EGU21-10557
https://doi.org/10.5194/egusphere-egu21-10557
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

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

Janine A. de Wit1,2, Ruud P. Bartholomeus1,2, Gé A.P.H. van den Eertwegh3, and Marjolein H.J. van Huijgevoort1
Janine A. de Wit et al.
  • 1KWR Water Research Institute, the Netherlands (janine.de.wit@kwrwater.nl)
  • 2Wageningen University, Soil Physics and Land Management Group, Wageningen, the Netherlands
  • 3KnowH2O, Berg en Dal, 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.

We focus on the data and model results of several field experiments using subirrigation conducted in the Dutch Pleistocene uplands (± 2017-2020). The effects of subirrigation on the groundwater table and soil moisture conditions will be shown, including water supply rate and hydrological boundary conditions. We also provide both the set-up and results of field scale model simulations (SWAP; Soil-Water-Atmosphere-Plant model) to i) quantify the impact of subirrigation on all components of the (regional) water balance (including transpiration, drainage and groundwater recharge), ii) quantify crop yields, and iii) optimize the configuration and management of subirrigation systems for different soil types, hydrological boundary conditions, and climate scenarios.  

How to cite: de Wit, J. A., Bartholomeus, R. P., van den Eertwegh, G. A. P. H., and van Huijgevoort, M. H. J.: Effects of the use of drainage-/ infiltration systems in the Pleistocene uplands of the Netherlands, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-10557, https://doi.org/10.5194/egusphere-egu21-10557, 2021.