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    Mean Flow and Turbulence in Open-Channel Bend

    Source: Journal of Hydraulic Engineering:;2001:;Volume ( 127 ):;issue: 010
    Author:
    Koen Blanckaert
    ,
    Walter H. Graf
    DOI: 10.1061/(ASCE)0733-9429(2001)127:10(835)
    Publisher: American Society of Civil Engineers
    Abstract: Flow over a developed bottom topography in a bend has been investigated experimentally. The measuring section is in the outer-bank half of the cross section at 60° into the bend. Spatial distributions of the mean velocities, turbulent stresses, and mean-flow and turbulent kinetic energy are presented. The cross-sectional motion contains two cells of circulation: besides the classical helical motion (center-region cell), a weaker counterrotating cell (outer-bank cell) is observed in the corner formed by the outer bank and the water surface. The downstream velocity in the outer half-section is higher than the one in straight uniform flow; the core of maximum velocities is found close to the separation between both circulation cells, well below the water surface. The turbulence structure in a bend is different from that in a straight flow, most notably in a reduction of the turbulent activity toward the outer bank. Both the outer-bank cell and reduced turbulent activity have a protective effect on the outer bank and the adjacent bottom and thus influence the stability of the flow perimeter and the bend morphology.
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      Mean Flow and Turbulence in Open-Channel Bend

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    contributor authorKoen Blanckaert
    contributor authorWalter H. Graf
    date accessioned2017-05-08T20:43:56Z
    date available2017-05-08T20:43:56Z
    date copyrightOctober 2001
    date issued2001
    identifier other%28asce%290733-9429%282001%29127%3A10%28835%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/25111
    description abstractFlow over a developed bottom topography in a bend has been investigated experimentally. The measuring section is in the outer-bank half of the cross section at 60° into the bend. Spatial distributions of the mean velocities, turbulent stresses, and mean-flow and turbulent kinetic energy are presented. The cross-sectional motion contains two cells of circulation: besides the classical helical motion (center-region cell), a weaker counterrotating cell (outer-bank cell) is observed in the corner formed by the outer bank and the water surface. The downstream velocity in the outer half-section is higher than the one in straight uniform flow; the core of maximum velocities is found close to the separation between both circulation cells, well below the water surface. The turbulence structure in a bend is different from that in a straight flow, most notably in a reduction of the turbulent activity toward the outer bank. Both the outer-bank cell and reduced turbulent activity have a protective effect on the outer bank and the adjacent bottom and thus influence the stability of the flow perimeter and the bend morphology.
    publisherAmerican Society of Civil Engineers
    titleMean Flow and Turbulence in Open-Channel Bend
    typeJournal Paper
    journal volume127
    journal issue10
    journal titleJournal of Hydraulic Engineering
    identifier doi10.1061/(ASCE)0733-9429(2001)127:10(835)
    treeJournal of Hydraulic Engineering:;2001:;Volume ( 127 ):;issue: 010
    contenttypeFulltext
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