Philipsdam | |
---|---|
Coordinates | 51°39′41″N4°9′42″E / 51.66139°N 4.16167°E |
Carries | N257 |
Owner | Rijkswaterstaat |
Characteristics | |
Total length | 6.1 kilometres (3.8 mi) |
History | |
Architect | F.W. de Vlaming (locks and buildings) F.L. Halenbeek (Landscape) |
Engineering design by | Deltadienst |
Constructed by | Several contractors, including: Combinatie Zinkcon bv Aannemers Combinatie Zinkwerken bv J. Heijmans bv Baggermaatschappij 'Holland' bv. |
Construction start | 1976 |
Construction end | 1987 |
Location | |
The Philipsdam is a compartmentalisation dam constructed as part of the Delta Works in the Netherlands. It separates water of the lakes Krammer and Volkerak from the Oosterschelde, and connects the Grevelingendam to Sint Philipsland. [1]
In 1974, it was decided by Rijkswaterstaat and the Den Uyl cabinet to construct the Oosterscheldekering as a storm surge barrier at the mouth of the Oosterschelde, instead of completely closing off the tidal inlet at that location. The construction of the Oosterscheldekering required the compartmentalisation of the basin. [2]
The compartmentalisation model chosen involved the construction of the Philipsdam, the Oesterdam, and a discharge channel for managing the level and quality of the lake that would then form behind the dams. The overall project was also required to create a freshwater lake for water management purposes, ensure a tide-free navigation on the Scheldt-Rhine connection, and achieve a tidal difference of 2.7m at Yerseke. [2]
To prevent unacceptable flow velocities from being realised in the Scheldt-Rhine Canal during the works, the closing phases of both the Philipsdam and the Oesterdam had to be coordinated with each other. [3] A number of alternatives to the final location of the Philipsdam and the lock complex were investigated, with an important consideration being the preservation of valuable intertidal areas along with considerations of the closure method to be employed. [4] [5] [6]
The decision-making process for the nature and location of the Philipsdam involved a comprehensive consideration of multiple factors, leading to the selection of the variant at a sandbank known as Plaat van de Vliet as the preferred option. Key considerations included: [7] The connection of the damn to the Grevelingendam instead of the southern shore of Goeree-Overflakkee was chosen to allow for the option of turning the Grevelingenmeer into a freshwater basin by feeding it via a discharge sluice from the Krammer, which was ultimately decided against. [8] The benefit of this route is that it also removed the requirement for an additional road bridge across the Krammer instead connecting it to the existing road over the Grevelingendam. [8]
Waterway | Max. Ebb Speed (m/s) | Max. Ebb Volume (m³/s) | Max. Flood Speed (m/s) | Max. Flood Volume (m³/s) |
---|---|---|---|---|
Slaak | 0.9 | 2000 | 0.75 | 2000 |
Krammer | 1.05 | 11000 | 1.05 | 12500 |
The road connection on the south side of the dam required significant research during the design stage, as it runs through vulnerable nature reserves. [12]
Construction on the Philipsdam commenced in 1976, starting with the creation of a 96-hectare temporary work island on a sandbank known as Plaat van de Vliet. [9] [4] [13] [14]
Eighteen months after initiation, the island's construction concluded, paving the way for the commencement of the locks aimed at facilitating inland navigation and accommodating yachts. By 1983, the Krammer locks complex was completed, and the dam was officially inaugurated on February 2, 1987. A second lock for yachts was added in 1994. [10]
The Philipsdam functions as a dam, a fresh-salt water separator, and a lock system. It mitigates tidal influences within the Scheldt-Rhine connection, ensuring the Port of Antwerp remains accessible. To the dam's west lies saltwater, while to its east, freshwater flows from the Waal and Bergse Maas. [10]
On the dam's saltwater side, the Oosterschelde's water level is maintained, ensuring the conservation of salt marshes and mudflats vital for oyster farming. The freshwater side supports extensive vegetation due to its drier conditions. The inclusion of a lock complex facilitates the passage of ships, featuring an innovative system for fresh-salt water separation. [11] [9] [10]
In addition to the main road over the crest of the dam, there is a parallel road on its eastern side which was constructed to offer access to recreational zones. The dam's southern route was deliberately positioned as far west as possible from the Plaat van Vliet and Krammerse Slikken, maximising the recreational potential of these mudflats. Efforts were made to preserve the ecological and tidal areas of the Slaak (the region between the dam and the northern side of Sint Philipsland), whilst minimising the impact on agricultural land in Sint Philipsland. [10]
The locks are technically sophisticated because they must avoid the exchange between the freshwater Volkerak and the brackish water of the Oosterschelde. The locks are designed so that there is no influx of saltwater that enters the Volkerak and only a little fresh water in the Oosterschelde. The locks rely on the physical principle that saltwater is denser and sinks, while freshwater rises. By a complex system of pipes and pumps, the saltwater is pumped from the bottom, or conversely, freshwater is pumped from the top, depending on the direction of the ship. Locks on inland waterways are 280 metres long and 24 metres wide. [5]
The dam considerably changed the surrounding landscape. Shortly after closure, the water became fresh and the level in the Krammer-Volkerak was fixed at zero centimeters NAP (Amsterdam Ordnance Datum). As a result, nearly two thousand hectares of salt marshes, mudflats, and sandflats permanently dried out. Shoreline erosion was mitigated by constructing foreshores. In the 1990s, around forty islands were created that are of great importance for coastal breeding birds, meaning that the alluvial tidal marsh now supports rich animal life. An observation hut was installed to facilitate the observation of the many species of birds, such as the pied avocet. [10]
The Delta Works is a series of construction projects in the southwest of the Netherlands to protect a large area of land around the Rhine–Meuse–Scheldt delta from the sea. Constructed between 1954 and 1997, the works consist of dams, sluices, locks, dykes, levees, and storm surge barriers located in the provinces of South Holland and Zeeland.
The Eastern Scheldt is a former estuary in the province of Zeeland, Netherlands, between Schouwen-Duiveland and Tholen on the north and Noord-Beveland and Zuid-Beveland on the south. It also features the largest national park in the Netherlands, founded in 2002.
The Afsluitdijk is a major dam and causeway in the Netherlands. It was constructed between 1927 and 1932 and runs from Den Oever in North Holland province to the village of Zurich in Friesland province, over a length of 32 kilometres (20 mi) and a width of 90 metres (300 ft), at an initial height above Amsterdam Ordnance Datum of between 6.7 metres (22 ft) along the section at Friesland, and 7.4 metres (24 ft) where it crosses the deep channel of the Vlieter. The height at the greater sea depths west of Friesland was required to be a minimum of 7 metres everywhere when originally constructed.
The Haringvliet is a large inlet of the North Sea, in the province of South Holland in the Netherlands. It is an important estuary of the Rhine-Meuse delta.
The Scheldt–Rhine Canal (Schelde-Rijnkanaal) in Belgium and the Netherlands connects Antwerp with the Volkerak, and thereby the Scheldt with the Rhine.
The Oosterscheldekering, between the islands Schouwen-Duiveland and Noord-Beveland, is the largest of the Delta Works, a series of dams and storm surge barriers, designed to protect the Netherlands from flooding from the North Sea. The construction of the Delta Works was a response to the widespread damage and loss of life in the North Sea flood of 1953.
The Deltar was an analogue computer used in the design and execution of the Delta Works from 1960 to 1984. Originated by Johan van Veen, who also built the initial prototypes between 1944 and 1946, its development was continued by J.C. Schönfeld and C.M. Verhagen after van Veen's death in 1959.
The Krammer is a body of fresh water located in the western part of Volkerak in the Netherlands.
The Volkerak is a body of water in the Netherlands. It is part of the Rhine–Meuse–Scheldt delta, and is situated between the island Goeree-Overflakkee to the north-west and the Dutch mainland to the south and east. The western part of the Volkerak is also called Krammer. Tributaries of the Volkerak are the Dintel and Steenbergse Vliet.
The Oesterdam is a compartmentalisation dam in The Netherlands, situated between Tholen and South Beveland in the eastern part of the Eastern Scheldt. The dam, with a length of 10.5 kilometres, is the longest structure built for the Delta Works. The Oesterdam was necessitated, like the Philipsdam, after the decision was taken to close off the Eastern Scheldt with a storm surge barrier, rather than a solid dam.
The Markiezaatskade is a compartmentalisation dam in The Netherlands, situated between South Beveland and Molenplaat, near Bergen op Zoom. The dam was constructed as part of the Delta Works, and has a length of 4 kilometres.
The Volkerakdam or Volkerakwerken is the name given to a group of hydraulic engineering structures located between Goeree-Overflakkee and North Brabant in The Netherlands. The works are not a single dam, but are composed of three distinct structures: a dam between Goeree-Overflakkee and Hellegatsplein, a series of locks from Hellegatsplein to North Brabant, and a bridge from Hellegatsplein to Hoekse Waard. The works cross three separate bodies of water: the Haringvliet, Hollands Diep and Volkerak. The works together comprise the fifth project of the Delta Works.
The Grevelingendam is a dam located in the Grevelingen sea inlet between Schouwen-Duiveland and Goeree-Overflakkee in The Netherlands. The Grevelingendam was the fourth structure constructed as part of the Delta Works.
The Stormvloedkering Hollandse IJssel, Hollandse IJsselkering or Algerakering is a storm surge barrier located on the Hollandse IJssel, at the municipal boundary of Capelle aan den IJssel and Krimpen aan den IJssel, east of Rotterdam in The Netherlands. The construction of the works comprised the first project of the Delta Works, undertaken in response to the disastrous effects of the North Sea flood of 1953. Prior to 1954, the spelling Hollandsche was used in the official name.
The Zandkreekdam is a compartmentalisation dam located approximately 3 kilometres north of the city of Goes in The Netherlands, which connects Zuid-Beveland with Noord-Beveland, and separates the Oosterschelde from the Veerse Meer.
Frank Spaargaren was a Dutch hydraulic engineer who was one of the main designers of the Oosterscheldekering and served as a director of the Waterloopkundig Laboratorium in Delft.
Jan Fokke Agema was a Dutch hydraulic engineer and professor at Delft University of Technology. He is notable for his design of the harbour entrance at Hoek van Holland and involvement in the construction of the Oosterscheldekering. The prof. dr.ir. J.F. Agemaprijs is named for him, and has been awarded every five years since 2000.
A compartmentalisation dam is a dam that divides a body of water into two parts. A typical use of such a dam is the regulation of water levels separately in different sections of a basin. One application of a compartmentalisation dam is to facilitate closures of areas with multiple tidal inlets, such as in the case of the Delta Works.
In coastal and environmental engineering, the closure of tidal inlets entails the deliberate prevention of the entry of seawater into inland areas through the use of fill material and the construction of barriers. The aim of such closures is usually to safeguard inland regions from flooding, thereby protecting ecological integrity and reducing potential harm to human settlements and agricultural areas.
Information (in Dutch) about the Philipsdam From the Watersnoodmuseum Knowledge Centre website