首页> 外文会议>International conference on ocean, offshore and arctic engineering;OMAE2011 >LARGE DISPLACEMENT FINITE ELEMENT ANALYSIS OF SUBMARINE SLIDE DUE TO GAS HYDRATE DISSOCIATION
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LARGE DISPLACEMENT FINITE ELEMENT ANALYSIS OF SUBMARINE SLIDE DUE TO GAS HYDRATE DISSOCIATION

机译:天然气水合物分解对海底滑坡的大位移有限元分析

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Gas hydrate dissociation will reduce the stability of the submarine slope, which has been increasingly considered as a potential geohazard. In this study, a conventional geotechnical model is used to simulate gas hydrate dissociation while the thermal and geochemical effects are considered by reducing geotechnical strength parameters (c-Φ) and stiffness (E). The stability analysis of submarine slope due to gas hydrate dissociation is carried out using the large displacement finite element model - RITSS (Remeshing and Interpolating Technique with Small Strain model). The strength and stiffness parameters of gas hydrates are reduced gradually after each remesh according to the strength-dissociation relationship. The large displacement analysis procedure considering dissociation is given and the effects of the thickness of the top normal soil layer on slope stability is discussed.
机译:天然气水合物的解离会降低海底斜坡的稳定性,而海底斜坡的稳定性已被越来越多地视为潜在的地质灾害。在这项研究中,使用传统的岩土模型来模拟天然气水合物的分解,同时通过降低岩土强度参数(c-Φ)和刚度(E)来考虑热和地球化学效应。利用大位移有限元模型-RITSS(小应变网格划分和插值技术),对因天然气水合物分解而引起的海底边坡进行了稳定性分析。每次重熔后,气体水合物的强度和刚度参数会根据强度-解离关系逐渐降低。给出了考虑解离的大位移分析程序,并讨论了顶部正常土层厚度对边坡稳定性的影响。

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