{"title":"Pseudo-inviscid theory for transom-stern flow at low Froude numbers","authors":"Lawrence J. Doctors","doi":"10.1016/j.apor.2024.104332","DOIUrl":null,"url":null,"abstract":"<div><div>A simple model of the water flow behind a transom stern is presented. The water is assumed to separate cleanly from the bottom of the transom and it is considered that this domain of the flow is inviscid. Immediately aft of the transom is a stagnant region, in which the pressure can be computed on purely hydrostatic grounds. It is this hydrostatic pressure that acts upon the free-surface of the first water domain. Linearized free-surface theory is utilized to perform the analysis. The theoretical results for the length of the hollow and its profile area are seen to be much higher than the experimental data would suggest. It is thought that the source of the discrepancy is the hydraulic jump in the free surface which cannot be modeled using the current theory.</div></div>","PeriodicalId":8261,"journal":{"name":"Applied Ocean Research","volume":"154 ","pages":"Article 104332"},"PeriodicalIF":4.4000,"publicationDate":"2025-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Applied Ocean Research","FirstCategoryId":"5","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S014111872400453X","RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"2024/12/2 0:00:00","PubModel":"Epub","JCR":"Q1","JCRName":"ENGINEERING, OCEAN","Score":null,"Total":0}
引用次数: 0
Abstract
A simple model of the water flow behind a transom stern is presented. The water is assumed to separate cleanly from the bottom of the transom and it is considered that this domain of the flow is inviscid. Immediately aft of the transom is a stagnant region, in which the pressure can be computed on purely hydrostatic grounds. It is this hydrostatic pressure that acts upon the free-surface of the first water domain. Linearized free-surface theory is utilized to perform the analysis. The theoretical results for the length of the hollow and its profile area are seen to be much higher than the experimental data would suggest. It is thought that the source of the discrepancy is the hydraulic jump in the free surface which cannot be modeled using the current theory.
期刊介绍：
The aim of Applied Ocean Research is to encourage the submission of papers that advance the state of knowledge in a range of topics relevant to ocean engineering.
京公网安备 11010802042870号
京ICP备2023020795号-1
分享
求助内容：
应助结果提醒方式：
扫码关注我们
