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Three-dimensional poro-elastic integrated model for wave and current-induced oscillatory soil liquefaction around an offshore pipeline
Institution:1. Department of Bridge Engineering, School of Civil Engineering, Southwest Jiaotong University, Chengdu, 610031, China;2. State Key Laboratory of Ocean Engineering, Department of Civil Engineering, Shanghai Jiao Tong University, Shanghai, 200240, China;1. Key Laboratory for Mechanics in Fluid Solid Coupling Systems, Institute of Mechanics, Chinese Academy of Sciences, Beijing, 100190, China;2. School of Engineering Science, University of Chinese Academy of Sciences, Beijing, 100049, China;3. Civil Infrastructure Operations Dept, China State Construction Engineering Corp. Ltd, Beijing, 100044, China;1. Center for Marine Geotechnical Engineering, Department of Civil Engineering, State Key Laboratory of Ocean Engineering, Shanghai Jiao Tong University, Shanghai 200240, China;2. Griffith School of Engineering, Griffith University Gold Coast Campus, Queensland, QLD 4222, Australia;3. School of Civil Engineering, Southwest Jiaotong University, Chengdu, Sichuan 610031, China;1. State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing, Jiangsu, 210098, China;2. College of Harbour, Coastal and Offshore Engineering, Hohai University, Nanjing, Jiangsu, 210098, China;3. Technical University of Denmark, Department of Mechanical Engineering, DK-2800, Kgs. Lyngby, Denmark;4. School of Engineering and Built Environment, Griffith University Gold Coast Campus, Queensland, 4222, Australia;5. Faculty of Engineering and Informatics, University of Bradford, Bradford, BD7 1DP, UK
Abstract:To obtain a better understanding of the oscillatory soil liquefaction around an offshore pipeline, a three-dimensional integrated model for the wave–seabed–pipeline interaction (WSPI) is proposed by combining the Reynolds-Averaged Navier–Stokes equations for flow simulations and the dynamic Biot’s equation (“u-p” approximation) for the poro-elastic seabed model. Compared with previous investigations, the wave–current interaction is included in the present WSPI system. At a given time step, the wave pressure extracted from the flow model is applied on the seabed surface to determine the corresponding oscillatory seabed response around an offshore pipeline. The integrated numerical model is first validated using previous laboratory experiments. Then, a parametric study is conducted to examine the effects of flow obliquity and pipeline burial depth on the soil response around an offshore pipeline. Numerical results indicate that the soil under the pipeline is more susceptible to liquefaction at a reduced flow obliquity and pipeline burial depth. Moreover, the liquefaction depth in the case where the wave travels along the current can increase by 10%–30% compared to that in the case where the wave travels against the current, when the magnitude of the current velocity is 1 m/s.
Keywords:WCI  WSPI  Flow obliquity  Pipeline  Burial depth  Liquefaction
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