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Seabed Friction On Carbonate Soils: Physical Modelling of Axial Pipe-Soil Friction

机译:碳酸盐土壤上的海底摩擦:轴向管道-土壤摩擦的物理模型

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This paper is concerned with the ‘friction’ and ‘sliding resistance’ that can be mobilised on the unusualcarbonate sediments prevalent across many parts of the world, including Offshore Australia. Physicalcentrifuge model testing was conducted to evaluate the axial pipe-soil resistance on a soil obtained fromthe North West Shelf, offshore Australia. Tests were performed at a range of speeds, spanning drained/undrained conditions, interspersed with consolidation periods. The resulting axial friction factors aregenerally higher than is often assumed in conventional design practice for pipeline end expansion orbuckling and walking analysis, which is consistent with the high friction angles and dilatancy of theseangular carbonate soils. In addition, the results demonstrate the effect that soil drainage response andhistory of pipeline sliding movements can have on the axial-pipe friction. Overall, the results highlight theimportance of making site-specific assessments of seabed sliding resistance, rather than rely on non-sitespecificresults (particularly from different regions) that may display a very different soil response. Lastly,recommendations are made for design assessments of the sliding resistance of carbonate soils.
机译:本文关注的是可以动员的“摩擦”和“滑动阻力” 碳酸盐沉积物遍布世界各地,包括澳大利亚近海。身体的 进行了离心模型测试,以评估从 西北大陆架,澳大利亚近海。测试以一定速度进行,涵盖排空/ 不排水的条件,以及巩固期。产生的轴向摩擦系数为 通常高于常规设计实践中通常认为的管道端部扩展或 屈曲和行走分析,这与这些材料的高摩擦角和扩张性是一致的 角质碳酸盐土壤。此外,结果证明了土壤排水反应和 管道滑动的历史可以对管道的轴向产生摩擦。总体而言,结果突出了 进行特定地点的海床滑动阻力评估的重要性,而不是依赖非特定地点的评估 结果(尤其是来自不同地区的结果)可能显示出截然不同的土壤响应。最后, 针对碳酸盐土壤的滑动阻力的设计评估提出了建议。

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