent particles is viewed as a flexible contact whose stress-displacement law is assumed to control the material fracture and fragmentation process. To reproduce rock anisotropy, an innovative orthotropic cohesive law is developed for contact which allows the interfacial shear and tensile behaviours to be different from each other. The model is applied to a crystallized igneous rock and the individual and interactional effects of the microstructural parameters on the material compressive and tensile failure response are examined. A new methodical calibration process is also established. It is shown that the model successfully reproduces the rock mechanical behaviour quantitatively and qualitatively. Ultimately, the model is used to understand how and under what circumstances micro-tensile and micro-shear cracking mechanisms control the material failure at different loading paths.
机译:提出了一个离散元模型来检查岩石的强度和破坏。该模型由为此目的而开发的UDEC实现。该材料表示为在其内聚边界相互作用的不规则尺寸的可变形颗粒的集合。两个相邻粒子之间的界面被视为一个柔性触点,其应力-位移定律被认为可控制材料的破裂和破碎过程。为了再现岩石的各向异性,开发了一种用于接触的创新正交各向异性内聚定律,该定律使界面的剪切和拉伸行为互不相同。该模型适用于结晶火成岩,并研究了微观结构参数对材料压缩和拉伸破坏响应的个体和相互作用影响。还建立了新的方法化校准过程。结果表明,该模型成功地定量,定性地再现了岩石力学行为。最终,该模型用于了解微拉伸和微剪切裂纹机制如何以及在何种情况下控制不同加载路径下的材料破坏。

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