A discharge sluice must drain off inland water and stem offland water. The discharge sluices in the Afsluitdijk ('Closure Dike') by the IJsselmeer is a good example. The IJsselmeer is constantly being fed fresh water from rainwater as well as the rivers IJssel, Vecht and Eem. In order to get rid of the excess water, water is spouted into the Wadden Sea during low tide. The Afsluitdijk has a total of 25 discharge sluices. The same principle is used by Lauwersoog, where water is spouted from the Lauwersmeer into the Wadden Sea. Other discharge sluices in the Netherlands can be found in polders that discharge into rivers or the sea. Discharge sluices are by far the most important type of sluice for managing inland water levels.
In Groningen and Northern Overijssel, a sluice is called a 'zijl' (no difference in English). The sluices in Groningen often discharge into the sea and restrain high-tide water. Many towns thank their name on such a 'zijl', for example Delfzijl, Termunterzijl, Noordpolderzijl and Dokkumer Nieuwe Zijlen. In Frisian a sluice is called a 'syl'. Many towns in East Friesland (Germany) end with -siel (German syl), such as Bensersiel, Harlesiel and Neuharlingersiel.
A discharge sluice located under the dike is called a culvert. These sluices were built in the Netherlands during the Roman Times. They were made from hollowed-out trees with a lid so that the water could exit but not enter. In Friesland, a discharge sluice is called a pump.