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Advances in Offshore Seismic Slope Stability: A Case History

机译:海上地震坡稳定性进展:案例历史

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This paper presents a case history showing how the integration of detailed geophysical and geotechnical data and advanced numerical modeling can overcome the limitations of conventional analysis in predicting seismic stability of decpwater slopes. Submarine landslides represent one of the most critical gcohazards for offshore pipelines and deepwater hydrocarbon developments. This is particularly true for seismically active regions where earthquakes are expected to be a triggering mechanism. A typical issue encountered in these cases is the coexistence of several detrimental aspects: poor geomechanical properties of shallow sediments; presence of steep slopes; and/or severe seismic input. The combination of these aspects often makes it difficult to match results of conventional pseudo-static slope stability analysis with field observations. These methods are generally conservative for deepwater conditions and are not able to reproduce observed past failures modes. This case history is of a complex slope system in the Mediterranean Sea. Morphologically the system presents a number of canyons and large-scale landslide features, overlain by a limited number of shallow planar slides. Geochronological testing constrained the large, deep slides to the distant past while confirming the shallow slides as recent phenomena. The use of high quality sampling and advanced laboratory tests provided the necessary input for dynamic nonlinear FEM analyses using OpenSees software. Numerical results based on a set of real time histories confirmed field observations and highlighted the possible formation of seismically triggered shallow slides. The paper describes how geophysical data, accurate soil sampling and advanced laboratory testing together with an advanced numerical model can develop reliable slope stability assessments for projects in difficult environmental conditions.
机译:本文提出了一种案例历史,展示了详细地球物理和岩土地数据和先进的数值模型的集成如何克服常规分析预测Deppwater斜坡的地震稳定性的局限性。潜艇山体滑坡代表了海上管道和深水碳氢化合物发展中最关键的Gcohazard之一。这对于地震活动区域尤其如此,其中地震预期是触发机制。在这些情况下遇到的典型问题是若干不利方面的共存:浅层沉积物的地质力学性质差;陡坡的存在;和/或严重的地震投入。这些方面的组合通常使得难以通过现场观测匹配传统伪静态斜面稳定性分析的结果。这些方法通常是保守的深水条件,并且不能再现出现过去的失败模式。这种情况历史是地中海的复杂斜坡系统。形态学上系统呈现了许多峡谷和大规模滑坡特征,通过有限数量的浅平面幻灯片覆盖。地理论系测试限制了遥远的过去的大,深幻灯片,同时确认浅幻灯片作为最近的现象。使用高质量采样和先进的实验室测试提供了使用Opensees软件的动态非线性分析的必要输入。基于一组实时历史的数值结果证实了现场观察,并突出了地震触发浅幻灯片的可能形成。本文介绍了地球物理数据,准确的土壤采样和先进的实验室测试以及先进的数控模型如何为困难环境条件的项目开发可靠的边坡稳定性评估。

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