2008
DOI: 10.1061/(asce)0733-9429(2008)134:2(196)
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2D Modeling of Heterogeneous Dispersion in Meandering Channels

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Cited by 35 publications
(33 citation statements)
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“…5 shows the variation of Φ/Φ max , where Φ max is the maximum crosssectional mean shear factor, along the dimensionless longitudinal distance, x/L C , where L C is the arc length of one period of the Scurved channel. This figure reveals that Φ/Φ max varies periodically and is the highest near the apex of the bends (Seo et al, 2008). Furthermore, values of Φ/Φ max in the second bend are larger than those in the first bend.…”
Section: Application Of Transverse Velocity Equationmentioning
confidence: 85%
“…5 shows the variation of Φ/Φ max , where Φ max is the maximum crosssectional mean shear factor, along the dimensionless longitudinal distance, x/L C , where L C is the arc length of one period of the Scurved channel. This figure reveals that Φ/Φ max varies periodically and is the highest near the apex of the bends (Seo et al, 2008). Furthermore, values of Φ/Φ max in the second bend are larger than those in the first bend.…”
Section: Application Of Transverse Velocity Equationmentioning
confidence: 85%
“…We can calculate the transverse dispersion coefficient using the slope of the straight line which is fitted to the plot of variance (σ 2 y ) against longitudinal distance (x). The simple moment method (simple MM) by Sayre and Chang [4] can be derived from the generalized MM, Equation (2). Neglecting the transverse velocity and the tracer impinging on banks, and assuming a constant longitudinal velocity, Equation (2) becomes:…”
Section: Methodsmentioning
confidence: 99%
“…Estimated dispersion coefficients based on numerical models are sometimes unrealistic, and may not be transferable to other sites or problems [1]. Thus, reliable methods have been proposed that avoid the uncertainties associated with simulations and reduce the computational burden associated with numerical models, while facilitating the direct determination of dispersion coefficients [2].…”
Section: Introductionmentioning
confidence: 99%
“…This expression results from the transformation of the dispersion process in the Lagrangian frame into that in the fixed Eulerian frame, using the 2D depth-averaged velocity field. Therefore, using this expression, the Lagrangian motion of tracer clouds can be considered in the fixed Cartesian coordinate (Lee and Seo, 2007;Seo et al, 2008).…”
Section: Governing Equationmentioning
confidence: 99%