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Offshore Renewable Energy Site Suitability Mapping (ORESSuM)
Research · September 2015
DOI: 10.13140/RG.2.1.3988.5284
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Some of the authors of this publication are also working on these related projects:
Irish Sea Suitability Mapping for Novel Offshore Foundations (ISSMaNOF) View project
Scour Potential Evaluation of the Western Irish Sea Mud Belt (SCOPE) View project
Mark Coughlan
Irish Centre for Research in Applied Geosciences
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ORESSuM
Offshore Renewable Energy Site Suitability
Mapping
Mark Coughlan,Dr. Andrew Wheeler and Dr. Boris Dorschel
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Executive Summary
High wind speeds coupled with energetic tidal regimes and strong waves exist off the coast of
Ireland. It forms a large, relatively untapped renewable energy source that could help Ireland reach
its green energy targets in the future. So far offshore wind energy has only been harnessed at
Arklow Bank on the east coast whereas tidal and wave energy devices are still largely at the research
and development stage.
In order to expand the offshore renewable energy sector Ireland needs to be able to provide
detailed information and data from a variety of disciplines when it comes to site selection for
offshore installations. In this regard a large amount of data pertinent to the offshore renewable
energy sector has been collected over the decades, particularly as part of the INFOMAR program.
This data forms a sound basis from which to create geological models for areas identified as being
potential sites for development. However, there is scope for additional data collection, especially
with reference to studying seabed dynamics. Practices such as the deployment of ADCP’s and other
such current velocity monitoring equipment during the course of site surveys would greatly enhance
the comprehensiveness of the survey and its ability to provide the necessary data for not only the
initial geological model but also subsequent studies such as scour modeling and sediment transport
which, over time, need to be monitored throughout an installations lifetime.
Similarly, the importance of adequate sample collection is highlighted in the case studies mentioned
within with particular reference made to the OSIG guidelines which serve as a useful reference with
regard to site survey best practice.
By assessing the INFOMAR dataset and its ability to meet industry requirements it is possible to
tailor future INFOMAR data collection and, in doing so, address one of Ireland’s key policy objectives
of enhancing the knowledge economy and renewable energy sector, which are the current
government’s perceived key economic drivers.
3
Contents
Contents………………………………………………………………………………………………………………………….. 3
1 Project Background…………………………………………………………………………………………………….. 5
1.1 Renewable Energy……………………………………………………………………………………………….. 5
1.2 Sites Around Ireland …………………………………………………………………………………………….. 5
1.3 Current State of Irish Offshore Renewable Sector ……………………………………………………… 5
1.4 Scope of the Study ………………………………………………………………………………………………. 7
2 Methods …………………………………………………………………………………………………………………… 7
2.1 Industry Appraisal ……………………………………………………………………………………………….. 7
2.2 Data Collection and Integration ……………………………………………………………………………… 8
3 Appraisal of Industry Needs …………………………………………………………………………………………. 9
3.1 Introduction ……………………………………………………………………………………………………….. 9
3.2 Geological Features ……………………………………………………………………………………………… 9
3.2.1 Seafloor Morphology …………………………………………………………………………………… 10
3.2.2 Quaternary Geology ……………………………………………………………………………………. 10
3.2.3 Solid Geology …………………………………………………………………………………………….. 11
4 General Physical Features ………………………………………………………………………………………….. 13
4.1.1 Seabed Bathymetry …………………………………………………………………………………….. 13
4.1.2 Wind Characteristics ……………………………………………………………………………………. 14
4.1.3 Wave Characteristics …………………………………………………………………………………… 14
4.1.4 Tidal Regime ………………………………………………………………………………………………. 17
4.1.5 Distance to Shore ……………………………………………………………………………………….. 18
4.2 Ecological Factors ………………………………………………………………………………………………. 19
4.2.1 Special Areas of Conservation (SAC’s) …………………………………………………………….. 19
4.2.2 Special Protection Areas (SPA’s) ……………………………………………………………………. 19
4.3 Socio-economic Factors………………………………………………………………………………………. 22
4
4.3.1 Commercial Navigation ……………………………………………………………………………….. 23
4.3.2 Fisheries ……………………………………………………………………………………………………. 23
4.3.3 Cables ………………………………………………………………………………………………………. 23
4.3.4 Shipwrecks ………………………………………………………………………………………………… 28
4.3.5 Military Installations and Firing Ranges …………………………………………………………… 28
5 Assessment of INFOMAR Dataset Compatibility …………………………………………………………….. 31
6 Site Survey Methodology …………………………………………………………………………………………… 34
6.1 Current Information …………………………………………………………………………………………… 34
6.2 Desktop Study …………………………………………………………………………………………………… 36
6.3 Geophysical Survey ……………………………………………………………………………………………. 37
6.4 Geotechnical Survey …………………………………………………………………………………………… 41
7 Case Studies ……………………………………………………………………………………………………………. 45
7.1.1 Sheringham Shoals ……………………………………………………………………………………… 45
7.1.2 Scroby Sands ……………………………………………………………………………………………… 48
8 Conclusions …………………………………………………………………………………………………………….. 53
8.1 Data Gap Analysis………………………………………………………………………………………………. 53
8.2 General Conclusions …………………………………………………………………………………………… 54
9 Recommendations ……………………………………………………………………………………………………. 56
10 References …………………………………………………………………………………………………………… 61
1 Project Background
1.1 Renewable Energy
Renewable energy comes from inexhaustible sources which are continually replaced (e.g. wind,
hydro power, direct solar power, wave, biomass, geothermal and tidal). The utilization of these
sources produces little or no carbon dioxide as well as other such greenhouse gases identified as the
main drivers of global climate change today, widely considered the most pressing environmental
issue of the modern age.
The Irish State is committed to achieving a target of 16% of all its energy needs (heat, transport,
electricity) to come from renewable sources by 2020 under Directive 2009/28/EC as part of the EU’s
commitment to the Framework Convention on Climate Change signed at Kyoto in 1997. Ireland has
at its disposal ample potential from renewable sources to achieve this goal, particularly in its
offshore sector (i.e. offshore wind, wave and tidal energy)
1.2 Sites Around Ireland
The greatest potential for offshore wind energy in particular lies off the western coast. However,
water depth increases too rapidly and so installations have to be located close to land where wave
exposure is high and connection to the grid presents a problematic issue. Similarly, wave energy
potential is greatest off the west coast and is a more feasible option here than wind. The south coast
is generally unfeasible due to a lack of shallow water close to shore and the close proximity of
bedrock or rock exposure to the seabed. The east coast provides the necessary shallow water
conditions to make wind energy viable as well as depths with high energy hydrodynamic regimes
which make tidal energy a possibility. However, this high energy also makes scour a destructive and
limiting factor.
1.3 Current State of Irish Offshore Renewable Sector
In recent years tidal and ,in particular, wave energy have become the main focus of offshore
renewable energy in Ireland whereas wind has become the most viable and hence most developed
with installations constructed at Skerd Rocks, Codling Bank, and Arklow Bank, with further sites set
to be developed at Dundalk Bay, Bray and Kish Banks. The Irish Government has set a target to have
500MW of wave and tidal capacity in operation by 2020, transforming the island of Ireland into
‘Europe’s Battery’.
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Research into tidal energy has been largely conducted in estuaries most notably Strangford Lough
which has the worlds first commercial scale turbine commissioned in 2007. Issues identified with the
installation of these turbines focus mostly on socio-economic factors and their operational layout.
Socio-economic factors relate to navigation paths for commercial and recreational vessels being
blocked. Usually, turbines are constructed in banks with lines of turbines one behind the other
resulting in energy being dissipated once it passes the first line contributing to lower energy yields
for subsequent lines of turbines. Areas within the Irish Sea have been identified where tidal energy is
high and that are sufficiently distanced from shore so that the above constraints are negated.
However, the high energy hydrodynamic regimes of these areas also have increased seabed scour
which is a limiting factor in constructing foundations.
Ireland has a first-rate ocean energy research base represented by both academic and commercial
interests with world class levels of expertise in project design, testing and mooring design. The
Marine Institute, in association with Sustainable Energy Ireland, has established an Ocean Energy
Test Site for scaled prototypes of wave energy devices in Galway Bay where, most notably, Ocean
Energy Ltd. and Wavebob Ltd. are currently testing prototypes. The Sustainable Energy Authority of
Ireland also plans to develop a National Wave Energy Test Site to be located off Annagh Head, west
of Belmullet in County Mayo. This test site will provide a location for the temporary mooring and
deployment of wave energy machines in order to monitor their ability to generate electricity and
survive open ocean conditions.
Wind currently remains the most viable of all offshore renewable energy sources because of
Ireland’s large wind resource (up to 9m/sec in some places). The majority of these projects have
targeted the banks located offshore of the eastern coast. This includes most notably the
construction of seven turbines at Arklow Bank located roughly 11.7km offshore in an average water
depth of 20m. Each capable of generating up to 3.6MW, totaling 25MW altogether. Phase 2 of the
Arklow Bank project is currently dormant but environmental impact assessments (EIA’s) and site
surveys are currently being carried out at Codling Bank, Dundalk Bay and the Kish and Bray Banks in
the Irish Sea as well as Skerd Rocks on the west coast for the potential construction of turbines. With
increasing technology in this sector the construction of windfarms in water depths between 30-40m
is becoming more and more feasible. This pushes locations for potential windfarms further offshore
away from banks where sedimentary environments are less mobile and therefore scour is less of a
problem.
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1.4 Scope of the Study
We will assess the current state of the offshore renewable energy sector in Ireland identifying the
key datasets as identified by industry as being of vital importance in the construction of offshore
renewable energy installations, investigating the availability of these datasets and assessing
INFOMAR’s ability to provide such datasets highlighting gaps
The chief data requirements referred to consider seabed geology and sedimentary dynamics related
data. However, the scope of the study also considers socio-economic, ecological, metocean and
general physical factors.
A number of case studies regarding data use in successful offshore projects are also presented.
2 Methods
2.1 Industry Appraisal
Telephone interviews and email correspondence were carried out with people identified as having
an interest and currently working in the offshore renewable sector in Ireland as well as abroad.
Similarly the Irish Renewable Energy Summit 2010 was attended in order to network and speak first
hand with industry players as well as gather information regarding the current state of the sector.
The information sought through these correspondences was;
The company’s current interest in Irelands offshore renewable energy sector;
The perceived datasets required in offshore installation construction;
Which of these datasets were sourced from INFOMAR or other state bodies;
Which of these datasets were acquired by third party investigations and surveys;
The level of satisfaction regarding dataset availability and usability;
Any potential areas that company had earmarked for future site investigation.
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2.2 Data Collection and Integration
The basic data source for this desktop study report comes from phone interviews, email
correspondence and data exchange with key people involved in the offshore renewable energy
sector and government bodies undertaken during early 2010. These correspondences provide
technical and non-technical information as well as data pertinent to the industry. Available
information and data, where possible, were summarised in excel spreadsheets, geo-referenced,
incorporated into a GIS. The table below gives an overview of the available data sets and their
sources utilized.
Data Type Data Source
Seabed Sediment Classification GSI (INFOMAR)
Bedforms and Topograhy GSI (INFOMAR)
Faults GSI (INFOMAR)
Water Depth (Bathymetry) GSI (INFOMAR)
Wind Speed, Direction, Frequency Marine Institute
Wave Height, Direction, Period and Power Marine Institute
Tidal Range and Period Marine Institute
Offshore Weather Reports Marine Institute and Met Eireann
Special Areas of Conservation National Parks and Wildlife Service
Special Protected Areas National Parks and Wildlife Service
Commercial Navigation Irish Maritime Development Office
Fisheries Marine Institute
Pipelines and Cables Kingfisher Information Service, Department of
Petroleum Affairs
Shipwrecks Underwater Archeological Unit
Military Exclusion Zones Department of Defence
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3 Appraisal of Industry Needs
3.1 Introduction
Site suitability mapping is an integral part of the construction of offshore installations and requires
data acquisition from across a variety of disciplines. INFOMAR offers a variety of mapping products
for different offshore areas. However, very often companies are forced to carry out in-house surveys
or hire private specialized groups to supplement publically provided data or gather data that is
missing or outstanding.
By documenting industry data needs and subsequently assessing INFOMAR’s ability to satisfy these
needs it is possible in the future to tailor INFOMAR site surveying to maximize data collection
potential hence increasing its data output helping make offshore renewable energy a more
economically viable option in Ireland.
The various datasets and requirements we identified in consultation with industry can subsequently
be grouped into the following broad headings:
Geological Features (Chapter 3.2)
General Physical Features (Chapter 3.3)
Ecological Factors (Chapter 3.4)
Socio-economic Factors (Chapter 3.5)
3.2 Geological Features
An in-depth knowledge of the seabed geology is particularly important to offshore renewable energy
resource development as it heavily influences anchoring and foundation construction for offshore
renewable energy installations which in turn affects cost, one of the main drivers in such projects.
Generally speaking, Geological Features can be divided into three distinct headings:
1) Seafloor Morphology, including:
Seabed slopes and gradients
Bedforms
Seabed Dynamics
2) Quaternary Geology, including:
Sediment type and classification
Depth of transition to bedrock
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3) Solid Geology, including:
Bedrock description
Faults
Oil/gas accumulations
3.2.1 Seafloor Morphology
3.2.1.1 Seabed Dynamics
Seabed dynamics is primarily concerned with mobile sediment and the hydrodynamic regime which
drives them. Essentially the prime concern associated with seabed dynamics is scour which
destructively affects foundations of offshore installations. Negating scour is a costly issue in
construction and where possible areas with high scour potential are excluded from site mapping.
Predicting scour is largely done by modeling based on a series of geotechnical parameters measured
in the sediment from the area under investigation.
3.2.1.2 Seabed Slopes and Gradients
Seabed gradients and slopes are also important in the site identification process as installation
foundations are generally not constructed on slopes greater than 5
o
3.2.1.3 Bedforms
Bedforms are the result of sediment mobility and hence are important to identify when establishing
the hydrodynamic regimes, hence scour potential, of potential sites.
3.2.2 Quaternary Geology
Quaternary geology and associated structures heavily affect foundation design. Classification of
these sediments can be carried out using acoustic techniques. Sub-bottom profiling can identify
sedimentary strata continuity and thickness as well as sedimentary mega-structures. However,
acoustic data must be supported by groundtruthing by way of coring and sampling.
3.2.2.1 Sediment Type and Classification
Information regarding seabed sediments is an important factor in offshore installation construction
as analysis of sediment samples can influence foundation design. They may be used in geotechnical
investigations to assess the various properties of the sediment including strength, cohesion,
liquefaction potential and scour potential as well as the extent of sediment mobility across an area.
As a rule, dense sands and silts are preferred, although gravel is often acceptable.
11
Seabed sediment studies have been carried out most successfully utilizing a combination of broad
scale remote sensing (i.e. acoustic backscatter) and small scale ground-truthing. Information
regarding seabed sediments should be ideally consist of a shapefile containing polygons showing the
dominant type of sediment. This data should be referenced to WGS84 and interpolated from the
best available data for the area. Similarly, for developers who do not have access to adequate
mapping software, a Google Earth kmz file available to download should be provided.
3.2.2.2 Depth of Transition to Bedrock
One of the prime concerns for offshore renewable energy installation construction is the depth to
bedrock and subsequently its composition and competency. Again, this is primarily to assess
suitability for foundation construction. Monopile foundations are preferred for windfarm
development, usually reaching a depth of roughly 35m. Therefore it is important to carry out seismic
surveys which image the sub-seabed to at least 50m. A potential error arising from sub-bottom
profiling is the misinterpreting of glacial till as bedrock so groundtruthing becomes all the more
important in that respect. Coring has the added advantage of providing physical samples for lab
based geotechnical and physical property analysis.
3.2.3 Solid Geology
3.2.3.1 Bedrock Description
As mentioned the depth from seabed to bedrock is of importance in relation to foundation design
and construction. In addition, the subsequent composition and competency of this bedrock is also
important information.
Information regarding bedrock description should be delivered using a shapefile which uses
polygons to show the predominant bedrock with information regarding type, age and formation
name. The additional option of a Google Earth kmz file would be of use to developers who didn’t
have access to adequate mapping software.
3.2.3.2 Faults
Sub-seabed faults are naturally planes of weakness and knowledge of their locations is vital in siting
installation construction. Although Ireland is seismically a quiet area, within the Irish Sea low
magnitude events are often recorded. Similarly, faults can act as conduits allowing for the
accumulation off shallow gas. Therefore the mapping of scarps and other features is important and
can be done using multibeam and side scan sonar techniques.
12
3.2.3.3 Oil/Gas Accumulations
Gas, which may accumulate in the subsurface, proves problematic for site investigations and
foundation installations. Some of the potential risks resulting from shallow gas accumulations
include:
Loss of vessel buoyancy
Blowouts
Gas kicks and minor flows
Loss of drill/installation jack up
Uncontrolled environmental emissions
Technogenic hydrate formation
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4 General Physical Features
Only certain general physical features are applicable to each of the three main types of offshore
renewable energy. In addition, the limits or constraints the data associated with these features
places on siting potential installations is less strict as the technology can often be tailored to meet
varying conditions in the wind, wave or tidal regime at a certain site.
The main general physical features are:
1) Water depth, namely:
Seabed Bathymetry
2) Wind characteristics, including:
Wind speed
Frequency
Direction
3) Wave characteristics, including:
Average period
Wave height
Direction
Significant wave height exceeded 10% and 50% of the time
4) Tidal regime, including:
Maximum current amplitude
Spring tidal ranges
Tidal Period
5) Distance to shore
6) Landfall description
7) Offshore weather reports
4.1.1 Seabed Bathymetry
Water depth is an important factor in site identification for installations and so detailed and
widespread bathymetric maps are a necessity. Construction costs of offshore installations increases
with water depth and so generally greater than 35m water depth is not exceeded. In saying so,
evolving technology is pushing installations to potentially greater depths.
Bathymetry should be delivered in an ASCII file as gridded data referenced to WGS84, interpolated
from the best available data for the area and corrected to mean sea level as well as lowest
astronomical tide. The gridded data should be prepared up to the high water line. The gridded data
14
should be available in resolutions of 1 minute, down to 3 seconds. The additional option of a Google
Earth kmz file for download would help those developers who do not have access to mapping
software.
4.1.2 Wind Characteristics
Wind characteristics are an obvious important consideration for installing wind energy installations.
Generally a wind speed of 9 ms
-1
is preferred. Wind data recorded should consist of wind speed,
direction, frequency and maximum gust. In order to assess the wind generating potential of an area
there must be a continual dataset recording hourly for the past decade.
The Marine Institute has 6 weather buoys located around the Irish coast which constantly record
wind speed and direction as well as the maximum gust. This data is available from the Marine
Institute in an excel spreadsheet form (http://www.marine.ie/home/).
4.1.3 Wave Characteristics
The 6 Marine Institute buoys also collect wave data in the form of wave height, period, peak period,
mean wave spread and mean direction. These data sets are provided by the Marine Institute as excel
spreadsheets. Also available are shapefiles for the average practicable power (see Figure. 3-1) and
the average wave height (see Figure 3-2). The data from these attributes were derived from the
Marine Institute’s Accessible Wave Energy Resource Atlas published in 2005.
http://www.marine.ie/home/
15
Figure 4-1: Annual Average Wave Power
16
Figure 4-2: Annual Average Wave Height
17
4.1.4 Tidal Regime
In order to harness tidal energy an understanding of the hydrodynamic regimes is needed. ADCP
deployments provide crucial hydrodynamic data that are necessary to calibrate tidal models. Tidal
models can then input …
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