Abstract

An optimized parameterization of the non-dimensional longitudinal dispersion coefficients in Greek rivers, $$K_{x_a } $$ , is described in terms of parameters derived from cross-section river geometry and longitudinal velocity data. Optimization is accomplished, using various combinations of the selected parameters, either for subsets of $$K_{x_a } $$ values, according to the cross-section aspect ratio range, or for the entire $$K_{x_a } $$ population. The use of shape factors associated with the river cross-section transverse profiles of depth-mean longitudinal velocities and the normalized intensities of longitudinal velocity variations from the overall mean cross-sectional velocity improves the parameterization. The statistical behavior of $$K_{x_a } $$ in terms of skewness, flatness and other shape coefficients is also examined. $$K_{x_a } $$ histograms show that these coefficients have a log-normal distribution. An empirical expression for $$K_{x_a } $$ is also proposed that takes into account both contributions from the transverse velocity profile and from the vertical profile of longitudinal velocities, at each cross-section, in shaping the value of dispersion coefficients when the aspect ratio of the cross-section is of O(1) and/or when $$K_{x_a } $$ is of O(1).

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