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Satellite image of Noordoostpolder, Netherlands (595.41 km²)

A polder is a low-lying tract of land enclosed by embankments 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:

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 ground swell due to water pressure on ground water or rain fall and transportation of water by rivers and canals. This usually means that the polder has an excess of water that needs to be pumped out or drained by opening sluices at low tide. However, care must be taken in not setting the internal water level too low. Polder land made up of peat (former marshland) will show accelerated compression due to the 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 mostly built using locally available materials and each has its own risk factor: sand is prone to collapse due to oversaturation by water while dry peat is lighter than water, making the barrier potentially unstable in very dry seasons. Some animals dig tunnels in the barrier, undermining the structure; the muskrat is notorious for this behavior. For this reason in the Netherlands it is actively hunted to extinction. No such care is taken in neighboring Germany though, causing the stock to be constantly resupplied across the border.

Polders are most commonly found, though not exclusively so, in river deltas, former fen lands and coastal areas.

Contents

Polders and the Netherlands

Windmill in North-Holland, the polder lies lower than the surrounding water on the other side of the dike

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

The Dutch have a long history of reclamation of marshes and fenland, resulting in some 3,000 polders [1] nationwide. About half of all polder surface within northwest Europe is located within the Netherlands. The first embankments in Europe were constructed in Roman times. The first polders were constructed in the 11th century. Due to flooding disasters water boards called waterschap (below sealevel) or hoogheemraadschap (above sea level) were set up to maintain the integrity of the water defenses 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 currently. As such, they are the oldest democratic institution in the country. The necessary co-operation 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 damage in lives, property and rebuilding costs is offset against the cost of water defenses. From these calculations follow an acceptable flood risk from the sea at 1 in 4,000–10,000 years, while it is 1 in 100–2,500 years for a river flood. The established policy forces the Dutch government to improve flood defenses as new data on threat levels becomes available. For comparison, the risk of the (repaired) New Orleans dike system in the future collapsing due to sea flooding is estimated at 1 in 100 years[2] (i.e. flooding risks in New Orleans remain 100 times higher compared to Rotterdam which is set at 1/10,000)

Examples of polders

Belgium

Canada

France

Germany

Guyana

Black Bush Polder, Corentyne, Berbice

Italy

  • Delta of the river Po such as Bonifica Valle del Mezzano

Netherlands

(This is by no means an exhaustive list)

Poland

United Kingdom

United States

See also

References

  1. ^ "TKijk naar de geschiedenis". Rijkswaterstaat. https://www.rijkswaterstaat.nl/rws/waterinnovatiebron/cgi-bin/toonlijst.pl?config=config&var=volgnr&val=1&layout=index-forceframe&confignr=1&menu=1067260347&menuitem=1120115781. Retrieved 2008-01-21.  
  2. ^ [1]
  • 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


1911 encyclopedia

Up to date as of January 14, 2010

From LoveToKnow 1911

POLDER, the Dutch name for a piece of low-lying, marshy land reclaimed from the sea or other water by drainage and diking (see Holland).


<< Polar Regions

Pole (Family) >>


Simple English

is a Polder. Old land is mostly green, new one is darker in color.]]

Empoldering is a method of reclaiming land from the sea. Empoldering involves the use of polders, and is also a way to control floods. A polder is a piece of land in a low-lying area that has been reclaimed from a body of water by building dikes and drainage canals.


Although empoldering is usually carried out in low-lying coastal areas, it can be also carried out in inland areas such as lakes and rivers. It is commonly carried out in countries like the Netherlands, where much of the country is below sea level and subject to flooding. About one-fifth of the land in the Netherlands has been reclaimed from the sea. Their largest and most successful project is the Zuider Zee project.


Polders have 2 distinct features. Firstly, they are enclosed by dikes to keep the water out. The dikes also serve to protect the polder from erosion. Secondly, polders are continually maintained by systems of drainage canals and pumps which prevent them from becoming waterlogged and hence, suitable for cultivation.

Process:

Stage 1: Dike constructed around the area to be reclaimed to keep water from coming in.

Stage 2: The area is drained using pumps and drainage canals.

Stage 3: "Reeds"(a type of salt tolerant plant) are sown by aircraft to help the soil form.

Stage 4: After 3 years, reeds are burnt and the ash is used as fertilisers for the soil.

Stage 5: After a period of up to 15 years, the polder is ready for growing crops, building houses and constructing roads.

Limits of land reclamation:

1. Cost of reclaiming from deeper waters,

2. Availability of sand,

3. Dispute over territorial boundaries.








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