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    Flow in a Channel With a Time-Dependent Indentation in One Wall

    Source: Journal of Fluids Engineering:;1990:;volume( 112 ):;issue: 004::page 468
    Author:
    M. E. Ralph
    ,
    T. J. Pedley
    DOI: 10.1115/1.2909429
    Publisher: The American Society of Mechanical Engineers (ASME)
    Abstract: Computations and flow visualization experiments have been carried out on 2-D flow in a channel, with an indentation in one wall that can move in and out. There is plane Poiseuille flow upstream and attention is focussed on the flow downstream of the indentation. Four time-courses of indentation motion are examined: I oscillation between a flush and an indented postion; II advance from flush to indented, after which it remains stationary; III retraction to flush from a steady indentation; IV small amplitude oscillation about a substantially indented position. Various values of Reynolds number, Re, and Strouhal number, St, are employed (250≤Re≤911; 0.01≤St≤0.1). The results show that (a) vorticity waves and eddies are generated in cases I and II (as in reference [11]); (b) in case II at higher experimental Re the flow does not become steady because the steady flow is unstable to a Rayleigh wave, on the shear layer bounding the main separation region, whose wavelength is significantly less than that of the vorticity wave; (c) in case III the waves that are generated at each parameter set seem to be Rayleigh waves not vorticity waves; (d) in case IV short waves give way to longer waves whose amplitude is comparable with the mean indentation height not the oscillation amplitude. Although resembling vorticity waves these do not propagate like the forced waves of case I and presumably represent a nonlinear interaction between Rayleigh waves, vorticity waves, and the very long, weak waves present even in steady flow. Further downstream, in many cases, the 2-D waves break down into turbulence via 3-D disturbances.
    keyword(s): Channels (Hydraulic engineering) , Flow (Dynamics) , Waves , Vorticity , Oscillations , Rayleigh waves , Shear (Mechanics) , Computation , Poiseuille flow , Flow visualization , Wavelength , Separation (Technology) , Motion , Turbulence , Eddies (Fluid dynamics) AND Reynolds number ,
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      Flow in a Channel With a Time-Dependent Indentation in One Wall

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    http://yetl.yabesh.ir/yetl1/handle/yetl/107064
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    contributor authorM. E. Ralph
    contributor authorT. J. Pedley
    date accessioned2017-05-08T23:32:55Z
    date available2017-05-08T23:32:55Z
    date copyrightDecember, 1990
    date issued1990
    identifier issn0098-2202
    identifier otherJFEGA4-27054#468_1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/107064
    description abstractComputations and flow visualization experiments have been carried out on 2-D flow in a channel, with an indentation in one wall that can move in and out. There is plane Poiseuille flow upstream and attention is focussed on the flow downstream of the indentation. Four time-courses of indentation motion are examined: I oscillation between a flush and an indented postion; II advance from flush to indented, after which it remains stationary; III retraction to flush from a steady indentation; IV small amplitude oscillation about a substantially indented position. Various values of Reynolds number, Re, and Strouhal number, St, are employed (250≤Re≤911; 0.01≤St≤0.1). The results show that (a) vorticity waves and eddies are generated in cases I and II (as in reference [11]); (b) in case II at higher experimental Re the flow does not become steady because the steady flow is unstable to a Rayleigh wave, on the shear layer bounding the main separation region, whose wavelength is significantly less than that of the vorticity wave; (c) in case III the waves that are generated at each parameter set seem to be Rayleigh waves not vorticity waves; (d) in case IV short waves give way to longer waves whose amplitude is comparable with the mean indentation height not the oscillation amplitude. Although resembling vorticity waves these do not propagate like the forced waves of case I and presumably represent a nonlinear interaction between Rayleigh waves, vorticity waves, and the very long, weak waves present even in steady flow. Further downstream, in many cases, the 2-D waves break down into turbulence via 3-D disturbances.
    publisherThe American Society of Mechanical Engineers (ASME)
    titleFlow in a Channel With a Time-Dependent Indentation in One Wall
    typeJournal Paper
    journal volume112
    journal issue4
    journal titleJournal of Fluids Engineering
    identifier doi10.1115/1.2909429
    journal fristpage468
    journal lastpage475
    identifier eissn1528-901X
    keywordsChannels (Hydraulic engineering)
    keywordsFlow (Dynamics)
    keywordsWaves
    keywordsVorticity
    keywordsOscillations
    keywordsRayleigh waves
    keywordsShear (Mechanics)
    keywordsComputation
    keywordsPoiseuille flow
    keywordsFlow visualization
    keywordsWavelength
    keywordsSeparation (Technology)
    keywordsMotion
    keywordsTurbulence
    keywordsEddies (Fluid dynamics) AND Reynolds number
    treeJournal of Fluids Engineering:;1990:;volume( 112 ):;issue: 004
    contenttypeFulltext
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