Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8908184 | Geomorphology | 2018 | 49 Pages |
Abstract
The results illustrate the differences in hydrodynamics and mixing length in relation to confluences with equal density tributaries. At low-density differences, and higher discharge ratio (Qr) between the two rivers, the flow is similar to equi-density confluent meander bends. In contrast, at high-density differences (low Qr), the tributary flow is confined to near the confluence but the density difference causes the flow to move across channel. In this case, the density difference causes the lateral spread of the tributary flow to be greater than at a greater Qr when the density difference is less. These results illustrate the potential importance of density differences between tributaries in determining the rate and spatial extent of mixing and sediment dispersal at confluent meander bends.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Herrero Horacio S., DÃaz Lozada José M., GarcÃa Carlos M., Szupiany Ricardo N., Best Jim, Pagot Mariana,