Title: Ad van der Spek
1Ad van der Spek Jan Mulder
- Large-scale future maintenance of the Dutch
coast - Learning from nature
2Introduction
- Goal
- putting coastal maintenance into the right
perspective - connecting daily practice to long-term coastal
evolution, anticipating future accelerated
sea-level rise
3Long-term coastal evolution
- supply gt demand
- regression
- supply demand
- stabile
- supply lt demand
- transgression
4Accommodation space ( demand ! )
- basal topography relative sea level
5Long-term coastal evolution
- 1. basal topography relative sea level
- accommodation space
- demand
- 2. accommodation space sediment supply
- coastal evolution !!
6Future changes in balance
- topography is fixed
- RSLR accelerates (predictions)
- sediment supply ???
7Large-scale coastal evolutionexamples from The
NetherlandsRelative sea-level rise
- trendcurve
- absolute sea-level rise
- land subsidence
8Paleo-geographyc. 5000 BP
9Paleo-geographyc. 2600 BP
10Holocene sediment budget
- Define sources and sinks
- Calculate the volume of coastal deposits
- Construct a time frame
- curve relative sea-level rise
- growth of volume with time
- Sediment Accumulation during Holocene
11Holocene sediment budget1. Sources sinks
- sinks
- coastal plain deposits
- tidal basins
- barriers
- sources
- North Sea floor
- Pleistocene headlands
- rivers
- older coastal deposits
12Sink the coastalplain
- tidal basins
- estuaries
- beach barriers
13Cross-section
14Total volume Holocene coastal deposits
- ( in billion m3 )
- lithology volume percentage
- --------------------------------------------------
-------------------------------- - sand 151 - 157 67 -70
- mud 59 - 65 26 - 29
- peat 11 5
- --------------------------------------------------
-------------------------------- - Total 226 100
15Holocene sediment budgetInfilling with time
- period percentage volume volume / yr
- (billion m3) (million m3)
- --------------------------------------------------
-------------------------------------- - Atlantic 60 136 41
- (8000-5000 BP)
- Subboreal 30 67 27
- (5000-2900 BP)
- Subatlantic 10 23 7
- (since 2900 BP)
- --------------------------------------------------
--------------------------------------
16Conclusion
- No longer natural
- large-scale
- sediment accumulation
- !!!
17The Hague, we have got a problem !
- Solution
- Do it yourself !
- Nourish the beach and shoreface (1990)
- Nourish the coastal foundation (2001)
- Nourish the coastal plain? (20..?)
18Keeping up by nourishing sand
19Keeping up with sea-level rise
-
- Sea-level rise 18 60 85 cm/century
- Coastal foundation 7 23 33
- Wadden Sea 4,5 15 21
- Westerschelde 0,5 1,7 2,4
- ______________________________________
- Total volume
- nourishments 12 40 57 Mm3/year
20 how about the coastal plain ?
coastal foundation
coastal plain
21Interested?
- Regional Sediment Deficits in the Dutch
Lowlands Implications for Long-Term Land-Use
Options - Van der Meulen et al. (2007), J. Soils Sediments
7 (1) 9-16 - http//www.tno.nl/content.cfm?contextmarktencont
entcaselaag1188item_id406
22Concluding remarks
- help mother nature !
- it works !
- plenty of sand in the North Sea
- raising the coastal plain?
- we have got time, but dont wait too long!
23Thank you for your attention !
24Holocene sediment budget3. Constructing a time
frame
- curve relative sea-level rise
- assumptions
- basin fills up to MSL
- growth of volume with time
- corrections
- infilling tidal basins lagging behind RSLR
- reworking of older coastal deposits
25Flow deposits sand on edge of tidal flats