Maarten Jansen, Leon de Jongste, Marcel Klinge, Sebastiaan Schep, Paul Stook, Gustav Egbring
Friday 3 july 2015
14:45 - 15:00h at Antarctica (level 0)
Themes: (T) Sediment management and morphodynamics, (ST) Basin-wide sediment management
Parallel session: 16A. Sediment - Coast
Many shallow lakes suffer from accumulation of fine sediment. The fines may have several origins, such as erosion of banks or shallows, degradation of peat layers, internal organic production, external inflow. The accumulation may cause several problems, ranging from problems for human use of the water (boating, swimming, drinking water) to ecological problems (increased turbidity, loss of vegetation cover and associated biodiversity). Removing the sediment by dredging is usually expensive because of the large quantities, the large surface area that needs to be treated and the costs associated with transport, storage and/or disposal. Moreover, dredging usually does not restore the water ecologically. An interesting solution to reduce or solve the problems with fine sediment in a cost effective manner is to steer the transport of fine sediment with relative small measures. Fine sediment could be caught by the creation of lee areas, where silt can settle. Depending on water depth and transparency submerged and/or emerged vegetation may develop, thus increasing further settlement conditions and local biodiversity recovery. Depending on the specific functioning of the system, steering the fines may contribute significantly to the ecological recovery of the entire lake. The principle of steering fines in shallow lakes is applied in the Wormer- and Jisperveld, The Netherlands, which consists of three shallow lakes connected to each other by small channels. Banks of the lakes and the channels with orientation in south western direction. Due to the erosion, large parts of the lakes and channels are filled with organic silt. This limits the ecological functioning and gives problems to boats, because of shallow areas. To get insight in the wave attack and present transport patterns of fines, a hydrodynamic model was set up. Special attention was paid to the interaction between currents and waves. After that, the model was used to examine the best way to create lee areas and to optimise the effectiveness of measures. The most promising measures were implemented in Wormer- and Jisperveld last year. Since then the silt transports decreased significantly. In some lee areas emerged vegetation developed, demonstrating the potential of this approach to solve problems with fines and to contribute to ecological recovery of the lakes.