Polder. A polder is a low-lying tract of land that forms an artificial hydrological entity, enclosed by embankments known as dikes.
The three types of polder are: 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; these are also known as koogs, especially in Germany. The ground level in drained marshes 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 and 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 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 tu
The three types of polder are: 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; these are also known as koogs, especially in Germany. The ground level in drained marshes 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 and 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 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 tu
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