Spatial distribution of yield accelerations and permanent displacements: A diagnostic tool for assessing seismic slope stability
Seismically-induced permanent displacements of slopes are commonly evaluated using the Newmark sliding block approach. The conventional Newmark approach, while convenient in application, is often applied to a singular potential failure mechanism, omits consideration of the spatial distribution of po...
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| Published in | Soil dynamics and earthquake engineering (1984) Vol. 126; p. 105811 |
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| Main Authors | , , , |
| Format | Journal Article |
| Language | English |
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01.11.2019
Elsevier BV |
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| Online Access | Get full text |
| ISSN | 0267-7261 1879-341X |
| DOI | 10.1016/j.soildyn.2019.105811 |
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| Abstract | Seismically-induced permanent displacements of slopes are commonly evaluated using the Newmark sliding block approach. The conventional Newmark approach, while convenient in application, is often applied to a singular potential failure mechanism, omits consideration of the spatial distribution of potential failure mechanisms, neglects complex yet realistic failure geometry, and does not consider the temporal evolution of the critical mechanism. The proposed diagnostic tool applies the Newmark approach within a rigorous limit equilibrium framework to produce spatial distributions of yield accelerations and seismically-induced permanent displacements, or yield maps and surface-associated displacement maps, respectively. In this study, the application and utility of these diagnostic tools are demonstrated through a sensitivity analysis considering various soil strength parameters, horizontal and vertical motions, and complex slope and failure geometries. Additionally, it is shown that the proposed diagnostic tool reasonably estimates post-seismic geometry, shown by a comparison to an experimental shake table study. Using yield and displacement maps, both coseismic displacement and the range of potentially unstable geometry may be constrained. Moreover, the spatial and temporal evolution of possible seismically-induced displacements may be considered. This tool provides a rational means of applying sliding block approaches that reduces the need to assume the surface of maximum displacement a priori while retaining the simplicity that has facilitated the application of the sliding block approach versus more complex numerical models. The proposed diagnostic tools also provide a framework for future potential analyses, as it can be modified to incorporate other slope stability methods or seismic analyses.
•The proposed diagnostic tools are an extension of the traditional safety map for seismic slope stability, including a map of yield accelerations and coseismic permanent displacements.•Consideration of generalized failure geometry and rotation is considered in quantification of slope permanent displacements.•Slopes subject to seismic excitation have a single surface that yields the largest coseismic displacement, however, many other potential failure mechanisms may exhibit similar permanent displacement.•Consideration of vertical accelerations results in shifts of the surface of maximum displacement during seismic excitation.•These diagnostic tools may provide important information regarding seismic slope performance when considering complex slope geometry (e.g. tiered slopes, generalized failure geometry). |
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| AbstractList | Seismically-induced permanent displacements of slopes are commonly evaluated using the Newmark sliding block approach. The conventional Newmark approach, while convenient in application, is often applied to a singular potential failure mechanism, omits consideration of the spatial distribution of potential failure mechanisms, neglects complex yet realistic failure geometry, and does not consider the temporal evolution of the critical mechanism. The proposed diagnostic tool applies the Newmark approach within a rigorous limit equilibrium framework to produce spatial distributions of yield accelerations and seismically-induced permanent displacements, or yield maps and surface-associated displacement maps, respectively. In this study, the application and utility of these diagnostic tools are demonstrated through a sensitivity analysis considering various soil strength parameters, horizontal and vertical motions, and complex slope and failure geometries. Additionally, it is shown that the proposed diagnostic tool reasonably estimates post-seismic geometry, shown by a comparison to an experimental shake table study. Using yield and displacement maps, both coseismic displacement and the range of potentially unstable geometry may be constrained. Moreover, the spatial and temporal evolution of possible seismically-induced displacements may be considered. This tool provides a rational means of applying sliding block approaches that reduces the need to assume the surface of maximum displacement a priori while retaining the simplicity that has facilitated the application of the sliding block approach versus more complex numerical models. The proposed diagnostic tools also provide a framework for future potential analyses, as it can be modified to incorporate other slope stability methods or seismic analyses.
•The proposed diagnostic tools are an extension of the traditional safety map for seismic slope stability, including a map of yield accelerations and coseismic permanent displacements.•Consideration of generalized failure geometry and rotation is considered in quantification of slope permanent displacements.•Slopes subject to seismic excitation have a single surface that yields the largest coseismic displacement, however, many other potential failure mechanisms may exhibit similar permanent displacement.•Consideration of vertical accelerations results in shifts of the surface of maximum displacement during seismic excitation.•These diagnostic tools may provide important information regarding seismic slope performance when considering complex slope geometry (e.g. tiered slopes, generalized failure geometry). Seismically-induced permanent displacements of slopes are commonly evaluated using the Newmark sliding block approach. The conventional Newmark approach, while convenient in application, is often applied to a singular potential failure mechanism, omits consideration of the spatial distribution of potential failure mechanisms, neglects complex yet realistic failure geometry, and does not consider the temporal evolution of the critical mechanism. The proposed diagnostic tool applies the Newmark approach within a rigorous limit equilibrium framework to produce spatial distributions of yield accelerations and seismically-induced permanent displacements, or yield maps and surface-associated displacement maps, respectively. In this study, the application and utility of these diagnostic tools are demonstrated through a sensitivity analysis considering various soil strength parameters, horizontal and vertical motions, and complex slope and failure geometries. Additionally, it is shown that the proposed diagnostic tool reasonably estimates post-seismic geometry, shown by a comparison to an experimental shake table study. Using yield and displacement maps, both coseismic displacement and the range of potentially unstable geometry may be constrained. Moreover, the spatial and temporal evolution of possible seismically-induced displacements may be considered. This tool provides a rational means of applying sliding block approaches that reduces the need to assume the surface of maximum displacement a priori while retaining the simplicity that has facilitated the application of the sliding block approach versus more complex numerical models. The proposed diagnostic tools also provide a framework for future potential analyses, as it can be modified to incorporate other slope stability methods or seismic analyses. |
| ArticleNumber | 105811 |
| Author | Mathews, Nicolas Leshchinsky, Ben A. Olsen, Michael J. Klar, Assaf |
| Author_xml | – sequence: 1 givenname: Nicolas surname: Mathews fullname: Mathews, Nicolas email: mathewsn@oregonstate.edu organization: School of Civil and Construction Engineering, Oregon State University, 101 Kearney Hall, Corvallis, OR, 97331, USA – sequence: 2 givenname: Ben A. surname: Leshchinsky fullname: Leshchinsky, Ben A. email: ben.leshchinsky@oregonstate.edu organization: College of Forestry, Oregon State University, 319 Snell Hall, Corvallis, OR, 97331, USA – sequence: 3 givenname: Michael J. surname: Olsen fullname: Olsen, Michael J. email: michael.olsen@oregonstate.edu organization: School of Civil and Construction Engineering, Oregon State University, 101 Kearney Hall, Corvallis, OR, 97331, USA – sequence: 4 givenname: Assaf surname: Klar fullname: Klar, Assaf email: askla@byg.dtu.dk organization: Department of Civil Engineering, Denmark Technical University, Building 119, Room 141, 2800, Kgs. Lyngby, Denmark |
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| CitedBy_id | crossref_primary_10_1016_j_enggeo_2023_107387 crossref_primary_10_1061__ASCE_GM_1943_5622_0001831 crossref_primary_10_3389_feart_2024_1355767 crossref_primary_10_1029_2020JF005669 crossref_primary_10_1061_IJGNAI_GMENG_8697 crossref_primary_10_1007_s11440_024_02443_4 crossref_primary_10_1016_j_compgeo_2022_105048 crossref_primary_10_1007_s40098_022_00634_y crossref_primary_10_1061_IJGNAI_GMENG_8954 |
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| Keywords | Landslides Yield map Generalized limit equilibrium Safety map Slope stability Sliding block Displacement map |
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| Snippet | Seismically-induced permanent displacements of slopes are commonly evaluated using the Newmark sliding block approach. The conventional Newmark approach, while... |
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| SubjectTerms | Diagnostic software Diagnostic systems diagnostic techniques Displacement Displacement map dynamics earthquakes Evolution Failure mechanisms Generalized limit equilibrium Geometry geophysics Landslides Mathematical models Numerical models Parameter sensitivity Safety map Seismic stability Sensitivity analysis Sliding Sliding block Slope stability Slopes Soil analysis Soil strength Spatial distribution Stability analysis Yield map |
| Title | Spatial distribution of yield accelerations and permanent displacements: A diagnostic tool for assessing seismic slope stability |
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