1 / 33

Eric Struyf Kris Bal Sofie Van Belleghem Patrick Meire

Eric Struyf Kris Bal Sofie Van Belleghem Patrick Meire. Top-bottom investigation of water and nutrient fluxes to the coastal zone through a lowland river basin. Introduction.

lilli
Download Presentation

Eric Struyf Kris Bal Sofie Van Belleghem Patrick Meire

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Eric Struyf Kris Bal Sofie Van Belleghem Patrick Meire Top-bottom investigation of water and nutrient fluxes to the coastal zone through a lowland river basin

  2. Introduction The accurate quantification of fluxes of water and fluxes of dissolved constituents throughout whole river basins is of major importance. This study can act as the working tool for river managers and modellers to anticipate future changes in hydrology due to climate change and development of vegetation throughout the Schelde basin (France, Belgium, The Netherlands)

  3. Overview • Focus on two research projects within the total framework of integrated river basin management • The effect of vegetation on drainage in upper river basin sub catchments • The possible effect of changing external forcing conditions (increasing discharge) on the eventual transport of water and nutrients towards the coastal area through estuarine ecosystems

  4. Vlissingen North Sea Belgian-Dutch border Schelde North sea Channel Gent-Terneuzen Antwerp Temse Durme Dendermonde Rupel Schelde Schelde Dender Gent The Schelde estuary Nete sub-catchment • Entire salt gradient • Highly eutrofied • Highly industrialized Struyf E., S. Van Damme, P. Meire 2004: Estuarine, Coastal and Shelf Science: in press

  5. Part 1 : The effects of mowing on the discharge capacity of lowland rivers

  6. Increased nutrient fluxes towards the river stimulate plant growth : - discharge capacity will decrease - possibility that adjacent valuable land will flood

  7. Pro’s and cons of watervegetation Pro : - Vegetation acts as a sieve for suspended solids and nutriënts - Vegetation acts as refugia areas for organisms during extreme discharge conditions. • Vegetation has a positive effect on the diversity of organisms within and outside a river Contra : - increases the resistance - often seen as a nuisance in waterways (perception)

  8. This study • Partial removement of macrophytes in three different mowing patterns for three different macrophytes • Patterns with the most ecological potential This as a compromise between the drainage and life support function of waterways

  9. Pattern 1 Pattern 3 Pattern 2 : two sides of macrophytes

  10. In-situ determination of biomass

  11. In-situ determination of biomass

  12. Streamvelocity within the patterns (ex-situ) vegetation Velocity is higher for pattern 2 (all species)

  13. Open water Velocity in pattern 2 is slightly higher then in the other patterns

  14. Determination of the resistance ex-situ Pattern influence Pattern 2 had the highest Km values especially in the higher discharge range Km = V*(R2/3*S1/2)-1

  15. - species with their biomass at the watersurface have higher Km values Species influence

  16. Conclusion • Pattern two has the lowest resistance despite of higher biomasses • Plant architecture influences the resistance : * species with high leaf areas (Callitriche sp.) and branched leaves (Ranunculus aquatilis) have high resistances * concentration of biomass at the surface will impede the water flow less - The patterns have a better relative drainage at higher discharges

  17. Part 2: the effects of hydrological changes on nutrient fluxes throughout estuarine waters to the coastal zone Struyf E., S. Van Damme, P. Meire 2004: Estuarine, Coastal and Shelf Science: in press

  18. Changes in hydrological conditions throughout the river shed eventually influence discharge conditions in estuarine waters and can result in: • - major changes in nutrient fluxes towards brackish and salt estuarine and coastal waters • major changes in nutrient concentrations in the freshwater part of estuarine waters Struyf E., S. Van Damme, P. Meire 2004: Estuarine, Coastal and Shelf Science: in press

  19. Why is nutrient flux towards and through estuarine waters so important? • Estuarine and coastal waters are the main fishery grounds on Earth • Diatom communities are fundamental in estuarine food webs and play an essential role in productivity • The optimal balance between diatom communities and less preferred fytoplankton communities (e.g green algae) is dependent on nutrient ratios within coastal waters • Increase in N and P fluxes to coastal waters can induce eutrophication (explosive growth of algae e.g. Phaeocystis) and subsequent negative effects as oxygen depletion, fish kills, foam production... Struyf E., S. Van Damme, P. Meire 2004: Estuarine, Coastal and Shelf Science: in press

  20. Eutrophication Picture taken from: http://staff.science.uva.nl/~dcslob/lesbrieven/TomTahey/bovenbouwtekst3.htm Struyf E., S. Van Damme, P. Meire 2004: Estuarine, Coastal and Shelf Science: in press

  21. This case study • 1996-2000: a period characterised by steadily increasing discharges in the Schelde estuary • The period 1996-2000 was taken as a reference period for possible major future changes in hydrological conditions • - Vegetation in upper catchments • - Global change • - Urbanisation Struyf E., S. Van Damme, P. Meire 2004: Estuarine, Coastal and Shelf Science: in press

  22. Yearly average discharge in the freshwater zone of the estuary 73 m3.s-1 28 m3.s-1 Discharge from freshwater part towards brackish and coastal waters increased 2 to 3 fold in between 1996-2000. Struyf E., S. Van Damme, P. Meire 2004: Estuarine, Coastal and Shelf Science: in press

  23. Increasing discharge apparent in both winter and summer: absolute discharge increase was higher in winter Struyf E., S. Van Damme, P. Meire 2004: Estuarine, Coastal and Shelf Science: in press

  24. Increase in nitrate loadings Nitrate input from the freshwater to the brackish increased concurrently with discharge, ammonia loadings were stable Dissolved nitrogen output doubled between 1996-2000 16500 tons Discharges in the freshwater estuary 8000 tons Struyf E., S. Van Damme, P. Meire 2004: Estuarine, Coastal and Shelf Science: in press

  25. Higher run-off Non-point pollution (mainly agriculture) towards the estuary increased Discharged suspended solids towards the estuary: indicator for surface run-off Similar patterns in nitrate discharge and loss from agricultural soil, nitrate mainly originates from agriculture, ammonia relates to point-pollution. 340000 tons Estimates show a big increase 90000 tons Source: AWZ Source: VMM Struyf E., S. Van Damme, P. Meire 2004: Estuarine, Coastal and Shelf Science: in press

  26. P and Si discharge Dissolved silica export tripled Phosphorus export was less influenced Hydrology changes can have major impact on nutrient ratios Struyf E., S. Van Damme, P. Meire 2004: Estuarine, Coastal and Shelf Science: in press

  27. Nitrogen in the freshwater zone summer In winter, nitrate concentrations increase with discharge, in summer they decrease. Relations were opposite for ammonia. winter winter The natural, seasonal cycle appears to be flattened out by increasing discharge summer Struyf E., S. Van Damme, P. Meire 2004: Estuarine, Coastal and Shelf Science: in press

  28. The amount of nitrate in the Schelde however is also influenced by the presence or absence of macrophytes in the upper sub- catchments (Nete) Data S. Van Belleghem When macrophytes are present (Summer) total N concentrations are lowered. When the plants decay (Winter) N is released which causes an increased N flux towards the upper sub-catchment and eventually the schelde

  29. Silica in the freshwater zone Diatoms: summer - spring: uptake of DSi winter - autumn: no uptake winter Diatom communities appear not adapted to high discharges With increasing discharge, summer concentrations approach winter concentrations summer Struyf E., S. Van Damme, P. Meire 2004: Estuarine, Coastal and Shelf Science: in press

  30. Impact on management • Higher discharges appear to: • dilute pollutants and nutrients • increase nutrient loadings towards coastal zone Dilution effect masks the problem of increasing loadings from non-point pollution. Dilution could affect political and public perception about the effectivity of pollution reducing measures Struyf E., S. Van Damme, P. Meire 2004: Estuarine, Coastal and Shelf Science: in press

  31. Flemish government has drastically increased investments in point-pollution reduction in the last decade to REDUCE nutrient loadings. Source: VMM Due to hydrological changes, the nutrient loadings have increased over the same period. Struyf E., S. Van Damme, P. Meire 2004: Estuarine, Coastal and Shelf Science: in press

  32. General conclusion * Global change will increase discharge. Consequently nutrient run-off towards coastal zones will increase. * Vegetation however increases the residence time of water due to higher resistances. Self purifying capacity of the river is restored through the stimulation of ecosystem processes. * Vegetation management is a tool which can buffer the fluctuations in discharge in the river basin.

  33. Acknowledgements We like to thank L. Clement for analyzing our water samples. We especially like to thank Flanders Hydraulics and AWZ for their cooperation

More Related