Transcritical Flow Over a Bump using Forced Korteweg-de Vries Equation

IF 0.3 Q4 MATHEMATICS
Vincent David, A. Bahar, Z. A. Aziz
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引用次数: 2

Abstract

The flow of water over an obstacle is a fundamental problem in fluid mechanics. Transcritical flow means the wave phenomenon near the exact criticality. The transcritical flow cannot be handled by linear solutions as the energy is unable to propagate away from the obstacle. Thus, it is important to carry out a study to identify suitable model to analyse the transcritical flow. The aim of this study is to analyse the transcritical flow over a bump as localized obstacles where the bump consequently generates upstream and downstream flows. Nonlinear shallow water forced Korteweg-de Vries (fKdV) model is used to analyse the flow over the bump. This theoretical model, containing forcing functions represents bottom topography is considered as the simplified model to describe water flows over a bump. The effect of water dispersion over the forcing region is investigated using the fKdV model. Homotopy Analysis Method (HAM) is used to solve this theoretical fKdV model. The HAM solution which is chosen with a special choice of }-value describes the physical flow of waves and the significance of dispersion over abump is elaborated.
用强迫Korteweg-de-Vries方程求解凸块上的跨临界流动
水在障碍物上的流动是流体力学中的一个基本问题。跨临界流动是指在精确临界附近的波动现象。跨临界流不能由线性解处理,因为能量不能传播离开障碍物。因此,进行研究以确定合适的模型来分析跨临界流动是很重要的。本研究的目的是将凸块上的跨临界流动分析为局部障碍物,从而使凸块产生上游和下游流动。非线性浅水强迫Korteweg-de-Vries(fKdV)模型用于分析凸块上方的流动。该理论模型包含代表底部地形的强迫函数,被认为是描述凸起上方水流的简化模型。利用fKdV模型研究了强迫区上的水分散效应。利用同源分析法(HAM)求解该理论fKdV模型。通过特殊的}-值选择的HAM解描述了波的物理流动,并阐述了在abump上色散的意义。
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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来源期刊
Matematika
Matematika MATHEMATICS-
自引率
25.00%
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0
审稿时长
24 weeks
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