| PP Seepage of saline water | |
|---|---|
| Context | PP Ontpoldering Perkpolder |
| Decompositie type | IOR |
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).
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| Produceert | |
|---|---|
| Consumeeert | |
| Onderdeel van | PP Groundwater processes |
| Instantie van | |
| Betreft |
Draagt bij aan.
| Draagt bij aan | PP Saline groundwater in adjacent area |
|---|---|
| Waarde | + |
| Opmerkingen |
Connectie.
| Connectie type | seq |
|---|---|
| Connecteert naar | PP Functioning of seepage system |
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| Opmerkingen |
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| Komt van | Type | Connectie type | Conditie | Waarde | Opmerkingen |
|---|---|---|---|---|---|
| PP Saline groundwater in tidal basin | Contributes | + |
