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Numerical Research on Energy Evolution in Granite under Different Confining Pressures Using Otsu’s Digital Image Processing and PFC2D

机译:不同局部图像处理和PFC2D不同狭窄压力下花岗岩能量演化的数值研究

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摘要

Research on energy accumulation and releasing in the rock plays a key role on revealing its failure mechanism. This paper establishes a microscopic structure model of granite using Otsu digital image processing (DIP) technology and particle flow code software (PFC2D). A series of numerical compression tests under different confining pressures were conducted to investigate the macro and micro characteristics of energy evolution in granite. The results showed that the energy evolution of granite is divided into three stages: stable accumulation, slow dissipation, and rapid release. With increasing confining pressure, the strain energy accumulation ratio decreased exponentially and the peak value of strain energy increased linearly. It was found that the energy accumulation speed in the pre-peak stage increased as a linear function, while the energy release speed in the post-peak stage decreased as an exponential function. In addition, the feldspar is the main microstructure which played a major part in accumulating energy in granite. However, the unit mineral energy of mica particles was bigger than that of feldspar and quartz. When subjected to increasing confining pressure, the feldspar’s total energy growth rate was fastest. Meanwhile, the mica’s unit energy growth rate was fastest.
机译:岩石中能量积累和释放的研究在揭示其失效机制方面发挥着关键作用。本文建立了使用OTSU数字图像处理(DIP)技术和粒子流代码软件(PFC2D)花岗岩的微观结构模型。进行了不同限制压力下的一系列数值压缩试验,以研究花岗岩中能量演化的宏观和微观特征。结果表明,花岗岩的能量演化分为三个阶段:稳定的积累,慢速耗散和快速释放。随着狭窄压力的增加,应变能量累积比指数呈指数增长,应变能量的峰值线性增加。发现预峰值阶段中的能量累积速度随着线性函数而增加,而后峰阶段的能量释放速度随着指数函数而降低。此外,长石是主要的微观结构,它在花岗岩中积累了能量的主要部分。然而,云母颗粒的单位矿物能大于长石和石英的矿物能量。当受到增加的压力时,长石总能量增长率最快。同时,云母的单位能量增长率最快。

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