Case study:Freiston Managed Realignment Scheme: Difference between revisions
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|Picture description=Panorama of westerly breach (view east) (Taken by: C. Scott, ABPmer, April 2010) | |Picture description=Panorama of westerly breach (view east) (Taken by: C. Scott, ABPmer, April 2010) | ||
|Project summary=In 1983, HM Prison Service (HMP) claimed 66ha of intertidal habitat to gain land for arable production by building a new seaward defence. During the 1990s, the Environment Agency identified this 1,750m stretch of seawall owned by HMP as at high risk of failure, and following a cost benefit analysis decided to strengthen the old, landward, bank in order to form the flood defence. The Royal Society for the Protection of Birds (RSPB) was very keen to take this opportunity to realign the defences and recreate intertidal habitats, and, following discussions with the Environment Agency, English Nature and HMP, acquired the land. | |Project summary=In 1983, HM Prison Service (HMP) claimed 66ha of intertidal habitat to gain land for arable production by building a new seaward defence. During the 1990s, the Environment Agency identified this 1,750m stretch of seawall owned by HMP as at high risk of failure, and following a cost benefit analysis decided to strengthen the old, landward, bank in order to form the flood defence. The Royal Society for the Protection of Birds (RSPB) was very keen to take this opportunity to realign the defences and recreate intertidal habitats, and, following discussions with the Environment Agency, English Nature and HMP, acquired the land. | ||
Prior to the realignment, in 2000, some 1,100m of the remnant landward sea wall were enforced, and a new 500m cross wall built. The material for these works was sourced on site (the borrow pit was later developed into a 15ha saline lagoon). Prior to breaching the sea wall, the vegetation on the 66ha site was cut, baled and removed, field drains were infilled (as far as fill material was available) and some 1,200m of artificial creek system were dug (two channels leading from each breach). Outside the site, some 50m of the external primary creek network were deepened. Finally, three 50m wide breaches were created in the outer sea wall (with channels initially 2m wide and 1m deep). | Prior to the realignment, in 2000, some 1,100m of the remnant landward sea wall were enforced, and a new 500m cross wall built. The material for these works was sourced on site (the borrow pit was later developed into a 15ha saline lagoon). Prior to breaching the sea wall, the vegetation on the 66ha site was cut, baled and removed, field drains were infilled (as far as fill material was available) and some 1,200m of artificial creek system were dug (two channels leading from each breach). Outside the site, some 50m of the external primary creek network were deepened. Finally, three 50m wide breaches were created in the outer sea wall (with channels initially 2m wide and 1m deep). | ||
The site is owned and managed by the Royal Society for the Protection of Birds (RSPB). Its Freiston Shore reserve incorporates the 66ha realignment site, a 15ha saline lagoon and 72ha of wet grassland. Furthermore, Freiston Shore already protects 683ha of saltmarsh and mudflats, which form part of the Wash Special Protection Area (SPA) (RSPB website, 2010). | The site is owned and managed by the Royal Society for the Protection of Birds (RSPB). Its Freiston Shore reserve incorporates the 66ha realignment site, a 15ha saline lagoon and 72ha of wet grassland. Furthermore, Freiston Shore already protects 683ha of saltmarsh and mudflats, which form part of the Wash Special Protection Area (SPA) (RSPB website, 2010). | ||
|Monitoring surveys and results=An initial four-year environmental monitoring programme of the site, and adjacent intertidal habitats, has recently concluded (Brown et al., 2007). The majority of the monitoring was undertaken between 2001 and 2006 by the Natural Environment Research Council’s Centre for Ecology and Hydrology (CEH), the Cambridge Coastal Research Unit (CCRU), and Birkbeck College (University of London). It investigated accretion/erosion rates, sediment properties, vegetation colonisation, establishment and succession, invertebrate colonisation, and fish | |Monitoring surveys and results=An initial four-year environmental monitoring programme of the site, and adjacent intertidal habitats, has recently concluded (Brown et al., 2007). The majority of the monitoring was undertaken between 2001 and 2006 by the Natural Environment Research Council’s Centre for Ecology and Hydrology (CEH), the Cambridge Coastal Research Unit (CCRU), and Birkbeck College (University of London). It investigated accretion/erosion rates, sediment properties, vegetation colonisation, establishment and succession, invertebrate colonisation, and fish utilisation. Accretion and vegetation was surveyed inside the realignment for an additional (5th) year in 2007 (Brown, 2008). Furthermore, the RSPB undertook monthly bird monitoring (for breeding and water birds, as well as wintering passerines), and the National Oceanographic Centre measured wave activity and tide heights for one year after the breach. | ||
utilisation. Accretion and vegetation was surveyed inside the realignment for an additional (5th) year in 2007 (Brown, 2008). Furthermore, the RSPB undertook monthly bird monitoring (for breeding and water birds, as well as wintering passerines), and the National Oceanographic Centre measured wave activity and tide heights for one year after the breach. | |Lessons learn='''Accretion''': The recent monitoring reports (Brown et al., 2007; Brown 2008) concluded that in the five years after breaching the sea wall, the Freiston managed realignment site has accreted sediment at similar rates to those of the adjacent salt marsh at the equivalent elevation range. Mean annual accretion rates (after removing a few sites influenced by high deposition of material washed in around the central breach area) ranged between 6 and 10mm per year, and the pattern of natural inter-annual variations inside the realignment matched those outside. | ||
|Lessons learn=Accretion: The recent monitoring reports (Brown et al., 2007; Brown 2008) concluded that in the five years after breaching the sea wall, the Freiston managed realignment site has accreted sediment at similar rates to those of the adjacent salt marsh at the equivalent elevation range. Mean annual accretion rates (after removing a few sites influenced by high deposition of material washed in around the central breach area) ranged between 6 and 10mm per year, and the pattern of natural inter-annual variations inside the realignment matched those outside. | |||
Vegetation: Vegetation establishment and spread have been judged as highly successful, as these have been more rapid than in other (earlier) managed realignment sites. By September 2005, 70% of the area was covered by plants, initially with pioneer species such as glasswort (Salicornia) and and annual sea-blite (Suaeda maritima) dominating. By the second and third year, perennial species such as sea purslane (Halimone portulacoides) and sea aster (Aster tripolium) had become more prevalent (Badley and Allcorn, 2006). It was estimated that the realignment site’s species abundance and community types could be equivalent to those outside the site within a further 5 years. This successful vegetation establishment was attributed mainly to the suitable site elevations and the abundant supply of seeds and tiller fragments from the extensive external salt marsh. Overall, no clear evidence was found to suggest that the realignment site has had any | '''Vegetation''': Vegetation establishment and spread have been judged as highly successful, as these have been more rapid than in other (earlier) managed realignment sites. By September 2005, 70% of the area was covered by plants, initially with pioneer species such as glasswort (Salicornia) and and annual sea-blite (Suaeda maritima) dominating. By the second and third year, perennial species such as sea purslane (Halimone portulacoides) and sea aster (Aster tripolium) had become more prevalent (Badley and Allcorn, 2006). It was estimated that the realignment site’s species abundance and community types could be equivalent to those outside the site within a further 5 years. This successful vegetation establishment was attributed mainly to the suitable site elevations and the abundant supply of seeds and tiller fragments from the extensive external salt marsh. Overall, no clear evidence was found to suggest that the realignment site has had any | ||
adverse effects on the adjacent saltmarsh in general (Brown et al., 2007). | adverse effects on the adjacent saltmarsh in general (Brown et al., 2007). | ||
Invertebrates: The realignment site lies at an elevation suitable for salt marsh establishment therefore most of the invertebrates found were species associated with the developing salt marsh. The nature of the fauna (seasonal and weather-dependent activity of mobile organisms and large variation in numbers of small species) made it difficult to make comparisons between years, or between the realignment site and the adjacent marsh, from an annual survey. However, most species found outside were recorded in the site and many species have increased in abundance (Brown et al., 2007). | |||
Fish: The annual fish surveys showed that at least 11 species utilised the realignment site during the first | '''Invertebrates''': The realignment site lies at an elevation suitable for salt marsh establishment therefore most of the invertebrates found were species associated with the developing salt marsh. The nature of the fauna (seasonal and weather-dependent activity of mobile organisms and large variation in numbers of small species) made it difficult to make comparisons between years, or between the realignment site and the adjacent marsh, from an annual survey. However, most species found outside were recorded in the site and many species have increased in abundance (Brown et al., 2007). | ||
four years of its existence. It was found to act as an important fish nursery area for several commercially important species (such as bass, sprat, and herring), which were shown to be feeding in the realignment site. The site also provides nursery habitat throughout the entire tidal cycle (i.e. fish continue to use the site when it is disconnected from the sea, with the continuous utilisation of permanently flooded channels). In order to improve the site’s fish nursery function, the addition of shallow pools or pans was recommended along with research into creek configuration(design and density) (Brown et al., 2007). | |||
Birds: Badley and Allcorn (2006) concluded from four years’ of bird monitoring that the realignment supported ‘large numbers of wintering waterbirds, several species in nationally important (i.e. > 1%) of the UK population) numbers’. These include dark-bellied brent goose and golden and grey plover (for which the following respective peak counts were observed during the 2005/06 period: 1,727, 5,000 and 263). In 2006, the realignment did not contain areas of high enough elevation to support breeding waders, as it was completely inundated during spring tides. The adjacent saline lagoon has developed into a habitat of high ornithological value; it provides a home for breeding, roosting and wintering water birds. Avocets bred for the first time in South Lincolnshire on the newly created lagoon islands. Now, around 40 pairs of avocets choose the lagoon to breed each year. Furthermore large flocks of knot roost on the lagoon and nearby reservoir (RSPB website, | '''Fish''': The annual fish surveys showed that at least 11 species utilised the realignment site during the first four years of its existence. It was found to act as an important fish nursery area for several commercially important species (such as bass, sprat, and herring), which were shown to be feeding in the realignment site. The site also provides nursery habitat throughout the entire tidal cycle (i.e. fish continue to use the site when it is disconnected from the sea, with the continuous utilisation of permanently flooded channels). In order to improve the site’s fish nursery function, the addition of shallow pools or pans was recommended along with research into creek configuration(design and density) (Brown et al., 2007). | ||
'''Birds''': Badley and Allcorn (2006) concluded from four years’ of bird monitoring that the realignment supported ‘large numbers of wintering waterbirds, several species in nationally important (i.e. > 1%) of the UK population) numbers’. These include dark-bellied brent goose and golden and grey plover (for which the following respective peak counts were observed during the 2005/06 period: 1,727, 5,000 and 263). In 2006, the realignment did not contain areas of high enough elevation to support breeding waders, as it was completely inundated during spring tides. The adjacent saline lagoon has developed into a habitat of high ornithological value; it provides a home for breeding, roosting and wintering water birds. Avocets bred for the first time in South Lincolnshire on the newly created lagoon islands. Now, around 40 pairs of avocets choose the lagoon to breed each year. Furthermore large flocks of knot roost on the lagoon and nearby reservoir (RSPB website, | |||
2010). | 2010). | ||
Morphology: Whilst overall, the site appears to be draining well, in 2006, some 5.6ha were not draining after the tide has receded, with subsequent implications for sediment stability and vegetation development. In contrast to some other realignment sites (e.g. Tollesbury), creeks in the site were developing through the agricultural soil (Brown et al., 2007). PhD research (Symonds, 2006; Symonds and Collins, 2007) into the impacts of the realignment on intertidal morphology (undertaken at the University of Southampton) found that in the first one to two months following the breaching, the channels created within the breaches increased | |||
'''Morphology''': Whilst overall, the site appears to be draining well, in 2006, some 5.6ha were not draining after the tide has receded, with subsequent implications for sediment stability and vegetation development. In contrast to some other realignment sites (e.g. Tollesbury), creeks in the site were developing through the agricultural soil (Brown et al., 2007). PhD research (Symonds, 2006; Symonds and Collins, 2007) into the impacts of the realignment on intertidal morphology (undertaken at the University of Southampton) found that in the first one to two months following the breaching, the channels created within the breaches increased | |||
substantially from 2m wide by 1m deep to 20m by 4m (see Figure 1a; also visible in Plate 2). However, this initial erosion was restricted to the breaches; it subsequently took almost two yearsof gradual erosion before the channels within the breaches, and the natural saltmarsh creeks they connect to, had eroded to a sufficient volume to allow the site to drain simultaneously with the fronting saltmarsh (and thus reduce the amount of standing water within the site during low water). | substantially from 2m wide by 1m deep to 20m by 4m (see Figure 1a; also visible in Plate 2). However, this initial erosion was restricted to the breaches; it subsequently took almost two yearsof gradual erosion before the channels within the breaches, and the natural saltmarsh creeks they connect to, had eroded to a sufficient volume to allow the site to drain simultaneously with the fronting saltmarsh (and thus reduce the amount of standing water within the site during low water). | ||
In addition to the erosion of the breaches, the managed realignment also directly impacted and creeks over the mid to lower intertidal zones (see Figure 1b). This was caused by the water draining from the managed realignment, following high spring tides, flowing over the intertidal zone as sheetflow and enhancing the natural creek development. This was a temporary effect; once the channels draining the site had reached sufficient dimensions to hold most of the water at most times, the sheetflow diminished considerably and the creeks returned to pre-realignment equilibrium. Unfortunately these changes in intertidal morphology made the area around an oyster farm, located to the south of the site, unstable and ultimately led to the closure of the farm. | In addition to the erosion of the breaches, the managed realignment also directly impacted and creeks over the mid to lower intertidal zones (see Figure 1b). This was caused by the water draining from the managed realignment, following high spring tides, flowing over the intertidal zone as sheetflow and enhancing the natural creek development. This was a temporary effect; once the channels draining the site had reached sufficient dimensions to hold most of the water at most times, the sheetflow diminished considerably and the creeks returned to pre-realignment equilibrium. Unfortunately these changes in intertidal morphology made the area around an oyster farm, located to the south of the site, unstable and ultimately led to the closure of the farm. | ||
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{{Case study subcatchment}} | {{Case study subcatchment | ||
{{Site}} | |Subcatchment=Wash | ||
}} | |||
{{Site | |||
|WFD water body code=GB640523160000 | |||
|WFD (national) typology=coastal | |||
|WFD water body name=Wash Outer | |||
|Heavily modified water body=No | |||
|Protected species present=No | |||
|Invasive species present=No | |||
|Dominant hydrology=Tidal, | |||
}} | |||
{{Project background}} | {{Project background}} | ||
{{Motivations}} | {{Motivations | ||
{{Measures}} | |Specific mitigation=Flood risk management, | ||
}} | |||
{{Measures | |||
|Management interventions=Managed realignment (Three 50m wide breaches were created in the outer sea wall) | |||
}} | |||
{{Hydromorphological quality elements header}} | {{Hydromorphological quality elements header}} | ||
{{End table}} | {{End table}} | ||
Latest revision as of 10:29, 8 May 2015
Project overview
| Status | Complete |
|---|---|
| Project web site | |
| Themes | Habitat and biodiversity |
| Country | England |
| Main contact forename | Susanne |
| Main contact surname | Armstrong |
| Main contact user ID | |
| Contact organisation | |
| Contact organisation web site | |
| Partner organisations | |
| Parent multi-site project | |
| This is a parent project encompassing the following projects |
No |
Project summary
In 1983, HM Prison Service (HMP) claimed 66ha of intertidal habitat to gain land for arable production by building a new seaward defence. During the 1990s, the Environment Agency identified this 1,750m stretch of seawall owned by HMP as at high risk of failure, and following a cost benefit analysis decided to strengthen the old, landward, bank in order to form the flood defence. The Royal Society for the Protection of Birds (RSPB) was very keen to take this opportunity to realign the defences and recreate intertidal habitats, and, following discussions with the Environment Agency, English Nature and HMP, acquired the land.
Prior to the realignment, in 2000, some 1,100m of the remnant landward sea wall were enforced, and a new 500m cross wall built. The material for these works was sourced on site (the borrow pit was later developed into a 15ha saline lagoon). Prior to breaching the sea wall, the vegetation on the 66ha site was cut, baled and removed, field drains were infilled (as far as fill material was available) and some 1,200m of artificial creek system were dug (two channels leading from each breach). Outside the site, some 50m of the external primary creek network were deepened. Finally, three 50m wide breaches were created in the outer sea wall (with channels initially 2m wide and 1m deep).
The site is owned and managed by the Royal Society for the Protection of Birds (RSPB). Its Freiston Shore reserve incorporates the 66ha realignment site, a 15ha saline lagoon and 72ha of wet grassland. Furthermore, Freiston Shore already protects 683ha of saltmarsh and mudflats, which form part of the Wash Special Protection Area (SPA) (RSPB website, 2010).
Monitoring surveys and results
An initial four-year environmental monitoring programme of the site, and adjacent intertidal habitats, has recently concluded (Brown et al., 2007). The majority of the monitoring was undertaken between 2001 and 2006 by the Natural Environment Research Council’s Centre for Ecology and Hydrology (CEH), the Cambridge Coastal Research Unit (CCRU), and Birkbeck College (University of London). It investigated accretion/erosion rates, sediment properties, vegetation colonisation, establishment and succession, invertebrate colonisation, and fish utilisation. Accretion and vegetation was surveyed inside the realignment for an additional (5th) year in 2007 (Brown, 2008). Furthermore, the RSPB undertook monthly bird monitoring (for breeding and water birds, as well as wintering passerines), and the National Oceanographic Centre measured wave activity and tide heights for one year after the breach.
Lessons learnt
Accretion: The recent monitoring reports (Brown et al., 2007; Brown 2008) concluded that in the five years after breaching the sea wall, the Freiston managed realignment site has accreted sediment at similar rates to those of the adjacent salt marsh at the equivalent elevation range. Mean annual accretion rates (after removing a few sites influenced by high deposition of material washed in around the central breach area) ranged between 6 and 10mm per year, and the pattern of natural inter-annual variations inside the realignment matched those outside.
Vegetation: Vegetation establishment and spread have been judged as highly successful, as these have been more rapid than in other (earlier) managed realignment sites. By September 2005, 70% of the area was covered by plants, initially with pioneer species such as glasswort (Salicornia) and and annual sea-blite (Suaeda maritima) dominating. By the second and third year, perennial species such as sea purslane (Halimone portulacoides) and sea aster (Aster tripolium) had become more prevalent (Badley and Allcorn, 2006). It was estimated that the realignment site’s species abundance and community types could be equivalent to those outside the site within a further 5 years. This successful vegetation establishment was attributed mainly to the suitable site elevations and the abundant supply of seeds and tiller fragments from the extensive external salt marsh. Overall, no clear evidence was found to suggest that the realignment site has had any adverse effects on the adjacent saltmarsh in general (Brown et al., 2007).
Invertebrates: The realignment site lies at an elevation suitable for salt marsh establishment therefore most of the invertebrates found were species associated with the developing salt marsh. The nature of the fauna (seasonal and weather-dependent activity of mobile organisms and large variation in numbers of small species) made it difficult to make comparisons between years, or between the realignment site and the adjacent marsh, from an annual survey. However, most species found outside were recorded in the site and many species have increased in abundance (Brown et al., 2007).
Fish: The annual fish surveys showed that at least 11 species utilised the realignment site during the first four years of its existence. It was found to act as an important fish nursery area for several commercially important species (such as bass, sprat, and herring), which were shown to be feeding in the realignment site. The site also provides nursery habitat throughout the entire tidal cycle (i.e. fish continue to use the site when it is disconnected from the sea, with the continuous utilisation of permanently flooded channels). In order to improve the site’s fish nursery function, the addition of shallow pools or pans was recommended along with research into creek configuration(design and density) (Brown et al., 2007).
Birds: Badley and Allcorn (2006) concluded from four years’ of bird monitoring that the realignment supported ‘large numbers of wintering waterbirds, several species in nationally important (i.e. > 1%) of the UK population) numbers’. These include dark-bellied brent goose and golden and grey plover (for which the following respective peak counts were observed during the 2005/06 period: 1,727, 5,000 and 263). In 2006, the realignment did not contain areas of high enough elevation to support breeding waders, as it was completely inundated during spring tides. The adjacent saline lagoon has developed into a habitat of high ornithological value; it provides a home for breeding, roosting and wintering water birds. Avocets bred for the first time in South Lincolnshire on the newly created lagoon islands. Now, around 40 pairs of avocets choose the lagoon to breed each year. Furthermore large flocks of knot roost on the lagoon and nearby reservoir (RSPB website, 2010).
Morphology: Whilst overall, the site appears to be draining well, in 2006, some 5.6ha were not draining after the tide has receded, with subsequent implications for sediment stability and vegetation development. In contrast to some other realignment sites (e.g. Tollesbury), creeks in the site were developing through the agricultural soil (Brown et al., 2007). PhD research (Symonds, 2006; Symonds and Collins, 2007) into the impacts of the realignment on intertidal morphology (undertaken at the University of Southampton) found that in the first one to two months following the breaching, the channels created within the breaches increased substantially from 2m wide by 1m deep to 20m by 4m (see Figure 1a; also visible in Plate 2). However, this initial erosion was restricted to the breaches; it subsequently took almost two yearsof gradual erosion before the channels within the breaches, and the natural saltmarsh creeks they connect to, had eroded to a sufficient volume to allow the site to drain simultaneously with the fronting saltmarsh (and thus reduce the amount of standing water within the site during low water). In addition to the erosion of the breaches, the managed realignment also directly impacted and creeks over the mid to lower intertidal zones (see Figure 1b). This was caused by the water draining from the managed realignment, following high spring tides, flowing over the intertidal zone as sheetflow and enhancing the natural creek development. This was a temporary effect; once the channels draining the site had reached sufficient dimensions to hold most of the water at most times, the sheetflow diminished considerably and the creeks returned to pre-realignment equilibrium. Unfortunately these changes in intertidal morphology made the area around an oyster farm, located to the south of the site, unstable and ultimately led to the closure of the farm.
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