浮冰的水弹性响应和波散射场研究

Xi Zhang, Tingqiu Li, Zuyuan Liu
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引用次数: 0

摘要

边缘冰区(MIZ)是海冰和开阔水域之间的区域,其结构主要由波浪和冰的相互作用决定。因此,掌握边缘冰区的特征对北极航线开辟和自然资源开发具有重要意义。本文研究了浮冰在波浪中的水弹性响应,基于计算流体力学(CFD)技术建立了三维数值波浪槽。离散流体域和冰域分别采用有限体积法(FVM)和有限元法(FEM)。在流体域和浮冰域的交界处创建了一个映射界面,通过形状函数插值法和最小二乘法进行数据映射。本研究通过一系列数值模拟来研究波浪与浮冰的流固相互作用(FSI)。在给定的入射波参数下,研究了不同形状的浮冰在波浪激励下的垂直弯曲变形、浮冰变形对波场的影响,并强调了波浪冲刷对透射波场的影响。结果表明,浮冰的形状对其弹性变形和散射波场有显著影响,而波浪冲刷现象则会衰减散射波。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Research on the hydroelastic response of ice floes and wave scattering field
The marginal ice zone (MIZ) is the area between sea ice and open water, the structure of which is mainly determined by wave and ice interactions. Thus mastering the characteristics of MIZ is of great significance to the Arctic routes opening and the natural resources development. In this paper, the hydroelastic response of ice floes in waves is studied, a three-dimensional numerical wave tank is established based on the computational fluid dynamics (CFD) technology. The finite volume method (FVM) and finite element method (FEM) are respectively utilized for discrete fluid domain and ice domain. A mapping interface at the junction of the fluid and ice floes domains is created to perform data mapping by the shape function interpolation method and the least square method. This work presents a series of numerical simulations to study the fluid-solid interaction (FSI) of waves and ice floes. Under the given incident wave parameters, the vertical bending deformation of ice floes with different shapes under the excitation of waves, the effect of ice floes' deformation on the wave field are studied, and the effect of wave overwash on the transmitted wave field is emphasized. Results show that the shape of the ice floes significantly affects its elastic deformation and scattered wave field, and the wave overwash phenomenon attenuates the scattering wave.
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