Document of bibliographic reference 307840

BibliographicReference record

Type
Bibliographic resource
Type of document
Journal article
BibLvlCode
AS
Title
Modeling the transition to high sediment concentrations as a response to channel deepening in the Ems river estuary
Abstract
Many estuaries are strongly modified by human interventions, including substantive channel deepening. In the Ems River Estuary (Germany and Netherlands), channel deepening between the 1960s and early 2000s coincided with an increase in the maximum near‐bed suspended sediment concentration from moderate (∼1 kg/m3) to high (>10 kg/m3). In this study the observed transition in the suspended sediment concentration in the Ems is qualitatively reproduced by using an idealized width‐averaged iFlow model. The model is used to reproduce observations from 1965 and 2005 by only changing the channel depth between the years. Model results show an increase in sediment concentrations from approximately 1–2 kg/m3 to 20–30 kg/m3 near the bed between 1965 and 2005 if the river discharge is below 70 m3/s, which holds approximately 60% of the time. Thereby, this study for the first time provides strong evidence for earlier published hypotheses that channel deepening was the main driver of the increased sediment concentrations in the Ems. The results are explained using two aspects: sediment transport (longitudinal processes) and local resuspension (vertical processes). The magnitude of the sediment import increased, because a combination of channel deepening and sediment‐induced damping of turbulence increased the M2–M4 tidal asymmetry. This effect is particularly strong, because the M4 tide evolved to a state close to resonance. All imported sediment is kept in suspension when it is assumed that resuspension is sufficiently efficient, which depends on the value of the erosion parameter used and inclusion of hindered settling in the model.
WebOfScience code
https://www.webofscience.com/wos/woscc/full-record/WOS:000464656900013
Bibliographic citation
Dijkstra, Y.M.; Schuttelaars, H.M.; Schramkowski, G.; Brouwer, R.L. (2019). Modeling the transition to high sediment concentrations as a response to channel deepening in the Ems river estuary. JGR: Oceans 124(3): 1578-1594. https://dx.doi.org/10.1029/2018jc014367
Topic
Marine
Fresh water
Brakish water
Is peer reviewed
true
Access rights
open access
Is accessible for free
true

Authors

author
Name
Yoeri Dijkstra
author
Name
Henk Schuttelaars
author
Name
George Schramkowski
Identifier
https://orcid.org/0000-0002-2120-1085
author
Name
Ronald Brouwer
Identifier
https://orcid.org/0000-0001-6154-3410
Affiliation
Vlaamse overheid; Beleidsdomein Mobiliteit en Openbare Werken; Vlaams Ministerie Mobiliteit en Openbare Werken; Departement Mobiliteit en Openbare Werken; Waterbouwkundig Laboratorium

Links

referenced creativework
type
DOI
accessURL
https://dx.doi.org/10.1029/2018jc014367

thesaurus terms

term
ANE, Ems Estuary (term code: 181970 - defined in term set: ASFA Geoterms)
Sediment transport (term code: 7391 - defined in term set: ASFA Thesaurus List)

geographic terms

geographic terms associated with this publication
Ems Estuary

Document metadata

date created
2019-03-12
date modified
2025-05-16