Abstract

AbstractHuman interference in estuaries has led to increasing problems of mud, such as hyper‐turbidity with adverse ecological effects and siltation of navigation channels and harbours. To deal with this mud sustainably, it is important to understand its long‐term effects on the morphology and dynamics of estuaries. The aim of this study is to understand how mud affects the morphological evolution of estuaries. We focus on the effects of fluvial mud supply on the spatial distribution of mudflats and on how this influences estuary width, depth, surface area and dynamics over time. Three physical experiments with self‐forming channels and shoals were conducted in a new flume type suitable for tidal experiments: the Metronome. In two of the experiments, we added nutshell grains as mud simulant, which is transported in suspension. Time‐lapse images of every tidal cycle and digital elevation models for every 500 cycles were analysed for the three experiments. Mud settles in distinct locations, forming mudflats on bars and sides of the estuary, where the bed elevation is higher. Two important effects of mud were observed: the first is the slight cohesiveness of mud that causes stability on bars limiting vertical erosion, although the bank erosion rate by migrating channels is unaffected. Secondly, mud fills inactive areas and deposits at higher elevations up to the high‐water level and therefore decreases the tidal prism. These combined effects cause a decrease in dynamics in the estuary and lead to near‐equilibrium planforms that are smaller in volume and especially narrower upstream, with increased bar heights and no channel deepening. This trend is in contrast to channel deepening in rivers by muddier floodplain formation. These results imply large consequences for long‐term morphodynamics in estuaries that become muddier due to management practices, which deteriorate ecological quality of intertidal habitats but may create potential area for marshes. © 2018 The Authors. Earth Surface Processes and Landforms Published by John Wiley & Sons Ltd.

Highlights

  • Estuaries are tidally influenced coastal bodies of water that are connected to a river system supplying fresh water and sediments

  • We focus on the effect on large-scale parameters that determine landward tidal penetration, bar pattern and large-scale dynamics, such as width, depth and depth distribution, surface area, volume and cumulative erosion and deposition over time

  • Besides the increase in bar height, the results showed that mud supply influences the width, size and dynamics of the estuary morphology

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Summary

Introduction

Estuaries are tidally influenced coastal bodies of water that are connected to a river system supplying fresh water and sediments. Estuaries occur in a wide variety of planform shapes and shoal patterns, which are caused by inherited initial conditions and changing boundary conditions It is still unclear how these conditions contribute to the evolution of estuaries and a full understanding of their behaviour is still lacking. Very few studies consider the decadal to centennial effects of mud on the morphology of the estuary Studying these long-term trends might give better insights into more sustainable or more efficient management strategies, and prediction of long-term morphological behaviour may improve by accounting for mud. If we can determine how tidal channels migrate over time in relation to the amount of cohesive mud in the system, we can perhaps better manage causes of hyper-turbidity and dredge more sustainably by migrating the shipping route in accordance with the natural trend of the estuary

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