Case study:Logie Burn Restoration Project: Difference between revisions
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{{Case study status | {{Case study status | ||
|Approval status= | |Approval status=Approved | ||
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{{Location | {{Location | ||
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|Contact organisation=Scottish Natural Heritage | |Contact organisation=Scottish Natural Heritage | ||
|Contact organisation url=www.snh.gov.uk/ | |Contact organisation url=www.snh.gov.uk/ | ||
|Partner organisations=SEPA | |||
|Multi-site=No | |Multi-site=No | ||
|Project picture=Logie Burn (before and after) II.jpg | |Project picture=Logie Burn (before and after) II.jpg | ||
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|Project summary=The Logie Burn is graded as poor for its ecological status due to diffuse sediment and nutrient inputs in addition to morphological alteration. These issues are related to agricultural and drainage improvement over many decades that have also led to a deterioration of water quality in Loch Davan into which the Logie Burn flows. | |Project summary=The Logie Burn is graded as poor for its ecological status due to diffuse sediment and nutrient inputs in addition to morphological alteration. These issues are related to agricultural and drainage improvement over many decades that have also led to a deterioration of water quality in Loch Davan into which the Logie Burn flows. | ||
During the 1960s, two meanders in a lower part of the channel were cut-off through the creation of a straight | During the 1960s, two meanders in a lower part of the channel were cut-off through the creation of a straight 187 m reach leading to a localised loss of morphological and habitat diversity. The restoration project aimed to re-connect the two old meanders that had filled in with fine sediment and organic material but which essentially remained intact. The primary purposes of the re-connection were to restore morphology, improve habitat quality in the National Nature Reserve, improve water quality and reduce sedimentation in Loch Davan, enhance riparian habitat diversity and demonstrate this meander restoration to river managers. It is expected that the reconnected meanders and newly created backwaters will help to capture nutrient rich fine sediment and in turn reduce its transfer into Loch Davan. | ||
A monitoring program conducted by the James Hutton Institute, commenced in July 2011 to assess how the morphology, habitat, phosphorous storage and the flood attenuation capacity of the reach change over time. Topographical and sedimentary surveys were undertaken before and after the re-connection and will be repeated annually. In addition, stream flow is being continuously monitored to allow assessment of the flood attenuation capacity and to help understand the morphological changes observed. In 2012, a control reach upstream was established to facilitate comparison of changes in the impact (re-meandered) reach with those that | A monitoring program conducted by the James Hutton Institute, commenced in July 2011 to assess how the morphology, habitat, phosphorous storage and the flood attenuation capacity of the reach change over time. Topographical and sedimentary surveys were undertaken before and after the re-connection and will be repeated annually. In addition, stream flow is being continuously monitored to allow assessment of the flood attenuation capacity and to help understand the morphological changes observed. In 2012, a control reach upstream was established to facilitate comparison of changes in the impact (re-meandered) reach with those that occur within the existing, degraded stream. | ||
The River Restoration Centre would like to thank Estelle Gill and Stephen Addy, from Scottish Natural Heritage and The James Hutton Institute respectively, for providing the information and photographs for this case study. | The primary funder for the project was the Scottish Environment Protection Agency (SEPA). If you are interested in applying for funding to deliver other projects in Scotland, visit SEPA's Water Environment Fund webpage (http://www.sepa.org.uk/water/water_environment_fund.aspx). The River Restoration Centre would like to thank Estelle Gill and Stephen Addy, from Scottish Natural Heritage and The James Hutton Institute respectively, for providing the information and photographs for this case study. | ||
|Monitoring surveys and results=The first three years of monitoring are published in the following journal article: | |||
https://www.sciencedirect.com/science/article/pii/S0925857419300370 | |||
The data from this study are available from PANGAEA: | |||
https://doi.pangaea.de/10.1594/PANGAEA.898301 | |||
Monitoring work funded by the Scottish Government (RESAS) at the site is ongoing to give a long term (10 years) assessment of the project. | |||
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{{Case study subcatchment | |||
|Subcatchment=Dee (Scotland) | |||
}} | |||
{{Site | |||
|Name=Logie Burn | |||
|WFD water body code=23372 | |||
|WFD (national) typology=Mid-altitude, Small, Calcareous | |||
|WFD water body name=Logie Burn / Loch Davan | |||
|Pre-project morphology=Straightened, Single channel, | |||
|Reference morphology=Low gradient passively meandering, Single channel, | |||
|Heavily modified water body=No | |||
|Site designation=UK - National Parks, Special Area of Conservation | |||
|Local site designation=National Reserve, | |||
|Protected species present=Yes | |||
|Invasive species present=No | |||
|Species=Brook lamprey, Atlantic salmon (Salmo salar), Brown trout (Salmo trutta), | |||
|Dominant substrate=Fines, fine gravel, organic material | |||
|River corridor land use=Improved/semi-improved grassland/pasture, Broadleaf/mixed woodland (semi natural), | |||
|Average bankfull channel width category=5 - 10 m | |||
|Avrg bankfull channel width=5.6 | |||
|Average bankfull channel depth category=0.5 - 2 m | |||
|Avrg1 bankfull channel depth=0.48 | |||
|Mean discharge category=0.1 - 1.0 m³/s | |||
|Average channel gradient category=Less than 0.001 | |||
|Avrg channel gradient=0.0016 | |||
|Avrg unit stream power=3.44 | |||
}} | |||
{{Project background | |||
|Reach length directly affected=250 | |||
|Works started=2011/09/09 | |||
|Works completed=2011/10/15 | |||
|Funding sources=Scottish Environment Protection Agency, Scottish Natural Heritage | |||
|Monitoring Lead organisation=The James Hutton Institute | |||
|Monitoring Other contact forename=Stephen | |||
|Monitoring Other contact surname=Addy | |||
}} | |||
{{Motivations | |||
|Specific mitigation=Land drainage, | |||
|Hydromorphological quality elements=Continuity for organisms, Continuity of sediment transport, Quantity & dynamics of flow, Structure & condition of riparian/lake shore zones, Substrate conditions, | |||
|Biological quality elements=Macrophytes, lampreys, Atlantic salmon | |||
|Physico-chemical quality elements=Nutrient concentrations, | |||
|Other motivation=Demonstrate this type of restoration to river managers | |||
}} | |||
{{Measures | |||
|Bank and bed modifications measure=Re-profiling, construction of bunds, Creation of revetments, Bank stabilisation, Bank protection, | |||
|Floodplain / River corridor=Creation of backwaters, Creation of wetland, Livestock fencing, Fencing, | |||
|Planform / Channel pattern=Re-meandering | |||
|Other technical measure=The meanders were cleared of sediment, vegetation and organic debris | |||
|Wider stakeholder / citizen engagement=Information board erected, | |||
}} | |||
{{Hydromorphological quality elements header}} | |||
{{Hydromorphological quality element table row | |||
|Element=Flow velocities | |||
|Monitored before=Yes | |||
|Monitored after=Yes | |||
|Qualitative monitoring=No | |||
|Quantitative monitoring=Yes | |||
|Control site used=Yes | |||
|Result=Awaiting results | |||
}} | |||
{{Hydromorphological quality element table row | |||
|Element=Quantity & dynamics of flow | |||
|Monitored before=Yes | |||
|Monitored after=Yes | |||
|Qualitative monitoring=No | |||
|Quantitative monitoring=Yes | |||
|Control site used=No | |||
|Result=Awaiting results | |||
}} | |||
{{Hydromorphological quality element table row | |||
|Element=Width & depth variation | |||
|Monitored before=Yes | |||
|Monitored after=Yes | |||
|Qualitative monitoring=No | |||
|Quantitative monitoring=Yes | |||
|Control site used=Yes | |||
|Result=Awaiting results | |||
}} | |||
{{Hydromorphological quality element table row | |||
|Element=Substrate conditions | |||
|Monitored before=Yes | |||
|Monitored after=Yes | |||
|Qualitative monitoring=No | |||
|Quantitative monitoring=Yes | |||
|Control site used=Yes | |||
|Result=Awaiting results | |||
}} | |||
{{Hydromorphological quality element table row | |||
|Element=Continuity of sediment transport | |||
|Monitored before=Yes | |||
|Monitored after=Yes | |||
|Qualitative monitoring=No | |||
|Quantitative monitoring=Yes | |||
|Control site used=No | |||
|Result=Awaiting results | |||
}} | |||
{{End table}} | |||
{{Biological quality elements header}} | |||
{{Biological quality element table row | |||
|Element=Fish | |||
|Monitored before=No | |||
|Monitored after=Yes | |||
|Qualitative monitoring=Yes | |||
|Quantitative monitoring=No | |||
|Control site used=No | |||
}} | |||
{{End table}} | |||
{{Physico-chemical quality elements header}} | |||
{{Physico-chemical quality element table row | |||
|Element=Nutrient concentrations | |||
|Monitored before=Yes | |||
|Monitored after=Yes | |||
|Qualitative monitoring=No | |||
|Quantitative monitoring=Yes | |||
|Control site used=Yes | |||
|Result=Awaiting results | |||
}} | |||
{{End table}} | |||
{{Other responses header}} | |||
{{End table}} | |||
{{Monitoring documents}} | |||
{{Monitoring documents end}} | |||
{{Additional Documents}} | {{Additional Documents}} | ||
{{Additional Documents end}} | {{Additional Documents end}} | ||
{{Additional links and references header}} | {{Additional links and references header}} | ||
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|Link=http://www.therrc.co.uk/2012%20Conference/Outputs/Gill%20Final.pdf | |Link=http://www.therrc.co.uk/2012%20Conference/Outputs/Gill%20Final.pdf | ||
|Description=Gill, E.; Cooksley, S.; Janes, M. and Reid, C. (2012) The Logie Burn Restoration Project: In the RRC 13th Annual Conference | |Description=Gill, E.; Cooksley, S.; Janes, M. and Reid, C. (2012) The Logie Burn Restoration Project: In the RRC 13th Annual Conference | ||
}} | |||
{{Additional links and references | |||
|Link=https://www.sciencedirect.com/science/article/pii/S0925857419300370 | |||
|Description=Addy, S. and Wilkinson, M.E. (2019) Geomorphic and retention responses following the reconnection of a sand-gravel bed stream. Ecological Engineering, 130. P 131-146. https://doi.org/10.1016/j.ecoleng.2019.01.013 | |||
}} | |||
{{Additional links and references | |||
|Link=https://doi.pangaea.de/10.1594/PANGAEA.898301 | |||
|Description=Addy, Stephen; Wilkinson, Mark E (2019): Geomorphic, discharge and substrate river restoration monitoring data from the Logie Burn, Scotland (2011 to 2014). PANGAEA, https://doi.org/10.1594/PANGAEA.898301 | |||
}} | }} | ||
{{Additional links and references footer}} | {{Additional links and references footer}} | ||
{{Supplementary Information}} | {{Supplementary Information}} | ||
{{Toggle content end}} |
Latest revision as of 14:43, 25 February 2019
Project overview
Status | Complete |
---|---|
Project web site | |
Themes | Flood risk management, Habitat and biodiversity, Hydromorphology, Monitoring, Water quality |
Country | Scotland |
Main contact forename | Estelle |
Main contact surname | Gill |
Main contact user ID | |
Contact organisation | Scottish Natural Heritage |
Contact organisation web site | http://www.snh.gov.uk/ |
Partner organisations | SEPA |
Parent multi-site project | |
This is a parent project encompassing the following projects |
No |
Project summary
The Logie Burn is graded as poor for its ecological status due to diffuse sediment and nutrient inputs in addition to morphological alteration. These issues are related to agricultural and drainage improvement over many decades that have also led to a deterioration of water quality in Loch Davan into which the Logie Burn flows.
During the 1960s, two meanders in a lower part of the channel were cut-off through the creation of a straight 187 m reach leading to a localised loss of morphological and habitat diversity. The restoration project aimed to re-connect the two old meanders that had filled in with fine sediment and organic material but which essentially remained intact. The primary purposes of the re-connection were to restore morphology, improve habitat quality in the National Nature Reserve, improve water quality and reduce sedimentation in Loch Davan, enhance riparian habitat diversity and demonstrate this meander restoration to river managers. It is expected that the reconnected meanders and newly created backwaters will help to capture nutrient rich fine sediment and in turn reduce its transfer into Loch Davan.
A monitoring program conducted by the James Hutton Institute, commenced in July 2011 to assess how the morphology, habitat, phosphorous storage and the flood attenuation capacity of the reach change over time. Topographical and sedimentary surveys were undertaken before and after the re-connection and will be repeated annually. In addition, stream flow is being continuously monitored to allow assessment of the flood attenuation capacity and to help understand the morphological changes observed. In 2012, a control reach upstream was established to facilitate comparison of changes in the impact (re-meandered) reach with those that occur within the existing, degraded stream.
The primary funder for the project was the Scottish Environment Protection Agency (SEPA). If you are interested in applying for funding to deliver other projects in Scotland, visit SEPA's Water Environment Fund webpage (http://www.sepa.org.uk/water/water_environment_fund.aspx). The River Restoration Centre would like to thank Estelle Gill and Stephen Addy, from Scottish Natural Heritage and The James Hutton Institute respectively, for providing the information and photographs for this case study.
Monitoring surveys and results
The first three years of monitoring are published in the following journal article:
https://www.sciencedirect.com/science/article/pii/S0925857419300370
The data from this study are available from PANGAEA:
https://doi.pangaea.de/10.1594/PANGAEA.898301
Monitoring work funded by the Scottish Government (RESAS) at the site is ongoing to give a long term (10 years) assessment of the project.
Lessons learnt
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Catchment and subcatchmentSelect a catchment/subcatchment
Catchment
Subcatchment
Site
Project background
Cost for project phases
Reasons for river restoration
Measures
MonitoringHydromorphological quality elements
Biological quality elements
Physico-chemical quality elements
Any other monitoring, e.g. social, economic
Monitoring documents
Additional documents and videos
Additional links and references
Supplementary InformationEdit Supplementary Information
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