{"refrec":{"BRefID":391594,"RR":"<b>Meire, D.; Nguyen, D.; Stark, J.; Vanlede, J.</b> (2024). Een geïntegreerde aanpak voor de Durme: sub report 6. Scenarios intertidal areas. Version 4.0. <i>FH reports</i>, 19_016_6. Flanders Hydraulics: Antwerp. VI, 49 + 6 p. app. pp. <a href=\"https://dx.doi.org/10.48607/237\" target=\"_blank\">https://dx.doi.org/10.48607/237</a>","BEntID":389341,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". Version 4.0. <i>FH reports</i>, 19_016_6. Flanders Hydraulics: Antwerp.  VI, 49 + 6 p. app. pp. <a href=\"https://dx.doi.org/10.48607/237\" target=\"_blank\">https://dx.doi.org/10.48607/237</a>","DocTypID":13,"DocType":"Reports","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Meire, D.; Nguyen, D.; Stark, J.; Vanlede, J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Meire, D. <i>et al.</i>","Englishabstract":"<span lang=\"EN-US\" dir=\"ltr\">Within the framework of the Sigma plan, several areas will be attached to the Durme river in the near future. &nbsp;In this report, the influence of these additional intertidal areas, both in the form of depoldered areas &nbsp;(Klein Broek, Groot Broek) as well as a flood control area with controlled reduced tide FCA-CRT (De Bunt) &nbsp;on the tidal characteristics and velocity patterns along the Durme is examined.</span><br><span lang=\"EN-US\" dir=\"ltr\">All Sigma areas lead to an increase in the tidal prism in the Durme. Among the three areas, the polder Groot &nbsp;Broek has the largest influence on the hydrodynamics of the Durme river and De Bunt shows the least effect. &nbsp;The implementation of Groot Broek alone or together with the other two Sigma areas results in lower high &nbsp;waters in the Durme river. The largest reduction was calculated for the middle river section where the water &nbsp;levels are highest along the Durme river. A strong effect of the three Sigma areas on the current velocity was &nbsp;calculated downstream of the areas with higher peak velocities.</span><br><span lang=\"EN-US\" dir=\"ltr\">The peak velocity asymmetry isflood dominated in most of the river section. Activating the polder Klein Broek &nbsp;and/or Groot Broek weakens the flood dominant tidal asymmetry. The polder Groot Broek shows stronger &nbsp;effect and even alters the velocity asymmetry to ebb dominance at the river section near the mouth. In terms &nbsp;of sediment transport, the polder Klein Broek and Groot Broek could slow down the sedimentation process &nbsp;in the downstream part of the Durme river.</span>","AbstractOtherLang":null,"BibLvlCode":"MS","StandardTitle":"Een geïntegreerde aanpak voor de Durme: sub report 6. 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