Preprints
https://doi.org/10.5194/egusphere-2025-103
https://doi.org/10.5194/egusphere-2025-103
18 Feb 2025
 | 18 Feb 2025
Status: this preprint is open for discussion and under review for Earth Surface Dynamics (ESurf).

Effect of grain-sorting waves on alternate bar dynamics: Implications of the breakdown of the hydrograph boundary layer

Soichi Tanabe and Toshiki Iwasaki

Abstract. Understanding the morphological responses of gravel-bed rivers to changes in external forces (e.g. water and sediment supply conditions) is a critical concern in river science and engineering. However, this remains a challenging issue because river responses are highly dependent on the distance from the source point where such environmental changes occur. Here, we focus on the short-term effects of flood-scale non-equilibrium sediment supply on the downstream alternate bar dynamics in poorly sorted gravel-bed rivers using a numerical morphodynamic model. Specifically, we perform a two-dimensional morphodynamic calculation using iRIC-Nays2DH in a straight channel under repeated cycles of an unsteady water hydrograph and a constant supply of poorly sorted sediment. Under the well-sorted sediment cases, the upstream non-equilibrium sediment supply can affect only a limited distance from the upstream end (i.e. the hydrograph boundary layer). However, the inclusion of a poorly sorted sediment disrupts this concept, leading to the migration of low-amplitude bedload sheets far downstream. In this context, the upstream water and sediment boundary conditions may affect the far-downstream river dynamics through the migration of bedload sheets. The numerical results show that the migration of bedload sheets and the associated fine sediment transport greatly affect the alternate bar dynamics and change their texture. However, this effect of bedload sheets on bars cannot propagate across the entire channel and disappears completely in the alternate bars located further downstream. These results suggest that the upstream non-equilibrium sediment supply condition in poorly sorted sediment has a non-negligible role in downstream alternate bar dynamics even far from the sediment feed point. However, this effect becomes negligible in the further downstream reaches as long as active and larger morphological changes, such as alternate bars, greatly disperse the bedload sheets.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
Share
Soichi Tanabe and Toshiki Iwasaki

Status: open (until 01 Apr 2025)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
Soichi Tanabe and Toshiki Iwasaki
Soichi Tanabe and Toshiki Iwasaki

Viewed

Total article views: 111 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
92 16 3 111 4 3
  • HTML: 92
  • PDF: 16
  • XML: 3
  • Total: 111
  • BibTeX: 4
  • EndNote: 3
Views and downloads (calculated since 18 Feb 2025)
Cumulative views and downloads (calculated since 18 Feb 2025)

Viewed (geographical distribution)

Total article views: 119 (including HTML, PDF, and XML) Thereof 119 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 18 Mar 2025
Download
Short summary
We try to understand how the sediment supply from the upstream river reach affect the downstream river morphology using a numerical model. If the supplied sediment is composed of variety of size class of particles, a small size bed wave that is composed of mainly fine particles (sorting wave) can propagate to downstream very long distance. However, presence of bars suppresses the effect of sorting wave greatly, and thus the sediment supply has limited role in the downstream river morphology.
Share