土工基础 ›› 2021, Vol. 35 ›› Issue (6): 754-758.

• 专题论述 • 上一篇    下一篇

冲击荷载下珊瑚砂单颗粒动态破碎模拟研究

罗尚奕1,张浩天1,高康华2,侯蛤元3,杨 军4,张 欣1   

  1. (1.陆军工程大学 爆炸冲击防灾减灾国家重点实验室,南京 210007;2.92656部队,海口 571100;
    3.92829部队,广东湛江 524000;4.78315部队,成都 610031)
  • 收稿日期:2021-08-19 修回日期:2021-08-27 出版日期:2021-12-30 发布日期:2021-12-24
  • 通讯作者: 张浩天(1996-),男,博士研究生,研究方向为防灾减灾工程及防护工程。
  • 作者简介:罗尚奕(1996-),男,硕士研究生,研究方向为防灾减灾工程及防护工程。

Simulation of the Dynamic Breakage of a Single Coral Sand Particle under Impact Loads

LUO Shangyi1, ZHANG Haotian1, GAO Kanghua2, HOU Geyuan3, YANG Jun4, ZHANG Xin1   

  1. (1.State Key Laboratory of Disaster Prevention & Mitigation of Explosion & Impact, Army Engineering University of PLA, Nanjing 210007;2.PLA Division 92656, Haikou5 71100;PLA Division 92829, Zhanjiang 524000;PLA Division 78315, Chengdu 610031)
  • Received:2021-08-19 Revised:2021-08-27 Online:2021-12-30 Published:2021-12-24

摘要: 利用PFC2D(二维颗粒流程序)建立了考虑内孔隙随机分布的珊瑚砂动态冲击数值分析模型,结合力链分布、裂纹发展及破碎模式,从细观层面阐述颗粒破碎演化规律。结果表明,珊瑚砂单颗粒动态破碎强度符合Weibull分布。冲击荷载下,强力链首先出现在颗粒内孔隙端部和加载端附近,细观裂纹主要沿强力链生成,裂纹处力链发生弱化。裂纹多出现在拉应力集中区,主裂纹沿加载轴方向生长。朝内孔隙处偏转产生的次裂纹延伸到试样边缘,加之相邻裂纹间发生枝杈式贯通,使试样碎裂为多个部分。随着加载速率提高,裂纹更多源于内孔隙处且增速提高,裂纹贯通更加普遍。

关键词: 珊瑚砂, 颗粒破碎, 颗粒流程序, 内孔隙, 加载速率

Abstract: The particle flow code in two dimensions (PFC2D) software was used to construct a numerical model for analyzing the effects of dynamic impact loads on coral sands with random internal pore distributions. The evolution law of particle breakage was described combining of the force chain distributions, crack development and fragmentation patterns. The results indicate that the single-grain dynamic breakage strength in the coral sand follows the Weibull distribution pattern. Under impact loads, the force chains of a coral sand particle will first appear around the internal pore-end and loading-end. Most of the mesoscopic cracks form along these force chains, and the force chains will weaken around cracks. The cracks often appear in the tensile stress concentration zones and the primary crack will grow along the loading axis. The secondary cracks, which are formed by the crack deflection towards the internal pores, will extend towards the edges of the specimen and merge with adjacent cracks to penetrate the specimen, breaking it into multiple breakages. At higher loading rates, more cracks initiate from the internal pores and increase at a much faster rate. Crack penetration is also more common. 


Key words: coral sand, particle breakage, particle flow code, internal pores, loading rate

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