沙波区域海底管道侧向土抗力响应试验研究

    Experimental Study on the Mechanism of Lateral Resistance of Submarine Pipelines in the Sandwave Area

    • 摘要: 海底管道作为油气输送的关键设施,因其大跨度细长的结构特征,不可避免地需穿越地貌起伏的海底区域。但现行国际规范及主流研究多忽略地貌起伏影响,成果聚焦于平坦或倾斜海床。然而,沙波的存在改变了管-土接触状态及边界条件,其对管道侧向土抗力的影响尚不明确,给工程设计带来了显著的不确定性。针对该问题,系统开展了海底管道侧向土抗力模型试验研究。设计了不同沙波高度、长度、管-波间距试验组及平坦海床对照组等多组工况,重点探究了管-土相互作用响应曲线、管道破土抗力及管道运动模式的响应规律。并通过PIV技术提取了管道破土过程中土颗粒流动位移矢量图及管前土体的连续位移云图和最大剪应变云图,观测了管前土颗粒的运动趋势、滑裂面演变过程和破坏角度,并据此划分了管前土体机动场。研究发现,与DNV规范中平坦砂土海床三段式模型不同,在干砂及完全排水状态饱和砂土条件下,平坦海床与沙波海床的管道侧向土抗力曲线均呈现无明显应变软化阶段的两段式特征。然而,沙波的存在显著改变了具体的破坏机制:它使得破土模式由平坦海床的单一模式演变为波前穿出、穿透沙波及跨越沙波三种典型模式;同时,沙波参数的改变会显著影响管前土体破坏角度及被动土抗力系数,进而影响管道破土抗力值。该研究可为复杂地貌海底管道稳定性评估提供重要依据。

       

      Abstract: Subsea pipelines, as key infrastructure for offshore oil and gas transport, inevitably cross irregular seabed terrain due to their long-span, slender configuration. Existing international design codes and most prior studies largely idealize the seabed as flat or uniformly sloping, and therefore overlook the effects of geomorphic features such as sand waves. Yet, the presence of sand waves fundamentally alters pipe-soil contact conditions and boundary constraints, affecting lateral soil resistance and creating uncertainties in pipeline design. This study systematically investigates the lateral soil resistance of subsea pipelines through model tests examining various configurations of sand wave heights, lengths, and pipe-wave spacings alongside a flat seabed control. The experimental programme focused on the pipe-soil interaction response curves, the breakout resistance, and the resulting pipeline motion modes. Using Particle Image Velocimetry (PIV), we extracted soil particle displacement vectors, continuous displacement and shear strain contour maps during pipeline penetration, revealing soil kinematics, slip surface evolution, failure angles, and the corresponding kinematic zones. It is found that different from the DNV three-stage lateral resistance model for flat sandy seabeds, the pipeline lateral response on flat and sand-wave seabeds exhibits a two-stage characteristic without an obvious strain-softening stage under dry sand and fully drained saturated sand conditions. However, sand waves markedly alter failure mechanisms: the single breakout mode observed on flat seabeds transitions into crest breakout, intra-sand-wave penetration, and sand-wave overpassing on sand-wave terrain; variations in sand wave parameters notably affect the failure angle and passive resistance coefficients of the soil, impacting the breakout resistance. These findings provide a mechanistic basis for more reliable stability assessment and improved design of subsea pipelines in complex sand-wave seabed environments.

       

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