Effects of water level changes (like sea level rise or restoration of tidal areas) on groundwater in adjacent areas will propagate via hydraulic heads in the aquifer(s). The first step in quantifying these kinds of effects is to determine the net effect on the hydraulic head in the aquifer(s) as a result of changes at or nearby the surface. The composition of the subsoil and the morphology of the tidal area are the two most important factors controlling the tidal propagation in the aquifer. The tidal area morphology determines which part will be submerged and for what duration (Boersema et al. 2016).
Referenties
- Perkpolder tidal restauration, one year after realisation, draft progress report, Boersema, M., J. van der werf, P. de Louw, T. Ysebaert, T. Bouma, Centre of expertise Delta Technology, 27 november 2016.
Zie ook
- Perkpolder tidal restauration, one year after realisation, draft progress report
- Rammegors tidal restauration, final report
- Perkpolder Tidal Restauration
- Groundwater processes
- Understanding the morphological development of the Oesterdam nourishment
- Eastern Scheldt inlet morphodynamics
- Oesterdam sand nourishment - ecological and morphological development of a local sand nourishment
- Aspects of sediment- and morphodynamics of subtidal deposits of the Oosterschelde (the Netherlands)
- Oyster reefs and coastal protection
- Biogeomorphology of Spartina anglica tussocks, GIS based comparison of contrasting sites at the Westerschelde and Blackwater estuary
