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- Publisher Website: 10.1016/j.engfracmech.2014.02.022
- Scopus: eid_2-s2.0-84897546735
- WOS: WOS:000335101000001
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Article: Application of the numerical manifold method to model progressive failure in rock slopes
Title | Application of the numerical manifold method to model progressive failure in rock slopes |
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Authors | |
Keywords | Progressive failure Crack evolution technique Crack initiation criterion Rock slope Factor of safety Numerical manifold method Partition of unity method |
Issue Date | 2014 |
Citation | Engineering Fracture Mechanics, 2014, v. 119, p. 1-20 How to Cite? |
Abstract | The present study develops the numerical manifold method as a tool to investigate the progressive failure in rock slopes. The entire processes of the progressive slide surface development related to crack initiation, propagation, coalescence and degradation to eventual catastrophic failure are successfully captured. To overcome the limitation of the original NMM associated with an improper removal of the interface cohesion of the discontinuities, the displacement-dependent cohesion removal method is adopted. Simple examples of failure of rock slopes containing different arrangements of discontinuities are modeled and their results are compared with those based on the popular limit equilibrium method proposed by famous pioneers Jennings (1970) [1] and Jaeger (1971) [2]. The present results illustrate that the types of crack propagation and coalescence obtained by the developed NMM can help explain the relevant cracking processes in nature and experimental studies. © 2014 Elsevier Ltd. |
Persistent Identifier | http://hdl.handle.net/10722/214036 |
ISSN | 2023 Impact Factor: 4.7 2023 SCImago Journal Rankings: 1.232 |
ISI Accession Number ID |
DC Field | Value | Language |
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dc.contributor.author | Wong, Louis Ngai Yuen | - |
dc.contributor.author | Wu, Zhijun | - |
dc.date.accessioned | 2015-08-19T13:41:37Z | - |
dc.date.available | 2015-08-19T13:41:37Z | - |
dc.date.issued | 2014 | - |
dc.identifier.citation | Engineering Fracture Mechanics, 2014, v. 119, p. 1-20 | - |
dc.identifier.issn | 0013-7944 | - |
dc.identifier.uri | http://hdl.handle.net/10722/214036 | - |
dc.description.abstract | The present study develops the numerical manifold method as a tool to investigate the progressive failure in rock slopes. The entire processes of the progressive slide surface development related to crack initiation, propagation, coalescence and degradation to eventual catastrophic failure are successfully captured. To overcome the limitation of the original NMM associated with an improper removal of the interface cohesion of the discontinuities, the displacement-dependent cohesion removal method is adopted. Simple examples of failure of rock slopes containing different arrangements of discontinuities are modeled and their results are compared with those based on the popular limit equilibrium method proposed by famous pioneers Jennings (1970) [1] and Jaeger (1971) [2]. The present results illustrate that the types of crack propagation and coalescence obtained by the developed NMM can help explain the relevant cracking processes in nature and experimental studies. © 2014 Elsevier Ltd. | - |
dc.language | eng | - |
dc.relation.ispartof | Engineering Fracture Mechanics | - |
dc.subject | Progressive failure | - |
dc.subject | Crack evolution technique | - |
dc.subject | Crack initiation criterion | - |
dc.subject | Rock slope | - |
dc.subject | Factor of safety | - |
dc.subject | Numerical manifold method | - |
dc.subject | Partition of unity method | - |
dc.title | Application of the numerical manifold method to model progressive failure in rock slopes | - |
dc.type | Article | - |
dc.description.nature | link_to_subscribed_fulltext | - |
dc.identifier.doi | 10.1016/j.engfracmech.2014.02.022 | - |
dc.identifier.scopus | eid_2-s2.0-84897546735 | - |
dc.identifier.hkuros | 259205 | - |
dc.identifier.volume | 119 | - |
dc.identifier.spage | 1 | - |
dc.identifier.epage | 20 | - |
dc.identifier.isi | WOS:000335101000001 | - |
dc.identifier.issnl | 0013-7944 | - |