膨胀土边坡滑动与湿胀耦合作用对输油管道影响的模拟

Numerical simulation of the coupled effects of sliding and hygroscopic swelling in expansive soil slopes on oil pipelines

  • 摘要: 在膨胀土分布地区,输油管道受膨胀土边坡降雨软化滑动与湿胀耦合作用影响,可引发管道变形破裂,造成油气泄漏与爆炸等严重事故。本研究以南宁盆地某输油管道膨胀土边坡为例,通过室内干湿循环模拟试验,分析其强度劣化与膨胀变形特征。基于现场勘察与试验参数,建立边坡数值模型,引入湿胀本构模型,采用有限元流固耦合计算方法开展边坡变形破坏过程模拟计算。试验和数值模拟结果表明:研究区膨胀土强度随干湿循环次数增加而显著降低,黏聚力和内摩擦角降幅分别为59.73%和30.92%。在多轮降雨过程中,边坡膨胀土有效应力随含水率上升而持续下降,其强度随干湿循环而逐级降低,最终在第5次降雨后发生滑动破坏。位于滑坡前缘的输油管道受边坡软化滑动与吸湿膨胀综合影响,其后侧土压力随时间变化呈现出缓慢增大、加速增大与趋于平缓3个阶段,通过土压力变化侧面揭示了膨胀土边坡滑动与湿胀耦合作用造成输油管道初始受力、应力累积与最终破坏的渐进过程。管道临近破坏时其后侧土压力增长与位移出现显著解耦现象,即土压力增速放缓而位移急剧增大。上述现象和机制可为膨胀土边坡输油管道变形破坏预测模型与预警阈值建立提供科学参考依据。

     

    Abstract: In regions with expansive soil, oil pipelines are affected by rainfall-induced softening, sliding, and hygroscopic swelling of expansive soil slopes, leading to potential deformation and rupture. Such failures could result in severe accidents, including oil and gas leaks or explosions. Using an expansive soil slope in the Nanning Basin as a case study, laboratory drying-wetting cycle tests were conducted to examine the strength degradation and swelling deformation of the soil. Based on field investigations and experimental data, a numerical slope model was developed, incorporating a hygroscopic swelling constitutive model. The finite element fluid-structure interaction method was then applied to simulate the slope 's deformation and failure process. The experimental and numerical results demonstrated that the strength of expansive soil in the study area decreased significantly with increasing drying-wetting cycles, with cohesion and internal friction angle reductions of 59.73% and 30.92%, respectively. During multiple rainfall events, the effective stress of the expansive soil on the slope continuously declined as water content increased, leading to gradual strength degradation under drying-wetting cycles. Sliding failure ultimately occurred after the fifth rainfall. The oil pipeline at the landslide 's front edge was affected by the combined effects of slope softening, sliding, and hygroscopic swelling. The lateral earth pressure behind the pipeline exhibited three stages over time: slow increase, accelerated increase, and eventual stabilization. This progression reflected the pipeline 's initial loading, stress accumulation, and eventual failure due to the coupled effects of slope sliding and hygroscopic swelling. A significant decoupling between earth pressure and displacement was observed near pipeline failure: earth pressure accumulation decelerated, whereas displacement increased abruptly. These phenomena and mechanisms provide a scientific basis for developing deformation and failure prediction models and establishing early-warning thresholds for oil pipelines crossing expansive soil slopes.

     

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