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波浪作用下粉质土海床液化界面波压力的研究

任宇鹏 房虹汝 许国辉 许兴北

任宇鹏, 房虹汝, 许国辉, 许兴北. 波浪作用下粉质土海床液化界面波压力的研究[J]. 海洋学报, 2017, 39(1): 89-95. doi: 10.3969/j.issn.0253-4193.2017.01.009
引用本文: 任宇鹏, 房虹汝, 许国辉, 许兴北. 波浪作用下粉质土海床液化界面波压力的研究[J]. 海洋学报, 2017, 39(1): 89-95. doi: 10.3969/j.issn.0253-4193.2017.01.009
Ren Yupeng, Fang Hongru, Xu Guohui, Xu Xingbei. Wave pressure on the boundary of liquefied silty seabed under wave loading[J]. Haiyang Xuebao, 2017, 39(1): 89-95. doi: 10.3969/j.issn.0253-4193.2017.01.009
Citation: Ren Yupeng, Fang Hongru, Xu Guohui, Xu Xingbei. Wave pressure on the boundary of liquefied silty seabed under wave loading[J]. Haiyang Xuebao, 2017, 39(1): 89-95. doi: 10.3969/j.issn.0253-4193.2017.01.009

波浪作用下粉质土海床液化界面波压力的研究

doi: 10.3969/j.issn.0253-4193.2017.01.009
基金项目: 国家自然科学基金——海底粉质土液化重建地层特征及其风暴浪动力强度研究(41576039)。

Wave pressure on the boundary of liquefied silty seabed under wave loading

  • 摘要: 波浪作用下粉质土海床的液化是影响海上平台、海底管线等海洋构筑物安全的灾害之一。在进行构筑物设计中应考虑海床液化的深度问题,而液化土体对下部海床的界面波压力是计算海床孔隙水压力增长以及液化深度的重要参量。本文基于波致粉土海床自上而下的渐进液化模式,利用双层流体波动理论,推导了考虑海床土体黏性的海床界面波压力表达式,并与不考虑黏性时的界面波压力进行了比较分析。结果表明,计算液化后土体界面波压力时,是否考虑液化土体的黏性对结果影响较大,进而可能影响粉质土海床液化深度的确定。
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出版历程
  • 收稿日期:  2016-04-07
  • 修回日期:  2016-05-10

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