Effects of estuarine mudflat formation on tidal prism and large‐scale morphology in experiments

• Published in: Earth surface processes and landforms 2019-02, Vol.44 (2), p.417-432
• Main Authors: Braat, Lisanne, Leuven, Jasper R. F. W., Lokhorst, Ivar R., Kleinhans, Maarten G.
• Format: Article
• Language: English
• Subjects: Bank erosion; Brackishwater environment; Channels; Digital Elevation Models; Digital imaging; Dynamics; Earth; Earth surface; Ecological effects; Elevation; Erosion; Erosion rates; Estuaries; Estuarine dynamics; Estuarine environments; estuary morphodynamics; Evolution; Experiments; Floodplains; flume experiments; Flumes; Harbors; Harbours; Landforms; Marshes; Morphology; Mud; Mud flats; mudflat; Navigation; Planforms; River channels; Rivers; shoal accretion; Shoals; Siltation; Spatial distribution; Stability; Tidal cycles; Tidal prism; Tides; Turbidity; Water levels
• ISSN: 0197-9337; 1096-9837
• DOI: 10.1002/esp.4504

Human 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. Mudflats form on the sides of estuaries and on top shoals. The mud accretion elevates high intertidal areas up to supratidal elevations, which decreases tidal prism. This leads to a decrease in channel migration and to a near‐equilibrium planform that is smaller in volume and especially narrower upstream with increased bar heights and no channel deepening.