2012
DOI: 10.1007/s00603-012-0287-1
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Some Fundamental Issues and Verification of 3DEC in Modeling Wave Propagation in Jointed Rock Masses

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Cited by 63 publications
(18 citation statements)
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“…The dynamic relaxation algorithm is adopted to solve the systems of equations and the development of large displacements is allowed as the failure occurs [33,34]. In this study, the 3DEC discrete element numerical calculation software, which has the features of (1) allow limited displacements and rotations, including complete separation, and (2) automatic identification of new contacts during the calculation, was applied to reveal the anchorage mechanical behaviors of blocky rock mass under an applied axial load [35,36].…”
Section: Experiments Results Analysismentioning
confidence: 99%
“…The dynamic relaxation algorithm is adopted to solve the systems of equations and the development of large displacements is allowed as the failure occurs [33,34]. In this study, the 3DEC discrete element numerical calculation software, which has the features of (1) allow limited displacements and rotations, including complete separation, and (2) automatic identification of new contacts during the calculation, was applied to reveal the anchorage mechanical behaviors of blocky rock mass under an applied axial load [35,36].…”
Section: Experiments Results Analysismentioning
confidence: 99%
“…The deformation and damage of geomaterial and tunnel lining are dependent on the location of explosive position inside the tunnel and the radius of curvature of the tunnel [5]. Researchers also investigated the dynamic response of tunnel in weathered rock, propagation of shear wave and behaviour of rock subjected to blast loading [36][37][38]. Moreover, blast analysis of tunnel had been studied mostly using Ansys, LS-DYNA and Abaqus [3-5, 21, 28].…”
Section: Introductionmentioning
confidence: 99%
“…In Earth's crust, discontinuities, such as faults, joints, bedding planes, and fractures, are ubiquitous and they often control the hydraulic and mechanical behavior of rock masses [1][2][3][4]. Elastic waves propagating through jointed rock masses will attenuate (or slow down) because of the existence of abundant rock joints [5][6][7][8][9]. e properties of the jointed rock mass including the joint matching coefficient (JMC), joint roughness coefficient (JRC), and the joint stiffness affect not only the dynamic behavior of joint but also the stress wave energy attenuation confirmed by the laboratory experiment (i.e., split Hopkinson pressure bar (SHPB) and ultrasonic test) [10][11][12].…”
Section: Introductionmentioning
confidence: 99%