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It is critical to understand the dynamic tensile failure of confined rocks in many rock engineering applications, such as underground blasting in mining projects. To simulate the in situ stress state of underground rocks, a modified split Hopkinson pressure bar system is utilized to load Brazilian disc (BD) samples hydrostatically, and then exert dynamic load to the sample by impacting the striker on the incident bar. The pulse shaper technique is used to generate a slowly rising stress wave to facilitate the dynamic force balance in the tests. Five groups of Laurentian granite BD samples (with static BD tensile strength of 12.8 MPa) under the hydrostatic confinement of 0, 5, 10, 15, and 20 MPa were tested with different loading rates. The result shows that the dynamic tensile strength increases with the hydrostatic confining pressure. It is also observed that under the same hydrostatic pressure, the dynamic tensile strength increases with the loading rate, revealing the so-called rate dependency for engineering materials. Furthermore, the increment of the tensile strength decreases with the hydrostatic confinement, which resembles the static tensile behavior of rock under confining pressure, as reported in the literature. The recovered samples are examined using X-ray micro-computed tomography method and the observed crack pattern is consistent with the experimental result. Keywords Dynamic tensile strength Á Hydrostatic confinement Á Brazilian disc Á SHPB Á Rate dependence Á X-ray CT Abbreviations SHPB Split Hopkinson pressure bar BD Brazilian disc CT Computed tomography LG Laurentian granite ISRM International Society for Rock Mechanics List of SymbolsA b Cross-sectional area of the bars (mm 2 ) A s Contact area between the sample and the transmitted bar (mm 2 ) r 0 Pump oil pressure (MPa) r 1 Stresses of the sample at the transmitted bar end (MPa) r 2 Stresses of the sample at the incident bar end (MPa) e i Incident strain wave e r Reflected strain wave e t Transmitted strain wave P 1 Force on incident end of the Brazilian disc specimen (N) P 2 Force on transmitted end of the Brazilian disc specimen (N) E b Young's modulus of the bars (GPa) B Thickness of the Brazilian disc specimen (mm) D Diameter of the Brazilian disc specimen (mm) r Tensile stress at the center of the Brazilian disc specimen (MPa) S Dynamic tensile strength of the Brazilian disc specimen (MPa) S 0 Static Brazilian tensile strength of Laurentian granite (MPa) & Kaiwen Xia
It is critical to understand the dynamic tensile failure of confined rocks in many rock engineering applications, such as underground blasting in mining projects. To simulate the in situ stress state of underground rocks, a modified split Hopkinson pressure bar system is utilized to load Brazilian disc (BD) samples hydrostatically, and then exert dynamic load to the sample by impacting the striker on the incident bar. The pulse shaper technique is used to generate a slowly rising stress wave to facilitate the dynamic force balance in the tests. Five groups of Laurentian granite BD samples (with static BD tensile strength of 12.8 MPa) under the hydrostatic confinement of 0, 5, 10, 15, and 20 MPa were tested with different loading rates. The result shows that the dynamic tensile strength increases with the hydrostatic confining pressure. It is also observed that under the same hydrostatic pressure, the dynamic tensile strength increases with the loading rate, revealing the so-called rate dependency for engineering materials. Furthermore, the increment of the tensile strength decreases with the hydrostatic confinement, which resembles the static tensile behavior of rock under confining pressure, as reported in the literature. The recovered samples are examined using X-ray micro-computed tomography method and the observed crack pattern is consistent with the experimental result. Keywords Dynamic tensile strength Á Hydrostatic confinement Á Brazilian disc Á SHPB Á Rate dependence Á X-ray CT Abbreviations SHPB Split Hopkinson pressure bar BD Brazilian disc CT Computed tomography LG Laurentian granite ISRM International Society for Rock Mechanics List of SymbolsA b Cross-sectional area of the bars (mm 2 ) A s Contact area between the sample and the transmitted bar (mm 2 ) r 0 Pump oil pressure (MPa) r 1 Stresses of the sample at the transmitted bar end (MPa) r 2 Stresses of the sample at the incident bar end (MPa) e i Incident strain wave e r Reflected strain wave e t Transmitted strain wave P 1 Force on incident end of the Brazilian disc specimen (N) P 2 Force on transmitted end of the Brazilian disc specimen (N) E b Young's modulus of the bars (GPa) B Thickness of the Brazilian disc specimen (mm) D Diameter of the Brazilian disc specimen (mm) r Tensile stress at the center of the Brazilian disc specimen (MPa) S Dynamic tensile strength of the Brazilian disc specimen (MPa) S 0 Static Brazilian tensile strength of Laurentian granite (MPa) & Kaiwen Xia
Summary This paper deals with numerical modeling of dynamic failure phenomena in rate‐sensitive quasi‐brittle materials, such as rocks, with initial microcrack populations. To this end, a continuum viscodamage‐embedded discontinuity model is developed and tested in full 3D setting. The model describes the pre‐peak nonlinear and rate‐sensitive hardening response of the material behavior, representing the fracture‐process zone creation, by a rate‐dependent continuum damage model. The post‐peak response, involving the macrocrack creation accompanied by exponential softening, is formulated by using an embedded displacement discontinuity model. The finite element implementation of this model relies upon the linear tetrahedral element, which seems appropriate for explicit dynamic analyses involving stress wave propagation. The problems of crack locking and spreading typical of embedded discontinuity models are addressed in this paper. A combination of two remedies, the inclusion of viscosity in the spirit of Wang's viscoplastic consistency approach and introduction of isotropic damaging into the embedded discontinuity model, is shown to be effective in the present explicit dynamics setting. The model performance is illustrated by several numerical simulations. In particular, the dynamic Brazilian disc test and the Kalthoff–Winkler experiment show that the present model provides realistic predictions with the correct failure modes and rate‐dependent tensile strengths of rock at different loading rates. The ability of initial embedded discontinuity populations to model the initial microcrack populations in rocks is also successfully tested. Copyright © 2016 John Wiley & Sons, Ltd.
The coupling effect of temperature and impact loads can cause the concrete strength to decay and lead to the failure of the structure that cannot reach the designed load‐bearing strength. In this study, the evolution laws of dynamic compressive strength, dynamic increase factor (DIF), and absorbed energy of (1% polyvinyl alcohol [PVA] fiber +1% steel fiber) PS‐ECC (engineered cementitious composite) were obtained by a split Hopkinson compression bar test. The conclusions can be concluded: the dynamic compressive strength, DIF, and absorbed energy of PS‐ECC largely show a tendency to decrease with increasing temperature; however, the recovery effect occurs at 200°C due to the accumulation of steam inside the specimen to counteract the impact force. Then, 200°C becomes a threshold value, and the sensitivity of PS‐ECC to strain rate shows a steep drop when the temperature exceeds 200°C. Compared to 200°C, the growth rate of dynamic compressive strength, DIF, and energy absorption capacity from strain rate 50–80 s−1 decreases by 50.65, 55.24, and 45.71% at 300°C, the growth rate decreases by 55.87, 56.5, and 48.45% at 400°C. The impact energy absorption of PS‐ECC was provided mainly by PVA fiber. The energy absorption of PS‐ECC is almost the same at 300 and 400°C for the same strain rate due to PVA fiber burning disappears.
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