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Carbon Sequestration Pilot
Studies and the LI-8100
Black Warrior Basin Central test site near Tuscaloosa, AL
Adam
Dayan, a graduate student at the University of Alabama,
performs surface
CO2 monitoring with the LI-8100 and
8100-103 at the Black Warrior
Basin test site.
Illustration of Black Warrior Basin Test Site. Observation wells
are spaced approximately 150 ft. apart. Surface monitoring for
CO2 seepage is performed with LI-8100; subsurface CO2
monitoring and groundwater testing is also conducted.
[click here for larger image]
LI-COR LI-8100 Soil CO2 Flux Analyzer with 20 cm Chamber
It is rare that a day goes by when we’re not presented with more
concerns of the effects on global climate change due to increased
greenhouse gas emissions. While experts may not always agree on the
solution, most agree that technology-based solutions should be evaluated
and ready should they need to be implemented. One technology, of a
diverse portfolio of options, is Carbon Capture and Storage (CCS),
also known as carbon sequestration. Most efforts involving CCS focus
on the capture of CO2 from large-scale stationary sources with storage
in deep geologic formations (i.e., depleted oil and gas fields, saline
formations, and unmineable coal seams), or terrestrial sequestration
(i.e., trees, soil, etc.).
A number of U.S. and international collaborations are currently underway
with the goal of providing safe, cost-effective methods for capturing
and storing greenhouse gas emissions. One of these collaborations is the
Southeast Regional Carbon Sequestration Partnership (SECARB), which encompasses
eleven states in the southeastern United States. Funded primarily by the
U.S. Department of Energy (DOE) with cost-sharing from select industry
partners, SECARB currently has a number of active field tests, including:
1) two coal seam projects, one of which is in the Black Warrior Basin Central
near Tuscaloosa, Alabama, designed to test the economic feasibility
of CO2-enhanced gas recovery (EGR) and geologic sequestration, and 2) a
deep saline formation study near the Victor J. Daniel, Jr. power plant,
a coal-fired plant near Escatawpa, Mississippi, where geologic storage
will be evaluated.
As a vital part of the SECARB initiative, a prominent
southeastern electricity provider, Southern Company (Atlanta, GA)
is participating in these field tests that will monitor for long-term storage
permanence and environmental safety, using both surface and subsurface
detection methods.
Phase I of the test project (2003-2005) consisted of
characterizing the geologic formations as to their potential as sources/sinks
for CO2. Phase 2, which is currently ongoing, consists of the characterization
and validation of a selected geologic formation and demonstration
of sequestration through small-scale CO2 injections that will take
place in early 2008; surface monitoring will continue for several
years following CO2 injection. In Phase 3, the upcoming deployment
phase, large scale injections will take place to verify technical, regulatory,
and economic feasibility of carbon sequestration with the continued
evaluation of monitoring protocols.
For surface CO2 monitoring, Richard
Esposito of Southern Company along with other SECARB team members
selected the LI-COR LI-8100 Automated Soil CO2 Flux System and 8100-103
Soil Chamber to perform baseline monitoring before CO2 injection, to establish
natural rates of CO2 flux at the test sites. After Phase 2 injection, monitoring
will continue for approximately two years. Currently, Esposito and
colleagues are using the LI-8100 and the 8100-103 20 cm Survey Chamber
to take weekly soil CO2 flux readings over a roughly 5 square acre area
in the Black Warrior Basin, as well as at Mississippi Power Company’s Victor
J. Daniel, Jr. power plant. LI-COR Scientists traveled to Alabama and Mississippi
to visit with SECARB team members to demonstrate the use of the LI-8100
system at both sites. After using the LI-8100 for several months,
SECARB team members have been pleased with the performance, according to
Esposito.
Black Warrior Basin
The coal seam formation lies about 1200 ft. below ground surface,
and contains coal bed methane (CBM). Methane production has tapered
off, and in some areas future plans call for production to eventually
cease unless some type of enhanced recovery is not implemented. The injected
CO2 will be evaluated from the perspective of both enhanced CBM recovery
and carbon sequestration. Since coal seams are generally thin (< 2m)
and shallow, in geologic terms (< 1000m), surface monitoring of the
seepage of CO2 through soils to the atmosphere is very important.
The Black Warrior Basin is estimated by Jack Pashin at the Geologic Survey
of Alabama to have a potential storage capacity of 342 million tons of
CO2 in coal seams alone. Coal seams are potentially a very safe candidate
for the geological sequestration of CO2.
Victor J. Daniel, Jr. Power Plant
This pilot test is designed to evaluate a large, deep saline formation
for CO2 sequestration. The target reservoir is the massive sand unit
of the Lower Tuscaloosa Formation. This brine formation lies nearly
two miles below the surface and is overlain by several regional low-permeable
cap rocks As with the Black Warrior Basin site, Esposito and his
colleagues plan to collect baseline soil flux data before injection
takes place and to monitor for several years after injection.
The
LI-8100
The LI-8100 System provides the capability to perform rapid survey
type CO2 flux measurements with either a 10 cm (8100-102) or 20 cm
(8100-103) soil chamber, as well as long-term unattended measurements
with either of two long-term chambers. In addition, the LI-8150 Multiplexer
connects easily to the LI-8100 to provide for connection of up to
16 long-term chambers, giving wide spatial and temporal sampling coverage.
A trace gas sampling kit is also available (p/n 8100-664) that allows air
samples to be collected from the same air stream used to measure soil CO2
flux in the LI-8100’s soil chamber; the concentration of the gas species
for those collected air samples can then be analyzed in the laboratory
with gas chromatography or mass spectroscopy methods. If you would like
to learn more about how the LI-8100 can help in your research, call one
of our Application Scientists at LI-COR, or visit www.licor.com/8100.
Storage
Model
How Carbon Sequestration Works
- Depleted oil and gas fields are proven CO2 traps; in addition, their
geology and reservoir
characterization is generally well known. Oil fields offer the
opportunity for enhanced oil recovery (EOR) which helps off-set
the costs of sequestration operations.
- Deep saline formations contain
pore spaces filled with salt water and can possess very large capacity
for CO2 storage due to high porosity and permeability. Saline formations
are also often overlain by impermeable cap rocks that can make
them very safe storage sites.
- Unmineable coal seams are well assessed
and have a large capacity for CO2 storage; they are sometimes thin
and shallow, however, which makes monitoring important for the
protection of potable ground-water supplies and surface ecosystems very
important.
- As CO2 is pumped into the ground, it is trapped in the pore
spaces between the rocks. Depending on the characteristics of the
rocks and fluids, CO2 can be trapped in any of four ways:
- Structural & stratigraphic trapping – CO2 is initially more
buoyant than water, and rises to the top of the rock formation where
it is trapped by an impermeable seal or cap-rock such as shale or
anhydrite.
- Residual trapping
– CO2 becomes trapped as an immobile phase within the dead-end
pore spaces of the rocks, much like a sponge.
- Solution trapping
– CO2 dissolves into formation fluids such as into brines,
where it becomes heavier than the water without CO2, and thus
sinks to the bottom of the formation.
- Mineralization – CO2 reacts with naturally
occurring divalent cations to become part of the solid mineral
matrix and forms stable carbonate minerals.
For More Information
LI-8100 Automated Soil CO2 Flux System
www.southernco.com
www.doe.gov
www.netl.doe.gov/technologies/carbon_seq/partnerships/partnerships.html
www.secarbon.org
portal.gsa.state.al.us/CO2/SECARB2/secarb2.htm |
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