Report on the Eel Stock and Fishery in the Netherlands 2008
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Presentatie Bor Waal Merwede
Bouwsteen Beeld op de Rivieren 24 november 2020 – Bouwdag Rijn 1 Ontwikkelperspectief Waal Merwede 24 november 2020 – Bouwdag Rijn 1 Ontwikkelperspectief Waal Merwede Trajecten Waal Merwede • Midden-Waal (Nijmegen - Tiel) • Beneden-Waal (Tiel - Woudrichem) • Boven-Merwede (Woudrichem – Werkendam) Wat bespreken we? • Oogst gezamenlijke werksessies • Richtinggevend perspectief gebruiksfuncties rivierengebied • Lange termijn (2050 en verder) • Strategische keuzen Hoe lees je de kaart? • Bekijk de kaart via de GIS viewer • Toekomstige gebruiksfuncties zijn met kleur aangegeven • Kansen en opgaven met * aangeduid, verbindingen met een pijl • Keuzes en dilemma’s weergegeven met icoontje Synthese Rijn Waterbeschikbaarheid • Belangrijkste strategische keuze: waterverdeling splitsingspunt. • Meer water via IJssel naar IJsselmeer in tijden van hoogwater (aanvullen buffer IJsselmeer) • Verplaatsen innamepunten Lek voor zoetwater wenselijk i.v.m. verzilting • Afbouwen drainage in buitendijkse gebieden i.v.m. langer vasthouden van water. Creëren van waterbuffers in bovenstroomse deel van het Nederlandse Rijnsysteem. (balans • droge/natte periodes). Natuur • Noodzakelijk om robuuste natuureenheden te realiseren • Splitsingspunt is belangrijke ecologische knooppunt. • Uiterwaarden Waal geschikt voor dynamische grootschalige natuur. Landbouw • Nederrijn + IJssel: mengvorm van landbouw en natuur mogelijk. Waterveiligheid • Tot 2050 zijn dijkversterkingen afdoende -> daarna meer richten op rivierverruiming. Meer water via IJssel betekent vergroten waterveiligheidsopgave -
Kansen Voor Achteroevers Inhoud
Kansen voor Achteroevers Inhoud Een oever achter de dijk om water beter te benuten 3 Wenkend perspectief 4 Achteroever Koopmanspolder – Proefuin voor innovatief waterbeheer en natuurontwikkeling 5 Achteroever Wieringermeer – Combinatie waterbeheer met economische bedrijvigheid 7 Samenwerking 11 “Herstel de natuurlijke dynamiek in het IJsselmeergebied waar het kan” 12 Het achteroeverconcept en de toekomst van het IJsselmeergebied 14 Naar een living lab IJsselmeergebied? 15 Het IJsselmeergebied Achteroever Wieringermeer Achteroever Koopmanspolder Een oever achter de dijk om water beter te benuten Anders omgaan met ons schaarse zoete water Het klimaat verandert en dat heef grote gevolgen voor het waterbeheer in Nederland. We zullen moeten leren omgaan met grotere hoeveelheden water (zeespiegelstijging, grotere rivierafvoeren, extremere hoeveelheden neerslag), maar ook met grotere perioden van droogte. De zomer van 2018 staat wat dat betref nog vers in het geheugen. Beschikbaar zoet water is schaars op wereldschaal. Het meeste water op aarde is zout, en veel van het zoete water zit in gletsjers, of in de ondergrond. Slechts een klein deel is beschikbaar in meren en rivieren. Het IJsselmeer – inclusief Markermeer en Randmeren – is een grote regenton met kost- baar zoet water van prima kwaliteit voor een groot deel van Nederland. Het watersysteem functioneert nog goed, maar loopt wel op tegen de grenzen vanwege klimaatverandering. Door innovatie wegen naar de toekomst verkennen Het is verstandig om ons op die verandering voor te bereiden. Rijkswaterstaat verkent daarom samen met partners nu al mogelijke oplossingsrichtingen die ons in de toekomst kunnen helpen. Dat doen we door te innoveren en te zoeken naar vernieuwende manieren om met het water om te gaan. -
1 the DUTCH DELTA MODEL for POLICY ANALYSIS on FLOOD RISK MANAGEMENT in the NETHERLANDS R.M. Slomp1, J.P. De Waal2, E.F.W. Ruijg
THE DUTCH DELTA MODEL FOR POLICY ANALYSIS ON FLOOD RISK MANAGEMENT IN THE NETHERLANDS R.M. Slomp1, J.P. de Waal2, E.F.W. Ruijgh2, T. Kroon1, E. Snippen2, J.S.L.J. van Alphen3 1. Ministry of Infrastructure and Environment / Rijkswaterstaat 2. Deltares 3. Staff Delta Programme Commissioner ABSTRACT The Netherlands is located in a delta where the rivers Rhine, Meuse, Scheldt and Eems drain into the North Sea. Over the centuries floods have been caused by high river discharges, storms, and ice dams. In view of the changing climate the probability of flooding is expected to increase. Moreover, as the socio- economic developments in the Netherlands lead to further growth of private and public property, the possible damage as a result of flooding is likely to increase even more. The increasing flood risk has led the government to act, even though the Netherlands has not had a major flood since 1953. An integrated policy analysis study has been launched by the government called the Dutch Delta Programme. The Delta model is the integrated and consistent set of models to support long-term analyses of the various decisions in the Delta Programme. The programme covers the Netherlands, and includes flood risk analysis and water supply studies. This means the Delta model includes models for flood risk management as well as fresh water supply. In this paper we will discuss the models for flood risk management. The issues tackled were: consistent climate change scenarios for all water systems, consistent measures over the water systems, choice of the same proxies to evaluate flood probabilities and the reduction of computation and analysis time. -
Ontgonnen Verleden
Ontgonnen Verleden Regiobeschrijvingen provincie Noord-Brabant Adriaan Haartsen Directie Kennis, juni 2009 © 2009 Directie Kennis, Ministerie van Landbouw, Natuur en Voedselkwaliteit Rapport DK nr. 2009/dk116-K Ede, 2009 Teksten mogen alleen worden overgenomen met bronvermelding. Deze uitgave kan schriftelijk of per e-mail worden besteld bij de directie Kennis onder vermelding van code 2009/dk116-K en het aantal exemplaren. Oplage 50 exemplaren Auteur Bureau Lantschap Samenstelling Eduard van Beusekom, Bart Looise, Annette Gravendeel, Janny Beumer Ontwerp omslag Cor Kruft Druk Ministerie van LNV, directie IFZ/Bedrijfsuitgeverij Productie Directie Kennis Bedrijfsvoering/Publicatiezaken Bezoekadres : Horapark, Bennekomseweg 41 Postadres : Postbus 482, 6710 BL Ede Telefoon : 0318 822500 Fax : 0318 822550 E-mail : [email protected] Voorwoord In de deelrapporten van de studie Ontgonnen Verleden dwaalt u door de historisch- geografische catacomben van de twaalf provincies in Nederland. Dat klinkt duister en kil en riekt naar spinnenwebben en vochtig beschimmelde hoekjes. Maar dat pakt anders uit. Deze uitgave, samengesteld uit twaalf delen, biedt de meer dan gemiddeld geïnteresseerde, verhelderende kaartjes, duidelijke teksten en foto’s van de historisch- geografische regio’s van Nederland. Zo geeft het een compleet beeld van Nederland anno toen, nu en de tijd die daar tussen zit. De hoofdstukken over de deelgebieden/regio’s schetsen in het kort een karakteristiek per gebied. De cultuurhistorische blikvangers worden gepresenteerd. Voor de fijnproevers volgt hierna een nadere uiteenzetting. De ontwikkeling van het landschap, de bodem en het reliëf, en de bewoningsgeschiedenis worden in beeld gebracht. Het gaat over de ligging van dorpen en steden, de verkavelingsvormen in het agrarisch land, de loop van wegen, kanalen en spoorlijnen, dijkenpatronen, waterlopen, defensielinies met fortificaties. -
Dredging and Dumping in Laboratory Scale Experiments of Estuaries
Student number: 5821797 Effects of dredging and dumping in laboratory scale experiments of estuaries Cox, J.R. (Jana) Student number: 5821797 Utrecht University, Department of Physical Geography Faculty of Geosciences March 2018 – final version Master: Earth Surface and Water Track: Coastal and fluvial morphodynamics Supervisors: J.R.F.W Leuven & Prof. 0 M.G. Kleinhans Contents Table of figures ............................................................................................................................................. 3 Abstract ........................................................................................................................................................ 8 1. Introduction ......................................................................................................................................... 9 1.1 Review of the effects of dredging and dumping on estuaries & suggested mechanisms ................... 9 1.2 Description of the Western Scheldt estuary ..................................................................................... 11 1.2.1 Geological history of the estuary ............................................................................................... 11 1.2.2 Morphological development of the Western Scheldt estuary ................................................... 12 1.3 Current morphology of the Western Scheldt ................................................................................... 13 1.4 Sediment balance of the Western Scheldt estuary.......................................................................... -
Silt in the Markermeer/Ijmeer
Silt in the Markermeer/IJmeer A study on the effectivity and efficiency of proposed approaches concerning the deterioration of the lake and its surroundings Student: Iris van Gogh (3220052) Environmental biology Ecology and Natural Resources Management Supervisor: Dr. J.N.M. Dekker Energy and Resources Copernicus Institute of Sustainable Development Faculty of Geosciences, Utrecht University December, 2012 Preface Since I was born in Lelystad, the capital of the county Flevoland in the Middle of the Netherlands, I lived near the Markermeer for about 18 years of my life. I still remember the time being on an airplane and my dad showing me the Markermeer and IJsselmeer below us. The difference in color (blue for the IJsselmeer, while green/brown for the Markermeer) was enormous, and I know now, this is mainly caused by the high amount of silt in the Markermeer. A couple of years later I was, again due to my father, at an information day about water, distributing ‘dropjes’, a typical Dutch candy, wearing a suit looking like a water drop, named ‘Droppie Water’. I think it were those two moments that raised my interest for water and even though I was not aware of it at that time, I never got rid of it. Thanks to the Master track ‘Ecology and Natural Resources Management’ which I started in 2011, my interest for water was raised once, or actually thrice, again. After my first internship, which was about seed dispersal via lowland streams and arranging my second internship about heavily modified water bodies in Sweden (which I planned for the period between half of December 2012 and the end of July 2013) I wanted to specialize this master track in the direction of water. -
Physical Scaling of Tocardo's Eastern Scheldt Turbines
Physical Scaling of To- cardo’s Eastern Scheldt Turbines Additional Graduation Work B.J. van de Zande Delft University of Technology Physical Scaling of Tocardo’s Eastern Scheldt Turbines Additional Graduation Work by B.J. van de Zande in partial fulfillment of the requirements for the degree of Master of Science in Hydraulic Engineering at the Delft University of Technology, Faculty of Civil Engineering and Geosciences Student number: 4160207 Project duration: February 20, 2017 – June 1, 2017 Thesis committee: Prof. dr. ir. W.S.J. Uijttewaal, TU Delft Dr. ir. R.J. Labeur, TU Delft MSc. M.C. Verbeek, TU Delft An electronic version of this thesis is available at http://repository.tudelft.nl/. Cover image: Artist impression of tidal energy extraction in the Eastern Scheldt, The Netherlands (source: Jaarbericht Rijkswaterstaat 2015, p. 39) Preface This additional graduation work is submitted as part of the Master’s program Hydraulic Engineering at Delft University of Technology. I am convinced that, if humanity wants to maintain the quality of life that is experienced today, we should invest in more sustainable forms of energy generation. The subject of tidal energy extraction has drawn my attention since the power of water fascinates me. With this additional graduation work I hope to contribute to the knowledge that is being developed in the field of tidal energy. I would like to thank the members of this additional thesis committee prof. dr. ir. W.S.J. Uijttewaal, dr. ir. R.J. Labeur and MSc M.C. Verbeek for the feedback and guidance throughout this research. I owe a special word of thanks to Merel Verbeek, who provided me with this subject and was always open to answer my questions. -
The Ecology O F the Estuaries of Rhine, Meuse and Scheldt in The
TOPICS IN MARINE BIOLOGY. ROS. J. D. (ED.). SCIENT. MAR . 53(2-3): 457-463 1989 The ecology of the estuaries of Rhine, Meuse and Scheldt in the Netherlands* CARLO HEIP Delta Institute for Hydrobiological Research. Yerseke. The Netherlands SUMMARY: Three rivers, the Rhine, the Meuse and the Scheldt enter the North Sea close to each other in the Netherlands, where they form the so-called delta region. This area has been under constant human influence since the Middle Ages, but especially after a catastrophic flood in 1953, when very important coastal engineering projects changed the estuarine character of the area drastically. Freshwater, brackish water and marine lakes were formed and in one of the sea arms, the Eastern Scheldt, a storm surge barrier was constructed. Only the Western Scheldt remained a true estuary. The consecutive changes in this area have been extensively monitored and an important research effort was devoted to evaluate their ecological consequences. A summary and synthesis of some of these results are presented. In particular, the stagnant marine lake Grevelingen and the consequences of the storm surge barrier in the Eastern Scheldt have received much attention. In lake Grevelingen the principal aim of the study was to develop a nitrogen model. After the lake was formed the residence time of the water increased from a few days to several years. Primary production increased and the sediments were redistributed but the primary consumers suchs as the blue mussel and cockles survived. A remarkable increase ofZostera marina beds and the snail Nassarius reticulatus was observed. The storm surge barrier in the Eastern Scheldt was just finished in 1987. -
Half a Century of Morphological Change in the Haringvliet and Grevelingen Ebb-Tidal Deltas (SW Netherlands) - Impacts of Large-Scale Engineering 1964-2015
Half a century of morphological change in the Haringvliet and Grevelingen ebb-tidal deltas (SW Netherlands) - Impacts of large-scale engineering 1964-2015 Ad J.F. van der Spek1,2; Edwin P.L. Elias3 1Deltares, P.O. Box 177, 2600 MH Delft, The Netherlands; [email protected] 2Faculty of Geosciences, Utrecht University, P.O. Box 80115, 3508 TC Utrecht 3Deltares USA, 8070 Georgia Ave, Silver Spring, MD 20910, U.S.A.; [email protected] Abstract The estuaries in the SW Netherlands, a series of distributaries of the rivers Rhine, Meuse and Scheldt known as the Dutch Delta, have been engineered to a large extent. The complete or partial damming of these estuaries in the nineteensixties had an enormous impact on their ebb-tidal deltas. The strong reduction of the cross-shore tidal flow triggered a series of morphological changes that includes erosion of the ebb delta front, the building of a coast-parallel, linear intertidal sand bar at the seaward edge of the delta platform and infilling of the tidal channels. The continuous extension of the port of Rotterdam in the northern part of the Haringvliet ebb-tidal delta increasingly sheltered the latter from the impact of waves from the northwest and north. This led to breaching and erosion of the shore-parallel bar. Moreover, large-scale sedimentation diminished the average depth in this area. The Grevelingen ebb-tidal delta has a more exposed position and has not reached this stage of bar breaching yet. The observed development of the ebb-tidal deltas caused by restriction or even blocking of the tidal flow in the associated estuary or tidal inlet is summarized in a conceptual model. -
Annual Review 2012 Deltares
ANNUAL REVIEW 2012 ANNUAL Deltares P.O. Box 177 2600 MH Delft The Netherlands DELTARES 2012 T +31 (0)88 335 8273 [email protected] Annual Review www.deltares.nl Follow Deltares www.twitter.com/deltares www.linkedin.com/company/217430 Omslag_buiten_en.indd 1 15-04-13 13:57 DELTARES credits DELTARES, APRIL 2013 A great deal of care has gone into the production of this publication. Use of the texts or parts thereof is permitted on condition that the source is quoted. Re-use of the infor- Our mission mation shall be for the responsibility of the user. ADDRESS Developing and applying top-level expertise Deltares P.O. Box 177 in the field of water, subsurface and 2600 MH Delft www.deltares.nl infrastructure for people, environment and society. Deltares is thereby independent, EDITING Deltares communications department sets high demands on the quality of the [email protected] knowledge and advice and works closely IMAGES with governments, businesses and research Deltares, cover, pages 4, 8, 9, 11, 12, 13, 15, 16, 17, 19, 20, institutes at home and abroad. At Deltares, 21, 23, 28, 29, 30, 31, 34, 35, 36, 37, 38, 39, 42, 54, 55, 56 Dirk Hol, pages 3, 6, 10, 11, 14, 18, 20, 22, 26, 30, knowledge is the key. 32/33, 47, 48, 49, 50, 56 Ewout Staartjes, pages 14, 22, 28 Hans Roode, page 25 Mennobart van Eerden, Rijkswaterstaat, page 24 Rijkswaterstaat, page 8 Stichting Noordzee, page 13 The photos on pages 6, 10, 18, 26, 32/33, 47 and 49 were taken in the Deltares Facilities Hall in Delft. -
Summary Report Plastic Litter in Rhine, Meuse and Scheldt, Contribution to Plastic Litter in the North Sea
Summary report Plastic litter in Rhine, Meuse and Scheldt, contribution to plastic litter in the North Sea 1206088-000-ZKS-0004, 27 May 2013, final Contents 1 Introduction 1 1.1 Definitions, sources and pathways 1 1.2 Effects of plastic litter in the aquatic environment 2 2 Transport processes of plastic litter 5 2.1 Processes in rivers 5 2.2 Methodology and data availability 6 3 Quantification of transported plastic litter 9 3.1 Contribution to litter in the North Sea 9 3.2 River Rhine 12 3.3 River Meuse– coarse and fine fraction 13 3.4 River Scheldt – coarse and fine fraction 13 4 Governance 15 5 Monitoring 17 6 General conclusions 19 7 Recommendations 21 Summary report Plastic litter in Rhine, Meuse and Scheldt, contribution to plastic litter in the North i Sea 1206088-000-ZKS-0004, 27 May 2013, final 1 Introduction The Marine Strategy Framework Directive (MSFD) establishes a framework within which Member States shall take the necessary measures to achieve or maintain good environmental status in the marine environment by the year 2020 at the latest. The MSFD.installed to ensure Good Environmental Status (GES) by 2020 includes the qualitative descriptor ‘Marine Litter’ (MSFD, Annex I, descriptor 10). For freshwater, one of the main policy instruments is the Water Framework Directive (WFD), which does not include litter in determining ecological status for freshwater bodies. National authorities in the Netherlands are currently implementing the MSFD and need to provide the European Commission with data on the amounts of litter in the Dutch part of the North Sea. -
Rotterdam University of Applied Sciences Muh Aris Marfai, Gadjah Mada University, Yogyakarta
Connecting Delta Cities COASTAL CITIES, FLOOD RISK MANAGEMENT AND ADAPTATION TO CLIMATE CHANGE Connecting Delta Cities Jeroen Aerts, VU University Amsterdam David C. Major, Columbia University Malcolm J. Bowman, State University of New York, Stony Brook Piet Dircke, Rotterdam University of Applied Sciences Muh Aris Marfai, Gadjah Mada University, Yogyakarta COASTAL CITIES, FLOOD RISK MANAGEMENT AND ADAPTATION TO CLIMATE CHANGE Authors Acknowledgements Jeroen Aerts, David C. Major, Malcolm J. Bowman, We gratefully acknowledge the generous support and Piet Dircke, Muh Aris Marfai participation of Adam Freed (City of New York), Aisa Tobing (Jakarta Governor’s Office), Raymund Kemur Contributing authors (Ministry of Spatial Planning, Indonesia) and Arnoud Abidin, H.Z., Ward, P., Botzen, W., Bannink, B.A., Molenaar (City of Rotterdam). We thank the City of Lon- Nickson, A., Reeder, T. don, Alex Nickson, Tim Reeder of the UK Environment Agency, Robert Muir-Wood and Hans Peter Plag for their Sponsors participation and support. We furthermore thank Florrie This book is sponsored by the City of Rotterdam, de Pater of the Knowledge for Climate program for her and Rotterdam Climate Proof and the Dutch research support on communication aspects, Mr Scott Sullivan program for Climate (KvK). The Connecting Delta Cities and his staff of Stony Brook University for providing faci- network has been addressed as a joint action under lities and assistance at the Manhattan campus, Cynthia the Clinton C40 initiative. For more information on Rosenzweig and colleagues at Columbia and NASA GISS these initiatives and their relation to Connecting for information and participation, Klaus Jacobs of Colum- Delta Cities, please see: bia University, William Solecki of Hunter College and Colophon www.deltacities.com.