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The Influence of Silt Layer Orientation on Slope Stability in Shale Formations

dc.contributor.authorAlam, AKM Badrul
dc.contributor.authorFujii, Yoshiaki
dc.contributor.authorLi, Zhixue
dc.contributor.authorHasan Dipu, Nahid
dc.contributor.authorTajib–Ul–Islam, Md.
dc.contributor.authorAhmed Razo, Shakil
dc.date.accessioned2025-07-07T06:26:44Z
dc.date.available2025-07-07T06:26:44Z
dc.date.issued2025-06
dc.description.abstractShale rock masses often include silt layers, impacting slope stability in construction and mining. Analyzing their interaction is crucial for long-term stability. This study used an elasto-plastic model, incorporating the stress transfer method and Coulomb's criterion. It computed stress distribution, assessed failure potential, and identified vulnerable regions. A shale rock mass ranging from 14.75 to 16.75 meter thick, with silt layers varying from 0.36 to 0.5 meter thick was considered in the model. It examined four silt layer conditions: horizontal (SilHL), vertical (SilVL), in-facing (SilIN), and out-facing slope (SilOUT). Mechanical parameters like Uniaxial Compressive Strength (UCS), Tensile Strength (TS),andYoung’s modulus (E) were adjusted for varied scenarios: UCS (0.5 to 5 MPa), and E(6 to 60 MPa), keeping UCS/TS = 5 for all the conditions. In the elasto-plastic analysis, overall reductions of 20%, 40%, 60%, 80%, and 90% in E, UCS and TS were evaluated, taking into consideration the temporal degradation. The findings for SilHL indicate that: (i) when the E, UCS, and TS of the silt layer and shale were equivalent, significant structural failure occurred at 60% reduction, with pronounced collapse at 80% and complete failure at 90%; (ii) a lower Ein the silt layer with equivalent strength to shale showed no significant differences; (iii) reductions in both Eand UCS for the silt layer also revealed no notable differences. For SilVL, the results were similar, with (i) consistent effects as SilHL; (ii) slippage occurring with a lower Efor the silt layer; and (iii) bitension failure and toppling observed when the silt layer's strength was one-tenth that of shale. In SilIN, similar patterns emerged, with slippage and tension failures noted under reduced Eand UCS conditions. For SilOUT, results mirrored SilHL, with tension failures and divergence in failure patterns under reduced Eand UCS. The results of this study indicate that slope failure scenarios involving shale with a silt layer can be effectively simulated using the elasto-plastic method, particularly by incorporating reductions in strength and Young’s modulus. Furthermore, these findings highlight the critical need for additional research on specific slope configurations to refine design methodologies and enhance stability assessments within the context of the elasto-plastic model.en_US
dc.identifier.issn2224-2007
dc.identifier.urihttp://dspace.mist.ac.bd:8080/xmlui/handle/123456789/964
dc.language.isoenen_US
dc.publisherResearch and Development Wing, MISTen_US
dc.subjectShale rock masses, Silt layers, Slope stability, Elasto-plastic model, Temporal degradationen_US
dc.titleThe Influence of Silt Layer Orientation on Slope Stability in Shale Formationsen_US
dc.typeArticleen_US

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