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Experimental investigation and calibration of surface pressure modeling for trailing edge noise

    Research output: Chapter in Book/Report/Conference proceedingArticle in proceedingsResearchpeer-review

    Abstract

    The modeling of the surface pressure spectrum under a turbulent boundary layer is investigated in the presence of an adverse pressure gradient along the flow direction. It is shown that discrepancies between measurements and results from a well-known model increase as the pressure gradient increases. This model is modified by introducing anisotropy in the definition of the vertical velocity component spectrum across the boundary layer. The degree of anisotropy is directly related to the strength of the pressure gradient. It is shown that by appropriately normalizing the pressure gradient and by tuning the anisotropy factor, experimental results can be closely reproduced by the modified model.
    Original languageEnglish
    Title of host publicationProceedings of the 40th International Congress and Exposition on Noise Control Engineering 2011 (INTER-NOISE 2011)
    Publication date2011
    Pages222-228
    ISBN (Print)9781618392800
    Publication statusPublished - 2011
    EventINTER-NOISE 2011 : 40th International Congress and Exposition on Noise Control Engineering - Osaka, Japan
    Duration: 4 Sept 20117 Sept 2011
    Conference number: 40

    Conference

    ConferenceINTER-NOISE 2011 : 40th International Congress and Exposition on Noise Control Engineering
    Number40
    Country/TerritoryJapan
    CityOsaka
    Period04/09/201107/09/2011

    Keywords

    • Aeroelastic design methods
    • Acoustic variables control
    • Boundary layer flow
    • Exhibitions
    • Pressure gradient
    • Anisotropy
    • Airfoil noise
    • Surface pressure
    • Trailing-edge noise modeling
    • Adverse pressure gradient
    • Anisotropy factor
    • Degree of anisotropy
    • Experimental investigations
    • Flow direction
    • Modified model
    • Surface pressures
    • Trailing edge noise
    • Turbulent boundary layers
    • Vertical velocity components

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