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Distribution of turbulent velocity fluctuations in a natural river

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Turbulent characteristics of flow velocity in a natural river were systematically analyzed in this study. Flow velocities were measured with time at six different lateral locations and at three different vertical elevations on a major navigable waterway in the United States. Analyses of the velocity data include the cross-sectional and vertical distributions of longitudinal and transverse velocity components (u, v), the fluctuating velocity components (u1, v1) and their frequency-distribution curves, turbulent intensities (�x'�y), and turbulent shear stress (scientific formula not reproduced). These analyses have shown that the strongest velocity fluctuation occurs near the main channel area above the river bed.

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  • Upper Midwest Environmental Sciences Center (UMESC)

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Journal of Hydraulic Research 33(5):649-661. Reprinted by U.S. Geological Survey, Environmental Management Technical Center, Onalaska, Wisconsin

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