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    Opportunities for CO2

    Storage

    around Scotland an integrated strategic

    research study

    www.erp.ac.uk/sccs

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    University of Edinburgh, April 2009.

    A collaborative study published by the Scottish Centre for Carbon Storage

    Printed in Scotland by Scotprint, Haddington, East Lothian.

    Text and cover are printed on Revive 50/50 which is FSC Cover is laminated with cellogreen gloss

    and book can be recycled and is biodegradable.All parts are chlorine free, acid free, recyclable and bio-degradable.

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    ForewordRapid man-made climate change is the greatest environmental challenge acing us today. The principal

    human inuence on our climate is emission o greenhouse gases, including CO2, rom our use o ossil uels.

    The Scottish Climate Change Bill will introduce ambitious legislation to reduce these greenhouse

    gas emissions by 80 per cent by 2050. This will highlight many challenges or Scotland, particularly in

    terms o addressing our uture energy needs and in generating energy efciently and sustainably in

    environmentally neutral ways. We will thereore have to adopt new thinking, new solutions, and new

    technologies, and this presents the opportunity to put Scotland at the oreront o building a sustainable

    low carbon economy.

    A major contribution could be made by the capture and transport o CO2

    rom power stations and

    large industrial sites, to storage in underground reservoirs oshore thus demonstrating that this

    technology can play a key part in our sustainable energy uture.

    The Scottish Centre or Carbon Storage has brought together the expertise o a number o our leading

    scientists, engineers and technologists rom a range o disciplines and organisations to address the

    potential or, and challenges associated with, carbon capture and storage in Scotland.

    A key conclusion o the report is that Scotland has not only the storage capacity but also the

    geographical context and know-how to become a major hub or CO2

    transport and storage in Europe.

    Scotland is thereore uniquely placed to beneft rom being an early adopter and, through its world

    class science and technology, to be amongst the leading nations involved in the study o carbon capture

    and storage, exporting skills and knowledge globally into what could become one o the worlds largestenergy markets.

    This is the most comprehensive study o its type undertaken in the UK and I hope that the report

    will stimulate urther debate on the way orward or Scotland, in terms o carbon capture and storage

    technologies.

    Proessor Anne Glover, Chie Scientic Adviser or Scotland.April 2009.

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    Scottish Centre or Carbon Storage www.erp.ac.uk/sccs

    Contents

    Executive summary

    The way forward

    1 Introduction 14

    2 CO2

    sources 58

    3 CO2

    storage sites 916

    4 CO2- Enhanced Oil Recovery 1722

    5 CO2

    injection modelling

    within saline aquifers 2324

    6 CO2

    transport optionsbetween sources and storage sites 2530

    7 Economic modelling of potentialCCS schemes in Scotland 3134

    8 Business risks faced by earlyCCS projects 3536

    9 Business models 3738

    10 Funding mechanisms 3941

    11 Comparison with other carbonabatement options 42

    Concluding remarks 43

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    Scottish Centre or Carbon Storage www.erp.ac.uk/sccs

    Scottish Renewable Energy Zone (Designation o Area) (Scottish Ministers) Order 2005

    area o study

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    Scottish Centre or Carbon Storage www.erp.ac.uk/sccs

    Executive summaryCarbon Capture and Storage (CCS) is one o the critical technologies worldwide which will enable reduction o

    carbon dioxide (CO2) emissions arising rom large industrial sites. CCS allows the continued use o a diverse mix

    o energy sources, including ossil uels, which improves the security o cost-eective electricity supply. Scotland

    has the opportunity and responsibility to reduce CO2

    emissions arising rom burning o ossil uels and their

    impact on climate change.

    The EU plans to have 12 CCS plants operating by 2015. In February 2009, the UK Secretary o State or Energy

    and Climate Change stated an aspiration or the UK to have more than one demonstration project in operation

    enabled by government unding. However, these targets cannot be delivered without the underpinning knowledge

    rom studies such as this.

    Commitment to large-scale investment in CO2

    capture plant will require proven storage capability.

    This study

    presents the frst high-level screening o CO2

    storage sites available to Scotland

    evaluates the means by which CO2

    can be transported rom power plants and other industrial activities to

    storage sites, and

    investigates the costs and business constraints.

    This is the most comprehensive and ully integrated study perormed in the UK, and was achieved by a

    collaborative partnership o Scottish Government, research universities and institutes, and a broad base o

    support rom industry and business.

    The conclusions show that Scotland has an extremely large CO2

    storage resource. This is overwhelmingly in

    oshore saline aquiers (deeply buried porous sandstones flled with salt water) together with a ew specifc

    depleted hydrocarbon felds. The resource can easily accommodate the industrial CO2 emissions rom Scotlandor the next 200 years. There is very likely to be sufcient storage to allow import o CO

    2rom NE England,

    this equating to over 25% o uture UK large industry and power CO2

    output. Preliminary indications are

    that Scotlands oshore CO2

    storage capacity is very important on a European scale, comparable with that o

    oshore Norway, and greater than Netherlands, Denmark and Germany combined.

    CO2

    storage in oil felds may be easible in conjunction with CO2-Enhanced Oil Recovery (CO

    2-EOR). I oshore

    pipelines reliably delivering CO2

    could be developed through demonstration projects, then an increased number

    o oilfelds could become economic or EOR providing other critical actors such as oil price, additional oil

    recovery and inrastructure suitability are also avourable. Additional benefts include delayed decommissioning

    costs and extended beneft to the economy through development o technology and expertise in oshore CO2-

    EOR. However, contrary to many expectations, this study has shown that most oilfelds in the northern North

    Sea cannot easily be used solely or CO2

    storage because sea water injection, commonly used to maintain feld

    pressure during oil production, signifcantly reduces the amount o storage capacity or CO2.

    Pipelines are the best option or the secure and continuous transport o millions o tonnes o CO2

    rom dierent

    CO2

    sources to collection hubs onshore and then to oshore storage hubs or local distribution to diverse

    storage sites. Several routing options exist and, importantly, can include the connection o pipelines carrying CO2

    originating rom England or continental Europe. Capital and operational costs or CCS projects are similar to

    those o the hydrocarbon industry.

    Electricity generated in Scotland rom power plant ftted with CCS is shown by this study to be comparable in

    price to that generated rom other low-carbon technologies. The cost o abatement per tonne o CO2

    is cheaper

    on coal plants than on gas, because coal produces larger amounts o CO2

    per unit o electricity. However, the

    cost per unit o low-carbon electricity rom coal and gas CCS is approximately the same.

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    The key conclusions o the study are:

    1. The amount o CO2

    produced rom industrial sources within Scotland is about a tenth o that o

    the UK as a whole. Without CCS, Scotland is likely to produce between 300 and 700 million tonnes o CO2

    rom 2010 to 2050 that is, on average, between 8 and 18 million tonnes per year (Mt/year) depending on the

    proportions and types o power generation. In 2006, CO2

    output rom major industrial sources in NE England

    amounted to over 50 Mt/year.

    2. Geological reservoirs suitable or storage o CO2

    are classifed according to whether they contain

    (or have contained) oil, gas, or saline water. Saline aquiers have the largest storage potential but with

    uncertainties regarding storage capacity o individual sites. From a resource o more than 80 saline aquiers

    studied, ten have been identifed with a total potential CO2

    capacity in the range 4,600 to 46,000 million tonnes

    a capability to store more than 200 years o Scotlands CO2

    output rom its major fxed industrial sources.

    3. Initial costs o assessing potential saline aquier stores are likely to be considerably higher than or

    oil and gas felds which have previously been ully evaluated during many years o both exploration and

    production operations. Only detailed appraisal studies that include drilling o boreholes are likely to provide

    sufcient confdence to initiate a commercial-scale CCS project. Thus, pilot CO2

    capture projects will be an

    essential element o developing any new CO2

    storage site.

    4. From a resource o more than 200 hydrocarbon felds, 29 have been identifed as clearly having

    potential or CO2

    storage. Four gas condensate felds and one gas feld oer signifcant potential or CO2

    storage. However, most o the oil felds can only be used as CO2stores in conjunction with CO

    2-EOR technology.

    5. CO2-EOR may act as a stimulus or CCS especially i developers come to expect that the price

    o oil will remain over US$100 per barrel or the period o their investment. Development o a CCS

    inrastructure in Scotland could lead to application o CO2-EOR (and, thereore, additional oil production and

    revenue) in certain felds.

    6. Storage hubs are proposed to give multiple storage options within a geographical area to reduce

    costs and risks to CCS inrastructure. A pipeline network would be used to transport 20 million tonnes/

    year o CO2

    rom sources to distribution hubs oshore. Capital costs are 0.7 to 1.67 billion, depending on hub

    location. The hubs are proposed to give multiple storage options within a geographical area to minimise costs

    and risks to CCS inrastructure. The preerred route is through an onshore pipeline rom the Firth o Forth to

    St Fergus, then onwards to an oshore storage hub, while an oshore pipeline route rom the Firth o Forth

    should also be considered. Transport o additional CO2

    rom NE England is best served by a pipeline direct to an

    oshore storage hub. Ship transport is possible as an interim solution, ideally discharged at the oshore hub.

    7. A phased approach is appropriate to support the development o CCS technology. Direct

    Government unding will be required in the short term or R&D and pilot projects. In the medium term, CCSdemonstration projects required under the UK Government and EU programmes, will need income support.

    Other low-carbon technologies, such as renewable power generation, currently receive incentives which are

    envisaged to continue or the medium term. In the long term, low-carbon generation projects are capable

    o being supported by the price o carbon alone. However, the volatility o the carbon market will place an

    additional fnancial risk on such projects.

    8. The long term carbon abatement cost o CCS coal and CCS gas appear comparable with other

    available low-carbon power generation technologies and CCS has the potential to materially contribute to

    carbon abatement in Scotland.

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    Scottish Centre or Carbon Storage www.erp.ac.uk/sccs

    The way forwardScotland has the potential to become a signifcant player in the CCS industry both in its practical application,

    using its signifcant oshore resource, and in the development o exportable technology and skills. However,

    having examined

    the levels o unding required

    the levels o risk

    the regulatory structures

    and potential business models

    the study has concluded that CCS will not commence without signifcant Government support and initial unding,

    similar to that required to develop low carbon wind and marine technologies. This strategic study has identifed key

    initiatives that need to be acted upon to move CCS orward in Scotland.

    1. There is a need or more detailed evaluation o Scotlands oshore storage sites. Saline aquiers

    represent the major CO2

    storage opportunity. For these to be the basis o viable CCS projects there is a

    need or detailed mapping and evaluation o specifc saline aquiers, akin to that undertaken by the oil industry

    assessing hydrocarbon prospects prior to exploratory drilling. Early assessment will greatly speed-up the

    development o viable CCS projects.

    2. I CCS projects are to make progress in the short term, there is a need or direct Government

    assistance to support R&D activity, which can prove the availability o storage in oshore saline aquiers and

    gas felds. I sufcient storage capacity oshore Scotland is proven, then EU-sized transport and storage industries

    can develop. In the medium term, income support estimated at 100 M/year is required per project to construct

    and operate the number o large projects envisaged in the UK and the EU. This will reduce i the carbon market

    price reaches stability at a commercially attractive level, and make CCS a long-term proftable option.

    3. New alliances o businesses are needed to deliver CCS as early demonstration projects will ace

    uncertainties o cost, technical operation and income. These frst demonstrator projects are essential to start a

    process o learning, improvement, and cost reduction. No UK CCS will develop until these demonstrators are

    implemented and evaluated.

    4. At high oil prices CO2-EOR may lower the overall level o support required or early CCS

    demonstration projects, provide incentives or industry development and add volume to Scotlands

    hydrocarbon reserves. Projects to assess the viability o CO2-EOR in specifc oil felds or clusters o oil felds

    could thereore be important.

    5. A CCS transport inrastructure is essential to connect sources with stores. Subject to suitability,existing pipeline networks may be exploited to varying degrees within the context o early pilot operations

    through to industrial scale demonstration projects.

    6. Political and public support is crucial or progressing CCS. Public investment is likely to be required,

    initially at least, to ensure that the inrastructures are established and the private sector receives sufcient

    incentive to establish demonstration projects and to develop the technologies. To reduce the fnancial uncertainty

    to acceptable levels, additional monetary support is needed, as is given to renewable power generation.

    7. The successul development o CCS in Scotland requires an assessment o the existing diverse

    skills base to identiy where we need to build expertise. Academia and industry, working with the Scottish

    Government, can then address these issues.

    8. Initiate an environmental assessment that will engage the relevant agencies and allow early considerationo the environmental issues associated with the deployment o CCS.

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    Scottish Centre or Carbon Storage www.erp.ac.uk/sccs

    Aerial view o Longannet Power Station. Courtesy o ScottishPower.

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    Scottish Centre or Carbon Storage www.erp.ac.uk/sccs1

    1| IntroductionThis document reports the results and recommendations o a study o the key issues bearing on the

    development and deployment o Carbon Capture and Storage (CCS) technology in Scotland. It was

    unded by the Scottish Government and industry, and was conducted by the Scottish Centre or

    Carbon Storage in cooperation with key industry participants.

    The key issues are:

    identiying and assessing potential carbon storage sites in Scotland

    appraising Scottish inrastructure and the costs o developing it to enable CCS projects

    understanding the regulatory environment or CCS

    understanding the economics o CCS projects.

    This study has:

    identifed the principal sources o carbon dioxide (CO2) that could be captured and stored (that

    is, power generation and major fxed industrial plants) throughout Scotland and NE England and

    modelled their likely uture emissions

    screened potential CO2

    storage sites to identiy those that are likely to be sae and commercially and

    technically viable

    examined the economics and practicality o enhanced oil recovery using CO2 in North Sea oil felds

    developed a high-level model or a transport network capable o taking CO2

    rom these sources to

    oshore CO2

    storage sites

    examined current and uture regulations that may aect CCS

    identifed gaps between the current commercial/fscal conditions and those required to make CCS

    commercially viable

    created the evidence base and economic models required to support inormed decisions regarding

    the early development o CCS inrastructure in Scotland

    established the urther steps necessary to make large scale CCS in Scotland a reality.

    The results o this strategic study have been derived rom scientifc literature, data rom a variety o

    governmental organisations, and calculations and conclusions generated within the study itsel.

    It is now established that man-made emissions o carbon dioxide (CO2) are a major contributor to

    climate change. Carbon Capture and Storage (CCS) has the potential to enable very large reductions in

    CO2

    emissions arising rom major industrial sources such as the generation o electricity. CCS is one o

    several possible options or reducing the rate o build-up o CO 2 in the atmosphere and should be seenas orming part o an overall CO2

    mitigation strategy.

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    Scottish Centre or Carbon Storage www.erp.ac.uk/sccs2

    Adapted from IEA. World EnergyOutlook 2007. Fig 5.12

    World CO2emissions

    Figure 1

    Wedge diagram illustrating proportions o dierent init iativesrequired to reduce CO

    2concentration in the atmosphere.

    Adapted rom IEA. World EnergyOutlook 2007. Fig 5.12

    World CO2emissions

    CCS comprises a set o technologies that together enable CO2

    to be captured rom industrial point

    sources, be processed, transported via pipelines (or ships in certain cases) and injected into deep rock

    ormations at 1000 to 2500 m below the Earths surace (Figure 2). At present, a small number o CCS

    projects have been initiated within the UK and the EU but as yet there are none within UK waters

    o the North Sea. For instance, there are two projects operating within Norwegian waters, one at

    the Sleipner Field in the Norwegian sector o the northern North Sea, the other at the Snhvit Field

    oshore northern Norway which transports CO2

    via a 150 km pipeline to a subsea injection location.

    There is also a small scale injection test being undertaken at the K12B Gas feld oshore Netherlands.

    This can be illustrated using stabilisation wedges where each wedge represents a strategy to reduce

    CO2

    emissions (Figure 1). The thickening o each wedge reects take up o the particular CO2

    reducing

    initiative.

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    Scottish Centre or Carbon Storage www.erp.ac.uk/sccs3

    CO captured at the power plant2

    Oil field EnhancedOil Recovery (EOR)Gas field

    Saline aquifer

    Caprock

    Caprock

    CO is piped offshore2

    CO injection at a rig2

    CO is injected underpressure via a well intothe storage site

    2

    Compression

    Oil

    CO2

    Increasing temperatureand pressure

    BritishGeologicalSurvey

    Figure 2

    Schematic showing elements o CCS inrastructure and

    relationship with geological structure.

    Although a gas at the Earths surace, carbon dioxide takes a very dierent physical orm under only

    slightly changed conditions. Most people are amiliar with the cold, solid orm known as 'dry ice' that

    CO2

    takes when rozen. By contrast, when placed under moderate pressure (73.7 bar or greater),

    and warmed (to greater than 31.1C), it becomes a dense uid with properties o both a liquid

    (density) and a gas (viscosity). In this orm, CO2

    occupies one hundredth o the volume it does as a

    gas. Nevertheless, liquid CO2

    (density 0.7 g/cm3) is less dense than water (1.0 g/cm3) and like oil will

    oat upon water. Thus some orm o physical containment is needed to prevent upward migration and

    leakage in a subsurace store, and the physics o liquid CO2

    thereore place depth and temperature, as

    well as geological, constraints on any potential storage reservoir (Figure 2). In this dense state, CO2

    is

    readily and efciently transported by pipeline, as it ows like gas.

    Choice o study area

    The extent o the study area is shown by the limits o the Scottish Renewable Energy Zone which

    spans onshore Scotland and extends to oshore areas and is defned in The Renewable Energy Zone

    (Designation of Area) (Scottish Ministers) Order 2005, ISBN 0110736176 (see map acing Contents

    page). Although this limit excludes a large number o potential carbon dioxide storage sites it defnes

    an area covered by Scottish environmental statutes and as such lies within a legally defned area.

    Competition and/or co-operation with other potential carbon dioxide storage sites outwith the area

    defned in this study is possible but was not considered in detail in this study. The study ocussed on the

    oshore area to the east o Scotland as this is closest to the major Scottish and northern English CO2

    sources. The geological ormations with the greatest potential or storage o CO2

    are located oshore

    and include a large number o hydrocarbon felds and saline aquiers and the data to enable meaningul

    assessment.

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    Scottish Centre or Carbon Storage www.erp.ac.uk/sccs4

    Part o the Sleipner Field CCS inrastructure, oshore Norway. Courtesy o StatoilHydro.

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    Scottish Centre or Carbon Storage www.erp.ac.uk/sccs5

    S c o t l a n dS c o t l a n d

    E n g l a n dE n g l a n d

    N o r t h e r n I r e l a n dN o r t h e r n I r e l a n d

    0 25 50 75 100

    Kilometers

    Longannet

    U l s t e r U l s t e r

    L e i n s t e r L e i n s t e r

    I s l e o f M a nI s l e o f M a n

    W a l e sW a l e s

    Cockenzie

    Peterhead

    Greystones

    Drax

    Eggborough

    SaltendFerrybridge

    Teeside

    Scunthorpe

    St Fergus

    Stirling

    Grangemouth

    Mossmorran

    Legend

    2006 CO2 Emissions (Mt)

    0 - 2

    2 - 4

    4 - 6

    6 - 8

    8 - 10

    10 - 22

    The Scottish Renewable Energy Zone

    Steel Works

    Power Station

    Industrial Site

    Hunterston

    Figure 3

    Relative proportions o CO2

    emitted by source in 2006 in the UK.

    Domestic 14.3%

    Commercial and

    public services 3.9%

    Agriculture and

    orestry uel use 0.8%

    Transport 23.5%

    Power stations 33%

    Other energy

    industry 5.7%

    Other industrial 17.3%

    Other sectors 1.5%

    Figure 4

    Location o industrial sources o CO2

    emissions in

    Scotland and NE England that emitted more than100, 000 tonnes per year in 2006.

    2| CO2

    sourcesIn this section, the principal

    industrial sources o CO2

    (power generation and

    industrial plant) in Scotland

    and NE England are identifed,

    and the levels o output or

    sources in Scotland during

    2006 are quantifed. Likely

    levels o CO2

    output are then

    estimated or 2020, 2030 and

    2040 by considering various

    energy generation mixes. This

    inormation is used to quantiy

    CO2

    storage and transport

    requirements and to plan a

    network inrastructure that will

    respond to these requirements.

    Scotlands total CO2

    emissions in

    2006 were estimated to be 44 Mt,

    around 8% o the total UK emissions

    o approximately 557 Mt. The majority

    o the large fxed sources o CO2 arepower generation plants, which give

    rise to 33% (~184 Mt) o the UK total;

    integrated steel plants and the larger

    oil refnery/petrochemical complexes

    are urther signifcant sources. O the

    remaining sources o emissions, the

    largest single contribution was rom

    transport (23.5%) (Figure 3).

    All the major energy generators andindustrial point sources o CO

    2in

    England, Wales and Scotland that emit

    more than 10, 000 tonnes o CO2

    per

    year report this output to the National

    Atmospheric Emissions Inventory

    (NAEI) and the Scottish Environmental

    Protection Agency (SEPA) (Figure 4).

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    Scottish Centre or Carbon Storage www.erp.ac.uk/sccs6

    Figure 6

    CO2

    output at 2020 or

    11 Scottish scenarios.

    Figure 5

    Top ten CO2

    sources in Scotland

    and northern

    England in 2006. Drax Power station 22.4 Mt

    Longannet Power station 9.6 Mt

    Ferrybridge C Power station 8.9 Mt

    Eggborough Power station 7.6 Mt

    Scunthorpe steelworks 3.9 Mt

    Saltend CCHP 3.1 Mt

    Peterhead Power station 3.1 Mt Teeside steel works 3 Mt

    Cockenzie Power station 5 Mt

    Greystones Power station 4.9 Mt

    In 2006, approximately 18 Mt o CO2

    (around 41% o Scotlands total carbon emissions) was produced

    by Scotlands three largest power stations. The output o Longannet alone is approximately 10 Mt.

    A combined total o 71 Mt o CO2

    (~24% o total UK fxed industrial) was produced by the top ten

    sites in Scotland and NE England (Figures 4 and 5).

    For Scotland, the amount o CO2

    produced in the uture will largely depend upon the method o energy

    generation and the relative proportions o types o energy supplied. Likely levels o CO2

    production

    were considered or 2010, 2020, 2030 and 2040. For 2010, it was assumed there would be little

    change in output rom fgures provided or 2006 (Figure 5). A range o scenarios or CO2

    production

    in 2020, 2030 and 2040 is summarised below (Figures 6, 7 and 8). For each o these years, dierentenergy mixes were analysed, with no judgement as to which scenario was more likely, and a range

    o possibilities presented. (Tables 1, 2 and 3). The scenarios yield high, medium or low CO2

    output

    reecting the dierent energy mixes. The examples shown in Figures 6, 7 and 8 assume that carbon

    capture technology is not installed. Note that i carbon capture equipment were installed, gross (prior

    to capture and storage) CO2

    output would be higher, by between approximately 12% (CCS mature)

    and 25% (CCS immature) reecting the additional energy required to extract the CO2

    and puriy it.

    However, the extra CO2

    produced by the carbon capture process will, by defnition, be captured as

    part o this process and should not result in additional CO2

    being released into the atmosphere.

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    Scottish Centre or Carbon Storage www.erp.ac.uk/sccs7

    Energy mix Renewables % Nuclear % Coal % Gas % CO2

    output Mt

    1 30 15 45 10 23.6

    2 30 0 35 35 23.3

    3 40 0 30 30 19.9

    4 50 0 35 15 19.7

    5 30 15 27.5 27.5 18.3

    6 40 15 22.5 22.5 15.1

    7 50 15 17.5 17.5 11.7

    8 30 35 0 35 6.4

    9 40 35 0 25 4.7

    10 65 15 0 20 3.8

    11 50 35 0 15 2.8

    Energy mix Renewables % Nuclear % Coal % Gas % CO2

    output Mt

    1 40 0 30 30 15.1

    2 50 0 35 15 14.1

    3 40 15 22.5 22.5 11.5

    4 50 15 17.5 17.5 8.9

    5 30 35 17.5 17.5 8.9

    6 40 35 0 25 4.6

    Table 1

    Proportions o dierent

    energy generation methods

    or each o the 11 scenarios

    possible or 2020.

    Figure 7

    CO2

    output at 2030 or 6 Scottish scenarios.

    Table 2

    Proportions o dierent

    energy generationmethods or each

    o the 6 scenarios

    possible or 2030.

    For 2030, CO2

    production

    was calculated on the basis

    o electricity demand as at

    present. Calculations assuming

    a year on year 1% increase o

    electricity demand rom 2020

    to 2030 were also carried out

    but did not change the ranking

    o energy mix scenarios.

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    Scottish Centre or Carbon Storage www.erp.ac.uk/sccs8

    Energy mix Renewables % Nuclear % Coal % Gas % CO2

    output Mt

    1 40 0 55 5 18.6

    2 40 0 40 20 16.5

    3 50 0 35 15 14.1

    4 40 0 20 40 13.7

    5 50 0 20 30 11.9

    6 40 15 20 25 11

    7 60 0 20 20 10.1

    8 50 15 17.5 17.5 8.8

    9 40 35 0 25 4.6

    10 60 15 0 25 4.6

    11 50 35 0 15 2.8

    12 60 25 0 15 2.8

    Figure 8

    CO2

    output at 2040 or 12 Scottish scenarios.

    Table 3

    Proportions o dierent

    energy generation

    methods or each

    o the 12 scenarios

    possible or 2040.

    For 2040, CO2

    production

    was calculated on the basis

    o electricity demand as at

    present. Calculations assuming

    a year on year 1% increase in

    electricity demand rom 2030 to

    2040 were also carried out but

    did not change the ranking o

    energy mix scenarios.

    CO2

    Sourceskey conclusions

    For Scotland over a 40-year period rom 2010 to 2050, total output rom electricity generation alone

    will produce CO2

    outputs o:

    ~ 700 Mt or 17.5 Mt/year under a high CO2-output scenario;

    ~ 320 Mt or 8 Mt/year under a low CO2-output scenario assuming no nuclear power.

    Additional major sources in NE England produced ~50 Mt CO2

    in 2006. Thus, i outputs rom both

    regions are included, over the period to 2050, up to 3000 Mt CO2

    is potentially available or capture

    and storage. This is equivalent to 75 Mt CO2 per year taking this high-case scenario.

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    3| CO2

    storage sitesTo establish whether the Scottish oshore area has the potential or storing the amounts o CO

    2

    captured, the study identifed and assessed potential CO2

    storage sites in the oshore area in terms o

    their relative storage capacities and geotechnical criteria.

    Potential CO2

    storage sites in the oshore area are:

    saline aquiers and;

    hydrocarbon felds.

    Hydrocarbon felds have, by defnition, the proven ability to trap migrating gas and oil in suitable

    reservoir rock or many millions o years. Hydrocarbon felds that may be suitable or CO2

    storage are

    those that either have ceased production, or will do so within the period covered by the study, or

    those that are suitable or enhanced oil recovery using CO2

    (CO2-EOR).

    Only a relatively small proportion o reservoirs contain hydrocarbon accumulations; the vast majority

    o potential reservoir rocks (typically sandstone in the North Sea) are flled with saline water, and these

    are known as saline aquiers.

    Common to all types o storage site, the key metrics or assessing a potential site are:

    location;

    data availability;

    storage capacity;

    geotechnical characteristics o the storage site;

    timing o storage site availability.

    3.1 Location

    The area defned by the Scottish Renewable Energy Zone oshore has been examined (see map

    acing Contents page). It contains approximately 204 hydrocarbon felds (comprising 163 oil, 30 gas

    condensate and 11 gas felds) and 80 saline aquiers that might be suitable or the storage o CO 2. These

    numbers may increase in uture as urther hydrocarbon felds or saline aquiers may yet be discovered.

    3.2 Data availability

    Eighty (40%) o the known hydrocarbon felds and twenty-one (26%) o known saline aquiers were

    not screened and assessed because o various issues such as lack o readily available data, confdentiality,

    time or budget (Figures 11 and 12). Many o these sites could be suitable or CO2

    storage.

    Nevertheless, the storage sites remaining are considered to be representative o the whole area and

    include a large proportion o the potentially available capacity. Additional data rom companies and

    government may well augment this list o potential storage sites as well as improve our understanding

    o those already identifed.

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    British Geological Survey

    Figure 9

    Cartoon illustrating porosity and permeability within the reservoir volume.

    3.3 Storage capacity and suitability

    The CO2

    storage capacity o a

    hydrocarbon feld or saline aquier

    depends upon several actors. The

    total volume o the storage

    reservoir is relatively straightorward

    to determine, provided appropriate

    data is available. At a microscopic

    scale, reservoir rocks (or example,

    sandstones) contain spaces (between

    sand grains) within which uids can

    be stored, or through which uids

    can pass (Figure 9). The proportion

    o the total volume available or uids

    is its 'porosity', and the ease with

    which uids can pass through rock is

    described by its 'permeability'.

    These spaces are flled with either hydrocarbons (oil, gas or gas condensate) or saline water. These

    uids are all pressurised to a certain degree and must be displaced to allow storage space or CO2.

    Thus, it is important to distinguish whether a reservoir is in open pressure communication with

    surrounding rocks or whether it is closed.

    For oil felds not in pressure communication (closed), water is oten injected to pressurise the

    reservoir and produce oil. Once production has ceased, much o the oil has been replaced by water

    but the reservoir may still be under high pressure. CO2

    injection will cause urther pressurisation.

    This places signifcant limits on the amount o CO2

    that can be stored in this type o reservoir, since

    excessive pressure may ultimately cause racturing o the caprock. The capacity available or CO2

    can

    be increased by permitting urther uid production, either o additional oil or o the water previously

    injected which would require clean-up by extracting oil to meet current environmental standards prior

    to discharge to sea.

    For gas and gas condensate felds the situation is dierent (even i closed) as production is usually

    driven by expansion o the gas without the need or water injection to maintain pressure. Thus

    pressure is likely to be very low by the time these felds become ready or CO2

    storage.

    For closed saline aquiers pressure will again be the signifcant limiting actor. This was confrmed by

    numerical modelling carried out or this study and summarised later in this report (Section 5). Water

    production may be required to control pressure increase.

    CO2

    injected into open reservoirs is accommodated by lateral displacement o the existing uids,

    and gives rise to minimal, local changes in pressure. The storage capacity oopen saline aquiers is

    limited by how well the CO2

    displaces the saline water (its sweep efciency), the proportion o the

    saline aquier that is structurally closed (trapping the CO2) and the amount o CO

    2retained during

    migration. Open reservoirs oer better potential or CO2

    storage.

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    For the purpose o this strategic

    study, storage capacity was

    calculated at a basin-wide scale.

    This provides a ranking o potential

    storage sites but not absolute

    capacities. The best estimate o

    storage capacity o each reservoir

    will be refned as assessment

    becomes more ocused (Figure 10).

    For hydrocarbon felds, this basin-

    scale assessment enabled a ranking o

    their storage capacity. Following this

    analysis, the 95 hydrocarbon felds

    o estimated capacity less than 50

    Mt CO2

    were considered too small

    to be viable or CCS storage and so

    were not examined urther (Figure

    11). Note that stores with less than

    50 Mt CO2

    storage capacity may have

    value as satellites to larger sites or

    as part o a pilot or smaller scale demonstration project. Pressure-related issues urther constrain the

    possibilities o using oilfeld reservoirs or CCS.

    The majority o oil felds in the Scottish oshore area are closed and would require signifcant

    production o uids (mainly previously injected water) to enable secure injection o signifcant

    quantities o CO2. This is unlikely to be practical except in combination with enhanced oil recovery

    (CO2-EOR). As part o this study, oil felds were assessed or their suitability or CO

    2-EOR and this is

    detailed in the next section entitled CO2ENHANCED OIL RECOVERY (Section 4).

    The Brent Oil Field is a possible exception as pressure support has been withdrawn and water

    produced in order to drop the pressure and release the gas contained within the remaining oil. As a

    result, there may be a CO2

    storage opportunity once depressurisation is complete and production has

    ceased (Table 4).

    For gas and gas condensate felds, ewer limitations due to pressure in the reservoir are likely to

    be present. In all the gas condensate felds listed, there is minimal water replacement on production

    o hydrocarbons. Consequently, a large proportion o the pore space will be available or CO2

    storage.

    However, three o the gas condensate felds, classifed as High Pressure High Temperature (HPHT)

    felds, are likely to be too costly to develop as CO2

    stores. In the Frigg Gas Field, water is used to drive

    the gas and consequently a smaller proportion o the available pore space will be available or CO2

    storage (Table 4).

    UncertaintySt

    orageVo

    lume

    Country/StateScale Screening

    BasinScale Assessment

    Site Characterisation

    Site

    Deployment

    Prospective

    Storage Cap

    Contingent

    Storage Capacity

    Operational

    Storage CapacityDecreasing

    Uncertainty

    and Storage

    Volume

    Increasing

    Data and

    Eort

    Adapted rom CSLF 2007 Storage Pyramid

    modied 2008 CO2CRC

    Storage Capacity Estimation

    Total Pore

    Volume

    Figure 10

    Storage pyramid illustrating dierent stages in CO2

    storage capacity assessment. This study takes the

    assessment to near the top o basin-scale.

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    204 hydrocarbon elds identied

    within area o study

    80 hydrocarbon elds

    excluded through lack

    o data

    29 hydrocarbon elds taken

    orward or assessment

    95 hydrocarbon elds excluded as

    storage capacity less than 50 Mt

    Figure 11

    Numerical breakdown o the 204

    Hydrocarbon elds identied within the

    study area showing proportion o elds

    taken orward or assessment.

    Field name Verticaldepthto crest

    (m)

    AveragePorosity(%)

    AveragePermeability(milli-Darcies)

    Close oProductionyear

    Averagewaterdepth(m)

    EstimatedCO2 Storage(Mt)

    Brae North GC 3633 15 300 2015 99 52

    Franklin GC HPHT 5050 16 10 2030 93 62

    Elgin GC HPHT 5300 17 25 2030 93 63

    Shearwater GCHPHT

    4700Not

    availableNot

    available2015 92 66

    Brae East GC 3865 17 558 2020 116 111

    Britannia GC 3597 15 60 2030 136 181

    Bruce GC 3250 15 153 2020 122 197

    Frigg (UK) Gas Field 1785 29 1500 2008 112 171

    Brent Oil Field 2512 21 650 2015 140 456

    Table 4

    Hydrocarbon elds assessed as having potential or CO2

    storage alone.

    In summary, basin-scaleanalysis was used to identiy

    29 hydrocarbon felds with

    apparent potential or CO2

    storage (Figure 11). O these,

    our gas condensate felds (Brae

    North, Brae East, Britannia and

    Bruce felds), one gas feld (the

    Frigg Field, UK) and one oil feld

    (the Brent Field) present the most

    obvious opportunities as stores (Table 4) with total CO2 storage capacities o between 300 to 1000 Mt. Therange o storage potential values reects uncertainty with regard to assumptions in the calculation o storage

    capacity. The three HPHT gas condensate felds (Franklin, Elgin and Shearwater felds) are likely to be too

    expensive to develop as stores in the short term (Table 4). Fourteen oil felds, including the Brent Oil Field,

    have potential or CO2storage in conjunction with Enhanced Oil Recovery (see ollowing section 4). The

    remaining seven oil felds oer large storage capacities but reservoir pressure issues may present obstacles

    to their use or CO2storage (Figure 13).

    Green parameter is technically or economically avourable

    Orange parameter is technically or economically borderlineRed parameter is technically or economically unavourable

    GC = Gas Condensate feld

    HPHT = High Pressure High Temperature feld

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    Reservoir Attribute Best practice requirements Minimum technicalrequirements

    Depth >1000 m and < 2500 m >800 m and 500 mD >200 mD and 20% >10% and

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    Saline aquier Area (km2) CO2

    storage capacity (Mt CO2)

    assuming 0.2% storage efciency

    CO2

    storage capacity (Mt CO2)

    assuming 2% storage efciency

    Forties 16069 886 8856

    Grid 17147 785 7847

    Balder 6251 347 3465

    Flugga 1926 61 611

    Frigg 1712 58 575

    Mey 33190 1655 16549

    Heimdal 11065 618 6177

    Tay 2484 133 1328

    Captain 3438 36 363

    Mains 4601 24 241

    Total CO2

    storage capacity (Mt) 4603 46012

    Table 6

    Saline aquiers assessed as having potential or CO2

    storage showing

    the range o potential storage capacities calculated rom storage

    eciencies derived rom regional studies and numerical modelling.

    3.5 Timing o storage site availability

    As a practical working assumption, unless a hydrocarbon feld is to undergo CO2-EOR storage, CO

    2

    storage cannot begin until production ceases. Close o production (CoP) or all hydrocarbon feldswas estimated rom past production data (Table 4). For oil felds the CoP is o limited relevance, as use

    or storage without EOR is unlikely and CO2-EOR will necessarily begin prior to the estimated closure

    date. It has been assumed that there are no timing restrictions governing the availability o saline

    aquiers, although exploration and appraisal o saline aquiers may take a number o years. One o the

    most pertinent issues or the development o a CCS transportation pipeline involving hydrocarbon

    stores is the matching o timing o CO2

    supply (rom onshore sources) with available injection

    and storage capacity. Re-use o hydrocarbon production acilities may be an option in some cases.

    Historically, close o production orecast dates have tended to be unreliable, and depend on technology

    development, oil and gas prices, inrastructure lietimes, and other market actors.

    Oil & gas felds are currently better characterised in terms o both capacity and integrity than are saline

    aquiers so initially involve lower cost and risk. Without Enhanced Oil Recovery, oilfelds oer limited

    capacity due to the past replacement o produced oil with water or pressure support. Depleted gas

    and gas condensate felds oer good storage capability, although there are relatively ew in the

    Scottish Renewable Energy Zone. Storage o CO2

    in the oshore Scottish Renewable Energy zone is

    likely to be initially in depleted gas and gas condensate felds and in the ew oil felds where pressure

    conditions are avourable, whilst long-term storage and the majority o storage capacity potential is

    likely to be in saline aquiers.

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    Inverness

    Aberdeen

    GlasgowEdinburgh

    Figure 13

    The location o all 29 hydrocarbon elds and 10 saline aquiers

    identied as potential CO2

    storage sites within the Scottish oshore.

    Risks and uncertainties are associated with all types o subsurace CO2

    storage reservoir, but

    with appropriate, storage site specifc, appraisal it should be possible to reduce these to the level

    appropriate or business investment in and regulatory approval o a project typical o the oil and gas

    industry. It is likely that appraisal costs to reach this position will be higher or saline aquiers than or

    oil and gas felds, although saline aquier capacity or storage is also likely to be correspondingly greater.

    All 29 hydrocarbon felds and ten saline aquiers identifed in this study as having the potential to store

    CO2, either as part o an EOR project or purely as part o a CO

    2mitigation strategy are shown in

    Figure 13. The ten saline aquiers are colour coded according to whether they meet minimum or best

    practice geotechnical requirements (Table 5). They each have a unique size and shape, and the majority

    cover areas o several thousand square km. In some places, the saline aquiers overlap each other, being

    present at dierent depths at the same geographical location. The circles in Figure 13 denote their

    approximate central points.

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    CO2

    storage siteskey conclusions

    Basin-scale assessment has demonstrated

    From this frst assessment, ten saline aquiers have been identifed with a total CO2

    storage

    capacity o between approximately 4,600 and 46,000 Mt, providing a capability to store at least200 years o Scotlands CO

    2output.

    Further study is necessary to ully scope saline aquier storage potential.

    29 hydrocarbon felds (21 oil, 7 gas condensate and one gas feld) oer signifcant urther CO2

    storage potential. Amongst these:

    8 Gas and gas condensate felds oer the best potential or storage;

    Three high pressure high temperature gas condensate felds are unlikely to be used as

    storage sites due to prohibitive costs;

    Oil felds are unlikely to be employed as CO2

    stores except in conjunction with Enhanced

    Oil Recovery;

    The one remaining gas and our remaining gas condensate felds oer total ~ 700 Mt CO2

    storage potential;

    Unusually, the Brent Oil Field oers an opportunity or CO2

    storage o ~ 400 Mt.

    The potential storage capacities as currently assessed are sufcient to provide an approximate

    ranking o sites in terms o their storage potential but sites need to be evaluated individually using

    more detailed models.

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    Figure 14

    Oil elds suitable or CO2-EOR. Blue ovals show extent o detailed EOR study.

    4| CO2 Enhanced Oil Recovery

    The study assessed how enhanced oil recovery (EOR) by CO2

    ooding (CO2-EOR) might either beneft

    rom or be a beneft to CCS. It identifed oil felds within the Scottish Renewable Energy Zone, in

    which CO2-EOR was technically easible, and a more detailed technical and economic assessment o a

    single feld and feld cluster was carried out (an exchange rate o $1.4/ was used).

    CO2-EOR oers potential o economic gain through additional oil production as well as storage o the

    CO2. On average, primary and secondary oil recovery by water ood rom North Sea oilfelds accounts

    or 45% to 55% o oil originally in place, although in some felds it has approached 70%. The residual

    oil is trapped as by-passed droplets in the rock pores or as a flm on the rock grains and may occur

    as localised signifcantly higher saturation areas. EOR processes, employed as a third phase o oil feld

    development, seek to mobilise this oil and move it in a 'bank' towards the production wells. However,

    CO2-EOR is one o a number o competing 'Enhanced Recovery' techniques and to date has not been

    applied in the UK oshore.

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    Field name CO2

    storagecapacity/Mt CO

    2

    Close oProduction date

    Potentialor EOR

    Projected additional oilrecovered

    (million barrels)

    Dunlin Oilfeld 27 2015 Good 83

    Thistle Oilfeld 27 2015 Good 82

    Claymore Oilfeld(Central, Main andNorthern)

    47 2030 Good OK 142

    Cormorant Oilfeld 52 2020 Good 157

    Scott Oilfeld 31 2015 Good 95

    Statjord(UK) Oilfeld

    209 (UK + Norway) 2020 Good 635 (UK + Norway)

    Beryl A Oilfeld 77 2020 Good 232

    Ninian Oilfeld 96 2030 Good 292

    Brent Oilfeld 165 2015 Good 501

    Murchison(UK) Oilfeld

    26 2020 OK 79

    Miller Oilfeld 17 2008 OK 52

    Buzzard Oilfeld 36 2025 OK 108

    Piper Oilfeld 46 2030 OK 140

    Forties Oilfeld 138 2015 OK 420

    Table 7

    Oilelds identied in a desk top review as

    having potential or CO2-EOR.

    The majority o CO2-EOR projects worldwide to date have been implemented onshore in North

    American oilfelds since the 1970 s and it is experience rom these or which most relevant guidelines

    have been drawn up. No projects have yet been undertaken in the North Sea, although the Miller

    oilfeld was recently considered or CO2-EOR. Most existing North American projects have exploited

    natural CO2

    transported over extensive long-distance pipeline networks. Under these circumstances,

    an additional recovery o 5% to 15% o oil originally in place is typically achieved. The technique may not

    be as productive in North Sea oilfelds, because secondary water ood recovery techniques are more

    widely applied, and wells are drilled urther apart than on land.

    A high level desk-top review o all oil felds with an estimated CO2

    storage capacity o >50 Mt was

    carried out to identiy those felds suitable or CO2-EOR. The 14 felds are shown in Figure 14 and

    their details are tabulated in Table 7.

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    Figure 15

    Estimated CO2

    injection and recycle gas injection proles or the Claymore Field.

    To gain a more quantitative eel or the application o CO2-EOR in North Sea oil felds, a technical

    and economic assessment o a single large feld, the Claymore Field, was carried out (highlighted

    in Figure 14). Additionally, a cluster o three large felds, Claymore, Scott and Buzzard (highlighted in

    Figure 14), were assessed as an integrated CO2-EOR project. In all cases CO

    2-EOR was assumed to

    begin in 2017 (although Buzzard will not become available until 2023).

    The oil in Claymore is contained in our separate reservoirs. The total oil initially in place was

    1439 million barrels. For this study two possible scenarios were considered, a less likely scenario (30%

    probability) and a more likely scenario (70% probability) with the ormer yielding an optimistic and the

    latter a pessimistic recovery o additional oil. Starting in 2017, CO2

    would be injected at ~ 3.8 Mt/year

    with produced and recycled CO2eventually negating the capacity to take new CO

    2. Overall, the project

    would store 49.2 Mt CO2and produce between 119 and 163 million barrels o oil (Figure 15; Table 8).

    Capital costs (CAPEX) are derived rom the cost o converting existing acilities and the drilling and

    reurbishment o new and existing wells. Total capital investment is estimated to be around 1.1 to

    1.2 billion. Operating and monitoring costs (OPEX) are estimated to be around 90 million per year.

    Using an oil price o 50 (US$70) per barrel, and assuming that the project neither receives a subsidy

    nor pays or the CO2

    received, the internal rate o return is 12%16% and the net present value

    at a 10% discount rate is 206703 million (lower and upper values correspond to the lower and

    upper values o additional oil recovered). All analysis is beore tax and any beneft rom deerral o

    abandonment o the acilities is not included.

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    70 % probability scenario Gross Net*

    Additional oil (million barrels) 164 119

    CO2

    Injected (million tonnes) 49.2

    CO2 usage (tonne/barrel) 0.41

    Recycle CO2

    (million tonnes) 151.5

    30 % probability scenario Gross Net*

    Additional oil (million barrels) 208 163

    CO2

    Injected (million tonnes) 49.2

    CO2

    usage (tonne/barrel) 0.30

    Recycle CO2

    (million tonnes) 151.5

    70% probability scenario

    Additional oil (million barrels) 71

    CO2

    Injected (million tonnes) 52

    CO2

    usage (tonne/barrel) 0.73

    30% probability scenario

    Additional oil (million barrels) 101

    CO2

    Injected (million tonnes) 52

    CO2 usage (tonne/barrel) 0.51

    Table 8

    Claymore Field - additional oil production and CO2

    usage

    or 70% and 30% probability scenarios.*amount o oil produced rom CO

    2alone without

    contribution rom associated waterfood.

    Table 9

    Scott Field additional oil production and CO2

    usage

    or 70% and 30% probability scenarios.

    Sensitivity (to CAPEX, OPEX, oil price and CO2

    price/subsidy) calculations on the discounted

    cash ow analyses showed that project economics were most sensitive to oil price, then CO2

    price/

    subsidy, then CAPEX, and relatively insensitive to OPEX. Although oil and CO2

    price are subject to

    market orces, this analysis showed that project economics can be improved considerably by refning

    the design and thereby reducing capital costs and risks associated with conversion o acilities and wells

    to CO2

    ooding.

    4.1 Claymore, Scott and Buzzard cluster evaluation

    An analysis o CO2-EOR as an integrated project was carried out using the Claymore, Scott and

    Buzzard felds (highlighted in Figure 14).

    The Scott Field has two oil reservoirs divided by aults into several isolated blocks. The feld is

    signifcantly overpressured. Total oil originally in place was 946 million barrels. Note that the CO2

    use

    is much higher in Scott than or Claymore because o the signifcantly higher pressure in Scott and so

    higher CO2

    density (Table 9).

    Capital costs or the Scott Field are estimated at

    1.2 billion with operating costs, excluding taris, o

    around 45 million per year.

    Buzzard is located in the Outer Moray Firth. Fluids

    are contained by a combination o structural and

    stratigraphical trapping. Total oil originally in place

    was 1077 million barrels, taken rom published

    inormation. Forecasts have been downgraded by

    40% in the economic analysis over concerns that the

    CO2

    may not mix with the oil in a way benefcial to

    the EOR process (Table 10).

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    70 % probability scenario Gross Net*

    Additional oil (million barrels) 85 79

    CO2

    Injected (million tonnes) 46

    CO2 usage (tonne/barrel) 0.48

    30 % probability scenario Gross Net*

    Additional oil (million barrels) 117 111

    CO2

    Injected (million tonnes) 46

    CO2

    usage (tonne/barrel) 0.41

    Table 10

    Buzzard Field additional oil production and CO2

    usage

    or 70% and 30% probability scenarios.* amount o oil produced rom CO

    2alone without

    contribution rom associated waterfood.

    The presence o acilities or dealing with hydrogen sulphide or sour gas is likely to reduce the cost

    o adapting Buzzard to CO2

    injection so, or the purposes o this analysis the capital cost o conversion,

    is estimated at 700 million. The operating costs or Buzzard, excluding taris, are estimated at55 million per year.

    Aggregated results or this cluster o large felds give an additional oil recovery o 237331 million

    barrels or around 155 Mt o CO2

    stored. The aggregated capital cost o the cluster redevelopment

    would be around 3.1 billion with total operating costs over the project lietime o 2.6 billion.

    Using a 50 (US$70) per barrel oil price, and assuming that the project neither receives a subsidy nor

    pays or the CO2

    received, the internal rate o return is 13%18% and the net present value at a 10%

    discount rate is 4091717 million.

    The economics o exploiting CO2-EOR in the northern North Sea have been examined in somedetail. The combination o high capital requirements, high operating expense and relatively limited

    amounts o remaining oil gives rise to considerable sensitivity to both oil prices and the cost o CO2

    used or injection. CO2-EOR may act as a stimulus or CCS especially i developers come to expect that

    the price o oil will remain over US$100 per barrel or the period o their investment. Higher oil prices

    would make CO2-EOR projects more commercially viable and with that, the independent development

    o CCS. To date, the closest CCS has come to being realised in the UK is through a proposed CO2-

    EOR project (Miller Field) but the project was ahead o the political process and the feld had to

    move to decommissioning beore a government decision on policy support . However, development o

    CCS could lead to the application o EOR, since this reduces costs and uncertainties related to CO2

    supply.

    Power stations will produce a airly constant supply o CO2

    over many years. This study examined the

    CO2

    supply required or Enhanced Oil Recovery projects or a cluster o three large oil felds. Taking

    the three felds together, the supply o CO2

    required was substantial, approximately 11Mt/year or

    13 years, and comparable to the output rom a power station source.

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    CO2-enhanced oil recoverykey conclusions

    Ignoring risk premiums, and i the CO2

    is not a cost to the project, CO2-EOR may be economic in

    North Sea oil felds at an oil price o US $70 per barrel.

    I CO2 is a cost to projects in the 2040 ($28$56) per tonne range, an oil price o US $80$110 per barrel will be required to break even.

    I a subsidy is available or the CO2

    stored then the project could be economic at an oil price

    signifcantly lower than US $70 per barrel.

    Taking risks into account, it is unlikely that CO2-EOR will be commercially viable in North Sea

    felds at an oil price less than US $100 per barrel.

    The redevelopment o a mature North Sea feld or CO2-EOR is a major undertaking equivalent in

    complexity, scale and cost to the original development; each project will need to be the subject o

    detailed engineering design and economic appraisal including a ull assessment o the risks.

    CO2-EOR has never been applied oshore so early projects will carry signifcant additional

    fnancial risks.

    The total CO2

    storage capacity o all felds to which CO2-EOR might be applied is ~1000 Mt.

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    5| CO2

    injection modellingwithin saline aquifers

    In order to better understand how the available storage volume within a saline aquier might be

    aected by injection o large amounts o CO2

    the Tay Sandstone saline aquier (Figure 13) was selected

    or urther study. Key issues governing whether large volumes o CO2

    can be saely, reliably and

    securely injected into and stored within a saline aquier were investigated by modelling the injection

    o CO2. The main areas o investigation were the potential o the saline aquier to store the specifed

    volumes o CO2, the injectivity (including the number o wells required), the eect o orientation and

    location o wells, and the migration path o CO2

    away rom the injection points. Sensitivity to injection

    rate, the number o wells, length, and spacing and location o wells were investigated. Two CO2

    injection scenarios were investigated addressing sources rom Scotland and imported CO2:

    a baseline case o 15 Mt/year

    a high-use case at 60 Mt/year.

    5.1 Storage capacity o the Tay saline aquier

    Numerical modelling o the amount o CO2

    that can be stored in the Tay saline aquier gives a wide

    range o possibilities according to whether the saline aquier is considered open or closed. It is not

    yet clear which is the case. For this study, the Tay saline aquier was modelled or both scenarios.

    Tay saline aquier open (water naturally migrates out o the saline aquier) at an injection rate o

    15 Mt/year or 25 years, the saline aquier can readily store 375 Mt CO2.

    Tay saline aquier closed (water does not migrate out o the saline aquier) the saline aquier

    can store 375 Mt CO2

    provided water is produced at a rate o 40, 00060, 000 m3/day.

    Without water production it can store only 155 Mt CO2

    (0.4% o total pore volume) because o the

    increase in pressure as the CO2

    is injected.

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    5.2 Investigation o sensitivities in modelling the saline aquier

    Although the total volume o CO2

    injected at 15 Mt/year or 25 years injection is less than 1% o the

    total volume o water in the Tay ormation, the average reservoir pressure increased 50% by the

    end o the injection period. The pressure then reduced gradually as the CO2

    dissolved in water.

    The injectivity o the Tay saline aquier is very good, based on the reservoir properties collected

    rom current oil felds.

    Injection pressure varies with the porosity, permeability and the amount o reservoir rock.

    To reduce pressure at the injector well, additional injectors are recommended or the 15Mt/year plan. The injection rate or one well should be less than 6 Mt/year.

    Unless it is open, injection o 60 Mt/year CO2

    over 25 years into the Tay saline aquier is likely to

    lead to excessive pressure.

    The movement o CO2

    within the saline aquier can be controlled by appropriate location o

    injector wells.

    Injected CO2

    tends to move higher within the reservoir, but when it dissolves in water it tends to

    move downwards.

    I producing hydrocarbon felds are connected to the saline aquier, and CO2

    is injected into their

    vicinity, the CO2

    tends to move towards them, as they may be at a lower pressure than the saline

    aquier, and are usually higher on the structure.

    The presence o a relatively impermeable layer within the saline aquier did not act as a signifcant

    barrier to the lateral movement o CO2.

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    Tier Sourcecategory

    Source size (TonnesCO

    2/year)

    Examples

    0 Large > 1 million Coal fred power station, hydrocarbon refnery, major chemicalworks

    1 Medium 50,000 to 1 millionChemicals, glass, ood manuacturers, large Combined Heat & Power(CHP) & Combined Cycle Gas Turbines (CCGTs)

    2 Small 1,000 to 50,000 CHP units, incinerators, small to medium industrial works

    Table 11

    Source categories dened as Tiers with examples.

    6| CO2

    transport options betweensources and storage sites

    Successul implementation o CCS in Scotland will require a suitable transport network or CO2.

    This study examined options or transporting CO2

    between the sources and storage sites identifed.

    Various onshore and oshore routes and technologies were examined. The latest UK and international

    codes and standards applicable to CO2

    pipelines were used.

    Sources were categorised according to their output per year (Table 11). The tiers provide some

    indication o the potential or applying a CCS solution at each level and are linked to emission

    allowances allocated under the European Union Emissions Trading Scheme. Large (Tier 0) sourcesare recognised as the primary ocus or any CCS scheme as the cost o allowances under European

    Union Emissions Trading Scheme should make it more economical to store the carbon than to pay

    or or trade any excess over the emission allowance. The CO2

    transportation network will be built

    around these centres. Medium (Tier 1) sources may be less economically suited to a CCS solution.

    Their location is likely to determine whether they are included in the network. For instance, oshore

    installations (Medium (Tier 1) sources that produce in total 23.7 Mt/year o CO2) are not included in

    the example network discussed below. It is unlikely to prove either practical or economic to include

    most small (Tier 2) sources in a CCS scheme.

    All large Scottish sources are located along the Firth o Forth except the gas-fred power station atPeterhead. Several medium sized (Tier 1) clusters could easibly be associated with the large sources.

    For example, St Fergus Gas Terminal naturally links to the large Peterhead source and plants at Stirling

    and Mossmorran to the large Longannet power station (Figure 4). Future projects, such as replacement

    o power generation at the Hunterston Nuclear site, were not added to CO2

    volumes but network

    access was modelled, and replacement o existing plant was included.

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    6.1 Network design

    A well-developed oil and gas pipeline transport inrastructure is present throughout the onshore

    UK and the oshore UK Continental Shel. Parts o this inrastructure may become available or re-

    use and potentially could be used to transport CO2. For example, a previous proposal demonstrated

    that the pipeline rom the vicinity o Peterhead to the Miller feld is technically capable o carrying

    a substantial volume o CO2. It could well orm a key element in any uture oshore CO

    2pipeline

    network and the potential or its use in this context should be examined in detail as a priority.

    However, re-use o onshore and oshore pipelines raises major issues related to change o use in areas

    o planning, capacity and saety, in addition to various technical questions. Assessing the possibility o

    re-using each pipeline or CO2

    transport would require a line by line analysis and is beyond the scope

    o this study. However, in broad terms, and dependant upon pipelines becoming available, oshore

    pipelines are more likely to be suitable or re-use, whereas onshore, the potential or re-use will be

    more restricted. Importantly, sections o the onshore National Transmission System (NTS) could

    be used as part o a start up or phased approach while gas ow is low. Thus, taken together, use

    o existing onshore and oshore pipelines may be viable or the small volumes (~3Mt/year) o CO2

    required or a demonstration project.

    The design o a network or Scotlands CCS system thereore reects the location o the key large

    (Tier 0) emitters, all but one clustered around the Firth o Forth, and the various CO2

    storage options

    in the Scottish defned oshore area. These groupings and the distances between them naturally

    suggest an approach consisting osource hubs connected by a transport spine to storage hubs. The

    presence o a hub near several storage sites allows a variety o storage technologies (saline aquier,

    depleted hydrocarbon feld or CO2-EOR) to be pursued as opportunities permit, thereby lowering risk.

    Four storage hub locations were chosen to permit examination o relative transport costs between

    various areas and the eect o various assumptions about the re-use o existing inrastructure.

    The storage hubs are named ater local oil felds (Captain, Dunbar, Brae and Gannet; Figure 16) and are

    not necessarily optimal.

    6.2 Transport options

    The viability o transport by pipeline and ship were both assessed. Pipeline design is a complex issue

    with many actors aecting the building o this inrastructure. A CO2

    pipeline system must be able to

    accommodate the ull range o conditions rom ast ramp up rates and shut-downs o power stations

    and the closure o geological storage sites. It must accommodate varying ows, surges and variations in

    composition o the CO2

    uid itsel. Key issues unique to CCS are:

    chemical and physical properties o the CO2 including any impurities within the CO2 stream;

    consideration o pressures, to maintain the CO2

    in the required phase throughout the network

    without exceeding sae levels at other points;

    legislation specifc to CO2

    including UK Health and Saety requirements and international codes o

    practice.

    A pipeline operating pressure above 100 bar is desirable with a minimum pressure o 90 bar in order

    to prevent phase change within the pipe. This maintains the CO2

    well above its critical point pressure o

    73.9 bar. This pressure margin also allows or a degree o contamination o the CO2 stream.

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    Network Option

    1Peterhead to Forth (Longannet) onshore pipeline

    2Forth to Peterhead onshore pipeline

    3Forth (Longannet) with oshore pipeline route to Peterhead

    4Full network

    5Shipping rom Forth to Peterhead hub

    6Tyne/Tees direct to oshore storage hubs

    Table 12

    Summary o possible transport options

    identied through consideration o the

    locations o CO2

    sources and potential

    storage sites.

    Although elements within the National Transmission System onshore pipeline system may be available

    and suitable or use within a CO2

    pipeline network, this possibility was not considered within the

    economic assessment discussed below.

    In terms o the technical and economic viability otransporting CO2

    by ship, this study ocussed on

    transport o captured CO2

    rom a location in the Firth o Forth to the Peterhead area (Figure 16). The

    assessment was limited to vessel access, berthing and ship support services only. No account was taken

    o any specialist storage tanks, pressure and cooling systems necessary or loading and discharge o the

    CO2. Note that, to minimise disruption to the capture process, storage tanks should be sufcient to

    allow 50% redundancy over and above the ships cargo capacity.

    The model or costs o transport by ship assumes newly designed vessels o 18,000 m3 capacity, total

    cargo pumping rate o 1,500 m3/hr, no waiting on tides, and that discharge occurs in Peterhead Harbour

    (although discharge at an oshore location would considerably reduce overall harbour costs). A eet

    o our vessels would allow in excess o 13.5 Mt o CO2

    to be transported per year. Transportation

    cost would be in region o 4.57 per tonne. The capital cost or the vessels, whether new build or

    converted, has not been included in the cost model. In the fnal analysis, fve possible transport options,

    each with the same oshore storage hubs, were identifed and costed. Options or transporting CO2

    rom the Tees/Tyne area were also assessed (Table 12).

    Assessment o transport options

    Assessment o the fve pipeline and shipping options or transportation o CO2 shows that they arewithin the scope o costs or a major inrastructure project.

    The option using ship transport, a oating pipeline, is easible and may be comparable to pipeline

    options in terms o capital cost, but with up to our times higher operating expense.

    A more detailed examination would be required to accurately dierentiate between the onshore and

    oshore routes rom the Forth to Peterhead (options 2 and 3).

    This appraisal does not consider a phasing o the construction o the network but assumes a

    relatively quick build-up to ull capacity due to the small number o large sources.

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    Figure 16

    Summary o proposed CO2

    transportation routes.

    The implications oimporting CO2

    rom areas outside Scotland were investigated by examining the

    route rom the TeesTyne area to storage sites oshore Scotland (Option 6). Linking directly into a

    pre-existing network within Scotland would be costly in terms o both capital and operating costs, not

    least because pipelines are complex systems. This study suggests that multiple eeder pipelines rom

    the onshore clusters to the oshore storage sites is likely to oer a more cost-eective solution with

    CAPEX ranging rom 1.4 to 2.3 billion and OPEX ranging between 27.5 to 53.5 million dependingon storage hub destination. Whilst this introduces complexity into storage management, it allows or

    much more exibility in phasing construction and operations.

    Figures 17 & 18 show the costs o the various options. Option 2 (onshore pipeline) orms the lowest

    cost option in terms o capital expense (CAPEX) or all oshore hubs and the lowest cost option in

    terms o operating expense (OPEX) or all except the Gannet hub where Option 3 (oshore pipeline)

    is slightly less. Captain is the lowest cost target or Option 2. The overall costs o Options 2 and 3 are

    comparable. Option 3 is slightly more expensive, but constitutes a viable alternative to an extensive

    onshore pipeline. Option 1 (principal pipeline rom the Forth to the oshore hubs) and Option 4 (ull

    network) are more costly than either Option 2 or Option 3. The capital costs o shipping Option 5,are comparable with those o the other options, but the high operating costs and risks suggest that it is

    unlikely to prove a viable long term solution.

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    Figure 18

    Operational expenditure or the ve CCS network options

    investigated or each oshore hub (in Million per year).

    Figure 17

    Capital expenditure or the ve CCS network options investigated

    or each oshore hub (in Billion).

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    CO2

    transport options between sources and storage sites key conclusions

    Five network options, linking CO2

    source and storage hubs have been identifed and a technical

    and economic assessment undertaken.

    A sixth option, importing CO2 rom NE England was also investigated. Here, multiple eederpipelines to oshore hubs are likely to orm a more appropriate means o accepting additional

    CO2

    rom NE England rather than attempting the technically complex option o connecting

    directly into a pipeline network within Scotland.

    Some re-use o acilities is possible, especially in the early stages o CCS projects.

    The potential or using the Peterhead to Miller pipeline and the National Transmission System

    inrastructure as a key element o a Scottish CO2

    pipeline network should be examined in detail.

    A pipeline network used to transport 20 million tonnes/year o CO2

    rom sources to the storage

    hub at CAPEX costs o 0.7 to 1.67 billion and OPEX costs o 38 to 74 million dependingon hub location and excluding the shipping option. OPEX or shipping ranges rom 148 to 171

    million depending on hub location.

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    No. DriverSource

    Non-CCSTechnology

    CCS Technology StorageHub

    Primary transport required

    1 Longannet2.4 GW

    supercritical coal

    2.4 GW supercriticalcoal with postcombustion capture

    Brae

    Forth hub (vicinity oLongannet) to Brae withalternatives o new and existing(Miller) pipeline

    2 Longannet2.4 GW

    supercritical coal

    2.4 GW supercriticalcoal with postcombustion capture

    GannetForth hub to Gannet with newpipeline

    3 Peterhead 1.2 GW CCGT*1.2 GW CCGT withpost combustioncapture

    BraeN.E Scotland hub (vicinity oPeterhead and St Fergus) toBrae via existing Miller pipeline

    4 Longannet2.4 GW

    supercritical coal

    2.4 GW supercriticalcoal with postcombustion capture

    Gannet

    Import o CO2

    rom N.E.England hub (vicinity o Blythe/Lynemouth) connected intoScottish Network using newpipelines

    5 Peterhead 1.2 GW CCGT*1.2 GW CCGT withpost combustioncapture

    CaptainN.E Scotland hub to Captainusing new pipeline

    CCGT

    *

    , Combined Cycle Gas TurbineGW, Gigawatt

    Table 13

    CCS schemes selected or economic analysis.

    7| Economic modelling of potentialCCS schemes in Scotland

    Economic modelling o possible CCS projects in Scotland was carried out to compare costs

    with conventional non-CCS power stations. The CCS schemes were compared to each other and

    the 'without CCS' alternatives to estimate the level o subsidy that would be required to make CCS

    projects economic.

    Five sample schemes were selected or study as shown in Table 13. They are based on key CO2

    sources

    rom the power stations at Longannet and Peterhead combined with network and storage options

    selected rom the options presented earlier in this study.

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    Schemeno.

    Scheme Abatement cost(/t CO

    2)

    Required subsidy( M/year)

    Required subsidy(/t CO

    2

    captured)

    Electricity cost(/M Wh)

    2Longannetsupercritical coal toGannet hub

    37 98 7 65

    1Longannetsupercritical coal toBrae hub

    39 117 9 66

    4

    Longannetsupercritical coalto Gannet hub withimported CO

    2

    40 132 10 67

    5

    Peterhead CCGT to

    Captain hub withoutull network 64 93 30 65

    3Peterhead CCGT toBrae hub

    70 111 36 67

    Table 14

    Source to storage schemes ranked by cost o abatement (in /t CO2).

    Table 14 shows these schemes ranked by cost o abatement (in /t CO2). Each project was compared

    with its non-CCS alternative, shown in Table 13, to calculate the subsidy (in terms o /t CO2

    captured)

    required to give returns similar to those o the non-CCS alternative. On a lietime annual basis required

    subsidies range between 93 M per year or Scheme 5 to 132 M or Scheme 4. The required subsidy (in

    /t CO2

    ) is roughly equal to the abatement cost minus the assumed market price o CO2

    in 2020.

    The cost over the lietime o the energy generating system (levelised cost) o Scheme 3 and Scheme

    2 was compared to that o conventional coal- and gas-fred generation (Figure 19). Calculations o the

    required subsidy assumes a rate o return o between 9% to 11%. This shows that despite the di erence

    in abatement cost, gas-and coal-fred CCS schemes have very similar levelised costs (Figure 19 and Table13). However, although the amount o fnancial support or gas-fred CCS projects is similar to that

    required to support coal-fred CCS, the tonnage o CO2

    abated is much higher in a coal scheme.

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    Figure 19

    Breakdown o levelised costs in 2020.

    Figure 20

    Comparison o the impact o sensitivities on

    power generation by CCS Coal and CCS Gas.

    Sensitivities on the assumptions The high degree o uncertainty in elements o cost and the

    perormance o CCS plant in the economic modelling exercise ows through to the estimates o the

    cost o electricity generation o CCS Coal and CCS Gas schemes in quite a dierent way (Figure 20).

    For example, actors which have a strong impact on the power station element o the levelised costs

    o the schemes such as a reduced load actor (50% instead o 85%), higher discount rates and a higher

    CAPEX will have a disproportionate eect on the economics o CCS Coal because o the greater weight

    o the power station costs in CCS Coal. Conversely, assumptions that have a strong impact on uel costs

    such as sensitivities to commodity prices will have a stronger eect on the economics o CCS Gas.

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    Impact o CO2-EOR on results CO

    2-EOR may have the ability to lower the overall subsidy

    required and provide an additional incentive or development o CCS. It may add value to Scotlands

    hydrocarbon reserves by prolonging the lie o oil felds, delaying their closure and postpone

    decommissioning costs.

    Modelling o CCS Schemes key conclusions

    The underlying economics o energy projects drive power industry development.

    The levelised costs (in /M Wh) o CCS Gas and CCS Coal are similar.

    CCS schemes are likely to be signifcantly more expensive than standard conventional Combined

    Cycle Gas Turbine and pulverised coal plant.

    Uncertainty in the costs and perormances o CCS schemes can considerably aect assessment o

    the relative merits o coal- and gas-fred schemes.

    High or low uture commodity prices will determine whether costs or CCS will be competitive

    with non CCS power generation.

    Although the costs o CCS schemes are similar, CCS coal-fred power generation abates more

    CO2

    than CCS gas.

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    Business Risks

    RevenuesTechnical and

    OperationCosts

    Financing CapexSite

    Availability

    Flexible

    running

    System

    Integration

    Operational

    Perormance

    Skill

    Shortages

    Electricity

    Spark

    Spreads

    EU ETS*

    Funding

    PolicyOil Price Opex

    Figure 21

    The key areas o business risk.

    8| Business risks facedby early CCS projects

    The principal fnancial risks associated with anticipated revenue, costs and technical/operational aspects

    o CCS projects were identifed to inorm the discussion o business models or early CCS projects.

    Early CCS projects are likely to consist o dedicated transport and storage acilities matched with

    each source. This study concentrated on the risks associated with projects o this nature. A more

    mature CCS industry may well consist o multiple projects with a shared inrastructure many capture

    projects eeding into a CO2

    pipeline network which is then linked to a multitude o storage sites.

    The confguration o these early projects means they are likely to ace additional business risks. Three

    key areas o business risk and their mitigation were investigated: Revenue stream risks, Cost risks and

    Technical and Operational risk (Figure 21).

    *EU ETS is European Union

    Emissions Trading Scheme

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    Revenue streams the power station will be the principal source o income to any CCS project

    selling low-carbon electricity to the market. Uncertainty over gas, coal and carbon prices in the long

    term brings with it uncertainty regarding the gross margin or power generators. Furthermore, the

    UK electricity generation mix is likely to evolve in the years to 2020 both as a result o policy and in

    response to commodity prices; more nuclear and renewables capacity could result in lower usage levels

    o CCS plants and thereore lower overall revenues.

    Costs Capital costs (CAPEX) orm the single largest source o cost uncertainty and are likely to

    dominate the character o overall schemes. The technologies o pipeline systems and storage sites are

    better known than those o other elements, so their capital costs are more certain. However, these

    orm a large proportion o the total capital requirement so any overrun will have a disproportionate

    impact on overall project returns. Uncertainty in the thermal efciency o CCS plants will give rise to

    signifcant elements o risk in the operational cost (OPEX), through uel costs. The relative novelty o

    CCS technology and the risks associated with it suggest that the costs o fnancing early projects will be

    higher than those o more mature technologies.

    Technical and Operational risks There will be signifcant cost savings rom learning eects.

    Technical and operational efciency will also improve with experience. The two areas most likely to

    achieve signifcant improvement are the power plant (which currently accounts or approximately two

    thirds o lietime costs in each CCS scheme) and storage sites. Pipelines are much more o a known

    quantity, and levels o operational risk can be well estimated in advance. Some additional fnancial risk

    may be associated with the construction o early CCS power plants, where delays are more likely than

    or conventional stations because o the complexity o the projects.

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    *

    * Short run marginal cost

    Figure 22

    Mitigation o risks in a CCS scheme.

    Figure 23

    Summary o the three

    business models

    examined in this study.

    9| Business mo