Polder in-Betrieb.jpg on:
[Wikipedia]
[Google]
[Amazon]
A polder () is a low-lying tract of land that forms an artificial hydrology, hydrological entity, enclosed by embankments known as levee, dikes. The three types of polder are:
# Land reclamation, Land reclaimed from a body of water, such as a lake or the seabed
# Floodplain, Flood plains separated from the sea or river by a dike
# Marshes separated from the surrounding water by a dike and subsequently drained; these are also known as ''koogs'', especially in Germany
The ground level in drained marshes subsidence, subsides over time. All polders will eventually be below the surrounding water level some or all of the time. Water enters the low-lying polder through infiltration (hydrology), infiltration and water pressure of groundwater, or rainfall, or transport of water by rivers and canals. This usually means that the polder has an excess of water, which is pumped out or drained by opening sluices at low tide. Care must be taken not to set the internal water level too low. Polder land made up of peat (former marshland) will sink in relation to its previous level, because of peat decomposing when exposed to oxygen from the air.
Polders are at risk from flooding at all times, and care must be taken to protect the surrounding dikes. Dikes are typically built with locally available materials, and each material has its own risks: sand is prone to collapse owing to saturation by water; dry peat is lighter than water and potentially unable to retain water in very dry seasons. Some animals dig tunnels in the barrier, allowing water to infiltrate the structure; the muskrat is known for this activity and hunted in certain European countries because of it. Polders are most commonly, though not exclusively, found in river deltas, former fenlands, and coastal areas.
Flooding of polders has also been used as a military tactic in the past. One example is the flooding of the polders along the Yser River during World War I. Opening the sluices at high tide and closing them at low tide turned the polders into an inaccessible swamp, which allowed the Battle of the Yser#Battle, Allied armies to stop the German army.
Netherlands has a large area of polders: as much as 20% of the land area has at some point in the past been reclaimed from the sea, thus contributing to the development of the country. IJsselmeer is the most famous polder project of the Netherlands. Some other countries which have polders are Bangladesh, Belgium, Canada and China. Some examples of Dutch polder projects are Beemster, Schermer, Flevopolder and Noordoostpolder.
The Netherlands is frequently associated with polders, as its engineers became noted for developing techniques to drain wetlands and make them usable for agriculture and other development. This is illustrated by the saying "God created the world, but the Dutch created the Netherlands".
The Dutch people, Dutch have a long history of reclamation of marshes and fenland, resulting in some 3,000 ''polders'' nationwide. By 1961, about half of the country's land, , was reclaimed from the sea. About half the total surface area of ''polders'' in north-west Europe is in the Netherlands. The first embankment dam, embankments in Europe were constructed in Roman times. The first polders were constructed in the 11th century. The oldest extant polder is the Achtermeer polder, from 1533.
As a result of flooding disasters, Water board (The Netherlands), water boards called ''waterschap'' (when situated more inland) or ''hoogheemraadschap'' (near the sea, mainly used in the Holland region) were set up to maintain the integrity of the water defences around polders, maintain the waterways inside a polder, and control the various water levels inside and outside the polder. Water boards hold separate elections, levy taxes, and function independently from other government bodies. Their function is basically unchanged even today. As such, they are the oldest democratic institutions in the country. The necessary cooperation among all ranks to maintain polder integrity gave its name to the Dutch version of Third Way (centrism), third-way politics—the ''Polder Model''.
The North Sea flood of 1953, 1953 flood disaster prompted a new approach to the design of dikes and other water-retaining structures, based on an acceptable probability of overflowing. Risk is defined as the product of probability and consequences. The potential damage in lives, property, and rebuilding costs is compared with the potential cost of water defences. From these calculations follows an acceptable flood risk from the sea at one in 4,000–10,000 years, while it is one in 100–2,500 years for a river flood. The particular established policy guides the Dutch government to improve flood defences as new data on threat levels become available.
Major Dutch polders and the years they were laid dry include Beemster (1609–1612), Schermer (1633–1635), and Haarlemmermeerpolder (1852). Polders created as part of the Zuiderzee Works include Wieringermeerpolder (1930), Noordoostpolder (1942) and Flevopolder (1956–1968)
* De Moeren, near Veurne in West Flanders
* Polders along the Yser river between Nieuwpoort, Belgium, Nieuwpoort and Diksmuide
* Polders of Muisbroek and Ettenhoven, in Ekeren and Hoevenen
* Polder of Stabroek, in Stabroek
* Kabeljauwpolder, in Zandvliet
* Scheldepolders on the left bank of Scheldt, the Scheldt
* Uitkerkse polders, near Blankenberge in West Flanders
* Prosperpolder, near Doel, Antwerp and Kieldrecht.
In Germany, land reclaimed by diking is called a ''koog''. The German ''Deichgraf'' system was similar to the Dutch and is widely known from Theodor Storm's novella ''The Rider on the White Horse''.
* Altes Land near Hamburg
* Blockland, Bremen, Blockland and Hollerland near Bremen
* Nordstrand, Germany
* Bormerkoog and Meggerkoog near Friedrichstadt
* 36 ''koogs'' in the district of Nordfriesland
* 12 ''koogs'' in the district of Dithmarschen
In southern Germany, the term ''polder'' is used for retention basins recreated by opening dikes during river floodplain restoration, a meaning somewhat opposite to that in coastal context.
* Achtermeer, the oldest polder, from 1533
* Alblasserwaard, containing the windmills of Kinderdijk, a World Heritage Site
* Alkmaar
* Andijk
* Anna Paulownapolder
* Beemster, a World Heritage Site
* Bijlmermeer
* Flevopolder, the largest artificial island in the world, youngest polder, last part drained in 1968
* 's-Gravesloot
* Haarlemmermeer, containing Schiphol airport
* Krimpenerwaard
* Lauwersmeer
* Mastenbroek
* Noordoostpolder
* Prins Alexanderpolder
* Purmer
* Schermer
* Watergraafsmeer
* Wieringermeer
* Wieringerwaard
* Wijdewormer
* Zestienhoven, home of the Rotterdam The Hague Airport (Overschie), in the city of Rotterdam.
* Zuidplaspolder, along with Lammefjord in Denmark the lowest point of the European Union
Rapport 358
* Stenak, Morten. 2005. ''De inddæmmede Landskaber – En historisk geografi.'' Landbohistorik Selskab. *
Polders of the World. Keynotes International Symposium
'. 1982. Lelystad, The Netherlands * Ven, G.P. van de (ed.) 1993, 4th ed. 2004. ''Man-made Lowlands. History of Water Management and Land Reclamation in the Netherlands'', Matrijs, Utrecht. * Wagret, Paul. 1972. ''Polderlands.'' London: Methuen.
– ''in a northwest European and a landmark context''.
{{Authority control Polders, Artificial landforms Land reclamation Environmental soil science Riparian zone Coastal construction Freshwater ecology
A polder () is a low-lying tract of land that forms an artificial hydrology, hydrological entity, enclosed by embankments known as levee, dikes. The three types of polder are:
# Land reclamation, Land reclaimed from a body of water, such as a lake or the seabed
# Floodplain, Flood plains separated from the sea or river by a dike
# Marshes separated from the surrounding water by a dike and subsequently drained; these are also known as ''koogs'', especially in Germany
The ground level in drained marshes subsidence, subsides over time. All polders will eventually be below the surrounding water level some or all of the time. Water enters the low-lying polder through infiltration (hydrology), infiltration and water pressure of groundwater, or rainfall, or transport of water by rivers and canals. This usually means that the polder has an excess of water, which is pumped out or drained by opening sluices at low tide. Care must be taken not to set the internal water level too low. Polder land made up of peat (former marshland) will sink in relation to its previous level, because of peat decomposing when exposed to oxygen from the air.
Polders are at risk from flooding at all times, and care must be taken to protect the surrounding dikes. Dikes are typically built with locally available materials, and each material has its own risks: sand is prone to collapse owing to saturation by water; dry peat is lighter than water and potentially unable to retain water in very dry seasons. Some animals dig tunnels in the barrier, allowing water to infiltrate the structure; the muskrat is known for this activity and hunted in certain European countries because of it. Polders are most commonly, though not exclusively, found in river deltas, former fenlands, and coastal areas.
Flooding of polders has also been used as a military tactic in the past. One example is the flooding of the polders along the Yser River during World War I. Opening the sluices at high tide and closing them at low tide turned the polders into an inaccessible swamp, which allowed the Battle of the Yser#Battle, Allied armies to stop the German army.
Netherlands has a large area of polders: as much as 20% of the land area has at some point in the past been reclaimed from the sea, thus contributing to the development of the country. IJsselmeer is the most famous polder project of the Netherlands. Some other countries which have polders are Bangladesh, Belgium, Canada and China. Some examples of Dutch polder projects are Beemster, Schermer, Flevopolder and Noordoostpolder.
Etymology
The Dutch language, Dutch word ''polder'' derives successively from Middle Dutch ''polre'', from Old Dutch ''polra'', and ultimately from ''pol-'', a piece of land elevated above its surroundings, with the augmentative suffix ''-er'' and Epenthesis, epenthetical '' -d-''. The word has been adopted in thirty-six languages.Netherlands
The Netherlands is frequently associated with polders, as its engineers became noted for developing techniques to drain wetlands and make them usable for agriculture and other development. This is illustrated by the saying "God created the world, but the Dutch created the Netherlands".
The Dutch people, Dutch have a long history of reclamation of marshes and fenland, resulting in some 3,000 ''polders'' nationwide. By 1961, about half of the country's land, , was reclaimed from the sea. About half the total surface area of ''polders'' in north-west Europe is in the Netherlands. The first embankment dam, embankments in Europe were constructed in Roman times. The first polders were constructed in the 11th century. The oldest extant polder is the Achtermeer polder, from 1533.
As a result of flooding disasters, Water board (The Netherlands), water boards called ''waterschap'' (when situated more inland) or ''hoogheemraadschap'' (near the sea, mainly used in the Holland region) were set up to maintain the integrity of the water defences around polders, maintain the waterways inside a polder, and control the various water levels inside and outside the polder. Water boards hold separate elections, levy taxes, and function independently from other government bodies. Their function is basically unchanged even today. As such, they are the oldest democratic institutions in the country. The necessary cooperation among all ranks to maintain polder integrity gave its name to the Dutch version of Third Way (centrism), third-way politics—the ''Polder Model''.
The North Sea flood of 1953, 1953 flood disaster prompted a new approach to the design of dikes and other water-retaining structures, based on an acceptable probability of overflowing. Risk is defined as the product of probability and consequences. The potential damage in lives, property, and rebuilding costs is compared with the potential cost of water defences. From these calculations follows an acceptable flood risk from the sea at one in 4,000–10,000 years, while it is one in 100–2,500 years for a river flood. The particular established policy guides the Dutch government to improve flood defences as new data on threat levels become available.
Major Dutch polders and the years they were laid dry include Beemster (1609–1612), Schermer (1633–1635), and Haarlemmermeerpolder (1852). Polders created as part of the Zuiderzee Works include Wieringermeerpolder (1930), Noordoostpolder (1942) and Flevopolder (1956–1968)
Examples of polders
Bangladesh
Bangladesh has 139 polders, of which 49 are sea-facing, while the rest are along the numerous Distributary, distributaries of the Ganges-Brahmaputra-Meghna River delta. These were constructed in the 1960s to protect the coast from tidal flooding and reduce salinity incursion. They reduce long-term flooding and waterlogging following storm surges from tropical cyclones. They are also cultivated for agriculture.Belgium
* De Moeren, near Veurne in West Flanders
* Polders along the Yser river between Nieuwpoort, Belgium, Nieuwpoort and Diksmuide
* Polders of Muisbroek and Ettenhoven, in Ekeren and Hoevenen
* Polder of Stabroek, in Stabroek
* Kabeljauwpolder, in Zandvliet
* Scheldepolders on the left bank of Scheldt, the Scheldt
* Uitkerkse polders, near Blankenberge in West Flanders
* Prosperpolder, near Doel, Antwerp and Kieldrecht.
Canada
* Tantramar Marshes * Holland Marsh * Pitt Polder Ecological Reserve * Grand Pré, Nova Scotia * Minas BasinChina
* The city of Kunshan has over 100 polders.History
The Jiangnan region, at the Yangtze River Delta, has a long history of constructing polders. Most of these projects were performed between the 10th and 13th centuries. The Chinese government also assisted local communities in constructing dikes for swampland water drainage. The Lijia (里甲) self-monitoring system of 110 households under a ''lizhang'' (里长) headman was used for the purposes of service administration and tax collection in the polder, with a ''liangzhang'' (粮长, grain chief) responsible for maintaining the water system and a ''tangzhang'' (塘长, dike chief）for polder maintenance.Denmark
* Filsø * LammefjordenFinland
* Söderfjärden * Munsmo * Two polders ( in total) near Vassor in KorsholmFrance
* Marais Poitevin * Les Moëres, adjacent to the Flemish polder ''De Moeren'' in Belgium.Germany
In Germany, land reclaimed by diking is called a ''koog''. The German ''Deichgraf'' system was similar to the Dutch and is widely known from Theodor Storm's novella ''The Rider on the White Horse''.
* Altes Land near Hamburg
* Blockland, Bremen, Blockland and Hollerland near Bremen
* Nordstrand, Germany
* Bormerkoog and Meggerkoog near Friedrichstadt
* 36 ''koogs'' in the district of Nordfriesland
* 12 ''koogs'' in the district of Dithmarschen
In southern Germany, the term ''polder'' is used for retention basins recreated by opening dikes during river floodplain restoration, a meaning somewhat opposite to that in coastal context.
Guyana
* Black Bush Polder, Corentyne, Berbice.India
* Kuttanad Region, KeralaIreland
* Lough Swilly, Co. County Donegal, Donegal. Near Inch Island and Newtowncunningham.Italy
* Delta of the river Po River, Po, such as Bonifica Valle del MezzanoJapan
* Around the Ariake Sea in Kyushu, mainly in Saga Prefecture, Saga but also in Fukuoka Prefecture, Fukuoka and Kumamoto Prefecture, Kumamoto PrefecturesLithuania
* Rusnė IslandNetherlands
* Achtermeer, the oldest polder, from 1533
* Alblasserwaard, containing the windmills of Kinderdijk, a World Heritage Site
* Alkmaar
* Andijk
* Anna Paulownapolder
* Beemster, a World Heritage Site
* Bijlmermeer
* Flevopolder, the largest artificial island in the world, youngest polder, last part drained in 1968
* 's-Gravesloot
* Haarlemmermeer, containing Schiphol airport
* Krimpenerwaard
* Lauwersmeer
* Mastenbroek
* Noordoostpolder
* Prins Alexanderpolder
* Purmer
* Schermer
* Watergraafsmeer
* Wieringermeer
* Wieringerwaard
* Wijdewormer
* Zestienhoven, home of the Rotterdam The Hague Airport (Overschie), in the city of Rotterdam.
* Zuidplaspolder, along with Lammefjord in Denmark the lowest point of the European Union
Poland
* Vistula delta near Elbląg and Nowy Dwór Gdański * Warta delta near Kostrzyn nad OdrąSingapore
* Parts of Pulau TekongSlovenia
* The Ankaran, Ankaran/Ancarano Polder ( sl, Ankaranska bonifika), Semedela Polder (), and Škocjan Polder () in reclaimed land around Koper, Koper/Capodistria.South Korea
* Parts of the coast of Ganghwa Island, adjacent to the river Han River (Korea), Han in Incheon * Delta of the river Nakdong River, Nakdong in Busan * Saemangeum in North Jeolla ProvinceSpain
* Parts of Málaga were built on reclaimed landUnited Kingdom
* Traeth Mawr * Sunk Island, on the north shore of the Humber east of Kingston upon Hull, Hull *Caldicot and Wentloog Levels along the Severn Estuary in South Wales * Parts of The Fens **Branston, Lincolnshire, Branston Island, by the River Witham outside the conventional area of the fens but connected to them. * Parts of the coast of Essex * Some land along the River Plym in Plymouth * Some land around Meathop east of Grange-over-Sands, reclaimed as a side-effect of building a railway Embankment (transportation), embankment * The Somerset Levels and North Somerset Levels * Romney Marsh * Sealand, Flintshire * Humberhead LevelsUnited States
* New Orleans * Sacramento – San Joaquin River DeltaSee also
*Afsluitdijk *Flood control in the Netherlands *Land reclamation *WindpumpReferences
Further reading
* Derex, Jean-Michel, Franco Cazzola (eds.) 2004. 2nd ed. 2013. ''Eau et développement dans l'Europe moderne''. Paris, Maison des Sciences De L'Homme * Farjon, J.M.J., J. Dirkx, A. Koomen, J. Vervloet & W. Lammers. 2001. ''Neder-landschap Internationaal: bouwstenen voor een selectie van gebieden landschapsbehoud.'' Alterra, WageningenRapport 358
* Stenak, Morten. 2005. ''De inddæmmede Landskaber – En historisk geografi.'' Landbohistorik Selskab. *
Polders of the World. Keynotes International Symposium
'. 1982. Lelystad, The Netherlands * Ven, G.P. van de (ed.) 1993, 4th ed. 2004. ''Man-made Lowlands. History of Water Management and Land Reclamation in the Netherlands'', Matrijs, Utrecht. * Wagret, Paul. 1972. ''Polderlands.'' London: Methuen.
External links
– ''in a northwest European and a landmark context''.
{{Authority control Polders, Artificial landforms Land reclamation Environmental soil science Riparian zone Coastal construction Freshwater ecology