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    Linear Instability Theory for Frequency Assessment of Coherent Vortices in Submerged and Aside Rigid Canopies

    Source: Journal of Hydrologic Engineering:;2010:;Volume ( 015 ):;issue: 012
    Author:
    S. Patil
    ,
    V. P. Singh
    ,
    A. K. Rastogi
    DOI: 10.1061/(ASCE)HE.1943-5584.0000277
    Publisher: American Society of Civil Engineers
    Abstract: Two-layer system of flow through and above vegetation linked by shear flow exhibits periodic oscillations at the interface called the Kelvin-Helmholtz vortices. A dispersion relation for the vortices is derived as a function of flow and vegetation parameters and extended to aside vortices that exist in horizontally stratified flow. Nonlinearity exists in the oscillations in vertically stratified flow however is suppressed in horizontally stratified flow because of the horizontally bounded flow and depth-wise phase difference in the oscillations. The relation for both the vortex types provides a simple way to calculate vortex frequency using measurable flow and vegetation parameters. Results show that the vortex frequency for rigid plants is a function of flow hydraulics and stem density, whereas for flexible plants it is a function of the geometry of bending stems.
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      Linear Instability Theory for Frequency Assessment of Coherent Vortices in Submerged and Aside Rigid Canopies

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    http://yetl.yabesh.ir/yetl1/handle/yetl/63148
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    contributor authorS. Patil
    contributor authorV. P. Singh
    contributor authorA. K. Rastogi
    date accessioned2017-05-08T21:48:49Z
    date available2017-05-08T21:48:49Z
    date copyrightDecember 2010
    date issued2010
    identifier other%28asce%29he%2E1943-5584%2E0000296.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/63148
    description abstractTwo-layer system of flow through and above vegetation linked by shear flow exhibits periodic oscillations at the interface called the Kelvin-Helmholtz vortices. A dispersion relation for the vortices is derived as a function of flow and vegetation parameters and extended to aside vortices that exist in horizontally stratified flow. Nonlinearity exists in the oscillations in vertically stratified flow however is suppressed in horizontally stratified flow because of the horizontally bounded flow and depth-wise phase difference in the oscillations. The relation for both the vortex types provides a simple way to calculate vortex frequency using measurable flow and vegetation parameters. Results show that the vortex frequency for rigid plants is a function of flow hydraulics and stem density, whereas for flexible plants it is a function of the geometry of bending stems.
    publisherAmerican Society of Civil Engineers
    titleLinear Instability Theory for Frequency Assessment of Coherent Vortices in Submerged and Aside Rigid Canopies
    typeJournal Paper
    journal volume15
    journal issue12
    journal titleJournal of Hydrologic Engineering
    identifier doi10.1061/(ASCE)HE.1943-5584.0000277
    treeJournal of Hydrologic Engineering:;2010:;Volume ( 015 ):;issue: 012
    contenttypeFulltext
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