introduction to geologic co2 storage and the illinois basin

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  • 7/31/2019 Introduction to Geologic CO2 Storage and the Illinois Basin

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    Robert J. FinleyMidwest Geological Sequestration Consortium

    Illinois State Geological Survey

    University of Illinois, USA

    RECS-2012

    Birmingham, Alabama

    6 June 2012

    A 1-Million Tonne Demonstration of Carbon

    Sequestration from a Biofuel Source:

    The Illinois Basin - Decatur Project (IBDP)

    Introduction to Geologic Storage

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    The Midwest Geological Sequestration Consortium is funded by the U.S. Department ofEnergy through the National Energy Technology Laboratory (NETL) via the Regional CarbonSequestration Partnership Program (contract number DE-FC26-05NT42588) and by a cost

    share agreement with the Illinois Department of Commerce and Economic Opportunity,Office of Coal Development through the Illinois Clean Coal Institute.

    The Midwest Geological Sequestration Consortium (MGSC) is a collaboration led by thegeological surveys of Illinois, Indiana, and Kentucky

    Landmark Graphics software via University Donation Program and cost share plus Petrelsoftware via Schlumberger Carbon Services

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    Capture CO2 at asource

    Compress it and putit in a pipeline

    Put it into a sink,or subsurface

    storage site

    Source

    Sink

    Pipeline

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    Reservoir

    Seal

    Shale Seal

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    So what is successfulstorage?No CO2 leaks to endanger man or the environment around the storage site, no migration of CO 2

    where not expected, and no leaks of other subsurface fluids

    Storage requires capacity, injectivity, and containmentwhich are based on characteristics ofthe geologic framework into which the CO2 is injected for storage

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    Sand grain

    Pore space

    CO2 Storage in Sandstone Reservoir Pore Space

    Pin head

    The porosity of a reservoir providesthe storage space while the

    permeability allows fluid flow to beinjected into the reservoirpores.

    Capacity and Injectivity

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    Containing CO2 in the reservoir is a function of a seal or caprock above thereservoir that has low permeability (and typically low porosity, as well) such as ashale, low-permeability siltstone or limestone, or a bedded salt

    Fractures in a rock mayprovide CO2 migration pathways, as mayfaults, surfacesacross which rocks are offset, or broken

    The orientation of faults and/orfractures can often be predicted

    from the geologic history of a region

    Normal fault

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    Pin headNo pore space visible

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    The act of characterizingTo describe the qualities or peculiarities of--- Websters Dictionary

    The CO2 can be captured from the sourceThe CO2 can be delivered to the siteSite geology is suitable to meet criteria of capacity, injectivity, and containmentPublic engagement and acceptance can be gained to enable the projectPermit requirements can be successfully met

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    Staff with diverse expertise necessaryOrganizational focus to define key components:Requires a reservoir-seal system

    Requires a site to access the systemMust meet a regulatory frameworkMust identify the source of CO2 (volume, quality)

    Integrated teams must be developed

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    GeologyReservoir engineeringHydrologyGeochemistryGeophysicsPermittingCommunications and outreachPetrophysicsRisk assessment

    Drilling and well completionChemical engineeringMechanical engineeringSurveying and photogrammetryGeographic Information Systems

    (GIS)

    Project management, operations, andbusiness

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    A collaboration of the Midwest GeologicalSequestration Consortium, the ArcherDaniels Midland Company (ADM),Schlumberger Carbon Services, and othersubcontractors to inject 1 million metrictons of anthropogenic carbon dioxide at adepth of 7,000 +/- ft (2,000 +/- m) totest geological carbon sequestration in asaline reservoirat a site in Decatur,Illinois

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    IBDP fully operational 24/7IBDP is the first 1 million tonne

    carbon capture and storage project

    from a biofuel facility in the US

    Injection through fall 2014Intensive post-injection monitoring

    under MGSC through fall 2017

    Cumulative Injection (6/1/12):169,148 tonnes

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    IBDP is the first demonstration-scale (1 million tonne) US project to use carbon dioxide (CO 2)from an industrial source within the DOE Regional Carbon Sequestration Partnership (RCSP)program

    IBDP is a fully integrated demonstration, from a compression- dehydration facility and a shortpipeline to delivery of supercritical CO2 to a three-well injection and observation system on anintensely monitored site

    IBDP is the product of four years of effort, from date of funding to CO2 in the reservoir,including site characterization, permitting, 5,424 m (17,900 ft) of drilling, reservoir geology,engineering, and geophysics, risk assessment, outreach, and baseline monitoring

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    Mt. Simon Sandstone

    Eau Claire Shale

    Illinois Basin

    Stratigraphic

    Column

    Maquoketa Shale

    New Albany Shale

    Mississippian sandstone and carbonate oil reservoirs

    St. Peter Sandstone

    Pennsylvanian coal seams

    reservoir

    seal

    back-up seals

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    Nemec, 1992

    Project Description: Geology

    Brahmaputra River System

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    MGSC Injection and geophone wells

    MGSC monitoring well

    0.5 mile

    photo by Illinois Dept. of Transportation, 8 November 2010

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    A

    B

    C

    D

    n A Dehydration/compression facilitylocation

    n B Pipeline route (1.9 km)n C Injection well siten D Verification/ monitoring

    well site

    n E Geophone well

    800 m

    A

    B

    C

    D

    A

    B

    C

    D

    E

    800 m

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    Soil flux

    Groundwater

    Eddy Covariance

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    Verification well rig on site

    Injection well

    Twenty-one artificial reflectors

    installed in updip plume direction

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    Top of

    CO2

    InjectionPerforations

    RST*Log

    7,000

    6,900

    6,800

    7,100

    Logged March 1, 2012 with ~75,000 tonnes

    metric tons injected from Schlumberger Carbon Services

    *Reservoir Saturation Tool

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    Injection Well

    Geophone in special carrier

    strapped to 3.5 inch (8.9 cm)

    tubing

    3,500 ft (1,060m) well with 31

    geophonescemented intouncased holeon tubing string

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    23

    Baseline 2 Image Monitor 1 Image Difference Image

    Shown above in the left two panels is a west-east image section Rightmost panel is the difference of the two The input to migration is the processed and cross-equalized, notch

    filtered upgoing data

    2000

    3000

    4000

    5000

    6000

    7000

    Offset (ft)-1000 -500 500 10000

    Depth(

    ft)

    2000

    3000

    4000

    5000

    6000

    7000

    -1000 -500 500 10000 -1000 -500 500 10000

    from Schlumberger Carbon Services

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    24

    VSP well

    Injection well

    Verification well

    NRMS computed between5000-5500 ft (1524-1677 m) depth

    NRMS computed between6950-7100 ft (2119-2165 m) depth

    -200

    0

    200

    400

    600

    800

    0-400 400-800 800

    -200

    0

    200

    400

    600

    800

    0-400 400-800 800

    NRMS0

    14

    27

    41

    55

    69

    82

    96

    110

    0

    14

    27

    41

    55

    69

    82

    96

    110

    NRMS

    Preliminary Analysis

    from Schlumberger Carbon Services

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    P port

    samplingport

    Nine Sampling Levels In theMount Simon Sandstone

    Two Sampling LevelsAbove the Eau Claire Shale

    Two Fluid Sample SetsCollected Preinjection

    *Mark of Schlumberger

    November 2010

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    June-August 2011

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    Constituent Shallow

    Groundwater

    Ironton-

    Galesville

    Mt. Simon

    (injection

    formation)

    Conductivity (mS/cm) 1.5 80 170

    TDS (mg/L) 1,000 65,600 190,000

    Cl- (mg/L) 170 36,900 120,000

    Br- (mg/L) 1 180 680

    Alkalinity (mg/L) 380 130 80

    Na+ (mg/L) 140 17,200 50,000

    Ca2+ (mg/L) 100 5,200 19,000

    K+ (mg/L) 1 520 1,700

    Mg2+ (mg/L) 50 950 1,800

    pH (units) 7.2 6.9 5.9

    Shallow groundwater(16 well average)

    Ironton-Galesville(2 zone average; swabonly)

    Mt. Simon(9 zone average)

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    CO2 in Annulus

    Westbay Zones

    CO2 in Reservoir

    Non-CO2 FluidMovement

    from Schlumberger Carbon Services

    3

    2

    Westbay Zones 2 and 3equivalent to lower and upperperforations, respectively

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    1.21 MPa (175 psi) increase

    at level of perforations

    100 m above perforations

    33 m above perforations

    0

    50,000

    100,000

    150,000

    200,000

    250,000

    300,000

    350,000

    400,000

    450,000

    500,000

    2900

    2950

    3000

    3050

    3100

    3150

    3200

    3250

    3300

    3350

    3400

    MetricTonnes

    Pressure,psi

    IllinoisBasinDecaturProject

    PressuredataasobservedinVerificationWell#1(VW1)

    VW1is1000ftfromInjectionWellCCS#1

    Perf_Z2_Pressure

    Perf_Z3_Pressure

    Perf_Z4_Pressure

    Perf_Z5_Pressure

    Perf_Z6_Pressure

    CumulativeInjection(tons)

    Plottedpressure dataisbasedonaveragesforeachday.

    1.21 MPa (175 psi) increaseat level of perforations

    33 m above perforations

    100 m above perforationsfrom Schlumberger CarbonServices multilevelgroundwatercharacterization andmonitoring system

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    Injection Well

    Verification

    Well

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    Precambrian High

    Valley eroded into Precambrian

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    InjectionWell

    VerificationWell

    Mount Simon SandstoneDeposition on Pre-existingTopography(4.3 m [14 ft] depth steps)

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    35

    Two of the 4-Component geophonesare within the Mt. Simon, the third ispositioned above the caprock

    (Eau Claire Shale).

    Ground Level

    24 levels of the 3-Component geophonesare collecting microseismic data.Active Levels are 8 to 31.

    Inactive, are levels 1 to 7, not shown.

    TD= 7236 feet MDGranite Wash

    (Base of the Mt. Simon)

    Top of the Mt. SimonSandstone

    St. PeterSandstone

    GeophysicalWell #1

    With OYO 3Cgeophones

    VerificationWell #1

    ADM CCS #1 (Injectionwell)

    With PS3 OYO 4C

    geophones

    Perforation Zone Within the Mt.Simon

    2

    3

    1

    3130

    29

    8

    ~ 675 ft msl

    From Schlumberger Carbon Services

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    1Schlumberger PS3 System

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    Min -3.85

    Max -1.73Diff 2.12

    Avg. -3.213465784

    STD 0.348842139

    ft

    from Schlumberger Carbon

    Services

    23

    1

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    Injection Well with Sensorsfrom Schlumberger Carbon Services

    Preliminary Analysis

    1

    3 2

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    courtesy Schlumberger Carbon Services

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    Reservoir Model: Eclipse 2011.2 20 20 mile coverage ~ 3M Cells, 143 143 148 Cell Horizontal Dimensions are from

    5 ft and 50 ft at wells to 1500 ft atthe model boundaries

    Cell Vertical Dimensions from 3 ft to30 ft

    Infinite acting boundary conditions

    Reservoir Model Static Modelfrom Schlumberger Carbon Services

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    March 2012

    from Schlumberger Carbon Services

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    2013

    from Schlumberger Carbon Services

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    2014

    from Schlumberger Carbon Services

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    IBDP

    IBDP

    IL-ICCS

    IL-ICCS

    Injection

    Verification

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    (IL ICCS) Project will Prove CCS at Scale Commercial scale operations of one million metric tons

    per year will be achieved

    Will build on the leading-edge technology of the IllinoisBasin - Decatur Project by expanding injected volumes

    Will add an education and training component throughRichland Community College, National SequestrationEducation Center

    IBDP and IL ICCS will be a first in the world to assess twoinjected carbon dioxide plumes in the same reservoirthat resemble volumes derived from a commercial coal-

    fired power plant

    20192017

    IBDP

    IL-ICCS

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    MIDWEST CARBON

    SEQUESTRATION

    2012

    SCIENCECONFERENCEThe Midwest Geological SequestrationConsortium (MGSC), one of the USDepartment of Energy RegionalCarbon SequestrationPartnerships, the SequestrationTraining and EducationProgram (STEP), andSchlumberger CarbonServices are hosting aknowledge sharingevent at the IllinoisBasin-DecaturProject (IBDP).

    This 2day event features:

    A full day of presentations on the IBDP1-million tonne saline reservoir injectiondemonstration, including geology,geophysics, environmentalmonitoring, outreach/education, andcompression/infrastructure. A visit to the

    Project site at the Archer Daniels MidlandCompany in Decatur, Illinois will be offered.

    A STEP developed educational opportunitywill be available to all attending.

    Networking opportunities including anopening mixer, conference reception anddinner, and meeting lunches.

    September 17 19 2012Champaign, IL USA

    SAVE THE DATE!

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    Midwest GeologicalSequestration Consortium

    [email protected]

    Photo credits: Daniel Byers