Numerical Simulation of the Rock SHPB Test with a Special Shape Striker Based on the Discrete Element Method

被引:226
作者
Li, Xibing [1 ]
Zou, Yang [1 ,2 ]
Zhou, Zilong [1 ]
机构
[1] Cent South Univ, Sch Resources & Safety Engn, Changsha 410083, Hunan, Peoples R China
[2] Ecole Polytech Fed Lausanne, LMR, Sch Architecture Civil & Environm Engn, CH-1015 Lausanne, Switzerland
基金
中国国家自然科学基金;
关键词
SHPB; Special shape striker; Discrete element method; Strain rate effect; DYNAMIC-BEHAVIOR; STRAIN RATES; CONCRETE; COMPRESSION; STRENGTH; FAILURE; FRICTION; MODEL;
D O I
10.1007/s00603-013-0484-6
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
A split Hopkinson pressure bar (SHPB) system with a special shape striker has been suggested as the test method by the International Society for Rock Mechanics (ISRM) to determine the dynamic characteristics of rock materials. In order to further verify this testing technique and microscopically reveal the dynamic responses of specimens in SHPB tests, a numerical SHPB test system was established based on particle flow code (PFC). Numerical dynamic tests under different impact velocities were conducted. Investigation of the stresses at the ends of a specimen showed that the specimen could reach stress equilibrium after several wave reverberations, and this balance could be maintained well for a certain time period after the peak stress. In addition, analyses of the reflected waves showed that there was a clear relationship between the variation of the reflected wave and the stress equilibrium state in the specimen, and the turning point of the reflected wave corresponded well with the peak stress in the specimen. Furthermore, the reflected waves can be classified into three types according to their patterns. Under certain impact velocities, the specimen deforms at a constant strain rate during the whole loading process. Finally, the influence of the micro-strength ratio () and distribution pattern on the dynamic increase factor (DIF) of the strength DIF were studied, and the lateral inertia confinement and heterogeneity were found to be two important factors causing the strain rate effect for rock materials.
引用
收藏
页码:1693 / 1709
页数:17
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