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Advances in Offshore Seismic Slope Stability: A Case History

机译:近海地震边坡稳定性研究进展

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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:本文介绍了一个案例历史,说明了详细的地球物理和岩土数据以及先进的数值模型的集成如何克服常规分析在预测decpwater边坡的地震稳定性方面的局限性。海底滑坡代表了海上管道和深水碳氢化合物开发的最关键的生态危害之一。对于地震可能是触发机制的地震活跃地区尤其如此。在这些情况下遇到的典型问题是以下几个方面并存:浅层沉积物的不良地质力学特性;陡坡的存在;和/或剧烈地震输入。这些方面的结合常常使常规的拟静力边坡稳定性分析的结果与现场观测结果难以匹配。这些方法对于深水条件通常是保守的,并且不能重现观察到的过去失效模式。该案例历史涉及地中海复杂的斜坡系统。从形态上讲,该系统具有许多峡谷和大规模的滑坡特征,并被数量有限的浅层平面滑坡所覆盖。地质年代学测试将大型的深层滑坡限制在遥远的过去,同时确认了浅层滑坡是最近的现象。高质量采样和高级实验室测试的使用为使用OpenSees软件进行动态非线性FEM分析提供了必要的输入。基于一组实时历史的数值结果证实了野外观察,并强调了地震触发的浅层滑坡的可能形成。本文描述了地球物理数据,准确的土壤采样和先进的实验室测试以及先进的数值模型如何在困难的环境条件下为项目开发可靠的边坡稳定性评估。

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