Abstract

This paper investigates the interplay between the flow, suspended sediment concentration (SSC), and net deposition at the lateral interface between a main channel and riverbank/floodplain vegetation consisting of emergent flexible woody plants with understory grasses. In a new set of flume experiments, data were collected concurrently on the flow field, SSC, and net deposition using acoustic Doppler velocimeters, optical turbidity sensors, and weight-based sampling. Vegetation largely affected the vertical SSC distributions, both within and near the vegetated areas. The seasonal variation of vegetation properties was important, as the foliage strongly increased lateral mixing of suspended sediments between the unvegetated and vegetated parts of the channel. Foliage increased the reach-scale net deposition and enhanced deposition in the understory grasses at the main channel–vegetation interface. To estimate the seasonal differences caused by foliation, we introduced a new drag ratio approach for describing the SSC difference between the vegetated and unvegetated channel parts. Findings in this study suggest that future research and engineering applications will benefit from a more realistic description of natural plant features, including the reconfiguration of plants and drag by the foliage, to complement and replace existing rigid cylinder approaches.

Highlights

  • In rivers and streams, vegetated riparian zones in the streamwise direction are common

  • The interface region is of major importance, as it controls the lateral transport of suspended sediment (SS) and net deposition in the vegetated areas

  • We aimed to provide insights on sediment transport and mixing efficiencies by linking the velocity differences with the drag induced by the vegetation

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Summary

Introduction

In rivers and streams, vegetated riparian zones in the streamwise direction are common. The vegetated areas induce flow resistance and influence the mean and turbulent properties of the flow, resulting in a velocity difference between the main channel and adjacent vegetation, which can result in a strong mixing layer [1,2]. The mixing efficiency is expected to be affected by mean flow velocities and foliage, which regulates the suspended sediment load between the main channel and vegetated floodplain [3]. The interface region is of major importance, as it controls the lateral transport of suspended sediment (SS) and net deposition in the vegetated areas. Maintenance of the floodplain/riverbank vegetation provides means to enhance flow conveyance and prevent excessive flooding, e.g., [6] and to control SS transport and net deposition [4,7].

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