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SUBCRITICAL WAVE WAKE UNSTEADINESS

机译:次波唤醒不稳定

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摘要

Vessel wave wake in deep water is well understood, shallow water less so, specifically the effect of restricted water. This operational zone is highly dynamic and non-linear in nature, thus being worthy of closer examination. The paper reviews the primary mechanisms for unsteadiness in wave wake: starting acceleration and soliton generation. A comprehensive set of experiments was conducted using an NPL catamaran hull form to investigate unsteadiness in both wave height and wave angle. The results show that the unsteadiness was primarily due to soliton generation, and that blockage has a significant effect. As a result, additional metrics, aimed at defining shallow water effects in the transcritical region, are proposed.
机译:众所周知,深水区的船舶波唤醒,浅水区的唤醒较少,特别是限制水的作用。该操作区域本质上是高度动态和非线性的,因此值得仔细检查。本文回顾了波浪尾流不稳定的主要机制:开始加速和产生孤子。使用NPL双体船船体形式进行了一组全面的实验,以研究波高和波角的不稳定性。结果表明,不稳定主要归因于孤子的产生,并且阻塞具有显着影响。结果,提出了旨在定义跨临界区的浅水影响的其他指标。

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