Synergies Between VLFS Hydroelasticity And Sea-Ice Research
Synergies Between VLFS Hydroelasticity And Sea-Ice Research
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DOI：
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发表时间：
2008
影响因子：
0.8
通讯作者：
V. Squire
中科院分区：
文献类型：
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作者：
V. Squire
一个明显的重叠之间存在的出版物，描述海冰如何响应海浪场和那些涉及到一个非常大的浮动结构（VLFS）经历类似的强迫。当代水弹性理论已经同时但独立地开发，尽管正在研究的主题和应用的方法的相似性。虽然海冰是一种天然的异质材料，在所有空间尺度上都表现出可变性，例如它可能包含裂缝，开放和重新冻结的引线，压力脊，或厚度或性质的逐渐或突然变化，但VLFS也可能是不均匀的-特别是当它们由具有不同材料模量或形状的几个相互连接的部分制成时。在这项工作中，基本的数学理论和物理学的发展，水弹性的特点，从两个语料库和提请注意的连接和解释，可能有利于这两个领域的研究。特别注意解释显然无关的分析，其中存在的潜在关系不一定是显而易见的。
A conspicuous overlap exists between publications that describe how sea-ice responds to an ocean wave field and those that relate to a very large floating structure (VLFS) experiencing comparable forcing. Contemporary hydroelastic theory has been developed concurrently yet independently despite the similarity of the topics being studied and the methods being applied. While sea-ice is a natural heterogeneous material that shows variability on all spatial scales, e.g. it may contain cracks, open and refrozen leads, pressure ridges, or gradual or abrupt changes of thickness or property, VLFSs can also be nonuniform – particularly when they are manufactured from several interconnected parts with differing material moduli or shapes. In this work the basic mathematical theory and physics is developed that characterizes hydroelasticity, drawing from both corpora and calling attention to connexions and interpretations that could benefit both spheres of research. Particular attention is given to explaining apparently unrelated analyses where an underlying relationship exists that is not necessarily plainly evident.