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A 3-DIMENSIONAL EULERIAN FINITE ELEMENT MODEL FOR ICE SCOUR

机译:冰激淋的三维二维EULERIAN有限元模型

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The main objective of this paper is to present a Finite Element (FE) numerical model of the ice scour process. The FE model is developed to study the soil deformation and transport process around the scouring ice and to investigate the effects of the ice scour on a pipeline buried or laid in a trench cut on the seabed. The focus of this paper is on the scours caused by ice ridges commonly observed in the Beaufort Sea. The developed FE model is a new application of the Arbitrary-Lagrangian-Eulerian (ALE) method to a soil mechanics problem involving very large deformations. Soil material, originally positioned in front of the ice ridge, is transported forward and sideways through the FE mesh and deposited in the berms formed on both sides of the scour. The soil material below the scour depth similarly moves across the mesh simulating the subscour effect. An inviscid CAP plasticity constitutive model is used to model the soil material. This paper focuses on the interaction between the ice ridge and the seabed. It describes soil transport process involved during the interaction. The soil deformation field obtained from the model is compared with the empirical deformation functions commonly used in current design methods. Future papers will report on the interaction between the ice ridge, the infill in the pipeline trench, and the pipeline; the influence of the soil properties of the trench and the seabed will also be studied.
机译:本文的主要目的是提出冰冲刷过程的有限元(FE)数值模型。有限元模型的开发是为了研究冲刷冰周围的土壤变形和运输过程,并研究冰冲刷对埋在海床挖沟中或埋在海床上的管道的影响。本文的重点是在波弗特海常见的冰脊造成的冲刷。开发的有限元模型是任意拉格朗日-欧拉(ALE)方法在涉及非常大变形的土壤力学问题中的新应用。最初位于冰岭前面的土壤物料通过有限元网格向前和向侧面运输,并沉积在冲刷两侧形成的护堤中。冲刷深度以下的土壤材料类似地在网格上移动,模拟了暗挖效应。使用无粘性CAP可塑性本构模型对土壤材料进行建模。本文着重于冰脊和海床之间的相互作用。它描述了相互作用过程中涉及的土壤运输过程。将模型获得的土壤变形场与当前设计方法中常用的经验变形函数进行比较。以后的论文将报道冰脊,管道沟槽中的填充物和管道之间的相互作用。还将研究海沟和海床的土壤特性的影响。

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