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    Hydrodynamic tests on a fixed plate in uniform flow

    Access Status
    Fulltext not available
    Authors
    Klaka, Kim
    Penrose, John
    Horsley, Richard
    Renilson, M.
    Date
    2005
    Type
    Journal Article
    
    Metadata
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    Citation
    Klaka, Kim and Penrose, John and Horsley, Richard and Renilson, Martin. 2005. Hydrodynamic tests on a fixed plate in uniform flow. Experimental Thermal and Fluid Science. 30 (2): pp. 131-139.
    Source Title
    Experimental Thermal and Fluid Science
    DOI
    10.1016/j.expthermflusci.2005.04.002
    Faculty
    Centre for Marine Science and Technology
    School of Science
    Faculty of Science and Engineering
    School
    Centre for Marine Science & Technology (COE)
    Remarks

    The link to the journal's home page is: http://www.elsevier.com/wps/find/journaldescription.cws_home/505737/description#description

    Copyright © 2005 Elsevier Ltd. All rights reserved

    URI
    http://hdl.handle.net/20.500.11937/24665
    Collection
    • Curtin Research Publications
    Abstract

    The forces and moments acting on a vertical flat plate in open flow running normal to the surface of the plate have been subject to investigation for several decades. However, the forces and moments acting on surface-piercing plates, plates slightly inclined to the vertical and plates extending close to a lower boundary have not received such attention. A series of experiments was conducted as part an investigation into the hydrodynamics of sailing yacht keels, with particular application to the case of a yacht drifting laterally down stream. The results may be of value for a wider range of engineering problems involving the flow of water over surface-piercing plates. It was found that drag force and heel moment varied approximately as flow speed squared for all plates investigated; the influence of plate angle on drag coefficient was small, with no clear trend; the magnitude of the drag coefficients for the surface-piercing plates was greater than for published data on fully submerged plates; and the centre of pressure was at approximately 50% of the span. The data scatter at low Froude numbers restricts the validity of these conclusions to Froude numbers greater than 0.1.

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