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Patrick Meire - Academia.edu

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</a></div></div></div></div><div class="right-panel-container"><div class="user-content-wrapper"><div class="uploads-container" id="social-redesign-work-container"><div class="upload-header"><h2 class="ds2-5-heading-sans-serif-xs">Uploads</h2></div><div class="documents-container backbone-social-profile-documents" style="width: 100%;"><div class="u-taCenter"></div><div class="profile--tab_content_container js-tab-pane tab-pane active" id="all"><div class="profile--tab_heading_container js-section-heading" data-section="Papers" id="Papers"><h3 class="profile--tab_heading_container">Papers by Patrick Meire</h3></div><div class="js-work-strip profile--work_container" data-work-id="99924468"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/99924468/The_Scheldt_estuary_a_description_of_a_changing_ecosystem"><img alt="Research paper thumbnail of The Scheldt estuary: a description of a changing ecosystem" class="work-thumbnail" src="https://attachments.academia-assets.com/100884371/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/99924468/The_Scheldt_estuary_a_description_of_a_changing_ecosystem">The Scheldt estuary: a description of a changing ecosystem</a></div><div class="wp-workCard_item"><span>Hydrobiologia</span><span>, 2005</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Estuaries are naturally highly dynamic and rapidly changing systems, forming a complex mixture of...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Estuaries are naturally highly dynamic and rapidly changing systems, forming a complex mixture of many different habitat types. They are very productive biomes and support many important ecosystem functions: biogeochemical cycling and movement of nutrients, mitigation of floods, maintenance of biodiversity and biological production. Human pressure on estuaries is very high. On the other hand, it is recognized that estuaries have a unique functional and structural biodiversity. Therefore, these ecosystems are particularly important for integrating sound ecological management with sustainable economics. These opportunities are explored for the Scheldt estuary, a well-documented system with an exceptional tidal freshwater area. In this article a description of the Scheldt estuary is presented, illustrating that human influence is intertwined with natural dynamics. Hydrology, geomorphology, trophic status and diversity are discussed, and possible future trends in both natural evolution and management are argued.</span></div><div class="wp-workCard_item"><div class="carousel-container carousel-container--sm" id="profile-work-99924468-figures"><div class="prev-slide-container js-prev-button-container"><button aria-label="Previous" class="carousel-navigation-button js-profile-work-99924468-figures-prev"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">arrow_back_ios</span></button></div><div class="slides-container js-slides-container"><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325021/figure-1-map-of-the-scheldt-estuary"><img alt="Figure 1. Map of the Scheldt estuary. " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/figure_001.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325039/figure-3-duration-of-the-period-of-rising-tide-along-the-lon"><img alt="Figure 3. Duration of the period of rising tide along the lon- gitudinal gradient of the Scheldt estuary (based on data of the Maritime Access Division of the Flemish Government). Figure 2. Fresh water discharge in the Scheldt estuary at Schelle (period 1990-2004) (source data: Maritime Access Division, Flemisch Government). " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/figure_002.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325052/figure-3-the-scheldt-estuary-description-of-changing"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/100884371/figure_003.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325064/figure-4-amounts-of-dredged-volume-in-the-scheldt-estuary-in"><img alt="Figure 4. Amounts of dredged volume in the Scheldt estuary in Belgium (B) and the Netherlands (NL) (period 1990-2003) (source: Maritime Access Division of the Flemish government). " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/figure_004.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325074/figure-5-channel-depth-at-locations-in-the-westerschelde"><img alt="Figure 5. Channel depth at 4 locations in the Westerschelde (GLLWS = level at averaged minimal low spring tide) (based on data of the Ministry of Transport, Public Works and Water Management of the Netherlands). " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/figure_005.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325083/figure-6-habitat-area-evolution-in-the-westerschelde-over"><img alt="Figure 6. Habitat area evolution in the Westerschelde over the last centuries. NAP =the Dutch standard altitude reference level, the relation with the Belgian TAW standard is: NAP (m) + 2.33 m=TAW (m) (source: Ministry of Transport, Public Works and Water Management of the Netherlands). " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/figure_006.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325092/figure-7-evolution-of-mean-high-water-level-mhw-squares-and"><img alt="Figure 7. Evolution of mean high water level (MHW, squares) and mean low water level (MLW, open circles) in the Scheldt estuary near Antwerpen (based on data of the Maritime Access Division of the Flemish Government). Intertidal habitat was also lost due to dike building. In order to protect the land against storm floods from the North Sea all dikes along the estuary (more than 700 km) have been heightened and strengthened. Therefore, the base of the dikes needed to be widened, which was mostly done on the marshes and not on the landside of the dike. By now, over more than 50% of the total length of the estuary lacks tidal marshes in front of the dike. This disrupted the connectivity of marshes along the salinity gradient. " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/figure_007.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325098/figure-8-diversity-number-of-species-along-the-salinity-gra"><img alt="Figure 8. Diversity (number of species) along the salinity gra- dient of the Scheldt estuary (after Van den Bergh et al., 2001). " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/figure_008.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325105/table-1-some-characteristics-of-the-scheldt-estuary-at"><img alt="Table 1. Some characteristics of the Scheldt estuary at several locations (based on data of the Maritime Access Division of the Flemish Government). For positions of the locations see Figure 1 " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/table_001.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325115/table-2-habitat-surface-ha-in-the-scheldt-estuary-ited-and"><img alt="Table 2. Habitat surface (ha) in the Scheldt estuary ited and resuspended by the tidal flow. The dis- tribution of suspended matter is influenced by a range of interrelated processes (e.g. temperature and biological activity, fresh water discharge and salinity, hydrodynamic conditions and turbulence, mineralogical composition, chemical conditions, aggregation and flocculation). In the Scheldt estuary, the turbidity maximum is situated at about 110 km from the mouth during dry periods and at about 50 km during wet periods (Wollast, 1988). Two MTZ might be observed, one at the freshwater/seawater interface, and a second one originating from tidal asymmetry (Baeyens et al., 1998; Fettweis et al., 1998; Herman &amp; Heip, 1999). " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/table_002.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325125/table-3-river-bank-characteristics-of-the-zeeschelde-between"><img alt="Table 3. River bank characteristics of the Zeeschelde between the Dutch Belgian border and Ghent (after Hoffmann &amp; Meire, 1997 observed along the salinity gradient of the Schelde estuary (Ysebaert et al., 2000). Biodiversity " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/table_003.jpg" /></a></figure></div><div class="next-slide-container js-next-button-container"><button aria-label="Next" class="carousel-navigation-button js-profile-work-99924468-figures-next"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">arrow_forward_ios</span></button></div></div></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="3a93f4f36ef063972004cf7e1acbde07" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:100884371,&quot;asset_id&quot;:99924468,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/100884371/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="99924468"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="99924468"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 99924468; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=99924468]").text(description); $(".js-view-count[data-work-id=99924468]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 99924468; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='99924468']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "3a93f4f36ef063972004cf7e1acbde07" } } $('.js-work-strip[data-work-id=99924468]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":99924468,"title":"The Scheldt estuary: a description of a changing ecosystem","translated_title":"","metadata":{"publisher":"Springer Science and Business Media LLC","grobid_abstract":"Estuaries are naturally highly dynamic and rapidly changing systems, forming a complex mixture of many different habitat types. They are very productive biomes and support many important ecosystem functions: biogeochemical cycling and movement of nutrients, mitigation of floods, maintenance of biodiversity and biological production. Human pressure on estuaries is very high. On the other hand, it is recognized that estuaries have a unique functional and structural biodiversity. Therefore, these ecosystems are particularly important for integrating sound ecological management with sustainable economics. These opportunities are explored for the Scheldt estuary, a well-documented system with an exceptional tidal freshwater area. In this article a description of the Scheldt estuary is presented, illustrating that human influence is intertwined with natural dynamics. 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Nevertheless, insitu ob...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Tidal wetlands are increasingly valued for their role in coastal defense. Nevertheless, insitu observations of storm surge attenuation within wetlands are still scarce. We present water level measurements along a 4 km intertidal channel and on the surrounding marsh platform for regular spring to neap tides and two major storm surge tides, showing the effects of flood wave height and marsh geomorphology on the amount of flood wave attenuation. Undermarsh tides with peak water levels below marsh platform elevation are mostly amplified (up to 4 cm/km) within the channels. Overmarsh tides with peak water levels above the marsh platform are generally attenuated along the channels, with maximum attenuation rates of 5 cm/km for tides that inundate the marsh platform by 0.5-1.0 m. For lower or higher flood waves, including storm surges, attenuation rates decrease. Furthermore, the observations show that the maximum attenuation occurs along narrow channel transects where the width of the platform is larger, whereas attenuation rates are lower along wider channels with smaller adjacent marsh platforms. These observations are confirmed by an analytical approximation of tidal wave propagation through convergent channels. The analytical model indicates that differences in attenuation rates are induced by variations in the cross-channel averaged friction between channel sections and between tides with varying peak water levels. Finally, the highest attenuation rates of up to 70 cm/km are observed over short distances on the vegetated marsh platform. We conclude that this 2 study provides an empirical basis for the wider implementation of nature-based flood defense 18 strategies.</span></div><div class="wp-workCard_item"><div class="carousel-container carousel-container--sm" id="profile-work-95887013-figures"><div class="prev-slide-container js-prev-button-container"><button aria-label="Previous" class="carousel-navigation-button js-profile-work-95887013-figures-prev"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">arrow_back_ios</span></button></div><div class="slides-container js-slides-container"><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754256/figure-1-observations-of-tidal-and-storm-surge-attenuation"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/97942111/figure_001.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754263/figure-2-observations-of-tidal-and-storm-surge-attenuation"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/97942111/figure_002.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754269/figure-3-observations-of-tidal-and-storm-surge-attenuation"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/97942111/figure_003.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754273/figure-4-observations-of-tidal-and-storm-surge-attenuation"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/97942111/figure_004.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754277/figure-5-observations-of-tidal-and-storm-surge-attenuation"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/97942111/figure_005.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754284/figure-6-observations-of-tidal-and-storm-surge-attenuation"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/97942111/figure_006.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754288/figure-7-observations-of-tidal-and-storm-surge-attenuation"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/97942111/figure_007.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754294/figure-8-observations-of-tidal-and-storm-surge-attenuation"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/97942111/figure_008.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754298/table-1-values-denote-that-amplification-was-observed"><img alt="values denote that amplification was observed. " class="figure-slide-image" src="https://figures.academia-assets.com/97942111/table_001.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754310/table-2-hmean-maximum-channel-depth-below-mhwl-hyax-and"><img alt="(Hmean), Maximum channel depth below MHWL (hyax) and cross-sectional area (A,). 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Nevertheless, insitu observations of storm surge attenuation within wetlands are still scarce. We present water level measurements along a 4 km intertidal channel and on the surrounding marsh platform for regular spring to neap tides and two major storm surge tides, showing the effects of flood wave height and marsh geomorphology on the amount of flood wave attenuation. Undermarsh tides with peak water levels below marsh platform elevation are mostly amplified (up to 4 cm/km) within the channels. Overmarsh tides with peak water levels above the marsh platform are generally attenuated along the channels, with maximum attenuation rates of 5 cm/km for tides that inundate the marsh platform by 0.5-1.0 m. For lower or higher flood waves, including storm surges, attenuation rates decrease. Furthermore, the observations show that the maximum attenuation occurs along narrow channel transects where the width of the platform is larger, whereas attenuation rates are lower along wider channels with smaller adjacent marsh platforms. These observations are confirmed by an analytical approximation of tidal wave propagation through convergent channels. The analytical model indicates that differences in attenuation rates are induced by variations in the cross-channel averaged friction between channel sections and between tides with varying peak water levels. Finally, the highest attenuation rates of up to 70 cm/km are observed over short distances on the vegetated marsh platform. We conclude that this 2 study provides an empirical basis for the wider implementation of nature-based flood defense 18 strategies.","owner":{"id":184662190,"first_name":"Patrick","middle_initials":null,"last_name":"Meire","page_name":"MeireP","domain_name":"independent","created_at":"2021-02-03T07:39:55.559-08:00","display_name":"Patrick Meire","url":"https://independent.academia.edu/MeireP"},"attachments":[{"id":97942111,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942111/thumbnails/1.jpg","file_name":"10505.pdf","download_url":"https://www.academia.edu/attachments/97942111/download_file","bulk_download_file_name":"Observations_of_tidal_and_storm_surge_at.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942111/10505-libre.pdf?1674982274=\u0026response-content-disposition=attachment%3B+filename%3DObservations_of_tidal_and_storm_surge_at.pdf\u0026Expires=1743224694\u0026Signature=MHsC3evubGCkKckaE8Pzwry2bV3pV8p3c8h-cHqgyTUE0y7XWN6YZVtcNq9SzPT6galJmFojfHSjFHVPRQlZI5snb21ceONogfjXUrzD2EyLWybWDVJXmXjsn7fvG6VtW4P9bgMWdrwvLJbajqY8ztpr1o~xe92IjmwgXmBVCGvf57-A~hr6PdCdxN216kbI8dEwc71xAju4o2piSYPg30F2DW5qTlHlIzr5pEJapQXZjyES-DjBVAi-ZGi~XCrKGa5ZHRntHQRiexeqH-WUx90IBiiZGYdmvV4E22ljwZvfk2iBBfjD~bgfThIH5IDYNNvBh~W4kXc8RH3xjEUB8Q__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":7710,"name":"Biology","url":"https://www.academia.edu/Documents/in/Biology"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences"},{"id":162136,"name":"Storm","url":"https://www.academia.edu/Documents/in/Storm"},{"id":216197,"name":"Biological Oceanography and Limnology","url":"https://www.academia.edu/Documents/in/Biological_Oceanography_and_Limnology"},{"id":398869,"name":"Intertidal Zone","url":"https://www.academia.edu/Documents/in/Intertidal_Zone"},{"id":556983,"name":"Storm surge","url":"https://www.academia.edu/Documents/in/Storm_surge"},{"id":580672,"name":"Tidal Flat","url":"https://www.academia.edu/Documents/in/Tidal_Flat"},{"id":951108,"name":"Attenuation","url":"https://www.academia.edu/Documents/in/Attenuation"},{"id":956838,"name":"Marsh","url":"https://www.academia.edu/Documents/in/Marsh"},{"id":1227220,"name":"Surge","url":"https://www.academia.edu/Documents/in/Surge"},{"id":3647976,"name":"Flood Myth","url":"https://www.academia.edu/Documents/in/Flood_Myth"}],"urls":[{"id":28485835,"url":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Flno.10104"}]}, dispatcherData: dispatcherData }); 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This theory implies that thresholds of environmental factors can mark a limit between two opposing stable ecosystem states, e.g. vegetated marshes and bare mudflats. While elevation relative to mean sea level is considered as the overall threshold condition for colonization of mudflats by vegetation, little is known about the individual driving mechanisms, in particular the impact of waves, and more specifically of wave period. We studied the impact of different wave regimes on plants in a full scale flume experiment. Seedlings and adult shoots of the pioneer Scirpus maritimus were subjected to two wave periods at two water levels. Drag forces acting on, and sediment scouring occurring around the plants were quantified, as these are the two main mechanisms determining plant establishment and survival. 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It has nume...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Silicon is one of the most important elements in the current age of the anthropocene. It has numerous industrial applications, and supports a high-tech multi-billion Euro industry. Silicon has a fascinating biological and geological cycle, interacting with other globally important biogeochemical cycles. 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Nevertheless, spatial planning decisions would benefit from systematic considerations of their effects on ecosystem services. Assessing the impacts of policy on a wide range of ecosystem services contributes to more cost-effective policy implementation, establishing win-win situations across different environmental domains. The “nature value explorer” (natuurwaardeverkenner in Dutch) is a web application developed to explore the quantity and value of ecosystem services in Flanders, Belgium, as part of environmental impact assessments. The tool estimates the impact of land-use and land-cover change on regulating and cultural ecosystem services. 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Nevertheless, spatial planning decisions would benefit from systematic considerations of their effects on ecosystem services. Assessing the impacts of policy on a wide range of ecosystem services contributes to more cost-effective policy implementation, establishing win-win situations across different environmental domains. The “nature value explorer” (natuurwaardeverkenner in Dutch) is a web application developed to explore the quantity and value of ecosystem services in Flanders, Belgium, as part of environmental impact assessments. The tool estimates the impact of land-use and land-cover change on regulating and cultural ecosystem services. The web application is successful in drawing the interest of policy makers and is used in several cases to support decisions in infrastructural projects as well as nature restoration projects.","owner":{"id":184662190,"first_name":"Patrick","middle_initials":null,"last_name":"Meire","page_name":"MeireP","domain_name":"independent","created_at":"2021-02-03T07:39:55.559-08:00","display_name":"Patrick Meire","url":"https://independent.academia.edu/MeireP"},"attachments":[],"research_interests":[{"id":26,"name":"Business","url":"https://www.academia.edu/Documents/in/Business"},{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":2312,"name":"Ecosystem Services","url":"https://www.academia.edu/Documents/in/Ecosystem_Services"},{"id":7710,"name":"Biology","url":"https://www.academia.edu/Documents/in/Biology"},{"id":62646,"name":"Environmental Resource Management","url":"https://www.academia.edu/Documents/in/Environmental_Resource_Management"},{"id":95993,"name":"Web Application","url":"https://www.academia.edu/Documents/in/Web_Application"},{"id":417820,"name":"Scenario Analysis","url":"https://www.academia.edu/Documents/in/Scenario_Analysis"},{"id":457859,"name":"Cost Benefit Analysis","url":"https://www.academia.edu/Documents/in/Cost_Benefit_Analysis"},{"id":2497410,"name":"Monetary valuation","url":"https://www.academia.edu/Documents/in/Monetary_valuation"},{"id":2960847,"name":"ecosystem valuation","url":"https://www.academia.edu/Documents/in/ecosystem_valuation"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95887007-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95887006"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95887006/Dissolved_Silicon_and_Its_Origin_in_Belgian_Beers_A_Multivariate_Analysis"><img alt="Research paper thumbnail of Dissolved Silicon and Its Origin in Belgian Beers—A Multivariate Analysis" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title">Dissolved Silicon and Its Origin in Belgian Beers—A Multivariate Analysis</div><div class="wp-workCard_item"><span>Silicon</span><span>, 2012</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">ABSTRACT Beer is a quintessential part of Belgian heritage. We performed a detailed analysis of f...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">ABSTRACT Beer is a quintessential part of Belgian heritage. We performed a detailed analysis of factors controlling Si content in Belgian beers as a case study to coincide with the 2011 IBiS meeting in Antwerp (Belgium). Beer is one of the richest dietary sources of Si. Three decades of research have yielded evidence of a role for Si in human physiology: it plays an essential role in bone mineral density and reduces the biological availability of aluminium. We analysed 119 Belgian beers: highest dissolved Si concentrations were found in high fermentation, traditionally brewed ales. Concentrations ranged between 214 and 2,071 μmol L − 1. This is probably due to the complexity and length of the brewing procedure: longer, more complicated processing and presence of brewing sediment in the bottle allows more Si to dissolve out of the base products like hop, barley or even rice. As a side effect of fermentation, alcohol content was related to Si content.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95887006"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95887006"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95887006; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95887006]").text(description); $(".js-view-count[data-work-id=95887006]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95887006; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95887006']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=95887006]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95887006,"title":"Dissolved Silicon and Its Origin in Belgian Beers—A Multivariate Analysis","translated_title":"","metadata":{"abstract":"ABSTRACT Beer is a quintessential part of Belgian heritage. We performed a detailed analysis of factors controlling Si content in Belgian beers as a case study to coincide with the 2011 IBiS meeting in Antwerp (Belgium). Beer is one of the richest dietary sources of Si. Three decades of research have yielded evidence of a role for Si in human physiology: it plays an essential role in bone mineral density and reduces the biological availability of aluminium. We analysed 119 Belgian beers: highest dissolved Si concentrations were found in high fermentation, traditionally brewed ales. Concentrations ranged between 214 and 2,071 μmol L − 1. This is probably due to the complexity and length of the brewing procedure: longer, more complicated processing and presence of brewing sediment in the bottle allows more Si to dissolve out of the base products like hop, barley or even rice. As a side effect of fermentation, alcohol content was related to Si content.","publisher":"Springer Nature","publication_date":{"day":null,"month":null,"year":2012,"errors":{}},"publication_name":"Silicon"},"translated_abstract":"ABSTRACT Beer is a quintessential part of Belgian heritage. We performed a detailed analysis of factors controlling Si content in Belgian beers as a case study to coincide with the 2011 IBiS meeting in Antwerp (Belgium). Beer is one of the richest dietary sources of Si. Three decades of research have yielded evidence of a role for Si in human physiology: it plays an essential role in bone mineral density and reduces the biological availability of aluminium. We analysed 119 Belgian beers: highest dissolved Si concentrations were found in high fermentation, traditionally brewed ales. Concentrations ranged between 214 and 2,071 μmol L − 1. This is probably due to the complexity and length of the brewing procedure: longer, more complicated processing and presence of brewing sediment in the bottle allows more Si to dissolve out of the base products like hop, barley or even rice. As a side effect of fermentation, alcohol content was related to Si content.","internal_url":"https://www.academia.edu/95887006/Dissolved_Silicon_and_Its_Origin_in_Belgian_Beers_A_Multivariate_Analysis","translated_internal_url":"","created_at":"2023-01-29T00:36:08.956-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":184662190,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Dissolved_Silicon_and_Its_Origin_in_Belgian_Beers_A_Multivariate_Analysis","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"ABSTRACT Beer is a quintessential part of Belgian heritage. We performed a detailed analysis of factors controlling Si content in Belgian beers as a case study to coincide with the 2011 IBiS meeting in Antwerp (Belgium). Beer is one of the richest dietary sources of Si. Three decades of research have yielded evidence of a role for Si in human physiology: it plays an essential role in bone mineral density and reduces the biological availability of aluminium. We analysed 119 Belgian beers: highest dissolved Si concentrations were found in high fermentation, traditionally brewed ales. Concentrations ranged between 214 and 2,071 μmol L − 1. This is probably due to the complexity and length of the brewing procedure: longer, more complicated processing and presence of brewing sediment in the bottle allows more Si to dissolve out of the base products like hop, barley or even rice. As a side effect of fermentation, alcohol content was related to Si content.","owner":{"id":184662190,"first_name":"Patrick","middle_initials":null,"last_name":"Meire","page_name":"MeireP","domain_name":"independent","created_at":"2021-02-03T07:39:55.559-08:00","display_name":"Patrick Meire","url":"https://independent.academia.edu/MeireP"},"attachments":[],"research_interests":[{"id":498,"name":"Physics","url":"https://www.academia.edu/Documents/in/Physics"},{"id":511,"name":"Materials Science","url":"https://www.academia.edu/Documents/in/Materials_Science"},{"id":523,"name":"Chemistry","url":"https://www.academia.edu/Documents/in/Chemistry"},{"id":1907,"name":"Nutrition","url":"https://www.academia.edu/Documents/in/Nutrition"},{"id":7710,"name":"Biology","url":"https://www.academia.edu/Documents/in/Biology"},{"id":11406,"name":"Silicon","url":"https://www.academia.edu/Documents/in/Silicon"},{"id":67429,"name":"Brewing","url":"https://www.academia.edu/Documents/in/Brewing"},{"id":269129,"name":"Fermentation","url":"https://www.academia.edu/Documents/in/Fermentation"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95887006-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95887005"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/95887005/Landscape_cultivation_alters_%CE%B4_30_Si_signature_in_terrestrial_ecosystems"><img alt="Research paper thumbnail of Landscape cultivation alters δ(30)Si signature in terrestrial ecosystems" class="work-thumbnail" src="https://attachments.academia-assets.com/97942107/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95887005/Landscape_cultivation_alters_%CE%B4_30_Si_signature_in_terrestrial_ecosystems">Landscape cultivation alters δ(30)Si signature in terrestrial ecosystems</a></div><div class="wp-workCard_item"><span>Scientific reports</span><span>, Jan 13, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Despite increasing recognition of the relevance of biological cycling for Si cycling in ecosystem...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Despite increasing recognition of the relevance of biological cycling for Si cycling in ecosystems and for Si export from soils to fluvial systems, effects of human cultivation on the Si cycle are still relatively understudied. Here we examined stable Si isotope (δ(30)Si) signatures in soil water samples across a temperate land use gradient. We show that - independent of geological and climatological variation - there is a depletion in light isotopes in soil water of intensive croplands and managed grasslands relative to native forests. Furthermore, our data suggest a divergence in δ(30)Si signatures along the land use change gradient, highlighting the imprint of vegetation cover, human cultivation and intensity of disturbance on δ(30)Si patterns, on top of more conventionally acknowledged drivers (i.e. mineralogy and climate).</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="5e065f5077ec46cb09ee36b61b09fdad" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942107,&quot;asset_id&quot;:95887005,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942107/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95887005"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95887005"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95887005; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95887005]").text(description); $(".js-view-count[data-work-id=95887005]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95887005; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95887005']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "5e065f5077ec46cb09ee36b61b09fdad" } } $('.js-work-strip[data-work-id=95887005]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95887005,"title":"Landscape cultivation alters δ(30)Si signature in terrestrial ecosystems","translated_title":"","metadata":{"abstract":"Despite increasing recognition of the relevance of biological cycling for Si cycling in ecosystems and for Si export from soils to fluvial systems, effects of human cultivation on the Si cycle are still relatively understudied. Here we examined stable Si isotope (δ(30)Si) signatures in soil water samples across a temperate land use gradient. We show that - independent of geological and climatological variation - there is a depletion in light isotopes in soil water of intensive croplands and managed grasslands relative to native forests. Furthermore, our data suggest a divergence in δ(30)Si signatures along the land use change gradient, highlighting the imprint of vegetation cover, human cultivation and intensity of disturbance on δ(30)Si patterns, on top of more conventionally acknowledged drivers (i.e. mineralogy and climate).","ai_title_tag":"Human cultivation impacts δ(30)Si signatures in soils","publication_date":{"day":13,"month":1,"year":2015,"errors":{}},"publication_name":"Scientific reports"},"translated_abstract":"Despite increasing recognition of the relevance of biological cycling for Si cycling in ecosystems and for Si export from soils to fluvial systems, effects of human cultivation on the Si cycle are still relatively understudied. Here we examined stable Si isotope (δ(30)Si) signatures in soil water samples across a temperate land use gradient. We show that - independent of geological and climatological variation - there is a depletion in light isotopes in soil water of intensive croplands and managed grasslands relative to native forests. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95887005-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95887004"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95887004/Determination_of_groundwater_fluxes_in_the_Belgian_Aa_River_by_sensing_and_simulation_of_streambed_temperatures"><img alt="Research paper thumbnail of Determination of groundwater fluxes in the Belgian Aa River by sensing and simulation of streambed temperatures" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title">Determination of groundwater fluxes in the Belgian Aa River by sensing and simulation of streambed temperatures</div><div class="wp-workCard_item"><span>IAHS Publications- …</span><span>, 2008</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95887004"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95887004"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95887004; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95887004-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95887003"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/95887003/Pathological_investigations_on_guillemots_Uria_aalge_stranded_on_the_Belgian_coast_during_the_winter_of_1993_94"><img alt="Research paper thumbnail of Pathological investigations on guillemots (Uria aalge ) stranded on the Belgian coast during the winter of 1993-94" class="work-thumbnail" src="https://attachments.academia-assets.com/97942110/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95887003/Pathological_investigations_on_guillemots_Uria_aalge_stranded_on_the_Belgian_coast_during_the_winter_of_1993_94">Pathological investigations on guillemots (Uria aalge ) stranded on the Belgian coast during the winter of 1993-94</a></div><div class="wp-workCard_item"><span>Veterinary Record</span><span>, 1998</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d0260093b22df7cc96e29d664f69066d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942110,&quot;asset_id&quot;:95887003,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942110/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95887003"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95887003"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95887003; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95887003-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95887002"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/95887002/Ecological_Rehabilitation_of_the_Schelde_Estuary_The_Netherlands_Belgium_Northwest_Europe_Linking_Ecology_Safety_Against_Floods_and_Accessibility_for_Port_Development"><img alt="Research paper thumbnail of Ecological Rehabilitation of the Schelde Estuary (The Netherlands-Belgium; Northwest Europe): Linking Ecology, Safety Against Floods, and Accessibility for Port Development" class="work-thumbnail" src="https://attachments.academia-assets.com/97942109/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95887002/Ecological_Rehabilitation_of_the_Schelde_Estuary_The_Netherlands_Belgium_Northwest_Europe_Linking_Ecology_Safety_Against_Floods_and_Accessibility_for_Port_Development">Ecological Rehabilitation of the Schelde Estuary (The Netherlands-Belgium; Northwest Europe): Linking Ecology, Safety Against Floods, and Accessibility for Port Development</a></div><div class="wp-workCard_item"><span>Restoration Ecology</span><span>, 2005</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Long-Term Vision for the Schelde estuary was determined as &#39;&#39;the development of a healthy and...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The Long-Term Vision for the Schelde estuary was determined as &#39;&#39;the development of a healthy and multifunctional estuarine water system that can be utilized in a sustainable way for human needs.&#39;&#39; This Dutch-Flemish managerial plan sets quality targets for the condition of the estuary by the year 2030 and the management measures to achieve them. Targets were developed and integrated from three central perspectives: accessibility of the ports, safety against floods in the densely populated catchment, and ecosystem health. This study focuses on the ecological rehabilitation of the estuary and the creation of sustainable nature, seeking possible alliances with security measures against floods, navigation requisites for port activities, and enhancement of the estuary&#39;s educational and recreational values. The estuary and its valley were subdivided into ecologically relevant zones. Key parameters were identified, and a conceptual rehabilitation model was developed, based on a problem analysis. Goals were set in a semiquantified way for most attributes of the estuarine functioning and prioritized for each zone. Rehabilitation measures with maximal contribution to the priority goals were identified for each zone. Spatial analysis of the study area indicated optimal areas for the implementation of these measures. To exemplify the array of possibilities on an ecosystem level, two different rehabilitation plans were proposed, each from a different approach. The potential contribution to the rehabilitation of the estuary was compared for both alternatives.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="bf9d5aae669bb8f683fd849abecf7d65" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942109,&quot;asset_id&quot;:95887002,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942109/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95887002"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95887002"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95887002; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95887002]").text(description); $(".js-view-count[data-work-id=95887002]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95887002; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95887002']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "bf9d5aae669bb8f683fd849abecf7d65" } } $('.js-work-strip[data-work-id=95887002]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95887002,"title":"Ecological Rehabilitation of the Schelde Estuary (The Netherlands-Belgium; Northwest Europe): Linking Ecology, Safety Against Floods, and Accessibility for Port Development","translated_title":"","metadata":{"publisher":"Wiley-Blackwell","ai_title_tag":"Ecological Rehabilitation of the Schelde Estuary: Balancing Ecology, Flood Safety, and Port Accessibility","grobid_abstract":"The Long-Term Vision for the Schelde estuary was determined as ''the development of a healthy and multifunctional estuarine water system that can be utilized in a sustainable way for human needs.'' This Dutch-Flemish managerial plan sets quality targets for the condition of the estuary by the year 2030 and the management measures to achieve them. Targets were developed and integrated from three central perspectives: accessibility of the ports, safety against floods in the densely populated catchment, and ecosystem health. This study focuses on the ecological rehabilitation of the estuary and the creation of sustainable nature, seeking possible alliances with security measures against floods, navigation requisites for port activities, and enhancement of the estuary's educational and recreational values. The estuary and its valley were subdivided into ecologically relevant zones. Key parameters were identified, and a conceptual rehabilitation model was developed, based on a problem analysis. Goals were set in a semiquantified way for most attributes of the estuarine functioning and prioritized for each zone. Rehabilitation measures with maximal contribution to the priority goals were identified for each zone. Spatial analysis of the study area indicated optimal areas for the implementation of these measures. To exemplify the array of possibilities on an ecosystem level, two different rehabilitation plans were proposed, each from a different approach. The potential contribution to the rehabilitation of the estuary was compared for both alternatives.","publication_date":{"day":null,"month":null,"year":2005,"errors":{}},"publication_name":"Restoration Ecology","grobid_abstract_attachment_id":97942109},"translated_abstract":null,"internal_url":"https://www.academia.edu/95887002/Ecological_Rehabilitation_of_the_Schelde_Estuary_The_Netherlands_Belgium_Northwest_Europe_Linking_Ecology_Safety_Against_Floods_and_Accessibility_for_Port_Development","translated_internal_url":"","created_at":"2023-01-29T00:36:08.500-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":184662190,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":97942109,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942109/thumbnails/1.jpg","file_name":"174185.pdf","download_url":"https://www.academia.edu/attachments/97942109/download_file","bulk_download_file_name":"Ecological_Rehabilitation_of_the_Schelde.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942109/174185-libre.pdf?1674982265=\u0026response-content-disposition=attachment%3B+filename%3DEcological_Rehabilitation_of_the_Schelde.pdf\u0026Expires=1743224695\u0026Signature=YZ6d7gW8tpZFOKdM8kCqW-3EV3YoQH82AUc-t8aCqf9QW2MlTLXX-oe3gDel0ITotlNMqqbCv527d-TFkdHzYtWd2Bb4F6izjSBqoDIxwZnGR3GiigqrXEYtB9soN3uWGeaGVJmbvMNq7KZGYA4j7ZOn6I4PTuYyuBJPL-20SxvdYHtKcDUGZ-xROk4d1TDEnhvORVYHk~MnuZCLwgdnvgWjH1xVQ3xS7t9jp0z7r~MDlOvSFm7q6MvklDFRi2~dfEeUzqP47jdJ92ykisl9bjGLcis4k5vvP-p~94WpUoEPba8aoCwKiAKxFLAOiQ4dRyCnhfhlpj2eY5h21Jw3Yw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Ecological_Rehabilitation_of_the_Schelde_Estuary_The_Netherlands_Belgium_Northwest_Europe_Linking_Ecology_Safety_Against_Floods_and_Accessibility_for_Port_Development","translated_slug":"","page_count":11,"language":"en","content_type":"Work","summary":"The Long-Term Vision for the Schelde estuary was determined as ''the development of a healthy and multifunctional estuarine water system that can be utilized in a sustainable way for human needs.'' This Dutch-Flemish managerial plan sets quality targets for the condition of the estuary by the year 2030 and the management measures to achieve them. Targets were developed and integrated from three central perspectives: accessibility of the ports, safety against floods in the densely populated catchment, and ecosystem health. This study focuses on the ecological rehabilitation of the estuary and the creation of sustainable nature, seeking possible alliances with security measures against floods, navigation requisites for port activities, and enhancement of the estuary's educational and recreational values. The estuary and its valley were subdivided into ecologically relevant zones. Key parameters were identified, and a conceptual rehabilitation model was developed, based on a problem analysis. Goals were set in a semiquantified way for most attributes of the estuarine functioning and prioritized for each zone. Rehabilitation measures with maximal contribution to the priority goals were identified for each zone. Spatial analysis of the study area indicated optimal areas for the implementation of these measures. To exemplify the array of possibilities on an ecosystem level, two different rehabilitation plans were proposed, each from a different approach. The potential contribution to the rehabilitation of the estuary was compared for both alternatives.","owner":{"id":184662190,"first_name":"Patrick","middle_initials":null,"last_name":"Meire","page_name":"MeireP","domain_name":"independent","created_at":"2021-02-03T07:39:55.559-08:00","display_name":"Patrick Meire","url":"https://independent.academia.edu/MeireP"},"attachments":[{"id":97942109,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942109/thumbnails/1.jpg","file_name":"174185.pdf","download_url":"https://www.academia.edu/attachments/97942109/download_file","bulk_download_file_name":"Ecological_Rehabilitation_of_the_Schelde.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942109/174185-libre.pdf?1674982265=\u0026response-content-disposition=attachment%3B+filename%3DEcological_Rehabilitation_of_the_Schelde.pdf\u0026Expires=1743224695\u0026Signature=YZ6d7gW8tpZFOKdM8kCqW-3EV3YoQH82AUc-t8aCqf9QW2MlTLXX-oe3gDel0ITotlNMqqbCv527d-TFkdHzYtWd2Bb4F6izjSBqoDIxwZnGR3GiigqrXEYtB9soN3uWGeaGVJmbvMNq7KZGYA4j7ZOn6I4PTuYyuBJPL-20SxvdYHtKcDUGZ-xROk4d1TDEnhvORVYHk~MnuZCLwgdnvgWjH1xVQ3xS7t9jp0z7r~MDlOvSFm7q6MvklDFRi2~dfEeUzqP47jdJ92ykisl9bjGLcis4k5vvP-p~94WpUoEPba8aoCwKiAKxFLAOiQ4dRyCnhfhlpj2eY5h21Jw3Yw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"},{"id":1362,"name":"Spatial Analysis","url":"https://www.academia.edu/Documents/in/Spatial_Analysis"},{"id":2256,"name":"Rehabilitation","url":"https://www.academia.edu/Documents/in/Rehabilitation"},{"id":5221,"name":"Restoration Ecology","url":"https://www.academia.edu/Documents/in/Restoration_Ecology"},{"id":17374,"name":"Restoration","url":"https://www.academia.edu/Documents/in/Restoration"},{"id":22142,"name":"Ecosystem health","url":"https://www.academia.edu/Documents/in/Ecosystem_health"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences"},{"id":62646,"name":"Environmental Resource Management","url":"https://www.academia.edu/Documents/in/Environmental_Resource_Management"},{"id":95108,"name":"RECREATION","url":"https://www.academia.edu/Documents/in/RECREATION"},{"id":202017,"name":"Integrated Management","url":"https://www.academia.edu/Documents/in/Integrated_Management"},{"id":379570,"name":"Estuary","url":"https://www.academia.edu/Documents/in/Estuary"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95887002-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95887001"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/95887001/Macrobenthic_species_response_surfaces_along_estuarine_gradients_prediction_by_logistic_regression"><img alt="Research paper thumbnail of Macrobenthic species response surfaces along estuarine gradients: prediction by logistic regression" class="work-thumbnail" src="https://attachments.academia-assets.com/97942091/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95887001/Macrobenthic_species_response_surfaces_along_estuarine_gradients_prediction_by_logistic_regression">Macrobenthic species response surfaces along estuarine gradients: prediction by logistic regression</a></div><div class="wp-workCard_item"><span>Marine Ecology Progress Series</span><span>, 2002</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e6c4edc92eef43f7c8da91169bc4f024" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942091,&quot;asset_id&quot;:95887001,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942091/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95887001"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95887001"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95887001; 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Ecological response surfaces are derived for 10 estuarine macrobenthic species. Logistic regression is applied on a large data set, predicting the probability of occurrence of macrobenthic species in the Schelde estuary as a response to the predictor variables salinity, depth, current velocity and sediment characteristics. Single logistic regression provides good descriptions of the occurrence along 1 environmental variable. The response surfaces obtained by multiple logistic regression provide estimates of the probability of species occurrence across the spatial extent of the Schelde estuary with a relatively high degree of success. Results from subsampling 50% of the original data 10 times indicate that final models were stable. A visual geographical comparison is presented between the mapped probability surfaces and the species occurrence maps. We conclude that where patterns of distribution are strongly and directly coupled to physicochemical processes, as is the case at the estuarine macro-and meso-scale, our modelling approach was capable of predicting macrobenthic species distributions with a relatively high degree of success, although processes controlling estuarine macrobenthic distribution cannot be determined using this method. However, the models and predictions could be used for evaluation of the effects of different management schemes within the Schelde estuary.","ai_title_tag":"Logistic Regression of Estuarine Macrobenthos","publication_date":{"day":null,"month":null,"year":2002,"errors":{}},"publication_name":"Marine Ecology Progress 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in the Southern Bight of the North Sea" class="work-thumbnail" src="https://attachments.academia-assets.com/97942103/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95887000/Diversity_of_the_nematode_communities_in_the_Southern_Bight_of_the_North_Sea">Diversity of the nematode communities in the Southern Bight of the North Sea</a></div><div class="wp-workCard_item"><span>Netherlands Journal of Sea Research</span><span>, 1990</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The nematode communities from 102 stations in the Southern Bight of the North Sea, sumpled betwee...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The nematode communities from 102 stations in the Southern Bight of the North Sea, sumpled between 1972 and 1984, are exam ined. On the whole, 456 species, belonging to 159 genera and 37 families were found. Multispecies patterns are ana lysed by means of cluster analysis (Bray-Curtis dissimilarity coefficient), Twinspan c1 assitïcation and DCA ordination. Generall y, the Southern Bight can be div ided into six main areas on the base of nematode species composition. Sediment structure was fou nd to be the determining environmental factor in the species composition of nematode communit ies. Also several other environmental factors, (temperature, salinity, chlorophyll a, N03-, NH4+) seem ta influence the distribution of the nematode species. One of the most striking features of the coastal ecosystemS , and of the Belgian coastal zone in particular, is the importance of the role of the bacteria. A general increase of the level of primary production in the coastal area , as a result of increasing nutrient input, does not necessarily lead to an increase of pelagie or demersal fish production, but cou Id induce a modification of the food web , in particular the enhancement of microbiological activity at the expense of long trophic chains dominated by macroorganisms. The near absence of nematode-predators in the reg ion off the Belgian east coast, the dom inance of bacterivores, the very low spec ies diversity of the nematode community and the paucity of higher metazoans within the area, can be partly explained on the basis of the increase in nutrient input within the area, and partly on the basis of the high amount of &quot;mixed&quot; pollution. Résumé: Identification des assemblages de nématodes de 102 stations de la partie sud de la mer du Nord où des prélèvements ont été effectués de 1972 il 1984 : 456 espèces ont été répertoriées, appartenant il 159 gen res et 37 familles. Interprétation des communautés par l&#39;analyse des groupements d&#39;espèces (coelficient de dissimilarité de Bray-Curtis et classification polythétique Twinspan) et par l&#39;analyse factorielle des correspondances (DCA). Global ement, le bassin du sud de la mer du Nord peut être di visé en six zones principales définies par la composition spécifiq ue des nématodes. La structure sédimentaire apparaît comme le facte ur du milieu déterminant de la composition spécifique de la nématocoenose ; cependant, d&#39;autres facteurs (température, salinité, ch lorophylle a, N03-, NH4+) semblent égaiement influer sur la distribution des espèces. L&#39;importance du rôle des bactéries représente l&#39;un des caractères les plus remarq uables des écosystèmes côtiers et, en particulier, de celui de la côte belge. Dans cette région, un accroissement du taux de production primaire, lié il une intensification de l&#39;apport de nutriments, n&#39;entraîne pas nécessairement l&#39;augmentation de la production en poissons pélagiques ou démersaux ; mais il pourrait provoquer des modifications des réseaux trophiques, notamment la stimulation de l&#39;activité microbiologique aux dépens des chaînes trophiques longues dominées par les macro-organismes. Au large de la côte est de Belgique, la dominance des nématodes bactérivores, la quasi-absence des prédateurs, la très faible diversité spécifique des communautés de ce groupe et la pauvreté des métazoaires supérieurs peuvent trouver leur expl ication d&#39;une part dans l&#39;augmentation de l&#39;apport en nutriments et d&#39;autre part dans la grande quantité de po llution diffuse.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ca98f2c0f41741edf5d1f9822e10153a" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942103,&quot;asset_id&quot;:95887000,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942103/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95887000"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95887000"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95887000; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95887000]").text(description); $(".js-view-count[data-work-id=95887000]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95887000; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95887000']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "ca98f2c0f41741edf5d1f9822e10153a" } } $('.js-work-strip[data-work-id=95887000]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95887000,"title":"Diversity of the nematode communities in the Southern Bight of the North Sea","translated_title":"","metadata":{"publisher":"Elsevier BV","ai_title_tag":"Nematode Community Diversity in the North Sea","grobid_abstract":"The nematode communities from 102 stations in the Southern Bight of the North Sea, sumpled between 1972 and 1984, are exam ined. On the whole, 456 species, belonging to 159 genera and 37 families were found. Multispecies patterns are ana lysed by means of cluster analysis (Bray-Curtis dissimilarity coefficient), Twinspan c1 assitïcation and DCA ordination. Generall y, the Southern Bight can be div ided into six main areas on the base of nematode species composition. Sediment structure was fou nd to be the determining environmental factor in the species composition of nematode communit ies. Also several other environmental factors, (temperature, salinity, chlorophyll a, N03-, NH4+) seem ta influence the distribution of the nematode species. One of the most striking features of the coastal ecosystemS , and of the Belgian coastal zone in particular, is the importance of the role of the bacteria. A general increase of the level of primary production in the coastal area , as a result of increasing nutrient input, does not necessarily lead to an increase of pelagie or demersal fish production, but cou Id induce a modification of the food web , in particular the enhancement of microbiological activity at the expense of long trophic chains dominated by macroorganisms. The near absence of nematode-predators in the reg ion off the Belgian east coast, the dom inance of bacterivores, the very low spec ies diversity of the nematode community and the paucity of higher metazoans within the area, can be partly explained on the basis of the increase in nutrient input within the area, and partly on the basis of the high amount of \"mixed\" pollution. Résumé: Identification des assemblages de nématodes de 102 stations de la partie sud de la mer du Nord où des prélèvements ont été effectués de 1972 il 1984 : 456 espèces ont été répertoriées, appartenant il 159 gen res et 37 familles. Interprétation des communautés par l'analyse des groupements d'espèces (coelficient de dissimilarité de Bray-Curtis et classification polythétique Twinspan) et par l'analyse factorielle des correspondances (DCA). Global ement, le bassin du sud de la mer du Nord peut être di visé en six zones principales définies par la composition spécifiq ue des nématodes. La structure sédimentaire apparaît comme le facte ur du milieu déterminant de la composition spécifique de la nématocoenose ; cependant, d'autres facteurs (température, salinité, ch lorophylle a, N03-, NH4+) semblent égaiement influer sur la distribution des espèces. L'importance du rôle des bactéries représente l'un des caractères les plus remarq uables des écosystèmes côtiers et, en particulier, de celui de la côte belge. Dans cette région, un accroissement du taux de production primaire, lié il une intensification de l'apport de nutriments, n'entraîne pas nécessairement l'augmentation de la production en poissons pélagiques ou démersaux ; mais il pourrait provoquer des modifications des réseaux trophiques, notamment la stimulation de l'activité microbiologique aux dépens des chaînes trophiques longues dominées par les macro-organismes. Au large de la côte est de Belgique, la dominance des nématodes bactérivores, la quasi-absence des prédateurs, la très faible diversité spécifique des communautés de ce groupe et la pauvreté des métazoaires supérieurs peuvent trouver leur expl ication d'une part dans l'augmentation de l'apport en nutriments et d'autre part dans la grande quantité de po llution diffuse.","publication_date":{"day":null,"month":null,"year":1990,"errors":{}},"publication_name":"Netherlands Journal of Sea Research","grobid_abstract_attachment_id":97942103},"translated_abstract":null,"internal_url":"https://www.academia.edu/95887000/Diversity_of_the_nematode_communities_in_the_Southern_Bight_of_the_North_Sea","translated_internal_url":"","created_at":"2023-01-29T00:36:08.199-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":184662190,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":97942103,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942103/thumbnails/1.jpg","file_name":"286799.pdf","download_url":"https://www.academia.edu/attachments/97942103/download_file","bulk_download_file_name":"Diversity_of_the_nematode_communities_in.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942103/286799-libre.pdf?1674982304=\u0026response-content-disposition=attachment%3B+filename%3DDiversity_of_the_nematode_communities_in.pdf\u0026Expires=1743224695\u0026Signature=Jgb~CvNX2f~lurU4KFw-OlbU2CgZRO28CvMazP2huahtDlnWCSqy~3zcu5H6I8eGtM-Dlr6JNjz4Rg-PvDVRupzpsiyrXgID-SW3BCy~MGlwZlMnTZseLwTedJyyBowZIb2llpA3XTUB0ZYt9WtHX0eJui2qMP1bDYkbaTvtqRX1rKQWeIVP5fUJO8T~kOnIM0HY1Na2xOxscjr~--K8tsbt9cxP~soyOxC2Zqa1P86puGCBngjZqJoo9Pd7-LH-FQS~VAnKmeGZ4fTs2r47db8gEVYvYc37xu~oWYRjlUjJghG-wQ~xqGql8njkyHufpIaKkD6RrLLFTbWPKn5klg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Diversity_of_the_nematode_communities_in_the_Southern_Bight_of_the_North_Sea","translated_slug":"","page_count":23,"language":"en","content_type":"Work","summary":"The nematode communities from 102 stations in the Southern Bight of the North Sea, sumpled between 1972 and 1984, are exam ined. 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A general increase of the level of primary production in the coastal area , as a result of increasing nutrient input, does not necessarily lead to an increase of pelagie or demersal fish production, but cou Id induce a modification of the food web , in particular the enhancement of microbiological activity at the expense of long trophic chains dominated by macroorganisms. The near absence of nematode-predators in the reg ion off the Belgian east coast, the dom inance of bacterivores, the very low spec ies diversity of the nematode community and the paucity of higher metazoans within the area, can be partly explained on the basis of the increase in nutrient input within the area, and partly on the basis of the high amount of \"mixed\" pollution. Résumé: Identification des assemblages de nématodes de 102 stations de la partie sud de la mer du Nord où des prélèvements ont été effectués de 1972 il 1984 : 456 espèces ont été répertoriées, appartenant il 159 gen res et 37 familles. Interprétation des communautés par l'analyse des groupements d'espèces (coelficient de dissimilarité de Bray-Curtis et classification polythétique Twinspan) et par l'analyse factorielle des correspondances (DCA). Global ement, le bassin du sud de la mer du Nord peut être di visé en six zones principales définies par la composition spécifiq ue des nématodes. La structure sédimentaire apparaît comme le facte ur du milieu déterminant de la composition spécifique de la nématocoenose ; cependant, d'autres facteurs (température, salinité, ch lorophylle a, N03-, NH4+) semblent égaiement influer sur la distribution des espèces. L'importance du rôle des bactéries représente l'un des caractères les plus remarq uables des écosystèmes côtiers et, en particulier, de celui de la côte belge. Dans cette région, un accroissement du taux de production primaire, lié il une intensification de l'apport de nutriments, n'entraîne pas nécessairement l'augmentation de la production en poissons pélagiques ou démersaux ; mais il pourrait provoquer des modifications des réseaux trophiques, notamment la stimulation de l'activité microbiologique aux dépens des chaînes trophiques longues dominées par les macro-organismes. 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The water quality of a river is the result of complex anthropogenic systems (buildings, waste water treatment infrastructure, regulations, etc.) and biogeochemical and eco-hydrological interactions. It is therefore essential to obtain more insight in the factors that determine the water quality in a river. Research into the relation between land use and water quality is necessary. Human activities have a huge impact on the flow regimes and associated water quality of river systems. Effects of land use bound activities on water quality are often investigated, but these studies generally ignore the hydrological complexity of a human influenced catchment. Infrastructure like sewer systems and wastewater treatment plants (WWTP) can displace huge quantities of polluted water. The transfers change flow paths, displace water...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="27297acdadd9a1260d1ea03e85df413f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942101,&quot;asset_id&quot;:95886999,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942101/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95886999"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95886999"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95886999; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95886999]").text(description); $(".js-view-count[data-work-id=95886999]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95886999; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95886999']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "27297acdadd9a1260d1ea03e85df413f" } } $('.js-work-strip[data-work-id=95886999]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95886999,"title":"The effects of sewer infrastructure on water quality: implications for land use studies","translated_title":"","metadata":{"abstract":"The European Water Framework Directive requires a good ecological status of the European water bodies and the necessary measures to obtain this have to be implemented. The water quality of a river is the result of complex anthropogenic systems (buildings, waste water treatment infrastructure, regulations, etc.) and biogeochemical and eco-hydrological interactions. It is therefore essential to obtain more insight in the factors that determine the water quality in a river. Research into the relation between land use and water quality is necessary. Human activities have a huge impact on the flow regimes and associated water quality of river systems. Effects of land use bound activities on water quality are often investigated, but these studies generally ignore the hydrological complexity of a human influenced catchment. Infrastructure like sewer systems and wastewater treatment plants (WWTP) can displace huge quantities of polluted water. The transfers change flow paths, displace water...","publication_date":{"day":null,"month":null,"year":2010,"errors":{}}},"translated_abstract":"The European Water Framework Directive requires a good ecological status of the European water bodies and the necessary measures to obtain this have to be implemented. The water quality of a river is the result of complex anthropogenic systems (buildings, waste water treatment infrastructure, regulations, etc.) and biogeochemical and eco-hydrological interactions. It is therefore essential to obtain more insight in the factors that determine the water quality in a river. Research into the relation between land use and water quality is necessary. Human activities have a huge impact on the flow regimes and associated water quality of river systems. Effects of land use bound activities on water quality are often investigated, but these studies generally ignore the hydrological complexity of a human influenced catchment. Infrastructure like sewer systems and wastewater treatment plants (WWTP) can displace huge quantities of polluted water. 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Kris Van Looy a , Corresponding Author Contact Information , E-mail The Corresponding Author ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">... Kris Van Looy a , Corresponding Author Contact Information , E-mail The Corresponding Author , E-mail The Corresponding Author and Patrick ... their distribution patterns, more has to be known about their population biology and dynamics (Burkart, 2001; Lowe, 2002; Malanson ...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95886998"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95886998"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95886998; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95886998]").text(description); $(".js-view-count[data-work-id=95886998]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95886998; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95886998']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=95886998]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95886998,"title":"A conservation paradox for riparian habitats and river corridor species","translated_title":"","metadata":{"abstract":"... Kris Van Looy a , Corresponding Author Contact Information , E-mail The Corresponding Author , E-mail The Corresponding Author and Patrick ... their distribution patterns, more has to be known about their population biology and dynamics (Burkart, 2001; Lowe, 2002; Malanson ...","publisher":"Elsevier BV","publication_date":{"day":null,"month":null,"year":2009,"errors":{}},"publication_name":"Journal for Nature Conservation"},"translated_abstract":"... 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Kris Van Looy a , Corresponding Author Contact Information , E-mail The Corresponding Author , E-mail The Corresponding Author and Patrick ... their distribution patterns, more has to be known about their population biology and dynamics (Burkart, 2001; Lowe, 2002; Malanson ...","owner":{"id":184662190,"first_name":"Patrick","middle_initials":null,"last_name":"Meire","page_name":"MeireP","domain_name":"independent","created_at":"2021-02-03T07:39:55.559-08:00","display_name":"Patrick Meire","url":"https://independent.academia.edu/MeireP"},"attachments":[],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"},{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":7710,"name":"Biology","url":"https://www.academia.edu/Documents/in/Biology"},{"id":9846,"name":"Ecology","url":"https://www.academia.edu/Documents/in/Ecology"},{"id":28235,"name":"Multidisciplinary","url":"https://www.academia.edu/Documents/in/Multidisciplinary"},{"id":85707,"name":"Habitat","url":"https://www.academia.edu/Documents/in/Habitat"},{"id":86882,"name":"Rare species","url":"https://www.academia.edu/Documents/in/Rare_species"},{"id":124470,"name":"Bank","url":"https://www.academia.edu/Documents/in/Bank"},{"id":152553,"name":"Comparative Analysis","url":"https://www.academia.edu/Documents/in/Comparative_Analysis"},{"id":163827,"name":"Floodplain","url":"https://www.academia.edu/Documents/in/Floodplain"},{"id":174975,"name":"Habitat fragmentation","url":"https://www.academia.edu/Documents/in/Habitat_fragmentation"},{"id":586072,"name":"Plant species","url":"https://www.academia.edu/Documents/in/Plant_species"},{"id":1002371,"name":"Riparian Habitat","url":"https://www.academia.edu/Documents/in/Riparian_Habitat"},{"id":1565270,"name":"Art for Nature and Wildlife Conservation","url":"https://www.academia.edu/Documents/in/Art_for_Nature_and_Wildlife_Conservation"}],"urls":[{"id":28485829,"url":"https://api.elsevier.com/content/article/PII:S1617138108000605?httpAccept=text/xml"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95886998-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95886997"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/95886997/Variability_in_stock_assessment_of_cockles_Cerastoderma_edule_L_in_the_Oosterschelde_in_1980_1990_in_relation_to_environmental_factors"><img alt="Research paper thumbnail of Variability in stock assessment of cockles (Cerastoderma edule L.) in the Oosterschelde (in 1980–1990), in relation to environmental factors" class="work-thumbnail" src="https://attachments.academia-assets.com/97942100/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95886997/Variability_in_stock_assessment_of_cockles_Cerastoderma_edule_L_in_the_Oosterschelde_in_1980_1990_in_relation_to_environmental_factors">Variability in stock assessment of cockles (Cerastoderma edule L.) in the Oosterschelde (in 1980–1990), in relation to environmental factors</a></div><div class="wp-workCard_item"><span>Hydrobiologia</span><span>, 1994</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The edible cockle (Cerastoderma edule L.) is a dominant suspension feeder in the Oosterschelde, a...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The edible cockle (Cerastoderma edule L.) is a dominant suspension feeder in the Oosterschelde, a 351 km 2 tidal bay in the SW Netherlands. To establish its role in the benthic foodweb, and to assess the impact of human activities, data on density, age composition, biomass and growth were collected from several tidal flats in the Oosterschelde between 1980 and 1990. To estimate the overall biomass development of the cockle, a simple model was used, in which three growing seasons are defined for the cockle population. A standard individual growth curve was constructed. A negative exponential mortality function was assumed to estimate the number of recruits. By combining the estimated number of recruits, the estimated specific mortality rate and the standard individual growth curve, numbers and biomass of each age group in the Oosterschelde population were estimated. Average biomass (including shell organics) per m 2 of tidal flat in August varied from 140 g AFDW in 1980 to 21 g AFDW in 1989, implying a total cockle stock on all tidal flats of 19170 to 2350 tonnes AFDW (72 x 10 3 to 9 X 10 3 tonnes flesh), respectively. A comparison of results from field surveys and the reconstructed stock estimations showed large deviations. However, an uncertainty analysis performed on the model showed that most field data fitted within the minimum and maximum biomass calculated. Total biomass is largely dependent on the strength of certain year classes. In this respect, the year classes 1979, 1982, and 1985 were good. Effects of the construction of the storm-surge barrier and the compartmentalisation dams could not be demonstrated. The year-to-year variation in cockle stocks, assessed in the way described in this paper should be regarded as relative, because a systematic survey of the intertidal flats was not performed every year, but population dynamics from selected stations were used instead.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="9a770ccdab6f79ff307a29c449d78b84" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942100,&quot;asset_id&quot;:95886997,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942100/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95886997"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95886997"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95886997; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95886997]").text(description); $(".js-view-count[data-work-id=95886997]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95886997; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95886997']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "9a770ccdab6f79ff307a29c449d78b84" } } $('.js-work-strip[data-work-id=95886997]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95886997,"title":"Variability in stock assessment of cockles (Cerastoderma edule L.) in the Oosterschelde (in 1980–1990), in relation to environmental factors","translated_title":"","metadata":{"publisher":"Springer Nature","grobid_abstract":"The edible cockle (Cerastoderma edule L.) is a dominant suspension feeder in the Oosterschelde, a 351 km 2 tidal bay in the SW Netherlands. 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A comparison of results from field surveys and the reconstructed stock estimations showed large deviations. However, an uncertainty analysis performed on the model showed that most field data fitted within the minimum and maximum biomass calculated. Total biomass is largely dependent on the strength of certain year classes. In this respect, the year classes 1979, 1982, and 1985 were good. Effects of the construction of the storm-surge barrier and the compartmentalisation dams could not be demonstrated. The year-to-year variation in cockle stocks, assessed in the way described in this paper should be regarded as relative, because a systematic survey of the intertidal flats was not performed every year, but population dynamics from selected stations were used instead.","publication_date":{"day":null,"month":null,"year":1994,"errors":{}},"publication_name":"Hydrobiologia","grobid_abstract_attachment_id":97942100},"translated_abstract":null,"internal_url":"https://www.academia.edu/95886997/Variability_in_stock_assessment_of_cockles_Cerastoderma_edule_L_in_the_Oosterschelde_in_1980_1990_in_relation_to_environmental_factors","translated_internal_url":"","created_at":"2023-01-29T00:36:07.780-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":184662190,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":97942100,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942100/thumbnails/1.jpg","file_name":"978-94-011-1174-4_28.pdf","download_url":"https://www.academia.edu/attachments/97942100/download_file","bulk_download_file_name":"Variability_in_stock_assessment_of_cockl.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942100/978-94-011-1174-4_28-libre.pdf?1674982284=\u0026response-content-disposition=attachment%3B+filename%3DVariability_in_stock_assessment_of_cockl.pdf\u0026Expires=1743224695\u0026Signature=dxJJ74~I1rRw2Y6gqZPKlRW3mDGhCRVFx6yNLCzamRQssuj6bdbPd~kCbYG8mxmdPsvGkvn1uti~~EnssmDnyFO~UTEMtt2gXzzzwfOgddCAutgfN7xyQRaii2rhbQt-41iswsfGi2Vsq1y7aRE-eWdQQLuLCHHoCbWHPLGR7pJ~QF4-NnUgEoiTbbUdF3CXAOzRcWq938fE8hTgPwW9d64Mxg0cEA5fQvOfCvn1fwMkkQLxV9AeCuWVCGW60ldoEK7ZdMc~Zw5adXTQl4wdRwl5qMBZa2B3D7fffXIgBqr3hwhoW4HXZkLtXW6RW8Rl8meTTO6NIyfdtBvSB1UiKw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Variability_in_stock_assessment_of_cockles_Cerastoderma_edule_L_in_the_Oosterschelde_in_1980_1990_in_relation_to_environmental_factors","translated_slug":"","page_count":15,"language":"en","content_type":"Work","summary":"The edible cockle (Cerastoderma edule L.) is a dominant suspension feeder in the Oosterschelde, a 351 km 2 tidal bay in the SW Netherlands. To establish its role in the benthic foodweb, and to assess the impact of human activities, data on density, age composition, biomass and growth were collected from several tidal flats in the Oosterschelde between 1980 and 1990. To estimate the overall biomass development of the cockle, a simple model was used, in which three growing seasons are defined for the cockle population. A standard individual growth curve was constructed. A negative exponential mortality function was assumed to estimate the number of recruits. By combining the estimated number of recruits, the estimated specific mortality rate and the standard individual growth curve, numbers and biomass of each age group in the Oosterschelde population were estimated. Average biomass (including shell organics) per m 2 of tidal flat in August varied from 140 g AFDW in 1980 to 21 g AFDW in 1989, implying a total cockle stock on all tidal flats of 19170 to 2350 tonnes AFDW (72 x 10 3 to 9 X 10 3 tonnes flesh), respectively. A comparison of results from field surveys and the reconstructed stock estimations showed large deviations. However, an uncertainty analysis performed on the model showed that most field data fitted within the minimum and maximum biomass calculated. Total biomass is largely dependent on the strength of certain year classes. In this respect, the year classes 1979, 1982, and 1985 were good. Effects of the construction of the storm-surge barrier and the compartmentalisation dams could not be demonstrated. The year-to-year variation in cockle stocks, assessed in the way described in this paper should be regarded as relative, because a systematic survey of the intertidal flats was not performed every year, but population dynamics from selected stations were used instead.","owner":{"id":184662190,"first_name":"Patrick","middle_initials":null,"last_name":"Meire","page_name":"MeireP","domain_name":"independent","created_at":"2021-02-03T07:39:55.559-08:00","display_name":"Patrick Meire","url":"https://independent.academia.edu/MeireP"},"attachments":[{"id":97942100,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942100/thumbnails/1.jpg","file_name":"978-94-011-1174-4_28.pdf","download_url":"https://www.academia.edu/attachments/97942100/download_file","bulk_download_file_name":"Variability_in_stock_assessment_of_cockl.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942100/978-94-011-1174-4_28-libre.pdf?1674982284=\u0026response-content-disposition=attachment%3B+filename%3DVariability_in_stock_assessment_of_cockl.pdf\u0026Expires=1743224695\u0026Signature=dxJJ74~I1rRw2Y6gqZPKlRW3mDGhCRVFx6yNLCzamRQssuj6bdbPd~kCbYG8mxmdPsvGkvn1uti~~EnssmDnyFO~UTEMtt2gXzzzwfOgddCAutgfN7xyQRaii2rhbQt-41iswsfGi2Vsq1y7aRE-eWdQQLuLCHHoCbWHPLGR7pJ~QF4-NnUgEoiTbbUdF3CXAOzRcWq938fE8hTgPwW9d64Mxg0cEA5fQvOfCvn1fwMkkQLxV9AeCuWVCGW60ldoEK7ZdMc~Zw5adXTQl4wdRwl5qMBZa2B3D7fffXIgBqr3hwhoW4HXZkLtXW6RW8Rl8meTTO6NIyfdtBvSB1UiKw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":7710,"name":"Biology","url":"https://www.academia.edu/Documents/in/Biology"},{"id":9846,"name":"Ecology","url":"https://www.academia.edu/Documents/in/Ecology"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences"},{"id":100077,"name":"Stock assessment","url":"https://www.academia.edu/Documents/in/Stock_assessment"},{"id":213948,"name":"General Science","url":"https://www.academia.edu/Documents/in/General_Science"},{"id":509556,"name":"Human Activity","url":"https://www.academia.edu/Documents/in/Human_Activity"},{"id":580672,"name":"Tidal Flat","url":"https://www.academia.edu/Documents/in/Tidal_Flat"},{"id":1443257,"name":"Cockle","url":"https://www.academia.edu/Documents/in/Cockle"},{"id":1582364,"name":"Growth Curve","url":"https://www.academia.edu/Documents/in/Growth_Curve"},{"id":1660649,"name":"Bay","url":"https://www.academia.edu/Documents/in/Bay"},{"id":3807870,"name":"Environmental factor","url":"https://www.academia.edu/Documents/in/Environmental_factor"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95886997-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95886996"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/95886996/Effect_of_sedimentological_and_hydrodynamical_changes_in_the_intertidal_areas_of_the_Oosterschelde_estuary_SW_Netherlands_on_distribution_density_and_biomass_of_five_common_macrobenthic_species_Spio_martinensis_Mesnil_Hydrobia_ulvae_Pennant_Arenicola_marina_L_Scoloplos_armiger_Mull_"><img alt="Research paper thumbnail of Effect of sedimentological and hydrodynamical changes in the intertidal areas of the Oosterschelde estuary (SW Netherlands) on distribution, density and biomass of five common macrobenthic species: Spio martinensis (Mesnil), Hydrobia ulvae (Pennant), Arenicola marina (L.), Scoloplos armiger (Mull..." class="work-thumbnail" src="https://attachments.academia-assets.com/97942102/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95886996/Effect_of_sedimentological_and_hydrodynamical_changes_in_the_intertidal_areas_of_the_Oosterschelde_estuary_SW_Netherlands_on_distribution_density_and_biomass_of_five_common_macrobenthic_species_Spio_martinensis_Mesnil_Hydrobia_ulvae_Pennant_Arenicola_marina_L_Scoloplos_armiger_Mull_">Effect of sedimentological and hydrodynamical changes in the intertidal areas of the Oosterschelde estuary (SW Netherlands) on distribution, density and biomass of five common macrobenthic species: Spio martinensis (Mesnil), Hydrobia ulvae (Pennant), Arenicola marina (L.), Scoloplos armiger (Mull...</a></div><div class="wp-workCard_item"><span>Hydrobiologia</span><span>, 1994</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In order to evaluate the impact of the construction of the storm-surge barrier and secondary dams...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">In order to evaluate the impact of the construction of the storm-surge barrier and secondary dams on macrobenthos of the tidal flats in the Oosterschelde (SW Netherlands), changes in distribution, density and biomass of five common species (Spin martinensis, Hydrobia ulvae, Arenicola marina, Scoloplos armiger and Bathyporeia sp) were analysed. Data on macrobenthos were collected from 1979 to 1989 on five different tidal flats. Changes in sediment texture and hydrodynamic factors during the construction and after the completion of the coastal engineering project were taken into account. Three severe winters in a row caused more disturbance in the population of the main predator of S. armiger than did the hydrodynamical changes. A temporary prolongation of the emersion time (in 1986 and 1987) caused a temporary decrease in juvenile A. marina. But afterwards they still occupy the samè nursery grounds&#39;. Increased wave action on the edges of the flats probably created new niches for Bathyporeia sp. and Spio martinensis, replacing other benthic species. It is not yet clear what has caused the decline of H. ulvae in many places in the Oosterschelde estuary. Parasitic infestation is one of the possibilities .</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c73884cda43af178be4f6316fd1aaca2" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942102,&quot;asset_id&quot;:95886996,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942102/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95886996"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95886996"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95886996; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95886996]").text(description); $(".js-view-count[data-work-id=95886996]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95886996; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95886996']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "c73884cda43af178be4f6316fd1aaca2" } } $('.js-work-strip[data-work-id=95886996]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95886996,"title":"Effect of sedimentological and hydrodynamical changes in the intertidal areas of the Oosterschelde estuary (SW Netherlands) on distribution, density and biomass of five common macrobenthic species: Spio martinensis (Mesnil), Hydrobia ulvae (Pennant), Arenicola marina (L.), Scoloplos armiger (Mull...","translated_title":"","metadata":{"publisher":"Springer Science and Business Media LLC","grobid_abstract":"In order to evaluate the impact of the construction of the storm-surge barrier and secondary dams on macrobenthos of the tidal flats in the Oosterschelde (SW Netherlands), changes in distribution, density and biomass of five common species (Spin martinensis, Hydrobia ulvae, Arenicola marina, Scoloplos armiger and Bathyporeia sp) were analysed. Data on macrobenthos were collected from 1979 to 1989 on five different tidal flats. Changes in sediment texture and hydrodynamic factors during the construction and after the completion of the coastal engineering project were taken into account. Three severe winters in a row caused more disturbance in the population of the main predator of S. armiger than did the hydrodynamical changes. A temporary prolongation of the emersion time (in 1986 and 1987) caused a temporary decrease in juvenile A. marina. But afterwards they still occupy the samè nursery grounds'. Increased wave action on the edges of the flats probably created new niches for Bathyporeia sp. and Spio martinensis, replacing other benthic species. It is not yet clear what has caused the decline of H. ulvae in many places in the Oosterschelde estuary. Parasitic infestation is one of the possibilities .","publication_date":{"day":null,"month":null,"year":1994,"errors":{}},"publication_name":"Hydrobiologia","grobid_abstract_attachment_id":97942102},"translated_abstract":null,"internal_url":"https://www.academia.edu/95886996/Effect_of_sedimentological_and_hydrodynamical_changes_in_the_intertidal_areas_of_the_Oosterschelde_estuary_SW_Netherlands_on_distribution_density_and_biomass_of_five_common_macrobenthic_species_Spio_martinensis_Mesnil_Hydrobia_ulvae_Pennant_Arenicola_marina_L_Scoloplos_armiger_Mull_","translated_internal_url":"","created_at":"2023-01-29T00:36:07.638-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":184662190,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":97942102,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942102/thumbnails/1.jpg","file_name":"250441.pdf","download_url":"https://www.academia.edu/attachments/97942102/download_file","bulk_download_file_name":"Effect_of_sedimentological_and_hydrodyna.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942102/250441-libre.pdf?1674982259=\u0026response-content-disposition=attachment%3B+filename%3DEffect_of_sedimentological_and_hydrodyna.pdf\u0026Expires=1743224695\u0026Signature=Qlh44chTRUyHq6BDsTaL-DXDskTLgENoRs8dq0O375FqythoWYI79Grdm4G3uTVfLd1gMqZN0hxYH6VlAzkmdbGj7ETs5K2aTXcPr~MgOlHFZuEWJxCg3jgIFYZ0NysgjmgFYvpK~8ZBfsDK5b8jpK8aADePzuI9hSoUPD7N2cK65enWDONHCeDYfOxT1c~K64JcFnr7aI9FYjg~zklKXVsS6lOP70jgip1jcPS8hngeJBLSI20LhN8jcB3dNOcmC0BVYa1NtkonjuNum90jAXPO4reXovHUKD1KzYfQFbAlek7ZZyzW626YDs0F2-OYoKvenbHdXwtRK7eamk5Hcw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Effect_of_sedimentological_and_hydrodynamical_changes_in_the_intertidal_areas_of_the_Oosterschelde_estuary_SW_Netherlands_on_distribution_density_and_biomass_of_five_common_macrobenthic_species_Spio_martinensis_Mesnil_Hydrobia_ulvae_Pennant_Arenicola_marina_L_Scoloplos_armiger_Mull_","translated_slug":"","page_count":15,"language":"en","content_type":"Work","summary":"In order to evaluate the impact of the construction of the storm-surge barrier and secondary dams on macrobenthos of the tidal flats in the Oosterschelde (SW Netherlands), changes in distribution, density and biomass of five common species (Spin martinensis, Hydrobia ulvae, Arenicola marina, Scoloplos armiger and Bathyporeia sp) were analysed. Data on macrobenthos were collected from 1979 to 1989 on five different tidal flats. Changes in sediment texture and hydrodynamic factors during the construction and after the completion of the coastal engineering project were taken into account. Three severe winters in a row caused more disturbance in the population of the main predator of S. armiger than did the hydrodynamical changes. A temporary prolongation of the emersion time (in 1986 and 1987) caused a temporary decrease in juvenile A. marina. But afterwards they still occupy the samè nursery grounds'. Increased wave action on the edges of the flats probably created new niches for Bathyporeia sp. and Spio martinensis, replacing other benthic species. It is not yet clear what has caused the decline of H. ulvae in many places in the Oosterschelde estuary. Parasitic infestation is one of the possibilities .","owner":{"id":184662190,"first_name":"Patrick","middle_initials":null,"last_name":"Meire","page_name":"MeireP","domain_name":"independent","created_at":"2021-02-03T07:39:55.559-08:00","display_name":"Patrick Meire","url":"https://independent.academia.edu/MeireP"},"attachments":[{"id":97942102,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942102/thumbnails/1.jpg","file_name":"250441.pdf","download_url":"https://www.academia.edu/attachments/97942102/download_file","bulk_download_file_name":"Effect_of_sedimentological_and_hydrodyna.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942102/250441-libre.pdf?1674982259=\u0026response-content-disposition=attachment%3B+filename%3DEffect_of_sedimentological_and_hydrodyna.pdf\u0026Expires=1743224695\u0026Signature=Qlh44chTRUyHq6BDsTaL-DXDskTLgENoRs8dq0O375FqythoWYI79Grdm4G3uTVfLd1gMqZN0hxYH6VlAzkmdbGj7ETs5K2aTXcPr~MgOlHFZuEWJxCg3jgIFYZ0NysgjmgFYvpK~8ZBfsDK5b8jpK8aADePzuI9hSoUPD7N2cK65enWDONHCeDYfOxT1c~K64JcFnr7aI9FYjg~zklKXVsS6lOP70jgip1jcPS8hngeJBLSI20LhN8jcB3dNOcmC0BVYa1NtkonjuNum90jAXPO4reXovHUKD1KzYfQFbAlek7ZZyzW626YDs0F2-OYoKvenbHdXwtRK7eamk5Hcw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":9846,"name":"Ecology","url":"https://www.academia.edu/Documents/in/Ecology"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences"},{"id":162645,"name":"Population Density","url":"https://www.academia.edu/Documents/in/Population_Density"},{"id":379570,"name":"Estuary","url":"https://www.academia.edu/Documents/in/Estuary"},{"id":398869,"name":"Intertidal Zone","url":"https://www.academia.edu/Documents/in/Intertidal_Zone"},{"id":556983,"name":"Storm surge","url":"https://www.academia.edu/Documents/in/Storm_surge"},{"id":580672,"name":"Tidal Flat","url":"https://www.academia.edu/Documents/in/Tidal_Flat"},{"id":581940,"name":"Macrobenthos","url":"https://www.academia.edu/Documents/in/Macrobenthos"},{"id":1237825,"name":"Population dynamic","url":"https://www.academia.edu/Documents/in/Population_dynamic"},{"id":1443257,"name":"Cockle","url":"https://www.academia.edu/Documents/in/Cockle"}],"urls":[{"id":28485828,"url":"http://link.springer.com/content/pdf/10.1007/BF00024633.pdf"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95886996-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95886995"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/95886995/Tracing_Si_N_P_ecosystem_pathways_is_relative_uptake_in_riparian_vegetation_influenced_by_soil_waterlogging_mowing_management_and_species_diversity"><img alt="Research paper thumbnail of Tracing Si–N–P ecosystem-pathways: is relative uptake in riparian vegetation influenced by soil waterlogging, mowing management and species diversity?" class="work-thumbnail" src="https://attachments.academia-assets.com/97942105/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95886995/Tracing_Si_N_P_ecosystem_pathways_is_relative_uptake_in_riparian_vegetation_influenced_by_soil_waterlogging_mowing_management_and_species_diversity">Tracing Si–N–P ecosystem-pathways: is relative uptake in riparian vegetation influenced by soil waterlogging, mowing management and species diversity?</a></div><div class="wp-workCard_item"><span>Hydrobiologia</span><span>, 2011</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Despite the growing concern about the importance of silicon (Si) in controlling ecological proces...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Despite the growing concern about the importance of silicon (Si) in controlling ecological processes in aquatic ecosystems, little is known about its processing in riparian vegetation, especially compared to nitrogen (N) and phosphorus (P). We present experimental evidence that relative plant uptake of N and P compared to Si in riparian vegetation is dependent on mowing practices, water-logging and species composition. Results are obtained from a controlled and replicated mesocosm experiment, with a full-factorial design of soil water logging and mowing management. In our experiments, the Si excluding species Plantago lanceolata was dominant in the mown and non-waterlogged treatments, while Si accumulating meadow grasses and Phalaris arundinacea dominated the waterlogged treatments. Although species composition, management and soil moisture interacted strongly in their effect on relative Si:N and Si:P uptake ratios, the uptake of N to P remained virtually unchanged over the different treatments. Our study sheds new light on the impact of riparian wetland ecosystems on nutrient transport to rivers. It indicates that it is essential to include Si in future studies of the impact of riparian vegetation on nutrient transport, as these are often implemented as a measure to moderate excessive N and P inputs.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="73e5ce0fd115dee024a90293657320f8" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942105,&quot;asset_id&quot;:95886995,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942105/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95886995"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95886995"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95886995; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95886995]").text(description); $(".js-view-count[data-work-id=95886995]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95886995; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95886995']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "73e5ce0fd115dee024a90293657320f8" } } $('.js-work-strip[data-work-id=95886995]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95886995,"title":"Tracing Si–N–P ecosystem-pathways: is relative uptake in riparian vegetation influenced by soil waterlogging, mowing management and species diversity?","translated_title":"","metadata":{"publisher":"Springer Nature","grobid_abstract":"Despite the growing concern about the importance of silicon (Si) in controlling ecological processes in aquatic ecosystems, little is known about its processing in riparian vegetation, especially compared to nitrogen (N) and phosphorus (P). We present experimental evidence that relative plant uptake of N and P compared to Si in riparian vegetation is dependent on mowing practices, water-logging and species composition. Results are obtained from a controlled and replicated mesocosm experiment, with a full-factorial design of soil water logging and mowing management. In our experiments, the Si excluding species Plantago lanceolata was dominant in the mown and non-waterlogged treatments, while Si accumulating meadow grasses and Phalaris arundinacea dominated the waterlogged treatments. Although species composition, management and soil moisture interacted strongly in their effect on relative Si:N and Si:P uptake ratios, the uptake of N to P remained virtually unchanged over the different treatments. Our study sheds new light on the impact of riparian wetland ecosystems on nutrient transport to rivers. It indicates that it is essential to include Si in future studies of the impact of riparian vegetation on nutrient transport, as these are often implemented as a measure to moderate excessive N and P inputs.","publication_date":{"day":null,"month":null,"year":2011,"errors":{}},"publication_name":"Hydrobiologia","grobid_abstract_attachment_id":97942105},"translated_abstract":null,"internal_url":"https://www.academia.edu/95886995/Tracing_Si_N_P_ecosystem_pathways_is_relative_uptake_in_riparian_vegetation_influenced_by_soil_waterlogging_mowing_management_and_species_diversity","translated_internal_url":"","created_at":"2023-01-29T00:36:07.536-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":184662190,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":97942105,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942105/thumbnails/1.jpg","file_name":"d953772c.pdf","download_url":"https://www.academia.edu/attachments/97942105/download_file","bulk_download_file_name":"Tracing_Si_N_P_ecosystem_pathways_is_rel.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942105/d953772c-libre.pdf?1674982256=\u0026response-content-disposition=attachment%3B+filename%3DTracing_Si_N_P_ecosystem_pathways_is_rel.pdf\u0026Expires=1743224695\u0026Signature=XjPoj7UaCKEA-4GHaZe~LqytV74wIGzx5N5E~kUnM9zh7WC36LKkfzcQl77DQN0xgmlzvZ1RT70e-TQU4nHxmLOsBhx3xhQ72UzlwAPejtiMbH0Z4Pn~e1sW-Kqr5z37HfIj5VxSQlpflkbZyt30eeAEpnnhsTpgU5NELqOBU3AJ~11ZWWvOPGH3r4XagPewLd-xsJC61Klnsf8g4MY-EqPftia558tzEULyB1Do2FBiiKAfhWaTpqVY~B-0ffzrHYQyJFxKNC-fxdpPIW7jrm38GpOMwcG~0ZRAgZJohy85gApq3SCMbu70~LvFy8voKSo-QaxT0K-9BufvjdfYFg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Tracing_Si_N_P_ecosystem_pathways_is_relative_uptake_in_riparian_vegetation_influenced_by_soil_waterlogging_mowing_management_and_species_diversity","translated_slug":"","page_count":10,"language":"en","content_type":"Work","summary":"Despite the growing concern about the importance of silicon (Si) in controlling ecological processes in aquatic ecosystems, little is known about its processing in riparian vegetation, especially compared to nitrogen (N) and phosphorus (P). We present experimental evidence that relative plant uptake of N and P compared to Si in riparian vegetation is dependent on mowing practices, water-logging and species composition. Results are obtained from a controlled and replicated mesocosm experiment, with a full-factorial design of soil water logging and mowing management. In our experiments, the Si excluding species Plantago lanceolata was dominant in the mown and non-waterlogged treatments, while Si accumulating meadow grasses and Phalaris arundinacea dominated the waterlogged treatments. Although species composition, management and soil moisture interacted strongly in their effect on relative Si:N and Si:P uptake ratios, the uptake of N to P remained virtually unchanged over the different treatments. Our study sheds new light on the impact of riparian wetland ecosystems on nutrient transport to rivers. It indicates that it is essential to include Si in future studies of the impact of riparian vegetation on nutrient transport, as these are often implemented as a measure to moderate excessive N and P inputs.","owner":{"id":184662190,"first_name":"Patrick","middle_initials":null,"last_name":"Meire","page_name":"MeireP","domain_name":"independent","created_at":"2021-02-03T07:39:55.559-08:00","display_name":"Patrick Meire","url":"https://independent.academia.edu/MeireP"},"attachments":[{"id":97942105,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942105/thumbnails/1.jpg","file_name":"d953772c.pdf","download_url":"https://www.academia.edu/attachments/97942105/download_file","bulk_download_file_name":"Tracing_Si_N_P_ecosystem_pathways_is_rel.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942105/d953772c-libre.pdf?1674982256=\u0026response-content-disposition=attachment%3B+filename%3DTracing_Si_N_P_ecosystem_pathways_is_rel.pdf\u0026Expires=1743224695\u0026Signature=XjPoj7UaCKEA-4GHaZe~LqytV74wIGzx5N5E~kUnM9zh7WC36LKkfzcQl77DQN0xgmlzvZ1RT70e-TQU4nHxmLOsBhx3xhQ72UzlwAPejtiMbH0Z4Pn~e1sW-Kqr5z37HfIj5VxSQlpflkbZyt30eeAEpnnhsTpgU5NELqOBU3AJ~11ZWWvOPGH3r4XagPewLd-xsJC61Klnsf8g4MY-EqPftia558tzEULyB1Do2FBiiKAfhWaTpqVY~B-0ffzrHYQyJFxKNC-fxdpPIW7jrm38GpOMwcG~0ZRAgZJohy85gApq3SCMbu70~LvFy8voKSo-QaxT0K-9BufvjdfYFg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":7710,"name":"Biology","url":"https://www.academia.edu/Documents/in/Biology"},{"id":9846,"name":"Ecology","url":"https://www.academia.edu/Documents/in/Ecology"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":53108,"name":"Phosphorus","url":"https://www.academia.edu/Documents/in/Phosphorus"},{"id":53796,"name":"Aquatic Ecosystem","url":"https://www.academia.edu/Documents/in/Aquatic_Ecosystem"},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences"},{"id":83037,"name":"Soil moisture","url":"https://www.academia.edu/Documents/in/Soil_moisture"},{"id":107374,"name":"Factorial Design","url":"https://www.academia.edu/Documents/in/Factorial_Design"},{"id":151091,"name":"Nitrogen","url":"https://www.academia.edu/Documents/in/Nitrogen"},{"id":168668,"name":"Species Diversity","url":"https://www.academia.edu/Documents/in/Species_Diversity"},{"id":199046,"name":"Species Composition","url":"https://www.academia.edu/Documents/in/Species_Composition"},{"id":228848,"name":"Phalaris arundinacea","url":"https://www.academia.edu/Documents/in/Phalaris_arundinacea"},{"id":238233,"name":"Riparian vegetation","url":"https://www.academia.edu/Documents/in/Riparian_vegetation"},{"id":1016853,"name":"Plantago Lanceolata","url":"https://www.academia.edu/Documents/in/Plantago_Lanceolata"},{"id":1222799,"name":"Soil Water","url":"https://www.academia.edu/Documents/in/Soil_Water"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95886995-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95886994"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/95886994/Freshwater_marshes_as_dissolved_silica_recyclers_in_an_estuarine_environment_Schelde_estuary_Belgium_"><img alt="Research paper thumbnail of Freshwater marshes as dissolved silica recyclers in an estuarine environment (Schelde estuary, Belgium)" class="work-thumbnail" src="https://attachments.academia-assets.com/97942112/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95886994/Freshwater_marshes_as_dissolved_silica_recyclers_in_an_estuarine_environment_Schelde_estuary_Belgium_">Freshwater marshes as dissolved silica recyclers in an estuarine environment (Schelde estuary, Belgium)</a></div><div class="wp-workCard_item"><span>Hydrobiologia</span><span>, 2005</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Compared to knowledge about N and P processing in the aquatic continuum of lakes, wetlands and es...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Compared to knowledge about N and P processing in the aquatic continuum of lakes, wetlands and estuaries, knowledge concerning transport and cycling of Si is only fragmentary. Furthermore, Si research in estuaries has mainly been focused on subtidal benthic sediments and uptake and recycling by diatom communities. The biogeochemical cycling of Si in tidal wetlands, which can contain large amounts of Si, has thus far been neglected. We have conducted several whole ecosystem Si mass-balances on a freshwater marsh located in the Schelde estuary (6 tidal cycles, 2 with BSi included). Our measurements show that the freshwater marsh acts as an important source of dissolved Si to the main river (1-18% more export than import, on average 0.114 g m)2). This export is compensated by import of amorphous silica into the marsh (19-55% more import than export). The marsh was shown to act as silica recycler, resupplying biologically available dissolved Si to the estuarine ecosystem. Extrapolations show that during summer and spring months, when dissolved silica is depleted due to diatom growth, almost half of the total dissolved silica load in the main river channel could result from marsh recycling.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b2f26e8e586f96dfa51c2231c953fae1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942112,&quot;asset_id&quot;:95886994,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942112/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95886994"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95886994"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95886994; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95886994]").text(description); $(".js-view-count[data-work-id=95886994]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95886994; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95886994']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "b2f26e8e586f96dfa51c2231c953fae1" } } $('.js-work-strip[data-work-id=95886994]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95886994,"title":"Freshwater marshes as dissolved silica recyclers in an estuarine environment (Schelde estuary, Belgium)","translated_title":"","metadata":{"publisher":"Springer Science and Business Media LLC","ai_title_tag":"Marshes as Dissolved Silica Recyclers in Estuaries","grobid_abstract":"Compared to knowledge about N and P processing in the aquatic continuum of lakes, wetlands and estuaries, knowledge concerning transport and cycling of Si is only fragmentary. Furthermore, Si research in estuaries has mainly been focused on subtidal benthic sediments and uptake and recycling by diatom communities. The biogeochemical cycling of Si in tidal wetlands, which can contain large amounts of Si, has thus far been neglected. We have conducted several whole ecosystem Si mass-balances on a freshwater marsh located in the Schelde estuary (6 tidal cycles, 2 with BSi included). Our measurements show that the freshwater marsh acts as an important source of dissolved Si to the main river (1-18% more export than import, on average 0.114 g m)2). This export is compensated by import of amorphous silica into the marsh (19-55% more import than export). The marsh was shown to act as silica recycler, resupplying biologically available dissolved Si to the estuarine ecosystem. Extrapolations show that during summer and spring months, when dissolved silica is depleted due to diatom growth, almost half of the total dissolved silica load in the main river channel could result from marsh recycling.","publication_date":{"day":null,"month":null,"year":2005,"errors":{}},"publication_name":"Hydrobiologia","grobid_abstract_attachment_id":97942112},"translated_abstract":null,"internal_url":"https://www.academia.edu/95886994/Freshwater_marshes_as_dissolved_silica_recyclers_in_an_estuarine_environment_Schelde_estuary_Belgium_","translated_internal_url":"","created_at":"2023-01-29T00:36:07.325-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":184662190,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":97942112,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942112/thumbnails/1.jpg","file_name":"113427.pdf","download_url":"https://www.academia.edu/attachments/97942112/download_file","bulk_download_file_name":"Freshwater_marshes_as_dissolved_silica_r.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942112/113427-libre.pdf?1674982255=\u0026response-content-disposition=attachment%3B+filename%3DFreshwater_marshes_as_dissolved_silica_r.pdf\u0026Expires=1743224695\u0026Signature=Ob5GCIYRYwaBdTEEFFB8XD2M1uodrfUEhIRBPY3MPswGxd-qS6Pk166PzWkvIRbpSyZGbGCxiyyAnHGD-~F26X~-lnaLFV83qYM58Dim4KC4pI0IXGwz69l0kf9-3g49ELv9bVj4-181bfpgaCz4V3p9a3J-EB~s3HElNKh6C7YOxAvEVd-JBq6nw3SPgxLL7e-Jm7xWATR291DnPbmznq3oeYNsAZfWLqrBN8G45waCqK410pleao2G1UBiQVWn3kQ-NArEQ326BSZ~eJcDHRb5UYvZUTqbOhK1c3afTyFyFKtbfxG94HHsd9MCimfSq50dI-qOvdXf6Wuc7m0QAQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Freshwater_marshes_as_dissolved_silica_recyclers_in_an_estuarine_environment_Schelde_estuary_Belgium_","translated_slug":"","page_count":9,"language":"en","content_type":"Work","summary":"Compared to knowledge about N and P processing in the aquatic continuum of lakes, wetlands and estuaries, knowledge concerning transport and cycling of Si is only fragmentary. Furthermore, Si research in estuaries has mainly been focused on subtidal benthic sediments and uptake and recycling by diatom communities. The biogeochemical cycling of Si in tidal wetlands, which can contain large amounts of Si, has thus far been neglected. We have conducted several whole ecosystem Si mass-balances on a freshwater marsh located in the Schelde estuary (6 tidal cycles, 2 with BSi included). Our measurements show that the freshwater marsh acts as an important source of dissolved Si to the main river (1-18% more export than import, on average 0.114 g m)2). This export is compensated by import of amorphous silica into the marsh (19-55% more import than export). The marsh was shown to act as silica recycler, resupplying biologically available dissolved Si to the estuarine ecosystem. Extrapolations show that during summer and spring months, when dissolved silica is depleted due to diatom growth, almost half of the total dissolved silica load in the main river channel could result from marsh recycling.","owner":{"id":184662190,"first_name":"Patrick","middle_initials":null,"last_name":"Meire","page_name":"MeireP","domain_name":"independent","created_at":"2021-02-03T07:39:55.559-08:00","display_name":"Patrick Meire","url":"https://independent.academia.edu/MeireP"},"attachments":[{"id":97942112,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942112/thumbnails/1.jpg","file_name":"113427.pdf","download_url":"https://www.academia.edu/attachments/97942112/download_file","bulk_download_file_name":"Freshwater_marshes_as_dissolved_silica_r.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942112/113427-libre.pdf?1674982255=\u0026response-content-disposition=attachment%3B+filename%3DFreshwater_marshes_as_dissolved_silica_r.pdf\u0026Expires=1743224695\u0026Signature=Ob5GCIYRYwaBdTEEFFB8XD2M1uodrfUEhIRBPY3MPswGxd-qS6Pk166PzWkvIRbpSyZGbGCxiyyAnHGD-~F26X~-lnaLFV83qYM58Dim4KC4pI0IXGwz69l0kf9-3g49ELv9bVj4-181bfpgaCz4V3p9a3J-EB~s3HElNKh6C7YOxAvEVd-JBq6nw3SPgxLL7e-Jm7xWATR291DnPbmznq3oeYNsAZfWLqrBN8G45waCqK410pleao2G1UBiQVWn3kQ-NArEQ326BSZ~eJcDHRb5UYvZUTqbOhK1c3afTyFyFKtbfxG94HHsd9MCimfSq50dI-qOvdXf6Wuc7m0QAQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":9846,"name":"Ecology","url":"https://www.academia.edu/Documents/in/Ecology"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences"},{"id":83587,"name":"Wetland","url":"https://www.academia.edu/Documents/in/Wetland"},{"id":98440,"name":"Silica","url":"https://www.academia.edu/Documents/in/Silica"},{"id":184353,"name":"Diatom","url":"https://www.academia.edu/Documents/in/Diatom"},{"id":254223,"name":"Biogenic silica","url":"https://www.academia.edu/Documents/in/Biogenic_silica"},{"id":379570,"name":"Estuary","url":"https://www.academia.edu/Documents/in/Estuary"},{"id":956838,"name":"Marsh","url":"https://www.academia.edu/Documents/in/Marsh"},{"id":1707373,"name":"Mass Balance","url":"https://www.academia.edu/Documents/in/Mass_Balance"},{"id":4023440,"name":"Biogeochemical Cycle","url":"https://www.academia.edu/Documents/in/Biogeochemical_Cycle"}],"urls":[{"id":28485827,"url":"http://link.springer.com/content/pdf/10.1007/s10750-004-7104-0.pdf"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95886994-figures'); } }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="14298159" id="papers"><div class="js-work-strip profile--work_container" data-work-id="99924468"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/99924468/The_Scheldt_estuary_a_description_of_a_changing_ecosystem"><img alt="Research paper thumbnail of The Scheldt estuary: a description of a changing ecosystem" class="work-thumbnail" src="https://attachments.academia-assets.com/100884371/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/99924468/The_Scheldt_estuary_a_description_of_a_changing_ecosystem">The Scheldt estuary: a description of a changing ecosystem</a></div><div class="wp-workCard_item"><span>Hydrobiologia</span><span>, 2005</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Estuaries are naturally highly dynamic and rapidly changing systems, forming a complex mixture of...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Estuaries are naturally highly dynamic and rapidly changing systems, forming a complex mixture of many different habitat types. They are very productive biomes and support many important ecosystem functions: biogeochemical cycling and movement of nutrients, mitigation of floods, maintenance of biodiversity and biological production. Human pressure on estuaries is very high. On the other hand, it is recognized that estuaries have a unique functional and structural biodiversity. Therefore, these ecosystems are particularly important for integrating sound ecological management with sustainable economics. These opportunities are explored for the Scheldt estuary, a well-documented system with an exceptional tidal freshwater area. In this article a description of the Scheldt estuary is presented, illustrating that human influence is intertwined with natural dynamics. Hydrology, geomorphology, trophic status and diversity are discussed, and possible future trends in both natural evolution and management are argued.</span></div><div class="wp-workCard_item"><div class="carousel-container carousel-container--sm" id="profile-work-99924468-figures"><div class="prev-slide-container js-prev-button-container"><button aria-label="Previous" class="carousel-navigation-button js-profile-work-99924468-figures-prev"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">arrow_back_ios</span></button></div><div class="slides-container js-slides-container"><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325021/figure-1-map-of-the-scheldt-estuary"><img alt="Figure 1. Map of the Scheldt estuary. " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/figure_001.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325039/figure-3-duration-of-the-period-of-rising-tide-along-the-lon"><img alt="Figure 3. Duration of the period of rising tide along the lon- gitudinal gradient of the Scheldt estuary (based on data of the Maritime Access Division of the Flemish Government). Figure 2. Fresh water discharge in the Scheldt estuary at Schelle (period 1990-2004) (source data: Maritime Access Division, Flemisch Government). " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/figure_002.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325052/figure-3-the-scheldt-estuary-description-of-changing"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/100884371/figure_003.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325064/figure-4-amounts-of-dredged-volume-in-the-scheldt-estuary-in"><img alt="Figure 4. Amounts of dredged volume in the Scheldt estuary in Belgium (B) and the Netherlands (NL) (period 1990-2003) (source: Maritime Access Division of the Flemish government). " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/figure_004.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325074/figure-5-channel-depth-at-locations-in-the-westerschelde"><img alt="Figure 5. Channel depth at 4 locations in the Westerschelde (GLLWS = level at averaged minimal low spring tide) (based on data of the Ministry of Transport, Public Works and Water Management of the Netherlands). " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/figure_005.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325083/figure-6-habitat-area-evolution-in-the-westerschelde-over"><img alt="Figure 6. Habitat area evolution in the Westerschelde over the last centuries. NAP =the Dutch standard altitude reference level, the relation with the Belgian TAW standard is: NAP (m) + 2.33 m=TAW (m) (source: Ministry of Transport, Public Works and Water Management of the Netherlands). " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/figure_006.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325092/figure-7-evolution-of-mean-high-water-level-mhw-squares-and"><img alt="Figure 7. Evolution of mean high water level (MHW, squares) and mean low water level (MLW, open circles) in the Scheldt estuary near Antwerpen (based on data of the Maritime Access Division of the Flemish Government). Intertidal habitat was also lost due to dike building. In order to protect the land against storm floods from the North Sea all dikes along the estuary (more than 700 km) have been heightened and strengthened. Therefore, the base of the dikes needed to be widened, which was mostly done on the marshes and not on the landside of the dike. By now, over more than 50% of the total length of the estuary lacks tidal marshes in front of the dike. This disrupted the connectivity of marshes along the salinity gradient. " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/figure_007.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325098/figure-8-diversity-number-of-species-along-the-salinity-gra"><img alt="Figure 8. Diversity (number of species) along the salinity gra- dient of the Scheldt estuary (after Van den Bergh et al., 2001). " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/figure_008.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325105/table-1-some-characteristics-of-the-scheldt-estuary-at"><img alt="Table 1. Some characteristics of the Scheldt estuary at several locations (based on data of the Maritime Access Division of the Flemish Government). For positions of the locations see Figure 1 " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/table_001.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325115/table-2-habitat-surface-ha-in-the-scheldt-estuary-ited-and"><img alt="Table 2. Habitat surface (ha) in the Scheldt estuary ited and resuspended by the tidal flow. The dis- tribution of suspended matter is influenced by a range of interrelated processes (e.g. temperature and biological activity, fresh water discharge and salinity, hydrodynamic conditions and turbulence, mineralogical composition, chemical conditions, aggregation and flocculation). In the Scheldt estuary, the turbidity maximum is situated at about 110 km from the mouth during dry periods and at about 50 km during wet periods (Wollast, 1988). Two MTZ might be observed, one at the freshwater/seawater interface, and a second one originating from tidal asymmetry (Baeyens et al., 1998; Fettweis et al., 1998; Herman &amp; Heip, 1999). " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/table_002.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/53325125/table-3-river-bank-characteristics-of-the-zeeschelde-between"><img alt="Table 3. River bank characteristics of the Zeeschelde between the Dutch Belgian border and Ghent (after Hoffmann &amp; Meire, 1997 observed along the salinity gradient of the Schelde estuary (Ysebaert et al., 2000). Biodiversity " class="figure-slide-image" src="https://figures.academia-assets.com/100884371/table_003.jpg" /></a></figure></div><div class="next-slide-container js-next-button-container"><button aria-label="Next" class="carousel-navigation-button js-profile-work-99924468-figures-next"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">arrow_forward_ios</span></button></div></div></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="3a93f4f36ef063972004cf7e1acbde07" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:100884371,&quot;asset_id&quot;:99924468,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/100884371/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="99924468"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="99924468"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 99924468; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=99924468]").text(description); $(".js-view-count[data-work-id=99924468]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 99924468; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='99924468']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "3a93f4f36ef063972004cf7e1acbde07" } } $('.js-work-strip[data-work-id=99924468]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":99924468,"title":"The Scheldt estuary: a description of a changing ecosystem","translated_title":"","metadata":{"publisher":"Springer Science and Business Media LLC","grobid_abstract":"Estuaries are naturally highly dynamic and rapidly changing systems, forming a complex mixture of many different habitat types. 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Nevertheless, insitu ob...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Tidal wetlands are increasingly valued for their role in coastal defense. Nevertheless, insitu observations of storm surge attenuation within wetlands are still scarce. We present water level measurements along a 4 km intertidal channel and on the surrounding marsh platform for regular spring to neap tides and two major storm surge tides, showing the effects of flood wave height and marsh geomorphology on the amount of flood wave attenuation. Undermarsh tides with peak water levels below marsh platform elevation are mostly amplified (up to 4 cm/km) within the channels. Overmarsh tides with peak water levels above the marsh platform are generally attenuated along the channels, with maximum attenuation rates of 5 cm/km for tides that inundate the marsh platform by 0.5-1.0 m. For lower or higher flood waves, including storm surges, attenuation rates decrease. Furthermore, the observations show that the maximum attenuation occurs along narrow channel transects where the width of the platform is larger, whereas attenuation rates are lower along wider channels with smaller adjacent marsh platforms. These observations are confirmed by an analytical approximation of tidal wave propagation through convergent channels. The analytical model indicates that differences in attenuation rates are induced by variations in the cross-channel averaged friction between channel sections and between tides with varying peak water levels. Finally, the highest attenuation rates of up to 70 cm/km are observed over short distances on the vegetated marsh platform. We conclude that this 2 study provides an empirical basis for the wider implementation of nature-based flood defense 18 strategies.</span></div><div class="wp-workCard_item"><div class="carousel-container carousel-container--sm" id="profile-work-95887013-figures"><div class="prev-slide-container js-prev-button-container"><button aria-label="Previous" class="carousel-navigation-button js-profile-work-95887013-figures-prev"><span class="material-symbols-outlined" style="font-size: 24px" translate="no">arrow_back_ios</span></button></div><div class="slides-container js-slides-container"><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754256/figure-1-observations-of-tidal-and-storm-surge-attenuation"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/97942111/figure_001.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754263/figure-2-observations-of-tidal-and-storm-surge-attenuation"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/97942111/figure_002.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754269/figure-3-observations-of-tidal-and-storm-surge-attenuation"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/97942111/figure_003.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754273/figure-4-observations-of-tidal-and-storm-surge-attenuation"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/97942111/figure_004.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754277/figure-5-observations-of-tidal-and-storm-surge-attenuation"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/97942111/figure_005.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754284/figure-6-observations-of-tidal-and-storm-surge-attenuation"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/97942111/figure_006.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754288/figure-7-observations-of-tidal-and-storm-surge-attenuation"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/97942111/figure_007.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754294/figure-8-observations-of-tidal-and-storm-surge-attenuation"><img alt="" class="figure-slide-image" src="https://figures.academia-assets.com/97942111/figure_008.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754298/table-1-values-denote-that-amplification-was-observed"><img alt="values denote that amplification was observed. " class="figure-slide-image" src="https://figures.academia-assets.com/97942111/table_001.jpg" /></a></figure><figure class="figure-slide-container"><a href="https://www.academia.edu/figures/25754310/table-2-hmean-maximum-channel-depth-below-mhwl-hyax-and"><img alt="(Hmean), Maximum channel depth below MHWL (hyax) and cross-sectional area (A,). 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Furthermore, the observations show that the maximum attenuation occurs along narrow channel transects where the width of the platform is larger, whereas attenuation rates are lower along wider channels with smaller adjacent marsh platforms. These observations are confirmed by an analytical approximation of tidal wave propagation through convergent channels. The analytical model indicates that differences in attenuation rates are induced by variations in the cross-channel averaged friction between channel sections and between tides with varying peak water levels. Finally, the highest attenuation rates of up to 70 cm/km are observed over short distances on the vegetated marsh platform. 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This theory implies that thresholds of environmental factors can mark a limit between two opposing stable ecosystem states, e.g. vegetated marshes and bare mudflats. While elevation relative to mean sea level is considered as the overall threshold condition for colonization of mudflats by vegetation, little is known about the individual driving mechanisms, in particular the impact of waves, and more specifically of wave period. We studied the impact of different wave regimes on plants in a full scale flume experiment. Seedlings and adult shoots of the pioneer Scirpus maritimus were subjected to two wave periods at two water levels. Drag forces acting on, and sediment scouring occurring around the plants were quantified, as these are the two main mechanisms determining plant establishment and survival. 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It has nume...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Silicon is one of the most important elements in the current age of the anthropocene. It has numerous industrial applications, and supports a high-tech multi-billion Euro industry. Silicon has a fascinating biological and geological cycle, interacting with other globally important biogeochemical cycles. 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Nevertheless, spatial planning decisions would benefit from systematic considerations of their effects on ecosystem services. Assessing the impacts of policy on a wide range of ecosystem services contributes to more cost-effective policy implementation, establishing win-win situations across different environmental domains. The “nature value explorer” (natuurwaardeverkenner in Dutch) is a web application developed to explore the quantity and value of ecosystem services in Flanders, Belgium, as part of environmental impact assessments. The tool estimates the impact of land-use and land-cover change on regulating and cultural ecosystem services. 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Nevertheless, spatial planning decisions would benefit from systematic considerations of their effects on ecosystem services. Assessing the impacts of policy on a wide range of ecosystem services contributes to more cost-effective policy implementation, establishing win-win situations across different environmental domains. The “nature value explorer” (natuurwaardeverkenner in Dutch) is a web application developed to explore the quantity and value of ecosystem services in Flanders, Belgium, as part of environmental impact assessments. The tool estimates the impact of land-use and land-cover change on regulating and cultural ecosystem services. The web application is successful in drawing the interest of policy makers and is used in several cases to support decisions in infrastructural projects as well as nature restoration projects.","owner":{"id":184662190,"first_name":"Patrick","middle_initials":null,"last_name":"Meire","page_name":"MeireP","domain_name":"independent","created_at":"2021-02-03T07:39:55.559-08:00","display_name":"Patrick Meire","url":"https://independent.academia.edu/MeireP"},"attachments":[],"research_interests":[{"id":26,"name":"Business","url":"https://www.academia.edu/Documents/in/Business"},{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":2312,"name":"Ecosystem Services","url":"https://www.academia.edu/Documents/in/Ecosystem_Services"},{"id":7710,"name":"Biology","url":"https://www.academia.edu/Documents/in/Biology"},{"id":62646,"name":"Environmental Resource Management","url":"https://www.academia.edu/Documents/in/Environmental_Resource_Management"},{"id":95993,"name":"Web Application","url":"https://www.academia.edu/Documents/in/Web_Application"},{"id":417820,"name":"Scenario Analysis","url":"https://www.academia.edu/Documents/in/Scenario_Analysis"},{"id":457859,"name":"Cost Benefit Analysis","url":"https://www.academia.edu/Documents/in/Cost_Benefit_Analysis"},{"id":2497410,"name":"Monetary valuation","url":"https://www.academia.edu/Documents/in/Monetary_valuation"},{"id":2960847,"name":"ecosystem valuation","url":"https://www.academia.edu/Documents/in/ecosystem_valuation"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95887007-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95887006"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95887006/Dissolved_Silicon_and_Its_Origin_in_Belgian_Beers_A_Multivariate_Analysis"><img alt="Research paper thumbnail of Dissolved Silicon and Its Origin in Belgian Beers—A Multivariate Analysis" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title">Dissolved Silicon and Its Origin in Belgian Beers—A Multivariate Analysis</div><div class="wp-workCard_item"><span>Silicon</span><span>, 2012</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">ABSTRACT Beer is a quintessential part of Belgian heritage. We performed a detailed analysis of f...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">ABSTRACT Beer is a quintessential part of Belgian heritage. We performed a detailed analysis of factors controlling Si content in Belgian beers as a case study to coincide with the 2011 IBiS meeting in Antwerp (Belgium). Beer is one of the richest dietary sources of Si. Three decades of research have yielded evidence of a role for Si in human physiology: it plays an essential role in bone mineral density and reduces the biological availability of aluminium. We analysed 119 Belgian beers: highest dissolved Si concentrations were found in high fermentation, traditionally brewed ales. Concentrations ranged between 214 and 2,071 μmol L − 1. This is probably due to the complexity and length of the brewing procedure: longer, more complicated processing and presence of brewing sediment in the bottle allows more Si to dissolve out of the base products like hop, barley or even rice. As a side effect of fermentation, alcohol content was related to Si content.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95887006"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95887006"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95887006; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95887006]").text(description); $(".js-view-count[data-work-id=95887006]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95887006; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95887006']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=95887006]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95887006,"title":"Dissolved Silicon and Its Origin in Belgian Beers—A Multivariate Analysis","translated_title":"","metadata":{"abstract":"ABSTRACT Beer is a quintessential part of Belgian heritage. We performed a detailed analysis of factors controlling Si content in Belgian beers as a case study to coincide with the 2011 IBiS meeting in Antwerp (Belgium). Beer is one of the richest dietary sources of Si. Three decades of research have yielded evidence of a role for Si in human physiology: it plays an essential role in bone mineral density and reduces the biological availability of aluminium. We analysed 119 Belgian beers: highest dissolved Si concentrations were found in high fermentation, traditionally brewed ales. Concentrations ranged between 214 and 2,071 μmol L − 1. This is probably due to the complexity and length of the brewing procedure: longer, more complicated processing and presence of brewing sediment in the bottle allows more Si to dissolve out of the base products like hop, barley or even rice. As a side effect of fermentation, alcohol content was related to Si content.","publisher":"Springer Nature","publication_date":{"day":null,"month":null,"year":2012,"errors":{}},"publication_name":"Silicon"},"translated_abstract":"ABSTRACT Beer is a quintessential part of Belgian heritage. We performed a detailed analysis of factors controlling Si content in Belgian beers as a case study to coincide with the 2011 IBiS meeting in Antwerp (Belgium). Beer is one of the richest dietary sources of Si. Three decades of research have yielded evidence of a role for Si in human physiology: it plays an essential role in bone mineral density and reduces the biological availability of aluminium. We analysed 119 Belgian beers: highest dissolved Si concentrations were found in high fermentation, traditionally brewed ales. Concentrations ranged between 214 and 2,071 μmol L − 1. This is probably due to the complexity and length of the brewing procedure: longer, more complicated processing and presence of brewing sediment in the bottle allows more Si to dissolve out of the base products like hop, barley or even rice. As a side effect of fermentation, alcohol content was related to Si content.","internal_url":"https://www.academia.edu/95887006/Dissolved_Silicon_and_Its_Origin_in_Belgian_Beers_A_Multivariate_Analysis","translated_internal_url":"","created_at":"2023-01-29T00:36:08.956-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":184662190,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Dissolved_Silicon_and_Its_Origin_in_Belgian_Beers_A_Multivariate_Analysis","translated_slug":"","page_count":null,"language":"en","content_type":"Work","summary":"ABSTRACT Beer is a quintessential part of Belgian heritage. We performed a detailed analysis of factors controlling Si content in Belgian beers as a case study to coincide with the 2011 IBiS meeting in Antwerp (Belgium). Beer is one of the richest dietary sources of Si. Three decades of research have yielded evidence of a role for Si in human physiology: it plays an essential role in bone mineral density and reduces the biological availability of aluminium. We analysed 119 Belgian beers: highest dissolved Si concentrations were found in high fermentation, traditionally brewed ales. Concentrations ranged between 214 and 2,071 μmol L − 1. This is probably due to the complexity and length of the brewing procedure: longer, more complicated processing and presence of brewing sediment in the bottle allows more Si to dissolve out of the base products like hop, barley or even rice. As a side effect of fermentation, alcohol content was related to Si content.","owner":{"id":184662190,"first_name":"Patrick","middle_initials":null,"last_name":"Meire","page_name":"MeireP","domain_name":"independent","created_at":"2021-02-03T07:39:55.559-08:00","display_name":"Patrick Meire","url":"https://independent.academia.edu/MeireP"},"attachments":[],"research_interests":[{"id":498,"name":"Physics","url":"https://www.academia.edu/Documents/in/Physics"},{"id":511,"name":"Materials Science","url":"https://www.academia.edu/Documents/in/Materials_Science"},{"id":523,"name":"Chemistry","url":"https://www.academia.edu/Documents/in/Chemistry"},{"id":1907,"name":"Nutrition","url":"https://www.academia.edu/Documents/in/Nutrition"},{"id":7710,"name":"Biology","url":"https://www.academia.edu/Documents/in/Biology"},{"id":11406,"name":"Silicon","url":"https://www.academia.edu/Documents/in/Silicon"},{"id":67429,"name":"Brewing","url":"https://www.academia.edu/Documents/in/Brewing"},{"id":269129,"name":"Fermentation","url":"https://www.academia.edu/Documents/in/Fermentation"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95887006-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95887005"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/95887005/Landscape_cultivation_alters_%CE%B4_30_Si_signature_in_terrestrial_ecosystems"><img alt="Research paper thumbnail of Landscape cultivation alters δ(30)Si signature in terrestrial ecosystems" class="work-thumbnail" src="https://attachments.academia-assets.com/97942107/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95887005/Landscape_cultivation_alters_%CE%B4_30_Si_signature_in_terrestrial_ecosystems">Landscape cultivation alters δ(30)Si signature in terrestrial ecosystems</a></div><div class="wp-workCard_item"><span>Scientific reports</span><span>, Jan 13, 2015</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Despite increasing recognition of the relevance of biological cycling for Si cycling in ecosystem...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Despite increasing recognition of the relevance of biological cycling for Si cycling in ecosystems and for Si export from soils to fluvial systems, effects of human cultivation on the Si cycle are still relatively understudied. Here we examined stable Si isotope (δ(30)Si) signatures in soil water samples across a temperate land use gradient. We show that - independent of geological and climatological variation - there is a depletion in light isotopes in soil water of intensive croplands and managed grasslands relative to native forests. Furthermore, our data suggest a divergence in δ(30)Si signatures along the land use change gradient, highlighting the imprint of vegetation cover, human cultivation and intensity of disturbance on δ(30)Si patterns, on top of more conventionally acknowledged drivers (i.e. mineralogy and climate).</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="5e065f5077ec46cb09ee36b61b09fdad" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942107,&quot;asset_id&quot;:95887005,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942107/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95887005"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95887005"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95887005; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95887005]").text(description); $(".js-view-count[data-work-id=95887005]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95887005; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95887005']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "5e065f5077ec46cb09ee36b61b09fdad" } } $('.js-work-strip[data-work-id=95887005]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95887005,"title":"Landscape cultivation alters δ(30)Si signature in terrestrial ecosystems","translated_title":"","metadata":{"abstract":"Despite increasing recognition of the relevance of biological cycling for Si cycling in ecosystems and for Si export from soils to fluvial systems, effects of human cultivation on the Si cycle are still relatively understudied. Here we examined stable Si isotope (δ(30)Si) signatures in soil water samples across a temperate land use gradient. We show that - independent of geological and climatological variation - there is a depletion in light isotopes in soil water of intensive croplands and managed grasslands relative to native forests. Furthermore, our data suggest a divergence in δ(30)Si signatures along the land use change gradient, highlighting the imprint of vegetation cover, human cultivation and intensity of disturbance on δ(30)Si patterns, on top of more conventionally acknowledged drivers (i.e. mineralogy and climate).","ai_title_tag":"Human cultivation impacts δ(30)Si signatures in soils","publication_date":{"day":13,"month":1,"year":2015,"errors":{}},"publication_name":"Scientific reports"},"translated_abstract":"Despite increasing recognition of the relevance of biological cycling for Si cycling in ecosystems and for Si export from soils to fluvial systems, effects of human cultivation on the Si cycle are still relatively understudied. Here we examined stable Si isotope (δ(30)Si) signatures in soil water samples across a temperate land use gradient. We show that - independent of geological and climatological variation - there is a depletion in light isotopes in soil water of intensive croplands and managed grasslands relative to native forests. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95887005-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95887004"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/95887004/Determination_of_groundwater_fluxes_in_the_Belgian_Aa_River_by_sensing_and_simulation_of_streambed_temperatures"><img alt="Research paper thumbnail of Determination of groundwater fluxes in the Belgian Aa River by sensing and simulation of streambed temperatures" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title">Determination of groundwater fluxes in the Belgian Aa River by sensing and simulation of streambed temperatures</div><div class="wp-workCard_item"><span>IAHS Publications- …</span><span>, 2008</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95887004"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95887004"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95887004; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95887004-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95887003"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/95887003/Pathological_investigations_on_guillemots_Uria_aalge_stranded_on_the_Belgian_coast_during_the_winter_of_1993_94"><img alt="Research paper thumbnail of Pathological investigations on guillemots (Uria aalge ) stranded on the Belgian coast during the winter of 1993-94" class="work-thumbnail" src="https://attachments.academia-assets.com/97942110/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95887003/Pathological_investigations_on_guillemots_Uria_aalge_stranded_on_the_Belgian_coast_during_the_winter_of_1993_94">Pathological investigations on guillemots (Uria aalge ) stranded on the Belgian coast during the winter of 1993-94</a></div><div class="wp-workCard_item"><span>Veterinary Record</span><span>, 1998</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d0260093b22df7cc96e29d664f69066d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942110,&quot;asset_id&quot;:95887003,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942110/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95887003"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95887003"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95887003; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95887003-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95887002"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/95887002/Ecological_Rehabilitation_of_the_Schelde_Estuary_The_Netherlands_Belgium_Northwest_Europe_Linking_Ecology_Safety_Against_Floods_and_Accessibility_for_Port_Development"><img alt="Research paper thumbnail of Ecological Rehabilitation of the Schelde Estuary (The Netherlands-Belgium; Northwest Europe): Linking Ecology, Safety Against Floods, and Accessibility for Port Development" class="work-thumbnail" src="https://attachments.academia-assets.com/97942109/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95887002/Ecological_Rehabilitation_of_the_Schelde_Estuary_The_Netherlands_Belgium_Northwest_Europe_Linking_Ecology_Safety_Against_Floods_and_Accessibility_for_Port_Development">Ecological Rehabilitation of the Schelde Estuary (The Netherlands-Belgium; Northwest Europe): Linking Ecology, Safety Against Floods, and Accessibility for Port Development</a></div><div class="wp-workCard_item"><span>Restoration Ecology</span><span>, 2005</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Long-Term Vision for the Schelde estuary was determined as &#39;&#39;the development of a healthy and...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The Long-Term Vision for the Schelde estuary was determined as &#39;&#39;the development of a healthy and multifunctional estuarine water system that can be utilized in a sustainable way for human needs.&#39;&#39; This Dutch-Flemish managerial plan sets quality targets for the condition of the estuary by the year 2030 and the management measures to achieve them. Targets were developed and integrated from three central perspectives: accessibility of the ports, safety against floods in the densely populated catchment, and ecosystem health. This study focuses on the ecological rehabilitation of the estuary and the creation of sustainable nature, seeking possible alliances with security measures against floods, navigation requisites for port activities, and enhancement of the estuary&#39;s educational and recreational values. The estuary and its valley were subdivided into ecologically relevant zones. Key parameters were identified, and a conceptual rehabilitation model was developed, based on a problem analysis. Goals were set in a semiquantified way for most attributes of the estuarine functioning and prioritized for each zone. Rehabilitation measures with maximal contribution to the priority goals were identified for each zone. Spatial analysis of the study area indicated optimal areas for the implementation of these measures. To exemplify the array of possibilities on an ecosystem level, two different rehabilitation plans were proposed, each from a different approach. The potential contribution to the rehabilitation of the estuary was compared for both alternatives.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="bf9d5aae669bb8f683fd849abecf7d65" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942109,&quot;asset_id&quot;:95887002,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942109/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95887002"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95887002"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95887002; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95887002]").text(description); $(".js-view-count[data-work-id=95887002]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95887002; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95887002']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "bf9d5aae669bb8f683fd849abecf7d65" } } $('.js-work-strip[data-work-id=95887002]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95887002,"title":"Ecological Rehabilitation of the Schelde Estuary (The Netherlands-Belgium; Northwest Europe): Linking Ecology, Safety Against Floods, and Accessibility for Port Development","translated_title":"","metadata":{"publisher":"Wiley-Blackwell","ai_title_tag":"Ecological Rehabilitation of the Schelde Estuary: Balancing Ecology, Flood Safety, and Port Accessibility","grobid_abstract":"The Long-Term Vision for the Schelde estuary was determined as ''the development of a healthy and multifunctional estuarine water system that can be utilized in a sustainable way for human needs.'' This Dutch-Flemish managerial plan sets quality targets for the condition of the estuary by the year 2030 and the management measures to achieve them. Targets were developed and integrated from three central perspectives: accessibility of the ports, safety against floods in the densely populated catchment, and ecosystem health. This study focuses on the ecological rehabilitation of the estuary and the creation of sustainable nature, seeking possible alliances with security measures against floods, navigation requisites for port activities, and enhancement of the estuary's educational and recreational values. The estuary and its valley were subdivided into ecologically relevant zones. Key parameters were identified, and a conceptual rehabilitation model was developed, based on a problem analysis. Goals were set in a semiquantified way for most attributes of the estuarine functioning and prioritized for each zone. Rehabilitation measures with maximal contribution to the priority goals were identified for each zone. Spatial analysis of the study area indicated optimal areas for the implementation of these measures. To exemplify the array of possibilities on an ecosystem level, two different rehabilitation plans were proposed, each from a different approach. The potential contribution to the rehabilitation of the estuary was compared for both alternatives.","publication_date":{"day":null,"month":null,"year":2005,"errors":{}},"publication_name":"Restoration Ecology","grobid_abstract_attachment_id":97942109},"translated_abstract":null,"internal_url":"https://www.academia.edu/95887002/Ecological_Rehabilitation_of_the_Schelde_Estuary_The_Netherlands_Belgium_Northwest_Europe_Linking_Ecology_Safety_Against_Floods_and_Accessibility_for_Port_Development","translated_internal_url":"","created_at":"2023-01-29T00:36:08.500-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":184662190,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":97942109,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942109/thumbnails/1.jpg","file_name":"174185.pdf","download_url":"https://www.academia.edu/attachments/97942109/download_file","bulk_download_file_name":"Ecological_Rehabilitation_of_the_Schelde.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942109/174185-libre.pdf?1674982265=\u0026response-content-disposition=attachment%3B+filename%3DEcological_Rehabilitation_of_the_Schelde.pdf\u0026Expires=1743224695\u0026Signature=YZ6d7gW8tpZFOKdM8kCqW-3EV3YoQH82AUc-t8aCqf9QW2MlTLXX-oe3gDel0ITotlNMqqbCv527d-TFkdHzYtWd2Bb4F6izjSBqoDIxwZnGR3GiigqrXEYtB9soN3uWGeaGVJmbvMNq7KZGYA4j7ZOn6I4PTuYyuBJPL-20SxvdYHtKcDUGZ-xROk4d1TDEnhvORVYHk~MnuZCLwgdnvgWjH1xVQ3xS7t9jp0z7r~MDlOvSFm7q6MvklDFRi2~dfEeUzqP47jdJ92ykisl9bjGLcis4k5vvP-p~94WpUoEPba8aoCwKiAKxFLAOiQ4dRyCnhfhlpj2eY5h21Jw3Yw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Ecological_Rehabilitation_of_the_Schelde_Estuary_The_Netherlands_Belgium_Northwest_Europe_Linking_Ecology_Safety_Against_Floods_and_Accessibility_for_Port_Development","translated_slug":"","page_count":11,"language":"en","content_type":"Work","summary":"The Long-Term Vision for the Schelde estuary was determined as ''the development of a healthy and multifunctional estuarine water system that can be utilized in a sustainable way for human needs.'' This Dutch-Flemish managerial plan sets quality targets for the condition of the estuary by the year 2030 and the management measures to achieve them. Targets were developed and integrated from three central perspectives: accessibility of the ports, safety against floods in the densely populated catchment, and ecosystem health. This study focuses on the ecological rehabilitation of the estuary and the creation of sustainable nature, seeking possible alliances with security measures against floods, navigation requisites for port activities, and enhancement of the estuary's educational and recreational values. The estuary and its valley were subdivided into ecologically relevant zones. Key parameters were identified, and a conceptual rehabilitation model was developed, based on a problem analysis. Goals were set in a semiquantified way for most attributes of the estuarine functioning and prioritized for each zone. Rehabilitation measures with maximal contribution to the priority goals were identified for each zone. Spatial analysis of the study area indicated optimal areas for the implementation of these measures. To exemplify the array of possibilities on an ecosystem level, two different rehabilitation plans were proposed, each from a different approach. The potential contribution to the rehabilitation of the estuary was compared for both alternatives.","owner":{"id":184662190,"first_name":"Patrick","middle_initials":null,"last_name":"Meire","page_name":"MeireP","domain_name":"independent","created_at":"2021-02-03T07:39:55.559-08:00","display_name":"Patrick Meire","url":"https://independent.academia.edu/MeireP"},"attachments":[{"id":97942109,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942109/thumbnails/1.jpg","file_name":"174185.pdf","download_url":"https://www.academia.edu/attachments/97942109/download_file","bulk_download_file_name":"Ecological_Rehabilitation_of_the_Schelde.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942109/174185-libre.pdf?1674982265=\u0026response-content-disposition=attachment%3B+filename%3DEcological_Rehabilitation_of_the_Schelde.pdf\u0026Expires=1743224695\u0026Signature=YZ6d7gW8tpZFOKdM8kCqW-3EV3YoQH82AUc-t8aCqf9QW2MlTLXX-oe3gDel0ITotlNMqqbCv527d-TFkdHzYtWd2Bb4F6izjSBqoDIxwZnGR3GiigqrXEYtB9soN3uWGeaGVJmbvMNq7KZGYA4j7ZOn6I4PTuYyuBJPL-20SxvdYHtKcDUGZ-xROk4d1TDEnhvORVYHk~MnuZCLwgdnvgWjH1xVQ3xS7t9jp0z7r~MDlOvSFm7q6MvklDFRi2~dfEeUzqP47jdJ92ykisl9bjGLcis4k5vvP-p~94WpUoEPba8aoCwKiAKxFLAOiQ4dRyCnhfhlpj2eY5h21Jw3Yw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"},{"id":1362,"name":"Spatial Analysis","url":"https://www.academia.edu/Documents/in/Spatial_Analysis"},{"id":2256,"name":"Rehabilitation","url":"https://www.academia.edu/Documents/in/Rehabilitation"},{"id":5221,"name":"Restoration Ecology","url":"https://www.academia.edu/Documents/in/Restoration_Ecology"},{"id":17374,"name":"Restoration","url":"https://www.academia.edu/Documents/in/Restoration"},{"id":22142,"name":"Ecosystem health","url":"https://www.academia.edu/Documents/in/Ecosystem_health"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences"},{"id":62646,"name":"Environmental Resource Management","url":"https://www.academia.edu/Documents/in/Environmental_Resource_Management"},{"id":95108,"name":"RECREATION","url":"https://www.academia.edu/Documents/in/RECREATION"},{"id":202017,"name":"Integrated Management","url":"https://www.academia.edu/Documents/in/Integrated_Management"},{"id":379570,"name":"Estuary","url":"https://www.academia.edu/Documents/in/Estuary"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95887002-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95887001"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/95887001/Macrobenthic_species_response_surfaces_along_estuarine_gradients_prediction_by_logistic_regression"><img alt="Research paper thumbnail of Macrobenthic species response surfaces along estuarine gradients: prediction by logistic regression" class="work-thumbnail" src="https://attachments.academia-assets.com/97942091/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95887001/Macrobenthic_species_response_surfaces_along_estuarine_gradients_prediction_by_logistic_regression">Macrobenthic species response surfaces along estuarine gradients: prediction by logistic regression</a></div><div class="wp-workCard_item"><span>Marine Ecology Progress Series</span><span>, 2002</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e6c4edc92eef43f7c8da91169bc4f024" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942091,&quot;asset_id&quot;:95887001,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942091/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95887001"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95887001"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95887001; 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Ecological response surfaces are derived for 10 estuarine macrobenthic species. Logistic regression is applied on a large data set, predicting the probability of occurrence of macrobenthic species in the Schelde estuary as a response to the predictor variables salinity, depth, current velocity and sediment characteristics. Single logistic regression provides good descriptions of the occurrence along 1 environmental variable. The response surfaces obtained by multiple logistic regression provide estimates of the probability of species occurrence across the spatial extent of the Schelde estuary with a relatively high degree of success. Results from subsampling 50% of the original data 10 times indicate that final models were stable. A visual geographical comparison is presented between the mapped probability surfaces and the species occurrence maps. We conclude that where patterns of distribution are strongly and directly coupled to physicochemical processes, as is the case at the estuarine macro-and meso-scale, our modelling approach was capable of predicting macrobenthic species distributions with a relatively high degree of success, although processes controlling estuarine macrobenthic distribution cannot be determined using this method. However, the models and predictions could be used for evaluation of the effects of different management schemes within the Schelde estuary.","ai_title_tag":"Logistic Regression of Estuarine Macrobenthos","publication_date":{"day":null,"month":null,"year":2002,"errors":{}},"publication_name":"Marine Ecology Progress 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in the Southern Bight of the North Sea" class="work-thumbnail" src="https://attachments.academia-assets.com/97942103/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95887000/Diversity_of_the_nematode_communities_in_the_Southern_Bight_of_the_North_Sea">Diversity of the nematode communities in the Southern Bight of the North Sea</a></div><div class="wp-workCard_item"><span>Netherlands Journal of Sea Research</span><span>, 1990</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The nematode communities from 102 stations in the Southern Bight of the North Sea, sumpled betwee...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The nematode communities from 102 stations in the Southern Bight of the North Sea, sumpled between 1972 and 1984, are exam ined. On the whole, 456 species, belonging to 159 genera and 37 families were found. Multispecies patterns are ana lysed by means of cluster analysis (Bray-Curtis dissimilarity coefficient), Twinspan c1 assitïcation and DCA ordination. Generall y, the Southern Bight can be div ided into six main areas on the base of nematode species composition. Sediment structure was fou nd to be the determining environmental factor in the species composition of nematode communit ies. Also several other environmental factors, (temperature, salinity, chlorophyll a, N03-, NH4+) seem ta influence the distribution of the nematode species. One of the most striking features of the coastal ecosystemS , and of the Belgian coastal zone in particular, is the importance of the role of the bacteria. A general increase of the level of primary production in the coastal area , as a result of increasing nutrient input, does not necessarily lead to an increase of pelagie or demersal fish production, but cou Id induce a modification of the food web , in particular the enhancement of microbiological activity at the expense of long trophic chains dominated by macroorganisms. The near absence of nematode-predators in the reg ion off the Belgian east coast, the dom inance of bacterivores, the very low spec ies diversity of the nematode community and the paucity of higher metazoans within the area, can be partly explained on the basis of the increase in nutrient input within the area, and partly on the basis of the high amount of &quot;mixed&quot; pollution. Résumé: Identification des assemblages de nématodes de 102 stations de la partie sud de la mer du Nord où des prélèvements ont été effectués de 1972 il 1984 : 456 espèces ont été répertoriées, appartenant il 159 gen res et 37 familles. Interprétation des communautés par l&#39;analyse des groupements d&#39;espèces (coelficient de dissimilarité de Bray-Curtis et classification polythétique Twinspan) et par l&#39;analyse factorielle des correspondances (DCA). Global ement, le bassin du sud de la mer du Nord peut être di visé en six zones principales définies par la composition spécifiq ue des nématodes. La structure sédimentaire apparaît comme le facte ur du milieu déterminant de la composition spécifique de la nématocoenose ; cependant, d&#39;autres facteurs (température, salinité, ch lorophylle a, N03-, NH4+) semblent égaiement influer sur la distribution des espèces. L&#39;importance du rôle des bactéries représente l&#39;un des caractères les plus remarq uables des écosystèmes côtiers et, en particulier, de celui de la côte belge. Dans cette région, un accroissement du taux de production primaire, lié il une intensification de l&#39;apport de nutriments, n&#39;entraîne pas nécessairement l&#39;augmentation de la production en poissons pélagiques ou démersaux ; mais il pourrait provoquer des modifications des réseaux trophiques, notamment la stimulation de l&#39;activité microbiologique aux dépens des chaînes trophiques longues dominées par les macro-organismes. Au large de la côte est de Belgique, la dominance des nématodes bactérivores, la quasi-absence des prédateurs, la très faible diversité spécifique des communautés de ce groupe et la pauvreté des métazoaires supérieurs peuvent trouver leur expl ication d&#39;une part dans l&#39;augmentation de l&#39;apport en nutriments et d&#39;autre part dans la grande quantité de po llution diffuse.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ca98f2c0f41741edf5d1f9822e10153a" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942103,&quot;asset_id&quot;:95887000,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942103/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95887000"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95887000"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95887000; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95887000]").text(description); $(".js-view-count[data-work-id=95887000]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95887000; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95887000']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "ca98f2c0f41741edf5d1f9822e10153a" } } $('.js-work-strip[data-work-id=95887000]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95887000,"title":"Diversity of the nematode communities in the Southern Bight of the North Sea","translated_title":"","metadata":{"publisher":"Elsevier BV","ai_title_tag":"Nematode Community Diversity in the North Sea","grobid_abstract":"The nematode communities from 102 stations in the Southern Bight of the North Sea, sumpled between 1972 and 1984, are exam ined. On the whole, 456 species, belonging to 159 genera and 37 families were found. Multispecies patterns are ana lysed by means of cluster analysis (Bray-Curtis dissimilarity coefficient), Twinspan c1 assitïcation and DCA ordination. Generall y, the Southern Bight can be div ided into six main areas on the base of nematode species composition. Sediment structure was fou nd to be the determining environmental factor in the species composition of nematode communit ies. Also several other environmental factors, (temperature, salinity, chlorophyll a, N03-, NH4+) seem ta influence the distribution of the nematode species. One of the most striking features of the coastal ecosystemS , and of the Belgian coastal zone in particular, is the importance of the role of the bacteria. A general increase of the level of primary production in the coastal area , as a result of increasing nutrient input, does not necessarily lead to an increase of pelagie or demersal fish production, but cou Id induce a modification of the food web , in particular the enhancement of microbiological activity at the expense of long trophic chains dominated by macroorganisms. The near absence of nematode-predators in the reg ion off the Belgian east coast, the dom inance of bacterivores, the very low spec ies diversity of the nematode community and the paucity of higher metazoans within the area, can be partly explained on the basis of the increase in nutrient input within the area, and partly on the basis of the high amount of \"mixed\" pollution. Résumé: Identification des assemblages de nématodes de 102 stations de la partie sud de la mer du Nord où des prélèvements ont été effectués de 1972 il 1984 : 456 espèces ont été répertoriées, appartenant il 159 gen res et 37 familles. Interprétation des communautés par l'analyse des groupements d'espèces (coelficient de dissimilarité de Bray-Curtis et classification polythétique Twinspan) et par l'analyse factorielle des correspondances (DCA). Global ement, le bassin du sud de la mer du Nord peut être di visé en six zones principales définies par la composition spécifiq ue des nématodes. La structure sédimentaire apparaît comme le facte ur du milieu déterminant de la composition spécifique de la nématocoenose ; cependant, d'autres facteurs (température, salinité, ch lorophylle a, N03-, NH4+) semblent égaiement influer sur la distribution des espèces. L'importance du rôle des bactéries représente l'un des caractères les plus remarq uables des écosystèmes côtiers et, en particulier, de celui de la côte belge. Dans cette région, un accroissement du taux de production primaire, lié il une intensification de l'apport de nutriments, n'entraîne pas nécessairement l'augmentation de la production en poissons pélagiques ou démersaux ; mais il pourrait provoquer des modifications des réseaux trophiques, notamment la stimulation de l'activité microbiologique aux dépens des chaînes trophiques longues dominées par les macro-organismes. Au large de la côte est de Belgique, la dominance des nématodes bactérivores, la quasi-absence des prédateurs, la très faible diversité spécifique des communautés de ce groupe et la pauvreté des métazoaires supérieurs peuvent trouver leur expl ication d'une part dans l'augmentation de l'apport en nutriments et d'autre part dans la grande quantité de po llution diffuse.","publication_date":{"day":null,"month":null,"year":1990,"errors":{}},"publication_name":"Netherlands Journal of Sea Research","grobid_abstract_attachment_id":97942103},"translated_abstract":null,"internal_url":"https://www.academia.edu/95887000/Diversity_of_the_nematode_communities_in_the_Southern_Bight_of_the_North_Sea","translated_internal_url":"","created_at":"2023-01-29T00:36:08.199-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":184662190,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":97942103,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942103/thumbnails/1.jpg","file_name":"286799.pdf","download_url":"https://www.academia.edu/attachments/97942103/download_file","bulk_download_file_name":"Diversity_of_the_nematode_communities_in.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942103/286799-libre.pdf?1674982304=\u0026response-content-disposition=attachment%3B+filename%3DDiversity_of_the_nematode_communities_in.pdf\u0026Expires=1743224695\u0026Signature=Jgb~CvNX2f~lurU4KFw-OlbU2CgZRO28CvMazP2huahtDlnWCSqy~3zcu5H6I8eGtM-Dlr6JNjz4Rg-PvDVRupzpsiyrXgID-SW3BCy~MGlwZlMnTZseLwTedJyyBowZIb2llpA3XTUB0ZYt9WtHX0eJui2qMP1bDYkbaTvtqRX1rKQWeIVP5fUJO8T~kOnIM0HY1Na2xOxscjr~--K8tsbt9cxP~soyOxC2Zqa1P86puGCBngjZqJoo9Pd7-LH-FQS~VAnKmeGZ4fTs2r47db8gEVYvYc37xu~oWYRjlUjJghG-wQ~xqGql8njkyHufpIaKkD6RrLLFTbWPKn5klg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Diversity_of_the_nematode_communities_in_the_Southern_Bight_of_the_North_Sea","translated_slug":"","page_count":23,"language":"en","content_type":"Work","summary":"The nematode communities from 102 stations in the Southern Bight of the North Sea, sumpled between 1972 and 1984, are exam ined. 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A general increase of the level of primary production in the coastal area , as a result of increasing nutrient input, does not necessarily lead to an increase of pelagie or demersal fish production, but cou Id induce a modification of the food web , in particular the enhancement of microbiological activity at the expense of long trophic chains dominated by macroorganisms. The near absence of nematode-predators in the reg ion off the Belgian east coast, the dom inance of bacterivores, the very low spec ies diversity of the nematode community and the paucity of higher metazoans within the area, can be partly explained on the basis of the increase in nutrient input within the area, and partly on the basis of the high amount of \"mixed\" pollution. Résumé: Identification des assemblages de nématodes de 102 stations de la partie sud de la mer du Nord où des prélèvements ont été effectués de 1972 il 1984 : 456 espèces ont été répertoriées, appartenant il 159 gen res et 37 familles. Interprétation des communautés par l'analyse des groupements d'espèces (coelficient de dissimilarité de Bray-Curtis et classification polythétique Twinspan) et par l'analyse factorielle des correspondances (DCA). Global ement, le bassin du sud de la mer du Nord peut être di visé en six zones principales définies par la composition spécifiq ue des nématodes. La structure sédimentaire apparaît comme le facte ur du milieu déterminant de la composition spécifique de la nématocoenose ; cependant, d'autres facteurs (température, salinité, ch lorophylle a, N03-, NH4+) semblent égaiement influer sur la distribution des espèces. L'importance du rôle des bactéries représente l'un des caractères les plus remarq uables des écosystèmes côtiers et, en particulier, de celui de la côte belge. Dans cette région, un accroissement du taux de production primaire, lié il une intensification de l'apport de nutriments, n'entraîne pas nécessairement l'augmentation de la production en poissons pélagiques ou démersaux ; mais il pourrait provoquer des modifications des réseaux trophiques, notamment la stimulation de l'activité microbiologique aux dépens des chaînes trophiques longues dominées par les macro-organismes. 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The water quality of a river is the result of complex anthropogenic systems (buildings, waste water treatment infrastructure, regulations, etc.) and biogeochemical and eco-hydrological interactions. It is therefore essential to obtain more insight in the factors that determine the water quality in a river. Research into the relation between land use and water quality is necessary. Human activities have a huge impact on the flow regimes and associated water quality of river systems. Effects of land use bound activities on water quality are often investigated, but these studies generally ignore the hydrological complexity of a human influenced catchment. Infrastructure like sewer systems and wastewater treatment plants (WWTP) can displace huge quantities of polluted water. The transfers change flow paths, displace water...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="27297acdadd9a1260d1ea03e85df413f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942101,&quot;asset_id&quot;:95886999,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942101/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95886999"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95886999"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95886999; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95886999]").text(description); $(".js-view-count[data-work-id=95886999]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95886999; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95886999']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "27297acdadd9a1260d1ea03e85df413f" } } $('.js-work-strip[data-work-id=95886999]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95886999,"title":"The effects of sewer infrastructure on water quality: implications for land use studies","translated_title":"","metadata":{"abstract":"The European Water Framework Directive requires a good ecological status of the European water bodies and the necessary measures to obtain this have to be implemented. The water quality of a river is the result of complex anthropogenic systems (buildings, waste water treatment infrastructure, regulations, etc.) and biogeochemical and eco-hydrological interactions. It is therefore essential to obtain more insight in the factors that determine the water quality in a river. Research into the relation between land use and water quality is necessary. Human activities have a huge impact on the flow regimes and associated water quality of river systems. Effects of land use bound activities on water quality are often investigated, but these studies generally ignore the hydrological complexity of a human influenced catchment. Infrastructure like sewer systems and wastewater treatment plants (WWTP) can displace huge quantities of polluted water. The transfers change flow paths, displace water...","publication_date":{"day":null,"month":null,"year":2010,"errors":{}}},"translated_abstract":"The European Water Framework Directive requires a good ecological status of the European water bodies and the necessary measures to obtain this have to be implemented. The water quality of a river is the result of complex anthropogenic systems (buildings, waste water treatment infrastructure, regulations, etc.) and biogeochemical and eco-hydrological interactions. It is therefore essential to obtain more insight in the factors that determine the water quality in a river. Research into the relation between land use and water quality is necessary. Human activities have a huge impact on the flow regimes and associated water quality of river systems. Effects of land use bound activities on water quality are often investigated, but these studies generally ignore the hydrological complexity of a human influenced catchment. Infrastructure like sewer systems and wastewater treatment plants (WWTP) can displace huge quantities of polluted water. 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Kris Van Looy a , Corresponding Author Contact Information , E-mail The Corresponding Author ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">... Kris Van Looy a , Corresponding Author Contact Information , E-mail The Corresponding Author , E-mail The Corresponding Author and Patrick ... their distribution patterns, more has to be known about their population biology and dynamics (Burkart, 2001; Lowe, 2002; Malanson ...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95886998"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95886998"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95886998; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95886998]").text(description); $(".js-view-count[data-work-id=95886998]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95886998; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95886998']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=95886998]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95886998,"title":"A conservation paradox for riparian habitats and river corridor species","translated_title":"","metadata":{"abstract":"... Kris Van Looy a , Corresponding Author Contact Information , E-mail The Corresponding Author , E-mail The Corresponding Author and Patrick ... their distribution patterns, more has to be known about their population biology and dynamics (Burkart, 2001; Lowe, 2002; Malanson ...","publisher":"Elsevier BV","publication_date":{"day":null,"month":null,"year":2009,"errors":{}},"publication_name":"Journal for Nature Conservation"},"translated_abstract":"... 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Kris Van Looy a , Corresponding Author Contact Information , E-mail The Corresponding Author , E-mail The Corresponding Author and Patrick ... their distribution patterns, more has to be known about their population biology and dynamics (Burkart, 2001; Lowe, 2002; Malanson ...","owner":{"id":184662190,"first_name":"Patrick","middle_initials":null,"last_name":"Meire","page_name":"MeireP","domain_name":"independent","created_at":"2021-02-03T07:39:55.559-08:00","display_name":"Patrick Meire","url":"https://independent.academia.edu/MeireP"},"attachments":[],"research_interests":[{"id":261,"name":"Geography","url":"https://www.academia.edu/Documents/in/Geography"},{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":7710,"name":"Biology","url":"https://www.academia.edu/Documents/in/Biology"},{"id":9846,"name":"Ecology","url":"https://www.academia.edu/Documents/in/Ecology"},{"id":28235,"name":"Multidisciplinary","url":"https://www.academia.edu/Documents/in/Multidisciplinary"},{"id":85707,"name":"Habitat","url":"https://www.academia.edu/Documents/in/Habitat"},{"id":86882,"name":"Rare species","url":"https://www.academia.edu/Documents/in/Rare_species"},{"id":124470,"name":"Bank","url":"https://www.academia.edu/Documents/in/Bank"},{"id":152553,"name":"Comparative Analysis","url":"https://www.academia.edu/Documents/in/Comparative_Analysis"},{"id":163827,"name":"Floodplain","url":"https://www.academia.edu/Documents/in/Floodplain"},{"id":174975,"name":"Habitat fragmentation","url":"https://www.academia.edu/Documents/in/Habitat_fragmentation"},{"id":586072,"name":"Plant species","url":"https://www.academia.edu/Documents/in/Plant_species"},{"id":1002371,"name":"Riparian Habitat","url":"https://www.academia.edu/Documents/in/Riparian_Habitat"},{"id":1565270,"name":"Art for Nature and Wildlife Conservation","url":"https://www.academia.edu/Documents/in/Art_for_Nature_and_Wildlife_Conservation"}],"urls":[{"id":28485829,"url":"https://api.elsevier.com/content/article/PII:S1617138108000605?httpAccept=text/xml"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95886998-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95886997"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/95886997/Variability_in_stock_assessment_of_cockles_Cerastoderma_edule_L_in_the_Oosterschelde_in_1980_1990_in_relation_to_environmental_factors"><img alt="Research paper thumbnail of Variability in stock assessment of cockles (Cerastoderma edule L.) in the Oosterschelde (in 1980–1990), in relation to environmental factors" class="work-thumbnail" src="https://attachments.academia-assets.com/97942100/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95886997/Variability_in_stock_assessment_of_cockles_Cerastoderma_edule_L_in_the_Oosterschelde_in_1980_1990_in_relation_to_environmental_factors">Variability in stock assessment of cockles (Cerastoderma edule L.) in the Oosterschelde (in 1980–1990), in relation to environmental factors</a></div><div class="wp-workCard_item"><span>Hydrobiologia</span><span>, 1994</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The edible cockle (Cerastoderma edule L.) is a dominant suspension feeder in the Oosterschelde, a...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The edible cockle (Cerastoderma edule L.) is a dominant suspension feeder in the Oosterschelde, a 351 km 2 tidal bay in the SW Netherlands. To establish its role in the benthic foodweb, and to assess the impact of human activities, data on density, age composition, biomass and growth were collected from several tidal flats in the Oosterschelde between 1980 and 1990. To estimate the overall biomass development of the cockle, a simple model was used, in which three growing seasons are defined for the cockle population. A standard individual growth curve was constructed. A negative exponential mortality function was assumed to estimate the number of recruits. By combining the estimated number of recruits, the estimated specific mortality rate and the standard individual growth curve, numbers and biomass of each age group in the Oosterschelde population were estimated. Average biomass (including shell organics) per m 2 of tidal flat in August varied from 140 g AFDW in 1980 to 21 g AFDW in 1989, implying a total cockle stock on all tidal flats of 19170 to 2350 tonnes AFDW (72 x 10 3 to 9 X 10 3 tonnes flesh), respectively. A comparison of results from field surveys and the reconstructed stock estimations showed large deviations. However, an uncertainty analysis performed on the model showed that most field data fitted within the minimum and maximum biomass calculated. Total biomass is largely dependent on the strength of certain year classes. In this respect, the year classes 1979, 1982, and 1985 were good. Effects of the construction of the storm-surge barrier and the compartmentalisation dams could not be demonstrated. The year-to-year variation in cockle stocks, assessed in the way described in this paper should be regarded as relative, because a systematic survey of the intertidal flats was not performed every year, but population dynamics from selected stations were used instead.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="9a770ccdab6f79ff307a29c449d78b84" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942100,&quot;asset_id&quot;:95886997,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942100/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95886997"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95886997"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95886997; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95886997]").text(description); $(".js-view-count[data-work-id=95886997]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95886997; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95886997']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "9a770ccdab6f79ff307a29c449d78b84" } } $('.js-work-strip[data-work-id=95886997]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95886997,"title":"Variability in stock assessment of cockles (Cerastoderma edule L.) in the Oosterschelde (in 1980–1990), in relation to environmental factors","translated_title":"","metadata":{"publisher":"Springer Nature","grobid_abstract":"The edible cockle (Cerastoderma edule L.) is a dominant suspension feeder in the Oosterschelde, a 351 km 2 tidal bay in the SW Netherlands. 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A comparison of results from field surveys and the reconstructed stock estimations showed large deviations. However, an uncertainty analysis performed on the model showed that most field data fitted within the minimum and maximum biomass calculated. Total biomass is largely dependent on the strength of certain year classes. In this respect, the year classes 1979, 1982, and 1985 were good. Effects of the construction of the storm-surge barrier and the compartmentalisation dams could not be demonstrated. The year-to-year variation in cockle stocks, assessed in the way described in this paper should be regarded as relative, because a systematic survey of the intertidal flats was not performed every year, but population dynamics from selected stations were used instead.","publication_date":{"day":null,"month":null,"year":1994,"errors":{}},"publication_name":"Hydrobiologia","grobid_abstract_attachment_id":97942100},"translated_abstract":null,"internal_url":"https://www.academia.edu/95886997/Variability_in_stock_assessment_of_cockles_Cerastoderma_edule_L_in_the_Oosterschelde_in_1980_1990_in_relation_to_environmental_factors","translated_internal_url":"","created_at":"2023-01-29T00:36:07.780-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":184662190,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":97942100,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942100/thumbnails/1.jpg","file_name":"978-94-011-1174-4_28.pdf","download_url":"https://www.academia.edu/attachments/97942100/download_file","bulk_download_file_name":"Variability_in_stock_assessment_of_cockl.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942100/978-94-011-1174-4_28-libre.pdf?1674982284=\u0026response-content-disposition=attachment%3B+filename%3DVariability_in_stock_assessment_of_cockl.pdf\u0026Expires=1743224695\u0026Signature=dxJJ74~I1rRw2Y6gqZPKlRW3mDGhCRVFx6yNLCzamRQssuj6bdbPd~kCbYG8mxmdPsvGkvn1uti~~EnssmDnyFO~UTEMtt2gXzzzwfOgddCAutgfN7xyQRaii2rhbQt-41iswsfGi2Vsq1y7aRE-eWdQQLuLCHHoCbWHPLGR7pJ~QF4-NnUgEoiTbbUdF3CXAOzRcWq938fE8hTgPwW9d64Mxg0cEA5fQvOfCvn1fwMkkQLxV9AeCuWVCGW60ldoEK7ZdMc~Zw5adXTQl4wdRwl5qMBZa2B3D7fffXIgBqr3hwhoW4HXZkLtXW6RW8Rl8meTTO6NIyfdtBvSB1UiKw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Variability_in_stock_assessment_of_cockles_Cerastoderma_edule_L_in_the_Oosterschelde_in_1980_1990_in_relation_to_environmental_factors","translated_slug":"","page_count":15,"language":"en","content_type":"Work","summary":"The edible cockle (Cerastoderma edule L.) is a dominant suspension feeder in the Oosterschelde, a 351 km 2 tidal bay in the SW Netherlands. To establish its role in the benthic foodweb, and to assess the impact of human activities, data on density, age composition, biomass and growth were collected from several tidal flats in the Oosterschelde between 1980 and 1990. To estimate the overall biomass development of the cockle, a simple model was used, in which three growing seasons are defined for the cockle population. A standard individual growth curve was constructed. A negative exponential mortality function was assumed to estimate the number of recruits. By combining the estimated number of recruits, the estimated specific mortality rate and the standard individual growth curve, numbers and biomass of each age group in the Oosterschelde population were estimated. Average biomass (including shell organics) per m 2 of tidal flat in August varied from 140 g AFDW in 1980 to 21 g AFDW in 1989, implying a total cockle stock on all tidal flats of 19170 to 2350 tonnes AFDW (72 x 10 3 to 9 X 10 3 tonnes flesh), respectively. A comparison of results from field surveys and the reconstructed stock estimations showed large deviations. However, an uncertainty analysis performed on the model showed that most field data fitted within the minimum and maximum biomass calculated. Total biomass is largely dependent on the strength of certain year classes. In this respect, the year classes 1979, 1982, and 1985 were good. Effects of the construction of the storm-surge barrier and the compartmentalisation dams could not be demonstrated. The year-to-year variation in cockle stocks, assessed in the way described in this paper should be regarded as relative, because a systematic survey of the intertidal flats was not performed every year, but population dynamics from selected stations were used instead.","owner":{"id":184662190,"first_name":"Patrick","middle_initials":null,"last_name":"Meire","page_name":"MeireP","domain_name":"independent","created_at":"2021-02-03T07:39:55.559-08:00","display_name":"Patrick Meire","url":"https://independent.academia.edu/MeireP"},"attachments":[{"id":97942100,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942100/thumbnails/1.jpg","file_name":"978-94-011-1174-4_28.pdf","download_url":"https://www.academia.edu/attachments/97942100/download_file","bulk_download_file_name":"Variability_in_stock_assessment_of_cockl.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942100/978-94-011-1174-4_28-libre.pdf?1674982284=\u0026response-content-disposition=attachment%3B+filename%3DVariability_in_stock_assessment_of_cockl.pdf\u0026Expires=1743224695\u0026Signature=dxJJ74~I1rRw2Y6gqZPKlRW3mDGhCRVFx6yNLCzamRQssuj6bdbPd~kCbYG8mxmdPsvGkvn1uti~~EnssmDnyFO~UTEMtt2gXzzzwfOgddCAutgfN7xyQRaii2rhbQt-41iswsfGi2Vsq1y7aRE-eWdQQLuLCHHoCbWHPLGR7pJ~QF4-NnUgEoiTbbUdF3CXAOzRcWq938fE8hTgPwW9d64Mxg0cEA5fQvOfCvn1fwMkkQLxV9AeCuWVCGW60ldoEK7ZdMc~Zw5adXTQl4wdRwl5qMBZa2B3D7fffXIgBqr3hwhoW4HXZkLtXW6RW8Rl8meTTO6NIyfdtBvSB1UiKw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":7710,"name":"Biology","url":"https://www.academia.edu/Documents/in/Biology"},{"id":9846,"name":"Ecology","url":"https://www.academia.edu/Documents/in/Ecology"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences"},{"id":100077,"name":"Stock assessment","url":"https://www.academia.edu/Documents/in/Stock_assessment"},{"id":213948,"name":"General Science","url":"https://www.academia.edu/Documents/in/General_Science"},{"id":509556,"name":"Human Activity","url":"https://www.academia.edu/Documents/in/Human_Activity"},{"id":580672,"name":"Tidal Flat","url":"https://www.academia.edu/Documents/in/Tidal_Flat"},{"id":1443257,"name":"Cockle","url":"https://www.academia.edu/Documents/in/Cockle"},{"id":1582364,"name":"Growth Curve","url":"https://www.academia.edu/Documents/in/Growth_Curve"},{"id":1660649,"name":"Bay","url":"https://www.academia.edu/Documents/in/Bay"},{"id":3807870,"name":"Environmental factor","url":"https://www.academia.edu/Documents/in/Environmental_factor"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95886997-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95886996"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/95886996/Effect_of_sedimentological_and_hydrodynamical_changes_in_the_intertidal_areas_of_the_Oosterschelde_estuary_SW_Netherlands_on_distribution_density_and_biomass_of_five_common_macrobenthic_species_Spio_martinensis_Mesnil_Hydrobia_ulvae_Pennant_Arenicola_marina_L_Scoloplos_armiger_Mull_"><img alt="Research paper thumbnail of Effect of sedimentological and hydrodynamical changes in the intertidal areas of the Oosterschelde estuary (SW Netherlands) on distribution, density and biomass of five common macrobenthic species: Spio martinensis (Mesnil), Hydrobia ulvae (Pennant), Arenicola marina (L.), Scoloplos armiger (Mull..." class="work-thumbnail" src="https://attachments.academia-assets.com/97942102/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95886996/Effect_of_sedimentological_and_hydrodynamical_changes_in_the_intertidal_areas_of_the_Oosterschelde_estuary_SW_Netherlands_on_distribution_density_and_biomass_of_five_common_macrobenthic_species_Spio_martinensis_Mesnil_Hydrobia_ulvae_Pennant_Arenicola_marina_L_Scoloplos_armiger_Mull_">Effect of sedimentological and hydrodynamical changes in the intertidal areas of the Oosterschelde estuary (SW Netherlands) on distribution, density and biomass of five common macrobenthic species: Spio martinensis (Mesnil), Hydrobia ulvae (Pennant), Arenicola marina (L.), Scoloplos armiger (Mull...</a></div><div class="wp-workCard_item"><span>Hydrobiologia</span><span>, 1994</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In order to evaluate the impact of the construction of the storm-surge barrier and secondary dams...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">In order to evaluate the impact of the construction of the storm-surge barrier and secondary dams on macrobenthos of the tidal flats in the Oosterschelde (SW Netherlands), changes in distribution, density and biomass of five common species (Spin martinensis, Hydrobia ulvae, Arenicola marina, Scoloplos armiger and Bathyporeia sp) were analysed. Data on macrobenthos were collected from 1979 to 1989 on five different tidal flats. Changes in sediment texture and hydrodynamic factors during the construction and after the completion of the coastal engineering project were taken into account. Three severe winters in a row caused more disturbance in the population of the main predator of S. armiger than did the hydrodynamical changes. A temporary prolongation of the emersion time (in 1986 and 1987) caused a temporary decrease in juvenile A. marina. But afterwards they still occupy the samè nursery grounds&#39;. Increased wave action on the edges of the flats probably created new niches for Bathyporeia sp. and Spio martinensis, replacing other benthic species. It is not yet clear what has caused the decline of H. ulvae in many places in the Oosterschelde estuary. Parasitic infestation is one of the possibilities .</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c73884cda43af178be4f6316fd1aaca2" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942102,&quot;asset_id&quot;:95886996,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942102/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95886996"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95886996"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95886996; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95886996]").text(description); $(".js-view-count[data-work-id=95886996]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95886996; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95886996']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "c73884cda43af178be4f6316fd1aaca2" } } $('.js-work-strip[data-work-id=95886996]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95886996,"title":"Effect of sedimentological and hydrodynamical changes in the intertidal areas of the Oosterschelde estuary (SW Netherlands) on distribution, density and biomass of five common macrobenthic species: Spio martinensis (Mesnil), Hydrobia ulvae (Pennant), Arenicola marina (L.), Scoloplos armiger (Mull...","translated_title":"","metadata":{"publisher":"Springer Science and Business Media LLC","grobid_abstract":"In order to evaluate the impact of the construction of the storm-surge barrier and secondary dams on macrobenthos of the tidal flats in the Oosterschelde (SW Netherlands), changes in distribution, density and biomass of five common species (Spin martinensis, Hydrobia ulvae, Arenicola marina, Scoloplos armiger and Bathyporeia sp) were analysed. Data on macrobenthos were collected from 1979 to 1989 on five different tidal flats. Changes in sediment texture and hydrodynamic factors during the construction and after the completion of the coastal engineering project were taken into account. Three severe winters in a row caused more disturbance in the population of the main predator of S. armiger than did the hydrodynamical changes. A temporary prolongation of the emersion time (in 1986 and 1987) caused a temporary decrease in juvenile A. marina. But afterwards they still occupy the samè nursery grounds'. Increased wave action on the edges of the flats probably created new niches for Bathyporeia sp. and Spio martinensis, replacing other benthic species. It is not yet clear what has caused the decline of H. ulvae in many places in the Oosterschelde estuary. Parasitic infestation is one of the possibilities .","publication_date":{"day":null,"month":null,"year":1994,"errors":{}},"publication_name":"Hydrobiologia","grobid_abstract_attachment_id":97942102},"translated_abstract":null,"internal_url":"https://www.academia.edu/95886996/Effect_of_sedimentological_and_hydrodynamical_changes_in_the_intertidal_areas_of_the_Oosterschelde_estuary_SW_Netherlands_on_distribution_density_and_biomass_of_five_common_macrobenthic_species_Spio_martinensis_Mesnil_Hydrobia_ulvae_Pennant_Arenicola_marina_L_Scoloplos_armiger_Mull_","translated_internal_url":"","created_at":"2023-01-29T00:36:07.638-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":184662190,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":97942102,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942102/thumbnails/1.jpg","file_name":"250441.pdf","download_url":"https://www.academia.edu/attachments/97942102/download_file","bulk_download_file_name":"Effect_of_sedimentological_and_hydrodyna.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942102/250441-libre.pdf?1674982259=\u0026response-content-disposition=attachment%3B+filename%3DEffect_of_sedimentological_and_hydrodyna.pdf\u0026Expires=1743224695\u0026Signature=Qlh44chTRUyHq6BDsTaL-DXDskTLgENoRs8dq0O375FqythoWYI79Grdm4G3uTVfLd1gMqZN0hxYH6VlAzkmdbGj7ETs5K2aTXcPr~MgOlHFZuEWJxCg3jgIFYZ0NysgjmgFYvpK~8ZBfsDK5b8jpK8aADePzuI9hSoUPD7N2cK65enWDONHCeDYfOxT1c~K64JcFnr7aI9FYjg~zklKXVsS6lOP70jgip1jcPS8hngeJBLSI20LhN8jcB3dNOcmC0BVYa1NtkonjuNum90jAXPO4reXovHUKD1KzYfQFbAlek7ZZyzW626YDs0F2-OYoKvenbHdXwtRK7eamk5Hcw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Effect_of_sedimentological_and_hydrodynamical_changes_in_the_intertidal_areas_of_the_Oosterschelde_estuary_SW_Netherlands_on_distribution_density_and_biomass_of_five_common_macrobenthic_species_Spio_martinensis_Mesnil_Hydrobia_ulvae_Pennant_Arenicola_marina_L_Scoloplos_armiger_Mull_","translated_slug":"","page_count":15,"language":"en","content_type":"Work","summary":"In order to evaluate the impact of the construction of the storm-surge barrier and secondary dams on macrobenthos of the tidal flats in the Oosterschelde (SW Netherlands), changes in distribution, density and biomass of five common species (Spin martinensis, Hydrobia ulvae, Arenicola marina, Scoloplos armiger and Bathyporeia sp) were analysed. Data on macrobenthos were collected from 1979 to 1989 on five different tidal flats. Changes in sediment texture and hydrodynamic factors during the construction and after the completion of the coastal engineering project were taken into account. Three severe winters in a row caused more disturbance in the population of the main predator of S. armiger than did the hydrodynamical changes. A temporary prolongation of the emersion time (in 1986 and 1987) caused a temporary decrease in juvenile A. marina. But afterwards they still occupy the samè nursery grounds'. Increased wave action on the edges of the flats probably created new niches for Bathyporeia sp. and Spio martinensis, replacing other benthic species. It is not yet clear what has caused the decline of H. ulvae in many places in the Oosterschelde estuary. Parasitic infestation is one of the possibilities .","owner":{"id":184662190,"first_name":"Patrick","middle_initials":null,"last_name":"Meire","page_name":"MeireP","domain_name":"independent","created_at":"2021-02-03T07:39:55.559-08:00","display_name":"Patrick Meire","url":"https://independent.academia.edu/MeireP"},"attachments":[{"id":97942102,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942102/thumbnails/1.jpg","file_name":"250441.pdf","download_url":"https://www.academia.edu/attachments/97942102/download_file","bulk_download_file_name":"Effect_of_sedimentological_and_hydrodyna.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942102/250441-libre.pdf?1674982259=\u0026response-content-disposition=attachment%3B+filename%3DEffect_of_sedimentological_and_hydrodyna.pdf\u0026Expires=1743224695\u0026Signature=Qlh44chTRUyHq6BDsTaL-DXDskTLgENoRs8dq0O375FqythoWYI79Grdm4G3uTVfLd1gMqZN0hxYH6VlAzkmdbGj7ETs5K2aTXcPr~MgOlHFZuEWJxCg3jgIFYZ0NysgjmgFYvpK~8ZBfsDK5b8jpK8aADePzuI9hSoUPD7N2cK65enWDONHCeDYfOxT1c~K64JcFnr7aI9FYjg~zklKXVsS6lOP70jgip1jcPS8hngeJBLSI20LhN8jcB3dNOcmC0BVYa1NtkonjuNum90jAXPO4reXovHUKD1KzYfQFbAlek7ZZyzW626YDs0F2-OYoKvenbHdXwtRK7eamk5Hcw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":415,"name":"Oceanography","url":"https://www.academia.edu/Documents/in/Oceanography"},{"id":9846,"name":"Ecology","url":"https://www.academia.edu/Documents/in/Ecology"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences"},{"id":162645,"name":"Population Density","url":"https://www.academia.edu/Documents/in/Population_Density"},{"id":379570,"name":"Estuary","url":"https://www.academia.edu/Documents/in/Estuary"},{"id":398869,"name":"Intertidal Zone","url":"https://www.academia.edu/Documents/in/Intertidal_Zone"},{"id":556983,"name":"Storm surge","url":"https://www.academia.edu/Documents/in/Storm_surge"},{"id":580672,"name":"Tidal Flat","url":"https://www.academia.edu/Documents/in/Tidal_Flat"},{"id":581940,"name":"Macrobenthos","url":"https://www.academia.edu/Documents/in/Macrobenthos"},{"id":1237825,"name":"Population dynamic","url":"https://www.academia.edu/Documents/in/Population_dynamic"},{"id":1443257,"name":"Cockle","url":"https://www.academia.edu/Documents/in/Cockle"}],"urls":[{"id":28485828,"url":"http://link.springer.com/content/pdf/10.1007/BF00024633.pdf"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95886996-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95886995"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/95886995/Tracing_Si_N_P_ecosystem_pathways_is_relative_uptake_in_riparian_vegetation_influenced_by_soil_waterlogging_mowing_management_and_species_diversity"><img alt="Research paper thumbnail of Tracing Si–N–P ecosystem-pathways: is relative uptake in riparian vegetation influenced by soil waterlogging, mowing management and species diversity?" class="work-thumbnail" src="https://attachments.academia-assets.com/97942105/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95886995/Tracing_Si_N_P_ecosystem_pathways_is_relative_uptake_in_riparian_vegetation_influenced_by_soil_waterlogging_mowing_management_and_species_diversity">Tracing Si–N–P ecosystem-pathways: is relative uptake in riparian vegetation influenced by soil waterlogging, mowing management and species diversity?</a></div><div class="wp-workCard_item"><span>Hydrobiologia</span><span>, 2011</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Despite the growing concern about the importance of silicon (Si) in controlling ecological proces...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Despite the growing concern about the importance of silicon (Si) in controlling ecological processes in aquatic ecosystems, little is known about its processing in riparian vegetation, especially compared to nitrogen (N) and phosphorus (P). We present experimental evidence that relative plant uptake of N and P compared to Si in riparian vegetation is dependent on mowing practices, water-logging and species composition. Results are obtained from a controlled and replicated mesocosm experiment, with a full-factorial design of soil water logging and mowing management. In our experiments, the Si excluding species Plantago lanceolata was dominant in the mown and non-waterlogged treatments, while Si accumulating meadow grasses and Phalaris arundinacea dominated the waterlogged treatments. Although species composition, management and soil moisture interacted strongly in their effect on relative Si:N and Si:P uptake ratios, the uptake of N to P remained virtually unchanged over the different treatments. Our study sheds new light on the impact of riparian wetland ecosystems on nutrient transport to rivers. It indicates that it is essential to include Si in future studies of the impact of riparian vegetation on nutrient transport, as these are often implemented as a measure to moderate excessive N and P inputs.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="73e5ce0fd115dee024a90293657320f8" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942105,&quot;asset_id&quot;:95886995,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942105/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95886995"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95886995"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95886995; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95886995]").text(description); $(".js-view-count[data-work-id=95886995]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95886995; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95886995']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "73e5ce0fd115dee024a90293657320f8" } } $('.js-work-strip[data-work-id=95886995]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95886995,"title":"Tracing Si–N–P ecosystem-pathways: is relative uptake in riparian vegetation influenced by soil waterlogging, mowing management and species diversity?","translated_title":"","metadata":{"publisher":"Springer Nature","grobid_abstract":"Despite the growing concern about the importance of silicon (Si) in controlling ecological processes in aquatic ecosystems, little is known about its processing in riparian vegetation, especially compared to nitrogen (N) and phosphorus (P). We present experimental evidence that relative plant uptake of N and P compared to Si in riparian vegetation is dependent on mowing practices, water-logging and species composition. Results are obtained from a controlled and replicated mesocosm experiment, with a full-factorial design of soil water logging and mowing management. In our experiments, the Si excluding species Plantago lanceolata was dominant in the mown and non-waterlogged treatments, while Si accumulating meadow grasses and Phalaris arundinacea dominated the waterlogged treatments. Although species composition, management and soil moisture interacted strongly in their effect on relative Si:N and Si:P uptake ratios, the uptake of N to P remained virtually unchanged over the different treatments. Our study sheds new light on the impact of riparian wetland ecosystems on nutrient transport to rivers. It indicates that it is essential to include Si in future studies of the impact of riparian vegetation on nutrient transport, as these are often implemented as a measure to moderate excessive N and P inputs.","publication_date":{"day":null,"month":null,"year":2011,"errors":{}},"publication_name":"Hydrobiologia","grobid_abstract_attachment_id":97942105},"translated_abstract":null,"internal_url":"https://www.academia.edu/95886995/Tracing_Si_N_P_ecosystem_pathways_is_relative_uptake_in_riparian_vegetation_influenced_by_soil_waterlogging_mowing_management_and_species_diversity","translated_internal_url":"","created_at":"2023-01-29T00:36:07.536-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":184662190,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":97942105,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942105/thumbnails/1.jpg","file_name":"d953772c.pdf","download_url":"https://www.academia.edu/attachments/97942105/download_file","bulk_download_file_name":"Tracing_Si_N_P_ecosystem_pathways_is_rel.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942105/d953772c-libre.pdf?1674982256=\u0026response-content-disposition=attachment%3B+filename%3DTracing_Si_N_P_ecosystem_pathways_is_rel.pdf\u0026Expires=1743224695\u0026Signature=XjPoj7UaCKEA-4GHaZe~LqytV74wIGzx5N5E~kUnM9zh7WC36LKkfzcQl77DQN0xgmlzvZ1RT70e-TQU4nHxmLOsBhx3xhQ72UzlwAPejtiMbH0Z4Pn~e1sW-Kqr5z37HfIj5VxSQlpflkbZyt30eeAEpnnhsTpgU5NELqOBU3AJ~11ZWWvOPGH3r4XagPewLd-xsJC61Klnsf8g4MY-EqPftia558tzEULyB1Do2FBiiKAfhWaTpqVY~B-0ffzrHYQyJFxKNC-fxdpPIW7jrm38GpOMwcG~0ZRAgZJohy85gApq3SCMbu70~LvFy8voKSo-QaxT0K-9BufvjdfYFg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Tracing_Si_N_P_ecosystem_pathways_is_relative_uptake_in_riparian_vegetation_influenced_by_soil_waterlogging_mowing_management_and_species_diversity","translated_slug":"","page_count":10,"language":"en","content_type":"Work","summary":"Despite the growing concern about the importance of silicon (Si) in controlling ecological processes in aquatic ecosystems, little is known about its processing in riparian vegetation, especially compared to nitrogen (N) and phosphorus (P). We present experimental evidence that relative plant uptake of N and P compared to Si in riparian vegetation is dependent on mowing practices, water-logging and species composition. Results are obtained from a controlled and replicated mesocosm experiment, with a full-factorial design of soil water logging and mowing management. In our experiments, the Si excluding species Plantago lanceolata was dominant in the mown and non-waterlogged treatments, while Si accumulating meadow grasses and Phalaris arundinacea dominated the waterlogged treatments. Although species composition, management and soil moisture interacted strongly in their effect on relative Si:N and Si:P uptake ratios, the uptake of N to P remained virtually unchanged over the different treatments. Our study sheds new light on the impact of riparian wetland ecosystems on nutrient transport to rivers. It indicates that it is essential to include Si in future studies of the impact of riparian vegetation on nutrient transport, as these are often implemented as a measure to moderate excessive N and P inputs.","owner":{"id":184662190,"first_name":"Patrick","middle_initials":null,"last_name":"Meire","page_name":"MeireP","domain_name":"independent","created_at":"2021-02-03T07:39:55.559-08:00","display_name":"Patrick Meire","url":"https://independent.academia.edu/MeireP"},"attachments":[{"id":97942105,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/97942105/thumbnails/1.jpg","file_name":"d953772c.pdf","download_url":"https://www.academia.edu/attachments/97942105/download_file","bulk_download_file_name":"Tracing_Si_N_P_ecosystem_pathways_is_rel.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/97942105/d953772c-libre.pdf?1674982256=\u0026response-content-disposition=attachment%3B+filename%3DTracing_Si_N_P_ecosystem_pathways_is_rel.pdf\u0026Expires=1743224695\u0026Signature=XjPoj7UaCKEA-4GHaZe~LqytV74wIGzx5N5E~kUnM9zh7WC36LKkfzcQl77DQN0xgmlzvZ1RT70e-TQU4nHxmLOsBhx3xhQ72UzlwAPejtiMbH0Z4Pn~e1sW-Kqr5z37HfIj5VxSQlpflkbZyt30eeAEpnnhsTpgU5NELqOBU3AJ~11ZWWvOPGH3r4XagPewLd-xsJC61Klnsf8g4MY-EqPftia558tzEULyB1Do2FBiiKAfhWaTpqVY~B-0ffzrHYQyJFxKNC-fxdpPIW7jrm38GpOMwcG~0ZRAgZJohy85gApq3SCMbu70~LvFy8voKSo-QaxT0K-9BufvjdfYFg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":7710,"name":"Biology","url":"https://www.academia.edu/Documents/in/Biology"},{"id":9846,"name":"Ecology","url":"https://www.academia.edu/Documents/in/Ecology"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences"},{"id":53108,"name":"Phosphorus","url":"https://www.academia.edu/Documents/in/Phosphorus"},{"id":53796,"name":"Aquatic Ecosystem","url":"https://www.academia.edu/Documents/in/Aquatic_Ecosystem"},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences"},{"id":83037,"name":"Soil moisture","url":"https://www.academia.edu/Documents/in/Soil_moisture"},{"id":107374,"name":"Factorial Design","url":"https://www.academia.edu/Documents/in/Factorial_Design"},{"id":151091,"name":"Nitrogen","url":"https://www.academia.edu/Documents/in/Nitrogen"},{"id":168668,"name":"Species Diversity","url":"https://www.academia.edu/Documents/in/Species_Diversity"},{"id":199046,"name":"Species Composition","url":"https://www.academia.edu/Documents/in/Species_Composition"},{"id":228848,"name":"Phalaris arundinacea","url":"https://www.academia.edu/Documents/in/Phalaris_arundinacea"},{"id":238233,"name":"Riparian vegetation","url":"https://www.academia.edu/Documents/in/Riparian_vegetation"},{"id":1016853,"name":"Plantago Lanceolata","url":"https://www.academia.edu/Documents/in/Plantago_Lanceolata"},{"id":1222799,"name":"Soil Water","url":"https://www.academia.edu/Documents/in/Soil_Water"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") if (false) { Aedu.setUpFigureCarousel('profile-work-95886995-figures'); } }); </script> <div class="js-work-strip profile--work_container" data-work-id="95886994"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/95886994/Freshwater_marshes_as_dissolved_silica_recyclers_in_an_estuarine_environment_Schelde_estuary_Belgium_"><img alt="Research paper thumbnail of Freshwater marshes as dissolved silica recyclers in an estuarine environment (Schelde estuary, Belgium)" class="work-thumbnail" src="https://attachments.academia-assets.com/97942112/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95886994/Freshwater_marshes_as_dissolved_silica_recyclers_in_an_estuarine_environment_Schelde_estuary_Belgium_">Freshwater marshes as dissolved silica recyclers in an estuarine environment (Schelde estuary, Belgium)</a></div><div class="wp-workCard_item"><span>Hydrobiologia</span><span>, 2005</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Compared to knowledge about N and P processing in the aquatic continuum of lakes, wetlands and es...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Compared to knowledge about N and P processing in the aquatic continuum of lakes, wetlands and estuaries, knowledge concerning transport and cycling of Si is only fragmentary. Furthermore, Si research in estuaries has mainly been focused on subtidal benthic sediments and uptake and recycling by diatom communities. The biogeochemical cycling of Si in tidal wetlands, which can contain large amounts of Si, has thus far been neglected. We have conducted several whole ecosystem Si mass-balances on a freshwater marsh located in the Schelde estuary (6 tidal cycles, 2 with BSi included). Our measurements show that the freshwater marsh acts as an important source of dissolved Si to the main river (1-18% more export than import, on average 0.114 g m)2). This export is compensated by import of amorphous silica into the marsh (19-55% more import than export). The marsh was shown to act as silica recycler, resupplying biologically available dissolved Si to the estuarine ecosystem. Extrapolations show that during summer and spring months, when dissolved silica is depleted due to diatom growth, almost half of the total dissolved silica load in the main river channel could result from marsh recycling.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b2f26e8e586f96dfa51c2231c953fae1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{&quot;attachment_id&quot;:97942112,&quot;asset_id&quot;:95886994,&quot;asset_type&quot;:&quot;Work&quot;,&quot;button_location&quot;:&quot;profile&quot;}" href="https://www.academia.edu/attachments/97942112/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95886994"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95886994"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95886994; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95886994]").text(description); $(".js-view-count[data-work-id=95886994]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95886994; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95886994']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "b2f26e8e586f96dfa51c2231c953fae1" } } $('.js-work-strip[data-work-id=95886994]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95886994,"title":"Freshwater marshes as dissolved silica recyclers in an estuarine environment (Schelde estuary, Belgium)","translated_title":"","metadata":{"publisher":"Springer Science and Business Media LLC","ai_title_tag":"Marshes as Dissolved Silica Recyclers in Estuaries","grobid_abstract":"Compared to knowledge about N and P processing in the aquatic continuum of lakes, wetlands and estuaries, knowledge concerning transport and cycling of Si is only fragmentary. Furthermore, Si research in estuaries has mainly been focused on subtidal benthic sediments and uptake and recycling by diatom communities. The biogeochemical cycling of Si in tidal wetlands, which can contain large amounts of Si, has thus far been neglected. We have conducted several whole ecosystem Si mass-balances on a freshwater marsh located in the Schelde estuary (6 tidal cycles, 2 with BSi included). Our measurements show that the freshwater marsh acts as an important source of dissolved Si to the main river (1-18% more export than import, on average 0.114 g m)2). This export is compensated by import of amorphous silica into the marsh (19-55% more import than export). The marsh was shown to act as silica recycler, resupplying biologically available dissolved Si to the estuarine ecosystem. 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