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7/26/2019 SECARB Integrated CCS Project
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JohnRyan MacGregorAdvanced Resources International, Inc.
RECS 2016
June 15, 2016
The SECARB Anthropogenic Test:A fully integrated CCS Pilot Project
Citronelle, Alabama
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AcknowledgementThis presentation is based upon work supported by the Department of Energy National Energy
Technology Laboratory under DE-FC26-05NT42590 and was prepared as an account of work
sponsored by an agency of the United States Government. Neither the United States
Government nor any agency thereof, nor any of their employees, makes any warranty, express or
implied, or assumes any legal liability or responsibility for the accuracy, completeness, or
usefulness of any information, apparatus, product, or process disclosed, or represents that its use
would not infringe privately owned rights. Reference herein to any specific commercial product,process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily
constitute or imply its endorsement, recommendation, or favoring by the United States
Government or any agency thereof. The views and opinions of authors expressed herein do not
necessarily state or reflect those of the United States Government or any agency thereof.
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The Regional Carbon Sequestration
Partnership (RCSP) Initiative
3
The RCSP is a DOE funded cooperative agreement of seven
regional Partnerships
Tasked with:-
Determining best geologicalstorage approaches for each
region
- Application and assessment of
storage technologies todemonstrate permanent storage
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Anthropogenic Test Project Background
The SECARB Anthropogenic Test is a fully
integrated Carbon Capture and Storage
project
CO2 is captured from SouthernCompanys Plant Barry (a 2,657 MW
coal-fired power plant)
A ~12 mile pipeline delivers the CO2to Denburys Citronelle Oilfield
The captured CO2is injected into thesaline bearing Paluxy formation
(~9,400 feet deep)
Approximately 114 thousand metric
tons of CO2were injected between8/12 and 9/14
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5
Stages of a Fully Integrated Project
Production andCapture
Transportation
Storage
Image: Science News
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6
Challenges
Getting all
their lawyers
to agree
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Capture and Compression
7
Plant Barry, Alabama
CO2 is captured from a 25 MW
slipstream from Plant Barry Flue Gas
- (2,600 MW system)
500 tonnes/day capture capacity
CO2is captured and compressed
using Mitsubishi Heavy Industries
compression technology
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8
Flue gas first reacts with KS-1 amine-based solvent
CO2is released from the solvent
CO2 is then compressed to a supercritical state (to 1500 psi)
CO2Capture
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9
Esposito, 2015
Capture Facility Aerial Overview
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Capture Plant Performance
10
*As of 12/16/2014
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Transportation Pipeline
11
Commissioned March 2012
4 (10 cm) carbon-steel pipeline
12 mile (19 km) run from Plant Barry property
to SECARB injection site.
1500 psi operating pressure
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Application of Directional Drilling
12
18 sections were directionally drilled to overcome infrastructure,wetland, and endangered species habitat (some up to 3,000 feet
long and up to 60 ft deep).
Pipeline buried 5 feet within surface vegetation maintenance
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13
Photos: Numerous Google Image searches
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Injection Site
14
CO2Booster Pump
300 HP variable speed electric
motor
130 stages (impellers)
4 suction 3 discharge
Inlet pressure 1300 psi outletpressure 3200 psi
Max rate approx. 14 MMCFD
CO2
Satellite link for communication
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Well Site Photos
15
Injection well with slick-line unit
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Injection Site Design, Drilling and
Completion Flow Chart
16
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Anthropogenic Test Gantt Chart
17
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UIC Class V Permit
Class V Experimental Injection Well permit
Short duration of injection (3 years) and modest volumes of
CO2
Characterization and modeling of stacked CO2storage
CO2injection under real world operating conditions
Demonstration of experimental monitoring tools and methods
Site closure based on USDW non-endangerment and CO2
containment demonstration (5-yr renewal)
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Study Area Background
The Citronelle Oilfield lies atopthe Citronelle Dome
What makes the Citronelle Dome amenableto CO2sequestration?
Well defined reginal geology from oil exploration
and production
Gulf coast sediments comprise excellent qualityreservoirs
A proven structural trap
Structural closure is exhibited in all directions
The limbs of the dome gently dip ~1
Plant Barry
Plant
Barry
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Gulf coast sedimentary strata
consist of extensive deposits of
high porosity and permeability
formations
CO2 is injected into thePaluxy Formation
The fields target oil
reservoir lies below the
CO2injection zone
Study Area Stratigraphy
CO2InjectionZone
Numerous confining units ofimpermeable marine shale and the
Selma Group 2,000+ ft chalk unitprovide confining zones to restrict
CO2migration
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21
Regional Seal Cross Section
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Storage Site: The Citronelle Oilfield
CO2 is injected at theSoutheast Unit in
Citronelle Oilfield
Structure Map of Ferry Lake Anhydrite
SubseaDepth
-10,300-10,350
-10,400-10,450
-10,500
-10,550-10,600
-10,650-10,700
-10,750-10,800
-10,850
-10,900
One injection well perforated in multiple zonesin the Paluxy Formation
Two in-zone observation wells perforated in theinjection zone
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!"#"$%&%#' ()*& +",-%
.%") !%#$%"0*,*&12 ! "# $%$
!3#3'*&12 4 & '(
5 678 5*'&")9% :#3$ ;)= 5*'&")9% :#3$ ;)
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MVA Program Drivers
!
Multiple lines of evidence to confirm CO2containment
Soil CO2flux and tracer monitoring
Crosswell seismic and VSP
Cased hole pulsed neutron logging ( in- and above-zone saturation)
Groundwater (USDW) monitoring
In- and above-zone pressure
! Assure non-endangerment of USDWs
Groundwater (USDW) monitoring
! Inform the reservoir simulation
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Monitoring Techniques
25
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Stacked Sand Perforated Zones
!"#$
%#&
%
'#(
!)#*
$$#$
!
!!
!"#$%&'"()
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MVA Elements and Frequency
!"#$%#&"&' ("#$)*+ ,&-.$/.*+ 0##&-*
(%*/'$"#/
!"#$%&'(%)
+(,%-.'/()
0/$.1
2)-**"3
!"#$ &$'(
)*"'+,-./0* 1.23$#+4 56!789
:;< 1'*=0>4//5
?@A ="$'20B 3*011'*0 C D"23"1#/#"+
E010*="#* &$'#, 1.23$#+4
F+G0D/#"+B /0230*./'*0 C 13#++0* $"41
:'$10 +0'/*"+ $"41
?*"11-0$$ 10#12#D
H0*/#D.$ 10#12#D 3*"$0 5H!:9
675/.%8/#$-*
7#1/*#I'/0,
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CO2Injection History
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Deep MVA Pressure Response
Downhole pressure data is a primary input to the history match
and plume model
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InjectionZ
one
Confining Zone
Pixelized difference tomography results without seismicreflection overlay showing positive velocity differencesin warm colors and negative differences in cool colors
First arrivals from repeat surveywere of sufficient quality to
produce a velocity difference
image (right) showing regions
where seismic velocity has
changed over time
Time-lapse difference image
indicates a decrease in seismic
velocity in the upper injection zone
of up to 3%, suggesting an
increase in CO2saturation
Time-Lapse Differencing Using the
Baseline and Repeat Velocity Tomograms
More importantly, no negative velocityanomalies are observed in or above
the confining unit!implying nodetectable leakage out of inj. zone
No significant negativevelocity anomalies
Decrease in velocity(negative anomaly)
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Predicted Radial CO2Plume Extent on
October 31, 2017 of 600 ft
Despite the high permeability of the formation and a gentle dip, there is nota substantial change in the plume extent in the three years following the
cessation of injection.
In fact, the plume extent has equilibrated.
This is due to injection into multiple zones, the limited injection volume and
injection shut ins which allowed for equilibration during the injection phase
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Questions?