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考虑锚胫作用下拖曳锚在成层土中的嵌入机制

熊树森 黄蕴晗 赖莹

岩土力学2024,Vol.45Issue(5):1495-1504,10.
岩土力学2024,Vol.45Issue(5):1495-1504,10.DOI:10.16285/j.rsm.2023.0835

考虑锚胫作用下拖曳锚在成层土中的嵌入机制

Embedment mechanism of a drag anchor in layered soils considering shank effect

熊树森 1黄蕴晗 2赖莹3

作者信息

  • 1. 浙江大学超重力研究中心,浙江杭州 310058
  • 2. 江苏海洋大学土木与港海工程学院,江苏连云港 222002
  • 3. 浙江大学建筑工程学院,浙江杭州 310058
  • 折叠

摘要

Abstract

The development of deep water mooring system and its mooring foundation has become a key issue in the development of clean energy"offshore wind power"projects.The drag embedment anchor,owing to its high bearing capacity and ease of installation,presents promising prospects.A prediction model for the trajectory,pitch angle and capacity of the anchor in layered soil,considering the effect of shank,is established based on the upper limit analysis.Verification of the model using existing model tests demonstrates that the trajectory prediction error of the model,accounting for the shank effect is limited to 13.5%.Furthermore,compared with the model that does not consider the shank effect,the trajectory and angle prediction error are reduced by 78.32%and 36.9%respectively.The strength,thickness and depth of stiff layer jointly restrict the embedding capability of the anchor.The influence of strength is found to be the most significant,with a higher strength ratio leading to a shallower embedding depth until the stiff layer becomes impenetrable.Additionally,greater depth is associated with increased bearing capacity.When the stiff layer can be penetrated,depth has minimal impact on trajectory and angle.However,when the stiff layer cannot be penetrated,the greater depth will result in a deeper embedment depth and smaller final angle.Lastly,the thickness of the stiff layer is found to positively correlate with the bearing capacity during the embedding process.

关键词

拖曳锚/预测模型/成层土/锚胫作用/轨迹

Key words

drag anchor/prediction model/layered soils/shank effect/trajectory

分类

建筑与水利

引用本文复制引用

熊树森,黄蕴晗,赖莹..考虑锚胫作用下拖曳锚在成层土中的嵌入机制[J].岩土力学,2024,45(5):1495-1504,10.

基金项目

国家自然科学基金(No.52279112).This work was supported by the National Natural Science Foundation of China(52279112). (No.52279112)

岩土力学

OA北大核心CSTPCD

1000-7598

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