11. Geology, Hydrology, Soils & Flood Risk

11.1.   Introduction

11.1. Introduction

  1. This chapter presents the assessment of the likely significant effects on the environment of the Berwick Bank Wind Farm onshore transmission works (OnTW) (the Proposed Development) on Geology, Hydrology, Soils & Flood Risk. Specifically, this chapter considers the potential impact of the Proposed Development landward of Mean Low Water Springs (MLWS) during the construction, operational and maintenance, and decommissioning phases.
  2. This chapter summarises information contained within Volume 4, Appendix 11.1 (Berwick Bank Wind Farm: Flood Risk Assessment) and Appendix 11.2 (Berwick Bank Wind Farm: Drainage Strategy).

11.2.   Purpose of this Chapter

11.2. Purpose of this Chapter

  1. This chapter:
  • Presents the existing environmental baseline established from desk studies, site-specific surveys and consultation with stakeholders;
  • Identifies any assumptions and limitations encountered in compiling the environmental information;
  • Presents the potential environmental impacts on geology, hydrology, soils & flood risk arising from the Proposed Development, and reaches a conclusion on the likely significant effects on geology, hydrology, soils & flood risk  based on the information gathered and the analysis and assessments undertaken; and
  • Highlights any necessary monitoring and/or mitigation measures recommended to prevent, minimise, reduce or offset the likely significant adverse environmental effects of the Proposed Development on geology, hydrology, soils & flood risk.

11.3.   Study Area

11.3. Study Area

  1. The geology, hydrology, soils & flood risk study area will cover the Proposed Development site and any potential effects up to 1 km from the site (refer to Volume 4, Figure 11.1   Open ▸ ). It is considered that this geology, hydrology, soils & flood risk typical study area buffer distance is appropriate considering the size of the development and allows potential effects on downstream receptors to be identified. The geology, hydrology, soils & flood risk study area includes the intertidal area and considers potential effects on offshore receptors that may arise as a result of the upgradient works.

11.3.1.              Intertidal Area

  1. The planning application boundary for the Application extends to MLWS.  The infrastructure to be located between Mean High Water Springs (MHWS) and MLWS consists of cables to be installed via trenchless technology (e.g. horizontal directional drilling (HDD)).  Impacts associated with this infrastructure have been assessed in the Offshore EIA Report (Volume 2, Chapter 7), although given the commitment to use trenchless technology no likely significant effects have been predicted.
  2. The Offshore EIA Report is available online at the Berwick Bank Wind Farm website; www.berwickbank.com. An electronic copy has been submitted to East Lothian Council Planning Department.
  3. The potential effects of the onshore infrastructure located above MHWS on the intertidal area have been assessed in this chapter.

11.4.   Policy and Legislative context

11.4. Policy and Legislative context

  1. A summary of the policy provisions relevant to Geology, Hydrology, Soils & Flood Risk are provided in Table 11.1   Open ▸ below. A summary of the relevant legislative provisions are provided in Table 11.2   Open ▸ below.
Table 11.1:
Summary of Scottish Policy and East Lothian Policy (Local Development Plan (LDP) 2018) Relevant to Geology, Hydrology, Soils & Flood Risk

Table 11.1:  Summary of Scottish Policy and East Lothian Policy (Local Development Plan (LDP) 2018) Relevant to Geology, Hydrology, Soils & Flood Risk

 

Table 11.2:
Summary of Legislative Provisions Relevant to Geology, Hydrology, Soils & Flood Risk

Table 11.2: Summary of Legislative Provisions Relevant to Geology, Hydrology, Soils & Flood Risk

11.5.   Consultation

11.5. Consultation

  1. A summary of the key issues raised during consultation activities undertaken to date specific to geology, hydrology, soils & flood risk is presented in Table 11.3   Open ▸ below, together with how these issues have been considered in the production of this Geology, Hydrology, Soils & Flood Risk chapter. Further detail is presented within Volume 1, Chapter 2 of the Onshore EIA Report and the Pre-Application Consultation (PAC) Report.

 

Table 11.3:
Summary of Key Consultation Undertaken for the Proposed Development Relevant to Geology, Hydrology, Soils & Flood Risk

Table 11.3:  Summary of Key Consultation Undertaken for the Proposed Development Relevant to Geology, Hydrology, Soils & Flood Risk

11.6.   Methodology to Inform Baseline

11.6. Methodology to Inform Baseline

  1. This section sets out a summary of the methodology to inform the analysis of the baseline within the geology, hydrology, soils & flood risk study area.
  2. A desk-based assessment has been undertaken to establish the catchments’ characteristics and baseline geological and hydrological conditions of the geology, hydrology, soils & flood risk study area. As part of the desk-based assessment, information regarding Private Water Supplies (PWS), historic landfill sites, water quality and flood risk data, abstraction licences and monitoring locations have been obtained to inform the assessment. Where available, classification of waterbodies has been referenced as determined by SEPA through River Basin Management Planning, under the Water Framework Directive.
  3. Site surveys have been undertaken to further assess baseline conditions from information gathered from the desk-based assessment. Site surveys included a hydrological / geological walkover, watercourse assessments and flood risk assessments.

11.6.1.              Desktop Study

  1. Information on geology, hydrology, soils & flood risk within the geology, hydrology, soils & flood risk study area was collected through a detailed desktop review of existing studies and datasets. These are summarised in Table 11.4   Open ▸ below.
Table 11.4:
Summary of Key Desktop Studies & Datasets

Table 11.4:  Summary of Key Desktop Studies & Datasets

11.6.2.              Site-Specific Surveys

  1. To inform the Geology, Hydrology, Soils & Flood Risk chapter, site-specific surveys were undertaken. A summary of the surveys undertaken to inform the geology, hydrology, soils & flood risk assessment of effects is outlined in Table 11.5   Open ▸ below.
Table 11.5:
Summary of Site-Specific Survey Data

Table 11.5:  Summary of Site-Specific Survey Data

11.7.   Baseline Environment

11.7. Baseline Environment

11.7.1.              Overview of Baseline Environment

  1. This section sets out a summary of relevant baseline data for the geology, hydrology, soils & flood risk study area under the following headings:
  • Hydrology;
  • Water Resources;
  • Hydrogeology;
  • Flood Risk;
  • Geology;
  • Soils; and
  • Other Designated Sites.

Hydrology

Surface Water Catchments
  1. The geology, hydrology, soils & flood risk study area is situated within six surface water catchments as shown in SEPA’s Baseline Confluence Nested Catchments data file;
  • East Lothian Coastal between Dry Burn and Spott Burn (ID 12575);
  • Dry Burn @ mouth (ID 18113);
  • East Lothian Coastal between Thornton Burn and Dry Burn (ID 12687);
  • Thornton Burn @ mouth (ID 13453);
  • East Lothian Coastal between Dunglass Burn and Thornton Burn (ID 19745); and
  • Dunglass Burn @ mouth (ID 16994).
    1. An overview of the surface water catchments is provided in Volume 2, Figure 11.2   Open ▸
    2. Of the above catchments “East Lothian Coastal between Dry Burn and Spott Burn” and “Dunglass Burn @ mouth” are outwith the site and not hydraulically connected with the Proposed Development.
    3. The “Dry Burn @ mouth” catchment is approximately 19 km2 and the Dry Burn watercourse is classified by SEPA as being of ‘Moderate’ status (SEPA, 2020). The north western extents of the Proposed Development are located within the “Dry Burn @ mouth” catchment. A small number of minor unnamed tributaries to the Dry Burn are located within the geology, hydrology, soils & flood risk study area.
    4. The “East Lothian Coastal catchment between Thornton Burn and Dry Burn” is approximately 4km2. The main watercourse in this catchment is unnamed and originates from the agricultural land to the west of Innerwick and flows to the settlement of Skateraw. The watercourse (hereafter referred to as the Innerwick Burn) is not classified by SEPA. The Innerwick Burn has been surveyed for the purpose of informing the drainage strategy for the onshore substation and it has been identified that it is heavily modified with multiple culverts and discharges to the Dry Burn to the north of the settlement of Skateraw. The onshore substation is located within this catchment area. No other watercourses are located within this catchment.
    5. The “Thornton Burn @ mouth” catchment is approximately 14 km2 and is classified by SEPA as being of ‘Good’ status (SEPA, 2020). The main watercourse within the catchment is known as the Thornton Burn within the downstream reaches. Within the geology, hydrology, soils & flood risk study area, the Thornton Burn is also known as the Braidwood Burn (predominant watercourse) and the Ogle Burn (tributary to the Braidwood Burn) is located further upstream near to Thorntonloch. The southern extents of the Proposed Development are located within this catchment.
    6. The “East Lothian Coastal between Dunglass Burn and Thornton Burn” catchment is approximately 17 km2 with no named watercourses present. Several minor unnamed watercourses are present draining the catchment area to the coastline. The southern extents of the site are located within this catchment but no Proposed Development is located within this catchment with the exception of a short section of access track to the proposed Branxton grid substation. This short section of track is located within the western extents of the catchment.
    7. The coastal waters at the site are classified by SEPA under the Barns Ness to Wheat Stack coastal water body and are considered to be of Good status (SEPA, 2020).
    8. Thorntonloch Beach is a Bathing Waters protected area, classified as being of Excellent status (SEPA, 2020). No Proposed Development infrastructure is located in the vicinity of the Bathing Waters but development is located within the catchment of the Thornton Burn which drains to the Bathing Waters.  

Water Resources

Public Water Supplies
  1. In the scoping response, Scottish Water confirmed there are no Scottish Water drinking water catchments or water abstraction sources, which are designated as Drinking Water Protected Areas under the Water Framework Directive, within the geology, hydrology, soils & flood risk study area. The geology, hydrology, soils & flood risk study area is located within a groundwater Drinking Water Protected Area (DWPA) – as is the case for the majority of Scotland with the exception of the Scottish Borders and Dumfries and Galloway council areas.
Private Water Supplies
  1. In response to a Freedom of Information (FOI) consultation request ELC provided the details of PWS within 5 km of the coordinates X 374080, Y 673982 (the centre of the site). ELC identified nine PWS supplies serving a total of 28 properties and one factory.
  2. All supplies are located outside of the geology, hydrology, soils & flood risk study area, inland and therefore upgradient of the site. The closest PWS is located over 1.4km from the site.
SEPA CAR Abstractions
  1. In the scoping response ELC note “The nearest SEPA licensed groundwater abstractions (CAR/S/1014268) is ~320m north of the proposed Skateraw and Crowhill substation locations on the opposite side of the railway line and trunk road. The next nearest licensed or registered groundwater abstractions are over 2km away at Dunbar Cement Works.” CAR/S/1014268 is recorded by SEPA as a “pumping test” in the received information from the FOI and is located within the geology, hydrology, soils & flood risk study area and site. The Dunbar Cement Works is not located within the geology, hydrology, soils & flood risk study area.
  2. Locations of PWSs and abstraction locations are provided in Volume 2, Figure 11.3   Open ▸

Hydrogeology

Aquifer Classification
  1. The geology, hydrology, soils & flood risk study area is situated within Torness (bedrock) and Torness Coastal (superficial) aquifers. The aquifers are classified as having Good status (SEPA, 2020).
Aquifer Productivity
  1. The geology, hydrology, soils & flood risk study area is underlain by moderately productive aquifers.
  2. Aquifer flow within the geology, hydrology, soils & flood risk study area is described as virtually all through fractures and other discontinuities.
  3. A summary of the hydrogeology within the geology, hydrology, soils & flood risk study area is provided in Volume 2, Figure 11.4   Open ▸
Groundwater Dependent Terrestrial Ecosystems
  1. The geology, hydrology, soils & flood risk study area does not contain any peatlands or wetlands. Therefore no Groundwater Dependent Terrestrial Ecosystems (GWDTE) are present.

Flood Risk

  1. A Flood Risk Assessment (FRA) has been carried out and included as Volume 4, Appendix 11.1.
  2. All potential sources of flooding to the site have been considered with respect to the following Proposed Development permanent infrastructure:
  • Landfall,
  • Cable Route and
  • Onshore Substation.
    1. Assessment of flood risk to the landfall is confirmed to be overall at ‘no risk’ or ‘low risk’ of flooding from all sources. Following initial screening, further assessment was undertaken to accurately determine the coastal flood extent in relation to the landfall which was found to be at ‘low risk’ from coastal flooding.
    2. Assessment of flood risk to the cable route is confirmed to be overall at ‘no risk’ or ‘low risk’ of flooding from all sources. Following initial screening, further assessment was undertaken to determine the fluvial flood risk in relation to the cable route watercourse crossings which were found to be at ‘negligible risk’ from fluvial flooding.  
    3. Assessment of flood risk to the onshore substation is confirmed to be, with mitigation applied, overall at ‘low risk’ of flooding from land or from sewers / artificial drains, and at ‘no risk’ of flooding from all other sources (see Volume 4, Appendix 11.2).

Geology

Bedrock Geology
  1. Review of the BGS 1:50k geological mapping indicates the very west of the geology, hydrology, soils & flood risk study area is underlain by Great Conglomerate Formation consisting of conglomerate and sandstone and Stratheden Group and Inverclyde Group consisting of sandstone and argillaceous rocks in the very south west.
  2. The majority of the southern and central area of the geology, hydrology, soils & flood risk study area is underlain by the Ballagan Formation consisting of Sandstone, Siltstone and Dolomitic Limestone.
  3. The bedrock geology in the north of the geology, hydrology, soils & flood risk study area is dominated by various limestone units including Hurlet Limestone, Lower Limestone Formation (consisting of Limestone, Argillaceous Rocks and Subordinate Sandstone), Blackhall Limestone and Main Hosie Limestone.
  4. Several faults are recorded across the geology, hydrology, soils & flood risk study area, predominantly in the northern areas and along the western and southern extents.
  5. An overview of the bedrock geology within the geology, hydrology, soils & flood risk study area is provided in Volume 2, Figure 11.5   Open ▸
Superficial Geology
  1. Review of the BGS 1:50k geological mapping indicates the very west of the geology, hydrology, soils & flood risk study area is underlain by predominantly Till deposits with some areas of Alluvial deposits along watercourse extents.
  2. Glaciofluvial Deposits - Gravel, Sand and Silt is the dominating superficial deposit across the remainder of the geology, hydrology, soils & flood risk study area in addition to Alluvial deposits along watercourse extents and Raised Marine deposits Of Holocene Age - Sand and Gravel, Marine Beach Deposits - Gravel, Sand and Silt and Blown Sand along areas of the coastline.
  3. Areas of no superficial deposits are also recorded, primarily at the steep sides of watercourses.
  4. Review of the BGS 1:50k geological mapping indicates the intertidal area is underlain by Marine Beach Deposits - Gravel, Sand and Silt and Blown Sand along areas of the coastline and Raised Marine Deposits Of Holocene Age - Sand and Gravel, as well as areas where no superficial deposits are recorded.
  5. An overview of the superficial geology within the geology, hydrology, soils & flood risk study area is provided in Volume 2, Figure 11.6   Open ▸ : Superficial Geology.
Review of Ground Investigation Information
  1. A site-wide ground investigation was undertaken in September 2020 (report published January 2021) to inform the Proposed Development layout and design. The results of the ground investigation broadly concur with the published geology from BGS. Bedrock was generally encountered at depths between 3 – 10m and its nature varied dependent on the location, similar to the BGS findings. Superficial deposits were confirmed to be Glaciofluvial in nature, generally with considerable clay content and poor infiltration capacity. No ‘made ground’ was encountered and no indication of any ground contamination. A potential source of contamination has been identified at the area defined as the ‘Skateraw Borrow Pit’. Further ground investigation undertaken in 2022 identified pulverised fuel ash (PFA) within the subsoil. Further chemical composition testing of the PFA will be undertaken to determine the level of contamination. This further analysis will inform the approach to manage the contamination, which will be determined post consent and agreed with ELC and other relevant stakeholders prior to the commencement of construction.
Mineral Reserves
  1. Existing and historic quarries are present across ELC for the extraction of hard rock, limestone and sands and gravels. Skateraw quarry lies within the geology, hydrology, soils & flood risk study area, previously used for extraction of sands and gravels. Planning permission was originally granted in 2001 with an extension in 2011. The planning consent for the quarry expired in 2017.
  2. No hard rock or limestone quarries are present within the geology, hydrology, soils & flood risk study area.
  3. The superficial deposits and bedrock geology underlying the Proposed Development are widely present within the geology, hydrology, soils & flood risk study area and beyond.
Geologically Designated Sites
  1. The landfall passes through the Barns Ness Coast Site of Special Scientific Interest (SSSI) and Geological Conservation Review Site. This is designated for the presence of biologically important habitats and for Lower Carboniferous Limestone which is rich in fossils. This geology is of particular interest as there is an exposed almost complete, though heavily faulted, section through the whole lower limestone group. The Landfall location avoids the ‘crucial areas’ of the feature (a term defined in the EIA Scoping Opinion (Volume 4, Appendix 2.2).
  2. The use of trenchless technology (e.g. HDD) from offshore to onshore transition allows for the landfall site and transition pits to be located inland of the Barns Ness Coast SSSI. In addition, the use of trenchless technology will ensure that the works will pass underneath the SSSI as agreed within the EIA Scoping Opinion (Volume 4, Appendix 2.2).
  3. The Local Geodiversity Site at Thorntonloch is located within the geology, hydrology, soils & flood risk study area, and is a very good example of rock coast landforms in sedimentary rocks. The Local Geodiversity Site is not within the site boundary and no Proposed Development works will be undertaken near to this location.
  4. Locations of the relevant designated sites are provided in Volume 2, Figure 11.7   Open ▸ Designated Sites.

Soils

  1. The geology, hydrology, soils & flood risk study area is located in predominantly agricultural land. Impacts on agriculture are included in Land Use, Tourism and Recreation Volume 1, Chapter 14.
  2. Soils within the geology, hydrology, soils & flood risk study area are predominantly classified within the generalised soil type of Brown Soils, with isolated areas of mineral gleys and alluvial soils.
  3. Topsoil compaction risk within the geology, hydrology, soils & flood risk study area (Volume 2, Figure 11.9) is predominantly moderate, interspersed with areas of high risk.
  4. Subsoil compaction risk within the geology, hydrology, soils & flood risk study area (Volume 2, Figure 11.10   Open ▸ ) ranges from moderate to extreme. Areas of extreme vulnerability are predominantly within the area of the site around the A1 and East Coast Main Line, and along the Braidwood Burn.
  5. Soil runoff risk within the geology, hydrology, soils & flood risk study area (Volume 2, Figure 11.11) is predominantly low to moderate.

11.7.2.              Future Baseline Scenario

  1. The Town and Country Planning (Environmental Impact Assessment) (Scotland) Regulations 2017, require that a “a description of the relevant aspects of the current state of the environment (the “baseline scenario”) and an outline of the likely evolution thereof without development as far as natural changes from the baseline scenario can be assessed with reasonable effort on the basis of the availability of relevant information and scientific knowledge” is included within the Onshore EIA Report.
  2. In order to ensure that the Proposed Development is assessed against a realistic baseline scenario, i.e. what the baseline conditions are likely to be once the Proposed Development is operational, a description of the likely future baseline conditions is provided within this section.
  3. The relevant climate change projections using the UK Climate Change Projections 2018 (UKCP18) are:
  • winter rainfall is projected to increase and summer rainfall is most likely to decrease; and
  • an increase in frequency of winter storms over the UK.
    1. Increased winter rainfall and increased frequency of winter storms may increase the probability of flood risk and drainage systems may require increased capacity.
    2. Decrease in summer rainfall may affects water supplies dependent on local rainfall, surface water and / or groundwater.
    3. SEPA’s most recent climate change allowances guidance published in 2022 are partially based on UKCP18 findings and provides climate change allowances for sea level rise, rainfall intensity and river flows for Scotland. Relevant allowances for all types of flooding described have been used within the assessment and in the FRA and surface water drainage design.
    4. The relevant climate change allowances for the Proposed Development which is situated in the Forth River Basin are:
  • Peak river flow allowance: Total change to 2100 – 56%
  • Seal level rise allowance: Cumulative rise from 2017 to 2100 in metres – 0.86
  • Peak rainfall intensity allowance: Total change to 2100 – 39%

11.7.3.              Data Assumptions And Limitations

  1. Data limitations include:
  • No water quality or flow monitoring has been undertaken to date. Baseline water quality monitoring is typically undertaken 12 months prior to commencement of construction (i.e., post consent).
  • The Flood Estimation Handbook (FEH) Web service, used for determining catchment characteristics, only analyses catchments greater than 0.5 km2 and does not account for any in-channel artificial modifications to watercourses (i.e. culverting, weirs etc).
  • SEPA do not provide flood risk mapping for watercourses with a total catchment area of less than 3km2 or water framework directive (WFD) classification for watercourses with a total catchment area of less than 10km2 (unless they require specific management).

11.8.   Key Parameters for Assessment

11.8. Key Parameters for Assessment

11.8.1.              Maximum Design Scenario

  1. The maximum design scenario(s) summarised here have been selected as those having the potential to result in the greatest effect on an identified receptor or receptor group. These scenarios have been selected from the details provided in Volume 1, Chapter 5 of the Onshore EIA Report. Effects of greater adverse significance are not predicted to arise should any other development scenario, based on details within the Project Design Envelope (e.g. different infrastructure layout), to that assessed here, be taken forward in the final design scheme.
  2. The geology, hydrology, soils & flood risk assessment has been based on the maximum Proposed Development footprint and areas of temporary infrastructure along with a construction programme of 40 months. Assessment of flood risk has been on 1 in 200 year return period flood events with associated climate change uplifts.
  3. This assessment has considered the following potential impacts:
  • temporary direct impacts to statutory designated sites due to the maximum temporary footprint of the Proposed Development during construction;
  • changes to natural drainage patterns due to construction activities;
  • temporary increase in erosion of soils due to construction activities;
  • increase in flood risk due to construction activities and the maximum temporary and permanent infrastructure footprint;
  • pollution of watercourses and waterbodies due to surface water runoff during construction, operation, and decommissioning; and
  • indirect impacts on private and public water supplies.

11.8.2.              Impacts Scoped out of the Assessment

  1. Impacts scoped out of the assessment were agreed with key stakeholders through consultation within the Scoping Opinion or through the additional information provided in the Section 11.7 Baseline Environment within this chapter. Section 11.7 summarises the Baseline Environment specific to areas of Proposed Development, therefore enabling an assessment of potential pathways to be undertaken and more accurately determine potential impacts in comparison to the Scoping Report (which was assessed on the full site boundary). These, together with a justification, are presented in Table 11.6   Open ▸ .
Table 11.6:
Impacts Scoped Out of the Assessment for Geology, Hydrology, Soil and Flood Risk (tick confirms impacts scoped out)

Table 11.6:  Impacts Scoped Out of the Assessment for Geology, Hydrology, Soil and Flood Risk (tick confirms impacts scoped out)

11.9.   Methodology For Assessment of Effects

11.9. Methodology For Assessment of Effects

11.9.1.              Overview

  1. The geology, hydrology, soils & flood risk assessment of effects has followed the methodology set out in Volume 1, Chapter 2 of the Onshore EIA Report. Specific to the assessment of geology, hydrology, soils & flood risk, the following guidance documents have also been considered:
  • Pollution Prevention Guidelines (PPGs) are a series of documents developed by the Environment Agency for England and Wales, the Northern Ireland Environment Agency (NIEA) for Northern Ireland, and SEPA for Scotland. A review plan for PPGs is currently underway, resulting in a replacement guidance series, titled Guidance for Pollution Prevention (GPPs). GPPs provide good practice guidance for the whole of the UK, and environmental regulatory guidance to Scotland, Wales and Northern Ireland. The following PPGs and GPPs have been considered to be of particular relevance as part of this assessment:

           PPG1: General guide to the prevention of pollution (EA, SEPA & EHSNI, 2013);

           GPP2: Above ground oil storage tanks (EA, SEPA & EHSNI, January 2018);

           GPP5: Works and maintenance in or near water (EA, SEPA & EHSNI, January 2017);

           PPG6: Working at construction and demolition sites (EA, SEPA & EHSNI, 2012); and

           GPP21: Pollution incidence response planning (EA, SEPA & EHSNI, 2017).

  • SEPA Supporting Guidance (SAT-SG-75) – Sector specific guidance: construction sites (SEPA, 2018);
  • SEPA (2010) Engineering in the Water environment: Good Practice Guide, River Crossing, 2nd Edition;
  • SEPA Guidance Note 2a: Development Management Guidance on Flood Risk (2018)
  • SEPA Guidance Note 31: Guidance on Assessing the Impacts of Development Proposals on Groundwater Abstractions and Groundwater Dependent Terrestrial Ecosystems (2017);
  • SEPA Policy 19: Groundwater Protection Policy for Scotland (Version 3, 2009);
  • SEPA Policy 41: Planning Authority Protocol - Development at Risk of Flooding: Advice and Consultation (2016);
  • Technical Flood Risk Guidance for Stakeholders - SEPA Requirements for Undertaking a Flood Risk Assessment (Version 12, 2019);
  • Special Requirements for Civil Engineering Contracts for the Prevention of Pollution v2 (SEPA, 2006);
  • CIRIA C532: Control of Water Pollution from Construction Sites - Guidance for Consultants and Contractors (CIRIA, 2001);
  • CIRIA (2015) The SuDS Manual, Report C753;
  • SEPA (2014) Regulatory Method (WAT-RM-08) Sustainable Urban Drainage Systems, Version 5.2; and
  • IEMA (2022) A New Perspective on Land and Soil in Environmental Impact Assessment.

 

  1. In addition, the assessment of geology, hydrology, soils & flood risk has considered the legislative framework as defined by:
  • Directive 2007/60/EC on the assessment and management of flood risks (EC, 2007);
  • 2000/60/EC Water Framework Directive (EC, 2000);
  • The EC Groundwater Directive (Directive 2006/118/EC);
  • The Control of Pollution Act 1974 (COPA), as amended;
  • Environment Act 1995 (UK Government, 1995);
  • Flood Prevention and Land Drainage (Scotland) Act 1997 (Scottish Executive, 1997);
  • The Water Environment and Water Services (Scotland) Act 2003 (WEWSA);
  • Flood Risk Management (Scotland) Act 2009 (Scottish Government, 2009);
  • The Water Environment (Controlled Activities) (Scotland) Regulations 2011 as amended (Scottish Government, 2011);
  • The Private Water Supplies (Scotland) Regulations  2006;
  • The Water Intended for Human Consumption (Private Supplies) (Scotland) Regulations 2017;
  • The Water Resources (Scotland) Act 2013 (Scottish Government, 2013); and
  • The Private and Public Water Supplies (Miscellaneous Amendments) (Scotland) Regulations 2015.

11.9.2.              Impact Assessment Criteria

  1. Determining the significance of effects is a two-stage process that involves defining the magnitude of the potential impacts and the sensitivity of the receptors. This section describes the criteria applied in this chapter to assign values to the magnitude of potential impacts and the sensitivity of the receptors. The terms used to define magnitude and sensitivity are based on those which are described in further detail in Volume 1, Chapter 2 of the Onshore EIA Report.
  2. The criteria for defining magnitude in this chapter are outlined in Table 11.7   Open ▸ below.
Table 11.7:
Definition of Terms Relating to the Magnitude of an Impact

Table 11.7:  Definition of Terms Relating to the Magnitude of an Impact

 

  1. The criteria for defining sensitivity in this chapter are outlined in Table 11.8   Open ▸ below.
Table 11.8:
Definition of Terms Relating to the Sensitivity of the Receptor

Table 11.8:  Definition of Terms Relating to the Sensitivity of the Receptor

 

  1. The significance of the effect upon geology, hydrology, soils & flood risk is determined by correlating the magnitude of the impact and the sensitivity of the receptor, as outlined in Table 11.9   Open ▸ below.
Table 11.9:
Matrix Used for the Assessment of the Significance of the Effect

Table 11.9: Matrix Used for the Assessment of the Significance of the Effect

11.10.            Primary & tertiary mitigation

11.10. Primary & tertiary mitigation

  1. As part of the Proposed Development design process, a number of measures have been proposed to reduce the potential for impacts on geology, hydrology, soils & flood risk (see Table 11.10   Open ▸ ). These include measures which have been incorporated as part of the Proposed Development’s design (referred to as ‘primary mitigation’) and measures which will be implemented regardless of the impact assessment (referred to as ‘tertiary mitigation’). As there is a commitment to implementing these measures, they are considered inherently part of the design of the Proposed Development and have therefore been considered in the assessment presented in Section 11.11 below (i.e. the determination of magnitude and therefore significance assumes implementation of these measures). These measures are considered standard industry practice for this type of development.
Table 11.10:
Measure Adopted as Part of the Proposed Development (Primary & Tertiary Mitigation)

Table 11.10:  Measure Adopted as Part of the Proposed Development (Primary & Tertiary Mitigation)

11.11.            Assessment of Significance

11.11. Assessment of Significance

  1. The potential impacts arising from the construction, operational and maintenance and decommissioning phases of the Proposed Development, along with the maximum design scenario against which each impact has been assessed is given below.
  2. An assessment of the likely significance of the effects of the Proposed Development on geology, hydrology, soils & flood risk receptors caused by each identified impact is given below.

Impacts on Hydrology

  1. During the construction phase, there is potential for pollution to enter watercourses (and Thorntonloch Bathing Waters indirectly) as a consequence of runoff from construction areas, chemical / fuel spills and untreated foul water discharge. Provision and implementation of the CEMP including construction drainage measures seeks to put in place appropriate measures to limit the likelihood of any such impact on watercourses local to the Proposed Development. In addition, a minimum buffer of 50m to all classified watercourses has been maintained except where watercourse crossings are required (see Volume 4, Appendix 11.1) and a small section around the Landfall Location. In addition, a WQMP would be implemented to monitor the quality of local watercourses before, during and after construction that are in hydraulic continuity with the Proposed Development.
  2. During the operational and maintenance phase, there is potential for pollution to enter the Innerwick Burn adjacent to the onshore substation as a consequence of runoff from the onshore substation. Provision of a permanent surface water drainage strategy seeks to provide appropriate treatment for the Proposed Development runoff prior to discharge to the watercourse. There is potential for pollution to enter local watercourses during maintenance of the cable route (e.g., cable replacement). Any maintenance works of the cable route would mimic the construction phase processes albeit in a more minor and short-term fashion and the relevant appropriate measures will be undertaken following a specific method statement maintenance events.
  3. During the decommissioning phase, there is potential for pollution to enter watercourses as a consequence of decommissioning activities (similar to the construction phase but to a lesser degree).

Construction phase

Magnitude of impact
  1. The impact is predicted to be of local spatial extent across watercourse extents downstream of construction areas and coastal waters adjacent to landfall, medium term duration, intermittent and high reversibility (given the relatively small near coast catchment areas). It is predicted that the impact will affect the receptor directly. Considering the tertiary measures in place to control drainage during construction within the CEMP, the magnitude is therefore considered to be negligible.
Sensitivity of the receptor
  1. The watercourses within the assessment range from high to negligible sensitivity based on their classification. The Thornton Burn is of high sensitivity (due to Good Status Classification), the Dry Burn of medium sensitivity (due to Moderate Status Classification), other unnamed watercourses of negligible sensitivity (due to being unclassified) and the Barness to Wheat Stack coastal water body is of high sensitivity (due to Good Status Classification. The overall sensitivity is considered to be high.
Significance of the effect
  1. Overall, the magnitude of the impact is deemed to be negligible and the sensitivity of the receptor is considered to be up to high. The effect will, therefore, be of minor adverse significance, which is not significant in EIA terms.
Secondary mitigation and residual effect
  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.

Operation and maintenance phase

Magnitude of impact
  1. The impact is predicted to be of local spatial extent of watercourse extents downstream of the Proposed Development, long term duration, intermittent and high reversibility. It is predicted that the impact will affect the receptor directly. Considering the tertiary measures in place to control drainage during the operational and maintenance phase through the implementation of the surface water drainage strategy, the magnitude is therefore considered to be negligible.
Sensitivity of the receptor
  1. The Innerwick Burn adjacent to the onshore substation is heavily modified and unclassified therefore is considered to be of negligible sensitivity. All other watercourses within the study area will not be impacted during the operational phase as the remaining Proposed Development outwith the Innerwick Burn catchment will be below ground (i.e., cable routes).
Significance of the effect
  1. Overall, the magnitude of the impact is deemed to be negligible and the sensitivity of the receptor is considered to be negligible. The effect will, therefore, be of negligible adverse significance, which is not significant in EIA terms.
Secondary mitigation and residual effect
  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.

Decommissioning phase

Magnitude of impact
  1. The magnitude of impact for the decommissioning phase is assumed to be equivalent to the construction phase due to similar processes of plant use, excavation and stockpiling. The magnitude is therefore considered to be negligible.
Sensitivity of the receptor
  1. The watercourses within the assessment range from high to negligible sensitivity based on their classification. The Thornton Burn is of high sensitivity, the Dry Burn of medium sensitivity and other unnamed watercourses of negligible sensitivity. The overall sensitivity shall be considered high.
Significance of the effect
  1. Overall, the magnitude of the impact is deemed to be negligible and the sensitivity of the receptor is considered to be up to high. The effect will, therefore, be of minor adverse significance, which is not significant in EIA terms.
Secondary mitigation and residual effect
  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.

 

Impacts on hydrogeology

  1. During the construction phase, there is potential for pollution transmittal through the geology into the underlying aquifers as a consequence of runoff from construction areas, chemical / fuel spills and untreated foul water discharge. Provision and implementation of the CEMP including construction drainage measures seeks to put in place appropriate measures to limit the likelihood of any such impact on underlying aquifers and the Skateraw abstraction. In addition, a 250 m buffer around the Skateraw abstraction has been maintained with the exception of some enabling works (down gradient) and a minimal encroachment of the cable route to west that is located on the opposite side of the Innerwick Burn, thus not in hydraulic continuity with the abstraction point. The abstraction source would be included within the WQMP for monitoring before, during and after construction. The clay content observed within the superficial deposits over the geology, hydrology, soils & flood risk study area indicates the likelihood for transmittal of pollutants into the groundwater to be negligible. Ground investigation results and primary mitigation within the onshore substation earthworks design indicate that groundwater will not be encountered during construction and therefore no interaction with the groundwater DWPA is expected.

Construction phase

Magnitude of impact
  1. The impact is predicted to be of local spatial extent (within vicinity of Skateraw abstraction), medium term duration, intermittent and medium reversibility (due to the anticipated recharge rates of this local abstraction source). It is predicted that the impact will affect the receptor directly. The magnitude is therefore considered to be low.
Sensitivity of the receptor
  1. The Skateraw abstraction is deemed to be of medium vulnerability, medium recoverability and medium value. The abstraction is controlled under a simple licence and therefore less than 2,000m3/day and used for non-domestic purposes. The sensitivity is therefore considered to be medium.
Significance of the effect
  1. Overall, the magnitude of the impact is deemed to be low and the sensitivity of the receptor is considered to be medium. The effect will, therefore, be of minor adverse significance, which is not significant in EIA terms.
Secondary mitigation and residual effect
  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.

Increase in Flood Risk

  1. During the construction phase, the removal of soil may increase runoff and downstream fluvial and surface water flood risk if unmitigated. A CEMP will be in place during construction and will include a detailed drainage strategy outlining temporary drainage measures to control increase in surface runoff. The CEMP will also outline the methodology for the construction of watercourse crossings to avoid an increase in flood risk to downstream receptors.
  2. During the operational and maintenance phase, if unmitigated the runoff from the onshore substation has the potential to increase flood risk downstream. The permanent surface water drainage strategy will ensure that the runoff from developed areas will be properly managed and attenuated prior to discharge to the water environment to seek to maintain the pre-development runoff rates / hydrological regime. The proposed drainage strategy has the additional benefit of managing runoff from a catchment area that is partially related to a pre-existing flooding issue. This pre-existing flooding issue will be reduced through the implementation of attenuated runoff from the area and formally discharging to the nearby watercourse. For the duration of the operation of the onshore substation, the maintenance of the drainage strategy will be the responsibility of the substation site owner.

Construction phase

Magnitude of impact
  1. The impact is predicted to be of local spatial extent downgradient / downstream of all construction areas, short term duration, intermittent and medium reversibility. It is predicted that the impact will affect the receptor directly. Considering the tertiary measures in place to control drainage during construction within the CEMP, the magnitude is therefore considered to be negligible.
Sensitivity of the receptor
  1. Fluvial and surface water flood risks in the area are low and thus the sensitivity of the receptor is low.
Significance of the effect
  1. Overall, the magnitude of the impact is deemed to be negligible and the sensitivity of the receptor is considered to be low. The effect will, therefore, be of negligible adverse significance, which is not significant in EIA terms.
Secondary mitigation and residual effect
  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.

Operation and maintenance phase

Magnitude of impact
  1. The impact is predicted to be of local spatial extent downgradient and downstream of the onshore substation location, long term duration, intermittent and medium reversibility. It is predicted that the impact will affect the receptor directly. Considering the tertiary measures in place to control drainage during the operational and maintenance phase through the implementation of the surface water drainage strategy and the benefit of reducing a localised pre-existing flooding issue, the magnitude is therefore considered to be low.
Sensitivity of the receptor
  1. Fluvial and surface water flood risks in the area are low and thus the sensitivity of the receptor is low.
Significance of the effect
  1. Overall, the magnitude of the impact is deemed to be low and the sensitivity of the receptor is considered to be low. The effect will, therefore, be of minor beneficial significance.
Secondary mitigation and residual effect
  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.

Impacts to statutory geologically designated sites

  1. During the construction phase, the landfall will be installed in the location of the Barns Ness Coast SSSI and Geological Conservation Review Site. It avoids the ‘crucial areas’ of the SSSI feature. Trenchless technology (e.g., HDD) will be used as opposed to open cut trenching which enables the cable transition pits and trenchless technology construction compound to be located out with (inland of) the SSSI boundary.  The cables will be installed in ducted boreholes that are drilled, at depth to pass underneath the SSSI.  The use of trenchless technology will therefore pose a minimal risk of disturbance to the SSSI.  During the decommissioning stage, the cables will either remain in-situ and be pulled out from the landfall location. Given the works will pass underneath the SSSI at depth, the decommissioning phase will pose a minimal risk of disturbance to the SSSI.

Construction phase

Magnitude of impact
  1. The impact is predicted to be of local spatial extent within the geological conservation area, short term duration, continuous and low reversibility. It is predicted that the impact will affect the receptor directly. However, considering the use of trenchless technology (e.g. HDD) and avoidance of damage to the SSSI due to the depth of the cable, the magnitude is therefore considered to be negligible.
Sensitivity of the receptor
  1. The Barns Ness Coast SSSI is an area containing geological features considered to be of national interest. Barns Ness Coast Geological Conservation Review site is an area containing features of designated regional importance. Taking the higher sensitivity receptor, the SSSI, the geological site is deemed to be of high national geological value. The sensitivity of the receptor is therefore, considered to be high.
Significance of the effect
  1. Overall, the magnitude of the impact is deemed to be negligible and the sensitivity of the receptor is considered to be high. The effect will, therefore, be of minor adverse significance, which is not significant in EIA terms.
Secondary mitigation and residual effect
  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.

Decommissioning phase

Magnitude of impact
  1. The impact is predicted to be of local spatial extent within the geological conservation area, short term duration, continuous and low reversibility. It is predicted that the impact will affect the receptor directly. However, considering the use of trenchless technology (e.g. HDD) and avoidance of damage to the SSSI due to the depth of the cable, the magnitude is therefore considered to be negligible.
Sensitivity of the receptor
  1. The Barns Ness Coast SSSI is an area containing geological features considered to be of national interest. Barns Ness Coast Geological Conservation Review site is an area containing features of designated regional importance. Taking the higher sensitivity receptor, the SSSI, the geological site is deemed to be of high national geological value. The sensitivity of the receptor is therefore, considered to be high.
Significance of the effect
  1. Overall, the magnitude of the impact is deemed to be negligible and the sensitivity of the receptor is considered to be high. The effect will, therefore, be of minor adverse significance, which is not significant in EIA terms.
Secondary mitigation and residual effect
  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.

 

Impacts to soils

  1. During the construction phase, there is potential for increased compaction, erosion and loss of soils as a consequence of construction traffic, disturbance, creation of construction areas and excavations. Provision and implementation of the CEMP including a Soil Management Plan will ensure standard industry practice measures are followed with respect to stripping of soils, stockpiling, backfilling and reinstatement. Loss of soils from the operational phase will be predominantly from the construction of Proposed Development areas (and thus captured in the construction phase assessment) with potential minor impacts as described above relating to any maintenance works. Any maintenance works will be undertaken following a specific method statement.
  2. During the decommissioning phase, there is potential for increased compaction, erosion and loss of soils as a consequence of decommissioning activities (similar to the construction phase but to a lesser degree). Provision and implementation of the Decommissioning Programme will ensure standard industry practice measures are followed with respect to stripping of soils, stockpiling, backfilling and reinstatement.

Construction phase

Magnitude of impact
  1. The impact is predicted to be of local spatial extent across all construction areas and immediately downgradient, short term duration, intermittent and high reversibility. It is predicted that the impact will affect the receptor directly. However, considering the tertiary mitigation in place through implementation of the CEMP, the magnitude is considered to be low.
Sensitivity of the receptor
  1. Soils within proximity to the Proposed Development are predominantly able to support arable agriculture (Class 1, 2 and 3.1) and are predominantly moderately to highly vulnerable to compaction and erosion. The sensitivity is therefore considered medium.
Significance of the effect
  1. Overall, the magnitude of the impact is deemed to be low and the sensitivity of the receptor is considered to be medium. The effect will, therefore, be of minor adverse significance, which is not significant in EIA terms.
Secondary mitigation and residual effect
  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.

Operation and maintenance phase

Magnitude of impact
  1. The impact is predicted to be of local spatial extent across all Proposed Development areas, short term duration (maintenance works), intermittent and high reversibility. It is predicted that the impact will affect the receptor directly. The magnitude is considered to be low.
Sensitivity of the receptor
  1. Soils within proximity to the Proposed Development are predominantly able to support arable agriculture (Class 1, 2 and 3.1) and are predominantly moderately to highly vulnerable to compaction and erosion. The sensitivity is therefore considered medium.
Significance of the effect
  1. Overall, the magnitude of the impact is deemed to be low and the sensitivity of the receptor is considered to be medium. The effect will, therefore, be of minor adverse significance, which is not significant in EIA terms.
Secondary mitigation and residual effect
  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.

Decommissioning phase

Magnitude of impact
  1. The magnitude of impact for the decommissioning phase is assumed to be equivalent to the construction phase due to similar processes of plant use, excavation and stockpiling. Therefore, the magnitude is considered to be low.
Sensitivity of the receptor
  1. Soils within proximity to the Proposed Development are predominantly able to support arable agriculture (Class 1, 2 and 3.1) and are predominantly moderately to highly vulnerable to compaction and erosion. The sensitivity is therefore considered medium.
Significance of the effect
  1. Overall, the magnitude of the impact is deemed to be low and the sensitivity of the receptor is considered to be medium. The effect will, therefore, be of minor adverse significance, which is not significant in EIA terms.
Secondary mitigation and residual effect
  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.

11.11.1.         Proposed Monitoring

  1. Proposed monitoring measures are outlined in Table 11.11   Open ▸ below.
Table 11.11:
Monitoring Commitments for Geology, Hydrology, Soils and Flood Risk

Table 11.11:  Monitoring Commitments for Geology, Hydrology, Soils and Flood Risk

  1. Water quality monitoring of watercourses within the Proposed Development Area and the Skateraw abstraction source is proposed to monitor the quality of these areas during and after construction. Pre-construction monitoring is proposed to develop a baseline water quality dataset for which the construction and post-construction quality can be compared against to assess any potential impacts. Water quality monitoring allows for ongoing monitoring of water quality and to enable a suitable response to be implemented in the unlikely event that effects on the water environment are observed.  

11.12.            Cumulative Effects Assessment

11.12. Cumulative Effects Assessment

11.12.1.         Methodology

 

  1. The Cumulative Effects Assessment (CEA) takes into account the impact associated with the Proposed Development together with other relevant local plans, projects and activities. Cumulative effects are therefore the combined effect of the Proposed Development in combination with the effects from a number of different projects, on the same receptor or resource. Please see Volume 1, Chapter 2 of the Onshore EIA Report for detail on CEA methodology.
  2. The projects and plans selected as relevant to the CEA presented within this chapter are based upon the results of a screening exercise (see Volume 4, Appendix 2.4). Each project or plan has been considered on a case by case basis for screening in or out of this chapter's assessment based upon data confidence, effect-receptor pathways and the spatial/temporal scales involved.
  3. The specific projects scoped into the CEA for geology, hydrology, soils and flood risk, are outlined in Table 11.12   Open ▸ .
Table 11.12:
List of Other Projects Considered Within the CEA for Geology, Hydrology, Soils & Flood Risk

Table 11.12:  List of Other Projects Considered Within the CEA for Geology, Hydrology, Soils & Flood Risk  

 

11.12.2.         Maximum Design Scenario

  1. The maximum design scenarios summarised here have been selected as those having the potential to result in the greatest effect on an identified receptor or receptor group. The cumulative effects presented and assessed in this section have been selected from the details provided in Volume 1, Chapter 5 of the Onshore EIA Report as well as the information available on other projects and plans, to inform a ‘maximum design scenario’. Effects of greater adverse significance are not predicted to arise should any other development scenario, based on details within the Project Design Envelope, to that assessed here, be taken forward in the final design scheme.
  2. The cumulative assessment has been undertaken assuming the potential for construction programmes to overlap and the maximum footprint of the Proposed Development and cumulative projects.

11.12.3.         Cumulative Effects Assessment

  1. An assessment of the likely significance of the cumulative effects of the Proposed Development upon geology, hydrology, soils and flood risk receptors arising from each identified impact is given below.

Tier 1

  1. There are considered to be no likely significant cumulative impacts with the Berwick Bank offshore infrastructure.

Tier 2

Cumulative impact on hydrology

  1. There is potential for the construction phase of the Proposed Development to coincide with the construction phase of the cumulative projects stated above. This creates a potential for cumulative water quality impacts to occur.
  2. There is potential for the operation and maintenance phase of the Proposed Development to coincide with the operation and maintenance phase of the cumulative projects stated above. The proposed onshore substation is to be located within the surface water catchment of the Innerwick Burn, no above ground development from the cumulative projects stated above is proposed within the Innerwick Burn catchment and thus there is no risk of cumulative impact. However, it is possible that ongoing maintenance works from the Proposed Development and cumulative projects could occur simultaneously and within the same surface water catchment.  
  3. There is potential for the decommissioning phase of the Proposed Development to coincide with the decommissioning phase of the cumulative projects stated above. This creates a potential for cumulative water quality impacts to occur.
  4. Cumulative projects are assumed to be subject to similar tertiary mitigation as the Proposed Development in that, provision and implementation of the CEMP including construction drainage measures would be required to limit the likelihood of any such impact to the water environment given this is standard practice for projects of this scale. In addition, any maintenance works will be subject to specific method statements for undertaken the proposed works and decommissioning of project will be undertaken in accordance with a Decommissioning Programme.
Construction phase

Magnitude of impact

  1. The cumulative impact is predicted to be of local spatial extent within individual surface water catchments, short term duration, intermittent and high reversibility (given the relatively small near coast catchment areas). It is predicted that the impact will affect the receptor directly. The magnitude is therefore considered to be negligible.

 

Sensitivity of receptor

  1. The watercourses within the assessment range from high to negligible sensitivity based on their classification. The Thornton Burn is of high sensitivity (due to Good Status Classification), the Dry Burn of medium sensitivity (due to Moderate Status Classification), other unnamed watercourses of negligible sensitivity (due to being unclassified) and the Barness to Wheat Stack coastal water body is of high sensitivity (due to Good Status Classification. The overall sensitivity is considered to be high.

 

Significance of effect

  1. Overall, the magnitude of the impact is deemed to be negligible and the sensitivity of the receptor is considered to be high. The cumulative effect will, therefore, be of minor adverse significance, which is not significant in EIA terms.

 

Secondary mitigation and residual effect

  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.
Operation and maintenance phase

Magnitude of impact

  1. The cumulative impact is predicted to be of local spatial extent within individual surface water catchments, short term duration, intermittent and high reversibility (given the relatively small near coast catchment areas). It is predicted that the impact will affect the receptor directly. The magnitude is therefore considered to be negligible.

 

Sensitivity of receptor

  1. The watercourses within the assessment range from high to negligible sensitivity based on their classification. The Thornton Burn is of high sensitivity (due to Good Status Classification), the Dry Burn of medium sensitivity (due to Moderate Status Classification), other unnamed watercourses of negligible sensitivity (due to being unclassified) and the Barness to Wheat Stack coastal water body is of high sensitivity (due to Good Status Classification. The overall sensitivity is considered to be high.

Significance of effect

  1. Overall, the magnitude of the impact is deemed to be negligible and the sensitivity of the receptor is considered to be high. The cumulative effect will, therefore, be of minor adverse significance, which is not significant in EIA terms.

 

Secondary mitigation and residual effect

  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.
Decommissioning phase

Magnitude of impact

  1. The cumulative impact is predicted to be of local spatial extent within individual surface water catchments, short term duration, intermittent and high reversibility (given the relatively small near coast catchment areas). It is predicted that the impact will affect the receptor directly. The magnitude is therefore considered to be negligible.

 

Sensitivity of receptor

  1. The watercourses within the assessment range from high to negligible sensitivity based on their classification. The Thornton Burn is of high sensitivity (due to Good Status Classification), the Dry Burn of medium sensitivity (due to Moderate Status Classification), other unnamed watercourses of negligible sensitivity (due to being unclassified) and the Barness to Wheat Stack coastal water body is of high sensitivity (due to Good Status Classification. The overall sensitivity is considered to be high.

 

Significance of effect

  1. Overall, the magnitude of the impact is deemed to be negligible and the sensitivity of the receptor is considered to be high. The cumulative effect will, therefore, be of minor adverse significance, which is not significant in EIA terms.

 

Secondary mitigation and residual effect

  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.

Cumulative impact on hydrogeology

  1. There is no potential cumulative impact on hydrogeology as the cumulative projects stated above do not fall within 250 m of the Skateraw abstraction point.

 Cumulative impact on Flood Risk

  1. There is potential for the construction phase of the Proposed Development to coincide with the construction phase of the cumulative projects stated above. This creates a potential for cumulative increase of flood risk due to the removal of soils.
  2. There is potential for the operation and maintenance phase of the Proposed Development to coincide with the operation and maintenance phase of the cumulative projects stated above. The proposed onshore substation is to be located within the surface water catchment of the Innerwick Burn, no above ground development from the cumulative projects stated above is proposed within the Innerwick Burn catchment and thus there is no risk of cumulative impact.
  3. Cumulative projects are assumed to be subject to similar tertiary mitigation as the Proposed Development in that, provision and implementation of the CEMP including construction drainage measures would be required to limit the likelihood of any such impact to the water environment given this is standard practice for projects of this scale.
Construction phase

Magnitude of impact

  1. The impact is predicted to be of local spatial extent downgradient / downstream of all construction areas, short term duration, intermittent and medium reversibility. It is predicted that the impact will affect the receptor directly. Considering the tertiary measures in place to control drainage during construction within the CEMP, the magnitude is therefore considered to be negligible.

 

Sensitivity of receptor

  1. Fluvial and surface water flood risks in the area are low and thus the sensitivity of the receptor is low.

 

Significance of effect

  1. Overall, the magnitude of the impact is deemed to be negligible and the sensitivity of the receptor is considered to be low. The effect will, therefore, be of negligible adverse significance, which is not significant in EIA terms.

 

Secondary mitigation and residual effect

  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.

Cumulative impact on statutory geologically designated sites

  1. From the cumulative projects stated above, there is potential for cumulative impacts relating to the proposed SPEN Eastern Link Project. The Eastern Link Project details several potential landfall locations, some of which are located within the Barns Ness Coast SSSI. In the event that the project selects a landfall location within the SSSI, there is potential for a cumulative impact on the feature from the construction phases and decommissioning phases.
  2. The SPEN Eastern Link Project is assumed to be subject to similar site design, and trenchless technology (e.g. HDD) would be used as opposed to open cut trenching at the statutory site to minimise disturbance of the SSSI. Similarly, a trenchless technology approach will ensure minimal disturbance of the SSSI if the cables are to be pulled out from the landfall location during decommissioning.
Construction phase

Magnitude of impact

  1. The impact is predicted to be of local spatial extent within the geologically conservation area, short term duration, continuous and low reversibility. It is predicted that the impact will affect the receptor directly. However, considering the use of trenchless technology (e.g. HDD) and avoidance of damage to the SSSI due to the depth of the cable, the magnitude is therefore considered to be negligible.

 

Sensitivity of receptor

  1. The Barns Ness Coast SSSI is an area containing geological features considered to be of national interest. Barns Ness Coast Geological Conservation Review site is an area containing features of designated regional importance. Taking the higher sensitivity receptor, the SSSI, the geological site is deemed to be of high national geological value. The sensitivity of the receptor is therefore, considered to be high.

 

Significance of effect

  1. Overall, the magnitude of the impact is deemed to be negligible and the sensitivity of the receptor is considered to be high. The effect will, therefore, be of minor adverse significance, which is not significant in EIA terms.

 

Secondary mitigation and residual effect

  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.
Decommissioning phase

Magnitude of impact

  1. The impact is predicted to be of local spatial extent within the geological conservation area, short term duration, continuous and low reversibility. It is predicted that the impact will affect the receptor directly. However, considering the use of trenchless technology (e.g. HDD) and avoidance of damage to the SSSI due to the depth of the cable, the magnitude is therefore considered to be negligible.

 

Sensitivity of receptor

  1. The Barns Ness Coast SSSI is an area containing geological features considered to be of national interest. Barns Ness Coast Geological Conservation Review site is an area containing features of designated regional importance. Taking the higher sensitivity receptor, the SSSI, the geological site is deemed to be of high national geological value. The sensitivity of the receptor is therefore, considered to be high.

 

Significance of effect

  1. Overall, the magnitude of the impact is deemed to be negligible and the sensitivity of the receptor is considered to be high. The effect will, therefore, be of minor adverse significance, which is not significant in EIA terms.

 

Secondary mitigation and residual effect

  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.

Cumulative impact on soils

  1. There is potential for the construction phase of the Proposed Development to coincide with the construction phase of the cumulative projects stated above. This creates a potential for increased compaction, erosion and loss of soils as a consequence of construction activities in areas where the Proposed Development and cumulative projects are closely located.  
  2. There is potential for the operation and maintenance phase of the Proposed Development to coincide with the operation and maintenance phase of the cumulative projects stated above. It is possible that ongoing maintenance works from the Proposed Development and cumulative projects could occur simultaneously and within localised areas that could have a cumulative impact on local soils.  
  3. There is potential for the decommissioning phase of the Proposed Development to coincide with the decommissioning phase of the cumulative projects stated above. This creates a potential for cumulative impacts to local soils to occur.  
  4. Cumulative projects are assumed to be subject to similar tertiary mitigation as the Proposed Development in that, provision and implementation of the CEMP including a Soil Management Plan. In addition, any maintenance works will be subject to specific method statements for undertaken the proposed works and decommissioning of project will be undertaken in accordance with a Decommissioning Programme.
Construction phase

Magnitude of impact

  1. The impact is predicted to be of local spatial extent across all construction areas and immediately downgradient, short term duration, intermittent and high reversibility. It is predicted that the impact will affect the receptor directly. However, considering the tertiary mitigation in place through implementation of the CEMP, the magnitude is considered to be low.

 

Sensitivity of receptor

  1. Soils within proximity to the Proposed Development are predominantly able to support arable agriculture (Class 1, 2 and 3.1) and are predominantly moderately to highly vulnerable to compaction and erosion. The sensitivity is therefore considered medium.

 

Significance of effect

  1. Overall, the magnitude of the impact is deemed to be low and the sensitivity of the receptor is considered to be medium. The effect will, therefore, be of minor adverse significance, which is not significant in EIA terms.

 

Secondary mitigation and residual effect

  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.
Operation and maintenance phase

Magnitude of impact

  1. The impact is predicted to be of local spatial extent across all construction areas and immediately downgradient, short term duration, intermittent and high reversibility. It is predicted that the impact will affect the receptor directly. However, considering the tertiary mitigation in place through implementation of the CEMP, the magnitude is considered to be low.

 

Sensitivity of receptor

  1. Soils within proximity to the Proposed Development are predominantly able to support arable agriculture (Class 1, 2 and 3.1) and are predominantly moderately to highly vulnerable to compaction and erosion. The sensitivity is therefore considered medium.

 

Significance of effect

  1. Overall, the magnitude of the impact is deemed to be low and the sensitivity of the receptor is considered to be medium. The effect will, therefore, be of minor adverse significance, which is not significant in EIA terms.

 

Secondary mitigation and residual effect

  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.
Decommissioning phase

Magnitude of impact

  1. The impact is predicted to be of local spatial extent across all construction areas and immediately downgradient, short term duration, intermittent and high reversibility. It is predicted that the impact will affect the receptor directly. However, considering the tertiary mitigation in place through implementation of the CEMP, the magnitude is considered to be low.

 

Sensitivity of receptor

  1. Soils within proximity to the Proposed Development are predominantly able to support arable agriculture (Class 1, 2 and 3.1) and are predominantly moderately to highly vulnerable to compaction and erosion. The sensitivity is therefore considered medium.

 

Significance of effect

  1. Overall, the magnitude of the impact is deemed to be low and the sensitivity of the receptor is considered to be medium. The effect will, therefore, be of minor adverse significance, which is not significant in EIA terms.

 

Secondary mitigation and residual effect

  1. No secondary mitigation is considered necessary because the likely effect in the absence of secondary mitigation is not significant in EIA terms.

11.12.4.         Proposed Monitoring

  1. No geology, hydrology, soil and flood risk additional monitoring to test the predictions made within the assessment of likely significant cumulative effects is considered necessary.

11.14. Summary of Impacts, Mitigation Measures, Likely Significant Effects and Monitoring

  1. Information on geology, hydrology, soils and flood risk within the geology, hydrology, soils and flood risk study area was collected through desktop review, site surveys and consultation.
  2. Table 11.13   Open ▸ presents a summary of the potential impacts, mitigation measures and the conclusion of likely significant effects in EIA terms in respect to geology, hydrology, soils and flood risk. The impacts assessed include: hydrology, hydrogeology, flood risk, contaminated land, statutory geological designated sites and soils. Overall, it is concluded that there will be no likely significant effects arising from the Proposed Development during the construction, operational and maintenance or decommissioning phases.
  3. Table 11.14   Open ▸ presents a summary of the potential cumulative impacts, mitigation measures and the conclusion of likely significant effects on geology, hydrology, soils and flood risk. The cumulative effects assessed include: hydrology, flood risk, geologically designated sites and soils. Overall, it is concluded that there will be no likely significant cumulative effects from the Proposed Development alongside other projects/plans.

 

 

Table 11.13:
Summary of Likely Significant Environmental Effects, Mitigation and Monitoring

Table 11.13:  Summary of Likely Significant Environmental Effects, Mitigation and Monitoring

 

Table 11.14:
Summary of Likely Significant Cumulative Environment Effects, Mitigation and Monitoring

Table 11.14:  Summary of Likely Significant Cumulative Environment Effects, Mitigation and Monitoring

 

11.15.            References

11.15. References

 

CIRIA (2001). C532: Control of Water Pollution from Construction Sites - Guidance for Consultants and Contractors

CIRIA (2015). C753: The SuDS Manual.

COPA (1974) The Control of Pollution Act, as amended.

EA, SEPA & EHSNI  (2013). PPG1: General guide to the prevention of pollution.

EA, SEPA & EHSNI (2018). GPP2: Above ground oil storage tanks.

EA, SEPA & EHSNI (2017). GPP5: Works and maintenance in or near water.

EA, SEPA & EHSNI (2012). PPG6: Working at construction and demolition sites.

EA, SEPA & EHSNI (2017). GPP21: Pollution incidence response planning.

EC (2007). Directive 2007/60/EC on the assessment and management of flood risks.

EC (2000). Directive 2000/60/EC: Water Framework Directive.

EC (2006). Directive 2006/118/EC: The EC Groundwater Directive.

Scottish Executive (1997). Flood Prevention and Land Drainage (Scotland) Act

Scottish Government (2009). Flood Risk Management (Scotland) Act

Scottish Government (2011). The Water Environment (Controlled Activities) (Scotland) Regulations, as amended.

Scottish Government (2009). The Private Water Supplies (Scotland) Act.

Scottish Government (2017). The Water Intended for Human Consumption (Private Supplies) (Scotland) Regulations.

Scottish Government (2013). The Water Resources (Scotland) Act.

Scottish Government (2015). The Private and Public Water Supplies (Miscellaneous Amendments) (Scotland) Regulations.

Scottish Government (2023). National Planning Framework 4. Available at: https://www.transformingplanning.scot/national-planning-framework/adopted-npf4/

SEPA (2018). Supporting Guidance (SAT-SG-75) – Sector specific guidance: construction sites.

SEPA (2018). Guidance Note 2a: Development Management Guidance on Flood Risk.

SEPA (2017). Guidance Note 31: Guidance on Assessing the Impacts of Development Proposals on Groundwater Abstractions and Groundwater Dependent Terrestrial Ecosystems.

SEPA (2009). Policy 19: Groundwater Protection Policy for Scotland.

SEPA (2016). Policy 41: Planning Authority Protocol - Development at Risk of Flooding: Advice and Consultation.

SEPA (2019). Technical Flood Risk Guidance for Stakeholders - SEPA Requirements for Undertaking a Flood Risk Assessment.

SEPA (2006). Special Requirements for Civil Engineering Contracts for the Prevention of Pollution.

SEPA (2014). Regulatory Method (WAT-RM-08) Sustainable Urban Drainage Systems.

UK Government (1995). Environment Act.

WEWSE (2003). The Water Environment and Water Services (Scotland) Act.

 

BGS (2020). Online Geology of Britain Viewer. Available at: http://mapapps.bgs.ac.uk/geologyofbritain/home.html

BGS (2020). Online GeoIndex Onshore. Available at:                                            https://www.bgs.ac.uk/map-viewers/geoindex-onshore/

CEH (2022). Flood Estimation Handbook Web Service. Available at:

https://fehweb.ceh.ac.uk/GB/map

SEPA (2022). Scotland’s Environment Web Map. Available at: https://map.environment.gov.scot/sewebmap/

SEPA (2022). SEPA Flood Maps. Available at:

https://map.sepa.org.uk/floodmaps

SEPA (2022). Environnent Data. Available at :

https://www.sepa.org.uk/environment/environmental-data/

SEPA (2022). Water Classification Hub. Available at:

https://www.sepa.org.uk/data-visualisation/water-classification-hub/

SEPA (2017). National Soil Map of Scotland. Available at: https://soils.environment.gov.scot/maps/soil-maps/national-soil-map-of-scotland/

SNH (2011). Geological Conservation Review Dataset. Available at:

https://apps.snh.gov.uk/sitelink-api/v1/sites/153/documents/3

 

[1] C = Construction, O = Operational and maintenance, D = Decommissioning