Effects of particle size on dynamic constitutive relation and energy absorption of calcareous sand

被引:70
作者
Lv, Yaru [1 ,3 ]
Wang, Yuan [1 ]
Zuo, Dianjun [2 ]
机构
[1] Hohai Univ, Coll Mech & Mat, Nanjing 210098, Jiangsu, Peoples R China
[2] MOT Geotech Engn Res Ctr, Tianjin Res Inst Water Transport Engn, Xingang Rd 2, Tianjin 300456, Peoples R China
[3] Hong Kong Univ Sci & Technol, Dept Civil & Environm Engn, Clear Water Bay, Hong Kong, Peoples R China
基金
中国国家自然科学基金;
关键词
Particle size; Dynamic constitutive relation; Particle crush; Energy absorption; BREAKAGE;
D O I
10.1016/j.powtec.2019.07.088
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
The dynamic responses of calcareous sand at high strain rates, closely relating to geotechnical and ocean engineering, are still not fully understood. This paper reports a series of split-Hopkinson pressure bar tests on porous calcareous and solid silica sands, with particle sizes of 0.15-0.30 mm, 030-0.60 mm, 0.60-1.18 mm and 1.18-2.00 mm. The particle size affects the impact stress-strain behaviour during particle crush, which mainly occurs at the final strain-hardening stage for silica sand, but occurs in the entire loading process for calcareous sand. The natural crushability of calcareous sand, quantified by fractal dimension, is approximately 1.2 times that of silica sand. The two sands show opposite responses for particle size in confined/bulk modulus and capability of energy absorption. This is because, as the particle size increased, calcareous and silica sands have opposite changes in terms of the void ratio and friction angle due to inter-particle voids and mineral composition. (C) 2019 Elsevier B.V. All rights reserved.
引用
收藏
页码:21 / 30
页数:10
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