Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/121292
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dc.contributorMainland Development Office-
dc.creatorChen, J-
dc.creatorZhou, J-
dc.creatorJiang, N-
dc.creatorLi, H-
dc.creatorHu, Y-
dc.creatorLuo, H-
dc.creatorZhang, J-
dc.date.accessioned2026-09-21T06:07:16Z-
dc.date.available2026-09-21T06:07:16Z-
dc.identifier.urihttp://hdl.handle.net/10397/121292-
dc.language.isoenen_US
dc.publisherMDPI AGen_US
dc.rightsCopyright: © 2026 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).en_US
dc.rightsThe following publication Chen, J., Zhou, J., Jiang, N., Li, H., Hu, Y., Luo, H., & Zhang, J. (2026). Stability Assessment of Reservoir Bank Anti-Dip Slopes Using a Modified Goodman–Bray Method and Monte Carlo Simulation. Water, 18(4), 505 is available at https://doi.org/10.3390/w18040505.en_US
dc.subjectAnti-dip layered rock massen_US
dc.subjectFactor of safetyen_US
dc.subjectFailure-mode probabilityen_US
dc.subjectGB methoden_US
dc.subjectMonte Carlo simulationen_US
dc.subjectReservoir water actionen_US
dc.subjectToppling slopeen_US
dc.titleStability assessment of reservoir bank anti-dip slopes using a modified Goodman-Bray method and Monte Carlo simulationen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume18-
dc.identifier.issue4-
dc.identifier.doi10.3390/w18040505-
dcterms.abstractToppling failure is a fundamental mode of instability in rock slopes and occurs predominantly in reservoir bank anti-dip bedded rock masses. Reservoir impoundment changes seepage conditions and weakens slopes, whereas discontinuity non-persistence introduces uncertainty and complicates the identification of coupled toppling–sliding mechanisms. To address this, a probabilistic framework using the Goodman–Bray limit equilibrium method is developed. Equivalent strength parameters are introduced to unify the strength contrast between unsaturated and saturated segments along a common basal surface. Basal discontinuity connectivity is modeled as a random variable, and a Monte Carlo simulation is used to derive failure mode probabilities and a probability-weighted factor of safety. The framework is applied to the Huangcaoping anti-dip slope in the Dagangshan reservoir area at a normal water level of 1130 m. The most probable scenario has a probability of 0.116, involving sliding at 1120–1420 m and toppling at 1420–1550 m, with a probability-weighted mean factor of safety of 0.978. Predicted failure characteristics and deformation intervals are consistent with engineering observations, confirming the method’s effectiveness. This integration enables the simultaneous characterization of stability levels and the evolution mechanism. The approach provides mechanism-explicit mode likelihoods and a robust stability metric to support hazard assessment, monitoring placement, and reinforcement design.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationWater (Switzerland), Feb. 2026, v. 18, no. 4, 505-
dcterms.isPartOfWater (Switzerland)-
dcterms.issued2026-02-
dc.identifier.scopus2-s2.0-105031217853-
dc.identifier.eissn2073-4441-
dc.identifier.artn505-
dc.description.validate202609 bcch-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Scopus/WOSen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextThis research was funded by The National Natural Science Foundation of China (52379105), the China Postdoctoral Science Foundation (2025M773145), and the Sichuan Province Innovative Talent Funding Project for Postdoctoral Fellows (BX202408).en_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryCCen_US
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