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The Frost Heave Calculation of Permafrost Pipeline

机译:永久冻土管道的霜冻升降计算

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Frost heave is the primary factor for potential destruction of the permafrost pipeline. Considering the Fenghuoshan area of the Ge-La Pipeline, the paper develops the finite element model for frost heave, and determines the amount of frost heave, frost stress around the pipe and Von Mises equivalent stress of the pipe wall, based upon the coupled thermo-mechanical method. The results indicate that the direction of frost heave is essentially vertical; the maximum frost stress occurs in the soil adjacent to the central section of the pipe, and the maximum Von Mises equivalent stress occurs at the top of the pipe. Based on a sensitivity analysis, the frost stress and Von Mises equivalent stress diminish with an increase of trench width and buried depth. The relationship between the frost stress and Von Mises equivalent stress and the pipe diameter and trench obliquity is rather complex. The frost stress value reaches a peak when the diameter is 150mm, and the Von Mises equivalent stress value reaches a peak when the trench obliquity is 10 degrees. The above results and methods have important significance for the design and construction of a permafrost pipeline.
机译:霜冻是永久冻土管道潜在破坏的主要因素。考虑到GE-LA管道的凤凰山地区,该纸张开发了霜冻升降的有限元模型,并根据耦合的热量确定霜冻升降量,管道周围的霜冻压力和von的等效应力,基于耦合的热量 - 机械方法。结果表明,霜冻的方向基本上是垂直的;在与管道中央部分相邻的土壤中发生最大霜应力,并且在管道顶部发生最大VONS等效应力。基于灵敏度分析,霜冻应力和von误差等同的应力随着沟槽宽度和埋深深度而增加。冰霜应力和von之间的关系相当于应力和管道直径和沟槽倾斜相当复杂。当直径为150mm时,霜应力值达到峰值,并且当沟槽倾斜度为10度时,von误差等效应力值达到峰值。上述结果和方法对永久冻土管道的设计和构建具有重要意义。

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