2009
DOI: 10.1016/j.ijimpeng.2009.04.008
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Strain-rate effects on the strength and fragmentation size of rocks

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Cited by 125 publications
(33 citation statements)
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“…During the low rate loading, the stress distribution at the micro level is constant throughout the material, and the crack propagation focuses on the weakest areas of the sample. At higher strain rates, however, the stress increases very rapidly and exceeds the material fracture strength in several locations, not only at the weakest point [29]. This leads to simultaneous initiation and propagation of multiple cracks and finally complete pulverization of the sample, as well as a fast release of elastic strain energy as kinetic energy of the rock particles, acoustic emission, and generation of frictional heat.…”
Section: Analysis Of Resultsmentioning
confidence: 99%
“…During the low rate loading, the stress distribution at the micro level is constant throughout the material, and the crack propagation focuses on the weakest areas of the sample. At higher strain rates, however, the stress increases very rapidly and exceeds the material fracture strength in several locations, not only at the weakest point [29]. This leads to simultaneous initiation and propagation of multiple cracks and finally complete pulverization of the sample, as well as a fast release of elastic strain energy as kinetic energy of the rock particles, acoustic emission, and generation of frictional heat.…”
Section: Analysis Of Resultsmentioning
confidence: 99%
“…An objective of this study is to provide further insights into some salient features of the deformation dynamics of brittle solids, specifically the ceramic materials with the inferior grain boundary strength and low fracture energy. With these materials in mind, the strain rate range of these virtual idealized experiments (10 s À1 , 1 Â 10 9 s À1 ]) tentatively labeled medium-to-high reaches the theoretical limit, _ " 0 ¼ " 0 = 0 %10 9 s À1 ; defined by the assumed limit failure strain, " 0 ¼ 0.001, and a temporal parameter of the order of Debye's atomic vibration period, 0 ¼ 10 À12 s (Qi et al, 2009). The lower and upper ends of the range investigated herein are customarily explored by the split Hopkinson bar (below 10 4 s À1 ) and the planar impact tests (up to 10 8 s À1 ), respectively (Field et al, 2004).…”
Section: Introductionmentioning
confidence: 96%
“…In addition, in DEM, cracks form, interact, and coalesce into macroscopic fractures as a consequence of bond breakage between particles. This ensures that the numerical model can simulate the dynamic crushing failure of rock effectively (Hazzard et al 2000;Qi et al 2009). …”
Section: Introductionmentioning
confidence: 99%