Difference between revisions of "Improve/Create water storage"
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==General description == | ==General description == | ||
Water quantity and the flow regime can be altered by different factors such as changes in land cover, soil structure and compacting, loss of floodplains and wetlands, and stormwater runoff from urban areas. Loss of water retention combined with accelerated runoff typically increases the frequency and magnitude of flood peaks but also reduces the availability of water to streams during the prevailing low flow (base flow) periods. | Water quantity and the flow regime can be altered by different factors such as changes in land cover, soil structure and compacting, loss of floodplains and wetlands, and stormwater runoff from urban areas. Loss of water retention combined with accelerated runoff typically increases the frequency and magnitude of flood peaks but also reduces the availability of water to streams during the prevailing low flow (base flow) periods. | ||
| − | Preferably, a more natural flow regime can be restored by increasing water infiltration and retention at the catchment scale by e.g. changes in land cover and floodplain restoration (see measure [http://wiki.reformrivers.eu/index.php/Improve_water_retention#General_description/ water retention]) since this addresses both, increased peak flows and reduced base flows. An alternative local end-of-pipe solution to reduce peak flows caused by stormwater runoff are retention and detention basins, which are of special importance for small rivers where single effluents may already cause massive erosion, affect water quality, and organisms are flushed away (catastrophic drift). | + | Preferably, a more natural flow regime can be restored by increasing water infiltration and retention at the catchment scale by e.g. changes in land cover and floodplain restoration (see measure [http://wiki.reformrivers.eu/index.php/Improve_water_retention#General_description/ Improve water retention]) since this addresses both, increased peak flows and reduced base flows. An alternative local end-of-pipe solution to reduce peak flows caused by stormwater runoff are retention and detention basins, which are of special importance for small rivers where single effluents may already cause massive erosion, affect water quality, and organisms are flushed away (catastrophic drift). |
Please note: | Please note: | ||
* polders are not covered here but in the fact-sheet [http://wiki.reformrivers.eu/index.php/Link_flood_reduction_with_ecological_restoration#General_description/ Link flood reduction with ecological restoration] | * polders are not covered here but in the fact-sheet [http://wiki.reformrivers.eu/index.php/Link_flood_reduction_with_ecological_restoration#General_description/ Link flood reduction with ecological restoration] | ||
Revision as of 11:32, 22 December 2015
Contents
- 1 Improve/Create water storage
- 1.1 General description
- 1.2 Applicability
- 1.3 Expected effect of measure on (including literature citations):
- 1.4 Temporal and spatial response
- 1.5 Pressures that can be addressed by this measure
- 1.6 Cost-efficiency
- 1.7 Case studies where this measure has been applied
- 1.8 Useful references
- 1.9 Other relevant information
Improve/Create water storage
Category 01. Water flow quantity improvement
General description
Water quantity and the flow regime can be altered by different factors such as changes in land cover, soil structure and compacting, loss of floodplains and wetlands, and stormwater runoff from urban areas. Loss of water retention combined with accelerated runoff typically increases the frequency and magnitude of flood peaks but also reduces the availability of water to streams during the prevailing low flow (base flow) periods. Preferably, a more natural flow regime can be restored by increasing water infiltration and retention at the catchment scale by e.g. changes in land cover and floodplain restoration (see measure Improve water retention) since this addresses both, increased peak flows and reduced base flows. An alternative local end-of-pipe solution to reduce peak flows caused by stormwater runoff are retention and detention basins, which are of special importance for small rivers where single effluents may already cause massive erosion, affect water quality, and organisms are flushed away (catastrophic drift). Please note:
- polders are not covered here but in the fact-sheet Link flood reduction with ecological restoration
- anthropogenic peak flows are also caused by hydropeaking; read more about measures to modify hydropeaking here
Applicability
Detention basins are dry between floods, fill and store water during floods, slowly drain when water levels in the receiving channel recede, and hence attenuate the runoff and reduce peak flows but have very limited effects on water quality.
Retention basins have a permanent pool of water (like ponds) and, except for the runoff exceeding the capacity of the basin that drains to the channel, the water is stored permanently. Besides reducing peak flows, retention basin have a larger effect on water quality through sedimentation of pollutants and uptake of nutrients by plants. However, due to the water permanently stored, they have a lower capacity and hence, have to be larger. In contrast to infiltration basins, they are usually not explicitly built for groundwater recharge (in contrast to infiltration basins) but still may increase the risk of groundwater contamination (Fischer et al. 2003).
It is important to only reduce the peak flows and to ensure that low flows and environmental flows are maintained in receiving channels.
Expected effect of measure on (including literature citations):
- Peak flows are substantially reduced (e.g. by a minimum of 50% in Muschalla et al. 2014).
- Effects on water quality are limited (Sebastian et al. 2015) and higher in retention compared to detention basins.
- Effects on biota are less well studied. There are clear regulations to assess potential effects of stormwater runoff and estimate the size of detention and retention basins in some member states (e.g. Northrhine-Westphalia, Germany BWKM3 M7), and several more general approaches are available (e.g. Bledsoe et al. 2012).
Temporal and spatial response
Pressures that can be addressed by this measure
Cost-efficiency
Case studies where this measure has been applied
- Regge Velderberg
- Uilenkamp - Meander reconnection
- Sweden- Restoration of the Freshwater Pearl Mussel and its habitats (LIFE04/NAT/SE/000231)
- Polder Ingelheim – Restoring former floodplains (INTERREG Sustainable Development of Floodplains)
- Bemmelse Waard – Restoring former floodplains (INTERREG Sustainable Development of Floodplains)
- Hondsbroeksche Pleij – Restoring former floodplains (INTERREG Sustainable Development of Floodplains)
- Narew river restoration project
- Warta Middle River Valley
Useful references
- Bledsoe, B.P., Stein, E.D., Hawley, R.J., et al. (2012). Framework and tool for rapid assessment of stream susceptibility to hydromodification. Journal of the American Water Resources Association, 48, 788-808.
- Fischer, D., Charles, E.G., Baehr, A.L. (2003). Effects of stormwater infiltration on quality of groundwater beneath retention and detention basins. Journal of Environmental Engineering - ASCE, 129, 464-471.
- Muschalla, D, Vallet, B., Francois, A., et al. (2014). Ecohydraulic-driven real-time control of stormwater basins. Journal of Hydrology, 511, 82-91.
- REFORM Wiki - Modify hydropeaking : http://wiki.reformrivers.eu/index.php/Modify_hydropeaking
- Sebastian, C., Becouze-Lareure, C., Kouyi, G., et al. (2015). Event-based quantification of emerging pollutant removal for an open stormwater retention basin - Loads, efficiency and importance of uncertainties. Water Research, 73, 239-250.
- USGS - Runoff (surface water runoff) : http://water.usgs.gov/edu/runoff.html (accessed October 7th, 2015).
- MKULNV NRW (Ministerium für Klimaschutz, Umwelt, Landwirtschaft, Natur- und Verbraucherschutz des Landes Nordrhein-Westfalen): http://www.flussgebiete.nrw.de/index.php/Ma%C3%9Fnahmen/M1.0 (German)
