Estuarine morphodynamics and development modified by floodplain formation

Maarten Kleinhans, Lonneke Roelofs, Steven Weisscher, Ivar Lokhorst, Lisanne Braat

Research output: Contribution to journalArticleAcademicpeer-review

Abstract

Rivers and estuaries are flanked by floodplains built by mud and vegetation. Floodplains affect channel dynamics and the overall system's pattern through apparent cohesion in the channel banks and through filling of accommodation space and hydraulic resistance. For rivers, effects of mud, vegetation and the combination are thought to stabilise the banks and narrow the channel. However, the thinness of estuarine floodplain, comprised of salt marsh and mudflats, compared to channel depth raises questions about the possible effects of floodplain as constraints on estuary dimensions. To test these effects, we created three estuaries in a tidal flume: one with recruitment events of two live vegetation species, one with mud and a control with neither. Both vegetation and mud reduced channel migration and bank erosion and stabilised channels and bars. Effects of vegetation include local flow velocity reduction and concentration of flow into the channels, while flow velocities remained higher over mudflats. On the other hand, the lower reach of the muddy estuary showed more reduced channel migration than the vegetated estuary. The main system-wide effect of mudflats and salt marsh is to reduce the tidal prism over time from upstream to downstream. The landward reach of the estuary narrows and fills progressively, particularly for the muddy estuary, which effectively shortens the tidally influenced reach and also reduces the tidal energy in the seaward reach and mouth area. As such, estuaries with sufficient sediment supply are limited in size by tidal prism reduction through floodplain formation.

Original languageEnglish
Pages (from-to)367-381
JournalEarth Surface Dynamics
Volume10
Issue number2
DOIs
Publication statusPublished - 29 Apr 2022

Bibliographical note

Funding Information:
Financial support. This research has been supported by the Nederlandse Organisatie voor Wetenschappelijk Onderzoek (grant no. Vici 016.140.316/13710) and the European Research Council, H2020 European Research Council (ESTUARIES (grant no. 647570)).

Publisher Copyright:
© 2022 Maarten G. Kleinhans et al.

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