| Authors |
C. Yang, K. Romanak, The University of Texas at Austin; R.M. Holt, The
University of Mississippi; J. Lindner, L. Smith, Mississippi State University;
R. Trevino, The University of Texas at Austin; F. Roecker, Y. Xia, J. Rickerts,
Mississippi State University; S. Horvorka, The University of Texas at
Austin
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| Source |
Carbon Management Technology Conference,
7-9 February 2012,
Orlando, Florida, USA
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| Preview |
Abstract
The early field project of the Southeast Regional Carbon Sequestration
Partnership (SECARB) was conducted in Cranfield Field, western Mississippi.
Injection was into coarse grained fluvial deposits of the Cretaceous lower
Tuscaloosa formation forming a gentle anticline at depths of 3300 m. CO2
injection started in July 2008, growing to ~23 wells with total injection rates
greater than one million tons/year. Focused monitoring programs of deep
subsurface and near-surface have been implemented at different study areas.
Here we present results of the near-surface monitoring program over a 3-year
period including shallow groundwater monitoring and soil-gas monitoring. A
general methodology for detecting CO2 leakage into shallow groundwater
chemistry is proposed. A set of geochemical indicator parameters can be
identified based on characterization of groundwater geochemistry over the
monitoring area and then further tested and validated with numerical modeling
approaches, lab experiments and field experiments. For the soil-gas monitoring,
a site (P-site) where there are a plugged & abandoned well, a nearby open
pit, and an engineered pad, representing a typical near-surface environment for
soil monitoring, was selected for detail study. The site was heavily
instrumented with different sensors for measuring soil-gas concentrations at
different depths, soil water content, matric potential, and weather
information. Three monitoring technologies were assessed: soil CO2
concentration measurements alone, CO2 flux measurements on the land surface,
and soil-gas component measurements. The results indicate that soil-gas
component measurements provide more reliable information for gas leakage
detection. The methodologies of near-surface monitoring developed in this study
can be used to improve monitoring CO2 leakage at other carbon dioxide
sequestration projects. This early field project is funded by the US Department
of Energy, National Energy Technology Laboratory as part of the Regional Carbon
Sequestration Partnerships program. SECARB is led by Southern States Energy
Board.
1. Introduction
The Southeast Regional Carbon Sequestration (SECARB) partnership is one of
seven Regional Carbon Sequestration Partnerships (RCSP) across the United
States and portions of Canada The US Department of Energy, began a 10-year
phase III program which includes two large volume injection projects in the
lower Tuscaloosa Formation, a formation representative of the Gulf Coast wedge:
the early test and an anthropogenic test (Hovorka et al., 2011; Litynski et
al., 2009; Rodosta et al., 2011). The “Early Test” began in July 2008, led by
the Bureau of Economic Geology and linked to a new CO2–EOR project conducted by
Denbury Onshore LLC at Cranfield Field in western Mississippi. The Cranfield
site is about 15 miles east to Natchez, MS. Tuscaloosa oil and gas production
at Cranfield began in 1944 with drilling of wells in the oil rim below a large
gas cap at the top of the structure (Mississippi Oil and Gas Board, 1966). By
1966, nearly all the wells were plugged and abandoned and the Tuscaloosa
reservoir was idle and in pressure recovery until Denbury began injection for
the EOR project.
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