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Polder

 

Polder

Polder at Neßmersiel, Germany, aerial view in May 2012

A polder is a low-lying tract of land enclosed by embankments (barriers) known as dikes that forms an artificial hydrological entity, meaning it has no connection with outside water other than through manually operated devices. There are three types of polder:

  • Land reclaimed from a body of water, such as a lake or the sea bed
  • Flood plains separated from the sea or river by a dike
  • Marshes separated from the surrounding water by a dike and subsequently drained

The ground level in drained marshes subsides over time and thus all polders will eventually be below the surrounding water level some or all of the time. Water enters the low-lying polder through water pressure of ground water, 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 in dry conditions.

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 well known for this activity and actively hunted in certain European countries because of it. Polders are most commonly, though not exclusively, found in river deltas, former fenlands and coastal areas.

Contents

  • Polders and the Netherlands 1
  • See also 2
  • References 3
  • External links 4

Polders and the Netherlands

Pumping station in Zoetermeer, Netherlands. The polder lies lower than the surrounding water on the other side of the dike. The Archimedes' screws are clearly visible.

The Netherlands is frequently associated with polders. This is illustrated by the English saying: God created the world but the Dutch created Holland (sic).

The Dutch have a long history of reclamation of marshes and fenland, resulting in some 3,000 polders[1] nationwide. About half the total surface area of polders in north-west Europe is in the Netherlands. The first embankments in Europe were constructed in Roman times. The first polders were constructed in the 11th century. As a result of flooding disasters, water boards called waterschap (when situated more inland) or hoogheemraadschap (near the sea, mainly used in the Holland region)[2] 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 bodies 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 institution in the country. The necessary cooperation between all ranks in maintaining polder integrity also gave its name to the Dutch version of third way politics—the Polder Model.

The 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 to 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 becomes available.

Some famous Dutch polders and the year they were laid dry are:

As part of the Zuiderzee Works:

See also

References

  1. ^ "TKijk naar de geschiedenis". Rijkswaterstaat. Retrieved 2008-01-21. 
  2. ^ http://www.waterschappen.nl/mijn-waterschap.html
  • Farjon, J.M.J., J. Dirkx, A. Koomen, J. Vervloet & W. Lammers. 2001. Neder-landschap Internationaal: bouwstenen voor een selectie van gebieden landschapsbehoud. Alterra, Wageningen. Rapport 358.
  • Morten Stenak. 2005. De inddæmmede Landskaber - En historisk geografi. Landbohistorik Selskab.
  • Ven, G.P. van de (red.) 1993. Leefbaar laagland: geschiedenis van waterbeheersing en landaanwinning in Nederland. Matrijs, Utrecht.
  • Wagret, P. 1972. Polderlands. London : Methuen.

External links

  • Polder landscapes in the Netherlands — in a northwest European and a landmark context.
  • How to make a polder — online film
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