2003
DOI: 10.1016/s1365-1609(03)00072-8
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Strain-rate dependency of the dynamic tensile strength of rock

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Cited by 256 publications
(75 citation statements)
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“…Dynamic loading is commonly encountered due to shocks, blasting, high-speed trains, etc. If the loading rate is very high during experiment, waves are propagated and their superposition produces a stress distribution different from the quasi-static situation (Kumar 1968;Zhang et al 2000;Cho et al 2003;Zhu and Tang 2006). However, no universal loading rate threshold has been established to differentiate between quasi-static and dynamic behaviours of the material.…”
Section: Loadingmentioning
confidence: 99%
See 1 more Smart Citation
“…Dynamic loading is commonly encountered due to shocks, blasting, high-speed trains, etc. If the loading rate is very high during experiment, waves are propagated and their superposition produces a stress distribution different from the quasi-static situation (Kumar 1968;Zhang et al 2000;Cho et al 2003;Zhu and Tang 2006). However, no universal loading rate threshold has been established to differentiate between quasi-static and dynamic behaviours of the material.…”
Section: Loadingmentioning
confidence: 99%
“…A loading rate equal to 0.05 MPa/s for uniaxial compression experiment on granite is proposed in Zhao (2000). A threshold of deformation rate equal around 0.1-1 s −1 is proposed in Cho et al (2003) for a Hopkinson bar test on granite.…”
Section: Loadingmentioning
confidence: 99%
“…Discontinuities play a critical role in creating a complex fracture network, and the influence of dynamic tension on the evolution of the fracturing network, which should be deeply investigated. Among the published literature, the Brazilian test [10,11], flattened Brazilian disc tests [12][13][14][15][16], Semicircular bending (SCB) test [17], and the split Hopkinson pressure bar (SHPB) tests [18][19][20][21] were mainly adopted to research the mechanical properties of rock material under dynamic tension. It was found that the strength of rock presented rate dependency; rock strength increases with the increase of strain rate, and almost all the studies are focused on dolerite [22], limestone [10], granite [17,19], tuff [21], sandstone [23], and basalt [21].…”
Section: Introductionmentioning
confidence: 99%
“…The crack initiation step can be simulated using sophisticated ratedependent constitutive models. Several models have been proposed for random generation of cracks in rocks under dynamic loading, including Cho et al (2004aCho et al ( , 2008, Cho and Kaneko (2004), Zhu et al (2004Zhu et al ( , 2007, and Ma and An (2008). The second stage of gas fracturing, gas penetration into existing cracks, is of great importance because it predominantly determines the final crack extension.…”
Section: Introductionmentioning
confidence: 99%