动态载荷诱发的有缺陷花岗岩断裂行为:基于 DIP 和 PFC 的研究

Xiao Wang, Wenbin Sun, Changdi He, Wei Yuan, V. Sarfarazi, Haozheng Wang
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引用次数: 0

摘要

本研究探讨了裂隙花岗岩在劈裂-霍普金森压杆测试下的动态行为和断裂机制,重点关注晶粒尺寸和裂隙尺寸等因素。通过数字图像处理和离散元方法,构建了基于真实花岗岩样品的粒子流代码二维(PFC2D)模型,有效克服了以往研究主要依赖随机参数的局限性。结果表明,花岗岩的裂纹分布受晶粒尺寸和缺陷尺寸的影响很大。拉伸裂缝占主导地位,矿物边界(如长石和石英之间)成为主要裂缝部位。裂纹长度和宽度对花岗岩的裂纹密度、分布和动态强度都有重要影响。具体来说,动态强度往往会随着裂纹的扩大而降低,并随着裂纹角度(最大 90°)的增大而增加。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Fracturing behaviors of flawed granite induced by dynamic loadings: A study based on DIP and PFC
This study explored the dynamic behaviors and fracturing mechanisms of flawed granite under split‐Hopkinson pressure bar testing, focusing on factors like grain size and flaw dimensions. By means of digital image processing and the discrete element method, Particle Flow Code 2D (PFC2D) models were constructed based on real granite samples, effectively overcoming the limitations of prior studies that mainly relied on randomized parameters. The results illustrate that the crack distribution of granite is significantly influenced by grain size and flaw dimensions. Tension cracks predominate and mineral boundaries, such as between feldspar and quartz, become primary crack sites. Both flaw length and width critically affect the crack density, distribution, and dynamic strength of granite. Specifically, dynamic strength tends to decrease with the enlargement of flaws and increase with an increase in flaw angles up to 90°.
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