The Effect of Ground Displacement and Stress Relief on Pipeline Behaviour: A Case Study

H. Karimian, Chris Campbell, C. Blackwell, C. Dooley, P. Barlow
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Abstract

The Wapiti River South Slope is located 25 km southwest of Grande Prairie, AB. The slope is 500 m long and consists of a steep lower slope and a shallower upper slope, both of which are located within a landslide complex with ground movements of varying magnitudes and depths. The Alliance Pipelines Ltd. (Alliance) NPS 42 Mainline (the pipeline) was installed in the winter of 2000 using conventional trenching techniques at an angle of approximately 8° to the slope fall line. Evidence of slope instability was observed in the slope since the first ground inspection in 2007. Review of the available geotechnical data indicates two different slide mechanisms. In the lower slope, there is a shallow translational slide within a colluvium layer that is draped over a stable bedrock formation. In the upper slope, there is a deep-seated translational slide within glaciolacustrine and glacial till deposits that are underlain by pre-glacial fluvial deposits. Both the upper and lower slope landslide mechanisms have been confirmed to be active in the past decade. Large ground displacements in the order of several meters between 2012 and 2014 in the lower slope led to a partial stress relief and subsequent slope mitigation measures in the spring and summer of 2014, which significantly reduced the rate of ground movement in the lower slope. Surveying of the pipeline before and after stress relief indicated an increase in lateral pipeline deformation (in the direction of ground movement) following the stress relief. This observation was counter-intuitive and raised questions regarding the effectiveness of partial stress relief to reduce stresses and strains associated with ground movements. Finite element analysis (FEA) was conducted in 2017 to aid in assessing the condition of the pipeline after being subject to the aforementioned activities, and subsequent ground displacement from July 2014 to December 2016. This paper presents the assumptions and results of the FEA model and discusses the effect of large ground displacement, subsequent stress relief and continued ground displacement on pipeline behaviour. The results and findings of the FEA reasonably match the observed pipeline behaviour before and after stress relief. The FEA results showed that while the lateral displacement of the pipeline that was caused by ground movement actually increased following the removal of the soil loading, the maximum pipeline strain was reduced in the excavated portion. The results also indicated that ground displacement in the upper slope following the stress relief had minimal effect on pipe stresses and strains in the lower slope.
地面位移和应力释放对管道性能的影响:一个实例研究
Wapiti河南坡位于美国AB州Grande Prairie西南25公里处。该坡长500米,由陡峭的下坡和较浅的上坡组成,这两个斜坡都位于一个滑坡综合体内,其地面运动强度和深度都不同。联盟管道有限公司(Alliance)的NPS 42干线(管道)于2000年冬季安装,采用传统的沟槽技术,与斜坡落差线的角度约为8°。自2007年第一次地面检查以来,在边坡中观察到边坡失稳的证据。对现有岩土数据的回顾表明了两种不同的滑动机制。在较低的斜坡上,有一个覆盖在稳定的基岩地层上的崩积层内的浅平移滑动。在上斜坡,在冰川期前的河流沉积下的冰湖和冰碛物沉积物中存在深层平移滑动。近十年来,上、下两坡滑坡机制都被证实是活跃的。2012年至2014年期间,下边坡发生了数米量级的大位移,导致2014年春夏进行了部分应力消除和后续的减坡措施,显著降低了下边坡的地面移动速度。应力消除前后的管道测量表明,应力消除后,管道侧向变形(在地面移动方向上)增加。这一观察结果是违反直觉的,并提出了关于局部应力释放以减少与地面运动有关的应力和应变的有效性的问题。2017年进行了有限元分析(FEA),以帮助评估管道在受到上述活动影响后的状况,以及2014年7月至2016年12月期间的后续地面位移。本文给出了有限元模型的假设和结果,并讨论了大的地面位移、随后的应力释放和持续的地面位移对管道性能的影响。有限元分析的结果和发现与应力消除前后观察到的管道行为相当吻合。有限元分析结果表明,土体荷载解除后,地面移动引起的管道侧向位移增大,但开挖部分管道最大应变减小。结果还表明,应力释放后上边坡的地面位移对下边坡管道应力应变的影响最小。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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