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- W2317864947 abstract "In many natural rivers, aquatic vegetation occurs in patches of finite length. In such vegetated flows, the shear layer has not formed at the upstream edge of the vegetation patch and coherent motions develop downstream. The longitudinal advection of these coherent vortices contributes significantly to mass and momentum transport. However, there is almost no detailed information about the developing process of large-scale coherent structure within the vegetation patch. So, in this study, we consider the effect of the limited length vegetation patch. Flow images were taken by CCD and the instantaneous velocity vectors are analyzed by PIV techniques. The results showed that (i) the 3-D diverging flow occurs at the vegetation patch edge and (ii) as the coherent structures develop downstream in nonwake zone, the rate of the vertical momentum transport by Sweep motions becomes larger." @default.
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- W2317864947 date "2013-01-01" @default.
- W2317864947 modified "2023-10-16" @default.
- W2317864947 title "EXPERIMENTAL STUDY ON DIVERGING FLOW AT THE BOUNDARY BETWEEN FLAT BED ZONE AND VEGETATION PATCH ZONE" @default.
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- W2317864947 doi "https://doi.org/10.2208/jscejhe.69.i_871" @default.
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