海底陡坡泥石流事件的地质灾害研究及穿越管线的结构响应:第二部分- CFD和FSI分析

Hyunchul Jang, L. Lai, K. Hayes, Anthony Musto
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引用次数: 0

摘要

由于海底地震,海底可能会发生泥石流。这些极端事件对海底管线和设备的结构完整性有重大影响。对发生在悬崖上的海底泥石流事件进行了数值地质灾害研究。该研究的目的是确定在极端泥石流事件下,两条管线和一条脐带缆穿过悬崖区域的结构响应,并评估对额外稳定辅助设备的需求。该研究使用了几种数值方法,如计算流体动力学(CFD)、有限元分析(FEA)和流固耦合(FSI)。首先考虑了不同级别的CFD模型(不含流线),以显示在考虑粘性海水柱、粘塑性多层土壤和高流动性泥浆相的最终CFD模型中加入额外物理因素的影响。该CFD模拟每隔1 s提取一次泥石流速度场,并应用于Abaqus有限元模拟方法。这在另一篇论文[1]中提出。本文采用FSI模拟方法,将泥石流碎屑的演变与有限元流线模型直接耦合。这使得有限元模型可以不断更新由泥石流运动产生的载荷。根据位移形状和结构载荷对流线结构响应进行了监测和评估。该方法通过考虑海水、多层土壤和泥浆层的粘性效应,减少了传统方法的保守性。这项研究的主要发现是,泥石流事件并没有显著地改变悬崖上的流线。两条管线的响应都在结构设计限制内。研究还发现锚定对结构响应没有显著影响。然而,脐带缆的压缩极限超出了设计极限的四倍。这是由于高速泥前缘与最初静止的脐带相互作用,并在泥石流事件的初始阶段将其推向压缩状态。提出的解决方案是线路改道,这有助于将压缩水平降低到设计限制内。该分析有助于降低项目的资本支出和安装成本,不需要额外的脐带压缩缓解组件,也省去了预先计划的锚。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geohazard Study of Mudslide Event at a Subsea Escarpment and Structural Response of Crossing Flowlines: Part II – CFD and FSI Analysis
Mudslides can occur on the seafloor due to subsea earthquakes. These extreme events have a significant impact on the structural integrity of subsea flowlines and equipment. A numerical geohazard study was performed on a subsea mudslide event occurring at an escarpment. The study objective was to determine the structural response of two flowlines and one umbilical crossing an escarpment area subject to the extreme mudslide event and to assess requirement for additional stabilization ancillaries. The study utilized several numerical methodologies such as Computational-Fluid-Dynamics (CFD), Finite-Element-Analysis (FEA), and Fluid-Structure-Interaction (FSI). Different levels of CFD models were first considered (without flowlines) to show the effect of including additional physics with the final CFD model considering a viscous seawater column, viscoplastic multi-layered soil and high-mobility mud phases. The mudslide velocity field from this CFD simulation is extracted at every 1 s and applied to the Abaqus FEA simulation approach. This is presented in a separate paper [1]. The current paper utilized a FSI simulation approach where the evolution of mudflow debris is directly coupled with the FEA flowline model. This allows the FEA model to continuously update loading created by the mudslide motion. The flowline structural responses were monitored and assessed in terms of displaced shapes and structural loading. This methodology reduces conservatism over conventional approaches by considering viscous effects of the seawater, multi-layer soil and mud layers. Key findings from the study is that the mudslide event did not significantly displace flowlines over the escarpment. The two flowline responses were within structural design limits. It was also found anchoring did not significantly affect structural responses. The umbilical line, however, exceeded compression limits by four times the design limit. This is due to the high velocity mud-front interacting with an initially stationary umbilical and pushing it into compression during the initial stages of the mudslide event. The solution proposed was line rerouting which helped reduce compression levels to within design limits. This analysis assisted the project in CAPEX and installation cost reduction with no requirement of further umbilical compression mitigation components, and the omission of the pre-planned anchors.
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