由部分静止海洋波引起的多孔海底的动态反应和液化潜力
Guocai Wang1,2, Yiyang Liu3, Kai Liu4
1Zhejiang Key Laboratory of Civil Engineering Structures & Disaster Prevention and Mitigation Technology, Zhejiang University of Technology, Hangzhou, 310023, China. wgc@zjut.edu.cn.
Scientific reports
|November 5, 2023
概括
海洋波反射显著影响多孔海底动力学和液化潜力. 完全反射的静电波可以将海底液化深度增加80%以上,这对沿海工程设计至关重要.
科学领域:
- 地质技术工程 地质技术工程
- 海洋学 海洋学 海洋学
- 沿海工程 沿海工程
背景情况:
- 设计海上结构需要了解海洋波对多孔海底的影响.
- 海底动态反应和液化是沿海和地质工程中的关键因素.
研究的目的:
- 开发一种分析解决方案,用于分析在部分静止海浪下波弹性海底的动态反应和液化潜力.
- 研究波浪反射和其他海底参数对动态反应和液化潜力的影响.
主要方法:
- 使用Biot的理论对合变形和流体流动进行多孔海底的建模.
- 用线性波理论描述海洋波,并应用混合边界值条件.
- 导出海底移位,有效应力和多余孔水压的明确表达式.
主要成果:
- 静止波的反射系数显著影响海床的动态反应和液化潜力.
- 完全反射的静止波在特定条件下将海底液化深度提高了82.49%.
- 诸如相位滞后,波浪周期,水深,和度,透度和剪切模量等参数会影响海底反应.
结论:
- 静止波反射是海底多孔弹性行为的一个关键因素.
- 分析解决方案提供了一种方法来预测波浪诱导的海底反应和液化.
- 研究结果为设计更安全,更有弹性的海上结构和防波堤提供了指导.
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