Model results suggest that 1) varying lateral bed-slope factor has strong impacts; larger value leads to gentler channel-shoal interface or smaller lateral channel bedslope. 2) Different sediment transport formulas lead to considerable differences in morphodynamic patterns. 3) Sediment transport formulas considering both suspension and bed load transport tolerate a smaller morphological acceleration factor and requires a larger bed-slope factor.
|Publication status||Published - 2017|
|Event||10th Symposium on River coastal and estuarine morphodynamics: Back to Italy - Trento - Padova, Italy|
Duration: 15 Sep 2017 → 22 Sep 2017
Conference number: 10
|Conference||10th Symposium on River coastal and estuarine morphodynamics|
|City||Trento - Padova|
|Period||15/09/17 → 22/09/17|