The closure of the Haringvliet in 1970 caused the salt water, the greatest tidal action, and also certain fish species to disappear from Dutch waters. The Kier Decision is intended to make fish migration possible again by also opening the sluices partially at high tide, within preconditions for flood safety, freshwater supply and shipping. However, the fresh-salt “behaviour” in the Haringvliet under different conditions still involves uncertainties at present. There was virtually no experience with it, which means important knowledge is still lacking, for example to be able to analyse possible scenarios in advance using models.
It was therefore not possible to determine a priori an operational programme that provides the required certainty with regard to the freshwater supply. For instance, it was expected that the salt water would move mainly through the deeper parts (for example the old tidal channels) of the Haringvliet. However, it was still unclear at which (river) discharge the position of the fresh-salt transition can be controlled under different conditions, especially in the deeper parts.