A Probabilistic High-Pressure Zone Model of Dynamic Ice Structure Interactions and Associated Ice-Induced Vibrations

R. Hossain, R. Taylor, L. Moro
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Abstract

During ice-structure interactions that are dominated by ice compressive failure, the majority of the ice loads are transmitted through localized contact regions known as high-pressure zones (hpzs). This paper presents a probabilistic modelling framework for dynamic ice-structure interaction based on the mechanics of hpzs. Individual hpzs are modelled as a nonlinear spring-damper system where the stiffness is modelled as a function of nominal strain, with the degree of softening depending on the average strain-rate. Both spalling and crushing failure mechanisms were assessed in the context of periodical sinusoidal response. For spall dominated failure, the model structure showed presence of frequency lock-in in the speed range of 100–125mm/s, beyond which the failure was found to be random in nature with lower amplitude of structural response. The amplitude was also found to be significantly influenced by structural parameters with structural damping having the highest contribution. For pure crushing, an estimated equilibrium layer thickness based on theoretical calculations also showed presence of frequency lock-in. The work highlights the importance of understanding the interplay between these mechanisms, as well as the role of ice conditions and structural parameters on the processes that dominate an interaction.
动态冰结构相互作用和相关冰激振动的概率高压区模型
在以冰压缩破坏为主的冰-结构相互作用中,大部分冰荷载通过局部接触区域传递,称为高压区(hpzs)。本文提出了一种基于冰-结构动力相互作用的概率模型框架。单个hpz被建模为一个非线性弹簧-阻尼器系统,其中刚度被建模为标称应变的函数,软化程度取决于平均应变率。在周期性正弦响应的背景下,评估了剥落和破碎破坏机制。在100 ~ 125mm/s速度范围内,模型结构表现出频率锁住现象,超过该速度范围,结构响应幅值较低,失效本质上是随机的。振幅也受结构参数的显著影响,其中结构阻尼的贡献最大。对于纯破碎,基于理论计算的估计平衡层厚度也显示了频率锁定的存在。这项工作强调了理解这些机制之间相互作用的重要性,以及冰况和结构参数在主导相互作用的过程中的作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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