2022
DOI: 10.1007/s10346-022-01918-3
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Predictive model of regional coseismic landslides’ permanent displacement considering uncertainty

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Cited by 9 publications
(4 citation statements)
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“…For example, we test a wide range of COV values to identify the most suitable Gaussian distribution that cohesion and friction-angle values could follow. We should stress that although shear strength parameters generally follow a normal distribution [61][62][63] , this assumption may not hold everywhere. Therefore, upon acquisition of site-specific geotechnical analyses that would yield skewed distributions of shear-strength parameters, these would need to be addressed accordingly.…”
Section: Discussionmentioning
confidence: 99%
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“…For example, we test a wide range of COV values to identify the most suitable Gaussian distribution that cohesion and friction-angle values could follow. We should stress that although shear strength parameters generally follow a normal distribution [61][62][63] , this assumption may not hold everywhere. Therefore, upon acquisition of site-specific geotechnical analyses that would yield skewed distributions of shear-strength parameters, these would need to be addressed accordingly.…”
Section: Discussionmentioning
confidence: 99%
“…For each landslide thickness, we randomly create shear-strength parameters using a Monte Carlo simulation, a commonly used approach for addressing the uncertainty of soil and rock properties in engineering geological problems 63,83,84 . To run the simulations, we estimate the distribution of shear-strength parameters.…”
Section: Back-analysesmentioning
confidence: 99%
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“…This method remains one of the most used, physics-based, models to simulate co-seismic permanent displacements in terms of failure probability of slopes. It calculates the critical acceleration (A c ) that sufficiently reduces the shear resistance to trigger ground motion, when seismic intensity exceeds the seismic strength of the slope (Jibson et al 2004(Jibson et al , 2006Jibson 2011;Chen et al 2019;Jin et al 2019;Xi et al 2022). The traditional and modified forms of the ND method have been successfully implemented to evaluate co-seismic landslides triggered by the 1994 M w 6.7 Northridge, 1999 M w 7.5 Chi-Chi, 2008 M w 7.9 Wenchuan, 98 earthquakes in Greece, 2013 M s 7.0 Lushan, Kumaun Himalaya, 2015 M w 7.8 Gorkha, and Mid Niigata Prefecture earthquakes (e.g., Jibson et al 2000;Wang and Lin 2010;Chen et al 2014;Chousianitis et al 2014;Yuan et al 2016;Shinoda and Miyata 2017;Jin et al 2019;Kumar et al 2021;Maharjan et al 2021).…”
Section: Introductionmentioning
confidence: 99%