Seismic Coefficients for Simplified Deepwater Slope Stability Assessment Under Earthquake Loading

A. Trandafir
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Abstract

Pseudostatic limit-equilibrium based slope stability analyses are carried out on a routine basis to evaluate stability of submarine slopes under earthquake loading. For slopes in deepwater settings, a major challenge in performing pseudostatic slope stability analyses is selection of an appropriate seismic coefficient. Most published displacement-based methodologies for seismic coefficient selection were developed using simplified sliding block models for seismic slope performance evaluation that are unable to capture the complex deformation mechanism of deepwater slopes during earthquakes. To address this challenge, this study employs two-dimensional dynamic finite-element based deformation analysis to investigate the earthquake response of submarine clay slopes characterized by morphology, stratigraphic architecture and geotechnical properties representative for the deepwater environment. Finite-element computed seismic slope performance indicators, including horizontal peak ground acceleration at the seafloor and earthquake-induced maximum shear strain within the slope, along with horizontal seismic coefficients required to trigger slope instability in limit-equilibrium based pseudostatic stability analyses are used to develop a rational shear strain-based correlation relationship for deepwater slope seismic coefficient selection.
地震荷载作用下简化深水边坡稳定性评价的地震系数
基于拟静力极限平衡的边坡稳定性分析是评价地震作用下海底边坡稳定性的常规方法。对于深水环境下的斜坡,进行假静力坡稳定性分析的主要挑战是选择合适的地震系数。大多数已发表的基于位移的地震系数选择方法是使用简化滑动块模型开发的,用于地震边坡性能评估,无法捕捉地震期间深水边坡的复杂变形机制。为了解决这一挑战,本研究采用基于二维动态有限元的变形分析来研究具有深水环境特征的海底粘土边坡的地震响应,这些边坡具有形态、地层结构和岩土力学性质。利用有限元计算的地震边坡性能指标,包括海底水平峰值地面加速度和边坡内地震引起的最大剪切应变,以及基于极限平衡的伪静力稳定性分析中触发边坡失稳所需的水平地震系数,建立了基于剪切应变的合理关联关系,用于深水边坡地震系数选择。
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