Effects of the use of drainage-/ subirrigation systems in the Pleistocene uplands of the Netherlands

“The Netherlands is a low-lying, flood prone country, located in a delta. Most Dutch agricultural fields are drained to quickly get rid of excess water to increase crop production. Additionally, the freshwater demand of different sectors (agriculture, industry, drinking water) increases, causing an increased pressure on the groundwater system. The combination of fast drainage and increased use of groundwater for human activities led to declining groundwater tables in the Dutch Pleistocene uplands. Given the changing climate resulting in prolonged dry periods, solutions for water retention are needed to decrease the pressure on the groundwater system to guarantee the future water supply for different sectors.
One of the solutions could be to modify the current drainage systems to drainage-infiltration (DI)- systems with a dual purpose. First, the DI-system stores water during (heavy) rainfall in the soil, but if the risk of flooding increases, the DI-system discharges water. Second, (external) water is actively pumped into the drainage network to raise groundwater tables (subirrigation). Through efficient use of the available external water source (treated waste water, industrial waste water, surface water or groundwater) the pressure on the groundwater system reduces.”

(Citation: de Wit, J.A., Bartholomeus, R.P., van den Eertwegh, G.A.P.H., van Huijgevoort, M.H.J. – Effects of the use of drainage-/ subirrigation systems in the Pleistocene uplands of the Netherlands – European Geosciences Union (EGU) Abstract, 26 April 2021)